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
53°
52°
51'
50°
49°
4 8° 47° 46° 45°
48°
47'
46°
T.
1 — r
44°
48°
'?^ — *-
-X k\x X K K X *—* «/-» ^1
< N« *
45°
44°
\
_ \
43°
42°
47°
46'
45°
44°
- 43'
•— TRACKLINE-1965
* TRADITIONAL TRACKLINE
42°
- 41'
53° 52°
50° 49°
48'
47° 46° 45° 44°
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'
49*
48*
47*
45'
44'
43'
42*
FROM DATA COLLECTED II -12 APRI L 1965
z
UJ
UJ
111 K
-I
z o
^u
in
S
I
o
I I I I I
10 20 30 40 50
CURRErrr velocity cm/sec
I I
I I
45*
440
43*
420
50*
49'
48*
47*
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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TEMPERATURE "C
8
3 .4 .5 .6 .7 .8 .9 35.0
Figure 7A. Mean temperature-salinity plot of all stations on the first and third surveys situated in the Labrador
Current during 1965.
49°25W
971.20
K 971.10
UJ
I-
^ 971.00
< 970.90 -
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^L'lL-^-n.,.,
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a.
INBOARD
BANKS
STATIONS
:^^.: -..D...- •
9260
i«=^=X
9306
X-
THROUGH
STATIONS
FIRST SURVEY (3 APRIL) STATION 9256-9260
CHECK SURVEY (12 APRIL) STATION 9302-9306
THIRD SURVEY (23 MAY) STATI 0 N 939 1 - 9387
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
9256
TEMPERATURE °C
9257 9258 9259
t 300
:::-:->:-:':'!>t-,,.__
y/
;;•>;■;■;■;■:■:•>;■;■;■•■ -:■: ■■■.■X;:;;;;-;-;^^
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CHECK SURVEY
9302 9303
0 C
TEMPERATURE "C
9304
400
500
9302 9303
100
S 200
iij
o
t
UI
u 300
400
500
SALINITY %.
9304
9305
_3
3 5 ^^
34 0 y^
/ 34 5
■
THIRD SURVEY
9391
300
500
TEMPERATURE "C
9389
100
200
g 300
SALINITY %.
9390 9389
9388
^
~ 33 0 "
335
34,0
34,5
-
Figure 94. Temperature and salinity Histribiitioti along section U for the first, check and third Ice Patrol surveys
1965.
20
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21
FIRST SURVEY
TEMPERATURE "C AND FLOW VELOCITY cm/sec
5 300
TEMPERATURE
FLOW VELOCITY
CHECK SURVEY
TEMPERATURE "C AND FLOW VELOCITY cm/sec
9302 9303 9304 9305
THIRD SURVEY
TEMPERATURE °C AND FLOW VELOCITY cm/sec
9389
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
33.4
VOLUME FLOW m'xl0 6/sec
33.3
33.2
33.
33.0
32.9
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
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4- + -
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FIRST SURVEY -50 METER LEVEL
■
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48*
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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
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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
6 May 1965
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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V
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73
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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
000
JLL
32 kt
WEA-
THER
CODE
0005
DEPTH Im
SOUND
VELOCITY
056
056
056
056
056
056
STD
OBS
STD
STD
STD
OBS
OBS
STD
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
3289
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
089
089
089
089
089
STO
OBS
STD
STD
STO
OBS
STD
OBS
STD
STD
OBS
OBS
STD
OBS
OBS
OBS
OBS
STD
OBS
STD
OBS
STD
STD
OBS
STO
STD
OBS
STO
STD
OBS
STD
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*88
3*880
3*88
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
I*PE *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
*NOm*L»->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
STD
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
3514
35143
3502
34798
3479
3475
34742
3497
34974
34920
3494
34944
3494
3493
34931
3495
3497
34968
3496
3495
34952
3495
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
131
131
STO
OBS
STO
STO
STD
STO
STD
STO
STO
OBS
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
3577
3577
3577
3577
3577
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
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
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
-0020
-0021
-0021
0008
0016
00*4
0063
33200
3320
3321
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
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
-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
OBS
STD
OBS
STD
STD
STD
STD
OBS
OBS
STD
OBS
STD
STD
OBS
STD
OBS
STD
STD
OBS
STD
STD
OBS
STD
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
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
092
092
092
092
092
STD
OBS
STD
STO
OBS
STD
STD
OBS
STO
OBS
STD
STD
STD
OBS
STD
STD
STD
OBS
STD
OBS
STD
STD
OBS
STD
STD
OBS
STD
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
2707
2599
2595
2577P
2599
2714
2719
2722
2724
2725
2728
2731
2737
2740
2753
2753
2755
2771
2772
2774
2775
2775
2776
2777
2777
2777
2778
2778
2778
2778
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
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
STD
STD
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
3445
3446
34457
3444
34327
3433
3433
3434
34337
34802
3481
3488
3492
34950
3495
3492
34917
3492
3492
34920
3491
3491
34905
3491
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
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
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
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
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
3489
34894
3489
3490
34901
3490
3490
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
-0052
-0054
-0065
-0057
-0058
-0057
-0057
-0007
0045
0094
0139
0154
0209
0267
0314
0373
0374
0382
0388
3329
33285
3329
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
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
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
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
018
STO
CBS
OBS
STO
OBS
STD
STD
STD
OBS
0000
0000
0008
0010
0015
0020
0030
0050
0050
0091
0091
0066
00*3
-0007
-0007
-0008
-0009
-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
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
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
139
STD
OBS
STD
STD
OBS
STD
OBS
STD
OBS
STD
STD
STD
OBS
STD
STD
OBS
STD
STD
STD
OBS
STD
STD
OBS
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
3494
34931
3493
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
*NOM*LT-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
OBS
STD
STD
STD
OBS
STD
STD
STD
OBS
STD
STD
OBS
STD
STD
OBS
STD
STD
OBS
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
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
OBS
STD
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
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
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
STD
STD
STD
OBS
OBS
0000
0000
0010
0020
0026
0030
0050
0075
0088
0100
0125
0150
0166
T0181
-0054
-0054
-0056
-0058
-0059
-0072
-0123
-0153
-0154
-0100
-0015
0035
0050
0050
3288
32878
3288
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
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
-0079
-0082
-0085
-0091
-0091
-0105
-0125
-0137
-0128
-0103
-0096
-0015
0034
0047
0066
0144
3286
32860
3286
3287
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
094
094
STD
OBS
STD
STD
OBS
STD
OBS
STD
OBS
OBS
STD
STO
STD
OBS
STD
STD
OBS
STD
OBS
STD
STD
OBS
STD
STD
OBS
STD
STD
OBS
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
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
141
STO
OBS
STD
STD
STD
STD
STD
OBS
STD
OBS
STD
STD
STD
STD
OBS
STD
OBS
STD
STD
OBS
STD
STD
OBS
STD
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
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
167
167
157
167
167
STD
OBS
STD
STD
OBS
STD
OBS
STD
STD
OBS
STD
OBS
STD
STD
STD
STD
STD
OBS
STD
OBS
STD
STD
OBS
STD
STD
OBS
STD
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
3397
33966
3414
34151
3424
3435
34367
3451
34634
3464
3468
3475
3480
3483
34831
3484
34838
3486
3488
34884
3489
3490
34902
3490
3490
34902
3490
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
063
063
063
063
STD
OBS
STD
OBS
STD
STD
OBS
STD
OBS
STD
STD
STD
STD
STD
OBS
STD
STD
OBS
STD
STD
OBS
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
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
OBS
STD
OBS
STD
OBS
STD
OBS
STD
STD
STD
STD
OBS
STD
STD
OBS
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
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
STD
OBS
STD
STD
OBS
STD
OBS
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
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
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
037
037
037
037
037
STO
OBS
ST3
OBS
STD
STD
STD
OBS
STD
STD
STD
OBS
STD
OBS
STD
STD
OBS
STD
OBS
STD
STD
OBS
STD
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
3490
34895
3490
3490
34898
3490
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
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
01*0
0057
0005
-00*4
-0111
-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
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
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
*NOM*L'-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
OBS
STD
STD
STD
STD
OBS
STD
STD
OBS
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
3490
34902
3490
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
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
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
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
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
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
229
STD
OBS
STD
STD
OBS
STD
STD
OBS
STD
OBS
STD
OBS
STD
OBS
STD
OBS
0000
0000
0010
0020
0025
0030
0050
0062
0075
0088
0100
0114
0125
0129
0150
0165
0280
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
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
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
151
151
151
STD
OBS
STD
OBS
STD
OBS
STD
STD
OBS
STD
STD
STD
OBS
STD
OBS
STD
STD
OBS
STD
OBS
STD
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
3488
34888
3489
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
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
214
214
214
STD
OBS
STD
OBS
STD
STO
OBS
STD
STD
OBS
STD
STD
STD
STD
OBS
STO
OBS
STD
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
3491
34913
3492
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
015
015
015
015
015
015
STO
OBS
STD
STD
OBS
STD
STD
OBS
STD
STO
STO
STD
STD
OBS
STD
STD
OBS
STD
OBS
STO
STD
OBS
STD
STD
OBS
STD
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
3408
34100
3411
3420
3428
3436
3450
34509
3464
3473
34736
3482
34817
3485
3487
34873
3489
3491
34910
3492
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
048
048
048
048
STD
OBS
STO
STO
OBS
STO
STO
OBS
STD
STD
OBS
STO
OBS
STO
OBS
STD
OBS
STD
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
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
092
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
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
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
006
006
006
006
STD
CBS
STD
STD
STD
OBS
STD
STD
OBS
STD
STD
STD
STD
OBS
STD
OBS
STD
STD
OBS
STD
STD
OBS
STD
STD
OBS
STD
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
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
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
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
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