CENTRAL CALIFORNIA COASTAL CIRCULATION STUDY
CTD OBSERVATIONS
CRUISE 8404, OCTOBER 1984
by
Dudley B. Chelton
P. Michael Kosro
/
,/college
of Oceanography)
Oregon State University1
Corvallis, Oregon 97331
Data Report 128
Reference 87-04
January 1987
Minerals Management Service
U.S. Department of the Interior
Contract No. 14-12-0001-30020
Raytheon Service Company
Subcontract No. 9330936556
PREFACE
This report represents the third in a series of four data reports on CTD
data collected as part of the Central California Coastal Circulation Study
(CCCCS).
The introductory text of each report summarizes the scope and purpose
of CCCCS, gives an overview of oceanographic and meteorological conditions
during the particular CCCCS survey presented in the report, and summarizes the
sampling procedures, calibration and data processing techniques applied to the
data.
Much of this text is the same for all four reports.
However, rather
than reference the text of the first report in subsequent reports, all of the
details are included in the text of each report.
Although this results in a
certain amount of redundancy, the advantage is that each report is totally self
contained.
Most of the differences in the text for the four reports are in the
overview of oceangraphic and meteorological conditions and the discussion of
sampling and calibration procedures.
asterisk in the Table of Contents.
These sections are marked with an
TABLE OF CONTENTS
Preface
Abstract
Introduction
1
*Overview of October 1984 oceanographic and meteorological conditions
.
6
*Sampling Procedures
14
*Calibration
17
Data Processing
27
Data Presentation
31
Acknowledgements
37
References
38
Figure Sections
Locations, times, and depths of October 1984 CTD stations
Maps of October 1984 CTD station locations and bathyinetry
Data Listings at Selected Depths
Vertical Profiles
Temperature -
Salinity
Plots
Maps, Full CCCCS Region
Maps, Snapshot 1
Maps, Snapshot 2
Difference Maps, Snapshot 2 minus Snapshot 1
Vertical Sections
Difference Sections, Snapshot 2 minus Snapshot 1
*
text
in sections marked with an asterisk is different in each of the four
CCCCS CTD Data Reports.
all four reports.
The other sections are essentially identical for
III
ABSTRACT
CTD observations were made over the continental shelf and upper
continental slope from the coast to approximately 60 km off central California
between latitudes 34°N and 37.5°N.
The measurements were made by Raytheon
Service Company as part of the Central California Coastal Circulation Study
sponsored by the Minerals Management Service.
The objectives of this 18-month
field program were to obtain a set of observations of the ocean water mass and
velocity fields and develop a detailed description of these fields and their
seasonal and shorter period variations.
The ultimate goal is to assess the
impact of exploitation of offshore oil and gas resources of the outer
continental shelf region.
This data report contains vertical profiles,
horizontal maps at selected depths, and vertical sections of temperature,
salinity,
dynamic height and relative geostrophic velocity from a total of
123 CTD casts made between 7 October 1984 and 19 October 1984.
INTRODUCTION
The Central California Coastal Circulation Study (CCCCS) was an 18-month
field program designed to study the variability of water mass characteristics
and velocity field on the continental shelf and upper continental slope from
Point Conception to San Francisco.
This study was funded by the U.S.
Department of Interior, Minerals Management Service (MMS) as part of an overall
assessment of the impact of development of oil and gas resources on the
ecosystem of the California Current System.
The region from Point Conception
to Point Buchon (100 km to the north), extending 50 km offshore, is of
particular interest as this will be the focus of oil and gas exploration and
production in the immediate future.
However, MMS
is
also interested in how
this region relates to the large scale flow of the California Current System.
Historically, repeated surveys of the California Current System have been
conducted since 1949 by the California Cooperative Oceanic Fisheries
Investigations (Ca1COFI).
The primary purpose of these surveys is to gain an
understanding of the ecological factors controlling the fisheries in this
region and develop a useful fisheries management strategy.
The area sampled
most intensely by Ca1COFI ranges from San Francisco in the north to southern
Baja California and extends offshore a distance of approximately 500 km.
Hydrographic measurements have been made on a geographically fixed grid with
65 km spacing in both the alongshore and cross-shore directions (somewhat
tighter cross-shore spacing nearshore).
The 35-year Ca1COFI data set has been very useful for studies of the
seasonal (Reid, Roden and Wyllie, 1958; Lynn, 1967; Hickey, 1979; Chelton,
1984) and interannual (Chelton, Bernal and McGowan, 1982) variability of water
mass characteristics and the flow field in this region.
However, the
relatively coarse 65 km grid spacing has restricted these studies to rather
large spatial scales of variability.
Finer spatial resolution is necessary to
study the fate of pollutants associated with oil and gas development on the
outer continental shelf.
The purpose of CCCCS was to collect a set of
measurements capable of resolving finer spatial scales and shorter temporal
scales than can be studied from the Ca1COFI data.
2
The field work for CCCCS was conducted from February 1984 through July
1985 by Raytheon Service Company.
Measurements collected during this 18-month
field study can be categorized as:
(a)
Measurements and data collected over the entire 18-month period.
Measurements of this type included:
(1) Moored current meter data and bottom pressure gauge measurements
(30 minute interval).
(2) Meteorological data (hourly interval).
(3) Sea-level
gauge) observations (hourly interval).
(4) Infrared satellite imagery (including all sufficiently clear images).
(b)
Measurements and observations related to the episodic sampling of summer,
fall and winter seasons (with two winter samplings).
Measurements of this
type included:
(1) Hydrographic measurements (20 km CTD spacing with XBTs in between).
(2) Lagrangian surface current drifter studies.
The continuous measurements extended from February 1984 through July 1985.
The episodic operations took place in February, July and October 1984 and
January 1985.
A preliminary analysis of the entire CCCCS data set is presented
in Chelton, Bernstein, Bratkovich and Kosro (1987).
This data report deals
only with the CTD hydrographic component of the study for Raytheon cruise 8404
carried out from 7 October 1984 to 19 October 1984.
The CCCCS CTD sampling grid was designed to have approximately 20 km
cross-shore station spacing along each of six standard Ca1COFI lines between
Point Conception and San Francisco (Ca1COFI lines 63, 67, 70, 73, 77 and 80).
These parallel lines (Fig. 1) are oriented approximately perpendicular to the
central California coastline.
The CCCCS sampling grid extends offshore from
the coast to the standard Ca1COFI stations 60 along each line (a distance of
approximately 60 km).
This coupling to the Ca1COFI grid was motivated by the
desire to relate the CCCCS measurements to historical data at the same
locations.
As discussed previously, the standard Ca1COFI lines are separated by 65 km
in the alongshore direction.
The southern portion of the CCCCS sampling region
was sampled more closely in the alongshore direction.
The line spacing was
approximately 10 km from Point Conception at 34.4°N to Point Buchon at 35.25°N.
For the first three surveys (February, July and October 1984),
this so-called
3
CaICOFI Grid and COCOS Sampling Region
38°N
36°
340
127°W
125°
123°
121°
The standard Ca1COFI grid pattern off the central California coast.
The numbers at the offshore locations refer to the Ca1COFI line numbers.
The numbers at the southern locations refer to Ca1COFI station numbers
along each line. The full CCCCS sample region and the CCCCS snapshot
sample region are indicated by the boxed areas.
Fig. 1.
Time, date and Raytheon CTD station number for selected milestones
Table 1.
during the October 1984 CCCCS cruise.
Milestone
CTD station no.
date
time (PDT)
start of snapshot 1
1145
Oct.
7,
1984
101
end of snapshot 1
1702
Oct.
10,
1984
211
start of snapshot 2
0343
Oct.
11,
1984
401
end of snapshot 2
1000
Oct.
14,
1984
503
Oct.
15,
1984
Oct.
16,
1984
Oct.
17,
1984
anchor at San Simeon
due to poor weather conditions (20-30 kt winds and
14-18 ft seas)
restart CTD operations
0815
return to San Simeon
due to poor weather
600
restart CTD operations
0700
Oct.
18,
1984
614
last CTD station
2359
Oct.
19,
1984
648
5
37
36
35
34
123
Fig.
122
121
120
Map of the CCCCS study region overlayed on depth contours in meters.
The dots indicate the locations of CCCCS CTD stations.
Current meter
moorings are shown by squares and NDBC wind buoys are shown by
Current meter moorings and NDBC buoys are identified by letters and
numbers, respectively.
6
"snapshot region8' was sampled twice over an eight day period to investigate how
rapidly the water mass and flow field characteristics change in this region.
Each CTD station in snapshot 1 was resampled approximately four days later in
For the January 1985 survey, the snapshot region was sampled only
snapshot 2.
once.
Some of the important milestones of the October 1984 survey are listed in
Table 1.
The relationship between the CCCCS full and snapshot sampling regions and
the Ca1COFI sampling grid is shown in Fig. 1.
stations are shown in Fig. 2.
The locations of the CCCCS CTD
Locations of the CCCCS current meter moorings
and NDBC wind buoys are shown in the figure as squares and triangles,
respectively.
For reference, the 100, 200, 500 and 1000 m isobaths for the
CCCCS survey region are also shown.
OVERVIEW OF OCTOBER 1984 OCEANOGRAPHIC AND METEOROLOGICAL CONDITIONS
The seasonal average winds are equatorward throughout the year over the
CCCCS sampling region.
These equatorward winds are weakest during January and
begin to increase in February.
and June.
The strongest equatorward winds occur in May
The average October wind stress is shown in Fig. 3.
The cross-shore
and alongshore coherences of this large-scale wind field are large.
Superimposed on this relatively simple seasonal cycle of wind stress are strong
fluctuating poleward and equatorward wind events associated with 2-10 day time
scale weather patterns.
The frequency and intensity of these short time scale
wind events vary from year to year.
Time series of the alongshore component of vector winds and wind stress
measured at NDBC buoy 46028 (Fig. 2) during September and October of 1984 are
shown in Fig. 4.
The winds were equatorward throughout the two month period.
There were two strong equatorward wind events in early September, followed by
four moderate wind events separated by 5 to 9 day intervals.
On 15 October,
about 2/3 of the way through the October 1984 CCCCS CTD survey, there was an
isolated very strong wind event.
This was followed by moderate to light winds
for the last two weeks of October.
Maps of vector winds measured by a hand-held anemometer on board the ship
at most of the October 1984 CCCCS CTD stations during snapshots 1 and 2 are shown
in Fig. 5.
Consistent with the time series of winds measured at NDBC buoy
46028, winds were equatorward throughout the survey.
Both surveys of the
7
Fig.
Map of average seasonal wind stress for the month of October over the
California Current region. These wind stresses were calculated at 6-hour
intervals front quasi geostrophic vector winds determined from sea level
pressure fields generated by Fleet Numerical Oceanography Center. The
6-hourly data were then averaged to obtain monthly averages. The seasonal
average was determined from the monthly averages at each grid point by a
least squares fit to an annual plus a semiannual harmonic over the period
1946-1976.
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Time series of the alongshore component (defined to
vector wind and wind stress from measured winds at NDBC
Fig. 2) for the period September through October 1984.
indicate equatorward winds.
Times are Pacific Daylight
marks correspond to hour 0000 of the day indicated.
Fig. 4.
be 325T) of
buoy 46028 (see
Negative values
Time (PDT) and tic
9
SNAPSHOT
1
0
350 N
0
/OOct
,,'\
9Oct
V
8Oct
Ocaim
—+
20 knots
7Cc/i
340
1210301
I20°30'
l21°W
,
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,
,0
,
,
/5 Oct
—
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,'
,
/4
Oct /
/
/3
Oct
/
/2 Oct
0
0
0 calm
20 knots
12l°30'
Fig.
// Oct
121°W
+
1200 3Q1
Maps of vector winds measured by a hand-held anemometer at CTD
stations during snapshots 1 and 2 of the October 1984 CCCCS cruise, Dashed
Scale is shown at the
lines define day boundaries during the CTD survey.
lover left corner of the maps.
5.
10
snapshot region were completed just prior to the strong wind event on 15
October.
Typical wind speeds observed during both snapshots were 10-15 knots.
Seasonal variations in the flow field off the central California coast
have been described by Reid, Roden and Wyllie (1958), Hickey (1979) and Chelton
(1984).
In the offshore region ( 100 km from the coast), the seasonal
average geostrophic surface flow of the California Current is southward year
round with the strongest flow from May through July and weakest flow in
January-February.
Except for March in the seasonal cycle, there is a region of
nearshore counterflow present throughout the year just south of Point
Conception between the Channel Islands and the coast.
This seasonal average
nearshore counterflow extends north of Point Conception beginning in
September-October and is present everywhere north of 30° latitude from
October through February.
The poleward nearshore surface counterflow north of
Point Conception is known as the Davidson Current.
The October seasonal average
dynamic height of the surface relative to 500 m is shown in Fig. 6 for the
central California Current region.
The surface flow is weak and poleward
across the inshore 100 km along the entire central California coast.
farther offshore is weak and equatorward.
The flow
There is an indication of relatively
strong equatorward flow in the southwest corner of the region, suggesting the
possibility that a "core" of the California Current may exist farther offshore
during the fall.
The seasonal average deep flow of the California Current system (below
150 m) is weak and southwards in the offshore region.
There is a nearshore
northward flow present in the seasonal cycle throughout the year north of 30°
latitude.
This undercurrent is strongest in December and weakest in April and
flows against the seasonal average surface current from March through August.
The October seasonal average dynamic height of the 200 m surface relative to 500 m
is shown in Fig 6 for the central California Current region.
The flow at 200 m
has essentially the same structure as the surface flow, though the equatorward
flow in the region offshore is considerably weaker at 200 m.
October seasonal average 10 m temperature and salinity in the central
California Current region are also shown in Fig. 6.
The seasonal temperature
pattern for October is characterized by relatively strong cross-shore gradients
across most of the region.
north of about 35.5°N.
The strongest gradients are close to the coast
This temperature pattern is suggestive of moderate
11
Seasonal average October temperature and salinity at 1.0 in depth and
dynamic heights of the sea surface and the 200 in surface relative to 500 in
Ca1COFI grid points used are
for the central California Current region.
indicated on the plot. The seasonal average was determined at each grid
point by a least squares fit to an annual plus a semiannual harmonic over
the period 1950-1978.
Fig. 6.
12
coastal
upwelling.
The isotherms in the offshore regions generally parallel
the geostrophic surface flow inferred from the surface dynamic topography.
There is no evidence for nearshore poleward flow in the 10 m temperature.
In
contrast, the seasonal average 10 m salinity is suggestive of poleward flow
nearshore.
There is a broad band of relatively high salinity water
across the inshore 100-150 km extending as far north as San Francisco.
These seasonal patterns of the flow field, temperature and salinity smooth
out the patterns observed during any particular cruise.
There was a Ca1COFI
hydrographic survey at approximately the same time as the October 1984 CCCCS
survey.
These data can be used to determine the large scale patterns of
temperature, salinity and dynamic height at the time of the CCCCS survey.
The
Ca1COFI cruise sampled the central portion of the California Current system
beginning 10 October, three days after the start, and ending 23 October, four
days after completion of the October 1984 CCCCS survey.
The ordering of the
Ca1COFI station sampling was somewhat irregular due to the fact that two ships
were used in the survey.
Ca1COFI lines 77 and 80 (see Fig. 1) were sampled
between 10 and 13 October by the R/V New Horizon.
The Ca1COFI lines farther
north were sampled between 16 and 23 October by the R/V David Star Jordan.
The October 1984 0/500 m and 200/500 m dynamic heights determined from the
Ca1COFI data are shown in Fig. 7.
As noted above, October normally marks the
transition period between summertime nearshore equatorward flow and the
poleward Davidson Current counterflow (Fig. 6).
were relatively normal.
Conditions during October 1984
Flow in the offshore region (beyond about 150 km from
the coast) was equatorward with a strong onshore component (meander) at about
34.5°N.
The nearshore flow was poleward from Point Conception to as far north
as about 35°N and essentially zero farther north.
It thus appears that the
Davidson Current was indeed in the process of formation, but had not yet fully
established itself along the entire central California coast.
The pattern of flow at 200 m in the offshore region was essentially the
same as the surface flow, though the equatorward flow was weaker.
Across the
inshore 150-200 km, there was no clear pattern in the flow at 200 in.
There was
evidence for an eddy-like feature just north of Point Conception at 200 m
depth.
Interestingly, there was little indication of this feature in the
surface dynamic topography.
13
dynamic heights of
Fig. 7. Maps of temperature and salinity at 10 w depth and
the sea surface and the 200 in surface relative to 500 in determined from
Ca1COFI measurements over this central
the October 1984 Ca1COFI data.
California Current region were made between 10 and 23 October.
The temperature and salinity at 10 m depth from the October 1984 Ca1COFI
data are also shown in Fig. 7.
The temperature field was generally very
similar to the seasonal average October pattern, though with more meandering of
the isotherms.
The very nearshore waters (within about 40 km of the coast)
were about 0.5 to 1°C colder than normal along Ca1COFI lines 60 through 73 (see
Fig. 1 for Ca1COFI line numbering convention).
These lines were all sampled
after the very strong equatorward wind event on 15 October (Fig. 4).
and 80 were sampled before this wind event.
Lines 77
Thus, the cold nearshore
temperatures along the northern lines are likely remnants of intense coastal
associated with the strong wind event.
The salinity at 10 m was also approximately normal, though with a very
broad, weakly defined "tongue" of slightly high salinity water extending
offshore about 250 km between San Francisco and Monterey Bay.
There was a
return onshore "tongue" just to the south, between Point Sur and Point Buchon.
These salinity features are consistent with advection by the surface flow,
as
inferred from surface dynamic topography.
Finally, for reference we show in Fig
*
8 an infrared satellite image taken
on 12 October 1984, in the middle of the CCCCS survey.
This image is generally
consistent with the 10 m temperature map constructed from the Ca1COFI data
(Fig. 7), though the satellite image resolves considerably more structure in
the temperature field.
October (Fig. 4).
This image was taken before the strong wind event on 15
Nonetheless, there is evidence very near the coast for cold
water associated with the moderate upwelling prior to 15 October.
There are
several relatively narrow cold water tongues extending offshore from the coast,
most notably off Point Sur and Point Conception.
SAXPLING PROCEDURES
A Neil
Brown Instrusient Systems (NBIS) Mark III conductivity, temperature,
depth (CTD) probe was used to obtain vertical profiles of temperature and
salinity at a total of 123 stations during October 1984.
The CTD was lowered
through the water column at a rate of approximately 70-80 m per minute.
During the previous two CCCCS hydrographic surveys (February and July 1984),
measurements of conductivity, temperature and pressure were digitally recorded
at a sample interval of 31.25 msec.
During the October 1984 and January 1985
surveys, Raytheon personnel made a decision to increase the sample interval to
16
250 msec.
Measurements were made from the sea surface to within 3 m of the
bottom or until the cast reached 800 m of cable length.
The sample depth at
maximum cable outlay varied with current and surface wind conditions.
The
effects of the increased sample interval (reduced sampling rate) are examined
in this and the following section of this report.
The conductivity of seawater is a function of both temperature and
salinity.
The temperature effects are much greater than the salinity effects
and therefore must be removed in order to determine salinity from measurements
of conductivity.
However, the response time of the thermistor is much longer
than that of the conductivity probe.
This difference in response time must be
accounted for when using thermistor measurements of temperature to remove the
temperature component of conductivity variations.
The method used here "speeds
up" the effective response time of the thermistor so that it matches the
essentially instantaneous response of the conductivity probe.
The differential equation relating the measured temperature T to the
true temperature T is
A
— T,
T + ?
where r is the time constant of the thermistor and the independent variable t
represents time as the CTD falls through the water column.
this
adequately small sample interval
Assuming an
expression can be solved for the true
temperature at time t by first differencing to obtain
T(t) =
T(t)
+
[T(t)
-
For the February and July 1984 CCCCS CTD surveys where the sample
interval
was 31.25 msec, it was determined that the time constant r for the
thermistor on this particular CTD was 68 msec (see Chelton and Kosro, 1987a;
1987b).
The 250 msec sample interval used during the October 1984 survey thus
considerably undersamples the response time of the themistor.
In regions of
rapid temperature change with depth (e.g., at the base of the mixed layer),
this undersampling makes it impossible to make accurate corrections to the
measured temperature using the equation above.
The high-frequency temperature
variations are aliased by the infrequent sampling.
The reduced sampling rate
thus raises the question of whether the 68 msec thermistor time constant
17
deduced previously from the 31.25 msec February and July 1984 data is still the
correct value for the 250 msec October 1984 data.
The time constant r for the thermistor on the CTD probe was determined,
as in the two previous CTD surveys, from the phase spectrum between measured
temperature and conductivity (see Millard, Toole and Swartz, 1980).
The upper
2048 samples (corresponding to a depth interval of about 600 m) of the CTD
profile at Raytheon station 414 was used to calculate the auto and cross
spectra of measured temperature and conductivity.
The data were band averaged
to obtain 16 degrees of freedom for calculation of coherence and phase.
coherence and phase plots are shown in Fig. 9.
the slope of the phase spectrum.
The
The time constant r is equal to
The spread of phase values for this CTD
station is consistent with the value of 0.068 sec determined previously from
the February and July 1984 CCCCS CTD data (Chelton and Kosro, l987a; 1987b),
shown by the solid line in the figure.
It thus appears that reducing the sampling rate does not have a large
effect on the apparent time constant of the thermistor.
That a response time
of 68 msec can be determined at all from coarse 250 msec data is due to the
fact that the spectrum of temperature with depth is fundamentally "red"; spikes
and steps in temperature profiles are generally much less energetic than the
underlying slow variation of temperature with depth.
It should be noted that
the fact that the apparent time constant is unchanged by undersampling the
response time of the thermistor does not indicate that no information is lost
by reducing the sampling rate.
Indeed, in regions where temperature changes
rapidly with depth (e.g., the base of the mixed layer), the temperature
measured by the thermistor cannot be accurately corrected from the 250 msec
samples.
This is clearly apparent from the expression above for the corrected
temperature.
Since temperature cannot be corrected in such cases, the
temperature effects on conductivity also cannot be removed accurately.
Consequently, we can expect errors in computed salinity in regions of rapid
temperature change with depth.
The magnitude of these errors is examined in
the next section.
CALIBRATION
The CTD was calibrated by the manufacturer for conductivity, temperature
and pressure on 15 August 1984 and again on 25 September 1984, two weeks prior
18
0.35
8404/414
0.30
0.25
S
0.20 U.
5
-
0.10 -
S
5
S
U
0.05 -
U
0.00 -
U
S
I
0.0
1.0
I
I
2.0
I
I
3.0
I
I
4.0
w (sec1)
(sec1)
Fig.
Squared coherence and phase plots for temperature vs. conductivity at
individual points at each
October 1984 Raytheon CTD station 414.
frequency correspond to different subrecords of 2048 samples from CTD
cast 414.
The spectral estimates for each subrecord were based on 16
degrees of freedom. The straight line for the phase plot corresponds to a
line with a slope of 0.068.
9.
19
to the October 1984 CCCCS survey.
Historically, the electronics of this
particular CTD have had very little problem with drifts in calibration.
During
eight hydrographic cruises over a two year period in an experiment on Georges
Bank, no calibration drifts were detected in five calibrations by NBIS spread
over the two years.
As in the previous two CCCCS CTD surveys, the number of in situ bottle
samples collected during the October 1984 survey was too small to provide
adequate salinity calibration.
A Niskin bottle was mounted 2 m above the CTD
probe on six casts during the October 1984 CCCCS cruise.
Four of the Niskin
bottles were tripped at the maximum depth of the CTD casts where variations in
salinity with depth and over time are generally small.
These in situ water
samples were processed by D. Hammond at the University of Southern California.
The accuracy of salinity determined from these bottle samples is estimated to
be
The results of these in situ salinity comparisons are summarized
in Table 2.
After applying the corrections determined from the 25 September
1984 pre-cruise calibration by NBIS, the, average difference between CTD and
bottle salinities was
with a standard deviation of
(see
Table 2).
As an independent test of these salinity calibrations, the corrected
Raytheon CTD salinities were compared with nearly coincident bottle salinities
collected by Ca1COFI.
An example T-S plot comparison of CCCCS and Ca1COFI data
separated in time by 4-5 days is shown in Fig. 10.
The differences between the
ranging from about 24.25 to 25.5) are
two salinities in the therniocline
probably due to a combination of the difference in sample times and the complex
spatial structure of the intrusive salinity features found throughout the
October 1984 survey (see further discussion below).
In the deeper water where
temporal changes in salinity are generally small, there is no obvious evidence
in this example for any significant systematic differences.
In all, there were
28 CCCCS and Ca1COFI station pairs separated spatially by less than 3 km and
temporally' by less than 2 weeks.
For each station pair, Raytheon temperature
and salinity were interpolated to the density found at the Ca1COFI bottle
sample.
The Raytheon and Ca1COFI salinities were compared for samples that
were either within the mixed layer
deeper than the main thermocline
within .5 of the surface value) or
greater than 26.5).
The overall average
20
Comparison between CTD salinities and in situ bottle
Table 2.
The salinity
salinities for the October 1984 CCCCS survey.
difference values refer to CTD minus bottle salinities.
CTD
Sta. No.
Bottle Depth
Bottle Sal.
CTD Sal.
(in)
CTD Depth
Sal Difference
(m)
(0/00)
130
712
34.317
34.334
712
0.017
145
12
33.460
33.456
12
-0.004
211
488
34.162
34.145
488
-0.017
409
683
34.281
34.311
683
0.030
446
64
33.305
33.318
64
0.013
627
742
34.369
34.366
742
-0.003
21
20
16
12
8
4
32
33
SALINITY
Fig. 10.
34
35
(ppt)
Temperature-Salinity plots for nearly coincident Raytheon and Ca1COFI
Solid line corresponds to Raytheon CTD data at
hvdrographic measurements.
station ill (7 October 1984). and symbols (triangles, circles, diamonds
and pluses) correspond to four separate Ca1COFI bottle casts at station 60
on line 80 (11 and 12 October 1984).
22
with a standard
difference between CCCCS and Ca1COFI salinities was
deviation of
The relatively large standard deviations of the differences between CTD
and bottle salinities in both the simultaneous Raytheon and the
nearly-coincident Ca1COFI bottle measurements are rather disturbing.
Further
analysis was conducted in an attempt to determine whether these large standard
deviations could be due to the 250 msec sample interval.
Inspection of the
temperature and salinity profiles presented later in this report for the
October 1984 CCCCS CTD measurements reveals that many of the CTD casts show
large salinity spikes at the base of the mixed layer.
The coincidence of these
features with rapid temperature variations at the base of the mixed layer is
alarming in view of the above discussion of possible salinity errors that could
be introduced by undersampling the temperature variability.
There were few
examples of similar salinity features in either of the two preceding CCCCS CTD
surveys (see Chelton and Kosro, 1987a; 1987b).
It is important to determine
whether the apparent salinity intrusions in the October 1984 data are a
manifestation of undersampling.
From the profiles and vertical sections of October 1984 salinity, it is
apparent that these intrusions generally have vertical dimensions of tens of
meters (larger than the vertical dimensions of the regions of most rapid
temperature changes with depth), and horizontal scales that span several CTD
stations.
The salinity intrusions are also relatively persistent, as can be
seen from Fig. lla which shows two CCCCS salinity profiles at the same location
separated in time by 3.5 days.
These characteristics all suggest that the
apparent salinity intrusions are likely real.
evidence that the intrusions are real.
Fig. lib presents additional
Ca1COFI bottle samples on the same day
and within 3 km of a CCCCS CTD cast both show a large salinity intrusion
centered at about 75 m depth (though this feature is not as well resolved by
the discrete Ca1COFI bottle samples).
Furthermore, examination of September
1982 CTD profiles off central California collected by J. Huyer of Oregon State
University showed very similar salinity intrusions (see Fleischbein, Schramm,
Huyer and Smith, 1983).
This suggests that these features in the salinity
field may be a common phenomenon occurring during the fall in this nearshore
region along the central California coast.
A final piece of evidence that the
salinity intrusions in the October 1984 CCCCS data are real is that there is no
23
SALINITY
33.0
0
33.6
34.2
34.8
33.0
0
34.2
34.8
—Sta,4I1
Sta. 145
100
33.6
Sta.445 —
100
200
200
300
300
400
400
500
500
•CaICOFI
Sta. 80.60
FuJ
0
Fig.
11.
Examples of large salinity spikes at the base of the mixed layer
during October 1984. Left: two CCCCS CTD salinity profiles at the same
location separated in time by 3.5 days (Raytheon stations 145 and 445).
Right: CCCCS CTD (Raytheon station 411, continuous line) and CaICOFI
bottle samples (Ca1COFI station 80.60, dots) of salinity at the same
location (within 3 kin) separated in time by less than a day.
indication of any intrusive features in the January 1985 CCCCS CTD data where
the sample interval was also 250 msec (see Chelton and Kosro, l987c).
From the above discussion, the salinity intrusions in the October 1984
CCCCS CTD data are apparently real and not the result of undersampling the
temperature signal with the reduced sampling rate. Still, it is useful to
examine the effects of the 250 msec sample interval in greater detail to
determine whether such intrusions could perhaps be somehow exaggerated by the
reduced sampling rate. It is also useful to try to quantify the magnitude of
error expected from the undersampling.
A search of the July 1984 CCCCS CTD data where the sample interval was 31.25
msec found several casts with a salinity spike at the base of a well-defined
mixed layer.
An example (Raytheon station 118) is shown in Fig. 12.
An
expanded view of the salinity spike is shown by the continuous line in Fig. 13.
This salinity intrusion was about 0.5 m thick with an amplitude of about
To simulate the reduced sampling rate of the October 1984 CCCCS CTD
survey, the raw 31.25 msec conductivity and temperature data from this July 1984
CTD cast were subsampled at 250 msec intervals.
The subsampled conductivity
and temperature were then processed to obtain salinity as described in the next
section. The resulting salinity determined from the subsampled data is shown
by the dotted line in Fig. 13.
The salinity intrusion is neither widened in
depth nor increased in amplitude when the data are subsampled.
Though the shape and amplitude of the salinity intrusions found during the
July 1984 survey were not changed significantly by the subsampling, it is
apparent from Fig. 13 that the reduced sampling rate does introduce random
An attempt was made
differences in salinity with amplitudes of order
to quantify the magnitude of these errors. Four CTD casts from the July 1984
CCCCS CTD survey were processed to obtain salinity from both the original 31.25
intervals. These
four casts were selected on the basis of very well-defined mixed layers with
rapid temperature changes with depth at the base of the mixed layer in order to
msec measurements and subsampled measurements at 250 msec
maximize errors introduced by undersampling the response time of the
thermistor. The 31.25 msec data were linearly interpolated to the depths of the
250 msec data and the salinities were compared.
An example plot of the
differences between salinities computed from 31.25 msec and 250 msec measurements
is shown in Fig. 12 for July 1984 Raytheon station 118.
This example was
25
0
9
II
13
SALINITY
SALINITY
TEMPERATURE (°C)
15
33.6
33.8
DIFFERENCE
34.0
-.04
0
20
E
40
I
I-
0
60
60
80
80
100
100
Fig.
Temperature and salinity profiles from an example CCCCS CTD cast
taken in July 1984 (Raytheon station 118).
These profiles were deduced
using a 31.25 asec sample interval.
Also shown is a profile of differences
between sa].inities computed from conductivity and temperature sampled at
31.25 msec and subsampled at 250 msec intervals. The subsampling of the raw
31.25 msec data simulates errors introduced by the reduced sampling rate
during the October 1984 CCCCS CTD survey.
12.
0
.02
26
SALINITY
20
L
I
I
33.68
33.64
33.60
33.56
I
I
I—
3
1984
CCCCS Station 118
S
.
S
21
S
S
I
22
F-
w
23-
24.
S
S
25
.
I
I
I
I
Expanded view of the salinity spike at the base of the mixed layer in
the July 1984 CCCCS CTD station shown in Fig. 12 (Raytheon station 118).
The solid and dashed lines correspond to salinities determined from
conductivity and temperature sampled at 31.25 macc and 250 msec intervals,
respectively.
Fig. 13.
27
typical of the four casts examined.
than
Salinity differences were generally less
and evenly distributed between positive and negative.
Overall,
the standard deviation of these salinity errors introduced by the reduced
However, it is apparent from
sampling rate was small (about
Fig. 12 that the amplitude of the salinity errors can be considerably larger in
regions of rapid temperature change with depth.
In summary, it appears from the above analysis that the reduced sampling
rate for the October 1984 CTD measurements did not seriously affect the
salinity calibration in an average sense; the Raytheon salinities generally
appear to be accurate to somewhat better than
However, in regions of
rapid temperature changes with depth, errors of
and larger can be
expected.
These errors are an unavoidable result of undersaxnpling the response
time of the thermistor on the CTD and cannot be corrected from the 250 msec
measurements.
DATA PROCESSING
As with the February and July 1984 CTD data, after converting binary field
data to engineering units, the first step in the data processing was to search
the 250 msec digitized temperature and conductivity data for gross spikes.
If
a value of conductivity or temperature differed from the previous value (250
msec earlier) by more than 2 mmhos or 2°C, the sample value was eliminated.
The temperature profiles were then corrected for the slower response time of
the thermistor relative to the conductivity probe using a time constant of
0.068 see, as discussed previously.
The values of pressure were then examined
to eliminate ascending data caused by boat roll from wave action.
remaining data were then tested for gross spikes in pressure.
The
Samples where
the value of pressure differed from the previous value by more than 10 db were
eliminated.
The de-spiked conductivity, temperature and pressure data were subsampled
to eliminate measurements separated by less than 0.1 db for the upper 100 db of
each cast and 0.2 db for the deeper portion of each cast.
Corrections were
applied to conductivity and temperature as per calibration by the CTD
manufacturer (NBIS), as discussed in the previous section.
Temperature and
conductivity were then tested for smaller single point spikes by comparison of
each sample value with the value predicted by linear extrapolation from the
28
previous two sample values.
If the measured value differed from the predicted
value by more than 0.75°C or 0.75 mmhos, the sample observation was eliminated.
Finally, the vertical profiles of temperature and conductivity were smoothed
using a five point 1-4-6-4-1 weighted running average filter.
smoothed once and conductivity was smoothed twice.
Temperature was
These de-spiked, subsampled
and smoothed measurements of conductivity, temperature and pressure constitute
the processed data set used to compute salinity, depth,
specific volume
anomaly and dynamic height.
Since one of the objectives of CCCCS was to compare the CTD measurements
with historical Ca1COFI data, it is desirable to use the Ca1COFI algorithms to
compute the various parameters of interest to assure compatibility of the data.
However, Ca1COFI hydrographic data consist exclusively of Nansen bottle
measurements.
The Southwest Fisheries Center (SWFC), National Marine Fisheries
Service in La Jolla, California conducts regular CTD surveys on the Ca1COFI
grid.
The CTD data are included in the archived Ca1COFI data set.
The SWFC
algorithms (provided by R. Lynn) were therefore used to process the CCCCS CTD
data.
Salinities were calculated from conductivity, pressure and temperature at
the subsampled pressure levels using the algorithms for the Practical Salinity
Scale 1978 (Lewis and Perkins, 1981).
A standard reference conductivity of
C(35,15,0) — 42.9149 was used.
Pressure was converted to depth using the algorithm described by Saunders
Then the vertical profiles of salinity, temperature and
and Fofonoff (1976).
depth were subsampled at 2 m intervals from the surface to the bottom of the
cast.
Values were determined by linear interpolation between the nearest pair
of sample observations.
The temperature and salinity values at 2 m intervals were used to compute
the density parameter
and the specific volume anomaly 6 using the algorithms
described in LaFond (1957).
The specific volume anomalies were vertically
integrated to obtain the dynamic height of the sea surface relative to pressure
at each sample depth (or equivalently, the dynamic depth of each sample
pressure surface).
Historically, the pressure at 500 m is used as a reference
surface for estimating the dynamic topography of the sea surface in the
California Current.
However, a number of deep water CTD casts did not extend
29
all the way to 500 m.
reference level.
For these casts, it was not possible to use 500 in as a
The dynamic height at depth z relative to z
is computed by
p(z)
'o
f
Sdp
p(z
where p(z) and p(z) are the pressures at depths z and z0.
Examination of the
specific volume anomaly 6 in deep water found that it varied approximately
linearly with depth.
Thus, dynamic height should show a quadratic dependence
on the reference depth z
0
Using CTD data from stations that extended deeper than 500 in,
casts to a number of shallower depths between 400 and 470 in.
dynamic heights relative to the bottom 100 in
of
We
we simulated
fit the
reference levels in the
simulated shallow casts to a second order polynomial by least squares.
quadratic fit was then extrapolated to a reference level of 500 in.
The
The
resulting estimates of dynamic height relative to 500 in were then compared with
the actual values.
It was found that extrapolations from depths of 440 m or
deeper resulted in an average bias of less than 0.5 mm and an rms error of less
than 1 mm.
Extrapolations from depths of 400 in gave considerably larger errors
(a bias of 1.7 mm and an rms error of 2.8 mm).
This vertical extrapolation to
obtain dynamic heights relative to 500 m was therefore somewhat arbitrarily
applied only to CTD casts deeper than 440 m.
Although the 500 m reference level may give adequate representation of the
sea surface topography, some other method must be used to estimate the dynamic
topography of the sea surface over the upper continental slope and continental
shelf where the water is shallower than 500 in.
The method commonly used (e.g.,
Reid and Mantyla, 1976; Huyer, 1980) is to extrapolate isopycnals horizontally
from deep water onto the shelf using the method first suggested by Montgomery
(1941).
The extrapolation of a deep isopycnal into shallow water is based on
the last observed cross-shore slope of the isopycnal in the deeper water
offshore.
This method of horizontal extrapolation was applied to the CTD data here
to stations in water shallower than 500 m to construct horizontal maps of
dynamic height and vertical sections of geostrophic velocity relative to
500 in.
The same extrapolation technique was applied to CTD data in water shallower
than 200 in
to
construct horizontal maps of dynamic height relative to 200 m.
30
We note, however, that the accuracies of the extrapolations for either the
500 m or 200 in
reference
This
level have not yet been thoroughly demonstrated.
is particularly true for geostrophic velocity.
Small errors in horizontally
extrapolated dynamic height can lead to very large errors in geostrophic
velocity (particularly for the close 20 km station spacing used in this study).
The bathymetry maps presented in the data report should allow the reader to
judge the regions of dynamic height maps that are questionable due to possible
errors introduced by horizontal extrapolation.
In the vertical section plots
of relative geostrophic velocity, the bottom profile can be used to identify
questionable areas.
After the figures in the February and July 1984 CCCCS CTD data reports
(Chelton and Kosro, l987a; l987b) were generated, two errors were found in the
computer software used to compute the specific volume anomaly and dynamic
depths at all CTD stations.
supplied by R. Lynn at SWFC.
These errors existed in the original software
The first error was the use of surface pressure
rather than in situ pressure for computing specific volume anomaly at all CTD
sample depths.
This systematically underestimated the actual specific volume
anomaly, which resulted in an underestimate of the dynamic depth computed by
vertically integrating specific volume anomaly.
The second error was the use
of geometric depth as the variable of integration rather than pressure.
pressure in decibars is slightly larger than the depth in meters.
a pressure of 500 db corresponds to a depth of 496.7 in
California coast.
off
The
For example,
the central
This second error also resulted in an underestimate of
dynamic depths.
Thus, the net effects of these two computational errors was to
underestimate the dynamic depths at all sample depths.
Fortunately, these
errors are very nearly consistent from station to station so that the errors
consist essentially of a depth-dependent constant bias.
Thus, horizontal
gradients of dynamic depths (used to infer relative geostrophic velocities) are
very nearly the same as for correctly computed dynamic depths.
Consequently,
to maintain consistency between the four CCCCS CTD data reports, the specific
volume anomaly and dynamic depths for the October 1984 data were computed using
exactly the same computer software as in the February and July 1984 data
reports.
31
Table 3 gives a summary of the relation between true dynamic heights and
the underestimated dynamic heights determined from all 123 CTD stations in the
October 1984 CCCCS survey.
The table entries include all of the relative dynamic
heights presented in this report.
The worst case (0/500 m dynamic height)
consists of a bias (correct minus incorrect value) of 2.7 dyn cm with an rms
deviation of 0.09 dyn cm about this bias.
Thus, the erroneous dynamic heights
presented in this report can be corrected by simply adding the biases listed in
Table 3, and the corrected dynamic heights will be accurate to within an rms
error of no worse than 0.09 dyn cm.
DATA PRESENTATION
The hydrographic data are summarized in data listings, vertical profiles,
T-S plots, maps and vertical sections.
All contouring in the vertical sections
and maps was done objectively using an automatic contouring routine based on
Laplacian interpolation.
smoothed in any way.
The contour plots included in this report were not
We give here a few brief comments on each of the data
products contained in this report.
1,
Locations, times and deDths of CTD stations.
The Raytheon station number,
date and time, latitude, longitude, maximum sample depth and water depth
is listed for each CTD cast in the CCCCS survey.
casts are local Pacific Daylight Time (PDT).
Times for October 1984 CTD
Note that the Raytheon
station numbering convention was different for each of the four CCCCS CTD
surveys.
2.
Mars of CTD station locations and bathymetry.
Maps are presented showing
the geographical locations of each CTD station in the CCCCS full,
snapshot 1 and snapshot 2 sample regions.
The CTD stations are located at
the lower left corner of each station number label.
The line numbers
define the convention adopted here for plotting vertical sections of
temperature, salinity,
and relative geostrophic velocity.
In the
southern portion of the full CCCCS sample grid, only the CTD stations
along the two long lines of snapshot 2 (lines 13 and 20) are included in
the maps of the full CCCCS region.
This was done to avoid contour mapping
biases introduced by nonhomogeneous sampling of the northern vs. southern
portions of the full survey region.
32
Statistics for comparison between true dynamic heights and the
incorrect dynamic heights for the October 1984 CCCCS data
presented in this report.
Column entries are: the relative
dynamic height reference surfaces; number of samples at these
references surfaces; average bias (correct minus incorrect
relative dynamic heights); standard deviation (rms error about
average bias); minimum error; maximum error; and range of
Table 3.
errors.
Reference
Surfaces
Number
samples
bias
Stnd.Dev.
(dyn cm)
(dyn cm)
Range error
Min.error
Max.error
(dyn cm)
(dyn cm)
(dyn cm)
0/100
87
0.3333
0.0217
0.2686
0.3842
0.1156
0/200
85
0.7703
0.0326
0.6724
0.8331
0.1607
50/200
85
0.6155
0.0251
0.5497
0.6686
0.1190
100/200
85
0.4364
0.0181
0.3916
0.4708
0.0792
0/500
55
2.6699
0.0888
2.4956
2.8451
0.3495
50/500
55
2.5117
0.0842
2.3359
2.6880
0.3521
100/500
55
2.3314
0.0798
2.1535
2.5201
0.3665
200/500
55
1.8963
0.0674
1.7432
2.0726
0.3294
33
Bathymetry maps for the full and snapshot CCCCS sample region are
Isobaths corresponding to 100 m, 200 in, 500 m and 1000 in
also presented.
bottom depth are shown.
These maps have been produced the same size as
the data maps presented later in the report and are thus useful for
identifying the nearshore CTD stations for which dynamic heights relative
to 200 m and 500 in have been extrapolated inshore as described in the
previous section.
3.
Data listings.
The header information for each listing contains the
Raytheon CTD station number, and latitude, longitude and water depth at
the station location.
Sample depth (in), water temperature (°C), salinity
and dynamic depth (DELD) relative to the sea surface (dyn in)
are listed at depth intervals of 10 in from the surface to 200 m, depth
intervals of 20 in from 200 to 300 in and depth intervals of 50 in for depths
greater than 300 in.
given.
Data values at the bottom sample depth are also
Note that these dynamic depths are systematically low by a
-
depth-dependent, approximately constant bias, as discussed in the previous
section (see Table 3).
Note also that the density parameter is
and not
the more conventional a0 (where 9 refers to potential temperature).
The
two differ by very little for the shallow water depths (less than 500 in)
considered here.
If the CTD cast was in water deeper than 500 m and the cast did not
extend to a depth of 500 in (but did extend deeper than 440 in), dynamic
depth of the 500 in surface was estimated by vertical extrapolation as
described in the previous section.
These vertically extrapolated dynamic
depths are given in the data listings.
Finally, dynamic depths of the
200 m and 500 in surfaces in nearshore stations in water shallower than 200
and 500 in were determined by horizontal extrapolation from the deeper
stations offshore as discussed in the previous section.
These
horizontally extrapolated dynamic depths are given in the data listings.
Temperature, salinity and
are not given at the depths of these
vertically and horizontally extrapolated dynamic depths.
4.
Vertical profiles of temperature, salinity and
Profiles are presented
for all 123 CTD casts during the October 1984 CCCCS cruise.
CTD profiles
from snapshot 1 and snapshot 2 at the same location are superimposed on
314
the same plot (dashed lines for snapshot 1 and continuous lines for
snapshot 2).
5.
The dots correspond to a potential
Potential Temterature-Salinitv plots.
temperature, salinity pair at 10 m intervals for all CTD casts.
plots are included for the full CCCCS
6.
region,
snapshot 1 and snapshot 2.
Included are maps of temperature, salinity and
Maps.
Separate
at
depths of 10 m, 50 m, 100 m, 200 m and 400 m; relative dynamic heights
of 0/100 m, 0/200 m, 50/200 m, 100/200 m, 0/500 m, 50/500 m, 100/500 m
and 200/500 m surfaces; depth, temperature and salinity on
surfaces of
25.0, 25.8 and 26.6 (corresponding roughly to depths at the bottom of the
mixed layer, in the therinocline and below the thermocline).
The relative
dynamic heights are systematically low due to an error in computation, as
discussed in the previous section.
If the biases in Table 3 are added,
the resulting plots are accurate to an rms error of no worse than
0.09 dyn cm.
conventional
surfaces are not the more
Note that the plots on
surfaces.
As mentioned previously, the differences are
very small for these water depths less than 500m.
Maps are grouped by
data type (i.e., all of the temperature maps together, all of the salinity
maps together, etc.).
As discussed in the previous section, dynamic
heights relative to 200 m and 500 m at nearshore stations in water
shallower than 200 m and 500 m were determined by horizontal extrapolation
from the deeper stations offshore.
The bathymetry maps summarized
previously can be used to determine the regions where the extrapolation
was used.
The maps for the full CCCCS region, snapshot 1 and snapshot 2 are
presented in separate sections of the report.
In the full area maps, all
of the lines north of the snapshot region are included but only the two
longest lines of snapshot 2 (lines 13 and 20) are included so as not to
"oversample" the southern portion of the map relative to the northern
portion.
This avoids mapping biases introduced by the nonhomogeneous
sampling of the northern vs. southern portions of the full CCCCS survey
region.
For all plots, the data values are written on the plot with the lower
left corner of the first character of the data label defining the station
location.
Contour intervals are 0.5°C,
0.1, 1 dyn cm and 10 m
35
for
maps of temperature, salinity,
surfaces, respectively.
dynamic height, and depth of
In maps where the dynamic range of the variable
plotted is small, intermediate contours are drawn as dashed lines.
7.
Difference mans.
Snapshot 2 minus snapshot 1 temperature, salinity and
differences are presented at depths of 10 m, 50 m, 100 m, 200 m and 400 m.
Contour intervals are 0.5°C,
and
respectively.
and 0.1 for temperature, salinity,
Negative contours are drawn as dashed lines.
Difference maps for dynamic height and variables on
surfaces are not
included.
8.
Vertical sections.
Plots of temperature, salinity,
and geostrophic
velocity relative to 500 m are presented for depths from the sea surface
to 500 m.
Vertical sections include three cross-shore and three
alongshore lines in the snapshot region (both snapshot 1 and snapshot 2),
all of the cross-shore lines north of the snapshot region and three
alongshore lines for the full CCCCS region.
As with the maps, the
southern portion of the full CCCCS region alongshore sections include only
stations from the two long lines in snapshot 2 (lines 13 and 20) so as not
to "oversample" the southern portion of the sections relative to the
northern portion.
The line numbers correspond to the convention defined
in the station location maps discussed previously.
For easy reference, a
The
map of the station locations is included with each vertical section.
plots are grouped by data type.
Contour intervals are 1°C,
0.2,
and relative geostrophic
and 5 cm/s for temperature, salinity,
Positive values correspond to poleward and
velocity, respectively.
onshore velocity, respectively, in the cross shore and alongshore
geostrophic velocity sections.
The CCCCS station numbers and locations
are given along the top of the section plots.
9.
Difference sections.
Vertical sections of snapshot 2 minus snapshot 1
temperature, salinity and
are given for three cross-shore and three
alongshore lines in the snapshot region.
Contour intervals are 0.5°C,
and 0.1 for temperature, salinity and
contours are drawn as dashed lines.
respectively.
For easy reference, a map of the
station locations is included with each vertical section.
grouped by data type.
Negative
The plots are
The CCCCS station numbers and locations are given
along the top of the section plots.
The top row of station numbers refers
36
to
snapshot 2 and the bottom row refers to snapshot 1.
Difference
sections for relative geostrophic velocity are not included.
37
ACKNOWLEDGEMENTS
The collection and initial processing of the CCCCS CTD data presented in
this report were carried out by Raytheon Service Company under Minerals
Management Service Contract No. 14-12-0001-30020.
Gary Parker was chief
scientist on the cruises with responsibility for CTD data collection.
data processing was done by Marian Falla.
Initial
The data listings and plots in this
report were done at Oregon State University under Raytheon Service Company
Subcontract No. 9330936556.
38
REFERENCES
Chelton,
off
D,B., 1984: Seasonal variability of
alongshore geostrophic velocity
central California. Journal of Georhysical Research,
3473-3486.
Chelton, D.B., P.A. Bernal, and J.A. McGowan, 1982: Large-scale interannual
physical and biological interaction in the California Current. Journal of
1095-1125.
Marine Research,
Chelton, D.B., R.L. Bernstein, A. Bratkovich, and P.M. Kosro, 1987: The central
California coastal circulation study.
Trans.
Union,
Amer.
pp. 1, 12-13.
.Cheltou, D.B., and P.M. Kosro, 1987a:
Central California Coastal Circulation
Study CTD observations: Cruise 8401, February 1984.
Oregon State
University Rep. 126, Ref 87-02.
Chelton, D.B., and P.M. Kosro, l987b:
Central California Coastal Circulation
Study CTD observations: Cruise 8403, July 1984.
Oregon State University
Rep. 127, Ref 87-03.
Chelton, D. B., and P. M. Kosro, 1987c: Central California Coastal Circulation
Study CTD observations: Cruise 8501, January 1985.
Oregon State
University Rep. 129, Ref. 87-05.
Fleischbein, J., R.E. Schranim, A. Huyer, and R.L. Smith, 1983:
observations off Oregon and California:
September 1982.
CTD
R/V Wecoma, W82O9A, 7-24
Report 106, Reference 83-13, Oregon State
Hickey, B.M., 1979: The California Current system - hypotheses and facts.
Progress in Oceanograihv,
191-279.
Huyer, A., 1980: The offshore structure and subsurface expression of sea level
off Peru, 1976-1977. Journal of Physical
1755-1768.
39
La Fond, E.C., 1957: Processing Oceanographic Data. Hydrographic Office Pub.
614, U.S. Navy Hydrographic Office.
Lewis, E.L.,, and R.G. Perkin, 1981: The Practical Salinity Scale 1978:
conversion of existing data. Deer-Sea Research,
307-328.
Lynn, R.J., 1967: Seasonal variation of temperature and salinity at 10 m in the
California Current. California Cooperative Fisheries Investigations
Report, 19, 157-174.
Millard, R., J. Toole, and M. Swartz, 1980: A fast responding temperature
413-427.
measurement system for CTD applications. Ocean Engineering,
Montgomery, R.B., 1941: Transport of the Florida Current off Habana.
of. Marine Research,
Journal
198-219.
Reid, J.L, G.I. Roden, and J.G. Wyllie, 1958: Studies of the California Current
System. California Cooperative Oceanic Fisheries Investigations Reports,
28-57.
Reid, J.L., and A,W. Mantyla, 1976: The effect of the geostrophic flow upon
coastal sea level variations in the northern Pacific Ocean.
Geophysical Research,
Journal of
3100-3110.
Saunders, P.M., and N.P. Fofonoff, 1976: Conversion of pressure to depth in the
ocean. Deep-Sea Research,
109-111.
LISTING OF LOCATION TINES AND DEPTHS OF CTD STATIONS
RAYTHEON CRUISE 8404
STATION
DAY HOUR
101
102
103
106
109
111
114
117
119
120
121
122
123
124
127
130
131
134
137
138
139
142
145
146
149
152
155
156
159
162
165
166
169
172
176
177
178
180
7 Oct 1145
1233
1320
1532
1800
2015
2207
2348
8 Oct 0132
0231
0313
0350
0437
0510
0650
0834
1000
1140
1414
1526
1612
1743
1926
2102
2250
9 Oct 0039
0157
0300
0424
0602
0730
0900
1038
182
184
187
190
192
195
198
201
202
1228
1442
1813
1905
2012
2110
2154
2320
10 Oct 0105
0306
0530
0704
0852
1040
1142
LATITUDE
34
34
34
34
25.1
20.4
18.4
12.8
8,0
9.6
34 14.9
34
34
34
34
34
34
34
34
34
34
34
34
34
34
34
34
34
34
34
34
34
34
34
34
34
34
34
34
34
19.5
23,3
25.0
26.3
28,3
31.8
30.3
24.6
20.3
25.2
29.5
34.7
41,3
38.8
34.1
29.6
34.4
39.3
44.8
48.5
54.4
49.4
44.0
40.0
44.8
49.2
54.6
35
0.6
35
35
34
34
34
34
34
34
34
6.8
4.7
1.7
59.4
58.0
53.9
49.5
44.0
54.0
58.8
35
4.1
35 10.4
35 15.3
LONGITUDE
120
120
120
120
120
27.1
27.1
31.1
42.1
52.1
121 8.2
120 56.9
120
120
120
120
120
120
120
120
47.4
40.2
35.9
32.9
29.6
34.5
38.4
50.4
121
121
0.5
3.7
120
120
120
120
120
54.4
42.6
41.5
46.4
57.9
121
7.5
12]. 10.9
121
1.1
120
120
120
120
49.9
40.6
43.1
53.4
121 4.7
121 14.2
121 17.6
121
7.7
120
120
120
120
120
121
56.8
43.4
44,5
48.9
55.4
121
121
121
121
121
0.3
3.2
11.3
20.9
31.9
24.3
121 15.1
121 3.7
120 51.7
120 55.5
ZMAX
78
316
426
682
658
702
672
608
454
264
98
28
32
82
672
726
722
686
66
42
88
650
614
646
586
102
32
42
214
524
642
568
544
310
48
42
DEPTH
80
320
435
690
1000
1000
936
760
460
270
101
30
41
85
823
1000
1100
730
69
44
92
657
1200
915
595
102
34
44
220
531
775
576
565
320
50
45
92
97
242
418
484
560
662
448
586
478
250
425
493
570
450
670
454
595
493
52
54
58
57
464
205
208
211
132].
1536
1702
401
402
403
406
411
414
417
419
420
421
422
423
424
427
430
409
431
434
437
438
439
442
445
446
449
452
455
456
459
462
465
466
469
472
476
477
478
480
481
482
484
487
490
492
495
500
11 Oct 0343
503
508
509
510
600
601
0427
0509
0644
1103
1252
1426
1546
1636
1729
1758
1850
1930
2116
2303
2829
12 Oct 0034
0231
0447
0553
0636
0816
0955
1127
1313
1500
1616
1731
1854
2034
2203
2332
13 Oct 0114
0301
0507
0609
0653
0754
0845
0923
1210
1347
1531
14 Oct 0140
0326
0801
1000
1453
1521
1634
16 Oct 0815
0840
9.0
3.5
34 59.1
34 25.2
34 20.6
34 18.4
34 13.1
34 10.0
34 15.1
34 19.7
34 23.4
34 25.0
34 26.6
34 28.4
34 31.7
34 30.3
34 24.6
34 20.1
34 8.4
34 25.2
34 29.5
34 35.0
34 41.5
34 39.0
34 34.2
34 29.9
34 34.7
34 39.2
34 44.8
35
35
34 48.4
34 54.3
34 49.6
34 44.1
34 39.9
34 44.5
34 49.3
34 54.8
35
1.0
35
7.1
35 4.9
35
1.8
34 59.5
34 58.1
34 54.0
34 49.5
34 44.0
35 10.3
35
4.0
35 9.3
35 15.4
35 38.8
35 37.9
35 34.8
35 38.8
35 38.0
7.7
121 18.7
121 27.6
120 27.1
120 27.1
121
120
120 42.0
121 8.1
120 56.9
120 47.3
120 40.3
120 35.9
120 32.6
120 29.8
120 34.6
120 38.2
120 50.5
121 0.5
120 51.9
121 3.8
120 54.4
120 42.5
120 41.3
120 46.4
120 57.8
121 7.5
121 10.8
121 1.3
120 49.9
120 40.7
120 43.1
120 53.3
121 4.7
121 14.2
121 17.8
121 8.3
120 56.7
120 43.3
120 44.3
120 49.0
120 55.5
121 0.3
121 3.2
121 11.2
121 20.9
121 32.1
120 51.5
121 3.8
121 7.4
120 55.3
121 15.7
121 17.8
121 23.4
121 15.8
121 17.9
544
620
502
74
312
426
688
682
642
654
456
274
92
28
36
80
634
658
706
676
672
60
42
88
642
648
624
598
102
32
44
212
524
680
568
554
306
46
38
92
244
418
484
560
464
674
550
626
497
80
320
433
700
1000
1000
665
460
270
93
32
40
85
830
1000
1000
1000
730
65
45
92
660
1200
900
602
108
40
48
218
532
775
576
565
317
50
45
95
250
425
493
570
470
950
50
55
480
534
490
548
52
30
86
55
32
90
478
485
30
84
33
88
602
603
605
607
609
614
616
618
620
622
627
629
631
633
635
640
642
644
645
648
0936
1030
1157
1335
1520
18 Oct 0700
0813
0948
1121
1332
2135
2340
19 Oct 0108
0255
0425
1753
1908
2025
2132
2359
35 35.3
35 33.4
35 29.3
35 24.6
35 20.3
36
36
36
7.4
3.4
35 59.7
35 53.2
36 28.3
36 34.4
36 38.4
36 43.6
36 47.6
37 21.8
37 17.6
37 13.1
37 10.5
37
3.0
121 23.7
121 27.9
121 36.4
121 46.2
121 55.4
121 44.3
121 51.9
122 0.5
122 8.7
122 21.6
122 46.1
122 32.7
122 24.1
122 12.4
122 3.1
122 30.2
122 39.7
122 49.0
122 55.4
123 10.8
474
662
730
698
632
292
692
716
690
658
742
748
736
730
232
42
482
670
990
1050
2200
299
930
1280
1540
1920
3000
2975
2380
1025
236
45
94
98
254
492
458
258
500
2560
MA2S OF CTD STATION LOCATIONS AND BATHThETRY
STATION LOCATIONS
37
36
35
34
123
122
121
120
STATION LOCATIONS
SNAPSHOT 1
202
201
205
177
178
195
208
150
35
175
211
181
195
192
181
157
180
172
184.
159
159
¶65
155
155
152
162
9
I
155
139
146
137
142
145
124
134
121
131
120
127
101
119
130
102
117
103
114
106
ill
109
121
120
STATION LOCATIONS
SNAPSHOT 2
503
492
500
477
476
495
480
475
481
482
472
484
487
459
469
456
456
455
452
462
438
465
449
446
439
437
442
445
424
434
421
431
420
427
419
430
402
417
403
414
405
411
409
34
120
FULL CCCCS REGION DEPTH (M)
37
36
35
34
123
122
121
120
SNAPSHOT REGION DEPTH (M)
35
34
121
120
DATA LISTINGS
34 25.1N
STA 101
0.
10.
20.
30.
40.
50.
60.
70.
200.
500.
17.117
16.852
16.307
14.626
13.647
13.145
12.718
12.516
120 27.1W
24.313
24.378
24.508
24.886
25.107
25.230
25.338
25.394
33.441
33.4.45
33.450
33.457
33.480
33.508
33.538
33.559
0..
80
0.000
0.036
0.071
0.104
0.133
0.162
0.188
0.215
0.491
0.891
0.
10.
20.
30.
40.
50.
60.
70.
80.
90.
100.
110.
120.
130.
140.
150.
160.
170.
180.
190.
200.
220.
240.
260.
280.
300.
500.
STA 103
34 18.4N
120 31.1W
0— 435
34 20.4N
STA 102
16.336
16.175
16.126
14.646
12.951
12.596
12.401
11.926
11.703
11.401
11.123
10.946
10.739
10.417
10.260
10.026
9.768
9.526
9.298
9.107
8.938
8.645
8.382
8.041
7.839
7.539
STA 106
120 27.1W
33.462
33.464
33.464
33.425
33.496
33.541
33.550
33.588
33.600
33.608
33.633
33.654
33.691
33.736
33.763
33.808
33.862
33.893
33.940
33.972
34,003
34.038
34.069
34.094
34.105
34.124
34 12.8N
24.511
24.549
24.560
24.856
25.259
25.364
25.409
25.528
25.580
25.641
25.711
25.759
25,824
25.916
25.964
26.039
26.124
26.189
26.262
26.318
26.369
26.442
26.507
26.578
26.617
26.675
0— 320
0.000
0.034
0.068
0.102
0.130
0.157
0.183
0,208
0.233
0.257
0.280
0.303
0.325
0.346
0.367
0.387
0.407
0.425
0.443
0.461
0.478
0.510
0.541
0.572
0.601
0.629
0.886
120 42.1W
0— 690
0.000
0.034
0.067
0.098
0.127
0.154
0.180
0.205
0.230
0.253
0.276
0.299
0.321
0.342
0.364
0.384
0,404
0,424
DELD
0.
10.
20.
30.
40.
50.
60.
70.
80.
90.
100.
110.
120.
130.
140.
150.
160.
170.
180.
190.
200.
220.
240.
260.
280.
300.
350.
400.
500.
16.314
16.127
13.704
12.809
12.553
11.960
11.758
11.492
11.256
11.167
10.902
10.635
10.295
10.213
10.007
9.895
9.740
9.626
9.433
9,198
9.156
8.925
8.523
8.381
8.268
8.111
7.267
6.824
33.450
33.451
33.381
33.397
33.487
24.506
24.550
25.020
25.211
25.331
33.554. 25.495
33.570
33.597
33.623
33.633
33.673
33.713
33.770
33.781
33.810
33.822
33.852
33.873
33.916
33.978
33.987
34.021
34.058
34.069
34.078
34.086
34.136
34.153
25.546
25.616
25.679
25.703
25.781
25.860
25.963
25.986
26.043
26.072
26.120
26.156
26.222
26.308
26.322
26.385
26.477
26.507
26.531
26.562
26.723
26.798
-
10.
20.
30.
40.
50.
60.
70.
80.
90.
100.
110.
120.
130.
140.
150.
160.
16.007
15.952
15.684
13.811
13.161
12.466
12.195
11.903
11.608
11.279
11.055
10.888
10.720
10.503
10.343
10.067
10.002
33.467
33.472
33.468
33.377
33.427
33.430
33.515
33.588
33.610
33.625
33.650
33.663
33.682
33.710
33.742
33.801
24.589
24.606
24.662
24.995
25.165
25.303
25.421
25.533
25.605
25.677
25.737
25.776
25.821
25.881
25.933
26.026
33.814.
26.04.7
170.
9.891
180.
190.
9.722
9.624
33.838
33.871
33.887
26.085
26.139
26.168
0.460
0.493
0.526
0.557
0.567
0.617
0.687
0.752
200.
9.301
22.922
26.248
0.479
220.
240.
260.
280.
300.
350.
400.
8.980
6.483
8.179
7.820
7.659
7.286
6.855
33.969
34.009
34.058
34.063
34.102
34.139
34.156
26.336
26.445
26.529
26.587
26.641
26.723
26.796
0.514
0.547
0.578
0.607
0.636
0.705
0.770
0,875
450,
500.
6.562
34,169
26.846
5.774
5.928
5.615
5.384
5.159
34.150
34.271
34.280
26.932
27.008
27.054
27.125
27.166
0.832
0.891
0.000
0.034
0.066
0.095
0.122
0.147
0.172
0.196
0.220
0.243
0.266
0.287
0.308
0.329
0.349
0.368
0.388
0.406
0.425
0.442
0.
550.
600.
650.
682.
3,334
34.352
0.443
0.461
0.946
0.998
1.047
1.077
STA 109
0,
10.
20.
30.
40.
50.
60.
70.
80.
90.
100.
110.
120.
130.
140.
150.
160.
170.
180.
190.
200.
220.
240.
260.
280.
300.
350.
400.
450.
500.
550.
600.
650.
658.
34
18.157
18.074
17.169
16.085
14.366
14.106
13.362
13.170
12.405
11.811
11.387
10.812
10.623
10.304
9.963
9.833
9.588
9.475
9.148
9.007
8.930
8.596
8,347
8.155
7.967
7.697
6.940
6.539
6.417
6.003
5.881
5.772
5.440
5.332
114
0.
10.
20.
30.
40.
50.
60.
70.
80.
90.
100.
110.
120.
130.
140.
150.
160.
170.
180.
190.
200.
220.
240.
260.
280.
300.
350.
400.
450.
500.
550.
600.
650.
672.
8.0W
33.525
33.526
33.510
33.498
33.466
33.470
33.481
33.487
33.491
33.533
33.597
33.661
33.692
33.751
33.812
33.832
33.876
33.898
33.955
33.990
34,004
34.040
34.070
34.078
34.094
34.107
34.162
34.168
34.189
34.211
34.260
34.280
34.326
3.4.323
34 14.9W
18.222
18.163
18.134
18.109
15.815
13.339
13.245
13.055
12.476
12.077
11.549
10.951
10.588
10.108
9.914
9.678
9.562
9.463
9.304
9.203
9.123
8.835
8.531
8.136
8.026
7.800
7.413
6.998
6.611
6.405
6.124
5.748
5.447
5.310
120 52.1W
0—1000
24.126
24.148
24.353
24.595
24.947
25.005
25.166
25.210
25.362
25.507
25.635
25.788
25.845
25.947
26.052
26.090
26.165
26.201
26.298
26.348
26.371
26.452
26.513
26.549
26.589
26.639
26.789
26.848
26.880
26.951
27.005
27.035
27.112
27.122
0.000
0.038
0.075
0.110
0.142
0.171
0.201
0.229
0.256
0.281
0.305
0.328
0.350
0.372
0.392
0.411
0.430
0.448
0.466
0.484
0.500
0.333
0.564
0.594
0.624
0.653
0.720
0.782
0.842
0.899
0.954
1.006
1.056
1.064
120 56.9W
0— 936
24.088
24.125
24.145
24.151
24.508
24.940
25.101
25.206
25.346
25.467
25.604
25.740
25.812
25.963
26.030
26.125
26.159
26.186
26.249
26.290
26.317
26.395
26.477
26.563
26.587
26.644
0.000
0.038
0.076
0.114
0.151
0.183
0.212
0.240
0.268
0.294
26.722
0.738
0.804
0.865
0.923
33.495
33.525
33.541
33.541
33.305
33.182
33.367
33.453
33.488
33.546
33.596
33.630
33.641
33.728
33.772
33.844
33.863
33.877
33.924
33.956
33.974
34.015
34.060
34.092
34.103
34.133
34.161
34.174
34.206
34.239
34.268
34.285
34.295
34.298
0.318
0.342
0.364
0.385
0.405
0.425
0.443
0.462
0.480
0.498
0.515
0.549
0.581
0.612
0.641
0.670
26.790
26.868.
26.922
26.981
27.041
27.086
27.105
-
0.979
1.032
1.083
1.105
34
STA 111
0.
10.
20.
30.
40.
50.
60.
70.
80.
90.
100.
110.
120.
130.
140.
150.
160.
170.
180.
190.
200.
220.
240.
260.
280.
300.
350.
400.
450.
500.
550.
600.
650.
700.
702.
18.063
18.060
18.061
18.068
17.308
14.981
13.966
12.839
12.172
11.602
11.396
10.949
10.634
10.089
9.841
9.580
9.374
9.106
8.966
8.800
8.625
8.371
8.109
8.096
7.721
7.387
7.023
6.824
6.591
6.378
6.155
5.934
5.723
5.489
5.481
STA 117
100.
110.
120.
130.
140.
150,
160.
170.
180.
190.
200.
220.
240.
260.
280.
300.
350.
400.
450.
500.
550.
600.
608.
-
0—1000
33.540
33.351
33.553
33.553
33.382
33.331
33.367
33.386
33.403
33.491
33.508
33.555
33.617
33.685
33.728
33.800
33.842
33.877
33.904
33.941
33.968
33.996
34.013
34.088
34.081
34.073
34.087
34.146
34.219
34.235
34.252
34.287
24.161
24.170
24.171
24.170
24.222
24.728
24.955
25.197
25.339
25.513
25.565
25.682
25.785
25.932
26.007
26.107
26.174
0.000
0.038
0.075
0.113
0.150
0.185
0.216
0.245
0.272
0.298
0.323
3.4.303
27.059
34.321
34.323
27.102
27.104
0.369
0.391
0.411
0.431
0.450
0.468
0.485
0.503
0.519
0.552
0.583
0.613
0.642
0.670
0.739
0.803
0.864
0.923
0.979
1.033
1.085
1.134
1.136
120 47.4W
0— 760
34 19.5W
17.195
17.075
16.629
13.537
13.684
12.778
12.453
12.228
11.977
11.857
11.364
11.136
11.041
10.908
10.727
10.250
9.991
9.629
9.446
9.322
9.127
8.864
8.643
8.436
8.293
7.754
7.421
6.916
0.
10.
20.
30.
40.
50.
60.
70.
80.
90.
8.2W
9.6W
6.267
5.862
5.750
5.515
5.453
121
33.492
33.493
33.468
33.133
33.456
33.406
33.494
33.533
33.575
33.583
33.625
33.648
33.659
33.673
33.694
33.767
33.810
33.877
33.914
33.938
33.976
34.022
34.049
34.061
34.077
34.056
34.133
34.158
34.173
34.220
34.279
34.293
34.301
26.24.4
26.288
26.343
26.391
26.452
26.505
26.565
26.615
26.656
26.719
26.793
26.881
26.922
26.964
27.020
24.333
24.363
24.447
24.863
25.081
25.224
25.355
25.428
25.509
25.537
25.661
23.721
25.746
25.780
25.829
25.969
26.046
26.159
26.218
26.256
26.318
26.396
26.451
26.493
26.527
26.591
26.699
26.789
26.888
26.976
27.036
27.076
27.090
0.000
0.036
0.071
0.104
0.134
0.163
0.190
0.216
0.241
0.265
0.289
0.312
0.335
0.358
0.380
0.401
0.421
0.440
0.459
0.477
0.494
0.528
0.560
0.592
0.622
0.652
0.722
0.788
0.849
0.906
0.959
1.010
1.018
STA 119
34 23.3N
120 40.2W
B— 460
120 35.9W
34 25.ON
5Th 120
SAL
0.
10.
20.
30.
40.
50.
60.
70.
80.
90.
100.
110.
120.
130.
140.
150.
160.
170.
180.
190.
200.
220.
240.
260.
280.
300.
350.
400.
450.
500.
15.086
15.069
14.908
13.075
12.906
12.755
12.460
12.200
11.907
11.669
11.207
10.832
10.572
10.288
10.196
10.028
9.836
9.565
9.464
9.386
9.251
9.025
8.660
8.200
8.071
7.810
7.343
6.864
6.219
STA 121
0.
10.
20.
30.
40.
50.
60.
70.
80.
90.
200.
500.
33.469
33.470
33.456
33.522
33.532
33.535
33.542
33.567
33.579
33.602
33,634
33.670
33.712
33.756
33.771
33.800
33.835
33.885
33.909
33.925
33.952
33.992
34.040
34.025
34.063
34.079
34.127
34.152
34.200
34 26.3N
16.093
16.089
13.672
13.287
12.977
12.354
12.223
11.923
11.733
11.596
24.795
24.799
24.824
25.255
25.296
25.328
25.391
25.460
25.525
25.587
25.697
25.792
25.870
25.954
25.981
26.032
26.092
26.175
26.211
26.236
26.279
26.347
26.441
26.500
26.549
26.601
26.705
26.791
26.915
0.000
0.032
0.063
0.092
0.119
0.146
0.172
0.198
0.223
0.247
0.271
0.294
0.316
0.336
0.357
0.377
0.397
0.416
0.434
0,452
0.470
0.504
0.537
0.569
0.599
0.628
0.698
0.764
0.825
0.880
120 32.9W
B— 101
33.490
33.488
33.477
33.518
33.534
33.570
33.582
33.608
33.625
33.642
24.587
24.587
25.100
25.209
25.284
25.433
25.467
25.545
25.593
25.632
0.000
0.034
0.065
0.094
0.121
0.147
0.173
0.197
0.222
0.246
0.466
0.871
0.
10.
20.
30.
40.
50.
60.
70.
80.
90.
100.
110.
120.
130.
140.
150.
160.
170.
180.
190.
200.
220.
240.
260.
500.
15.740
15.624
13.524
12.984
12.817
12.484
12.381
12.066
11.857
11.581
11.468
10.808
10.673
10.476
10.058
9.911
9.824
9.678
9.492
9.368
9.199
8.780
8.534
8.385
33.395
33.489
33.494
33.527
33.542
33.561
33.567
33.592
33.605
33.622
33.626
33.718
33.733
33.754
33.813
33.833
33.840
33.868
33.900
33.919
33.937
33.992
34.035
34.053
B— 270
DELD
24.594
24.692
25.143
25.277
25.321
25.402
25.426
25.505
25.554
25.619
25.643
25.833
25.869
25.919
26.037
26.077
26.097
26.144
26.199
26.234
26.276
26.385
26.457
26.494
0.000
0.033
0.063
0.091
0.118
0.144
0.170
0.195
0.220
0.244
0.267
0.290
0.311
0.333
0.353
0.373
0.392
0.411
0.429
0.447
0.465
0.499
0.531
0.562
0.872
.
5Th 122
0.
10.
20.
200.
500.
34 28.3N
16.749
14.869
14.605
120 29.6W
33.491
33.482
33.487
24.437
24.852
24.912
30
B-.
0.000
0.033
0.064
0.465
0.866
.
34 31.8N
5Th 123
0.
10.
20.
30.
16.327
15.314
14.412
14.006
120 34.5W
33.493
33.462
33.483
33.494
24.536
24.740
24.951
25.044
200.
500.
D—
41
0.000
0.034
0.064
0.094
0.466
0.880
34 30.3N
STA 124
0.
10.
20.
30.
40.
50.
60.
70.
80.
15.050
14.254
13.586
13.391
13.237
13.064
12.877
12.606
12.290
120 38.4W
33.492
33.488
33,503
33.508
33.514
33.522
33.533
33.546
33.568
24.821
24.988
25.137
25.181
25.217
25.258
25.302
25.366
25.4.43
200.
500.
STA 127
34 24.6N
0.
16.960 33.462
16.967 33.466
16.900 33.463
16.030 33.344
13.288 33.186
13.180 33.216
12.824 33.343
12.568 33.366
11.786 33.427
11.482 33.513
11.135
33.575
10.642 33.663
10.343
33.710
10.055 33.752
9.890 33.780
9.588 33.844
9.366 33.877
9.292 33.903
9.181 33.920
9.115 33.920
9.040 33.915
8.852 34.009
8.547 34.039
8.076 34.039
7.835 34.069
7.827 34.108
7.320 34.150
6.876 34.174
6.286 .34.190
6.164 34.247
24.366
24.367
24.381
24.490
24.954
24.998
25.166
25.234
25.430
25.553
25.664
25.820
25.908
23.990
26.040
26.140
26.202
26.234
26.265
26.276
26.284
26.387
26.458
26.530
26.589
26.621
26.727
26.807
26.899
26.959
0.000
0.036
0.071
0.107
0.139
0.169
0.198
0.226
0.252
0.277
0.301
0.324
0.346
0.366
0.386
0.406
0.424
10.
20.
30.
40.
50.
60.
70.
80.
90.
100.
110.
120.
130.
140.
150.
160.
170.
180.
190.
200.
220.
240.
260.
280.
300.
350.
400.
120 50.4W
D.- 823
Sm 130
34 20.2N
121
0.000
0.031
0.060
0.088
0.116
0,143
0.171
0.197
0.223
0.464
0.876
D—1000
0.000
0.039
0.078
0.117
0.155
0.188
0.218
0.245
0.272
0.297
0.321
0.344
0.365
0.387
0.407
0.427
0.446
0.465
0.483
0.500
0.517
0.550
0.581
0.612
0.641
0.669
0.737
0.800
0.460
0.478
0.495
0.329
0.561
0.592
0.622
0.651
0.719
0.784
18.751
18.756
18.751
18.719
15.609
13.607
12.845
12.249
11.732
11.351
11.044
10.709
10.442
10.099
9.945
9.737
9.536
9.342
9.075
8.870
8.819
8.675
8.431
8.172
7.839
7.479
7.219
6.878
33.573
33.570
33.570
33,571
33.080
33.051
33.290
33.349
33.382
33.496
33.561
33.627
33.661
33.718
33.748
33.783
33.820
33.865
33.905
33.957
33.966
34.027
34.076
34.079
34.093
34.086
34.169
34.195
24.016
24.012
24.013
24.022
24.382
24.785
25.122
25.283
25.405
25.563
25.669
25.780
25.853
25.956
26.006
26.068
26.129
26.197
26.271
0.84.4
450.
6.508
34.221
26.893
0.901
500.
6.291
34.249
26.94.4
0.442
85
0.5W
10.
20.
30.
40.
50.
60.
70.
80.
90.
100.
110.
120.
130.
140.
150.
160.
170.
180.
190.
200.
220.
240.
260.
280.
300.
350.
400.
0.
D-.
26.34.4
26.359
26.429
26.505
26.547
26.607
26.654
26.756
26.824
550.
5.879
34.270
27.013
0.955
550.
6.038
34.281
27.002
0.860
0.918
0,972
600.
3.329
34.301
27.081
1,007
600.
5.811
34.296
27.043
1.025
650.
672.
5.275
5.150
34.309
34.316
27.118
27.138
1.055
650.
5.380
34.309
27.105
1.075
1.076
700.
726.
5.049
34.326
34.345
27.158
1.122
1.145
450.
500.
4.949
27.184
34 25.2N
STA 131
0.
10.
20.
30.
40.
50.
60.
70.
80.
90.
100.
110.
120.
130.
140.
150.
160.
170.
180.
190.
200,
220.
240.
260.
280.
300.
350.
400.
450.
500.
550.
600.
650.
700.
722.
19.016
19.018
19.002
17.970
15.525
13.939
12.816
12.498
11.809
11.327
11.087
33.573
33.573
33.569
33.470
33.368
33.300
33.280
33.339
33.424
33.498
33.568
10.694 '
33.637
10,327
10.110.
9,789
9.501
9.368
9.140
8.977
8.755
8.539
8.241
8.050
7.818
7.534
7.414
6.910
6.676
6.515
6.190
5.935
5.514
5.221
5.047
5.009
33.670
33.712
33.759
33.798
33.844
33.869
33.900
33.952
33.984
34.016
34.065
34.063
34.073
34.073
34.102
34.161
34.232
34.259
34.287
34.289
34,318
34.338
34.360
STA 137
0.
10.
20.
30.
40.
50.
60.
200.
500.
121
34 34,7N
14.888
14.821
14.758
14.500
14.133
13.657
13.180
3.7W
D—1100
23.949
23.948
23.950
24.130
24.621
24.909
25.120
25.227
25.423
25.570
25.667
25.791
25.880
25.949
26.040
26.118
0.000
26.176
26.232
26.282
26.358
26.416
26.487
26.554
26.587
26.636
26.653
26.746
26.824
26.901
26.965
27.020
27.074
27.131
27.167
27.189
120 42.6W
33.488
33.487
33.486
33.478
33.487
33.507
33.520
24.853
24.867
24.879
24.928
25.012
25.126
25.233
STA 134
34 29.SN
0.079
0.119
0.155
0.186
0.216
10.
20.
30.
40.
50.
60.
17.407
17.395
17.255
16.076
14.065
12.849
12.343
0.244
70.
12.195
0.270
0.295
0.319
0.342
0.363
0.384
0,405
0.424
0.443
0.461
0.479
0.496
0.512
0.544
0.574
0.604
0.633
0.661
0.729
0.792
0.852
0.909
0.963
1.014
1.063
1,109
1.129
80.
90.
11.621
11.119
10.878
10.623
10.216
9.886
9.692
9.618
9.502
9.299
9.177
9.093
8.864
8.786
8.351
8.068
7.815
7.737
7.265
6.905
6.426
6.035
5.710
5.367
5.080
5.060
0.040
D-'
69
0.000
0.031
0.062
0.093
0.123
0.152
0.180
0.466
0.875
0.
100.
110.
120.
130.
140.
150.
160.
170.
180.
190.
200.
220.
240.
260.
280.
300.
350.
400.
450.
500.
550,
600.
650.
686.
STA 138
0.
10.
20.
30.
40.
200.
500.
D-' 730
24.284
24.287
24.306
24.419
0.000
0.036
0.073
0.109
0.142
0.172
0.201
0.228
0.253
0.278
0.300
0.323
0.344
0.364
0.384
0.403
0.422
0.440
0.458
0.475
0.492
0.525
0.557
0.587
0.617
0.645
0.713
0.777
0.837
0.894
0,948
0.998
1.046
1.079
33.493
33.494
33.475
33.266
33.233
33.206
33.283
33.394
33.474
33.565
33.640
33.665
33.716
33.761
33.817
33.837
33.867
33.908
33.933
33.944
33.989
34.041
34.040
34.066
34.094
34.119
34.152
34.178
34.218
34,246
34.277
34.298
34.315
34.330
34 41.3N
15.925
15.763
14,795
13.576
13.163
120 54.4W
24.83].
25.056
25.213
25,327
25.497
25.659
25.760
25.825
25.935
26.026
26.102
26.129
26.172
26.237
26.276
26.298
26.369
26.423
26.489
26.552
26.612
26.642
26.736
26.806
26.902
26.975
27.040
27.098
27.146
27.160
120 41.5W
33.421
33.426
33.380
33.487
33.520
24.572
24.613
24.790
25.127
25.236
D-'
44
0.000
0.034
0.067
0.097
0.125
0.496
0.907
34 38.8N
STA 139
0.
10.
20.
30.
40.
50.
60.
70.
80.
200.
500.
16.401
16.290
15.721
14.862
14.411
14.084
12.931
12.314
12.086
STA 145
0.
10.
20.
30.
40.
50.
60.
70.
80.
'90.
100.
110.
120.
130.
140.
150.
160.
170.
180.
190.
200.
220.
240.
260.
280.
300.
350.
400.
450.
500.
550.
600.
614.
120 46.4W
33.4.43
24.481
33.446
33.468
33.474
33.479
33.486
33.506
33.549
33.581
24.509
34 29.6N
24.654
24.847
24.947
25.022
25.272
25.424
25.493
121
17.415
17.417
17.205
15.708
12.876
12.238
11.554
11.708
11.507
10.715
10.461
10.414
10.109
9.829
9.688
9.494
9.326
9.092
8.883
8.754
8.641
33.454
33.454
33.489
33.393
32.996
33.065
33.116
33.235
33.483
33.389
33.492
33.581
33.657
33.775
33.814
33.847
33.884
33.926
33.973
34.004
34.014
8.4.49
34.022
8.274
8.065
7.725
7.628
7.240
6.786
6.340
6.157
5.843
5.443
3,314
34.059
34.086
34.085
34.119
34.158
34.182
34.197
34.237
34.257
34.267
34.286
0—
92
0.000
0.035
0.068
0.101
0.131
0.161
0.189
0.215
0.241
0.502
0.910
7.5W
D—1200
24.252
24.252
24.329
24.600
24.888
25.065
25.232
25.296
25.525
25.594
25.719
25.796
25.907
26.046
26.100
26.158
26.214
26.285
26.354
26.398
26.425
26.460
26.515
26.569
26.618
26.659
26.745
26.825
26.897
26.952
27.008
27.065
27.095
0.000
0.037
0.073
0.109
0.141
0.170
0.199
0.226
0.252
0.276
0.299
0.322
0.343
0.364
0.383
0.402
0.421
0.438
0.456
0.472
0.488
0.520
0.551
0.582
0.611
0.639
0.707
0.770
0.830
0.887
0.942
0.993
1.007
0.
10.
20.
30.
40.
50.
60.
70.
80.
90.
100.
110.
120.
130.
140.
150.
160.
170.
180.
190.
200.
220.
240.
260.
280.
300.
350.
400.
450.
500.
550.
600.
650.
17.561
17.562
17.489
16.543
14.541
13.045
12.293
12.230
11.496
11.974
11.461
11.075
10.764
10.384
10.182
9.859
9.723
9.573
9,350
9.270
8.954
8.534
8.185
8.002
7.867
7.711
7.324
6.498
6.005
6.042
5.756
5.403
5.239
STA 146
0.
10.
20.
30.
40.
50.
60.
70.
80.
90.
100.
110.
120.
130.
140.
150.
160.
170.
180.
190.
200.
220.
240.
260.
280.
300.
350.
400.
450.
550.
600.
646.
120 57.9W
0— 657
24.259
24.259
24.280
24.471
24.701
24.868
25.030
25.132
25.238
25.507
25.603
25.735
25.804
25.925
25.985
26.082
26.130
26.178
26.240
26.261
26.333
26.424
26.513
26.563
26.595
26.638
26.724
26.801
26.905
26.968
27.022
27.083
27.123
0.000
0.037
0.073
0.109
0.143
0.174
0.205
0.233
0.262
0.288
0.312
0.335
0.358
0.379
0.400
0.419
0.438
0.457
0.475
0.493
0.511
0.544
0.575
0.605
0.635
0.663
0.732
0.796
0.857
0.914
0.967
1.018
1.068
121 10.9W
0- 915
33.383
33.386
33.399
33.413
33.238
32.984
33.048
33.119
33.305
33.390
24.239
24.280
24.382
24.710
24.932
25.154
25.277
25.482
25.631
0.000
0.037
0.074
0.110
0.144
0.176
0.205
0.233
0.259
0.283
33.1.49
25.702
0.307
33.528
33.639
33.757
33.791
33.826
33.860
33.868
33.920
33.917
33.949
25.792
25.932
26.061
26.126
26.179
26.242
26.266
26.335
26.342
26.378
26.424
26.493
26.541
26.596
26.657
26.782
26.864
26.921
26.964
27.032
27,104
27.154
0.329
0.351
0.371
0.390
0.409
0.427
34 34.1N
STA 142
33.509
33.510
33.514
33.472
33.194
33.013
33.034
33.150
33.110
33.572
33.573
33.653
33.670
33.741
33.774
33.827
33.860
33.889
33.922
33.932
33.960
33.993
34.039
34.067
34.083
34.108
34.148
34.102
34.153
34.239
34.262
34.285
34.310
34 34.4N
17.242
17.229
17.120
16.732
14.659
12.603
11.690
11.319
10.984
10.508
10.361
10.194
9.874
9.656
9.422
9.263
9.035
8.924
8.743
8.680
8.608
8.420
8,264
8.071
7.888
7.635
7.036
6.405
5,979
5.859
5.566
5.304
4.991
33.97'l
34.028
34.052
34.088
34.118
34.170
34.166
34.169
34,204
34.244
34.296
34.313
24.21.4
0.445
0.462
0.479
0.496
0.529
0.560
0.591
0.620
0.649
0.716
0.778
0.836
0.892
0.945
0.996
1.039
34 39.3N
STA 149
0.
10.
20.
30.
40.
50.
60.
70.
80.
9C.
100.
110.
120.
130.
140.
150.
160.
170.
180.
190.
200.
220.
240.
260.
280.
300.
350.
400.
450.
500.
550.
586.
16.583
16.574
16.408
16.235
13.844
13.640
13.794
12.342
11.712
11.123
10,464
10.191
9.994
9.902
9.689
9.313
9.166
9.076
8.965
8.715
8.600
8.383
8.205
8.099
8.010
7.773
7.366
6.868
6.042
5.692
5.444
5.371
5Th 155
0.
10.
20.
30,
200.
500.
33.434
33.434
33.397
33.339
33.071
33.230
33.401
33.377
33.486
33.557
33.672
33.733
33.761
33.783
33.791
33.863
33.895
33.909
33.917
33.965
33.987
34.033
34.046
34.061
34.092
34.084
34.101
34.145
34.155
34.248
34.276
34.291
34 48.5N
15.269
14.961
13.478
13.115
121
1.1W
24.432
24.434
24.444
24.440
24.752
24.916
25.017
25.286
25.490
25.652
25.858
25.952
26.007
26.040
26.082
26.200
26.248
26.274
26.297
26.374
26.409
26.479
26.516
26.544
26.581
26.610
26.681
26.786
26.902
27.020
27.071
27.092
120 40.6W
SAL
33.447
33.449
33.460
33.472
24.738
24.807
25.126
25.209
tb.- 595
0.000
0.035
0.070
0.105
0.139
0.170
0.200
0,229
0,254
0.279
0.301
0.322
0.342
0.362
0.382
0,401
0.419
0.437
0.454
0.471
0.488
0.519
0.550
0.580
0.610
0.639
0.709
0.775
0.836
0.891
0.942
0.978
D—
34
0.000
0.032
0.062
0.090
0.435
0.853
34 44.8N
STA 152
0.
10.
20.
30.
40.
50.
60.
70.
80.
90.
100.
200.
17,124
16.392
15.699
14.224
13.236
12.695
12.008
11,567
11.400
11.242
11.254
120 49.9W
33.484
33.450
33.443
33.403
33.405
33.470
33.559
33.609
33.638
33.657
33.655
24.34.4
24.488
24.640
24.928
25.133
25.290
25.490
25.612
25.665
25.708
25.705
500.
STA 156
0.
10.
20.
30.
40.
200.
500.
120 43.1W
SAL
33.414 24.539
33.406 24.894
33.371 25.167
33.377 25.207
33.459 25.305
34 54.4N
16.052
14.397
12.931
12.755
12.569
0—
0.000
0.036
0.070
0.101
0.131
0.159
0.185
0.209
0.233
0.256
0.279
0.463
0.874
D—
44
0.000
0.033
0,062
0.090
0.117
0.457
0.939
__
=
34 49.4N
STA 159
0.
10.
20.
30.
40.
50.
60.
70.
80.
90.
100.
110.
120.
130.
140.
150.
160.
170.
180.
190.
200.
500.
17.199
17.204
16.849
15.093
12.706
12.408
11.045
11.317
11.107
10.829
10.489
10.466
10.445
10.338
10.131
9.858
9.656
9.360
9.227
9.166
9.141
STA 165
0.
10.
20.
30.
40.
50.
60.
70.
80.
90.
100.
110.
120.
130.
140.
150.
160.
170.
180.
190.
200.
220.
240.
260.
280.
300.
350.
400.
450.
500.
550.
600.
642.
D-. 220
24.343
24.341
24.404
24.719
25.059
25.261
25.415
25.561
25.656
25.759
25.870
25.885
25.896
25.931
25.993
26.073
26.127
26.203
26.239
26.259
26.267
0.000
0.036
0.072
0.105
0.136
0.164
0.190
0.215
0.239
0.262
0.284
0.306
0.327
0.348
0.368
0.388
0.408
0.426
0.444
33.505
33.505
33.478
33.373
33.174
33.360
33.234
33.484
33.559
33.627
33.693
33.708
33.717
33.739
33.772
33.815
33.842
33.878
33.896
33.909
33.914
34 40.ON
17.146
17.142
17.100
16.967
16.327
12.970
12.450
11.943
11.517
11.655
11.156
10.932
10.482
10.190
10.076
9.666
9.444
9.332
9.019
8.640
8.295
7.953
7.786
7.612
7.297
7.509
7.149
6.617
6.075
5.845
5.642
5.554
5.382
120 53.4W
121 14.2W
33.385
33.385
33.384
33.379
33.319
32.957
32.940
32,935
33.026
33.203
33.273
33.307
33.383
33.434
33.447
33.656
33.775
33.788
33.867
33.907
33.928
33.962
33.993
34.003
34.007
34.099
34.135
34.189
34.178
34.198
34.244
34.255
34.286
24.263
24.264
24.273
24.301
24.357
24.840
24.928
25.035
25.169
25.281
25.425
25.493
25.630
25.719
25.749
25.981
26.110
26.138
26.250
26.340
26.410
26.488
26.537
26.570
26.617
26.660
26.755
26.854
26.916
26.961
27.022
27.042
27.087
0.462
0.480
0.933
D-. 775
0.000
0.037
0.073
0.110
0.146
0.179
0.210
0.240
0.269
0.296
0.322
0.348
0.372
0.396
0.418
0.440
0.460
0.479
0.497
0.514
0.531
0.563
0.594
0.623
0.653
0.681
0,748
0.811
0.870
0.926
0.980
1.032
1.075
34 44.ON
STA 162
0.
10.
20.
30.
40.
50.
60.
70.
80.
90.
100.
110.
120.
130.
140.
150.
160.
170.
180.
190.
200.
220.
240.
260.
280.
300.
350.
400.
450.
500.
524.
=
17.125
17.119
16.404
15.306
14.379
13.598
12.994
12.460
11.582
11.202
10.649
10.439
10.192
9.925
9.782
9.566
9.357
9.293
9.221
9.019
8.984
8.731
8.615
8.479
8.266
7.945
7.560
7.094
6.244
5.840
5.771
5Th 166
0.
10.
20.
30.
40.
50.
60.
70.
80.
90.
100.
110.
120.
130.
140.
150.
160.
170.
180.
190.
200.
220.
240.
260.
280.
300.
350.
400.
450.
500.
350.
568.
121
SAL
33.495
33.494
33.411
33.473
33.484
33.490
33.506
33.483
33.472
33.546
33.644
33.689
33.736
33.770
33.795
33.834
33.878
33.887
33.886
33.941
33.949
33.983
34.011
34.046
34.050
34.060
34.099
34.127
34.084
34.233
34.255
34 44.8N
17.230
17.228
17.230
16.525
13.937
13.180
12.789
12.921
12.958
12.718
12.462
12.108
11.385
10.655
10.195
9.847
9.580
9.409
9.241
8.997
8.828
8.368
8.073
7.841
7.439
7.119
6.591
6.491
6.383
6.280
5.863
5.665
4.7W
D-. 531
24.352
24.353
24.456
24.750
24.958
25.125
25.259
25.345
25.502
25.629
25.804
25.875
25.954
26.026
26.070
26.136
26.204
26.222
26.232
26.307
26.320
26.386
26.426
26.474
26.510
26.566
26.652
26.740
26.820
26.989
27.015
0.000
0.036
0.072
0.105
0.136
0.165
0.194
0.220
0.246
121 17.6W
33.375
33.373
33.374
33.390
33.190
33.125
33.117
33.258
33.394
33.496
33.324
33.542
33.616
33.625
33.697
33.753
33.819
33.850
33.872
33.886
33.906
33.958
33.965
33.989
33.999
34.004
34.039
34.091
34.172
34.196
34.221
34.246
24.236
24.235
2.235
24.412
24.825
24.928
24.999
25.081
25.179
25.305
25.377
25.458
25.650
25.788
25.924
26.026
26.122
26.174
26.219
26.268
26.311
26.422
26.473
26.525
26.591
26.640
26.740
26.794
26.872
26.904
26.977
27.021
0.270
0.293
0.315
0.336
0.356
0.376
0.395
0.414
0.432
0.450
0.467
0.484
0.518
0.551
0.583
0.614
0.644
0.716
0.784
0.848
0.906
0.932
D— 576
0.000
0.037
0.074
0.111
0.144
0.175
0.204
0.234
0.262
0.290
0.316
0.342
0.366
0.389
0.411
0.431
0.451
0.469
0.488
0.505
0.523
0.556
0.588
0.619
0.649
0.678
0.745
0.810
0.872
0.930
0.987
1.006
34 49.2N
STA 169
0.
10.
20.
30.
40.
50.
60.
70.
16.447
16.440
15.771
12.848
12.339
11.812
11.662
11.484
80.
90.
11.358
10.833
121
SAL
7.7W
1— 565
STA 172
33.362
33.361
33.274
32.946
32.935
32.979
33.052
24.408
24.409
24.494
24.855
24.945
25.079
25.162
0.000
0.035
0.070
0.104
0.134
0.164
0.192
17.712
17.698
17.122
14.307
13.588
13.042
12.804
33.533
24.241
0.000
10.
20.
30.
40.
50.
60.
33.532
33.485
33.356
33.286
33.408
33.428
24.243
24.345
24.875
24.970
25.174
25.236
0.037
0.074
0.107
0.137
0.166
33.208
33.343
33.350
33.488
33.599
33.707
25.316
25.444
25.543
25,696
25.827
25.957
0.220
0.246
0.271
0.294
0.317
0.338
70.
80.
90.
100.
110.
120.
12.078
11.593
11.139
10.681
10.560
10.109
33.423
33.455
33.511
33.609
33.655
33.771
25.372
25.487
25.613
25.771
25.828
25.996
0.193
0.220
0.246
C.271
0.294
0.316
0.337
33.686
33.747
26.012
26.090
0,359
0,378
130.
9.684
33.812
26.099
0.357
33.835
33.883
33.904
26.148
26.212
26.246
0.397
0.416
140.
150.
160.
9.626
9.367
9.249
33.819
33.881
33.907
26.114
26.205
26.244
0.376
0.394
0.412
33,930
33.953
33.955
33.961
33.997
26.278
26.319
26.322
26.337
26.399
0.430
0.447
0.465
34.028
34.068
34.070
34.075
26.457
26.547
26.556
26.574
0.
100.
10.571
10.312
10.045
130.
9.620
140.
150.
160.
170.
9.429
9.498
9.336
9.225
180,
190.
200.
9.142
8.920
8.776
33.919
33.962
33.977
26.271
26.340
26.374
0.434
0.451
0,469
0.485
170.
180.
190.
200.
9.149
9.007
9.000
8.933
220.
240.
260.
280.
300.
350.
400.
450.
500.
8.515
8.409
8.239
8.040
7.862
7.555
7.073
6.402
5.895
0.518
0.550
0.580
0.610
0.640
0.711
0.778
0.841
0.900
0.946
8.720
8.500
8.109
8.064
7.967
5.728
26.436
26.482
26.522
26.553
26.582
26.670
26.748
26.844
26.969
27.038
220.
240.
260.
280.
300.
500.
544.
34.004
34.043
34.061
34.061
34.066
34.121
34,134
34.140
34.216
34.277
35
0—
SAL
110.
120.
STA 176
120 56.8W
34 54.6N
0.6N
120 43.4W
0—
50
Sm 177
35
6.8N
120 Ii.4.5W
0.482
0.515
0.548
0.578
0.608
0.638
0.904
0-.
45
SAL
0.
15.333
33.357
24.655
0.000
0.
14.717
33.464
24.871
0.000
10.
14.482
33.217
24.731
0.033
10.
14.721
33.465
24.871
0.031
13.725 33.210
13.225 33.353
12.794 33.378
24.883
25.095
25.199
0.064
0.093
0.122
0.458
0.891
20.
30.
40.
200.
500.
14.632
13.346
13.012
33,467
33.419
33.488
24.892
25.122
25.242
0.062
0.092
0.119
0.473
0.647
20.
30.
40.
200.
500.
STA 178
0.
10.
20.
30.
40.
50.
60.
70.
80.
90.
200.
500.
35
15.005
14.895
14.570
13.765
13.211
11.779
11.843
11.898
11.802
11.603
SIA 181
4.7N
120 48.9W
SAL
33.433
33.435
33,434
33.348
33.252
33.215
33.279
33.564
33.579
33.586
97
STA 180
35
1,7N
120 55.4W
D— 250
24.346
24.348
24.569
25.080
25.276
25.386
25.481
25.626
25.715
25.825
25.876
25.918
25.993
26.079
26.115
26.122
26.163
26.187
26.233
26.261
26.329
26.427
26.562
0.000
0.036
0.071
0.102
0.130
0.156
0.182
0,206
0.230
0.232
0.274
0.295
0.315
0.335
0.354
0,373
0.392
0.411
0.429
0.447
0,464
0.498
0.528
0,854
DELD
24.785
24.811
24.8'79
24.981
25.020
25.267
25.305
25.515
25.544
25.587
.
34 59.4N
D—
121
0.3W
0.000
0.032
0.063
0.093
0.123
0.152
0.179
0.204
0.229
0.253
0.469
0.850
D— 425
0.
10.
20.
30.
40.
50.
60.
70.
80.
90.
100.
110.
120.
130.
140.
150.
160.
170.
180.
190.
200.
220.
240.
500.
33.506
17.186
33.506
17.176
15.249 33.221
13.312 33.357
12.333 33.362
11.486 33.298
10.966 33.300
33.462
10.857
10.978 33.605
10,657 33.673
10.488 33.701
10.342 33.722
10.059 33.757
9.778 33.807
9.703 33.837
9.677 33.840
9.537 33.863
9.431 33.876
9.296 33.902
9.196 33.917
8.967 33.957
8.607 -34.011
8.050 34.074
STA 182
34 58.ON
121
3.2W
D— 493
24.457
24.456
24.486
24.595
24.831
25.097
25.334
25.527
25.623
25.724
25.855
26.009
26.108
26.151
26.193
26.251
26.320
26.329
26.381
26.410
26.438
26.468
26.511
26.533
26.574
26.609
26.716
26.807
26.909
0.000
0.035
0.070
0.104
0.136
0.167
0.194
0.220
0.244
0.268
0.290
0.311
0.330
0.349
0.368
0.386
0.403
0.420
0.437
0.454
0.470
0.502
0.533
0.563
0.593
0.622
0.692
0.757
0.817
0.872
SIGMA
0.
10.
20.
30.
40.
50.
60.
70.
80.
90.
100.
110.
120.
130.
140.
150.
160.
170.
180.
190.
200.
220.
240.
260.
280.
300.
350.
400.
500.
16.634
16.631
16.358
14.058
12.935
11.472
11.233
10.999
11.018
11.176
10.925
10.631
10.182
9.821
9.585
9.307
9.159
8.991
8.844
8.718
8.551
8.240
8.194
8.034
7.777
7.659
7.138
6.560
33.471
33.470
33.459
33.422
33.260
33.131
33.139
33.213
33.356
33.560
33.619
33.676
33.735
33.818
33.901
33.930
33.931
33.975
33.986
34.012
34.041
34.058
34.097
34.097
34.100
34.129
34.141
24.449
24.457
24.978
25.080
25.259
25.304
25.408
25.515
25.645
25.736
25.832
25.955
26.061
26.120
26.230
26.277
26.320
26.362
26.390
26.437
26.507
26.327
26.582
26.619
26.639
26.736
26.824
0.000
0.035
0.070
0.102
0.132
0.160
0.187
0.214
0.239
0.263
0.286
0.309
0.330
0.350
0.370
0.388
0.406
0.423
0.4.40
0.457
0.473
0.504
0.335
0.565
0.594
0.622
0.691
0.754
0.869
0.
10.
20.
30.
40.
50.
60.
70.
80.
90.
100.
110.
120.
130.
140.
150.
160.
170.
180.
190.
200.
220.
240.
260.
280.
300.
350.
400.
450.
500.
16.625
16.626
16.488
15.910
14.981
13.318
12.486
11.684
11.334
11.031
10.502
9..987
9.641
9.484
9.349
9.147
8.924
8.887
8,704
8.609
8.505
8.446
8.302
8.196
8.013
7.814
7.284
6.573
6.098
33.479
33.478
33.475
33.446
33.486
33,433
33.474
33.328
33.569
33.629
33.678
33.762
33.814
33.836
33.863
33.895
33.937
33.942
33.971
33.989
34.005
34.032
34.059
34.067
34.084
34.091
34.129
34.121
34.173
-
5Th 184
0,
10.
20.
30.
40.
50.
60.
70.
80.
90.
100.
110.
120.
130.
140.
150.
160.
170.
180.
190.
200.
220.
240.
260.
280.
300.
350.
400.
450,
500.
550.
560.
34 53.9N
17.060
17.055
17.033'
16.566
13.308
12.421
11.918
11.221
10.990
10.709
10.609
10.334
9.776
9.512
9.651
9.384
9.277
9.245
9.032
8.661
8.518
8.075
7.787
7.688
7.477
7.083
6.561
6.525
5.909
5.877
5.733
5.732
STA 190
0.
10.
20.
30.
40.
50.
60.
70.
80.
90.
100.
110.
120.
130.
140.
150.
160.
170.
180.
190.
200.
220.
240.
260.
280.
300.
350.
400.
450.
500.
550.
600.
650.
662.
33.298
33.297
33.258
32.952
32.942
32.965
33.046
33.139
33.320
33.378
33,550
33.445
33,574
33.647
33.661
33.758
33.829
33.886
33.911
33.941
33.959
33.970
33.993
34.015
34.010
34.070
34.153
34.136
34.192
34.245
34.245
34 44.ON
17.554
17.563
17.558
14.117
13.524
13.358
12.257
11.729
11.521
11.126
121 11.3W
SAL
33.299
3449.SN
STA 187
121 20.9W
1— 450
grin
24.218
24.218
24.222
24.301
24.769
24.935
25.047
25.238
25.352
25.542
25.604
25.785
25.798
25.942
25.976
26.031
26.123
26.184
26,263
26.341
26.386
26.467
26.519
26.551
26.599
26.650
26.768
26.838
26.904
26.952
27.012
27.012
121 31.9W
10.779
10.607
10.287
10.131
9.980
9.798
9.605
9.443
9.341
9.246
9.031
8.845
8.683
8.506
8.193
7.845
7.329
6.608
6.508
6.129
5.655
33.470
33.471
33.473
33.383
33.422
33.476
33.512
33.588
33.614
33.654
33.670
33.690
33.711
33.745
33.788
33.822
33.858
33.895
33.924
33.944
33.961
34.008
34.048
34.059
34.075
34.104
34.136
34.164
34.143
34.157
34.206
34.238
24.231
24.230
24.232
24,935
25.088
25.163
25.407
25.565
25.623
25.727
25.772
25.817
25.863
25.945
26.006
26.057
26.116
26.177
26,226
5.025
4.775
34.314
34.356
27.151
27.213
10.941.
0-. 570
26.258
26.287
26.358
26.419
26.453
26.493
26.563
26.640
26.736
26.819
26.844
26.932
27.016
0.000
0.
0.037
0.074
0.111
0.145
0.176
0.206
0.234
0.261
10.
0.286
0.3 11
0.334
0.356
0.377
0.398
0.418
0.438
0.456
0.474
0.491
0.508
0.541
0.572
0.602
0.631
0.660
0.728
0.790
0.850
0.907
0.961
0.972
0-' 670
0.000
0.037
0.074
0.109
0.138
0.167
0.194
0.219
0.243
0.266
0.289
0.311
0.332
0.354
0.374
0.394
0.413
0.432
0.450
0.468
0.486
0.520
0.553
0.585
0.617
0.647
0.719
0.787
0.851
0.913
0.971
1.02 6
1.07 6
1.087
20.
30.
40.
50.
60.
70.
80.
90.
100.
110.
120.
130.
140.
150.
160.
170.
180.
190.
200.
-220.
240.
260.
280.
300.
350.
400.
450.
500.
17.259
17.267
17.261
14.680
12.961
12.548
11.979
11.633
11,230
10.880
10.789
10.607
10.254
10.126
9.972
9.751
9.679
9.428
9.348
9.231
9.124
8.992
8.830
8.531
8.276
7.956
7.398
STA 192
0.
10.
20.
30.
40.
50.
60.
70.
80.
90.
100.
110.
120.
130.
140.
150.
160.
170.
180.
190.
200.
220.
240.
260.
280.
300.
350.
400.
500.
6.4.43
6.126
33.395
33.395
33.389
33.401
33.456
33.496
33.534
33.588
33.632
33.674
33.689
33.720
33.769
33.779
33.805
33.842
33.855
33.892
33.920
33,951
33.978
34.004
34.016
34.025
34.037
34.040
34.111
34.034
34.106
34 54.ON
24.24.4
24.242
24.239
24.830
25.227
25.338
25.476
25.583
25.691
25,786
25.814
25.870
25.969
25.999
26.046
26.112
26.133
26.204
26.238
26.281
26.320
26.361
26.396
26.450
26.498
26.548
26.685
26.755
26.853
0.000
0.037
0.074
0.108
0.137
0.164
0.190
0.215
0.238
0.261
C.283
0.326
0.346
0.366
0.385
0.404
0.423
0.441
0.459
0.476
0.510
0.543
0.575
0.607
0.637
0.709
0.776
0.838
0.897
121 24.3W
0-' 454
17.263
33.396
24,244
0.000
17.266
17.257
13.360
12.749
12.450
11.932
11.654
11.163
11.018
10.664
10.404
10.149
9.973
9.753
9.584
9,497
9.357
9.260
9.187
9.050
8.860
8.622
8.465
8.322
8.179
7.870
7.312
33.396
33.396
33.307
33.405
33.505
33.579
33.614
33,642
33.661
33.705
33.741
33.785
33.815
33.863
33.897
33.912
33.939
33.956
33.971
33.991
34.027
34.057
34.078
34.094
34.104
34.125
34.161
24.243
24.245
25.032
25.229
25.365
25.520
25.599
25.711
25.752
25.849
25.921
25.999
0.037
0.074
0.108
0.137
0.163
0.189
0.213
0.237
0.259
0.281
0.303
0.323
0.343
0.363
0.381
0.400
0.418
0.435
0.453
0.470
0.503
0.535
0.567
0.597
0.627
0.700
0.768
26.127
26.182
26.207
26.252
26.280
26.304
26.342
26.400
26.461
26.501
26.535
26.736
0.895.
34 58.8N
STA 195
121 15.1W
0.
17.039
33.295
10.
20.
30.
40.
50.
60.
70.
80.
90.
17.04.4
33.296
17.034
16.678
14.583
13.112
12.166
12.446
11.688
11,396
11.132
10.655
10.264
10.061
9.903
9.569
9.373
9.294
9.136
8.947
8.837
8.563
8.260
7.876
7.537
7.264
6.809
6.195
5.887
5.646
5.501
5.433
33.294
33.261
33.280
33.385
33.325
33.545
33.571
33.611
33.650
33.687
33.716
33.770
33.773
33.803
33.848
33.863
33.890
33.930
33.947
33.990
34.022
34.041
34.025
34.029
34.038
34.037
34.075
34.124
34.179
34.236
100.
110.
120.
130.
140.
150.
160.
170.
180.
190.
200.
220.
240.
260.
280.
300.
350.
400.
450.
500.
550.
586.
STA 201
0.
10.
20.
30.
40.
50.
200.
500.
35 10.4N
14.109
13.851
13.833
13.662
13.640
13.282
24.219
24.219
24.220
24.278
24.759
25.142
25.280
25.396
25.559
25.644
25.722
25.836
25.926
26.003
26.032
26.111
26.178
26.202
26.250
26.310
26.341
26.417
26.489
26.561
26.598
26.640
26.710
26.790
26.859
26.927
26.988
27.041
120 51.7W
33.372
33.388
33.393
33.424
33.430
33.421
24.928
24.995
25.002
25.061
25.070
25.136
D-. 595
0.000
0.037
0.074
0.111
0.146
0.176
0.204
0.230
0.256
0.279
0.303
0.325
0.346
0.367
0.387
0.406
0.425
0.443
0.461
0.479
0.496
0.529
0.561
0.591
0.621
0.649
0.719
0,784
0.845
0.904
0.960
0.997
B-.
58
0.000
0.030
0.060
0.089
0.118
0.147
0.477
0.835
STA 198
0.
10.
20.
30.
40.
50.
60.
70.
80.
90.
100.
110.
120.
130.
140.
150.
160.
170.
180.
190.
200.
220.
240.
260.
280.
300.
350.
400.
450.
500.
16.497
16.486
16.185
15.595
13.867
13.285
12.842
11.907
11.003
11.339
11.316
10.965
10.545
10.243
9.771
9.565
9.387
9.209
8.978
8.759
8.618
8.357
8.126
7.873
7.698
7.374
6.921
6.411
5.996
STA 202
0.
10.
20.
30.
40.
50.
200.
300.
121
35
33,476
33.476
33.466
24.484
24.487
24.548
33.446
24.666
33.333
33.292
33.320
33.163
33.218
33.507
33.587
33.619
33.672
33.718
33,799
33.832
33.857
33.894
33.944
33.984
34.012
34.057
34.081
34.094
34.115
34.090
34.105
34.116
34.183
24.949
25.036
25.145
25.203
25.411
25.574
25.640
25.728
25.843
25.931
26.074
26.134
26.183
26.241
26.317
26.382
26.426
26.501
26.555
26.603
26.645
26.672
26.747
26.824
26.930
120 55.5W
SAL
33.477 25.024
33.479 25.109
33.485 25.157
33.489 25.170
33.487 25.249
33.482 25.324
35 15.3N
14.041
13.634
13.421
13.374
12.969
12.570
3.7W
D— 493
DELD
0.000
0.035
0.069
0.103
0.134
0.164
0.192
0.220
0.247
0.271
0.295
0.318
0.341
0.362
0.382
0.401
0.420
0.438
0.456
0.472
0.489
0.520
0.551
0.580
0.608
0.636
0.704
0.767
0.826
0.882
B—
57
0.000
0.029
0.057
0.086
0.113
0.141
0.460
0.857
STA 205
35
110.
120.
130.
140.
150.
160.
170.
180.
190.
200.
220.
240.
260.
280.
300.
350.
400.
450.
500.
15.968
15.401
15.121
14.777
14.466
13.130
12.933
12.292
12.021
11.635
11.316
10.843
10.468
10.235
10.053
9.774
9.541
9.195
8.973
8.703
8.554
8.364
7.890
7.648
7.372
7.289
6.809
6.714
6.251
5.950
544.
5.695
0.
10.
20.
30.
40.
50.
60.
70.
80.
90.
100.
STA 211
17.703
17.364
14.272
13.027
12.260
11.912
11.729
11.448
11.160
10.949
10.758
10.578
10.359
10.198
10.032
9.876
9.734
170.
9.575
180.
190.
200.
220.
240.
260.
280.
300.
350.
400.
450.
9.466
9.401
9.289
9.045
8.783
8.516
8.322
8.068
7.332
6.923
6.600
5.786
5.751
-
500.
502.
121
33.281
33.269
33.246
33.219
33.185
33.406
33.422
33.444
33.494
33.549
33.591
33.626
33.665
33.712
33.749
33.796
33.845
33.867
33.880
33.895
33.912
33.941
33.987
33.990
33.999
34.018
34.052
34.177
34.199
34.201
34.248
34 59.1W
10.
20.
30.
40.
50.
60.
70.
80.
90.
100.
110.
120.
130.
140.
150.
160.
0.
9.0W
7.7W
550
24.455
24.572
24.616
24.670
24.710
25.155
25.206
0.000
0.034
0.068
0.101
0.134
0.164
0.192
0.219
0.245
0.270
0.294
0.317
0.339
0.360
0.381
0.401
0.420
0.438
0.456
0.474
0.491
0.524
0.556
0.586
0.615
25.347
25.438
25.552
25.643
25.756
25.852
25.929
25.989
26.071
26.149
26.221
26.267
26.321
26.358
26.410
26.517
26.554
26.601
26.627
26.720
26.832
26.910
26.950
27.019
121 27.6W
33.379
33.400
33.208
33.470
33.502
33.553
33.602
33.621
33.647
33.666
33.690
33.718
33.745
33.771
33.811
33.836
33.869
33.886
33.912
33.926
33.947
33.990
34.045
34.067
34.092
34.074
34.094
34.170
34.202
34.133
34.140
24.126
24.222
24.768
25.224
25.398
25.504
25.576
25.643
25.715
25.768
25.820
25.874
25.932
25.981
26.040
26.086
26.135
26.175
26.213
26.234
26.269
26.342
26.427
26.485
26.534
26.558
26.681
26.797
26.867
26.917
26.927
0.644
0.712
0.776
0.836
0.893
0.940
D- 497
0.000
0.037
0.073
0.102
0.129
0.154
0.179
0.203
0.226
0.249
0.271
0.292
0.313
0.334
0,354
0.374
0.393
0.412
0.430
0.448
0.466
0.500
0.533
0.565
0.596
0.626
0.697
0.763
0.824
0.883
0.885
STA 208
0.
10.
20.
30.
40.
50.
60.
70.
80.
90.
100.
110.
120.
130.
140.
150.
160.
170.
180.
190.
200.
220.
240.
260.
280.
300.
350.
400.
450.
500.
550.
600.
620.
35
17.665
17.278
17.236
17.218
16.263
13.721
12.725
12.401
12.333
11.738
11.382
11.138
10,763
10,451
10.169
9.889
9.684
9.537
9.279
9.140
8.918
8.539
8.167
7.895
7.512
7.367
7.060
6.359
5.816
5.835
5.260
5.107
5.030
STA 401
0.
10.
20.
30.
40.
50.
60.
70.
200.
500.
121 18.7W
SAL
33.369 24.127
33.357 24.210
33.356 24.220
33.355 24.223
33.423 24.497
33.381 25.016
33.374 25.210
33.460 25.339
33.535 25.410
33.474 25.475
33.545 25.596
33.615 25.694
33.665 25.800
33.688 25.873
33.719 25.945
33.747 26.014
33.784 26.078
33.817 26.127
33.866 26.208
33.896 26.253
33.941 26.323
33.995 26.425
34.002 26.487
34.012 26.535
34.022 26.599
34.057 26.647
34.093 26.719
34.074 26.798
34.070 26.863
34.165 26.936
34.150 26.994
34.199 27.051
34.224 27.079
3.5W
34 25.2W
17.193
17.151
15.035
14.378
14.154
13.866
13.549
13.058
120 27.1W
33.508
33.505
33.470
33.469
33.490
33.500
33.503
33.534
24.346
24.353
24.807
24.947
25.010
25.078
25.145
25.268
D— 626
0.000
0.038
0.075
0.112
0.148
0.180
0.209
0.236
0.262
0.287
0.312
0.335
0.358
0.380
0.401
0.421
0.441
0.460
0.479
0.497
0.514
0.547
0.579
0.610
0.639
0.668
0.736
0.801
0.862
0.920
0.976
1.028
1.048
0—
80
0.000
0.036
0.069
0.100
0.130
0.160
0.188
0.216
0.495
0.885
STA 402
0.
10.
20.
30.
40.
50.
60.
70.
80.
90.
100.
110.
120.
130.
140.
150.
160.
170.
180.
190.
200.
220.
240.
260.
280.
300.
500.
34 20.6N
16.978
16.721
14.962
13.631
13.202
12.621
12.290
12.022
11.692
11.595
11.423
11.119
10.775
10.534
10.243
10.129
10.037
9.998
9.795
9.642
9.560
8.956
8.761
8.450
8.162
7.720
STA 406
120 27,1W
33.50].
24.39].
33.489
33.464
33.494
33.506
33.554
33.581
33.595
33.623
33.631
33.642
33.672
33.712
33.744
33.788
33.810
33.827
33.835
33.874
33.898
33.902
33.986
34.020
34.070
34.090
34.124
24.442
24.818
25.121
25.217
25.369
25.454
25.515
25.599
25.623
25.664
25.742
25.834
25.901
25.986
26.023
26.051
26.064
26.129
26.173
26.189
26.353
26.410
26.497
26.557
26.649
34 13.1N
120 42.0W
D— 320
0.000
0.035
0.069
0.099
0.127
0.154
0.180
0.205
0.229
0.253
0.277
0.300
0.322
0.344
0.364
0.385
0.404
0.424
0.443
0.462
0.480
0.516
0.549
0.580
0.611
0.639
0.870
700
18.4N
S'IA 403
0.
10.
20.
30.
40.
50.
60.
70.
80.
90.
100.
110.
120.
130.
140.
150.
160.
170.
180.
190.
200.
220.
240.
260.
280.
300.
350.
400.
500.
16.289
15.944
14.060
13.172
12.594
12.305
12.035
11.876
11.724
11.587
11.431
11.298
11.191
10.870
10.373
10.104
9.741
9.447
9.190
9.087
8.937
8.737
8.515
8.107
7.947
7.607
6.965
6.625
STA 409
34
120 31.2W
0— 433
24.529
24.589
25.014
25.224
25.376
25.443
25.512
25.554
25.589
25.623
25.663
25,698
25.716
25.804
25.941
26.026
26.127
26.214
26.282
26.309
26.352
26.388
26.487
26.554
26.591
26.665
26.779
26.859
0.000
0.034
0.066
0.095
0.122
0.148
0.173
0.197
0.222
0.245
0.269
0.292
0.315
0.338
0.359
0.380
0.399
0.418
0.436
0.453
0.470
0.503
0.535
0.566
0.595
0.624
0.691
0.752
0.859
33.473
33.449
33.470
33.507
33.556
33.570
33.594
33.609
33.618
33.629
33.643
33.657
33.655
33,695
33.759
33.809
33.861
33.910
33.943
33.957
33.981
33.987
34.070
34.076
34.092
34.123
34.154
34.197
8.4N
120 51.9W
0-1000
24.035
24.036
24.036
24.076
24.214
24.864
25.125
25.245
25.369
25.460
25.542
25.676
25.805
0.000
0.039
0.078
0.116
0.154
0.188
0.218
0.246
0.273
0.299
0.324
0.348
0.370
100.
110.
120.
16.821
16.343
15.156
14.015
12.382
12.073
11.817
11.484
11.171
10.904
10.848
10.788
10.459
130.
10.311
33.750
25.945
0.340
130.
10.421
33.733
25.913
0.392
140.
150.
160.
9.932
9.813
9.558
9.406
9.322
190.
200.
220.
240.
260.
280.
300.
350.
400.
450.
500.
550.
9.250
9.088
8.892
8.554
8.375
8.088
7.803
7.180
6.479
5.921
5.866
5.676
33.913
33.979
34.011
34.051
34.066
34.088
34.087
34.109
34.146
34.189
34.263
34.299
26.054
26.084
26.151
26.204
26.228
26.249
26.326
26,383
26.467
26.506
26.566
26.608
26.714
26.838
26.944
27.010
27.062
0.360
0.379
0.398
0.417
0.435
0.453
0.470
0.504
0.536
0.567
0.597
0.627
0.697
0.760
0.819
0.873
0.925
140.
150.
160.
170.
180.
190.
200.
220.
240.
10.079
10.020
9.546
9.501
9.451
9.409
9.350
8.815
6.662
8,275
7.985
7.954
7,376
6.919
6.369
5.974
33.790
33.809
33.901
33.910
33.919
33.926
33,939
34,022
34.039
34.073
34.116
34.134
34.140
34.191
34.211
34.246
34.266
26.015
26.041
26.191
26.206
26.221
26.233
26.253
26.403
26.441
26.527
26.604
26.623
26,711
26.815
26.856
26.932
26.998
0.412
0.432
170.
180.
33.808
33,820
33.851
33.888
600.
650.
5.462
5.194
34.332
0.975
1.022
34.294
34,309
34.328
34.332
27.1.5
1.041
1.090
5.068
5.712
5.295
5.108
5.097
27.053
688,
27.113
27.166
27,190
27.153
27.157
1.138
1.143
0.
10.
20.
30.
40.
50.
60.
70.
80.
90.
33.477
33.458
33.465
33.378
33,333
33.336
33.424
33.483
33.623
33.667
33.682
33.690
33.739
24.409
24.506
24.776
24.953
25.244
25,306
25.422
25.529
25.694
25.777
25.798
25.815
25.911
0.000
0.035
0.068
0.099
0.128
0.155
0,181
0.206
0.230
0.253
0.275
0.297
0.319
10.
20.
30.
40.
50.
60.
70.
80.
90.
100.
110.
120.
18.658
18.662
18.662
18.470
17.662
14.158
13.305
13.033
12.509
12.084
11.792
11.271
10.797
33.567
33.570
33.570
33.560
33.482
33.301
33.413
33.499
33.526
33.538
33.574
33.622
33.679
33.901
34.358
34.370
1.056
0.
260:
280.
300.
350.
400,
450.
500,
550.
600.
650.
700.
706.
0451
0.470
0.488
0.506
0.524
0.558
0.590
0.622
0.651
0.680
0.750
0.814
0.875
0.934
0.989
STA 411
0.
10.
20,
30.
40.
50.
60.
70.
80.
90.
100.
110.
120.
130.
140.
150.
160.
170.
180.
190.
200.
220.
240.
260.
280.
300.
350.
400.
450.
500.
550.
600.
650.
682.
STA 417
0.
10.
20.
30.
40.
50.
60.
70.
80.
90.
100.
110.
120.
130.
140.
150.
160.
170.
180.
190.
200.
220.
240.
260.
280.
300.
350.
400.
450.
500.
550.
600.
650.
654.
34 10.ON
18.300
18.298
18.294
18.284
17.459
16.285
14.813
13.277
12.698
12.172
11,630
11.024
10.726
10.376
9.910
9.631
9.486
9.222
9.044
9.047
8.795
8.501
8.232
7.961
7.662
7.405
6.923
6.725
6.513
6.264
6.022
5.753
5.530
5.441
5.336
D—1000
24.109
24.110
24.112
24,119
24.283
24.522
24.763
24.966
25.177
25.369
25,540
25.696
25.785
25.884
26.016
26.101
26.146
26.232
26.297
26.338
26.381
26.449
26.540
26.571
26.613
26.646
26.758
26.841
26.898
26.953
27.001
27.057
27.103
27.121
0.000
0.038
0.076
0.115
0.152
0.187
0.220
0.251
0.280
0.308
0.333
0.357
0,379
0.401
0.422
0.441
0.460
0.479
0.496
0.513
0.530
120 47.3W
0— 665
33.548
33.549
33.550
33.556
33.508
33.462
33.351
33.200
33.325
33,442
33.532
33.591
33.638
33.686
33.753
33.803
33.830
33.886
33.932
33.986
33.990
34.017
34.082
34.070
34.068
34.063
34.119
34.191
34.228
34.256
34.278
34.305
34.329
34.338
34 19.7N
15.572
15.419
15.101
14.453
13.375
12.862
12.509
12.056
11.684
11.091
10.882
10.676
10.405
10.132
9.960
9.666
9.435
9.232
9.001
8.752
8.578
8.259
8.193
7.675
7.446
7.346
6.814
6.683
6.317
6.078
5.750
5.399
5.362
8.1W
121
33.453
33.461
33.468
33.441
33.270
33.284
33.313
33.404
33.460
33.523
33,594
33.630
33.669
33.722
33.746
33.792
33.844
33.882
33.917
33.960
33.984
34.016
34.077
34.051
34.076
34.106
34.108
34.207
34.227
34.252
34.260
34.291
34.330
24.676
24.716
24.791
0.563
0.594
0.623
0.653
0.681
0.747
0.811
0.870
0.927
0.982
1.034
1.083
1.114
18.813
18.785
18.758
18.715
14.267
13.371
12.849
12.156
11.561
11.073
10.847
10.606
10.159
10,061
9.863
9.696
9.476
9.337
9.199
9.084
8.725
8.432
8.331
8.131
7.552
7.549
7.217
6.687
6.384
6.156
5.996
5.799
5.496
0.
10.
20.
30.
40.
50.
60.
70.
80.
90.
100.
110.
120.
130.
140.
150.
160.
170.
180.
190.
200.
220.
240.
260.
280.
300.
350.
400.
450.
500.
550.
600.
642.
STA 419
25.000
25.114
25.204
0.000
0.033
0.065
0.096
0.126
0.155
0.183
10.
20.
30.
40.
50.
60.
25.361
0.210
70.
25.474
25.631
25.724
25.788
25.866
25.954
26.002
26.087
26.165
26.227
26.292
26.365
26.410
26.484
26.542
26.598
26.651
26.688
26.764
26.860
26.923
26.974
27.021
27.089
27.122
0.236
0.261
0.284
0.306
0.328
0.349
0.369
0.389
0.408
0.426
0.444
0.461
0.477
0.509
0.540
0.569
0.598
0.625
0.692
0.755
0.813
0.869
0.923
0.974
1.022
80.
27.127
1.026
24.910
34 15.1N
STA 414
90.
100.
110.
120.
130.
140.
150.
160.
170.
180.
190.
200.
220.
240.
260.
280.
300.
350.
400.
450.
500.
-
33.538
33.538
33.542
33.546
33.166
33.313
33.392
33.426
33.469
33.529
33.602
33.638
33.722
33.741
33.772
33.797
33.835
33.887
33.960
33.977
34.024
34.057
34.054
34.064
34.067
34.115
34.165
34.217
34.239
34.266
34.287
34.301
34.308
34 23.4N
16.224
16.080
15.157
13.424
12.984
12.622
12.259
12.096
11.782
11.602
11.342
11.216
10.876
10.778
10.368
10.198
9.869
9.669
9.493
9.361
9.284
8.854
8.370
8.050
7.963
7.716
7.281
6.675
6.295
0.
120 56.9W
0—1000
23.974
23.981
23.991
24.005
24.737
25.035
25.199
25.360
25.504
25.639
25.736
25.806
25.949
25.980
26.038
26,086
26.151
26.215
26.294
26.326
26.419
26.490
26.503
26.541
26.629
26.667
26.753
26.867
26.924
26.975
27.012
27.048
27.090
0.000
0.039
0,079
0.118
0.154
0.185
0.214
0.241
0.266
0.291
0.314
0.336
0.358
0.378
0,398
0.418
0.437
0.455
0.473
0.490
0.507
0.539
0.570
0.600
0.629
0.657
0.725
0.787
0.845
0.901
0.955
1.007
1.049
120 40.3W
0— 460
33.482
33.480
33.479
33.512
33.529
33.555
33.563
33.564
33.598
33.616
33.646
33.661
33.683
33.692
33.754
33.781
33.835
33.866
33.893
33.926
33.941
33.993
34.014
34.062
34.095
34.122
34.135
34.163
34.188
24.551
24.582
24.788
25.178
25.279
25.370
25.446
25.478
25.563
25.610
25.681
25.716
25.794
25.818
25.938
25.989
26.086
26.144
26.193
26.241
26.265
26.374
26.466
26.552
26.590
26.648
26.721
26.826
26.896
0.000
0.034
0.066
0.097
0.124
0.150
0.176
0.202
0.226
0.251
0.274
0.297
0.320
0.342
0.363
0.383
0.403
0.422
0.441
0.459
0.477
0.511
0.544
0.574
0.604
0.632
0.701
0.765
0.826
0.882
34 25.ON
STA 420
120 35.9W
0— 270
34 26.6N
STA 421
120 32.6W
0—
0.
17.179
33.497
24.341
0.
16.971
33.490
24.385
0.000
10.
20.
30.
40.
16.449
15.578
14.058
13.454
33.482
33.469
33.489
33.504
24.500
24.687
25.029
25.165
0.036
0.069
0.100
0.129
10.
20.
30.
16.966
15.700
14.956
13.833
33.492
33.486
33.483
33.496
24.387
24.673
24.834
25.081
0.036
0.070
0.102
0.133
50.
60.
70.
80.
12.874
12.751
12.393
12.102
33.548
33.548
33.583
33.585
25.315
25.339
25.436
25.493
0.156
0.183
0.209
0.234
50,
60.
70.
80.
13.609
90.
100.
110.
120.
130.
140.
150.
160.
170.
180.
190.
200.
220.
240.
260.
500.
11.713
11.270
10.968
10.868
10.601
10.403
10.239
10.101
9.809
9.712
9.528
9.407
9.243
8.963
8.644
33.609
33.645
33.685
33.698
33.747
33.759
33.787
33.801
33.849
33.865
33.896
33.915
33.934
33.975
34.017
25.584
25.694
25.780
25.807
25.892
25.936
25.986
26.020
26.107
26.136
26.190
26.225
26.266
26.343
26.426
0.259
0.283
0.305
0.327
0.349
0.370
0.391
0.411
0.430
0.450
0.468
0.486
0.522
0.557
0.590
0.903
90.
200.
500.
11.844
33.509
33.515
33.522
33.556
33.619
25.138
25.172
25.205
25.357
25.567
0.161
0.189
0.217
0.244
0,270
STA 422
0.
10.
20.
200.
500.
34 28.4N
16.308
16.147
15.350
120 29.8W
33.471
33.476
33.486
2.524
24.565
24.750
0—
32
0.000
0.034
0.067
0.505
0.940
40.
13463
13.325
12.689
STA 423
0.
10.
20.
30.
200.
0.498
0.925
34 31.7N
16.375
16.248
15.238
14.270
120 34.6W
33.495
33.490
33.485
33.485
24.527
24.552
24.774
24.982
0—
40
0.000
0.034
0.067
0.098
0.453
34 30.3N
STA 424
0.
10.
20.
30.
40.
50.
60.
70.
80.
16.719
16.659
14.162
13.667
13.332
12.695
12.604
12.473
12.261
120 38.2W
33.494
33.498
33.492
33.504
33.519
33.555
33.558
33.5U
33.576
24.447
24.464
25.010
25.121
25.201
25.355
25.375
25.405
25.456
200.
500.
STA 430
34 20.1N
121
0.5W
D—
34 24.6N
STh 427
85
0.000
0.035
0.067
0.096
0.124
0:151
0.177
0.203
0.229
0.455
0.857
0.
10.
20.
30.
40.
50.
60.
70.
80.
90.
100,
110.
120.
130.
140.
150.
160.
170.
180.
190.
200.
220.
240.
260.
280.
300.
350.
400.
450.
500.
550.
600.
634.
16.353
16.280
15.817
15.226
14.930
14.080
12.818
12.082
11.613
11.140
10.725
10.279
10.055
9.873
9.604
9.256
9.209
9.077
8.813
8.698
8.568
8.399
8.173
7.934
7.793
7.554
7.077
6.735
6.404
6.252
5.827
5.618
5.284
STA 431
D-.1000
120 50.5W
SAL
33.435
33.421
33.440
33.464
33.470
33.433
33.412
33.430
33.489
33.544
33.628
33.697
33.735
33.765
33.803
33.844
33.872
33.888
33.946
33.964
33.979
34.012
34.034
34.057
34.061
34.066
34.094
34.180
34.219
34.262
34.261
34.298
34.312
34 25.2N
24.486
24.492
24.612
24.761.
24.830
24.982
25.221
25.377
25.510
25.639
25.778
25.909
25.977
26.031
26.106
26.194
26.223
26.257
26.344
26.376
26.408
26.460
26.511
26.565
26.589
26.627
26.716
26.831
26.906
26.960
27.013
27.068
27.119
121
3.8W
D— 830
0.000
0.035
0.068
0.101
0.133
0.163
0.192
0.219
0.245
0,269
0.292
0.314
0.334
0.354
0.374
0.393
0.411
0.429
0.446
0.463
0.479
0.511
0.543
0.573
0.602
0.631
0.700
0.764
0.824
0.881
0.935
0.986
1.020
D—1000
SIC.MA
0.
10.
20.
30.
40.
50.
60.
70.
80.
90.
100.
110.
120.
130.
140.
150.
160.
170.
180.
190.
200.
220.
240.
260.
280.
300.
350.
400.
450.
500.
550.
600.
630.
€58.
17.869
17.880
17.868
16.054
14.549
13.189
12.475
12.228
11.805
11.444
33.529
33.529
33.528
33.380
33.265
33.185
33.218
33.291
33.398
11.061.
10.552
10.308
9.907
9.816
9.657
9.386
9.097
8.813
8.726
8.560
8.415
8.177
7.906
7.720
7.571
7.267
6.849
6.482
6.245
5.907
5.561
5.351
5.314
260.
280.
300.
350.
400.
16.402
15.634
13.682
12.255
11.680
11.864
11.323
11.043
10.495
10.117
9.927
9.567
9.381
9.271
9.008
8.897
8.770
8.620
8.327
8.053
7.797
7.563
7.319
6.871
6.605
450,
6.363
500.
550.
600.
6.186
5.822
5.464
33.364
33.364
33.364
33.371
33.295
33.132
33.125
33.199
33.432
33.487
33.561
33.650
33.696
33.752
33.809
33.839
33.870
32.916
33.929
33.956
33.976
34.013
34.030
34.053
34.074
34.081
34.145
34.210
34.234
34.258
34.287
34.290
650.
676.
4.888
4.757
34.282
34.305
33.577
33,633
33.658
33.715
33,761
33.789
33.857
33.890
33.935
33.950
33.973
34.002
34.022
34.050
34.065
34.095
34.146
34.197
34.218
34.261
34.270
34.302
24.200
24.197
24.199
24.512
24.754
24.972
25.138
25.242
25.404
25.564
25.679
25.812
25.874
25.987
26.038
26.086
26.183
26.256
26.336
26.361
26.404
26.449
26.502
26.564
26.603
26.648
26.731
26.829
26.895
26.960
27.010
27.078
0.000
0.037
0.075
0.111
0.144
0.175
0.204
0.232
0.258
0.283
0.307
0.330
0.351
0.372
0.392
0.412
0.431
0.449
0.466
0.483
0.500
0.563
0.593
0.623
0.651
0.720
0.783
0.844
0.901
0.955
1.006
240..
34.327
34.329
27.123
27.129
1.035
1.062
33.518
0.
10.
20.
30.
40.
50.
60.
70.
80.
90.
100.
110.
120.
130.
140.
150.
160.
170.
180.
190.
,
200.
220.
16.437
16.441
16.44.4
0.000
0.035
0.071
0.106
0.141
0.173
0.203
0.231
0.258
0.283
0.307
0.329
0.351
24.412
24.411
24.410
24.426
24.541
24.832
25.108
25.273
25.419
25.562
25.669
25.835
25.936
26.116
26.170
26.212
26.290
26.318
26.359
26.397
26.472
26.526
26.582
26.632
26.673
26.785
26.872
26.923
26.965
27.034
27.080
0.391
0.410
0.428
0.446
0.463
0.480
0.497
0.529
0.559
0.589
0.618
0.646
0.712
0.773
0.832
0.888
0.941
0.992
27.141
27,174
1.040
0.371.
1.065
34 29.5N
STA 434
0.
10.
20.
30.
40.
50.
60.
70.
80.
90.
100.
110.
120.
130.
140.
150.
160.
170.
180.
190.
200.
220.
240.
260.
280.
300.
350.
400.
450.
500.
550.
600.
650.
672.
16.459
16.462
16.460
16.305
14.529
13.484
12.399
11.789
11.449
11.016
10.676
10.517
10.207
9.844
9.644
9.363
9.228
9.026
8.776
8.660
8.545
8.376
8.223
8.005
7.771
7.608
7.224
6.649
6.076
5.914
5.641
5.351
5.092
5.004
STA 438
0.
10.
20.
30.
40.
200.
500.
33.407
33.407
33.406
33.386
33.225
33.321
33.364
33.460
33.510
33.580
33.633
33.660
33.711
33.763
33.801
33.863
33.892
33.924
33.958
33.977
33.989
34.052
34.071
34.092
34.096
34.121
34.171
34.124
34.134
34.212
34.263
34.292
34.328
34.336
34 41.5N
14.975
14.894
14.324
14.045
13.983
120 54.4W
24.440
24.439
24.439
24.460
24.727
25.018
25.265
25.455
25.557
25.689
25.791
25.839
25.932
26.034
26.097
26.191
26.236
26.294
26.359
26.392
26.419
26.495
26.533
26.582
26.619
26.663
26.756
26.799
26.882
26.963
27.037
27.096
27,154
27.171
120 41.3W
33.417
33.448
33.494
33.502
33.300
24.779
24.820
24.977
25.042
25.053
D— 730
0.000
0.035
0.070
0.105
0.139
0.170
0.198
0.224
0.249
0.273
0.295
0.317
0.339
0.359
0.378
0.397
0.415
0.433
0.450
0.467
0.483
0.515
0.546
0.575
0.605
0.633
0.699
0.763
0.824
0.880
0.934
0.984
1.032
1.052
0—
45
0.000
0.032
0.062
0.092
0.121
0.462
0.890
STA 437
0.
10.
20.
30.
40.
50.
60.
34 35.ON
16.207
16.209
16.212
14.761
13.437
13.016
12.564
120 42.5W
33.490
33.490
33.491
33.458
33.512
33.529
33.560
24.562
24.561
24.561
24.857
25.175
25.272
25.385
200.
500.
STA 439
0.
10.
20.
30.
40.
50.
60.
70.
80.
200.
500.
34 39.ON
16.308
16.284
13.969
13.818
13.047
12.899
12.687
12.413
11.977
120 46.4W
33.490
33.488
33.492
33.497
33.531
33.541
33.553
33.571
33.596
24.538
24.543
25.050
25.086
25.267
25.304
25.356
25.422
25.525
D—
65
0.000
0.034
0.068
0.101
0.130
0.157
0.184
0.459
0.863
0—
92
0.000
0.034
0.066
0.095
0.123
0.150
0.176
0.202
0.228
0.462
0.882
STA 442
0.
10.
20.
30.
40.
50.
60.
70.
80.
90.
100.
110.
120.
130.
140.
150.
160.
170.
180.
190.
200.
220.
240.
260.
280.
300.
350.
400.
450.
500.
550.
600.
642.
STA 446
0.
10.
20.
30.
40.
50.
60.
70.
80.
90.
100.
110.
120.
130.
140.
150.
160.
170.
180.
190.
200.
220.
240.
260.
280.
300.
350.
400.
450.
500.
550.
600.
624.
34 34.2N
16.460
16.464
16.463
14.921
12.506
12.044
12.128
11.151
11.362
10.781
10.615
10.476
10.230
9.866
9.582
9.436
9.290
9.134
8.879
8.690
8.607
8.447
8.369
7.955
7.832
7.716
7.233
6.551
6,301
5.915
5.633
5.352
5.114
33.446
33.448
33.447
33.264
33.086
24.470
24.471
D-. 660
24.673
25.030
25.220
25.331
25.516
25.577
25.765
25.817
25.868
25.939
26.042
26.131
26.184
26.254
26.312
26.361
26.386
26.407
26.458
26.508
26.571
26.607
26.635
26.730
26.793
26.864
26.959
27.036
27.101
27.150
0.000
0.035
0.069
0.104
0.135
0.163
0.190
0.216
0.240
0.263
0.285
0.307
0.328
0.348
0.368
0.386
0.404
0,422
0.439
0.456
0.472
0.504
0.535
0.566
0.595
0.623
0.691
0.756
0.818
0.875
0.929
0.979
1.019
121 10.8W
0-. 900
33.218
33.382
33.388
33.516
33.624
33.654
33.688
33.725
33.778
33.831
33.868
33.928
33.970
33.981
33.975
33.986
34.020
34.067
34.068
34.091
34.106
34.138
34.100
34.149
34.206
34.261
34.299
34.326
34 34.7N
16.377
16.338
16.294
16.037
13.741
12.378
11.967
11.394
10.937
10.654
10.253
10.112
9.925
9.903
9.590
9.274
9.136
8.940
8.908
8.817
8.732
8.308
8.080
7.913
7.630
7.484
6.778
6.580
6.216
5.881
5.126
5.187
4.982
120 57.8W
33.276
33.275
33.273
33.259
33.205
33.038
33.293
33.289
33.413
33.483
33.550
33.656
33.717
33.755
33.818
33.880
33.889
33.921
33.931
33.956
33.970
34.009
34.035
34.085
34.117
34.123
34.115
34.146
34.170
34.201
34.196
34.325
34.333
24.469
24.358
24.367
24.375
24.424
24.876
25.017
25.292
25.395
25.573
25.678
25.799
25.905
25.984
26.018
26.119
26.219
26.248
26.304
26.317
26.352
26.376
26.471
26.526
26.590
26.657
26.683
26.774
26.825
26.892
26.959
27.046
27.141
27.171
0.000
0.036
0.072
0.107
0.141
0.171
0.199
0.225
0.251
0.274
0.297
0.319
0.339
0.359
0.379
0.397
0.415
0.433
0,450
0.467
0.484
0.516
0.547
0.577
0.606
0.633
0.700
0.763
0.823
0.880
0.934
0.982
1.004
STA 445
0.
10.
20.
30.
40.
50.
60.
70.
80.
90.
100.
110.
120.
130.
140.
150.
160.
170.
180.
190.
200.
220.
240.
260.
280.
300.
350.
400.
450.
500.
550.
600.
648.
STA 449
0.
10.
20.
30.
40.
50.
60.
70.
80.
90.
100.
110.
120.
130.
140.
150.
160.
170,
180.
190.
200.
220.
240.
260.
280.
300.
350.
400.
450.
500.
550.
598.
34 29.9N
16.982
16.982
16.963
15.659
14.665
11.905
11.660
11.522
10.789
10.508
10.447
9.924
9.729
9.569
9.309
9.157
9.018
8.910
8.792
8.695
8.474
8.212
8.023
7.843
7.620
7,525
7.128
6.672
6.302
6.062
5.529
4.995
4.895
33.486
33.487
33.484
33,439
33.467
33.049
33.084
33.255
33.332
33.380
33.538
33.580
33.703
33.776
33.806
33.894
33.938
33.951
33.962
33.987
34.012
34.042
34.070
34.097
34.123
34.139
34.171
34.188
34.236
34.259
34.243
34.234
34.267
34 39.2N
16.442
16.378
14.876
14.285
13.338
12.738
12.543
11.779
11.262
10.828
10.570
10.178
10.050
9.818
9.558
9.355
9.133
9.009
8.722
8.575
8.522
8.340
6.199
7.967
7.817
7.657
7.257
6.426
5.933
5.779
5.463
5.228
7.5W
0—1200
24.379
24.379
24,382
24.646
24.884
25.115
25.187
25.345
25.537
25.623
25.757
25.878
26,007
26.090
26.156
26.249
26.305
26.333
26.360
26.395
26.448
26.512
26.562
26.610
26.663
26.688
26.770
26.846
26.932
26.982
27.035
27.091
27.129
0.000
0.036
0.071
0.106
0.137
0.168
0.196
0.223
0.249
0.273
0.295
0.317
0.338
0.358
0.377
0.395
0.413
0.430
0.447
0.463
0.479
0.511
0.541
0.570
0.599
0.626
0.692
0.754
0.813
0.869
0.922
0.972
1.018
1.3W
0— 602
24.481
24,496
0.000
0.025
0.068
0.099
0.128
0.156
0.182
0.208
0.232
0.256
0.278
0.299
0.320
0.340
0.359
121
121
33.456
33.456
33.441
33.446
33.481
33.517
33.526
33.498
33.556
33.619
33.672
33.744
33.753
33.793
33.841
33.876
33.913
33.932
33.974
32.994
34.006
34.043
34.061
34.088
34.091
34.111
34.137
34.110
34.180
34.274
34.289
34.22
24.819
24.949
25.171
25.318
25.363
25.486
25.626
25.753
25.839
25.963
25.992
26.062
26.142
26.203
26.268
26.302
26.380
26.419
26.436
26.493
26.529
26.585
26.609
26.648
26.726
26.817
26.936
27.029
27.080
27.126
-
0.377
0.395
0.413
0.430
0.446
0.462
0.494
0.524
0.554
0.583
0.612
0.680
0.744
0.803
0.858
0.908
0.955
34 44.8N
STA 452
0.
10.
20.
30.
40.
50.
60.
70.
80.
90.
100.
200.
500.
15.336
14.836
13.118
12.649
12.317
12.048
12.025
11.692
10.566
10.143
10.141
STA 456
0.
10.
20.
30.
40.
200.
500.
33.461
33.454
33.538
33.550
33.571
33.595
33.594
33.604
33.720
33.779
33.781
34 54.3N
14.910
14.794
13.674
12.646
12.482
120 49.9W
24.735
24.838
25.259
25.360
25.441
25.510
25.515
25.584
25.878
25.997
25.998
120 43.1W
33.416
33.416
33.466
33.534
33.558
24.792
24.817
25.091
25.349
25.399
0— 108
0.000
0.
0.032
0.061
0.088
0.114
0.139
0.164
0.189
0.211
0.232
0.253
0.434
0.829
10.
20.
30.
D—
48
15.027
14.926
14.275
13.600
120 40.7W
33.449
33.446
33.444
33.495
24.793
24.813
24.949
25.129
200.
500.
STA 459
0.000
0.
0.032
0.062
0.090
0.116
0.444
10.
20.
30.
40.
50.
60.
70.
80.
90.
100.
110.
120.
130.
140.
150.
160.
170.
180.
190.
200.
500.
0.883
34 48.4N
STh 455
34 49.6N
16.129
16.142
16.085
13.279
13.435
12.667
12.409
11.827
11.284
10.986
10.482
10.384
10.166
10.004
9.714
9.475
9.326
9.138
8.942
8.740
8.605
120 53.3W
33.425
33.425
33.426
33.080
33.341
33.415
33.394
33.524
33.587
33.662
33.720
33.725
33.768
33.801
33.855
33.891
33.905
33.918
33.941
33.970
33.995
24.529
24.527
24.540
24.873
25.043
25.253
25,286
25.497
25.646
25.758
25.892
25.913
25.983
26.037
26.127
26.195
26.230
26.271
26.320
26.374
26.415
40
0.000
0.032
0.062
0.092
0.425
0.820
D— 218
0.000
0.034
0.068
0.101
0.131
0.159
0.186
0.212
0.236
0.259
0.280
0.302
0.322
0.342
0.362
0.380
0.416
0.434
0.451
0.467
0.891
34 44.1N
STA 462
0.
10.
20.
30.
40.
50.
60.
70.
80.
90.
100.
110.
120.
130.
140.
150.
160.
170.
180.
190.
200.
220.
240.
260.
280.
300.
350.
400.
450.
500.
524.
16.368
16.369
16.223
14.508
13.235
12.847
12.592
11.959
10.572
10.775
10.588
10.414
10.273
10.009
9.874
9.602
9.358
9.201
9.086
8.887
8.745
8.405
8.271
8.126
7.884
7.758
7.296
6.917
6.203
5.850
5.793
STA 466
121
33.409
33.407
33.425
33.404
33.318
33.420
33.435
33,417
33.400
33.588
33.665
33.702
33.717
33.766
33.787
33.825
33.863
33.892
33.910
33.950
33.975
34.022
34.043
34.060
34.071
34.079
34.135
34.139
34.160
34.231
34.243
34 44.5N
4.7W
D-' 532
24.462
24.461
24.508
24.870
25.065
25.221
25.283
25.390
25.628
25.738
25.831
25.890
25.926
26.009
26.048
26.123
26.193
26.240
26.273
26.335
26.377
26.467
26.504
26.539
26.583
26,608
26.719
26.774
26.886
26.986
27.003
0.000
0.035
0.069
0.102
0.132
0.160
0.187
0.213
0.239
0.262
0.284
0.306
0.327
0.347
0.367
0.387
0.405
0.423
0.441
0.458
0.475
0.508
0.539
0.569
0.599
0.628
0.697
0.763
0.824
0.881
0.907
121 17.8W
0-
576
34 39.9N
5Th 465
0.
10.
20.
30.
40.
50.
60.
70.
80.
90.
100.
110.
120.
130.
140.
150.
160.
170.
180.
190.
200.
220.
240.
260.
280.
300.
350.
400.
450.
500.
550.
600.
650.
680.
16.805
16.810
16.509
15.756
14.513
12.982
12.545
12.088
11.859
11.261
10.758
10.761
10.287
9.853
9.519
9.273
9.141
8.981
8.917
8.596
8.324
8.112
7.941
7,692
7.551
7.384
6,928
6.333
6.181
5.936
5.851
5.574
5.236
5.171
STA 469
121 14.2W
33.469
33.468
33.424
33.336
33.144
33.008
33.048
33.313
33.494
33.513
33.560
33.614
33.674
33.753
33.794
33.807
33.823
33.870
33.871
33.923
33.936
34.005
34.045
34.082
34.105
34.115
34.143
34.149
34.175
34.192
34.213
34.251
34.295
34.306
34 49.3N
24.407
24.405
24.442
24.545
0— 775
0.000
0.035
0.071
24.877
24.993
25.285
25.468
25.593
25.720
25.761
25.890
26.025
26.112
26.163
26.196
26.258
26.269
26.360
26.412
26.498
26.555
26.620
26.659
26.690
26.776
26.860
26.900
26.944
26.972
27.036
27.112
27.128
0.105
0.138
0.170
0.200
0.229
0,254
0.279
0.302
0.325
0.347
0.367
0.387
0.406
0.424
0.442
0.460
0.477
0.494
0.525
0.555
0.585
0.613
0.640
0.707
0.768
0.827
0.884
0.940
0.993
1.043
1.071
8.3W
D— 565
24.669
121
0.
16.601
33.308
24.332
0.000
0.
16.712
33.458
24.421
0.000
10.
16.602
16.589
16.411
14.919
14.120
13.443
12.577
11.879
11.562
11,390
11.049
10.600
33.309
33.306
33.300
33.165
33.171
24.332
24.333
24.369
24.598
24.772
25.008
25.263
25.520
25.607
25.658
25.743
0.036
0.072
0.108
0.143
0.175
0.206
0.235
0.261
0.285
0.309
0.332
0.354
10.
20.
30.
40.
50.
6Ô.
70.
80.
90.
100.
110.
120.
10.205
33.743
0.375
130.
9.876
9.619
9.477
9.332
9.236
9.046
8.871
8.322
8.148
7.958
7.862
7.704
33.793
33.851
140.
150.
160.
170.
180.
190.
200.
220.
240.
260.
280.
300.
33.455
33.367
33.279
33.236
33.233
33,276
33.399
33.581
33.519
33.581
33.700
33.772
33.815
33.841
33.873
33.909
33.933
33.952
33.955
33.972
34.010
33.978
34.005
24.426
24.763
25.011
25.147
25.328
25.377
25.454
25.658
25.882
25.951
26.061
26.126
26.169
26.202
26.571
26.607
0.395
0,414
0.433
0.451
0.469
0.487
0.503
0.536
0.567
0.597
0.627
0.656
16.678
14.873
13.359
12.499
11,522
11.438
11.539
11.195
9.614
9.489
9.385
9.332
9.272
9.194
9.042
8.813
8.626
8.408
8,395
8.259
8.088
7.847
7.624
7.477
7.225
34.013
26.450
26.505
26.516
26.570
26.597
26.632
0.035
0.069
0.100
0.129
0.156
0.183
0.208
0.233
0.255
0.276
0.296
0.315
0.334
0.353
0.371
0.388
0.405
0.422
0.438
0.454
0.485
0.516
0.546
0.575
0.604
7.156
6.381
6.115
34.117
34.073
34.103
26.724
26.794
26.852
0.725
0.790
0.852
350.
400.
450.
6.835
6.315
6.339
34.020
34.051
34.162
26.692
26.785
26.869
0.674
0.740
0.801
20.
30.
40.
50.
60.
70.
80.
90.
100.
110.
120.
130.
140.
150.
160.
170.
180.
190.
200.
220.
240.
260.
280.
300.
350.
400.
450.
500.
33.297
33.405
33.566
33.602
33.627
33.657
33.704
33.873
33.901
33.923
33.961
33.995
34,032
34.037
34.059
34.051
34.068
25.859
25.957
26.052
26.140
26.181
26.226
26.259
26.319
26.373
26.456
26.517
26.563
34,014
26.251
26.315
26.363
26.412
26.416
6.145
34.179
26.908
0.911
500.
6.182
34.205
26.923
0.860
550.
5.779
34.236
26.999
0.967
550.
3.735
34.267
27.029
0.914
568.
5.667
34.251
27.025
0.986
554,
5.734
34.271
27.032
0.918
34 54.8N
STA 472
120 56.7V
1-. 317
STA 476
35
120 43.3W
1.ON
0—
50
SAL
0.
16.631
10.
20.
30.
40.
50.
60.
70.
80.
90.
100.
110.
120.
130.
140.
150.
160.
170.
180.
190.
200.
220.
240.
260.
280.
300.
500.
16.625
16.403
14.501
13.838
13.230
12.533
11.608
11.104
11.008
10.892
10.418
10.047
9.664
9.467
9.370
9.250
9.150
8.910
8.813
8.785
8.500
8.117
8.017
8.008
7.931
SIA 477
0.
10.
20.
30.
200.
500.
35
14.134
14.001
13.529
13.156
33.468
33.468
33.447
33.284
33.261
33.352
33.342
•33.450
33.533
33.564
33.670
33.719
33.772
33.840
33.865
33.878
33.897
33.906
33.952
33.974
33.983
34.018
34.069
34.079
34.080
34.088
7.1N
24.447
24.449
24.484
24.778
24.899
25.093
25.222
25.481
25.637
25.678
25.781
25.902
26.007
26.124
26.176
26.202
26.236
26.259
26.334
26.366
26.378
26.449
26.547
26.570
26.572
26.589
120 44.3W
33.353
33.328
33.379
33.391
24.909
24.917
25.054
25.138
0.000
0.035
0.070
0.104
0.135
0,164
0.193
0.219
0.243
0.267
0.290
0.311
0.332
0.352
0.370
0.389
0.407
0.425
0.442
0.459
0.476
0.
10.
20.
30.
40.
200.
500.
14.496
14,465
14.320
13.505
13.149
33.366
33.368
33.380
33.436
33.460
24.843
24.851
24.890
25.102
25.192
0.000
0.031
0.062
0.092
0.121
0.476
0.887
0.508
0.539
0.569
0.598
0.628
0.884
D-.
45
0.000
0.030
0.060
0.089
0.469
0.889
STA 478
35
4.9N
120 49.0W
0—
95
SAL
SIGNA
33.370
33.367
33.365
24.688
24.689
24.822
25.109
25.235
25.414
0.000
0.033
0.065
0.095
0.123
0.149
0.
10.
20.
30.
40.
50.
60.
15.229
15.210
14.590
13.489
13.033
12.403
25.482
0.175
70.
12.027
33.586
25.508
0.200
80.
11.833
11.425
33.597
33.637
25.552
25.659
0.224
0.248
0.473
0.887
90.
200.
500.
33.4.41
3.557
12.135
__
STA 480
0.
10.
20.
30.
40.
50.
60.
70.
80.
90.
100.
110.
120.
130.
140.
150.
160.
170.
180.
190.
200.
220.
240.
500.
35
15.788
15,789
15.788
15.479
13.827
12.079
12.329
12.112
11.753
11.327
10.828
10.654
10.443
10.267
9.915
9.651
9.338
9.219
9.006
8.893
8.847
8.801
8.737
STA 482
1.8N
120 55.5W
33.402
33.402
33.402
33.381
33.264
33.140
33.257
33.430
33.594
33.638
33.690
33.713
24.589
24.588
24.589
24.641
24.904
25.153
25.196
25.371
25.565
25.678
25.808
25.857
33.74.4
25.918
33.766
33.804
33.838
33.891
33.914
33.953
33.967
33.978
33.986
33.995
25.965
26.054
26.125
26.218
26.254
26.319
26.348
26.364
26.378
26.395
34 56.1N
121
D— 250
0.000
0.034
0.067
0.101
0.133
0.162
0.190
0.217
0.243
0.266
0.289
0.311
0.332
0.353
0.373
0.392
0.411
0.429
0.446
0.463
0.480
0.513
0.546
0.884
3.2W
0— 493
0.
10.
20.
30.
40.
50.
60.
70.
80.
90.
100.
110.
120.
130.
140.
150.
160.
170.
180.
190.
200.
220.
240.
260.
280.
300.
350.
400.
500.
0.3W
121
SAL
33.407
24.589
34 59.5N
STA 481
15.800
15.797
15.289
13.281
12.652
11.160
10.937
10.850
10.684
10.638
10.472
10.234
9.775
9.516
9.371
9.339
9.197
9.151
9.012
8.834
8.611
8.363
8.248
8.078
7.860
7.705
7.182
6.371
STA 484
33.406
33.392
33.287
33.298
33.250
33.379
33.381
33.492
33.628
33.689
33.736
33.801
33.843
33.875
33.897'
33.912
33.928
33.955
33.980
34.002
34.030
34.045
34.075
34.103
34.107
34.096
34.139
34 54.ON
24.590
24.691
25.032
25.166
25.408
25.547
25.565
25.680
25.793
25.870
25.947
26.075
26.151
26.200
26.222
26.257
26.276
26.320
26.367
26.420
26.479
26.508
26.557
26.612
26.638
26.704
26.847
121 11.2W
0— 425
0.000
0.034
0.067
0.098
0.126
0.153
0.178
0.203
0.227
0.249
0.271
0.292
0.312
0.332
0.350
0.368
0.386
0.404
0.421
0.438
0.455
0.487
0.518
0.548
0.577
0.605
0.675
0.739
0.852
D— 570
16.752
15.748
15.500
13.970
12.758
12.740
12.061
11.525
11.159
10.938
33.483
33.374
33.387
33.351
33.328
33.360
33.381
33.352
33.359
33.466
24.431
24.576
24.641
24.941
25.167
25.196
25.343
25.420
25.492
25.615
0.000
0.035
0.068
0.100
0.129
0.157
0.184
0.210
0.235
0.260
10.
20.
30.
40.
50.
60.
70.
80.
90.
18,716
16.576
16.417
16.117
13.183
13.000
12.458
12.784
11.611
10.826
33.307
33.300
33.291
33.270
33.022
33.009
33.193
33.381
33.299
33.368
24.304
24.332
24.361
24.413
24.847
24.874
25.122
25.204
25.363
25.558
0.000
0.036
0.072
0.108
0.140
0.171
0.201
0.229
0.256
0.282
10.867
10.503
10.315
9.873
33.561
33.682
33.715
33.784
25.701
25.859
25.917
26.046
0.283
0.305
0.327
0.347
100.
110.
120.
130.
10.742
10.052
10.331
10.054
33.481
25.661
25.748
0.305
0.329
33.671
33.731
25.880
0.350
25.974
0.372
9.568
9.291
33.635
33.891
26.136
26.225
0.366
140.
9.832
33.815
26.076
0.391
160.
170.
180.
190.
200.
220.
240.
260.
260.
300.
9.161
8.977
8.895
8.797.
8.540
8.383
8.156
7.860
7.613
33.914
33.945
33.959
33.984
34.008
34.027
34.052
34.092
34.103
26.264
26.318
26.342
26.376
26.435
26.474
26.528
26.603
26.648
150.
0.402
0.420
0.437
0.454
0.470
0.502
0.533
0.562
0.591
160.
170.
180.
190.
200.
220.
240.
260.
280.
9.423
9.049
8.893
8.712
8.516
6.312
8.005
7.624
7.290
7.163
33.841
33.899
33.933
33.940
33.967
33.969
33.987
26.165
26.270
26.322
26.355
26.407
26.439
26.500
0.410
0.428
7.492
34.110
26.671
0.619
300.
350.
7.006
6.432
6.064
34.104
34.090
34.164
26.734
26.801
26.906
0.686
0.751
0.811
350.
400.
450.
0.866
500.
550.
0.
10.
20.
30.
40.
50.
60.
70.
80.
90.
100.
110.
120.
130.
140.
150.
400.
450.
500.
0.
-
560.
33.4.40
34.018 .26.580
0.4.46
0.463
0.479
0.495
0.327
0.557
0.586
0.614
34.033
34.033
26.639
26.657
7.055
34.063
26.695
0.641
6.495
5.970
5.682
34.042
34.070
34.100
26.755
26.903
0.708
0.770
0.830
-5.582
34.139
26.946
0,887
5.495
5.473
34.185
34.193
26.994
27.003
0.941
0.952
26.84-4
STA 487
0.
10.
20.
30.
40.
50.
60.
70.
80.
90.
100.
110.
120.
130.
140.
150.
160.
170.
180.
190.
200.
220.
240.
260.
280.
300.
350.
400.
450.
500.
34 49.5N
17.354
17,299
17.180
16.320
14.082
13.444
12.393
12.142
11.388
11.240
10.939
10.638
10.362
10.175
10.010
9.939
9.770
9.648
9.519
9.421
9.287
9.015
8.690
8.498
8.262
7.998
7.359
6.961
6.576
STA 492
121 20.9W
SAL
33.365
33.365
33.356
33.335
33.396
33.423
33.473
33.502
33.597
33.633
33.671
33.706
33.749
33.772
33.811
33.826
33.858
33.882
33.906
33.930
33.954
33.999
34.013
34.053
34.073
34.075
34.100
34.165
34.153
24.199
24.212
24.233
24.417
24.952
25.105
25.350
25.421
25.635
25.690
25.773
25.854
25.935
25.986
26.043
26.067
26.120
26.159
26.199
26.234
26.275
26.354
26.416
26.477
26.528
26.570
26.682
26.789
26.831
0-. 470
0 .000
0.037
0.074
0.111
0.143
0.173
0.200
0.226
0.251
0.274
0.297
0.319
0.340
0.361
0.381
0.400
0.420
0.439
0.457
0.475
0.493
0.528
0.561
0.592
0.623
0.653
0.725
0.791
0.853
0.914
35 10.3N
120 31.5W
0—
55
34 44.ON
STA 490
0.
10.
20.
30.
40.
50.
60.
70.
80.
90.
16.799
16.786
16.726
14.357
13.189
12.284
915
11. 502
11. 206
11.
10.945
100.
10. 763
110.
120.
130.
10.519
10.414
10.160
10.023
9,795
9.688
9.604
9,445
140.
150.
160.
170.
180.
190.
200.
220.
240.
260.
280.
300.
350.
400.
9.344
9.208
8.980
8.843
8.655
8.492
8.340
7.838
7.241
450.
500.
550.
600.
650.
6.873
674.
4.871
STA 495
6.351
6.123
5.245
4.998
35
121 32.1W
0— 950
24.313
24.316
0.000
0.036
0.072
0.106
0.136
0.163
0.188
33.344
33.344
33.345
33.341
33.436
33.555
33.582
33.619
33.646
33.663
33.700
33.734
33.742
33.789
33.812
33.857
33.877
33.894
33.925
33.946
33.970
34.016
34.049
34.060
34.081
34.097
34.130
34.133
34.179
34.171
34.203
34.277
34.308
34.331
4.ON
24.331
24.853
25.166
25.435
25,526
25.631
25.706
25.766
25.827
25.897
25.921
26.001
26.042
26.116
26.149
26.176
26.227
26.259
26.300
26.373
26.420
26.458
26.499
26.535
26.636
26.724
26.811
26.875
26.930
27.096
27.150
27.182
121
0.212
0.236
0.258
0.280
0.302
0.323
0.343
0.363
0.383
0.402
0.420
0.439
0.456
0.474
0.508
0.541
0.573
0.604
0.635
0.708
0.777
0.842
0.902
0.960
1.014
1.062
1.084
3.8W
D- 490
Si-.
0.
10.
13.257
33.378
25.108
0.000
0.
14.694
33.262
24.721
0.000
13.236
33.392
25.122
12.754
30.
33.430
25.247
10.
20.
12.526
33.455
25.311
40.
12.408
12.248
33.486
33.493
25.358
25.394
0.029
0.056
0.083
0.110
0.136
0.449
0.845
14.698
14.709
14.408
14.016
12.605
12.150
11.092
10.984
10.830
10.580
10.431
10.202
10.061
9.766
9.495
9.389
9.329
9.206
9.113
33.265
33.267
33.239
33.191
33.179
33.316
33.394
33.426
33.549
33.677
33.704
33.740
33.760
33.811
24.722
24.722
24.764
24.809
25.082
25.275
8.929
8.563
8.261
8.129
7.741
7.400
7.324
6.378
6.018
33.943
34.003
34.026
34.046
34.052
34.038
34.146
34.103
34.178
0.032
0.065
0.097
0.129
0.159
0.167
0.213
0.238
0.261
0.284
0.305
0.326
0.346
0.366
0.385
0.404
0.422
0.440
0.458
0.475
0.509
0.54:.
0.571
0.601
0.630
0.699
0.763
0.823
0.678
50.
200.
500.
20.
30.
40.
50.
60.
70.
80.
90.
100.
110.
120.
130.
140.
150.
160.
170.
180.
190.
200.
220.
240.
260.
280.
300.
350.
400.
450.
500.
33.849
33.864
33.873
33.892
33.911
25.532
25.575
25.698
25.841
25.888
25.956
25.996
26.085
26.159
26.188
26.205
26.240
26.269
26.324
26.428
26.492
26.528
26.589
26.628
26.723
26.818
26.923
STA 500
0.
10.
20.
30.
40.
50.
60.
70.
80.
90.
100.
110.
120.
130.
140.
150.
160.
170.
180.
190.
200.
220.
240.
260.
280.
300.
350.
400.
450.
500.
534.
35
14.928
14.936
14.776
14.585
14.159
11.961
11.562
11.455
11.199
10.976
10.673
10.626
10.389
9.960
9.759
9.231
9.032
8.865
8.778
8.564
8.469
8.195
7.807
7.560
7.382
7.147
6.580
6.293
5.923
5.510
5.515
STA 508
9.3N
121
33.239
33.246
33.208
33.119
32.903
33.310
33.367
33.429
33.531
33.601
33.643
33.655
33.686
33.727
33.773
33.809
33.873
33.912
33.915
33.939
33.951
33.986
33.975
33.984
34.013
34.009
34.029
34.094
34.137
34.162
34.226
35 38.8N
7.4W
0— 548
24.653
24.656
24.662
24.634
24.558
25.307
25.425
25.493
25.618
25.712
25.798
25.817
25.882
25.987
26.056
26.170
26.253
26.309
26.326
26.378
26.402
26.470
26.520
26.562
26.610
26.640
26.733
26.822
26.903
26.974
27.023
0.000
0.033
0.066
0.099
0.132
0.162
0.188
0.213
0.238
0.261
0.284
0.306
0.327
0.348
0.368
0.387
0.406
0.423
0.440
0.457
0.474
0.506
0.537
0.567
0.596
0.625
0.693
0.758
0.818
0.875
0.911
121 15.7W
D—
32
35 15.4N
STA 503
0.
10.
20.
30.
40.
50.
200.
500.
13.953
13.002
12.125
11.842
11,726
11.538
STA 509
120 55.3W
33.442
33.440
33.44.4
33.509
33.542
33.580
35 37.9N
25.015
25.206
25.380
25.483
25.530
25.594
0—.
55
0.000
0.029
0.056
0.081
0.106
0.130
0.419
0.813
12]. 17.8W
90
33.177
33.178
33.126
32.964
32.992
33.165
33.292
33.442
24.799
24.795
24.837
25.084
25.179
25.316
25.409
0.000
33.511
25.539
25.662
SAL
0.
10.
20.
30.
12.557
11.840
11.794
33,294
33.294
33.344
33.430
25.184
25.181
25.356
25.431
0.000
0.028
0.055
0.081
0.
10.
20.
30.
40.
50.
60.
70.
80.
86.
14.013
14.035
13.633
11.719
11.320
11.300
11.332
11.376
11.544
11.281
33.607
25.48].
0.032
0.063
0.093
0.121
0.149
0.175
0.201
0.225
0.240
35 34.8N
STA 510
0.
10.
20.
30.
40.
50.
60.
70.
80.
90.
100.
110.
120.
130.
140.
150.
160.
170.
180.
190.
200.
220.
240.
260.
280.
300.
350.
400.
450,
478.
121 23.4W
15.503 33.383
15.505 33.338
15.484 33.333
15.508
33.339
15.307
33.316
32.986
12.805
11.397
32.857
10.894 32.880
10.702
32.901
10.592
32.923
11.030 33.311
33.516
10.521
9.965 33.601
9.434 33.691
9.059 33.738
9.006 33.845
8.951 33.888
8.770 33.897
8.509 33.912
8.330 33.941
8.254 33.948
8.015 33.987
7.716 34.000
7.871 34.081
7.625 34.081
7.429 34.100
6.884 34.118
6.463
34.154
34.163
5.966
5.764 34.217
STA 601
35 38.ON
24.638
24.603
24.603
24.603
24.629
24.895
25.060
25.168
25.218
25.253
25.478
25.726
25.888
26.046
26.143
26..235
26.277
26.313
26.365
26.415
26.432
26.498
26.553
26.593
26.629
26.672
26.762
26.847
26.918
26.986
121 17.9W
D'— 485
0.000
0,033
0.067
0.100
0.134
0.166
0.196
0.225
0.252
0.280
0.307
0.331
0.353
0.373
0.392
0.411
0.428
0.446
0.463
0.479
0.495
0.527
0.557
0.587
0.615
0.643
0.710
0.773
0.832
0.863
D—
88
35 38.8N
STA 600
0.
10.
20.
30.
11.877
11.879
11.817
11.426
121 15.7W
SAL
33.279
33.281
33.336
33.472
25.298
25.299
25.354
25.532
200.
500.
STA 602
0—
33
0.000
0.027
0.053
0.079
0.443
0.856
35 35.3N
121 23.7W
0— 482
0.
13.382
33.122
24.885
0.000
0.
10.
20.
30.
12.881
12.053
11.898
33.100
24.968
0.031
10.
14.858
14.856
33.271
33.269
24.692
24.691
0.000
0.033
33.078
25.110
0.060
20.
14.850
33.270
33.104
25.159
0.088
30.
14.735
33.259
40.
50.
60.
70.
80.
200.
11.789
33.171
33.251
23.231
25.338
25.546
25.644
25.725
0.116
40.
50.
60.
70.
80.
11.493
32.970
24.693
24.705
25.130
0.065
0.098
0.128
11.045
32.997
25.232
0.156
33.183
33.416
33.484
25.392
25.578
25.737
0.183
0.208
0.231
33.555 25.811
33.607 25.914
33.624 25.981
33.657 26.048
33.732 26.109
33.783 26.172
33.840 26.224
33.881 26.282
33.909 26.336
33.916 26.370
33.946 26.404
33.969 26.438
34.032 26.489
33.994 26.331
34.077 26.580
0.254
0.275
0.296
0.316
0.336
0.354
0.373
0.391
0.408
0.425
0.441
0.457
0.489
0.520
0.549
500.
11.544
11.226
11.129
11.018
33.444
33.548
33.626
0.144
0.169
0.193
0.216
0.451
0.859
90.
10.952
10.924
10.320
10.207
100.
110.
120.
130.
140.
150.
160.
170.
180.
190.
200.
220.
240.
260.
9.838
9.510
9.257.
9.240
9.094
9.050
8.822
8.678
8.496
8.427
8.318
8.312
7.828
7.936
280.
300.
350.
7.666
7.327
6,880
3.076
34.104
34.114
26.619
26.661
26.760
0.578
0.607
0.673
400.
450.
500.
6.403
5.738
34.137
34.131
26.842
26.921
0.736
0.796
0.851
__
35 33.4N
STA 603
15.276
15.260
15.237
15.121
14.730
13.558
10.921
10.864
10.436
10.141
9.788
9.515
9.156
8.926
8.847
8.796
8.732
8.473
8.438
8.261
8.180
7.680
7.527
7.298
7.035
6.838
6.307
5.829
6.038
5.755
5.530
5.227
4.820
4.817
0.
10.
20.
30.
40.
50.
60.
70.
80.
90.
100.
110.
120.
130.
140.
'150.
160.
170.
180.
190.
200.
220.
240.
260.
280.
300.
350.
400.
450.
500.
550.
600.
650.
662.
STA 607
0.
10.
20.
30.
40.
50.
60.
70.
80.
90.
100.
110.
120.
130.
140.
150.
160.
170.
180.
190.
200.
220.
240.
260.
280.
300.
350.
400.
450.
500.
550.
600.
650.
698.
33.317
33.316
33.314
33.303
33.274
33.177
33.097
33.369
33.502
33.581
33.650
33,673
33.756
33.784
33.831
33.873
33.918
33.936
33.940
33.964
33.978
24.636
24.639
24.643
24.660
24.723
24.892
25.332
25.552
25.730
25.843
25.956
26.019
26.142
26.200
26.249
26.290
26.335
26.389
26.397
26.443
26.467
33.98.4
26.545
34.007
34.027
34,025
34.027
34.063
34.104
34.220
34.236
34.255
34.300
34.370
34.373
26.585
26.634
26.669
26.697
26.796
26.889
26.954
27.002
27.045
27.116
27.219
27.221
35 24.6N
16.034
16.026
16.025
16.018
16.008
15.966
11.897
10,867
10.394
10.227
10.216
9.713
9.458
9.256
9.087
8.814
8.761
8.714
8.400
8.366
8.091
7.774
7.692
7.568
7.105
6.728
6.402
6.049
5.653
5.278
5.013
4.813
4.688
4.541
121 27.9W
121 46.2W
33.414
33.417
33.420
33.424
33.423
33.412
33.189
33.232
33.344
33.425
33.557
33.652
33.710
33.766
33.788
33.786
33.896
33.936
33.948
33.986
33.976
33.989
34.033
34.052
24.543
24.547
24.549
24.554
24.555
24.557
25.225
25.445
25.581
25.707
25.811
25.969
26.057
26.133
26.178
26.219
26.313
26.351
26.409
0— 670
nrio
0.000
0.033
0.066
0.099
0.132
0.164
0.192
0.218
0.241
0.263
0.285
0.305
0.326
0.343
0.361
0.378
0.396
0.412
0.429
0.445
0.461
0.492
0.521
0.550
0.578
0.605
0.671
0.732
0.789
0.844
0.896
0.946
0.991
1.002
0—1050
0.000
0.034
0.068
0.102
0.136
0.170
0.201
0.227
0.252
0.276
5Th 605
0.
10.
20.
30.
40.
50.
60.
70.
80.
90.
100.
110.
120.
130.
140.
150.
160.
170.
180.
190.
200.
220.
240.
260.
280.
300.
350.
400.
450.
500.
550.
600.
650.
700.
730.
STA 609
35 29.3N
15.596
15.491
15.468
15.450
15.417
15.345
13.639
10.866
10.211
9.839
9.680
9.525
9.132
8.964
8.841
8.728
8.560
8.465
8.222
8.025
7.863
7.687
7.588
7.356
7.358
7.092
6.222
6.203
5.874
5.686
5.572
5.229
5.046
4.862
4.760
121 36.4W
33.331
33.330
33.329
33.328
33.330
33.328
32.847
33.395
33.545
33.638
33.675
33.696
33.729
33.744
33.824
33.882
33.912
33.961
33.970
33.966
33.981
34.005
34.046
34.052
34.090
34.075
34.056
34.138
34.190
34.227
34.262
34.280
34.291
34.355
34.381
35 20.3N
33.491
33.490
33.490
33.489
0.359
0.377
0.396
0.413
0.430
0.447
16.491
16,490
16.479
16.453
16.448
15.716
13,385
11.500
11.121
10.708
10.062
9.658
9.430
9.171
9.013
8.815
6.602
8.458
8.216
26.4.45
0.463
190.
8.149
34.028
34.086
34.113
34.146
34.168
34.207
34.239
26.678
26,335
26.581
26.615
26.659
26.713
26.801
26.868
26.944
27.006
27.067
27.116
0.479
0.509
0.539
0.568
0.596
0.624
0.689
0.750
200.
220.
240.
260.
280.
300.
350.
400.
8.045
7.836
7.424
7.241
7.030
6.897
6.791
6.472
0.808
450.
5.787
0.863
0.914
0.964
500.
550.
600.
5.434
5.148
4.916
34.187
34.278
34.316
27.161
27.207
1.011
632.
4.803
3.4.026
0.298
0.319
-0.339
1.054
26.162
26.244
26.307
26.357
26.410
26.454
26.481
26.516
26.560
26.607
26.645
26.674
26.700
26.801
26.868
26.951
27.003
27.045
27.100
27.130
27.202
27.234
121 55.4W
10.
20.
30.
40.
50.
60.
70.
80.
90.
100.
110.
120.
130.
140.
150.
160.
170.
180.
0.
24.577
24.600
24.604
24.607
24.616
24.630
24.621
25.572
25.802
25.938
25.993
26.035
26.124
0— 990
0.000
0.034
0.067
0.101
0.134
0.167
0.200
0.227
0.250
0.271
0.292
0.312
0.331
0.350
0.368
0.386
0.403
0.419
0.435
0.451
0.467
0.497
0.526
0.555
0.582
0.610
0.675
0.736
0.793
0.848
0.900
0.950
0.998
1.043
1.069
0—2200
33.962
24.497
24.496
24.499
24.504
24.505
24.603
25.035
25.373
25.496
25.689
25.840
25.957
26.065
26.170
26.247
26.302
26.360
26.412
26.448
0.000
0.035
0.069
0.103
0.138
0.172
0.203
0.231
0.256
0.280
0.302
0.323
0.343
0.362
0.380
0.398
0.415
0.432
0.448
34.019
26.503
0.463
34.027
34.029
33.999
34.009
34.232
26.325
26.558
26.593
26.627
26.669
26.701
26.785
26.839
26.900
26.972
27.036
27.098
0.479
0.509
0.538
0.567
0.595
0.622
0.685
0.750
0.810
0.866
0.920
0.970
34.263
27.136
1.001
33.489
33.400
33.317
33.285
33.356
33.509
33.561
33.625
33.714
33.796
33.862
33.892
33.924
-33.962
3.025
34.042
34.131
34.146
34.112
34.149
_
STA 614
0.
10.
20.
30.
40.
50.
60.
70.
80.
90.
100.
110.
120.
130.
140.
150.
160.
170.
180.
190.
200.
220.
240.
260.
280.
500.
36 10.8W
11.560
11.449
11.436
11.376
11.165
11.134
10.983
10.939
10.878
10.830
10.808
10.518
10.271
10.134
9.883
9.694
9.519
9.305
9.235
9.119
8.741
8.482
8.305
8.112
7.890
121 44.3W
33.391
33.387
33.386
33.421
33.511
33.546
33.594
33.635
33.651
33.659
33.658
33.696
33.736
33.752
33.800
33.832
33.868
33.901
33.913
33.925
33.980
34.012
34.032
34.051
34.073
25.444
25.461
25.463
25.501
25.609
25.642
25.706
25.746
25.769
25.783
25.787
25.867
25.941
25.977
26.057
26.113
26.170
26.231
26.251
26.279
26.382
26.447
26.490
26.534
26.584
0— 299
0.000
0.025
0.051
0.076
0.100
0.124
0.147
0,170
0.193
0.215
0.237
0.259
0.280
0.301
0.321
0.340
0.359
0.377
0.395
0.413
0.430
0.462
0.493
0.524
0.554
0.824
5Th 616
0.
10.
20.
30.
40.
50.
60.
70.
80.
90.
100.
110.
120.
130.
140.
150.
160.
170.
180.
190.
200.
220.
240.
260.
280.
300.
350.
400.
450.
500.
550.
600.
650.
692.
STA 618
0.
10.
20.
30.
40.
50.
60.
70.
80.
90.
100.
110.
120.
130.
140.
150.
160.
170.
180.
190.
200.
220.
240.
260.
280.
300.
350.
400.
450.
500.
550.
600.
650.
700.
716.
36
12.604
12.421
12.133
11.094
10.661
10.477
10.241
10.175
10.120
9.787
9.646
9.447
9.333
9.207
9.031
8.890
8.828
8.769
8.689
8.495
8.398
8.281
8.046
7.868
7.735
7.597
7.180
6.566
6.033
5.726
5.444
5.285
4.999
4.917
7.4W
121 51.9W
33.381
33.405
33.434
33.463
33.551
33.640
33.662
33.743
33.761
33.763
33.820
33.869
33.883
33.935
33.941
33.970
33,979
33.985
33.987
33.992
34.006
34.009
34.031
34.044
34.067
34.106
34.126
34.175
34.198
34.268
34.302
34.330
34.366
3.4.376
D— 930
25.239
25.293
25.370
25.584
25.729
25.831
25.889
25.962
25.986
26.044
26.111
26.183
26.212
26.273
26.305
26.351
26.368
26.381
26.396
26.430
26.456
26.475
26.528
26.565
26.602
26.652
26.728
26.850
26.937
27.031
27.092
27.133
27.195
27.212
0.000
0.027
0.054
0.080
0.103
0.125
0.147
0,168
0.189
0.209
0.228
0,247
0.265
0.283
0.300
0.317
0,334
0.351
0.367
0.383
0.400
0.431
0.462
0.492
0.521
0.549
0.618
0.682
0.740
0.794
0.845
0.893
0.939
0.976
0—1540
13.222
13.219
13.215
13.137
12.680
33.397
33.412
33.412
33.401
33.423
25.129
23.141
25.142
25.146
25.256
0.000
0.028
0.057
0.085
0.113
10.
20.
30.
40.
13.142
13.131
13.107
12.982
12.449
122 8.7W
SAL
33.390 25,140
33.391 25.143
33.391 25.148
33.393 25.174
33.413 25.295
11.629
11.172
33.495
33.583
25.512
25.663
0.139
0.163
50.
60.
11.816
11.088
33.474
33.453
25.461
25.577
0.139
0.163
10.824
10.485
10.068
9.795
9.588
9.529
9.374
9.177
9.021
8.825
8.691
8.718
8.651
8.508
8.341
8.126
7.854
7.900
7.683
7.145
6.734
6.407
5.649
5.555
33.633
33.670
33.685
33.712
33.782
33.829
33.861
33.897
33.910
33.919
33.947
33.974
33.989
34.005
34.034
34.041
34.044
34.089
34.097
34.117
34.164
34.203
34.188
34.254
25.764
25.852
25.936
26.002
26.091
26.138
26.188
26.248
26.283
26.321
70.
26.403
26.438
26.486
26.524
0.186
0.208
0.229
0.250
0.270
0.289
0.307
0.325
0.343
0.360
0.377
0.394
0.410
0.427
0.458
0.489
33.458
33.468
33.560
33.649
33.715
33.772
33.842
33.862
33.911
33.928
33.971
33.989
33.990
34.015
26.566
0.519
26.595
26.633
26.725
26.818
26.892
26.977
27.041
0.548
0.577
0.645
0.710
0.770
0.826
0.879
10.697
10.530
10.245
10.172
10.236
9.796
9.697
9.494
9.267
9.163
8.980
8.874
8.825
8.642
8.283
8.090
7.958
7.732
7.455
6.522
6.553
6.121
5.869
5.680
34.039
34.168
34.208
34.227
34.291
25.651
25.688
25.808
25.890
25.930
26.050
26.12a
26.170
26.244
26.274
26.337
26.368
26.376
26.425
26.492
26.543
26.575
26.613
26.658
26.749
26.846
26.934
26.981
27.055
0.187
0.210
0.233
0.254
0.275
0.296
0.315
0.334
0.352
0.370
0.357
0.404
0.421
0.437
0.469
0.499
0.529
0.558
0.587
0.654
0.717
0.776
0.831
0.884
5.434
5.093
4.887
4.763
34.290
34.316
34.357
34.353
27.083
27.145
27.201
27.212
0.930
0.978
1.023
1.037
5.315 34.293
5.004 34,314
4.841 34.331
27.101
27.154
27.185
0.934
0.981
1.017
36
3.4W
122
SAL
0.5W
0-1280
26.364
26.381
STA 620
0.
80.
90.
100.
110.
120.
130.
140.
150.
160.
170.
180.
190.
200.
220.
240.
260.
280.
300.
350.
400.
450.
500.
550.
600.
650.
690.
35 59.7W
3.4.031
34.058
34.074
34.081
34.087
0.000
0.028
0.057
0.085
0.112
STA 622
35
40.
50.
60.
70.
80.
90.
100.
15.242
15.254
15.208
15.110
12.393
11.793
10.927
10.692
10.147
9.703
9.685
110.
120.
130.
140.
150.
160.
170.
180.
190.
200.
220.
240.
260.
280.
300.
350.
400.
450.
500.
550.
600.
650.
658.
0.
10.
20.
30.
STA 629
53.2N
122 21.6W
33.345
33.345
33.347
24.666
24.663
24.675
33.344
24.694
33.281
33.375
33.422
33.455
33.518
33.565
33.687
25.202
25.389
25.582
25.650
25.792
25.904
26.002
9.471
9.192
9.029
8.855
8.670
8.666
8.489
8.376
8.108
8.044
7.737
7.574
7.323
7.050
6.890
6.668
6.224
5.685
5.756
33.738
33.812
33.840
33.895
33.910
33.963
33.981
33.984
33.961
33.971
33.982
34.002
34.018
34.018
34.029
34.115
34.128
34.135
34.238
26.076
26.180
26.227
26.298
26.338
26.380
26.422
26.441
26.464
26.481
26.535
26.574
26.623
26.661
26.692
26.789
26.857
26.931
27.003
5.491
5.226
4.944
4.913
34.265
34.300
34.314
34.317
27.057
27.117
27.160
27.166
36 34.4N
122 32.7W
D—1920
40.
50.
60.
70.
80.
90.
100.
110.
33.461
33.462
33.457
33.445
33.445
33,489
33.548
33.616
33.662
33.731
33.763
33.792
0.310
0.328
0.346
0.363
0.380
0.396
120.
130.
140.
150.
160.
170.
9.854
9.502
9.308
8.828
8.624
8.475
33.814
33.837
33.856
33.838
33.876
33.919
0.412
180.
8.299
33.956
0.428
0.444
0.475
0.504
0.533
0.561
0.589
0.655
0.717
0.775
0.831
190.
200.
220.
240.
260.
280.
300.
350.
400.
450.
500.
8.041
7.957
7.794
7.477
7.274
7.158
7.164
6.989
6.472
6.128
5.884
0.883
0.932
0.979
0.986
550.
600.
650.
700.
742.
5,479
5.252
4.870
4.961
4.775
33.982
33.982
33.988
33.995
34.032
34.054
34.111
34.171
34.175
34.217
34.246
34.238
0—2975
0.
14.910
33.475
24.838
14.930
14.908
13.746
12.048
11.730
11.408
10.916
10.816
10.555
10.274
10.068
9.806
9.382
9.116
8.800
8.827
8.729
8.467
8.368
8.231
7.896
7.712
7.672
7.333
7.062
6.835
6.551
33.476
24.835
33.474
33.477
24.838
25.085
33.502
33.576
25.439
25.556
33.597
25.631
33.650
33.684
33.708
33.726
33.765
25.761
25.805
25.870
25.932
25.998
33.775
33.799
26.050
26.138
33.841
33.856
33.920
33.941
33.971
26.214
26.276
26.322
26.353
26.417
33.995
26.4S2
34.006
34.030
34.056
34.095
34.087
34.094
34.158
34.190
26.481
26.549
26.597
26.633
26.675
26.719
26.800
26.863
0.000
0.031
0.063
0.093
0.120
0.145
0.169
0.192
0.215
0.236
0.258
0.278
0.298
0.318
0.336
0.354
0.371
0.388
0.405
0.421
0.437
0.467
0.497
0.526
0.554
0.581
0.645
0.707
34.224
34.233
34.281
34.310
34.335
34.355
34.363
26.934
26,993
27.052
27.098
27.149
27.191
27.238
0.765
0.821
0.873
0.923
0.971
1.016
1.057
50.
60.
70.
80.
90.
100.
110.
120.
130.
140.
150.
160.
170.
180.
190.
200.
220.
240.
260.
280.
300.
350.
400.
450.
500.
550.
600.
6.217
5.812
5.636
5.452
650.
5.181
700.
748.
4.962
4.597
122 46.1W
14.958
14.956
14.929
14.797
14.693
13.011
11.368
10.781
10.448
10.390
10.273
10.080
0.000
0.033
0.066
0.098
0.131
0.157
0.183
0.206
0.229
0.251
0.271
0.291
10.
20.
30.
40.
36 28.3N
STA 627
0.
10.
20.
30.
Sm 631
0.
10.
20.
30.
40.
50.
60.
70.
80.
90.
100.
110.
120.
130.
140.
150.
160.
170.
180.
190.
200.
220.
240.
260.
280.
300.
350.
400.
450.
500,
S50.
600.
650.
700.
736.
13.951
13.965
13.862
13.682
13.543
11.862
11.248
11.344
10.862
10.491
9.907
9.634
9.308
9.086
9.000
8.777
8.805
8,437
8.323
8.165
8.166
7.948
7.665
7.398
7.228
7,170
6.595
6.352
6.254
5.755
5.518
5.156
5.016
4.756
4.619
24.839
24,861
25.242
25.601
25.759
25.853
25.917
25.961
26,017
26.072
26,148
26.195
26.257
26.319
26.376
26.432
26.491
26,503
26.532
26.583
26.641
26.674
26.718
26.789
26.862
26.940
26.994
0.000
0.031
0.063
0.094
0.125
0.155
0.180
0.204
0.226
0,247
0.268
0.288
0.308
0.327
0.345
0.363
0.381
0.398
0.414
0.430
0.445
0.476
0.506
0.534
0.562
0.589
0.655
0.716
0.775
27.221
0.830
0.883
0.933
0.981
1.027
1.063
122 24.1W
0—2380
34.276
34.277
34,354
34.366
36 38.4N
24.817
24.818
24.820
0—3000
33.389
33.397
27.037
27.095
27.140
27.190
24.975
34.038
34.046
34.064
34.105
34.116
34.149
26.476
26.335
26.590
26.634
26.672
26.712
26.799
26.858
0.000
0.030
0.060
0.089
0.118
0,147
0.172
0.196
0.219
0.241
0.262
0.282
0.301
0.319
0.337
0.355
0.372
0.389
0.405
0.422
0.437
0.468
0.498
0.526
0.554
0.582
0.647
0.708
34.214
34.216
34.237
34.272
34.316
34.345
34.372
26.921
26.986
27.032
27.103
27.156
27.206
27.243
0.767
0.823
0.876
0.926
0.973
1.018
1.049
33.40.4
33.408
33.403
33.350
33.419
33.622
33.632
33.697
33.707
33.741
33.761
33.834
33.884
33.872
33.917
33.914
33.933
33.949
33.987
34.022
24.978
25.004
25.044
25.069
25.356
25.523
25.663
25.757
25.873
25.980
26.052
26.121
26.213
26.267
26.292
26.323
26.377
26.409
26.446
STA 633
36 43.6N
Q11
0.
10.
20.
30.
40.
50.
60.
70.
80.
90.
100.
110.
120.
130.
140.
150.
160.
170.
180.
190.
200.
220.
240.
260.
280.
300.
350.
400.
450.
500.
550.
600.
650.
700.
730.
STA 640
14.147
14.158
14.072
13.134
11.894
11.576
11.201
10.570
10.301
10.160
9.984
9.783
9.722
9.474
9.193
9.113
9.007
8.859
8.714
8.601
8.474
8.133
7.714
7.506
7.404
7.236
6.996
6.646
6.338
5.904
5.456
5.190
4.875
4.671
4.510
33.376
33.389
33.402
33.348
33.439
33.536
33.598
33.672
33.741
33.767
33.790
33.820
33.824
33.850
33.909
33.925
33.942
33.956
33.972
33.98234.012
34.049
34.068
34.096
34.110
34.125
34.147
34.172
34.190
34.207
34.246
34.286
34.309
34.349
34.374
37 21.8N
0.
13.063
10.
20.
30.
40.
200.
500.
12.759
12.471
11.367
11.037
122 12.4w
24.924
24.932
24.960
25.109
25.419
25.553
25.669
25.839
25.940
25.984
26.032
26.088
26.102
26.163
26.255
26.280
26.311
26.345
26.380
26.405
26.448
26.529
26.606
26.658
26.683
26.719
26.769
26.837
26.892
26.960
27.047
27.110
27.164
27.219
27.256
122 30.2W
r—1025
0.000
0.030
0.061
0.090
0.118
0.143
0.167
0.189
0.211
0.231
0.251
0.271
0.290
0.309
0.327
0.345
0.362
0.379
0.396
0.412
0.428
0.460
0.489
0.517
0.545
0.572
0.638
0.700
0.760
0.818
0.871
0.921
0.968
1.012
1.037
D—
45
STA 635
0.
10.
20.
30.
40.
50.
60.
70.
80.
90.
100.
110.
120.
130.
140.
150.
160.
170.
180.
190.
200.
220.
500.
36 47.6N
12.408
12.417
12.380
11.902
11.271
10.898
10.547
10.503
10.385
10.015
9.818
9.606
9.394
9.337
9.247
9.186
9.134
8.961
8.813
8.736
8.660
8.172
122
33.427
33.433
33.449
33.470
33.515
33.631
33.693
33.706
33.726
33.777
33.809
33.843
33.875
33.884
33.898
33.907
33.915
33.941
33.961
33.973
33.983
34.047
3.1W
D— 236
25.312
25.315
25.335
25.441
25.592
25.750
25.859
25.878
25.913
26.017
26.074
26.136
26,196
26.212
26.238
26.255
26.269
26.317
26.356
26.377
26.397
26.522
0.000
0.027
0.053
0.079
0.104
0.127
0.150
0.171
0.192
0.213
0.232
0.252
0.270
0.289
0.307
0.324
0.342
0.359
0.377
0.393
0.410
0.441
0.803
.
.
STA 642
37 17.6N
122 39.7W
98
S&L
33.239
33.270
33.330
33.583
33.631
25.039
25.123
25.225
25.628
25.725
0.000
0.029
0.057
0.083
0.106
0.391
0.800
0.
10.
20.
30.
40.
50.
60.
70.
80.
90.
200.
500.
13.838
13.467
13.098
12.695
11.561
10.872
10.452
10.294
9.927
9.723
33.392
33.372
33.361
33.372
33.413
33.498
33.582
33.598
33.685
33.764
25.001
25.061
25.126
25.214
25.461
25.631
25.790
25.830
25.960
26.056
0.000
0.030
0.058
0.086
0.113
0.137
0.160
0.182
0.203
0.223
0.424
0.827
STA 644
0.
10.
20.
30.
40.
50.
60.
70.
80.
90.
100.
110.
120.
130.
140.
150.
160.
170.
180.
190.
200.
220.
240.
500.
.
37 13.],N
15.578
15.549
15.503
15.367
15.061
14.895
13.026
12.064
11.224
10.289
9,983
9.746
9.360
9.278
9.109
9.073
9.048
8,946
8.803
8.573
8.507
8.352
8.069
122 49.0W
33.486
33.484
33.486
33.472
33.457
33.464
33.412
33.417
33.460
33.615
33.675
33.689
33.738
33.772
33.895
33.905
33.912
33.943
33.957
33.985
33.991
34.011
34.042
24.700
24.705
24.717
24.736
24.792
24.833
25.180
25.370
25.559
25.843
25.942
25.993
26.094
26.134
26.258
26.271
26.281
26.321
26.354
26.412
26.427
26.466
26.533
0— 258
0.000
0.032
0.065
0.097
0.129
0.161
0.191
0.218
0.243
0.266
0.288
0.308
0.328
0.347
0.365
0.383
0.400
0.418
0.435
0.451
0.467
0.499
0.530
0.864
STA 645
0.
10.
20.
30.
40.
50.
60.
70.
80.
90.
100.
110.
120.
130.
140.
150.
160.
170.
180.
190.
200.
220.
240.
260.
280.
300.
350.
400.
450.
500.
STA 648
37
3.ON
123 10.8W
0—2560
0.
10.
15.508
15.514
33.468
33.468
24.702
24.701
0.000
0.032
20.
30.
40.
50.
15.317
15.514
15.491
14.812
11.310
10.896
10.169
9.904
9.864
9.545
9.319
8.656
33.470
8.449
33.864
33.945
33.979
24.701
24.703
24.716
24.833
25.613
25.717
25.836
25.952
26.002
26.068
26.071
26.258
26.336
0.065
0.098
0.130
0.162
0.189
0.212
0.234
0.256
0.276
0.296
0.315
0.334
0.351
0.368
0.384
0.400
0.416
0.432
0.447
60.
70.
80.
90.
100.
110.
120.
130.
140.
150.
160.
170.
180.
190.
200.
220.
240,
260.
280.
300.
350.
400.
450.
500.
8.614
8.524
8.365
8.299
8.229
8.041
33.471
33.481
33.441
33.550
33.588
33.579
33.670
33,725
33.742
33.700
33.804
26.374
26.415
33.989
34.013
34.041
34.040
26.447
.7.732 34.037
26.579
26.608
26.642
26.686
26.722
26,784
26.854
26.920
7.626
7.558
7.081
7.089
6.622
6.457
6.063
34.054
34.085
34.055
34.103
34.101
34.162
34.181
26.476
26.508
26.335
0.477
0.506
0.535
0.563
0.590
0.655
0.717
0.776
0.831
37 10.5N
li
14.930
14.900
14.883
14.715
14.710
14.656
14.184
13.784
12.098
11.589
10.158
9.774
9.413
9.131
9.067
9.050
8.912
8.772
8,721
8.539
8.450
8.104
7.911
7.718
7.479
7.342
6.869
6.502
6.080
122 55.4W
33.442
24.808
33.439
33.430
33.423
33.423
33.418
33.401
33.409
33.419
33.424
33.613
33.677
33.761
33.834
33.894
33.906
33.938
33.957
33.962
24.812
24.809
24.840
24.841
24.849
24.935
25.025
25.365
25.464
25.865
25.979
26.104
26.206
26.264
26.276
26.323
26.359
26.371
26.411
26.431
26.525
26.572
26.612
26.651
26.674
26.770
26.831
26.915
33.977
33.985
34.038
34.062
34.076
34.082
34.087
34.125
34.140
34.177
0— 500
0.000
0.031
0.063
0.094
0.126
0.157
0.188
0.217
0.245
0.271
0.294
0.315
0.335
0.354
0.372
0.389
0.406
0.424
0.4.40
0.457
0.473
0,504
0.534
0.563
0.592
0.620
0.686
0.749
0.808
0.865
VERTICAL PROFILES
OCTOBER 1984
101 (-)
STATION
STATION 401
10.0
I
I
I
15.0
I
20.0
1T1
33.0
34.2
33.8
Ii
34.8
I
I
24.0
I
100 —
100
200 -
200 —
200
300
300 —
300 -
400 -
400 -
400
500
500 —
500
1984
STATION
102
25.0
26.0
I
100 -
OCTOBER
)
SIGMA—T
TEMPERkTETRE
5.0
(
(
27.0
STATION 402
)
TEMPERATURE
SIGMA—T
100
100
100
200
200
200
300
300
300
400
400
400
500
500
500
28.0
I
I
(
)
OCTOBER 1984
STATION
103
(
STATION 403
)
TEMPERATURE
)
(
)
SIC
100
100
100
200
200
200
300
300
300
400
400
400
500
500
500
OCTOBER 1984
(
STATION
106 (
STATION 406
)
TEMPERATURE
10.0
SIGMA—T
100
100
100
200
200
200
300
300
300
400
400
400
500
500
500
OCTOBER 1984
109
STATION
TEMPERATURE
STATION 409
)
(
SALiNITY
20.0
33.0
100
100
200
200
200
300
300
300
400
400
400
500
500
500
STATION
111 (•
(
)
24.0
100
OCTOBER 1984
)
SIC MA—T
34.8
33.8
(
STATION 411
)
TEMPERATURE
100
100
200
200
300
300
300
400
400
400
500
500
500
OCTOBER 1984
STATION
TEMPERATURE
5.0
10.0
114
(•
STATION 414 (
)
)
SIGMA—T
SALThflTY
24.0
15.0
100
100
100
200
200
200
300
300
300
400
25.0
25.0
28.0
.0
400
500
500
OCTOBER 1984
STATION
500
117
STATION 417
)
TEMPERkTDBE
100
100
100
200
200
200
300
300
300
400
400
400
500
500
500
(
)
OCTOBER 1984
STATION
119
(
STATION 419
)
TEMPERATURE
(
)
(
)
SIGMA—T
100
100
100
200
200
200
300
300
300
400
400
400
500
500
500
OCTOBER 1984
STATION
TEMPERATURE
120
(
STATION 420
)
SALThflTY
20.0
33.0
SIGMA—T
33.5
100
100
100
200
200
200
300
300
300
400
400
400
500
500
500
OCTOBER 1984
10.0
5.0
•1
15.0
121
STATION
STATION 421
)
(•
24.0
20.0
sIaMk—T
28.0 27.0
I
100
100
200 -
200
200 -
300
300
300 -
400 -
400
400 -
500
500
500 -
OCTOBER 1984
TEMPERkTURE
10.0
15.0
I'll liii
28.0
j
100
5.0
25.0
)
(
1z2(•
STATION
)
422(
STATION
SLLThJTrY
20.0
33.0
33.6
34.2
34.8
I
I
100-
100—
100—
200-
200—
200-
300-
300—
300-
400-
400—
400-
500—
500—
500-
I
)
OCTOBER 1984
STATION
STATION
123
10.0
15.0
20.0
33.0
ii
33.6
24.0
34.6
34.2
100
100
200
200
200
300
300
300
400
400
400
600
500
500
OCTOBER 1984
STATION
TEMPERATEJRE
10.0
15.0
20.0
33.0
25.0
26.0
27.0
26.0
I
I
100
5.0
)
(
SIGMA—T
RATEJRE
5.0
423
124
STATION
)
SALINITY
34.2
424
)
(
SIGM&—T
34.8
33.8
24.0
I
25.0
28.0
I
I
100
100
100
200
200
200
300
300
300
400
400
400
500
500
500
28.0
27.0
I
I
OCTOBER 1984
STATION
127 (•
)
STATION 427
(
)
STATION 430
(
)
TEMPERATURE
100
100
100
200
200
200
300
300
300
400
400
400
500
500
500
OCTOBER 1984
5.0
100
TEMPERATURE
10.0
15.0
STATION
130
)
(
SIGMA—T
SALThflTY
20.0
34.2
34.8
24.0
100
100
200
200
300
300
300
400
400
400
500
500
500
.0
OCTOBER 1984
STATION
131 (
STATION 431
)
TEMPERATURE
)
(
SIGM.A—T
25.0
100
100
200
200
200
300
300
300
400
400
400
500
500
500
OCTOBER 1984
STATION
134
STATION 434 (
)
TEMPERATURE
SIGMA—T
34.2
34.8
24.0
100
100
100
200
200
200
300
300
300
400
400
400
500
500
500
25.0
)
OCTOBER 1984
TEMPERATURE
5.0
10.0
15.0
137 (•-)
STATION
SALINITY
20.0
33,0
33.5
437
STATION
(
)
SIGMA.—T
34.2
34.8
24.0
25.0
26.0
27.0
26.0
I
I
100
100
100
200 —
200 -
200
300 —
300 -
300
400
400 -
400
500-
500-
500—
OCTOBER
1984
10.0
15.0
STATION 438
STATION
TEMPERATURE
5.0
-
)
SALINITY
20.0
33.0
33.8
34.2
I
34.8
24.0
I
25.0
28.0
I
-
100 —
100
200—
200—
200-
300—
300-
300-
400—
400-
400—
500-
500-
500—
100
(
27.0
28.0
OCTOBER 1984
TEMPERkTtTRE
10.0
15.0
5.0
I
I
I
STATION
139 (
STATION 439
)
20.0
24.0
25.0
25.0
)
(
27.0
28.0
I
100 -
100
100
200 -
200
200 —
300 -
300
300 -
400 -
400
400 -
500 -
500
500
OCTOBER
1984
STATION
142
(•
STATION
)
442
SIGMA—T
33.0
33.6
34.2
100
100
100
200
200
200
300
300
300
400
400
400
600
500
500
(
)
OCTOBER 1984
STATION
145 (•-)
STATION 445
TRMPERATtTRE
(
)
(
)
SIGMk—T
100
100
100
200
200
200
300
300
300
400
400
400
500
500
500
OCTOBER 1984
STATION
146
STATION
)
(
TEMPERATURE
446
SIGMA—T
20.0
33.0
33.6
34.2
25.0
34.8
100
100
100
200
200
200
300
300
300
400
400
400
500
500
500
28.0
27.0
28.0
OCTOBER 1984
TEMPERATURE
15.0
STATION
149
(•
STATION 459
)
)
(
)
SIGMA—T
20.0
100
100
200
200
200
300
300
300
400
400
400
500
500
500
OCTOBER 1984
(
STATION
152
(•
STATION 452
)
SIGMA—T
24.0
25.0
28.0
27.0
I
—
100
100
100 —
200
200
200
-
300
300
300
-
400
400
400 -
500
500
500 -
28.0
OCTOBER 1984
TEMPERATURE
5.0
10.0
15.0
155 (-)
STATION
33.8
34.2
I
I
34.8
24.0
100
—
100
200 —
200
-
200
300-
300-
300—
400—
400 -
400
500
500 —
500
OCTOBER 1984
STATION
156
25.0
15.0
20.0
33.0
33.6
34.2
I
28.0
28.0
27.0
STATION
)
(-
-
SALiNITY
10.0
)
(
I
—
5.0
455
SALiNITY
20.0 33.0
I
100
STATION
456
)
(
SICMA—T
34.8
24.0
I
100
100 -
100
200-
200—
200-
300
300 —
300 -
400—
400-
400—
500 -
500
500 —
—
25.0
26.0
27.0
28.0
OCTOBER 1984
STATION
159
(•
STATION 459
)
TEMPERA.TEIRE
)
SIGMA—T
100
100
100
200
200
200
300
300
300
400
400
400
500
500
500
OCTOBER 1984
STATION
162
(•
STATION 462
)
TEMPERATURE
15.0
(
SIGMA.—T
20.0
100
100
100
200
200
200
300
300
300
400
400
400
500
500
500
(
)
OCTOBER 1984
STATION
165
(•
STATION 465
)
(
)
(
)
SIGMA—T
100
100
100
200
200
200
300
300
300
400
400
400
500
500
500
OCTOBER 1984
STATION
166
(•
STATION 466
)
SALDJITY
100
100
200
100
200
300
300
300
400
400
400
500
500
500
OCTOBER 1984
STATION
169
(
STATION 469
)
)
(
)
SIGMA—T
TEMPERATURE
25.0
100
100
100
200
200
200
300
300
300
400
400
400
500
500
500
OCTOBER 1984
(
STATION
172
(
33.8
27
STATION 472
)
TEMPERATURE
33.0
28.0
34.2
t
100 —
100
200-
200
300 -
300
400
400 -
400
500
500 -
500
OCTOBER 1984
176
STATION
STATION
(•-)
476
)
(
SIGMA—T
5.0
•1
10.0
I
I
I
20.0
15.0
I
I
I
33.0
I
I
100 —
100
100
200 —
200
200
300 —
300
300
400 —
400
400
500 —
500
500
OCTOBER 1984
STATION
177
STATION
)
TEMPERATURE
5.0
10.0
15.0
28.0
27.0
28.0
I
I
I
25.0
24.0
34.6
34.2
33.6
477
)
(
SIGMA.—T
20.0
33.0
33.6
34.2
24 0
34.8
I
I
25.0
28.0
l
100
100
100
200
200
200
300
300
300
400
400
400
500
500
500
27.0
28.0
OCTOBER 1984
TEMPERATURE
10.0
5.0
I
I
III
15.0
178(
STATION
STATION
)
IIIj
I
I
-
I
24.0
34.8
34.2
33.6
33.0
S
I
I
100
100—
200
200 -
200
—
300
300
300
—
400 -
400 -
500—
500 -
STATION
26.0
27.0
'
I
500—
180(
STATION
)
'Do
200
200
28.0
400—
.
TEMPERATURE
100
25.0
.I\I
h—.-—
100-
100
)
SIGMA—T
20.0
.
OCTOBER 1984
478(
300
300
300
400
400
400
500
500
500
480(
)
OCTOBER 1984
STATION
181 (
STATION 481
)
(
)
(
)
SIGMA—T
100
100
200
200
200
300
300
300
400
400
400
500
500
500
OCTOBER 1984
STATION
TEMPERATURE
10.0
15.0
182
(
STATION 482
)
SALINITY
SIGMA—T
100
100
100
200
200
200
300
300
300
400
400
400
500
500
500
OCTOBER 1984
STATION
184
STATION 484
)
(
TEMPERATURE
100
100
100
200
200
200
300
300
300
400
400
400
500
500
500
OCTOBER 1984
STATION
TEMPERATURE
15.0
187
SALINiTY
33.5
34.2
20.0
)
(
SIGMA—T
34.8
100
100
200
200
300
300
400
400
400
500
600
500
(
)
OCTOBER 1984
STATION
190 (
STATION 490
)
)
(
TEMPERATURE
15.0
20.0
34.2
25.0
34.8
28.0
27.0
100
100
200
200
200
300
300
300
400
400
400
500
OCTOBER 1984
26.0
500
STATION
198 (•
STATION 495
)
SLLINITY
)
(
SIGMA—T
28.0
100
100
200
100
200
300
300
300
400
400
400
500
500
500
OCTOBER 1984
TEMPERATtJRE
5.0
10.0
15.0
201
STATION
(-)
33 0
34.2
33.8
24.0
34.8
100
100 -
100
200-
200-
200-
300—
300-
300-
400 —
400
400 -
500 —
500
OCTOBER 1984
STATION 202
10.0
15.0
)
(
20.0 33.0
34.8
34.2
33.6
I
I
28.0
27.0
26.0
-
-
503
STATION
SALINiTY
TKMPERA.TURE
5.0
500
—
25.0
)
(
III
SALINTI'Y
20.0
492
STATION
24.0
25.0
I
I
100-
100—
100—
200-
200—
200—
300-
300—
300—
400-
400—
400—
500
500—
500—
SIGMA—T
26.0
27.0
I
)
(
28.0
STATION 205
OCTOBER 1984
TEMPERATURE
15.0
10.0
(•
STATION 500
)
SIG)Lk—T
20.0
33.0
100
100
100
200
200
200
300
300
300
400
400
500
500
(
)
OCTOBER 1984
5.0
TEMPERATURE
10.0
15.0
600
STATION
SALINTI'Y
20.0
33.0
33.6
34.2
24 0
34.8
100
100
100
200
200
200
300
300
300
400
400
400
500
500
500
OCTOBER 1984
25.0
10.0
15.0
27.0
28.0
27.0
28.0
STATION 601
TEMPERkTtJRE
5.0
I'
26.0
SIGMA.—T
20.0
33.0
33.6
34.2
ii
34.8
24.0
I
100
100 —
100
200
200 —
200
300
300 —
400
400 —
400
500
500 —
500
S
300
25.0
26.0
OCTOBER 1984
STATION 602
SIG
TEMPERkTtTRE
27.0
100
100
200
200
300
300
300
400
400
400
500
500
500
100
OCTOBER 1984
STATION 603
TEMPERATURE
SIGMá.—T
SALINTFY
34.2
100
100
100
200
200
200
300
300
300
400
400
400
500
500
500
25.0
OCTOBER 1984
STATION 605
TEMPERATURE
SIGMA—I
100
100
100
200
200
200
300
300
300
400
400
400
500
500
500
OCTOBER 1984
STATION 607
TEMPERATURE
SIGMA—I
5,
25.0
100
100
100
200
200
200
300
300
300
400
400
400
500
500
500
28.0
27.0
28.0
STATION 609
OCTOBER 1984
TEMPERATURE
10.0
15.0
SIGILA.—T
SALINTFY
20.0
33.6
34.2
34.8
24.0
100
100
100
200
200
200
300
300
300
400
400
400
500
500
500
OCTOBER 1984
STATION 614
TEMPERATURE
SALINITY
SIGM&—T
24.0
100
100 —
200
200
-
300
300
-
400
400
400
-
500
500
500
—
25.0
25.0
27.0
28.0
OCTOBER 1984
STATION 616
TEMPER1LTURE
SIGMA—T
33.0
33.8
34.2
34.8
25.0
100
100
100
200
200
200
300
300
300
400
400
400
500
500
500
OCTOBER 1984
28.0
STATION 618
SIGMA—T
100
100
100
200
200
200
300
300
300
400
400
400
500
500
500
27.0
28.0
OCTOBER 1984
STATION 620
TEMPERkFURE
25.0
100
100
100
200
200
200
28.0
300
300
400
400
400
500
500
500
OCTOBER 1984
STATION 622
SIGMA—T
TEMPERATURE
100
100
100
200
200
200
300
300
300
400
400
400
500
500
500
27.0
28.0
OCTOBER 1984
STATION 827
ZIGMA—T
TEMPERATURE
100
100
200
200
200
300
300
300
400
400
400
500
500
500
OCTOBER 1984
STATION 629
TEMPERATURE
SIGMA—T
SALThJTTY
34.2
34.8
100
100
100
200
200
200
300
300
300
400
400
400
500
500
500
OCTOBER 1984
STATION 631
SALINITY
25.0
100
100
100
200
200
200
300
300
400
400
500
500
OCTOBER 1984
28.0
500
STATION 633
SIGMA—T
25.0
100
100
100
200
200
200
300
300
300
400
400
400
500
500
500
OCTOBER 1984
STATION
635
SIGILA.—T
TKMPERILTURE
34.2
34.8
24.0
100
100
100
200
200
200
300
300
300
400
400
400
500
500
500
OCTOBER 1984
STATION
640
SIGMA.—T
TEMPERATURE
5.0
10.0
I
I
I
I
I
20.0
15.0
I
I
I
33.0
I
33.8
34.2
Fj
34.8
25.0
24.0
I
I
100
—
100 -
100 -
200
-
200 -
200 -
300
—
300 -
300 -
400
—
400 -
400 -
500—
500—
500—
25.0
28.0
27.0
I
OCTOBER 1984
TEMPERATURE
10.0
15.0
5.0
I
I
642
STATION
20.0
—
I
I
I
II
34.8
34.2
33.8
33.0
I
24.0
100 -
100—
200—
200
200—
300—
300-
300-
400
400
—
400
500
—
500
500
OCTOBER 1984
26.0
28.0
27.0
I
100-
—
25.0
I
STATION 644
SIGMk—T
SALThflTY
TEMPERATURE
28.0
100
100
100
200
200
200
300
300
300
400
400
400
500
500
500
27.0
28.0
OCTOBER 1984
STATION 645
TEMPERATURE
SIGILA—T
26.0
100
100
100
200
200
200
300
300
300
400
400
400
500
500
500
OCTOBER 1984
STATION 648
SIGMA—T
TEMPERATURE
100
100
100
200
200
200
300
800
300
400
400
400
500
500
500
27.0
26.0
POTENTIAL TEMPERATURE - SALINITY PLOTS
OCTOBER 1984
20
18
0
12
B
4
32
33
34.
SALINITY (ppt)
35
OCTOBER 1984
SNkPSHOT
1
20
16
12
8
4
32
33
34
SALINITY (ppt)
35
Fri
Ftj
S
zI.
CD
0)
0)
4s
0
C')
0
S
CD
z
CD
cc
0
a
S
0
MAPS, FULL CCCCS REGION
TEMPERATURE
37
36
35
34
123
122
121
120
TEMPERATURE
37
36
35
34
123
122
121
120
lOOM
TEMPERATURE (DEG C)
37
36
35
34
123
122
121
120
200 M
TEMPERATURE (DEG C)
37
36
35
34
123
122
121
120
TEMPERA'flJRE
37
36
35
34
123
122
121
120
SALINITY
37
36
35
34
123
122
121
120
SALINITY
37
36
35
34
123
122
121
120
lOOM
SALINITY (PPT)
37
36
35
34
123
122
121
120
SALINITY
37
36
34
123
122
121
120
SALINITY
37
36
35
34
123
122
121
120
1OM
SIGMA—T
37
36
34
123
122
121
120
50M
SIGMA—T
37
36
35
34
123
122
121
120
100 M
SIGMA—T
37
36
35
34
123
122
121
120
200
SIGMA—T
M
37
36
35
34
123
122
121
120
400 M
STGMA—T
OCTOBER 1984
26.83
37
26.88
2684
26.86
26.86
/
II
I
I
26.83
0'
36
\.
28.82
26.85
I
__•%
26.86
/
26.84
28.87
26.84
—5
35
(__J
Iii/O)
I
is)
5.83
25.86
28.87
26.84
34
123
122
121
120
DYNAMIC HEIGHT
37
36
35
34
123
122
121
120
DYNAMIC HEIGHT
37
36
35
34
123
122
121
120
50/200 M
DYNAMIC HEIGHT (DYN CM)
37
36
35
34
123
122
121
120
DYNAMIC HEIGHT
100/200 M
CM)
OCTOBER 1984
18.0
17.9
37
z
17.7
17.7
17.6
17.9
17.8
F-'
10 20 30 40 50
CTJRRENI SPEED (CM/S)
36
17.3
17.7
35
I
19.4
19.4
192
19.7
34
123
122
121
120
0/500 M
DYNAMIC HEIGHT (DYN CM)
37
36
35
34
123
122
121
120
DYNAMIC HEIGHT (DYN CM)
37
36
35
34
123
122
121
120
100/500
DYNAMIC HEIGHT (DYN CM)
M
37.
36
35
34
123
122
121
120
DYNAMIC HEIGHT
37
36
35
34
123
122
121
120
0t25.O
DEPTH (M)
37
36
35
34
123
122
121
120
TEMPERATURE (DEG C)
crt=25.O
37
36
35
34
123
122
121
120
SALINITY (PPT)
37
36
35
34
123
122
121
120
37
36
35
34
123
122
121
120
TEMPERATURE
37
36
34
123
122
121
12D
SkLINITY
37
36
35
34
123
122
121
120
37
36
35
34
123
122
121
12D
TEMPERATURE (DEG C
OCTOBER 1984
7.77
37
7.66
7.75
7.59
7.71
I
F.
77&'
36
7.62
7.44
1k.:
_4.4.
4.
I
4.
35
--
4.
1
/7.92
7.67
7.79
34
123
122
121
120
SALINITY (PPT)
37
36
35
34
123
122
121
120
MAPS, SNAPSHOT 1
1OM
TEMPERATURE (DEG C)
OCTOBER 1934
SNAPSHOT 1
35
17.36
17.27
17.27
17.2.3
16.17
16.13
15.95
18.07
34
II
I
121
120
TEMPERATURE (DEG C)
50 M
.35
34
121
120
lOOM
TEMPERATURE (DEC C)
OCTOBER 1.984
SNAPSHOT 1
11
11.38
10.49
35
10.68
10.94
11.14
/
11.47
1135
34
121
120
200M
TEMPERATURE (DEG C)
OCTOBER 1984
SNAPSHOT
1
8.55
8.62
8.92
8.97
35
8.55
8.84.'
8.50
I
9.05
8.83
8.52
'0
ii
p
II I
/
—
I
•
I
—
——
p
'I
I
8.9(
1/'i
8.61
\
I
8.95
¼
854
¼
8.86
..
9.20
—1>854
I
I
/
'
9.25
8.94
A62
9.18
I1
6.63
34
121
120
40DM
TEMPERATURE (DEC C)
OCTOBER 1984
SNAPSHOT 1
8.71
35 —
0'
6.62
i
I
I
I
I
I
8.50
I
I
8.79
——
1
—I
I/
I
-' 6.80
I
I
—
8.88
I
6.66
—
6.88
6.82
8.82
7.00
8.85
5.62
34
121
120
1OM
SALINITY (PPT)
OCTOBER 1984
SNAPSHOT 1
33.48
35
33.45
33.47
3.34',
33.45
3349
33.44
33.57
33.47
33.49
33.49
33.45
3335
33.53
34—
121
120
SALINITY
34
121
120
lOOM
SALINITY (PPT)
OCTOBER 1.934
SNAPSHOT 1
35
33.59
33.55
33.53
33.57
33.63
I
I
33
34
121
120
200M
OCTOBER 1984
SNAPSHOT
1
33.91
II
33.94
—i
I It
I
-
35
r
CA
Ci,
33.99
33.96
a'
33.98,1
33.95
—
33.91
33.98
33.91
33.93
33.99
33.96
33.99
I
I
33.94
33.92
I
33.97
I
33.98
33.99
I'
3397
1 33.92
33.97
34
121
120
SALINITY
35
34
121
120
1OM
SIGMA—T
35
34
121
120
50M
SIGMA—T
35
34
121
120
1DOM
SIGMA—T
35
34
121
120
20GM
SIGMA—T
OCTOBER 1934
SNAPSHOT 1
26.36
(6.43
28.32
2633
35
2617/
26.44
283L
254g
0)
Il)
26.34
26.39
,l'
C',
26.32
2517
26.37
——
28.29
26.31
I
I/
28.32
7
41
—t
26.36
6.33
26.42
25.37
_0
26
26.28
,F
28.26
-I
2517
•C?
26.32
25.39
—
(
34
121
120
40GM
SIGMA—T
OCTOBER 1984
SNAPSHOT
1
26.53
26.82
26.80
35
25.80
26.82
26.7
0'
28.76
I
25.81
26.75
,1
2.8.74
ee
25.79
2è186
2683
26.81
26.82
26.61
25.79
28.82
/2.8.79
26.79
I,
34
121
120
DYNAMIC HEIGHT (DYN
35
34
121
120
0/200 M
DYNAMIC HEIGHT (DYN CM)
OCTOBER 1984
SNAPSHOT
1
z
35
I
O
.
I
I
10 20 30 40 50
CURRENT SPEED (CM/S)
4&5
47.5
51.7
46.0
47.9
5L9
34
121
120
50/200
DYNAMIC HEIGHT (DYN CM)
M
OCTOBER 1984
SNAPSHOT I
z
32.7
35
0
0
10 203040 50
CURRENT SPEED
31
(cM/S)
1.9
32.6
32.9
32.1
32.6
32.4
33
31.2
33.2
32.6
33.4
34—.
121
120
100/200 M
DYNAMIC HEIGHT (DYN CM)
OCTOBER 1984
SNAPSHOT
1
19.7
19.3
20.21
19.1
35
18.8
719.3
19.3,
—a
II
10 20 3040 50
-
.1&4
SPEED (cM/S)
/
119.2
¼
19.8
20
19.9
19.8
2C.3
19.7
34
121
120
DYNAMIC HEIGHT
35
34
121
120
DYNAMIC HEIGHT (DYN CM)
50/500 M
35
34
121
120
100/500 M
DYNAMIC HEIGHT (DYN CM)
OCTOBER 1984
SNAPSHOT 1
p89.9
35
613
613
o
to 20 30 40 50
CURRENT SPEED (CM/S)
62.4
59.4
60.5
60.6
51.5
34
121
120
200/500
DYNAMIC HEIGHT (DYN CM)
M
OCTOBER 1984
SNAPSHOT 1
40.2
35
41
—.
I
o
.
I
to 20 30 40 50
CURRENT SPEED (CM/S)
427
4.0.3
40.2
40.5
41.5
40.8
.1
40.3
34
121.
120
35
34
121
120
TEMPERATURE
35
34
121
120
SALINITY (PPT)
35
34
121
120
DEPTH (M)
OCTOBER 1984
SNAPSHOT 1
116
115
69
35
>//07
00
110
119
107
117
112
104
115
112
34121
120
TEMPERATURE (DEG
35
34
121
120
SALINITY
35
34
121
120
DEPTH (M)
35
34
121
120
.6
TEMPERATURE
OCTOBER
SNAPSHOT
p.91
7.52
35
7.92
I
1
7.89
i
7.53
7.84
II
/ 7.85
I
a''\
.54
_1
7.31
I
I
/I
7.55
i
/I
I
7.85
7.84
7.37
—
7.89
7.84
7.92
7.90
7.81
7.91
•1.96
7.77
7.55
7.92
34
121
120
cTt26.6
SALINITY
OCTOBER 19B4
SNAPSHOT t
34.01
,/34.1o
34.02
35
34.
34.09
34.09
34.03
34.08
34.09
I.1
39'/
'I
/
34.09
I
1
34.09
34.09
34119
34.08
34.09
34.10
34.05
3.4.10
34.01
34.08
34
121
120
MAPS, SNAPSHOT 2
TEMPERATURE (DEG C)
10 M
35
34
iai
120
________________
50M
TEMPERATURE (DEG C)
OCTOBER 1984
SNAPSHOT 2
.1
12.40
35—
I 3.44
12.52
1231
34
—
I
121
120
TEMPERATURE (DEC C)
100 M
35
34
121
120
20GM
TEMPERATURE (DEG
OCTOBER 1984
SNAPSHOT 2
8.85
35
8.61
8.60
-8.52
8.73
8.55
8.82
G.41
8.56
9.56
8.58)
I
tO
9.09
I
,L35
34
121
120
40GM
TEMPERATURE
OCTOBER 1984
SNAPSHOT 2
6.29
6.38
35
6.37
t
t
9.43
I
I
7.24
*01
II
L.58
635
6.57
8.85
6.80
—
'
6.73
1.0
5.53
/I
I
6.69
5.73
5.02
34
121
120
1OM
SALINITY (PPT)
OCTOBER 1984
SNAPSHOT 2
33.25
35
33.47
33.36
33.42
33.43
33.46
33.45
33.41
33.34
33.45
33.46
53.49
33.49
33.45
33.49
33.41
33.42
33.46
33.49
33.44
33.49
33.54
33.55
33.57
34
121
120
50 M
SALINITY (PPT)
35
34
121
120
lOOM
SALINITY (PPT)
35
34
121
120
200M
SALINITY (PPT)
OCTOBER 1984
SNAPSHOT 2
35-
33.98
.00
.01
33.98
——
F
—.33.95
34.00
33.97
34.00
33.97
34.01
33.97
33.99
33.99
33.98
33.92
33.98
33.90
33.98
33.98
3398
33.99/
p.94
34
121
120
400M
SALINITY
OCTOBER 1934
SNAPSHOT 2
34.09
.10
35
34.14
34h9
34rn
C?
I
,1
¼
¼
¼
¼
34.13 ¼.
k05
(
3415
34.11
¼
I
34.10
¼
34.12
34.18
3416
TI3
34
121
120
10 M
SIGMA—T
35
34
121
120
50 M
SIGMA—T
35
34
121
120
100 M
SIGMA—T
35
34
121
120
200M
SIGMA—T
OCTOBER 1984
SNAPSHOT 2
26.36
35—.
25.42
26..30
26.38
26.44
26.41
26.45
26.42
26.22
26.16
26.38
26.33
/
—
34—
121
120
40DM
SICM.A—T
35
34
121
120
DYNAMIC HEIGHT (DYN CM)
0/100 M
35
34
121
120
DYNAMIC HEIGHT
35
34
121
120
DYNAMIC HEIGHT (DYN CM)
50/200 M
35
34
121
120
100/zoo M
DYNAMIC HEIGHT (DYN CM)
OCTOBER 1984
SNAPSHOT 2
19(
19.2
19.1
35
18.7
'II,
t
19.4*
,1
o
to 20 30 40 50
SPEED (cM/S)
18.1
II
18.7
, —.
18.7
—
I 'I
—
16.4
'v
18.8
18.7
ZQ.4
*9.2
19.7
,120.0
34
121
120
DYNAMIC HEIGHT
35
34
121
DYNAMIC HEIGHT
35
34
121
120
100
DYNAMIC HEIGHT (DYN CM)
QOM
OCTOBER 1984
SNAPSHOT 2
z
59.1
59.4
59.6
35
55.1
C.)
o
10 20 3040 50
CURREN'T SPEED (CM/S)
52.2
59.D
58.5
52.1
59.j
59.4
34
121
120
200/500 M
DYNAMIC HEIGHT (DYN CM)
OCTOBER 1984
SNAPSHOT 2
40.1
40.4.
\
40.6
20 30 40 50
CURREN'T SPEED (cM/S)
40.6
42.8
39.8
30.7
417
40.1
40.5 \
39.1
39.0
40
/—
41.0
121
120
DEPTH (M)
35
34
121
120
crt=25.O
TEMPERATURE (DEG C)
OCTOBER 1984
SNAPSHOT 2
1
35
I
3J0
14.10
34
I
121
I
120
tTt2S.O
SALINITY (PPT)
35
34
121
120
35
34
121
120
crt=25.8
TEMPERATURE (DEG C)
OCTOBER 1984
SNAPSHOT 2
10.68
10.85
35
10.82
10.89
/10.81
10.83
0
'-4
10.88
1025
1057
.c,
10.85
10.37 )
10,58
10.55
I 10.85
10.89
10.54
1028
10.5.3
10.58
-,
II
/
1064
10.82
34121
120
SALINITY (PPT)
crt=25.B
35
34
121
120
ut=26.6
DEPTH (M)
OCTOBER 1984
SNAPSHOT 2
35
1392
34
215
e80
278
58
34121
120
6.6
TEMPERATURE (DEG C)
OCTOBER 1984
SNAPSHOT 2
7.7-5
I
35
I
7.87
7.86
7.87
7.85
7.87
7.52
/7.72
7.92
'
7.98
7.57
7.81
7.84
7.79
34
121
120
SALINITY
OCTOBER 1984
SNAPSHOT 2
34.00
I
35
34.10
34.09
34.09
34.02
34.07
34.12
34.01
I/
34.06
34.06
34.09
34.09
34.09
34.09
.3410
34.06
34.05
.1410
34.11
34.06
34.10
34.08
34.06
34.07
34
121
120
DIFFERENCE MAPS, SNAPSHOT 2 MINUS SNAPSHOT 1
TEMPERATURE (DEG C)
10 M
35
34
121
120
50M
TEMPERATURE (DEG C)
SNAPSHOT 2
MINUS
SNAPSHOT
I
35 -
—023
—0.26
—0.42 9
0.02
0.08
0.35
0.05
34I
121
I
120
lOOM
TEMPERATURE (DEG C)
SNAPSHOT 2
MINUS
SNAPSHOT 1
S.
0.34
35
—0.01
I
—0.11
(0.85
—0.41
—0.20
\—
0.30
04;
0.23
34
121
120
TEMPERATURE (DEG C)
200 M
35
34
121
120
40GM
TEMPE RATURE (DEG C
SNAPSHOT 2
MINUS
SNAPSHOT 1
—0.42
-0.03
35
—0.19
—0.14
0.0
052
—0.76
—0.18
—0.44
-0.11
—0.26
—0.07
-0.14
—0.1k
-0.03
—0.23
—0.20
—0.31
—0.38..
—0.10
0.38
34
121
120
SALINITY
35
34
121
120
50 M
SALINITY (PPT)
34
121
120
lOOM
SALINITY (PPT)
35
34
121
120
200M
SALINITY (PPT)
SNAPSHOT 2
MINUS
SNAPSHOT
0.04
-0.07
0.02
0.02
0.03
00
0.03
0.01
0.02
0.02
0.03
0.00
0
.c
-0.010
—0.02
-L
0.02
—0.10
/
-——-S
34
121
120
400M
SALINITY (PPT)
SNAPSHOT 2
MINUS
SNAPSHOT 1
-•0.0I
35 —
—0.00
—0.03
0
01
I
—,
—0.04
—0.03
—0.00
0.01
0.01
0.01-
0,04
0.04
0.02.
34-
I
I
121
I
120
10 M
SIGMA—T
35
34
121
120
50M
SIGMA—T
35
34
121
120
lOOM
SIGMA—T
35
34
121
120
200M
SIGMA—T
SNAPSHOT 2
MINUS
SNAPSHOT
1
0.04
—0.10
C
35
0
0.04
0.05
0
—0.04
0.08
0.06
0.06
0.00
0.07
0.02
0.05
—0.05
0.12
—0.18
0.04
0.03
0.08
-•0
1
34
121
120
400M
SIGMA—T
35
34
121
120
VERTICAL SECTIONS
_____—t,
OCTOBER 1984
TEMPERATURE (DEG C)
119 1201211.2
117
114
111
..— I
/I
12
100
38
c_
_________—11-____ I
37
36
8-
/
35
400
I
80
I___ —
I
20
40
DISTANCE OFFSHORE (EM)
80
OCTOBER 1984
TEMPERATURE (DEG C)
152
0
100
10__________
155
38
/
37
___•____••___—9 —
38
300 —
—
35
400
I
80
iI'
I
20
40
80
DISTANCE OFFSHORE (EM)
0
34
120
OCTOBER 1984
TEMPERATURE (DEC C)
38
100
37
38
300
35
400
34
DISTANCE OFFSHORE (1(k)
OCTOBER 1984
TEMPERATURE (DEC C)
0
100
—
38
12
10
9 200
37
9-
I-
38
300
35
400
40
DISTANCE OFFSHORE (1(k)
34
120
OCTOBER 1984
TEMPERATURE (DEG C)
446
0
455
452
449
38
12—"
100 —
37
10
—9
38
..—
35
400 —
I
80
80
I
I
I
20
40
0
34
DISTANCE OFFSHORE (1CM)
TEMPERATURE (bEG C)
OCTOBER 1984
38
100
37
200
38
hoo
35
400
80
DISTANCE OFFSHORE (1CM)
34
120
TEMPERLTURE (DEC C)
899
0
697
I
OCTOBER 1984
605
I
603 602
60600
38
I
37
I
I
38
300
I
35
80
80
40
20
DISTANCE OFFSHORE (1CM)
(DEC C)
0
34
OCTORER 1984
38
37
200
38
35
34
DISTANCE OFFSHORE (iaO
120
OCTOBER 1984
TEMPERLTURE (DEG C)
627
629
633
631
635
38
I
1O—
100
37
38
300 —
35
400509oo
80
20
40
DISTANCE OFFSHORE (1CM)
0-
645
34
OCTOBER 1984
TEMPER&TUR.E (DEG C)
646
0
644
642
840
38
/
37
200—
-
38
300-
7—
35
400 —
6
502oo
80
40
20
60
DISTANCE OFFSHORE (Kg)
0
34
120
(DEC C)
OCTOBER 1984
38
37
36
35
34
)IOBTE
fl
DISThNCE ALONGSHORE (1cM)
TEMPERATURE (DEC C)
208 195 184 169 162 149
I.
I
OCTOBER 1984
142 134
127 117
108
38
I
12
100 —
-
-d
37
36
30Q
s5
400
—
50140
I
100
80
80
40
DISTANCE ALONGSHOEE (1CM)
20
0
34
120
OCTOBER 1984
TEMPERATURE (DEG 0)
211 192 157 186 155
U
100
--
I
I-
I
146 145 131
I
130
114
I
—
37
10
9
200 —
38
300
1
I
35
I
I
120
NORTH
100
80
80
40
DISTANCE ALONGSHORE (KM)
TEMPERATURE (flEa C)
20
0
sotrra
:34
OCTOBER 1984
38
37
200
-I
38
35
40
NORTH
DISTANCE ALONGSHORE (XM)
34
120
0
OCTOBER 1984
TEMPERATURE (DEG C)
484 469 462 419 442 434 427 417 446
100 —
38
37
200 —
38
300 —
35
400 —
6
I
120
100
80
60
40
DISTANCE ALONGSHOEE (EM)
TEMPERATURE (bEG C)
20
0
34
OCTOBER 1984
38
0
100
37
200
38
300
35
400
120
NORTh
100
80
80
40
DISTANCE ALONGSHORE (EM)
34
20
SOUTE
OCTOBER 1984
TEMPERATURE (DEG C)
-S
250
300
200
SOUTH
DISTANCE ALONGSEORE (IQL)
OCTOBER 1984
TEMPERATURE (DEs C)
644
631
417
484
605
618
38
100
37
36
300
35
350
300
250
200
150
DISTANCE ALONGSRORE (KhL)
100
50
0
SOtTIH
34
120
1984
TEMPERATURE (DEG C)
627
648
622
609
480
411
38
100
37
38
300
35
400 —
I
350
300
250
200
150
100
DISTANCE ALONGEHORE (1CM)
50
0
34
120
(P1'?)
OCTOBER 1984
38
37
38
35
34
DISTANCE OFFSHORE (KM)
SALINiTY (P1'?)
OCTOBER 1984
38
SNAPSHOT 1
-
37
38
35
80
80
40
DISTANCE OFFSHORE
34
123
122
121
120
SALINTN (PPT)
OCTOBER 1984
38
37
38
35
34
DISTANCE OFFSHORE (1CM)
SALINTI'y (PPT)
OCTOBER 1984
38
0
100
37
200
36
ths
300
35
400
34
DISTANCE OFFSHORE
(flQ
123
122
121
220
skuNrrY (PP'r)
OCTOBER 1984
38
100
37
36
35
400
34
OFFSHORE (EM)
38
a
100
37
-d
'-4
35
400
SO
DISTANCE OFFSHORE (1CM)
34
120
SALIN1TY (PPT)
OCTOBER 1984
38
37
38
n
35
34
DISTANCE OFFSHORE (1CM)
SALINITY (PPT)
OCTOBER 1984
38
37
' 200
36
35
34
DISTANCE OFFSHORE (nO
OCI'OBER 1984
SA.LINrTY (PPT)
629
o
/
635
633
631
I
I
100
33.6
—
/
38
/
37
1
200 —
38
300
34.1
/
400
35
0
34
DISTANCE OFFSHORE (1CM)
OCTOBER 1984
SALINiTY (PPT)
100
646
645
644
642
640
38
I
—
37
—
/
200 —
36
300 —
35
400 —
I
80
I
I
60
40
20
DISTANCE OFFSHORE (KM)
0
34
SALINFFY (PPT)
OCTOBER 1984
38
37
36
300
35
34
40
DISTANCE ALONGSHORE (lot)
B°tJTB
38
37
200
36
n
35
100
NOflZ
DISTANCE ALONGSHORE (101)
Sn
125
122
121
120
(PP'r)
211
1984
192 167 166 165 146 145 131 130 114
109
38
37
S.
—
38
35
-
120
100
80
80
40
ALONGSHORE (1cM)
20
0
34
38
0
100
37
S.
38
300
35
400
100
DISTANCE
80
60
40
(1CM)
34
SALINITY (PPT)
0
100
OCTOBER 1984
484 469 462 449 442 434 427 417
406
38
'EE
-
37
200
38
300
35
400 —
I
120
NORTE
100
60
80
40
DISTANCE ALONGSHORE (Kkl)
I
20
SALINiTY (PPT)
0—
0
34
120
1984
467 466 465 446 445 431
43D 414
409
38
100 —
37
6
200
—
38
300 —
35
400-
-
120
100
DISTANCE
8604020
(Ickc)
0
123
SALINiTY (PPT)
OCTOBER 1984
38
37
38
35
34
DISTANCE ALONGSEORE (IOL)
SOUTH
OCTOBER 1984
0
644
100
&51
618
—
484
605
417
38
37
38
300
35
400
300
WORTH
250
DISTANCE
200
50
150
(KM)
0
sOirrE
34
123
122
121
120
OCFOBER 1984
SALINITY (PPT)
648
627
411
490
609
622
38
100
37
38
300
35
40050
I
350
300
250
200
I
150
DISTANCE ALONGSHORE (1CM)
100
50
0
SOUTE
1984
SIGMA—T
38
0
100
37
-S
-I
38
300
35
400
34
DISTANCE OFFSHORE (Ku)
OCTOBER 1984
146
149
152
—
155
38
—
100
__—
37
7
26.2— /
200 —
2.6.4
36
300 —
35
400 —
I
60
-1
I
I
80
40
20
DISTANCE OFFSHORE (Ku)
0
34
120
SIGMA-T
1984
38
37
36
35
34
DISTANCE OFFSHORE (1CM)
1984
SIGM&—T
414
411
0
417
419
38
,..I—
10±
200
37
L
38
—
35
400 —
I
502oo
80
I
I
I
I
60
40
20
DISTANCE OFFSHORE (1CM)
0
34
SIGMk—T
OCTOBER
446
449
452
1984
455
38
—
37
———25.2—--
/
/
/
38
/
35
—
'be
I
80
I
80
40
20
DISTANCE OFFSHORE (Kit)
0
34
OCTOBER 1984
SIGMA—T
38
100
37
38
35
400
509go
80
60
40
20
DISTANCE OFFSHORE (KM)
0
1984
SIGMA—T
38
37
38
35
34
40
DISTANCE OFFSIHORE (x'!)
1984
38
5.
100
—.--------—-------—-----
37
200
38
C-
300
35
400
SOIoo
80
40
60
DISTANCE OFFSHORE
20
34
120
//
OCTOBER
SIGMI&—T
627
629
631
633
535
1984
38
37
/7
—
38
300 —
400 —
I
502 00
80
80
I
40
21)
0
34
DISTANCE OFFSHORE (Ku)
SIGMA—T
OCTOBER 1984
38
200
36
35
34
DISTANCE OFFSHORE (KM)
120
SIGMA-T
OCTOBER 1984
38
37
36
300
35
34
80
DISTANCE
SIGMA—T
100
200
OCTOBER 1984
208 195 184
0
SOVTfl
(1CM)
169 162 149
142 134
127 117
106
38
--
37
—
36
300 —
400
-
35
I
120
I
100
80
80
40
DISTANCE ALONGSBDRE (1CM)
20
0
SOIJTR
34
123
122
121
120
OCTOBER 1984
38
100
37
36
300
35
400
50940
)1ORTK
00
60
100
DISTANCE ALONGSHORE (IckO
34
OCTOBER 1984
38
37
200
I,,
38
35
34
DISTANCE ALONGSHORE (Ku)
OCTOBER 1984
SIGMA—T
38
100
37
'-V
38
35
400
50?40
120
100
80
80
40
DISTANCE ALONG$HORE (1CM)
OCTOBER 1984
487 456 465 446 445 431 430 414
gIGM.&—T
0
34
20
-
38
100 —
37
'-V
-
200
—
38
I
300
—
35
400
50146__J_
I
120
100
80
80
40
DISTANCE ALO}JGSHORE (KkC)
20
0
80UTh
34
120
OCTOBER 1984
SIGMA—T
38
37
a
38
35
34
SOUTH
DISTANCE ALONGSHORE (IQL)
OCTOBER 1984
-.
644
618
631
100 —
605
38
28.0
37
.4
200
•
38
35
I
-
35D
I
300
I
I
I
200
150
100
DISTANCE ALONGSEORE (IOL)
250
I
50
0
SOtTTE
34
120
OCTOBER 1984
SIGMk—T
38
3?
36
F-'
n
35
250
34
200
DISTANCE ALONGEHORE
(1CM)
WErE
cURREN'r (cM/s)
1984
38
100
37
38
hoo
35
400
34
DISTANCE OFFSHORE (KLt)
CURRENT (CM/S)
OCTOBER 1984
0
38
100
37
e-.
36
F-
35
400
SdIoo
BC)
40
60
DISTANCE OFFSHORE (KM)
34
120
1984
CURRENT (CM/s)
38
100
37
36
35
DISTANCE OFFSHORE (Ilk)
CURRENT (CM/S)
OCTOBER 1984
38
100
3?
38
300
35
400
34
DISTANCE OFFSHORE (Ia!)
CURRENT (CM/s)
OCTOBER 1984
0
38
100
37
-I
35
35
400
34
50
DISTANCE OFFSHORE
CURRENT (CM,'S)
OCTOBER 1984
477
0
38
100
27
35
C-
35
400
34
DISTANCE OFFSHORE
120
1984
CURRENT (CM/s)
38
100
37
-%
38
300
35
400
34
DISTANCE
(Ku)
CURRENT (CM/S)
1984
38
100
37
200
38
300
35
400
34
DISTANCE OFFSHORE (Ku)
CURRENT (c}L/S)
OCTOBER 1984
38
37
38
123
DISTANCE OFFSHORE (1CM)
OCTOBER 1984
CURRENT (CM/S)
648
545
-3
844
J
642
840
—
/
100—
200 —
38
37
36
300
—
35
400I
80
I
I
50
40
DISTANCE OFFSHORE (1CM)
20
34
120
CURRENT (cM/s)
OCTOBER 1984
38
37
36
35
400
34
NORTH
DISTANCE ALONGSHORE (1CM)
CURRENT (CM/S)
SOUTH
OCTOBER 1984
38
37
36
C.-
300
35
400
34
DISTANCE ALONGSHORE (IQL)
SOUTH
120
OCTOBER 1984
CURRENT (cM/S)
38
100
37
36
300
35
400
80
60
34
40
DISTANCE ALONGSIIORE (Ku)
CURRENT (cM/S)
481 4
OCTOBER 1984
424 420
100
403
36
37
38
35
400
34
WORTE
DISTANCE ALONGSHORE (RIO
120
CURRENT (cM/s)
OCTOBER
1984
38
0
100
37
36
300
35
400
100
NOETH
80
60
40
0
DISTANCE ALONGSHORS (1CM)
38
100
37
36
C-
300
35
400
34
ROBTE
DISTANCE ALONGSHORE (KM)
SOUTE
120
OCTOBER 1984
CURRENT (cM/S)
38
37
38
35
300
250
34
200
DISTANCE ALONGSHORE (ICW)
SOtT!H
OCTOBER 1984
CURRENT (CM/S)
38
37
38
35
150
DISTANCE ALONGSEIORE
34
sotrra
CURRENT (CM/s)
1984
38
100
37
38
35
400
34
NORffl
DISTANCE ALONGSHORE (1CM)
DIFFERENCE SECTIONS, SNAPSHOT 2 MINUS SNAPSHOT 1
SNAPSHOT 1
SNAPSHOT 2
TEMPERATURE (DEC C)
38
0
100
37
36
300
35
400
SOIoo
34
80
40
DISTANCE OFFSHORE (EM)
SNAPSHOT 2 ILNUS SNAPSHOT
TEPERATURE (DEC C)
446
449
452
1
455
38
3?
38
35
123
DISTANCE OFFSHORE (EM)
2 MINUS SNAPSHOT 1
TEMPERATURE (DEC C)
490
484
480
38
1.00
3?
36
300
35
400
34
80
40
DISTANCE OFFSHORE (EM)
SNAPSHOT 2 MDJUS SNAPSHOT 1
TEMPERATURE (DEG C)
500 485 481 472 459 452 439 437 424 420
19 137
403
38
3?
36
35
34
NORTE
DISTANCE ALONGSHORE (EM)
SNAPSHOT 2 MINUS SNAPSHOT 1
TEMPERATURE (DEG C)
38
100
37
—'
w
/
/
300
'C
a
I
38
35
_.,
400
34
DISTANCE ALONGSHORE (Ku)
SNAPSHOT 2 MNtJS SNAPSHOT 1
TEMPERATURE (bEG C)
38
37
38
35
worm
80
100
80
DISTANCE ALONGSHORE (1CM)
34
SOUTE
2
1
0
100
40
SNAPSHOT 2
(PPT)
SNAPSHOT 1
38
35
34
DISTANCE OFFSHORE (KIt)
SNAPSHOT 2 MIMTJS SNAPSHOT 1.
SALINiTY (PPT)
487
38
37
36
35
34
DISTANCE OFFSHORE
(1CM)
SNAPSHOT 2 MiNUS SNAPSHOT 1
(P71)
38
37
36
35
34
NORTH
DISTANCE ALONGSHORE
(fat)
123
122
121
120
SNAPSHOT 2 IONUS SNAPSHOT 1
38
37
36
35
34
DISTANCE ALONGSHORE (1CM)
SOUTE
SNAPSHOT 2 MNIJS SNAPSHOT 1
SALThIFfl' (PPT)
38
3?
36
35
100
3iOBTB
80
80
34
40
DISTANCE ALONGSHOEE (1CM)
SOUTh
1
38
37
36
300
35
34
OFFSHORE
SNAPSHOT 2
SNAPSHOT 1
38
37
36
85
34
OFFSHORE
120
SNAPSHOT 2 M]NUS SNAPSHOT 1
SLGMk-1T
487
484
48381 480
478 477
38
37
36
35
80
123
80
40
DISTANCE OFFSHORE (Ku)
SNAPSHOT 2
SNAPSHOT 1
38
37
-4
36
35
34
WORTH
DISTANCE ALONGSHORE (ICLO
123
122
121
120
SNAPSHOT 2
SNAPSHOT 1
484 489 462 449 442 434 427 417
142 1J4 127 117
208 195 184 169 162 149
I
I
I
I
406
I
106
38
37
—
20036
30035
400
ran
120
NOZtE
100
80
DISTANCE
60
40
(1CM)
20
0
34
SOUTH
SNAPSHOT 2 MNUS SNAPSHOT 1
36
37
36
35
100
NORTH
34
80
DISTANCE ALONGSHORE (1CM)
SOUTH