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UNITED STATES COAST GUARD

OCEANOGRAPHIC REPORT No. 11

CG 373-11

DATA LIBRARY

Woods Hole Oceanographic Institution

OCEANOGRAPHY OF THE GRAND BANKS REGION OF NEWFOUNDLAND IN 1965

UNITED STATES COAST GUARD

OCEANOGRAPHIC

UNITED STATES COAST GUARD OCEANOGRAPHIC UNIT

DMA LIBRARY

Hoods Hole Oceanographic in*"

REPORT No. 11

CG 373-11

OCEANOGRAPHY OF THE GRAND BANKS REGION OF NEWFOUNDLAND IN 1965

Ronald C. Kollmeyer Thomas C. Wolford Richard M. Morse

WASHINGTON, D.C. $ JUNE 1966

Abstract

Three oceanogi'iipliic surveys were conducted m the vicinity of the Grand Banks of Newfoundhmd ui support of International Ice Patrol operations 1965. Measiu-enients of temperature ajid salinitj' obtauied from serial Nanseii bottle observations were used to determine tlie dyinimic topography, a principal factor m studyLng the most probable drift of icebergs endangering shipping Lu this area. A short check s»n'\'ey of one standard section was conducted during the season in order to detect any short term changes in the Labrador Current. Subsequent analysis of selected oceanographic sections was ac- complished to calcidate the voliune flow and heat transport througli these sections. In addition, an isentropic analysis was undertaken in order to make a comparison with the circulation deduced from the dynamic topography.

A change iu vertical sampling technique was attempted in order to define more acciu'ately the ma.ximum and minimum points in the distribution of temperature and salinity.

Studies of iceberg deterioration and specific drift factors were hiitiated during Ice Patrol 1964 and were conthuied during 1965 with some increase in emphasis.

Contents

Page

Abstract "i

Oceanography of the Grand Banks Region of Newfoundland

in 1965 1

Introduction 1

Narrative 1

General 1

Additional projects 2

Instrumentation 2

Personnel 3

Dynamic height charts 3

General 3

Treatment of data 4

Chart discussion 4

General circulation 5

Volume and heat flow 5

Dynamic height changes 5

Isobaric slope 6

Eastern banks and slope controls 6

Circulation response 7

Future work 8

Isentropic analysis 8

Basic concepts 8

Chart preparation 9

Chart analysis 9

Isentropic and geostrophic comparison 10

References 12

Illustrations (A) 13

Tables (A) 38

Interim reports 41

Iceberg deterioration 41

Introduction 41

Previous \\ork 41

Theoretical analysis 42

Statistical approach 47

Data collection 49

Data correlation ^0

References ^1

Illustrations (C) 53

Tables (C) 64

Papers 65

An examination of vertical sampling methods and their

influence on dynamic height calculations 65

Introduction 65

Sampling methods 65

Continvious sampling devices 68

References '"

Illustrations (D) ''I

Tables (D) 79

Tables of oceanographic data "^

Illustrations

Figure Page

1 A. Trackline and station array 13

2A.-5A. Dynamic topography charts, Grand Banks of

Newfoundland 14

6A. T-S plot of water masses, vicinity of the Grand Banks of

Newfoundland 18

7 A. T-S plot of Labrador Current stations 19

8A. Dynamic heights along section U 19

9 A. Temperature and salinity distribution along section U_ _ 20 lOA. Temperature and salinity distribution in trough area of

section U 21

llA. Velocity distribution along section U 22

12A. T-S plot of stations 9259 and 9388 23

13A. Mean T-S plots of stations located on the Grand Banks. 24 14A. Volume flow variation and Grand Banks salinity change

for section U 24

15 A. -23 A. Isotherm contours on various sigma-t surfaces 25

24A.-26A. Isotherm contours at selected depths 34

27A.-28A. Vertical distribution of salinity along the core of

the Labrador Current 37

Tables

I A. Volume and heat flow data for section U 38

IIA. Annual dynamic heights and volume flow for section U,

1949-64 39

Iceberg Deterioration Illustrations

Figure Page

1C.-5C. Hourly meteorological observations 53

6C. Blackbody heat radiation at various temperatures 55

7C. Plan view of iceberg showing rotation during photo- graphic sequence 56

SC.-9C. Sample round of iceberg photographs 57

lOC. Dye spots on iceberg 59

lie. Example of measurement of iceberg from photograph. __ 60

12C. Example of topographic iceberg map construction 61

13C. Topographic map of iceberg, at beginning and end of

study 62

14C. Photographs showing wastage during the study period. 63

Tables

IC. Estinuited deterioration time for various sized icebergs.. 64

An Examination of Vertical Sampling Methods and Their Influence on Dynamic Height Calculations

Illustrations

Figure Page

1D.-4D. Vertical distribution of temperature and salinity for

stations 9400, 9252, 926S and 9270 71

5D.-6D. Vertical distribution of temperature, salinity and

density for station 9244 74

7D. Dynamic height errors between two stations and the

residting calculated current velocity error 75

8D. Vertical distribution of temperature, salinity and specific

volume anomaly for station 9399 76

9D. Example of error introduced by straight line numerical integration of a smooth curve of specific \-olume anomaly 76

lOD.-llD. Vertical distribution of temperature, salinity and specific volume anomaly for stations 9399, 9386 and 9248 \ 77

12D. Vertical distribution of specific volume anomaly and the resulting error from straight line nun)erical inte- gration of the curve 78

Tables

ID. Comparison of the nmnber of Nansen bottles used be- tween standard depth and gradient sampling 79

IID. Standard deviations between standard depths and

gradient sampling dynamic height computation 79

HID. Errors in dynamic heights determined from the meas- urement of areas between straight line numerical integration and a smooth curve 79

IVD. Instrument measurement error 80

VD. Thermometer comparisons 80

Oceanography of the Grand Banks of Newfoundland in 1965

by Ronald C. Kollmeyer, U.S. Coast Guard

Introduction

The Ice Patrol surveys during 1965 were con- ducted in a son^e^^■hat different manner from the standard sampHng routine of the past. A new oceanographic station array was established paralleling the old standard surveys in some areas and diifering considerably in others. Figure lA shows the old trackline of the southern survey and the new trackline used in 1965. The purpose of revisuig the trackline was to reach a compromise between adequate sampling of the area while keeping the survey as synoptic as possible. The new station array included 62 stations compared to 97 stations of the previous method and allowed completion in 7 days in lieu of 14 days.

The standard sections of previt)us years have retained their designations in the new station array despite their relocation. Their new positions are not significantly different and allow comparison with historical Ice Patrol data. Figure lA shows the section designations under the new and the old station arrays.

The standard treatment has been given the data as in past years with the exception of the volume and heat flow comparison for the standard sections. Annual volume and heat flow com- parisons lose their significance imless adjusted for time. They are virtually meaningless unless compared to flow buildups and declines irrespective of the specific calendar survey dates. Past data indicates the major buildup and decline in the \-ohune flow of the Labrador Current can occur anytime during the spring. This requires that the data must be adjusted in time by volume flow maximums in order to make comparisons on an annual basis. It will be shown hi the following sections that monthly surveys will not provide the information required to define the accelerations of this system. Past data analysis techniques have not even shown the volume flow trends which would allow an annual time matching of the flow peak or peaks.

The sampling of the water mass was accom- plished by first conducting an electronic bathy- thermograph lowering to 410 meters at each station. Nansen bottles were then hung at levels that would obtain temperature and salinity data wliich would best describe the water column. The merits, results, and comparisons of this technique are examined in a following paper.

Some methods of presentation, new to Ice Patrol, have been attempted in an effort to analyze the data more effectively. Ultimately, they may lead to an understandmg of the cuTulation m the area which will allow formulation of better samplmg techniques and possible prediction of current changes necessary for the solution of the berg tracking problem .

NARRATIVE

General

Three oceanographic cruises were conducted by USCG cutter Even/reen, a 180-foot tender class oceanographic vessel, in support of the Interna- tional Ice Patrol during the spring and summer of 1965. A summary of the location and extent of each cruise follows.

The first cruise began on 30 March 1965, with the occupation of Evergreen Station 9235 on the southwestern slope of the Tail-of-the-Banks and proceeded northward with serial stations ter- minating at station 9296 on the Grand Banks west of Flemish Cap on 7 April 1965. This cruise was designed to delineate the three principle water types in the area, namely, the Labrador Current Water, Mixed Water, and Atlantic Current Water, and to provide, within 12 hours of observation, vertical temperature distribution and dynamic heiglit at each station to commander, Interna- tional Ice Patrol. Serial stations 9253 through 9260 were reoccupied as stations 929S through

9306 on 11 and 12 April 1965, and referred to herein as tlie check survey to detect any changes in the horizontal and vertical distribution of water mass types and associated dynamic prop- erties. The first cruise was terminated on 12 April 1965. During the second cruise, which lasted from

24 April to 12 May 1965, Evergreen occupied serial stations 9313 to 9351 to pi'ovide a dynamic topo- graphic chart of the water over the northeastern slope of the Grand Banks. These stations, which were occupied duruig the period 7 May to 10 May 1965, were in eastward oriented sections termi- nating at the latitude of Flemisli Cap and rep- resent an attempt to define any easterly branch- ing of the Labrador Current.

The thu'd cruise began with the occupation of station 9352 on 19 May 1965. A line of serial stations running east to the northern tip of Flemish Cap was occupied to provide overlap with the sections completed on the previous cruise. Serial stations weve occupied d(jwn to the Tail-of-the- Banks which approximated those occupied during the first cruise. Occupation of station 9408 on

25 May 1965, completed the survey for the season.

Additional Projects

As a part of a continuing study of iceberg drift and deterioration, a series of photographs, sup- ported by sextant angles and range finder dis- tances, were taken at 30-degree intervals around a berg to permit detection of mass wastage. These observations were made at approximately 24-hour intervals during the period from 26 April to 6 May 1965. A track of the drift of the same berg was maintained by hourly navigational positions ob- tamed by radar reference to a buoy from 26 to 29 April 1965. Experimental dye-marking of the berg selected for these studies was also performed.

A study of the effect of pH of seawater upon its electrical conductivity, as utilized in salinity measurements witii the inductive salinometer, was conducted during the first cruise as was a study of the possibility of classification of surface water type by Forel Color Scale. Inconclusive results were obtained and no data is presented.

During the first cruise an investigation was made of the steady state conditions presumptive in geostrophic circulation by means of analysis of electronic bathythermograph (ELBT) traces. The traces obtained gave indications of gross changes in the thermal structure over all periods covered by the study (6-minute to 1-week scales).

Instrumentation

Teflon-lined water sampling bottles of the Nansen type, manufactured by the Ballauf Manu- facturing Co. or the United Machine Co., were used during each cruise. Temperatures were measured with protected deep-sea reversing ther- mometers mostly of Richter & Wiese manufacture, but with some manufactured by G. M. Manufac- turing Co., Kahl Scientific Instrument Corp., and Walter H. Kessler Co., Inc. Thermometer per- formance was continually monitored by pairing and intercomparison. The following standard de- viations from the accepted paired average reflect thermometer performance during the season.

Cruise	Standard devia- tion C° C)	Number of comparisons
1st		±0	005	342
2d		±	007	177
3d		±	008	294

Depths of observation are based on wire angle geometry and thermometric computations from unprotected deep-sea reversing thermometers. The salinity of each seawater sample collected was measured with an RS-7A inductive salinom- eter manufactured by Industrial Instruments Corp.. Forty-one replicate salinity samples were intercompared using a Hytech Corp. 6210 in- ductive salinometer which yielded a standard deviation of 0.007°/«.. The salinity determination procedures used were those described by Morse (1963). It is considered that the precision of measurement was within 0.005 /= and that the accuracy of the reported salinities is ±0.01 / = .

Depth to the bottom at each station was de- termined with an Alpine Precision Echo Sounder Recorder (PESR).

All observed data were processed by a PDP-5 digital computer manufactured by the Digital Equipment Corp. The computer was programed for the correction of reversing thermometers and determination of thermometric depth; computa- tion of sigma-t, specific volume anomaly and dynamic height integration; and computation of volume transport. The programing of the com- puter lias been described in greater detail by O'Hagan (1964), and Morse and O'Hagan (1964).

At eacli station a Hylech Corp. electronic bathytiiermograph (ELBT) Model 480 MOD I,

way used to determine the vertical thermal gradient to 400 m. to facilitate selection of sam- pling depths for the subsequent Nansen cast. As a result vertical thermal gradient sampling rather than standard depth sampling was accomplished.

A small shipboard fabricated marker buoy of light construction, floated by 12 inner tubes riding to 570 fathoms of nylon and dacron line secured to a 10-foot length of chain and a 75- pound danforth anchor was used in conjunction with the Hytech ELBT for a preliminary and cursory internal wave study. This buoy was lost due to a loss of floatation.

For iceberg drift studies a Geodyne Corp. toroidal fiberglass buoy equipped with a tripod mast, antenna array, and Motorola Co. radar transponder, Model SST-133X, was moored with a fixed bridle, swivel, ballast ball, 120 fathoms of 1 inch braided nylon, one shot (15 fathoms) of one-half inch anchor chain and a 75-pound dan- forth anchor in a reference position. Evergreen's. radar was used hourly to determine navigational positions and the drift track of the berg with refer- ence to the buoy. Horizontal control is estimated to be valid within 200 to 300 yards. The buoy was an unqualified success, operating at radar ranges of up to 12 miles and up to 70 hours on a single charge of the two serial 12 volt standard truck type, lead acid cells.

Twin drogues made of 28-foot cargo parachutes suspended at 10 and 70 meters depth from a buoy of truck type inner tubes and bamboo poles, and equipped with a radar reflector and light were used as an adjunct to the iceberg drift study for acquir- ing subsurface current information.

Personnel

The oceanographic work of the first and second cruises was under the direction of Lt. Comdr. Richard M. Morse, USCG who was assisted by Lt. Comdr. Ronald C. Kollmeyer, USCG; Mr. Thomas C. Wolford, oceanographer, USCG; Mr. Robert B. Elder, oceanographer, USCG; and Ens. Melvin S. Swanson, USCGR. Lieutenant Commander Kollmeyer directed the third cruise assisted by Mr. Wolford and Ensign Swanson. Technical assistants for the entire season were David C. Lockhart, aerographer's mate first class and Edward S. Olszewski, sonarman second class. Dennis L. Noble, aerographer's mate first class; John T. Nichols, sonarman second class; and James D. Brower, aerographer's mate third class assisted during the first and second cruises; and

William H. Harrell, sonarman first class; William E. Heller, aerographer's mate second class; and David J. Wood, sonarman second class assisted during the third cruise.

DYNAMIC HEIGHT CHARTS

General

The dynamic height topographic charts of the sea surface, for the Grand Banks region of Newfoundland, are presented in figures 2A through 5A. They were constructed from data obtained on the first, check, second, and third surveys conducted during Ice Patrol 1965.

The first and third survey charts, figures 2A and 5A, represent data obtained using the new station array. They describe the surface currents, their velocities and directions, as determined from dynamic computations. The check survey, figure 3A, consisting of section U and a portion of the the section immediately to the south was obtained appro.ximately 1 week after the occupation of these same stations on the first survey. The purpose of this immediate reoccupation was to examine short term changes that may occur in the flow pattern of the Labrador Current not de- tected in the past due to intervals of a month or more between surveys.

The second survey chart, figure 4A, is a sup- plemental survey of the northern area, adjacent to the main region of interest. It provided the characteristic description of the easterly flow and southward turning of the Labrador Current prior to its entering the area of major interest.

The third survey, figure 5A, describes the circulation in the area of major interest during the late spring. Flow patterns are quite different than found in early spring as seen in figure 2A.

The designated section U is noted on figures 2A, 3A, and 5A. This section includes the most interesting flow patterns of the region. Starting at the westernmost end of the section, the typical high stand of Banks water is always observed which grades into the main southward flowing stream of the Labrador Current. Just to the east of this current, a trough or low stand of mixed water is found with the northward flowing Atlantic Current fonning the eastern boundary of the section. The circulation changes which oc- curred in this section between the several surveys will be discussed in detail in the following sections.

Treatment of Data

Numerical integration of the anomaly of specific volume, based on the temperature and salinity distribution obtained at each station, was accomplished on shipboard using a Digital Equipment Corp. PDP-5 computer. All deep sea reversing thermometers were corrected by the computer thus eliminating all hand com- putations. Actual observations were used as data inputs for the computation of dynamic heights. No scaled data for standard depths, other than the 1,000-meter reference level, were used in the computations. The programs used are described by O'Hagan (1964).

Daily transmissions of the computed dynamic heights for each station occupied, along with the temperatiu-e distribution down to 150 meters, were made to Commander, International Ice Patrol, Argentia, Newfoimdland. This allowed the immediate construction and use of portions of the sea surface topography charts for iceberg drift prediction.

Chart Discussion

The first survey chart, obtained during 30 March to 7 April 1965, figure 2A, shows the Labrador Current flowing south along the 100-fathom curve. At the Tail-of-the-Banks, part of the current flows west and another portion recurves to the east forming a pool of quiet water. Some fila- ments in this area turn and flow northward con- tributing to the mixed water area of the trough. This trough area is the region of current reversal where the Labrador Current floM's south on the western side and the Atlantic CiuTent flows north on the eastern side. The water in this region has a low specific volume. It is made up of a mixture of Labrador Current water and Atlantic Current water giving a water mass characteristic between the two as seen in the T-S curve of figure 6A. This mixture produces a water mass of a character- istically low dynamic stand compared to the much higher topography towards the Banks and towards the Atlantic Current to the east. For this reason it is referred to as the low or trough of the circu- lation pattern. This is a characteristic feature generally found ui the vicinity of tlie 1,000-fathom curve and sometimes extends as far south as the Tail-of-the-Banks.

The meanders of the Atlantic Current outlhie the pool of water formed to the east of the tail. This appears to be supplied by the water oi the

Labrador Current spilling into the area and is a normal circulation feature found in past years.

An area of contour uncertainty exists in the northeast part of the current chart, figure 2A, at 46°30' N., 48°00' W. Insufficient data in the area prevents the determination of flow direction from dynamic topography alone and will be discussed ui the following section in isentropic analysis.

The check survey chart, obtained during 11-12 April 1965, figure SA, represents an interesting reoccupation of section U within 9 days ol the first occupation. The 971.1 dynamic meter streamline, nonexistent in that area on the first survey, was found. In addition, the 971.0 dynamic meter streamline was found to have shifted east by about 30 miles, while the trough feature shifted eastward less than 10 miles resulting in a swifter flowing Labrador Current.

The second survey, 7-10 May 1965, figure 4A, shows the Labrador Current tracking along the 100-fathom curve with some lateral filaments spilling onto the Banks as it turns to the south. The 971.0 and 970.9 dynamic meter streamlines are in much the same position, passing through section F, as on the first survey. The 971.1 dynamic meter streamline was not observed, however, contours up to 971.08 dynamic meters ( are drawn and indicate that lighter water was further up on the Banks. This was also reflected in figure 3 A, the check survey, where 971.1 dynamic meter streamline appeared well up on the Banks in section U.

The third survey, 19-25 May 1965, figure 5A, showed the Labrador Current as a strong uniform flow along the 100-fathom curve from 47°30' N. to 43°00' N. The characteristic trough was greatly elongated and the pool of quiet water found during the first survey was missing. The streamlines of the Atlantic Current tended to turn north at the Tail-of-the-Banks \nthout describing any low velocity or stationary pool of A\ater. A cyclonic eddy occurred to the east at 44°00' N., 46°00' W. This eddy or gyre ex- hibited water cliaracteristics similar to those found in the pt>ol of water, described by the first survey data, at the Tail-of-the-Banks. The eddy appeared to be the residt of the pinching off of tlie pool and its subsequent movement to the north- east. This pinching ofi" of an eddy is a phennom- ena exhibited by Gulf Stream filaments and de- scribed by Fuglister et al. (19-51). Insufficient

data prevents a detailed description of this eddy, however, its presence is apparent.

GENERAL CIRCULATION

Volume and Heat Flow

A summary of volume flow through the desig- nated section U is given in table lA. The compu- tations were made by a modified method described by Jakhelln (1936). It is interesting to note that the volume flow through section U doubled during the 9-day interval between the section occupation on the first survey and the check survey. The volume flow then remained relative- ly constant between the check survey and the third survey. It appears that a radical change took place on the Banks between the first and check surveys. Not only is 'a greater volume observed on the check survey but a significantly warmer mean temperature and higher minimum temperature is also found. The third survey volume flow remains high; however, the mean temperature, minimum temperature, and mini- mimi salinity drop below the first survey values indicating that the Labrador Current is exhibiting its full flow characteristics.

The general water characteristics of the Labra- dor Current between the first and third surveys are quite different. Figure 7A shows a T-S plot of the Labrador Current. The points are mean values (for the given depths) of all stations on each of the first and third surveys situated in the southward flowing stream. This is similar to figure 6A showing the Labrador Current character- istics for the entire season. On the first survey, the water was less stratified than during the third survey. This is indicated in figure 6A by the smaller sigma-t change across the same depth interval on the first survey tlum on the third, particularly from 100 to 150 meters. A com- parison of the water mass between the two surveys shows the third survey found colder, less saline water down to a level between 100 and 150 meters and then a sharp density increase with warmer, more saline water below 150 meters. This density gradient defines the deptli limits of change of the Labrador flow. This change at depth of the density structure between surveys can be traced to spring changes in the east-west slope of the (7, surfaces resulting in greater stratification, and will be treated more fully in the following chapter on isen tropic analysis.

Dynamic Height Changes

A surface dynamic height plot of tlie stations of section U on the first, check, and third sur- veys, figure 8A, shows that in 9 days a change in height of the inboard station occurred without a significant change in the trough dynamic height. Tlie trough is located in water which is a mixture of the Labrador Current and the Atlantic Current and does not show the extreme characteristics of either current system. Apparently the abrupt change in elevation of the stations on the Banks and the mcrease in volume flow is related to the change of water characteristics on the Grand Banks and continental slope as shown on the temperature-salmity sections, figure 9A. These sections were constructed from the temperatures and salinities of stations in section U on the first, check, and third surveys.

The temperature and salmity distributions of section U durmg the three occupations are clearly shown in figure 9A. The first survey reveals that the cold water is generally confined to the surface along with reduced salmity required for stability, probably reflecting the results of disintegrating sea ice. The check survey shows colder water of low salinity to be subsurface and connected to a colder water mass on the Banks. The density of this water is less than the first survey water at the same depth indicating that it probably did not result from surface sinking. By the third survey the situation had again changed showing a core of cold water off the Banks, with even lower salinity than cold water of the previous survey. The salinity decreases as the Banks are approached indicatmg that different water mass has also arrived there. The temperature of the Banks water has also increased above what it was earlier, but this can be explained by the warmer air temperatures as summer approaches.

Because of the method ol computing currents in the shallo\\' Banks water, the deeper \\ater areas to the east along the slope and below the core of the Labrador Current greatly influence the dy- namic height on the Banks. This is the water located between stations 9252 and 9258 ; 9303 and 9304 ; 9390 and 9389 ; on the first, check, and third surveys, respectively, of figure 9A. Between these stations the water shows a definite salinity re- duction with time. First, an increase in the amount of water of less than 34.07oo was observed during the check survey. This is followed by an increase in the amount of water of less than

33.5°/oo and the arrival 33.0°/oo water found during the thu'd survey. The salinity reduction m this area and on the Banks would cause the calculated elevation of the sea surface as the Banks are approached. In the trough area, the dynamic height change between the first survey, station 9259 ; and the check survey; station 9305, as shown in figure SA, is almost negligible. A significant change is detected on the third survey. Exami- nation of the temperature and salinity curves of figure lOA discloses that significant salinity changes were not found in this area until the third survey, when both s^ reduction in salinity and temperature was observed. Because the trough stations showed little elevation change over the short period between the first and check surveys, it would seem that the flow of the Labrador Current at this time affected or was affected by the characteristics of the Banks and adjacent continental slope water.

Isobaric Slope

The Labrador Current can be thought of as an edge phenomenon, flowing as the result of steady state requii'ements of the sea height difference between light, low salmity water on the Grand Banks and slope and the heavier, higher salinity water located off the slope between the Labrador and the Atlantic Current. This edge phenomenon can be obsers^ed from the velocity profiles and isotherms for the Labrador Current m section U, figure 1 lA. It can be seen that the fastest flowing water is not necessarily the coldest, but grades colder and less saline as the Banks are approached. Thus, a wedge of low tempei-ature, low salinity water overrides mixed water of less scAcre char- acteristics. Because light-cold water and heavy- warm water are anomalous relationships, it is apparent tluit sainiity cojitrols the density in this current regime.

Figure SA sliows the section U plot of the dynamic heights indicating the gross changes that occurred over the periods between the surA-eys. Note that only snudl changes occurred on the Banks between the check siu'vey and tlie third survey which were separated by more than a month. Observe also the gradual elevation of the trough station during the two periods, leading to the s])eculati()n that this mixed water is slowly changing its characteristics as the spring pro- gresses. However, this cannot be conclusively proved because the location of tiie lowest station, in dynamic height, does not mean thiit it was

actually situated at the lowest sea surface eleva- tion point. Figure 12A, a T-S plot from stations 9259 and 9388 of the first and third surveys in the mixed water trough shows a density decrease with time above 600 meters, with the reduced salinity causing the density to decrease even under condi- tions of decreasing temperature at mid-depth.

The changing isobaric slope between the two water masses allows greater or lesser volumes of water to be transported. This slope can be ad- justed either by a changing of the dynamic height of the trough (mixed water) or the surface dynamic height on the Banks.

The changes observed between the survey periods leads to the hypothesis that an increase in the dynamic height of the water on the Banks and slope caused a swifter warmer current to flow during the check survey than during the first survey. This increase of the height of the water on the Banks could be caused by the influx of arctic and sub-arctic melt water from the north. It could be assumed here that we were observing cause, adjustment, and affect. This means that the increase in elevation of water on the Banks and slope, with a resulting water volume flow- increase, causes entrainment of the existing water in the area. This slope water woidd then become colder with the arrival from the north of greater volumes of cold w-ater to fulfill the mass continuity requirements being satisfied by entrainment. Alternately, the warmer mean temperatures ob- served during the check survey could be the result of linearizing the velocity data between stations thus causing an apparent volume flow in warmer water. The small reduction of the volvune flow, as seen on the third survey, would result from the greater elevation of the sea surface in the trough area due to the eventual mixing of these more severe water properties as the water transits to the Tail-of-the-Banks and then back up through section U.

Eastern Banks and Slope Controls

The concepts discussed above are postulated from only three sections and need further work to be completely substantiated; however, the spring fresliening of the Grand Banks water is a fact and its influence on the mixed water and the resulting slope of llie sea surface between tiie two water masses is a logical outcome. It is apparent from a fiu'tlier amilysis of the data, that tlie water on the Grand Banks changes as the season progresses aiul wovdd require some form of ad-

justment and continuity of flow in the current or the mixed water laying further to the east.

Figure 13A is a T-S plot of the more westerly stations on the Banks in 1965. The figure in- cludes north-south lines of the first, check, and third survey stations, and two second survey stations which straddle the northern end of the first and third survey lines. Each station is represented by a point determined from the sta- tion's average salinity and average temperature, the use of which are permitted by shallow depth and homogeneity of the water. The stations taken on each of the separate surveys are con- nected by lines for clarity. Although these sta- tions are not centrally located on the Banks, they are representative of the Banks water slightly mod- ified by the swifter flowing current to the east. The salinity of the water on the Banks during the third survey (stations 9353 to 9403) has been re- duced by about 0.2%o from the first survey (sta- tions 9238 to 9296). As expected, the water is warmer to the south because of warmer air tem- peratures.

The stations occupied during the second survey, numbers 9342 and 9343, whose locations match stations 9296 of the first survey and 9352 of the third, show that the low salinity water had already arrived at the northern end of the Grand Banks when the second survey was made. On the check survey, the salinities of stations 9301 and 9302 fall nicely between the first and third survey sta- tions of similar location, stations 9255, 9256 and 9373, 9391 respectively. Salinity decreases were observed at both stations while mean temperatures remained about the same. A period of only 9 days separated the check survey stations from the first survey stations, however, the salinities had already lowered by half of the total change foiuid during the third survey, 7 weeks after the first survey.

The above findings tend to indicate tliat the pronounced water characteristics indigenous to the Labrador Current in tlie spring, arrive rather abruptly. This is also supported by the volume flow data from tlie check survey. This is contrary to previous beliefs that gradual temperature and salinity changes take place during the early spring and that the changes w liich occur in tlie current system occur over a period of months. Rather, it is apparent tliat tlie time scale of change is more on the order of 1 to 2 weeks and perhaps less.

Circulation Response

The abrupt changes in water characteristics and dynamic heights that occurred on the Banks and slope were in response to the arrival of the colder, less saline water from the north. It is reasonable to conclude that because these changes occur on the Banks and slope first, a certain period of lag is to be expected prior to the arrival of this water in the trough area. The water in the Labrador Current must circuitously flow down toward the Tail-of-the-Banks before its arrival in tlie trough area. As pointed out above, the dynamic height of the trough area during the three surveys showed a gradual increase in elevation. Figure 8A shows that although an abrupt change had occurred in the dynamic height of the Banks and slope water between the first and the check survey, the trough station on the check survey changed little in dynamic height. Conversely, the Banks station on the third survey changed little from the check survey while the trough station exhibited a considerable change. This leads to the conclusion that the low salinity water observed in the main stream of the Labrador Current during the check survey had not had suffi- cient time to complete the trip to the trough area and influence the water type there. However, on the third survey significant changes in the water properties above 400 meters occurred. Figure IDA indicates these temperature and salinity changes which occurred in the trough area during the survey intervals. Between the dates of the check survey and the third survey light, low salinity water arrived at the trough. The effect was to raise the elevation of the trough and thus reduce volume flow.

If section U is examined over a year (figure 14A), limited correlation appears to exist between the change in mean salinity of the Banks' water and the volume of water flowing south. An exact correlation cannot be made here because of the influence of temperature on the water's specific volume, the time lag, and unknown mixing proportions which tend to modify the elevation of the water in the trough area. This is evident from the volume reduction that occurred on the third survey even though tlie Banks station decreased in salinity and liad a higher dynamic height. If the check survey had not been con- ducted, the rapid rise of volume flow would not have been observed and the portion of figure 13A for 1965 would have looked hke that for 1964. This kink in the volume flow curve for 1965

tends to indicate that the adjustments were caught prior to any low saHnity influence and subsequent elevation of the trough region as observed on the third survey.

Data of the Banks salinity and volume flow from past years, presented in Table IIA, do not show good correlation with the concept of salinity decrease on the Banks and increase in volume flow. These data are from surveys which were separated m time by a month or more and hence cannot be expected to show a correlation due to the lag time between the arrival of the low salmity water on the Banks and the mixing of the water in unknown proportions in the trough area. The only way to observe this postulated salinity de- crease and volume increase is to start the survey before the water of lowered salinity completes its swing towards the Tail-of-the-Banks and then north to the trough area. At a current velocity of 1 to 2 knots, less than a week is required. Lateral mixing in section U is held to a minimum because of the steep east-west slope of the a, surfaces. This will be discussed in further detail in the section on isentropic analysis. As the current passes the trough area, some alteration of the properties take place in the trough; how- ever, the greatest changes occur while the water completes its trip from north to south and then north to the trough region. Data of previous years do not provide any means for determming short-term volume flow tendencies or the rate of change of the salinity of the Banks water. The significant flow changes observed durmg 1965 \\ere the result of closely timed, repeated sections.

Future Work

A greater understanding of the salinity-volume flow relationships would enable a temperature- salinity monitoring system on the Banks to uidi- cate salinity reduction and volimae changes occurring to the Labrador Ciu-rent. These could liave implications in iceberg drift prediction.

Weekly fluctuations oi the Labrador Current might be superimposed on seasonal variations which woidd tend to alias the data collected at monthly intervals thus rendering year to year comparisons misleaduig. Atten^pts will be made during the spring of 1966 to more accurately define the flo\\ changes and to determine wliether or not these changes are of a short- or long-term duration.

ISENTROPIC ANALYSIS Basic Concepts

A method of observing water movements and changes in property distribution for comparison with dynamic heights is desired. It would be advantageous to have such a comparison in the hope of verifying and eliminating ambiguities in dynamic height contour charts. Isentropic analy- sis provides this independent method for deter- mining water movement. Rossby et al. (1937) pioneered isentropic analysis of the atmosphere. They showed that atmospheric specific humidity proved valuable for observing the distribution of identifying properties on surfaces of equal density. Parr (1938a) and Montgomery (1938) applied a similar technique to the oceans and found it extremely useful in tracing water mass source and movements. Parr (1938a) made direct compari- sons of isentropic charts with Ice Patrol dynamic height charts and indicated that true water move- ments at the southern end of the Grand Banks, Newfoundland, could better be deduced from the analysis of water circulation on density surfaces. Montgomery (1938) extended his analysis to water movements of the upper layers of the southern North Atlantic Ocean and deduced source loca- tions of the various density layers.

The implementation of isentropic analysis calls for the determination of the surfaces of constant entropy. According to Montgomery (1938), this surface is best approximated by the surface of constant potential density which at pressures of less than 1,000 decibars is equivalent to surfaces of equal sigma-t. This appro .ximation is necessary because no surfaces exist in the ocean along which the mi.xing of water masses can take place without altering the mass distribution and therefore the entropy or energy level of the system.

A sigma-t or quasi-isentropic surface presenta- tion is useful because flow patterns on these surfaces represent the nearest approach to the true conditions of movement. In addition, the currents tend to flow parallel to the contour lines of the sigma-t surface therefore providing informa- tion on the direction of movement. These are axiomatic truths because of the hydrodynamic fact that flow will take place along levels of equal density unless active mixing alters the energy levels. Some departure will take place because of the effect known as cabbeliiig ' where water

I Smith (1931) describes this phenomena. Von Xx\ (1963) refers to it as caballing.

8

mixed (ni a signia-t surface will seek a slightly deeper density surface.

It is eniphasized here that the basis of isen- tropic analj^sis is the deductidn of flow patterns from the distribution of dissolved substances which are independent of the density determina- tions. Furthermore, flow patterns are independent of the assumptions lor geostrophic movement and hence can \-erify or disclose any deviations from computed gradient flow. Oxygen and other chem- ical properties, due to then- independence from density computations are ideal flow indicators on the density surfaces when due consideration is gi^'en to biological changes. However since these values are not always available, either tempera- ture or salinity may be used. Parr (1938b) fa- vored temperature because he felt the interpolated values are more certam than those of salinity. Montgomery (1938) on tlie other hand takes the view that salmity is superior due to the strong vertical temperature gradients and the actual temperature on the sigma-t surface would not be representative. For Ice Patrol requirements, the wide range of temperature compared to the accuracy of detennination provides for very great property variation on the sigma-t surface which is the best definitive characteristic of tlie current system. It would be redundant to contour both temperature and salinity since they are used to define the sigma-t surface initially.

Chiirt Preparation

Charts of the temperature distribution on se- lected sigma-t surfaces in the Grand Banks area during the first and third surveys, were prepared from the plots of temperature versus sigma-t at each station. These are shown hi figures 15A to 23A. The depth of the surface at each station has been indicated and a comparison with the surface dynam.ic height contours nuiy be made with figures 2A and 5A. On each chart, the intersection of the sigma-t surface witli the sea surface is shown as a broken luie and, \\hen it occm-s, the intersection with the bottom as a dashed luie.

Chart Analysis

An examination of tlie isentropic charts, figui'es 15A to 17A, reveals that the distribution of the 1° C. isotherm clearly delineates the boundary of the Labrador Current. A comparison with the 25 and 50 meter horizontal isotherm charts of figures 24A and 25A for the same survey shows that the horizontal isotherm charts do not clearly

display the water tongues characteristic of the Labrador cold core. However on the sigma-t surface charts the tongues of water are very nicely demarked, therefore, several levels were prepared for analysis of the water movement.

The sigma-t surfaces of 26.7, 26.8, and 27.0, figures 15A to 17 A, from the first survey show a severe downward slope towards the Banks. This slope would tend to reduce or even eliminate horizontal mixing because a crossing of strong horizontal density gradients would be required. The third survey isentropic charts, figures ISA to 20A, show a definite leveling of these surfaces and a slight increase in depth. This is probably due to the greater volumes of lighter water in the area since a 26.6 surface can be drawn for the third survey, whereas, on the first survey, water of a sigma-t of 26.7 was the lightest water present in abimdance. If a comparison is made between the isotherm charts, plotted on the 25- and 50-meter levels for the first survey, and the isentropic tem- perature distribution charts, definite differences can be seen. As pointed out above, the tongues of water cannot be observed on the constant depth charts, figures 24A and 25A, even though these levels are in the depth range of the sigma-t charts which clearly describe the boundaries of the tem- perature tongues. This is apparently because these tongues of water are moving along steeply sloped surfaces and horizontal slices at specific levels fail to capture them. A comparison at the third survey sigma-t charts and the horizontal presentation at 75 meters, figures ISA to 23A and 26A show that the isotherms appear quite similar in their distribution on both types of presentation. Horizontal mixing can now take place due to the lessened horizontal gradient and the tongue like property distribution is destroyed as the Labrador Current flows south. Both presentations of the third survey are similar with the water grading from cold to \\ arm toward the east as the influence of the Atlantic Current begins to dominate the temperature distribution. This greater horizontal mi.xing is obvious from tlie north-south tempera- ture distribution of the Labrador where the third survey shows the arrival of colder water at the head of the system than found on the first survey. In addition, this colder water appears to be warmed faster as it travels south thus indicating more active mixing is taking place with tlie warmer Atlantic Current.

The unique display of tongues of cold water on the sigma-t surfaces leads to the question as to

what is actually being observed. From the volume flow calculations, the flow during the first survey is minimal. This leads to the postiilation that late winter steady state conditions are described. That is to say that the cold water input at the head of the system is being advected south and warmed sufficiently such that steady conditions of tlie conveyor belt form exist. On the other hand, the beginning of cold water intrusion into a background of existing winter water conditions might be a better conclusion.

The arguments for steady state are few indeed since 1 week after the first survey, a vast increase of water along with profound property changes occurred in the Labrador Current. If steady state conditions existed on the first survey, great mixing would be required to warm the prow of cold water moving south. The warming would result from the warmer water on all sides of the tongue including in front of the intruding prow. The anomalous point is that the salinity along the core of the Labrador during the first survey grades lower to the south. This was quite difi^erent from the expected situation of the Labrador Current grading more saline to the south. Figures 27A and 2SA are plots of salinity at the center stations along the Labrador Current during the first and third surveys. It shows that the salinity graded lower from north to south during the first survey and then higher from north to south on the third siu'vey. The lateral salt distribution grades higher to the east and slightly less to the west. On the Banks the salinity grades liigher to the south during the first survey, as expected. If mixing and warming are occurring with resulting steady state conditions as envisioned above, then the contribution from the east would cause higher salinities as the water moved south rather than the lower salinities actually observed. Water from the west would tend to lower the salinity slightly, but this effect woidd be masked by the much greater salt content of the water from the east. A more reasonable explanation is that we are observing the intrusion of new water from the north, the initial arrival of more severe properties resulting from the spring freshening of the Labrador Curi'ent.

The higher salinity to the north observed on the first survey can be attributed to the winter in- crease in salinity and off-shore mixing further tiorth due to a reduced flow rate. This would not be observed later in the season because of the increased flow and contribution of sea ice melt

water. In this situation the intruding cold water could account for the great slopes of the sigma-t surfaces which would also tend to isolate these tongues from any lateral influence. This colder water mass seems to be invading a more imiform environment and a leveling adjustment towards some form of equilibrium has not had time to take place. Horizontal mixing, across sigma-t surfaces, would be minimal initially, but would eventually become dominate and alter the property distribution to that found on the third survey. This theory is also compatible with the great freshening of flow observed only 1 week after the first survey. Water velocities of only 0.5 knots would be required to move the intruding cold water from the north, found on the first survey, down to section U of the check siu'vey. Velocities of this magnitude were found in the Labrador Current during the first and check survey periods. It could also be expected that some indication of a change of this niagnitude would be observed in the first survey results. Again a relation is seen with the speculation from the previous section in that there is a salinity flow control on the Banks and slope and that this initial flow is tied in with new water arriving on the Banks and slope. This causes a change in the dynamics of the regime and requires a supply of water to fill the continuity conditions of flow, thus explaining the warmer temperatures observed during the check survey of section U where warmer water is drawn in to meet increased mass continuity requirements.

Some surface influence is also shown in the sigma-t presentation. This is indicated by the crowding of the isotherms as the sigma-t surface approached the sea surface and is particularly apparent in the southeastern regions of the Banks nearer to the Atlantic Current. Montgomery (1938) cited the sea surface intersection with the sigma-t surfaces as the fonuation region of the water found on or slightly below the particular intersecting sigma-t surface. No doubt some sur- face mixing and sinking is taking place, however, the water on the sigma-t surfaces flowing along the Banks' slope has its source outside of the immediate area of interest.

Isentropir and Geostrophic Comparison

The fact that these isentropic presentations disclose flow tendencies independent of geostrophic computations provides a useful tool for comparison with the dyiuunic calculations. Certain areas of uncertainty in the calculated surface circulation

10

can be substantiated or altered based on the isen- tropic flow patterns. Parr (193Sb) objected to some interpretations, on the part of Ice Patrol, of the dynamic height charts used for iceberg drift predictions. Parr's isentropic analysis near the southern end of the Banks tended to show a large pooling tendency which was not shown on the dynamic charts. This pool is now generally accepted as a quasi-fixed feature. Parr's work did show that better water movement infonnation could be obtained from isentropic analysis, how- ever the discrepancies that he found were much greater than can be discovered using present day data collection techniques. Prior to World War II the sparseness of station data coupled with technique diff'erences probably accounted for a weakness in the dynamic height charts.

Good comparisons can be seen between the circulation deduced from the isentropic charts and the dynamic height charts shown in figures 2A and 5A. Where the dynamic height charts present quantitative current information, futvu'e changes are reflected in the isentropic charts. Figures 15A to 18A indicate that cold water was entering the system during the first survey, and ultimately was seen to have a definite circulation effect based on data obtained on the check survey conducted only 8 days later. This cold water intrusion from the north is not indicated in the dynamic height charts. Basically, the direction of flow of the dynamic height and the isentropic charts match very nicely in all areas. Figure 2A, shows an area of uncertainty, indicated by dotted streamline, in the northwest section current pat- tern deduced by dynamic heights, ln)wever, the sigma-t surface of 26.7, figure 15A, distinctly

' shows the water flowing onto the Banks in that i

area. A cyclonic flow pattern is defined by the

dynamic height streamlines based on third survey data, figure 5A, in the southeast quadrant of the survey area. A look at the isentropic charts sub- stantiates this circulation. Several sigma-t levels definitely show the cyclonic circulation with water of low temperature and low salinity entering from the east. This is incongruous with the water types usually found in the Atlantic Current and it can be concluded that this is a closed cell which prob- ably had its origin from the cold water pool nor- mally found at the Tail-of-the-Banks as shown in figure 2A. Ijooking at the 26.6 a, level, figure ISA, the cell appears separate from the general near sur- face How. On this level, water of 11.0° C. enters from the east which is anomalously warm and is

probably near surface water being entrained from the warmer layers of the Atlantic Current.

At the 26.8-tr, level, figure 19A, the cell remains quite warm and shallow and affected by the warmer surface water movements. A slight indication of upwelling is seen now from the temperature lowering near the center of this cyclonic circulation with warmer water at the periphery being drawn around the eddy.

The 27.0-0-, level, figure 20A, reflects active upwelling in the eddy center not only by colder temperatures, but also by a definite dome in the depth of the sigma-t surface. Warmer water of the Atlantic Current appears to be moving anti- cyclonically around the eddy in a northwesterly dh-ection. Although it is not shown in these illustrations, the data indicates not only a cooling of the eddy waters but also a reduction in salinity. On this level, the coldest water appears to be displaced slightly to the north from the 26.8-0-, level. The 27.2-0-, level, figure 2lA, is incon- clusive as to whether or not a circulation connection exists with the northwest meander of the Atlantic Current cited above. In this situation the eddy does not appear to be closed. Although isotherm contours do not indicate the circulation in the case of the 27A-(j, and 27.6-(r, levels, figures 22A and 23A, the topography of the sigma-t surfaces again show that the cyclonic circulation seems to be causing some upward movement of the water in the eddy.

In conclusion, it has been shown tliat isen- tropic analysis is an excellent tool for depicting details of the circulation in the vicinity of the Grand Banks. The presentations would be more accurate if a nondensity related property such as oxygen was used. For Ice Patrol current pre- diction procedures, it appears that detailed analy- sis of this nature is not warranted in all areas on a routine basis, however, to completely define and predict the Labrador's variation, the cold water core should be examined with this method. Because the water moves along sigma-t surfaces, the intrusive flow of the Labrador Current water is clearly shown by the isotherms in contrast to the rather nondescript presentation of the hori- zontal levels. The method is probably most valuable for observing the trend of future condi- tions, since water masses of differing charac- teristics wliich ultimately influence the entire area can frequently be traced from their point of original entry.

11

REFERENCES

Fuglister, F. C. ot ul. (1951). Somo results of a multiple ship survey of the Gulf Stream. Telhis, 3: 1-14.

Jakhelln, A. (1936). The water transport of gradient currents. Geofysiske Publikasjoner. Vol. XI, No. 11. Oslo.

Montgomery, R. B. (1938). Circulation in tlie upper layers of the southern North Atlantic deduced with the use of isentropic analysis. Paper Phys. Oceauo. Met., MIT and WHOI, vol". VI, No. 1, pp. 1-53.

Parr, A. E. (1938a). On the validity of the dynamic topo- graphic method for the determination of ocean current trajectories. Jour. Mar. Res., vol. I, No. 2, pp. 119-132.

Parr, A. E. (1938b). Isopycnic analysis of current flow I

by means of identifying properties. Jour. Mar. Res., Res., vol. I, No. 2, pp. 133-154.

Hosby, C. G. et al. (1937). Isentropic Analysis. Bull. Amer. Met. Soc, vol. 18, No. 6-7, pp. 201-209.

Smith, E. H. (1937). The Mariou Expedition to Uavis Strait and Baffin Bay. U.S. Treasury, U.S. Coast Guard, Bull. 19, Pt. 2, Report of the International Ice Patrol Service in the North Atlantic Ocean. 259 p.

Von Arx, W. S. (1962). Introduction to Physical Ocean- ography. Addison- Wesley Pub. Co., 422 p.

12

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Figure lA. Trackline and station array of past Ice Patrol seasons comparea with the 1965 Ice Patrol season. Section

letter designations are shown.

13

Figure 2A. Dynamic topography of the sea surface relative to the 1,000-decibar surface, from data collected during the first survey 30 March-7 April 1965. Oceanographic station positions are indicated and the station numbers given at turning points.

14

50'

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FROM DATA COLLECTED II -12 APRI L 1965

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Figure 3A. Dynamic topography of the sea surface relative to the 1,000-decibar surface, from data collected during the check survey 11-12 April 1965. Oceanographic station positions are indicated and the station numbers given at turning points.

15

Figure 4A. Dynamic topography of the sea surface relative to the 1,000-decibar surface, from data collected during the second survey 7-10 May 1965. Oceanographic station positions are indicated and the station numbers given at turning points.

16

Figure 5A. Dynamic topography of the sea surface relative to the 1,000-decibar surface, from data collected during the third survey 19-25 May 1965. Oceanographic station positions are indicated and the station numbers given at turning points.

17

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18

TEMPERATURE "C 8

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Figure 7A. Mean temperature-salinity plot of all stations on the first and third surveys situated in the Labrador

Current during 1965.

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Figure 8A. Surface dynamic heights in dynamic meters along section Li for the first, check, and third Ice Patrol

surveys 196.5.

19

FIRST SURVEY

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TEMPERATURE °C 9257 9258 9259

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1965.

20

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21

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CHECK SURVEY

TEMPERATURE "C AND FLOW VELOCITY cm/sec

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THIRD SURVEY

TEMPERATURE °C AND FLOW VELOCITY cm/sec

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Figure llA. Velocity distribution along section U for the first, check and third Ice Patrol surveys 1965. The 0.0° C. and 4.0° C. isothemis are indicated by dashed lines.

22

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23

TEMPERATURE "C 8

FIRST SURVEY

CHECK SURVEY

THIRD SURVEY

Figure 13A. Mean temperature-salinity plots, averaged over total depth, of the most westerly stations on the Grand Banks of Newfoundland for the first, check, second and third lee Patrol surveys 1965. Stations 9342 and 9343 from the second survey are shown as almost coincident points.

SALINITY %o

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VOLUME FLOW m'xl0 6/sec

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33.2

33.

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VOLUME FLOW SALINITY

APR

6

JUN

Figure 14A. Variation of volume flow through section U and the change in salinity of the water on the Grand

Banks during 1964—65.

24

Figure 15A. Sigma-t level, 26.7, showing isotherm contours and sigma-t surface intersections with the bottom and sea surface. Based on data collected during the first survey of Ice Patrol 1965.

25

+ +

• + + + + + + +

FIRST SURVEY SIGMA- 1 SURFACE 26.8

+ + + + + -t + + -

+ +

53"

52'

51'

50"

49"

48°

47'

46"

Figure 16A. Sigma-t level, 26.8, showing isotherm contours and signia-t surface intersections with the iiottoni and sea surface. Based on data collected during the first survey of Ice Patrol 1965.

26

Figure 17A. Signia-t level, 27.0, showing isotherm contours and sigma-t surface intersections with the bottom and sea surface. Based on data collected diu-ing the first survey of Ice Pati-ol 1965.

27

Figure 18A. Sigma-t level, 26.6, showing isotherm contours and sigma-t surface intersections with the bottom and sea surface. Based on data collected during the third survey of the Ice Patrol 1965.

28

Figure 19A. Sigma-t level, 26.8, showing isotherni contours and signia-t surface intersections with the bottom and sea surface. Based on data collected during the third survey of the Ice Patrol 1965.

29

Figure 20A. Sigma-t level, 27.0, showing isotherm contours and signia-t surface intersections with the bottom and sea surface. Based on data collected during the third survey of the Ice Patrol 1965.

30

Figure 21A. Signia-t level, 27.2, showing isotherm eoiitoui-s and signia-t surface intersection with the Ijottom. Based on data collected during the third survey of Ice Patrol 1965.

31

Figure 22A. Sigma-t level, 27.4, showing isotherm contours and sigma-t surface intersection with the bottom. Based on data collected during the third survey of Ice Patrol 1965.

32

Figure 23X. Sigma-t level, 27.6, showing isotherm contours and sigma-t surface intersection with the bottom. Based on data collected during the third survey of Ice Patrol 1965.

33

Figure 24A. Isotherm contours at the 25 meter level. Based on data collected din-ing the first survey of Ice Patrol

1965. Contour interval: Heavy lines 2° C, light 0.2° C.

34

5r 50*	49*		48* 47*			46*	45
o	+ + - 4- + - 1 1	- + + - + + 1 1	~\	- + 1	■+ - OOftns \|9296	--'■+ + --0.0-+ + - , -' ' 1.0°	- 4 - + ■3	+ 4 .:^ lOOfms
	1 1	1 1		1	1 '	ol t,° /I ° '	/	/		1 '
	+ + -	- + +		- +	+ -	- +,;'+ -	- \	4		- 4	47:,:''':
	+ + -	- + +		- +	^9275	^MJl-	I?	"	\	- 4 lOOOfm
o	1 1	1 1			1 /	■ y/ /		1		J 1	1
	1 1 + + - ■ + + -	1 1 - 4- + - + +	/-	9274X/	1 /	yi	0\	1	1 4 +
o	1 1	-0.3" 1 1	/	~ ~l /	J //	/yX/	1 1		1
	1 1	' '/		/ ^	■//	yy/	1 1		1
	■ + + -	- +'"yb	'P	'it	/^	/ y ^°°	- + + -	- 4-	+
	■ + + -	- + f	\	M	'm	- + + -	- + + -	- 4	4
LO	1 1	9255/,'^'		{%	' 1 V	1 1	1 1		1
^	1 1 ■ + + -	1 /4i _ 0.0" < ■"	O	f h		1 + -	^ 8.0" 1 - 4- + -	1 1 - 4 + -	- +	1 +
	- + + -	/			c	_, 70"	- 4- + -	- +	+ ■
	+^	='^ + -
o	1 1	100 ftTI^ rl> 1 1		1000 fms	1	1 1		1	1
>	\ J— -'\ -		J	1	1	1 1	' '	1	1
	■ + 4- ^	- \ >	-	V +	+ -	^ 4 + -	1- + + -	- 4	4 ■
	/-		FIRST SURVEY -50 METER LEVEL		■
	+ + -	- + +	-	- +	+ -	- + + -	- + 4 -	- 4	+ ■
o	T-- T [1 I				1 — ' — ' —

o

48*

47«

46"

45*

44«

43*

42'

51'

50*

49'

48*

47'

46*

45«

Fifiure 25.\. Isotherm contovirs at the 50 meter level. Based on data collected during the first survey of Ice Patrol

1965. Contour interval: Heavy lines 2° C, light 0.2° C.

35

Figure 26A. Isotherm contours at the 75 meter level. Based on data collected during the third survey of Ice Patrol

1965.

36

33.000

SALINITY %o

34.000 9 r I

35 000

100

200

w 300

400

500

FIRST SURVEY

STATION LOCATIONS

NORTH 9277

9272

9258

9254

SOUTH 9240

9240

Figure 27A. Vertical distribution of salinity for the line of (center) stations along the fxjre of the Labrador Current . Based on data collected during the first survey of Ice Patrol 1965.

SALINITY %o

34.0

100 -

200 -

s 300 -

400 -

500

Figure 28A.

Vertical distribution of salinity for the line of (center) stations along the core of the Labrador Current. Based on data collected during the third survey of Ice Patrol 1965.

37

Table lA

1st survey

Check survey

3d survey

Volume m.'XlOVsec

Heat °C m.3X10»/sec

Mean temperature "C

Minimum temperature °C Minimum salinity

2. 504

5. 522

2. 20

-.24

33. 122

4. 983 12. 352

2. 48 -. 34 33. 084

4. 708 10. 202

2. 17 -. 49 32. 895

38

n

ill	1 iCDiOO^OS-^-^cD^CDOSC^COTt^OOOiO^iOt^WO'OiCt^Os 1 it^iOCO— i(MI^OC<3-0<-HOO->l"0-HiOCOiCCOOOOOC<50-*aitO	^s	to in oi 0
1 ! 1 1 1 1 1 ' 1 1 ' 1 1 ' ' 1 1 1 ' ' 1 ' 1 1 1 1 1 1	7 1	1 Y
s X < I	. c « .S	■ I'l'OO-Ht^OOtDMOOt^lNOOt^COOSOaiGON-^OS-^tOIN— !■* 1 iP3U30<NOTf05a>t^lNCOirainoOOOtO>OC>lC<5t^-HiOW5-TtlcO<N 1 i->J<-H''rfc^-'-<"c^CO'rf^^MT)ilOT);irf-^>rfro-"iO"^rtCO«5lO	IM 00 to ■* to •*	in in CO t^ •*' to
si £•2 le a T3		0 0 CO 0 04 (M	CO 0 —> 04
° 1 1 1 1 1 1 1 1 1 1 1 1 1 1 1 1 1 1 1 1 1 1 1 1 1 1 1 1 1 1 1 1
z a .9 2	Tfo-. ooo-HiraO''^t^Tj<m'M-Homoot^os--*c^t^oo'McD50 — CT>1<iCOC^iraaiOOCO-HC^c<5C<100t^001r^rt05COiNOi005COt^O>CO	CO 00 ■* in 00 00	00 05 CO 00
	(N 00 ^ lO 00 00	CO 00 00 05 CO 00
g	1 s §	■I^iOOCOSOOOOiOC<5NiCMOO-C005C-105r^f0005 — OiOOJCOOl-*	CO •* O) t^ 00 Ol	CO in cq 00 —1 01
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S 2 ■- -i fl o 2 ^ 1	o^o-HOooodoodddooooooodoo'doooo	10 0 05 01 d d 05 0>	c<i 0 CO 0 05 05 d d Ol o>
s	>> 1 03 a 03 S	OOOOOOCOOC C«500C<100O00O'NiCO00>OIN CO— 1— iOTHa0'C000005CO000002Cq02O02Xt^-HW02O'O0;00O00	to Tj- 0 00	CO 0
	CO CO	CO CO CO CO
aP §1	t^Oiooxai-^t^050c^OiM'-Hoocc'^iocooooc^ooc^co»co5Tt<x	0 0 00 to	■* 0
o-i - r,-^ -II -H\|\| «\|\| ^i-H -H	1 -	1 1
		10 lO ^ 0	in 0 0 ->
	01 05	05 05
	03 P	r^''''iTt<'i'''t'/35i'l'iiii' ' iio ' ' ' '-^lO 'to ' ' '00 'irjoi 'o ^ eo 5">'— 5">' 5">' 5">ix 5">' 'Ooi ' inO '"5 ' ^ 'o5»o 'co 'to 'toco ' 1 1 1 ; ; 12" ' 1 ' loi-^ \|oi 1 ; \|oi \|i-iOi [S \|05 \|0505 1 ^2<='SS-'' S ^"v^^Mtp >>Scd gt-lt-^oc So5 ^2o >,J J:(N S t-'S oi3"'0'22"' s^Su'Sm (S^ic gu^^ic s'O's sto — co sto 3 a,<35 '-^ "^'"'c^ '"' -H'S^r-.'-S-H — I'-S— l^'-S-^'-Srt'-S-H^j^ (Mi^oiTOO>raS<tOTt<f-io<t;Sco§aO(Nio§oo<t;§t^t^ioScoSS'M COI 1 1 1 l«01\| 1 1 ItOt^lOll 1 ICOIOt^lOOIlOICOO"* -Ht^tO(NOiroC^C^Tf<COO— iO)(N— 1— i-*-^MC-)iOC<0C^C-I— lOlC^-ilNCO-^	1 r to to 05 05 < s to CO 10 IM

39

Interim Report

Iceberg Deterioration

by

Ronald C. Kollmeyer, U.S. Coast Guard

Introduction

The problem of iceberg deterioration is an intimate part of iceberg forecasting. The ability of commander, International Ice Patrol to make accurate predictions of the positions of icebergs that may menace the shipping lanes depends not only on reliable drift data but dependable esti- mates of life expectancy as well. At present, the only way to determine when a berg can be dropped from consideration is by direct observation of its progressive reduction in size. Hence, as tech- niques of drift prediction are perfected and scouting for position becomes less necessary, there must be a corresponding increased ability to predict deterioration rate, if any substantial saving in man hours, fuel and equipment are to be safely realized. This will require perfection of the techniques to the point where accurate automatic downgrading of specific bergs can be made with complete confidence without actually viewing them.

Some attention has been given to the problem of iceberg deterioration since 1912, however no quantitative work was ever accomplished which would lead to reasonably precise predictions.

The idealized solution to the problem calls for a detailed examination of the heat budget of an iceberg. Basically, the heat transfer into a berg causes melting, the rate of which is dependent upon many factors. Coupled with the melting is the phenomena of calving or the breaking off of ice pieces. The calving problem complicates prediction schemes because of its randomness in both quantity and frequency. Mass distribution, prominence configuration and existing cracks all play a part in calvnng thus rendering the calving problem unpredictable under any conditions.

Detailed heat transfer studies can be accom- plished for small areas of ice surface, but difficulty arises when these studies are extended to the entire surface of an iceberg. Unequal heat transfer, caused by unequal temperature distributions and

turbulence, prevents the extension of mathemati- cal relationships to actual conditions and makes modeling difficult. The underwater configuration also plays a major part in the deterioration by presenting varying siu"face areas for a given mass. These shapes can only be speculated on until actual observations are made. In the interim gross conclusions must be drawn to categorize the subsurface shapes and sizes into groups, sub-groups and deterioration types. These types reflect the mass to surface area ratios which affect the heat transfer and melting rates. At present only the portion of the berg above the water can be classified by deterioration type. Bergs of the drydocked or pinnacle shapes tend to have low mass to surface area ratios while a blocky or spherical berg tends to have a larger ratio. While these ratios play a role in grouping surface deterioration types, no consideration can be given to the underwater portion because of the lack of ability to determine the underwater configuration.

The logical direction for research in berg de- terioration should be along statistical lines. Basic deterioration parameters must be measured along with quantitative mass size changes in an attempt to correlate the data and develop an effective method for predicting deterioration rates. This prediction method must be based on easily ob- tainable parameters such as air and water tem- peratures, wind velocities, sea state, berg size, and configiu-ation.

Previous Work

In the past no really quantitative work has been performed on berg deterioration. Much is available in the descriptive field of berg disin- tegration but basic correlative data along with mass changes are not available.

Barnes (1912) one of the early observers of bergs, made water temperature measurements in the vicinity of icebergs in and near the Strait of

41

Belle Isle and postulated the causes of observed surface warming as a berg is approached. He further elucidated on this warming phenomena near bergs and the part it plays in deterioration in a 1913 report and agam in 1927. Barnes (1927) looked closely at the physical properties of bergs, including the quantities of entrapped air. He speculated on the causes of calving based on his observations of river ice. A correlation was drawn by Barnes between the internal thermal stresses set up by natural conditions, i.e., the sun, and the calving that resulted. He cites observa- tions made in bright sunlight, concluding that the penetrating rays through the clear melt water on the bergs surface sets up the expansion stresses. He attempted to create these stresses by using thermite bombs to mduce greater calvmg. Zeusler (1926) and Ricketts (1930) made quaUtative studies of the melting processes supported by actual ob- servations. Smith (1931) summarized the basic knowledge to date, citing the various methods of berg deterioration and the conditions causing them. He made detailed observations of several bergs deteriorating under different environmental conditions. The next work of significance occurred when Bidlard (1960) reported on the attempts to destroy bergs. Thermite bombs were used to duplicate the experiments of Barnes (1927). High explosive bombs were also tried to fracture the larger bergs, and the melting of a berg was "hastened" by covering it with lampblack. All of these methods attained only a limited degree of success and were not pursued further. In 1960 a program was initiated to gather statistical deterioiation data on bergs. Coast Guard ships of opportimity were to make studies on deteriora- tion when required to standby dangerous bergs drifting in the shipping lanes. No information as to whether or not the project gathered any useful data is available, however, very few bergs in the past 5 years have required a standby vessel.

In 1964 a preliminary study was conducted by Ice Patrol (Kollmeyer et al, 1964) in order to gain some insight into the problem and to develop the techniques required for future work. A berg was observed oA'er a week's time in a relatively warm air environment and \n water slightly above 0° C. Unfortunately quantitative size measiu-ements were of no value due to the in- accuracy of radar deterinuied ranges and no correlation work could be accomplished. Tlie various problems encountered, particularly those of size and shape measurements, lead to the use

of more elaborate and effective equipment during the 1965 study.

Theoretical Analysis

The deterioration parameters that can be considered the most important are those which contribute to the actual melting of a berg. Calvmg or breakage is random, and at the present time cannot be directly tied to environ- mental conditions. AU forms of heat transfer must be exammed. Basic prmciples of thermo- dynamics indicate that to develop a workable estimate and prediction system, all aspects of radiative heat transfer along with detailed anal- ysis of the small scale phenomena of the fluid boundary layers must be investigated.

The intent herein is not to present an all en- compassing document of heat transfer to icebergs, but to outline an intensive study that will ul- timately lead to accurate deterioration prediction models.

The heat budget of an iceberg can be described as follows:

Net heat added = heat required to raise a berg's temperature. In this treatment, complete melt- ing is the primary concern, therefore the net heat added will be considered as that heat used to raise a berg's temperature to 0° C. and to melt the ice (heat of fusion).

Q,= direct incoming solar radiation

Qr = solar radiation reflected from a berg's

surface ^o=convective-conductive heat from the air Q„=convective-conductive heat from the water Qaa,r=air and water radiative transfer to berg Qir= iceberg back radiation A quantitative look must be given to the heat budget equation of a berg to determine which terms are important and which ones can be dropped. A hypothetical berg will be used for this purpose. Deterioration data based on years of experience will be drawn from Ice Patrol (Lenczyk 1964), as shown in table IC. Listed therein are rules of thumb used to predict the life of various sized bergs in several different water temperature envu-onments. These are gross figures and will be utilized only to show the im- portance of each heat transfer process. The selected figures to be used are 2.2° C. water tem-

42

perature, medium sized, blocky berg, and a de- terioration time of 20 days (2.88X10^ mm.)- The dimensions of the berg selected are 100 meters wide, 100 meters long, and 300 meters in overall height. Using an ice density of 0.9 gm/cm' (Smith 1931) this gives an above the water height of 30 meters. With a total mass of 2.7 X 10'^ gms and a surface area of 1.4 X 10^ cm^.

Because the berg is constantly being reduced in size, it will be assumed that this reduction is linear as far as its surface area is concerned over the 20-day period. This means that a representative area, integrated with respect to time, can be as- sumed to be one-half of the initial surface area which would be 7.0X10" cm^

Before proceeding with the analysis a few more assumptions must be m.ade. The net heat added to an iceberg must be utilized for both raising the berg's temperatiu'e to its melting point and for heat of fusion to melt the berg. Barnes (1927) has shoMTi that the icebergs are basically fresli water and can even be compared to distilled water. Due to the bergs glacial origin this seems reason- able and therefore, the physical constants for fresh water such as heat of fusion may be applied to icebergs.

According to Bader (1961) direct temperature measiu-ements of the Greenland ice cap indicate that as the various glaciers flow towards the sea they assume an internal temperature similar to tlie mean annual ah- temperatiu-es. Furthermore, the internal temperatiu-es are found to be quite uni- form from top to bottom varying only about 1° C. Bader shows that in the xicinity of the Jacobs- haven glacier, postulated by Smith (1931) to be a prime source of bergs, a temperatiu-e of about — 12° C. would apply. For this paper this figure will be assumed to be the minimum mternal temperature of an iceberg.

Durmg melting, the berg's surface would be 0° C. and it would have a negative internal tempera- ture gradient. This gradient would certamly be a variable and some actual measurements will be required. For the purpose of this treatment it will be assumed that a specific portion of received heat will be utilized for raising the berg's surface temperatvu'e to 0° C. prior to melting and mam- tauiing the thermal gradient.

The quantities (Qs—Qr) of equation (1) are affected by the icebergs particular properties of absorption and reflection. Q^, the incoming solar radiation, is an environmental property which not only tends to provide direct heat energy for

melting the bergs surface but also indirect energy for heating the bergs environment.

The nature of the ice surface on which this incoming radiation (Q^) falls, is an important factor in determinimg the effectiveness of this heat source. Before any heating can take place, the radiant energy must penetrate this surface. The ratio of reflected energy to incident energy, or albedo, provides the first tool for estimating the heat energy available for melting. The albedo percentage must be estimated from meas- urements made on snow fields since no direct observations have been made on icebergs. Clean snow fields are very similar to icebergs because of the extreme whiteness of bergs due to their saturation with air bubbles. The air bubbles decrease the transparency of bergs and cause scattering of the incident radiation increasing the reflection. Albedo measurements have been made for sea ice, however, puddhng, brine pockets, and darkened transparent areas can severely reduce the albedo and prevent comparison.

Chernigovskii (1939) shows snow albedos range from 87 percent during March to 60 percent during July in the Arctic. This reduction is due primarily to melting, puddling and surface texture changes during the summer. Numerous investi- gators have looked at the albedo of Antarctic snow fields. Hoinkes (1960) indicates that values ranging from 75 to 93 percent have been found for instantaneous measurements. A value of 80 percent seems reasonable for a berg and will be assumed until more accurate measurements can be obtained. Actually, the albedo of a snow field should be somewhat lower than a berg's because of the berg's facets. These facets cause random reflection which scatters a great deal of the inci- dent radiation. This phenomena is variable depending on a particular berg's configuration and can be treated in general terms only, how- ever, it is reasonable to suspect that the albedo might be a good deal higher than the assumed 80 percent.

Solar radiation values from Hess (1959) show that at 45° N., a latitude of Ice Patrol interest, the maximum incommg radiation reaching the earth's surface during March and June ranges from 0.14 to 0.38 gm cals/cm^min on a 24-hour basis. Some direct measurements, figure Ic, show that during a week in April 1965 an average of 0.14 gm cals/cm^/min were received in the Ice Patrol area of the Grand Banks of Newfoundland.

43

Using an albedo of 80 percent, a figure for solar radiation into the berg {Q,— Qt) of 0.03 gm cals/ cmVmin is obtained. Applying this figure to the hypothetical berg described above, and taking only that portion of the berg above the water that receives this radiation, it is found that 1.1 XIO' cm-X0.03 gm cal/cmVminX2.88X 10* min = 0.095X10'^ gm cals of heat received by the berg during its 20-day decay period.

Back radiation (Q,,) from a berg represents a loss of heat in the budget. Surface and near surface radiative losses will be the most important and would certainly be more intense than any radiation from the colder interior. The Stefan- Boltzman radiation law states that Q=kcT*; where a is the universal cgs units constant of 8.312X 10-" gm cals/cm7°K* min, Tis the absolute temperature degrees Kelvin, and k is blackbody or perfect radiation constant. According to Shumskiy et al. (1964) the radiative ability of snow, the k constant, is as high as 0.99. If 0° C. is assumed for the surface, an upper value of radiated heat loss from the berg can be estimated and would be on the order of 0.46 gm cals/cmVmin. Assuming radiative heat loss from the total surface of the hypothetical berg results in a Qtr of 0.46 gm cals/cm7mmX2.88X10* minX7.0X10» cm^ = 9.26X10'^ gm cals during the decay period.

It should be pointed out that the maximum radiative intensity from the sun comes in at about 0.48/i, indicating that the greatest mtensity lies in the visible range. The reradiated energy from the berg wUl follow the Wien's displacement law which states that the maximum radiative frequency (^max) is a function of temperature:

2897

"max rpo

where T is in degrees Kelvin. This says that the berg will radiate energy in the vicinity of lO/i or long wave radiation. The frequency of emission is also the frequency of greatest absorption therefore a berg will readily receive long-wave radiation from its fluid environment.

Radiative heat transfer from the berg's en- vironment (Qaw,) involves so called blackbody radiation based on the environmental absolute temperatures. Using the Stefan-Boltzman radia- tion law and assuming perfect blackbody radiation for temperatures from 0° C. to 20° C, it is found that the radiative heat transferred to a berg varies from 46.1X10-' gm cals/cmVmin to 61.3X10"- gm cals/cm7min as shown in figure 6C. This trans-

fer of heat will affect the berg proportionately as the air and/or sea temperature varies. The fluid environment radiation is not perfect black- body radiation as is the sun's but is considered more of a greybody type. However for the pur- poses of this paper, perfect radiation will be as- sumed to obtain maximum heat transfer values. Because most of the berg's mass is below the water surface, the water will dominate the radiative heat transfer quantities. This long-wave radiation is absorbed most readily by a berg and since the fluid environment is surrounding the berg on all its facets, reflection due to angular mcidence would be minimal. For this reason, consideration of an albedo would probably not apply in this situation. As can be seen from figure 6C, even with the air at a higher or lower temperature than the water, the overall radiative effect will be little changed. This is true not only because of the small magni- tude change m Q due to warmer or cooler air, but because of the smaller surface area presented to the air compared to that bathed in the sea. Usmg the total hypothetical berg surface area and equal air and water temperatures, arbitrarily taken at 2.2° C, gives a heating contribution of 0.48 gm cals/cmVminX 7.0X10* cm2X2.88X10' min = 9.67X10'' gm cals.

Summing up the computed quantities thus far:

Q,-Q,=0.095X10'2 gm cals

Qa^r=+9.67X10''gmcals

-9.26X10'''gm cals

Qir-

" 0. 505 X 10*2 gm cals

net heat added.

As mentioned, the net heat added to a berg is utilized for both melting and raising the berg's temprature to 0° C. The amount of heat needed to raise the hypothetical berg's 2.7 X 10'^ gms of ice from — 12° C. to 0° C. will be given bv:

where :

Q^r = c,XAT°XM

Af=mass of the berg

Cp=specific heat of ice at —12° C.

therefore :

Q^r=0A9 gm cals/gm °C.X 12°X2.7X 10'' gm

= 1 5.85 X 10"' gm cals.

The rest of the added heat must go into the heat of fusion which would equal: Q/=hfXM

44

where:

/i/=heat of fusion of water

therefore Qf=^79.7 gm cals/gmsX2.7X10'' gms = 2 1 5.0 X 10'- gm cals. This means that 230.9 X 10'^ gm cals of heat are needed to melt this model berg in the 20-day period. However, only 0.505X10'^ gm cals have been accounted for. Therefore the remaining heat must come from sensible heat transfer from the environment by conduction and convection. Because the heat transferred by conduction and convection amounts to approx- imately 500 times the amount of heat added by radiation, the terms (Qs—Q,), Qu, and Qau^, can be dropped from the heat budget equation as negligible and the most attention must be given to conduction and convection. This is somewhat contrary to what is found in the literature con- cerning studies of glaciers. Heat budgets pre- sented by Hoinkes (1964) for various glaciers in the northern hemisphere show that short-wave radiation accounts for up to 89 percent of the source of incoming heat after consideration of albedo. This means only 11 percent of the in- coming heat is suppUed by environmental tem- peratures. These figures are not apphcable to an iceberg due to the percent of surface area exposed to solar radiation and because of the berg's warmer environmental subarctic tempera- tures. The submergence of a berg in a compara- tively warm liquid, with a high specific heat, cannot be compared with the exposure of a glacier's surface to arctic winds.

The problem of examining the conductive- convective terms, Qa and Q^, is complicated by the turbulence of the environmental fluids and the random surface configurations of the visible and submerged portions of the berg. For these reasons, the terms Qa and Q^,, the conductive- convective heat flow from the fluid environment to the berg must be examined from first principles of thermodynamics in order to gain a more thorough undertanding of the problem. Prandtl (1952) analyzed the heat flow, from a moving fluid, through a boundary. The following discus- sion is based on his treatment. In the case of laminar flow of fluid past a boundary, i.e., water or air flow past a berg's surface, it is a fundamental concept that a velocity gradient is established as the boundary is approached. This gradient ranges between the velocities of 0 at the boundary to maximum flow at a given distance away from the boundary. The gradient is the result of fluid

friction. The thickness of the velocity gradient, or boundary layer, is a function of the viscosity of the fluid and the velocity of flow. In the case of laminar flow, all movement is parallel to the direction of flow.

Heat transfer in laminar flow is given by the equation of continuity as follows:

bx dy dz

0

Qi is the heat transfer along the direction of flow given by Qi = CppuT, where Cp is t!ie constant pressure specific heat, p is the density, T is the temperature and u is the rate of flow. Qo is the heat lost in the direction of maximum temperature gradient, in this case to the boundary due to con-

duction, and is given by ^2= — ^ ^ where k is the

molecular thermal conductivity coefficient. Since the thermal conductivity of fluids is small, there is an abrupt fall in temperature as the boundary is approached. The thickness of the thermal boundary layer in laminar flow is a function of the velocity distribution near the boundary and the thermal conductivity of the fluid. A low thermal conductivity and high viscosity will form a thick heat barrier giving a low heat transfer compared to higher conductivity and low viscosity for the same fluid velocities. Q3 is the same as Q2 in tne h direction. No thermal gradient is assumed in the direction of flow due to flow velocity («), hence no molecular transfer. In nature, flow is seldom laminar. In the case of fluid movement around icebergs, configuration and surface rough- ness would rule out laminar flow entirely. The above relationship must be modified to include turbulence.

In turbulent flow the boundary layer concept is retained, however, great reduction in its thickness occurs. Turbulence provides still another mech- anism for heat transfer; that of apparent heat conduction. The temperature distribution away from the boundary, in the turbulent case, is uniform due to mixing. As the boundary is approached tliere is an abrupt fall in temperature. This provides for a heat flow in the direction of the maximum gradient. This is given by

Q=—c„A„-r- where A, is the eddy exchange t '^ ^ on

coefficient. 'I'his type of heat flow disappears as

the laminar subboundary layer is readied wliere

molecular transfer must complete the flow. The

45

equation of continuity shown by Prandlt (1952) now takes the form of:

P<-pU-^-^. ^(Cp^,+ ^) ^j-

dx dy

-i{(^^.-f^)f}-o

Assume now an element of fluid on the boundary surface with one side acting as the heat flow boundary and with no heat flow assumed in the direction as shown below.

It can be assumed that the heat (Q) lost through the boundary surface must pass through the boundary layer and must equal the heat lost between the sections y^ z, and ?/2 22- This is true even in the turbulent case since A, is zero in the laminar subboundary layer. The continuity ex- pression shown above now reduces to

pCpU

dT dx'

by \ dy J

or over the area of the surfaces

c,pjju{T,-T,)dydz= fjk (^yxdz

From this expression it is apparent that the heat transfer through the boundary surface is controlled entirely by the thickness of the lammar sub- boundary layer and the thermal conductivity. This means that if u is low enough, assuming good mixing within the elemental volume, the heat flow through the boundary will be limited by the amount of heat coming in. In this case the temperature T.2 would be equal to the temper- ature at the boundary. As u increases, T2 will become greater than the boundary temperature and approach Tj in value. At the same tune

more heat will be provided for boundary transfer. When this occurs, the heat flow across the bound- ary tends toward an equilibrium condition where

Ii—To^O, and ;r >^ —

dy dy

tion is never reached as long as (u) increases.

The equilibrium condi-

dT

This is because the gradient ~ will increase with

(u) as the thickness of the laminar subboundary

layer is reduced.

The difficulty in evaluating the conductive-

convective heat transfer relationship shown above

is lack of knowledge of the temperature gradient

dT

-5— near the surface of the berg. The gradient is

impossible to measure due to its minute thickness

when turbulent flow exists. It does not lend itself

to modeling due to the variable effects of large and

small eddies created by the erratic surface shapes

found on bergs. Schlicting (1960) shows the

Reynolds analogy which allows the derivation of

relations for heat transfer from relations for

turbulent flow. This is convenient since fluid

velocity measurements near boundaries have been

made and eventually may be attempted in the

vicinity of an iceberg. In the Reynolds analogy,

A u

Prandtl numbers given by P i = -r andP=^Cp t

A^ K

are defined showing the relationship of the eddy and molecular transfer coefficients for convenience of notation. The basic equation showing momen- tum transfer and heat transfer, within both the turbulent and laminar subboundary layers is given by:

= (M+^r) -T- (stress)

(2)

q=-Cj,g\

\dT

(heat)

- = velocity gradient in a particular layer

(3)

where : du df

(/r_ temperature gradient in a particular dy layer

/i = molecular coefficient of viscosity .4r = eddy coefficient of momentum transfer y4j = eddy coefficient of thermal conductivity

17 = gravity fp = specific heat

/: = molecular thermal conductivity

46

The assumption is introduced that the ratio q will

r remain constant across the width of the boundary layer. This is reasonable since the momentum lost in the turbulent layer is that transferred to the laminar layer in the absence of friction, and the heat lost from the turbulent layer is that transmitted through the laminar layer. The reader is referred to Schlicting (1960) for a com- plete treatment of this development. The end result of the integration and combination of the above equatic^ns, (2) and (3), is an expression for the local coefficient of heat transfer across a boundary :

(4)

[■+*«-0]

where :

T=stress in the laminar subboundary layer [7m = average fluid velocity at a great distance from the boundary surface u, = average fluid velocity at the top of the

laminar subboundary layer P=ratio of molecular momentum and

thermal transfer coefficients P, = ratio of turbulent momentum and thermal transfer coefficients </ = gravity Cp = specific heat

A basic problem of measurement of the boundary layer stress (t) remains in equation (4). Simpli- fication of this equation is required before the calculation of Qa and Qw can be attempted and used in practical deterioration problems.

Statistical Approach

Certain simplifications of equation (4) will now be made. P, can be set equal to 1, which implies that the turbulent mechanism for the exchange of momentum is the same as that for heat. Ac- cording to Schlictuig ( 1 960) , because the boimdary velocity and temperature profiles are quite similar, little error will result from this assumption. The Prandtl number P will equal 1 when dealing with gases, but will differ considerably in liquids. This means that the heat transfer between the air-ice boundary and the water-ice boundary should receive sliglitly different treatment.

Tlie stress term in the above equation can be

further broken down into r= — ;— '• With w, =0 at

dy

the wall, and linearizing the gradient, the equation (4) will now take the form:

[C'„+17,(^-.)]:

Now setting P=\ and P,= \ as stipulated above for the air exposed portion of the berg, the equa- tion evolves down to:

(5)

with F being equal to a number made up by gravity, specific heat, viscosity, and the term

y

- representing the laminar subboundary layer

velocity gradient. This gradient is impractical to determine in the field at this time and requires that an empirical approach be attempted. A general expression for heat transfer is:

q = a{T„ — T^)

(6)

where:

T'„ = average air temperature at a great

distance from the berg 7"^ = surface temperature of the iceberg,

assumed to be 0° C a = coefficient of heat transfer

Thus combming equations (5) and (6) the rate of heat transfer per unit area from the air environ- ment to the berg becomes:

5=a7'„==^ /''gmcals/cm2/sec (7)

For a water environment the relationship is not as concise because P^^l, therefore

gCpUin

{U^+uAP-\)]

y

(8)

The measurement of [/„ for water would be very difficult if not impossible. Water movement rela- tive to the berg will be very small in the horizontal and totally negligible when compared to the turbulence caused by the rolling of a berg. Water velocities of several knots are possible as a berg oscillates or rolls in a seaway. This is a variable and depends upon the bergs size stability and the

47

state of the sea. The characterization of the roll- ing effects is best approached from a categorization based on sea state and berg size and wiU be treated so below. It eliminates the need to measure oscillatory periods and to further break down the equation for a in a water environment. Thus the intangible values of equation (8) must be combined with the known constant terms of g and Cp and will result in the simplified relationship a = R. However, the value R will now be determined for sea conditions as well as for berg size in order to include the considerations of water velocity and turbulent heat transfer. With this approach the

heat transfer equation from the water environment to the berg is given by :

q=RT^ gm cals/cm^/sec (9)

Bergs of characteristic size, shape and sea state environment can be observed, cataloged and their characteristic deterioration constants R and F determined.

To apply equations (7) and (9), a statistical program would have to be initiated to determine the constants of R and F in the air and water environment. Bergs must be categorized into groups and subgroups and the R and F values assigned as follows:

Water portion: (R value)

Large	Medium	Small

Rough Moderate Calm

Sea State

Air portion: (F value)

Whereas the underwater portion will be affected by sea state and size, the above the water portion will be affected by size and deterioration type. Evidence tends to indicate that certain bergs, i.e., drydock and pinnacle types, deteriorate faster than domed or blocky shaped bergs. Until a technique is developed for observing the under- water portion of a berg, this shape modifier will have to be neglected for the water environment. In order to obtain R and F, an empirical relation- ship is developed to define the required measure- ments as follows:

Deterioration time

heat of fusion + temperature change of ice heat flux above and below the water

Large	Medium	Small
Fast	Slow	Fast	Slow	Fast	Slow

Deterioration Type

where :

A/=heat of fusion for fresh water AMi=mass change above the water

Ar° = change of temperature from —12° C. to 0° C.

AM2=mass change below the water

Ta„ = air temperature, representative, away from the berg's immediate environ- ment

7'Ki„=water temperature, representative, away from the berg's immediate environment

t/^„„=fluid velocity, air, measured at approxi- mately one-half the berg height, away from the berg's immediate environment Cp=specific heat

This can be further simplified because of the known constants involved, therefore:

D time (hrs) =0.024 [J^ 4^+^^J (10)

With the above equation it is now possible to solve for F or R. In order to do this, bergs must be located in certain environments which will

48

cause the elimination of one of the tenns. For example, in order to solve for F, a berg must be located in water which is 0° C. or less. This all but eUminates the melting of the underwater portion and allows the dropping of the tenn containing R thus allowing the solution for F. Accurate mass measurements with time must be made in order to detennine AM,. Conversely, a cold air and warm water environment will allow the determination of R with the eUmination of the F term.

The known density value will allow computa- tion of total mass and mass change from the measurement of the above the water volume, therefore, only these measurements need be made. By studying many bergs in various environments the values of F and R can be detennined and the table shown above can be completed. The figures for F and R will become more reliable as more bergs are observed.

After F and R are characterized, the equation for deterioration time, equation 10, can be modi- fied for practical application. This is done by substituting the total mass (M,) of the berg that must deteriorate above the water (.1 M!) and below the water (.9 M,) for the A/Wi and AA/2 values respectively. Further simplication of terms of equation (10) gives:

thus,

^ AM, , „ .9M, G=^r- and S=-^-

D time=0.024 [g^ + ~']

where the 6 and S terms can be precomputed and a table prepared similar to that above for F and A'. Because the table is already broken down for size, only the estimation or rather the designation of the mass values of the small, medium, and large bergs must be made. These characteristic values for mass are best left to be designated from the size measurements obtained for the determination of R and f\ The basic approach is to determine the values of R and F for many bergs and then attempt to categorize these bergs for mass and size into the types and groups shown above. A more sophisticated breakdown could be employed depending on the direction dictated by the obtained data.

This approach is at best only a start. A better breakdown for size and shape may evolve as the study progresses. A more detailed deterioration

expression cannot be used because of the limitation requirement of minimal data gathering for a par- ticular berg. Thus, this system is presented which would allow deterioration predictions to be made based on data collected by either ships or aircraft without the involvement of scientific personnel.

Data Collection

During the interval between the first and second current surveys of Ice Patrol 1965, an iceberg was studied for the drift and deterioration rate. Many environmental measurements were made, along with actual size measurements of the berg in an effort to initiate a deterioration study.

Environmental parameters were measured on an hourly basis and are presented in figures IC through 5C. They include: air temperature, sea surface temperature, barometric pressure, wind direction, wind velocity, wave height, wave direc- tion, and incident solar radiation. The solar radiation was measured continuously and recorded by an Epply pyrheliometer.

Several oceanographic casts were made in the vicinity of the berg during the study period fo 27 April to 6 May 1965. The stations occupied can be found in the appendix and include stations 9307 to 9312.

Size measurements of the berg were accom- pHshed daily by a photographic mapping tech- nique. A series of photographs were taken around the berg at approximately 30° intervals of arc. This provided photographs covering all sides of the berg. Overlapping pictures of the starting point were made at the completion of the round of photographs and used to estimate the amount of berg rotation during the photographing process. With this knowledge, and assuming uniform rota- tion, the pictures obtained at the recorded intervals could be adjusted to their true angular aspect. This process is displayed graphically in figure 7C. A sample series of photographs are shown in figures 8C and 9C.

The subject berg had a surface configuration which was characteristic enough to detect the rotation. Provisions were made however to put a dye spot on the berg (figure IOC) to provide a benchmark to detect this motion. For this par- ticular berg, the dye mark was utilized solely to test the various dyes selected for use. The dye Rhodamine B was found to be the most satis- factory and the use of a sporting bow with a glass vial tipped arrow, figure IOC, proved to be a successful means of dye application.

49

The method of measurement employed the use of an optical rangefinder and a standard naviga- tion sextant. While the distance of the ship from the iceberg was being determined with the range- finder, certain characteristic elevations of the berg, above the waterline, were being measured with the sextant. The results of these measurements allowed trigonometric computation of certain vertical dimensions which were used as caUbration measurements for the round of photographs which were subsequentlj" taken. Several elevation meas- urements were made on the different parts of the berg and the mean for each characteristic height was used. With each photograph calibrated by one or more ineasured elevations, other dimensions of the berg could be picked off tlie various photo- graphs. After each photograph was adjusted for the correct angular aspect, the horizontal widths were measured starting at the waterline and at 25-foot intervals to the top of the berg. Indenta- tions, gaps, and other surface discontimuties were also measured in relation to the centerline as shown in figure llC. With these measurements, along with a relatively constant distance from the t)erg for each photograph, a topographic map of tlie bergs configuration above the water was constructed, as shown in figure 12C. Starting with the waterline, levels at 25-foot intervals were subsequently constructed. The picture measurements provided the widths and distances for the construction of guide points on a plan view of tlie berg. Once the guide points were estab- lished, some artistic work was required to connect the points and fill in the measurement gaps using the photographs for reference. For the accura- cies involved, the distance from the berg for pictures taken beyond 400 yards could be con- sidered at infinity because it affected the angle of the constructed tangent lines very little.

Once the scaled mapping was completed, a planimeter was used to compute the areas at each level. These areas were then integrated over the entire height and the total volume above the water was obtained.

Daily measurements were obtained in an effort to observe the changes with time in order to correlate the measured mass reductions with the observed meteorological and oceanographic pa- rameters. Due to the cold conditions existing during tiie study period, and tiie apparent slight deterioration, only two volumetric determinations were made. The maps used in these determina- tions are shown in figure 13(_\ Tlie amount of

visual change in the berg is displayed in figure 14C showing similar aspect photographs taken at an interval of 10 days.

Data Correlation

Environmental conditions of the study berg remained relatively constant during the study period. Figures IC and 4C, the plots of air temperature during part of the study period and the surface water temperatures as measured by the ship's hull probe, show a sUght warming tendency of the water. The upper water layers, less than 5 meters, indicate temperatures above 0° C during the last few days of the study, how- ever, the Nansen cast information indicates that the berg's basic environment was subzero water. This indicated that little subsurface deterioration took place which seems to be substantiated from the size measurements. Looking at figure 14C, calving did occur during the period of study and probably accounted for most of the loss of mass above the water. Little or no correlation with deterioration is seen from the wave height and wave direction observations. As was pointed out in the previous sections, the sea state ^vill cause oscillatory motions of the berg and will contribute to the subsurface turbulence in the bergs vicinity, thus circulating the water and hastening melting in the warmer environments. Wind velocity and direction during the study period are shown in figure 2C.

Calculations based on the topographic maps constructed from the berg's measurements provide the volume of the above-the-water portion of the berg. The total mass of the iceberg may be obtained using the iceberg's density and the total volume determination. Smith (1931) has made actual measurements of iceberg density. He show s a figure of 0.8997 gm/cm' as a mean. Due to the contained air, this density value will vary from berg to berg and within different parts of the berg. However the density variation will be within relatively narrow limits and the figure 0.9 gm/cm' will be sufficiently accurate in comparison to the accuracy in size determination. Using Archimedes flotation principle tlie mass of the iceberg can be calculated as follows:

Percent of ice below the water

density of berg density of sea water Total berg volume

volume aboxe tlie water

percent of total volume above the water

50

Total berg mass= total berg volumeXberg density These calculations were perfonned for the study berg and the tabulated results are shown below

28 April

Volume Mass

707,300m' 636,570X10' kg.

6 May

Volume Mass

624,200m3 561, 780 X 10' kg.

The above calculations detennine that a change of 12 percent took place over an S-day period. The accuracy of these calculations is based on the accuracy of measurement and the precision of construction of the topographic map of the berg. Because a good deal of artwork is involved, the precision of construction probably contributes most of the error. For this reason, tlie work done on size measurements performed this year are believed to have a probable error of 5 percent and could be as high as 10 percent. Because of this, and the small mass change, more frequent topo- graphic maps were not prepared.

Referring to the statistical approacli, this study berg is difficult to categorize. The air tempera- tures are cold showing a mean of about 1.1° C. with a general rise to a maximum of 5° C. to- wards the end of the survey. This air temperature rise is reflected in the sea water temperature at the surface. In order to determine the deteriora- tion constants S or G, the melting of the berg above the water and below the water must be

quantitatively tagged. As pointed out in the previous sections, this can only be done by elimi- nating one of the melting environments, i.e., obtain a berg in a cold water, w.rm air or warm water, cold air environment. Unfortunately, this study berg falls into a cold water, cold air category where little deterioration can occur. The water is as cold as can be expected any time of the year and the air is only slightly above freezing, but the berg did change its mass 12 percent in 8 days. As the berg deteriorates its overall surface area will be reduced. If environ- mental conditions are held constant and similar to the first 8 days, the observed volume loss of 1.04X10* m'/day would diminish due to a di- minished surface area for heat transfer. However, if it is assumed that in the extreme case this rate will remain constant, a minimum of 70 days woidd be required for this berg to deteriorate. The true situation is that because of the reduced sur- face area and therefore reduced heat transfer much longer would be required to melt the berg. This berg would be considered as nondeteriorating in terms of significant changes over a 1- or 2-week period. It is therefore impossible to tag the cause of the observed limited deterioration or to calculate either of the deterioration constants relating to the air or water environment.

The study conducted did demonstrate that more severe difl^erences must exist in the bergs environment to allow computation of the desired constants. It also provided for the development and improvement of the mapping technique employed.

REFERENCES

Bader, H. (1961). The Greenland Ice Sheet. Cold Re- gions Science and Engineering I-B2. U.S. Army Cold Regions Research and Engineering Laboratory, 18 p.

Barnes, H. T. (1912). The rise of temperature associated with the melting of icebergs. Nature No. 2250, vol. 90, pp. 408-410.

Barnes, H. T. (1913). Iceberg Melting. Nature, No. 2260, vol. 90, pp. 671-673.

Barnes, H. T. (1927). Some Physical Properties of Ice- bergs and a Method for their Destruction. Proceedings of the Royal Society. A. vol. H4, pp. 161-168, London.

BuUard, R. P. (1960). U.S. Treasury, U.S. Coast Guard, Bull. 46, Report of the International Ice Patrol Service in the North Atlantic Ocean. Pp. 21-30.

Chernigovskii, N. T. (1939). Radiation penetrating the snow and ice cover of the arctic seas. Problemy Arktiki, No. 6, pp. 31-38.

Hess, S. L. (1959). Introduction to Theoretical Meteor- ology. Henry Holt and Co., New York. 362 p.

Hoinkes, H. C. (1960). Studies of solar radiation and albedo in the Antarctic (Little America V and South Pole, 1957-58). Archin Meteor. Geophys. Bioklimat., Ser. B, 10, pp. 175-181.

Hoinkes, H. C. (1964). Glacial Meteorology. Research in Geophysics. Vol. 2, Solid Earth and Interface Phe- nomena. MIT Press.

KoUmeyer, R. C. et al. (1964). Oceanography of the Grand Banks region and the Laborador Sea in 1964. U.S. Treasury, U.S. Coast Guard, Oceanographic Report No. 10, CG 373-10. 285 p.

Lenczyk, R. E. (1964). U.S. Treasury, U.S. Coast Guard, Bull. 50, Report of the International Ice Patrol Service in the North Atlantic Ocean. Pp. 98.

Pnindtl, L. (1952). Essentials of Fluid Blackie and Son, Ltd., Glasgow. 452 p.

Dynamics.

Ricketts, N. G. (1930). U.S. Treasury, U.S. Coast Guard, Bull. 18, Report of the International Ice Patrol Service in the North Atlantic. Pp. 1-5: 67-74: 75-122.

Schlichting, H. (1960). Boundary Layer Theory. .McGraw-Hill Book Co., Inc., pp. 488-511.

Shumskiy, P. A. et al. (1964). Ice and its Changes. Research in Geophysics, ^'ol. 2, Solid Earth and Inter- face Phenomena. MIT Press.

Smith, E. H. (1931). The Marion Expedition to Davis Strait and Baffin Bay. U.S. Treasury, U.S. Coast Guard, Bull. 19, pt. 3, Report of the International Ice Patrol Service in the North Atlantic Ocean. 221 p.

Zeusler, F. A. (1926). U.S. Treasury, U.S. Coast Guard, Bull. 13, Report of the International Ice Patrol Service in the North Atlantic Ocean. Pp. 36-44 and 61-66.

52

AVERAGE HOURLY SOLAR RADIATION

HOURLY TEMPERATURE °C

iiIimiiiiiiiiImimiiiiiiIiimiiiiiiiIiiiiiiiiiiiIiiiiimiiiiIiiiiimiiimiiiiiiiiiiiIiiiiiimiiiIiiiiiiiiiiiIiiimiiiiiiIiiiiiiiiiiiIiiiiimiiiiIiiiiiiiiim

270000 280000 290000 300000 010000 020000 03OO00 040000 050000

APRIL MAY

GMT

Figure IC. Average hourly incident solar radiation and hourly dry-bulb air temperature observed during the

iceberg study 26 April-6 May 1965.

WIND DIRECTION

000

WIND VELOClTr

36

GMT

Figure 2C. Hourly true wind direction and velocity observed during the iceberg study 26 April-6 May 1965.

53

WAVE DIRECTION

000

340

320

300

280

260

240

220

200

ISO

160

140

120

100

80

60

40

20

A^

n

\./V^ \

WAVE OICEcnON CTrut

XJ

71

JJ

Va.

Y

WAVE HEIGHT

18

17

16

15

14

13

12

I I

10

9

8

7

6

5

4

3

2

I

II li iiiiliiiiniiiiilii I II 1 1 Nil I nil 11 1 III mill nil I iiiIiiiiiiiiimIiiiiiiiiiiiIiiiii Iiiiiiiiiiiil iiiiiliiiii Iiiiiiiiiiiil ml I

2700O0 280000 290000 300000 010000 020O00 030000 040000 050000

APRIL MAY

GMT

Figure 3C. Hourly true wave direction and significant wave height observed during the iceberg study 26 April-

6 May 1965.

SUHFOCE SEOWflTER TEMPERATURE - CENTIGRflOE + 2

SURFACE SEAWATEfi TEM PEHATURE -CENTIGRADE

+ 2*

Figure 4C. Hourly seawater surface temperature observed during the iceberg study 26 April-6 May 1965,

BAROMETRIC PRESSURE - MILLIBARS

1025,0 I

1020.0

— 1015.0

— 1010,0 1005 0 1000.0 995.0 990.0

il III mm II III Mill mill II III 1 1 III li Ml I II II II 1 1 Mill 1 1 II 1 1 II ill INI ill I II I

n lim illini liiiiimiiilii

iimmmlii nliimiimi limimml

290000

APRIL

O3OO0O

MAY

Figure 5C. Hourly barometric pressure observed during the iceberg study 26 April-6 May 1965.

54

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56

ITl

Figure 7C. (Upper drawing) Plan view of iceberg waterline showing initial and final berg aspect at the commencement and termination of a round of photographs. (Lower drawing) True photograph azimuth after angular compensation for berg rotation during round of photographs.

350°T

020° T

055°T |IO°T

Figure 8C. Sample round of iceberg photographs starting from 290° T. (See next figure.)

57

I40°T

200° T

260° T

170°T

F

240° T

290° (overlap)

Figure 9C. Sample round of iceberg photographs (continued from previous figure). Photograph repeated at 290° T (overlap) shows berg rotation during period of photographs.

58

Figure IOC. Dye spots on iceberg, close up picture (a); at distance picture (b), circled for clarity, tipped arrow used in dye application, picture (c); archer in action, picture (d).

Bow and glass

59

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50Ft

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50 Ft

100

200

300

400

500

600

SCALE IN FEET

Figure 13C. Completed topographic iceberg map used for measurement of berg volume al>ove the water. Upper map based on observations obtained at commencement of study 28 April 1965 and lower map based on observations obtained at the termination of the study 6 May 1965.

62

Figure 14C. Similar aspect iceberg photographs showing wastage during the study period.

taken on 26 April 1965, right photograph on 6 May 1965.

Left photograph was

63

TABLE IC.

Estimated deterioration time in days for icebergs

Sea water temperature	Small berg under 50' high, less than 200' long	Medium berg 50'-150' high, 200'-400'^ long	Large berg over 150' high, over 400' long
32	Days 15	Days 40	Days 90
36	8	16	35
40	5	10	20

64

An Examination of Vertical Sampling Methods and Their Influence on Dynamic Height Calculations

by Ronald C. Kollmeyer, U.S. Coast Guard

Introduction

The primary objective of the Ice Patrol surveys is to gather dynamic height information on the Labrador Current and Gulf Stream off the Grand Banks of Newfoundland for the purpose of pre- dicting iceberg drift from geostrophic current maps. Dynamic heights are calculated from temperature and salinity measurements of the water at various depths.

For 35 years Ice Patrol surveys have sampled temperature and salinity at standard depths of 0. 25, 50, 75, 100, 150, 200, 300, 400, 600, 800, 1,000, and 1,500 meters. This standard sampling system is a compromise between the ideal of continuous vertical water column values on the one hand, and the practical necessity of rapid survey with a minimum quantity of samples on the other.

A greater economy of effort and equipment, and more reliable oceanographic inferences, could be obtained if gradient depths (i.e., depths of sharp water property change) were known prior to attaching Nansen bottles to the wire. The intervals between bottles would then be set to assure that no important changes were missed, and that depths of changes were more accurately determined. Toward this end an electronic bathy- thermograph with a depth limit of 410 meters was used during Ice Patrol 1965 to provide information critical to the spacing of Nansen bottles. This gradient sampling method is com- pared to the standard sampling method herein, in an attempt to determine their merits and failings.

A continuous sampling device which gives a very great or unlimited number of data points such as to provide an unbroken record of tempera- ture and salinity through the entire column is ideal, eliminating problems arising from Nansen bottle spacing altogether. The measurement ac- curacies of such a device, as they apply to dynamic

height calcidation, was examined and the results comprise the latter part of this paper.

Sampling Methods

Analysis of the waters off the Grand Banks discloses that this area has some of the most un- usual variation in vertical distribution of water properties in the world. With the Labrador Cur- rent running parallel to the Gulf Stream in some areas and sinking beneath it in other locations, vertical changes in temperature and salinity are quite severe over short distances. Figures iD, 2D and 3D show e.xamples of temperature and salinity distribution of water columns down to 1,000 meters as determined from data obtained during Ice Patrol 1965.

Designing an adequate sampling program for water masses such as shown presents a problem. Since great changes in the vertical distribution of temperature and salinity occur at various levels for different stations, a fixed point sampling pro- gram will frequently miss critical maximum and minimum points in the property distribution. An example of this is demonstrated in figure 2D where the extreme values would have been missed by the standard sampling points shown above. Conversely, many Ice Patrol areas are very uni- form, as shown in figure 4D, where using even a small number of Nansen bottles would suffice.

During Ice Patrol 1965, a gradient sampling approach was used. This method allows the posi- tioning of Nansen bottles to be based on the results of a preliminary bathythennograph drop at each station. A Hytech Electronic Bathythermograph, Model 480 MOD 1 with a modified sensing fish was used to detennine the temperature structure down to 410 meters, the limiting depth of the instnmient. Thus a more complete description of the temperature distribution will be obtained by reversing thermometers and if a stable water column is assumed the variation of salinity with

65

depth will be adequately described. Past Ice Patrol data indicate stable water columns below 100 meters are the rule.

Ice Patrol requirements are better fulfilled by the gradient sampling method. First, better temperature-salinity information is obtained for the dynamic height calculations required for sur- face current detemiinations and, second, a more accurate picture of the vertical variations of tem- perature is described for tracing and analysis of the Labrador Current. As an added feature to this method, it is noted from figure 4D that many areas of the Grand Banks are quite unifonn in their property distribution allowing fewer Nansen bottles than usual to be used on a cast, thus de- creasing time on station, reducing data processing time, and risking less equipment. This is illus- trated by Table ID, where each station on two of the surveys of 1965 is compared for the number of bottles used with the standard depth and the gradient sampling methods.

The advantage of the gradient sampling method lies in the obtaining of better definition of the property distribution. With a more accurate de- scription of the temperature and salinity struc- ture, the accuracy of the dynamic height calcula- tions will also improve. To show this, a standard model of the temperature and salinity structure for each station taken during the first and third surveys was prepared. All observed data points obtained from the gradient sampling method were used to provide a graphic plot of temperature and salinity versus depth. Supplemental tempera- tures were gleaned from the bathythennograph records and along with the observed data were plotted on H.O. 17325 temperature-salinity- density paper. Corresponding supplemental sa- linities were then obtained for an assumed stable water column. Tlie resulting composite tempera- ture-depth and salinity-depth plots are certainly a close approach to describing the properties of each water column. Figure 5D shows an example of a property distribution plot based on observed values from Nansen bottles and the bathythenno- graph supplemental points.

The dynamic heights based on observed gradient sampling values w ere computed immediately dur- ing the survey. Later, a second set of points representing the temperature and salinity values at the standard Ice Patrol depths were abstracted from the composite distribution curves to 1,000 meters and processed on tlie computer for dynamic heights. Figure 6D shows what the property

distribution would look like if this water mass had been sampled using the standard Ice Patrol depths only. Although the density distribution is ade- quately described, in figure 6D, important tem- perature and salinity distribution detail is lacking. A third set of points representing any significant change in temperature and salinity witli depth were abstracted from the curves and processed by the computer. This third set of points was sufficient to adequately describe the distribution of temperature and salinity and the resulting dynamic height is considered the closest approach to the true value. Figure 5D, shows an example of the vertical distribution of these 3 sets of computer processed points: the observed Nansen bottle points, abstracted standard depth points, and abstracted true points.

Table IID shows the comparison between the surface dynamic heights of the two sampling methods and the true value. It can be seen that both methods give residts quite close to the true dynamic height value of the station with the gradient method giving slightly better results; standard deviations are (r=± 0.0039 DM for gradient sampling and (7= ±0.0052 DM for stand- ard sampling. These values are for all 119 sta- tions taken on the first and third surveys of Ice Patrol. These stations were taken both on and off the Grand Banks and include shallow stations where the cumulative errors are minimal in many cases. A total of 62 stations were taken in water greater than 1,000 meters, the assumed depth of no motion, and a more realistic comparison is shown from these; (r=± 0.0044 DM for gradient sampling, and (r=± 0.0065 DM for standard sampling. The gradient method is, however, head and shoulders above standard sampling because the extreme temperature values obtained more accurately describe the existing distribution. These values are essential for the proper analysis and interpretation of the water masses of the Ice Patrol area. Table IID also presents the maximum differences from the true value. In the case of gradient sampling, a large difference occurred due to the missing of gradients caused by encountering a greater than anticipated wire angle.

The errors listed above for the gradient sampling method and the standard depth method can sig- nificantly influence the calculated current. The influence is dependent upon the station spacing and the current velocity. In figure 7D, station interval is plotted against calculated current

66

error at 45° North latitude. The two curves reflect a total error between 2 stations of 0.0088 DM for gradient sampling and 0.0130 DM for standard depth sampling. For stations 10 miles apart, the standard depth sampHng method can cause an error of up to 6.8 cm/sec or about one- tenth of a knot. In some low current areas, the velocity of the surface current could be of this magnitude resulting in a 100-percent error factor. The gradient samphng error is slightly better, showing a 4.6 cm/gec possible error. These current velocity errors do not reflect any instru- ment measurement error which coidd add more than 0.01 DM of error to dynamic height calcu- lations.

The close comparison between the dynamic heights determined from standard depth sampling and gradient sampling indicates that the vertical distribvition of temperature and salinity at a number of stations does not have to be com- pletely described in detail in order to do dynamic calculations for the sea surface. A plot of the specific volume anomaly (5) versus depth is, in general, quite uniform with only gradually changing gradients. In many cases only a few data points in the water column are required to draw a curve which describes the mass distri- bution. Due to the regularity of change of the anomaly curve within a stable water mass, the trapezoidal rule employed in the numerical integration of a water column for dynamic heights will give satisfactory answers in many cases from a curve constructed with only a few points. As an example, figure 8D shows large alternating changes of temperature and salinity with depth; however, the specific volume anomaly versus depth curve is extremely regular, indicating that this particular water column could have been sampled by almost any method and with a mini- mum of data points for the determination of the surface dynamics. However, some stable water columns do not have so smooth a curve and many sample points woidd be necessary for an adequate description.

For Ice Patrol survey work, dynamic height information and a complete description of temper- ature and salinity distribution must be obtained quickly. These two aims require two different sampling techniques: first, only a few data points critically located and rapidly obtained are needed in any given water column for the adeqiuite determination of dynamic heights based on a smooth curve (the exact number of samples

required needs further study because it depends on the water mass involved) ; second, a detailed description of the properties requiring a great number of point samples which is virtually pro- hibitive from the synoptic standpoint. In this situation the ultimate solution is attainable only with a continuous sampling device. A sampler such as this could be lowered in a water column and provide as many data points as considered necessary to fulfill both requirements of Ice Patrol sm-veys along with adding to the rapidity with which a survey can be conducted.

The state of the art in the field of electronic continuous samplers leaves much to be desired. Whereas the point sampling technique using Nansen bottles and reversing thermometers can miss maximum-minimum temperature informa- tion and also fail to describe the gradients of density exactly, the inherent inaccuracies of a continuous sampler also pose a problem.

In using a continuous sampler for the accom- plishment of Ice Patrol survey aims the data abstracted from its output must be sufficiently accurate to perform dynamic height calculations. BasicaUy, two causes of error must be considered when comparing the final results of the point (Nansen bottles) versus continuous sampling systems :

(o) missed density gradients (6) instrument accuracy

As discussed above, a good approach to the true dynamic height of a water column can be made from several data points and a smooth drawn anomaly curve. This method could give accu- racies to within ±2 dynamic centimeters or better depending on the water column. However, the possibility of missing the gradients still exists and generally the missed gradient error must be minimized because of additional instrument errors that must be considered in any sampHng system.

In general, with a fixed number of samples of the vertical distribution of some property, the error in describing the distribution by point sample and using straight fine integration between these points for dynamic computations is shown in figure 9D and given by the relationship :

_ change of property gradient

error— ^^^^^ number of samples over given distance

where the change of gradient of some property (P)

is -rFT„f and tlie fixed number of samples (n) over

a given distance is defined by y;. At the limit

67

condition, -rjy^ > 0, any^ will suffice to give 0

error. However as the second derivative of a distribution curve segment increases, the error

also increases if j^ remains the same. If ^ is

allowed to vary wath the second derivative, the error resultant can be held constant. The error can be held constant or minimized when using a continuous sampler by abstracting sufficient data points in the areas of greatest property change; or at close spaced uniform intervals over the entire

water column, therefore, making -^ large enough

to handle any gradien t change. Predicting density gradient changes directly from the temperature and salinity data is difficult; therefore the abstract- ing of closely spaced uniform interval data points would be the superior method.

An approach was made to this problem by using gradient sampling in an effort to properly describe the density distribution and catch the important changes in gradient. However it was found that the areas of greatest temperature variations are not necessarily the areas of greatest variations in density gradient. On the contrary, figure 8D shows great variations with depth of both tem- perature and salinity in the upper 200 meters but almost a straight line distribution of density. On the other hand, between 400 and 600 meters, the temperature and salinity gradients are almost vertical while the density gradient is about half of the slope observed in the upper 200 meters where great temperature and salinity variations existed. Past practice has been to sample these deeper levels more sparsely because of the less acute changes exhibited by temperature and salinity, however, this could lead to anomaly errors. Figures lOD and llD show examples of intermediate level density gradients missed by the standard sampling.

In order to compare the point sampling method with that of a continuous sampler, an approach similar to that used for comparing gradient sam- pling with standard depth sampling was utilized. Stations representing the various water types found in the Ice Patrol area were plotted to pro- vide vertical temperatiu-e and salinity distribution curves as described above. Several of these stations were then processed for the anomaly of specific volume and this was plotted against depth with smooth curves drawn between the points. Then straight lines were drawn between the

standard Ice Patrol sampling depths. By past methods, the values at the standard depths would have been numerically integrated linearizing the data between each standard depth. The areas bounded by the curve of the specific volume anomaly and the straight lines between the stand- ard sampling levels represent the errors introduced in the dynamic height calculations by standard level, fixed sample number method of data col- lection. This error was then measiu-ed by use of a planimeter to obtain the area bounded by the curves which represents the integration error between each depth interval (figure 12D). Table HID lists the results of this analysis giving the errors, plus or minus, on either side of the idealized distribution curve.

Because of the random character of the anomaly distribution curve, the accumulated errors tend to cancel each other and reduce the totals in most cases. The trend of the curves is towards the more gradual anomaly change with depth resulting in an error which is positive or greater than the true value. Although the accumulated error represents the probable error of standard depth sampling, it is obvious that from the several stations so analyzed that the error ranges from small to large depending on positive or negative error values along the curve. Only 15 stations were selected for this treatment so statistical treatment is not very effective, however, the station dis- tribution is an example of the variety of water masses found in the survey area.

It is attempted herein to show the conditions that can exist and how great the errors can be. Each water column exhibits a random distribution of standard sampling depth errors and a truly representative error is difficult to define. Table HID indicates what can be expected by insuffi- ciently describing the gradient of density and basing dynamic height computations on the straight line distribution between points. These figures are comparable to the errors determined by standard level sampling versus gradient sampling shown above. Continuous Sampling Devices

A continuous sampling system which gives an unlimited number of points would be the ultunate solution to the problem of calculating dynamic heights with a minimum of gradient errors. The advantages of a continuous sampling system can be offset to a greater or lesser extent by the in-

68

ability of the instrument to measure water prop- erties with sufficient accuracy.

The continuous sampHng devices that are avail- able on the market today provide a measurement accuracy from 0.01° C. to 0.05° C in temperature and about 0.03°/oo in salinity. Kollmeyer (1964) pointed out that errors of ±0.02° C. and 0.02°/oo can, under some circumstances, result in a maxi- mum possible error of 0.0169 dynamic meters in 1,000 meters. To evaluate the final accuracies in dynamic heights obtained from a continuous sampler, a more realistic analysis is required here. A selected group of stations, some of which were used in the comparative anomaly plots above, were processed several additional times on the computer using different error values of temperature and salinity. The errors used were designed to be additive therefore increasing the anomaly of specific volume and giving a maximum error. As mentioned above, there were a great number of points used such that they do approach the con- cept of continuous samples. The results are shown in table IVD, with errors given in dynamic meters difference from the true values.

The instrument error is also present when using Nansen bottles and reversing thermometers. Whitney (1957) indicates that accuracies of ±0.024° C. for 0.05° C. scale graduations and ±0.036° C. for0.1° C. graduations can be expected, and Kollmeyer (1964) indicates ±0.01° C. and ±0.02° C. respectively. During Ice Patrol 1965 some 813 thermometer comparisons were made during the surveys. Each Nansen bottle con- tained two thermometers with the accepted temperature value being the average figure ex- cept in cases of obvious malfunction. Since the true value of the temperature is not known, the error in these thermometer readings can be represented by the standard deviation of each thermometer from its paired average. Table VD shows this deviation for each survey during the 1965 Ice Patrol season giving the largest 95-percent confidence limit of ±0.016° C. ob- tained during the third survey. An analysis conducted this year on Ice Patrol between two different inductive salinometers. Industrial In- struments Model RS-7A and Hytech Model 6210 using 3 different operators and duplicate bottled salinity samples yielded a standard deviation between duplicate samples of 0.007°/oo over 41 comparisons. This gives a 95-percent confi- dence limit of 0.014°/oo for a laboratory salinometer at sea.

From table IVD it can be seen that the average of the maximum instrument error in dynamic heights over 1,000 meters for point sampling is ±0.0124 DM using measurement accuracies of ±0.016° C. and ±0.014°/oo. The average of the maximum instrument error for a continuous sampler ranges from ±0.0234 DM to ±0.0286 DM over measurement accuracies of ±0.01° C. and ±0.05° C. respectively and with a salinity error of ±0.03°/oo. It is obvious that the errors from both instruments suites will be random, tending to result in a bell-shaped distribution curve with the maximum errors of table IVD as its practical end points. With this assumption it is then possible to compute the 2<r or 95-percent confidence limit of measurement accuracy for these dynamic heights. Table IVD also lists this 2(r value.

It can be observed from table IVD that the greatest dynamic height error contribution is from the salinity measurement error which is about five times as great as the error in temper- ature measurement. A temperature measure- ment error of ±0.05° C only accounts for about 0.005 dynamic meters while a salinity measure- ment error of ±0.03°/oo accounts for about 0.025 dynamic meters over 1,000 meters.

In order to evaluate the accuracy of a continuous sampler versus the Nansen bottle point sampling method for dynamic height calculations, the errors must be considered as follows: Total error (5)= instrument error (5t)+missed gradient error (Sg).

The total error for the continuous sampler falls within a range of ±0.0231 DM to ±0.0282 DM, depending on the temperature error, and using the average 95-percent confidence figures for instrument error from table IVD and a missed gradient error of 0. For point sampling, the missed gradient error value is so variable and dependent on the water mass and density gradient levels that it is difficult to assign a fixed error, however, from the comparisons of the fixed sampling method and the gradient sampling method presented herein, it has been shown that over 1,000 meters of integration, the 95-percent confidence limit of point sampling error is ±0.0133 DM due to missed gradients. Using this figure and the average 95-percent confidence limit mstrument error of ±0.0122 DM from table IVD for Nansen bottles, the error resulting from the use of standard depth point sampling is equal to

69

±0.0255 DM. By comparing this figure with dynamic height calculations are concerned with

that of the greatest continuous sampler error of the contmuous sampler providing a much more

±0.0282 DM shown above, it is concluded that complete description of the temperature and

both systems give comparable results insofar as salinity distribution.

REFERENCES

KoUmeyer, Ronald C. (1964). An Examination of Errors Whitney, G. G., Jr. (1957). Factors Affecting the Accu-

in Dynamic Height Determinations. U.S. Coast racy of Thermometric Depth Determination. Journal

Guard. Unpublished manuscript, series, October 1963. du Conseil, vol. XXII, No. 2, pp. 167-173.

70

STATION 9400

U 700

♦■TEMPERATURE "C

3300 12 3 4 5 6 7

SALlNITYVoa

8 9 34O0 I 2

3 4 5 6 7 S 9 3500 t

"1 I \ rill i^F^

Figure ID. Vertical distribution of temperature and salinity for station 9400 based on observed data points.

STATION 9252

UJ 700

+ TEMPERATURE*C

94 000 12 3 4 5 6 7

SALINITYVoo

a 9 35 000 I 2

3 4 5 6 7 8 9 36.000 t

I T-t

J I I I I I I

~STaNDARD DEPTH POINTS

I I I I — I

Figure 2D. Vertical distribution of temperature and salinity for station 92.52 based on observed data points.

71

STATION 9268

t TEMPERATURES

SALINITY %o

34 0012 3 45 6 7 8 935 001 2 34 5 6 7B9 36 0O

1 1 / I

1 1 1 I I I II I I I I I I I I I I I I I I I

UJ TOO

S

Figure 3D. Vertical distribution of temperature and salinity for station 9268 based on observed data points.

STATION 9270

+ TEMPERATURE °C

SALINITY %,

33 000 1234 56 799 34 00 I 2 345 6 78 9 3500

n — rn — r~i — r

"1 — I I I

"I I I I I r

UJ TOO

Figure 4D. Vertical distribution of temperature and salinity for station 9270 based on observed data points.

72

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74

CURRENT ERROR CM/SEC 14.0

I 3.0

12.0

I .0

10.0

9.0

8.0

7.0

6.0

5.0

4.0 —

3.0

2.0 I .5

— 0.0088 DM ERROR

0.0130 DM ERROR

45° NORTH LATITUDE

10 15 20 25

STATION SPACING NAUTICAL MILES

30

35

Figure 7D. Curves representing a surfaee dynamic height error between any two stations showing the relation between the station spacing and computed current velocity error.

75

STATION 9399

+ TEMPERATURE»C

SALINITY%.

3 4 5 6 7 8 9 3600

I I I I

I I I I I I

O OBSERVED VALUES X SUPPLEMENTAL POCNTS (ELEBT)

SPECIFIC VOLUME ANOMALY

40 50 60 70 eo 90 100 IIO 120 130 i

Figure 8D. Vertical distribution of temperature, salinity and specific volume anomaly for station 9399 based on observed values and supplemental points from the electronic bathythermograph.

ANOMALY OF SPECIFIC VOLUME

I h-

Q. UJ O

(n a:

Ui

I- lij

ANOMALY ERROR

POINT SAMPLES

Figure 9D. Plot showing the anomaly of specific volume error that results from the straight line numerical integration of the point samples. This error is the result of the straight line's departure from the smooth "true" curve.

76

STATION 9386

+ TEMPERATURE "C

SALINITY %.

5408 9 3500 12 3 4

SPECIFIC VOLUME ANOMALY

40 50 60 70 80 90 rOO MO 120 130 140

Figure lOD. Vertical distribution of temperature, salinity and specific volume anomaly for station 9386 based on observed values. Shown also are the Standard depth points along each curve.

STATION 9248

+ TEMPERATURE °C

SALINITY %o

SPECIFIC VOLUME ANOMALY

0 40 50 60 70 80 90 tOO IIO 120 130

Figure IID. Vertical distribution of temperature, salinity and specific volume anomaly for station 9248 based on observed values. Shown also are the Standard depth points along each curve.

77

STATION 9237

SPECIFIC VOLUME ANOMALY

0 40 50 60 70 80 90 100 110 120 130 140 150 160

"1 \ 1 ^>^ I

100

200

300

400

-J \ \ \ \ \

X
H	500
Q.
UJ
Q
if)	600
OC
hi
\-
LU	700

800

900

1000 —

1100

1200 >—

Figure 12D. Vertical distribution of the specific volume anomaly showing straight lines drawn between Standard depth levels. The area between the straight lines and the smooth "true" curve represents the numerical integration error.

78

TABLE ID. Comparison of number of Nansen bottles used for gradient sampling during Ice Patrol 1965 and what would have been used for standard depth sampling

Survey

Number of stations

Gradient sampling

Standard

depth sampling

Difference

1st. 3d.

62 57

517 464

637 576

120 112

TABLE IID.	Standard deviations between standard depths and gradient sampling dynamic height	computations
	Nimiber of stations	True standard ((t)	&	Maximum difference	True gradient (<r)	&	Maximum difference
Stations to	62	±0.0066 DM.	±0.0133 DM_	+ 0.020 DM--	±0.0044 DM.	±0.0088 DM.	-0.012 DM.
1,000
meters.
All stations.- -	119	±0.0052 DM.	±0.0104. DM _	-0.008 DM--	±0.0039 DM-	±0.0078 DM.	-0.014 DM.

TABLE HID. Plus and minus errors in dynamic heights obtained from the measurement of the areas bounded by the idealized distribution curve of the specific volume anomaly and straight lines between standard depths

Station No.

+ error

— error

Alg. sum. dy- namic meters

9236

9244

9247

9248

9249

9379

9386

9396

9399

9407

9241

9408

9242

9243

9240

9385

9398

0. 0075 .0035 .0025 .0107 .0036 .0040 .0221 .0067 .0040 .0109 .0041 .0034 .0075 . 0050 .0040 .0047 .0061

0. 0007 .0043 .0004 .0018 .0020 .0009 .0038 .0054 .0016 . 0023 .0013 .0019 .0004 .0018 .0016 .0038 .0030

+ 0.0068 - . 0008 +.0021 +.0089 +.0016 + .0031 + .0183 +.0013 + . 0024 + . 0086 +.0028 +.0015 + .0071 +.0032 + . 0024 + . 0009 +.0031

79

TABLE IVD. Instrument measurement error

Station No.

True

dynamic

height

DM

Dynamic height with maximum instrument

error ±0.05° C. ± 0.0307„<, DM

Maximum error	2<7 0f normal distribution curve
0. 0279	0. 0275
.0270	.0266
.0279	.0275
.0291	.0287
.0320	.0316
.0293	.0289
.0284	.0280
.0280	.0276
.0279	.0275
.0309	.0305
.0281	.0277
.0291	.0287
.0285	.0281
.0289	.0285
.0257	.0253
.0286	.0282

Dynamic height with maxiniam instrument

error ±0.01° C. ± 0.0307oo DM

Maximum error	2a of normal distribution curve
0. 0234	0. 0231
.0234	.0231
.0233	.0230
.0235	.0232
.0271	.0267
.0233	.0230
.0236	.0233
.0234	.0231
.0235	.0232
.0235	.0232
.0235	.0232
.0234	.0231
.0234	.0231
.0231	.0228
.0196	.0193
.0234	.0231

Dynamic

height with

maximum

instrument

error

±0.016° C, ±

0.014°/„„ DM

Maximum error

2<7 0f

normal

distribution

curve

9236

9241

9242

9243

9247

9248

9249

9268

9379

9385

9396

9398

9399

9400

9408

Averages -

0. 5737 .5925 .5663 .6825 .5950 .7341 .5892 .5291 .5248 .6035 .5613 .6960 .6028 .5960 . 5332

0.6016 .6195 .5942 .7116 .6270 .7634 .6176 .5571 .5527 .6344 .5894 .7251 .6313 .6249 .5589

0.5971 .6159 .5896 .7060 .6221 .7574 .6128 .5525 .5483 .6270 .5848 .7194 . 6262 .6191 .5528

0. 5859 .6043 .5786 .6947 .6084 .7466 .6015 .5413 .5370 .6158 .5734 .7086 .6152 .6086 .5454

0.0122 .0118 .0123 .0122 .0134 .0125 .0123 .0122 .0122 .0123 .0121 .0126 .0124 .0126 .0122 .0124

0.0120 .0116 .0121 .0120 .0132 .0123 .0121 .0120 .0120 .0121 .0119 .0124 .0122 .0124 .0120 .0122

•All Dynamic Heights must be added to the standard 970.403 based on the 1,000-decibar level.

TABLE VD. Thermometer comparisons

Survey	a		2»		Number of comparisons
1st	±0.005°	c	±0.010°	c__..	342
2d	±0.007°	c	±0.014°	C.-_.	177
3d	±0.008°	c	±0.016°	c_.._	294

TABLE OF OCEANOGRAPHIC DATA

The following is the observed and interpolated data for the Coast Guard Oceanograpliic Unit oceanographic stations taken in conjunction with the International Ice Patrol 1965 in the Grand Banks of Newfoundland area. The data was obtained from CG cutter Evergreen, 30 March 1965, to 25 May 1965. Presentation is from National Oceanographic Data Center Cruise Listing No. 31-540. Notes:

Depth to bottom — -uncorrected sounding depth in meters based on a

speed of sound in sea water of 4,800 ft. /sec. Depth (m) — postscript T indicates a depth determined by ther-

mometric calculations. Sound velocity — in meters per second to tenths according to Wilson's

formula. A complete description of codes can be found in NODC publication M-2, "Processing Physical and Chemical Data From Oceano- graphic Stations."

80

REFERENCE	SHIP CODE	LATITUDE 1/10	LONGITUDE ■ '1/10	if	MARSDEN	STATION T	Mt			ORIGINATOR'S \|	DEPTH	MAX.		WAVE		WEA- THER CODE	CLOUD CODES			NODC
CttY	ID. NO.	SQUARE	IGMTl	YEAR	CRUISE NO.	STATION NUMBER	TO BOTTOM	OF S'MPL'S	OBStKVA llUNi		STATION
CODE	10"	r	MO	DAY HR.1/10	DIB.	HCI PER SEA	IT?[- AMT
31	540	EV	4	202	N	OSl^tS w		150	21 03	30 153	1965	001	9235	3383	14	30	9 D	XI	8 5		0001
		•	WATER	WIND	BARO- METER (mbit	AIR TEMP.	■c	VIS, COD	NO. OBS. DEPTHS	SPECIAL OBSERVATIONS	'-
	COLOR CODE	TRANt.	DIR.	S»EfO OH «OtCt	DRY BULB	WEI BULB
		04		29	S12	119	072	061	3	10
	MEiSfNGI HR 1/10	CAST NO.	CARD TYPE	DEPTH Iml	I *c	s •/..	SIGMA-T	SMCIF1C VOIUME ANOMALT->10'	SAD DYN. M. X 10=	SOUND VELOCITY	03 ml/I	P04-P ug -oi/l	rOTAL-P vg ■ oi/l	N02-N ug - 01/1	NO]-N ug - ot/l	SIO4-S. vg - ol/l	s PH C
			STD	0000	0192	3352	2681	0012441	0000	14559		i
153		OBS	0000 0192 33517 2681		14559
		STD	0010 0213 3360 2686	0011967	0012 14571
		STD	0020 0233 3368 2691	0011515	0024 14582
		STD	0030 0252 3376 2696	0011063	0035 14593
		STD	0050 0287 3390 2704	0010303	0057 14614
		STD	0075 0324 3406 2714	0009436	0081 14536
		STD	0100 0354 3420 2722	0008577	0104 14555
		STD	0125 0376 3432 2729	0008007	0125 14670
153		OBS	0133 0382 34352 2731		14674
		STD	0150 0384 3440 2735	0007507	0144 14678
		STD	0200 0393 3453 2744	0006557	0180 14692
153		OBS	0221 0397 34583 2748		14698
		STD	0250 0405 3459 2748	0005390	0212 14705
		STD	0300 0419 3464 2750	0006213	0244 14721
153		OBS	0373 0440 34805 2761		14744
		STD	0400 0482 3490 2753	0005122	0300 14767
153		OBS	0401 0483 34898 2764		14768
153		OBS	0446 0460 34909 2767		14765
		STD	0500 0435 3490 2769	0004549	0349 14764
		STD	0600 0399 3488 2771	0004488	0395 14765
153		OBS	T0674 0380 34874 2773		14770
		STD	0700 0378 3488 2773	0004378	0439 14773
		STD	0800 0372 3488 2774	0004352	0483 14788
		STD	0900 0366 3489 2775	0004316	0526 14802
153		OBS	0902 0366 34889 2775		14802
		STD	1000 0364 3489 2775	0004369	0570 14817
		STD	1100 0362 3489 2776	0004429	0614 14833
153		OBS	T1152 0361 34892 2776		14842
		STD	1200 0360 3489 2776	0004488	0658 14849
		STD	1300 0358 3489 2776	0004545	0703 14865
153		OBS	T1359 0357 34888 2776		14875
REFERENCE	SHIR CODE		LATITU	DE 1/10	LOF	GITUDE '1/10	ii	MAHSD!N SQUARE	STATION TIME (GMTI	YEA«	ORIGINATOR'S 1	DEPTH TO	MAX. DEPTH OF S'MPL'S	WAVE OBSERVATIONS	WEA. THER CODE	CLOUD CODES		NODC STATION NUMBER
CIRY coot	ID. NO.	CRUISE NO.	STAT NUW	ON
10*	r	Mpn	DAY H	R.l/lO	BER -v^..^"-	Dl>- HGT\| n»] H*	HPi *w
31	5'eO	EV	<l	225	N	05116 W		150	21 (	}3	30 1	96	19_65_	001	9236	2487	12	28	Ul	X2	6 8	0002
			WATEH	WIND	BARO- METES (mbl)	AIR TEMP.	•c	VIS- COD	NO. OBS. DEPTHS	SPECIAL OBSERVATIONS
	COLOS CODE	IBANS.	DIR.	SPffD OR FOUCf	DRY BULB	WEI BULB
		06		12	S04	071	039	039	B	15
	MESSENGR tIME 01 HR VIO	CAST NO.	CARD TYPE	DEPTH (ml	r -c	s v..	SIGMA-T	SPECIFIC VOLUME ANOMALY-IIO'	SAD DYN. M. K 10'	5°""° 0! ml/1 VELOCITY "'	P04-P	TOTAL-f i.a ■ o'/i	NO:-N U3 - or/1	NOj-N ^g - at/1	SlO^-Si US - ai/t	s .H C
			STD	0000	0047	3328	2672	0013332	0000	14491
196		OBS	0000 0047 33283 2672		14491
		STD	0010 0041 3329 2672	0013276	0013 14489
		STD	0020 0035 3329 2673	0013220	0027 14488
		STD	0030 0029 3329 2674	0013172	0040 14487
		STD	0050 0016 3330 2675	0013062	0065 14485
196		OBS	0060 0010 33300 2675		14484
196		OBS	0056 0204 33544 2683		14575
		STO	0075 0391 3382 2688	0011870	0097 14561
196		OBS	0086 0538 34076 2692		14728
		STD	0100 0586 3427 2702	0010554	0125 14752
196		OBS	0102 0589 3*291 2703		14754
		STD	0125 0561 3450 2723	0008669	0149 14749
196		OBS	0127 0555 34513 2725		14747
		STD	0150 0438 3447 2735	0007507	0170 14702
196		OBS	0152 0435 34470- 2735		14701
196		OBS	0178 0495 34628 2741		14732
		STD	0200 0514 3469 2743	0005790	0205 14745
196		OBS	0203 0516 34703 2744		14746
		STD	0250 0508 3480 2753	0005959	0237 14752
		STD	0300 0498 3487 2760	0005380	0266 14757
196		OBS	0305 0497 34876 2760		14757
		STD	0400 0472 3494 2768	0004570	0316 14764
196		OBS	T0404 0471 34943 2758		14764
		STD	0500 0425 3492 2772	0004398	0361 14761
		STD	0600 0394 3491 2774	0004209	0404 14764
196		OBS	0604 0393 34909 2774		14764
		STD	0700 0384 3491 2775	0004207	0445 14776
		STD	0800 0375 3491 2776	0004208	0488 14789
196		OBS	0802 0375 34906 2776		14789
		STD	0900 0366 3490 2776	0004233	0531 14802
		STD	1000 0360 3490 2777	0004248	0573 14816
196		OBS	1018 0359 34897 2777		14818
		STD	1100 0356 3489 2777	0004357	0615 14831
		19	6		08	S	T119-	J	0	355	3«	»8	86	21	7	b							14(	i46

81

REFERENCE	SHIP CODE	LATITUDE 1/10	LONGITUDE ■1/10	n	MARSDEN	STATION	Tl	WE			ORIGINATOR'S	DEPTH	MAX	.		WAVE		WEA- THER CODE	CLOUD			4Cynr
cr(T CODE	ID. NO.			YEAH	CRUISE STATION NO. NUMBER	TO BOTTOM	OF S'MPL-S		CODES		STATION NUMBER
10*	r	MO	DAY	HR.1/10	DID.	HGI P£B SEA
31	540	EV	«	250	N \|05(	3'.2 W		150	20	33	30	239	1965	001 9237	\|l207	11	30	7 i*	X7	6 8	0003
		WATER	WIND	BARO- METER tmb»l	AIR TEMP.	■c	^».dEs	SPECIAL OBSERVATIONS
	COLOR CODE	TRANS.	OIR.	SPEED OP FOPCE	DRY WET BULB BULB
				11	S06	051	006 006	7	10
	MESSENC* TIWE 0 HH 1/10	CAST NO.	CARD TYPE	DEPTH Iml	I -c	s •/..	SIGMA-T	SPEClfiC VOLUME ANOMALT-X10'	SAD DYN. M. « loi	SOUND VELOCITY	Ol ml/1	PO4-P UB - 01/1	TOTAl_P ug . oi/l	NO3-N V9 - ol/l	NOj-N W9 - ol/l	SIO^-S. wg -ol/l	pH	c c
			STD	0000	0158	3304	2645	0015845	0000	14537
239		OBS	0000 0158 33038 2645	14537
		STD	0010 0125 3309 2552 0015242	0016 14525
		STD	0020 0098 3313 2657 0014776	0031 14515
239		OBS	0024 0088 33145 2658	14511
		STD	0030 0083 3315 2659 0014532	0045 14510
		STD	0050 0068 3317 2662 0014300	0074 14507
		STD	0075 0049 3319 2665 0014010	0109 14503
239		OBS	0088 0039 33207 2666	14500
		STD	0100 0012 3329 2674 0013083	0143 14491
239		OBS	0108 0001 33345 2679	14487
		STD	0125 0038 3350 2690 0011615	0174 14510
		STD	0150 0091 3372 2704 0010253	0202 1*541
		STD	0200 0185 3409 2728 0008123	0247 14597
239		OBS	0219 0218 34213 2735	14616
		STD	0250 0253 3434 2741 0006895	0285 14642
		STD	0300 0324 3452 2750 0006139	0318 14579
239		OBS	0387 0396 34740 2751	14727
		STD	0400 0397 3475 2761 0005247	0375 14730
		STD	0500 0402 3480 2765 0005023	0425 14749
239		OBS	T0574 0405 34823 2766	14753
		STD	0500 0406 3483 2767 0004935	0476 14758
		STD	0700 0408 3484 2757 0004980	0525 14785
239		OBS	0758 0409 34847 2758	14795
		STD	0800 0405 3485 2768 0004980	0575 14801
		STD	0900 0399 3487 2771 0004843	0624 14815
239		OBS	T0953 0397 34871 2771	14823
		STO	1000 0396 3487 2771 0004884	0673 14831
		239		OBS		T1052		0395	34874		2771							14841

REFERENCE

SHIP

CODE

LATITUDE

1/10

if

MADSDEN

STATION

Tl

V.I

ORIGINATOR'S

DEPTH

MAX

WAVE

WEA- THER CODE

CLOUD COOES

CI»»

CODE

ID. NO.

LONGITUDE

CRUISE

NO.

STATION

NUMBER

TO BOTTOM

OF

S-MPL-S

STATION NUMBER

10*

1"

MO

DAY

HR.1/10

DIS-

net PER SEA

TfPi Iam

31

540

EV

4313

N

05017 W

150

30

33

31

036

1965

001

9238

3073

01

31

3 i*

X7 1 5 fe

0004

WATER

WIND

BARO- METER

AIR TEMP. -C

VIS. COD

NO.

OBS.

DEPTHS

SPECIAL OBSERVATIONS

COLOR CODE

TRANS.

DIR.

SPEED

OR fOSCE

DRY BULB

WET BULB

11

SO 3

00 3

Oil

006

7

03

MESSENGR 1 f-A5I

HR I/IO

CARD TYPE

DEPTH (ml

T -C

s •/..

SIGMA-T

specific VOLUME ANOMAL»-»10'

SAD

DYN. M.

t 10^

SOUND VELOCITY

03 ml/l

PO4-P

lOTAi-P

NO3-N KB - or/I

NO3-N pg - ol/l

SI O4-ST ng - ot/l

pH

S

c c

STD

0000

0218

3278

2621

0018193

0000

14560

036

OBS 0000 0218 32783 2621 14550

STD 0010 0218 3278 2621 0018187 0018 14562

STD 0020 0217 3279 2621 0018175 0036 14563

STD 0030 0214 3279 2621 0018156 0055 14563

036

OBS 0040 0211 32786 2621 14554

STD 0050 0206 3280 2523 0017989 0091 14563

03

b

OB.

5

0070

0

94

32

8

31

26

2i

145

62

82

SHIP CODE

LATITUDE

1/10

31 540 EV 4258 N 05019 W

STATION TIME

150 |20 |03 |31 |056 Il965 |001|9239

OBIGINATOR'S

AIR TEMP. K

000

JLL

32 kt

WEA- THER CODE

0005

DEPTH Im

SOUND VELOCITY

056

056 056

STD

OBS STD STD STD

OBS

OBS STD

OBS STD STD STD

OBS STD

OBS

0000 0000 0010 0020 0030 0030 0041 0050 0051 0075 0081 0100 0125 0150 0162 0200 T0203

0200 0200 0200 0201 0201 0201 0199 0160 0155 0029 0007 0014 0031 0057 0073 0136 0142

3289

32886

3289

32890

32887

3295

32956

3323

33288

3333

3341

3353

33597

3387

33890

2630 2630 2630 2630 2631 2631 2630 2638 2639 2669 2674 2677 2683 2691 2696 2714 2715

0017283 0000

0017280 0017

0017270 0035

0017266 0052

0015533 0086

0013631 0123

0012789 0156

0012263 0188

0011491 0217

0009420 0270

145 54 14554 14555 14557 14559 14559 14560 14545 14543 14494 14486 14493 14506 14523 14533 14572 14575

REFERENCE	SHIP CODE	LATITUDE 1/10	LONGITUDE •l/io	Si	MARSDEN	STATION Tl	«E			ORIGINATOR'S	DEPTH	MAX			WAVE		WEA- THER CODE	CLOUD CODES			NODC
CIRY CODE	ID. NO.				CRUISE NO.	STATION NUMBER	TO BOTTOM	OF S-MPL-S			STATION NUMBER
10- 1 r	MO DAY H	.1/10	DIP.	HGT PEP SEA	iin *Mi
31	540	EV	4	246	N	05020 W		150	I20	33 31 0	70	1965	001	9240	1134	10	21	4 5	X2	2 8		0006
			WATER	WIND	BARO- METER (mbll	AIR TEMP. \:	VIS. coo	NO. OBS. DEPTHS	SPECIAL OBSERVATIONS
	COLOR CODE	IRANS.	DIR.	SPEED OR fORCt	DRY BULB	WET BULB
				04	S09	99 3	006	006	8	09
	MESSENCR TIME 0 HR I/IO	CAST NO.	CARD TYPE	DEPTH (ml	T r	s •/..	SIGMA-T	SPECIFIC VOLUME ANOM*LT-(IO'	SAD DYN. M. < 10'	SOUND VELOCITY	O7 ml/I	POi-P vo -ol/l	tOtAl-P vg ■ 01/1	N03-N Hg- ol/l	NOj-N	SI O4-S. Itg - ol/l	pH	c c
			STD	0000	0089	3313	2658 0014694	0000	14508
070		OBS	0000 0089 33134	2658 14508
		STD	0010 0086 3314	2658 0014631 0015 14508
		STD	0020 0082 3314	2658 0014608 0029 14508
		STD	0030 0078 3314	2659 0014585 0044 14508
		STD	0050 0068 3316	2661 0014375 0073 14507
070		OBS	0061 0061 33169	2662 14505
		STD	0075 0050 3319	2664 0014040 0108 14503
		STD	0100 0031 3323	2669 0013638 0143 14499
070		OBS	0117 0018 33256	2671 14496
		STD	0125 0027 3336	2679 0012622 0176 14503
		STD	0150 0067 3368	2703 0010410 0205 14530
070		OBS	0178 0136 34009	2725 14570
		STD	0200 0209 3424	2738 0007171 0249 14609
070		OBS	T0203 0218 34268	2739 14614
		STD	0250 0261 3437	2744 0006675 0283 14642
		STD	0300 0300 3447	2749 0006263 0315 14668
		STD	0400 0358 3468	2760 0005329 0373 14712
070		OBS	T0402 0359 34688	2760 14713
		STD	0500 0375 3473	2762 0005233 0426 14737
		STD	0600 0391 3478	2764 0005163 0478 14761
070		OBS	T0601 0391 34777	2764 14761
		STD	0700 0403 3482	2766 0005074 0529 14783
070		OSS	T0796 0408 34853	2768 14801
		STD	0800 0408 3485	2768 0004982 0580 14802
		STD	0900 0406 3486	2769 0004971 0629 14818
		STD	1000 0397 3488	2771 0004874 0679 14831
		07	0		OB	S	T1014		0	395	348	77	27	7	;								146	33

83

EV

LATITUDE

1/10

'tZ3e H

LONGITUDE

•1/10

05019 W

150 l20 103 l3

1 b89 11965 I0pil92»l

03

S02

ORIGINATOR'S

986

AIR TEMP. "C

000 000 B

DEPTH

TO

BOTTOM

16

11701 I 11 I 32 >

Olt HCTJfE*! UA

X2 4 Is

0007

DEPTH Iml

SIGM

SPTCIFIC VOLUM

089 089

089 089 089 089

089

STO OBS STD

STD STO

OBS STD

OBS STD STD

OBS

OBS STD

OBS

OBS STD

OBS STD STD

OBS STO STD

OBS STD STD

OBS

0000 0000

0010 0020 0030 0038 0050 0067 0075 0100 0106 0115 0125 0125 0130 013* 01*4 0150 0172 0200

T0239 0250 0300 0383 0*00 0500

T0577 0600 0700 0758 0800 0900

T0977 1000 1100

T1I*8

0065 0065 0052 00*0 0028 0019 0007 -0010 0058 0270 0321 0178 0157 0157 0180 0200 0230 025* 0321 0312 0309 0316 03*5 0382 0387 0*07 0*11 0*06 0389 0380 0377 0371 0367 0366 036* 036*

3319

33188

3321

3323

3325

33259

3329

33312

3358

3*0*

3*055

3*022

3*03

3*027

3*11*

3*221

3*312

3*3*

3**29

3**6

3*509

3*53

3*62

3*7*0

3*76

3*8*

3*873

3*87

3*88

3*881

3*88

3*880

3*88

3*881

2663 2663 2666 2668

2670 2672 267* 2677 2695 2717 271* 2723 2725 2725 2730 2737 27*2 27*2 27*3 27*7 2751 2752 2755 2762 2763 2757 2770 2770 2772 2773 277* 277* 2775 2775 2775 2775

001*151 0000

0013913 001*

0013697 0028

0013*82 00*1

001309* 0068

0011121 0098

0009132 012*

0008363 01*5

0005762 0006*03

0005950 000559*

0005065 000*780

000*612 000**83

000**1* 000**39

000**66 000*519

016* 0197

0228 0257

0310 0350

0*07 0*52

0*96 05*1

0585 0530

1**97 1**97 1**93 1**90 1**86 1**8* 1**81 1**76 1*512 1*517 1*6*0 1*578 1*571 1*571 1*583 1*59* 1*610 1*522 1*556 1*557 1*563 1*568 1*690 1*721 1*725 1*752 1*767 1*768 1*778 1*785 1*790 1*80* 1*815 1*818 1*83* 1*8*2

84

REFERENCE	SHIR CODE	LATITUDE 1/10	LONGITUDE • -i/io	if	MARSDEN	STATION TIME			ORIGINATOR'S	DEPTH	MAX. DEPTH OF VMPL-		WAVE		WEA- THER CODE	CLOUD CODES				ODC
cut	ID. NO.	SQUARE	IGMTI	YEAR	CRUISE NO.	STATION NUMBER	TO BOTTOM	OBStKVAIIU>H>		S ATION NUMBER
CODE	10*	r	"mO~	DAY H	H.I/IO	Olt	HGI «» SE»	UPE AM
31	SAO	EV	4212	N	05022 W		150	20	D3	31 131	1965	001	9242	3036	12	01	3 C	X7	5 8		Qooa
			WATER	WIND	RARO- METER (mbtl	AIR TEMP.	■c	° DEPTHS	SPECIAL OBSERVATIONS
	COLOR CODE	IRANI	DIR.	into 0* tO»C£	DRY euLB	WET BULB
				16	505	997	025	025	7 12
	»>"i"<^"lc*si "»' "'NO. HR 1/10	CARD TYPE	DEPTH Iml	T t	S v..	SIGMA-T	SPECIFIC VOIUMI ANOMAL»-I10'	SAD DYN. M. K I0>	SOUND VELOCITY	Ol ml/I	P04-P vg -ol/l	IOTAl_f Ut • o./l	NO3-N MS - Cl/I	N03-N ve ■ ot/i	SI04-Si wg - oi/l	pH	C C
		STD	0000	0284	3355	2676	0012918	0000	14599
131	OBS	0000 0284 33547 2676		14599
	STD	0010 0286 3355 2676	0012917	0013 14602
131	OBS	0012 0290 33557 2677		14604
	STD	0020 0345 3367 2581	0012527	0026 14631
	STD	0030 0401 3379 2685	0012156	0038 14558
131	OBS	0035 0423 33638 2686		14558
	STD	0050 0429 3384 2686	0012078	0062 14573
	STD	0075 0440 3385 2585	0012056	0092 14682
131	OBS	0086 0444 33886 2688		14586
	STD	0100 0310 3390 2702	0010533	0121 14632
	STD	0125 0196 3401 2720	0008777	0145 14588
131	OBS	0131 0192 34055 2724		14588
	STD	0150 0336 3*32 2733	0007543	0155 14657
131	OBS	0180 0506 34657 2742		14738
	STD	0200 0496 3469 2746	0006583	0201 14737
	STD	0250 0477 3477 2754	0005827	0232 14739
	STD	0300 0467 3484 2761	0005252	0250 14744
131	OBS	0300 0467 34838 2751		14744
131	OBS	T0398 0471 34945 2759		14753
	STD	0400 0470 3495 2759	0004673	0309 14753
	STD	0500 0444 3495 2772	0004381	0354 14769
131	OBS	0594 0424 34953 2774		14775
	STD	0600 0423 3495 2774	0004245	0397 14777
	STD	0700 0413 3494 2775	0004300	0439 14789
	STD	0800 0403 3493 2775	0004350	0483 14801
	STD	0900 0393 3493 2775	0004322	0526 14813
131	OBS	T0992 0383 34921 2776		14825
	STD	1000 0376 3492 2777	0004282	0569 14823
131	OBS	T1016 0363 34920 2778		14820
	STD	1100 0360 3492 2779	0004181	0611 14833
	STD	1200 0356 3492 2779	0004218	0653 14848
131	OBS	T1201 0356 34918 2779		14848
REFERENCE	SHIP CODE	LATITU	OE 1/10	LONGITUDE '1/10	If	MARSDEN SQUARE	STATION TIME IGMTI	YEAR	ORIGINATOR'S	DEPTH TO BOTTOM	MAX. DEPTH OF S'MPL-	WAVE OBSERVATIONS	WEA- THER CODE	CLOUD CODES		NODC STATION NUMBER
CItT CODE	ID. NO.	CRUISE NO.	STATION NUMBER
10-	r	MO 1	DAY H	«.1/10	01*.	HOI rtt tlA	"PL AMT
31	R^^n	FV	&1&0	N	osoiq w		ISO	10	D3	31 1	70	1965	00 L	9243	i7B6		3?	2 12	XI	6 6		0009
			WATER	WIND	BARO- METER Imbll	AIR TEMP.	S^	VIS. COO	NO. OBS. DEPTHS	SPECIAL OBSERVAHONS
	COLOS CODE	TRANS,	DIR.	S'EEO	DRY lULB	WET BULB
		03		30	S14	003	067	050	B_	15
	MESMNOl c,5, TIME 0 NO.	CARD TTPE	DEPTH Iml	I X	s •/..	SIGMA-T	SPECIFIC VOLUME ANOMALV-IIO'	SAD DYN. M. X 10^	SOUND VELOCITY	Ol ml/l	PO4-P vt ■ o'/l	lOTAl-P	NO3-N „t - Ol/I	NO3-N KB - ot/l	SIO4-SI ,8 - ol/l	pH	1 c c
	HR 1/10
		STD	0000	1312 13573	2595	0011135	0000	15022
170	OBS	0000 1312 35729 2595		15022
	STD	0010 1312 3573 2695	0011193	0011 15023
	STD	0020 1312 3572 2695	0011242	0022 15025
	STD	0030 1312 3572 2594	0011300	0034 15027
170	OBS	0030 1312 35718 2694		15027
170	OBS	0040 1297 35705 2696		15023
	STD	0050 1132 3535 2701	0010719	0055 14964
170	OBS	0056 1049 35167 2702		14933
	STD	0075 1042 3515 2702	0010617	0082 14933
	STD	0100 1035 3515 2703	0010523	0109 14935
	STD	0125 1030 3514 2703	0010654	0135 14937
170	OBS	0133 1029 35141 2703		14938
	STD	0150 1028 3514 2703	0010682	0162 14941
	STD	0200 1026 3515 2704	0010696	0215 14948
170	OBS	0210 1025 35155 2705		14950
	STD	0250 0909 3503 2715	0009785	0267 14912
170	OBS	0287 0825 34951 2722		14886
	STD	0300 0808 3496 2725	0008845	0313 14881
170	OBS	0313 0782 34945 2728		14873
170	OBS	T0363 0500 34814 2743		14808
170	OBS	0384 0625 34880 2745		14822
	STD	0400 0634 3494 2748	0006596	0391 14829
170	OBS	0415 0540 34987 2751		14835
	STD	0500 0573 3499 2750	0005549	0453 14822
	STO	0500 0511 3500 2768	0004950	0506 14814
170	OBS	T0622 0500 34998 2769		14813
	STD	0700 0473 3498 2771	0004721	0554 14814
	STD	0800 0443 3497 2774	0004535	0600 14818
170	OBS	0827 0436 34969 2774		14820
	STD	0900 0418 3497 2775	0004332	0645 14825
	STD	1000 0399 3497 2779	0004182	0687 14833
170	OBS	T1052 0393 34973 2779		14839
	STD	1100 0392 3497 2779	0004197	0729 14847
	STO	1200 0388 3495 2778	0004393	0772 14852
		17	0	OB	S	T123	3	0	387	3	♦ <	»42	2-	f7	8								14	368	i	\l	(^

fiEFEHENCE				LONGITUDE ' '1/10	il	MARSDEN	STATION	TIME	YEAR	ORIGINATOR'S	DEPTH	MAH			WAVE	WEA- THER CODE	CLOUD CODES
CODE	10. NO.	CODE	1/10			CRUISt NO.	STATION NUMBER	TO BOTTOM	OF S'MPL'S			STATION NUMBER
10-	r	MO	DAY	MR.1/10	Dm.	MGT PES SEA	TYPE AW
31	540	EV	4203 N	04954 W		149	29	D3	31	223	1965	001	9244 3430	11	78	t* U	X2	6 2	0010
		WATER	WIND 1 „^o^	- R 1	AIR TEMP. "C	VIS. COD	NO. OBS. DEPTHS
	COLOR CODt	IRANS.	DIR.	""0 MEiE	DRY WET BULB BULB	OBSERVATIONS
				28	S20 020	022	006	8	17
	MESSENCB (-AST T.M£ o\q^ HR 1/10	CARD TYPE	DEPTH (ml	T -C	S '/..	SIGMA-T	SPEClfiC VOLUME ANOMALT-OO'	SAD DYN. M. X 10'	SOUND VELOCITY	Oj ml/l	PO4-P IC P9-01/I u	TAl-P	NO3-N ug - ot/l	NO3-N yg-ol/l	SlO^-Si wg - oVI	PH	c c
		STD	0000	0663	3432	2695	0011126	0000	14757
223 OBS	0000 0663 34316 2695	14757
STD	0010 0697 3435 2693	0011327 0011 14782
STD	0020 0739 3443 2694	0011307 0023 14802
223 OSS	0027 0772 34502 2694	14815
STD	0030 0793 3456 2696	0011107 0034 14826
STD	0050 0909 3488 2703	0010491 0055 14877
223 OBS	0052 0919 34905 2703	14881
STD	0075 0946 3497 2704	0010474 0082 14895
STD	0100 0975 3504 2704	0010491 0108 14912
STD	0125 1004 3510 2704	0010521 0134 14927
223 OBS	0132 1012 35122 2705	14931
STD	0150 0980 3506 2705	0010490 0160 14922
223 OBS	0169 0946 34996 2706	14912
223 OBS	0185 0664 34569 2715	14801
223 OBS	0195 0719 34756 2722	14827
STD	0200 0719 3477 2723	0008827 0209 14828
223 OBS	0211 0720 34792 2725	14830
223 OBS	0227 0821 35006 2727	14875
223 OBS	0236 0770 34943 2729	14856
STD	0250 0630 3469 2729	0008281 0251 14800
223 OBS	T0262 0574 34608 2730	14778
223 OBS	0288 0656 34867 2740	14819
STD	0300 0686 3494 2741	0007247 0290 14833
223 OBS	0313 0710 35008 2743	14846
STD	0400 0589 3498 2757	0005808 0355 14812
223 OBS	T0418 0568 34974 2759	14806
STD	0500 0539 3497 2763	0005378 0411 14808
STD	0600 0507 3497 2766	0005138 0464 14811
STD	0700 0480 3496 2769	0004948 0514 14817
223 OBS	0794 0458 34956 2771	14823
STD	0800 0457 3496 2771	0004810 0563 14824
STD	0900 0441 3496 2773	0004666 0611 14834
223 OBS	0968 0428 34968 2775	14840
STD	1000 0421 3497 2776	0004489 0655 14842
		223	OBS	T1069		0404	3'>965		2778								14847

REFERENCE	SHIP CODE	LATITUDE 1/10	LONGITUDE * '1/10	_2 ii	MARSDEN	STATION T	ME			ORIGINATOR'S	DEPTH	MAX	.		WAVE		WEA- THER CODE	CLOUD CODES
CTRY CODE	ID. NO.			CRUISE NO.	STATION NUMBER	TO BOTTOM	OE S'MPL'S			STATION NUMBER
to-	r	MO	DAV HR.1/10	01=.	HGI PER UA	IPE W
31	540	EV	<	f225	N	04927 W		149	29 (	)4	01 D	24	1955	001	9245	?743	11	26	3 3	X?	5 8	0011
				WATER	WIND	BARO- METER Imbil	AIR TEMP. -C	VIS. COD	NO. OBS. DEPTHS	SPECIAL OBSERVATIONS
	COLOR CODE	IRANI.	DIR.	SPEED oa FOIICE	DRV BULB	WET BULB
			28	SIO	054	022	017	7	10
	MESSiNCI TIME 0 HR 1/10	CAST NO.	CARD TYPE	DEPTH Iml	T y:	S •''..	51GMA-T	SPECIFIC VOLUME NOmL»->10'	SAD DYN. M. X 10^	SOUND VELOCITY	O2 ml/1	Pd-p	TOTAL-P	NO3-N vg - oi/i	NO3-N wg ■ oi/l	SIO4-SI ua - oi/l	pH	s c c
			STD	0000	0428	3382	2684	0012156	0000	14665
	024		OBS	0000 0428 33822	2584 14665
	024		OBS STD STD STD	0009 0428 33822 0010 0428 3382 0020 0426 3382 0030 0423 3382	2684 14666 2584 0012163 0012 14665 2585 0012150 0024 14567 2585 0012145 0035 14668
	024		OBS STD	0041 0421 33821 0050 0394 3379	2685 14668 2685 0012105 0061 14658
	024		OBS STD STD STD STD	0052 0367 33776 0075 0390 3395 0100 0430 3424 0125 0452 3449 0150 0487 3470	2687 14648 2598 0010883 0089 14663 2717 0009129 0114 14687 2734 0007618 0135 14708 2747 0006349 0153 14725
	024		OBS STD STD STD	0151 0488 34711 0200 0483 3480 0250 0476 3486 0300 0469 3492	2748 14726 2756 0005614 0183 14733 2761 0005143 0210 14740 2767 0004672 0234 14746
	024		OBS STD	T0327 0454 34938 0400 0445 3495	2759 14748 2772 0004297 0279 14753
	024		OBS STD STD	T0499 0428 34954 0500 0428 3495 0600 0416 3496	2774 14752 2774 0004167 0321 14762 2776 0004079 0353 14774
	024		OBS STD STD STD	0605 0415 34951 0700 0403 3495 0800 0390 3494 0900 0377 3493	2776 14774 2777 0004087 0403 14785 2777 0004104 0444 14796 2778 0004109 0485 14807
	024		OBS STD	T0902 0377 34934 1000 3494	2778 14807
		02	l>		OB-	5	1077				34	9	44

86

540

SHIP CODE

EV

LATITUDE

1/10

4248 N

149 |29 104 lOl P55 Il965

SPEED

OR (OBCE

ORIGINATOR'S

001 I 9246

028

NO.

OBS.

DEPTH

2624 I 12 I 27 k

HCnPEB SE*

NODC STATION NUMBER

0012

MESSENC* HR 1/10

SPECIFIC VOLUME

S104-Si

055

055 056

055 055

055

055 055

055

STD

OBS STD STD

OBS STD

OBS

OBS STD STD

OBS STD

OBS STD STD

OBS STD

OBS

OBS STD

OBS STD STD

OBS STO STD

OBS STD STD

OBS

0000 0000 0010 0020 0021 0030 0031 0041 0050 0075 0092 0100 0122 0125 0150 0154 0200 0213 0233 0250

T0252 0300 0400 0400 0500 0600 0603 0700 0800

T0808 0900 1000

T1027 1100 1200 1208

0619 0619 0629 0739 0755 0963 0974 0958 0969 0999 1019 0926 0742 0731 0665 0658 0671 0674 0622 0613 0612 0564 0487 0487 0457 0432 0431 0412 0397 0396 0390 0384 0382 0383 0388 0389

3427

34273

3455

3481

34837

3508

35092

35142

3514

35143

3502

34798

3479

3475

34742

3497

34974

34920

3494

34944

3494

3493

34931

3495

3497

34968

3496

3495

34952

3495

34946

3495

3496

34956

2698 2698 2718 2723 2723 2710 2709 2715 2714 2708 2705 2711 2722 2723 2729 2729 2746 2745 2748 2751 2751 2757 2766 2766 2771 2775 2775 2776 2777 2777 2778 2778 2778 2779 2779 2778

0010899 0000

0008966 0010 0008478 0019

0009818 0028

0009496 0047 0010030 0072

0009822 0096

0008672 0119 0008151 0140

0006657 0178

0006203 0210

0005654 0004913

0004539 0004219

0004132 0004111

0004145 0004159

0004240 0004347

0239 0292

0339 0383

0425 0466

0507 0549

0591 0634

14749 14749 14758 14807 14813 14896 14901 14897 14903 14918 14928 14893 14824 14820 14798 14796 14811 14815 14797 14796 14796 14785 14770 14770 14774 14781 14781 14789 14799 14800 14813 14827 14830 14843 14862 14864

1 REFERENCE	SHIP CODE	LATITUDE l/IO	LONGITUDE ■ '1/10	°i	MARSDEN	STATION TIME			ORIGINATOR'S	DEPTH	MAX			WAVE		WEA- THER CODE	CLOUD CODES		1	^ODC
'cTRT	ID. NO.			TEAR	CRUISE NO.	STATION NUMBER	TO BOTTOM	OF S'MPL'S		STATION NUMBER
CODE	10"	r	MO	DAY H	R.VIO	DIR.	MGT n» SI*	UPl AM
31	540	EV I422I	N	04836 W		149	28	34	01 0	91	1965	001	9247	210	10	?8	b 5	XI	3 2	0013
			WATER	WIND		AIR TEMP. X	VIS. coo	NO. OBS. DEPTHS	SPECIAL OBSERVATIONS
	COLOR CODE	IRANS.	DIR.	SPEED 0» fORCE	MEIER (mbd	DRY BULB	WET BULB
				28	S15	066	033	025	7	11
	MESSENGII [(-AST TIME , ^0 HR 1/10	CARD TYPE	DEPTH (ml	T -C	s •/..	SIGMA-T	specific volume anomal«-xid'	SAD OYN. M. K 10^	SOUND VELOCITY	0? ml/l	PO4-P va-a./i	lOTAi-r	NOi-N vg - oi/l	NOi-N W8 - oi/l	SIO4-S1 tig -Ql/I	pH	S c c
		STD	0000	0716	3436	2692	0011465	0000	14788
091	OBS	0000 0716 34363 2692 14788
	STD	0010 0743 3445 2695 0011196 0011 14802
	STO	0020 0768 3452 2696 0011036 0022 14814
	STD	0030 0790 3459 2699 0010841 0033 14825
	STD	0050 0827 3467 2699 0010815 0055 14843
091	OBS	0061 0843 34702 2699 14852
091	OBS	0070 0854 34714 2699 14858
	STD	0075 0852 3474 2701 0010704 0082 14858
	STD	0100 0839 3483 2710 0009895 0108 14858
	STD	0125 0826 3490 2718 0009237 0132 14858
	STD	0150 0814 3494 2723 0008801 0154 14858
091	OBS	0161 0808 34954 2725 14858
	STD	0200 0696 3488 2735 0007669 0195 14820
091	OBS	0240 0631 34874 2743 14801
	STD	0250 0626 3489 2745 0006783 0231 14801
091	OBS	0272 0616 34910 2748 14801
091	OBS	0286 0502 34758 2750 14755
	STD	0300 0510 3479 2752 0006134 0264 14761
	STD	0400 0569 3501 2762 0005357 0321 14804
091	OBS	T0402 0570 35010 2762 14805
	STD	0500 0528 3501 2767 0004936 0373 14804
	STD	0600 0485 3501 2772 0004510 0420 14803
091	OBS	T0608 0482 35013 2773 14803
	STD	0700 0436 3498 2775 0004303 0464 14799
	STD	0800 0400 3494 2776 0004273 0507 14800
091	OBS	0813 0396 34931 2776 14800
	STD	0900 0377 3491 2776 0004287 0550 14807
	STD	1000 0367 3491 2777 0004256 0592 14819
		09	1	08	3	T1039		0:	67	34	9	08	27	7'	7						148	25

87

LATITUDE

1/10

31 5*0lEV <t201 N 04818 W

LONGITUDE

1*9

28 I0» to

llli.

11965

SCEtD

oa

FOllCI

ORIGINATOR'S

BARQ. METER (mbi)

108

00119246

061

050

12

B457 I 09 I 28

Gli PES U*

WEA- THER CODE

XI 3 I3

NOOC STATION NUMBEfi

S«ClFrc VOLUME

SAD

DYN. M.

X 10^

131 131

131

131 131

131

131 131

STO

OBS STO STO STD STO STD STO STO

OBS STO

OBS

OBS STD

OBS STO

OBS

OBS STD

OBS STD STD STD STD

OBS STD

OBS

0000 0000 0010 0020 0030 0050 0075 0100 0125 0137 0150 0165 0200 0219 0227 0250

T0282 0300 0303 0322 0400

T0486 0500 0600 0700 0800 0827 0900

T0914

1352 1352 1352 1353 1353 135* 1355 1356 1357 1357 13*8 132* 1250 1121 10*8 09*0 0885 0906 0910 0858 0660 0*99 0*97 0*81 0*65 0**9 0**5 0*33 0*31

3577

35770

3577

35771

3576

35753

3560

35375

35253

3501

3*98*

3515

35157

35113

3*96

3*852

3*86

3*88

3*90

3*92

3*922

3*96

3*973

2690 2690 2690 2690 2690 2690 2690 2689 2689 2689 2690 269* 2698 2705 2708 2708 2715 272* 272* 2729 27*6 2758 2759 2762 2765 2769 2770 277* 2775

0011615

0011651 0011686 0011722 0011793 0011875 001196* 0012055

0010*29 0008961

000571* 0005*85 00052*5 0005008

0000

0012 0023 0035 0059 0088 0118 01*8

0012013 0178

0011*36 0237

0291 03*0

0006898 0*19

0*82 0538 0592 06*3

000*589 0691

15036 15036 15037 15039 150*1 150** 150*9 15053 15058 15060 15059 16053 15032 1*988 1*962 1*923 1*907 1*921 1*922 1*906 1*8*0 1*788 1*789 1*800 1*810 1*820 1*823 1*831 1*832

REFERENCE

SHIP CODE

LATITUDE

1/10

LONGITUDE

■i/io

°i

MARSDEN

STATION Tl

VIE

ORIGINATOR'S

DEPTH

MAX.

WAVE

WEA- THER CODE

CLOUD CODES

slODC

CTBY CODE

10.

NO.

YEAR

CRUISE NO.

STATION NUMBER

10

BOTTOM

OF S'MPL-S

STATION NUMBER

10*

r

MO DAY HR,1/I0

OIR.

MGI n» SEA

ITP( AM

31 5*0

EV

«

301

N

0*656 W

1*9

36

3* 01 2

12

1965

001

9249 _ _

749

10

?6

1* 5

XI

6 4

0015

WATER

w

ND

BARO- METER

(mbil

AIR TEMP. X.

VIS. COD

NO.

OBS. DEPTHS

SPECIAL

OBSERVATIONS

COLOR CODE

tRANS.

DIR.

OR FORCE

DRY

BULB

WEI

8ULB

26

SIO

098

050

044

B

13

MESSENCI

TIME £

HR 1/10

CAST NO.

CARD

TYPE

DEPTH Iml

T -C

s -I.

SIGMA-T

iREClFIC VOLUME ANOMALT-llO'

SAD

DYN. M.

X 10^

SOUND VELOCITY

0? ml/l

PO<-P ug ■ oi/i

tOTAL-P t,g - oi/l

N03-N

US- o\/\

NO3-N ug - oi/l

SI04-S. wg . ol/l

pH

S

c c

STD

0000

053*

3415

2698

0010843

0000

14713

212

OBS

0000 053* 3*1*7

2698 14713

STO

0010 05*0 3*16

2698 0010826 0011 14717

STO

0020 05*6 3*20

2701 0010606 0022 14722

212

OBS

0025 05*9 3*229

2703 14724

STD

0030 0573 3*28

2704 0010334 0032 14735

STD

0050 0658 3**6

2707 0010047 0052 14775

212

08S

0050 0658 3**62

2707 14775

STO

0075 0716 3*6*

2713 0009523 0077 14804

STD

0100 0772 3*76

2715 0009447 Old 14832

STD

0125 082* 3*83

2712 0009723 0125 14857

212

OBS

0125 082* 3*830

2712 14857

212

OBS

0135 08** 3*8*1

2710 14866

212

OBS

01*5 0775 3*779

2716 14841

STD

0150 0678 3*66

2720 0008984 0148 14802

212

OBS

0160 0515 3**65

2726 14735

STD

0200 0599 3*71

2735 0007667 0190 14779

212

OBS

02*0 0628 3*862

2743 14800

STO

0250 0605 3*86

2746 0006711 0225 14792

STD

0300 0517 3*8*

2755 0005865 0257 14764

212

OBS

T0333 0*83 3*820

2757 14756

STD

0*00 0*82 3*90

2764 0005085 0312 14767

212

OBS

0*15 0*81 3*913

2765 14770

STD

0500 0*61 3*93

2769 0004727 0361 14776

STD

0600 0**2 3*95

2772 0004463 0407 14784

212

OBS

T0610 0**0 3*95*

2773 14785

STO

0700 0*3* 3*95

2773 0004462 0451 14798

STD

0800 0*28 3*95

2774 0004511 0496 14812

STD

0900 0*22 3*95

2774 0004550 0541 14826

212

OBS

T0981 0*17 3*9*5

2775 14837

STD

1000 0*13 3*95

2775 0004515 0587 14839

21

2

OB

B

T10*e

01

.00

349

55

27

T

r

148

42

88

REFERENCE	SHIP CODE	LATITUDE t/10	LONGITUDE ■1/10	If	MASSDEN	STATION T	ME			ORIGINATOR'S	DEPTH	MAX. DEPTH OP S'MPL-		WAVE		WEA- THEH CODE	CLOUD CODES			ODC
CIM CODi	10. NO.				CRUISE NO.	STATION NUMBER	BOTTOM	OBSt.v«..vr.j		NUMBER
10-	r	MO	DAY H	k.\/}0	Ol«.	HGI Hi if*	TYPt *M
31	«<>0	EV	4	316	N	0*732 W		149	37 04	02 311	1965	001	9250	bsBs	11	27	4 3	xo	B	0016
			WATES	WIND	BARD- METER (mbil	AIR TEMP.	•c	VIS COO	NO. OBS. DEPTHS	SPECIAL OBSERVATIONS
	COLOR CODS	tRAVS.	Old.	S«fO (OIC(	DRT BULB	WET BULB
				28	S09	112	044	039	7	10
	MtSKNCt 1 IIMI 01 HR 1/10	CAST NO.	CARD TTPE	DEPTH (ml	I *c	s ■/..	SiGMA-T	SPECIFIC VOLUME ANOMALT-XlO'	SAD OYN. M. . 10=	SOUND VELOCITY	Ol ml/l	POi-P	lOTAL-P vg - 01/1	NOj-N pg - ol/l	NOj-N pg - oi/l	SI04-Si Vfl - 01/1	PH	S C C
			STD	0000	0854	3491	2714	0009337	0000	14849
Oil		OBS	0000 0854 34910 2714		14849
		STD	0010 0967 3494 2714	0009327	0009 14856
		STD	0020 0880 3497 2716	0009320	0019 14862
		STD	0030 0891 3500 2715	0009285	0028 14869
		STD	0050 0913 3506 2716	0009220	0046 14881
Oil		OBS	0064 0926 35091 2717		14888
		STD	0075 0931 3510 2717	0009228	0070 14892
		STD	0100 0943 3513 2717	0009248	0093 14901
		STD	0125 0954 3515 2718	0009254	0116 14910
		STD	0150 0966 3519 2718	0009282	0139 14918
Oil		OBS	0186 0982 35235 2719		14931
		STD	0200 0846 3506 2727	0008490	0183 14880
on		OBS	0239 0624 34831 2741		14797
		STD	0250 0618 3487 2745	0006788	0222 14797
on		OBS	T0267 0606 34905 2749		14796
		STD	0300 0562 3488 2753	0006076	0254 14783
on		OBS	0318 0543 34875 2755		14778
		STD	0400 0503 3495 2765	0004962	0309 14777
on		OBS	0425 0492 34953 2768		14776
		STD	0500 0471 3496 2770	0004592	0357 14780
		STD	0600 0445 3497 2773	0004379	0402 14786
on		OBS	T0640 0436 34967 2774		14789
		STD	0700 0422 3496 2775	0004266	0445 14793
		STD	0800 0404 3495 2776	0004216	0487 14802
on		OBS	0859 0395 34941 2775		14808
		STD	0900 0391 3494 2777	0004216	0629 14813
		STD	1000 0384 3494 2778	0004216	0571 14827
		STD	1100 0382 3494 2778	0004272	0514 14843
		Oil		OBS	TllOO	0382	34944	2778								14843

REFERENCE	SHIP CODE	LATITUDE l/IO	LOF	GITUDE ■1/10	i^	MARSDEN	STATION TIME			ORIGINATOR'S	DEPTH	MAX. DEPTH OF S^MPL*		WAVE		WEA- THER CODE	CLOUD CODES			NODC
CTRY cool	ID. NO.				CRUISE NO.	STATION NUMBER	BOTTOM			NUMBER
	10'	r	MO	DAY HR.1/10	Dl«-	HOT n* SEA	tin AM
31	S4n	EV	4331	H	04801 W	149	38	')4	0? 0	6?	1965	001	9251	3365	12	27	3 2	X7	6 6		0017
			WATER	WIND	BARO- METER Imb.l	AIR TEMP.	^	VIS. COO	NO. OBS. DEPTHS	SPECIAL OBSERVATIONS
	COLOR CODE	IRANS.	DIR.	into OR FORCE	DRY BULB	WET BULB
				26	S25	119	033	028	6	12
	MISUNGP 1 t-AST '»•' =J NO. HR 1/10	CARD TTPE	DEPTH (ml	T X	s v..	SIGMA-T	SfECIMC VOLUME ANOMAI.1-II0'	SAD DYN. M. I 10=	SOUND VELOCITY	Oj ml/l	P04-P ug -ol/i	lOTAL-r 09 - o'/l	NO3-N ug - ol/l	NO3-N MS - Ol/l	SI 04-Si MB - o'/1	pH	S c c
		STD	0000	0727	3456	2706	0010144	0000	14795
062	OBS	0000 0727 34560 2705		14795
	STD	0010 0732 3457 2705	0010172	0010 14799
	STD	0020 0736 3457 2705	0010206	0020 14802
	STD	0030 0741 3458 2705	0010234	0031 14806
052	OBS	0045 0748 34590 2705		14811
	STD	0050 0774 3465 2706	0010205	0051 14823
	STD	0076 0889 3490 2708	0010085	0076 14874
	STD	0100 0980 3512 2710	0009948	0101 14916
062	OBS	0107 1002 35179 2711		14924
062	OBS	0116 1027 35246 2712		14935
	STD	0125 0978 3518 2715	00C9517	0126 14919
062	OBS	0133 0935 35124 2718		14903
062	OBS	0142 0583 34587 2722		14803
	STD	0150 0671 3470 2724	0008594	0148 14800
	STD	0200 0612 3479 2739	0007235	0188 14786
052	OBS	T0224 0592 34818 2744		14782
	STD	0250 0591 3483 2745	0006746	0223 14786
	STD	0300 0590 3486 2748	0005574	0255 14794
062	OBS	0368 0588 34894 2751		14806
	STD	0400 0575 3490 2753	0005223	0320 14805
	STD	0500 0533 3492 2769	0005674	0380 14805
062	OBS	0565 0504 34932 2754		14804
	STD	0600 0482 3494 2767	0005015	0433 14801
	STD	0700 0431 3494 2773	0004510	0481 14796
062	OBS	0764 0405 34942 2776		14797
	STD	0800 0398 3493 2775	0004294	0526 14799
	STD	0900 0381 3492 2775	0004260	0568 14808
062	OBS	T0985 0371 34911 2777		14818
	STD	1000 0370 3491 2777	0004292	0610 14820
	STD	1100 0364 3491 2777	0004305	0553 14834
		05	2	OB	S	T116(		0	563	3*	g	10	21	7	7							14(	)45

89

REFERENCE

SHIP CODE

LATITL

DE

10

^GITUDE "1/10

§1

MARSDEN

STATION T

ME

ORIGINATOR'S |

DEPTH TO

BOTTOM

MAX OEPTI-

OF S'MPL

WAVE

W!A

THER CODE

CLOUD COOES

NODC

CTRY COOi

ID. NO.

SQUARE

(GMT)

YEAR

CRUISE NO.

STATION NUMBER

OBSERVATIONS

STATION NUMBER

1/10

10-

r

MO

DAV IH

R.l/tO

S DM,

MGl PfR SE»

lYPI AM

31

540

EV

4343

N 04

838 W

149

38

04 02 b99

1965

001

9252 2688

11

28

'* ¥*

XI

3 5

0018

WATER

WIND

BARO- METER lmb»l

AIR TEMP, t

VIS. COD

NO.

OSS.

DEPTHS

SPECIAL OBSERVATIONS

COLOR CODE

THAN

DIR.

into

OR fORCE

DRY

BULa

WET

BULB

28

S20

142

oil

006

7

14

HR I/loT

CARD TYPE

DEPTH 1ml

T -C

S •''..

SIGMA-T

SPECIFIC VOLUME ANOMALT-«10'

S A 0

DYN. M

K 10'

SOUND

VELOCITY

02 ml/I

PO4-P

lOIAl-P

vg - Qt/I

NOj-N ug - al/l

NOj-N ua - oi/l

SIO4-S1

uq -ol/l

pH

S

c c

STD

0000

0430 13407

2704

0010281

0000

14669

099

OBS

0000 0430 34074 2704 14669

STD

0010 0586 3437 2709 0009789 0010 14739

STD

0020 0692 3458 2712 0009562 0020 14786

099

OBS

0021 0700 34592 2712 14789

STD

0030 0746 3470 2714 0009410 0029 14809

099

OBS

0032 0755 34718 2714 14814

STD

0050 0775 3473 2712 0009629 0048 14624

STD

0075 0804 3477 2711 0009778 0072 14840

STD

0100 0832 3484 2712 0009716 0097 14856

STD

0125 0860 3494 2715 0009444 0121 14872

099

OBS

0126 0861 34942 2715 14872

099

OBS

0136 0863 34988 2719 14875

STD

0150 0570 3453 2724 0008585 0143 14757

099

OBS

0168 0418 34380 2730 14595

099

OBS

0179 0449 34524 2738 14712

STD

0200 0443 3461 2745 0006592 0181 14714

099

OBS

T0237 0432 34666 2751 14717

STD

0250 0379 3464 2754 0005744 0212 14696

099

OBS

0263 0334 34622 2757 14679

STD

0300 0361 3470 2761 000515i. 0239 14697

STD

0400 0414 3486 2768 0004611 0288 14738

099

OBS

0421 0421 34889 2770 14745

STD

0500 0421 3492 2772 0004346 0333 14759

STD

0600 0422 3496 2775 0004154 0375 14776

099

OBS

0625 0422 34963 2775 14780

STD

0700 0428 3497 2775 0004265 0418 14796

STD

0800 0437 3498 2775 0004409 0461 14816

099

OBS

0813 0438 34978 2775 14819

STD

0900 0395 3493 2776 0004351 0505 14814

099

OBS

0996 0363 34896 2776 14816

STD

1000 0362 3490 2776 0004301 0548 14817

STD

1100 0348 3490 2778 0004218 0591 14828

099

OBS

T1107 0348 34896 2778 14829

REFERENCE

SHrp

CODE

LATITU

DE 1/10

LONGITUDE * '1/10

ii

MARSDEN

SQUARE

STATION TIME (GMTl

YEAR

ORIGINATOR'S 1

DEPTH

TO OTTOM

MAX.| ^^^,

WEA- THER

CODE

CLOUD CODES

NODC STATION NUMBER

CIRY

ID.

NO.

CRUISE

NO.

STATION

NUMBER

OF

S'MPL'

OBSERVATIONS

CODE

10"

T

MO

3AY H

.1/10

Did.

HGT PER St*

TYPE AMI

31

540 EV

4344

N 048

47 W

149

38 c

)4 0

2 1

26

1965

001

9253 I

«?*>

13

26

5 B

XI

3 5

0019

WATER

WIND

9AR0.

METER imbil

AIR TEMP. "C

VIS. CODf

NO.

OBS. DEPTHS

SPECIAL OBSERVATIONS

COLOR llBANS CODE i"i

DIB.

SPIED

08 fO«C(

DRY BULB

WET

BULB

26

S18

159

033

022

8

10

'"' • NO. HH 1/10

CARD TYPE

DEPTH (m>

I *c

s •/.,

SIGMA-T

SPECIFIC VOLUME ANOMaL'-xID'

SAD

DYN. M.

t 10'

SOUND VELOCITY

Oj ml/1

P04-P

TOTAl-P vg . «t/l

NOj-N

ug - ot/l

NOj-N VB - ol/l

SI04-Si

pg - ol/l

PH

s

C C

STD

0000

0030

33&5

2694

0011201

0000

14487

126

OBS

0000 0030 33551 2694 14487

STD

0010 0044 3357 2695 0011124 0011 14495

STD

0020 0057 3360 2697 0010967 0022 14503

STD

0030 0070 3363 2698 0010812 0033 14511

STD

0050 0097 3371 2703 0010362 0054 14528

STD

0075 0131 3383 2711 0009667 0079 14548

STD

0100 0165 3398 2720 0008767 0102 14570

STD

0125 0199 3416 2732 0007562 0123 14591

126

OBS

0135 0212 34236 2737 14600

STD

0150 0265 3438 2744 0006554 0141 14627

126

OBS

0162 0297 34469 2749 14644

126

OBS

0188 0331 34569 2753 14564

STD

0200 0343 3450 2755 0005644 0171 14672

STD

0250 0385 3470 2758 0005366 0199 14700

STD

0300 0420 3479 2762 0005100 0225 14724

126

OBS

T0324 0433 34828 2754 14733

STD

0400 0462 3493 2768 0004629 0273 14759

126

OBS

0432 0466 34954 2770 14767

STD

0500 0425 3492 2772 0004386 0319 14760

STD

0600 0362 3489 2774 0004224 0362 14759

126

OBS

T0550 0369 34885 2775 14761

STD

0700 0370 3490 2775 0004102 0403 14770

STD

0800 0371 3491 2777 0004131 0444 14787

126

OBS

0853 0372 34916 2777 14798

STD

0900 0371 3491 2777 0004217 0486 14804

STD

1000 0357 3491 2777 0004256 0529 14819

126

OBS

T1098 0364 34907 2777 14834

STD

1100 0364 3491 2777 0004327 0571 14834

STO

1200 0360 3491 2777 0004363 0615 14849

12(

3

OB,

>

T1294

03

57

34S

07

27

78

148

64

90

REFERENCE

SHIP CODE

LATITUDE

I/IO

LOF

GITUDE • 'I/IO

^2 1°

MARSDEN

STATION

Tl

VIE

ORIGINATOR'S

DEPTH

MAX.

WAVE

WEA- THER

CODE

CLOUD CODES

ODC

CODE

ID. NO.

CRUISf

NO.

STATION NUMBER

BOTTOM

OF S'MPL'S

NUMBER

-

10"

r

MO

DAY

HR.1/10

□ IR.

Hci n» St 4

Tin AM

31

540

EV

4355

N

04907 W

149

39 04

02

167

1965

001

9254 }172

nl

29

5 (*

XO

0

0020

WATER

WIND

BARO- MEIER (mbsl

AIR TEMP. X.

VIS,

coo

NO. OBS. DEPTHS

SPECIAL OBSERVATIONS

COLOR CODE

IflANS.

OIR.

into

Oft fOBCE

DRY 8ULB

WET

BULB

2U

51*

183

022

017

7

04

MESSENCR CAST II«B „\o. MR 1/10

CARD TYPE

DEPTH Im)

T -C

s •''..

SIGMA-T

SPECIFIC VOLUME ANOMALT-XIO'

SAD DVN. M.

X id'

SOUND VELOCITY

0 2 ml/I

P04-P

lOTAl-P

NOz-N «9-o!/l

NO3-N ug - oi/l

SIO4-S1 ug -ol/l

pH

c

STD

0000

0044

3315

2662

001'.285

0000

14487

167

OBS

0000 0044 33156 2662 14487

STD

0010 0044 3318 2653 0014138 0014 14489

STD

0020 0044 3319 2665 0013998 0028 14491

STD

0030 0044 3321 2666 0013851 0042 14493

STO

0050 0043 3325 2569 0013565 0070 14497

STD

0075 0043 3330 2673 0013202 0103 14501

167

OBS

0075 0043 33296 2673 14501

STD

0100 0062 3366 2702 0010504 0133 14519

167

OBS

0100 0052 33664 2702 14519

STD

0125 0095 3393 2721 0008683 0157 14542

157

OBS

0140

0122

34047

2729

14558

REFERENCE

SHIP

CODE

latitude

1/10

°z

MARSDEN

STATION

Tl

■Al

ORIGINATOR'S

DEPTH

MAX

■

WAVE

WEA- THER CODE

CLOUD CODES

ODC

CHY CODf

ID.

NO.

LONGITUDE

"1/10

CRUISE NO.

STATION NUMBER

TO BOTTOM

OF S'MPL'S

STATION NUMBER

10-

r

MO

DAY

HR.1/10

Dl^ iHCnPE"! SEA

HPf AWT

31

540

EV

4359

N

04920 W

149

39

34

02

180

1965

001

9255 D058

00

26

kkl

XI

2 4

0021

WATER

WIND

BARO- METER (mbil

AIR TEMP, "C

Vli.

COD

NO. OBS. DEPTHS

SPECIAL OBSERVATIONS

COLOR CODE

TRANS.

DIR.

SPtfO

0« FOIICE

DRY BULB

WET BULB

25

SI5

166

022

017

7

02

WEIIENGd [cast IIME 0 NO. HR 1/10

CARD

TYPE

DEPTH Iml

I -c

s v..

SIGMA-T

SPECIFIC VOIUME ANOM At,Y-KIO'

SAD

DVN. M.

X 10^

SOUND VELOCITY

02 ml/1

PO4-P

)ig -ot/l

TOTAl-P

Ufl - ot/l

NOi-N ug-ol/l

NO)-N

ug - ai/1

SI04-S<

vg - ol/l

pH

S

C C

STD

0000

0052

3320

2665

0013998

0000

14492

I

180

OBS 0000 0052 33199 2665 14492 STD 0010 0049 3320 2665 0013976 0014 14492 STD 0020 0047 3320 2665 0013961 0028 14493 STD 0030 0044 3320 2665 0013939 0042 14493

18

0

OB

3

0035

OC

43

33

2

01

26

66

14493

REFERENCE

SHIP

CODE

LATITUDE

1/10

n

MARSDEN

STATION

Tl

-AE

ORIGINATOR'S

DEPTH

1 MAX

■

WAVE

WEA- THER CODE

CLOUD

COOES

>10DC

CTIY

ID. NO.

LONGITUDE * '1/10

YEAR

CRUISE NO.

STATION NUMBER

TO -•■■■ BOTTOM 5.^°;.3

STATION NUMBER

ID-

r

MO

DAY

HR.1/10

OIR,

HGT P£> SEA

I'Pf AM

31

540

EV

4439

N

04920 W

149

49

D4

02

239

1965

001

9256

3082 00

26

5 I2 1 XO

0

0022

WATER

WIND

BARO- METER (trbil

AIR TEMP. "C

COD

NO.

OBS. DEPTHS

SPECIAL OBSERVATIONS

COLOR CODE

TRANS.

DIR.

SPEtO

OS FORCE

DRY BUL8

WET

BULB

23

514

176

017

006

B

02

TIME 0/*^; HR 1/10

CARD TYPE

DEPTH (ml

r -c

s •/..

SIGMA-T

SKCIFIC VOLUME ANOMALY-IIO'

SAD

DYN. M. X 10^

SOUND VELOCITY

0; ml/I

P04-P

V9-0./I

TOTAl-P

w9-ot/l

N02-N

119 -ol/l

N0)-N wg - ol/l

SIO«-S.

ug - ol/l

pH

i

C C

STD

0000

0012

3312

2661

0014389

0000

14472

239

OBS 0000 0012 33122 2661 14472 STD 0010 0013 3315 2663 0014200 0014 14475 STD 0020 0014 3317 2665 0014004 0028 14477 STD 0030 0015 3320 2667 0013816 0042 14480 STD 0050 0017 3325 2671 0013432 0070 14485

23

9

OB

3

0050

OC

17

33

2

49

26

7

14^

♦ 85

91

REFERENCE

SHIP

CODE

ii

MARSDEN

STATION

Tl

WE

ORIGINATOR-S

DEPTH

MAX.

WAVE

WEA- THER CODE

CLOUD CODES

GDC

cmt

coot

ID. NO.

LATITUDE

l/IO

LONGITUDE

"1/10

CRUISE NO.

STATION NUMBER

BOTTOM

OF S'MPL-S

NUMBER

10"

r

MO

DAY

HRJ/IO

OIR.

Hci nt SEA

iin *w

31

S4n

FV

'►43 7 N

04905 W

149

49 04

03

D15

1965

001

9257 3128

ni

?3

5 2

xo

0

0023

WATER

WIND

BARO- METER (mb»l

AIR TEMP. T

VIS. COD

NO.

DBS.

DEPTHS

SPECIAL OBSERVATIONS

COLOR CODE

TKANS.

DIR.

SPttO

o«

fOHCt

DRY BULB

WET BULB

20

508

196

017

7

04

MESSENr,ll[cAST I.ME O.^N0.

HH VIO 1

CARD TYPE

DEPTH (m)

T -C

s v..

S1GMA-T

SMCinC VOLUME ANOMAU-XIO'

5 A D

DYN. M.

X 10^

SOUND VELOCITY

Oi ml/I

PO*-P VS - ol/l

lOTAL-P vg - Bl/1

NOi-N ug - ol/l

NO)-N )>g - Dl/1

SIO4-S1

na-o'/i

pH

I C

C

1

STO

oooo

-0019

3320

2669

0013655

0000

14459

015 015 015

OBS STD STD STD

OBS STD

OBS STO

OBS

0000 0010 0020 0030 0035 0050 0055 0075 0095

-0019

-0020

-0021

0008

0016

00*4

0063

33200

3320

3321

33213

3340

33458

3363

33726

2669 2569 2669 2669 2670 2683 2688 2700 2707

0013619 0013590 0013554

0014 0027 0041

0012236 0067

0010664 0095

14459 14461 14462 14464 14464 14483 14488 14506 14520

LATITUDE

1/10

LONGITUDE

'l/IO

ORIGINATOR'S

31

4435 N 04852 W

149 48 04 03 335 1965 001 925

SfEtD

OR FO»C!

200

AIR TEMP. "C

032

3420 I 04 I 26 K

07

0024

035

035 035

035

STD

OBS STD STD

OBS STO STD STD

OSS STD STD STD STD

OBS

OBS STD

OBS STO

OBS

0000 0000 0010 0020 0029 0030 0050 0075 0079 0100 0125 0150 0200 0227

T0246 0250

T0296 0300

T0395

-0018

-0020

-0022

-0024

-0023

0005

0043

0049

0088

0134

0180

0273

0323

0410

0405

0363

0364

0392

3323

33230

3324

3327

33301

3331

3348

3367

33701

3380

3392

3406

3438

34579

34728

3473

34727

3473

34827

2671 2671 2672 2674 2677 2678 2590 2703 2705 2711 2718 2725 2744 2755 2758 2759 2763 2763 2768

0013430

0013341 0013100

0012787 0011612 0010354

0009524 0009015 0008291 0006653

0005354 0004953

0000

0013 0027

0040 0054 0091

0115 0140 0161 0199

0229 0254

14460 14460 14461 14462 14463 14464 14482 14506 14510 14533 14559 14585 14539 14558 14710 14708 14598 14599 14728

92

REFERENCE	SHIP CODE	LATITUDE I/IO	LONGITUDE =y ■ "1/10 -	MARSDEN	STATION	Tl	WE			ORIGINATOR'S	DEPTH	MAX. DEPTH OF S-MPL*		WAVE		WEA- THER CODE	CLOUD COOES		NODC
CTST CODt	10. NO.				CRUISE NO.	STATION NUMBER	BOTTOM		NUMBER
10-	r	MO	DAT	HH.1/10	OlR.	HGI PER SE*	r»Pi *w
31	540	FV	4	431	N	04(	139 W 1	149	48 04	03	D54	1965	001	9259 20X2	12	20	3 5	xo	0	0025
			WATER	WIND	BARO- METER [mbil	AIR TEMP, "C	^»-dEs	SPECIAL OBSERVATIONS
	COLOR CODE	TRANS.	OIR.	S«ED OR FORCE	DRY BULB	WET eULB
				20	S12	200	022	oil	7	\|09
	MESSENGR 1 IIME or HR 1/10	CAST NO.	CARD TYPE	DEPTH (ml	I -c	s ■/..	SiGMA-T	SMClfIC VOLUME *NOMAH-«10'	SAD DYN, M. t io3	SOUND VELOCITY	Ol ml/l	PO4-P VB - o'/l	TOTAl-P vB-ot/l	NOj-N ug- ol/l	NO3-N iig - ol/l	SIO^-SI lifl - 01/1	pH	S C C
			STD	0000	0154	3390	2715	0009288	0000 1 14547 1
054		OBS	0000	0154 33898 2715 14547
		STD	0010	0176 3397 2719 0008895 0009 14560
		STD	0020	0198 3405 2723 0008451 0018 14572
		STD	0030	0219 3412 2727 0008082 0026 14584
		STD	0050	0259 3425 2734 0007427 0042 14606
		STD	0075	0307 3440 2742 0006721 0059 14633
		STD	0100	0351 3454 2749 0006091 0075 14658
05A		OBS	0102	0354 34550 2750 14660
		STD	0125	0397 3467 2755 0005588 0090 14683
		STD	0150	0436 3478 2759 0006193 0103 14705
ObU		OBS	0182	0471 34890 2764 14727
		STD	0200	0470 3490 2765 0004716 0128 14730
		STD	0250	0468 3493 2768 0004510 0151 14737
		STD	0300	0466 3497 2771 0004303 0173 14745
054		OBS	T0303	0466 34967 2771 14746
		STD	0400	0435 3495 2773 0004143 0215 14749
054		OBS	0402	0434 34954 2773 14748
		STD	0500	0404 3492 2774 0004124 0257 14752
		STD	0600	0373 3489 2775 0004105 0298 14755
054		OBS	T0602	0372 34891 2775 14755
		STD	0700	0366 3489 2775 0004152 0339 14768
		STD	0800	0360 3488 2776 0004200 0381 14782
054		OBS	0804	0360 34884 2776 14783
		STD	0900	0360 3490 2777 0004168 0423 14799
		STD	1000	0361 3490 2777 0004258 0465 14816
054		OBS	T1026	0361 34906 2777 14821
		STD	1100	0359 3491 2778 0004268 0508 14832
		STD	1200	0355 3491 2778 0004287 0550 14847
		054		OBS	T1208	0355	34909		2778								14849

LATITUDE

1/10

LONGITUDE * "l/IO

STATION TIME

ORIGINATOR'S

NODC STATION NUMBER

04756 W

149 |47 104 103 llOO 11965 |001|9260

S09

196

028

3383 I 11 I 25 B

0026 1

1R I/IO

DEPTH 1ml

SPECIFIC VOLUME

SAD OYN. M.

X 10'

100

100 100 100

100 100

100

100 100

100

STD

OBS STD

OBS STD STD STD STD

OBS

OBS STD

OBS STD STD

OBS STD

OBS STD STD

OBS

0000 0000 0010 0019 0020 0028 0030 0034 0050 0075 0100 0125 0135 0144 0150 0153 0200 0250

T0290 0300 0386 0400 0500

T0583 0600 0700 0779 0800 0900

T0992 1000 1100

T1150

0880 0880 0876 0871 0870 0865 0865 0864 0855 0841 0824 0807 0799 0792 0785 0782 0658 0556 0496 0487 0430 0429 0417 0404 0399 0375 0362 0362 0360 0358 0359 0369 0377

3501

35010

3501

35005

3500

34993

3499

34979

3497

3494

3491

3487

34857

34842

3483

34825

3484

3486

34866

3487

34872

3488

3491

34924

3492

3490

34886

3489

34895

3490

3492

34931

2718 2718 2718 2719 2719 2719 2719 2718 2719 2718 2719 2718 2718 2718 2718 2718 2737 2752 2760 2761 2767 2768 2772 2774 2775 2775 2776 2776 2776 2777 2777 2778 2778

0008984 0000

0008944 0009

0008947 0018

0008966 0027

0009003 0045

0009065 0067

0009084 0090

0009178 0113

0009201 0136

0007458 0006085

0004628 0004371

0004191 0004161

0004194 0004227

0004236 0004292

0178 0211

0005252 0240

0289 0334

0377 0419

0460 0503

0545 0588

14860 14860 14860 14859 14859 14858 14859 14859 14858 14856 14854 14851 14849 14848 14846 14845 14805 14772 14754 14752 14743 14745 14757 14765 14766 14772 14780 14783 14799 14814 14816 14837 14849

93

RSFEHENCE	SKIP CODE	LATITUDE I/IO	LONGITUDE 5^	MARSDEN	STATION	TIME			ORIGINATOR'S	DEPTH	MAX.		WAVE		WEA- THER CODE	CLOUD CODES			NODC
cr«T CODE	ID. NO.				CRUISE NO.	STATION NUMBER	TO BOTTOM	OF S'MPL'S			STATION NUMBER
10"	r	MO	DAY	HR.1/10	DIP.	HOT PEP SEA	lypE AM
31	540	FV	4	417	N	04"	ri7 w 1	149	47 04	03	152	1965	001	9261 3749	12	15	3 2	xo	0	0027
		WATER	WIND	BARO- METER (mb)l	AIR TEMP. "C	^"■dEs	SPECIAL OBSERVATIONS
	COLOR CODE	IWN5.	OIR.	SPEED OP FORCE	DRY BULB	WET BULB
		03		16	S17	179	128	117	B	10
	MESStNGR TIME c HR 1/10 '	CAST NO.	CARD TYPE	DEPTH Iml	T "C	s •/..	SIGMA-T	SPECIFIC VOLUMt ANOMAIT-XIO'	SAD DVN. M. xioi	SOUND VELOCITY	Oj «l»l/l	POj-P vg - oi/l	rOTAL-P VB - °>/l	NOj-N us - PI/I	NOj-N pg - ot/1	SIO4-SI PS - ol/l	pH	S C C
			STD	0000	1082	3539	2713	0009425	0000	14938
145		OBS	0000	1082 35391 2713 14938
		STD	0010	1082 3539 2713 0009448 0009 14940
		STD	0020	1081 3539 2713 0009461 0019 14941
		STD	0030	1080 3539 2713 0009484 0028 14943
		STD	0050	1079 3539 2713 0009520 0047 14946
		STD	0075	1078 3539 2713 0009570 0071 14949
		STD	0100	1077 3538 2714 0009620 0095 14953
		STD	0125	1075 3538 2714 0009572 0119 14956
		STD	0150	1074 3538 2714 0009714 0144 14960
		STD	0200	1071 3538 2714 0009814 0192 14967
		STD	0250	1058 3537 2714 0009904 0242 14974
145		OBS	0256	1058 35373 2714 14975
145		OBS	0265	1066 35375 2715 14976
145		OBS	0293	1020 35232 2712 14962
		STD	0300	0961 3515 2715 0009845 0291 14941
146		OBS	0307	0909 35079 2718 14922
145		OBS	T0375	0740 34979 2737 14867
		STD	0400	0707 3498 2741 0007409 0377 14859
		STD	0500	0595 3498 2756 0006047 0445 14831
152		OBS	T0594	0516 34975 2756 14814
		STD	0600	0513 3498 2766 0005131 0500 14814
		STD	0700	0468 3497 2771 0004763 0550 14812
152		OBS	0787	0438 34957 2773 14814
		STD	0800	0435 3496 2774 0004542 0596 14815
		STD	0900	0413 3495 2775 0004449 0641 14822
152		OBS	T0999	0397 34935 2776 14832
		STD	1000	0397 3494 2776 0004423 0586 14832
		STD	1100	0387 3493 2777 0004422 0730 14844
		152		OBS	T1165	0383	34930		2777								14854

REFERENCE

SHIP CODE

LATITUDE

1/10

LONGITUDE * '1/10

if

MARSDEN

STATION

TIME

ORIGINATOR'S

DEPTH

MAX.

WAVE

WEA- THER CODE

CLOUD CODES

JOOC

CTRY CODE

ID. NO.

CRUISE NO.

STATION

NUMBER

TO BOTTOM

OF S'MPL'5

STATION

NUMBER

10*

r

MO

DAY

HR.I/10

DIR-

MGT pen SEA

fyPE AM

31

540

EV

C

408

N

04637 W

149

46

H

03

196

1965

noi

9262

3840

12

14

2 I2 1x1

6 7

0028

WATER

WIND

BARO- METER

AIR TEMP. "C

coo

NO.

OBS. DEPTHS

SPECIAL OBSERVATIONS

COLOR

CODE

IM.NS.

DIR.

SPttD

OK fOBCE

DRY BULB

WET BULB

14

S20

142

139

122

8

07

MESSENGR

TIME 0

HR 1/10

CAST NO.

CARD TYPE

DEPTH Iml

T -C

s v..

SIGMA-T

SPfClfIC VOLUME ANOMALI-X'O'

SAD

DYN. M.

K 10^

SOUND

VELOCITY

O3 ml/l

POi-F"

lOIAl-P

NO3-N

uS-ol/l

NOj-N wg - ol/l

SIO4-S. vg - ol/l

pH

s c c

STD

0000

1137

3549

2711

0009660

0000

14959

196

OBS STD STD STD STD STD STD STD STD STD STD STD

0000 1137 35489 2711 14959 0010 1136 3549 2711 0009668 0010 14960 0020 1136 3549 2711 0009700 0019 14962 0030 1135 3549 2711 0009707 0029 14963 0050 1134 3549 2711 0009747 0049 14965 0075 1133 3549 2711 0009798 0073 14970 0100 1132 3549 2711 0009842 0097 14974 0125 1131 3549 2711 0009894 0122 14977 0150 1130 3548 2712 0009945 0147 14981 0200 1128 3548 2712 0010045 0197 14989 0250 1127 3548 2712 0010165 0247 14996 0300 1125 3548 2712 0010276 0299 15004

196

OBS STD

0371 1125 35475 2712 15015 0400 1125 3548 2712 0010522 0403 15020

196

OBS STD

0410 1125 35476 2712 15022 0500 0752 3507 2742 0007553 0493 14894

196

OBS STD STD

T0561 0582 34902 2752 14835 0600 0561 3492 2756 0005158 0561 14833 0700 0512 3496 2755 0005356 0619 14830

196

OBS STD STD

0759 0485 34975 2769 14829 0800 0464 3497 2771 0004793 0670 14827 0900 0424 3495 2774 0004553 0717 14827

195

OBS STD STD

T0978 0402 34937 2775 14830 1000 0397 3493 2776 0004467 0762 14832 1100 0385 3493 2777 0004424 0805 14844

19

6

OB

5

T1154

03

85

34

9

28

27

7

1

148

53

94

REFERENCf	SHIP CODE	LATITUDE I/IO	LONGITUDE 'I/IO	ii	MARSDEN	STATION	TIME			ORIGINATOR'S	DEPTH	MAX. DEPTH OF S'MPL'S		WAVE		WEA- THER CODE	CLOUD CODES			gone
coot	ID. NO.				CRUISE NO.	STATION NUMBER	TO BOTTOM			STATION NUMBER
10*	1"	MO	DAY	HR.l/10	0I«.	HGI Ft« SEA	M'l AM
31	640	EV	4400	N	04555 W		149	45 04	03	239	1965	001	9253 3750	13	15	7 2	Xft	5 8	0029
			WATER	WIND	BARO- METER (mbil	AIR TEMP. X	DEPTHS
	COLOR CODE	ia*Ns.	OIR.	SPEED Ot fOBCE	DRY BULS	WET BULB	OBSERVATIONS
			13	524	095	133	122	2	108
	MEiltNC IIMI HR 1/1	» CAST ^ NO.	CARD TYPE	DEPTH Iml	r X	s •/..	SIGMA-T	SPECIFIC VOIUME ANOMALT-IIO'	SAD OYN. M. X 10=	SOUND VELOCITY	Oj ml/l	PO*-P VB-o'/l	TOTAL-P ipg - oi/i	NOl-N wg - al/I	NOj-N ng - oi/l	SI 04-Si llfl - ot/l	pH	s c c
			STD	0000	1054	3533	2713	0009406	0000	14928
	239	OBS	0000 1054 35329 2713 14928
			STD	0010 1053 3533 2713 0009442 0009 14929
			STD	0020 1051 3532 2713 0009454 0019 14930
			STD	0030 1049 3532 2713 0009473 0028 14931
			STD	0050 1045 3531 2713 0009511 0047 14932
			STD	0075 1038 3530 2714 0009517 0071 14934
			STD	0100 1029 3529 2715 0009497 0095 14935
	239	OBS	0111 1024 35287 2715 14934
			STD	0125 1014 3528 2717 0009385 0118 14933
			STD	0150 0997 3527 2719 0009222 0142 14931
			STD	0200 0961 3524 2722 0008974 0187 14926
			STD	0250 0926 3519 2724 0008879 0232 14920
			STD	0300 0891 3512 2725 0008935 0276 14914
	239	OBS	0304 0888 35118 2725 14914
			STD	0400 0666 3494 2744 0007128 0357 14842
	239	OBS	0405 0557 34938 2745 14839
			STD	0500 0567 3494 2757 0005934 0422 14819
			STD	0600 0497 3495 2766 0005147 0477 14807
	239	OBS	T0613 0490 34948 2767 14805
			STD	0700 0465 3495 2770 0004783 0527 14811
			STD	0800 0441 3495 2773 0004585 0574 14817
	239	OBS	T0a26 0435 34952 2774 14819
			STD	0900 0419 3496 2776 0004403 0619 14825
			STD	1000 0400 3496 2778 0004250 0662 14834
	239	OBS	T1062 0391 34963 2779 14840
			STD	1100 0385 3495 2779 0004203 0704 14844
			STD	1200 0375 3494 2778 0004316 0747 14857
		239	OBS	T1273		0371	34920		2771									14867

REFERENCE

SHIP CODE

LATITU

DE

L0^

GITUOE * '1/10

if

MARSDEN

STATION T

ME

ORIGINATOR'S

DEPTH

MA>

WAVE

WEA- THER CODE

CLOUD COOES

CRY

coot

to.

NO.

CRUISE NO.

STATION NUMBER

TO BOTTOM

Of

S'MPl'S

STATION NUMBER

1/10

10*

r

MO

DAY 1-

t.1/10

Dt«.

HGI nt SEA

un AM

31

540

EV

i

430

N 04'

>55 W

149

45

D4

04 0

42

1965

001

9264 _ _

3749

11

16

k I

X4

7 8

0030

WATER

WIND

AIR TEMP. -C

COD

NO.

OBS. DEPTHS

SPECIAL OBSERVATIONS

COLOR CODE

IRANS.

DIR.

SPEED

OR fOKCE

METER

lmb»)

DRY BULB

WET 6UIB

18

518

044

111

110

6

11

MESSfNCa

IIWI c HH 1/10

CAST NO.

CARD TYPE

DEPTH Iml T *C

s v..

SlGMA-T

SPECIFIC VOlUMt

ANOMALY~lia'

SAD

DYN. M.

X 103

SOUND

VELOCITY

Ol ml/I

PO«-P

Vt ■ 81/1

lOTAL-P

NOj-N

Ufl - Ol/I

NOj-N

we - oi/i

SlO^-Si

Ufl - Ql/I

pH

S

c c

STD

0000 0451

3418

2710

0009684

0000

14679

042

OBS STD

STD

0000 0451 34182 2710 14679 0010 0457 3422 2712 0009575 0010 14688 0020 0475 3426 2714 0009371 0019 14593

042

OBS STD

0025 0475 34273 2715 14695 0030 0473 3428 2715 0009210 0028 14694

042

OBS STD

STD STD

0039 0458 34300 2718 14694 0050 0457 3431 2720 0008836 0045 14691 0075 0434 3432 2723 0008545 0068 14686 0100 0415 3433 2725 0008299 0089 14682

042

OBS STD STD STD

0121 0402 34343 2728 14680 0125 0401 3434 2729 0008076 0110 14681 0150 0395 3435 2730 0007979 0130 14683 0200 0384 3437 2732 0007793 0169 14686

042

OBS

STD

0215 0380 34371 2733 14687 0250 0418 3447 2737 0007423 0207 14710

042

OBS STD

T0262 0428 34504 2738 14717 0300 0443 3457 2750 0005248 0241 14732

042

OBS STD STD

0371 0457 34884 2765 14752 0400 0446 3489 2757 0004781 0297 14752 0500 0413 3489 2771 0004482 0343 14755

042

OBS

STD STD

0584 0392 34893 2773 14760 0500 0389 3489 2773 0004272 0387 14762 0700 0372 3490 2775 0004105 0429 14771

042

OBS STD STD

0737 0357 34906 2777 14775 0800 0355 3491 2777 0004103 0470 14785 0900 0362 3491 2777 0004135 0511 14800

042

OBS STD STD

T0946 0350 34907 2777 14807 1000 0357 3490 2778 0004183 0552 14815 1100 0351 3490 2778 0004232 0594 14829

04

2

OB

3

T1108

o:

50

34

8

99

27

li

148

30

95

■ SHIP CODE

31 5401 EV

LATITUDE

VIO

DAY HR.1/)I

149 155 104 104 |092 11965 |001|9265

SPtEO

OR

fOBCe

S08

ORIGINATOR'S

BARO- METER (mbt)

037

AIR TEMP. X.

122 117

3596 I 12 I 16 6

WEA- THER CODE -

NOOC STATION NUMBER

0031

SPECIFIC VOlUMt

SOUND VELOCITTf

092

092 092

092

STD

OBS STD STO

OBS STD STD

OBS STO

OBS STD STD STD

OBS STD

OBS STD STD

OBS

0000 0000 0010 0020 0027 0030 0050 0053 0075 0090 0100 0125 0150 0191 0200 0250 0300

T0318 0400 0425 0500 0600

T0641 0700 0800 0851 0900 1000

T1072 1100 1200

T1249

0915 0915

0907 0880 0851 0818 0638 0557 0518 0477 0474 0467 0462 0458 0459 0465 0470 0472 0447 0439 0408 0378 0369 0364 0358 0357 0359 0364 0357 0365 0356 0348

3494

34938

3483

3473

3443P

3465

3451

34452

3442

34393

3440

3443

3446

34533

3457

3474

3487

34897

3494

34947

3492

3490

34891

3489

3490

34896

3490

3491

34920

3492

3491

34903

2707

2599

2595

2577P

2599

2714

2719

2722

2724

2725

2728

2731

2737

2740

2753

2755

2771

2772

2774

2775

2776

2777

2778

0010052

0010749 OOIllOO

0010795 0009435

0008396 0008122 0007870

0007065 0005910 0005057

0004195 0004105

0004098 0004094

0004147 0004203

0004255 0004292

0000

0010 0021

0032 0053

0008706 0075

0097 0117 0137

0175 0207 0234

0004383 0282

0324 0366

0407 0448

0489 0531

0573 0516

148 72 14872 14869 14859

14837 14768 14737 14722 14707 14708 14709 14712 14718 14720 14733 14745 14750 14753 14754 14753 14757 14760 14768 14782 14790 14799 14818 14831 14835 14848 14853

SHIP CODE

LATITUDE

1/TO

STATION TIME

ORIGINATOR'S

HGtjPEP SEA

WEA- THER CODE ■

31

EV

04555 W

149 155 104 104 1140 11955

SPEED

OR FORCE

001 I 9266

BARO- METER

061

5155 I 11 I 19 b

0032

140

140 140

140 140 140 140

STD

OBS STD STD STD

OBS STD

OBS STD STD STD

OBS

OBS STD STD STD

OBS STD STO

OBS STD STD

OBS

0000 0000 0010 0020 0030 0047 0050 0073 0075 0100 0125 0126 0148 0150 0200 0250

T0295 0300 0400 0429 0500 0600

T0542 0700 0800 0852 0900 1000

T1084

0480 0480 0476 0471 0457 0459 0436 0304 0304 0302 0299 0299 0560 0559 0544 0523 0501 0498 0430 0416 0404 0389 0384 0377 0357 0363 0360 0356 0355

3445

34460

3445

3446

34457

3444

34327

3433

3434

34337

34802

3481

3488

3492

34950

3495

3492

34917

3492

34920

3491

34905

3491

34912

2729 2729

2730 2730 2731 2731 2732 2737 2737 2737 2738 2738 2747 2748 2755 2761 2755 2756 2771 2772 2774 2775 2775 2775 2777 2777 2778 2778 2778

0007901

0007872 0007835 0007806

0007243 0007202 0007150

0005353 0005725 0005241

0004783 0004340

0004166 0004086

0004109 0004084

0004090 0004127

0000

0008 0016 0024

0007641 0039

0058 0076 0094

0111 0141 0168

0193 0239

0281 0323

0354 0405

0445 0487

14695 1*695 14595 14694 14694 14694 14584 14631 14631 14634 14637 14637 14756 14756 14759 14750 14759 14758 14746 14745 14752 14762 14767 14773 14786 14793 14799 14814 14828

96

REFERENCE	SHIP CODJ	LATTTUDE 1/10	LONGITUDE • -i/io	■^5	MARSDtN	STATION Tl	ME			ORIGINATOR'S 1	DEPTH TO lOTTOM	MAX. DEPTH OF S'MPL'		WAVE	1	WEA- THER CODE	CLOUD COOES			NODC
CItT	ID. NO.	SQUARE	IGMTI	YEAR	CRUISE NO.	STATION NUMBER	OBSt-.-..wr..		STATION NUMBER
CODI	10-	r	«51	OAT H	R.1/10	Da.	HOT n* it*	"" **"
31	B,j,n	FV/	^<i7Q	N	04f^'^4 W		\U9	56 04	04 174	1965	001	9267	bl4S	1?	18	4 I4	X2	4 6		0033
			WATER	WIND	BARO- METER	AIR TEMP.	■^_._	VIS. CODI	NO. OBS. DEPTHS	SPECIAL OBSERVATIONS
	COLOR CODE	IRANI	DUE.	into Ol fOtCI	DRY BULR	WET flULR
				14	S06	044	061	056	6	14
	MlSifNM CAST Ti"t 9, NO. HR 1/10	CARD TYPE	DEPTH On)	T V	s •/..	SIGMA-T	SMCinC VOLUM( ANOMAL'-IIO'	SAD DYN. M. I IjJ	SOUND vELOCirr	Ol ml/1	PB - o'/l	rOTAi-f ,g - B./l	NQi-N vg - oi/l	NO3-N vg - at/I	SI 0*-Si „g - oI/l	pH	C
		STD	0000	0454	3442	2729	0007957	0000 U4683
174	OBS	0000 0454 34416 2729		14683
	STD	0010 0398 3441 2734	0007445	0008 14661
17*	OBS	0010 0398 34410 2734		14661
	STD	0020 0385 3442 2736	0007289	0015 14658
	STD	0030 0374 3442 2737	0007155	0022 14655
	STD	0050 0355 3443 2740	0006923	0036 14650
174	OBS	0060 0348 34434 2741		14649
	STD	0075 0345 3445 2742	0006722	0053 14550
	STD	0100 0340 3447 2744	0006551	0070 14652
	STD	0125 0335 3449 2746	0006374	0086 14655
174	OBS	0125 0335 34485 2746		14655
	STO	0150 0443 3473 2755	0005635	0101 14708
174	OBS	0150 0443 34731 2755		14708
174	OBS	0165 0432 34717 2755		14705
174	OBS	0180 0436 34734 2756		14710
	STD	0200 0458 3481 2759	0005260	0128 14723
174	OBS	T0225 0477 34872 2762		14736
	STD	0250 0476 3490 2764	0004848	0154 14740
174	OBS	T0298 0475 34925 2767		14748
	STO	0300 0473 3492 2766	0004718	0178 14747
174	OBS	0397 0414 34899 2771		14739
	STD	0400 0414 3490 2771	0004320	0223 14739
	ST3	0500 0399 3490 2773	0004215	0265 14749
174	OBS	T0596 0387 34909 2775		14760
	STO	0600 0386 3491 2775	0004127	0307 14751
	STD	0700 0374 3490 2776	0004135	0348 14772
174	OBS	0790 0365 34896 2776		14783
	STD	0800 0365 3490 2776	0004160	0390 14784
	STD	0900 0360 3490 2777	0004184	0432 14799
	STD	1000 0355 3490 2777	0004214	0474 14814
174	OBS	T1003 0355 34897 2777		14814
	STD	1100 0356 3490 2777	0004298	0515 14831
174	OBS	T1176 0360 34898 2777		14846
REFERENCE	1	OF 1/10	lot	GITUDE ■ -1/10	il	MARSOEN SQUARE	STATION TIME IGMTt	TEAR	ORIGINATOR'S \|	DEPTH TO	MAX, DEPTH OF S-MPL*	WAVE OBSERVAnONS	WEA- THER CODE	CLOUD CODES		NODC
CTIY	ID. NO.	CODE	LATITU	CRUISE NO.	STAT NUV	ON	STATION NUMBER
coot	10-	T	MO	DAY H	R.l/10	BER	S D«.	HClj «t SEA	tin AW
31	540	EV	4528	N	04718 W		149	57	34	04 2	17	1965	001	9268	1920	10	14	u	XI	3 5	0034
			WATER	WIND	lARO- MITER tffib»l	AIR TEMP.	■c	VIS. COD!	NO. OBS. DEPTHS	SPECIAL OBSERVATIONS
	COLOR CODE	TRANS.	DIR.	smo o« FOICt	DRY ■ ULR	WET BULB
				14	S16	034	057	061	7	14
	MtlttNCt icAST "•" 0. NO. HR 1/10	CARD TYPE	DEPTH In)	T t	s •/..	SIGMA-T	SWCifiC VOLUME ANOMALT-110'	SAO DYN, M .loJ	SOUND VELOCin	Oj ml/l	PO*-P	lOTAL-f ■S - o'/l	NO;-H ■.g - Ol/I	NO3-N i«g - oi/l	SI o*-s. vg - Qt/t	pH
		STD	0000	0550	3437	2714	0009325	0000	14722
217	OBS	0000 0550 34374 2714		14722
	STD	0010 0548 3438 2715	0009294	0009 14723
	STD	0020 0546 3438 2715	0009262	0019 14724
	STO	0030 0544 3436 2716	0009230	0028 14725
	STD	0050 0541 3439 2717	0009160	0046 14727
217	OBS	0070 0537 34396 2717		14729
	STD	0075 0532 3441 2719	0008941	0069 14728
217	OBS	0096 0511 34416 2722		14723
	STD	0100 0495 3440 2723	0008627	0091 14717
217	OBS	0105 0474 34389 2724		14709
	STD	0125 0368 3431 2729	0008034	0112 14666
217	OBS	0125 0368 34306 2729		14666
217	OBS	0143 0496 34583 2737		14726
	STD	0150 0507 3462 2739	0007173	0131 14733
217	OBS	0176 0529 34717 2744		14747
	STD	0200 0524 3475 2747	0006464	0155 14750
217	OBS	T0202 0524 34760 2748		14750
217	OBS	T0224 0539 34854 2753		14761
	STD	0250 0510 3486 2757	0005535	0195 14754
	STD	0300 0464 3487 2763	0004989	0221 14743
217	OBS	0320 0449 34880 2766		14740
	STD	0400 0428 3490 2770	0004467	0268 14745
217	OBS	T0476 0412 34916 2773		14751
	STO	0500 0408 3492 2773	0004233	0312 14753
	STD	0600 0395 3491 2774	0004205	0354 14764
217	OBS	0644 0390 34911 2775		14770
	STO	0700 0387 3491 2775	0004208	0396 14778
	STD	0800 0379 3491 2776	0004199	0438 14791
217	OBS	T0836 0376 34913 2776		14796
	STD	0900 0370 3491 2777	0004205	0480 14804
	STD	1000 0358 3490 2777	0004254	0522 14815
		21	7	OB	S	T100(	)	0	358	3<	tt	96	21	7	7						14(	)15

97

REFERENCE

SHIP CODE

LATITUDE

1/10

LONGITUDE * -1/10

1^

°2

WARSDEN

STATION

TR

n

ORIGINATOR'S 1

DEPTH

MAX.

WAVE

WEA- THER CODE

CLOUD CODES

*ODC

crur CODE

ID.

NO.

CRUISE NO.

STATION

TO

OF S'MPL-S

STATION NUMBER

10*

r

MO

DAY

HR.1/10

OiR.

«GI PER SEA

nPE .M

31

540

EV

4

529

N

04743 W

149

57 04

05

004

1965

001

9269 1390

13

20

i 2

XI

0035

WATER

WIND

8AR0-

METER

Imbil

AIR TEMP. T;

VIS- CODE

NO. OBS.

DEPTHS

SPECIAL OBSERVATIONS

COLOR CODE

IftANS.

SPEfO OIH. oa foaCE

DRY

flULE

WET

BULB

1

15 S15

027

080

070

7

09

HH 1/10

CAST NO.

CARD

TYPE

DEPTH Iml

T -c

s */..

SIGMA-T

SPECIFIC VOLUME ANOMAll-xlO'

SAD

DYN. M.

11 10=

SOUND VELOCITY

Ol ml/I

PO4-P

TOTAL-P ug - Ql/1

NO2-N us - ol/l

NO3-N pg - ol/l

SIO4-S. tig - oi/l

PH

S

c c

STD

0000

0198

3413 I2730

0007837

0000

14570

004

OBS

0000 0198 34130 2730 14570

STD

0010 0191 3413 2730 0007782 0008 14568

STD

0020 0186 3413 2731 0007742 0016 14568

STD

0030 0183 3413 2731 0007716 0023 14568

00*

OBS

0043 0182 34135 2731 14570

STD

0050 0192 3417 2734 0007509 0039 14576

STD

0075 0225 3430 2741 00067-8 0056 14596

STD

0100 0256 3441 2748 0006222 0073 14616

STD

0125 0284 3451 2753 0005723 0088 14633

STD

0150 0309 3459 2757 0005362 0101 14649

004

OBS

0166 0324 34638 2760 14659

STD

0200 0353 3470 2762 0004991 0127 14678

STD

0250 0384 3478 2765 0004747 0152 14700

004

OBS

T0294 0402 34829 2767 14716

STD

0300 0402 3483 2767 0004608 0175 14717

STD

0400 0398 3486 2770 0004436 0220 14732

004

OBS

0431 0396 34871 2771 14736

STD

0500 0384 3488 2773 0004229 0264 14743

STD

0600 0371 3488 2774 0004177 0306 14754

004

OBS

T0650 0366 34886 2775 14760

STD

0700 0364 3489 2775 0004142 0347 14768

STD

0800 0361 3489 2776 0004187 0389 14783

004

OBS

0868 0359 34888 2776 14793

STD

0900 0359 3489 2776 0004230 0431 14799

STD

1000 0358 3489 2776 0004282 0474 14815

STD

1100 0357 3490 2777 0004325 0517 14831

004

OBS

T1103 0357 34896 2777 14832

STD

1200 0356 3491 2778 0004321 0560 14848

STD

1300 0354 3492 2779 0004305 0603 14864

004

OBS

T1303

0354

34915

2779

14864

REFERENCE

SHIP CODE

LATITU

DE

L0^

GITUDE

T/10

ii.

MAR$DEN

SIATIQN TIME

ORIGINATOR'S

DEPTH

MAX.

DEPTH Of

S'MPL'S

WAVE

WEA- THER CODE

CLOUD CODES

MODC

CIBY CODE

ID. NO.

YEAR

CRUISE STATION NO. NUMBER

TO BOTTOM

STATION NUMBER

1/10

10'

r MO

DAY H

R.I/IO

DHL

HGT PER SEA

ITPf AM

31

540

FV

4531

N 04f

JOl w

149

58 0^

05 n

?5

1965

001 9270

189

1 1

21

k 2

xo

0

nn3A

WATER

WIND

BARO- METER

Imbsl

AIR TEMP. *C

VIS. COD

NO.

OBS.

DEPTHS

SPECIAL OBSERVATIONS

COLOR CODJ

TftANS.

OIR.

5 PEED

FORCt

DRY BULB

WET BULB

20

S20

047

044

039

8

10

"'""•;=> 1 CAST TIME 0. fjQ

HR 1/10

CARD TYPE

DEPTH Iml

T -C

s v..

SIGMA-T

SPECIFIC VOLUME ANOMAi'-lt'O'

SAD

DYN. M.

« 10'

SOUND VELOCITY

02 ml/I

PO4-P

TOTAL-P

wg • oi/l

NOj-N US - ol/l

NO3-N vi - al/l

SIO*-Si

PB-ol/l

pH

S

C

c

STD

0000

0057

3361 I2697 0010930 1 0000

14500

025

DBS

0000 0057 33505 2697 14500

STD

0010 0062 3364 2700 0010688 0011 14504

STD

0020 0066 3368 2702 0010446 0021 14508

STD

0030 0071 3371 2705 0010205 0032 14512

025

OBS

0037 0074 33734 2707 14515

STD

0050 0136 3400 2724 0008405 0050 14549

STD

0075 0215 3433 2745 0006483 0069 14592

025

OBS

0078 0221 34348 2745 14596

025

OBS

0097 0242 34407 2748 14609

STD

0100 0244 3441 2749 0006093 0085 14610

STD

0125 0264 3447 2752 0005852 0100 14624

STD

0150 0282 3453 2755 0005594 0114 14637

025

OBS

0151 0283 34529 2755 14637

STD

0200 0322 3463 2759 0005219 0141 14663

STD

0250 0353 3471 2762 0004958 0166 14686

STD

0300 0376 3477 2765 0004785 0191 14705

025

OBS

T0333 0387 34807 2757 14715

STD

0400 0391 3484 2769 0004510 0237 14729

025

OBS

0482 0392 34874 2772 14743

STD

0500 0390 3487 2772 0004339 0281 14745

STD

0600 0381 3488 2773 0004310 0325 14758

025

OBS

T0551 0376 34878 2774 14764

ST3

0700 0371 3488 2774 0004255 0368 14770

STD

0800 0363 3488 2775 0004261 0410 14784

025

OBS

0872 0359 34883 2776 14794

STD

0900 0359 3488 2776 0004276 0453 14799

STD

1000 0358 3489 2776 0004335 0495 14815

STD

1100 0357 3489 2776 0004400 0540 14831

02

5

OB

3

T1114

0:

57

34

8

36

27

7^

148

34

98

REfEfiENCE

SHIP CODE

LATITUDE

l/IO

LONGITUDE * "1/10

li

MARSDEN

STATION TIME

ORIGINATOR'S

DEPTH

MAX.

WAVE

WEA- THER CODE

CLOUD CODES

NODC

CODE

.EI. NO.

(GMTI

CRUISE

NO.

STATION NUMBER

BOTTOM

OF S'MPL'S

NUMBER

10'

T

MO

DAY HR.l/10

DIB.

HGI PER iF*

ITPt »M

31

540

FV

4

532

N

04816 W

149

58 OA

05 343

1965

001

9271 3713

06

?l

5 &

xo

0

0037

WATER

WIND

BAHO- METEH

(mb»)

AIR TEMP. "C

VI5. COD

NO.

OBS.

DEPTHS

SPECIAL OBSERVATIONS

COLOR CODE

TRANS, im,

DIR.

set ID

OR FORCt

DRY BULB

WET BULB

20

S26

044

022 |oil

B

06

MESSfNGi [

TIME 0'

HR VIO'

CAST NO.

CARD TYPE

DEPTH [ml

T -C

s •/..

r.r.. . T 5'tCIFlC VOLUMt

SAD

DVN. M.

X 10'

SOUND VELOCITY

Oj mt/l

PO^-P

lOIAl-P

NOj-N

NO3-N PB - 01/1

SIO4-S.

pg - 01/1

pH

S

c c

STD

0000

0031

3356 12695 I0OIII6I 1 0000

14487

043

OBS STD STD

0000 0031 33557 2695 14487 0010 0031 3356 2695 0011169 0011 14489 0020 0032 3356 2695 0011177 0022 14491

043

OBS STD STD

0024 0032 33555 2695 14491 0030 0050 3364 2700 0010624 0033 14502 0050 0104 3388 2716 0009111 0053 14533

043

OBS STD STD STD STD

0058 0123 33962 2722 14544 0075 0138 3402 2725 0008272 0075 14554 0100 0160 3409 2730 0007900 0095 14569 0125 0180 3416 2734 0007523 0114 1*583 0150 0198 3423 2738 0007140 0133 14596

043

OBS STD STD STD

0174 0215 34283 2741 1460B 0200 0228 3433 2743 0006646 0167 14619 0250 0251 3441 2748 0006264 0199 14638 0300 0273 3448 2752 0005962 0230 14657

043

OBS STD STD

STD

T0388 0308 34594 2758 14688 0400 0312 3461 2758 0005421 0287 14692 0500 0346 3471 2763 0005093 0339 14724 0600 0374 3478 2766 0004954 0390 14754

043

OBS

T0606

0376

34781

2766

14756

REFERENCE	SHIP CODE	LATITUDE 1/10	LONGITUDE * 'l/lO	^	MARSDEN	STATION	TIME			ORIGINATOR'S	DEPTH	MAX.		WAVE		WEA- THER CODE	CLOUD CODES		NODC
CTRY CODE	ID. NO.				CRUISE NO.	STATION NUMBER	TO BOTTOM	OF			STATION NUMBER
10-	T	MO	DAY	HR.1/10	S'MPL'S	Dia,	HGT f(R iE*	jyn AM
31	540	EV '	.534	N	04830 W		149	58	D4	05	057	1965	001	9272 )210	02 1 21	5 5	XO	0	0038
			WATER	WIND	BARO- METER (mbil	AIR TEMP. -C	VIS. COD	NO. OBS. DEPTHS	SPECIAL OBSERVATIONS
	COLOR CODE	IRANS.	DIR.	SPEtO OR FORCE	DRY BULB	WET BULB
				20	S24	051	Oil	006	8	05
	MESSENCS TIME c HR 1/10	CAST NO.	CARD TYPE	DEPTH (ml	I 'c	s v..	SlGMA-T	SPECIFIC VOLUME ANOMAIY-IIO'	SAD DYN, M.	SOUND VELOCITY	Ol ml/l	POi-P	lOIAl-R »B - ot/l	N03-N ug . oi/l	NOj-N US - oi/l	SI04-Si ug - oi/l	pH	S c c
			STD	0000	-0041	3328	2676	0012953 0000	14450
057		OBS	0000 -0041 33280 2576	1*450
		STD	0010 -0041 3330 2677	0012834 0013 14452
		STD	0020 -0041 3331 2678	0012716 0025 14454
057		OBS	0023 -0041 33315 2679	14454
		STD	0030 -0027 3340 2685	0012083 0038 14463
057		OBS	0048 0008 33577 2598	14485
		STD	0050 0012 3359 2698	0010807 0061 14487
		STD	0075 0052 3371 2706	0010099 0087 14511
057		OBS	0097 0083 33810 2712	14530
		STD	0100 0087 3382 2713	0009466 0112 14533
		STD	0125 0114 3391 2718	0008956 0135 14550
		STD	0150 0136 3398 2722	0008578 0156 14565
		05	7		OB	B	T0196		0	57	3^.	0	58		27	2	7			145	83

REFERENCE

SHIP CODE

LATITUDE

1/10

li

MARSDEN

STATION

TIME

ORIGINATOR'S

DEPTH TO

BOTTOM

MAX

■i

WAVE

WEA- THER CODE

CLOUD CODES

NODC

CIRY

ID. NO.

LONGITUDE * '1/10

YEAR

CRUISE NO.

STATION NUMBER

OF S'MPL'S

NUMBER

10'

1"

MO

DAY

HR.1/10

OIR.

HGI PER SEA

ITPt AM

31

540

FV

4534

N

04842 W

149

58 (

34

05

D70

1965

001

9273

ni9

01

21

5 5

XO

0

0039

WATER

WIND

BARO- METER (mbtl

AIR TEMP. 'C

VIS.

NO.

OBS. DEPTHS

SPECIAL OBSERVATIONS

COLOR CODE

TRANS.

DIR-

SPEED

OR (ORCE

DRY BULB

WET BULB

20

S22

051

017

006

7

04

HR 1/10 T

CARD TYPE

DEPTH Iml

T -C

s •/..

SIGMA-I

SPECIFIC VOLUME *SOMALi-<10'

; ,/" VELOCITY

0; ml/l

P04-P

„B -01/1

TOTAL-P

vg - ol/l

NOj-N Ufl - ol/t

N03-N

va - oi/i

SIO^-SI

pH

S

c

STD

0000

-0027

3333

2679

0012643

0000 14457

070

OBS 0000 -0027 33328 2679 14457 STD 0010 -0028 3333 2680 0012603 0013 14458 STD 0020 -0030 3334 2680 0012571 0025 14459 STD 0030 -0031 3334 2580 0012531 0038 14460

070

OBS 0043 -0033 33344 2681 14462 STD 0050 -0027 3340 2685 0012075 0062 14467

070

OBS 0061 -0018 33472 2590 14474 STD 0075 -0008 3353 2695 0011163 0091 14481

07

0

OB

S

0095

OC

)05

33

5

41

26

9f

14^

91

99

KEfERENCe

SHIP CODE

LATITUDE

1/10

ii

MARSDEN

STATION

Tl

^E

ORIGINATOR'S

DEPTH

MAX.

WAVE

WEA- THER

CODE

CLOUD CODES

<ODC

CTRY COOl

ID. NO.

* '1/10

CRUISE NO,

STATION NUMBER

BOTTOM

OF S-MPL-S

STATION NUMBER

10-

r

MO

DAY

HH.1/10

DHL

MGT PER iE*

lYPl *M

31

•yi^O

FV

4533

N

04855 W

149

58 04

05

DfllS

1965

001

9274 _ )073

01

?l

t* 2

XI

3 2

0040

WATER

WIND

BARO- METER

Imbi)

AIS TEMP. T

,„c NO. CODE 06S. ^°°' DEPTHS

SPECIAL

OBSERVATIONS

COLOR CODE

IRANS.

DIR.

SPIED

OR FORCf

DRY BULB

WET BULB

20 S22

051

017

006

7

l03

TIMf Of fjo

HR 1/10

CARD TYPE

DEPTH (ml

I 'c

s ■''..

SPfClfIC VOLUME ANOMAL»-X10'

SAD

OYN. M.

SOUND VELOCITY

O; ml/I

PO4-P PS - am

rOTAL-P vg - ol/l

NO3-N

ug • al/l

NO3-N KB - ol/l

SIO4-S1 ug-ol/l

pM

s c c

STD

0000

-0033

3317

2666

0013857

0000

14452

086

OBS 0000 -0033 33166 2666 l^ASZ

STD 0010 -0033 3317 2666 0013853 0014 1'.45'.

STD 0020 -0033 3317 2666 0013849 0028 14456

STD 0030 -0034 3317 2666 0013842 0042 14457

0 86

OBS 0030 -0034 33166 2666 14457

STD 0050 -0037 3318 2568 0013715 0069 14459

086

OBS

0050

-0039

33187

2666

14460

REFERENCE

SHIP CODE

LATITUDE

1/10

°z

MARSDEN

STATION

Tt

ViE

ORIGINATOR'S

DEPTH

MAX.

WAVE

WEA- THER CODE

CLOUD

CODES

NODC

CIRT CODE

ID. NO.

LONGITUDE

"1/10

YEAR

cruise! STATION

10

BOTTOM

OF S'MPL-S

STATION NUMBER

10*

r

MO

DAY

HR.l/10

NUMBER

0(B..

HGI PER SEA

ITPl AM

31

540

EV

4621

N

04800 W

149

68

)4

05

145

1965

001

9275 ni9

01

71

B 3

XI

6 5

0041

WATER

WIND

BARO- METER Imbil

AIR TEMP, r

VIS- COD

NO.

OBS.

DEPTHS

SPECIAL OBSERVATIONS

COLOR CODE

ia*Ni.

DIR.

SPEED

OR FORCE

DRY BULB

WEI

BULB

24

S24

075

033

022

7

04

MESSING* CAST TIME 0 "-NO. HR 1/lQ

CARD TYPE

DEPTH (ml

T TC

s v..

SIGMA-T

SPECIFIC VOIUME *NOMAt'-X10'

SAO

DYN. M. X 10^

SOUND VELOCITY

Ol ml/I

PO4-P

t>B - a>/l

lOTAl-p

ug - ai/l

NOi-N

ug - ai/l

NO2-N ug - ol/l

SIO4-SI wfl - ol/l

pH

S

c c

STD

0000

-0046

3317

2667

0013790

0000

14446

145

OBS 0000 -0046 33168 2667 14446

STD 0010 -0047 3317 2667 0013751 0014 14447

STD 0020 -0048 3318 2668 0013704 0027 14449

STD 0030 -0049 3318 2668 0013665 0041 14450

145

OBS 0035 -0050 33183 2668 14450

STD 0050 0007 3342 2685 0012079 0067 14482

STD 0075 0078 3371 2704 0010248 0095 14523

1*»5

OBS 0085 0099 33795 2710 14535

14

?

OB

3

0099

0]

20

33

8

82

27

It

>

14548

SHIP CODE

LATITUDE

1/lC

n

MARSDEN

STATION

OBiriNATOB*";

MAX

WEA- THER CODE

CLOUD CODES

LONGITUDE * 'I/IO

SQUARE

(GMT)

YEAR

TO

BOTTOM

DEPTH

OF S'MPL-S

OBSERVATIONS

STATION NUMBER

CTRY CODE

ID. NO.

CRUISE NO.

STATION NUMBER

10"

r

MO

DAT

HR.l/10

OIR.

HGT PER SEA

lYPI AM

31

540

EV

4619

N

04744 W

149

67

34

05

158

1965

001

9276

3157

01

73

0 4

XI

2 6

0042

WATER

WIND

BARO- METER

(mbil

AIR TEMP. X.

VIS. COD

NO.

OBS.

DEPTHS

SPECIAL OBSERVATIONS

COLOR CODE

IRANi,

OIR.

SPEED

OH FORCE

DRY BULB

WEt

BULB

23

S28

088

028

017

8

04

MESSENCH CAST ""= « NO. HR 1/10

CARD TYPE

DEPTH (ml

T -C

s */„

SIGMA-T

SPECIFIC VOLUME ANOMALY-XIO'

SAD

OYN. M.

X 10^

SOUND

VELOCITY

03 ml/I

PO.-P

lOTAl-P

NOj-N

ug - ol/l

NO]-N ug - ol/l

SI04-Si

UB - Ol/l

pH

S

c

C

STD

0000

-0020

3334

2679

0012619

0000

14461

158

OBS 0000 -0020 33335 2679 14461

STD 0010 -0022 3335 2680 0012530 0013 14461

STD 0020 -0024 3336 2681 0012442 0025 14462

STD 0030 -0026 3337 2682 0012353 0037 14463

158

OBS 0034 -0027 33369 2682 14463

STD 0050 -0011 3345 2688 0011766 0062 14475

STD 0075 0019 3358 2697 0010914 0090 14494

158

OBS 0087 0036 33641 2701 14505

STD 0100 0056 3371 2706 0010120 0116 14517

STD 0125 0100 3385 2714 0009321 0141 14543

15

3

OB

3

0145

0]

40

33

9

72

27

2

145

66

100

REFERENCE

SHIP CODE

LATITUDE

1/10

LONGITUDE

■i/io

MARSDEN

STATION

ri

WE

ORIGINATOR'S

DEPTH

MA

■

WAVi

WEA- THER

CODE

CLOUD CODES

CODE

ID.

NO.

CRUISE NO.

STATION

NUMBER

TO

BOTTOM

OF S'MPL-S

STATION

NUMBER

10*

1"

MO

DAY

HR.l/lO

D\>.

HGI ^E» StA

UH *w

31

540

EV

4

615

N

04723 W

149

67 04

05

177

1965

001

9277 D366

02

69

9 7

XI

3 4

0043

WATER

WIND

BARO- METER

[mbil

AIR TEMP. "C

SPECIAL

OBSfRVATIONS

COLOR CODE

TIANS.

D1R.

SPEED

lORCE

DRY BULB

BULB

22

525

095

033

022

8

08

MESSENGR

TIME 0 HR I/IO

CAST NO.

CARD TYPE

DEPTH Iml

T X

s •/..

SIGMA-T

SPECIfIC VOLUME ANOMALT-llO'

5 A D OVN. M.

SOUND

VELOCITY

0] ml/1

PO4-P

roiAL-r

NOi-N wg - or/I

NOi-N »a - al/l

SIO*-Si VB-at/1

pH

C

c

STD

0000 1-0046

3330

2678

0012788

0000

i^^^e

177

OBS STD STD

0000 -0046 33299 2678 14448 0010 -0046 3330 2678 0012761 0013 14450 0020 -0046 3331 2678 0012734 0026 14451

177

OBS

STD

0023 -0046 33306 2678 14452 0030 -0002 3348 2690 0011583 0038 14476

177

OBS

0032 0012 33526 2593 14483

177

OBS STD

0045 0114 33880 2716 14537 0050 0134 3397 2722 0008619 0058 14548

177

OBS STD STD STO STD

0059 0157 34128 2732 14566 0075 0189 3420 2736 0007259 0078 14579 0100 0220 3431 2743 0006685 0095 14598 0125 0248 3440 2747 0006245 0111 14616 0150 0274 3448 2752 0005878 0127 14632

177

OBS

0154 0278 34497 2753 14635

177

OBS STD

T0175 0297 34557 2756 14648 0200 0318 3462 2759 0005255 0154 14652

177

OBS

T0221

0334

34674

2761

^►673

REFERENCE	1/10	LONGITUDE ' "1/10	n	MARSDEN	STATION	Tl	we			ORIGINATOR'S ]	DEPTH	MAI	.		WAVE		WEA- THER CODE	CLOUD coots
CI«T CODE	ID. NO.				CRUISE NO.	STATION	TO BOTTOM	OF S-MPL'S			STATION
10-	r	MO	DAY	HR.l/JO	NUMBER	DID.	HOT nt SEA	I»»l »w
31	540	EV 4614	N	04707 W		149	67	Di*	05	196	1965	001	9278	042	10	24	5 2	XI	3 1	0044
			WATER	WIND	BARO- METER Imbil	AIR TEMP. -C	COD	NO. OBS. DEPTHS	SPECIAL OBSERVATIONS
	COLOR CODE	IBANS,	DIR.	SPIED 0» fO»CE	DRY BUIB	WET BULB
			24	S30	098	033	022	7	09
	MISilNG.lcAST TIME 0, NO. HR VIO	CARD TYPE	DEPTH (ml	I t	s */..	SIGMA-T	SPECIFIC VOLUME ANOMALf-XlO'	S AO DYN. M. K 10^	SOUND VELOCtTT	Ol ml/l	PO^-P ve.»./i	rOTAL-P va ■ Di/i	NO3-N ug - Qt/I	NOj-N MB ■ al/l	SIO4-S. wg - Ol/I	PH	c c
		STD	0000	0139	3393	2718	0008953	0000	14541
	196	OBS	0000 0139 33929 2718 145*1
		STD	0010 0141 3393 2718 0008959 0009 14543
		STD	0020 0142 3394 2719 0008896 0018 14546
		STD	0030 0144 3395 2720 0008758 0027 14549
	196	OBS	0035 0145 33967 2721 14550
		STD	0050 0174 3407 2727 0008136 0044 14567
		STD	0075 0217 3422 2735 0007330 0063 14592
		STD	0100 0254 3436 2744 0006583 0080 14614
		STD	0125 0285 3447 2750 0005042 0096 14633
		STD	0150 0312 3457 2755 0005540 0111 14550
	195	OBS	0181 0335 34653 2760 14667
		STD	0200 0342 3466 2750 0005186 0137 14672
		STD	0250 0359 3473 2764 0004865 0153 14689
	196	OBS	0251 0359 34735 2754 14589
	196	OBS	0291 0418 34865 2768 14722
		STO	0300 0415 3487 2769 0004448 0186 14723
		STD	0400 0388 3487 2772 0004254 0229 14728
	196	OBS	T0407 0387 34874 2772 14729
		STD	0500 0375 3488 2773 0004155 0271 14739
		STO	0600 0357 3488 2775 0004141 0313 14752
	196	OBS	0620 0356 34880 2775 14755
		STD	0700 0352 3488 2775 0004143 0354 14767
		STD	0800 0359 3489 2776 0004172 0396 1*782
	196	OBS	T0835 0358 34887 2776 14787
		STD	0900 0356 3489 2776 0004214 0438 14797
		STD	1000 0355 3489 2776 0004293 0480 14814
		196	OB,	>	TIOOO		03	55	3**	8	86		27	7t							148	14

101

REFERENCE		LATITUDJ I/IO	LONGITUDE ■ '1/10	n	MARSDEN		STATION T	ME	YEAR	ORIGINATOR'S	DEPTH	MAX. DEPTH OF S-MPL-		WAVE		WEA- THER CODE	CLOUD CODES			NODC
ClaT CODE	ID. NO.	CODE			CRUISE NO.	STATION NUMBER	TO BOTTOM			STATION NUMBER
10*	T	MO	DAY H	H.1/10	DHL	HGI PER SEA	UPt AM
31	•^AO	EV	4	613	N	04650 W		149	66	04	05 215	1965	001	9279	Il218	12	24	5 2	xo	X 0	0045
				WATER	~^'^0 1 ..or	R	AIR TEMP.	c	VIS. COD	NO. OBS. DEPTHS	SPECIAL OBSERVATIONS
	COLOR TRANS, CODE 1-"!	OIR.		DRY BULB	WET BULB
		24	S29 102	039 \|028	8	09
	HR 1/10	C*SI NO.	CARD TYPE	DEPTH (ml	T -C	s */..	SIGMA-T	SPECIFIC VOLUME ANOM*LT-<10'	SAD DVN. M. X 10^	SOUND VELOCITY	Ol ml/l	PO*-P	lOTAL-P vg - o'/l	N03-N ue - al/l	N03-N t.g - oi/l	sio*-s. pg-oi/l	PH	5 C C
			STD	0000	0207	3415	2731	0007721	0000	14574
	215		DBS	0000 0207 34154 2731		14574
			STD	0010 0209 3416 2731	0007716	0008 14577
			STD	0020 0211 3416 2731	0007719	0015 14579
	215		OSS	0022 0211 34160 2731		14580
			STD	0030 0218 3419 2733	0007545	0023 14584
	215		OBS	0035 0223 34214 2735		14588
			STD	0050 0245 3429 2739	0007010	0038 14601
			STD	0075 0278 3440 2745	0006468	0054 14621
			STD	0100 0307 3450 2750	0005985	0070 14639
			STD	0125 0333 3459 2755	0005565	0084 14655
	215		OBS	0145 0350 34649 2758		14667
	-		STD	0150 0353 3466 2759	0005250	0098 14669
			STD	0200 0380 3475 2763	0004885	0123 14690
			STD	0250 0398 3481 2766	0004657	0147 14706
	215		OBS	0271 0403 34837 2768		14712
			STD	0300 0398 3485 2769	0004416	0170 14715
			STD	0400 0384 3487 2772	0004212	0213 14726
	215		OBS	T0459 0377 34878 2773		14733
			STD	0500 0374 3488 2774	0004121	0255 14738
			STD	0600 0367 3488 2775	0004133	0296 14752
	215		OBS	0691 0362 34888 2776		14765
			STD	0700 0362 3489 2776	0004105	0337 14767
			STD	0800 0361 3489 2776	0004150	0378 14783
			STD	0900 0359 3490 2777	0004189	0420 14799
	215		OBS	T0977 0356 34898 2777		14810
			STD	1000 0355 3490 2777	0004189	0462 14814
			STD	1100 0350 3490 2778	0004212	0504 14828
		215		OBS	T118<;		03^5		34905	2779								14841

REFERENCE

SHIP CODE

LATITUDE

I/IO

LOh

GITUDE * -1/10

°i

MARSDEN

STATION

TIME

ORIGINATOR'S

DEPTH

MAX.

WAVE

WEA- THER CODE

CLOUD COOES

^ODC

CT«T CODE

ID.

YEAR

CRUISE NO.

STATION NUMBER

TO

BOTTOM

OF S'MPL'S

STATION NUMBER

10*

T

MO

DAY

HR.1/10

DIR.

HCJ-E. Si.

irp( AM

31

540 EV

4

518

N

04631 W

149

66

34

06

013

1965

001

928D_.

060

11

23

51

XO

0

0046

WATER

WIfiO

BARO- METER (mbO

Alft TEMP. -C

VIS.

coo

NO.

OBS.

DEPTHS

SPECIAL OBSERVATIONS

COLOR CODE

TRANS.

DIR.

SPEED

OR FORCE

DRV BULB

WET BULB

22

S23

129

039

028

6

08

MESSENGR

TIME c

HR 1/10

CAST NO.

CARD

TYPE

DEPTH (m)

I -c

s •/..

StGMA-T

5»ECIFIC VOLUME AMOMALf-IlO'

SAD DYN. M.

SOUND VELOCITY

Ol ml/l

PO*-P

lOTAL-P

N03-N

ug-ol/l

NO3-N ug - ol/l

SI 04-Si

pH

! C

c

STD

0000

0326

3446

2745

0006414

0000

14630

013

OBS STD STD STD STD

0000 0326 34456 2745 14630 0010 0324 3448 2747 0006227 0006 14631 0020 0323 3450 2749 0005069 0012 14632 0030 0321 3452 2750 0005911 0018 14634 0050 0318 3456 2754 0005596 0030 14635

013

OBS STD STD STD STD STD

0069 0315 34594 2757 14638 0075 0320 3451 2758 0005256 0044 14542 0100 0337 3465 2759 0005131 0057 14654 0125 0353 3470 2762 0004928 0069 14665 0150 0366 3474 2764 0004776 0081 14675 0200 0386 3480 2766 0004571 0105 14693

013

OBS STD

0205 0387 34808 2767 14694 0250 0396 3485 2769 0004347 0127 14705

013

OBS STD STD

T0285 0399 34875 2771 14713 0300 0395 3488 2771 0004197 0148 14714 0400 0375 3488 2774 0004064 0190 14722

013

OBS STD STD

0461 0366 34878 2775 14729 0500 0362 3488 2775 0003992 0230 14733 0600 0355 3489 2777 0003929 0269 14747

013

OBS STD STD STD

T0699 0351 34896 2777 14762 0700 0351 3490 2778 0003895 0309 14762 0800 0352 3491 2779 0003913 0348 14779 0900 0353 3491 2778 OOO4OO6 0387 14796

013

OBS STD

T0939 0353 34913 2779 14803 1000 0354 3491 2779 0004074 0428 14814

01

3

OB

5

105c

0

)55

3;.

9

14

27

7^

)

148

24

102

REFERENCE

SHIP

CODE

LATITUDE

VTO

LONGITUDE

•1/10

s?

MARSDEN

STATION T

ME

ORIGINATOR'S 1

DEPTH

1 MAX

WAVE

WEA

THES CODE

CLOUD

CODES

CT»r

COD(

ID.

NO.

CRUISE NO.

STATION NUMBER

BOTTOM j.^O;

STATION NUMBER

10*

r

MO

DAY H

R.1/10

S DIR.

HGI PER SEA

11 P( AM

31

540

EV

4519

N

04548 W

149

65

04

D6 b48

1965

001

9281 )421 1 04

21

B 3

xo

0

0047

WATER

WIND

BARO- METER

AIR TEMP. 'C

VIS. CODE

NO.

OBS.

DEPTHS

SPECIAL OBSERVATIONS

COLOR CODE

(ml

D1R.

SPEED

0(1 (ORCE

DRY BULB

WET BULB

26

S28

135

039

028

6

05

MESSENCR CAST TIME <.\l HR 1/10

CARD TYPt

DEPTH (ml

T 'C

s */..

SIGMA-T

SfEClFlC VOLUME ANOMAL'-XIO'

SAD

DYN. M X 10^

SOUND VELOCITY

02 ml/l

PO*-P

TOTAL-P ug - ol/l

NOj-N vg - ol/l

NO3-N wg - ol/l

SIO«-Si

ua-oi/i

pH

S

c c

STD

0000

0374

3440

2736

0007279

0000

14650

048

OBS STD STD STD STD STD STD

0000 0374 34400 2736 14650 0010 0374 3440 2736 0007263 0007 14651 0020 0374 3441 2736 0007254 0015 14553 0030 0373 3441 2736 0007237 0022 14654 0050 0373 3441 2737 0007212 0036 14657 0075 0372 3442 2738 0007174 0054 14661 0100 0371 3443 2738 0007143 0072 14665

048

OBS

STD

0111 0371 34429 2738 14667 0125 0391 3455 2747 0006353 0089 14679

048

OBS STD STD

STD

0142 0410 34688 2755 14592 0150 0410 3471 2757 0005446 0104 14694 0200 0408 3481 2765 0004723 0129 14702 0250 0400 3488 2771 0004164 0151 14708

048

OBS STO

0255 0399 34881 2771 14709 0300 0387 3488 2773 0004046 0172 14711

048

OBS

T0357 0362 34889 2776 14712

REFERENCE

SHIP CODE

LATITU

DE

1/10

LONGITUDE * '1/10

So

MARSOEN SQUARE

STATION TIME (GMTl

YEAR

ORIGINATOR'S I

DEPTH

TO

MAX

DEPTH

OF

S'MPL-

WAVE OBSERVATIONS

WEA- THER CODE

CLOUD CODES

NOOC STATION

NUMBER

CTRV CODE

ID.

NO.

CRUISE NO.

STATION

10*

r

MO

DAY H

R.l/lO

NUMBER -vyi.v./™

S OIB,

MGI PER SEA

IIPI AM

31

S40

EV

4622

N

04504 W

149

65 (

)4 r

>6 D

8?

1965

001

9282 )869

09

23

tf 2

XO

0

0048

WATER

WIND

BARO- METER (mbt)

AIR TEMP. "C

VIS CODE

NO.

OBS. DEPTHS

SPECIAL OBSERVATIONS

COLOR CODE

"tV

DIR.

SPEED FORCE

DRY BULB

WET BULB

23

S18

149

039

022

8

07

MESSENGR (-AST TIME 0 NO. HR 1/10

CARD TYPE

DEPTH (ml

T "C

S '/..

SIGMA-T

SPECIFIC VOLUME ANOM*l»-»10'

SAD

DYN. M X 10'

SOUND VELOCITY

0,^1/1 ^'O'-;^

TOTAl-P

NOj-N

Kg - Qt/I

NO3-N vg - ol/l

SIO«-S.| i>g - ol/l

s c c

STD

0000

0404

3444

2736

0007246

0000

14663

082

OBS STD STD STD STD STD STD

0000 0404 34443 2736 14663 0010 0403 3444 2735 0007244 0007 14664 0020 0402 3444 2735 0007241 0014 14665 0030 0400 3444 2735 0007239 0022 14666 0050 0398 3444 2737 0007232 0036 14658 0075 0395 3444 2737 0007233 0054 14671 0100 0392 3444 2737 0007225 0072 14674

082

OBS STD STD

0123 0389 34442 2738 14677 0125 0391 3445 2739 0007104 0090 14578 0150 0416 3455 2751 0005957 0107 14595

082

OBS STD STD STD STD

T0178 0438 34825 2753 14711 0200 0433 3484 2755 0004764 0133 14713 0250 0423 3487 2758 0004483 0157 14718 0300 0413 3489 2771 0004276 0178 14722 0400 0395 3491 2774 0004031 0220 14731

082

OBS STD

STD

0404 0394 34911 2774 14731 0500 0379 3490 2775 0004003 0260 14741 0600 0363 3489 2776 0003989 0300 14751

082

OBS STD STD

T0502 0363 34894 2776 14751 0700 0350 3490 2777 0004029 0340 14766 0800 0357 3490 2777 0004062 0381 14781

082

OBS

T0815 0356 34897 2777 14783

082

OBS

0862 0355 34897 2777 14791

REFERENCE

SHtP CODE

LATITU

DE

i/lo

LONGITUDE

"1/10

n

MARSDEN SQUARE

STATION TIME (GMTl

YEAH

ORIGINATOR'S 1

DEPTH

TO OTTOM

MAX. DEPTH

OF S'MPL'

WAVE OBSERVATIONS

WEA- THER CODE

CLOUD CODES

NODC STATION NUMBER

cur

CODE

ID. NO.

CRUISE

NO.

STATION NUMBER

10- 1 1-

MO

3AY H

.1/10

DIR. HGTJPEd] SEA

typ! AMI

31

540

EV

4700

N

044

52 W

149

74 |c

4 C

T^^

33

1965

001

9283 D

147

01

23

7kl

XI

8 6

0049

WAIfR

WIND

BARO- METER Imbl)

AIR TEMP. "C

VIS COD!

NO.

OBS. DEPTHS

SPECIAL OBSERVATIONS

COLOR CODE

TRANS

DIR.

5P(£D

OR FORCE

DRY BULB

WET BULB

29

S19

166

039

028

7

04

HR 1/10

CARD TYPE

DEPTH Iml

T 'C

s ■/.,

SIGMA-T

SPtCltIC VOLUME ANOMAL»-«10'

SAO DYN. M.

X 10'

SOUND VELOCITY

0: m!/l

?0i~?

lOTAL-P

NOj-N vg - Ol/l

NOi-N tig - Ol/l

SlO^-Si

ng - o./l

pH

s c

c

STD

0000

0379

3443

2738

0007079

0000 14652 1

133

OBS

STD STD STD STD

0000 0379 34433 2738 14652 0010 0378 3443 2738 0007078 0007 14653 0020 0378 3443 2738 0007086 0014 14555 0030 0377 3443 2738 0007086 0021 14656 0050 0375 3443 2738 0007091 0035 14559

133

OBS STD STD

0059 0374 34432 2738 14660 0075 0372 3444 2739 0007034 0053 14661 0100 0368 3445 2740 0005942 0071 14664

133

OBS STO

0123 0354 34457 2741 14666 0125 0365 3445 2741 0005848 0088 14667

13'

OB;

0138

03

74

34/(

89

27

43

146

73

103

REFERENCE

SHIP COOE

LATITUDE

1/10

n

MARSDEN

STATION

Tl

«£

OftlGINATOR'S

DEPTH

MAX. DEPTH

OF S'MPL'S

WAVE

WEA- THER CODE

CLOUD CODES

NODC

CT«Y CODE

10. NO.

LONGITUDE

'1/10

CRUISE NO.

STATION NUMBER

TO

BOTTOM

STATION

NUMBER

10-

1'

MO

DAY

HR.V10

DtH

HCT PER SEA

l>PE AM

31

5*0

EV

*655

N

0*513 W

149

65 OU

06

173

1965

001

9284 )186

02

26

W 2

XI

6 6

0050

WATER

WIND

BARO- METER

AIR TEMP. -Z

coo

NO. OBS. DEPTHS

SPECIAL OBSERVATIONS

COLOR CODE

TRANS.

DIR.

SPHO

OH FOUCE

DRt BULB

WEI BULB

21

SIO

166

039

028

7

04

"""•«:■ IcASl

tlMi ., „o

HR 1/10

CARD TYPE

DEPTH (ml

T t

S •''..

SIGMA-T

SPECIFIC VOLUME ANOMAlY-llo'

SAD

DVN. M.

X 10^

SOUND VELOCITY

Ol ml/l

PO*-P

vg - ai/t

rOTAL-f

NOi-N vg - ol/l

NO3-N Vt ■ ol/l

SIO^-S.

Vi - ol/l

PH

S C

c

STD

0000

038<» l3'»43

2737

0007142

0000

14654

173

OBS 0000 038* 3**31 2737 1*^65* STD 0010 038* 3**3 2737 00071*3 0007 1*656 STD 0020 0383 3**3 2737 00071*2 001* 1*657 STD 0030 0382 3**3 2738 000713* 0021 1*658 STD 0050 0381 3**3 2738 000713* 0036 1*661

173

OBS 0058 0380 3**3* 2738 1*662 STD 0075 0378 3*** 2738 0007111 0053 1*66* STD 0100 0375 3*** 2739 0007079 0071 1*667

173

OBS 0121 0372 3***1 2739 1*669 STD 0125 0373 3**5 27*0 0007001 0089 1*670 STD 0150 0382 3*52 27** 0006586 0106 1*679

173

OBS

0169

039A

34606

2750

14689

REFERENCE

SHIP CODE

LATITUDE

'A

MARSDEN

STATION

Tl

^i

ORIGINATOR'S

DEPTH

MAX

,

WAVE

WEA- THER CODE

CLOUD CODES

NODC

cmv

ID.

CRUISE

STATION

TO BOTTOM

OF

STATION

CODE

I/IO

"l/lO

10'

r

MO

DAY

HR.1/10

NUMBER

S'MPL'S

DIP.

HCI PEP SE*

I»P( AM

31

540

EV

*700

N

0*521 W

149

75

3*

06

184

1965

001

9285 3192

02

27

B k

XI

6 6

0051

WATER

WIND

AIR TEMP. -Z

NO.

COLOR

I>A»5.

SPEED

METER

DRT

WET

con

OBS.

CODE

""'

FOSCE

(mbil

BULB

27

SIO

169

028

017

7

04

TIM. 0)^*^^

HR I/IO 1

CARD TYPE

DEPTH (ml

T -C

s •'..

SIGMA-T

SPECIFIC VOLUME ANOMALr-«10'

SAD

DYN. M.

t 10'

SOUND VELOCITY

0; ml/1

PO4-P

lOTAl-P

NO3-N

i>g -ol/l

NOj-N

SIOi-S. VB - at/I

pH

c c

1

STD

0000

0358

3**2

2739

0006963

0000

14643

184

OBS 0000 0358 3**22 2739 1*6*3

STD 0010 0359 3**3 2739 0006938 0007 1*6*5

STD 0020 0361 3*** 27*0 0006907 001* 1*6*8

STD 0030 0362 3*** 27*0 0006882 0021 1*650

STD 0050 0365 3**5 27*1 0006827 003* 1*655

STD 0075 0368 3**7 27*2 0006759 0051 1*660

STD 0100 0371 3**9 27*3 0006686 0068 1*666

STD 0125 0375 3*50 27** 0006619 0085 1*672

184

OBS 0127 0375 3*50* 27** 1*672

184

OBS 0137 0395 3*605 2750 1*68*

STD 0150 0397 3*70 2757 0005389 0100 1*688

18

4

OB,

3

T0183

0^

03

3*

7

60

27

6]

14697

REFERENCE

SHIP CODE

LATITUDE

1/10

LONGITUDE

■1/10

ii

MARSDEN

STATION

Tl

ME

ORIGINATOR'S

DEPTH

MAX. DEPTH

OF S'MPL'S

WAVE

WEA- THER CODE

CLOUD CODES

■JODC

CTRY

ID. NO.

YEAR

CRUISE NO.

STATION NUMBER

TO BOTTOM

STATION NUMBER

CODE

10- 1 r 1

MO

DAY

MR.l/lO

DIR.

MGT fEK IE*

TIP! AM

31

5*ol EV

*700

N

0*536 W

149

(75 1

34

06

199

1965

001

9286

D252

03

24

7 5

XI

3 6

0052

WATER

WIND

BARO- METER (mbil

AIR TEMP. X.

VIS. COD

NO.

OBS. DEPTHS

SPECIAL OBSERVATIONS

COLOR

CODE

TRANS.

DIR.

SPEED

OB fOPCE

OUT BULB

WET BULB

24

S07

169

028

017

7

05

MESSING

TIME

HR l/l

"IcAST «T NO.

CARD TYPE

DEPTH Iml

T -C

s •/..

SIGMA-T

SPECIFIC VOLUME ANOMALT-dO'

SAD

DYN. M.

X 10'

SOUND VELOCITY

Ol ml/1

PO,-P vg - Ol/l

rOTAL-P

NO7-N

ug - ol/l

NOj-N vg- ol/l

SI04-Si

vg - ot/l

pM

S C

c

STD

0000

0364

3442

2736

0007072

0000

14646

19'

?

OBS

0000 036* 3**15 2738 1*646

STD

0010 0363 3**2 2738 0007073 0007 1*6*7

STO

0020 0362 3**2 2738 000707* 001* 1*6*8

STO

0030 0352 3**1 2738 0007082 0021 1*6*9

STD

0050 0360 3**1 2738 000708* 0035 1*652

STD

0075 0358 3**1 2738 0007003 0053 1*655

19

J

OBS

0076 0358 3**13 2738 1*655

STD

0100 0351 3**3 27*0 0006938 0071 1*656

STD

0125 03*3 3*** 27*2 0006780 0088 1*557

19

9

OBS

0125 0343 3***1 27*2 1*657

STD

0150 0389 3*65 275* 0005680 0103 1*68*

19

9

OBS

0176 0*18 3*802 2763 1*702

STD

0200 0411 3*81 2765 000*7*4 0129 1*70*

STD

0250 0398 3*83 2768 000*491 0153 1*707

19

9

OB

T0252

0

J97

34

6

34

27

6E

147

07

104

REfERENCE

SHIP CODE

LATITUDE

I/IO

LONGITUDE ' -1/10

n

MARSDEN

STATION

TIME

ORIGINATOR'S

DEPTH

MAX.

WAVE

WEA- THER

CODE

CLOUD COOES

NODC

CTRY CODE

ID. NO.

CRUISE NO.

STATION

NUMBER

TO BOTTOM

Of S'MPL'S

STATION NUMBER

10*

r

MO

DAY

HR.1/10

Dll

HGiPE. U*

UK AW

31

540

EV

i

E659

N

04549 W

149

65 04

06

M7

1965

001

9287 )280

03

24 E> k 1

XI

3 6

0053

WATtR

WIND

BARO- METER

AIR TEMP. *C

v,,^ NO.

-■o^'.^s

SPECIAL OBSERVATIONS

COLOR CODE

TIANS.

OIR.

Sf£(D

Ol fOUCt

DRY

BULB

WET BUL8

27 S02

166

028

Oil

7

l06

MiSiENCR

TIME c

HR 1/10

CAST NO.

CARD

TYPE

DEPTH Iml

T -C

s •/..

SIGMA-T

srjcidC voiUMt

ANOMAU-XIO'

SAD DVN. M.

X 10^

SOUND

VELOCITY

Oj mi/I

PO4-P

V8 - -t/l

lOTAl-P

NO3-N ua • oi/i

NOi-N us - Ol/I

SI04-S>

Itg - ol/l

PH

S

c c

STD

0000

0358

3442

2739

0006978

0000

14643

217

DBS STD STO STD STD STD STD

0000 0358 34420 2739 14643 0010 0356 3443 2740 0006892 0007 14644 0020 0354 3444 2741 0005799 0014 14645 0030 0352 3445 2742 0005713 0021 14646 0050 0348 3447 2744 0005534 0034 14548 0075 0343 3450 2747 0005319 0050 14650 0100 0338 3452 2749 0005096 0065 14652

217

CBS

0100 0338 34523 2749 14652

217

DBS STD STD

0120 0391 34650 2754 14580 0125 0389 3455 2754 0005542 0080 14580 0150 0382 3466 2755 0005512 0094 14581

217

DBS STO

0150 0382 34663 2756 14681 0200 0409 3479 2753 0004884 0120 14702

217

CBS STD

0215 0411 34818 2755 14705 0250 0405 3485 2758 0004441 0143 14710

217

OBS

T0280

0389

34856

2770

14708

REEERENCE

SHIP CODE

LATITUDE

I/IO

LONGITUDE

•1/10

°?

MARSOEN

STATION T

ME

ORIGINATOR'S

DEPTH

MAX.

DEPTH

OF

S'MPL'S

WAVE

WEA- THER CODE

CLOUD COOES

40DC

crpT

10,

NO.

YEAR

CRUISE NO.

STATION NUMBER

TO

BOTTOM

STATION NUMBER

10-

1*

MO

DAY H

R.l/lO

DIR.

HCI Ht SEA

TfPE AM

31

540

EV

«

701

N

04605 W

149

76

54

06 2

33

1965

001

9288 3334

03

24

1 4

XI

3 5

0054

WATER

WIND

BARO- METER Imbil

AIR TEMP. T

VIS,

coo

NO.

OBS.

DEPTHS

SPECIAL OBSERVATIONS

COLOR CODE

TRANS.

DIR.

SPEED

OR EOfCf

DRY BULB

WET BULB

27

S02 |l63

039

022

8

05

MESSENGI

TIME 0 HR 1/10

CAST NO.

CARD TYPE

DEPTH (m)

I ic

s •/..

SIGMA-T

SPECIFIC VOLUME

*NOM*11-I10'

SAO

DYN. M. I 10>

^°'"'° Oj ml/l VELOCITY "' "

PO4-P v9 -o.yi

?OTAl-P

vg - o./l

N03-N

UB • Ql/I

NO3-N «S - ol/l

SIO*-SI lig - ol/l

pH

S

c c

STD

0000

0363

3443

2739

0005980

0000

14645

233

OBS STD STD STD STD

0000 0363 34425 2739 14645 0010 0355 3444 2741 0006808 0007 14644 0020 0349 3444 2741 0006760 0014 14643 0030 0343 3445 2743 0005537 0020 14642 0050 0334 3447 2745 0006419 0033 14642

233

OBS STD STO

0052 0330 34481 2747 14642 0075 0330 3449 2747 0006242 0049 14644 0100 0329 3451 2749 0005113 0065 14648

233

OBS STD STD

0118 0329 34524 2750 14651 0125 0341 3456 2752 0005866 0080 14658 0150 0376 3456 2755 0005475 0094 14579

233

OBS STD STD STD

T0178 0406 34758 2751 14697 0200 0401 3478 2753 0004897 0120 14599 0250 0389 3482 2768 0004503 0143 14703 0300 0378 3485 2772 0004108 0165 14707

23

3

OB

5

0334

0:

70

34

8

92

27

7!

14710

REFERENCE

SHIP CODE

LATITUDE

I/IO

LONGITUDE ■ "I/IO

ii

MARSDEN

STATION TIME

YEAR

ORIGINATOR'S

DEPTH

MA

.

WAVE

'

WEA- THER

CODE

CLOUD CODES

CTRT CODE

10. NO.

CRUISE NO.

STATION NUMBER

TO BOTTOM

OF S'MPL-S

OBSERVATIONS

STATION NUMBER

MO

DAY H

R.1/10

OiR-

MGll ^ER SEA

IVPt AM

31

540

EV

4700

N

04619 W

149 76

34

07 3

08

1965

001

9289

3328

03

?4

iL

XI

4 3

0055

WA

EH

WIND

BARO- METER Imbil

AIR TEMP. "C

VIS.

COD

NO.

OBS.

DEPTHS

COLOR CODE

'tV'

OIR.

SfEfO

OR FORCE

DRY BULB

WET BULB

OBSERVATIONS

00

soo

166

022

Oil

8

04

MESSENC

TIME HR 1/1

*icAST °T NO.

CARD TYPE

DEPTH Iml

T -C

s •/„

SlGMA-T

SPECIFIC VOLUME

ANOMAU-HO'

SAD

DYN. M. X 10^

SOUND VELOCITY

Ol ml/I

PO4-P

rOTAL-P vg - Ol/l

NOi-N US - a'/l

NO3-N vg - ol/l

SI 04-Si VS - al/l

rH

s c

c

STD

0000

0351

3463

2756

0005316

0000

14643

00

J

OBS STD STD STD STD STO STD STD

0000 0351 34632 2755 0010 0353 3464 2757 0020 0356 3465 2757 0030 0358 3466 2758 0050 0363 3467 2758 0075 0369 3469 2759 0100 0374 3471 2760 0125 0380 3473 2751

14643

0005285 0005 14646 0005263 0011 14646 0005233 0016 14651 0005175 0026 14657 0005110 0039 14664 0005047 0052 14670 0004977 0064 14677

00

i

OBS

0128 0381 34731 2751

14678

00

i

OBS STD STD STD STO

0143 0402 34796 2754 0150 0401 3480 2755 0200 0393 3482 2758 0250 0384 3485 2770 0300 0375 3487 2773

14690 0004682 0076 14691 0004458 0099 14696 0004238 0121 14701 0004018 0142 14706

00

i

OB.

3

T0328

0:

71

34

8

86

27

75

147

09

105

REFERENCE

SHIP CODE

LATITUDE

l/IO

L0^

GITUDE '1/10

'^z

MARSDEN

STATION

TIME

ORIGINATOR'S

DEPTH

TO

BOTTOM

MAX.

WAVE

WEA- THER CODE

ClOUD CODES

NODC

cut

CODE

ID.

NO.

YEAR

CRUISE

STATION NUMBER

OF S'MPL'S

STATION NUMBER

10*

r

MO

DAY

HR.1/10

DIR.

HGi nn s

A

IlPf AW

31

540

EV

i

700

N

04533 W

149

75

34

07

022

1965 001

9290

0732

07

24

2 k

XI

4 4

0056

WATER

WIND

BARO- METER

Imbsl

AIR TEMP.

•c

VIS,

COD

NO.

OBS.

DEPTHS

SPECIAL OBSERVATIONS

COLOR TRANS, CODE 1"^'

OIR.

SPEED

oa FOBCi

DRY BULB

WET BULB

00

SOO

159

022

Oil

8

05

MESSINCR HR 1/10

CAST NO.

CAfiD TYPE

DEPTH (ml

T t

s •/..

SIGMA-T

SPECIFIC VOLUME ANOMALY-XIO'

SAO

DYN. M X 10^

SOUND VELOCITY

Qj ml/1

P04-P

wa - OP/I

rOTAL-P

vg ■ oi/i

NO,-N

ug - oi/l

NO3-N wg - ol/l

SI 04-S-

l>g - ol/l

PH

s c

C

STD

OOOO

0368

3465

2755 0005355

OOOO

14650

022

OBS

STD STD STD STD STD STD STD STD

OOOO 0368 34648 2756 0010 0358 3465 2757 0005321 0020 0367 3466 2757 0005288 0030 0367 3466 2757 0005254 0050 0355 3467 2758 0005187 0075 0364 3459 2759 0005099 0100 0363 3470 2751 0005018 0125 0362 3471 2752 0004930 0150 0361 3472 2753 0004849

0005 0011 0016 0026 0039 0052 0064 0077

14650 14652 14553 14655 14558 14562 14565 14669 14673

022

OBS

0160 0360 34728 2753

14574

022

OBS STD STD STD STD

0192 0402 34826 2757 0200 0401 3483 2757 0004500 0250 0393 3485 2770 0004315 0300 0386 3486 2771 0004215 0400 0374 3488 2774 0004031

0100 0122 0143 0184

14599

14700 14705 14710 14722

022

OBS STD

STD

T0426 0371 34886 2775 0500 0365 3489 2775 0003965 0600 0359 3489 2776 0003972

0224 0264

14725 14735 14749

022

OBS

T0675

0357

34892

2777

14760

SHIP CODE

LATITUDE

1/10

LONGITUDE \i '1/10

ORIGINATOR'S

WEA- THER CODE

540

04647 W I 1149 76 04 07 338 1965 QOl 9291

00

SCO

AIR TEMP. -C

017

Oil

1152 I 10 I 00 b

0057

DEPTH Im

lOTAL-

UB - 01/

038 038

038

STD

OBS STD STD STD STD

OBS STO

OBS STD STD STD

OBS

OBS STD STD STD

OBS STD STD

OBS STD STO STD

OBS

OOOO OOOO 0010 0020 0030 0050 0065 0075 0079 0100 0125 0150 0173 0197 0200 0250 0300

T0395 0400 0500

T0594 0500 0700 0793 0800 0900 1000

T1012

0349 0349 0350 0350 0350 0351 0352 0333 0326 0334 0344 0353 0362 0386 0386 0386 0385 0382 0382 0373 0357 0357 0351 0357 0357 0353 0350 0350

3459

34588

3459

3450

3460

3451

34517

3461

34613

3453

3465

3470

34743

34803

3481

3484

3485

34893

3489

34894

3489

3490

34901

3490

34898

2753

2753 2753 2754 2754 2755 2755 2757 2757 2758 2759 2762 2764 2767 2757 2770 2771 2774 2774 2775 2775 2775 2777 2777 2777 2778 2778 2778

0005629

0005611 0005586 0005569 0005526

0005254 0005139 0004951

0004496 0004318 0004204

0004019 0004005

0004029 0004020

0004045 0004084 0004131

OOOO

0006 0011 0017 0028

0005345 0041

0055 0058 0080

0104 0125 0147

0188 0229

0269 0309

0349 0390 0431

14641 14641 14543 14545 14547 14651 146 54 14547 14545 14652 14661 14569 14678 14692 14593 14702 14710 14725 14726 14738 14751 14752 14766 14780 14781 14796 14812 14814

106

REFERENCE

SHIP

LATITUDE

1/10

LONGITUDE

' ■i.'io

MARSDEN

STATION

Tl

ME

ORIGINATOR'S

DEPTH

MAX. DEPTH

OF S-MPL'S

WAVE

WEA- THtR CODE

ClOUD

CODES

CUT CODE

ID.

CRUISE NO.

STATION NUMBER

TO BOTTOM

STATION

10*

r

MO

DAt

HR.1/10

DIP,

MCI PES •.

A

tYP[ AM

«umot-(

31

540 EV

I

»700

N

04700 W

149

77

D4

07

064

1965

001

9292

1088

10

00

0 Ix

xo

0

0058

WATER

WIND

BARO- METER (mb»l

AIR TEMP,

■c

coo

NO.

OBS.

DEPTHS

SPECIAL OBSERVATIONS

COLOR CODE

'»''

DIH.

SPEED

OR FOPCE

DRY WET BULB BULB

00

SOO

152

017 Oil

7

07

MESSEMCR HR l/IO

CAST NO.

CARD TTPE

DEPTH (ml

T T:

S v..

SIGMA-T

SPECIFIC VOLUME ANOMALT-KIO'

SAD

OTN. M.

« 10'

SOUND VELOCITY

0? ml/I

vg - ol/l

TOTAl-P 1.9-ol/t

NOj-N

ug . ol/l

NO3-N

vg - ol/l

S10*-S' pg - ol/l

pH

C C

STD

0000 0083

3377

2709 0009795

0000

14514

064

DBS STD STD STD STD STD STD

0000 0083 33773 2709 0010 0107 3387 2715 0009201 0020 0131 3396 2721 0008670 0030 0153 3404 2726 0008211 0050 0195 3420 2736 0007304 0075 0241 3437 2746 0006387 0100 0281 3452 2754 QOO5605

14514 0009 14527 0018 14541 0027 14554 0042 14578 0060 14604 0074 14628

064

OBS

STD STD STD STD

0122 0310 34626 2760 0125 0312 3463 2760 0005070 0150 0326 3466 2761 0004993 0200 0351 3472 2763 0004821 0250 0371 3477 2765 0004689

146*5 0088 14647 0100 14657 0125 14677 0149 14694

064

OBS STD

T0259 0377 34788 2766 0300 0385 3482 2768 0004504

14700 0172 14709

064

OBS STD STD

0393 0399 34875 2771

0400 0398 3488 2771 0004287

0500 0385 3488 2773 0004240

14731 0216 14732 0258 14743

064

OBS STD STD

T0590 0376 34888 2774 0600 0375 3489 2775 0004147 0700 0370 3489 2775 0004180

14754 0300 14756 0342 14770

064

OBS STD STD STD

T0784 0365 34896 2776 0800 0364 3490 2776 0004162 0900 0359 3490 2777 0004182 1000 0355 3490 2777 0004212

14782 0384 14784 0425 14799 0467 14814

064

OBS

T1041

0353

34897

2777

14820

LATITUDE

I/IO

DAV HR.I/K

ORIGINATOB'S

T

CLOUD THER COOES I CODE

NODC STATION NUMBER

0it71it W

\i*9 11 04 07 083 |1965 001 9293

09

SPttD

OR FORCE

506

AIR TEMP. *C

Oil

b612

24 |4

X2 I 6 l8

0059

s •/..

NOj-N

083 083

STD

OBS STD STD STD

OBS STD

OBS STD STD STD STD

OBS STD STD STD

OBS STD STD

OBS

0000 0000

0010 0020 0030 0035 0050 0053 0075 0100 0125 0150 0159 0200 0260 0300 0389 0400 0500 T0579

-0052

-0054

-0065

-0057

-0058

-0057

-0007

0045

0094

0139

0154

0209

0267

0314

0373

0374

0382

0388

3329

33285

3329

3330

33300

3331

33319

3353

3374

3394

3412

34178

3433

3449

3463

34796

3480

3484

34866

2677 2677 2677 2678 2678 2678 2679 2680 2695 2709 2722 2733 2737 2745 2753 2760 2767 2767 2770 2771

0012B72

0012830 0012782 0012740

0011168 0009830 0008601 0007538

0006492 0005802 0005217

0004635 0004533

0000

0013 0026 0038

0012640 0064

0094 0120 0143 0163

0198 0229 0256

0306 0351

14445 14445 14446 14447 14448 14448 14451 14452 14482 14512 14542 14568 14577 14610 14646 14676 14719 14721 14741 14757

lOI

REFERENCE

SHIP CODE

LATITUDE

I/IO

LONGITUDE i^ '1/10 ~

MARSDEN

STATION

Tl

ME

ORIGINATOR'S

DEPTH

MAX.

WAVE

WEA-

IHEfi CODE

CLOUD CODES

cm

ID.

NO.

CRUISE STATION NO. NUMBER

TO BOTTOM

OF S'MPL'S

STATION NUMBER

CODE

10*

1"

MO

DAY

HR.1/10

DIR-

MGllPEP SE*

lYPl AM

31

540

EV

4

700

N

04

?30 W 1

149

77 04

07

095

1965

001 9294 3212

02

25

3I

X?

3^8

0060

WATER

WIND

BARO- METER (mbil

AIR TEMP. 'C

VIS COD

NO. OBS. DEPTHS

SPECIAL OBSERVATIONS

COLOR CODE

IftANS,

DIR.

SPEED

OB FOPCE

DRY

BULB

WET BULB

04

S05

156

005

000

5

06

MESSENCa

riMt c

HR l/IO

CAST NO.

CARD

TYPE

DEPTH (ml

T -C

s ■'..

SIGMA-T

SPECIFIC VOLUME

ANOMALT-Xia'

SAD

DYN. M.

X 10'

SOUND VELOCITY

03 ml/I

PO,-P

„.../i

tOTAl-P KB -oi/l

N03-N

NOi-N 1,8 ■ 01/1

SIOh-Si

V9 . o./l

pH

S

c c

STD

0000

-0098

3307 I266I 1 0014382

0000

14421

096

OBS STD STD

0000 0010 0020

-0098 33067 2661 14421 -0101 3307 2661 0014351 0014 14421 -0103 3307 2661 0014315 0029 14422

096

OBS STD STD

0029 0030 0050

-0104 33074 2662 14423 -0104 3308 2662 0014247 0043 14423 -0098 3316 2668 0013641 0071 14430

096

OBS

STD

0072 0075

-0092 33247 2675 14438 -0090 3325 2675 0012965 0104 14439

095

OBS STD STD

0097 0100 0125

-0049 33357 2682 14464

-0034 3339 2584 0012105 0135 14471

0072 3365 2700 0010658 0164 14528

096

OBS

STD STD

0125

0150 0200

0075 33550 2701 14529 0103 3385 2714 0009344 0189 14549 0162 3405 2725 0008243 0233 14586

096

OBS

T0208

0171

34059

2725

14591

REFERENCE

SHIP

CODE

LATITUDE

\/\0

LONGITUDE * '1/10

l\

MARSDEN

STATION

TIME

ORIGINATOR'S

DEPTH

MAX. DEPTH

OF S'MPL'S

WAVE

WEA- THER CODE

CLOUD CODES

CTHY CODE

ID. NO.

CRUISE

STATION NUMBER

TO

BOTTOM

STATION NUMBER

10*

r

MO

DAY

HR.1/10

\ "O-

DIP.

HGI PER SEA

ITPE AM

31

540

EV

I*

659

N

04744 W

149

67

54

07

108

1965

'001

9295 3181

02

27

3 2

XI

3 6

0061

WATER

WIND

BARO- METER Imbtl

AIR TEMP. -C

^"dEs

SPECIAL OBSERVATIONS

COLOR CODE

TRANS.

DIR.

SPEED

OR FOPCE

DRT BULB

WET

BULB

.

01

S02

159

006

000

8

05

MESUNCR

TIME 01 HR I/IO

CAST NO.

CARD TYPE

DEPTH Iml

I -c

s •/..

SlGMA-T

iCECIdC VOLUME ANOWALT-XIO'

SAO

DYN. M.

X 10^

SOUND VELOCITY

O2 ml/I

PO4-P „ - .1/1

lOTAl-p „ - .1/1

NOj-N

m-oi/i

NO]-N Kg - ol/l

SIO4-SI pg - DI/I

;H

s

c c

STD

0000 1 -0090

3312

2665

0014016

0000

14425 1

108

OBS STD STO STD STD STO

0000 -0090 33118 2665 14425 0010 -0091 3311 2664 0014059 0014 14426 0020 -0092 3311 2654 0014050 0028 14427 0030 -0093 3311 2564 0014051 0042 14428 0050 -0095 3310 2563 0014109 0070 14431 0075 -0098 3310 2664 0014087 0105 14434

108

OBS STD STD

0085 -0099 33099 2663 14435 0100 -0098 3310 2654 0014059 0141 14438 0125 -0095 3311 2664 0014023 0176 14443

108

OBS

STD

0125 -0095 33106 2654 14443 0150 -0105 3317 2669 0013481 0210 14443

108

OBS

0150 -0106 33170 2669 14443

10

3

OB

T0175

OC

73

33

5

96

27

0«

14537

REFERENCE	SHIP CODE	LATITUDE 1/10	LONGITUDE '1/10	°s	MARSDEN	STATION Tl	VE			ORIGINATOR'S	DEPTH	MAX	•,		WAVE		WEA- THtll CODE	CLOUD CODES		NODC
CIRY CODE	ID. NO.			YEAR	CRUISE NO.	STATION NUMBER	TO BOTTOM	OF S'MPL'S		STATION NUMBER
10-	1"	MO	DAY H	.1/10	DIB.	HGI PE» if*	ITPl *M
31	540	EV	4	700	N	04800 W		149	78	D4	07 124	1955	001	9296	0144	01	04	2 4	X4	5 8	0062
				WATER	WIND	BARO- METER (mbll	AIR TEMP. X	"-D?p"t^HS	SPECIAL OBSERVATIONS
	COLOR CODE	TRANS-	DIR.	SPEED OR fORCE	DRY BULB	WET BULB
			02	S02	173	022	Oil	5 07
	MESSENCR 1 TIME 01 HR 1/10	CAST NO.	CARD TYPE	DEPTH (m)	T -C	s •/..	SlGMA-T	SPECIFIC VOLUME ANOMALY-IIO'	SAO DYN. M. I 10'	SOUND VELOCITY	Oi ml/I	PO4-P vg - ot/i	lOTAl-P UB- o'/l	NOj-N UB-ol/l	NO3-N llfl - Dl/I	51 04-Si ug - oi/l	pH	i c c
			STD	0000	-0058	3307	2650	0014503	0000	14439
	124		OBS STD STD ST3	0000 -0058 33069 0010 -0050 3307 0020 -0053 3307 0030 -0057 3307	2660 2660 2650 2660	14439 0014483 0014 14440 0014460 0029 14440 0014433 0043 14440
	124		OBS STD	0035 -0059 33073 0050 -0077 3310	2650 2653	14440 0014195 0072 14439
	124		OBS STD	0050 -0077 33097 0075 -0073 3325	2663 2675	14439 0013027 0105 14447
	124		OBS	0075 -0073 33250	2675	14447
	124		OBS STD STD	0090 -0040 33375 0100 -0024 3345 0125 0034 3355	2684 2590 2703	14467 0011616 0137 14477 0010377 0164 14511
	124		OBS	0125 0034 3380P	2714P
		12	>t		OB	3	0135		OC	64	33	7	44	27	Oi	)						145	27

108

REFERENCE

SHIP CODE

LATITUDE

1/10

LONGITUDE ■ '1/10

ii

MARSDEN

STATION T

ME

ORIGINATOR'S

DEPTH

MAX. DEPTH

OF S'MPfS

WAVE

WEA- THER CODE

CLOUD CODES

coot

10. NO.

CRUISE NO.

STATION NUMBER

TO

BOTTOM

STATION NUMBER

- 10-

r

MO

DAY H

R.1/10

oia.

hgtI rif SEA

TYPE AM

31

540

EV

i

1410

N 1 04(

142 W

149

48 04

09 324

1965

CKS

9297 3896

08

^4

2I

XI

5 3

0053

WATER

WIND

BARO- METER (mbi)

AIR TEMP. "C

vii.

COD

NO. OBS. DEPTHS

SPECIAL OeSERVATIONS

COLOR CODE

TRANS.

OIR.

SPEED oa

EOSCf

DfiV BUL9

WET

euLB

33

S12

234

000 -006

8

07

ME5SENGB HR I/IO

C*ST NO.

CARD TYPE

DEPTH (ml

T \:

s •/■..

SIGMA-T

SPECIFIC VOlUMf ANOMAH-IlO'

SAD

DfN. M. X 10^

SOUND VELOCITY

Ol ml/I

P04-P

TOTAL-P

ve - Di/i

NOj-N

P9- ol/l

NO3-N KS - Ol/I

SI 04-Si UO-al/l

pH

S

c

STD

0000

-0033

3323

2672

0013367

0000

14453

024

OBS STD STD STD

0000 -0033 33230 2672 14453 0010 -0026 3330 2677 0012858 0013 14459 0020 -0018 3337 2682 0012354 0026 14465 0030 -0009 3343 2687 0011933 0038 14472

024

OBS STD STD . STD STD STD STD

0047 0006 33538 2695 14463 0050 0011 3356 2696 0011031 0061 14486 0075 0053 3371 2705 0010105 0087 14512 0100 0092 3385 2715 0009269 0111 14535 0125 0129 3399 2724 0008449 0134 14558 0150 0162 3411 2731 0007777 0154 14578 0200 0222 3431 2742 0005748 0190 14616

024

OBS STD STD

0211 0233 34352 2745 14623 0250 0264 3445 2750 0006077 0222 14644 0300 0300 3455 2755 0005685 0252 14669

024

OBS STD STD

T0365 0338 34670 2761 14698 0400 0354 3471 2762 0005093 0305 14711 0500 0385 3481 2767 0004773 0355 14743

024

OBS STD

T0542 0393 34832 2768 14753 0500 0391 3485 2770 0004622 0402 14762

024

OBS STD STD

0576 0388 34858 2772 14773 0700 0387 3487 2772 0004534 0448 14777 0800 0384 3487 2772 0004583 0493 14792

024

OBS

T0804

0384

34859

2772

14793

REFERENCE	SHIP CODE	LATITUDE 1/10	LONGITUDE ' "I/lO	ii	MARSDEN	STATION	11	WE			ORIGINATOR-S	DEPTH TO BOTTOM	MAK	;		WAVE		WEA- THER CODE	CLOUD COOES			"JOOC
CT»»	ID. NO.				CRUISE NO.	STATION NUMBER	OF S'MPL-S			STATION NUMBER
CODE	10- 1 r	MO	DAV	HH.1/10	DIK.	HCI PEP !£*	7»Pl AM
31	540	EV	4346	N	04840 W		149	138 1	D4	u	119	1965	CKS	9298	829	13	13	2 4	X4	X 9	0064
			WATER	WIND	BARO< METER Ifnb»l	AIR TEMP. "C	COD	NO. OBS. DEPTHS	SPECIAL OBSERVATIONS
		COLOR CODE	IRANi.	DIR.	S?E(0 OR FOJiCt	DRY BULB	WEI eULB
				12	S13	071	061	061	1	08
	MtSSENGP (-.c, ""' ° NO. HR 1/10	CARD TYPE	DEPTH Iml	T -C	s '/.,	SIGMA-T	SPECIFIC VOLUME ANOM*LY_II0'	SAD DVN. M X 10'	SOUND VELOCITY	O7 ml/1	P04-P	TOTAl-P vg - o'/l	NO3-N V9 - ol/l	NOj-N »i ■ ol/l	SIO«-S. HO -or/I	pH	s c c
		STD	0000	0103	3355	2690	0011640	0000	14520
119	OBS	0000 0103 33546 2690	14520
	STD	0010 0102 3361 2595 0011147 0011	14522
	STD	0020 0101 3356 2699 0010761 0022	14523
	STD	0030 0100 3372 2704 0010299 0033	14525
119	OBS	0037 0099 33759 2707	14527
	STD	0050 0119 3384 2712 0009509 0053	14539
	STD	0075 0154 3398 2721 0008585 0075	14561
	STD	0100 0187 3410 2728 0008020 0095	14581
	STD	0125 0217 3422 2736 0007353 0116	14600
	STD	0150 0245 3433 2742 0005752 0133	14518
	STD	0200 0292 3451 2752 0005844 0155	14649
119	OBS	T0225 0311 34582 2755	14662
	STD	0250 0319 3461 2758 0005378 0193	14670
	STD	0300 0334 3455 2760 0005261 0219	14585
	STD	0400 0358 3473 2754 0004985 0271	14713
119	OBS	0444 0355 34754 2765	14724
	STD	0500 0375 3480 2767 0004728 0319	14738
	STD	0500 0385 3485 2771 0004480 0355	14759
119	OBS	0664 0387 34878 2772	14771
	STD	0700 0382 3488 2773 0004389 0410	14775
	STD	0800 0371 3488 2774 0004352 0453	14787
119	OBS	0884 0355 34885 2775	14798
	STD	0900 0365 3489 2775 0004297 0496	14801
	STD	1000 0365 3490 2775 0004318 0540	14818
	STD	1100 0357 3490 2775 0004413 0583	14836
119	OBS	T1124 0357 34905 2777	14840
	STD	1200 0356 3491 2777 0004443 0627	14852
	STD	1300 0363 3491 2777 0004475 0572	14868
		11	9	OB	3	T1321		0;	62	34	9	08		27	7	7						148	71

109

REFERENCE

SHIP CODE

LATITUDE

I/IO

LONGITUDE ' '1/10

i'i

MARSDEN

STATION T

ME

ORIGINATOR'S

DEPTH

MAX

WAVE

WEA- THER CODE

ClOUD CODES

NOOC

CIRT

CODE

ID.

NO.

CRUISE NO.

STATION NUMBER

BOTTOM

OF

S'MPL-

STATION NUMBER

10-

r

MO

DAY HH.1/10

S Di".

HOT PER SfA

lYPt AM

31

540

EV

i

347

N

04846 W

149

38

D4

11 147

1965

CKS

9299 )759

04

13

2 2

X4

4 8

0065

WATER

WIND

eAHO- METER

(mbll

AIR TEMP. -C

„,< NO. CODE °"- DEPTHS

SPECIAL OBSERVATIONS

COLOR CODE

THANS.

Olft.

SPEED

OR FORCE

DRY BULB

WET BULB

16

510

003

050

044

1

06

MESSENGR HR 1/10 '

CAST NO.

CARD TYPE

DEPTH (ml

I t

s ■/„

S1GMA-T

S«CIFIC VOLUME ANOMAlY-mo'

SAD

DYN. M.

X 10'

SOUND VELOCITY

Ol ml/l

PO4-P

„fl - o./l

TOTAL-P vg • ol/l

NO3-N

ug-ol/l

NOj-N

pg - or/I

SIO<-Si ug -al/l

pH

S

c

STD

0000 I 0022

3332

2676

0012963 loOOO

14480

147

OBS STD STD

0000 0022 33315 2676 14480 0010 0035 3339 2681 0012453 0013 14488 0020 0044 3354 2693 0011362 0025 14496

147

OBS

STD

0020 0044 33539 2693 14495 0030 0046 3380 2714 0009384 0035 14502

147

OBS STD STD STD STD STD

0040 0048 34028 2732 14508 0050 0060 3404 2732 0007633 0052 14515 0075 0089 3406 2732 0007654 0071 14533 0100 0115 3409 2733 0007594 0090 14549 0125 0138 3412 2733 0007525 0109 14564 0150 0159 3415 2734 0007453 0128 14578

147

OBS STD STD

0198 0191 34203 2736 14600 0200 0192 3421 2737 0007264 0165 14501 0250 0207 3426 2740 0007026 0200 14617

147

OBS STD

0297 0226 34326 2743 14634 0300 0227 3433 2744 0006687 0235 14635

147

OBS

T0396 0277 34497 2753 14675

REFERENCE

SHIP CODE

LATITUDE

1/10

LONGITUDE

'i/lo

°i

MAfiSDEN SQUARE

STATION TIME IGMTl

YEAR

ORIGINATOR'S

DEPTH TO

BOTTOM

MAX.

DEPTH

OF

S'MPL-

WAVE OBSERVATIONS

WEA- THER CODE

CLOUD CODES

NODC STATION

CTBY

coot

ID. NO.

CRUISE NO.

STATION NUMBER

10'

r

MO

DAV HR.1/10

DIR. HGTiPCel SEA

IYP£ AMI

.-.UIVTOL-

31

540

EV

4

355

N

04907 W

149

39

D4

11 169

1965

CKS

9300 0165

02

.11

3I4I

X4

4 8

0066

WAE.

WIND

BARO- METER

AIR TEMP. -C

V. ! -°-

SPECIAL OBSERVATIONS

COLOR CODE

IRANS,

DIR.

SPEED

OR FORCE

DRY BULB

WET BULB

COD

OSS. DEPTHS

16

SIO

997

072

0

08

MESSENGR

TIME a

HR 1/10 1

CAST NO.

CARD TYPE

DEPTH (ml

T t

s •/..

SIGMA-T

SCECIflC VOLUME ANOMALT-HO'

SAD

DYN. M.

I 10'

SOUND VELOCITY

0; mU\

PO^-P

lOIAl-P „9 - ol/l

N02-N u8 - al/l

NO3-N vg - ol/l

SlO^-Si

wg - ol/l

PH

s

c c

1

STD

0000

0070

3315

2660

0014452

0000

14499

159

OBS

STD

0000 0070 33152 2660 14499 0010 0052 3315 2561 0014355 0014 14493

169

OBS

0010 0052 33152 2561 14493

169

OBS STD STD

0015 0000 33200 2568 14470 0020 -0002 3321 2669 0013647 0028 14470 0030 -0004 3325 2572 0013338 0042 14472

169

OBS

0030 -0004 33249 2672 14472

159

OBS STD STD

0040 -0005 33322 2678 14474 0050 -0003 3335 2680 0012566 0058 14477 0075 0002 3346 2689 0011722 0098 14485

169

OBS STD

0075 0002 33463 2689 14485 0100 0050 3367 2703 0010421 0126 14514

159

OBS STD STD

0100 0050 33666 2703 14514 0125 0057 3370 2705 0010194 0152 14522 0150 0064 3374 2707 0009961 0177 14529

16

5

OB

S

T0160

oc

67

33

7

51

27

Of

14533

REFERENCE

SHIP CODE

LATITUDE

1/10

ii

MARSDEN

STATION

TIME

ORIGINATOR'S

DEPTH

MAX

WAVE

WEA- THER CODE

CLOUD CODES

NODC

CTRY

coot

ID. NO.

LONGITUDE * "l/IO

CRUISE NO.

STATION NUMBER

TO BOTTOM

Of S'MPL'S

STATION NUMBER

10*

r

MO

DAY

HR.1/10

DIR-

M0J,„ S,A

lYPt AW

31

540

EV

4400

N

04919 W

149

49 (

14

n

laa

1965

TKS

9301

D038

00

14

3I

X4

4 8

0067

WATffi

WIND

BARO- METER Imbsl

AIR TEMP, "C

VIS, COD

NO.

OBS. DEPTHS

SPECIAL

OBSERVATIONS

COLOR CODE

IRANi.

SPEID DIR. OR

FORCE

DRY BULB

WET BULB

36 SIO

973

050 050

7

02

MESSENGR CAST TIME c\q_ HR 1/10

CARD TYPE

DEPTH [ml

T -C

s-/..

SIGMA-T

SPECIFIC VOLUME

ANOMAH-IIO'

5 A D

DYN. M.

X 10'

SOUND VELOCITY

03 ml/l

PO4-P

TOTAl-P

NO2-N vg ' ol/l

NO3-N vg - ol/l

510^-Si vg - al/l

pH

s c c

STD

0000 1 0059

3314 I2559

0014523

0000

14494

188

OBS 0000 0059 33135 2659 14494 STD 0010 0054 3313 2660 0014502 0015 14493 STD 0020 0049 3313 2660 0014489 0029 14493 STD 0030 0044 3313 2660 0014469 0043 14492

18

3

OB

S

0035

oc

41

33

1

30

26

6C

144

91

110

SHIP CODE

0*919 W

O DAY HR.1/1

1*9 *9 0* 12 OIB 1965 CKS 9302

SPUD

OR tORCi

ORIGINATOR'S

3057 I 00 I 17 13

OBSERVATIONS

0068

018 018

018

STO

CBS

OBS STO

OBS STD STD STD

OBS

0000 0000 0008 0010 0015 0020 0030 0050 0050

0091

0066

00*3

-0007

-0008

-0009

13309 33092 33117 3313 33173 3317 3317 3317 33170

265* 265* 2658 2660 2666 2666 2666 2666 2666

0015025

001**76 0015

0013906 0013908 0013912

0029 00*3 0071

1*508 1*508 1**98 1**88 1*467 1**68 1**69 1**72 1**72

HEfERENCE

SHIP CODE

LATITUDE

l/IO

n

MARSOEN

STATION

TIME

ORIGINATOR'S

DEPTH

MAX.

DEPTH

OF S'MPL-S

WAVE

WEA- THER CODE

CLOUD CODES

CI»« CODE

10.

NO.

LONGITUDE * 'l/IO

cruise) STATION

TO BOTTOM

STATION NUMBER

.0- 1 r

MO

DAY

MR.1/10

DH. |mGI| Pf»l SEA

l»PI AM

31

540

EV

**38

N

04905 W

149

149 1

D4

12

046

1965

CKS

9303 :071

00

14

U2I

X4

* 8

0069

WATER

WIND

BARO- METER Imbi)

AIR TEMP, -C

VIS- COO

NO. OBS. DEPTHS

SPECIAL OBSERVATIONS

COLOR CODE

TRANS. Iml

OIR.

SPEED

0»

DRY BULB

WET BULB

16

508

963

050 050

0

03

TIME ,\a. HR 1/10

CARD TYPE

DEPTH Iml

T -C

s •/,.

SIGMA-T

incmc VOLUME

ANOMALIr-XlO'

SAD

OVN. M. X 10'

SOUND VELOCITY

0; ml/I

P04-P

WR-OI/I

TOTAL-P V9 ■ »l/l

NO3-N

us - Ql/I

NO3-N

110 - ol/l

SlO^-Si

we - oi/i

pH

S

c c

STD

0000

0030

3325

2670 0013498

0000

14482

048

OBS 0000 0030 33250 2670 1**82

STO 0010 0024 3325 2670 0013466 0013 1**81

STD 0020 0017 3325 2671 0013*38 0027 1**80

048

OBS 0020 0017 332*9 2671 1*480

STD 0030 0009 3327 2673 0013238 0040 14478

STD 0050 -0012 3335 2680 0012525 0066 14473

0*

J

OB

3

0050

-0(

nz

33

3

50

26

8C

14473

REFERENCE

SHIP CODE

LATITUDE

1/10

LONGITUDE ' 'l/IO

if

MARSDEN

STATION

11

^E

ORIGINATOR'S

DEPTH

OF S'MPL'S

WAVE

WEA- THER CODE

CLOUD COOES

^ODC

CIRY CODE

ID. NO.

YEAR

CRUISE NO.

STATION NUMBER

TO BOTTOM

STATION NUMBER

10-

r

MO

DAY

HH.1/10

DIB.

HGT PER SfA

UPE AM

31

5*0

EV

i

1*35

N

0*855 W

149

48

14

1?

:i7a

1965

CK.S

9304

D603

05

14

ft 2

X6

5 8

0070

WATER

WIND

BARO- METER Imbsl

Aid TEMP. "C

VIS.

coo

NO.

OBS. DEPTHS

SPECIAL

OBSERVATIONS

COLOR CODE

TRANS.

DIR.

SPEED

OB fOflCl

DRY BULB

WET BULB

15

516

932

061

1

07

MESSENGR

HR l/IO

CAST

NO.

CARD

TYPE

DEPTH Iml

T -C

s v..

SIGMA-T

SPECIFIC VOLUME ANOMALI-HO'

SAD

OYN. M.

X 10^

SOUND VELOCITY

O3 ml/l

POi-P

rOTAl-p vg ■ oi/l

NO3-N ua - Qi/i

NO]-N

ug - oi/l

SIO*-Si P9 - or/1

pH

s

c c

STO

0000

-0034

3308

2660

0014480

0000

14451

i

078

OBS STD STD STD

0000 -003* 3308* 2660 1**51 0010 -0023 3311 2661 001*321 001* 1**58 0020 -0013 3317 2666 0013905 0029 1**65 0030 -0002 3327 2673 0013185 0042 14473

078

OBS STD

0049 0018 33557 2695 1**89

0050 0025 3358 2697 00109*8 0066 1**93

078

OBS STD STD STD STD

0058 0082 33737 2706 1*522 0075 0083 3375 2707 0009973 0092 1*526 0100 0087 3377 2709 00098*6 0117 1*532 0125 0096 3381 2711 0009600 01*1 1*5*1 0150 0109 3386 2715 0009306 0165 1*551

078

OBS STD STD STD

0193 0142 33978 2722 14575 0200 0157 3402 2724 0008*36 0209 1*583 0260 02** 3*30 27*0 0007032 02*8 1*633 0300 0296 3**9 2750 0006098 0281 1*667

078

OBS

T0315 030* 3452* 2752 1*673

078

OBS STD STD

0370 0307 3*597 2758 1*685 0400 0313 3*6* 2761 0005206 0337 1*693 0500 0357 3*75 2765 000*909 0388 1*730

07

3

OB

5

T0533

0-

79

34

7

89

27

6f

3

141

45

111

31 540 EV

LATITUDt

1/10

4437 N

LONGITUDE

■1/10

04836 W

ORIGINATOR'S

149 48 04 12 139 1965 CKS 9305

SPEED

(0»CE

AIR TEMP. "C

15 S12 902 078 078 1 11

12

NODC STATION NUMBER

0071

SIGM

SOUND VELOCITY

139

139 139 139

139 139

139

139 139

STD

OBS STD STD

OBS STD

OBS STD STD STD

OBS STD STD

OBS STD STD STD

OBS STD STD

OBS STD

OBS

0000 0000 0010 0020 0022 0030 0043 0050 0065 0075 0100 0125 0128 0150 0200

T0234 0250 0300 0400 0467 0500 0600

T0641 0700 0800 0821 0900 1000

T1024 1100

T1189

0197 0197 0215 0244 0251 0305 0354 0343 0329 0341 0369 0395 0398 0420 0460 0479 0476 0468 0448 0434 0424 0399 0392 0388 0381 0379 0370 0361 0360 0357 0356

3364

33636

3373

3384

33862

3398

34114

3413

34183

3426

3444

3459

34602

3468

3482

34894

3490

3492

3494

34947

3494

34931

3493

34927

3492

3491

34910

3491

34911

2690 2690 2697 2703 2704 2709 2715 2717 2723 2728 2739 2749 2749 2753 2760 2764 2765 2767 2771 2773 2774 2776 2776 2776 2777 2777 2778 2778 2778 2778 2778

0011574

0010997 0010390

0009842

0009063

0008085 0007016 0006168

0005774 0005207

0004844 0004661 0004394

0004196 0004079

0004085 0004096

0004131 0004171

0000

0011 0022

0032

00 51

0072 0091 0108

0123

0150

0175 0199 0244

0287 0329

0369 0410

0452 0493

0004222 0535

14563 14563 14573 14589 14593 14619 14644 14641 14638 14646 14664 14682 14683 14697 14724 14739 14740 14745 14754 14759 14760 14766 14770 14778 14792 14794 14804 14817 14820 14832 14846

REFERENCE

SHIP CODE

LATITUDE

1/10

LONGITUDE

* '1/10

n

MARSDEN

STATION

Tl

VIE

ORIGINATOR'S

DEPTH

MAK

■

WAVE

WEA- THER CODE

CLOUD

CODES

'JODC

CUT CODE

31

ID. NO.

CRUISE NO.

STATION NUMBER

TO BOTTOM

OF S'MPL'S

STATION NUMBER

10-

r

MO

OAT

HH.VIO

OIR.

HGI PER SEA

tYPE AM

540

EV

4429

N

04758 W

149

47

D4

1?

180

1965

CK.S

9306

292

11

64

0 5

X4

4 8

0072

WATER

WIND

BARO- METER

AIR TEMF. -C

VIS, COD

NO. OBS. DEPTHS

SPECIAL OBSERVATIONS

COLOR

CODE

ISANS.

DIR.

OR tO«C(

DRY BULB

WEI

GULS

14

S30

831

111

106

5

11

■'"■ ""o

HR 1/10

CARD TYPE

DEPTH 1ml

T -C

s ■''..

SIGMA-I

SPECIFIC VOLUMt ANOM*I.»-X10'

SAD DYN. M.

X to5

SOUND VELOCITY

Ol ml/l

ro4~r

TOTAl_P vg - ol/l

NOj-N ug - al/l

NO)-N lig - o'/I

SI 0«-Si

wg - ol/l

pH

S

c c

STD

0000

0432

3404

2701

0010564 0000 1 14669

180

OBS

0000 0432 34039 2701 14669

STD

0010 0431 3404 2701 0010566 0011 14670

180

OBS

0014 0429 34045 2702 14670

STD

0020 0417 3405 2704 0010350 0021 14666

STD

0030 0399 3405 2705 0010181 0031 14660

STD

0050 0371 3406 2709 0009852 0051 14652

180

OBS

0064 0358 34077 2712 14649

STD

0075 0351 3409 2713 0009457 0075 14648

180

OBS

0078 0350 34097 2714 14648

STD

0100 0352 3415 2718 0009032 0099 14653

STD

0125 0354 3424 2725 0008393 0120 14659

180

OBS

0129 0354 34251 2726 14660

STD

0150 0373 3434 2731 0007848 0141 14673

180

OBS

T0176 0399 34459 2738 14690

STD

0200 0436 3459 2744 0006667 0177 14711

180

OBS

0231 0468 34721 2751 14731

STD

0250 0468 3475 2754 0005875 0208 14735

STD

0300 0462 3481 2759 0005414 0237 14741

180

OBS

T0339 0452 34847 2763 14744

STD

0400 0424 3487 2758 0004647 0287 14743

180

OBS

0429 0412 34885 2770 14743

STD

050O 0397 3489 2772 0004297 0332 14748

STD

0600 0379 3489 2774 0004191 0374 14757

STD

0700 0365 3489 2776 0004124 0416 14768

STD

0800 0354 3490 2778 0004012 0456 14780

STD

0900 0346 3490 2778 0004004 0496 14793

186

OBS

T0930 0344 34906 2779 14798

STD

1000 0341 3491 2780 0003953 0536 14808

STD

1100 0340 3492 2780 0003947 0576 14824

18

i

OB

s

T1128

03

40

34

9

24

27

8

148

29

112

RfFfRENCE

SHIP CODE

LATITUDE

1/10

LO

GITUDE * 'I/IO

n

MARSDEN

STATION

TIME

ORIGINATOR'S !

DEPTH

1 MA)

■

WAVE

WEA- THER

CODE

CLOUD CODES

NODC

cm

CODi

ID. NO.

CRUISE

NO.

STATION NUMBER

TO -■;■■

BOTTOM ;.„°'^.;

STATION

NUMBER

10*

r

MO

OAy

HR.I/10

D1«.

"01 UK SE*

tin AW

31

540

EV

4812

8N

050590W

150

80 04

29

201

1965

CI^S

9307 3192

1 02

29

4 2

X?

6 8

0073

WATER

WIND

BARO>

METER (mbl)

AIR TEMP. -C

^».D^S

SPECIAL OBSERVATIONS

COLOR CODE

TUNS.

DHL

into

Oi FO«C(

ORT BULB

WET BULB

30

S22

963

022

016

7

05

HR 1/10

CARD TYPE

DEPTH (ml

T t

s •/..

SIGMA-T

SfECIMC VOLUME

AHOMAlt-lie'

SAD

DYN. M.

X 10'

SOUND VELOCITY

0) ml/1

PO<-P vg - oi/l

lOTAl-P t>e - al/l

NOj-N vg - ot/1

NGj-N PS - al/l

SI04-S< i>g - ol/l

PH

s c c

1

STD

0000

-0102

3277

2637

0016648

0000

14415

201

OBS

0000 -0102 32770 2637 14415

STD

0010 -0098 3280 2539 0016422 0017 14418

STD

0020 -0095 3283 2542 0016198 0033 14422

STD

0030 -0091 3285 2543 0015050 0049 14426

STD

0050 -0084 3287 2644 0015910 0081 14433

201

OBS

0052 -0083 32871 2545 14433

201

OBS

0051 -0084 32870 2644 14435

STD

0075 -0077 3300 2655 0014925 0119 14442

STD

0100 -0059 3320 2670 0013452 0155 14457

STD

0125 -0035 3336 2682 0012337 0187 14475

201

OBS

0125 -0035 33358 2582 14475

STD

0150 -0004 3348 2690 0011545 0217 14495

201

OBS

T0169

0023

33545

2694

14511

REFERENCE

SHIP

CODE

ii

MARSDEN

STATION

Tl

WE

ORIGINATOR'S

DEPTH

MAI

WAVE

WEA- THER CODE

CLOUD CODES

CTIT CODI

ID. NO.

I/IO

'1/10

CRUISE NO.

STATION NUMBER

TO BOTTOM

Of S'MPL'S

STATION NUMBER

10*

r

MO DAY

HR.1/10

DIR.

HCI PER SEA

ITPI AM

31

540

EV

48126N

050590W

150

80

34 30

067

1965

CKS

9308 3150

01

27

3 2

XI

3 3

0074

WATER

WIND

BARO- METER |mb»)

AIR TEMP. "C

VIS- COD

NO.

OBS.

DEPTHS

SPECIAL OBSERVATIONS

COLOR CODE

TRANS.

DIH.

iCEID

OR FORCE

DRY BULB

WET BULB

26

S13

976

006

000

7

05

HR 1/10 J

CARD TYPE

DEPTH [ml

T -C

s ■/..

SIGMA-T

SPECIFIC VOLUME *NOM*II-I10'

SAD

DYN, M. X 103

SOUND

VELOCITY

Oj ml/I

POj-P VS - o'/l

TOTAL-P PB - ol/l

NOi-N pg - oi/l

NOj-N PB- ol/l

SlO^-Si

pg - al/l

pH

S

c c

STD

0000 1-0083

3286

2643

0016048

0000

14425

067 OBS 0000 -0083 32856 2643 14425

STD 0010 -0084 3286 2643 0016032 0016 14426

STD 0020 -0085 3286 2644 0016016 0032 14427

STD 0030 -0085 3286 2644 0016000 0048 14^*29

STD 0050 -0087 3286 2644 0015961 0080 14431

067 OBS 0054 -0087 32862 2644 14^*32

STD 0075 -0113 3297 2653 0015034 0119 14i>25

067 DBS 0079 -0118 33000 2656 14423

STD 0100 -0035 3333 2680 0012559 0153 14470

067 OBS 0118 0008 33490 2691 14495

STD 0125 0018 3352 2693 0011357 0183 14501

06

7

OB

3

0138

oc

26

335

41

26

9fi

14507

REFERENCE

SHIP CODE

LATITUDE

1/10

LONGITUDE

• -i/io

li

MARSDEN

STATION

TIME

ORIGINATOR'S

DEPTH

MAK

■

WAVE

WEA-

THER

CODE

CLOUD CODES

CRT CODE

ID.

NO.

CRUISE

NO.

STATION NUMBER

TO BOTTOM

OF S'MPL'S

STATION NUMBER

lo-

r

MO

DAY

HB.1/10

DIR.

MCI PER S

A

irp( AM

31

540

EV

4

812

SN

050590W

150

80

34

30

173

1965

CKS

9309

3192

02

20

3 I2

X?

6 8

0075

WATER

WIND

BARC METE Imbi

-

R

1

AIR TEMP, -C

VIS- COD

NO.

OBS. DEPTHS

SPECIAL OBSERVATIONS

COLOR CODE

IRAN5.

DIR.

SPEED

DRY BULB

WET BULB

26

S17

017

005

003

7

05

MESSENCR

TIME 0

HR T/10

CAST NO.

CARD TYPE

DEPTH (ml

T -C

s •/..

SIGMA-T

SPECIFIC VOLUME

AKOMALT-lia'

SAD

DYN, M. X 10^

SOUND VELOCITY

03 ml/I

PO4-P VB - o'/l

rOTAl-P

UB - o*/l

NO3-N

ug • ol/l

NO3-N t)g - ol/l

SI o*-si

ug - Ol/l

pH

s

c c

STD

0000 1-0110

3275

2636

0016763 0000

14411

173

OBS STD STD STD STD

0000 -Olio 32752 2535 0010 -0109 3276 2537 0020 -0108 3277 2537 0030 -0108 3278 2538 0050 -0105 3281 2540

14411 0015674 0017 14413 0015585 0033 14415 0016505 0050 14417 0016329 0083 14422

173

OBS STD

0060 -0105 32817 2641 0075 -0136 3293 2551

14424 0015250 0122 14413

173

OBS STD STD

0075 -0136 32933 2551 0100 -0094 3313 2565 0125 -0051 3330 2578

14413 0013857 0159 14440 0012711 0192 14465

173

OBS STD

0135 -0034 33355 2682 0150 -0008 3345 2688

14477 0011754 0222 14492

17

3

OB

5

T0170

OC

26

33

5

55

26

9!

145

13

113

REFERENCE

SHIP CODE

LATITUDE

1/10

LONGITUDE * -1/10

i^

MARSDEN

STATION

TIME

ORIGINATOR'S

DEPTH

MAX

WAVE

WEA- THER CODE

CLOUD CODES

CTRV CODE

ID. NO.

YEAR

CRUISE NO.

STATION

NUMBER

TO

OF

STATION NUMBER

10*

1*

MO

DAY

HR.1/10

BOTTOM jj.^pi^.j

Dl». H&ll?£ft| S

A

fin At*

31

540

EV

L

>812

BN

050590W

150

80

05

01

D79

1965

CKS

9310 )247 1 02

23 ?

u

XI

0 1

0076

WATER

WIND

BARO- METER (mbt)

AlB TEMP. X

VIS.

coo

NO. OBS.

DEPTHS

SPECIAL OBSEHVAIIONS

COLOR TRANS.

CODE '")

D1R.

SftED

FO»ce

09.1 BULfl

WET BULB

25

510

058

003

000

7

06

MES5ENGR

IIMf C

HR 1/10

CAST NO.

CARD

TYPE

DEPTH Iml

T -C

s •/..

SIGMA-T

SPECIFIC VOLUME ANOMALT-XlO'

SAD

DYN. M.

X 10'

SOUND VELOCITY

0; ml/I

P04-P

ve-o'/i

(OTAL-P

ug - ol/l

N02-N i>g - ol/l

NO3-N vg - ol/l

S104-Si

wg - oi/l

PH

c c

STD

0000

-0085

3280

2639

0016501

0000

14423

079

OBS STO STO STD

0000 -0085 32796 2639 14423 0010 -0088 3280 2539 0016494 0016 14423 0020 -0091 3280 2639 0016478 0033 14423 0030 -0094 3279 2639 0016471 0049 14424

079

OBS STO

0041 -0097 32793 2639 14424 0050 -0112 3282 2641 0016202 0082 14419

079

OBS STD

0057 -0122 32843 2643 14416 0075 -0144 3296 2654 0015021 0121 14410

079

OBS STD STD

0082 -0146 33008 2657 14411 0100 -0091 3318 2670 0013485 0157 14442 0125 -0031 3336 2682 0012340 0189 14477

079

OBS STD STD

0143 0000 33459 2688 14495 0150 0003 3347 2689 0011655 0219 14498 0200 0025 3355 2694 0011183 0276 14517

079

OBS

T0205

0027

33554

2695

14519

REPEftENCE

SHIP CODE

ii

MARSDEN

STATION

Tl

WE

ORIGINATOR'S

DEPTH

MAX. DEPTH

OF S'MPl'S

WAVE

WEA- THER

CODE

CLOUD COOES

JODC

CTBY CODE

ID. NO.

1/10

' 'l/IO

CRUISE NO.

STATION NUMBER

TO BOTTOM

STATION NUMBER

10-

r

MO

DAY

HR.1/10

DIt

HGT nt StA

TYPE AM

31

540

EV

47570N

050515W

150

70

05

0?

075

1965

CKS

9311 3133

01

?4

2 2

X4

X 9

0077

WATER

WIND

BARO- METER

AIR lEMP. -C

VIS,

coc

NO.

OBS. DEPTHS

SPECIAL

OBSERVATIONS

COLOR CODE

'""'■

DIR.

SPEED

OB FO«Ct

DRY BULB

WET

BULB

31

SO 2

986

on

006

6

05

""■ •: no!

HK l/)0

CARD

TYPE

DEPTH (ml

T X

s •/..

SIGMA-T

SPECIFIC VOLUME ANOMALr-JlO'

SAD

DYN. M.

X 103

SOUND VELOCITY

Oj ml/I

PO4-P

V9 -ol/l

TOTAL-P

NOl-N ug - ot/1

NO3-N vg-oi/l

SI04-Si

PH

S

c c

STD

0000

-0157 3284

2644

0015936

0000

14390

075 OBS 0000 -0157 32844 2644 14390

STD 0010 -0078 3285 2643 0016105 0016 14429

075 OBS 0010 -0078 32850 2643 14429

STD 0020 -0087 3285 2643 0016046 0032 14426

STD 0030 -0097 3286 2644 0015994 0048 14423

STD 0050 -0115 3266 2645 0015887 0080 14418

STD 0075 -0138 3287 2646 0015751 0120 14411

075 OBS 0075 -0138 32867 2646 14411

STD 0100 -0030 3337 2683 0012246 0155 14473

075 OBS 0100 -0030 33374 2683 14473

STD 0125 0007 3348 2690 0011636 0184 14496

07

0

OB

3

0125

OC

07

33

4

75

26

9C

)

14496

REFERENCE

SHIP CODE

MARSDEN

STATION

Tl

WE

ORIGINATOR'S

DEPTH

MAX. DEPTH

OF S'MPL'S

WAVE

WEA- THER CODE

CLOUD CODES

NOOC

CI»»

CODE

10.

NO.

UTITUDE

1/10

LONGITUDE

•i/io

YEAR

CRUISE NO.

STATION NUMBER

TO BOTTOM

STATION NUMBER

10*

1"

MO

DAY

HR.1/10

DtfL

HGI PER SEA

ITP[ *M

31 540

FV

47570N

05O515W

150

70

■)-,

0?

20?

1965

CKS

9312

141

01

??

2 2

XI

2 2

0078

WATER

WIND

BARO- METER {mb»l

AIR TEMP. X:

VIS. COD

NO,

OBS. DEPTHS

SPECIAL OBSERVATIONS

COLOR CODE

TPANS,

DIR.

SPEED

OB FOBCE

DRY BULB

WET BULB

22

SO9

010

017

009

7

05

MtSSENC«lcAST

I.ME Of f^Q

HR 1/10

CARD

TYPE

DEPTH (ml

T -C

s ■'..

SIGMA-T

SPECIFIC VOLUME ANOMALT-XlO'

SAD DYN. M.

X 10'

^°^^° Oiml/I VELOCITY "^ '^'

PO4-P

i>i ■ ol/l

TOTAL-P wg - Ol/l

NO3-N

ug - ol/l

NOj-N

M9-0I/I

SI O4-SI vg - ol/l

pH

S

c c

STD

0000

-0037

3284

2640

0016328

0000

14446

202 OBS 0000 -0037 32841 2640 14446

STD 0010 -0079 3284 2642 0016163 0016 14428

202 DBS 0010 -0079 32842 2642 14428

STD 0020 -0088 3285 2643 0016082 0032 14426

STD 0030 -0097 3285 2644 0016001 0048 14423

STD 0050 -0115 3287 2645 0015850 0080 14418

202 OBS 0073 -0135 32879 2647 14413

STD 0075 -0122 3294 2651 0015236 0119 14420

202 OBS 0098 -0020 33396 2684 14478

STD 0100 -0019 3340 2685 0012106 0153 14479

STD 0125 -0001 3344 2687 0011846 0183 14491

20

2

OB

D

0127

OC

00

33

4

45

26

8"

r

14^

92

114

REFERENCE		LATITUDE l/IO	LONGITUOE * "l/io	i\|	MARSDEN	STATION	Tl	WE			ORIGINATOR'S	DEPTH	MAX. DEPTH OF S'MPL"		WAVE		WEA- THER CODE	CLOUD COOES		NODC
cr«T	10. NO.	CODE				CRUISE NO.	STATION NUMBER	BOTTOM			NUMBER
CODE	10-	r	MO	DAY	MR.1/10	DIX.	MGT Pt» itA	ItPE *w
31	■)40	FV	4	844	N	04S19 W		149	88 05	07	089	1965	002 9313	2195	12	34	5 4	X?	6 8	0079
			WATER	WIND	BARO- METER Imbjl	AIR TEMP,	■c	™-dEs	SPECIAL OBSERVATIONS
	COLOR CODE	TRANS.	DIR.	SPEED OB fO«C£	DRY BULB	WEI BULB
				34	S16	081	044	039	7	08
	Mf55ENG» TIMt 0 HR 1/10	CAST NO.	CARD TYPE	DEPTH ImJ	I -c	s •/..	SIGMA-T	S^fCIFIC VOLUME NOMLT-X10'	SAO DYN. M. X 10'	SOUND VELOCITY	Ol ml/l	PO4-P	TOTAL-P Jig - ol/l	NOj-N MS - ol/l	NOj-N iig - or/l	SIO4-SI vg - oi/l	pH	S c c
			STD	0000	0350	3452	2748	0005150	0000	14641
089		OBS	0000 0350 S'tSZO 2748	14641
		STD	0010 0346 3452 2748 0006121	0006 14541
		STD	0020 0344 3452 2748 0006111	0012 14542
		STD	0030 0341 3452 2749 0006091	0018 14642
		STD	0050 0338 3452 2749 0006087	0031 14544
089		OBS	0055 0337 34519 2749	14546
		STD	0075 0341 3455 2751 0005901	0046 14550
		STD	0100 0349 3452 2756 0005470	0050 14658
		STD	0125 0355 3469 2761 0005032	0073 14665
		STD	0150 0362 3474 2764 0004736	0085 14574
089		OBS	0174 0367 34790 2767	14680
		STD	0200 0367 3480 2768 0004375	0108 14685
		STD	0250 0366 3481 2769 0004335	0130 14593
		STD	0300 0355 3482 2770 0004295	0151 14701
		STD	0400 0363 3484 2772 0004216	0194 14717
089		OBS	0404 0353 34842 2772	14717
		STD	0500 0365 3485 2773 0004180	0236 14734
		STO	0500 0367 3488 2774 0004161	0277 14752
089		OBS	0610 0367 34878 2774	14754
		STD	0700 0367 3489 2775 0004146	0319 14769
		STD	0800 0365 3489 2776 0004210	0361 14785
089		OBS	0820 0364 34894 2776	14788
		STD	0900 0359 3489 2776 0004226	0403 14799
		STD	1000 0354 3489 2777 0004252	0445 14813
089		OBS	T1051 0352 34888 2777	14821
		STD	1100 0350 3489 2777 0004308	0488 14828
		STD	1200 0348 3489 2777 0004372	0532 14844
		089		OBS	T124:		0347	34885		2777								14831

REFERENCE	SHIP CODE	LATITUDE 1/10	LONGITUDE * -1/10	li	MARSDEN	STATION	Tl	tAE			ORIGINATOR'S	DEPTH	MAX DEPTH OF S'MPL-		WAVE		WEA- THER CODE	CLOUD CODES			NODC
CT.y CODE	ID. NO.				CRUISE NO,	STATION NUMBER	BOTTOM	OBStBv«iiu">		NUMBER
10-	r	MO	DAY	MR.I/10	DIP.	HCI PER SE»	TYPE *M
31	'140	EV	4839	N	04825 U		149	88 (	)«!	07	109	1965	no?	9314	2085	13	nl		X5	5 8	0080
			WATER	WIND	BARO- METER (mbl)	AIR TEMP.	■c	VIS- COO	NO. OBS. DEPTHS	SPECIAL OBSERVATIONS
	COLOR CODE	TdANS,	DIR.	SFEEO OR fOBCE	DRY BULB	WET BULB
				36	518	095	055	050	5	08
	"iSiiNMlcAST ""' "NO. HR 1/10	CARD TYPE	DEPTH (ml	T -C	s ■/..	SIGMA-T	SPECIfiC VOLUWi ANOMALY-IIO'	SAO DYN. M. » 10=	SOUND VELOCITY	Oj ml/l	PO4-P	lOTAL-P	N03-N WB - ol/l	NOj-N vg . ot/l	SI 04-Si 119 . o(/l	pH	S c c
		STD	0000	0344	3449	2746	0006299	0000	14638
109	OBS	0000 0344 34493 2745		14538
	STD	0010 0344 3450 2746	0006279	0006 14640
	STD	0020 0343 3450 2747	0005257	0013 14641
	STO	0030 0342 3450 2747	0006247	0019 14642
	STD	0050 0341 3451 2747	0006208	0031 14645
	STD	0075 0340 3451 2748	0005170	0047 14549
	STD	0100 0339 3452 2749	0006125	0062 14553
109	OBS	OHO 0338 34523 2749		14554
	STD	0125 0343 3457 2752	0005810	0077 14559
	STD	0150 0350 3464 2757	0005371	0091 14667
	STD	0200 0361 3475 2755	0004620	0116 14682
109	OBS	0221 0355 34794 2758		14587
	STD	0250 0355 3480 2768	0004402	0139 14692
	STD	0300 0365 3482 2770	0004294	0150 14701
	STD	0400 0364 3485 2773	0004152	0203 14717
109	OBS	T0441 0354 34857 2773		14724
	STD	0500 0364 3486 2773	0004163	0244 14734
	STD	0600 0364 3487 2774	0004175	0285 14751
109	OBS	T0662 0354 34879 2775		14751
	STD	0700 0364 3488 2775	0004187	0328 14767
	STD	0800 0364 3489 2775	0004199	0370 14784
109	OBS	0883 0362 34900 2777		14797
	STD	0900 0361 3490 2777	0004158	0411 14800
	STD	1000 0356 3490 2778	0004171	0453 14814
	STD	1100 0352 3491 2778	0004184	0495 14829
109	OBS	T1125 0351 34908 2778		14833
	STD	1200 0349 3490 2778	0004281	0537 14845
	STD	1300 0348 3489 2777	0004422	0581 14851
		10	9	OB	S	T132i		0	348	3^	8	88		27	7	7						14(	55

115

REFCRENCE

SHIP CODE

LATITUDE

1/10

LONGITUDE

'I/IO

li

MABSOEN

STAriON

Tl

VIE

ORIGINATOR'S

DEPTH

•,

WAVE

WEA- THER CODE

CLOUD CODES

^ODC

CTBY CODE

ID. NO.

CRUISE NO.

STATION NUMBER

TO BOTTOM

OF S'MPL-S

STATION NUMBER

10*

r

MO

DAY

MR.1/10

DIIL

HGT PtR S(A

tvn *M

31

540

EV

u

835

N

04831 W

1^9

88 05

07

127

196S

002

9315 1866

12

35

3 4

X?

5 a

nn«i

WATER

WIND

BARO- METER

lmb»l

AIR TEMP. -C

^°°' DEPTHS

SPECIAL OBSERVATIONS

COLOR CODE

'^.T-

DIR.

SPEED

FORCE

DRY BULB

WET BULB

36

S18

112

061

050

B

10

MESSENO 1

TlwC 01 Hft 1/10

CAST NO.

CARD TYPE

DEPTH Iml

T -C

s •/..

SIGMA-T

Sl-fClflC VOLUME ANOMALT-XlO'

SAD

DYN. M.

X 10'

SOUND VELOCITY

Oj ml/1

PO4-P

IOI4t-P

NOi-N

ue - ot/i

NO3-N

PB - 01/1

SI0<-S1

pH

S

c c

STO

0000

0264

3423

2732

0007591

0000

14600

127

OBS

0000 0264 34230 2732 14600

STD

0010 0266 3427 2735 0007310 0007 14503

STD

0020 0268 3430 2738 0007105 0015 14606

STD

0030 0270 3433 2740 0006901 0022 14509

127

OBS

0041 0272 34347 2741 14612

STD

0050 0262 3435 2743 0006622 0035 14509

127

OBS

0052 0250 34362 2743 14609

127

OBS

0072 0305 34500 2750 14533

STD

0075 0308 3451 2751 0005901 0051 14535

STD

0100 0327 3459 2755 0005490 0055 14549

STD

0125 0344 3465 2759 0005142 0078 14561

STD

0150 0359 3472 2763 0004867 0091 14672

127

OBS

0181 0374 34783 2765 14586

STD

0200 0373 3479 2757 0004539 0114 14687

STO

0250 0371 3480 2758 0004485 0137 14695

STD

0300 0369 3481 2769 0004435 0159 14702

STD

0400 0355 3483 2771 0004329 0203 14717

127

OBS

T0414 0364 34830 2771 14719

STD

0500 0367 3485 2772 0004291 0245 14736

STD

0500 0370 3487 2773 0004274 0289 14753

127

OBS

T0621 0371 34870 2773 14757

STD

0700 0371 3488 2774 0004287 0332 14770

STD

0800 0369 3489 2775 0004285 0375 14786

127

OBS

0828 0368 34889 2776 14791

STD

0900 0365 3489 2776 0004290 0417 14801

STD

1000 0360 3489 2776 0004318 0461 14815

127

OBS

T1056 0357 34891 2777 14824

STD

1100 0359 3489 2776 0004378 0504 14832

STD

1200 0357 3489 2776 0004544 0549 14852

127

OBS

T1242

0372

34895

2775

14862

SHIP CODE

LONGITUDE

•i/io

ORIGINATOR'S

Gil PES SEA

NODC STATION NUMBER

31 540 EV 4829 N 04842 W

149 |88 105 |07 |144 Il965 |002 9316

36 S15 122

BARO- METER (mbil

072

056 7

546

11

12

0082

I X

s '

SPECIFIC VOLUME

SOUND VELOCITY

NO3-N ug - ol/l

14A

144 144 144

144

144 144 144 144 144 144

STD

OBS STD STD

OBS STD

OBS STD STD STD

OBS STD STD

OBS

0000 0000 0010 0020 0021 0030 0031 0050 0057 0076 0100 0126 0129 0150 0200 0250 0269 0300 0400

T0414 0500 0600

T0621 0700 0800 0828 0900 1000

T1055 1100 1200

T1242

0110 Olio 0109 0108 0108 0095 0094 0125 0139 0182 0236 0281 0287 0308 0349 0375 0380 0379 0375 0375 0373 0371 0371 0371 0371 0371 0366 0350 0358 0356 0354 0353

3369

33588

3 360

3352

33519

3370

33714

3390

33953

3412

3431

3447

34489

3465

3470

3479

34807

3481

3482

34820

3484

3486

34866

3487

3488

34880

3488

3489

34886

3489

34888

2593 2593 2594 2695 2596 2703 2704 2717 2721 2730 2741 2750 2751 2755 2752 2757 2758 2768 2759 2769 2771 2772 2772 2773 2774 2774 2776 2775 2775 2776 2777 2777

0011362

0011244 0011124

0010423

0009098

0007823 0006813 0006998

0005678 0004962 0004690

0004513 0004603

0004412 0004405

0004377 0004376

0004366 0004359

0004387 0004430

0000

0011 0022

0033

0053

0074 0092 0108

0123 0149 0173

0195 0241

0285 0329

0373 0417

0461 0604

0648 0592

14523 14523 14525 14525 14626 14623 14523 14543 14651 14575 14606 14531 14635 14548 14576 14597 14700 14705 14722 14724 14738 14764 14757 14770 14787 14792 14802 14815 14824 14831 14847 14853

116

REFSRENCE	SHIP CODE	LATITUDE 1/10	LONGITUDE ■ ■i/u	n	MAR$OEN	STATION	Tl	WE			ORIGINATOR'S	DEPTH	MAX	;		WAVE		WEA- THER CODE	CLOUD CODES			ODC
CIIY	ID. NO.				CRUISE NO.	STATION NUMBER	BOTTOM	OF S'MPL'S			STATION NUMBER
	10*	r	MO	DAY	HR.l/IO	DIP.	HOT PEP SE*	irPE AM
31	san	FV	4	821	N	0*854 W		149	88 05	07	161	1965	00?	9317	097	09	_3^i_	5 3	X4	4 5	0083
			WATER	WIND	BARO- METER Imbil	AIR TEMP.	•c	coo	NO. OBS. DEPTHS	SPECIAL OBSERVATIONS
	COLOR CODE	TKANS.	DID.	SPIED OR FOPCI	DRY WET BULB BULB
				35	S12	125	039 028	7	08
	MESSfNGR 1 TIME 01 HR 1/10 T	CAST NO.	CARD TYPE	DEPTH (ml	T -C	s ■/..	SIGMA-T	JPtCtfiC VOLUME ANOMAL'-XIO'	SAD DYN. M. > 10>	SOUND VELOCITY	02 ml/1	PO<-P l/B-o'/l	rOTAL-P „a ■ .1/1	NO3-N us - ot/l	NO3-N PO- ol/l	SIO<-Si pg - 01/1	PH	S C C
	1		STD	0000	0109	3346	2683	0012300	0000	14521
161		OBS	0000 0109 SSfce* 2683	14521
		STD	0010 0098 3352 2688 0011808	0012 14519
161		OBS	0019 0090 33566 2692	14517
		STD	0020 0092 3357 2692 0011393	0024 14518
		STD	0030 0107 3365 2698 0010875	0035 14528
		STD	0050 0137 3381 2709 0009853	0055 14547
		STD	0075 0172 3398 2720 0008811	0079 14569
		STD	0100 0204 3414 2730 0007846	0100 14589
		STD	0125 0234 3428 2739 0007036	0118 14608
		STD	0150 0260 3440 2746 0006360	0135 14625
161		OBS	0195 0301 34576 2757	14653
		STD	0200 0304 3458 2757 0005427	0164 14655
		STD	0250 0333 3465 2760 0005137	0191 14677
		STD	0300 0356 3472 2763 0004955	0216 14696
161		OBS	T0341 0370 34760 2765	14709
		STD	0400 0370 3478 2767 0004721	0265 14719
		STD	0500 0370 3482 2770 0004525	0311 14736
161		OBS	0568 0370 34845 2772	14748
169		OBS	T0584 0370 34838 2771	14750
		STD	0600 0370 3484 2771 0004463	0355 14753
		STD	0700 0369 3486 2773 0004396	0400 14769
169		OBS	0782 0369 34871 2774	14783
		STD	0800 0371 3487 2774 0004404	0444 14787
		STD	0900 0384 3488 2773 0004569	0489 14809
		169		OBS	T0905		0385	34884		2773							14810

REFERENCE	SHIP CODE	LATITUDE 1/10	LOP	GITUDE '1/10	li	MARSDEN	STATION	TIME			ORIGINATOR'S	DEPTH	MAX. DEPTH OF S'MPL'S		WAVE		WEA- THER CODE	CLOUD CODES				JODC
City CODE	ID. NO.				CRUISt NO.	STATION NUMBER	TO BOTTOM			STATION NUMBER
10*	r	MO	DAY	HR.I/10	01R.	HGI PEP SE*	IfP! *M
31	•>40	FV	4	814	N	04903 W		149	89	^5	07	185	1965	00?	9318	3320	03	34	5 3	XI	7 7		0084
			WATER	WIND	BARO- METER [mbil	AIR TEMP,	•c	VIS. COO	NO. OBS. DEPTHS	SPECIAL OBSERVATIONS
	COLOR CODE	IKANS.	DIR.	SPIED OR FORCE	DRY BULB	WEI BULB
				32	S12	129	022	Oil	7	10
	MEtSENGR 1 TIME 0' HR 1/10	CAST NO.	CARD TYPE	DEPTH Im)	T -C	s ■/.,	SIGMA-T	SPECIFIC VOLUME ANOMALY-llO'	SAD DYN. M. > 10=	SOUND VELOCITY	01 ml/l	PO<-P	lOTAL-f vfl - o./l	NOi-N UB - ol/l	NQj-N KB - ot/l	SI O4-S. UB - Ol/I	pH	s c c
			STD	0000	-0016	3303	2655	0014975	0000	14458
185		OBS	0000 -0016 33029 2655	14458
		STD	0010 -0023 3303 2655 0014936	0015 14457
		STD	0020 -0029 3304 2656 0014829	0030 14456
185		OBS	0029 -0035 33054 2657	14455
		STD	0030 -0042 3306 2658 0014620	0045 14452
185		OBS	0040 -0100 33082 2552	14427
		STD	0050 -0090 3309 2552 0014204	0073 14433
185		OBS	0073 -0071 33275 2577	14448
		STD	0075 -0070 3331 2679 0012581	0107 14450
185		OBS	0083 -0064 33431 2689	14455
185		OBS	0088 0080 33505 2688	14523
185		OBS	0098 0062 33511 2697	14518
		STD	0100 0062 3363 2599 0010764	0136 14519
185		OBS	0107 0053 33698 2704	14521
		STD	0125 0102 3384 2713 0009410	0161 14544
		STD	0150 0152 3403 2725 0008311	0183 14573
		STD	0200 0239 3435 2744 0006587	0221 14524
185		OBS	0219 0267 34445 2749	14640
		STD	0250 0307 3458 2757 0005490	0251 14665
		STD	0300 0358 3474 2764 0004825	0277 14697
		18	5		OB	3	T0316		0:	70	34	7	78		27	b(	3							147	05

117

REFERENCE	SHIP CODE	LATITUDE VIO	LONGITUDE ' '1/10	ii	MARSDEN	STATION	Tl	ME			ORIGINATOR'S	DEPTH	MAX.		WAVE		WEA- THER CODE	CLOUD CODES			<ODC
CTRT CODE	ID. NO.				CRUISE NO.	STATION NUMBER	BOTTOM	OF S'MPL-S			STATION NUMBER
10-	r	MO	DAY	HR.1/10	DIP.	MGI PIP SI*	t'Pi AM
31	■)40	FV	«	807	N	04912 W		149	89 05	07	199	1965	00?	_9J15_	^230	02	33	5 3	X?	7 8	0085
			WATER	WIND	SARO- METER Imbtl	AIR TEMP.	■c	coo	NO. OBS. DEPTHS	SPECIAL OBSERVATIONS
	COLOR CODE	TftANt,	DIR.	SCEfO OR fOUCt	DRT BULB	WET BULB
					32	318	135	022	017	7	07
	MISStNGR TIME t HR 1/10 '	CAST NO.	CARD TYPE	DEPTH Iml	T -C	s •/..	S1GMA-T	SPECIFIC VOLUME ANOMALT-X10'	SAD DYN. M. > 10'	SOUND VELOCITY	Oj ml/1	PO,-P wa-ai/i	TOTAl-p „a - oi/i	NOl-N ua - oi/l	NO,-N wa - oi/i	S1O4-SI PS - oi/i	pH	5 C C
			STD	0000	-0053	3266 12643	0016106	0000	14439
199		OBS	0000 -0053 32862 2643		14439
		STD	0010 -0064 3287 2643	0016031	0016 14435
		STD	0020 -0075 3287 2644	0015949	0032 14432
		STD	0030 -0086 3288 2645	0015875	0048 14429
199		OBS	0045 -0101 32882 2646		14424
		STD	0050 -0106 3289 2647	0015684	0080 14423
		STD	0075 -0131 3296 2653	0015057	0118 14416
199		OBS	0088 -0142 32996 2656		14414
		STD	0100 -0151 3302 2659	0014524	0155 14412
		STD	0125 -0170 3310 2666	0013844	0190 14408
199		OBS	0135 -0177 33144 2669		14407
		STD	0150 -0101 3323 2674	0013040	0224 14446
199		OBS	0150 -0101 33230 2674		14446
199		OBS	0170 0019 33480 2689		14509
		STD	0200 0114 3375 2705	0010178	0282 14560
		199		OBS	T0225		0116	33887		2716								14557

LATITUDE

1/10

LONGITUDE

'1/10

ORIGINATOR'S

WEA- THER CODE

I 31

540

EV

4800 N

04925 W

149 |89 I05 |07 I2I3 Il965 1002 19320

33 316 142

BARO- METER

Imbsl

022 017

3165 I 02 I 32 B

0086

SPECIFIC VOLU

PO4-P vo - oi/l

213

213 213 213

213

STD

OBS STD STD

OBS STD

OBS STD STD

OBS

0000 0000 0010 0020 0024 0030 0048 0050 0072 0075 0100 0120 0125 0150 T0151

-0011

-0011 -0012 -0013 -0013 -0028 -0075 -0082 -0138 -0137 -0121 -0096 -0088 -0038 -0011

3282

32816

3282

32817

3283

32888

3289

32978

3299

3309

33205

3324

3343

33531

2637

2537 2637 2637 2637 2639 2646 2546 2555 2566 2563 2572 2674 2688 2595

0016625

0016618 0016602

0016435 0015763

0014810 0014074

0013023 0011766

0000

0017 0033

0120 0156

0190 0221

144 58 14458 14459 14460 14461 14455 14437 14434 14413 14414 14427 14443 14448 14478 14494

REFERENCE

SHIP CODE

LATITUDE

1/10

LONGITUDE ' '1/10

ii

MARSDEN

STATION

T

ME

ORIGINATOR'S

DEPTH

MAX

:i

WAVE

WEA- THER CODE

CLOUD COOES

CIPY CODE

ID. NO.

YEAR

CRUISE NO.

STATION NUMBER

TO BOTTOM

OF S'MPL'S

STATION NUMBER

10'

1-

MO

DAY

HH.1/10

Oi»-

HCi n» 5fA

Tr»! AW

31

540

EV

4752

N 1 04<

)35 W

149

79

05

07

226

1965

002

9321

D163

02

33

3 5

X7

5 8

0087

WATER

WIND

BARO- METER Imbtl

AIR TtMP. -C

coo

NO.

OBS. DEPTHS

SPECIAL OBSERVATIONS

COLOR TRANS. CODE im)

DIP.

SPEED oa

(0«CE

DRY BULB

WET BULB

32 |s22

152

017

Oil

7 |04

MESSENC

TIME HR 1/1

"IcAST «, NO.

CARD

TYPE

DEPTH Iml

T 'C

S '/.. SIGMA-T

SPEClfIC VOLUME ANOMAL'-IIO'

SAO

DYN. M. X 10^

SOUND VELOCITY

Ol ml/l

V8 - ot/l

lOTAL-P

NO3-N

ug - ol/l

NO3-N US • Ol/l

SIO4-S1 pg-oi/l

pH

S

c c

22(

>

STD OBS

0000 0000

-0080 -0080

3282 2640 32819 2640

0016341

0000

14426 14426

STD

0010 -0077 3282 2540 0015339 0016 14429

STD

0020 -0074 3282 2640 0016329 0033 14432

STD

0030 -0070 3282 2640 0016327 0049 14435

22

OBS

0031 -0070 32823 2640 14435

STD

0050 -0090 3284 2642 0016120 0081 14430

STD

0075 -0115 3292 2650 0015410 0121 14423

STD

0100 -0141 3305 2661 0014322 0158 14417

22

3

OBS

0104 -0145 33072 2663 14416

STD

0125 -0097 3323 2674 0013068 0192 14444

STD

0150 0001 3348 2690 0011570 0223 14497

22

3

OB

D

T0155

OC

26

33

5

33

26

9:

145

10

118

REFfRtNCt

SHIP CODE

^«

MARSDEN

STATION TIME

ORIGINATOR'S

DEPTH

MAX.

DEPTH

OF

WAVE

WEA-

CLOUD 1 1 NODE

cmt

ID.

LONGITUDE

X?

CRUISE

STATION

TO BOTTOM

THER

CODES

STATION

cool

1/10

■1/10

10'

r

MO

DAY

HH.VIO

NUMBER

S'MPL'S

Din

HOT PER SEA

T'PE AM

31

"740

FV

4738

N

04857 W

149

7B

:>'}

08

n,7

1965

00?

9322 3152

ni

34

6 4

X7

5 a

WATER

WIND

BARO- METER

AIR TEMP. *C

VIS. con

NO. OBS.

SPECIAL OBSERVATIONS

COLOR

TRANS.

SPEED

OdY

WET

CODE

'""

lOtCt

(mbt)

BUL8

BULB

32 S18

146

006

000

7

05

M£SSENG» LcAST ""' • NO. HR 1/10

CARD lYPJ

DEPTH (ml

T -C

s */„

SIGMA-T

SPECIFIC VOLUMt

ANOMAir-KlO'

SAD DYN. M.

X 10'

SOUND VELOCITY

0; ml/I

PO4-P

WB-ol/l

TOTAL-P v9 ■ o'/l

NO,-N us • oi/l

NO3-N

VS - ot/l

SIO4-SI pg - oi/l

PH

S

c

STD

0000

-0074 I328A

2641

0016239 0000

14429

017

OBS 0000 -0074 32835 2641 14429

STD 0010 -0078 3284 2642 0016197 0016 14428

STD 0020 -0084 3284 2642 0016156 0032 14427

STD 0030 -0092 3284 2643 0016101 0049 14425

STD 0050 -0112 3285 2644 0015988 0081 14419

017

OBS 0052 -0114 32849 2544 14419

017

OBS 0072 -0141 32977 2655 14411

STD 0075 -0135 3302 2558 0014585 0119 14415

STD 0100 -0084 3330 2579 0012592 0153 14447

STD 0125 -0026 3350 2593 0011295 0183 14481

017

OBS 0128 -0018 33512 2694 14485

017

OBS

T0149

0038

33590

2697

14515

LONGITUDE

'1/10

O DAY iHR.I/ll

ORIGINATOR'S

on PER SE»

WEA- THER CODE

31 1540 EV

04845 W

149 178 105 IO8 1032 11965 |002|9323

AIR TEMP. "C

33 S14 142 022 017 7 05

3186

NO. OBS. DEPTHS

J12_

X2 5 l8

0089

NOj-N ug- ol/l

032 032

STD

OSS STD STD

OBS STD STD STD

OBS

0000 0000 0010 0020 0026 0030 0050 0075 0088 0100 0125 0150 0166 T0181

-0054

-0056

-0058

-0059

-0072

-0123

-0153

-0154

-0100

-0015

0035

0050

3288

32878

3288

32874

3288

3293

3302

33077

3321

3343

3356

33604

33610

2644 2644 2544 2644 2644 2645 2651 2659 2663 2572 2587 2695 2698 2698

00159 00159

00158 00153 00145

00132 00118 00111

76 79

85 27 37

24 79 45

0000

0016 0032

0048 0079 0115

0151 0183 0211

14439 14439 14439 14440 14440 14435 14415 14407 14409 14438 14485 14514 14524 14526

MO DAY HR.1/1

ORIGINATOR'S

OBSERVATIONS

31 540 EV 4750 N 04833 W

149 178 105 lOB 1045 11965 |002|9324

Oil

221 I 02 I 35 3 |3

0090

'"«~='1CAST TIME 0- NO.

SPECIEIC VOLUME

SAD DYN. M.

X 10'

SOUND VELOCITY

NOi-N

ug • oi/l

NOj-N U9 - 01/1

SIO4-S1

xg - oi/l

045

045 045

STD

OBS STD STD STD

OBS STD STD

OBS STD

OBS

OBS STD

OBS

0000 0000

0010 0020 0030 0030 0050 0075 0091 0100 0125 0132 0150

T0158 0193 0200

T0218

-0079

-0082

-0085

-0091

-0105

-0125

-0137

-0128

-0103

-0096

-0015

0034

0047

0066

0144

3286

32860

3286

3287

32869

3290

3294

32959

3300

3314

33194

3337

33508

33655

3373

33973

2643 2643 2644 2544 2645 2545 2548 2561 2553 2555 2567 2671 2582 2591 2702 2707 2721

0016030

0015992 0015950 0015905

0015515 0015266

0014742 0013735

0000

0016 0032 0048

0079 0118

0155 0191

0012330 0224

0010024 0280

14427 14427 14427 14427 14426 14426 14423 14419 14416 14422 14440 14445 14488 14515 14528 14538 14580

119

REFERENCE

SHIP CODE

LATITUDE

1/10

LONGITUDE * "I/IO

n

MARSOEN

STATION TIME

TEAR

ORIGINATOR'S

DEPTH

MAX.

WAVE

WEA- THER CODE

CLOUD

CODES

CliT

CODE

ID. NO.

CRUISE

NO.

STATION NUMBER

TO

BOTTOM

OF S'MPL'S

STATION NUMBER

10"

T

MO

DAY HR.1/10

OIB,

HCf n* ua

Tin AM

31

'>i*0

FV

*

759

N

0*821 W

1^9

78

DS

08 0

58

1965

002

9325 0282

03

35

4 3

X4

4 3

0091

WATER

WIND [ j^g^

R

AIR TEMP. ^C

V15.

coo

NO.

OBS. DEPTHS

SPECIAL OBSERVATIONS

COLOR CODE

IBANi.

imj

DIR.

i«tO METF

FOSCf ''"'•'

DRY BULB

wtl

flULB

35

SIO 146

072

067

7

06

TIMt 0 HB 1/10

CAST NO.

CARD

TYPE

DEPTH Iml

T -C

s •/■..

SIGMA-T

IPtCIFIC VOIUME AN0MALl-«'6'

SAD

DYN. M. X 10^

SOUND VELOCITY

Oj ml/1

PO4-F'

lOTAi-r

wg - oi/l

NOj-N

Kg . ar/l

NOj-N

va - oi/i

SlO^-Si

V9 - ot/l

pH

s

c c

STD

0000

-0052 13284

2641

0016278

0000

14439

058

OBS STD STD

0000 -0052 328*0 26*1 0010 -0055 328* 26*1 0020 -0058 3285 26*2

14439 0016240 0016 14439 0016202 0032 14440

058

OBS

STD STD

0025 -0059 328*7 26*2 0030 -0078 3286 26*3 0050 -013* 3292 2650

14440 0016017 0049 14432 0015373 0080 14410

058

OBS STD

0051 -0136 32923 2660 0075 -01*3 3301 2658

14409 0014640 0117 14411

058

OBS STD STD STD

STD

0091 -01*8 33086 266* 0100 -0112 3320 2672 0125 -0022 33*8 2691 0150 005* 3371 2706 0200 0161 3*05 2726

14412

0013260 0152 14432 0011466 0183 14482 0010107 0210 14524 0008238 0256 14585

058

OBS STO

T0223 0191 3*15* 2732 0250 0210 3*22 2736

14604 0007351 0295 14618

058

OBS

T027*

0213

342'»3

2738

14623

REFERENCE

SHIP

CODE

LATITUDE

1/10

LONGITUDE

'I/IO

li

MARSDEN

STATION Tl

WE

ORIGINATOR'S

DEPTH

MAX

•,

WAVE

WEA- THER

CODE

CLOUD

CODES

■JODC

CTKT COOf

ID.

NO.

YEAR

CRUISE NO.

STATION NUMBER

TO BOTTOM

OF S'MPL'S

STATION

NUMBER

10"

T

MO

DAY H

.1/10

OIB-

HGI »E« SEA

TYPE AM

31

540

FV

4

805

N

0*812 W

149

86

35

0« D

75

1965

00?

9326

3*13

n*

35

t* I*

XI

7 6

0092

WATER

WIND

BARO- METER (mbil

AIS TEMP. X

„,t NO.

COOE 0"5- DEPTHS

SPECIAL OBSERVATIONS

COLOR CODE

TRANS.

DIR.

SPEED

OP (OtCI

DRY BULB

WET BULB

35

S13

1*9

022

017

7 07

MESStNCR 1 TIME 01

HH VIO

CAST NO.

CARD TYPE

DEPTH (ml

T -C

s •/„

SIGMA-T

SPECIFIC VOIUME ANOMALT-IIO'

SAO

DYN. M. X 10'

SOUND VELOCITY

Ol ml/I

PO^-P

PB - oi/l

rOTAl-P

Vfl . ol/l

NOl-N WB-oi/l

NO3-N Vfl - oi/l

siOi-si

MS - =1/1

pH

s c

c

STD

0000 1-0031

3287

26*3

0016122

0000

1***9

075

OBS

0000 -0031 32871

26*3 1***9

STD

0010 -0032 3287

26*3 001611* 0016 1**50

075

OBS

0010 -0032 32871

26*3 1**50

STD

0020 -0113 3292

26*9 0015*52 0032 1**15

075

OBS

0026 -01*2 329*7

2652 1**03

STD

0030 -01*8 3297

265* 001*967 00*7 1**01

075

OBS

0036 -0156 33000

2657 1*398

STD

0050 -0106 3318

2670 0013*62 0076 1**27

STO

0075 -002* 33*7

2690 00115*7 0107 1**73

STD

0100 0051 3373

2708 00099*0 013* 1*515

STD

0125 0117 3396

2722 0008597 0157 1*552

STD

0150 0175 3*16

273* 0007*95 0177 1*685

075

OBS

T0166 0208 3*271

27*0 1*60*

STD

0200 0265 3**5

2750 0006056 0211 1*636

075

OBS

0233 0310 3*59*

2757 1*663

STO

0250 0329 3*65

2760 000517* 0239 1*675

STD

0300 0368 3*78

2767 000*627 0263 1*702

STD

0*00 0372 3*78

2766 000*736 0310 1*720

07

5

OB

3

T0*00

03

72

3*

7

83

27

b(

1*7

20

120

31 1540 EV

LA TIT U DC

1/10

LONGITUDE ' "1/10

149 187 l05 lO

DAY HR.U10

8 1094

11965

ORIGINATOR'S

O92I9327

AID TFMP

AIR TtMP. "C

35 S13 152 044 |033 7 12

11042 I n9 I 35 b

Gil Pm SEA

WEA- THER CODt

XI 0 7

0093

SPECIFIC VOLUME

SAO

DYN. M.

11 10^

SOUND VELOCltV

PO<-P wfl ■ ol/l

094

094 094

094

094 094

094

094 094

STD

OBS STD STD

OBS STD

OBS

OBS STD STO STD

OBS STD STD

OBS STD

OBS STD STD

OBS

0000 0000 0010 0020 0026 0030 0041 0050 0061 0072 0075 0100 0125 0144 0150 0200 0215 0250 0283 0300 0400

T0410 0500 0600

T0615 0700 0800

T0820

T0891

0125 0125 0129 0134 0136 0153 0186 0187 0188 0303 0304 0307 0311 0314 0315 03Z2 0324 0349 0356 0368 0375 0376 0378 0381 0381 0378 0375 0374 0374

3367 33666

3371

3376

33805

3385

33936

3395

33958

34401

3440

3442

3444

34448

3447

3460

34635

3470

34755

3477

3482

34823

3484

3486

34862

3487

3488

34884

34885

2698 2698 2701 2705 2708 2711 2715 2716 2717 2743 2743 2744 2745 2745 2747 2757 2759 2762 2765 2766 2759 2759 2770 2772 2772 2773 2774 2774 2774

0010862 0000

0010555 0011 0010205 0021

0009653 0031 0009158 0050

0006568 0005598 0005522

0005318 0005443

0004702 0004490

0004464 0004432

0004419 0004395

0070 0085 0103

0119 0148

0004993 0174

0198 0244

0289 0334

0378 0422

14531 14531 14535 14539 14542 14551 14569 14571 14573 14631 14632 14638 14544 14548 14550 14663 14657 14684 14698 14701 14722 14724 14740 14758 14760 14773 14789 14792 14804

REFERENCE

SHIP CODE

LATITUDE

Via

LONGITUDE

■1/10

^i

MARSDEN

STATION T

ME

ORIGINATOR'S

3EPTH

MA

■

WAVE

WEA- THER CODE

CLOUD

CODES

MODC

CMT COD!

ID. NO.

YEAR

CRUISE

NO.

STATION NUMBER

TO BOTTOM

OF S'MFl-S

OBSERVATIONS

STATION NUMBER

10*

r

MO

DAT H

R.1/10

0I».

HGT P£« if*

IIH AM

31

540

EV

4817

N

04745 W

149

87

35

08 1

13

1965

00?

9328

573

12

ni

6 2

XI

4 2

0094

WATER

WIND

BARO.

METER (mbi)

AIR TEMP, r

VIS- COD

NO. OBS.

DEPTHS

SPECIAL

OBSERVATIONS

COLOR CODE

IRANS,

DIR.

OR

FORCE

DRY BUIB

WET

BULB

34

SIO

156

039 |033

8

10

HR 1/10 T

CARD TYPE

DEPTH (ml

T -C

s v..

SIGMA-T

SMClfiC VOLUME ANOMALT-HO'

SAD

DYN. M. K 10'

SOUND VELOCITY

0 3 ml/1

P04-P

TOTAL-P MB - o'/l

NOj-N ug - oP/l

NO3-N wg • or/I

SI04-S.

JJfl-Ol/l

pH

S

c

STD

0000

0216

3401

2719

0008879

0000

14576

113

OBS

0000 0216 34010 2719 14576

STD

0010 0217 3403 2720 0008777 0009 14578

113

OBS

0010 0217 34025 2720 14578

STD

0020 0232 3415 2729 0007949 0017 14588

STO

0030 0247 3425 2736 0007239 0025 14598

STD

0050 0275 3438 2743 0005588 0039 14615

113

OBS

0062 0294 34395 2743 14525

STD

0075 0247 3437 2745 0006435 0055 14507

113

OBS

0078 0238 34361 2745 14503

STD

0100 0265 3444 2749 0005071 0071 14520

STD

0125 0292 3452 2753 0005718 0085 14637

STD

0150 0316 3450 2757 0005351 0099 14652

STD

0200 0354 3472 2763 0004B51 0125 14578

113

OBS

0207 0358 34730 2764 14681

STO

0250 0360 3475 2755 0004554 0148 14590

STD

0300 0363 3478 2767 0004571 0171 14599

STD

0400 0367 3482 2770 0004409 0215 14718

113

OBS

T0414 0368 34825 2770 14721

STD

0500 0365 3483 2771 0004398 0260 14734

STD

0500 0362 3484 2772 0004374 0304 14749

113

OBS

T0621 0361 34846 2773 14753

STD

0700 0364 3485 2773 0004332 0348 14757

STD

0800 0367 3487 2774 0004382 0391 14785

113

OBS

0828 0368 34872 2774 14790

STD

0900 0366 3488 2775 0004374 0435 14802

STD

1000 0363 3489 2776 0004342 0479 14817

113

OBS

T1055 0361 34899 2777 14826

STD

1100 0359 3490 2777 0004349 0522 14832

STD

1200 0354 3489 2777 0004415 0565 14847

11-

0B£

T1242

03

51

34

8

87

27

77

148

53

121

- SHIP CODE

31 5ft0lEV

LONGITUDE

DA¥ HH.1/10

149 87 105 08 [I'll 1965 002 9329

ORIGINATOR'S

BARO- METER (mbll

AIB TEMP. *C

34 S12 163 039 033 8 09

2158

12

OBSERVATIONS

01

XI 8 n

NODC STATION NUMBER

0095

S104-SI

WB - ol/l

1*1 1*1

141 141

141

STO

OBS STD STD STD STD STD

OBS STD

OBS STD STD STD STD

OBS STD

OBS STD STD

OBS

0000 0000 0010 0020 0030 0050 0075 0081 0100 0104 0125 0150 0200 0250 0261 0300

T0380 0400 0500

T0575 0600 0700 0771 0800 0900

T0988 1000 1100

T1163

0330 0330 0328 0326 0323 0319 0313 0312 0355 0363 0364 0366 0369 0371 0372 0373 0375 0375 0376 0377 0376 0371 0368 0367 0363 0360 0360 0356 0353

3435

34348

3436

3437

3439

3444

3463

34552

3465

34668

3469

3472

3477

3480

34807

3482

34835

3484

3486

34871

3487

3488

34882

3488

3489

34892

3489

34894

2736 2736 2737 2738 2740 2744 2752 2754 2758 2758 2760 2762 2766 2768 2768 2769 2770 2771 2772 2773 2773 2774 2775 2775 2776 2776 2775 2777 2777

0007265

0007162 0007074 0006910 0006508 0005798

0005112 0004922 0004619 0004468

0004342 0004294

0004292 0004280

0004285 0004287

0004307 0004335

0000

0007 0014 0021 0035 0050

0005302 0064

0077 0090 0113 0136

0004379 0158

0202 0245

0288 0331

0374 0417

0459 0503

14530 14630 14531 14632 14633 14635 14638 14539 14651 14666 14670 14675 14685 14695 14597 14704 14718 14722 14739 14752 14755 14770 14781 14785 14800 14814 14816 14831 14840

SHIP CODE

LATITUDE

1/10

LONGITUDE

ORIGINATOR'S

NODC STATION NUMBER

31

540

EV

4818 N

149 |86 I05 IO8 Il67 11965 1002 I 9330

SPEED

OP POPCE

S12

BARO- METEft

(mbl)

1372 I 12 I 85 b

NO. OBS.

DEPTHS

0096

SPECIFIC VOIU

NO3-N PB - 01/1

SIO<-Si

pg • ol/l

157

157 167

167 167

167

157

167

STD

OBS STD STD

OBS STD

OBS STD STD

OBS STD

OBS STD STD STD STD STD

OBS STD

OBS STD STD

OBS

0000 0000 0010 0020 0021 0030 0031 0050 0075 0077 0100 0122 0125 0150 0200 0250 0300 0305 0400

T0407 0500 0600

T0609 0700 0800 0810 0900 1000

T1034 1100 1200

T1217

0250 0250 0237 0224 0223 0252 0255 0252 0248 0248 0293 0330 0331 0338 0352 0365 0381 0382 0366 0355 0371 0377 0377 0372 0367 0365 0360 0355 0354 0352 0349 0349

3395 33964

3397

33966

3414

34151

3424

3435

34367

3451

34634

3464

3468

3475

3480

3483

34831

3484

34838

3486

3488

34884

3489

3490

34902

3490

34902

3490

34904

2712

2712 2714 2715 2715 2726 2728 2734 2744 2745 2752 2759 2759 2762 2766 2768 2769 2769 2771 2771 2773 2774 2774 2775 2775 2776 2777 2778 2778 2778 2778 2778

0009490

0009387 0009284

0007446 0006522

0005169 0004955 0004608 0004417 0004383

0004232 0004238

0004202 0004159

0004149 0004175

0004214 0004251

0000

0009 0019

0008190 0028

0043 0061

0005786 0075

0090 0102 0126 0149 0171

0004261 0214

0256 0299

0341 0383

0424 0466

0508 0550

14590 14590 14585 14582 14582 14599 14600 14603 14607 14508 14633 14654 14655 14663 14678 14693 14708 14709 14718 14719 14737 14756 14758 14771 14786 14787 14799 14814 14819 14829 14845 14848

122

REFtHENCE

SHIP CODE

LONGITUDE ' -1/10

1^

MARSDEN

STATION

TIME

ORIGINATOR'S

DEPTH

MAX.

DEPTH

OF S-MPL'S

WAVE

WEA- THER CODE

CLOUD CODES

NODC STATION NUMBER

CTST

cool

10. NO.

LATITUDE

1/10

YEAR

CRUISt NO.

STATION NUMBER

TO BOTTOM

10*

!•

MO

DAY

HR.l/IO

DlfL

HGT fER S£*

r»Pt AM

31

540

EV

4810 N

04626 W

149

85

35

08

190

1965

00?

9331

1317

11

35

6 3

XI

2 3

WATER

WIND

BARO- METER {mbsl

AIB TEMP, -C

COD

NO.

OBS. DEPTHS

SPECIAL OBSERVATIONS

COLOR CODE

'""'■

DIR.

SPttD fOBCI

DRY BUL8

WET BULe

34

S13 159

044

038

8

10

"'""<=" IcASI ""' "NO. HH 1/tO

CARD TYPE

DEPTH Im)

T -C

s •/..

SIGMA-T

SPECIFIC VOLUME *NOM*H-«IO'

SAD

DYN. M.

X 10'

SOUND VELOCITY

0? ml/1

PO^-P vg -o./l

rOTAL-P ug -o'/l

NOj-N ug.-'l

NO3-N tig - ol/l

5104-Si

.9- o./l "^

S C C

STD

0000

0270 13404

2717

0009076

0000

14600

190 OBS

0000 0270 34040 2717 14600

STD

0010 0239 3405 2720 0008772 0009 14588

STD

0020 0217 3406 2722 0008555 0018 14580

STD

0030 0203 3406 2724 0008393 0026 14576

190 OBS

0047 0201 34076 2725 14578

STD

0050 0204 3410 2727 0008128 0043 14580

190 OBS

00580 0213 34151 2730 14585

STD

0075 0245 3429 2739 0007024 0062 14605

STD

0100 0286 3447 2750 0005026 0078 14629

STD

0125 0319 3462 2759 0005209 0092 14650

190 OBS

0129 0324 34541 2750 14653

STD

0150 0333 3467 2761 0004983 0105 14650

STD

0200 0352 3473 2754 0004756 0129 14678

STD

0250 0355 3478 2767 0004563 0152 14592

190 OBS

0275 0371 34798 2768 14599

STD

0300 0373 3481 2768 0004454 0175 14704

190 OBS

T0367 0378 34846 2771 14718

STD

0400 0378 3486 2772 0004223 0218 14723

STD

0500 0375 3488 2774 0004142 0260 14739

190 OBS

T0549 0375 34892 2775 14747

STD

0500 0373 3489 2775 0004102 0301 14755

STD

0700 0359 3489 2776 0004139 0342 14770

190 OBS

0731 0368 34894 2776 14774

STD

0800 0367 3490 2776 0004196 0384 14786

STD

0900 0363 3490 2775 0004221 0426 14801

190 OBS

T0935 0361 34898 2777 14805

STD

1000 0356 3490 2777 0004201 0468 14814

STD

1100 0347 3490 2778 0004177 0510 14827

190

OBS

T1102

0347

34901

277e

14828

REFEftENCE

SHIP

CODE

LATITUDE

l/IO

LONGITUDE

'1/10

= 0

MARSDEN

STATION T

ME

ORIGINATOR'S

DEPTH

MAX

;

WAVE

WEA- THER CODE

CLOUD COOES

JODC

CIRY

CODE

ID.

NO.

YEAR

CRUISE NO.

STATION NUMBER

TO BOTTOM

OF S'MPL-S

STATION NUMBER

- 10-

r

MO

DAY H

R.I/10

OIR.

MGI PER 5E*

TIP! *w

31

540

EV

I

i759

N

04600 W

149

75

»

Ofl 2

16

1965 002

9332

914

08

33

3 2

X6

3 8

0098

WATER

WIND

BABO- METER Imbl)

AtR IEMP. -C

VIS. COD

NO.

OBS. DEPTHS

SPECIAL OBSERVATIONS

COLOR CODE

TRANS.

OIR.

SPEED

OR FORCE

DRY BULB

WET

BULB

32

S20

159

044

039

7

07

MESSENGR

TIME c HR 1/10

CAST NO.

CARD TYPE

DEPTH Iml

T -C

s •/„

S(GMA-T

SPICIfIC VOLUME ANOMALif-«IO'

SAO

DYN. M,

X 103

SOUND VELOCITY

Ol ml/I

PO<-P vg - or/i

TOTAL-P Ut ■ ol/l

N03-N

Pfl - ar/l

NOj-N PB - ot/l

SIO<-Si

wg - oi/l

pH

S C

c

STD

0000

0381

3426

2724

0008423

0000

14651

215

OBS

STD

0000 0381 34257 2724 14551 0010 0380 3425 2723 0008453 0008 14552

216

OBS

0011 0380 34253 2723 14652

215

OBS STD STD STD STD STD STD STD

0019 0379 34254 2724 14553

0020 0379 3426 2724 0008399 0017 14653 0030 0380 3431 2728 0008043 0025 14656 0050 0383 3441 2736 0007330 0040 14562 0075 0386 3452 2744 0006554 0058 14668 0100 0388 3462 2752 0005854 0073 14675 0125 0391 3470 2758 0005305 0087 14581 0150 0394 3478 2754 0004756 0100 14588

216

OBS STD STD STD

0165 0396 34818 2757 14592 0200 0391 3483 2758 0004397 0123 14595 0250 0384 3485 2771 0004222 0144 14701 0300 0378 3485 2772 0004131 0155 14707

216

OBS STD STD

T0383 0370 34878 2774 14717 0400 0370 3488 2774 0003989 0206 14720 0500 0366 3488 2775 0004035 0246 14735

215

OBS STD STD

0583 0352 34886 2775 14747 0500 0351 3489 2775 0003994 0285 14750 0700 0355 3489 2777 0004013 0326 14754

21

3

OB

3

0773

0:

49

34

8

91

27

7-

147

73

123

REFEHtNCE

SHIP CODE

LATITUDE

l/IO

LONGITUDE

■1/10

°i

MARSDEN

STATION T

ME

ORIGINATOR'S

DEPTH

MAX.

WAVE

WEA- THER CODE

CLOUD CODES

NODC

CUT CODE

ID.

NO.

CRUISE NO.

STATION

NUMBER

TO BOTTOM

OF S-MPL*S

STATION NUMBER

10'

1*

MO

DAY H

R.1/10

Dl«.

HGl PER iEA

ITP( AM

31

540

EV

1

t740

N

04600 W

149

76

D5

09 004

1965

002

9333 D570

06

30

5 2

X?

8 8

0099

WATtR

WIND

BARO- METER (mb*)

AIR TEMP. "C

--D^P^^HS

SPECIAL OBSERVATIONS

COLOR CODE

'"":'■

D1R.

into

FORCE

DRY eULB

WET BULB

34

S12

152

039

028

8

06

MtSSENGR

TIME a

HR I/IO'

CAST

NO.

CARD TYPE

DEPTH (ml

I -c

s •/..

SIGMA-T

i^ClflC VOLUME

anomal'-iid'

SAD

DYN. M.

X 10^

SOUND VELOCITY

Ol m1/l

PO4-P

lOTAL-P UB ■ ol/l

NOi-N US - 01/1

NOj-N VB - ot/l

SI 04-Si Wfl - ot/l

pH

S

c c

STD

0000 1 0344

3429

2730

0007844

0000

14635

004

OBS STD STD STD STD

0000 0344 34288 2730 14635 0010 0339 3429 2730 0007789 0008 14635 0020 0334 3429 2731 0007734 0016 14634 0030 0328 3429 2732 0007680 0023 14634 0050 0318 3430 2733 0007571 0039 14633

004

OBS STD

0052 0317 34298 2733 14632 0075 0332 3442 2741 0006797 0056 14644

004

OBS STD STD STD STD STD STD

0098 0346 34535 2749 14656 0100 0346 3454 2750 0006046 0073 14656 0125 0350 3460 2754 0005655 0087 14663 0150 0355 3465 2758 0005340 0101 14669 0200 0363 3475 2765 0004713 0126 14682 0250 0371 3482 2769 0004314 0149 14695 0300 0379 3486 2772 0004144 0170 14707

004

OBS STD

T0323 0383 34879 2773 14713 0400 0371 3489 2775 0003925 0210 14721

004

OBS STD

T0414 0370 34894 2775 14723 0500 0368 3489 2776 0003949 0249 14736

004

OBS

T0560

0366

34893

2776

14745

SHIP CODE

LATITUDE

1/10

ORIGINATOR'S

hciiperT sea

WEA- THER CODE

NODC STATION NUMBER

31

540

EV

4738 N

04615 W

149 176 105 109 021 11965 100219334

02

BARO- METER

AIR TEMP. *C

033

3410 I 04 I 32 5

06

X2 8 IB

OlOO

DEPTH I

SPEClfiC VOLUME

NO3-N

021

021 021

021 021 021

STD

OBS STD STD STD STD STD

OBS STD

OBS STD STD STO

OBS STO

OBS STD

OBS

0000 0000 0010 0020 0030 0050 0075 0088 0100 0122 0125 0150 0200

T0222 0250

T0273 0300

T0387

0377 0377 0378 0378 0379 0380 0381 0382 0368 0349 0352 0369 0387 0388 0378 0372 0373 0374

3435

34354

3439

3443

3446

3451

3455

34563

3456

34557

3457

3465

3477

34801

3481

34819

3483

34859

2732 2732 2735 2738 2740 2744 2747 2748 2749 2751 2751 2756 2764 2766 2768 2769 2770 2772

0007654

0007398 0007110 0006899 0005551 0006287

0005895 0005481 0004805

0004460

0004299

0000

0008 0015 0022 0035 0051

0006104 0057

0082 0096 0122

0145

0167

14650 14650 14553 14655 14657 14662 14657 14670 14666 14661 14653 14575 14693 14697 14598 14699 14704 14720

124

31 S^tO EV

LATITUDE

t/10

0'f63't W

1A9 176 105

9 fc)63 ll?6'5 100719335

ORIGINATOR'S

BARO- METER Imbtl

31 S14 149 028 017 8

112.

JJ.

JIZ.

WEA- THER CODE ■

X2 6 '8

OlOl

SOUND VELOCITY

SIO*-Si

063 063

063

063 063

STD

OBS STD

OBS STD STD

OBS STD

OBS STD STD STD STD STD

OBS STD STD

OBS STD

OBS

0000 0000 0010 0014 0020 0030 0042 0050 0065 0075 0100 0125 0150 0200 0223 0250 0300 T0366 0400 0500 0551 0600 0700 0746 0800 0900 0961 1000 1085

0283 0283 0330 0341 0322 0302 0296 0312 0339 0343 0351 0358 0365 0373 0376 0374 0372 0370 0371 0374 0376 0374 0370 0368 0365 0359 0356 0354 0350

3408

34080

3423

34273

3428

3430

34323

3438

34479

3451

3458

3464

3469

3477

34799

3481

3482

34834

3484

3487

34880

3488

3489

34896

3490

34903

3490

34903

I 2719 2719 2727 2729 2732 2735 2737 2740 2745 2748 2752 2756 2760 2765 2767 2768 2769 2771 2771 2773 2774 2774 2775 2776 2776 2777 2778 2778 2778

0008881 0008162

0007691 0007386

0006221 0005790 0005427 0005141 0004664

0004419 0004369

0004299 0004199

0004180 0004165

0004136 0004152

0000 0009

0016 0024

0006899 0038

0055 0070 0084 0097 0121

0144 0166

0209 0252

0294 0336

0377 04 19

0004155 0460

14606 14606 14630 14636 14629 14622 14622 14631 14646 14650 14659 14667 14674 14687 14692 14696 14704 14714 14720 14738 14748 14755 14770 14777 14785 14799 14808 14814 14826

SHIP CODE

LATITUDE

1/10

ORIGINATOR'S

149 176 105

9 1079 11965 1002 1 9336

IPiED

OR FO«CE

AIR TEMP. "C

022

1161 I 11 I 31 B

0102

AESSENCR

TIME HH 1/10

SPECIFIC VOIU

079

079 079 079 079 079 079

079 079

STD

OBS STD STD

OBS STD

OBS STD STD STD STD

OBS STD STD

OBS STD

OBS

0000 0000 0010 0020 0029 0030 0048 0050 0070 0075 0083 0100 0102 0125 0148 0150 0200 0250 0300

T0373 0400 0500

T0559 0600 0700 0758 0800 0900

T0977 1000

T1065

0194 0194 0191 0187 0184 0185 0204 0224 0319 0303 0281 0253 0252 0295 0332 0333 0346 0358 0367 0376 0376 0376 0376 0375 0371 0368 0365 0359 0356 0355 0354

3376

33760

3379

3382

33843

3385

34062

3411

34379

3437

34353

3437

34378

3455

34712

3471

3474

3475

3479

34827

3483

3486

34858

3487

3488

34886

3489

34891

3489

34893

2701 2701 2703 2706 2708 2708 2724 2726 2739 2740 2742 2745 2745 2756 2755 2755 2755 2755 2767 2770 2770 2772 2773 2773 2774 2775 2776 2775 2777 2777 2777

0010371 0010137

0009876

0008205

0006912

0005499

0005444

0004650 0004630 0004603 0004542

0004425 0004291

0004295 0004255

0004210 0004226

0000

0010 0021

0031

0049

0068

0084

0099

0112 0135 0158 0181

0225 0270

0313 0355

0398 0440

0004248 0482

14563 14563 14564 14564 14565 14565 14579 14589 14637 14631 14623 14614 14614 14639 14660 14661 14675 14589 14701 14718 14722 14739 14749 14755 14770 14779 14785 14799 14810 14814 14824

125

SHIP

CODE

EV

LATITUDE

I/IO

LONGITUDE * '1/10

1^-9 l7 6 l05

9 b94 Il965 IOO2I 9337

31 S08

ORIGINATOR'S

017

Oil

[1097,1 Q9 1 32

DIB, MGl] PER 5EA

WEA- THER CODE

0103

SfECIfIC VOLL

SOUND VELOCITY

094 094

STO

OBS STD STD STD

OBS STD STD STD STO STD STD

OBS STD STD

OBS STD

OBS

0000 0000 0010 0020 0030 0039 0050 0075 0100 0125 0150 0200 0200 0250 0300

T0378 0400 0500 0561 0600 0700 0731 0800

T0852 0860

0139 0139 0138 0136 0135 0134 0152 0190 0225 0256 0284 0329 0329 0346 0360 0376 0378 0383 0384 0382 0378 0376 0372 0369 0362

3357

33566

3360

3364

3368

33719

3380

3398

3415

3429

3442

3463

34629

3469

3474

34799

3481

3485

34864

3487

3488

34881

3489

34889

34887

2689 2689 2692

2695 2698 2702 2707 2718 2729 2738 2746 2758 2758 2762 2764 2767 2768 2771 2772 2772 2774 2774 2775 2775 2776

0011711

0011446 0011135 0010825

0010030 0008942 0007933 0007142 0006417 0005293

0005039 0004846

0004596 0004442

0004373 0004344

0000

0012 0023 0034

0055 0078 0100 0118 0135 0165

0190 0215

0262 0308

0352 0395

0004319 0438

14536 14536 14537 14539 14541 14542 14553 14577 14598 14618 14636 14666 14666 14683 14698 14718 14723 14742 14753 14758 14773 14778 14788 14795 14793

REFERENCE

SHIP CODE

LATITUDE

1/10

LONGITUDE

■1/10

°i

MARSDEN

STATION Tl

^^E

ORIGINATOR'S

DEPTH

MAX

.

WAVE

WEA- THER CODE

CLOUD CODES

MODC

CIRt

10.

NO.

YEAR

CRUISE NO.

STATION NUMBER

TO

BOTTOM

OF S'wPL'S

STATION NUMBER

CODE

10*

1"

MO DAY [H

.1/10

Ot»-

HGI PER iEA

TTFE AM

31

540

EV

4729 N

04715 W

149

77

35

09 |ll3

1965

00?

9338

3649

05

31

3 3

X7

6 6

0104

WATER

WIND

BARO- METER (mbsl

AIR TEMP. "C

VIS.

coo

t NO.

OflS. DEPTHS

SPECIAL OBSERVATIONS

COLOR CODE

TR*NS.

DIR.

SPEED

OR EORCE

DRY BULB

WEI BULB

31

SIO

161

039

022

7 |07

MESSENGR

TlwE 0 HR 1/10

CAST

NO.

CARD TYPE

DEPTH (ml

T -C

s •/..

SIGMA— T

SPECIEIC VOLUME

ANOMALT-IIO'

SAD

DYN, M.

X 10^

SOUND VELOCITY

Ol ml/1

P04-P

^9 -ol/l

lOTAl-P

vg • 01/1

NO;-N U9-..I/I

NO3-N pg - oi/l

SIO«-Si

h.g - al/\

pH

S

c

STD

0000

0062

3345

2685

0012123

0000

14500

113

OBS STD

0000 0062 33452 0010 0057 3345

2685 14500 2685 0012118 0012 14499

113

OBS STD STD

0018 0053 33447 0020 0058 3346 0030 0079 3351

2685 14499

2686 0012039 0024 14501 2688 0011774 0036 14513

113

OBS STD STD STD STD STD

0044 0108 33590 0050 0114 3363 0075 0141 3381 0100 0167 3397 0125 0194 3412 0150 0221 3425

2693 14530 2696 0011072 0059 14534 2708 0009885 0085 14553 2719 0008858 0109 14570 2729 0007931 0130 14589 2738 0007169 0148 14606

113

OBS

STD STD

0185 0258 34409 0200 0278 3447 0250 0331 3463

2747 14630 2750 0006019 0181 14642 2758 0005343 0210 14676

113

OBS STD

T0261 0340 34659 0300 0355 3470

2760 14682 2762 0005095 0236 14695

113

OBS STD STD

0353 0370 34755 0400 0372 3479 0500 0375 3484

2764 14711 2767 0004677 0285 14720 2771 0004427 0330 14738

11

3

OB

3

T0540

0:

76

34

8

47

27

71

147

46

126

REFERENCE

SHIP CODE

LATITUDE

1/10

LONGITUDE ' "1/10

MARSDEN

STAT

ON T

ME

ORIGINATOR'S |

DEPTH TO

MAX DEPTH

OF S-MPL

WAVE

WEA- THER CODE

CLOUD COOES

•40DC

CIIY

ID.

NO.

YEAR

CRUISE NO.

STATION

STATION NUMBER

10-

r

MO

DAY M

R.1/10

NUMBER uw^-m

S on.

MGt PER SE*

IVfE AM

31

•i^O

EV

4

725

N

04726 W

149

77

D5

09 129

1955

002

9339 3293

03

_ 3 0

3 2

X?

7 8

nln5

WATER

WIND

BARO- METER In^bil

AIR TEMP. "C

VIS.

coot

NO. OBS.

DEPTHS

SPECIAL OBSERVATIONS

COLOR CODE

TRANS.

DIR.

SPEIO

OB FO«Cf

DRY BULB

WET BULB

30

S15

169

044

028

8

08

MESSENOR

TIME 0 HR 1/10 ]

CAST NO.

CARD TYPE

DEPTH Iml

T -C

s ••'..

SIGMA-T

SPECIFIC VOLUME ANOMAir-IlO'

SAD DYN. M

SOUND VELOCITY

03 ml/I

PO4-P

TOTAl_P j>B- al/1

NO;-N

ug - ot/1

NO3-N vg - oi/l

SI04-Si

Dg - oi/l

pH

S

c

STD

0000 1-0014

3295

2548

0015587

0000

14458

129

OBS STD STD STD

0000 -0014 32950 2648 0010 -0015 3295 2548 0020 -0016 3295 2549 0030 -0017 3296 2649

14458 0015555 0016 14459 0015542 0031 14451 0015511 0047 14452

129

OBS

STD

0032 -0017 32957 2549 0050 -0027 3304 2555

14462 0014827 0077 14462

129

OBS

0063 -0034 33108 2562

14461

129

OBS STD

0072 -OHO 33165 2669 0075 -0089 3320 2671

14428 0013352 0112 14439

129

OBS STD STD STD

0088 -0011 33338 2579 0100 -0002 3339 2583 0125 0023 3352 2592 0150 0055 3365 2702

14479 0012253 0144 14486 0011383 0174 14504 0010492 0201 14524

129

OBS STD STD

0151 0055 33664 2702 0200 0203 3419 2734 0250 0274 3445 2750

14525 0007501 0246 14606 0006090 0280 14649

129

OBS

T0260 0278 34481 2751

14652

129

OBS

0278 0278 34489 2752

14655

REFERENCE

SHIP CODE

LATITU

DE 1/10

LON

GITUDE '1/10

li

MARSDEN SQUARE

STATION TIME IGMTl

YEAR

ORIGINATOR'S |

DEPTH

TO OTTOM

MAX. DEPTH

OF S-MPL-

WAVE

OBSERVATIONS

WEA- THER CODE

CLOUD CODES

NQDC STATION NUMBER

CI»Y

CODE

ID.

NO.

CRUISE NO.

STATION NUMBER

10-

1*

MO

DAY M

R.l/10

DIR.

HGT PER ;e*

lyn AMI

31

540

EV

4

725

N

04742 W

149

77 (

)5

09 1

45

1955

00?

9340 3243

02

32

2 I2 XO

0

Qln6

WATER

WIND

BARO. METER (mbtl

AIR TEMP. *C

VIS, COD!

NO. OBS. DEPTHS

SPECIAL OBSERVATIONS

COLOR CODE

'tv-

DIR.

SPEED

OR FORCE

DRV BULB

WET BULB

30

S08

175

039

033

8

06

MESSENGR 1 TIME 01 HR 1/10

CAST NO.

CARD TYPE

DEPTH Iml

T -C

s ■''..

SIGMA-T

SPECIFIC VOLUME ANOMALY-KlO'

SAD OYN. M.

X 10'

SOUND VELOCITY

Ol ml/1

P04-P

TOTAL-P

N03-N

ug - ol/i

NO3-N \,g ■ a\/\

SlOj-S. vg -ol/l

pH

STD

0000

-0036

3288

2644

0016025

0000

14447

145

OBS STD STD STD

0000 -0036 32881 2544 0010 -0052 3289 2645 0020 -0056 3289 2545 0030 -0078 3290 2647

14447 0015914 0016 14441 0015819 0032 14436 0015726 0048 14433

145

OBS STD

0030 -0078 32898 2647 0050 -0097 3300 2555

14433 0014871 0078 14429

145

OBS STD

0060 -0106 33057 2650 0075 -0088 3315 2557

14427 0013746 0114 14439

145

OBS STD STD STD

0075 -0088 33149 2557 0100 -0009 3340 2584 0125 0054 3361 2598 0150 0100 3377 2708

14439 0012143 0146 14483 0010868 0175 14519 0009930 0201 14546

145

OBS STD

0190 0140 33916 2717 0200 0141 3393 2718

14573 0008999 0248 14575

14

5

ob;

>

0220

01

42

33

9

47

27

1<:

14579

REFERENCE	SHIP CODE	LATITUDE 1/10	LONGITUDE ■1/10	li	MARSDEN	STATION	TIME			ORIGINATOR'S	DEPTH	MA«	.		WAVE		WEA- THER CODE	CLOUD CODES				MODC
CTRT	ID. NO.			YEAH	cruise! STAT	ON BER	TO BOTTOM	OF S'MPL'S	OBSERVATIONS		STATION NUMBER
CODE	to- ! r	MO	DAY	HR.1/10			OIR.	HGI PER S(A	TYPE AM
31	540	EV	4	724	N	04757 W		149	177 1	35	09	159	1965	002	9341	3201	02	31	2 2	XO	0		0107
				WATER	WIND	BAHC METE Imbl	- R	AIR TEMP.	•c	VIS, COD	NO. OBS. DEPTHS	SPECIAL OBSERVATIONS
	COLOR CODE	TRANS, Iml	DIR.	SPEED FORCE	DRY BULB	WET BULB
			29	S09	169	039	028	8	09
	MESSENGR [ HR 1/10	CAST NO.	CARD TYPE	DEPTH Iml	T -C	S •''..	SIGMA— T	SPtCIFIC VOLUME ANOMALY-XlO'	SAD DYN. M. X loJ	SOUND VELOCITY	Oj m1/l	PO4-P	TOTAl_p vg . ol/l	N03-N ug - ol/l	NO3-N vg - ol/l	SIO4-SJ UB - ol/l	pH	S c c
			STD	0000	0008 [3290	2643	0016089	0000	14467
	159		OBS	0000 0008 32897 2643		14467
			STD	0010 -0009 3293 2646	0015758	0015 14462
			STD	0020 -0020 3296 2549	0015478	0032 14459
			STD	0030 -0027 3301 2554	0015053	0047 14458
	159		OBS	0045 -0029 33104 2661		14451
			STD	0050 -0027 3315 2665	0013988	0076 14463
	159		OBS	0055 -0024 33177 2557		14456
	159		OBS	0070 -0095 33215 2673		14435
			STD	0075 -0084 3325 2675	0012987	Olio 14442
	159		OBS	0090 -0039 33358 2682		14467
			STD	0100 0000 3342 2685	0012057	0141 14487
	159		OBS	0100 0000 33417 2585		14487
	159		OBS	0110 0025 33456 2688		14501
			STD	0125 0045 3350 2589	0011659	0171 14514
			STD	0150 0055 3360 2595	0011014	0199 14528
	159		OBS	0150 0065 33599 2695		14528
		15	9		OB	3	T0175		0(	)66	33	7	32		27	0-	7							145	34

127

REFERENCE

SHIP CODE

LATITUDE

l/IO

li

MARSDEN

STATION

Tl

WE

ORIGINATOR'S

DEPTH

MAX

-

WAVE

WEA- THER CODE

CLOUD COOES

NOOC

crsv

CODE

ID. NO.

' '1/10

CRUISE

NO,

STATION NUMBER

BOTTOM

OF S-MPL'S

STATION NUMBER

n-

r

MO

DAY

HR,1/10

DtR.

HGT fl« SEA

TYfl AM

31

•J40

EV

4722

N

04812 W

149

78

35

09

171

1965

002

9342 D174

02

30

2 2

xo

0

0108

WATER 1 WIND

BARD.

METER Imbtl

AIR TEMP. "C

DEPTHS

SPECIAL OBSERVATIONS

COLOR CODE

I«ANS. o|R_

SPEtO

OB FOUCf

DRY eULB

WET BULB

27

S08

179

033

022

8

04

HR 1/10 1

CARD TYPE

DEPTH (m)

I -c

s •/..

SIGMA-T

SPECIFIC VOLUME ANOMAL'-HIO'

SAD

DYN. M.

X I03

SOUND VEIOCITY

Oj ml/1

POi-P

lOTAL-P ug - oi/l

N03-N

ug - or/I

NOj-N

PB- Ql/I

SI04-SI pg-ol/l

PH

1

STD

0000

-0011

3283

2638

0016533

0000

14458

171

OBS 0000 -0011 32828 2538 14458 STD 0010 -0043 3284 2641 0016308 0015 14445 STD 0020 -0059 3285 2543 0016107 0033 14434 STD 0030 -0089 3287 2544 0015942 0049 14427 STD 0050 -0112 3289 2547 0015666 0080 14420

171

OBS 0055 -0115 32909 2549 14421 STD 0075 -0090 3304 2658 0014573 0118 14436 STD 0100 -0034 3331 2678 0012716 0152 14470 STD 0125 0014 3351 2592 0011413 0182 14499

171

OBS 0130 0023 33545 2694 14505 STD 0150 0055 3355 2701 0010568 0210 14524

171

OBS

0150

0069

33688

2703

14533

REFERENCE

SHIP CODE

LATITUDE

1/10

LONGITUDE

"1/10

Si

MARSDEN

STATION

Tl

WE

ORIGINATOR'S

DEPTH

MAX.

WAVE

WEA- THER

CODE

CLOUD CODES

NOOC

CIRY CODE

ID. NO.

YEAR

CRUISE NO.

STATION NUMBER

TO BOTTOM

OF S'MPL'S

STATION NUMBER

10'

r

MO

DAY

HR.1/10

DIK-

MGTl Pt» SEA

HPI AM

31

540

EV

i

.701

N

04801 W

149

78

15

09

20?

1965_

00?

9343 n50__

01

74

A

X4

X 9

0109

WATER

WIND

BARO- METER

AIR lEMP. "C

Vt5, coo

NO.

OBS. DEPTHS

SPECIAL OBSERVATIONS

COLOR CODE

TRANS.

OIR.

I»E(0

OS FOIICE

DRY BULB

WET SULB

25

S09

169

000 ■

006

1

06

MESSENGR

TII^^E z

HR l/IO

CAST NO.

CARD TYPE

DEPTH (ml

I -c

s ■/..

SIGMA-T

SPECIFIC VOLUME ANOMALY-XIO'

SAD DYN. M.

SOUND VELOCITY

Ol m(/l

POi-P

HB-o'/l

lOTAl-P

vi ■ oi/i

NOi-N wg . ot/l

NO3-N vg - o./l

SI04-Si

KS - Ol/I

pH

STO

0000

3284

2638

0016504

0000

14463

202

OBS STD

0000 0000 32838 2638 14453 0010 -0005 3284 2539 0015471 0016 14462

202

OBS STD STD

0012 -0007 32839 2639 14462 0020 -0021 3284 2540 0016392 0033 14457 0030 -0037 3284 2640 0016315 0049 14451

202

OBS

STD

0030 -0037 32841 2640 14451 0050 -0077 3293 2649 0015474 0081 14437

202

OBS STD

0072 -0089 33088 2562 14437 0075 -0086 3312 2665 0013976 0118 14440

202

OBS STD STD

0097 -0051 33344 2682 14458 0100 -0053 3338 2684 0012101 0150 14462 0125 0053 3364 2700 0010634 0179 14519

20

>

OB

3

0127

oc

65

33

5

58

27

0

14525

REFERENCE

SHIP CODE

LATITUDE

1/10

°z

MARSDEN

STATION T

ME

ORIGINATOR'S

DEPTH

MAX.

DEPTH

OF S'MPL'S

WAVE

WEA- THER CODE

CLOUD CODES

NODC

cmr CODE

10.

NO.

LONGITUDE

■1/10

YEAR

CRUISE NO.

STATION

NUMBER

TO

BOTTOM

STATION NUMBER

10-

r

MO

DAY y

l.l/lO

DI(L

HCI fE« SEA

Jin AM

31

540

EV

4659

N

04738 W

149

67

35

09 2

18

1965

00?

9344

M75

02

?5

3 4

X4

X 9

0110

WATER

WIND

BARO- METER Imbtl

AIR TEMP. -C

VIS, COD

NO.

OBS.

DEPTHS

SPECIAL OBSERVATIONS

COLOR CODE

TRANS.

D1R.

SPEED

01 fO'Ct

DRY BULB

WET BULB

25

SIO

159

Oil

006

1

04

HR I/IO

CARD TYPE

DEPTH Iml

T "C

s •/..

SlGMA-T

SPfCIFIC VOLUME *NOMAL<->IO'

SAD

DYN. M.

X 10^

SOUND VELOCITY

Ol ml/1

PO*-P

vg - ol/l

rOTAL-f ug - Ql/I

NO7-N

ug - al/l

NO3-N lig-ol/l

SIO4-S.

yg-ol/l

pH

STO

0000

-0023

3288

2643

0016062

0000

14453

218

OBS 0000 -0023 32883 2643 14453 STD 0010 -0034 3291 2646 0015798 0016 14450 STD 0020 -0045 3294 2649 0015543 0032 14447 STD 0030 -0057 3297 2551 0015282 0047 14443 STD 0050 -0079 3302 2556 0014759 0077 14437 STD 0075 -0108 3309 2653 0014132 0113 14429

218

OBS 0078 -0111 33098 2564 14428

218

OBS 0087 -0051 33255 2675 14460 STD 0100 -0027 3335 2681 0012428 0146 14474 STD 0125 0020 3352 2592 0011375 0176 14502 STD 0150 0067 3369 2703 0010362 0203 14530

21

3

OB

3

T0169

01

02

33

8

13

27

1

145

51

128

REFfRENCE

SHIP CODE

LATITUDE

1/10

LONGITUDE ' '1/10

H

MARSDEN

STATION

Tl

wt

ORIGINATOR'S

DEPTH

MAX.

WAVE

WEA- THER CODE

CLOUD CODES

NODC

[;nr

ID. NO.

CRUISE NO.

STATION NUMBER

BOTTOM

OF S'MPL'S

STATION NUMBER

001

10*

!■

MO

DAV

HR.VIO

DIR.

HGI PER i£A

TYPE AM

31

540

EV

/

.700

N

04730 W

149

77 05

09

P37

1963

00?

9345 52iO_

02

70

2 2

X4

X 9

0111

WATER

WIND

BARO- METER

(mbil

AIR TEMP. X

coo

NO.

OBS.

DEPTHS

SPECIAL OBSERVATIONS

COLOR

coot

'T^

DIR.

S«EO

0« (OtCt

DRY BULB

WET BULB

24

508

152

■005 008

1

07

MtSSENCR

TIME « HR 1/10 '

CAST NO.

CARD

TYPE

DEPTH 1ml

T -C

s •/..

S1GMA-T

SPECIFIC VOLUME ANOMALT-XIO'

SAO

DYN. M.

R 10'

SOUND VELOCITY

Ol ml/I

PO4-P

VB - al/l

lOYAl-P

vB - oi/l

NOj-N UB - al/i

NO,-N HB - Ql/I

SIO4-S1

UB - Ql/I

pH

S C C

STD

0000

-0035

3287

2643

0016106

0000 1 14447

237

CBS STD

0000 -0035 32871 2543 14447 0010 -0038 3287 2643 0016097 0015 14447

237

DBS STD

0010 -0038 32870 2643 14447 0020 -0084 3288 2545 0015880 0032 14428

237

OBS STD STD

0021 -0088 32877 2645 14425 0030 -0086 3291 2648 0015606 0048 14429 0050 -0083 3299 2654 0014995 0078 14435

237

OBS STD STD

0053 -0080 33057 2659 14439 0075 -0049 3314 2665 0013961 0115 14457 0100 0008 3329 2674 0013064 0148 14489

237

OBS STO

0105 0018 33315 2576 14495 0125 0052 3340 2681 0012453 0180 14515

237

OBS STO STD

0131 0052 33435 2583 14521 0150 0092 3355 2591 0011549 0210 14539 0200 0158 3398 2721 0008745 0251 14583

237

OBS

0210

0170

34088

2729

14592

EFERENCE

SHIP CODE

LATITUDE

1/10

LONGITUDE * "1/10

if

MARSDEN

STATION T

ME

ORIGINATOR'S

DEPTH

MAX. DEPTH

OF S-MPL'S

WAVE

WtA-

THER CODE

CLOUD COOES

^ODC

11'

ID.

NO.

CRUISE NO.

STATION

NUMBER

TO BOTTOM

STATION NUMBER

JUl

10*

r

MO

DAY H

R.1/10

Oil.

HCI rtt SEA

iin AM

Jl

540

EV

i

t700

N

04716 W

149

77

D-i

10 0

19

1965

002

9346

710

05

23

3 2

X4

X 9

0112

WATER

WIND

BARD-

METER

(mbi)

AIR TEMP. X.

VIS. COD

NO.

OBS. DEPTHS

SPECIAL OBSERVATIONS

COLOR CODE

ikam;

DIR.

OR FORCE

DRY BULB

WET BULB

20

S14

146

-006

■006

1

09

MESSENCI

TIME 0 HR 1/10'

CAST NO.

CARD TYPE

DEPTH Iml

T -C

s •/..

SIGMA-T

SPECIFIC VOLUME AN0MAL1-I1D'

SAD

DYN. M. K 10^

SOUND VELOCITY

Ol ml/l

Vfl - ol/l

roTAL-r vfl • m/i

NOl-N

WS - Ol/l

N03-N

wa- ol/l

SIO^-Si US - ot/l

pH

S

C

c

STD

0000

00 76

3320

2664

0014096

0000

14503

019

OBS

0000 0076 33203 2664 14503

019

OBS STD STD

0009 0060 33205 2665 14497

0010 0052 3321 2665 0013913 0014 14493 0020 -0017 3325 2672 0013275 0028 14464

019

OBS STO STD STD

0022 -0028 33258 2574 14459 0030 -0020 3332 2678 0012724 0041 14465 0050 0003 3345 2588 0011755 0065 14481 0075 0041 3363 2700 0010548 0093 14505

019

OBS STD STD

0080 0050 33651 2702 14510 0100 0097 3376 2707 0009984 0119 14535 0125 0148 3391 2715 0009185 0143 14565

019

OBS

STD

0126 0150 33915 2715 14566 0150 0185 3409 2728 0008098 0164 1*588

019

OBS STD STD

0174 0220 34246 2737 14510 0200 0257 3440 2745 0006450 0201 14537 0250 0334 3452 2757 0005447 0231 14577

019

OBS STD

0258 0342 34547 2759 14682 0300 0354 3470 2762 0005085 0257 14695

019

OBS STD

STD

0375 0371 34766 2755 14715 0400 0375 3478 2766 0004789 0305 14721 0500 0382 3484 2770 0004505 0353 14741

01

9

OB

5

0519

0:

82

34

8

43

27

7C

)

147

44

129

SHIP CODE

LATITUDE

l/IO

04700 W

ORIGINATOR'S

149 77 05 10 337 Il965 |002 I 9347

|22

SU

BARO- METER Imbi)

AIR TEMP. 'C

005

11

262 I 12 I 23 B

HGIIPERl SEA

0113

SPICIfIC VOLUME

SOUND VELOCITY

rOIAL-P

vg - oi/l

SI 0*-Si

037 037

037

STO OBS

ST3

OBS STD STD STD

OBS STD

OBS STD STD

OBS STD

OBS STD STD

OBS STD STO

OBS

0000 0000 0010 0015 0020 0030 0050 0073 0075 0100 0125 0145 0150 0159 0200 0250 0257 0300

T0389 0400 0500

T0585 0500 0700 0782 0800 0900

T0993 1000 1100 1166

0224 0224 0270 0289 0289 0289 0289 0289 0293 0332 0352 0354 0351 0341 0353 0368 0371 0373 0375 0375 0373 0371 0370 0356 0352 0351 0357 0354 0354 0352 0352

3381

33808

3399

34069

3407

3408

3411

34183

3420

344 3

3457

34638

3454

34551

3471

3478

34803

3481

34843

3485

3488

34897

3490

34895

3490

34898

3490

34894

2702 2702 2713 2717 2716 2718 2721 2727 2728 2742 2751 2757 2757 2759 2752 2767 2758 2758 2771 2771 2774 2776 2776 2776 2776 2775 2777 2777 2777 2777 2777

0010469

0009459

0009019 0008949 0008735

0008106 0005740 0005895

0004915 0004583

0004256 0004110

0004040 0004090

0004128 0004152

0004192 0004255

0000

0010

0019 0028 0046

0057 0085 0101

0005380 0115

0141 0165

0004454 0187

0231 0273

0314 0354

0395 0437

0479 0521

14577 14577 14601 14611 14612 14614 14617 14622 14625 14649 14653 14668 14668 14667 14678 14693 146 98 14704 14720 14722 14738 14752 14754 14769 14780 14783 14798 14812 14813 14829 14840

REEERENCE

SHIP CODE

LATITUDE

1/10

LONGITUDE ■ M/IO

i|

MARSDEN

STATION T

Mf

ORIGINATOR'S

DEPTH

MAX.

DEPTH

OF S'MPl'S

WAVE

WEA- THER

CODE

CLOUD

CODES

^ODC

CTRT

coot

ID. NO.

CRUISE NO.

STATION NUMBER

TO

BOTTOM

STATION NUMBER

10-

r

MO

DAY H

R.1/10

Ol«.

HGI fER if*

IVPt AM

31

540

EV

«

700

N

04645 W

l*f9

76

35

10 0

53

1965

002

9348

914

09

23

2 2

XI

5 6

0114

WATER

WIND

BARO- METER (mb.)

AIR lEMP. "C

COD

NO. OBS.

DEPTHS

SPECIAL OBSERVATIONS

COLOR

CODE

TKANS,

DIR-

s«to

0« FOBCf

DRY BULB

WET

BULfl

19

SIO

119

017

Oil

B

08

MESSENCR ' HR 1/10

CAST

NO.

CARD TYPE

DEPTH Iml

T -C

s •/..

sigma-t

SMClfiC VOLUME *NOMAL»->10'

SAD OVN. M.

SOUND VElOCITy

Ol ml/l

PO4-P

lOTAl-P

WB • ol/i

N03-N

ug - 01/ 1

NO3-N vi - oi/l

SI 0*-S. vg - 01/1

pH

S

c c

STD

0000

0517

3435

2717

0009079

0000

14709

053

OBS STD STD STD

0000 0517 34357 2717 14709 0010 0510 3436 2717 0009028 0009 14707 0020 0500 3435 2718 0008951 0018 14705 0030 0487 3435 2720 0008836 0027 14701

053

OBS STD STD

0048 0458 34345 2723 14692 0050 0453 3435 2723 0008494 0044 14690 0075 0395 3444 2737 0007249 0054 14671

053

OBS STD STD STD STD

0080 0386 34451 2739 14669 0100 0388 3454 2745 0005451 0081 14674 0125 0391 3462 2752 0005903 0097 14680 0150 0395 3470 2757 0005356 0111 14687 0200 0403 3480 2765 0004745 0136 14700

053

OBS STD

0213 0406 34825 2766 14704 0250 0414 3487 2769 0004424 0159 14714

053

OBS STD STD

T0250 0414 34865 2769 14714 0300 0400 3487 2770 0004287 0181 14715 0400 0380 3488 2773 0004094 0222 14724

053

OBS STD STD

0425 0375 34881 2774 14727 0500 0373 3489 2775 0004058 0263 14738 0500 0358 3490 2775 0004025 0304 14753

053

OBS STD STD

0539 0355 34899 2776 14758 0700 0352 3490 2777 0004016 0344 14767 0800 0355 3490 2777 0004023 0384 14781

05

3

OB

3

T0851

o:

51

34

9

01

27

7E

147

87

130

REFERENCE

SHIP CODE

LATITUDE

I/IO

LONGITUDE ' '1/10

if

MARSDEN

STATION TIME

ORIGINATOR'S |

DEPTH

TO

BOTTOM

MAX

DEPTH

Of

S-MPL*

WAVE

WEA- THER

coot

CLOUD CODES

^ODC

cur CODI

ID. NO.

CRUISE

NO.

STATION NUMBER

10*

r

MO

DAY H

8.1/10

S Dl»-

HGT PER SEA

iin AM

31

540

EV

4559

N

04530 W 1

149

66

I'i

10 D68

1965

00?

9349 D360

03

22

3 2

XI

3 2

i 0115

WATER

WIND

BARO- METER (mbi)

AIR TEMP. -C

VIS. CODI

NO.

OBS. DEPTHS

SPECIAL OBSERVATIONS

COLOR CODE

T1U.NS.

DIR.

irtiD

OB FORCE

DRY BULB

WEI

BULB

20

S14

098

039

028

8

07

MESSENGt 1 (-457 "»' "NO. HR 1/10

CARD

TYPE

DEPTH Iml

T -C

s •/..

StGMA-T

SPECIFIC VOLUME ANOMALT-XIO'

SAD

DYN. M

n lo'

SOUND

VELOCITY

Ol ml/l

POi-P

TOTAL-P

t>a -oi/t

NO2-N

ug • ot/l

NO)-N vg - oi/l

SI O4-S. vg - Ol/l

pH

;

STD

0000

0476

3436

2722

0008609

0000

14692

068

CBS STO STD STD

STD

0000 0475 34360 2722 14692 0010 0472 3436 2722 0008580 0009 14692 0020 0458 3436 2723 0008556 0017 14592 0030 0455 3436 2723 0008534 0025 14692 0050 0457 3436 2724 0006481 0043 14692

068

OBS STD

0052 0455 34357 2724 14592 0075 0417 3437 2729 0007995 0053 14680

058

OBS STD

0082 0414 34392 2731 14680 0100 0451 3451 2736 0007324 0082 14700

058

OBS STD

0112 0453 34570 2741 14703 0125 0416 3460 2747 0005307 0100 14691

068

OBS STD STD

0142 0380 34643 2754 14579 0150 0382 3457 2755 0005460 0114 14581 0200 0392 3479 2755 0004707 0140 14695

068

OBS STD STD

T0227 0394 34839 2759 14701 0250 0393 3485 2770 0004315 0152 14705 0300 0385 3488 2772 0004092 0183 14710

068

OBS

T0330 0376 34890 2775 14711

REFERENCE

SHIP CODE

LA TIT U

DE 1/10

LONGITUDE * 'I/lO

ii

MAHSDEN

SQUARE

STATION TIME (GMTI

YEAR

ORIGINATOR'S 1

DEPTH TO

OTTOM

MAX. DEPTH

OF S*M PL-

WAVE OBSERVATIONS

WEA-

THER CODE

CLOUD CODES

NODC

STATION NUMBER

CIRT COO(

ID. NO.

CRUISE

STATION

NUMBER

10*

r

MO

DAY H

R.l/lO

Dl«.

MGI PER SE*

r»p[ AMI

31

540

EV

4658

N

04617 W

149

66 {

)5

10 0

79

1965

002

9350 D311

OB

19

3 2

X?

2 8

0116

WATER

WIND

BARO- METER (mbil

AlH TEMP. X

VIS, CODE

NO.

OBS.

DEPTHS

SPECIAL OBSERVATIONS

COLOR CODE

TRANS,

DIR-

SPIED

OR fORCt

DRY BULB

WET BULB

20

S13

098

044

033

8

05

MESSENOR CAST IIVE o '"n^. HR 1/10

CARD TYPE

DEPTH Iml

T "C

S •'',.

SIGMA-T

SPECIFIC VOLUWE

ANOMAIT-KIO'

SAD

OVN. M X 10^

SOUND VELOCITY

Ol tnl/l

PO4-P

ve • or/i

TCTAL-P

vg ■ Bi/I

NOi-N

«9 - ol/l

NOj-N vg ■ ol/l

SI04-Si Its - ol/l

.H

STD

0000

0419

3435

2727

0008072

0000

14668

079

OBS STD STD STD

STO STD

0000 0419 34353 2727 14668 0010 0419 3436 2728 0008041 0008 14670 0020 0420 3436 2728 0008017 0016 14672 0030 0420 3437 2729 0007984 0024 14574 0050 0421 3438 2729 0007929 0040 14677 0075 0422 3439 2730 0007865 0060 14682

079

OBS STD

0080 0422 34397 2731 14683 0100 0387 3445 2738 0007117 0078 14672

079

OBS STD

0124 0375 34555 2748 14573

0125 0377 3456 2748 0006214 0095 14574

079

OBS STD STD STD

0149 0400 34715 2758 14589

0150 0400 3472 2758 0005287 0110 14689 0200 0392 3478 2764 0004757 0135 14595 0250 0384 3485 2770 0004233 0157 14701

07

)

OB

>

T0272

03

80

34

8

77

27

i:

14703

REFERENCE

SHIP CODE

LATITUDE

1/10

LONGITUDE

■ -1/10

n

MARSDEN

STATION

Tl

WE

ORIGINATOR'S

DEPTH

MAX.

DEPTH

OF S'MPL'S

WAVE

WEA- THER CODE

CLOUD CODES

NODC

CIRT CODE

ID.

NO,

CRUISE NO.

STATION NUMBER

TO

BOTTOM

STATION

NUMBER

10* 1 r

MO

DAY

HR.1/10

DIR.

MGt fER S

A

ITPE AM

31

540

EV

4

700

N

04500 W

149

176 1

)5

10

D95

1965 002

9351

)302

03

21

b \z

X6

5 8

0117

WATER

WIND

BARO- METER

imbll

AIR TEMP. "C

v,s '*°- "-d?pVhs

SPECIAL OBSERVATIONS

COLOR CODE

IRANS,

OIH.

SPEED

DRY BULB

WET BULB

20

S18

085

044

033

7 04

MESSENGR

TIME d

HR 1/10

CAST NO.

CARD TYPE

DEPTH Iml

T -Q

s •/..

SIGMA-T

SPECIFIC VOLUME ANOMAH-IIO'

SAD

DYN. M.

X 10^

SOUND VELOCITY

Oj ml/1

PO4-P

roTAi_p

NO3-N

ug • al/l

NOj-N ufl - ol/l

SI 04-Si vg - ol/l

pH

s c c

STD

0000

0437

3439

2728

0007976

0000

14676

095

OBS STD STD STD STD STD STD

0000 0437 34390 2728 14676 0010 0434 3440 2729 0007904 0008 14676 0020 0431 3440 2730 0007838 0015 14677 0030 0428 3441 2731 0007766 0024 14677 0050 0422 3442 2733 0007628 0039 14678 0075 0415 3444 2735 0007457 0058 14680 0100 0408 3445 2737 0007278 0076 14681

095

OBS STD STO STD

0102 0407 34457 2737 14681 0125 0405 3458 2747 0006345 0093 14686 0150 0402 3459 2756 0005512 0108 14590 0200 0395 3484 2769 0004363 0133 14597

095

OBS STD

0204 0394 34848 2759 14698 0250 0385 3486 2771 0004135 0154 14702

09

5

OB

5

0280

0

378

34

6

73

27

1:

i

141

04

131

EV

LATITUDE

1/10

4722 N

LONGITUDE

•1/10

04818 W

MO DAY Ha.1/10:

149 l78 105 Il9 1094 11965 |003|9352

32

SPtED

Olt »0»CE

S18

ORIGINATOR'S

AIR TEMP. "Z

028 028 2 04

bl59 I 01 I 36 >

[Gri ftS SEA

X* 7 l8

NODC STATION NUMBER

0118

SPECIFIC VOLL

SlO^-Si

09* 09*

094

STD

OBS STO STD STD STD

OBS STD

OBS STD STO

OBS

0000 0000 0010 0020 0030 0050 0050 0076 0080 0100 0126 01*6

01*0

0057

0005

-00*4

-0111

-012*

-0127

-0105

-0045

0032

328*

32835

328*

3285

3287

3294

32938

3309

33122

3325

3343

33575

2630 2530 2535 2539 2643 2551 2551 2564 2565 2676 2588 2596

0017273

0015812

0015*33 0016065 0015301

0012897 00117**

0000

0017 003* 0050 0081

001*080 0118

0152 0183

1*526 1*526 1**95 1**69 1***8 1**21 1**21 1*421 1**21 1**36 1**71 1*512

REFERENCE

SHIP CODE

LATITUDE

1/10

LONGITUDE

■1/10

°i

MARSOEN

STATION

Tl

^i

ORIGINATOR'S 1

DEPTH

MAX

■

WAVE

WEA- THER CODE

CLOUD CODES

'4O0C

criY coot

ID. NO.

YEAR

CRUISE NO.

STATION NUMBER

TO BOTTOM

OF S'MPL'S

STATION NUMBER

10*

1*

MO

OAV

MR.1/10

DIR.

HCI PER SEA

"PE AM

31

540

EV

4

722

N 1 04f

i07 w

149

78

15

19

106

1965

003

9353 )181

02

35

3 3

X4

7 8

0119

WATER I WIND

BARO- METER Imbt)

AIR TtMP. 'C

VIS, COD

NO.

OBS. DEPTHS

SPECIAL

OBSERVATIONS

COLOR CODE

tRANS.

OIR.

SPEfO OR

Foact

DRY BULB

WET eULB

34

516

173

033

5

05

MESSING*

TIMI C

HR 1/10 '

CAST

NO.

CARD TYPE

DEPTH Iml

T -C

s •/..

SIGMA-T

SPICIfIC VOLUMI ANOMALI-IIO'

SAD

OYN. M.

t 10^

SOUND

VELOCITY

Oj ml/I

PO4-P ws - o'/l

TOTAL-P ■>g - ol/l

NO3-N

ug . ol/l

NO3-N pg . o./l

SI 0*-Si UB - ol/l

PH

S

C

c

STO

0000

0133

3282

2629

0017374

0000

14523

106

OBS STD STD STD STO

0000 0133 32816 2629 14523 0010 0075 3283 2634 0016931 0017 14499 0020 0025 3284 2638 0016567 0034 14478 0030 -0017 3286 2641 0016259 0050 14460 0050 -0076 3289 2646 0015807 0082 14437

106

OBS STD

0050 -0076 32887 2646 14437 0075 -0089 3301 2656 0014806 0121 14436

106

OBS STD STD

0090 -0097 33109 2664 14437 0100 -0053 3327 2676 0012942 0155 14461 0125 0025 3354 2694 0011241 0186 14505

106

OBS STD

0140 0050 33630 2700 14520 0150 0052 3363 2700 0010680 0213 14522

10

J

OB,

3

0165

oc

55

33

6

38

27

OC

14326

REFERENCE

SHIP CODE

LATITUDE

1/10

LONGITUDE

•i/io

°i

MARSOEN

STATION

Tl

WE

ORIGINATOR'S

DEPTH

MAX. DEPTH

OF S'MPL'S

WAVE

WEA- THER CODE

CLOUD COOES

■4000

CTRY CODE

10.

NO.

YEAR

CRUISE NO.

STATION NUMBER

TO

BOTTOM

STATION

NUMBER

10-

r

MO

DAY

HR.1/10

Dit. |MGrlPe»| s

A

IVPE AM

31

540

EV

4

723

N

0*751 W

1*9

77

D5

19

122

1965

003

935*

3210

02

35

Ul

X4

6 8

0120

WATER

WIND

BARO- METER

(mbl)

AIR TEMP.

^

VIS. COD

NO.

OBS.

DEPTHS

SPECIAL OBSERVATIONS

COLOR CODE

tRAHS.

OIR.

SPEED

OR PORCE

DRY BULB

WET BULB

3*

518

186

039

033

^

07

MESSENCR

TIME ( HR 1/10

CAST NO.

CARD TYPt

DEPTH Iml

T -C

s •/..

SIGMA-T

SPECIFIC VOLUME

ANOWALY-XIO'

SAO DYN. M.

1 loi

SOUND VELOCin

03 ml/I

PO4-P V9 - ol/l

lOTAL-P MB • o'/l

NOj-N

ug - oi/I

NOj-N VB - Qt/I

SIO4-S. MB - ol/l

pH

s

c c

STD

0000

0106

3283

2632

0017129

0000

14511

122

OBS

0000 0105 32827 2632

1*511

STD

0010 0100 3283 2632

0017083

0017 1*510

122

OBS

0017 0095 32829 2633

1*509

STO

0020 0059 328* 2635

0016822

003* 1**98

STO

0030 -0005 3287 26*1

0016223

0051 1**66

122

OBS

00*3 -0075 32912 25*8

1**36

STD

0050 -0076 3293 26*9

0015*77

0082 1**37

STD

0075 -OOBl 3302 2566

001*759

0120 1***1

122

OBS

0084 -0082 33051 2650

1***2

STD

0100 -0059 3316 2667

001379*

0156 1**52

122

OBS

0110 -01500 33200 26730

STD

0125 -0049 3323 2672

0013252

0190 1**66

STD

0150 -0030 3334 2680

0012491

0222 1*481

122

OBS

0172 -0012 33*85 2691

14*95

12

2

OB

3

T0193

OC

53

33

5

67

27

o;

145

35

132

REFeHENCE

SHIP CODE

LATITUDE

I/IO

LONGITUDE

"1/10

ii

MASSOEN

STATION

Tl

Wl£

ORIGINATOR'S

DEPTH

MAX.

WAVE

WEA- THER CODE

CLOUD CODES

■iODC

CItT

CODt

ID. NO.

CRUISE NO.

STATION NUMBER

TO BOTTOM

OF S'MPL-S

STATION NUMBER

10*

r

MO

DAY

HR.1/10

Dl«.

KGT HH !(A

ITfl AM

31

540

EV

i

723

N

04733 W

149

77 05

19

137

1965

003

9355 )267

02

36

3 4

X?

6 e

0121

WATER

WIND

BARO- METER

(mbs)

AIR TEMP. "C

SPECIAL OBSESVATIONS

COLOR CODE

'r.r-

OIR.

SPHO

0> fORCf

DRY

BULB

WET BULB

34

508

207

028

7

07

MESSCNGI HH l/IO

CAST

NO.

CARD TYPE

DEPTH (ml

T -C

s ■''..

SIGMA-T

ipfcinc voiuMt

ANOMALY-IIO'

SAO

DYN. M.

SOUND VELOCITY

Ol ml/I

P04-P

tOT*l-P

NOj-N

NO3-N

va - oi/i

SIO«-Si

i;g - ol/l

pH

C C

STD

0000

Q13U

3284

2631

0017221

0000

14524

137

OBS STD STD

0000 0134 32837 2631 14524 0010 0060 3285 2535 0015699 0017 14492 0020 0007 3285 2540 0016361 0033 14470

137

OBS STD STO

0025 -0012 32867 2541 14462 0030 -0015 3287 2542 0016184 0050 14451 0050 -0027 3290 2545 0015896 0082 14460

137

OBS STD

0050 -0027 32900 2645 14460 0075 -0112 3297 2653 0015037 0121 14425

137

OBS STD STD

0081 -0124 32994 2555 14421 0100 -0120 3305 2551 0014307 0157 14427 0125 -0101 3319 2671 0013359 0192 14442

137

OBS STD STD

0125 -0100 33191 2571 14442 0150 -0036 3334 2681 0012461 0224 14478 0200 0092 3374 2706 0010110 0280 14550

137

OBS

T0233 0173 34078 2728 14596

137

OBS

T0243

0197

34192

273S

14610

REFERENCE

SHIP CODE

LATITUDE

1/10

LONGITUDE

■1/10

ii

MARSDEN

STATION

TIME

ORIGINATOR'S

DEPTH

MAX.

DEPTH

OF S-MPL-

WAVE

WEA- THER CODE

CLOUD CODES

NOOC

cool

ID. NO.

CRUISE NO.

STATION NUMBER

BOTTOM

NUMBER

10*

r

MO DAY

HR.1/10

Dl».

HGI n» SE*

I.fi AM

31

540

FV

4

722

N

04718 W

149

77

D5 19

150

1965

003

9356

3329

03

36

3 2

X?

6 8

0122

WATER

WIND

BARO- METER

Imbtl

AIR TEMP. "C

VIS.

coo

NO.

OBS. DEPTHS

SPECIAL OBSERVATIONS

COLOR CODE

TRANS.

DIR.

SPEED

0»

DRY BULB

WET BULB

33

S13

210

022

017

8

05

MEISENCK

IIMf (

HR l/IO

CAST NO.

CARD

TYPE

DEPTH Iml

T -C

s •/..

SIGMA-T

SPtClflC VOlUMt

SAD

DYN. M.

X 10'

SOUND

VELOCITY

Oj ml/l

PO4-P

»g - ol/l

TOTAI-P

NO2-N

„a - al/l

N03-N

WB - -t/l

SI04-Si wg - oi/l

pH

S

c c

STD

0000

0243

3307

2641

0016241

0000

14575

150

OBS STD STD STD

0000 0243 33055 2541 14575 0010 0150 3310 2650 0015389 0016 14541 0020 0090 3313 2557 0014730 0031 14511 0030 0034 3317 2654 0014122 0045 14488

150

OBS STD STD

0045 -0027 33237 2672 14463 0050 -0025 3325 2573 0013231 0073 14455 0075 -0015 3335 2680 0012503 0105 14475

150

OBS STD STD

0098 -0005 33508 2593 14486 0100 -0000 3353 2694 0011195 0134 14489 0125 0069 3376 2709 0009815 0161 14528

150

OBS STD STD STD STD

0126 0072 33758 2709 14529 0150 0131 3395 2721 0008695 0184 14563 0200 0228 3430 2741 0006873 0223 14618 0250 0293 3452 2753 0005811 0254 14558 0300 0324 3464 2760 0005239 0282 14681

15

D

OB

5

T0301

0

J26

346

48

27

6

D

14e

83

133

REFERENCE

SHIP CODE

LATIIUDE

1/10

lONGIlUDE * '1/10

ii

MARSDEN

STATION

T1

.E

ORIGINATOR'S

DEPTH

MAX.

WAVE

WEA- THER CODE

ClOUD CODES

NODC

cr«T COOi

ID. NO.

CRUISE NO.

STATION NUMBER

BOTTOM

OF S'MPL'S

STATION NUMBER

10"

r

MO

DAV

HR.1/10

DIR.

HGI PER SE*

TYPE AM

31

•0,0

FV

A

722

N

0<(704 W

149

77

DS

19

167

1965

003

9357 D927

09

36

3 2

X?

6 8

0123

WATER

WIND

8AH0- METER

(rnbd

AIR TEMP. -C

VIS. COD

NO.

OBS.

DEPTHS

SPECIAL OBSERVATIONS

COLOR CODE

IRANS.

D1R.

SPEED FORCE

DRY BULB

WET eULB

33

Sll

220

056

050

8

11

M(55(NG« 1

TIME or

HR 1/10 '

CASl NO.

CARD TYPE

DEPTH [ml

I -c

s •/..

SlGMA-T

iPECIFIC VOLUME AHOMAtr^IlO'

SAO

DlfN. M. X 10^

SOUND VEIOCITT

Oj ml/1

PO4-P

vg - ol/l

TOTAL-P »g - ol/l

NOl-N

Wfl - OI/l

NO,-N lig - ol/l

SIO*-S. uO - ol/l

PH

c c

STO

0000

031A

3350

2670

0013525

0000

14612

167

OBS

0000 0314 33500 2670 1*612

STD

0010 0269 3364 2685 0012097 0013 14595

STD

0020 0205 3373 2697 0010926 0024 14571

167

OBS

0025 0167 33761 2703 14555

167

OBS

0029 0133 33778 2706 14541

ST3

0030 0140 3379 2707 0010021 0035 14544

167

OBS

0049 0252 34008 2716 14600

STD

0050 0252 3401 2716 0009183 0054 14600

STD

0075 0251 3414 2726 0008208 0076 14606

STD

0100 0251 3427 2737 0007234 0095 14611

167

OBS

0122 0250 34376 2745 14616

STD

0125 0257 3439 2746 0006396 0112 14620

167

OSS

0146 0297 34490 2750 14642

STD

0150 0301 3450 2751 0005966 0128 14644

STD

0200 0339 3466 2760 0005155 0155 14671

167

OBS

T0219 0350 34705 2762 14680

STD

0250 0356 3473 2764 0004838 0180 14688

STD

0300 0365 3476 2765 0004747 0204 14700

167

OBS

0389 0376 34809 2768 14720

STD

0400 0376 3481 2768 0004577 0251 14722

STD

0500 0378 3484 2770 0004465 0296 14740

167

OBS

T0580 0380 34856 2771 14754

STD

0600 0380 3486 2772 0004427 0341 14757

STD

0700 0381 3487 2772 0004455 0385 14775

167

OBS

0764 0382 34872 2772 14786

STD

0800 0380 3488 2773 0004493 0430 14791

167

OBS

T0856

037A

34879

2774

14798

REFERENCE	SHIP CODE	LATITUDE 1/10	LO	GITUDE ■ 'I/IO	1^	MARSDEN	STATION T	ME			ORIGINATOR'S	DEPTH	MAX. DEPTH OF S'MPL-S		WAVE		WEA- THER CODE	CLOUD CODES			MODC
CIRY CODf	ID. NO.			YEAR	CRUISE NO.	STATION NUMBER	TO BOTTOM			STATION NUMBER
10-	r	MO	DAY H	R.1/10	OIR-	MGI PER SEA	trpt AM
31	540	EV	4721	N	04650 W		149	76	D5	19 1	83	1965	00 3	9358	225	u	36	2 3	X?	6 8	0124
			WATER	WIND	BARO- METER Imbd	AIR TEMP. -C	COD	NO. OBS. DEPTHS	SPECIAL OBSERVATIONS
	COLOR CODE	'""-	DIR.	SPIED OR FORCE	DRY BULB	WET BULB
				33	S09	234	050	044	8	11
	"!""<=" IcAST ""' ' NO. MR 1/10	CARD TYPE	DEPTH Iml	I -c	s •/..	SIGMA-T	SPECIFIC VOLUME NOML'-H0'	SAD DYN. M.	SOUND VELOCITY	Oj ml/l	PO4-P	IOTAl_P KB - ol/l	NO2-N UB- ol/l	NO3-N UB - ol/l	SI04-Si UB - ol/l	pH	S C c
		STD	0000	0385	3391	2696	0011069	0000	14648
183	OBS	0000 0386 33912 2695 14648
	STD	0010 0313 3399 2709 0009823 0010 14520
	STO	0020 0259 3405 2718 0009003 0020 14603
183	OBS	0021 0256 34053 2718 14602
	STD	0030 0276 3411 2722 0008608 0029 14608
183	OBS	0047 0293 34161 2724 14619
	STD	0050 0253 3415 2727 0008132 0045 14507
183	OBS	0058 0193 34161 2733 14578
	STD	0075 0223 3427 2739 0006999 0064 14595
	STD	0100 0262 3442 2748 0006197 0081 14618
	STD	0125 0295 3454 2754 0005594 0096 14638
183	OBS	0136 0307 34583 2757 14646
	STD	0150 0317 3461 2758 0005285 0109 14653
	STD	0200 0348 3471 2763 0004867 0135 14676
183	OBS	T0236 0364 34763 2766 14689
	STO	0250 0366 3477 2766 0004638 0158 14692
	STD	0300 0370 3480 2768 0004498 0181 14703
	STD	0400 0377 3484 2770 0004361 0225 14723
183	OBS	T0418 0378 34846 2771 14726
	STD	0500 0378 3486 2772 0004317 0269 14740
	STO	0600 0379 3488 2773 0004254 0312 14757
183	OBS	0527 0379 34884 2774 14752
	STD	0700 0374 3489 2775 0004232 0354 14772
	STO	0800 0369 3490 2775 0004218 0396 14786
183	OBS	T0832 0367 34897 2776 14791
	STD	0900 0364 3490 2777 0004211 0439 14801
	STD	1000 0360 3490 2777 0004246 0481 14816
183	OBS	1065 0357 34902 2777 14826
	STD	1100 0351 3490 2778 0004202 0523 14829
		18	3	OB,	>	T1119		03	47	34	9	04	27	7c								148	30

134

LATITUDE

1/10

4722 N

LONGITUDE

DAY HR.l/K

149 |76 |05 Il9 1202 ll?65

SPEED

fOtCf

ORIGINATOR'S

8AR0.

METES

0031 9359

AIR TEMP, "C

061

253 I 11 I 35 >

<CllPE< SEA

WEA- THER CODE

XI 6 '6

NOOC STATION NUMBER

0125

SfEClFIC VOLL

SOUND VELOCITY

NO3-N ug - ol/l

SIO<-Si

202

202 202 202

202

202 202

STD

OBS STD STD STD STD STD STD

OBS STD

OBS STD STD STD STD

OBS STD STD

OBS

OSS

0000 0000 0010 0020 0030 0050 0075 0100 0119 0125 0134 0150 0165 0200 0250 0300 0400

T0414 0500 0500

T0619 0700 0800 0825 0900 1000

T1027

T1067

0494 0494 0489 0482 0475 0456 0427 0391 0359 0344 0331 0358 0380 0379 0378 0377 0375 0375 0373 0370 0369 0366 0362 0351 0355 0349 0348 0347

3408

34081

3418

3426

3434

3447

3458

3464

34645

3463

34626

3469

34745

3477

3480

3482

3486

34867

3488

3489

34894

3490

34902

3490

34903

34902

2698 2698 2706 2713 2720 2733 2745 2753 2757 2757 2758 2760 2753 2755 2757 2759 2772 2773 2774 2775 2775 2775 2777 2777 2778 2778 2778 2778

0010897

0010111 0009446 0008781 0007625 0006522 0005729

0004728 0004538 0004424 0004194

0004110 0004092

0004061 0004102

0004092 0004097

0000

0011 0020 0029 0046 0053 0079

0005358 0093

0005073 0106

0130 0153 0175 0219

0260 0301

0342 0383

0424 0465

14695 14695 14696 14596 146 96 14593 14687 14676 14666 14660 14655 14671 14684 14690 14698 14706 14722 14725 14738 14754 14756 14769 14784 14787 14797 14611 14815 14822

REFERENCE

SHIP CODE

LATITUDE

I/IO

LONGITUDE

"I/lO

°i

MARSDEN

STATION T

ME

ORIGINATOR'S 1

DEPTH

MAX

",

WAVE

WEA- THER CODE

CLOUD CODES

^ODC

cmT 10. CODE NO.

YEAR

CRUISE NO,

STATION

TO

OF

S'MPL'S

STATION NUMBER

10"

!•

MO

DAY H

R.1/10

NUMBER =w..w™.

DIB_ lMCr|»E«| S(*

I'Pi AM

31 540

EV

4

722

N

04620 W

149

76

)5

19 2

18

1965

003

9360 D540

05

34

Ul

XI

6 2

0126

WATER

WIND

BARO- METER

AIR TEMP, "C

VIS- CODf

NO. OBS.

DEPTHS

SPECIAL OBSERVATIONS

COLOR CODE

'"?■

out.

S»E(tJ

0« (0«Cf

DRY BULe

WET BULB

36

S04

240

050

044

8

07

MESEENCR

TIME e

HR 1/10

CAST

NO.

CARD

TYPE

DEPTH Iml

I -c

s •''^

S1GMA-T

SPECIFIC VOLUME ANOWAir-dO'

SAD DYN. M.

X 10'

SOUND

VELOCITY

0} ml/l

PO*-P

tOIAl-P

vg ■ oi/l

NOl-N ug - ol/I

NO3-N vg - e'/l

SIO,(-S. wg.or/[

pH

C C

STD

0000

0472

3422

2711

0009640

0000

14688

218

OBS STD

0000 0472 34217 2711 14688 0010 0469 3422 2711 0009500 0010 14689

218

OBS STD

0015 0468 34233 2713 14689 0020 0404 3427 2722 0008566 0019 14664

218

OBS STD STD

0024 0360 34292 2729 14646 0030 0360 3432 2731 0007778 0027 14648 0050 0362 3440 2737 0007204 0042 14653

218

OBS STD STD STD STD STD

0074 0353 34491 2744 14658

0075 0363 3449 2744 0006540 0059 14659 0100 0368 3455 2748 0006213 0075 1*665 0125 0374 3450 2752 0005881 0090 14673 0150 0379 3465 2755 0005555 0104 14680 0200 0389 3475 2753 0004905 0131 14694

218

OBS STO STD

T0246 0399 34858 2770 14707 0250 0398 3485 2770 0004293 0154 14707 0300 0392 3488 2772 0004128 0175 14713

218

OBS STD STD

T0397 0382 34893 2774 14725 0400 0382 3489 2774 0004041 0215 14725 0500 0374 3488 2774 0004121 0255 14738

21

3

08

3

0501

0;

74

34

8

79

27

7'

141

39

135

rii .i-,f ;r:i^ .

LATITUDE

ORIGINATOR'S

J DEPTH

1 '° BOTTOM

31

*720 N

1*9 |76 |05

9 1233

1965

00319361

BARO- METER

(mbl)

AIR TEMP. "C

393 I 0* I 3* b

NO.

OBS.

DEPTH

8 07

XI 7 '2

0127

SAD

DTN. M.

X 10^

NOj-N VS - ol/l

233

233 233 233

233

STD OBS

STD STD STD

OBS STD STD

OBS STD

OBS STD STD

OBS

0000

0000 0010 0020 0030 003* 0050 0075 0086 0100 0125 0137 0150 0189 0200

T02*l 0250 0300

T0370

0502 0502 0*65 0*35 0*12 0*0* 0*0* 0*0* 0*0* 0*11 0*20 0423 0*23 0*22 0*31 0*52 0**7 0*16 037*

3*20

3*200

3*2*

3*28

3*32

3*3*3

3***

3*58

3*625

3*67

3*7*

3*767

3*78

3*830

3*86

3*932

3*93

3*91

3*888

2706 2706 2713 2720 2726 2728 2736 27*7 2751 2753 2758 2760 2761 2765 2766 2770 2770 2772 2775

0010091

0009*0* 0008802 0008279

0007315 0006287

0005706 0005299

0005053

000*592

000*299 000*1*8

0000

0010 0019 0027

00*3 0060

0075 0089

0102

0126

01*8 0169

1*700 1*700 1*687 1*677 1*669 1*667 1*671 1*677 1*679 1*685 1*69* 1*698 1*700 1*707 1*713 1*729 1*728 1*72* 14717

LATITUDE

1/10

LONGITUDE

"1/10

ORIGINATOR'S

31 5*0 EV

*721 N

0*5*8 W

1*9 l75 lOS

006 006

006

STD

OBS STD

OBS STD STD STD STD STD STD

OBS STD STD STD

OBS

0000 0000 0010 0015 0020 0030 0050 0075 0100 0125 01*2 0150 0200 0250 T0290

0 b06 11965

05*5 05*5 05*1 0538 0528 0510 0*75 0*38 0408 038* 0371 0372 0377 0382 0386

3*31

3*310

3*31

3*310

3*32

3*33

3*37

3**1

3**5

3*50

3*53*

3*56

3*66

3*77

3*868

00319367

BARO- METER

2710 2710 2710 2711 2713 2715 2723 2730 2736 27*3 27*7 27*8 2756 276* 2772

AIR TEMP. 'C

056 050

SPECIFIC VOLL

0009503 0009238 0008578 0007912 0007327 000673*

0006259 0005529 000*800

Iri311 I 03 I 3* b l3

00097*7

0009713 0010

0019 0029 00*7 0067 0086 010*

0120 01*9 0175

SOUND VELOCITY

1*719 1*719 1*719 1*719 1*716 1*710 1*700 1*689 1*681 1*676 1*673 1*675 1*687 1*699 1*709

XO X '0

0128

NOj-N ifg - ot/l

limiNCl

'i\mt

REFERENCE

SHIP CODE

LATITUDE

1/10

LONGITUDE

1/10

°l

MARSDEN

STATION

TIME

ORIGINATOR'S

DEPTH

MAX. DEPTH

OF S-MPL*S

WAVE

WEA- THER

CODE

CLOUD COOES

MOOC

CTKT CODE

ID.

NO.

YEAR

CRUISE NO.

STATION NUMBER

TO BOTTOM

SIAIiON

NUMBER

10*

r

MO

DAY

HR.1/10

DIR-

HGi nt it*

n»[ *M

31

5*0

EV

t

e722

N

0*523 W

1*9

75

^^

?0

027

1965

003

9363

32^7

02

TS

2 2

XO

X 0

0129

WATER

WIND

BARO- METER Imbtl

AIR TEMP. "C

"".D°^s

SPECIAL OBSERVATIONS

COLOR CODE

IRANS.

OIR.

SPEfO

CR FORCE

DRY BULB

WET BULB

31

S06

2*7

050

0**

8 0^

MESitNCR

HR 1/10

CAST NO.

CARD TYPE

DEPTH Iml

T -C

s '/.,

SIGMA-I

SPECIFIC VOLUME

ANDWALT-IIO'

SAD

DYN. M.

X 10'

SOUND VELOCIIT

Oi ml/l

PO«-P pfl - dr/l

rOTAL-»

NOj-N i>g - ot/l

NOj-N Ui- ol/l

S10«-Si US - ol/l

pH

s c c

STD

0000

0551

3*26

2705

0010220

0000

1^721

027

OBS STD STD

0000 0551 3*256 2705 1*721 0010 0*96 3*2« 271* 0009361 0010 1*701 0020 0**7 3*32 2722 0008626 0019 1*682

027

OBS STD STD STD STD STD

0025 0*26 3*335 2725 1*675 0030 0*20 3*35 2727 000813* 0027 1*673 0050 0*00 3*39 2732 0007652 00*3 1*669 0075 0381 3**6 27*0 0006961 0061 1*666 0100 0369 3*52 27*6 0006*1* 0078 1*666 0125 0365 3*60 2752 0005833 0093 1*669

027

OBS STD STD

0125 0365 3*595 2752 1*669 0150 0368 3*67 2758 0005321 0107 1*675 0200 0396 3*83 2768 000***1 0132 1*698

02

7

08

3

0200

02

96

3*

8

31

27

5£

l'^6

98

136

■ nil

mi

(0,.i

ll.tf

, 1

SHIP CODE

31 540 EV

LATITUDE

1/TO

4722 N

LONGITUDE

■l/IO

048

048 048 048

STD OBS

STD STD

OBS STD STD

OBS STD STO

OBS

OOGO

0000 0010 0020 0025 0030 0050 0051 0075 0100 0102 0125 0150 0177

STATION TIME

MO DAY HR.I/10

0536 0536 0482 0442 0427 0422 0407 0406 0395 0384 0383 0386 0390 0394

149 74 05 20 046 11965 10031 9364

SrEtD

on

FOtCf

3430

34299

3433

3435

34361

3437

3438

34382

3440

3444

34441

3450

3459

34705

ORIGINATOR'S

BARO- METER (mbtl

247

2710 2710 2719 2725 2727 2728 2731 2731 2734 2738 2738 2742 2749 2758

050

SFtCIFIC VOLUME

0009727

NO. OBS. DEPTHS

05

000891 000834

000804 000778

000755 000716

000675 000614

0000

0009 0018

0026 0042

0061 0080

0097 0113

02

35 |2

ICIIPH SEA

WEA- THER CODE

14716 14716 14695 14681 1*675 14674 14671 14671 14671 14671 14671 14677 14684 14691

0130

REFERENCE	SHIP CODE		LATITU		LONGITUDE ' '1/10	li	MARSDEN	STATION	TIME			ORIGINATOR'S	DEPTH	MAX. DEPTH OF S-MPL'		WAVE		WtA- THER CODE	CLOUD CODES			NODC
CIRT CODE	ID. NO.	DE l/IO				CRUISE NO.	STATION NUMBER	BOTTOM
10'	r	MO	DAY	HR.l/10	Dl".	M01\|»E« S£A	lYU »W		131
31	SiO	FU	4	623	N	04511 U		149	65	IS	70	108	1965	003	9365	?n5fl	12	^4	61	XI	4 2		r
			WATER	WIND	BARO- METER (mbfl	AIR TEMP.	i:	VIS. coo	NO. OBS. DEPTHS	SPECIAL OBSERVATIONS
	COLOR CODE	'""'■	DIR.	SFEED 0« FORCE	DRY BULB	WET BULB
				01	510	274	089	072	3	09
	MtSSENCR TIME c HR l/IO	CAST NO.	CARD TYPE	DEPTH Iml	T 1:	s •/..	SIGMA-T	SPECIFIC VOLUME ANOMALT-IIO'	SAD DYN. M. > 10"	SOUND VELOCITY	Oj ml/1	PO4-P ..9 • ol/l	tOTAl-r	NOj-N ug - or/I	NOj-N wa- ot/i	SI04-SI VS - ol/l	pM	S c c
			STD	0000 I 0571	3440	2713	0009396	0000	14731
108		OBS	0000 0571 34397 2713		14731
		STD	0010 0518 3442 2722	0008629	0009 14712
		STD	0020 0472 3444 2729	0007988	0017 14694
		STD	0030 0433 3446 2735	0007424	0025 14680
108		OBS	0030 0433 34462 2735		14680
		STD	0050 0423 3452 2740	0005905	0039 14680
		STD	0075 0412 3459 2747	0006293	0056 14680
		STD	0100 0403 3465 2753	0005775	0071 14682
		STD	0125 0396 3470 2757	0005352	0085 14683
108		OBS	0128 0395 34707 2758		14684
		STD	0150 0394 3473 2760	0005128	0098 14687
		STD	0200 0391 3479 2765	0004694	0123 14695
		STD	0250 0388 3483 2769	0004410	0145 14702
108		OBS	T0262 0387 34842 2770		14704
		STD	0300 0395 3486 2771	0004276	0167 14714
		STO	0400 0415 3492 2773	0004149	0209 14740
108		OBS	0411 0417 34929 2773		1*743
		STD	0500 0391 3491 2775	0004082	0250 14746
		STD	0600 0371 3490 2776	0004028	0291 14754
108		OBS	T0635 0366 34897 2776		1*758
		STD	0700 0365 3490 2776	0004079	0331 14768
		STD	0800 0363 3490 2776	0004143	0372 1*784
108		OBS	0844 0362 34895 2776		14791
		STD	0900 0359 3490 2777	0004189	0414 14799
		STD	1000 0354 3489 2777	0004222	0456 14813
108		OBS	T1075 0352 34893 2777		14825
		STD	1100 0351 3489 2777	0004298	0499 14829
		10	8		OB	S	T116	S	0	350	3'	.«	9C		2-	n	7							14<	139

137

REFERENCE

SHIP CODE

LATITUDE

1/10

LONGITUDE

' -1/10

ii

MARSOEN

STATION TIME

ORIGINATOR'S 1

DEPTH TO

BOTTOM

MAX

DEPTH

OF S'MPL'

WAVE

WEA- THER

CODE

CLOUD CODES

■JODC

CUT CODE

NO.

CRUISE NO.

STATION NUMBER

10-

r

MO

DAY H

R.l/lO

S OIR.

HOT n» SE*

ITU AM

31

s*n

EV

*720

N

0*506 W

U9

76

D5

19 233

1965

003

9361 D393

04

34

5 3

XI

7 2

1 0127

WATER

WIND

AIR TEMP. X

CODE

NO.

OBS.

DEPTHS

SPECIAL OBSERVATIONS

COLOR CODE

I PUNS.

D1R.

iriiO

OR fO»CE

METER

(mbll

DRY

BULB

WEI BULB

3'f

506

247

056

039

6

07

HR 1/10

CARD TYRE

DEPTH (ml

T -C

S '/..

SIGMA-T

i^ECIFIC VOIUME ANOMALT-llO'

SAO

DYN. M t 10^

SOUND VELOCITY

Oj ml/I

P04-P

rOTAL-P ug - o./(

NOj-N US - ol/l

NO3-N

PS - o'/l

SI04-Si

we • oi/i

pH

STD

0000

0502

3A20

2706

0010091

0000

14700

233

OBS

0000 0502 3*200 2705 1*700

STD

0010 0*65 3*2* 2713 0009*0* 0010 1*587

STO

0020 0*35 3*28 2720 0008802 0019 1*677

STD

0030 0*12 3*32 2725 0008279 0027 1*669

233

OBS

003* 0*0* 3*3*3 2728 1*667

STD

0060 0*0* 3*** 2736 0007315 00*3 1*571

STD

0075 0*0* 3*58 27*7 0005287 0050 1*577

233

OBS

0085 040* 3*625 2751 1*679

STD

0100 0*11 3*57 2753 0005706 0075 1*685

STD

0125 0*20 3*7* 2758 0005299 0089 1*69*

233

OBS

0137 0*23 3*757 2750 1*598

STD

0150 0*23 3*78 2761 0005053 0102 1*700

233

OBS

0189 0*22 3*830 2755 1*707

STD

0200 0*31 3*86 2756 000*592 0126 1*713

233

OBS

T02*l 0452 3*932 2770 1*729

STD

0250 0**7 3*93 2770 000*299 01*8 1*728

STD

0300 0*16 3*91 2772 000*1*8 0169 1*72*

233

OBS

T0370 037* 3*888 2775 1*717

REFERENCE

SHIR CODE

LATITU

DE 1/)0

LONGITUDE ' '1/10

MARSDEN SQUARE

STATION TIME IGMT)

YEAR

CR

ORIGINATOR'S [

DEPTH

TO OTTOM

MAX. DEPTH

OF S'MPL-

WAVE OBSERVATIONS

WEA- THER CODE

CLOUD CODES

NODC STATION NUMBER

CIRT CODE

10. NO.

JISE

STATION NUMBER

10'

r

MO

OAV H

R.l/10

DIR-

HGT f(R SEA

H^t AMI

31

5*0

FV

*721

N

0*5*8 W

1A9

75

)5

20 0

06

1965

003

9362 _ 3311

n3

34

5 3

xn

X 0

0128

WATER

WIND

SARO-

METER

AIR TEMP. -C

VIS CODE

NO.

OBS. DEPTHS

SPECIAL OBSERVATIONS

COLOR CODE

TRANS,

OIR.

OR FOBC

DRY BULB

WET BULB

34

S06

251

056

050

8

04

»"""':> IcASt

HR 1/10

CARD TYPE

DEPTH (ml

T 1C

s ■/„

SIGMA-T

incinc VOLUME

*NOMALt-X10'

SAD DYN. M

X 10^

SOUND VELOCITY

02 ml/1

PO4-P

va -01/1

lOTAl-P ua - ar/1

N03-N

t>g - *i/l

NOi-N vg - at/I

S104-S1

wg . or/I

pM

STD

0000

05^*5

3'»31

2710

0009747

OOOO

14719

006

OBS

0000 05*5 3*310 2710 1*719

STD

0010 05*1 3*31 2710 0009713 0010 1*719

006

OBS

0015 0538 3*310 2711 1*719

STD

0020 0528 3*32 2713 0009503 0019 1*716

STD

0030 0510 3*33 2715 0009238 0029 1*710

STO

0050 0*75 3*37 2723 0008578 00*7 1*700

STD

0075 0*38 3**1 2730 0007912 0067 1*589

STD

0100 0408 3**5 2736 0007327 0086 1*681

STD

0125 038* 3*50 27*3 000673* 010* 1*676

006

OBS

01*2 0371 3*53* 27*7 1*673

STD

0150 0372 3*55 27*8 0005259 0120 1*675

STD

0200 0377 3*65 2756 0005529 01*9 1*687

STD

0250 0382 3*77 275* 000*800 0175 1*699

00(

5

OB

3

T0290

03

86

34

e

68

27

7i

14709

I

REFEHENCt

SHIP CODE

LAT(TUDE

1/10

LONGITUDE

1/10

i|

MARSOEN

STATION

TIME

ORIGINATOR'S

DEPTH

MAX.

WAVE

WEA- THER

CODE

CLOUD CODES

NODC

CIRT CODE

ID. NO.

CRUISE NO.

STATION NUMBER

BOTTOM

Of S'MPL'S

NUMBER

10*

r

MO

DAY

HR.1/10

OIR,

MGT PER SE*

tVPl AM

31

540

FV

*

722

N

0*523 W

149

75

35

?0

n?7

1965

003

9363

D247

02

35

2 2

xo

X 0

0129

WATER

WIND

BARO- METER (mbl)

AIR TEMP. "C

VIS.

coo

NO. OBS. DEPTHS

SPECIAL OBSERVATIONS

COLOR CODE

T)l*NS.

OIR.

SPEED

fORCE

DRY

BULB

WET BULB

31

506

247

050

044

8

04

MESStNCR

TIME c

HR 1/10

CAST NO.

CARD TYPE

DEPTH [ml

T -C

s •/..

SIGMA-T

SPECIFIC VOLUME ANOMALV-HO'

SAD DYN. M.

X 10=

SOUND VELOCITY

0; ml/l

PO4-P

rOTAL-P vg - ol/l

N03-N

US • Qt/I

N03-N

vg - ol/l

SI04-S<

pg - ol/l

pH

S

c c

STD

0000

0551

3426

2705

0010220

0000

14721

027

OBS STD STD

0000 0551 3*255 2705 1*721 0010 0*95 3*29 271* 0009361 0010 1*701 0020 0**7 3*32 2722 0008525 0019 1*682

027

OBS STD STD STD STD STD

0025 0*26 3*335 2725 1*675 0030 0*20 3*35 2727 000813* 0027 1*573 0050 0*00 3*39 2732 0007652 00*3 1*569 0075 0381 3**6 27*0 0006961 0051 1*656 0100 0369 3*52 27*6 0005*1* 0078 1*666 0125 0365 3*60 2752 0005833 0093 1*669

027

OSS STD STD

0125 0365 3*595 2752 1*669 0150 0368 3*67 2758 0005321 0107 1*575 0200 0395 3*83 2758 000***1 0132 1*598

02

7

08

3

0200

03

96

34

8

31

27

6(

146

98

136

REFERENCE

SHIP CODE

LATITUDE

1/10

LONGITUDE

'I/IO

ii

MARSDEN

STATION

TIME

ORIGINATOR'S

DEPTH

MAX.

WAVE

W(A. THER CODE

CLOUD COOES

NODC

CItT

coot

ID. NO.

CRUISE NO.

STATION NUMBER

BOTTOM

OF S'MPL-S

NUMBER

10*

V

MO

DAV

MH.1/10

Oil. |HGTJrE*| SEA

HfE AM

31

540 EV

il

722

N

04452 W

149

74 05

20

048

1965

003

9364

0214

02

35

bbl

xo

0

0130

WATER

WIND

lADO- METER

Imbll

AIR TEMP.

•z

"-o?pVhs

SPECIAL OBSERVATIONS

COLOR CODt

'T,""

DIR.

fOtCt

DRT BULB

WET BULB

31

506

247

050

044

6

[05

MtSSENCI j HR 1/10

c»si

NO.

CARD TTPE

DEPTH (ml

I -c

S ■''..

SIGMA-T

S«C1FIC VOLUMf

SAD

DVN. M.

X 10=

SOUND VELOCITY

Oj ml/I

PO*-P

Vfl - Ol/I

TOTAL-f ue - Qi/l

NOj-N

ufi - or/I

NOj-N

PB ■ at/I

S10^-Si

we - Ol/I

pH

S

c c

STD

0000

0536

3430

2710

0009727

0000

14716

048 048

OBS STD STD

0000 0536 34299 2710 0010 0482 3433 2719 0020 0442 3435 2725 0025 0427 34361 2727 0030 0422 3437 2728 0050 0407 3438 2731

0008910 0008348

0008041 0007789

14716 0009 14695 0018 14681

14675 0026 14674 0042 14671

048

OBS

0051 0406 34382 2731

14671

STD STD

0075 0395 3440 2734 0100 0384 3444 2738

0007551 0007161

0061 14671 0080 14671

048

OBS STD STD

0102 0383 34441 2738 0125 0386 3450 2742 0150 0390 3459 2749

0006758 0006141

14671 0097 14677 0113 14684

048

OBS

0177

0394

34705

2758

14691

REFERENCE	SHIP CODE	LATITUDE 1/10	LONGITUDE * '1/10	Ii	MARSDEN	STATION	Tl	«^E			ORIGINATOR'S	DEPTH	MAX. DEPTH OF S-MPL*		WAVE		WEA- THER CODE	CLOUD CODES			NODC
CUT CODE	ID. NO.				CRUISE NO.	STATION NUMBER	BOTTOM	°''		NUMBER
10*	r	MO	DAY	MR.1/10	OIA	HGll Ptt SEA	irPE *M
31	liO	FV	4	623	N	n4Sii w		149	65	15	?fl	lOft	1965	001	9365	?05B	12	34	6l	XI	4 2	0131
			WATER	WIND	BARO- METER (mbt)	AIR TEMP,	•c	VIS, COO	NO. OBS, DEPTHS	SPECIAL OBSERVAHONS
	COLOR CODE	'»"'■	DIR.	SPEED 0» FOKCl	DRt BULB	WET BULB
				01	510	274	089	072	3	09
	MESSENGI 1 TIME o. HR 1/10	CAST NO.	CARD TTPE	DEPTH Iml	I ic	s •/..	SIGMA-T	S«CltlC VOLUME *nOmah->10'	SAD DVN. M. > I0>	SOUND VELOCITY	Oj ml/l	PO4-P VS - Ol/I	fOTAl-P	NOj-N ug - Ol/I	NOj-N V9 ■ Ol/I	SlO^-Si wg - Ol/I	pH	S C c
			STO	0000	0571	3440	2713	0009396	0000	14731
108		OBS	0000 0571 34397 2713		14731
		STD	0010 0518 3442 2722	0008629	0009 14712
		STD	0020 0472 3444 2729	0007988	0017 14694
		STD	0030 0433 3446 2735	0007424	0025 14680
108		OBS	0030 0433 34462 2735		14680
		STD	0050 0423 3452 2740	0006906	0039 14680
		STD	0075 0412 3459 2747	0006293	0056 14680
		STD	0100 0403 3465 2753	0005775	0071 14682
		STD	0125 0396 3470 2757	0005352	0085 14683
108		OBS	0128 0395 34707 2758		14684
		STD	0150 0394 3473 2760	0005128	0098 14687
		STD	0200 0391 3479 2765	0004694	0123 14695
		STD	0250 0388 3483 2769	0004410	0145 14702
108		OBS	T0262 0387 34842 2770		14704
		STD	0300 0395 3486 2771	0004276	0167 14714
		STD	0400 0415 3492 2773	0004149	0209 14740
108		OBS	0411 0417 34929 2773		14743
		STO	0500 0391 3491 2775	0004082	0250 14746
		STD	0600 0371 3490 2776	0004028	0291 14754
108		OBS	T0635 0366 34897 2776		14758
		STD	0700 0365 3490 2776	0004079	0331 14768
		STD	0800 0363 3490 2776	0004143	0372 14784
108		OBS	0844 0362 34895 2776		14791
		STD	0900 0359 3490 2777	0004189	0414 14799
		STD	1000 0354 3489 2777	0004222	0456 14813
108		OBS	T1075 0352 34893 2777		14825
		STD	1100 0351 3489 2777	0004298	0499 14829
		10	8		OS	S	T116	J	0	350	3'	>8	9C		2-]	7	7						14(	J 39

137

REFERENCE	SHIP CODE	LATITUDE 1/10	LONGITUDE "1/10	ii	MARSDEN	STATION	Tl	WE			ORIGINATOR'S	DEPTH	MAX.		WAVE		WEA- THEft CODE	CLOUD CODES			NODC
CIRT CODE	ID. NO.				CRUISE NO.	STATION NUMBER	TO BOTTOM	OF VMPL'S			STATION NUMBER
10-	!■	MO	DAY	HR.I/10	0\K	HGI PER S!A	HPf *M
31	"140	EV	4	619	N	04550 W		149	55	15	20	138	1965	003	9366	0640	06	36	3 3	XI	0 3	0132
			WATER	WIND	BARO- METER tmbs)	AIR TEMP.	*c	^o=.d£s	SPECIAL OBSERVATIONS
	COLOR CODE	'»"'	Olft.	S»EEO OR FORCE	DRY auLa	WET BULB
				08	S07	281	072	061	8	08
	MESSENGR TIME 01 HR 1/1D	CAST NO.	CARD TYPE	DEPTH (ml	T -C	s •''„	SIGMA-T	SFEClfIC VOLUME *NOMALT-»IO'	SAD DYN. M. < 10=	SOUND VELOCITY	Oj ml/1	PO4-P ve - o'/i	lOTAl-P ug - oi/l	NO2-N ug • Qt/I	NO3-N	SI 0*-S. wg-ol/l	pH	S c c
			STD	0000	056Z	3409	2690	0011620	0000	1^723
138		OBS	0000 0552 34086 2690		14723
		STD	0010 0487 3409 2699	0010764	0011 14594
		STD	0020 0429 3411 2707	0010057	0022 14672
138		OBS	0020 0429 34105 2707		14672
		STD	0030 0435 3415 2710	0009710	0031 14677
		STD	0050 0446 3425 2716	0009169	0050 14686
		STD	0075 0460 3435 2723	0008591	0073 14597
138		OBS	0086 0466 34393 2725		14702
		STD	0100 0449 3442 2729	0007981	0093 14698
		STO	0125 0419 3449 2738	0007157	0112 14690
		STD	0150 0389 3457 2748	0005286	0129 14683
138		OBS	0152 0387 34582 2749		14683
		STD	0200 0469 3484 2751	0006158	0158 14728
138		OBS	T0218 0478 34887 2763		14735
		STD	0250 0437 3486 2766	0004710	0182 14723
138		OBS	T0289 0400 34845 2768		14714
		STD	0300 0397 3485 2769	0004405	0205 14715
		STD	0400 0375 3490 2775	0003892	0247 14723
138		OBS	T0406 0374 34905 2776		14723
		STD	0500 0360 3491 2777	0003777	0285 14733
		STD	0500 0353 3491 2778	0003773	0323 14747
		138		OBS	T0518	0352	34908		2778								147<i9

REFERENCE

SHIP CODE

LATITUDE

1/10

LONGITUDE

■1/10

ii

MARSDEN

STATION

Tl

^E

ORIGINATOR'S

DEPTH

MAX.

WAVE

WEA- THER CODE

CLOUD

CODES

NODC

CIRY

id.

NO.

CRUISE NO.

STATION NUMBER

TO BOTTOM

OF S'MPL-S

NUMBER

10-

r

MO

DAY

HH.l/10

DIP.

M&i n» w

HP( *M

31

540

FV

4

619

N

04635 W

1A9

66

:>'>

?0

173

1965

003

9367

933

09

01

6 4

XI

4 2

0133

WATER

WIND

BARO- METER (mbt)

AIR TEMP. "C

VIS.

coo

NO.

OBS. DEPTHS

SPECIAL

OBSERVATIONS

COLOR CODE

TR*NS.

DIR.

SPEtD fOBCf

DRY BULB

WET

BULB

36

S06

257

09A

072

8

09

MESSENGR

TIME e

HR 1/10

CAST NO.

CARD TYPE

DEPTH (ml

T t

s •/..

SIGMA-T

SPECIfIC VOLUME ANOMALr-IlD'

SAO DYN. M.

X 10'

SOUND VELOCITY

Oj m\/i

PO«-P

lOIAL-P 1.9 - Ol/I

NOj-N U9 - ol/l

NO3-N pg - ot/1

SIO4-S1 pg - Ql/l

pH

S

c

STO

0000

0603

3A19

2693

0011318

0000

1^741

173

OBS STO STO STD STD STD STD

0000 0603 34191 2693 14741 0010 0572 3424 2701 0010596 0011 14731 0020 0542 3429 2709 0009887 0021 14721 0030 0515 3434 2716 0009219 0031 14712 0050 0454 3444 2729 0007935 0048 14696 0075 0410 3454 2743 0006648 0066 14679 0100 0367 3463 2755 0005568 0081 14666

173

OBS STD STD STD STD STD

0103 0362 34639 2756 14665 0125 0366 3468 2759 0005206 0095 14671 0150 0371 3472 2752 0004973 0108 14577 0200 0380 3479 2766 0004587 0131 14590 0250 0390 3486 2770 0004279 0154 14703 0300 0399 3489 2772 0004126 0175 14716

173

OBS STD STD

0305 0400 34893 2772 14718 0400 0398 3492 2775 0003989 0215 14733 0500 0390 3492 2775 0003996 0255 14745

173

OBS

T0509 0389 34923 2776 14747

173

OBS STD

0549 0384 34916 2776 14751 0500 0375 3492 2777 0003953 0295 14756

173

OBS

STD

T0666 0368 34916 2777 14764 0700 0358 3491 2777 0003979 0335 14770

173

OBS STD

0732 0358 34912 2777 14775 0800 0366 3491 2777 0004055 0375 14785

173

OBS STD

T0834 0365 34911 2777 14791 0900 036.? 3491 2778 0004098 0415 14800

17

3

OB

S

T0915

0

i6i

3A

9

12

27

7

3

i4e

02

1.38

REFERENCE

SHtP CODE

LATITUDE

i/lo

LONGITUDE

"l/IO

^.

MARSDEN

STATION

Tl

WE

ORIGINATOR'S

DEPTH

MAX

■

WAVE

WEA- THER CODE

CLOUD COOES

ODC

CIIY CODE

10. NO.

SS

CRUISE NO.

STATION

NUMBER

aOTTOM

OE S'MPL'S

STATION NUMBER

10'

r

MO

DAT

MH.1/10

OIR.

HCllPiP S£*

lift *w

31

Sid

EV

•>

619

N

OtibiZ W

1*9

66

D5

20

193

1965

003

9368

280

08

3*

2I2

XI

* 2

013*

WATER

WIND

BARO- METER

(mbil

AlH TEMP.

■c

VIS coo

NO.

OBS.

DEPTHS

SPECIAL OBSERVATIONS

COLOR CODE

'""'■

DIR.

OR fORCi

DRY BULB

WET

BULB

12

S03

254

111

083

8

11

MESSENGR

Tiwf o! HR 1/10

CAST NO.

CARD TYRE

DEPTH (ml

T TC

s •/..

SIGMA-T

SPECIFIC VOLUME

ANOMALY-XIO'

SAD DTN. M.

< loJ

SOUND VELOCITY

Oj ml/I

PO4-P

TOTAl-p

va - oi/i

NO3-N

WB - oi/l

NO,-N pg - ol/l

SI04-Si VB - al/l

PH

S C

c

STD

0000

0*65

3*09

2701

0010558

0000

1*683

193

OBS

0000 0*65 3A085 2701

1*683

STD

0010 0*04 341A 2712 0009535

0010 1*660

STD

0020 0357 3*20 2722 00086*3

0019 1*6*3

STD

0030 0325 3*26 2729 0007906

0027 1*632

STD

0050 0301 3*37 27*1 0006862

00*2 1*626

193

OBS

0050 0301 3*372 27*1

1*626

STD

0075 0350 3*51 27*6 000632*

0059 1*653

193

OBS

0075 0350 3*505 27*6

1*653

STD

0100 0352 3*53 27*8 0006179

007* 1*659

STD

0125 0355 3*58 2752 00058**

0089 1*66*

STD

0150 0357 3*63 2756 0005512

010* 1*670

193

OBS

0175 0359 3*708 2762

1*675

STD

0200 0*39 3486 2766 0004679

0129 1*716

193

OBS

0230 0*59 34922 2768

1*730

STD

0250 0*20 3*87 2768 000**51

0152 1*716

193

OBS

T0255 0*12 34865 2769

1*71*

STD

0300 0405 3487 2770 0004340

017* 1*718

STD

0400 0390 3489 2773 0004141

0216 1*729

193

OBS

0400 0390 34888 2773

1*729

STD

0500 0375 3*89 277* 000*072

0257 14739

193

OBS

T054* 0371 3*888 2775

1*7*5

STD

0600 0369 3*90 2776 000*006

0298 1*753

193

OBS

T0666 0366 3*90* 2777

1*763

STD

0700 0352 3*90 2777 0003986

0338 1*767

193

OBS

T0798 0355 3*902 2778

14780

STD

0800 0355 3*90 2777 000*023

0378 1*781

193

OBS

0835

0355

3*900

2777

14786

LONGITUDE

STATION TIME

DAY HR.1/10

ORIGINATOR'S

OBSERVATIONS

NODC STATION NUMBER

31 5*0 EV 4617 N 0*714 W

1*9 57 05 20 21* 1965 00319369

BARO- METER

2*7

3**a I 0* I 31 g

0 1

0135

M'jS^'I'iRj.CAST

HR 1/

NO3-N

ug • ai/l

21* 21*

214 21* 214

21*

21* 21*

STD

OBS

OBS STD STD

OBS STD

OBS STD STD

OBS STD STD STD STD

OBS STD

OBS

0000

0000 0009 0010 0020 0023 0030 00*7 0050 0061 0075 0100 0104 0125 0150 0200 0250

T0286 0300

T0383

0239

0239 0113 0106 00*8 003* 0016 -0012 -0015 -0018 003* 0116 0128 0160 0195 0256 030* 0332 03*1 0375

3295 32954

33079

3308

3313

33150

3321

33325

3333

33381

3356

3386

33900

3402

3415

3*38

3456

34654

3469

34791

2633 2633 2552 2552 2660 2662 2668 2578 2579 2683 2695 2714 2717 2724 2732 2745 2755 2760 2752 2767

0015203 0014500

001114* 00093*5

0008437 0007721 0006505 0005612

0000

0016 0031

0013729 00*5

001256* 0071

0101 0127

0149 0169 0206 0235

0005030 0262

1*572 14572 1*519 1*516 1**92 1**87 1**80 1**72 1**71 1**72 1*501 1*5*6 1*553 14572 1*593 14632 14663 14582 14589 1*718

139

31 540 EV 4619 N 04731 W

LONGITUDf

■1/10

ORIGINATOR'S

149 67 05 20 229 1965 003 9370

SPEtO

OH FOIICt

BARO- METER (mbil

AIR TEMP, "C

050 8

J12_

OBSERVATIONS

Gri FfR St A

03 B |4

WEA- THER CODE

0136

SPICITIC VOLUME

SAO OYN. M,

NO]-N Vi - 01/1

229

229 229 229 229 229

STD OBS

STD

STD OBS

STD

STD OBS

0000 0000 0010 0020 0025 0030 0050 0062 0075 0088 0100 0114 0125 0129 0150 0165

0280

0138

0030

-0018

-0022

-0039

-0050

0029

0070

0042

0037

0059

0066

0077

0085

3298

32975

3302

3307

33091

3310

3317

33209

3335

33452

3348

33548

3364

33666

3376

33777

2631 2631 2645 2655 2650 2561 2667 2671 2678 2684 2688 2594 2700 2702 2709 2709

0017211

00158 00148

55 57

00143 00137

68 82

0000

0017 0032

0047 0075

0012717 0108

0011792 0138

0010558 0156

0009862 0192

14590 14590 14530 14483 14462 14452 14458 14455 14496 14518 14508 14508 14522 14525 14535 14542

i

REFERENCE

SHIP CODE

latitude

1/10

if

MARSDEN

STATION

TIME

ORIGINATOR'S

DEPTH

MAX

•,

WAVE

WEA- THER CODE

CLOUD COOES

CTRY CODE

10. NO.

* "1/10

CRUISE NO.

STATION NUMBER

TO BOTTOM

OF S'MPL-S

STATION

NUMBER

10'

r

MO

DAY

HR.V10

OIK.

HGI PER S£*

T»Pt *W

31

540

FV

4619

N

04745 W

149

67

^5

?.o

239

1965

003

9371 }146

01

03

3 4

XI

4 3

0137

WATER

WIND

BARO- MEIEtt Imbil

AIR TEMP. X

COD

NO.

OBS.

DEPTHS

SPECIAL OBSERVATIONS

COLOR CODE

TkANS.

DIR.

into

OR FOKCE

DRY BULB

WEI BULB

09

S12

247

050

044

8

04

""SEMOrIcaST ""■ '■' NO.

HR 1/10

CARD TYPE

DEPTH Iml

T -C

1

S ■''..

SIGMA-T

SPtClfiC VOLUMf ANOM*LY-»10'

SAD

OYN. M.

X 10^

SOUND

VELOCITY

Ol ml/I

PO4-P

roTAL-p

wg-o'/l

NO:-N

ws - ol/l

NOa-N k.g - ol/l

SI04-S> 1.9.01/1

pH

S

c c

STD

0000 1 0225

3284

2625

0017788

0000

14564

239

OBS 0000 0225 32843 2625 14554 STD 0010 0118 3285 2633 0017025 0017 14518

239

OBS 0012 0099 32852 2534 14510 STD 0020 0052 3289 2640 0016351 0034 14491 STD 0030 0001 3295 2547 0015643 0050 14470 STD 0050 -0069 3306 2559 0014508 0080 14442

239

OBS 0060 -0089 33119 2665 14435 STD 0075 -0062 3321 2571 0013374 0115 14452 STD 0100 -0018 3338 2683 0012255 0147 14479 STD 0125 0027 3357 2595 0011054 0175 14505

23"

}

OB,

3

0125

oc

27

33

5

66

26

9f

14506

REFERENCE

SHIP CODE

LATITUDE

1/10

Si

MAR5DEN

STATION

Tl

WE

ORIGINATOR'S

DEPTH

MAI

.

WAVE

WEA- THER CODE

CLOUD

CODES

■^ooc

CTIT

cool

10.

NO.

LONGITUDE ■ -1/10

YEAR

CRUISE

NO.

STATION

NUMBER

TO BOTTOM

OF S'MPL'S

STATION

NUMBER

10"

1*

MO

DAY

HR.1/10

DIR.

HCI P(« 5[A

Uft AM

31

540

EV

4619

N

04800 W

149

68

35

21

010

1965

003

9372

3119

01

05

2 4

xo

X 0

0138

WATER

WIND

BARO-

METER

(mb»l

AIR TEMP. TC

VIS.

COD

NO.

oes.

DEPTHS

SPECIAL OBSERVATIONS

COLOR CODE

TRANS.

DIR-

SPftD

OR FORCt

DRY BULB

WET

eULB

09

SIO

247

050

044

8

04

HR 1/10 T

CARD

TYPE

DEPTH (ml

T "C

s •/..

SIGMA-T

SPECIFIC VOlUMt

ANOMAIY-XIO'

SAD

DYN. M. X 10^

SOUND VELOCITY

Ol ml/l

PO4-F'

vg • ol/l

TOTAL-P 1,9. 81/1

NOj-N

vs - o'/l

NO3-N

SI04-Si US . ol/t

pH

S

c c

STD

0000

0306

3295

2627

0017628

0000 14601

010

OBS 0000 0305 32948 2627 14601 STD 0010 0200 3300 2639 0016421 0017 14557 STD 0020 0117 3305 2549 0015497 0033 14522

010

OBS 0025 0083 33068 2653 14508 STD 0030 0065 3307 2554 0015046 0048 14501 STD 0050 0014 3314 2662 0014248 0078 14482

010

OBS 0059 0002 33186 2665 14478 STD 0075 0012 3330 2575 0013012 0112 14487

01

5

OB

3

0098

OC

26

33

5

35

26

9:

145

01

140

REFfBENCE

SHIP CODE

LATITUDE

1/10

LO

GITUOE ■1/10

n

MARSDEN

STATION

TIME

ORIGINATOR'S

DEPTH

MAX.

WAVE

WEA- THER CODE

CLOUD CODES

NODC

CTIT CODE

ro.

NO.

CRUISE NO.

STATION NUMBER

BOTTOM

OF S'MPL'S

NUMBER

10'

T

MO

DAY

HR.I/10

Ol«.

MCI PE« SEA

lYPt »M

31

«>4n

EV

*531

N

04908 W

149

59 05

21

072

1965

003

9373 3070

no

13

2 2

X4

7 8

0139

WATER

WIND

BARO- METER (mbi)

AIR TEMP. "C

VIS. COD

S?s "E^'*^

ofpTHS OBSERVATIONS

COLOR CODE

TRANS.

DIR.

SPEED

fORCE

DRY BULB

WET

BULB

12

S17

166

057

056

1

04

MtSSEHGB CAST

IIME 0 fjo HR 1/10

CARD TYPE

DEPTH Iml

T -C

S 'I.

SIGMA-T

SPECIflC VOLUME ANOMALT-XIO'

SAD

DYN. M. X 10^

SOUND VELOCITY

Oj ml/1

PO4-P

TOTAL-P

NO,-N ug - ol/l

NO3-N vg - ot/l

S10*-Si tig • Ql/I

pH

S

c c

STD

0000

0254

3293

2629

0017385

0000

14578

072

OBS

0000 025^ 32925 2629 1*578

STD

0010 0093 3295 2643 0016117 0017 14508

STD

0020 0011 3297 2649 0015516 0033 14473

072

OBS

0020 0011 32973 2649 14473

STD

0030 0009 3300 2651 0015298 0048 14474

072

OBS

0030 0009 33000 2651 14474

STD

0050 0071 3310 2655 0014887 0078 14507

072

OBS

0050

0071

33095

2655

14507

REFERENCE

SHIP

CODE

LATITUDE

I/IO

°z

MARSDEN

STATION

Tl

WE

ORIGINATOR'S

DEPTH

MAX.

DEPTH

OF S'MPL-S

WAVE

WEA- THER CODE

CLOUD

slODC

CIIY CODE

10.

NO.

LONGITUDE ' 'I/ID

CRUISE NO.

STATION NUMBER

BOTTOM

STATION NUMBER

10"

r

MO

DAY

HR.l/lO

DIB.

MCI PEP St»

tVPt AM

31

S4n

FV

4530

N

04846 W

149

58

^S

21

098

1965

003

9374 D134

13

2 2

X4

7 8

0140

WATER

WIND

AIR TEMP. "C

VIS.

COD

NO. OBS. DEPTHS

SPECIAL OBSERVATIONS

COLOR CODE

IftANS.

DIR.

SPEED FO»CE

METER

(mbll

DRY BULB

WET BULB

13

S18

152

061

1

04

MESSEMGR 1 CAST HR 1/10

CARD TYPE

DEPTH Im)

I *c

s v..

SIGMA-T

SPECifiC VOLUME

*NOMAL<-I10'

SAD

DYN. M.

t 10'

SO^'^O 03 ml/I VELOCITY "'

PO*-P

Vi ■ 91/1

lOTAL-P vg -ol/l

NO3-N

ug - ot/l

NO3-N

ug - ol/l

SI 04-si

k>g - ol/l

pH

S

c c

STD

0000

0215

3290

2630

0017322

0000

14560

098

OBS 0000 0215 32895 2630 14560

STD 0010 0144 3292 2637 0016663 0017 14531

STD 0020 0084 3295 2643 0016066 0033 14506

098

OBS 0020 0084 32950 2643 14506

STD 0030 0044 3300 2649 0015469 0049 14490

STD 0050 -0015 3309 2659 0014496 0079 14468

098

OBS 0065 -0041 33152 2666 14459

STD 0075 -0036 3320 2669 0013555 0114 14464

STD 0100 -0025 3330 2677 0012833 0147 14474

09

i

OB

3

0115

-OC

)18

33

3

65

26

8*

14481

REFERENCE	SHIP CODE	LATITUDE 1/10	LONGITUDE sH ■ -l/io"^	MARSDEN	STATION	Tl	WE			ORIGINATOR'S	DEPTH			WAVE		WEA- THER CODE	CLOUD CODES			NODC
CTST CODE	ID. NO.				CRUISE NO.	STATION NUMBER	BOTTOM	OF S'MPl-S		NUMBER
10-	r	MO	DAY	HR.1/10	DIIL	MGt PH SEA	Il-PE AM
31	540	EV	4	530	N	n4f	)32 W 1	149	58	15	?1	1 13	1965	003	9375	183	02	13	2 2	X4	7 8	0141
			WATER	WIND		- R	AIR TEMP.	■c	VIS, coo	NO. OBS. DEPTHS	SPECIAL OBSERVATIONS
	COLOR CODE	IRANS.	OIR-	SPEED OB fOPCE	METE Imbi	DRY BULB	WET BULB
			14	S18	146	072	072	1	06
	MESSENGR TIME □ HR 1/10	CAST NO.	CARD TYPE	DEPTH Iml	T 1:	s •'..	SIGMA-T	SPECIFIC VOLUME ANOMALT-llO'	SAD DYN. M, X 10'	SOUND VELOCITY	03 ml/1	PO4-P vg -ol/l	roT*i-p	NO3-N ug - ol/l	NOj-N iig - ol/l	SIO4-S. vg - ol/l	pH	S c c
			STD	0000	0185	3286	2629	0017400	0000	14547
	113		OBS	0000	0185 32857 2629		14547
			STD	0010	0181 3286 2630	0017336	0017 14547
	113		OBS	0010	0181 32862 2630		14547
			STD	0020	0046 3295 2645	0015863	0034 14489
	113		OBS	0025	-0003 32980 2650		14468
			STD	0030	-0021 3299 2652	0015241	0050 14460
	113		OBS	0049	-0060 33066 2659		14446
			STD	0050	-0058 3308 2660	0014396	0079 14448
			STD	0075	-0018 3336 2681	0012414	0113 14474
	113		OBS	0089	-0001 33471 2690		14486
			STO	0100	0003 3348 2690	0011569	0143 14490
			STD	0125	0013 3351 2692	0011407	0171 14499
			STO	0150	0022 3354 2694	0011247	0200 14508
		11	3		OB	5	0162	OC	)27	33	5	50		26	9								14^	12

141

REfEfiENCE

SHIP CODE

LATITUDE

1/10

LONGITUDE ' '1/10

11

MARSDEN

STATION

TIME

ORIGIN ATOIt'S

DEPTH

MAX. DEPTH

OF S'MPL'

WAVE

WEA- THER CODE

CLOUD CODES

OOC

CIRT CODE

ID.

NO.

CRUISE NO.

STATION NUMBER

TO

BOTTOM

STATION NUMBER

10-

r

MO

DAY

HR.I/10

018.

HC1 PER SEA

H« *M

31

San

EV

4

532

H

04822 W

149

58 05

21

1^1

1965

00^

9376

bft49

06

12

2 2

X4

9 8

nl4?

WATER

WIND

BAfiO. METER

(mbd

AIR TEMP.

•c

VIS, COD

NO.

OBS.

DEPTHS

SPECIAL OBSERVATIONS

COLOR CODE

TitANS.

OIR.

SPIED fOBCE

DRY BULB

WET

BULB

14

S18

132

078

1

08

ME55ENGR [

TIME 01

HR t/10

C»SI NO.

CARD TYPE

DEPTH (ml

r -c

s •''..

SIGMA-T

SPECIFIC VOLUME ANOMALT-XIO'

SAD

DYN. M.

K 10^

SOUND

VELOCITY

Ol tnl/l

PO4-P

t>S - o'/l

lOTAl-P

va - o'/i

NOj-N uO - at/I

NOs-N vg ■ 01/1

SIO«-Si PB.at/t

pH

s

c c

STD

0000

0264

3312

2644

0015994

0000

14585

131

OBS STD STD

0000 0264 33119 2644

0010 0255 3312 2645 0015916

0020 0245 3312 2645 0015846

14585 0016 14582 0032 14580

131

OBS

STD

0020 0245 33120 2645

0030 -0016 3315 2664 0014048

14580 0047 14465

131

OBS STD STD

0030 -0016 33149 2664

0050 0004 3337 2681 0012446

0075 0038 3363 2700 0010639

14465 0073 14480 0102 14504

131

OBS STD STD STD

0075 0038 33629 2700 0100 0103 3386 2715 0009262 0125 0159 3406 2727 0008127 0150 0208 3423 2737 0007217

14504 0127 14540 0149 14572 0168 14600

131

OBS STD STD

0165 0234 34324 2743

0200 0270 3444 2749 0006175

0250 0312 3458 2756 0005537

14615 0201 14638 0231 14667

131

OBS STD

T0297 0340 34676 2761 0300 0341 3468 2761 0005105

14688 0257 14689

131

OBS STD STD

T0379 0365 34761 2765 0400 0366 3478 2767 0004696 0500 0372 3483 2770 0004469

14713 0306 14717 0352 14737

131

OBS

T0595

0377

34839

2770

14755

LATITUDE

1/10

LONGITUDE

'1/10

DAY HR.1/10

ORIGINATOR'S

31 540 EV

4530 N

04813 W

149 |58 05 I2I 1151 11965 |003|9377

BARO- METER (mbil

AIR TEMP. IC

11

12 k.

0143

IR l/tO

SOUND VELOCITY

151 151 151

151

151 151

151

151 151

STD

OBS STD

OBS STD STD

OBS STD STD STD

OBS STD

OBS STD STD

OBS STD

OBS STD STD

OBS STD STD STD

OBS STD

OBS

0000 0000 0010 0015 0020 0025 0030 0060 0064 0075 0100 0125 0133 0150 0196 0200 0250

T0294 0300 0392 0400 0500 0591 0600 0700 0789 0800 0900 1000

T1012 1100

T1123

0492 0492 0479 0440 0359 0295 0306 0340 0351 0326 0285 0267 0265 0286 0330 0332 0354 0366 0366 0371 0372 0378 0380 0380 0377 0375 0375 0374 0371 0370 0364 0362

3386

33858

3405

34077

3402

33974

3401

3414

34211

3425

3433

3441

34434

3450

34551

3465

3472

34763

3477

34824

3483

3486

34880

3488

34888

3489

3488

34882

3488

34876

2680

2580 2697 2703 2707 2709 2711 2718 2723 2728 2739 2747 2749 2752 2750 2761 2763 2765 2766 2770 2770 2772 2773 2773 2774 2774 2774 2774 2774 2774 2775 2775

0012549

0010979

0010017

0009624 0008961

0008022 0007081 0006330

0005088 0004893

00C4383 0004313

0004276 0004303

0004339 0004437 0004510

0000

0012

0022

0032 00 51

0072 00 91 0108

0005832 0123

0150 0175

0004685 0199

0244 0288

0331 0374

0417 0461 0505

0004527 0551

14592 14592 14690 14575 14541 14614 14620 14540 14548 14539 14527 14524 14625 14638 14666 14668 14587 14599 14701 14719 14720 14740 14755 14758 14773 14787 14789 14805 14820 14822 14834 14837

142

RErERENCE	SHIP CODE	LATITUDE 1/10	LONGITUDE * '1/10	°z	MARSDEN	STATION	Tl	«			ORIGINATOR'S	DEPTH	MAK. DEPTH OF S'MPL-		WAVE		WEA- THER CODE	CLOUD COOES			NODC
C?tT CODE	ID. NO.				CRUISE NO.	STATION NUMBER	BOTTOM			NUMBER
10-	r	MO	DAY	HR.1/10	DIP.	HGt PER !E*	TYPE AM
31	^iCI	FV	1\|	530	N	04754 W		149	57	15	21	183	IQfiS	003	937B	1460	12	16	4 2	X4	X 8	0144
			WATER	WIND		- R 1	AIR TEMP.	■c	CODF 0"5- DEPTHS	SPECIAL OBSERVATIONS
	COLOR CODE	TRANS.	DIR.	into FO«ce	METE (mbi	DRY BULB	WET BULB
				16	S22	105	089	089	1	10
	MISSENG» TIME c HR I/IO	CAST NO.	CARD TYPE	DEPTH (ml	I ■c	s •/..	SIGMA-T	SPtClfIC VOLUME ANOM*f(-»10'	SAD DYN. M. I 10'	SOUND VELOCITY	03 ml/I	PO4-P VB-ol/l	lOTAL-P ve • 01/1	N0:-N vg - oi/l	NOi-N ^g - oi/l	SIO^-Sl ug - oi/l	PH	S C C
			STD	0000	0490	3398	2690	0011642	0000	14692
183		OBS	0000 0490 33976 2690		14692
		STD	0010 0480 3398 2691	0011500	0012 14690
		STD	0020 0437 3399 2696	0011025	0023 14674
183		OBS	0021 0431 33988 2697		14671
		STO	0030 0341 3402 2709	0009859	0033 14635
183		OBS	0037 0288 34048 2716		14614
		STD	0050 0283 3408 2719	0008908	0052 14614
		STD	0075 0273 3420 2729	0007932	0073 14616
183		OBS	0079 0271 34222 2731		14616
		STD	0100 0311 3441 2743	0006699	0091 14639
		STD	0125 0352 3462 2755	0005520	0107 14664
183		OBS	0131 0361 34660 2758		14669
		STD	0150 0362 3468 2759	0005189	0120 14673
		STO	0200 0365 3473 2763	0004887	0145 14683
		STD	0250 0368 3478 2767	0004587	0169 14693
		STD	0300 0372 3482 2769	0004365	0191 14704
		STD	0400 0378 3487 2773	0004146	0234 14723
183		OBS	T0419 0379 34880 2773		14727
		STD	0500 0371 3488 2774	0004066	0275 14737
		STD	0600 0365 3489 2775	0004059	0316 14751
183		OBS	T0630 0363 34888 2776		14755
		STD	0700 0362 3489 2776	0004091	0356 14767
		STD	0800 0360 3489 2776	0004153	0398 14782
183		OBS	0843 0359 34893 2776		14789
		STD	0900 0357 3489 2777	0004177	0439 14798
		STD	1000 0354 3490 2777	0004203	0481 14814
183		OBS	T1078 0352 34899 2778		14826
		STO	1100 0353 3490 2777	0004263	0523 14830
		183		OBS	T1152	0355	34896		2777								14839

SHIP CODE

LATITUDE

I/IO

LONGITUDE

* "l/lO

ORIGINATOR'S

GTl PER SE»

EV

04719 W

149 157 105 I2I 1214 11965 100319379

BARO- "l"> MEIER

Imbi)

14 S24 112

100

t?195 I 12 I 14 l4 12

0145

SPECIFIC VOLU

SOUND VELOCITY

SIO4-

pg - o

214

214 214 214 214

214

214 214

STD

OBS STD

OBS STD STO

OBS STD STD

OBS STD STD STD STD

OBS STO

OBS STD

OBS STO STO

OBS STO STD

OBS STD STD

OBS STD

OBS

0000 0000 0010 0016 0020 0030 0037 0050 0075 0077 0100 0125 0150 0200 0203 0250 0280 0300 0330 0400

T0407 0500 0600 0612 0700 0800 0815 0900 1000

T1042 1100

T1153

0601 0601 0613 0620 0601 0557 0531 0499 0450 0447 0449 0451 0453 0458 0458 0379 0378 0420 0460 0432 0430 0425 0416 0415 0399 0384 0382 0371 0362 0360 0359 0359

3392

33919

3397

34014

3407

3419

34254

3428

3434

34349

3447

3457

3466

3476

34761

3475

34734

3482

34907

3491

34906

3491

34913

3492

34922

3492

3491

34909

3491

34904

2672 2672

2574 2677 2684 2699

2707 2713 2723 2724 2733 2741 2748 2755 2756 2763 2762 2764 2767 2770 2770 2771 2772 2772 2775 2776 2776 2777 2778 2778 2777 2777

0013328

0013103

0012225 0010820

0009514 0008563

0007603 0006903 0005278 0005531

0004958

0004875

0004467

0004461 0004458

0004285 0004205

0004143 0004197

0000

00 13

0025 0037

0058 0080

0101 0119 0135 0165

0191

0216

0263

0307 0352

0396 0438

0480 0522

0004275 0564

14737 14737 14744 14748 14742 14728 14719 14708 14693 14592 14598 14705 14711 14722 14723 14597 14702 14724 14747 14747 14747 14760 14773 14775 14783 14793 14795 14804 14817 14823 14832 14841

143

31

540

SHIP CODE

EV

LATITUDE

1/10

4532 N

LONGITUDE

•1/10

04635 W

149 [56 [05 \22 |015 |l965 |003 9380

ORIGINATOR'S

119

AIR TEMP. "C

083

2963

12

0146

SOUND

VELOCITY

PO<-P

015

015 015

015

STO

OBS STD STD

OBS STD STO STO STD STD

OBS STD STD

OBS STD

OBS STO STD

OBS STD STD

OBS

0000 0000 0010 0020 0025 0030 0050 0073 0075 0100 0125 0150 0200 0202 0250 0300

T0302 0400 0403 0500 0600

T0604 0700 0800 0803 0900 1000

T1027 1100 1200

T1216

0672 0572 0589 0523 0497 0494 0483 0471 0470 0459 0448 0438 0416 0415 0436 0457 0458 0436 0435 0394 0364 0363 0352 0341 0341 0338 0336 0335 0333 0331 0331

3398 33982

3403

3406

34076

3408

34100

3411

3420

3428

3436

3450

34509

3464

3473

34736

3482

34817

3485

3487

34873

3489

3491

34910

3492

34925

3493

3494

34937

2668 2668 2682 2693 2697 2698 2699 2702 2703 2711 2718 2726 2739 2740 2748 2753 2754 2762 2762 2769 2774 2774 2777 2779 2780 2781 2781 2781 2782 2783 2783

0012368 0011395

0010937 0010839

0010501 0009737 0009046 0008357 0007128

0006340 0005956

0004562 0004175

0003977 0003803

0003765 0003822

0003791 0003801

0000

0013 0025

0036 0058

0085 0110 0133 0155 0194

0227 0258

0005191 0314

0363 0406

0447 0486

0524 0562

0500 0538

14766 14756

14735 14710 14701 14700 14699 14698 14598 14599 14700 14700 14701 14702 14720 14738 14739 14747 14747 14746 14751 14751 14763 14775 14775 14790 14805 14810 14822 14838 14B40

LATITUDE

1/10

STATION TIME

O DAY HR.l/I

ORIGINATOR'S

NODC STATION NUMBER

31 540 EV 4536 N 04504 W

149 156 105 122 048 11965

S14

0031 9381

BARO- METER

AIR TEMP. ^

083

3383 I 12 I 24 13 |3

0147

MISSENCR LcAST NO.

R 1/10

SI 04-Si

048

048 048 048 048 048 048

048 048

STD

OBS STO STO

OBS STD STD

OBS STO

OBS STD

OBS STD STD STD

OBS STD

OBS STD STD STD

OBS STO STD

OBS

0000

0000 0010 0020 0025 0030 0050 0050 0075 0100 0111 0125 0125 0150 0150 0200 0200 0250 0250 0300

T0311 0400 0500 0600 0601 0700 0796 0800 0900 1000 1021 1100 1200

T1200

0735 0735 0588 0560 0654 0567 0700 0700 0553 0526 0610 0672 0672 0584 0584 0427 0427 0418 0418 0444 0448 0429 0408 0386 0385 0385 0383 0382 0357 0358 0357 0358 0359 0359

3391

33905

3400

3409

34131

3415

3428

34283

3430

3445

34580

3477

34771

3473

34727

3455

34555

3474

34742

3483

34849

3487

3489

3491

34907

3493

34933

3493

3492

3491

34904

3491

3492

34920

2553 2553 2657 2678 2682 2582 2588 2688 2594 2711 2723 2730 2730 2738 2738 2743 2743 2758 2758 2763 2764 2767 2771 2775 2775 2777 2777 2777 2778 2778 2778 2778 2779 2779

0013820 0012804

0012386 0011928

0011358 0009732

0008041

0007286

0006826

0005387

0005063

0004725 0004437 0004144

0004086 0004097 0004173

0004232 0004255

0014 0028

0040 0055

0094 0120

0142

0162

0197

0227

0253

0302 0348 0391

0004046 0432

0473 0514 0555

0597 0639

14790 14790 14774 14755 14755 14771 14789 14789 14779 14771 14758 14797 14797 14755 14765 14707 14707 14714 14714 14734 14738 14745 14753 14761 14761 14777 14792 14792 14803 14615 14818 14832 14849 14849

144

REFERENCE	SHIP CODE	LATITUOE I/IO	LONGITUDE l/lO	ii	MARSDEN	STATION TIME			ORIGINATOR'S 1	DEPTH TO BOTTOM	MAX. DEPTH OF S'MPL-		WAVE		WEA- THER CODE	CLOUD CODES			h	00c
CUT coot	10. NO.				CRUISE NO.	STATION NUMBER			NUMBER
10-	T	MO	DAY HB.1/10	Dis.	HGI PE* SEA	TYPE AMI
31	540	EV	4	510	N	04548 W		1*9	55 05	22 D84	1965	003	9382	b	566	12	25	3 3	X2	6 8	0146
				WATER	WIND	BARO- METER (mbt)	AIR TEMP.	■^	VIS. COOi	NO. OBS. DEPTHS	SPECIAL OBSERVATIONS
	COLOR CODE	IWNS.	DIR.	SPIED 0« (Oiici	DRY BULB	WET BULB
			24	508	132	083	078	7	11
	MfttlNCI [ HR t/10	CAST NO.	CARD TTFE	DEPTH tmt	T 1C	s */„	SIGMA-T	SPECIFIC vOlUMt ANOMALT-llO'	SAD DYN. M X lo'	SOUND VELOCITY	Oj ml/l	P04-P	tOTAL-P vg ■ ol/l	NOl-N VS - oi/l	NOi-N HB - ol/l	SIO^-SJ vt - ol/l	,H C
			STD	0000	1310	3541	2671	0013451	0000	15017								1
	084		DBS STD STD	0000 1310 35408 2671 0010 1352 3552 2578 0012743 0020 1380 3577 2684 0012228	15017 0013 15035 0026 15048
	084		OBS STD STD	0025 1390 35833 2587 0030 1385 3583 2588 0011938 0050 1365 3579 2589 0011859	15053 0038 15052 0051 15048
	084		OBS STD STD STD STD	0052 1351 35771 2690 0075 1331 3573 2592 0011679 0100 1293 3565 2694 0011521 0125 1254 3559 2696 0011373 0150 1215 3552 2698 0011244	15045 0091 15041 0120 15031 0149 15021 0177 15011
	084		OBS	0155 1208 35505 259B	15009
	084		OBS STD STD	0186 1279 35718 2701 0200 1226 3561 2703 0010908 0250 1059 3530 2710 0010286	15041 0232 15024 0285 14970
	084		OBS STD STD	T0285 0961 35150 2715 0300 0931 3514 2720 0009429 0400 0759 3505 2740 0007558	14938 0334 14930 0419 14880
	084		OBS STD STD	T0414 0739 35053 2743 0500 0643 3504 2755 0006224 0600 0556 3503 2755 0005315	14874 0488 14851 0545 14832
	084		OBS STD STD	0621 0541 35022 2766 0700 0507 3502 2770 0004849 0800 0468 3501 2774 0004547	14830 0597 14829 0644 14829
	084		OBS STD STD	0828 0458 35005 2775 0900 0433 3498 2776 0004441 1000 0405 3495 2776 0004417	14830 0689 14831 0733 14836
	084		OBS STD STD	T1055 0393 34943 2777 1100 0385 3494 2778 0004338 1200 0374 3493 2778 0004365	14840 0777 14844 0820 14855
	084		OBS	T1241 0372 34924 2778	14852
REFERENCE	SHIF CODE		LATITU	DE l/IO	LONGITUDE s^ • -1/10 -	MARSDEN SQUARE	STATION TIME IGMTJ	TEAR	ORIGINATOR'S 1	DEPTH TO BOTTOM	MAX DEPTH OF S'MPL-	WAVE OBSERVATIONS	WEA- THER CODE	CLOUD CODES	j NOOC
CUT CODE	10. NO.	CRUISE NO.	STATION NUMBER		NUMBER
10-	r	MO	DAY M	R.1/10	S DIP-	HGt PES Sf*	IIPl AM
31	540	EV	4	442	N	04600 W	149	46	■)5	?? 1	IR	1965	003	9383	658	11	24	3 2	X2	6 8	0149
				WATER	WIND	BAOO- METER (mbt)	AIR TEMP.	■c	VIS. CODE	NO. OBS. DEPTHS	SPECIAL OBSERVATIONS
	COLOR CODE	TftANS.	DIR.	SPEED 0» fOKCE	DRt BULB	WET BULB
			24	SO 9	152	083	072	7	12
	MfSi(NC« tiME o. HR 1/10	CAST NO.	CARD TYPE	DEPTH Im)	T r	s •/„	SIGMA-T	SPECIHC VOLUME ANOMALt-HO'	SAD DYN. M > Id'	SOUND VELOCITY	Oj m1/l		TOTAl_P 1,9 - al/l	NO2-N	NOi-N PB - o'/l	SIO«-Si MS - ot/l	PH	5 ;
			STD	0000	1005	3445	2653	0015126	0000	14899
	118		OBS STD	0000 1005 34445 2653 0010 1073 3463 2656 0014909	14899 0015 14927
	118		OBS STD	0015 1107 34727 2557 0020 1041 3484 2678 0012844	14941 0029 14920
	118		OBS STD STD STD	0024 0995 34919 2592 0030 0994 3493 2592 0011457 0050 0991 3495 2594 0011315 0075 0988 3497 2597 0011120	14905 0041 14905 0054 14908 0092 14911
	118		OBS STD STD STD STD	0080 0987 34976 2597 0100 0925 3493 2704 0010450 0125 0858 3488 2711 0009875 0150 0803 3482 2715 0009506 0200 0731 3472 2717 0009375	14912 0119 14892 0144 14870 0158 14853 0216 14832
	118		OBS STD	0209 0723 34695 2717 0250 0724 3486 2730 0008278	14830 0250 14839
	118		OBS STD	0291 0724 34904 2733 0300 0685 3485 2734 0007914	14846 0300 14832
	118		OBS	0349 0575 34759 2742	14795
	118		OBS STD STD	T03B4 0592 34903 2751 0400 0589 3492 2752 0006258 0500 0573 3501 2762 0005509	14809 0371 14811 0430 14822
	118		OBS STD STD	0580 0559 35036 2765 0500 0541 3502 2755 0005159 0700 0468 3498 2772 0004660	14830 0483 14825 0532 14812
	118		OBS STD STD	0778 0430 34952 2775 0800 0425 3495 2775 0004381 0900 0415 3497 2777 0004310	14809 0578 14811 0521 14823
	118		OBS STD	T0995 0411 34973 2777 1000 0411 3497 2778 0004315	14838 0564 14838
		11	8		OB	S	T1058	0	412	3	4«	>94	2	^7	9						14	349

145

REFERENCE

SHIP CODE

LATITUDE

1/10

LONGITUDE

'1/10

°z

MARSDEN

STATION

TIME

ORIGINATOR'S

DEPTH

MAX

■

WAVE

WEA- THER CODE

CLOUD CODES

gODC

CTRY

coot

10. NO.

YEAR

CRUISE

NO.

STATION NUMBER

TO

BOTTOM

Of S'MPL-S

STATION NUMBER

10*

1*

MO

DAY

HH.I/10

Dl>,

HGI H» SEA

IY»( AM

31

540

FV

4

410

N

04603 W

149

46

■)-,

22

156

196 5_

003

9384 3931

12

04

3 2

X?

6 8

nl5n

WATER

WIND

BARO- METER

(mbll

AIR TEMP. X. j

NO. OBS. DEPTHS

SPECIAL OBSERVATIONS

COLOR CODE

'Vn!;^-

DIR.

SfEtO

OR FOaCt

DRY BULB

WET COD BULB

22

S08

156

106

089 8

11

MESSENCR TIME a

HR 1/10

CAST NO.

CARD

TYPE

DEPTH Im)

T -C

s •/„

SIGMA-T

SMClfiC VOLUME ANOMAL»->10'

SAD

DYN. M. t 10^

SOUND VELOCITY

Ol ml/I

PO4-P

lOTAL-f

ue ■ oi/i

NO3-N

ui - a\/\

NO3-N

llfl- Ol/I

SlOi-Si

wa - oi/i

pH

S

c

STD

0000

1040

3A74

2670

0013521

0000

14915

156

OBS

0000 1040 34740 2670 14915

STD

0010 0992 3478 2681 0012460 0013 14900

STD

0020 0958 3482 2690 0011641 0025 14890

STD

0030 0938 3486 2697 0011050 0036 14884

156

OBS

0032 0936 34870 2698 14884

STD

0050 0982 3498 2699 0010906 0058 14905

156

OBS

0073 1010 35084 2702 14921

STD

0075 1000 3507 2703 0010590 0085 14917

STD

0100 0884 3497 2714 0009540 0110 14877

STD

0125 0790 3489 2722 0008783 0133 14845

STD

0150 0718 3484 2729 0008185 0154 14820

156

OBS

0185 0656 34828 2737 14801

STD

0200 0655 3487 2740 0007195 0193 14804

STD

0250 0655 3496 2747 0006602 0227 14813

156

OBS

0253 0655 34966 2747 14814

156

OBS

T0291 0621 34980 2753 14807

STD

0300 0612 3498 2754 0005964 0259 14805

STD

0400 0535 3498 2764 0005113 0314 14790

156

OBS

0422 0522 34982 2766 14788

STD

0500 0507 3500 2769 0004773 0364 14795

STD

0600 0486 3502 2773 0004478 0410 14804

156

OBS

T0633 0478 35026 2774 14806

STD

0700 0456 3501 2775 0004291 0454 14808

STD

0800 0429 3499 2777 0004217 0496 14813

156

OBS

T0842 0420 34981 2777 14816

STD

0900 0411 3498 2778 0004173 0538 14822

STD

1000 0398 3497 2779 0004184 0580 14833

156

OBS

1070 0390 34964 2779 14841

STD

1100 0387 3496 2779 0004215 0622 14845

156

OBS

T1183

0380

34956

2779

14856

REFERENCE

SHIP CODE

LATITUDE

1/10

LONGITUDE ' '1/10

ii

MARSDEN

STATION

Tl

WE

ORIGINATOR'S [

DEPTH

MAX

-

WAVE

WEA- THER CODE

CLOUD COOES

^ODC

CI«Y

CODE

ID.

NO.

YEAH

CRUISE NO.

STATION

TO

OF S'MPL'S

STATION NUMBER

10-

r

MO

DAY

HH.VIO

NUMBER ow.iv/™.

OIR.

HGI PER SEA

TVPf AW

31

540

EV

4

1410

N

04636 W

149

46

35

22

185

1965

003

9385 3931

12

23

3 2

X?

6 8

0151

WATER

WIND

BARO- METER

(mbtl

AIR TEMP. X

VIS. CODE

NO.

OBS.

DEPTHS

SPECIAL OBSERVATIONS

COLOR

CODE

IRANS.

I<n)

DIR.

SPEED

OR fORCE

DRY BULB

WET BULB

23

SIO

159

083 072

8

09

MESSENGR

TIMt a

HR l/lo'

CAST NO.

CARD TYPE

DEPTH Iml

T -C

s •''..

SIGMA-T 'ZoLl?"^^'^'

SAD

DYN. M.

X 10^

SOUND VELOCITY

Ol ml/l

PO^-P

lOIAL-P

NO2-N

ug - 01..' 1

NOj-N ug - ol/l

SIO^-Si vi ■ oi/l

pH

s c

c

STD

0000

0799

3391

2644 0015995 0000

14815

185

OBS STD STD

0000 0799 33907 2644 14815 0010 0908 3442 2667 0013803 0015 14864 0020 0999 3485 2686 0012056 0028 14905

185

OBS STD STD STD STD

0020 0999 34853 2686 14905 0030 0993 3488 2689 0011789 0040 14905 0050 0981 3493 2695 0011251 0063 14904 0075 0967 3500 2703 0010580 0090 14904 0100 0952 3506 2710 0009910 0116 14904

185

OBS STD STD

0122 0939 35122 2717 14903 0125 0925 3510 2718 0009267 0140 14898 0150 0819 3498 2725 0008584 0162 14861

185

OBS STD STD STD STD

0189 0684 34823 2732 14813 0200 0681 3484 2734 0007801 0203 14814 0250 0666 3489 2740 0007254 0241 14817 0300 0648 3495 2747 0006674 0275 14819 0400 0600 3506 2762 0005350 0336 14817

185

OBS STD STD

T0408 0596 35070 2763 14817 0500 0520 3502 2769 0004770 0386 14801 0600 0460 3498 2773 0004453 0432 14792

185

OBS STD STD

T0612 0454 34976 2773 14792 0700 0431 3496 2774 0004362 0476 14797 0800 0411 3495 2776 0004299 0520 14805

185

OBS STD STD

0816 0408 34949 2776 14806 0900 0401 3495 2777 0004275 0562 14817 1000 0392 3495 2778 0004259 0605 14830

185

OBS

STD

T1041 0389 34952 2778 14836 1100 0384 3495 2778 0004252 0648 14843

18

5

OB

5

T1184

0:

77

34

9

39

27

li

J

148

54

146

REFERENCE

SHIP CODE

LATITUDE

1/10

LONGITUDE

* -1/10

°z

MARSDEN

STATION TIME

ORIGINATOR'S

DEPTH

MAX.

DEPTH

OF S-MPL'

WAVE

WEA- THER CODE

CLOUD CODES

NODC

CTt* CODE

ro.

NO.

CRUISE NO.

STATION NUMBER

BOTTOM

NUMBER

10*

r

MO

DAT HR.I/10

DIB.

KCT f[« it*

r»PE AM

31

s*n

EV

*

*16

N

0*715 W

149

*7

15

22 218

196i

003

9386

1*023

11

?1

5 4

X?

5 8

0152

WATER

WIND

BARO- METER (mbll

AIR TEMP.

•c

VIS ~°-

--d?pVhs

SPECIAL OBSERVATIONS

COLOR CODE

TBANS.

OIR.

SPEED

OP FOPCE

DRY flULB

WET

euLB

20

SI*

1*5

083

078

6

08

MEtSENCR 1 TIME or HR 1/10

CAST NO.

CARD TYPE

DEPTH Iml

T i:

s •/„

SIGMA-T

mane voiuwi

SAD

DTN. M.

11 I0>

SOUND VELOCITY

Oj ml/I

PO4-P

MB- ""'1

rOT*L-P ..fl • o</l

NOj-N

wg - ot/l

nOt-n

WB- ol/l

SI 04-Si pg-ol/l

PH

S C

c

STD

0000

1062

3*95 12582

0012361

0000

14926

218

OBS STD STD STD STD STD STD STD STD

0000 1052 3*9*7 2582 0010 1053 3*99 2685 0012083 0020 1063 3502 2688 0011885 0030 1064 3506 2691 0011630 0050 1065 3513 2696 0011177 0075 1066 3520 2701 0010737 0100 1068 3527 2706 001031* 0125 1069 3532 2710 0010021 0150 1071 3537 2713 0009745

14925 0012 1*928 002* 1*930 0036 1*933 0059 1*937 0086 1*9*3 0112 1*9*8 0138 1*953 0153 14959

218

OBS STD STD STD

0171 1072 35399 2715 0200 1074 35*0 2715 0009681 0250 1077 35*1 2715 0009821 0300 1081 35*1 2715 0009961

14953 0211 14968 0260 14978 0309 14987

218

OBS

T0317 1082 35*14 2715

14991

218

OBS STD STD

0353 10*6 35314 2714

0400 0889 3520 2731 0008515

0500 0533 3503 2755 0005162

14982 0402 1*931 0*75 1*8*7

218

OBS STD STD

05*5 0553 34979 2752

0500 052* 3*98 2755 0005262

0700 0*77 3*97 2770 000*822

1*821 0532 1*819 0583 1*816

218

OBS STD STD

T07*5 0*58 3*97! 2772 0800 0435 3496 2774 0004512 0900 0404 3494 2775 0004385

1*815 0629 1*815 0674 1*818

218

OBS STD

0957 0392 34932 2776

1000 0386 3493 2777 000*320

1*823 0717 1*827

218

OBS

T1099

0380

3*931

2777

14841

REFERENCE

SHIP CODE

latitude

1/10

LONGITUDE

"1/10

°2

MARSDEN

STATION T

ME

ORIGINATOR'S

DEPTH

MAX. DEPTH

OF S'MPL'

WAVE

WEA- THER CODE

CLOUD CODES

NODC

CIPT CODE

ID. NO.

CRUISE NO.

STATION NUMBER

TO

BOTTOM

NUMBER

10-

r

MO

DAY H

R.1/10

DIB. MCTlK»| SE*

f»Pi *w

31

5*0

FV

*

*23

N

04758 W

149

47

15

23 3

13

1965

003

9387

521

13

24

Epkl

xa

7 8

0153

WATER

WIND

BARO- METER (mbll

AIR TEMP.

X

VIS- COO

NO.

OBS.

DEPTHS

SPECIAL OBSERVATIONS

COLOR CODE

TRANS.

DIR.

SPEED

OR fOPCE

DRt BULB

WET BULB

20

SIO

139

050

044

7

10

MES5ENCP 1 TIME or HR 1/10

CAST NO.

CARD TIPE

DEPTH 1ml

T -C

s •/..

SIGMA-T

SPECIFIC VOLUME ANOMAII-IIO'

SAD

DTN. M.

< 10=

SOUND VELOCITY

O3 ml/l

PO4-P Vfl • 0'/'

rOTAL-f vg - a. /I

NO3-N

US - Ot/l

NO]-N

SI 04-si

vg - oi/l

pH

S

c c

STD

0000

0760

3377

2639

0016450

0000

14798

013

OBS

0000 0760 33772 2639

1*798

STD

0010 0996 3*60 2667 0013856

0015 1*899

STD

0020 1186 3527 268* 0012200

0028 14977

013

OBS

0028 1303 35702 2595

15023

STD

0030 1293 3558 2695 0011212

0040 15020

STD

0050 1203 3552 2701 0010750

0052 1*991

STD

0075 1109 3535 2705 0010376

0088 14960

013

OBS

0098 1042 352*0 2709

14938

STD

0100 10*1 352* 2709 0010075

0114 14938

STD

0125 1029 3524 2711 0009952

0139 14938

STD

0150 1017 3523 2712 0009827

0164 14938

STD

0200 0993 3523 2715 0009579

0212 1*937

013

OBS

0218 0984 35226 2717

1*937

STD

0250 0867 3510 2727 0008612

0258 1*897

STD

0300 0726 3495 2737 0007554

0298 1*8*9

013

OBS

T0327 0570 34922 27*2

1*831

STD

0400 0615 3*98 2754 0005147

0367 14822

013

OBS

0*35 0591 35000 2759

14819

STD

0500 0552 3500 2763 0005312

0425 1481*

STD

0600 0498 3500 2770 0004744

0475 1*808

013

OBS

0551 0474 3500* 2773

1*807

STD

0700 0*52 3*99 277* 0004391

0521 1*806

STD

0800 0*15 3*96 2776 0004272

056* 1*807

013

OBS

T0868 0397 34943 2777

1*810

STD

0900 0394 3494 2777 0004251

0605 1*81*

STD

1000 0384 349* 2778 000*252

06*9 1*827

STD

1100 0377 3*93 2778 000*285

0692 1*840

013

OBS

T1108 0376 3*93* 2778

14841

STD

1200 0371 3493 2778 0004305

0735 14854

STD

1300 0366 3493 2779 0004335

0778 14869

01

3

OB

S

1306

0

365

31

9

32

27

7

?

1*E

70

147

REfEBtNCE

SHIP CODE

LATITUDE

l/IO

LONGITUDE

'1/10

if

MARSDEN

STATION T

ME

ORIGINATOR'S

DEPTH

MAX.

WAVE

WEA. TMEH CODE

CLOUD CODES

NOOC

CTrtr

ID. NO.

CRUISE NO.

STATION

NUMBER

BOTTOM

OF S'MPL-S

STATION NUMBER

10*

1*

MO

DAY H

R.1/10

OIR.

HOT ?i» St*

TTPI iW

31

540

FV

4

430

N

04836 W

149

48 05

23 D56

1965

003

9388 2743

12

21

1 2

X7

X 8

0154

WATER

WIND

BARO- METER

(mbll

AIR TEMP. X

COD

NO.

OBS.

DEPTHS

SPICtAL OBSERVATIONS

COLOR CODE

IRAHS.

DIR.

SFt(D

OR fORCE

DRY BULB

WET BULB

21

SOB

105

050

044

7

09

MESSENCR

TIME fl

HR 1/10 '

CAST NO.

CARD TYPE

DEPTH (ml

T 1C

s •/..

SIGMA-T

SPtCIHC VOLUMt

ANOMALT-XlO'

SAD

OYN. M. X 10^

SOUND

VELOCITY

Oj ml/1

P04-P

tOTAl_p

va - o'/i

NO3-N

JIB- oi/l

NOj-N US - 01/1

SIO*-Si JIB - ol/l

PH

S

c c

STO

0000

0450

3380 I268O

0012529

0000

14673

056

OBS

0000 0450 33802 2680 14673

STD

0010 0451 3380 2680 0012560 0013 14675

056

OBS

0016 0451 33798 2680 14676

STD

0020 0426 3380 2683 0012320 0025 14667

STD

0030 0369 3382 2690 0011625 0037 14645

STD

0050 0274 3387 2703 0010421 0059 14608

056

OBS

0051 0270 33877 2704 14606

STD

0075 0286 3401 2713 0009454 0084 14619

STD

0100 0302 3416 2723 0008533 0106 14632

STD

0125 0318 3430 2733 0007626 0127 14645

STD

0150 0335 3444 2743 0006728 0144 14658

STD

0200 0367 3472 2762 0004952 0174 14684

056

OBS

0201 0368 34730 2763 14685

STD

0250 0381 3478 2765 0004743 0198 14699

STD

0300 0394 3482 2767 0004571 0221 14713

STD

0400 0420 3492 2772 0004246 0265 14742

056

OBS

T0402 0420 34919 2772 14742

STD

0500 0395 3490 2773 0004195 0307 14747

STD

0600 0369 3489 2775 0004075 0349 14753

056

OBS

T0602 0368 34889 2775 14753

STD

0700 0364 3489 2776 0004092 0390 14768

STD

0800 0360 3490 2777 0004096 0431 14783

056

OBS

0805 0360 34898 2777 14783

STD

0900 0357 3490 2777 0004115 0472 14798

STD

1000 0355 3491 2778 0004138 0513 14814

056

OBS

T1032 0354 34908 2778 14819

STD

1100 0352 3491 2779 0004162 0554 14829

STD

1200 0350 3491 2779 0004219 0596 14845

056

OBS

T12ie

0350

34914

2779

14848

REEERENCE	SHIP CODE	LATITUDE l/IO	LONGITUDE '1/10	si	MARSDEN	STATION Tl	ME			ORIGINATOR'S	DEPTH	MAX. DEPTH OP S'MPL'S		WAVE		WEA- THER CODE	CLOUD CODES			NODC
CODE	ID. NO.				CRUISE NO.	STATION NUMBER	BOTTOM			NUMBER
10- 1 1-	MO	DAY HR.1/10		DilL	MGI PER SE*	irp( AM
31	540	EV	4	431	N	04850 W		149	148	35	23 0	76 Il965	003	9389	1390	12	20	2 2	X2	6 8	0155
			WATER	WIND	BARO- METER Imbll	AIR TEMP.	■c	VIS. COD	NO. ,„r.-,.. 1
	COLOR CODE	'»f'	DIR.	SPEED OP fOPCE	DRY BULB	WET BULB	OBS. DEPTHS	OBSERVATIONS
				23	S03	112	033	028	S	11
	MESSENGK \| HR l/IO	CAST NO.	CARD TYPE	DEPTH (ml	T -C	s •/„	SIGMA-T	SPECIfIC VOLUME ANOMALT-XIO'	SAD DYN. M. x 10'	5°""° 0, ml/1 VELOCITY "'	PO4-P	tOTAL-P	NOj-N V3 -or/l	NO3-N U9 - ot/l	Sl04-Si ug - oi/l	pH	S c c
			STD	0000	0196	3290	2631	0017187	0000	14552
076		OBS	0000 0196 32895	2631	14552
		STD	0010 0195 3290	2631 0017177	0017 14553
076		OBS	0015 0195 32897	2632	14554
		STD	0020 0052 3303	2651 0016284	0033 14493
076		OBS	0025 -0049 33141	2665	14449
		STD	0030 -0034 3319	2668 0013658	0048 14457
076		OBS	0048 0017 33366	2680	14486
		STD	0050 0022 3339	2682 0012381	0074 14489
		STD	0075 0085 3366	2700 0010669	0103 14525
		STD	0100 0139 3389	2715 0009270	0128 14557
076		OBS	0120 0174 34046	2725	14578
		STD	0125 0179 3407	2727 0008197	0149 14581
		STD	0150 0203 3417	2733 0007632	0169 14597
		STD	0200 0246 3435	2744 0006646	0205 14627
076		OBS	0214 0257 34398	2746	14635
		STD	0250 0285 3450	2752 0005889	0236 14654
		STD	0300 0319 3462	2759 0005340	0264 14678
		STD	0400 0365 3478	2767 0004684	0315 14717
076		OBS	T0426 0373 34813	2769	14725
		STO	0500 0378 3484	2770 0004462	0360 14740
076		OBS	0576 0381 34862	2772	14754
		STD	0600 0381 3486	2772 0004405	0405 14758
		STD	0700 0380 3487	2773 0004423	0449 14774
076		OBS	T0769 0380 34879	2773	14786
		STD	0800 0380 3488	2773 0004454	0493 14791
		STD	0900 0379 3489	2774 0004463	0538 14807
076		OBS	0982 0379 34891	2774	14821
		STO	1000 0378 3489	2774 0004520	0583 14823
		STD	1100 0374 3490	2775 0004529	0628 14839
		07	6		OB	S	TII5-		0	370	34	a	98	27	7	3						146	46

148

■ SHIP CODE

31 5*0lEV

LATITUDE

1/10

LONGITUDE

■i/io

DAY HR.V10

1*9 *9 05 23 392 1965 003 9390

S«fD

OR (0»C(

ORIGINATOR'S

AIR TEMP. "C

27 511 105 033 028 8 03

31*1

_ai_

25 |2

WEA- THER CODE

X2 6 la

NODC STATION NUMBER

0156

NOj-N ug- oi/l

SIO*-Si ug • 01/1

092

STD

OBS STD STD

OBS STD STD STD STD

OBS

0000 0000 0010 0020 0027 0030 0050 0075 0100 0106

0201 0201 0129 0068 0032 0031 0022 0011 -0000 -0003

3291

32910

3296

3300

33029

330*

3312

3320

3326

3327*

2632 2632 26*1 26*8 2652 2653 2660 2667 2672 267*

0017108

0016255 0015597

0015097 001**39 0013769 0013252

0000

0017 00 3 3

00*8 0077 0113 01*7

1*55* 1*55* 1*525 14*99 1**85 1**85 14*85 1**85 14*85 1**85

REFERENCE

SHIP CODE

LATITUDE

1/10

LO

GITUDE ' 'l/IO

MARSDEN

STATION

TIME

ORIGINATOR'S

DEPTH

MAX

■

WAVE

WEA.

TMER CODE

CLOUD CODES

NODC

cr«T CODI

ID. NO.

CHUISt

NO.

STATION

NUMBER

TO

BOTTOM

OF S'MPL'S

STATION NUMBER

10-

r

MO

DAY

HH.VIO

OIR.

HC PEB SEA

tTPf AM

31

5*0

FV

4*37

N

0*919 W

149

49

OS

73

103

1965

003

9391 3064

01

?7

3 4

X?

6 B

0157

WATER

WIND

BARO- METER

AIR TEMP. •€

VIS,

coo

NO.

OBS. DEPTHS

SPECIAL OBSERVATIONS

COLOR CODt

IRANS.

D1R.

SPEED

oir

FO»C(

DRY BULe

WET

BULB

26

SIO

105

033

028

B

05

MESSENOH CAST

ii»i ,\a.

HR 1/10

CARD TYPE

DEPTH Iml

T -C

s •/..

SIGMA-T

SPECIFIC VOLUME ANOMALT-XlO'

S Ao

DVN. M. X .0^

SOUND VELOCITY

Oj ml/I

PO*-P

rOTAL-P wg • ol/l

NOj-N

vg - ot/l

NOj-N VO - ot/l

S10*-Si

ug - ol/l

pH

i

C

c

STO

0000

0233

3304

2640

0016339

0000

14570

103

OBS

0000 0233 330*2 26*0 1*570

103

OBS

0007 0231 33048 2641 14571

STD

0010 0206 3304 2642 0016160 0016 1*560

103

OBS

0018 0146 33028 2645 14535

STD

0020 0133 3303 2646 00157*8 0032 1*529

STO

0030 0079 330* 2651 0015360 00*8 1*507

STD

0050 0029 3306 2655 001*9*7 0078 1*487

10

3

OB,

0056

OC

28

33

0

64

26

5 =

14488

REFERENCE

SHIP CODE

LATITUDE

1/10

n

MARSDEN

STATION

Tl

\Al

ORIGINATOR'S

DEPTH

MAK.

WAVE

WEA- THER CODE

CLOUD CODES

-lODC

CUT

COOf

ID. NO.

' '1/10

CRUISE NO.

STATION NUMBER

TO BOTTOM

Of S'MPL'S

STATION NUMBER

10-

r

MO

DAY

HR.1/10

OIL

MCT PER S

A

lYf[ AM

31

540

EV

4400

N

04918 W

1*9

49

T5

?3

137

1965

003

9392

044

no

26

3 k

X?

6 8

0158

WATER

WIND

BARO- METER Imbil

AIR TEMP. 'C

VIS. COD

NO.

OBS. DEPTHS

SPECIAL OBSERVATIONS

COLOR CODE

HANS, Iml

DIR.

SPEED

o»

fOPCE

DRY

BULB

WET

BULB

20

SOS

105

067

056

8

04

TIME c\l HR 1/10

CARD

TYPE

DEPTH (ml

I -c

s ■/..

SlGMA-T

SPECIFIC VOLUME ANOMALT-KIO'

SAD

DYN. M.

X 10^

SOUND VELOCITY

Oj ml/1

PO4-P

vs - o'/l

lOTAl-P

ua ■ ol/l

NOl-N wg - ol/l

NOj-N

vg - ol/l

SI 0<-Si pg - ol/l

pH

S

c

C

STD

0000

0299

3305

2635

0016821

0000

14599

137

OBS 0000 0299 33047 2635 14599 STO 0010 0242 3305 2640 0016350 0017 14576

137

OBS 0015 0212 33055 2643 14564 STO 0020 0173 3306 2646 0015803 0033 14547

137

OBS 0025 0149 33058 2648 14538 STD 0030 0147 3306 2648 0015607 0048 14537

13

7

OB

5

0035

0

44

33

0

61

26

4£

145

37

149

REFERENCE	SHIP CODE	LATITUDE I/IO	LONGITUDE ■1/10	= i	MARSDEN	STATION	TIME			ORIGINATOR'S	DEPTH	MAX	.		WAVE		WEA- THER CODE	CLOUD CODES			NODC
CTRY CODE	10. NO.				CRUISE NO.	STATION NUMBER	TO BOTTOM	OF S'MPL'S			STATION NUMBER
10*	1*	MO	DAY	HR.VIO	Dia.	HGI PER SEA	ITPE AM
31	540	EV	I	>355	N	04907 W		149	39 05	23	151	1965	003	9393	bl83	02	21		X?	7 8		0159
				WATER	WIMD		- R	AIR TEMP.	•c	>,,< NO. CODE 0"5- DEPTHS	SPECIAL OBSERVATIONS
	COLOR CODE	IRAM-	DIR.	0» fOBCE	MET! Imbi	DRY BULB	WET BULB
			18	S16	088	050	044	3	05
	MEJSENGR HR 1/10	CAST NO.	CARD TYPE	DEPTH Iml	T -C	s •''..	SIGMA-T	SFEClfiC VOLUME *NOMALT-<IO'	SAD DYN. M. X 10^	SOUND VELOCITY	07 ml/1	POi-P VB • ol/l	TOTAL-P u9 - 01/1	NOj-N wg - ot/1	NOj-N Itg - Ql/I	SIO.-Si PS - 01/1	PH	S c c
			STD	0000	0199	3297	2637	0016662	GOOD	14554
	151		CBS	0000 0199 32967 2637		14554
			STD	0010 0088 3307 2652	0015175	0016 14508
			STD	0020 0002 3316 2665	0014024	0031 14472
	151		OBS	0020 0002 33163 2665		14*72
			STD	0030 0003 3319 2657	0013819	004* 1*7
			STD	0050 0004 3325 2671	0013352	0072 1*479
			STD	0075 0006 3336 2580	0012524	0104 14*85
	151		OBS	0081 0006 33390 2583		14487
			STD	0100 0045 3357 2695	0011124	0134 14510
			STD	0125 0089 3376 2708	0009935	0160 14537
			STD	0150 0124 3391 2718	0009026	0184 14559
	151		OBS	0152 0127 33917 2718		1*560
		151		OBS	0179		0156	34022		2724								14579

REFERENCE

SHIP CODE

LATITUDE

1/10

LONGITUDE

■1/10

ii

MARSDEN

STATION

Tl

\M

ORIGINATOR'S

DEPTH

MAX. DEPTH

OF S'MPL'S

WAVE

WEA- THER CODE

CLOUD CODES

CIRY

ID. NO.

CRUISE NO.

STATION NUMBER

TO BOTTOM

STATION NUMBER

CODE

10-

1*

MO

DAY HR.l/lO

OIR.

HGI PES SEA

TffI AM

31

540

EV

4

348

N

04856 W

149

38

36

23

165

1965

00 3

9394

887

08

18

b 3

X8

7 8

0160

WATER

WIND

BARO- METER

(mbtl

AIR TfMP. X

VIS.

coo

NO.

OBS. DEPTHS

SPECIAL OBSERVATIONS

COLOR CODE

IRANS.

DIR.

SPtEO

0« (ORCE

DRY BULB

WET BULB

18

512

081

050

044

7

07

MESSENCR

TIME I

HH 1/10

CAST NO.

CARD TYPE

DEPTH Iml

I -c

s •/..

SIGMA-T

SPEC'FIC VOLUME ANOM*t.T-<IO'

SAD

DVN. M.

SOUND VELOCITY

0: ml/l

fOi-P

lOTAl-F

ug - ol/l

NOj-N

ug - ol/l

NOi-N vg - ol/l

SIO,-Si ug - ol/l

pH

S

c c

STD

0000

0184

3293

2635

0016831

0000

14547

165

OBS STD STD STD

0000 0184 32931 2635 145*7 0010 0183 3313 2551 0015315 0016 1*551 0020 0182 3332 2665 0013857 0031 1*555 0030 0180 33*8 2579 00125*7 00** 1*568

165

OBS STD STD

00*9 0178 3373* 2700 1*564 0050 0177 3374 2700 0010658 0057 1*553 0075 0159 3395 2719 0008871 0092 1*663

165

OBS STD STD STD STO

0079 0158 33988 2721 14563 0100 0196 3413 2730 0007861 0113 14585 0125 0238 3429 2739 0006993 0131 14610 0150 0274 3443 2748 0006254 01*8 1*632 0200 0332 3*65 2750 0005163 0176 1*668

155

OBS STD STD

0209 03*0 3*678 2751 1*673 0250 0350 3*72 276* 0004853 0201 14685 0300 0350 3477 2767 0004521 0225 14598

165

OBS STD STD

T0384 0373 34827 2770 1*718 0*00 037* 3*83 2770 000**05 0270 1*721 0500 0378 3*85 2772 000*313 031* 1*7*0

155

OBS STD STD

T0657 0380 3*877 2773 1*752 0600 0380 3*88 2773 000*291 0357 1*768 0700 0380 3*88 2773 000*351 0*00 1*77*

16

5

OB

S

T076*

o:

J79

3*

8

84

27

7i

147

84

150

REFERENCE

SHIP CODE

_.

MARSDEN

STATION TIME

ORIGINATOR'S

DEPTH

MAX

WAVE

WEA-

CLOUD

NODC

crsT

COOf

NO.

LATITUDE

1/10

LONGITUDE

"1/10

Si

CRUISE NO.

STATION

NUMBER

TO BOTTOM

OF S'MPL'

THER CODE

STATION NUMBER

10"

1-

MO

DAY

HR.l/lO

S DIB- |hCT]«»| SfA

TYFl AW

31

5*0

FV

/

f3*5

N

0*8*2 W

149

38 05

23

179

1965

003

9395 ___ 2396

jl

16

^U

X8

7 8

0161

WATER

WIND

AiB TEMP, r:

SPECIAL OBSERVATIONS

COLOR CODE

TRAWS.

DIR.

S»EIO

OR FORCE

METER tmbil

DRT BULB

WEI

BULB

COD

OBS. DEPTHS

16

S16

061

050

5 111

MESStNO

TIME ( HR 1/)0

CAST NO.

CARD TYPE

DEPTH Iml

I -c

s ■'..

SIGMA-T

SfECIFIC VOLUME AMOMALT-KIO'

SAO

DYN. M.

t 10^

SOUND VELOCITY

Ol ml/l

PO,-P

lOTAl-p

vg - ol/l

NOj-N ut - ol/l

NOj-N KB - o'/l

SIO4-S1

MB - Ot/I

PH

S

c c

STD

0000

0408

3362

2670

0013^87

0000

14653

179

OBS

STD

0000 0*08 33619 2670 1*653 0010 0*07 3363 2671 0013*07 0013 1*655

179

OBS STD

0015 0*06 3363* 2672 1*655 0020 0362 3376 2686 001200* 0026 1*639

179

OBS STD STO

0029 0298 33945 2707 1*616

0030 0297 3395 2707 0009999 0037 1*615 0050 0277 3*05 2717 0009087 0056 1*611

179

OBS STD STD STD

0073 0268 3*166 2727 1*613 0075 0270 3*18 2728 0008061 0078 1*61* 0100 0298 3*36 27*0 0006960 0096 1*633 0125 0321 3*51 2750 0006056 0113 1*6*9

179

OBS STD STD STO

01** 0337 3*607 2756 1*660 0150 03*0 3462 2757 0005425 0127 14663 0200 0360 3471 2762 0004985 0153 14681 0250 0375 3478 2766 000465* 0177 14696

179

OBS STD STD

T0290 0384 34824 2768 14707 0300 0385 3483 2769 000**25 0200 14709 0400 0390 3*87 2771 000*278 02*3 1*729

179

OBS STD

0*14 0391 34875 2772 1*731 0500 0382 3*88 2773 000*207 0286 1*7*2

179

OBS STO STD

T0586 0376 3*889 277* 14754 0600 0376 3489 2775 0004158 0328 14756 0700 0373 3490 2776 0004139 0369 14771

179

OBS STD STD STD

0785 0370 34906 2776 14784 0800 0369 3491 2776 0004140 0*11 1*787 0900 0365 3491 2777 000417* 0452 14801 1000 0360 3491 2777 0004205 049* 1*816

179

OBS STD

T1003 0360 3*906 2777 1*817 1100 0359 3*91 2778 000*2*5 0536 1*832

179

OBS

TllOl

0359

34910

2778

14833

REFERENCE

SHIP CODE

LATITUDE

1/10

LOF

GITUDE * '1/10

ii

MARSDEN

STATION T

ME

ORIGINATOR'S

DEPTH

MAX.

WAVE

WEA- THER CODE

CLOUO CODES

NODC

CTIT CODE

ID. NO.

CRUISE STATION NO. NUMBER

BOTTOM

OF S'MPL'S

NUMBER

10- 1 1-

MO DAY H

R,1/10

OIB.

HOT nt UA

iin AM

31

■i40

FV

4330

N

04S06 W

1*9

138 1

35 23 2

13

1965

003 9396

3292

11

24

k 3

X?

7 8

0162

WATER

WIND

BARO- METER (mbtl

AIR TEMP, "C

VIS- COD

NO.

OBS. DEPTHS

SPECIAL OBSERVATIONS

COLOR CODE

'""■

DIR.

into

OR FORCE

DRY BULB

WET BULB

25

S21

037

067

6

12

»'""<" CAST '!"' % NO. HR 1/10

CARD lYPE

DEPTH Iml

T -C

s ■/..

SIGMA-T

SPECifIC VOIUME

ANOMALT-dO'

SAD DYN. M.

SOUND VELOCITY

Oj ml/t

PO<-P lOTAL-P

VB - a'/l vg - o'/l

NOj-N vg - 01/1

NOj-N

»o - or/l

SI04-Si

ug - ol/l

pH

S

c c

STD

0000

0609

3332

2524

0017883

0000

14732

1 1

213

OBS

0000 0609 33323 262* 1*732

STD

0010 0606 3332 262* 0017856 0018 1*733

213

OBS

0015 0505 33325 2625 1*733

STO

0020 0*68 3336 2643 0016055 0035 14678

213

OBS

0026 0329 33*01 2561 1*621

STD

0030 0344 3351 2668 0013729 0050 14630

STD

0050 0417 3397 2697 0010980 0074 14670

STD

0075 0509 3434 2716 0009206 0100 14717

213

OBS

0091 0558 34463 2719 14746

STD

0100 0507 3**5 2725 0008*2* 0122 1*722

STD

0125 039* 3*39 2733 0007537 01*2 14678

213

OBS

0131 0380 3*381 273* 1*573

STD

0150 0*25 3**9 2738 0007250 0160 1*597

213

OBS

0187 0*8* 3*665 27*5 14730

STD

0200 0479 3*58 27*7 0005*56 0195 1*730

STD

0250 0*67 3*75 275* 0005863 0225 1*73*

213

OBS

T0279 0*55 3*791 2757 1*739

STD

0300 0*71 3*82 2759 0005*18 025* 14745

STD

0*00 0499 3498 2768 0004730 0304 14775

213

OBS

0403 0500 34980 2768 14776

STD

0500 0453 3496 2772 000**11 0350 1*773

STD

0500 0*17 3*9* 277* 000*2*7 0393 1*77*

213

OBS

0600 0417 34940 2774 14774

STD

0700 0399 3493 2775 0004211 0436 14783

213

OBS

0794 0387 34920 2775 1*793

STD

0800 0387 3*92 2776 000*240 0478 1479*

STD

0900 0382 3*92 2776 000*26* 0520 1*809

STD

1000 0375 3*92 2777 000*262 0563 1*823

213

OBS

T1013 0374 34922 2777 1*824

STD

1100 0357 3492 2778 0004268 0606 14836

21

3

OB

5

Tins

0

365

349

18

27

7

3

14f

38

151

31 540 EV 4316 N 04731 W

LONGIIUDf

■1/10

149

MO DAY HI1.1/1Q

37 105 124 1006

1?65

26

s«eD

fO»CE

S30

ORIGINATOR'S

0Q3I9397

AIR TEMP. *C

061

NO.

OBS.

DEPTHS

3584 I 13 I 25 |6 l3

NODC STATION

NUMBER

0163

MESSENCR I

TIME 01

HRVToT

DEPTH Iml

006

006 006

006

STD

CBS STD STD STD

OBS STD STD

OBS STD STD STD STD

OBS STD

OBS STD STD

OBS

0000 0000 0010 0020 0030 0032 0050 0075 0080 0100 0125 0150 0200 0239 0250

T0290 0300 0400 0426 0500 0600 0639 0700 0800

T0855 0900 1000 1085 1100 1200

T1274

0878 0878 0853 0848 0833 0830 0923 1024 1041 1024 1003 0983 0941 0908 0873 0766 0757 0673 0652 0579 0505 0483 0471 0451 0440 0431 0412 0397 0394 0378 0366

3416

34157

3418

3419

3421

34214

3462

3508

35157

3515

3513

3512

3510

35075

3505

34982

3499

3503

35038

3501

3499

34983

3499

34993

3499

3497

34961

3496

3494

34926

2651

2651 2655 2559 2662 2553 2680 2699 2702 2704 2707 2710 2715 2718 2722 2733 2735 2750 2754 2761 2768 2770 2772 2774 2776 2777 2777 2778 2778 2778 2778

0015282

0014944 0014608 0014281

0012633 0010913

0010480 0010284 0010090 0009708

0007874 0005558

0005593 0004927

0004622 0004485

0004343 0004355

0004301 0004340

0000

0015 0030 0044

0071 0101

0127 0153 0179 0228

0009074 0275

0318 0390

0451 0503

0551 0596

0641 0584

0727 0771

14848 14848 14844 14840 14836 14836 14879 14925 14934 14931 14927 14924 14915 14910 14899 14864 14862 14846 14842 14825 14811 14808 14814 14822 14827 14830 14839 14847 14848 14857 14865

REFERENCE

SHIP CODE

LATITUDE

1/10

L0^

GITUDE ■ -1/10

if

MARSOEN

STATION T

ME

ORIGINATOR'S

DEPTH

MAX.

WAVE

WEA- THER CODE

CLOUD CODES

■JODC

CTIT CODI

ID.

NO.

CRUISE NO.

STATION NUMBER

BOTTOM

OF

S'MffS

NUMBER

10*

r

MO

DAY H

R.1/10

Dl».

HCI '(t SE*

un AM

31

S^O

FV

4

304

N

04704 W

149

37

■)">

24 D

34

1965

003

9398

3749

12

26

5 2

X?

7 8

0164

WATER

WIND

lARO- METER

(mbd

AIR TEMP. X.

COD

NO.

OBS. DEPTHS

SPECIAL OBSERVATIONS

COLOR CODE

TRANS.

OIR.

SMtO

0> FORCE

DRY BULB

WET

flULfl

27

S23

071

083

072

W

10

MESSENGR

TIME 0.

HR 1/10

CAST NO.

CARD KPE

DEPTH Iml

I t

s •''..

SIGMA-T

SfECIFIC VOLUME ANOM*LI->IO'

SAD

OYN. M.

X 10'

SOUND

VELOCITY

Oj ml/1

PO«-P

vg - Ol/I

TOTAL-f

NOj-N

N03-N l^g - ol/l

SIO*-Si

ve - 01/1

pH

s c

c

STD

0000

1088

3A97

2679

0012633

0000

14935

034

OBS STD STD

0000 1088 34970 2579 14935 0010 1088 3498 2680 0012590 0013 14937 0020 1089 3498 2680 0012620 0025 14939

034

OBS STD STD STD STD

0024 1089 34985 2580 14940 0030 1075 3499 2683 0012334 0038 14936 0050 1035 3502 2693 0011483 0062 14925 0075 0999 3506 2702 0010647 0089 14917 0100 0978 3509 2708 0010137 0115 14913

034

OBS STD

0101 0977 35091 2708 14913 0125 0976 3512 2711 0009934 0140 14917

034

OBS STD STD

0140 0975 35137 2712 14919 0150 0981 3517 2714 0009598 0165 14924 0200 1009 3526 2716 0009607 0213 14943

034

OBS STD STD

0233 1027 35279 2714 14955 0250 0980 3523 2718 0009453 0251 14941 0300 0854 3510 2729 0008508 0306 14900

0 34

OBS STD

STD

T0377 0699 34963 2741 14852 0400 0672 3497 2745 0006988 0383 14845 0500 0571 3499 2760 0006637 0446 14821

034

OBS STD STD

T0571 0519 34995 2767 14812 0500 0509 3499 2758 0004977 0499 14813 0700 0476 3499 2772 0004684 0548 14816

034

OBS STD STD

0771 0455 34980 2773 14819 0800 0446 3498 2774 0004498 0594 14820 0900 0418 3496 2776 0004405 0538 14824

034

OBS STD STD

T0997 0399 34954 2777 14833 1000 0399 3495 2777 0004316 0682 14833 1100 0387 3495 2778 0004257 0725 14845

03

4

OB

S

T117e

0

J83

3^

9

52

27

7

3

14fi

56

152

REfERENCe	SHIP CODE	LATITUDE l/IO	LONGITUDE * "1/10	If	MAIISOEN	STATION TIME			ORIGINATOR'S 1	DEPTH TO BOTTOM	MAX. DEPTH OF S'MPL-		WAVE	n	WEA- THER CODE	CLOUD CODES			NODC
CIRY coot	10. NO.	SQUAB!	IGMTl	YEAR	CRUISE NO.	STATION NUMBER 1	08StKV«lluni		STATION NUMBER
10-	r	MO 1	Kih-i H	R.l/lO	Dl«,	MGI »l« i(A	MH. AMI
31	540	EV	4217	N	04821 W		149	28 05	24 112	1965	003	9399	^558	12	28	^ I2	X2	6 8		0165
			WATffi	WIND	lARO- METER (mbd	AIR TEMP.	•c	VIS. C00(	NO. OBS. DEPTHS	SPECIAL OBSERVATIONS
	COLOR coot	tMNS.	OIR.	i«(0 Ol	DRY 8ULB	WET BULB
				11	S19	102	061	050	8	12
	"ISSK-OrIcASI ""1 "' NO. HR 1/10	CARD TYPE	DEPTH (ml	T 1C	s •/..	SIGMA-T	sreciFic voiuME ANOMALT-IIO'	SAD DYN. M X 10^	SOUND VELOCITY	Ol ml/l	PO4-P	tOTAL-P Vfl - 0</l	N03-N wg - or/I	N0)-N l>g - ot/l	SlO^-Si vg - ot/l	pH
		STO	0000	0B67	3452	2682	0012402	0000 1 14849 1							1
112	OBS	0000 0867 34523 2582		14849
	STD	0010 0866 3456 2685	0012111	0012 14850
	STD	0020 0854 3460 2688	0011827	0024 14852
	STD	0030 0863 3464 2591	0011534	0036 14853
112	OBS	0035 0862 34558 2593		14854
	STO	0050 0690 3439 2597	0010999	0058 14787
112	OBS	0050 0509 34258 2598		14755
	STD	0075 0569 3442 2703	0010514	0085 14783
	STD	0100 0759 3458 2709	0009991	0111 14829
	STD	0125 0868 3494 2714	0009585	0135 14875
112	OBS	0139 0924 35082 2716		14900
	STD	0150 0825 3493 2720	0009044	0159 14852
112	OBS	0174 0599 34750 2725		14815
	STD	0200 0783 3498 2730	0008149	0202 14855
112	OBS	T0224 0825 35110 2734		14877
	STD	0250 0753 3505 2740	0007285	0240 14853
	STD	0300 0539 3497 2750	0005392	0274 14815
112	OBS	0332 0584 34929 2754		14798
	STD	0400 0512 3489 2759	0005531	0334 14779
112	OBS	0400 0512 34888 2759		14779
	STD	0500 0483 3495 2768	0004839	0386 14785
	STD	0500 0456 3498 2773	0004405	0432 14791
112	OBS	0503 0455 34983 2773		14791
	STD	0700 0429 3498 2776	0004190	0475 14795
	STD	0800 0406 3497 2778	0004091	0517 14803
112	OBS	T0807 0405 34955 2777		14804
	STD	0900 0387 3494 2777	0004182	0558 14811
	STD	1000 0374 3493 2778	0004191	0600 14822
112	OBS	1030 0372 34925 2778		14825
	STD	1100 0371 3493 2778	0004242	0542 14838
112	OBS	T1170 0370 34938 2779		14849
REFERENCE	SHIP CODE	LATITU	DE 1/10	LONGITUDE ' '1/10	ii	MARSDEN SQUARE	STATION TIME (GMTI	YEAR	ORIGINATOR'S \|	°\'2" o'JpVh 80TT0M 5.„°;.	WAVE OBSERVATIONS	WEA- THER CODE	CLOUD CODES		NODC STATION NUMBER
CIRT coot	ID. NO.	CRUISE NO.	STATION NUMBER
10'	r	MO^	OAV H	R.l/tO	0l«.	HGl fIR SEA	t'fl AM
31	s^n	FU	47?7	N	04841 W		149	28	35	24 1	35	1965	203	9400	237 11	29_	(» I2	XI	8 7		0166
			WATER	WIND	lARC METE Imbi	- R	AIR TEMP.	•c	COOE	NO. OBS. DEPTHS	SPECIAL OBSERVATIONS
	COLOR CODE	tHANS.	OIIL	S»EtO fOlCt	DRY BULB	WET BULB
				29	SIB	105	050	044	P	13
	MESSENGR CAST "»i "NO. HR 1/10	CARD TYPE	DEPTH (ml	T -C	S '>..	SIGMA-T	SPECIFIC VOLUME ANOMALY-X10'	SAD OYN. M < loi	SOUND VELOCITY	0: ml/l	PO*-P	IOIAl_P Kfl - oi/l	N03-N ug - ol/l	NOj-N VB - ol/l	SIO^-Si vg - ot/l	pH	S c c
		STD	0000	0406	3344	2656	0014853	0000	14650
135	OBS	0000 0405 33435 2656		14650
	STD	0010 0649 3401 2573	0013249	0014 14759
	STD	0020 0840 3447 2582	0012434	0027 14841
	STD	0030 0979 3483 2687	0011945	0039 14899
135	OBS	0030 0979 34827 2587		14899
	STD	0050 0943 3487 2697	0011102	0052 14889
	STD	0075 0898 3492 2708	0010057	0089 14878
135	OBS	0081 0887 34935 2711		14875
	STD	0100 0535 3451 2714	0009482	0113 14775
135	OBS	0102 0617 34483 2714		14768
	STD	0125 0485 3437 2721	0008787	0135 14717
135	OBS	0132 0484 34334 2719		14716
	STD	0150 0555 3472 2728	0008236	0157 14794
135	OBS	0172 0805 35072 2734		14860
	STD	0200 0793 3504 2734	0007857	0197 14860
	STD	0250 0708 3498 2741	0007165	0235 14834
135	OBS	T0275 0532 34950 2749		14808
	STO	0300 0534 3483 2752	0006105	0268 14771
135	OBS	0308 0508 34802 2753		14761
	STO	0400 0455 3485 2752	0005275	0325 14760
135	OBS	T0403 0454 34849 2752		14760
	STD	0500 0458 3492 2768	0004757	0375 14774
	STD	0600 0445 3497 2773	0004398	0421 14785
135	OBS	0600 0446 34965 2773		14785
	STO	0700 0424 3495 2775	0004279	0464 14794
135	OBS	T0791 0409 34958 2776		14802
	STO	0800 0409 3496 2777	0004201	0507 14804
	STD	0900 0404 3495 2777	0004237	0549 14819
135	OBS	T0995 0397 34952 2778		14831
	STD	1000 0397 3495 2778	0004246	0591 14832
	STD	1100 0385 3495 2778	0004255	0534 14844
		13	5	OB	S	T112	?	0	382	^'■	+ c	46	2-	7	8							14	B46

153

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. _ . .	£^ i&i :965 3C3 9^::	25^2	- -
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CBS STD STD STC ST

STD STC

-."iZ	3 3*3	265:
:*^52	33*25	265:
0391	33*;	2659
C3*C	33*8	2:i6
C297	3353	;i"-
0239	336*	Icr"
C22?	3368t	;i = ;
Q2S6	3396	;~ : :
:373	3*29	t. • i. ■
0*38	3*56	ZT^Z
Cio;	3 a""?	2^;i

16*	0 = 5	";33S	. - = t	:---;;	: ■ - :
16*	03£	C399	».— o*.	J-- 1	I ~~ :
	STD	3*0 C	:*62	■a*.; ~	; ~~i
	STD	C50C	3**£	3'^ii	t. ■ : —
16*	03S	TC599	C3	398	2776
	STD	:50:	C3	3*98	2776
	STD	:': :	1-2:	3*98	277-
16*	OBS	:~ = ~	:-:?	3*971	277 5
	5T:	: : ; :	: -:5	3*97	2778
	STC		: ; =-	3*96	277 =
	STD	1 ; : :	- : -	39	277:
16*	OBS	T1015	0382	391	2775
	STO	1100	0375	3*95	2775
Ifr*	CSS	'1103	C375	395	2779

:::3:-'0	00*3	: -r : :
:::is77	0068	:*587
: : : ? 9*2	0095	1*623
;CC51S2	0118	166
0006837	0137	1*699
OC05717	0152	1728 1728
: ::::30	0180	1*737
: :-'-zo	0205	175
; : -r**	0229	1753 1759 1*760
: : ; - 3 :• .	:27*	1*760
------	:3i6	1771 1781
: ; ;---:	:358	1*782
:.:-:-.-	:399	1792 1803
:::_::-	r*AC	18 0
:;:-:-:	:-8i	181
— - - . ;	:;23	:B26 :82g
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	STD	oooo	ZZ9Z	33*-	2669	0013579	ococ	1*611
192	OES	DOCO	029C	33*66	2659			1*6C1
	STD	wi:	:263	3359	2632	: : - 3t 2 —	;: ". 3	1*593
	STD	0C20	C2*3	3371	2693		: ; : ^	1*33-
	STD	003C	C228	3382	27:3			133
192	oas	00*8	0218	3*011	271 =			;*;3;
	ST3	0050	0220	3*03	272:	: : - : " ^ 1		:-: 5 =
	STD	0075	02*9	3*28	273c	J0C7.31	jl "^5	i*60T
192	oas	0086	0263	3*371	27**			1*616
	STO	0100	0285	3**5	27*«	0006168	0092	1*629
192	OBS	0120	0313	3*553	275*			165
	STD	0125	0317	3*57	2755	3005567	0106	168
	STO	0150	0338	3*66	2760	0005106	0120	1*662
	STD	0200	0369	3*79	27S7	00O*7	01*3	1*686
192	03S	T0216	0376	34822	2769			1*692
	STD	2250	0378	3*«3	2770	000*310	0165	1*698
	STD	0300	038C	38	2770	000*302	0137	1*707
192	oas	: : = -	3381	3*857	2771			1*717
	st;	: - :	0380	3*«7	277 3	:::-i69	0229	172
	st;		C377	3*88	277i	1 1 1 — " ~ -	0271	170
192	OSS	- ' = _ -	0376	3*888	2771			176
	st:		037*	3*89	2773		.312	1*755
	STD	— ■		3*89	2775	j--*-i3:>	i35*	1*770
192	oas			3*392	2775			1*773
	c-		.'—,-.	3*9C	2776	000*170	0396	1*786
	: ":		- - -	3*90	2 776	00025	0*38	1*802
192	: t :	" ' - ; '	' t 6	3*9S 1	2776			1*808
	—		- - ^ =	3*90	2776	;::6.299	0*81	1*813
192	: z 1	- - ' -.	: : i:	3*901	2776			1*323

154

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1	STD	0000	332B	33:c	2625	3C17*21	0000	1*611
239	OBS	0000	0328	33^GC	2629			1*611
	STD	0010	0327	330C	2629	0017**1	0017	1*612
239	OBS	0010	0327	32997	2629			1*612
	STD	0020	0296	3301	2632	0017085	0035	1*601
	STD	0030	0236	330*	26*0	0016387	0051	1*577
239	OBS	00*9	0039	33135	2650			1**93

l£S5l=sC!	.Z--.-.ZI i =		"*'>:'"'	CCC--''!*!	-'.r-.	-«j. '	:!-:J . • '■: ■	.-;/,	'r^.'^	"":*
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1 31 I540I EV 1 4257 N	050C4 W .	: - - -	:= Z5 c::	1965 ::; =^:-	c:;:		I •- 2	XI	3 2	. 0170-

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	STD	0000	0155	3299	26*1	0C16256	0000	150
02*	OBS	0000	0165	3299C	26*1			150
	STD	0010	0155	3300	26*2	0016219	0016	151
	STD	0020	0165	3330	26*2	3016182	0032	153
02*	OBS	0025	0165	33002	26*2			15*
	STD	0030	01*9	3315	2555	001*863	00*8	150
02*	OBS	00*7	0108	33519	2595			1*531
	STD	0050	0113	3355	2697	001091*	007*	1*5 3«.
	STD	0075	0150	3385	2711	00096*2	0099	1*557
	STD	0100	018*	30	272*	0008*52	0122	1*57?
	STD	0125	0216	3*21	2735	0007*20	01*2	1*599
02*	OBS	01**	0238	3*329	27*3			161
	STD	0150	02**	3*35	27**	0006602	0159	1*618
	STD	0200	0287	3**9	2751	00059*9	0191	166
	STD	0250	0323	3*62	2758	00053*1	0219	1*672
	STD	0300	0352	3*72	2763	000*915	02*5	169
02*	OBS	0382	038*	3*837	2769			1*723
	STD	0*00	038*	38	2770	000*3	0291	1*726
	STD	0500	0383	3*87	2772	000*291	0335	172
02*	OBS	T0572	0382	3*880	2773			175
	STD	0600	038C	3*88	2773	000*275	0378	1*758
02*	OBS	T0S16	0378	3*879	2773			1*759

155

REFERENCE	SHIP CODE	LATITUDE 1/10	LONGITUDE ' -1/10	S 2	MARSDEN	STATION Tl	^E			ORIGINATOR'S	DEPTH	MAX		WAVE		WEA- THER CODE	CLOUD CODES			NODC
CI«T coot	ID. NO.				CRUISE NO.	STATION NUMBER	BOTTOM	OP S'MPL'			NUMBER
10'	r	MO	DAY HR.l/IO	DIB.	MGI PtR SEA	T»PE AMI
31	S4n	FV	4	249	N	04902 W		1^9	29 05	24 164	1955	003	9401	2542	11	30	4 3	XI	3 7		0167
			WATER	WIND		- R 1	AIR TEMP.	r	"-D^p'^S	SPECIAL OBSERVATIONS
	COLOR CODE	TRANS.	OIR.	into	METE (mbs	DRY euLB	WET BULB
				29	S20	105	067	050	8	\|09
	M(SS£MG« 1 TIMt o> HR 1/10 '	CAST NO.	CARD TYPE	DEPTH Iml	I -c	s •/..	SIGMA-T	SPECIFIC VOLUMF ANOMALT-X10'	SAD OYN. M. < 10=	SOUND VELOCITY	03 ml/1	P04-P	TOTAL-P jjB - or/I	NO3-N ug - ol/l	NOj-N tig - ol/l	SI 04-Si vg - ol/l	pH	S c c
			STD	0000	0452	3343	2650	0015384	0000	14659
164		OBS	0000 0452 33425	2650		14569
		STD	0010 0391 3345	2559	0014604	0015 14546
		STD	0020 0340 3348	2666	0013915	0029 14626
		STD	0030 0297 3353	2674	0013170	0043 14510
		STD	0050 0239 3364	2687	0011877	0058 14589
164		OBS	0056 0229 33684	2692		14587
		STD	0075 0296 3396	2708	0009942	0095 14523
		STD	0100 0373 3429	2727	0008182	0118 14564	•
		STD	0125 0438 3456	2742	0005837	0137 14599
		STD	0150 0490 3479	2754	0005717	0152 14728
164		OBS	0150 0490 34789	2754		14728
		STD	0200 0489 3486	2760	0005230	0180 14737
		STD	0250 0487 3491	2764	0004900	0205 14745
		STD	0300 0486 3495	2767	0004644	0229 14753
164		OBS	T0338 0485 34963	2768		14759
164		OBS	0399 0462 34967	2771		14750
		STD	0400 0462 3497	2772	0004331	0274 14760
		STD	0500 0448 3498	2774	0004204	0315 14771
164		OBS	T0599 0434 34984	2775		14781
		STD	0600 0434 3498	2775	0004146	0358 14782
		STD	0700 0420 3498	2777	0004084	0399 14792
164		OBS	0797 0408 34971	2778		14803
		STD	0800 0408 3497	2778	0004107	0440 14804
		STD	0900 0394 3496	2778	0004140	0481 14814
		STD	1000 0383 3494	2778	0004203	0523 14826
164		OBS	T1015 0382 34941	2778		14828
		STD	1100 0375 3495	2779	0004180	0565 14840
		164		OBS	T1103	0375	34945	2779								14840

REFERENCE	SHIP CODE	LATITUDE 1/10	LONGITUDE "1/10	if	MAHSOEN	STATION	Tl	;r			ORIGINATOR'S	DEPTH	MAX DEPTH OF S'MPL-		WAVE		WEA- THER CODE	CLOUD COOES				ODC
CIPY coot	ID. NO.				CRUISE NO.	STATION NUMBER	BOTTOM
10*	r	MO	DAY	HR.1/10	S DIB. HGlj Pt«] S(*	UPt AM		168
31	540	EV	4	303	N	04915 W		149	39	D5	24	19?	1965	003	9402	353	10	?9	,u	X	X		C
			WATER	WIND	BARO- METER (mb»l	AIR TEMP.	x	VIS- COD	NO. DBS. DEPTHS	SPECIAL OBSERVATIONS
	COLOR CODE	IftANS.	DIR.	SPEiD OP FOICE	DRY BULB	WET BULB
				25	S17	112	061	044	8	10
	MESStNGP TIMt t HB I/IO'	CAST NO.	CARD TYPE	DEPTH Iml	T 1C	s •/..	SIGMA-T	SPECIFIC VOLUME ANOMALY-XIO'	SAD DYN. M. X 10=	SOUND VELOCITY	Ol ml/l	PO<-P vg -ol/l	rOTAL-P	NOi-N vs - Ol/l	NO3-N 1,8 - Ol/l	SIO4-S1 wg - Ql/l	pH	S c c
			STD	0000	0290	3347	2669	0013579	0000	14601
192		OBS	0000 0290 33465 2569	14501
		STD	0010 0253 3359 2582 0012427	0013 14593
		STD	0020 0243 3371 2693 0011365	0025 14587
		STD	0030 0228 3382 2703 0010421	0036 14584
192		OBS	0048 0218 34011 2719	14585
		STD	0050 0220 3403 2720 0008780	0055 14586
		STD	0075 0249 3428 2738 0007132	0075 14607
192		OBS	0086 0253 34371 2744	14516
		STD	0100 0285 3445 2748 0006158	0092 14529
192		OBS	0120 0313 34553 2754	14645
		STD	0125 0317 3457 2755 0005557	0106 14648
		STD	0150 0338 3456 2750 0005106	0120 14652
		STD	0200 0369 3479 2767 0004474	0143 14686
192		OBS	T0216 0375 34822 2759	14692
		STD	0250 0378 3483 2770 0004310	0165 14698
		STD	0300 0380 3484 2770 0004302	0187 14707
192		OBS	0354 0381 34857 2771	14717
		STD	0400 0380 3487 2773 0004159	0229 14724
		STD	0500 0377 3488 2774 0004153	0271 14740
192		OBS	T0542 0376 34888 2774	14745
		STD	0600 0374 3489 2775 0004135	0312 14755
		STD	0700 0371 3489 2775 0004185	0354 14770
192		OBS	0715 0370 34892 2775	14773
		STD	0800 0358 3490 2775 0004170	0396 14785
		STD	0900 0367 3490 2776 0004245	0438 14802
192		OBS	T0939 0366 34901 2776	14808
		STD	1000 0365 3490 2775 0004299	0481 14818
		19	2		OB	S	T102!	J	0	365	3*	<5	01		27	7	b							14(	J23

154

REFESENCE

SHIP CODE

LATITUDE

1/10

Si

MARSDEN

STATION

TIME

ORIGINATOR'S

DEPTH

MAX. DEPTH

OF S'MPL'S

WAVE

WEA- THER

CODE

CLOUD CODES

NODC

criiY coot

ID. NO.

LONGITUDE

■ -i/io

CRUISE NO.

STATION

NUMBER

TO BOTTOM

STATION NUMBER

10'

r

MO

DAy

MR.V10

01*.

HC1 PER St A

Uft AM

31

^i*0

EV

4310

N

05004 W

150

30 05

24

Z39

1965

003

9403 0064

00

22

3 2

XI

3 3

0169

WATER

WIND

BARO- METER

(mbil

AIR TEMP. "C

-^ S?s

=°-DmHS

SPECIAL OBSERVATIONS

COLOR CODE

TRANS.

DIR.

SPHD

0« FORCE

DRY BULB

WET

BULB

23

S12

091

056

033

8

03

MfSSENO" rAST ""' •> NO.

HR 1/)0

CARD

TYPE

DEPTH Im)

T -C

s ■/„

SIGMA-T

SPECIFIC VOLUME ANOMALI-tlD'

SAD

DVN. M.

X 10'

SOUND

vELOcirr

Ol ml/1

PO4-P

rOTAL-P

NOi-N ug - al/l

NOj-N ua - Qt/I

S104-Si

ng - Qi/I

pH

S

c c

STD

0000

0328

3300

2629

0017421

0000

14611

239

OBS 0000 0328 33000 2629 14611 STD 0010 0327 3300 2629 0017441 0017 14612

239

OBS 0010 0327 32997 2629 14612 STD 0020 0296 3301 2632 0017086 0035 14601 STD 0030 0236 3304 2640 0016387 0051 14577

239

DBS

0049

0039

33135

2660

14493

REFERENCE

SHIP CODE

LATITUDE

1/10

0°

MARSDEN

STATION

TIME

ORIGINATOR'S

DEPTH

MAX.

WAVE

WEA- THER CODE

CLOUD CODES

ODC

CIPT

coot

ID. NO.

LONGITUDE

•1/10

CRUISE NO.

STATION NUMBER

TO BOTTOM

OF S'MPL'S

NUMBER

10'

r

MO

DAY

HR,1/10

Oii-

MGT PER StA

ltR( AM

31

540

FV

4257

N

05004 W

150

20

Ti

25

oin

1965

003

9404 D128

nl

??

4 2

XI

3 2

0170

WATER

WIND

BARO- METER

(mbll

AIR TEMP. X:

VIS,

coo

NO.

OBS. DEPTHS

SPECIAL

OBSERVATIONS

COLOR CODE

TRANS.

DIR.

SPEED

OR FORCE

DRY BULB

WET

BULB

22

S12

098

056

033

6

03

MES!ENG»lcAST

T.ME 0, NO. HR 1/10

CARD TYPE

DEPTH (m)

T "C

s •/..

SIGMA-T

SPfCIF'C VOLUME ANOMAII-«10'

SAD

OYN. M.

1 10'

SOUND VELOCITY

03 ml/I

rot-p

„t • ol/l

TOTAl-R

NO;-N

vg - ol/l

N0]-N

no - al/l

SI04-Si

PS - Ol/l

pH

s c c

STD

0000

0303

3301

2632

0017164

0000

14600

010

OBS 0000 0303 33006 2632 14600

STO 0010 0170 3315 2654 0015075 0016 14546

STD 0020 0062 3327 2670 0013508 0030 14501

010

OBS 0024 0025 33312 2675 14485

STD 0030 0026 3332 2676 0012906 0044 14486

STD 0050 0028 3336 2679 0012616 0069 14491

STO 0075 0031 3341 2683 0012245 0100 14497

01

D

OB

3

0097

OC

33

4

56

268'

r

14503

REFERENCE

SHIP CODE

LATITUDE

1/10

LONGITUDE ' -1/10

°i

MARSDEN

STATION

TIME

ORIGINATOR'S

DEPTH

MAX.

WAVE

WEA- THER

CODE

CLOUD CODES

>JODC

CIRV

CODE

ID.

NO.

CRUISE NO.

STATION NUMBER

TO

BOTTOM

OF

S"MPL-S

STATION NUMBER

10*

r

MO

DAY

HR.1/10

OiR-

HGI PER SEA

UPl AM

31

S4n

EV

4

244

N

05004 W

150

20

•)5

?5

:)?4

1965

003

9405

5845

06

26

3 3

XI

4 2

0171

WATER

WIND

BARO- METER (mbtl

AIR TEMP, r

VIS. COD

NO.

OBS.

DEPTHS

SPECIAL OBSERVATIONS

COLOR CODE

TRANS.

DIH.

SPEED

fORCt

DRY

BULB

WET BULB

24

S16

105

044

039

8

07

MESStNGR

TIME c

HR I/IO

CAST NO.

CARD TYPE

DEPTH (ml

T -C

s •/..

SIGMA-T

SPECIFIC VOLUME ANOMALT-XIO'

SAD

OYN. M.

X 10^

SOUND VELOCITY

0; ml/I

PO4-P

vg • ol/l

TOTAL-P vg - ol/l

N03-N

ug - Qt/I

NO3-N WB - o'/l

SIO4-S.

ng-ol/l

pH

5 C

c

STD

0000

0165

3299

2641

0016256

0000

14540

024

DBS STD STD

0000 0165 32990 2641 14540 0010 0165 3300 2642 0016219 0016 14541 0020 0165 3300 2642 0016182 0032 14543

024

OBS STD

0025 0165 33002 2642 14544 0030 0149 3316 2656 0014663 0048 14540

024

OBS STD STD STD STD

0047 0108 33619 2695 14531 0050 0113 3365 2697 0010914 0074 14534 0075 0150 3385 2711 0009642 0099 14557 0100 0184 3404 2724 0008452 0122 14579 0125 0216 3421 2735 0007420 0142 14599

024

OBS STD STD STD STD

0144 0238 34329 2743 14614 0150 0244 3435 2744 0006602 0159 14618 0200 0287 3449 2751 0005949 0191 14646 0250 0323 3462 2758 0005341 0219 14672 0300 0352 3472 2763 0004915 0245 14694

024

OBS STD

STD

0382 0384 34837 2769 14723 0400 0384 3484 2770 0004434 0291 14726 0500 0383 3487 2772 0004291 0335 14742

024

OBS

ST3

T0572 0382 34880 2773 14754 0600 0380 3488 2773 0004276 0378 14758

02

4

OB

5

T0616

0'

J78

34

8

79

27

7

}

14-J

59

155

REFERENCE	SHIP CODE	LATITUDE VIO	LONGITUDE * '1/10	n	MARSDEN	STATION Tl	WE			ORIGINATOR'S	DEPTH	MAX.		WAVE		WEA- THER CODE	CLOUD CODES
cruT CODE	ID. NO.				CRUISE NO.	STATION NUMBER	TO BOTTOM	OF S'MPL-S			STATION NUMBER
10-	r	MO	DAT H	.1/10	OIR-	HC nt SEA	lYPt AM
31	540	FV	4213	N	05005 W	150	20	35	25 0	57	1965	003	9405 3109	11	?^	2 3	XI	4 2	0172
			WATER	w	INO	BARO- METER Imbt)	AIR TEMP. "C	.,„ NO.	SPECIAL OBSERVATIONS
	COLOR CODE	TRANS.	DIR.	SPEED OR fORCE	DRY BULB	WET BULB
				25	Sll	102	056	044	8	10
	»ESSI~G.lcASI IIME 0 NO. HH 1/10	CARD TYPE	DEPTH Iml	I -c	s •/..	SIGMA-T	SPECIFIC VOLUME ANOMALT->ia'	SAD DYN. M. X 10>	SOUND VELOCITT	0 2 ml/l	PO*-P	lOTAL-P	NOj-N us - ol/l	NOj-N „B - ol/l	SI 0<-Si ua - ol/l	PH	S c c
		STO	0000	0452	3317	2630	0017324	0000	14666
057	CBS	0000 0452 33157	2630 14666
	STD	0010 0419 3317	2634 0016974 0017 14554
	STD	0020 0394 3317	2535 0016719 0034 14545
057	OBS	0025 0384 33176	2638 14641
	STD	0030 0395 3331	2647 0015707 0050 14548
	STD	0050 0435 3380	2582 0012451 0078 14575
	STD	0075 0489 3425	2712 0009578 0105 14708
	STO	0100 0541 3456	2730 0007953 0128 14738
057	OBS	0121 0585 34688	2735 14761
	STD	0125 0572 3469	2735 0007390 0147 14756
057	OBS	0145 0539 34694	2741 14745
	STD	0150 0555 3473	2742 0005912 0165 14754
057	OBS	0193 0554 35023	2751 14808
	STD	0200 0655 3502	2752 0006080 0197 14806
	STD	0250 0598 3500	2758 0005565 0226 14791
	STD	0300 0549 3499	2763 0005095 0253 14779
057	OBS	T0389 0482 34968	2769 14766
	STD	0400 0479 3497	2770 0004543 0301 14767
	STD	0500 0453 3497	2773 0004344 0346 14773
057	OBS	0587 0429 34969	2775 14777
	STO	0600 0423 3496	2775 0004167 0388 14777
	STD	0700 0387 3492	2776 0004148 0430 14778
057	OBS	0789 0355 34905	2777 14783
	STD	0800 0365 3491	2777 0004073 0471 14785
	STD	0900 0356 3491	2777 0004153 0512 14802
	STD	1000 0355 3491	2777 0004234 0554 14818
057	OBS	1017 0355 34913	2777 14821
	STD	1100 0364 3492	2778 0004232 0596 14835
		057	OBS	T1129		0364	34920	2778								14839

REFERENCE

SHIP CODE

LATITUDE

1/10

LONGITUDE

' -1/10

if

MARSDEN

STATION

TIME

ORIGINATOR'S

DEPTH

MAX. DEPTH

OF S*MPL-S

WAVE

WEA- THER

CODE

CLOUD CODES

■JOOC

CTRY CODE

ID.

NO.

YEAR

CRUISE NO.

STATION

NUMBER

TO

BOTTOM

STATION NUMBER

10-

r

MO

DAY

HH.1/10

DIB.

HGT P(R SE*

irPi *M

31

540

EV

«

140

N

05004 W

150

10

D5

25

115

1965

003

9407

3566

11

31

2 2

XI

4 2

0173

WATER

WIND

BARO- METER

(mbl)

AIR TEMP. "C

VIS. COD

NO. OBS.

DEPTHS

SPECIAL OBSERVAnONS

COLOR CODE

TWNS.

DIR.

into

OB FOUCI

DRY BULB

WET BULB

32

S14

115

106

067

B

09

MESSENGR

YIMt 0

HR t/io'

CAST NO.

CARD TYPE

DEPTH (ml

T -C

s •/..

SIGMA-T

SPECIFIC wOlUMt ANOMALI-IlO'

SAD

OVN. M,

X 10'

SOUND VELOCITY

Ol ml/l

PO4-P

TOTAL-r

NO3-N

ug • or/I

NOj-N

vg - Ql/I

SI 0«-Si wg - or/I

pH

s

c c

STD

0000

1515

3600

2673

0013277

0000 i 15091

115

OBS

STO STD STD STD

0000 1515 35998 2573 15091 0010 1515 3600 2672 0013311 0013 15092 0020 1515 3600 2672 0013354 0027 15094 0030 1515 3599 2672 0013388 0040 15096 0050 1514 3599 2672 0013456 0057 15099

115

OBS STO STD STD STD

0059 1514 35990 2672 15100 0075 1481 3593 2675 0013288 0100 15092 0100 1430 3583 2678 0013035 0133 15078 0125 1381 3575 2582 0012697 0165 15065 0150 1333 3557 2685 0012395 0197 15053

115

OBS STD STD

0195 1249 35544 2593 15030 0200 1241 3553 2594 0011777 0257 15028 0250 1153 3542 2702 0011076 0314 15005

115

OBS STD

T0252 1149 35418 2703 15004 0300 1009 3527 2717 0009763 0366 14960

115

OBS STD STD

0385 0805 35080 2735 14895 0400 0778 3507 2738 0007755 0454 14887 0500 0626 3501 2755 0006215 0524 14844

115

OBS STD STD

T0575 0545 34989 2753 14823 0600 0534 3499 2755 0005292 0581 14823 0700 0494 3500 2770 0004833 0632 14823

115

OBS STO STO

0771 0470 35001 2773 14825 0800 0462 3499 2773 0004621 0679 14826 0900 0436 3498 2775 0004478 0725 14832

115

OBS STD STD

T0987 0417 34962 2776 14838 1000 0414 3495 2776 0004454 0770 14839 1100 0397 3495 2777 0004412 0814 14849

11

5

OB

5

1126

0

J93

3A

9

4^

27

7

r

148

51

156

REFERENCE

SHIP CODE

LATITUDE

I/IO

LONGITUDE ■ ■1/10

li

MABSDEN

STATION

Tl

'M

ORIGINATOR'S

DEPTH

MAX

■

WAVE

WEA.

THER CODE

CLOUD CODES

^ODC

CTRT CODE

ID. NO.

CRUISE NO.

STATION

NUMBER

TO BOTTOM

OF S'MPL'S

STATION NUMBER

10'

1"

MO

DAY

HR.1/10

DIR.

HGi n» sf*

ItP( AM

31

540

EV

I

232

N

05011 W

150

20

35

25

168

1965

003

9408 2614

12

?4

1 2

XI

0 1

0174

WATER

WIND

BARO- METER

(mbtl

AIR TfMP. t

"=.dEs

SPECIAL

OBSERVAHONS

COLOR CODE

IHANS.

OIR.

SPIED

01 fOBCt

DRT BULB

WET BULB

26

S12

098

061

044

8

12

MESSfNC*

tIMl 0

HR 1/10 '

CAST NO.

CARD TYPE

DEPTH (ml

T -C

s •/..

SIGMA-T

SPECIFIC VOlUMt

ANOMAIT-IIO'

SAD

DYN. M. X 10'

SOUND VELOCITY

Ol ml/I

P04-P

t.g - ol/l

rOTAL-P

Vfl - ot/(

NO3-N

UB - ol/l

NOj-N

vg - oi/l

SI D4-S. UQ . ol/l

pM

S

c c

STD

0000

0435

3334

2645

0015882

0000

14661

168

OBS STD STO STD

0000 0435 33336 2645 14661 0010 0422 3336 2649 0015551 0016 14657 0020 0396 3339 2654 0015089 0031 14649 0030 0357 3342 2660 0014520 0046 14634

168

OBS STD

0032 0348 33427 2661 14631 0050 0232 3375 2697 0010990 0071 14588

168

OBS STD STD

0052 0225 33788 2700 14586 0075 0330 3431 2733 0007604 0095 14642 0100 0443 3459 2744 0006643 0112 14698

168

OBS STD

0112 0498 34625 2740 14723 0125 0444 3457 2742 0006826 0129 14702

168

OBS STD STD STO

0128 0433 34560 2742 14698 0150 0439 3462 2746 0006418 0146 14704 0200 0451 3474 2755 0005707 0176 14719 0250 0464 3483 2760 0005227 0203 14734

168

OBS STD

0275 0470 34856 2762 14741 0300 0434 3486 2756 0004707 0228 14730

168

OBS STO

T0381 0426 34887 2759 14741 0400 0454 3494 2770 0004453 0274 14756

168

OBS STD STD

0411 0468 34973 2771 14764 0500 0432 3495 2773 0004243 0318 14764 0600 0402 3493 2775 0004150 0360 14757

168

OBS STD STD

0619 0397 34929 2775 14769 0700 0385 3492 2776 0004103 0401 14777 0800 0375 3492 2777 0004139 0442 14789

168

OBS

STD STD

T0831 0373 34912 2777 14793 0900 0374 3492 2777 0004195 0484 14805 1000 0375 3493 2777 0004234 0525 14822

168

OBS

STD

T1058 0375 34930 2778 14832 1100 0369 3492 2778 0004292 0559 14837

168

OBS

1171

0353

34906

2778

14842

* U.S GOVERNMENT PRINTING OFFICE : 1966 O — 2t5-485

157

f