CENTRAL CALIFORNIA COASTAL CIRCUlATION STUDY
CTD OBSERVATIONS
CRUISE 8501, JANUARY 1985 by
Dudley B. Chelton
P. Michael Kosro
/College of Oceanography,
Oregon State University1
Corvallis, Oregon 97331
Data Report 129
Reference 87-05
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 fourth 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
*Overview of January 1985 oceanographic and meteorological conditions
..
*Sampling Procedures
*Caljbratjon j iii
1
6
12
15
18
Data Processing
Data Presentation
Acknowledgements
References
21
26
27
Figure Sections
Locations, times, and depths of January 1985 CTD stations
Maps of January 1985 CTD station locations and bathymetry
Data Listings at Selected Depths
Vertical Profiles
Temperature -
Plots
Maps, Full CCCCS Region
Maps, Snapshot Region
Vertical Sections
* text in sections marked with an asterisk is different in each of the four
CCCCS CTD Data Reports.
The other sections are essentially identical for all four reports.

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, a.1, dynamic height and relative geostrophic velocity from a total of
73 CTD casts made between 24 January 1985 and 4 February 1985,

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 (tide gauge) observations (hourly interval).
(b)
(4) Infrared satellite imagery (including all sufficiently clear images).
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 8501 carried out from 24 January 1985 to 4 February 1985.
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 desire to relate the CCCCS measurements to historical Lata at the same the 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
38°N
36°
127°W 125° 123° 121°
Fig. 1.
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 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.

Table 1.
Time, date and Raytheon CTD station number for selected milestones during the January 1985 CCCCS cruise.
Milestone time (PST) start of snapshot
CTD winch failure; steam to
Pt. Hueneme for repair restart CTD operations end of snapshot anchor behind Pfeiffer Point due to poor weather (20-30 kt winds and 8-10 ft seas) restart CTD operations anchor at Santa Cruz due to poor weather (20-35 kt winds and 8-14 ft seas) restart CTD operations last CTD station
1023
0616
1746
0600
0631
0601
0521 date
Jan.
24, 1985
Jan.
25, 1985
Jan.
26, 1985
Jan.
28, 1985
Jan.
30, 1985
CTD station no.
1
14
108
.
Feb.
1, 1985
Feb.
2, 1985
131
Feb.
3, 1985
Feb.
4, 1985
146
167

5
37
36
35
34
Fig.
2.
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 triangles.
Current meter moorings and NDBC buoys are identified by letters and numbers, respectively.

6
"snapshot region" 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 snapshot 2.
once.
For the January 1985 survey, the snapshot region was sampled only
Some of the important milestones of the January 1985 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.
The locations of the CCCCS CTD stations are shown in Fig. 2.
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 JANUARY 1985 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.
The strongest equatorward winds occur in May and June.
The average January 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 by NDBC buoy 46028 (Fig. 2) from 6 December 1984 to 7 February 1985 are shown in Fig. 4.
The most noteworthy feature of the winds during this time period was a strong equatorward pulse on 14 December.
Otherwise, the winds during December and early January fluctuated between moderately strong equatorward and poleward events.
After the first week of January, winds remained generally equatorward and gradually increased in intensity by the end of this 2-month period.
A map of vector winds measured by a hand-held anemometer on board the ship
at most of the CCCCS CTD stations during the January 1985 snapshot is shown in
Fig.
5.
Consistent with the time series of winds measured at NDBC buoy 46028 after the start of the CTD survey on 24 January, the winds were equatorward

7
40°
350
30°
25°
20°
Fig. 3.
Map of average seasonal wind stress for the month of January over the
California Current region.
These wind stresses were calculated at 6-hour intervals from 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.

8
0
(0
E z t&j
0
U) z
S
December 1984 January 1985 February
3.0
E
U
C
>..
U)
0.0
U)
Ui
U) z
S
-1.5
—3.0
December 1984 January 985 February
Fig. 4.
Time series of the alongshore component (defined to be 325T) of vector wind and wind stress from measured winds at NDBC buoy 46028 (see
Fig. 2) for the period 6 December 1984 to 7
February
19E5.
Negative values indicate equatorward winds.
Times are Pacific Standard Time (PST) and tic marks correspond to hour 0000 of the day indicated.

9
HOT
350
340
28 Jan
'I
V
0 calm
27
LJC/7
V
I
I
/
0
/
,
,
0
/
/
/
20 knots 24 Jan
121°W
0
120°30'
Fig. 5.
Map of vector wind.s
measured by a hand-held anemometer at CTD stations during the snapshot of the January 1985 CCCCS cruise.
day
Dashed lines define boundaries during the CTD survey.
Scale is shown at the lower let: corner of the map.

10 throughout the snapshot survey.
to 20 knots.
Winds measured from the ship ranged from calm
Seasonal variations in the flow field off the central California coast have been described by Reid, Roden and Wyllie (1958), Mickey (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 300 latitude October through February.
The poleward nearshore surface counterfiow north of
Point Conception is known as the Davidson Current.
The January 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 relatively strong and poleward across the inshore 100 km (the Davidson Current).
Beyond approximately 150 km from the coast, the flow is relatively strong and equatorward, with a slight onshore component in the northwestern region.
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 January 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 is relatively strong and poleward over the inshore 100 km, and weak and equatorward beyond 150 km from the coast.
January seasonal average 10 m temperature and salinity in the central
California Current region are also shown in Fig. 6.
Isotherms are oriented from northwest to southeast across much of the region.
There is a suggestion of an offshore tongue of water just south of Monterey Bay, possibliy indicative of a seasonally occurring jet-like feature emanating from this region.
The
January seasonal average salinity shows evidence for the strong and narrow
Davidson Current nearshore, with a band of relatively high salinity water

11
127W I25 I23 121' 119'
Fig. 6.
Seasonal average January temperature and salinity at 10 in depth and dynamic heights of the sea surface and the 200 in surface relative to 500 rn for the central California Current region.
Ca1COFI grid points used are 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.

12 extending from Point Conception to the northern portion of the sample region.
Salinities decrease offshore.
These seasonal patterns of the flow field, temperature and salinity smooth out the patterns observed during any particular cruise.
For the three previous
CCCCS CTD surveys (February, July and October, 1984), there were nearly coincident Ca1COFI surveys from which to infer the large-scale conditions in the California Current at the time of the CCCCS surveys.
There were no coincident Ca1COFI surveys during January 1985.
The nearest Ca1COFI samples of the central California coastal region were in early March of 1985, and then only Ca1COFI lines 77 and 80 (see Fig. 1) were sampled.
Consequently, the large-scale characteristics of the California Current System at the time of the
January 1985 CCCCS survey cannot be determined.
Finally, for reference we show in Fig. 7 an infrared satellite image taken on 30 January 1985, in the middle of the CCCCS survey.
The poleward flow of the Davidson Current is clearly evident as a tongue of warm water extending approximately 100 km offshore from Point Conception to at least as far north as Monterey Bay.
This flow pattern suggested by the satellite-measured temperature field strongly resembles the seasonal flow pattern for January
(Fig. 6), suggesting that conditions in the California Current during the
January 1985 CCCCS CTD survey were approximately normal for this time of year.
SA14PLING PROCEDURES
A Neil
Brown Instrument Systems (NBIS) Mark III conductivity, temperature, depth (CTD) probe was used to obtain vertical profiles of temperature and salinity at a total of 73 stations during January 1985.
The CTD was lowered through the water column at a rate of approximately 70-80 m per minute.
During the first 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
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) were

lb thoroughly examined in the October 1984 CCCCS CTD data report (Chelton and
Kosro, 1987c).
The results are summarized briefly in 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
T + r — T, where r is the time constant of the thermistor and ths independent variable t represents time as the CTD falls through the water column.
Assuming an adequately small sample interval this 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 nisec, it was determined that the time constant for the thermistor on this particular CTD was 68 msec (see Chelton and Kosro, 1987a;
1987b).
This time constant was also found to be consistent with the October
1984 CTD data where the sample interval was 250 msec.
The reduced sampling rate thus did not have a large effect on the apparent time constant.
Since there was no reason to expect that it changed between the first three and last
CTD surveys, the time constant r was not recomputed for the January 1985 data.
A value of 68 msec was assumed for correcting measured temperatures using the expression above.
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

15 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 as discussed in the next section.
CALIBRATION
The CTD was calibrated by the manufacturer for conductivity, temperature and pressure on 14 January 1985, 10 days prior to the January 1985 CCCCS survey.
It was recalibrated by NBIS on 21 March 1985, about 1.5 months after completion of the January 1985 CCCCS survey and the calibrations were found to be the same.
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 first three CCCCS CTD surveys, the number of in situ bottle samples collected during the January 1985 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 January 1985 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
The results of these in situ salinity comparisons are summarized be in Table 2.
After applying the corrections determined from the 14
January 1985 pre-cruise calibration by NBIS, the average difference between
CTD and bottle
(see Table 2).
salinities was with a standard deviation of
If the Niskin bottle at Raytheon CTD station 154 is excluded from the calibration, the average difference between CTD and bottle salinities increases to
During the first three CCCCS CTD surveys (February,
July and October
1984), we were fortunate to identify high quality "data of opportunity" to

16
Table 2.
Comparison between CTD salinities and in situ bottle salinities for the January 1985 CCCCS survey.
The salinity difference values refer to CTD minus bottle salinities.
CTD
Sta. No.
Bottle Depth
(m)
Bottle Sal.
CTD Sal.
CTD Depth Sal Difference
10
42
62
87
108
154
736
740
644
746
8
40
34.404
34.393
34.316
34.356
33.230
33.316
34.416
34.408
34.333
34.396
33.234
33.282
736
740
644
746
8
40
0.012
0.015
0.017
0.040
0.004
-0.034

17 supplement the small number of simultaneous in situ bottle calibrations.
In all cases, it was found that the CTD calibrations by NBIS yielded salinity values accurate to better than 0.010/00.
There were no coincident data of opportunity to calibrate the January 1985 CCCCS CTD data.
The nearest Ca1COFI survey of the central California coastal region was in early March 1985 which is too much later than the January 1985 CCCCS survey to be of any value in calibration.
The accuracy of salinities determined from the January 1985 data must therefore be inferred from the six in situ bottle calibrations in
Table 2.
The effects of the reduced sampling rate on salinity estimates was thoroughly examined in the October 1984 CCCCS CTD data report (Chelton and
Kosro, 1987c).
Briefly, the reduced sampling rate was simulated by subsampling
31.25 msec measurements from July 1984 at intervals of 250 msec.
Salinities computed from the two sample rates were then compared.
Differences were generally less than and evenly distributed between positive and negative.
Overall, the standard deviation of these salinity errors introduced by the reduced sampling rate was small (about
However, the amplitude of the salinity errors was considerably larger in regions of rapid temperature change with depth.
It is noteworthy that the January 1985 CCCCS
CTD data show no evidence of the salinity intrusions found at the base of the mixed layer in the October 1984 CCCCS CTD data.
This indicates that the reduced sampling rate does not introduce large-amplitude spurious spikes in the salinity profiles.
The salinity intrusions observed in the October
1984 CCCCS
CTD data are evidently real features of the salinity field at that time.
In summary, it appears from the above analysis that the reduced sampling rate for the October 1984 and January 1985
CTD measurements did not seriously affect the salinity calibration in an average sense; the January 1985 Raytheon salinities generally appear to be accurate to somewhere around
However, in regions of rapid temperature changes with depth, errors of and larger can be expected.
These errors are an unavoidable result of undersampling the response time of the thermistor on the CTD and cannot be corrected from the 250 msec measurements.

18
DATA PROCESSING
As with the February, July and October 1984 CTD data, after converting binary field data to engineering units, the first step in the data processing was to search the January 1985 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 sec, as discussed previously.
The values of pressure were then examined to eliminate ascending data caused by boat roll from wave action.
The remaining data were then tested for gross spikes inpressure.
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 subsanipled 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 previous two sample values.
If the measured value differed from the predicted value by more than 0.75°C or 0.75 nimhos, 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.
Temperature was smoothed once and conductivity was smoothed twice.
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

19 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,O) —
42.9149
was used.
Pressure was converted to depth using the algorithm described by Saunders and Fofonoff (1976).
Then the vertical profiles of salinity, temperature and 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.
all the way to 500 m.
However, a number of deep water CTD casts did not extend.
For these casts, it was not possible to use 500 m as a reference level.
The dynamic height at depth z relative to z0 is computed by o p(z) f p(z0)
6dp 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 z0.
Using CTD data from stations that extended deeper than 500 m, we simulated casts to a number of shallower depths between 400 and 470 m.
We fit the dynamic heights relative to the bottom 100 m of reference levels in the simulated shallow casts to a second order polynomial by least squares.
The quadratic fit was then extrapolated to a reference level of 500 m.
the actual values.
It was found that extrapolations from depths
The resulting estimates of dynamic height relative to 500 in were then compared with of 440 m or

20 deeper resulted in an average bias of less than 0.5 mm and an rins error of less than 1 mm.
Extrapolations from depths of 400 m gave considerably larger errors
(a bias of 1.7 nun and an rms error of 2.8 nun).
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 m.
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 m.
The same extrapolation technique was applied to CTD data in water shallower than 200 m to construct horizontal maps of dynamic height relative to 200 m.
We note, however, that the accuracies of the extrapolations for either the
500 m or 200 m reference level have not yet been thoroughly demonstrated.
This 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, 1987a; 1987b) 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

21 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.
The pressure in decibars is slightly larger than the depth in meters.
For example, a pressure of 500 db corresponds to a depth of 496.7 m off the central
California coast.
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 both the October 1984 and January 1985 data were computed using exactly the same computer software as in the February and July 1984 data reports.
Table 3 gives a summary of the relation between true dynamic heights and the underestimated dynamic heights determined from all 73 CTD stations in the
January 1985 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 2.6 dyn cm with an rms deviation of 0.07 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 rn's error of no worse than 0.07 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.
The contour plots included in this report were not smoothed in any way.
We give here a few brief comments on each of the data products contained in this report.
Note that there was only one snapshot

22
Table 3.
Statistics for comparison between true dynamic heights and the incorrect dynamic heights for the January 1985 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 errors.
Reference
Surfaces
Number samples
Bias
(dyn cm)
Stnd.Dev.
(dyn cm)
Min.error
(dyn cm)
Max.error
(dyn cm)
Range error
(dyn cm)
0/100
0/200
50/200
100/200
0/500
50/500
100/500
200/500
53
53
53
53
35
35
35
35
0.2998
0.7252
0.5941
0.4254
2.6052
2.4741
2.3076
1.8861
0.0112
0.0250
0.0222
0.0171
0.0708
0.0700
0.0698
0.0601
0.2581
0.6695
0.5581
0.3959
2.4259
2.2873
2.1228
1.7197
0.3272
0.7929
0.6523
0.4658
2.7361
2.5978
2.4316
1.9971
0.0691
0.1234
0.0942
0.0699
0.3102
0.3104
0.3088
0.2775

23 survey during the January 1985 cruise.
Consequently, there are no difference maps or difference sections presented 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.
Times for January 1985 CTD casts are local Pacific Standard Time (PST).
Note that the Raytheon station numbering convention was different for each of the four CCCCS CTD
2.
surveys.
Mans of CTD station locations and bathvmetrv.
Maps are presented showing the geographical locations of each CTD station in the CCCCS full and snapshot 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 the snapshot (lines 2 and 9) 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.
Bathymetry maps for the full and snapshot CCCCS sample region are also presented.
Isobaths corresponding to 100 m, 200 m, 500 m and 1000 m 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 m have been extrapolated inshore as described in the
3.
previous section.
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 (m), water temperature (°C), salinity and dynamic depth (DELD) relative to the sea surface (dyn m) are listed at depth intervals of 10 m from the surface to 200 m, depth intervals of 20 m from 200 to 300 m and depth intervals of 50 m for depths greater than 300 m.
Data values at the bottom sample depth are also given.
Note that these dynamic depths are systematically low by a depth-dependent, approximately constant bias, as discussed in the previous

2k
4.
5.
6.
section
(see Table 3).
Note also that the density parameter is and not the more conventional a9 (where 9 refers to potential temperature).
The two differ by very little for the shallow water depths (less than 500 m) considered here.
If the CTD cast was in water deeper than 500 m and the cast did not extend to a depth of 500 m (but did extend deeper than 440 m), dynamic depth of the 500 m 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 m surfaces in nearshore stations in water shallower than 200 and 500 m 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.
Vertical Drofiles of temDerature. salinity and Profiles are presented for all 73 CTD casts during the January 1985 CCCCS cruise.
Potential Tenmerature-Salinity tlots.
The dots correspond to a potential temperature, salinity pair at 10 m intervals for all CTD casts.
Separate plots are included for the full and snapshot CCCCS regions.
Maps.
Included are maps of temperature, salinity and at depths of 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 thermocline and below the therniocline).
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 mis
of no worse than
0.07 dyn cm.
Note that the plots on surfaces are not the more conventional a9 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

25
7.
shallower than 200 in and 500 in 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 and shapshot CCCCS regions 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 the snapshot (lines 2 and 9) 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.l°/,,,,, 0.1, 1 dyn cm and 10 m for maps of temperature, salinity, dynamic height, and depth of surfaces, respectively.
In maps where the dynamic range of the variable plotted is small, intermediate contours are drawn as dashed lines.
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, 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 the snapshot (lines 2 and 9) 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 map of the station locations is included with each vertical section.
The plots are grouped by data type.
Contour intervals are 1°C, 0.l°/,,,, 0.2, and 5 cm/s for temperature, salinity, and relative geostrophic velocity, respectively.
Positive values correspond to poleward and 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.

26
ACKNOWLEDGENENTS
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.
Initial data processing was done by Marian Falla.
The data listings and plots in this report were done at Oregon State University under Raytheon Service Company
Subcontract No. 9330936556.

27
REFERENCES
Chelton, D.B., 1984: Seasonal variability of alongshore geostrophic velocity off central California. Journal of Geophysical 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
Marine Research,
1095-1125.
Chelton, D.B., R.L. Bernstein, A. Bratkovich, and P.M. Kosro, 1987: The central
California coastal circulation study.
Trans.
Amer. Geovhys. Union, pp.
1, 12-13.
Chelton, 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, 1987b: 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 8404, October 1984.
Oregon State
University Rep. 128, Ref 87-04.
Hickey, B.M., 1979: The California Current system -
Progress in
191-279.
hypotheses and facts.
Huyer, A., 1980: The offshore structure and subsurface expression of sea level off Peru, 1976-1977. Journal of Physical Oceanography,
1755-1768.
La Fond, E.G., 1957: Processing Oceanographic Data. Hydrographic Office Pub.
614, U.S. Navy Hydrographic Office.

28
Lewis, E.L., and R.G. Perkin, 1981: The Practical Salinity Scale 1978: conversion of existing data. Deey-Sea Research, 307-328.
Lynn, R.J., 1967: Seasonal variation of temperature and salinity at 10 m in the
California Current. California CooDerative Fisheries Investigations
ReDort, 157-174.
Montgomery, R.B., 1941: Transport of the Florida Current off Habana.
Journal of Marine Research, 198-219.
Reid, J.L, G.I. Roden, and 3.0. Wyllie, 1958: Studies of the California Current
System. California CooDerative Oceanic Fisheries Investigations ReDorts,
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.
Journal of
Ceoihvsical Research, 3100-3110.
Saunders, P.M., and N.P. Fofonoff, 1976: Conversion of pressure to depth in the ocean. Deet-Sea Research, 109-111.

LISTING OF LOCATION TIMES AND DEPTHS OF CTD STATIONS

RAYTHEON CRUISE 8501
'
STATION
1
2
3
6
35
36
89
92
95
98
99
79
81
84
87
52
53
56
59
62
63
66
69
73
74
75
77
78
39
42
43
46
49
8
10
13
14
16
17
18
19
20
21
24
27
28
31
34
DAY HOUR LATITUDE LONGITUDE ZMAX DEPTH
24 Jan 1023
1110
34 25.1
34 19.9
120 27.2
120 27.8
76
342
424
82
350
432 1150
1328
1538
34 18.4
34 12.9
34 8.3
120 31.1
120 42.1
120 52.0
692
740
702
914
1759 34 9.9
121 8.2
738 2100
1956 34 15.3
120 56.8
736 950
26 Jan
0616 34 19.8
120 47.4
728 750
0745
0837
34 23.4
120 40.2
442 450
34 25.2
120 35.8
246 253
0913 34 26.5
120 32.9
92 97
0947
1039
1117
1258
1440
1555
34 28.4
120 29.7
34 31.9
120 34.7
24
28
80
30
32
34 30.4
120 38.5
85
34 24.7
120 50.5
702 712
34 20.1
121 0.6
738 1000
34 25.2
121 3.9
738 1100
1731
34 29.4
120 54.5
684 695
1923 34 34.9
120 42.5
62 67
2040
2128
34 41.4
34 39.0
120 41.6
120 46.3
42
86
46
90
2308
27 Jan 0050
0219
0404
34 34.2
120 57.8
638 648
34 29.9
121 7.4
740 1100
34 34.7
121 10.9
724 915
34 39.3
121 1.2
586 595
34 44.8
120 49.8
94 100 0555
0708
0806
34 48.5
120 40.7
34 54.4
120 43.1
34
42
35
45
0929
1102
1235
34 49.6
120 53.4
214 220
34 44.3
121 4.8
522 530
34 40.0
121 14.3
696 708
1350
1517
1704
34 4.4.7
12]. 17.7
564 573
34 49.1
121 8.4
552 561
34 54.7
120 56.7
304 312
1857
35
1953 35
120 43.2
7.0
120 44.6
4.8
120 49.0
44
38
49
42
2052 35
2155 35
2245
1.5
90 95
120 55.4
240 245
34 59.5
121 0.3
416 422
2326
34 58.0
121 3.2
482 491
28 Jan
0042
34 54.1
12]. 11.2
558 567
0216
0359
34 49.5
121 20.9
498 508
34 44.1
121 32.2
746 915
0608 34 53.9
121 24.2
446 453
0733 34 58.7
121 15.3
586 595
0915 35
4.2
121 3.7
476 483
1058
1149
35 10.3
120 51.6
35 15.4
120 55.5
50
52
57
56

102
105
108
113
114
115
116
118
120
122
131
133
135
137
139
146
148
150
152
154
159
162
163
165
167
1331
1526
1746
29 Jan 2107
2131
2225
2319
30 Jan 0050
0245
0431
1 Feb 0631
0757
0929
1059
1505
3 Feb 0601
0740
0934
1108
1325
2135
4 Feb 0054
0237
0403
0521
35 9.2
35 3.7
34 59.0
35 38.8
35 37.8
35 35.3
35 33.3
35 29.3
35 24.6
35 20.3
36 10.8
36 7.5
36 3,4
35 59.7
35 53.1
36 47.5
36 43.4
36 38.4
36 34.4
36 28.4
37 3.0
37 10.3
37 13.2
37 17.7
37 21.9
121 7.6
121 18.6
121 27.4.
121 16.2
121 18.0
121 23.7
121 28.1
121 36.4
121 46.2
121 55.3
121 44.3
121 51.9
122 0.6
122 8.7
122 21.7
122 3.0
122 12.4
122 24.2
122 32.8
122 45,9
123 11.2
122 55.3
122 49.0
122 39.4
122 30.2
548
625
494
37
93
484
663
970
1100
2000
392
1000
1280
1555
2000
313
950
2380
3000
2000
2560
496
255
98
47
540
616
484
34
90
476
656
702
712
656
386
664
698
720
668
306
742
712
714
718
698
488
250
92
42

MAPS OF CTD STATION LOCATIONS AND BATHYMETRY

37
STATION LOCATIONS
36
35
34
123 122 121 120

35
STATION LOCATIONS
67
JANUARY 1985
SNAPSHOT
$9
84
105
9Z
62
43
102
95
79
78
77
98
75
74
73
69
53
56
52
59
35
46
36
39
42
SI
21
28
24
Is
17
27
3
2
13
10
8
34
121 120

36
35
37
FULL CCCCS REGION DEPTH
34
123 122 121 120

35
SNAPSHOT REGION DEPTH
34
121 120

DATA LISTINGS

_
5Th
1 34
25.1W
120 27.2W
0.
13.786
33.390
25.009
10.
13.667
33.406
25.046
20.
13.650
33.410
25.053
30.
40.
50.
13.555
33.416
25.077
13.379
33.439
25.130
12.961
33.450
25.222
60.
70.
12.125
33.576
25.481
11.458
33.634
25.651
200.
500.
D— 82
0.000
0.029
0.059
0.088
0.116
0.144
0.171
0.195
0.450
0.870
SIA
2
19.9W
120 27.8W
350
110.
120.
130.
140.
150.
0.
13,771.
33.398
10.
13.727
33.402
25.018
25.031
0.000
0.029
20.
13.656
33.403
25.046
0.059
30.
13.542.
33.416
25.079
0.088
40.
50.
13.311
33.445
25.148
12.674
33.509
25.324
0.117
0.14.4
60.
70.
80.
90.
12.135
33.572
25.477
11.795
33.614
25.573
11.587
33.643
25.634
11.333
33.673
25.704
0.170
0.194
0.218
0.242
100.
160.
170.
180.
190.
200.
220.
240.
260.
280.
300.
500.
10.897
33.720
25.819
10.792
33.733
25.848
10.611
33.754
0.286
25.896
0.307
10.347
25.984
0.328
10.179
33.837
26.035
9.859
33.882
26.124
0.264
0.348
0.368
9.694
33.906
26.171
9.335
33.947
9.277
33.954
26.261
0.386
0.405
26.276
0.422
9.103
33.980
26.325
0.439
9,020 33.992
26.347
0.456
8.930
34.007
26.373
8.703
34.045
26.438
8.277
34.078
26.530
7.968
34.102
26.596
7.663
34.125
26.658
0.490
0.523
0.554
0.584
0.612
0.869
5Th
70.
80.
90.
100.
110.
120.
130.
140.
150.
160.
.170.
180.
190.
200.
220.
240.
260.
280.
300.
350.
400.
500.
0.
10.
20.
30.
40.
50.
60.
3
34 18.4W
120 31.1W
14. 055
13.638
13.614
13.585
13.497
13.254
12.263
11.809
11.
715
11. 580
11. 230
10.927
10.670
10.322
10.026
9 .943
9.645
9.434
9.314
9.150
8.998
8.760
8.371
8.147
7.859
7 .745
7.231
6.778
24.951
25.046
25.059
25.068
25.105
25.171
25
.41.0
25.566
25.590
25.628
25.726
25.799
25.875
25.962
26.063
26.087
26.159
26.223
26.256
26.321
26.358
26.425
26.506
26,357
26. 618
26.61.2
26.739
26. 825
33.386
33.399
33.408
33.2.13
33.437
33.459
33.356
33.608
33.
617
33.634
33. 677
33.701
33.740
.33.775
33.839
33.
832
33. 881
33.919
33.936
33.985
34.001
34.039
34.067
34.087
34.110
34.120
34.150
34.179
D-. 432
0.428
0.445
0.462
0.495
0.527
0.557
0.586
0.614
0.682
0.746
0.870
0.000
0.029
0.059
0.088
0.117
0.145
0.172
0.197
0.221
0.245
0.268
0.290
0.312
0.333
0.353
0.373
0.392
0.410
5Th
6 31.
12.9W
120 42.1W
1)— 702
0.
13.516
33.411
25.081
10.
0.000
13.304
33.398
25.114
0.029
.20.
SIC..MA
13.218
33.410
25.140
0.057
30.
40.
50.
60.
70.
80.
90.
100.
110.
120.
130.
140.
150.
12.954
33.436
25.213
12.581
33.472
25.314
0.085
0.112
12.327
33.485
25.331.
12.226
33.495
0.139
25.399
0.165
11.330
33.596
25.641
0.190
11.199
33.606
25.677
10.926
33.641
25.753
10.655
33.677
25.828
10.556
33.694
25.859
10.117
33.757
25.983
9.893
33.796
26.052
9.635
33.845
26.133
9.481
33.873
26.180
0.213
0.236
0,258
0.280
0.301
0.321
0.340
0.359
160.
260.
280.
9.168
3_.924
26.271
170.
180.
9.085
33.940
26.296
8.913
33.967
26.345
8.611
34.002
26.419
0.394
0.411
190.
0.428
200.
8.565
34.006
26.429
220.
8.175
34.045
26.519
0.1.76
240.
7.998
34.063
26.560
0.506
7.885
34.075
26.586
7.758
34.081
26.610
0.377
0.535
0.561.
300.
350.
400.
450.
500.
550.
600.
650.
692.
.
7.683
34.091.
26.631
7.366
34.122
0.593
26.698
0.663
6.843
34.133
26.780
6.440
0.729
34.168
26.861
0.791
6.072
34.196
26.930
0.849
5.658
34.217
26.999
0.904
5.473
34.301
27.088
0.956
5.121.
34.341
27.161
..003
4.942
34.365
27.201
1,041

STA
0.
10.
20.
30.
40.
50.
60.
70.
80.
280.
300.
350.
400.
450.
500.
550.
600.
650.
700.
740.
90.
100.
110.
120.
130.
140.
150.
160.
170.
180.
190.
200.
220.
240.
260,
8 34 S.3N
120 52.0k'
SAL
13.597
33.445
25.091
13.329
33.416
25.123
13.302
33.435
25.143
13.217
33.441
25.164
13.060
33.454
25.206
12.598
33.460
25.301
12.097
33.506
25.433
11.777
33.496
25.485
10.520
33.652
25.832
10.089
33.710
25.952
9.872
33.753
26.022
9.493
33.846
26.157
9.296
33.875
26.212
9.208
33.890
26.237
9.107
33.894
26.257
8.938
33.932
26.314
8.819
33.952
26.348
8.754
33.963
26.366
8.633
33.977
26.397
8.492
33.998
26.435
8.387
34.010
26.460
8.073
34.048
26.537
7.803
34.049
26.578
7.572
34.088
26.642
7.477
34.129
26.688
7.330
34.143
26.720
6.915
34.150
26.783
6.346
34.191
26.892
6.218
34.212
26.924
6.063
34.231
26.960
5.705
34.282
27.045
5.507
34.304
27.086
5.207
34.319
27.134
5.072
34.348
27.173
4.822
34.377
27.224
914
0.461
0.491
0.520
0.547
0.574
0.640
0.701
0.759
0.815
0.869
0.919
0.967
1.013
1.049
0.000
0.029
0.057
0.085
0.113
0.141
0.167
0.192
0.215
0.236
0.256
0.276
0.294
0.312
0.330
0.348
0.365
0.381
0.398
0.414
0.430
STA 10 34 9.9N
121 8.2W
280.
300.
350.
400.
450.
500.
550.
600.
650.
700.
738.
70.
80.
90.
100.
110.
120.
130.
140.
150.
160.
170.
180.
190.
200.
220.
240.
260.
0.
10.
20.
30.
40.
50,
60.
13.432
33.438
25.118
13.332
33.474
25.167
13.275
33.474
25.178
13.194
33.478
25.197
13.172
33.480
25.203
13.164
33.482
25.210
12.566
33.505
25.342
11.602
33.465
25.494
10.744
33.495
25.671
10.503
33.535
25.744
10.124
33.592
25.854
9.654
33.683
26.004
9.333
33.776
26.128
9.270
33.795
26.154
9.069
33.851
26.229
8.925
33.879
26.274
8.734
33.917
26.334
8.565
33.949
26.385
8.409
33.969
26.425
8.302
33.983
26.452
8.167
34.004
26.488
8.007
34.023
26.527
7.740
34.045
26.584
7.531
34.058
26.624
7.294
34.069
26.667
7.057
34.082
26.710
6.540
34.125
26.814
0.000
0.028
0.056
0.084
0.112
0.140
0.167
0.193
0.217
0.240
0.262
0.283
0.303
0.321
0.340
0.358
0.375
0.392
0.408
0.424
0.440
0.470
0.500
0.529
0.557
0.585
0.649
6.352
34.177
26.880
0.710
6,077 34.233
26,959
4.760
34.397
27.247
0.767
5.693
34.274
27.040
4.983
34.373
27.202
0.821
5.394
34.306
27.101
5.195
34.333
0.871
27.146
0.919
0.964
1.006
4.635
34.417
27.277
1.038
STA 13 34 15.3N
120 56.8W
D.- 950
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.
736.
13.474
33.425
25.101
13.354
33.424
25.123
13.296
33.428
25.138
13.244
33.438
25.156
13.138
33.451
25.187
12.911
33.461
25.241
12.295
33.506
25.395
11.814
33.547
25.518
11.158
33.597
25.677
10.503
33.667
25.847
9.948
33.727
25.989
9.802
33.786
26.059
9.591
33.820
26.120
9.469
33.864
26.175
9.310
33.897
26.226
9.186
33.908
26.235
8.973
33.935
26.310
8.848
33.954
26.345
8.752
33.970
26.373
8.391
34.003
26.423
8.427
34.025
26.466
8.098
34.060
26.543
7.976
34.075
26.573
7.702
34.096
26.630
7.567
34.126
26.673
7.547
3.167
26.708
7.172
34.187
26.776
6.875
34.201
26,829
6.305
34.216
26.917
5.830
34.239
26.995
5.626
34.276
27.049
5,471 34.310
27.093
5.205
34.331
27.144
5.049
34.358
27.183
4.802
34.393
27.239
0.337
0.355
0.373
0.390
0.406
0.423
0.439
0.470
0.499
0.528
0.556
0.583
0.649
0.712
0.771
0.827
0.880
0.000
0.029
0.057
0.085
0.113
0.141
0.168
0.193
0.217
0.240
0.261
0.281
0.300
0.319
0.930
0.977
1.023
1.054
STA 14
0.
10.
20.
30.
40.
50.
60.
70.
80.
90.
34 19.8N
120 47.6W
SAL
13.615
33.466
25.103
13.620
33.465
25.101
13.499
33.475
25.134
13.171
33.490
25.212
12.910
33.508
25.277
12.475
33.534
25.382
12.291
33.552
25.432
11.951
33.588
23.524
11.431
33.638
25.659
11.119
33.668
25.739
100.
110.
120.
130.
140.
150.
160.
170.
180.
190.
200.
220.
240.
260.
280.
300.
350.
400,
450.
500.
550.
600.
650.
700,
728.
10.875
33.676
25.788
10.611
33.725
25.874
10.387
33.763
25.942
10.161
33.790
26.002
9.954
33.825
26.064
9.682
33.878
26.151
9.559
33.903
26.190
9.354
33.947
26.258
9.173
33.976
26.310
9.050
33,993 26.343
ti- 750
D!LD
0.000
0.029
0.057
0.085
0.113
0.139
0.165
0.190
0.215
0.238
0.260
0.282
0.303
0.323
0.343
0.362
0.381
0.399
0.416
0.434
8.875
34.012
26.386
0.450
8.577
34.050
26.462
0.483
8.279
34.090
26.539
0.513
8.142
34.112
26.377
8.007
34.126
0.543
26.608
0.372
7.792
34.130
26.643
0.601
0.669
7.455
34.166
26.720
7.021
34.197
26.806
6.216
34.181
26.901
5.991
34.269
26.998
0.734
0.794
0.850
5,757 34.304
27.055
0.902
5.478
34.331
27.111
0.951
5.236
34.358
27.162
0.998
4,928 34.400
27.230
4.873
34,408 27.243
1.043
1.066

STA 16 34
23.4N
__
120 40.2W
0.
13.596
33.419
25.070
10.
13.598
33.417
25.069
20.
13.599
33.417
25.068
30.
13.591
33.416
25.069
40.
13.484
33.432
25.104
50.
13.278
33.461
25.167
60.
12.928
33.502
25.269
70.
12.199
33.388
25.477
80.
11.957
33.611
25.540
90.
11.506
33.637
25.645
100.
11.285
33.665
25.706
110.
150.
11.072
33.698
25.771
120.
10.678
33.751
25.882
130.
10.382
33.784
25.959
140.
10.252
33.822
26.011
9.791
33.882
26.135
160.
9.637
33.909
26.182
170.
9.479
33.937
26.230
180.
9.309
33.959
26.275
190.
200.
220.
240.
9.154
33.979
26.316
9.057
33.995
26.3—4
8.952
34.011
26.373
8.545
34.050
26.467
260.
8.273
34.078
26.531
280.
7.958
34.100
26.595
300.
7.804
34.115
26.630
350.
7.119
34.137
26.744
400.
6.678
34.163
26.826
500.
450
0.000
0.029
0.058
0.087
0.116
0.144
0.172
0.198
0.223
0.247
0.270
0.293
0.315
0.336
0.356
0.376
0.394
0.413
0.430
0.448
0.465
0.498
0.531
0.561
0.591
0.620
0.688
0.752
0.867
STA
17
0.
13.756
33.442
25.055
10.
20.
13.760
33.4.41
25.054
13.761
33.440
25.033
30.
13.727
33.437
25.058
40.
13.600
33.432
50.
60.
33.445
13.135
33.479
70.
12.647
33.532
25.347
80.
12.304
33.568
25.080
25.131
25.210
25.441
90.
12.200
33.582
25.472
100.
110.
11.840
33.615
25.566
11.167
33.691
25.748
120.
10.908
33.725
25.821
130.
10.514
33.788
25.939
140.
10.360
33.811
25.984
150.
10.340
33.812
25.988
160.
10.332
33.811
25.989
170.
10.260
33.822
26.010
180.
9.705
33.895
26.160
190.
200.
220.
240.
9.299
33.951
26.271
8.916
34.006
26.375
8.262
34.076
26.531
8.209
34.069
26.534
500.
25.2N
120 35.8W
SAL
1— 253
0
0.276
0.300
0.322
0.343
0.364
0.384
0.404
0.425
0.444
0.462
0.480
0.511
0.541
0.000
0.029
0.058
0.088
0.117
0.145
0.173
0.200
0.226
0.252
0.878
18
34 26.5N
120 32.9W
D— 97
0.
13.760
33.447
25.059
10.
13.761
33.447
25.038
20.
30.
60.
13.759
33,446 25.058
40.
13.392
33.665
25.148
50.
13.519
13.223
33.451
33.480
25.111
25.193
13.001
33.498
25.251
70.
80.
90.
12.686
33.323
25.332
12.133
33.591
25.491
12.098
33.596
25.502
200,
500.
0.000
0.029
0.058
0.087
0.116
0.144
0.171
0.198
0.224
0.249
0.484
0.879
SIA 19
34 28.4N
120 29.7W
t— 30
0.
10.
20.
200.
500.
13.681
33.434
25.065
13.653
33.432
25.069
13.627
33.431
25.074
0.000
0.029
0.058
0.488
0.880

STA
0.
10.
20.
200.
500.
20 34 31.9N
120
13.613
33.44.4
25.087
13.536
33.446
25.10.4
13.492
33.4.48
25.114
D— 32
0.000
0.029
0.057
0.478
0.903
STA
0.
10.
21
13.650
30.4N
120 3E.5T.
D— 85
SAL
33.452
25.085
0.000
13.646
33.452
25.086
0.029
20.
30.
40.
50.
60.
70.
80.
200.
500.
13.625
33.45].
25.090
13.598
33.456
25.099
13.523
13.351
13.153
12.689
12.315
33.460
25.117
33.467
25.157
33.484
33.523
25.332
33.567
25.210
25.438
0.058
0.087
0.115.
0.144
0.172
0.199
0.225
0.469
0.889
=
0.
24 36 24.7N
120 50.5W
1— 712
13.705
33.466
25.085
0.000
10.
20.
30.
40.
50.
60.
70.
80.
90.
100.
110.
120.
130.
140.
150,
160.
170.
180.
190.
200.
220.
240.
260.
13.695
33.466
25.087
13.226
33.486
25.197
12.926
33.513
25.277
12.294
33.554
25.432
11.747
33.608
25,577
11,596 33.630
25.622
11.270
33.664
25.709
11.002
33.689
25.776
10.806
33.709
25.827
10.638
33.741
25.881
10.352
33.782
25,962
0.029
0.057
0.085
0.111
0.136
0.160
0.184
0.206
0.228
0.250
0.271
10.205
33.795
25.998
10.031
33.824
26.050
9.917
33.840
26.082
0.291
0.311
9.701
33.877
26.147
9.473
33.910
26.210
0.350
0.368
9.367
33.926
26.240
8.687
34.040
26.437
0.386
9.214
33.960
26.291
9.0.43
33.987
26.339
0.404
0.421
8.926
34.005
26.373
0.438
0.470
8.440
34.077
26.504
8.231
34.099
26.551
0.331
0.502
0.532
280.
300.
350.
400.
450.
8.141
34.109
26.375
7.997
34.121
26.606
7.41].
34,164 26.725
6.889
34.192
26.820
6.410
34.219
26.905
0.562
0.591
0.660
0.725
0.785
500.
550.
5.871
34.230
26.983
5.773
34.292
27.044
5.289
34.343
27.143
5.189
34.352
27.162
0.841
0.894
600.
650.
0.942
0.988
700.
4.997
34.381
27.207
4.991
34.382
27.208
1.033
702.
1.035
300.
350.
400.
450.
500.
550.
600.
650.
700,
738.
150.
160.
170.
180.
190.
200.
220.
240.
260.
280.
0.
10.
20.
27 34 20.1N
121 0.6W
D—1000
SAL
13.311
33.450
25.152
13.295
33.450
25.156
13.278
33.453
25.161
0.000
0.028
0.056
30.
13.272
33.456
25.164
0.085
40.
13.163
33.465
25.193
50.
12.864
33.481
25.265
60.
70.
12.092
32.519
25.444
11.395
33.582
25.622
80.
90.
100.
10.889
33.626
25.747
10.453
33.697
25.880
110.
120.
130.
140.
10.171
33.717
25.943
9.785
33.771
26.050
9.696
33.810
26.096
9.543
9.200
33.828
33.870
26.135
26.224
0.113
0.140
0.167
0.191
0.214
0.236
0.237
0.277
0.297
0.316
0.334
9.126
33.896
26.255
8.995
33.927
26.300
8.826
32.960
26.333
8.646
33.980
26.397
8.517
34.029
26.455
8.378
34.034
26.480
8.142
34.061
26.537
7.900
34.084
26.591
7.663
34.116
26.651
0.352
0.370
0.387
0.404
0.420
0.435
0.466
0.496
0.325
7.558
34.131
26.678
7.510
0.552
34.145
26.696
0.579
7.212
34,199 26.780
0.645
6.969
34.209
26.822
6.504
34.220
26.894
5.985
34.226
26.965
0.708
0.768
0.825
5.685
34.284
27.048
5.478
34.310
27.094
0.928
5.244
34.349
27.153
0.975
4.929
34.360
27.198
0.878
1.021
4.801
34.385
27.233

STh 25
0.
10.
34 141 3.9W
SAL SIGMA
13.389
33.468
25.150
13.384
33.469
25.152
20.
30.
40.
50.
60,
13.354
33.472
25.160
13.241
33.464
25.177
13.145
33.472
25.203
12.770
33.496
25.295
12.107
33.520
25.442
70.
80.
90.
100.
110.
120.
130.
140.
150.
160.
170.
180.
t—1100
0.000
0.028
0.057
0.085
0.112
0.140
11.543
33.576
25.590
10.922
33.601
25.722
10.581
33.650
25.821
0.166
0.191
0.214
0.237
10.065
33.739
25.978
0.258
9.866
33.775
26.040
0.278
9.604
33.836
26.131
0.297
9.446
33.883
26.194
0.316
9,282 33.915
26.245
0.334
0.351
8.992
33.947
26.316
8.835
33.967
26.357
8.639
33.983
26.401
8.323
34.019
26.446
0.368
0,385
0.401
190.
200.
220.
240.
260.
280.
8.430
34.039
26.476
0.417
8.330
34.046
26.497
0.433
8.170
34,075 26.544
0.463
8.042
34.097
26.580
0.493
7.871
34.100
26.608
7.779
34.142
26.654
0.522
0,550
300.
7.595
34.156
26.692
0.578
350.
4.00.
7.203
34.192
26.776
0,644
6.586
34.176
26.848
0.706
450.
6.125
34.190
26.919
0.766
500.
550.
5.995
34.248
26.981
0.821
5.74.4
34.276
27.035
0.874
600.
5.482
34.301
27.087
0.925
650.
700.
738.
5.325
34.357
27.150
5.021
34.386
27.208
4.749
34.400
27.251
0.973
1.018
1.050
STA
30.
31 34 120 54.5W
695
SPL
0.
13.409
33.429
25.116
10.
20.
0.000
13.415
33.429
25.115
13.364
33.4.47
0.029
25.140
0.057
12.962
33.483
25.247
0.085
40.
12.469
33.548
25.394
50.
60.
70.
12.275
33.568
25.446
11.898
33.593
25.537
11.477
33.625
25.641
0.112
0.137
0.162
0.186
80.
11.333
33.649
25.685
0.210
90.
11.191
33.668
25.726
0.233
100.
10.760
33.720
25.844
0.255
110.
10.370
33.752
120.
10.181
33.807
25.936
26.011
130.
10.029
33.832
26.057
0.276
0.297
0.317
140.
9.864
33.848
26.097
0.336
150.
9.696
33.856
26.131
0.355
160.
9,651 33.884
26.161
0.374
170.
280.
9.352
33.927
26.243
0.392
180.
260.
9.170
33.963
26.301
0.410
190.
9.053
33.986
26.338
0.427
200.
8.940
34.004
26.369
0.44.4
220.
8.743
34.034
26.424
0.476
240.
8.482
34.069
26.492
0.508
8.329
34.092
26.533
0.539
8.061
34.113
26.590
0.569
300.
7.872
34.131
26.632
0.597
350.
7.360
34,3.64
400.
6.822
34.168
26.732
26.810
450.
6.260
34.179
26.893
0.666
0.730
0.791
500.
5.947
34.220
26.965
0.847
550.
5.779
34.279
27.033
0.901
600.
5.512
34.320
27.098
0.951
650.
5.170
34.353
27.165
0.998
684.
4.956
34.379
27.211
1.028
0.
10.
20.
30.
40.
50.
60.
200.
500.
STA 34 34 34.9N
120 42.5W
B— 67
13.599
33.441
25.087
0.000
13.601
33.441
25.087
13.599
13.575
0.029
33.443
25.088
0.058
33.444
25.094
0.087
13.314
33.473
25.169
0,115
13.066
33,494 25.235
12.900
33.511
25.281
0.143
0.170
0.471
0.893
STA 35
34 41.4N
120 41.6W
B— 46
0.
10.
20.
30.
40.
200.
500.
13.456
33.467
25.136
13.427
33.466
25.141
13.422
33.466
25.142
0.000
0.028
0.057
13.407
33.467
25.146
13.353
0.085
33.476
25.164
0,113
0.476
0.880

STA 36 34 39.ON
120 46.3W
S.4L
0.
12.588
33.446
10.
20.
30.
40.
25.093
13.392
33.445
13.382
33.446
25.092
25.095
13.276
33.454
25.163
13.195
33.467
25.189
50.
60.
70.
80.
12.786
33.517
25.308
12.297
33.570
25.444
3..270
33.575
25.453
11.928
33.612
25.546
200.
500.
D— 90
0.000
0.029
0.058
0.086
0.114
0.141
0.167
0.193
0.218
0.466
0.869
220.
240.
260.
280.
300,
350.
400.
450.
500.
550.
600.
638.
90.
100.
110.
120.
130.
140.
150.
160.
170.
180.
190.
200.
STA 39 34 120 57.8W
STOMA
0.
13.407
33.469
25.1.47
10.
13.414
33.469
25.146
20.
30.
13.405
33.467
25.147
13.201
33.461
25.183
40.
50.
60.
70.
80.
12.918
33.487
25.259
12.547
33.491
25.335
12.164
33.558
25.461
11.148
33.699
25.758
10.905
33.727
25.823
10.756
33.752
25.869
10.372
33.772
25.917
10.388
33.799
25.970
10.222
33.823
26.017
10.114
33.839
26.048
10.006
33.851
26.076
9.681
33.870
26.145
9.294
33.931
26.256
9.249
33.940
26.270
9.113
33.964
26.311
9.015
33.983
26.341
8.903
34.000
26.372
8.636
34.037
26.443
8.412
34.073
26.506
8.130
34.089
26.561
7.855
34.120
26.626
7.613
34.143
26.679
7.089
34.141
26.752
6.651
34.150
26.819
6.225
34.194
26.909
5.981
34.223
26.963
5.805
34.268
27.021
5.564
34.320
27.091
5.161
34.370
27.179
D— 648
0.334
0.353
0.371
0.389
0.407
0.424
0.441
0.473
0.504
0.535
0.564
0.592
0.659
0.722
0.782
0.839
0.892
0.943
0.979
0.000
0.028
0.057
0.085
0.112
0.139
0.165
0.189
0.211
0.232
0.254
0.274
0.295
0.
10.
20.
30.
40.
50.
60.
70.
80.
190.
200.
220.
240.
260.
280.
300.
250.
400.
450.
500.
550.
600.
650.
700.
740.
90.
100.
110.
120.
130.
140.
150.
160.
170.
180.
STA 42 34 29.9N
121 7.4W
D—ll00
13.295
33.447
25.153
0,000
13.303
33.446
25.151
0.028
12.301
33.447
25.152
0.037
13.111
33.468
25.206
0.085
12.546
33.497
25.339
0.112
11.681
33.518
25.519
10.851
33.610
25.741
0.137
0.161
10.651
33.645
25.804
10.255
33.703
25.918
10.024
33.737
25.983
9.924
33.756
26.016
9.646
33.809
26.103
9,512 33.874
26.176
9.428
33.893
26.204
9.287
33.916
26.245
9.030
33.942
26.307
8.862
33.983
26.365
0.184
0.205
0.226
0.246
0.266
0.285
0.303
0.321
0.339
0.356
8.713
33.998
26.401
8.599
3.4.021
0.372
26.436
0.388
8.487
34.041
26.469
0.404
6.334
26.512
8.227
34.091
26.548
0.420
0.450
8.099
34.128
26.596
0.479
8.009
34.149
26.626
0.508
7.894
34.163
26.654
0.536
7.796
34.172
26.676
7.518
34.189
26.729
7.024
34.198
26.806
0.564
0.632
0.697
6.314
34.183
26.890
0.758
6.012
34.238
26.971
5.762
34.287
27.042
5.612
34.317
27.083
5.318
34.349
27.14.4
4.971
34.383
27.212
4.730
34.408
27.259
0.814
0.868
0.918
0.966
1.011
1.045
0.
10.
20.
30.
40.
50.
60.
70.
80.
90.
350.
400.
450.
500.
550.
600.
650.
700.
724.
190.
200.
220.
240.
260.
280.
300.
100.
110.
120.
130.
140.
150.
160.
170.
180.
STA 43 34 34.7N
121 10.9W
D— 915
13.346
33.433
25.132
13.347
33.434
25.132
13.351
33.43.4
25.132
13.344
33.434
25.134
22.872
33.476
25.260
12.090
33.541
25.461
11.080
33.620
25.709
10.688
33.654
25.805
10.232
33.706
25.921
10.062
33.767
26.000
9.881
33.809
26.064
9.724
33.827
26.104
9.503
33.877
26.180
9.280
33.921
26.250
9.090
33.972
26.321
6.948
33.997
26.363
8.864
34.010
26.386
8.750
26.418
8.666
34.035
26.437
8.541
34.050
26.468
8.404
34.079
26.511
6.335
34.098
26.537
8.189
34.128
26.582
8.074
34.141
26.610
7.987
34.155
26.634
7.892
34.163
26.654
0.000
0.028
0.057
0.085
0.113
0.139
0.164
0.186
0.208
0.228
0.248
0.268
0.286
0.305
0.322
0.339
0.356
0.372
0.388
0.404
0.420
0.450
0.480
C.509
0.538
0.566
7.387
34.184
26.744
0.633
6.638
34.169
26.836
6.179
3.4.192
26.914
5.804
34.239
26.999
0.697
0.757
0.613
5.615
34.302
27.071
5.454
34.336
0.865
27.117
0.914
5.336
34.350
27.143
0.962
5.030
3.383
27.205
1.007

STA 46
0.
10.
20.
39.3N
121
SAL
13.479
3.. .450
25.118
13.482
33.4.48
25.116
13.486
33.449
25.116
30.
40.
50.
60.
70.
80.
90.
100.
110.
120.
130.
140.
150.
160.
170.
180.
190.
200.
220.
240.
13.108
33.484
25.219
12.483
33.527
25.375
12.132
33.565
25.472
11.573
33.648
25.641
11.261
33.690
25.731
11.121
33.704
25.767
10.860
33.723
25.828
10.630
33.741
25.883
10.186
33.794
26.000
10.033
33,819 26.046
9.933
33.839
26.078
9.837
33.852
26.104
9.686
33.872
26.145
9.457
33.913
26.215
9.397
33.922
26.232
9.240
33.949
26.279
9.157
33.964
26.303
9.105
33.973
26.319
8.698
34.011
26.413
8.498
34.032
26.461
260.
280.
300.
350.
400,
450.
500.
550.
586.
8.147
34.060
26.536
7.950
3.4.074
26,576
7.745
34.090
26.618
7.181
34.135
26.735
6.662
34.160
26.825
6.352
34.191
26.890
5.794
34.263
27.019
5.427
34.334
27.119
4.998
34.387
27.212
0— 595
0.594
0.663
0.727
0.787
0.843
0.893
0.926
0.000
0.029
0.057
0.086
0.112
0.138
0.162
0.185
0.208
0.230
0.252
0.272
0.292
0.312
0.331
0.350
0.369
0.387
0.404
0.422
0.439
0.472
0.504
0.535
60.
70.
80.
90.
200.
500.
0.
10.
20.
30.
40.
50.
STh 49 120 49.8w
1— 100
13.331
33.477
25.169
0.000
13.327
33.476
25.169
0.028
13.322
33.479
25.172
0.056
13.227
33.482
25.194
12.561
33.539
25.369
0.084
0.111
0.136
11.959
33.607
25.537
11.716
33.625
25.596
11.253
33.686
25.729
0.161
0.184
10.760
33.725
25.847
10.473
33.772
25.934
0.206
0.227
0.456
0.873
STA 52
0.
10.
20.
30.
200.
500.
34 48.5N
120 40.7W
0.-
35
13.383
33.462
25.147
0.000
13,377 33.462
25.148
0.028
13,319 33.470
25.166
0.057
13.297
33.473
25.173
0.085
0.471
0.897
53 34 54.4N
120 43.1W
0— 45
0.
13.178
33.488
25.209
0.000
10.
13.174
33.488
23.209
0.028
20.
13.167
33.493
25.215
0.055
30.
12.897
33.487
25.263
0.083
12.441
33.551
25.402
40.
200.
500.
0.109
0.450
0.905

STA 56
0.
10.
20.
30.
40.
50.
60.
70.
80.
90.
100.
110.
34 49.6N
120 53.4k' 0—. 220
SAL
12.332
33.48].
25.172
0.000
0.028
13.325
33.482
25.174
13.302
33.480
25.177
13.208
33.487
25.201
13.103
33.495
25.228
12.796
33.323
25.311
12.415
33.553
25.408
0.056
0.084
0.112
0.139
0.165
0.190
11.868
33.611
25.357
11.637
33.635
25.615
11.339
33.666
25.698
10.516
33.742
25.903
10.314
33.775
25.964
10.208
33.790
25.993
0.214
0.238
0.260
0.280
0.301
120.
130.
140.
150.
160.
170.
180.
190.
200.
500.
9.881
33.844
26.091
9.707
33.871
26.141
9.654
33.882
26.159
9.438
33.912
26.218
9.413
33.918
26.226
9.259
33.941
26.269
9.088
33.971
26.320
9.024
33.975
26.333
0.321
0,340
0.359
0.377
0.395
0.413
0.430
0.448
0.884
STh 55
0.
10.
34
121
S4Z
4.8w
0— 530
13.561
33.439
25.093
13.529
33.436
25.097
0.000
0.029
20.
0.057
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.
522.
13.502
33.441
25.107
13.487
33.440
25.109
12.968
33.497
25.257
12.459
33.549
25.397
12.063
33.594
25.507
11.751
33.628
25.592
11.292
33.625
25.674
10.746
33.697
25.828
10.342
33.745
25.936
10.056
33.801
26.028
9.900
33.838
26.083
9.845
33.846
26.099
9.709
33.868
26.138
9.594
33.887
26.173
9.498
33.904
26.201
9.393
33.915
26.227
9.263
33.931
26.261
9.139
33.963
26.305
9.101
33.969
26.316
8.897
34.013
26.383
8.741
34.034
26.424
8446
34.065
26.494
8.348
34.069
26.512
8.063
34.068
26,554
7.574
34.123
26.669
6.946
34.141
26.771
6.454
34.193
26.879
5.861
34.251
27.001
5.735
34.275
27.035
0.086
0.114
0.141
0.166
0.191
0.215
0.237
0.258
0.279
0.298
0.317
0.337
0.355
0.374
0.392
0.410
0.427
0.445
0.478
0.511
0.542
0.573
0.603
0.675
0.742
0.804
0.860
0.883
.
STA 62
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.
34 40.ON
121 14.3W
0- 708
SAL
13.543
33.445
25.102
12.338
33.445
25.143
12.330
33.433
25.151
13.318
33.467
25.164
13.084
33.475
25.217
12.659
33.492
25,314
11.653
33.535
25.539
10.927
33.647
25.737
10.780
33.732
25.849
10.583
33.758
25.904
10.367
33.779
25.958
10.250
33.791
25.988
9.948
33.832
26.070
9.604
33.885
26.169
9.448
33.912
26.216
9.303
33.933
26.255
9.131
33.968
26.308
9.070
33.981
26.331
8.924
33.996
26.366
8.865
34.010
26.386
8.819
34.018
26.400
8.524
34.038
26.461
8.420
34.086
26.314
8.238
34.119
26.568
0.000
0.028
0.037
0.085
0,113
0.140
0.166
0.189
0.211
0.233
0.254
0.274
0.294
0.313
0.331
0.349
0.367
0.384
0.401
0.418
0.434
0.466
0.497
0.527
300.
250.
400.
450.
500.
550.
600.
650.
696.
8.079
34.137
26.606
7.782
34.156
26.665
7.085
34.160
26.768
6.599
34.170
26.841
6.317
34.193
26.897
5.910
34.227
26.975
5.674
34.280
27.046
5.473
34.314
27.098
5.326
34.344
27.140
5.049
34.376
27.197
0.357
0.585
0.652
0.715
0.775
0.885
0.925
0.983
1.025
STA 63 34 44.7N
121 17.7W
0- 573
0.
10.
20.
30.
40.
50.
60.
70.
220.
240.
260.
280.
300.
350.
400.
450.
500.
550.
564.
80.
90.
100.
110.
120.
130.
140.
150.
160.
170.
180.
190.
200.
13.455
33.468
25.137
12,352 33.473
25.162
13.049
33.489
25.235
12.180
33.569
25.466
11.944
33.597
25.532
11.586
33.642
25.634
11.282
33.664
25.706
11.049
33.683
25.763
10.710
33.731
25.861
10.486
33.749
25.913
10.178
33.796
26.003
10.056
33.814
26.038
9.887
33.834
26.082
9.639
33.876
26.156
9.381
33.921
26.233
9.315
33.936
26.256
9.147
33.965
26.306
8.893
33.990
26.366
8.782
34.010
26.399
8.70].
34.022
26.421
8.639
34.030
26.437
8.344
34.092
26.530
8.106
34.119
26.588
7.829
34.140
26.646
7.571
34.139
26.682
7.284
34.126
26.713
6.964
34.176
26.797
6.538
34.173
26.852
6.356
34.186
26.886
6.051
34.237
26.966
5.880
34.264
27.008
5.751
34.285
27.041
0.318
0.336
0.354
0.371
0.387
0.404
0.420
0.451
0.481
0.509
0.537
0.564
0.629
0.691
0.751
0.808
0.862
0.877
0.000
0.028
0.056
0.082
0.107
0.131
0.135
0.178
0.200
0.221
0.242
0.262
0,281
0.300

STA
34 49.1N
.21
8.4'.
1.— 561
SAT
0.
13.743
33.467
25.077
10.
13.591
33.455
25.099
0.000
0.029
20.
13.516
33.432
25.113
0.058
30.
13.481
33.457
25.123
0.086
40.
13.222
33.483
25.195
0.115
50.
12.004
33.578
25.506
0.141
60.
11.635
33.618
25.606
0.165
70.
80.
90.
100.
10.744
10.297
33.714
25.841
0.188
33.784
25.974
10.152
33.801
26.012
9.976
33.836
26.069
0.209
0.230
0.249
110.
9.790
33.866
26.124
0.269
120.
9.601
33.894
26.177
130.
9.596
33.896
26.179
0.287
140.
9.553
33.903
26.192
0.306
0.324
150.
9.457
33.913
26.215
0,343
160.
9.388
33.922
26.233
0.361
170.
9.379
33.924
26.236
0.379
180.
190.
9.300
33.935
26.258
9,208 33.946
26.281
0.396
0.414
200.
220.
9.125
33.961
26.307
8.457
34.058
26.487
0.432
0.464
240.
8,364 34.078
26.517
0.494
260.
280.
300.
350.
400.
450.
500.
550.
552.
8.196
34.106
26.564
7.935
34.136
26.627
7.887
34.144
26.640
7.674
34.168
26.690
7.099
34.176
26.778
6.524
34.179
26.858
6.152
34.228
26.945
5.616
34.291
27.062
5.614
34.292
27.063
0.525
0.554
0.582
0.651
0.717
0.779
0.837
0.891
0.893
STA
69 34 54.7N
.20 56.7w
li SAL
0.
13.563
33.469
25.116
10.
13.529
33.468
25.122
20.
13.426
33.469
25.143
30.
13.339
33.476
25.167
40.
13.258
33.485
25.190
50.
13.218
33.487
25.199
60.
12.808
33.517
25.304
70.
12.275
33.549
25.432
11.755
33.602
25.571
80.
90.
11.494
33.623
25.636
100.
11.041
33.663
25.749
110.
10.924
33.690
25.791
120.
10.709
33.719
25.852
130.
10.390
33.758
25.937
140,
10.145
33.782
25.998
150.
9.895
33.823
26.072
160.
170.
180.
190.
200.
9.632
33.866
26.147
9.471
33.904
26.206
9.393
33.917
26.228
9.234
33.944
26.276
9.005
33.976
26.337
220.
240.
260.
280.
8.563
34.020
26.441
8.431
34.032
26.471
8.258
34.048
26.510
8.239
34.053
26.516
300.
8.182
34.061
26.531
500.
3.2
0.000
0.029
0.057
0.085
0.113
0.141
0.168
0.194
0.219
0.243
0.266
0.289
0.310
0.332
0.332
0.372
0.391
0.410
0.428
0.446
0.463
0.496
0.528
0.559
0.589
0.620
0.890
5Th 73
0.
10.
35
13.191
l.ON
120 43.2W
£— 49
SAL
33.492
25.209
13.202
33.490
25.205
D:-LD
0.000
0.028
20.
30.
40.
13.129
33.492
25.221
13.025
33.498
25.246
12.796
33.517
25.307
0.055
0,083
200.
500.
0.110
0.496
0.946
5Th 74 35 7.ON
120 44.6W
1)—
42
0.
13.109
33.499
25.230
10.
13.110
33.498
20.
13.098
33.497
25.230
25.231
0.000
0.027
0.055
30.
13.065
33.496
25.237
0.062
200.
0.474
500.
0.891

__
SIA 75 35 120 49.QV
0.
13.432
33.482
23.153
10.
13.394
33.481
30.
12.377
33.548
25.160
20.
12.968
33.485
25.248
25.412
40.
12.195
33.567
25.461
50.
12.041
33.586
25.505
60.
11.910
33.598
25.539
70.
11.702
33.618
25.594
80.
11.325
33.652
25.689
90.
10.84.4
33.711
25.821
200.
500.
0—
95
0.000
0.028
0.056
0.083
0.108
0.13 3
0.158
0.182
0.206
0.229
0.465
0.880
5Th 77 35 1.5W
120 55.4k
0.
13.461
33.467
25.135
10.
13.468
33.466
25.133
20.
13.468
33.466
25.133
30.
13.451
33.466
25.136
4C.
13.126
33.486
25.217
50.
12.814
33.518
25.303
60.
12.377
33.559
25.420
70.
150.
11.864
33,589
80.
11.551
33.617
25.621
90.
11.316
33.648
25.687
100.
11.218
33.660
25.715
110.
11.031
33.685
25.767
120.
10.482
33.764
25.926
130.
10.266
33.793
25.986
140.
10.187
33.802
26.006
9.914
33.842
25.540
26.084
33.870
26.141
160.
9.705
170.
9.622
33.884
26.165
180.
9.533
33.897
26.190
190.
9.225
33.941
26.275
200.
9.062
33.962
26.317
220.
240.
8.827
33.997
26.382
8.588
34.025
26.441
500.
0- 245
0.000
0.028
0.057
0.085
0.113
0.140
0.167
0.192
0.216
0.240
0.263
0.285
0.307
0.328
0.348
0.368
0.387
0.406
0.424
0.442
0,460
0.493
0.526
0.870
5Th 78 34 59.5W
121 0.3W
0.
13.530
40.
13.375
50.
13.056
33.474
10.
12.526
33.475
25.128
20.
13.474
30.
13.467
33.475
33.481
33.500
70.
2.1.353
32.337
25.127
25.139
25.140
25.163
25.242
60.
12.689
33.528
25.336
25.424
80.
11.525
33.611
25.621
90.
11.226
33.627
25.687
100.
110.
10.238
33.782
120.
10.030
33.815
26.044
130.
10.520
33.735
25.897
9.801
33.850
25.979
26.109
140.
9.589
33.887
26.173
150.
9.513
160.
170.
9.282
33.944
26.268
180.
9.410
9.237
190.
9.059
33.901
33.913
33.953
26.197
26.223
26.282
33.982
26.332
200.
6.932
33.998
26.366
220.
8.796
34.018
26.403
240.
8,636 34.039
26.444
260.
280.
300.
350.
400.
500.
8.414
34.060
26.495
8.070
34.081
26.564
7.906
34.109
26.610
7.376
34.130
26.703
7.046
34.144
26.760
0- 422
0.432.
0.484
0.516
0.547
0.578
0.607
0.676
0.743
0.258
0.000
0.028
0.057
0.085
0.114
0.142
0.169
0.195
0.220
0.243
0.265
0.286
0.306
0.326
0.345
0.363
0.381
0.399
0.417
0.434
5Th 79
150.
160.
170.
180.
190.
200.
220.
240.
80.
90.
100.
110.
120.
130.
140.
260.
280.
300.
350.
400.
450.
500.
0.
10.
20.
30.
40.
50.
60.
70.
34 58.0W
121 3.2W
13.532
12.533
13 .446
13.233
13.142
12.625
12.240
11.808
11.220
10.595
10.408
10. 223
9.986
9.873
9.754
9.629
9 .4.45
9.329
9.310
9.198
9.177
8.833
8.632
8.417
8.269
8.118
7.284
6.668
6.358
33.466
25.120
33.467
25.121
33.467
25.138
33.483
25.189
33.485
25.213
33.534
25.353
33.564
25.450
33.593
25.554
33.648
25.705
33.680
25.841
33.723
23.907
33.773
25.978
33.822
26.056
33.842
26.091
32.862
26.127
33.877
26.158
33.909
26.214
33.933
26.252
33.936
26.257
33.953
26.288
33.955
26.293
34.014
26.394
34.038
26.445
34.059
26.494
34.081
26.333
34.106
26.576
34.118
26.707
34.163
26.827
34.208
26.903
0- 491
0.000
0.029
0.057
0.085
0.113
0.140
0.166
0.191
0.215
0.237
0.258
0.279
0.299
0.319
0.338
0.357
0.375
0.393
0.411
0.428
0.446
0.480
0.312
0.544
0.374
0.604
0.674
0.738
0.797
0.853

STA 81 3..
5...1N
Ill
11.2;'
L— 567
SAL
0.
13.518
33.453
25.113
10.
13,512 33.452
25.114
20.
13.453
33.457
25.129
0.000
0.029
0.057
30,
40.
50.
60.
12.978
33.500
25.257
0.085
12.079
33.581
25.494
1.1.744
33.610
25,579
0.112
0.136
11.684
33.616
25.595
0.160
70.
80.
90.
100.
110.
120.
130.
140.
150.
160.
170.
11.535
33.623
25.628
11.103
33.675
25.747
10.723
33.723
25.852
10.500
33.754
25.915
10.216
33.793
25.995
9.963
33.832
26.068
9.825
33.854
26.109
9.441
33.913
26.217
9.321
33.933
26.253
9.170
33.954
26.294
9.144
33.958
26.301
0.184
0,207
0.229
0.251
0.271
0.291
0.311
0.329
0.347
0.365
0.382
180.
9.135
33.959
26,304 0.400
190.
9.116
33.959
26.306
0.417
200.
8.906
33.995
26.367
0.434
220.
240.
8.622
34.018
26.430
8.336
34.049
26.498
0.467
0.498
260.
8.122
34.084
26.558
0.528
280.
300.
450.
7.825
34.145
26.650
6.295
34.202
26.907
0.587
350.
7.412
34.179
26.736
0.654
400.
6.759
34.165
26.816
0.718
0.779
500.
550.
558.
8.062
34.100
26.579
5.965
34.247
26.985
5.603
34.294
27.066
5.599
34.294
27.067
0.558
0.835
0.887
0.895
STh
=
84
0.
3-. 49.5N
121
SIC. MA t— 508
13.328
33.474
25.167
0.000
13.329
33.474
25.167
0.028
10.
13.330
33.473
25.166
20.
0.056
13.324
33.474
25.168
0.084
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.
12.778
33.521
25.313
12.134
33.579
25.482
11.867
33.604
25.551
11.575
33.641
25.635
11.295
33.673
25.711
10.987
33.713
25.797
10.389
33.761
25.940
10.109
33.805
26.022
9.845
33.844
26.097
9.569
33.891
26.180
9.373
33.923
26.237
9.174
33.949
26.290
8.940
33.988
26.357
8.833
34.006
26.388
8.820
34.009
26.392
8.701
34.022
26.421
8.540
34.051
26.469
8.311
34.091
26.535
8.018
34.117
26.600
7.874
34.124
26.627
7.816
34.127
26.637
7.662
34.136
26.667
7.324
34.174
26.745
6.634
34.178
26.844
6.288
34.203
26.909
0.112
0.138
0.163
0.187
0.210
0.232
0.254
0.275
0.294
0.313
0.331
0.349
0.366
0.383
0.399
0.707
0.766
0.823
500.
0.415
0.431
0.462
0.492
0.520
0.549
0.577
0.644
8Th 87
34 44.1N
121 32.2W
0— 915
0.
13.175
33.469
25.194
0.000
10.
13.179
33.467
25.192
0.028
20.
13.184
33.468
25.191
0.056
30.
40.
50.
60.
13.083
33.483
25.223
0.084
12.477
33.517
25.368
0.110
11.394
33.501
25.559
0.136
10.850
33.507
25.662
0.159
70.
10.545
33.696
25.862
0.182
80.
10.107
33.750
25.980
0.202
90.
9.834
33.811
26.073
0.222
100.
190.
9.705
33.834
26.113
8.447
0.242
110.
9.561
33.855
26.1.53
0.261
120.
9.414
33.881
26.197
0.279
130.
140.
150.
9.290
33.902
26.234
0.297
9.160
33.918
26.268
0.315
8.864
33.956
26.344
C.332
160.
8.661
33.980
26.394
0.349
170.
8.640
33.997
26.411
0.365
180.
8.467
34.023
26.458
0.382
34.028
26.465
0.397
200.
8.325
34.041
26.496
0.413
22C.
240.
8.036
34.069
26.559
7.728
34.084
26.616
0.643
0.473
260.
7.315
26.645
0.501
280.
7.307
34.094
26.684
0.528
300.
7,233 34.130
26.723
0.555
350.
400.
6.754
34.150
26.805
0.620
6.478
34.217
26.894
0.681
450.
6.195
34.228
26.940
0.738
500.
5.706
34.210
26.987
0.793
550.
3.550
34.271
27.055
0.846
600.
3.128
34.287
27.118
0.896
650.
5.009
34.342
27.175
0.942
700.
4.845
34.368
27.214
0.986
746.
4.656
34.396
27.258
1.025
60.
70.
80.
90.
100.
110.
120.
130.
140.
150.
160.
170.
180.
190.
200.
220.
240.
260.
280.
300.
350.
400.
500.
0.
10.
20.
30.
40.
50.
STA 89
34 53.9N
121
24.2W
0— 453
13.390
33.472
25.153
13.393
33.470
25.151
0.000
0.028
13.393
33.471
25.152
13.243
33.476
25.186
12.181
33.552
25.452
11.429
33.663
25.679
11.244
33.680
25.726
0.057
0.085
0.111
0.136
0.159
0.181
10.729
33.756
25.877
10.442
33.797
25.959
9.987
33.830
26.063
0.202
0.222
9.884
33.842
26.089
9.706
33.877
26.146
9.473
33.919
26.217
0.241
0.260
0.279
9.429
33.923
26.227
0.297
9.249
33.955
26.281
9.101
33.978
0.314
26.323
0.332
8.999
33.985
26.345
8.688
34.040
26.437
C.349
0.365
8.639
34.051
26.454
0.381
8.526
34.053
26.473
8.364
34.067
26.508
8.155
34.094
26.561
7.866
34.108
26.615
0.397
0.413
0.443
0.472
7.594
34.111
26.657
0.500
7.486
34.122
26.681
0.528
7.396
34.134
26.703
0.355
7.153
34.180
26.774
0.621
6.692
34.199
26.852
0.683
0.798

STA 92 =E
0.
5S.7N
121
SAL
13.506
33.455
25.117
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.
586.
1— 595
0.000
13.506
33.454
25.116
0.029
13.264
33.460
25.169
12.784
33.506
23.300
0.057
0.084
12.408
33.542
25.401
0.111
12.060
33.586
25.500
0.136
11.486
33.617
25.633
0.161
10.956
33.684
25.780
0.184
10.616
33.733
25.879
10.459
33.756
25.924
10.231
33.785
25.986
10.057
33.816
26.040
9.872
33.847
26.095
0.205
0.227
0.247
0.267
0.287
9.792
33.857
26.117
0.306
9.625
33.882
26.164
0.325
9.471
33.910
26.210
0.343
9.404
33.923
26.232
0.361
9.248
33.940
26.270
0.379
9.103
33.964
26.313
9.066
33.976
26.327
9.025
33.978
26.336
0.397
0.414
0.431
8.702
34.007
26.409
7.758
34.119
26.639
0.464
8.340
34.050
26.499
0496
8.048
34.085
26.570
0.527
0.556
7.757
34.144
26.659
0.584
7.223
34.172
26.758
6.742
34.168
26.821
6.234
34.197
26.911
0.651
0.715
0.774
6.012
34.236
26.970
5.725
34.287
27.046
5.432
34.326
27,112
0.831
0.884
0.919
STA
0.
li
95 35 121 3.7k'
SAL SIC.MA
13.458
33.472
25.139
E— 483
0.000
10.
20.
30.
40.
50.
60.
70.
80.
13.463
33.471
25.138
13.466
33.471
25.137
13.465
33.471
23.138
13.436
33.470
25.142
12.761
33.522
25.317
12.447
33.553
25.402
12.415
33.559
25.413
12.336
33.563
25.43].
0.028
0.057
0.085
0.113
0.141
0.167
0.193
90.
100.
0.219
0,244
0.268
110.
120.
130.
140.
150.
160.
170.
180.
190.
200.
220.
240.
260.
280.
300.
350.
400.
450.
11.955
33.597
25.530
11,530 33.648
25.648
11.202
33.682
25.735
10.857
33.722
25.828
9.984
33.807
26.045
9.782
33.859
26.120
9.540
33.900
26.192
9.331
33.931
26.250
9.170
33.957
26.296
9.001
33.987
26.346
8.917
34.005
26.374
8.826
34.023
26.403
8.624
34.058
26.461
8.489
34.082
26.501
8.375
34.096
26.329
8.142
34,113 26.578
8.026
34.121
26.601
7.354
34,125 26.702
6.753
34.163
26.815
6.516
36.188
26.866
0.291
0.313
0.334
0.354
0.372
0.390
0.408
0.425
0.442
0.458
0.491
0.522
0.533
0.582
0.612
0.681
0.747
0.808
500.
0.867
5Th 98
0.
10.
20.
30.
35. 10.3N
120 51.6W
1-.
57
SAL
13.204
33.423
25.199
0.000
13.204
33.486
23.202
0.028
13.182
33.489
25.208
0.056
13.133
33.493
25.221
0.083
40.
50.
12.969
33.501
25.259
12.655
33.527
23.342
0.111
200.
0.479
500.
0.896
STA 99
0.
10.
35
12.942
15.4N
120 35.5W
b— 56
51C.MA
D!LD
33485 23.253
0.000
12.959
33.498
23.259
0.027
20.
0.054
30.
40.
50.
200.
500.
12.953
33.498
25.261
12.942
33.498
25.263
12.934
33.498
25.264
12.862
33.501
25.281
0.082
0.109
0.136
0.431
0.832

__
STA 102
0.
10.
20.
30.
35
13.4.45
13.440
13.442
13.413
12.653
40.
50.
12. 300
11. 869
11. 489
11.162
10.975
10.766
10.245
10.005
9.487
9.325
9,343
9.122
8.938
8.856
8.764
8.727
8.608
8.477
8.288
8.031
7.761
7.192
6.579
6.283
5.951
5.632
60.
70.
80.
260.
280.
300.
350.
400.
450.
500.
540.
90.
100.
110.
120.
130.
140.
150.
160.
170.
180.
190.
200,
220.
240.
9.2N
121 7.6w
SAL
33.459
33.460
33.464
33.469
33.536
33.573
33.612
33.640
33.
679
33.698
33. 734
33.774
33.801
33.878
33. 906
33.918
33. 966
34.005
34.019
34.038
34.046
34.066
34.085
34.110
34.119
34.129
34.130
34.143
34.206
34.242
34.280
26. 647
26.729
26.823
26.911
26.
982
27.049
25.132
25.134
25.137
25.146
25.349
25.445
25.357
25.649
25.739
25.788
25.853
25.975
26.037
26.183
26. 231
26.237
26.311
26.370
26.394
26.424
26.436
26.
470
26.505
26.553
26.599
1— 548
0.000
0.028
0.057
0.08 5
0.112
0.139
0.164
0.188
0.211
0.233
0.255
0.27 6
0.296
0.315
0.333
0.351
0.369
0.386
0.402
0.419
0.435
0.466
0.498
0.528
0.537
0.586
0.654
0.718
0.777
0.833
0.875
__
=
35 3.7N
SAL
121 18.6k'
0.
13.410
33.469
25.147
10.
13.412
33.468
25.146
20.
30.
40.
60.
13.407
33.471
25.149
13.270
33.469
12.502
33.551
70.
11.256
33.667
25.175
25.390
50.
12.119
33.582
25.487
11.631
33.630
25.616
25.714
80.
90.
170.
11.122
33.690
25.755
10.837
33.720
8.994
33.947
25.830
100.
10.438
33.757
25.928
110.
10.022
33.777
26.015
120.
130.
9.909
33.801
26.053
9.799
33.821
26.087
140.
9.642
33.845
26.132
150.
9.477
33.878
26.185
160.
9.293
33.905
26.235
26.316
180.
8.862
33.963
26.349
190.
8.691
33.994
26.400
200.
8.578
34.004
26.426
220.
8.415
34.039
26.479
240.
8.206
34.073
26.337
260.
350.
8.089
34.087
26.565
280.
7.835
34.093
26.608
300.
7.619
34.101
26.646
7.241
34.151
26.739
400.
6.676
34.175
26.835
450.
6.229
34.193
26.908
500.
6.034
34.229
26.962
550.
5.754
34.282
27.039
600.
616.
5.407
34.324
27.114
5.310
34.335
27.134
1'— 625
0.000
0.028
0.057
0.085
0.112
0.137
0.161
0.185
0.208
0.230
0.251
0.271
0.291
0.311
0.330
0.349
0.367
0.384
0.401
0.418
0.434
0.466
0.497
0.527
0.556
0.584
0.652
0.715
0.775
0.831
0.885
0.934
0.949
160.
170.
180.
190.
200.
220.
240.
260.
280.
300.
350.
400.
450.
500.
STA 108
=
34 59.ON
121
S4L
27.4W
0.
13.202
33.235
25.009
12.201
33.232
25.006
10.
20.
30.
40.
50.
60.
70.
80.
90.
100.
110.
120.
130.
140.
130.
13.098
33.353
25.120
13.036
33.460
25.215
13.014
33.464
25.222
12.832
33.495
25.278
12.341
33.325
25.401
11.826
33.326
25.499
11.021
33.605
25.707
10.625
33.671
25.829
10.295
33.721
25.925
9.936
33.792
26,042
9.683
33.827 .26.111
9.514
23.858
26.163
9.305
33.896
26.226
9.157
33.921
26.270
8.992
33.950
26.319
8.854
33.971
26.237
8.763
33.987
26.384
8.680
33.994
26.403
8.387
3.036
26.48].
8.125
34.073
26.551
7.867
34.105
26.613
7.646
34.114
26.632
7.425
34.125
26.692
7.265
34.143
26.729
6.791
34.135
26.804
6.327
34.206
26.880
6.271
34.219
26.923
Ii— 494
0.000
0.030
0.059
0.087
0.115
0.142
0.168
0.423
0.439
0.470
0.499
0.327
0.555
0.582
0.646
0.707
0.765
0.821
0.194
0.217
0.240
0.261
0.281
0.301
0.320
0.338
0.356
0.373
0.390
0.407
STA 113
0.
10.
20.
30.
200.
500.
35 38.8N
121 16.2W
0—.
12.778
33.517
25.310
12.640
33.524
25.342
12.499
33.541
23.383
12.405
33.553
25.410
37
0.000
0.027
0.053
0.079
0,443
0.865

STA 114
35
121 18.0w
SIGMA
0.
12.929
33.512
25.276
10.
12.942
33.511
25.273
20.
30.
40.
50.
60.
70.
80.
90.
12.912
33.513
25.281
12.832
33.516
25.299
12.638
33.530
25.348
12.499
33.5.44
25.385
12.262
33.566
25.447
12.097
33.583
25.492
11.908
33.600
25.541
11.741
33.614
25.583
200.
500.
Li.93
0.000
0.027
0.054
0.081
0.108
0.134
0.160
0.185
0.210
0.234
0.442
0.858
STA 115 35 35.3N
121 23.7w
SAL
0.
13.165
33.494
25.216
10.
13.161
33.492
25.214
484
0.000
20.
30.
70.
13.168
33.492
25.213
13.168
33.492
25.214
11.357
33.656
25.686
0.055
0.083
40.
12.961
33.502
25.262
0,110
50.
33.563
25.442
0.137
60.
11.869
33.601
25.549
0.162
0.185
80.
10.886
33.706
25.810
0.028
0.208
90.
10.733
33.723
25.851
0.230
100.
110.
120.
130.
140.
10.475
33.761
25.925
10.301
33.781
25.971
10.084
33.809
26.030
9.763
33.851
26.116
9.532
33.897
26.190
0.251
0.272
0.292
0.311
0.330
150.
9.353
33.918
26.236
0.348
160.
9.035
33.974
26.331
0.366
170.
180.
8.958
33.986
26.353
8,851 33.992
26.374
0.382
0.399
190.
200.
8.616
34.020
26.433
8.565
34.029
26.4.48
8.498
34.043
26.469
0.415
0.432
220.
0.463
240.
8.087
34.066
26.549
0.494
260.
7.959
34.081
26,58C 0.324
280.
7,690 34.092
26.62E
0.553
300.
350.
400.
450.
500.
7.507
34.103
26.662
7.110
34.128
26.739
6.772
34.161
26.811
6.549
34.182
26.857
0.581
0.648
0.713
0.774
0.831
STA 116 35 33.3N
121 28.1W
SAL
0.
13.164
10.
12.199
33.493
25.215
33.490
25.205
20.
13.196
33.489
25.205
30.
40.
50.
60.
13.114
33.496
25.228
12.620
33.525
25.347
11.918
33.371
25.517
11.660
33.559
25.556
70.
80.
90.
100.
110.
120.
130.
10.963
33.631
25.754
10.596
33.698
25.855
10.384
33.749
25.931
10.036
33.811
26.039
9.876
33.848
26.095
9.600
33.896
26.178
9486 33.914
26.211
140.
150.
160.
170.
9.402
33.929
26.236
9.287
33.936
26.261
9.157
33.960
26.300
9.073
33.976
26.327
180.
190.
200.
220.
240.
260.
280.
300.
6.894
33.999
26.373
8.768
34.017
26.407
8.626
34.035
26.4.43
8.374
34.058
26.500
8.064
34.100
26.580
7.906
34.116
26.615
7.398
34.117
26.661
7.287
34.109
26.699
6.899
34.149
26.784
350.
400.
450.
500.
550.
6.339
34.178
26.856
6.180
34.228
26.942
5.830
34.277
27.025
5.572
34.316
27.087
600.
5.327
34.340
27.136
650.
3.203
34.353
656.
5.195
34.355
27.161
27.163
0— 663
0.000
0.028
0.055
0.083
0.110
0.136
0.160
0.183
0.205
0.227
0.247
0.266
0.285
0.304
0.322
0,340
0.257
0.374
0.391
0.408
0.424
0.435
0.485
0.514
0.543
0.570
0.636
0.698
0.756
0.811
0.861
0.909
0.956
0.961
STA 118 35 29.3N
121
36.4W
t— 970
SAL
0.
12.259
33.485
25.190
0.000
10.
12.270
33.485
25.187
20.
13.268
33.484
25.187
30.
13.272
33.484
25.187
40.
13.268
33.484
23.187
0.028
0.036
0.084
0.112
50.
60.
70.
13.035
33.483
25.232
12.098
33.546
25.463
11.284
33.635
25.683
0.139
0.166
0.190
80.
90.
100.
110.
120.
130.
140.
150.
160.
170.
180.
190.
200.
220.
240.
260.
280.
300.
350.
400.
450.
10.787
33.687
25.813
10.494
32.733
23.900
10.029
33.796
26.029
9.868
33.825
26.079
9.663
33.252
26.133
9.491
33.884
26.187
9.350
33.907
26.228
9.172
33.940
26.283
9.029
33.963
26.323
8.857
33.986
26.368
8.696
34.010
26.412
8.558
36.042
26.459
8.418
34.063
26.497
8.294
34.082
26.531
8.162
34.091
26.338
7.780
3.4.081
26.607
7.387
34.080
26.662
7.209
34.088
26.694
6.737
34.125
26.787
6.497
34.180
26.863
6.308
3.206
26.908
0.212
0.234
0.254
0.274
0.293
0.312
0.330
0.348
0.365
0.382
0.399
0.415
0.430
0.461
0.491
0.520
0.548
0.576
0.642
0.703
0.762
500.
550.
600.
650.
700.
702.
5.976
34.250
26.985
5.646
34.297
27.064
5.447
34.323
27.108
5.040
34.371
27.194
4.738
34.400
21.252
4.712
34.401
27.256
0.818
0.870
0.920
0.965
1.009
1.010

=
0.
10.
20.
30.
40.
50.
60.
70.
80.
260.
280.
300.
350.
400.
450.
500.
90.
100.
110.
120.
130.
140.
150.
160.
170.
180.
190.
200.
220.
240,
550.
600.
650.
700.
712..
35 2'..6N
121
12.839
33.280
25.2.15
0.000
12.842
33.279
25.113
0.029
12.911
33.377
25.176
0.057
12.963
33.500
25.260
12.886
33.481
25.261
0.084
0.112
0.138
0.163
11.963
33.548
25.491
11.747
33.561
25.541
11.189
33.616
25.686
10.742
33.659
25.799
10.274
33.695
25.908
9.932
33.742
26.003
9.672
33.773
26.071
9.232
33.824
26.182
9.137
33.858
26.224
8.961
33.899
26.284
8.827
33.923
26.324
8.774
33.931
26.339
8.352
33.962
26.397
8.455
33.988
26.433
8.294
34.006
26.471
8.173
34.018
26.499
7.931
34.048
26.558
7.706.
34.064
26,604
7.463
34.089
26.658
7.195
34.110
26.713
7.004
34.111
26.740
6.732
34.137
26.813
6.316
34.204
26.905
6.066
34.249
26.973
5.796
34.279
27.031
5.374
34.302
27.077
5.246
34.347
27.151
4.986
34.376
27.205
0.187
0.209
0.231
0.251
0.271
0.290
0.308
0.326
0.344
0.360
0.377
0.394
0.410
0.425
0.456
0.485
0.513
0.541
0.567
0.632
0.692
0.748
0.802
0.853
0.901
0.946
4.750
34.400
27.250
0.988
4.712
34.403
27.257
0.998
110.
120.
130.
140.
150.
160.
170.
180.
190.
200.
220.
240.
260.
280.
STA 12 35 20.3N
121
=11
SAL
0.
12.949
33.487
25.253
10.
12.951
33.487
25.253
20.
12.960
33.487
25.251
12.961
33.487
25.251
30.
12.957
33.487
25.251
40.
50.
12.813
33.464
25.262
12.169
33.551
25.454
60.
11.579
33.576
25.5814
70.
80.
11.266
33.600
25.660
90.
100.
10.252
33.651
25.878
9.995
33.698
25.958
300.
350.
400.
450.
500.
550.
600.
650.
656.
9.780
33.739
26.026
9,659 33.786
26.083
9.605
33.871
26.158
9.384
33.901
26.218
9.209
33.929
26.268
8.976
33.934
26.309
8.745
33.962
26.367
8.585
34.004
26.425
8.565
34.032
26.450
8.424
34.047
26.484
8.029
34.056
26.550
7.778
34.071
26.599
7.511
34.081
26.645
7.343
34.109
26.691
7.155
34.124
26.729
6.700
34.168
26.826
6.390
34.208
26.899
6.174
34.224
26.940
5.948
34.252
26.990
5.549
34.293
27.073
5.352
34.333
27.128
5.132
34.358
27.173
5.089
34.359
27.179
0.521
0.549
0.576
0.640
0.699
0.737
0.812
0.864
0.912
0.959
0.964
0.000
0.027
0.055
0.082
0.109
0.137
0.163
0.187
0.211
0.234
0.254
0.275
0.294
0.313
0.332
0.350
0.367
0.384
0.401
0.417
0.432
0.463
0.492
SIA 131 36 10.8N
121 44.3W
t— 392
0.
11.851
33.589
25.543
10.
11.855
20.
33.591
25.544
11.857
33.593
25.545
0.000
0.025
0.049
30.
11.562
33.603
25.607
0.073
40.
11.063
33.678
25.757
0.097
50.
10.811
33.712
25.828
0.119
60.
70.
80.
10.543
33.745
25.901
10.204
33.782
23.988
10.031
33.811
26.040
0,140
0.161
0.181
90.
9.904
33.821
26.070
0.201
100.
9.703
33.856
26.130
110.
9.628
33.865
26.149
120.
130.
9.455
5.313
33.893
26.200
0.220
0.238
0.257
1140.
150.
9.066
160.
8.885
33.967
26.349
170.
180.
33.914
26.2140
0.275
9.164
33.934
26.279
0.293
190.
8.334
33.945
34.014
26.303
6.743
33.987
26.387
8.617
34.007
26.423
26.4.41
0.310
0.327
0.344
0.360
0.377
200.
220.
240.
8.491
34.022
26.454
0.392
8.146
34.056
26.333
0.424
7.984
34.073
26.570
0.453
260.
7.799
34.089
26.610
0.482
280.
7.648
34.096
26.638
300.
7.483
34,110 26.672
350.
7.095
34.133
26.745
500.
0.311
0.339
0.605
0.780
STA 133 36
7.5N
121 51.9W
SAL
0.
12.006
33.559
25.491
0.000
10.
12.011
33.557
25.488
0.025
20.
12.009
33.357
25.489
0.050
30.
12.010
33.556
25.487
0.075
40.
11.996
33.559
25.493
0.100
50.
11.930
33.571
25.514
0.125
60.
11.861
33.585
25.538
70.
11.754
80.
11.24.4
0.130
33.604
25.573
0.174
33.666
25.715
0.198
90.
10.903
33.700
25.802
0.220
100.
10.283
33.772
110.
9.956
33.813
120.
9.744
33.837
130.
9.396
33.874
25.967
26.054
26.109
0.242
0.262
0.281
26.194
0.300
140.
170.
190.
200.
260.
9.191
8.661
6.426
33.919
34.005
180.
8.575
34.016
26.263
150.
8.932
33.967
26.342
26.414
0.318
0.335
160.
8.813
33.983
26.373
0.352
0.369
220.
8.073
240.
26.436
0.385
34.041
26.478
0.400
8.391
34.043
26.486
0.416
34.074
26.558
0.447
7.904
34.088
26.594
0.476
7.666
34.109
26.645
0.505
280.
7.448
34.121
26.686
0.532
300.
350.
7.341
3.126
26.705
0.560
6.684
34.133
26.517
0.624
400.
6,334 34.190
450.
6.096
314.221
26.892
0.685
26.947
0.742
500.
5.849
550.
34.244
26.996
0.797
5.366
34.284
27.087
0.848
600.
650.
664.
5.090
34.337
27.162
0.896
4,856 34.375
27.219
0.941
4.816
34.380
27.227
0.953

SIA 135
36 3.4N
122 0.6w
0.
SA'
12.229
33.543
25.436
10.
20.
30.
40.
50.
60.
70.
12.233
33.539
25.432
12.231
33.540
25.433
12.224
33.542
25.436
12.220
33.541
25.436
12.003
33.571
25.501
11.850
33.578
25.535
11.138
33.663
25.731
0.000
0.026
0.051
0.077
0.102
0.127
0.152
0.176
80.
90.
10.824
33.699
25.816
10.335
33.774
25.959
10.220
33.787
25.990
0.198
0.219
100.
0.239
110.
10.027
33.806
26.037
0.260
120.
9.606
33.864
26.152
0,279
130.
9.520
33.870
26.171
140.
9.312
33.883
26.215
150.
9.238
0.298
0.316
33.890
26.233
0.334
160.
8,965 33.967
26.336
170.
8.890
33.985
26.362
180.
8.780
33.998
26.390
0.351
0.368
0,385
190.
8.613
34.007
26.423
0.401
200.
8.414
34.035
26.475
0.417
220.
6.173
34.052
26.525
0.448
240.
260.
7.698
34.096
26.630
0.507
280.
7.436
34.107
26.677
300.
7.274
34.132
26.719
0.535
0.562
350.
7.936
34.074
26.578
6.740
34.160
26.815
0.478
0.627
400.
6.366
34,184 26.883
450.
5.943
34.220
26.966
0.687
0.744
500.
5.887
34.281
27.021
0.798
550.
5.595
34.312
27.082
0.849
600.
5.250
650.
34.324
27.133
0,898
5.004
34.343
27.177
0.944
698.
4.879
34.374
27.216
0.986
STA 137
0.
10.
35 59.7N
122
SAL
12.532
33.524
25.363
12.531
33.522
25.362
20.
30.
40.
50.
60.
70.
12.527
33.521
25.362
12.527
33.521
25.362
12.529
33.325
25.364
12.525
33.523
25.363
12.439
33.531
25.387
11.797
33.584
25.549
0.000
0.026
0.053
0.079
0.105
0.131
0.137
0.183
80.
90,
11.196
33.666
25.723
10.871
33.710
25.816
10.375
33.749
25.899
10.213
33.797
25.999
0.206
0.228
0.250
100.
110.
0.271
120.
10.020
33.826
26.033
0.290
130.
9.747
33.857
26.124
140,
180.
8.921
33.943
26.325
0.310
9.377
33.892
26.179
0.329
150, 9.412
33.916
26.225
0.347
160.
9.296
33.928
26.253
0.365
170.
9.163
33.948
26.290
0.382
0.400
190.
8.680
34.012
26.417
0.416
200.
8.442
34.031
26.469
0.432
220.
8.210
34.060
26.526
0.463
240.
8.009
34.067
26.562
0.493
260.
7.772
34.084
26.610
0,522
280.
7.469
3.4.095
26.662
300.
0.551
7.290
34.110
26.700
0.578
350.
6.883
34.142
26.781
0.644
0.707
400.
450.
500.
6.609
34.170
26.840
6.120
34.228
26.950
5.778
34.257
27.015
0.765
0.819
550,
600.
650.
700.
720.
5.571
34.287
27.065
0.871
5.343.
34.328
27.125
0.920
5.085
34.348
27.171
0.966
4.948
34.375
27.208
4.844
34.392
27.233
1.011
1.028
139 35 33.1N
122 21.7W
D—2000
0.
10.
20.
30.
40.
50.
60.
70.
80.
90.
100.
110.
120.
130.
140.
150.
160.
170.
180.
12.672
33.231
25.110
12.676
33.231
25.109
12.672
33.231
25.110
12.643
33.232
25.116
12.583
33.231
25.127
12.234
33.291
25.240
11.670
33.306
25.358
10.800
33.505
23.669
10.707
33.581
23,745
10.011
33.574
25.859
9.598
33.644
25,982
9.376
33.710
26.070
9.177
33.770
26.149
9.063
33.801
26.192
9.226
33.924
26.261
9.051
33.961
26.318
8.786
32.931
26.337
8.651
33.994
26.407
8.554
34.018
26.441
0.000
0.029
0.057
0.086
0.115
0.170
0.195
0.218
0.240
0.261
0.281
0.300
0.318
0.336
0.354
0.371
0.387
0.404
190.
200.
220.
240.
260.
280.
300.
350.
400.
8.373
34.028
26.476
0.419
6.185
34.037
26.512
7.826
34.029
26.559
0.435
0.465
7.517
34.048
26.618
7.282
0.494
3.4.070
26.669
0.522
7.001
34.062
26.702
0.550
6.771
34.066
26.737
3.904
34.035
26.825
5.846
34.133
26.910
0.576
0.641
0.701
450.
500.
5.680
34.198
26.981
0.757
3.732
34.300
27.055
0.809
550.
5.550
34.337
27.106
600.
5.296
34.357
27.153
0.859
0.906
650.
5.102
34.376
27.191
0.952
666.
4.982
34.385
27.213
0.967
STA 146 36 47.5N
122 3.0W
0— 313
0.
10.
110.
120.
130.
140.
150.
160.
170.
180.
190.
200.
20.
30.
40.
50.
60.
70.
80.
90.
100.
220.
240.
260.
280.
300.
500.
12.221
33.528
25,426
12.240
0.000
33.527
25.422
0.026
12.245
33.527
25.421
0.051
12.241
33.528
25.422
12.241
33,528 25.423
11.839
33.572
25.533
11.492
33.604
25.622
10.987
33.664
25.760
10.582
33.707
25.864
10.112
33.789
26.010
9.947
33.815
26.037
9.709
33.841
26.118
9.510
33.857
26.163
9.207
33.908
26.252
6.856
33.960
26.349
8.702
33.976
26.385
8.582
33.980
26.407
8.503
33.990
26.427
7.892
34.046
26.562
7.626
34.071
26.621
7.429
34.089
26.663
7.204
34.106
26.709
0.077
0.103
0.128
0.152
0.175
0.197
0.218
0.238
0.257
0,276
0.294
0.311
0.328
0.344
0.361
8.420
33.991
26.441
0.377
8.202
34.014
26.491
0.392
8.128
34.021
26.508
8.033
0.408
3.031
26.530
0.438
0.468
0.497
0.526
0.553
0.800

ST4 148 36 43.4N
122
SAL
L— 950
0.
10.
12.311
12.312
20.
12.319
30.
12.322
33.463
25.356
40.
12.332
50.
12.344
33.463
33.463
33.462
25.356
0.053
33.466
33.471
25.359
25.359
25.357
25.359
0.000
0.026
0.079
0.105
0.132
60.
11.532
33.393
25.450
0.158
70.
80.
90.
10.886
33.492
25.644
10.625
33.598
25.772
0.182
0.205
10.214
33.708
25.929
0.227
100.
9.831
33.763
26.033
0.247
110.
9.712
33.830
26.108
0.267
120.
9.601
33.851
26,143 0.286
130.
9.361
33.898
26.219
0.304
140.
9.145
150.
8.942
160.
8.873
33.921
26.272
0.322
33.931
26.328
0,339
33.963
26.348
0.356
8.623
33.994
26.411
0.373
170.
180.
8.483
34.009
26.445
190.
260.
280.
300.
350.
400.
450.
500.
8.402
34.018
26.464
200.
8.275
34.032
220.
8.128
34.076
240.
26.494
0.389
0.405
0.420
26.551
0.451
7.925
34.100
26.600
0.480
7.865
34.113
26.619
0.509
7.624
34.080
26.628
0.538
7.348
34.078
26.666
0.566
6.904
34.120
26.761
0.633
6.430
34.157
26.853
0.696
6.001
34,174 26.923
0.754
5.596
34.226
27.014
0.809
550.
5.356
34.270
27.077
0.860
600.
5.152
34.310
27.133
0.909
650.
700.
742.
4.923
34.348
27.190
4.670
34.382
27.246
4.542
34.398
27.272
0.955
0,998
1.033
STA 132
=
36 34.4N
122
S.AL
32.8W
SIC-MA
0.
12.097
33.254
25.238
12.096
33.254
25.238
12.094
33.257
25.240
10.
20.
0.000
0.027
0.055
30.
40.
50.
12.094
33.257
25.241
12.099
33.260
25.242
12.120
33.276
25.250
0.082
0.110
0.137
60; 11.883
33.410
25.399
70.
0.164
11.126
33.525
25.627
0.189
80.
10.676
33.611
25.774
0.211
90.
100.
10.485
33.668
25.851
9.864
33.597
25.902
0.233
0.255
110.
120.
9.435
33.677
26.034
9.225
33.721
26.103
0.275
0.294
1.30.
140.
2.50.
160.
170.
180.
190.
200.
220.
240.
9.197
33.881
26.233
2.904
0.313
33.913
26.304
0.331
8.771
33.951
26.255
0.348
8.618
33.958
26.384
0.364
6.505
33.997
26.432
0.381
8.440
34.019
26.459
7.852
34,074 26.591
0,397
6.357
34.033
26.482
2.250
34.047
0.412
26.510
0.428
8.068
34.054
26.542
0.458
0.488
260.
7.627
34.091
26.637
0.317
280.
7,453 34.096
26.665
0.545
300.
7.241
34.106
26.703
0.372
350.
6,746 34,127 26,788 0.538
400.
450.
6.306
34.163
26.875
6.004
34.199
26.942
0.699
0.757
500.
550.
600.
650.
700.
714.
5.663
34.226
27.005
5.404
34.275
27.076
5.023
34.288
27.131
4.983
34.350
27.184
4.824
34.371
27.219
0.612
0.863
0.912
0.958
1.001
4.767
34.377
27.230
1,023
_
STA 150 36 36.4N
122
SAL
L2380
0.
12.102
33.302
25.274
0.000
10.
12.101
33.301
25.273
0.027
20.
12.102
33.302
25.274
0.054
12.106
33.301
25.272
0.081
30.
40.
12.103
33.313
25.282
0.108
50.
11.942
33.468
25.432
0.135
60.
11.000
33.417
25.566
0.160
70.
10.184
33.438
25.724
0.183
80.
9.857
33.581
25.891
0.205
90.
9.944
33.683
25.955
0.226
100.
9.524
33.729
26.061
0.246
110.
120.
600.
650.
700.
9.270
33.814
26.169
9,331 33.864
26.198
0.265
0.284
130.
9.138
33.904
26.259
0.302
140.
9.045
33.934
26.298
220.
240.
7.870
34.072
26.586
0.477
260.
7.699
34.084
26.620
0.506
280.
7.458
34.098
26.666
300.
0.319
150.
8.842
33.965
26.335
0.336
160.
6,724 33.980
26.385
0.353
170.
8.587
34.005
26.426
0.369
180.
8.444
34.025
26.463
0.385
190.
8.367
34.036
26.483
0.401
200.
8.269
34.041
26.502
0.417
8.094
34.054
26.539
0.447
0.534
7.209
34.105
26.707
0.561
350.
6.734
34.134
26.795
0.627
400.
6.220
34.163
26.886
0.688
450.
5.909
34.190
26.946
0.745
500.
5.672
34.223
27.002
0.800
550.
5.413
34.269
27.070
0.852
5.143
34.316
27.139
4.963
34.349
0.900
27.186
0.946
4,745 34.380
27.235
0.989
712.
4.711
34.385
27.243
0.999
STA 154
0.
10.
36 28.4N
122 45.9W
SAL SIGMA
12.045
33.274
25.263
12.047
33.274
25.263
20.
30.
40.
50.
12.032
33.277
25.268
12.020
33.282
25.274
12.013
33.282
25.275
60.
70.
80.
12.013
33.282
25.275
12.014
33.283
25.276
11.953
33.330
25.323
11.236
33,527 25.608
90.
100.
110.
120.
130.
140.
150.
160.
170.
180.
190.
200.
220.
240.
260.
280.
10.738
33.600
25.754
10.302
33.691
25.901
9.950
33.754
26.009
9.693
33.801
26.089
9.430
32.850
26.171
9.239
33.877
26.223
9.084
8.832
8.719
33.919
23.949
33.984
26.280
26.344
26.389
8.605
33.999
26.418
6.542
34.020
26.445
2.268
34.007
26.476
7.920
34.015
26.534
7.638
34.020
26.579
7.408
34.031
26.621
300.
350.
400.
450.
7.395
34.073
26.656
7.277
34.105
26.697
6.665
3.112
26.787
6.420
34.165
26.861
500.
550.
600.
650.
700.
718.
5.991
34.185
26.932
5.585
34.232
27.020
5.398
34.277
27.078
5.191
34.318
27.135
=
0.000
0.027
0.054
0.081
0.109
0.136
0.163
0.190
0.215
0.238
0.260
0.280
0.300
0.319
0.337
0.355
0.372
0.389
0.405
0.422
0.437
0.468
0.498
0.527
0.355
0.562
0.648
0.710
0.768
0.823
0.874
0.922
4.955
34.340
27.180
0.969
4.737
34.372
27.230
..012
4.673
34.363
27.246
1.027

STA 159
0.
37 3.ON
123
SAL
11.561
33.194
25.291
10.
20.
30.
40.
11.558
33.194
25.291
11.604
33.231
25.312
11.963
33.457
25.420
11.993
33.467
25.422
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.
698.
0.000
0.027
0.054
0.080
0.105
11.982
33.467
25.424
11.597
33.537
25.550
10.943
33.676
25.776
10.742
33.702
25.833
10.365
33.738
25.927
10.050
33.766
26.002
0.131
0.156
0.180
0.202
0.223
0.244
9.832
33.787
26.052
9,534 33.837
26.143
5.326
34.315
27.116
0.263
0.283
9.432
33.854
26.170
9.343
33.878
26.206
9.237
33.897
26.238
9.056
33.933
26.295
8.813
33.960
26.355
8.669
33,979 26.393
0.302
0.320
0.338
0.356
0.373
0.390
8.563
33.982
26.411
8.4.45
33.991
26.436
0.406
0.422
6.179
34.037
26.513
7.877
34.058
26.574
7.612
34.082
26.632
7.439
34.091
26.663
0.453
0.484
0.513
0.541
7.221
34.105
26.705
6.712
34.125
26.791
6.349
34.168
26.873
0.568
0.634
5.492
34.287
27.075
0.695
6.058
34.206
26.940
5.763
0.753
3.251
27.013
0.807
0.859
0.908
5.181
34.340
27.153
4.926
34.353
27.193
0.955
0.999
STA 162 37 10.3N
122 55.3w
L— 496
150.
160,
170.
180,
190.
200.
220.
240.
260.
0.
60.
11.378
32.993
25.168
0.000
10.
20
11.376
32.992
25.168
0.028
.11.386
32.991
25.166
0.056
30.
11.391
33.003
25.174
40.
50.
11.826
33.423
25.419
11.852
33.469
25.450
0.084
0.111
0.136
0.162
70.
80.
90.
100.
110.
120.
130.
140,
11.818
33.489
25.472
11.402
33.579
25.619
10.702
33.695
25.834
10.289
33.756
25.953
10.225
33.769
25.975
0.186
0.209
0.230
0.251
0.271
0.290
0.309
280.
300.
350.
400.
450.
500.
9.969
33.796
26.039
9.685
33.825
26.109
9.433
33.858
26.176
9.122
33.913
26.269
8.918
33.944
26.326
8.818
33.954
26.350
8.675
33.972
26.386
8.490
33.998
26.435
8.412
34.009
26.455
8.352
34.018
26.471
8.053
34.046
26,539
7.928
34.058
26.567
7.608
34.076
26.627
7.481
34.088
26.655
7.337
34.098
26.684
6.930
34.125
26.761
6.387
34.169
26.869
5.880
34.211
26.967
0.327
0.345
0.362
0.378
0.394
0.410
0.426
0.457
0.487
0.516
0.544
0.572
0.638
0.701
0.757
0.810
110.
120.
130.
140.
150.
160.
170.
180.
190.
200.
220.
240.
500.
S'2.4 163
0.
10.
20.
30.
40.
37 13.2N
122 49.0W
SA'.
11.4.46
32.951
21.124
11.450
32.952
25.124
11.456
32.953
25.124
11.731
33.245
25.299
11.919
33.428
25.406
50.
60.
70.
80.
90.
100.
11.878
33.472
25.448
11.543
33.536
25.575
1..336
33.599
25.646
11.025
33.623
10.671
33.683
25.721
25.830
10.455
33.695
25.877
9.848
33.716
25.997
9.510
33.809
26.126
9.309
33.881
26.214
8.947
8.4.62
33.920
26.303
8.835
33.945
34.000
26.340
26.441
8.350
34.010
26.466
8.297
8.239
34.014
26.477
34.018
26.489
8.127
34.025
26.511
7.616
34.070
26.622
7.601
34.073
26.626
D— 255
0.000
0.028
0.057
0.085
0.111
0.137
0.162
0.125
0.209
0.231
0.252
0.273
0.293
0.312
0.329
0.346
0.363
C.379
0.394
0.410
0.425
0.454
0.483
0.805
STA 165 37 17.7N
122 39.4W
StL
0.
1..417
32.932
21.114
10.
11.412
32.935
25.118
20.
11.473
33.000
25.157
30.
11.613
33.201
25.287
40.
11.815
33.379
25.387
50.
11.835
33.469
25.449
60.
11.573
33.321
25.543
70.
10.913
33.620
25.739
80.
90.
9.942
33.745
9.628
33.804
26.004
26.102
200.
500.
D— 98
0.000
0.029
0.057
0.084
0.111
0.137
0.162
0.185
0.207
0.226
0.418
0.792

SIA 167 37 219N
47
0.
200.
11.591
33.247
25.326
40.
11.550
0.000
10.
11.647
33.258
25.325
0.027
20.
11.878
33.335
25.342
30.
11.911
33.515
25.475
0.053
0.079
33.551
25.570
0.103
0.403
500.
0.771

VERTICAL PROFILES

200—
300 -
400 -
JANUARY 1985
5.
I I I I
10.0
,,,,,/I
15.0
STATION
1
SALUflTY
20.0
33.0
33.6
34.2
I
34.8
24.0
25.0
28.0
27.0
I
K!
100—
100100 —
200 -
300
—
200—
300
400
—
400
500 500
—
500
100
400
500
200
300
JANUARY 1985
TEMPERLTURE
300
400
500
100
200
STATION 2
34.2
34.8
100
200
300
400
500
SIGMA—T
25.0
25.0
27.0
26.0

400
500
100
200
300
100
200
300
400
500
JANUARY 1985
TEMPERATURE
100
200
300
400
500
STATION 3
33.0
33.8
34.2
34.8
100
200
300
400
500
SICMA—T
25.0
28.0
27.0
28.0
JANUARY 1985 STATION 6
SIGMA-T
300
400
100
200
500
300
400
100
200
500

JANUARY 1985
5.0
TEMPER1LTURE
10.0
15.0
20.0
STATION 8
300
400
500
100 -
200
100
200
300
400
500
100
200
300
400
500
SIGMA—T
27.0
28.0
100
400
500
200
300
JANUARY 1985
15.0
20.0
STATION 10
33.8
34.2
34.8
300
400
100
200
500
100
200
300
400
500
SIGIdA—T

100
200
300
400
500
JANUARY 1985 STATION 13
200
300
400
500
100
200
300
400
500
JANUARY 1985
STATION 14
BIGMA—T
24.0
25.0
26.0
27.0
28.0
I
I
100 -
200 -
300 -
400 -
500 -
SIGMA—T
100
200
300
400
500
100
200
500

100
200
300
400
500
JANUARY 1985
TEMPERATURE
STATION 16
300
400
500
400
500
100
200
300
300
400
100
200
500
JANUARY
TEMPERATURE
10.0
15.0
STATION 17
SALINiTY
34.2
34.8
SIGMA—T
24.0
25.0
26.0
100
200
300
400
500
28.0

200
300 -
400 -
500 -
100
JANUARY 1985
5.0
I I
TEMPERATURE
10.0
15.0
I
I
I
20.0
I
I
STATION 18
300
400
500
24.0
SIGMA—T
25.0
26.0
27.0
25,0
100
200
300 -
400 -
500 -
JANUARY 1985 STATION 19
5.0
10.0
15.0
20.0
IIIIIIII/I[T111L 33.0
I
33.8
I
34.2
I
34.8
S1C.MA—T
24.0
25.0
28.0
27.0
28.0
I
100 — 100 -
100
200200200-
300300300-
400—
500—
400—
500—
400-
500-

300
400
100
200
500
JANUARY 1985
5.0
10.0
15.0
20.0
33.0
33.8
34.2
I
34.8
I
SIGMA—T
24.0
25.0
28.0
27.0
28.0
I
100
200
100
200
300 300
400
500
400
500
100
JANUARY 1985
5.0
10.0
15.0
20.0
33.0
33.8
34.2
I
I
I I
I
34.8
I
SIGMA—T
24.0
25.0
28.0
27.0
28.0
I
4
100 100
200 200 200
300
400
300
400
300
400
500 500 500

JANUARY 1985
SIGMA—T
100
200
300
400
500
100
200
300
400
500
100
400
500
300
400
500
JANUARY 1985
10.0
15.0
20.0
33.6
34.2
34.8
100 100
200
300
400
500
300
400
500
100
200
SIGMA—T

JANUARY 1985
TBMPERATUEE
5.0
200
100
200
400
500
400
500
100
200
300
400
500
JANUARY 1985
TEMPERATuRE
STATION 31
SALINITY too
400
500
100
200
300
400
500
100
200
300
400
500
SIGMA—T
28.0

JANUARY 1985
5.0
TEMPERATURE
10.0
15.0
20.0
33.0
33.6
'i' 'i' SIGML—T
24.0
25.0
26.0
27.0
28.0
100—
100100—
200—
300—
300 -
400—
500
500—
500—
100
JANUARY 1985
20.0
33.0
I
SALINiTY
33.6
34.2
34.8
I
SIGMA—T
24.0
25.0
28.0
27.0
28.0
100
too -
200
—
200
200 -
300 -
300
300 -
400
400
400 — soa —
500
500 —

JANUARY 1985
100
200
300
200
300
400
500 500
100
200
300
JANUARY 1985
SALmnTrY
500
100
200
300
400
500
100
200
300
SIGMA—T
24.0
25.D
28.0
27.0
28.0
100 -
200 —
300 —
400 -
500 —
500

1 DO
200
300
400
500
JANUARY 1985
SALIPflTY
100
100 -
200
300
400
500
25.0
28.0
27.0
28.0
' I
100
JANUARY 1985
10.0
15.0
20.0
33.8
34.2
34.8
24.0
SIGIL&—T
25.0
28.0
27.0
28.0
I
J
100
200 200 -
300
400
300
400 -
500 500

100
200
300
400
500
JANUARY 1985
'TEMPERATURE
STATION 46
100
200
300
400
500
400
500
200
300
SIGMA—T
JANUARY 1985 STATION
5.0
ii
TEMPERATURE
10.0
15.0
33.0W
49
SALINITY
33.8
34.2
34.8
I
I
I
24.0
25.0
SIGMA.—T
26.0
27.0
28.0
100 -
100 — 100 —
200 -
200
-
200
—
300 -
300 300 —
400
—
500
—
400
500
400
-
500
-

200-
300-
400-
500-
JANUARY 1985
5.0
TRMPERLTURE
10.0
15.0
STATION
20.0
33.0
33.8
I
34.2
34.6
I
I
SIGMIL—T
24.0
25.D
28.0
27.0
28.0
100 — 100
200
100 —
200-
300
400-
500
300—
400-
500-
JANUARY 1985
5.0
TRMPERLTtJKE
10.0
15.0
STATION
20.0
33.0
I I
33.8
I I
34.2
I
I
34.8
SIGMA—T
240 25.0
28.0
27.0
26.0
100100100-
200
300-
200-
300-
200-
300-
400 -
500-
400 -
500-
400
500

JANUARY 1985
100
300
400
600
100
200
300
400
500
100
200
300
400
500
JANUARY 1985
TEMPERATURE
10.0
15.0
20.0
sAuNrrY
32.6
34.2
100
200
300
400
500
300
400
100
200
500
SIGMA—T

400
500
200
300
JANUARY 1985
5.0
TEMPERLTURB
10.0
100
200
300
400
500
200
300
400
SIGILA.—T
100
200
500
JANUARY 1985
100
200
300
400
500
34.2
300
400
500
100
200
SIGIdA—T
25.0
25.0

100
200
400
500
JANUARY 1985
20.0
33.0
100
200
300
400
500
100
200
300
400
500
SIGIL&—T
100
200
300
JANUARY 1985
TRMPER&TtTRE
500
100
200
300
400
500
SLL]NITY
34.8
24.0
SIGMA—T
100
200
300
400
500

100
JANUARY 1985
5.0
I I I
TBMPER&TITRE
I
10.0
I
I I I
15.0
I I I
SALINFI'Y
20.0
33.0
33.8
I I
I
I I
34.2
I
I
34.8
I
24.0
SIGMA—T
25.0
26.0
27.0
28.0
I
1.00
100
200 200 200
300 300 300
400 400 400
500 500 500
200 -
300 -
400 -
JANUARY
5.0
10.0
15.0
20.0
33.0
33.6
I I
34.2
I
I
34.8
I
24.0
25.0
28,0 27.0
28.0
I j
100 -
100 100
200
300
400
200
300
400
500 500 500

200—
300—
400
JANUARY 1985 STATION
5.0
liii
TEMPERATURE
10.0
15.0
I I I
20.0
33.0
I
I
75
33.6
I
I
34.2
34.8
—I——I
I
SIGM&—T
24.0
25.0
26.0
27.0
I
—
I
I
28.0
I
100-
100—
200—
300—
400
200
-
300-
400
-
500 -
500 500 too
200
300
400
500
JANUARY 1985
TEMPERATURE
SALINiTY
100
200
300
400
500
24.0
25.0
28.0
27.0
28.0
100
200
300
400
500

400
JANUARY 1985
TEIIPERLTURE
100
200
300
400
500
SIGMk—T
500
300
400
100
200
500
JANUARY 1985
100
200
300
4.00
33.8
34.2
34.8
100
200
300
400
500
25.0
SIGMA—T
28.0
27.0
28.0

300
400
100
200
500
JANUARY 1985
TEMPERATURE
100
200
300
400
500
100
200
300
400
500
SIGMA—T
28.0
27.0
28.0
100
JANUARY 1985
TEMPERATURE
SALDJTFY
300
400
100
200
500
100
200
300
400
500
SIGMA—T

JANUARY 1985
SIGUA—T
26.0
27.0
28.0
100
200
300
500
300
400
500
300
400
100
200
500
100
200
JANUARY 1985
SALINITY
500
400
500
200
300
300
400
100
200
500
SIG4Et&-T

400
500
JANUARY 1985
TBMPER&TURB
15.0
20.0
SALINITY
100
400
500
200
300
100
200
300
400
SIGMA—T
100
200
300
400
500
JANUARY 1985
SALINITY
400
600
200
300
100
400
500
200
300
SIGMk—T

JANUARY 1985
5.0
10.0
15.0
20.0
33.0
33.8
34.2
34.8
I
SIGMA—T
24.0
25.0
28.0
27.0
28.0
100-
100100-
200-
300-
300— 300—
400 -
400 400 -
600
500 600
5.0
TE]APBRAi'URE
15.0
20.0
1111111
33.0
SALINITY
33.6
34.2
34.8
1
4
I
4
I
4
SIGMA—T
24.0
25.0
28.0
27.0
28.0
I
4
100
100
100
-
200—
200—
300
400—
400
-
500—
500—
500

300
400
100
200
500
JANUARY 1985
10.0
15.0
20.0
STATION 102
100
200
300
400
500
300
400
100
200
500
JANUARY 1985
TEMPERATURB
STATION 105
33.0
I
33.8
I I
34.2
34.8
I
100
200
300 -
400 -
500
400
500
100
200
300
300
400
100
200
500
SIGML—T

400
500
100
200
300
JANUARY 1985
TEMPER&TURE
STATION 108
100
200
24.0
SIGMA—T
25.0
28.0
27.0
300
400
100
200
500
100
JANUARY 1985
5.0
TEMPERATURE
10.0
15.0
STATION
20.0
33.0
113
SALThflTY
33.6
34.2
34.8
24.0
I
25.0
J
26.0
27.0
28.0
I
100 100 -
200200-
200
300-
300—
300 —
400-
400-
400 —
500-
500-
500

JANUARY 1985 STATION 114
100
200
300
400
600
100
200
300
500
300
400
500
100
JANUARY 1985
10.0
15.0
STATION 115
100
200
300
400
500
200
300
400
500
SIGMA—T
24.0
25.0
28.0
27.0
I
I
I
0
100 —
200 -
300 -
400
500 -
SIGMA—T

300
400
'Do
200
JANUARY 1985
TEMPERATURE
STATION 116
200
300
400
500
300
400
100
200
500
SIGMA—T
25.0
28.0
27.0
300
400
500
100
200
JANUARY 1985
TEMPERATURE
STATION 118
SALINiTY
400
500
100
200
300
400
500
100
200
SIGIL&—T

JANUARY 1985 STATION 120
SIGMk—T
100
200
100
200
300
400
500
100
200
300
JANUARY 1985 STATION 122
100
400
500
200
300
SIGMk—T
25.0
2&0 28.0
500
100
200
300
400
500
300
400
500 too
200

JANUARY 1985
STATION 131
100
200
300
400
500
100
200
300
200
300
400
500
JANUARY 1985
TEMPERATURE
300
400
500
100
200
STATION 133
33.8
34.2
34.8
400
600
200
300
100
400
500
200
300
SJGMA—T

300
400
500
100
200
100
200
300
400
500
JANUARY 1985
TEMPERLTURE
STATION 135
100
200
300
400
500
300
400
100
200
500
JANUARY 1985 STATION 137
100
200
24.0
'
25.0
28.0
27.0
28.0
I
I I
100 -
200 —
300 -
400 -
500 -

300
400
500
JANUARY 1985
TEMPERATURE
STATION 139
100
200
300
400
500
300
400
100
200
SIGMA—T
100
200
300
400
500
JANUARY 1985
TEMPERATURE
STATION 146
100
400
500
200
300
SIGMA—T
24.0
25.0
28.0
27.0
28.0
100
200
300

200
300
JANUARY 1985
TEMPBRAThTRE
300
400
100
200
500
STATION 148
33.0
33.8
34.2
34.8
400
500
100
200
300
SIGMA—T
28.0
27.0
28.0
400
500
100
200
300
JANUARY 1985
TEMPERATURE
STATION 150
100
200
300
400
300
400
500
100
200
SIGMA—T

100
400
500
200
300
JANUARY 1985
TEMPERATURE
STATION 152
300
400
500
100
200
300
SIGMA-T
300
400
500
100
200
JANUARY 1985
TEMPERATURE
10.0
15.0
STATION
100
200
300
500
SALINITY
300
400
100
200
500
SIGMA—T

100
200
300
400
JANUARY 1985
STATION 159
SALUfiTY
100
200
300
500
SIGMA—T
24.0
25.0
26.0
27.0
100
200
300
400
500
100
200
300
500
JANUARY 1985
TSMPERATURE
STATION 162
SALINITY
300
400
100
200
500
100
200
300
400
500
SIGMA—T

300
400
100
200
500
JANUARY 1985
5.0
TEMPERATURE
10.0
400
500
100
200
STATION 163
SALINITY
33.0
SIGMA—T
24.0
25.0
26.0
27.0
26.0
100 —
200 -
300 -
400 -
500 -
JANUARY 1985
I
I
TEMPERATURE
I
10.0
I
I
15.0
I 1
I
STATION
20.0
33.0
I
165
SALINITY
33.6
34.2
I
I
I
I I
34.8
SIGMA—T
24.0
25.0
28.0
27.0
26.0
100 — 100 100—
200 -
400—
500—

JANUARY 1985
STATION 167
5.0
I I I I
10.0
J
I I
15.0
I
1
20.0
33.0
33.6
I
34.2
I
34.8
24.0
25.0
100 -
100 -
100
200
200 — 200
300
—
$00 -
300
400 -
400
400
500 500 -
500

POTENTIAL TENPERATURE-SALINITY PLOTS

MAPS. FULL CCCCS REGION

36
35
37
TEMPERATURE (DEG C)
10 M
34
123 122 121 120

37
TEMPERATURE (DEG
36
35
34
123 122 121 120

37
TEMPERATURE
36
35
34
123 122 121 120

36
35
37
TEMPERATURE
34
123 122 121 120

36
35
37
TEMPERATURE (DEG C)
400 M
34
123 122 121 120

36
35
37
SALINITY
34
123 122 121 120

37
SALINITY
36
35
34
123 122 121 120

37
SALINITY (PPT)
36
100 M
35
34
123 122 121 120

36
35
34
37
SALINITY (PPT) 200 M
120

37
SALINITY (PPT)
36
35
34
123 122 121 120

36
35
37
10 M
34
123 122 121 120

36
35
37
STGMA—T
34
123 122 121 120

37
SIGMA—T
100 M
36
35
34
123 122 121 120

36
35
37
SIGMA—T 200
M
123 122 121 120

37
26.87
28.87
26.86
26.88
25.89
26.85
36
S.'
26.91
I
I
I
I
I
28.88
/
/
I
26.85)
JANUARY 1985
400
M
35
4
S
26.81
26.83
34
123 122 121

37
DYNAMIC HEIGHT
0/100 M
36
35
34
123 122 121 120

37
DYNAMIC HEIGHT (DYN CM)
36
35
34
123 122 121 120

37
DYNAMIC HEIGHT (DYN CM)
50/200 M
36
35
34
123 122 121 120

37
DYNAMIC HEIGHT (DYN CM)
100/200 M
36
35
34
123 122 121 120

36
35
37
DYNAMIC HEIGHT
34
123 122 121 120

37
DYNAMIC HEIGHT
36
50/500 M
34
123 122 121 120

HEIGHT (DYN CM)
36
35
34
123 122 121 120

36
35
37
DYNAMIC HEIGHT
200/500 M
34
123 122 121 120

37
DEPTH (M)
36
35
34
123 122 121 120

37
TEMPERATURE (DEG C)
36
35
34
123 122 121 120

36
35
37
SALINITY
34
123 122 121 120

37
36
35
34
123 122 121 120

37
TEMPERATURE (
36
35
34
123 122 121 120

35
34
37
SALINITY (PPT)
36
120

37
36
35
34
123 122 121 120

37
TEMPERATIJRE
36
35
34
123 122 121 120

36
35
37
SALINITY
34
123 122 121 120

MAPS, SNAPSHOT

35
TEMP ERATURE
34
121
120

35
TEMPERATURE
34
121 120

35
TEMPERATURE
34
121 120

35
TEMPERATURE (DEG C) 200 M
34
121 120

35
TEMPE RATURE (DEG C)
JANUARY 1985
SNAPSHOT
400M
6.69
6.68
6.74
'——S.'.
6.75
6
6.66
———,
6.65
6.82
6.89
/
5.68
6.69
8.84
6.78
34
121 120

35
SALINITY
JANUARY 1985
SNAPSHOT
3350
33.47
33.47
33.47
33.45
33.45
33.46
33.47
33.47
33.47
33.41
33.41
33.49
33.48
33.50
33.40
33149
33.47
33.41
33.44
33.46
33.44
33.45
33.46
33.46
33.48
33.44
33.47
33.43
33.44
33.47
33.45
33.47
33.45
33.43
33.47
33.46
33.45
33.42
33.46
33.44
33.40
33.40
33.42
fl40
33.47
33.42
1OM
34
121 120

35
SALINITY (PPT)
3,3.57
3350
3352
33.58
JANUARY 1985
SNAPSHOT
50M
33.50
33.58
33.50
,..—
33.57
33.52
33.52
33.57
3346
33.48
33.46
33.46
3349
33.46
33.51
34
121
120

35
SALINITY (PP'
34
121 120

35
SALINITY (PPT)
JANUARY 1985
SNAPSHOT
200M
34.05
34.03
34.02
33.95
33.96
33.96
33.98
33.97
tP
34.07
34.00
34.00
34.03
34.00
3401
34.01
3400
33.99
34.01
34.00
34.01
34
121 120

35
SALINITY (PPT)
JANUARY 1985
SNAPSHOT
400M
34.14
34.15
34.18
34.21
(
34.17
34.16
14
34.17
34.16
34.17
34.17
34.18
34.16
34.17
34.20
34.15
34.17
34.19
34.16
3410
I,
,'
34.18
34.18
34.19
34
121 120

35
10 M
34
121 120

35
5GM
34
121 120

35
100 M
34
121 120

35
200
M
34
121 120

35
26.89
26.82
26.58/
26.8.3
26.52
26.82
25.81
(S26.76
26.5
26)5
%26.84
26.83
26.84
26.81
26.85
26.81
26.82
26.82
26.63
28.85
26.81
26.88
25.63
25.78
JANUARY 1985
SNAPSHOT
400M
34
121 120

35
DYNAMIC HEIGHT (DYN CM) 0
JANUARY
1985
SNAPSHOT
M
255
24.2
28.1
24.1
25.8
2'
25.5
25.8
25.7
20
26.1
25.8
25.2
25.5
o 10
20 30 40 50
CURRENT SPEED (CM/S)
25.5
258
25.4
34
120
121

35
DYNAMIC HEIGHT (DYN CM)
0/200 M
34
121
120

35
DYNAMIC HEIGHT
34
121
120

34
DYNAMIC HEIGHT (DYN CM)
100/200 M
JANUARY 1985
SNAPSHOT
17i
17.8
I
1' p17.7
I
I
)8.O
19.0
IB.7
18.5
19.7
17.1
10 20 30 40 50
SPEED (CM/s)
19.
20.3
17.8
-
121 120

35
DYNAMIC HEIGHT
34
121 120

35
DYNAMIC HEIGHT (DYN CM)
34
121 120

35
DYNAMIC HEIGHT (DYN CM)
34
121 120

35
DYNAMIC HEIGHT (DYN CM)
200/500 M
34
121 120

35
34
121 120

35
TEMPERATURE (DEC
34
121 120

35
SALINITY (PPT)
JANUARY 1985
SNAPSHOT
5.4
33.54
33.52
33.54
33.55
33.54
33.55
33.55
33.55
33.55
33.55
33.54
33.55
33.55
33.56
33.50
33.54
I' 3155
33.52
33.52
33.52
33.51
33.51
33.54
——
33.55
.33.55
3354
33.54
33.51
33.50
34
121 120

35
34-
I I
121
77
96
82
/f
88<\
115
111
98
120

35
TEMP ERATURE
JANUARY 1985
SNAPSHOT
10.!;
10.98
10.67
10.92
10.97
10.83
10.82
10.94
10.89
10.97
10.93
10.87
10.95
10.91
10.86
10.97
10.85
10.70
10.65\
10.92
10.89
10.99
11.00
10.68
'I.
10.84
10.75
10.92
10.96
10.63
34
121 120

35
SALINITY (PPT)
34
121 120

DEPTH(M)
JANUARY 1985
SNAPSHOT
35
278
,/t298
233
34-
248
241
285
282
\267
283
245
121 120

35
TEMP ERATURE
34
121 120

35
SALINITY (PPT)
-
JANUARY 1985
SNAPSHOT
34.12
34.W
34.12
34,12
3411
34.07
34.10
34.12
34.13
34.11
34.12
34.13
34.08
34,13
34.13
34.11
34.12
\ 34.12
34.10
34.12
34.1
34.08
34,06
3&1 1
34.10
34
121 120

VERTICAL SECTIONS

n
TEMPERATURE (bEG C)
DISfANCE OFFSHORE (Xli)
38
37
36
35
34
TEMPERAtURE (DEC C)
DISFM4CE OFFSHORE (EM)
1985
36
35
34
38
37

100
0
TEMPERLTURE
87
I
84 — i3
(DEG C)
81
I
äANIJARY 1985
7978 77 75 74
I I I
38
37
36
300
400
35
I
80 80
DISTIINCE
40
(KM)
I
20 0
34
TEMPERLTURE (flEa C)
DISTANCE
IANUARY 1985
36
35
34
38
37
(Ku)

TEMPERATURE (BEG C) JANUARY 1985
36
35
38
37
34
DISTANCE OFFSHORE (EM)
1CC)
TEMPERATURE (BEG C)
152 150
I I I
—______
I
___—_-t1-
JANUARY 1985
146
200
300
400 —
I I
80
I I
60
DISTANCE
I
40
OFFSHORE (EM)
20
38
37
36
35
34
120

'V
TEMPERATURE (DEG C)
159 162
I
153
100 —
-
200 to
/ f
185
JANUARY 1985
167
300 —
—
— 7
400 —
502oo
I
I
I
I
I
80 80 40
DISTANCE OFFSHORE (1CM)
20
I
0
38
37
38
35
0
100 — iii
JANUARY 1985
102 95 78 69 55 49 36 34 21 17
I
3
38
37
200
300 -
400—
___•__>
NORTH
120 100 80 60
I
40
(IckQ
I
20
—
38
35
34

o
TEMPERATURE (DEG C)
105
81
-
100 —
46 39
31
JANUARY 1985
24 14
200 -
38
400
LJU1140
120 100
DISTANCE
80 60
I 'T
?
40
(1CM) i
20
C)
•
TEMPERATURE (DEG C)
100 —
-
108 iii
63 62 iii
42 28 27
I
JANUARY 1985
13
I
8
I
36
36
300 —
400
120 100
DISTANCE
80 60
•
40
(1CM)
20 0 sowrK
34
120

0
—
165
I
100
300
(nRa C)
148
I I
300 250 200 150
ALONGSff ORE (EM)
75
I
JANUARY 1985
17
38
37
36
35
50 0
34
TEMPERATURE (DEa C) 1985
38
37
36
35
34

___________________________________
TEMPERATURE (DEG C)
159 154
I
139
100 —
200
—
300
400
122
I\I
-
JANUARY 1985
87 10
0
I
I
350
I I
300
I I
250
I
200
I
150
DISTANc.E ALONGSEOEE (EM)
100
I
50
I
0
38
37
38

_____________
0
-
100 -
200 —
-
300
400
(PPT)
10 13 14
JANUARY 1985
16 1715
( l
0
34
$8
37
38
35
DISTANCE OFFSHORE
-p
SALINITY (PPT)
DISTANCE OFFSHORE
JANUARY 1985
38
37
36
SNAPSHOT
LINE 6
$5
++
34
123
I I
122 121 120

sA.uNrrY (PPT)
87 84 81
7978 77
JANUARY 1985
75 74
I I
100
—
300
400
—
I
80
I I
80
DLSTANCE
I
40
OFFShORE (KM)
I
20
38
3?
36
35
0
34
0
SALINiTY (PPT)
122
-
120
100 -
118
JANUARY 1985
116115
/
I
38
3?
36
400
I
I I
80
I
60
I
40
OFFSHORE (Ku)
I
20
35
34

SALINiTY (PPT) JANUARY 1985
80
DISTANCE OFFSHORE (K3&)
38
37
36
35
34
123 122 121 120
100 siLnJrry (PP'r)
154 152 150 148
JANUARY 1985
146
38
37
/
36
300
400
35
80 80
DISTANCE r
40
OFFSHORE
20 0
34

a
SALiNiTY (PPT)
159
-___
162
LW
-
—
—
34.0
183 165 167
1985 a' —
400 —
0
34
80 80 40
(KI{)
20
38
37
38
35
SALiNiTY (PPT) JANUARY 1985
102 95 76 69 56 49 36 34 21 17 3
I I I I I I
—
100 -
300 —
/
\
400 —
140 120
I I
100
I
80 60
I
1
40
DISTANCE ALONGSHORE (1CM)
I I
20 0
36
35
34
3-,
38

a
100
-
(Pi"r)
105 92 81 56 59 46 39
31
24 14
I I I I I I I I
—
— 34fr—___________
6
C..
1985
300
-
C
400—
-
120 100 80 80 40
ALONGS!IORE
(1cM)
20 0 souTh
38
37
38
35
34
-t
(PPT)
DISThNCE
1985
(1cM) SOUTh
38
35
38
37
34

* n
SALINITY (P1'?)
NORTH DISTANCE ALONGSE ORE (1CM)
JANUARY 1985
SOUTH
38
37
38
35
34
* n
SALINITY (P1'?)
NORtH DISTANCE ALONGSHORE (flQ
JANUARY 1985
SOUTH
36
35
34
38
37

e-.
n
WORTH cm)
AIAMJGSHORE (nL)
JANUARY 1985
SOUTH
38
35
38
37
34

___
SIGML—T
100
0
—
-
200
-
-
—
—
—
10
I
I
400 —
-
50 lao
13
I
I
25.8
14
I
16
I
I
r
1985
80
I
80
I
40
I
DISTANCE OFFSHORE (EM)
20 0
38
37
36
35
34 a
100
300
400
50900
JANUARY 1985
80
OFFSHORE (EM)
38
35
38
37
34
123 122 120

0
SIGMA—?
87 84 81
7978 77
JANUARY 1985
75 74
100
38
37
'-a
300 —
36
35
80 80 40
DISTANCE OFFSHORE (KIL)
20 U
34
SIGMA—'T JANUARY 1985
36
35
38
37
34
DISTANCE OFFSHORE (KM)

0
SIGMA—T
139
I a
100 —
800 —
400 —
137
I
135
JANUARY 1985
133 131
I I
I
26.0
I
I
38
37
36
80 80 40
DISTANCE OFFSHORE (KLt)
20
35
34 a
0
SIG.MA—T
154 152
I
100
—
150
26.2
148
I
I
JANUARY 1985
146
/
/
/
/ 38
37
36
400
35
I I I
80
I I
80
I
40
DISTANCE OFFSHORE
(at)
20 0
34
123 122 121 120

_______________
0
100 —
SIGMA-'I
159
— 25.6
_- 26
200
/
165
JANUARY 1985
157
300—
—
400t—
/
I
1
80 50 40
DISTANCE OFYSHOBE (Kkl)
20 0
37
38
35
34
-S
I-
SIGML—T JANTJARY 1985
36
35
34
38
37
DISTAiCE ALONGSHORE (IGL)
120

100 —
—
SIGWL—T
-
105 92 liii
81
86 59
I
46
I
39 31
III JANUARY 1985
14
I
6
300
-
400
-
50I
40 120 100 80 60 40
DISTANCE ALONGSHORE (1CM)
20
BOUTE
0
37
38
38
35
34
0
100'
200
—
—
200 —
JANUARY 1985
108 89 84 63 62 43 42 28 27 13 8
38
37
36
35
400
§OI 40
I
120 100
DISTANCE
60 80 40
(1CM)
20
SOUTE
0
34
120
120

___________________
SEGMA-T
NOBTE ALONGSEIORE (xli)
JANUA.RY 1985
38
37
36
35
34
100
163
—
150
254
135
I
I
I
(
118 ii
81
MNUARY 1985
14
I
I-
300
400
-
\
I
I
250 300 250
I
200
I I
150
I
100
I
50
I
0
120

________________
I
159 154 139 122 87
1985
10
38
26.2
28$
—28.8—
50
350 300 250
DJSTANcE
200
I I
150
I
(L&)
I
100 50 0

CURRENT (CM/S) JA]JUARY 1985
38
37
35
35
34
DISTANCE OFFSHORE (EM)
0
CURRENT (CM/S)
43 46 46 52
1985
100
200
ID
/ s—
300
400
I cr—
I
80
I I
60
I
/
I
40
I
DISTANCE OFFSHORE (IOL)
I
20
I
0
38
37
38
35
34

0
100
400
CURRENT (CM/S) JANUARY 1985
35
34
38
37
38
50
DIStANCE OFFSHORE (Dl)
CURRENT (CM/S) JANUARY 1985
38
37
36
35
34
DISTANCE OFFSHORE (1CM)
120

100
400
CURRENT (CM/S) JAIJUARY 1985
38
37
38
35
60 40
DISTANCE OFFSHORE (KM)
123 122 121 120
100
200
400
CURRENT (CM/s)
DISTANCE OFFSHORE
JANUARY 1985
38
37
38
35
34

100
300
400
CURRENT (CM/S) JANUARY 1985
38
35
38
37
34
DISTANCE OFFSHORE (1CM)
100
300
400
CURRENT (CM/S) JANUARY 1985
38
37
38
35
DISTANCE ALC}NGSHORE (1CM) noun
34
120

400
38
.37
35
35
DISTANCE ALONGSHORE (1CM) 8OUTZ
34
123 122 121 120
100
400
CURRENT (cM/S) JANUARY 1985
36
35
38
37
34
DISTANCE ALONGSHORE (1CM)

100
S
300
400
CURRENT (CM/S)
AL0NGSHORE (EM)
JANUARY 1985
38
37
36
35
123
S
300
400
0
CURRENT (CM/S)
100
502oo xorz
JA.NTJA.RY 1985
38
35
34
38
37

300
400
0
CURRENT (cM/s)
250 200 150
DISTAJC ALONGSHORE (n)
JANUARY 1985
36
35
38
37
34