UNITED STATES COAST GUARD OCEANOGRAPHIC REPORT No. 12 CG 373-12 OCEANOGRAPHY OF THE LABRADOR SEA IN THE VICINITY OF HUDSON STRAIT IN 1965 UNITED STATES COAST GUARD OCEANOGRAPHIC UNITED STATES COAST GUARD OCEANOGRAPHIC UNIT DATA LIBRARY' woods Hole Ocea™9*^ REPORT No. 12 CG 373-12 OCEANOGRAPHY OF THE LABRADOR SEA IN THE VICINITY OF HUDSON STRAIT IN 1965 Ronald C. Kollmeyer David A. McGill Nathaniel Corivin — f\i in ?'-- :c\) £ o J o 5 = 0 CO = o WASHINGTON, D.C. $ MARCH 1967 ii Abstract From the data collected on the Labrador Current Expedition, July- August 1965, there is indicated substantiation of the current system defined by Smith (1937), "Marion Expedition." The data further shows that Hudson Strait exercises a control on the Labrador Current to the extent that a characteristic water tyjie is formed and pulsed eastward by tidal variations through tlie strait entrance, fonning the cold core and main flow of the Labrador Current. Contributions from the Baffin Land Current, flowing westward into Hudson Strait along the northern shore, appear to form one of the mixing constituents; with Hudson Bay acting as a modifier tending to warm and dilute the waters prior to their outflow along the southern shore of Hudson Strait. Ill CONTENTS Page Contribution to and efl'ect of the Hudson Strait outflow on the Labrador Current Abstract iii Introduction 1 Narrative 2 Data treatment 3 Isentropic analysis 5 Dynamic height charts 7 • Property distributions 9 Temperat ure-sahnity relationships 10 Temperature-time study 11 Mean salinity distributions 11 Volume flow 12 Futvu'e work 14 Summary 14 References 15 Illustrations 16 Nutrient distributions along the Labrador and Baffin Island Coast, 1965 Methods 35 Distribution of nutrients 35 Discussion 36 Bibliography 38 Illustrations 40 Tables 37 Tables of oceanographic data 42 Illustrations Contribution to and Effect of the Hudson Strait Outflow on the Labrador Current Figure ^age 1 . Oceanographic station sampling array 16 2. Dynamic height contours, MARION Expedition 17 3. Solenoid division for volume, mass and heat transport calculations, Baffin Land Current 18 4. Solenoid division for volmne, mass and heat transport calculations. Resolution Island 18 5. Thermocline, temperature minimum and nitrite maximum 19 6. Depth plot of the 26.2 sigma-t surface with nitrite contours 20 7. Depth plot of 27.0 sigma-t siu-face with nitrite contours 21 8. Surface dynamic height chart of survey area 22 9. T-S relationships of 17 years of data 23 10. Temperature distribution in northern Labrador Sea 24 1 1 . Salinity distribution in northern Labrador Sea 25 12. Temperature distribution in vicinity of Hudson Strait 26 13. Salinity distribution in vicinity of Hudson Strait 27 14. Temperature distribution in southwestern and central Labrador Sea... 28 15. Sahnity distribution in southwestern and central Labrador Sea 29 16. T-S relationships in the vicinity of Hudson Strait 30 17. T-S relationships in the entrance to Hudson Strait 31 IS. ELEBT time series study 32 19. Mean salinity of sections in the vicinity of Hudson Strait 33 20. Net volume flow and salt transport of sections in vicinity of Hudson Strait 34 Nutrient Distributions Along the Labrador and Baffin Island Coast, 1965 1. Vertical distribution of nitrite-nitrogen, section E, F, G, and H 40 2. Vertical distribution of nitrite-nitrogen, sections A, B, C, D, and D' 41 Tables Nutrient Distributions Along the Labrador and Baffin Island Coast, 1965 I. Relative changes in concentration among the nutrient elements in coastal sections near Labrador and Baffin Island 37 II. Distribution of total organic phosphorus for coastal sections near Labrador and Baffin Island 37 VI Contribution to and Effect of the Hudson Strait Outflow on the Labrador Current By Ronald C. Kollmeter, U.S. Coast Guard INTRODUCTION An oceanogi-aphio expedition to the western Labrador Sea, under the control of the Interna- tional Ice Patrol Section of the Coast Guard Oceanographic Unit, Washington, D.C., was con- ducted during July and August of 1965. The purpose of the expedition was to gather quantita- tive physical and chemical data from the upper reaches of the Labrador Current. The survey trackline and station locations are shown in figure 1. Knowledge of the circulation of the upper reaches of the Labrador Current, and its relation- ship to the Hudson Strait entrance, Baffin Land Current, and the western Labrador Sea has been primarily derived from Smith (1937). His stud- ies were based on the various cruises of the Coast Guard cutters MARION and GENERAL GREENE. This work has formed the heart of the published information concerning the area. In recent years, Dunbar (1951) has discussed the entire region, including the area west of the Hud- son Strait entrance and cited the lack of quantita- tive knowledge in the Baffin Bay, Labrador Sea, and Hudson Strait areas. The main circulation features postulated by Smith (1937) are shown in figure 2. The pri- mary interest of the present investigation con- ducted by the International Ice Patrol, centers around the entrance to Hudson Strait. As can be seen. Smith depicts much of the Baffin Land Cur- rent being deflected into Hudson Strait both north and south of Resolution Island. He also shows a large outpouring from Hudson Strait just north of Cape Chidley. The area outlined in figure 2 could be tagged as the "birthplace" of the Labra- dor Current. Smith (1937) points out that in this area three water masses join to form the south- ward flowing Labrador Current which can be fol- lowed down to the southern tip of the Grand Banks of Newfoundland. He envisioned the Baf- fin Current, from the north, joining and mixing with both the Hudson Strait outflowing and the recurved West Greenland Current, resulting in the formation of the characteristic Labrador Current. This joining of the water masses ac- counted for the two distinct bands or filaments of the current; an inshore portion, cold and low in salinity, and an ofl'shore portion of warmer more highly saline water moving swiftly along the shelf break. Smith postulated the circulation in and out of Hudson Strait from iceberg and sea ice observa- tions. He noted the lines of icebergs moving into the strait on the northern side and iceberg move- ment out of the strait along the southern limits, off Cape Chidley. He also noted the rather diffuse movement of the icebergs to the east of Resolu- tion Island indicating a definite weakening of the southward flow in that area. This information was supported by many oceanographic stations to the east of Resolution Island, but only four sta- tions across the entrance to Hudson Strait. These four stations were insufficient to describe the prop- erty distribution and did not permit any detailed examination of the quantitative transport and exchange through the strait. No data was obtained by Smith concerning the water exchange just north of Resolution Island. His data north of this area, at the latitude of Loks Land, shows that the Baffin Land Current nar- rows, accelerates and at least in part appears to turn into Hudson Strait through Gabriel Strait. Velocity values calculated by Smith show a much stronger current flowing south of Hudson Strait than was found to the north. This acceler- ation was attributed to both the Hudson Strait discharge and the convergence of the West Green- land Current. Smith also speculates that the land drainage from Hudson Bay Basin alone indicates that the discharge through Hudson Strait probably exceeds the inflow. Campbell (1958) presented the most compre- hensive study to date of the circulation in Hudson Bay, Fox Basin, and Hudson Strait. It was quan- titative in nature and presented the detailed cir- culation features of Hudson Strait which were speculated on by Smith (1937). Campbell's data were obtained during the autumn 1955 and sum- mer 1956 and shows the seasonal influences on the areas. This work provides the complementary data needed to connect the circulation and inter- changes occurring across the entrance to Hudson Strait as found during the subject 1965 expedition. The generalized circulation picture for the noithwestern part of the Labrador Sea is quite clear. The oceanographic sections occupied dur- ing the 1965 expedition were specifically designed to describe in detail the contributions of the water masses that make up the Labrador Current and to quantitatively describe the interchange at the Hudson Strait entrance. Recent findings as to seasonal and annual varia- tions in temperature and volume flow of the Labrador Current has initiated new thoughts con- cerning spring iceberg threat predictions on the Grand Banks. Fluctuations in the heat and vol- ume transport of the Labrador Current, coupled with the variations in available icebergs during the spring, tend to cause the iceberg threat of one year to differ sharply from another. Iceberg mortality during transit from north to south, particularly along the coast of Labrador, is greatly influenced by the temperature and velocity of the Labrador Current. This is particularly true in the current area west of the swiftest flowing boundary fila- ment, flowing along the shelf break, wliich divides the cold, low salinity water to the west from the warm, saltier water of tlie Labrador Sea. This inshore or shelf portion of the Labrador Current acts as the deep freeze which conveys the icebergs south. "Water properties in this current band are characteristically cold, less than 2° C, and low in salinity, less than 34.0%=. This property com- bination results in lighter water than that found in tlie more saline Labrador Sea and accounts for the boundary or frontal zone which generally lies along the shelf break. These horizontal property differences, between the coastal water and the Labrador Sea, sets up the west to east pressure gradient whicli results in the southward trans- port along the western boundary of the Labrador Sea. Smith (1937) points out that variations in tlie amount of light, low salinity water available along the Labrador coast will cause variations in the velocity of both the boundary current filaments and the inshore water mass that carries the icebergs south. Likewise the temperature of this water not only influences the current velocity but also dictates the deterioration rate of the icebergs as they are transported south. An understanding of the origin and control of this characteristic water mass will ultimately allow perfection of ice season severity predictions when combined with knowl- edge of the count of available icebergs which are to be transported south. NARRATIVE The oceanographic expedition was conducted by the CGC EVERGREEN, a 180-foot buoy tender class oceanographic vessel, in support of the Inter- national Ice Patrol. The expedition departed Boston, Mass., on 19 July 1965, and arrived at the first oceanographic station (9409) off the coast of South Wolf Island, Newfoundland, on 25 July 1965. The stations shown on figure 1, were occupied in a serial man- ner, terminating on 13 August 1965, at station number 9508 in the center of the southern end of the Labrador Sea. Sea ice along the coast of Labrador and Baffin Island offered no obstacle to the survey work. Most of the ice fields encountered averaged from two-tenths to four-tenths and generally the ves- sel's speed of advance was maintained at 10 knots making good the base course. Two heavy fields of ice were encountered where the ice had been packed in strings up to 15 feet thick by the wind. The EVERGREEN was delayed approximately 2 hours by these floes which were mostly rotten ice and in general easily pushed aside or cracked apart. Most of this ice was encountered off Cape Dyer, Baffin Island, on the northern most section occupied. No accurate count was kept of the ice- bergs sighted but a gross estimate is that 150 ice- bergs, mostly grounded, were passed and sighted either visually or on radar. Oceanographic stations generally consisted of electronic bathythermograph lowerings, Nansen casts, and bottom sampling. One hundred Nansen casts, sixty-nine core or grab samples, and one hundred forty-five electronic bathythermograms were obtained. The distribution of these sam- plings are shown in figure 1. Teflon-lined water sampling bottles of the Nan- sen type, manufactured by the Ballauf Manu- facturing Co. or the United Machine Co., were used during the expedition. Temperatures were measured with protected deep sea reversing thermometers manufactured by Kicliter and Wiese, Kahl Scientific. Instrument Corp., and Walter H. Kessler Co., Inc. The temperatures were obtained from paired averages and are con- sidered accurate to ±0.01° C. The salinity of each sea water sample collected was measured with an KS-7A inductive salinometer manufactured by Industrial Instruments Corp. It is considered that the precision of measurement was within ±0.005%<. and that the accuracy of the reported salinities is ±0.01%o. Water samples were also obtained for dissolved oxygen analysis by the Modified Winkler method according to the meth- od described by Jacobson et al. (1950). Addi- tional water samples were bottled and frozen for later analyses of the nutrient content by David A. McGill of the Woods Hole Oceanographic Institu- tion, and the results are included as a separate paper. The temperature distribution of the water in the upper 400 meters was examined just prior to making a Nansen cast and at many locations be- tween Nansen stations. This was accomplished by using a Hytech Corp., electronic bathytheiTno- graph (ELBT) Model 480 MOD 1. A standard Phleger, 1 foot, gravity corer was used to obtain samples of the sediments at selected locations. In areas of rock and sand bottoms, clamshell grabbers and orange peel bucket samples were used. These sample^s are still being analyzed, and therefore the data are not presented herein. DATA TREATMENT The temperatui'e and salinity data obtained at each station were processed on the Digital Equip- ment Corp. PDP-5 computer as discussed by O'Hagen (1964), and Morse and O'Hagen (1964). This was accomplished shortly after the comple- tion of each station. Values of sigma-t and dynamic heights based on the 1,000-decibar level were detennined at each sample depth. Computer interjDolation for the Ice Patrol standard levels was performed according to Kollmeyer (1964). The oceanographic work was under the direc- tion of Lt. Comdr. Eonald C. Kollmeyer, USCG, who was assisted by Mr. Thomas C. Wolford, oceanographer, Lt. (jg.) John Goras, USCGR, and Mr. John Flick, electronic technician. Tech- nical assistants were William H. Harrell, sonar- man first class, David J. Wood, sonarman second class, Edward S. Olszewski, sonarman second class, William F. Heller, aerographer's mate sec- ond class, and James D. Brower, aerographer's mate third class. Dynamic heights of the sea surface were sum- med using both observed specific volume anomaly values and the interpolated standard deptii values. Determinations of dynamic heights in shallow water were performed in the manner described by Helland-Hansen (1934). This method assumes that level isosteric surfaces extend from the water- sediment interface, on the continental slope, into the bottom of a point directly below the next serial station. This method allows the extension of the pressure surfaces, related to the 1,000-decibar level of no motion, above the shelf as far as the coast. Facilitation of these shallow water com- putations is accomplished by constructing a prop- erty section, along a line of stations, for both temperature and salinity. The isotherms and isohalines are then extended or extrapolated to points along the bottom. Where doubt existed as to isopleth contours near the bottom, vertical dis- tribution curves of temperature and salinity for the questioned stations were drawn and the re- quired bottom data extrapolated. By this pro- cedure, temperature and salinity values at the bot- tom, beneath each station, were established as well as values at significant points of bottom topog- raphy slope changes. Data points were then available for temperature and salinity values at the standard depths and along the bottom to supple- ment the observed values, thereby providing a close approach to completely describing the water column from the surface to the bottom or 1,000 meters as the case may be. All of the data points of temperature and salinity were then processed in the computer and the i-elative dynamic lieight at each value point determined. Tlie depth values of tlie 26.:2 and '27.0 sigma-t surfaces were interpolated by computer from the complete data array. In addition, the nitrite (NOn — N) concentrations at the depth of these sigma-t surfaces were obtained by computer inter- polation thus allowing prepai'ation of isentropic charts with nitrite concentration contoui's. They are presented in a subsequent section. Volume flow computations were accomplished by a computer program specifically written to pro- vide transport information tlirough vertical prop- erty sections. The program provides volume flow information through solenoids which subdivide a property section into small i-ectangles. The so- lenoids are bounded by the data obtained from adjacent stations at the various standai-d depth levels as sliown in figures 3 and 4. The volume flow information was calculated through each solenoid using the following equations: V=v,„XA A=dXh (1) (2) (3) V= volume flow z)m=mean water velocity within the solenoid A = area of solenoid bounded by station location and standard depths (Z?^ — Z?b)= difference between the mean dy- namic height values of adjacent stations, based on 1000-decibar level, at a point between the upper and lower standard depth values bounding the solenoid y=corioUs force L=distance between adjacent sta- tions d=vevtic&l distance between the standard depth values bounding the solenoid Combining equations (1), (2), and (3): -DB)d y^mD^ / (4) The volume flow calculations are now independ- ent of the distance between adjacent stations. This allows simplified volume flow computations through solenoid located along the bottom in shal- low water. Data points along the bottom at sig- nificant slope changes within a particular solenoid can therefore be treated like data obtained from the nearest station higlier on the slope as shown below. The computer receives the previously determined dynamic height values at the standard deptli boundaries and any values in between for the par- ticular solenoid being examined. It then, com- putes the mean dynamic height within the stand- ard depth boundaries for each of the two stations bounding the solenoid and thus arrives at a figure for {Da — Db). Equation (4) is then automati- cally solved and the volume flow results with tlie dimensions of lO^m^/sec. The direction of flow is indicated by a plus or minus sign in the answer. By the above-described process, an entire sec- tion can be broken into the desired solenoids and tlie entire volume flow, magnitude and direction can be determined. Summations of the solenoids by direction of transport or other unique i)roperty may be made, thus allowing the computation of salt and heat transports. More detail in tlie re- sulting transport description can be obtained by closer vertical sample spacing and by closer station spacing thereby resulting in a greater number of solenoids within a given section. OM 20M lOOM IIOM 120M I40M I50M STA A .574 DM .571 DM STA B , J^ota Points .573DM .562 DM ivS^.560DM OM 20M SAME! loOM '^ ■ I lOM I20M I40M I50M STA A STA -8- ,.574 DM 1 ,.571 DM ,,.569DM ,,.562DM (> ,.560DM ,^ 4, .573DM .562DM .560 DM Property transport of heat and salt were com- puted for each solenoid in the survey sections using the following equations: Q,=Fxr„ (5) where Q,=heat transport °C. m'/sec rm=niean value of the temperature within the solenoid V= volume flow and where M. M,= VXS,nXpn. (6) salt transport (10*) gms/sec mean value of the salinity within the solenoid p„=M' density of seawater \^= volume flow Equation (5) is not a true heat flow calculation, however this method is representative of the heat and allows intercomparison of the heat flow tlirough the various sections. The mean tempera- tures are arrived at for each solenoid by using a weighted mean obtained from the isotherm distri- bution of the property sections. Equation (6) gives the grams of salt transported through each solenoid. The mean salinity was determined, similar to the mean temperature, by using the salinity distribution sections. A mean density (p,„) of 1.03 gms/cm^ was selected to speed com- putations. Actual densities range from 1.025 gms/cm^ to 1.028 gms/cm^. However, the error in rounding to 1.03 gms/cm^ is negligible com- pared to the estimated error of 10 percent for the overall procedure. Figures 3 and 4 show the diagrammatic construc- tion of a volume-salt-heat transport section. Each solenoid contains 6 values resulting from the above calculations. These values are: direction of movement, volume flow, mean temperature, mean salinity, heat flow, and salt transport. Tliis allows the sunnning of the data contained in tlio various solenoids according to the desired pi-es- entation or analyzation of the data. For ex- ample; in this paper direction of movement was considered along with particular water character- istics. Solenoids which contained water at a tem- perature of less than 2.0° C. and a salinity of less than 34.3%o were summed. These solenoids are emphasized in figures 3 and 4 by solid outlines for southward-moving water and dashed for north- ward-moving water. The computer reduction of the volume flow data eliminates the traditional subjective velocity curve drawings and makes the sections more comparable because of their uniformity of treatment. The method is limited by the recognized errors of dynamic height computations in addition to the errors and assumptions included by working in shallow water. It is believed however, that this procedure is as accurate as any indirect method presently in use. ISENTROPIC ANALYSIS Analysis of surfaces of equal entropy was at- tempted for the area adjacent to the entrance to Hudson Strait. Sigma-t surfaces, although not coincident with true isentropic surfaces, are con- sidered a close approach for purposes of analysis. Kollmeyer (1966), depicted the core of the Lab- rador Current using this method and showed pic- torial differences between presenting isotherms at horizontal depth levels versus presenting them on sigma-t surfaces. The isotherms on the sigma-t surfaces clearly displayed the cold core of the Labrador Current whereas the horizontal isotherm plots showed only a west-to-east temperature gradient. A similar treatment of the data is at- tempted herein, except for the fact that nitrite {NO..-N) data are contoured on the sigma-t sur- faces in lieu of temperature data. In addition, the topography of the sigma-t surface is shown. According to Montgomery (1938), the move- ment of the water masses are defined for flow direction by the contours of the property distribu- tion. Nitrites were chosen as tlie property to be contoured because they are independent of the density and the properties which determine den- sity, and form an independent chemical property to examine on the surface. There seems to be some relationship between the maximum nitrite concen- tration and the temperature minimum zones in the area of analysis. Figure 5 shows the depth of location of the temperature minimum and the depth of the nitrite maxinunn. In the areas of the cold cores of the Labrador Current, the nitrite maximum is located well below the minimum tem- perature. In the warmer areas, on the eastern edges near the Labrador Sea and the near-shore water, the minimum temperatures generally coin- cide with the maximum nitrite concentrations. No nitrite minimum is indicated within the cold cores. This separation between tlie temperature minimum and nitrite maximum within the colder water core is of interest because it adds still another property anomaly that may be used in the study of the cold water forming the Labrador Current. At present, the only inference that can be made to the above- mentioned phenomena is that the cold core(s) of the Labrador Current appear to be intrusive in the area. That is to say that the cold cores are filaments moving through water on the shelf which could be considered resident water experi- encing slower movement. This resident water is more at equilibrium with the environmental and biological conditions than the intrusive water. Oceanic areas generally exhibit a nitrite maximum at or just below the thermocline at about 75 metei-s according to Sverdrup, et al. (1942). This is the case, as can be seen in figure 5, for all the waters except the cold cores of the Labrador Current. Li those sections which describe the Baffin Land Current to the north (stations 9477-9508) the nitrite maximum occurs above the temperature minimum ; however, close examination of the data in this area discloses that due to the large amounts of cold homogenized water, the time temperature minimum is not clearly defined. Furthermore, it can be seen that the nitrite maximum actually lies just below the thermocline as in all the other areas shown in figure 5 with the exception of the cold core of the Labrador Current. The nitrite concentrations generally varied widely in vertical and horizontal distributions and, except for a few instances, nitrite was never com- pletely absent. Figure 6 is a plot of the 26.2 sigma-t surface showing both tlie depth contours of the surface and the nitrite concentrations. The striking slope of the sigma-t surface clearly defines the limits of the water with tlie particular density of 1.0262 gms/cm^ A sea surface intersection with the sigma-t surface tends to indicate the movement of the water masses into Hudson Strait on the north- ern side and out the southern side. No water of density of 1.0262 gms/cm^ was found in the section running east of Resolution Island. This indicates the lack of any flow connection, above the 25-meter level, between the water lying to the north and south of Resolution Island. The 26.2 sigma-t surface north of Resolution Is- land intersects the sea surface to the east and south but is relatively flat in topographic description to the west. There exist an almost uniform depth level of about 25 meters which extends west to the coast of Baffin Island. To the south of Resolution Island the 26.2 sigma-t surface slopes nnich more steeply in the strait entrance and along the Labrador coast. Intersection of the sigma-t surface with the bot- tom can be seen near the Labrador coast. The topography, in this area, goes to gi-eater depths and is not flat like that to the north. The surface extends below 100 meters in an area just off the mouth of Hudson Strait and in general lies below the 50-meter depth level. This great difference in depth level, north and south of Resolution Is- land, indicates that greater quantities of lighter water seem to be present south of Resolution Island. The great slope of the sigma-t surfaces imply severe slopes of the isobaric surfaces and qualita- tively indicate the circulation in the area. The contours of the nitrite concentrations tend to sup- port these circulation patterns. It is quite apparent from figure 6 that the water flow is into Hudson Strait north of Resolution Island and out of the strait south of Resolution Island with no north-south flow connection shown for water of this density. The broad contours of nitrites to the north are nondescriptive because of their uniformity. To the south, however, there exists a tongue of higher nitrites emanating from inside the point of Cape Chidley and flowing out in a broad pattern. Somewhat isolated to the east is a second nitrite concentration giving indi- cation of a pulselike structure in the flow pattern coming from the strait. This pulselike structure can also be observed in the depth of the sigma-t surface coincident with this higlier nitrite concen- tration pulse. The topography here dips to a depth in excess of 100 meters, thus indicating a slug or pulse of lighter water moving through the area. Figure 7 shows the 27.0 sigma-t surface. Again, nitrite concentrations as well as the topography are contoured on the sigma-t surface. This sur- face intersects the sea surface in only a limited area just to the northeast of Resolution Island. This is an area of flow direction transition where lighter water, on the left side of the flow pattern moving into Hudson Strait, is in close proximity with the heavier water flowing south, just east of Resolu- tion Island. Here again the general flow patterns are shown in both the slope of the sigma-t surface and the nitrite distribution. The 27.0 sigma-t surface slopes in varying degrees, from a level of 50 meters, westward to intersect with the bottom along both the Baffin Island and Labrador coasts. To the east of Resolution Island, the surface re- mains quite level, at 50 meters, to within 20 miles of the coast and then abruptly deepens southward to a depth in excess of 250 meters. To the north of Resolution Island, the surface dips slightly be- low 150 meters before intersecting the bottom. Here again is the indication of the existence of lighter water to the south of the entrance to Hud- son Strait. Lesser amounts of this light water exists to the north of the strait entrance and is virtually absent due east of Resolution Island. The circulation depicted by the nitrite concen- tration supports the flow pattern shown by the sigma-t surface slope. Water movement at these depths are indicated as bemg into the strait on the north, and south of Resolution Island and out in the center of the entrance between Resolution Island and Cape Chidley. The outflow of water appears again to assume a slug or pulselike struc- ture described by both the nitrite distribution and the contours of the sigma-t depth topography. In this case the water moving out of the entrance appears to be of minimum nitrite concentration, deflecting or distorting the water of higher con- centrations which are flowing from the north, immediately to the east of Resolution Island. DYNAMIC HEIGHT CHARTS A dynamic height chart of the area adjacent to the entrance to Hudson Strait was constructed to provide quantitative current information. This chart is presented as figure 8. As previously mentioned, all dynamic heights are computed rel- ative to the 1,000-decibar level of assumed no motion. No direct current measurements are available in this area to provide a comparison with absolute values. The concept of "relative"' cur- rents is useful however; because the question of relative contributions of the several water masses in the area to the Labrador Current was the primary concern of the expedition. One basic assumption required in the dynamic treatment of oceanographic data is that of steady state. That is, conditions are such in the area of consideration, that the various forces acting on the water are in a dynamic equilibrium. In the steady state situation, an adequate description of the pressure distribution, resulting from the mass distribution, will describe the water movements relative to a reference level. There exists great doubt as to the existence of any equilibrium attainment of the forces in the vicinity of the entrance of Hudson Strait because of tides and the resulting tidal currents. These tidal movements result in water being moved in- dependent of the more discrete pressure-mass dis- tribution forces. The tides in this area are semi- diurnal and relatively equal. With a discrete pressure-mass distribution force impressed on the oscillating tidal movement, the resulting net move- ment would be governed by the direction of the pressure-mass distribution force. It would be ex- pected that this long term net movement would be reflected in a description of the mass distribu- tion obtained from the point sampling of tempera- ture and salinity. A major redistribution of the mass features in the entrance of Hudson Strait by the tidal currents seems unlikely because of the di- rectional changes of the tidal currents every 6 hours. With the quantities of water present, the time frame for redistribution appears much t«o short. The current and volume flow data calculated from the mass distribution in the area would cer- tainly not be representative of the instantaneous particle movement, but should be representative of the longer period movement tendencies. These tendencies depicted by the mass distribution should be comparable between the sections of the survey area. With this assumption in mind, the dynamics of the area are presented and extended, in a later section, to include volume flow computations. Figure (8) shows the surface circulation in and near the entrance to Hudson Strait. The circula- tion, deduced by the dynamic method matches quite well with qualitative flow depicted from the isentropic distributions. A broad low-velocity BaflSn Land current flows from the north towards the entrance to Hudson Strait. A turning to the right of the inshore filaments occurs, resulting in water movement into the strait north of Resolu- tion Island. A convergence of the broad current band located further offshore occurs along with a commensurate acceleration. This jet then flows in to Hudson Strait just to the south of Resolution Island. This is exactly what was indicated on the 27.0 sigma-t level shown in figure (7). The 26.2 sigma-t level, however, showed a shallow flow into the strait north of Resolution Island. The section east of Resolution Island has rela- tively flat topography except for the first two sta- tions near the island. The surface waters seem to meander from offshore in towards the island with the 971.0 dynamic meter contour demarking the outboard extremity of the convergence men- tioned above. Watei-s further offshore make a slow circuitous trip towards the strait and then turn back to the east under the influence of the outflow of Hudson Strait. The east-west section off Resolution Island is the area where Smith (1937) cited the delay or hesitation in the move- ment of icebergs during their trip south. To the south of Resolution Island, in the strait entrance, high speed currents are displayed. The northern one-third of the strait lias the strong westerly current discussed above while the south- em two-thirds has a very strong eastward outflow in the center and slight reversal to the west around the islands just to the north of Cape Chidley. A strong outflow in the passage between Cape Chid- ley and the offshore island is also indicated. The water flowing out of the strait turns sharply soutii and commences its passage towards the Grand Banks. The central jet of water pass- ing out of the strait diverges as it turns south. This divergence continues until a broad flat area is developed in the southernmost section of figure 8. To the east of this divergence, offshore waters from the Western Labrador Sea converge to- wards, and are entrained with, the fast-moving filaments of the current. To the west, the dynamic height of the stations along the coast i-equire the topographic contours to be drawn into the coast. This is an unusual situation and points up the limitations of the dynamic method. In the area just to the east of Cape Chidley, the contours also turned severly clockwise and intereect the coast. In the center of this area, the 971.3 dynamic meter contour forms a loop indicating a circular path or eddy in the water. The area thus described by the contour represents a hill, elevated above the waters to the east and south and violated steady state requirements for geostrophic flow. The light water is definitely present, as indicated in the property sections shown later herein, and should ultimately flow towards a lower geopotential level if the assumption of hydrostatic equilibrium at 1000 meters holds. This means that cross isobaric transport will probably take place before geo- strophic flow along the isobare is set up. Witliout any dii'ect current measurements in this area, reference must again be made to tlie isentropic charts of figui'es 6 and 7 for comparison. It can be observed that the flow of water, as depicted by the nitrite concentrations, on both the 26.2 and 27.0 sigma-t surfaces, indicate water movement to be generally in a southeasterly direction off the Hud- son Strait entrance. This tends to support the dynamics shown in figure 8. To 'be noted here is the expected coincidence of the 971.3 dynamic meter line which describes an eddy off Cape Chidley, with the depression in the 27.0 sigma-t surface thus indicating the large slug or pulse of light water present in the area. There is a distinct possibility that this pulse- like structure of the water is a direct result of pumping action caused by the tides. As pointed out aJbove, the pressure-mass distribution indicates a force moving water out of the strait entrance. This force would become the dominant force at the end of the ebb cuiTent flowing east from the strait entrance. In this situation, resident water from inside the strait would pass through the strait entrance as the tidal currents ebbed and be- gan to turn, thus allowing a net transport out. Tliis pressure-mass force tending to move water out of the strait would have the effect of prolong- ing the ebb current and delaying the start, of the flood. At this time the characteristic water from inside the strait would pass eastward and turn south prior to the tidal cuiTent reversal and the movement of the adjacent waters back into the strait. Because the pressure-mass distribution force is constantly being exerted, less water move.s back into the strait than is moved out. As will be shown in a following section characteristic Labrador Current water was found on both sides of Cape Chidley, but very little was found directly in the entrance to the strait. This can be explained by tlie fact that tlie major amount of water moving in and out of the entrance by tidal action is a moderate mixture of the water found east and west of tlie entrance. Tlie data in the area was obtained during a 12-hour period. The tidal current was ebbing when the stations were ocx^upied in the southern lialf of the entrance, and flooding when stations were occupied in the northern half of the entrance. Because of this, it is believed that the survey vessel was in the wrong part of the strait entrance for observing the outpouring of the char- acteristic Labi-ador Current water at the end of the ebb current. This outpouring probably occui-s just to the north of Cape Chidley and is supplied by the band of cold low salinity water located just 8 inside Cape Chidley. A comparison of this water mass with tliat found outside tlie strait will be made in a following section. PROPERTY DISTRIBUTIONS As stated in the introduction, the main interest of the expedition was to trace, and examine the cir- culation of the cold low salinity water that makes up what is observed as the Labrador Current off the Grand Banks of Newfoundland. The analy- zation of the data herein is therefore confined to the consideration of water of this nature. For the purposes of this analysis, an arbitrary water mass was defined on the basis of l7-year mean temperature-salinity relationships. Shown in fig- ure 9 are tlie mean T-S cui-ves of the three basic water masses found off the Grand Banks. These means are based on International Ice Patrol Sur- veys during the period 1948 to 1964. The point located on the T-S cui-ve for Labrador Current water defines the limits for analysis of water which has a temj^erature of less than 2° C. and a salinity of less than 34.3%o. Tliis point roughly confines this water to the upper 200 meters. Using a limit- ing definition such as this, certain areas contrib- uting water to the volume flow of the Labrador Current are immediately excluded from consider- ation as sources of the cold portion of the current. The boundaries of this cold water are also well defined in the property sections. Only about 5 percent of the cold, low salinity water found, failed to fulfill the T-S requirements. That is, if the water was less then 2° C. it was almost always less than 34.3%^ in salinity. These defined limits encompass broad current areas, above the shelf, just inside the swifter flow- ing boundaiy current. As mentioned previously, this broad current area provides the cold environ- ment in which the iceljergs are transported south. It is also the area of the light water, variations in which cause the volume and velocity fluctuations in the southward flowing current. The salinities and temperature obtained in the various sections vary quite significantly within the above definition. Tliese variations provide the basis for some of the conclusion drawn in subseqent sections herein. Figures 10 througli 15 present the temperature and salinity distribution along the sections ob- tained during the expedition. Inserts in each fig- ure give tlie relative locations of the individual sec- tions. The 2° C. limit is shown by lx)ld lines on each of the temperature sections. As can be seen, the temperature gradients both horizontal and vertical, become much stronger above the 2° C. isotherm. This provides a useful boundary in the analysis of these water masses. Figures 10 and 11 show the water properties in the northern reaches of the expedition and includes the line of stations occupied down the center of the Labrador Sea. Section H, taken halfway across the Davis Strait, shows large quantities of cold low salinity water. This is the only section where a considerable disagreement exists between the relative position of the 2° C. isothenn and the 34.3%o isohaline. In this section, water of higher salinity exists which is much less than 2° C. in temperature. Significant here, however, is the ob- servations that this disagreement exists well below 200 meters and probably represents a water mass of Baffin Bay Basin origin. The section imme- diately to the south, section G has a much shal- lower depth, thus this more saline, denser water is prevented from moving south into the area of interest. Connecting the sections G and H in the west, figures 10 and 11 is section I. Because this section is located in the center of the northern end of the Labrador Sea, it crosses an east to west circulation of portions of the West Greenland Current as well as the eastern edge of the southward flowing Baffin Grand Current. To be noted in this section is the tongue of flow temperature water emanating from Baffin Bay. This tongue narrows and all but dis- appears to the south in this section. This is be- cause of the east-to-west drift, encountered by the outflowing Baffin Bay water which causes a dis- placement to the right towards the coast and out of the limits of section T. To the south, section F shown in figures 12 and 13, running east from Resolution Island shows a lack of water less than 2° C. Water of a salinity of less than 33.0%^ was totally missing. The sec- tions to the north had great quantities of water less than 2° C. and 33.0%^. This supports the cir- culation regime observed in the dynamic height and isentropic charts where little of the water from the north appears to pass through this sec- tion. The water in this section is totally different than that from the north and appears to be sup- plied by water from the east. One small offshore cold core, and a slightly larger core of cold water near Resolution Island are found in the section. These small cold cores appear to be the only con- nection of this section with those to the north. The eastern limits of section F grade warmer and more saline, virtually eliminating any speculation that the water from the north is skirting the east- ernmost stations. With the east eliminated as a pathway for the cold, low-salinity water from the north, section E would therefore represent one route taken by this southward moving water. Section E displays the considerable amounts of cold, low-salinity water expected. The cold core observed in section F, close to Resolution Island represents the other route taken by this water. This flow of water from the north was described in both the dynamic height and the isentropic charts. After leaving section F, the cold water turns to the west, just south of Resolution Island and flows into Hudson Strait. Section D, across the entrance to Hudson Strait, shows cold, low-salinity water in stations 9457 and 9458 just south of Resolution Island. In the deeper half of section D, warmer, higher salinity water is present, similar to that found in section F and probably connected with it. The isotherms and isohalines are severely sloped downward to the south in section D and show the existence of water lower in salinity then has been found thus far. Section D', obtained just inside of the strait entrance shows similar salinities, but much lower temperatures. This same situation exists in sec- tion C, figures 14 and 15, taken east of Cape Chid- ley. Lower salinities then found to the north are present along with reasonably cold water. The circulation has already been shown to be out of the strait through D', D, and C. The water property sections supports this with the exception of the lack of any very cold water directly in the strait entrance, section D. This has been discussed in the previous section and will be mentioned again in the treatment of T-S curves below. The shelf depth to the south of section C be- comes shallower, probably accounting for, in part, the anomalous dynamic height contours and the apparent damming or buildup of low density water in the western half of this section. Section B and A to the south, show the cold, low salinity cores of the Labrador Current. Section J, figures 14 and 15, is presented for general interest showing the imiformity in tem- perature and salinity of the central Labrador Sea down to Ocean Station BRAVO. Only in the north are there any characteristic differences. This small core of lower temperature-salinity water represents the southern boundary of the westward flowing filaments of the West Green- land Current. TEMPERATURE-SALINITY RELATIONSHIPS Figures 16 and 17 show the T-S diagrams for each station taken in the vicinity of the Hudson Strait entrance. On each T-S diagram there is a cross ( + ) giving the location of the upper limits of the defined water mass of 2° C. and 34.3%o. Shown also is a comparative diagram of the 17- year mean of the water mass characteristics of the Labrador Current. Comparing the eastern ends of sections G, F, C, and B of figures 16 and 17, the rather abrupt changeover of the water mass characteristics is apparent. As the easternmost stations are ap- proached, the T-S relationships changes from within the defined limits to completely outside, thus forming a good eastern boundary for later volume analysis. Section F shows very little of the defined water except at stations 9471 and 9470. However, there is still a profound change in the T-S relationships offshore between stations 9465 and 9464. The warm, saline waters located at the eastern ends of these sections are those of the Labrador Sea. The transition zones between the characteristic defined water and that of tlie Labra- dor Sea, are naturally coincident with the swift flowing boundary current shown in the dynamic height chart figure 8. The water characteristics of section E match very well the charactristics of the water to the north in section G. This, as pointed out above, seems to be one of the paths that cold water takes flowing from the north. Stations 9471 and 9470, of section F, are a second path taken by this water as it flows south and can be followed through Hudson Strait entrance, section D, at stations 9458 and 9457. The water flowing south in the vicinity of stations 9469 through 9566 of section F, seems to match characteristics with the waters at stations 9437 and 9436 of section C. This agrees quite well with the dynamics shown in figure 8 where an area of low topographic definition dis- plays a slow meandering current which moves west and then recurves to the southeast and flows through section C. In section D, station 9455 appears to be at the transition zone between the characteristically lower salinity water running out of Hudson Strait and 10 the slightly higher salinity water running in. The T-S diagrams of section D abruptly shift toward the lower salinity values and lower temperatures ,d station 9454. Section C, west of station 9437, exhibits water characteristics much less saline, but not quite as cold as the waters to the north in section G. Lo- cal warming, and some mixing of water from the east, can account for the elevation in temperatures, however, no water from the north or east can con- tribute the low salinity values found in section C. Section D does not contain these low values of salinity either, but they are found in section D'. This section, just to the west of Cape Ohidley, seems to be the source of the low salinity waters of section C even though no good continuity of low salinity water can be shown to connect them. As discussed in a previous section, tidal fluctuations, mixing and improper timing of the survey ship in transiting section D probably accounts for the lack of continuity of the water masses. Section B, to the south, shows low salinity and slightly warmer water. Warming would be ex- pected here as the colder water passed south into shallower shelf areas. The circulation concepts postulated from the dynamic height and the isentropic charts appear to be borne out by tracing the flow patterns using T-S relationships. TEMPERATURE TIME STUDY Presented in figure 18 is a time-series study of the temperature structure of the water in the en- trance to Hudson Strait. The location was in the vicinity of station number 945'2, about 8 miles north of the islands off Cape Chidley. An attempt was made to observe the cold, low salinity water, mov- ing eastward out of the strait from its source southwest of Cape Chidley. ITnfortunately this area turned out to be an area of low geostrophic current. Radar was used to keep the ship's posi- tion fixed and drift plots of the vessels were used to determine the tidal current changes. Figure 18 shows the electronic bathythermograph (ELBT) records obtained in this location along with ELBT records obtained both inside the strait, station 9461, section D' and outside the strait, stations 9444, 9443, section C. Station 9461 is located within the cold, low salinity water mass believed to be the source of the characteristic Labrador Current. The arrival of the colder water, at least as cold as found in quantity in section C, stations 9443 and 9444, can be seen in figure 18. This arrival appears nicely timed with the end of the observed ebb current. The temperature structure shows the increase and decrease in the amount of cold water moving through the strait to be obviously con- nected with the tidal current as hypothesized previously. The failure to obtain a Nansen cast at the time of the arrival of this cold water prevents the proof of lowered salinity of this water, how- ever, from the other evidences presented this is a logical assumption. MEAN SALINITY DISTRIBUTIONS One of the more revealing analyzations of the data is presented in figure 19. Show^l here is the mean salinity of the southward moving water within the defined characteristics of less than 2° C. and 34.3%o. These mean salinities were obtained by using the values of the salt transport and the volume flow in the following equation : S»/oo = Ms Vp where : M5=salt transport V= volume flow p= density of sea water The mean salinities of the water exchanged through the entrance of Hudson Strait were com- puted for both directions of flow because of the large changes in the salt concentration and flow patterns across the entrance. The northernmost section of figure 19, section G, shows a 33.37%o mean salinity for the south- ward flowing Baffin Land Current. Further to the south, this current appears to shed a lower salinity filament which flows into Hudson Strait, north of Resolution Island through section E. The source of this lower salinity filament is the inshore or coastal portion of the Baffin Land Cur- rent. The salinity of the section extending east of Resolution Island, section F, is higher than the Baffin Land Current in section G to the north. This increase in salinity is the result of both the loss of the inshore filament flowing through sec- tion E, and the intrusion of more saline water from the western Labrador Sea. Directly to the south of section F, section C ex- hibits a mean salinity considerably lower than any 11 of the sections to the north. This indicates that a supply of less saline water is being introduced into the circulation of the area. The eastern ap- proaches to this section are eliminated as the source due to the higher salinity of the Labrador Sea. The northern approaches obviously do not contain any significant quantities of low-salinity water. Only the waters outflowing from Hudson Strait are comparable in mean salinities with the waters of section C and section B further to the south. A clear pattern appears in this mean salinity dis- tribution. High-salinity water from the north appears to turn into Hudson Strait, in the north- ern half, while lower salinity water is put into the system from Hudson Strait in the southern half. Campbell (1958) found the circulation in Hud- son Strait to be westward along the northern coast and eastward along the southern coast. He also found a recurving and a mixing of the water flow- ing along the northern shore, with the water to the south. This occui-s roughly midway along the strait and provides the mechanism for altering the high salinity water flowing in, by mixing it with very low salinity water flowing out of Hudson Bay. Campbell (1958) shows the salinity dis- tribution, at 20 meters, for October 1955 and July 1956, in Hudson Strait and the outlet of Hudson Bay. He found a high-salinity inflow into the strait from the east, greater than 33.0%o and an outflow from Hudson Bay of less than 30.0%o. These would be the necessary concentrations for the mixing and formation of the mean salinities observed flowing eastward through the entrance of Hudson Strait. Contributions from other sources in the Hudson Bay, Hudson Strait area are also cited by Campbell. Their existence elim- inates any simplified or unique mixing ratios be- tween BafHn Land Current water and the resident water of HudscFii Bay. Campbell shows the area of recurvature of the inpouring Baffin Land Cur- rent and subsequent mixing with the eastward moving water of Hudson Strait, to be east of the majoi-, resident water sources. The sum total of the low salinity contributions from Hudson Bay and Foxe Channel located just north of Hudson Bay, form the major water masses which combine witli the inflowing Baffin Current, modifying it into a characteristic water mass. Thus the cir- culation system in Hudson Strait appears to ab- sorb tlie high salinity water, mix it with very low salinity water, and eject this mixture as the char- acteristic low salinity water which forms the shelf portion of the Labrador Current. VOLUME FLOW Figure 20 presents the summarized volume flow and salt transport values, in each direction, for the defined water mass. Presented also are the net transports. The question of the validity of the dynamic height calculations was raised in a pre- vious section. The limitations of the dynamic method are carried over into the volume flow and salt transport calculations because they are based on the dynamic heights. The areas bounded by sections G, E, F, and F, D, C should fulfill the requirements of conservation of mass. That is to say, the volume of water and salt flow into a par- ticular closed area, should equal the volume flowing out. The particular area defined above, and shown in figure 20 are bounded either by the sections listed, land masses, or the Labrador Sea which falls outside the defined water mass characteristics of less than 2° C. and 34.3%,,. The sections of G, E, and F, the Baffin Island coast, and the 2° C. isotherm, shown in figure 20, define a closed area which should fulfill the require- ments of mass consen^ation. First looking at the net volume fiow values of figure 20. Section G, net south : 1.85 X 10«mVsec -0.59XlO«mVsec Section E, net west: i.gBXWmVsec This figure compares with net volume trans- port south through section F of 1.07xlO«mVsec. Repeating these computations for the salt trans- port : Section G, net south : 638.0 X 10» gms/sec - 198.9 X10« gms/sec Section E, net east : 439.1 xlO« gms/sec This compares witli tlie net salt transjjort soutli through section F of 371.5 X lO^gms/sec. These in-and-out figures agree within 15 percent for botli volume and salt transport. Extending these comparisions to tlie area south of Resolution Island bounded by sections F, D, and C and the 2° C. isotherm to the east, the following calculations are made : Section F, net south : 1.07X WmVsec + 2.23 X lO^mVsec Section D, net east : " .. 30 x 10«mVsec Comparing this figure with the flow south through section C, the value of 3.57xl0''mVsec 12 can be observed in figure 20. Again repeating for the salt transport. : Section F, net south : 371.5 X lO^ gms/sec ^ . ^ , +731.1X108 gms/sec Section D, net east : ii02.6X 10« gms/sec The outflow south from this area through sec- tion C shows a salt transport, of 1198.2X10* gms/sec. In this area, the in-and-out figures of the volume and salt transport agree within 8 percent. The relatively close agreement of the flow fig- ures, to and from these bounded areas supports the circulation and flow computations deduced from the dynamic heights. It reaffirms the valid- ity of the dynamic method, particularly in shal- low water. A 10 percent accuracy is as good as can be expected in view of the great number of as- sumptions, technique errors, and nonmass related flow forces. It is singularly reassuring, if not surprising, that the percentage agreement shown above is as close as it is. The water exchange through the Hudson Strait entrance, north and south of Resolution Island shows a net flow, to the east, of 1.64:Xl0^mVsec. This volume flowout, accounts for almost 50 per- cent of the net flow to the south through section C. As pointed out in the previous section, high- salinity water flows into Hudson Strait and is mixed, midway up the strait, with low-salinity water moving out of the Hudson Bay, Foxe Chan- nel area. The mean salinity of the net. westward water flow into the Hudson Strait entrance is 33.36%o and the mean salinity of the net outflow is 32.72%o. A simple mixing calculation will show the required salinity of the mixing con- stituent that combines with the inpouring Baffin Land Current water, resulting in the character- istic cold, low salinity water of the shelf portion of the Labrador Current. Referring to figure 20, across the entrance to Hudson Strait, the follow- ing equation is applied : V,Mt = V,Mi + V.M. where Vt = total volume flowout, 4.78 X lO'^mVsec Mt = mean salinity out, 32.72%o Vi=volume flow in, 3.14 X lO^mVsec Mi=mean salinity in, 33.36%o V2 = volume flow of mixing constituent, 1.64 X lO^mVsec Ms = mean salinity of mixing constituent Solving the above equation results in a value for Mo of 31.49%o. This value falls very nicely with- in the approximate limits of the salinities of the water masses available within Hudson Strait, dis- cussed in two previous sections, which undoubt- ably combine and form the mixing constituent for subsequent combination with the Baffin Land Cur- rent water. The volume flow of section B is quite low com- pared to that through section C. The mean salin- ity of sections B and C are quite comparable, how- ever the volume flow is only half that of C. Tliere are several possible explanations for this disagree- ment: First, the depth of section C is greater by at least 100 meters than section B. If it is assumed that tlie gradient pressure force of section C is act- ing along prescribed geostrophic principles, the strong flow south, induced in section C, is forced through section B, resulting in a swift barotropic flow and not detectable by an examination of the mass distribution. Second, the situation may exist in section C, where the outflowing tidal pulses, speculated on previously, cause a pileup of the light water. This is indicated by the dynamic height contours which intersect the coast of Labrador. In this situation, the time lag of the adjustment period is such that this mass or slug of light water is at least a semi- permanent feature in the area. Therefore as found, the geostrophic movement south is slow through section B, but over a given time period is sufficient to carry off the periodic tidal buildup of the water emanating from Hudson Strait at section C. This concept would still allow the use of the dynamic method for examining the pres- sure-mass distribution flow tendencies. One sup- porting point for this argument is that the total outflow from Hudson Strait, 1 .64 X l()''mVsec, is only slightly less than the 1.68X lO'^rnVsec net southward flow through section B. The limited southward flow from section F, which appears to be continuous through section C and B has prop- erties within the defined water mass but on the warm, higher salinity end. This can be seen from the T-S curves of figures 12 and 14. Being warmer and saltier, and in proximity with the boundary Labrador Sea water, makes it more sus- ceptible to receiving heat and salt, as it moves south thereby removing good portions of its volume flow from the defined water mass analyzed prior to its arrival at sectioTi B. 13 No complete explanation can be given at this time. It is hoped that a similar cruise being under- taken in 1966 will clarify the situation. Section A, well to the south and not shown on figure 20, had a volume flow 1.28 X lO^mYsec and a mean salinity 33.53%o. This section is sufficiently far to the south of section B to peniiit lateral en- trainment of the Labrador Sea water from the east which not only reduces the amomit of the de- fined water mass but also causes a salt and heat increase. This would make these volume and salt figures noncomparable with the values found in the north. Smith (1937) did a limited amount of quanti- tative work in the entrance to Hudson Strait based on the 4 stations he obtained there. He estimated the net discharge to be LOXlO^m^/sec, but points up the probability of the seasonal and yearly changes that occur. His calculations lacked data in the strait north of Resolution Island. Quantitative flow work in Hudson Strait was perfonued by both Campbell (1958) and Farqu- harson and Sauer (1960). Campbell determined the summer rate of the eastward current in Hud- son Strait to be about 17 kilometers per day. Tlie work done by Farquhai-son tends to support this finding through the use of current meters. The data from the 1965 expedition show a 49 kilometer per day current flowing east through the entrance across a 19-mile wide group of stations. Camp- bell ( 1958) also made transport calculations of this eastward flowing current within the strait. He shows a net eastward flow of 0.3 X 10*'m'/sec. Cal- culations based on the 1965 expedition indicates a net eastward transport of 1.64X lO'^m^/sec, con- siderably higher than found by Campbell (1958). The explanation of the discrepancies of the re- sulting figures presented herein and those arrived at by Campbell (1958) is found in the dift'erences of location time, number of data points, and method of dynamic calculations. Campbell's cal- culations for July were made well within Hudson Strait and not in the restrictive entrance which would tend to increase the current velocities. His volume flow values were arrived at for a location west of Ungava Bay which undoubtedly con- tributes a good deal of water to the net eastward flow. The station location used by Campbell left large gaps between the end of his sections and the coast. He speculates that as much of the flow could be passing through this gap as passes through the entire calculated section. Further- more, his usage of a variable depth of no motion within the strait limited by a maximum of about 350 meters, would not result in comparable com- putations with those made using a 1000-meter depth of no motion. In addition to the points above, the difTerent years in which the data was obtained could account for the incomparability alone. FUTURE WORK Another expedition is planned during July and August of 1966 to the Hudson Strait area. Survey work will be performed both inside and outside the entrance of the strait in an effort to tie the circulation of both areas together. In addition, parachute drogues will be used, during several tidal cycles, in order to obtain direct measure- ments of the net flow through the strait. Multiple section occupations over several tidal cycles will also be attempted in order to verify the constancy of the distribution of mass regardless of the tidal current fluctuation. SUMMARY The circulation of the Baffin Land Current is into Hudson Strait, north and south of Resolution Island. No large volume flow appears to be con- tinuous between the Baffin Land Current and the Labrador Current. To the east of Resolution Is- land low velocity currents flow in a general south- erly direction. The water flowing into Hudson Strait has a mean salinity 0.64%^ higher than the mean salinity of the water flowing out of the strait. It is further indicated that the character- istic low salinity water of the Labrador Current emanates directly out of the strait and is the re- sult of the mixing, within Hudson Strait, between very low-salinity resident waters and the inflowing Baffin Land Current. Calculations show that 1.64X lO^m^/sec outflow from Hudson Strait is contributed to the Labrador Current. Calcula- tions further show that this net outflow forms at least 50 percent of the Labrador Current flowing south of Hudson Strait. 14 REFERENCES Campbell, N. J. (1958). The Oceanography of Hudson Strait. Bull. Fish. Res. Board of Canada No. 12. 60 pp. Dunbar, M. J. (1951), Eastern Arctic Waters. Res. Board of Canada No. 88. 131 pp. Bull. Pish. Farquharson, W. I., and Sauer, C. D. (1960), Tidal and Oceanographic Survey of a Section of Hudson Strait, Department of Mines and Technical Surveys, Ottawa. Helland-Hansen, B. (1934), The Sognefjord Section. Oceanographic Observations in the Northernmost Part of the North Sea and the Southern Part of the Nor- wegian Sea. J. Johnstone Mem. Vol. p. 257. Liverpool, 1934. Jacobson, J. P., Robinson, R. J., and Thompson, T. G. (1950), A Review of the Determination of Dissolved Oxygen in Sea Water by the Winkler Method. Union Geodes et Geophys. Int. Assoc. d'Oceanog. Phy., Pub. Scientif. No. 11. Kollmeyer, R. C. (1966), The Oceanography of the Grand Interpolated Oceanographic Data. U.S. Coast Guard unpublished manuscript series, Oct. 1964. Kollmeyer, R. C. (1966), The Oceanography of the Grand Banks Regions of Newfoundland in 1965. U.S. Coast Guard Oceanographic Report OG 373-11. Montgomery, R. B. (1938), Circulation in the Upper Layers of the Southern North Atlantic Deduced with the use of Isentropic Analysis. Papers Phys. Oceano. Met., MIT and WHOI, Vol. VI, No. 2, p. 1^3. Morse, R. M. and O'Hagan, R. M. (1964), Operational Notes on Shipboard Computer. U.S. Coast Guard un- published manuscript series, Oct. 1964. O'Hagan, R. M. (1964), A Shipboard Computer for the Evaluation of Oceanographic Data. U.S. Coast Guard unpublished manuscript series Dee. 19(>4. Smith, E. H. (1937), The Marion Expedition to Davis Strait and Baffin Bay. U.S. Treasury, U.S. Coast Guard Bull. 19, Part 2 Report of the International Ice Patrol Service in the North Atlantic Ocean. 259 pp. Serdrup, H. U., Johnson, M. W., and Fleming, R. H. (1942), Tlie Oceans. 1087 pp., Prentice-Hall Inc. 15 Figure 1. Station array and types of sampling accomplished at each location during the Labrador Current Expedition, July-August 1965. 16 Figure 2. Station array and dynamic height streamlines obtained by Smith (1937) from the CGC MARION Expedition. 17 c 477 94 76 9479 34 80 -"Ht-T- 40 -»■ 9491 H4 1 4. s 3482 >!1 40 3 94 83 «. !0 . 9484 ..1 1 ■ 7 i 948- — ST — TTJ it!t — 4f^ rW .o4ao -»H^ -»- o;.* 46 - 00. 077- -0.5!!_ — s*- 0,0 74. .0 — Irr- OO. 0O07 0,7 00.0 — ir?- —55^ 100 -i's -^ — 1.01* iaia J.^ - m till ",i. ^.flU osao nil ,-.ga» 0I7« -r-^ ■ 0" as25 — Hf?- 0 0 0071 1. lit x'i °';° .„„ 0114 » K -.03 ca42 iJ 0« >.00« 03»0 ,1 .. -141 ,041 is tft .02 I0!0 ...! 174 04S, le.os -, , , ... rri H as B -1 • N -1 t 10 0> - 0?3 .07.4 2 6 *■ 127 77 .4 70. 0..7 7! 77 200 -' • »• <•' — J»ij -21 L. ^" 0 5 ' ... s^. o,.o !S SO - .„ .,<5' . .. 00 00 oo 01.4 4 B9 s V ,.0. 0„ 0.0. .,» ,4. 04,7 ,..7 ,0, ,4.7 .7,40 300 091 \ \ '•,V_ 079 .000. . le (02 OOJ 400 BOO — CODE FOR SOLINOID NUMBERS \ \ Hi. Si »E4NTEH^»C D.MCtlONOf FLOW «»- S»LlNliy %o 60O " >4 T 49 N HUt riXkHSVOIIT VOLUUE 'LOO SALT TH*HS»0»I \. mO'-.J/lK »IO«mV..C "lO ■g »•■/••< \ \ 700 NORTHWARD FLOW \ - 01. 0O» '•• I04,.J 800 \ S4.9 900 - \ \ 04, 0,0. \ Figure 3. Solenoid division of section across Baffin Land Current, located off Loks Land, as used in the volume, mass, and heat transport calculations. C 0 r 100 471 94 70 9469 9468 9467 9466 9465 946 2 0 5 33 1 5 33 ; "i? 386 13 24 28 Ol'l'3 24 46 -ti — -4^ 05 -H^ 3S J ju^; — 08 03BS 13 28 07 .0300 0 594 03 76 0913 -rrl^ 07 5 — Ifr- ■ 1 0 OB47 s3fl 19.04 03 0249 8 64 P3 0IS9 5 54 04 04 99 IB 93 00 0265 9 17 oe;4 M s 10 S 16 ~ N 34 0 0^ T048 ^1^57 1,3 33 70 0198 6 89 23 53 \" 5 — JTB— '- 20 ^ 4 0 ' 34 6 \ (fl .0TT4 2T 26 .001 000. -07 .02 0108 iM 14 .05 45 19 2S .06 0.:66 37 0932 32 21 TT" — !— 40 S 4 5 S 34 6 '■• " 3 5 ** 2on 1431 0596 21 24 OS 01 17 4.17 06 0171 6oe .13 0363 12 90 05 0123 430 29 OGOO i< 46 4 0 f\ 346 S 14 T 4 4 S 34 78 42 " ,47 4 3 300 V ^ 3304 10 86 0383 13 69 03 0066 B.OO ,1 0670 iZM 4, s 34 T \ 4Z s 34 TB 4 4 S 39 e 43 " 34 8 4 3 " 34 8 4S S 348 4» S 400 1 0493 1 1 026> »36 10 02 42 8 67 05 0126 4 92 01 0030 1 08 06 0129 4 64 \ 43 s 34 77 ■>l H 34 S 4.2 •* S4a 43 " -•4 8 4 3 X 1- HI \ iff d: 500 ^ .^^ ^^ ^^_^^ \ z sor) - 09 0200 7.16 19 .0441 ^"---16 02 ,, 0264 910, . 01- —.0026- 93 05 -;;r 996 \ \ - 17 33 4 0 \ TOT - CODE FOR SOLINOID NUMBERS \ MEAH TEMP "C DIftECTION OF FLOW ME4N SALINITY %„ SCORT VOLUME FLOW SALT TBANSPORT 80^ X106°« V..C KIO*n.Vi»e )(IO«g"i/i»e 17 030o\ 1078 3 9 "\ 39 9 -- NORTHWARD FLOW \ 900 0074 \ Figure 4. Solenoid division of section to the east of Resolution Island as used in the volume, mass, and heat transport calculations. 18 JS a. ■8 U e •S S 3 0. 0 a ■8 s '* o j: "ft e g 6 Hld30 5»3X3IM 19 LABRADOR SEA Figure 6. Depth plot of the 26.2 sigma-t surface showing the contours of the nitrite (ISOt—lS) distribution. Shown also are the surface intersections with the sea surface and bottom. 20 UNGAVA BAY INTERNATIONAL ICE PATROL -U.S. COAST GUARD LABRADOR CURRENT EXPEDITION JULY -AUGUST 1965 nilrlte-N on 27 0 6r surface NOj-NjjgA/L depth in meTers LABRA DOR SEA 60° Figure 7. Depth plot of the 27.0 sigma-t surface showing the contours of the nitrite (.!\0,—lS) distribution shown also are the surface intersections with the sea surface and bottom. 21 Figure 8. Surface dynamic height chart of the survey area, in dynamic meters based on a lOOO-decibar level I of no motion. 22 5 £ ca S o "O V 00 cs ■a •o e s a o Z ca ^ ™ o ■« -5 s * j: m - E O 4j *- c en CIS 4) u S 4) H 3 23 CO u l» b o 2 .a E V JS C e B a u O J3 U o \^ e e s e « 24 ' \ s 1 1 \ ■ / ) \\ / \ /\ ( ^. ■ y IP' / T 1 ft ^ / i i \A, 1 / . a V u o •a es fa o e 0) -s o s« c 9 ■§ CD Vi 25 H1A3Q SU313 o ^\ ^N /^ T — ' S o i m / ° o o o / 1 '/V -^ / / Hldaa SU313M nia3Q st>3j.3n 26 I \ V° a >-- I I I I I I I I I T 1 1 N x / / y \ u (^ ^ ^-^ \ \V -~~^^ ^^. ,..--J^ a "* z o c "N X N jK «n "^ ~ ) v- 1 1 •s / // / \y p [ Kfi J ' — ;—•->>. >Ud3a U3X3n s e \ «:^. 1111111111111111111 1 1 1 1 1 1 1 1 1 1 1 4^1 ! I U I I I I 1 » I I I U I I I !- 11 y ;: > IIPT -^- '>. \ f i' 'I . s 1 1 1 1 1 1 1 1 1 1 J 1 1 1 1 1 M 1 1 1 ,1 •/ XX 1.1 1 J u u ,1 ^ 1 1 1 1 1 I ^' I 1 I M I I I 1 I 11 >^ fi \ I I « ^ I I 1 I 1 I I I I I t^ I : I I LII I Ml M II I I I I I I K 1 1 U I 1 1 I e I I • ^ a i a •■i B s « t ^ 31 - S^.^^ Ri m ^, K , X — 1 ro t- < Ml a. S I 1 1 1 1 I I I ' I ,f^° u «• o a <»■ o a <"? U r- 0 < -> K D J= V> T 0 c * o ■t » lo 1 ?« o to jZO CO < -< p =1 e in -J 0 9 u 0 o ro -0 o a> o ■y. o u: s ■0 c a ,t^ o o u o o s CVJ 0 3 ^ a N. a c« S^ M 0 o q: o: 3 O •-■' 0 QD Q - e » 1^ .2 S o o u - m z ^ s= C\J UJ « J, o 1 ^ 41 J ■^ s ^ \0 - 9~ .5 §1 «: U O _4j 3 61 32 J.33J-HXd3a Figure 19. Mean salinity values in %o of the water flowing through the sections obtained in the vicinity of the entrance of Hudson Strait. 33 60° ^ 638.0 gms/SEC 1.85 M^/SEC • • 0.59 M3/SEC 1 983 gms/SEC V .'371 .5 gms/SEC I.OTM^/SEC 1- F -1' 11982 3.^7 gms/SEC M^/SECx C • ••♦• ••♦ 'V B INTERNATIONAL ICE PATROL - U.S. COA: LABRADOR CURRENT EXPEDITION JULY- AUGUST 1965 net transport of salt and water volume, nymericol volues X 10"* and 10"^ respectively, defined woter mass < 2''C, 34.3°/«,. *I.68m3/SEC 1 LABRADOR SEA 3U- 60° Figure 20. INet volume flow and salt transport through the sections obtained in the vicinity of the entrance oi Hudson Strait. 34 Nutrient Distribution Along the Labrador and Baffin Island Coast, 1965 David A. McGill and Nathaniel Corwin ^ Woods Hole Oceanographic Institution, Woods Hole, Mass. Interest in the oceanographic conditions of the Labrador Sea has greatly intensified in recent years, as the important relationship of this area to the western North Atlantic has been demon- strated. For many years the standard section from South "\A'olf Island, Labrador to Cape Fare- well, Greenland has been occupied by the U.S. Coast Guard in a post season cruise by the Ice Patrol. Analysis of this section has shown the presence of coastal currents near Labrador with markedly different characteristics from the off- shore water masses. The nutrient chemistry of tins standard section has been examined by the present autliors in recent years and show a similar abrupt transition between the coastal and offshore conditions. Wliile recent Soviet research reports (VNIRO-PINRO, 1960; 1962) have given in- formation on the chemistry and biology of the region south of the standard section along the Newfoundland coast and banks, details on the coastal conditions in northern Labrador and Baf- fin Island have been lacking. Accordingly, the 1965 post season Ice Patrol survey was planned to provide data on coastal sections from South Wolf Island, Labrador to the margin of the Baffin Sea basin. The report on the nutrient chemistry for the coastal waters surveyed which is given here greatly augments the available observations, especially in the Hudson Strait and Ungava Bay area, which has been previously little studied (Dunbar, 1951). METHODS The analytical techniques have been given in previous reports, especially McGill and Corwin (1965) where references to individual methods may be found. Frozen samples collected during the Ice Patrol Post Season Survey were stored until analysis could be undertaken in Woods Hole. 'Contribution No. 1838 form the Woods Hole Oceanographic Institution. This work was supported in part by the Office of Naval Research under contract Nonr-2196(00) NR-083-004. The assistance of John Schilling and Mrs. Juanita Mogardo is again gratefully acknowledged. The nutrient data are published in this volume along with the other observations at each station. Since relatively little detail exists in the contours of these sections due to the greatly restricted depths along the continental shelf, profiles of all the dis- tributions are not given. Only the nitrite- nitrogen profiles are shown and the significance of these is discussed below. The other distribution patterns are described verbally. The locations of the sections mentioned are shown on the inset maps accompanying figures 1 and 2. DISTRIBUTION OF NUTRIENTS Inoi-ganic phosphate-phosphorus values near 0.5 f«gA/l at the surface along the cost occur through- out the area. In the southern sections, the surface phosphate concentration decreases at the offshore extremity to values near 0.20 /igA/1. A concen- tration of 1.00 MgA/1 is reached near a depth of 200 meters in all sections. Along the continental slope in deep water the phosphate level increases to about 1.10 /xgA/1. Sections A, B, and C— south of Hud- son Strait — show a value of about 0.90 ftgA/l at 100 meters on the continental shelf. This general pattern also occurs in section D across the mouth of Hudson Strait. The small decline in surface values at stations 9455-9457 (at the northern end of the section) relative to the remainder of the sec- tion may possibly indicate the westward-moving inflow to the Hudson Strait. Section D' repre- senting Ungava Bay (see map) has relatively high phosphate concentrations : 1.00 /ligA/l occurs near 100 meters and occupies the remainder of the basin except where a near-shore current is suggested at stations 9463. Sections E and F are generally similar to section D. In section G a bubble of phosphate greater than 1.00 /xgA/1 is found at about 50 meters and this may represent the outflow from Davis Strait in a current moving southwest- ward toward the coast after exchanges with Baffin 35 Bay water. Section H is clearly much different from the other sections, being north of the still at Davis Strait. The increase of nutrient concentra- tions in deep water below the sill depth is indicated by phosphate values of greater than 1.20 /igA/1. Total phosphorus distribution is consistent with the pattern just described for the inorganic phos- phate. Values average 0.10 to 0.20 /u.gA/1 greater than inorganic readings, especially near the sur- face and in the areas near shore or over the con- tinental shelf. Section D again suggests an inflow to Hudson Strait with lower total phosphorus values on the northern side and an outflow from Ungava Bay on the southern side having higher values. The high nutrient level at 50 meters in Section G persists. In Baffin Bay (section H) the pattern is extremely complex : The water below sill depth shows a total phosphorus concentration over 1.30 /igA/1 and near stations 9499 and 9500, on the landward end of the profile, total phosphorus values greater than 1.50 ju.gA/1 are found. As in the other sections, the variations in near-surface values found here between individual stations is presumably due to phosphorus in biological combination. The organic phosphorus is derived as the dif- ference of the observations on total and inorganic concentrations. These values are also reported with the data tables which accompany this volume. Values of organic phosphorus greater than 0.20 jtigA/1 occur at the surface in section A, B, and C and again at G and H. The continental self in A, B, and C has organic phosphorus values from 0.10 to 0.20 ugA/l while lower tend to be found in the deeper water offshore along the continental slope. Similarly low values are found in section F although at "section G the organic phosphorus level increases again. These data are perhaps best handled statistically, as in the following section. The nitrate-nitrogen distribution in all sections is well stratified. Zero surface values increase to 5.0 jugA/l at 50-75 meters and values of 10 n*gA/l occur by about 200 meters. The offshore deep waters on the continental slope in sections A, B, and C show a continued increase in nitrate concentration to values greater than 15 /xgA/l. Similar high values are found below 300 metei-s in sections F and I and at station 9485 in section G. Relatively low nitrate concentrations are found in the Hudson Strait and Ungava areas. Nitrite-nitrogen distribution are reported sepa- rately from the values for nitrate concentration. The nitrite concentrations are also shown in figures 1 and 2. In the stations in the Baffin Bay area, section H, the high nitrite values are found close to the surface. In the other sections, the only statistically significant values are grouped near 100 meters, with the highest values in all cases oc- curring on the seaward end of the profile, especially in the southern end of the Labrador Sea (fig. 2). Low nitrite concentrations with a very indefinite pattern of distribution, found in the section for Hudson Strait and Ungava Bay (sections D and D', fig. 2), contrast with the strongly emphasized peak concentrations for the Labrador Sea. The silicate-silicon distribution also shows con- siderable horizontal stratification from values less than 5 /^gA/l at the surface to concentrations of about 10 figA/l at 100 meters. Higher values oc- cur in deep offshore water of section A, B, and C. The silicate level on the continental self in section C is slightly reduced, which may relate to the low values (less than 10 /xgA/l) foimd also in section D at the entrance of Hudson Strait. The Ungava Bay area (section D'), on the other hand, shows silicates greater than 10 /*gA/l below 100 meters. Stratification is well marked in sections F and G, though the high nutrient level in section G recurs in the silicate concentrations at about 100 meters on stations 9479-9482. High silicates, up to values greater than 30 /igA/1, are found in the deep water of section I. Such values are characteristic of Baffin Bay at the depth below the sill (McGill and Corwin,1962). DISCUSSION Analytical results for the various nutrient de- terminations from the coastal sections near Labra- dor and Baffin Island are in good agreement with each other. The nutrient concentrations show a general increase witli depth. A simple regression analysis gives ratios by atoms for the relative changes in nutrient concentration in each section, as reported in table I, which also gives the 95 per- cent confidence intervals as determined in Simpson (1960). The AN : AP ratio is in general agree- ment with the value of 16 : 1 which is widely accepted despite the variations in some regions which are discussed by Armstrong (1965). Sec- ' jn D', in Ungava Bay, is the only area of this survey with a marked change from this value. A considerable reduction is found in Ungava Bay — the value obtained is equivalent to winter values 36 for regions such as Long Island Sound (Riley and Conover, 1956) and New England coastal surface waters (Ketchum et al. 1958). - The ^jSi : AF ratios in table I are more variable from section to section. The liighest ratio occurs in the Baffin Bay waters of section H, where sili- cate accumulates below sill depth. The value found agrees with our previous observations (Cor- win and McGill, 1965). By contrast, a low value is obtained for section F. Without biomass measurements or productivity estimates, this varia- tion in the coastal sections cannot be correlated with any changes in populations, thougli this is one obvious agent affecting \Si:i^P through growth of phytoplankton skeletons and other metabolic changes. Land drainage might augment the local supplies, as in section E where the ASi: aP ratio is slightly increased, but this effect likewise cannot be estimated from available information. The AS! : Af and AN : aP ratios do not vary con- sistently together, which adds to the difficulty of interpretation. In data of previous years for the section from South Wolf Island to Cape Farewell, Greenland, which includes the deep water offshore, the AS I -.aN-.aP has been in good agreement with the theoretical ratio of change in sea water (see Mc- Gill and Corwin, 1965). It is probable that bio- logical assimilation in the surface waters near shore acts as a differential agent to alter the ratios selectively, while process of regeneration in deep water of the main Labrador Sea restore the nutri- ent quantities to solution. In the coastal sections surveyed in 1965 assimilative processes predomi- nate, thus producing the variable ratios given in table I. TABLE I. Relative changes in concentration among the nutrient elements in coastal sections near Labra- dor and Baffin Island Area Section : G-_ F.. E._ D.. D'_ C._ B_. ASi 23. 82 ±3. 13. 39 ±2. 9. 27±0. 16. 89±3. 10. 15 ±3. 11. 18±0. 11. 88±0. 10. 87± 1. 13. 01±1. 42 ( 87) 40 ( 58) 80( 50) 53( 26) 05 ( 82) 87 ( 52) 93(160) 40( 95) 17(106) AN 16. 40± 15. 02± 17. 62± 15. 95± 15. 57± 9. 45 ± 18. 14± 18. 10± 17. 31 ± 3. 16( 87) 3. 64 ( 58) 1. 87 ( 50) 7. 21( 25) 2. 88 ( 82) 1. 75 ( 52) 1. 76(159) 2. 99( 95) 1. 89(106) AP Organic phosphorus distribution is i)erhaps best, represented as a frequency distribution. The statistical parameters resulting from such treat- ment are given in table II. The mean value given includes observations from all depths on the sec- TABLE 11. Distribution of total organic phosphorus for coastal sections near Labrador and Baffin Island, arranged as a frequency distribution and with 95 percent confidence interval calculated for the mean in each section Note— The number of data pairs used in the regression is given in paren- theses. Nnety-five percent confidence intervals arc calculated from Simpson el al.. 1960. Section I 9493-9500 Section G — 9477-9485 Section F — 9464-9471 Section E 9471-9474 Section D 9448-9458 Mouth of Hudson Strait Section D' 9459-9463 ITnOava Bay Section C — 9435-9448 Section B — 9422-9432 Section A 9409-9420 s n s/V"- sj^fri- sl-^- s' n X .e2 S s|^|n. n X s' s slyfn- n X sK... s s/V"- « s/V"- Frequency distribu- tion values g."! percent corifldence interval 58 1716 0393 1982 0260 86 1645 ,0362 , 1903 .0205 50 . 1210 .0147 . 1211 .0171 26 . 1231 .0346 . 1856 .0365 83 . 1560 .0243 . 1560 .0171 42 . 1667 .0331 . 1820 .0281 158 . 1845 . 0428 . 2069 .0165 92 . 1707 .0306 . 1749 .0182 106 . 1637 . 0292 . 1709 . 0166 ± 0. 0533 ±. 0408 ± . 0346 ±.0753 ±. 0340 ±. 0568 ± . 0323 ± . 0362 ± . 0330 37 tion. Highest organic phosphoi-us values are found in the surface waters in all sections. The mean value from section to section shows only limited variation, the most marked change occur- ring in sections E and F. It is possible that the decrease there from the level of organic phos- phorus observed in all other sections represents some local excess in land runoff or drainage. No noticeable difference is seen in Ungava Bay or Hudson Strait from values along the Labrador and Baffin Island coast. The coastal concentra- tions of mean organic phosphoi-us are somewhat in excess of values reported for the full section across the Labrador Sea to Greenland. They are less than obsei-vations of 1964 in the area of Kane Basin and Smith Somid. Vaccaro and Eyther (1960) have pointed out that high concentrations of nitrite-nitrogen in nat- ural waters mark locations where important bio- logically induced changes in combined nitrogen are progressing. The assimilation of nitrate- nitrogen by marine phytoplankton is often accom- panied by the production of significant amounts of extracellular nitrite. Increasing concentra- tions of nitrite can be expected in the upper layers of the ocean when an adequate standing crop of phytoplankton is present and an excess of nitrate is available. Such conditions are characteristic of the summer season in tlie Labrador Sea. The nitrite-nitrogen distributions shown in figure 1 in- dicate that this biological activity is concentrated in surface waters off the continental slielf and sea- ward of the continental slope. This is the same pattern as obtained in previous yeare in the Labra- dor Sea (see Corwin and McGill, 1963). In the absence of other data, this distribution pattern can serve as an indication of the relative produc- tion in these coastal sections. Hopefully, direct measurements will be attempted in the future and the relation of biological and cliemical parameters made more evident for this region. Nutrient distribution patterns can also be ex- amined for indication of local currents and water masses. In general, the distribution of phosphate, nitrate, and silicate is consistent with the pattern of surface currents given by Dunbar (1951) . This is particularly true in the Hudson Strait area, where a segment of the Labrador Current entei-s along the Baffin Island coast and an outflow to the Labrador Sea occupies the area near the Que- bec coast. Such a pattern is indicated by the nu- trients in section D. This circulation has given 38 evidence in the past of an increased Atlantic influ- ence from 1930 to 1948, as demonstrated by both physical and biological criteria (Dunbar, 1951). Increased penetration by Atlantic water would tend to raise the nutrient levels slightly and such exchange might represent one factor in long-term budgets for the area. The nutrient quantities would also be involved in any "feedback" mecha- nism as proposed by Dunbar (1951) regulating water balance between parts of the Arctic Basin and the Labrador Sea. The general pattern of distribution in the coastal sections in the Labrador Sea suggests a phenom- enon analogous to the i^ersistence of "winter wa- ter" on the continental shelf in temperate latitudes (Ketchum and Corwin, 1963). Observations for other ijeriods of the year are needed to detail the sequence of changes taking place on the conti- nental shelf. The available nutrient observations indicate a distinct change between onshore and off- shore water but give only limited details to char- acterize the circulation. Russian observations on zooplankton populations suggest some systematic shift of boreal and warm water forms by season (Vladimirskaya, 1965), but agree that the higher biomass is found in the boreal fauna. BIBLIOGRAPHY Armstrong, F. A. J. 1965. Phosphoru.s. In: Riley and Skirrow, Ed. Chemical Oceanography. Vol. 1. Acade- mic Press, New York 323-364. Corwin, Nathaniel and D. A. McGill. 1963. Nutrient Distribution in the Labrador Sea and Baffin Bay. U.S. Coast Guard Bull. 48 : 79-94. Dunbar, M. J. 1951. Eastern Artie Waters. Fish. Res. Bd., Canada Bull. No. 88, 131 pp. Ketchum, B. H., R. F. Vaccaro, and N. Corwin. 195S. The annual cycle of [iho-sphorus and nitrogen in New- England coastal water.s. Jour. Mar. Res. 17 : 283-301. Ketchum, B. H. and N. Corwin. 1963. The persistence of "winter" water on the continental shelf south of Long Island, N.Y. Limnol. and Oceanogr. 9(4) : 467-47.5. McGill, D. A. and N. Corwin. 1965. The distribution of nutrients in the I^brador Sea, summer 1964. U.S. . Coast Guard Oceanographic Report No. 10 (CG 373- 10) : 25-33. Riley, G. A. and S. A. M. Conover. 19.56. Oceanography of Long Island Sound, 1952-1954. III. Chemical Ocean- ography. Bull. Bingham Oceanogr. Coll. 15 : 47-61. Simpson, G. G., A. Roe, and R. G. Levvontin. 19C0. Quan- titative Zoology Rev. Ed. Harcourt, Brace and Co. New York, 440 pp. Vaccaro, R. F. and J. H. Ryther. 1960. Marine phy- plankton and the distribution of nitrite in the sea. Jour. Conseil 25(3) : 260-271. \'NIRO-PIXRO. 1960. All-Uniou Research Institute of Marine Fisheries and Oceanography ; Polar Research Institute of Marine Fisheries and Oceanography 1960. Soviet Fi.sheries Investigations in North European Seas. Moscow, 468 pp. (In Russian, English summaries). VNIRO-PINRO. 1962. Soviet Fisheries Investigations in Northwestern Atlantic. Moscow. 376 pp. (In Rus- sian, English Summaries). Vladimirskaya, E. V. 1965. Quantitative distribution and seasonal dynamics of zooplankton in the Newfound- land area. (In Russian, English abstract.) Okeanol. Issled. Result Issled. Programme Mezhd. Geofiz. Goda. Mezhd. Geofiz. Komitet Presldiume, Akad. NaukSSSR. 13: 137-142. 39 9* 90* 48- SO* SS* ao" 49* SECTION E NO2-N 9476 75 74 73 72 LEGEND I I O- 0.10 pgA/i I I 0.10-0.20 0.20- 0.30 0.30-0.40 OVER 0.40 R -1 \ %==^ - 1 — 1 40 Figure 1. Vertical distribution of nitrite-nitrogen, sections E, E, G, and H. SECTION D NO2-M • O •! / / V r t/ LEGEND I I O- 0.10 MgA/l I 1 0 10-0.20 0.20- 0.30 0.30-0.40 OVER 0.40 TO- 68* «0* 59* SO* «* TO- eS* 80- 35" 5 SOUND VELOCITY Ol Tll/l PO4-P TOTAL-P „g - ot/l NO:-N ., - ol/l NOj-N ,1 - ol/l St 04-Si wg - ot/l PH _ STD 0000 0661 3200 2514 0028378 0000 14736 727 035 OBS 0000 0651 32004 2514 14736 ' 727 '038 058 002 000 002 035 OBS STD STD 0005 0665 31935 2508 0010 0466 3218 2550 0020 0154 3259 2609 14737 725 039 0024898 0027 14560 782 0019289 0049 14537 869 055 002 000 001 035 OBS STD STD 0025 0060 32753 2629 0030 0056 3285 2537 0050 0016 3318 2565 14493 900 050 0015599 0057 14494 871 0013975 0097 14483 783 095 005 006 004 035 OBS STD 0050 0016 33177 2665 0075 -0088 3329 2578 14483 085 0012582 0131 14441 730 099 Oil 049 007 035 OBS STD 0075 -0088 33288 2578 0100 -0056 3345 2691 14441 730 104 0011463 0161 14462 742 113 015 085 Oil 035 OBS STD STD 0100 -0056 33462 2591 0125 0013 3370 2707 0150 0084 3393 2722 14462 742 096 0009961 0188 14501 724 0008624 0211 14541 712 108 015 083 009 035 OBS 0150 0084 33929 2722 14541 712 094 104 024 103 010 035 OBS 0165 0127 34065 2730 14565 707 098 107 019 106 010 035 OBS 0175 0201 34287 2742 14602 579 101 110 010 118 Oil REFERENCE SHIP CODE LATITU DE 1/10 LONGITUDE * '1/10 n MAttSDEN SQUARE STATION TIME IGMTl YEAR ORIGINATOR'S | DEPTH TO BOTTOM MAX. DEPTH OF S-MPL- WAVE OBSERVATIONS WEA- THER CODE CLOUD CODES NODC STATION NUMBER CTRT CODE 10. NO. CRUISE NO. STATION NUMBER 10* r MO DAY H ;.I/10 OIK. HGT n» SEA TYPf AM 31 5*9 EV 5 401 8N 05 520 W 186 i»5 37 25 0 48 1965 LCE 9411 C 137 01 13 0 2 XO 0 0003 WATER WIND BARO- METER {mbd AIR TEMP. X. VIS. CODE NO. OBS. DEPTHS SPECIAL OBSERVATIONS COLOR CODE I»*NS. °"- SPIED OR FORCf DRY BULB WET BULB '■' S14 041 094 089 7 07 MESStNCR [ HR 1/10 CAST NO. CARD TYPE DEPTH [ml T -C s •/.. SIGMA-T SPECIfIC VOLUME ANOMALT-IIO' SAO DYN. M < to' SOUND VELOCITY 02 ml/l P04-P „a ■ oi/i TOTAl-P ue - Qi/i N03-N pg . Ol/l NOj-N pg - ol/l SI 0*-Si pg - Ol/l pH STD 0000 06 2A 3208 1 2524 | 0027351 0000 1 14722 1 733 048 OBS STD 0000 0524 '32082 2524 0010 0621 3208 2525 14722 ' 733 048 0027319 0027 14722 737 076 002 002 002 048 OBS STD 0010 0621 32083 2525 0020 0343 3242 2581 14722 737 043 0021941 0052 14613 822 062 001 000 002 0*8 OBS STD STD 0025 0230 32559 2602 0030 0145 3267 2617 0050 -0073 3302 2656 14567 844 043 0018560 0072 14531 817 0014784 0106 14440 744 067 003 000 003 048 OBS STD 0050 -0073 33022 2655 0075 -0074 3325 2574 14440 744 094 0013052 0140 14447 733 106 009 069 009 048 OBS STD 0075 -0074 33245 2574 0100 -0059 3345 2590 14447 733 098 0011580 0171 14461 734 110 013 085 on 048 OBS STD 0100 -0059 33445 2590 0125 -0022 3362 2702 14461 734 100 0010398 0199 14484 733 110 017 088 on 04 B OB 5 0132 -0( )08 32 6 62 27 0 3 14£ 92 732 097 1 09 017 085 01 3 43 REFERENCE SHIP COOE LATnUDE 10 4GITUDE i| MARSDEN STATION T ME ORIGINATOR'S 1 DEPTH TO BOTTOM MAX DEPTH Of WAVE WEA- THER CLOUD COOES CItT ID. CRUISE STATION 1 STATION COOl l/IO ■l/IO 10* r MO DAY HR.1/10 BER S'MPL'Sl OUL MCI PER H* nn *M 31 549 EV )4106N ] 05 5095W 186 45 07 25 066 1965 LCE 9412 0149 01 1 15 0 2 xo 0 0004 WATER WIND AIR TEMP. r: COLOR iWNi into METER DRY V. ET CODI oes. OBSERVATIONS CODE i"i FOtCE (mbll BULfi BULB 17 S16 037 094 089 7 07 MEiSENCI HH 1/10 CAST NO. CARD TYPE DEPTH (ml I X s •/.. SIGMA-T SfECIFIC VOLUME ANOMALt-XlO' SAO DYN. M X10» SOUND VELOCITY Ol ml/l PO4-P ve - «>/i IOTAl_P .,0 - o./l NO3-N i>e - oi/i NO3-N ug - 01/1 SIOi-SI vg • ol/l pH STO 0000 0619 3185 2507 0029045 0000 14717 728 11 066 OBS STD 0000 ' 0519 31848 2507 ' 0010 0616 3185 2507 0029028 ' 14717 ' 728 ' 038 0029 14717 729 064 003 000 002 066 OBS STD 0010 0616 31847 2507 0020 0274 3223 2572 0022808 14717 729 037 0055 14580 806 065 002 000 002 066 OBS STD STD 0025 0143 32392 2595 0030 0055 3253 2610 0019161 0050 -0112 3295 2653 0015129 14526 825 053 0076 14493 799 0110 14421 735 079 005 005 003 066 OBS STO 0050 -0112 32960 2653 0075 -0033 3322 2570 0013447 14421 735 104 0146 14455 746 112 012 038 010 066 OBS STD 0075 -0033 33216 2570 0100 -0022 3343 2687 0011854 14465 745 095 0178 14478 732 118 013 068 009 066 OBS STD 0100 -0022 33430 2687 0125 -0016 3361 2701 0010503 14478 732 085 0205 14487 720 093 015 082 009 066 OBS 0149 -0016 33751 2713 14493 710 098 112 016 102 012 REFERENCE SHIP CODE -S MARSDEN STATION TIME ORIGINATOR'S j oEpiH DEPTH OF S'MPL' WAVE WEA- CLOUD CODI ID. NO. LATITU OE VIO LONGITUDE * 'l/IO CRUISE STAT NUW ON 'o THER CODE COOES STATION NUMBER 10* r MO DAY H R.l/10 Dl«. »CI PE» SE* ITPf AM 31 549 EV 418 6N 054589W 186 44 07 ?5 C 83 1965 LCE 9413 0159 01 16 2 2 X4 7 8 0005 COLOR IRANI S«EO METER DRY ET COD! OBS. CODE iml fO»Cf |mb»l BULB BULB 17 S14 030 078 078 0 07 MtSSENCI TIME o HR 1/10 CAST NO. CARD TYPE DEPTH (in) T -C s •/.. SIC^MA-T S^ECLflC VOUUMt ANOMALT-XIO' SAD DYN. M I I0> SOUND VELOCITY Ol ml/l P04-P TOTAl-P NOj-N ug - oi/l NO3-N ug - oi/l SI O.-Si pg - ot/l pH C C STD 0000 0622 13160 2487 0030916 0000 14715 729 083 OBS STD 0000 0622 31603 2487 0010 0580 3172 2501 0029537 14715 729 038 0030 14701 741 066 001 000 002 083 OBS STO 0010 0580 31724 2501 0020 0155 3241 2595 0020605 14701 741 038 0055 14531 799 057 001 000 002 083 OBS STO STO 0025 0008 32660 2524 0030 -0021 3271 2629 0017381 0O50 -0084 3295 2551 0015281 14468 814 057 0074 14456 796 0107 14434 747 087 005 022 004 083 OBS 0050 -0084 32952 2651 14434 747 091 108 010 062 008 083 OBS STD 0074 -0043 33288 2577 0075 -0042 3329 2577 0012844 14462 741 085 0142 14462 741 098 009 071 008 083 OBS STD STD 0098 -0028 33430 2587 0100 -0027 3344 2588 0011755 0125 -0016 3357 2598 0010808 14474 732 085 0173 14475 731 0201 14486 722 104 014 073 010 083 OBS 0148 -0011 33659 2705 14494 714 097 109 017 097 012 REFERENCE SHIP CODE LATITUDE I/IO LONGITUDE * 'l/lo n WARSOEN SQUARE STATION TIME '■ DIR. S«ED OR fORCt DRY BULB WET BULB 16 S14 024 072 072 0 11 MfSSEUGfl 1 (-AST ""' » NO. HB 1/10 CARD TYPE DEPTH Iml T -C s •/.. SIGMA-T SPtCIFIC VOLUMt ANOMAlT-IlO' SAD DYN. M. X 10' SOUND VELOCITY Oj ti»l/l POA-r lOTAL-P ug - ol/l NOj-N wg - ol/l NO3-N n - Ol/l SlO^-Si uO-oi/l pH S C c STD oooo 0465 3263 2586 0021464 0000 14554 743 ' 173' OBS STD 0000 0465 32634 2585 0010 0296 3307 2637 0016520 ' 14564 743 044 0019 14500 781 069 004 000 003 173 OBS STD 0010 0295 33071 2537 0020 0295 3344 2567 0013828 14600 781 047 0034 14605 737 072 008 007 004 173 OBS STD STD 0025 0288 33588 2579 0030 0267 3355 2587 0050 0182 3394 2715 0011939 0009179 14606 720 054 0047 14598 710 0058 14569 579 071 Oil 035 005 173 OBS STD 0051 0178 33950 2717 0075 0252 3420 2730 0007843 14567 578 078 0090 14511 551 089 022 081 008 173 OBS STD 0075 0255 34210 2731 0100 0307 3438 2741 0006889 14513 550 087 0108 14537 544 098 031 100 007 173 OBS STD STD 0102 0311 34388 2741 0125 0361 3453 2747 0150 0395 3454 2753 0006283 0005816 14639 643 092 0124 14656 635 0140 14685 526 101 038 117 008 173 OBS STD 0152 0397 34543 2753 0200 0395 3468 2756 0005597 14688 525 099 0168 14595 621 108 005 121 009 173 OBS STD STD T0203 0395 34679 2756 0250 0423 3475 2758 0300 0440 3480 2751 0005381 0005243 14596 621 103 0195 14716 618 0222 14732 614 109 003 145 010 173 OBS STD 0304 0441 34803 2751 0400 0440 3483 2753 0005124 14733 514 105 0274 14749 515 lis 00 3 134 010 173 OBS 0404 0440 34834 2753 14750 515 105 002 132 010 17 3 OB S T045' 0 '♦36 3' ^i 37 2- 6 £» 14- Tbt 612 107 115 003 150 010 46 REFERENCE SHIP CODE LONGITUDE * -1/10 n MAHSDEN STATION T ME ORIGINATOR'S 1 DEPTH TO BOTTOM MA 7 WAVE WEA- THER CODE CLOUD CODES CI«Y CODE ID. NO. LATITUDE 1/10 SQUARE IGMTI EAR CRUISE NO. STATION NUMBER DEPTH OE S'MPL'S OBSERVATIONS STATION NUMBER 10* r MO DAT MR.l/10 OIK. MCI Pt« S * lypi AM IT 5*9 EV 5503 N 053463W 186 53 ^ 25 193 1965 LCE 9419 1083 11 14 2 2 X4 X 9 0011 WATER WIND AIR TEMP. X NO. COLOR CODE TRANS. DIR. SPEED OR FORCt METER (mb»1 DRY BULB WET GULB VIS, cool OBS. DEPTHS SPECIAL OBSERVATIONS 15 S19 OlA 078 078 0 13 HR 1/10 CARD TYPE DEPTH Iml T "Z s •/.. SIGMA-T SPECIFIC VOLUME ANOMALV-IIO' S li D DYN. M X 10" SOUND VELOCITY 03 ml/1 PO<-P us - Ol/I TOTAl-P ;iB - 01/1 NOj-N ug • ol/l NOj-N KB • at/I SI 0*-SI VB - ol/l PH s c c STD 0000 0511 3275 2590 0021079 0000 14685 735 - 193 OBS 0000 0511 '327*9 2590 ' ' ' 14685 735 '045 068 005 000 003 193 OBS 0009 0509 32753 2591 14685 742 043 063 005 000 003 STD 0010 0510 3287 2600 0020166 0021 14687 738 STD 0020 0516 3379 2672 0013345 0037 14704 707 193 OBS 0024 0519 34053 2692 14709 697 042 060 009 024 005 STD 0030 0475 3413 2704 0010357 0049 14693 690 193 OBS 0048 0389 34326 2728 14663 672 064 079 016 058 005 STD 0050 0387 3434 2730 0007900 0067 14662 671 193 OBS 0072 0382 34533 2746 14667 657 084 093 005 097 007 STD 0075 0387 3456 2747 0006268 0085 14670 656 193 OBS 0095 0414 34702 2756 14686 646 097 102 034 133 008 STD 0100 0416 3471 2756 0005457 0100 14688 543 STD 0125 0424 3476 2759 0005190 0113 14696 530 STD 0150 0430 3480 2762 0004979 0126 14703 620 193 OBS T0189 0435 34843 2765 14712 510 107 115 004 152 010 STD 0200 0434 3484 2755 0004752 0150 14714 610 STD 0250 0430 3484 2755 0004758 0174 14720 610 193 OBS 0277 0428 34842 2755 14724 510 101 113 002 153 010 STO 0300 0426 3484 2765 0004791 0198 14727 612 193 OBS T0367 0420 34836 2766 14735 616 105 115 003 130 010 STD 0400 0416 3484 2766 0004797 0245 14739 516 STD 0500 0407 3485 2768 0004743 0294 14752 616 193 OBS 0552 0404 34849 2758 14759 616 113 124 004 155 Oil STD 0600 0403 3485 2769 0004756 0341 14757 517 STO 0700 0400 3485 2769 0004817 0389 14782 618 193 OBS T0742 0398 34857 2770 14789 518 105 118 005 132 012 STD 0800 0395 3487 2771 0004715 0437 14798 519 STD 0900 0391 3488 2772 0004574 0483 14812 522 197 OBS T0914 0390 34883 2773 14814 522 110 123 004 127 Oil STD 1000 0383 3489 2774 0004594 0530 14825 623 197 OBS 1075 0374 3A896 2775 14835 623 no 119 003 160 Oil 47 REFERENCE SHIP CODE LATITUDE LONGITUDE "1/10 ^s MARSDEN STATION Tl ^E ORIGINATOR'S OIPIH MAX. DEPTH OF S-MPL' WAV£ WEA- THER CODE CLOUD CODES 00c cr«¥ ID. NO. CRUISE NO. STATION NUMBER BOTTOM NUMBER COOf 10* r MO DAT HR.1/10 018. Mcr f[« s( * irpi AM 31 5*9 EV 55106N 053352W 186 53 37 26 001 1965 LCE 9*20 2121 15 14 2 2 X4 X 9 0012 WATER WIND BARO- METER Imbtl AIR TEMP. '^ "depths SPECIAL OBSERVATIONS COLOR CODE IMNS. DIR. SPEED OR fOICf DRY BULB WET euLB 15 S17 017 078 072 0 12 "'lit". =*" IIM[ 0 NO. HR 1/10 CARD TYPE DEPTH Iml T -C s •/.. SIGMA-T SPECIFIC VOLUME ANOMALT-XIO' SAO DYN. M. X 10' SOUND VELOCITY 0; m1/l PO4-P TOTAL~P NO3-N uB - ol/l NOj-N WB • at/I SIO<-SI vB - ot/l s PH C STD 0000 0648 3345 2629 0017377 0000 14750 696 ' 001' OBS 0000 ' 06«e '33454 2629 ' 1*750 696 032 059 005 004 003 001 OBS STD STD 0005 0699 33834 2652 0010 0658 3403 2673 0020 0585 3437 2710 0013213 0009790 1*776 684 032 0015 1*763 680 0027 14740 573 056 007 010 004 001 OBS STD STD 0024 0559 34479 2721 0030 0534 3450 2726 0050 0464 3458 2741 0008235 0006885 14731 670 057 0036 14722 665 0051 14698 652 071 012 040 006 001 OBS STD STD STD 0074 0406 34655 2753 0075 0406 3466 2753 0100 0409 3472 2758 0125 0412 3477 2761 0005707 0005312 0004992 14579 640 091 0057 14579 640 0080 14685 538 0093 14691 536 104 041 095 008 001 OBS STD STD STD 0149 0415 34811 2764 0150 0415 3481 2764 0200 0411 3482 2765 0250 0408 3483 2766 0004739 0004695 0004652 14697 535 100 0105 14597 635 0129 14704 636 0152 14711 636 113 002 135 009 001 OBS STD STD 0299 0406 34833 2767 0300 0406 3483 2767 0400 0403 3483 2767 0004650 0004716 14718 537 103 0176 14718 637 0223 14734 625 111 001 155 009 001 OBS STD T0402 0403 34829 2767 0500 039* 3483 2768 0004726 14734 625 107 0270 14746 625 114 004 158 010 001 OBS STD STD STD 0599 0385 34826 2769 0600 0385 3483 2769 0700 0374 3486 2772 0800 0366 3488 2775 0004704 0004447 0004281 14759 524 109 0317 14759 624 0363 14771 630 0405 14785 636 120 003 130 010 001 OBS STD STD T0800 0366 34882 2775 0900 0362 3488 2775 1000 0359 3488 2776 0004320 0004362 14785 635 108 0449 14800 639 0493 14815 5*2 116 002 159 010 001 OBS STD STD 1025 0358 34883 2776 1100 0356 3488 2776 1200 0354 3489 2776 0004406 0004454 14819 543 104 0537 14831 538 0581 14847 532 113 003 088 010 001 OBS STD STD STD T12n9 0354 34885 2776 1300 0353 3488 2776 1400 0353 3488 2776 1500 0353 3488 2776 0004528 0004515 0004709 14848 631 105 0625 14863 631 0671 14880 631 0718 14897 631 120 002 153 oil 001 OBS T151S 0353 34881 2776 14900 631 103 118 002 142 oil LONGITUDE ■1/10 STATION TIME ORIGINATOR'S 5750 N 05140 W 187 71 07 27 123 1955 LCE 9421 0085 01 05 0 X 0013 06 508 105 AIR TEMP. "C 05 SPECIFIC VOLUI 123 123 123 123 123 STD OBS STD OBS STD STD OBS STD OBS STD OBS 0000 0000 0010 0015 0020 0030 0040 0050 0065 0075 0080 0523 0523 0257 0151 0132 0083 0043 0013 -0012 -0013 -0014 3051 30512 3147 31812 3188 3201 32117 3220 32275 3228 32288 2412 2412 2513 25*7 2554 2568 2578 2587 259* 2594 2595 0038020 002843* 0033 002**88 0023220 0050 0084 0021418 0128 0020650 0181 1*660 1*660 1*561 1*52* 1*513 14494 14479 14468 14450 14451 1*462 48 LATITUDE * 1/10 EV 58438N LONGlTUDt * '1/10 DAY HB.1/10 187 ft2 07 28 208 1955 LCE 9422 FORCE OWGINATOR'S BARO- METER (mbi) 33 S17 125 094 078 0 05 0090 WEA- THER CODE NODC STATION NUM8ER 0014 DEPTH (ml T i: Oj ml/I SI04-Si pg - oi/l 208 208 208 208 208 STD OBS STD STD OBS STD STD OBS STD OBS OBS 0000 0000 0010 0020 002? 0030 0050 0050 0075 0C75 0080 0327 0327 0244 0176 0148 0126 0062 0052 0032 0032 0027 3145 31451 3158 3186 31931 3198 3214 32135 3226 32262 32274 2506 2506 2531 2550 2557 2563 2579 2579 2591 2591 2592 0026747 0024913 0023590 0022152 0000 0028 00 54 0078 0124 0021025 0178 14590 14590 14558 14532 14522 14513 14490 14490 14482 14482 14481 770 770 779 788 792 780 749 749 749 749 742 082 008 023 006 076 101 010 033 007 085 112 009 039 007 087 087 107 105 Oil 010 045 045 008 007 LATITUDE I/IO DAY HR.1/1( ORIGINATOR'S Cfl »EI IE* NODC STATION NUMBER 31 549 EV 56463N 062343W 187 82 07 28 221 1955 LCE 9423 01 3 2 XI 3 |7 BARO- METER (mbil AIR TEMP. "C 050 0015 06 221 221 221 221 221 221 STD OBS STD STD OBS STD OBS STD OBS STD OBS STD STD OBS 0000 0000 0010 0020 0024 0030 0049 0050 0072 0075 0097 0100 0125 0135 T 1: 0460 0450 0303 0178 0135 0091 -0011 -0012 -0048 -0056 -0095 -0093 -0078 -0072 3172 31717 3185 3200 32053 3214 32357 3238 32559 3258 32741 3275 3287 32890 2514 2514 2540 2551 2558 2578 2601 2602 2618 2620 2534 2635 2544 2546 0028315 0025835 0023853 0016691 0015889 0000 0027 0052 0022273 0075 0019933 0117 0018215 0155 0209 0249 SOUND VELOCITY 14550 14550 14585 14535 14518 14500 14459 14459 14449 14446 14434 14435 14448 14453 0 3 ml/I 760 760 798 816 818 799 758 758 751 743 702 701 692 689 045 073 002 002 001 003 003 002 087 113 OOB 030 005 089 098 007 041 005 104 129 008 074 009 108 124 010 080 Oil EV 58537N LONGITUDE ■1/10 062085W 239 239 239 239 239 239 STD OBS STD STD OBS STD STD OBS STD OBS STD OBS STD OBS STD OBS T 1: 0000 0000 0010 0020 0025 0030 0050 0050 0075 0075 0100 0100 0125 0125 0150 0190 0486 0486 0322 0193 0142 0112 0022 0022 -0025 -0025 0005 0006 0044 0044 0067 0074 187 82 07 28 239 1955 LCE 9424 SO 2 3169 31692 3198 3223 32353 3248 3284 32841 3296 32958 3318 33179 3337 33355 3351 33541 ORIGINATOR'S BARO- METER 2509 2509 2548 2578 2592 2604 2638 2638 2549 2649 2655 2566 2579 2579 2689 2699 057 0028764 0025083 0022215 0019803 0016558 0192 07 0000 0027 00 51 0072 0108 09 WEA- THER CODE XI 3 |5 SOUND VELOCITY 0015452 0148 0013900 0185 0012675 0218 0011702 0248 14650 14650 14596 14545 14525 14514 14481 14481 14465 14455 14487 14487 14511 14511 14528 14539 0015 Ol ml/1 768 768 812 832 834 815 756 756 719 719 712 712 712 712 697 543 077 003 000 003 102 074 005 007 003 072 095 on 038 006 090 105 012 052 009 094 112 012 079 010 081 110 012 069 009 49 REfERENCE SHIP CODE LATITUDE I/IO LONGITUDE ■ -1/10 ii MARSDEN STATION TIAAE ORIGINATOR'S ' DEPTH MAX. DEPTH OE S'MPL- WAVE WEA- THER CODE CLOUD CODES NOOC CIRY CODE ID. NO. CRUISE NO. STATION NUMBER BOTTOM NUMBER 10" r MO DAY HR.I/10 Oil. HOT PER S A TYPI *M 31 5*9 EV 5 901 3N 061428W 187 91 07 29 020 1965 LCE 9425 0155 01 06 0 2 X4 X 9 0017 WAIER WIND BARO- METER Imbtl AIR TEMP. •= VIS. COO NO. OBS. DEPTHS SPECIAL OBSERVATIONS COLOR coot IRANS. DIR. SCEEO OR FOUCE DRY BULB WET BULB 10 SOB 132 057 051 1 08 MESSENCR TIME < HR 1/10 CAST NO. CARD TYPE DEPTH tml T r s •/.. SIGMA-T sreciFic voiuMi ANOM*L»-I10' SAD DYN. M. X 10= SOUND VELOCITY Oj ml/l PO4-P 1.9 -ol/l lOTAL-P NOi-N ug - of/I NOj-N vg - 01/1 SI04-S< tig - ol/l PH STD 0000 0437 13183 2526 0027210 0000 1*6*2 777 ' 020' OBS STD 0000 0*37 3163* 2525 0010 0353 3185 2535 0025260 ' 1*642 777 048 0027 1*608 779 074 003 000 002 020 OBS STD 0010 0353 31859 2535 0020 0140 3213 2574 0022634 1*608 779 051 0051 14520 795 094 005 000 002 020 OBS STD 0025 0063 32255 2589 0030 0038 3242 2603 0019863 14488 796 070 0072 14479 779 090 006 024 003 020 OBS STD 0049 -0029 32830 2539 0050 -0032 3284 2640 0016334 14458 732 092 0109 14455 731 112 010 067 008 020 OBS STD 0074 -0052 32990 2653 0075 -0049 3300 2554 0015031 14453 712 101 0148 14455 714 124 014 058 Oil 020 OBS STO 0098 0012 33202 2557 0100 0018 3322 2568 0013647 14490 724 085 0184 14493 722 098 012 023 009 020 OBS STO 0108 0035 33273 2572 0125 0035 3338 2580 0012512 14503 713 085 0216 14507 598 095 012 072 010 020 OBS 01*3 0034 33485 2689 1*511 687 101 111 014 084 012 REFERENCE SHIP CODE LATITUDE 1/10 LONGITUDE ' '1/10 MARSDEN STATION 11 WE ORIGINATOR'S OEPIH MAX. V VAVE WEA- THER CODE CLOUD CODES NODC STATION NUMBER cr«Y CODE 10. HO. CRUISE NO. STATION NUMBER BOTTOM OP S'MPL'S OBSruvMiurij 10' r MO DAY HR.1/10 DIP. IHGI! PtSl S * lypt AM 31 5*9 EV G 907 9N 051177W 187 91 37 29 042 1955 LCE 9425 3177 02 03 |iM X4 X 9 0018 WATER WIND BARO- METER ImbO AIR TEMP. '^ VIS. COD NO. OBS. DEPTHS SPECIAL OBSERVATIONS COLOR CODE IHANS. DIR. SPEED 0" fOPCE DRY BULB WET BULB 00 SOO 139 0*4 039 2 06 MESSENGR TIME e HR 1/10 CAST NO. CARD lYPE DEPTH Onl I -c s •/.. SIGMA-T SPECIFIC VOLUME ANOMAlT-xlO' SAD DYN. M. X10= SOUND VELOCITY Ol ml/1 POi-P KB - ol/l tOTAL-P vB - o'/l NO2-N wg - ol/l NO3-N VB - ot/l S10*-Si vg - ol/l pH STD 0000 0386 3151 2505 0029158 0000 1*615 785 [ 0*2 OBS STD STD 0000 ' 0386 31513 2505 0010 0198 3177 2541 0020 0065 3199 2567 0025742 0023281 ' 1*616 786 052 0027 1*539 781 0052 1**84 774 082 003 002 002 0*2 OBS STD STD 0025 0019 32086 2577 0030 0011 3215 2583 0050 -0008 3239 2503 0021799 0019866 14465 771 079 0075 14453 767 0115 14461 751 101 008 032 004 042 OBS STD 0050 -0008 32391 2503 0075 -0005 3259 2527 0017563 14451 751 087 0163 14471 737 105 009 053 008 0*2 OBS STD 0075 -0005 32593 2527 0100 -0008 3285 2540 0016297 14471 737 088 0205 14475 730 101 010 063 008 042 OBS STD STD 0100 -0008 32856 2640 0125 0007 3310 2559 0150 0041 33*1 2682 0014500 0012313 14476 730 090 0244 14490 715 0277 14514 593 104 010 065 008 04 2 OB S 016C 0 559 33 5 52 25 9 I« 14525 582 097 110 017 081 Oil REFERENCE SHIP CODE LATITUDE 1/10 LONGITUDE ■ '1/10 MARSDEN STATION TIME ORIGINATOR'S DEPTH MAX. WAVE WEA- THER CODE CLOUD CODES NODC STATION NUMBER CTBY CODE ID. NO. CRUISE NO. STATION NUMBER BOTTOM OF S'MPL'S OBScKV«.iuni> 10* r MO DAY HR.1/10 DIP- HOT PER SEA typi AM 31 5*9 EV t )915 *N 050498W 187 90 37 29 058 1965 LCE 9*27 0210 02 00 0 X X4 X 9 0019 WATER WIND BARO- METER (mbpl AIR TEMP. •= VIS COD NO. OBS. DEPTHS SPECIAL OBSERVATIONS COLOR CODE TRANS, DIR. SPEED OP FOPCE DRY BULB WET BULB 00 SOO 142 044 039 0 06 MESSENCK TIME □ HR 1/10 CAST NO. CARD TYPE DEPTH Iml I -c s •/„ SIGMA-T SPECIFIC VOLUME ANOMALY-IIO' SAD DYN. M. X 10! SOUND VELOCITY Oj ml/l P04-P ug -or/I roTAi-p UB - ot/l NO3-N ttg - Ol/l NOj-N pg - ot/l SI Oa-SI pg - ol/l pH STD 0000 02*6 3194 2552 002*758 0000 14561 838 068 OBS STD STD 0000 02*6 '319*4 2552 0010 0160 3204 2565 0020 0108 3218 2580 0023443 0022055 1*561 ' 838 054 0024 14525 838 0047 14505 831 087 004 003 003 058 OBS STD 0025 009* 32257 2588 0030 0100 3238 2596 0020495 14502 825 051 0068 14507 814 085 007 018 005 058 OBS STD STD 0040 0104 32584 2613 0050 0077 3273 2625 0075 0035 3302 2652 0017599 0015237 14513 795 052 0105 14505 786 0147 14494 752 081 005 028 004 068 OBS STD STD 0075 0035 33024 2652 0100 0044 3317 2663 0125 0065 3335 2577 0014152 0012801 14494 762 071 0184 14504 738 0216 14520 714 079 009 045 005 058 OBS STD 0125 0055 33364 2577 0150 0100 3361 2595 0011144 14520 714 081 0248 14544 591 094 013 072 008 05 e OB S 018' 0 172 34 C 44 27 2 5 14? 88 661 098 1 10 022 112 01 5 50 REFtBENCE SHIP CODE LATITUDE VIO LONGITUDE * '1/10 So MARSDEN STATION TIME ' ORIGINATOR'S DEPTH MAX. DEPTH OF S'MPL' WAVE WEA- THER CODE CLOUD COOES p ODC ;t«v ODi 1CJ. NO. CRUISE NO. STATION NUMBER BOTTOM OBSt»v«iiv.."» NUMBER 10* r MO DAY HR.1/10 OlIL MCI PER SE* TYPE AMI 31 5«9 EV 5 922 2N 060256W 187 90 07 29 088 1965 LCE 9428 0256 03 00 0 X X4 X. 9 0020 WATER WIND BARO- METER Imbll AIR TEMP. ■c VIS. COO NO. OBS. DEPTHS SPECIAL OBSERVATIONS COLOR CODE TMkNl. DIR. SPEED 0* EOICE DRY BULB ■ATET BULB 06 SO 5 132 039 039 1 07 MEStENCI TIME 0< HR t/10 CAST NO. CARD TYPE DEPTH Iml t t S •''.. SIGMA-T iPEClfiC VOLUME ANOMAl.T-»IO' SAD DTN. M. X 10' SOUND VELOCITY Oj ml/l PC^-P PI . ../I TOTAl-P va - p'/i NOj-N US - oi/l NO3-N wg - 01/1 SI 04-Si i.0 . ol/l pM S C C STD oooo 0267 3173 2533 0026574 OOOO 14567 822 088 OBS STD 0000 ' 0267 '31725 2533 0010 0133 3182 2550 0024937 14567 822 062 0026 14511 835 101 004 008 004 088 OBS STD 0010 0133 31822 2550 0020 0057 3215 2580 0022020 14511 835 052 0049 14483 832 089 004 007 003 088 OBS STO 0024 0036 32276 2592 0030 0033 3246 2606 0019534 14476 831 087 0070 14478 804 107 009 032 006 0 88 OBS STD STD 0049 0028 32941 2645 0050 0028 3295 2646 0075 0031 3318 2665 0015766 0014021 14485 737 080 0105 14486 736 0143 14494 710 096 016 058 007 088 OBS STD STD 0097 0033 33385 2681 0100 0040 3342 2683 0125 0095 3366 2699 0012238 0010732 14502 695 091 0175 14506 695 0204 14538 690 108 012 074 088 OBS STD STD STO 0145 0133 33824 2710 0150 0142 3386 2712 0200 0213 3416 2731 0250 0255 3430 2739 0009528 0007807 0007127 14561 685 087 0229 14566 684 0273 14610 666 0310 14638 642 099 018 092 008 08 8 OBS 0256 0258 34309 2739 14641 639 097 104 026 124 009 REFERENCE SHIP CODE LATITUDE l/IO LONGITUDE 'l/IO ii MARSDEN STATION Tl ^E ORIGINATOR'S DEPTH MAX. DEPTH OF S'MPL' WAVE WEA- THER CODE CLOUD CODES GDC CIPT CODE ID. NO. CRUISE NO. STATION NUMBER BOTTOM NUMBER 10- r MO DAY HR.I/10 DIIL HGI PER S * IIPl AM 31 549 EV 59292N 060005W 187 90 37 29 121 1965 LCE 9429 1646 12 13 0 2 X4 4 8 0021 WATER WIND BARO- METER Imbll AIR TEMP. •c VIS. COD NO. OBS. DEPTHS SPECIAL OBSERVATIONS COLOR CODE TRANS. DIR. SPEED OR FORCE DRY BUL8 WET BULB 16 S04 146 067 061 1 14 MBiSBNC. IcAST ""1 ■!, NO. Hfi 1/10 CARD TYPE DEPTH (ml T 1C s •/.. SIGMA-T SPECIFIC VOLUME ANOMALT-XIO' SAD DYN. M. X 10= SOUND VELOCITY O3 ml/l POi-P „ . .,/! lOIAL-P vB • pl/l NO2-N ug - nl/l NO3-N VO - ot/l 1 SI04-Si VB - di/l PH S C c STD 0000 0444 3324 2636 0016694 0000 14663 746 121' OBS STD STD 0000 0444 33240 2636 0010 0386 3331 2648 0020 0342 3337 2657 0015612 0014763 14663 ' 746 ' 034 0016 14642 752 0031 14625 758 056 007 008 003 121 OBS STD 0024 0328 33392 2660 0030 0316 3341 2663 0014239 14620 760 050 0046 14615 755 071 007 020 003 121 OBS 0032 0307 33426 2665 14613 753 034 052 008 057 003 121 OBS STD 0046 0171 33761 2702 0050 0174 3380 2705 0010182 14560 732 064 0070 14563 725 082 019 057 004 121 OBS STD 0069 0204 33993 2718 0075 0223 3406 2722 0008587 14582 696 080 0094 14592 687 091 022 097 005 121 OBS STD STD 0092 0279 34233 2731 0100 0314 3432 2735 0125 0400 3455 2745 0007404 0006519 14522 668 093 0114 14539 570 0131 14583 675 104 031 108 007 121 OBS STD 0136 0426 34616 2748 0150 0438 3465 2749 0006188 14697 577 099 0147 14705 651 105 005 134 008 121 OBS STD STD T0178 0458 34720 2752 0200 0463 3475 2754 0250 0472 3482 2759 0005764 0005397 14718 537 085 0177 14724 535 0205 14737 535 098 002 148 008 121 OBS STD 0273 0474 34841 2760 0300 0474 3486 2762 0005180 14742 634 103 0231 14747 534 109 004 152 008 121 OBS STD STD T0366 0475 34892 2764 0400 0463 3488 2764 0500 0434 3487 2767 0005013 0004861 14759 633 106 0282 14759 534 0332 14764 635 114 002 133 009 121 OBS STD STD 0565 0421 34869 2768 0600 0419 3488 2769 0700 0414 3489 2771 0004716 0004682 14759 535 105 0379 14774 532 0426 14789 624 117 001 142 009 121 OBS STD STO T0770 0409 34900 2772 0800 0405 3490 2772 0900 0395 3490 2773 0004598 0004573 14798 619 113 0473 14802 517 0519 14814 614 118 001 154 012 121 OBS STD STO 0987 0388 34899 2774 1000 0387 3490 2774 1100 0382 3490 2775 0004568 0004597 14826 613 114 0564 14828 513 0610 14842 517 131 003 162 013 12 1 OB S T116 5 0 381 3' »S 06 2- n 5 14 553 619 112 125 003 153 013 51 31 549 LATITUDE VIO 59362N LONGITUDE '1/10 059343W 158 158 158 158 158 158 158 158 158 158 158 STD OBS STD STD OBS STD OBS STD OBS STD STD OBS STD STD OBS STD STD OBS STD OBS STD STD OBS STD OBS STD STD OBS STD STD OBS 0000 0000 0010 0020 0023 0030 0045 0050 0057 0075 0100 0110 0125 0150 T0179 0200 0250 0263 0300 T0350 0400 0500 0526 0600 0695 0700 0800 T0899 0900 1000 T1082 07 I -c 0688 0688 0669 06't3 0634 0612 0551 0516 0431 0433 0442 0446 0460 0476 0486 0477 0461 0458 0453 04*6 0437 0421 0417 0408 0397 0396 0386 0377 0377 0369 0363 158 1965 SrEED OR EORCE 3350 33500 3370 3387 33923 3400 34216 3434 34669 3470 3479 34817 3485 3489 34916 3490 3489 34884 3489 34888 3489 3490 34902 3491 34922 3492 3492 34917 3492 3491 34909 BAflO- METER Imbt) SIGMA-T 2628 2628 2646 2663 2668 2677 2702 2715 2751 2753 2750 2761 2752 2754 2765 2764 2765 2765 2756 2757 2758 2771 2771 2773 2775 2775 2775 2777 2777 2777 2777 AIR TEMP. T 17 S03 159 083 072 1 12 SPECIFIC VOll 0017537 0015816 0014234 0012895 0009253 0005683 0005129 0004900 0004805 0004798 0004750 DEPTH TO BOTTOM 2140 0004543 0004490 0004251 0004228 0004235 0004258 0000 0017 0032 0045 0067 0086 0100 0112 0124 0148 0172 09 0 2 WEA- THER CODE 0022 SOUND VELOCIIT 0004745 0196 0243 0288 0004367 0333 0375 0418 0461 0503 14756 14766 14763 14755 14754 14747 14728 14716 14588 14691 14700 14704 14712 14724 14733 14732 14734 14735 14739 14744 14749 14759 14761 14770 14781 14782 14794 14807 14807 14820 14831 662 582 735 758 759 730 583 675 552 548 640 538 640 642 643 542 640 639 638 637 534 529 628 527 525 525 627 528 628 531 534 105 079 007 010 004 058 Oil 035 004 107 045 099 007 117 010 138 009 113 004 154 010 100 001 097 007 110 001 145 009 128 002 140 009 115 002 155 Oil 110 124 002 151 Oil 107 118 002 149 010 LATITUDE t/10 LONGITUDE * -i/io 185 186 186 186 186 186 186 186 186 CARD STD OBS STD STD OBS STD STO OBS STD OBS STO OBS STD STD OBS STD OBS STD STD OBS STO OBS STD STD OBS STD STD OBS STD STD OBS STD STD OBS DEPTH Iml 0000 0000 0010 0020 0025 0030 0050 0051 0075 0076 0100 0102 0125 0150 0152 0200 T0203 0250 0300 0305 0400 T0406 0500 0500 0509 0700 0800 T0812 0900 1000 T1036 1100 1200 1218 07 T -C 0808 0808 0807 0774 0746 0675 0479 0473 0439 0438 0461 0463 0482 0494 0495 0491 0491 0480 0469 0468 0449 0448 0432 0416 0415 0402 0389 0388 0377 0367 0364 0359 0353 0352 186 1965 SPEED OR FORCE S02 3400 33995 3405 3414 34184 3424 3445 34455 3468 34690 3480 34811 3485 3490 34899 3491 34910 3491 3491 34905 3490 34897 3490 3491 34911 3492 3492 34920 3492 3492 34915 3492 3492 34922 ORIGINATOR'S LCE 173 2649 2649 2655 2566 2673 2688 2729 2730 2751 2752 2758 2759 2750 2752 2762 2763 2764 2765 2765 2766 2758 2757 2759 2772 2772 2774 2775 2776 2777 2778 2778 2779 2779 2779 9431 AIR TEMP. *C 100 0015467 0014987 0013945 0011892 0008021 0005900 0005258 0005134 0004969 DEPTH TO BOTTOM SAD DVN. M. X 10^ DEPTH OF S'MPL'S Gfl PER i£* NODC STATION NUMBER SOUND VELOCITY 0004815 0004747 0004515 000445B 0004357 0004270 0004213 0004182 0004172 0004182 0015 0030 0043 0063 0080 0094 0107 0119 0004892 0144 0168 0192 0004704 0240 0286 0332 0376 0419 0461 0503 0545 0687 14819 14819 14821 14811 14802 14776 14702 14700 14693 14693 14708 14709 14721 14731 14732 14738 14739 14742 14746 14746 14754 14754 14753 14773 14774 14784 14795 14797 14807 14819 14824 14833 14847 14850 Ol ml/l 582 682 580 576 577 677 575 575 551 650 641 540 540 540 540 540 540 540 539 639 636 535 530 525 624 525 626 526 529 532 633 536 537 637 NOj-N SI04-Si 019 043 002 004 004 025 048 005 013 004 095 074 023 054 004 115 049 112 008 126 020 120 010 128 009 172 Oil 105 007 105 008 007 130 009 129 004 149 010 095 103 003 147 009 115 132 005 002 012 Oil 109 115 003 140 Oil 52 MFfHENCE SHIP coot LO ^CITUDE §i MARSOEN STATION T ME ORIGINATOR'S 3EPTH MAH . WAVE WEA- THER CLOUD CODES CTIT ID. LATITUDE SQUARE IGMT) EAR CRUISE STATION TO BOTTOM OF OBSERVATIONS STATtON COD( NO. 1/10 ■ 'l/io 10* r MO DAY H H.l/tO NO. NUMBER S-MPL-S OIH. MGI HI ilA CODE TTPl *w NUMBER 31 5*9 EV 59505N 0S84«3H 166 ?8 dTI 29 207 1965 LCE 9432 2743 12 12 1 3 1 X4 X 9 0024 WATER WIND BARO- AIR TEMP. -C 1 NO. COLOR TftANS. D1R. S«fO METER DRY WET coy.pA^-., SPECIAL OBSERVAHONS • CODE ln>I fOdCE {mbl) BULB BULB * 18 SO 2 169 094 089 r~ 12 "'"""' 1 CAST IIMi or NO. Hfi VtO CARD TYfS DEPTH (ml T "C s v.. S1GMA-T specific voiuMi ANOMALY-XIO' SAO DYN. M. t 10» SOUND VELOCITY Oj ml/I lOTAl-P vg • ol/l NOi-N ug - al/l NO]-N i«g - ol/l SI04-Si vg - ol/l pH I C c STO 0000 1 0831 3398 2645 0015930 0000 14828 667 ~ 207 OBS 0000 0831 33977 2645 14828 ' 667 022 051 003 005 002 STD 0010 07*8 3399 2658 0014689 0015 14798 678 STD 0020 0667 3408 2676 0012968 0029 14769 684 207 OBS 0025 0627 34142 2686 14754 686 041 059 Oil 028 005 STO 0030 0571 3428 2704 0010310 0041 14735 686 STD 0050 0430 3473 2756 0005401 0056 14685 678 207 OBS 0051 0427 34747 2758 14685 677 082 095 028 088 005 STD 0075 0449 3477 2757 0005327 0070 14698 649 207 OBS 0076 0450 648 095 107 061 125 008 STD 0100 0475 3479 2755 0005485 0083 14714 642 207 OBS 0102 0477 641 099 109 001 141 008 STO 0125 0488 3482 2757 0005429 0097 14723 640 STD 0150 0499 3484 2757 0005438 0111 14732 639 207 OBS 0152 0500 34845 2757 14733 539 103 115 003 142 010 STD 0200 0485 3490 2763 0004889 0136 14735 637 207 OBS T0203 0484 34907 2764 14735 537 097 110 002 152 009 STD 0250 0473 3490 2755 0004810 0161 14739 638 STD 0300 0452 3490 2766 0004742 0185 14743 638 207 OBS 0305 0461 34896 2766 14743 638 101 111 001 155 010 STD 0400 0439 3489 2767 0004702 0232 14749 631 207 OSS T0406 0438 34884 2767 14750 631 101 109 001 158 010 STD 0500 0425 3489 2769 0004610 0278 14750 630 STD 0500 0412 3489 2771 0004551 0324 14771 528 STD 0700 0400 3489 2772 0004520 0370 14783 627 STD 0800 0388 3489 2773 0004474 0415 14794 625 207 OBS T0812 0387 34892 2774 14796 625 108 121 001 150 Oil STO 0900 0375 3489 2775 0004423 0459 14805 533 STD 1000 0357 3489 2775 0004404 0503 14819 542 207 OBS 1036 0354 34886 2775 14824 545 109 122 004 161 Oil STD 1100 0360 3489 2776 0004398 0547 14833 643 STD 1200 0357 3490 2777 0004392 0591 14848 634 20- OBS T1218 0357 34899 2771 14851 631 107 119 002 150 Oil I 53 I REFERENCE SHIP CODE LONGITUDE s o MARSDEN STATION T ME ORIGINATOR'S DEPTH MAX. DEPTH OF WAVE WEA- THER CODE CLOUD CODES ^ODC cmT CODE ID. LATITUDE SQUARE IGMTI YEAR CRUISE STATION TO BOTTOM OBSERVATIONS STATION NUMBER NO, I/IO 1/10 ~ 10* 1" MO DAY M R.1/10 NO. NUMBER S'MPL'S OIR. HCI PER 1 A irPE AM 31 5*9 EV 60258N 058477W 222 08 07 30 012 1965 LCE 9433 2614 13 26 0 2 X* X 9 0025 WATER WIND AIR TEMP. -C NO. COLOR THAN 5. ifttD METER DRY WET CO^D^.PA^.-.. SPECIAL OBSERVATIONS CODE In.) (Oice (mbtl 8ULB BULB ucriMi 12 S03 159 067 067 1~ 12 f^ESSENCR cA^T HR 1/10 T CARD TYPE DEPTH Iml T IC s •/„ SIGMA-T SftCIFIC VOlUMt ANOMAU-llO' 5 A D DYN. M. SOUND VELOCIIY Ol ml/I PO<-P vg-o./l lOTAL-P vB - o'/l NO3-N ug - ol/l NO3-N iig - ot/l SIO^-SI wg - ol/l pH C STD 0000 0838 3*07 2651 0015347 0000 14832 *2* 012' ' OBS 0000 ■ 0838 '34069 '2551 ' 1*832 ' *2* '023 058 005 003 003 012 OBS 0005 0771 3*070 2561 1*807 575 050 007 002 005 STO 0010 0765 3*08 2563 001*238 0015 1*805 675 STD 0020 0752 3*10 2666 0013907 0029 1*802 578 012 OBS 0026 07** 3*117 2568 1*800 579 029 0*5 003 005 003 STD 0030 059* 3*15 2579 0012735 00*2 1*782 580 STO 0050 0502 3*35 2716 0009022 005* 1*711 585 012 OBS 0052 0*88 3*359 2721 1*705 586 0*3 095 003 000 003 STD 0075 0*69 3*58 27*0 0005955 008* 1*70* 651 STD 0100 0*55 3*75 2756 0005*93 0100 1*705 6*1 012 OBS 010* 0*53 3*781 2758 1*705 538 10* 119 057 120 009 STD 0125 0*61 3*81 2759 0005210 0113 1*712 538 STD 0150 0*59 3*8* 2751 0005101 0125 1*720 537 STD 0200 0*80 3*89 2753 000*907 0151 1*733 536 012 OBS 0211 0*81 3*89* 2763 1*735 635 102 127 005 150 010 STD 0250 0*81 3*90 276* 000*879 0175 1*7*2 635 STD 0300 0*79 3*91 2755 000*831 0200 1*750 53* 012 OBS T0316 0*77 3*918 2765 1*752 533 102 137 003 158 Oil STD 0*00 0*60 3*91 2767 000*725 02*7 1*758 528 012 OBS 0*21 0*56 3*913 2758 1*760 527 108 119 001 158 Oil STD 0500 0*37 3*91 2770 000*598 029* 1*765 627 STD 0500 0*16 3*91 2772 000**95 0339 1*773 527 012 OBS 0527 0*11 3*90* 2772 1*775 527 082 09* 002 153 010 STD 0700 0*03 3*91 2773 000**05 038* 1*78* 628 STD 0800 0392 3*91 2774 000*372 0*28 1*795 529 STD 0900 0381 3*91 2775 000*33* 0*71 1*808 530 012 OBS 0950 0375 3*91* 2775 1*815 531 116 12* 007 162 012 STD 1000 0369 3*91 2777 000*280 051* 1*820 632 STD 1100 0359 3*91 2778 000*2*5 0557 1*833 533 012 OBS T115* 0355 3*908 2778 1*8*0 533 103 119 002 159 Oil STD 1200 0356 3*91 2778 000*285 0500 1*8*8 533 STD 1300 0356 3*92 2779 000*322 05*3 1*855 532 nl2 OBS T1336 0356 3*919 2779 1*871 631 101 108 001 158 Oil REfERENCE SHIP CODE LATITUDE LONGITUDE MARSDEN SQUARE STATION TIME IGMTI YEAR ORIGINATOR'S DEPTH TO BOTTOM MAX. DEPTH OF WAVE OBSERVATIONS WEA- THER CLOUO CODES NOOC STATION CIRY ID. CRUISE STATION CODE NO. 1/10 ■1/10 10* r MO DAY H R,1/10 NO. NUMBER S'MPL'S Dlft. HGI PER i A CODE TYPE AM NUMBER 31 5*9 EV 60272N 059308W 222 09 07~ 30 0 53 1965 LCE 9434 2450 12 00 0 X X* X 9 0026 WATER WIND BARO- AIR TEMP. "C NO. COLOR IRANS. DIR. S«£D METER DRY WET VIS. coo OBS. SPECIAL OBSERVATIONS CODE ""' FOflCt Imbil BULB BULB DEPTHS 18 S02 1^6 056 056 r~ 11 """!>«:■ IcASl ""' •no. HH VIO CARD TYPE DEPTH Iml T -C s ■/.. SIGMA-T SPECIFIC VOLUMt ANO'MALt-IlO' 5 Ao DYN. M. t I03 SOUND VELOCITY Oj ml/l PO.-P vfl -ol/l NOj-N ug - ol/l NOj-N US - ol/l SI O.-Si pg . ol/l pH I C C STD 0000 0746 3395 2655 0014952 0000 14795 673 053 ' OBS 0000 ' 07*6 339*9 2555 ' 1*795 573 '021 0*3 009 002 002 STD 0010 0710 339* 2650 001*52* 0015 1*782 590 053 OBS 0011 0705 339*3 2660 1*781 591 021 038 013 003 002 STD 0020 0675 3396 2656 00139*3 0029 1*770 589 STD 0030 0609 3399 2676 0012953 00*2 1*7*5 585 053 OBS 0035 0553 33997 2683 1*728 585 033 0*6 010 022 003 STD 0050 0375 3*38 273* 0007*52 0053 1*558 55* 053 OBS 0050 0375 3*38* 273* 1*658 65* 077 093 039 095 005 STD 0075 0*05 3*5* 27** 0005598 0080 1*577 550 STD 0100 0*30 3*57 2751 0005903 0095 1*693 639 STD 0125 0*50 3*78 2758 0005315 0110 1*707 530 053 OBS 0129 0*53 3*800 2759 1*709 629 102 112 001 1*6 008 STD 0150 0*52 3*81 2760 0005157 0123 1*713 630 STD 0200 0*50 3*83 2752 00050*7 01*9 1*720 532 STO 0250 0**8 3*85 2763 000*938 017* 1*728 53* STD 0300 0**6 3*87 2755 000*829 0198 1*735 537 053 OBS 0309 0**6 3*858 2755 1*737 537 103 118 002 1*6 009 STD 0*00 0*2* 3*85 2757 000*721 02*5 1*7*3 539 053 OBS T0*13 0*21 3*859 2757 1*74* 539 10* 115 001 15* 009 STD 0500 0*11 3*85 2758 0004675 0293 1*75* 538 STD 0500 0*03 3*87 2770 000*608 0339 1*757 637 053 OBS 0519 0*02 3*87* 2771 1*770 537 10* 111 000 1*5 009 STO 0700 0*02 3489 2772 0004543 0385 1*78* 535 STO 0800 0398 3*91 277* 000***2 0*30 1*799 53* 053 OBS T082* 0397 3*911 277* 1*803 533 109 115 000 155 010 STO 0900 0387 3*91 2775 000*390 047* 14811 531 STO 1000 0375 3491 2775 0004341 0518 1*823 528 053 OBS 105* 0371 3*91* 2777 1*830 526 110 118 001 1*5 Oil STO 1100 0368 3*91 2777 000*331 0551 1*836 527 STD 1200 0362 3*91 2778 000*350 050* 1*851 532 05 3 OB 5 T12*2 o: 61 3^ 9 11 27 7E 148 57 635 109 119 005 163 010 54 31 I 549 LATITUDE LONGITUDE ! 060055W 223 00 082 082 082 082 STO DBS STD STD OBS STD STD OBS STD STD STD OBS STD STD OBS STD STD OBS STD STD OBS STD STD OBS STD OBS STD OBS DEPTH Im) 0000 0000 0010 0020 0027 0030 0050 0058 0075 0100 0125 01** 0150 0200 0239 0250 0300 T0375 0*00 0500 T056* 0600 0700 0731 0800 T0896 0900 T0992 MO DAY HH.I/ T IC 071* 071* 0561 0**8 0392 0389 0378 0376 0397 0*22 0*40 0450 0*50 0**7 04*1 0*36 0*16 0393 0390 0380 0376 0376 0376 0375 0373 0369 0370 0382 07 30 082 1965 22 3381 33807 3390 3400 34074 3411 3434 34415 3452 3466 3477 3*827 3*83 3*85 3*865 3486 3485 34840 3484 3*84 34833 3483 3484 34838 348* 348*5 3485 3*874 ORIGINATOR'S LCE 9435 146 26*8 2648 2675 2696 2708 2711 2731 2737 2743 2751 2758 2762 2762 2764 2766 2766 2767 2769 2769 2770 2770 2770 2770 2770 2771 2772 2772 2773 AIR TEMP. X 061 0015583 0013013 0011040 0009632 0007812 0006668 000589* 0005284 000*969 00048*0 0004699 0004608 0004507 000*521 000*574 000*641 000*659 00046** 2103 SAD DTN. M. X to' 0000 001* 0026 0037 0054 00 72 0088 0102 0115 0139 0163 0186 0232 0277 0323 0369 0415 0*62 3 2 X2 7 |8 SOUND VELOCITY 14780 1*780 1*722 1*679 1*657 1*657 1*659 1*660 1*673 1*690 1*703 1*711 1*712 1*719 1*723 1*723 1*723 1*725 1*728 1*7*1 1*7*9 1*755 1*772 1*777 1*787 14802 1*803 1*82* 0027 03 ml/l 680 680 686 692 696 693 673 666 655 6*2 631 625 625 522 618 615 60* 593 593 592 591 591 593 593 591 588 588 598 019 0*0 000 001 002 056 070 058 047 00* 079 088 039 099 006 105 116 001 1*5 008 108 118 042 1*9 010 112 127 003 156 013 112 121 002 162 013 106 118 000 158 014 115 123 002 155 014 11* 120 000 165 014 549 EV LONGITUDE ■1/10 60279N 060464W 223 12* 12* 12* 12* 12* 12* 124 124 lYPE STD OBS STD STD OBS STD STD OBS STD OBS STD OBS STD STD OBS STD OBS STD STD STD OBS STD STD OBS STD STD OBS STD STD OBS OBS STD STO OBS 0000 0000 0010 0020 0027 0030 0050 0053 0075 0080 0100 0106 0125 0150 0160 0200 0213 0250 0300 0400 T0426 0500 0500 T0639 0700 0800 T0851 0900 1000 T1065 T1085 1100 1200 T1277 07 30 T IC 056* 056* 04*3 03*7 0295 0282 0213 0206 0178 0172 0252 027* 03*4 0411 0430 0450 0455 0459 0453 0*73 0475 0461 0**1 0*33 0*15 0395 0388 0388 0389 0389 0393 0393 0392 0391 12* 1965 SPEED FORCE SO 8 3329 33292 33** 3357 336*3 3357 3382 33835 339* 33975 3*20 34252 3*4* 3452 34658 3475 34773 3480 348* 3*89 3*901 3*91 3*91 3*911 3490 3489 34886 3489 3490 34900 34911 3*91 3*92 34926 ORIGINATOR'S 146 2627 2527 2552 2672 2683 2585 2704 2706 2716 2720 2731 273* 2742 2749 2751 2756 2757 2759 2761 275* 2755 2757 2759 2770 2771 2773 2773 2773 277* 277* 2774 2775 2775 2775 9436 AIR TEMP. "C 061 056 SPECIFIC VOLUME 0017591 0015189 0013299 0011987 0010315 0009159 0007774 0005797 0006130 0005395 0005204 0005050 0004875 000*748 0004619 0004555 0004574 0004518 DEPTH TO BOTTOM NO. OBS. DEPTHS 15 2 2 XI 0000 0016 0031 0043 0056 0129 0145 0005621 0175 0202 0229 0280 0330 0378 0425 0471 0516 0562 0004641 0609 0004559 0655 I 14714 14714 14667 1*630 14510 14505 14580 14578 14571 14559 14511 14522 14658 14693 14703 14719 14724 14732 14742 14753 14769 14775 14784 14787 14789 14797 14803 14811 14828 14839 14844 14847 14863 14875 0028 0: ml/l 594 594 714 726 729 725 706 703 58* 678 647 640 533 625 624 621 520 621 622 624 62* 619 611 608 599 589 585 587 590 592 597 597 599 600 NO3-N us - at/I St 0^-Si «0-ol/l 018 037 002 001 001 041 050 007 031 002 055 074 091 095 102 115 108 079 087 107 107 110 103 111 108 118 126 122 015 057 004 020 085 005 019 124 007 014 144 008 003 144 008 001 146 010 006 163 010 002 152 013 008 169 012 000 151 013 111 120 000 158 012 55 REFERENCE SHIP CODE LAmuDE 1/10 lONGITUOt ■ -vio -2 ii MARSDEN STATION TIME ORIGINATOR'S DEPTH MAX. DEPTH Of S'MPL- WAVE WEA- THER CODE CLOUD COOES NODC STATION NUMBER cool 10. NO. CRUISt NO. STATION NUMIER BOTTOM ^"""'"" 10' r MO DAY MR.1/10 DIA MCI f(t »* Itfl AM 31 5*9 EV 60282M 061039W 223 01 07 30 140 1965 LCE 9437 0561 05 10 0 2 X2 4 8 0029 WATER WIND (ARO- MtTER (mbtl AIR lEWP. ^ ==».oEs SPECIAL OISERVATIONS COLOR coot 1IANS. DIR. trfto fO>Ci DRT euLO WEI RULB 16 SO 8 135 061 050 8 >^ »I!IIKC. c»st TI»I . NO. HR 1/10 CARD lYfE DEPTH (ml T TC s ■/.. SICMA-T ANOMAH-DO' SAD DYN. M. X 10' SOUND VELOCITT Oiml/I POj-P ne • ot/i rOTAL-P irg - ot/l NOj-N .g - .1/1 NO,-N PS - 01/1 S10«-Si „ . =1/1 pH S c c STD 0000 0331 3314 2639 0016413 0000 14614 737 1*0' 08S 0000 0331 33137 2639 14614 737 036 056 001 013 003 STD 0010 0303 3334 2658 0014645 0016 14605 731 STD 0020 0239 3348 2575 0013075 0029 14582 727 STD 0030 0139 3355 2688 0011852 0042 14541 726 140 DBS 0030 0139 33548 2688 14541 726 059 071 012 048 004 140 DBS 0039 0018 33556 2595 14488 727 069 082 Oil 058 005 STO 0050 0042 3359 2597 0010961 0065 14501 713 140 CBS 0064 0073 33834 2715 14521 683 088 096 000 090 005 STO 0075 0265 3424 2733 0007566 0088 14613 644 140 CBS 0079 0310 34335 2737 14634 635 097 105 021 131 007 140 OSS 0098 0336 34395 2739 14649 625 082 088 018 105 005 STD OIW) 0343 3441 2740 0006993 0106 14553 625 140 OBS 0118 0397 34531 2744 14680 519 098 107 005 141 008 STO 0125 0418 3459 2746 0006403 0123 14591 615 140 OBS 0147 0466 34720 2751 14717 508 098 109 001 148 008 STD 0150 0458 3473 2752 0005914 0138 14718 508 140 OBS T0196 0482 34805 2756 14732 605 099 105 001 125 008 STD 0200 0481 3481 2757 0005515 0157 14733 505 STD 0250 0469 3483 2750 0005288 0194 14736 599 STO 0300 0454 3484 2762 0005100 0220 14738 594 140 OBS T0304 0453 34842 2752 14739 593 109 123 005 140 012 140 OBS T0362 0432 34845 2755 14740 586 112 122 002 158 012 STD 0400 0432 3485 2765 0004925 0270 14746 585 140 OBS 0478 0*33 34845 2765 14759 585 099 113 002 147 on REFERENCE SHIP CODE LATITUDE 1/10 LON GITUDE si MARSDEN STATION TIME ORIGINATOR'S DEPTH MAX. DEPTH OF S-MPL- WAVE WEA- THER CODE CLOUD CODES NODC CIRT ID. NO. cruise! STATION NUMBER CODE * '1/10 - 10- r «0 DAY H ILl/lO Dl». JHCI]'»| I * TVtt AM 31 5*9 EV 60284N 051237W| 223 01 37 30 1 57 1965 LCE 9438 |0402 03 13 |iM X4 7 8 0030 WATER WIND BARO- METER Imbtl AIR TEMP. 'C VIS. cool NO. OBS. DEPTHS SPECIAL OBSERVATIONS COLOR coot IRANI. DIR. inio o« fOtCt DRY BUL8 WET BULB 15 S09 135 050 040 1 11 . MESSENCR r^sT "»' • NO. HR 1/10 CARD TYPE DEPTH Iml T X s •/.. SiGMA-T SKClflC VOIUMI ANOMALT-XIO' SAD DYN. M. X 10' SOUND VELOCITY Oj ml/I PO<-P l.g - ol/l TOTAl-P „g - ot/l NO,-N ug - ot/l NO)-N pg - ol/l SIO.-SI PH S C C STO 0000 0236 3081 12462 0033292 oooo 14541 897 157' OBS STD 0000 ' 0235 30810 2452 0010 0179 3097 2479 0031699 14541 897 068 0032 14520 888 088 018 051 006 157 OBS STD 0013 0162 30999 2482 0020 0124 3105 2488 0030793 14513 886 052 0054 14498 881 109 005 000 004 157 OBS STD 0020 0124 31046 2488 0030 0002 3195 2567 0023288 14498 881 054 0091 14455 811 095 005 001 003 157 OBS STD 0040 -0060 32569 2519 0050 -0029 3279 2536 0016729 14438 759 087 0131 14457 727 101 009 054 009 157 OBS STD 0059 -0009 32931 2646 0075 0005 3304 2655 0014952 14470 709 093 0170 14480 707 104 010 075 009 157 OBS STD 0079 0009 33070 2657 0100 0022 3321 2557 0013743 14483 706 093 0205 14495 701 115 Oil 064 009 157 OBS STD STO 0118 0050 33372 2579 0125 0056 3344 2583 0150 0140 3373 2702 0012229 0010498 14513 695 094 0239 14522 594 0257 14563 583 108 013 080 010 157 OBS T0150 0177 33868 2711 14583 675 080 093 003 088 005 157 OBS STD T0194 0335 34459 2744 0200 0345 3449 2746 0005490 14556 629 094 0310 14671 526 103 012 135 008 157 OBS STD STD T0236 0393 34531 2752 0250 0405 3467 2754 0300 0428 3478 2750 0005799 0005251 14700 511 103 0340 14708 606 0358 14727 595 113 003 134 009 15 7 OB S 030 2 0 428 3' *■ ^80 2- 76 0 14 727 595 107 115 003 149 Oil 56 <1EFEUNCE SHIf CODE LATITUD£ lyio LONGITUDE ■ '1/10 li MASSOEN STATION TIME ORIGINATOR'S | DEPTH TO BOTTOM MAX. DEPTH Of S'MPL'S WAVE WEA- THER CODE CLOUD CODES — S?. ID. NO. CRUISE NO. STATION NUMBER OBSERVATIONS STATION NUMBER 10- r MO DAV HR.1/10 OH. MCilrfl if* I'PI AM 3ii 5*9 EV i028 5N 061382W 223 01 07 30 170 1965 LCE 9439 0389 OA 19 il^ X4 7 8 0031 •water WIND AIR TEMP. X. COLOR ItAHi. snto MSTER DRt WET COf)F OBS. OBSERVATIONS •"' IO»CI ln. MGI Pt« JtA ItPl AM 31 549 EV 6 028 3N 062208W 223 02 D7 30 205 1965 LCE 9441 0342 03 12 0 4 XI 3 7 0033 WATER WIND BARO- METER (mbfl AIR TEMP. •c ^dEs SPECIAL OBSERVATIONS COLOR CODE tl*NS. DIR. SPEED OP fOPCI DRY RULB WET BULB 16 SOS 125 092 092 8 11 MESStNCR TIME e MR 1/10 ' CAST NO. CARD TYPE DEPTH Iml T -C s •/„ SIGMA-T iPtClfIC VOLUME ANOMALT-XIO' SAO DTN. M. X lo' SOUND VELOCITf Oj ml/l POi-P "9 • ""'1 rOTAl-P „t ■ ol/l NOl-N lis - oi/l NO3-N us - ot/l S104-SI VB - oi/l pH S c c STD 0000 0222 3117 2492 0030438 0000 14340 915 ' 205' OBS STD STD 0000 ' 0222 31173 2492 0010 0138 3151 2532 0020 0080 3192 2561 0025580 0023892 14540 915 044 105 0029 14510 840 0054 14490 790 004 000 001 205 OBS STD 0021 0075 31945 2553 0030 0055 3205 2572 0022775 14489 785 073 103 0077 14483 774 010 029 005 206 OBS STD 0040 0044 32186 2584 0050 0046 3238 2599 0020200 14481 750 082 096 0120 14485 745 009 052 006 205 OBS STD 0059 0047 32520 2511 0075 0008 3255 2523 0017951 14490 735 088 0168 14475 724 010 055 008 206 OBS STD 0079 0002 32680 2625 0100 0009 3288 2541 0015191 14475 722 089 107 0210 14484 730 Oil 059 008 206 OBS STD STD 0118 0014 33084 2658 0125 0037 3318 2554 0150 0108 3350 2586 0014045 0012029 14492 733 092 117 0248 14505 732 0281 14545 730 012 068 009 205 OBS T0154 0118 33552 2589 14552 730 074 088 014 052 005 206 OBS STD 0191 0194 33998 2720 0200 0203 3402 2721 0008784 14598 570 093 102 0333 14504 668 019 108 008 205 OBS T0213 0227 34091 2724 14617 651 095 107 020 108 008 206 OBS STD 0242 0328 34427 2742 0250 0340 3448 2745 0006555 14570 529 100 109 0371 14577 525 012 131 005 205 OBS T0265 0344 34536 2750 14682 623 104 112 006 134 Oil SHIP CODE LONGITUDE STATION TIME ORIGINATOR'S NODC STATION NUMBER 549 EV 60292N 223 02 07 30 230 1965 LCE 9442 03 17 0034 230 230 230 230 230 230 230 230 230 230 STD OBS STD OBS STD OBS STD OBS STD OBS STD OBS STD STD OBS STD OBS STD OBS STD OBS 0000 0000 0010 0010 0020 0024 0030 0048 0050 0072 0075 0094 0100 0125 T0142 0150 T0187 0200 T0223 0250 0255 T 1; 0314 0314 0172 0072 0043 0032 0010 0009 0002 0001 -0002 -0001 0007 0018 0025 0054 0116 0183 0221 0224 s •/.. 3089 30887 3119 31189 3141 31497 3164 31959 3198 32157 3218 32317 3242 3279 32995 3302 33356 3369 34075 3414 34175 2462 2452 2497 2520 2529 2541 2567 2569 2584 2585 2597 2605 2634 2650 2552 2678 2700 2727 2729 2731 AIR TEMP. "C 0033286 0029990 0027741 0025790 0023080 0021507 0019556 0016863 0015200 0010546 0008052 SAD DYN. M. X 10^ 0000 0032 0061 0087 0136 0192 0243 0289 0329 0394 0440 14575 145 76 14520 14479 14468 14456 14463 14453 14456 14457 14470 14473 14485 14497 14502 14530 14550 14599 14621 14625 03 ml/l 909 909 880 880 822 804 790 750 759 752 752 749 742 719 708 706 697 680 562 568 571 TOTAL-P „9 ■ oi/l NO3-N Itg - ol/l NO3-N VS ■ ol/l S10<-Si VS - ol/l 055 106 095 091 098 068 000 000 002 100 003 003 003 096 007 030 005 104 012 Oil 005 102 008 051 007 099 009 053 008 138 009 082 010 106 Oil 095 010 096 015 113 009 111 015 095 009 58 31 549 LATITUDE 1/10 50293N DAY HR.1/10 223 Q2 07 31 005 1965 LCE 9443 into fOICI ORIGINATOR'S flARO- METER (mbl) 102 0307 03 IB 1 2 WEA- THER CODE 003S DEPTH Iml T X S •/.. SOUND VELOCITY NOj-N HS - ol/l SIO4-SI 005 005 005 005 005 005 005 005 005 STO OBS STD OBS STD OBS STD STD OBS STD OBS STD OBS STD STD OBS STD OBS STD OBS 0000 0000 0010 0016 0020 0027 0030 0050 0052 0075 0079 0100 0104 0125 0150 0158 0200 T0210 0250 0283 0181 0181 0159 0142 0125 0102 0095 0056 0052 0015 0010 -0016 -0019 -0010 0004 0009 0042 0049 00 75 0096 3113 31128 3114 31171 3120 31259 3128 3147 31493 3180 31859 3229 32351 3250 3269 32758 3317 33253 3352 33669 2491 2491 2494 2497 2500 2506 2509 2526 2528 2554 2550 2595 2600 2612 2526 2632 2563 2669 2689 2700 0030511 0030283 0029531 0028848 0027193 0024476 0020582 001899* 0017502 0014136 0011677 0000 0030 0050 0090 0146 0210 0257 0316 0352 0441 0506 14521 14521 1*513 14507 14501 1*492 14490 14478 14477 14468 14467 14464 14465 14474 1*487 14*92 1*520 14526 14548 14565 923 923 923 923 902 869 858 804 800 776 773 759 757 744 730 726 705 701 691 689 053 100 071 096 087 105 095 113 099 112 004 073 002 004 000 002 005 003 002 007 032 005 009 039 007 010 0*2 008 Oil 072 009 010 083 009 01* 099 010 REFERENCE SHIP CODE LATITUDE 1/10 LONGITUDE •1/10 Si MARSDEN STATION Tl M ORIGINATOR'S DEPTH MAX. DEPTH OF S'MPL' WAVE WEA- THER CODE CLOUD CODES NODC CIRT CODE ID. NO. CRUISE NO. STATION NUMBER BOTTOM 10- T MO DAY HR.1/10 DIR. HOT PER S * Un AM 31 5*9 EV 6 029 «N 053157W 223 03 07 31 023 1965 LCE 9*** 0316 03 15 1 2 X4 6 8 0036 WATER WIND SARO- METER Imbil AIR TEMP. ^ VIS. COD NO. OBS. DEPTHS SPECIAL OBSERVATIONS COLOR CODE TRANS. DIR. SPEED OR EOtCt DRY BULB WET BULB 16 SIO 102 089 089 5 10 MtSSENCP j HR 1/10 CAST NO. CARD TYPE DEPTH Iml I -c s ■/.. SIGMA-T SPlClflC VOLUME ANOMALf-XlO' SAD DYN. M. t 10= SOUND VELOCITY 0; ml/1 P0«-P lOTAl-P ve - ot/i NOi-N wg - ol/l NOj-N ws - ol/l SI 0*-Si VB - ol/l PH S c c STD 0000 0258 3001 2395 0039551 0000 1*5*0 919 ' 023 OBS STD 0000 0258 30005 2395 0010 0170 3106 2*85 0030959 1*5*0 919 0*5 0035 1*517 90* 08* 003 000 002 023 OBS STD 0011 0162 31128 2492 0020 0093 3126 2507 0028993 1*515 901 05* 0065 1**87 850 102 006 002 002 023 OBS STD STD 0026 0050 31354 2516 0030 0056 3144 2523 0050 00*1 3182 2555 0027430 0024450 1**7* 838 060 0093 1**7* 832 01*5 1**75 802 095 009 015 003 023 OBS STD 0051 00*0 31839 2555 0075 0029 3214 2581 0021941 1**75 801 072 0203 1*479 773 095 007 030 004 023 OBS STD 0077 0027 32170 2583 0100 -0005 3248 2510 0019180 14479 771 081 0255 14472 748 100 007 041 006 023 OBS STD STD 0102 -0007 32507 2512 0125 -0014 3268 2526 0150 -0021 3283 2639 0017505 0016*19 14472 745 089 0301 14475 735 0343 14478 725 102 009 059 008 023 OBS STD 015* -0022 32850 2540 0200 0010 3299 2650 0015332 14478 724 095 0*23 14503 716 11* 010 073 010 023 OBS STD 0206 0015 33011 2652 0250 0058 3320 2564 001*011 1*506 715 095 0*96 1*535 707 105 012 079 010 023 OBS T0284 0092 33343 2574 1*559 701 098 107 010 084 Oil 02 3 OB S 029! s 0 178 3- is 16 2- 1 4 1*( )07 670 087 101 016 099 010 59 REFERENCE SHIP CODE LATITUDE 1/10 LONGITUDE '1/10 ii MARSDEN STATION TIME ORIGINATOR'S I DEPTH MAX. WAVE WEA- THER CODE CLOUD CODES NODC Ci«r ID. NO. YEAR CRUISE NO. STAT NUM ON TO OF S'MPL'S STATION NUMBER CODt 10- 1 r MO DAY HR.1/10 DH. HGT P(l S A r>p( AM 31 549 EV i 029 3N 053362W 223 |03 1 D7 31 041 1955 LCE 9445 0325 02 00 0 X X4 7 1 0037 WATER WIND BARO- METER Imbf) AIR TEMP. •c VII, CODd NO. OBS. DEPTHS SPECIAL OBSERVATIONS COLOR CODE TRANi. D1R. into FORCE DRY BULB WET BULB 14 SO 4 033 033 0 08 ME$$fNCIl IIMi 0 HH 1/10 1 CAST NO. CARD TYPE DEPTH (m) I "C s •/.. SIGMA-T SPECIFIC VOLUME ANOMALT-X10' SAD DYN. M. X 10= SOUND VELOCITY Ol ml/1 P04-P lOTAL-P UB - ol/l NO2-N UB -al/l NOi-N ut ■ Ol/l SI O4-SI VS - ot/l pH S C c 1 5TD 0000 0205 3158 2525 0027255 0000 14538 901 041 OBS STD STD 0000 0205 31577 2525 0010 0132 3175 2544 0020 0079 3192 2561 0025479 0023887 14538 901 041 0026 14509 844 0051 14490 801 084 005 001 002 041 OBS STD STD 0026 0058 32010 2569 0030 0057 3207 2574 0050 0049 3234 2596 0022525 0020524 14482 781 075 0074 14483 775 0117 14487 750 092 010 041 005 041 OBS STD 0061 0049 32357 2597 0075 0049 3265 2522 0018077 14487 749 084 0166 14495 725 099 Oil 054 008 041 OBS STD 0077 0049 32588 2624 0100 0065 3304 2651 0015257 14496 724 091 0207 14512 713 102 Oil 059 009 041 OBS STD STD 0102 0066 33060 2653 0125 0067 3308 2654 0150 0069 3312 2658 0014971 0014575 14513 712 094 0245 14517 706 0282 14523 702 113 012 088 009 041 OBS STD 0154 0070 33125 2658 0200 0080 3325 2658 0013575 14524 701 098 0353 14538 597 111 012 088 010 041 OBS 0206 0081 33276 2659 14540 695 094 107 Oil 098 010 041 OBS 0231 0084 33357 2675 14547 692 096 110 012 090 010 REFERENCE SHIP CODE LATITUDE 1/10 LONGITUDE '1/10 ii MARSDEN STATION TIME ORIGINATOR'S DEPTH j MAX. WAVE WEA- THER CODE CLOUD COOES NODC STATION NUMBER Ci»r CODE 10. NO. CRUISE NO. STATION NUMBER bo/.om1"o^" 10- r MO DAY HR.1/10 S'MPL'S DlR. HGri PES S A TYPE AM 31 549 EV e 029 2N 053561W 223 03 07 31 063 1965 LCE 9446 0316 03 00 o|x X4 7 8 0038 WATER WIND BARO- METER Imbi) AIR TEMP. •c COD NO. OBS. DEPTHS SPECIAL OBSERVATIONS COLOR CODE 1RANJ. DIR. OB DRY BULB WET GULB 17 S08 088 033 033 0 10 MESSENGr[ HR 1/10' CAST NO. CARD TYPE DEPTH 1ml T -C s •/.. SIGMA-T SPECIFIC VOLUME ANOMALY-IIO' SAD DYN. M. I 10= SOUND VELOCITY 0; ml/I P04-P -O-o'/l TOTAl-P ,.0 • ol/l NOj-N ua - ol/l NOj-N Wg - ol/l SI O^-SI OB - 01/1 pH C C STD 0000 0237 13158 2523 0027492 0000 1A552 886 063 OBS STD 0000 0237 31575 2523 0010 0094 3185 2554 0024518 14552 886 047 0026 14494 322 094 004 001 003 063 OBS STD 0010 0094 31848 2554 0020 0084 3211 2575 0022465 14494 822 067 0049 14494 705 092 006 028 005 053 OBS STD 0024 0079 32194 2583 0030 0065 3231 2593 0020843 14494 785 077 0071 14491 770 099 008 053 007 063 OBS STD 0044 0047 32500 2609 0050 0047 3253 2511 0019064 14487 746 087 0111 14488 744 101 010 067 008 053 OBS STD 0057 0047 32513 2518 0075 0049 3254 2620 0018230 14492 740 085 0158 14495 738 100 010 055 009 053 OBS STD 0089 0051 32568 2622 0100 0052 3257 2522 0018027 14499 735 089 0203 14501 734 101 010 064 009 053 OBS STD 0111 0054 32568 2622 0125 0057 3285 2637 0016654 14504 731 090 0246 14510 723 104 010 075 009 063 OBS STD 0128 0058 32882 2639 0150 0060 3290 2640 0016312 14511 722 090 0288 14516 720 101 010 082 009 063 OBS STD STD T0194 0064 32929 2543 0200 0069 3297 2646 0250 0134 3355 2588 0015810 0011835 1*525 716 092 0368 14529 713 0437 14575 577 010 008 05 3 OB 5 026: 0 159 33 7 71 27 0 + It*' 91 664 103 109 014 112 012 60 fiJFERENCE SHIP CODE LATITU 1 GITUDE ■ '1/10 ii MARSDEN STATION TIME ORIGINATOR'S DEPTH TO BOTTOM MAX. DEPTH OF S'MPL' WAVE WEA- THER CODE CLOUD CODES NODC STATION NUMBER Clit CODE ID. NO. DE LOh 1/10 CRUISE STATION NO. NUMBER 10" r MO DAY HR.1/10 0I«. HOT nt SEA l»PI AMI 31 549 EV i 0270N 1 05 4128W 223 04 07 31 088 1965 LCE 9447 |0201 02 15 0 X XI 2 2 0039 WATER WIND BARO- METER (mbil AIR TEMP. x VIS. CODE NO. OBS. DEPTHS SPECIAL OBSERVATIONS COLOR CODE ''t.T DIR. into o» Fotce DRt BULB WET BULB 15 S05 078 022 022 8 05 MtSSENCt j HR l/IO CAST NO. CARD TYPE DEPTH Iml T X s •/.. SIGMA-T SPECIFIC VOLUME ANOMALT-IlO' SAD DYN. M X 10' SOUND VELOCITY Ol ml/l P0<-P rOTAL-P va - «•/! NOj-N vs - ot/l NOj-N WQ - Ot/l SI04-Si Pt . ol/l PH STD 0000 0074 3158 2534 0026453 0000 1 14479 774 088 CBS STO STD STD 0000 0074 31581 2534 0010 0062 3190 2560 0020 0054 3216 2581 0030 0049 3236 2598 0023955 0021929 0020352 14479 77* ■ 0025 14480 765 0048 14482 757 0059 14484 751 088 OBS STD 0030 0049 32353 2598 0050 0051 3253 2511 0019084 1*484 751 079 099 0109 14490 743 008 051 008 088 OBS STD 0059 0052 32590 2615 0075 0053 3253 2619 0018324 14493 740 083 101 0155 14*95 737 007 058 008 088 OBS STD STD 0089 0053 32674 2523 0100 0055 3273 2627 0125 0059 3284 2636 0017571 0015751 1*500 734 090 102 0200 1*503 730 0243 1*511 72* 010 068 009 088 OBS STD 0148 0053 32931 2643 0150 0053 3294 2643 0015011 1*517 719 090 103 0284 14518 719 009 074 009 088 OBS 0171 0067 33012 2649 1*524 715 093 106 010 085 010 RefEBENCE SHIP CODE LATITU DE 1/10 LONGITUDE |y ■1/10 ~ MARSDEN SQUARE STATION TIME 1GMT> TEAR ORIGINATOR'S | DEPTH TO BOTTOM DEPTH OF S'MPL- WAVE OBSERVATIONS WEA- THER CODE CLOUD CODES NODC STATION NUMBER CIS' CODl ID. NO. CRUISE NO. STATION NUMBER 10* 1* MO DAY t- R.l/10 Dia. MGll Pf"| 5£* I. PI AM 31 549 EV t 027 ON 054252W 223 04 37 31 0 99 1965 LCE 9448 |0442 02 34 olxl XI 3 3 00*0 WATER WIND BARQ. METER imbl) AIR TEMP. TC V(S. CODE NO. OBS. DEPTHS SPECIAL OBSERVATIONS COLOR CODE TWNS, DIR. SPEED OK FO>CE DRY BULB WET BULB 14 S04 146 038 033 8 08 MfSSENOR HR l/IO CAST NO. CARD TYPE DEPTH Im) T -C S v.. SIGMA-T SPtClfIC VOLUME ANOMAK-HO' SAD DYN. M XIO! SOUND VELOCITY Ol ml/1 P04-P VO - ot/l TOTAl-P Mfl-oi/l N02-N US - at/I NO3-N pg - ol/l SI04-Si pg - ol/l pH S c STD 0000 0057 3261 2617 0018545 0000 14486 736 099 OBS STD STD 0000 ' 0057 '32506 2617 0010 0056 3249 2508 0020 0054 3238 2599 0019415 0020275 14486 735 087 104 0019 14485 743 0039 14485 749 010 064 009 099 OBS STD 0023 0054 32342 2595 0030 0054 3247 2505 0019561 14485 751 086 102 0059 1*487 744 008 069 009 099 OBS STD 0043 0054 32520 2518 0050 0055 3262 2518 0018411 1**92 737 089 103 0097 1*493 7*0 010 070 009 099 OBS STD 0065 0055 32622 2618 0075 0055 3262 2519 0018386 14^,95 743 089 10* 0143 14498 739 013 073 009 099 OBS STD STD 0087 0055 32627 2519 0100 0055 3252 2618 0125 0055 3252 2618 0018408 0018403 14499 735 089 104 0189 14502 735 0235 14505 737 010 075 009 099 OBS STD 0130 0055 32515 2618 0150 0055 3261 2517 0018474 14505 737 089 104 0281 1*510 737 010 075 009 099 OBS STD 0173 0055 32597 2616 0200 0054 3260 2515 0018572 1*513 736 090 125 0373 1*517 737 01* 054 010 099 OBS 0215 0054 32594 2615 1*520 737 089 105 on 072 009 REFERENCE SHIP CODE LATITU DE 1/10 LONGITUDE ' '1/10 n 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 Cr(Y ID. COOi NO. CRUISE NO. STAT NUW ON BER 10* r MO DAY H R.l/lO S Oii. MGI PER SEA TYPE AM 31 549 EV ( >031 2N 06 «268W 223 04 07 31 1 07 1965 LCE 9449 |( )284 03 16 0 X XI 3 3 3041 WATER WIND BARO- METER Imbil AIR TEMP. •c VIS. CODE NO. OBS. DEPTHS SPECIAL OBSERVATIONS COLOR CODE IRANS. DIR. SPEED OH FORCE DRY BULB WET BULB 14 504 078 039 033 8 08 MESSENCR TIME 0 HR 1/10 CAST NO. CARD TYPE DEPTH Iml T -C s •/.. SIGMA-I SPECIFIC VOLUME ANOMALT-X10' SAD DYN. M t 10' SOUND VELOCITY 03 ml/1 PO<-P ., . .1/1 lOTAL-P NOi-N UO ■ ol/l NOj-N pg - ol/l SI 04-si ,1 - ol/l pH s c c STD 0000 00 34 3194 12565 0023495 0000 1**66 773 107 OBS STD STD 0000 0034 31943 2555 0010 0037 3215 2582 0020 0040 3233 2595 0021849 0020563 1**66 773 081 103 0023 1**72 755 0044 14477 759 007 051 008 107 OBS STO STD 0025 0041 32403 2602 0030 0042 3244 2504 0050 0044 3257 2615 0019730 0018759 1**80 755 085 105 0054 1*482 752 0103 14488 739 008 063 008 107 OBS 0050 0044 32558 2515 14488 739 084 106 009 070 009 107 OBS STD 0074 0048 32559 2623 0075 0048 3267 2523 0017995 14495 735 090 104 0148 14495 735 007 073 009 107 OBS STD STD 0097 0047 32779 2531 0100 0047 3280 2533 0125 0048 3295 2645 0015995 0015855 1*500 725 090 104 0192 1*500 72* 0233 1*507 717 008 078 010 107 OBS STD 0147 0049 33039 2652 0150 0049 3304 2552 0015171 1*512 713 093 109 0272 1*513 713 009 082 010 107 OBS STD STD 0195 0049 33073 2655 0200 0049 3308 2555 0250 0050 3313 2559 0014859 0014477 1*521 714 094 105 0347 14522 714 0420 14531 711 008 089 010 10 7 OB S T025' f 0 D50 3: SI 33 2« 6 0 1* 532 711 093 1 05 009 09* 01 0 61 REFERENCE SHIP CODE LATITUDE I/IO tONGITUDE 'I/IO MARSDEN STATION Tl VIE ORIGINATOR'S DEPTH MAX. WAVE WEA- THER CODE CLOUD CODES NODC cool ID. NO. CRUISE NO. STATION NUMBER BOTTOM OF S'MPL'S NUMBER 10- r MO DAY HR.1/10 Olfc HG? PER S A TTPf AM 31 549 EV 6 038 ON 064288W 223 04 37 31 125 1965 LCE 9450 0243 02 00 0 X XI 8 4 0042 WATtR WIND BARQ. MEIER (mbi) AIR TEMP. ^ „,< NO. --d?pVhs 1 ::oLOR CODE IRANS. Iml OIR. iffiD fO«Cf DRY BULB WET BULB OBSERVATIONS 25 S07 088 051 056 8 08 MtSSfNCR IIM[ 0 HR 1/10 CAST NO. CARD TYPE DEPTH (ml I 'c s •/.. SIGMA-I SflClfIC VOlUMt ANOMALT-IIO' SAD DYN. M. X 10^ SOUND VELOCITY Oj ml/1 PO*-P V9 -ol/l lOTAl-r NOj-N ug - ol/l NO)-N MB • ol/l SI04-S> wg - ol/l s PH C STO 0000 0031 3246 2607 0019525 0000 14472 757 125 OBS STD STD 0000 ' 0031 '32451 2607 0010 0031 3252 2511 0020 0030 3255 2615 0019070 0018760 ' 14472 ' 757 '085 0019 14474 751 0038 14476 747 101 010 065 008 125 OBS STD 0024 0030 32556 2515 0030 0031 3257 2515 0018713 14477 745 087 0057 14478 745 103 009 069 009 125 OBS STD 0048 0032 32558 2515 0050 0033 3259 2617 0018536 14482 740 092 0094 14483 737 110 014 056 009 125 OBS STD STD 0074 0044 0075 0044 3279 2632 0100 0050 3296 2646 0017052 0015816 715 093 0139 14495 715 0180 14504 721 126 009 066 009 125 OBS STD STD 0100 0050 32957 2545 0125 0059 3308 2655 0150 0069 3319 2663 0014926 0014144 14504 721 090 0218 1*514 720 0255 14524 719 102 010 080 009 125 OBS STD T0152 0070 33193 2563 0200 0090 3330 2671 0013433 14525 719 096 0324 14543 705 117 Oil 081 Oil 125 OBS T0205 0092 33325 2573 14545 703 107 140 013 092 oil 125 OBS 023] 0102 33457 2683 14556 691 093 106 010 098 017 LONGITUDE ■i/lo STATION TIME ORIGINATOR'S OBSERVATIONS WEA- CLOUD THER CODES CODE NODC STATION NUMBER 60437N 064318W 223 04 07 31 148 1955 LCE 9451 0310 30 P 4 T X s v.. SAD DYN. M. K 10" SOUND VELOCITY Oiml/ L-P NO2-N ot/i ug - ot/l NOj-N wg - ol/l 1*8 148 148 148 148 148 148 148 148 STD OBS STD STD OBS STD OBS STO STD OBS OBS STO STO OBS STD OBS STD OBS STD OBS 0000 0000 0010 0020 0025 0030 0049 0050 0075 0075 0096 0100 0125 T0142 0150 70184 0200 T0236 0250 0288 0162 0162 0096 0052 0035 0039 0046 0045 0043 0043 0053 0054 0060 0064 0055 0085 0119 0159 0180 0183 3160 31501 3181 3201 32120 3220 32495 3250 3251 32514 32780 3279 3288 32979 3303 33317 3356 33916 3399 33997 2530 2530 2551 2559 2579 2585 2509 2609 2518 2518 2631 2632 2639 2647 2551 2572 2590 2715 2720 2720 0024819 0023053 0019287 0018397 0017109 0015452 0015337 0011651 0008849 0025 0050 0021547 0072 0113 0160 0204 0245 0286 0354 0405 14519 1*519 14494 14479 14474 14477 14487 14488 14492 14492 14502 1*503 1*511 14518 14520 14539 14550 14593 1*501 1*609 853 853 812 781 758 755 751 751 740 740 732 731 724 718 715 697 582 560 559 557 054 077 003 008 004 082 097 007 051 007 085 105 Oil 072 008 090 105 009 072 008 09* 103 009 070 009 092 102 010 083 009 095 104 010 155 010 103 113 Oil 115 Oil 105 129 013 115 013 62 SHIP CODE 31 5*9 EV LATITUOi 1/10 lONGITUDt ' '1/10 ORIGINATOR'S 223 04 07 31 160 1965 LCE 9452 SPEED EO»CE AIR TEMP. "C 039 06 03 21 1 2 WEA- THER CODE NODC STATION NUMBER 0044) CARD DEPTH (ml I t s •'■.. SOUND VELOCITY Ol ml/I NOj-N iig - oi/l SI 04-Si VB - oi/l 150 150 160 160 160 STD OBS STO STD STD OBS STD OBS STD STD OBS STO STO OBS STD STD OBS 0000 0000 0010 0020 0030 0033 0050 0060 0075 0100 0115 0125 0150 T0172 0200 0250 T0272 0108 0108 0068 0037 0014 0009 0001 -0002 -0002 -0002 -0002 -0000 0005 0010 0C25 0066 0090 3176 31758 3190 3201 3210 32126 3219 32246 3243 3267 32781 3279 3285 32930 3307 3342 33611 2546 2546 2550 2570 2578 2581 2586 2591 2505 2625 2634 2535 2539 2545 2556 2582 2596 0025283 0023985 0022991 0022194 0019585 0017744 0016829 0015389 0014803 0012373 0000 0025 0048 0071 0021441 0114 0155 0212 0256 0297 0375 0443 14497 14497 14483 14472 14454 14463 14453 14454 14459 14475 14480 14483 14490 14497 14511 14542 14559 836 835 811 792 778 775 771 768 757 742 735 734 730 725 717 697 585 062 088 005 021 005 082 099 008 054 007 088 106 010 128 009 091 105 009 063 009 093 108 010 082 010 100 102 010 088 on LATITUDE LONGITUDE )/io ■ 'I/ll ORIGINATOR'S Cn PES iEA 31 549 EV 50536N 054346W 223 04 07 31 173 1965 LCE 9453 0421 03 BARO- METER Imbil 0045 AIR TEMP. 'C 039 t -c SAD DVN. M. X 10= SOUND VELOCITY Ol ml/I NOj-N NOs-N 173 173 173 173 173 173 173 173 STD OBS STD STD OBS STD OBS STO STD OBS STD STD OBS STD OBS STD OBS STO STO OBS 0000 0000 0010 0020 0024 0030 0042 0050 0075 0075 0100 0125 T0131 0150 T0152 0200 T0210 0250 0300 T0324 0035 0035 0033 0032 0031 0022 0011 0018 0031 0031 0029 0023 0021 0012 0008 0005 0004 0043 0146 0217 3218 32183 3218 3217 32169 3235 32599 3250 3251 32607 3253 3265 32653 3272 32757 3296 33022 3335 3391 34237 2584 2584 2584 2583 2583 2598 2519 2518 2518 2518 2520 2522 2623 2628 2632 2648 2653 2678 2716 2737 0021667 0021702 0021737 0018388 0018390 0018213 0018023 0017412 0015534 0012767 0009210 0022 0043 0020321 0064 0103 0149 0195 0240 0284 0357 0438 0493 14470 14470 14471 14471 14472 14471 14472 144 76 14485 14486 14490 14491 14492 14492 14492 14500 14502 14531 14593 14533 789 789 790 791 791 773 748 748 745 746 742 739 738 743 744 732 728 707 572 651 080 097 009 049 007 078 101 009 045 007 090 107 009 071 009 091 104 009 070 009 091 104 009 070 009 090 113 009 070 010 101 104 010 090 010 102 114 008 125 012 63 REFERENCE SHIP CODE LATITUDE 1/10 LONGITUDE * '1/10 ii MARSOeN STATION T ME ORIGINATOR'S DEPTH MAX. WAVE WEA- THER CODE CLOUD CODES NODC coot ID. NO. CRUISE NO. STATION NUMBER TO BOTTOM OF S'MPL-S STATION NUMBER 10- r MO DAY HR.1/10 oil. KCI f(« S A lYPl AM 31 549 EV 50596N 054257W 223 04 37 31 190 1965 LCE 9454 0428 04 22 1 2 X4 X 9 0046 WATER WIND BARO- METER (mbil AIR TEMP. "c VIS, COD NO. OBS. DEPTHS SPECIAL OBSERVATIONS COLOR CODE TIMNS. OIR. 0« DRY euLG WET BULB 20 sio 091 022 022 0 10 MESSENCI [-irT "»■ 'NO. MR I/IO CARD TYPE DEPTH (ml I "c s •/.. SIGMA-T JfECIFIC VOlUMt ANOMAH-Xia' SAO DYN. M. SOUND VELOCITY Oa ml/I PO.-P lOTAL-P NOi-N US • ol/l NOj-N n - =1/1 SIO«-Si vB - oi/l PH STD 0000 0095 3220 2582 0021827 0000 14497 822 ' 190 DBS STO STD 0000 0095 32202 2582 0010 0053 3227 2590 0020 0020 3233 2597 0021087 0020458 14497 822 051 0021 14481 815 0042 14458 808 079 005 025 004 190 OBS STD STD 0028 0000 32375 2501 0030 -0003 3238 2502 0050 -0025 3245 2508 0019955 0019357 14461 803 074 0062 14450 803 0102 14454 794 094 007 038 008 190 OBS STD 0055 -0028 32453 2510 0075 -0030 3285 2542 0015179 14454 789 083 0145 14462 750 102 008 045 007 190 DBS STD 0083 -0031 32982 2551 0100 -0025 3317 2555 0013820 14464 737 097 0184 14472 711 102 Oil 071 009 190 OBS STD STD 0108 -0024 33245 2572 0125 -0018 3325 2572 0150 -0008 3333 2578 0013240 0012567 14475 703 095 0218 14481 705 0250 14491 709 107 010 079 010 190 OBS STD 0151 -0004 33400 2584 0200 0112 3388 2715 0009180 14495 711 098 0305 14561 574 110 008 077 010 , 190 OBS STD STO T0215 0143 34003 2724 0250 0154 3405 2728 0300 0178 3414 2732 0008125 0007718 14579 554 102 0348 14591 557 0387 14611 547 113 008 119 Oil 190 OBS T0302 0179 34145 2733 14512 547 097 102 008 099 Oil 190 OBS STD T0381 0240 34294 2740 0400 0251 3432 2741 0007022 14553 545 104 0461 14552 640 106 009 133 Oil 190 OBS 0428 0265 34355 2742 14573 531 no 119 Oil 127 012 REFERENCE SHIP CODE . MARSOEN STATION TIME ORIGINATOR'S DEPTH MAX. WAVE WEA- CLOUD NODC CIRT CODE 10. NO. LATITUDE 1/10 LONGITUDE * -1/10 Si YEAR CRUISE NO. STATION NUMBER TO BOTTOM OP S"MPL-S THER CODE STATION NUMBER 10* r MO DAY H R.l/10 DIP. [HCTl P(>| S K lYPI AM 31 549 EV 51029N 054312W 223 14 07 31 2 11 1965 LCE 9455 0557 05 20 H^l XI 3 6 0047 WATER WIND AIR TEMP. •c SPECIAL OBSERVATIONS COLOR CODE IRAMS. SPEtO DIR. OP FORCE METE (mbt R DRY BULB WET BULB COO OBS. DEPTHS 21 S08 081 061 050 8 10 MESStNGI CAST TIME t\a. HR 1/10 CARD TYPE DEPTH (ml T -C s •/.. SIGMA-T SPECIFIC VOIUME ANOMALT-IIO' SAD DYN. M. I 10' SOUND VELOCITY OS ml/I PO«-P ug - 01/1 lOIAl-P us - oi/l NOi-N UB - ol/l NOj-N pg - ol/l SIO«-Si wg - ol/l pH STD 0000 0191 3328 2662 0014239 0000 14555 746 211' OBS STD STD 0000 0191 33279 2562 0010 0189 3328 2563 0020 0183 3328 2563 0014220 0014180 14555 746 054 0014 14556 747 0028 14555 747 070 007 034 005 211 OBS STD STD 0025 0178 33287 2564 0030 0171 3330 2565 0050 0143 3335 2571 0013971 0013415 14554 748 050 0043 14551 749 0070 14543 751 057 007 033 004 211 OBS STD 0051 0142 33348 2571 0075 0126 3337 2574 0013125 14543 751 056 0103 14540 759 082 008 037 005 211 OBS STD 0077 0123 33373 2575 0100 0078 3343 2582 0012375 14539 760 063 0135 14523 738 079 009 039 005 211 OBS STD STD 0102 0075 33435 2582 0125 0087 3370 2703 0150 0127 3397 2722 0010379 0008592 14523 736 052 0153 14535 720 0187 14551 696 078 008 045 005 211 OBS STD 0155 0138 34016 2725 0200 0302 3441 2743 0005687 14557 591 094 0225 14552 529 106 014 107 008 211 OBS STD STD T0206 0317 34442 2745 0250 0320 3447 2747 0300 0323 3449 2748 0006435 0006350 14660 623 098 0258 14669 604 0290 14578 582 104 009 164 010 211 OBS STD T0306 0323 34493 2748 0400 0326 3450 2748 0006395 14580 579 103 0354 14695 620 112 008 118 Oil 211 OBS STD T0408 0325 34498 2748 0500 0329 3450 2748 0006485 14698 522 105 0418 14714 525 118 009 131 012 21 1 08 S T054< ) 0 331 3* 5 07 27 4 9 14- r23 527 64 - SHIP CODE EV LATITUDE LONGITUDE 1/10 ' 1/10 61077N 064461W 223 lA 07 31 229 1965 LCE 9*56 snto fO«CI OftlGINATOR'S lARO- METER AIR TEMP. "C 09 03 19 iCIlKtl StA WEA- THER CODE X4 X l9 NODC STATION NUMBER DEPTH ( T "C S •''.. SIGM SOUND vaOCITY O? ml/l NO3-N wg - oi/l SI 04-Si wg ■ el/l 229 229 229 229 229 229 229 229 229 STD OBS STD STD OBS STD OBS STD OBS STD OBS STD OBS STD STD OBS STD STD OBS OBS 0000 0000 0010 0020 0022 0030 0041 0050 0062 0075 0082 0100 0122 0125 0150 T0168 0200 0250 T0250 0280 0162 0162 01*1 0121 0117 0099 0084 0086 0089 0130 0149 0184 0223 0228 0267 0289 0311 0328 0328 0329 3331 33306 3332 3333 33337 3336 33389 3330 33408 3345 33503 3386 34168 3419 3431 34381 3444 3448 34482 34480 2667 2667 2569 2671 2672 2675 2678 2678 2680 2680 2683 2709 2731 2732 2739 2742 2745 2747 2747 2747 0013594 0013393 0013032 0012728 0012544 0009814 0007667 0007098 0006544 0006425 0014 0027 0040 0066 0098 0126 0148 0166 0200 0233 14543 145*3 14535 14528 14527 14520 14516 14518 14522 14543 14553 14576 14601 14604 14627 1*6*1 14656 14672 1*672 1*678 745 745 745 74* 7*4 74 5 746 747 74 8 738 730 691 657 655 644 637 533 626 626 622 058 076 007 043 005 064 084 008 045 006 057 118 Oil 055 006 055 085 010 054 005 05* 075 012 05* 005 101 119 012 128 010 103 110 010 125 010 099 104 010 020 134 139 Oil 025 SHIP CODE LONGITUDE STATION TIME ORIGINATOR'S Gil rER SEA WEA. THER CODE 61122N 064504W 223 14 08 01 014 1965 LCE 9457 0311 03 20 1 X XI 3 |7 SPEED 01 fORCE BARO- METER [mbil 085 AIR TEMP. "C 022 NO. OBS. DEPTHS 09 DEPTH Iml T t s ■/.. 02 ml/I 014 014 014 014 014 014 014 014 014 STD OBS STD STD OBS STD STD OBS STD OBS STD OBS STD STD OBS OBS STD OBS STD OBS 0000 0000 0010 0020 0025 0030 0050 0052 0075 0078 0100 0104 0125 0150 0155 0192 0200 T0223 0250 T0286 0135 0135 0108 0089 0080 0079 0073 0072 0068 0067 0083 0085 0088 0092 0093 0127 0163 02*1 02*9 0259 3315 33154 3321 3325 33272 3327 3328 33278 3335 33362 3355 33575 336 1 3368 33702 33864 3400 34278 3430 34332 2656 2656 2652 2657 2669 2669 2670 2670 2676 2677 2691 2693 2696 2701 2703 2714 2722 2738 2739 2741 001*816 001*226 0013811 0013578 0013505 0012925 0011*93 0011070 001056* 0000 0015 0029 00*2 0069 0102 0133 0161 0188 0008631 0236 0007065 0275 1*528 1*528 1*519 1*512 1*510 1*510 1*511 1*510 1*513 1*51* 1*527 1*529 1*53* 1*5*1 1*5*3 14565 14586 14527 14536 14546 752 752 7*5 7*0 739 740 7*5 7*5 732 730 718 715 599 686 684 578 665 637 537 536 051 075 007 029 020 080 095 010 0*8 007 075 093 009 054 008 070 078 010 067 008 084 098 010 082 010 091 136 105 153 010 010 092 098 009 010 099 107 008 129 010 103 112 008 128 Oil 65 REFERENCE SHIP CODE LATITUDE 1/10 LONGITUDE * -1/10 ii MARSOEN STATION TIME ORIGINATOR'S DEPTH MAX. DEPTH OF S'MPL'S WAVE WEA- THER CODE CLOUD CODES NODC CT«Y CODE 10. NO. YEAR CRUISE NO. STATION NUMBER TO BOTTOM STATION NUMBER 10' r MO DAY HR.1/10 DIR. MGT PER S A TYPE AM 31 549 EV 6 117 4N 064464W 223 14 38 01 036 1965 LCE 9458 0265 02 20 2 2 XI 3 5 0050 WATER WIND ( BARO. METER (mbi) AIR TEMP. ^ ""o?pV„s SPECIAL OBSERVATIONS COLOR CODE '""'■ D1R. iPEt OR FORC DRY BULB WET BULB 20 S09 081 039 039 7 08 MESSfNCR IIMI ( HR 1/10 CAST NO. CARD TYPE DEPTH Iml T -C s ■/.. SIGMA-T l«ClflC VOLUME *NOM*l.»-YI0' SAD DYN. M. I 10' SOUND VELOCITY 03 ml/1 PO4-P WB-ol/l IOTAl_P „9 - ol/l NO2-N US - 01/1 NOj-N US - 01/1 S10<-Si ue • 01/1 PH S C c STD 0000 0003 3321 2668 0013660 0000 14469 745 036 OBS STD STD 0000 0003 33212 2668 0010 0002 3322 2669 0020 0001 3322 2670 ' 14469 ' 745 085 0013608 0014 14471 745 0013556 0027 14472 745 102 012 065 008 0 36 OBS STD 0025 0001 33227 2670 0030 0001 3323 2670 14473 745 087 0013528 0041 14474 743 098 012 063 008 036 OBS STD 0048 0001 33228 2670 0050 0001 3322 2669 14477 741 085 0013577 0068 14477 742 098 Oil 063 008 036 OBS STD 0071 0001 33179 2666 0075 0002 3316 2664 14480 745 092 0014032 0102 14481 744 101 013 062 009 0 36 OBS STD STD 0095 0003 33116 2661 0100 0001 3313 2662 0125 -0008 3321 2669 14484 740 087 0014249 0138 14484 740 0013589 0173 14485 740 096 Oil 062 008 0 36 OBS STD 0141 -0014 33250 2672 0150 -0019 3326 2673 14485 740 089 0013149 0206 14485 739 104 Oil 064 009 036 OBS STD T0186 -0030 33314 2678 0200 -0029 3333 2679 14486 735 082 0012553 0270 14489 733 096 013 069 009 036 OBS 023e -0016 33378 2683 14502 725 093 108 015 068 010 REFERENCE SHIP CODE LATITUDE 1/10 LONGITUDE ' '1/10 ii MAHSDEN STAT ON T ME ORIGINATOR'S DEPTH MAX. WAVE WEA- THER CODE CLOUD CODES ^ODC CIPY CODE ID. NO. CRUISE NO. STATION NUMBER TO BOTTOM OF S'MPL'S STATION NUMBER 10- r MO DAY H R.1/10 DIR- HOT PEP SEA ITPl AM 31 549 EV 60437N 066051W 223 06 08 01 1 00 1965 LCE 9459 0540 06 20 3 X XI 3 7 0051 WATER WIND BARO- METER (mbtl AIR TEMP. 'C VIS COD NO. OBS. DEPTHS SPECIAL OBSERVATIONS COLOR CODE '»" OIR. SPIED OP FORCE DRY BULB WET BULB 16 SIO 075 050 044 10 MES5ENCR CAST TIME 0 '-^0 HR 1/10 CARD TYPE DEPTH 1ml T -C s •/.. SIGMA-T SPECIFIC VOLUME ANOMALl-XIO' SAD DYN. M. < 10= SOUND VELOCITY 02 ml/l PO,-P lOTAL-P NO3-N uB - ai/l NOa-N PB - 01/1 S104-Si UO - 01/1 pH S C C STD 0000 0203 3149 2519 0027887 0000 145 36 867 ' 100 OBS STD STD 0000 0203 31492 2519 0010 0125 3208 2571 0020 0061 3255 2612 0022926 0018990 14536 867 052 0025 14511 852 0046 14490 832 077 004 004 003 100 OBS STD STD 0025 0033 32742 2629 0030 0006 3286 2640 0050 -0057 3323 2673 0016353 0013252 14481 819 060 0064 14471 796 0094 14450 733 085 009 024 004 100 OBS STD 0050 -0057 33230 2673 0075 -0040 3341 2686 0011966 14450 733 084 0125 14455 718 104 010 058 009 100 OBS STD 0075 -0040 33406 2686 0100 -0043 3346 2690 0011548 14465 718 095 0155 14458 707 110 012 074 009 100 OBS STD 0100 -0043 33458 2690 0125 -0025 3357 2699 0010766 14468 707 097 0182 14482 587 114 Oil 075 010 100 OBS STO STD 0141 -0014 33532 2703 0150 -0009 3365 2704 0200 0023 3374 2710 0010226 0009707 14491 678 103 0209 14495 676 0259 14519 565 112 012 096 012 100 OBS STD STD 0200 0023 33739 2710 0250 0057 3383 2715 0300 0098 3395 2722 0009210 0008583 14519 665 105 0305 14544 562 0350 14572 655 118 Oil 105 013 100 OBS STD T0300 0098 33948 2722 0400 0201 3423 2738 0007264 14572 555 104 0430 14639 532 110 012 119 012 100 DBS STD STD T0402 0202 34236 2738 0500 0216 3426 2739 0600 0231 3429 2740 0007181 0007141 14539 631 103 0502 14562 627 0573 14686 523 109 004 129 012 10 0 OB 5 T0602 0, '31 34 2 94 27 4 ) 146 86 523 115 121 002 138 01; 66 KEfERENCE SHIP CODE LONGITUDE "1/10 B MARSDEN STATION TIME r ORIGINATOR'S MA . WAVE WEA- THER CODE CLOUD COOES r— CTST CODt ID. NO. 1/10 CRUISE NO. STATION NUMBER TO BOTTOM Of S-MPL-S OBSERVATIONS STATION NUMBER r DAY M R.i/10 DHL NCT PtR S£* ITf AM 31 549 EV 50378N 065511W 223 05 08 01 lU 1965 LCE 9460 0338 03 13 2 2 XI 3 6 0052 WATER WIND AIR TEMP. X. MO COLOR CODE TRANS. In.) DIR. 5«tO OR FORCf METER (mb«l DRY BULB WET BULB COD. OBS. '-°°' DEPTHS OBSERVATIONS 13 S08 064 8 09 1 IIMf 0 ^p HR 1/10 CARD TYPE DEPTH Iml T "C S •''.. SIGMA-T S«CI»IC VOlUME ANOMAIT-XIQ' S Ao DYN. M. X 10^ SOUND VELOCm 0? ml/I PO4-P i.g • Bi/I lOTAL-P «g - Bl/I NOs-N US - ol/l NOj-N tig - oi/l SIO,-Si iig - ol/l pM C c STD 0000 0102 3208 2572 0022826 0000 14499 876 - 114 OBS 0000 0102 32076 2572 ' 14499 ' 825 ' 064 089 006 026 005 114 OBS 0008 0088 32088 2574 14494 770 064 079 005 028 STD 0010 0079 3213 2578 0022288 0023 14491 780 STD 0020 0031 3237 2599 0020206 0044 14474 806 114 OBS 0020 0031 32371 2599 14474 806 073 0 96 006 039 007 STD 0030 -0033 3274 2632 0017103 0062 14451 759 114 OBS 0040 -0074 32978 2653 14437 745 094 106 008 064 010 STD 0050 -0081 3301 2656 0014847 0094 14436 740 114 OBS 0051 -0086 33057 2660 14435 735 103 123 007 071 012 STD 0075 -0090 3312 2665 0013962 0130 14438 731 114 OBS 0081 -0091 33141 2567 14438 730 101 113 008 077 010 0100 0011 3319 2665 0013840 0165 14489 727 114 OBS T0120 0095 33238 2555 14531 723 108 131 009 077 Oil STD 0125 0093 3324 2666 0013905 0200 14531 722 STD 0150 0080 3327 2669 0013599 0234 14530 718 114 OBS 0155 33307 7I4 101 110 008 084 Oil 0200 0054 3343 2683 0012230 0299 14529 702 STD 0250 0029 3369 2706 0010104 0355 14529 678 114 OBS T0253 0027 33713 2708 14529 576 109 112 010 102 013 EV LATITUDE * 1/10 60308N 223 132 132 132 132 132 132 132 132 132 132 STD OBS STD STD OBS STD OBS STD OBS STD OBS STD STD OBS STD OBS STD STD OBS OBS STD OBS DEPTH Iml 0000 0000 0010 0020 0024 0030 0045 0050 0069 0075 0092 0100 0125 0138 0150 T0185 0200 0250 T0256 T0275 0300 T0380 05 08 T t 0158 0158 0054 -0020 -0041 -0049 -0068 -0072 -0084 -0083 -0081 -0079 -0072 -0058 -0050 -0002 0023 0078 0082 0089 0096 0109 132 SPEtO OR FOPCE S12 3145 31448 3210 3258 32729 3285 33074 3309 33180 3324 33372 3339 3344 33458 3350 33611 3370 3389 33907 33930 3395 33993 ORIGINATOR'S LCE BARO- METER Imbll 2518 2518 2575 2519 2631 2642 2650 2562 2570 2574 2685 2586 2590 2592 2694 2701 2707 2719 2720 2721 2723 2725 AIR TEMP. .C 051 0027934 0022389 0018384 0015199 0014267 0013067 0011924 0011557 0010003 0008887 DEPTH TO BOTTOM 0421 0000 0025 0045 0063 0093 0127 0159 0188 WEA- THER CODE SOUND VELOCITY 0011179 0215 0269 0317 0008554 0350 14515 14515 14479 14453 14446 14445 14442 14441 14440 14442 14448 14451 14459 14463 14474 14503 14518 14554 14557 14564 14572 14591 0053 O3 ml/l 865 865 827 797 787 777 754 752 735 724 702 701 598 696 694 685 681 666 564 658 553 553 SIO«-Si no - ol/l 561 082 007 010 004 073 088 008 037 005 084 099 009 045 007 087 100 009 053 008 104 133 Oil 082 Oil 104 112 012 092 012 102 107 012 092 012 102 113 oil 106 012 095 109 009 104 010 100 112 008 109 012 67 LATITUDE 1/10 LONGITUDE 0651S8W OAV HR.1/10 223 05 08 01 148 1965 LCE 9*62 12 FORCt S12 ORIGINATOR'S aABQ. METER imbil 037 083 0251 02 CI] rER SEA XI 3 16 NODC STATION NUMBER 0054 DEPTH (ml SPECIFIC VOLUME Ol ml/1 lAB IAS 148 148 148 148 STD OBS STD STD OBS STD STD OBS STD OBS STD OBS STD STD OBS STD OBS 0000 0000 0010 0020 0025 0030 0050 0051 0075 0076 0100 0101 0125 0150 T0151 0200 T0227 00 5 5 0055 0024 -0007 -0023 -0048 -0105 -0106 -0071 -0070 -0051 -0050 -0032 -0015 -0014 00 16 0031 3155 31554 3162 3175 31837 3200 3256 32584 3304 33053 3312 33125 3325 3336 33365 3355 33639 2533 2533 2539 2551 2559 2573 2620 2622 2658 2659 2663 2664 2673 2681 2682 2695 2701 0026566 0025915 0024785 0022710 0018217 0014641 0014095 0013174 0012406 0000 0025 0052 0075 0115 0157 0193 0227 0259 0011105 0318 14470 14470 14459 14448 14443 14434 14419 14419 14445 14446 14450 14461 14475 14488 14489 14513 14526 865 86 5 857 850 845 822 752 750 726 725 722 722 714 696 595 529 576 059 081 005 Oil 004 077 098 008 027 005 092 124 Oil 057 009 102 108 012 076 Oil 092 107 012 078 010 105 110 013 090 Oil 103 111 Oil 099 012 LATITUDE 1/10 LONGITUDE sj STATION TIME ORIGINAIOII'S OBSEHVATIONS 31 549 EV 60194N 223 05 08 01 165 1965 LCE 9463 02 00 XI 3 |3 0055 SPEED fOPCE SIO 037 128 NO. OBS. DEPTHS 06 TYPE S •/.. NOa-N PS - ol/l SI 0*-Si 155 155 165 165 165 165 STD OBS STD STD OBS STD STD OBS STD OBS STD STD OBS STD OBS 0000 0000 0010 0020 0025 0030 0050 0050 0075 0078 0100 0125 T0125 0150 T0179 0083 0083 0051 0022 0008 -0008 -0054 -0054 -0052 -0063 -0026 0002 0003 0006 0010 3010 30101 3038 3070 30886 3116 3198 31978 3230 32347 3290 3332 33329 3337 33425 2415 2415 2439 2466 2481 2504 2571 2571 2598 2602 2645 2677 2578 2581 2685 0035515 0032938 0029291 0022844 0015881 0012800 0000 0037 0071 0102 0154 0020335 0208 0253 0289 0012418 0321 14463 14453 14454 14447 14444 14441 14434 14434 14439 14440 14458 14491 14492 14498 14505 84 8 84 8 867 885 895 873 803 803 760 755 726 704 691 690 064 095 005 007 005 059 104 003 001 003 073 112 008 098 005 087 105 010 047 008 101 115 012 100 Oil 078 098 007 035 005 68 REFERENCE SHIP COOE LONGITUOE '1/10 MASSDEN STATION Tl ME ORIGINATOR'S | DEPTH MAX, WAVE WEA- THER CODE CLOUD CODES NODC CItt CODE 10. NO. LATITUDE 1/10 CRUISE NO. STAT HUM ON OP S'MPL'S STATION NUMBER 10* 1" MO DAY HR.l/10 DUL HOT P(« S » TTPI AM 31 549 EV 61357N 05000 W 223 10 08 02 201 1965 LCE 9464 1719 13 20 5 3 X2 5 e 0056 WAUR WIND BARO- METER (mbll AIR TEMP. •c VIS. COD NO. OBS. DEPTHS SPECIAL OBSERVATIONS COLOR CODE TtANS. DIR. %rHO Of fOICI ORT BULB WET BULB 28 SIO 078 057 061 8 12 »■"■"=' lc«i t,»l . NO. HR V10 CARD TTPE DEPTH Iml T -C s •/., SIGMA-T Irtcific VOIUWE ANOMALT-X10' SAO DVN. M. X 10' SOUND VELOCITT 03 ml/I P04-P KB - Ol/I roiAi-p KB - ot/l NOj-N .1 - Bl/I NOj-N i>g - oi/l SI 04-S. ue - oi/i PH S c c STD 0000 0676 I33A4 2624 0017854 0000 14761 576 1 201 ■ OBS 0000 0676 33437 2624 14761 575 019 037 002 000 001 STD 0010 0659 3356 2635 0015735 0017 14757 593 STD 0020 0623 3371 2553 0015183 0033 14745 703 201 OBS 0028 0581 33839 2568 14732 706 028 049 004 010 002 STD 0030 0554 3389 2675 0013032 0047 14722 705 STD 0050 0371 3430 2728 0008046 0068 14555 689 201 OBS 0055 0349 34383 2737 1464fl 683 088 098 032 092 005 STD 0075 0393 3463 2752 0005801 0085 14673 549 201 OBS 0083 0405 346<'3 2756 14580 540 101 109 045 096 008 STD 0100 0415 3474 2758 0005232 0100 14688 533 201 OBS 0110 0423 34761 2759 14693 630 100 113 003 142 007 STD 0125 0440 3478 2759 0006209 0113 14703 630 STD 0150 0452 3481 2759 0005249 0126 14717 629 201 OBS 0156 0472 34823 2759 14724 629 105 115 002 153 009 STD 0200 0479 3485 2760 0005195 0152 14732 635 201 OBS T0224 0483 34873 2752 14738 638 104 109 001 152 009 STD 0250 0480 3488 2752 0005077 0177 14741 636 STD 0300 0474 3488 2763 0005043 0203 14747 634 STD 0400 0462 3488 2765 0004979 0253 14759 529 201 OBS T0443 0456 34886 2755 14764 527 107 113 003 149 010 STD 0500 0448 3489 2757 0004873 0302 14770 525 STD 0600 0433 3490 2769 0004729 0350 14780 523 201 OBS T0662 0425 34905 2771 14787 621 111 118 000 164 010 STD 0700 0420 3491 2771 0004640 0397 14791 520 STD 0800 0407 3490 2772 0004599 0443 14803 518 201 OBS T0879 0397 34902 2773 14812 615 107 117 001 164 Oil STD 0900 0394 3490 2773 0004561 0489 14814 517 STD 1000 0383 3490 2775 0004520 0534 14825 523 STD 1100 0374 3490 2775 0004499 0579 14839 629 201 OBS T1117 0373 34899 2776 14841 630 112 117 003 134 Oil STD 1200 0357 3490 2775 0004522 0625 14853 529 STD 1300 0363 3490 2775 0004570 0570 14858 524 20 I OBS T132C 0362 3^894 2776 14871 523 113 121 002 166 Oil REFERENCE SHIP CODE LATITUDE 1/10 LONGITUDE ■1/10 i| MAItSDEN STATION Tl WE ORIGINATOR'S DEPTH ■ V VAVE WEA- THER coot CLOUD CODES ^ODC CUT CODE ID. NO. YEAR CRUISE NO. STATION NUMBER TO BOTTOM OF S'MPL'S STATION NUMBER 10- r MO DAY HR.l/10 DIB- iMCTlfERl S(» IT« AW 31 549 EV 5 137 N 050383W 223 10 D8 02 228 1965 LCE 9455 0538 05 13 |3M X2 7 8 0057 WATER WIND BARO. METER tmb»l AIR TEMP. r -^'JL SPECIAL OBSERVATIONS COLOR CODE TMiNt DIR. into FO»Cf DRY BULB WET BULB 24 508 766 072 061 8 10 wESiENGI 1 TIME or HR 1/10 CAST NO. CARD TYPE DEPTH Iml T X S v.. SIGMA-T SPECIFIC VOLUME AHOMALT-IIO' SAD DYN. M. SOUND VELOCITY Ol ml/I PO4-P roTAi-f VB-O./I NOj-N ut - ot/l NOj-N Hi ■ Ol/I SI Ot-Si KB - Ol/I pH S c c STD 0000 0523 3324 2628 0017530 0000 14696 707 228 OBS 0000 0523 33239 2628 14596 707 STD 0010 0333 3334 2655 0014903 0015 14519 743 STD 0020 0178 3342 2575 0013083 0030 14555 755 228 OBS 0025 0102 33464 2583 14522 774 STD 0030 0055 3347 2587 0011945 0043 14502 773 STD 0050 -0075 3355 2699 0010736 0055 14446 755 228 OBS 0052 -0079 33565 2700 14445 752 STD 0075 0021 3378 2713 0009400 0091 14498 700 228 OBS 0078 0031 33803 2715 14503 694 STD 0100 0081 3394 2723 0008519 0113 14532 662 228 OBS 0104 0097 33975 2725 14540 657 STD 0125 0297 3434 2738 0007118 0133 14635 537 STD 0150 0453 3463 2745 0005499 0150 14710 621 228 OBS 0155 0474 34558 2746 14721 519 STD 0200 0490 3474 2750 0006141 0181 14736 515 228 OBS T0204 0491 34744 2750 14737 615 STD 0250 0500 3480 2754 0005865 0211 14749 612 STD 0300 0510 3484 2755 0005742 0240 14751 608 228 OBS T0305 0511 34844 2755 14753 508 STD 0400 0481 3487 2762 0005297 0295 14757 610 228 OBS T0409 0476 34871 2752 14766 610 STD 0500 0413 3483 2755 0004921 0346 14754 591 22 B OB 5 T053: 0 J83 3* 7 94 27 6 3 14^ 47 580 69 REFERENCE SHIP GITUOE ii MARSOEN STATION T ME 1 ORIGINATOR'S DEPTH MAX. DEPTH OF WAVE WEA- THER CLOUD CODES NODC Cl«* ID. CRUISE STATION TO BOTTOM STATION COD( 1/10 ■1/10 10- r MO DAV HR.1/10 S-MPL- DIR. HOT PER SE* CODE TYPE AM 31 549 EV 61372N 051164W 223 11 38 03 014 1965 LCE 9466 0576 05 24 3 2 XI 3 6 0058 WATfR WIND AIR TEMP. ■c NO. COIOR IHANS. *n»° METER DRY WET coo iml FORCE Imb 1 BULB DEPTHS 26 SIO 122 061 050 8 11 MtSSENCR[rAST ""' • NO. HR 1/10 CARD irPE DEPTH Iml T -C s v.. SIGMA-T SPECIFIC VOLUME ANOMAIY-XIO' 5 A 0 DTN. M. X id' SOUND VELOCITY Oj ml/l PO4-P roTAi-p Vfl - ol/l NOi-N wg - al/l NOj-N UB - Qt/I SIO*-Si MB • ol/l PH S c c STD 0000 I 0528 3326 2629 0017405 0000 1*699 706 014 ■ OBS 0000 0528 33263 2629 14699 706 018 031 003 000 001 STD 0010 0516 3326 2630 0017314 0017 1*695 717 014 OBS 0010 0516 33259 2630 14695 717 039 075 000 000 001 STD 0020 0488 3328 2635 0016866 0034 14686 723 014 OBS 0025 0460 33291 2639 14675 728 018 0 36 001 002 002 STD 0030 0390 3332 2648 0015589 0051 14647 737 STD 0050 0164 3345 2676 0012766 0079 14554 771 014 OBS 0051 0155 33460 2679 14550 773 032 051 006 021 001 STD 0075 0001 3364 2703 0010367 0108 14487 735 014 OBS 0076 -0001 33652 2704 14486 733 073 087 015 075 004 STD 0100 0055 3382 2715 0009278 0133 14518 698 014 OBS 0102 0061 33832 2715 14521 695 085 0 96 021 103 006 STD 0125 0181 3407 2726 0008211 0154 14582 667 STD 0150 0288 3429 2735 0007432 0174 14636 644 014 OBS 0152 0296 34304 2736 14640 6*2 092 099 016 132 008 STD 0200 0430 3460 2746 0006528 0209 14709 620 014 OBS T0203 0436 34612 2746 1*712 619 094 102 000 1*2 008 STD 0250 0464 3474 2753 0005899 0240 14733 514 STD 0300 0493 3482 2756 0005692 0269 1*754 609 014 OBS T0302 0494 34822 2756 1*755 609 103 112 000 151 009 STD 0400 0433 3483 2764 0005068 0323 14746 587 014 OBS T0406 0431 34827 2764 147*6 586 STD 0500 0428 3482 2764 0005130 0374 1*750 576 014 OBS 0566 0425 34821 2764 14770 575 REFERENCE SHIP CODE LATITUDE 1/10 LONGITUDE ■i/io ii MARSDEN STATION TIME ORIGINATOR'S DEPTH MAX. WAVE WEA- THER CODE CLOUD CODES ^ODC CTRY CODE ID. NO. CRUISE NO. STATION NUMBER TO BOTTOM OF S'MPL-S STATION NUMBER ID* r MO DAY HR.1/10 DIR. HGI PER S A lYPt AM 31 549 EV 6 137 5N 061543W 223 11 08 03 040 1965 LCE 9467 0588 05 17 7 2 XI 0 2 0059 WATER WIND BARD' METER (mbil AIR TEMP. ■c VIS. COD NO. OBS. DEPTHS SPECIAL OBSERVATIONS COLOR CODE TRANS. DIR. SPEtO o« FOUCt DRY BULB WET BULB 25 S08 112 044 044 8 09 MESSENGR TIME c HR 1/10 CAST NO. CARD TYPE DEPTH Iml T -C s ■/.. S(GMA-T SPECIFIC VOLUME ANOM*L»-I10' SAD DYN. M. X 10' SOUND VELOCITY Ol T-l/l PO4-P VB -o'/l lOTAL-P j,B ■ or/I NOb-N ug - al/l NO3-N PB - ol/l SIO*-Si pg - at/I pH 5 C C STD 0000 0368 3332 2650 0015377 0000 14532 7*5 ' 040 OBS STD STD 0000 0368 33318 2550 0010 0341 3335 2655 0014899 0020 0306 3338 2661 001*359 14532 ' 745 030 0015 14623 7*7 0030 1*610 748 049 004 010 002 040 OBS STD STD 0025 0286 33398 2664 0030 0248 3351 2576 0012922 0050 0158 3385 2711 0009676 14602 749 038 0043 14588 737 0065 14557 700 054 006 020 003 040 OBS 0050 0158 33852 2711 14557 700 071 083 027 070 006 040 OBS STD STD 0074 0186 34018 2722 0075 0187 3402 2722 0008619 OlOO 0221 3413 2728 0008053 1*575 679 080 0089 1*576 679 OHO 1*596 555 088 029 090 006 040 OBS STD T0103 0225 34147 2729 0125 0325 3438 2739 0007071 1*599 663 090 0129 1*549 641 102 028 112 007 040 OBS STD 0148 0388 34545 2745 0150 0388 3455 2745 0006421 14682 527 097 0145 14582 627 110 001 132 008 040 OBS STD STD STD T0198 0382 34599 2751 0200 0383 3460 2751 0006040 0250 0403 3470 2757 0005543 0300 0417 3477 2761 0005217 14688 525 099 0177 14589 624 0206 14707 613 0232 14722 504 103 001 144 009 040 OBS STD STD T0386 0432 34837 2764 0400 0432 3483 2764 0004999 0500 0428 3481 2763 0005206 1*7*3 595 0284 1*746 595 0335 14760 597 04 0 OB 5 0517 0^ *27 34 8 10 27 6 5 1*7 63 597 70 MfERENCE SHIP CODE- LATITUDE 1/10 LONGITUDE ■ "1/10 n MARSDEN STATION TIME ORIGINATOR'S DEPTH MAX, DEPTH OF S'MPL' WAVE WEA- THER CODE CLOUD CODES NOOC COOf ID. NO. CRUISE NO. STATION NUMBER TO BOTTOM STATION NUMBER 10* 1* MO DAY HR.V10 01". HGI PER SEA UPl *MT 31 549 EV 51377N 0523B4W 223 12 08 03 070 1965 LCE 9*68 0594 05 13 «v XI 3 1 0060 WATER WIND BARO- METER (mbit AIR TEMP. ■c COD NO. OBS. DEPTHS SPECIAL OBSERVATIONS COLOR CODE TRAM DIR. OR FORCE DRY BULB WET BULB 23 S04 125 044 039 8 11 xlSiiMC.lcASt "**' \ NO. HR 1/10 CARD TYPE DEPTH tml T X s •/.. SIGMA-T JPtClHC VOLUMl ANOMALT-HO' SAO OVN. M. X 10> SOUND VELOCITY 0? ml/1 vg • ol/l TOTAL-P vg • 01/1 NOl-N ws - ot/l NOj-N kis - ot/l 5iO,-Si ,1 - .1/1 PH S c c STD 0000 039* 3331 2647 0015702 0000 14643 749 070 OBS STD 0000 0394 33307 2647 0010 0394 3330 2647 0015747 14643 ' 749 ' 027 0016 14645 754 049 003 005 003 070 OBS STD 0010 0394 33302 2547 0020 0377 3331 2549 0015534 14645 754 030 0031 14639 754 049 004 005 003 070 OBS STD 0023 0368 33321 2551 0030 0331 3334 2556 0014898 14636 754 027 0047 14622 752 046 004 005 003 070 OBS STD 0045 0257 33403 2567 0050 0230 3345 2573 0013246 14593 745 034 0075 14583 742 045 004 014 003 070 OBS STD 0067 0153 33593 2690 0075 0147 3355 2696 0011063 14558 729 055 0105 14553 721 072 013 041 004 070 OBS STD STD 0090 0133 33782 2707 0100 0138 3387 2713 0125 0179 3411 2730 0009415 0007894 14551 705 059 0131 14555 592 0152 14582 663 090 020 064 005 070 OBS STD 0134 0204 34192 2734 0150 0293 3439 2743 0006723 14595 655 091 0171 14540 646 102 034 105 008 070 OBS STD STD T0179 0413 34650 2752 0200 0427 3468 2752 0250 0449 3475 2756 0005897 0005663 14699 632 093 0202 14709 529 0231 14727 621 101 000 130 007 070 OBS STD T0270 0452 34759 2757 0300 0444 3479 2759 0005362 14732 518 097 0259 14734 612 102 004 129 008 070 OBS STD STD T0366 0429 34832 2754 0400 0424 3483 2765 0500 0417 3483 2765 0004930 0004966 14739 503 0310 14742 500 0360 14756 598 07 D OBS T0504 0417 34830 2765 14757 598 REFERENCE SHIP CODE LATITUDE l/IO LONGITUDE ' '1/10 ii MARSDEN STATION Tl « 1 EAR ORIGINATOR'S DEPTH MAX. WAVE WEA- THER CODE CLOUD CODES NODC CTRY CODE ID. NO. CRUISE NO. STATION NUMBER TO BOTTOM OF S'MPL'S NUMBER >o* 1 r MO DAY HR.1/10 DIB. MGI PfR S A TYPE AM 31 549 EV 6138 N 063175W 223 |l3 08 03 091 1965 LCE 9469 0531 05 19 2 3 XI 0 1 0051 WATER WIND AIR TEMP. ^ SPECIAL OBSERVATIONS COLOR CODE IRANS. DIR. SPEED OR FORCE METE |mb» R DRY BULB WET BULB COD OBS. DEPTHS 22 305 125 100 078 8 10 "'"'""IcAST CARD DEPTH tm) T "C s •/.. SIGMA-T iPECIFIC VOLUME SAD SOUND 02 ml/I PO<-P rOTAL-P NOj-N NO,-N S1Q4-Si pH S r HR 1/10 ANOMALY XIO X 10^ vs - OI/( Hfl - Ol/I VO - ot/l kig - ot/l PO - ot/l c STD 0000 0393 3330 2646 0015776 0000 14643 748 ' 091' OBS STD STD 0000 0393 33295 2646 0010 0307 3337 2650 0020 0238 3345 2673 0014453 0013219 14543 748 025 0015 14609 746 0029 14582 742 045 003 003 002 091 OBS STD STD 0027 0199 33520 2681 0030 0185 3355 2584 0050 0130 3374 2704 0012149 0010339 14566 737 047 0042 14561 734 0064 14543 713 050 010 033 004 091 OBS STD 0053 0127 33759 2705 0075 0151 3399 2722 0008588 14542 710 072 0088 14559 684 081 020 061 005 091 OBS STD 0080 0152 34034 2725 0100 0230 3422 2735 0007444 14565 579 084 OIOB 14602 658 091 032 095 006 091 OBS STD STD 0105 0250 34276 2737 0125 0328 3444 2743 0150 0402 3459 2748 0006547 0005262 14612 653 090 0125 14551 540 0142 14689 529 095 032 115 007 091 OBS STD 0160 0422 34538 2750 0200 0438 3470 2753 0005865 14699 526 096 0172 14713 527 105 000 139 008 091 OBS STD STD 0213 0441 34721 2754 0250 0441 3476 2757 0300 0441 3480 2750 0005501 0005254 14717 627 098 0200 14724 610 0227 14733 594 106 001 144 008 091 OBS STD T0318 0441 34808 2751 0400 0440 3482 2762 0005193 14736 590 111 0279 14749 590 116 005 157 Oil 091 OBS STD T0424 0439 34828 2753 0500 0440 3483 2763 0005224 14753 590 0332 14765 591 09 1 OB S 053] 0 J.40 3^1 8 36 276 3 141 71 591 71 31 6137'.N MO DAY HR.1/10 223 13 08 03 118 1965 LCE 9470 21 S»EfO fOUCt ORIGINATOR'S 129 AIR lEMP. X 09 0*30 0* 13 2 * Gil «« UA NODC SIATION NUMRtR T -C S SAO OYN. M. % 10^ Ol ml/I 118 118 118 118 118 118 118 118 118 STD OBS STD STD OBS STD STD OBS STD OBS STD OBS STD STD OBS STD OBS STD STD OBS STD OBS 0000 0000 0010 0020 0028 0030 0050 0054 0075 0080 0100 0106 0125 0150 0160 0200 T0213 0250 0300 T0318 0400 T0422 0411 0411 0404 0396 0390 0353 0094 0065 0065 0065 0086 0100 0227 0347 0380 0405 0410 0410 0410 0410 0412 0413 3309 33089 3310 3314 33181 3319 3338 33424 3377 33822 3389 33921 3418 3442 34495 3459 34609 3465 3469 34698 3473 34730 2628 2528 2630 2633 2637 2642 2677 2582 2710 2714 2718 2720 2732 2740 2743 2748 2749 2752 2755 2756 2758 2758 0017507 0017359 0016994 0016225 0012851 0009715 0008929 0007734 0006995 0005991 0005740 0017 0035 00 51 0080 0109 0132 0153 0171 0006340 0204 0235 0265 0005559 0321 14548 14648 14546 14645 14644 14629 14521 14510 14518 14519 14533 14541 14604 14663 14580 14698 14703 14709 14718 14721 14735 14740 733 733 737 740 74 3 741 719 715 697 693 580 576 556 634 626 602 596 588 581 579 577 577 LONGITUDE MO DAY HR.1/10 ORIGINATOR'S 31 51379N 223 14 08 03 140 1965 LCE 9471 0095 01 13 1 4 XI 0 l4 0063 SPIED FO»CE BARO- METER lmb*l 05 140 140 140 TYPE STD OBS STD STD OBS STD STD OBS OBS STD OBS 0000 0000 0010 0020 0025 0030 0050 0060 0070 0075 0080 0184 3305 0184 0110 0056 0036 0029 0012 0012 0014 0013 33045 3311 3315 33190 3322 3329 33287 33285 3329 2544 2644 2554 2552 2565 2568 2574 2674 2674 2574 0015958 0000 14549 755 0014999 0014314 0013716 0013118 0015 0030 00 44 0071 0013094 0104 14 549 14518 14496 14488 14486 14483 14483 14487 14488 756 74 8 741 738 735 729 729 729 729 PO*-P TOTAl_P NO3-N - oi/l ug - oi/l 086 087 103 095 009 013 068 065 SI 04-si ve ■ oi/l 069 081 006 004 006 084 095 008 058 008 008 008 0012 33290 2674 14488 729 087 097 009 064 008 REFERENCE SHIP CODE LATITUDE l/lo LONGITUDE ' "l/io ii MAHSDEN STATION Tl M ORIGINATOR'S DEPTH MAX. WAVE WEA- THER CODE CLOUD CODES NODC CIRT ID. CODE NO. CRUISE NO. STATION NUMBER BOTTOM OF S'MPL'S NUMBER 10' r MO OAY HR.1/10 OIR. HGT n» if* IVft AM 31 549 EV 6 149 2N 064329W 223 14 08 03 167 1965 LCE 9472 0274 02 21 2 2 XI 3 2 0064 WATER WIND BARO- METER Imbll AIR TEMP. 'C COD NO. OBS. DEPTHS SPECIAL OBSERVATIONS COLOR CODE '»"■ DIR. SPEED FORCE DRY BULB WET BULB 18 S12 102 089 057 s 07 MESStNCR HR )/10 CAST NO. CARD TYPE DEPTH Iml T ■C s '/.. SIGMA-T SPECIFIC VOLUME SAO DYN. M. X 10" SOUND VELOCITY 0; ml/I PO4-P roiAL-p ug ■ oi/l NOj-N wg - oi/l NOj-N vt • or/I Sl04-Si PS . al/l pH S c c STD 0000 0201 13283 2626 0017700 0000 14553 763 ' 167 OBS 0000 0201 32832 2626 14553 763 STD 0010 0175 3287 2531 0017235 0017 14544 762 STD 0020 0150 3291 2536 0016758 0034 14535 761 167 OBS 0025 0138 32931 2638 14531 760 STD 0030 0132 3294 2539 0016425 0051 14529 758 STD 0050 0086 3301 2648 0015518 0083 14513 751 167 OBS 0051 0083 33015 2648 14512 751 STD 0075 -0017 3318 2557 0013792 0120 14472 742 167 OBS 0075 -0020 33194 2558 14471 741 STD 0100 -0085 3350 2595 0011059 0151 14449 716 167 OBS 0102 -0088 33519 2697 14449 714 STD 0125 -0047 3355 2707 0009980 0177 14473 698 STD 0150 -0008 3377 2714 0009317 0201 14497 585 167 OBS 0152 -0005 33782 2715 14499 684 STD 0200 0055 3390 2721 0008658 0245 14535 569 16 7 OB S 020 5 0 058 3: ? 02 2- 2 1 14 )38 668 72 - SHIP coot 31 549 EV LAHTUOf 1/10 6158 N 06A308W ORIGINATOR'S 223 lA 08 03 183 1965 LCE 9473 into fO«Cf S12 112 AIR lEMP. X 0293 ci^ rE( i(A 0 2 XI 0 |4 NODC STATION NUMBEIt 0065 DEPTH Ifn) T -C iKClFIC VOLUI lOTAl-P Vfl - cl/l NO:-N SI04-Si 183 183 183 183 183 5TD OBS STD STD OBS STD STD OBS STD OBS STD STD OBS STD OBS 0000 0000 0010 0020 0025 0030 0050 0050 0075 0075 0100 0125 0125 0150 0175 0222 0222 0209 0197 0191 0185 0161 0161 -0085 -0085 -0071 -0057 -0057 -0042 -0027 3238 32376 3258 3274 32813 3285 3303 33025 3328 33282 3347 3361 33606 3368 33703 2588 2588 2605 2619 2625 2628 2644 2644 2678 2678 2692 2703 2703 2708 2709 0021308 0000 14556 809 0019670 0018374 0017458 0015970 0011342 0010350 0020 0040 00 57 0091 0012738 0127 0157 0184 0009842 0209 14556 14555 1*554 14553 14552 14547 14547 14442 14442 14455 14458 14468 14480 14491 809 786 767 760 75 5 740 74 0 727 727 711 599 599 591 588 058 087 002 005 003 100 154 005 021 006 082 097 008 050 007 093 107 Oil 071 010 096 103 010 095 010 099 107 010 098 010 LONGITUOJ MO DAY HR.1/1 ORIGINATOR'S OBStRVATTONS WfA. THER CODE NODC STATION NUMBER 31 5*9 EV 5203 N 054294W 223 24 08 03 193 1965 LCE 9474 0293 03 17 0 2 3 l8 0066 16 SIO BARO- METER AIR TEMP. *C 083 061 DEPTH (ml T t s •/„ SPECIFIC VOLUME 01 1 NOj-N ug - aiyi NOj-N Pfl - ol/l 193 193 193 193 193 W3 193 193 STD OBS STD STD OBS STD OBS STD OBS STD OBS STD STD OBS STD OBS STD STD OBS 0000 0000 0010 0020 0025 0030 0049 0050 0073 0075 0097 0100 0125 0146 0150 T0194 0200 0250 T0293 020* 0204 0113 0035 0003 -0030 -0105 -0104 -0088 -0087 -0081 -0080 -0075 -0069 -0068 -0054 -0052 -0038 -0028 3233 32333 3253 3272 32810 3292 33239 3325 33435 3344 33517 3352 3355 33577 3358 33615 3362 3355 33700 2586 2586 2508 2527 2636 2545 2575 2575 2590 2591 2597 2507 2599 2701 2701 2704 2704 2706 2709 0021507 0019430 0017567 0015739 0012932 0011522 0010925 0010704 0010238 0009982 0020 0039 00 55 0084 0115 0143 0170 0010493 0195 0248 0299 14548 14548 14512 14481 14468 14455 14428 1*429 14443 144*3 14*51 14452 1*459 14455 14457 14481 14483 14498 14511 817 817 803 787 779 757 734 733 717 716 709 706 705 702 702 598 698 595 595 055 085 001 045 002 073 088 009 094 105 009 073 010 094 101 010 088 010 097 110 012 035 010 094 108 010 085 010 091 113 010 093 009 096 098 016 099 010 LATITUDE I/IO DAY HR.1/1( ORIGINATOR'S Gfl PER SEA WEA- THER CODE NODC STATION NUMBER 31 5*9 EV 62112N 06*278W 223 24 08 03 209 1965 LCE 9475 02 0067 BARO- METER (mbll AIR TEMP. X 07 T t SPECIFIC VOLUME Ol ml/I 209 209 209 209 209 209 01* STD OBS STD STD OBS STD OBS STD OBS STD OBS STD STD OBS STD OBS 0000 0000 0010 0020 002* 0030 0047 0050 0070 0075 0093 0100 0125 T01*l 0150 T0156 0184 0184 0189 0195 0197 0143 0023 0008 -0062 -0055 -0076 -0080 -0091 -0094 -0093 -0092 3250 32497 3255 3252 32552 3259 32841 3289 33119 3315 33250 3328 3332 33331 3333 33332 2500 2600 2605 2609 2612 2619 2538 2542 2564 2567 2575 2677 2681 2682 2682 2582 0019686 0019259 0018395 0015128 0013745 0012750 0012401 0000 0020 0039 0058 0093 0130 0153 0195 0012296 0225 1*5*1 1*5*1 1*5*6 1*551 1*553 14531 1*481 14476 14450 14450 14**9 1***9 1***8 14*50 1*451 793 793 784 777 775 775 768 755 745 740 72 7 727 725 724 728 053 088 005 015 003 074 093 007 017 005 007 037 005 090 101 Oil 059 008 088 098 Oil 072 008 097 118 014 078 010 14455 738 095 104 012 074 010 73 REFERENCE SHIP CODE LATITUDE 1/10 LONGITUDE "1/10 ii MARSDEN STATION TIME ORIGINATOR-S | DEPTH TO BOTTOM MAX. DEPTH OF S'MPL' WAVE WEA- THER COOf CLOUD COOES NOOC CUT CODf ID. NO. YEAR CRUISE NO. STATION NUMBER STATION NUMBER 10" 1 r MO DAY HH.1/10 DIR. MGT PER St* 1YN *M 31 5*9 EV 52155N 054282W 223 [2* |08 03 218 1965 LCE 9476 0121 01 11 1 2 XI 3 4 0058 WATER WIND BAfiO- MEIER (mbi) AIR TEMP, •c codf NO. OBS. DEPTHS SPECIAL OBSERVATIONS COLOR CODE '"';'■ DIR. S^EED OR FORCE DRY BULB WET BULB 11 S12 091 072 056 8 05 m(«ingr1cast ""' ° NO. HR 1/10 CARD TYRE DEPTH Iml T -C s •/.. SIGMA-T SfECIFIC VOLUME ANOMAlt-IlO' SAD DYN. M X 10= SOUND VELOCITY Oj ml/I PO.-P TOTAl-p vg - ot/l NO)-N ug - al/l NOi-N pg - ot/l SIO^-S- PB - ol/l PH S c c STD 0000 0021 3235 2598 0020350 0000 14455 800 218 08S STD STD 0000 0021 32347 2598 0010 0017 3242 2604 0020 0014 3250 2511 0019772 00191*1 ' 14465 ' 800 0020 14467 798 0040 14468 796 218 OBS STD STD 0025 0012 32545 2514 0030 -0016 3261 2521 0050 -0084 3280 2639 0018167 0016*60 14468 795 00,58 14457 784 0093 14432 754 218 OBS STD 0050 -0084 32798 2539 0075 -0075 3292 2548 0015521 14432 754 0133 14442 750 218 OBS STD 0075 -0075 32923 2548 0100 -0075 3296 2552 001521* 14442 750 0171 14445 749 21S OBS 0100 -0076 32951 2552 14446 749 REFERENCE SHIP CODE LATITU DE 1/10 LONGITUDE '1/10 MARSDEN SQUARE STATION TIME (GMT( YEAR ORIGINATOR'S | DEPTH TO BOTTOM MAX. DEPTH OF S'MPL- WAVE OBSERVATIONS WEA- THER CODE CLOUD CODES NODC STATION NUMBER CTRY CODf ID. NO. CRUISE NO. STATION NUMBER 10- r MO DAY HR.VIO DIR. HCI PER 5 * TYPE AM 31 5*9 EV 6356 5N 053558W 223 33 ,8 0* 106 1965 LCE 9477 |0269 03 11 0 X XI 3 7 0059 WATER WIND BARO- METER lmb»l AIR TEMP. •c VIS, COOf NO. OBS. DEPTHS SPECIAL OBSERVATIONS COLOR CODE tllANS. DIR. SPEED OR FORCE DRY BULB WET BULB 16 SIO 068 035 033 8 09 ""' •NO. HR 1/10 CARD TYPE DEPTH (ml r -c s •/.. SIGMA-T SPECIFIC VOLUMt ANOMA1.V-I10' SAO DYN. M K 10' SOUND VELOCITY Oj ml/I PO^-P «g.Ql/l TOTAl-P t>9 ■ ol/l NO:-N Jig - ol/l NOj-N pg - 01/1 SIOj-S- pg - ol/l PH s c c STD 0000 0281 3170 2530 00268*0 0000 14573 818 106 OBS STD 0000 0281 31704 2530 0010 0224 3197 2555 002**3* ' 14573 ■ 818 074 0026 14553 814 095 009 020 004 105 OBS STD 0010 0224 31966 2555 0020 0182 3204 2564 0023585 14553 814 096 0050 14537 820 103 015 046 007 105 OBS STD STD 0025 0156 32089 2570 0030 0112 3219 2580 0050 -0029 3255 2517 0022010 0018563 14527 822 108 0072 14510 821 0113 14454 814 118 010 072 010 106 OBS STD 0051 -0035 32557 2518 0075 -0132 3290 2548 001551* 14451 814 107 0155 14415 759 117 008 089 012 106 OBS STD 0076 -0134 32911 2549 0100 -0154 3307 2553 001*133 14414 767 098 0193 14411 730 107 009 109 Oil 106 OBS STD STD 0102 -0155 33082 2564 0125 -0134 3319 2672 0150 -0120 3328 2579 0013252 0012592 14411 728 105 0227 14425 707 0259 14438 594 116 Oil 088 012 105 OBS STD 0152 -0119 33290 2580 0200 -0120 3342 2590 0011*93 14439 593 0319 14448 595 106 OBS STD T0203 -0120 33430 2691 0250 -0112 3348 2695 0011035 14449 595 0376 14461 587 105 OBS T0254 -0111 33481 2595 14462 685 REFERENCE SHIP CODE LATITU DE 1/10 LONGITUDE ■ -1/10 i'i MARSDEN SQUARE STATION TIME (GMTl YEAR ORIGINATOR'S 1 DEPTH TO BOTTOM MAX. DEPTH OF S'MPL' WAVE OBSERVATIONS WEA- THER CODE CLOUD CODES NODC STATION NUMBER CTRY CODE ID. NO. CRUISE NO. STAT NUW ON BER 10* 1 !• MO DAY HR,I/10 DIR. HGT PER SEA UPt AM 31 549 EV 5354 7N 06 3123W 223 |33| 08 0* 132 1965 LCE 9478 C )333 03 18 2 2 XI 3 7 0070 WATER WIND BARO- METER Imbil AIR TEMP. K. VIS. CODE NO. OBS. DEPTHS SPECIAL OBSERVATIONS COLOR CODE TRANS. OIR- SPEED OR FORCE DRY BULB WET BULB 16 S12 068 061 056 8 09 MISiENCII C-..T "»' "NO. HR 1/10 CARD TYPE DEPTH (ml T -C s •/.. SIGMA-T SPECIFIC VOLUME ANOMALT->10' SAD DYN. M « IOI SOUND VELOCITY Oj ml/l PO*-P IOTAL_p vg ■ Dl/I NO2-N ug - 01/1 NOj-N PB - ol/l SI o.-s. p, - .1/1 pH s c c STD 0000 0*90 3255 2577 0022330 0000 14573 725 132 OBS STD STD 0000 0490 32553 2577 0010 0381 3255 2595 0020 0268 3276 2515 0020540 0018750 14673 725 051 0021 14531 752 0041 14585 786 081 001 000 003 132 OBS STD STD 0025 0211 32808 2523 0030 0132 3287 2534 0050 -0089 3309 2652 0015958 0014230 14562 793 065 0059 14528 791 0090 14433 781 098 003 002 004 132 OBS STD 0050 -0089 33087 2652 0075 -0154 3328 2579 0012570 14433 781 081 0124 14410 731 098 014 038 005 132 OBS STD 0075 -0154 33276 2679 0100 -0168 3340 2690 0011535 14410 731 088 0154 14409 719 101 015 075 009 132 OBS STD STD 0100 -0168 33404 2690 0125 -0169 3344 2693 0150 -0159 3349 2697 0011239 0010875 14409 719 097 0182 14413 738 0210 14418 743 112 012 075 010 132 OBS STD 0150 -0159 33485 2597 0200 -0131 3358 2704 0010216 14418 743 089 0263 14445 715 102 nl4 085 008 132 OBS STD STD T0200 -0131 33582 2704 0250 -0020 3380 2717 0300 0034 3391 2723 0009005 0008470 14445 715 095 0311 14508 557 0354 14543 541 135 014 088 009 132 OBS T0300 0034 33909 2723 14543 641 102 004 114 014 13 2 OB S T032 ■) 0 040 3. jc 23 2- '■2 4 14 j50 535 119 1 43 003 120 01 3 74 REFERENCE SHIP CODE LATITUDE 1/10 LONGITUDE "1/10 n MARSDEN STATION TIME ORIGINATOR'S 1 DEPTH TO BOTTOM DEPTH Of S'MPL- WAVE WEA- THER CODE CLOUD CODES NODC STATION NUMBER CUT cooe ID. NO. CRUISE NO. STATION NUMBER 10* r MO DAY HR.1/10 OIR. MCT PER S A UFE AM 31 549 EV t .354 7N 062255W 223 32 08 04 154 1965 LCE 9479 |0194 02 13 2 3 X2 5 18 0071 WATER WIND BARO- METER (mbil AIR TEMP. r VIS. COOi NO. OBS. DEPTHS SPECIAL OBSERVATIONS COLOR COOE tSANS. DIR. OR fORCI DRY BULB WET BULB 13 509 075 061 056 8 07 MtSSEMGR IIMt 0 HR 1/10 CAST NO. CARD TYPE DEPTH (ml T x: s •/.. SIGMA-T SPtCIIIC VOLUME AN0MALT-X16' SAD DYN. M X 10' SOUND VELOCITY Ol ml/l PO.-P lOTAL-P WB - oi/l NOj-N ug - 01/1 NO3-N US . ol/l 51 04-Si PR - Ol/l pH STD 0000 0495 3232 2558 0024156 0000 14672 723 154 OBS STD STD 0000 ' 0495 '32317 2558 0010 0348 3257 2593 0020 0210 3277 2620 0020847 0018238 14572 ■ 723 052 0023 14515 772 0042 14550 798 074 001 000 002 154 OBS STD STD 0025 0144 32852 2531 0030 0062 3291 2641 0050 -0150 3308 2563 0016249 0014103 14532 801 056 0059 14497 782 0090 14405 727 075 004 005 004 154 OBS STD 0050 -0150 33080 2663 0075 -0158 3321 2574 0013082 14405 727 110 0124 14407 711 121 018 072 on 154 OBS STD 0075 -0158 33208 2574 0100 -0155 3347 2595 0011053 14407 711 108 0154 14415 705 115 007 077 Oil 154 OBS STD STD 0100 -0155 33470 2595 0125 -0161 3348 2596 0150 -0164 3348 2596 0010991 0010935 14415 706 103 0181 14417 719 0209 14420 725 112 007 084 oil 154 OBS T0150 -0154 33479 2595 14420 726 097 113 012 085 009 154 OBS T0180 -0154 33468 2695 14425 727 085 095 Oil 089 009 REFERENCE SHIP COOE LATITU DE 1/10 LONGITUDE • '1/10 MAHSOEN SQUARE STATION TIME IGMTI YEAR ORIGINATOR'S [ DEPTH TO MAX. DEPTH OF S'MPL* WAVE OBSERVATIONS WEA- THER CODE CLOUD CODES NODC STATION NUMBER cut CODf ID. NO. CRUISE NO. STAT NUM ON 10* r MO DAY H R.1/I0 DIR. HOI PER SE A TYPE AMI 31 5A9 EV 6 354 7N 051452W 223 31 D8 04 1 79 1965 LCE 9480 0218 02 10 2 3 X5 5 8 0072 WATER WIND BARO- METER tmb»l AIR TEMP. ^ VIS, COOE NO. OBS. DEPTHS SPECIAL OBSERVATIONS COLOR CODE TRANS. DIR. SPEED OR FORCE DRY euLB WET BULB 12 S07 064 072 054 8 07 MESStNCR IIME 01 HR 1/10 CAST NO. CARD TYPE DEPTH Iml T y: S •''.. SIGMA-T SPECIFIC VOLUME ANOMALY-IIO' SAO DYN. M. X io> SOUND VELOCITY Ol ml/1 P04-P KR - Ot/I TOTAL-P NOi-N us - ol/l NOj-N ut - 01/1 SI 04-Si MS - 01/1 S ,H C STD 0000 0462 3249 2575 0022487 0000 14661 733 1 179 OBS STD STD 0000 0462 32494 2575 0010 0431 3250 2579 0020 0359 3254 2589 0022143 0021175 ' 14561 733 055 0022 14650 753 0044 14621 768 078 001 000 003 179 OBS STD STD 0025 0307 32571 2597 0030 0195 3255 2512 0050 -0105 3289 2647 0019051 0015572 14500 774 0054 14554 782 0099 14423 787 005 000 005 179 OBS STD 0050 -0105 32892 2647 0075 -0156 3308 2553 0014107 14423 787 082 0135 14405 729 082 018 035 005 179 OBS STD 0075 -0155 33075 2653 0100 -0155 3324 2575 0012857 14406 729 107 0170 14413 706 122 015 119 009 179 OBS STD STD 0100 -0155 33235 2575 0125 -0159 3335 2685 0150 -0162 3343 2692 0011955 0011285 14413 705 100 0201 14417 707 0230 14421 707 109 008 081 Oil 179 OBS STD 0150 -0162 33434 2692 0200 -0125 3355 2701 0010474 14421 707 095 0284 14448 700 107 005 085 010 179 OBS 0200 -0125 33551 2701 14448 700 100 110 008 100 Oil REFE ENCE SHIP coot LATITU DE 1/10 LONGITUDE s^ ' -1/10 - MARSDEN SQUARE STATION TIME IGMTI YEAR ORIGINATOR'S | DEPTH TO OTTOM MAX. DEPTH OF S'MPL- WAVE OBSERVATIONS WEA- THER CODE CLOUD CODES NODC STATION NUMBER cm CODt 10. NO. CRUISE NO. STAT NUM ON tER 10' r MO DAY H 1.1/10 OIR. HGI PER SEA 1YPE AM 31 549 EV ( 354 5N 05 1005W 1 223 31 08 04 2 07 1965 LCE 9481 C 256 02 13 2 3 X6 5 8 0073 WATER WIND BARO- METER Imbi) AIR TEMP. ■c VIS. CODE NO. OBS. DEPTHS SPECIAL OBSERVATIONS COLOR CODE TRANS. DIR- SPEfO OR fOflCI DRY BULB WET BULB 10 508 054 057 051 8 09 MtSJiNGR tIME 0 MR 1/10 CAST NO. CARD TYPE DEPTH (ml T -C S •''.. SIGMA-T SPECIFIC VOLUME AN0MAL1-I1D' SAO DYN. M. X 10' SOUND VELOCITY 02 ml/1 PO4-P vs-o'/l TOTAl-P „g - ol/l NOj-N UR - Ot/I NOs-N ui • Ol/l S104-Si ws - 01/1 pH STD 0000 ] 0517 3238 2560 0023922 0000 14682 725 1 207 OBS STD STD 0000 0517 32379 2560 0010 0498 3242 2555 0020 0479 3246 2571 0023431 0022951 ' 14682 725 058 0024 14677 724 0047 14671 723 075 000 000 002 207 OBS STD 0025 0470 32478 2573 0030 0309 3252 2500 0020145 14668 723 062 0068 14603 732 084 003 000 004 207 OBS STD 0049 -0095 33042 2559 0050 -0097 3305 2559 0014487 14430 746 044 0103 14429 7^5 104 024 053 008 207 OBS STD 0073 -0133 33260 2678 0075 -0135 3327 2678 0012555 1^419 723 100 0137 14^*18 721 110 010 070 Oil 207 OBS STD STD 0096 -0162 33350 2685 Olno -0161 3335 2586 0125 -0153 3345 2594 0011891 0011128 14410 705 099 0168 14412 705 0196 14421 708 110 001 088 012 207 OBS STD T0145 -0147 33545 2701 0150 -0136 3357 2703 0010321 14428 710 087 0223 14435 704 103 005 096 009 207 OBS STD T0190 -0050 33776 2716 0200 -0020 3383 2719 0008790 14484 663 095 0271 14501 657 101 002 110 Oil 207 OBS STD 0225 0027 33911 2724 0250 0037 3392 2723 0008446 14527 641 107 0314 14536 622 110 004 122 014 20 7 OB S 025C 0 337 33 9 15 27 2 3 14" 36 522 101 1 15 005 119 01 4 75 REFERENCE SHIP CODE LATITUDE 1/10 LONGITUDE ■1/10 =5 Bo °1 MARSDEN STATION Tl VIE ORIGINATOR'S DEPTH MAK. DEPTH OF S'MPL" WAVE WEA- THER CODE CLOUD CODES ODC CUT CODE ID. NO. IGMTl CRUISE NO. STATION NUMBER BOTTOM NUMBER 10' 1- MO DAY HR.1/10 D.B. NCI PER S A HP! AM 31 5»9 EV 63542N 060157W 223 30 08 04 236 1965 LCE 9482 0439 04 08 1 2 X6 5 8 0074 WATER WIND lARO- METER Imbll AIR TEMP. ^ VIS. COO NO. OBS. DEPTHS SPECIAL OBSERVATIONS COLOR CODE TRANS. UKl OIR. SPEED Ol (DICE DRY BULB WET BULB 06 S09 034 058 056 7 10 MISSING. 1 CAST ""' -i NO. Hfi 1/10 CARD TYPE DEPTH tml I t s •/.. SIGMA-T SPtClflC VOLUME ANOMALT-llO' SAD DYN. M. 1 loi SOUND VELOCITY Oj ml/l POj-P VB-ol/l TOTAl-P 119 - ot/l NOl-N wg - ot/l NO,-N vg - oi/l SI 04-S. pg • Ql/I PH S c c STO 0000 0510 [3229 2554 0024494 0000 14678 738 ' 236 OBS 0000 0510 32293 2554 14678 738 061 082 002 000 003 STD 0010 04*2 3233 2565 0023500 0024 14652 743 236 OBS 0010 0442 32334 2565 14652 743 065 107 002 002 004 STD 0020 0323 3243 2584 0021694 0047 14604 789 236 OBS 0026 0245 32509 2597 14573 803 061 079 002 001 002 STD 0030 0160 3263 2613 0018960 0067 14537 791 STO 0050 -0130 3307 2662 0014233 0100 14414 744 236 OBS 0052 -0147 33101 2665 14407 740 100 123 021 062 008 STO 0075 -0161 3327 2679 0012598 0134 14406 708 236 OBS 0078 -0162 33292 2681 14407 706 106 113 005 082 012 STD 0100 -0171 3338 2688 0011711 0164 14407 712 236 OBS 0104 -0172 33392 2689 14408 713 096 110 004 091 010 STD 0125 -0168 3343 2692 0011317 0193 14413 720 STD 0150 -0153 3349 2697 0010882 0221 14426 729 236 OBS 0155 -0148 33507 2698 14429 731 077 087 002 073 007 STO 0200 -0086 3368 2710 0009635 0272 14468 669 236 OBS T0206 -0075 33709 2712 14474 663 103 113 004 100 Oil STD 0250 0083 3405 2731 0007707 0315 14559 660 STD 0300 0207 3434 2746 0006444 0351 14526 557 236 OBS T0307 0220 34370 2747 14533 657 118 129 010 149 018 STD 0400 0267 3455 2758 0005434 Q410 14572 557 236 OBS 0414 0274 34578 2759 14678 557 REFERENCE SHIP CODE LATITUDE 1/10 LOh GITUDE ■ -i/io n MARSDEN STATION Tl WE ORIGINATOR'S DEPTH MAX DEPTH OF S'MPL- WAV! W(A- THfK CODE ClOUO CODES ^ODC CtRl COD! ID. NO. CRUISE STATION NO. NUMBER BOTTOM NUMBER ID- r MO DAY HR.1/10 S D(«. HCI ^E» Si* nrt AM 31 549 EV 6 353 9N 059289W 222 39 08 05 022 1955 LCE 9483 0515 05 10 1 2 X2 5 8 0075 WATER w NO BARO- METER tmbtl AIR TEMP. 'C VIS. COD NO. OBS. DEPTHS SPECIAL OBSERVATIONS COLOR CODE TR*NS. OIR. SPEED OP (OflCE DRY BULB WEI BULB 11 SOB 007 067 057 6 11 MESSENGR i TIME J: HR l/IO CAST NO. CARD TYPE DEPTH Iml T i: s •/.. SIGMA-T SPECIFIC VOLUME ANOMALT-IlO' SAD DYN. M. X loJ SOUND VELOCITY 02 ml/I VB • oi/l roTAL-r «e- oi/i NOi-N i>a - oi/i NOj-N SI o^-s. ug - ol/l pH S c c STD 0000 0540 3240 2560 0023982 0000 14592 711 022 OBS 0000 0540 32404 2550 14692 711 STD 0010 0452 3248 2575 0022538 0023 14658 733 022 OBS 0010 0452 32475 2575 14658 733 STO 0020 0255 3297 2533 0017059 0043 14582 790 022 OBS 0025 0170 33140 2553 14548 803 STD 0030 0089 3317 2660 0014419 0059 14513 778 STD 0050 -0127 3327 2678 0012708 0085 14418 715 022 OBS 0051 -0133 33280 2579 14416 713 STD 0075 -0149 3342 2691 0011478 0115 14414 715 022 OBS 0076 -0150 33429 2592 14414 715 STD 0100 -0152 3350 2697 0010842 0144 14418 722 022 OBS 0102 -0152 33508 2698 14418 722 STO 0125 -0101 3363 2706 0009994 0170 14448 720 STD 0150 -0035 3378 2716 0009111 0194 14485 702 022 OBS 0152 -0029 33795 2717 14488 700 STD 0200 0136 3411 2733 0007504 0235 14575 511 022 OBS 0203 0146 34133 2734 14580 507 STD 0250 0325 3446 2745 0005561 0271 14571 503 STD 0300 0446 3469 2751 0005131 0303 14733 599 022 OBS T0307 0457 34717 2752 14739 598 STD 0400 0469 3483 2759 0005488 0361 14751 588 022 OBS T0403 0469 34828 2750 14762 587 STD 0500 0366 3475 2754 0005005 0413 14733 555 02 2 OB S T050 ? 0 351 3' *1 38 2" 6 5 14 ?28 562 76 31 LAT1TUD€ 1/10 53538N lONGITUOf 058442W 222 08 052 1965 16 01 »0«Cf S20 OtUGlNATOIt'S DEPTH TO BOTTOM NO. OBS. DtPTHS 11 DEPTH OP VMPL-S 07 4 2 WEA- THER CODE NODC STATION NUMBER DEPTH i I -c S •''.. SIGMA-T O? ml/1 052 052 052 052 052 052 052 052 052 052 STD OBS STD STD OBS STD STD OBS STD OBS STD OBS STD STD OBS STO OBS STD STD OBS STO OBS STD STD OBS STD OBS 0000 0000 0010 0020 0025 0030 0050 00 51 0075 0075 0100 0102 0125 0150 0152 0200 0203 0250 0300 0305 0400 0405 0500 0500 T0507 0700 T0725 0554 05 54 0590 0508 0460 0369 0141 0135 0162 0164 0248 0255 0328 0387 0391 0439 0442 0480 0504 0505 0495 0494 0475 0457 0455 0299 0242 3325 33248 3325 3331 33346 3342 3357 33579 3389 33898 3410 34118 3431 3448 3*487 3458 34586 3479 3487 34874 3489 34891 3490 3490 34900 3470 34531 2512 2612 2621 2535 2543 2558 2597 2598 2713 2714 2723 2724 2733 2741 2741 2751 2751 2755 2759 2759 2752 2752 2754 2767 2767 2757 2766 0018991 0018142 0016855 0014638 0010942 0009422 0008495 0007525 0005935 0005711 0005450 0005155 0005015 0000 0019 00 36 0052 0077 0103 0125 0145 0164 0006026 0196 0225 0253 0005313 0307 0359 0410 0004829 0450 14749 147*9 1*725 1*594 145 76 14639 14547 145*4 14563 14554 14608 14511 14649 14681 1*683 . 14714 14715 14740 14750 1*751 14773 14773 14781 14790 14791 14737 14716 583 683 732 760 757 757 723 722 596 595 674 573 563 553 652 567 668 642 625 624 525 525 524 623 623 545 517 REFERENCE SHIP CODE LATITUDE 1/10 LONGITUDE ■ 'l/IO ii MARSDEN STATION Tl ME ORIGINATOR'S DEPTH MAX. DEPTH Of S'MPL- WAVE WEA- THER CODE CLOUD CODES NODC CItT CODE 10. NO. CRUISE NO. STATION NUMBER BOTTOM NUMBER 10- 1" MO DAY HH.1/10 DIR. HCI PER S * lYPl AMY 31 5*9 EV 63S36N 058000W 222 38 38 05 085 1965 LCE 9*85 1130 10 13 5 2 X5 7 8 0077 WATER WIND BARO- METER Imbil AIR TEMP. r VIS. COD NO. OBS. DEPTHS SPECIAL OBSERVATIONS COLOR CODE TUNS. Mil OIR. SPEED OR FORCE DRY BULB WET BULB 16 S20 997 083 083 6 13 MlllENG. CAST TIME o\i, MR 1/10 CARD TYPE DEPTH Im) T -C 5 •/.. SIGMA-T SPECIFIC VOLUME ANOMALI-llO' SAD DVN. M. 11 10' SOUND VELOCin Ol ml/l PO*-P ,1 - .1/1 TOTAl-P KB- 01/1 NOj-N vg ■ ot/l NOi-N >, - 01/1 SI 0*-Si wa - m/l PH S c C STD 0000 0588 3334 2615 0018731 0000 1*76* 68* ' 085 OBS STD STD 0000 0688 33340 2615 0010 0594 3337 2517 0020 0700 3341 2519 0018571 0018404 1*76* 684 010 0019 14769 585 0037 14773 686 037 001 000 001 085 OBS STO 0021 0701 33412 2519 0030 05*5 3358 2650 0014502 14774 686 015 0054 14715 743 041 000 000 001 085 OBS STD 00*2 0404 339*5 2597 0050 0357 3*05 2709 0009814 14553 757 032 0078 14650 722 012 026 003 085 OBS STD 0061 03*0 3*185 2722 0075 035* 3429 2729 0007980 14642 581 083 0100 14552 57* 092 025 082 005 085 OBS STD 0081 0361 34338 2732 0100 0391 3445 2739 0007081 14557 670 086 0119 14574 653 10* 038 104 007 085 OBS STD STD 0123 0421 34579 2745 0125 0423 3459 2745 0150 04*7 3457 2750 0006455 0006135 14692 538 100 0136 14593 538 0152 14709 532 108 019 129 008 085 OBS STD STD STO 0165 0460 3*712 2751 0200 0475 3477 2754 0250 0492 3*83 2757 0300 0503 3488 2750 00057*8 0005550 0005354 14717 530 095 0181 14730 631 0210 14745 532 0237 14759 532 115 002 1*9 008 085 OBS STD STD T0334 0507 34907 2751 0400 0498 3491 2763 0500 0484 3491 2754 0005200 0005149 14767 633 101 0290 14774 633 0341 14785 633 115 004 153 008 085 OBS STD STD 0516 0482 3*91* 2765 0600 0470 3490 2755 0700 0456 3489 2755 0005147 0005183 14787 533 106 0393 14795 531 0445 14805 629 117 001 152 009 085 OBS STD 0701 0456 34890 2766 0800 0435 3490 2769 0004955 14805 629 101 0495 14814 524 125 001 1*1 009 09* OBS STD T0868 0427 0900 0427 3491 2771 0004885 0544 14828 516 085 OBS STD T0913 0424 34914 2771 1000 0350 3492 2779 0004013 1*829 515 107 0589 1*812 110 000 159 010 09 * OB S 100 3 0 350 3 »< )lf 2 77 9 1* B12 77 REFERENCE SHIP CODE LATITUDE 1/10 LONGITUDE * -1/10 if MARSOEN STATION TIME ORIGINATOR'S DEPTH MAX . WAVE WEA- TMER CODE ClOUD CODES NODC CTRV CODE ID. NO. CRUISE NO. STATION NUMBER TO BOTTOM OF S-MPL-S STATION NUMBER 10* r MO OAV MR.1/10 Dl«. MOT PER SEA IIPl AW 31 5A9 EV 54255N 057500W 222 1*1 08 05 138 1965 LCE 9486 0870 08 17 7 3 X2 7 8 0078 WATER WIND BARQ. METER Imbil AIR TEMP. •c ^».dEs SPECIAL OBSERVATIONS COLOR CODE TRANS. DIR. SPIED OR DRY euLB WET BULB 15 S20 980 089 078 6 1 12 """INS^lcASI TIME 0. NO. HR 1/10 CARD TYPE DEPTH Iml T -C s •/„ SIGMA-T SPECIFIC VOIUME ANOMALT-XlO' SAD DYN. M. X 10^ SOUND VELOCITY 0? ml/1 (•04-? KB ■ o'/l rOTAL-P 1-8 -ot/l NOj-N tig - ol/l NO3-N Ve - ol/l SI O4-SI wg - ol/l pH S C c STD 0000 0578 3316 2602 0019941 0000 14756 569 158 OBS 0000 0578 33161 2602 14758 659 STD 0010 0673 3317 2503 0019859 0020 14757 575 STD 0020 0668 3317 2604 0019777 0040 14757 582 158 OBS 0025 0665 33171 2605 14757 685 STD 0030 0547 3323 2624 0017895 0059 14711 736 STD 0050 0155 3344 2677 0012864 0039 14554 808 158 OBS 0050 0155 33438 2577 14554 808 158 OBS 0055 -0028 33559 2698 14471 721 STD 0075 0023 3366 2704 0010325 0118 14497 700 158 OBS 0075 0023 33660 2704 14497 700 158 OBS 0099 0085 33865 2715 14532 675 STD 0100 0090 3388 2717 0009029 0142 14535 674 STD 0125 0197 3411 2728 0008029 0164 14590 653 158 OBS 0147 0280 34294 2736 14532 537 STD 0150 0291 3432 2737 0007232 0183 14638 635 158 OBS T0198 0435 34605 2746 14711 611 STD 0200 0439 3462 2745 0006475 0217 14713 611 158 OBS T0244 0515 34798 2752 14754 602 STD 0250 0514 3480 2752 0005029 0248 14754 501 STD 0300 0507 3482 2755 0005858 0278 14760 595 158 OBS T0369 0497 34853 2758 14768 592 STD 0400 0493 3486 2750 0005494 0335 14772 594 STD 0500 0481 3490 2764 0005212 0388 14784 602 158 OBS T0526 0478 34906 2765 14787 604 STD 0600 0410 3488 2770 0004505 0438 14770 592 15 8 OB S 060C 0' .10 34 8 81 27 7 3 14- 70 592 78 31 SHIP CODE LATITUDE VIO 6A550N LONGITUDE ■1/10 STATION TIME 222 47 08 05 179 1965 LCE 9488 S«tD 0» fOUCi S18 ORIGINATOR'S AIR TtMP. \: 078 078 07 15 Mcn rt«| sfA WEA- THER coot NODC STATION NUMBER 0080 DEPTH I Oj ml/I 179 179 179 179 179 179 179 179 179 179 179 STD OBS STD STD OBS STD STD OBS STD OBS STD OBS STD STD OBS STD OBS STD OBS STD OBS STD OBS STD STD OBS OBS 0000 0000 0010 0020 0026 0030 0050 0051 0075 0077 0100 0102 0125 0150 0152 0200 T0203 0250 0281 0300 T0306 0400 0408 0500 0500 T0510 T0580 0564 0664 0659 0653 0550 0484 -0074 -0090 -0107 -0108 0141 0157 0191 0246 0251 0413 0420 0485 0500 0496 0495 0495 0495 0415 0303 0290 0193 3322 33220 3322 3322 33225 3327 3345 33465 3355 33580 3387 33888 3404 3420 34217 3454 34558 3473 34789 3480 34806 3487 34873 3480 3470 34688 34502 2609 2609 2610 2511 2511 2635 2592 2693 2701 2703 2713 2714 2723 2732 2733 2743 2744 2750 2753 2754 2755 2760 2760 2763 2756 2767 2758 0019324 0019255 0019186 0015908 0011428 0010535 0009435 0008513 0007750 0006798 0005228 0005878 0005452 0005167 0004801 0019 0039 0057 0085 0112 0137 0160 0180 0216 0249 0279 0336 0389 0439 14753 14753 14752 14752 14752 14685 14445 14438 14436 144 36 14558 14565 14586 14617 14619 14701 14704 14742 14754 14755 14756 14772 14774 14755 14723 14718 14587 573 573 575 577 578 583 708 709 589 688 575 575 561 645 645 618 517 503 599 598 598 600 600 582 562 560 477 REFERENCE SHIP CODE LATITUDE 1/10 LONGITUDE ■ '1/10 Si MARSDEN STATION TIME ORIGINATOR'S DEPTH MAX. DEPTH OF S'MPL'S WAVE WEA- THER CODE CLOUD CODES •JODC CIRY CODE ID. NO. TEAR CRUISE NO. STATION NUMBER TO BOTTOM STATION NUMBER 10* r MO DAY HR.1/10 DIIU HOT nt lEA urt AM 31 5*9 EV 6 510 ON 057420W 222 57 08 05 202 1965 LCE 9489 0680 06 15 5 2 X6 5 8 0081 WATER WIND BARO- MEIER (mb*l AIR TEMP, y: VIS, COD NO. OBS. DEPTHS SPECIAL OBSERVATIONS COLOR CODE TRANS. OIR. SPEfO OB FOUCI DRT BULB WEI BULB 15 S18 956 072 072 6 11 MlSitNGR 1 MR T/10 CAST NO. CARD TYPE DEPTH 1ml T X 5 •/.. SIGMA-T SPECIFIC VOLUME ANOMALY-nO' SAO DVN. M. X 10^ SOUND VElOCITt 03 "»l/l POt-P lOTAl-f vg - ol/l NOl-N NOj-N VB - ot/l SI O4-S' pg - ol/l PH s c c STD 0000 0405 3168 12517 0028078 GOOD 14626 730 202 OBS STD STD 0000 0405 31679 2517 14526 ' 730 ' 0010 0304 3258 2598 0020398 0024 14597 757 0020 0193 3317 2553 0015084 0042 14558 783 202 OBS STD 0021 0181 33210 2558 14553 786 0030 0040 3328 2572 0013314 0056 14492 754 202 OBS STD 0042 -0089 33352 2584 14435 724 0050 -0124 3338 2687 0011873 0081 14421 715 202 OBS STD 0053 -0154 33426 2692 14410 709 0075 -0147 3347 2595 0011101 0110 14416 718 202 OBS STD STD 0084 -0133 33513 2598 14424 719 0100 -0091 3353 2598 0010807 0137 14447 597 0125 0016 3371 2708 0009939 0163 14503 656 202 OBS STD 0125 0015 33705 2708 14503 656 0150 0215 3417 2732 0007726 0185 14503 636 202 OBS STD STD T0168 0315 34418 2743 14553 518 0200 0311 3443 2744 0006619 0221 14556 604 0250 0303 3445 2745 0005438 0254 14561 582 202 OBS STD 0257 0302 34452 2747 14662 579 0300 0392 3463 2752 0005998 0285 14710 603 202 OBS STD STD T0348 0456 34754 2756 14746 618 0400 0418 3474 2759 0005518 0343 14739 615 0500 0344 3471 2763 0005105 0395 14724 582 202 OBS STD T0544 0312 34689 2755 14717 557 0500 0137 3452 2755 0004609 0444 14648 515 20 i OB 3 T0500 0 37 34 5 22 27 et 146 48 515 79 REFERENCE SHIP CODE LATITUDE 1/10 LONGITUDE ■ 'I/IO ii MARSDEN STATION TIME ORIGINATOR'S DEPTH MAX DEPTH OF S'MPL" WAVE WEA- THER CODE CLOUD CODES NODC cm coot ID. NO. CRUISE NO. STATION NUMBER BOTTOM STATION NUMBER 10* r MO DAY HR.1/10 S OIF. MGI ftF IIA UFI AM 31 5*9 EV 6 525 ON 057390W 222 57 38 05 222 1965 LCE 9490 0622 05 15 7 3 X5 5 8 0082 WATER WIND BARD- METER (mbil AIR TEMP. •c VIS ''°- "-d?pV„s SPECIAL OBSERVATIONS COLOR CODE TBANV OIR. SPfED OR FO«Ct DRY 8ULB WET flULB 16 S17 953 078 072 5 12 MEJSENCR IIMf 0 HR 1/10 CAST NO. CARD TYPE DEPTH Onl I "c s */.. SIGMA-T SPEC'HC VOLUME ANOMALT-110' SAD OYN. M. X 10= SOUND VELOCITY 03 ml/I PO<-P vg - oi/i TOTAl-p vg • 01/1 NOj-N vg - 01/1 NOj-N PO - ol/l SI 04-S. PR . a1/1 PH S C C STD 0000 0385 3151 12505 0029195 0000 14615 735 222 OBS 0000 03B5 31507 2505 14515 736 STD 0010 0194 3233 2586 0021463 0025 14545 756 STD 0020 0053 3292 2642 0016127 0044 14492 777 222 OBS 0025 0002 33141 2563 14472 787 STD 0030 -0010 3321 2669 0013508 0059 14468 764 222 OBS 0049 -0066 33412 2688 14449 712 STD 0050 -0072 3342 2688 0011780 0084 14446 713 222 OBS 0073 -0157 33480 2696 14411 722 STD 0075 -0156 3349 2597 0010923 0113 14412 722 222 OBS 0097 -0133 33569 2703 14427 720 STD 0100 -0126 3358 2703 0010305 0139 14431 714 STD 0125 -0058 3372 2713 0009434 0154 14454 670 222 OBS 0146 -0015 33831 2719 14494 642 STD 0150 -0005 3385 2720 0008723 0187 14499 539 222 OBS 0196 0120 34117 2734 14567 505 STD 0200 0135 3414 2735 0007370 0227 14575 503 222 OBS T0244 0254 34372 2745 14538 581 STD 0250 0257 3438 2745 0006540 0252 14640 577 222 OBS T0294 0277 34467 2750 14657 550 STD 0300 0287 3449 2751 0006015 0293 14663 551 222 OBS 0348 0360 34646 2757 14704 565 222 OBS T0398 0425 34782 2761 14742 597 STD 0400 0422 3478 2761 0005300 0350 14741 595 STD 0500 0254 3462 2754 0004866 0400 14684 541 222 OBS 0573 0132 3*503 2765 14541 501 SHIP CODE LONGITUDE ■1/10 STATION TIME ORIGINATOR'S NODC STATION NUMBER 31 5*9 EV 65410N 057430W 222 57 08 05 007 1965 LCE 9491 0587 05 14 4 2 16 JPEtO OR fOFCt AIR TEMP, r 061 DEPTH (ml T IC SAD DYN. M. X lo' Ol ml/1 NOj-N iia - ol/l SI 04-Si PS - OI/I 007 007 007 007 007 007 007 007 007 007 STD OBS STD STD OBS STD STD OBS STD OBS STD OBS STD STD OBS STD OBS OBS STD STD OBS STD OBS STD OBS 0000 0000 0010 0020 0027 0030 0050 0053 0075 0080 0100 0106 0125 0150 0150 0200 0213 0245 0250 0300 T0319 0400 T0425 0500 T0525 0266 0266 0095 -0031 -0093 -0100 -0127 -0129 -0119 -0114 -0083 -0058 0052 0158 0184 0170 0165 0219 0230 0306 0319 0248 0227 0167 0147 3097 30965 3205 3285 33238 3327 3343 33452 3359 33625 3373 33768 3394 3411 34153 3426 34302 34410 3443 3457 34505 3457 34550 3452 34504 2472 2472 2570 2641 2575 2677 2691 2593 2704 2705 2714 2715 2724 2731 2734 2742 2745 2751 2751 2756 2757 2761 2762 2753 2754 0022984 0016274 0012803 0011481 0010255 0009308 0008348 0007749 0028 0047 0052 0086 0113 0138 0150 0180 0005721 0215 0005934 0248 0005591 0277 0005U9 0330 0004839 0380 I 14557 14557 14497 14452 14430 14428 14420 14420 14431 14434 14453 14462 14523 14577 14591 14592 14593 14523 14629 14672 14682 14654 14559 14544 14540 755 765 765 763 762 753 705 700 574 569 648 543 543 534 627 574 565 552 553 558 570 548 535 477 451 80 SHIP CODE 31 549 EV LONGITUDE ' VIO 057*90W 0 DAT Ha.1/' 222 67 08 06 0'»2 1965 LCE 9492 21 into foacE S18 OtlGINATOrS lARO- METER AM TEMP. X 050 13 05 icijrfil s(A WEA- THER CODE X2 7 Is NODC STATION NUMBER 0084 M ESSEN Gl I, HR VIO T DEPTH Iml T X s •/.. SAO OYN. M. t 10^ Ol ml/I NOj-N NOj-H pg - ol/l SI Of Si wg • dl/l 0*2 0*2 0*2 0*2 0*2 0*2 0*2 0*2 0*2 0*2 0*2 0*2 0*2 STD OBS OBS STD STD OBS STD STD OBS STD OBS STD OBS STD STD OBS STD OBS STD OBS STD OBS OBS STD OBS OBS 0000 0000 0007 0010 0020 0026 0030 0050 00 51 0075 0075 0100 0102 0125 0150 0152 0200 0202 0250 0254 0300 T0305 0364 0400 0405 T0455 0261 0261 0258 0169 -0053 -0155 -0155 -0160 -0160 -0163 -0163 -0162 -0152 -0154 -0122 -0118 0025 00 28 0020 0019 0057 0066 0258 0202 0197 0175 3086 30852 30858 3125 3231 32754 3280 3301 33018 3328 33291 3338 33392 3353 3365 33675 3392 33929 3417 34178 3422 34235 34539 3451 34500 34496 2464 2464 2464 2502 2599 2537 2541 2558 2559 2580 2681 2588 2589 2700 2710 2711 2724 2725 2745 2745 2747 2747 2758 2760 2760 2761 0033074 0029507 0020288 0015254 0014615 0012517 0011734 0010589 0009579 0008343 0006411 0005256 0031 0055 00 74 0105 0139 0170 0197 0223 0258 0305 0336 0005205 0394 14553 1*553 1*553 1*519 14430 14394 1*395 14399 14399 14405 14405 14411 14412 14422 14443 14445 14522 1*524 14532 14532 1*558 1*563 1*652 14543 14541 14640 757 757 757 758 760 752 750 708 705 589 688 684 683 556 634 633 614 613 556 531 530 549 535 533 522 LATITUDE 1/10 LONGITUDE '1/10 ORIGINATOR'S Gr «« St* WEA- THER CODE EV 664 ION 057550W 222 57 08 05 077 1965 LCE 9493 05 3 2 0085 S^EED S13 BARO- METER AIR TEMP, t; 028 025 11 T "C SOUND VELOCirr 0 3 ml/ NOi-N iig- nt/l NOs-H Wfl - ol/l SI 04-Sf VO - ol/l 077 077 077 077 077 077 077 077 077 077 077 STD OBS STD OBS STD OBS STD STD OBS STD OBS STD OBS STD STD OBS STD OBS STD STD OBS STD OBS STD OBS 0000 0000 0010 0010 0020 0025 0030 0050 0052 0075 0078 0100 0104 0125 0150 0155 0200 0207 0250 0300 T0315 0400 T0407 0500 T0575 0275 0275 0274 0274 -0021 -0141 -0144 -0158 -0159 -0166 -0157 -0159 -0158 -0159 -0151 -0151 -0114 -0105 -0005 0074 0092 0116 0117 0118 0118 3108 31075 3105 31051 3214 32599 3265 3285 32873 3299 33005 3315 33192 3332 3347 33503 3378 33814 340 2 3421 34257 3439 34397 3447 34487 2480 2480 2478 2478 2583 2624 2628 2546 2647 2557 2558 2570 2573 2583 2595 2598 2719 2721 2734 2745 2748 2757 2757 2753 2754 0031561 0031737 0021745 0017434 0015772 0014735 0013429 0012184 0011013 0007408 0006441 0005389 0004821 0000 0032 0058 0078 0111 0149 0185 0217 0246 0008764 0295 0335 0370 0429 0480 14562 14562 14563 14553 1*447 1*398 1*398 14398 14398 14400 144 00 14410 14411 14415 14422 14423 14455 14452 14518 14565 14577 14603 14605 14622 14535 752 752 757 757 79 5 805 793 747 744 720 717 694 591 593 595 596 627 518 581 548 540 518 517 512 508 I 060 090 001 000 005 059 075 000 000 005 089 106 010 026 008 017 059 Oil 055 123 001 058 012 113 127 001 085 014 097 109 004 089 Oil 115 125 001 119 015 120 122 000 153 019 119 127 000 154 022 129 148 001 152 026 81 REFERtNCE SHIP CODE LATIIUOE 1/10 lONGlTUOE •1/10 So MARSOEN STATION Tl VIE ORIGINATOR'S DEPTH DEPTH OF S'MPL- WAVE WEA- THER CODE CLOUD COOES NOOC CtM CODt ID. NO. CRUISE STATION NO. NUMBER BOTTOM NUMBER 10* r MO DAY HR.VIO 01*. MCT H» i A npt AM 31 5*9 EV 66410M 058210W 222 68 38 06 092 1965 LCE 9494 0713 06 16 2 2 X4 7 8 0086 WATER WIND BARO- METER (mbl) AIR TEMP. •c c"oL -°- '''^°* DEPTHS SPECIAL OBSERVATIONS COLOR CODE tHANS. DIR. SPEtO OR fOPCl DRV BULB WET BULB 18 S12 966 022 022 3 11 MEHINC» r.cT ""1 "NO. HB 1/10 CARD TtPE DEPTH Iml I -c s •/.. SIGMA-T SPECIFIC VOLUME ANOMALI-IIO' SAD DVN. M. X 10" SOUND VELOCITY Oi ml/1 PO*-P va-o>/i rOTAl-P „9 • ot/l NOi-N PS - ol/l NOj-N >g - ol/l SI04-Si MS - ol/l PH S c c STD 0000 ] 0084 2993 2401 0039112 0000 14461 800 092 OBS STD 0000 0084 29930 2401 0010 -0005 3177 2553 0024623 14461 800 060 0032 14447 840 080 002 000 005 092 OBS STD 0010 -0005 31773 2553 0020 -0056 3252 2616 0018669 14447 840 070 0054 14431 778 095 004 001 007 092 OBS STD 0023 -0082 32682 2629 0030 -0115 3278 2638 0016514 14427 764 077 0071 14414 753 091 008 018 007 092 OBS STD 0047 -0164 32965 2655 0050 -016* 3299 2656 0014761 14395 727 100 0102 14397 722 115 005 061 010 092 OBS STD 0070 -0161 33127 2667 0075 -0160 3316 2570 0013445 14403 697 112 0138 14405 695 125 004 078 013 092 OBS STD STD 0094 -0156 33273 2679 0100 -0155 3330 2681 0125 -0151 3343 2692 0012366 0011363 14412 587 115 0170 14414 587 0200 14421 683 132 003 086 014 092 OBS STD 0139 -0149 33499 2697 0150 -0140 3356 2702 0010385 14426 677 112 0227 14433 667 125 002 096 014 092 OBS STD STO 0186 -0103 33750 2716 0200 -0070 3383 2721 0250 0022 3405 2735 0008558 0007335 14459 535 111 0274 14477 522 0314 14531 581 120 005 115 015 092 OBS STD 0281 0059 34153 2741 0300 0063 3418 2743 0006597 14555 561 146 0349 14560 552 127 002 136 017 092 OBS STO STD STD T0379 0075 34270 2750 0400 0075 3429 2751 0500 0077 3438 2758 0600 0079 3444 2763 0005855 0005199 0004742 14580 522 125 0411 14584 520 0466 14502 509 0516 14621 499 136 002 158 021 092 OBS T0600 0079 3444« 2763 14621 499 119 129 002 132 024 REFERENCE SHIP CODE LATITUDE 1/10 LONGITUDE "1/10 i| MARSDEN STATION TIME ORIGINATOR'S DEPTH MAX. WAVE WEA- THER CODE CLOUD CODES NODC CIR* coot ID. NO. CRUISE NO. STATION NUMBER BOTTOM OF S'MPL'S NUMBER 10- T MO DAY HR.l/lO DIP. HGT PER SE* lYPi *M 31 549 EV 5O410N 058450W 222 68 08 06 115 1965 LCE 9495 0820 07 14 3 2 X4 7 8 0087 WATER ] WIND BARO- METER Imbl) AIR TEMP. •c VIS. COD NO. OBS. DEPTHS SPECIAL OBSERVATIONS COLOR CODE IRANS. DlR. SPEED 0« fOPCI DRV BULB WET BULB 18 S12 966 039 039 3 12 ""' = NO. HR 1/10 CARD TYPE DEPTH tml T -C s •/.. SIGMA-T SPECIFIC VOLUME ANOMAlt-116' SAD DYN. M, <10> SOUND VELOCITY Ol ml/I PO4-P TOTAL-P NOi-N ug - al/l NOj-N PS ■ ol/l SI O4-S. vo - ol/l pH S C C STD 0000 -0053 2998 2410 0038215 0000 14394 808 ' 116 OBS STD 0000 -0063 29976 2410 0010 0033 3232 2595 0020524 ' 14394 808 064 0029 14472 870 084 004 000 002 115 OBS STD 0010 0033 32318 2595 0020 -0077 3257 2628 0017482 14472 870 055 0048 14428 847 079 002 000 006 115 OBS STD STD 0025 -0117 32812 2641 0030 -0132 3289 2648 0050 -0154 3317 2671 0015522 0013377 14412 832 072 0055 14407 798 0094 14399 708 109 Oil 015 008 116 OBS STD 0051 -0165 33184 2672 0075 -0147 3342 2591 0011485 14399 706 100 0125 14415 708 110 007 069 013 115 OBS STD 0076 -0146 33427 2691 0100 -0123 3352 2706 0010009 14415 703 095 0152 14433 552 114 Oil 078 on 115 OBS STD STD 0101 -0122 33523 2707 0125 -0117 3372 2714 0150 -0112 3382 2722 0009250 0008506 14434 650 111 0176 14442 633 0198 14449 613 124 002 111 014 116 OBS STD 0150 -0112 33818 2722 0200 -0052 3397 2733 0007495 14449 613 118 0238 14483 569 127 003 118 017 116 OBS STD STO T0200 -0052 33974 2733 0250 -0020 3405 2737 0300 0009 3412 2741 0007105 0005725 14483 559 122 0275 14512 549 0309 14535 535 131 002 115 019 116 OBS 0305 0011 34122 2741 14536 534 128 140 002 021 116 OBS STD STD T0398 0029 34240 2750 0400 0030 3424 2750 0500 0055 3433 2755 0005919 0005504 14552 522 120 0373 14552 522 0430 14595 519 131 002 145 021 116 OBS STD STD T0599 0078 34413 2751 0600 0078 3441 2751 0700 0069 3445 2754 0004957 0004555 14520 511 126 0482 14520 511 0530 14533 498 133 000 153 025 11 5 OB S T070( ! 0 357 3« yi 5C 2- 5 5 14( >33 497 130 139 002 155 029 82 664 ION 059100W 222" MESSINGI HR I/IO 137 137 137 137 137 137 137 137 137 137 137 STO OBS STD STD OBS STD STD OBS STD OBS STD OBS STD STD OBS STD OBS STD STO OBS STD OBS STD STD OBS STD STO OBS STD OBS DEPTH (in) 0000 0000 0010 0020 0025 0030 0050 0052 0075 0077 0100 0102 0125 0150 0152 0200 T0203 0250 0300 0304 0400 T0404 0500 0600 T0605 0700 0800 TOSOq 0900 T0910 69 STATION TIME (GMTl 08 06 COLOR CODE T t -0002 -0002 0042 0087 0113 0079 -0057 -0068 -0150 -0152 -0111 -0107 -0040 0013 0016 0054 0056 0O62 0069 0069 0058 0058 0064 0070 0070 0059 0048 0047 0047 0047 137 s •/„ 3003 30033 3088 3162 32019 3229 3325 33310 3342 33436 3358 33592 3373 3386 33865 3405 34058 3417 3425 34260 3434 34346 3440 3446 34460 3447 3447 34473 3447 34459 sriEO 01 foicf S20 BARO- METER 956 2413 2413 2479 2536 2567 2590 2674 2579 2591 2592 2703 2704 2712 2720 2720 2733 2734 2742 2748 2749 2755 2757 2761 2765 2755 2757 2767 2758 2757 2767 9495 DRY BULB 022 DEPTH TO BOTTOM 0928 0037968 0031553 0026214 0021055 0013099 0011476 0010355 0009477 0008740 NO. OBS. DEPTHS 12 0006664 0006103 0004952 0004574 0004410 0004330 0000 0035 0054 0087 0122 0152 0180 0204 0227 MAX. DEPTH OF S'MPL'S 09 WEA- THER CODE SPECIAL OBSERVATIONS 0007524 0268 0303 0335 0005362 0392 0444 0492 0537 0580 0004327 0624 14423 14423 14457 14489 14507 14496 14451 14447 14414 14413 14438 14441 14478 14508 14510 14537 14539 14551 14563 14564 14577 14577 14596 14517 14518 14629 14540 14542 14657 14658 NOOC STATION NUMBER 0088 02 ml/I 799 799 814 830 839 819 745 74 0 712 710 592 591 679 660 558 601 598 563 536 534 513 512 512 512 512 500 488 487 489 490 053 078 124 123 125 128 085 002 000 007 058 Oil 000 003 107 Oil 050 007 098 016 083 009 101 009 098 009 110 005 115 Oil 121 004 131 014 131 003 155 021 137 001 156 024 140 001 151 027 135 001 158 034 139 000 160 035 31 SHIP CODE LATITUDE ' l/IO EV 66410N I 059340W ';?ir'ic«j CARD STD 154 OBS STD STD 154 OBS STD STD 154 OBS 154 OBS STD 154 OBS STD STD 154 OBS STD 154 OBS STD STD 154 OBS STD 154 OBS 154 OBS STD STD 154 OBS STD STD 154 OBS STD 154 OBS DEPTH 1ml 0000 0000 0010 0020 0025 0030 0050 0050 0074 0075 0099 0100 0125 0148 0150 T0198 0200 0250 0296 0300 T0345 T0394 0400 0500 T0594 0600 0700 T0795 0800 0814 222 08 06 T •C -0009 -0009 -0073 -0120 -0138 -0145 -0164 -0164 -0151 -0151 -0165 -0164 -0145 -0129 -0126 -0028 -0020 0159 0274 0285 0343 0262 0254 0138 0070 0059 0059 0058 0058 0059 154 SPEED 0« '01ICE S12 3039 30387 3160 3247 32782 3285 3308 33077 33255 3326 33430 3344 3357 33681 3360 33809 3391 3422 34408 3441 34517 3451 3445 34426 3443 3443 34433 3444 34441 ORIGINATOR'S 2442 2442 2542 2613 2639 2645 2664 2654 2678 2578 2692 2693 2703 2711 2712 2725 2726 2740 2746 2745 2756 2755 2761 2752 2753 2763 2764 2764 2764 9497 0836 022 017 0035229 DEPTH TO BOTTOW 13 SAD DTN. M. » 10= 0000 0025705 0030 0018885 0053 0015893 0070 0014091 0100 0012675 0134 0011268 0154 0010305 0190 0009436 0215 0008181 0259 0006953 0297 0005597 0331 0005624 0005055 0004803 0004707 0392 0445 0495 0542 0004571 0589 DEPTH OF S'MPL-S 17 SOUND VELOCITY 14425 14425 14413 14405 14402 14400 14398 14398 14406 14406 14411 14411 14425 14439 14441 14498 14502 14595 14555 14551 14558 14565 14531 14515 14515 14528 14644 14545 14647 WEA- THER CODE 03 ml/l 812 812 820 827 831 805 729 729 598 699 713 712 679 657 656 533 532 611 597 597 589 556 564 535 516 516 509 503 504 507 NOj-K 065 089 088 110 099 115 112 121 NOj-N wg - ot/l NODC STATION NUMBER 0089 002 013 001 001 115 120 110 121 003 005 109 121 117 121 001 002 129 134 123 134 001 002 000 006 029 009 053 Oil 084 015 095 109 013 087 013 092 014 121 013 105 113 002 133 013 146 013 138 015 125 134 000 155 025 163 030 159 031 83 REFERENCE SHIP CODE LATITUDE I/IO LONGITUDE ■1/10 s° MARSO£N STATION TIME ORIGINATOR'S DEPTH MAX. DEPTH OF S-MPL- WAVE WEA- THER CODE CLOUD CODES NODC CIRt CODl ID. NO. CRUISE NO. STATION NUMBER BOTTOM NUMBER 10* ! r MO DAV HR.1/10 0\BL iHCTlPEHl i A Tin AM 31 549 EV 6641 N 06000 W 223 160 1 38 06 175 1965 LCE 9498 0640 06 18 iH XI 4 1 0090 WATER WIND BAftO. MtlER AIR TEMP. •c ^"■dEs SPECIAL OBSERVATIONS COLOR CODt TitANS. LmJ OIR, fOtCt DRY BULB WET BULB 18 SIO 990 028 022 8 11 MtSSENGi ! r.jT "»' ". NO. HR )/10 CARD TYPE DEPTH 1ml T X s ■''.. SIGMA-T specific VOLUME ANOMAl»-»IO' SAD OYN. M. X 10= SOUND VELOCITY 03 ml/I P04-^ VB-ot/l lOTAL-f ug . «i/l NOj-N vB - oi/l NO3-N VB . 01/1 SI 04-Si vg - ol/l pH S C c STD 0000 0009 3053 2*52 0034200 0000 14435 823 ' 175 OBS STD STD 0000 0009 30530 2452 OCIO -0075 3182 2559 0020 -0133 3268 2631 0024012 0017239 14435 823 067 0029 14416 791 0050 14402 766 086 001 000 006 175 OBS STD 0022 -0142 32796 2640 0030 -0156 3285 2645 0015869 14400 762 097 0066 14395 753 120 024 045 010 175 OBS STD 0044 -0170 32927 2651 0050 -0170 3293 2652 0015208 14392 739 107 0097 14393 734 124 005 061 on 175 OBS STD 0065 -0169 32991 2657 0075 -0167 3309 2665 0013965 14397 720 105 0134 14401 709 121 001 074 012 175 OBS STD STD 0088 -0164 33201 2674 0100 -0159 3327 2679 0125 -0147 3341 2690 0012587 0011528 14406 696 107 0167 14412 678 0197 14423 655 118 002 079 014 175 OBS STD 0130 -0145 33441 2693 0150 0019 3354 2694 00112O5 14425 654 117 0226 14506 653 131 003 104 016 175 OBS STD STD T0172 0139 33641 2695 0200 0100 3376 2707 0250 0031 3398 2729 0010012 0007917 14565 666 107 0279 14554 646 0323 14534 618 121 003 097 013 175 OBS STD T0255 0024 34003 2731 0300 0184 3428 2743 0006710 14532 515 113 0350 14615 505 123 004 127 014 175 OBS STD T0336 0259 34425 2748 0400 0152 3440 2755 0005588 14556 593 108 0422 14619 549 110 002 124 013 175 OBS STD STD T0488 0065 34383 2759 0500 0065 3439 2760 0600 0067 3441 2761 0005069 0004897 14595 514 106 0475 14597 514 0525 14615 516 115 001 152 023 175 OBS T0628 0068 3441<; 2762 14620 517 218 270 026 154 039 STATION TIME DAY HR,1/1I ORIGINATOR'S WEA- THER CODE NOOC STATION NUMBER 06025 W 223 60 08 06 195 1965 LCE 9499 0525 05 18 2 2 XI 3 |2 0091 S18 BARO- METER Imbtl AlH TEMP. *C T X SIGM SOUND VELOCITY Ol ml/I NO3-N UB - ol/l NOj-N VB - 01/1 SIO*-Si 195 195 195 195 195 195 195 195 195 84 STD OBS STD STD OBS STD STD OBS STD OBS STD OBS STD STD OBS STD OBS STD STD OBS STD OBS STD OBS 0000 0000 0010 0020 0025 0030 0050 0052 0075 0078 0100 0104 0125 0150 T0155 0200 T0205 0250 0300 T0309 0400 T0407 0500 051 1 -0045 -0045 -0081 -0111 -0125 -0134 -0162 -0163 -0160 -0160 -0159 -0159 0025 0128 0133 -0083 -0101 -0061 -0023 -0017 0030 0032 0037 0037 3161 31611 3201 3235 32525 3263 3300 33022 3306 33073 3320 33222 3338 3354 33567 3380 33821 3395 3407 34084 3423 34241 3434 34353 2542 2542 2575 2603 2518 2527 2657 2559 2552 2663 2673 2575 2681 2588 2589 2720 2722 2731 2739 2740 2749 2750 2758 2759 0025719 0022535 0019832 0017613 0014587 0014212 0013122 0012459 0011857 0007567 0006929 0006010 0005219 0000 0024 0045 0064 0096 0132 0167 0199 0229 0008732 0280 0321 0358 0423 0479 14425 14425 14415 14408 14404 1*403 14398 14398 14404 14404 14410 14411 14503 14555 14559 14471 14464 14492 14519 14524 14562 14564 14583 14586 853 853 845 830 818 800 739 735 728 726 695 690 668 645 541 611 607 575 550 545 525 524 514 513 055 095 094 111 113 001 000 004 013 025 009 131 Oil 066 013 118 009 079 012 126 002 089 014 144 004 108 017 127 002 130 018 176 004 145 022 152 004 154 023 172 005 157 026 REF RtNCE - SHIP CODE LONGITUDE •i/io n MARSDEN STATION 1ME TEAR ORIGINATOR'S DEPTH TO BOTTOW MAI DEPT OF S'MPL WAV( WEA THER - COD CLOUD CODE 1 CODE NO. 1/10 10* -r-p- MO DAY HR.V10 CSUIS NO. STATION NUMBER ^ OBSERVATIONS STATION 31 549 EV 6641 N 06052 W 223 60 08 06 n — '- 216 1965 LCE 9500 0421 04 18 V K XI 3 3 0092 =c°o'-o°e" "t:' ""■ SPtiD 0» FOUC 8AR0. *"• ' METER DRY tmbil BULB WET BULB „,. NO. CODE 0»5. "°' DEPTHS SPECIAL OBSERVATIONS 1 |20 524 983 1 022 017 8 |08 MEHINC« CAST •"'* » NO. HR 1/10 CARD TYPE DEPTH (m) I ic s ■''.. SIGMA-T SPECIFIC VOLUME ANOMALT-IIO' IAD DVN. M X 10^ SOUND VELOCITT Oj ml/ PO<-P IOTAl_f Vfl - ol/l NOj-N we - oi/i NOj-N VS - OI/I SIO4-S VB - ot/ pH 1 C C STD 1 0000 j -0053 3143 2527 0027073 0000 14419 fl3«^ - iio OBS 0000 -0053 31431 2527 ' 'i4419'his ' riAz. '^o-. '««, ',„ ' ' STD 0010 -0094 3186 2563 0023648 0025 l^^o" 820 '' "" °°' °°* STD 0020 -0126 3222 2593 0020790 0048 14399 803 "^ °f?D roll :'olH IIU" lire 0018587 0067 Hill ]V. ''' ''' -' °" °- 31. oil' iiii ziiti mi itti — ^ -- mil ^33 STD 0075 -0172 3296 2654 0014953 0140 Hill ill "" °^° °'° '-' °IJD ^?0^^ Ztlll IWf \IT. 0013731 0176 ]^ Vol ^ ^^ °- °- 013 STD 0125 -0147 3328 2680 0012524 0209 14421 674 i° "■'• -"" "" '"' "■■"■ •"' 1"" "S ■" '" "" •" "• '" ° J s :;;;; ?«f i;;t ...,„, ,„. i::i; j=; ■" - »" ... •" STD 0250 -0058 3394 2730 0007757 0333 14493 573 2 °pD 'im -zii \:iT \]ii 0006816 0370 j:^?: hi -^ -^ «- >- °" 216 OBS T0388 0015 341,2 2747 145» 522 133 142 004 153 023 SHIP CODE LATITUDE I/IO LONGITUDE ■i/io 1 MARSDEN STATION TIME | YEAH ^ ORIGINATOR'S 1 DEPTH TO OTTOM MAX. DEPTH OF WAVE OBSERVATIONS WEA- THER CODE CLOUD CODES NOOC STATION CODE NO. 10' <■ WO 1 AY H Ll/lO RUISE NO. STATION NUMBER 31 549 EV 6256 N 05711 W ?22 21 C 8 0 8 1 85 1 965 I -CE 9501 2261 22 35 2 2 X8 5 fl r WATER WIND BARO- METER iTlbi) AIR TEMP. X 1 VIS. ODE NO. OBS. 3EPTHS SPECIAL OBSERVATIONS ' \ V^ J J \ :OLOR CODE TItANL U,K SPEED OR FORCE DRY BULB WET BULB r^ ' . 1 31 SIO 054 128 111 3 18 '=;s-ic- CARD TYPE DEPTH Im) I ic s */.. SIGMA-T * tClfIC VOLUME SAD DYN. M. SOUND PO«-P IOTAL-p| NOj-N NOj-N SIO4 S< s X 10' VELOCITY VB ■ o./l B - oi/l ue - oi/i PS - ol/l Vi • ol/l pH c STD 0000 I 0782 3398 |2652 Ic (015229 0000 14R09 ft7? - °l?n nn?S °^" "'■'^ ^"^ 14809 '672 ' III ll\. "■''* 3403 2563 0014202 0015 14793 680 r.11 r}° °*** 3*1° ^*"'5 0013050 0028 14776 688 ^?r. ^n'* ""^ "*1^* ^'»^ I'-^fi* 693 STD 0030 0523 3424 2594 0011236 0040 14755 686 «= "^' 3453 2730 0007864 0050 14720 664 ^rn ^r' °"* '*"* ^^33 1471, ^63 ^»'. n«I ^Z °"' 3472 2745 0006515 0078 14728 663 c?,^ ^ZS ""* 34740 2746 14729 663 rl °° °^1^ 3479 2751 0005933 0093 14730 651 185 OBS 0103 0514 34802 2752 14730 550 STD 0125 0520 3486 2756 0005498 0107 14737 553 1«.i r.lV IW ""^ 3490 2759 0005288 0121 14744 657 OBS 0156 0526 34911 2760 14745 658 1«5 rXl Tn^o^ ^"' ""* "*1 0005123 0147 14755 532 185 OBS T0209 0532 34948 2762 14757 629 STD 0250 0521 3495 2763 0005030 0172 14759 534 IB.; rX\° ll°° °^°^ 3494 2764 0004968 0197 14762 540 It. n'nn °'" ^'""'° '"'*'' 1*7" 641 J °''*3 3493 2765 0004873 0247 14768 630 OBS T0419 0478 34925 2765 ,4759 528 STD 0500 0461 3492 2768 0004772 0295 14776 527 r.V^ °^°° "**! 3492 2770 0004659 0342 14784 626 cr. 2^" °*35 34921 2771 14786 625 STD 0700 0422 3492 2772 0004545 0388 14793 523 STD 0800 0405 3492 2774 0004442 0433 14802 620 185 DBS 0851 0397 34921 2775 14807 519 STD 0900 0392 3492 2775 0004399 0477 14813 520 .f^" '°°° °"3 3492 2775 0004395 0521 14825 623 185 OBS 1071 34913 ^25 STO 1100 0373 3491 2777 0004389 0565 14839 628 r.V° ]^°° °'*' 3491 2778 0004356 0509 14851 640 199 OBS T1252 0358 34913 2778 ,4858 l.f, 185 OBS 1277 0360 34914 2778 \IHI ^2^ 11^ ] ?.?. "^° 3492 2779 0004349 0552 14867 628 STD 1400 0355 3492 2779 0004381 0695 14882 623 „f °^^^ 3493 2780 0004337 0739 ,4897 619 199 OBS 1559 0348 34931 2781 ,4906 5 6 r.1 "° °"^ 3493 2782 0004250 0847 14931 630 OBS T1643 0322 34934 2783 14943 635 STD 2000 0303 3493 2785 0004044 0950 14951 615 199 OBS T2031 0296 34933 2786 , *g64 'l4 C >BS 2219 023 7 3 492 5 2790 1497 0 6 37 85 REFERENCE SHIP CODE LATITUDE 1/10 LONGITUDE * '1/10 MARSOEN STATION TIME ORIGINATOR'S DEPTH MAX. DEPTH OE S'MPL- WAVE WEA- THER CODE CLOUD CODES NODC CUT CODf 10. NO. SQUARE (GMTt YEAR CRUISE NO. STATION NUMBER TO BOTTOM OBStKVHiiun] STATION 10' r M0~] DAY HR.1/10 01". HGI fl» SEA TYPi AM 31 5*9 EV 5200 N 05610 W 222 26 08 09 023 1965 LCE 9502 2651 26 29 1 2 XI 4 T7 0094 WATER WIND BARO- METER (mb*) AIR TEMP. •c VIS. COO NO. OBS. DEPTHS SPECIAL OBSERVATIONS COLOR CODE TfcANS. DIR. OR FORCt DRY euLB WET BULB 34 S12 075 094 078 8~ 18 MtSSENCR 1 CAST ""1 • NO. H« I/IO CARD TYPE DEPTH (ml I -c s •/.. SIGMA-T SPECIFIC VOLUME *NOMALY-mo' SAO DYN. M. > 10= SOUND VELOCITY 01 ml/1 PO4-P lOTAL-r vg - ol/l NO3-N ug - 01/1 NOj-N l>g - 01/1 sio^-s. UB - 01/1 PH C C STD 0000 0779 3377 2636 0016758 0000 14805 532 ' 039' OBS 0000 ' 0779 '33767 2636 14805 532 STD 0010 0506 3388 2568 0013693 0015 14740 582 STD 0020 0476 S^Ol 2594 0011258 0028 14590 711 039 OBS 0028 0403 34117 2710 14663 720 STD 0030 0398 3415 2714 0009344 0038 14661 712 STD 0050 0368 3449 2744 0006588 0054 14655 554 039 OBS 0057 0356 34555 2750 14558 541 STD 0075 0395 3455 2753 0006571 0059 14574 535 039 OBS 0085 0407 34590 2755 14681 531 STD 0100 0417 3472 2757 0005393 0083 14588 524 0 39 OBS 0112 0424 34747 2758 14594 521 STD 0125 0432 3477 2759 0005199 0096 14700 526 STD 0150 0444 3480 2760 0005129 0109 14709 533 039 OBS 0158 0452 34826 2751 14715 535 STD 0200 0452 3485 2752 0005005 0135 14725 632 0 39 OBS T0222 0455 34857 2753 14731 631 STD 0250 0463 3467 2754 0004922 0159 14734 534 STD 0300 0458 3487 2754 0004921 0184 14741 541 0 39 OBS 0337 0454 34875 2755 14745 545 STD 0400 0445 3488 2755 0004807 0233 14752 505 0 39 OBS 0450 34889 584 STD 0500 0432 3489 2769 0004689 0280 14753 587 STD 0500 0419 3489 2770 0004641 0327 14774 599 039 OBS 0575 0411 34891 2771 14783 612 STD 0700 0409 3489 2771 0004501 0373 14787 523 STD 0800 0399 3490 2773 0004505 0419 14799 556 0 39 OBS 0899 34912 573 STD 0900 0390 3491 2775 0004440 0453 14812 573 STD 1000 0382 3491 2775 0004435 0508 14825 562 STD 1100 0374 3491 2775 0004425 0552 14839 554 039 OBS T1150 0371 34907 2775 14845 650 STD 1200 0357 3491 2777 0004448 0595 14853 649 STD 1300 0361 3491 2777 0004450 0641 14867 544 039 OBS T1347 0359 34908 2778 14874 641 STD 1400 0358 3491 2778 0004479 0685 14883 633 STD 1500 0356 3492 2779 0004451 0730 14899 523 023 OBS T1531 0355 34924 2779 14904 522 STD 1750 0345 3493 2781 0004455 0842 14937 539 023 OBS 1789 0343 34932 2781 14942 542 023 OBS T1957 0325 34935 2783 14965 632 STD 2000 0322 3494 2783 0004283 0951 14969 627 023 OBS 2218 0294 34936 2786 14995 611 STD 2500 0245 3493 2790 0003593 1148 15023 630 023 OBS T2566 0233 34925 2791 15028 641 86 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 cur 10. NO. SQUARE (GMIl YEAR CRUISE NO. STATION NUMBER TO BOTTOM OBStHVAIIUN> STATION NUMBER COD£ 10* r MO DAY HRJ/IO DIR. HCI PER St* IT« AM 31 5*9 EV 6104 N 05534 H 222 15 08 09 115 1965 LCE 9503 2987 28 35 1 X X2 4 8 0095 WATER WIND BARO- METER (mbtl AIR TEMP. •c VIS. coo NO. OBS. DEPTHS SPECIAL OBSERVATIONS COLOR CODE IRAN 5. 01R. 5fM0 0» fORCt DRY BULB WET BULB |35 S12 095 097 086 8~ 19 HR I/IO CARD TYPE DEPTH Im) T *C s v.. S1GMA-T tPtClMC VOLUME ANOMALI-IIO' SAD DYN. M. I loi SOUND VELOCITY Ol m1/l PO*-P V0 - 01/1 roiAL-r vfl ■ al/l NOi-N vg - oi/l NOj-N ttg - oi/l Sl04-Si MS - 81/1 pH s c c STD 0000 0804 3408 2657 0014755 0000 14819 560 128 OBS 0000 ■ 0804 34083 2657 14819 ' 660 STD 0010 0803 3412 2660 0014498 0015 14821 660 STD 0020 0802 3415 2663 0014245 0029 14822 660 128 OBS 0025 0801 34173 2564 14823 660 STD 0030 0724 3428 2684 0012238 0042 14795 558 STD 0050 0471 3458 2748 0005210 0051 14702 547 128 OBS 0052 0458 34706 2751 14597 646 STD 0075 0484 3483 2758 0005255 0075 14714 637 128 OBS 0077 0485 34832 2758 14714 636 STD 0100 0487 3485 2759 0005166 0088 14719 638 128 OBS 0102 0487 34856 2760 14720 638 STD 0125 0493 3488 2751 0005039 0101 14726 638 STD 0150 0499 3489 2751 0005055 0113 14733 537 139 OBS 0153 0500 34895 2751 14734 537 STD 0200 0483 3489 2753 0004941 0138 14735 535 139 OBS 0204 0482 34885 2753 14735 536 STD 0250 0474 3488 2763 0004971 0163 14739 634 STD 0300 0462 3488 2755 0004891 0188 14742 632 128 OBS T0305 0461 34876 2754 14743 632 STD 0400 0430 3487 2758 0004583 0236 14745 533 139 OBS 0405 0429 34874 2768 14746 633 STD 0500 0407 3487 2770 0004571 0282 14752 534 STD 0600 0391 3485 2771 0004540 0328 14752 535 139 OBS T0605 0390 34861 2771 14753 635 STD 0700 0385 3488 2773 0004423 0372 14776 533 STD 0800 0379 3489 2774 0004370 0415 14791 631 139 OBS 0810 0378 34894 2775 14792 531 STD 0900 0370 3489 2775 0004331 0460 14804 533 STD 1000 0364 3489 2776 0004354 0503 14818 535 139 OBS T1037 0362 34892 2775 14823 536 STD 1100 0362 3490 2775 0004392 0547 14834 634 STD 1200 0361 3490 2777 0004419 0591 14850 531 139 OBS T1241 0350 34903 2777 14857 530 STD 1300 0358 3491 2778 0004398 0535 14866 628 115 OBS 1365 0357 34924 2779 14877 526 STD 1400 0357 3493 2780 0004320 0579 14882 623 STD 1500 0355 3493 2780 0004388 0722 14899 517 115 OBS 1560 0354 34935 2780 14908 615 STD 1750 03*4 3494 2781 0004385 0832 14936 518 115 OBS 1851 0335 34935 27R2 14950 619 STD 2000 0322 3494 2783 0004283 0940 14969 515 115 OBS T2C47 0317 34934 2784 14975 614 STD 2500 0276 3493 2787 0004010 1148 15035 519 115 OBS 2545 0269 34925 2787 15040 521 115 OBS T2844 0204 34908 2792 15064 536 87 REFERENCE . MARSDEN STATION TIME ORIGINATOR'S DEPTH MAX. DEPTH WAVE OBSERVAHONS WEA- CLOUD COOES NODC CtIT CODf 10. NO. SHIP coot LATITUDE I/IO LONGITUDE ■ "1/10 ii SQUARE (GMTI YEAR CRUISE NO. STATION NUMBER TO BOTTOM OF S-MPL- THER CODE STATION NUMBER 10* r MOl DAY H R.l/10 oin Hci nt JE* It« *MT 31 5*9 EV 6008 N 0S«*3 M 222 04 38 09 207 1965 LCE 9504 319* 32 28 3 2 XI 8 6 0096 WATER WIND BARC AIR TEMP. :^ 1 NO. COLOR CODE TRANS. OIR, srEto lOKCt METER (mbll DRY BULB WET BULB "°jo?p'^s OBSERVATIONS 28 SOT 119 100 083 8 |18 M(H(NC«lcAST CARD TYPE DEPTH Iml T -C s v.. SIGMA-I iPIClfiC VOLUME ANOMAH-X10' SAD DYN. M. X 10' SOUND VELOCITY Oj ml/l POi-P vg - ol/l lOTAl-r vg ■ oi/l NOj-N US - ol/l NOj-N «B - ot/l MB -Ol/l "" s c c H(t 1/10 ~ ~ STD 0000 0888 342i» 2656 0014823 0000 lttB53 666 ' 218' OBS 0000 0888 3*239 2556 1*853 566 STD 0010 0829 3432 2572 0013370 0014 1*833 666 STD 0020 0763 3440 2688 0011859 0027 1*810 656 218 OBS 0027 0711 34461 2700 1*792 566 STD 0030 0675 3449 2707 0010027 0038 1*779 564 STD 0050 0501 3457 2743 0006514 0054 1*714 550 218 OBS 0053 0485 34587 2747 1*709 649 STD 0075 0454 3479 2758 0005230 0069 14701 542 218 OBS 0080 0450 34805 2760 14700 541 STD 0100 0452 3482 2761 0005005 0082 14704 639 218 OBS 0105 0452 34550 27480 538 STD 0125 04*4 3483 2763 000*877 0094 1*705 639 STD 0150 0435 3484 2764 0004733 0106 1*705 6*0 218 OBS 0160 0432 348*6 2755 14706 641 STD 0200 0422 3485 2757 000*571 0130 1*709 540 218 OBS 0213 0418 34855 2757 14709 540 STD 0250 0404 3484 2768 0004505 0152 14709 545 STD 0300 0391 3483 2768 0004492 0175 14712 652 218 OBS T0315 0388 34826 2758 14713 554 STD 0400 0383 3485 2771 0004350 0219 14725 543 218 OBS 0426 0382 34855 2771 14729 541 STD 0500 0384 3485 2771 0004379 0253 14743 640 STD 0600 0387 3487 2772 0004428 0307 14751 639 218 OBS T0635 0388 34875 2772 1*757 639 STD 0700 0378 3488 2773 0004381 0351 14773 639 STD 0800 0366 3488 2774 0004325 039* 14785 538 218 OBS 0847 0352 34875 2775 14791 638 STD 0900 0351 3488 2775 0004323 0437 1*800 545 STD 1000 0358 3488 2775 0004372 0481 14815 654 218 OBS T1081 0355 34886 2775 14828 655 STD 1100 0355 3489 2776 0004375 0525 14831 653 STD 1200 0353 3489 2775 0004440 0559 14847 543 218 OBS T1273 0352 34884 2775 14858 537 STD 1300 0352 3488 2775 0004520 0614 14863 536 STD 1400 0354 3488 2775 0004524 0559 1*880 531 STD 1500 0355 3488 2776 0004721 0706 1*898 627 207 OBS 1564 0356 348S2 2776 1*909 525 STD 1750 0350 3490 2778 0004727 0824 14938 520 STD 2000 0337 3493 2781 0004559 0940 14975 513 207 OBS T2050 0333 34930 2782 14982 612 STD 2500 0289 3494 2787 0004135 1157 15041 528 207 OBS T2531 0285 34939 2787 15045 529 STD 3000 0215 3491 2791 0003556 1350 15095 537 207 OBS 3008 0214 34906 2791 15095 637 207 OBS 3151 0177 3A907 2 7Q4 15105 6A0 88 RtfdlENCE SHIP CODE LONGITUDE •1/10 1^ MARSDEN STATION T ME ORIGINATOR'S | DEPTH MAX ■ WAVE WEA- THER CODE CLOUD CODES NODC Clit CODf ID. NO. LATITUDE I/IO SQUARE IGMTI YEAR CRUISE STATION TO OF S'MPL'S OBSERVATIONS STATION NUMBER 10* r MO DAY HR.l/lO NO. NUMBER "■-'■•"'" 0I». MCI »[« H* un AM 31 549 EV 5915 N 05355 W 186 93 08 10 050 1965 LCE 9505 3191 28 20 1 2 XI 4 U 0097 WATER WIND BARO- METER tmbll A IB T(MP. "C VIS. coot NO. OBS. DEPTHS SPECIAL OBSERVATIONS COLOR CODE TRANS. DIR. SPEED OR FORCE DRY BULI WET BULB 19 SIO 112 100 086 8~ 18 "'"""" I CAST ""1 =' NO. HR VIO CARD TYPE DEPTH lr>) T -C s v.. SIGMA-T SPECIFIC vOtUME AN0MAEY-11D' SAD DYN. M. XIO^ SOUND VELOCITY 03