A SUMMARY
OF

TEMPERATURE-SALINITY CHARACTERISTICS

ay

OF THE

PERSIAN GULF

GENERAL SERIES

PUBLICATION G.4

The National Oceanographic Data Center is sponsored by government agencies
having an interest in the marine environment; it is governed by an Advisory Board com-
posed of representatives of these activities and the National Academy of Sciences. The
U. S. Naval Oceanographic Office is assigned responsibility for management of the

National Oceanographic Data Center.

The Sponsoring Agencies are:
Atomic Energy Commission
Bureau of Commercial Fisheries
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Coastal Engineering Research Center
Department of the Navy
Geological Survey
Health, Education & Welfare
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Weather Bureau

: Office

ANN

0 0301 o041243 3

NATIONAL OCEANOGRAPHIC DATA CENTER

GENERAL SERIES

A SUMMARY OF TEMPERATURE-SALINITY CHARACTERISTICS
OF THE
PERSIAN GULF

PUBLICATION G-4

1964

For sale by authorized Sales Agents of the U. S. Naval Oceanographic Office, Washington, D.C. 20390

This is a chronological compilation of pertinent analysis, data
and textual material taken from publications (papers)
authored by:

GERHARD SCHOTT (1908) (1918)
BRUNO SHULTZ (1914)

H. BLEGVAD (1944)

K. O. EMERY (1956)

H. DUBACH & T. WEHE (1959)

Assemblage of this material, with an analysis of recent un-
published (post 1950) temperature and salinity data, was by:

HAROLD W. DUBACH

Publications in the NODC General Series:

1. Introduction to the National Oceanographic Data Center, NODC Pub. G-1, 1963
2. Oceanographic Vessels of the World, NODC Pub. G-2, Volume I, 1961,

and Volume Il, 1963
3. Data Report EQUALANT |, NODC Pub. G-3, 1964

PREFACE

In the performance of its prime mission, which is to process and archive oceano-
graphic data and provide these data on request to the scientific community, the Data
Center has found it essential that the data be evaluated before being added to the
archive. In the evaluation process, certain analyses of the data are made; these for-
mulate the basis by which the Data Center oceanographers assess the data quality.
Of course, referral to the analyses contained in contemporary and historical research
papers of recognized scientists serve as a basic evaluation reference point. When such
analytical informetion is assembled, it seems desirable that the Data Center make this
material available in a consolidated package for use by others. This is the first such
document; others will follow at irregular intervals as our processing of station data for
the world oceans proceeds.

ACKNOWLEDGMENTS

The assistance of Mr. William Lyons and Mrs. Wilhelmenia Bowe in pre-
paring the art work, Mr. Albert Bargeski in preparing the data appendixes,
Miss Jacqueline Mothershead for her typing assistance, Mrs. Eugenia Pakulis
for her aid in preparing translations, and Mr. William Myers for his helpful
comments is sincerely appreciated.

vi

TABLE OF CONTENTS

Page
IGTROGUCHOR se Wry ORAS ei nc: Mans 1 et eT RR an TR eh 1
COMM ities SOM tes ee Pei AN iy iho Eien SA Te 1
Sectionyl—LocationsGhartsty sn.) 5. es eee ee 5
Section Il—Schott’s and Schultz's Analyses .................. 15
Section ili BlegvacisrAnalysismgs) |) i ee 29
SectioniV—EmenyissAnalysisn.. 0. 4). anno ee 33
Section V—Dubach’s and Wehe’s Analysis.................... 4]
SectionsVi—RecentsDatayAnalysis.. 441.5... 4.4 9540. ee. 53
Data Appendix
Appendix A— Historical Data (Pre—1950).................... 87
Appendix B— Recent Observations (Post—1950) ............... 103
Bib OGROD pene et eM een ai cane etre es. key LS, trees 221

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Figure Ill-

Figure IV-

Figure V-

Figure VI-

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FIGURES

Location of Surface Observations—Persian Gulf, 1907....................
Location of Surface Observations—Persian Gulf, 1910-11..................
Station Locations—Persian Gulf, Mar.-Apr. 1937 and Feb.-Apr. 1938.........
Station Locations—Persian Gulf, Aug. 1948........................----
Station Locations—Kuwait Harbor, Feb. 1949...........................
Station Locations—Northern Part Persian Gulf, Dec. 1949-Apr. 1950,

Noy i'9 5p Rebs 952 vandyApnodliO 52 0) or oe ce nao. See ne
Station Locations—Northern Part Persian Gulf, Feb.-Mar. 1960..............

Inventory of Bathythermograph Data—Persian Gulf, monthly for each 1° square. .

Persian Gulf—Temperature (°C)—surface, Feb. .........................
Persian Gulf—Temperature (°C)—surface, Mdy .........................

Persian Gulf—Temperature (°C)—surface, Aug. .........................
Persian Gulf—Temperature (°C)—surface, Nov. ....................-....-.
Persian Gulf—Salinity (°/, ,)—surface, Jan., Feb., Mar. ...................
Persian Gulf—Salinity (°/, ,)—surface, Jul., Aug., Sept. ...................

Persian Gulf—Fluctuation of Mean Monthly Air and Water

Temperatures at 29°N, 49°-50°E, 26°N, and 56°-57°E ................

Persian Gulf—Temperature (°F)—surface, Feb., Mar.,

andrAprealaften KO MEmeny) ccs ces cc taoats a cre wearer sy eis Hi a eee a
Persian Gulf—Temperture (°F)—surface, Aug. ..........................
Persian Gulf—Salinity (°/ , .)—surface, Aug. ................-..0..2-0--
Persian Gulf-Temperature (°F) and Salinity (°/ ,,) Sections, Aug..........---
Kuwait Harbor—Temperature (°F)—surface, Feb. ........................
Kuwait Harbor—Temperature (°F)—bottom, Feb. ........................
Kuwait Harbor—Salinity (°/ , ,)—surface, Feb. ...................---.-..
Kuwait Harbor—Salinity (°/, ,)—bottom, Feb. ..........................
Kuwait Harbor—Diurnal Warming Study, 3 Jan. 1949 ...................
Kuwait Harbor—Diurnal Warming Study, 27 Feb. 1949 ...................
Fahihil—Diurnal Warming Study, 21 Mar. 1949 ......................-..

Northern Part, Persian Gulf—Temperature (°C)—

surfacemmeb» NGS 2) Man ali aOw mere ete oe eee es a See F

Northern Part, Persian Gulf—Temperature (°C)—

HOlmetersstFeb: 1952. Mars UGSO se et cae ce os ee aa

Northern Part, Persian Gulf—Temperature (°C)—

20imeterss | Febs. 19:52) (Mar UG SO! eye eee eas ew, sue at Sa.

Northern Part, Persian Gulf—Temperature (°C)—

SOnmeterns, repel Sil hei me oe end ig ce cern pen ange ee ant Ue eg ess

Northern Part, Persian Gulf—Salinity (°/, .)—surface,

[ital ope cS t Xel reall ce) 0 Mean at prem eNeenee cemne ems aN Shore auch src Gace arate rae eee tth ro 17 pare

58

59

Figure VI- 6.

VI- 7.

FIGURES (con’t)

Northern Part, Persian Gulf—Salinity (°/..)—

lO%meterss Feb NOS 25 MarliG5 One se ae ei ne se

Northern Part, Persian Gulf—Salinity (°/..)—

20 meters, Feb. 1952, Mar. 1950 ...................00.

Northern Part, Persian Gulf—Salinity (°/..)—

SO)imeters; Feb: USS 2 eee ee enna eeu anya,

Northern Part, Persian Gulf—Temperature (°C)—

surface; hebv=Mare 19 6O) a sete ne eae ee lian Tse earth

Northern Part, Persian Gulf—Temperature (°C)—

NO%meters; Feb:-Mar: P9GOR ese cr toran sie oo en ees 3 oe

Northern Part, Persian Gulf—Temperature (°C)—

20imeterssiRe bis Marr GOOrs fein ois tae a ie eee ore ee

Northern Part, Persian Gulf—Temperature (°C)—

30metershiFeb = Manral9GO!. <n oes ee ge

Northern Part, Persian Gulf—Salinity (°/..)—

surface, Feb.-Mar. 1960 ...... ee a a Ae

Northern Part, Persian Gulf—Salinity (°/..)—

lOkmeters; Febs-War- li POO ween tee caress ne eye

Northern Part, Persian Gulf—Salinity (° / oo)—

20imeters;Reb:-Mans 960) 2s oie cece Gan San oer

Northern Part, Persian, Gulf—Salinity (° /o0o)—

30iimeters; Febs-Mara sli 2O Ones et ecco ecesae oe eee

Northern Part, Persian Gulf—Temperature (° C)—

SUNFACE, APT OOo en ree aor en pa tee ne Tea) Stel ie a Rae

Northern Part, Persian Gulf—Temperature (°C)—
10 meters, Apr. 1952
Northern Part, Persian Gulf—Temperature (°C)—

2Otimetersi <A pie MO SDs ns coe a ee ceo ese ie tte ee

Northern Part, Persian Gulf—Temperature (°C)—

30%metersApreoM9 52 Ae eo we alge can yar ace a eke ee eRe

Northern Part, Persian Gulf—Salinity (°/..)—

Surface Apie UGS Qi ec ceres te nek ese ee me ene crt tare Hae

Northern Part, Persian Gulf—Salinity (°/..)—

hO\meters sApr G52) oon ee eee en Nene Gh er

Northern Part, Persian Gulf—Salinity (°/..)—

20imetersssAprs UGS 20 cese cx ee RA ieee es nie en

Northern Part, Persian Gulf—Salinity (°/..)—

3O0umeters Apr. NOS 2a ness Sc) Eee Ine cmon crn ae epee

Northern Part, Persian Gulf—Temperature (°C)—

surface; Nove GSI) teks eat ceo. ee eee cn ech cee suche ea

Northern Part, Persian Gulf—Temperature (°C)—

LOcmeterssiNovaliG Si 2 os 8 ee CLS rea oer

Page

Figure VI-27.
VI-28.
VI-29.
VI-30.
VI-31.

VI-32.

FIGURES (con’t)

Northern Part, Persian Gulf—Temperature (°

2OimeterseiINOvanlGSillee ss he Mr ene We os ee ee RL ee Ai SP eh pen OEE oy
Northern Part, Persian Gulf—Temperature (°C)—

BOPMEtEeNsINOV Ml no essttet 9 Ms. ee 2 ENS ee De Oe Cee, A ate Se
Northern Part, Persian Gulf—Salinity (°/..)—

SULLACE HI NOVRI Olle nt mene ti ay <i Nee Dt np teas SERS ope es, 3
Northern Part, Persian Gulf—Salinity (°/..)—

NOWMET ETS GINOVAR Pollitt ve eral tok cee Re EE Ae Ge ee Os eee
Northern Part, Persian Gulf—Salinity (°/.0)—

2OimetersmlNovanll a lies tect es ates ti ee cee inte ake Asa ans
Northern, Part, Persian Gulf—Salinity (°/. 0)—

SOIMEtErSMINOVaNUO OIL eit ce san ro ede ee ae Ty ates

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INTRODUCTION.

Between the covers of this publication are assembled the data
and analyses of all the known temperature and salinity observa-
tions made in the Persian Gulf. Charts previously published have
been reproduced along with each author's comments on the temperature-
salinity regime and its relationship to other environmental factors
as determined by the particular set(s) of observations available
for study at the time.

An analysis of recent temperature-salinity observations (taken
since 1950) has been prepared and is included; charts for each ob-
servation series are presented for the surface, 10-meter, 20-meter,
and 30-meter levels. The position or location of observations are
shown in Section I; the appendixes contain the observational data
upon which the analyses are based. The distribution of bathyther-
mograph data by 1° squares has been charted and included in Section
I (Figure I-8). Results of a 1961 survey (NODC Cruise 31865) were
received and the processing completed just before going to press.
These are included in order that this document might be as complete
as possible; analyses for these data are not presented.

COMMENT .

Schott, in his classical treatment of the Gulf, presents four
seasonal temperature distributions and two (winter and summer) for
salinity conditions. From the information and data contained in
References 5 and 6 and Tables 1 and 2, it appears that the summer
salinity chart is based primarily on data collected in the month
of September and may not be totally indicative of the summer ex-
treme. Salinity data for the winter (February) season appears to
be adequate and representative. Temperature data appears to be
plentiful for August as well as other months. Schott's data
summary shows that the absolute temperature maximum for all lati-
tudes in the Gulf occur in August; all areas except one show the
maximum occuring in the ten-day period between the 11th and 2l1st.

Apparently, K. O. Emery was guided by Schott'’s temperature
analysis in planning his 1948 survey; his survey was undertaken
at the very height of the summer season, all the work being con-
ducted between the 15th and 30th of August (NODC Cruise 3150),
Emery’s work alone provides the only collection of oceanographic
stations for the summer months; he also has provided probably
the greatest volume of BI observations covering mid-summer

conditions for the Persian Gulf. Of course, surface samples
(shown on chart) aided Emery in his analyses of surface con-
ditions (Figures IV-1 and IV-2).

Blegvad's work was confined to the winter and early-spring
months and was concentrated in the eastern half of the Gulf. Since
his work was done as a supplement to a fishery investigation of the
Persian Gulf funded by the Iranian Government, it may not have been
appropriate for him to sample the temperature-salinity conditions
of the entire Gulf area. Apparently, no analysis was ever attempted
by Blegvads only a table of observations is shown in his work (Ref-
erence 1, Table dt) emken On Emery prepared the analysis shown in
Figure III-1; it is based on a composite of Schott's and Blegvad's
data.

The study by Dubach and Wehe (Reference 2) covers a very limited
area (Kuwait Harbor) and a short time interval; however, it probably
supplies a good indication of mid-winter inshore conditions.

The more recent surveys conducted in the decade 1950-59
obviously were not intended to provide information to improve the
past understanding of the temperature-salinity characteristics
and their interrelationship with other environmental features for
the entire Gulf area. The 1951-52 (NODC Cruises 31505 and 31496)
data provides material for appraising the variation in temperature-
salinity features in the northern part of the Gulf along two lines
of observations extending from Iran to the Arabian Peninsula. The
arrangement of observations for March 1950 (NODC Cruise 31382)
leaves something to be desired; the two station lines oriented .
SE-NE show the influence of the outflow of Shatt al Arab. It
would be interesting, indeed, to examine other environmental data
including stream flow rates, rainfall, wind, etc. for the same
period and to relate these to the conditions observed in the Gulf.
The reason for the arrangement of the remaining stations is not
known; it appears most haphazard.

The design of the February-March 1960 survey (NODC Cruise
31658) is systematic and provides a good pattern of data. Both
the surface temperature and surface salinity patterns indicate
a very weak outflow (almost unnoticeable effect) of Shatt al
Arab; this makes for an interesting comparison with the March
observations of a decade earlier. Again, it is highly probable
that meteorological conditions for the Gulf and its surrounding
area were influential in establishing the recorded temperature-
salinity conditions. (In all post 1950 analyses, dashed and dotted
lines are used for intermediate intervals and/or extrapolative
analysis.)

In the early analysis by Schott and Emery, the isolines for
both surface temperature and salinity generally parallel the long

axis of the Gulf, a condition which is most pronounced in the summer
months. The more recent data, available only for the northern por-
tion of the Gulf, produces a more east-west orientation of isolines;
this is particularly apparent in the February-March 1960 surface-
temperature and salinity analysis (Figures VI-9 through VI-16). It
is not truly clear whether this geographic stratification within
the Persian Gulf is indicative of a seasonal change, a long-term
(decade) change, or a bias occuring in sampling the area.

This review of the existing information for the Persian Gulf,
I believe, emphasizes the need to develop adequate data sampling
patterns. This and several other gulfs and lakes of the world of-
fer excellent model areas in which to conduct full-scale studies
in a “natural environmental laboratory."

Certainly, a better understanding of some of the air-sea rela-
tionships can be obtained by instrumenting such bodies of water for
special studies; perhaps, initially, some more definitive values
for energy transfer between air and sea can be derived by using
"nodel-scale bodies of water" located at different latitudes. Other
microstructure studies might be conducted simultaneously as well.
Following are some comparative areal figures for gulfs and lakes
that might serve as models:

WATER BODY AREA*
(approximate)

Pencaeird Gillen aeteetlelts! ells) leis EOS COO SG. amides
Great Lakes (total). ...... 94,700 sq. miles
Guilt of Sto Mewrence 2 2... . Qil,S800) sq. miles
Guike Ge Cailkiomule 2 5 5 5 6 6 6 G2HE00 ieig imilles
Baie S82 5656006666 6 6 IGBQ000 seg miles
MGSO BP 5 5 og obo 6 6 o MVG.E0O Sei, uniles
Wks SUSE, 5 5 og co oo Gl SL GOO Bei, miles

*Source: The World Almanae and Book of Facts,
New York World-Telegram and The Sun,
196}.

The present day availability of improved oceanographic instru-
mentation and numbers of buoys, towers, and other platforms makes
a rigorous study of energy exchange for "model areas" entirely
feasible. Considering that many nations (and activities within
each) have an active interest in oceanographic (marine) studies,
perhaps a joint cooperative-comparative investigation could be
undertaken, with each conducting work in the closest adjacent area;
thus costs would be kept reasonable.

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STATION LOCATIONS
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1951 —1952

Station Locations—Northern Part Persian Gulf, Dec. 1949-Apr. 1950,

Nov. 1951, Feb. 1952, and Apr. 1952

12

STATION LOCATIONS
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FAHAHIL

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Figure I- 7. Station Locations—Northern Part Persian Gulf, Feb.-Mar. 1960

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SECTION II
SCHOTT’S AND SCHULTZ’S ANALYSES

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PERSIAN GULF
FLUCTUATION OF MEAN MONTHLY TEMPERATURES

MONTH
xil l iH] Hl IV Vv Vi Vil Vill IX x xl

== — WATER TEMPERATURE
@@@ AIR TEMPERATURE
29° LATITUDE (N)
49°-50° LONGITUDE (E)
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OOO AIR TEMPERATURE

26° LATITUDE (N)
56°-57°LONGITUDE (E)

Vi Vil Vill IX xl
MONTH
Persian Gulf—Fluctuation of Mean Monthly Air and Water
Temperatures at 29°N, 49°-50°E, and 26°N, 56°-57°E

Figure Il- 7.

23

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The following excerpts (translated from German) are taken from
Reference oy Section III. Ozeanographie, pages 7-9.

"1. Water Temperature. Up to now, only observations of sur-
face water temperature can be evaluated. If we start with winter
(February) . . . we can immediately notice in numerous places the
contrast between the Persian side and the Arabian side of the Gulf.
This contrast is the basis of the essential characteristics of al-
most all natural conditions in the Gulf. Along the Persian coast,
the water in winter at the same latitude is definitely warmer than
along the Arabian coast. The same is also evident, to a varying
extent, for temperatures during the spring and fall months. Only
in mid-summer are all coastal zones heated more, up to 32°C. and
even 33°C., than the central northern part where observations
show 30°C. and less. The distribution of the February isotherms
shows clearly that warm ocean water of over 20°C. penetrates the
Strait of Hormuz and flows to the right (north) toward the Persian
coast, while on the other side, cool water of less than 15°C. from
Shatt al Arab bypasses the Bay of Kuwait and flows south along the
Arabian coast. Thus it happens that at this time off Bahrein the
temperature is approximately 17°C., whereas in the vicinity of
Lingeh, at the same geographic latitude, it is 21°C. to 21.5°C.
Due to these conditions, the spreading of corals and pearls, which
is restricted according to different sources mainly by the northern
border of Cape Abu Ali, most likely depends upon the following:
The cooler and simultaneously less saline water of the northern
part of the Arabian side of the Gulf, which is also apparently
mixed with detrital materials of the Shatt, is unfavorable to
these organisms.

"Compared with the Persian Gulf, the water of the Gulf of
Oman, aS a part of the open ocean, seems to be relatively warm
during all months except for summer and part of fall. In August
when the Southwest Monsoon of the Arabian Sea provides strong
direct cooling and simultaneously also an indirect supply of cold
water from the lower part of the south Arabian coast up to Ras al
Hadd, the Gulf of Oman is considerably cooler than the closed-up,
shallow, and intensively heated water of the Persian Gulf.

"The mean water temperature fluctuations, which were determined
from the February-August differences . .. bring out the afore-
mentioned difference between the two gulfs. A yearly fluctuation
of 15°C. to 17°C. and more in the northwest corner off Kuwait and
Bushire stands in contrast to a fluctuation of 8°C. at Masqat and
only 2°C. to 3°C. at Ras al Hadd to the southeast. The modifying
effect of the ocean water can still be recognized westward of the
Strait of Hormuz by other factors, especially the configuration of
the 10°C. amplitude isoline.

24

"Although in Table 2, showing the data for 1° longitudinal
sections running from north to south, the differences between the
Arabian side and Persian side are eliminated, one can observe the
following facts about the yearly course: Accordingly, in both
gulfs the lowest temperatures occur in February, while in the
Persian Gulf and in the Strait of Hormuz, the highest occur in
August. This warming is thus in agreement with the general warm-
ing applicable to greater water surfaces. A different situation
presents itself in the Gulf of Oman where in the northwestern
part (the section between 57° to 58°E.) the maximum of 31.0°C.
is reached in July, while in other sections located farther to
the east maximums of 29.8°C. and 28.7°C. are attained in June;
the most easterly section has, in addition, a secondary maximum
of 28.1°C. in October, while the secondary minimum (27.6°C.)
occurs in September. This is analogous to the typical Indian
Ocean conditions: May and June are the warmest months in the
western Indian Ocean, constituting a transitional period between
the two monsoons. Then, with the rainy stormy Southwest Monsoon
eomes a cooling over the northern Arabian sea. The effect of this
eooling period ends only in October when this wind diminishes. Air
temperatures follow similar patterns.

"Noteworthy are the combined absolute extremes of water tem-
perature shown at the bottom of Table 2. The maximums definitely
exceed 31°C., are up to 33.0.) inlitherGule of Oman, up to gh? ©... aia
the Strait of Hormuz, and even up to 36.0°C. in the Persian Gulf.
This unusually high water temperature has been observed halfway
between Lingeh and Bahrein about 25 sea miles off the Persian
coast in mid-August at 4 p.m.! ‘The absolute minimum observed up
to now in mid-January not far from the mouth of the Schatt was
1223" Ga

"2. Salinity (Table 1). In two earlier reports prepared by
Schott (Reference 5) and Schulz (Reference Ty it was shown on the
basis of recent salinity observations that in the Persian Gulf the
surface water along the northern half of the Persian coast reaches
and exceeds 0% salinity and that there is a noticeable fluctua-
tion of salinity during the year, so that a minimum occurs in early
summer and a maximum in late fall and winter. Inasmuch as the col-
lection of surface water samples is now more abundant, one can see
the actual conditions more clearly. Throughout the entire year,
there is an area in the Persian Gulf where the salinity exceeds
40% reaching its greatest expansion in winter between the islands
west of Lingeh and almost touching the Qatar Peninsula, and up to
the northeast corner of the Gulf north of Bushire where salinities
up to hO.5% have been observed. This area shrinks during spring
and early summer to such an extent that in May and June the 4O .0foo
isohaline encloses only a narrow strip off Bushire in the direction
of the Shatt, approximately where the 40.5% isohaline lies in
February. The late-summer and fall months seem to be in agreement

25

with the yearly average. The 40.0% isohaline then extends approx-
imately from Cape Naband northward to the delta of the Shatt.

"Such a high salinity concentration in the Persian Gulf depends,
like in the Red Sea, upon the very high air temperatures and great
evaporation of water and upon the extremely small supply of fresh
water runoff. Considering this last point, one might naturally as-
sume that the highest salinity could be expected along the Arabian
coast in the deep bays of the Pirate Coast where no rivers reach
the sea, while along the Persian coast there are a few small rivers
that flow into the Gulf and besides, the Persian side ... receives
quite an amount of rain, at least more than the Arabian side does.
However, these two factors are not decisive. Decisive is the flow
received from the sole large stream system, the Euphrates and Tigris,
whose quantities of fresh water due to the influence of the earth's
rotation (Coriolos Force. Ed.), flow exclusively southward along
the Arabian coast (are deflected to the right. Ed.), as might al-
ready have been guessed from the isotherms of the surface waters . .
The runoff from the Shatt al Arab affects the constantly present
strong pressure of the isohalines toward the east from the mouth,
where the salinity is about 40%, while 35% and even 30% appear
halfway between Fao and Kuwait Bay. The isohalines here, like the
isotherms, run from north to south instead of from west to east.

"With these facts in mind the yearly fluctuations, especially
the freshening of the Gulf water in spring and early summer (May-
June), can be explained. In contrast to the Nile, which has its
high flood in October and its low-water stand in April-May, the
Euphrates and Tigris taken together show their greatest runoff in
April at Hit and Baghdad resulting from the melting of snow in the
Armenian mountains. Both combined carry approximately 5,700 cubic
meters of water per second. In August flow has decreased, and in
October the combined flow of both streams returns to a minimum of
700 cubie meters. If we consider that the stream flow takes sev-
eral weeks after passing Baghdad until it reaches the Gulf, the
minimum salinity of the months May-June seems to fit pretty well
into the picture. Without the Euphrates and Tigris runoff, we
could analogously expect the salinity in the Persian Gulf area
not affected by the Indian Ocean, that is, approximately west
from Lingeh, to be the same as in the northern Red Sea (89.5%)
However in August-September, that is, during the period between
extremes, the 39.5% isohaline runs exactly in the middle or along
the longitudinal axis of the Gulf from NW to SH, and the area in
which there is a noticeable general decrease of salinity, due to
the dispersion of the Shatt water, can be estimated to occupy a
little less than half of the Persian Gulf, that is, about 100,000
square kilometers,

"Tt should be kept in mind that in this area, which borders
and is influenced by the Arabian Sea, salinities can be considered

26

high, at values of 38205 when compared with oceanic conditions.
Even the Gulf of Oman only occasionally in its northwestern part
gets over 37%, and at Ras al Hadd the average observed value
should be at most 36 .5 0 and possibly even less, since along the
southern coast of Arabia there is a heterogeneous cold and low-
saline water which usually comes from the depth up to the surface

(Reference G)im alt oe Eo

The following excerpts (translated from German) are taken from
Reference 7, pages 400-401.

"For the Persian Gulf, reliable surface salinity data were
obtained for the first time in 1907 when, during the months of
February and May-June, officers of the Hamburg-American Line col-
lected water samples for titrimetric determination of salinity
(Reference 5). These observations become useful (for analysis)
when complemented by the observations taken in the years 1910 and
1911 because out of the total of 25 water samples, only three
were taken in May and three in October; the remaining samples
were all taken in September (presumably 1910-11. Ed.). The Sep-
tember observations are regularly scattered throughout the area,
so that one can obtain an insight to the salinity distribution
during this month.

"Just as in February and May-June, the salinity in September
increases from east to west, and by following the 39.5% isohaline
which runs approximately from Ras Rekkan (the most northern point
of the Qatar Peninsula) up to Kangan, Persia (now Iran. Ed.), the
Persian Gulf may be divided into a less saline eastern and a more
saline western half. Toward the east, the salinity decreases in
the Strait of Hormuz down to between 38.22% and 37.43%. West of
the 39.5 foo isohaline, however, the salinity increases off Bushire
to 40.90%. Two additional observations of over 0% indicate
that the Persian coast, from approximately 52°E. up to Shatt al
Arab, is bordered by a lens of water of over 40% salinity. This
appears to be true also in February and May-June, and salinities
may be over LO foo throughout the year in the northeastern part of
the Gulf.

"The observed differences in salinities for September and for
February and May-June are considerable. The generally valid assump-
tion that salinity in September is higher than in June, but lower
than in February is evident; thus, September can be considered as
a transitional period between the months of salinity extremes. ‘This
can be seen from the following observations taken at approximately
the same locations in February and June 1907 and in September
TO Mew ay ores ad

27

Longitude September
HS e Remarks

Latitude
1911

miles N. from

Approx. 16 sea
Ras Rekkan

B= ake} Approx. 25 sea
26° 18! miles S.E. from
26° 20! Lingeh

" . . . During February, the month of maximum salinity, the
Apeinaisine (39. Oe ) runs approximately north-south along 54°E. In
May-June, it runs farthest to the west in a northeasterly direction
between 50° and 51°E. In September, it occupies the already des-
eribed position, approximately between 51° and 52°E. This indicates
that the salinity in September has again increased from the summer
minimum which is due, according to Schott's theory, to the high run-

off of the Tigris and Euphrates (Reference 5) ....

28

SECTION Iil
BLEGVAD’S ANALYSIS

29

(Asawz °© *y 4840) “dw pup
“pw ‘gad ‘e2Djins—(4,) ainyosodwia|—yjns upisiag

“L cil e4n61y

WadV— HIYVW— AY NUE:
3D V4uns
(4.) auniveaawal

31

The following excerpts are taken from Reference 1, Section on The
Physical Conditions of the Iranian Gulf, pages 11-12.

"Of the physical conditions of the Iranian Gulf the following
statements may be given here. In spite of the large quantities of
fresh water that are carried into the Gulf through Shatt al Arab
by the rivers Euphrat, Tigris and Karun the salinity is very high,
averaging about ho-hi %. This is undoubtedly due to the very rapid
evaporation from the surface of the sea, particularly in summer,
for during the hot season the temperature of both air and water is
very high. At the Bahrein Islands, for instance, the sea water has
been found to have a temperature of 36.5°C. (A. Mohr). In winter,
however, the temperature is much lower, the average mostly being
15-18°C. in- the open sea. The... temperatures and salinities
measured during the cruise (appear in Appendix A. Ed.) coo 8
salinities being determined by means of the areometer .. .

"In other words the highest salinity, 42.6%, was measured at
the Bahrein Islands, the lowest one, 37.2-37.3% (Stations 47, 51
and 58), in the Strait of Hormuz. Generally speaking the salinity
of the Gulf seems to decrease in an easterly direction: between
the Strait of Hormuz and Bushire it was about 38%, at Bushire about
hO%, and at the island of Kharg about 41%. Even in the estuary at
Bender Shahpur (St. 79) it was found to be 41.2%.

"The lowest temperature of the sea water, 14.9°C., was observed
in the locality last mentioned during a windy and rainy period in
the month of February. In March the temperature of the surface rise
to 18-22°, in April to 23-2)°C.”

Figure III-1 shows surface temperatures for February, March and
April compiled from Blegvad and Schott by K. O. Emery.

32

SECTION IV
EMERY’S ANALYSIS

‘Bay ‘aopjins—(4

°

) auinpiaduay

JINS uvisiag

L

~Aj 240614

isnonv
3D vans
(4.) 3untvazdwal

35

“Bny ‘aopjins—(°° /,) Ayluljpog—jjnd upisieg

‘Z -Al 24nBi4

isnonyv

.. aowauns
(°°7.) AUNITYS

36

SII] |.
CINE

a

hea

A

AIH

Va
Nn

WS

Ne :

| Ve

s/} \\
a

PASS

= 6
af

TS
co

cf

SW =

on

Hi Z
L

pu

ul

yes BHA
YY, 4G

Aug.

>) Sections,

(°F) and Salinity (°/ ,

Gulf-Temperature

Persian

IV-3

Figure

The following excerpts are taken from Reference 3, Sections on
Temperature and Salinity, pages 2358-2363.

"TEMPERATURE

"Studies of water temperature in this region are of special
interest because summer air temperatures are as great at 123°F. ...
During the 2 weeks spent in the Gulf of Oman and the Persian Gulf,
625 bathythermograph lowerings were made, but the records for 185
were lost in shipping. Most of the lowerings were accompanied by a
thermometer measurement of the surface water collected in a bucket
or in a cup attached to the thermometer. Strong surface heating in
the afternoon produced a marked temperature gradient near the water
surface. Below the zone of surface heating the water was usually
isothermal to depths of 20 to 75 feet. In order to avoid the effects
of diurnal temperature variations the surface temperature was taken
from the bathythermograms at an indicated depth of 10 feet.

"The resulting 'surface' temperature values were plotted and
isotherms drawn as shown by Figure IV-1. During this August study
there was noted a general increase in temperature from about 75°F.
in the Arabian Sea to more than 92° along both sides of the Persian
Gulf. In the Strait of Hormuz the surface temperatures were mostly
between 89° and 90°, with the lower values extending as a tongue
through the middle of the strait into the Persian Gulf. A similar
tongue of 89°-90° water extended from the delta southeastward into
the other end of the Gulf. This tongue was reflected and continued
in the 90°-92° temperature belt which extended from the head of the
Gulf to a point two-thirds of the distance to the Strait of Hormuz.
Along both sides of the Gulf the nearshore water temperature reached
nearly 94°. In fact, several thermometer measurements of surface-
water temperatures in the early afternoon yielded values of 95.2°,
indicating gradients of about 2° in 5-10 feet. The whole picture
of the distribution of surface temperatures in August, 1948, is
different from that presented by Schott (1918p) for the summer
months, but it is based on considerably more data than were avail-
able to Schott.

"Some idea of the distribution of surface temperatures in win-
ter is given in Figure ITI-1, a compilation of measurements by
Schott (1908) and Blegvad (1944). Although details can not be de-
termined from so few data, it is obvious that the temperatures of
winter are far different from those of summer, with values of only
60° at the head of the Gulf, increasing to about the same 75° in
the Arabian Sea that we found in August. Thus, the water at the
head of the Gulf undergoes an annual change of at least 30°.

38

"Temperatures at a depth of 164 feet (50 meters) were based
only on bathythermograms. These data are less numerous than for
surface temperatures because much of the area of the Gulf is
shallower than 164 feet and also because many of the lowerings made
in the rest of the area were too shallow. Temperatures at 164 feet
were less than 70° in the Arabian Sea, increasing to more than 80°
in the Strait of Hormuz. Values again decreased from the strait to
as low as 67.2° within the Persian Gulf. ‘The latter temperatures
are lower than those of water found at any depth in the strait, so
they probably mark the position of patches of bottom water remaining
after the previous winter.

"SALINITY

"During the two-week stay in the Persian Gulf and the Gulf of
Oman, samples of the surface water were collected at 122 stations
for salinity determinations. At eighteen of these stations vertical
series of water samples were also obtained, usually from depths of
66, 164, and 328 feet (20, 50, and 100 meters). All of the water
samples were titrated for chloride content, from which total salinity
was computed.

"Results of the salinity measurements are shown in Figure IV-2.
Some of the irregularity of the isohalines results from the use of
water samples collected a few days apart by different ships. Surface
salinity increased from about 36 5% - » - in the middle of the Gulf
of Oman to values higher than 42.0% in the Persian Gulf. The main
surface salinity gradient was transverse to the Persian Gulf, with
salinities of less than 38.0% common on the northeastern side, in-
creasing to more than 41.0% on the southwestern side. The greatest
salinities of all, 42.4%, occured in Kuwait and Bahrein bays, where
water circulation is impeded. It is interesting to note that the
salinity off the delta at the head of the Gulf was about BOn Over
greater than the salinity along most of the northeastern side of the
Gulf. Thus, it appears that the discharge of fresh river water was
small during this period.

"The vertical series of salinity determinations show that with-
in the Persian Gulf, salinity consistently increased with depth.
The value at 164 feet was about 40.0% along the northeastern side
and about 41.0% along the axis of the Gulf. In the Gulf of Oman
salinity remained more nearly constant with depth, and in one series
even decreased with depth. The lowest salinity obtained in the re-
gion was 35.5% at a depth of 672 feet (200 meters) in the Gulf of
Oman.

"Only three earlier sets of salinity measurements from the

Persian Gulf could be found. Two sets were taken by German steam-
ships. One of these, covering the period February, May, and June,

39

1907, was discussed by Schott (1908), while the other set, obtained
in September of both 1910 and 1911, was described by Schulz (191).
The third set was taken by Blegvad (1944) in March and April, 1937,
and February, March, and April, 1938. Although the data are less
eomplete than our records for August, they yield interesting compar-
isons. The sketchy information for the Gulf of Oman and most of the
Strait of Hormuz shows that the salinity is fairly constant from
February through September. In the Persian Gulf during all four sea-
sons the salinity increases from northeast to southwest across the
Gulf, although on the basis of scantier information Schott (1918b)
indicated an increase in the opposite direction for late winter and
early fall. No very great seasonal variation appears to exist in

the southeastern half of the Gulf, but the condition is different

in the northwestern half. A comparison of the four sets of isohalines
shows that over much of the latter area the salinity for the February-
March-April period was between 40% and 41%, whereas for the May-
June period it was between 39% and 40%, and for August it was mostly
between 38% and 39 foo but for September it rose again to 39 foo to
HOW, Thus, it appears that the salinity during winter is greater
than in sumer. Schott (1908) considered this condition to result
from variation in flow of fresh water through the Shatt al Arab. He
stated that the flow is least from September to November and that in
December local rainfall causes an increase, and the discharge con-
tinues rather high through January, February, and March. In April
the melting snow of the Armenian mountains causes another increase
that finally reaches a high point in May and June. In July the river
discharge falls again. The high salinity in the northwestern half

of the Gulf may also be controlled by variation in the rate of evap-
oration. When the temperature of the air is greater than that of

the water, as during the summer, evaporation from the sea is at a
minimum. During the winter the air is colder than the sea, so evap-
oration is greater then... . Thus, the annual variation of evap-
oration exerts a seasonal control on surface salinity that is nearly
parallel with the control by variation of runoff."

Sections of temperature and salinity for the Persian Gulf for
August prepared by K. O. Emery are shown in Figure IV-3.

40

SECTION V
DUBACH’S AND WEHE’S ANALYSIS

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“LA 2anBiy

{ Tihinws

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43

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44

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+ AG G3LVIIGNI SSW3Y1LX3

46

The following excerpts are taken from Reference 2, Sections II.
Temperature and III. Salinity, pages 2-5.

"TT, Temperature

"Figure I-5 shows the locations of oceanographic stations and
diurnal warming observations made in and near Kuwait Harbor. Fig-
ures V-1 and V-2, respectively, present typical midwinter surface
and bottom temperatures in Kuwait Harbor, and Table 5 gives the
observed data upon which these figures are based. The usual Nansen
bottles and reversing thermometers were used for making the oceano-
graphic stations.

"In winter, water temperature in Kuwait Harbor and vicinity
varies little either horizontally or vertically. The surface tem-
perature ranges from a low of about 56°F. in the southern and western
portions of the bay to nearly 60°F. just off Jazirat Faylakah. The
difference between the surface and bottom is of the same order of
magnitude; a maximum vertical temperature gradient of 3°F. was re-
corded at the mouth of the harbor in a depth of 26 feet.

"This is quite in contrast to the summer conditions reported
by Dr. K. O. Emery for August 1948. Observations taken by him
show surface temperatures in excess of 90°F. and bottom temperatures
of about 85 F. These temperatures result in a gradient of 5° to
7°F. in approximately 45 or 50 feet of water. The gradient increases
markedly farther east of Fahihil where bottom temperatures reach
(im tO hteke in asdepth of about 75 feet. Development of this ex-
tremely warm surface layer probably begins in April or May when the
mean maximum air temperature begins to show an appreciable increase.
Also the general decrease in cloudiness with the advent of spring
provides for increased solar heating (insolation) of surface waters.
A reduction in frequency of frontal passages with their typical
gusty "shamal" type winds is another factor contributing to the
development of a strong gradient between the surface and bottom
water through the spring and early summer months. Without these
squally "shamal" type winds, mixing is reduced to a minimum. In
autumn, beginning in October, the processes are reversed.

"Even in winter, solar insolation frequently raises midafter-
noon air temperatures to the seventies; thus it is reasonable to
expect some diurnal fluctuations in the water temperature near the
surface. The two time-depth sections taken in Kuwait Harbor in
January and February and one section taken off Fahihil in March
illustrate well midwinter diurnal warming of the surface waters
(Figs. V-5, V-6, and V-T> respectively). These sections are based
on BI observations taken at approximately half-hourly intervals

50

while drifting along the tracks shown in the insets on Figure I-5.
No drift chart is available for the February observations, but the
drifting boat started from approximately the same position as that
oO was dees OloseinremiOgs. 5 6 6 As

"Diurnal temperature ranges of 1.3° and 3.1°F. were recorded
at the surface for the two Kuwait Harbor series of observations;
off Fahihil the range was 2.2°F. The February series is particu-
larly interesting in that it shows an appreciable diurnal range
and the mixing effect of a strong wind in midafternoon. In this
series the highest surface temperature was observed at 1300 LST
(about the time of maximum air temperature and maximum solar in-
solation). Soon after 1300 a "shamal" type wind began; wind speeds
increased to Beaufort force 4 by 1400 and remained so to the end of
the observation period. Within two hours after the maximum temper-
ature was observed, mixing had reduced the surface temperature by
3°F., and by 1600 (3 hours after the beginning of the "shamal")
the entire water column was nearly isothermal.

"Tt is possible then that diurnal heating could account entirely
for the total range of temperatures shown on the surface temperature
chart, Figure V-1; the oceanographic station observations were taken
in the same week as the BI observations for the second time-depth
section. (This is the reason that local time also is given for the
oceanographic stations shown in Figure I-5.)

"A comparison of the three diurnal warming sections illustrates
well the monthly increase in water temperature, particularly that
in the surface layer. It appears that as a general rule the maxi-
mum air temperature and maximum surface water temperature are within
a few degrees of each other except, of course, when increased wind
speeds prevent formation of or destroy the warmer surface layer by
mixing.

“II. Sedaivaatiey

"Salinity observations were taken on 23-2) February 1949 only,
when the series of oceanographic stations (Figure I-5) was occupied.
Water samples were collected at the surface and near‘ the bottom,
and only at the surface where depths were less than 2 meters. Of
the 32 samples taken, eight were missing or the sample bottles
broken in transit before reaching the laboratory. Three of these,
the surface samples for Stations 2, 4, and 14, would have been
helpful in adding detail to the analysis in certain areas.

"Surface and bottom salinity charts, presented as Figures V-3
and V-4, respectively, are based on these data. Over the harbor

area the total salinity range at the surface is about 3.5% (parts
per thousand); maximum salinities are observed in the shoal waters

51

near the head of the embayment. The freshest water, which inciden-
tally exceeds the average salinity of water in the open ocean by
more than 2%, was observed in the very shallow water immediately
west of Jazirat Faylakah. Apparently brackish drainage water from
Khawr as Sabiniyan and/or Shatt al Arab reaches the area here and
reduces the gulf surface salinity from its normal value of about
40% to about 38%. Even though rainfall is meager in this area

(4 to 11 inches annually), most of the precipitation can be expected
during the months of January and February. It is reasonable then

to expect salinities in the extreme eastern portion of Kuwait Harbor
(in the vicinity of Jazirat Faylakah) to be reduced slightly below
the indicated surface values which were observed during a period of
no rainfall. Salinities of 39% or less extending into Kuwait Harbor
would be most unusual, because the tides produce strong currents
between Ras al Ardh and Jazirat Faylakah that effectively mix the
surface waters every few hours.

"As would be expected salinity values at depth are nearly the
same or slightly higher than the surface values. Even the greatest
difference between the surface and bottom is hardly significant; at
the harbor entrance (Station 12) a gradient of only 0.4% is observed
through a 12-foot depth."

52

SECTION VI
RECENT DATA ANALYSIS

53

RA'S AS ZAWR

RAS AL MISH “AB

Figure VI- 1.

TEMPERATURE (°C)
SURFACE

MARCH
1950

FEBRUARY
1952

BUSHIRE

Northern Part, Persian Gulf—Temperature (°C)—

surface, Feb. 1952, Mar. 1950

55

RA'S AS ZAWR

Figure VI- 2.

TEMPERATURE (°C)
DEPTH 10 METERS

Northern Part, Persian Gulf—Temperture (°C)—

10 meters, Feb. 1952, Mar. 1950

56

Figure VI-

3.

TEMPERATURE (°C)
DEPTH 20 METERS

FEBRUARY— MARCH
1950

FEBRUARY
1952

Northern Part, Persian Gulf—Temperature (°C)—

20 meters, Feb. 1952, Mar. 1950

57

Figure VI- 4.

,

ores,

peae en

TEMPERATURE (°C)
DEPTH 30 METERS

FEBRUARY

Northern Part, Persian Gulf—Temperature (°C)—

30 meters, Feb. 1952

58

SALINITY (°/..)

SURFACE

MARCH
1950

S
SS

S
SS
Sos
1.0, FEBRUARY
; 1952

A'S AL MISH "AB

Figure VI- 5. Northern Part, Persian Gulf—Salinity (°/, .)—surface,
Feb. 1952, Mar. 1950

59

RA'S AL MISH "AB

Figure VI- 6.

SALINITY (°/,.)
DEPTH 10 METERS

MARCH
1950

FEBRUARY
1952

Northern Part, Persian Gulf—Salinity (°/..)—

10 meters, Feb. 1952, Mar. 1950

60

Figure VI- 7.

SALINITY (°/,.)
20 METERS

Northern Part, Persian Gulf—Salinity (°/..)—

20 meters, Feb. 1952, Mar. 1950

61

FEBRUARY
1952

SALINITY (°/,.)

DEPTH 30 METERS

FEBRUARY
1952

RA'S AS ZAWR

a

RA'S AL MISH "AB

a
oon?
tug gonenttesnences®

a
*#eaenecsee”

Figure VI- 8.

Northern Part, Persian Gulf—Salinity (°/..)—
30 meters, Feb. 1952

62

TEMPERATURE (°C)

SURFACE

FEBRUARY — MARCH
1960

RA'S AS ZAWR

RA'S AL MISH "AB

eee et

Figure VI- 9. Northern Part, Persian Gulf—Temperature (°C)—

surface, Feb.-Mar. 1960

63

RA'S AL MISH ‘AB.

Figure VI-10.

TEMPERATURE (°C)
DEPTH 10 METERS

FEBRUARY —MARCH
1960

Northern Part, Persian Gulf—Temperature (°C)—
10 meters, Feb.-Mar. 1960

64

RA'S AS ZAWR

Figure VI-11.

TEMPERATURE (°C)
DEPTH 20 METERS

FEBRUARY — MARCH
1960

SUSHIRE

Northern Part, Persian Gulf—Temperature (°C)—

20 meters, Feb.-Mar. 1960

65

TEMPERATURE (°C)

DEPTH 30 METERS

--—

ee
~~.
~

Figure VI-12. Northern Part, Persian Gulf—Temperature (°C)—
30 meters, Feb.-Mar. 1960

66

RAS AS ZAWR

RAS AL MISH “AB

RAS AL BADI'A’

Figure VI-13.

SALINITY (°/,.)
SURFACE

FEBRUARY - MARCH
1960

~,

So oe aoe oe reser as eee
ee,
~s,

Northern Part, Persian Gulf—Salinity (°/..)—
surface, Feb.-Mar. 1960

67

BUSHIRE

Figure VI-14.

SALINITY (°/..)
DEPTH 10 METERS

Northern Part, Persian Gulf—Salinity (°/.)—

10 meters, Feb.-Mar. 1960

68

SALINITY (°/,.)

DEPTH 20 METERS

)

Joo

—Salinity (°

Mar. 1960

Northern Part, Persian Gulf

Figure VI-15.

Feb

20 meters,

69

Figure VI-16.

SALINITY (°/,.)
DEPTH 30 METERS

FEBRUARY— MARCH

Northern Part, Persian Gulf—Salinity (° / oo)—

30 meters, Feb.-Mar. 1960

70

RA'S AS ZAWR

RA'S AL MISH “AB

TEMPERATURE (°C)

SURFACE

Figure VI-17.

Northern Part, Persian Gulf—Temperature (°C)—
surface, Apr. 1952

71

BUSHIRE

TEMPERATURE (°C)
10 METERS

ees
a

‘

Figure VI-18.

Northern Part, Persian Gulf—Temperature (° C)—
10 meters, Apr. 1952

72

RA'S AS ZAWR

RA'S AL MISH “AB

Figure VI-19.

TEMPERATURE (°C)
20 METERS

Northern Part, Persian Gulf—Temperature (° C)—

20 meters, Apr. 1952

73

Figure VI-20.

TEMPERATURE (°C)
30 METERS

Northern Part, Persian Gulf—Temperature (°C)—

30 meters, Apr. 1952

74

RA'S AS ZAWR

RA'S AL MISH “AB

Figure VI-21.

SALINITY (°/,.)
SURFACE

Northern Part, Persian Gulf—Salinity (°/.0o)—

surface, Apr. 1952

75

BUSHIRE

SALINITY (°/,.)

DEPTH 10 METERS

Figure VI-22. Northern Part, Persian Gulf—Salinity (°/..)—
10 meters, Apr. 1952

76

SALINITY (°/,.)

DEPTH 20 METERS

APRIL 1952

Figure VI-23. Northern Part, Persian Gulf—Salinity (°/o.)—
20 meters, Apr. 1952

77

SALINITY (°/,.)
DEPTH 30 METERS

Figure VI-24. Northern Part, Persian Gulf—Salinity (°/.o)—
30 meters, Apr. 1952

78

RA'S AS ZAWR

RA'S AL MISH “AB

RAS AL BADI'A’

Figure VI-25.

TEMPERATURE (°C)
SURFACE

NOVEMBER
1951

Northern Part, Persian Gulf—Temperature (°C)—

surface, Nov. 1951

79

TEMPERATURE (°C)
DEPTH 10 METERS

Figure VI-26. Northern Part, Persian Gulf—Temperature (°C)—
10 meters, Nov. 1951

80

TEMPERATURE (°C)
DEPTH 20 METERS

Figure VI-27. Northern Part, Persian Gulf—Temperature (°C)—
20 meters, Nov. 1951

81

TEMPERATURE (°C)
DEPTH 30 METERS

Figure VI-28. Northern Part, Persian Gulf—Temperature (°C)—
30 meters, Nov. 1951

82

o

cP 50

SALINITY (°/,.)

SURFACE

NOVEMBER
1951

)

A0.3
BUSHIRE
40.2

RAS AS ZAWR

RA'S AL MISH “AB

RAS AL BADIA

Figure VI-29. Northern Part, Persian Gulf—Salinity (°/..)—
surface, Nov. 1951

83

RA'S AS ZAWR

RA’S AL MISH “AB

Figure VI-30.

SALINITY (°/,.)
10 METERS

Northern Part, Persian Gulf—Salinity (°/..)—

10 meters, Nov. 1951

84

SALINITY (°/..)
20 METERS

NOVEMBER
1951

RA'S AL MISH “AB.

CG

RAS AL BADIA
Y

Figure VI-31. Northern Part, Persian Gulf—Salinity (°/.o)—
20 meters, Nov. 1951

85

SALINITY (°/,.)
30 METERS

RA'S AS TAWR

RA'S AL MISH AB

Figure VI-32. Northern Part, Persian Gulf—Salinity (°/ oo)—
30 meters, Nov. 1951

86

APPENDIX A
HISTORICAL DATA (PRE-1950)

87

Table 1:

Table 2:
Table 3:

Table 4:

INDEX OF HISTORICAL DATA (PRE-1950)

Surface Water Observations (Temperature and Salinity) Persian Gulf (ASSYRIA and
CANADIA), 1907, Schott.

Surface Water Temperature (°C) Observations, 1908, Schott.

Surface Water Observations (Temperature and Salinity) of the Persian Gulf (SICILIA
and EKBATANA), 1910-11, Schulz.

Observations of the Persian Gulf (M/S RASHGOO), 1937-38, Blegvad.

NODC Machine Listing:

31804 —

Table 5:

U. S. Naval Oceanographic Office, CARPELLOTTI
Washington, D.C. Manuscript Data. MASSEY

For Stations in the Persian Gulf. 15-26

Aug. 1948 22 Stations

Oceanographic Stations—Kuwait Harbor (USS JOHN BLISH), 1949, Dubach and Wehe.

88

SURFACE WATER OBSERVATIONS OF THE PERSIAN GULF

LATITUDE LONGITUDE | WATER TEMP. SALINITY
(N) °C Vass

1907 SHIP ASSYRIA E

FEBRUARY

Table 1: Surface Water Observations (Temperature and Salinity) Persian Gulf (ASSYRIA and
CANADIA), 1907, Schott.

89

SURFACE WATER TEMPERATURE

LOCATION PERSIAN GULF

EAST LONGITUDE

51°-52° 52°-53°

DECEMBER
JANUARY
FEBRUARY
MARCH
APRIL

MAY

JUNE

JULY
AUGUST
SEPTEMBER

OCTOBER
NOVEMBER

NO. OF OBS.

YEARLY AVERAGE

ABSOLUTE MAXIMUM

( DATE )

ABSOLUTE MINIMUM

( DATE )

Table 2: Surface Water Temperature (°C) Observations, 1908, Schott.

90

SURFACE WATER OBSERVATIONS OF THE PERSIAN GULF

22 SEPTEMBER
22
23
23
23
23
24

24

AUGUST

SEPTEMBER

LATITUDE
(N)

29° 20’
29° 42’
27° 40’
26° 16’

26° 22’

28° 08’
28° 15’
2 malod
24° 56’

26’

LONGITUDE
(E)

SHIP SICILIA

53°
52°
51°

51°

30’
35’
54’

04’

BUSHEHR (BUSHIRE)

49°

54’

WATER

°€

Surface Water Observations (Temperature and Salinity)
and EKBATANA), 1910-11, Schulz.

91

TEMP. SA

LINITY

OBSERVATIONS OF THE PERSIAN GULF
SHIP: M/S RASHGOO

STATION DEPTH WATER TEMP. SALINITY
NUMBER (METERS ) ae 7.

4 MARCH 1937 SFC (0)
SFC (0)
SFC (0)
SFC (0)
SFC (0)
SFC (0)
SFC (0)
20
41
SFC (0)
10
20
30
50
71
SFC (0)
22
SFC (0)
10
30
32
SFC (0)
SFC (0)
SFC (0)
SFC (0)
SFC (0)
FEBRUARY 1938 SFC (0)
SFC (0)
SFC (0)
BAHREIN SFC (0)
N.E. OF QAIS
26° 38’N
54° 12’E SFC (0)
10
28
Table 4: Observations of the Persian Gulf (M/S RASHGOO), 1937-38, Blegvad.

92

ORIGINATOR'S

CRUISE STATION
NUMBER

MARSDEN
SQUARE

a

eee

STATION TIME

LONGITUDE
Wo.
O51415E

NODC
STATION

NUMBER
0001

[ REFERENCE | suis
mami | cope LATITUDE
NUMBE “0

31 504 cP |2523 N

eu 7 NO.| TYPE 2 ANOMALY — X 107) VELOCITY
Wo
2478 | 0031803 | 0000 15596
OBS 0000 339 4090 2478 15596
5 OBS 0007 350 P 4021P 2384Q
t

REFERENCE WAVE Nope
LATITUDE LONGITUDE SQUARE (GMT) year | cruisi TATION a STATION
2 ivi0 wea UME

31)SO4/CP |26055N

TO
fee a pee eo
SPECIAL
COLOR OBSERVATIONS
== “ a

SPECIFIC VOLUME
ANOMALY — X 107,

PO, —P |TOTAL—P| NO, —N|NO,—N SIO ,—Si
pg-at/I] pg-at/! |ug-at/1| pg-ot/I| pg-at/!

REFERENCE

MARSDEN
SQUARE

STATION TIME
(GMT)

WAVE
OBSERVATIONS

FATIIUDE
“1/10

LONGITUDE
* 700

05033 E

BAROMETER
(mbs)

SPECIAL
OBSERVATIONS

SPECIFIC VOLUME] pynyy. | SOUND

ANOMALY—X107] 193 | VELOCITY

MESSENGER 2 aa
ae TYPE
V0
0022777 15621

1 OBS 0000 344 4241 2572 15621

PO, —P |TOTAL—P NO,—N}|NO,—N S10,-Si

On GA Vimecn/All seas lb sca/Al eyecy/fll been

2 OBS 0015 344 4318 2631 15631

93

[REFERENCE | MARSDEN DEPTH oe WAVE ctoup Rose
jamin | cone | LATITUDE LONGITUDE SQUARE CRUISE) STATION scoom OBSERVATIONS CODES STATION
NUMBER oem © an0 SS UBER | NUNBER! MPLES join. [wor] ren. [sea amr] [ rye [ ant. | BER

Sr soe er [z5510N [oszovoe] Fos[safos ie esol aees] [| [aot

[water |
coLor
CODE a ‘

OBS 0000 340 cee 2402 15588

5; OBS 0006 4021

WAVE
OBSERVATIONS

Pa sea
PATIpe LONGITUDE
“WO “10

= = CP |}26055N |051240E

MARSDEN STATION TIME
SQUARE (GMT)

SPECIAL
OBSERVATIONS

MESSENGER 3; CAST} CARD s %, SIGMA—T SPECIFIC VOLUME aN SOUND » mi/l PO, —P |TOTAL—P NO,—N|NO,—N si0,—-Si
nS 4 NO.| TYPE 2 ANOMALY—X107] x 193 VELOCITY pa-at/!| pg-at/! |ug-at/I} pg-at/1} yg-at/I
10

1 OBS 0006 4095

[REFERENCE | =
IDENTITY pale LATITUDE LONGITUDE | =
NUMBER “1/10 “1/10

31 |SO4|/MY |2313 N |059380E

ae MARSDEN STATION TIME [___oRIGINATOR's | Ss DEPTH Deer WAVE WEATHER CLOUD NODC
s ie Se CRUISE STATION OBSERVATIONS CODE CODES STATION
= sinsse| _Rawses_|_80rTOM meted Coan [vee [aur | NUMBER
SSS. 1948 area 3274 | 02 |

COLOR onsenvAtions
CODE

ie

(i al (27 EE ee
—P |TOTAL—P| NO, —N]NO,—N/|SIO,-Si
ee Df ee [ea =
Vio

STD 0000 3230 | 3694 2239 0054561 | 0000 |15525

OBS 0000 323 3694 2239 15525

STD 0010 3156 3697 2268 0051855 0053 15512

STD 0020 3010 3700 2321 0046799 0103 15485

1 oBs 0020 301 3700 2321 15485
STD 0030 2661 3662 2408 0038527 0145 15408

STD 0050 2140 3608 2522 0027723 O211 15279

1 OBS 0050 214 3608 2522 15279
STD 0075 2005 3604 2556 0024619 O277 15247

STD 0100 1870 3600 2588 0021655 0335 15213
OBS 0100 187 3600 2588 15213

94

LONGITUDE

0000
0010
0020
0020
0030
0050
0050
0075
0100
0100
0125
0150
0200
0203

SHIP
ar CODE LATITUDE LONGITUDE ap] tee |
“1/10 “1/10

31 |)SO4)MY |26045N |056470E

MARSDEN
SQUARE

Eee 030) 1948

[water |

com iE aes ie
CODE ane

318
2805
2500
250
2302
2010
201
1945
1880
188

eases
SQUARE

[ioe [ie [own | pay [ue 1710]

STATION TIME

3655
3643
3635
3635
3635
3636
3636
3637
3638
3638
3628
3611
3554
3550

eee TIME
eee

ORIGINATOR'S

STATION
NUMBER

[wind |

2228
2347
2438
2438
2497
2579
2579
2597
2614
2614

CRUISE

NUMBER

“ime | nr |
(mbs)

0055639

0044252
0035641

0030045
0022339

0020727
0019146

[__oRIGiNaTOR'S —_| ‘Ss

STATION
NUMBER

0010
0020
0020
0030
0050
0050
0075
0080

[REFERENCE | aun
ipetiy| cope | LATITUDE
NUMBER eee 710)

31 )SO4/MY |26165N

LONGITUDE

056340E

0000
0000
0010
0020
0020
0030
0050
0050
0075
0090

MARSDEN
SQUARE

STATION TIME

RES Seu CARD
IME TYPE
HR 1/10

SPECIFIC VOLUME
ANOMALY — X 107

0055611

0052955
0047791

0036930
0026735

[.__ORIGINATOR's | Ss

CRUISE STATION
eal a

SPECIFIC VOLUME
ANOMALY — X 107!

0062332

0060159
0055252

0039605
0018598

0011389

95

DErTH beer
2oltom ore
i

SPECIAL
OBSERVATIONS:

PO, —P |TOTAL—P} NO, —N|NO,—N
yg-at/I |ug-at/I| »g-ot /1] pg-at/I

ea |

SOUND
VELOCITY

SPECIAL
OBSERVATIONS:

arse
PAURLIDE LONGITUDE
“110 “10

=| ea MY |}26250N |056315E

MARSDEN Sere | TIME [__oricinator's | ‘Ss Deri WAVE warn CLOUD NODC

SQUARE Sere | nah OBSERVATIONS (OE CODES STATION

[vor [i | mowra T oay [ar 1710] NUMBER || NUMBER os Coens [ rrre | aur. | Uaee
Se 0010

color sretD
ca See

eas | en ea ee Prem eee
ree [| fe eel es = soi
a 7 NO.| TYPE ° [ANOMALY — X 10) x 103 2 yg-at/I| pg-at/! |ug-at/!| pg-at/1] yg-at/I
at}

STD 0000 3230 |3748 0050690 15530

OBS 0000 323 3748 2280 15530

STD 0010 3205 3787 2318 0047079 0049 15531

STD 0020 3180 3824 2355 0043618 0094 155232

1 OBS 0020 318 3824 2355 15532

STD 0030 2880 3860 2486 0031149 0132 15477

STD 0050 2440 3920 2672 0013531 0176 15390

1 O8S 0050 244 3920 2672 15390

STD 0075 2347 3968 2737 0007534 0203 15377

STD 0100 2280 4006 2785 0003033 0216 15369

1 OBS 0100 228 4006 2785 15369

STD 0125 2280 4033 2806 0001200 0221 15377

STD 0150 2280 4050 2819 0000087 0223 15383

STD 0200 2280 4053 2821 0000090 0223 15391

1 OBS 0200 228 4053 2821 15391

=e =| | - Se ee
TY LATITUDE LONGITUDE SQUARE MAT) CRUISE
eae Gee | a nen [fw] [a [Ouse] SOMGR | sottom |. oh ean tra aT
31 |S04|MY [26310N |055510E| fio3|é65[os|izjovo[isse{ [| — |oos9[oo|] |
ee [an rene ec]

SPECIFIC VOLUME SOUND | 9 m/l PO, —P |TOTAL—P| NO,—N | NO,—N/|SIO,—Si
ANOMALY — X 107 cH Ls VELOCITY. 2 »o- sat /t pg-at/l |ug-at/!| yg-at/1 aeevi

0053476 | 0000 |15546

cLouD NODC
naa ae | NUMBER
[ire [aa NUMBER

0011

1 OBS 0000 331 3748 2250 15546
STD 0010 3111 3741 2317 0047179 0050 15508
STD 0020 2960 3734 2364 0042724 0095 15478

1 OBS 0020 296 3734 2364 15478
STD 0030 2856 3768 2425 0036981 0135 15462
STD 0050 2790 3916 2558 0024370 0196 15468

1 OBS 0050 279 3916 2558 15468

(| MARSDEN [Sara TIME [_oriGinator's —_| Derma WAVE wana
oe LATITUDE LONGITUDE 5] sais | SQUARE [Sara STATION OBSERVATIONS ES STATION
= aut cong | Foe Te [owe Tar Tur v7i0] Nomex] t0rvOM jaan NUMBER

31 [so4|mMy |26165N |055455— fit eben toe 0012
[water | Wind |

_ L SPECIAL
vee a

SPECIFIC VOLUME een SOUND 0, mi/I , —P |TOTAL—P| NO, —N|NO,—N/SIO,—Si
ANOMALY—X107| x 193 VELOCITY yo- (ais pg-at/I |ug- ceri yg-at/1| yg- <or/i

0053572 15538

1 OBS 0000 328 3732 2249 15538
STD 0010 3066 3754 2342 0044738 0049 15500
STD 0020 2910 3775 2412 0038163 0091 15472

1 OBS 0020 291 3775 2412 15472
STD 0030 2812 3796 2460 0033578 0126 15456
STD 0050 2790 3835 2497 0030178 0190 15459

1 OBS 0050 279 3835 2497 15459

96

[ REFERENCE | a MARSDEN | STATION TIME ORIGINATOR'S WAVE weamiee | CLOUD NODC

ull SQUARE GMT, OBSERVATIONS CODES STATION

pari’ | €ope | LATITUDE LONGITUDE a (GMT) as STATION
NUMBER “10 “ino [-rvre [ Aut. |

CRUISE STATION
eC S{_O1k [WG a [Sn AMT]
pea] oe[au rio ieee] | pease | oo |

|__water [Wino | poeeel es]

CoLoR | TRANS, pea
= ai an
SOUND

SPECIFIC VOLUME
ANOMALY — X 107, VELOCITY

31)SO4|MY |}26050N |055420E

PO, —P |TOTAL—P| NO, —N |NO,—N|SI0,—Si
ug-at/I) pg-at/! |yg- “at /l yg-at/1} yg- ~at/I

0055419
OBS 0000 330 3716 2230 15540
sTD 0010 3720
STD 0020 3723
1 OBS 0020 3723
STD 0030 3779
STD 0050 3994
1 OBS 0050 3994

ORIGINATOR'S. WAVE CLOUD
WEATHER | CODES

MARSDEN STATION TIME
SQUARE ae YEAR licruisell STATION OBSERVATIONS _ | WEATH
[io [wom] NUMBER] NUMBER samme on verre amr] “re [a

peo|e [ee rfc aa ia
[__WaTeR | nana] | anew. ec
BAROMETER rot
a cm (mbs) | DRY BULB ES OBS.
FORCE

SOUND
VELOCITY

REFERENCE
LATITUDE

IpeNTiTY
NUMBER 2 ano

31 )SO4)MY |26025N

NODC
STATION
NUMBER

LONGITUDE
710
O55115E

SPECIFIC VOLUME

SIGMA—T | ANOMALY —X 107|

PO, —P |TOTAL—P| NO, —N]NO,—N|SIO,—Si
ug-at/I| pg-at/l }ug-at/!| yg-at/1| pg-at/I

2205 | 0057815

1 OBS 0000 338 3722 2205 15556
STD 0010 3103 3765 2338 0045189 0052 15509
sTD 0020 2890 3817 2450 0034508 0091 15473
1 OBS 0020 289 3817 2450 15473
STD 0030 2742 3877 2544 0025577 0121 15450
STD 0050 2640 4023 2688 0012061 0159 15447
1 OBS 0050 264 4023 2688 15447

WAVE
OBSERVATIONS

NODC
STATION
NUMBER

REFERENCE
SHIP

countay| ioptity | Cope
CODE | NUMBER

=| MARSDEN | STATION TIME ORIGINATOR'S DEPTH
LATITUDE LONGITUDE |=S| SQUARE YEAR | CRUISE STATION a
“0 2 yi || = : NUMBER| NUMBER TTOM

| 0069

SOUND
VELOCITY

BAROMETER
(mbs)

SPECIFIC VOLUME

0048641

OBS 0000 343 3875 2301 15581
sTD 0010 3186 3934 2435 0035895 0042 15543
STD 0020 2930 3979 2559 0024184 0072 15499

1 OBS 0020 293 3979 2559 15499
STD 0030 2662 4011 2672 0013500 0091 15447
STD 0050 2090 4034 2861 =-0004341 0100 15316

1 OBS 0050 209 4034 2861 15316

97

27130N |052400E

sTD 0000
1 OBS 0000
STD 0010
STD 0020
1 OBS 0020
STD 0030
1 OBS 0040

ar se SHIP
wary | CODE TAUTUDE LONGITUDE
“10 “10

MARSDEN
SQUARE
ce ee OC

sci i
A

oaehe
Pot fad e

STATION TIME
(GMT)

Ske

3803
3811
3819
3819
3868
3945

pawn |
COLOR
ets 2
oa a ea

NESSENGER & CAST| CARD =
TUME NO.| TYPE
Ls V0

SIGMA—T

2236

SPECIFIC VOLUME
ANOMALY — X 107

0054883

ORIGINATOR'S

STATION
NUMBER

tae
M,.
x x 103

SOUND °. 1/1 PO, —P |TOTAL—P’ NO,—N NO,—N S10, -Si
vetocity | ~2.™/° |yg-at/I| pg-at/! |wo-at/!| yg-at/I mec

15579
15579

WAVE cloud Nopc
OBSERVATIONS eae CODES STATION
[vee [ ant. |

| oin. [wer rer. [sea aur]

NUMBER

MARSDEN

SQUARE

STATION. TIME
(GMT)

STATION
NUMBER

REFERENCE
ak wariTuo LONGITUDE
“Wo “10
31 |SO4|MY |27125N |052070E

MESSENGER 2 DEPTH (m)

TIME

MR 1/10

SPECIFIC VOLUME
ANOMALY — X 107!

WAVE
OBSERVATIONS

CLOUD

WEATHER
CODE CODES

NODC
STATION
NUMBER

4 s10,-Si
pg-ot/! |wg-at/!| yg-at/1] pg-at/I

31 |SO4|MY |27360N |051255E

OBS 0000
sTD 0020
1 OBS 0020

[REFERENCE |
inary] ope | LATITUDE LONGITUDE
NUMBER “10 “1/0

LOZ

3460
346
3195
2930
293
2664
2130
213

MARSDEN
SQUARE

[oe Tae [mowra Tay Tut. 10]

3842
3866
3893
3893
3923
3992
3992

aie TIME
aie

0052088

0041075
0030349

0019876
-0000253

|__oricinator’s | Ss

CRUISE STATION
NUMBER NUMBER

HS Betaest tee

SPECIFIC VOLUME ae

ANOMALY — X 107)

98

x to"

pel
BOTTOM

berm

WAVE CLOUD NODC
OBSERVATIONS | FAME! CODES STATION

NUMI
MES aiania [re Tan ee

0018

PO, —P |TOTAL—P| NO,—N NO,—N|S!IO,—Si
pg-at/!| pg-at/l | uo- Spf yg-at/1| yg- ~at/I

REFERENCE

REFERENCE
COUNTRY
CODE

31 |S04 | MY

LATITUDE
IAN

SHIP.
CODE PATOL LONGITUDE
“1/0 “10

LONGITUDE

DRIFT
INDICATOR

MARSDEN
SQUARE

MONTH

STATION TIME

D

[__warer _|

colon | TRANS
CODE | (m)

SIGMA—T

19 |110) 1948

ORIGINATOR'S

CRUISE STATION
NUMBER NUMBER

WIND

BAROMETER
(mbs)

SPECIAL
OBSERVATIONS

WAVE clouD Nopc
OBSERVATIONS wane CODES STATION
: NUMBER
| 0019

SPECIFIC VOLUME
ANOMALY — X 107}

MARSDEN
SQUARE

STATION TIME

2331
2331
2437
2548
2548
2664
2910
2910

| 0045785

0035716
0025187

0014183
-0009004

VELOCITY

15566
15529
15487
15487
15441
15330
15330

PO, —P |TOTAL—P| NO, —N|NO,—N
ug-at/I| yg-at/l |ug-at/!} yg-at/1| yg-at/|

STATION
NUMBER

SPECIFIC VOLUME
ANOMALY — X 107

WAVE
OBSERVATIONS

REFERENCE

1 OBS 0000 342 3831
STD 0010 3831
STD 0020 3831
1 OBS 0020 3831
STD 0030 3881
STD 0050 4082
1 OBS 0050 4082
SHIP c= | MARSDEN | STATION TIME
iam | cope | LATITUDE LONGITUDE |=S| SQUARE
NUMBER 220i 2 iy ||
31 |SO4|MY |28020N |050140E

0000
0010
0020
0020
0030
0050
0050

CRUISE

ORIGINATOR'S

STATION
NUMBER

WAVE

SPECIFIC VOLUME
ANOMALY — X 107

ZAD

_DYN. M.

xX 103

SPECIAL
OBSERVATIONS

CODE
MGT.| PER. [SEA ANT.|

NO,—N|SIO,-Si
pg-at/! |yg-at/I] pg-at/1} yg-at/I

NODC
STATION
NUMBER

NODC
STATION
NUMBER

0021

SOUND
VELOCITY

PO, —P |TOTAL—P] NO, —N|NO,—N|SIO,—Si
wg-at/I| yg-at/l | ug-at/!| yg-at/1| pg-at/I

0035177
0023864

0012738
-0008067

99

0046570 | 0000

0041
0070

0089
0093

15567
15567
15539
15502
15502
15454
15319
15319

pH

ORIGINATOR'S

WAVE
OBSERVATIONS

MARSDEN | STATION TIME
unTRY =o A LATITUDE LONGITUDE SQUARE
rca “no “0 [tor [ie | wowra [pay ae. 1710]

sti] ne
ETaCca ca

cLouD Nopc
[ree Ta Nunes

0022

[WATER |
aDo'L SPECIAL
feel Semel |

SPECIFIC VOLUME SOUND P |TOTAL—P. NO,—N|NO,—N/|SIO
[som fasts ot ee. aad AN CE st YAN EA eh

0042048 15581

1 OBS 0000 339 3947 2370 15581
STD 0010 3128 3964 2478 0031771 0037 15535
STD 0020 2880 3979 2576 0022572 0064 15488
1 OBS 0020 288 3979 2576 15488
sTD 0030 2646 3992 2662 0014376 0083 15441
sTD 0050 2220 4014 2809 0000588 0098 15347
1 OBS 0050 222 4014 2809 15347

100

OCEANOGRAPHIC STATIONS - Kuwait Harbor

Date: 23-24 February 1949
Ship: U.S.S. JOHN BLISH

Station Time Depth Temp. Sal.
No. Date (LST) (m.) (°F .) (%o)
1 2/23 0903 Surf. 56.1* 40.21
12 5Dn29 40.28
2 2/23 1020 Surf. 56.8* M.**
11 54.45 40.93
3 2/23 1214 Surf. 56.8* 41.20
2 55.86 41.17
4 jf) 723) 1410 Surf. DU! M.**
4 55.81 M.**
5 2/23 1635 Surf. 58.1* 40.53
3.5 55.84 40.51
6 2/24 0824 Surf. 56.5* 40.16
5.5 56.33 M.**
7 2/24 1112 Surf. 58.63 40.11
17 55.96 40.10
8 2/24 1209 Surf. 59.23 40.29
3:5 56.60 40.22
9 2/24 1242 Surf. 59.43 39.96
5 56.69 40.17
10 2/24 1325 Surf. 29)5 29) 40.06
8 56.53 M.**
11 2/24 1336 Surf. 57.39 M.**
8 56.22 40.06
12 2/24 1420 Surf. 58.32 S)8) 5 8)/4
4 56.40 39.90
13 2/24 1457 Surf. 57.73 39.32
3 55.77 39).29)
14 2/24 1531 Surf. 57.98 M.**
(252) 55.43 38.20
15 2/24 1558 Surf, 57.86 M. **
225 56.69 37.89
16 2/24 1625 Surf. 57.91 37.97
17 2/24 1700 Surf. 57.50 37.77
Note:

* Bucket thermometer used, read only to tenths °F.
** Sample bottles lost or broken, values missing.

23 Feb..- Wind: B. F. 2 24 Feb. - Wind: B. F. 1
Sea: Code 2 Sea: Code 2
Weather: 00/01 Weather: 02
Table 5: Oceanographic Stations—Kuwait Harbor (USS JOHN BLISH), 1949, Dubach and Wehe,

101

ei

» F Py “1 i aN ao) ~F ip as
SS:0r Pare <7 ‘
“NY oa ae me so! €Sis
Pe : £e0e Choe ig ;
P im, 1% bs o,e¢ Mpe. . t J : 2s \§
> {,t* 63.24 $
~* b *. 72 tiv Oth TERNS
: ow 2 A, oF b
< tS 3 ¥e swe ; <t A a4 \ ==
¢..03 bO.C¢ <x
7", {hh #; ; Yi ‘SEQ bo \$
a? bh @. 4 < rid
< ti) f CARs s/cite | aS \S
i Y Ae i i
M . & ewe? wus f 63:45
G} é ,
| ee Sie eS \
y a, ‘
‘i vA RY i eSAS
2 fd :
rs “4 tir a a Pata
( f ne. 5
a at rit osu! As
5 fu a t
f rs ef} os
ile 2 bite : 5
‘thy ? a
. 54 .V¢e tue Sex -S \S
"UF, 41 Poy ad
(ve ittie Hy I Be YS
4 ‘ ne
. ‘920M
: t @
é 1 oOo? f reed Boal pron ty? eho
RSitet FSLUSV',G3SA0 10 xa teo! eaiticd Plug cvtgged ead
el
d rT Ve iat & ; . 4 a! Pye iW « An és
by , {

A 10\00 :42dtes¥

2159 MMOL ZHU wsdusl Kewe moore a

ahold. eg

APPENDIX B
RECENT OBSERVATIONS (POST-1950)

INDEX OF RECENT OBSERVATIONS (POST-1950)

NODC Machine Listing:

31382 —

Table 6:

U.S. Naval Oceanographic Office, MAURY
Washington, D. C. STALLION
Manuscript Data. ALLEGHENY
4 Dec.—20 April 1950

74 Stations

Surface and Subsurface Salinity Observations (USS STALLION and MAURY), 1951,
U. S. Naval Oceanographic Office, Washington, D. C. Manuscript Data.

NODC Machine Listings:

31805 —

31496 —

31658 —

31865 —

U. S$. Naval Oceanographic Office, MAURY
Washington, D.C. Manuscript Data. & others
9,12, 15, 17, 23 Feb. 1951. 5 Stations

U. S. Naval Oceanographic Office, ALLEGHENY

Washington, D.C. Manuscript Data.
Cruise A, B, C, 24-25 Nov. 1951,
20-21 Feb. 1952, 9-10 April, 1952.
51 Stations

U.S. Naval Oceanographic Office, REQUISITE
Washington, D.C. Manuscript Data.
16 Feb.—5 Mar. 1960, 55 Stations

U. S. Naval Oceanographic Office, REQUISITE
Washington, D.C. Manuscript Data.

For Stations in the Persian Gulf

and Arabian Sea. 4 Jan.—31 Mar. 1961

206 Stations

104

SURFACE OBSERVATIONS

NODC POSITION
REF. STATION
NO. i LATITUDE

00382| 0001 29 06 N

SUBSURFACE OBSERVATIONS

SAMPLE 7 S °/oo ot = AD 0, mi/I vs
DEPTH (M) v y y v y
STD 0000 21 04 |40 58 28 75 |0 000
OBS) 0000 21 04 |40 58 23 175)
STD 0010 21 06 40 53 Zone OmOOG=
OBS 0010 Zi WG \BO Sz) 283 Tal

SURFACE OBSERVATIONS

NODC DATE
REF, STATION

ic} AY
[00384 0002 | 12 | os | ise] os | 29

POSITION

LONGITUDE

06'N| 048 10€

WIND

ANEMO. AIR
SPEED DIR. Uist: FRESE.
[1314 |
SAMPLE =AD O,mi/I ys
DEPTH (M) Vv Vv Vv
STD 0 000
OB
STD 0 006-
0B

| SURFACE OBSERVATIONS

POSITION

COL.} TRANS.

SPEED DIR.

SAMPLE Tc 5 "/os oh DAD O,mi/l ‘i
DEPTH (M) v y v vy v v
STD 0000 20 Pi Fo | SO 28 73 |0 000
QBS) 0000 20) Gil |KO GO) PAS} TFS}
STD 0010 20 88 |40 66 28 86 |0 006=
ORS) 0010 20 88 40 66 28 86

105

SURFACE OBSERVATIONS
REF. EPTH SAMPLE

a Real am PORE cLouD SWELL WATER
HGT. | PRESS. ae eeusle

SUBSURFACE OBSERVATIONS

STATION

SAMPLE
DEPTH (M)

STD 0000
ORS 0000
STD 0010
OBS 0010

SURFACE OBSERVATIONS
NODC DATE POSITION
STATION

SONIC MAX.
BP |e Te Tar van [| armas
[ coup | SWELL

ANEMO.| AiR | AIR TEMPERATURE |
HGT. | PRESS. im ESUGER
wee ee eee eee

SUBSURFACE OBSERVATIONS

TRANS

STD

STD

SURFACE OBSERVATIONS

POSITION

SONIC MAX.
DEPTH SAMPLE
LONGITUDE UNCORRECTED] DEPTH
/
050 11€E 0016 | 00 |
CLOUD | SEA SWELL WATER

10
HUMID- WEATHER

frveelawr.| ove. [ ant. | orm. [awr, TRANS.
01 ee

SAMPLE
DEPTH (M)

STD 0000 28
OBS 0000 28
STD 0010 28
OBS 0010 28

106

SURFACE OBSERVATIONS

NODC | DATE POSITION
REF. STATION
NO. MO. | DAY YEAR HOUR LATITUDE LONGITUDE
= > -
00382 0006 | 12 | 16 | 1949 ag at ; 050 11 €

AIR TEMPERATURE

COL

.| TRANS.
07

SAMPLE T°c | S °/oo ot

DEPTH (M) Vv Vv
STD 0000 19 86 |40 28 28
OBS) 0000 19 86 |40 28 28
‘STD 0010 19 76/40 26 28
OBS 0010 19 76/40 26 28

| SURFACE OBSERVATIONS |

POSITION sonic MAX.
DEPT SAMPLE
LONGITUDE UNCORRECTED DEPTH

On0 an TE 0016 | 00 |

WATER

SUBSURFACE OBSERVATIONS

SAMPLE S °/oo ot = AD O, mi/| NA

HUMID-

ITY EATHE
TYPE amt,| DIR. AMT. | DIR.
| 00 4

SUBSURFACE OBSERVATIONS

DEPTH (M) Vv Vv Vv Vv
STD 28 78 |0 000
OB 28 78
STD 28 81 |0 006-
OB 28 81
SURFACE OBSERVATIONS
NODC DATE POSITION | SONIC MAX.
REF. STATION DEPTH SAMPLE
NO. MO. | pay YEAR HOUR LATITUDE | LONGITUDE UNCORRECTED] DEPTH
| 00382 0008 | 01 [17 —- 14 06 N| 048 11 € 0018 | 00
AIR TEMPERATURE CLOUD | SEA | SWELL WATER

SAMPLE 7 °c S65 ot = AD O,mi/l vy
DEPTH (M) v v v v vy v
STD 0000 14 40 |40 23 30 16 |0 000
ORS) 0000 14 40 |40 23 30 16
STD 0010 ia 9S) Ao) We 30 08 |0 019=
ORS 0010 14 39/40 12 30 08

107

SURFACE OBSERVATIONS

POSITION sonic MAX.

NODC DATE
reseed ames or [ar aoso| os [as oe'ap ee aE] or [wo

ee aig | AIRTEMPERATURE |), cLoup a SWELL WATER
HGT. | PRESS. ve yeletsals
(ee e2s | ee Ee

SUBSURFACE OBSERVATIONS

SAMPLE vi oe AD rae
DEPTH (M)

STD

STD

SURFACE OBSERVATIONS

NODC DATE POSITION
REF

5 STATION
00382] 0010 Bees

DIR.

STD

STD

SURFACE OBSERVATIONS

POSITION SONIC MAX.
STATION SAMPLE
LATITUDE | toncituve | UNCORRECTED DEPTH

rans pore eae os oe

WIND peerel| cae | See | cLoup iad SWELL WATER
—| GT. | PRESS. many (eeutlehe .

SPEED DIR. DRYW | WETY ; J COL.| TRANS.
[EPS ck |g | aia a | 03

SUBSURFACE OBSERVATIONS

SAMPLE
DEPTH (M)

STD 0000

OBS 0000
STD 0010
a4 0010

SURFACE OBSERVATIONS |

DATE POSITION ir SONIC MAX.
STATION DEPTH SAMPLE
MO. | DAY | YEAR HOUR LATITUDE LONGITUDE IUNCORRECTED| DEPTH
ot, an assela a 2s [ea aE 0011 | 00 |

WATER
COL.| TRANS.
SAMPLE Tec} S\c/oo ot ZAD O,mi/! vy yall
DEPTH (M) vy vy vy v vy y
STD 0000 ial 80 |40 44 30 88 |0 000
OBS 0000 ial 80 |40 44 30 88
STD 0010 ial 78 |40 51 30 93 |0 026-
OBS 0010 iba 78 |40 51 30 93
SURFACE OBSERVATIONS
DATE POSITION
ae | sonic | AK
HOUR | LATITUDE LONGITUDE JUNCORRECTED DEPTH

0013

1950 | 06 | 29° 08’N| 048 30 € | 0011 | 00 |

WR) ANEMO. AIR
SPEED DIR. HGT. PRESS.

WATER

AIR TEMPERATURE HUMID- CLOUD SEA | SWELL
ITY EATHER VIS,
WET ¥ TYPEJAMT.| DIR. | AMT. | DIR. |AMT.

COL.| TRANS.
| 07 36 | 0 al |
SUBSURFACE OBSERVATIONS
SAMPLE ye 3 Yeo ot ZAD O, mi/I vy
DEPTH (M) v y vy y y y
STD 0000 iil 28! BS 1 30 00 /)0 000
OBS 0000 ii 2a 9 we 2i0) (0X0)
STD 0010 ii O77 |BS Be 29 9710 O18=
OBS 0010 TAL Mente jE ae 29 OF

NO.

SURFACE OBSERVATIONS

DATE | POSITION SONIC MAX.
STATION DEPTH SAMPLE
| MO. | DAY | YEAR | HOUR | LATITUDE LONGITUDE UNCORRECTED] DEPTH
0014 | o1 | 24| 1950 | 05 | 29 o7/N| 048 10'E 0018 | 00

|.07 36

WIND Rea |S eanaen | WAIR TEMPERATURES || ony CLOUD | SEA SWELL | WATER
HGT. | PRESS. To tiny | NERO WHS:
SPEED DIR. pRYW | WETY TYPE amt.| pin. | amt. | DIR. “ cou] TRANS.

4

| comes eee

STD

STD

SUBSURFACE OBSERVATIONS
SAMPLE | TG S °/oo ot x AD O.mi/I \
DEPTH (M) y y y y y y
0000 40 O1
OBS} 0000 13° 22440 O1 30 25%
0010 40 02
OBS 0010 15 85%40 02 29 66%

109

NODC

DATE

Geri Gg RECO EUeOE

AIR TEMPERATURE

HUMID-

POSITION

LATITUDE LONGITUDE

| crouo |

SUBSURFACE OBSERVATIONS

serra
SAMPLE T°c S */oe
DEPTH (M) v
STD 0000 ii BE es 37
OBS 0000 li B38 Be By
STD 0010 Wal Sis} |S) AG
oBg 0010 li B88 |B 4S)

SURFACE OBSERVATIONS

DATE

STATION |

aoe Se ecstin ee ry Fl

5 [29 20N[ owe ie | oot | 00 |

mom fe
ieee

SURFACE OBSERVATIONS

Sone MAX.
SAMPLE
UNCORREGTED DEPTH

SAMPLE
DEPTH (M)

SWELL
VIS.
ree Fao Tras

SONIC MAX.
DEPTH SAMPLE
Css ee DEPTH

WATER

WATER

TRANS.

SURFACE OBSERVATIONS

PRESS.

DRYY

HOUR

LATITUDE

POSITION

LONGITUDE

DEPTH
UNCORRECTED

SONIC MAX
SAMPLE

DEPTH

04

29

20° N| 048°

IR TEMPERAT!
AIR INS Us Bhs [ae] oe
ITY

WET | wery |

STD
OB

STD
OB

SAMPLE
DEPTH (M)

0000
0000
0010
0010

| croup |

Cece
Ste ee oo

SUBSURFACE OBSERVATIONS

ive

SWELL

S °/eo ot EAD O, mi/| vs
v v
68 |38 77 | 29 600 000
68 138 77 | 29 60
44 139 78 | 30 23 |0 017-
44 |39 78 | 30 23

110

SURFACE OBSERVATIONS

Nopc | DATE POSITION SONIC MAX.
REF. STATION DEPTH SAMPLE
NO. | MO. | DAY YEAR | HOUR LATITUDE LONGITUDE UNCORRECTED] DEPTH
g : : ;
00382) 0018 | 01 | 27| 1950| 09 | 29 03'N| 048 10° 0015 | 00
ANEMO. AIR” AIR TEMPERATURE HUMID- CLOUD SEA SWELL WATER
HGT. | PRESS.|__ | Tne eee UE:
DRY Vv WET Vv [rvee|amr. DIR. AMT. | DIR. Jaw. cou.| TRANS.
| oa al 3 | | | 04 |
SUBSURFACE OBSERVATIONS al
SAMPLE O, m/l vy
DEPTH (M) Vv
=
STD
STD
| SURFACE OBSERVATIONS
NODC DATE POSITION | SONIC MAX.
REF. STATION DEPTH SAMPLE
NO. MO. DAY YEAR HOUR LATITUDE | LONGITUDE lUNcoRRECTED DEPTH
ug / © 7
| 00382 0019 | 01 | 27 | 1950 | 18 | 29° 26'N| 047 58 E | 0015 | 00

SEA | SWELL WATER |
T VIS.
DIR. | AMT. | DIR. |AMT. cou. | TRANS.
4 | | 02
SUBSURFACE OBSERVATIONS
SAMPLE TG S Yeo ot = AD O, mi/I yy
DEPTH (M) Vv y v y y v
STD 0000 40 02
OBS 0000 06 82%40 02 31 42
Sd) 0010 40 12
ops 0010 11 69440 12 30 65
SURFACE OBSERVATIONS |
NODC DATE | POSITION | SONIC MAX.

REF. STATION

NO.

LONGITUDE

JUNCORRECTED

DEPTH SAMPLE

DEPTH

|
| MO. DAY
00382| 0020 | 01 | 28

YEAR | HOUR LATITUDE |
1950 | 06 | 29 26°N| 047 58’e | 0015 | 00 |

AIR TEMPERATURE CLOUD SEA SWELL WATER
| ee ie aie
SPEED DIR. DRY W WET W | [rvPE AMT.| DIR. AMT. | DIR. [aw COL.} TRANS.
iz 27 | | 00 | 4] Pl 03
SUBSURFACE OBSERVATIONS
Aah REE v y She /ae) ot ZAD O,mi/I vy
uy v v v
=
STD 90000 10 Gt AO s2 | al on ld wo
O84 0000 10 61 KO 32 | aa of
STD 0010 @8 97140 32 | 31 31 lo o20=
oBs| 0010 o8 S7IRO Ze ian an

SURFACE OBSERVATIONS

POSITION SONIC MAX.
STATION DEPTH SAMPLE
> | Hour | LATITUDE LONGITUDE IUNCORRECTED| DEPTH

HUMID: | cron | SWELL WATER
ba eee

O,mi/I vy

SAMPLE
DEPTH (M)

stp | 0000
ons 0000
stp | 0010

OBS 0010

SURFACE OBSERVATIONS

POSITION

Tea [vem [rene [earns | tne

AIR WATER

PRESS. YY :
: ; ; i COL.| TRANS.

STATION

ANEMO.
HGT.

SPEED DIR.

SAMPLE ue ZAD O, mi/I vy
DEPTH (M) vy Vv Vv Vv Vv

STD 95 10 000
95

STD Sil lf) ale
91

SURFACE OBSERVATIONS

| POSITION
STATION

MAX.
SAMPLE
DEPTH

ANEMO. AIR AIR TEMPERATURE HUMID:
Ae PRESS.
SUBSURFACE OBSERVATIONS

SAMPLE Sic/es ot ZAD O,ml/I vi
DEPTH (M) v Vv v v Vv

STD BS) Ot 30 210 000
OB Be) rf Be Bal

STD BS) 7 30 28 0 020-
OB EMS) rls 30 28

112

SURFACE OBSERVATIONS

113

NODC DATE POSITION SONIC MAX.
REF. STATION DEPTH SAMPLE
NO. | MO. DAY YEAR | HOUR LATITUDE LONGITUDE IUNCORRECTED] DEPTH
| 00382] oo24 | 01 | 30] 1950] 15 | 29° 06’N| ova 10 & | 016 | 00 |
WIND ANEMO. AIR AIR TEMPERATURE HUMID- | CLOUD | SEA SWELL WATER
auene MEH GIRgs CRESS 9 |e inn sents aa] MAIS»
SPEED DIR. | DRY VW WET Vv TYPEJAMT.| DIR. AMT. DIR. AMT. cot. | TRANS. |
04 32 | | 00 3 | 03 |
SUBSURFACE OBSERVATIONS
SAMPLE TG S °/oo ot = AD O,mi/I ~] ys
DEPTH (M) Vv vy Vv vy Vv | vy
STD 0000 12 43 |40 08 | 30 4710 000
OBS 0000 12 423 |20 @8 | 30 47
STD 0010 12 #3
.OBS| 0010 12 ag
SURFACE OBSERVATIONS
NODC DATE POSITION SONIC MAX.
REF. STATION DEPTH SAMPLE
NO. | MO. | DAY | YEAR HOUR LATITUDE LONGITUDE UNCORRECTED] DEPTH
00382 0025 | 01 | 31 | 1950/04 | 29 06’N| 048 10° € | 0016 | 00
WIND ANEMO. AIR AIR TEMPERATURE HUMID- CLOUD SEA | SWELL WATER
Hen, || Ass. |——— J nary ARAN WIS 1
SPEED DIR. DRY Vv WET ¥ TYPEJAMT.} DIR. AMT. DIR. AMT. COL.| TRANS.
09 3] | 00 | | 3 7 04
SUBSURFACE OBSERVATIONS
SAMPLE 7 S °/e0 at | DAD om | y,
DEPTH (M) ¥ Vv Vv Vv | Vv
STD 0000 Ll 87
OBS| 0000 11 87
STD 0010 12 25
OBS 0010 12. 15
SURFACE OBSERVATIONS
NODC DATE | POSITION SONIC MAX.
REF. STATION DEPTH SAMPLE
NO. MO. | DAY YEAR | HOUR | LATITUDE | LONGITUDE UNCORRECTED] DEPTH
00382] 0028 | o2 | 19|1950| 07 | 29 00'N| 048 12 € | oo18 | 00 |
WIND AIR TEMPERATURE CLOUD SEA SWELL WATER
He _layeno.| aL MYND: exnien vs
SPEED DIR. DRY © WET ¥ TYPEJAMT.| DIR. AMT. DIR. AMT. cou. | TRANS.
i@ a2 | 00 4 | 04
SUBSURFACE OBSERVATIONS
SAMPLE ve S °/oo or ZAD O, mi/I v7
DEPTH (M) Vv Vv Vv vy vy
STD 0000 11 74(39 88 | 30 45 |0 000 |
oBs| 0000 ll Ta |S 88 | ad 25
STD | 0010 iil GOS Be |) 30 Wall @22—
OBS 0010 li 69/9 a8 | 30 46

SURFACE OBSERVATIONS

POSITION

NODC | DATE

REF. STATION

NO. | MO. DAY
00382 0029 | 02 | 20] 1950

AIR TEMPERATURE

A
rer] om [a
4

DRYY WET Y
SUBSURFACE OBSERVATIONS
= SAME iG S °/oo ot = AD | Oo, ml/I | vy
(M)
v v v v | v
STD 0000 W2 io) BS) Bie 30 36 |0 000
OBS) 0000 2 iho) eS) He 20h 36
STD | 0010 iil SXo) jes) So) 30 44 10 021-
an 0010 iil = SX0) |S) SO) 30 44
| SURFACE OBSERVATIONS
Nopc POSITION | SONIC
REF. STATION DEP’
NO. LATITUDE | LONGITUDE JUNCORR
00382] 0030 29. 21'n| 048 10 € | 0018

SUBSURFACE OBSERVATIONS
SAMPLE Te S "/oo ot ZAD O,mi/I Vy
DEPTH (M) v 7 v Vv Vv
STD 0000 12 55(139 29 | 29 83 ]0 000
OBS 0000 12.955 39 29 | 29 983
STD 0010 11 63139 95 | 30 53]0 019-
OB 0010 11 63139 95 | 30 53
|
SURFACE OBSERVATIONS
NODC POSITION
REF. STATION
NO. ) LONGITUDE
00382 0031 | o2 | 23 048. 10€

SPEED DIR.

STD

STD

WIND

SUBSURFACE OBSERVATIONS

SAM PLE. | Toc S °/oe ot = AD O, mi/I ys
| SEER (M) Vv y y vy
0000 12 96 |S OT QS) 57 |{0) (LOVo)
OBS 0000 12 Sis |BS ()7/ Ps) Sh7/
0010 iz 5G |S 69) 29 93/0 015-
OBS 0010 13 BE |s9 GS 29 93

114

T
ECTED| DEPTH

SURFACE OBSERVATIONS

NODC DATE POSITION | SONIC MAX.
REF. STATION DEPTH SAMPLE
NO. MO. | DAY | YEAR HOUR LATITUDE LONGITUDE UNCORRECTED] DEPTH
| 00382] 0032 | 02 | 27 | 1950 | 05 | 29° 24’N| 048 00'E 0022 | 00 |
WIND ANEMO. AIR SWELL | Wit WATER
HGT. PRESS. S
SPEED DIR. DIR. aw, COL.| TRANS.
06 29 | [|
i" SUBSURFACE OBSERVATIONS
SAMPLE Te S °/oo ot = AD O, m/l Yy
DEPTH (M) y v y v
OBS} 0000 12 94%40 72% 320 86%
OBS 0010 13 20%39 43% | 29 80%
SURFACE OBSERVATIONS
POSITION SONIC MAX.
STATION DEPTH SAMPLE
LATITUDE LONGITUDE UNCORRECTED] DEPTH
00382} 0033 29° 06 N| 048 10°£ | 0018
aig | AIR TEMPERATURE | 4. er cLoup SEA swell |
DIR. wety | |v | TYPE|AMT.| DIR. | Amt. | DIR. |AMT. COL.| TRANS.
eee 1 fe]
SUBSURFACE OBSERVATIONS
SAMPLE T °c S °/oo ot AD O.mi/| vs
DEPTH (M) Vv Vv v
STD 0000 13 82 |S 7/3) 2S) Sho) Ko) (oye)
OBS 0000 1g gees 7a) 29 90
STD 0010 12 Ties Ve 50) 4s IIo) alts}
OBS 0010 l2 Vii eA 30 14
SURFACE OBSERVATIONS |
DATE | POSITION SONIC MAX.
REF. STATION DEPTH SAMPLE
NO. MO. DAY YEAR | HOUR LATITUDE LONGITUDE |UNCORRECTED DEPTH
00382} 0034 | 03 | 01 | 1950 | 04 | 29 06'N | 048 10€ | 0018 | 00
WIND AIR TEMPERATURE CLOUD SEA SWELL | WATER |
=> EATHER VIS.
DIR. TYPE|AMT.| DIR. AMT. DIR [amr | COL.} TRANS. |
O7 32 00 3 |
SUBSURFACE OBSERVATIONS
SAMPLE ] T°c S °/oo ot = AD O,mi/I vy
DEPTH (M) Vv Vv Vv
STD 0000 13} 7S)
OBS} 0000 sky 79)
OBS 0005 13 Bis |BO WE 30). 02

5

SURFACE OBSERVATIONS

NODC DATE POSITION SONIC
REF. | STATION DEPTH
NO. MO, | DAY a HOUR ret LONGITUDE UNCORRECTED] DEPTH
00382) 0035 | 03 [ 01 | a ra N 048 10° E 0018
WIND anemo.| ain | AIR TEMPERATURE i SWELL ATER
ie Nui Me d T amt. DIR. |AMT. 5 COL.| TRANS.
al
SUBSURFACE OBSERVATIONS :
SAMPLE | T°C | S"/ce an SAD Omi | y =
DEPTH (M) y y y | y
STD 0000 WA a ull
OBS 0000 1 al
Sp) 0010. is} BV)
OBS 0010 13) 56
SURFACE OBSERVATIONS
se
NoDc | DATE in POSITION SONIC MAX.
REF. | STATION DEPTH | SAMPLE
NO. MO. YEAR | HOUR LATITUDE LONGITUDE UNCORRECTED| DEPTH
3 = -
0036 | 03 | 05] 1950| 11 | 29 = 048 30 | oo16 | 00
AMEN oul NenTE A cLoup | SWELL WATER
= peel
HET Sy ERESS | ete cae COL.| TRANS.
SUBSURFACE OBSERVATIONS |
SAMPLE T°c S °/ee ot SAD Om | yy
DEPTH (M) y y y y y
STD 0000 1G 9439 47 29 45 |0 000
oBS| 0000 14 94 |39 47 29 45
oBSs| 0010 17 620)
SURFACE OBSERVATIONS
=
DATE POSITION SONIC MAX.
STATION DEPTH _| SAMPLE
pAY | YEAR | HOUR LATITUDE LONGITUDE UNCORRECTED] DEPTH
w / ny /
0037 Saas 1950] 05 [ 29 05 N]}] 048 30 E 0016 00
—
WIND anemo.| aig | AIR TEMPERATURE | ip | ctouo SEA SWELL WATER
HGT. | PRESS. any (MeAUIES
SPEED DIR. pRYY | WETY [TvRE AMT.| DIR. Za * Yeor | TRANS.
[oe 16 | IE | 02 04
SUBSURFACE OBSERVATIONS
SAMPLE ree S °/ao ot = AD O, mi/I v7
| a a | y y y y y
STD i 9000 14 96/39 51 29 48 |0 000
ops 90900 14 (SYS BS) Si 2 48
STD 0010 is) Bie
OBS 0010 13) Sie

116

SURFACE OBSERVATIONS

|

POSITION SONIC MAX.
STATION DEPTH SAMPLE
Ke Ee LATITUDE LONGITUDE UNCORRECTED] DEPTH
; ; .
29 048 10€E | 0016 | 00
AIR TEMPERATURE HUMID | CLOUD | SEA | SWELL | WATER
ITY Fi EATHER VIS.
DRY WV WET V [TYPE AMT.| DIR. AMT. | DIR. lan. COL.| TRANS
00 | 1 |

| SUBSURFACE OBSERVATIONS

SAMPLE Te S °/eo ot = AD O,mi/I yy
DEPTH wall v y Vv Vv Vv v
STD 0000 I” Bi pS ws 28 64 10 000
OBS} 0000 ly Bil po is 28 64
STD 0010 13 @l (BS 22 BS) — if) |e) OOS
OBS 0010 13 © |B9 22 29 i©

SURFACE OBSERVATIONS

POSITION SONIC MAX.
DEPTH SAMPLE
LONGITUDE UNCORRECTED] DEPTH

14 | 1950 14 5 : j 00

MO.

03

aweno. | am AIR TEMPERATURE | raul cLouD SEA SWELL ae WATER
AGT vy CRESS: DRYY WET Y ny. [rvpe|at DIR. | AMT DIR [amr COL. TRANS. |
| 2] iF] |
SUBSURFACE OBSERVATIONS
SAMPLE T°c S °/oo ot = AD O,mi/I vy al
DEPTH (M) y v v y v y
STD 0000 13 86 /B9 we 28 26/10 000
OBS 0000 if Bio |i) ile) 28 26
OBS 9005 15 71 BO 19 23) O68
STD 0010 15 43/39 26 29 18 |0 006
OBS 0010 15 4
OBS 0015 16 91439 36 28 90%

SURFACE OBSERVATIONS

NODC MAX.

| DATE POSITION | SONIC
REF. STATION DEPTH SAMPLE
NO. MO. | DAY YEAR HOUR LATITUDE LONGITUDE UNCORRECTED] DEPTH
00382| 0040 | 03 | 14] 1°50] 15 | 29 iv Nil ows iv = 0020 [ 00

WIND ANEMO | CLOUD SEA Lz SWELL | WATER
HGT. EATHE vis.
SPEED DIR. P AMT. | COL

AIR TEMPERATURE

[rvPe AMT.| DIR. | AMT. TRANS.

00 oo | 1
SUBSURFACE OBSERVATIONS
SAMPLE Tac S °/oo ot = AD O, ml/! vy
DEPTH (M) y y y y y vy
STD 0000 Ue SvA |eiis) 58 28 44 |0 000
OBS 0000 Iie) Bj te hts 58 28 44
OB 0005 15 62 38 se 28 82
STD 0010 13 §©O© 29 Ao 29 15) |(0) Oo
OBS 0010 13 00)
OBS 0015 15 @@ BS) 29 Bs si)

117

SURFACE OBSERVATIONS

POSITION
STATION

00382) 0041

SPEED DIR. is a 6 0 ; TRANS.

SUBSURFACE OBSERVATIONS

<< —
SAMPLE S °/oo ot DAD O,mi/I vy
DEPTH (M) vy Vv Vv Vv v

88 24 19 |0 000
88 24 19
60 Zh (3 7/
83 29 8710 010
83 pas) 3) 7/
87 28} 9p

SURFACE OBSERVATIONS

POSITION | SONIC

DEPTH
LATITUDE LONGITUDE UNCORRECTED] DEPTH
Ze) Tae) Maeve 0018

WATER
VIS.
- COL.| TRANS.

STATION

‘ay | YEAR

0042 14 | 1950

SUBSURFACE OBSERVATIONS

=AD Om | y
v v

SAMPLE S °/oo ot
DEPTH (M) vy vy

86 28 5410 000
86 28 54
54 29 44
67 29 930 OO

719 29 Be

SURFACE OBSERVATIONS

POSITION SONIC
STATION DEPTH

LONGITUDE UNCORRECTED
. /
048 40 E

WIND ANEMO. AIR AIR TEMPERATURE H
PRESS.

SPEED DIR. en. > 3 3 : COL.} TRANS.
SUBSURFACE OBSERVATIONS
es 1h ae Se
SAMPLE ye S °/oo ot = AD
DEPTH (M) v
STD 0000 14 43/38 80 29 05 |O 000
OBS 0000 14 43 |38 80 29 05
OBS 0005 39 45
STD 0010 14 55 |39 65 29 68/0 012=
OBS 0010 14 55 (39 65 29 68
OBS 0015 14 25 |40 09 30 09

118

SURFACE OBSERVATIONS
NODC DATE | POSITION SONIC MAX.
REF. STATION DEPTH SAMPLE
. MO. | DAY | YEAR HOUR LATITUDE LONGITUDE UNCORRECTED] DEPTH
z 7 = 7 = =
00382) 0044 | 03 | 14|/ 1950] 21 | 29 13’N| 048 51’E 0013 | 00
WIND ANEMO. AIR AIR TEMPERATURE HUMID- \ | CLOUD SEA SWELL : WATER |
HGT. | PRESS. in ea TW? eae MSI
[SPEEP DIR. DRY v WETW | TyPE[AMT. DIR. AMT. | DIR. AMT. COL.| TRANS.
| 02 20 | [ool | 2 | |
SUBSURFACE OBSERVATIONS
SAMPLE T°c S feo a Sap | Gail vi |
DEPTH (M) Vv Vv vy vy Vv
iE
STD 0000 16 12/89 25 || 29 1 lo wae
OBS 0000 16 12/99 25 | 29 oi
OBS 0005 15 @B3/9 32 | a0 22
STD 0010 14 a7 199 o7 || 29 4 lo Ongie
OBS 0010 39 97
OBS 0015 13 25/59 o7 | 30 21
SURFACE OBSERVATIONS
DATE POSITION SONIC MAX.
STATION DEPTH SAMPLE
. MO. | DAY | YEAR | HOUR LATITUDE LONGITUDE UNCORRECTED| DEPTH
o 7 o
00382) 0045 | 03 | 14 | 1950 | 2 |e “AN NOs ose 0024 | 00
AIR TEMPERATURE SWELL | WATER
VIS.
DIR. law. cot.| TRANS.
QD 23 eel |
SUBSURFACE OBSERVATIONS
SAMPLE ToC Sic/co ot = AD O, mi/I vy
DEPTH (M) Vv Vv Vv Vv Vv
ala
STD 0000 39 86
OBS! 0000 14 00439 86 | 29 96%
0B 0005 15) 65) 139) 96 | 29) "66
STD 0010 13 Ti k@ 20 | 2 Be
OBS 0010 15 Wi AO 20 || 2s aA
OBS 0015 15 40 |40 36 | 30 03
SURFACE OBSERVATIONS
NODC DATE POSITION SONIC MAX.
REF. STATION DEPTH SAMPLE
NO. MO. | DAY | YEAR HOUR LATITUDE LONGITUDE UNCORRECTED| DEPTH
| 00382) 0046 | 03 | 14 | TSSIOn eal cman IN od ommnn> are | 0031 | 00
WIND AIR TEMPERATURE | CLOUD SEA SWELL WATER
meno | are, MOM Weare | he |
(SPEED DIR. DRY Vv WET ¥ TYPE|AMT.| DIR. AMT. DIR jan] lean TRANS.
03 23 00 | 2 | |
SUBSURFACE OBSERVATIONS
SAMPLE TC) S °/oo ot IAD O, mi/I vy
DEPTH (M) Vv Vv v Vv
ia
STD | 0000 16 23/40 a7 || 29 82 0 OOO
OBS 0000 16 93/40 \47 | 29 82
OBS 0005 16 33/40 41 | 29 85
stp ° | 0010 1G Wl PO AS | 29 96 0 OTe
OBS 0015 1589 40 52 | 30 04
STD 0020 14 39 |40 52 | 30 39 |0 036-
OBS 0020 14 39/40 52 | 30 39

119

STATION |

SURFACE OBSERVATIONS

rosea pour fos [as [asso] or [oe es7np one” a¥@ | ooze [00 |

DATE POSITION senile MAX.
EPTH SAMPLE
DAY YEAR HOUR LATITUDE LONGITUDE UNCORRECTED DEPTH

__|ANEMO.| AIR
SPEED DIR. BGT PRESS: _{cot.| TRaNs. |
Tae a
SUBSURFACE OBSERVATIONS
SAMPLE 7 oe S Yko ot DAD O, mi/| NA
DEPTH (M) v v v v v y
STD 0000 40 52
OBS) 0000 14 80440 52 320 29%
OBS 0005 6 335/405 52 29) 93
STD 0010 16 04 |40 48 ZS) SN
OBS 0010 16 O04 |40 48 DS) SF)
STD Apa Rae 15 92 |40 54 Zi) @)5)
OBS 0020 1S) SIF Ae) GVA \0) (0)

STATION

SURFACE OBSERVATIONS

POSITION

SONIC MAX.
DEPTH SAMPLE
UNCORRECTED| DEPTH

40 E | 0011

LONGITUDE

048

CHUN) ANEMO. AIR
SPEED DIR. HGT. PRESS.
| 02 09 |
SUBSURFACE OBSERVATIONS
SAMPLE Tao, S °/oo ot =AD O,mi/I vy
DEPTH (M) v Vv v
STD 0000 16 67189 85 || 29 34 | Ooo
OBS 0000 16 67/39 85 | 29 34
STD 0010 16 62
OBS 0010 16 62
SURFACE OBSERVATIONS
DATE POSITION sonic MAX.
STATION TH SAMPLE
a HOUR LATITUDE LONGITUDE BREOREC CIEE DEPTH
ae 03 1950 ae Nl Gae eee || @ezar || Oo
ANEMO. AIR AIR TEMPERATURE ao CLOUD SWELL | WATER
DCTs NESS: TYPE|AMT. AMT. DIR. ils COL.| TRANS.
a
SUBSURFACE OBSERVATIONS
SAMPLE | 1 °c S leo ot a =ZAD 0, mi/I ys y
DEPTH (M)
BE v v wus
STD 0000 16 03140 37 | 29 89/0 000
OBS 0000 16) 0340) 37 || 29) 89
OBS 0005 16 OF |4@ 26 || 2 OA
STD 0010 15 91 |40 44 | 29 97/0 017=
ORS 0010 15 On Gon aanl eon on
STD 0020 14 7940 50 | 30 28 |0 036-
ops 0020 14 7940 50 | 30 28

120

SURFACE OBSERVATIONS

DATE POSITION | SONIC MAX.
STATION DEPTH SAMPLE
MO. DAY | YEAR HOUR LATITUDE LONGITUDE JUNCORRECTED DEPTH
00382, 0050 | 03 | 16|1950| 04 | 28 20 N| 048 40 £ | 0011 | 00 |
WIND ail ANEMO. AIR AIR TEMPERATURE HUMID- ee CLOUD | SEA SWELL vie. WATER |
DIR. WiSIe HEISE hy TYPE amt.| DIR. AMT. | DIR. [awr. ae TRANS. |
| 00 | | 0 | | 06 |
SUBSURFACE OBSERVATIONS
SAMPLE alt u OG S °/oo ot ZAD O.ml/! vy
DEPTH (M) v y v
STD 0000 16 72189 87 || 2 3A lo Goo
OBS 0000 16 72/89 O87 | 2 34
STD 0010 16 81|40 03 | 29 44 |0 012-
oBg 0010 16 81|40 03 | 29 44
| SURFACE OBSERVATIONS
DATE POSITION SONIC
DEPTH
MO. | DAY | YEAR HOUR LATITUDE LONGITUDE UNCORRECTED} DEPTH
03 | 22| 1950] 05 | 28 40’N| 048 27 E 0007 | 00 |

1
ANEMO AIR AIR TEMPERATURE CLOUD SEA | SWELL | WATER
HGT. | press. EATHER VIS.
[TvPe| aw. DIR. | AMT. | DIR. amt. | a

| 00 | | 0 | | 06

SUBSURFACE OBSERVATIONS
SAMPLE T° S °/oo of = AD O,nl/I vy
DEPTH (M) Vv v v y
STD 0000 if 44139 20 28 65 10 000
OBS 0000 17 44/139 20 Zo oD
STD 0010 10 68 (B39 16 30 © |@ @l2o
OBS 0010 10 &§} (BO ile BOON,

SURFACE OBSERVATIONS

POSITION

LATITUDE LONGITUDE

26 aa Ni O48 27

WIND ANEMO, AIR CLOUD SEA | SWELL |
SPEED DIR. BSc ical DRY v TYPEJAMT.| DIR. AMT. | DIR.
| 1a TW | 2 |

|
SUBSURFACE OBSERVATIONS
SAMPLE 7G Sic/ce ot SAD O, m/l
DEPTH (M) Vv Vv vy v
STD 09000 17 SY IBS eS 28 58 |0 000
OBS) 0000 U7 6D ae 16 28 58
STD 0010 Q8 342 (9 Pil 30 55/0 O14—
OBS 0010 Oe 22 |e Pil BO) BG)

121

SURFACE OBSERVATIONS

POSITION

SUBSURFACE OBSERVATIONS

=
DAD 0, mi/I \
v v v

SAMPLE | Toc | S °/oe ot
DEPTH (M) Vv v
STD 0000 ny Gi se) OZ 28 47 |0 000
OBS 0000 iv @il |e) 2 28 47
STD 0010 WT) (2 |eitsy teXs) 28 36 |0 003=
OBS 0010 U7 © \ee 28 3G

| SURFACE OBSERVATIONS

POSITION
STATION

DEPTH
YEAR HOUR LATITUDE LONGITUDE UNCORRECTED| DEPTH

1950] 04 j MAO NI) O28 27 0007 | 00 |

TEMPERATUR
AIR E HUMID- CLOUD ae SWELL WATER

SAMPLE
DEPTH (M)
STD 0000 18 34 |38 84 28 14 |0 000
OBS 0000 LSPS 43884: 28 14
STD 0010 18 06/38 96 73) “sal {f0) OL
OBS 0010 TS 065/38 39S 2E Bal

SURFACE OBSERVATIONS

POSITION
STATION

SAMPLE
DEPTH (M)

STD 9000
OBS 0000
STD 0010
OBg 0010

122

SURFACE

OBSERVATIONS

NODC POSITION | SONIC MAX.
Ria STATION DEPTH SAMPLE
NO. LATITUDE LONGITUDE JUNCORRECTED DEPTH
00382] 0057 12 | 28 47'N| 048 47 € | 0038 | 00
WIND AIR TEMPERATURE CLOUD SEA SWELL WATER
se (NEMS: ahR. er EATHER VIS. |
SPEED DIR. TYPE|AMT.| DIR. | AMT. | DIR. [an cou] Trans. |
=
[04 34 | 90 | 2 | | 08 |
SUBSURFACE OBSERVATIONS
SAMPLE Toc S "/oo ot = AD O,ml/I Vy
DEPTH (M) v y y v y
STD 0000 40 35
OBS) 0000 40 35
OBS) 0005 17 89 |40 48 2S) 32
STD 0010 RQ) A
OBS 0015 16 64/40 46 29 Bil
STD 0020 40° 33
OBS 0025 40 11
SURFACE OBSERVATIONS
| DATE POSITION SONIC MAX.
STATION DEPTH SAMPLE
| MO. DAY YEAR | HOUR LATITUDE LONGITUDE UNCORRECTED] DEPTH
00382) 0058 | 03 || 27 1950 | is | 2a” 51 N | 048 STE 0024 | 00 |
Re ANEMO.| AIR wis WATER
SPEED DIR. HET., |, PRESS: ‘IcoL.| TRANS.
04 O1
SUBSURFACE OBSERVATIONS
SAMPLE aac) S °/eo ot = AD O,mi/I yy
DEPTH (M) y y y y
STD 0000 18 29/40 42 29 37 |0 000
OBS 0000 18 29 |4@ 42 29 B37
OBS 0005 18 30/40 43 2S) BT
STD 0010 18 13/40 44 29) 4390) O12—
OBS 0015 40 44
Siro) 0020 7 23) |le) 39) Ds) (Sal |) 23
OBS 0025 16 9il Ao » Bo DY. V2
| SURFACE OBSERVATIONS
NODC | DATE POSITION SONIC MAX.
REF. STATION DEPTH SAMPLE
NO. | MO. DAY YEAR | HOUR LATITUDE | LONGITUDE UNCORRECTED] DEPTH
| 00382] 0059 | 03 | 27 1950[15 | 28 56°N| 049 11 E | 0048 | 00 |
WIND rena. A AIR TEMPERATURE SEA svete | WATER |
SPEED DIR. WEN EEE DRY YW WET V AMT. DIR. am,| coL.| TRANS.
04 01 | | | 3 L | 39
SUBSURFACE OBSERVATIONS
' =
SAMPLE re S °/oo ot =z AD O, m/l vy
DEPTH (M) y | y y y
STD 4 0000 18 50|40 47 | 29 35 |0 000
OBS 0000 18 50/40 47 Ds) 5)5)
OBS 0005 18 44 |40 44 DS Bho)
Sip) s || Ooo 40 52
oBS 0015 (A) 3)
STD 0020 40) Be
oBg 0025 40 44

123

SURFACE OBSERVATIONS

POSITION

coL.

TRANS,

we ANEMO
SPEED DIR BGT
[04 01
| SUBSURFACE OBSERVATIONS
SAMPLE Toc S °/oo or = AD O,ml/I vy
DEPTH (M) vy y Y
STD 0000 18 44 |40 39 29 31 10 000 |
OBS 0000 18 44 |40 QS) Bil
OBS 0005 18 44 |40 Bey Bid)
STD 0010 18 27 |40 42 29) B71 |(0) (oil ak
OBS 0015 40 41
STD 0020 17 42 |40 42 ZS) NS) |fo} (24
OBS 0025 16 74 |40 43 2S) i

00382

STATION

SURFACE OBSERVATIONS

POSITION

0061 | 03

MO.

INE ANEMO. AIR
SPEED DIR. | et PMESS:
04 Ol |
SUBSURFACE OBSERVATIONS
SAMPLE T° S °/oo ot DAD O,mi/I yy
DEPTH (M) vy . 7 Vv vy
stp | 0000 18 40140 41 | 29 33 |0 000
OBS 0000 18 4040 41 | 20 32
OBS 0005 18 35140 43 | 29 36
STD 0010 18 15(40 47 | 29 44 |0 012
OBS 0015 ana
STD 0020 17 29/40 43 | 29 63|0 025-
OBS 0025 16 62 \k@ 25 | 20 1

SURFACE OBSERVATIONS

POSITION

LONGITUDE

SONIC MAX.
DEPTH SAMPLE
UNCORRECTED} DEPTH

e7e | 000s | 00 |

0, mi/| ys

SAMPLE 7 ee AS es

DEPTH (M) vy
STD 0000 18 52 \40 55
OBS 0000 18 52 \40 55
OBS 0005 18 55 |40 65
STD 0010 18 19/40 50
OBS 0015 40 44
STD 0020 16 28 |40 47
OBS 0025 14 73/40 60

124

NODC

STATION

SURFACE OBSERVATIONS

DATE POSITION SONIC MAX.
DEPTH SAMPLE
MO. | DAY YEAR HOUR LATITUDE LONGITUDE UNCORRECTED} DEPTH
2 /
03 | 27| 1950 | 20 049. 19 | 0037 | 00

SPEED DIR.

01

SUBSURFACE OBSERVATIONS

SAMPLE icc; S S/o ot = AD O, m/l Vy
DEPTH (M) y y y v
STD Taos 18 55 |40 52 29 38 10 000
” asl 0000 19 55 %@ 92 29 38
OBS 0005 18 B59 AQ a3) BS) Sil
STD 0010 40 48
OBS 0015 40 53
Sip) 0020 BS 33}
OBS 0025 328° 90
SURFACE OBSERVATIONS
NODC DATE POSITION Soule MAX.
REF. STATION SAMPLE
NO. MO. DAY YEAR LONGITUDE UNCORRECTED DEPTH
| 00382| 0064 | 04 | 01 | 1950 048 10 € | 0009 | 00
WIND __|anemo.| air AIR TEMPERATURE WATER
SPEED DIR. HET ERESS:: DRY ¥ WET V COL.| TRANS.
[07 25 03
SUBSURFACE OBSERVATIONS
SAMPLE moc 5 Ws ot = AD O,mi/I vy
DEPTH (M) y y y y
STD 0000 19 ©2/85 25 25 23 |0 000
OBS 0000 IS @2 65 25 25 23
STD 0010 17 62 |BY7 Oil 2& F892 \0 OU)
OBS 0010 U7 ©2187 @i 25 92
SURFACE OBSERVATIONS
NODC lg DATE POSITION
REF. STATION
NO. MO. YEAR | HOUR LATITUDE LONGITUDE
00382| 0065 | 04 1950] 05 | 27" 05 1VE
WIND CLouD SEA
ANEMO.| AIR ee a
—.- EATHER
SPEED DIR. BGT ERE. | TYPE amt,| DIR. | AMT.
02 30 [oe | -
SUBSURFACE OBSERVATIONS
SAMPLE Tee Sic/as T a = AD O, mi/I \%
DEPTH (M) y y y y
STD 0000 19 56/40 64 29 20/0 000
OBS} 0000 19 56/40 64 2S 20)
STD 0010 WS) Be Ao) - Shi BQ 25) \0) Olio
OBS 0010 1S 32 |h0) Sie DE) TAT

" 125

SURFACE OBSERVATIONS

NoDC | POSITION SONIC MAX.
REF. STATION DEPTH SAMPLE
NO. | Mo.

LATITUDE LONGITUDE UNCORRECTED] DEPTH
=

[aae” ate | o0a7 | 00 |

00382 0066 | 04

AIR
PRESS.

ANEMO.

HGT.
DIR. kent

32

01

L SUBSURFACE OBSERVATIONS

SAMPLE Thc S °/oo ot AD O, ml/I vy

DEPTH (M) Vv v Vv
ae

OBS} 0000 18 28 Box

OBS} 0010 17 28 00#

SURFACE OBSERVATIONS

DATE POSITION SONIC MAX.
STATION DEPTH SAMPLE
| MO. DAY | YEAR LONGITUDE UNCORRECTED] DEPTH
-) / Ei 7
o7 | 1950 29. 00 N| 048 48 €

AIR TEMPERATURE
VIS.

DIR. | AMT. DIR. |AMT. p TRANS.
ee ea

02
SUBSURFACE OBSERVATIONS
penne T°c S °/oo ot = AD O, m/l vi
TH (M)
2 ¥ ¥ vy v y
STD 0000 20) ils) ei BS) 26 72 |0 000 ]
OBS 0000 20) ig |s7 Bs) 20 eZ
STD 0010 ie ile BS 7/8) 28) 92 |) WZ
OBS 0010 1g 16 py 79 Be Be

SURFACE OBSERVATIONS

NODC POSITION
REF. STATION
NO. LATITUDE

0068

00382

ee ae aiareeer ie eee CLOUD WATER
HGT. | PRESS. pane eens vis
TPE] [om Jour [oon [rans

02

SAMPLE

O,mi/I vy
DEPTH (M)

STD 95 |0 000
OB
STD 95 10 002
OB

126

SURFACE OBSERVATIONS

Nopc DATE POSITION | SONIC MAX.
REF. STATION DEPTH SAMPLE
NO. MO. DAY YEAR | HOUR LATITUDE | LONGITUDE UNCORRECTED] DEPTH

| 00382] 0069 | 04

28. 40 N| 048 30 € 0015 | 00

ANEMO. AIR
HGT. PRESS.

DIR.

| 08 05
SUBSURFACE OBSERVATIONS
SAMPLE 7 Ye S °/oo ot ZAD O,mi/I Vy
DEPTH (M) Vv v
|
STD 0000 19 79|38 42 | 27 44 |0 000
OBS 0000 19 (les aD | ar a.
STD 0010 19 84(138 63 | 27 59 |0 006
OBS 0010 19 84\b8 63 | a7 59
SURFACE OBSERVATIONS |
POSITION SONIC MAX.
STATION DEPTH SAMPLE
LATITUDE | LONGITUDE UNCORRECTED] DEPTH
35° N | 048 45° € | 0035 | oo |

WIND anemo.| ain | AIR TEMPERATURE | SWELL WATER
HGT. | PRESS. VIS.
SPEED DIR. pRYY | weTy AMT. | DIR. law. cou. | TRANS.
aoe tT eee Ee L#
SUBSURFACE OBSERVATIONS
SAMPLE T°c | S Vee ot DAD O,mi/\ | ‘i
DEPTH (M) Vv v
STD 0000 20 O9 38 2 2 26 10) OOO
OBS 0000 20 09 |38 28 2U 26
STD 0010 ls @2) 38. ©¢ 21 85 0 OW
OBS 0010 19 ©3288 69 Ai 35
SURFACE OBSERVATIONS |
NODC | DATE POSITION SONIC MAX.
REF. | STATION DEPTH _| SAMPLE
NO. | mo. | pay | YEAR | HOUR LATITUDE LONGITUDE UNCORRECTED] DEPTH
: 3 . 7
00382) 0071 | 04 iil || 1OSo0 || Os 29 35 N| 048 45 E 0027 | 00
WIND ee Pe Ee ee cLouD SEA SWELL WATER
ee | aes. yO” WEATHE VIS.
DRYY | WETY TYPE|AMT DIR. [an cot.| TRANS.
06 10 | | | [a | | | 08
[ SUBSURFACE OBSERVATIONS
_—
SAMPLE T°C S °/oo ot = AD O, mi/I 310°
DEPTH (M) v Y v y v | v
STD 0000 20 29 )38 48 2 AS 0 OOO) |
OBS) 0000 20 29 38 48 2 BE
STD 0010 18 64 388 63 2 Sil | OOS
OBS 0010 18 64 38 63 Qt Sil

127

SURFACE OBSERVATIONS

NODC DATE POSITION SONIC MAX.

REF. STATION DEPTH SAMPLE
NO. MO. LATITUDE LONGITUDE UNCORRECTED] DEPTH
00382) 0072 | 04 28° 4O’N| 048 26/E 0011

SPEED DIR.

CLOUD SWELL WATER
ER VIS.
See oe

SUBSURFACE OBSERVATIONS
SAMPLE Tee Ss °/ o DAD O, mi/I Vv
DEPTH (M) y y _ : y | y v Gy
STD 0000 19 83 138 40 27 42 |0 000 ie
OBS} 0000 WS) tis} jeits} (0) 27 42
STD 0010 19 79 38 46 27 47 |0 006
ops) 0010 19 7938 46 27 47
|
SURFACE OBSERVATIONS
array ie
NODC DATE POSITION SONIC MAX.
REF. STATION DEPTH SAMPLE
No. MO. | DAY YEAR HOUR LATITUDE LONGITUDE UNCORRECTED] DEPTH
00382] 0074 | 04 | 16 | 1950 | 09 | 28 55’N| 048 42° E 0035

STD

STD

WATER
ANEMO.
HGT. : any (eAubls
2 j ; : ; COL.| TRANS.
(ooh s

SUBSURFACE OBSERVATIONS

SAMPLE TOS S °/ee

DEPTH (M)

0000 2 Of IBY UT
OBS} 0000 2 O77 bv UT

0010 iS) BS) Bi SE)
OBS| 0010 1G 39 |B7 9

SURFACE OBSERVATIONS

[sre SONIC MAX.
STATION DEPTH SAMPLE
MO. | Hour | LATITUDE LONGITUDE UNCORRECTED] DEPTH

04

ANEMO, AIR AIR TEMPERATURE

HGT. | PRESS. .
pRYY | WETY -| DIR. i ; ; COL. | TRANS.

sal ee LS

SUBSURFACE OBSERVATIONS
SAMPLE moc S °/oo ot =AD O, mi/I ys
DEPTH (M) v v y v y
0000 20 94
OBS} 0000 20 94
0010 Pio) ii | tafe 26 76
OBS| 0010 20) il je7 fe 26 76

128

SURFACE OBSERVATIONS

DATE

POSITION

LATITUDE

NODC

REF. STATION

NO. MO.
00382) 0076 | 04

DAY | Y
(0) || il

EAR HOUR
950/10 | 29.

26'N

LONGITUDE

O47

56 E

WIND ie eneER Aron |
SPEED DIR. oo | RSS DRYY WET ¥ a!
Cas =
SUBSURFACE OBSERVATIONS
SAMPLE T°c S °/oo ot = AD O,ml/I yy
DEPTH (M) y v v
zs ———af
STD 0000 D2 seit Ala 25 86 10 000
oBs| 0000 DE Bh lr Be 25 gs
STD 0010 2i 82 (BY B37 AS iT \0 O20
OBS 0010 Dh D2 Sh7 26 iT
SURFACE OBSERVATIONS
DATE POSITION | SONIC MAX.
STATION DEPTH | SAMPLE
: Mo. | DAY | YEAR | HOUR LATITUDE | LONGITUDE JUNCORRECTED DEPTH
00382| 0077 | 04 | 21] 1950] 04 | 29° 26’N| 047 56 © | 0011 | 00 |
AIR TEMPERATURE CLOUD SEA SWELL WATER
myer. | Ae MuND- enna | vs
DIR. TYPE|AMT.| DIR. | AMT. COL.| TRANS.

SUBSURFACE OBSERVATIONS

SAMPLE moc il °/oo ot = AD
DEPTH (M) vy vy vy y
STD 0000 al aie Br 35 26 06 |0 000
OBS} 0000 Zl Be |b BS 26 06
STD 0010 2 87 Br ae 25 37 0 O20)
OBS) 0010 2il BF IBY Ba 25 87

129

LATITUDE (N) DATE DEPTH SALINITY

LONGITUDE (E)| TIME (GMT) (METERS) iy ac
1951

SHIPS: USS STALLION — USS MAURY

0939

9 FEBRUARY
0939
FEBRUARY (?)

0957
FEBRUARY

0945
FEBRUARY

FEBRUARY

0930
FEBRUARY

0930
FEBRUARY

0930
FEBRUARY

1300
FEBRUARY

0930
FEBRUARY

1205
FEBRUARY

0957
FEBRUARY

0915
FEBRUARY

0000
APRIL

0800
APRIL

Table 6: Surface and Subsurface Salinity Observations (USS STALLION and MAURY), 1951,
U. S. Naval Oceanographic Office, Washington, D. C. Manuscript Data.

130

STATION

NUMBER

SPECIFIC VOLUME
ANOMALY — X 107

4046 2924

“SQUARE
PAG
12 |097| 1951

TUDE LONGITUDE
a0 “W110

31 |SO5 |MU

0010529 |-o000

ORIGINATOR’S

STATION
NUMBER

SPECIFIC VOLUME
ANOMALY — X107|

131

NO,—N|NO,—N
wg-at/!} wg-at/1| pg-at/I

[REFERENCE | erp MARSDEN | STATION TIME | _oriGinator's | DerrH : WAVE cLouD NODC
iam’ | cope | LATITUDE LONGITUDE SQUARE (GMT) CRUISE STATION OBSERVATIONS WATE CODES STATION
uu oie | vo | oe ae now oar a] re or eset] eT NOMEEE

31/SO05|)MU | 2657 N

ss off aon t= A

ceases SOUND | 5 47; | POa—P [TOTAL—P]NO,—N|NO,—N snes!
X 102 VELOCITY 2 »g- sar/l yg-at/! |ug- aA yg-at/|

15246

MESSENGER 2 CAST, SPECIFIC VOLUME
ANOMALY — X 107

WAVE
OBSERVATIONS

NODC
STATION
NUMBER

[ REFERENCE | MARSDEN | STATION TIME [__oricinator’s |
counTaY LATITUDE LONGITUDE a a CRUISE | STATION
cove “0 tno im NUMBER

31|SO5|MU | 2657 N |05003 E

SPECIAL
OBSERVATIONS

mEssnGeR CAST] CARD SPECIFIC VOLUME SOUND PO, —P |TOTAL—P| NO, —N|NO,—N|SIO,—Si
rs 0, mi/I
: ANOMALY — X 107| velocity | ~? meatal iaeciyA yroeccn/ ress ot/1} ug ~at/I

15244

Teese) SHIP MARSDEN | STATION TIME : WAVE a ctouD Nopc
counray| inary | Cope | LATITUDE LONGITUDE SQUARE STATION OBSERVATIONS | ™! 1S —— STATION
CODE | NUMBER sno “no [oar [AR 1710 or NUMBER NUMBER
31|S05| MU 04756 E

SPECIFIC VOLUME SOUND | 9) ai/t PO, —P |TOTAL—P| NO, —N|NO,—N|SIO,—Si
ANOMALY — X 107| VELOCITY a irescu/Al irecty/a psec /l oo -at /1} yg - ~at/I

15099

132

SURFACE OBSERVATIONS

DATE POSITION ] sonic MAX.
STATION DEPTH SAM
YEAR HOUR LATITUDE LONGITUDE JUNCORRECTED DEPTH
1951/10 | 28 13’N] 049° OO E | 00 |
|
AIR TEMPERATURE CLOUD SWELL WATER
pace HUW eare | ‘us
TYPE|AMT. AMT. ata | COL. TRANS.
00 36) | a | 05
SUBSURFACE OBSERVATIONS
SAMPLE TC S °/oo oR > AD Om | y,
DEPTH (M) v y y y v
SHAD) 0000 2s} tis}
OBS) 0000 23 82) AO Or |) 28 Oss
OBS| 0010 BE BY Ro) elke || 27 Ee
SURFACE OBSERVATIONS
eo STATION | ae oN SONIC NAK
* DEPTH SAMPLE
NO. | MO. DAY | YEAR | HOUR LATITUDE LONGITUDE JUNCORRECTED DEPTH
00496] 0002 | ii || 24 1951 | 12 | 28 18'N| 049 o7 Ee | 0029 | 00 |
WIND ANEMOUI AIR AIR TEMPERATURE | cLouD SEA SWELL | WATER
HGT. | PRESS. ITY EATHER VIS
SPEED TyPE|AMT. DIR. | AMT. | DIR. fawr.| COL.| TRANS.
| 03 a [ | 90 | | 26], 2 | | 07
SUBSURFACE OBSERVATIONS
SAMPLE aoc S °/oo ot =AD O, mi/I yy
DEPTH (M) v y y y
STD 0000 Ae, 2
OBS) 0000 BGs 2 \8o) Tea) QU TAS
OBS) 0003 24 90/40 61* |] 27 64%
OBS) 0008 24 82 140 64% | 27 69%
STD 0010 24 80
STD 0020 24 80
OBS) 0020 24 80 |40 53%] 27 61%
| SURFACE OBSERVATIONS
NODC - DATE POSITION | SONIC MAX.
REF. STATION DEPTH SAMPLE
NO. MO. DAY | YEAR HOUR LATITUDE LONGITUDE lUNcORRECTED DEPTH
00496 0003 | 11 2h || WOSU |) we 28 24 N]} 049 i IE | 0032 00
WIND Avene.) AR AIR TEMPERATURE WATER
DIR. Here || MRRESS: DRY ¥ WET YW COL,| TRANS.
| | 06
SUBSURFACE OBSERVATIONS
SAMPLE Toc S "Joo ot SAD O,mi/I ys
DEPTH (M) v Vv Vv v
STD 0000 26 39)
OBS) 0000 DiS 2hS) AO) Sisko) Qi aS
OBS| 0005 26 18
STD 0010 D5 (0) |
OBS 0010 Vy) 0) (40) I OS
STD 0020 25 44
OBS 0020 DS lh, WhO) Gila |] BI Bh7sH
STD 0030 25 34
OBS) 0030 25 34 |40 48%] 27 40%

133

SURFACE OBSERVATIONS

NODC POSITION
REF.
NO.

avene.|| am AIR TEMPERATURE
lsreeo orn. HGT. | PRESS. [Davy
SUBSURFACE OBSERVATIONS
SAMPLE T°c S °/ee ot = AD O, mi/I \
DEPTH (M) v y y y
STD 0000
OBS} 0000 27 (95)
OBS! 0005 2 Sil
STD 0010
OBS 0010 2 ike)
STD 0020
OBS} 0020 AT 20)
STD 0030
OBS} 0030 2U 22

SURFACE OBSERVATIONS

POSITION

SONIC MAX.
DEPTH SAMPLE
UNCORRECTED} DEPTH

[9037 | 00

LATITUDE | LONGITUDE

28 36° N| 049° 33 £

SUBSURFACE OBSERVATIONS
SAMPLE mac I Soe ot = AD
DEPTH (M) Vv Vv Vv Vv
tam =
STD 0000 2s) 162
OBS 0000 25 U2\30 B40 27 719
OBS 0005 25 iki |A@ Al 2@v ae
STD 0010 ZO
OBS 0010 25 SOLE ON Svea | S2i Zo
STD 0020 25 04
OBS 0020 25 04/40 17* | 27 26%
STD 0030 26 24
OBS 0030 26 24140 19* | 26 90%

134

| SURFACE OBSERVATIONS |
NODC DATE POSITION SONIC MAX.
REF. STATION

DEPTH SAMPLE

NO. MO. | DAY YEAR | HOUR | LATITUDE LONGITUDE UNCORRECTED] DEPTH
00496 0006 | 11 | 24] 1951] 18 | 28° 42’N| 049 42’ 0040 | 00

AIR TEMPERATURE WATER
HOMID- WEATHER vis. |
| TYPEJAMT.| DIR. AMT DIR AMT coL.| TRANS. |
| 00 | | a5 || 2 | |
SUBSURFACE OBSERVATIONS
SAMPLE Te S °/eo ot = AD O,mi/I vy
DEPTH (M) Vv Vv Vv v Vv Vv
an || 2s
STD 0000 23 89
OBS| 0000 23 89 40 30% | 27 71%
OBS| 0005 24 94 140 28% | 27 37
STD 0010 24 94
OBS| 0010 24 94139 97% | 27 14
STD 0020 24 96
OBS| 0020 24 96 * #
STD 0030 25 42
OBS| 0030 25 42 \40 19% | 27 16%
SURFACE OBSERVATIONS
| DATE POSITION | SONIC MAX.
STATION DEPTH SAMPLE
| MO. DAY | YEAR HOUR LATITUDE | LONGITUDE UNCORRECTED] DEPTH
00496] 0007 195% |) 20 || 2a~ 49’ N | 049 «STE 0040 | 00
WIND ANEMO AIR SEA SWELL dist WATER
DIR. GIS. PRESS AMT. DIR. jan. COL.| TRANS

05 32 : 25 2 |

SUBSURFACE OBSERVATIONS

—|

SAMPLE TCC [Son ore SAD O,mi/| vs
Leet (M) v v y y v v
STD 0000 23 es)
OBS) 0000 23 s83 40 O38 |) 27 32
OBS! 0005 24 74 |40 28% | 27 was
STD 0010 24 75

OBS 0010 24 75

STD 0020 2a 13

OBS| 0020 Qu 7/3) 40) @Bo || ZY 2B
STD 0030 24 98

OBS 0030 24 98

135

SURFACE OBSERVATIONS

NO

oc
REF. STATION
NO.

YEAR

POSITION

LATITUDE

00496 0008 | 11

24

19)5 il

21 | 28 54’N

ae i ANEMO.| AIR
Sn HGT. | PRESS.
03 |
_ SUBSURFACE OBSERVATIONS
SAMPLE T°c S °/oo ot = AD O, mi/I vy
DEPTH (M) v v v v y vy
STD 0000 22 22
OBS! 0000 QED 22
OBS 0005 Ale Oil (0) Os |) 2 . Bil
STD 0010 246 9)
ops 0010 24 S140 Ole |-27 18
STD 0020 Due Ss)
OBS| 0020 at Ssh 0) WAS || BT DT
STD 0030 25 96
OBS) 0030 Ay S36 to Asiur || 2 Oe:
SURFACE OBSERVATIONS
NODC | DATE POSITION SONIC MAX.
REF. STATION DEPTH SAMPLE
NO. | MO. UNCORRECTED] DEPTH

004964 0009 | 11

WATER

TRANS.

SUBSURFACE OBSERVATIONS |

SAMPLE Tacc S °/oo cn = AD O, mi/| \
DEPTH (M) v st v v v Vv
0000 Diu OA
0000 21 9440 35%) 28 32%

0005 24 91 |40 30* | 27 40%
0010 24 92
0010 26 Of h0) Bile | 27 Beit
0020 24 93
0020 24 93140 25%] 27 36%
0030 25 44
0030 Zi ih Ao) sh T/er || BT 2Eha|

136

00496) 0010

STATION

SURFACE OBSERVATIONS

LAT

POSITION

| SONIC

ITUDE- LONGITUDE

MAX.
SAMPLE
DEPTH

2a 42’nN| 050° 38 E

DEPTH
UNCORRECTED
f 0036 | 00 |

AIR TEMPERATURE [ CLOUD SEA SWELL | WATER
ANEMO. AIR HUMID-
EATHER; vis.
SPEED DIR. ISH FREES: Uy a DIR. AMT. DIR. AMT. ory
02 01 | | 00 | Ea | |
SUBSURFACE OBSERVATIONS
SAMPLE T°c S °/oo ot = AD O, mi/| \
DEPTH (M) y y vy v

STD 0000 23 il

OBS} 0000 23 (il (AO) dae |) 2 Veh

OBS! 0005 Pik Tal Wo) aoe |) ea shila)
STD 0010 24 71

OBS) 0010 Be Tail NAO) Wz || BY Bees
STD 0020 Do, lb

OBS) 0020 Bi TES N80) UB || BT BP)
STD 0030 25) {0}

OBS} 0030 Be (05) AO OB | Br Boral

SURFACE OBSERVATIONS
POSITION | SONIC
REF. | STATION DE
HOUR LATITUDE | LONGITUDE
00496 o3 | 28° 35’N

WIND

CLOUD

Ry
TYPE|AMT. DIR.

[ [36

COL.| TRANS.

SUBSURFACE OBSERVATIONS

SPEED DIR.
@Q2 22
SAMPLE Toc S °/oo ot
DEPTH (M) v v
STD 0000 24 06
OBS) 0000 24 06 |40) (O62 ||) 27
OBS| 0005 De TS AO) OSs | 27
STD 0010 24 74
OBS 0010 24 74
STD 0020 24 713
OBS 0020 24 73140 03% | 27
STD 0030 Ze) BNie)
OBS 0030 23) Be WA0) Og | QT

= AD

v

O,mi/|

60%

137

SURFACE OBSERVATIONS

POSITION SONIC MAX.
DEPTH SAMPLE
LONGITUDE UNCORRECTED] DEPTH

COL.| TRANS.

SAMPLE Toc S °/oe
DEPTH (M) v
STD 0000 23 94
OBS| 0000 23 94 140 O8* j
OBS| 0005 24 67140 05*| 27 228
STD 0010 24 66
ops 0010 «=| 24 66/39 99%| 27 244
STD 0020 A BG
OBS| 0020 24 66 140 05*|27 294
STD 0030 25 21
OBS| 0030 25) 2140 ose 27 lle

SURFACE OBSERVATIONS

POSITION

ANEMO. | AIR AIR TEMPERATURE

HGT. | PRESS.

COL.| TRANS.

SAMPLE
DEPTH (M)
STD 0000
OBS} 0000
STD 0010
OBS 0010
STD 0020
OBS 0020
STD 0030
OBS} 0030
OBS 0040

138

SURFACE OBSERVATIONS

STATION

POSITION

HOUR | LATITUDE

LONGITUDE

UNCORRECTED] DEPTH

SONIC MAX.
DEPTH SAMPLE

“n | 050

139

0014 [11 | 25[ 1951] 07 | 28 14 06 & | 0053 | 00
WIND AIR TEMPERATURE CLOUD | SEA | SWELL WATER
ANEMO. AIR HUM D:
Gann ia VIS.
SPEED DIR. Hiei. NESS TYPE/AMT.} DIR. AMT. | DIR. lan. lcon TRANS
24 00 0 | | |
SUBSURFACE OBSERVATIONS
SAMPLE T°c 5 °/oo ot DAD 0, mi/| y
DEPTH an vy v v Vv
STD 0000 24 33
OBS! 0000 24 33/39 99% | 27 34%
STD 0010 25 39
OBS| 0010 25 39 139 99%] 27 O2H
STD 0020 25 38
OBS) 0020 25 3) |B) O23 || 26 Se
STD 0030 25° 31
OBS) 0030 25 31/19 92%] 26 90x
STD 0050 25 28
OBS| 0050 25 28139 94*| 27 01%
SURFACE OBSERVATIONS
NODC DATE POSITION SONIC
REF. STATION DEPTH
pay | YEAR LATITUDE | LONGITUDE UNCORRECTED] DEPTH
0015 | 11 | 25 | 1951 28 08’ N| 049 58 E 0045 | 00 |
WIND ANEMO. AIR AIR TEMPERATURE HUMID- CLOUD SEA SWELL
HGT. | PRESS. pin” MABANULHets
SPEED DIR. DRY W WET WV TyPE|AMT. DIR. AMT. DIR.
|03 35 | | | | oo] | | eo] e
SUBSURFACE OBSERVATIONS
= SAMPLE T°c S °/oo ot > AD O,ml/I 7
(M)
v vy y
STD 0000 24 89
ORS) 0000 24 89139 94%| 27 134
STD 0010 25 46
oRS| 0010 25 46/139 90%] 26 934
STD 0020 D5 3\5)
ORS| 0020 25 33 (39 96x | 27 O14
STD 0030 25 35
OBS) 0030 25 35 |39 92%] 26 97%
ORS| 0040 26 30/40 03% | 26 764

SURFACE OBSERVATIONS

POSITION SONIC MAX.

:
7

0043 00

WATER

ANEMO.

SPEED DIR. HGT- | wery | iTvPe| 7 TRANS.

03) 35

SAMPLE
DEPTH (M)
STD
OBS
OBS
STD
OBS
STD
OBS
STD
OBS

SURFACE OBSERVATIONS

POSITION

DATE |

STATION |
MO. DAY YEAR HOUR LATITUDE
foie eae | Sass ie
WIND ANEMO AIR AIR TEMPERATURE HUMID WATER
2 ~ WEATHER f
SPEED DIR HK a | DRYYW WETW Ua COL.
03 35 | | | |
SAMPLE Tee S °/oo or ZAD O,mi/I Vy
DEPTH (M) v y v Vv v Vv
STD 0000 25 28
OBS 0000 25 28\40 os*| 27 124
OBS 0005 25 50 |40 12*| 27 08%
STD 0010 25 50
OBS 0010 | 25 50 |40 14*| 27 00%
STD 0020 25 50
OBS 0020 25 50|40 06*| 27 03%
STD 0030 ey itl
OBS 0030 26 10 |40 o8*| 26 86%

140

SURFACE OBSERVATIONS

DATE POSITION SONIC MAX.

STATION DEPTH SAMPLE
DAY YEAR | HOUR LATITUDE | LONGITUDE JUNCORRECTED DEPTH
00496 0018 25 1951 | is ar 48’ N | 049 «434 € | 0036 | 00 |

Be ANEMO.| AIR
SPEED DIR. nee eee 5 ? : : ; COL.| TRANS.
[03 35 |
SUBSURFACE OBSERVATIONS
SAMPLE T°c S ho ot = AD O, mi/| yy;
DEPTH (M) y
v v voiy v ¥
STD 0000 24 67
OBS) 0000 De © (sO ye] BY B77
OBS| 0005 25 iS AQ 2s) 2 2G!
STD 0010 25 14
OBS) 0010 DS We AO) Besley || 21 Zea
STD 0020 Bs) INS)
OBS 0020 25 WBiA@Q 2b] 2v 2ex
STD 0030 23) ©7/
OBS) 0030 DS) (i lo) BO || 2 sabes}
SURFACE OBSERVATIONS
NODC POSITION SONIC MAX.
REF. STATION DEPTH SAMPLE
NO. LATITUDE LONGITUDE UNCORRECTED] DEPTH
00496 0019 367 Ni W298 BEE 0011 | 00 |
AIR TEMPERATURE CLOUD SEA SWELL WATER
Al
MGT. | PRESS. MY) WEATHE WHE:
SPEED DIR. DRY ¥ WET ¥ TyPE|AwT.| DIR. | AMT. | DIR. |AMT. COL.| TRANS:
| | | 00 | | oo | 0 05
SUBSURFACE OBSERVATIONS
ers, T 3 5.%bo ot SAD O, mi/| y
v v v v v
STD 0000 24 94 |
OBS) 0000 24 94 |40 37% | 27 44%
OBS) 0005 DE 7 (ee) Sher |) BY B=
STD 0010 23 1/0)
OBS) 0010 23 70 |40 68%} 28 064

141

SURFACE OBSERVATIONS

POSITION

SUBSURFACE OBSERVATIONS
oar nec S °/oo ot ZAD O, mi/I vy
v v v v v v

stp |0000 |18 33

ops} 0000 «| 18 «433 40 90% | 29 73

OBS 0005 17 80
sTD | 0010 |16 94

OBS 0010 | 16 94 (40 88*| 30 06
STD) h0020) | Ipt7e59

ops 0020 |17 59 40 88*| 29 90%
Sip | || GOSO | AY BS

ops} 0030 «=| 17 85 \40 82* | 29 5)

SURFACE OBSERVATIONS

DATE POSITION SONIC :
DEPTH
ay | year | Hour | LATITUDE LONGITUDE UNCORRECTED] DEPTH
02

copase| ee [oe conf os SE]

ANEMO. AIR AIR TEMPERATURE HUMID- CLOUD WATER
HGT. PRESS.
DRYY Bu TYPE|AMT. lam. TRANS.

STATION

SAMPLE | S °/oo ot
DEPTH (M) v y
STD 0000 19 44
OBS| 0000 19 44 |40 90%
OBS 0005 16 83/40 86%
STD 0010 1G g
OBS 0010 16 63 |40 88%
STD 0020 16 88
OBS 0020 16 88
STD 0030 17 «(08
OBS 0030 17 08 |40 86%

142

SURFACE OBSERVATIONS

POSITION | SONIC MAX.
STATION DEPTH SAMPLE
YEAR HOUR LATITUDE ie LONGITUDE isattianl DEPTH
00496 0015 | 02 1952] 24 | 28 08’N| 049 58E 0047 | 00
CLOUD | SEA | SWELL WATER |
VIS.
TYPEJAMT.| DIR. AMT. | DIR. [an coL.| TRANS |
SUBSURFACE OBSERVATIONS
SAMPLE T°c Sic/an ct SAD O, mi/I ys
DEPTH (M) Vv L Vv Vv Vv
STD 0000 WW? 768
OBS| 0000 17 78 \40 88*|29 85
STD 0010 1G OF
OBS| 0010 16 07 |\40 88*| 30 274
STD 0020 15 oe
OBS| 0020 15 42 |40 82¥| 30 384
STD 0030 1@ 12
OBS| 0030 16 12140 84%] 30 23%
OBS| 0040 16 17140 82*| 30 204
SURFACE OBSERVATIONS
ie POSITION | SONIC MAX.
DEPTH SAMPLE
DAY YEAR HOUR LATITUDE LONGITUDE UNCORRECTED cau
| 21 | 1952 Tn a os oocae | 0047 | 00

SEA SWELL WATER
nee me
DIR. | AMT. DIR. [awr.| COL.| TRANS.
SUBSURFACE OBSERVATIONS
SAMPLE Tac) | S °/oo ot = AD O, mi/I \7
DEPTH (M) Vv Vv Vv Vv
STD 0000 lv 22
OBS) 0000 il? 22180 98) 30 OB:
STD 0010 1D 38 |
OBS 0010 1% se FO Ga} S@ 27
STD 0020 ld 9B
OBS 0020 40 86% 4
STD 0030 13 Di
OBS 0030 13 O97 BOQ sac |) 0) 27
OBS 0040 16 74 |40 80* | 30 05%

143

NODC

REF.
NO.

+——

STATION

SAMPLE

DATE

POSITION SONIC MAX.
DEPTH SAMPLE
1952 Denn aul Nu OSOn ae 0053

SURFACE OBSERVATIONS

DEPTH (M)

SURFACE OBSERVATIONS

POSITION

LONGITUDE
oso ave

SUBSURFACE OBSERVATIONS
—
SAMPLE T°c S °/eo ot =AD 0, mi/I \
DEPTH (M) y Y v v
0000 20 00
OBS) 0000 20 00
0010 16 68
OBS 0010 16 68 40 26% | 29 65%
i 0020 15) 8!
OBS 0020 IZ Bil AO Hocus |) sho) oer
0030 ie Ss)
OBS 0030 16 G3 @ sr) 29 oy
OBS 0040 1G O80) Bere} 29) 176

144

SURFACE OBSERVATIONS

NODC DATE | POSITION SONIC

REF. STATION DEPTH

NO. MO. DAY | YEAR HOUR | LATITUDE | LONGITUDE UNCORRECTED] DEPTH
05 28

| 00496 0011 | o2 | 21| 1952 Y

35 n| 050 30 €E 00

| SWELL WATER
vis.
amt. | DIR. |AMT.| — |COL.| TRANS.
SUBSURFACE OBSERVATIONS
SAMPLE TOG S\°/co ot = AD O, mi/I \y
DEPTH (M) v v v y y y
STD 0000 ii} BN)
OBS) 0000 1g $3
STD 0010 16 16
ops 0010 1G WS AQ Beier || BS 7/5,
STD 0020 ie 27 :
OBS 0020 16 27 |40 14%) 29 eee
Srp) 0030 ie) | teh 7/
OBS 0030 16 87 40 O5%}] 29 44%
OBS) 0040 ie 2

SURFACE OBSERVATIONS

POSITION SONIC MAX.
DEPTH SAMPLE
LONGITUDE UNCORRECTED] DEPTH

STATION

| 00496 0010 | 02

WIND ANEMO.| AIR WATER”
SPEED DIR. HET ERESS: leon.) trans. |
| pias

SUBSURFACE OBSERVATIONS
SAMPLE T&G S °/eo ot = AD O,ml/I yy
DEPTH (M) y v v v y Y
STD 0000 18 89
OBS) 0000 18 89 OO Os | 28 95
STD 0010 WS) Ba
OBS 0010 19 34 140) 55%) 29° 19
STD 0020 Zi 29
OBS 0020 Si 2S) 40 Bile |) 25 Sil
STD 0030 Zi O
OBS 0030 Zi (os) Ao) ior |] Bish (2
bail 0040 US) Io) Ee) Safar |] 2S) Baye

145

SURFACE OBSERVATIONS

DATE POSITLON

Rees STATION

EPTH
YEAR HOUR LATITUDE LONGITUDE UNCORRECTED DEPTH

no sowe [ox [masse] [oo oral eso" oF [ame [0

WATER

COL.) TRANS.

SAMPLE = AD O, mi/I vi

DEPTH (M)

STD 0000
OBS} 0000
OBS} 0005

STD 0010

STD 0020
OBS) 0020

STD 0030
OBS} 0030

SURFACE OBSERVATIONS

NODC DATE ee oneaercsi ens ny) aa seule MAX.
REE: STATION SAMPLE

SPEED DIR.

SAMPLE
DEPTH (M)

STD 0000
OBS) 0000
OBS| 0009

STD 0010
OBS 0018

STD 0020
OBS 0027

STD 0030
OBS) 0036

146

STATION

SURFACE OBSERVATIONS

DATE

YEAR | HOUR

1952 | 01

| POSITION SONIC MAX.
DEPTH SAMPLE
LATITUDE | LONGITUDE UNCORRECTED] DEPTH
; . : =
28 49 N | 049 «SIE 0048 | 00

AIR TEMPERATURE

PRESS.

STD
OBS
OBS

STD
OBS

STD

OBS
STD
OBS

SAMPLE
DEPTH (M)

0000
0000
0008
0010
0016
0020
0025
0030
0033

COL.

TRANS.

SUBSURFACE OBSERVATIONS

T°C S °/oo ot
v Vv
lg 33)
its} Bis} Ao) 7 7i |) BS Oss
iff I@ |h0 6274) 29 Bal
U7 Ao)
15) 57 140) “90Rs ||| 30) “4ule4
Ie Bi
17 46 40 70* |] 29 80%
17 93
it) OG 80) skis |) BS 7/3)

NODC
REF. STATION
NO.

DATE

SURFACE OBSERVATIONS

HOUR
14

POSITION SONIC MAX.
DEPTH SAMPLE
LATITUDE LONGITUDE UNCORRECTED] DEPTH
7 o /
42 N | OAC = 0044 | 00

=z AD

O,ml/I

HUMID

| 2a

| CLOUD

SE

AMT.

DIR.

A
AM

WATER

COL.} TRANS.

EATHER
iy TYPE
01

[

SWELL |
VIS.
T. | DIR. |AMT.
1

10

SUBSURFACE OBSERVATIONS

SAMPLE Tee Sieae ot SAD O.mi/I vs
DEPTH (M) vy Vv v
STD 0000 i? ve
OBS) 0000 17 78 40 93% | 29 89%
OBS 0009 13 90/40 88*| 30 78%
STD 0010 14 48
OBS 0018 17 49/40 82% | 29 88%
STD 0020 il? 32
OBS 0026 ly SO AO Bears |) 2S He)

147

NO
Ree

SPEED DIR.

oc DATE Rares ry
STATION
33 E

SURFACE OBSERVATIONS

ANEMO.
HGT.

AIR
PRESS.

SAMPLE
DEPTH (M)
OBS
OBS
OBS
OBS
OBS
SURFACE OBSERVATIONS
DATE POSITION
STATION

YEAR | Hour | LATITUDE LONGITUDE

00496 0004

re [oie |e :

WIND

SPEED DIR.

ANEMO.
HGT.

AIR
PRESS.

13

STD

STD

STD

STD

SAMPLE
DEPTH (M)

0000
OBS) 0000

OBS 0008
0010
OBS 0015
0020
OBS 0023
0030
OBS 0031

148

SURFACE OBSERVATIONS

| POSITION

SONIC MAX.
DEPTH SAMPLE
LATITUDE | LONGITUDE UNCORRECTED] DEPTH

SWELL WATER |
VIS.
SPEED DIR. DIR. [amr COL.| TRANS. |
fe SUBSURFACE OBSERVATIONS
SAMPLE ToC S °/eo ot = AD O,mi/I vy
DEPTH (M) y y y y y
STD 0000 2k wal
OBS) 0000 Zul al (te Se Sy ah yaa
OBS; 0005 21 45 141 24% | 29 14%
STD 0010 21 46
OBS 0010 Bil 46 |41 29% | 29 18%
SURFACE OBSERVATIONS
NODC | DATE POSITION
REF, | STATION
: Mo | DAY | YEAR | HOUR | LATITUDE | LONGITUDE
00496 0002 | 04 | 09 | 1952] 10 eRe a) Reon ae
WIND AIR TEMPERAIURE WATER |
ANEMO.| AIR HUMID-
——} EATHER
HO |) PRE em | Ge ITY . CoL.| TRANS. |
—————
03° 21 | | |
SUBSURFACE OBSERVATIONS
SAMPLE Tc 5 °/ee ois SAD O,mi/l vi
DEPTH (M) | y Y y y y y
STD 0000 Bil si9)
OBS} 0000 Peles SN | HOMO OPcniee ee olOR
OBS) 0005 2 35 [AQ O62 || 264 27
STD 0010 20 44
OBS 0010 20' 44 140) 1676) 28 ail
STD 0020 20 04
OBS| 0020 20) O44 40) 9ivee | 219 33%

149

SURFACE OBSERVATIONS

NODC DATE POSITION
REF. STATION E
NO. YEAR | HOUR LATITUDE LONGITUDE UNCORRECTED] DEPTH

00496 0003 | 04 | 09 1952 | ii | ee ae Ni) Ge” Ave | 0038 | 00

WIND anemo.| ain | AIR TEMPERATURE WATER |
SPEED DIR. HGKer FesESS. DRY V WETY COL.| TRANS. |
[o1 21 | 12

aE
SAMPLE
DEPTH (M)
i
STD 0000 ae,
OBS) 0000 Be Tis WAAL SiByer ly ie} taht
OBS 0005 1S Si thi Bis} 2e eZ
STD 0010 WS) UY
OBS 0010 19) U7 tei “Zee | 29 Wee
STD 0020 WE Wy
OBS 0020 wey 7? fal Bie) 2S) 7S]
OBS} 0030 41 35% %

SURFACE OBSERVATIONS

| POSITION | SONIC
STATION

DEPTH
LATITUDE | LONGITUDE UNCORRECTED] DEPTH
a 7 & 7
2 Oa N | 049 24 E

WATER

TyPE| AMT. | DIR. | amr.

DIR. AMT. ; coL.| TRANS.
| | 21| 1

SUBSURFACE OBSERVATIONS

SAMPLE y Se Si°/eo ot = AD
DEPTH (M) Vv y vy vy
STD 0000 23 33)
OBS} 0000 Bs) S)6) [AO) Bilt? || BE 11
STD 0010 19 41
OBS) 0010 19 41/140 62% |} 29 23
STD 0020 18 D6
OBS) 0020 18 56/40 86%) 29 64
STD 0030 18 48
OBS 0030 18 48 |40 97% | 29 74
OBS 0040 17 OF Et OOx |) 2 Sal

150

SURFACE OBSERVATIONS

NODC DATE POSITION SONIC MAX.
REF. STATION DEPTH SAMPLE
NO. MO. | DAY | YEAR HOUR LATITUDE oa UNCORRECTED| DEPTH
00496 0005!] 04 | 09] 1952] 14 | 28 oe OAD a | 0047 | 00
WIND ANEMO. AiR AIR TEMPERATURE HUMID- fre fermen SEA SWELL WATER |
SPEED DIR. : y TYPE|AMT. AMT. DIR. COL.} TRANS.
01 20 15
SUBSURFACE OBSERVATIONS
SAMPLE T°C S °/oo ot |] Zap O, mi/I y =|
DEPTH (M) vy || v y v
STD 0000 23 06
OBS| 0000 23 06 40 68% | 28 25
STD 0010 10 73
OBS| 0010 18 73 140 55% | 29 35
STD 0020 19 81
OBS| 0020 19 81/|40 57*|] 29 08”
STD 0030 21 94
OBS| 0030 21 94 |40 61*| 28 52%
SURFACE OBSERVATIONS
NODC | DATE | POSITION SONIC MAX.
REF. STATION DEPTH SAMPLE
NO. | MO. | DAY YEAR | HOUR | LATITUDE LONGITUDE UNCORRECTED] DEPTH
00496 0006 | 04 | 09 1952 | 15 28" 42’ N | O95 a2’ b 0047 | 00
WIND 13 ANEMO. AIR SWELL [ee WATER
SPEED DIR. BSUS! | ERIS. AMT. DIR [ant cou. | TRANS.
02 08 | 1 | | 15 |
SUBSURFACE OBSERVATIONS
SAMPLE iTacc S "Jeo ot = AD O, ml/I Y
DEPTH (M) V y v v
STD 0000 24 17
oBS| 0000 24 17(40 50*|27 78%
STD 0010 18 70
OBS 0010 18 70/40 61*| 29 414
STD 0020 ome
OBS| 0020 19 36 |\40 57*| 29 20%
STD 0030 DO ath
OBS| 0030 20) 24 40) rie) 29) 2s
OBS| 0040 40 79% 4

151

SURFACE OBSERVATIONS

POSITION SONIC MAX.
DEPTH SAMPLE

UNCORRECTED] DEPTH

DIR.

LATITUDE LONGITUDE
28 49’N| 040 5a Ee

02 08

See a T y Po ot y y = AD 4 | Vy y
STD 0000 23 00 |
ORS} 0000 23 00 40 37* | 28 03%
STD 0010 20 31
OBS| 0010 20 31 (40 30* | 28 74%
STD 0020 19 «75
“ OBS 0020 19 75 |40 44% | 29 oe
STD 0030 18 61
ORS, 0030 18 61/40 73% | 29 22)
ORS| 0040 40 71¥

SUBSURFACE OBSERVATIONS

SURFACE OBSERVATIONS

00496

POSITION SONIC MAX.

STATION DEPTH SAMPLE
fe YEAR HOUR | vatituve | LONGITUDE UNCORRECTED] DEPTH
2 /
1952] 18 a 54’ N 59 E |

Ain | SWELL
DIR. RRESS: DIR. |AMT. ‘Icot.| TRANS.
10
SUBSURFACE OBSERVATIONS
SAMPLE TAG Sie/aes ot = AD O, m/l 7
DEPTH (M) v y v y v y
all
STD 0000 21 94
OBS| 0000 Bil SA WA) Or |) Ae} BB.
STD 0010 2:0)- 181
OBS 0010 20 81/40 34% | 28 63%
STD 0020 iG) ys) ,
OBS 0020 19 BO 462] 29 7
STD 0030 18 84
OBS 0030 18 84 |40 66* | 29 41%
OBS 0040 18 @s) (20) Om || 29 173,

152

SURFACE OBSERVATIONS

STATION

POSITION

SONIC

MAX.

DEPTH SAMPLE
LATITUDE LONGITUDE UNCORRECTED] DEPTH
00496 0010 | 28 42’N| 050 38 | 0042 | 00 |
ANEMO. AIR SWELL | ia WATER
DIR. WISus | PSS DIR. |AMT. COL.| TRANS
SUBSURFACE OBSERVATIONS
SAMPLE T 4 S °/oo ot ZAD O,ml/I vy y
DEPTH (M) Vv vy
STD 0000 23 33
oBSs| 0000 23 33
STD 0010 20 86
ons 0010 20 86|39 90*| 28 284
STD 0020 20 16
OBS 0020 20 16 (39 96%| 28 52%
STD 0030 19 86
OBS 0030 19 86 139 99%] 28 63
OBS 0040 19 27|40 06*| 28 84
SURFACE OBSERVATIONS
NODC | DATE POSITION | SONIC MAX.
REF. STATION DEPTH SAMPLE
NO. | MO. DAY YEAR | HOUR Z LATITUDE : LONGITUDE —— DEPTH
00496 0009 | 04 | 09 1952|1 19 01’ Nn | 050 OF E 0047 | 00 |
AIR TEMPERATURE CLOUD SWELL WATER
TYPE|AMT.| DIR. AMT. DIR. lant. COL.} TRANS.
10

[

SUBSURFACE OBSERVATIONS

SAMPLE moc S °/oo
DEPTH (M) vy
STD 0000 23)
OBS} 0000 25 00 40 70*
STD 0010 20 18
OBS) 0010 20 18 [40 44%
STD 0020 1s) ws)
OBS) 0020 19 19 40 57%
STD 0030 18 86
OBS) 0030 18 86 |40 59%
OBS) 0040 18 36 |40 62*

ot

= AD

Vv Vv

O,ml/I

Mj

35%
50%

153

SURFACE OBSERVATIONS

STATION

| 00496 0011 (co a aores

WIND ANEMO. AIR AIR TEMPERATURE
SPEED HGT. PRESS.

SUBSURFACE OBSERVATIONS |
SAMPLE Too S °/oe ot AD O,ml/I vi
DEPTH (M) Vv Vv Vv v Vv vy
STD 0000 aS) Te
OBS) 0000 23 78 |40 12%] 27 61%
STD 0010 20 65
OBS| 0010 20 65 |40 10* | 28 49%
OBS 0019 19 85 40 35*| 28 90
STD 0020 19 80
STD 0030 19 30
OBS| 0038 18 91/40 39% | 29 18%
STD 0050 18 35
OBS| 0057 18 04 |40 53% | 29 52

SURFACE OBSERVATIONS

NODE DATE fa. bepetrosione) ot) © na SONIC MAX.
STATION EPTH SAMPLE

SUBSURFACE OBSERVATIONS
SAMPLE ToC q ot SAD 0, mi/I ys

DEPTH (M) y i y y Y y
STD 0000 23 67

ORS 0000 23 67/40 61* | 28 O1%
STD 0010 20 86

OBS 0010 20 86/40 34% | 28 62

OBS 0019 19 60/40 35% | 28 274
STD 0020 19) Be)

OBS 0029 19 36 40 44%] 29 10%
STD 0030 19 oe

OBS 0048 17 96 |40 66* | 29 644%

154

SURFACE OBSERVATIONS

POSITION SONIC

STATION DEPTH
| mo. | oay | YEAR HOUR LATITUDE LONGITUDE IUNCORRECTED| DEPTH

/

AY
00496 0013 10 28 14 N| 050 O68 € 0056 | 00

RE PAIR TEMPERATIRE | cLouD SEA SWELL WATER |
HGT. | PRESS. Ta ESE ] VIS.
SPEED DIR. TYPE|AMT.| DIR. | AMT. | DIR. lant. COL.| TRANS.
01 20 o1| 20 | 1 | |

| SUBSURFACE OBSERVATIONS

SAMPLE 7 °c S °/oo ot DAD O,mi/| \%
DEPTH (M) v y v v y vy

78

78 |40 80* | 28 42

56

56 140 57% | 28 88

10

10 |40 80*] 29 45

82

82 |40 82% | 29 54

09

09 40 86% | 30 25

SURFACE OBSERVATIONS

NODC DATE POSITION | SONIC MAX. ;
REF. STATION DEPTH SAMPLE
No. MO. ‘| pay YEAR HOUR LATITUDE LONGITUDE UNCORRECTED] DEPTH

00496 0013 | 04 | 10 152 | O20 ize ea oso TRE 0058 | 00 |

WIND

ANEMO. AIR AIR TEMPERATURE | ne CLOUD SEA | SWELL fea WATER |
: “| DRYY WET ¥ ly TYPE/AMT.| DIR. AMT. | DIR. lant. cou.| trans. |
| | =O Pa ee ne
SUBSURFACE OBSERVATIONS
SAMPLE T°c S °/oo ot = AD O,ml/I 17
DEPTH (M) v Vv Vv v Vv vy
STD 0000 23 06 |
OBS| 0000 23 06 |40 52 | 28 1g
STD 0010 20 03
OBS| 0010 20 03 |40 39% | 28 89%
STD 0020 19 68
OBS| 0020 19 68 40 34% | 28 94%
STD 0030 19 «13
OBS| 0030 19 13/40 62* | 29 30%
STD . | 0050 18 30
OBS} 0050 18 30/40 95 | 29 te)

155

SURFACE OBSERVATIONS

NODC ~ POSITION SONIC MAX,
REF. STATION DEPTH SAMPLE
DAY UNCORRECTED| DEPTH

NO.
oe [a0 see | oor | 00 |

WIND ee Pe iceareraie | ee | cuouo | SWELL WATER
HGT. | PRESS. ITY eave |
SUBSURFACE OBSERVATIONS

SAMPLE = vs
DEPTH (M) v v Y Y
STD 0000 Zit (S7/
OBS} 0000 21 67 |40 71* | 28 67%
OBS} 0007 21 20/40 84* | 28 91%
STD 0010 20 46
OBS 0017 19 30/40 97%] 29 53%
STD 0020 1S) Wé
OBS! 0026 18 97/40 84* |} 29 51%
STD 0030 18 84
OBS} 0046 18 45 |40 77* | 29 60%

SURFACE OBSERVATIONS

POSITION SONIC MAX,
STATION DEPTH SAMPLE
LATITUDE LONGITUDE UNCORRECTED] DEPTH
y 7

WIND Aral Ap || Acie |e | cuouo |
HGT. | PRESS. ITY eave |
a on Ee ice
6

ee a eo

SUBSURFACE OBSERVATIONS
SAMPLE ue S °/eo 1 ot = AD O, mi/I Ys
DEPTH (M) y y v v v v
STD 0000 21 94
OBS| 0000 21 94 |40 70* | 28
STD 0010 22 {os
OBS 0010 22 06 |40 82* | 28 65%
STD 0020 l9 @&
OBS 0020 19 66 |40 88* |] 29 36%
STD 0030 19 34
OBS) 0030 19 34 |40 88* | 29 45%
OBS) 0039 18 84 |40 91* | 29 60%

156

SURFACE OBSERVATIONS

NODC POSITION | SONIC MAX.
REF. STATION DEPTH SAMPLE
NO. YEAR LATITUDE LONGITUDE UNCORRECTED] DEPTH
00496 0017 | 04 | 10| 1952 27 ++53’N| 049 43’ E
AIR TEMPERATURE CLOUD SEA SWELL WATER
Huw al VIS.
WET ¥ TYPE|JAMT.| DIR. AMT. DIR. AMT. COL.| TRANS.
| 01 | 16 | 2 | | |
SUBSURFACE OBSERVATIONS
SAMPLE T °c S */eo ot SAD O,mi/| vi “|
DEPTH (M) Vv Vv Vv Vv
OBS| 0000 40 95% x
OBS| 0009 20 53 140 95% | 29 18
STD 0010 20 49
OBS| 0019 20 17 |40 86* | 29 21%
STD 0020 20 4
OBS} 0028 19 84 |40 91% | 29 34%
STD 0030 19 74
OBS| 0038 19 24 40 91% | 29 4
SURFACE OBSERVATIONS
NODC DATE | POSITION SONIC MAX.
REF. STATION DEPT: SAMPLE
No. MO. | DAY YEAR | HOUR | LATITUDE LONGITUDE luNcoRRECTED DEPTH
| Tne 0018 | 04 | 10] 1952] 09 | 27 48’ N| 049 34 & | 0042 | 00
WIND ANEMO. AIR TEMPERATURE SEA | SWELL | ie WATER |
SPEED DIR. HEU AMT. | DIR. an,| COL.| TRANS. |
18 1 | | 17 |
SUBSURFACE OBSERVATIONS
SAMPLE TAC) 3 Yoo ot = AD O, mi/I v7
DEPTH (M) Vv Vv v vy vy
STD 0000 22 2
OBS} 0000 22 22 140 99% | 28 73%
STD 0010 20 60
OBS| 0010 20 60140 93% | 29 14%
STD 0020 19 86
OBS} 0020 19 86 40 86* |] 29 29%
STD 0030 19 76
OBS 0030 19 76/41 15* | 29 54%
OBS 0049 19 27 |41 417* | 29 69%

157

SURFACE OBSERVATIONS

POSITION SONIC MAX.
DEPTH SAMPLE
LATITUDE LONGITUDE UNCORRECTED] DEPTH
Ss /

oso" 3a | voes [or |

STATION

00658 PGlA

anemo.| aig | AIR TEMPERATURE CLOUD SEA SWELL
HGT. | PRESS EATHE
Sg oo SS

SUBSURFACE OBSERVATIONS

SAMPLE = AD Vi VAI
DEPTH (M)

STD

STD
STD

STD

STD
OB

SURFACE OBSERVATIONS

DATE POSITION

AY | YEAR =| LATITUDE
17 | 1960 28 59’N| 050°

STATION

| wisn ANEMO. AIR
HGT. | PRESS
30

Saas Toc Ozmi/l
DEPTH (M) Vv
STD
OBS
OBS
STD
OBS
OBS
STD
OBS

158

SURFACE OBSERVATIONS

Nope DATE POSITION SONIC MAX.
REF. | STATION DEPTH __| SAMPLE
No. mo. | DAY | YEAR | HOUR LATITUDE LONGITUDE UNCORRECTED] DEPTH

00658 P12 | o2 | 19] 1959| 06 | 29 0022 | 00
WATE
| Paenceeaonen | eee 4 R

HGT. | PRESS ivan WERE Mi
pRYY | WETY cou,| TRANS.

19

28) 9)

SAMPLE
DEPTH (M)

SURFACE OBSERVATIONS

(eof Sas

NODC | POSITION SONIC MAX.
REF. STATION DEPTH SAMPLE
NO. LATITUDE LONGITUDE UNCORRECTED] DEPTH
| 00658 Pell | 02 | 19 050 03/E | 0049 | 00 |
WIND ATG INIA AIR TEMPERATURE SWELL WATER
HGT. | PRESS VAIS
SPEED] DIR. DRY WET V DIR. |AMT. cou,| TRANS. |
ee i eae eal
SUBSURFACE OBSERVATIONS
SAMPLE sly re S °/oo ot = AD OzmI/I VE
DEPTH (M) vy v v y y
STD 0000 Us AS | Be 29 46 |0 000- =
OBS 0000 IS) LS) AO) Sh 29 46
OBS 0005 UO Ie eG 82 29 46
STD 0010 19 17/40 84 29) 46) 08 O13 =
OBS 0010 19 17 |40 84 29 46
STD 0020 19 10/40 82 BS) ES (0) OBR
OBS 0020 US) LO) |K@) 29 46
STD 0030 19 O7 |40 85 2) BO) |@ Ozi)o
OBS 0030 19 O07 |40 85 2) 5@
OBS 0040 19 09 |40 82 29 47
OBS 0049 19 08 |40 89 2S) Be

159

SURFACE OBSERVATIONS

DATE

STATION

DAY | YEAR
20} 1960

POSITION SONIC MAX.
DEPTH
HOUR LATITUDE LONGITUDE UNCORRECTED] DEPTH
00 28 44

AIR TEMPERATURE

HUMID- J
Ty WEATHER

jaw. COL

SAMPLE
DEPTH (M)

STD
OBS

OBS

y STD
OBS

STD
OBS

STD
OB
OBS

NODC
REF. STATION
NO.

SURFACE OBSERVATIONS

00658 PG2l

SAMPLE
DEPTH (M)

Ozmi/

160

SAMPLE

WATER

POSITION SONIC MAX.
DEPTH SAMPLE
LATITUDE LONGITUDE UNCORRECTED] DEPTH

WATER

COL.) TRANS.

TRANS.

SURFACE OBSERVATIONS

NODC DATE POSITION

SONIC MAX.
SAMPLE

DEPTH

DEPTH
UNCORRECTED

LONGITUDE

Ol

REF. STATION
NO. MO. DAY YEAR HOUR LATITUDE
00658 PG20 | 02 20] 1960} 12 PSL ONN

050 50’E | 0055

vis.
AMT. DIR. AMT. COL.} TRANS.
ai a
SUBSURFACE OBSERVATIONS ]
SAMPLE 2 ° o ZA 2m Vv
DEPTH (M) a we JL ‘y v : y E | v
STD 0000 NE) BS) ee) Des) 28 92 |0 O00—
obs 0000 LS) Be Voy Qe 28 92
OBS 0005 1S Be Who 27 28 93
STD 0010 Sy Be AO) 627 28) 93390) O0N—
OBS 0010 Sy BA WAG) AT 28 93
STD 0020 19 46/40 26 28 9410 015—
OBS 0020 19 46 |40 26 28 94
STD 0030 ie) Zyl AO) QS) 28 9710 023=
OBS 0030 NE Bil "RO BS) 28 Cy)
OBS 0040 US B22 40) 2S 28 o7/
STD 0050 19 61/40 64 29 19 10 040=
OBS 0050 19 61/40 64 29 19
OBS 0055 19 59 |40 66 2D Bil

SURFACE OBSERVATIONS

Nopc POSITION
REF. | STATION
NO. ; LATITUDE | LONGITUDE

a7. 227 N| @Sn OVE

SONIC MAX.
DEPTH SAMPLE
UNCORRECTED] DEPTH

SEA

anemo.| aig | AIRTEMPERATURE | 41 CLOUD
HGT. | PRESS my | EARS
DRYW | WETY TYPE|AMT.

DIR. AMT.
14 | 18 9 | 02 | | 0 | 30| 3
SUBSURFACE OBSERVATIONS |
SAMPLE Tacc 3 Yan ot = AD Ozmi/i Ve
DEPTH (M) v v Vv Vv vy
STD 0000 20 39139 84 | 28 37/0 000-
OBg 0000 20 39/39 84 | 28 37
obs 0005 20 39/39 84 | 28 37
STD 0010 20 38139 85 | 28 3810 002=
OBg 0010 20 38139 85 | 28 38
OBg 0015 20 40|39 86 | 28 38
STD 0020 20 33/40 06 | 28 55|0 005=
OBJ 0025 20 29/40 18 | 28 65
STD | 0030 20 30/40 21 | 28 67/|0 O10-
OBg 0035 20 30|40 22 | 28 68
OBg 0045 2 27\20 22 || 28 eo
STD *| 0050 20 28/40 22 | 28 69/0 020=
OBY 0063 2® 29/60 22 || 28 68

161

SURFACE OBSERVATIONS

POSITION SONIC MAX.
STATION DEPTH SAMPLE
S LATITUDE LONGITUDE UNCORRECTED] DEPTH

°

PG23 27° 06/N| 050 46/E

HUMID-
ITY

SAMPLE
DEPTH (M)

Oami/I

SURFACE OBSERVATIONS

POSITION SONIC MAX.

STATION DEPTH SAMPLE
ie ee a LATITUDE LONGITUDE UNCORRECTED] DEPTH

“ 54/N 4 Y 0053

| wino | ANEMO. AIR ¢ CLOUD WATER
SPEED Res AGT: PRESS TyPE|ANT. , . , o cou] TRANS.
SUBSURFACE OBSERVATIONS

SAMPLE TaoG G Wha ot = AD O2mi/I Ve
DEPTH (M) Vv Vv Vv Vv Vv vy
STD 0000 2 S739 ©o% 27 9410 000
OBS 0000 2 37 |39 64 Atl 94
OBg 0005 21 37139 64 27 94
STD 0010 2h AU\S9 62 27 96/0 002
OBS 0010 2 27 |B9 62 2 DS
STD 0020 20 YS |S 62 28 04/0 003
OBS 0020 ZA) QPS) 2 28 04
STD 0030 20 7 29 79 28 22 |0 003
OBS 0030 20 7vI3B9 7S 23 22
OBS 0040 ZO Cons.) 709) 28 25
STD 0050 P20) (0) I) 81 28 29/0 OO1
OBY 0050 AQ) ©@ |B Gail 2s} 2S)
OBS 0053 20 5 \39 2 28 28

162

SURFACE OBSERVATIONS

NODC POSITION
REF. STATION
NO. MO.

| 00654 PG26 | 02 3] 1960

WATER

‘|cot.| TRANS.

AIR TEMPERATURE

WIND

ANEMO. AIR
HGT. PRESS

SAMPLE
DEPTH (M)

SURFACE OBSERVATIONS

POSITION

STATION

HOUR LATITUDE LONGITUDE
06 | 27 442’N/ 051 25’E

00658) PG25

ANEMO. AIR
HGT. PRESS

SAMPLE
DEPTH (M)

STD 0000
OBS 0000
OBS 0005
STD
OBS 0010
OBS 0015
OBS 0018

163

SURFACE OBSERVATIONS

POSITION SONIC MAX.
SAMPLE

DEPTH
LATITUDE LONGITUDE UNCORRECTED] DEPTH
42’N]| 051 25/E 0018

WATER

TRANS.

coL.

SAMPLE
DEPTH (M)

STD 0000

SURFACE OBSERVATIONS

DATE POSITION

SONIC MAX.
DEPTH SAMPLE
UNCORRECTED] DEPTH

DAY YEAR | HOUR LATITUDE LONGITUDE
23 1960 | 24 | 27. 42/N 0018
CLOUD | SEA SWEL WATER |
HOM)P- WEATHE : VIS.
TYPE awt,| DIR. AMT. DIR. AMT. COL.| TRANS.

| 02 | o| 35

SUBSURFACE OBSERVATIONS

SAMPLE TAIG S °/oo ot AD O2mi/I Ve
DEPTH (M) vy | v v
STD 0000 Zi O23 |BO ae 2 92 |0 @O@O
OBS 0000 Qn (Os) 39 AS) 2Y 22
STD 0010 Zi OO |BY BO Zin Ze | OmOO?Z
OBS 0010 Ah Of [BS HO Zale.
OBS 0018 2 038839949 2 eA

SURFACE OBSERVATIONS

DATE | POSITION

| DAY | YEAR | HOUR | LATITUDE | LONGITUDE
| 24 | 1960 | 06 | aT” 42/N | 051 25’E

CLOUD | SEA | SWELL WATER

TYPE amt,| DIR. AMT.
0 | 31
—!

COL.) TRANS.

SAMPLE
DEPTH (M)

164

SURFACE OBSERVATIONS

=

DATE POSITION SONIC MAX.
STATION DEPTH SAMPLE
MO. | DAY YEAR LATITUDE LONGITUDE UNCORRECTED] DEPTH
24 | 1960] 12 | aT 42’N | O51 25/E | 0018 | 00
AIR TEMPERATURE HUMID CLOUD SEA | SWELL | WATER
ITY ~ IWEATHE VIS.
TYPE|AMT. DIR. AMT. DIR. jamr.| COL.| TRANS.
05 | @ || 30 | 3
SUBSURFACE OBSERVATIONS
SAMPLE Ir T°c Sio7en Ozmi/I Ve
DEPTH (M) vy y Vv
STD 0000 2h 87 \S9 Oi 1
OBS 0000 Al 87 \39 Ol
STD 0010 21 60/39 06
OBg 0010 21 60/39 06
oBgd 0018 21 SA (89 9
SURFACE OBSERVATIONS |
DATE | POSITION SONIC MAX.
STATION DEPTH SAMPLE
YEAR HOUR | LATITUDE LONGITUDE UNCORRECTED] DEPTH

MO. DAY
2 24

PG25 | 0

1960

[

19 | ayia 42'N | 051 25/E

ANEMO.
HGT.

AIR
PRESS

CLOUD | SEA

ie SWELL |
VIS

WATER

awt,| DIR. | amr. | DIR. [amr]

cou| TRANS.

13 0 | 31 | 1 | | | 5 |
SUBSURFACE OBSERVATIONS a
SAMPLE Talc S °/oo ot = AD O2mi/l Ve
DEPTH (M) y v v v
STD J 0000 Zi UsT/ |v) as) ZU AD || OOO
OBS 0000 2k wy IBD 16 2 65)
STD 0010 21 45/39) 8 2 Ar |O OOS
OBS 0010 AN Gs) |S. US ZU DY
OBS 0018 2 39 |39 20 2 ©@

165

SURFACE OBSERVATIONS

POSITION
STATION

LATITUDE LONGITUDE

00658 PG22 1960 | 10 ; 40'N | 050 36/E

SAMPLE
DEPTH (M)

STD
OBS
OBS

STD
OBS
STD
OBS
STD
OBS
OBS

STD
OBS
OBS

SURFACE OBSERVATIONS

POSITION SONIC MAX.

DEPTH SAMPLE
LONGITUDE UNCORRECTED] DEPTH

00658 PG19 52’N!1 050 15/E 0058

SEA | SWELL | WATER

vis.
TRANS.

AMT. | DIR. awt,|

SAMPLE
DEPTH (M)

Ozmi/I

STD
oBSg
OBS

STD
oBS

STD

OBS

STD
OB
OB

STD
OB
OB

166

SURFACE OBSERVATIONS

NODC DATE POSITION SONIC MAX.
REF. STATION DEPTH SAMPLE
NO. MO. DAY YEAR | HOUR LATITUDE | LONGITUDE UNCORRECTED] DEPTH
00658 PGLs | o2 | 26 1960 | 15 |) aa" 02’N | 049° «#+51’E 0046 | 00
AIR AIR TEMPERATURE HUMID- CLOUD SEA | SWELL | WATER
PRESS ITY EATHE VIS.
DRY YW WET ¥ TyPE|AMT, DIR. AMT. | DIR.
ier | 22) 8 | | 02 | Onl 1
SUBSURFACE OBSERVATIONS
SAMPLE T°c S Yas ot = AD Ozmi/ Ve
DEPTH (M) y vy v
STD 0000 20 13/40 69 | 29 09 ]|0 000-
OBg 0000 20 13/40 69 | 29 09
OBS 0005 20 08 |40 72 | 29 12
STD 0010 1S) Sil AQ il 29 27/|0 010-
OBg 0010 19 51/40 71 DS eal
STD 0020 19 241/40 75 | 29 37 jo o21-
OBS 0020 19 2AWAOQ 75 | 2 37
STD 0030 19 05/40 82 | 29 48 jo 033-
OB 0030 19 05/40 82 | 29 48
OBg 0040 18 98/41 03*| 29 66
OBS 0045 18 98/40 94 | 29 59
SURFACE OBSERVATIONS
DATE POSITION SONIC MAX.
STATION DEPTH SAMPLE
NO. MO. | DAY YEAR | HOUR LATITUDE LONGITUDE UNCORRECTED] DEPTH
00658 PGi7 | 02 | 27 1960 | no | as a7’ N| O50™ OBE | 0055 | Ol |

AIR TEMPERATURE

HUMID- WEATHER

WATER

| VIS.
| COL.| TRANS.

CLOUD SEA
SPEED DIR. eM des WET ¥ Lue TYPE|AMT.| DIR. AMT. DIR. [awr.
| 32 | | 15 23 9 | | 02 Oo] 33 1| |
SUBSURFACE OBSERVATIONS

SAMPLE ye S /s5 ot

DEPTH (M) y v vy
STD 0000 20 26/40 55 28
OB 0000 20 26 |40 55 28
OBS 0005 20 08 [40 75* | 29
STD 0010 19 90/40 58 29
OBS 0010 19 90 |40 58 29
STD 0020 19 69 |40 57 29
OBS 0020 19 69/40 57 29
STD 0030 19 43 |40 75 29
OBS 0030 19 43/40 75 29
STD 0050 18 95/40 83 29
OBg 0050 18 95/40 83 29
OBS 0055 18 94/40 87 29

167

NODC
REF.

a

STATION

12

DEPTH SAMPLE
00658 PG16 Merve 1960] 00 | 28° 31’n| 050 21'€ | 0052

| wino| Pom | tet AIR
HGT. PRESS

SURFACE OBSERVATIONS

AIR TEMPERATURE

DRY Ea WET | wery |

CLOUD SWELL
EATHE
= AMT. T. COL.| TRANS.

STD

STD

STD

STD

STD

OBS
OBS

OBS
OBS

OBS
OBS

OBS

SAMPLE
DEPTH (M)

0000
0000
0005
0010
0010
0020
0020
0030
0030
0040
0050
0050

Ozmi/

NODC
re

STD

STD

STD

STD

STATION

OBS
OBS

OBS
OBS
OBS

OBS
OBS

SAMPLE
DEPTH (M)

0000
0000
0005
0010
0010
0020
0020
0030
0030
0040
0046

SURFACE OBSERVATIONS

POSITION

Ozmi/I

168

SURFACE OBSERVATIONS

NODC DATE POSITION SONIC MAX.
REF. STATION DEPTH SAMPLE
No. HOUR LATITUDE | LONGITUDE UNCORRECTED] DEPTH
00658 PGO9 toy 2a" 72a Nees) ees | 0043 | 00 |
WIND AIR TEMPERATURE CLOUD SEA SWELL WATER
ANEMO.| AIR HUMID-
HGT. | PRESS pany {PASM | | VEE |
SPEED] DIR. aa DIR. AMT, | mnt COL. TRANS. |
| | 34 11 62 | 2 1 | ae) 7
SUBSURFACE OBSERVATIONS
SAMPLE Toc) S Vo ot = AD Ozmi/ Ve y
DEPTH (M) v y y
STD 0000 19 49/40 91 Zee oe OM OO
OBS 0000 19 49 |40 91 29 43)
OBS 0005 19 51/40 90 29 42
STD 0010 sy 2S Ae) Se 2 BO) |O Ole
OBS 0010 ie) 2H_IA@Q 92 2S) 3)(0)
STD 0020 LO 78 lel @4 29 72/0 O27=
OBS 0020 I} /S} WAL ZS) YB
STD 0030 18 45 |41 10 BS) 8). [0) OVA
OBS 0030 18 45/41 10 BS) (35)
OBS 0040 18 38 /41 12 Ze) 338)
| SURFACE OBSERVATIONS
NODC DATE | POSITION
REF. STATION
NO. MO. | DAY YEAR HOUR | LATITUDE LONGITUDE
| 00658] Pc9a | o2 | 28| 1960/13 | 28° 43’N| 048 54/E

AIR TEMPERATURE CLOUD | SEA SWELL WATER
AMD: IWEATHE VIS.
TyPE|AwT.| DIR. amr. | DIR. [amr COL.| TRANS.
ah 7 | @2 || a 3 | 33 1 | | | 7 |
SUBSURFACE OBSERVATIONS
SAMPLE Le S °/o0 ot = AD Ozmi/I VE
DEPTH (M) vy Vv Vv Vv .7
eee ae
STD 0000 1g) 2 an 27 || 20) Ws) Ike) Coe
OBS 0000 18 Sill ay | 30 o9
OBS 0005 18 Ania 36 | 30 aH
STD 0010 17 94/41 40 | 30 21/0 019-
OBS 0010 17 94% /4n 40 || 3@ Bi
STD 0020 17 38/41 56 | 30 48 |o 040-
OBS 0020 17 38 (41 56 | 30 48
STD 0030 17 36/41 56 | 30 48 jo 062-
OBS 0030 17 36/41 56 | 30 48
OBS 0036 17 34 (41 55 | 30 48

169

SURFACE OBSERVATIONS

POSITION

STATION

| 00658 pcos | 02

ee ANEMO.| AIR

|sPeeD| DIR. HGT. PRESS
Paine 09

reac] oe [oro]
alee

SAMPLE | imac | S oo Ve
DEPTH (M) vy vy v

STD 0000 ng} Sal si 27 29 86 |0 000=

OBS 0000 We Sil ek 27 2) BS
STD 0010 18 58/41 26 29 94 )0 Ol17=

OBS 0010 18 58/41 26 29 94

OBS 0015 18 32/41 29 30) (0)2)
STD 6020 18 15/41 30 30 08 |0 034-—

OBS 0025 18 05/41 30 BQ shal
STD 0030 Tey @)aL esi 240) A IK) @DZ—

OBS 0030 Wey OL Wen hal 30 27

SURFACE OBSERVATIONS

POSITION SONIC MAX.
DEPTH SAMPLE

MO.
2 [2s] aseo] oo [29° «zn| oss” soe | cour | 00

| wisn | =e ain | AIR TEMPERATURE |.) cLoup SEA SWELL
HGT. | PRESS Yael ee
on A
eee ee ee ei

SUBSURFACE OBSERVATIONS

SAMPLE ac = AD ae VE
DEPTH (M) v v vy

STATION

PGOL

170

0065

STATION

SURFACE OBSERVATIONS

DATE POSITION

8 PGOl | 02

DAY | YEAR HOUR LATITUDE | LONGITUDE

29 | 1960 o3 || 29° 42’N| 048” 50/E

SONIC MAX.
DEPTH SAMPLE
UNCORRECTED} DEPTH

oo17 | 00 |

WIND ane. ane AIR TEMPERATURE | 44. ne EtG CLOUD SEA SWELL a WATER
SPEED] DIR. lciees Wlaies uy TyPE| amr. DIR. | AMT. | DIR. |AMT. COL.} TRANS.
12 06 | 03 8[ 4] 15 1| i
SUBSURFACE OBSERVATIONS
SAMPLE
DEPTH (M)
STD 0000
OBS 0000
OBY 0007
STD 0010
OBS 0015
SURFACE OBSERVATIONS
NODC DATE POSITION SONIC MAX.
REF. | -STATION DEPT SAMPLE
NO. MO. DAY | YEAR | HOUR LATITUDE LONGITUDE UNCORRECTED] DEPTH
B if - /
00659 PGOl |} 02 29 | 1960 | 06 | 28) 42 N| 048 5) [e 0016 | 00

WIND AIR TEMPERATURE SWELL WATER
ANEMO.| AIR HUMID-
WEATHER} VIS.
BOTS PERESS TN ol) DURE [awr. cou.| =
| C8 | 02 | 4 14 al | ul | |
| SUBSURFACE OBSERVATIONS
SAMPLE ¥ OG S Veo ot =AD OzmI/| VE
DEPTH (M) v y v v. vy
STD 0000 if 7 |B So) ae 18 |}0 O000—
OBS 0000 etal SOO) OS) Akt}
OBS 0008 RY 22ZIOQ 35) 29 Bey)
STD QG010 17 23 |40 46 2 i IQ) Oit2>
OBS 0016 17 25/40 81 29 9B
[ SURFACE OBSERVATIONS al
NODC | DATE POSITION SONIC MAX.
REF. STATION DEPTH SAMPLE
No. MO. DAY | YEAR HOUR LATITUDE le LONGITUDE UNCORRECTED] DEPTH
= 7 - -
00658 PGOl | 02 29 | 1960 | 09 29 42 n | 048 biome: 0016 | 00 |
WIND AIR TEMPERATURE CLOUD SEA SWELL WATER
lsree0] overs | PRESS ty (WEATHE ia
DIR. DRY ¥ WET ¥ : TyPE|AMT. DIR. | AMT. | DIR. |AMT. COL.| TRANS.
16 asa ene | “he ala sla
SUBSURFACE OBSERVATIONS
SAMPLE TOG S °/oo ot ZAD Ozmi/\ Mi
DEPTH (M) y v v v y Vv
STD 0000 17 52/40 88 ZS) D2 \6) OC)=
OBS 0000 Ue By yO asks} 2D M2
OBS 0008 17 «644 |40 93 29 ei
STD 0010 17 42 |40 94 2) 99 10 @Ly=
OBS 0016 17 38 |40 97 39) (2

171

STATION

SURFACE OBSERVATIONS

POSITION SONIC

DEPTH
UNCORRECTED} DEPTH

| LONGITUDE

PGOl

SAMPLE iG Ozmi/
DEPTH (M) vy

STD

OBS

OB
STD

OBS

SURFACE OBSERVATIONS
NODC DATE POSITION SONIC MAX.
REF. STATION DEPTH SAMPLE
NO. MO. DAY YEAR ] Hour LONGITUDE UNCORRECTED] DEPTH
| 00658 PGOL | 02 29 1960 | 18
WIND anema.|| ane AIR TEMPERATURE WATER
HGT. | PRESS DRYY cou] Trans. |
| 08 19 4 | 7
SAMPLE Ve
| DEPTH (M) v

STD 0000

OBS 0000

OBS 0007
STD 0010

OBg 0015

SURFACE OBSERVATIONS

NODC DATE
REF. STATION
NO. MO. DAY | YEAR

POSITION

SONIC

DEPTH
LONGITUDE UNCORRECTED] DEPTH

| 00654 PCO! | 02 | 29 | 1960

WIND

WATER

ANEMO.| AIR
Biota |) TAMERS COL.| TRANS.
08
SUBSURFACE OBSERVATIONS
SAMPLE Toc S/o ot = AD Oem i/\ Mi
DEPTH (M) vy v Vv Vv
STD 0000 li 46140 85 29 91 )0 000- i
OBS 0000 17 46 |40 85 ZS Sil
OBS 0007 lf S540 99) 30 00
STD 0010 17 55 |41 00 30 00 ]j0 O17-
OBS 0015 17 54/41 Ol 2 OOP

172

SURFACE OBSERVATIONS

NODC | POSITION
REF. STATION
NO. MO. YEAR | HOUR |
| 00658 PGO1 | 03 1960 | 00 | 9
ANEMO. AIR AIR TEMPERATURE
HGT. PRESS DRY ¥ WET Y
oa | 18 9|
SAMPLE T°c S "Jeo ot = AD OzmI/I VE
DEPTH (M) y v v Y v
STD 39 |40 69 |0 000-
39 |40 69
41 |40 26
STD 42 |40 01 |o 016-
44 |40 01
| SURFACE OBSERVATIONS
NODC DATE | POSITION SONIC MAX.
REF. STATION DEPTH SAMPLE
NO YEAR | HOUR | LATITUDE LONGITUDE UNCORRECTED] DEPTH
00658 PGOl o1]19e0| 03 | 29° 42’n|[ 048 50'E | oo16 | 00
LAND ANEMO.| AIR SEA | SWELL
SPEED DIR. ASI FMSSS AMT. | DIR. AMT. COL.| TRANS.
| | 05 | 08 1|
SAMPLE
DEPTH (M)
STD
0B
0B
STD
OB
SURFACE OBSERVATIONS “|
NODC DATE POSITION SONIC MAX.
REF. STATION DEPTH SAMPLE
NO. MO. DAY YEAR | HOUR | LATITUDE LONGITUDE UNCORRECTED] DEPTH
| 00658 Pcol | 03 | 01| 1960] 06 | 29° 42’N| 048° 50’E | 0016 | 00 |
CLOUD SEA WATER
EMO. AIR E
ae PRESS Y EATHE | | VIS |
TYPE|AMT.| DIR. AMT. cou_| TRANS. |
09 | oz] 6] 4 oa] 2|
SUBSURFACE OBSERVATIONS
SAMPLE Tac S "Jeo ct =AD Ozmi/I Ve
DEPTH (M) v v Vv v v v
51140 o7 | 29 30/0 o00-
51140 o7 | 29 30
44140 14 | 29 37
DANK) AL || BD Az |0 One
39) ay | 2 BG

173

STATION

SURFACE OBSERVATIONS

POSITION

LATITUDE LONGITUDE

PGO1l

SAMPLE
DEPTH (M)

0000
0000
0007
0010
0015

SAMPLE
DEPTH (M)

NODC
REF.
NO.

STATION

SURFACE OBSERVATIONS

POSITION

LATITUDE LONGITUDE

CLOUD SEA

O2zmi/I

SURFACE OBSERVATIONS

SONIC MAX.
DEPTH SAMPLE
UNCORRECTED] DEPTH

048 50'E 0016

LL Ieee) he a Le

SONIC MAX.
DEPTH SAMPLE
UNCORRECTED} DEPTH

Qom lane Ge Noacmns ONE 0016 | 00 |

DATE POSITION SONIC MAX.
DEPTH SAMPLE
YEAR | HOUR LATITUDE | LONGITUDE UNCORRECTED] DEPTH
GO ij a qe
01 1960 | is 25°) we N | 048 50'E | 0016

TRANS.

SAMPLE SES a5 ot = AD O2mi/I
DEPTH (M) Vv v y
STD 0000 17 91/40 45 29 49/0 O00-
OBS 0000 17 91/40 45 29 49
OBS 0007 ey al WA) 5) 29 BU
STD 0010 17 82 |40 60 29 63 |0 014-
OBS 0015 17 54/40 71 BS 18

174

SURFACE OBSERVATIONS

POSITION

STATION

WATER

SAMPLE Ozmi/I

DEPTH (M)

SURFACE OBSERVATIONS

NODC POSITION
REF. STATION

NO.

00658

DAY YEAR HOUR LATITUDE LONGITUDE UNCORRECTE

PG8A

AIR TEMPERATURE

HUMID-
pryYy | wety | |”
20 0| |
SUBSURFACE OBSERVATIONS
abet
SAMPLE acc S °/oo ot = AD OzmI/I Ve

DEPTH (M) vy Vv vy Vv Vv vy

STD 0000 Le OD |e Bil 30 05/0 000—-
OBS 0000 Le SS) |e il BOOS

OBS 0005 18 03 |j41 21 30 O04

STD 0010 1s) 2 RIL 22 30) O50 @iee
OBS 0010 ey OZ |\EAl 22 20) @5
OBS 0014 18 OO

175

foo Eee

@2 |) 1960 | oS | 25° OT Nl O28" S7E 0014 | 00 |

COL.| TRANS.

D| DEPTH

SURFACE OBSERVATIONS

POSITION SONIC MAX.
DEPTH SAMPLE
LONGITUDE UNCORRECTED] DEPTH

AIR
PRESS

ANEMO.
HGT.

SAMPLE : Ozmi/I
DEPTH (M)

SURFACE OBSERVATIONS

NODC POSITION SONIC MAX.
REF. STATION DEPTH SAMPLE
NO. | wo. | UNCORRECTED] DEPTH

SAMPLE
DEPTH (M)
STD
OB
OB
STD
OB
STD
OB
STD
OB

176

| SURFACE OBSERVATIONS

POSITION SONIC MAX.
DEPTH SAMPLE
YEAR | Hour | LATITUDE | LONGITUDE UNCORRECTED} DEPTH

Te [on

WATER

COL.| TRANS.

SAMPLE
DEPTH (M)

O2zmi/I

SURFACE OBSERVATIONS

POSITION SONIC
DEPTH

UNCORRECTED} DEPTH

STATION

LATITUDE | LONGITUDE
29° 47/N | 049° «32/E | 0012 | 00 |

HUMID-

ayy : ; = TRANS.

SAMPLE
DEPTH (M)

SURFACE OBSERVATIONS

NODC DATE POSITION

REF. STATION
NO. MO DAY YEAR HOUR LONGITUDE
| 00658 PGoz | 03 | 02 | 1960 | 21 | ag ai Nee TSZE | 0014

SEA | SWELL

AMT. | DIR.

SAMPLE
DEPTH (M)

ot = AD Omi | VE

STD 0 000=
OB
OB

STD OO eS
OB

177

SURFACE OBSERVATIONS

NODC POSITION
ee STATION

LATITUDE
00658 PGO2 04

WHA) ANEMO.| AIR

HGT. PRESS

SAMPLE 7G

|_DEPTH (M) v
STD 0000 7 83
OBS 0000 iy 83
OBS 0005 uy ey
STD 0010 17 56
OBg 0010 WT BMS)

SURFACE OBSERVATIONS

POSITION

ee STATION

SAMPLE
DEPTH (M)

SURFACE OBSERVATIONS

POSITION

LATITUDE | LONGITUDE

AIR TEMPERATURE
HUMID-

ony | wey [om [aw [om awn) [cou] tans

OE g 1 Sie _|

SAMPLE Ozmi/I

DEPTH (M)

178

SURFACE OBSERVATIONS

AIR
PRESS

ANEMO.
HGT.

POSITION SONIC
DEPTH
LATITUDE | LONGITUDE UNCORRECTED] DEPTH
/ ° /
47 N| 049° «32’/E | 0012

WATER

iS)

COL.| TRANS.

SUBSURFACE OBSERVATIONS

SAMPLE 7m °c S °/oo =z AD
DEPTH (M) y
STD 0000 17 58/41 19
OBg 0000 17 58/41 19
OBG 0005 17 63/41 18
STD 0010 UY © (Gil Ail
OBS 0010 Lif 627 14a 2

SURFACE OBSERVATIONS

STATION

PGO2

04 | 1960 | 03

POSITION

LATITUDE

LONGITUDE

Ozmi/

SONIC MAX.
DEPTH SAMPLE
UNCORRECTED] DEPTH

47’ N | 049°

32’ E

COL.) TRANS.

SAMPLE
DEPTH (M)

Ozmi/I VE
v v

STD
OB
OB
STD
OB
SURFACE OBSERVATIONS
NODC DATE POSITION
REF. STATION
NO. MO. YEAR = LATITUDE | LONGITUDE
| aes PGO2 | 03 DD a7! N | 049° «32’E
AIR AIR TEMPERATURE CLOUD SEA SWELL

PRESS

HUMID- “ef
ITY EATHE

TYPE

16

AMT. AMT. | DIR.
1

SAMPLE mc Sic/en ot =AD
DEPTH (M) y v Vv
7p Shah eh 2X0) 30 07 |0 000—
Tf Sak al 2@) 30), O7/
17 66/41 20 3H) ALB
te Aad |b 2o© 30 ABO OnAS
Ri Diy leat AO 30) LB)

179

SURFACE OBSERVATIONS
NODC DATE POSITION SONIC MAX.
REF. STATION DEPTH SAMPLE
NO. DAY | toncitupe [UNCORRECTED DEPTH

| toncitupe |

C2 HWEINEE ty iAvvcaee AR AIR TEMPERATURE
14

ee ae
SUBSURFACE OBSERVATIONS

DEPTH (M) vy Vv v Vv Vv

STD é

OBS

OB
STD

OB
STD

OB
STD

OB

SURFACE OBSERVATIONS

REF. STATION DEPTH SAMPLE
0065q PGO4 1960 29° 44’N] 050° 12/E 0017 | 00 |

Pepe pe fee oe eee eee

SUBSURFACE OBSERVATIONS

SAMPLE
DEPTH (M)
STD
OB
OB
STD
OB
OB

SURFACE OBSERVATIONS

POSITION SONIC MAX.
STATION DEPTH SAMPLE
o >

| swe |
TRANS.

180

SURFACE OBSERVATIONS

DATE ne SONIC MAX.
DEPTH SAMPLE
YEAR HOUR LATITUDE |_ tonerrupe UNCORRECTED] DEPTH

1961] 16 26° 34/N| 05 TARTS 0051 00

WATER
COL.| TRANS.

STATION

SUBSURFACE OBSERVATIONS
Se at T y ne ot y y = AD tae Ve y

STD 0000 22 45 |36 99 25 62 |0 000
OBS 0000 22 Usb) |e) SIS) Be (a2

STD | 0010 22 44 |37 Ol 25 64/0 024
OBS 0010 22 44/37 O1 25 64

STD 0020 22 38 |37 10 25 72 10 047
OBS 0020 22 38) 7 no) 25 72

STD 0030 2A BY \s7- ies 23 18 | O70)
OBS 0030 22 Bi \BT 14 25 16
OBS 0040 BA EP I7/ 18 25 als

STD 0050 Bin PNT 2 25 80/0 114
OBS 0050 22 BQIBT B22 25 80

SURFACE OBSERVATIONS

POSITION

HOUR | LATITUDE LONGITUDE
1961 o | 26° 055° 48/E

Ol

AWENON MATE CLOUD SEA SWELL WATER
WIG 1} Gis) TYPE|AMT.| DIR. | AMT. | DIR. |AMT. COL.| TRANS
U7 | 80] 6] 6] 09 1 | 7
SUBSURFACE OBSERVATIONS
a
SAMPLE Tac) S °/oo ot = AD Ozmi/I Ve
DEPTH (M) vy y v y y Vv
STD 0000 2A S29 7 O2 25 66 |]0 000
OBS 0000 22 39 187 O2 Zoo)
STD 0010 22 39 |B7 3) (6S) |) @22)
STD 0020 22 80) |B7/ 1) 25 72 |0 046
OBS 0025 22 HOB 12 Zoe, 3
STD 0030 2 Be} |B Ze) 72) |KO) (OVS)
STD 0050 AR BE \ET Bik 2B (3) |) iis)
OBS 0050 O22 BRIA Bil (iz) {s\5)

181

SURFACE OBSERVATIONS

POSITION

ANEMO. AIR
HGT. PRESS

ITY

Ee SUBSURFACE OBSERVATIONS
SAMPLE S °/oo iG ot =z AD Oami/| Ve
DEPTH (M) Vv Vv Vv
STD 0000 22 BSB \o PY
OBS 0000 22 3 |B ©
STD 0010 Be EEN 2
aa 0010 22 |B 02
STD 0020 22 41/37 04 25 6710 O47
OBS 0020 22 Gi sy Oc 25 67
STD 0030 22 BE ye 1s) 25 7510 070
OBS 0030 AA M37 Us 28 12
OBS 0040 22S S| Sie 25 Uy
STD | 0050 BA AB NET 20) 25 84 ]0 115
OBS 0050 22 28 |B 20 25 84

SURFACE OBSERVATIONS

POSITION SONIC MAX.
DEPTH SAMPLE
LONGITUDE UNCORRECTED] DEPTH

foot [oe |

SAMPLE

DEPTH (M)
STD 0000
OBS 0000
STD 0010
STD 0020
OBS 0025
STD 0030
OBS 0049

182

SURFACE OBSERVATIONS

STATION
MO.

DATE

pay | YEAR | HOUR

LATITUDE

POSITION

LONGITUDE

PG29

Ol

14

SUBSURFACE OBSERVATIONS
SAMPLE Toc S °/oo Oami/l
DEPTH (M) v
STD
OB
STD 0010 22 78 |36 85 25 42/0 026
OBS 0010 22 78/36 85 2B te
STD 0020 22 ©3/26 97 2 Bi) | Oat
OBS 0020 22 3 \36 7/ 2) 62
STD 0030 22) a5 3 00 25 62/0 @75
089 0030 22 CY 1320 OC 25 62
OBS 0040 22 23 \87 iB 23 72
STD 0050 QA 2a iey7 abil 2) Ui iO aan
OBS 0050 BQ) Abs est wil 25) TT

1961

05

26

CLOUD

LoL Se

34/N

055°

SEA

48/E

SWELL

VIS.

WATER

TRANS.

COL.

SURFACE OBSERVATIONS

POSITION

STATION

LONGITUDE

00865) PG29

CLOUD WATER

ANEMO.| AIR HUMID-
Hots || ERESS De ia ne TYPE|AMT.| DIR. | AMT. cou| TRANS
19 | 01 | 8} 5] 06
SUBSURFACE OBSERVATIONS
as
SAMPLE Tacc S °/oo ct ZAD O2mi/ Ve
DEPTH (M) y v y vy v
STD 0000 22 83 |B 2 22 Ze (0) OOO |
OBS 0000 22 83 |B 82 25) 38
STD 0010 22 TS |B B7/ 25 44 10 026
STD 0020 22 (55 |B 83) 23 il \@) Osi
OBS 0025 22 ©0 |B YS Be Be)
STD 0030 2A Be eis OP) 22 DE) | OVD
STD 0050 QQ BANU ND Ze ka Jl |{e) kA
OBS) 0050 22 22 (37 Ns 22m ok

183

|

SURFACE OBSERVATIONS

POSITION
STATION

DAY HOUR LATITUDE

AIR
PRESS

DRYY | WETY

18 19 4

SAMPLE
DEPTH (M)

STD
OBS
STD
OB
STD
OB
STD

OBS
OBS
OBS

SURFACE OBSERVATIONS

NODC POSITION SONIC
REF. | STATION DEPTH
se ; iz LONGITUDE UNCORRECTED

AIR TEMPERATURE H

MAX.
SAMPLE
DEPTH

WATER

‘\coL.

pee ee eet
i ea

SAMPLE
DEPTH (M)

STD 0000
OBS 0000
STD 0010
STD 0020
OBS 0023
STD 0030
OBS 0049

184

TRANS.

NODC

REF. STATION
NO. MO.
Ol

00865 PG29

SURFACE OBSERVATIONS

POSITION

per

ANEMO. AIR
HGT. PRESS

19

LATITUDE

LONGITUDE

OR” ZEvTs

STD

STD

STD

STD

SAMPLE
DEPTH (M)

NODC

REF. STATION

NO.

MO.

DATE

DAY

O2zmi/I

SURFACE OBSERVATIONS

|

YEAR

HOUR |

LATITUDE

POSITION

LONGITUDE

00865] PG30 | O1 | 14 1961 | 21 | 26° 20/N | 055° 517E

ANEMO. AIR
9 PRESS
Her pRYY | WETY
1) ZN:

SAMPLE Toc Siejeq
DEPTH (M) v

0000 22 8 \s7 Bs)
0000 22 WS |i Bey)
0010 2A B)\t B39
0010 2A SIS) er Be)
0020 22. 9 \37 EO
0020 22 96 |37 40
0030 23 00/37 40
0030 23 00 |37 40
0050 23 BO |r Til
0050 223 30 \87 2
0070 Ae NZ IBS 92

185

SURFACE OBSERVATIONS

NODC DATE POSITION SONIC MAX.
REF. STATION DEPTH SAMPLE
NO. MO. DAY YEAR HOUR LATITUDE LONGITUDE UNCORRECTED] DEPTH
00865] PG30 | O01 1961 25° AON] OSS" Sr7= | 0073
WATER
ANEMO.| AIR
HGT. | PRESS aw aol) qae.
ue nae
SAMPLE To S °/oo ot DAD O2zmi/ VE i
DEPTH (M) y v
STD 0000 2 US |r sas
OBS 0000 22 UOHi(ee Ba
STD 0010 22 B82 \37 BS
STD 0020 22 Bt |e a
STD 0030 22 Bi i? Be
OBS 0036 RA OG Be
STD 0050 faz} PAS} ENS} {0S}
obs 0070 Ae Ut) gil

SURFACE OBSERVATIONS

00865

STATION

MAX.

SAMPLE
DEPTH

POSITION SONIC
DEPTH
LONGITUDE UNCORRECTED

WIND
SPEED| DIR. "[cou.] trans. |
05 | 04 er
SUBSURFACE OBSERVATIONS
eam
SAMPLE Tao Sice/ce = AD 2m I/I Vv
DEPTH (M) y y I i v v et : y
STD 0000 22 BR \h/ B22 25 77 |0 000
OBS 0000 22 SB IBV Bs 23 17
STD 0010 22 Ol |\}7 aé Za 1S | O22
OBS 0015 22 02 \37 25 BE 17
STD 0020 22 92 |B 25 2 TT 0) OG)
STD 0030 2A Wil |e Be 2A 0 | OB
OBS) 0030 22, Hil jar 2a 2 1/8
OBS 0040 BA W277 Be 2A We
STD 0050 22 BS Ne SNe 25 800 112
OBS 0050 22 sols 328 22 8)
OBS 0060 23 OBO 25 Zon SS)
OBS 0070 CUy Sah es) | 7/(0) 2 Re

186

SURFACE OBSERVATIONS

STATION

LATITUDE

POSITION

LONGITUDE

SAMPLE

DEPTH (M)

SONIC

DEPTH
UNCORRECTED

WATER

COL.

SURFACE OBSERVATIONS

DATE
STATION
MO. | DAY | YEAR HOUR LATITUDE
PG30 | O1 LB || LPS | OF 6

Ozmi/I

POSITION

LONGITUDE

HUMID-
ITY

SONIC
DEPTH
UNCORRECTED} DEPTH

SAMPLE

DEPTH (M)

TRANS.

MAX.
SAMPLE

WATER

COL.| TRANS.

187

113

O2mi/

~

SURFACE OBSERVATIONS

DATE POSITION

MAX.
SAMPLE
DEPTH

ANEMO. AIR
HGT.

NODC SONIC
REF. STATION DEPTH
NO. MO. DAY YEAR HOUR LATITUDE LONGITUDE UNCORRECTED

00865] PG30 | 01 iS | 1961 Pua || AS aon | O55" Sn = 0073

SEA SI

PRESS

WELL

20

SUBSURFACE OBSERVATIONS

SAMPLE Te S °/oo ot AD Ozmi/ Ve
DEPTH (M) y y vy vy y vy
STD 0000 ABZ BOWS 22 25 76 |0 O00
OBS 0000 22 BO \|Bv 22 2D US
STD 0010 RA Ys Tf BZ Zon | OmOR2
STD 0020 ie DUIS 23 25 7710 045
OBS 0029 2A BUNS 23 2D i Til
STD 0030 2A BS ef 21/ 25 9) 0 OT
STD 0050 23) S5N88) 845) 26 47 j0 105
ar oo061 24 01 |39 50 2 7
SURFACE OBSERVATIONS
NODC DATE | POSITION SONIC MAX.
REF. STATION DEPTH SAMPLE
NO. MO. DAY | YEAR HOUR LATITUDE LONGITUDE |UNcoRRECTED DEPTH
oo8es pe30|o1 | 15] 1961] 15 | 26 20'N 055 51/E 0073

WATER
‘|coL.| TRANS.

0019

0020
0030
0033
0043
0050
0052
0062
0071

ANEMO! |e AIR AIR TEMPERATURE | 14, aris
HGT. | PRESS Y ATHE
| 20
SAMPLE Talc
DEPTH (M)

Ozmi/i

22 BAIR Be 2D Uy
UR 32 IE SNS 25 79 10 044
BA Wet Be 2 79 |0 066
22 WA\Bt BS 25 2
22 iwi 7 B39 25 80
23 Wf 37 SY 23 38) | Rilo

188

STATION

SURFACE OBSERVATIONS

POSITION SONIC
DEPTH

MAX.
SAMPLE

A pay | YEAR | HOUR | LATITUDE LONGITUDE UNCORRECTED} DEPTH
7 7 3 7
| 00865) PG30 | O1 | 5) | 1961 | 18 | 26 20 N} 055 Hike 0073 | Ol |
UND ANEMO. AIR WATER
HST ues COL.} TRANS.
21
SUBSURFACE OBSERVATIONS
SAMPLE ue Sic/eo ot = AD OzmI/ Ve
DEPTH (M) Vv Vv L Vv y Vv vy
STD 0000 23 TS\B Be 25 81/0 000
OBS 0000 22 TOlBt 3 22 gil
STD 0010 22 78 |37 44 23 BT IO O22
STD 0020 22 BO |S Be 25 90)0 043
STD 0030 23 00/37 48 25 83 |0 065
OBS 0036 23 LIL IBe 69 22) 9B
STD 0050 23 44/38 24 26 28/0 104
OBS 0069 24 O07 |139 46 2 OZ
| SURFACE OBSERVATIONS
NODC MAX.
REF. STATION SAMPLE

DATE POSITION SONIC
DEPTH
DAY | YEAR HOUR LATITUDE | LONGITUDE UNCORRECTED
. / e i
NB || L9e | 2x 26 20 n | 055 Dll _Je |

DEPTH

AIR TEMPERATURE

SAMP.

DEPTH

STD 0000
OBg 0000
STD 0010
STD 0020
= 0020
STD 0030
OB 0035
OB 0045
STD 0050
OBS 0055
OB 0065
STD 0075
OB 0075

WE Toc S °/oo ot Ozmi/I
aD v v Vv Vv v v

23 EO BS Bt 26 52/0 104

247 ON IBS 2 BY 233 |@) LBs

189

SURFACE OBSERVATIONS

DATE POSITION
MO. DAY YEAR HOUR LATITUDE LONGITUDE
5 /

Ol

SONIC MAX.
STATION DEPTH SAMPLE
UNCORRECTED] DEPTH

SAMPLE
DEPTH (M)
STD
OBS
STD
STD
STD
OB
STD
OB

SURFACE OBSERVATIONS

POSITION

LATITUDE | LONGITUDE

7
055 48 E

ANEMO. AIR
HGT. PRESS

Hens,

SAMPLE
DEPTH (M)

Ozmi/I Ve

STD 0000
OBS 0000
OBS 0005

STD 0010
OBS 0010
OBS 0015

190

00865] PG45

SURFACE OBSERVATIONS

POSITION

STATION

Ol

LATITUDE

LONGITUDE

7
Som

055

7
48 E

ANEMO.| AIR HUMID- bye ate SEOuD | ae
SPEED] DIR. MGT RRESS MS TYPE awt,| DIR. | AMT.
| 01 | 03 20 [a2 a2 ee Cire
SUBSURFACE OBSERVATIONS
SAMPLE acc § eo ot SAD Oami/l Vi
DEPTH (M) v v v v y
STD 0000 22 UT2\36 Bi 25 41 |0 000
OBS 0000 22 Y2 BS wil Ze 4
OBS 0005 2A Ti |BO 82 2p ) 42
STD 0010 22 44/36 85 25 52/0 025
OBS 0010 22 44 |36 85 Zoe.
OBS 0015 22 O26 7 23 (5
SURFACE OBSERVATIONS |
NODC POSITION | SONIC MAX.
REF. STATION DEPTH SAMPLE
NO. LATITUDE LONGITUDE UNCORRECTED] DEPTH
2 / a /
| oo8ed pG4s | Ol 12 | 26 39 N]| 055 48 E | 0015
WIND AIR TEMPERATURE CLOUD SEA SWELL WATER
ANEMO.| AIR HUMID: bye ate | iS |
TyPE|ANT. DIR. | AMT. | DIR. [amr| cou] TRANS. |
03 | 4 | 4 | 00 | 0 7
SUBSURFACE OBSERVATIONS
SAMPLE 7 OG S °/oo ot = AD Ozmi/l Ve
DEPTH (M) v v y vy
STD 0000 Bey Is, 25 25 2910 000
OBS 0000 Ze Mey lee 2 23 29
OBS 0005 22 TU 86 82 25 40
STD 0010 Bp “vil |leiey — (3}3) Zo or | OMOZ6
OBS 0010 Age CN VeNsy Bie || Bay
OBS 0015 22 BY \B6 85 Ap ayh

191

SURFACE OBSERVATIONS

DATE ae SOUE
STATION PTH
YEAR | HOUR LATITUDE LONGITUDE UNCORRECTED DEPTH
/
PG45 | 01 16 | 1961] 15 39. 055 48 E 0015

jt an

AIR TEMPERATURE

SAMPLE
DEPTH (M)

STD 0000
OBS 0000
OBS 0005

STD 0010
OBS 0010
OBS 0015

WATER

i coL.

SAMPLE
DEPTH (M)

Ozmi/I

192

SURFACE OBSERVATIONS

NODC DATE | POSITION
REF. STATION
NO. MO. DAY YEAR | HOUR | LATITUDE | LONGITUDE UNCORRECTED] DEPTH
Dp / i 7
00865 PG45 | Ol Lg? || Jeska | Ol | 26 3S) Nn | 055 48 E | 0015 00
WIND avee.|| ai AIR TEMPERATURE | 11 wd CLOUD | SEA | SWELL ee WATER
RIG || SHES DRY ¥ WET Y Way TYPE aur,| DIR. | AMT. COL.| TRANS.
17 20 0 | | | yer) Geil Xs) | 3)2) | 1
SUBSURFACE OBSERVATIONS
SAMPLE TC, S °/oo ot = AD OemI/I Ve
DEPTH (M) y vy y y
STD 0000 22 48/36 88 22) BS} (0) @O@©O
OBS 0000 Bfo ley NBisy teh} 25 3
OBS 0005 22 49/136 86 Aisy Bil
STD 0010 22 30 | BS 22) 20) 10) 0)22)
OBS 0010 2A BO) |B 85) Be, '3\(0)
OBS 0015 22 DO 136) 1384 25 49
| SURFACE OBSERVATIONS
POSITION SONIC
STATION DEPTH
HOUR LATITUDE LONGITUDE UNCORRECTED] DEPTH
= 7 -
PG45 04 26 aS) IN |) OBS 48
WIND PNEMOMIEATR AIR TEMPERATURE | J... CLOUD SEA | SWELL |
HGT. | PRESS nine |) =U
SPEED] DIR. DRY W WET YW TYPE|AMT.| DIR aut. | DIR. jamr-|
| o2 | 01 | 18 18 9 | | 02 || Oi) OD] Ox 1 | |
SAMPLE O2mi/I Ve
DEPTH (M) y
STD
STD

193

SURFACE OBSERVATIONS

NODC DATE POSITION SONIC MAX.
ae STATION DEPTH SAMPLE

YEAR HOUR LATITUDE LONGITUDE UNCORRECTED] DEPTH
00865 PG45 1961 26 99 Moss 4a & 0015 | oo |

WATER

0 ; COL.) TRANS.

DEPTH (M)

STD 0000
OBS 0000
OBS 0005

STD 0010
OBS 0010
OBS 0015

SURFACE OBSERVATIONS

DATE POSITION SONIC MAX.
STATION DEPTH SAMPLE
MO. DAY | YEAR HOUR LATITUDE LONGITUDE UNCORRECTED] DEPTH

7 a 7
00865 PG32 | Ol | 17 | 1961 O7 | cosa | Ol

WIND

ANEMO. WATER

HGT.

AIR
PRESS

‘|cot.| TRANS

| 20

SAMPLE
DEPTH (M)

STD 0000
OBS 0000
STD 0010
OBS 0010
STD 0020
OBS 0020
STD 0030
OBS 0030
OBS 0044
STD 0050
OBS 0064
STD 0075
OBS 0084

SURFACE OBSERVATIONS

DATE
STATION
MO. pay | YEAR | HOUR
1

00864 p63 | 0) i7| 1961 | 12 | 26

NODC POSITION SONIC MAX.
REF. DEPTH SAMPLE
NO. LATITUDE | LONGITUDE UNCORRECTED} DEPTH

/ aq /
a NiLoss Bee

ae@.|| AIR AIR TEMPERATURE | oe CLOUD | SEA WATER
HTM PRESS ny TyPe|awT.| pir. | AMT. i cou] TRANS
| 02 3 | 1 | 26
SUBSURFACE OBSERVATIONS
SAMPLE T°Cc 8 ko ot = AD Ozmi/ VE
DEPTH (M) vy v Vv vy Y y
——__—

STD Pe) (KO) NE SNS 25 76]|0 000

OB 25 O@Ol8¢ Bi 25

OB AP OS NB —- Bi 25 TO
STD 25 O77 1IB0¢ BY 25 13 10 O23)

OB 2A T3uB7 Bi 25 81%
STD 23 23137 ©3 25 88/0 045

OB 23 A2Y\BY Be 2 3)
STD 23 26\37 93 26 10/0 065

OB 23 AS ise Nt2 26 24

OB 23 44/38 78 A ©)

SURFACE OBSERVATIONS

NODC DATE | POSITION
REF. STATION
NO.. MO. DAY YEAR | HOUR | LATITUDE | LONGITUDE

00865 pea | 01 17 | 1961 | 15 | 26) o5 nN | O55 S55 00

WATER
COL.| TRANS.

ered

SUBSURFACE OBSERVATIONS

SAMPLE S Vg ot = AD | O2mi/I Ve
DEPTH (M) Vv Vv Vv
STD Sy7/ 25 78 |0 000
OB a7 22 1
STD 45 22) 8350) O22
STD 43 25 80]0 044
OBS 56 25 89
STD 98 26 16 |0 064
OBS Zt 26 96

195

SURFACE OBSERVATIONS

DATE POSITION

STATION

MO. | DAY | YEAR HOUR LATITUDE LONGITUDE
a 7 2. 7
PG31 | ol U7 || Led | RS 26 O05 Nj 055 55 E—

ANEMO. AIR
HGT. PRESS

TRANS.

SAMPLE ree S °/oo ot O2miI/
DEPTH (M) .7 Vv Vv Vv

STD 0000 22 85 |37 41 25 82 |0 OOO
08s 0000 22 BS er Gil 22 (2

STD 0010 22 90/37 44 25) 8358) 022
OBS 0010 22 90/37 44 23 83

STD 0020 23 10 |37 76 26 02 |0 043
OBS 0020 23 10 |37 76 ZS 02

STD 0030 23 2h Bt 94 26 11 |0 062
08s 0030 23 24 |37 94 26 11
OBS 0045 23, OU |39 B36 2 2

SURFACE OBSERVATIONS

POSITION SONIC MAX.
STATION DEPTH SAMPLE
LONGITUDE UNCORRECTED] DEPTH

o 7
055 BS) le

SAMPLE ot = AD OzmI/I Ve
DEPTH (M) y v vy y v
STD 3)7/ 25 8310 000
Si B25 {32}

STD
STD

STD

196

SURFACE OBSERVATIONS

POSITION

STATION }——
MO.

LATITUDE

LONGITUDE

7 3 7
00865) PG3l | Ol 05 N]| 055 BS ls 00
WIND AMET. AIR WATER |
SPEED] DIR. BST | PRESS coL| TRANS. |
04 | 25 LS)
SUBSURFACE OBSERVATIONS
SAMPLE re 5 Vos ot = AD O2mi/ VE
DEPTH (M) vy v
STD 0000 22 TAB? 39 25 84 1|0 000
OBS 0000 22 Tas 39 25 84
STD 0010 22 80 \387 37 23 i 0) O22
OBS 0010 22 BO 37 Bi 2B Bil
STD 0020 22 os a7 Ail 25 8210 044
OBS 0020 22 S887 4a 23) 32
STD 0030 23 23/27 93 26) 09) 10) O65
OBS 0030 23 2 |v 93 26 O09
OBS 0045 23 DOWDE Be 2B 5
SURFACE OBSERVATIONS |
NODC DATE | POSITION SONIC MAX.
REF. STATION DEPTH SAMPLE
No. MO. | DAY YEAR | HOUR | LATITUDE | LONGITUDE UNCORRECTED] DEPTH
- / °. 7
00865 PG31 | Ol | 18 1961 | 3) | 26 05 n | OD) 5S |= 0048 00 |
WIND aneo.|| AIR AIR TEMPERATURE | 14 Ee ee CLOUD | SEA SWELL ies WATER
SPEED| DIR. HEM /GRRESS DRY W WET ¥ uy TyPe|anr.| DIR. | AMT. | DIR. |AMT. COL.| TRANS.
04 | 20 | 20 20 0 | | o1| 6 @ | 20 1 6
SUBSURFACE OBSERVATIONS
SAMPLE TG S °/oo ot = AD O2mI/I Ve
DEPTH (M) y v Vv Vv
STD 0000 22 UDa\Iav 31 25 82 )|0 000
OBS 0000 22 US \3% BT 25 32
STD 0010 22 BO \B7 39) Qs) 2 (0) O22
STD 0020 22 9 |B 40 25 83/0 044
OBS 0024 BE Iss |i Gil 23 82
STD 0030 23 W@\B7 ©2 25 94 |0 065
OBS 0045 23 55/38 @7 | 26 42

197

SURFACE OBSERVATIONS

DATE POSITION
REF, | STATION
DAY | YEAR | HOUR LATITUDE LONGITUDE
> - = :
00864 Po31| 01 | 18] 1961 | 06 05 N 055 55 6
aemo.| ain. | AIR TEMPERATURE
Bee | PISS ft oeos | aes
ani 20 | |
SUBSURFACE OBSERVATIONS
SAMPLE Oami/ Vi
DEPTH (M) v
STD 0000 22 719
OBS 0000 22 79 138 48% 26 65%
STD 0010 22 TS NSH 36 25 81
OBS 0010 Qe Te ier Be Bey 8) Il
STD 0020 22 UB NG -BxS 25) 82
OBS 0020 22 USS BU SxS 25 82
SiH) 0030 2S B30) eh sits) 26 05
OBS 0030 23) BO |i ahh Ae — (0)5)
OBS 0045 Be ET BS) ©) 2S sll
SURFACE OBSERVATIONS
DATE POSITION SONIC MAX,
STATION DEPTH _| SAMPLE
YEAR | HOUR | LATITUDE LONGITUDE UNCORRECTED| DEPTH
6 °, 7 S /
00865 PG31 1961 | 09 | 26 OS MNGROD Be IE | ~ 0048

WIND

ANEMO.
HGT.

=
>
=
m
Ee)

TYPE|AMT.| DIR. | AMT. | DIR. AMT. COL.| TRANS.
O02 | 6 4 | Ai 1 | | 6 | |
SUBSURFACE OBSERVATIONS
SAMPLE T°c S °/oo ot = AD O2mI/I Ve
DEPTH (M) v v v v Vv
STD 0000 22 BO VN 33) 25 78/0 000
OBS 0000 22 BO |B 33) 25 is
STD 0010 22 Uv \30¢ 233 22 U9 | O22
STD 0020 22 UZ \3 Be 25 79/10 044
OBS 0024 22 U2\3B 32 25 9
STD 0030 22 B85 50 Bis 25 95 10 066
OBS 0044 23 40) |B) BY) 26 56

198

SURFACE OBSERVATIONS

STATION

DATE

POSITION

PG31

YEAR HOUR
IQoK |p Ae

LATITUDE LONGITUDE
7 * /
O05 N}| 055 Dis [5

Avia AIR TEMPERATURE | 144) ate cLouD | SEA SWELL wa WATER
RRESS DRY WET WV ay TYPE an, DIR. | AMT. | DIR Jaw. coL.| TRANS. |
im a2 2 | ol a | 4 | > 2 | 6 ;
SUBSURFACE OBSERVATIONS
SAMPLE SAD O2mi/I Ve
DEPTH (M) y
STD 0000 000
OBS 0000
STD 0010 022
OBS 0010
STD 0020 044
OBS 0020
STD 0030 063
OBg 0030
OBS 0045
SURFACE OBSERVATIONS |
NODC DATE | POSITION SONIC MAX.
STATION DEPTH SAMPLE
[ | DAY YEAR HOUR LATITUDE | LONGITUDE UNCORRECTED] DEPTH
5 7 > =
00865) PG28 |} O1 | 20} 1961 | 06 26 U7 n | 055 BORE | 0070 | Ol
WIND aneus.|| am AIR TEMPERATURE | 14. nates CLOUD SEA | SWELL ere WATER |
SPEED| DIR. HGnsan RERESS Us! TYPEJAMT.| DIR. aut. | DIR. [an COL. TRANS. |
| o8 | 05 [aa 22 8 | op il || © || @5 3 | | al |
[ SUBSURFACE OBSERVATIONS
SAMPLE Tac) S °/oe ot = AD O2mI/I Ve
DEPTH (M) vy y vy y v
STD 0000 2a) OZ |e Se) 25 43 |0 O00
OBS 0000 22, 2 |\B@ Y2 25 43
STD 0010 23 W336 OF 25 41 |0 026
OBS 0010 Zon OSn SiG Se Ae it
OBS 0019 22, ©© |BQ ©5 25 43
STD 0020 22 O97 \Bo 9 25 47 1/0 O51
OBS 0029 BA 32 |r 34s 25) 183
STD 0030 22 84 |37 36 23 19 |O0 Ore
OBS 0048 23 2338 2h 26 34
STD 0050 23 28 \38 39) 26 441)0 113
OBS 0067 23 76 |40 06 2t Dt

199

SURFACE OBSERVATIONS

NODC DATE POSITION SONIC MAX.

REF. STATION DEPTH SAMPLE

NO. MO. DAY YEAR HOUR LATITUDE | LONGITUDE UNCORRECTED| DEPTH
y / Es /

0086 pois | Ol | 20) || WSoat_ | 22 24 50 n | 053 Z2cme

AIR
PRESS

ANEMO.
HGT.

AIR TEMPERATURE

HUMID-
ITY

EATHER:

13 02
SUBSURFACE OBSERVATIONS
SAMPLE ye S °/oo ot ZAD Ozmi/i
DEPTH (M) vy vy vy vy
STD 0000 2 2 |i 0) 2S) BT |) @OQ@=
OBS 0000 Ail ©2 |e SO) 2) Si
OBS 0005 Ail (ots eT 0) 29 29
STD 0010 21 64 |41 45 ZS) 23) \I0) (0) sal
OBS 0010 21 64/41 45 29 25)
OBS 0015 Zl Be \fal 2 ws) 135)
STD 0020 Pal yey SIE Sho) DS) (92 |(0) W)\2zi>
08g 0020 21 53/41 90 BS) 2
SURFACE OBSERVATIONS
NODC | DATE | POSITION SONIC MAX.
REF. STATION DEPTH SAMPLE
: DAY YEAR | HOUR | LATITUDE | LONGITUDE UNCORRECTED] DEPTH
3 7 a 7
2l 1961 | 06 | 24 50 n | 053 Acme
AIR a F WATER
PRES .
P : : COL.| TRANS.

17

SAMPLE Ue i S)°/e0 ot EAD Ozmi/ V5
DEPTH (M) y vy v Vv
STD 0000 Bi BB Wei oe 29 66/0 O00-
OBg 0000 21 52/41 94 22 (iS
OBS 0005 Qi Byte Wat Gil 2) 3)
STD 0010 Al Bil Wee O7/ 29 7S |@ Ola
OBS 0010 Pil Bli|ee2 O7 29 Tis
OBS 0015 foal GIS) eZ (Oy) 28) 7/8
STD 0020 21 50/42 08 2X TT | OF0—>
OBS 0020 21 50/42 08 2 7

200

SURFACE OBSERVATIONS

NODC DATE POSITION SONIC MAX.
REF. STATION DEPTH SAMPLE
NO. MO. | DAY YEAR HOUR LATITUDE | LONGITUDE UNCORRECTED] DEPTH
5 7; - =
| 00865) P618 | Ol Pa ee oe ee 24 50 n | 053 2 I | 0020 00
WIND aweme.|| air AIR TEMPERATURE | 14 pee CLOUD | SEA ; WATER |
SPEED| DIR Berea eaas> ny TyPe|awr,| DIR. cou.| TRANS. |
| 03 | 09 | 12 00 | | o| 09
SUBSURFACE OBSERVATIONS
SAMPLE TG S °/oo ot = AD O2zmI/I Ve
DEPTH (M) vy v vy y y y
ee Se Ee ee

STD 0000 O22 Ot |e Bes 2 2i |\Q) OOO

OBg 0000 22 Oli 54 2S Pir

OBS 0005 Al YS iA BH 2 30
STD 0010 Ai Bis veil 82 29 55 10 O20

OBY 0010 Pp ey <i 2B) B53)

OBY 0015 2 BQ hil 9S 28) 66
STD 0020 2 Bah ei 7 23) 98} 0) O2E>

OBgG 0020 2 Sayyau M7 2 fe}

SURFACE OBSERVATIONS

NODC DATE | POSITION
REF. STATION DEPTH
NO. MO, DAY YEAR HOUR | LATITUDE | LONGITUDE UNCORRECTED

°

00864 PG18 Ol 21 | 1961 | 22 | 24 50. N | 05, 2a |

WIND AIR TEMPERATURE cLouD SEA SWELL WATER
ANEMO.| AIR HUMID-
HGT. | PRESS Dorvy | wery | ITY pee | : | be |
DRYW | WETY TYPE/AMT.| DIR. | AMT. | DIR. |AMT. COL.| TRANS.
ne) ae | 62 olzel al lal
[. SUBSURFACE OBSERVATIONS
SAMPLE T°c S °/oe ot SAD Ozmi/I Ve
DEPTH (M) y y y y Y
STD 0000 21 84 (|41 38 29 14 |0 OO0O-—
OBS 0000 Ail 84 |41 38 29 14
OBS 0005 20 58441 36 29 48%
STD 0010 Zell 70 |41 52 29 2B | Oto
OBS 0010 Zi TQ) veal 52 29 28
OBS 0015 Zale yt | See Ie AS abi,
STD d 0020 21 56 |41 87 29 39) 0 O228-
OBS 0020 Ai Be A hz 29529)

201

SURFACE OBSERVATIONS

NODC DATE POSITION SONIC
REF. STATION DEPTH
NO. MO DAY | YEAR HOUR | LATITUDE | LONGITUDE UNCORRECTED] DEPTH
5 / /
00865} PGOl | Ol 25 | MW Sxeyil ||) ae | 26 28 n | O51 ZORE 0027
WIND

ANEMO. AIR

HGT. | PRESS
20
SAMPLE ot
DEPTH (M) y vy v | vy
STD 0000 20 18/40 55 BS ST) | OQ
OBS 0000 20 18 |j40 55 PY NES) Tf
OBS 0005 ZOOS | ea Z28 96
STD 0010 20 14 |40 55 28 981/10 O008-
OBS 0015 20 10/40 55 ASK *SKS)
STD 002C 20 O7 |j40 57 29 ONS ON OMG
- 0025 20 04/40 60 29 04
| SURFACE OBSERVATIONS
NODC DATE POSITION SONIC MAX.
REF. STATION DEPTH SAMPLE
NO. MO. DAY | YEAR | HOUR | LATITUDE LONGITUDE UNCORRECTED] DEPTH
= 7; =
00864 PGO7 | Ol 25 | 1961 | 18 | 26 Be IN || @Bal 0068 Ol
WAND ANEMO.| AIR WATER
T. | PRESS

SAMPLE
DEPTH (M)

STD

OBS
STD
OBS
STD
OBS
STD
OBS
OBS
STD
OBS

202

SURFACE OBSERVATIONS

STATION
MO.

POSITION SONIC MAX.
DEPTH SAMPLE
UNCORRECTED} DEPTH

00864 PG07 | 01

WIND ANEMO.| AIR SEA | SWELL + WATER
SPEED] DIR. SUSY se) aM, | DIR. |amr. COL.| TRANS.
| 02 | 33 20 2 | |

SUBSURFACE OBSERVATIONS
SAMPLE Tac S °/oo ot = AD O2mi/\ Ve
DEPTH (M) v Vv v v Vv
STD 0000 2h W2 a9 gil 28 17 |}O0 O0O-
OBS 0000 2h O2 39 Bil 28 dl 7
STD 0010 Cdl Als) 18)'5) SiS) Bs 22 0) OO i=
OBg 0010 2k ZSE\I39 OS 23 22
STD 0020 21 22/40 O04 B23 BE) 10) O@2>
OBJ 0020 21 22/40 04 28 29)
Sip 0030 21 24/40 05 BS 2S) (0 OW Z—
OB 0030 21 24 |40 05 2S 2S)
OBS 0045 21 46 |40 33 28 44 :
STD 0050 21 50/40 39 28 48/10 008-
OBS 0065 21 54/40 45 2s Dil
SURFACE OBSERVATIONS
NODC DATE | POSITION SONIC
REF. STATION DEPTH
No. MO. | DAY YEAR | HOUR | LATITUDE LONGITUDE UNCORRECTED] DEPTH
a 7 a 7
| 00865) PGO7 | Ol 26 1961 | 18 | 26 22 IN | OB 48 E 0068 | Ol |
WIND WATER
ANEMO.| AIR HUMID
IWEATHE :
SPEED] DIR. HT) /BRESS, Uys COL.| TRANS.
| 01 | 25 | 17 | 02
SUBSURFACE OBSERVATIONS
SAMPLE TG S °/oo ot = AD Ozmi/I Ve
DEPTH (M) vy v v vy Vv
STD 0000 2 2839 6s 28 00 |O0 000
OBS 0000 2 Ze) |S) fais} 28 00
STD 0010 2l 26 \39 72 Zo) OSs OOO n
Bg 0010 Al 26 |B9 72 28 O38
STD 0020 Zi Ake so 92 28 19 jO OOL1
OBS 0020 Ai 24 |S) §2 28 19
STD 0030 2) 22) 410) Feo: ZO ile | OmOOO
OBS 0030 21 22 |40 02 2s BT
OBS 0045 Zi 4S |4OQ 7 Bis) 35)
STD 0050 21 40 |40 23 Aish Bis} 0) (NO)Z1—
“S* 0065 21 52 |40 46 Bish |B

203

STATION

ae [ow | vam [ren |
27

SURFACE OBSERVATIONS

POSITION SONIC MAX.
DEPTH SAMPLE
LATITUDE LONGITUDE UNCORRECTED] DEPTH

e 7 cs 7
27 16 N{ O51 56 E 0051 00

SEA

TYPE/AMT.| DIR.

SUBSURFACE OBSERVATIONS
SAMPLE ree S Soo or AD Ozmi/I VE
DEPTH (M) y v v v v v
STD 0000 21 78 139 O83 27 36/40 OOO
OBS 0000 21 138139) {0s 2 BS
STD 0010 f21V ts} lies} (0)5) QT © Sy Th IQ). (0K0) 7/
OBS 0010 il 32 Weis) (0)5) At 2) 7
STD 0020 Zi fio) isis) 1S) 2? 45/0 014
OBS 0020 ZO ONO si 2 45)
STD 0030 21 96/39 14 ZY BS) 10) W2r
OBg 0030 Al SEES 1A) an BS
STD 0050 22 44 |40 05 20 25 1@ O30
OBS 0050 22 44 |40 05 2 93
SURFACE OBSERVATIONS
NODC DATE | POSITION SONIC

REF.

STATION
MO DAY

YEAR HOUR | LATITUDE

DEPTH
| LONGITUDE UNCORRECTED} DEPTH

NO
00864 P

7

G04 | Ol | 27 | 1961 |] 04 | 27 36 N Ol
ANEMO.| AIR See Te ORES HUMID: EATHER
| 16 2a a 2 7 fT om
ar aaa |
SUBSURFACE OBSERVATIONS
SAMPLE ile T°c mil S "Joo ot = AD Ozmi/I Ve
DEPTH (M) y Y v vy v Vv
STD 0000 Zi 8 39 7 2? 37/0 000
OBS 0000 AM HS |S) (0)7/ AT Sif
STD 0010 Zk 87 BOS @5 Zs OOK
OBS 0010 2N b&i7/ 32 @5 2 35
STD 0020 Al iS) |S) OS C2 25 ll @ilS
OBS 0020 21 895/39) 306 2 B5
STD 0030 22 82/39 69 2 AS |@ O22
OBS 0035 ey 110) |S) 8) 27 66
STD 0050 faey Alls) |40) 25) 27 89 |0 029
OBS 0050 23 He EO 2S 2Y we
OBS 0060 22 88/40 31 28 O02

204

SURFACE OBSERVATIONS

NODC DATE | POSITION SONIC MAX.
REF. STATION DEPTH SAMPLE
NO. MO. | DAY YEAR | HOUR | LATITUDE | LONGITUDE UNCORRECTED] DEPTH
S i . 7
00865 PGO5 | Ol | Zi || West | 10 But 17 N | 052 40 E | 0055 (il
MIND ANEMO.| AIR WATER
HGT. | PRESS cor eT
++
Sees
SUBSURFACE OBSERVATIONS
SAMPLE 7 2 S °/oo ot = AD O2mI/I Ve
DEPTH (M) v v vy y v
STD 0000 22 22 \88 Be 26 88 |0 OOO
OBS 0000 Dp 22 \eN3 BS) 26 88
STD 0010 Qu fesil ess} By 7/ 27 00/0 O11
OBS 0010 2k il Be Sy 27 (00)
STD 0020 Bil Bi Be 6 2 Wr (Ci O22
OBS 0020 2 Bil |B 6%) 2 OT
STD 0030 BS OS eo) iil 27 8210 028
OBS 00350 23) ODe|40) et 2 &2
OBS 0040 23 05 |40 20 2 89)
STD 0050 Be) (0)3) Bio) il 27 90)j0 034
OBS 0055 23 W2|\KkO 22 2Y Sil
|
SURFACE OBSERVATIONS
NODC DATE POSITION SONIC MAX.
REF. STATION DEPTH SAMPLE
No. MO. DAY | YEAR HOUR LATITUDE LONGITUDE UNCORRECTED| DEPTH
2 / Dy 7
00864 P605 | Ol 27 | ian | 23 All U7 Nj) OS2 40 E 0055 | Ol

WIND arena! aya || A TEFSRATORE | oceans SWELL a WATER
HGT. | PRESS ITY ;
DRYW | WETY DIR. AMT. co. TRANS.
Tn onal 7a

|
|

SAMPLE
DEPTH (M)

0000
0000
0010
0010
0020
0020
0030
0030
0040
0050
0055

38 47

38 47

38 45

38 45

38 68

38 68

39 76 || 2r 600 O25
39 7 | 27 60

40 18 | 27 a7

40 23 21 9110 036
0 26 || 27 96

205

SURFACE OBSERVATIONS

NODC
REF.
NO.

STATION

DATE

| POSITION SONIC MAX.

MO.

DAY

YEAR | HOUR | LATITUDE | LONGITUDE

DEPTH
UNCORRECTED

SAMPLE
DEPTH

| 00865 pGo5 | 01

WIND WATER
ANEMO. AIR
HGT. PRESS ; coL.| TRANS. |
| 13 2 |
SUBSURFACE OBSERVATIONS
SAMPLE Tf &@ S °/oo ot = AD Ozmi/i VE
DEPTH (M) Vv Vv Vv v Vv
Ne ee eee
STD 0000 21 66/38 44 | 26 950 000
OBS 0000 21 66|38 44 | 26 95
STD 0010 21) 6738 945) || 26) 5y/omonr
oBg 0010 21 67/38 45 | 26 95
STD 0020 21 98/38 85 | 27 17]0 021
OBS 0020 al 93/53 85 | 2e. a7
STD 0030 22 84/39 88 | 27 70|0 028
oBg 0030 22 BRED 85 | 20 TO
OBY 0040 23. 05|40 13 | 27 83
STD 0050 22 98|40 24 | 27 94/0 034
OBS 0050 2a 9840) 1248 eno

SURFACE OBSERVATIONS

POSITION

NODC DATE

REF. STATION

NO. MO. | DAY | YEAR HOUR LATITUDE
| 00865 pG0e | Ol | 29 | DG |G:
WIND AIR TEMPERATURE

ANEMO. AIR

HGT. PRESS

SUBSURFACE OBSERVATIONS
SAMPLE T°c S °/oo ot = AD OzmI/ Ve
DEPTH (M) v v Y v vy
0000 Al GE 9 GS 27 81/0 000
cies 0000 21 44139 49 21 taal
0010 Ail G2 |B xs} 27 81 jO 003
OBS 0010 2 G2 iB 4s Zu {31)
0020 Oil Gi i) Bs 27 83/0 006
OBS 0020 ak Gy Bo 3) ZU es)
0030 Zl 90 |3) Ve 28 04 |0 008
OBS 0030 2 YO 39 Ve 28 04
OBS 0039 2N SNe; |KO) @il 28 06
0050 Zs is| Ono 28 07 |0 010
OBS 0054 Ak OT |KO OS 28 08
OBS 0074 22 34/40 26 28 14

206

SURFACE OBSERVATIONS

NODC POSITION SONIC MAX.
REF. STATION
NO.

DEPTH SAMPLE
LATITUDE | LONGITUDE UNCORRECTED] DEPTH
5 7 = =
00865 PGil 26 22 N{ 052 AG Ie 0066 Ol

ES SS) TyPE|AMT. DiR. | AMT. COL.| TRANS.
03 5 | 6 | 33 | 2 | |
SUBSURFACE OBSERVATIONS
SAMPLE | u oe S Whe Ozmi/l
DEPTH (M) v
STD leone A As es) teh
OBS 0000 2h AB ISO ez)
STD 0010 2k 26 \239 16
OBS 0010 Al AS BS) 5
STD 0020 Bik 2S) BV) Ts)
OBS 0020 Bil) BSF ENS). Tle)
STD 0030 Zi BO WBS 7/
OBS 0030 2 BO) IBS) 7/7/
OBS 0040 21 44/139 95
STD 0050 21 46/40 10 Zone i|On OR
OBS 0060 21 48 |40 22 As 35)
SURFACE OBSERVATIONS
NODC | DATE POSITION SONIC MAX.
REF. STATION DEPTH SAMPLE
NO. MO. YEAR HOUR LATITUDE | LONGITUDE UNCORRECTED] DEPTH
a 7 a 7
00865) PGOS | O1 30 | 1961 20 02 n| O51 Dee 0033 | 00
WIND AIR TEMPERATURE WATER
ANEMO.| AIR HUMID
IWEATHE VIS.
aie aes| baled WETY Uae | COL.| TRANS.
| ig) | | 03 | 5 | 7

SUBSURFACE OBSERVATIONS
SAMPLE if Tac Sac ot = AD OzmI/ Ve
DEPTH (M) v y v v Vv v
STD 0000 20 96/40 O7 28 39/0 O000-
OBS 0000 20 96 |40 O7 28939
STD 0010 20 99/40 06 AS BT |) OO@2=
OBS 0010 20 99/40 06 23 Bi
OBS 0019 20 72 |40 25 Q&S 159)
STD 0020 ZOOM Onn Ono 28 63 |0 006-
STD 0030 1S) O8 40) 72 ZS) NB) |) OZ
OBS 0032 19 80 |40 84 2S) 28)

207

SURFACE OBSERVATIONS

NODC DATE POSITION SONIC MAX.
REF. STATION DEPTH SAMPLE
NO. mo. | DAY | YEAR HOUR LATITUDE LONGITUDE UNCORRECTED] DEPTH
S = - -
00865 PG1O} Ol SHO) |, Wess Ps | 25 44 N]} 052 28 E 0046 00
WIND AIR TEMPERATURE c WATER

ANEMO. AIR

HUMID-

LOUD SEA
EATHE
Gna HERES iN TYPE/AMT.| DIR. | AMT.
12 70s) Rell en ae | ee
—=Sal
SUBSURFACE OBSERVATIONS
—_—|
SAMPLE acc Sio/se ot ZAD OzmI/I Ve
DEPTH (M) y vy vy vy vy Vv
e591) (2) 0000 Di a) AO) 28 26/0 O00-
OBS 0000 21 Seo) a2 28 AS
STD 0010 21 S45/40) 3 28 27) ||) C@K=
OBS 0010 21 54 |40 13 2 ATi
STD 0020 21 56 |40 16 28 29/0 003-
OBgG 0020 21 56/40 16 28 29
STD 0030 21 55 |40 14 28 27 )0 004—-
OBS 0035 21 54/40 12 2826
SURFACE OBSERVATIONS
eas Be
NODC DATE | POSITION
REF. STATION
No. MO. DAY YEAR HOUR | LATITUDE LONGITUDE
& / 7
| 00865 PGO9 | 01 Zl} WOS WR | OS 25 Zi || _ Ob2 36 E
WIND CLOUD
AIR
PRESS ay) WEATHE |

TYPE aut.| DIR.

SAMPLE
DEPTH (M)

STD 0000
OBS 0000

0010
0010
0020
0020
0030
0030

OBS

OBS
STD
OBS

4 6 | 33

SUBSURFACE OBSERVATIONS

O2mi/I Ve

60
60

0 013-

208 o

SURFACE OBSERVATIONS

NODC POSITION SONIC MAX.
REF. STATION DEPTH SAMPLE
NO HOUR LATITUDE LONGITUDE UNCORRECTED] DEPTH
° / 0 7
| el PGO9 | Ol 14 25 21 n | 052 Biome 0029 | 00 |

AIR TEMPERATURE

HUMID- WATER

us = ie - COL.) TRANS.

| SUBSURFACE OBSERVATIONS

SAMPLE TG | 3 Ykeo ot | = AD Ozmi/I Ve
DEPTH (M) y v v v v

STD 0000 20 90/40 39 28 65/0 O000=—

OBS 0000 20 90 |40 39 Bey (35)

OBS 0005 20 94/40 40 28 64
STD 0010 20 94/40 40 28 64/0 005=

OBS 0015 20 92 |40 40 2s} 95)
STD 0020 20 90/40 44 28 68/0 010—

OBS 0025 20 86/40 50 ZO meee

SURFACE OBSERVATIONS

DATE | POSITION

STATION

MO. | DAY

YEAR | HOUR | LATITUDE

00865 PG25 | 02 | 02 1961 | ia | 25

WIND AEM Cul Waren EAUSUEMEERATURE S| | ony cLoup WATER
HGT. | PRESS miny | PELL ;
SPEED] DIR. TYPE|AMT.| DIR. 3 ; : COL.| TRANS.
| 06 | 16 | a2 ee Eales
SUBSURFACE OBSERVATIONS
SAMPLE Tee S “Joo ct = AD OomI/I VE
DEPTH (M) y y y y y y
STD QO 000
OB
STD Q Oll
OB
OB
STD QO O16
OB

vv 209

SURFACE OBSERVATIONS

DATE POSITION SONIC MAX.
STATION DEPTH SAMPLE
MO. | DAY YEAR | HOUR LATITUDE LONGITUDE UNCORRECTED} DEPTH
Ol

©

© /
26 Oa Ness DOs ez

AIR TEMPERATURE CLOUD SEA

rl | oe [reer] om [a
fosfzs | [as feeal | | oal[sfesl «)

SAMPLE = AD
DEPTH (M)

SURFACE OBSERVATIONS

DATE | POSITION

oO. DAY YEAR | HOUR | LATITUDE LONGITUDE
2 || @2 |

7 s 7
1961 | 09 26 26 n | 055 O1l_E

STATION

NO. M
| 00865 PG2T | 0

aNemo.| ain | AlR TEMPERATURE ‘ ; ] WATER
HGT. | PRESS 4 B
: : : ; : COL.| TRANS.
le ? : aa
SAMPLE
DEPTH (M)
STD 0000
OBS 0000
OBS 0005
STD 0010
OBS 0010
OBS 0015

210

SURFACE OBSERVATIONS

POSITION SONIC MAX.
STATION DEPTH SAMPLE
MO. LATITUDE | LONGITUDE UNCORRECTED] DEPTH
: 7 2 7
PG22 | 02 09 n | 054 2 [= | 0088 Ol |
ANENOS| AIR CLOUD | SEA | SWELL all WATER
Hea RRESS DRY ¥ WET ¥ TyPe|ant,| DIR. aut. | DIR. [amr-| [cot.] TRANS.
18 ZOm> | SleZalees 1| |
SAMPLE 7 ee OzmI/l
DEPTH (M) vy
SD) 0000 Dn Sie}
OBS 0000 Zi Sei
STD 0010 22 @ll
OBS 0010 22 O1
STD 0020 2 Se}
OBg 0020 Zi OE
STD 0030 22 04
OBg 0030 22 O04
OBS 0045 23 O04
STD 0050 BS (0)6)
OBS 0060 BS) (0G)
STD 0075 23 Of
OBS 0085 23 (os
SURFACE OBSERVATIONS
NODC DATE | POSITION SONIC MAX.
REF. STATION DEPTH SAMPLE
NO. MO. DAY YEAR HOUR | LATITUDE LONGITUDE UNCORRECTED] DEPTH
$ 7 2. 7
00865 PG22 | 02 OVS} ISS ab | es |) Ze) O09 N} 054 36 E | 0088.
arene! ane AIR TEMPERATURE | 1.41 ate CLOUD | SEA SWELL sate WATER
BCT acRESS Huy TYPE|AMT. DIR. | AMT. | DIR. |AMT. COL.| TRANS.
| Ne 00 | | o | O7 1 7
E SUBSURFACE OBSERVATIONS
SAMPLE Te Sho/ 25 ot = AD Ozmi/I Ve
DEPTH (M) vy y y y
STD 0000 ZA OER 38 i, 26 63 |0 000
OBS 0000 Pe (Oe eyes 7 2 (3)
STD 0010 22 OWS |B 7 26 63 |0 014
OBS 0015 22 O35 Be iy 26 63
STD 0020 22 Ws |B} 2 26 6510 028
OBS 0025 RA OS 33 22 Ps (8)
STD 0030 22 S2\|B8 27 27 10/0 040
OBS 0035 22 84 |39 54 27 44
OBS 0045 23 06/40 16 Zip, 185)
STD 0050 232 06 |j40 20 2 eye} |e) Oz)
ops 0060 23 06/40 26 2 23
STD ~°| 0075 23 (0/0) 32 2 Di NO Odes
OBS 0085 23 08/40 34 2 VE

211

SURFACE OBSERVATIONS

STATION

DATE POSITION

P
UNCORRECTED

| 00864 PG23

DEPTH
MO. | DAY | YEAR | HOUR LATITUDE LONGITUDE
2 / Y /
02 @S | XPOS) 25 41 N| 054 43 E

WIND AIR TEMPERATURE
EMO.| AIR HUMID
ANGI. | PRESS IT cr
18 | 00 |
SUBSURFACE OBSERVATIONS
SAMPLE TraAG) S °/oo ot = AD O2mi/ Ve
DEPTH (M) Vv Vv Vv y
STD 0000 Zl SONS S34 27 59 }0 000
OBS 0000 2 BOWES) ss 2Yy Be
STD 0010 al BB |39 B36 27 58 j)0 005
OBg 0010 2 88 |B 36 2t Be
STD 0020 Ai SHfe\
OBG 0020 2159/8
STD 0030 22 NO
OBS 0030 22 KO)
OBg 0039 Ak 7a
STD 0050 Ql 67
oBg 0054 21 64
SURFACE OBSERVATIONS
NODC DATE
REF. STATION | pe te
: MO. DAY YEAR | HOUR | LATITUDE LONGITUDE UNCORRECTED] DEPTH
= ; -
Bea. | oe [oallasen a2 as a Nose sie | oo |
ANEMO.| AIR ARV UISURECATORE 1 scarry CLOUD | SEA | SWELL WATER
HGT. | PRESS ity |WEATHE
TyPE| AMT. DIR. amr. | DIR. COL.| TRANS
18 | 20 6 | col [ol eal 2
SUBSURFACE OBSERVATIONS
SAMPLE ° °/oo aces
DEPTH (M) ‘ y a ct ” 4 = AD O2mi/I Ve
STD 0000 2Q 8a
OBS 0000 20 84
STD 0010 20 88
OBS 0013 20 89
STD 0020 20 90
OBS 0023 20 90/41 44 29 45

212

SURFACE OBSERVATIONS

| POSITION

STATION
MO. | DAY LATITUDE

AIR TEMPERATURE

ANEMO.| AIR HUMID- |v eatHeRt
HGT. | PRESS DRYY WETY ITY
| tS) | Aut 7 | | | eye) Ol 2 |
SUBSURFACE OBSERVATIONS
SAMPLE Tac: Shp ot = AD Ozmi/ Ve
DEPTH (M) v | v y
STD 0000 20 96 |40 96 29 O7 |0 000-
OBS 0000 20 96/40 96 29 OF
STD 0010 20 92140 96 BEY ois) 0) OOK)
OBg 0010 20 92 )40 96 Zo OS
STD 0020 20 91/40 95 2D 07 © OLS
OBS 0020 20) 91140 = 915 22) Of
STD 0030 20 92/40 95 2D OT 10 O27
OBS 0033 20 92 )40 95 Ze) OT
SURFACE OBSERVATIONS |
NODC POSITION SONIC MAX.
REF. STATION DEPTH SAMPLE
NO. LATITUDE LONGITUDE UNCORRECTED] DEPTH

=

7
25 20 N

=

7
054 16 0035 00

CLOUD SEA | SWELL WATER
HUMID-
WEATHE ;
Une — DIR. aw. | DIR. lam. coL.| TRANS. |
Moa Lele ase eae
SUBSURFACE OBSERVATIONS
SAMPLE S Jeo ot =AD OzmI/I Ve
DEPTH (M) Vv Vv v
STD 0000 Zi AS Aso) hil 28 89/0 O000-
OBS 0000 21 16/40 81 28 89
STD 0010 21 13/40 80 28 90/0 OO7-
OBS 0010 2k 213 40 8© 28 90
STD 0020 20 96/40 89 2) Oil |@ OLB=
OBS 0020 20 96 |40 89 2 wil
STD 0030 20 V5 |EOQ M6 29 O7 |O0 024-
OBS 0033 20 95 |40 98 29 08

213

| SURFACE OBSERVATIONS

POSITION SONIC MAX.
. STATION DEPTH SAMPLE
oO. YEAR HOUR LATITUDE LONGITUDE UNCORRECTED] DEPTH
o / a 7
00865, PG20 Se 08 | 1961] 03 | 25 20 N 15 E

ANEMO. AIR AIR TEMPERATURE HUMID CLOUD | sweut | ais WATER
c PRESS i

re ie ee eee ok

SUBSURFACE OBSERVATIONS

Ozmi/t

SURFACE OBSERVATIONS

POSITION

SAMPLE O2mi/ Ve
DEPTH (M) y
=e}
STD 0 000-
OBS
STD 0 000-
oBg
STD 0 O0Ol1=
OBS
STD 0 002=
OBS
OBY
STD 0 003-
OBS
ri

214

STATION

SURFACE OBSERVATIONS

DATE

POSITION

MO. DAY YEAR | HOUR | LATITUDE | LONGITUDE UNCORRECTED] DEPTH
pelcl Nocll oollimcenl Noalllizelmuss INilwosstulz6 ell Noogatl|loo
SEA | SWELL WATER |
VIS.
cou.| TRANS. |

SAMPLE
DEPTH (M)

STD 0000 ail (0) \Isifs}_ BS) Qt 22
OBS 0000 2h tO Bs bs BY Pa
OBS 0005 2il 10/38 60 200 22
STD 0010 Aq Mees |e} SSL Zul iree
OBg 0010 2 Wes Sey il 2 22
OBS 0015 AN 12/38 63 27 24
STD 0020 21 03 38 14 2a 25)
OBS 0020 ask {o)zy eM! 74 27 35
SURFACE OBSERVATIONS |
Nopc DATE POSITION SONIC MAX,
REF. | STATION DEPTH _| SAMPLE
NO. YEAR | our LATITUDE LONGITUDE UNCORRECTED] DEPTH
0086 PGi3) 02 10 See 04 26 53°N 053 26 0022 00
WIND cLoup | SEA | SWELL | WATER
ANEMO.| AIR HUMID
EATHE VIS.
SPEED] DIR. | Pcie eB RESS fin = AMT) pin. | amt.| pir. [AMT [cou.] trans.
03 15 | 00 | a) fa) a 7
r= |
SUBSURFACE OBSERVATIONS
SAMPLE | y OG “|| S "Joo ot ] = AD Ozmi/I T Ve |
DEPTH (M) y y y
STD 0000 20 98 |38 74 27 36/0 000
OBS 0000 20 98 |38 74 BU 2S
OBS 0005 20 98 |38 74 AY BMS)
STD 0010 20 99 |38 76 QU 2X3 | O@7
OBS 0010 20 99 |38 76 Ot BE
OBS 0015 Bik (2 eve! 7/5) 2 BE
STD 0020 21 00 /38 76 2U B37 |Q Olé
OBg 0020 al @OOlEG TS || 2e Br
215

SURFACE OBSERVATIONS

NODC POSITION
REF. STATION PTH
NO. — LATITUDE LONGITUDE UNCORRECTED DEPTH
. /

HGT. | PRESS

SEA SWELL WATER
vis.
AMT. COL.| TRANS.

SURFACE OBSERVATIONS

POSITION

ao | ae. Sees
LONGITUDE
a /
(Niassa) Glee le

WIND
SPEED DIR.
05 | 32
SUBSURFACE OBSERVATIONS
SAMPLE T°c S °/eo DAD O2mI/I
DEPTH (M) v
STD 0000 Ai ig} |e) 7/2
OBg 0000 Ai is} (Ex 7/2
OBg 0005 21 18(|38 70
STD 0010 Al AGO IE 72
0Bg 0010 2 2ons8 72
OBY 0015 Al Ra\|Be 7
STD 0020 21 16/38 75
OBS 0020 21 16/38 75

216

| SURFACE OBSERVATIONS

NODC POSITION SONIC MAX.
REF. STATION DEPTH SAMPLE
NO. MO. YEAR HOUR LATITUDE | LONGITUDE UNCORRECTED] DEPTH

é 1

p 7 o 7
26 51 n | 053 OO E 0080 io)

AIR TEMPERATURE SEA SWELL WATER
vis.
DRY WV WET YW AMT DIR. |AMT COL.| TRANS.
15 re) 3 | i | | 7
SUBSURFACE OBSERVATIONS
SAMPLE ree S °/oo cn = AD Ozmi/I Ve
DEPTH (M) y y y y y ‘|

STD 0000 2h Ber Ves 77 7/ 2 22) |) (oxoyo)
OBS 0000 21 54/38 77 Aut Bz)

STD 0010 Ar BO) BE) 7 2f 24/0 008
a8 0010 2 BOSS 77 27 24

STD 0020 Bil Bie IB} 7 2Y 3s |) OAT
ops 0020 Cl B85) eis 7 2 Be

SID .|| GOO) Zl GO ee 23 27 38/0 024
OBS 0030 2 PeGe 318) 93 By BN}
OBS 0045 2 YB WBS #5) 2 1/0)

STD 0050 ee say ess) Tea 24 Ur iO O84
OBg 0059 22 70/40 02 2 By5

STD 0075 22 68 |40 03 27 86/0 043
OBS 0079 22 68/40 03 27 86

SURFACE OBSERVATIONS

POSITION
REF, STATION
NO. £ LATITUDE LONGITUDE

tal: 7 ° 7
00865 PG14 39 N| 053 28 le

WIND CLOUD SEA [ SWELL WATER
E VIS.
SPEED| DIR. TYPE|AMT.| DIR. au, | DIR. [amr. COL.| TRANS
| 10 | 32 0 | 32
SAMPLE TOG S °/oo ot Oami/
DEPTH (M) vy v v
STD 0000 Au ibys bz 27 O02 |0 000
OBS 0000 AN il isis Bz Bi (2
OBS 0009 AN Br jee Bs 27 06
STD 0010 BN yf} \eis} 3} 27 08 |0 O10
OBS 0018 Ail ( WENe} TS) 2 2@
STD 0020 21 64 |38 19 27 22 |0 020
OBS 0027 2k ©3236 O82 BU zi
STD 0030 2h B77 |Be o> Bll EST NO (0\27
OBS 0045 A Sb |e) Sars |) By (oye
Sif.) | 0050 Zi US 9 FO) 28 2) 10) O25
OBS 0068 22 39 |]40 19 280M
STD d 0075 Zee oe Om tS Zon OL | OMO38
OBS 0077 22 64/40 18 2T, ‘h2)

217

SURFACE OBSERVATIONS

SONIC MAX.
DEPTH SAMPLE
YEAR LATITUDE LONGITUDE UNCORRECTED] DEPTH

POSITION

STATION

PGL5

ie
mes) a

SUBSURFACE OBSERVATIONS

SAMPLE Ozmi/
DEPTH (M)

SURFACE OBSERVATIONS

DATE POSITION

STATION
NO. : MO. | DAY | YEAR oot
| 00865 PGLe | o2 | 16 | 1961 | 07

AIR TEMPERATURE

LATITUDE LONGITUDE

SONIC MAX.
DEPTH SAMPLE
UNCORRECTED] DEPTH

SEA
[af amo

ANEMO, AIR
HGT. PRESS

16

Rais: |

SAMPLE O2zmI/
DEPTH (M)

218

SURFACE OBSERVATIONS

NODC DATE POSITION SONIC MAX,

REF. STATION DEPTH SAMPLE

NO. MO. DAY YEAR HOUR LATITUDE [ LONGITUDE UNCORRECTED] DEPTH
5 7 0 7

00864 pci | 02 1S || LISA || 1S 22) 19 n | 053 25) 00

ANEMO.| AIR : SUAIER
WISI, |) NESS COL.| TRANS.
14 [|
SAMPLE 7 IG S Yeo
DEPTH (M)
STD
OBYg
OBYg
STD 0010 20 90 |/40 42 23 87 10 O@5=
OBS 0015 20 91/40 42 Omen
STD 0020 20 89/40 45 28 69/0 010=
OBS 0025 20 87 |40 46 ZO meal
STD 0030 20 86 |40 46 28 71/0 O16-
OBS 0035 20 86/40 46 28 Uh,
SURFACE OBSERVATIONS |
NODC DATE POSITION SONIC MAX.
REF. STATION DEP1H SAMPLE
NO. MO. DAY | YEAR HOUR LATITUDE | LONGITUDE UNCORRECTED] DEPTH
o 7 ° 7 oF
| 00865 pais | 02 16 | 1961 | 20 | 25 O7 N | 053 27 |e | 0026 | oo |
If
WIND ANEMO.| AIR AIR TEMPERATURE LORS CLOUD SEA SWELL | WATER |
Hct. | PRESS ITY EATHE VIS,
DRY W WET YW TYPE|AMT.| DIR. aur, | DIR. [amr cou,| TRANS. |
| 15 19 4 | 00 ©} || BO) 1 v
SUBSURFACE OBSERVATIONS
SAMPLE re S Joo ot = AD O2mI/I VE
DEPTH (M) v v v v
STD | 0000 20 74
OBS 0000 20 74 |37 33* | 26 36%
OBS 0009 20 TOO 7 28 82
STD 0010 20 69/40 6/7 Ze.
OBS 0014 20) 53/40 93 29 16
OBS 0019 20 54 |40 96 29 18
STD 0020 20 54/40 96 29 18
08s 0023 20) D240) 9/6 29 19

219

BIBLIOGRAPHY

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