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AD-fA132 083 DATA VALIDATION AND SUMMARY FOR THE NRL REMOTE SENSING 1/2 EXPERIMENT PHELPS..(U) NAVAL RESEARCH LAB WASHINGTON DC UNC47 SIFED J A KAISER 02 SEP 83 NRL-MR-5165 FG88 N

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Page 1: DATA VALIDATION AND SUMMARY FOR THE NRL REMOTE … · For several years, Synthetic Aperture Radar (SAR) images of the sea surface revealed planar signatures which were remarkably

AD-fA132 083 DATA VALIDATION AND SUMMARY FOR THE NRL REMOTE SENSING 1/2EXPERIMENT PHELPS..(U) NAVAL RESEARCH LAB WASHINGTON DC

UNC47 SIFED J A KAISER 02 SEP 83 NRL-MR-5165 FG88 N

Page 2: DATA VALIDATION AND SUMMARY FOR THE NRL REMOTE … · For several years, Synthetic Aperture Radar (SAR) images of the sea surface revealed planar signatures which were remarkably

1.8.

IIIJIL2

MICRCOP RESLUTON TST HAR

NATINALBLJRAU F SINDADS 163

Page 3: DATA VALIDATION AND SUMMARY FOR THE NRL REMOTE … · For several years, Synthetic Aperture Radar (SAR) images of the sea surface revealed planar signatures which were remarkably

NRL Memorandum Report 5165

Data Validation and Summary for theNRL Remote Sensing Experiment:

Phelps Bank, July, 1982

Part I: Hydrography

J. A. C. KAISER

Ocean Dynamics BranchMarine Technology Division

September 2, 1983

DTIC? S ELECTEDlo ,.,EP 6 I8

C)

LUj.-_LL. NAVAL RESEARCH LABORATORY

Washington, D.C.

CApproved for public release. distribution unlimited.

83 09 oi 06C

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SECiURITY L&SsIFrCA'CN OF .. $ PAGE '4Whon Oat. Ent. ra;

REPORT DOCUMENTATION PAGE READ INSTRUCTIONSREPORT__ DOCUMENTATION _PAGE_ BEFORE COMPLETING FORM

I REPORT NUMBER 2. GOVT ACCESSION NO. 3. RECIPIENT'S CATALOG NUMBER

NRL Memorandum Report 5165 _

4. TITLE 'wd S&brWrIe, S. TYPE OF REPORT a PERIOD COVERED

DATA VALIDATION AND SU'MARY FOR THE NRL Interim report on a continuingREMOTE SENSLNG EXPERIMENT: PHELPS BANK, JULY, 1982 NRL problem.Part I: Hydrography , PERFORMING ORG. REPORT NUM9ER.

7 AUTNOR() B. CONTRACT OR GRANT NUMBER(;)

J. A. C. Kaiser

S. PERFORMING ORGANIZA':CN NAME AND ADDRESS 0. PROGRAM ELEMENT. PROJECT, TASK

AREA & WORK UNIT NUMBERS

Naval Research Laboratory 61153N; RR01310441;Washington, DC 20375 58-1557-A3

11. CONT*OLL.NG OFFICE NAME AND ADDRESS 12. REPORT OAT!

September 2, 1983I3. NUMBER OF PAGES

14914. MONITORING AGENCY NAME A AODRESSOI" different from Controlllng Office) IS. SECURITY CLASS, 'of thie report)

UNCLASSIFIEDISO. OECLASSIFICATtON/DOWNGRADING

SCNEDULE

16. DISTRIBUTION STATEMENT tot this Report)

Approved for public release; distribution unlimited.

17. DISTRIBUTION STATEMENT fot the abetract engered In Black 20, It different f/em Report)

I$. SUPPLEMENTARY NOTES

IS. KEY WORDS (Coatlnu e on rever* aide If nec..ery and Identify by block number)

Nantucket Shoals Continental shelfHydrography CTD profilesNRL Remote Sensing Experiment Coastal processesPhelps Bank

20. AbSTRACT (Continue an reverse aide It noce.toy m. Identify by block nufibe.)

) During the NRL Remote Sensing Experiment in the Phelps Bank region (40? 50N, 690-20'W) hydro- 4

graphic data were obtained with a Nell-Brown CTD (conductivity-temperature-depth) profiler and withXBT (expendable bathythermograph) probes. The data is summarized, profiled and contoured. Thecontoured data is corrected for tidal advection and for the temporal change during the survey. The T, S(temperature, salinity) relation for the area is highly structured indicating the effects of mixing of shelfwater and deep upwelling water in the presence of surface mixed layers having origins within and .

without the area

DD I o. , 1473 f'TION OF' I NOV 65 IS OBSOLETE :94S/)f 0102-014- 6601

SECURITY CLASSIFICATION Of THIS PAGE (WDec- Dee Entered)

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CONTENTS

I. INTRODUCTION 1

II. INSTRUMENTATION 3

A. CTD Instrument 3B. XBT Instrument 4

C. Navigation 5

III. DATABASE 6

IV. DATA PROCESSING 11

A. CTD Data 11

B. XBT Data 12

C. Tidal Adjustment of Data 12

D. Temporal Adjustment of Data 15

E. Summary of Corrections 15

V. hYDROGRAPHIC DATA 17

ACKNOWLEDGMENTS 45

REFERENCES 46

APPENDICES

A. Plots of CTD Casts 47

B. Tabulations of CTD Casts 89

C. Plots of XBT Drops 129

DTIC ,. .

SELECTE

---

SEP16 983 / .

iii ... .

vl .. ... .

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FIGI RES

3.1 Map of CTD casts and XBT drops 7

4.1 Reconstructed tidal ellipses West and East of Phelps Bank 13

4.2 Adjustments to CTD lowering locations due to tidal motions 14

4.3 Temporal trend in the CTD data 16

5.1 Temperature map, Om 18

5.2 Temperature map, 10m 19

5.3 Temperature map, 20m 20

5.4 Temperature map, 30m 21

5.5 Temperature map, 40m 22

5.6 Temperature map, 60m 23

5.7 Temperature map, bottom 24 05.8 Salinity map, Gm 25

5.9 Salinity map, 10m 26

5.10 Salinity map, 20m 27

5.11 Salinity map, 30m 28

5.12 Salinity map, 40m 29

5.13 Salinity map, 60m 30

5.14 Salinity map, bottom 31

5.15 Sigma-T map, Gm 32

5.16 Sigma-T map, 10m 33

5.17 Sigma-T map, 20m 34

5.18 Sigma-T map, 30m 35

5.19 Sigma-T map, 40m 365.20 Sigma-T map, 60m 375.21 Sigma-T map, bottom 385.22 Composite T-S diagram and characteristics of distinct water masses 39-405.23 Map of surface water mass types 415.24 Map of deep water mass types 42

5.25 Composite map of Temperature profiles 43

5.26 Composite map of Salinity profiles 44

A.1-A.41 Lowering profiles: Temperature, Salinity, Sigma-T, and

T-S diagrams 48-88

C.l-C.29 XBT Temperature Profiles 130-144

TABLES

2.1 CTD System Characteristics 5

3.1 CTD Casts 8-9

3.2 XBT Drops 10

4.1 Corrections to Data 16

B.1-B.41 CTD Data Tabulated in 1 Meter Bins 89-128

iv

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DATA VALIDATION AND SUM!MARY FOR THENRL REMOTE SENSING EXPERIMENT: 0

PHELPS BANK, JULY, 1982Part I: Hydrography

I. INTRODUCTION

For several years, Synthetic Aperture Radar (SAR) images of the sea

surface revealed planar signatures which were remarkably similar to the

bathymetric contours below the water in depths less than about 30m. Such

sea-surface bathymetric signatures were also observed by side-looking air-

borne radar (SLAR). To address the scientific questions raised by these

observations, a multi-institutional program (the .irborne Surveillance

Phenomenology Program; ASPP) was established at the Naval Research Labor-

atory, Washington, DC (The original plans are described in Valenzuela and

Chen, 1983.). In July, 1982 as the initial field effort of ASPP, a pilot

experiment was conducted southeast of Nantucket Island centered around

Asia Rip (40*50'N, 60*20'W). The experiment was to establish techniques

for a comprehensive experiment in 1984, to learn about the oceanographic

and meteorological environs of Asia Rip, and to obtain a data set for pre-

liminary analysis.

The Nantucket Shoals area was chosen for the experiment because SAR

imagery obtained in this area by SEASAT in 1978 (Beal, et al, 1981; p.22)

showed a wealth of bathymetric signatures.

During the pilot experiment, meteorological, radar and wave buoy data

were gathered. A hydrographic survey of the area was made with a Neil-

Brown conductivity-temperature-depth (CTD) profiler as time permitted.

Forty-one casts were obtained supplemented by 29 T-11 expendable bathy-

thermograph (XBT) probe drops. The data was confined to the tessera

Manuscript approved July 21, 1983.

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40030 ' to 41l!0'N and 68°55 ' to 69°45'W. The data was obtained in two

segments: 11 to 14 and 17 to 21 July, 1982. This report summarizes the

hydrographic situation in the operational area during the experiment

based primarily on the CTD data. The data has been corrected for temporal

changes during the survey period and adjusted for tidal displacements. In

appendices, the CTD and XBT casts are plotted and average CTD data in 1

meter bins are tabulated.

=•1"'-4

2

iS

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II. INSTRLMENTATION

The hydrographic situation at Nantucket Shoals was primarily derived

from casts made with a conductivity-temperature-depth (CTD) profiling

instrument. Expendable bathythermograph (XBT) probes were also dropped to

obtain additional temperature profiles.

A. CTD Instrument

The CTD was manufactured by Neil Brown Instrument Systems and

is very similar to their Mark III instrument. The instrument measures

each channel of data at a 31 Hertz rate. The electrical conductivity of

the water is determined by a four-electrode cell 3 cm long. The tempera-

ture is measured by both a platinum resistance element (time constant

•5sec) and a thermistor with a time constant of about .05sec. The analog

signal from each temperature sensor is combined so that the platinum

element provides long term stability and accuracy and the thermistor pro-

vides fast response. The pressure is read by a strain gauge sensor. The

conductivity, temperature and pressure signals are digitized by three

separate 16-bit-plus-sign digitizers and mixed into a digital data stream.

The digital data is then transmitted up the hydrowire in frequency-shifted-

key (FSK) format using 5 and 10 Hz frequencies. This FSK data stream is

converted to TTY-compatible digital data to provide a serial data stream.

It is also unmixed and converted to TTY-compatible format to provide a

parallel digital data stream and it is digital-to-analog converted to pro-

vide parallel analog signals. (Brown and Morrison, 1978, provide details

of the CTD instrument).

The serial digital data is logged on an HP-1000 computer

through the general purpose interface bus onto 800 bpi 9-track tape. The

3

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serial FSK data is also recorded on a high quality audio recorder

(7.5 ips) to provide backup recording. The parallel analog signals are

plotted on a 2-channel X-Y-Y' recorder to provide real time monitoring.

The inaccuracies, resolution, and total noise of the CTD

channels are in Table 2.1. The inaccuracies are based on the calibration

history of the instrument. The system noise is the white noise floor of

each channel and the resolution is the digital least count. An evaluation

of the CTD characteristi-s will be found in Kaiser and Clamons, 1983. The

instrument used in this experiment is referred to as CTD-II in that report.

B. KBT Instrument

The XBT probes used for this experiment were standard

Sippican Corporation (Marion, Mass.) type T-ll fine structure XBT's.

These probes have a nominal accuracy and resolution of 0.10 C. The probes

free fall in the water, and knowing the fall rate equation, their depth-

time dependence can be determined. The average fall rate for T-11 probes

is 1.75 m/sec. Their nominal depth accuracy is 2%.

Normally the XBT data are recorded on an HP-1O00 computer

using a digital multimeter. Some were, but computer malfunction required

the post cruise manual digitization of the XBT charts on a digitizing

table. This does not significantly change the accuracy and resolution of

the final digital XBT data.

4

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Table 2.1. CTD System Characteristics

Channel Resolution Inaccuracy System Noise

Temperature, °C .0005 .005 .0002

Conductivity, mmho/cm .001 .005 .0004

Pressure, dbar .025 1.6(.2)* .02

*This is over the total range of 1600 dbar. With zero correction, over

the 0-100 dbar range the inaccuracy is .2 dbar.

C. Navigation

The primary navigation aid was two Northstar 7000 Loran-C

systems. These have a nominal accuracy of 0.1 km in the Nantucket Shoals

area due to the excellent Loran coverage there. The time delays and

calculated latitude and longitude information from the Loran-C sets were

logged on an HP-1000 computer and updated every minute. The complete time

series of navigation for this experiment will be found in Kaiser and

Munch, 1983. The position for each cast was determined at the time the

CTD or XBT entered the water. In most cases the CTD casts were less than

600 sec in duration and the XBT drops required less than 50 sec.

5

IL

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III. DATABASE

The data base used here consists of 41 CTD casts and 29 XBT profiles.

The geographical distribution of these are shown in Fig. 3.1 with the

lowering or drop number. The CTD and XBT logs are in Tables 3.1 and 3.2

respectively.

The CTD cast depths and water depths are in Table 3.1. For most of

the casts we tried to keep the CTD about 5 m above the bottom, but this

varies; we did not have a bottom finder on the CTD. The actual bottom

depths were determined from a Raytheon precision depth recorder.

CTD lowerings 7-13 and 27-34 were recorded on audio tape but inad-

vertently the tapes were erased. Since the casts were also plotted on an

analog recorder, the analog traces were hand digitized on a digitizing

table.

XBT drops 14-23 were to determine the existance of a weak east-west

front. XBT drops 24-32 were to resurvey the same front about 1/2 tidal

cycle later.

To convert from Julian day to calendar day, the following corres-

pondence applies: JD 192 is July 11; JD 198 is July 17; and JD 202 is

July 21.

0

0

0

6.

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S 0

41000' 0 03 a 39 acG

_0 0 0 0_* S 3 0-0 0

3i .0 -0 0 0 0 0

2- 2 3 33 1

.0 0

70

0 0 0 0 0 019 2d 34 16 i 5 35 12 11

0 0 0 0 020 23 22 14 13

040030 '/ II I 3 I II

69030 , 69000,

Fig. 3.1. Location of CTD casts (0) and .XBT drops (0) with their

identifiers. The 20 m isobath is included. .4

1

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TABLE 3.1. CTD CASTS

DAY-TIE;!LOWILATITUDE LONGITUDE!CAST WATER HA.ND

GMT T N W DEPTH DEPTH DIGITIZED

I M

192-2329 1 40049.22 ' 169017.77 ' 51 55193-0021 2 40049.84: 69013.31 ' 55 61193-0104 3 40049.85? 69007.09 ' 66 65

193-0143 4 40049.81? 69002.19 ' 80 84

193-0250 5 40054.88 ' 690 1.15' 79 80

193-0314 6 40055.01' 690 8.00? 68 74

193-0348 7* 40054.96 ' 69014.01? 62 65 X

193-2212 8 40044.56 ' 69013.32 ' 51 61 x193-2257 9 40044.71 ' 690 5.17' 69 71 x

193-2339110 40044.90 ' 68058.15? 62 72 X

194-0017 11 40040.23 ' 68059.52 ' 62 66 X194-0101 12 40039.84 ' 69006.64 ' 63 78 X

194-0139 13 40035.16 ' 69006.79 ' 77 80 x194-0222 14 40034.96 ' 69013.95 ' 56 60194-0303 15 40039.66 ' 69013.93 ' 54 58

194-0343 16 40040.06' 69019.90' 49 55194-2218 17 40050.04:169035.04? 35 39

194-2256 18 40045.24? 69035.86 ' 40 45

194-2333 19 40040.25 69036.09 ' 45 50

195-0011 20 40035.16 ' 69036.16 ' 59 62

195-0112 21 40032.04? 69027.20 ' 55 59195-0204 22 40034.79? 69020.06 ' 55 60

195-0246 23 40034.85? 69026.53 ' 49 54195-0330 24 40039.58? 69026.71 ' 50 55

198-0739 25 40054.29? 69042.95 ' 28 32198-0815 26 40050.26? 69043.05 ' 35 38198-0853 27 40045.13 69042.95 ' 39 42 X

198-1000 28 40045.06? 69027.35 ' 48 50 X198-1031 29 40049.87? 69027.26 ' 47 50 X

198-1101 30 40054.87? 69027.27 ' 22 26 x

198-1156 31 40055.12 ' 69035.73 ' 38 40 x

198-1228 32 40059.88 ' 69035.77 ' 38 43 X

198-1302 33 41004.92 ' 69035.96 ' 21 31 X198-1957 34 40039.99 ' 69027.12 ' 53 55 x198-2157 35 40040.44 ' 69012.92' 62 66

8

II

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7 1

TABLE 3. 1. CTD CASTS (Cant)

DAY-TIME ILOWILATITUDE LONGITUDE CAST WATER HAN\DGMT !# N W DEPTH DEPTH DIGITIZED

M

200-1410136 40050.30? 69007.16?1 69 73* 200-2235137 40045.42? 69-36.15'1 36 40

200-2351 38 40053.10? 69020.96' 36 45201-1630 39 40059.29' 69013.49' 31 70201-1645 40 40059.14? 69013.19? 67 69

41 41000.15' 69019.58' 47 49

*Lowering 7 was machine digitized to 44 m and hand digitized to 61 m

9p

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TABLE 3.2. XBT DROPS

DAY-TIMEIDROP)LATITUDE LONGITUDE WATER 0

GMT NO N W DEPTHM

191-0946 7 40048.50 ' 69026.81 ' -191-1022 8 40047.00 ' 69029.00 ' -

192-1215 9 40046.96 ' 69029.04 ' - Bad192-1845 10 40049.96 ' 69018.94? -

193-1935 11 40052.00 ' 69016.79 ' 53

194-1820 12 40049.92 ' 69034.64 ' 35 Questionable

195-1515 13 40047.42 ' 69021.73? 33

198-1730 14 40053.71 ' 69030.91 ' 37 Front transect No. 1

198-1745 15 40052.5 ' 69030.60 ' 37 Front transect No. 1

198-1800 17 40050.5 ' 69030.19t 37 Front transect No. 1

198-1815! 18 40048.1 69030.02: 4L Front transect No. 1

198-1830! 19 40'46.5 ? 69029.95? 44 Front transect No. 1

198-18451 20 40044.9 69*29.93 ' 44 Front transect No. I

198-19001 21 40042.8 69030.001 48 Front transect No. 1

198-19151 22 40041.0 ' 69029.96 ' 48 Front transect No. I

198-1930 23 40040.0 1 69029.92 ' 48 Front transect No. 1

198-2355 24 40 39.7 ' 69029.8 ' 43 Front transect No. 2

199-0010 25 40042.4 ? 69029.8 1 48 Front transect No. 2

199-0025 26 40043.3 69029.8 44 Front transect No. 2

199-0035 27 40 044.9 ' 69029.8 ' 46 Front transect No. 2

199-0050 28 40046.6 ' 69029.6 45 Front transect No. 2

199-0105 29 40048.3 ' 69029.4 43 Front transect No. 2

199-0120 30 40050.14 ' 69029.4 ' 45 Front transect No. 2

199-0135 31 40051.9 ' 69029.4 ' 38 Front transect No. 2

199-0145 32 40053.0 ' 69029.5 I 34 Front transect No. 2

199-2025 33 40050.7 ' 69007.6 ' 70

200-0305 34 40057.1 ' 690 6.6 ' 75200-1200 35 4050.5 ' 69011.2 1 70

202-1800 36 40049.1 ' 69033.7 ' 40

10

101

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LL

IV. DATA PROCESSING

A. CTD Data

'A ~IIThe CTD data was transcribed from audio tape to 9-track 800 bpi

tape by an HP-1O00 computer. 31 data scans/second were logged. These

data were digitally processed before plotting or other processing. The

data was scanned and, starting at a minimum pressure (0 dbar), all data

scans were discarded if (Pn+l - Pn) <0, where n is the data scan number

and p the pressure. Then the data was wild point edited. All data scans

in which Pn+l - Pn > Kl were discarded. Then all data points which had

I(Tn+l - Tn)/(Pn+l - Pn) I >A2

(Cn+l - Cn)/(Pn+l - Pn)! >K3

were discarded. The K I - K3 are chosen for a particular data set. They

represent, respectively, the maximum allowable time derivative of

pressure, the pressure derivative of temperature, and the pressure deriv-

ative o- -onductivity. For this data we chose K1 = .2 dbar/scan, K 2

3.*C/dbar and K3 - 2. mmho/cm-dbar. These values are small enough so

that data at the bottom of a mixed layer will not be discarded.

Density and salinity were then calculated from the edited data.

No attempt was made to smooth or lag the temperature vis-a-vis the con-

conductivity to prevent "spiking". The density and salinity algorithms

are documented in Rosenblum (1980). The algorithms are based on those of

the Woods Hole Oceanographic Institution.

0

9I

_O.1

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:4*0!

B. XBT Data

The XBT data wer, all hand digitized from the standard XBT charts

and converted to temperature and depth using the standard Sippican con-

versions. The data was digitized by measuring the coordinates of signifi-

cant points. These are points which can be connected linearly and in so

doing the reconstructed profile is within .10C from the original curve.

The digitized data is then reconstructed by linearly interpolating between

successive significant points.

C. Tidal Adjustment of Data

The hydrographic data were obtained throughout the experimental

period and at random phases of the tidal cycle, which is semi-diurnal in

the area.

Actual tidal ellipses were determined with drifters at 6 and 19 m

west and east of Phelps Bank (69*20'W) (see Greenewalt and Gordon, 1982).-4

Each tidal ellipse, determined from their measurements and referenced to

the maximum flood current at Pollack Rip is plotted in Fig. 4.1. The

maximum excursion due to the tides was 6.5 n.mi, while the nominal grid

point spacing in the hydrographic survey was 5 n.mi. To accurately plot

maps, the lowering locations were all adjusted to a "reference" location

in the tidal cycle. It was decided to use the center of the ellipse even

though the tidal motion would never bring the water to that point; any

point on the ellipse represents an extreme location. The adjustment to

each of the 41 lowerings is shown in Fig. 4.2. The points being geo-

graphic locations and the circles the adjusted locations.

These tidal corrections were only made to the upper 30 m of the

water column. Deeper water most certainly moves in different trajectories

12

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4-

7 ~

4

9

3

N 1

01mm01

00

WEST EAST

Fig. 4.1. Tidal ellipses west and east of Phelps Bank constructed from

the data of Greenewalt and Gordon (1982). The points labelled

"0" refer to the maximum flood current at Pollock Rip.

13

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:43

00

II

3-41o00'_

17/7 29

L~ 273 60

/5 23

18 24V?34 76 f1

335

11

20 21Q.,

40030'F, I, , ,, ,,, I I, I I, I ,,,,I I I I ,I ,I , I ,69030 ' 69o00 ,

Fig. 4.2. Adjustment to the location of CTD lowerings due to tidal

motion. The circle is the adjusted location; the point the

geographic location.

14

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due to bathymetric influences. Bottom water probably is almost completely

uncoupled from the upper tidal motion.

D. Temporal Adjustment of Data:

The hydrographic survey was carried out over a time span of 9

days. A few lowerings were reoccupied during the period and they indicate

a definite temporal trend in the deep (below 30 m) water. Above 30 m no

trend could be discerned. The trends were obtained by comparing lowerings

3 to 36, 15 to 35, and 24 to 34. These trends are plotted in Fig. 4.3.

The temperature trend is most definite; salinity has a weaker trend and

sigma-T no trend. The temperature and salinity corrections are -.097*C/day

and -.04*/oo/day with no correction is made at 198!0600Z. These temporal

corrections are only applied at or below 30 m depth.

E. Summary of Corrections:

Both tidal and temporal corrections have been made to the data.

The corrections are summarized in Table 4.1.

15

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r.. * - rLow No.

p~El allOgmcT 1 120 "

p.) .- - I el q o o

192 194 196 198 200 202

Time, JD

Fig. 4.3. Temporal trends in the salinity, sigma-T and temperature based

on reoccupied stations.

TABLE 4.1. CORRECTIONS TO DATA

(Ti - Tidal, Te - Temporal)

DEPTH VARIABLE

Temperature Salinity Sigma-T

,m Ti Ti Tj SI0'm Ti Tj Ti20,m Tj Tj Tj30,m TiTe Ti,Te Ti40,m Te Te --

60,m Te TeBottom Te Te .,

16

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V. HYDROGRAPHIC DATA

The hydrographic fields, corrected as described in IV, is mapped at 0,

10, 20, 30, 40, 60 m depths and at the bottom. Temperature, salinity and

sigma-T maps have been constructed at each depth (Figs. 5.1 through 5.21).

The location of Phelps Bank and Asia Rip are shown as the broken line near

69*20'W. The appropriate isobath is plotted on the 10 m to 60 m charts.

This isobath was taken from the Department of Commerce 1:400,000, Georges

Bank and Nantucket Shoals chart, July, 1980. The bottom data was from the

deepest portion of the lowering, usually within 5 m of the bottom (see

Table 3.1). A T-S diagram for each cast was plotted (Appendix A) and then

all were combined, Fig. 5.22a. The composite T-S diagram suggests six

distinct water masses can be identified. These are delineated in

Fig. 5.22b. Note that types A, E and F represent surface water. Types

B, C, and D are deep water with type C probably resulting from mixing of

types B and D. The locations of these watermass types are shown in

Fig. 5.23 and Fig. 5.24. Type C occurs over the shallower water in and

around Phelps Bank, a result of tidal mixing across the bank.

Selected temperature profiles from the area are geographically

positioned in Fig. 5.25. The regions of surface warming are evident, but

mixing between types B, C, D are only evident on the salinity profiles,

which are on Fig. 5.26.

17

S

Page 24: DATA VALIDATION AND SUMMARY FOR THE NRL REMOTE … · For several years, Synthetic Aperture Radar (SAR) images of the sea surface revealed planar signatures which were remarkably

II I i I I I I~j III I I11111 I I I it 11 11 11 I ii ji I I

13 12

41 000'13

- 16I

14 1156S )

113

181

Page 25: DATA VALIDATION AND SUMMARY FOR THE NRL REMOTE … · For several years, Synthetic Aperture Radar (SAR) images of the sea surface revealed planar signatures which were remarkably

13~

122

121

2 Ki3*00

12 D*\ 0 ) p

12 1 3

Fig. 5.2. Temperature field at 10 mtidally adjusted.6 0 '

19

Page 26: DATA VALIDATION AND SUMMARY FOR THE NRL REMOTE … · For several years, Synthetic Aperture Radar (SAR) images of the sea surface revealed planar signatures which were remarkably

41 000-- /

/ -a

40030' r

- . ( 122% .. ,..

);,.

•/ 12311

12 13 14

69030 , 69000'Fig. 5.3. Temperature field at 20 m tidally adjusted.

-4

20

Page 27: DATA VALIDATION AND SUMMARY FOR THE NRL REMOTE … · For several years, Synthetic Aperture Radar (SAR) images of the sea surface revealed planar signatures which were remarkably

JI

11.'N

/ , 7/ K 7'

/ / 12

40030

6930 6900

Fig 5..Tmeauefeda/ 0mtmoal n ial dutd

/ /2/

LO 0

Page 28: DATA VALIDATION AND SUMMARY FOR THE NRL REMOTE … · For several years, Synthetic Aperture Radar (SAR) images of the sea surface revealed planar signatures which were remarkably

'41, T I I I I I 10

/ 7 -

41/ / 000'77/

4000't1 1 f t6930 69000

Fi. .. epeaur iedat40mtepral ajstd

7-20

Page 29: DATA VALIDATION AND SUMMARY FOR THE NRL REMOTE … · For several years, Synthetic Aperture Radar (SAR) images of the sea surface revealed planar signatures which were remarkably

A0

L

7Z/6

/ 67' 03' 697700'

Fig.7 /.6 /eprtr /il a- 60Mtepral ajstd

7<1A,

7,7 *77 /3

Page 30: DATA VALIDATION AND SUMMARY FOR THE NRL REMOTE … · For several years, Synthetic Aperture Radar (SAR) images of the sea surface revealed planar signatures which were remarkably

12..5

-112

N, 12~ 1.5 4

1 0

124

Page 31: DATA VALIDATION AND SUMMARY FOR THE NRL REMOTE … · For several years, Synthetic Aperture Radar (SAR) images of the sea surface revealed planar signatures which were remarkably

/ 32

* ~41 000'

N (*)3'.. S

/2. 33.

333

69030' 69000'Fig. 5.8. Salinity field at 0 M tidally adjusted.

25

Page 32: DATA VALIDATION AND SUMMARY FOR THE NRL REMOTE … · For several years, Synthetic Aperture Radar (SAR) images of the sea surface revealed planar signatures which were remarkably

32

41 000' 325 33

32.5

32

33 33

32. 533AL

69030' 6900Fig. 5.9. Salinity field at 10 m tidally adjusted.

26 '

Page 33: DATA VALIDATION AND SUMMARY FOR THE NRL REMOTE … · For several years, Synthetic Aperture Radar (SAR) images of the sea surface revealed planar signatures which were remarkably

00

3232

/ ~ ~33.5

4000'vy

7 /7

Page 34: DATA VALIDATION AND SUMMARY FOR THE NRL REMOTE … · For several years, Synthetic Aperture Radar (SAR) images of the sea surface revealed planar signatures which were remarkably

oil

p 3.

7/ 2.333.

334

033'

69030' 69000'Fig. 5.11. Salinity field at 30 mn tidally and temporally adjusted.

28

Page 35: DATA VALIDATION AND SUMMARY FOR THE NRL REMOTE … · For several years, Synthetic Aperture Radar (SAR) images of the sea surface revealed planar signatures which were remarkably

-- - - - -- -

41000' 3

33.5-

.00 I I

4 31329

110

Page 36: DATA VALIDATION AND SUMMARY FOR THE NRL REMOTE … · For several years, Synthetic Aperture Radar (SAR) images of the sea surface revealed planar signatures which were remarkably

41

41 00' 0,

X, ~//

'/7~~~ 3,,/t

r / y Y~ <// 1

40030'7 //

/930 69/000'

Fig. ~ 5.13 Saint fil /t6 epoal dutd

4100/ 4>~ ~'4' ~ / >;

Page 37: DATA VALIDATION AND SUMMARY FOR THE NRL REMOTE … · For several years, Synthetic Aperture Radar (SAR) images of the sea surface revealed planar signatures which were remarkably

70

32..

6930 41000'Fig.5.1. Sliniy feldat he btto teporaly djuted

I3

Page 38: DATA VALIDATION AND SUMMARY FOR THE NRL REMOTE … · For several years, Synthetic Aperture Radar (SAR) images of the sea surface revealed planar signatures which were remarkably

0

24 21.5

41 000' /2

/ 23

23.51

24 0 0-2

2 1 11 4. 5 ~.

69030' 69000'Fig 5.5. igm-T field at 0 m. .

32

9

Page 39: DATA VALIDATION AND SUMMARY FOR THE NRL REMOTE … · For several years, Synthetic Aperture Radar (SAR) images of the sea surface revealed planar signatures which were remarkably

0 !0

24.5.5-

255400J , 69 305900

Fig. .16.SigmaT fild a24.5m

33*

Page 40: DATA VALIDATION AND SUMMARY FOR THE NRL REMOTE … · For several years, Synthetic Aperture Radar (SAR) images of the sea surface revealed planar signatures which were remarkably

41 000

-25

41030' -- 2.-./ :

-/ //

/// : ,5/- -

<100 / / -

- // --

34

24.5 , --

7-25 /(-40o30 I II I III

O3'69030 , 69000 , -0

Fig. 5.17. Sigma-T field at 20 m. 1

:9;

34]

Page 41: DATA VALIDATION AND SUMMARY FOR THE NRL REMOTE … · For several years, Synthetic Aperture Radar (SAR) images of the sea surface revealed planar signatures which were remarkably

/7 7

/ /t 5

/ / / 7 -- 255.

00

000

1000

.4-. 2626

69030' 69000'Fig. 5.18. Sigma-T field at 30 m.

35

-

Page 42: DATA VALIDATION AND SUMMARY FOR THE NRL REMOTE … · For several years, Synthetic Aperture Radar (SAR) images of the sea surface revealed planar signatures which were remarkably

*2 5

41 000'

25 /

410O' F,//*6903' 6000

Fi. .1. SimaT ildat4/m

36I

Page 43: DATA VALIDATION AND SUMMARY FOR THE NRL REMOTE … · For several years, Synthetic Aperture Radar (SAR) images of the sea surface revealed planar signatures which were remarkably

p.A 1 1 1 1 1 1 1 1 1

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Fig 5.0 Sim- f ,el /t 60/ /m/.

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Page 44: DATA VALIDATION AND SUMMARY FOR THE NRL REMOTE … · For several years, Synthetic Aperture Radar (SAR) images of the sea surface revealed planar signatures which were remarkably

0

41 000'/

/ d

2 5;

40*30'69030' 69000'

Fig. 5.21. Sigma-T field at bottom.

38

Page 45: DATA VALIDATION AND SUMMARY FOR THE NRL REMOTE … · For several years, Synthetic Aperture Radar (SAR) images of the sea surface revealed planar signatures which were remarkably

35 1318

STA 711 LOW 1

14

-6 1910

LoC-) 3

0 4'

'9 ~ -12

<9

Icc,

- IFig 5.22 (a) Co ps8 - i g a

04 172020 24

339

313

Page 46: DATA VALIDATION AND SUMMARY FOR THE NRL REMOTE … · For several years, Synthetic Aperture Radar (SAR) images of the sea surface revealed planar signatures which were remarkably

E

U

18STA 7

11 LOW 1

A F14

I

CO /00

19

0.0w =I- ( .- 12 9

La

37La2 5 23 8"22.

c " -1725

32.00 3. 33.00 4 3.00 2

B SALInT,°o

C DFig. 5.22 (b) Delineation of 6 water types encountered

in the Nantucket Shoals area.

40

1.0 3.0 3. 30 0 40 45 50 55

Page 47: DATA VALIDATION AND SUMMARY FOR THE NRL REMOTE … · For several years, Synthetic Aperture Radar (SAR) images of the sea surface revealed planar signatures which were remarkably

II

BOB

41000'13CD D

B m B B.C*BIC

B

B B 'B- .BC ME

B Jr D

B OB (DJ

-AB-

B*CD

COD

- kc D

+" D

40030'69030 ' 69000'

Fig. 5.23. Location of water Lypes in Lhe upper portion of Lhe water

co lumn.

41

Page 48: DATA VALIDATION AND SUMMARY FOR THE NRL REMOTE … · For several years, Synthetic Aperture Radar (SAR) images of the sea surface revealed planar signatures which were remarkably

I11I1I1f I I tIj III I Iil IlI II l I I1 1 I li I I IIIIl

41 000' >4 7&6

BS

X C DE

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column

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Page 49: DATA VALIDATION AND SUMMARY FOR THE NRL REMOTE … · For several years, Synthetic Aperture Radar (SAR) images of the sea surface revealed planar signatures which were remarkably

10' I

410-

* 50'

40'

30' li I 1111

*40' 30' 20' 10' 6,90Fig. 5.25. Map of typical temperature profiles.

43

Page 50: DATA VALIDATION AND SUMMARY FOR THE NRL REMOTE … · For several years, Synthetic Aperture Radar (SAR) images of the sea surface revealed planar signatures which were remarkably

1 0 ' | T 1 -l j I I I I i I I J l l I| I I I i [ I i | l l I I f 1

410 .

/-- 50'(

40' - ["- i'_ _ p

30' , ii II, I III, , , , , I , ,, , , , , 1 I 1 , , , 1, , , , , ,, 1 I II

40' 30' 20' 10' 690Fig. 5.26. Map of typical salinity profiles.

44

Page 51: DATA VALIDATION AND SUMMARY FOR THE NRL REMOTE … · For several years, Synthetic Aperture Radar (SAR) images of the sea surface revealed planar signatures which were remarkably

ACKNOWLEDGMENLTS

This work was supported by the Naval Research Laboratory core program.

Scientific and technical personnel who contributed to this work were

W. Garrett, NRL Code 4350, senior scientist; Jack Ostrander, NRL Code 5004,

navigator; Lee Houston, Ralph Gallatin and William Robey, NRL Code 5004,

technicians; and especially CAPT John W. Areus and the crew of the

USNS HAYES who operated in extremely difficult conditions.

45

Page 52: DATA VALIDATION AND SUMMARY FOR THE NRL REMOTE … · For several years, Synthetic Aperture Radar (SAR) images of the sea surface revealed planar signatures which were remarkably

REFERENCES

Beal, R.C., P.S. De Leonibus and I. Katz (1981). Spaceborne Synthetic

Aperture Radar for Oceanography. Johns Hopkins University Press,

Baltimore. 215p.

Brown, N.L. and G.K. Morrison (1978). W.H.O.I./Brown Conductivity,

Temperature and Depth Microprofiler. (Unpublished Manuscript) Woods

Hole Oceanographic Institute Report WHOI 78-23, Woods Hole, MA 02543.

Greenewalt, D. and C. Gordon (1982). Lagrangian Current Measurements at

Phelps Bank. NRL Memorandum Report 4965, US Naval Research Laboratory,

Washington, DC 20375, 55p. AD-A123-223. 0

Kaiser, J.A.C. and J.D. Clamons (1983). Characteristics of NRL (NBIS

CTD's, Data Validation and Offline Analysis. NRL Report (in

preparation).

Kaiser, J.A.C. and R.A. Munch (1983). Data Validation and Summary for

the NRL Remote Sensing Experiment. Part II. Meteorology. NRL Report

(in preparation).

Rosenblum, L.J. (1980). Real-Time and Applications Software for the

Neil Brown/W.H.O.I. CTD Microprofiler. NRL Report 8444. Naval

Research Laboratory, Washington, DC 20375, 44p. AD-A094-610.

Valenzuela, G.R. and D.T. Chen (1983). Plan for a Remote Sensing

Experiment in the Nantucket Shoals (SEBEX) (December 1, 1980).

NRL Report 8659. Naval Research Laboratory, Washington, DC 20375,

31p. AD-B071-765L.

46

Page 53: DATA VALIDATION AND SUMMARY FOR THE NRL REMOTE … · For several years, Synthetic Aperture Radar (SAR) images of the sea surface revealed planar signatures which were remarkably

APPENDIX A. PLOTS OF CTD CASTS

Lowerings 1 to 41 are plotted sequentially in Figs. A.1 to A.41.

The left-hand plate contains profiles of temperature (solid line),

salinity (long dashed line) and sigma-T (short dashed line). The right-

hand plate is the T-S diagram for the lowering. All casts are plotted on

uniform size blocks with uniform axes. These data have been processed in

accordance with IV-A.

47

I

Page 54: DATA VALIDATION AND SUMMARY FOR THE NRL REMOTE … · For several years, Synthetic Aperture Radar (SAR) images of the sea surface revealed planar signatures which were remarkably

.-. ,-. - -----. -'. . -~ - - -.- ~-.-. - -

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APPENDIX B. TABULATIONS OF CTD DATA

Lowerings 1 to 41 are tabulated sequentially in Tables. The data was

processed in accordance with IV-A. After pressure reversal and wild point

elimination, the data was averaged over 1 meter bins. Depth, temperature,

conductivity, salinity and sigma-T are tabulated. The average vertical

velocity of the CTD for each bin is also tabulated along with counts of

accepted and rejected data scans.

Lowerings 8 to 13 and 27 to 34 were hand digitized. Data was inter-

polated to every .1 m depth so the point counts represent this. The

vertical velocity is unobtainable for these lowerings so it was omitted.

A

89

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ST~ixT TIMr 1910021/ POSIT 'TN 40 44 046 .- ''t "

S TA NO 7 OW NO3 i iN S-T N 0 , T.fl 6481m SIZE = OM DEPTHS fop 0 0M i; rrim J0 A,- ,ul (FACl- P!F5 = 3 urkfR

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36 35 33 t 197c; 11 1973 33 3521 2 6491 37 3R26 73 42 1 037 36 31 i1 1990 11 1980 33.331.9 23 654 37 r832 79 9 ;C 038 37 54 1t.t772 11.1772 33 3370 23 6692 37 S694 27 .- " - a

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13 k 30 47 11 1 II 07 1 1 .33 376 ,'i 7A37 37 49A2 48 64 A . 032 30 S3 1 1 0667 13 0667 33 3763 23 771t 37 4962 h,3 49 ,4," ,; .3 3 4 1t . A3.3 k i 0 ,3:3 33 .5799 23 762.1 37 4910 .4 71 ,,1 0S4 33 30 11 t0 31 0601. 33 361± 2S 7877 37 .19,6 79 39 ;'15, 34 94 , 1. 31608 L I A08 3.3 10 1 77 ?1 37 .9,7 ;, a * "

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MAXIMUM O.PTH OF CIAST = ,6. 021

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4( ,D-Ai32 083 DATA VALIDTiON AND SUMMARY FOR THE NRL REMOTE SENSING 212

EXPERIMENT PHELPS--(U) NAVAIL RESEARCH LAB WASHINGTON DCJ A KAISER 02 SEP 83 NRL-MR-5165

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MAXrMujm nprH OF CAW" 79 nim

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Page 102: DATA VALIDATION AND SUMMARY FOR THE NRL REMOTE … · For several years, Synthetic Aperture Radar (SAR) images of the sea surface revealed planar signatures which were remarkably

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46 45 75 11 2423 11.423 32 3 33 25 4962 37 370 40 7 , 047 ,4 6 it 2433 11 2433 33 11? 3 ' 313" 37 305- ;5 ' "48 47 72 I1 2429 i. 1 2429 33 11 25 I7 I7 3A r 15 /4'49 14 /21 1. 2-4356 1'1 2436 i3 .109 23 C 32073 37 s7& ' Ps .Sll 49 74 11 2440 11 2440 .35 t 109 2s 5292 . '/3 3 ,

4 l '14 7 It 2430 tI 2430 i3 , ,'4 .', 0 328 7 Ii ,- 7352 1 so tit 2418 I 241 R - 324 2 t4,1 .7 S5,15 1 09

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-. 54 75 ," 2402 2q32 3I , , 5 343? 1; 59") 1t. 1 , V

5o 5s 79 ii .2419 1 2419 3.11 12,4 25 55S2 37 38392 :0 ,4 19 56.,s4 11 2427 11 2q27 3 1.26 5 6S556 37 i9f1)7. '43 "

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0 3 9 8i 1t 2426 1.242 f 71 12 2r q16 37 )643 b S4 n

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?3 75 11 2434 1. 2434 33 1141 3 59- 37 39581. L4 19;51 -), -,f -S S9?

64 77 .. 24249 U 2429 3 '2,. 23 3994 17 3q2 -5

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* 79 77 77 11 2472 It 2472 33 '062 25 6374 7 3971. 1 A79 /8 76 1i , 47A I. 2478 33 ,124 S ,40 (7 3i7 ';6 U 4 11

MAXIMOM DFPTH nF R#5Ti -W 79 2(14

94

Page 103: DATA VALIDATION AND SUMMARY FOR THE NRL REMOTE … · For several years, Synthetic Aperture Radar (SAR) images of the sea surface revealed planar signatures which were remarkably

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Page 104: DATA VALIDATION AND SUMMARY FOR THE NRL REMOTE … · For several years, Synthetic Aperture Radar (SAR) images of the sea surface revealed planar signatures which were remarkably

II

DEPTH PIN AvERAGED CTD DATA

START TIME t93/0348Z POSITION 40 54 94N 69 t4 OWSTA NO 7t LOWN 76PINST ONOM 'TA P E=N O I o UFC RS=I0DASIZE - OM. DEPTHS T = 0 (I, BTTOM = 100 OM SURFACE 9S = I O0DOR

BIN DBAR FAST-T ACCUR-T SAL SIGMA-T COND VEL NO POINTS/BIN

NO A DEG-C DEG-C PPT G/CMXE3 MM/CM M/SEC _ OT4L __SED _WLD

46 It 2205 It 220 32 0740 24 4844 16 2930 to*Z 10 to 0i S3 it 1. it.220S 32 0782 24 4926 36 2977 *z** 9 9 0

3 2 SS i.1947 it 1947 32 109S 24 3260 36 3070 1*** 9 9 04 3 S7 II 1856 i 1856 32 t316 24 SSiO 36,3219 **d** 9 9 0S 4 S8 i 1830 11.1830 32 1484 24 S686 36 3371 Zz4* 9 9 0

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10 9'58 11.2462 11 2462 32 4638 24 8266 36 %1S8 9**9 9 9l010 14 It 2448 it 2448 32 4924 24 8566 36.7440 a 0

1 11 1 11.1779 it 1779 32 5329 24 9036 36.7254 **** 9 9 03 12 Ss 11 1476 11 t476 32 i3s3 24 Qt91 36 7044 4*X* 9 y 014 13 S7 it IS38 it.1S38 32 5904 24 9599 36.7630 dz*** 9 01 14 S9 it i563 1t.1S63 32 h211 24 9849 36 7968 ***Z* 9 9 0to Is So i1 1291 1t 129t 32 6454 250169 36.7974 **E* 8 3 0

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20 19 38 it t719 11.1719 32 8320 ?S 1722 37 0265 ***E* 9 9 0

21 20 54 11 2957 i1 2557 12 9190 2.5 2278 37 1868 1(*** 8 8 022 21 51 1t 2971 it 2971 32.;281 25 2344 37 23R0 *** 9 9 023 22 53 t 3183 Ii 3183 2 9314 2S 2342 37 2610 Z** 9 9 024 23. SS i 3200 11 3200 32 9493 25 250 37 2811 ***XS 9 9 32S 24 57 It 3200 11,3200 32.9S46 25.2646 37.2870 d** 3 0 0;1 ; s ss it i200 it 3200 32. S$42 , ; 7,4 37-1870 *11*** a a 0

27 26.5? It 31i8 I 3118 32 991i 25 2895 37 2870 *4** 9 9 027 S4 II 3146 it 314h 32 95153 ,S 2872 37 .1370 *4*.t* 9 9 0

a; 28 q6 it 2955 11 29ss 32 9808 2 3021 37 2930 4**** 9 9 f!10 /9 ;8 It 2993 it 2981 3.3 01)9 2S 3499 .57.J322 t**A 9 .? 0

31 30 55 It 307S it 3075 33.31SS 25 35t9 37 3400 *** 8 8 032 31.S2 I 1 017 kt.317 13 0i 25 .3687 5 140() p**:4* . 9'" 033 32 54 It 299S 11,2905 33 0219 25 36S4 3V.3400 4**4 9 9 0:34 3.3 S5 it 3040) 11 34401 .3.3. 11279 159 361 19 1502 **** 9 '0 03s 34 57 41 2903 It 2903 33.0743 29.4069 37 3857 4*4*4 9 9 0

16 3s 59 1.1 273 .t 270; 3 09 9 2S 44 7 3 3930 :4 9 9 037 36 S6 1 270S t1.2705 33 0985 21 4384 37 3930 *a4* 8 8 038 1 7 53 It ,d/Os i11 2705 i3 981 29 441.3 .37. 5930 11;4 * 1 9 0*9 38 15 11 2705 it 2705 33 a976 25 4570 373930 4*4** 9 9 (140 39 7 Ii 2705 it 370S 3.3 1197P 25 4'#'?" 37 393n *4:* 9 9 0

4t 40 54 It 2705 1t 270S 13 n968 25 4609 37 3930 4*4*4 8 8 0'42 41 So It 2705 iI Q '1 ;1 4964 /s v842 7 10.93) 94*4 ' 043 42 S2 It 2705 I1 2705 33 09h6 21 459A 37 3930 k%**** 9 9 144 43 94 it 713 1 1 7t3 L3 49413 ,j '"1713 17. W9.10 it 9 y 04s 44 56 t1 2763 it 27h3 33 099 2s 49?06 17 3930 9 9 0

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5t so s8 it t268 It 1268 3 1964 29 6059 37 3670 **4* 9 9 'i52 I q6 I , hO it , 461 1.; 14i2 s ,7 h,.16 / 4(Al i It ,4 4 6 0S3 52 53 11 1150 11150 13 '017 2 628 1 3?7 .4 4* 9 .* 95,4 3;.3 csx5 t t w k4 '1.1 11149 ;S ;102, 'S .2,, ; 7 i50.3 *it~ 9A kS S457 1t 0858 it 0858 1 3.2/43 2" 1 .37 37 .191 ** 9 .; ,

36 S5 59 It 1830 4 0830 33 2057 29 6q30 37 3,iR7 4**z44* ? y,7 1 56 it 6 :30 1.1 830 i.i , ,2 ' )Q4 ' 37 .13 i t4 A 8 0

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MAXIMUN DEPTH ]IF CAST 62 0,N

96

- - - - - - -

Page 105: DATA VALIDATION AND SUMMARY FOR THE NRL REMOTE … · For several years, Synthetic Aperture Radar (SAR) images of the sea surface revealed planar signatures which were remarkably

DEP T"- R4N E4Fl.ef r

START TIME t93/22i22 PCIS9ITtION 40 41 3n N 69 11 32wTA N9 L=7 N' 1 INST ND . TPiiE NC ,IN SIE A DEPTHS T6P I iM, A FTT1M IJl '3M SLIkFAiE PqE- IiDPR

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46 t; 163 5

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3 bS 12 8619 12 8619 32 A794 ?4 ali7 18 6067 73 - 04 3 57 12 68S t2 6885 32 7227 ?4 7.?77 3P 2039 *1*4 9 0s 4.S 12 5307 12 i007 33 7696 24 A069 38 i620 **** 4 0

6 S 59 12 6126 12 o126 32 8036 24 8107 3p 2999 *-3*4 3 4 47 6 53 1.2 2951 1.? 2951 32 7616 24 850 37 9672 **1.0 9 08 7 55 t2 3158 12 3156 32 8767 24 9402 38 t06e *** * 9 09 8 56 2 2S83 12 2583 32 9240 24 99i9 38 .32 **.It * 0Uo 9 se 12 '725 12 0725 33 0035 25 0908 38 011o ***** 9 9 0

11 10 94 1t 8671 11 8671 33 0463 .9 1647 37 8729 *4** R 8 012 11 S1 1 '567 it 7567 33 0716 25 2187 37 7984 *44 9 1 013 12 55 11 h114 it 6114 33 0548 25 ,297 57 6490 4*4** 9 9 014 13 57 Ii 5717 11 57t7 33 0731 2 r583 37 6320 *4*4 9 9 0IS 14 99 it 4922 i1 4922 33 0801. 23 2910 37 9670 4*44 9 0

1b Is S6 11 4474 1i 4474 33 3808 25 2979 37 5273 **** 3 0 017 16 S2 11 4468 11 4468 33.0865 29 5062 7 5330 **4 9 9 .)is 17,54 ii.S426 I G426 33.1638 25 3q97 7 09

96 944 q

19 18 96 11 5341 i1 5341 33 k939 25 3S70 17 n822 V**:1* 9 ? 020 1958 i 4762 it 4762 33 1247 ,? 3479 37 6000 *4** 9 9 0

21 20.54 11 4767 11 4767 33 1283 2.3491 37 6049 ***IN* R 3 022 21 Si it 4631 It 4631 33 1364 25 3680 37 6007 *4*4 9 9 023 22 S3 i1 9200 't 5200 33 2030 2S.4049 J7 721.0 *4* 9 9 024 23.85 11 4105 it 4105 33.1837 2 4213 37 6017 *44 9 9 025 24.57 11.3887 it 2887 33 t6a '5.4361 37 4750 4*4 9 9 0

26 25 55 10.2536 i 2538 33 t741 29.4489 37.4496 a444* 8 8 027 2h 52 11 2355 11 235 33 1782 2.4h636 37.4376 ?44*4 9 9 028 27 54 t.2602 i1.2602 33.2158 23.4971 37 4987 444*4 9 9 029 28.56 11.2844 Ix.2844 33 24S2 AS 9227 37 3909 i4iii 9 9 030 29.58 11.2856 i.2856 33.2442 25.5246 37.58i4 4*44* 9 9 0

31 30.55 it 2331 11.2331 33 2978 25.9492 37 5176 a4.4* 0 8 032 31.92 11 2066 11.2066 33.2437 25 5472 37 4796 *4*44 9 9 033 32 54 11 799 11.1799 33.259; 25 9620 37.4716 444.1 9 9 034 3355 11 1612 it 1612 33 2671 25.5827 37 4626 *4*44 9 9 035 34 57 it 1580 11.1980 33 2660 25 5798 37.4590 4;an 9 9 0

36 35 9 it 1537 ti 1537 33 2659 25 6027 37 4553 44*44 9 9 0

37 36 96 11 .136 11 1365 33 2747 3; 5984 37 4490 *4444 8 8 038 37 q3 t 1233 It 1233 33 2803 25 6193 37 4430 444*4 9 9 639 38 95 11 1094 11 1094 33 2865 AS S426 37.4370 *) * 9 9 040 39 97 11.0937 11.0937 33.2867 25.6362 37.4232 *4 9 9 0

41 40,54 11 0830 11.0830 33 2857 29.6410 7? 429 q*4* 4 8 042 41.90 11 0830 It 0830 33 2793 29 6326 37.4069 44*4 9 9 043 42,;2 11 0830 11 01)03 33 27l0 29.6261 37 *406) 4*4* 9 9 044 43 54 11.0830 11.0830 33 2776 25.6483 37 4060 *4444 9 9 045 44 96 11 0830 1t 0030 33.,772 29.6986 37O 4lki .*4A* 9 9 0

46 45 53 11.0830 t1.0830 33 2873 25 6637 37 4166 *44* 8 3 047 46 90 11 0830 i 1)830 33 .303k 29 6094 37 4330 .k** 9 9 048 47 52 l 0823 i1.0823 33 3033 25 6974 37 4330 ***** 0 9 049 48 94 ti 0709 It 0705 33 3136 29I069 37 41330 t4:K** 9 9 050 49 56 tJ 0705 t 0709 33 3132 25.7091 37 4330 **4 9 9 0

53 50 98 l 0705 i 0705 33 .127 25 7097 37 4330 4t 9 -

MAXIMUM DEPTH OF CAST 51.1.0m

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26 Is 5 S 1 .0833 it 0833 33 4S67 2S 7146 37 3790 ***** 8 8 0-7 26 S i 0830 11 0830 33 4060 26 7109 37 S790 .k*** 9 9 5is 7 64 11 0830 1t 0830 33.4561 26.7197 37.5790 ***** 9 9 0

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36 35 59 it 0830 It 0830 33 4626 25 7465 37 5790 *4*4* 9 9 037 36 56 1t 0830 It.0830 33 422 2S.1406 .37 6790 .4Ia** 0 8 038 37.53 i1 0830 t1 0830 33 4SiS 25.7632 37 .790 **4* 9 9 039 38.66 It 0830 11 0830 33.45t4 2.7613 37 0790 ,1*44 9 9 040 39.57 it 0830 it 0830 33.4509 S.7899 37.6790 4*44 9 9 1)41 40 64 11.0826 It 0826 33 4609 25. 76R1 37 6790 * 842 41 SO it 0708 i1.0708 33.4612 25.79t2 37.5790 ***** 9 9 0 .":

43 42 S2 i1 0705 1i.070S 33.4611 20.1966 37 5790 *4*4 9 9 044 43 54 l1.0706 11 070S 33.4606 2S,7950 37 6790 4441* 9 9 045 44 66 11 070S 11 0706 33 4602 26 8009 37 S790 :.*.f* 9 9 0

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bt 60.59 tI 1 0401 11 0401 33. 4811 dA 8 2S 6 / S791) A.OK ua2 61..A 4 1 0434 1 1 13434 33 477h 2 S 915f C; 3 790l 'K H I3 62 C; it 0.186 i1 0386 33 4817 6 9,7 37 ,T9) 44.41* 9 9 064 61 It 0330 01 1330 30 4863 26.9178 7 q790 *4*

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31 30 ss 11 1229 11 1229 33 3640 2s 8053 37 7257 ***A* 0 8 032 31 52 11 14t2 11.14t2 33 5691 25 80i 37.7481 *4*4 9 9 033 32 54 i1ji484 11.1484 33 380Q 25 832S 37 7743 *44 9 9 034 3355 1631 it 1631 33.800 25.R209 37 7801 **4 9 9 035 34 57 it 1673 I1 1673 33.3874 2q 8314 .37 7920 *44 9 9 0

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Page 111: DATA VALIDATION AND SUMMARY FOR THE NRL REMOTE … · For several years, Synthetic Aperture Radar (SAR) images of the sea surface revealed planar signatures which were remarkably

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Page 112: DATA VALIDATION AND SUMMARY FOR THE NRL REMOTE … · For several years, Synthetic Aperture Radar (SAR) images of the sea surface revealed planar signatures which were remarkably

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Page 113: DATA VALIDATION AND SUMMARY FOR THE NRL REMOTE … · For several years, Synthetic Aperture Radar (SAR) images of the sea surface revealed planar signatures which were remarkably

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Page 115: DATA VALIDATION AND SUMMARY FOR THE NRL REMOTE … · For several years, Synthetic Aperture Radar (SAR) images of the sea surface revealed planar signatures which were remarkably

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Page 117: DATA VALIDATION AND SUMMARY FOR THE NRL REMOTE … · For several years, Synthetic Aperture Radar (SAR) images of the sea surface revealed planar signatures which were remarkably

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MAXIMUM DEPTH OF A.5T 9 99 21M

109

Page 118: DATA VALIDATION AND SUMMARY FOR THE NRL REMOTE … · For several years, Synthetic Aperture Radar (SAR) images of the sea surface revealed planar signatures which were remarkably

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11 t 77 1. 1141 t 5141 32 .2%; 25 )64S 37 3259 46 'zt2 11 68 1 1 15 1 1q .5qI 32 8493 25 0886 37 380 43 7 IRl3 t 2 76 t 541) 1 ,406 32 8693 ,21 t039 37 3953 42 25 a14 13 7 ii 5373 11 5373 2 8714 2C 109t 3)7 3949 48 .- ; II5 14 70 ti 4791. . 47 i 32.274,; 2s ).Z31 i7 46 71) , 4 0

t 1S 76 11 4345 I1 4340 32,8734 2F 13R6 37 7040 61 4Q 47t7 16 72 It 4073 tl 4073 32 ;3710 20 tS3t 37 98'i9 36 ' j18 17 t7 1,t 3484 11 3484 32 881t3 2S 1769 37 '3q4 7u 44 4119 t8 70 tt 3389 11. 389 32 930s 2.9 2153 57 2771 83 - 020 19 77 11 3796 11 3794 32 9762 2S 2490 37 3n10 48 60

1 20 68 11. 3795 11 3795 33 0020 135 2764 37 3880 52 50 .8p 72 1 4279 t1 4279 33 0274 2s 293S 37 4579 Ri 8 j7

23 22 73 it 5074 tt 5074 33 0867 2S 3253 57 910 s91o 4724 23,68 It 0812 it 5812 33 1362 25 3563 37 7093 so b3 5o 025 24 69 lx.6845 x1.684S 33 076 35 3941. 37 :3773 77 40 39 11

26 25 70 i1.6983 ti.n983 33 277R 25 4513 37.9622 6 32 2 ,)27 26 71 11 5846 11. 6846 33 3351 2.6247 37 91,67 73 -. 928 27 72 ti 4789 11.4789 33 3389 25,0527 17 8239 37 R0 'A ,i29 28.68 1t3933 1.3933 .33.37k9 20.3959 37 7792 3 In 31 030 29 70 1i 3849 it 3849 33 3908 25 n208 37 79i2 1 19 26 26 01

31 30 73 it 3572 it 3572 33 4006 2; 6377 37 77i, 1. 33 30 032 31 77 t.3307 it 3307 33 4108 2s 6s52 37 7625 St 59 00 133 32 63 Li .2936 t1 2936 33 4046 25., 6579 37 72,b 48 -4 ,7 034 33 70 it 2857 I1 2857 33 4173 25 6736 37 7286 90 30 -, aj 1-35 34 74 it 2868 i1 2868 33 4ps 2.673 17 7380 79 . 34 a

36 35 7S I 2786 t! 2786 33 4280 25 69S4 37 7338 48 49 (I37 36 66 t1 2649 11.2649 33 4267 26 70n0 37 720; 77 . 35 338 37 70 1i227Q 11.2270 33 4370 20 7274 3Z 6964 1.10 .28R 28 039 38 71 It 242 ti.2429 .33.3. . 9438 17740 1) 1 '4 '7 2640 39 88 it 2540 t 2540 33 4894 25.7731 37 7749 34 -7 4

41 40 57 It 2s. :x.20051 33 ;034 25 78l14 37 790' 3 65 )

42 4t b7 It 2436 tt2436 33 0266 25 8032 37 8038 1 to 21 ' ;43 42 73 11 2349 1.2349 33 5488 20 8361 37 A.88 i ", , 3 344 43 70 it 2338 i 2338 33 0630 25 8486 37.83. 1 0Q 1 /849 44 .91 1i.2354 It 2394 33.;79 20 8550 37 84, 49

46 45 67 It 2413 A1.24 1-1 33 5986 20 8717 37 8682 $5, 6,h 4847 46 73 1l 25t0 t 21; 33 60S9 2. Ht9 37 '9W:6 ?i3 31 3.448 47 77 i1 2633 t 2633 33 6252 25 9069 37 9244 4h C;4 U49 48 64 11. 2;77 11.2777 33 h422 20; Q300 37 9 99 o' 4,1so 49 69 11 3041 Ix 3041 33 6673 25 9423 5P 009 1 S I t 4

51 50 93 11. 3279 tI 3279 33 6901 25 9S77 38 "S0t LI -).52 50 86 11 4170 11 41 70 33.730 26 n 38 a:) a

53 3;2 b2 144011 4 43 311 15 ' 6 td 8 Si54 53 76 11 ,727 11 4727 33 Q o 38 6 i : 3(13Q R ; I0;3 4 '0 Ii o63 t. o26.3 33 915 26 .022 58 9n8 ',-

MAXIUIJM DEPTH OF ,A,4T = k0 n

111

Page 120: DATA VALIDATION AND SUMMARY FOR THE NRL REMOTE … · For several years, Synthetic Aperture Radar (SAR) images of the sea surface revealed planar signatures which were remarkably

DEPTH FTN AVERAGFD CT1 DTA

........- ---------- --- --------- --- ----- ---- ------------ ...- ------------. ..........................57ART TIMR '95,02,4Z 82511101N 40 34 R5N,. 6-9 Pfi 53WTA NO 7. uOW M1. 2. -ZNST NO IP NO

BIN SIZE = I '3M DEPTHS TOP R7"1. 810TT8m u i.40 3M SURFACE PREU = ri IDIh,,4

PIN DBAR AST-T ACCUR-T SAL STMA-T COND VEL N(") P 0 T NT5S,'Ni 7TvNO m DEC-C DEG-C PPT G/ -, 3 MM/Cil M/-EKt Ti 1L '15FD M1L D

1 61 1 81 t

Q, t18s1 32 4881 24 ,293 37 381)9 20 'i9 A,'=2 1 66

" 10SS 12 lOSS 312 s304 24 62R 37 S534 19 1e4 +7 .

3 2 72 12 ,"

. 12 k7 ,2 32 5412 24 '834 37 6244 74 4.3 4'14 3 18 t2 t39q t 39S 3? s290 24 6847 37 ;836 57 54 9;R5 4 58 12 25s8 t2 2s5 3.2 5726 24 7003 37 7.343 ,21 L40 ,)

5 70 t2 4q76 1.2 4576 32 s730 24 oo7') 37 ?IR0 39 3. 4

7 b 79 12 2369 %2 2 59 3 1294 24 ,804 37 i73.3 47 -,7 0a 7 59 12 13404 12 0404 32 _tlo2 24 7179 37 4?63 32 94 8 a9 74 i t 7903 i t 79 t)3 32 4600 , *7208 37 071 8 s-; S6 49

78 n 70 it 39,,6 It 3966 l? 4001 24 75.2 36 78,6 40 79 oS 0

14 7t .t '648 11 t 4 3;2 .4447 ?.1 8142 356 '7134 ")2 t '2 2 2409 9409 12 4520 24 82S 36 e,999 38 79 ,-

o'3 1.2 0 Il >94 I1 20:4 12 ,SSI 24 ,4,2 3, n8,3 49 '3 42t4 13 '4 ±1 1994 1' 1994 32 4hnO 24 831 . i3, o7?8 77 41 39 'IiS "4 -i 2 i 19q:? it 19 9 32 '41) 24 861-, 6 .;6 , ,.d .59 HO .-R '5

16 .5 64 11 1934 it 19314 43 4,64 24 8665 3n 6737 -3 t't7 137 - ~ i4 32 4iaP 24 3720 3-6 ,76e, 7- '24316 i" 3 17 U t955 it " 32 4',at '4 ,17-R 76 .'8 38 79 ,2 ,91t $8 r.S Lt i? 39 i 1939 2 4726 34 d t )6 i 8 ,3 o7 ,4, 43'o Iq 7t it 1924 1! t924 12,4799 i4 9980 36 6131i 7 44 39/

': 90 , 9 1t1 189 it 389 32 4893 !,0 9 111 .3k, ,95 3, 95 7'.2 2t 73 1, 1,B 11 "81ea 3,.1 5026 34 24 3 3 -io 7364 7'0 44 4') ,

23 22 75 it ,869 h L ,R69 32.32 7 a'4. '?44-

.,? .' ad 10 46 ,24 23.O it t897 ti 1097 32 q407 34 7947 36 749t. 39 84 625; 34 71 11. 19.t it '961 02 53i 6 24 ?7737 36 7734 3 1 54 33 0

23 -- 76 it 200t it 001 32 5624 24 9938 16 7812 75, 41 38 0?7 2b nO 11 203 1 ti 2021 32 %29 24 9903 36 7840 114 q3 028 27 o9 i '398 i 2396 32 5987 as 0255; 36 3546 37 34 0?9 E3 7, i 2t86 t t Z16 3 ,83 05 '1913 .4 t7 .i730 29 b7 it 2081 i1 208t 3? 72S3 25 t358 36 9154 G0 63 54 ,0

A 33 71 1c07 11 21S7 -2 7597 ' 68 .~915 ~ 0 q

32 41 73 11 2084 t1 9084 32 7858 25Ss '9e, 37 0178 41 78 a,- 073 32 m4 t 2040 l'i 2040 2 142; 35 , , '.') 37 45C25 ,.-i ,7 49 034 33 72 1i 2034 11 2034 32 3760 '5 1-717 37 0qS 08 36 3-4 0it; 34 /2 'i I'S0 ii 21t') 32 9091 , '98 37 I'.9 H. 146 33 4

3h 35 73 it 2 21', 1. 21h 32 9412 as l'S) 37 18q8R 114 8, J"i7 S17 oh . 23t0 .1 .23..0 33 00,#H S 78' 32 , I,,R 0 1 's u31 37 70 1 '949 1.1 ,949 3,3 (1963; 2S 4-98 37' 4L37 1 13 23 27 03 8 73 1 t4' I . OR6 33 L69-, 25 s079 '7 SOn '; 33 30 340 -34 75 3 5 260 1 J264 33 2222 5 5491 .7 c,704 ,_ 1.',q

11 '40 73 5 t 33); 11 1 i 03 1 3.3 '6h I , Is 0, 32 G 1 5 " 3 -5 H3 3S 9 u4,3 41 73 11 7,j64 it 3"A4 3 a3n9 37 779 k1 3 ,, 143 4' 79 34n0 . 3463 33 1. ) . 37 3'12 -A'3 7Z: S 044 43 58 t; 3349 11 3349 33 4t(t 95 7-]9-7 37 7,1116 23 133 H4 0)40 44 I 1 30 i;9 $081 13 45; 6 2S I'7i n 3' 7 ? ,A. Oil " .O 0

40 45 -3 it 2971 it 297, 33 490"

, 7f4H 37 01179 43 3, ir

47 4. ,7 it 2908 '1 2908 i3 ,l; 93 1').;4 "7 322- ., d, I)r 48 47 73 11 ,28964 11 286 13 '17 R2 -814 37 1,164 f4 00 ;., 0

49 ,48 76, 1 28104 It 2*804 Vi ' ,22P7 S3 64'1..5 37 14710 i '.>:'R 1:j

mo4 1M11M SFP To-i gl i43 ,9 4Q a m

112

• - (I - II m ad 0

Page 121: DATA VALIDATION AND SUMMARY FOR THE NRL REMOTE … · For several years, Synthetic Aperture Radar (SAR) images of the sea surface revealed planar signatures which were remarkably

- ,7 -lz - - - -' T , -,3 - -7 I - - -- , - - - - - - -- - - -- --. , - -:i € - -d -- -- -, ,i..4 -, T 7ME,937. 4 3s. r4 7 w

LW?) OuAR A Sr ~ -- T 7%'M' ,Wfi v,

'41) .1 3W.i1- , ,T 17 4ri4 M M ,/ ,

1 'P'% t € 4 '-,- .P -, 3..is~ 4, . ,',4' iIb 9 ) -41 -t2 1' '9 1 i18% '1 'vj63 92"11 , 7,q 3,o3i3 I -.

4 3 21 7 7 1 , ,4 '4 ..4 4 7I ,,.' 44 -.4 0

1 7 1 5 F', t 2 ', I ''h; 7p "*I'4 4 m 4 -4',<1

17 7, I ,29 1'. 38.,2 2 230' , 4 7'4' 36 ,341 'I it 1"

'P ).' 7 5977 2 -C 7 3,_3i '"; 4 -21i r,;P 2-4 n j24 ' '1 72 : 3t'A IA .2' 32272880 4 -2,' 3 -, ORz4 74 73

k 6, i k P',i It 5P , 2 CI* Q,, '4 ., .) 36 9-> 1 .3 j22 11 719 '1 '2P it 9ii 32 IR4A Q4 714 36P033 ,. 1'3 :2 A '2 '± "t'92 3P 124 4 3e, ,9'?. ,J 3i4 t3 71 ' 1 ',9 11 S P? 32 3449 24 1;A,? 3A '04 '16 " 1

.3 4' '9 i'5 3 5343 '4 4 ;- Q1'

is 15 I t 2 13t ?21 '4 470 34' 6 1 7 47026 2 ' '0 % i

9- 3 1 '393 32 449 '4 43 3j 'Pi0 '4 IY 3

78 7 4 1 ' 29 t 9 32 3497 4 -36 ' -i13 ", 734 4:" 28. ,.3 t .215 u .220 S, 2 1 8 ' '69, 36 il3T. - : 323 t9 2? 1i 213 it 2136 32 3979 9, 870 b)3 734 4 27 2 1

31 .$) 75 t47 i 1at ,)37 .2 3,9') 2) .460 363 I., '4 3 '1' 1 75 I -, 112t j Ii 32 39 0 4 04 11. 43 7t 1 8

23 74''

* 3 32.0 ti, 2097 :5 2092 3 2 .94 94 6234 1., 92749 71 'a S9

24 23 74 it 2.37 tA 2137 32 3749 24 8S 36 e40.24 4 '325 24 78 it 2t96 11 256, i2 3779 24 " t4 34 , 647 9 96 2 1 f

26 25 60 11 287 1t 2i87 32.380t 24 ,8431 36.613 6 I427 26.71 t1 218 11,b i.. 2 38:9 4 9.5 36, s, 1. 17 17 028 27 74 tt 2189 it 2i89 32 3823 24.8999 3i, mx6i 3 Q) p29 28.73 11 2,21 t2182 12 3 2t4 86,4m 616 33 'P7 ,35 030 29 68 ti 2144 t 2144 32 3879 24 8780 36 6i87 73 42 3i 1

51L 30 74 11 2t36 1 2136 Q5 3904 214 4341. 36 6210 70 44 41. 332 31 71 1t 2017 1l 2111 32 3929 24 R834 ;6 217 43 -t 5i) 033 .32 69 I 2097 it 2097 5,23954 24 682 36 o

2 33 7 2? 39 3

34 33 72 t 2089 It 2089 32.406,4 24 909 36. 6341 .,6 48 44 055 34 72 11 2089 k.12089 32 4273 244 'P27 3 6 70 -9 46 07 03 0

36 35 68 it 209t ti.2091 32 4027 4 9229 36 619 57 54 48 037 36 7 1 it 2091 11 2091 32. 4286 24 9396, 36, i,9142 h 48 'is 035 4E 74 it 2890 it 2090 4 4 P4 9479 J6 7 86 47 @6 S- 0

3 83T 67 1 4 .1.81 46 2j4 9979 '6 4z 67 46 451 040 39 71 .I 2076 it 2076 32 4346 54.9S49 36 6644 46

-.. 41 40 82 1.1 2079r it 207S 32 4346 24 96,94 316.66,47 S36 's 5') 042 41.61 11.2079 it 2 079 32 4335 24.969,7 "36 f642 3o :01 4643 426,8 I± I'080 11 2 08 0 32. 1.34S 214 96,9 .46,6S7 .95 34 '51t

*.44 43.78 it 2085 11.2085 32.4381 24.97'9q 3(6 6703 .59 59. 41 44c9 44.6? it 2146 1 21;?46 32. 4720 29; 0 )77 36.7104 26 1. )9 1' 0

46 45 70 i 2157 11 2157 32.4749 29s l168 36 7149 43 72 61 0)47 46. 70 it 219 1 S 12198 3.? 4879 29 41379 5r, 7289 40 '7 -.) 048 47 71 It 2'157 1, 2157 32I 941 9 97 36 7S659 4' 76 '1 149 48 74 11 2093 1t 2093 32.5763 25 t1f.5 3, 8134 , .22 77 0s0 49 69 It 2027 t1 2027 32 e049 29 ,i73 36 8368 .st , 53 0

MAXIMUM OEPTH OF CA'T S 0 I''

113

I"

Page 122: DATA VALIDATION AND SUMMARY FOR THE NRL REMOTE … · For several years, Synthetic Aperture Radar (SAR) images of the sea surface revealed planar signatures which were remarkably

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74 1 45; - -, 7. '1 Y ~ i~4''

4 7 c &'5 Ct w <3 2T 4 -4

v.@

.. 1 E am 7 , ." 7; -M1

64 si 6S3 t2, 3' O j ,1 37 ' 4

7 9 n 4,3 ' -bS 7 4 .4 4104, 1 13 10 4 72 '649 A2 34 3 .142 13 oo;;' i- l 3

so. .6t I' 04.3 7' 8,3 q I47 v4 A7 37 41

i ±2 76 0 r844 o7 52 o44 "24 r,9(0 4ai 84 79 '2 6313 Q o,313, 3l 4147 o.97,1 "-,

17 4 16 ? ''o74 ,, ,l 3 .1 . 24 1'4

13 Sl 643 1~- s44 ,. V -d ' 1 '44') '4 o047 37-'4

b 1 43 1.21 .Ro 31 '448 24 P-_14 C 7 qjt

t. 27 113 12 o4 1? ,44 3; 7443 t. -4 11709 7 3,

1 1 18 6;79 e6 2 84 6c'R 3 714

3 24 62472 3-, 3 112 14 31 2 ?b

714 t2 J 754 31 4 4 1 3; 4~ ' 37 1

18 20 4 Si i 3 ,'1 2 7)J 31 -44 4 ,) i,0 3 4'; I-

141* I ? 1 78 '2 901 ?12 ooll 's34 '4 7

7c -' '416

-o 2 q4 t ;2 I 3 44h 24 1o R 37 4.,44 11 13 a' I 2 Io' 1'2 o,9l -3: 74,47 3-4 1o4 "503 7 -

.3 58 12 nS ' 0 n8 11 4,1 4 '14 7, -, 44 :,

9 78 "2 2 1 1 7

. 1 444 . 'j '4 J

DFPTH 8TN AVERA GED GPO 087A

STAR TIME 19,69 PST 405 2,4 1H. 9 4-7~

STA NO 7. LOW 8 21 ?NST .1 , rAPE t 0 1SIN SIZE = " FM DEPTHS. TOP S; BOTTDM = 100 3M SURFACE PE5 : 4 O4D91 3

-. N DGAR FAST-T ACCLIR-T SAL SICMA-T GOND 'dEL NP PI3TNTS/T418NO 4 DEC-C DEC-C PPT CICM*:43 ,II//rI MiSF.C rflr4L ISED .eiLD

24 1 44 1 441 12 4651 31 74322 24 0726 37 137 0 2 7 4 1* ' 1 91 12 4620 12 4420 31 6277 24 0726 37 t408 2, iSt 68 0

3 05 12 49666 12 45666 .31 429', 24 0}808 37 1.383 40 77 o 7

0I4 3 95 12 4569 12 4969 34 .3296 24 0R8 37 1393 4?7 4o 47 1

* 3 00 12 456S '2 4565 31 629T 24 0900 37 1390 3? 3? 45 )

6 4 01 12 4559 12 4959 31 6300 24 0997 37 1393 44 o7 So, 0"7 4.99 12 4556 12 4556 31 8363 24 '62 0 37 '3 8 an 49 446 7 98 12 4556 12 45546 31 . 301 24 1O95 37 1440 64} 39 33

0 ,0 12 4592 12 4592 31 8303 24 14 3 7 1402, 7S 42 1013 10 03' 12 4551 12

° 4551 31 6.,304 24 1164 37 1407 36 -.; -,O ,

*11 10 96 12.4941 12 4541 31.8308 24 119237.t407 55 96 40 0±2 i2 00 12.4543 12.4443 31 6307 24 1291 37 1412 70 45 43 0

- 3 13.63 12 4943 12.4543 Il 831') 24 1295 X7 1419 e8 46 44 0 :14 14 05 12 4545 12.4545 31 6309 24 13.70 37 420 70 43 "37 ,)±5 15 346 t2. 4544 1,2 4944 3;1 8309 .24 1391 17 '427 0

7 49 39

to 1=6 03 12.4527 12 4527 3' 6,313 24 1463 37 1420 39 93 57* 7 17 00 i2.4 ;.3 0,2 4515 51 -4319 24 I1 37 4') 6'b 49 46 l

16 16 01. 12 4514 12 4514 3' 4314t 24 13440 37 0423' oh 5t 44 't'9 '9 10 0.2 4513l 12 451.3 3t ,-3'9 3 4 .22 3 7 '.42.7 -9 49 4726 20 01 12 4915 '2 4S15 31 6317 ,24° 1o53' .37 143 0 01 49 44

21, 21 02 12 4914 12 4914 31 :-33'16 24 770}.3 37 :433 35 36 483 022 22 05, 12 4912 '2 4912 3 1 '03 1 24 1784 ,7 ±.40 c-c 47 43 ,42 23] 03 '2 4307 i2 ,&S67 31 83 21 34 11t 37 3435 34 37 Aj2°4 23 96 12 494 ±2 4414 31 63J9 24 807 "7 t449 "

24 24 02 7 4316 ' 4918: 31 8.318 24 13"9 3" ,5 499 49€ Or" . :% 98 44).8 '.2 4St,"} 3i -3)7 ,24 ,'773i ;7 I.: V :, 49

*26 26 00 12 4462 t2 4482°

31 8.390 24 2'ltOd '; 1 7e 7 4o 3,29: ,t'I 04 .,3 431o 1,' ,

4'Uo 3; 17314 31t ,-l'3,' 5" ~} r T 4)

31 30 76 12°

-4o8 '.2 43,7 3;i 71181 34 .)j55 3' 4,7.' .1," *.;e '32 32a 0.' 12 4524: :2 4424 3l '3314 ,2, 2208 57 '4H4 71 42 .374 333 33 08 ta 49,-9 2 43,29 It 1)3'? ,'4 ,2;30) 32 .4m, - ,24 0334 34 1,2 12 4537 1.- 4937 It 8-312 24 234' 37 t'fO 04 712 tSo

mAXTIUM :)FTH -,F m 4 )

14x544J4H RRPI AVRFE Cs.- -' 3 "U

----------------------------------------------------114----STR IE t8atZ PSTTN 4 02, 94 q

Page 123: DATA VALIDATION AND SUMMARY FOR THE NRL REMOTE … · For several years, Synthetic Aperture Radar (SAR) images of the sea surface revealed planar signatures which were remarkably

-~f ---- -- -- - ---- - - -

-- 7-7

42 " 4l Y,: 1A45" %' "',4 % '

s:N i ZZE z I )m 0;3 F kjT 7%1v.r. ' '.

.4N DBAR F49T-T ACCUP-r ',Al , *.a-T ND . , ,.. 2 -' p.NO I DE&;-C 083.-C p p 'iin.3 ;M-'4 M'/l

4 '~~'

4o, 12 '000 t2 2000 '1 , ', 99W , ',i '3Ij1 AA kO .2 :3 i i 7tj7 11 71.

77 3.- ,p,44 '4 1923 '6 -'41 4***

3 33 1: 4498 1t 4 49 3. 28 ' ' ?87 4 30 2 9 t f. 94 3 37 11 440C0 1 4400 -iR 16 4 IV 56 90 A A 93 4 38 It 4400 1t 4400 32 '0 i 44j 36 2937 9,4 AS

s7 3 t' 4253 1i 4 32 184 ?8 04 76 oa1s,4 4.* '0 S-3, 3 420') It 4230 1 32 2644 -4 '94 36 cOS6 1*M .Aj S 1 53 it4204 t 420; 32 , -7 7 4 5796 3, 599P2 X* A 9

2t 1 410 1G 0 41 .2 0 32 t9 47 '4 ,,347 , 09 £i 7t 8 53 ti 4060 tm 40.,0 32 ?2 '4 ,9?4 36 539 0 os 70

22 2t 4 4000 1 2 4000 32 212 64 '3 91 At n* 0 j j2 0 13 i) 40 1) 3.-0 32 20 o 4 ;0' ,, '0 4*:1 9 ,a

% 3 7; 9 430 1 4010 32 231 2 4 '1 3 7; 4907 ps kK,14 t 17 3 ?I9 '? t 39t 32 2t9 ,4 o2 t

3c ,. 0 ;*;E 90

IS 5 t 9 11 3900 t 390 3 22.0 2 708 3", R80 E.K*A ,

lb is 3 I 1 3867 1 3367 32 1930 '4 -,:47 So SnaG $(A** R7 o 52 l 3'414 t1. 3514 32 210 , 29' 3.2 It0 "*K.k. 9 '

14 8 ? 34 xl 3G8 11.3068 32 2233 24 722 3C 3380 i**** 9 .9.9 .3 56 i ik8 1 t 3ilS 32 22t 2417 t4 36. 9220 .* 9 4 3S20 jS3 tI 3066 i 3 0e)6 32.2144 24 **0* 3 320 *m 9

it 20 4 1i 2Q43 it 2943 32 22x4 24 .7524 3' 300 atlt a j22 1 51 i 2939 t1 2939 32 21? 24 r394 36 3480 ****4 9 9

23 22 53 iL 24 11.24 32 2324 24 779 36 3080 tgns 9 '?4 3 35 It 206 it .2606 32 2239 2 4 0 36 4907 S*x 9 9 025 24 57 Ii 2652 11 2652 32 2169 '4 702?2 16.4860 *4.*9 ' 0

26 25 55 i1 2598 it 2598 32.2212 24 7086 36 4880 *sa 8 0 0.?7 '26 52 11 2454 11.2454 32 233 4 224 73229 36.4880 **

28 2S4 It 2588 t1.2q68 32.2212 2 4 7225 36 4880 As29 28t S36 11 2980 11 2960 .32 22153 24 7-316 36. 4880 Itz*-%*930 29 58 11.2475 11.2475 32.2303 24 7507 3o 4880 A*1* 9 ?

31 30 55 It 2401 t1.2401 32 2363 24 7520 36 4880 .14*2 8 8 032 31 S2 it 2400 It 2400 32 2361 24 7664 36.480 1*** 9 933 32 54 %1.2400 11.2400 32 '36 24 7771 36 4880 A*,** I34 33 55 ii 2400 11.2400 32 2352 24,760S 36.4880 4***1 9 9 339 34 S7 it 2400 it 21400 32 22348 24 7671 .6.4880 4*.(* ? 02

S, 35 59 i 2400 It 2400 32.2344 24~7734 36 4(480 ***9 9 037 36 56 It 22400 i 20400 32.2340 24.7705 '36 4880 841 4 13

37J t 148g8 t 1 408 .- 2436 24 773 6. 48S :*.4* 9 Q 0Bi .3a 1 -4 1240 4 4M 2.73t 488 9 9 0

MAXIMUMl DEPTH 38 C365T = 39 '348

* '1115

*

Page 124: DATA VALIDATION AND SUMMARY FOR THE NRL REMOTE … · For several years, Synthetic Aperture Radar (SAR) images of the sea surface revealed planar signatures which were remarkably

DEPT blN AvERAGED 0rr , 7.-

3TART TIME P3 ) 0 7

P!-)'t17'. N 40) 4q OhNSTA NO 7.. ,W NI) ., 1,4Sr NO 2 fPl NU?IN SIZE = i OM DZPT4S T2P = 0 'm, EfITTOm = t,)O OM SURFACE PRF5 = t DeR

BIN DRAR FAST-T ACCUR-T SAL SIlMA-T CCNM) QFL ,4( P,- I NTS , N 5BNa I)EG-C T)E(G-r PPT G/GM**3 Mml -- M M/'SEG TOI'L (J5ED 41iLD

1 46 Ii 5600 it 5600 32 4030 24 6783 -3 C91 t***E LO .132 I33 t 600 it s0o 32 4012 ?4 6822 36 9 i97 KX 9 93 2. i5 It S92 i I 592 32 386S 24 b762 _A 'i3 *t* 9 9 ,4 3 57 it 5400 it 5400 32 3997 ?4 0"74S 7 *9td K* 9 . J53 4 52 I' S400 L1 3-S400 32 993 24 h986 3- I I 9

6 S S; 11 q400 i1 5400 32 399 24 702 36 0tto 4(Ak*A 37 6 53 11 .400 it S400 32 ,398 ,. 2)4 3 ?i.) 0.: 9 18 7 5S it 5400 ti 5400 32 39890 24 71b 37 .t1t3 =K** 9 99 8 56 it 5400 ti 5400 .32 419 24 74S% 16 94.2 ** 0 . ,

20 9 so it 5400 it 5400 32 4474 24 7o,3i 36 qA23 ?*,* . 9

t 22.34 ii 3400 t1 3400 .2 s7fl) ,24 7890 37 q9,.0 * 0 a 812 t S1 Ii 5400 ii 5409 32 4854 24 05 37 120 **,** 9 9 023 2.53 it 5400 t I400 32 ;28 24 A31.? 37 1397 K 9. 9 9 ,2t4 13 S7 11 5400 1t 5400 32 3443 24 954 37 I3t. *m*** 0 4 ,

7 14 52 11 5400 t S400 32 '.;S99 4 967i 37 253i7 ;g.lm, 9 0

28 2.5 11 49 11 5490 32 59t 4 9567 37 )92 A)M*A*M a 329 19 52 ,1 ;4900 11.9400 32 079 24 39106 "37 Wt30 9** 1 9 9 ,)

20 29 5 tI 540 ii 5400 32 6076 24 9652 37 (190 ** * 9 9 x

9 3 S 11 54 11. 3400 32 4918 24 94254 37 .130 , *W 9-".'

30 19 se It 5400 i 5400 3, 3897 24 9295 17 1120 *,*v 9 ?

3 3 S 1t.4 t.55400 32 3919 24 9791.37 .330 .ft=* . 9 034 3.55 ti 4920 .1454 32 .0903 24967 37 i3% ,.1*1 9 9

3 24 5t ii 500 It 5S00 32 58R9 24 9951 37 i 330 ***** 9 '9 r

a3 35 5 it 3460 11400 32..156 29.0170 "7 130 ,*** 9 9 ,37 3 5 It 5600 It S400 32 02 L4 944 37 i330 K*.** 9 4 "-

25 3,7 4 tl S400 it ;400 3P '-98 24 9421. 17 t.301 .,2*7

38 37b 53 It 5600 1.t S4 32 499 24 96931 37 1530 -** 9 9 1

28 27,4 $ it 5498 It 54980 3 2 59736 24 ,9567 ,37 1320t .*,(x ? a9 ,

39 3 59 i3 560 11 -0 32 ,049 P4 320T3 37 t330 *?** 9 038 37 S2 11 .500 it S'S i 3;3 -9q 24 98 37 1 5-3 0 (*** 9 9 J ,.,

40 39 S7 '1 5;600 Ii SOO 32 6039 2 0205 37 i.30 :** 3 9

433 40 S4 I i S600 it.5n40 32 0d.S 2 22 3 :.

S4-

4S 50 it 5600 Ii 500 32' 6039 24.9480 3' i.30 *** 9 9 .-s43 42 32 1. S600 11 S600 32 0

20 24 ,?449 S7 LS.3I 1) . 9 3 3

44 4.3 54 Ii 5600 i SnO)O 32: 6.123 ,25 0276 -32 ;5- 30 4((( 9 .3 145 44 59 it 5600 it.S600 32 .01. 25 1432 3) .30 9 9 0

46 4 53 it S600 it 5600 32 O01S 2. -0-45 004 '37 I., 9*.** R847 4S 50 .1 600 it 5600 32 604. 2 9 Ii? 37 153) 9*W.* 0

40 9 47 t2 i 5600 it 5.00 32 6007 2s 029 37 q3) **** 0 ,

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S

116

42 4 S it 600 it , 00 3- 6 3t 1 o4 0 413 0 0(4 *_

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Page 125: DATA VALIDATION AND SUMMARY FOR THE NRL REMOTE … · For several years, Synthetic Aperture Radar (SAR) images of the sea surface revealed planar signatures which were remarkably

- - - - - -- - - -- - ---- - - -- - - --,- - -

-r P , t .'T , , ".r 0i

-l.N S,2E = -. - - -- - -- T- - --- * , -i , - ,- : * - , ..z .14- -- ,-- - - - -' 3 .- -X~ - -, 2 - -=1 -' i, -" -- -- - -- - -- - - -- -- - - ) 3 1 -m tt - - - --

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17 -52 13 A 94 '4 ; 4,1 2'.4 , -.- cll

1'.. m- 7]I * iT = 47 i.

2 1 ? q4r S.'6 '4 -.i-- S4 0 0 1 71 1.

-ci ;41 L , 4 -).- 4 '. " 1)a w t A '9 I*

22 ,1 s i 4I; l

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37 .5 , ;400 1 "410 5-' 40 '-4 ','1. %*A'* 3 "

30 373 1)40 I0 0 -'49 A * 40 1 o

S9'6 A6 r) 3-1 1i j~, -7 '10 '4 1,5i 1.41 'KA O

40 39 9?5 t ' 14o0 Ii 60 341 - '-9b '454 , , it..3 7 39 tt*.**-

1104 4 3 1 1 1 ; 4,) .1 0, o A - i

31, 4 3 4 ' '60 404 4, t~! %a ' ' 0 .t0

-' 45 qc I I 40 0 1 .0 3 0 4 0 -1 ii,' 4 *2,1

4S 47 3 1i 34.0 1 5411' 0 - S'3 -4 3 l?? i. -, .* 0

4? 39 56 tl q64,) 0 1 3-4 0 p5 . 9~~''c ij, -I-f 3 t -i A 1

41 4 4 t-? Gd I . 4> -lY 4 i- 3)P .

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4 4 11 4 A.

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13 Sci 1, 7,74i i, 3c)j 32 '00 '6 793 1SsI-z 10 i9 93 () 'O 4x 4)0 'A 0r 1 -I

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MAXZMIJM .3;t ri I F 7,' a 03-iM

117

Page 126: DATA VALIDATION AND SUMMARY FOR THE NRL REMOTE … · For several years, Synthetic Aperture Radar (SAR) images of the sea surface revealed planar signatures which were remarkably

CEO P~ O 49-'G& TD JT4

t.AuT 7mtT 1, . R 1i H 7 0QST. .N 40 33 T r, 4: J- -

S4 Nf0 7, ,.>W NG 31, N, "' G *,EOlIN SIZE = '3)M DEPTHS To p 3' JM. po7:a.M .= '0 JM h SuRFACa PYm t , lijbP

EIN DBAR FA. ,7-T AC 'LR- T SAL S. rmA-T 0ND -YEL =C P r) I ', . N

NO m DEG-C DO;-C 0 T ar tl*3 raM, tM m, sc;,c T'j. ,

,: M 4 L-

1 46 12 14 00 2 1400 11 9986 34 283 37 a320 mt9* tO I)2 5 S3 12 1400 t2 1400 71 9981 24 ':'9 s7 333 **m3 2 3S I2 1400 J.2 1400 31 997'7 24 i :7 .)O 3 E*** 9 t4 3 37 12 1400 12 14t0 31 9 9 77232 3'7 0 3 U13 4 38 :2 1400 12 k400 31 Q9 9 4 :7,2 37 l.3P I *, 41

z 5S3 12 1400 12 1400 3: t Q'19 '4 917q3 - 1 324 n9**D 3 2 1400 2 o4 01) 3t 999: 4 ,!F9 '7 ),S-t 4t l

' r, L2 13997 12 1399 321 0,:7 4 "; S 7) 1 3,81 *:Xn%* ?'1 3,6 i:2 i337 12 t 337 32 )094 ,4 1)74 32 411) $(*.a *l 9 7 0

"0A t.2 149 t 1249 3. 394 , 212 37 440 fla * d

1 3C;4 12 12 00 :2 1:200o 5" 2 6 ) -4 Qd~ ,3 ;7 4"? z 0:1 Si 1 2 :200 t42 1200 72 - 4 7 4' 119 -I - ).. sa*i 1

123 ',. 1200 '2 1216 0 32 1 . 4 '4,;9 3t,S 4 74 .. 1 1200 t2 201 -3, 3;,4 '4 7I; '7 ', 0 t ta AS

L S 4 ,? t ? :200 :2 k2'0 :2 :, 4 47 , 7.q 9 A

2: '3 So :2 :200 12 2 00 "; 394 4 ,"'t 3)9 54'' 1inS 7 4 1

It '0 ,' 12 1 400 :- 1 ,0 ". 91 . '4 Z!. sI , ' )i.3* 2:3: 12 :g0 1.2 :2107 -, H 77- 37 x, **It-

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.70 14 1 384 51 9,3 '4 ' 7 0 '10 tst'tt ;'2 :2 :247 12 4 ,i 3: 47 34 ';"9 ", 1,0 7m,-6 7 152 .

S3 272 3 32f 37 49* 34S c ii 7 1j ~A* '4-4 33 :2 1.?99 12 1299 3: 9901 4 3 7 spO si,€ A J3

Z5 24 ,7 :2 1268 12 1208 32 0013 '4 184 37 0320 * i 9 ?

2o 'S -5 Z 2 124: 1 2 t241 32 )022 24 7794 17 0,. 0 **I* o ' a

-7 32 54 I; - .2 0 D k 0 -5 2 )0 9 4,- 4 t ; -i l j7 ;).3;'; . 9 ,

27 . 2 S2 :2 k22 32 002'"? 33 SS28 34 3 :200 i2 1200 32 0049 '4 394 T7 '0 t.ut 9 919 s1 ,b :2 12o0 1, 1200 32 004s -. 4,? 37 io n.i, 9 ' J30 29 r8 a '2 i2011 12 :200 32- 3104 1 2-t4! 4IS 37 032n **tsi 9

30 35 S 12 iJD :2 :200 5 2 :'0037 '4 5~ )7 1'. -- 1 0:)3p 52 i O 2 120) t2 :200 32-11 003 3 214 4 193 3-. 0"10 t~

33 32 54 2 :21)F .2o 20 ~20029 24 413 11*54 37 31, 4L34 33 55 12 1200 12 t.20?0 32 ,002 24 433 17 0320 **lA 9

* 38 34 S7 2 :200 1,, 200 32 002: 24 4,.14 37 1,,.3 Ait** 9

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38 37 3 1 1200 t2 '013 0 32- 0o09 24 4491 o' 0n1

*4*

118

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.-- -- - -- -- ~ - - r f r .-- - -- - - - -

7,k 7:MW k , Ins & , 7 , 4 7. '. 4 ,,-

S, TIZE i m DEPT,,S 3"1p )m -- ,r' , " ,;

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4 3 7 i2 4400 1. 4 0J 3: ,39 24 - - ' S'OL * .0 4 :;a '2 4440 344.: I i. *~ .*79 , 1 j A I

3 3 12 4400 12 44.)J 3' a 7., 24 0479 1,** 1 .,6 3 12 4400 1,2 44 1)0 r1. 72 24 ) 9I 1, 9 *.*

.3 7 C3 12 4400 12 4400 3 i . 3.1 0935 31 SX'0 *4*44 1 4 '9 a 36 12 4400 1.2 44 00 L Tx -). 0:.4 2" '31 37 11 I) 14.9*

10 9 SP I2 4400 t2 .4400 9 ., 0 24 14146 3 t'1

**)A 9 , 0

I1 10 1 4 12 44i)0 t2 4400 3!' "-% I K*4.4 .1 4 1

t :2 x t I 1.4400 1 2 440a0 3, -3 19, 34 1 35 77 1 1' 44044*X 9 9;13 12 55 12 4386 12 4781, 1. A o,) -4 ,232 p;, :, :* *A 4*4 13 G7 '2 4274 12 127.4 '.; r 24t 1)41 ti) *44 '5 51: 1.4 S9 1 4200 12 4200 13 i,10 24 '44.1 ,' 'IJ *444* 4

lb 13 r6 12 4200 12 4200 31 a306 24 1 02 17 1 :10 **Sk*A . A . ,17 3S2 t2 4200 12 4200 It 32 '4 .S34 .7 , i; *(.*s*;%* 9 a 5 .

* l8 17 54 t1~ 4% 1' 1,0') 1r 3283x 0 4**5 4 .9 tO So 4..0 t,_ 4,-00 u 4 I4 4 37130 4 * 4 A

20 19 3a 12 4200 2 123 3t q290 24 1or, 37 i'20 %x*44 4 0

1 20 S4 12 4200 12 4.300 31 ,526 24 t7,49 i7 . '.20 444.* 8 ,22 Sl 5i 12.4200 t2 4200 3 32S2 2a 171., 37 4..,23 44,l* 5 )23 22 5.3 t2 4200 t2 4200 i iA278 24 '771 37 x120 4 .4 9 -524 23 S 12 4200 x2 4200 31 @274 24 1890 37 t120 ****X 9 9 025 24 7 12.4200 t2 4200 31. 82170 24 1928 .37 1120 4*4 9 9 0

26 2S S 12 4t98 1c 4t8 Si &2be 24 1897 37 120 44.444 3 127 26 32 k,2 4174 12 4174 3t 3235 24 1974 37 k x1O 4*AA 9 9 328 27 ;4 1.24145 'P 414r 31 8305 24 1965 37 tt20 4*4 9 9 029 28.36 t2.411 V3 2. 4tt 31 8.327 24.2289 37 ii2o .9**: ' 9 0 030 29 38 12 40R6 2 4086 31 2347 24 2144 37 W20 9**41 9 ? .

3t 0 55 1 . 40;8 12 4058 3 1 4367 24 2423 7 1120 .* * a 3 032 i 2 1

. 4030 12 4030 31 R387 24 2303 37 1120 9** 9 9 0

33 32.54 12 4003 12 4003 31 841)6 24 2486 37 t1.20 *4* 9 ? 034 33 55 12 4000 12 4000 31 8404 24 2472 77 11.20 (**** 9 9 035 34 7 %2 4000 12 4000 3t i1400 24 ,254 37 I .20 *** 9 9 0

36 35 59 12 4000 %2 4000 31 3396 24 2666 37 tt2O *4*4 9 037 36.56 12 4000 12 4000 3t 8393 .4 26k8 7 1:20 ;o **** 13 0 138 37 53 . 2.4000 12.4000 31 8389 24 2649 37 t120 *4K** 9 9 3 5

MAXIMUM DEPTH OF cAsr = 38 J2M

119

Page 128: DATA VALIDATION AND SUMMARY FOR THE NRL REMOTE … · For several years, Synthetic Aperture Radar (SAR) images of the sea surface revealed planar signatures which were remarkably

r]

I,

FN:.' 3 E ) !3 Tl5m-M Im

iTN DbAR ;' - I-T T , .4z T C 1 - T D t7No 'O .g-c i;-E. G -( I, -m - - , ,:,

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33 7 3 26.)0 "3 2,0' j 1 %7 ,, 4, K A4 3 57 13 2 73 1 AA al

3 3 S- 13 260) t3 .''J 3: " )7 1 a t./

10 s 1; 13 NJ 1) 1. ) -' I It t,'. 4; mI7 6 153 13 41.41 1.; '643 1 1 ,o I it ;7 3-1 SA~ tint A I. 7 55 t3 2734 13 2734 31 97 -2 77 ", , *** -

a 8 6 13 S .53 13 275"i3 3- , I , ,9 !" , -;7 t S I

J.0 9 5 13 2622 i3 2622 -1 4 ,l2 ' - 61 7 6:' , 9*5.5*

tO iB 54 '3 206') 13 ' 300 31 .134 '' -47n -7 "15.54 1

13 1 5 5l; i3 60) t3 mo "11 ,1 ,7 5*5

34 nO' S 5 .q Q -5,, ,12h)1 1aaA4 13 60 132 ,0 0 3: 2O'.

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is 1 :413 202 i 2022 '1 *1. -11- *5K**

21 20 54 13 i,,U0 1.3 16:3 0 31 62t8 23 ; t*

MAXIMUM DEPTH 'F CAST = 21 )IM

'III

120

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Page 129: DATA VALIDATION AND SUMMARY FOR THE NRL REMOTE … · For several years, Synthetic Aperture Radar (SAR) images of the sea surface revealed planar signatures which were remarkably

D,PTH k;-Lyg',, CTD DtA

........- ---------- -- --------- ---- -------------------------.. .------------.. . .......... ....... ........*.START T:ME ,9R8it 577 Pfli37flN, 4,3 ;Q;N 10 ';Y 2 I 1w374 NOF 7 .. 'w O5,': Nf , 40BIN SIZE = )M DEP]'4 3 3P Om . OTOM -10

P, r JTRFACE 'RES =

BIN DBAR FAST-T ACrLR-7 SAL :5 ".A- T 20ND VYEt 4) P 31vT/P I N

SN 6 0&G- C WG- c OPT , .s X3 mmrm m/ .-;E,: -r t*ft llFT, WILD)...............................................................................................

i53 2 t0 1 Z000 32 1h 3n u30 3 n 4.1* 3

2 SS 12 794 1 n 33 t *?4 4-4 37 3a0 gS 4 P 9 44 3 S3 ii 7800 it tIQ7 12 1428 15 4 o44 37 3343 ,A - 9S :4 58 ii 7433 1 9401. 32 5334 34 -34 37 3.3a0 4a %A 0

t i 3S 1x 4600 tI 7A4.0 32 ,<120 34 9009 37 3340 litSa 4 0a2 7t SS 1 7947a 11 7947 32 ah70 ,724 29- 4 ; 40 a **s ? 0oi

9 a. S 11 7400 1 74-600 3? 631 .4 8446 37 3340 *44l A aiS 74 ' it 7400 U 740, 3? -C? 7'2 34 37 3340 A 0 . 9 0

It to 6 it 7400 i1 7443 32 ,3J0 14 3,919 57 j340 4 4 .3 p20 i92 i 734- O t 1 7401 32. ',1314 24 -17 1s 37 3.346 cass 4 31 "7 34 11 7400 1'. 7410.) 3 2 4 4 ;Q34 37 31340 t.SS* g 0 3

1i i5 6 t 7400 1 - 740 .7 ,32 1 24 90 3 " 7 3340 9****

V 17 t 3 1 i2 11l 00 1i 72900 3? ,j4 I . 4 I 4031 37 3 340 4 .*1* 9 A, 3S

24 23 4 i1 7200 7200 32 43 4 47 37 3340 15 5*19 9 923; 24 7 it 7200 lx 733Q) 3? o4

9 ,.4 165.) 3 7 3340 5.,54.4 o 9 0

26 253 5 72.00 1 0 3? 643 8 4 9o80 37 334) * 0 8 027 .9.6 2 it 72,40 ii 7490 3?2 o'3 , 4 "q6, .7 3340 4L* 9 4A 028 27 34 t7 L 3 i, 7200 32 , 47 , 4 4231 37 3740 ;4 * 9 9 ,

3 2851 it 7:560 it 700 32 o443 1 t ,~3 3340 s** 6 3

30 29 0 11. 7200 it 7200 32 4,38 4 9447 37 3340 Al0IA

2 1 -I0 33 it 7200 It 7200 32 64 4 24 9 .12 3. 40 .9e,80 37 3 0 o32 31 32 I % 7155 x 7135 3, 0479 ?4 983 37 334f) i5A* A 9 9 033 j7. 54 11 7300 11 7200 12 *,n 35 014 ? 3 37 33s4 r .*4* 9 9 034 32 58 ii 7289 it n

089

3? 6938 34 0714 37 32i40 K**4* 9 9 ii33 34 37 11 700 it 690 12 -,77 2 i1 37 3344 sa 0 9 0

36 3159 t.. f0 ii 6800S 3Z2,71 .2 03653 37 3340 *1*4 9 9 037 36.3 6 . 74.3 .,243 3? 1- 1i02 ! 0514 ' 37 3.40 1114 A4t A 0 038 37 53 .I I M97 iS t39

7 3 o937 ,23 0686 37 3340 ***A* 9 9 1

39 3 8S t3 1.I 4 1 644 j6447 3, 7713 23 18io 37 3340 9.4** 7 9 040 39 32 1 1 . .4) o . o4650 32 704, 2s 0 1J4 37 3340 t***l 9 9 0

42 16 306 tt.200 It 5300 .1 /743 .17 1aG 4 3 ,7 1 540 *#** 9 . 0- 373 433 1 1t. 200 i ,h50 .2 7,37 I 'S L66 3'7 .3:,I *.*. 9 9 044 43 C4 11 o 4 t 3 4 Q , , q .186 3/ 340 ili3.*4 7 as ,43 ,4 3 1 . 60 9 t .409 52 7' 4-" , - 314 I*U . *4* 9 04o 4 S3 it 38423 l it 43 77 '4 1 i t 5 7 14 4 13 9 1

47 't3 S0 I. S440 i1. 46:30 ' 7.) L. ? 4 33 3t -4n.1 *) 9

48 47 ? 1i ;o0)0 t 13600 '_ 776, 2q 2jj' 1*4 ,, 9 ...

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MAAMIoio 1Pr0 7 Fi -F,.. = 33 -#.1

121

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Page 130: DATA VALIDATION AND SUMMARY FOR THE NRL REMOTE … · For several years, Synthetic Aperture Radar (SAR) images of the sea surface revealed planar signatures which were remarkably

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1 2 68 1 a 3,6vt 1 R 371 3,3 ,°,182 23 45, o 44 1Ca 3 '79 7

2 3 39 13 3482 t 8 3482 33 t61t 23 8q77 44 t179 57 5 4

t3 4.17 1, 3113 19 3113 33 ;l174 ?3 8716 44 '343 2. 46 3 04 5 35 1 a 2i 3/ 1 2363 33 212.S- 23 89728 44 001 1 03 5,5 6 3t 1 , 646 i -1. 6h 13 2 20 2 23 "-PO0 41 '9694 t8 1 7t 20

29 7 91 91 1.7 9S9 33 t980 23 9976 43 7446 ., 41

K 9 23 17 3822 1.7 3822 33.235S 24 '357 4.1 237,, 34 '4 . -9 tO 30 17 2, 17 ,m 3"3 2328 24 1tAo 4.3 Q.41 -t 3

to it 36 17 0790 t7 47Q9 33 235B 24 2179 4,? 9487 38 St -7 ,

i1 12.28 it. 9028 '6 ,9029 33 2394 P4 266 42 79S2 49 ,3 4t ,12 13 32 t6 4169 1.6 4169 33 2157 24 3632 4" 3Q67 32 -'2 4r313 14 4 kS o32 : ,325 "33 2711 24 ;899 4. t4 34 .8 " J14 15 29 15 2688 tS 2688 33 2844 24 6836 4' 313 3 3 4I1S 16 34 is5 loit I GS i I, 1 33 -500)0 .4 7391 4,, 1 47

'1 ,2:9 3

16 t7 27 14 8809 t4 R809 33 3±80 24 79A7 40 9,97 4,3 -17 10. 31 14 i,-3 !4 r, S3 37 301- 24 8424 40 7399 7 S18 19 37 144358 t4 4358I 33 2953 24 8937 40 SiRS S;4

20 27 %3 ?271 "3 92"73 33 ?a69 24 9497 5' -8 34 .,0 2: 29 t3.0197 t3 Ji97 33 2480 25 iS70 39 t6'8 6, 48 4,

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2 24 28 12 013S V2 0835 .33 479.3 21 53t 4 ; 32"1, 46 3524 2S 38 12 3228 12 0228 33 9i29 2q 37t8 38 3625 '6.5 26 30 11 9980 :1 9F0 33 .209 '9 q871 38 .878 34 18 o ,

26 27 28 it 95i5 i1 97s.s 33 5276 2S.607. 38 4524 46 ,9 -,

,?7 28 0 It 9310 i1 9.30 33. 537t 25.6299 3f3 4455 ro ,3 4a 3'8 29 33 t: 8960 1.39603 33 5404 25 0355 383 4151 3 5: 4, ,"9 30 31 11 8;2? 0 1 8520 .33 9497 2S 6372 38 3843 43 "2 ,J I30 31 25 ti 3208 11,3208 33.5608 25 679S 38 3672 38 3; o1 )

31 32 29 ki 7844 1 7 64 33.56t4 29 6949 38 1415 ') 3 4, 033 3 it 7440 11 7440 ,3 C794 25 71.3 3 31.60 49 4o o34 .4 11 70t9 it 701.9 3 88S 2 738 3$ 8167 4 1.3 -;q

34 35 3' 11.6337 t 337 33.S994 2S 764t I F 23;q 46 7 00 k3S 36 32 it .S685 ti 3685 33.6178 2S. 7909 .38 1940 49 4 49 0

36 37 30 1 5380 il 5380 33 63S5 25.8193 38 1842 C5 C6 4," 037 31 31 tt.5.242 it 3242 33 6415 25 R293 38 iH7130 7 'S4 4i3 3

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41 42.34 tt Si33 I t 51S3 33 65/4 29 8654 38 16G76 1 1 3' 04 43 32 it siso 1.1 350 33 6638 2S 8776 34 1943 le 43h S1343 44 .2 5 ,t '3149 ,1. 3149 33 646 ,5 1,871 8 i19s '0 4 ,144 45 31 it 5146 it -,14m 33 6696 2S 0849 38 2007 8: 39 31 145 46,736 i 134 xi 534 33.677o 25 i)3. 3I8 20H) n3 49 44 a4h 47.26 1 5139 it 5139 33 t777 23 9007 3R 2092 7' .4 047 48 29 11 341 xl 0141 33,77 25 ,?14n 3i a'O 9413 49 3P 11 51.40 t q:40 .3,3 6/'7 2S 9226 38 i')2 91 34 3 049 90 38 11 3)44 11 3144 .5 67Ht 25 '3'?7i 3H 2113 " 1' 43 0sl3 51 27 tl.5S4S i 3145 33 6780 2s 9250 38 2'17 2q tO7 76

;i '2 26 i1 3t44 11 7144 3.3 6777 2c; ?9P4 i31 2'.17 7: 43 39 '52 33 34 tl 514 t! ;14 5 33.677q 5 933' 38 ,2' ' 4 77 .33 34 34 L3 ' 4

9 ii I149 33 477., 25 "y401) 0 1;) .,0 '11 7,

54 55 37 t1 q149 1) 5j49 33 6771 2 946,? 38 r:. a'' - 8"

3,, .5 9 it 15i4. 49 3149 33 .',77; 2 ' "486 48 3 lR ,

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MAXIMUM P)EPTH O'F CA';T : , '''

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26 25 79 1j '477 it3.477 1t 2 ?'8 '4 68'4 .33)24 39

49 74 I27 2 90 at i ,.4 1 1 1 94 o6 2 267 24 .- 0,

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39 34 82 1 t,S, L 46 n 32 497 24 7240 36 894 39 2 44 0

3I 35 83 ti t9S4 6S54 32 2696 24 7143 36 894q '38 40 99 0

MAXIMJM DFPT OF :,.A; = 3 It -I

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Page 134: DATA VALIDATION AND SUMMARY FOR THE NRL REMOTE … · For several years, Synthetic Aperture Radar (SAR) images of the sea surface revealed planar signatures which were remarkably

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2 1 20 833 1 3350 i C 7r 2 "l:,i 44 74"3 36 ;" LI5.322 n 70 1 1 2-3n3 Ii 23168 32 91 4, 3431 0

24 36 3 t 235 t I = 3. 1S 32 3688 24 77S 10 5343 1 17 1 225 S 34 70 1 1 2402 iL 240? 2 3 2''S ",4 '9)8 36 3732 2"1 1-28 9?2

* n 25n x 93 ti24 32 4247 1'sC 3 7258 19 1 "t, S* 7 26 74 1t 312 3 xi 33123 3? 4c8 '3 1)4 3 : lR. 1. 72 14 .3

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3 1 30 80 11 4121 1i1 43.23 32 5 734, 24 99r06 16, %7S 40 9.3 1)

*MAXIMUM DEPTH FW CAST =31 m'

126

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Page 136: DATA VALIDATION AND SUMMARY FOR THE NRL REMOTE … · For several years, Synthetic Aperture Radar (SAR) images of the sea surface revealed planar signatures which were remarkably

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M

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APPENDIX C. ?LOTS OF XB7 DROPS

All the XBT's were hiand digitized from the original charts and then

replotted using the standard temperature and depth conversions of the

Sippican Corporation, Marion, M.ass. Drops 7 to 36 are included.

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.. DISTRIBUTION LIST

Naval Research Laboratory4555 Overlook Avenue, S.W.Washington, DC 20375Attn: W. Keller, Code 7910 1 cv

Naval Research Laboratory4555 Overlook Avenue, S.1.Washington DC 20375Attn: W. Plant, Code 7910 1 cy

Naval Research Laboratory4555 Overlook Avenue, S.W.Washington, DC 20375Attn: G. Valenzuela, Code 7910 - cy

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Naval Research Laboratory

4555 Overlook Avenue, S.W.Washington, DC 20375Attn: J. McGrath, Code 5810 1 cy

Naval Research Laboratory

* * 4555 Overlook Avenue, S.W.

Washington, DC 20375Attn: W. Garrett, Code 7910 1 cy

Naval Research Laboratory4555 Overlook Avenue, S.W.Washington, DC 20375Attn: L. Galli, Code 5004 1 cy

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Naval Research Laboratory4555 Overlook Avenue, S.W.Washington, DC 20375Attn: D. Chen, Code 7910 1 cy

145

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Naval Research Laboratory4555 Overlook Avenue, S.W.

Washington, DC 20375

Attn: D. Schuler, Code 7943 ! cy

Naval Systems Research & Development Center

Bethesda, .M 20084Attn: R. Lai, Code 1568 1 cy

10S

Brook RoadWormley, Godalming

Surrey, GU8, 5UBAttn: N.D. Smith 1 cy

NSTL StationBay St. Louis, MS 39529Attn: P. Smith, Code 335 1 cy

Scripps Institute of Oceanography

!GPPLa Jolla, CA 92093Attn: R.H. Stewart 1 cy

Naval Research Laboratory4555 Overlook Avenue, S.;.

Washington, DC 20375Code 2628 22 cysCode 5810 Attn: J.A.C.Kaiser 22 cys

1

146

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