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OCEANGGAPHY 


SSO i a <a 


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


The Sponsoring Agencies are: 


Atomic Energy Commission 
Bureau of Commercial Fisheries 
Coast Guard 
Coastal Engineering Research Center 
Department of the Navy 


sence Services Administration 


tion Control Administration 
gical Survey 
ucation & Welfare 


cience Foundation 


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NATIONAL OCEANOGRAPHIC DATA CENTER 


CATALOG SERIES 


COMPUTER PROGRAMS 
IN 
OCEANOGRAPHY 


Compiled by C. DINGER 


PUBLICATION C-5 
(Second Revision) 


1970 


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ACKNOWLEDGMENT 


The cooperation of the individuals and organiza- 
tions who contributed program abstracts is greatly 
appreciated. 


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DISCLAIMER 


This catalog is mainly a compilation of informa- 
tion voluntarily contributed by various individuals 
and institutions. The National Oceanographic Data 
Center cannot assume responsibility for the accuracy 
of the abstracts or the proper functioning of the 
programs, except for those originated at the Center. 


Any information to correct or update the pro- 
grams in this catalog will be appreciated. 


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CONTENTS 


Introduction. 
Sources of Information. 
Program Abstracts, by Category. 


Biological Oceanography 
Chemical Oceanography . 
Data Reduction. 
Editing and Special Input /Output . 
Geoscience. . 
Geophysics, Mesinen : 
Sediment Analysis and Meehenies 
Graphical Display . 
Mathematics, Applied. ato 
Curve and Surface Fitting 
Mathematical and Statistical iaeiinsiis 
Navigation and Charting 
Physical Oceanography . ¢ 
Air-Sea Interaction and Heat ‘Budget 
Currents and Transfer Processes 
Ice in the Sea. SEL CHG Gis we =o 
Physical Properties: Analyses and 
Summaries : 
Physical Quantities, iConputation ‘of é 
Sound-Ray Path. 
Sound-Normal Modes. 
Sound-Speed Computations. 
Tides, Astronomical 
Waves and Hydromechanics. 
Retrieval of Ocean Data . 


Index by Agency or Institution. 
Index by Programming Language . 
Index by Computer Make and Model. 
Computer Program Abstract Form. 


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INTRODUCTION 


This second major revision of the National Ocean- 
ographic Data Center's (NODC's) catalog Computer 
Programs in Oceanography is issued to foster awareness 
of computer programs related to oceanography and to 
facilitate their exchange between interested groups. 


As in the first revision, the material is 
arranged under subject headings, with each entry con- 
taining the program title, program language, computer 
system the program is written for, indication whether 
a copy is on file at NODC, brief program description 
provided by originator, and name and address of per- 
son to contact for further details. 


This catalog only begins to reflect the present 
programs originated by NODC for the new in-house com- 
puter. Supplements or revised editions will be 
issued, and abstracts of NODC's latest programs will 
be incorporated, as well as contributions from other 
institutions not received in time for inclusion in 
this catalog. Also, a revised edition of the NODC 
publication G-15, User's Guide to NODC's Data _ Proces- 
sing Systems, planned for the near future will con- 
tain updated computer programming information. 


Documentation on file at NODC or assistance in 
locating a program can be obtained by writing to: 


The Director 
National Oceanographic Data Center 
Washington, D. C. 20390 


Contributors of new programs are requested to 
fill out the abstract form in the back of this cat- 
alog and send it to the abcve address. 


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SOURCES OF INFORMATION 


Catalogs of computer programs pertaining to dis- 
ciplines related to oceanography have been compiled 
by various organizations. The following is a listing 
of such publications known to NODC at this time. The 
Center would appreciate further information about 
existing computer programs for inclusion in following 
editions of this catalog. 


RESEARCH COMPUTATION CENTER PROGRAM LIBRARY 


A compilation of computer programs written by 
Naval Research Laboratory personnel. For further in- 
formation, contact: 


Mrs. Janet P. Mason, Code 7813 

Mathematics and Information Services Division 
Naval Research Laboratory 

Washington, D. C. 20390 


NATIONAL COMPUTER PROGRAM INDEX 


Includes GOSSIP (Geologically Oriented Scheme 
for Sharing Information in Programming) and the 
Rokdoc Package, a library of routines for statistical 
analysis, summary, and display of data concerning 
sedimentary rocks. Inquiries should be directed to: 


Assistant Librarian 
Department of Geology 
University of Reading 
Whiteknights Park 
Reading RGG-2AB 
England 


COOPERATIVE OCEANOGRAPHIC PROGRAMMING EFFORT (COPE) 


A compilation of computer programs in use at the 
Woods Hole Oceanographic Institution. For further 
information, contact: 


Editors of COPE 
Woods Hole Oceanographic Institution 
Woods Hole, Massachusetts 02543 


COMPUTER SOFTWARE MANAGEMENT AND INFORMATION CENTER 
(COSMIC) 


A catalog of programs generated by the NASA 
space effort. Many of the programs are of a general 
nature. For further information, contact: 


COSMIC 

Computer Center 
University of Georgia 
Athens, Georgia 30601 


NAVAL ORDNANCE LABORATORY LIBRARY 
OF COMPUTER PROGRAMS 


A catalog of programs in use at _ the Naval 
Ordnance Laboratory. For further information, contact: 


Mathematics Department 

U. S. Naval Ordnance Laboratory 
at White Oak 

Silver Spring, Maryland 20910 


KANSAS GEOLOGICAL SURVEY - COMPUTER CONTRIBUTIONS 


A series of publications devoted to computer 
programs and examples of problem-solving applications 
in the earth sciences. For further information, 
contact: 


Dr. Daniel F. Merriam, Editor 
Computer Contributions 

Kansas Geological Survey 
University of Kansas 
Lawrence, Kansas 66045 


PROGRAM ABSTRACTS BY CATEGORY 


BIOLOGICAL OCEANOGRAPHY 
—X%—K-H— HK —H—-4— HH — HE 


RYLD»> BIOM LANGUAGE - FORTRAN IV 
COMPUTER —- IBM 1130 
(COPY ON FILE AT NODC) 

COMPUTES THE APPROXIMATE YIELD OF A FISH STOCK PER RECRUITMENT By EI- 
THER OF TWO METHODS (ARITHMETIC OR EXPONENTIAL APROXIMATIONS)» OR THE 
PROGRAM SIMPLY COMPUTES THE STOCK BIOMASS WHEN THERE IS NO FISHINGe 
OUTPUT—— AN EQUILIBRIUM YIELD MATRIX WITH UP TO 400 ENTRIES CORRES— 
PONDING TO 20 AGES AT ENTRY AND 20 MULTIPLIERSe AUTHORS—-— LeVe PIENAAR 
AND JeAe THOMSON» TECHNICAL REPORT NOe 92 (UNPUBLISHED MANUSCRIPT», NOV 
1968).e EARLIER VERSION OF PROGRAM WRITTEN BY Le Ee GALES, COLLEGE OF 
FISHERIES» UNIVERSITY OF WASHINGTONe DIRECT INQUIRIES TO — 


FISHERIES RESEARCH BOARD OF CANADA 
BIOLOGICAL STATION 
NANAIMOs Be Ce 


CHLOROPHYLL PIGMENT AND CAROTENOID PIGMENT LANGUAGE — FORTRAN II 
COMPUTER - IBM 1620 II 
(COPY ON FILE AT NODC) 
TWO SIMILAR BUT SEPARATE ROUTINESe CALCULATION METHOD BASED ON THE 
USE OF 1¢0 CMe CELLSe DATA CARDS INPUT, OUTPUT IS PRINTED LISTING AND 
PUNCH CARDSe AUTHOR-— DRe MALCOLM HAIRe 


INSTITUTE OF MARINE SCIENCE 
ADELPHI UNIVERSITY 
OAKDALE» LONG ISLANDs NeYe 11769 


COMBINED CHLOROPHYLL AND PRODUCTIVITY LANGUAGE — FORTRAN IV 
COMPUTER - CDC 6400 


(COPY ON FILE_AT NODC) 4 2 
COMPUTES ASSIMILATION OF PRODUCTIVITY IN SEA WATER AND. COMPUTES. THE 
QUANTITIES OF CHLOROPHYLL As Bs AND Cs» AND THE AMOUNT OF CAROTENOIDS 
IN SEA WATERe WRITTEN BY MARSHA WALLIN, NOV 19636 BASED UPON TWO 
PROGRAMS PREPARED IN 1962 FOR THE IBM 709 BY MeRe RONAe THE CHLORO- 
PHYLL PROGRAM DETERMINES THE AMOUNT OF PLANKTON PIGMENTS USING THE E- 
QUATIONS OF RICHARDS AND THOMPSONe THE PRODUCTIVITY PROGRAM (CARBON 
14) DETERMINES THE PRODUCTION OF MARINE PHYTOPLANKTON BY USING NEIL- 
SEN'S METHOD. OUTPUT CONSISTS OF BOTH PRINTED MATTER AND OF LIBRARY 
CARDSe THE LIBRARY CARDS MAY BE USED AS INPUT TO A MULTIPLE REGRES- 
SION PROGRAM TO DERIVE A RELATION BETWEEN PRODUCTIVITY AND CHLOROPHYLL 
A. FINALLYs A PLOT ROUTINE MAY BE CALLED TO GRAPH ONE OR SEVERAL VAR- 
TABLES AS A FUNCTION OF DEPTHs OR TO DISPLAY THE HORIZONTAL DISTRIBU- 
TION OF ANY GIVEN PROPERTYe REVISED IN 1969 FoR THE CDC-64006. 


DRe Ge Ce ANDERSON 
DEPARTMENT OF OCEANOGRAPHY 
UNIVERSITY OF WASHINGTON 
SEATTLE» WASHe 98105 


ECOPROD LANGUAGE -— FORTRAN IV 
COMPUTER -— CDC 6600 


(COPY ON FILE AT NODC) 
COMPUTES GROSS AND NET PRODUCTIVITY» RESPIRATIONs P/R RATIO» PHOTOSYN- 
THETIC QUOTIENT, EFFICIENCY, DIFFUSION COEFFICIENT, GIVEN SUNLIGHT DA- 
TA AND DIURNAL MEASURES OF OXYGEN AND/OR CARBON DIOXIDEe CORE STORAGE 


REQUIRED-- 255,000 60-BIT WORDS» AUTHOR-- WILLIAM LONGLEYe 


THE UNIVERSITY OF TEXAS 
PAGE 905 


MARINE SCIENCE INSTITUTE 
PORT ARANSAS» TEXAS 78373 


JOB (SPECIES DIVERSITY) LANGUAGE — FORTRAN IV 
COMPUTER - CDC 6600 
(COPY ON FILE AT NODC) 

CALCULATES SPECIES DIVERSITY INDEX FOR NUMBERS OF ORGANISMS AND/OR 
WEIGHT OF ORGANISMS» UTILIZING THE DIVERSITY INDEX EQUATION DERIVED 
FROM MARGALEFe PROGRAM CALLS SUBROUTINE *tSEASON' WHICH CALCULATES 
SEASONAL AVERAGES FOR A GIVEN STATION, SEASONAL LIMITS BEING INDICATED 
BY A CONTROL CARDe THIS SUBROUTINE OUTPUTS MEANs STANDARD DEVIATION, 
AND RANGE OF DIVERSITY INDICES FOR EACH SEASONAL GROUPe OTHER DESIRED 
GROUPINGS MAY BE ENTERED BY A GROUPING CONTROL CARD. CORE STORAGE NEC-— 
ESSARY-- 50000 60-BIT WORDSe AUTHOR-- AeDe EATONe 


WILLIAM LONGLEY 

THE UNIVERSITY OF TEXAS 
MARINE SCIENCE INSTITUTE 
PORT ARANSAS» TEXAS 78373 


OXYGEN LANGUAGE — FORTRAN IV 
COMPUTER - CDC 6600 
(COPY ON FILE AT NODC) 
DETERMINES PRODUCTIVITY BY OXYGEN DIURNAL CURVE METHODe INPUT INCLUDES 
OXYGEN CONCENTRATION AND OXYGEN PROBE PARAMETERS. OUTPUT CONTAINS NET 
AND GROSS PRODUCTIVITY AND P/R PLUS ORIGINAL DATAs AUTHOR-— WILLTAM 
LONGLEY. 


THE UNIVERSITY OF TEXAS 
MARINE SCIENCE INSTITUTE 
PORT ARANSAS»s TEXAS 78373 


MARINE BIOLOGICAL ENVIRONMENTAL SUMMARIES LANGUAGE — FORTRAN 
COMPUTER ~- IBM 7074 


CODED CHARACTERISTICS FOR SPECIFIED LOCALITIES ARE SUMMARIZED FOR THE 
FOLLOWING MARINE BIOLOGICAL PHENOMENA-- AMBIENT BACKGROUND NOISE, AT-— 
TACHED AND FLOATING MARINE VEGETATIONs BIOLUMINESCENCEs AND DANGEROUS 
MARINE LIFEe CHARACTERISTICS INCLUDE-— HABITAT, PERIOD OF ACTIVITYs 
FREQUENCYs RANGE OF SOUND» MAXIMUM SOUND PRESSURE LEVEL» AREAL DISTRI- 
BUTION OF MARINE VEGETATION, TYPE AND INTENSITY OF BIOLUMINESCENCE 9 
AND CAUSES AND EFFECTS OF SPECIFIED DANGEROUS MARINE LIFEs AUTHOR-— 
ReMe HOLCOMBE. OS NOo 53338. 


OCEANOGRAPHIC ANALYSIS OIVes CODE 3301 
NAVAL OCEANOGRAPHIC OFFICE 
SUITLANDs MD. 20390 


LENGTH-WEIGHT FREQUENCY LANGUAGE — FORTRAN IV 
COMPUTER - IBM 360/65 


CALCULATES LENGTH-WEIGHT FREQUENCY DISTRIBUTION VALUES FROM SKIPJACK 
CATCH DATAs 


BUREAU OF COMMERCIAL FISHERIES BIOLOGICAL LABe 
ATTNe DRe ReAe BERKLEY» OCEANOGRAPHER 

P.O. BOX 3830 

HONOLULUs HAWAII 96812 


BIODETERIORATION PROJECT LANGUAGE — AUTOCODER 
COMPUTER — IBM 7074 
(COPY ON FILE AT NODC) 
MONTHLY AND YEARLY SUMMARTES OF THE RESULTS OF FOULING MEASURED ON 
EXPOSED AND CONTROL PANELSe OS NO, 52272, AUTHOR-- JUDY YAVNER, 


PAGE 006 


DEVELOPMENT DIVISION» CODE 2300 
NATIONAL OCEANOGRAPHIC DATA CENTER 


WASHINGTON» DeCe 20390 


CONCENTRATIONS PER SQUARE METER OF SURFACE IN THE LANGUAGE — FORTRAN IV 


OCEAN AND LAKES FROM CONCENTRATIONS PER VOLUME COMPUTER — IBM 7094-II/ 


(UWMS-1006) 7040 DCS 
(COPY ON FILE AT NODC) 
COMPUTES VARIOUS CHEMICAL AND BIOLOGICAL COMPOUND CONCENTRATIONS AS 


WELL AS PRODUCTIVITY RATES PER SQUARE METER OF WATER SURFACE, FROM IN- 


TEGRATED VALUES ON "PER VOLUME* BASIS. TEN CONCENTRATIONS AND RATES 


ARE INTEGRATED OVER UP TO SEVEN PAIRS OF OPTIONAL DEPTH LIMITS. REFo 


A 31-PAGE REPORT (UWMS-1006, JUN 1966) BY THE DEPARTMENT OF OCEANO- 


GRAPHY» APPLIED MATHEMATICS SECTIONe CORE STORAGE NEEDED- 2231 WORDS. 


SOURCE DECK HAS 771 CARDS. 


He MACINTOSH» COMPUTER SERVICES 
DEPARTMENT OF OCEANOGRAPHY 
UNIVERSITY OF WASHINGTON 
SEATTLE» WASHe 98105 


PHYTOPLANKTON NUMBERS» VOLUMES AND SURFACE AREAS LANGUAGE = FORTRAN IV 


BY SPECIES (UWMS-1008 AND UWMS-1009) COMPUTER - IBM 7094-II/ 


7040 DCS 
(COPY ON FILE AT NODC) 

TWO PROGRAMS» DIFFERING IN INPUT FORMAT ONLY» COMPUTE CONCENTRATIONS 
OF CELL NUMBERS» CELL SURFACE AREAS» AND CELL AND PLASMA VOLUMES IN 
MARINE PHYTOPLANKTON POPULATIONS. ALSO MEAN CELL AREAS» MEAN CELL 
VOLUMES AND MEAN PLASMA VOLUMES AS WELL AS THE RATIOS CELL AREA TO 
CELL VOLUME AND CELL AREA TO PLASMA VOLUME ARE COMPUTED OPTIONALLY. 
THE INPUT QUANTITIES ARE OBTAINED FROM MICROSCOPICAL EXAMINATION OF 
SEAWATER SAMPLES. A SUBROUTINE COMPUTES THE AREAs VOLUME AND PLASMA 
VOLUME OF A CELL FROM MEASURED DIMENSIONS OF DIVERSE SPECIESe CORE 
STORAGE REQUIRED-- 239836 WORDS FOR MAIN PROGRAM AND SUBROUTINES IN 


FORTRAN AND MAPe SOURCE DECK HAS 1211 CARDSe REFe A 93 PAGE REPORT-—- 
SPECTAL REPORT NO. 38 (M66-41,JULY 1936), BY PAAVO Eo. KOVALA AND JERRY 


De LARRANCEe 


He MACINTOSH» COMPUTER SERVICES 
DEPARTMENT OF OCEANOGRAPHY 
UNIVERSITY OF WASHINGTON 
SEATTLEs WASHe 98105 


CHLOROPHYLL CALCULATIONS LANGUAGE — MAC 
COMPUTER - ICT 1301 


CALCULATES CHLOROPHYLL USING THE FORMULA OF STRICKLAND IN *A MANUAL OF 
SEA WATER ANALYSIS' PP. 110-1122 AUTHORS-- AeMe SHIPLEY AND De SACKSe 


UNIVERSITY OF CAPE TOWN 
OCEANOGRAPHY DEPARTMENT 

STTNe MRe AoMe SHIPLEY 
PRIVATE BAGs RONDEBOSCH»s CePeo 
REPUBLIC OF SOUTH AFRICA 


PROGRAM REGROUP LANGUAGE —- FORTRAN 
COMPUTER - CDC 3600 
(COPY ON FILE AT NODC) 
THE PROGRAM DETERMINES THE NUMBERS OF OCCURSENCES AND JOINT OCCUR- 
RENCES OF THE SPECIES IN THE SET OF SAMPLESe IT THEN CALCULATES AN 
INDEX OF AFFINITY FOR EACH PAIR OF SPECIESe THE SPECIES ARE ORDERED 
IN TERMS OF THE NUMBERS OF AFFINITIES THEY HAVE AND THIS LIST IS 


PRINTED ALONG WITH A LIST OF NAMES» CODE NUMBERS AND NUMBERS OF OCCUR- 


RENCESe THE PROGRAM THEN DETERMINES THE LARGEST GROUP THAT COULD BE 


FORMEDs TESTS TO SEE WHETHER THAT MANY SPECIES ALL HAVE AFFINITY wITH 


EACH OTHER AND» IF THEY DOs PRINTS OUT THE GROUPe IF THEY DO NOT IT 


PAGE 007 


TRIES THE NEXT SMALLER GROUP,» ETCe THOSE SPECIES WHICH HAD AFFINITY 
ONLY WITH THIS GROUP — AND/OR EARLIER GROUPS — ARE LISTEDe THE RE- 
MAINING SPECIES ARE REORDERED AND THE PROCESS CONTINUED UNTIL ALL SPE- 
CIES HAVE BEEN PUT EITHER IN GROUPS OR IN THE LIST OF SPECIES wITH 
AFFINITIES WITH GROUPSe LIMITS-- 200 SPECIESe DIRECT INQUIRIES TO-- 


DRe Ese We FAGER 

SCRIPPS INSTITUTION OF OCEANOGRAPHY 
P.O. BOX 109 

LA JOLLA» CALTFORNIA 92037 


CHLOR LANGUAGE — FORTRAN IV 
COMPUTER - CDC 3600 


THIS PROGRAM WILL EITHER CALCULATE CHLOROPHYLL As By C CONCENTRATIONS 
IN MICROGRAMS PER LITER OF SEAWATER AND THE CONVERSION FACTORS FOR THE 
FLUOROMETER USING SPECTROPHOTOMETER READINGS,» OR CALCULATE CHLOROPHYLL 
A AND PHAEOPHYTIN CONCENTRATIONS IN MICROGRAMS PER LITER OF SEAWATER, 
USING THE FLUOROMETER READINGS. A SIMILAR PROGRAM WAS WRITTEN EARLIER 
AT SeleOo FOR THE CDC 1604. 


MRe DAVID WIRTH 

OCEANIC RESEARCH DIVISION 

SCRIPPS INSTITUTION OF OCEANOGRAPHY 
P.O. BOX 109 

LA JOLLA» CALIFORN'A 92037 


NUTRIENT CHEMISTRY CONCENTRATION LANGUAGE - (NOT GIVEN) 
COMPUTER - CDC 1604 


COMPUTES CONCENTRATIONS OF INORGANIC PHOSPHORUS, SILICATE, NITRITE» 
NITRATE» FROM THE APPROXIMATE RAW DATAe 


SCRIPPS INSTITUTION OF OCEANOGRAPHY 
LA JOLLA» CALIFORNIA 92037 
PRIMARY PRODUCTIVITY LANGUAGE — (NOT GIVEN) 
COMPUTER —- CDC 1604 


COMPUTES PRIMARY PRODUCTIVITY FROM ACTIVITY OF CARBON» DURATION OF IN- 
CUBATIONs TYPE OF INCUBATION, SAMPLE ACTIVITY AND DEPTHe 


SCRIPPS INSTITUTION OF OCEANOGRAPHY 
LA JOLLA» CALIFORNIA 92037 
ZOOPLANKTON VOLUME LANGUAGE — (NOT GIVEN) 
COMPUTER - CDC 1604 
COMPUTES ZOOPLANKTON VOLUME FROM VARIOUS TY°ES OF HAULe 


SCRIPPS INSTITUTION OF OCEANOGRAPHY 
LA JOLLA» CALIFORNIA 92037 


PAGE 008 


CHEMICAL OCEANOGRAPHY 
—R-H 8 —-O— FH 


ALKALINITY AND SPECIFIC ALKALINITY LANGUAGE — FORTRAN AND 
FORCOM 
COMPUTER = IBM 1620 


THE INPUT CARDS OF THIS PREGRAM ARE PRE-PUNCHED WITH THE STATION NUM- 
BER» DATEs WIRE LENGTH AND BOTTLE NUMBER», THEN SENT TO THE CHEMISTRY 
LABORATORY WHERE THE PH VALUE AND THE SALINITY VALUE ARE PUNCHED ON 
THE CARDSe THE CARDS ARE THEN RETURNED AND PROCESSED THROUGH THE COM-— 
PUTERe 


UNIVERSITY OF MIAMI 

MARINE LABORATORY 

COMPUTING CENTER 

1 RICKENBACKER CAUSEWAY 
VIRGINIA KEY» MIAMI» FLORIDA 


SALINITY VALUE CALCULATION LANGUAGE — FORTRAN AND 
FORCOM 
COMPUTER - IBM 1620 


THE INPUT CARDS ARE PRE-PUNCHED WITH STATION NUMBER» DATE» WIRE LENGTH 
AND BOTTLE NUMBER» THEN SENT TO THE CHEMISTRY LABORATORY WHERE THE X 
AND Y ARM READINGS ARE PUNCHEDe THE CARDS ARE THEN RETURNED AND PRO- 
CESSED THROUGH THE COMPUTERe AN 80-80 BOARD ON THE IBM 407 IS USED 
FOR LISTING THE OUTPUT OF THIS PROGRAMe 


UNIVERSITY OF MIAMI 

MARINE LABORATORY 

COMPUTING CENTER 

1 RICKENBACKER CAUSEWAY 
VIRGINIA KEYs MIAMI» FLORIDA 


SPECTAL CHEMISTRY CALCULATIONS LANGUAGE - FORTRAN IV 
COMPUTER - IBM 1130 


READS SPECIAL CHEMISTRY (PHOSPHATEs SILICATEs NITRATE» ETCe) RAW DATA 
CARDS» AND COMPUTES FINAL VALUES, OUTPUT FROM THE PROGRAM—~- WORKING 
RECORD OF THE DATA FILE» FINAL REPORT IN PUBLISHABLE FORM, PLOTS OF 
ANY VARIABLES VSe DEPTH, PLOTS OF ANY VARIABLE vSe VAREABLE» AND STAN- 
DARD OBSERVED CARDSe DOCUMENTATION=-— OPERATING INSTRUCTIONS ONLYe 


UNIVERSITY OF WASHINGTON 
DEPARTMENT OF OCEANOGRAPHY 

22A OCEANOGRAPHY TEACHING BLDGe 
ATTNe MRSe HELLA MACINTOSH 
SEATTLE» WASHe 98105 


WATER CHEMISTRY LANGUAGE - FORTRAN Iv 
COMPUTER -— IBM 360/65 
(COPY ON FILE AT NODC) 

CALCULATES THE DIELECTRIC CONSTANT OF WATER O TO 360 DEGe C (WATER 
SATURATED FOR T OVER 100 DEGe C), THE DENSITY OF WATER (0 TO 360 DEGe 
CC)» THE EXTENDED DEBYE-HUECKEL ACTIVITY COEFFICIENTS OF CHARGED spEC- 
IES» THE ACTIVITY PRODUCTS FOR 33 HYDROLYSIS REACTIONS INCLUDING OX- 
IDES» HYDROXIDESs CARBONATES»s SULFIDES AND SILICATES» THE CONCENTRA- 
TIONS AND ACTIVITIES OF 10 ION PAIRS OR COMPLEXES» AND OF 22 AQUEOUS 
SPECIES» THE OXIDATION POTENTIAL CALIBRATIONS» THE STANDARD STATE OXI- 
DATION POTENTIALS AND EH VALUES AT EQUILIBRIUM FOR 13 REDOX REACTIONS, 
MOLES AND PPM OF CATIONS AT EQUILIBRIUM WITH 42 SOLID PHASES AND THE 
CHEMICAL POTENTIALS FOR EACH OF THE 42 REACTIONS ALONG WITH ACTIVITY 
PRODUCT/EQUILIBRIUM CONSTANT RATIOS FOR THE HYDROLYSIS REACTIONS. 
PROGRAM NO. MO101, FEB 1968, 


PAGE 009 


Ue Se GEOLOGICAL SURVEY 

COMPUTER CENTER DIVISION 

ATTNe RALPH EICHERs CHIEF 

BRANCH OF SCIENTIFIC APPLICATIONS 
WASHINGTON» De Co 20242 


TSALBP LANGUAGE — FORTRAN II 
COMPUTER -— CDC 3100 


CALCULATES THE SALINITY ANOMALY FROM A STANDARD T/S OR THETA/S CURVE 
FOR NORTH ATLANTIC CENTRAL WATER BY LeVe WORTHINGTONe THE RESULTS ARE 
OUTPUT ON THE LINE PRINTER» STATION BY STATION, STORAGE REQuUIREMENT-— 
2540 DECIMALe AUTHOR-- AeBe GRANT (JUNE 1968), 


DIRECTOR 

ATLANTIC OCEANOGRAPHIC LABORATORY 
BEDFORD INSTITUTE 

DARTMOUTHs NOVA SCOTIA» CANADA 


TSATBP LANGUAGE -— FORTRAN II 
COMPUTER -— CDC 3100 


CALCULATES THE PERCENTAGE OF OXYGEN SATURATION IN SEA WATER» ACCORDING 
TO TABLES AND FORMULAE BY MONTGOMERY (1967)s AS WELL AS AN OXYGEN A- 
NOMALY ON A SIGMA-T SURFACE, ACCORDING TO A TABULATED CURVE BY RICH-— 
ARDS AND REDFIELD (1955)e THE RESULTS ARE OUTPUT ON THE LINE PRINTER,» 
STATION BY STATIONe AUTHOR-- AeBe GRANT (JUNE 1968).6 


DIRECTOR 

ATLANTIC OCEANOGRAPHIC LABORATORY 
BEDFORD INSTITUTE 

DARTMOUTHs NOVA SCOTIA» CANADA 


PERCENTAGE SATURATION OF OXYGEN IN LANGUAGE — FORTRAN IV-G 
ESTUARINE WATERS COMPUTER — IBM 360/65 
(COPY ON FILE AT NODC) 

COMPUTES THE PERCENTAGE SATURATION OF DISSOLVED OXYGEN IN ESTUARINE» 
OR BRACKISH WATERe BECAUSE OF THE TEMPERATURE COMPENSATION AT A FIXED 
25 DEGe C IN THE CONDUCTIVITY MEASUREMENTS» SALINITY IS GIVEN AS INPUT 
AND IS USED TO COMPUTE CHLORINITY.s» THIS COMPUTED CHLORINITYs WITH THE 
ACCOMPANYING TEMPERATURE» IS USED TO DETERMINE THE OXYGEN SOLUBILITY 
OF THE WATERe THE MAXIMUM PERCENTAGE SATURATION OF THE DISSOLVED Oxy- 
GEN IN THE WATER IS CALCULATED FROM THE GIVEN OXYGEN CONTENT AND THE 
COMPUTED OXYGEN SOLUBILITYe THE SAME PROCEDURE IS USED TO ASCERTAIN 
THE MINIMUM PERCENTAGE SATURATION OF OXYGENe INDEPENDENTLY OF THE 
DISSOLVED OXYGEN DATA, THERE IS ANOTHER SET OF MEASURED TEMPERATURE 
AND CONDUCTIVITY FROM WHICH SALINITY IS COMPUTEDe PROGRAM NOs B5285 
BY PATRICIA As FULTONs APR 1969-6 


Us Se GEOLOGICAL SURVEY 

COMPUTER CENTER DIVISION 

ATTNe RALPH EICHER»s CHIEF 

BRANCH OF SCIENTIFIC APPLICATIONS 
WASHINGTONs De Ce 20242 


AOU» I SAOU LANGUAGE — FORTRAN 
COMPUTER - IBM 360/65 


CALCULATES SIGMA-T» SATURATION VALUES OF OXYGEN, APPARENT OXYGEN UTIL- 


IZATION» AND RATIOS OF AcQeUe TO PHOSPHATE* USES He O« FORMAT (1960) 
CARDS. 


BUREAU OF COMMERCIAL FISHERIES 
HONOLULU» HAWAIT 96812 


PAGE 010 


OXYGEN/NITROGEN SATURATION LANGUAGE —- FORTRAN 


COMPUTER - IBM 7074 


GIVES OXYGEN IN ML/L» MG/L» AND PERCENT SATURATION, ALSO GIVES APPAR- 
ENT OXYGEN UTILIZATIONs NITROGEN IN ML/L, AND NITROGEN PERCENT SATURA- 
TIONe THE PROGRAM WILL ACCEPT DATA DERIVED FROM EITHER GAS PARTITION-—- 
ER OR TITRATION METHODSe OS PROGRAM NOe 59209, BY GORDON WILCHERe 


OCEAN SURVEYS DIVISIONs CODE 9230 
NAVAL OCEANOGRAPHIC OFFICE 
SUITLAND» MD. 20390 


SALINITY LANGUAGE — FORTRAN IV 


COMPUTER - HONEYWELL516 
(COPY ON FILE AT NODC) 
CONVERTS READINGS FROM THE SALINOMETER TO SALINITIES» GIVEN THE TEMP— 
ERATURE AND CONDUCTIVITY RATIOce TELETYPE I/Oco 


COMMANDING OFFICER 

UeSe COAST GUARD OCEANOGRAPHIC UNIT 
BLDGe 159-E»s NAVY YARD ANNEX 
WASHINGTONs De Ce 20390 


OXYGEN LANGUAGE — FORTRAN Iv 


COMPUTER — HONEYWELL516 
(COPY ON FILE AT NODC) 
COMPUTES VALUES OF OXYGEN. TELETYPE I/0. 


COMMANDING OFFICER 

UeSe COAST GUARD OCEANOGRAPHIC UNIT 
BLDGe 159-E» NAVY YARD ANNEX 
WASHINGTONs De Ceo 20390 


PHOSPHATE LANGUAGE - FORTRAN IV 


INDUCTIVE SALINOMETER SALINITY CONVERSION 


COMPUTER -— HONEYWELL516 
(COPY ON FILE AT NODC) 
COMPUTES PHOSPHATE VALUES. TELETYPE 1/0. 


COMMANDING OFFICER 

UeSe COAST GUARD OCEANOGRAPHIC UNIT 
BLDGe 159-Es NAVY YARD ANNEX 
WASHINGTON» De Ce 20390 


LANGUAGE — PDP8 FORTRAN 
COMPUTER — PDP-5, 8S 
(COPY ON FILE AT NODC) 
ACCEPTS BOTTLE NUMBER» TEMPERATURE OF SAMPLE, AND CONDUCTIVITY RATIO 
OF SAMPLE AND OUTPUTS A SALINITY CORRECTED FOR TEMPERATURE AND SHEAR. 


COMMANDING OFFICER 

UeSe COAST GUARD OCEANOGRAPHIC UNIT 
BLDGe 159-Es NAVY YARD ANNEX 
WASHINGTON» De Co 20390 


SPECIFIC CONDUCTIVITY WITH PRESSURE EFFECT LANGUAGE - FORTRAN 


COMPUTER - IBM 0S/360 
(COPY ON FILE AT NODC) 

COMPUTES SPECIFIC CONDUCTIVITIES FROM MEASURED VALUES OF RESISTANCE 
FOR THE ELECTROLYTIC SOLUTION AND THE PRESSURES AT WHICH THE MEASURE- 
MENTS WERE MADE. THE PROGRAM ALSO DETERMINES OTHER USEFUL QUANTITIES 
NEEDED TO DETERMINE THE EFFECT OF PRESSURE ON THE IONIC CONDUCTANCE 
THROUGH THE UPPER 2000 METERS OF THE OCEAN'S WATER COLUMNe THE CON- 
DUCTIVITY INCREASE WHICH RESULTS SOLELY FROM SOLUTION CONCENTRATION 
CHANGES DURING COMPRESSION IS DETERMINED AND FOUND TO BE A SIGNIFICANT 


PAGE 011 


ERROR SOURCEe REFe THESIS BY MICHAEL Es MAYS (DEC 1968, 89 P)e 


NAVAL POSTGRADUATE SCHOOL 
MONTEREY» CALIFORNIA 93940 


SALINITY — CONDUCTIVITY FORMULA LANGUAGE — FORTRAN 
COMPUTER - IBM 7074 


EVALUATES A NEWLY DEVELOPED EQUATION RELATING SEA WATER ELECTRICAL 
CONDUCTIVITY AND SALINITY. AUTHOR-- Wels GUIDRYe OS NO~ 20184. 


COMPUTER DEPARTMENTs CODE 0831 
NAVAL OCEANOGRAPHIC OFFICE 
SUITLAND» MD. 20390 


CHLORINITY — SALINITY LANGUAGE —- FORTRAN II 
COMPUTFR — IBM 7094 


SUBROUTINE COMPUTES CHLORINITY AND SALINITY FROM MEASUREMENTS OF TEMP— 
ERATURE AND CONDUCTIVITYe USES MODIFICATION OF POLLAK*S (1954) EQUA— 
TIONS RELATING CONDUCTIVITYs TEMPERATURE» AND CHLORINITYe 


HARVEY Ee WALTERS 

CHESAPEAKE BAY INSTITUTE 

THE JOHNS HOPKINS UNIVERSITY 
CHARLES AND 34TH STe 
BALTIMORE» MDe 21218 


TOTAL CO(2) LANGUAGE — FORTRAN II 
COMPUTER — IBM 7094 


COMPUTES TOTAL CO(2) FROM MEASUREMENTS OF TEMPERATURE» CHLORINITY» PHs 
AND ALKALINITYe FOLLOWS METHOD OF HeWe HARVEY (1960)e¢ LINEAR INTER- 
POLATION IN TWO VARIABLES IS PERFORMED IN THE TABLESe OUTPUT IS A 
TABULATION FOR EACH STATION OF DEPTHs INPUT DATA» AND TOTAL CO(2).6 
OPTIONALLY» OFF-LINE CALCOMP PLOTS OF TOTAL CO(2) VSe DEPTH CAN BE 
PRODUCED. CORE STORAGE NECESSARY-- 3430 WORDS PLUS PLOTTER ROUTINESe 


HARVEY Ee WALTERS 

CHESAPEAKE BAY INSTITUTE 

THE JOHNS HOPKINS UNIVERSITY 
CHARLES AND 34TH STe 
BALTIMORE» MDe 21218 


GAMMA-RAY SPECTRA LANGUAGE — FORTRAN 
COMPUTER — (NOT GIVEN) 
(COPY ON FILE AT NODC) 

IDENTIFIES AND MEASURES COMPONENTS IN A MIXTURE OF GAMMA-EMITTING RA- 
DIONUCLIDESe THE COMPUTER PROGRAM WILL BE USEFUL IN ANALYZING THE 
LARGE NUMBER OF LOW ACTIVITY MIXTURES OF RADIONUCLIDES THAT ARE TO BE 
MADE IN THE PROGRAM TO DETERMINE THE PHYSICAL-CHEMICAL SPECIES OF THE 
RADIONUCLIDE DEBRIS PRODUCED BY UNDERWATER NUCLEAR EXPLOSIONSe REFe 
REPORT TR-67-465 UeSe NAVAL RADIOLOGICAL DEFENSE LABORATORY» By JAMES 
Fe PESTANER AND DANIEL Le LOVE> 


DIVISION OF BIOLOGY AND MEDICINE 
UeSe ATOMIC ENERGY COMMISSION 
WASHINGTONs De Co 20545 


OPTIMIZATION OF VTE SALINE WATER PLANTS LANGUAGE — FORTRAN IV 
COMPUTER - IBM 7094 
(COPY ON FILF AT NODC) 
PROGRAM AND SUBROUTINES TO DEVELOP AN OPTIMUM DESIGN OF A MIMIMUM COST 
VTF (VERTICAL TUBE EVAPORATOR) FALLING FILM PLANT FOR PRODUCING FRESH 
WATER FROM SFA WATER. RESEARCH AND DEVELOPMENT PROGRESS REPORT NO« 


PAGE 012 


404 (FEB 19695 164 P)e 
UeSe DEPARTMENT OF THE INTERIOR 


OFFICE OF SALINE WATER 
WASHINGTON» DeCe 20240 


PAGE 013 


DATA REDUCTION 
—¥ —#—#—#— 8-4 -—* 


PHYSICAL OCEANOGRAPHY DATA REDUCTION LANGUAGE - FORTRAN II 
PROGRAMS FOR THE CDC 3100 COMPUTER — CDC 3100 
(COPY ON FILE AT NODC) 

AN OCEANOGRAPHIC DATA PROCESSING SYSTEM DESIGNED TO ACCEPT THE DATA 
FROM THE ORIGINAL LOG SHEETSe COMPUTES OBSERVED TEMPERATURES AND 
PRESSURES FROM THERMOMETER READINGS» SALINITIES FROM THE CONDUCTIVITY 
RATIO READINGS» THE DISSOLVED OXYGEN FROM THE TITRES AND THE REACTIVE 
SILICA CONCENTRATIONS FROM THE OpTICAL DENSITIESe THE DATA INPUT MAY 
BE PUNCHED PAPER TAPE FROM THE PDP-8 SYSTEM (Bele COMPUTER NOTE 68-5- 
C) OR PUNCHED CARDSe THE FINAL PROGRAM IN THE SYSTEM COMPUTES DEPTH, 
POTENTIAL TEMPERATUREs SURFACE DENSITY ANOMALY 9 POTENTIAL SURFACE DEN- 
SITY ANOMALY AND SPECIFIC VOLUME ANOMALYe THE PROGRAM ALSO CAN COM-— 
PUTE THE DYNAMIC HEIGHT AND POTENTIAL ENERGY ANOMALY AT GIVEN PRESS- 
URES AND MAY ALSO GIVE A MAGNETIC TAPE OF THE DATA IN CARD IMAGE OF 
THE CODC FORMATe CORE STORAGE-- 16Ke REFe Bele COMPUTER NOTE 68-10-C 
(OCT 1968» 280 PAGES)» BY Re REINIGERs CeKe ROSS» Pe TRITES AND DeJe 
LAWRENCE. 


DIRECTOR 

ATLANTIC OCEANOGRAPHIC LABORATORY 
BEDFORD INSTITUTE 

DARTMOUTHs NOVA SCOTIA» CANADA 


PHYSICAL OCEANOGRAPHY DATA REDUCTION LANGUAGE — PAL III 
PROGRAMS FOR THE PDP-8 COMPUTER — PDP-8 
(COPY ON FILE AT NODC) 
A SYSTEM OF PROGRAMS THAT ACCEPTS RAW DATA AS RECORDED ON DECK SHEETSe 
CALCULATES THE CORRECTED TEMPERATURES» USES THE HIGHEST ORDER LEAST 
SQUARES FIT TO OBTAIN THE SMOOTHED PRESSURES» CALCULATES DEPTH, SPE- 
CIFIC VOLUME ANOMALYs POTENTIAL TEMPERATURE» AND DENSITY ANOMALIESe 
ALSO FORMATS RAW CHEMISTRY DATAe INCLUDES A SET OF PLOTTING ROUTINESe 
CORE STORAGE-=- 4Ke REFe Bele COMPUTER NOTE 68-5-C (258 P» MAY 1968), 
BY CeKe ROSSs Re REINIGERs AeBe GRANTe 


DIRECTOR 

ATLANTIC OCEANOGRAPHIC LABORATORY 
BEDFORD INSTITUTE 

DARTMOUTH» NOVA SCOTIA» CANADA 


STADAT 2 LANGUAGE —- FORTRAN II 
COMPUTER - GE 225 
(COPY ON FILE AT NODC) 

A CHAIN OF EIGHT PROGRAMS WHICH REDUCE AND EDIT HYDROGRAPHIC STATION 
DATAs CALCULATE AND SMOOTH THERMOMETRIC DEPTHSe BASED UPON wOODS HOLE 
Oele PROGRAM 'tHYLOG! (VERSION FOR GE-225)e THE FINAL DATA MAY BE EI- 
THER A PRINTOUT OR NODC FORMAT PUNCHCARDSe REFe BIO COMPUTER NOTE 66- 
5-Ce AUTHOR-- FeKe KEYTEe (SEE ALSO "ON THE FORMULAS FOR CORRECTING 
REVERSING THERMOMETERS! REFe NOe 64-298 WHOI» BY FREEMAN Ke KEYTEe) 


BEDFORD INSTITUTE 
DARTMOUTHs NeSes CANADA 


REDUCTION AND DISPLAY OF DATA ACQUIRED AT SEA LANGUAGE — FORTRAN II 


COMPUTER —- IBM 1130 
(COPY ON FILE AT NODC) 
A SYSTEM OF PROGRAMS (NAVIGATIONs GRAVITY» TOPOGRAPHY» MAGNETICS) FOR 
THE REDUCTION» STORAGE AND DISPLAY OF UNDERWAY DATA ACQUIRED AT SEAco 
THE COMPUTER INSTALLATION CONSISTS OF AN IBM 1130 AND INCLUDES RANDOM 
ACCESS DISK CARTRIDGES AND AN ON-LINE CALCOMP 30 INe PLOTTERe A.IARGE 


PAGE 014 


NUMBER OF THE PROGRAMS UTILIZE NAVIGATION POINTS TOGETHER WITH RAW 
DIGITIZED GEOPHYSICAL DATA PRESEfeTED AS A TIME SERIES, WHERE THE DIFF- 
ERENT DATA MAY BE READ AT UNEQUAL TIME INTERVALSe REFe TECHe REPORT 
NOe 1 (AUGUST 19695 348 Pe) BY MANIK TALWANI 6 


LAMONT—DOHERTY GEOLOGICAL OBSERVATORY 
COLUMBIA UNIVERSITY 
PALISADES» NEW YORK 10964 


RICHARDSON CURRENT METER FILM READING LANGUAGE - DECAL 
COMPUTER — PDP-7(9) 


A SYSTEM OF PROGRAMS UNDER AN ON-LINE TYPEWRITER CONTROL PROGRAM TO 
AUTOMATICALLY READ DATA (CURRENT SPEED AND DIRECTION)» RECORDED ON 16- 
MM FILM» INTO A PDP-7 COMPUTER» USING A PROGRAMMABLE FILM READING DE- 
VICEe DATA OUTPUT IS AVAILABLE IN THE FORM OF NUMERICAL LISTINGS OR 
IN DIGITAL FORM ON MAGNETIC TAPEe A DIGITAL X-Y PLOTTER MAY ALSO BE 
USED TO PRODUCE GRAPHS AND HISTOGRAMS OF CURRENT SPEED AND DIRECTIONe 
THE MOST IMPORTANT IN THE SYSTEM OF PROGRAMS IS THE *tNINEPOINT FIILM 
READER?'.« THE OTHER PROGRAMS ARE-- 'CHANNEL POSITIONING!» *ENTER CHAN- 
NELS's *WRITE DATA'»s *GRAPHING's "CLEAR NINEPOINT RECORD!» "AUTOMATIC 
FRAME ADVANCEts *LEFT OR RIGHT SCAN*'» *ALL CHANNELS ON TOTALS',» *DOT 
SCANNING!» *DIAMOND SCANNERts *MICROSCOPE't»s AND # TEST SINGLE CHANNEL? 
BROCHURE DESCRIBING THE SYSTEM IS AVAILABLE ON REQUESTe 


DRe DANIEL Me FORSYTH 
INFORMATION INTERNATIONAL» INCeo 
89 BRIGHTON AVENUE 

BOSTONs MASSACHUSETTS 02134 


BRAINCON DATA REDUCTION LANGUAGE - FORTRAN IV 
COMPUTER = IBM 1800 SYS 
(COPY ON FILE AT NODC) 
CONVERTS DATA IN THE FORM OF ANGULAR POSITIONS OF THE ROTOR AND COM— 
PASS ARCS FROM BRAINCOM TYPE 316 CURRENT METERS INTO VALUES OF CURRENT 
SPEED AND DIRECTIONs TILT DIRECTION» N-S AND E-W CURRENT COMPONENTS 
AND DISPLACEMENTS (IN KILOMETRES) FROM ANY ARBITRARY ORIGENe DATA IS 
OUTPUT TO LINEPRINTER WITH COLUMN HEADINGS AND MAGNETIC TAPE WITHOUT 
HEADINGSe EXECUTION TIME-- OF THE ORDER OF 3 MINSe PER 100 CARDS (2 
MINSe FOR ONE DAY OF RECORD)e NeleOe PROGRAM NOco 178¢ AUTHOR-— We Je 
GOULDe 


NATIONAL INSTITUTE OF OCEANOGRAPHY 
WORMLEY»s GODALMINGs SURREY 
ENGLAND 


Q FACTORS LANGUAGE - FORTRAN V 
COMPUTER = ATLAS I 


CALCULATES THE PRESSURE IN DECIBARS FROM THE READING OF T(U)-T(W) Glv- 
EN BY AN UNPROTECTED REVERSING THERMOMETERe THE OUTPUT CONSISTS OF A 
TABLE OF VALUES OF PRESSURE FOR TEMPERATURES IN STEPS OF Ocl DEGR Ceo 
NeleQce PROGRAM 636 AUTHOR-- ELIZABETH PALETHORPEe DESCRIBED IN NeleOeo 
INTERNAL REPORT NOc 7s JAN 19686 


NATIONAL INSTITUTE OF OCEANOGRAPHY 
WORMLEY» GODALMING»s SURREY 


ENGLAND 
NIO PROGRAM 59 — THERMOMETER CORRECTIONS FOR LANGUAGE -— CHLF 3/4 
DEEP-SEA REVERSING THERMOMETERS COMPUTER -— MERCURY 


BOTH PROTECTED AND UNPROTECTED THERMOMETERS CAN BE DEALT WITHe CORR- 
ECTIONS ARE DEPENDENT ON THE WATER TEMPERATURE, THE AMBIENT TEMPERA- 
TURE IN THE LABORATORY» AND THE INDEX ERRORS OF THE THERMOMETERS» AU- 
THOR=- JAMES CREASEe REFo NeIleO5o INTERNAL REPORT NOco N6o 


PAGE 015 


NATIONAL INSTITUTE OF OCEANOGRAPHY 
WORMLEY»s GODALMINGs SURREY 
ENGLAND 


DEEp LANGUAGE — FORTRAN 
COMPUTER — HP 2115A 
(COPY ON FILE AT NODC) 
DIGITIZES SALINITY-TEMPERATURE-DEPTH DATA ON LINE USING TIME AS CRI- 
TERION FOR SELECTING POINTSe INPUT ARE FREQUENCIES FROM SeTeDe SYSTEM 
AND STATION HEADING DATA THROUGH TELETYPEe OUTPUT ON PAPER TAPE HAS 
STATION IDENTIFICATION FIELDS, TIME INTERVAL BETWEEN DATA POINTS, AND 
THE SeTeDe DATA — PRESSURE» TEMPERATURE» SALINITYe REFe FRB TECHNICAL 
REPORT NOe 152 (DEC 1969)» BY Ae HUYER AND Ce Ace COLLINS (UNPUBe MSe) 


DRe Ce Ae COLLINS 

MARINE SCIENCES BRANCHs DEMR 
PACIFIC OCEANOGRAPHIC GROUP 
BIOLOGICAL STATION 

NANAIMOs BeCe» CANADA 


TCHK2 (THERMOMETER CORRECT ) LANGUAGE — FORTRAN VI 
COMPUTER — IBM 1130 
(COPY ON FILE AT NODC) 

PURPOSE-- TO CORRECT DEEP-SEA REVERSING THERMOMETERS» TO COMPUTE THER- 
MOMETRIC DEPTHSs TO ALLOW SPURIOUS VALUES TO BE REMOVED FROM THE I-Z 
TABLE» TO SMOOTH THE L-z TABLEs AND TO PUNCH SMOOTHED DEPTH AND OB- 
SERVED TEMPERATURE AND SALINITY AND OXYGEN VALUES ONTO CARDS IN CODC 
FORMATe PROGRAM AND SUB-—PROGRAMS DESCRIBED IN FRB MANUSCRIPT REPORT 
NOe 1071 (DEC 1969s UNPUBLISHED MANUSCRIPT)» BY Ce Ae COLLINS» Re Le 
Ke TRIPE» AND Se Ke WONGe POG HAS TWO OTHER THERMOMETER CORRECTION 
PROGRAMS — TCHK1 USES THE L/Z METHOD, TCHK3 COMPUTES PRESSUREe 


PACIFIC OCEANOGRAPHIC GROUP 
BIOLOGICAL STATION 
NANAIMOs BeCes CANADA 


TEMPERATURE AND DEPTH CALCULATIONS LANGUAGE — FORTRAN AND 
AUTOCODER 
COMPUTER — I8M 1620 AND 
IBM 1401 


(COPY ON FILE AT NODC) 
AT PRESENT THERE IS NO PROVISION FOR CALCULATING WIRE ANGLE DEPTHe 
DENSITY VALUES USED ARE THOSE FOR THE NORTH ATLANTICe THE INPUT IS IN 
TWO PARTSe FIRST THE THERMOMETER TABLES ARE READ INy THEN THE DATA 
CARDSe THE OUTPUT CARD IS A REPRODUCTION OF THE INPUT DATA CARD, PLUS 
ALL NECESSARY CALCULATIONSe AUTHORS-- DeTe EGER» Dele SHAFFER. 


UNIVERSITY OF MIAMI 

MARINE LABORATORY 

COMPUTING CENTER 

1 RICKENBACKER CAUSEWAY 
VIRGINIA KEYs MIAMI» FLORIDA 


THERMOMETER CORRECTION LANGUAGE — FORTRAN IV 
COMPUTER — HONEYWEIL516 
(COPY ON FILE AT NODC) 
CORRECTS DEEP-SEA REVERSING THERMOMETERS AND CALCULATES THERMOMETRIC 
DEPTHS» GIVEN THE THERMOMETER CONSTANTS AND THE INDIVIDUAL THERMOMETER 
READINGSe TELETYPE 1/0 -— HIGH SpEED PAPER TAPE READER DESIRABLE 


COMMANDING OFFICER 

UeSe COAST GUARD OCEANOGRAPHIC UNIT 
BLDGe 159-E» NAVY YARD ANNEX 
WASHINGTON» De Ce 20390 


PAGE 016 


THERMOCHECK II -— TEMPERATURE CORRECTION LANGUAGE — FORTRAN IV 
COMPUTER -— CDC 3100 AND 
IBM 360/65 
(COPY ON FILE AT NODC) 
CORRECTS DEEP-SEA REVERSING THERMOMETERS,» CALCULATES THERMOMETRIC 
DEPTHe AUTHOR-— LEO Me FLETCHERe THE ORIGINAL VERSIONs WITH DOCU- 
MENTATIONs WAS WRITTEN IN FORTRAN FOR THE IBM 16206 


CANADIAN OCEANOGRAPHIC DATA CENTRE 
615 BOOTH STREET 
OTTAWAs CANADA 


TWO FIVE (HYDROGRAPHIC DATA REDUCTION) LANGUAGE — FORTRAN 63,5 
FORTRAN IV 

COMPUTER -— CDC 3600» 

IBM 1800 


PROCESSES RAW DATA TO OBTAIN CORRECTED DEPTH» TEMPERATURE», SALINITY > 
AND OXYGEN-- 1) PROTECTED DEEP-SEA REVERSING THERMOMETER READINGS TO 
OBTAIN THE CorRECTED IN-SITU WATER TEMPERATUREe 2) UNPROTECTED DEEP- 
SEA REVERSING THERMOMETER READINGS TO OBTAIN THE THERMOMETRIC DEPTHs 
CORRECTED FOR GRAVITY VARIATIONS AND FOR THE MEAN DENSITY OF THE OVER- 
LAYING WATER COLUMN IN ANY OCEANe 3) FITS LEAST SQUARES CURVES TO 
WIRE LENGTH VSe (WIRE LENGTH MINUS THERMOMETRIC DEPTH) TO DETERMINE 
THE ACCEPTED DEPTHe 4) CALCULATES SALINITY FROM RAW SALINITY READINGS 
5) CALCULATES DISSOLVED OXYGEN CONCENTRATIONS FROM TITRATIONSe REFe 

A REPORT (UNPUBLISHED MANUSCRIPT) BY NORMA MANTYLAe 


MRSe NORMA Le MANTYLA 

MARINE LIFE RESEARCH GROUP 

SCRIPPS INSTITUTION OF OCEANOGRAPHY 
PeOo BOX 109 

LA JOLLA» CALIFORNIA 92037 


SeleDe DATA PROCESSING LANGUAGE — FORTRAN IV 
COMPUTER - CDC 3600 
(COPY ON FILE AT NODC) 

A PROGRAM WITH SUBROUTINES TO PROCESS SALINITY-TEMPERATURE-DEPTH DATA 
RECORDED IN THE FIELDe DESCRIPTION AND LISTINGS IN A BCF SPECIAL SCI- 
ENTIFIC REPORT — FISHERIES NOe 588 'PROCESSING OF DIGITAL DATA 1OGGER 
STD TAPES AT THE SCRIPPS INSTITUTION OF OCEANOGRAPHY AND THE BUREAU OF 
COMMERCIAL FISHERIES» LA JOLLA CALIFORNIA! (JUNE 1969). BY DRe JAMES 
He JONES. 


DRe BRUCE TAFT 

OCEANIC RESEARCH DIVISION 

SCRIPPS INSTITUTION OF OCEANOGRAPHY 
PeOe BOX 109 

LA JOLLAs CALIFORNIA 92037 


THERMOMETER CORRECTION AND THERMOMETRIC DEPTH LANGUAGE — FORTRAN 
COMPUTER -— IBM 7074 
(COPY ON FILE AT NODC) 
COMPUTES THERMOMETER CORRECTIONS AND THERMOMETRIC DEPTHS AND THEN 
PRINTS THIS DATA IN THE FORMAT OF THE UeSe NAVAL OCEANOGRAPHIC 10G 
SHEET "Ate IMR NOe O-9-63 (UNPUBLISHED MANUSCRIPT)» AUTHOR-- Se Co 
PORTERe 


COMPUTER SYSTEMS DIVISION 


NATIONAL OCEANOGRAPHIC DATA CENTER 
WASHINGTONs De Ceo 20390 


PAGE 017 


BATHYMETRIC DATA REDUCTION LANGUAGE —- FORTRAN 
COMPUTER — IBM 7074 


PROCESSES DATA GATHERED WHILE NAVIGATING WITH ANY CIRCULAR AND/OR Hy- 
PERBOLIC SYSTEMe EIGHT OPTIONS ARE AVAILABLE PERTAINING TO POSITION 
CONVERSIONs FORM OF INPUTs DATA SMOOTHINGs SPECIAL CORRECTIONS, AND 
INTERPOLATION OF POSITION-DEPENDENT VALUES SUCH AS CONTOUR CROSSINGS. 
OS NO. 53559. 


Ge Ce DONOHUEs CODE 8006 
NAVAL OCEANOGRAPHIC OFFICE 
SUITLAND» MD. 20390 


SYNOPTIC PROGRAM (UWMS-0980) LANGUAGE —- FORTRAN II 
COMPUTER — IBM 7094-II/ 
7040 DCS AND 
cDC 6400 
(COPY ON FILE AT NODC) 
REDUCES DATA FROM RAW SHIP-BOARD OBSERVATIONSe CORRECTS THERMOMETERS 
AND COMPUTES THERMOMETRIC DEPTHS, WIRE ANGLE DEPTHS, SALINITIES FROM 
BRIDGE READINGS» OXYGEN VALUES FROM TITRATIONSs THEN COMPUTES SIGMA-T > 
OXYGEN SATURATION PERCENTs AND APPARENT OXYGEN UTILUZATIONe CORE STO- 
RAGE REQUIRED-- 255335 WORDS FOR MAIN PROGRAMs 2058 WORDS FOR SUBROUT— 
INESe REFe A 150 PAGE REPORT (UWMS-0980, APR 1967) AND TECHNICAL RE- 
PORT NO» 181 (M67-8» JAN 1968)» BY EUGENE Ee COLLIASe THERE IS ALSO 
A MORE LIMITED VERSION FOR THE IBM-11305« REVISED 1969 FOR THE CDC- 
6400. 


He MACINTOSH, COMPUTER SERVICES 
DEPARTMENT OF OCEANOGRAPHY 
UNIVERSITY OF WASHINGTON 
SEATTLE» WASHe 98105 


UNDERWAY DATA SYSTEM LANGUAGE — FORTRAN 
COMPUTER - IBM 1130 


PROCESSES DATA COLLECTED FROM UP TO 7 MONITORED SENSORS AND FROM THE 
AUTOANALYZER WHILE UNDERWAY. INPUT-—- PAPER TAPE — RECORDS TAKEN ABOUT 
ONCE A MINUTE.’ OUTPUT-- COLLECTED DATA PUNCHED ON CARDS AVERAGED OVER 
A GIVEN PERIODe DATA IS THEN USUALLY RUN THROUGH THE IBM CONTOURING 
SYSTEM (NCS) AND PLOTTEDe DOCUMENTATION-— OPERATING INSTRUCTIONS ONLY 


UNIVERSITY OF WASHINGTON 
DEPARTMENT OF OCEANOGRAPHY 

22A OCEANOGRAPHY TEACHING BLDGe 
ATTNe MRSe HELLA MACINTOSH 
SEATTLE» WASH. 98105 


SALINITY-TEMPERATURE-DEPTH CALCULATIONS LANGUAGE —- FORTRAN IV, 
ASSEMBLER 
COMPUTER — I8M 1130 


THIS SYSTEM READS AND EDITS PAPER TAPE FROM A BISSETT-BERMAN STD CASTe 
THE RAW DATA (FREQUENCIES) ARE CONVERTED TO REAL VALUESe INPUT TO 
PROGRAM-— PUNCHED PAPER TAPE FROM THE HEWLETT-PACKARD DAS» FOUR CHAN- 
NELS ARE PUNCHED — SALINITY, TEMPERATURE» SOUND VELOCITY, AND DEPTHe 
OUTPUT-- LISTING OF REAL VALUES», PLOT OF EACH VARIABLE VSe DEPTH, AND 
A SECTION PLOT OF SALINITY AND/OR TEMPERATURE VSe DEPTH FOR A MAXIMUM 
OF 10 STATIONSs DOCUMENTATION--— OPERATING INSTRUCTIONS ONLYe 


UNIVERSITY OF WASHINGTON 
DEPARTMENT OF OCEANOGRAPHY 

22A OCEANOGRAPHY TEACHING BLDGe 
ATTNe MRSe HELLA MACINTOSH 
SEATTLE» WASHe 98105 


PAGE 018 


Sele 


HYDR 


TEMP 


De CORRECTION LANGUAGE — FORTRAN IV 
COMPUTER — IBM 7094 


CORRECTS THE SALINITY AS RECORDED BY THE SeTeDe INSTRUMENT FOR ERRORS 
INTRODUCED BY THE TEMPERATURE GRADIENTs LOWERING SPEED» AND TIME CON- 
STANT OF THE SeTeDe AUTHOR-— Je HUBERTZ.e 


TEXAS A AND M UNIVERSITY 
COLLEGE OF GEOSCIENCES 
DEPARTMENT OF OCEANOGRAPHY 
COLLEGE STATIONs TEXAS 77843 


(0) LANGUAGE —- FORTRAN IV-E 
COMPUTER — IBM 360/50 


PROVIDES I/0 FOR HYDROGRAPHIC DATAe USES SUBROUTINES TO CORRECT RE- 
VERSING THERMOMETERS AND CALCULATE THERMOMETRIC DEPTHe APPLIES METER 
WHEEL CORRECTION» AVERAGES TEMPERATURE VALUES» WRITES ALTERNATE VALUES 
WHERE NECESSARYe WRITES APPROPRIATE MESSAGES ON CONDITION OF DATAe 
WRITES THERMOMETER HISTORY SHOWING WHICH THERMOMETERS MALFUNCT IONED 
AND WHICH PAIRS OF PROTECTED THERMOMETERS YIELD ALTERNATE VALUES. 
SUBROUTINES NEEDED-- TEMPs LINT» UTEMPs AZIZe WRITE-UPS FOR THIS AND 
OTHER UNIVe OF Re Ie PROGRAMS FOR PROCESSING OF HYDROGRAPHIC DATA ARE 
PRINTED IN A MEMORANDUM, DATED JANUARY 19705 WRITTEN BY Re Ke SEXTON® 


ROBERT Ke SEXTON 

NARRAGANSETT MARINE LABORATORY 
UNIVERSITY OF RHODE ISLAND 
KINGSTON» RHODE ISLAND 02881 


LANGUAGE - FORTRAN IV-E 
COMPUTER - IBM 360/50 


SUBROUTINE CALCULATES INDEX AND THERMAL EXPANSION CORRECTIONS FOR PRO- 
TECTED REVERSING THERMOMETERS», ASSOCIATES A TOLERANCE WITH EACH THER- 
MOMETER ACCORDING TO RANGEs SETS MESSAGE INDICATORS FOR VARIOUS DATA 
CONDITIONSe AUXILIARY AND MAIN INDEX CORRECTIONS ARE COMPUTED By 
LINEAR INTERPOLATION BETWEEN POINTS IN THE THERMOMETER DATA ARRAY 5 
"PTHRMt.» THERMAL EXPANSION CORRECTION IS COMPUTED USING EQUATION (29) 
PAGE 1ls FROM 'ON THE FORMULA FOR CORRECTING REVERSING THERMOMETERS! 4 
BY FeKe KEYTEs WHOIs REFe NOo 64-29. 

SUBROUTINES NEEDED-- LINT. 


ROBERT Ke SEXTON 

NARRAGANSETT MARINE LABORATORY 
UNIVERSITY OF RHODE ISLAND 
KINGSTON» RHODE ISLAND 02881 


UTEmP LANGUAGE - FORTRAN IV-E 


COMPUTER — IBM 360/50 


SUBROUTINE CALCULATES INDEX AND THERMAL EXPANSION CORRECTIONS FOR UN- 
PROTECTED THERMOMETERSe IT SELECTS A #Q* VALUE APPROPRIATE TO THE 
DEPTH OF REVERSALe SETS MESSAGE INDICATORS FOR VARIOUS DATA CONDI- 
TIONSe AUXILIARY AND MAIN INDEX CORRECTIONS ARE COMPUTED BY LINEAR 
INTERPOLATION BETWEEN POINTS IN THE THERMOMETER ARRAY» '"UTHRMte 
THERMAL EXPANSION CORRECTION IS COMPUTED USING EQUATION (8)» PAGE 8» 
FROM "ON THE FORMULAS FOR CORRECTING REVERSING THERMOMETERS'» BY FeKe 
KEYTE» WHOIs REFe NOco 64-29. IF A 'Q' VALUE FOR THE THERMOMETER IN 
QUESTION CHANGES WITH DEPTH, WIRE LENGTH IS USED TO COMPUTE THE 
CORRECT VALUE BY LINEAR INTERPOLATION BETWEEN PRESSURE POINTSe IF THE 
WIRE LENGTH IS OUTSIDE THE END POINTSs #Q* VALUES CORRESPONDING TO THE 
END POINT VALUE ARE USEDe 

SUBROUTINE NEEDED-- LINT 


ROBERT Ke SEXTON 
NARRAGANSETT MARINE LABORATORY 


PAGE 019 


UNIVERSITY OF RHODE ISLAND 
KINGSTON» RHODE ISLAND 02881 


REVERSING THERMOMETER CORRECTION LANGUAGE — FORTRAN IV 
COMPUTER — IBM 360/65 


CALCULATIONS OF CORRECTED TEMPERATURES AND THERMOMETRIC DEPTHS FROM 
REVERSING THERMOMETER READINGSe OUTPUT INCLUDES AVERAGE TEMPERATURE, 
DIFFERENCE BETWEEN CORRECTED TEMPERATURES» AND L-Z VALUESe 


BUREAU OF COMMERCIAL FISHERIES BIOLOGICAL LABe 
ATTNe DRe Re Ace BARKLEY 

PeO5o BOX 3830 

HONOLULU» HAWATI 96812 


THERMOMETER CORRECTION AND THERMOMETRIC DEPTH LANGUAGE — PAL III 
COMPUTER — PDP-5, 8S 


(COPY ON FILE AT NODC) 
CORRECTS BOTH PROTECTED AND UNPROTECTED REVERSING THERMOMETERSe DET- 
ERMINES THERMOMETRIC DEPTH BY AN ITERATIVE PROCESSe CAN CORRECT A 
MAXIMUM OF 58 THERMOMETERSe DESIGNED FOR USE ABOARD VESSELe WRITTEN 
FoR THE UeSe COAST GUARD BY LTe ReMe O'HAGAN (RETe)s DIGITAL EQUIPMENT 
CORPe»s MAYNARD» MASSe COPY OF PROGRAM IS DEPOSITED WITH DECUSe REF. 
UeSe COAST GUARD OCEANOGRAPHIC MANUSCRIPT "OCEANOGRAPHIC COMPUTER PRO- 
GRAMS FOR THE PDP-5'» 15 OCTe 1964 (UNPUBLISHED MANUSCRIPT) e 


DIGITAL EQUIPMENT CORPORATION 
MAYNARD» MASSACHUSETTS 01754 


HYLOG LANGUAGE — FORTRAN IV-H 
COMPUTER -— SDS SIGMA 7 


TAKES RAW OCEANOGRAPHIC STATION DATAs CORRECTS THE TEMPERATURES AND 


FINDS THE DEPTH OF EACH OBSERVATIONe INPUT-- CARDS AND 9-TRACK MAG- 
NETIC TAPE IN GENERALIZED FORMATe CORE STORAGE NEEDED-- 149452 WORDS. 


INFORMATION PROCESSING CENTER 

ATTNe MARY HUNT 

WOODS HOLE OCEANOGRAPHIC INSTITUTION 
WOODS HOLEs MASSACHUSETTS 02543 


THRCL LANGUAGE — FORTRAN IV-H 
COMPUTER - SDS SIGMA 7 


PREPARES A MAGNETIC TAPE FILE OF THERMOMETER CALIBRATION RECORDS TO BE 
USED WITH PROGRAM 'HYLOGt. THE THERMOMETER CALIBRATIONS ARE INPUT ON 
CARDS. 


INFORMATION PROCESSING CENTER 

ATTNe MARY HUNT 

WOODS HOLE OCEANOGRAPHIC INSTITUTION 
WOODS HOLEs MASSACHUSETTS 02543 


PAGE 020 


EDITING AND SPECIAL INPUT/OUTPUT 
—H—H%—H—K—HK—H—-H—H—K—H—H—H—H—H—H—* 


COMPUTER UTILITY PROGRAM LANGUAGE — FORTRAN 
COMPUTER — CDC 3800 


PROVIDES I/0 MEDIA TO MEDIA CONVERSIONS AND/OR TRANSFERS UNDER COMPUT— 
ER OPERATING SYSTEMS CONTROLe THIS PROGRAM PROVIDES A SIMPLE METHOD 
TO COPYs PRINTs COMPAREs PUNCHs SKIP» OR DESCRIBE RECORDS AND FILES 

ON AN INPUT SOURCE TO THE CDC 3800 COMPUTERe NRL MEMOe REPORT 19356 
AUTHORS-- Te ROZANSKI»s Je BURGESS» De GOSSETTs De SHANNON.’ 


DORIS E. GOSSETT 

RESEARCH COMPUTATION CENTER 

MATHEMATICS AND INFORMATION SCIENCES DIVISION 
NAVAL RESEARCH LABORATORY» WASHINGTON» De Co 20390 


NELEDIT LANGUAGE — FORTRAN 
COMPUTER -— CDC 3800 


EDITS CARDS OR CARD IMAGES UNDER OPERATING SYSTEM CONTROLe PROVIDES 

A SIMPLE METHOD OF RESEQUENCINGs SEQUENCINGs PRINTINGs INSERTING, DEL- 
ETING AND REPLACING CARD IMAGES WHICH EXIST ON AN INPUT SOURCE TO THE 
COMPUTERe NRL MEMOe REPORT 19366 AUTHORS-- Je BURGESS» De GOSSETT»s 
De SHANNON. 


DORIS Ee. GOSSETT 

RESEARCH COMPUTATION CENTER 

MATHEMATICS AND INFORMATION SCIENCES DIVISION 
NAVAL RESEARCH LABORATORY» WASHINGTONs De Ce 20390 


JOB EDIT FOR L-Z PROGRAM LANGUAGE - AUTOCODER 
COMPUTER - IBM 1401 


(COPY ON FILE AT NODC) 
USES OUTPUT TAPE FROM TEMPERATURE AND DEPTH PROGRAM AS INPUTe AUTHOR-- 
DeLe SHAFFER. 


UNIVERSITY OF MIAMI 

MARINE LABORATORY 

COMPUTING CENTER 

1 RICKENBACKER CAUSEWAY 
VIRGINIA KEY» MIAMI» FLORIDA 


A TAPE INPUT AND OUTPUT SUBROUTINE LANGUAGE — AUTOCODER 
COMPUTER - IBM 7074 
(COPY ON FILE AT NODC) 

THE *"TAPIO*' (TAPE INPUT AND OUTPUT) PROGRAM IS DESIGNED TO BE CALIED 
BY FORTRANe IT CAN BE USED To OPERATE DATA TAPES MUCH FASTER THAN 
OTHERWISE POSSIBLE» MAKING USE OF THE FEATURE OF 'SIMULTANEITY*e ALSO, 
IT WILL CALL AN *EDIT* PROGRAM AS REQUIREDs FOR INPUT AND OUTPUT PRO- 
CEDURESe USING TAPIO MAKES IT NECESSARY TO WRITE YOUR OWN EDIT PRO- 
GRAMe REFe IMR NOc M—-2-645 JAN 1965 (UNPUBLISHED MANUSCRIPT )e AUTHOR 
— PHILLIP Je LAUTENSCHLAGER. 


DATA SYSTEMS CENTER» CODE 083 
NAVAL OCEANOGRAPHIC OFFICE 
SUITLANDs MDe 20390 


LORAN EDIT LANGUAGE — FORTRAN 
COMPUTER - IBM 7074 
(COPY ON FILE AT NODC) 
EDITS LORAN RATES FOR CHARTING COORDINATES AND/OR FINAL LORAN-A AND 
LORAN-C TABLE PUBLICATIONe REFe A REPORT IR NOce 69-875 OCT 19695 BY 


PAGE 021 


KATHLEEN Ae JENNINGS» WHICH DESCRIBES THIS AND OTHER PROGRAMS AND PRO- 
CEDURES USED AT THE NAVAL OCEANOGRAPHIC OFFICE IN THE LORAN TABLE ED- 
ITING PROCESS. FURTHER INFORMATION MAY BE OBTAINED FROM THE FIELD 
MANAGEMENT AND DISSEMINATION DEPTe (CODE 44), OR THE AUTHORe 


NAVIGATIONAL SCIENCE DIVe,s CODE 5320 
TECHNICAL PRODUCTION DEPT. 

NAVAL OCEANOGRAPHIC OFFICE 

SUITLAND» MD. 20390 


SOUND SPEED EDIT LANGUAGE —- FORTRAN 
COMPUTER — IBM 7074 


TAKES NODC DATA CARDS HAVING TIME SERIES SOUND SPEED DATA, ADDS ON A 
BOTTOM PART BECAUSE THE TIME SERIES DATA DOES NOT GO TO THE BOTTOM OF 
THE WATER COLUMN»s AND REARRANGES THE DATA TO MAKE IT ACCEPTABLE TO 

THE RAY TRACE PROGRAM OF CISNEYe OS NOs 53817e¢ AUTHOR-—- ReRe GLEASONe 


EXPLORATORY OCEANOGRAPHY DIVe, CODE 7200 
NAVAL OCEANOGRAPHIC OFFICE 
SUITLAND» MD. 20390 


CARDS LANGUAGE — FORTRAN IV-E 
COMPUTER - IBM 360/50 


CONVERTS PUNCHED OUTPUT FROM 'SIGMAT' TO INPUT FOR 'HEIGHT'e 


ROBERT Ke SEXTON 

NARRAGANSETT MARINE LABORATORY 
UNIVERSITY OF RHODE ISLAND 
KINGSTON» RHODE ISLAND 02881 


DEPTHS LANGUAGE — FORTRAN IV-E 
COMPUTER — IBM 360/50 


CONVERTS PUNCHED OUTPUT FROM "HYDRO! TO INPUT FOR 'SIGMAT'« 


ROBERT Ke SEXTON 

NARRAGANSETT MARINE LABORATORY 
UNIVERSITY OF RHODE ISLAND 
KINGSTON» RHODE ISLAND 02881 


RDTHRM LANGUAGE — FORTRAN IV-E 
COMPUTER — IBM 360/50 


READS THERMOMETER DATA AS IT IS READ BY tHYDROt AND WRITES OUT THE 
DATA IN A FORMAT SUITABLE FOR CHECKINGe 


ROBERT Ke SEXTON 

NARRAGANSETT MARINE LABORATORY 
UNIVERSITY OF RHODE ISLAND 
KINGSTON» RHODE ISLAND 02881 


DATA LANGUAGE — FORTRAN IV-H 
COMPUTER — SDS SIGMA 7 


SUBROUTINE READS OCEANOGRAPHIC STATION DATA CARDS AND RETURNS THE IN- 
FORMATION CONTAINED THEREIN TO THE USERs ONE STATION FOR EACH CALLe 


INFORMATION PROCESSING CENTER 

ATTNe MARY HUNT 

WOODS HOLE OCEANOGRAPHIC INSTITUTION 
WOODS HOLE» MASSACHUSETTS 02543 


PAGE 022 


SCRUB LANGUAGE — FORTRAN IV-H 
COMPUTER — SDS SIGMA 7 


PROVIDES SEVERAL METHODS BY WHICH DATA STORED IN WHOI STANDARD FORMAT 
MAY BE EDITED AND TESTEDe OUTPUT IS THE CORRECTED vERSION OF THE DATA 
ON 9-TRACK MAGe TAPE 


INFORMATION PROCESSING CENTER 

ATTNe JOHN Ae MALTAIS 

WOODS HOLE OCEANOGRAPHIC INSTITUTION 
WOODS HOLEs MASSACHUSETTS 02543 


BATHYTHERMOGRAPH OUTPUT LANGUAGE — SPS 
COMPUTER — IBM 1401 
(COPY ON FILE AT NODC) 
TAPE TO CARD/PRINT EDITING PROGRAMe BLOCKED INPUT WITH MSQ@ OR CRUISE 
SEQUENCE FORMS CONTROLe USES TAPE SEARCH, SELECTION AND DUPLICATION. 
OS NOs 52291. AUTHOR--— JeCe JENSONe 


COMPUTER SYSTEMS DIVISION 
NATIONAL OCEANOGRAPHIC DATA CENTER 
WASHINGTON>s De Ce 20390 


CARD-TO-TAPE FOR INPUT TO THE 7074 LANGUAGE —- SPS II 
COMPUTER — IBM 1401 
(COPY ON FILE AT NODC) 
SPECIAL CARD-TO-TAPE ROUTINE FOR DATA INPUT TO THE IBM 70749 WITH 
OPTIONAL ZONE PUNCH EDITINGs PRINTOUT OF TAPE RECORDS» MULTI-FILE 
PROVISIONSe AUTHOR-= LARRY WOLCOTTe 


COMPUTER DEPARTMENTs CODE 083 
NAVAL OCEANOGRAPHIC OFFICE 
SUITLANDs MDe 20390 


OCEANS II REPORT GENERATOR LANGUAGE — SPS 
COMPUTER - IBM 1401 
(COPY ON FILE AT NODC) 
USED FOR HIGH SPEED PREPARATION OF OCEANS II OUTPUT FOR DATA RECORD 
PUBLICATIONe (NOTE-- CODC IS NOW USING A LATER VERSION OF THIS DECKe) 


CANADIAN OCEANOGRAPHIC DATA CENTRE 
615 BOOTH STREET 
OTTAWA» CANADA 


CONVERSION» NODC TO ICES LANGUAGE —- SPS 
COMPUTER -— IBM 1401 
(COPY ON FILE AT NODC) 

CONVERTS NODC OCEAN STATION DATA ON CARDS/TAPE TO ICES FORMAT CARDSe 
INCLUDES OPTIONAL SUBROUTINE IN SPS LANGUAGE FOR CALCULATION OF OXxYGEN 
PERCENT OF SATURATION USING FOX*S FORMULAEe OS NOc 522826 AUTHOR —- 
Ce DINGERe NODC-ICES AND ICES-NODC CONVERSION PROGRAMS ARE CURRENTLY 
BEING COMPLETELY REWRITTEN FOR THE IBM 360/405 IN ASSEMBLER AND PL/I 
LANGUAGES» BY SALLY KEEHNe 


COMPUTER SYSTEMS DIVISION 
NATIONAL OCEANOGRAPHIC DATA CENTER 
WASHINGTON>s De Ce 20390 


OCEAN STATION DATA OUTPUTs NODC FORMAT LANGUAGE —- SPS 
COMPUTER - IBM 1401 
(COPY ON FILE AT NODC) 
OCEAN STATION RECORDS ON TAPE ARE PUNCHED ON CARDS AND/OR EDITED INTO 
PRINTOUT. OS NOe 52280. ANOTHER VERSION OF THIS PROGRAM PRINTS» FOR 
FINAL NODC FILESs MONITORED STATION DATA FROM ZONE-EDITED, BLOCKED AND 
SORTED TAPE RECORDSe OS NOe 522875 BY Ce DINGERe A NEW STATION DATA 


PAGE 023 


OUTPUT PROGRAM IS AT PRESENT BEING WRITTEN FOR THE IBM 360/40» IN PL/I 
LANGUAGE, BY JOHN MCHUGH. 


COMPUTER SYSTEMS DIVISION 
NATIONAL OCEANOGRAPHIC DATA CENTER 
WASHINGTON» De Ceo 20390 


STATION DATA CONVERSION» CODC To NODC LANGUAGE — SPS 


COMPUTER — IBM 1401 
(COPY ON FILE AT NODC) 


CANADIAN OCEANOGRAPHIC DATA CENTRE STATION DATA IS TRANSFERRED OR CON- 
VERTED TO THE NEW NODC FORMATe CODC CRUISE MASTER CARDS MUST BE PRE- 
CEDED BY A NODC LEADER CARD. OS NOe 522126 AUTHOR-— RUDI SAENGER. 


COMPUTER SYSTEMS DIVISION 
NATIONAL OCEANOGRAPHIC DATA CENTER 
WASHINGTON» De Ce 20390 


PAGE 024 


GEOSCIENCE 
ee 


%-#-# GEOQPHYSICSs MARINE %—#-+ 


BLACKBODY SPECTRAL RADIANCE LANGUAGE —- FORTRAN 
COMPUTER ~— CDC 3800 


COMPUTES SPECTRAL RADIANCE OF A BLACKBODY RADIATOR USING ONE DEGREE 
INCREMENTS OF TEMPERATURE AND 06605 MICROMETER INCREMENTS OF WAvyE- 
LENGTHe INPUT PARAMETERS ARE TEMPERATURE ASD WAVELENGTHe 


APPLIED OCEANOGRAPHY BRANCH —- CODE 8310 
NAVAL RESEARCH LABORATORY 
WASHINGTONs De Ce 20390 


BLACKBODY RADIANCE LANGUAGE —- FORTRAN 
COMPUTER -— CDC 3808 


COMPUTES RADIANCE OF A BLACKBODY RADIATOR IN A SPECIFIED WAVELENGTH 
INTERVAL USING ONE DEGREE INCREMENTS OF TEMPERATURE AND 0-05 
MICROMETER INCREMENTS OF WAVELENGTHe INPUT PARAMETERS ARE TEMPERATURE 
AND WAVELENGTH. 


APPLIED OCEANOGRAPHY BRANCH —- CODE 8310 
NAVAL RESEARCH LABORATORY 
WASHINGTON» De Ce 20390 


LONG WAVE RADIATION LANGUAGE - FORTRAN IV 
COMPUTER - IBM 360/65 


CALCULATES RADIATION VALUES FOR THE SUOMI-KUHN RADIOMETER. INPUT DATA 
FROM THE TRADE WIND ZONE OCEANOGRAPHY PROGRAM RADIATION CARDSe 


BUREAU OF COMMERCIAL FISHERIES 


2570 DOLE STREET 
HONOLULUs HAWAII 96812 


OBSERVATION DRAPING (GRAVITY) LANGUAGE - FORTRAN 
COMPUTER — IBM 7074 


REDUCES OBSERVATION DATA TAKEN WITH LACOSTE-ROMBERG SEA/AIR OR SUB- 
MARINE GRAVIMETERS TO OBSERVED GRAVITY VALUE AND FREE-AIR ANOMALY. 
INTERPOLATES GEOGRAPHIC POSITION FROM SMOOTHED FIX» COURSE» AND SPEEDe 
GENERATES BC CHART NOe AND XsY COORDINATES FOR MERCATOR PROYECTION FOR 
EACH STATIONe OS NOco 535432 AUTHOR-—- ReKe LATTIMORE®e 


GRAVITY DIVISIONs CODE 83 
NAVAL OCEANOGRAPHIC OFFICE 
SUITLANDs MDe 20390 


REDUCTION AND DISPLAY OF DATA ACQUIRED AT SEA LANGUAGE - FORTRAN II 
COMPUTER — IBM 1130 
(COPY ON FILE AT NODC) 

A SYSTEM OF PROGRAMS (NAVIGATIONs GRAVITY» TOPOGRAPHY» MAGNETICS) FOR 
THE REDUCTIONs STORAGE AND DISPLAY OF UNDERWAY DATA ACQUIRED AT SEAe 
THE COMPUTER INSTALLATION CONSISTS OF AN IBM 1130 AND INCLUDES RANDOM 
ACCESS DISK CARTRIDGES AND AN ON-LINE CALCOMP 30 INe PLOTTERe A LARGE 
NUMBER OF THE PROGRAMS UTILIZE NAVIGATION POINTS TOGETHER WITH RAW 
DIGITIZED GEOPHYSICAL DATA PRESENTED AS A TIME SERIES» WHERE THE DIFF- 
ERENT DATA MAY BE READ AT UNEQUAL TIME INTERVALSe REFe TECHe REPORT 
NOe 1 (AUGUST 19695 348 Pe) BY MANIK TALWANTe 


PAGE 025 


LAMONT-DOHERTY GEOLOGICAL OBSERVATORY 
COLUMBIA UNIVERSITY 
PALISADES» NEW YORK 10964 


TALWANI 2-D GRAVITY LANGUAGE — FORTRAN IV-H 
COMPUTER - IBM 360/65 
(COPY ON FILE AT NODC) 

CALCULATES THE VERTICAL COMPONENT OF GRAVITATIONAL ATTRACTION OF TWO- 
DIMENSIONAL BODIES OF ARBITRARY SHAPE BY APPROXIMATING THEM TO MANY— 
SIDED POLYGONS. THE TECHNIQUE IS FROM TALWANI, WORZELs AND LANDISMAN 
IN JGR» VOLe 64 NOw 1» 1959. OUTPUT-- THE GRAVITY VALUES ARE PRINTED 
IN TABLES» AND THE CALCULATED PROFILE AND THE OBSERVED PROFILE IF ONE 
EXISTS ARE PLOTTED ON THE LINE PRINTER IN EITHER A PAGE SIZE PLOT OR 
AN EXTENDED PLOT WITH THE X-AXIS RUNNING DOWN THE PAGEe PROGRAM CON-— 
TAINS OPTION OF UNITS IN MILESs KILOFEETs OR KILOMETERSe THE PROGRAM 
NOe IS W9206 (MAYs 1968). 


Use Se GEOLOGICAL SURVEY 

COMPUTER CENTER DIVISION 

ATTNe RALPH EICHERs CHIEF 

BRANCH OF SCIENTIFIC APPLICATIONS 
WASHINGTONs De Ce 20242 


PROFILE CARD-TO-TAPE FOR GEOPAC LANGUAGE — FORTRAN IV-H 
COMPUTER — IBM 360/65 
(COPY ON FILE AT NODC) 
USED TO PUT DATAs USUALLY PROFILE DATA» PUNCHED ON CARDS ONTO MAGNETIC 
TAPE FOR SUBSEQUENT PROCESSING BY OTHER PROGRAMS IN A PACKAGE OF PRO- 
GRAMS FOR TWO-DIMENSIONAL GRAVITY AND MAGNETIC CALCULATIONSe OPTIONS 
IN THE PROGRAM ALLOW FOR THE PRELIMINARY OPERATIONS OF SCALING, SHIFT- 
ING, OR DETRENDING THE DATAs’ PROFILES MAY ALSO BE CONCATENATED TO 
COMBINE SEVERAL DATA SETS AS ONEe PROGRAM NOe W9325,5 BY RALPH EICHERe 


Use Se GEOLOGICAL SURVEY 

COMPUTER CENTER DIVISION 

ATTNe RALPH EICHERs CHIEF 

BRANCH OF SCIENTIFIC APPLICATIONS 
WASHINGTON»s De Co 20242 


2D MAGNETIC ANOMALIES LANGUAGE — FORTRAN 
COMPUTER — IBM 1800 SYS 


COMPUTES HORIZONTAL AND VERTICAL AND TOTAL MAGNETIC ANOMALIES ARISING 
FROM PRISMS OF ARBITRARY CROSS-SECTION AND MAGNETISATION AND INFINITE 
IN LENGTHe A VERSION FOR THE ATLAS I IS ALSO IN FORTRANe NeleOe PRO- 
GRAM 1025 BY Es PALETHORPE AND Jeo CREASEs REFe NeIleO5w INTERNAL REPORT 
NOs NelOs NOV 1968. 


NATIONAL INSTITUTE OF OCEANOGRAPHY 
WORMLEYs GODALMINGs SURREY 


ENGLAND 
COMPUTATION AND PLOTTING OF MAGNETIC ANOMALIES LANGUAGE — FORTRAN II 
AND GRADIENTS COMPUTER — IBM 7094 W/ 


CALCOMP 
(COPY ON FILE AT NODC) 

COMPUTES THE ANOMALY PROFILES FOR TOTAL FIELD» HORIZONTAL AND VERTICAL 
COMPONENTS, FIRST AND SECOND VERTICAL DERIVATIVES AND FIRST AND SECOND 
HORIZONTAL DERIVATIVES OVER A UNIFORMLY MAGNETIZED TWO-DIMENSIONAL 
POLYGON OF IRREGULAR CROSS-SECTIONe OUTPUT MAY BE PRINTED OR PLOTTED. 
REF. *POTENTIAL APPLICATIONS OF MAGNETIC GRADIENTS TO MARINE GEOPHYS-— 
ICS' BY WILLIAM Ee BYRD» JRe» JUNE 19674 PROGRAM MODIFIED AND EXPAND- 
ED FROM TALWANI AND HEIRTZLER (1964). 


DEPARTMENT OF GEOLOGY AND GEOPHYSICS 


PAGE 026 


MASSACHUSETTS INSTITUTE OF TECHNOLOGY 
CAMBRIDGE» MASSACHUSETTS 02139 


SOLAR RADIATION CONVERSION LANGUAGE — FORTRAN 
COMPUTER - IBM 7074 


AVERAGES THE RADIATION READINGS FROM THE EPPLEY PYRHELIOMETER AND 
BECKMAN-WHITLEY RADIOMETER FOR EVERY 15 MINUTESe CONVERTS FROM My TO 
LANGLEYS/MINe AND CALCULATES NET RADIATION FROM BOTH INSTRUMENTSe A 
MODIFICATION OF THIS PROGRAM WAS MADE TO INCLUDE A THORNTHWAITE NET 
RADIOMETERe ORIGINAL PROGRAM BY SeMe LAZANOFF REWRITTEN BY MARY Eco 
MYERSe 


COMPUTER DEPARTMENTs CODE 0831 
NAVAL OCEANOGRAPHIC OFFICE 
SUITLANDs MD. 20390 


SEAMOUNT MAGNETIZATION LANGUAGE — FORTRAN 
COMPUTER — IBM 7074 


COMPUTES THE MAGNITUDE AND DIRECTION OF MAGNETIZATION OF A UNIFORMLY 
MAGNETIZED BODY FROM ITS SHAPE AND MAGNETIC INTENSITYe OS NOe 535336 
AUTHOR-- Ge VAN VOORHIS. 


MAGNETICS DIVISIONs CODE 8200 
NAVAL OCEANOGRAPHIC OFFICE 
SUITLAND» MDe 20390 


VAM INTERPOLATION II LANGUAGE — FORTRAN 
COMPUTER - IBM 7074 


COMPUTES INCLINATION» MAGNETIC HEADINGs RELATIVE BEARING, AND DECIIN- 
ATIONe OUTPUT CONTAINS TRACKs DATEs AIRCRAFT TIMEs POSITION, DECI_IN- 
ATIONs DIPs HORIZONTAL INTENSITY (FORCE)»s ALTITUDEs AND GROUND SPEED 
FOR EACH FIVE MINUTES OF TIMEe OS NOco 350325 BY We He HANCOCKe 


NAVAL OCEANOGRAPHIC OFFICE 
SUITLANDs MDe 20390 


SEISMIC SLOPING LAYER COMPUTATION LANGUAGE - FORTRAN II 
COMPUTER - IBM 709 


GIVES TRUE VELOCITIES AND THICKNESSES OF LAYERS FOR SEISMIC REFRACTION 
PROFILESe INPUT ARE HORIZONTAL AND AVERAGE VERTICAL WATER VELOCITIES 
AND APPARENT ONE-WAY VELOCITIES OF SUBSURFACE INTERFACES DERIVED FROM 
TRAVEL-TIME GRAPHS. COMPUTATION FOLLOWS GEOMETRIC METHOD FOR PIANE 
SEISMIC WAVES UTILIZING SNELL'S LAWe AUTHOR--— JOHN ANTOINEe 


TEXAS A AND M UNIVERSITY 
COLLEGE OF GEOSCIENCES 
DEPARTMENT OF OCEANOGRAPHY 
COLLEGE STATION» TEXAS 77843 


TIME TERMs SEISMIC REFRACTION INTERPRETATION LANGUAGE -— FORTRAN IV 
COMPUTER -— IBM 7094 
(COPY ON FILE AT NODC) 

ANALYZES A SET OF DATA THAT APPEARS TO HAVE BEEN GENERATED By A HEAD 
WAVE SYSTEM PROPAGATING ALONG A PARTICULAR BOUNDARYe READS THE STAN- 
DARD TRAVEL-TIME DATA CARDS (CARNEGIE INST» WASHs DTM)e TIME TERMS ARE 
CALCULATED FOR THE BEST LEAST-SQUARE FITTING VELOCITY» IN ADDITION» 
CALCULATES THE STANDARD DEVIATION OF THE SOLUTION AS A FUNCTION OF 
VELOCITY AND EXAMINES THE MATRIX OF RESIDUALS FOR FREQUENCY AND DEPEN- 
DENCE UPON DISTANCEe THESE FEATURES OF THE MATRIX ARE PRESENTED IN 
GRAPH FORMe AUTHOR-—- MeJe BERRYe 


PAGE 027 


UNIVERSITY OF TORONTO 
DEPARTMENT OF PHYSICS 
GEOPHYSICS LABORATORY 
ATTNe DRe Ge Fe WEST 
TORONTO 5 ONTARIO 


#-#-* SEDIMENT ANALYSIS AND MECHANICS ¥*—-#—* 


GEOLOGICAL SAMPLE CONVERSION LANGUAGE — FORTRAN 
COMPUTER — IBM 7074 
(COPY ON FILE AT NODC) ” 

CONVERTS-EDITS TO NODC FORMAT FOR CARDS» DATA ON SAMPLES COLLECTED OR 
STUDIED AS PART OF THE JOINT WOODS HOLE Ocle — UeSe GEOLOGICAL SURVEY» 
ATLANTIC CONTINENTAL MARGIN PROGRAMe INCLUDES AN INDICATOR OF DEPTH 
RANGE VIA TABLE LOOK-UP, AND COMPUTATION OF MARSDEN SQUAREe OS NOe —- 
5223le AUTHOR-- Re VAN WIE} 


COMPUTER SYSTEMS DIVISION 
NATIONAL OCEANOGRAPHIC DATA CENTER 
WASHINGTON» De Co 20390 


MASS PHYSICAL PROPERTIES LANGUAGE —- FORTRAN 
COMPUTER -— IBM 7074 


COMPUTES THE RESULTS OF ENGINEERING ANALYSES IN THE GEOLOGICAL LABe 
THESE ANALYSES INCLUDE DENSITY» SPECIFIC GRAVITY» VOID RATIOs ATTER- 
BURG LIMITS» COHESIONs COMPRESSIVE STRENGTHs CONSOLIDATIONs MOISTURE 
CONTENT» ETCe OS NOe 592026 


OCEAN SURVEYSs CODE 9200 
NAVAL OCEANOGRAPHIC OFFICE 
SUITLAND» MDe 20390 


SEDIMENT SIZE LANGUAGE — FORTRAN 
COMPUTER — IBM 7074 


COMPUTES THE FREQUENCY OF THE GRAIN SIZE DISTRIBUTION AND THE STATIS-— 
TICAL PARAMETERS» AND RECORDS PERTINENT FIELD DATA AND COMPOSITIONAL 
DATA DETERMINED IN THE LABORATORYe THE PROGRAM WILL HANDLE DATA FROM 
AN INDEFINITE NUMBER OF CORE SAMPLESe OUTPUT PRINTED IN TABULAR FORMe 
REFe INFORMAL MANUSCRIPT IM NOe 66-115 AUGe 19665 "SEDIMENT SIZE COM— 
PUTER PROGRAM'» AUTHORS-- DRe JeBe RUCKER AND ReAo STEWART» EXPLORA- 
TORY OCEANOGRAPHY DIVe CODE 7220. FURTHER INFORMATION MAY BE OBTAINED 
THROUGH DISSEMINATION DEPARTMENT» CODE 449 OR THE AUTHORS» 


NAVAL OCEANOGRAPHIC OFFICE 
SUITLAND» MD. 20390 


GRAIN SIZE LANGUAGE —- FORTRAN II 
COMPUTER — GE 225 


A COMPUTER PROGRAM FOR GRAIN-SIZE DATAs BY JOHN SHLEE AND JACQUELINE 
WEBSTER» 1965» WOODS HOLE OCEANOGRAPHIC INSTITUTION REFe NOe 65-42 
(UNPUBLISHED MANUSCRIPT)e THIS PROGRAM AND SEVERAL OTHERS FOR SEDI- 
MENT DATA PROCESSING ARE PRODUCTS OF THE UeSe GEOLOGICAL SURVEY'S MA- 
RINE GEOLOGY AND HYDROLOGY PROGRAMe 


Je WEBSTER 


WOODS HOLE OCEANOGRAPHIC INSTITUTION 
WOODS HOLE» MASSe 


PAGE 028 


STANDARD-SIZE ANALYSIS OF SEDIMENTS LANGUAGE — FORTRAN II 
COMPUTER -— IBM 1620 


COMPUTES THE MEANs STANDARD DEVIATIONs SKEWNESS» AND KURTOSIS BY THE 
METHOD OF MOMENTS FOR SIZE DISTRIBUTION OF PARTICLES AS DETERMINED By 
STANDARD SEDIMENT ANALYSISs THE FRACTION OF THE TOTAL SAMPLE IN EACH 
SIZE CLASSs AND THE FRACTION OF SAND-SIZE MATERIAL COMPOSED OF uP TO 
10 DIFFERENT COMPONENTSe AUTHORS-- JoeWe PIERCE» UeSe NATIONAL MUSEUM, 
AND Dele GOODs KANSAS GEOLe SURVEYe REFe SPECIAL DISTRIBUTION PUBLI- 
CATION 28 (1965)e RUNNING TIME-— LESS THAN 5 HOURS FOR 400 SAMPLESe 


DRe DANIEL Fe MERRIAMs EDITOR» COMPUTER CONTRIBUTIONS 
KANSAS GEOLOGICAL SURVEY 

COMPUTER APPLICATIONS LABORATORY 

THE UNIVERSITY OF KANSAS 

LAWRENCEs KANSAS 66045 


SEDIMENT DATA LANGUAGE — FORTRAN II 
COMPUTER — IBM 709 AND 
cDC 6400 


ALL SEDIMENT DATA COMPUTATIONS, SUCH AS MEANS AND STANDARD DEVIATIONS 
OF TEXTUREs TOTAL TEXTURE» CARBONATE AND NON-CARBONATE FRACTIONS» AS 
WELL AS ORGANIC NITROGEN AND CARBON DATA HANDLINGe PROGRAM REVISED IN 
1964. AUTHOR-- PROF e HeGe GOODELLe 


DEPARTMENT OF GEOLOGY 
FLORIDA STATE UNIVERSITY 
TALLAHASSEEs FLORIDA 32306 


ENGINEERING INDEX PROPERTIES OF CORE SAMPLES LANGUAGE — FORTRAN II-D 
COMPUTER -— IBM 1620 II 
(COPY ON FILE AT NODC) 
REDUCES DATA AND TABULATES RESULTS FOR TESTS ON BULK WET DENSITY» VANE 
SHEAR STRENGTHS, ORIGINAL WATER CONTENT,» LIQUID LIMIT» PLASTIC LIMIT, 
AND SPECIFIC GRAVITY OF SOLIDSe IN ADDITIONs FROM THE ABOVE RESULTS, 
OTHER INDEX PROPERTIES ARE SIMULTANEOUSLY COMPUTED AND TABULATEDe THE 
OUTPUT TABLE LISTS RESULTS IN COLUMNS REPRESENTING EACH DEPTH SEGMENT 
ANALYZEDe PUBLISHED AS AN NCEL TECHNICAL REPORTs REFe NOe R-566 (FEB 
1968s 165 P)»s BY MELVIN Ce HIRONAKAo 


UeSe NAVAL CIVIL ENGINEERING LABORATORY 
PORT HUENEMEs CALIFORNIA 93041 


GRAIN SIZE ANALYSIS WITH DIRECT PLOTTING LANGUAGE - FORTRAN II-D 
COMPUTER - IBM 1620 II 
(COPY ON FILE AT NODC) 
INPUT DATA ARE SAMPLE IDENTIFICATIONs SAMPLE WEIGHTS, HYDROMETER READ- 
INGSs AND SIEVE READINGSe OUTPUT ON IBM 1627 MODEL I PLOTTER IS A 
PARTICLE SIZE DISTRIBUTION CURVEe ANOTHER PROGRAM WRITTEN FOR OUTPUT 
ON CARDS OF A TABLE WITH PROPER HEADINGS -AND VALUES FOR PARTICLE DIA- 
METERS AND PERCENT FINER BY WEIGHTe REFe NCEL REPORT NOco R-5665 BY 
MELVIN Ce HIRONAKAc 


UeSe NAVAL CIVIL ENGINEERING LABORATORY 
PORT HUENEMEs CALIFORNIA 93041 


CARBONATE — ORGANIC CARBON ANALYSIS OF SEDIMENTS LANGUAGE — FORTRAN II-D 
COMPUTER — IBM 1620 II 
(COPY ON FILE AT NODC) 
REDUCES DATA FROM THE CARBON DETERMINATOR AND TABULATES RESULTS OF THE 
ANALYSIS OF DEEP OCEAN SEDIMENTS FOR CARBONATE AND ORGANIC CARBON PER- 
CENTAGESe OUTPUT IN SAME FORMAT AS IN PROGRAM FOR ENGINEERING INDEX 
PROPERTIES» TO WHICH THE OUTPUT FROM THIS PROGRAM IS ADDEDe PROGRAM 
LISTINGS AND WRITEUPS INCLUDED IN AN NCEL REPORTs NOe R-566s By MELVIN 
HTRONAKAe 


PAGE 029 


UeSe NAVAL CIVIL ENGINEERING LABORATORY 
PORT HUENEME» CALIFORNIA 93041 


DIRECT SHEAR TEST WITH DIRECT PLOTTING LANGUAGE — FORTRAN II-D 
COMPUTER — IBM 1620 II 
(COPY ON FILE AT NODC) 

REDUCES DATA AND PLOTS SHEAR STRESS VERSUS SHEAR DISPLACEMENT wITH AP- 
PROPRIATE HEADINGS AND LABELS» USING IBM MODEL I PLOTTERe ANOTHER 
PROGRAM» tDIRECT SHEAR TEST'» USES THE SAME DATA FORMATS BUT PRESENTS 
THE RESULTS IN THE FORM OF TABULATIONS RATHER THAN PLOTSe REFe NCEL 
REPORT R-56656 AUTHOR--— MELVIN Ce HIRONAKAc 


UeSe NAVAL CIVIL ENGINEERING LABORATORY 
PORT HUENEME,» CALIFORNIA 93041 


TRIAXIAL COMPRESSION TEST WITH DIRECT PLOTTING LANGUAGE - FORTRAN II-D 
COMPUTER — IBM 1620 IT 
(COPY ON FILE AT NODC) 
REDUCES THE DATA FROM TRIAXIAL COMPRESSION TESTS AND PLOTS STRESS VSe 
STRAIN WITH HEADINGS FoR SAMPLE IDENTIFICATION, LATERAL PRESSURE, ETCe 
ANOTHER PROGRAM REDUCES THE SAME RAW DATA AND PRESENTS THE RESULTS IN 
THE FORM OF TABULATIONS, ONE FOR EACH TESTe LISTINGS AND DESCRIPTIONS 
FOR BOTH PROGRAMS INCLUDED IN AN NCEL REPORT,» REFe NOe R-5665 BY MeCe 
HIRONAKAe 


UeSe NAVAL CIVIL ENGINEERING LABORATORY 
PORT HUENEME, CALIFORNIA 93041 


CONSOLIDATION TEST (E VSe LOG TIME PLOT) LANGUAGE - FORTRAN II-D 
COMPUTER — IBM 1620 II 
(COPY ON FILE AT NODC) 

REDUCES THE DATA OBTAINED FROM THE CONSOLIDATION TEST READINGSe INPUT 
INCLUDES SAMPLE IDENTIFICATION AND CHARACTERISTICS, AND TEST CHARAC- 
TERISTICSe THE OUTPUT FROM THIS PROGRAM IS IN TWO FORMS-— PLOTS AND 
PUNCHED CARDSe THE LOG OF TIME IS PLOTTED VSe THE VOID RATIOe THE 
CARDS ARE USED AS INPUT TO THE NEXT CONSOLIDATION TEST PROGRAM. 


UeSe NAVAL CIVIL ENGINEERING LABORATORY 
PORT HUENEME» CALIFORNIA 93041 


CONSOLIDATION TEST (E VSe LOG P AND C(V) VSe LANGUAGE — FORTRAN II-D 
LOG P PLOTS) COMPUTER - IBM 1620 II 
(COPY ON FILE AT NODC) 

DEVELOPES PLOTS FOR VOID RATIO VSe LOG OF PRESSURE AND COEFFICIENT OF 
CONSOLIDATION VSe LOG OF PRESSUREe THE INPUT TO THIS PROGRAM CONSISTS 
OF THE OUTPUT CARDS FROM THE PREVIOUS PROGRAM TOGETHER WITH THE VALUES 
OF VOID RATIO AND PRESSURE AT 100 0/0 CONSOLIDATION AND THE TIME AND 
VOID RATIO AT 50 0/0 CONSOLIDATIONe THESE DATA WERE OBTAINED FROM THE 
PLOTS OF VOID RATIO VSe LOG OF TIME IN ACCORDANCE WITH THE TERZAGHI 
CONSOLIDATION THEORYe EXAMPLES OF INPUT AND OUTPUT» WITH PROGRAM DE- 
SCRIPTIONS AND LISTINGS, INCLUDED IN NCEL REPORT R-566 (FEB 68, 165 P) 
BY MELVIN Ce HIRONAKAe 


UeSe NAVAL CIVIL ENGINEERING LABORATORY 
PORT HUENEME» CALIFORNIA 93041 


PERMEABILITY TEST WITH DIRECT PLOTTING LANGUAGE - FORTRAN II-D 
COMPUTER - I8M 1620 II 
(COPY ON FILE AT NODC) 

REDUCES TEST DATA AND PLOTS CURVE OF PERMEABILITY VERSUS TIME WITH AP- 
PROPRIATE HEADINGS AND LABELS» USING IBM 1627 MODEL I PLOTTERe THE 
PLOTTING SCALE IS A VARIABLE INCORPORATED IN THE PROGRAM, SINCE PERME- 
ABILITY VALUES FOR FINE-GRAINED SOILS VARY THROUGHOUT A WIDE RANGEe 
REF. NCEL REPORT R-566«e AUTHOR--— MELVIN Ce HIRONAKAe 


PAGE 030 


UeSe NAVAL CIVIL ENGINEERING LABORATORY 
PORT HUENEME» CALIFORNIA 93041 


SETTLEMENT ANALYSIS LANGUAGE - FORTRAN II-D 
COMPUTER —- IBM 1620 II 
(COPY ON FILE AT NODC) 
ESTIMATES SETTLEMENT VALUES FROM LABORATORY TEST RESULTS» FOR DEEP 
OCEAN FOUNDATION INVESTIGATIONSe INPUT ARE SEDIMENT PROPERTIES AND 
STRUCTURE CHARACTERISTICSe OUTPUT IS A TABLE LISTING TOTAL SETTLE- 
MENT» FOOTING DIMENSIONS» STRUCTURE LOAD, CHANGE IN THICKNESS OF IN- 
CREMENTAL LAYERS AT CORRESPONDING DEPTH IN SEDIMENT» INITIAL STRESS» 
AND CHANGE IN STRESSe EQUATIONS, ETCe,s DESCRIBED IN AN NCEL REPORT» 
NOe R-566s BY MELVIN Ce HIRONAKAc 


UeSe NAVAL CIVIL ENGINEERING LABORATORY 
PORT HUENEME» CALIFORNIA 93041 


SUMMARY PLOTS LANGUAGE — FORTRAN II-D 
COMPUTER - IBM 1620 II 
(COPY ON FILE AT NODC) 

PLOTS THE RESULTS FROM THE LABORATORY ANALYSIS OF CORE SAMPLESe THE 
INPUT DATA ARE THE OUTPUT RESULTS ON CARDS FROM THE PREVIOUS PROGRAMS 
AND MISCELLANEOUS ANALYSESe SINCE THE LINK SYSTEM OF PROGRAMMING IS 
USED, THE ITEMS TO BE PLOTTED CAN BE INCREASED oR DECREASED wITH 
SLIGHT MODIFICATIONSs DEPENDING ON THE USER'S REQUIREMENTSe OUTPUT IS 
A SEQUENCE OF PLOTSe THE DEPTH INTO THE SEDIMENT COLUMN IS PLOTTED 
WITH REFERENCE TO THE ORDINATEs AND THE VARIOUS PROPERTIES ALONG THE 
ABSCISSA ON VARIABLE SCALESe REFe A TECHNICAL REPORT NOe R-566 'COM- 
PUTER REDUCTION OF DATA FROM ENGINEERING TESTS ON SOILS AND OCEAN SED- 
IMENTS'e AUTHOR-- MELVIN Ce HIRONAKA» NCELe 


UeSe NAVAL CIVIL ENGINEERING LABORATORY 
PORT HUENEMEs CALIFORNIA 93041 


BKGEOL (SEDIMENT ANALYSIS STATISTICS) LANGUAGE - FORTRAN IV 
COMPUTER - IBM 7094-II/ 
7040 DCS 


(COPY ON FILE AT NODC) 
MODIFICATION OF UeWe ROUTINE 213 FOR THE 709 PREPARED IN FORTRAN II BY 
EeEe COLLIAS AND MeRe RONA (REFe TECHe REPORT NOe 875 1963)e ACCEPTS 
INPUT DATA IN A MORE ELEMENTARY FORM THAN PREVIOUS PROGRAM AND THE AN- 
ALYST MAKES NO CALCULATIONSe INCLUDES PROVISION FOR COMPENSATING FOR 
VARIATIONS IN DENSITYs TEMPERATUREs AND ERRORS IN PIPETTING DEPTH AND/ 
OR TIMEe OUTPUT IS A LIST OF INPUT DATAs LIST OF COMPONENT» RATIOs 
TRASKs INMANs AND FOLK AND WARD STATISTICS» SHEPARD DIAGRAM INFORMA-— 
TION AND PASSEGA'S C-M VALUESe OPTIONAL PUNCH CARD OUTPUTe PROGRAM 
DATE-— MAY 1966. AUTHOR-- WILLIAM ANIKOUCHINEs JORGs ESSAe (A PLOT 
ROUTINE WAS PREPARED TO GRAPH PERCENTILE VS PHI-SIZES FROM THE RESULTS 
OF THE MAIN PROGRAMe) 


We ANIKOUCHINEs RESe ASSOCIATE 
JORG-ESSA»s C/O DEPTe OF OCEANOGRAPHY 
UNIVERSITY OF WASHINGTON 

SEATTLE» WASHe 98105 


CONDU LANGUAGE - FORTRAN IV 
COMPUTER - IBM 7094-II/ 
7040 DCS 


(COPY ON FILE AT NODC) 
CALCULATES THERMAL CONDUCTIVITY OF MARINE SEDIMENTS FROM DATA OBTAINED 
WITH A TRANSIENT TYPE NEEDLE PROBE (ALPINE MODEL 328)e TEMPERATURE- 
MILLIVOLT CALIBRATION TABLES ARE INPUT AS DATAs WITH LINEAR INTERPOLA- 
TION EMPLOYED IN THE TABLE LOOK-UP SUBROUTINE» ADJACENT PAIRS OF TIME 
AND TEMPERATURE VALUES ARE USED TO CALCULATE CONDUCTIVITY VALUESe VAL- 
UES LYING OUTSIDE OF TWO STANDARD DEVIATIONS ARE REJECTEDe OUTPUT IS 


PAGE 031 


LISTING AND PLOTSe THE BEST CONDUCTIVITY VALUE IS COMPUTED AND PRINT— 
EDe AUTHOR-- WILLIAM ANIKOUCHINE»s JOINT OCEANOGRAPHIC RESEARCH GROUP 
(JORG> ESSA)» UNIVe OF WASHINGTONe A COPY OF THIS PROGRAM IS AISO ON 
FILE WITH THE PACIFIC OCEANOGRAPHIC LABORATORY, 1801 FAIRVIEW AvEe 
EAST» SEATTLE, WASHe,y MRe THEODORE Ve RYAN» DIRECTOR. 


RADMe HAROLD Je SEABORG 

DIRECTOR» PACIFIC MARINE CENTER 
COAST AND GEODETIC SURVEY» USESSA 
1801 FAIRVIEW AVENUE, EAST 
SEATTLE» WASHe 98102 


SEDIMENT GRANULOMETRIC ANALYSIS (UWMS-1003) LANGUAGE —- FORTRAN IV 
AND MAP 
COMPUTER — IBM 7094-II/ 
7040 DCS AND 
cDC 6400 
(COPY ON FILE AT NODC) ; 
THE OUTPUT LISTS INPUT DATA, COMPUTED FRACTION PERCENTAGESs ACCUMULAT-— 
ED PERCENTAGES» WEIGHT PERCENTAGES OF GRAVEL» SAND» SILTs AND CLAYs 
SAND/MUD RATIOs SHEPARD CLASS» TETRAHEDRAL GROUP» PHI-SIZES AT CERTAIN 
PERCENTILESs TRASK» INMAN»s FOLK AND WARD VALUES» AND MOMENTS MEASURES 
WITH AND WITHOUT SHEPARD!S CORRECTIONSe REFe A REPORT (UWMS-1003, 
AUG 1966) BY THE DEPTe OF OCEANOGRAPHYs APPLIED MATHEMATICS SECTIONe 
CORE STORAGE NECESSARY-- 5327 WORDSe SOURCE DECK HAS 775 CARDS. RE- 
VISED 1969 FOR THE CDC-6400, 


He MACINTOSHs COMPUTER SERVICES 
DEPARTMENT OF OCEANOGRAPHY 
UNIVERSITY OF WASHINGTON 
SEATTLE» WASHe 98105 


SEDIMENT TEXTURAL ANALYSIS LANGUAGE — FORTRAN 
COMPUTER -— (NOT GIVEN) 
(COPY ON FILE AT NODC) 
A COMPREHENSIVE PROGRAM, DESIGNED FOR SMALL COMPUTERS» FOR THE TEX- 
TURAL ANALYSIS OF GROUPED SEDIMENT DATA, INCLUDING SIEVED AND PIPETTED 
SAMPLESe THE PROGRAM CONVERTS THE RAW WEIGHTS OF SIZE-GRADED SEDIMENT 
INTO WEIGHT PERCENTS» CUMULATIVE PERCENTSs AND A FREQUENCY HISTOGRAM. 
COMPUTED STATISTICS INCLUDE-- PERCENTS OF GRAVEL» SAND» SILT» AND CLAY 
FoR LITHOFACIES ANALYSIS» AND MEANs STANDARD DEVIATIONs SKEWNESS» AND 
KURTOSIS» COMPUTED BY THE METHODS OF MOMENTS» TRASKs INMAN» AND FOLK 
AND WARDe REFe A REPORT (UNPUBLISHED) JULY '695 27 Ps BY SAM UPCHURCHe 


DIRECTOR 

GREAT LAKES RESEARCH CENTER 

DEPTe OF THE ARMY» CORPS OF ENGINEERS 
LAKE SURVEY DISTRICT 

DETROIT» MICHIGAN 48226 


PAGE 032 


GRAPHICAL DISPLAY 
HHH —H-H—-HKH- KKH 


GEOLOGICAL SAMPLING INVENTORY PLOT LANGUAGE — FORTRAN 
COMPUTER -— IBM 7074 AND 


CALCOMP 564 
(COPY ON FILE AT NODC) 


DISPLAYS GEOLOGICAL SAMPLING INVENTORY DATA AND LOCATION ON CALCOMP 
PLOTSs GIVEN THE MARSDEN SQUARE OR ADJACENT RECTANGULAR ARRAY OF 
MARSDEN SQUARESe INPUT IS THE NODC GEOSORTED FILE OF GEOLOGICAL 
DATAse AUTHOR-— ROBERT VAN WIEe 


COMPUTER SYSTEMS DIVISION», CODE 2400 
NATIONAL OCEANOGRAPHIC DATA CENTER 
WASHINGTONs DeCe 20390 


BOTTOM SEDIMENT DISTRIBUTION PLOT LANGUAGE - FORTRAN 
COMPUTER —- IBM 7074 W/ 


CALCOMP 564 
(COPY ON FILE AT NODC) 


PLOTS BOTTOM SEDIMENT NOTATIONS ON A MERCATOR PROJECTION OF ANY NUMBER 
OF DEGREES OF LATITUDE AND LONGITUDE AND TO A SPECIFIED SCALE* CALCOMP 
SUBROUTINES ARE USEDs ALSO A COUNT SUBROUTINE DESIGNED BY MRe WALTER 
YERGEN OF THIS DIVISIONe REFe IMR NOe O-10-665 MAY 1966 (UNPUBIISHED 
MANUSCRIPT)» BY ReJe VAN WYCKHOUSEs WHICH LISTS AN EARLIER PRUGRAM FOR 
PRIMARY GRAIN SIZE» AND AN INFORMAL REPORT IR NOe 68-495 JULY 19689 BY 
FREDERICK MAASe DDC USERS MAY OBTAIN COPIES OF THE LATTER REPORT DIR- 
ECTLY FROM DDC», OR THROUGH THE COMMANDER» NAVAL OCEANOGRAPHIC OFFICE, 
ATTNe CODE 40. 


OCEANOGRAPHIC ANALYSISs GEOLOGY SECeo 
NAVAL OCEANOGRAPHIC OFFICE 
SUITLANDs MDe 20390 


BIOP (BIOLOGY PLOT) LANGUAGE - FORTRAN IV 
COMPUTER - CDC 3600s 
CDC 160A 


DOES POSITION (LATITUDE, LONGITUDE) PLOTTING OF BIOLOGICAL SPECIES ON 
THE CALIFORNIA OFFSHORE IN MERCATOR PROJECTIONe AUTHORS-- MRe MANLEY » 
Le We YOUNGe 


MARINE LIFE RESEARCH GROUP 

SCRIPPS INSTITUTION OF OCEANOGRAPHY 
PeOe BOX 109 

LA JOLLA» CALIFORNIA 92037 


MATHEMATICAL SIMULATION OF MARINE SEDIMENTATION LANGUAGE - FORTRAN IV 
COMPUTER — IBM 7040 AND 
IBM 7094 


BY MATHEMATICAL-MEANSs IN SYMBOLIC THREE-DIMENSIONAL SPACE» THE MODEL 
IMITATES THE PROCESSES OF TECTONIC WARPINGs WINNOWING OF SEDIMENTS 
ALONG BEACHESs FORMATION OF DELTASs AND THE GROWTH AND INTERACTION OF 
ORGANISM COMMUNITIES» INCLUDING ALGAL BANKS AND CORAL REEFSe THE MODEL 
IS RUN FORWARDs BY INCREMENTS» THROUGH GEOLOGIC TIMEe OUTPUT IS IN 
THE FORM OF LITHOFACIES MAPSs STRUCTURE MAPS», BIOFACIES MAPS» SEA WA- 
TER DEPTH MAPS» AND GEOLOGICAL CROSS SECTIONS THAT SHOW BOTH STRUCTURE 
AND FACIES RELATIONSHIPSe COMPUTER CONTRIBUTION 95 BY JeWe HARBAUGH 
AND WeJe WAHLSTEDT» 1967e 


DRe DANIEL Fe MERRIAMs EDITOR 
COMPUTER CONTRIBUTIONS 
KANSAS GEOLOGICAL SURVEY 


PAGE 033 


THE UNIVERSITY OF KANSAS 
LAWRENCE» KANSAS 66044 


VECTOR TREND ANALYSIS OF DIRECTIONAL DATA LANGUAGE - FORTRAN IV 
COMPUTER — IBM 7090/94 


ANALYZES REGIONAL TRENDS IN DIRECTIONAL DATAe ORTHOGONAL POLYNOMIAL 
RESPONSE SURFACES ARE COMPUTED AND PLOTTED AS ISOAZIMUTH AND VECTOR 
TREND MAPS TO AID IN INTERPRETING REGIONAL FLOW PATTERNSe EXAMPLES 
ARE GIVEN OF THE STUDY OF THE DISTRIBUTION OF CURRENTS WHICH EXISTED 
WHEN A SEDIMENT WAS DEPOSITEDe REFe COMPUTER CONTRIBUTION ll» BY 
WILLIAM Te FOX (1967)e 


DRe DANIEL Fe MERRIAMs EDITOR 
COMPUTER CONTRIBUTIONS 

KANSAS GEOLOGICAL SURVEY 

THE UNIVERSITY OF KANSAS 
LAWRENCEs KANSAS 66044 


SIMULATION OF DELTAIC SEDIMENTATION LANGUAGE — FORTRAN IV-H 
COMPUTER — IBM 360/67, 
CALCOMP 


A SEDIMENT-LADEN RIVER FLOWING INTO A TIDELESSs CURRENTLESS MARINE BA- 
SIN IS MODELED AS A PLANE JET DISCHARGING HORIZONTALLY AT THE OCEAN 
SURFACEe A VELOCITY FIELD IS CALCULATED USING EQUATIONS FOR OPEN- 
CHANNEL AND PLANE JET FLOWe SEDIMENT BEHAVIOR IS TREATED STATISTICAL— 
LYe NOMINAL SEDIMENT PARTICLES ARE TRACED ALONG TRAJECTORIES FROM THE 
MOUTH AS THEY SPREAD LATERALLY AND SETTLE VERTICALLYe A DYNAMIC MODEL 
PERMITS A DELTA TO BUILD FORWARD DURING SEVERAL TIME INCREMENTS» NOM- 
INAL PARTICLE TRAJECTORIES ADJUSTING AUTOMATICALLY TO THE POSITION OF 
THE DELTA LIP. AUTHORS-- GeFe BONHAM-CARTER AND AeJe SUTHERLANDe 
COMPUTER CONTRIBUTION 24 (APR 1968). 


DRe DANIEL Fe MERRIAMs EDITOR 
COMPUTER CONTRIBUTIONS 

KANSAS GEOLOGICAL SURVEY 

THE UNIVERSITY OF KANSAS 
LAWRENCEs KANSAS 66044 


AUTOMATIC CONTOURING 


(ABSTRACT NOT RECEIVED.) COMPUTER CONTRIBUTION 23 "COMPUTER PROGRAMS 
FOR AUTOMATIC CONTOURING',s BY DeBe MC INTYRE»s DeDe POLLARD» AND Re 
SMITHs (1968). 


DRe DANIEL Fe MERRIAMs EDITOR 
COMPUTER CONTRIBUTIONS 

KANSAS GEOLOGICAL SURVEY 

THE UNIVERSITY OF KANSAS 
LAWRENCEs KANSAS 66044 


GRIDIT» REGRIDIT» AUTOMATED CONTOUR LANGUAGE - FORTRAN 
COMPUTER - (NOT GIVEN) 
(COPY ON FILE AT NODC) 
THREE PROGRAMS WHICH ENABLE THE USER TO GRAPHICALLY PRODUCE A CONTOUR 
MAP BY THE COMPUTER-PLOTTER METHOD. THE GRIDIT PROGRAM PRODUCES A 
DIGITIZED MATRIX FROM DATA POINTS WHICH HAVE BEEN SCREENED FOR GROSS 
ERRORS» REGRIDIT PRODUCES A DIGITIZED MATRIX FROM RAW UNCHECKED DATA 
POINTSe AUTOMATED CONTOUR CONSTRUCTS A CONTOUR CHART FROM A DIGITIZED 
MATRIXe AN EXAMPLE IS GIVEN FOR USE OF THE PROGRAM IN CONTOURING THE 
BATHYMETRY OF OCEAN BOTTOMe REFs IM NOw 67-4 (INFORMAL MANUSCRIPT) 
‘AN AUTOMATED PROCEDURE FOR PRODUCING CONTOUR CHARTS', BY ROGER Te 
OSBORN» FEBe 1967. 


HYDROGRAPHIC DIVes CODE 8100 


PAGE 034 


NAVAL OCEANOGRAPHIC OFFICE 
SUITLAND» MDe 20390 


FAA PLOT LANGUAGE - FORTRAN 
COMPUTER — I8M 7074 
(COPY ON FILE AT NODC) 

ACCEPTS THREE CARD IMAGES AND A SUPPLIED SET OF FAA DATA CARDS AS IN- 
PUTe THE OUTPUT IS A MAGNETIC TAPE TO DRIVE THE E-51,s E-103»5 OR THE 
E-108 CONCORD DIGITAL PLOTTERS USING THE ECHELON MODE.’ THE END PRO- 
DUCT IS A FILM POSITIVE WITH A PLUS SYMBOL FOR THE POSITION OF THE FAA 
PLOTSe THE MERCATORs TRANSVERSE MERCATORs AND LAMBERT CONIC CONFORMAL 
PROJECTION WITH TWO STANDARD PARALLELS ARE THE THREE PROJECTIONS WHICH 
CAN BE USED TO PLOT PROGRAM OUTPUTSe OcSe NO 656526 AUTHORS-— RONALD 
Me BOLTON AND Je PARRINELLO}’ 


NAUTICAL CHART DIVISIONs CODE 5620 
NAVAL OCEANOGRAPHIC OFFICE 
SUITLAND» MDe 20390 


SOUNDING PLOT LANGUAGE — FORTRAN 
COMPUTER - CDC 3100 AND 
IBM 7074 


ACCEPTS LORACs LORAN»s OR RAYDIST LANE VALUESe SHIPS TRACK AND SOUND- 
INGS ARE PLOTTED ON THE CALCOMP. PRIMARY VERSION IS FOR THE CDC-3100 
COMPUTERe AN OBJECT DECK FOR IBM 7074 WILL BE PRODUCEDe PLOTTING IS 
DONE IN UTM MODEe OS NOce 58419e¢ AUTHOR-- GeRe BILLSe 


GEODESY DIVISIONs CODE 8420 
NAVAL OCEANOGRAPHIC OFFICE 
SUITLAND» MDe 20390 


THREE-DIMENSTONAL SURFACE PLOTS LANGUAGE - FORTRAN 
COMPUTER - CDC 3800 


SUBROUTINE '"SURFACE* ALLOWS THREE-DIMENSIONAL PLOTS TO BE GENERATED ON 
THE 565 CALCOMP PLOTTERe THIS SUBROUTINE WILL PRODUCE A SURFACE PLOT 
OF DATA THAT CAN BE REDUCED TO ONE SINGLE-VALUED DEPENDENT AND TWO IN- 
DEPENDENT VARIABLESe NRL MEMO’ REPORT 2015¢ AUTHOR-- Je MOORE 


JOHN Ce MOORE 

RADAR TECHNIQUES 

RADAR DIVISION 

NAVAL RESEARCH LABORATORY» WASHINGTON» De Ceo 20390 


LINE PRINTER PLOTS LANGUAGE — FORTRAN» 
COMPASS 
COMPUTER - CDC 3800 


A SUBROUTINE PACKAGE WRITTEN AT THE UNIVERSITY OF WISCONSIN TO PRODUCE 
LINE PRINTER PLOTS HAS BEEN MODIFIED TO RUN ON NRL'S CDC 3800 . NRL 
MEMOe REPORT 20466 AUTHOR-- De DENTONe 


DIANNA Le DENTON 

RESEARCH COMPUTATION CENTER 

MATHEMATICS AND INFORMATION SCIENCES DIVISION 
NAVAL RESEARCH LABORATORY» WASHINGTON» De Ce 20390 


PLOT THETA-S CURVES LANGUAGE — FORTRAN II 
COMPUTER - CDC 3100/ 
PDP-8 AND 

CALCOMP 


PLOTS POTENTIAL TEMPERATURE VSe SALINITYe CARD INPUT» OUTPUT PRINTED 
LISTING AND PUNCHED PAPER TAPEe STATION PLOT USES A PDP-8 COMPUTER» 


PAGE 035 


PLOT 


PAPER TAPE READER» AND CALCOMPe AUTHOR-- Re REINIGERe 


DIRECTOR 

ATLANTIC OCEANOGRAPHIC LABORATORY 
BEDFORD INSTITUTE 

DARMOUTHs NOVA SCOTIA» CANADA 


STATION POSITIONS LANGUAGE - FORTRAN II 
COMPUTER — CDC 3100/ 
PDP-—8 AND 

CALCOMP 


PLOTS CRUISE STATION POSITIONS ON MERCATOR'S PROJECTION AND WRITES IN 
STATION NUMBERe 'PLOTL* PLOTTING ROUTINE USED WITH PDP-8 COMPUTER AND 
THE CALCOMPe AUTHOR-— Re REINIGER (SEPT 1968). 


DIRECTOR 

ATLANTIC OCEANOGRAPHIC LABORATORY 
BEDFORD INSTITUTE 

DARTMOUTHs NOVA SCOTIA» CANADA 


SECTION PLOTTING LANGUAGE — FORTRAN 
COMPUTER - CDC 3100/ 
PDP-8 AND 

CALCOMP 


CG 


TIME 


(C 


PLOG 


OPY ON FILE AT NODC) 

THE PROGRAM USES THE CDC 3100 PLOTTING SUBROUTINES TO GENERATE DATA 
FOR THE PDP-8 PLOTTING PROGRAMe THE USER MAY SPECIFY A LEGEND (UP TO 
480 CHARACTERS)» LABEL SIZES» SCALE FACTORS» THE PARAMETER TO BE PLOT- 
TED AND THE ISOPLETHS TO BE DETERMINEDe THE PLOTTING IS DONE ON A 
CALCOMP 31 IN. PLOTTER UNDER CONTROL OF THE PDP-8. CRUISE DATA IS 
READ FROM MAGNETIC TAPE BY THE CDC 3100 IN MODIFIED CODC FORMAT OR BI 
FORMATe STORAGE REQUIREMENTS—— 11000(8) IN THE CDC 3100 (INCLUDING 
PLOTTING SUB-PROGRAMS)e AN ITERATIVE METHOD IS USED IN CONJUNCTION 
WITH AN INTERPOLATION FUNCTION TO DETERMINE ISOPLETH DEPTHSe THE IN- 
TERPOLATION FUNCTION IS DESCRIBED IN A BEDFORD INSTITUTE REPORT, BIO 
66-3 (FEB 1966, UNPUBLISHED MANUSCRIPT) BY ReFe REINIGER AND CeKe ROSS 


DIRECTOR 

ATLANTIC OCEANOGRAPHIC LABORATORY 
BEDFORD INSTITUTE 

DARTMOUTHs NOVA SCOTIA» CANADA 


SERIES PLOTTING LANGUAGE — FORTRAN 32 
COMPUTER — CDC 3100/ 
PDP-8 AND 
CALCOMP 


OPY ON FILE AT NODC) 

THE PROGRAM USES THE CDC 3100 PLOTTING SUBROUTINES TO GENERATE DATA 
FOR THE PDP-8 PLOTTING PROGRAMe THE USER MAY SPECIFY A LEGEND (uP TO 
480 CHARACTERS), LABEL SIZES» SCALE FACTORS» THE PARAMETER TO BE PLOT-— 
TED AND THE ISOPLETHS TO BE DETERMINEDe THE PLOTTING IS DONE ON A 
CALCOMP 31 INe PLOTTER UNDER CONTROL OF THE PDP-8e CRUISE DATA IS 
READ FROM MAGNETIC TAPE BY THE CDC 3100 IN BI FORMATe TIME IS PLOTTED 
ALONG THE X AXIS (DRUM MOVEMENT) AND DEPTH ALONG THE Z AXIS (PEN MOVE- 
MENT)» STATIONS ARE PLOTTED TO THE NEAREST DAYe AUTHOR=— DeJe LAWR- 
ENCE (06/06/69). 


DIRECTOR 

ATLANTIC OCEANOGRAPHIC LABORATORY 
BEDFORD INSTITUTE 

DARTMOUTHs NOVA SCOTIAs CANADA 


LANGUAGE —- FORTRAN IV 
COMPUTER ~- IBM 1130/1BM 


PAGE 036 


1627 PLOTTER 
(COPY ON FILE AT NODC) 
PLOTS THE RESULTS OF HYDROGRAPHIC CASTS IN A FORMAT SUITABLE FOR PUB- 
LICATIONe PRODUCES 8 1/2 BY 10 INe PLOTS OF LOG(10}DEPTH VSe TEMPERA- 
TUREs SALINITY» AND OXYGENe 


DRe Ce Ae COLLINS 

MARINE SCIENCES BRANCH» DEMR 
PACIFIC OCEANOGRAPHIC GROUP 
BIOLOGICAL STATION 

NANAIMO» BeCes CANADA 


STPO1 LANGUAGE — FORTRAN IV 
COMPUTER — IBM 1130/1BM 
1627 PLOTTER 
(COPY ON FILE AT NODC) 
PLOTS DIGITIZED SeTeDe DATA IN A FORMAT SUITABLE FOR PUBLICATIONe THE 
PLOTTER DRAWS AND LABELS AXES AND PLOTS TEMPERATURE AND SALINITY VSe 
DEPTHe 


DRe Ce Ae COLLINS 

MARINE SCIENCES BRANCH» DEMR 
PACIFIC OCEANOGRAPHIC GROUP 
BIOLOGICAL STATION 

NANAIMO» BeCes CANADA 


PSAL1 (PLOT TEMPERATURE-SALINITY) LANGUAGE -— FORTRAN VI 
COMPUTER -— IBM 1130 
(COPY ON FILE AT NODC) 
PLOTS T-S AND EXPANDED T-S CURVESe INPUT—- HYDROGRAPHIC DATA IN CODC 
FORMATe ANOTHER PROGRAMs PSAL3»s PLOTS OXYGEN-SALINITY AND TEMPERA- 
TURE-OXYGEN CURVESe REFe FRB MSe REPORT NOe 1071 (DEC 1969)» BY CeAe 
COLLINS» RelLeKe TRIPE AND SeKe WONGe 


PACIFIC OCEANOGRAPHIC GROUP 
BIOLOGICAL STATION 
NANAIMOs BeCes CANADA 


GENERAL PURPOSE PLOT AND 'SPECTDPLOT® LANGUAGE — FORTRAN 
COMPUTER - IBM 7074 W/ 
CALCOMP 


(COPY ON FILE AT NODC} 
TWO PROGRAMS WITH CONSIDERABLE GENERALITY WHICH ALLOW THE USER TO DE- 
FINE HIS ORIGIN» SCALE FACTORSs GRID ANNOTATION AND DATA SET» OR ANY 
NUMBER OF DATA SETSe AN ADDED PROVISION ALLOWS DATA RECORDED IN THE 
FIELD (IeEe ABOARD RESEARCH SHIPS)» TO BE PROCESSED DIRECTLY FROM THE 
FIELD TAPES WITH A MINIMUM OF PREPARATORY PROCESSINGe EITHER THE ROT- 
ARY-TYPE OR FLAT-BED PLOTTER MAY BE USEDe OS NOSe 20255 AND 202646 
INFORMAL REPORT REFe NOe IR 69-65 (AUG 19695 70P)e AUTHOR-- ERNEST Le 
MABREYe FURTHER INFORMATION MAY BE OBTAINED FROM THE DISSEMINATION 
DEPTe (CODE 44)» OR THE AUTHOR. 


SCIENTIFIC APPLICATIONS DIVe.s CODE 0831 
COMPUTER DEPARTMENT 

NAVAL OCEANOGRAPHIC OFFICE 

SUITLAND» MDe 20390 


SHIPBOARD SURVEY SYSTEM —- ON-STATION PLOT LANGUAGE - FORTRAN 
COMPUTER — IBM 7074 
PLOTS SALINITY» SOUND SPEED, TEMPERATURE» AND AMBIENT LIGHT VERSUS 
DEPTHe INPUT IS FROM PROGRAM NOe 101322. AUTHOR-- Je WARDENe OS NO, 
10131. 


COMPUTER DEPARTMENT» CODE 083 
NAVAL OCEANOGRAPHIC OFFICE 


PAGE 037 


SUITLAND» MDe 20390 


PROFL LANGUAGE —- FORTRAN IV 
COMPUTER -— CDC 3600 


PLOTS DATA VALUES AGAINST DEPTH OR OTHER PARAMETERSe 


MRe DAVID WIRTH 

OCEANIC RESEARCH DIVISION 

SCRIPPS INSTITUTION OF OCEANOGRAPHY 
PeOw BOX 109 

LA JOLLA» CALIFORNIA 92037 


OCEANOGRAPHIC STATION CURVE PLOTTING FOR 1401 LANGUAGE -— AUTOCODER 
COMPUTER —- IBM 1401 
(COPY ON FILE AT NODC) 
USES A PLOT AND SYMBOL ROUTINE FOR THE IBM 1401. VARIABLES SCALED IN- 
CLUDE DEPTH» TEMPERATURE» SALINITYs SIGMA-Ts DELTA ALPHA s OXYGEN» AND 
PHOSPHATE* AUTHOR-— DeLe SHAFFER» INSTITUTE OF MARINE SCIENCE’ 


UNIVERSITY OF MIAMI 

MARINE LABORATORY 

COMPUTER CENTER 

1 RICKENBACKER CAUSEWAY 
VIRGINIA KEYs MIAMI» FLORIDA 


THE VORTEX OCEAN MODEL LANGUAGE -— DECAL 
COMPUTER - PDP-7(9) 


SIMULATES A VORTEX OCEAN MODEL AND DISPLAYS RESULTS ON COMPUTER SCOPE. 
COLLECTS STATISTICS ON THE MODELe RESEARCHER CAN CONTROL THE CONF IGU- 
RATION OF THE SIMULATION» MAY AT ANY TIME DURING COMPUTATION EXAMINE 
OR CHANGE THE VALUE OF ANY VARIABLEe IN THE MODEL» A SET OF VORTICES 
INTERACT IN A CIRCULAR OR UNBOUNDED OCEANe NUMBER OF VORTICES CAN BE 
VARIED FROM 1 TO 3le ALSO» A SPECIAL TEST POINT USED TO COLLECT STAT- 
ISTICS ON THE EFFECTS OF THE VORTICESe EACH VORTEX ROTATES WITH A 
STRENGTH, WHERE THE (1)TH VORTEX ROTATES WITH STRENGTH S(I)e THE RO- 
TATION OF EACH VORTEX AFFECTS THE POSITION OF ALL OTHERSe OPERATION 
IS SUFFICIENTLY FAST TO SHOW SEVERAL VORTICES IN OPERATIONs FLICKER- 
FREEe PROGRAM IS CONTROLLED FROM AN ON-LINE TYPEWRITER VIA CONTROL 
CHARACTERSe PROGRAM WRITEUP IS AVAILABLE ON REQUEST. 


DRe DANIEL Me FORSYTH 
INFORMATION INTERNATIONAL» INCe 
89 BRIGHTON AVENUE 

BOSTONs MASSACHUSETTS 02134 


WORLD OCEANOGRAPHIC DATA DISPLAY LANGUAGE — DECAL 
COMPUTER — PDP-7(9) 


THE WODD SYSTEM ENABLES A RESEARCHER TO CONDUCT AN ANALYSIS OF OCEANO- 
GRAPHIC DATA USING A SERIES OF VISUAL DISPLAYS GENERATED BY A DIGITAL 
COMPUTERe THE EVENTUAL GOAL OF THE SYSTEM WILL BE TO HOLD AND MAKE A- 
VAILABLE FOR DISPLAY THE ENTIRE BODY OF WORLD OCEANOGRAPHIC DATAe THE 
RESEARCHER WILL BE ABLE TO SELECT SPECIFIC DATA FOR DISPLAYs IN THE 
FORM OF CONTOUR LINES AGAINST A MAP OF SELECTED OCEANIC DATAes HE WILL 
BE ABLE TO VARY THE PARAMETERS OF THE DATA SELECTED AND OBSERVE THE 
RESULTING VARIATIONS IN THE CONTOUR LINESe AT ITS PRESENT STAGE OF 
DEVELOPMENT» THE SYSTEM CONSISTS OF A PDP-7 COMPUTER» A CATHODE RAY 
TUBE VISUAL DISPLAY UNIT» A MAGNETIC TAPE UNIT» A LIGHT PEN» INPUT- 
OUTPUT TYPEWRITERe BROCHURE DESCRIBING SYSTEM IS AVAILABLE ON REQUEST 


DRe DANIEL Me FORSYTH 
INFORMATION INTERNATIONAL» INCe 
89 BRIGHTON AVENUE 

BOSTONs MASSACHUSETTS 02134 


PAGE 038 


MACHINE PLOTTING ON MERCATOR-PROJECT ION LANGUAGE — FORTRAN 
COMPUTER - CDC 1604 W/ 
CALCOMP 165 
(COPY ON FILE AT NODC) 
UTILIZES MERIDIONAL PARTS TO LOCATE DATA POINTS ON MERCATOR-PROJECTION 
MAPSe FORTRAN PROGRAM USES A SHARED-TIME PLOTTING ROUTINEe THE CON-— 
TINENT OUTLINES CAN ALSO BE PLOTTED BY STRAIGHT-LINE SEGMENTSe REF e-- 
NUWC TP 89 (DEC 19685 44 Pe)e AUTHOR-- LeAw SMOTHERSe PROGRAMMER-— 
KeKe STARRe 


OCEAN SCIENCES DEPARTMENT 
NAVAL UNDERSEA RESEARCH AND DEVELOPMENT CENTER 
SAN DIEGO» CALIFORNIA 92132 


VACOTS (VERTICALLY ANALYZED CONTOURS OF LANGUAGE — FORTRAN 63 
OCEANOGRAPHIC TEMPERATURES AND SALINITIES) COMPUTER -— CDC 3600 W/ 
CALCOMP 


(COPY ON FILE AT NODC) 
PROVIDES A RAPID AND ACCURATE MEANS OF CONSTRUCTING VERTICAL CROSS-— 
SECTIONS OF SEA TEMPERATURES AND SALINITIESe ALTHOUGH THIS PROGRAM 
HAS BEEN DESIGNED TO USE SeTeDe DATA RECORDED ON MAGNETIC TAPE, OTHER 
VERSIONS ALSO ARE BEING USED TO CONTOUR BIOLOGICAL» CHEMICAL AND OTHER 
PHYSICAL OCEANOGRAPHIC DATA. EACH VERTICAL SECTION IS DIVIDED INTO 
TWO PARTS — THE UPPER SECTION FOR THE CONTOURS FROM SURFACE TO 300 Me 
AND THE LOWER SECTION FROM 300 Me TO 1000°Me CORE MEMORY SIZE NEEDED 
— 32,000 WORDSe RUNNING TIME-- TO ANALYZE AND PLOT CONTOURS AT INTER- 
VALS OF 1 DEGREE Ce FOR TEMPERATURE AND el 0/00 FOR SALINITY FROM THE 
SURFACE TO 1000 Me FOR 50 STATIONS REQUIRES 4 MINUTES OF COMPUTER TIME 
ON THE CDC 3600 AND 25 MINUTES ON THE CALCOMP 30 INe PLOTTERe AUTHOR 
— FORREST MILLER. 


BUREAU OF COMMERCIAL FISHERIES 
PeO5e BOX 271 
LA JOLLA» CALIFORNIA 92038 


TEMPERATURE-SALINITY PLOT LANGUAGE — FORTRAN 
COMPUTER - CDC 3100/ 
CALCOMP 750 
(COPY ON FILE AT NODC) 
PROVIDES FOR THE PRODUCTION OF TEMPERATURE-SALINITY DIAGRAMS FROM 
SERIAL OCEANOGRAPHIC OBSERVATIONSe INPUT IS DATA CARDS AND A PLOT 
CONTROL CARDe OUTPUT IS PLOTTER TAPE AND A PRINTED SUMMARY OF OQUT-OF- 
RANGE DATAe REFe MS REPORT NOe 6 (1967)e AUTHOR-- JeRe WILSUNe 


OCEANOGRAPHIC RESEARCH DIVISION 
MARINE SCIENCES BRANCH 

DEPTe OF ENERGY» MINES AND RESOURCES 
OTTAWAs CANADA 


TEMPERATURE-SALINITY CURVES LANGUAGE — FORTRAN IV 
COMPUTER - IBM 360/655 
CALCOMP 


(COPY ON FILE AT NODC) 
PLOTS TEMPERATURE VSe SALINITY CURVES ON 12 INe PLOTTER» EITHER SINGLE 
OR MULTIPLE STATIONS. INPUT IS ICES FORMAT HYDROGRAPHIC DATAe CORE 
STORAGE USED-- 31K BYTES (INCLUDES PLOT ROUTINES)» AUTHOR-— MARILYNN 
BORKOWSKIe 


BUREAU OF COMMERCIAL FISHERIES 

TROPICAL ATLANTIC BIOLOGICAL LABORATORY 
75 VIRGINIA BEACH DRIVE 

MIAMI,5 FLORIDA 33149 


OXYGEN» PHOSPHATEs DENSITY PLOTS LANGUAGE - FORTRAN IV 
COMPUTER — IBM 360/655 
CALCOMP 


PAGE 039 


(COPY ON FILE AT NODC) 
PLOTS OXYGEN VSe PHOSPHATE» OXYGEN VSe SIGMA-T» AND PHOSPHATE VSe SIG- 
MA-T (SINGLE OR MULTIPLE STATION) FOR PURPOSES OF QUALITY CONTROL AND 
STUDY OF WATER TYPESe INPUT IS HYDROGRAPHIC DATA IN ICES FORMATe CORE 
STORAGE USED-- 33K BYTES INCLUDING PLOT ROUTINESe AUTHOR-- MARILYNN 
BORKOWSKI. 


BUREAU OF COMMERCIAL FISHERIES 

TROPICAL ATLANTIC BIOLOGICAL LABORATORY 
75 VIRGINIA BEACH DRIVE 

MIAMI,» FLORIDA 33149 


MERCATOR STATION PLOT LANGUAGE — FORTRAN IV 
COMPUTER — IBM 360/65, 
CALCOMP 


WRITES STATION NUMBERS AT THEIR POSITIONS ON A MERCATOR PROYECTION IN 
ANY SCALE/DEGREEe INPUT-- STATION HEADER CARDS IN ICES FORMAT. 
AUTHOR-— MARILYNN BORKOWSKT. 


BUREAU OF COMMERCIAL FISHERIES 

TROPICAL ATLANTIC BIOLOGICAL LABORATORY 
75 VIRGINIA BEACH DRIVE 

MIAMI» FLORIDA 33149 


HORIZONTAL SECTIONS LANGUAGE —- FORTRAN IV 
COMPUTER — IBM 360/65, 
CALCOMP 


WRITES IN VALUES OF TEMPERATURE» SALINITY: OXYGEN» PHOSPHATE» ON SEP— 
ARATE MERCATOR PROJECTIONS» AT SPECIFIED DEPTHSe INPUT-— HYDROGRAPHIC 
DATA IN ICES FORMAT» AT STANDARD DEPTHSe AUTHOR-- MARILYNN BUORKOWSKIe 


BUREAU OF COMMERCIAL FISHERIES 

TROPICAL ATLANTIC BIOLOGICAL LABORATORY 
75 VIRGINIA BEACH DRIVE 

MIAMI» FLORIDA 33149 


GENERAL MERCATOR PLOT LANGUAGE —- FORTRAN IV 
COMPUTER — IBM 360/65, 
CALCOMP 


PLOTS ANY VARIABLE ON A MERCATOR PROJECTIONe HAS OPTION OF WRITING IN 
VALUE OR MAKING A POINT PLOTs AND OF CONNECTING THE POINTS WITH LINESe 
INPUT-—- ANY HEADER CARDS IN ICES FORMATe PROJECTION PLOT MAY BE IN 
ANY SCALE PER DEGREE» AND MAY INCLUDE A COASTLINE (OBTAINED FROM A 
DIGITIZED WORLD TAPE LAYOUT).+ CORE STORAGE NECESSARY-- 42K BYTES (IN- 
CLUDES PLOT ROUTINES)»« AUTHOR-- MARILYNN BORKOWSKIe 


BUREAU OF COMMERCIAL FISHERIES 

TROPICAL ATLANTIC BIOLOGICAL LABORATORY 
75 VIRGINIA BEACH DRIVE 

MIAMI» FLORIDA 33149 


ISOS»s0X0S»sPHOS LANGUAGE — FORTRAN IV 
COMPUTER — IBM 360/65 
WITH CALCOMP 


PLOTS ISENTROPIC SECTIONS FOR SALINITY» OXYGENs OR PHOSPHATE FOR THE 
STANDARD STATIONS OF THE TRADE WIND ZONE OCEANOGRAPHY PROGRAMe INPUT 
IS THE TRADE WIND ZONE OCEANOGRAPHY PROGRAM ISENTROPIC FORMAT CARDS. 


BUREAU OF COMMERCIAL FISHERIES 


Pe O. BOX 3830 
HONOLULU» HAWAII 96812 


PAGE 040 


TSIP» THOX s THOT LANGUAGE — FORTRAN IV 
COMPUTER - IBM 360/65 
WITH CALCOMP 


PLOTS TIME HISTORY OF TEMPERATURE» SALINITY» OR OXYGEN FOR STANDARD 
STATIONS OF THE TRADE WIND ZONE OCEANOGRAPHY PROGRAM PILOT STUDY. IN- 
PUT IS TRADE WIND ZONE OCEANOGRAPHY PROGRAM ISENTROPIC FORMAT CARDS. 


BUREAU OF COMMERCIAL FISHERIES 
Pe Oc BOX 3830 
HONOLULUs HAWAII 96812 


BATHYTHERMOGRAM COMPOSITE PLOT LANGUAGE — FORTRAN 
COMPUTER — I8M1401/7074 

(COPY ON FILE AT NODC) 
COMPUTES (1) NUMBER OF OBSERVATIONS AT 50 METER INTERVALS» (2) PERCEN- 
TAGE FOR EACH QUALITY CODE, (3) PLOTS PER SEASON AND AREA (AS DETER- 
MINED BY A 1401 PROGRAM) USUALLY TO 35 LINES PER PAGE (NEVER EXCEEDING 
44)e INPUT--— NODC FORMAT DIGITIZED BT DATAs SORTED BY STATION AND 
DEPTHe OUTPUT-— TAPE FOR CALCOMP 670/564 PLOTTERe OS NOeo 52208e AU- 
THOR-- RUDI SAENGERe 


COMPUTER SYSTEMS DIVISION 
NATIONAL OCEANOGRAPHIC DATA CENTER 
WASHINGTONs De Co 20390 


INVENTORY PLOT LANGUAGE - FORTRAN IV 
COMPUTER — IBM 360/405 
CALCOMP 763 


DISPLAYS AN INVENTORY OF STATION DATA PARAMETERS» BT DATAs GEOLOGICAL 
SAMPLES» ETCe (ANY GEOGRAPHICALLY SORTED DATA FILE)» BY 1-DEGREE, 2- 
DEGREEs AND 5-DEGREE SQUARESs AND ON ANY OF EIGHT MAP PROJECTIONS OF 
SPHEREe OUTPUT-- A TAPE FOR THE CALCOMP 780/763 DRUM PLOTTERe AU- 
THOR-— JOHN WARDe WILL USE A STATION DATA PARAMETER INVENTORY PROGRAM 
NOW BEING WRITTEN IN ASSEMBLER LANGUAGE BY JEFF GORDON», AND OTHER 


PROJECTED PROGRAMS. 


COMPUTER SYSTEMS DIVISION 
NATIONAL OCEANOGRAPHIC DATA CENTER 
WASHINGTON» De Ce 20390 


CRUISE TRACK — MERCATOR PROJECTION LANGUAGE — FORTRAN 
COMPUTER -— IBM 7074 
(COPY ON FILE AT NODC) 

INPUT-— NASA DIGITIZED WORLD LAYOUT TAPEs AND NODC FORMAT STATION DATA 
(UP TO 600 STATIONS IN A CRUISE).e PROCEDURE-- DETERMINE MAXIMUM AND 
MINIMUM LATITUDE» AND ROUND TO NEAREST FIVE DEGREESs THEN DETERMINE 
SCALE FACTORs LONGER SIDE EQUAL TO 20 INCHES» OUTPUT-- TAPE FOR CAL- 
COMP 670/564 PLOTTERe OS NOe 5221056 AUTHOR-- RUDI SAENGERe NOTE-- 
THIS WILL SOON BE REPLACED AT NODC BY A NEW MULTI-PROJECTION PROGRAM 
FOR CRUISE TRACKS» WRITTEN IN FORTRAN BY JOHN WARD FOR THE IBM 3606 


COMPUTER SYSTEMS DIVISION 
NATIONAL OCEANOGRAPHIC DATA CENTER 
WASHINGTON»s De Ce 20390 


VERTICAL SUMMARY HISTOGRAM PLOT LANGUAGE — FORTRAN 
COMPUTER -— IBM 7074 AND 
CALCOMP 564 
(COPY ON FILE AT NODC) 
PLOTS PERCENT-FREQUENCY HISTOGRAMS AT EACH OF A MAXIMUM OF 20 STANDARD 
DEPTHS» EACH PLOT FOR A GIVEN 1-DEGREE SQUARE AND MONTHe INPUT DATA 
ARE PREPARED BY THE STATION DATA VERTICAL ARRAY SUMMARY PROGRAMe NO’ 
522356 AUTHOR--— ROBERT VAN WIEe 


PAGE 041 


COMPUTER SYSTEMS DIVISION» CODE 2400 
NATIONAL OCEANOGRAPHIC DATA CENTER 
WASHINGTONs DeCe 20390 


DENSITY-SALINITY MID PLOT LANGUAGE — FORTRAN 
COMPUTER — IBM 7074 
(cOPY ON FILE AT NODC) 
USES SELECTED DENSITY-SALINITY VALUES (OUTPUT FROM PROGRAM NOe 52321) 
TO DRAW SINGLE PLOTS AND 6-4-6 COMPOSITE PLOTS IN A GEOGRAPHICALLY 
CONTIGUOUS AREAe THE COMPOSITE PLOTS ENABLE ANALYSES OF THESE MID- 
POINT VALUES IN RELATION TO THEIR SURROUNDINGSe CORRECTIONS CAN THEN 
BE MADE ON THOSE SELECTED DENSITY-SALINITY POINTS TO BETTER REPRESENT 
THE MIDPOINT VALUE OF THAT PARTICULAR WATER MASSe OS NOco 523220 AU- 
THOR—— ReP. STEIN 


DEVELOPMENT DIVISION, CODE 2310 
NATIONAL OCEANOGRAPHIC DATA CENTER 
WASHINGTONs De Ce 20390 


PRESORTED SIGMA-T VERSUS DEPTH AND SALINITY LANGUAGE — FORTRAN 
COMPUTER — IBM 7074 
(COPY ON FILE AT NODC) 

PLOTS SIGMA-T VERSUS DEPTH AND SALINITY» COMPOSITE BY MARSDEN SQUARES 
AND AREAS PREPUNCHED IN COL. 3-4e LIMITS-- DEPTH — 0 TO 3000s SIGMA-T 
— 22260 TO 29605 SALINITY -— 3265 TO 38¢5¢ INPUT-- NODC FORMAT STATION 
DATA ON TAPEs SORTED BY MARSDEN SQUAREs AREAs STATION AND DEPTHe OUT- 
PUT-- TAPE FOR CALCOMP 670/564 PLOTTERe OS NOs 522212 AUTHCR-- RUDI 
SAENGERe 


COMPUTER SYSTEMS DIVISION 


NATIONAL OCEANOGRAPHIC DATA CENTER 
WASHINGTONs De Ce 20390 


STATION DATA PLOT - SIX VARIABLES LANGUAGE — FORTRAN 
COMPUTER - IBM 7074 
(COPY ON FILE AT NODC) 

PLOTS TEMPERATURE VERSUS DEPTHs SALINITY: OXYGEN» PHOSPHATEe*® ALSO 

SALINITY AND SIGMA-T VERSUS DEPTHe LIMITS-- DEPTH —- 0 TO 12505 TEMP— 

ERATURE — 3¢5 TO 31eO05« INPUT-- NODC FORMAT OBSERVED DATA, SORTED BY 

STATION AND DEPTHe OUTPUT--— TAPE FOR CALCOMP 670/564 PLOTTERe OS NOe 

52206e AUTHOR-- RUDI SAENGER. 


COMPUTER SYSTEMS DIVISION 
NATIONAL OCEANOGRAPHIC DATA CENTER 
WASHINGTONs De Ce 20390 


SOUND VELOCITY DEPTH PROFILES LANGUAGE — FORTRAN 
COMPUTER — IBM 7074 W/ 
CALCOMP 564 
(COPY ON FILE AT NODC) 
PLOTS CURVES OF DEPTHS VERSUS SOUND VELOCITIES FOR SELECTED MONTHS IN 
A 1-DEGe SQUARE AREA FOR WHICH THERE ARE AT LEAST 8 STATIONS EXCEEDING 
150 METERS, OR FOR SELECTED SEASONS HAVING 5 OR MORE STATIONS EXCEED- 
ING 400 METERSe OS NOe 522284 AUTHOR-- ROBERT VAN WIEe 


COMPUTER SYSTEMS DIVISION 
NATIONAL OCEANOGRAPHIC DATA CENTER 
WASHINGTON, De Ce 20390 


VERTICAL SECTION PLOT — STATION DATA LANGUAGE — FORTRAN 


COMPUTER — IBM 7074 
(COPY ON FILE AT NODC) 
(1) EACH VERTICAL SECTION PLOT CONTOURS ONE OF THE FOLLOWING-— TEMPER-. 
ATURE» SALINITYs SIGMA-T» GYMNODINIUM BREVEs INORGANIC PHOSPHURUSs TO- 


PAGE 042 


TAL PHOSPHORUS» NITROGEN» SILICONs OR COPPERe 

(2) PLOTS VERTICAL SECTIONS WITH NUMERICAL INSTEAD OF CONTOUR LINES 
FOR PARAMETERS INORGANIC PHOSPHORUSs TOTAL PHOSPHORUS» NITROGEN, SILI- 
CONs OR COPPERe INPUT-—- OBSERVED NODC FORMAT STATION DATA TAPE ZONE- 
EDITED TO 120 CHARACTERS PER RECORD» SORTED BY CRUISE REFERENCE NO6 
OUTPUT-- INPUT TAPE TO CALCOMP PLOTTER 670/564. RUNNING TIME-- ABOUT 
70 SECTIONS PER HOURe OS NOe 522792 AUTHOR-—- ROBERT VAN WIE» MODIFY- 
ING AND CONTINUING OS NOSe 52278 AND 52279 BY DANIEL ROBERTS. 


COMPUTER SYSTEMS DIVISION 
NATIONAL OCEANOGRAPHIC DATA CENTER 
WASHINGTONs De Co 20390 


OCEANOGRAPHIC DATA PLOTTING PROGRAM FOR LANGUAGE -— FORTRAN II 
NeOeDeCe DATA COMPUTER - I8M 1620 FOR 
CALCOMP 560 
(COPY ON FILE AT NODC) 

THE INPUT DATA CARDS ARE RECEIVED FROM THE NATIONAL OCEANOGRAPHIC DATA 
CENTERe THE PROGRAM IS DESIGNED TO PLOT OCEANOGRAPHIC STATION DATA 
DOWN TO A DEPTH OF 109000 METERSe THIS IS DONE ON A SERIES OF UP TO 
5 GRAPHS, EACH OF WHICH HAS A RANGE OF 23000 METERSe THIS IS A COM- 
POSITE GRAPH CONSISTING OF TEMPERATUREs SIGMA-T» SOUND VELOCITY, SAL- 
INITYs OXYGEN AND PHOSPHATEe THE SALINITY» PHOSPHATE AND OXYGEN VAL-— 
UES ARE PLOTTED VS TEMPERATUREe DENSITYs SOUND VELOCITY AND TEMPERA- 
TURE ARE PLOTTED AGAINST DEPTHe ALL TEMPERATURE DEPENDENT VARIABLES 
ARE PLOTTED ON THE FIRST GRAPHe THE CONTINUING GRAPHS CONTAIN ONLY 
DEPTH DEPENDENT VARIABLESe THE GRAPH IS FULLY IDENTIFIED AS TO REFER- 
ENCE NUMBERs STATION LOCATION AND DATEs ETCe EACH CURVE IS IDENTIFIED 
BY ITS PLOTTING SYMBOLe AUTHORS-—- DeLe SHAFFER AND DeTe EGERe 


UNIVERSITY OF MIAMI 

MARINE LABORATORY 

COMPUTER CENTER 

1 RICKENBACKER CAUSEWAY 
VIRGINIA KEY» MIAMI» FLORIDA 


OCEANOGRAPHIC DATA PLOTTING PROGRAM, leCeEoSe LANGUAGE — FORTRAN II 
COMPUTER -— IBM 1620 FOR 
CALCOMP 560 
(COPY ON FILE AT NODC) 
THE INPUT TO THIS PROGRAM CONSISTS OF THE OUTPUT OF THE IN SITU OCEAN- 
OGRAPHIC DATA PROCESSING PROGRAMe HOWEVER» THIS PROGRAM REQUIRES THAT 
HEADER CARDS BE INCLUDEDe SINCE THE PROGRAM ESSENTIALLY INTEGRATES 
ONE STATION AT A TIME AND THEN PLOTS IT» THE HEADER CARDS SERVE TO IN- 
DICATE THE BEGINNING OF A NEW STATIONe AUTHOR-— Dele SHAFFERe 


UNIVERSITY OF MIAMI 

MARINE LABORATORY 

COMPUTER CENTER 

1 RICKENBACKER CAUSEWAY 
VIRGINIA KEYs MIAMI» FLORIDA 


HISTO > LANGUAGE — FORTRAN IV-H 
COMPUTER - SDS SIGMA 7 


PRODUCES HORIZONTAL BAR HISTOGRAMS OF ANY VARIABLE THAT IS STORED ON 
MAGNETIC TAPE IN STANDARD WHOI FORMATe OUTPUT IS A BAR HISTOGRAM 
DRAWN BY THE LINE PRINTERe THE WHOI GENERALIZED TAPE FORMAT IS PRE- 
SENTED IN A TECHNICAL REPORT 'A NINE CHANNEL DIGITAL MAGNETIC TAPE 

FOR STORING OCEANOGRAPHIC DATA'»s REFe NOe 69-555 JULY 19695 BY JOHN Ac 
MALTAISe 


INFORMATION PROCESSING CENTER 

ATTNe JOHN Ae MALTAIS 

WOODS HOLE OCEANOGRAPHIC INSTITUTION 
WOODS HOLE, MASSACHUSETTS 02543 


PAGE 043 


LISPLO LANGUAGE — FORTRAN IV-H 
COMPUTER -— SDS SIGMA 7 


LISTS AND PLOTS THE DATA STORED ON WHOI FORMAT MAGNETIC TAPEs OUTPUT 
IS ON THE LINE PRINTERe THREE TYPES OF PLOT ARE POSSIBLE —- A) VARIA- 
BLE VS TIME OR SEQUENCE NUMBER» B) ANGLE AND SPEED VS TIMEs C) TWO 
VARTABLES (ONE ON A MINUS AND ONE ON A PLUS SCALE) VS TIMEe 


INFORMATION PROCESSING CENTER 

ATTNe JOHN Aw MALTAIS 

WOODS HOLE OCEANOGRAPHIC INSTITUTION 
WOODS HOLEs MASSACHUSETTS 62543 


TSPLOT LANGUAGE — FORTRAN IV-E 
COMPUTER —- IBM 360/50 


GENERATES A PUNCHED DECK TO BE USED AS INPUT TO THE BENSON-LEHNER 
DELTA INCREMENTAL PLOTTERe FOR EACH HYDROGRAPHIC STATION A SEPARATE 
TEMPERATURE VSe SALINITY GRAPH IS DRAWNe SALINITY RANGE IS 320e6 0/00 
TO 37e¢8 0/006e ON THE SAME PAGE TWO TEMPERATURE VSe DEPTH GRAPHS ARE 
DRAWN» ONE FROM O TO 600 Ms THE OTHER FROM 200 M TO THE BOTTOMe THESE 
ARE COMPLETE WITH AXIS» TICK MARKS AND LABELSe SIZE OF GRAPHS IS AN 
INPUT VARIABLEe 


ROBERT Ke SEXTON 

NARRAGANSETT MARINE LABORATORY 
UNIVERSITY OF RHODE ISLAND 
KINGSTONs RHODE ISLAND 02881 


SEQUENTIAL PLOTTING LANGUAGE — FORTRAN 
COMPUTER -— (NOT GIVEN) 
(COPY ON FILE AT NODC) 

SUBROUTINES PRODUCE PLOTS USING A DIGITAL COMPUTER OUTPUT PRINTERe 
THE CONSECUTIVE XsY DATA POINTS ARE PLOTTED WITH SYMBOLS CONSISTING OF 
LETTERS AND NUMERALSe PERMITS RAPID PLOTTING OF EITHER A SINGLE- OR 
MULTIVALUED CURVE WHEN HIGH RESOLUTION IS NOT REQUIREDe REFe NELC RE- 
PORT 1613 (MAR 1969» 40 P) BY ReGe ROCKe DIRECT INQUIRIES TO-- 


NAVAL ELECTRONICS LABORATORY CENTER 
SAN DIEGO, CALIFORNIA 92152 


DATA FIELD GRID EXPANSION LANGUAGE — MACHINE 
COMPUTER - CDC 1604 AND 
CDC 3100 


EXPANDS A PORTION OF A 63X63 GRID DATA FIELD TO ANY DESIRED SCALE. 
THE EXTRACTED PORTION OF THE BASIC FIELD IS OF ARBITRARILY SELECTED 
SIZE» SCALE» LOCATIONs ORIENTATION» AND CONTOUR INTERVALe THE METHOD 
EMPLOYED IS DOUBLE INTERIOR QUADRATIC INTERPOLATION FROM THE ORIGINAL 
GRID POINTS TO THE LOCATION OF THE ARRAY IN THE NEW FIELDe THE TIME 
REQUIRED FOR THE EXTRACTION PROCESS IS SIX SECONDS IN THE 1604 AND 
LESS THAN TWO SECONDS IN THE 3100 COMPUTERe REFe TECHNICAL MEMO NOs 
1, ALSO TECHNICAL NOTE NOe 21 (1966) 


COMMANDING OFFICER 


FLEET NUMERICAL WEATHER CENTRAL 
MONTEREY» CALIFORNIA 93940 


PAGE 044 


MATHEMATICS» APPLIED 
H—-k—H—H—K—K—H#—K—K—H— 


*#-#-% CURVE AND SURFACE FITTING *-*-* 


LEAST SQUARES CURVE FITTING IN TWO» THREE» AND LANGUAGE — FORTRAN II 
FOUR DIMENSIONS COMPUTER -— CDC 3100 
(COPY ON FILE AT NODC) 

THREE SUBROUTINES» 'UCF's "'BCF's AND 'TCF' (FOR UNIVARIATE® BIVARIATE> 
AND TRIVARIATE CURVE-FIT)» FOR USE IN TWO-» THREE-» AND FOUR-SPACEe 
CURVE COEFFICIENTS CALCULATED BY REDUCTION TECHNIQUE DUE TO PeDe CROUT 
(1941)~2¢ OUTPUT-- PRINTOUT OF COEFFICIENTS» IN NORMALIZED FLOAT ING— 
POINTs AND DIFFERENCES CURVE-TO-POINTS» IN SAME FORMATe SATELLITE 
SUBROUTINE 'SYMMET*' IS CALLEDs WHICH SOLVES M SIMULTANEOUS ALGEBRAIC 
EQUATIONS IN Xe CORE STORAGE NECESSARY-— 2074(8)» 2076(8)»s AND 2256 
(8)>5 RESPECTIVELY» + 630(8) FOR SUBROUTINE SYMMETe REFe BeleQe COM- 
PUTER NOTE 68-1-Cs JAN 19682¢ AUTHOR-- FeKe KEYTEe 


DIRECTOR 

ATLANTIC OCEANOGRAPHIC LABORATORY 
BEDFORD INSTITUTE 

DARTMOUTH» NOVA SCOTIA» CANADA 


A GENERALIZED 2-DIMENSIONAL REGRESSION PROCEDURE LANGUAGE - ALGOL AND 
FORTRAN IV 

COMPUTER -— B5500 AND 

IBM 7040 


ENABLES SELECTION OF BEST FIT OF A SET OF OBSERVATIONS WITHOUT REGEN- 
ERATION OF LOWER ORDER COEFFICIENTSe USES THE MINIMIZATION PROPERTY 

OF ORTHOGONAL FUNCTIONSe AUTHOR-- JOHN Re DEMPSEY» NORTHERN NATURAL 

GAS COMPANYe PUBLISHED 1966 AS *COMPUTER CONTRIBUTION 2* WITH ALGOL 

LANGUAGE LISTINGe A FORTRAN VERSION HAS BEEN RUN ON THE IBM 7040.6 


DRe DANIEL Fe MERRIAMs EDITOR» COMPUTER CONTRIBUTIONS 
KANSAS GEOLOGICAL SURVEY 

THE UNIVERSITY OF KANSAS 

LAWRENCE» KANSAS 66044 


GENERAL REGRESSION LANGUAGE —- PL/1 
COMPUTER -— IBM OS/360 
(COPY ON FILE AT NODC) 

OBSERVATIONS MAY BE SELECTED BY GROUPS - UP TO 75 GROUPS ARE ALLOWED. 
THESE SELECTED OBSERVATIONS ARE TO BE USED TO COMPUTE SIMPLE CORRELA- 
TIONS BETWEEN ALL PAIRS OF THE SELECTED VARIABLESe SOME OF THE COR- 
RELATION COEFFICIENTS MAY BE FURTHER USED AS NORMAL EQUATION COEFFIC-— 
IENTS OR CONSTANTS FOR REGRESSION ANALYSES INVOLVING TWO OR MORE OF 
THESE VARIABLESe IF DESIREDs A DIFFERENT SUBSET OF OBSERVATIONS MAY 
BE SELECTED TO COMPUTE RESIDUALS», STANDARD ERRORS OF PREDICTED VALUES» 
ETCe EITHER CARDS OR TAPE MAY CONTAIN MOST OF THE DATAe IF TAPE IS 
TO BE USED FOR THE OBSERVATION MATRIX» IT MUST HAVE BEEN CREATED BY A 
DIFFERENT PROGRAM AND BE IN A SPECIAL PL/1 STREAM 1/0 FORMATe 


Ue Se GEOLOGICAL SURVEY 

COMPUTER CENTER DIVISION 

ATTNe RALPH EICHERs CHIEF 

BRANCH OF SCIENTIFIC APPLICATIONS 
WASHINGTON» De Co 20242 


GRAPHIC SYSTEM FOR CURVE FITTING LANGUAGE —- (NOT GIVEN) 
COMPUTER -— IBM 360/40 
W/ IBM 2250 


PAGE 045 


PROGRAM SYSTEM CONSISTS OF A SET OF NEARLY INDEPENDENT SECTIONS FUNC- 
TIONING ONLY WHEN CALLED BY THE 'tMAIN*t PROGRAMe THE USER ENTERS A 
CURVE INTO THE 360/40 VIA A RAND TABLET AND INTERACTIVELY TO SPECIFY 
VARIOUS WAYS OF FITTING, EDITING AND DISPLAYING THE CURVE ON AN IBM 
2250 SCOPE. THE LAST STEP OUTPUT IS PUNCH CARDS WITH DATA POINTS. OR 
COEFFICIENTSe THE SYSTEM FOR IBM 360 ALONG WITH THE PACKAGE OF GRAPH— 
ICS USED AT RAND TAKE UP ROUGHLY ONE-HALF OF THE COMPUTER CORE MEMORY. 
DOCUMENT BY AeSe PRIVERs SEPT 1969-¢ THE DDC NOw IS AD 693 920. 


THE RAND CORPORATION 
1700 MAIN ST. 
SANTA MONICAy CALIFe 90406 


BARTLETT'S CURVE FITTING LANGUAGE — FORTRAN 
COMPUTER — IBM 1800 SYS 
(COPY ON FILE AT NODC) 

BARTLETT'S METHOD FOR COMPUTING THE BEST VALUES FOR FITTING A LINEAR 
RELATIONSHIP OR AN EXPONENTIAL RELATIONSHIPe THE 70 0/0 AND 90 0/0 
CONFIDENCE LIMITS ON THE SLOPE ARE ALSO’ FOUNDe THE PROGRAM TAKES A 
MAXIMUM OF 99 SETS OF DATA EACH WITH A MAXIMUM OF 500 POINTSe NeleOe 
PROGRAM 174e AUTHOR--— MAUREEN TYLERe 


NATIONAL INSTITUTE OF OCEANOGRAPHY 
WORMLEY» GODALMINGs SURREY 
ENGLAND 


CRVFT LANGUAGE - FORTRAN II 
COMPUTER —- GE 225 
(COPY ON FILE AT NODC) 

ROUTINE TO FIND EITHER BEST LEAST SQUARES FIT TO N POINTS WITHIN SPEC- 
IFIED STANDARD DEVIATION 'SIGMA'ts OR FIT A SPECIFIED 'M-CURVE! ORDER 
CURVEe FORMER EXECUTED BY M-CURVE NEGATIVEs LATTER BY M-CURVE NON- 
NEGATIVEe IN EITHER CASE #SD! IS ACTUAL STANDARD DEVIATION AS CALCUL- 
ATEDe AUTHOR-—- FeKe KEYTEe LISTED IN APPENDIX 5 OF BIO COMPUTER NOTE 
66-5-Ce A 14-PAGE WRITEUP IS IN THE '#COPE! CATALOG (1965) OF WOODS 
HOLE OCEANOGRAPHIC INSTITUTION. 


DIRECTOR 

ATLANTIC OCEANOGRAPHIC LABORATORY 
BEDFORD INSTITUTE 

DARTMOUTHs NOVA SCOTIAs CANADA 


LEAST SQUARES PLOT LANGUAGE — FORTRAN 
COMPUTER -— IBM 7074 


FITS AN N-DEGREE POLYNOMIAL (MAXe N=10) OR AN EXPONENTIAL FUNCTION TO 
DATA POINTS (MAXe 300)s PLOTTING THE ACTUAL CURVE AND THE COMPUTED 
CURVE FOR COMPARISON OR PLOTTING THE DATA POINTS ONLY TO HELP IDENTIFY 
THE TYPE OF CURVE THEY REPRESENTe OS NOe 101122 AUTHOR-—- JAMES Se 
WARDENe 


COMPUTER DEPARTMENTs CODE 083 
NAVAL OCEANOGRAPHIC OFFICE 
SUITLANDs MD. 20390 


CALCULATING AND PLOTTING TIME-TREND CURVES LANGUAGE — FORTRANS FAP 
COMPUTER — IBM 7090/94 


COMPUTES AND PLOTS A SERIES OF SMOOTHED OR GRADUATED CURVES BASED ON A 
SEQUENCE OF GEOLOGIC OBSERVATIONSe NINE SMOOTHING FORMULAE ARE USED 
WHICH CORRESPOND TO CYCLES OF INCREASING MAGNITUDE WITHIN THE DATA» 

FOR EACH OF TEN VARIABLES WITH UP TO 500 OBSERVATIONS PER VARIABLEe 
LEAST SQUARES ANALYSIS IS USED TO FIT A SERIES OF 3RD ORDER POLYNOM-— 
TIALS TO THE DATAe STORAGE REQUIREMENTS-- 245757 LOCATIONSe RUNNING 
TIME-- ABOUT 2 MINUTES TO COMPUTE ALL NINE CURVES FOR 100 OBSERVATIONS ° 


PAGE 046 


ON A SINGLE VARIABLEe AUTHOR-— WILLIAM Te FOXs WILLIAMS COLLEGE. 
(SPECIAL DISTRIBUTION PUBLICATION 12) 


DRe DANIEL Fe MERRIAMs EDITOR» COMPUTER CONTRIBUTIONS 
KANSAS GEOLOGICAL SURVEY 

COMPUTER APPLICATIONS LABORATORY 

THE UNIVERSITY OF KANSAS 

LAWRENCE» KANSAS 66045 


TREND-SURFACE PROGRAM WITH UNRESTRICTED INPUT LANGUAGE — FORTRAN II 
AND IV» AND 
BALGOL 
COMPUTER - IBM 1620 


DIFFERS FROM PREVIOUS TREND-SURFACE PROGRAM FOR THE IBM 1620 (SPECIAL 
DISTRIBUTION PUBLICATION 145 BY Dele GOOD, 1964) IN ONE MAJOR ASPECT-- 
DATA ARE NOT STORED IN A DIMENSION ARRAY WITHIN THE COMPUTER» BUT ARE 
PROCESSED AND ACCUMULATED AS READ INe THE PROGRAMs THEREFOREs IS THE- 
ORETICALLY CAPABLE OF INCORPORATING AN INFINITE NUMBER OF DATA POINTS. 
PRODUCES VALUES UP TO THE FOURTH-DEGREE EQUATIONSe STORAGE REQUIRE- 
MENTS-— APPROXIMATELY 18K BITSe RUNNING TIME-—- TWO PASSES ARE NECESS-— 
ARY» REQUIRING ABOUT 12 MINUTES PER 100 DATA POINTS ON EACH PASSe AU- 
THORS-- ROBERT Je SAMPSON AND JOHN Ce DAVIS, IDAHO STATE UNIVe REFe-- 
SPECIAL DISTRIBUTION PUBLICATION 26 (1966). 


DRe DANIEL Fe MERRIAMs EDITOR» COMPUTER CONTRIBUTIONS 
KANSAS GEOLOGICAL SURVEY 

COMPUTER APPLICATIONS LABORATORY 

THE UNIVERSITY OF KANSAS 

LAWRENCEs KANSAS 66045 


MULTIVARIATE NON-LINEAR REGRESSION LANGUAGE - FORTRAN II 
AND IV 
COMPUTER - IBM 709 AND 
CDC 6400 


COMPUTES MULTIVARIATE NON-LINEAR REGRESSION (TREND SURFACE) THROUGH 
THE QUINTIC WITH ANALYSIS OF VARIANCE FOR SELECTION OF BEST FITs FOR 
N=25006 


DEPARTMENT OF GEOLOGY 
FLORIDA STATE UNIVERSITY 
TALLAHASSEE» FLORIDA 32306 


TREND SURFACES FOR DEGREES 1 THROUGH 6 LANGUAGE -— FORTRAN IV 
COMPUTER -— IBM 7040 


POLYNOMIAL SURFACES ARE FITTED UP TO THE SIXTH DEGREEe THE SURFACES 
MAY BE CONTOURED AND THE RESIDUALS PLOTTEDe RANGE IS UP TO 500 DATA 
POINTSe APPROXIMATELY 40 MINUTES ARE REQUIRED FOR 200 DATA POINTS FOR 
7-1/2 BY 9 TREND-SURFACE MAPS THROUGH SIXTH DEGREEe STORAGE REQUIRE- 
MENTS FOR THE 7040-—- 16K AND 4 MAGe TAPESe AUTHORS-— MONT O'LEARY OF 
THE UNIVe OF KANSAS» ReHe LIPPERT OF SHELL OIL COes OWEN Te SPITZ OF 
KANSAS GEOLe SURVEYe REVISED FROM Dele GOOD'S PROGRAM FOR THE I8M1620 
WHICH WAS PUBLISHED IN 1964 AS KANSAS GEOLOGICAL SURVEY SPECIAL DIS-— 
TRIBUTION PUBLICATION 14.6 


DRe DANIEL Fe MERRIAMs EDITORs COMPUTER CONTRIBUTIONS 
KANSAS GEOLOGICAL SURVEY 

COMPUTER APPLICATIONS LABORATORY 

THE UNIVERSITY OF KANSAS 

LAWRENCE» KANSAS 66045 


TREND MAP» WITH RESIDUALS AND CONTOURS LANGUAGE — MAD 
COMPUTER - IBM 7090 
(COPY ON FILE AT NODC) 


PAGE 047 


USES THE LEAST SQUARES TECHNIQUE TO FIT AN EQUATION TO GEOGRAPHICALLY 
DISPERSED DATAe OUTPUT INCLUDES PRINTED MAPSe AUTHOR-- WeRe TOBLER. 


THE UNIVERSITY OF MICHIGAN 
DEPARTMENT OF GEOGRAPHY 
ATTNe DRe We Re TOBLER 

ANN ARBOR» MICHIGAN 48104 


H-*#—* MATHEMATICAL AND STATISTICAL ANALYSIS *-*-* 


SBWRO (SHIPBORNE WAVE RECORDER ANALYSIS) LANGUAGE — FORTRAN Iv 
COMPUTER - IBM 1800 SYS 
(COPY ON FILE AT NODC) 
GIVEN VALUES OF THE HIGHEST AND SECOND HIGHEST CRESTS» THE LOWEST AND 
SECOND LOWEST TROUGHS» THE NUMBER OF ZERO CROSSINGS AND THE NUMBER OF 
CRESTS IN A SHORT RECORD FROM THE NeIeO5e SHIPBORNE WAVE RECORDER» COM- 
PUTES THE SPECTRAL WIDTH PARAMETER AND THE SIGNIFICANT WAVE HEIGHT AND 
ALSO THE PREDICTED MAXIMUM HEIGHT IN A PERIOD OF THREE HOURS» AND 
STORES THE RESULTS ON LINEPRINTER AND DISKe NeIeO5e PROGRAN NOw 89e 
AUTHOR-- EILEEN PAGEe 


NATIONAL INSTITUTE OF OCEANOGRAPHY 
WORMLEY» GODALMINGs SURREY 
ENGLAND 


HILOW (GENERATE ARBITRARY FILTER) LANGUAGE - FORTRAN IV 
COMPUTER — IBM 1800 SYS 
(COPY ON FILE AT NODC) 
GENERATES A LOWPASS» BANDPASS» OR HIGHPASS FILTER DEFINED BY 3 PARA- 
METERS» WITH OR WITHOUT ITS CONJUGATEs PUNCHES THE MULTIPLIERS ON 
CARDS» AND LISTS ITS AMPLITUDE RESPONSE OVER THE FULL FREQUENCY RANGE. 
NeIleO5«e PROGRAM NOe 158e AUTHOR-- DeEew CARTWRIGHT. 


NATIONAL INSTITUTE OF OCEANOGRAPHY 
WORMLEY» GODALMINGs SURREY 
ENGLAND 


SUBROUTINES DETRNDs AUTCOVs CRSCOVs FOURTR LANGUAGE — FORTRAN IV 
COMPUTER -— IBM 360/40 
(COPY ON FILE AT NODC) 

A SET OF PROGRAMS DEALING WITH SPECTRAe DETRND REMOVES THE MEAN» OR 
THE MEAN AND LINEAR TREND (SLOPE) FROM A TIME SERIESe AUTCOV COMPUTES 
THE AUTOCOVARIANCE OF THE TIME SERIESe CRSCOV COMPUTES THE AUTO- AND 
CROSS-COVARIANCES OF TWO SEQUENCESe FOURTR COMPUTES EITHER THE SINE 
OR COSINE FOURIER TRANSFORMe SMOOTHING OF EITHER IS OPTIONALe LISTED 
AND DESCRIBED IN THE PUBLICATION 'WATER WAVE TEACHING AIDS'» WHICH 
APPEARS AS TECHNICAL NOTE 13 OF THE MeleTe HYDRODYNAMICS LABORATORY e 
THESE ROUTINES ARE ADAPTED FROM A PROGRAM WRITTEN AT BELL TELEPHONE 
LABS BY MeJeRe HEALY (1962). 


PROFe RALPH He CROSS 

ROOM 48-209 HYDRODYNAMICS LABORATORY 
MASSACHUSETTS INSTITUTE OF TECHNOLOGY 
CAMBRIDGE» MASSACHUSETTS 02139 


DIGITAL POWER SPECTRUM ANALYSIS LANGUAGE - FORTRAN Iv 
COMPUTER — IBM 7090 


THE PROGRAM WAS ORIGINALLY INTENDED TO ANALYZE UNDERWATER SOUNDe THE 
HYDROPHONE OUTPUT IN ANALOG FORM IS FIRST DIGITIZEDe THE PROGRAM THEN . 
COMPUTES THE POWER SPECTRUM ESTIMATE UTILIZING THE FAST FOURIER TRANS-— 
FORMes THE POWER IS COMPUTED FOR A LINEAR SET OF FREQUENCIESe THIS 


PAGE 048 


INFORMATION IS WRITTEN ON AN OUTPUT TAPEe 


DRe Je We WRENCH» JRe 

HEAD» MATHEMATICAL COMPe DIVISION 

NAVAL SHIP RESEARCH AND DEVELOPMENT CENTER 
WASHINGTONs DeCe 20007 


STATISTICAL AND PEAK-TO-PEAK ANALYSIS LANGUAGE — FORTRAN Iv 
AND MAP 
COMPUTER -— IBM 7090 


USED IN THE ANALYSIS OF SHIP TRIAL DATA TO STUDY THE ELASTIC RESPONSES 
OF SURFACE SHIP STRUCTURES TO RANDOM SEA ENVIRONMENTe CALCULATES STA- 
TISTICAL AND PEAK TO PEAK PARAMETERS ASSOCIATED WITH DIGITIZED RANDOM 
DATAe PROCESSES UP TO 14 CHANNELS OF DATA CONCURRENTLY» AND ALLOWS 
SELECTION OF EITHER CALIBRATED OR UNCALIBRATED RESULTSe REFe NSRDC 
APPLIED MATHEMATICS LABORATORY TECHNICAL NOTE AML-35-695 MAY 1969, 

JB1M PROGRAM FOR STATISTICAL AND PEAK-TO-PEAK ANALYSIS'» BY MICHAEL 
CHERNIKe 


DRe Je We WRENCHs JRe 

HEAD» MATHEMATICAL COMPe DIVISION 

NAVAL SHIP RESEARCH AND DEVELOPMENT CENTER 
WASHINGTONs DeCe 20007 


PARTIAL AND ORDINARY COHERENCE LANGUAGE - FORTRAN IV 
AND MAP 
COMPUTER -— IBM 7090 


PROGRAM PRTCOH CALCULATES THE PARTIAL COHERENCE FOR RANDOM DATA FROM A 
LINEAR SYSTEMs AND OCOH CALCULATES THE ORDINARY COHERENCE FROM THE 
SAME DATAe THE DATA IS ASSUMED TO BE STATIONARY RANDOM DATA FROM A 
MULTIPLE-INPUT S*¥STEM WITH A SINGLE OUTPUTe BOTH PROGRAMS COMPUTE THE 
TRANSFER RESPONSE FUNCTION FOR EACH INPUTe REFe APPLIED MATHEMATICS 
LABORATORY TECHNICAL NOTE AML-31-695 MAY 19695 *COMPUTER PROGRAMS FOR 
PARTIAL AND ORDINARY COHERENCE! BY ANTHONY Ce MELODIAe 


DRe Je We WRENCHs JRo 

HEADs MATHEMATICAL COMPe DIVISION 

NAVAL SHIP RESEARCH AND DEVELOPMENT CENTER 
WASHINGTONs DeCe 20007 


SAVED (SHOCK AND VIBRATIONAL EXPERIMENTAL DATA LANGUAGE -— FORTRAN IV 
REDUCTION) AND MAP 
COMPUTER - IBM 7090 


REDUCES BLAST TEST DATA FROM ANY ONE OF FOUR TYPES OF TRANSDUCERS-— 
VELOCITY METERS» ACCELEROMETERSs PRESSURE GAUGES AND STRAIN GAUGESe 
THROUGH PROGRAMMED OPTIONS THE INPUT DATA» AFTER BEING CALIBRATED, MAY 
BE SMOOTHEDs FILTERED OR LISTED BEFORE BEING PLOTTED AS A FUNCTION OF 
TIMEe FOR VELOCITY DATAs TRANSDUCER CORRECTIONS WERE APPLIED AND DIS- 
PLACEMENT IS COMPUTED AND PLOTTEDe FOR ACCELERATION DATAs VELOCITY 
AND DISPLACEMENT ARE COMPUTED AND PLOTTED. INPUT DATA IS READ FROM A 
DIGITAL MAGNETIC TAPE IN A PREDEFINED FORMATe DESCRIPTION IS IN NSRDC 
APPLIED MATHEMATICS LABORATORY TECHNICAL NOTE AML-14-69»5 MARCH 1969¢ 
ENTITLED "A DIGITAL PROGRAM FOR REDUCING SHOCK AND VIBRATIONAL EXPERI- 
MENTAL DATA BY ANTHONY Ve CINCOTTAe 


DRe Je We WRENCH» JRe 

HEAD» MATHEMATICAL COMPe DIVISION 

NAVAL SHIP RESEARCH AND DEVELOPMENT CENTER 
WASHINGTONs DeCe 20007 


BLACKY (TIME SERIES ANALYSIS) LANGUAGE -— FORTRAN Iv 
COMPUTER — IBM 0S/360 
(COPY ON FILE AT NODC) 


PAGE 049 


NePeGeSe LIBRARY PROGRAMe COMPUTES» FOR TWO SIMULTANEOUS TIME SERIES» 
CROSS SPECTRAs POWER SPECTRA» PHASE AND COHERENCEe SUBPROGRAMS OBTAIN 
THE FILTERED SERIES» REMOVE THE TRENDs AND COMPUTE THE AUTO- AND CROSS 
CORRELATIONSe THESIS BY JOHN Ge MCMILLAN (JUNE 1968) USES DIGITAL A- 
NALYSIS BY PROGRAM BLACKY IN THE STUDY OF TEMPERATURE FLUCTUATIONS 
NEAR THE AIR-SEA INTERFACEs THE WAVE FIELD AT THE SAME POINTs AND THE 
DOWNSTREAM WIND VELOCITYe 


NAVAL POSTGRADUATE SCHOOL 
MONTEREY» CALIFORNIA 93940 


SPECTRAL ANALYSIS OF TIME SERIES LANGUAGE — FORTRAN IV 
AND AIGOL 60 
COMPUTER —- UNIVAC 1108 
AND B5500 
(COPY ON FILE AT NODC) 
FINDS THE SPECTRA» COSPECTRA»s QUADSPECTRA» COHERENCEs AND PHASE OF TWO 
TIME SERIES OR A SINGLE SPECTRUM OF ONE SERIESe USES THE FAST FOURIER 
TRANSFORM (ALGORITHM OF COOLEY AND TUKEYs 1965)e REFe SPECIAL REPORT 
NOe 6» MARCH 1969» BY EVERETT Je FEEe 


THE LIBRARIAN 

CENTER FOR GREAT LAKES STUDIES 
UNIVERSITY OF WISCONSIN-MILWAUKEE 
MILWAUKEE» WISCONSIN 53201 USA 


WAVEIN AND DIFRAK LANGUAGE - FORTRAN 
COMPUTER —- IBM 7094 AND 
CDC 6400 


A PAIR OF PROGRAMS FOR (1)SPECTRAL ANALYSIS OF WAVE DATAs AND (2) COM- 
PUTATION AND PLOT OF THE DIFFRACTION COEFFICIENTSe AUTHOR-- SHOU-SHAN 
FAN» CoEeReCos WASHe » DeCe 


PROFe ROBERT Le WIEGEL 
DEPARTMENT OF CIVIL ENGINEERING 
UNIVERSITY OF CALIFORNIA 
BERKELEY» CALIFe 94720 


POWER SPECTRUM ANALYSIS LANGUAGE — FORTRAN AND 
BINARY 
COMPUTER — IBM 7090 
AND IBM 704 


USED IN THE ANALYSIS OF OCEAN WAVE RECORDS» WHICH GIVE THE FLUCTUATION 
OF THE HYDROSTATIC PRESSURE AT A POINT UNDER THE SEA AS A FUNCTION OF 
TIMEe DIVIDED INTO TWO PROGRAMS—— AML PROBLEM 840-017C COMPUTES ONLY 
THE AUTOCORRELATION AND SPECTRAL ESTIMATES FOR EACH SINGLE TIME SER- 
IES» AML PROBLEM 840-157B COMPUTES» IN ADDITION, THE TWO CROSS—CORREL- 
ATIONSs»s NAMELYs THE IN-PHASE SPECTRUM (CO-SPECTRUM) AND THE OUT-—OF- 
PHASE SPECTRUM (QUA-SPECTRUM) FOR THE SIMULTANEOUS TIME RECORDS, ALSO 
COMPUTES THE MEASURE OF COHERENCY OF THE SYSTEMe REFe AML REPORT 131 
(1963)» *IBM 704 POWER-SPECTRUM ANALYSIS'.e 


MRe GENE He GLEISSNER 

HEADs APPLIED MATHEMATICS LABORATORY 

NAVAL SHIP RESEARCH AND DEVELOPMENT CENTER 
WASHINGTONs DeCe 20007 


PROJECT COD LIVER LANGUAGE — FORTRAN II 


AND MAP 
COMPUTER — IBM 7090 


DIGITAL POWER SPECTRA ANALYSISe BASIC WORK PERFORMED WITH HYDROPHONES 


USED FOR WAVE PHENOMENA STUDYe AN SC-4020 PLOTS DATA FOR DISCRETE AM-— 
PLITUDES VSe DISCRETE FREQUENCIESe ALSO USED IS AN ELECTRONIC ENGIN- 


PAGE 050 


EERING COMPANY DATA FORMAT TRANSLATOR (ANALOG-DIGITAL)e (PROGRAM DOCU- 
MENTED BUT CONTROLLED FOR DISTRIBUTION BECAUSE OF CLASSIFIED APPLICA- 
TIONS OF THE SPECIALLY DEVELOPED MATHEMATICAL TECHNIQUES USED) 


MRe GENE He GLEISSNER 

HEADs APPLIED MATHEMATICS LABORATORY 

NAVAL SHIP RESEARCH AND DEVELOPMENT CENTER 
WASHINGTONs DeCe 20007 


POWER SPECTRUM ANALYSIS LANGUAGE —- BASIC 
COMPUTER —- PB-250 
(COPY ON FILE AT NODC) 

COMPUTES POWER SPECTRA» CROSS-SPECTRA»s AND COHERENCIESe THE METHOD OF 
TUKEY IS USED TO CALCULATE THE REQUIRED SINGLE AND CROSS SPECTRAe THE 
MAXIMUM NUMBER OF LAGS ALLOWED IS 240 FOR SINGLE SPECTRUM AND 128 FOR 
CROSS-SPECTRAe MEMORY SIZE-- 696056 AUTHOR-- SeRe CLARKe REFe TECH- 
NICAL MEMORANDUM 64-5 (JULY 1964)e ALSO INCLUDED IN THE TECHe MEMO 
ARE PRETREATMENT AND CALIBRATION PROGRAMS» REFe ALSO PNL LABe NOTE 
61-11 "POWER SPECTRUM ANALYSIS WITH THE LGP-30'. 


PACIFIC NAVAL LABORATORY 
HeMeCe DOCKYARD 
ESQUIMALT» Be Ces CANADA 


POWER SPECTRA ESTIMATION LANGUAGE — FORTRAN 
COMPUTER — CDC 3200 


COMPUTES SPECTRUM AND AUTO-CORRELATION OF ONE TIME SERIES AND/OR THE 
SPECTRA» CO-SPECTRUMs QUADRATURE SPECTRUMs AUTO-CORRELATION AND CROSS- 
CORRELATION OF TWO SIMULTANEOUS TIME SERIESe PERFORMS FOURIER TRANS-— 
FORM ON COVARIANCE FUNCTIONS (TUKEY SPECTRUM ESTIMATION) ALSO PERFORMS 
SMOOTHING ON SPECTRA BY METHOD CALLED "HANNING'e NO OFFICIAL DOCU- 
MENTATION HAS BEEN PUBLISHED. 


NAVAL UNDERWATER WEAPONS RESEARCH 
AND ENGINEERING STATION 

ATTNe CODE DA3B 

NEWPORT» RHODE ISLAND 02840 


HARMONIC ANALYSIS LANGUAGE — MAC 
COMPUTER - ICT 1301 


HARMONIC ANALYSIS USING SHUSTER'S CRITERION FOR THE DETERMINATION OF 
SIGNIFICANT AMPLITUDESe AUTHORS-- AeMe SHIPLEY AND De SACKSe 


UNIVERSITY OF CAPE TOWN 
OCEANOGRAPHY DEPARTMENT 

ATTNe MRe AeMe SHIPLEY 
PRIVATE BAGs RONDEBOSCHs CePe 
REPUBLIC OF SOUTH AFRICA 


NUSPEC LANGUAGE — FORTRAN IV-H 
COMPUTER - SDS SIGMA 7 


A SET OF FOUR PROGRAMS WHICH COMPUTES THE AUTO— AND CROSS-SPECTRAL ES- 
TIMATES FOR TIME SERIES» FOR 1 TO 2048 FREQUENCIES. 


INFORMATION PROCESSING CENTER 

ATTNe ROBERT MILLARD 

WOODS HOLE OCEANOGRAPHIC INSTITUTION 
WOODS HOLEs MASSACHUSETTS 02543 


PAGE 051 


BETA-MODEL WITH WHITE FORCING AND VARIABLE BETA LANGUAGE — FORTRAN IV-H 
COMPUTER - SDS SIGMA-7 
(COPY ON FILE AT NODC) 
PROGRAM USED TO ESTIMATE THE SPECTRUM OF CURRENT RECORDS THAT ARE IR- 
REGULARLY SAMPLED, AND wITH EXTENSIVE GAPS» BY A NEW FORM OF COMPI_EX 
DEMODULATION»s ALLOWING EXAMINATION OF PERIODS UP TO 100 DAYSe SPECIAL 
APPLICATION TO THE SEARCH FOR THE EXISTENCE OF EQUIVALENT-—BAROTROPIC 
TOPOGRAPHIC (ROSSBY) WAVES ON THE WESTERN SIDE OF THE NORTH ATLANTIC. 
THE AUTOSPECTRA LEVEL OFF AT LOWEST FREQUENCIES, NO LONGER INCREASING 
AS A POWER LAWe STRONG COHERENCES WERE FOUND AT LOW FREQUENCIES BE- 
TWEEN THE U AND V COMPONENTS AND BETWEEN THE LEVELSe REFe A TECHNICAL 
REPORT NOe 69-67 (UNPUBLISHED MANUSCRIPT)» AUG 19695 BY RORY THOMPSON.’ 


DRe Ne Pe FOFONOFFs CHAIRMAN 

DEPTe OF PHYSICAL OCEANOGRAPHY 

WOODS HOLE OCEANOGRAPHIC INSTITUTION 
WOODS HOLE, MASSACHUSETTS 02543 


CIRCSTAT LANGUAGE — FORTRAN IV 
COMPUTER — CDC 3400 
(COPY ON FILE AT NODC) 

COMPUTES THE SIGNIFICANT STATISTICS FOR CIRCULAR NORMALLY DISTRIBUTED 
DATAs AS WELL AS GIVING CALCULATIONS FOR USE IN TESTING HYPOTHESESe 
A CONTROL CARD DETERMINES THE TEST PERFORMEDe IN ALL CASES» THE VEC- 
TOR DIRECTION, VECTOR LENGTH», AND VECTOR STRENGTH ARE COMPUTED. TESTS 
OF PREFERRED ORIENTATION ARE CONDUCTED BY THE RAYLEIGH R=-TEST OR BY 
THE GREENWOOD—DURAND U-TESTe BIMODAL DATA MAY BE TREATED BY PROGRAM 
CIRCSTATe REFe TECHNICAL REPORT NOe 39 OFFICE OF NAVAL RESEARCH» FEBe 
1967» BY THOMAS Ae JONES. 


DEPARTMENT OF GEOLOGY 
NORTHWESTERN UNIVERSITY 
EVANSTONs ILLINOIS 60201 


BOMM (TIME SERIES) LANGUAGE — FORTRAN» 
COMPASS 

COMPUTER — IBM 0S/3605 
CDC 3600 


A COLLECTION OF PROGRAMS HAVING TIME SERIES AS OPERANDS PRIMARILY DE- 
SIGNED FOR ANALYSIS» CORRELATION AND DECOMPOSITION OF RECORDSe COPIES 
AVAILABLE THROUGH 'SHARE' AND 'COOP'e AUTHORS-- SIR EDWARD BULLARD» 
MRSe FLORANCE OGALBY DORMER, WALTER MUNK AND GAYLORD MILLERe 


MRSe FLORENCE Oe DORMER 

INSTITUTE OF GEOPHYSICS AND PLANETARY PHYSICS 
SCRIPPS INSTITUTION OF OCEANOGRAPHY 

PeO- BOX 109 

LA JOLLA» CALIFORNIA 92037 


ANALYSIS OF NON-LINEAR RESPONSE SURFACE LANGUAGE — FORTRAN IV 
COMPUTER — IBM 1130 
(COPY ON FILE AT NODC) 

ANALYZES THE DATA FROM RESPONSE SURFACE EXPERIMENTS WHEN TWO OR THREE 
FACTORS ARE MEASUREDe OPTIONS ALLOW CALCULATION OF MAXIMUM LIKELIHOOD 
ESTIMATES OF POWER TRANSFORMATIONS OF BOTH INDEPENDENT AND DEPENDENT 
VARIABLES, AND THE PLOTTING OF THEIR RELATIVE MAXIMUM LIKELIHOOD 
GRAPHS» AS A MEASURE OF THE PRECISION OF THE ESTIMATESe THE DATA IS 
THEN SUBJECTED TO ANALYSIS OF VARIANCEs USING ORTHOGONAL POLYNOMIALS, 
AND PRINCIPAL COMPONENT ANALYSIS», AND SPECIFIED CONTOURS OF THE DEPEN- 
DENT VARIABLE ARE PLOTTED, BOTH WITHOUT AND WITH TRANSFORMATIONe REFe 
FRB TECHNICAL REPORT NO. 87 (PUBLISHED MANUSCRIPT» AUG 1968) BY Je Ke 
LINDSEYe DIRECT INQUIRIES TO-- 


FISHERIES RESEARCH BOARD OF CANADA 
BIOLOGICAL STATION 
NANAIMO, Be Ceo 


PAGE 052 


MULDA LANGUAGE - FORTRAN IV 
COMPUTER - IBM 1130 
(COPY ON FILE AT NODC) 
A COMPLETE MULTIPLE DISCRIMINANT ANALYSIS IS PERFORMED By SIX INTERRE- 
LATED PROGRAMS WHICH ARE EXECUTED IN SUCCESSION THROUGH THE LINK FEA- 
TURE IN 1130 FORTRANe WILL ACCEPT UP TO 25 VARIATES AND AS MANY AS 10 
GROUPSe ANY NUMBER OF ADDITIONAL DATA CARDS CAN BE READ AND PROCESSED 
AFTER THE DISCRIMINANT ANALYSIS HAS BEEN COMPLETEDe THE VALUE OF THE 
DISCRIMINANT FUNCTION» CLASSIFICATION CHI-SQUARES AND PROBABILITIES OF 
GROUP MEMBERSHIP ARE COMPUTED AND PRINTED FOR EACH ADDITIONAL M-VARI- 
ATE OBSERVATIONe AUTHORS-- LeVe PIENAAR AND JeAce THOMSON, FRB TECHNI- 
CAL REPORT NOo 112» MAR 1969 (UNPUBLISHED MANUSCRIPT)e DIRECT INQUIR- 


HES Os 


FISHERIES RESEARCH BOARD OF CANADA 


BIOLOGICAL STATION 
NANAIMOs BeCo ; 


SCALING SUBROUTINE LANGUAGE — FORTRAN 
COMPUTER -— CDC 3800 


SCALES AN ARRAY OF FLOATING POINT NUMBERS» CORRESPONDING TO A SINGLE 
COORDINATEs PREPARING THEM FOR INPUT TO THE 565 CALCOMP PLOTTERe NRL 
MEMOe REPORT 2047¢ AUTHORS-- Je LANGWORTHY»s Je HOUSTONe 


JAMES Be LANGWORTHY 

THEORY BRANCH 

NUCLEAR PHYSICS DIVISION 

NAVAL RESEARCH LABORATORY» WASHINGTON» De Ce 20390 


EVALUATE BESSEL FUNCTIONS LANGUAGE — FORTRAN 
COMPUTER - CDC 3800 


A SET OF SUBROUTINES THAT EVALUATEs IN SINGLE AND DOUBLE PRECISION» 
BESSEL FUNCTIONS OF THE FIRST AND SECOND KINDS FOR ORDERS ZERO AND ONE 
FOR POSITIVE REAL ARGUMENTS. ALSO TO EVALUATEs IN SINGLE AND DOUBLE 
PRECISION» BESSEL FUNCTIONS OF THE FIRST AND SECOND KINDS FOR INTEGER 
OR FRACTIONAL ORDERS AND POSITIVE REAL ARGUMENTSe NRL MEMOe REPORTS 
1975-19782 AUTHORS-—- Je MASONs Re BAIERe 


JANET Pe MASON 

RESEARCH COMPUTATION CENTER 

MATHEMATICS AND INFORMATION SCIENCES DIVISION 
NAVAL RESEARCH LABORATORY» WASHINGTONs De Co 20390 


DETERMINANT OF A REAL SYMMETRIC MATRIX LANGUAGE — FORTRAN 
COMPUTER - CDC 3800 


A SUBROUTINE WRITTEN AT ARGONNE NATIONAL LABORATORY THAT SOLVES» IN- 
VERTS»s AND FINDS THE DETERMINANT OF SYMMETRIC REAL MATRICES» HAS BEEN 
MODIFIEDe IT REQUIRES THAT ONLY THE UPPER TRIANGULAR PORTION OF THE 
MATRIX BE INPUT» THEREBY REDUCING THE MATRIX STORAGE REQUIREMENT TO 
N(N+1)/72 LOCATIONSe NRL MEMOe REPORT 20090 AUTHOR-- Jo MASON 


JANET Pe MASON 

RESEARCH COMPUTATION CENTER 

MATHEMATICS AND INFORMATION SCIENCES DIVISION 
NAVAL RESEARCH LABORATORY» WASHINGTONs De Ceo 20390 


SUBROUTINE TO FIND THE REAL ZEROS OF A LANGUAGE — FORTRAN 
SINGLE-VALUED FUNCTION OF ONE REAL VARIABLE COMPUTER - CDC 3800 


FINDS THE REAL ZEROS OF A SINGLE-VALUED FUNCTION OF ONE REAL VARIABLE 
BY A MODIFIED METHOD OF FALSE POSITIONe FINDS WITHIN A SPECIFIED TOL- 


PAGE 053 


ERANCE (DELTA) THOSE POINTS X(I) ALONG A GIVEN CLOSED INTERVAL FOR 
WHICH THE FUNCTIONAL VALUE FX(I) SATISFIES THE ABSOLUTE VALUE OF FX(T) 
LESS THAN DELTA. EACH POINT AND THE CORRESPONDING FUNCTIONAL VALUE 
ARE STORED IN A TABLEe NRL MEMO.’ REPORT 1974+¢ AUTHORS-—- Je MASON> 

He TOOTHMAN. 


JANET P. MASON 

RESEARCH COMPUTATION CENTER 

MATHEMATICS AND INFORMATION SCIENCES DIVISION 
NAVAL RESEARCH LABORATORY» WASHINGTON; De Ce 20390 


CROSS-—ASSOCIATION OF NONNUMERIC SEQUENCES LANGUAGE — ALGOL 60 AND 
FORTRAN IV 

COMPUTER — ELLIOTT 803C 
IBM 7040/44 


READS A PAIR OF SEQUENCES WHOSE ELEMENTS BELONG TO A NONORDERED SETe 
THE DATA ARE READ IN A NUMERIC CODEe THE PROGRAM SLIDES THE SEQUENCES 
PAST EACH OTHER ONE OR MORE STEPS AT A TIME AND FOR EACH MATCH POSI- 
TION COUNTS THE NUMBER OF COMPARISONS (SIZE OF OVERLAP) e VARIOUS SIG- 
NIFICANCE MEASURES AND OVERALL SIMILARITY ESTIMATES ARE MADEe AUTHORS-— 
MeJe SACKIN AND PeHeAe SNEATHs UNIVe OF LEICESTER» DeFe MERRIAM, KAN- 
SAS GEOLe SURVEYe REFe SPECIAL DISTRIBUTION PUBLICATION 23 (1965).e 


DRe DANIEL Fe MERRIAMs EDITOR», COMPUTER CONTRIBUTIONS 
KANSAS GEOLOGICAL SURVEY 

COMPUTER APPLICATIONS LABORATORY 

THE UNIVERSITY OF KANSAS 

LAWRENCE» KANSAS 66045 


SIMULATION OF TRANSGRESSION AND REGRESSION WITH LANGUAGE - FORTRAN IV 
CONTINUOUS-TIME MARKOV MODELS COMPUTER - CDC 6400 


REPORT (COMPUTER CONTRIBUTION 26) IS CONCERNED WITH A STOCHASTIC SIMU- 
LATION MODEL IN WHICH THE PATTERN OF LITHOLOGIC SUCCESSION IS EXAMINED 
IN TERMS OF THE LENGTH OF TIME THAT THE SYSTEM REMAINS IN A GIVEN 
STATEs ONCE IT HAS ENTERED THAT STATEe THE MODEL IS ALSO BASED ON 
TRANSGRESSIVE-REGRESSIVE MOTION OF A SHORELINE (OR STRANDLINE)», WITH 
THE RESULTING LITHOLOGIC UNITS DEVELOPING AS RESPONSES TO THE MOVEMENT 
OF SEDIMENTARY MARINE OR NONMARINE ENVIRONMENTS LATERALLY AND THROUGH 
TIMEe AUTHOR-- WeCe KRUMBEINe TWO COMPUTER PROGRAMS ARE LISTED IN 
THE APPENDIX» ONE FOR TRANSFORMING A TRANSITION PROBABILITY MATRIX TO 
ITS CORRESPONDING TRANSITION RATE MATRIX AND VICE VERSA, AND THE OTHER 
("BOREHOLE') FOR SIMULATING LATERAL-SHIFT PHENOMENA, SUCH AS TRANS-— 
GRESSION AND REGRESSION WITH A CONTINUOUS-TIME DISCRETE-STATE MARKOV 
MODELe 


DRe DANIEL Fe MERRIAMs EDITOR 
COMPUTER CONTRIBUTIONS 

KANSAS GEOLOGICAL SURVEY 

THE UNIVERSITY OF KANSAS 
LAWRENCE» KANSAS 66044 


POWER SPECTRUM OF GEOLOGICAL SURFACES LANGUAGE — FORTRAN Iv 
COMPUTER -— GE 625 AND 
IBM 7040 


TWO-DIMENSIONAL POWER SPECTRUM IS USED FOR NUMERICAL DESCRIPTION OF 
OBSERVED SURFACESe DATA MUST BE GRIDDED — MAXIMUM IS 100 BY loo 
POINTSe RUNNING TIME FOR MAXIMUM ARRAY IS ABOUT 20 MINUTES ON GE 625. 
COMPUTER CONTRIBUTION 16% BY JeE5s ESLER AND FeWe PRESTONs 19674 


DRe DANIEL Fe MERRIAMs EDITOR 
COMPUTER CONTRIBUTIONS 

KANSAS GEOLOGICAL SURVEY 

THE UNIVERSITY OF KANSAS 
LAWRENCE» KANSAS 66044 


PAGE 054 


TREND ANALYSIS USING DOUBLE FOURTER SERIES LANGUAGE -— FORTRAN IV 
COMPUTER — GE 625 


HARMONIC ANALYSIS USEFUL FOR DATA SUSPECTED OF CONTAINING OSCILLATORY 
PHENOMENAe DESIGNED FOR DATA OBTAINABLE ON A REGULARLY SPACED, RECT- 
ANGULAR GRIDe THE PROGRAM COMPUTES COEFFICIENTS OF FOURIER SERIES AND 
EVALUATES AND PLOTS THE FUNCTIONe ALSO COMPUTES AND PLOTS RESIDUAL 
VALUESe ALLOWS UP TO 71 X 73 GRID POINTS AND UP TO 25TH HARMONIC IN 
BOTH DIRECTIONS. COMPUTER CONTRIBUTION 293 BY JOHN We HARBAUGH AND 
MICHAEL Je SACKIN (JUNE 1968)e AN EARLIER PROGRAM WAS DEVELOPED FOR 
DOUBLE FOURIER SERIES ANALYSIS OF SURFACES WITH IRREGULARLY SPACED 
DATAe REFe COMPUTER CONTRIBUTION 53s BY WeRe JAMES (1966). 


DRe DANIEL Fe MERRIAMs EDITOR 
COMPUTER CONTRIBUTIONS 

KANSAS GEOLOGICAL SURVEY 

THE UNIVERSITY OF KANSAS 
LAWRENCE» KANSAS 66044 


FOURIER ANALYSIS — PROGRAM L101 LANGUAGE -— FORTRAN 
COMPUTER —- IBM 7090 
(COPY ON FILE AT NODC) 
OBTAINS AMPLITUDES AND PHASES OF FREQUENCY COMPONENTS IN ANY RECORDe 
STANDARD FOURIER ANALYSIS PLUS USE OF TUKEY COSINE WINDOW TO REDUCE 
EDGE EFFECTSe CORE STORAGE USED-- 32Ke AUTHOR-- ALSOPe 


LAMONT-DOHERTY GEOLOGICAL OBSERVATORY 
COLUMBIA UNIVERSITY 
PALISADES» NEW YORK 10964 


CLUSTER ANALYSIS LANGUAGE - FORTRAN 
COMPUTER —- I6M 1800 SYS 
(COPY ON FILE AT NODC) 

CARRIES OUT A SINGLE LINKAGE CLUSTER ANALYSIS USING DATA IN THE FORM 

OF AN UPPER TRIANGULAR SIMILARITY MATRIXe OUTPUT-- A) SIMILARITY LEv- 

BEVORMGEUSTERTINGTGEYGUEs) /B) JANELST Oh TE TEINKAGES! THAT OGGURE Ary HAT 

SIMILARITY LEVEL» C) AT THE END OF THE CYCLE THE CLUSTER NUMBERS AND A 

LIST OF THE ENTITIES MAKING UP EACH CLUSTER IS PRINTEDe RUN TIME-- 

A MATRIX OF ORDER 60 TOOK APPROXIMATELY 15 MINUTES TO CLUSTERe NeleQe 

PROGRAM NO. 1666 AUTHOR-- Me FASHAMe 


NATIONAL INSTITUTE OF OCEANOGRAPHY 
WORMLEY»s GODALMINGs SURREY 
ENGLAND 


Q-MODE CLUSTER ANALYSIS LANGUAGE - FORTRAN IV 
COMPUTER - IBM 7090/94»5 
IBM 360/67 


CLASSIFIES OBJECTS INTO GROUPS ON THE BASIS OF A LARGE NUMBER OF NON- 
QUANTITATIVE CHARACTERSe HAS BEEN USED FOR GEOLOGICAL SAMPLES, BIO- 
LOGICAL TAXONOMYs ETCe RANGE LIMITED TO 130 OBJECTS AND 100 ATTRI- 
BUTESe OUTPUT MAY BE USED TO DRAW DENDROGRAMS WITH A CALCOMP PLOTTER. 
REFe COMPUTER CONTRIBUTION 17¢ AUTHOR-- GeFe BONHAM-—CARTER» STANFORD 
UNIVERSITY. 


DRe DANIEL Fe MERRIAMs EDITOR 
COMPUTER CONTRIBUTIONS 

KANSAS GEOLOGICAL SURVEY 

THE UNIVERSITY OF KANSAS 
LAWRENCE» KANSAS 66044 


MULTIVARIATE DISCRIMINANT ANALYSIS LANGUAGE - FORTRAN II 
COMPUTER - IBM 1620 


PAGE 05 


COMPUTES THE MULTIVARIATE DISCRIMINANT FUNCTION AND MAHALANOBI 5S! GEN- 
ERALIZED DISTANCE FOR TWO GROUPS, ANALYZES THE SIGNIFICANCE OF THE 
DIFFERENCE BETWEEN THE GROUPS, AND CLASSIFIES INDIVIDUAL SAMPLESe 20 
VARIABLES MAY BE CONSIDERED SIMULTANEOUSLY+* THE TWO SAMPLE GROUPS MAY 
CONTAIN ANY NUMBER OF SAMPLESe MATRIX INVERSION IS AVOIDED BY USING A 
MODIFICATION OF A PROCEDURE SUGGESTED GY RAO IN WHICH SAMPLES ARE OP— 
ERATED UPON ONE AT A TIMEe USES POOLED ESTIMATES OF VARIANCE AND CO- 
VARIANCE IN A SERIES OF SIMULTANEOUS EQUATIONS, WHICH ARE SOLVED BY 
THE GAUSS-JORDAN METHOD OF APPROXIMATIONSe CORE STORAGE USED-—- 20 Ke 
AUTHORS—-- JeCe DAVIS AND ReJe SAMPSON» COMPUTER CONTRIBUTION NOs Ge 


DRe DANIEL Fe MERRIAMs EDITORs COMPUTER CONTRIBUTIONS 
KANSAS GEOLOGICAL SURVEY 

THE UNIVERSITY OF KANSAS 

LAWRENCE» KANSAS 66044 


TWO-DIMENSIONAL AUTOCORRELATION LANGUAGE - FORTRAN 
COMPUTER — IBM 7090 AND 
IBM 1401 


(COPY ON FILE AT NODC) 
APPLIES REGRESSION AND CORRELATION ANALYSES TO A SAMPLE OF OCEAN TERR- 
AIN.e COMPUTES VARIANCE AND COVARIANCE AS FUNCTION OF POSITION IN DATA 
FIELDe REFe ARTHUR De LITTLEs INCe TECHNICAL REPORT NOe 1440464 -— 
"STATISTICAL ANALYSES OF QCEAN TERRAIN AND CONTOUR PLOTTING PROCED-— 
URESte APPENDICES B AND C OF REPORT DESCRIBE (BUT DO NOT LIST) TWO 
ROUTINES USED — 'CORRELATION CONSTANTS?! (IBM 7090 FORTRAN) AND 'tLOCAL 
MEANS AND VARIANCES! (IBM 1401 FORTRAN)« THE AeDe NOw IS AD-601-538. 
COPIES HAVE BEEN DEPOSITED WITH THE DEFENSE DOCUMENTATION CENTER. 


MISS MARIAN Le HOBBS» LIBRARIAN 
TRIDENT/ASW LIBRARY 

ARTHUR De LITTLEs INCe 

35 ACORN PARK 

CAMBRIDGE» MASSe 02140 


STAT USY IES Wo. Who WIM LANGUAGE — FORTRAN Iv 
COMPUTER — CDC 3100 
(COPY ON FILE AT NODC) 
THREE SEPARATE PROGRAMS FOR THE PROCESSING OF LIMNOLOGICAL DATAe THEY 
CALCULATE MEANS», STANDARD DEVIATIONSs STANDARD ERRORS AND OTHER STAT-— 
ISTICS OF VARIOUS LIMNOLOGICAL PARAMETERSe STATISTICS I GIVES WEIGHT— 
ED CRUISE-MEAN VALUES» CRUISE-MEAN EPILIMNION AND HYPOLIMNION VALUES, 
TABULATIONS OF THE RELATION BETWEEN TEMPERATURE AND OTHER PARAMETERS, 
AND NEAR-BOTTOM MEANSe STATISTICS II IS ESPECIALLY DESIGNED TO STUDY 
REGIONAL ANOMALIES IN THE DISTRIBUTION OF ANY PARAMETERe STATISTICS 
III IS A MORE SPECIALIZED PROGRAM ANALYSING THE VARIABILITY IN A SET 
OF DATA IN TERMS OF RANDOM AND SYSTEMATIC COMPONENTS INPUT-—- DATA ON 
TAPE IN CODC FORMATe PROGRAMS DESCRIBED IN MANUSCRIPT REPORT NOe 13 
(1970)>5 BY DRe He Ee SWEERS,. 


MARINE SCIENCES BRANCH 

DEPARTMENT OF ENERGY, MINES AND RESOURCES 
615 BOOTH STREET 

OTTAWAs ONTARIOs CANADA 


CURRENT LANGUAGE — FORTRAN IV 
COMPUTER - OS/360 


PROVIDES ELEMENTARY STATISTICS FOR THREE TIME SERIES OF CURRENT TEMP- 
ERATURE» SPEED» AND DIRECTIONe MEANS ARE COMPUTED HOURLY» DAILY AND 
FOR THE ENTIRE SERIESe A HISTOGRAM IS PROVIDED DAILY AND FOR THE SER- 
IES. VARIANCE AND STANDARD DEVIATION ARE COMPUTED FOR THE SERIESe 
OPTIONAL GRAPHICAL OUTPUTS HISTOGRAMS ARE PROVIDEDe APPLICATIONS ARE 
MADE TO CONTINUOUS BOTTOM CURRENT MEASUREMENTS IN A SUBMARINE CANYON 
AND CONCURRENT WIND» WAVE, AND TIDAL DATA» IN THESES BY JeJe DOOLEY» 
JUN 19685 AND BY IeJse NJUS»s DEC 19686 


PAGE 056 


NAVAL POSTGRADUATE SCHOOL 
MONTEREYs CALIFORNIA 93940 


SINGLE INTEGRATION LANGUAGE — FORTRAN 
COMPUTER ~- IBM 7074 


EQUALLY SPACED TIME SERIES DATA IS INTEGRATED ONCE USING TICK'S METH- 
THE DATA MUST BE SAMPLED AT A RATE OF AT LEAST TWICE THE NYQUIST 


ODe 
FREQUENCYe OS NOce 53477¢ AUTHOR-- DeBe ROSSe REFe IM NOo 66-36. 


EXPLORATORY OCEANOGRAPHY DIVe» CODE 7200 


NAVAL OCEANOGRAPHIC OFFICE 
SUITLAND» MDe 20390 


LANGUAGE -— FORTRAN IV-H 
COMPUTER - SDS SIGMA 7 


STATS 
COMPUTES AND LISTS STATISTICAL QUANTITIES RELATED TO VARIABLES STORED 
ON TAPE IN WHOI STANDARD DATA FORMAT. 

INFORMATION PROCESSING CENTER 


ATTNe JOHN Ace MALTAIS 
WOODS HOLE OCEANOGRAPHIC INSTITUTION 


WOODS HOLE, MASSACHUSETTS 02543 


PAGE 057 


NAVIGATION AND CHARTING 
H—K—K—HK—-K—¥ —H—H—H—H—H—H 


SATELLITE NAVIGATION LANGUAGE — FORTRAN AND 
ASSEMBLER 
COMPUTER -— IBM 1800 SYS 
(COPY ON FILE AT NODC) 
A SET OF PROGRAMS FOR VARIOUS ASPECTS OF SATELLITE NAVIGATIONe THE 
PROGRAMS FALL NATURALLY INTO TWO SECTIONS» THOSE INVOLVED IN THE ON- 
LINE REDUCTION OF DATA FROM THE SATELLITE AND THOSE INVOLVED IN THE 
ANALYSIS BOTH ON-LINE AND OFF-LINEe REFe NeIeOe REPORT Ne20»s AUG 28 
19696 


NATIONAL INSTITUTE OF OCEANOGRAPHY 
ATTNe MRe JAMES CREASE 

WORMLEY»s GODALMINGs SURREY 

ENGLAND 


ALERT LANGUAGE — FORTRAN IV 
COMPUTER - IBM 1130 
(COPY ON FILE AT NODC) 
CALCULATES THE RISE AND SET TIMES AND TIME OF CLOSEST APPROACH OF SAT- 
ELLITESe OUTPUT FROM PROGRAM IS A LISTING OF ALERT INFORMATION» AND 
PUNCH CARDS FOR NEXT PROGRAM 'ASORT'e CORE STORAGE USED-- 5836 WORDS. 


DRe Ce Ae COLLINS 

MARINE SCIENCES BRANCHs DEMR 
PACIFIC OCEANOGRAPHIC GROUP 
BIOLOGICAL STATION 

NANAIMO»s BeCes CANADA 


ASORT LANGUAGE — FORTRAN IV 
COMPUTER — IBM 1130 
(COPY ON FILE AT NODC) 

SORTS THE OUTPUT OF RISE TIMES OF SATELLITES FROM THE PROGRAM *ALERT! 
IN CHRONOLOGICAL ORDERe A LISTING IS PRINTED ON THE IBM 1132e CORE 
STORAGE REQUIREMENTS-— 129040 WORDSe DESCRIPTIONS OF BOTH PROGRAMS 
ARE IN FRB MANUSCRIPT REPORT NOe 1071 (DEC 1969)5 BY CeAew COLLINS» Re 
LeKe TRIPEs AND SeKe WONG (UNPUBLISHED MANUSCRIPT) e 


DRe Ce Ae COLLINS 

MARINE SCIENCES BRANCHs DEMR 
PACIFIC OCEANOGRAPHIC GROUP 
BIOLOGICAL STATION 

NANAIMO s BeCe» CANADA 


BECNAV (BEACON NAVIGATION PROGRAM) LANGUAGE — FORTRAN 
COMPUTER - CDC 3200 
(COPY ON FILE AT NODC) 

COMPUTES THE SHIPS POSITION AT EACH FIX FROM TwO OR MORE BEACONS WHOSE 
POSITION HAS BEEN ACCURATELY DETERMINEDe A FIX CONSISTS OF THE DELAY 
TIMES FROM TWO OR MORE BEACONSe CORE STORAGE NEEDED-— ABOUT 8K WORDS. 
AUTHOR-— Se KOCHANSKI» NSSNFe (PROGRAM DOCUMENTATION UNCLASSIFIED BUT 
DISTRIBUTION CONTROLLED BY NSSNF) 


COMMANDING OFFICER 

NAVAL STRATEGIC SYSTEMS NAVIGATION FACILITY 
FLUSHING AND WASHINGTON AVENUES 

BROOKLYN» NEW YORK 11251 


SPANS1A LANGUAGE — FORTRAN 
COMPUTER — CDC 3200 
(COPY ON FILE AT NODC) 


COMPUTES THE RELATIVE POSITION OF A TRIAD OF BEACONS USING THE DELAY 


PAGE 058 


TI@ES FROM THREE BEACONSe LIMIT, 40 FIXES PER TRACKe CORE STORAGE 
NEEDED-- ABOUT 14K WORDSe AUTHOR-— Se KOCHANSKI» NSSNF eo (PROGRAM 
DOCUMENTATION UNCLASSIFIED BUT DISTRIBUTION CONTROLLED By NSSNF) 


COMMANDING OFFICER 

NAVAL STRATEGIC SYSTEMS NAVIGATION FACILITY 
FLUSHING AND WASHINGTON AVENUES 

BROOKLYN» NEW YORK 11251 


SPANS1B LANGUAGE — FORTRAN 
COMPUTER -— CDC 3200 
(COPY ON FILE AT NODC) 
TRANSLATES AND ROTATES A SET OF BEACON COORDINATES FROM LOCAL COORDIN- 
ATES TO GEODETIC COORDINATESe INPUT TO PROGRAM-- SHIPS POSITIONS FROM 
EXTERNAL FIXES AND CORRESPONDING POSITIONS FROM *#*BECNAV! PROGRAM, AND 
BEACON POSITIONS IN LOCAL COORDINATES FROM 'SPANS1A'e AUTHOR-- Se KO- 
CHANSKI» NSSNFe (PROGRAM DOCUMENTATION UNCLASSIFIED BUT DISTRIBUTION 
CONTROLLED BY NSSNF ) 


COMMANDING OFFICER 

NAVAL STRATEGIC SYSTEMS NAVIGATION FACILITY 
FLUSHING AND WASHINGTON AVENUES 

BROOKLYNs NEW YORK 11251 


GREAT CIRCLE DISTANCE BETWEEN TwO POINTS LANGUAGE -— FORTRAN 
COMPUTER — CDC 3800 


DETERMINES THE DISTANCE IN NAUTICAL MILES ALONG THE GREAT CIRCLE PATH 

BETWEEN TwO POINTS ON THE EARTHs AND THE INITIAL AND FINAL BEARINGS OF 
THAT PATHe THE EARTH IS ASSUMED SPHERICAL WITH ONE NAUTICAL MILE PER 

MINUTE OF ARCe DOCUMENTATION AVAILABLE-- NRL COMPUTER NOTE 32.6 


DAVID CHANG» CODE 8170 
ACOUSTICS DIVISION 
NAVAL RESEARCH LABORATORY» WASHINGTON» De Ce 20390 


GREAT CIRCLE PATHS FROM A POINT LANGUAGE — FORTRAN 
COMPUTER - CDC 3800 


FROM A GREAT CIRCLE PATH SPECIFIED BY AN INITIAL POINT AND BEARING» 
THE PROGRAM GIVES THE LOCATIONS AND BEARINGS OF POINTS AT A GIVEN AR- 
RAY OF DISTANCES IN NAUTICAL MILES ALONG THAT PATHe DOCUMENTATION —- 
NRL COMPUTER NOTE 336 


DAVID CHANGs CODE 8170 
ACOUSTICS DIVISION 
NAVAL RESEARCH LABORATORY» WASHINGTONs De Ce 20390 


ASTRONOMIC POSITIONs AZIMUTH METHOD LANGUAGE -— FORTRAN IV-H 
COMPUTER - IBM 360/65 
(COPY ON FILE AT NODC) 

CALCULATES THE LATITUDE AND LONGITUDE OF AN ASTRONOMIC OBSERVATION 
STATIONs GIVEN MEASURED HORIZONTAL ANGLES BETWEEN STARS AND FIXED MARK 
ALONG WITH THE OBSERVATION TIMESe A SET OF OBSERVATION EQUATIONS IS 
SOLVED BY THE METHOD OF LEAST SQUARES TO OBTAIN CORRECTIONS TO ASSUMED 
VALUES OF LATITUDE, LONGITUDE, AND THE AZIMUTH OF THE REFERENCE MARK 
AS WELL AS PROBABLE ERRORS FOR THESE THREE QUANTITIESe THE ADJUSTMENT 
IS ITERATED FIVE TIMES OR UNTIL THE CORRECTIONS BECOME LESS THAN 00005 
SECONDS» EITHER OF WHICH CAUSES A PROGRAM HALT» OUTPUT-- A TABLE OF 
INPUT INFORMATION AND A RECORD OF THE PROCESS OF REFINEMENT FOR EACH 
SET OF STATION DATA READ INe STORAGE NEEDED-- APPROXe 373500 BYTES 
FOR THE PROGRAM PLUS ITS SUBROUTINESe AUTHOR-- SPENCER ROEDDERe A 
PREVIOUS VERSION OF THIS PROGRAM WAS WRITTEN IN ALGOL FOR THE BUR- 
ROUGHS 2205 IN SINGLE PRECISIONe 


UeSe GEOLOGICAL SURVEY 


PAGE 059 


COMPUTER CENTER DIVISION 

ATTNe RALPH EICHERs CHIEF 

BRANCH OF SCIENTIFIC APPLICATIONS 
WASHINGTONs De Ce 20242 


ASTRONOMIC LATITUDE LANGUAGE -— FORTRAN 
COMPUTER - (NOT GIVEN) 


(COPY ON FILE AT NODC) 

DETERMINATION OF FIRST ORDER ASTRONOMIC LATITUDE BY THE STERNECK METH- 
ODe ALSO A PROGRAM USING THE METHOD OF *#POLARIS AND SOUTH STAR'e ALSO 
SUBROUTINES FOR THE BALDINI, THE GARFINKEL» AND THE UeSe COAST AND GE- 
ODETIC SURVEY REFRACTION MODELSe REFe A REPORT *INVESTIGATIONS IN DE- 
TERMINING ASTRONOMIC LATITUDES AND THEIR COMPUTER PROGRAMS! IR NOs 68- 
21 (189 Pes APR 1968)e¢ AUTHOR-- LARRY BOURQUINs CODE 84305 GEODESY. 
FURTHER INFORMATION MAY BE OBTAINED THROUGH DISSEMINATION DEPARTMENT — 
CODE 44s OR THE AUTHORe 


NAVAL OCEANOGRAPHIC OFFICE 
SUITLAND» MDe 20390 


DEAD RECKONING NAVIGATION SYSTEM LANGUAGE — FORTRAN 
COMPUTER —- IBM 1130 


THIS SYSTEM IS USED AS A NAVIGATION AID TO COMPUTE AND PLOT THE CRUISE 
TRACK OF THE SHIP AND TO INDICATE THE LOCATIONS AT WHICH DATA WERE 
COLLECTED EN ROUTEe’ INPUT TO PROGRAM-—- SHIP'S SPEED AND HEADING» WIND 
SPEED AND DIRECTION FROM PAPER TAPE (HEWLETT-PACKARD DATA ACQUISITION 
SYSTEM)» AND FIXES ON CARDS. OUTPUT-- PLOT OF CRUISE TRACKe 
DOCUMENTATION-— OPERATING INSTRUCTIONS ONLYe 


UNIVERSITY OF WASHINGTON 
DEPARTMENT OF OCEANOGRAPHY 

22A OCEANOGRAPHY TEACHING BLDGe 
ATTNe MRSe HELLA MACINTOSH 
SEATTLEs WASHe 98105 


REDUCTION AND DISPLAY OF DATA ACQUIRED AT SEA LANGUAGE -— FORTRAN II 
COMPUTER -— IBM 1130 
(COPY ON FILE AT NODC) 

A SYSTEM OF PROGRAMS (NAVIGATION, GRAVITYs TOPOGRAPHY» MAGNETICS) FOR 
THE REDUCTIONs STORAGE AND DISPLAY OF UNDERWAY DATA ACQUIRED AT SEAe 
THE COMPUTER INSTALLATION CONSISTS OF AN IBM 1130 AND INCLUDES RANDOM 
ACCESS DISK CARTRIDGES AND AN ON-LINE CALCOMP 30 INe PLOTTERe A !ARGE 
NUMBER OF THE PROGRAMS UTILIZE NAVIGATION POINTS TOGETHER WITH RAW 
DIGITIZED GEOPHYSICAL DATA PRESENTED AS A TIME SERIES, WHERE THE DIFF- 
ERENT DATA MAY BE READ AT UNEQUAL TIME INTERVALSe REFe TECHe REPORT 
NOs 1 (AUGUST 19695 348 Pe) BY MANIK TALWANIe 


LAMONT-DOHERTY GEOLOGICAL OBSERVATORY 
COLUMBIA UNIVERSITY 
PALISADES» NEW YORK 10964 


SODANO INVERSE LANGUAGE —- FORTRAN 
COMPUTER — CDC 3100 
(COPY ON FILE AT NODC) 

COMPUTES THE NORMAL SECTION LENGTH AND THE FORWARD AND REVERSE AZI- 
MUTHS OF THE GEODESIC BETWEEN TWO POINTS FOR WHICH THE GEOGRAPHIC CO- 
ORDINATES ARE KNOWNe THIS COMPUTATION IS USEFUL IN DETERMINING AzI- 
MUTH AND DISTANCE BETWEEN TRIANGULATION STATIONS FOR WHICH GEOGRAPHIC 
POSITIONS HAVE BEEN DETERMINED BUT WHICH ARE NOT CONNECTED BY DIRECT 
OBSERVATIONe OS NOe 42366 AUTHOR-—- ANDREW CAMPBELLe MODIFIED By C. 
Ee PIERCE, MARCH 1967-6 


GEODESY DIVISION» CODE 8420 
NAVAL OCEANOGRAPHIC OFFICE 
SUITLAND MDe 20390 


PAGE 060 


SUBROUTINE 'CIRAZD! LANGUAGE — FORTRAN 
COMPUTER - IBM 7074 
(COPY ON FILE AT NODC) 

FINDS THE DISTANCE AND AZIMUTH BETWEEN TWO POINTS ON THE EARTH'S SUR- 

FACE WHEN THE EARTH IS ASSUMED TO BE A SPHERE= Re liheR POSE STS USED 

FOR THE CENTER POINTs THE ANGLE GIVEN IS WITH RESPECT TO GRID NORTHe 

BY USE OF TRIGONOMETRIC IDENTITIES AND ABSOLUTE VALUE FUNCTIONS», THIS 

PROGRAM AVOIDS MANY OF THE COMPUTATIONAL PROBLEMS USUALLY FOUND IN 

DISTANCE COMPUTATIONSe OceSe NO 5569056 AUTHOR-- BARRY TURETT. 


NAUTICAL CHART DIVISION» CODE 5600 
NAVAL OCEANOGRAPHIC OFFICE 
SUITLAND» MDe 20390 


CIRCULAR CHARTING LANGUAGE - FORTRAN 
COMPUTER -— IBM 7074 


COMPUTES COORDINATES FOR CONCENTRIC CIRCLES AT SPECIFIED INTERVALS 
ALONG LATITUDE AND/OR LONGITUDE WITH A FIXED BROADCASTING STATION 
POSITION AS COMMON CENTERe COMPUTED DISTANCES ARE GEODESICS BASED 
ON ANY SPECIFIED GEOIDe OS NOe 201326 AUTHOR-- CHARLES KIRKLAND. 


COMPUTER DEPARTMENTs CODE 0831 
NAVAL OCEANOGRAPHIC OFFICE 
SUITLANDs MDe 20390 


GEODETIC DATUM CONVERSION LANGUAGE - FORTRAN 
COMPUTER -— IBM 7074 


TRANSFORMS GEODETIC COORDINATES FROM ONE DATUM TO ANOTHER BY UTILIZING 
A GIVEN SHIFT (IN TERMS OF RECTANGULAR SPACE COORDINATES) BETWEEN THE 
ORIGINS OF TWO DATUMS AND APPLYING THIS SHIFT» TOGETHER WITH DIFFER- 
ENCES IN THE SPHEROIDAL PARAMETERS: IN FORMULAS DERIVED FOR THIS PUR- 
POSEe OS NOe 55305¢ AUTHOR-- ROBERT Me WILLEMSe 


NAVIGATIONAL SCIENCE DIVe» CODE 5300 
NAVAL OCEANOGRAPHIC OFFICE 
SUITLAND» MDe 20390 


GEODETIC DATUM REDUCTION LANGUAGE -— FORTRAN 
COMPUTER — IBM 7074 


REDUCES GEODETIC POSITIONS FROM ONE GEODETIC DATUM TO ANOTHER BY USE 
OF THE VENING MEINESZ EQUATIONSe THE PREFERRED DATUMS INVOLVED ARE 
EUROPEAN DATUMs NORTH AMERICAN DATUM AND TOKYO DATUMe OS NOe 55301. 
AUTHOR-— DeJe FINDLAYe 


NAVIGATIONAL SCIENCE DIVe» CODE 5300 
NAVAL OCEANOGRAPHIC OFFICE 
SUITLAND» MDe 20390 


COMPUTE GEOGRAPHIC POSITIONS LANGUAGE — SPS 
COMPUTER -— IBM 1620 
(COPY ON FILE AT NODC) 

USCGS PROGRAM NOce 15¢ COMPUTES GEOGRAPHIC POSITIONSs GIVEN STARTING 
POSITIONs AZIMUTHs AND LENGTH ON ANY ONE OF SIX SPHEROIDSe THREE TYPES 
OF COMPUTATIONS CAN BE OBTAINED-- SINGLE POSITIONS» A LOOP, OR A TRA- 
VERSEe CONTROL IS BY JOB CARDe LENGTH INPUT MAY BE IN METERS, FEET, 
STATUTE OR NAUTICAL MILES» OR ELECTRONIC LANES. 


ESSA» COAST AND GEODETIC SURVEY 


WASHINGTON SCIENCE CENTER» BLDGe 2 
ROCKVILLE» MDe 20852 


PAGE 061 


LORAN C (VERSION 2) LANGUAGE — SPS 
COMPUTER — IBM 1620 
(COPY ON FILE AT NODC) 

COMPUTES TABLES GIVING THE POINTS OF INTERSECTION OF LORAN C HyPER- 
BOLAS WITH MERIDIANS AND/OR PARALLELS OF THE EARTH SPHEROIDe MICRO- 
SECOND VALUES ARE COMPUTED AT INTERVALS VARYING FROM 1 1/4 MINe TO 20 
MINe FOR ANY OR ALL OF FOUR POSSIBLE PAIRS OF STATIONS.» PROGRAM CAN 
ALSO BE USED TO COMPUTE MICROSECOND VALUES AT GRID INTERSECTIONSe STO- 
RAGE 100K. PROGRAM CAN BE MODIFIED FOR USE ON IBM1620 OF 60K CAPACITY. 


ESSA:s COAST AND GEODETIC SURVEY 
WASHINGTON SCIENCE CENTER» BLDGe 2 
ROCKVILLE» MDe 20852 


GEODETIC POSITION COMPUTATION AND PLOT LANGUAGE — FORTRAN 
COMPUTER -— IBM 7074 W/ 
CALCOMP 564 
(COPY ON FILE AT NODC) 
COMPUTES GEODETIC POSITIONS AT DESIRED INTERVALS ALONG INCREMENTAL OR 
MISCELLANEOUS AZIMUTHSe OPTION TO PLOT OR LISTe PLOT USES THE 'LAMBt 
SUBROUTINE WITH TWO STANDARD PARALLELSe OS NOs 55321e AUTHOR-- MERLE 
Le NELSONe AN INFORMAL REPORT IR NOe 69-35 LISTS ADDITIONAL COMPUTER 
PROGRAMS AND DESCRIBES PROCEDURES FOR PRODUCTION OF SECONDARY PHASE 
CORRECTION CHARTS AND TABLESe THESE SUPPLEMENTARY PROGRAMS» WRITTEN 
bY MR EDWIN STEPHENSON AND MISS BARBARA GRAY», ARE IN 7074 AUTOCODER OR 
FORTRANe INFORMATION MAY BE OBTAINED FROM DISSEMINATION CONTROI DEPT. 
CODE 445 OR THE AUTHOR. 


NAVAL OCEANOGRAPHIC OFFICE 
WASHINGTONs DeCe 20390 


LORAN A AND C SKYWAVE LANGUAGE — FORTRAN 
COMPUTER — IBM 7074 


COMPUTES POINTS FOR LORAN SKYWAVES WHICH ARE PRODUCED WHEN TRANSMITTED 
RADIO SIGNALS THAT TRAVEL UPWARD AND OUTWARD ENCOUNTER THE IONOSPHERE. 
(TWO DIFFERENT PROGRAM DECKS USED FOR LORAN A AND C SKYWAVES) AUTHOR-- 
ROBERT VAN WIEe OS NOe 20158. 


COMPUTER DEPARTMENT: CODE 083 
NAVAL OCEANOGRAPHIC OFFICE 
SUITLAND»s MD. 20390 


LORAN COORDINATE COMPUTATION LANGUAGE — FORTRAN 
COMPUTER — IBM 7074 
(COPY ON FILE AT NODC) 
COMPUTES CHARTING COORDINATES ALONG LINES OF LATITUDE OR LONGITUDE FOR 
LORAN CURVES AT SPECIFIED INTERVALSe INCLUDES SUBROUTINE BSLN, TO 
COMPUTE COORDINATES ALONG THE BASELINE AND BASELINE EXTENSIONS» RUN— 
NING TIME-- 500-800 POINTS/MINUTE ON THE 7074e REFe IMR NOo N-1-64 
(UNPUBLISHED MANUSCRIPT)* OS NOs 20100¢ AUTHOR-- CHARLES KIRKILANDe 


COMPUTER DEPARTMENT s CODE 0831 
NAVAL OCEANOGRAPHIC OFFICE 
SUITLAND» MD. 20390 


LORAN TO GEOGRAPHIC, GEOGe TO LORAN CONVERSIONS LANGUAGE — FORTRAN 


COMPUTER - IBM 7074 
(COPY ON FILE AT NODC) 


CONVERTS LORAN TIME OR PHASE DIFFERENCES TO GEOGRAPHIC COORVINATES By 
NON-ITERATIVE METHOD (GEODESIC INVERSE DEVELOPED BY EeMe SODANO)e THE 
CONVERSIONS ARE FOR LORAN A OR LORAN C OR FOR A MIXTURE OF THE TWOe6 
REFe IMR NO« N-3-64 (UNPUBLISHED MANUSCRIPT). AUTHOR-— AeCe CAMPBELL. , 


PAGE 062 


GEODESY DIVISION» CODE 8430 
NAVAL OCEANOGRAPHIC OFFICE 


SUITLAND» MDe 20390 


SUBROUTINE SDANO : LANGUAGE — FORTRAN IV 
COMPUTER — IBM 1800 SYS 
(COPY ON FILE AT NODC) 
GIVEN THE GEOGRAPHICAL CO-ORDINATES OF TWO POINTS» SDANO CALCULATES 
THE GEODETIC DISTANCE AND AZIMUTHS BETWEEN THEMe BASED ON METHOD OF 
EeSe SODANO FOR A NON-ITERATIVE SOLUTION OF THE INVERSE AND DIRECT 
GEODETIC PROBLEMSe NeleOQe PROGe NOo —466 AUTHOR-- Me FASHAMe 


NATIONAL INSTITUTE OF OCEANOGRAPHY 
WORMLEY» GODALMINGs SURREY 
ENGLAND 


HNV1 (LORAN/DECCA FILE INITIALISATION) LANGUAGE = FORTRAN Iv 
COMPUTER - IBM 1800 SYS 
(COPY ON FILE AT NODC) 
GIVEN INPUT DATA ON A MASTER-SLAVE PAIRs HNV1 CALCULATES CERTAIN GEO- 
DETIC VALUES AND STORES THEN ON TAPE FILE FOR LATER USE BY PROGRAM 
HNAVe NeIeOo PROGRAM NOe 164¢ AUTHOR-—- Me FASHAMe 


NATIONAL INSTITUTE OF OCEANOGRAPHY 
WORMLEY» GODALMINGs SURREY 
ENGLAND 


HNAV (LORAN/DECCA COORDINATES CALCULATION) LANGUAGE - FORTRAN IV 
COMPUTER - IBM 1800 SYS 
(COPY ON FILE AT NODC) 

GIVEN A DECCAs LORAN-A OR LORAN-C FIX» CALCULATES THE LATITUDE AND 

LONGITUDE» THE METHOD FOR A HYPERBOLIC SYSTEM WITH SEPARATE MASTER IS 

USED FOR ALL CASESe THE CONSTANTS FOR THE HYPERBOLOIDS ARE CALCULATED 

IN METRES FOR BOTH LORAN AND DECCA THUS ALLOWING A FIX TO BE CALCULA- 

TED IF ONE LORAN READING AND ONE DECCA READING ARE KNOWNe NeleOe PRO- 

GRAM NOe 165¢6¢ USES 'SDANO' AND OTHER SUBROUTINESe AUTHOR-- Me FASHAM 


NATIONAL INSTITUTE OF OCEANOGRAPHY 
WORMLEY»s GODALMINGs SURREY 
ENGLAND 


SUBROUTINE 'MAP! LANGUAGE — FORTRAN IV 
COMPUTER - IBM 360/40, 
CALCOMP 763 


PROVIDES A WIDE VARIETY OF MAP PROJECTIONS AND GRIDS TO FACILITATE THE 
DISPLAY OF GEOGRAPHICAL DATAe THE PROGRAM HAS BEEN WRITTEN IN AS MOD- 
ULAR A FORM AS POSSIBLE TO ALLOW FOR EASE OF INSERTION OR DELETION OF 
ROUTINESe PRESENTLY UNDER DEVELOPMENT BY JOHN Oc WARDs THIRTEEN MAP 
PROJECTIONS ARE NOW AVAILABLEs AND IN THE NEAR FUTURE SIX MORE WILL 

BE ADDED. 


COMPUTER SYSTEMS DIVISION 
NATIONAL OCEANOGRAPHIC DATA CENTER 
WASHINGTONs De Ce 20390 


INDIVIDUAL POINT GENERATOR FOR MAP PROJECTIONS LANGUAGE — FORTRAN II 
COMPUTER -— IBM 7074 
(COPY ON FILE AT NODC) . é 
CONVERTS GEOGRAPHIC POSITIONS TO DISCRETE POINTS IN RECTANGULAR COOR- 
DINATES ON THE FOLLOWING PROJECTIONS-- MERCATOR» TRANSVERSE MERCATOR, 
GNOMONICs POLAR STEREOGRAPHICs AZIMUTHAL EQUIDISTANT» LAMBERT CONFORM— 
AL (WITH TWO OR ONE STANDARD PARALLELS) s LAMBERT AZIMUTHAL EQUAL AREA 
POLARs LAMBERT EQUAL AREA CYLINDRICAL» MILLER» ALBERS EQUAL AREA CON-— 
IC» RECTIFIED SKEW ORTHOMORPHICs AND OBLIQUE MERCATORe CARTOGRAPHIC 


PAGE 063 


DATA MAY BE PRODUCED IN EITHER GRAPHIC OR TABULAR FORMe OS NOew 55646 
(MAIN PROGRAM. EACH OF THE 13 PROJECTION SUBROUTINES HAS ITS OWN OPEN 
SHOP NUMBER)e AUTHORS-- RONALD BOLTONs LOUIS ROWENs GREGORY VEGA. 
REFe INFORMAL REPORT IR NOe 69-23» MAR 1969 !'COMPUTER PROGRAMS AND 
SUBROUTINES FOR AUTOMATED CARTOGRAPHY'» BY Je PARRINELLOs NAUTICAL 
CHART DIVISIONe FURTHER INFORMATION MAY BE OBTAINED THROUGH DISSEMIN- 
ATION DEPARTMENT CODE 445 OR THE AUTHORS. 


NAVAL OCEANOGRAPHIC OFFICE 
WASHINGTONs DeCe 20390 


INDIVIDUAL POINT GENERATOR FOR LANGUAGE — FORTRAN II 
DISTANCE AND AZIMUTH COMPUTATIONS COMPUTER — IBM 7074 


USES THE GEODETIC LATITUDE AND LONGITUDE OF TWO POINTS TO COMPUTE THE 
DISTANCE AND AZIMUTH FROM ONE POINT TO THE OTHERe RESULTS WILL BE IN 
TABULAR FORM WITH THE DISTANCE IN METERS AND THE AZIMUTH AND BACK AZI- 
MUTH IN DEGREES» MINUTES AND SECONDSe OcSe NOs 656163 BY ReMe BOLTON. 


NAUTICAL CHART DIVISION: CODE 5620 
UeSe NAVAL OCEANOGRAPHIC OFFICE 
WASHINGTON De Ce 20390 


PARAMETRIC MAP LANGUAGE — FORTRAN II 
COMPUTER — IBM 7074 


GENERATES ANY HYPERBOLIC NAVIGATION SYSTEM BY USING PARAMETRIC EQuUA- 
TIONSe GENERATES PLOTTING COORDINATES FOR LORAN As LORAN Cs OMEGA AND 
DECCA CHARTSe WILL PROCESS ALL LATTICE LINES THAT FALL WITHIN A SPEC- 
IFIED GEOGRAPHIC AREA» CAN BE DISPLAYED ON ANY OF THE FOLLOWING MAP 
PROJECTIONS-— MERCATORs TRANSVERSE MERCATOR: LAMBERT CONFORMAL CONIC, 
OBLIQUE MERCATOR» POLYCONICe OvcSe NOe 53012¢ AUTHORS-- ReAw BOLTON, 
ReMe BOLTON’ 


NAUTICAL CHART DIVISION» CODE 5620 
UeSe NAVAL OCEANOGRAPHIC OFFICE 
WASHINGTON De Ce 20390 


DECCA HI-FIX LANGUAGE — FORTRAN 
COMPUTER — PDP—-5s 8S 


GENERAL PURPOSE PROGRAM FOR CONVERSION OF HYPERBOLIC COORDINATES TO 
X-Y COORDINATE SYSTEMSe TYPE GEOGRAPHIC COORDINATES OF MASTER AND 
SLAVE STATIONS — PAPER TAPE OR KEYBOARD INPUT FOR LANE COUNTSs OUTPUT 
ON ASR-33 TELEPRINTERe WRITTEN FOR THE UeSe COAST GUARD BY LTe ReMe 
O'HAGAN (RETe)e COPY OF PROGRAM WAS DEPOSITED WITH DECUS (DIGITAL E- 
QUIPMENT CORP. USERS SOCIETY). 


DIGITAL EQUIPMENT CORPORATION 
MAYNARDs MASSACHUSETTS 01754 


HYPERMAP LANGUAGE — FORTRAN 
COMPUTER -— (NOT GIVEN) 
(COPY ON FILE AT NODC) 

A SERIES OF PROGRAMS FOR DRAWING MAPS AND PLOTTING DATA ON THEMe THE 

PROGRAM OPERATES UNDER A SIMPLE COMMAND LANGUAGE WHICH ENABLES THE US- 

ER TO REFER TO HIS DATA AND THE MAP DATA BY NAMEe THERE ARE ELEVEN 

PROJECTION OPTIONS AVAILABLE IN THE BASIC TRANSFORMATION SUBROUTINE > 

A MORE ADVANCED PACKAGE (WITH SEVERAL PROJECTIONS TAKING THE ELLIPTIC- 

ITY OF THE EARTH INTO ACCOUNT) IS UNDER DEVELOPMENTe AUTHOR-- DR ROB- 

ERT L PARKER» UNIVe OF CALIFORNIA AT SAN DIEGO. 


PROFe JOHN De. MUDIE 


SCRIPPS INSTITUTION OF OCEANOGRAPHY 
LA JOLLA» CALIFe 92037 


PAGE 064 


GENERAL MAP PROJECTION LANGUAGE — MAD 
COMPUTER -— IBM 7090 W/ 
CALCOMP 763 
(COPY ON FILE AT NODC) 

CONVERSION (OR GENERATION) OF LATITUDE AND LONGITUDE VALUES TU MAP 

PROJECTION COORDINATESe INCLUDES ALL COMMONLY EMPLOYED PROJECTIONS 

OF SPHEREe OBLIQUE CASES MAY BE AUTOMATICALLY OBTAINEDe AUTHOR-- We 

Re TOBLERe 


THE UNIVERSITY OF MICHIGAN 
DEPARTMENT OF GEOGRAPHY 
ATTNe DRe We Re TOBLER 

ANN ARBOR» MICHIGAN 48104 


FINITE MAP PROJECTION DISTORTIONS LANGUAGE — MAD 
COMPUTER —- IBM 7090 
(COPY ON FILE AT NODC) 

PROGRAMS AND SUBROUTINES TO ESTIMATE THE ERRORS INTRODUCED BY THE SUB- 
STITUTION OF MAP PROJECTION COORDINATES FOR SPHERICAL COORDINATESe 
STATISTICAL COMPUTATIONS OF FINITE DISTORTION ARE RELATED TO TISSOT'S 
INDICATRIX AS A GENERAL CONTRIBUTION TO THE ANALYSIS OF MAP PROJEC— 
TIONSe REFe TECHNICAL REPORT NOs 3 'GEOGRAPHICAL COORDINATE COMPUTA-— 
TIONS PART II's BY We Re TOBLERs DEPTe OF GEOGRAPHY. 


THE UNIVERSITY OF MICHIGAN 
ANN ARBOR» MICHIGAN 


PAGE 065 


PHYSICAL OCEANOGRAPHY 
HK —H KKK KAKA HHH 


%#-*-* AIR-SEA INTERACTION AND HEAT BUDGET *-*-* 


FUNCTION VAPW LANGUAGE — FORTRAN Iv 
COMPUTER — IBM 1801/02 
(cOPY ON FILE AT NODC) 
SUBPROGRAM CALCULATES SATURATION VAPOUR PRESSURE OVER WATERe INPUT IS 
TEMPERATURE IN DEGRe Ke USES AN EQUATION FROM SMITHSONIAN TABLES PAGE 
350. THE FUNCTION CONVERTS THE LOG OUTPUT OF THIS EQUATION TO ACTUAL 
PRESSURE IN MILLIBARSe NeIeOe PROGe NOewe -—24e AUTHOR-- Re HOWARTHe 


NATIONAL INSTITUTE OF OCEANOGRAPHY 
WORMLEYs GODALMINGs SURREY 
ENGLAND 


ATR-SEA LANGUAGE — FORTRAN 
COMPUTER — IBM 7074 


DETERMINES THE RELATION BETWEEN THE 500 MBe WIND FIELD AND OCEAN SUR- 
FACE CONDITIONS (WAVES), THROUGH THE USE OF STATISTICAL METHODSe OcSe 
PROGRAM NOe 534645 BY WeHe GEMMILLe 


OCEANOGRAPHIC PREDICTION DIVe, CODE 3400 
NAVAL OCEANOGRAPHIC OFFICE 
SUITLAND» MD. 20390 


CLOUD COVER AND DAILY SEA TEMPERATURE LANGUAGE — FORTRAN 
COMPUTER — IBM 7074 


DIVIDES CLOUD COVER INTO THREE GROUPS AND COMPUTES MEAN TEMPERATURE 
BY HOUR OF DAY AND BY DAY FOR EACH DEPTHe OS NOe 53414e AUTHOR-- De 
Be NIXe 


OCEANOGRAPHIC PREDICTION DIVes CODE 3400 
NAVAL OCEANOGRAPHIC OFFICE 
SUITLAND» MDe 20390 


LAYER DEPTH PLOT LANGUAGE — FORTRAN 
COMPUTER -— IBM 7074 


COMPUTES AND PLOTS LAYER DEPTH» ON A SYNOPTIC BASIS» FROM VARIOUS 
DEFINITIONSe OS NOe 534536¢ AUTHOR-— DeBe NIX 


OCEANOGRAPHIC PREDICTION DIVes CODE 3400 
NAVAL OCEANOGRAPHIC OFFICE 
SUITLAND» MD. 20390 


PREDICTION OF VERTICAL TEMPERATURE CHANGE LANGUAGE — FORTRAN 
COMPUTER -— IBM 7074 
(COPY ON FILE AT NODC) 

A TECHNIQUE BASED PRIMARILY ON HEAT BUDGET AND WIND MIXING CALCULA- 
TIONS HAS BEEN DEVELOPED FOR PREDICTING THE VERTICAL THERMAL STRUCTURE 
OF THE OCEANe THE TECHNIQUE ESSENTIALLY MODIFIES THE INITIAL THERMAL 
STRUCTURE THROUGH INCIDENT SOLAR RADIATION» BACK RADIATIONs SENSIBLE 
AND EVAPORATIVE HEAT EXCHANGE» CONVECTIVE HEAT TRANSFER IN THE WATER 
MASS» AND WIND MIXINGe PREDICTIONS ARE MADE AT 6-HOUR INTERVALS UNTIL 
1200Z ON THE DATE OF FORECASTe THE PREDICTED BT IS PRINTED OUT, ALSO 
CAN BE PLOTTED WITH A BENSON-LEHNER MODEL J PLOTTERe AUTHORS-- WeHe 
GEMMILL AND DeBe NIXe REFe IMR NOs 0-42-65 (UNPUBLISHED MANUSCRIPT). 


PAGE 066 


SEE ALSO IMR NOe 0-45-65 BY Be THOMPSON, AND IMR NOe 0-13-66 BY BAR- 
NETT AND AMSTUTZe PROGRAM LISTINGS SEPARATE FROM MANUSCRIPTSe 


OCEANOGRAPHIC PREDICTION DIVe,s CODE 3400 
NAVAL OCEANOGRAPHIC OFFICE 
SUITLAND» MD. 20390 


TWO-DIMENSIONAL POWER SPECTRUM FOR SWOP II LANGUAGE - FORTRAN 
COMPUTER - IBM 7074 


DETERMINATION OF SPECTRUM ASSOCIATED WITH THE SPATIAL DISTRIBUTION OF 
ENERGY AS OBTAINED FROM AN INSTANTANEOUS PICTURE OF THE OCEAN TAKEN 
FROM AIRCRAFT (SWOP II1)e OS NOe 534846 AUTHOR-- CeMe WINGERe 


OCEANOGRAPHIC PREDICTION DIVe»s CODE 3400 
NAVAL OCEANOGRAPHIC OFFICE 
SUITLAND» MDe 20390 


WIND STRESS LANGUAGE — FORTRAN 
COMPUTER - IBM 7074 


DETERMINES WIND STRESS ON THE OCEAN SURFACEe OS NOc 534622¢ AUTHOR-- 
WeHe GEMMILLe 


OCEANOGRAPHIC PREDICTION DIVe»s CODE 3400 
NAVAL OCEANOGRAPHIC OFFICE 
SUITLAND» MD. 20390 


TRANSPORT COMPUTATIONS FROM ATMOSPHERIC PRESSURE LANGUAGE - FORTRAN II 
AND Iv 
COMPUTER -— IBM 16205 
IBM 7040 AND 
IBM 1130 
(COPY ON FILE AT NODC — FORTRAN II FOR 1620 ONLY) 
COMPUTES» ACCORDING TO A SYSTEM OF ANALYSIS DESIGNED BY DRe NePe FOF-— 
ONOFFs THE STEADY STATE MASS TRANSPORT IN THE OCEAN FROM ATMOSPHERIC 
PRESSURE DATAs MERIDIONAL AND ZONAL COMPONENTS OF EKMAN TRANSPORT 9 
TOTAL MERIDIONAL TRANSPORT» INTEGRATED TRANSPORT AND INTEGRATED GEO- 
STROPHIC TRANSPORTe INPUT ARE SEA LEVEL PRESSURE CARDS FROM THE EX- 
TENDED FORECAST DIVe OF THE UeSe WEATHER BUREAUe OUTPUT ARE MEAN 
MONTHLY VALUES FOR THE SPECIFIED GRID OF ALTERNATE 5 DEGREES OF LATI- 
TUDE AND LONGITUDE IN THE NORTHERN HEMISPHEREe FORTRAN II PROGRAM IS 
PUBLISHED IN FISHERIES RESEARCH BOARD OF CANADA, MSe SERIES (OCEANe 
AND LIMNOL.) NOw 163% 1963 BY DRe CHARLOTTE FROESEe FORTRAN IV PRO- 
GRAM HELD BY STATISTICAL SERVICES» FISHERIES RESEARCH BOARD OF CANADA, 
BIOLOGICAL STATIONs NANAIMO, Be Cos CANADA 


OCEANOGRAPHER-IN-CHARGE 
PACIFIC OCEANOGRAPHIC GROUP 
BIOLOGICAL STATION 

NANAIMO», Be Ces CANADA 


SYNOPTIC ANALYSIS AND FORECASTING OF LANGUAGE — MACHINE 
SURFACE CURRENTS COMPUTER - CDC 1604 AND 
CDC 3200 


INPUT IS SURFACE WIND ANALYSIS/FORECAST»s SEA SURFACE TEMPERATURE ANAL— 
YSIS/FORECASTs 600 FEET TEMPERATURE ANALYSIS AND SOME CLIMATOLOGY e 
OUTPUT IS SURFACE CURRENT TRANSPORT IN NAUTICAL MILES PER 24 HOURS» 
CURRENT DIRECTION AND STREAM FUNCTIONe REFe FNWF TECHNICAL NOTE NOe 9 
AND HUBERT (1965)e DIRECT REQUESTS FOR INFORMATION TO-- 


COMMANDING OFFICER 


FLEET NUMERICAL WEATHER CENTRAL 
MONTEREY» CALIFORNIA 93940 


PAGE 067 


WIND CURRENTS LANGUAGE — MAD 
COMPUTER — IBM 7090 


COMPUTES CURRENTS FROM STANDARD WIND OBSERVATIONS. 


VINCENT NOBLE 

THE UNIVERSITY OF MICHIGAN 

GREAT LAKES RESEARCH DIVISION 
INSTITUTE OF SCIENCE AND TECHNOLOGY 
1077 NORTH UNIVERSITY BUILDING 

ANN ARBOR» MICHIGAN 48104 


RADIATION TEMPERATURE OF SEA SURFACE LANGUAGE -— FORTRAN 
COMPUTER — (NOT GIVEN) 


(COPY ON FILE AT NODC) 
EVALUATES THREE EMPIRICAL EQUATIONS», DEVELOPED BY REGRESSION METHODS, 
TO OBTAIN AN ESTIMATE OF THE DIFFERENCE BETWEEN SKIN AND BUCKET TEM-— 
PERATURES FROM STANDARD WEATHER OBSERVATIONS MADE AT SEAe THESIS BY 
ROBERT De BOUDREAUs REFe NO. 65-15T (1965s 79 P)e 


DEPTe OF OCEANOGRAPHY 
COLLEGE OF GEOSCIENCES 

TEXAS A AND M UNIVERSITY 
COLLEGE STATIONs TEXAS 77843 


SYNOPTIC ANALYSIS AND FORECASTING OF LANGUAGE — MACHINE 
POTENTIAL MIXED LAYER DEPTH COMPUTER -— CDC 1604 AND 
cDC 3200 


INPUT TO PROGRAM-- CLIMATOLOGY, SYNOPTIC WAVE HEIGHT ANALYSIS/FORE- 
CAST» SEA SURFACE TEMPERATURE ANALYSIS» 600 FEET TEMPERATURE ANALYSIS/ 
FORECAST» AND BT OBSERVATIONSe OUTPUT IS MIXED LAYER DEPTH IN FEET AT 
GRID POINTS (63X63 FIELD)» TENDENCY OF THERMOCLINE NEXT 24 HOURSs MAG-— 
NITUDE» AND SHORT TERM FLUCTUATIONS OF THE THERMOCLINEe REF-- SEE FNWF 
TECHNICAL NOTE NOe 10 AND/OR NOe 212¢ DIRECT INQUIRIES TO-- 


COMMANDING OFFICER 
FLEET NUMERICAL WEATHER CENTRAL 
MONTEREY» CALIFORNIA 93940 


*-*-% CURRENTS AND TRANSFER PROCESSES *-—*-* 


SURFACE CURRENT SUMMARY LANGUAGE - AUTOCODER 
COMPUTER —- IBM 7074 


(COPY ON FILE AT NODC) 
THE RESULTANT CURRENT SPEED AND RESULTANT CURRENT DIRECTIONS ARE COM— 
PUTED BY MARSDEN SQUARE, 1-DEGe OR 5-DEGe SQUARE AND MONTH FROM H 1-9, 
NETHERLANDS 193 OR JAPANESE 118 DATAe OS NOe 52252. AUTHOR-—- MAXINE 
JACKSONe 


COMPUTER SYSTEMS DIVISION 
NATIONAL OCEANOGRAPHIC DATA CENTER 
WASHINGTONs De Co 20390 


MODIFIED SURFACE CURRENTS LANGUAGE — AUTOCODER 
COMPUTER - IBM 7074 


(COPY ON FILE AT NODC) 
MODIFIES MeHe JACKSON'S PROGRAM TO PROVIDE THE SAME INFORMATION ON A 
FILE REPRESENTING THE H 1-95 118 (JAPANESE)s 193 (NETHERLANDS) FILES 
COMBINED» AUTHOR-- CeSe CALDWELL>. OS NOew 201566 


COMPUTER DEPARTMENT» CODE 083 


PAGE 068 


NAVAL OCEANOGRAPHIC OFFICE 
SUITLAND» MDe 20390 


STATISTICAL SURFACE CURRENT ROSE LANGUAGE -— AUTOCODER 
COMPUTER — IBM 7074 


CALCULATES FREQUENCIES OF A NORMAL DISTRIBUTIONs POPULATING THE 
DIRECTION-SPEED GROUPS OF A STANDARD ROSE FORMAT» WHICH BEST FITS 
THE ACTUAL DATA SURFACE (REFe SP-64 -A STATISTICAL ROSE PROGRAM—»5 
BY We YERGEN)» OS NO 53301le AUTHOR-—- We YERGENe 


OCEANOGRAPHIC ANALYSIS DIVe» CODE 3300 
NAVAL OCEANOGRAPHIC OFFICE 
SUITLAND» MD. 20390 


COMPUTE ADVECTION LANGUAGE — FORTRAN 
COMPUTER — IBM 1401 


COMPUTES HORIZONTAL ADVECTION FROM AN INITIAL POINT IN THE WATER COL— 
UMN FROM EQUATIONS DESCRIBED BY Ae FISHER» IM NOe 66-9 (INFORMAI MANU- 
SCRIPT)e FROM KNOWN INPUTS OF DENSITYs CURRENT VELOCITIES» AND TEMP— 
ERATURE GRADIENTS» ADVECTION IS COMPUTED FROM AN INITIAL POINT OVER A 
GIVEN DISTANCEs ASSUMING NO VERTICAL HEAT LOSS» HORIZONTAL COMPONENTS 
IN THE XsY PLANE ARE COMPUTED AND A RESULTANT VECTOR IS DETERMINEDe 

OS NOe 5349026 AUTHOR-- ReKe FRANKLINe 


OCEANOGRAPHIC PREDICTION DIVe» CODE 3400 
NAVAL OCEANOGRAPHIC OFFICE 
SUITLANDs MDe 20390 


GVPAsVPA LANGUAGE - FORTRAN IV 
COMPUTER -— IBM 360/65 


CALCULATES VELOCITIES AND TRANSPORTS FOR AS MANY AS 50 SUCCESSIVE STA- 
TION PAIRSe USES AS INPUT INTERPOLATED DATA ON CARDS FROM PROGRAM 
"DYNAM! » WHICH CALCULATES DYNAMIC HEIGHTS AT STANDARD DEPTHSe 


BUREAU OF COMMERCIAL FISHERIES 
Pe Oo BOX 3830 
HONOLULUs HAWAII 96812 


STANDARD-VECTOR DEVIATION ROSE FOR CURRENT DATA LANGUAGE — FORTRAN 
COMPUTER — IBM 7074 
(COPY ON FILE AT NODC) 
CALCULATES THE FOLLOWING PARAMETERS FOR A TWO DIMENSIONAL NORMAL EL- 
LIPTICAL DISTRIBUTED CURRENT FIELD-- MEAN SPEED,» COMPONENTS OF THE 
VECTOR MEAN» COMPONENTS OF THE STANDARD-VECTOR DEVIATION ALONG THE 
PRINCIPAL AXES» AND THE INCLINATION OF THE MAJOR AXISe PROGRAM HAS 
BEEN IN USE PRINCIPALLY AS AN AID IN AIR-SEA RESCUE OPERATIONSe INPUT 
IS CURRENT DATA WHICH HAS BEEN TABULATED IN SPECIFIED SPEED-INTERVAL 
CLASSES FOR EIGHT COMPASS POINTS.» REFe IMR O-22-65 (UNPUBLISHED MANU- 
SCRIPT)e AUTHOR-- DONALD Ae BURNS» CODE 72006 


OCEANOGRAPHIC ANALYSIS DIVe»s CODE 3300 
NAVAL OCEANOGRAPHIC OFFICE 
SUITLANDs MDe 20390 


GULF STREAM PATH LANGUAGE — FORTRAN 
COMPUTER - IBM 7074 


PREDICTS THE PATH OF THE GULF STREAM BY MEANS OF 1) A SINE GENERATED 
FUNCTION» 2) THE CONSERVATION OF POTENTIAL VORTICITYs» AND 3) HARMONIC 
ANALYSISe AUTHOR-- WeHe GEMMILLo 


OCEANOGRAPHIC PREDICTION DIVe» CODE 3430 
NAVAL OCEANOGRAPHIC OFFICE 


PAGE 069 


SUITLAND» MARYLAND 20390 


VELOCITY AND HORIZONTAL EDDY COEFFICIENTS LANGUAGE — FORTRAN 
COMPUTER —- IBM 709 


COMPUTATION OF VELOCITY AND HORIZONTAL MIXING EDDY COEFFICIENTS ALONG 
ISENTROPIC SURFACESe AUTHOR-- AeDe KIRWANe 


TEXAS A AND M UNIVERSITY 
COLLEGE OF GEOSCIENCES 
DEPARTMENT OF OCEANOGRAPHY 
COLLEGE STATIONs TEXAS 77843 


SALINITY DISTRIBUTION IN ONE-DIMENSIONAL ESTUARY LANGUAGE — FORTRAN 
COMPUTER -— (NOT GIVEN) 
(COPY ON FILE AT NODC) 
A MODEL IS CONSTRUCTED FOR AN ESTUARY TO PREDICT THE SALINITY DISTRIB- 
UTION FOR A GIVEN FRESH WATER INFLOWs WITH APPLICATION TO THE UPPER 
CHESAPEAKE BAY AND THE SUSQUEHANNA RIVERe BASED ON A SALT CONTINUITY 
EQUATION IN WHICH THE SEAWARD SALT ADVECTION IS BALANCED BY TURBUILENT 
DIFFUSION TOWARD THE HEAD OF THE BAYe IN FINAL FORM» IT IS A LINEAR» 
SECOND-ORDER» AND PARABOLIC PARTIAL DIFFERENTIAL EQUATION WITH VARIA- 
BLE COEFFICIENTS WHICH ARE FUNCTIONS OF BOTH SPACE AND TIMEe REFe 69- 
7s TECHe REPORT 54 (MAY 19695 7O0Pe) BY WILLIAM BOICOURTe 


CHESAPEAKE BAY INSTITUTE 
THE JOHNS HOPKINS UNIVERSITY 
BALTIMORE» MDe 21218 


PROCESSING OF OCEANOGRAPHIC OBSERVATIONS LANGUAGE — FORTRAN II 
COMPUTER — IBM 1620 II 
(COPY ON FILE AT NODC) 

A NUMBER OF PROGRAMS AND SUBROUTINES FOR PROCESSING 'MICHELSENS CON- 

TAINER' DATA (AUTOMATIC CURRENT AND TEMPERATURE MEASUREMENTS)» FOR 

PROCESSING EKMAN CURRENT METER DATAs AND FOR HARMONIC ANALYSIS AND 

POWER SPECTRUM ANALYSISe REFe TECHNICAL REPORT NOe 379 NATO SUBCOM-— 

MITEE ON OCEANOGRAPHIC RESEARCH (105 Pes FEB 1967)e« AUTHOR-— DRe HeEeo 

SWEERS (OF THE CANADIAN OCEANOGRAPHIC DATA CENTRE) e 


GEOPHYSICAL INSTITUTE 
UNIVERSITY OF BERGEN 
BERGEN» NORWAY 


DRIFT BOTTLE DATA COMPUTATION LANGUAGE — AUTOCODER 
COMPUTER ~— IBM 7074 
(COPY ON FILE AT NODC) 

COMPUTES THE FOLLOWING FROM BOTTLE RECOVERY INFORMATION-- BEARING» 
NAUTICAL MILES DRIFTEDs NUMBER OF DAYS ADRIFTs AND SPEED IN NAUTICAL 
MILES PER DAYe COMPUTES MARSDEN AND 1/4-DEGREE SQUARES OF RELEASE« 
OUTPUT ON MAGNETIC TAPEe AUTHOR-- JUDY YAVNERe USED WITH A TAPE TO 
PRINT/CARD EDITING AND SELECTION PROGRAMe AUTHOR-— JOHN JENSONe 


COMPUTER SYSTEMS DIVISIONs CODE 2400 
NATIONAL OCEANOGRAPHIC DATA CENTER 
WASHINGTON» DeCe 20390 


LATERAL RELATIVE DISTRIBUTION OF MATERIAL FROM LANGUAGE — FORTRAN II 
A CONTINUOUS SOURCE IN A CONSTANT CURRENT COMPUTER — IBM 7094 


PREDICTS THE RATIO OF THE CONCENTRATION OF A CONTAMINANT TO ITS CENTER 
LINE VALUE AS A FUNCTION OF LONGITUDINAL AND TRANSVERSE DISTANCE FROM 
THE SOURCE DUE TO HORIZONTAL ADVECTION AND DIFFUSION WHEN DISCHARGED 

S A VERTICAL LINE SOURCE OF UNIT DEPTH AND UNIT RATE OF DISCHARGE IN 
AN UNBOUNDED MEDIUMe INPUT ARE THE VELOCITY (A CONSTANT)» THE 1 LONGI- 
TUDINAL AND TRANSVERSE COORDINATES» AND THE DIFFUSION VELOCITY, IeEe,s 


PAGE 070 


THE SPREADING COEFFICIENTs A MEASURE OF THE HORIZONTAL DIFFUSIONe THE 
OKUBO-PRITCHARD MODEL FOR AN INSTANTANEOUS RELEASE 1S USED FOR THE MO- 
DELe AUTHORS-- HeEe WALTERS AND HeHe CARTERe 


HARVEY Ee WALTERS 

CHESAPEAKE BAY INSTITUTE 

THE JOHNS HOPKINS UNIVERSITY 
CHARLES AND 34TH STe 
BALTIMOREs MDe 21218 


CONTINUOUS LINE SOURCE (REFLECTED) LANGUAGE -— FORTRAN II 
COMPUTER -— IBM 7094 


PREDICTS THE HORIZONTAL STEADY STATE DISTRIBUTION OF A CONTAMINANT DUE 
TO HORIZONTAL ADVECTION AND DIFFUSION WHEN DISCHARGED AS A VERTICAL 
PLANE SOURCE OF UNIT DEPTH AND UNIT RATE OF DISCHARGE AND LOCATED PER- 
PENDICULAR TO A BOUNDARYe THE VELOCITY IS ASSUMED TO BE CONSTANTe THE 
OKUBO-PRITCHARD MODEL FOR AN INSTANTANEOUS RELEASE IS USEDe IT IS IN- 
TEGRATED LATERALLY TO TRANSFORM A VERTICAL LINE SOURCE SOLUTION TO A 
SOLUTION FOR A VERTICAL PLANE SOURCE AND IS TOTALLY RELECTED AT THE 
BOUNDARY TO QUANTITATE THE BOUNDARY EFFECTe AUTHORS-— HeEeo WALTERS 
AND HeHe CARTERe 


HARVEY Ee WALTERS 

CHESAPEAKE BAY INSTITUTE 

THE JOHNS HOPKINS UNIVERSITY 
CHARLES AND 34TH STeo 
BALTIMOREs MDe 21218 


CONTINUOUS SOURCE IN TIDAL ESTUARY PER LANGUAGE - FORTRAN II 
UNIT DEPTH AND UNIT RATE OF RELEASE COMPUTER - IBM 7094 


PREDICTS THE CENTERLINE LONGITUDINAL DISTRIBUTION OF A CONTAMINANT AS 
A FUNCTION OF PUMPING TIMEs DUE TO HORIZONTAL ADVECTION AND DIFFUSION 
WHEN DISCHARGED AS A VERTICAL LINE SOURCE OF UNIT DEPTH AT A CONSTANT 
RATE IN A TIDAL ESTUARYe INPUT ARE THE MAXIMUM TIDAL VELOCITY, THE 
NON-TIDAL VELOCITY» THE DIFFUSION VELOCITY IeE5se SPREADING COEFFICIENT, 
A MEASURE OF HORIZONTAL DIFFUSION» PUMPING TIME IeEe TIME SINCE SOURCE 
WAS INITIATED» AND THE LONGITUDINAL DISTANCE FROM THE SOURCE» STORAGE 
NECESSARY-- 15000 WORDS (CAN BE EASILY CHANGED TO 7000 WORDS)e AUTHORS 
— HeEe WALTERS AND HeHe CARTERe 


HARVEY Ee WALTERS 

CHESAPEAKE BAY INSTITUTE 

THE JOHNS HOPKINS UNIVERSITY 
CHARLES AND 34TH STe 
BALTIMOREs MDe 21218 


CONTINUOUS SOURCE IN TIDAL ESTUARY PER UNIT DEPTH LANGUAGE - FORTRAN II 
AND UNIT RATE OF RELEASE» WITH COOLING TERM COMPUTER - IBM 7094 


PREDICTS THE CENTERLINE LONGITUDINAL DISTRIBUTION OF HEAT AS A FUNC 
TION OF PUMPING TIME DUE TO HORIZONTAL ADVECTIONs DIFFUSION» AND AT- 
MOSPHERIC COOLING WHEN DISCHARGED AS A VERTICAL LINE SOURCE AT A CON- 
STANT RATE IN A TIDAL ESTUARYe THE OKUBO-PRITCHARD MODEL FOR AN IN- 
STANTANEOUS RELEASE IS USED FOR THE MODELe IT IS FURTHER ASSUMED THAT 
EACH INFINITESIMAL RELEASE COOLS EXPONENTIALLY WITH TIMEe THE RATE CO- 
EFFICIENT IS CALLED THE COOLING COEFFICIENTe CORE STORAGE NECESSARY-- 
15000 WORDS (CAN BE RUN USING 7000 WORDS)e AUTHORS-- HeEe WALTERS AND 
HeHe CARTERe 


HARVEY Ee WALTERS 

CHESAPEAKE BAY INSTITUTE 

THE JOHNS HOPKINS UNIVERSITY 
CHARLES AND 34TH STe 
BALTIMORE» MDe 21218 


PAGE O71 


CURRENT METER DYNAMICS LANGUAGE — MAC 
COMPUTER — IBM OS/360 


PROGRAM WITH SUBROUTINES AS ESTIMATOR FOR DERIVING POSITION AND EULER 
ATTITUDE (PITCH AND ROLL) ANGLES SO THAT PRECISE CURRENT METER DYNAM— 
ICS CAN BE OBTAINEDe APPLIED TO A REAL CASE PROBLEM FOR WHICH SIMUL- 
ATION RESULTS ARE DISCUSSED. THESIS BY MICHEL FROIDEVAUX (JAN 1968) 

tAPPLICATION OF STATISTICAL ESTIMATION TO THE DETERMINATION OF OCEAN 

CURRENT METER DYNAMICS', 


INSTRUMENTATION LABORATORY 
MASSACHUSETTS INSTITUTE OF TECHNOLOGY 
CAMBRIDGEs MASSACHUSETTS 02139 


CURRENT METER TURBULENCE LANGUAGE — FORTRAN 
COMPUTER — IBM 7074 


GIVES AN INDICATION OF TURBULENCE IN THE OCEAN BY COMPUTING MEASURES 
OF THE DEVIATIONS FROM MEANS OVER VARIOUS LENGTHS OF TIMEe OS NOe — 
57202~¢ AUTHOR-— ROBERT Re GLEASONe 


EXPLORATORY OCEANOGRAPHY DIVe»s CODE 7200 
NAVAL OCEANOGRAPHIC OFFICE 
SUITLAND» MD. 20390 


FLOW METER PLOTS LANGUAGE -— FORTRAN IV 
COMPUTER — IBM 360/65, 
CAL COMP 


(COPY ON FILE AT NODC) 
DETERMINES FLOW METER PERFORMANCE AND PLOTS NUMBER OF REVOLUTIONS VS. 
TIMEe OUTPUT GIVES THE COfFFICIENT OF CORRELATION AND STANDARD DEVIA- 
TIONs AND THE REGRESSION LINE AND 1¢96 STANDARD DEVIATIONS ARE MARKED 
OFF ON THE PLOTe CORE STORAGE USED-- 31K BYTES (WITH PLOT ROUTINES). 
AUTHOR-— MARILYNN BORKOWSKI. 


BUREAU OF COMMERCIAL FISHERIES 

TROPICAL ATLANTIC BIOLOGICAL LABORATORY 
75 WIRGINIA BEACH DRIVE 

MIAMI» FLORIDA 33149 


FILM DATA PROCESSING LANGUAGE — FORTRAN-—60 
COMPUTER — CDC 1604 


ACCEPTS RICHARDSON'S CURRENT DATA FROM A BINARY TAPE SUPPLIED By IN- 
FORMATION INTERNATIONALs INCe NORTH-SOUTH AND EAST-WEST VELOCITY COM- 
PONENTS ARE COMPUTED FROM THE COMPASSs VANE» RO AND R10 COUNTERS» AND 
ALL INFORMATION MAY BE PRINTED EVERY TIME SLICEe A HISTOGRAM OF THESE 
COMPONENTS IS PRINTED AT THE END OF EACH FILMe FURTHERMORE» AN ENVEL-— 
OPE OF THE CURRENT ANGLES AND CURRENT SPEEDS IS SHOWN AT 2-HOUR INTER- 
VALSe FINALLY» 6-HOUR MEANS AND STANDARD DEVIATIONS OF VELOCITY COM- 
PONENTS ARE PUNCHED ON CARDS FOR FURTHER PROCESSINGe 1200-CHARACTER 
RECORDS ARE READ INTO STORAGE BY MEANS OF A MACHINE LANGUAGE SUBROUT-— 
INEe THE REMAINING PROGRAM IS IN FORTRANe AUTHOR-— EMANUEL MEHR, 
COLLEGE OF ENGINEERING» NYU. 


NEW YORK UNIVERSITY 

SCHOOL OF ENGINEERING AND SCIENCE 
GEOPHYSICAL SCIENCES LABORATORY 

2455 SEDGWICK AVEes BRONX» NeYe 10468 


DATUBA LANGUAGE — FORTRAN-63 
COMPUTER - CDC 3800 


ANALYZES THE DEFLECTIONS OF A TRI-MOORED»s SUBSURFACE» BUOY-CABLE ARRAY. 
ACTED ON BY CURRENT—-INDUCED FORCESe SOLUTION IS BY THE METHODS OF 


PAGE 072 


IMAGINARY REACTIONS AND SUCCESSIVE APPROXIMATIONS»e CALCULATES THE 
HYDRODYNAMIC FORCES» AND BOTH NORMAL AND TANGENTIAL DRAGS ARE INCILUD- 
EDe DOCUMENTED IN NRL REPORT 6894 (MAY 1969)5 BY ReAcw SKOP AND ReEo 
KAPLANe MEMORY REQUIREMENTS-— APPROXe 16000 WORDS FOR THE ARRAYS IN 
COMMON AND 2100 WORDS FOR THE MAIN PROGRAM AND SUBPROGRAMSe 


NAVAL RESEARCH LABORATORY 
4555 OVERLOOK AVENUEs SeWe 
WASHINGTON» De Ce 20390 


CABLE CONFIGURATION LANGUAGE — FORTRAN Iv 
GOMPUTER = IBM 1800 SYS 
(COPY ON FILE AT NODC) 

COMPUTES THE EQUILIBRIUM CONFIGURATION AND TENSIONS OF A CABLE TOWING 
A SUBMERGED BODY FOR FAIRED, UNFAIREDs AND DISCONTINUOUS (LOWER PART 
FAIRED) CABLESe THE OUTPUT ON THE LINE PRINTER GIVES THE VALUES OF 
THE INPUT DATA FOLLOWED BY VARIOUS CALCULATED VALUESe THE SOLUTION IS 
FOUND FOR THE "HEAVY GENERAL CABLE* LAW OF CABLE LOADINGS AS DESCRIBED 
BY MeCe EAMES (1968)e EXECUTION TIME-— ABOUT 30 SECSe FOR EACH CASE. 
NeleOQo PROGRAM NOe 168¢ AUTHOR-- CATHERINE CLAYSONe 


NATIONAL INSTITUTE OF OCEANOGRAPHY 
WORMLEY»s GODALMINGs SURREY 
ENGLAND 


CURRENT METER ANALYSIS LANGUAGE -— FORTRAN IV 
COMPUTER -— IBM 1800 SYS 


READSs CALIBRATES AND PLOTS DATA FROM BERGEN OR PLESSEY CURRENT MET-— 
ERSe DATA IS READ FROM CARDSe ANY ONE OF THE READINGS MAY BE TAKEN 
AS ROTOR COUNT, THE DIFFERENCES BETWEEN CONSECUTIVE READINGS THEN BE- 
ING USED BY THE PROGRAM AS THE BASIS OF CURRENT SPEEDe THREE GRAPHS 
MAY BE PLOTTED (EeGe SPEED» DIRECTION, AND TEMPERATURE) e ALL RESULTS 
ARE ALSO OUTPUT TO MAGNETIC TAPEe NelIeO5o PROGRAM 111 BY WeleJe SLADE 
WRITE-UP IN NeleO5w INTERNAL REPORT NOe Nel2s DEC 1968-6 


NATIONAL INSTITUTE OF OCEANOGRAPHY 
WORMLEYs» GODALMINGs SURREY 
ENGLAND 


CURRENT METER CONVERSION LANGUAGE -— FORTRAN IV 
COMPUTER - IBM 1800 SYS 


CONVERTS RAW CURRENT METER DATA INTO CALIBRATED OUTPUT FOR RECORDING 
ON BOTH LINE-PRINTER AND MAGNETIC TAPEe NeleOs SUB-PROGRAM -ll»s BY 
WeTeJo SLADE (REFe NelTeO5s INTERNAL REPORT NOco Nol2)eo 


NATIONAL INSTITUTE OF OCEANOGRAPHY 
WORMLEY» GODALMINGs SURREY 
ENGLAND 


VEL LANGUAGE - FORTRAN IV-H 
COMPUTER - SDS SIGMA 7 


COMPUTES GEOSTROPHIC VELOCITY DIFFERENCE BETWEEN TWO OCEANOGRAPHIC 
STATIONSs ACCORDING TO A FORMULA DESCRIBED BY NePe FOFONOFF AND CHAR- 
LOTTE FROESEe (PROGRAM WRITTEN AS SUBROUTINE -— NO I/P OR O/P) 


INFORMATION PROCESSING CENTER 

ATTNe MARY HUNT 

WOODS HOLE OCEANOGRAPHIC INSTITUTION 
WOODS HOLE» MASSACHUSETTS 02543 


VTR LANGUAGE —- FORTRAN IV-H 
GOMPUTER SD SieSiG MAN, 


PAGE 073 


SUBROUTINE COMPUTES VOLUME TRANSPORT BETWEEN TWO STATIONSe 


INFORMATION PROCESSING CENTER 


ATTNe MARY HUNT 
WOODS HOLE OCEANOGRAPHIC INSTITUTION 
WOODS HOLE, MASSACHUSETTS 02543 


THISTO LANGUAGE —- FORTRAN IV-H 
COMPUTER — SDS SIGMA 7 


PRODUCES A TWO DIMENSIONAL FREQUENCY DISTRIBUTION OF SAMPLES AVERAGED 
OVER CHOSEN INTERVAL AGAINST TIMEe INPUT-- CONTROL CARDS AND 9-TRACK 
MAG. TAPEs’ OUTPUT—- A LINE PRINTER PLOT OF AVERAGED COMPASS» VANE» 


DIRECTION» AND SPEED AGAINST TIME. 


INFORMATION PROCESSING CENTER 


ATTNe JOHN Ae MALTAIS 
WOODS HOLE OCEANOGRAPHIC INSTITUTION 


WOODS HOLE, MASSACHUSETTS 02543 


VECTAV LANGUAGE — FORTRAN IV-H 
COMPUTER -— SDS SIGMA 7 


PRODUCES A NINE TRACK MAGe TAPE IN WHOI FORMAT OF EAST AND NORTH VEL- 
OCITY VECTOR AVERAGES AND THEIR CORRESPONDING POLAR REPRESENTATIONSe 


INPUT—— CONTROL CARDS AND DATA ON 9-TRACK TAPE. 


INFORMATION PROCESSING CENTER 

ATTNe JOHN Ae MALTAIS 

WOODS HOLE OCEANOGRAPHIC INSTITUTION 
WOODS HOLEs MASSACHUSETTS 02543 


PROVEC LANGUAGE — FORTRAN IV-H 
COMPUTER - SDS SIGMA 7 


COMPUTES PROGRESSIVE VECTORS FROM DIRECTION AND SPEED VALUESe INPUT-— 
CONTROL CARDS AND 9-TRACK MAGe TAPE IN WHOI FORMATe OUTPUT-—- LISTINGs 
ON LINE PRINTER» OF PROGRESSIVE VECTORS AND/OR A MAGe TAPE TO BE USED 
WITH A PDP-5 DRIVEN CALCOMP FOR A PLOT OF THE VECTORS. 


INFORMATION PROCESSING CENTER 


ATTNe JOHN Ae MALTAIS 
WOODS HOLE OCEANOGRAPHIC INSTITUTION 


WOODS HOLE» MASSACHUSETTS 02543 


¥—%—*% ICE IN THE SEA *—*—* 


LANGUAGE — FORTRAN 60 


ICEGRID MODIFIED 
COMPUTER — IBM 1604 


(COPY ON FILE AT NODC) 
INCORPORATES PROGRAMS 'ICEMELT!' AND "ICEGRID'e TAKES INTO CONSIDERA- 


TION THE EFFECTS OF MELTING ON THE PRODUCTION OF FIVE-DAY FORECASTS OF 


THE WIND DRIFT AND CONCENTRATION OF SEA ICEs USING EQUATIONS AFTER ZU- 
BOV AND AN EARLIER PROGRAM OF KNODLEe USES A 26X21 GRID-POINT ARRAY 
WITH VARIABLE SCALEe OUTPUT FIELDS ARE CONCENTRATION, DIRECTION AND 


DISTANCE OF MOVEMENTe DOCUMENTED IN THESIS BY KENNETH Me IRVINE (UN- 
PUBLISHED» 1965). 


NAVAL POSTGRADUATE SCHOOL 
MONTEREY» CALIFORNIA 93940 


PAGE 074 


ICE POTENTIAL LANGUAGE — FORTRAN 
COMPUTER — IBM 7074 


PROCESSES OBSERVED SEA ICE CONDITIONS SO THEY CAN BE USED IN FORECAST-— 
ING SEA ICE CONDITIONSe OS NOe 201412e AUTHOR-- LeAew WALKERe 


DATA SYSTEMS CENTER» CODE 0831 
NAVAL OCEANOGRAPHIC OFFICE 
SUITLANDs MDe 20390 


STATISTICAL ANALYSIS OF ICE DATA LANGUAGE — FORTRAN 
COMPUTER — IBM 7074 


COMPUTES THE MEAN CONCENTRATION VALUES» MEAN AGE SEVERITY VALUES» AND 
MEAN FLOE SIZE SEVERITY VALUE OF ICE DATAe AUTHOR-- BARBARA GRAY e 


OCEANOGRAPHIC PREDICTIONs CODE 3400 
NAVAL OCEANOGRAPHIC OFFICE 
SUITLAND» MDe 20390 


SEA ICE STUDIES LANGUAGE - FORTRAN IV 
COMPUTER — IBM 7090/94 
(COPY ON FILE AT NODC) 

A GENERALIZED PROGRAM WITH SEVERAL OPTIONS THAT ALLOW CONSIDERABLE 
LATITUDE IN THE SPECIFICATION OF INPUT AND OUTPUT DATAe A MAIN PROGRAM 
READS IN THE INPUT DATA AND SUMMARIZES THE RESULTS OF EACH YEAR'S IN- 
TEGRATIONe SUBROUTINE YARIT CALCULATES THE TEMPERATURE AND THICKNESS 
CHANGES OF THE ICE AND SNOW FOR EACH TIME STEP DURING THE YEARe SUB- 
ROUTINE FLIP TAKES THE MONTHLY VALUES OF THE INDEPENDENT ENERGY FLUXES 
AT THE UPPER BOUNDARY AND PRODUCES SMOOTHED VALUES FOR EACH TIME STEPe 
SUBROUTINE SALPR CALCULATES THE SALINITY PROFILE FOR EACH TIME STEPe 
FINALLYs SUBROUTINE RITE WRITES THE TEMPERATURE PROFILE» ICE THICKNESS 
AND MASS CHANGES FOR EACH 10-DAY PERIOD THROUGHOUT THE YEARe LISTED 
IN A MEMORANDUM RM-6093-PR (NOV 19695 173 P) "NUMERICAL PREDICTION OF 
THE THERMODYNAMIC RESPONSE OF ARCTIC SEA ICE TO ENVIRONMENTAL CHANGES! 
BY GeAe MAYKUT AND Ne UNTERSTEINERe PREPARED FOR UeSe AIR FORCE PRO- 
JECT RANDe 


THE RAND CORPORATION 
1700 MAIN STe 
SANTA MONICAs CALIFe 90406 


*#-#—- PHYSICAL PROPERTIES - ANALYSES AND SUMMARIES —-*-* 


DEVIATION OF TEMPe AND SALINITY PART 1 (DOTS-1) LANGUAGE — AUTOCODER 
COMPUTER - IBM 7074 
(COPY ON FILE AT NODC) 
A PROTOTYPE PROGRAM TO MONITOR NODC FORMAT COMPUTED OCEAN STATION DATA 
FOR ERRORS» OS NOe 52305¢ AUTHOR-- SeCe PORTERe 


DEVELOPMENT DIVISION, CODE 2320 
NATIONAL OCEANOGRAPHIC DATA CENTER 
WASHINGTONs DeCe 20390 


OBJECTIVE THERMOCLINE ANALYSIS LANGUAGE —- FORTRAN IV-H 
COMPUTER — IBM 360 SERe 
AND CDC 6500 
(COPY ON FILE AT NODC) 
READS DIGITIZED BATHYTHERMOGRAPH TRACES AND THEN ANALYZES THEM OBJECT- 
IVELY BY GAUSSIAN AND NON-GAUSSIAN METHODS FOR THE TOPs CENTER, AND 
BASE OF THE MAIN THERMOCLINEe ADDITIONALLY» SUCH FEATURES AS MULTIPLE 


PAGE 075 


THERMOCLINES» INVERSIONS» AND THERMAL TRANSIENTS ARE IDENTIFIED ALSO 
AND THEIR KEY POINTS ARE INCLUDED IN THE INFORMATIONAL DATA PRINTOUT. 


THESIS BY ERIC Fe GROSFILS "OBJECTIVE DIGITAL ANALYSIS OF BATHYTHERMO-— 
GRAPH TRACES' (UNPUBLISHED MANUSCRIPT, DECe 1968s 130 P)e 


NAVAL POSTGRADUATE SCHOOL 
MONTEREY» CALIFORNIA 93940 


GRADIENT SUMMARY BY 1-DEG SQUARE» MONTH LANGUAGE — AUTOCODER 
COMPUTER — IBM 7074 
(COPY ON FILE AT NODC) 

COMPUTES AND PRINTS AVERAGE TEMPERATURE GRADIENTS FOR EACH 20 METER 
DEPTH INTERVAL» BY EACH OF 12 MONTHS» ALONG WITH THE NUMBER OF OBS THE 
MEAN IS BASED ONe ANY SIGNIFICANT POSITIVE GRADIENTS (INCREASE OF 022 
DEGe C/20M OR MORE) SUMMARIZED SEPARATELY ON SAME PAGEe INPUT IS NODC 
DIGITIZED BT FILE» SORTED GEOGRAPHICALLYe OS NOe 624016 AUTHOR-— JEFF 


GORDON (REVISED JULY 1969)e 


COMPUTER SYSTEMS DIVe»s CODE 2400 
NATIONAL OCEANOGRAPHIC DATA CENTER 
WASHINGTONs De Ce 20390 


THERMOCLINE AND MIXED LAYER DEPTHS LANGUAGE -— AUTOCODER 
COMPUTER -— IBM 7074 
(COPY ON FILE AT NODC) 
DETERMINES AND PRINTS OUT THE DEPTHS OF THE MIXED LAYER AND TOP OF THE 
THERMOCLINE FOR INDIVIDUAL BT OBSERVATIONS» WITH MEANS FOR EACH MONTH 
WITHIN A 1-DEGREE SQUAREe USES GRADIENT CRITERIA GIVEN BY CODE 2120 
SCIENTIST (BASED LARGELY ON NODC!S GRADIENT SUMMARY PROGRAM OUTPUT) » 
AND ENTERED ON CONTROL CARDSe COMPARISON IS MADE WITH ABSOLUTE VALUE 
OF GRADIENT/ 10Me OS NOe 624026 AUTHOR-- JEFF GORDON (JULY 1969). 


COMPUTER SYSTEMS DIVes CODE 2400 
NATIONAL OCEANOGRAPHIC DATA CENTER 
WASHINGTON» De Ce 20390 


SeEeReCe BI ANALYSIS LANGUAGE -— AUTOCODER 
COMPUTER — IBM 7074 
(COPY ON FILE AT NODC) 
ERROR CHECKS DATA AND COMPUTES LAYER DEPTHs SURFACE EFFECT» MEAN 
GRADIENT» MAXIMUM NEGATIVE GRADIENT» ASCENDANT AND FIRST NEGATIVE 
GRADIENTe A SOUND VELOCITY COMPUTATION IS ALSO MADEe OS NOe 201136 
REPORT NOe O-31-63 (UNPUBLISHED MANUSCRIPT)e AUTHOR-- MeEeo MYERSe 


COMPUTER DEPARTMENT» CODE 0831 
NAVAL OCEANOGRAPHIC OFFICE 
SUITLAND» MDe 20390 


GDNP »GRAD LANGUAGE — FORTRAN Iv 
COMPUTER - IBM 360/65 
WITH CALCOMP 


CALCULATES THE GRADIENTS OF DENSITY» TEMPERATURE» AND SALINITY AS 
FUNCTIONS OF SIGMA-T ALONG 4 STANDARD SECTIONS IN THE TRADE WIND ZONE 
OCEANOGRAPHY PROGRAM PILOT STUDY AREAe CALCOMP DIGITAL PLOTTER RE- 


QUIRED FOR PROGRAM 'GRAD'. 
BUREAU OF COMMERCIAL FISHERIES 


Pe O« BOX 3830 
HONOLULU» HAWAII 96812 


BT TEMPERATURE GRADIENT DISTRIBUTION LANGUAGE — FORTRAN 
COMPUTER — IBM 7074 


COMPUTES A FREQUENCY TABLE OF GRADIENTS IN 30 INTERVALS BY DEPTHSe ANY 


PAGE 076 


EXCEPTIONS TO THE INTERVALS WITH THEIR CORRESPONDING DEPTH AND THE 
MEAN GRADIENT FOR EACH DEPTH IS PRINTED ALSO’ OS NOe 10120%¢ AUTHOR - 


MeVe JENNINGS. 


COMPUTER DEPARTMENT» CODE 0831 
NAVAL OCEANOGRAPHIC OFFICE 
SUITLAND» MD. 20390 


MONTHLY SONIC LAYER DEPTH LANGUAGE -— FORTRAN 
COMPUTER -— IBM 7074 


CALCULATES SONIC LAYER DEPTH FROM BT TRACES AND CONVERTS POSITION TO 
PLOT ON MERCATOR BASE WITHOUT OVERPRINTSe OS NOe 5348056 AUTHOR-- DeBe 


NIXe 


OCEANOGRAPHIC PREDICTION DIVes CODE 3400 
NAVAL OCEANOGRAPHIC OFFICE 
SUITLAND» MDe 20390 


SEA SURFACE TEMPERATURE DISTRIBUTION LANGUAGE - FORTRAN 
COMPUTER - IBM 7074 
(COPY ON FILE AT NODC) 
TABULATES THE FREQUENCY» PERCENT FREQe» CUMULATIVE PERCENT FREQes AND 
MEAN TEMPERATURE FOR ALL ONE-DEGREE SQUARES AND MONTHS PROVIDED By 
SEA SURFACE TEMPERATURE SUMMARY CARDS FROM ASHEVILLE», Ne Ce OS NOe 
201362 AUTHOR-- Je LECKIEe 


COMPUTER DEPARTMENT» CODE 0831 
NAVAL OCEANOGRAPHIC OFFICE 
SUITLAND» MD. 20390 


TEMPERATURE DISTRIBUTION BY ONE-DEGREE SQUARES LANGUAGE — FORTRAN 
COMPUTER - IBM 7074 
(COPY ON FILE AT NODC) 

COMPUTES AND TABULATES A FREQUENCY DISTRIBUTION FOR SELECTED TEMPER- 

ATURE INTERVALS AND STANDARD DEPTHS» AND THE MAXIMUMs MINIMUM s AND 

MEAN VALUES OF TEMPERATURE FOR EACH STANDARD DEPTHe A REPORT IS PRO- 

DUCED FOR EACH ONE-DEGREE SQUAREe OS NOe 20126 PART 5e AUTHOR-- CeSe 

CALDWELL. 


COMPUTER DEPARTMENT: CODE 083 
NAVAL OCEANOGRAPHIC OFFICE 
SUITLAND» MD. 20390 


TEMPERATURE AVERAGE SUMMARY BY 1-DEGREE SQUARES LANGUAGE — FORTRAN 
COMPUTER -— IBM 7074 
(COPY ON FILE AT NODC) 
COMPUTES FOR EACH ONE-DEGREE SQUARE WITHIN A MARSDEN SQes FROM GEO- 
GRAPHIC STATION DATAs A SEASONAL AVERAGE AND FREQUENCY AND A TWELVE 
MONTH AVERAGE AND FREQUENCY, AT EACH OF FOURTEEN SELECTED STANDARD 
DEPTHSe OS NOe 201232¢ AUTHOR-- CeSe CALDWELL. 


COMPUTER DEPARTMENT» CODE 083 
NAVAL OCEANOGRAPHIC OFFICE 
SUITLANDs MD. 20390 


VERTICAL TEMPERATURE GRADIENTS LANGUAGE — FORTRAN 
COMPUTER — IBM 7074 
(COPY ON FILE AT NODC) 

COMPUTES, FROM GEOGRAPHIC STATION DATAs THE VERTICAL TEMPERATURE GRAD- 
IENT LARGEST IN ABSOLUTE MAGNITUDE BETWEEN SUCCESSIVE STANDARD DEPTHS, 
FOR EACH STATIONe THESE GRADIENTS ARE TABULATED IN FREQUENCY DISTRIBU- 
TION FORMAT» AND AVERAGES ARE CALCULATED FOR EACH ONE-DEGREE SQUARE e 
OS NO«w 20126 PART 2¢ AUTHOR-- CeSe CALDWELL. 


PAGE O77 


COMPUTER DEPARTMENT» CODE 083 
NAVAL OCEANOGRAPHIC OFFICE 
SUITLAND» MD. 20390 


DENSITY (SIGMA-T) GRADIENT BY 1-DEGREE SQUARE LANGUAGE — FORTRAN 
COMPUTER — IBM 7074 
(COPY ON FILE AT NODC) 

COMPUTES» FROM GEOGRAPHIC STATION DATA» THE VERTICAL SIGMA-T GRADIENT 
LARGEST IN ABSOLUTE MAGNITUDE BETWEEN SUCCESSIVE STANDARD DEPTHS» FOR 
EACH STATIONe THESE GRADIENTS ARE TABULATED FOR FREQUENCY DISTRIBUTION 
FORMATs AND AVERAGES ARE CALCULATED FOR EACH 1-DEG SQe OS NOs 20122. 
AUTHOR-- CeSe CALDWELL. 


COMPUTER DEPARTMENT: CODE 083 
NAVAL OCEANOGRAPHIC OFFICE 
SUITLAND» MD. 20390 


THERMOCLINE ONE-DEGREE LANGUAGE - AUTOCODER 
COMPUTER - IBM 7074 
(COPY ON FILE AT NODC) 

PRODUCES A DESCRIPTION OF THE THERMOCLINE BY DEFINING THE TOPs BOTTOM, 
MAGNITUDE, AND INTENSITY OF THE THERMOCLINE AND THE MOST EXTREME IN- 
TENSITY WITHIN THE THERMOCLINEe THE PRINTED REPORT CONTAINS THE ABOVE 
QUANTITIES FOR EACH STATION WITHIN A 1-DEGREE SQUARE, ALSO AVERAGE 
VALUES FOR THE 1-DEGREE SQUARE. IN PRODUCTION MODE, THE PROGRAM USES 
A CONSTANT THERMOCLINE CRITERIONe IN THE TEST MODE, THE CRITERION MAY 
BE INCREMENTED FOR ANOTHER PASS OF THE SAME DATA TAPEs OS NOe 201265 
PART 46 AUTHOR-- CeSe CALDWELL. 


COMPUTER DEPARTMENTs CODE 083 
NAVAL OCEANOGRAPHIC OFFICE 
SUTTLAND» MARYLAND 20390 


SALINITY GRADIENT BY ONE-DEGREE SQUARE LANGUAGE — FORTRAN 
COMPUTER - IBM 7074 
(COPY ON FILE AT NODC) 

COMPUTESs FROM GEOGRAPHIC STATION DATAs THE VERTICAL SALINITY GRADIENT 
LARGEST IN ABSOLUTE MAGNITUDE BETWEEN SUCCESSIVE STANDARD DEPTHS» FOR 
EACH STATIONe THIS INFORMATION IS TABULATED IN FREQUENCY DISTRIBUTION 
FORM, AND AVERAGES ARE CALCULATED FOR EACH ONE-DEGREE SQUARE. THE FRE- 
QUENCY INTERVAL IS 0201 O0/00/M BETWEEN LIMITS OF -0.5 AND +205 O/00/Me 
OS NOs 20121. AUTHOR-- CeSe CALDWELL. 


COMPUTER DEPARTMENT» CODE 083 
NAVAL OCEANOGRAPHIC OFFICE 
SUITLAND» MD. 20390 


SALINITY DEVIATION COMPUTATION WITH PLOT LANGUAGE — FORTRAN 
COMPUTER — IBM 7074 
(COPY ON FILE AT NODC) 
THE DEVIATIONS OF SALINITY FROM RELATED MODELS ARE COMPUTED FOR SERIAL 
OCEANOGRAPHIC STATION DATA AND A SALINITY PROFILE PLOTTEDe OS NOe - 
52301le AUTHOR-— SeCe PORTER. 


DEVELOPMENT DIVISION, CODE 2320 
NATIONAL OCEANOGRAPHIC DATA CENTER 
WASHINGTONs De Ce 20390 


STATION DATA VERTICAL ARRAY SUMMARY LANGUAGE — AUTOCODER 
COMPUTER —- IBM 7074 
(COPY ON FILE AT NODC) 
SUMMARIZES FOR ANY COMBINATION OF SIX PARAMETERS ( TEMPERATURE» SAL- 
INITY» SIGMA-Ts OXYGENs SOUND VELOCITY» DYNAMIC DEPTH) AND COMPUTES 
MAXIMUM AND MINIMUM VALUES» NUMBER OF OBSERVATIONSs MEANS AND STANDARD 
DEVIATIONS AT STANDARD LEVELSe SUMMARIES MAY BE MONTHLY OR YEARLY AND 


PAGE 078 


BY SELECTED ONE-DEGREE SQUARESe THERE IS AN OPTION TO GENERATE A SPE- 
CIAL CONDENSED TAPE FOR INPUT TO A HISTOGRAM PLOT PROGRAMe OS NOe 


52257e AUTHOR-- MAXINE JACKSONe 


COMPUTER SYSTEMS DIVISION 
NATIONAL OCEANOGRAPHIC DATA CENTER 
WASHINGTON» DeCe 20390 


MARSDEN SQUARE AVERAGES FROM OCEAN STATION LANGUAGE — FORTRAN 
GEO-SORTED FILE COMPUTER -— IBM 7074 
(COPY ON FILE AT NODC) 

CALCULATES AVERAGE SEA SURFACE SOUND VELOCITY» AVERAGE LAYER DEPTH» 
AVERAGE DEPTH OF THE SOUND CHANNEL AXIS» AND AVERAGE SOUND VELOCITY AT 
THE SOUND CHANNEL AXISe THESE VALUES ARE CALCULATED FOR EACH ONE-DE- 
GREE QUADRANGLE FOR EACH MONTHe A SUBPROGRAM *AREAD! IS CALLED WHICH 
GAINS ACCESS TO THE NODC ARCHIVE TAPE FILE OF SORTED OCEANOGRAPHIC DA- 
TAe REFe INFORMAL REPORT IR NOe 67-95 (DEC 1967)» ENTITLED "EXTRACT-— 
ING INFORMATION FROM THE GEO-SORT FILE BY COMPUTER PROGRAMING!» BY Je 
Ce FRANCE» OCEANOGRAPHIC ANALYSIS DIVISION» CODE 33166 FURTHER INFOR- 
MATION MAY BE OBTAINED FROM DISSEMINATION DEPTe CODE 445 OR THE AUTHOR 


NAVAL OCEANOGRAPHIC OFFICE 
WASHINGTONs DeCe 20390 


STATION DATA PARAMETER INVENTORY LANGUAGE — FORTRAN 
COMPUTER — IBM 7074 


(COPY ON FILE AT NODC) 

LISTS GEOSORTED STATION DATAs ONE LINE FOR EACH STATIONs SHOWINGs BE- 
SIDES NORMAL IDENTIFICATION FIELDSs THE DEPTH TO BOTTOMs MAXIMUM SAMP— 
LE DEPTH, PRESENCE OR ABSENCE OF WATER COLOR AND TRANSPARENCY CODES» 
MAXIMUM DEPTH OF SOUND VELOCITIES» MINIMUM DEPTH» AND A VERTICAL IN- 
DICATOR WHICH IS THE ARITHMETIC AVERAGE OF VERTICAL SAMPLE SPACING IN 
TENS OF METERSe OS NO 52230¢ ALSO» PROGRAM CAN WRITE OUTPUT» INTER- 
NAL NOTATIONs FOR INPUT TO A PLOTTER PROGRAM (OS NOe 52229)e AUTHOR — 


ROBERT VAN WIEe 


COMPUTER SYSTEMS DIVISION 
NATIONAL OCEANOGRAPHIC DATA CENTER 
WASHINGTONs DeCe 20390 


DAILY SEAWATER OBSERVATIONS LANGUAGE -— FORTRAN IV 
COMPUTER - CDC 3100 


INPUTS DAILY OBSERVATIONS OF TEMPERATURE AND SALINITY AND OUTPUTS (1) 
QUARTERLY STATISTICS (2) ANNUAL STATISTICS (3) A LISTING OF SEVEN-DAY 
NORMALLY WEIGHTED MEANS FOR ONE YEAR (4) A PLOT OF NORMALLY WEIGHTED 
MEANS FOR ONE YEARe AUTHOR-- He SOMERSe EARLY VERSION IN FORTRAN II- 


D FOR THE IBM 1620. 


CANADIAN OCEANOGRAPHIC DATA CENTRE 
615 BOOTH STREET 
OTTAWA» CANADA 


OCEANOGRAPHIC SUMMARY (NOSe 192593) LANGUAGE — FORTRAN IV 
COMPUTER - I8M 360/65 


SUMMARIZES TEMPERATURE» SALINITY» DEPTH AND OXYGEN By 1-DEGREE SQUARES 
AND OTHER DEGREE AREAS WITHIN SELECTED MARSDEN SQUARES» AT SELECTED 
SIGMA-T LEVELSe VERSIONS OF PROGRAM FOR CARD OR TAPE INPUT» AND EITHER 
CHART OR VERTICAL SECTION OUTPUT. 


BUREAU OF COMMERCIAL FISHERIES BIOLOGICAL LABe 
ATTNe DRe Re Aco BARKLEY» OCEANOGRAPHER 


PeOe BOX 3830 
HONOLULU» HAWAII 96812 


PAGE 079 


SEA SENSE - DATA DISPLAY LANGUAGE — FORTRAN 
COMPUTER — IBM 7074 
(cOPY ON FILE AT NODC) 

EVALUATES NOMAD (NAVAL OCEANOGRAPHIC AND METEOROLOGICAL AUTOMATIC DE- 
VICE) BUOY DATAs AND OUTPUTS A DISPLAY OF EACH OF THE 5 METEOROLOGICAL 
PARAMETERS. THE DISPLAY IS PRINTED BY THE IBM 1401. IN ADDITION TO 
THE DISPLAY» THE PROGRAM TOTALS THE NUMBER OF OBSERVATIONS MISSING FOR 
ANY MONTHs AND PRINTS A HISTOGRAM OF THE DATA FOR EACH MONTHe THIS 
PROGRAM IS ONE OF A CONTINUING SERIES OF COMPUTER PROGRAMS IN PROJECT 
SEA SENSE. AUTHOR-- DIANA LAMAR. 


SERVICES DIVISIONs CODE 2210 
NATIONAL OCEANOGRAPHIC DATA CENTER 
WASHINGTON» De Ce 20390 


SEA SENSE — LIMIT LANGUAGE - FORTRAN 
COMPUTER — IBM 7074 
(COPY ON FILE AT NODC) 

COMPARES NOMAD BUOY DATA TO ESTABLISHED NORMALS OF ABSOLUTE VALUES AND 
TO ACCEPTABLE MAP DATAe A MONTHLY TOTAL FOR EACH PARAMETER IS COMPUT— 
ED AND PRINTED FOR DATA WHICH IS GOOD, BAD» DOUBTFUL AND MISSINGe ALSO 
COMPUTES THE PERCENT OF WIND SPEEDS IN EACH BEAUFORT FORCE CATEGORY 
AND PRINTS THIS WITH THE NORMALS EXPECTED FOR THAT MONTH. WIND DIREC-— 
TION PERCENTS ARE COMPUTED ACCORDING TO THE 9 CATEGORIES OF WIND DI- 
RECTIONs AND PRINTED VSe THE NORMALSe ALSO THE MEANS OF NOMAD AND MAP 
DATA ARE COMPUTED AND PRINTED VS» THE LIMIT MEANSe AUTHOR-- DIANA LA- 
MAR. 


SERVICES DIVISION, CODE 2210 
NATIONAL OCEANOGRAPHIC DATA CENTER 
WASHINGTONs De Ce 20390 


SEA SENSE — STANDARD DEVIATION LANGUAGE — FORTRAN 
COMPUTER — IBM 7074 
(COPY ON FILE AT NODC) 

COMPUTES THE MEAN AND STANDARD DEVIATION FOR EACH OF 5 METEOROLOGICAL 
PARAMETERS FOR EACH MONTH OF NOMAD BUOY DATAe IF MAP DATA IS AVAIL— 
ABLE, THE MEANS AND STANDARD DEVIATIONS AND MEANS AND STANDARD DEVIA- 
TIONS OF THE DIFFERENCES BETWEEN NOMAD AND MAP DATA ARE COMPUTED. ALSO 
COMPUTES THE TOTAL MEAN SIGNAL STRENGTH AND THE MEANS FOR EACH SYNOP-— 
TIC HOUR. AUTHOR-- DIANA LAMARe 


SERVICES DIVISION» CODE 2210 
NATIONAL OCEANOGRAPHIC DATA CENTER 
WASHINGTON» De Co 20390 


SYNOPTIC MARINE WEATHER DATA SUMMARY LANGUAGE - FORTRAN-62 
COMPUTER — CDC 3600 


COMPILATION OF MONTHLY SEA SURFACE TEMPERATURES AND ANOMALIES (DEG— 
REES CENTIGRADE)» AIR TEMPERATURES (DEGREES CENTIGRADE)» DEWPOINT TEM— 
PERATURES (DEGREES CENTIGRADE)»s BAROMETRIC PRESSURES (MILLIBARS)» X- 
AND Y- WIND VECTORS (KNOTS), WIND SPEEDS (KNOTS)»s CLOUD COVER (TENTHS 
OF SKY COVERED), AND HEAT BUDGET VALUES (ENERGY EXCHANGE ACROSS AIR- 
SEA INTERFACE IN CALORIES/CENTIMETER SQUARED/DAY) WITH NUMBER OF OBS- 
ERVATIONS BY FIVE DEGREE QUADRANGLES - PACIFIC OCEANe AUTHOR-- MARVIN 
We CLINE 


DIRECTOR 

FISHERY OCEANOGRAPHY CENTER 
BUREAU OF COMMERCIAL FISHERIES 
PeOe BOX 271 

LA JOLLA, CALIFORNIA 92038 


PAGE 080 


SEA 


SEA 


SURFACE TEMPERATURE DATA SUMMARY LANGUAGE — FORTRAN-62 
COMPUTER -— CDC 3600 


COMPILATION OF MONTHLY SEA SURFACE TEMPERATURES (DEGREES FAHRENHEIT ) 
WITH NUMBER OF OBSERVATIONS BY ONE-DEGREE QUADRANGLES - PACIFIC OCEAN. 


DIRECTOR 

FISHERY OCEANOGRAPHY CENTER 
BUREAU OF COMMERCIAL FISHERIES 
PeOw BOX 271 

LA JOLLA» CALIFORNIA 92038 


SURFACE TEMPERATURE AND ANOMALY SUMMARY LANGUAGE - FORTRAN-62 
COMPUTER — CDC 3600 


COMPILATION OF MONTHLY SEA SURFACE TEMPERATURES (DEGREES FAHRENHEIT 
AND CENTIGRADE) AND ANOMALIES FROM LONG TERM MEAN WITH NUMBER OF OB- 
SERVATIONS BY TWO-DEGREE QUADRANGLES — PACIFIC OCEAN. 


DIRECTOR 

FISHERY OCEANOGRAPHY CENTER 
BUREAU OF COMMERCIAL FISHERIES 
PeO5w BOX 271 

LA JOLLA» CALIFORNIA 92038 


HEMISPHERIC SEA SURFACE TEMPERATURE ANALYSIS LANGUAGE - MACHINE 


COMPUTER -— CDC 1604 


(A) MAINTAINS UP-TO-DATE LARGE SCALE SYNOPTIC SEA SURFACE TEMPERATURE 
DISTRIBUTION FOR NORTHERN HEMISPHERE» (8) SUPPLIES INPUT MATERIAL FOR 
DETAILED ANALYSIS OF SELECTED LOCAL REGIONS ON A CURRENT BASIS ONLYe 
OUTPUT FROM PROGRAM-- (A) CALCOMP HARD COPY MAP, SCALE 1/60 MILLIONs 
WITH ISOTHERMS AT 2-DEG INTERVALS» (B) 63X63 ARRAY OF GRID POINT VAL- 
UES ON POLAR STEREOGRAPHIC PROJECTION WITH EQUATOR AN INSCRIBED CIRCLE 
(C) CERTAIN MEAN CHARTS OF SEA SURFACE TEMPERATURE FOR 5 DAYS» 15 DAYS 
AND MONTHLYe REFe TECHNICAL NOTE NOe 21 (1966). 


COMMANDING OFFICER 
FLEET NUMERICAL WEATHER CENTRAL 


MONTEREY» CALIFORNIA 93940 


GG T SEA LANGUAGE — MACHINE 


COMPUTER -— CDC 1604 


CALCULATES THE LOCATION OF LARGE SCALE HYPER-BAROCLINIC ZONES IN THE 
OCEANSe INPUT IS THE OUTPUT FROM THE SEA SURFACE TEMPERATURE ANALY- 
SIS PROGRAMe OUTPUT ARE ISOLINES OF THE GG PARAMETERe THE DIRECTION- 
AL SECOND SPACE DERIVATIVE OF THE BASIC PARAMETER IS COMPUTEDe CORE 
STORAGE-- 32000 48-BIT WORDSe ADDITIONAL STORAGE REQUIREMENTS—— ONE 
MILLION WORD DRUMe DATA IS IN THE STANDARD FNWC FORMATe DIRECT RE- 
QUESTS FOR INFORMATION TO-- 


COMMANDING OFFICER 
FLEET NUMERICAL WEATHER CENTRAL 
MONTEREYs CALIFORNIA 93940 


AVERAGE TEMPERATURES IN WATER COLUMN LANGUAGE — MAD 


COMPUTER - IBM 7090 


COMPUTES AVERAGE TEMPERATURE FOR EACH 10 METER LAYER IN WATER COLUMN. 
AVERAGE COMPUTED FOR EACH 1-DEGe LATe X 1-DEGe LONGe SQUARE FOR EACH 
MONTHe INPUT—- DIGITIZED BT DATAe 


VINCENT NOBLE 
THE UNIVERSITY OF MICHIGAN 
GREAT LAKES RESEARCH DIVISION 


PAGE 081 


1077 NORTH UNIVERSITY BUILDING 
ANN ARBORs MICHIGAN 48104 


SUBSURFACE THERMAL STRUCTURE ANALYSIS LANGUAGE -— SCRAP 
COMPUTER -— CDC 1604 


PRODUCES ANALYSIS OF (1) TEMPERATURE AT TOP OF THERMOCLINE (2) TEMPER 
ATURE AT SELECTED SUBSURFACE LEVELS (3) GRADIENT» MAGNITUDE» AND BOT- 

TOM OF THERMOCLINE AND (4) THERMOCLINE TENDENCY AND FLUCTUATIONS. IN- 
PUT TO PROGRAM-- (1) SEA SURFACE TEMPERATURE ANALYSIS (2) GRADIENT OF 

TRANSIENTS (3) PREVIOUS ANALYSIS OF ALL LEVELS (4) CLIMATOLOGY OF ALL 

LEVELS (5) ANALYSIS OF MIXED LAYER DEPTH, AND CURRENT TRANSPORT (6) BT 
REPORTS (7) WAVE HEIGHT FORECASTS AND (8) MIXED LAYER DEPTH FORECASTS. 
INPUT IS IN FNWC STANDARD FORMAT FIELDSe REFe TECHe NOTE NOe 21. 


COMMANDING OFFICER 
FLEET NUMERICAL WEATHER CENTRAL 
MONTEREYs CALIFORNIA 93940 


OCEAN STATION DEPTH SUMMARY LANGUAGE —- SPS 
COMPUTER - IBM 1401 
(COPY ON FILE AT NODC) 
USES THE NODC MASTER CARD FILE FOR OCEAN STATIONS WORLDWIDE» WHICHs IN 
ADDITION TO ALL IDENTIFICATION FIELDSs CONTAINS DEPTH TO BOTTOM AND 
MAXIMUM SAMPLE INFORMATIONe THE RECORDS ARE PUT ON TAPE, GEO-SORTED, 
ZONE-EDITED AND BLOCKED. THE FILE IS UPDATED SEMIANNUALLYe THE SUM-— 
MARY PROGRAMs REQUESTED BY NAVOCEANO MARINE SCIENCES DEPTe,s MAKES A 
TALLY OF THE NUMBER OF STATIONS WITH MAXe SAMPLES WITHIN GIVEN INTER- 
VALS» WITHIN A GIVEN DISTANCE FROM THE BOTTOMs ETCe TOTAL COUNTS ARE 
PRINTED FOR EACH MARSDEN SQes AND GRAND TOTALS FOR THE FILEe OS NOe« 
52286e¢ AUTHOR-- Ce DINGER 


COMPUTER SYSTEMS DIVISION 
NATIONAL OCEANOGRAPHIC DATA CENTER 
WASHINGTONs De Co 20390 


%¥-%-% PHYSICAL QUANTITIES» COMPUTATION OF *-—#-* 


STATION DATA COMPUTE LANGUAGE — AUTOCODER 
COMPUTER — IBM 7074 
(COPY ON FILE AT NODC) 

INTERPOLATES FOR TEMPERATUREs SALINITYs AND OXYGEN AT STANDARD DEPTHS. 
COMPUTES SIGMA-T AND WILSON'S SOUND SPEED AT OBSERVED AND STANDARD 
DEPTHSs COMPUTES SPECIFIC VOLUME ANOMALY AND DYNAMIC DEPTH ANOMALY AT 
STANDARD DEPTHSe OS NOw 522515 AUTHOR-- MAXINE JACKSONe ANOTHER PRO- 
GRAM FOR NODC STATION DATA COMPUTATIONS WAS WRITTEN LATER FOR THE GE- 
235/DATANET 30 SYSTEM IN BASIC LANGUAGE, BY JIM NOELe CURRENTLY» THE 
'COMPUTE' PROGRAM IS BEING REWRITTEN IN PL/I FOR THE IBM 0S/360,5 BY 
MAXINE JACKSON AND MICHAEL FLANAGANe 


COMPUTER SYSTEMS DIVISION 
NATIONAL OCEANOGRAPHIC DATA CENTER 
WASHINGTON, De Ce 20390 


BATHYTHERMOGRAPH DATA CONVERTER LANGUAGE — AUTUYCODER 
COMPUTER —- IBM 7074 
(COPY ON FILE AT NODC) 
CONVERTS BT TEMPERATURE DATA FROM 10 FEET -— FAHRENHEIT» 2 FATHOMS - 
FAHRENHEIT, 6 METERS — CENTIGRADE TO 5 METERS — CENTIGRADE INTERVALS. 
OS NOs 32253. AUTHOR-—- MAXINE JACKSONe NODC HAS ALSO IN THE PROGRAM 
LIBRARY A FORTRAN LANGUAGE ROUTINE TO CONVERT BT DATA, NODC FORMAT > 


PAGE 082 


FROM FAHRENHEIT/FEET AT 10 FTe INTERVALS TO CELSIUS/METERS AT 5 METER 
INTERVALS USING LINEAR INTERPOLATIONe AUTHOR-— RUDI SAENGERe OS NO. 
522026 


COMPUTER SYSTEMS DIVISION 
NATIONAL OCEANOGRAPHIC DATA CENTER 
WASHINGTON» De Ce 20390 


NIO PROGRAM 58 ATLAS — STATION DATA LANGUAGE — EMA 
COMPUTER - ATLAS 1 


VARIOUS PROPERTIES OF SEA WATER ARE CALCULATED FROM THE SETS UF READ- 
INGS OF PRESSURE (OR DEPTH)» TEMPERATURE AND SALINITY TAKEN AT A STA- 
TIONe SOME RESULTS ARE GIVEN AT OBSERVED» AND SOME AT STANDARD, PRES-— 
SURESe THERE ARE SEVERAL VERSIONS OF THIS PROGRAM DEPENDING UN WHETH- 
ER PRESSURE OR DEPTH IS INPUTe AUTHOR-- JAMES CREASEe REFe NeleOo 
INTERNAL REPORT NOe N60 


NATIONAL INSTITUTE OF OCEANOGRAPHY 
WORMLEY» GODALMINGs SURREY 
ENGLAND 


INTERPOLATION OF SPECIFIC VOLUME ANOMALY LANGUAGE —- FORTRAN 
COMPUTER -— IBM 7074 
(COPY ON FILE AT NODC) 

COMPUTES SPECIFIC VOLUME ANOMALIES AND DYNAMIC DEPTH ANOMALIES AT OB- 
SERVED LEVELSe FIELDS OCCUPY THE SAME POSITIONS AS ON THE NODC FORMAT 
STANDARD CARD AND REPLACE SOME CHEMISTRY FIELDSe AT STANDARD DEPTHS 
SPECIFIC VOLUME ANOMALIES ARE INTERPOLATED FROM THE OBSERVED LEVEI_S 
RATHER THAN COMPUTED FROM INTERPOLATED TEMPERATURE AND SALINITY AS HAS 
BEEN DONE PREVIOUSLYe DYNAMIC DEPTH ANOMALIES AT THESE STANDARD 
DEPTHS ARE THEN COMPUTED FROM THESE INTERPOLATED SPECIFIC VOLUME ANOM- 
ALIESe AN OUTPUT LISTING MAY BE MADE WHICH COMPARES THE TWO FIELDS AT 
STANDARD DEPTHS WITH THE SAME TWO FIELDS APPEARING ON THE INPUT DATA 
TO SHOW THE RESULTANT DIFFERENCESe OS NOco 5223262 AUTHOR--— ROBERT VAN 
WIE. 


COMPUTER SYSTEMS DIVISIONs CODE 2400 
NATIONAL OCEANOGRAPHIC DATA CENTER 
WASHINGTONs DeCe 20390 


INTERPOLATION FOR OCEANOGRAPHIC DATA LANGUAGE - FORTRAN 
COMPUTER — CDC 3200 AND 
IBM 1620 


(COPY ON FILE AT NODC) 
INTERPOLATES THE VALUES OF DEPTH, TEMPERATURE» AND SALINITY AT ISEN- 
TROPIC LEVELS (CONSTANT VALUES OF THE DENSITY FUNCTIONS) e USES A FOUR- 
POINT LAGRANGIAN POLYNOMIAL, EXCEPT MODIFICATIONS ARE MADE WHERE COM-— 
MON OCEANOGRAPHIC CONDITIONS DISTORT THE POLYNOMIALe A DETAILED TECH- 
NICAL REPORT PUBLISHED IN TM NOe 312 (FEBe 1964) 3 AUTHORS-- Je FARRELL 
AND Re LAVOIEs COPIES OBTAINABLE FROM DDC» NUWSs NODC. 


NAVAL UNDERWATER WEAPONS RESEARCH 
AND ENGINEERING STATION 
NEWPORT» RHODE ISLAND 02840 


PHYSICAL OCEANOGRAPHY DATA REDUCTION LANGUAGE — FORTRAN II 
PROGRAMS FOR THE CDC 3100 COMPUTER - CDC 3100 
(COPY ON FILE AT NODC) 

AN OCEANOGRAPHIC DATA PROCESSING SYSTEM DESIGNED TO ACCEPT THE DATA 
FROM THE ORIGINAL LOG SHEETSe COMPUTES OBSERVED TEMPERATURES AND 
PRESSURES FROM THERMOMETER READINGS» SALINITIES FROM THE CONDUCTIVITY 
RATIO READINGSs THE DISSOLVED OXYGEN FROM THE TITRES AND THE REACTIVE 
SILICA CONCENTRATIONS FROM THE OPTICAL DENSITIESe THE DATA INPUT MAY 
BE PUNCHED PAPER TAPE FROM THE PDP-8 SYSTEM (Bele COMPUTER NOTE 68-5- 
C) OR PUNCHED CARDSe THE FINAL PROGRAM IN THE SYSTEM COMPUTES DEPTH, 


PAGE 083 


POTENTIAL TEMPERATUREs SURFACE DENSITY ANOMALY, POTENTIAL SURFACE DEN- 
SITY ANOMALY AND SPECIFIC VOLUME ANOMALYe THE PROGRAM ALSO CAN COM- 
PUTE THE DYNAMIC HEIGHT AND POTENTIAL ENERGY ANOMALY AT GIVEN PRESS— 
URES AND MAY ALSO GIVE A MAGNETIC TAPE OF THE DATA IN CARD IMAGE OF 
THE CODC FORMAT. CORE STORAGE-- 16Ke REFe Bele COMPUTER NOTE 68-10-C 
(OCT 19685 280 PAGES)» BY Re REINIGERs CeKe ROSS» Pe TRITES AND DeJeo 
LAWRENCE. 


DIRECTOR 

ATLANTIC OCEANOGRAPHIC LABORATORY 
BEDFORD INSTITUTE 

DARTMOUTHs NOVA SCOTTIAs CANADA 


WET LANGUAGE — FORTRAN 
COMPUTER — HP 2115A 
(COPY ON FILE AT NODC) 
FOR SHIPBOARD PROCESSING OF DIGITIZED SALINITY-TEMPERATURE-DEPTH DATAs 
INPUT IS ON PAPER TAPE (SEE FRB PROGRAM 'DEEP'). OUTPUT ARE PARAMET- 
ERS AT STANDARD PRESSURES — TEMPERATURE» SALINITY» SIGMA-Ts DELTA-D> 
SPECIFIC GRAVITY ANOMALYs SPECIFIC VOLUME ANOMALY» GEOPOTENTIAL ANOM-— 
ALYs AND POTENTIAL ENERGYe DOCUMENTATION IN FRB TECHNICAL REPORT NO’ 
152 (DECEMBER 1969)» BY Ae HUYER AND Ce Ae COLLINS (UNPUBLISHED MSe). 


DRe Ge Ae COLLINS 

MARINE SCIENCES BRANCHs DEMR 
PACIFIC OCEANOGRAPHIC GROUP 
BIOLOGICAL STATION 

NANAIMO s BeCes CANADA 


STPO2 LANGUAGE — FORTRAN IV 
COMPUTER - IBM 1130 
(GOPY ON FIEE Al NODE) 

COMPUTES DERIVED OCEANOGRAPHIC QUANTITIES FOR BISSETT-—BERMAN SeTeDe 
CASTSe PRINTED OUTPUT HAS PRESSURE» TEMPERATURE» SALINITY: DEPTH, 
SIGMA-T»s SPECIFIC VOLUME ANOMALY, POTENTIAL TEMPERATURE AND DENSITY» 
DYNAMIC HEIGHT, POTENTIAL ENERGY ANOMALY, OXGYEN CONTENTe SOUND VELOC- 
ITY OPTIONALe INPUT DATA IS IN CODC FURMATe DOCUMENTED IN FRB MANU-— 
SCRIPT REPORT (UNPUBLISHED) NO. 1071 (DECEMBER 1969), BY CeAe COLLINS, 
RelLeKe TRIPE AND SeKe WONG 


DRe Ge Ae COLLINS 

MARINE SCIENCES BRANCHs DEMR 
PACIFIC OCEANOGRAPHIC GROUP 
BIOLOGICAL STATION 

NANAIMOs BeCes CANADA 


HYDRO LANGUAGE — FORTRAN IV 
COMPUTER -— IBM 1130 
(COPY ON FILE AT NODC) 

COMPUTES DERIVED OCEANOGRAPHIC QUANTITIES FOR HYDROGRAPHIC CASTS. 

OUTPUT ON IBM 1132 PRINTER LISTS PRESSURE, TEMPERATURE», SALINITY, 

DEPTH» SIGMA-T»s SPECIFIC VOLUME ANOMALY», POTENTIAL TEMPERATURE AND 

DENSITY» DYNAMIC HEIGHT, POTENTIAL ENERGY ANOMALY» AND OXYGEN CONTENT > 

WITH SOUND VELOCITY OPTIONALe DESCRIPTION AND LISTINGS IN FRB (UNPUB- 

LISHED) MANUSCRIPT REPORT NOe 1071 (DEC 1969). 


DRe Ge Ae GEOLLINS 

MARINE SCIENCES BRANCH, DEMR 
PACIFIC OCEANOGRAPHIC GROUP 
BIOLOGICAL STATION 

NANAIMOs BeCes CANADA 


CADS (CALCULATE DEPENDENT QUANTITIES) LANGUAGE - FORTRAN IV 
COMPUTER - IBM 1800 


FROM THE OBSERVED DEPTHS, TEMPERATURES AND SALINITIES» CALCULATES THE 


PAGE 084 


VARIOUS DEPENDENT QUANTITIES» SUCH AS POTENTIAL TEMPERATURES» SPECIFIC 
VOLUME ANOMALIES» SIGMASs AND DYNAMIC HEIGHTSe INTERPOLATES FOR THESE 
QUANTITIES AT STANDARD DEPTH USING A DOUBLE LAGRANGE'S INTERPOLATION 
METHODe FROM A PAIR OF STATIONS WITH A REFERENCE DEPTHs MEAN LATITUDE 
AND DISTANCE BETWEEN STATIONSs CALCULATES AT STANDARD DEPTHS RELATIVE 
VELOCITIES AND VOLUME TRANSPORTSe AUTHORS-— MRe MANLEYs LeWe YOUNGe 


MARINE LIFE RESEARCH GROUP 

SCRIPPS INSTITUTION OF OCEANOGRAPHY 
PeOe BOX 109 

LA JOLLAs CALIFORNIA 92037 


GO (POTENTIAL TEMPes SIGMA THETAs OXYGEN) LANGUAGE — FORTRAN IV 
COMPUTER - IBM 1800 


GIVEN DEPTHS» TEMPERATURES» SALINITIES» AND OXYGENSs CALCULATES POTEN- 
TIAL TEMPERATURES» SIGMA THETA'Ss AND OXYGENS IN UNITS OF ML/KGe 
AUTHORS-—- MRe MANLEYs Le We YOUNGe 


MARINE LIFE RESEARCH GROUP 

SCRIPPS INSTITUTION OF OCEANOGRAPHY 
PeOcoe BOX 109 

LA JOLLA» CALIFORNIA 92037 


FUNCTION POTLT (POTENTIAL TEMPERATURE) LANGUAGE -— FORTRAN 
COMPUTER - I8M 1800 
(COPY ON FILE AT NODC) 
SUBPROGRAM COMPUTES POTENTIAL TEMPERATURE OF SEA WATER GIVEN SALINITY>5 
TEMPERATURE» AND PRESSUREe P IS IN NEWTONS/SQ Me 


NATIONAL INSTITUTE OF OCEANOGRAPHY 
WORMLEYs GODALMINGs SURREY 
ENGLAND 


FUNCTION ALPHA (SPECIFIC VOLUME) LANGUAGE — FORTRAN 
COMPUTER - IBM 1800 
(COPY ON FILE AT NODC) 
SUBPROGRAM COMPUTES SPECIFIC VOLUME OF SEA WATER GIVEN SIGMA-T», SIGMA- 
ZEROs TEMPERATURE» AND PRESSUREe P IS IN DECIBARS 


NATIONAL INSTITUTE OF OCEANOGRAPHY 
WORMLEY » GODALMINGs SURREY 
ENGLAND 


FUNCTION SIGMO LANGUAGE — FORTRAN 
COMPUTER — I8M 1800 
(COPY ON FILE AT NODC) 
SUBPROGRAM COMPUTES HYDROGRAPHIC FUNCTION SIGMA ZERO FROM SALINITYe 


NATIONAL INSTITUTE OF OCEANOGRAPHY 
WORMLEY » GODALMINGs SURREY 
ENGLAND 


FUNCTION SIGMT LANGUAGE 
COMPUTER 


FORTRAN 
IBM 1800 


(COPY CN FILE AT NODC) 
SUBPROGRAM COMPUTES HYDROGRAPHIC FUNCTION SIGMA-T» FROM SIGMA-O AND 
TEMPERATUREe 


NATIONAL INSTITUTE OF OCEANOGRAPHY 
WORMLEYs GODALMINGs SURREY 
ENGLAND 
IN SITU OCEANOGRAPHIC DATA PROGRAM LANGUAGE — FORTRAN IV 


PAGE 085 


COMPUTER —- IBM 360/65 


COMPUTES SIGMA-T> DELTA ALPHA (SPECe VOLe ANOMe)»s OXYGEN PER CENT SAT- 
URATIONe ICES FORMAT CARD-TO-CARDe OUTPUT CARDS CONTAIN THE COMPUTED 
PARAMETERS ALONG WITH THE HYDRO DATAe AUTHOR-- MARILYNN BORKOWSKI » 
MODIFYING AN EARLIER PROGRAM BY DeLe SHAFFER FOR THE IBM 16206¢ 


BUREAU OF COMMERCIAL FISHERIES 

TROPICAL ATLANTIC BIOLOGICAL LABORATORY 
75 VIRGINIA BEACH DRIVE 

MIAMI,» FLORIDA 33149 


OCEANS III LANGUAGE — FORTRAN IV 
COMPUTER — IBM 360/65 


OCEANOGRAPHIC STATION PROGRAM, USED FOR QUALITY CONTROL» INTERNAL ED- 

ITINGs UNIT CONVERSION» COMPUTATION OF MARSDEN SQUARE, SIGMA-T, SOUND 

VELOCITYe ALSO USED FOR INTERPOLATION TO STANDARD DEPTHS USING RATT— 

RAY'S SCHEME AND COMPUTATION OF SPECIFIC VOLUME ANOMALY» DYNAMIC DEPTH 
AND POTENTIAL ENERGY ANOMALYe EARLIER VERSION FOR THE IBM 1620 TITLED 
OCEANS II IS NO LONGER USED AT CODC. 


CANADIAN OCEANOGRAPHIC DATA CENTRE 
615 BOOTH STREET 
OTTAWAs CANADA 


DENSITY-SALINITY LINEAR INTERPOLATION LANGUAGE — FORTRAN 
COMPUTER — IBM 7074 
(COPY ON FILE AT NODC) 
SELECTED DENSITY-SALINITY VALUES TO REPRESENT THE WATER MASS MIDPOINTS 
OF PARTICULAR AREASe LINEARLY INTERPOLATES THESE DENSITY-SALINITY 
VALUES WITH THE RESULTING SALINITIES GIVEN AT EVERY 0-01 SIGMA-T IN- 
CREMENTe OS NOe 52321le AUTHOR-- RePe STEINe 


DEVELOPMENT DIVISION, CODE 2300 
NATIONAL OCEANOGRAPHIC DATA CENTER 
WASHINGTONs De Ce 20390 


SeTeDe EDIT AND INTERPOLATE LANGUAGE — FORTRAN 
COMPUTER -— IBM 1130 


EDITS» AVERAGES, AND INTERPOLATES STD DATA TO 3-METER INTERVALSe OUT- 
PUT-— SALINITIES AND TEMPERATURES ON CARDS IN CONDENSED FORMAT, AND A 
LISTING OF DISCARDED VALUESe PROGRAM NOs UWMS-11306 


UNIVERSITY OF WASHINGTON 
DEPARTMENT OF OCEANOGRAPHY 

22A OCEANOGRAPHY TEACHING BLDGe 
ATTNe MRSe HELLA MACINTOSH 
SEATTLE» WASHe 98105 


INTERPOLATION LANGUAGE — FORTRAN IV 
COMPUTER — IBM 360/65 


INTERPOLATES TEMPERATURE» SALINITY» OXYGENs PHOSPHATE FOR STANDARD 
DEPTHS» AND DEPTHs TEMPERATURE» SALINITY» OXYGEN» PHOSPHATE FOR STAN- 
DARD SIGMA-T SURFACESe INPUT 1S ICES FORMAT DATAe METHOD USED IS 
MEAN OF TWO LAGRANGE POLYNOMIALS, WITH LINEAR INTERPOLATION AT TOP AND 
BOTTOM OF CASTe CORE STORAGE USED-- 30K BYTESe AUTHOR-— MARILYNN Re 
BORKOWSKI. 


BUREAU OF COMMERCIAL FISHERIES 

TROPICAL ATLANTIC BIOLOGICAL LABORATORY 
75 VIRGINIA BEACH DRIVE 

MIAMI» FLORIDA 33149 


PAGE 086 


INTERPOLATION OF OCEAN STATION DATA AT LANGUAGE — FORTRAN 
ISENTROPIC LEVELS COMPUTER — IBM 7074 AND 
IBM 1620 
(COPY ON FILE AT NODC) 
INTERPOLATES DEPTHs TEMPERATURE» AND SALINITY AT ISENTROPIC LEVELSe 
NUOS (NUWR AND ES) PROGRAM FOR THE I8M 1620 REVISED FOR IBM 7074 BY 
RUDI SAENGERe THERE ARE TWO VERSIONS OF THIS PROGRAM — (1A) STARTING 
AT SIGMA-T OF FIRST DATA CARD COMPUTING 99 LEVELS» (1B) STARTING AT 
SIGMA-T 23200 COMPUTING 50 LEVELSe INPUT CONSISTS OF NODC'S OCEAN 
STATION DATA CARDSe 


COMPUTER SYSTEMS DIVISION 
NATIONAL OCEANOGRAPHIC DATA CENTER 
WASHINGTON» De Ce 20390 


SHIPBOARD SURVEY -- ON-STATION MODE LANGUAGE — FORTRAN 
COMPUTER -— IBM 7074 


PROCESSES MAGNETIC TAPES MADE ON-STATION TO-- (1) GENERATE A MAGNETIC 
TAPE OF SELECTED RECORDED DATA IN NUMERIC FORMAT FOR INPUT TO A PLOT—- 
TER PROGRAM (OS NOe 10131)% (2) COMPUTE SIGMA-Ts» SPECIFIC VOLUME ANOM- 
ALY AND DYNAMIC DEPTH ANOMALY» (3) PRODUCE PRINTER LISTINGS OF THE RE- 
CORDED DATA AND THE CORRESPONDING COMPUTED VALUES» USED IN SELECTING 
STATIONS FOR WHICH DATA IS TO BE PLOTTEDe OS NOe 101322e AUTHOR-- GAY 
Me BROOKe 


NAVIGATIONAL SCIENCE, CODE 5320 
NAVAL OCEANOGRAPHIC OFFICE 
SUITLAND» MDe 20390 


OCEANOGRAPHIC DATA PROGRAM F LANGUAGE -— FORTRAN Iv 
COMPUTER -— IBM 7094 
(COPY ON FILE AT NODC) 

LAGRANGIAN INTERPOLATIONS AT STANDARD DEPTHS AND COMPUTATION OF SUCH 
OCEANOGRAPHIC QUANTITIES AS DYNAMIC HEIGHT» THERMOSTERIC ANOMALY» SIG— 
MA-T» SOUND VELOCITY» ETCe ORIGINAL PROGRAM FOR THE IBM 650 BY KILMER 
AND DUXBURY» 1959s FOR INTERPOLATION AND CALCULATION OF DYNAMIC HEIGHT 
(TEXAS Ae AND Me TECHe REPORT NOe 59-24T)s REVISED NOV 1962 BY NOWLINe 
EACH STATION REQUIRES HEADER CARDS TO SPECIFY THE ARRANGEMENT OF THE 
PRINTED OUTPUT AND FOR ADDITIONAL INFORMATIONe 


TEXAS A AND M UNIVERSITY 
COLLEGE OF GEOSCIENCES 
DEPARTMENT OF OCEANOGRAPHY 
COLLEGE STATIONs TEXAS 77843 


SIGMAT LANGUAGE — FORTRAN IV-E 
COMPUTER - IBM 360/50 


CALCULATES SIGMA-Ts DELTA» DELTA-T»s POTENTIAL TEMPERATURE, POTENTIAL 
SIGMA-Ts AND POTENTIAL DELTA AT OBSERVED DEPTHSe THE CALCULATION OF 
POTENTIAL TEMPERATURE IS AN APPROXIMATION SINCE DEPTH IS USED INSTEAD 
OF PRESSUREe FORMULA USED FOR POTENTIAL TEMPERATURE IS THAT OF 
FOFONOFF AND FROESE (1958)e CALCULATION OF OTHER QUANTITIES IS 

THE SAME AS IN SUBROUTINE 'SIGMA't. 

SUBROUTINES NEEDED-- SIGMA. 


ROBERT Ke SEXTON 


NARRAGANSETT MARINE LABORATORY 
UNIVERSITY OF RHODE ISLAND 
KINGSTON» RHODE ISLAND 02881 


HEIGHT LANGUAGE - FORTRAN IV-E 
COMPUTER - I8M 360/50 


PAGE 087 


INTE 


AZIZ 


LINT 


DELI 


UTILIZES OUTPUT FROM PROGRAM 'CARDS!* TO CALCULATE DYNAMIC HEIGHTS, 
GEOSTROPHIC VELOCITIES» TRANSPORTS» AND DELTA VALUES INTERPOLATED AT 
STANDARD DEPTHS, AS WELL AS POTENTIAL DELTAs AND SIGMA-T AT OBSERVED 
DEPTHSe CAN ALSO YIELD PUNCHED OUTPUT FOR INPUT TO A PLOTTER ROUTINE. 
SUBROUTINES NEEDED-- SPEWIT, VEL, MSTRCDs» VTR»s PDENs EXTIME»s SIGMA» 
LAINTs DYNHTs HOLESe 


ROBERT Ke SEXTON 

NARRAGANSETT MARINE LABORATORY 
UNIVERSITY OF RHODE ISLAND 
KINGSTON» RHODE ISLAND 02881 


ST LANGUAGE — FORTRAN IV-E 
COMPUTER - IBM 360/50 


GIVEN SERIAL OBSERVATIONS OF TEMPERATUREs SALINITY AND DEPTHs IT COM- 
PUTES DELTA AT OBSERVED DEPTHS AND CREATES AN ARRAY '#ZSTD' OF STANDARD 
DEPTHS EVERY 20 M TO 100 Ms EVERY 100 M TO 800 Ms AND EVERY 200 M 
THEREAFTER s AND A CORRESPONDING ARRAY *t*SUMDEL' CONTAINING A NUMERICAL 
INTEGRATION OF DELTA WITH DEPTH»: IN DYNAMIC CENTIMETERS. 

SUBROUTINES-— SIGMAD, DELINT. 


ROBERT Ke SEXTON 

NARRAGANSETT MARINE LABORATORY 
UNIVERSITY OF RHODE ISLAND 
KINGSTONs RHODE ISLAND 02881 


LANGUAGE - FORTRAN IV-E 
COMPUTER — IBM 360/50 


SUBROUTINE COMPUTES THERMOMETRIC DEPTH FROM CORRECTED PROTECTED AND 
UNPROTECTED THERMOMETER READINGSe AN ESTIMATE OF DEPTH IS OBTAINED BY 
TAKING 100 TIMES THE DIFFERENCE IN UNPROTECTED AND PROTECTED THERMOM— 
ETER READINGSe THIS ESTIMATE IS USED TO CALCULATE A FIRST VALUE FOR 
MEAN DENSITY» RHOs USING AN EQUATION FROM A POLYNOMIAL FIT OF WUST'S 
DATA OF MEAN DENSITY WITH DEPTH IN THE NORTH ATLANTIC ('THERMOMETRIC 
MEASUREMENT OF DEPTH! BY Ge WUSTs IN THE HYDROGRAPHIC REVIEW 105 1933, 
TABLE 1» PAGE 34)-e THIS DENSITY IS USED IN THE EXPRESSION D (METERS) 
EQUALS (TU-TW/Q * RHO) TO CALCULATE DEPTHe THIS DEPTH IS USEV TO RE- 
CALCULATE THE MEAN DENSITY» RHO» AND THE LAST TWO STEPS ITERATED UNTIL 
SUCCESSIVE CALCULATIONS AGREE TO WITHIN Oe25 METERS. 


ROBERT Ke SEXTON 

NARRAGANSETT MARINE LABORATORY 
UNIVERSITY OF RHODE ISLAND 
KINGSTON» RHODE ISLAND 02881 


LANGUAGE — FORTRAN IV-E 
COMPUTER -— IBM 360/50 


SUBROUTINE PROVIDES LINEAR INTERPOLATION OF AN X VALUE FOR THE GIVEN Y 
VALUEs IF Y IS OUTSIDE THE LIMITS OF THE Y AXIS» THE CORRESPONDING X 
END POINT VALUE IS USED, AND THE MESSAGE INDICATOR IS SET TO SHOW 
THISe 


ROBERT Ke SEXTON 

NARRAGANSETT MARINE LABORATORY 
UNIVERSITY OF RHODE ISLAND 
KINGSTONs RHODE ISLAND 02881 


NT LANGUAGE — FORTRAN IV-E 
COMPUTER - IBM 360/50 
GIVEN OBSERVED DEPTHs TEMPERATURE AND SALINITY, STANDARD DEPTHS ARE 
GENERATED AND PLACED IN THE ARRAY BETWEEN THE OBSERVED DEPTHSe IT 
CALCULATES DELTA FOR OBSERVED DEPTHS AND INTERPOLATES DELTAS FOR 


PAGE 088 


STANDARD DEPTHS. 
SUBROUTINES NEEDED-- SIGMAD. 


ROBERT Ke SEXTON 

NARRAGANSETT MARINE LABORATORY 
UNIVERSITY OF RHODE ISLAND 
KINGSTONs RHODE ISLAND 02881 


SIGMA LANGUAGE -— FORTRAN IV-E 
COMPUTER -— IBM 360/50 


SUBROUTINE CALCULATES SIGMA-Ts DELTA» IN SITU SPECIFIC VOLUME AND 
STANDARD WATER COLUMN SPECIFIC VOLUME FROM THE GIVEN CHLORINITYs TEM— 
PERATURE AND DEPTHe THE EQUATIONS USED ARE THOSE CITED BY FOFONOFF IN 
"THE SEA'» VOLe ls INTERSCIENCE PUBLISHER s NeYeos 19625 MeNe HILL» EDes 
USING EQUATION (21)» PAGE 8, TO COMPUTE SIGMA ZERO, EQUATION (22) AND 
THE QUANTITIES FOLLOWING EQUATION (24) TO COMPUTE SIGMA-T, AND USING 
EQUATION (25) AND (26)s PAGE 10s TO COMPUTE SPECIFIC VOLUME. 


ROBERT Ke SEXTON 

NARRAGANSETT MARINE LABORATORY 
UNIVERSITY OF RHODE ISLAND 
KINGSTONs RHODE ISLAND 02881 


SIGMAD LANGUAGE -— FORTRAN IV-E 
COMPUTER - IBM 360/50 


DOUBLE PRECISION VERSION OF 'SIGMA'. 


ROBERT Ke SEXTON 

NARRAGANSETT MARINE LABORATORY 
UNIVERSITY OF RHODE ISLAND 
KINGSTON» RHODE ISLAND 02881 


DYNHT LANGUAGE — FORTRAN II 
COMPUTER — GE 225 


COMPUTES AN ARRAY OF DYNAMIC HEIGHTS (EXPRESSED IN DYNAMIC METERS) FOR 
SPECIFIED ARRAYS OF PRESSURE AND SPECIFIC VOLUME ANOMALIESe AUTHOR-- 
JACQUELINE WEBSTER. 


INFORMATION PROCESSING CENTER 
WOODS HOLE OCEANOGRAPHIC INSTITUTION 
WOODS HOLEs MASSe 02543 


PEN LANGUAGE — FORTRAN II 
COMPUTER - GE 225 


COMPUTES POTENTIAL ENERGY ANOMALY» USING THE TRAPEZOIDAL RULE OF INTE- 
GRATIONe PEN SUBROUTINE OCCUPIES 130(8) OR 88(10) LOCATIONS IN MEMO- 
RYe AUTHOR-- -JACQUELINE WEBSTER. 


INFORMATION PROCESSING CENTER 
WOODS HOLE OCEANOGRAPHIC INSTITUTION 


WOODS HOLE» MASSe 02543 


VFREQ LANGUAGE — FORTRAN II 
COMPUTER — GE 225 


COMPUTES TABLES OF VAISALA FREQUENCY (RADIANS/SECe) AND IN SITU DENS— 
ITY (GRAMS/CCe)s GIVEN TABLES OF DEPTH» TEMPERATURE» AND SALINITY AND 
THE LATITUDE OF OBSERVATIONe AUTHOR-— He PERKINSe 


INFORMATION PROCESSING CENTER 
WOODS HOLE OCEANOGRAPHIC INSTITUTION 


PAGE 089 


WOODS HOLEs MASSe 02543 


DYNAMIC HEIGHT CALCULATION LANGUAGE — FORTRAN II 


COMPUTER — IBM 1620 


INTEGRATES ONE STATION AT A TIME AND THEN PUNCHES THE VALUES IN ORDERe 
THERE IS AN OPTION» UNDER SENSE SWITCH CONTROL,» OF USING THE CALCOMP 
560 TO PLOT THE VALUE OF DYNAMIC HEIGHT AGAINST DEPTHe THE INPUT TO 
THIS PROGRAM IS THE SAME AS THAT FOR THE OCEANOGRAPHIC DATA PROCESSING 
PROGRAM FOR THE IeCeEeSe FORMAT 


UNIVERSITY OF MIAMI 

MARINE LABORATORY 

COMPUTER CENTER 

1 RICKENBACKER CAUSEWAY 
VIRGINIA KEY» MIAMI» FLORIDA 


OCEANOGRAPHIC DATA COMPUTATION LANGUAGE —- FORTRAN II 


SEA 


COMPUTER — IBM 709 AND 
CDC 6400 


COMPUTES SALINITY AND SIGMA-T FROM CHLORINITY AND TEMPERATURE INPUT 
DATAs AND COMPUTES DISSOLVED OXYGEN AND OXYGEN SATURATION. 


DEPARTMENT OF GEOLOGY 
FLORIDA STATE UNIVERSITY 
TALLAHASSEEs FLORIDA 32306 


WATER DENSITY -—- THERMOSTERIC ANOMALY LANGUAGE - FORTRAN II 
COMPUTER -— IBM 7094 


SUBROUTINE COMPUTES SIGMA-T AND DELTA-T FROM MEASUREMENTS OF TEMPERA- 
TURE AND CHLORINITYe SIGMA-T IS CALCULATED BY THE METHOD OF KNUDSEN. 
DELTA-T IS COMPUTED BY DEFINITION FROM SIGMA-Te 


HARVEY Ee WALTERS 

CHESAPEAKE BAY INSTITUTE 

THE JOHNS HOPKINS UNIVERSITY 
CHARLES AND 34TH STe 
BALTIMORE» MDe 21218 


SYNOPTIC PROGRAM (UWMS-0980) LANGUAGE —- FORTRAN II 


COMPUTER - IBM 7094-II/ 
7040 DCS AND 
CDC 6400 


(COPY ON FILE AT NODC) 


REDUCES DATA FROM RAW SHIP-BOARD OBSERVATIONSe CORRECTS THERMOMETERS 
AND COMPUTES THERMOMETRIC DEPTHS, WIRE ANGLE DEPTHS», SALINITIES FROM 
BRIDGE READINGS» OXYGEN VALUES FROM TITRATIONSs THEN COMPUTES SIGMA-Ts 
OXYGEN SATURATION PERCENT» AND APPARENT OXYGEN UTILUZATIONe CORE STO- 
RAGE REQUIRED-- 255335 WORDS FOR MAIN PROGRAM» 2058 WORDS FOR SUBROUT-— 
INESe REFe A 150 PAGE REPORT (UWMS-0980, APR 1967) AND TECHNICAL RE- 
PORT NOs 181 (M67-85 JAN 1968)» BY EUGENE Ee COLLIASe THERE IS ALSO 

A MORE LIMITED VERSION FOR THE IBM-11305 REVISED 1969 FOR THE CDC- 
64006 


He MACINTOSH, COMPUTER SERVICES 
DEPARTMENT OF OCEANOGRAPHY 
UNIVERSITY OF WASHINGTON 
SEATTLE, WASH. 98105 


INTERPOLATION PROGRAM (UWMS-0959) LANGUAGE — FORTRAN Iv 


COMPUTER — CDC 6400 
INTERPOLATES HYDROGRAPHIC DATA TO STANDARD DEPTHSs AND COMPUTES THE 


PAGE 090 


DYNAMIC QUANTITIESe THE INTERPOLATION METHOD TAKES AN AVERAGE OF THE 
POINTS OBTAINED FROM TWO PARABOLIC FITS» CORE STORAGE NEEDED-- 32 K 
WORDSe DOCUMENTATION-— USAGE INSTRUCTIONS» AN OLDER UNIVERSITY OF 
WASHINGTON PROGRAM INTERPOLATION FOR OFFSHORE OCEANOGRAPHIC DATA'»s IN 
FORTRAN IV FOR THE IBM 7094, IS IN THE LIBRARY FILE AT THE NODCe THIS 
INTERPOLATES OCEAN STATION VARIABLES TO STANDARD DEPTHSs USING LA- 
GRANGE SUBROUTINE, CALCULATES ERROR TERMS FOR INTERPOLATIONSs COMPUTES 
SIGMA-T» SPECIFIC VOLUME ANOMALYs DYNAMIC DEPTHs AND POTENTIAL ENERGY. 
THE DECK HAS ABOUT 1500 CARDS» INCLUDING TWO FAP SUBROUTINES AND A BI- 
NARY EDITOR PROGRAMe 


UNIVERSITY OF WASHINGTON 
DEPARTMENT OF OCEANOGRAPHY 

22A OCEANOGRAPHY TEACHING BLDGe 
ATTNe MRSe HELLA MACINTOSH 
SEATTLE» WASHe 98105 


OCEANOGRAPHIC REPORT PREPARATION LANGUAGE — FORTRAN IV 
COMPUTER - IBM 360/65 


INCLUDES CALCULATION OF SIGMA-T AND SPECIFIC VOLUME ANOMALY FOR OB- 
SERVED POINTS» RATTRAY-TYPE LAGRANGE INTERPOLATION AND DYNAMIC DEPTH 
CALCULATION AT STANDARD DEPTHS. 


BUREAU OF COMMERCIAL FISHERIES BIOLOGICAL LABeo 
ATTNe DRe Re Ae BARKLEY 

PeO5o BOX 3830 

HONOLULU» HAWAII 96812 


OCCOMP LANGUAGE —- FORTRAN IV-H 
COMPUTER - SDS SIGMA 7 


COMPUTES VARIOUS OCEANOGRAPHIC PARAMETERS FROM NODC FORMAT STATION DA- 
TA CARDSe OUTPUT IS ON LINE PRINTERe PROGRAM REQUIRES CORE STORAGE 
OF 12752 WORDS. 


INFORMATION PROCESSING CENTER 

ATTNe MARY HUNT 

WOODS HOLE OCEANOGRAPHIC INSTITUTION 
WOODS HOLEs MASSACHUSETTS 02543 


POTEMPs DPOTEM LANGUAGE - FORTRAN IV-H 
COMPUTER -— SDS SIGMA 7 
(COPY ON FILE AT NODC) 

SUBROTUINE COMPUTES THE POTENTIAL TEMPERATURE OF SEA WATER AT A GIVEN 
TEMPERATURE» SALINITY AND PRESSURE USING A FORMULA OF NePe FOFONOFF 
AND Ce FROESE IN THE PeOQeGe MS REPORT SERIES NOe 27e WRITTEN IN FOR- 
TRAN II FOR THE GE 225 BY Je WEBSTERe CONVERTED TO FORTRAN IV-H BY 
Me HUNT (APRIL 1968)e DPOTEM IS A FORM OF POTEMP USING DOUBLE PRECIS-— 
ION VARIABLES» STORAGE REQUIREMENTS—- 137(10) LOCATIONS FOR POTEMP>s 
116(10) LOCATIONS FOR DPOTEMe 


INFORMATION PROCESSING CENTER 

ATTNe MARY HUNT 

WOODS HOLE OCEANOGRAPHIC INSTITUTION 
WOODS HOLEs MASSACHUSETTS 02543 


SIGMAT»s DSIGMT LANGUAGE -— FORTRAN IV-H 
COMPUTER - SDS SIGMA 7 
SUBROUTINE COMPUTES SIGMA-T FROM TEMPERATURE AND SALINITY BY KNUDSEN#S 


FORMULA REWRITTEN BY FOFONOFF AND TABATAs DSIGMT IS DOUBLE-PRECISION 
FORM OF SIGMATe 


INFORMATION PROCESSING CENTER 
ATTNe MARY HUNT 


PAGE O91 


WOODS HOLE OCEANOGRAPHIC INSTITUTION 
WOODS HOLEs MASSACHUSETTS 02543 


SPVOL» DSPVOL LANGUAGE - FORTRAN IV-H 
COMPUTER -— SDS SIGMA 7 


SUBROUTINE COMPUTES THE SPECIFIC VOLUME OF SEAWATER AT A GIVEN TEMPER- 
ATURE» PRESSURE» SIGMA-O AND SIGMA-Ts USING THE FORMULA BY VeWe EKMANs 
REWRITTEN BY FOFONOFF AND TABALA (PeQ+eGe MANUSCRIPT SERIES NOe 25)¢ 
DSPVOL IS A FORM OF SPVOL USING DOUBLE-PRECISION VARIABLESe 'tALPHA',s 
THE OUTPUT FROM THE SUBROUTINE» IS THE SPECIFIC VOLUME IN MILLILITRES 
PER GRAM. THE USE OF SUBROUTINE SIGMAT WOULD BE REQUIRED BEFORE CALL- 
ING SPVOL»s AND DSIGMT WOULD BE REQUIRED BEFORE CALLING DSPVOLe STOR- 
AGE REQUIREMENTS—-- 239(10) LOCATIONS FOR SPVOLs 204(10) LOCATIONS FOR 
DSPVOLe WRITTEN IN FORTRAN II FOR THE GE 225 BY Je WEBSTER» CONVERTED 
TO FORTRAN IV-H BY Me HUNT (APRIL 1968).e 


INFORMATION PROCESSING CENTER 

ATTNe MARY HUNT 

WOODS HOLE OCEANOGRAPHIC INSTITUTION 
WOODS HOLE, MASSACHUSETTS 02543 


ATG LANGUAGE -— FORTRAN IV-H 
COMPUTER - SDS SIGMA 7 


CALCULATES ADIABATIC TEMPERATURE GRADIENT FOR SPECIFIED VALUES OF 
PRESSUREs TEMPERATURE» AND SALINITY,» USING AN EMPIRICAL FORMULA DEVEL— 
OPED BY NePe FOFONOFFe (PROGRAM WRITTEN AS SUBROUTINE e) 


INFORMATION PROCESSING CENTER 

ATTNe MARY HUNT 

WOODS HOLE OCEANOGRAPHIC INSTITUTION 
WOODS HOLE», MASSACHUSETTS 02543 


FORTRAN IV-H 
SDS SIGMA 7 


DSTABF LANGUAGE 
COMPUTER 


SUBROUTINE COMPUTES STABILITY FREQUENCY FROM HYDROGRAPHIC STATION DA- 
TAs ACCORDING TO A RELATIONSHIP DERIVED BY HESSELBERG AND SVERDRUPe 


INFORMATION PROCESSING CENTER 

ATTNe MARY HUNT 

WOODS HOLE OCEANOGRAPHIC INSTITUTION 
WOODS HOLE, MASSACHUSETTS 02543 


SVANOM LANGUAGE - FORTRAN IV-H 
COMPUTER - SDS SIGMA 7 


SUBROUTINE COMPUTES THE SPECIFIC VOLUME ANOMALY, GIVEN THE PRESSURE 
AND THE SPECIFIC VOLUME, FROM AN EMPIRICAL FORMULA DEVISED By FOFONOFF 


AND TABATA. 


INFORMATION PROCESSING CENTER 

ATTNe MARY HUNT 

WOODS HOLE OCEANOGRAPHIC INSTITUTION 
WOODS HOLEs MASSACHUSETTS 02543 


PRESS LANGUAGE -— FORTRAN IV-H 
COMPUTER — SDS SIGMA 7 


SUBROUTINE COMPUTES A SERIES OF PRESSURES FROM A GIVEN SERIES OF 


DEPTHS» TEMPERATURES» SALINITIES, AND THEIR LATITUDEe THE EQUATION 
FOR PRESSURE IS INTEGRATED BY SUCCESSIVE APPROXIMATIONS e 


PAGE 092 


INFORMATION PROCESSING CENTER 

ATTNe MARY HUNT 

WOODS HOLE OCEANOGRAPHIC INSTITUTION 
WOODS HOLE, MASSACHUSETTS 02543 


DELTA-ALPHA AND SIGMA-T LANGUAGE -— MAC 
GOMP.UTERG—) Gi S130 


CALCULATES DELTA-ALPHA AND SIGMA-T AS A FUNCTION OF SALINITY» TEMPERA-— 
TUREs AND DEPTHe AUTHORS-- AeMe SHIPLEY AND De SACKS 


UNIVERSITY OF CAPE TOWN 
OCEANOGRAPHY DEPARTMENT 

ATTNe MRe AeMe SHIPLEY 
PRIVATE BAGs RONDEBOSCH»s CePe 
REPUBLIC OF SOUTH AFRICA 


DYNAMIC HEIGHT AND CURRENT DYNAMICS LANGUAGE — MAD 
COMPUTER - IBM 7090 


COMPUTES DYNAMIC HEIGHT,» VOLUME TRANSPORT» AND NORMAL VELOCITY FOR 
FRESH WATERe 


VINCENT NOBLE 

THE UNIVERSITY OF MICHIGAN 

GREAT LAKES RESEARCH DIVISION 
INSTITUTE OF SCIENCE AND TECHNOLOGY 
1077 NORTH UNIVERSITY BUILDING 

ANN ARBOR» MICHIGAN 48104 


OCEANOGRAPHIC ANALYSIS AND STATION SUMMARY LANGUAGE — PAL ITI 
GOMEUTERT— PDS Songs) 


FORMATS AND RECORDS OCEANOGRAPHIC DATA INCLUDING SURFACE ENVIRONMENTAL 
PHENOMENA, COMPUTES SIGMA-T, THE ANOMALY OF SPECIFIC VOLUME» AND SOUND 
VELOCITY AT OBSERVED VALUES OF DEPTH-TEMPERATURE-SALINITYe COMPUTES 
SIGMA-T AND ANOMALY OF SPECIFIC VOLUME FROM SCALED VALUES OF TEMPERA-— 
TURE AND SALINITY» THE RESULTS OF A LAGRANGIAN INTERPOLATIONe DOES A 
DEPTH INTEGRATION OF ANOMALY OF SPECIFIC VOLUME FROM THE OBSERVED OR 
SCALED VALUES IN ORDER TO CALCULATE THE DYNAMIC HEIGHT FROM A LEVEL OF 
NO-MOTIONe PRINCIPALLY USED ABOARD OCEANOGRAPHIC VESSEL BY THE FIELD 
OCEANOGRAPHER IMMEDIATELY AFTER STATIONe WRITTEN FOR THE UeSe COAST 
GUARD BY LTe ReMe O'HAGAN (RETe)s DIGITAL EQUIPMENT CORPe,s MAYNARD» 
MASSe COPY OF PROGRAM DEPOSITED WITH DECUSe REFe UeSe COAST GUARD 
OCEANOGRAPHIC MANUSCRIPT 'OCEANOGRAPHIC COMPUTER PROGRAMS FOR THE PDP- 
5's 15 OCT. 1964 (UNPUBLISHED MANUSCRIPT)e« PROGRAM REVISED IN 19656 


DIGITAL EQUIPMENT CORPORATION 
MAYNARD» MASSACHUSETTS 01754 


DISSOLVED OXYGEN AND POTENTIAL TEMPERATURE LANGUAGE - PAL III 
COMPUTER -— PDP-5»5 8S 


CALCULATES DISSOLVED OXYGEN FROM A GIVEN THIOSULPHATE TITERe CALCUL— 
ATES PERCENT SATURATION OF OXYGEN (FOX'S FORMULAE)» CALCULATES POTEN- 
TIAL TEMPERATUREe ASR-33 TELEPRINTER INPUT-OUTPUTe PROGRAM PRINCI- 
PALLY USED ABOARD OCEANOGRAPHIC VESSELe WRITTEN FOR THE UeSe COAST 
GUARD BY LTe ReMe O'HAGAN (RETe)» DIGITAL EQUIPMENT CORPes MAYNARD» 
MASSe COPY DEPOSITED WITH DECUS. 


DIGITAL EQUIPMENT CORPORATION 
MAYNARDs MASSACHUSETTS 01754 
OCEAN STATION COMPUTATIONS LANGUAGE — (NOT GIVEN) 
COMPUTER - CDC 1604 


PAGE 093 


INTERPOLATION AT STANDARD DEPTHS OF TEMPERATURE AND SALINITYs SIGMA-T 
AND THE DYNAMICS COMPUTATIONSe» 


SCRIPPS INSTITUTION OF OCEANOGRAPHY 
LA JOLLA» CALIFORNIA 92037 


RADIATION ATTENUATION LANGUAGE — (NOT GIVEN) 
COMPUTER — CDC 1604 


COMPUTATION OF THE ATTENUATION COEFFICIENTS FROM SUBMARINE IRRADIANCE 
MEASUREMENTS. 


SCRIPPS INSTITUTION OF OCEANOGRAPHY 
LA JOLLA» CALIFORNIA 92037 


#-%-% SOUND — RAY PATH *-*-—* 


ACOUSTIC RAY TRACING LANGUAGE — FORTRAN II 
COMPUTER -— IBM 7090 
(COPY ON FILE AT NODC) 

CALCULATES UNDERWATER SOUND PROPAGATIONe PROGRAM REQUIRES INPUT WHICH 
DESCRIBES THE SOURCEs THE FIELD» THE SURFACE AND THE BOTTOMe OUTPUT 
IS A REPORT ON MAGNETIC TAPE WHICH GIVES RAY PATHs SLOPE» CURVATURE9s 
AND LENGTH. ALSO GIVEN ARE REFLECTION AND EXTREMA STATISTICS» TRAVEL 
TIMEs WAVE FRONT CURVATUREs AND INTENSITYe PROGRAM AND DOCUMENTATION 
PUBLISHED IN ARTHUR De LITTLE» INCe TECHNICAL REPORT NOco 1470764e THE 
AeDe NOe IS AD 605 328e ALSO AVAILABLE FROM THE DEFENSE DOCUMENTATION 
CENTERe 


MISS MARIAN Le HOBBSs LIBRARIAN 
TRIDENT/ASW LIBRARY 

ARTHUR De LITTLE s INCeo 

35 ACORN PARK 

CAMBRIDGE» MASS. 02140 


TRLOSS LANGUAGE — FORTRAN 
COMPUTER -— CDC 6600 


COMPUTES LONG-RANGE TRANSMISSION LOSS BY PROBABILISTIC METHODS, USING 
A STATISTICAL APPROXIMATION TO RAY-TRACINGe INPUT-- PUNCHED CARDS 
CONTAINING VELOCITY PROFILES» BOTTOMs TOPOGRAPHY (ROUGH) AND TARGET 
RANGES» OUTPUT-- LISTS OF INTENSITIES (RELATIVE TO SOURCE INTENSITY) 
AS FUNCTIONS OF DEPTH AT EACH OF THE TARGET RANGESe CORE STORAGE NEC-— 
ESSARY-- 30(8)K WORDSe AUTHOR-- MISS ELLEN WILLIAMS. 


MARTIAN Le HOBBS» LIBRARIAN 
ARTHUR De LITTLE» INC 

ACORN PARK 

CAMBRIDGEs MASSe 02140 


SONAR IN REFRACTIVE WATER LANGUAGE -— FORTRAN IV 
COMPUTER — UNIVAC 1108 
(COPY ON FILE AT NODC) 
TRACES SOUND RAYS» COMPUTES REVERBERATION, COMPUTES ACQUISITION LAMIN- 
AE (VERTICAL PLANE)» IN A LINEAR-GRADIENT OR CONTINUOUS-GRADIENT MEDI- 
UMe CORE STORAGE USED-- APPROXe 30,000 WORDSe SUPERSEDES ALL PREVI- 
OUS VERSIONS OF THE PROGRAM. DOCUMENTED AS NUC TECHNICAL PUBLICATION 
NOs 164 (VOLel» 196 P AND VOLe2s 356 P) 'DIGITAL COMPUTER PROGRAMS FOR 
ANALYZING ACOUSTIC SEARCH PERFORMANCE IN REFRACTIVE WATERS'» NUC PRO- 
GRAMS 800000 AND 800001, BY PHILIP MARSH AND AeBe POYNTER» ORUVNANCE 
SYSTEMS DEPARTMENT, DECEMBER 1969-6 (DOCUMENTS UNCLASSIFIED BUT TRANS- 


PAGE 094 


MITTALS CONTROLLED BY NUCe) 


NAVAL UNDERSEA RESEARCH AND DEVELOPMENT CENTER 
PASADENA LABORATORY 

ATTNe PHILIP MARSH 

3202 Ee FOOTHILL BLVD. 

PASADENA» CALIFe 91107 


RAY SORT LANGUAGE - FORTRAN IV 
COMPUTER - UNIVAC 1108 
(COPY ON FILE AT NODC) 

SORTS CERTAIN SOUND RAY DATA (FROM TAPE WRITTEN BY THE 'SONAR IN RE- 
FRACTIVE WATER* PROGRAM) BY DEPTHs INITIAL RAY ANGLE, AND DEPTH-INTER- 
SECTION NUMBERe SOURCE PROGRAM HAS 450 INSTRUCTIONSe CORE STORAGE-- 
ABOUT 312000 WORDSe DOCUMENTED AS NUC TECHNICAL PUBLICATION NOo 164 
(VOLel» 196 P AND VOLe2, 356 P) *DIGITAL COMPUTER PROGRAMS FOR ANALY— 
ZING ACOUSTIC SEARCH PERFORMANCE IN REFRACTIVE WATERS» NUC PROGRAMS 
800000 AND 800001, BY PHILIP MARSH AND AeBe POYNTERs ORDNANCE SYSTEMS 
DEPARTMENT» DECEMBER 1969¢ (DOCUMENTS UNCLASSIFIED BUT TRANSMITTAIS 
CONTROLLED BY NUCe) 


NAVAL UNDERSEA RESEARCH AND DEVELOPMENT CENTER 
PASADENA LABORATORY 

ATTNe PHILIP MARSH 

3202 Ee FOOTHILL BLVDe 

PASADENAs CALIFe 91107 


RAYMOR LANGUAGE — FORTRAN V 
COMPUTER - UNIVAC 1108 
(COPY ON FILE AT NODC) 
COMPUTES RAYLEIGH-MORSE BOTTOM REFLECTION COEFFICIENTS» ALSO PHASE 
CHANGES OF THE REFLECTED AND TRANSMITTED ACOUSTIC WAVEe AUTHOR-- 
JeCe REEVES. 


NAVAL UNDERSEA RESEARCH AND DEVELOPMENT CENTER 
PASADENA LABORATORY 

3202 Ee FOOTHILL BOULEVARD 

PASADENAs CALIFORNIA 91107 


NEWFIT LANGUAGE - FORTRAN V 
COMPUTER — UNIVAC 1108 
(COPY ON FILE AT NODC) 

FITS A VELOCITY PROFILE WITH A SERIES OF CURVE SEGMENTS HAVING CONTIN- 
UOUS FIRST DERIVATIVES AT POINTS OF INTERSECTIONe OUTPUT-= PRINTED 
LISTINGS OF ORIGINAL DATAs FITTED DATAs AND COEFFICIENTS OF CURVE SEG- 
MENTS —- ALSO CARDS FOR INPUT TO *#SONAR IN REFRACTIVE WATER! PROGRAMe 
NEWFIT IS THE MAIN ROUTINE OF THE NEW CURVE FITTING PROGRAMe A REPORT 
AP-PROG-C-8070 (FEB 19685 98 P)» BY MELVIN Oe BROWNs DOCUMENTS THE DE- 
TAILS OF THE ENTIRE PROGRAMe CORE STORAGE NECESSARY-- APPROXe 253000 
WORDSs INCLUDING LIBRARY AND SYSTEM ROUTINES. 


NAVAL UNDERSEA RESEARCH AND DEVELOPMENT CENTER 
PASADENA LABORATORY 

ATTNe PHILIP MARSH 

3202 Ee FOOTHILL BLVDe 

PASADENA» CALIFe 91107 


PATTERN FUNCTION CALCULATIONS LANGUAGE -— FORTRAN IV 
COMPUTER - UNIVAC 1108 
(COPY ON FILE AT NODC) 
COMPUTES TRANSDUCER PATTERN FUNCTIONS NEEDED IN THE SONAR EQUATIONS 
WHEN ESTIMATING SEARCH PERFORMANCE OF ACOUSTIC TORPEDOESe THE DESIRED 
PARAMETERS INCLUDE THE TRANSMIT AND RECEIVE DIRECTIVITY INDEXES AND 
THE VOLUME AND BOUNDARY REVERBERATION INDEXESe IN A VEHICLE EMPLOYED 
IN CIRCULAR SEARCHs THE REVERBERATION INDEXES ARE FUNCTIONS OF TURN 
RATE AND ELAPSED TIME IN THE PING CYCLEe THE OUTPUT IS USED BY THE 


PAGE 095 


‘SONAR IN REFRACTIVE WATER! PROGRAMe THEORYs FLOW CHARTS» AND LISTING 
GIVEN IN REPORT AP-PROG-C-7035 (APR 19675 80 P)s BY HERBERT Se KAPLANe 


NAVAL UNDERSEA RESEARCH AND DEVELOPMENT CENTER 
PASADENA LABORATORY 

ATTNe PHILIP MARSH 

3202 E5s FOOTHILL BLVDe 

PASADENA» CALIFe 91107 


HORIZONTAL GRADIENT RAY TRACING LANGUAGE - FORTRAN-63 


RAY 


COMPUTER - CDC 3800 


DESCRIBES ACOUSTIC PATHS OF UP TO 1000 RAYS AS THEY PROGRESS THROUGH 
THE OCEAN FROM A POINT SOURCE AT ARBITRARY RANGE AND DEPTHe ALL RAYS 
ARE TRACED SIMULTANEOUSLY IN ONE PASS THROUGH THE VELOCITY FIELDe AS 
THE RAYS ARE TRACED SEVERAL TYPES OF INTENSITY CALCULATIONS ARE PER- 
FORMED AND A MULTIPLOT OF RAYS CONSTRUCTEDe BASIC INPUT CONSISTS OF A 
MAGNETIC TAPE GENERATED BY THE 'GENERAL VELOCITY FIELD! PROGRAM. OUT- 
PUT--— RANGES» DEPTHSs TRAVEL TIME» SINE OF ANGLE» NUMBER OF TURNING 
POINTS» NUMBER OF SURFACE AND BOTTOM HITS» AND SIGNAL STRENGTH OF EACH 
RAY AT RANGES SPECIFIED BY THE USER. ALSO» TYPE I» II» III INTENSI- 
TIES» TRANSMISSION LOSS AND TRANSMISSION ANOMALYe BASIC IDEAS CON- 
TAINED IN HUDSON LAB TECHNICAL REPORT NOe 150 (1968)+¢ PROGRAM DOCU- 
MENTATION FORTHCOMINGe 


Je Je CORNYN, CODE 8140 
ACOUSTICS DIVISION 

NAVAL RESEARCH LABORATORY 
WASHINGTONs De Ce 20390 


TRACING LANGUAGE - FORTRAN IV 
COMPUTER - CDC 3800 


CALCULATES RAY THEORY» ARRIVALS AND INTENSITIES AT A LARGE NUMBER OF 
RECEIVERSe INPUT-- VELOCITY PROFILE EITHER AS V VSe Z OR T2S VSe Ze 
ALSO SOURCE AND RECEIVER DEPTHS», INITIAL RAY ANGLES AND RECEIVER RAN- 
GES, BEAM PATTERNS (IF ANY), BOTTOM LOSS TABLE, SURFACE LOSSs FREQUEN- 
CYe OUTPUT-- LISTINGS AND PLOTSe EITHER COHERENT OR RANDOM PHASE 
ARRIVAL SUMS ARE AVAILABLEe 


EDWARD Le WRIGHT» CODE 8172 
ACOUSTICS DIVISION 

NAVAL RESEARCH LABORATORY 
WASHINGTONs De Ceo 20390 


ACOUSTIC RAY TRACING LANGUAGE — FORTRAN-63 


RAY 


COMPUTER -— CDC 3800 


CALCULATES PATHS OF ACOUSTIC RAYS FROM A POINT SOURCE IN THE OCEAN? 
THROUGH A SERIES OF SOUND SPEED PROFILES» ALONG WITH THEIR TRAVEL 
TIMES AND TRANSMISSION LOSSESe REFLECTIONS OF THE RAYS FROM A LINEAR 
SEGMENTED BOTTOM ARE CALCULATEDe COMPUTES CLOSED FORM PATH ELEMENTS 
BETWEEN LAYER BOUNDARIES IN THE PROFILEe RAYS ARE TRACED SEQUENTIAL— 
LYe PROGRAM WILL BE DOCUMENTED IN A FORTHCOMING REPORT e 


Ee Be WRIGHT 

CODE 8177s ACOUSTICS DIVISION 
NAVAL RESEARCH LABORATORY 
WASHINGTONs De Ce 20390 


TRACE PROCESSING LANGUAGE -— FORTRAN-63 
COMPUTER -— CDC 3800 


USES OUTPUT OF RAY TRACING PROGRAM TO CALCULATE TRANSMISSION LOSS BY A 
CHOICE OF THREE METHODS. LOSS AT RECEIVERS IS COMFUTED BY-- A) PHASE- 
DEPENDENT RAY SUM, B) RANDOM—PHASE RAY SUMs C) STATISTICAL DISTRIBU- 


PAGE 096 


RAY 


TION OF ARRIVALSe OUTPUT-— TRANSMISSION LOSS AS A FUNCTION OF RANGE 
FOR UP TO 20 RECEIVER DEPTHS AND UP TO 200 RANGE INCREMENTS 


Ee Be WRIGHT 

CODE 8177» ACOUSTICS DIVISION 
NAVAL RESEARCH LABORATORY 
WASHINGTON»s De Ce 20390 


TRACING LANGUAGE - FORTRAN AND 
KLERER-MAY 
USER |ILANGe 

COMPUTER —- (NOT GIVEN) 


(COPY ON FILE AT NODC) 


A SERIES OF PROGRAMS FOR THE CALCULATION OF THE ACOUSTICAL FIELD IN 
LONG-RANGE (SEVERAL HUNDRED TO SEVERAL THOUSAND MILES)» LOW FREQUENCY 
UNDERWATER SOUND PROPAGATION IN THE DEEP OCEANe INVOLVES THE CALCULA- 
TION OF RAY TRAJECTORIESs AND INTENSITY CALCULATIONS THAT ARE BASED ON 
THE MAPPING OF RAY DENSITIES INTO THE FAR ACOUSTICAL FIELDe I/P FOR= 
MAT FROM NODC DATA TAPES OR FLEET. NUMERICAL WEATHER CENTRAL CARDS. 
REFe 'THE HUDSON LABORATORIES RAY TRACING PROGRAM! (JUNE 19689 363 P.) 
AUTHORS-- He DAVISs He FLEMING» WeAe HARDYs Re MININGHAMs AND Se ROS-— 
ENBAUMe 


RAYTR (RAY-TRACING) LANGUAGE -— FORTRAN Iv 


ORD 


ORD 


COMPUTER -— IBM 360/44 


TRACES SOUND RAY PATHS IN A LAYERED FLUID MEDIUMe TRAVEL-TIMES»s REL- 
ATIVE TRAVEL-TIMES» TOTAL PATH LENGTHS ALONG THE RAY, INTENSITIES AND 
THE COORDINATES OF FOCI ARE ALSO COMPUTEDe THE PROGRAM IS SIMILAR IN 
MANY RESPECTS TO HeWe DOSSOs ET AL "RAY TRACING WITH A PB-250'5 TECH. 
MEMOe 63-11 (UNPUBLISHED). THE NUMBER OF ALLOWED SOUND-SPEED vS DEPTH 
AND BOTTOM PROFILE DATA ENTRIES HAS BEEN INCREASED FROM 32 TO 3606 
AUTHOR-- ReWe DE JEANe DESCRIBED IN TECHNICAL MEMO 68-55 FEB 19686 


DEFENCE RESEARCH ESTABLISHMENT PACIFIC 
VICTORIA» Be Ce CANADA 


1 (OLMSTED RAY DIAGRAM PROGRAM NOe 1) LANGUAGE -— FORTRAN 
COMPUTER — GE 225 


CONSTRUCTS (OPTICAL/ACOUSTIC) RAYS IN A MEDIUM WHERE THE VELOCITY OF 
LIGHT/SOUND VARIES CONTINUOUSLY WITH ONE COORDINATE (DEPTH)e THE RAYS 
ARE CONFINED TO A RANGE-DEPTH PLANE OF FINITE DEPTH (A LAYER) AND MUST 
ORIGINATE FROM A SOURCE PLACED AT ANY DEPTH IN THE LAYER AND AT ANGLES 
OF INCIDENCE GREATER THAN O AND LESS THAN 180 DEGe WHEN A RAY REACHES 
A VERTEX (OF REFRACTION OR REFLECTION) THE REMAINDER OF THE RAY IS 
CONSTRUCTED BY SYMMETRY AND PERIODIC EXTENSION. POINTS ARE THEN COM- 
PUTED ALONG THESE RAYS AT INTERVALS OF EQUAL RANGEe AUTHOR-- COERT 
OLMSTED>s FEBe 1965-6 


WOODS HOLE OCEANOGRAPHIC INSTITUTION 
WOODS HOLE» MASSe 02543 


2 (OLMSTED RAY DIAGRAM PROGRAM NOe 2) LANGUAGE - FORTRAN 
GOMPUTERE IGEN 225 


SERVES THE SAME PURPOSE AS ORD 1 EXCEPT THAT THE OUTPUT POINTS ARE AT 
EQUAL TIME INCREMENTS RATHER THAN AT EQUAL RANGE INCREMENTS AND THUS, 
WHEN PLOTTEDs WILL ENABLE ONE TO TRACE WAVE FRONTS AS WELL AS RAYSe 
THERE TS NO SYMMETRICAL OR PERIODIC EXTENSIONe THE RAY PATH IS COM- 
PUTED LOCALLY ALL THE WAY OUT TO MAXIMUM RANGEe AUTHOR-- COERT OLM- 
STEDs FEBe 1965. 


WOODS HOLE OCEANOGRAPHIC INSTITUTION 
WOODS HOLEs MASSe 02543 


PAGE 097 


AN ACOUSTIC MODEL LANGUAGE — FORTRAN 
COMPUTER — IBM 7074 


PRESENTS A SOLUTION FOR THE RAYLEIGH REFLECTION COEFFICIENT WITH A 
FOUR LAYER MODELe OS NOs 20118e¢ AUTHOR-- MeEe MYERS 


COMPUTER DEPARTMENT» CODE 0831 
NAVAL OCEANOGRAPHIC OFFICE 
SUITLAND» MD. 20390 


CRITICAL ACOUSTIC RATIO LANGUAGE — FORTRAN 
COMPUTER -— IBM 7074 


DETERMINATION OF CRITICAL RATIO OF TRIGONOMETRIC FUNCTIONS OF ACOUSTIC 
ANGLES INVOLVED IN CONNECTION WITH THE CONVERGENCE INTERVAL FOR A 3- 
LAYER MODEL OF THE OCEANe OS NOe 534836 AUTHOR-- CeMe WINGER. 


OCEANOGRAPHIC PREDICTION DIVe, CODE 3400 
NAVAL OCEANOGRAPHIC OFFICE 
SUITLANDs MD. 20390 


RAY PATH LANGUAGE - FORTRAN 
COMPUTER -— IBM 7074 
(COPY ON FILE AT NODC) 
COMPUTES RANGES AND TRAVEL TIMES FOR SOUND RAYSe OS NOe 53810¢ AUTHOR 
LeWe CISNEY. 


EXPLORATORY OCEANOGRAPHY DIVes CODE 7200 
NAVAL OCEANOGRAPHIC OFFICE 


SUITLANDs MD. 20390 


BOTTOM REFLECTION ANALYSIS LANGUAGE — FORTRAN 
COMPUTER — IBM 7074 
(COPY ON FILE AT NODC) 
DETERMINES ENERGY LEVEL OF SOUND SOURCES AT CERTAIN DISCRETE FREQUEN- 
CIES BY MEANS OF HARMONIC ANALYSISe OS NOe 538066¢ AUTHOR-- teWe CIS-— 
NEY. 


EXPLORATORY OCEANOGRAPHY DIVe»s CODE 7200 
NAVAL OCEANOGRAPHIC OFFICE 
SUITLAND» MD. 20390 


CONVERGENCE ZONE RANGE LANGUAGE - FORTRAN 
COMPUTER - IBM 7074 
(COPY ON FILE AT NODC) 

COMPUTES RANGES TO THE FIRST CONVERGENCE ZONEe THE WIDTH OF THE 
RESWEPT AND INSONIFIED ZONES AND THE RELIABLE ACOUSTIC PATH RANGE 
ARE ALSO COMPUTED. IN ADDITION: LAYER DEPTHs CHANNEL DEPTH», OPTIMUM 
DEPTHs BOTTOM VELOCITYs AND DEPTH EXCESS ARE EXTRACTED AND LISTED 
IN THE OUTPUT. INPUT EITHER CARD OR TAPE’ OS NOe 53334-¢ (RESTRICTED) 
AUTHOR-— Re BUTTERWORTH. 


OCEANOGRAPHIC ANALYSIS DIVe»s CODE 3300 
NAVAL OCEANOGRAPHIC OFFICE 
SUITLAND>s MD. 20390 


LIGHT AND SOUND INSTRUCTION D LANGUAGE — FORTRAN 
COMPUTER -— IBM 7074 
(COPY ON FILE AT NODC) 
COMPUTES THE CONVERGENCE ZONE PARAMETERS USING THE V(X) METHOUV (EQUA- 
TIONS OF DONALD COLE)» BY ONE-DEGREE QUADRANGLE, BY MONTH AND By SEA- 
SONe AUTHOR-- MeCe CHURCH. 


PAGE 098 


RAY 


COMPUTER DEPARTMENT» CODE 083 
NAVAL OCEANOGRAPHIC OFFICE 
SUITLAND» MDe 20390 


TRACING LANGUAGE - FORTRAN II 
COMPUTER - IBM 704 


(COPY ON FILE AT NODC) 


COMPUTES HORIZONTAL RANGEs TRAVEL TIME» AND SPREADING LOSS THROUGH A 
MEDIUM CONSISTING OF LAYERS OF CONSTANT VELOCITY GRADIENT (THE v(x) 
METHOD OF DONALD COLE)e A PRINTED OUTPUT CONTAINS LAYERED INFORMA- 
TIONe OPTION TO WRITE A PLOTTER TAPE FOR USE ON THE EAI 3440 DIGITAL 
PLOTTERe REFe USL TECHe MEMORANDUM NOco 907-78-66 (APRIL 1966) 


PAULINE ONYX 
NAVY UNDERWATER SOUND LABORATORY:s BLDGe 80 


FORT TRUMBULL» NEW LONDON» CONNe 06320 


BOTTOM REFLECTIVITY LANGUAGE — FORTRAN II 


COMPUTER — IBM 704 


(COPY ON FILE AT NODC) 


TWO 


USL PROGRAM NOe 028956 COMPUTES THREE ACOUSTIC REFLECTION COEFFICIENTS 
AS A FUNCTION OF INCIDENT ANGLE AND FREQUENCYe THE PROGRAM ACCOUNTS 
FOR DIFFERENCE IN PATH LENGTHs DEPTH OF SOURCE AND RECEIVERS» WATER» 
BOTTOM SLOPEs VELOCITY GRADIENT AND RECORDED TRAVEL TIMEs REFe USL 
TECHe MEMORANDUMS NOSe 913-4-65 AND 907-144-65. THE LATTER REPORT 
ALSO SERVES TO DOCUMENT A SUPPLEMENTAL COMPUTER PROGRAM (USL NOe 0427, 
IN FORTRAN) FOR COMPUTING MEANS AND STANDARD DEVIATIONS OF THE THREE 
REFLECTION COEFFICIENTS. 


Re WHITTAKER 
NAVY UNDERWATER SOUND LABORATORY» BLDGe 80 
FORT TRUMBULL» NEW LONDON», CONNe 06320 


DIMENSIONAL RAY TRACE LANGUAGE — SCRAP» MAP 
COMPUTER - CDC 1604 AND 
CDC 3200 


DESCRIBES THE PATH OF SOUND EMITTED FROM A POINT SOURCE AS IT PROGRES- 
SES THROUGH THE OCEAN IN ONE HORIZONTAL DIRECTIONs TAKING INTO CONSID- 
ERATION BOTH HORIZONTAL AND VERTICAL VARIATION IN THE SOUND VELOCITY 
OF THE OCEANe ONE PATH IS TRACED FOR EACH SPECIFIED INITIAL ANGLE 
FROM THE HORIZONTALe BEHAVIOR OF RAY PATH IS CONTROLLED BY SOUND VEL- 
OCITY GRADIENTS— CORRECTION FOR EARTH CURVATURE IS ADDEDe OUTPUT IS A 
PRINTED LIST AND ALSO IN BINARY FORMAT SUITABLE FOR ADAPTATION TO A 
PLOTTERe DIRECT INQUIRIES FOR INFORMATION TO-— 


COMMANDING OFFICER 

FLEET NUMERICAL WEATHER CENTRAL 
NAVAL POSTGRADUATE SCHOOL 
MONTEREY» CALIFORNIA 93940 


THESIS3 (SONOBUOY FIXING ERROR) LANGUAGE — FORTRAN 


COMPUTER -— (NOT GIVEN) 


CALCULATES THE EFFECTS OF HORIZONTAL VELOCITY GRADIENTS IN SEA WATER 
WHEN OBTAINING A FIX ON A TARGET BY TWO PASSIVE DIRECTIONAL SENSORS. 
THESIS BY JAMES We PIGMAN (MAY 1966). 


NAVAL POSTGRADUATE SCHOOL 
MONTEREYs CALIFORNIA 93940 


NEAR-FIELD ARRAY TESTING LANGUAGE — FORTRAN 


COMPUTER — PDP-8 
PROGRAM INVESTIGATES THEORETICALLY THE EFFECT OF IRREGULARITIES IN THE 


PAGE 099 


POSITIONS OF TRANSDUCER ELEMENTS IN AN ACOUSTIC 'NEAR-FIELD! ARRAYe 
REPORT NOe NRL-6728 (MAY 1968» 40P) BY GERALD Ae SABINe DDC NO-~ IS 


AD-669-449,. 


UNDERWATER SOUND REFERENCE DIVe 
NAVAL RESEARCH LABORATORY 
ORLANDO», FLORIDA 


*¥-*-* SOUND -— NORMAL MODES *-*-* 


NORMAL MODE SOLUTIONS FOR SOUND SPEED PROFILES LANGUAGE -— FORTRAN IV 
COMPUTER - CDC 3800 


PROVIDES A NORMAL MODE SOLUTION OF THE WAVE EQUATION WITH THE SOUND 
SPEED PROFILE FOR THE MEDIUM REPRESENTED BY A S€T OF DISCRETE VALUES. 
THE SEA BOTTOM IS ASSUMED TO BE A SEMI-INFINITE FLUID, SPECIFIED BY A 
CONSTANT DENSITY AND A CONSTANT SPEED OF SOUND AND WITH NO ATTENUA- 
TIONe THE INTERFACE BETWEEN THE WATER COLUMN AND THE BOTTOM IS FLAT 
AND LEVELe USER SELECTS THE MAXIMUM NUMBER OF MODES DESIREDe OUTPUT— 
— THE NORMALIZED EIGENFUNCTIONS OR MODE SHAPES ARE OBTAINED FROM THE 
EIGENVALUES AND PLOTTEDe THE GROUP VELOCITY CHARACTERISTIC IS OB- 
TAINED OVER A RANGE OF FREQUENCIES AND TABULATEDe PROPAGATION LOSS IS 
PLOTTED AS A FUNCTION OF RANGEe DOCUMENTATION WILL BE IN A FORTH- 
COMING NRL REPORTe 


JOHN CYBULSKI 

CODE 8177s ACOUSTICS DIVISION 
NAVAL RESEARCH LABORATORY 
WASHINGTONs De Ce 20390 


PROPAGATION LOSS — NORMAL MODES LANGUAGE — FORTRAN 
COMPUTER - CDC 3800 


CALCULATES UNDERWATER SOUND PROPAGATION IN A HORIZONTALLY STRATIFIED 
MEDIUMe THE PROGRAM CALCULATES A SET OF HORIZONTAL PHASE VELOCITIES 
FOR THE NORMAL MODES AND THEN SERIES THE MODE AMPLITUDE FUNCTIONS TO 
FIND THE SOUND LEVELSe INPUT-- SOUND VELOCITY PROFILE» SOURCE DEPTH, 
POSITION OF RECEIVERS IN RANGE AND DEPTHs SURFACE LOSS» AND BOTTOM 
LOSS TABLE. OUTPUT-- PROPAGATION LOSS AT THE VARIOUS RECEIVERS»e PRO- 
CEDURE-- APPROXIMATE VALUES OF THE HORIZONTAL PHASE VELOCITY ARE CAL- 
CULATED USING RAY THEORY» EXACT VALUES ARE FOUND BY ITERATING IN THE 
COMPLEX PLANEe SOUND INTENSITIES ARE CALCULATED BY FORMING THE SERIES 
OF NORMAL AMPLITUDE FUNCTIONSe DOCUMENTATION-— FORTHCOMING NRL REPORT 


DRe He Pe BUCKER»s JRe 
CODE 8170 

NAVAL RESEARCH LABORATORY 
WASHINGTONs De Co 20390 


#-#%-% SOUND - SPEED COMPUTATIONS *-*-* 


SOUND VELOCITY LANGUAGE — FORTRAN 
COMPUTER = ED.Gs3 2.0/0 
(COPY ON FILE AT NODC) 
COMPUTES SOUND VELOCITY USING WILSON'S EQUATIONSe OUTPUT CARDS HAVE 
VELOCITY OF SOUND IN METERS/SECs PRESSURE IN KG/SQ-CMs SIGMA-T, IN 
ADDITION TO INPUT STATION DATA AND IDENTIFICATION’ 


NAVAL UNDERWATER WEAPONS RESEARCH 


PAGE 100 


AND ENGINEERING STATION 
NEWPORT» RHODE ISLAND 02840 


FATHOMETER CORRECTION LANGUAGE — FORTRAN 
COMPUTER — CDC 1604 
(COPY ON FILE AT NODC) 

CORRECTS ECHO SOUNDER READINGS BY COMPUTING ACTUAL TRAVEL TIME FROM A 
LINEAR SEGMENT VELOCITY PROFILEe INPUT-- DEPTH VSe VELOCITY POINTS ON 
CARDSe OUTPUT IS PRINTED LIST OF ACTUAL DEPTHSs FATHOMETER DEPTHS AND 
CORRECTIONS (FATHOMS)e A SUBROUTINE FOR THE CALCOMP PLOTS DIFFERENCES 
VSe ECHO SOUNDER DEPTHSe CORE STORAGE USED-- 41006 


COMMANDER 

NAVAL UNDERSEA RESEARCH AND DEVELOPMENT CENTER 
ATTNe De Fe GORDON 

SAN DIEGO» CALIFORNIA 92132 


GENERAL VELOCITY FIELD LANGUAGE — FORTRAN-63 
COMPUTER -— CDC 3800» 
DRUM SCOPE 


GIVEN A SERIES OF INCOMPLETE VELOCITY PROFILES ALONG A RANGE TRACK THE 
PROGRAM EXTRAPOLATES THE DEEP PROFILES TO THE BOTTOM USING WILSON'S 
EQUATION AND INTERPOLATES BETWEEN THE DEEP PROFILES IN ORDER TO EXTEND 
THE SHALLOW PROFILESe THE RESULT IS A COMPLETE DESCRIPTION OF THE 
VELOCITY FIELD OVER THE RANGE-DEPTH PLANEe OUTPUT FROM PROGRAM IN- 
CLUDES-- VELOCITYs GRADIENT» AND CURVATURE AT DEPTHS AND RANGES SPECI- 
FIED BY USERs A CALCOMP CONTOUR PLOT OF SPECIFIED VELOCITY FIELD» AND 
A 3-DIMENSIONAL PLOT OF VELOCITY VSe RANGE AND DEPTHe STORAGE NECES— 
SARY-- 1175450 OCTAL WORDS OF CORE AND 2 CDC-863 DRUMSe 


Je Je CORNYNs CODE 8140 
ACOUSTICS DIVISION 
NAVAL RESEARCH LABORATORY» WASHINGTON» De Ce 20390 


SVLIM LANGUAGE - FORTRAN II 
COMPUTER - CDC 3100 
(COPY ON FILE AT NODC) 

EXAMPLE OF 'LIMITS*' RETRIEVAL FUNCTIONS USED TO EXTRACT SOUND VELOCITY 
PROFILESe THE PROGRAM READS CONTROL CARDS SPECIFYING GEOGRAPHICAL AND 
SEASONAL LIMITS OF INTEREST» SCANS A COMPACTED NODC FORMAT FILE FOR 
OCEAN STATIONS FALLING WITHIN THE SELECTED LIMITS» CONVERTS THE PRO- 
FILE FROM METERS/SEC TO FEET/SEC AND PRINTS THE PROFILEe REFe INFORM-— 
AL REPORT IR NOe 69-595 JULY 19696 AUTHOR-- WALT YERGENs EXPLORATORY 
OCEANOGRAPHY DIVISION» CODE 7240. FURTHER INFORMATION MAY BE OBTAINED 
FROM THE DISSEMINATION DEPARTMENT CODE 445 OR THE AUTHOR. 


NAVAL OCEANOGRAPHIC OFFICE 
SUITLANDs MARYLAND 20390 


DETERMINATION OF POSSIBLE MAGNITUTE OF LANGUAGE -— FORTRAN 
ERROR IN VERTICAL SOUND VELOCITY COMPUTER - IBM 7074 
(COPY ON FILE AT NODC) 

PROGRAM REQUESTED BY THE COAST AND GEODETIC SURVEY TO CORRECT FATHOM-— 
ETER READINGSe PROVIDES-- (1) HARMONIC MEAN OF SOUND VELOCITY IN M/ 
SEC AT CHOSEN DEPTHS (2) MEAN VERTICAL SV AT ABOVE DEPTHS WITHIN ONE 
MARSDEN SQe (3) VARIANCE OF 2 (4) DIFFERENCE BETWEEN STANDARD AND COM-— 
PUTED SVs TESTED AGAINST GIVEN ALLOWABLE ERROR VALUES (5) NUMBER OF 
STATIONS USED AT EACH DEPTH WITHIN EACH MARSDEN SQe INPUT MUST BE IN 
NODC FORMAT TAPEs ZONE-EDITEDs IN DEPTH SEQUENCE AND SORTED ON MARSDEN 
SQUARESe AUTHOR-- RUDI SAENGERe OS NOe 52203. 


COMPUTER SYSTEMS DIVISION 


NATIONAL OCEANOGRAPHIC DATA CENTER 
WASHINGTONs De Ce 20390 


PAGE 101 


LIGHT AND SOUND INSTRUCTION B LANGUAGE — FORTRAN 
COMPUTER — IBM 7074 


COMPUTES THE HARMONIC MEAN SOUND VELOCITYs TRAVEL TIME» AND CORRECTION 
RATIO AT 100-FATHOM DEPTH INTERVALS BY ONE-DEGREE SQUAREe OS NOe — 
20111. AUTHOR-- MeCe CHURCH. 


COMPUTER DEPARTMENT s CODE 083 
NAVAL OCEANOGRAPHIC OFFICE 
SUITLAND» MD. 20390 


VELOCITY OF SOUND IN SEA WATER LANGUAGE — FORTRAN 
COMPUTER -— IBM 1620 
(COPY ON FILE AT NODC) 
COMPUTES ONE PAGE AT A TIME FOR A GIVEN DEPTH AND A GIVEN SET OF 10 
SALINITIES AND TEMPERATURES. A TABLE OF PRESSURES IS READ IN AND CON- 
VERTED TO DEPTHSe USES LATER VERSION OF WILSON'S FORMULA FOUND IN THE 
JASA VOL. 32 NO. 10 (1960). 


ESSAs COAST AND GEODETIC SURVEY 
WASHINGTON SCIENCE CENTER» BLDGe 2 
ROCKVILLE» MDe 20852 


WATERVEL LANGUAGE - FORTRAN AND 
BINARY 
COMPUTER - (NOT GIVEN) 


(COPY ON FILE AT NODC) 
COMPUTES SOUND VELOCITY AFTER WILSON (1960-2), SOUNDING VELOCITY, RE- 
FLECTION TIMEe VALUES INTERPOLATED FROM STANDARD DEPTHSe UNITS CON- 
VERSION ENGLISH TO METRICe AUTHOR-- HELEN KIRKe 


SCRIPPS INSTITUTION OF OCEANOGRAPHY 
ATTNe GeGe SHOR 
LA JOLLA» CALIFe 92038 


FUNCTION SDVEL LANGUAGE — FORTRAN 


COMPUTER — IBM 1800 SYS 
(COPY ON FILE AT NODC) 


SUBPROGRAM COMPUTES SOUND VELOCITY IN SEA WATER FROM TEMPERATURE» SAL-— 
INITY AND PRESSURE USING WILSON'S FORMULAEe A CONVERSION OF PRESSURE 
IS MADE FROM NEWTONS/SQ METRE TO KGF/CM SQe 


NATIONAL INSTITUTE OF OCEANOGRAPHY 
WORMLEY»s GODALMING»s SURREY 
ENGLAND 


SOUND VELOCITY IN OCEAN WATER LANGUAGE -— FORTRAN II 
COMPUTER - 18M 704 
(COPY ON FILE AT NODC) 

USL PROGRAM NOs 02406 COMPUTES SOUND VELOCITY AS A FUNCTION OF DEPTHs 
TEMPERATURE» SALINITY AND LATITUDE» EQUATIONS USED WERE OBTAINED FROM 
AN NEL PUBLICATION (MeAe PEDERSEN» ET ALs 1962)2¢ A PRINTED OUTPUT HAS 
THE INPUT PARAMETERS AND THE COMPUTED VALUES OF SOUND VELOCITY, PRESS- 
URE» AND DENSITY (RHO) FOR EACH DEPTH. REFe USL TECHe MEMORANDUM NO. 
907-94-66 (MAY, 1966). 


Me Je GOLDSTEIN 
NAVY UNDERWATER SOUND LABORATORY» BLDG. 80 
FORT TRUMBULL» NEW LONDON» CONN. 06320 


SDGVEL (SOUNDING CORRECTION) LANGUAGE — FORTRAN IV 
COMPUTER — IBM 7094-IT/ 


7040 DCS 
(COPY ON FILE AT NODC) 


PAGE 102 


CORRECTS OBSERVED DEPTHS FOR LATITUDINAL AND LONGITUDINAL VARIATION IN 
SOUNDING VELOCITYe SOUNDING VELOCITIES CALCULATED By NODC ARE ENTERED 
INTO STORAGE AS A LINEAR ARRAYe OBSERVED LATITUDEs LONGITUDEs AND 
DEPTH ARE ENTERED INTO THE TABLE AS SEARCH PARAMETERS» AND A THREE-DI- 
MENSIONAL LINEAR INTERPOLATION IS PERFORMED TO OBTAIN AN APPROPRIATE 
VALUE FOR SOUNDING VELOCITY. THIS IS APPLIED TO THE OBSERVED DEPTHe 

AN ITERATION ROUTINE REFINES THE CORRECTED DEPTH TO WITHIN A PREDETER- 
MINED ERRORe THE INPUT IS VIA PUNCHED CARDS AND A PRINTED OUTPUT IS 
PRODUCEDe ESTIMATED RUNNING TIME-- 0204 SECONDS PER DATA ENTRYe AU- 
THOR-— WILLIAM ANIKOUCHINE» JORG, ESSAc 


DEPARTMENT OF OCEANOGRAPHY 
UNIVERSITY OF WASHINGTON 
SEATTLE» WASHe 98105 


AN/UYK-1 SOUND VELOCITY LANGUAGE - LOGANDS AND 
LOGRAMS 
COMPUTER -— AN/UYK~1 


COMPUTES SOUND VELOCITY BY TWO DIFFERENT MEANS FOR COMPARISON WITH THE 
SOUND VELOCIMETER VALUE OBTAINED THROUGH BISSETT-BERMAN SYSTEMe ALSO 
COMPUTES PRESSURE» MEAN, VARIANCEs STANDARD DEVIATION, SIGMA-T, SPEC- 
IFIC VOLUMEs SPECIFIC VOLUME ANOMALYs AND DYNAMIC HEIGHT ANOMALY. OS 
NO 20154. AUTHOR-— OeAe SMITHe 


COMPUTER DEPARTMENT» CODE 0831 
NAVAL OCEANOGRAPHIC OFFICE 
SUITLANDs MDe 20390 


VELOCITY OF SOUND LANGUAGE = MAC 
GOMPUTER) = kGiaels3 Os 


CALCULATION OF VELOCITY OF SOUND IN SEA WATER» USING WILSON'S EQUA- 
TIONe (A MAC ROUTINE WAS ALSO WRITTEN FOR THE CALCULATION OF PRESSURE 
IN DECI-BARS) AUTHORS-- AeMe SHIPLEY AND De SACKSe 


UNIVERSITY OF CAPE TOWN 
OCEANOGRAPHY DEPARTMENT 

ATTNe MRe AeMe SHIPLEY 
PRIVATE BAGs RONDEBOSCH» CePe 
REPUBLIC OF SOUTH AFRICA 


SONVEL LANGUAGE — FORTRAN IV-H 
COMPUTER -— SDS SIGMA 7 


SUBROUTINE COMPUTES THE SPEED OF SOUND IN SEA WATER FROM THE TEMPERA-— 
TUREs SALINITY AND PRESSURE ACCORDING TO WeDe WILSON'S FORMULAS. AN 
EARLIER VERSION WAS WRITTEN BY JACQUELINE WEBSTER IN FORTRAN II FOR 
THE GE 225. 


INFORMATION PROCESSING CENTER 

ATTNe MARY HUNT 

WOODS HOLE OCEANOGRAPHIC INSTITUTION 
WOODS HOLE, MASSACHUSETTS 02543 


*-%-* TIDES, ASTRONOMICAL *-*-* 


HARMONIC ANALYSIS OF TIDAL DATA LANGUAGE — FORTRAN Iv 
p COMPUTER -— CDC 6600 
(COPY ON FILE AT NODC) 
THE PROGRAM GENERATES A VARIABLE LENGTH SINE TABLE IN FIVE QUADRANTS 


PAGE 103 


AND THE INDEPENDENT VARIABLES WHICH ARE FUNCTIONS OF TIME ARE EXTRACT- 
ED FROM THIS TABLEe THE LEAST SQUARES METHOD IS EMPLOYED AND THE HAR- 
MONIC CONSTANTS ARE DERIVED BY THE USE OF A MULTIPLE CORRELATION 
SCREENING PROCESS WHICH CAN BE TERMINATED WHEN THE REGRESSION EQUATION 
CONTAINS A SPECIFIED NUMBER OF TERMS OR WHEN THE NEXT CONSTITUENT WILL 
NOT EXPLAIN A PREDETERMINED FRACTION OF THE VARIANCEs TIDE HEIGHTS 
ARE READ INTO CORE STORAGE FROM MAGNETIC TAPE OR CARDSe OTHER INPUT 
INCLUDES CONSTITUENT SPEEDS IN DEGREES PER SOLAR HOUR» NODE FACTORS» 
AND EQUILIBRIUM ARGUMENTS IN DEGREESe THE OUTPUT IS AN ORDERED LIST- 
ING OF HARMONIC CONSTANTSe NO PROVISION IS MADE FOR ELIMINATION OF 
COMPONENT EFFECTSe CORE STORAGE NECESSARY - 383000 WORDSe AUTHOR —- 
ROBERT Ae CUMMINGSe EARLIER VERSIONS WRITTEN FOR THE IBM 1620-1 AND 
FOR THE IBM 7030 (STRETCH) COMPUTERSe 


OCEANOGRAPHY DIVISION 
ESSA» COAST AND GEODETIC SURVEY 
ROCKVILLE» MDe 20852 


TIDAL CURRENT PREDICTION LANGUAGE — FORTRAN IV 


COMPUTER - CDC 6600 


(cOPY ON FILE AT NODC) 


NIO 


COMPUTES HOURLY VELOCITIES OF THE CURRENT» TIMES OF SLACK AND TIMES 
AND VELOCITIES OF MAXIMUM CURRENT USING THE HARMONIC METHOD IN WHICH 
THE CONSTITUENT VELOCITIES ARE COMBINED INTO THE RESULTANT VELOCITYe 
HOURLY VALUES ARE SCREENED TO DETERMINE BETWEEN WHICH HOURS A SLACK 

OR MAXIMUM OCCURSe THEN CALCULATION AND COMPARISON OF THE VELOCITIES 
ARE MADE AT Oel HOUR INTERVALS UNTIL THE TIME OF SLACK OR EXTREME VEL— 
OCITY IS DETERMINEDe CORE STORAGE NECESSARY-- 112000 WORDSe AUTHOR — 
ROBERT Ae CUMMINGS.» 


OCEANOGRAPHY DIVISION 
ESSA» COAST AND GEODETIC SURVEY 
ROCKVILLE» MDe 20852 


PROGRAM 48 - TIDAL ANALYSIS AND PREDICTION LANGUAGE — CHLF 3/4 
COMPUTER — MERCURY 


GENERAL PURPOSE PROGRAM FOR (1) THE ANALYSIS OF A YEAR'S HOURLY OB- 
SERVED VALUES OF TIDAL HEIGHT INTO 63 TIDAL CONSTITUENTSs (2) THE PRE- 
DICTION OF VALUES OF TIDAL HEIGHT FOR A SPECIFIED PERIOD AND SPECIFIED 
INTERVAL BETWEEN PREDICTIONSs (3) THE CALCULATION OF RESIDUALS (OBSER- 
VATIONS — PREDICTIONS) FOR A SPECIFIED PERIOD AND INTERVALe AUTHOR-- 
JAMES CREASEe* REFe NeleOo INTERNAL REPORT NOe N55 PAGES 21-2656 THIS 
PROGRAM SHOULD BE ADAPTABLE TO THE ATLAS COMPUTER. 


NATIONAL INSTITUTE OF OCEANOGRAPHY 
WORMLEY » GODALMINGs SURREY 


ENGLAND 


THEORETICAL RADIAL TIDAL FORCE LANGUAGE — MAD 


COMPUTER - IBM 7090 


(COPY ON FILE AT NODC) 


THERE ARE THREE INPUT FORMATS TO THIS PROGRAM-- 1) ASTRONOMICAL DATA 
FROM THE NAUTICAL ALMANACe 2) THE SOLAR EPHEMERIS OBTAINED FROM THE 
SAME SOURCEe ONLY THE EARTH-SUN RADIUS VECTOR IS NEEDEDe 3) LIST OF 
LOCAL CONSTANTSs LATITUDE AND LONGITUDE IN DEGREES OF ARC AND MINUTES» 
ELEVATION IN CENTIMETERSe OUTPUT GIVES LUNAR» SOLAR» AND TOTAL TIDAL 
FORCES AND THE VECTOR DATEe PROGRAM ACCOMODATES MAXIMUM OF 725 HOURS 
(30 DAYS) OF DATA IN CORE STORAGEe AUTHOR-- HENRY Le POLLAKe 


DEPTe OF EARTH AND PLANETARY SCIENCES 
414 SPACE RESEARCH COORDINATION CENTER 
UNIVERSITY OF PITTSBURGH 

PITTSBURGHs PENNA 15213 


STRONOMICAL TIDE PREDICTION LANGUAGE -— FORTRAN 66 


PAGE 104 


COMPUTER - CDC 6600 
(COPY ON FILE AT NODC) 

COMPUTES HOURLY VALUES ALSO TIME AND HEIGHTS OF HIGH AND LOW WATER 
USING THE HARMONIC METHOD IN WHICH THE CONSTITUENT TIDES ARE COMBINED 
INTO THE RESULTANT TIDEe HOURLY VALUES ARE SCREENED TO DETERMINE BE- 
TWEEN WHICH HOURS A TIDE EXTREME WILL OCCUR»s THEN CALCULATION AND COM— 
PARISON OF THE TIDES ARE MADE AT Oel HOUR INTERVALS UNTIL THE EXTREME 
TIDE IS DETERMINEDe ANY ARBITRARY DATUM PLANE MAY BE SELECTED. THE 
OUTPUT IS OPTIONAL AND MAY BE HOURLY TIDESs HIGH AND LOW TIDES, OR 
BOTHe RUNNING TIME FOR BOTH--— ABOUT 25 SECONDS FOR ONE STATION FOR 
ONE YEARe AUTHORS--— NeAew PORE (WEATHER BUREAU) AND ReAe CUMMINGS 
(COAST AND GEODETIC SURVEY). EARLIER VERSIONS WRITTEN FOR THE IBM 704 
AND IN SOS FOR THE IBM 7090/7946 REVISED IN 19666 PROGRAM DESCRIPTION 
AND LISTING ARE GIVEN IN WEATHER BUREAU TECHNICAL MEMORANDUM WTBM TDL- 
65 JANUARY 1967. 


OCEANOGRAPHY DIVISION 
ESSA» COAST AND GEODETIC SURVEY 
ROCKVILLEs MDe 20852 


TIDES LANGUAGE — FORTRAN 60 
COMPUTER - (NOT GIVEN) 
(COPY ON FILE AT NODC) 
PREDICTS TIDES IN THE OPEN SEA UTILIZING THE BASIC HYDRODYNAMIC EQUA- 
TIONSs FOR THE PRINCIPAL LUNAR SEMIDIURNAL CONSTITUENT M2e APPLICA- 
TION IS MADE TO THE ANALYSIS OF THE TIDAL REGIME IN THE GULF OF MEX- 
TCO» REFe THESIS BY THOMAS He GAINERs JRe (MAY 19665 92 P)e 


NAVAL POSTGRADUATE SCHOOL 
MONTEREY» CALIFORNIA 93940 


TIDAL PREDICTION LANGUAGE -— MAC 
COMPUTER -— ICT 1301 
(COPY ON FILE AT NODC) 
COMPUTES TIMES OF HIGH AND LOW WATER FOR A PORT FOR ONE YEARe INPUT, 
ON PUNCHED CARDS» ARE SPEED» AMPLITUDES» AND INITIAL ANGLESe USES IT- 
ERATION METHODs FOLLOWING NEWTONe SOURCE LANGUAGE-- MANCHESTER AUTO- 
CODEe REQUIRES 800 WORDS STORAGE ON ICT 1301le 


UNIVERSITY OF CAPE TOWN 
OCEANOGRAPHY DEPARTMENT 

ATTNe MRe AeMe SHIPLEY 
PRIVATE BAGs RONDEBOSCHs CePe 
REPUBLIC OF SOUTH AFRICA 


PREDICTION OF HOURLY TIDE LANGUAGE — (NOT GIVEN) 
COMPUTER — MERCURY 


COMPUTES HEIGHT OF TIDE BY EVALUATING A HARMONIC FUNCTION USING 42 

COMPONENTS,» FOR EACH HOUR OVER A PERIOD OF 370 DAYSe INCLUDES SUB- 
ROUTINE FOR COSINE FUNCTIONe RUNNING TIME ABOUT 50 MINUTES FOR ONE 
STATION FOR 370-DAY PERIODe 


HYDROGRAPHER OF THE NAVY 
ARGENTINE NAVY HYDROGRAPHIC OFFICE 


AVENIDA MONTES DE OCA 2124 
BUENOS AIRES» REPUBLICA ARGENTINA 


%—-#%-—% WAVES AND HYDROMECHANICS *-*-* 


SURFACE WAVE RAYS LANGUAGE — FORTRAN II 
AND FAP 


PAGE 105 


COMPUTER — IBM7094/CAL- 
COMP 670/564 
(COPY ON FILE AT NODC) 

CALCULATES AND PLOTS WAVE-RAY PATTERNS FOR A COASTAL AREA OF INTEREST. 
GIVEN A GRID OF DEPTH VALUES» THE INITIAL POSITION OF A WAVE RAY» AND 
THE DIRECTION OF TRAVEL AND PERIOD OF THE WAVE, SUCCESSIVE POINTS ON 
THE RAY PATH ARE CALCULATED FOR OUTPUT ON TAPEe THE PLOTTER USES THIS 
TAPE TO PLOT THE WAVE RAYSe FOR EACH POINT ON THE PATHs WATER DEPTH 
AND BOTTOM SLOPE ARE INTERPOLATED FROM THE DEPTH GRID» WAVE SPEED AND 
CURVATURE ARE COMPUTED ACCORDING TO CLASSIC THEORY» AND THE COORDIN- 
ATES OF THE NEXT POINT ARE APPROXIMATED BY AN ITERATION PROCEDURE. AP- 
PROXIMATELY 112000 POSITIONS OF STORAGE ARE REQUIRED FOR THE DATA (ExX- 
CLUSIVE OF DEPTH GRID) AND THE PROGRAMe IN ADDITION, ONE MEMORY POSI-— 
TION IS NECESSARY FOR EACH COORDINATE INTERSECTION ON THE DEPTH GRID. 
REPORTED IN TECHNICAL MEMORANDUM NOe 17 (1966) OF THE UeSe ARMY COAST- 
AL ENGINEERING RESEARCH CENTER (CERC)»s WASHINGTONs DeCe 20016¢ AUTH- 
OR--— We STANLEY WILSON» JOHNS HOPKINS UNIVe CARD DECK AND TM17 DEPOS— 
ITSEDMWA ‘GERGe 


We Se WILSON 

DEPARTMENT OF OCEANOGRAPHY 
THE JOHNS HOPKINS UNIVERSITY 
BALTIMORE>s MDe 21218 


WAVES LANGUAGE — SCRAP 
COMPUTER — CDC 1604 


COMPUTES WIND WAVE AND SWELL--— HEIGHT, PERIODs DIRECTIONs MEAN WAVE 
HETGHT FOR PAST 36 HOURSe INPUT ARE SURFACE WINDSs SEA SURFACE TEMP- 
ERATURE» AND ANALYZED WAVE HEIGHTS FOR PAST 72 HOURSe OUTPUT ANALYSIS 
INCLUDES 123 24, 362 48 HOUR WIND WAVE AND SWELL HEIGHTS AND COMBINED 
HEIGHTS» ETCe CORE STORAGE NEEDED-- 76046(8) WORDS.» ADDITIONAL STOR- 
AGE-— 24 UNIVAC DRUM BLOCK AREAS OF 7634(8)~e DIRECT INQUIRIES TO-- 


COMMANDING OFFICER 
FLEET NUMERICAL WEATHER CENTRAL 
MONTEREY: CALIFORNIA 93940 


GENERATION OF WATER WAVES BY TURBULENT WIND FLOW LANGUAGE — FORTRAN 


COMPUTER — IBM 360/67 
(COPY ON FILE AT NODC) 


PROGRAM COMPUTES VELOCITY PROFILE» NORMAL PRESSUREs TANGENTIAL SHEAR 
STRESS» AND WAVE GROWTH RATEe REFe THESIS BY PAUL Re KLINEDINSTs JRes 
JUNE 1968 (UNPUBLISHED MSe). 


NAVAL POSTGRADUATE SCHOOL 
MONTEREYs CALIFORNIA 93940 


OPTIMUM TRACK SHIP ROUTING LANGUAGE — MACHINE AND 
FORTRAN IV 

COMPUTER — PB-440 AND 

UNIVAC 1107 


SELECTS OPTIMUM ROUTES FOR OCEAN VESSELS TRANSITING Ne ATLANTIC OCEAN, 
GIVEN INPUT DATA ON SEA HEIGHTS AND DIRECTIONe OUTPUT-- MAG TAPE AND 
PRINTOUT INDICATING OPTIMUM PATH OF SHIP», AND TIME REQUIRED TO CROSS 
BY BOTH OPTIMUM AND PRESPECIFIED FIXED ROUTE’ AUTHOR-- FeWe NAGLEe 


COMMANDING OFFICER 


NAVY WEATHER RESEARCH FACILITY 
BLDGe R-485 NAVAL AIR STATION 
NORFOLK, VIRGINIA 23511 


VC2AP3 SHIP ROUTING LANGUAGE — FORTRAN 
COMPUTER —- CDC 1604 


PAGE 106 


CALCULATES THE OPTIMUM TRACK SHIP ROUTE OF A VC2AP3 VESSEL ON A TRANS- 
PACIFIC VOYAGEe THE PROGRAM CAN BE MODIFIED EASILY TO PROVIDE ROUTES 
FOR OTHER TYPE VESSELS IN ANY OCEAN AREA OF THE Ne HEMISPHEREe USES 
TWO ADVANCES IN THE CALCULUS OF VARIATIONS METHOD FOR MINIMAL~-TIME 
SHIP ROUTINGe INCORPORATES LONG-RANGE (5-DAY AND 30-DAY) WEATHER 
FORECASTS TO EXTRAPOLATE THE FNWC OCEAN WAVE FIELD FORECASTS TO EIGHT 
DAYSe MAIN PROGRAM AND SUBROUTINES LISTED IN TECHNICAL REPORT NOe 81 
(JULY 1967) BY GeJe HALTINER» WeEe BLEICKs AND FeDe FAULKNERe 


NAVAL POSTGRADUATE SCHOOL 
MONTEREYs CALIFORNIA 93940 


SEICHE ANALYSIS LANGUAGE — FORTRAN II 
AND ALGOL 
COMPUTER - IBM 360/50 
(COPY ON FILE AT NODC) 
COMPUTES THE SEICHE PARAMETERS IN ACTUAL BASINS» GULFS OR BAYSe REF. 
SPECIAL REPORT NOo 4 "DIGITAL COMPUTER PROGRAMS FOR THE DEFANT METHOD 
OF SENGHE ANALYSUSIo JULY USesio Ei ieVEseri Jo [reales 


THE LIBRARIAN 

CENTER FOR GREAT LAKES STUDIES 
UNIVERSITY OF WISCONSIN-MILWAUKEE 
MILWAUKEE sWISCONSIN 53201 USA 


PROFIL (TSUNAMI PROFILES) LANGUAGE — FORTRAN IV 
COMPUTER - IBM 7094 


TREATS A TSUNAMI OR OTHER LONG WAVE AS IF IT WERE A TRAIN OF UNIFORM 
PERIODIC WAVES MOVING OVER A BOTTOM OF CONSTANT SLOPE» USING LINEAR 
SHALLOW-WATER THEORYe THE RESULTS ARE PLOTTED ON A SERIES OF GRAPHS. 
PROGRAM LISTED IN TECHNICAL REPORT HEL 16-1 (OCT 1966) "LONG WAVE PRO- 
FILES OVER A SLOPE's BY ReHe CROSS AND Rete WIEGELe 


UNIVERSITY OF CALIFORNIA 
HYDRAULIC ENGINEERING LABORATORY 
BERKELEYs CALIFORNIA 94720 


WAVE SHOALING LANGUAGE -— FORTRAN 
COMPUTER - IBM 7040 
(COPY ON FILE AT NODC) 

CALCULATES THE TRANSFORMATION OF A WAVE PROPAGATING FROM DEEP WATER TO 
THE SHOREs APPLYING THE PRINCIPLE OF CONSERVATION OF ENERGY FLUXe THE 
FIFTH ORDER GRAVITY WAVE THEORY OF SKJELBREIA AND HENDRIKSON (1960) IS 
USED IN THE CALCULATIONSe THE QUALITATIVE FEATURES OF THE RESULTS ARE 
THE SAME AS THOSE OBTAINED BY LE MEHAUTE AND WEBB (1964)e HOWEVER» 
THE SHOALING COEFFICIENT IS SMALLER IN MAGNITUDEe REFe NESCO REPORT 
SN-134-9 (1966)s5 BY ReCeYe KOH AND BeJe LE MEHAUTE*’ PROGRAMERS-—- ROB- 
ERT WHALIN AND MARYANN MOORE. 


NATIONAL ENGINEERING SCIENCE CO6 
711 SOUTH FATR OAKS AVEe 
PASADENA» CALIFORNIA 


SUBROUTINE LENG1 LANGUAGE — FORTRAN Iv 
COMPUTER - IBM 360/40 
(COPY ON FILE AT NODC) 

COMPUTES WAVE LENGTHS AND SPEED OF GRAVITY WAVES» GIVEN THE PERIOD AND 
WATER DEPTHs USING SMALL-AMPLITUDE (AND STOKES! SECOND-ORDER) WAVE 
THEORYe OUTPUT ARE WAVE LENGTH AND SPEED, AND THE DEEP-WATER WAVE 
LENGTHe THE IMPLICIT EQUATIONS ARE APPROXIMATEDs THEN ITERATION IS 
PERFORMED TO REDUCE THE ERRORe 


PROFe RALPH He CROSS 
ROOM 48-209 HYDRODYNAMICS LABORATORY 
MASSACHUSETTS INSTITUTE OF TECHNOLOGY 


PAGE 107 


CAMBRIDGE» MASSACHUSETTS 02139 


PROFILE LANGUAGE — FORTRAN IV 
COMPUTER — IBM 360/40 
(COPY ON FILE AT NODC) 
COMPUTES AND PLOTS THE WAVE PROFILE GIVEN THE SPECTRUM (IN THE FORM OF 
THE FOURIER COEFFICIENTS) « INPUT-- THE NUMBER OF COMPONENTS» AND THE 
NUMBER OF VALUES OF ETA TO BE COMPUTED AND PLOTTEDs ARE READ IN AT Ex- 
ECUTION TIMEe OUTPUT-- A PRINTER PLOT (ON A PRINTER WITH A 132-—CHAR- 
ACTER LINE) OF ETA VSe Te REFe TECHe NOTE NOe 13 "WATER WAVE TEACHING 
AIDS! (ReHe CROSS» SEP 1968)» HYDRODYNAMICS LABORATORYs DEPARTMENT OF 
CIVIL ENGINEERINGe 


PROFe RALPH He CROSS 

ROOM 48-209 HYDRODYNAMICS LABORATORY 
MASSACHUSETTS INSTITUTE OF TECHNOLOGY 
CAMBRIDGE» MASSACHUSETTS 02139 


SUBROUTINE PROF1 LANGUAGE - FORTRAN Iv 
COMPUTER - IBM 360/40 
(COPY ON FILE AT NODC) 

COMPUTES WATER SURFACE ELEVATIONS» ETA(X) OR ETA(T)»s OVER A WAVE PERI- 
ODs USING LINEAR WAVE THEORYe INPUT-- WAVE HEIGHTs PERIOD AND LENGTH, 
AND THE WATER DEPTHe OUTPUT-—- RETURNS THE THREE ARRAYS OF Xs Ts AND 
ETA FOR T=0s PER/40seeesPER AND X=0Os L/405 2L/4090eeesle WRITEUPS AND 
LISTING IN TECHNICAL NOTE NOe 13 OF THE HYDRODYNAMICS LABORATORYe AL-— 
TERNATIVE SUBROUTINES» PROF2 AND PROF3y ACCOMPLISH THE SAME PURPOSE 
USING STOKES! SECOND— AND THIRD-ORDER WAVE EQUATIONS. 


PROF e RALPH He CROSS 

ROOM 48-209 HYDRODYNAMICS LABORATORY 
MASSACHUSETTS INSTITUTE OF TECHNOLOGY 
CAMBRIDGEs MASSACHUSETTS 02139 


SUBROUTINE REFL1 LANGUAGE — FORTRAN Iv 
COMPUTER - IBM 360/40 
(COPY ON FILE AT NODC) 
COMPUTES WATER SURFACE PROFILES FOR THE PARTIAL (TWO-DIMENSIONAL) RE- 
FLECTION OF A LINEAR (SMALL-AMPLITUDE) WAVE FROM A STRUCTURE» INPUT - 
THE INCIDENT WAVE HEIGHTs PERIODs AND LENGTHs THE WATER DEPTH» AND THE 
REFLECTION COEFFICIENTs OUTPUT-- PRINTS WATER SURFACE PROFILES FOR 
TWO WAVE LENGTHS» FOR T = Os T/4s5 T/2, AND 3T/4e DOCUMENTATION IS IN 
TECHNICAL NOTE 135 MeIeTe HYDRODYNAMICS LABORATORY (SEPT 1968 92 P)e 


PROF e RALPH He CROSS 

ROOM 48-209 HYDRODYNAMICS LABORATORY 
MASSACHUSETTS INSTITUTE OF TECHNOLOGY 
CAMBRIDGE» MASSACHUSETTS 02139 


SUBROUTINES UOFT1ls WOFT1s UTOFT1» WTOFTI LANGUAGE — FORTRAN IV 
COMPUTER — IBM 360/40 
(COPY ON FILE AT NODC) 

COMPUTES VALUES OF U(T)» W(T)s THE PARTIAL DERIVATIVE OF U WITH RES- 
PECT TO Ts OR THE PARTIAL DERIVATIVE OF W WITH RESPECT TO Ts IeEe THE 
HORIZONTAL AND VERTICAL FLOW VELOCITIES AND THEIR ACCELERATIONS OVER A 
WAVE PERIOD AT A GIVEN DEPTH» Z» USING LINEAR WAVE THEORYe INPUT ARE 
WAVE HEIGHT» PERIOD» AND LENGTH» THE WATER DEPTH» AND THE DESIRED VAL- 
UE OF Ze OUTPUT-— RETURNS ARRAYS OF T AND U(T)»s W(T)»s ETCe» FOR T=0, 
PER/405 2PER/40,eeesPERe ALTERNATE SETS OF SUBROUTINES CARRY OUT THE 
SAME PURPOSE USING STOKES' SECOND- AND THIRD-ORDER WAVE EQUATIONS. 
WRITEUPS AND LISTINGS IN TECHNICAL NOTE NOw 13 OF THE MeleTe HYDRODY- 
NAMICS LABORATORY (SEPT 1968). 


PROFe RALPH He CROSS 
ROOM 48-209 HYDRODYNAMICS LABORATORY 
MASSACHUSETTS INSTITUTE OF TECHNOLOGY 


PAGE 108 


CAMBRIDGE» MASSACHUSETTS 02139 


SUBROUTINES UMAX1» WMAX1s UTMAX1s WTMAX1 LANGUAGE —- FORTRAN IV 
COMPUTER — IBM 360/40 
(COPY ON FILE AT NODC) 

COMPUTES U(MAX)» W(MAX)s THE PARTIAL DERIVATIVE OF U WITH RESPECT TO T 
(MAX)s OR THE PARTIAL DERIVATIVE OF W WITH RESPECT TO T (MAX) IeEe THE 
MAXIMUM FLOW VELOCITIES IN THE X AND Z DIRECTIONS AND THEIR CORRESPON- 
DING TEMPORAL ACCELERATIONS, AS A FUNCTION OF Zs FROM Z = -H TO Z = 
ETA(MAX)» USING LINEAR WAVE THEORYe INPUT-- WAVE HEIGHT» PERIOD» AND 
LENGTH» AND THE WATER DEPTHe OUTPUT--— RETURNS ARRAYS OF Z AND UMAX(z) 
ETCes FOR Z = -Hs —(29/30)Hs —(28/30)Hseee FOR Z LESS THAN ETA(MAX) 0 
ALTERNATE SETS OF ROUTINES CARRY OUT THE SAME PURPOSE USING STOKES! 
SECOND- AND THIRD-ORDER EQUATIONSe WRITEUPS AND LISTINGS IN TECHNICAL 
NOTE NOs 13 OF THE MeIeTe HYDRODYNAMICS LABORATORY e 


PROFe RALPH He CROSS 

ROOM 48-209 HYDRODYNAMICS LABORATORY 
MASSACHUSETTS INSTITUTE OF TECHNOLOGY 
CAMBRIDGE» MASSACHUSETTS 02139 


WAVE FORCE DISTRIBUTIONs TEMPORAL AND SPACIAL LANGUAGE — FORTRAN Iv 
COMPUTER — IBM 7090/94 
(COPY ON FILE AT NODC) 
GIVEN THE WATER DENSITY, THE WATER DEPTH», THE PILE DATA»y AND A CHOICE 
OF WAVE HEIGHT AND PERIOD COMBINATIONS» THIS PROGRAM COMPUTES THE DIS- 
TRIBUTION OF FORCE ALONG A PILE OF ANY SHAPEe ALSO CALCULATED IS THE 
FORCE AT THE WATER SURFACEe THESE DISTRIBUTIONS ARE CALCULATED FOR 
TWENTY EQUALLY SPACED POINTS THROUGHOUT THE WAVE CYCLEe IF THE VALUES 
OF C(M) AND C(D)» (MASS AND DRAG COEFFICIENTS)» ARE UNSPECIFIED, THE 
VALUES ASSUMED ARE C(M) = 260 AND C(D) = le6e THE PROGRAM ALLOWS OTH- 
ER VALUES TO BE SPECIFIED IN CASE THE SITUATION (IeEes THE PILE SHAPE) 
CALLS FOR ITe PROGRAM WRITTEN FOR THE WAVE RESEARCH LAB AT THE UNIVe 
OF CALIFe REFe HEL REPORT 9-4 "WAVE FORCE PROGRAMS'» BY ReHe CROSSe 


PROFe RALPH He CROSS 

ROOM 48-209 HYDRODYNAMICS LABORATORY 
MASSACHUSETTS INSTITUTE OF TECHNOLOGY 
CAMBRIDGE» MASSACHUSETTS 02139 


WAVE FORCES AND MOMENTS LANGUAGE = FORTRAN Iv 
COMPUTER - IBM 7090/94 
(COPY ON FILE AT NODC) 
GIVEN THE DESIRED COMBINATIONS OF WAVE HEIGHT AND PERIOD, PILE DIAMET- 
ER» AND WATER DEPTHs COMPUTES THE WAVE LENGTHs CHECKS FOR EXCESSIVE 
STEEPNESSs AND COMPUTES THE TOTAL FORCE ONs AND THE MOMENT ABOUT THE 
BASE OFs THE PILES CHOSENe THE FORMULAS USED ARE DERIVED FROM LINEAR 
THEORY EXCEPT THAT INTEGRATION IS CARRIED TO THE FREE SURFACEs AS CAL— 
CULATEDe FORCE AND MOMENT ARE COMPUTED FOR 40 POINTS IN A WAVE CYCLEe 
REFe Ue OF CALIFe HEL REPORT 9-4 "WAVE FORCE PROGRAMS! BY ReHe CROSS. 


PROFe RALPH He CROSS 
ROOM 48-209 HYDRODYNAMICS LABORATORY 
MASSACHUSETTS INSTITUTE OF TECHNOLOGY 


SEAKEEPING LANGUAGE - FORTRAN IV 
COMPUTER - IBM 1130 
(COPY ON FILE AT NODC) 
PREDICTS HEAVEs PITCH» AND ACCELERATION OF A DESIGNATED HULL FORM IN 
REGULAR WAVES OVER A RANGE OF WAVE LENGTHS AND WAVE AMPLITUDES. THE 
PROGRAM IS DIVIDED INTO FOUR MAINLINE SECTIONS-- PART I SETS UP THE 
INPUT DATA FOR THE TWO CALCULATING SECTIONS OF THE PROGRAMe PART II 
CALCULATES THE SIMULATED ADDED MASS AND AMPLITUDE OF THE GENERATED 
WAVES OF THE HULL FORMe PART III CALCULATES THE AMPLITUDES OF HEAVE, 
PITCH» AND ACCELERATION, AND PART IV PLOTS AND CURVE FITS THIS INFOR- 
MATIONe REPORT REFe NOe USCG-PROGRAM-ENE-12 (JUL 685 116 P) By JACK 


PAGE 109 


We LEWIS, ICEBREAKER DESIGN BRANCHe 


Ue Se COAST GUARD HEADQUARTERS 
NAVAL ENGINEERING DIVISION 
1300 E STes NW 

WASHINGTONs De Ce 20591 


LONGITUDINAL STRENGTH OF SHIP HULL LANGUAGE —- FORTRAN IV 
COMPUTER - IBM 7090 


EXTENDS THE STATIC BALANCE METHOD OF CALCULATING SHEAR AND BENDING 
MOMENT RESPONSES TO INCLUDE A WIDE RANGE OF WAVE HEIGHTS» LENGTHS, 

AND POSITIONS WITH RESPECT TO AMIDSHIPS FOR A SHIP VERTICALLY BALANCED 
IN HEAD-ON TROCHOIDAL WAVESe THE PROGRAM HAS THE OPTION OF INCLUDING 
OR OMITTING THE SMITH CORRECTIONs AND THE FINAL DATA MAY BE PRESENTED 
IN EITHER TABULAR OR GRAPHICAL FORMe PROGRAM YPO4 PROVIDES A MEASURE 
OF THE LONGITUDINAL STRENGTH FROM THE STATIC BALANCEe YPO5 IS A METH- 
OD OF PLOTTING THE LONGITUDINAL STRENGTH CURVES» PROGRAMMED BY MRSe 
SHARON Ee GOODe REFe REPORT NOe 2272 (JAN 67s 93 P)»s BY GEOFFREY Oo 
THOMASe DDC NOe IS AD-647-8076 


MRe GENE He GLEISSNER 

HEAD» APPLIED MATHEMATICS LABORATORY 

NAVAL SHIP RESEARCH AND DEVELOPMENT CENTER 
WASHINGTON s DeCe 20007 


WAVE STATISTICS (PART I AND PART IT) LANGUAGE — FORTRAN IV 
COMPUTER - IBM OS/360 


DETERMINES WAVE STATISTICS OF A SEA RECORDe THE STATISTICS INCIUDE-- 
NUMBER OF WAVESs ReMeSes MEAN» MAXe» AND SIGNIFICANT WAVE HEIGHT» AND 
SPECTRAL DECOMPOSITION OF THE SEA SURFACEe OUTPUT-- PRINTOUT OF WAVE 
STATISTICS, AND PLOT OF SPECTRAL ESTIMATEe AUTHOR--- Je Eo MAMRINGe 


PROFe FREDERICK Fe MONROE 

DEPTe OF OCEAN ENGINEERING 
FLORIDA ATLANTIC UNIVERSITY 
BOCA RATONs FLORIDA 33432 


WAVEIN AND DIFRAK LANGUAGE — FORTRAN 
COMPUTER - IBM 7094 AND 
CDC 6400 


A PAIR OF PROGRAMS FOR (1)SPECTRAL ANALYSIS OF WAVE DATA,» AND (2) COM-— 
PUTATION AND PLOT OF THE DIFFRACTION COEFFICIENTSe AUTHOR-- SHOU-SHAN 
FANs CeEeReCes WASHes Dele 


PROFe ROBERT Le WIEGEL 
DEPARTMENT OF CIVIL ENGINEERING 
UNIVERSITY OF CALIFORNIA 
BERKELEY» CALIFe 94720 


REFRACTION OF WAVES APPROACHING A COASTLINE LANGUAGE -— FORTRAN Iv 
COMPUTER -— IBM 7090/94 


A PROGRAM TO CONSTRUCT REFRACTION DIAGRAMS AND COMPUTE WAVE HEIGHTS 
FOR WAVES MOVING INTO SHOALING WATERe CONSISTS OF MAIN PROGRAM WAVES 
I AND SUBROUTINES RAYCONs REFRACs CURVE, DEPTH, HEIGHTs ERROR» WRITERe 
SOLVES THE REFRACTION EQUATION AND THE WAVE INTENSITY EQUATION FOR AR- 
BITRARY BOTTOM SHAPESe SOLUTION WAS SOUGHT BY USE OF THE NUMERICAL 
METHODS OF FINITE DIFFERENCESe ONE OF THREE HYDRAULIC ENGINEERING 
PROBLEMS DESCRIBED IN TECHe REPTe NOe TR-80 (JUN 675 185 P) BY Re Se 
DOBSONe PROGRAMS ARE LISTED IN THE REPORTe THE DDC NUMBER IS AD-659- 
309.6 


DEPTs OF CIVIL ENGINEERING 


PAGES GIO 


STANFORD UNIVERSITY 
STANDFORDs CALIFORNIA 


SIMULATION OF WIND-GENERATED WAVES LANGUAGE = FORTRAN IV 
COMPUTER — IBM 7090/94 


INVESTIGATES AND COMPARES THE LABORATORY SIMULATED AND PROTOTYPE "SEAt 
DATAe USES PROGRAMS WAVHTS (COMPUTE WAVE HEIGHTS AND THETR STATISTI- 
CAL PROPERTIES)» SPECTR (COMPUTE NORMALIZED SPECTRUM)» STATS (COMPUTE 
VARIOUS STATISTICAL PROPERTIES OF THE SEA SURFACE RECORD) » AND CONVRT 
(CONVERTS SCRAMBLED VOLTAGE RECORDS TO TIME SERIES OF SURFACE DIS- 
PLACEMENT)e REFe TECHe REPORT NOo 65 *LABORATORY SIMULATION OF SEA 


WAVES? (JUL 1966s 134 P)»s BY JOSEPH Me COLONELLe 


STANFORD UNIVERSITY 
DEPTe OF CIVIL ENGINEERING 


STANFORD» CALIFORNIA 


PAGE 111 


RETRIEVAL OF OCEAN DATA 
—¥—#—K—H#—H—K—H— HHH 


BIOLOGICAL STATION FILE LANGUAGE — EMA 
COMPUTER — ATLAS I 


A SET OF FOUR PROGRAMS WHICH CONSTITUTE A COMPLETE SYSTEM FOR PREPAR- 
ING» MAINTAINING AND ACCESSING A MAGNETIC TAPE FILE OF BIOLOGICAL STA- 
TION DATAe NeleQe PROGRAMS 945 94/As 94/Bs AND 94/Ce AUTHORS-—- MARG— 
ARET RINGROSE AND BRIAN HINDEe 


NATIONAL INSTITUTE OF OCEANOGRAPHY 
WORMLEY> GODALMINGs SURREY 


ENGLAND 
GREAT CIRCLE RETRIEVAL LANGUAGE — FORTRAN 
COMPUTER - CDC 3800 
THERE ARE THREE DIFFERENT OPTIONS AVAILABLE-—- (1) GIVEN TWO POINTS ON 


THE EARTH'S SURFACE» THE PROGRAM CALCULATES THE GREAT CIRCLE ROUTE BE- 
TWEEN THE TWO POINTS AND THE CORRESPONDING MARSDEN SQUARES ALONG AND 
AT A GIVEN DISTANCE FROM THE TRACKe THE DATA TAPES ARE SEARCHED BY 
MARSDEN SQUARES AND THE SOUND VELOCITY PROFILES» TEMPERATURE,» SALINITY 
AND DEPTH OF OBSERVATION ARE ABSTRACTEDe (2) INDIVIDUAL MARSDEN SQS. 
MAY BE INPUT INTO THE PROGRAM AND THE ABOVE QUANTITIES ARE ABSTRACTEDe 
(3) A POINT» A RADIUS OF INTEREST IN NAUTICAL MILES» AND A CLUSTER OF 
MARSDEN SQUARES MAY BE SPECIFIEDe THE PROGRAM WILL ABSTRACT ALL THE 
STATIONS WITHIN A CIRCULAR AREA OF THE POINT FOR THE GIVEN MONTHSe 

THE INPUT RETRIEVAL PROGRAM» BY WALTER YERGENs USES DATA TAPES COMPAC-— 
TED FROM THE NODC FILE» STORAGE REQUIREMENTS—-— 1053:056 OCTAL WORDS OF 
COREs AND ONE CDC DISC FILE. 


Be Ge ROBERTSs JRes CODE 8177 
ACOUSTICS DIVISION 
NAVAL RESEARCH LABORATORY» WASHINGTONs De Co 20390 


CORE COMPUTER PROGRAM LANGUAGE - FORTRAN 
COMPUTER = (NOT GIVEN) 
(COPY ON FILE AT NODC) 
A PROGRAM PACKAGE DESIGNED FOR USE ON A RECONNAISSANCE BASIS» LISTING 
ALL CORES IN THE L-—DGO COLLECTION CONTAINING CHARACTERISTICS SPECIFIED 
BY THE USERe THE PROGRAM OUTPUTS THE REQUIRED LIST OF CORES WITH A 
SHORT DESCRIPTION OF EACH COREe AS SPECIFIED ON FOUR CONTROL CARDS» 
CORES MAY BE REQUESTED FROM CERTAIN LOCATIONS» OF CERTAIN LENGTHS» 
TAKEN IN A CERTAIN RANGE OF WATER DEPTHS» OF SPECIFIED AGE» LITHOLOGY 
AND CONTAINING SPECIFIC PALEONTOLOGIC AND MINERALOGIC COMPONENTS. 
CORES WHICH ARE ORIENTEDs HAVE APPEARED IN PUBLICATIONS AND HAVE PAL- 
EOMAGNETIC DATA AVAILABLE CAN ALSO BE REQUESTED. 


MRe ROY Re CAPO 

CORE CURATOR 

LAMONT-—DOHERTY GEOLOGICAL OBSERVATORY 
PALISADES» NEW YORK 10964 


STORAGE AND RETRIEVAL OF GEOPHYSICAL DATA LANGUAGE — FORTRAN 
COMPUTER -— (NOT GIVEN) 
(COPY ON FILE AT NODC) 

A SYSTEM OF PROGRAMS AND SUBROUTINES FOR THE STORAGE» EDITING» AND RE- 
TRIEVAL OF DATAs SET UP BY THE MARINE GEOPHYSICS GROUP AT BEDFORD IN- 
STITUTE OF OCEANOGRAPHY. THE MAIN RETRIEVAL PROGRAM SEARCHES FOR A 
PARTICULAR FILE ON TAPE, READS AND PRINTS FILE LABELS» AND CONTROLS 
THE PROCESSING SUBROUTINES CALLEDe DOCUMENTED IN BIO COMPUTER NOTE 
67-3-C (NOV 1967)s BY De Ie ROSS. 


BEDFORD INSTITUTE 


PAGE 112 


DARTMOUTHs NOVA SCOTIA» CANADA 


OCEANS CATALOGUE TI AND II LANGUAGE -— FORTRAN IV 
COMPUTER -— CDC 3100 
PROGRAM I — FACILITATES UPDATING OF CHARTS THAT DEPICT THE GEOGRAPHIC-— 
AL DATA DISTRIBUTION ILLUSTRATED IN THE OCEANOGRAPHIC DATA CATAIOGUE. 
PROGRAM II - COMPILES AND LISTS AN INDEX OF CANADIAN REFERENCE NUMBERS 
IN GEOGRAPHICAL SEQUENCES FOR THE OCEANOGRAPHIC DATA CATALOGUE. AUTH- 


OR-- Je ZEBARTHe 
CANADIAN OCEANOGRAPHIC DATA CENTRE 


615 BOOTH STREET 
OTTAWA» CANADA 


PAGE 113 


eh 


WOLoa 


INDEX BY AGENCY OR INSTITUTION 


ADELPHI UNIVERSITY 


CHLOROPHYLL AND CAROTENOID PIGMENT IBM 16201IFORTRAN II 05 


ARGENTINE NAVY HYDROGRAPHIC OFFICE 


PREDICTION OF HOURLY TIDE MERCURY NOT GIVEN 105 


ARMY CORPS OF ENGINEERS», LAKE SURVEY DISTRICT 


SEDIMENT TEXTURAL ANALYSTS NOT GIVEN FORTRAN 32 


ARTHUR De LITTLEs INCe 


ACOUSTIC RAY TRACING IBM 7090 FORTRAN II 94 

TWO-DIMENSTONAL AUTOCORRELATION IBM 7090s FORTRAN 56 
IBM 1401 

TRLOSS (TRANSMISSION LOSS) CDC 6600 FORTRAN 94 


BEDFORD INSTITUTE OF OCEANOGRAPHY 


DATA REDUCTION FOR THE CDC 3100 CDC 3100 FORTRAN II 14583 
DATA REDUCTION FOR THE PDP-8 PDP-8 PAL III 14 
ISALBP (SALINITY ANOMALY) CDC 3100 FORTRAN II 10 
ISATBP (OXYGEN ANOMALY AND SATe) CDC 3100 FORTRAN II 10 
LEAST SQUARES CURVE FITTING CDC 3100 FORTRAN II 45 
PLOT STATION POSITIONS CDC 3100 FORTRAN II 36 
PLOT THETA-S CURVES CDC 3100 FORTRAN II 35 
SECTION PLOTTING CDC 3100 FORTRAN 36 
TIME SERIES PLOTTING CDC 3100 FORTRAN-32 36 
STADAT 2 GE 200 SERFORTRAN II 14 
RETRIEVAL OF GEOPHYSICAL DATA NOT GIVEN FORTRAN Walz 


BERGEN» UNIVERSITY OF 


PROCESSING OF OCEANOGRAPHIC OBSe IBM 1620I1IFORTRAN II 70 


BUREAU OF COMMERCIAL FISHERIES» HAWAII 


AOUsISAOU (CALCe OF OXYGEN» ETCe) IBM 360/65FORTRAN IV 10 
GDNP»sGRAD (CALCe OF GRADIENTS) IBM 360/65FORTRAN IV 76 
GVPAsVPA (CALC. OF CURRENTS) IBM 360/65FORTRAN IV 69 
TSOSsOXOSsPHOS (ISENTROPIC PLOT) IBM 360/65FORTRAN IV 40 
LENGTH-WEIGHT FREQUENCY IBM 360/65FORTRAN IV 06 
LONG WAVE RADIATION IBM 360/65FORTRAN IV 25 
OCEANOGRAPHIC REPORT PREPARATION IBM 360/65FORTRAN IV 91 
OCEANOGRAPHIC SUMMARY (NOS. 19293) IBM 360/65FORTRAN IV 719 
REVERSING THERMOMETER CORRECTION IBM 360/65FORTRAN IV 20 
TSIPsTHOXsTHOT (PLOT TIME HISTORY) IBM 360/65FORTRAN IV 41 


BUREAU OF COMMERCIAL FISHERIES, LA JOLLA 


SEA SURFACE TEMPe AND ANOMALY SUM, CDC 3600 FORTRAN-62 81 
SEA SURFACE TEMPe DATA SUMMARY CDC 3600 FORTRAN-62 81 
SYNOPTIC MARINE WEATHER DATA SUMMARY CDC 3600 FORTRAN-62 80 
VACOTS (VERTICAL SECTION PLOT) CDC 3600 FORTRAN-63 39 


PAGE 115 


BUREAU OF COMMERCIAL FISHERIES, MIAMI 


FLOW METER PLOTS IBM 360/65FORTRAN IV 72 
GENERAL MERCATOR PLOT IBM 360/65FORTRAN IV 40 
HORIZONTAL SECTIONS IBM 360/65FORTRAN IV 40 
IN SITU OCEANOGRAPHIC DATA IBM 360/65FORTRAN IV 85 
INTERPOLATION IBM 360/65FORTRAN IV 86 
MERCATOR STATION PLOT IBM 360/65FORTRAN IV 40 
OXYGEN» PHOSPHATE» DENSITY PLOTS IBM 360/65FORTRAN IV 39 
TEMPERATURE-SALINITY CURVES IBM 360/65FORTRAN IV 39) 


CALIFORNIAs UNIVERSITY OF 


WAVEIN AND DIFRAK IBM 70945 FORTRAN 509110 
CDC 6400 
PROFIL (TSUNAMI PROFILES) IBM 7094 FORTRAN IV 107 


CANADIAN OCEANOGRAPHIC DATA CENTRE 


DAILY SEAWATER OBSERVATIONS CDC 3100s FORTRAN IV> ue 
IBM 1620 FORTRAN II-D 
OCEANS II REPORT GENERATOR IBM 1401 SPS 23 
OCEANS ITI IBM 360/65FORTRAN IV 86 
OCEANS CATALOGUE I AND II cDC 3100 FORTRAN IV 113 
SUA USU MES 15 1th Vel CDC 3100 FORTRAN IV 56 
THERMOCHECK II -— TEMPe CORRECTION CDC 3100s FORTRAN IV 17 
IBM 360/65 
TEMPERATURE-SALINITY PLOT CDC 3100 FORTRAN 39) 


CAPE TOWNs UNIVERSITY OF 


CHLOROPHYLL CALCULATIONS KG 3 Ont MAG o7 
DELTA-ALPHA AND SIGMA-T lel 1301) (MAG 93 
HARMONIC ANALYSIS leh 1308 TMAG Sw 
TIDAL PREDICTION UG 3 Ol IMAG 105 
VELOCITY OF SOUND ICT 1301 MAC 103 


COAST AND GEODETIC SURVEYs SEATTLE 


CONDU (THERMAL CONDUCTIVITY) IBM7094-IIFORTRAN IV 31 
77040 DCS 


COAST AND GEODETIC SURVEYs WASHINGTON»s De Ceo 


ASTRONOMICAL TIDE PREDICTION CDC 6600 FORTRAN-66 104 

COMPUTE GEOGRAPHIC POSITIONS IBM 1620 SPS 61 

HARMONIC ANALYSIS OF TIDAL DATA CDC 6600» FORTRAN IV 103 
IBM 7030 FORTRAN II 

LORAN C IBM 1620 SPS 62 

TIDAL CURRENT PREDICTION CDC 6600 FORTRAN IV 104 

VELOCITY OF SOUND IBM 1620 FORTRAN 102 


COAST GUARD OCEANOGRAPHIC UNIT 


OXYGEN COMPUTATION H-516 FORTRAN IV al 
PHOSPHATE COMPUTATION H-516 FORTRAN IV ial 
SALINITY CONVERSION H-516 FORTRAN IV ll 
THERMOMETER CORRECTION H-516 FORTRAN IV 16 


COAST GUARD HEADQUARTERS» OFFICE OF ENGINEERING 


SEAKEEP ING IBM 1130 FORTRAN IV 109 


PAGE 116 


COLUMBIA UNIVERSITY» HUDSON LABORATORIES 


RAY TRACING 


NOT GIVEN FORTRAN AND 
USER LANGe 


COMMERCE» DEPARTMENT OF (SEE COAST AND GEODETIC SURVEY) 


DEFENSE, DEPARTMENT OF (SEE FLEETecees 


DEFENSE RESEARCH ESTABLISHMENT PACIFIC 


RAYTR (RAY-TRACING) 


DIGITAL EQUIPMENT COMPUTER USERS! 


DECCA HI-FIX 

DISSOLVED OXYGENs POTENTIAL TEMPe 

OCEAN STATION ANALYSIS AND SUMMARY 

THERMOMETER CORRe AND THERMOe DEPTH 
FLEET NUMERICAL WEATHER CENTRAL 

DATA FIELD GRID EXPANSION 

FORECASTING OF SURFACE CURRENTS 


GG T SEA 
POTENTIAL MIXED LAYER DEPTH 


SEA SURFACE TEMPERATURE ANALYSIS 


NAVAL eoes 


IBM 360/44FURTRAN 


SOCIETY 


PDP- 
PDP- 
PDP- 
PDP- 


CDC 
CDC 
CDC 
CDC 
CDC 
CDC 
CDC 
CDC 


SUBSURFACE THERMAL STRUCTURE ANALYSISCDC 


TWO DIMENSTONAL RAY TRACE 


WAVES 


FLORIDA ATLANTIC UNIVERSITY 


WAVE STATISTICS 


FLORIDA STATE UNIVERSITY 
MULTIVARIATE NON-LINEAR REGRESSION 
OCEANOGRAPHIC DATA COMPUTATION 


SEDIMENT DATA 


GEOLOGICAL SURVEY 


ASTRONOMIC POSITION 

GENERAL REGRESSION 

PERCENTAGE SATURATION OF OXYGEN 
PROFILE CARD-TO-TAPE FOR GEOPAC 
TALWANI 2-D GRAVITY 

WATER CHEMISTRY 


INFORMATION INTERNATIONAL» INCe 


RICHARDSON CURRENT METER FILM READ. 


PINGS We 7/ 


CDC 
CDC 
CDC 


IBM 


IBM 
CDC 
IBM 
CDC 
IBM 
CDC 


IBM 
IBM 
IBM 
IBM 
IBM 
IBM 


PDP- 


5s 8S 
bis) 18'S 
5s 8S 
5s 8S 


16045 
3100 
1604>5 
3200 
1604 
16045 
3200 
1604 
1604 
16049 
3200 
1604 


FORTRAN 
PAL 10st i 
PAE Steril 
PA ariel 


MACHINE 
MACHINE 


MACHINE 
MACHINE 


MACHINE 
SCRAP 
SCRAP » 


SCRAP 


OS/360FORTRAN 


7095 
6400 
71099 
6400 
6400 


FORTRAN 
AND IV 
FORTRAN 


FORTRAN 


360/65FORTRAN 
360/65PL/1 

360/65FORTRAN 
360/65FORTRAN 
360/65FORTRAN 
360/65FORTRAN 


7(9) 


DECAL 


NAVY eee) 


lV 


MAP 


II 


II 


IV-H 


IV-G 
IV-H 
IV-H 
IV 


97 


90 


29 


59 
45 
10 
26 
26 
09 


15 


THE VORTEX OCEAN MODEL PDP-7(9) DECAL 38 
WORLD OCEANOe DATA DISPLAY PDP-7(9) DECAL 38 
INTERIOR» DEPARTMENT OF THE (SEE BUREAU OF 
COMMERCIAL FISHERIES» GEOLOGICAL SURVEY) 
JOHNS HOPKINS UNIVERSITY 
CHLORINITY — SALINITY IBM 7094 FORTRAN II 12 
CONTINUOUS LINE SOURCE IBM 7094 FORTRAN II Til 
CONTINUOUS SOURCE PER UNIT DEPTH IBM 7094 FORTRAN II 71 
CONTINUOUS SOURCEs WITH COOLING TERM IBM 7094 FORTRAN II 71 
DENSITY — THERMOSTERIC ANOMALY IBM 7094 FURTRAN TI 90 
LATERAL RELATIVE DISTRIBUTION IBM 7094 FORTRAN II 70 
SALINITY DISTRIBUTION IN ESTUARY NOT GIVEN FURTRAN 70 
SURFACE WAVE RAYS IBM 7094 FORTRAN II 105 
TOTAL CO(2) IBM 7094 FORTRAN II 12 
KANSAS» UNIVERSITY OF - STATE GEOLOGICAL SURVEY 
AUTOMATIC CONTOURING NOT GIVEN NOT GIVEN 34 
CALCULATE AND PLOT TIME-TREND CURVES IBM7090/94FORTRANs FAP 46 
CROSS-ASSOCIATION OF SEQUENCES IBM7040/44FURTRAN IVs 54 
ELLIOTT803ALGOL 60 
MULTIVARIATE DISCRIMINANT ANALYSIS IBM 1620 FORTRAN II 55 
POWER SPECTRUM OF GEOLOGICAL SURFACE GE 6259 FORTRAN Iv 54 
IBM 7040 
Q-MODE CLUSTER ANALYSIS 1BM360/67 sFORTRAN IV 55 
IBM7090/94 
SIMULATION OF DELTAIC SEDIMENTATION IBM 360/67FURTRAN IV-H 34 
SIMULATION OF MARINE SEDIMENTATION IBM 70405 FORTRAN Iv 33 
IBM 7090/94 
SIMULATION OF TRANSGRESSION IN TIME CDC 6400 FORTRAN IV 54 
STANDARD-SIZE ANALYSIS OF SEDIMENTS IBM 1620 FURTRAN II 29 
TREND ANALYSIS USING FOURIER SERIES GE 625 FORTRAN IV 55 
TREND-SURFACE WITH UNRESTRICTED I/P IBM 1620 FORTRAN IIs 47 
IV, BALGOL 
TREND SURFACES DEGREES 1 10 6 IBM 7040 FORTRAN IV 47 
2-DIMENSIONAL REGRESSION B5500>5 ALGOL » 45 
IBM 7040 FORTRAN IV 
VECTOR TREND ANALe DIRECTIONAL DATA IBM7090/94FORTRAN IV 34 
LAMONT GEOLOGICAL OBSERVATORY (COLUMBIA UNIVERSITY) 
CORE INFORMATION NOT GIVEN FORTRAN Wi 
FOURIER ANALYSIS IBM 7090 FORTRAN 55 
REDUCTIONs DISPLAY OF SEA DATA IBM 1130 FORTRAN 14925360 
MASSACHUSETTS INSTITUTE OF TECHNOLOGY 
CURRENT METER DYNAMICS IBM OS/360MAC 72 
DETRNDs ETCe (SPECTRA SUBROUTINES) IBM 360/40FORTRAN IV 48 
LENG] (WAVE LENGTH AND SPEED) IBM 360/40FORTRAN IV 107 
MAGNETIC ANOMALTES AND GRADIENTS IBM 7094 FURTRAN II 26 
PROFILE IBM 360/40FORTRAN IV 108 
PROF1 (WATER ELEVe OVER WAVE PERIOD) I8M 360/40FORTRAN IV 108 
REFL1 (REFLECTED WAVE) IBM 360/40FORTRAN IV 108 
UMAX1s5 ETCe (MAXe FLOW VELOC.) IBM 360/40FORTRAN IV 109 
UOFT1> ETC. (FLOW VELOCITIES) IBM 360/40FORTRAN IV 108 
WAVE FORCE DISTRIBUTION I1BM7090/94FORTRAN IV 109 
WAVE FORCES AND MOMENTS IBM7090/94FORTRAN IV 109 


MIAMI» UNI 


VERSTTY (OF 


PAGE 


ALKALINITY AND SPECIFIC ALKALINITY IBM 1620 
DYNAMIC HEIGHT CALCULATION IBM 1620 
JOB EDIT FOR L-Z PROGRAM IBM 1401 
OCEANOe DATA PLOTTING FOR ICES DATA’ IBM 1620 
OCEANOe DATA PLOTTING FOR NODC DATA’ IBM 1620 
OCEAN STAe CURVE PLOTTING FOR 1401 IBM 1401 


SALINITY VALUE CALCULATION IBM 1620 
TEMPERATURE AND DEPTH CALCULATIONS IBM 1620 
IBM 1401 
MICHIGANs UNIVERSITY OF 
AVGe TEMPERATURES IN WATER COLUMN IBM 7090 
DYNAMIC HEIGHT AND CURRENT DYNAMICS IBM 7090 
GENERAL MAP PROJECTION IBM 7090 
MAP PROJECTION DISTORTIONS IBM 7090 
TREND MAP» WITH RESIDUALS IBM 7090 
WIND CURRENTS IBM 7090 
NATIONAL ENGINEERING SCIENCE COe 
WAVE SHOALING IBM 7040 


NATIONAL INSTITUTE OF OCEANOGRAPHY 


ALPHA (SPECIFIC VOLUME) IBM 1800 
BARTLETT'S CURVE FITTING IBM 1800 
BIOLOGICAL STATION FILE ATLAS I 

BRAINCON DATA REDUCTION IBM 1800 
CABLE CONFIGURATION IBM 1800 
CLUSTER ANALYSIS IBM 1800 
CURRENT METER ANALYSIS IBM 1800 
CURRENT METER CONVERSION IBM 1800 
HILOW IBM 1800 
HNAV (LORAN/DECCA COORDINATES CALC.) IBM 1800 
HNV1 (LORAN/DECCA FILE) IBM 1800 
POTLT (POTENTIAL TEMPERATURE) IBM 1800 
Q FACTORS ATLAS I 

SATELLITE NAVIGATION IBM 1800 
SBWRO (WAVE RECORDER ANALYSIS) IBM 1800 
SDANO (INVERSE GEODETIC) IBM 1800 
SDVEL IBM 1800 
STGMO IBM 1800 
SIGMT IBM 1800 
STATION DATA (ATLAS) ATLAS 1 

THERMOMETER CORRECTIONS MERCURY 

TIDAL ANALYSTS AND PREDICTION MERCURY 

2D MAGNETIC ANOMALIES IBM 1800 
VAPW (SATURATION VAPOR PRESSURE) IBM 1800 


NATIONAL OCEANOGRAPHIC DATA CENTER 


BATHYTHERMOGRAM COMPOSITE PLOT IBM 7074 
BATHYTHERMOGRAPH DATA CONVERTER IBM 7074 
BATHYTHERMOGRAPH OUTPUT IBM 1401 
BIODETERIORATION IBM 7074 
CONVERSION, NODC TO ICES IBM 1401 
CRUISE TRACK IBM 7074 
DENSITY-SALINITY LINEAR INTERPOL. IBM 7074 
DENSITY-SALINITY MID PLOT IBM 7074 
DEVIATION OF TEMPe AND SALINe PART 1 IBM 7074 
DRIFT BOTTLE DATA COMPUTATION IBM 7074 
ERROR IN VERTICAL SOUND VELOCITY IBM 7074 
GEOLOGICAL SAMPLE CONVERSION IBM 7074 


GEOLOGICAL SAMPLING INVENTORY PLOT IBM 7074 


PAGE 119 


FORTRAN 
FORTRAN II 
AUTOCODER 
FORTRAN II 
FORTRAN II 
AUTOCODER 
FORTRAN 
FORTRAN AND 
AUTOCODER 


MAD 
MAD 
MAD 
MAD 
MAD 
MAD 


FORTRAN 


FORTRAN 
FORTRAN 
EMA 
FORTRAN Iv 
FORTRAN IV 
FORTRAN 
FORTRAN IV 
FORTRAN IV 
FORTRAN IV 
FORTRAN IV 
FORTRAN Iv 
FORTRAN 
FORTRAN Vv 
FORTRAN AND 
ASSEMBLER 
FORTRAN IV 
FORTRAN IV 
FORTRAN 
FORTRAN 
FORTRAN 
EMA 

Cnlkbip 3/a 
Gallble ai/ 
FORTRAN 
FORTRAN IV 


FORTRAN 
AUTOCODER 
SPS 
AUTOCODER 
SPS 
FORTRAN 
FORTRAN 
FORTRAN 
AUTOCODER 
AUTOCODER 
FORTRAN 
FORTRAN 
FORTRAN 


09 
90 
21 
43 
43 
38 
09 
16 


81 
93 
65 
65 
47 
68 


107 


GRADIENT SUMMARY BY 1-DEG SQe» MONTH IBM 
INTERPOLATION OF OCEAN STATION DATA’ IBM 
INTERPOLATION SPECIFIC VOL ANOMALY IBM 


INVENTORY PLOT IBM 
OCEAN STATION DATA OUTPUTs NODC IBM 
OCEAN STATION DEPTH SUMMARY IBM 
SALINITY DEVIATION PROGPLOT IBM 
SEA SENSE —- DATA DISPLAY IBM 
SEA SENSE —- LIMIT IBM 
SEA SENSE — STANDARD DEVIATION IBM 
SIGMA-T VS DEPTHs SALINITY (PLOT) IBM 
SOUND VELOCITY DEPTH PROFILES IBM 
STATION DATA COMPUTE IBM 
STAe DATA CONVERSIONs CODC TO NODC IBM 
STATION DATA PARAMETER INVENTORY IBM 
STATION DATA PLOT —- SIX VARIABLES IBM 
STATION DATA VERTICAL ARRAY SUMMARY IBM 
SUBROUTINE 'tMAP# IBM 
SURFACE CURRENT SUMMARY IBM 
THERMOCLINE AND MIXED LAYER DEPTHS IBM 
THERMOMe CORRes THERMO. DEPTH IBM 
VERTICAL SECTION PLOT -— STATION DATA IBM 
VERTICAL SUMMARY HISTOGRAM PLOT IBM 


NAVAL CIVIL ENGINEERING LABORATORY 


CARBONATE-CARBON ANALYSIS OF SED. IBM 
CONSOLIDATION TESTS ON OCEAN SEDIMENTIBM 
DIRECT SHEAR TEST ON OCEAN SEDIMENT IBM 


ENGe INDEX PROPe OF CORE SAMPLES [BM 
GRAIN SIZE ANALYSIS = PLOT AND TAB IBM 
PERMEABILITY TEST ON OCEAN SED. IBM 
SETTLEMENT ANALYSIS IBM 
SUMMARY PLOTS OF SEDe TEST RESULTS IBM 
TRIAXIAL COMPRESSION TEST IBM 


NAVAL ELECTRONICS LABORATORY CENTER 


7074 AUTOCODER 
7074 FORTRAN 
7074 FORTRAN 
360/40FORTRAN IV 
1401 SPS 

1401 SPS 

7074 FORTRAN 
7074 FORTRAN 
7074 FORTRAN 
7074 FORTRAN 
7074 FORTRAN 
7074 FORTRAN 
7074 AUTOCODER 
1401 SPS 

7074 FORTRAN 
7074 FORTRAN 
7074 AUTOCODER 
360/40FORTRAN IV 
7074 AUTOCODER 
7074 AUTOCODER 
7074 FORTRAN 
7074 FORTRAN 
7074 FORTRAN 


16201 IFORTRAN 
16201 IFORTRAN 
16201 I FORTRAN 
16201 IFORTRAN 
16201 I FORTRAN 
16201 IFORTRAN 
16201 IFORTRAN 
16201 IFORTRAN 
16201 I FORTRAN 


SEQUENTIAL PLOTTING NOT GIVEN 
NAVAL OCEANOGRAPHIC OFFICE 
AIR-SEA IBM 7074 
AN/UYK-1 SOUND VELOCITY AN/UYK=-1 
ASTRONOMIC LATITUDE NOT GIVEN 
BATHYMETRIC DATA REDUCTION IBM 7074 
BOTTOM REFLECTION ANALYSIS IBM 7074 
BOTTOM SEDIMENT DISTRIBUTION PLOT IBM 7074 
BT ANALYSIS (SeEeReCe DATA) IBM 7074 
BT TEMPERATURE GRADIENT DISTRIBUTION IBM 7074 
CIRAZD (DISTANCE-AZIMUTH CALCe) IBM 7074 
CIRCULAR CHARTING IBM 7074 
CLOUD COVER AND DAILY SEA TEMPERATUREIBM 7074 
COMPUTE ADVECTION IBM 1401 
CONVERGENCE ZONE RANGE IBM 7074 
CRITICAL ACOUSTIC RATIO IBM 7074 
CURRENT METER TURBULENCE IBM 7074 
DENSITY GRADIENT BY 1-DEGREE SQUARE IBM 7074 
FAA PLOT IBM 7074 
GENERAL PURPOSE PLOT IBM 7074 
GEODETIC DATUM CONVERSION IBM 7074 
GEODETIC DATUM REDUCTION IBM 7074 
GEODETIC POSITION COMPe AND PLOT IBM 7074 
GRIDIT» REGRIDIT»s AUTOMATED CONTOUR NOT GIVEN 
GULF STREAM PATH IBM 7074 
ICE POTENTIAL IBM 7074 
LAYER DEPTH PLOT IBM 7074 


PAGE 120 


RH 
Ce 


FORTRAN 


FORTRAN 
LOGANDS 
FORTRAN 
FORTRAN 
FORTRAN 
FORTRAN 
AUTOCODER 
FORTRAN 
FORTRAN 
FORTRAN 
FORTRAN 
FORTRAN 
FORTRAN 
FORTRAN 
FORTRAN 
FORTRAN 
FORTRAN 
FORTRAN 
FORTRAN 
FORTRAN 
FORTRAN 
FORTRAN 
FORTRAN 
FORTRAN 
FORTRAN 


Dotter tel SiR 
9o90 000 0000 


44 


LEAST SQUARES PLOT 

LIGHT AND SOUND INSTRUCTION B 
LIGHT AND SOUND INSTRUCTION D 
LORAN A AND C SKYWAVE 

LORAN — COORDINATE COMPUTATION 
LORAN EDIT 

LORAN TO GEOGRAPHIC CONVERSION 
MARINE BIOLOGe ENVIRONe SUMMARIES 
MARSDEN SQe AVERAGES FROM GEOFILE 
MASS PHYSICAL PROPERTIES 

MODIFIED SURFACE CURRENTS 

MONTHLY SONIC LAYER DEPTH 
OBSERVATION DRAPING (GRAVITY) 
OXYGEN SATURATION 

PARAMETRIC MAP 


POINT GENERATOR FOR DISTANCE-AZIMUTH 
POINT GENERATOR FOR MAP PROJECTIONS 
PREDICTION OF VERTICAL TEMPe CHANGE 


RAY PATH 
SALINITY -— CONDUCTIVITY FORMULA 


SALINITY GRADIENT BY 1-DEGREE SQUARE 
SEA SURFACE TEMPERATURE DISTR+BUTION 


SEAMOUNT MAGNETIZATION 
SEDIMENT SIZE 


SHIPBOARD SURVEY -- ON-STATION MODE 
SHIPBOARD SURVEY -- ON-STATION PLOT 


SINGLE INTEGRATION 

SODANO INVERSE 

SOLAR RADIATION CONVERSION 
SOUND SPEED EDIT 

SOUNDING PLOT 


STANDARD-VECTOR DEVIATION ROSE 

STATISTICAL ANALYSIS OF ICE DATA 
STATISTICAL SURFACE CURRENT ROSE 
SVLIM (SOUND VELOCITY RETRIEVAL) 
TAPE INPUT AND OUTPUT SUBROUT+NE 


TEMPERATURE AVGe SUMMARY BY 1-DEG SQe 
TEMPERATURE DISTRIBUTION BY 1-DEG SQ. 


THERMOCLINE ONE-DEGREE 
2-DIMENSION POWER SPECTRUM (SWOP 
VAM INTERPOLATION ITI 

VERTICAL TEMPERATURE GRADIENTS 
WIND STRESS 


NAVAL POSTGRADUATE SCHOOL 


BLACKY (TIMESERIES ANALYSIS) 
CURRENT 

ICEGRID MODIFIED 

OBJECTIVE THERMOCLINE ANALYSIS 


SONOBUOY FIXING ERROR 

SPECIFIC CONDUCTIVITY 

TIDES 

VC2AP3 SHIP ROUTING 

WAVES GENERATED BY TURBULENT WIND 


NAVAL RESEARCH LABORATORY 


ACOUSTIC RAY TRACING 

BLACKBODY RADIANCE 

BLACKBODY SPECTRAL RADIANCE 
DATUBA (BUOY-CABLE DEFLECT.) 
DETERMINANT OF A SYMMETRIC MATRIX 
DISTANCE BETWEEN TWO POINTS 
EVALUATE BESSEL FUNCTIONS 

FIND REAL ZEROS OF FUNCTION 


PAGE 121 


IBM 
IBM 
IBM 
IBM 
IBM 
IBM 
IBM 
IBM 
IBM 
IBM 
IBM 
IBM 
IBM 
IBM 
IBM 
IBM 
IBM 
IBM 
IBM 
IBM 
IBM 
IBM 
IBM 
IBM 
IBM 
IBM 
IBM 
CDC 
IBM 
IBM 
CDC 
IBM 
IBM 
IBM 
IBM 
CDC 
IBM 
IBM 
IBM 
IBM 
IBM 
IBM 
IBM 
IBM 


IBM 
IBM 
CDC 
CDC 
IBM 
NOT 
IBM 
NOT 
CDC 
IBM 


CDC 
CDC 
CDC 
CDC 
CDC 
CDC 
CDC 
CDC 


7074 FORTRAN 
7074 FORTRAN 
7074 FORTRAN 
7074 FORTRAN 
7074 FORTRAN 
7074 FORTRAN 
7074 FORTRAN 
7074 FORTRAN 
7074 FORTRAN 
7074 FORTRAN 
7074 AUTOCODER 
7074 FORTRAN 
7074 FORTRAN 
7074 FORTRAN 
7074 FORTRAN II 
7074 FORTRAN 
7074 FORTRAN 
7074 FORTRAN 
7074 FORTRAN 
7074 FORTRAN 
7074 FORTRAN 
7074 FORTRAN 
7074 FORTRAN 
7074 FORTRAN 
7074 FORTRAN 
7074 FORTRAN 
7074 FORTRAN 
3100 FORTRAN 
7074 FORTRAN 
7074 FORTRAN 
3100s FORTRAN 
7074 

7074 FORTRAN 
7074 FORTRAN 
7074 AUTOCODER 
3100 FORTRAN TI 
7074 AUTOCODER 
7074 FORTRAN 
7074 FORTRAN 
7074 AUTOCODER 
7074 FORTRAN 
7074 FORTRAN 
7074 FORTRAN 
7074 FORTRAN 


OS/360FORTRAN IV 
OS/360FORTRAN IV 
1604 FORTRAN-60 
6500s FORTRAN IV-H 
0S/360 

GIVEN FORTRAN 
OS/360FORTRAN 
GIVEN FORTRAN-60 
1604 FORTRAN 
360/67FORTRAN 


3800 FORTRAN-63 
3800 FORTRAN 
3800 FORTRAN 
3800 FORTRAN-63 
3800 FORTRAN 
3800 FORTRAN 
3800 FORTRAN 
3800 FORTRAN 


99 
ial 
105 
106 
106 


GENERAL VELOCITY FIELD 

GREAT CIRCLE PATHS FROM A POINT 
GREAT CIRCLE RETRIEVAL 
HORIZONTAL GRADIENT RAY TRACING 
LINE PRINTER PLOTS 


NELEDIT 

PROPAGATION LOSS —- NORMAL MODES 

RAY TRACING 

RAY TRACE PROCESSING 

SCALING SUBROUTINE 

SOUND SPEED PROFILES — NORMAL MODES 
THREE-DIMENSIONAL SURFACE PLOTS 
UTILITY 


NAVAL RESEARCH LABORATORYs ORLANDO 


NEAR-FIELD ARRAY TESTING 


CDC 
CDC 
CDC 
CDC 
CDC 


CDC 
CDC 
CDC 
CDC 
CDC 
CDC 
CDC 
CDC 


PDP- 


3800 FORTRAN-63 101 


NAVAL SHIP RESEARCH AND DEVELOPMENT CENTER 


DIGITAL POWER SPECTRUM ANALYSIS 
LONGe STRENGTH OF SHIP HULL 
PARTIAL AND ORDINARY COHERENCE 
POWER SPECTRUM ANALYSIS 

PROJECT COD LIVER 

SAVED (BLAST TEST DATA REDUCTION) 


STATISTICAL AND PEAK-TO-PEAK ANALe 


IBM 
IBM 
IBM 


IBM 
IBM 
IBM 
IBM 


IBM 


NAVAL STRATEGIC SYSTEMS NAVIGATION FACILITY 


BECNAV (BEACON NAVIGATION) 
SPANSI1A (BEACON POSITION) 
SPANS1B (BEACON POSITION) 


CDC 
CDC 
CDC 


3800 FORTRAN 59 
3800 FORTRAN 2. 
32800 FORTRAN-63 96 
3800 FORTRAN» 35 
COMPASS 
3800 FORTRAN vat 
3800 FORTRAN 100 
3800 FORTRAN IV 96 
3800 FORTRAN-63 96 
3800 FORTRAN 3)5) 
3800 FORTRAN IV 100 
3800 FORTRAN 35 
3800 FORTRAN 21 
8 FORTRAN 99 
7090 FORTRAN IV 48 
7090 FORTRAN IV 110 
7090 FORTRAN IV 49 
AND MAP 
7090s FORTRAN 50 
704 
7090 FORTRAN II 50 
AND MAP 
7090 FORTRAN Iv 49 
AND MAP 
7090 FORTRAN Iv 49 
AND MAP 
3200 FORTRAN 58 
3200 FORTRAN 58 
3200 FORTRAN 59 


NAVAL UNDERSEA RESEARCH AND DEVELOPMENT CENTER», PASADENA 


NEWFIT 

PATTERN FUNCTION CALCULATIONS 
RAYMOR 

RAY SORT 

SONAR IN REFRACTIVE WATER 


UNTVAC1108FORTRAN IV 95 
UNIVAC1L1O8FORTRAN IV 95 
UNIVAC11O8FORTRAN V 95 
UNIVAC1108FORTRAN IV 95 
UNITVAC1L108FORTRAN IV 94 


NAVAL UNDERSEA RESEARCH AND DEVELOPMENT CENTER, SAN DIEGO 


FATHOMETER CORRECTION 
MACHINE PLOTTING ON MERCATOR PROJ. 
NAVAL UNDERWATER WEAPONS RESEARCH 
INTERPOLATION FOR OCEANOGRAPHIC DATA 
POWER SPECTRA ESTIMATION 
SOUND VELOCITY 
NAVY UNDERWATER SOUND LABORATORY 
BOTTOM REFLECTIVITY 


PAGE 122 


CDC 
CDC 


AND 
CDC 
IBM 


CDC 
CDC 


IBM 


1604 FORTRAN lol 
1604 FURTRAN 39) 
ENGINEERING STATION 


3200s FORTRAN 83 
1620 

3200 FORTRAN 51 
3200 FORTRAN 100 
704 FORTRAN II 99 


RAY TRACING IBM 704 FORTRAN II 99 
SOUND VELOCITY IN OCEAN WATER IBM 704 FORTRAN JI 102 


NAVY WEATHER RESEARCH FACILITY 
OPTIMUM TRACK SHIP ROUTING PB-4405 MACHINE 9 106 


UNIVACL1O7FORTRAN Iv 


NEW YORK UNIVERSITY 


FILM DATA PROCESSING CDC 1604 FORTRAN-60 72 


NORTHWESTERN UNIVERSITY 


CIRCSTAT CDC 3400 FORTRAN IV 52 


PACIFIC NAVAL LABORATORY» CANADA 


POWER SPECTRUM ANALYSIS PB-250 BASIC 51 


PACIFIC OCEANOGRAPHIC GROUP 


ALERT (SATELLITE TIMES) IBM 1130 FORTRAN Iv 58 
ANALe OF NON-LINEAR RESPONSE SURFACESIBM 1130 FORTRAN Iv Biz 
ASORM WCSORMMO/P MOF AERTS) IBM 1130 FORTRAN IV 58 
DEEP (SeTeDe DIGITIZING) HP 2115A FORTRAN 16 
HYDRO (COMPUTE FROM HYDRO DATA) IBM 1130 FORTRAN IV 84 
MULDA (MULTIPLE DISCRIMINANT ANAL.) IBM 1130 FORTRAN Iv 53} 
PLOG (PLOT HYDROe DATA) IBM 1130 FORTRAN IV 36 
PSAL1 (PLOT TEMPERATURE-SALINITY) IBM 1130 FORTRAN VI 3M 
RIED Meus Swoci Wintel) IBM 1130 FORTRAN IV 05 
STPO1L (PLOT SeTeDe DATA) IBM 1130 FORTRAN Iv Bi, 
STPO2 (COMPUTE FROM SeTeDe DATA) IBM 1130 FORTRAN Iv 84 
TCHK3 (THERMOMETER CORR.) IBM 1130 FORTRAN VI 16 
TRANSPORT COMP, FROM ATMOSe PRESSURE IBM 1620, FORTRAN II 67 

IBM 70405 AND Iv 

IBM 1130 
WET (SeTeDe DATA PROCESSING) HP 2115A FORTRAN 84 


PITTSBURGH» UNIVERSITY OF 

THEORETICAL RADIAL TIDAL FORCE IBM 7090 MAD 104 
RAND CORPORATION 

SEA ICE STUDIES IBM7090/94FORTRAN IV 75 


GRAPHIC SYSTEM FOR CURVE FITTING IBM 360/40(NOT GIVEN) 45 


RHODE ISLANDs UNIVERSITY OF 


AZIZ (THERMOMETRIC DEPTH) IBM 360/50FORTRAN IV-E 88 
CARDS IBM 360/50FORTRAN IV-E 22 
DELINT (DELTA CALC AND INTERPOLATION) IBM 360/50FORTRAN IV-E 88 
DEPTHS IBM 360/50FORTRAN IV-E 22 
HE I GHT IBM 360/50FORTRAN IV-E 87 
HYDRO IBM 360/50FORTRAN IV-E 19 
INTEST IBM 360/50FORTRAN IV-E 88 
LINT (LINEAR INTERPOLATION) IBM 360/50FORTRAN IV-E 88 
RDTHRM (READ THERMOMETER DATA) IBM 360/50FORTRAN IV-E 22 
SIGMA IBM 360/50FORTRAN IV-E 89 
SIGMAD IBM 360/50FORTRAN IV-E 89 
SIGMAT IBM 360/50FORTRAN IV-E 87 


PAGE 123) 


TEMP . IBM 360/50FORTRAN IV-E 19 
TSPLOT IBM 360/50FORTRAN IV-E 44 
UTEMP (UNPROTECTED THERMOMETER) IBM 360/50FORTRAN IV-E 19 


SALINE WATER» OFFICE OF 


OPTIMIZATION OF VTE WATER PLANTS IBM 7094 FORTRAN IV LZ 


SCRIPPS INSTITUTION OF OCEANOGRAPHY 


BIOP (BIOLOGY PLOT) CDC 3600 FORTRAN IV 33 
BOMM (TIME SERIES) IBM OS/360FORTRAN » 52 
CDC 3600 COMPASS 
CADS (CALC. DEPENDENT QUANTITIES) IBM 1800 FORTRAN IV 84 
CHLOR CDC 3600 FORTRAN IV 08 
GO (POTe TEMPes SIGMA THETAs OXYe) IBM 1800 FORTRAN Iv 85 
HYPERMAP NOT GIVEN FORTRAN 64 
NUTRIENT CHEMISTRY CONCENTRATION cpc 1604 (NOT GIVEN) 08 
OCEAN STATION COMPUTATIONS cDCc 1604 (NOT GIVEN) 93 
PRIMARY PRODUCTIVITY CDC 1604 (NOT GIVEN) 08 
PROFL CDC 3600 FORTRAN IV 38 
RADIATION ATTENUATION coc 1604 (NOT GIVEN) 94 
PROGRAM REGROUP CDC 3600 FORTRAN O7 
SeTeDe DATA PROCESSING CDC 3600 FORTRAN IV Lt 
Two FIVE (DATA REDUCTION) CDC 3600s FORTRAN-639 7 
IBM 1800 FORTRAN IV 
WATERVEL (SOUND VELOCITY) NOT GIVEN FORTRAN 102 
ZOOPLANKTON VOLUME cpc 1604 (NOT GIVEN) 08 


STANFORD UNIVERSITY 


REFRACTION OF WAVES I1BM7090/94FORTRAN IV 110 
SIMULATION OF WIND-GENERATED WAVES IBM7090/94FORTRAN IV aval 


TEXAS Ae AND Me UNIVERSITY 


OCEANOGRAPHIC DATA PROGRAM F IBM 7094 FORTRAN 87 
RADIATION TEMP. OF SEA SURFACE NOT GIVEN FORTRAN 68 
SEISMIC SLOPING LAYER IBM 709 FORTRAN II 2U 
SeTeDe CORRECTION IBM 7094 FORTRAN IV 19 
VELOCITYs HORIZe EDDY COEFFIFIENTS IBM 709 FORTRAN 70 


TEXAS» UNIVERSITY OF 


ECOPROD CDC 6600 FORTRAN IV 05 
JOB (SPECIES DIVERSITY) CDC 6600 FORTRAN IV 06 
OXYGEN CDC 6600 FORTRAN IV 06 


TORONTO, UNIVERSITY OF 


TIME TERM, SEISMIC REFRACTION INTERPeIBM 7094 FORTRAN IV 27 


TRANSPORTATION» DEPARTMENT OF (SEE COAST GUARD. ee) 


WASHINGTON» UNIVERSITY OF 


BKGEOL (SEDIMENT STATISTICS) IBM7094-IIFORTRAN IV 31 
77040 DCS 

CHLOROPHYLL AND PRODUCTIVITY IBM 709 FORTRAN 05 

CONCENTRATIONS PER SQUARE METER IBM7094-IIFORTRAN IV 07 
77040 DCS 

DEAD RECKONING NAVIGATION SYSTEM IBM 1130 FORTRAN 60 


PAGE 124 


INTERPOLATION PROGRAM 
PHYTOPLANKTON NUMBERS» ETCe 


SDGVEL (SOUNDING CORRECTION) 
SEDIMENT GRANULOMETRIC ANALYSIS 


SPECIAL CHEMISTRY CALCULATIONS 
SeTeDe CALCULATIONS 


SeTeDe EDIT AND INTERPOLATE 
SYNOPTIC PROGRAM 


UNDERWAY DATA SYSTEM 


WISCONSINs UNIVERSITY OF 
SEICHE ANALYSIS 


SPECTRAL ANALYSIS OF TIME SERIES 


CDC 6400 FORTRAN IV 90 
IBM7094-IIFORTRAN IV O7 
77040 DCS 

IBM7094-IIFORTRAN IV 102 
7/7040 DCS 

IBM7094-IIFORTRAN IV 32 
77040 DCS 

IBM 1130 FORTRAN IV 09 
IBM 1130 FORTRAN IV> 18 

ASSEMBLER 

IBM 1130 FORTRAN 86 


IBM7094-ITIFORTRAN II 18390 
77040 DCS» 


CDC 6400 

IBM 1130 FORTRAN 18 

IBM 360/50ALGOL » 107 
FORTRAN II 

B5500»s ALGOL 60, 50 


UNIVAC11O8FORTRAN IV 


WOODS HOLE OCEANOGRAPHIC INSTITUTION 


ATG (ADIABATIC TEMPERATURE GRADIENT 


BETA-MODEL WITH WHITE FORCING 
CRVFT (LEAST SQUARES FIT) 

DATA 

DSTABF (STABILITY FREQUENCY ) 
DYNHT (DYNAMIC HEIGHTS) 

GRAIN SIZE 

HISTO (HISTOGRAM PLOT ) 

HYLOG (HYDROe STAs DATA REDUCTION) 
LISPLO (LIST AND PLOT) 

NUSPEC (SPECTRUM ESTIMATION) 
OCCOMP (OCEANOGRAPHIC COMPUTE) 
ORD 1 (OLMSTED RAY DIAGRAM NOe 1) 
ORD 2 (OLMSTED RAY DIAGRAM NOe 2) 
PEN (POTENTIAL ENERGY ANOMALY ) 
POTEMP (POTENTIAL TEMPERATURE) 


PRESS 

PROVEC (PROGRESSIVE VECTORS) 
SCRUB (DATA EDIT AND CORRECT) 
SIGMAT 

SONVEL (SOUND VELOCITY) 

SPVOL 

STATS (STATISTICAL QUANTITIES) 
SVANOM (SPECIFIC VOLUME ANOMALY ) 
THISTO (TWO-DIMENe FREQe DISTRIBe) 
THRCL (THERMOMETER CALIBRATION) 
VECTAV (VECTOR AVERAGES) 

VEL (GEOSTROPHIC VELOCITY) 

VFREQ (VAISALA FREQUENCY COMP.) 
VTR (VOLUME TRANSPORT) 


PAGE 125 


SDS SIGMA7FORTRAN IV-H 92 
SDS SIGMAT7FORTRAN IV-H 52 
GE 225 FORTRAN 46 
SDS SIGMA7FORTRAN IV-H 22 
SDS SIGMATFORTRAN IV-H 92 
GE 225 FORTRAN II 89 
GE 225 FORTRAN II 28 
SDS SIGMA7FORTRAN IV-H 43 
SDS SIGMA7FORTRAN IV-H 20 
SDS SIGMA7FORTRAN IV-H 44 
SDS SIGMA7FORTRAN IV-H 51 
SDS SIGMA7FORTRAN IV-H_ 91 


GE 225 FORTRAN 97 
GE 225 FORTRAN 97 
GE 225 FORTRAN II 89 
GE 2255 FORTRAN IlI¢9 91 


SDS SIGMA7FORTRAN IV-H 

SDS SIGMA7FORTRAN IV-H 92 
SDS SIGMA7FORTRAN IV-H 74 
SDS SIGMA7TFORTRAN IV-H 23 
SDS SIGMA7FORTRAN IV-H 91 
SDS SIGMA7FORTRAN IV-H 103 
SDS SIGMATFORTRAN IV-H 92 
SDS SIGMA7FORTRAN IV-H 57 
SDS SIGMATFORTRAN IV-H 92 
SDS SIGMA7TFORTRAN IV-H 74 
SDS SIGMA7FORTRAN IV-H_ 20 
SDS SIGMA7FORTRAN IV-H 74 
SDS SIGMA7FORTRAN IV-H 73 
Ger225 FORTRAN II 89 
SDS SIGMA7FORTRAN IV-H_ 73 


7 : ; - te pista i! 


142 aie HiT aap ; 
“a” ” ' ‘ oer th ve 
i ee ue ist ‘R 
), e heh ii 


ck 


ey a ifs 
iM 7. He ‘ Mabe f 
oe Me | ai ade 
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be arsiwe 
4 Tle 
1 weve 
i te: wh, 
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ry Nap Ste, 
ha EE ify a 
Reh LO bee ane. 
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Pe ane awe ie 
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q mri Dee ee 
WA +9 HN Ae Sie eo 
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bpeaibsanbl rier 


INDEX BY PROGRAMMING LANGUAGE 


2-DIMENSIONAL REGRESSION 
SEICHE ANALYSIS 
SPECTRAL ANALYSIS OF TIME SERIES 
CROSS-ASSOCIATION OF SEQUENCES 


TREND-SURFACE WITH UNRESTRICTED 


JOB EDIT FOR L-Z PROGRAM 
CURVE PLOTTING FOR 1401 


OCEAN STAe 


TEMPERATURE AND DEPTH CALCULATIONS 
BATHYTHERMOGRAPH DATA CONVERTER 
BIODETERIORATION 


DEVIATION OF TEMP. 


AND SALINe 


DRIFT BOTTLE DATA COMPUTATION 


GRADIENT SUMMARY BY 1-DEG SQe» 


MODIFIED SURFACE CURRENTS 


BT ANALYSIS 


(SeEeReCe 


STATION DATA COMPUTE 
STATION DATA VERTICAL ARRAY SUMMARY 
STATISTICAL SURFACE CURRENT ROSE 
SURFACE CURRENT SUMMARY 
TAPE INPUT AND OUTPUT SUBROUTINE 
THERMOCLINE AND MIXED LAYER DEPTHS 


THERMOCLINE ONE-DEGREE 


DATA) 


RICHARDSON CURRENT METER FILM READe 


THE VORTEX OCEAN MODEL 
WORLD OCEANO. 


FATHOMETER CORRECTION 


. 


DATA DISPLAY 


MACHINE PLOTTING ON MERCATOR PROJ.) 
VC2AP3 SHIP ROUTING 
SECTION PLOTTING 
SODANO INVERSE 
SOUNDING PLOT 
TEMPERATURE-SALINITY PLOT 


BECNAV 
SPANSIA 
SPANS1B 


(BEACON NAVIGATION) 
(BEACON POSITION) 
(BEACON POSITION) 


INTERPOLATION FOR OCEANOGRAPHIC DATA 
POWER SPECTRA ESTIMATION 
SOUND VELOCITY 
PROGRAM REGROUP 
BLACKBODY RADIANCE 


BLACKBODY SPECTRAL RADIANCE 


DETERMINANT OF A SYMMETRIC MATRIX 


DISTANCE BETWEEN TWO POINTS 


EVALUATE BESSEL FUNCTIONS 


FIND REAL ZEROS OF FUNCTION 


GREAT CIRCLE PATHS FROM A POINT 


GREAT CIRCLE RETRIEVAL 


LINE PRINTER PLOTS 


NELEDIT 


PROPAGATION LOSS — NORMAL MODES 
SCALING SUBROUTINE 
THREE-DIMENSTONAL SURFACE PLOTS 


ALGOL»s BALGOL 
B5500 ALGOL 
IBM 360/50ALGOL 
B5500 ALGOL 60 
ELLIOTT803ALGOL 60 
I/P IBM 1620 BALGOL 
AUTOCODER 
IBM 1401 AUTOCODER 
IBM 1401 AUTOCODER 
IBM 1401 AUTOCODER 
IBM 7074 AUTOCODER 
IBM 7074 AUTOCODER 
PART 1 IBM 7074 AUTOCODER 
IBM 7074 AUTOCODER 
MONTH IBM 7074 AUTOCODER 
IBM 7074  AUTOCODER 
IBM 7074 AUTOCODER 
IBM 7074 AUTOCODER 
IBM 7074 AUTOCODER 
IBM 7074 AUTOCODER 
IBM 7074 AUTOCODER 
IBM 7074 AUTOCODER 
IBM 7074 AUTOCODER 
IBM 7074 AUTOCODER 
DECAL 
PDP-7(9) DECAL 
PDP-7(9) DECAL 
PDpP-7(9) DECAL 
FORTRAN 
CDC 1604 FORTRAN 
CDC 1604 FORTRAN 
CDC 1604 FORTRAN 
CDC 3100 FORTRAN 
CDC 3100 FORTRAN 
CDC 3100 FORTRAN 
cpc 3100 FORTRAN 
CDC 3200 FORTRAN 
CDC 3200 FORTRAN 
CDC 3200 FORTRAN 
CDC 3200 FORTRAN 
CDC 3200 FORTRAN 
CDC 3200 FORTRAN 
cpc 3600 FORTRAN 
CDC 3800 FORTRAN 
CDC 3800 FORTRAN 
cpc 3800 FORTRAN 
CDC 3800 FORTRAN 
CDC 3800 FORTRAN 
CDC 3800 FORTRAN 
CDC 3800 FORTRAN 
CDC 3800 FORTRAN 
CDC 3800 FORTRAN 
CDC 3800 FORTRAN 
CDC 3800 FORTRAN 
CDC 3800 FORTRAN 
CDC 3800 FORTRAN 


PAGE 127 


38 
38 


UT EST, 

WAVEIN AND DIFRAK 

TRLOSS (TRANSMISSION LOSS) 

CRVFT (LEAST SQUARES FIT) 

ORD 1 (OLMSTED RAY DIAGRAM NOe 1) 
ORD 2 (OLMSTED RAY DIAGRAM NOe 2) 
DEEP (SeTeDe DIGITIZING) 

WET (SeTeDe DATA PROCESSING) 


DEAD RECKONING NAVIGATION SYSTEM 
REDUCTION» DISPLAY OF SEA DATA 
SeTeDe EDIT AND INTERPOLATE 
UNDERWAY DATA SYSTEM 

COMPUTE ADVECTION 

ALKALINITY AND SPECIFIC ALKALINITY 


INTERPOLATION FOR OCEANOGRAPHIC DATA 


SALINITY VALUE CALCULATION 
TEMPERATURE AND DEPTH CALCULATIONS 
THERMOCHECK II -— TEMPe CORRECTION 
VELOCITY OF SOUND 

ALPHA (SPECIFIC VOLUME) 
BARTLETT'S CURVE FITTING 

CLUSTER ANALYSIS 

POTLT (POTENTIAL TEMPERATURE) 
SATELLITE NAVIGATION 

SDVEL 

SIGMO 

SIGMT 

2D MAGNETIC ANOMALIES 

WAVE SHOALING 

AIR-SEA 

BATHYMETRIC DATA REDUCTION 
BATHYTHERMOGRAM COMPOSITE PLOT 
BOTTOM REFLECTION ANALYSIS 

BOTTOM SEDIMENT DISTRIBUTION PLOT 


BT TEMPERATURE GRADIENT DISTRIBUTION 


CIRAZD (DISTANCE-AZIMUTH CALCe) 
CIRCULAR CHARTING 


CDC 
CDC 
CDC 


3800 
6400 
6600 


GE 225 
Ole 225) 
GE 225 
Ile? al abey/\ 
HP 2115A 
ANALe OF NON-LINEAR RESPONSE SURFACESIBM 


IBM 
IBM 
IBM 
IBM 
IBM 
IBM 
IBM 
IBM 
IBM 
IBM 
IBM 
IBM 
IBM 
IBM 
IBM 
IBM 
IBM 
IBM 
IBM 
IBM 
IBM 
IBM 
IBM 
IBM 
IBM 
IBM 
IBM 
IBM 
IBM 


CLOUD COVER AND DAILY SEA TEMPERATUREIBM 


CONVERGENCE ZONE RANGE 

CRITICAL ACOUSTIC RATIO 

CRUISE TRACK 

CURRENT METER TURBULENCE 

DENSITY GRADIENT BY 1-DEGREE SQUARE 
DENSITY-SALINITY LINEAR INTERPOL» 
DENSITY-SALINITY MID PLOT 

ERROR IN VERTICAL SOUND VELOCITY 
FAA PLOT 

GENERAL PURPOSE PLOT 

GEODETIC DATUM CONVERSION 

GEODETIC DATUM REDUCTION 

GEODETIC POSITION COMPe AND PLOT 
GEOLOGICAL SAMPLE CONVERSION 
GEOLOGICAL SAMPLING INVENTORY PLOT 
GULF STREAM PATH 

ICE POTENTIAL 

INTERPOLATION OF OCEAN STATION DATA 
INTERPOLATION SPECIFIC VOL ANOMALY 
LAYER DEPTH PLOT 

LEAST SQUARES PLOT 

LIGHT AND SOUND INSTRUCTION B 
LIGHT AND SOUND INSTRUCTION D 
LORAN A AND C SKYWAVE 

LORAN — COORDINATE COMPUTATION 
LORAN EDIT 

LORAN TO GEOGRAPHIC CONVERSION 
MARINE BIOLOGe ENVIRONe SUMMARIES 
MARSDEN SQ. AVERAGES FROM GEOFILE 
MASS PHYSICAL PROPERTIES 

MONTHLY SONIC LAYER DEPTH 


PAGE 128 


IBM 
IBM 
IBM 
IBM 
IBM 
IBM 
IBM 
IBM 
IBM 
IBM 
IBM 
IBM 
IBM 
IBM 
IBM 
IBM 
IBM 
IBM 
IBM 
IBM 
IBM 
IBM 
IBM 
IBM 
IBM 
IBM 
IBM 
IBM 
IBM 
IBM 
IBM 


1130 
1130 
1130 
1130 
1130 
1401 
1620 
1620 
1620 
1620 
1620 
1620 
1800 
1800 
1800 
1800 
1800 
1800 
1800 
1800 
1800 
7040 
7074 
7074 
7074 
7074 
7074 
7074 
7074 
7074 
7074 
7074 
7074 
7074 
7074 
7074 
7074 
7074 
7074 
7074 
7074 
7074 
7074 
7074 
7074 
7074 
7074 
7074 
7074 
7074 
7074 
7074 
7074 
7074 
7074 
7074 
7074 
7074 
7074 
7074 
7074 
7074 


FORTRAN 
FORTRAN 
FORTRAN 
FORTRAN 
FORTRAN 
FORTRAN 
FORTRAN 
FORTRAN 
FORTRAN 
FORTRAN 
FORTRAN 
FORTRAN 
FORTRAN 
FORTRAN 
FORTRAN 
FORTRAN 
FORTRAN 
FORTRAN 
FORTRAN 
FORTRAN 
FORTRAN 
FORTRAN 
FORTRAN 
FORTRAN 
FORTRAN 
FORTRAN 
FORTRAN 
FORTRAN 
FORTRAN 
FORTRAN 
FORTRAN 
FORTRAN 
FORTRAN 
FORTRAN 
FORTRAN 
FORTRAN 
FORTRAN 
FORTRAN 
FORTRAN 
FORTRAN 
FORTRAN 
FORTRAN 
FORTRAN 
FORTRAN 
FORTRAN 
FORTRAN 
FORTRAN 
FORTRAN 
FORTRAN 
FORTRAN 
FORTRAN 
FORTRAN 
FORTRAN 
FORTRAN 
FORTRAN 
FORTRAN 
FORTRAN 
FORTRAN 
FORTRAN 
FORTRAN 
FORTRAN 
FORTRAN 
FORTRAN 
FORTRAN 
FORTRAN 
FORTRAN 
FORTRAN 
FORTRAN 
FORTRAN 
FORTRAN 


60 
14925560 
86 
18 


OBSERVATION DRAPING (GRAVITY) IBM 7074 FORTRAN 
OXYGEN SATURATION IBM 7074 FORTRAN 
PREDICTION OF VERTICAL TEMP. CHANGE IBM 7074 FURTRAN 
RAY PATH IBM 7074 FORTRAN 
SALINITY — CONDUCTIVITY FORMULA IBM 7074 FYURTRAN 
SALINITY DEVIATION PROGPLOT IBM 7074 FORTRAN 
SALINITY GRADIENT BY 1-DEGREE SQUARE IBM 7074 FORTRAN 
SEA SURFACE TEMPERATURE DISTRIBUTION IBM 7074 FORTRAN 
SEA SENSE — DATA DISPLAY IBM 7074 FORTRAN 
SEAT SENSE = IM IBM 7074 FORTRAN 
SEA SENSE — STANDARD DEVIATION IBM 7074 FORTRAN 
SEAMOUNT MAGNETIZATION IBM 7074 FORTRAN 
SEDIMENT SIZE IBM 7074 FORTRAN 
SHtPBOARD SURVEY -- ON-STATION MODE IBM 7074 FYRTRAN 
SHIPBOARD SURVEY -- ON-STATION PLOT IBM 7074 FORTRAN 
SIGMA-T VS DEPTH» SALINITY (PLOT) IBM 7074 FYURTRAN 
SINGLE INTEGRATION IBM 7074 FORTRAN 
SOLAR RADIATION CONVERSION IBM 7074 FORTRAN 
SOUND SPEED EDIT IBM 7074 FORTRAN 
SOUND VELOCITY DEPTH PROFILES IBM 7074 FORTRAN 
SOUNDING PLOT IBM 7074 FORTRAN 
STANDARD-VECTOR DEVIATION ROSE IBM 7074 FORTRAN 
STATION DATA PARAMETER INVENTORY IBM 7074 FORTRAN 
STATION DATA PLOT - SIX VARIABLES IBM 7074 FORTRAN 
STATISTICAL ANALYSIS OF ICE DATA IBM 7074 FORTRAN 
TEMPERATURE AVGe SUMMARY BY 1-DEG SQeIBM 7074 FORTRAN 
TEMPERATURE DISTRIBUTION BY 1-DEG SQeIBM 7074 FURTRAN 
THERMOMe CORRe»s THERMOe DEPTH IBM 7074 FORTRAN 
2-DIMENSION POWER SPECTRUM (SWOP II) IBM 7074 FORTRAN 
VAM INTERPOLATION II IBM 7074 FORTRAN 
VERTICAL SECTION PLOT - STATION DATA IBM 7074 FORTRAN 
VERTICAL SUMMARY HISTOGRAM PLOT IBM 7074 FURTRAN 
VERTICAL TEMPERATURE GRADIENTS IBM 7074 FORTRAN 
WIND STRESS IBM 7074 FORTRAN 
VELOCITYs HORIZe EDDY COEFFIFIENTS IBM 709 FORTRAN 
FOURIER ANALYSIS IBM 7090 FORTRAN 
POWER SPECTRUM ANALYSIS IBM 70905 FORTRAN 
IBM 704 
TWO-DIMENSTONAL AUTOCORRELATION IBM 7090» FORTRAN 
IBM 1401 
CALCULATE AND PLOT TIME-TREND CURVES IBM7090/94FORTRAN > 
OCEANOGRAPHIC DATA PROGRAM F IBM 7094 FORTRAN 
WAVEIN AND DIFRAK IBM 7094 FORTRAN 


BOMM (TIME SERIES) 
SPECIFIC CONDUCTIVITY 


IBM OS/360FORTRAN 
IBM OS/360FORTRAN 


WAVES GENERATED BY TURBULENT WIND IBM 360/67FORTRAN 
DECCA HI-FIX PDP-5» 8S FORTRAN 
INDUCTIVE SALINOMETER SALINITY CONVe PDP-5s5 8S FORTRAN 
NEAR-FIELD ARRAY TESTING PDP-8 FORTRAN 
RETRIEVAL OF GEOPHYSICAL DATA NOT GIVEN FURTRAN 
SALINITY DISTRIBUTION IN ESTUARY NOT GIVEN FORTRAN 
CORE INFORMATION NOT GIVEN FORTRAN 
ASTRONOMIC LATITUDE NOT GIVEN FORTRAN 
GRIDITs REGRIDIT» AUTOMATED CONTOUR NOT GIVEN FORTRAN 
HY PERMAP NOT GIVEN FORTRAN 
RADIATION TEMP. OF SEA SURFACE NOT GIVEN FORTRAN 
RAY TRACING NOT GIVEN FORTRAN 
SEDIMENT TEXTURAL ANALYSIS NOT GIVEN FORTRAN 
SEQUENTIAL PLOTTING NOT GIVEN FORTRAN 
SONOBUOY FIXING ERROR NOT GIVEN FORTRAN 
WATERVEL (SOUND VELOCITY) NOT GIVEN FORTRAN 
DATA REDUCTION FOR THE CDC 3100 CDC 3100 FORTRAN 
ISALBP (SALINITY ANOMALY ) CDC 3100 FORTRAN 
ISATBP (OXYGEN ANOMALY AND SATe) CDC 3100 FORTRAN 
LEAST SQUARES CURVE FITTING CDC 3100 FORTRAN 
PLOT STATION POSITIONS CDC 3100 FORTRAN 
PLOT THETA-S CURVES CDC 3100 FORTRAN 
SVLIM (SOUND VELOCITY RETRIEVAL) CDC 3100 FORTRAN 
OCEANOGRAPHIC DATA COMPUTATION CDC 6400 FORTRAN 
SEDIMENT DATA CDC 6400 FURTRAN 


PAGE 129 


FAP 46 


II 14,583 
I! 10 
II 10 
It J 45 
II 36 
II 35 
If 1 101 
if 3 90 
pl 29 


SYNOPTIC PROGRAM 

STADAT 2 

DYNHT (DYNAMIC HEIGHTS) 

GRAIN SIZE 

PEN (POTENTIAL ENERGY ANOMALY ) 
POTEMP (POTENTIAL TEMPERATURE) 
VFREQ (VAISALA FREQUENCY COMP.) 
DYNAMIC HEIGHT CALCULATION 
MULTIVARIATE DISCRIMINANT ANALYSIS 
OCEANOe DATA PLOTTING FOR ICES DATA 
OCEANOe DATA PLOTTING FOR NODC DATA 
STANDARD-SIZE ANALYSIS OF SEDIMENTS 
TREND-SURFACE WITH UNRESTRICTED I/P 
TRANSPORT COMP. FROM ATMOS. 
CHLOROPHYLL AND CAROTENOID PIGMENT 
PROCESSING OF OCEANOGRAPHIC OBSe 
HARMONIC ANALYSIS OF TIDAL DATA 
BOTTOM REFLECTIVITY 

RAY TRACING 
SOUND VELOCITY 
PARAMETRIC MAP 


IN OCEAN WATER 


POINT GENERATOR FOR DISTANCE-AZIMUTH 


POINT GENERATOR FOR MAP PROJECTIONS 
MULTIVARIATE NON-LINEAR REGRESSION 
OCEANOGRAPHIC DATA COMPUTATION 
SEDIMENT DATA 

SEISMIC SLOPING LAYER 

ACOUSTIC RAY TRACING 

PROJECT COD LIVER 

CHLORINITY — SALINITY 

CONTINUOUS LINE SOURCE 

CONTINUOUS SOURCE PER UNIT DEPTH 
CONTINUOUS SOURCEs WITH 
DENSITY — THERMOSTERIC ANOMALY 
LATERAL RELATIVE DISTRIBUTION 
SURFACE WAVE RAYS 

TOTAL CO(2) 

MAGNETIC ANOMALIES AND GRADIENTS 
SYNOPTIC PROGRAM 


SEICHE ANALYSIS 
DAILY SEAWATER OBSERVATIONS 
CARBONATE-CARBON ANALYSIS OF SEDe 


PRESSURE 


COOLING TERM 


CDC 
GE 

GE 

GE 

GE 

GE 

GE 

IBM 
IBM 
IBM 
IBM 
IBM 
IBM 
IBM 
IBM 
18M 
IBM 
IBM 
IBM 
IBM 
IBM 
IBM 
IBM 
IBM 
IBM 
IBM 
IBM 
IBM 
IBM 
IBM 
IBM 
IBM 
IBM 
IBM 
IBM 
IBM 
IBM 
IBM 
IBM 
/7T0 
IBM 
IBM 
IBM 


CONSOLIDATION TESTS ON OCEAN SEDIMENTIBM 


DIRECT SHEAR TEST ON OCEAN SEDIMENT 
ENGe INDEX PROPe OF CORE SAMPLES 
GRAIN SIZE ANALYSIS - PLOT AND TAB 
PERMEABILITY TEST ON OCEAN SEDe 
SETTLEMENT ANALYSIS 

SUMMARY PLOTS OF SEDe TEST RESULTS 
TRIAXIAL COMPRESSION TEST 

DAILY SEAWATER OBSERVATIONS 

OCEANS CATALOGUE I AND II 

SUAVUSU MGS Wo gilt, ICI 


THERMOCHECK -— TEMPe CORRECTION 
CIRCSTAT 

BIOP (BIOLOGY PLOT) 

CHLOR 

PROFL 

SeTeDe DATA PROCESSING 


RAY TRACING 

SOUND SPEED PROFILES - NORMAL MODES 
CHLOROPHYLL AND PRODUCTIVITY 
INTERPOLATION PROGRAM 

MULTIVARIATE NON-LINEAR REGRESSION 
SIMULATION OF TRANSGRESSION IN TIME 
HARMONIC ANALYSIS OF TIDAL DATA 
TIDAL CURRENT PREDICTION 

ECOPROD 

JOB (SPECIES DIVERSITY) 


PAGE 130 


IBM 
IBM 
IBM 
IBM 
IBM 
IBM 
IBM 
CDC 
CDC 
CDC 
CDC 
CDC 
CDC 
CDC 
CDC 
CDC 
CDC 
CDC 
CDC 
CDC 
CDC 
CDC 
CDC 
CDC 
CDC 
CDC 


6400 FORTRAN 
200 SERFORTRAN 
225 FORTRAN 
225 FORTRAN 
225 FORTRAN 
225 FORTRAN 
225 FORTRAN 

1620 FORTRAN 

1620 FORTRAN 

1620 FORTRAN 

1620 FORTRAN 

1620 FORTRAN 

1620 FORTRAN 

1620 FORTRAN 


16201 I FORTRAN 
16201 IFORTRAN 
7030 FORTRAN 
704 FORTRAN 
704 FORTRAN 
704 FORTRAN 
7074 FORTRAN 
7074 FORTRAN 
7074 FORTRAN 
709 FORTRAN 
709 FORTRAN 
709 FORTRAN 
709 FORTRAN 
7090 FORTRAN 
7090 FORTRAN 
7094 FORTRAN 
7094 FORTRAN 
7094 FORTRAN 
7094 FORTRAN 
7094 FORTRAN 
7094 FORTRAN 
7094 FORTRAN 
7094 FORTRAN 
7094 FORTRAN 
7094-IIFORTRAN 
40 DCS 
360/50FORTRAN 
1620 FORTRAN 


16201 IFORTRAN 
16201 IFURTRAN 
16201 IFORTRAN 
162011 FORTRAN 
16201 IT FORTRAN 
162011 FORTRAN 


16201 IFORTRAN 
16201 I FORTRAN 
16201IFORTRAN 
3100 FORTRAN 
3100 FORTRAN 
3100 FORTRAN 
3100 FORTRAN 
3400 FORTRAN 
3600 FORTRAN 
3600 FORTRAN 
3600 FORTRAN 
3600 FURTRAN 
3800 FORTRAN 
3800 FORTRAN 
6400 FORTRAN 
6400 FORTRAN 
6400 FORTRAN 
6400 FORTRAN 
6600 FORTRAN 
6600 FORTRAN 
6600 FORTRAN 
6600 FORTRAN 


| 
gU0900000 


26 


OXYGEN CDC 6600 FORTRAN 
POWER SPECTRUM OF GEOLOGICAL SURFACE GE 625 FORTRAN 
TREND ANALYSIS USING FOURIER SERIES GE 625 FORTRAN 
OXYGEN COMPUTATION H-516 FORTRAN 
PHOSPHATE COMPUTATION H-516 FORTRAN 
SALINITY CONVERSION H-516 FORTRAN 
THERMOMETER CORRECTION H-516 FORTRAN 
SEAKEEP ING IBM 1130 FORTRAN 
ALERT (SATELLITE TIMES) IBM 1130 FORTRAN 
ASORT (SORT O/P OF ALERT) IBM 1130 FORTRAN 
ANALe OF NON-LINEAR RESPONSE SURFACESIBM 1130 FORTRAN 
HYDRO (COMPUTE FROM HYDRO DATA) IBM 1130 FORTRAN 
MULDA (MULTIPLE DISCRIMINANT ANAL.) IBM 1130 FORTRAN 
PLOG (PLOT HYDRO. DATA) IBM 1130 FORTRAN 
RYLD (FISH STOGK YIELD) IBM 1130 FORTRAN 
SPECIAL CHEMISTRY CALCULATIONS IBM 1130 FORTRAN 
SeTeDe CALCULATIONS IBM 1130 FORTRAN 
TRANSPORT COMP, FROM ATMOS. PRESSURE IBM 1130 FORTRAN 
STPO1l (PLOT SeTeDe DATA) IBM 1130 FORTRAN 
STPO2 (COMPUTE FROM SeTeDe DATA) IBM 1130 FORTRAN 
TREND-SURFACE WITH UNRESTRICTED I/P IBM 1620 FORTRAN 
BRAINCON DATA REDUCTION IBM 1800 FORTRAN 
CABLE CONFIGURATION IBM 1800 FORTRAN 
CURRENT METER ANALYSIS IBM 1800 FORTRAN 
CURRENT METER CONVERSION IBM 1800 FORTRAN 
HILO!s IBM 1800 FORTRAN 
HNAV (LORAN/DECCA COORDINATES CALCe) IBM 1800 FORTRAN 
HNV1 (LORAN/DECCA FILE) IBM 1800 FORTRAN 
SBWRO (WAVE RECORDER ANALYSIS) IBM 1800 FORTRAN 
SDANO (INVERSE GEODETIC) IBM 1800 FORTRAN 
VAPW (SATURATION VAPOR PRESSURE) IBM 1800 FORTRAN 
CADS (CALC. DEPENDENT QUANTITIES) IBM 1800 FORTRAN 
GO (POTe TEMPes SIGMA THETAs OXYe) IBM 1800 FORTRAN 
TWO FIVE (DATA REDUCTION) IBM 1800 FORTRAN 
TRANSPORT COMP. FROM ATMOSe PRESSURE IBM 7040 FORTRAN 
POWER SPECTRUM OF GEOLOGICAL SURFACE IBM 7040 FORTRAN 
TREND SURFACES DEGREES 1 TO 6 IBM 7040 FORTRAN 
SIMULATION OF MARINE SEDIMENTATION IBM 7040 FORTRAN 
2-DIMENSIONAL REGRESSION IBM 7040 FORTRAN 
CROSS-ASSOCIATION OF SEQUENCES IBM7040/44FORTRAN 
DIGITAL POWER SPECTRUM ANALYSIS IBM 7090 FORTRAN 
LONGe STRENGTH OF SHIP HULL IBM 7090 FORTRAN 
PARTIAL AND ORDINARY COHERENCE IBM 7090 FORTRAN 
SAVED (BLAST TEST DATA REDUCTION) IBM 7090 FORTRAN 
STATISTICAL AND PEAK-TO-PEAK ANAL. IBM 7090 FORTRAN 
ASTRONOMICAL TIDE PREDICTION IBM7090/94FORTRAN 
REFRACTION OF WAVES 1BM7090/94FORTRAN 
SIMULATION OF WIND-GENERATED WAVES IBM7090/94FORTRAN 
SEA ICE STUDIES I1BM7090/94FORTRAN 
SIMULATION OF MARINE SEDIMENTATION I1BM7090/94FORTRAN 
VECTOR TREND ANALe DIRECTIONAL DATA IBM7090/94FORTRAN 
WAVE FORCE DISTRIBUTION 1BM7090/94FORTRAN 
WAVE FORCES AND MOMENTS I1BM7090/94FORTRAN 
PROFIL (TSUNAMI PROFILES) IBM 7094 FORTRAN 
OPTIMIZATION OF VTE WATER PLANTS IBM 7094 FORTRAN 
SeTeDe CORRECTION IBM 7094 FORTRAN 
TIME TERMs SEISMIC REFRACTION INTERPeIBM 7094 FORTRAN 
CONDU (THERMAL CONDUCTIVITY) IBM7094-II FORTRAN 
77040 DCS 
BKGEOL (SEDIMENT STATISTICS) IBM7094-IIFORTRAN 
77040 DCS 
CONCENTRATIONS PER SQUARE METER 1BM7094-IIFORTRAN 
4/7040 DCS 
PHYTOPLANKTON NUMBERS» ETCe IBM7094—-IIFORTRAN 
77040 DCS 
SDGVEL (SOUNDING CORRECTION) 1BM7094-IIFORTRAN 
/7040 DCS 
SEDIMENT GRANULOMETRIC ANALYSIS I1BM7094-I IFORTRAN 
77040 DCS 


WAVE STATISTICS 


PAGE 131 


IBM OS/360FORTRAN 


IV 


IV 


102 


110 


BLACKY (TIME SERIES ANALYSIS) IBM OS/360FORTRAN 
CURRENT IBM OS/360FORTRAN 
DETRNDs ETCe (SPECTRA SUBROUT+NES) IBM 360/40FORTRAN 
LENG1 (WAVE LENGTH AND SPEED) IBM 360/40FORTRAN 
PROFILE IBM 360/40FORTRAN 
PROF1 (WATER ELEVe OVER WAVE PERIOD) IBM 360/40FURTRAN 
REFL1 (REFLECTED WAVE) IBM 360/40FORTRAN 
UMAXls»s ETCe (MAXe FLOW VELOC.) IBM 360/40FORTRAN 
UOFTls ETGCe (FLOW VELOCITIES) IBM 360/40FORTRAN 
INVENTORY PLOT IBM 360/40FORTRAN 
SUBROUTINE 'MAP!# IBM 360/40FORTRAN 
RAYTR (RAY-TRACING) IBM 360/44FORTRAN 
AOUsISAOU (CALCe OF OXYGEN» ETCe) IBM 360/65FORTRAN 
GDNP»GRAD (CALCe OF GRADIENTS) IBM 360/65FORTRAN 
GVPAsVPA (CALCe OF CURRENTS) IBM 360/65FORTRAN 
I1SOSsO0XOSsPHOS (ISENTROPIC PLOT) IBM 360/65FORTRAN 
LENGTH-WEIGHT FREQUENCY IBM 360/65FORTRAN 
LONG WAVE RADIATION IBM 360/65FORTRAN 
OCEANOGRAPHIC REPORT PREPARATION IBM 360/65FORTRAN 
OCEANOGRAPHIC SUMMARY (NOSe 19293) IBM 360/65FORTRAN 
REVERSING THERMOMETER CORRECTION IBM 360/65FORTRAN 
TSIPsTHOXsTHOT (PLOT TIME HISTORY) IBM 360/65FORTRAN 
FLOW METER PLOTS IBM 360/65FORTRAN 
GENERAL MERCATOR PLOT IBM 360/65FORTRAN 
HORIZONTAL SECTIONS IBM 360/65FORTRAN 
IN SITU OCEANOGRAPHIC DATA IBM 360/65FORTRAN 
INTERPOLATION IBM 360/65FORTRAN 
MERCATOR STATION PLOT IBM 360/65FORTRAN 
OXYGENs PHOSPHATEs DENSITY PLOTS IBM 360/65FORTRAN 
TEMPERATURE-SALINITY CURVES IBM 360/65FORTRAN 
OCEANS III IBM 360/65FORTRAN 
THERMOCHECK - TEMPe CORRECTION IBM 360/65FORTRAN 
WATER CHEMISTRY IBM 360/65FORTRAN 
Q-MODE CLUSTER ANALYSIS 1BM360/67 sFORTRAN 
1BM7090/94 
OPTIMUM TRACK SHIP ROUTING UNIVAC11O7FORTRAN 
NEWFIT UNIT VAC1108FORTRAN 
PATTERN FUNCTION CALCULATIONS UNIVAC1108FORTRAN 
RAY SORT UNIVAC1L1O8FORTRAN 
SONAR IN REFRACTIVE WATER UNIVAC1108FORTRAN 
SPECTRAL ANALYSIS OF TIME SERIES UNIVAC11O8FORTRAN 
AZIZ (THERMOMETRIC DEPTH) IBM 360/50FORTRAN 
CARDS IBM 360/50FORTRAN 
DELINT (DELTA CALC AND INTERPOLATION) IBM 360/50FURTRAN 
DEPTHS IBM 360/50FORTRAN 
HEIGHT IBM 360/50FORTRAN 
HYDRO IBM 360/50FORTRAN 
INTEST IBM 360/50FORTRAN 
LINT (LINEAR INTERPOLATION) IBM 360/50FORTRAN 
RDTHRM (READ THERMOMETER DATA) IBM 360/50FORTRAN 
SIGMA IBM 360/50FORTRAN 
SIGMAD IBM 360/50FORTRAN 
SIGMAT IBM 360/50FORTRAN 
TEMP IBM 360/50FORTRAN 
TSPLOT IBM 360/50FORTRAN 
UTEMP (UNPROTECTED THERMOMETER) IBM 360/50FORTRAN 
PERCENTAGE SATURATION OF OXYGEN IBM 360/65FORTRAN 
OBJECTIVE THERMOCLINE ANALYSIS CDC 6500 FORTRAN 
OBJECTIVE THERMOCLINE ANALYSIS IBM OS/360FORTRAN 
ASTRONOMIC POSITION IBM 360/65FORTRAN 
PROFILE CARD-TO-TAPE FOR GEOPAC IBM 360/65FORTRAN 
TALWANI 2-D GRAVITY IBM 360/65FORTRAN 
SIMULATION OF DELTAIC SEDIMENTATION IBM 360/67FORTRAN 
ATG (ADIABATIC TEMPERATURE GRADIENT SDS SIGMATFORTRAN 
BETA-MODEL WITH WHITE FORCING SDS SIGMA7FORTRAN 
DATA SDS SIGMA7FURTRAN 
DSTABF (STABILITY FREQUENCY) SDS SIGMA7FORTRAN 
HISTO (HISTOGRAM PLOT) SDS SIGMATFORTRAN 
HYLOG (HYDROs STAs DATA REDUCTION) SDS SIGMA7FORTRAN 
LISPLO (LIST AND PLOT) SDS SIGMA7FORTRAN 


PAGE 132 


NUSPEC 
OCCOMP 


(SPECTRUM ESTIMATION) 
(OCEANOGRAPHIC COMPUTE) 


POTEMP (POTENTIAL TEMPERATURE) 
PRESS 

PROVEC (PROGRESSIVE VECTORS) 
SCRUB (DATA EDIT AND CORRECT) 
SIGMAT 

SONVEL (SOUND VELOCITY) 

SPVOL 

STATS (STATISTICAL QUANTITIES) 
SVANOM (SPECIFIC VOLUME ANOMALY ) 
THISTO (TWO-DIMENe FREQGQe DISTRIBe) 
THRCL (THERMOMETER CALIBRATION) 
VECTAV (VECTOR AVERAGES) 

VEL (GEOSTROPHIC VELOCITY) 

VTR (VOLUME TRANSPORT ) 

Q@ FACTORS 

RAYMOR 

PSAL1 (PLOT TEMPERATURE-SALINITY) 
TCHK3 (THERMOMETER CORR.) 


TIME SERIES PLOTTING 

FILM DATA PROCESSING 

ICEGRID MODIFIED 

TIDES 

SEA SURFACE TEMPe AND ANOMALY SUM. 
SEA SURFACE TEMPe DATA SUMMARY 
SYNOPTIC MARINE WEATHER DATA SUMMARY 
VACOTS (VERTICAL SECTION PLOT) 
ACOUSTIC RAY TRACING 

DATUBA (BUOY-CABLE DEFLECTe) 
GENERAL VELOCITY FIELD 

HORIZONTAL GRADIENT RAY TRACING 
RAY TRACE PROCESSING 

TWO FIVE (DATA REDUCTION) 
ASTRONOMICAL TIDE PREDICTION 


MAC 


CURRENT METER DYNAMICS 
CHLOROPHYLL CALCULATIONS 
DELTA-ALPHA AND SIGMA-T 
HARMONIC ANALYSIS 

TIDAL PREDICTION 
VELOCITY OF SOUND 


MAD 


AVGe TEMPERATURES IN WATER COLUMN 
DYNAMIC HEIGHT AND CURRENT DYNAMICS 
GENERAL MAP PROJECTION 

MAP PROJECTION DISTORTIONS 
THEORETICAL RADIAL TIDAL FORCE 
TREND MAPs WITH RESIDUALS 

WIND CURRENTS 


PAL 


DISSOLVED OXYGENs POTENTIAL TEMP. 
OCEAN STATION ANALYSIS AND SUMMARY 
THERMOMETER CORRe AND THERMO. DEPTH 
DATA REDUCTION FOR THE PDP-8 


SCRAP 


SDS 
SDS 
SDS 
SDS 
SDS 
SDS 
SDS 
SDS 
SDS 
SDS 
SDS 
SDS 
SDS 
SDS 
SDS 
SDS 
ATLAS I 


SIGMA7FORTRAN 
SIGMA7FORTRAN 
SIGMATFORTRAN 
SIGMA7FORTRAN 
SIGMATFORTRAN 
SIGMATFORTRAN 
SIGMATFYURTRAN 
SIGMATFORTRAN 
SIGMA7FORTRAN 
SIGMA7FORTRAN 
SIGMATFURTRAN 
SIGMA7FORTRAN 
SIGMA7FORTRAN 
SIGMA7FORTRAN 
SIGMA7FORTRAN 
SIGMATFORTRAN 


FORTRAN V 


UNIVAC1108FURTRAN V 


IBM 1130 
IBM 1130 
cbc 3100 
CDC 1604 
CDC 1604 
NOT GIVEN 
CDC 3600 
CDC 3600 
CDC 3600 
CDC 3600 
CDC 3800 
CDC 3800 
CDC 3800 
CDC 3800 
CDC 3800 
CDC 3600 
CDC 6600 


FORTRAN VI 
FORTRAN VI 
FORTRAN-32 
FORTRAN-60 
FORTRAN-60 
FORTRAN-60 
FORTRAN-62 
FORTRAN-62 
FORTRAN-62 
FORTRAN-63 
FORTRAN-63 
FORTRAN-63 
FORTRAN-63 
FORTRAN-63 
FORTRAN-63 
FORTRAN-63 
FORTRAN-66 


IBM OS/360MAC 


NGS. Op 
vey LBOar1 
IcT 1301 
IMEI abeiloyat 
WEF short 


IBM 7090 
IBM 7090 
IBM 7090 
IBM 7090 
IBM 7090 
IBM 7090 
IBM 7090 


PDP-5» 8S 
PDP-5» 8S 
PDP-5» 8S 
PDP-8 


SUBSURFACE THERMAL STRUCTURE ANALYSISCDC 1604 


WAVES 


PAGE 133 


CDC 1604 


MAC 
MAC 
MAC 
MAC 
MAC 


MAD 
MAD 
MAD 
MAD 
MAD 
MAD 
MAD 


PAL 
PAL 
PAL 
PAL 


a ae) 
| 
mee 


SCRAP 
SCRAP 


105 
103 


81 
93 
65 
65 
104 
47 
68 


93 
93 
20 
14 


82 
106 


TWO DIMENSIONAL RAY TRACE 


OCEANS II REPORT GENERATO 
BATHYTHERMOGRAPH OUTPUT 


CONVERSIONs NODC TO ICES 
OCEAN STATION DATA OUTPUT 


OCEAN STATION DEPTH SUMMA 
STAe DATA CONVERSIONs COD 
COMPUTE GEOGRAPHIC POSITI 
LORAN C 


SeTeDe CALCULATIONS 
SATELLITE NAVIGATION 
GENERAL REGRESSION 
POWER SPECTRUM ANALYSIS 
THERMOMETER CORRECTIONS 
TIDAL ANALYSIS AND PREDIC 
BOMM (TIME SERIES) 

LINE PRINTER PLOTS 
BIOLOGICAL STATION FILE 
STATION DATA (ATLAS) 
AN/UYK-1 SOUND VELOCITY 


SPS 


R 


» NODC 

RY 

C TO NODC 
ONS 


MISCELLANEOUS 


TION 


PAGE 134 


CDC 1604» SCRAP, MAP 
CDC 3200 

IBM 1401 SPS 

IBM 1401 SPS 

IBM 1401 SPS 

IBM 1401 SPS 

IBM 1401 SPS 

IBM 1401 SPS 

IBM 1620 SPS 

IBM 1620 SPS 

IBM 1130 ASSEMBLER 
IBM 1801 ASSEMBLER 
IBM 360/65PL/1 
PB-250 BASIC 
MERCURY  CHLF 3/4 
MERCURY  CHLF 3/4 
CDC 3600 COMPASS 
CDC 3800 COMPASS 
ATLAS I EMA 

ATLAS 1. EMA 
AN/UYK-1 LOGANDS 


39. 


INDEX BY COMPUTER MAKE AND MODEL 


BURROUGHS 


2-DIMENSIONAL REGRESSION B5500 
SPECTRAL ANALYSIS OF TIME SERIES B5500 


CONTROL DATA CORPORATION 


FATHOMETER CORRECTION CDC 
MACHINE PLOTTING ON MERCATOR PROJ. CDC 
VC2AP3 SHIP ROUTING CDC 
FILM DATA PROCESSING CDC 
ICEGRID MODIFIED CDC 
DATA FIELD GRID EXPANSION CDC 
FORECASTING OF SURFACE CURRENTS CDC 
GG T SEA CDC 
POTENTIAL MIXED LAYER DEPTH CDC 
SEA SURFACE TEMPERATURE ANALYSIS CDC 
SUBSURFACE THERMAL STRUCTURE ANALYSISCDC 
TWO DIMENSTONAL RAY TRACE CDC 
WAVES CDC 
NUTRIENT CHEMISTRY CONCENTRATION CDC 
OCEAN STATION COMPUTATIONS CDC 
PRIMARY PRODUCTIVITY CDC 
RADIATION ATTENUATION CDC 
ZOOPLANKTON VOLUME CDC 
DATA REDUCTION FOR THE CDC 3100 CDC 
ISALBP (SALINITY ANOMALY ) CDC 
ISATBP (OXYGEN ANOMALY AND SATe) CDC 
LEAST SQUARES CURVE FITTING CDC 
PLOT STATION POSITIONS CDC 
PLOT THETA-S CURVES CDC 
SECTION PLOTTING CDC 
TEMPERATURE-SALINITY PLOT CDC 
SODANO INVERSE CDC 
SOUNDING PLOT CDC 
SVLIM (SOUND VELOCITY RETRIEVAL) CDC 
DAILY SEAWATER OBSERVATIONS CDC 
OCEANS CATALOGUE I AND II CDC 
STAT USUMES iO WHO > WITH CDC 
THERMOCHECK -— TEMPe CORRECTION CDC 
TIME SERIES PLOTTING CDC 
DATA FIELD GRID EXPANSION CDC 
BECNAV (BEACON NAVIGATION) CDC 
SPANS1A (BEACON POSITION) CDC 
SPANS1B (BEACON POSITION) CDC 
INTERPOLATION FOR OCEANOGRAPHIC DATA CDC 
POWER SPECTRA ESTIMATION CDC 
SOUND VELOCITY CDC 
FORECASTING OF SURFACE CURRENTS CDC 
POTENTIAL MIXED LAYER DEPTH CDC 
TWO DIMENSIONAL RAY TRACE CDC 
HYDROGRAPHIC DATA PROGRAM CDC 
RADIONUCLIDE SPECTRUM ANALYSIS (2) CDC 
TEMPERATURE CORRECTIONS CDC 
CIRCSTAT CDC 
BOMM (TIME SERIES) CDC 
PROGRAM REGROUP CDC 
BIOP (BIOLOGY PLOT) CDC 
CHLOR CDC 
PROFL CDC 
SeTeDe DATA PROCESSING CDC 
SEA SURFACE TEMPe AND ANOMALY SUM. CDC 
SEA SURFACE TEMPe DATA SUMMARY CDC 
SYNOPTIC MARINE WEATHER DATA SUMMARY CDC 
VACOTS (VERTICAL SECTION PLOT) CDC 


PAGE 135 


1604 
1604 
1604 
1604 
1604 
1604 
1604 
1604 
1604 
1604 
1604 
1604 
1604 
1604 
1604 
1604 
1604 
1604 
3100 
3100 
3100 
3100 
3100 
3100 
3100 
3100 
3100 
3100 
3100 
3100 
3100 
3100 
3100 
3100 
3100 
3200 
3200 
3200 
3200 
3200 
3200 
3200 
3200 
3200 
3300 
3300 
3300 
3400 
3600 
3600 
3600 
3600 
3600 
3600 
3600 
3600 
3600 
3600 


ALGOL 
ALGOL 60 


FORTRAN 
FORTRAN 
FORTRAN 
FORTRAN-60 
FORTRAN-60 
MACHINE 
MACHINE 
MACHINE 
MACHINE 
MACHINE 
SCRAP 
SCRAP» MAP 
SCRAP 

(NOT GIVEN) 
(NOT GIVEN) 
(NOT GIVEN) 
(NOT GIVEN) 
(NOT GIVEN) 
FORTRAN II 
FORTRAN II 
FORTRAN II 
FORTRAN II 
FORTRAN I 
FORTRAN I 
FORTRAN 
FORTRAN 
FORTRAN 
FORTRAN 
FORTRAN II 
FORTRAN IV 
FORTRAN IV 
FORTRAN IV 
FORTRAN IV 
FORTRAN-32 
MACHINE 
FORTRAN 
FORTRAN 
FORTRAN 
FORTRAN 
FORTRAN 
FORTRAN 
MACHINE 
MACHINE 
SCRAP» MAP 
FORTRAN 
FORTRAN 
FORTRAN 
FORTRAN IV 
COMPASS 
FORTRAN 
FORTRAN IV 
FORTRAN IV 
FORTRAN IV 
FORTRAN IV 
FORTRAN-62 
FORTRAN-62 
FORTRAN-62 
FORTRAN-63 


45 


14583 


TWO FIVE (DATA REDUCTION) 
BLACKBODY RADIANCE 

BLACKBODY SPECTRAL RADIANCE 
DETERMINANT OF A SYMMETRIC MATRIX 
DISTANCE BETWEEN TWO POINTS 
EVALUATE BESSEL FUNCTIONS 

FIND REAL ZEROS OF FUNCTION 

GREAT CIRCLE PATHS FROM A POINT 
GREAT CIRCLE RETRIEVAL 

LINE PRINTER PLOTS 


NELEDIT 

PROPAGATION LOSS — NORMAL MODES 
SCALING SUBROUTINE 
THREE-DIMENSIONAL SURFACE PLOTS 

WIT Me UNS 

RAY TRACING 

SOUND SPEED PROFILES - NORMAL MODES 
ACOUSTIC RAY TRACING 

DATUBA (BUOY-CABLE DEFLECT.) 
GENERAL VELOCITY FIELD 

HORIZONTAL GRADIENT RAY TRACING 
RAY TRACE PROCESSING 

WAVEIN AND DIFRAK 

OCEANOGRAPHIC DATA COMPUTATION 
SEDIMENT DATA 

SYNOPTIC PROGRAM 

CHLOROPHYLL AND PRODUCTIVITY 
INTERPOLATION PROGRAM 

MULTIVARIATE NON-LINEAR REGRESSION 
SIMULATION OF TRANSGRESSION IN TIME 
OBJECTIVE THERMOCLINE ANALYSIS 
TRLOSS (TRANSMISSION LOSS) 
HARMONIC ANALYSIS OF TIDAL DATA 
TIDAL CURRENT PREDICTION 

ECOPROD 

JOB (SPECIES DIVERSITY) 

OXYGEN 

ASTRONOMICAL TIDE PREDICTION 


CDC 
CDC 
CDC 
CDC 
CDC 
CDC 
CDC 
CDC 
CDC 
CDC 


CDC 
CDC 
CDC 
CDC 
CDC 
CDC 
CDC 
CDC 
CDC 
CDC 
CDC 
CDC 
CDC 
CDC 
CDC 
CDC 
CDC 
CDC 
CDC 
CDC 
CDC 
CDC 
CDC 
CDC 
CDC 
CDC 
CDC 
CDC 


3600 
3800 
3800 
3800 
3800 
3800 
3800 
3800 
3800 
3800 


3800 
3800 
3800 
3800 
3800 
3800 
3800 
3800 
3800 
3800 
3800 
3800 
6400 
6400 
6400 
6400 
6400 
6400 
6400 
6400 
6500 
6600 
6600 
6600 
6600 
6600 
6600 
6600 


DIGITAL EQUIPMENT CORPORATION 


DECCA HI-FIX 

INDUCTIVE SALINOMETER SALINITY CONVe 
DISSOLVED OXYGEN» POTENTIAL TEMPe 
OCEAN STATION ANALYSIS AND SUMMARY 
THERMOMETER CORRe AND THERMO. DEPTH 
RICHARDSON CURRENT METER FILM READe 
THE VORTEX OCEAN MODEL 

WORLD OCEANOe DATA DISPLAY 
NEAR-FIELD ARRAY TESTING 

DATA REDUCTION FOR THE PDP-8 


PDP 
PDP 
PDP 
PDP 
PoP 
PDP 
PoP 
PDP 
PDP 
PoP 


GENERAL ELECTRIC 


STADAT 2 

CRVFT (LEAST SQUARES FIT) 

ORD 1 (OLMSTED RAY DIAGRAM NOe 1) 
ORD 2 (OLMSTED RAY DIAGRAM NOe 2) 
DYNHT (DYNAMIC HEIGHTS) 

GRAIN SIZE 

PEN (POTENTIAL ENERGY ANOMALY ) 
POTEMP (POTENTIAL TEMPERATURE) 
VFREQ (VAISALA FREQUENCY COMP .e) 
POWER SPECTRUM OF GEOLOGICAL SURFACE 
TREND ANALYSIS USING FOURIER SERIES 


PAGE 136 


—-5> 8S 
—5s 8S 
—-55 8S 
-5» 8S 
—5s5 8S 
-7(9) 
—1/ (6 ))) 
-7(9) 
=38 

-8 


FORTRAN- 


FORTRAN 
FORTRAN 
FORTRAN 
FURTRAN 
FORTRAN 
FORTRAN 
FORTRAN 
FURTRAN 
FORTRAN 
COMPASS 
FORTRAN 
FORTRAN 
FORTRAN 
FORTRAN 
FURTRAN 
FORTRAN 
FORTRAN 


FORTRAN— 
FORTRAN-— 
FURTRAN- 
FORTRAN-— 
FURTRAN- 


FORTRAN 
FORTRAN 
FORTRAN 
FORTRAN 
FORTRAN 
FORTRAN 
FURTRAN 
FORTRAN 
FORTRAN 
FORTRAN 
FORTRAN 
FORTRAN 
FORTRAN 
FORTRAN 
FORTRAN 


FORTRAN- 


FORTRAN 
FURTRAN 
PAL III 
PAL III 
PAL III 
DECAL 

DECAL 

DECAL 

FORTRAN 
PAL III 


200 SERFORTRAN 


22S) 
225 
225 
225 
225 
225 
225 
225 
625 
625 


FORTRAN 
FORTRAN 
FURTRAN 
FORTRAN 
FORTRAN 
FORTRAN 
FORTRAN 
FURTRAN 
FORTRAN 
FORTRAN 


63 


IV 
IV 
63 
63 
63 
63 
63 


96 


509110 


Tel 
Tal 


90 
29 


II 1890 


IV 
IV 
IV 
IV 
IV-H 


IV 
IV 
IV 
IV 
IV 
66 


II 


Il 
II 
Il 
Tod 
Tal 
IV 
IV 


05 
90 
47 
54 
75 
94 

103 

104 
05 
06 
06 

104 


HONEYWELL 


OXYGEN COMPUTATION H-516 FORTRAN IV 11 
PHOSPHATE COMPUTATION H-516 FORTRAN IV ial 
SALINITY CONVERSION H-516 FORTRAN IV 11 
THERMOMETER CORRECTION H-516 FURTRAN IV 16 
IBM 
REDUCTION» DISPLAY OF SEA DATA IBM 1130 FORTRAN 14525560 
SeTeDe CALCULATIONS IBM 1130 ASSEMBLER 18 
DEAD RECKONING NAVIGATION SYSTEM IBM 1130 FORTRAN 60 
SeTeDe EDIT AND INTERPOLATE IBM 1130 FORTRAN 86 
UNDERWAY DATA SYSTEM IBM 1130 FORTRAN 18 
SEAKEEPING IBM 1130 FORTRAN IV 109 
ALERT (SATELLITE TIMES) IBM 1130 FORTRAN IV 58 
ASORT (SORT O/P OF ALERT) IBM 1130 FURTRAN Iv 58 
ANALe OF NON-LINEAR RESPONSE SURFACESIBM 1130 FORTRAN Iv 52 
HYDRO (COMPUTE FROM HYDRO DATA) IBM 1130 FORTRAN Iv 84 
MULDA (MULTIPLE DISCRIMINANT ANAL.) IBM 1130 FORTRAN Iv 3)2) 
PLOG (PLOT HYDRO. DATA) IBM 1130 FORTRAN Iv 36 
REDE FAIS HI STOGK Vane bn IBM 1130 FORTRAN IV 05 
STPO1l (PLOT SeTeDe DATA) IBM 1130 FORTRAN IV B37 
STPO2 (COMPUTE FROM SeTeDe DATA) IBM 1130 FORTRAN IV 84 
SPECIAL CHEMISTRY CALCULATIONS IBM 1130 FORTRAN IV 09 
SeTeDe CALCULATIONS IBM 1130 FORTRAN Iv 18 
TRANSPORT COMP. FROM ATMOS. PRESSURE IBM 1130 FURTRAN IV 67 
PSAL1 (PLOT TEMPERATURE-SALINITY) IBM 1130 FURTRAN VI 37 
TCHK3 (THERMOMETER CORRe) IBM 1130 FORTRAN VI 16 
JOB EDIT FOR L—Z PROGRAM IBM 1401 AUTOCODER Au 
OCEAN STAe CURVE PLOTTING FOR 1401 IBM 1401 AUTOCODER 38 
TEMPERATURE AND DEPTH CALCULATIONS IBM 1401 AUTOCODER 16 
COMPUTE ADVECTION IBM 1401 FORTRAN 69 
TWO-DIMENSTONAL AUTOCORRELATION IBM 1401 FORTRAN 56 
OCEANS II REPORT GENERATOR IBM 1401 SPS 23 
BATHYTHERMOGRAPH OUTPUT IBM 1401 SPS 23 
CONVERSION, NODC TO ICES IBM 1401 SPS 23 
OCEAN STATION DATA OUTPUT» NODC IBM 1401 SPS 15 
OCEAN STATION DEPTH SUMMARY IBM 1401 SPS 82 
STAe DATA CONVERSIONs CODC TO NODC IBM 1401 SPS 24 
ALKALINITY AND SPECIFIC ALKALINITY IBM 1620 FURTRAN 09 
INTERPOLATION FOR OCEANOGRAPHIC DATA IBM 1620 FURTRAN 83 
SALINITY VALUE CALCULATION IBM 1620 FORTRAN 09 
TEMPERATURE AND DEPTH CALCULATIONS IBM 1620 FORTRAN 16 
THERMOCHECK II -— TEMPe CORRECTION IBM 1620 FORTRAN Ly 
VELOCITY OF SOUND IBM 1620 FORTRAN 102 
TRANSPORT COMP. FROM ATMOS. PRESSURE IBM 1620 FORTRAN II 67 
DYNAMIC HEIGHT CALCULATION IBM 1620 FORTRAN II 90 
MULTIVARIATE DISCRIMINANT ANALYSIS IBM 1620 FORTRAN II 55 
OCEANOe DATA PLOTTING FOR ICES DATA IBM 1620 FURTRAN II 43 
OCEANOe DATA PLOTTING FOR NODC DATA IBM 1620 FORTRAN II 43 
STANDARD-SIZE ANALYSIS OF SEDIMENTS IBM 1620 FORTRAN II 29 
TREND-SURFACE WITH UNRESTRICTED I/P IBM 1620 FORTRAN IIs 47 
IV, BALGOL 
DAILY SEAWATER OBSERVATIONS IBM 1620 FORTRAN II-D 79 
COMPUTE GEOGRAPHIC POSITIONS tM) S20 SRS 61 
LORAN C q BMG ZON eSIEIS 62 
CHLOROPHYLL AND CAROTENOTD PIGMENT IBM 16201IFURTRAN [I 05 
PROCESSING OF OCEANOGRAPHIC OBS. IBM 1620I1IFURTRAN [I 70 
CARBONATE-CARBON ANALYSIS OF SEDe IBM 1620I1IFORTRAN II-D 29 
CONSOLIDATION TESTS ON OCEAN SEDIMENTIBM 1620I1IFORTRAN II-D 30 
DIRECT SHEAR TEST ON OCEAN SEDIMENT IBM 1620I1IFORTRAN II-D 30 
ENGe INDEX PROPe OF CORE SAMPLES IBM 16201IFORTRAN II-D 29 
GRAIN SIZE ANALYSIS — PLOT AND TAB IBM 16201IFORTRAN II-D 29 
PERMEABILITY TEST ON OCEAN SEDeo IBM 16201IFORTRAN II-D 30 
SETTLEMENT ANALYSIS IBM 1620I1IFORTRAN II-D 31 
SUMMARY PLOTS OF SEDe TEST RESULTS IBM 16201IFORTRAN II-D 31 
TRIAXIAL COMPRESSION TEST IBM 1620IIFORTRAN II-D 30 
ALPHA (SPECIFIC VOLUME) IBM 1800 FORTRAN 85 


PAGE 137 


BARTLETT'S CURVE FITTING IBM 1800 FURTRAN 46 


CLUSTER ANALYSIS IBM 1800 FORTRAN 55 
POTLT (POTENTIAL TEMPERATURE) IBM 1800 FORTRAN 85 
SATELLITE NAVIGATION IBM 1800 FORTRAN AND 58 
ASSEMBLER 
SDVEL IBM 1800 FORTRAN 102 
SIGMO IBM 1800 FORTRAN 85 
SIGMT IBM 1800 FORTRAN 85 
2D MAGNETIC ANOMALIES IBM 1800 FORTRAN 26 
BRAINCON DATA REDUCTION IBM 1800 FORTRAN IV 15 
CABLE CONFIGURATION IBM 1800 FORTRAN IV 73 
CURRENT METER ANALYSIS IBM 1800 FORTRAN IV 73 
CURRENT METER CONVERSION IBM 1800 FORTRAN IV 73 
HILOW IBM 1800 FURTRAN Iv 48 
HNAV (LORAN/DECCA COORDINATES CALC.) IBM 1800 FURTRAN IV 63 
HNV1 (LORAN/DECCA FILE) IBM 1800 FURTRAN IV 63 
SBWRO (WAVE RECORDER ANALYSIS) IBM 1800 FORTRAN IV 48 
SDANO (INVERSE GEODETIC) IBM 1800 FORTRAN IV 63 
VAPW (SATURATION VAPOR PRESSURE) IBM 1800 FURTRAN IV 66 
CADS (CALC. DEPENDENT QUANTITIES) IBM 1800 FORTRAN IV 84 
GO (POTs TEMPes SIGMA THETA, OXYe) IBM 1800 FORTRAN Iv 85 
TWO FIVE (DATA REDUCTION) IBM 1800 FORTRAN IV 17 
HARMONIC ANALYSIS OF TIDAL DATA IBM 7030 FURTRAN [I 103 
POWER SPECTRUM ANALYSIS IBM 704 FORTRAN 50 
BOTTOM REFLECTIVITY IBM 704 FORTRAN JI 99 
RAY TRACING IBM 704 FORTRAN II 99 
SOUND VELOCITY IN OCEAN WATER IBM 704 FORTRAN II 102 
WAVE SHOALING IBM 7040 FORTRAN 107 
POWER SPECTRUM OF GEOLOGICAL SURFACE IBM 7040 FORTRAN IV 54 
SIMULATION OF MARINE SEDIMENTATION IBM 7040 FORTRAN IV 33 
TREND SURFACES DEGREES 1 TO 6 IBM 7040 FORTRAN IV 47 
2-DIMENSIONAL REGRESSION IBM 7040 FORTRAN IV 45 
TRANSPORT COMP. FROM ATMOSe PRESSURE IBM 7040 FORTRAN IV 67 
CROSS-ASSOCIATION OF SEQUENCES IBM7040/44FORTRAN IV 54 
BATHYTHERMOGRAPH DATA CONVERTER IBM 7074 AUTOCODER 82 
BIODETERIORATION IBM 7074 AUTOCODER 06 
DEVIATION OF TEMPe AND SALINe PART 1 IBM 7074 AUTOCODER 75 
DRIFT BOTTLE DATA COMPUTATION IBM 7074 AUTOCODER 70 
GRADIENT SUMMARY BY 1-DEG SQes» MONTH IBM 7074 AUTOCODER 76 
MODIFIED SURFACE CURRENTS IBM 7074 AUTOCODER 68 
BT ANALYSIS (S.EeReCe DATA) IBM 7074 AUTOCODER 76 
STATION DATA COMPUTE IBM 7074 AUTOCODER 82 
STATION DATA VERTICAL ARRAY SUMMARY IBM 7074 AUTOCODER 78 
STATISTICAL SURFACE CURRENT ROSE IBM 7074 AUTOCODER 69 
SURFACE CURRENT SUMMARY IBM 7074 AUTOCODER 68 
TAPE INPUT AND OUTPUT SUBROUTINE IBM 7074 AUTOCODER 21 
THERMOCLINE AND MIXED LAYER DEPTHS IBM 7074 AUTOCODER 76 
THERMOCLINE ONE-DEGREE IBM 7074 AUTOCODER 78 
AIR-SEA IBM 7074 FORTRAN 66 
BATHYMETRIC DATA REDUCTION IBM 7074 FURTRAN 18 
BATHYTHERMOGRAM COMPOSITE PLOT IBM 7074 FORTRAN 41 
BOTTOM REFLECTION ANALYSIS IBM 7074 FORTRAN 98 
BOTTOM SEDIMENT DISTRIBUTION PLOT IBM 7074 FORTRAN 33 
BT TEMPERATURE GRADIENT DISTRIBUTION IBM 7074 FORTRAN 76 
CIRAZD (DISTANCE-AZIMUTH CALCe) IBM 7074 FURTRAN 61 
CIRCULAR CHARTING IBM 7074 FURTRAN 61 
CLOUD COVER AND DAILY SEA TEMPERATUREIBM 7074 FORTRAN 66 
CONVERGENCE ZONE RANGE IBM 7074 FORTRAN 98 
CRITICAL ACOUSTIC RATIO IBM 7074 FORTRAN 98 
CRUISE TRACK IBM 7074 FORTRAN 41 
CURRENT METER TURBULENCE IBM 7074 FORTRAN 72 
DENSITY GRADIENT BY 1-DEGREE SQUARE IBM 7074 FORTRAN 78 
DENSITY-SALINITY LINEAR INTERPOL. IBM 7074 FORTRAN 86 
DENSITY-SALINITY MID PLOT IBM 7074 FORTRAN 42 
ERROR IN VERTICAL SOUND VELOCITY IBM 7074 FORTRAN 101 
FAA PLOT IBM 7074 FORTRAN 35 
GENERAL PURPOSE PLOT IBM 7074 FORTRAN 37 
GEODETIC DATUM CONVERSION IBM 7074 FORTRAN 61 
GEODETIC DATUM REDUCTION IBM 7074 FORTRAN 61 
GEODETIC POSITION COMP. AND PLOT IBM 7074 FORTRAN 62 


PAGE 138 


GEOLOGICAL SAMPLE CONVERSION 
GEOLOGICAL SAMPLING INVENTORY PLOT 
GULF STREAM PATH 

ICE POTENTIAL 

INTERPOLATION OF OCEAN STATION DATA 
INTERPOLATION SPECIFIC VOL ANOMALY 
LAYER DEPTH PLOT 

LEAST SQUARES PLOT 

LIGHT AND SOUND INSTRUCTION B 

LIGHT AND SOUND INSTRUCTION D 

LORAN A AND C SKYWAVE 

LORAN — COORDINATE COMPUTATION 

LORAN EDIT 

LORAN TO GEOGRAPHIC CONVERSION 
MARINE BIOLOGe ENVIRONe SUMMARIES 
MARSDEN SQes AVERAGES FROM GEOFILE 
MASS PHYSICAL PROPERTIES 

MONTHLY SONIC LAYER DEPTH 
OBSERVATION DRAPING (GRAVITY) 

OXYGEN SATURATION 

PREDICTION OF VERTICAL TEMP. CHANGE 
RAY PATH 

SALINITY — CONDUCTIVITY FORMULA 
SALINITY DEVIATION PROGPLOT 

SALINITY GRADIENT BY 1-DEGREE SQUARE 
SEA SURFACE TEMPERATURE DISTRIBUTION 
SEA SENSE -— DATA DISPLAY 

Sie/\ SENSE > (NLT 

SEA SENSE — STANDARD DEVIATION 
SEAMOUNT MAGNETIZATION 

SEDIMENT “STZeE 

SHIPBOARD SURVEY -- ON-STATION MODE 
SHIPBOARD SURVEY -- ON-STATION PLOT 
SIGMA-T VS DEPTHs SALINITY (PLOT) 
SINGLE INTEGRATION 

SOLAR RADIATION CONVERSION 

SOUND SPEED EDIT 

SOUND VELOCITY DEPTH PROFILES 
SOUNDING PLOT 

STANDARD-VECTOR DEVIATION ROSE 
STATION DATA PARAMETER INVENTORY 
STATION DATA PLOT — SIX VARIABLES 
STATISTICAL ANALYSIS OF ICE DATA 
TEMPERATURE AVGe SUMMARY BY 1-DEG SQ. 
TEMPERATURE DISTRIBUTION BY 1-DEG SQ. 
THERMOMe CORRes THERMOe DEPTH 
2-DIMENSION POWER SPECTRUM (SWOP IT) 
VAM INTERPOLATION II 

VERTICAL SECTION PLOT — STATION DATA 
VERTICAL SUMMARY HISTOGRAM PLOT 
VERTICAL TEMPERATURE GRADIENTS 

WIND STRESS 

PARAMETRIC MAP 

POINT GENERATOR FOR DISTANCE-AZIMUTH 
POINT GENERATOR FOR MAP PROJECTIONS 
CHLOROPHYLL AND PRODUCTIVITY 
VELOCITY» HORIZe EDDY COEFFIFIENTS 
MULTIVARIATE NON-LINEAR REGRESSION 
OCEANOGRAPHIC DATA COMPUTATION 
SEDIMENT DATA 

SEISMIC SLOPING LAYER 

FOURIER ANALYSIS 

POWER SPECTRUM ANALYSIS 
TWO-DIMENSTONAL AUTOCORRELAT ION 
ACOUSTIC RAY TRACING 

PROJECT COD LIVER 


DIGITAL POWER SPECTRUM ANALYSIS 
LONGe STRENGTH OF SHIP HULL 
PARTIAL AND ORDINARY COHERENCE 


RAGE ASS) 


IBM 
IBM 
IBM 
IBM 
IBM 
IBM 
IBM 
IBM 
18M 
IBM 
IBM 
IBM 
IBM 
IBM 
183M 
IBM 
IBM 
IBM 
IBM 
IBM 
18M 
IBM 
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IBM 
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IBM 
IBM 
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IBM 
IBM 
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IBM 
IBM 
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IBM 
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IBM 


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7090 
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FORTRAN 
FORTRAN 
FORTRAN 
FORTRAN 
FORTRAN 
FORTRAN 
FORTRAN 
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FORTRAN 
FORTRAN 
FORTRAN 
FORTRAN 
FORTRAN 
FORTRAN 
FORTRAN 
FORTRAN 
FORTRAN 
FORTRAN 
FORTRAN 
FORTRAN 
FORTRAN 
FORTRAN 
FORTRAN 
FORTRAN 
FORTRAN 
FORTRAN 
FORTRAN 
FORTRAN 
FORTRAN 
FORTRAN 
FORTRAN 
FORTRAN 
FORTRAN 
FORTRAN 
FORTRAN 
FORTRAN 
FORTRAN 
FORTRAN 
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FORTRAN 
FORTRAN 
FORTRAN 
FORTRAN 
FURTRAN 
FORTRAN 
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FORTRAN 
FORTRAN 


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IV 110 
IV 49 


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DYNAMIC HEIGHT AND CURRENT DYNAMICS 
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PAGE 140 


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AND MAP 
FORTRAN 
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MAD 
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IBM 
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IBM7090/94FORTRAN 
I1BM7090/94FORTRAN 
IBM7090/94FORTRAN 
IBM7090/94FORTRAN 
IBM7090/94FORTRAN 
IBM7090/94FORTRAN 
1BM7090/94FORTRAN 
IBM7090/94FORTRAN 
1BM7090/94FORTRAN 
1BM7090/94FORTRAN 
IBM 7094 FORTRAN 
IBM 7094 FORTRAN 
IBM 7094 FORTRAN 
IBM 7094 FORTRAN 
IBM 7094 FORTRAN 
IBM 7094 FORTRAN 
IBM 7094 FORTRAN 
IBM 7094 FORTRAN 
IBM 7094 FORTRAN 
IBM 7094 FORTRAN 
IBM 7094 FORTRAN 
IBM7094-I IFORTRAN 
7/7040 DCS 
IBM 7094 
IBM 7094 
IBM 7094 
IBM 7094 FORTRAN 
IBM 7094 FORTRAN 
IBM7094-IIFURTRAN 
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IBM7094-IIFURTRAN 
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IBM7094-IIFURTRAN 
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IBM7094-IIFORTRAN 
7/7040 DCS 
IBM7094-I IFORTRAN 
77040 DCS 
1BM7094-IIFORTRAN 
77040 DCS 
1BM7094-I IFORTRAN 
77040 DCS 

IBM OS/360FORTRAN 
IBM OS/360FORTRAN 
IBM OS/360FORTRAN 
IBM 0S/360FORTRAN 
IBM OS/360FURTRAN 
IBM OS/360FORTRAN 
IBM OS/360FURTRAN 
IBM O0S/360MAC 

IBM 360/40FURTRAN 
IBM 360/40FORTRAN 
IBM 360/40FORTRAN 
IBM 360/40FYRTRAN 
IBM 360/40FORTRAN 
IBM 360/40FURTRAN 
IBM 360/40FORTRAN 
IBM 360/40FORTRAN 


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11 70 
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11 12 
II 26 
87 

II 18,90 
iV LOY 
IV 33 
IV 12 
IV 19 
IV 27 
IV 31 
IV 31 
IV o7 
IV o7 
ty  IO2 
IV 32 
II 18590 
IV 56 
52 

11 

TRV TETO 
IV 49 
IV 56 
IV-H 75 
72 

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1V 48 
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IV. 108 
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IV. 108 
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UOFT1» ETC. (FLOW VELOCITIES) 
GRAPHIC SYSTEM FOR CURVE FITTING 
RAYTR (RAY-TRACING) 

SEICHE ANALYSIS 


AZIZ 
CARDS 
DELINT 
DEPTHS 
HE I GHT 
HYDRO 
INTEST 
LINT (LINEAR INTERPOLATION) 
RDTHRM (READ THERMOMETER DATA) 
SIGMA 
SIGMAD 
SIGMAT 
TEMP 
TSPLOT 
UTEMP 
AOU s ISAQU 


(THERMOMETRIC DEPTH) 


(DELTA CALC AND 


(UNPROTECTED THERMOMETER) 
(CALCe OF OXYGENs ETCe) 
GDNPsGRAD (CALCe OF GRADIENTS) 
GVPAsVPA (CALC. OF CURRENTS) 
ITSOSsOXOSsPHOS (ISENTROPIC PLOT) 
LENGTH-WEIGHT FREQUENCY 

LONG WAVE RADIATION 

OCEANOGRAPHIC REPORT PREPARATION 
OCEANOGRAPHIC SUMMARY (NOSe 192593) 
REVERSING THERMOMETER CORRECTION 
TSIPsTHOXsTHOT (PLOT TIME HISTORY) 
FLOW METER PLOTS 

GENERAL MERCATOR PLOT 

HORIZONTAL SECTIONS 

IN SITU OCEANOGRAPHIC DATA 
INTERPOLATION 

MERCATOR STATION PLOT 

OXYGENs PHOSPHATEs DENSITY PLOTS 
TEMPERATURE-SALINITY CURVES 
OCEANS III 
THERMOCHECK II - 
WATER CHEMISTRY 
PERCENTAGE SATURATION OF OXYGEN 
ASTRONOMIC POSITION 

PROFILE CARD-TO-TAPE FOR GEOPAC 
TALWANI 2-D GRAVITY 

GENERAL REGRESSION 

WAVES GENERATED BY TURBULENT WIND 
Q-MODE CLUSTER ANALYSIS 


TEMP. CORRECTION 


SIMULATION OF DELTAIC SEDIMENTATION 


INTERPOLATION) 


IBM 
IBM 
IBM 
IBM 


IBM 
IBM 
IBM 
IBM 
IBM 
IBM 
IBM 
IBM 
IBM 
IBM 
IBM 
IBM 
IBM 
IBM 
IBM 
IBM 
IBM 
IBM 
IBM 
IBM 
IBM 
IBM 
IBM 
IBM 
IBM 
IBM 
IBM 
IBM 
IBM 
IBM 
IBM 
IBM 
IBM 
IBM 
IBM 
IBM 
IBM 
IBM 
IBM 
IBM 
IBM 
IBM 
IBM 
IBM 


XEROX DATA SYSTEMS 


ATG (ADIABATIC TEMPERATURE GRADIENT 
BETA-MODEL WITH WHITE FORCING 
DATA 

DSTABF (STABILITY FREQUENCY ) 

HISTO (HISTOGRAM PLOT) 

HYLOG (HYDROe STAe DATA REDUCTION) 
LISPLO (LIST AND PLOT) 

NUSPEC (SPECTRUM ESTIMATION) 
OCCOMP (OCEANOGRAPHIC COMPUTE) 
POTEMP (POTENTIAL TEMPERATURE) 
PRESS 

PROVEC (PROGRESSIVE VECTORS) 

SCRUB (DATA EDIT AND CORRECT) 
SIGMAT 

SONVEL (SOUND VELOCITY) 

SPVOL 

STATS (STATISTICAL QUANTITIES) 


PAGE 141 


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360/40FORTRAN 


IV 


360/40(NOT GIVEN) 


360/44FORTRAN 
360/50ALGOL ,» 
FORTRAN 
360/50FORTRAN 
360/50FORTRAN 
360/50FURTRAN 
360/50FORTRAN 
360/50FORTRAN 
360/50FORTRAN 
360/50FORTRAN 
360/50FORTRAN 
360/50FORTRAN 
360/50FORTRAN 
360/50FORTRAN 
360/50FORTRAN 
360/50FORTRAN 
360/50FORTRAN 
360/50FORTRAN 
360/65FORTRAN 
360/65FORTRAN 
360/65FORTRAN 
360/65FORTRAN 
360/65FORTRAN 
360/65FORTRAN 
360/65FORTRAN 
360/65FORTRAN 
360/65FORTRAN 
360/65FORTRAN 
360/65FURTRAN 
360/65FORTRAN 
360/65FORTRAN 
360/65FORTRAN 
360/65FORTRAN 
360/65FORTRAN 
360/65FORTRAN 
360/65FORTRAN 
360/65FORTRAN 
360/65FORTRAN 
360/65FORTRAN 
360/65FORTRAN 
360/65FORTRAN 
360/65FORTRAN 
360/65FORTRAN 
360/65PL/1 
360/67FORTRAN 
360/67FORTRAN 
360/67FURTRAN 


SIGMA7FORTRAN 
SIGMA7FORTRAN 
SIGMATFORTRAN 
SIGMA7FORTRAN 
SIGMATFORTRAN 
SIGMA7FORTRAN 
SIGMATFORTRAN 
SIGMA7TFORTRAN 
SIGMATFURTRAN 
SIGMATFORTRAN 
SIGMA7FORTRAN 
SIGMA7FORTRAN 
SIGMATFORTRAN 
SIGMA7TFORTRAN 
SIGMATFORTRAN 
SIGMATFORTRAN 
SIGMATFORTRAN 


IV 


SVANOM 
THISTO 


(SPECIFIC VOLUME ANOMALY ) 
(TWO-DIMENe FREQe DISTRIB-) 
THRCL (THERMOMETER CALIBRATION) 
VECTAV (VECTOR AVERAGES) 

VEL (GEOSTROPHIC VELOCITY) 

VTR (VOLUME TRANSPORT) 


UNIVAC 
OPTIMUM TRACK SHIP ROUTING 
NEWFIT 
PATTERN FUNCTION CALCULATIONS 
RAY SORT 
RAYMOR 


SONAR IN REFRACTIVE WATER 
SPECTRAL ANALYSIS OF TIME SERIES 


OTHERS 


AN/UYK-1 SOUND VELOCITY 
BIOLOGICAL STATION FILE 
STATION DATA (ATLAS) 

Q@ FACTORS 

CROSS-ASSOCIATION OF SEQUENCES 
DEEP (SeTeDe DIGITIZING) 

WET (SeTeDe DATA PROCESSING) 
CHLOROPHYLL CALCULATIONS 
DELTA-ALPHA AND SIGMA-T 
HARMONIC ANALYSIS 

TIDAL PREDICTION 

VELOCITY OF SOUND 

THERMOMETER CORRECTIONS 

TIDAL ANALYSIS AND PREDICTION 
PREDICTION OF HOURLY TIDE 
POWER SPECTRUM ANALYSIS 
OPTIMUM TRACK SHIP ROUTING 


PAGE 142 


SDS 
SDS 
SDS 
SDS 
SDS 
SDS 


SIGMA7FORTRAN IV 
SIGMA7FURTRAN IV 
SIGMA7FURTRAN IV 
SIGMA7FURTRAN IV 
SIGMA7FORTRAN IV 
SIGMA7TFORTRAN IV 


UNTVAC1107FORTRAN IV 
UNIVAC1108FORTRAN IV 
UNIVAC11O8FORTRAN IV 
UNIVAC11O8FORTRAN IV 
UNIVAC1108FORTRAN V 
UNIVAC1L1O8FORTRAN IV 
UNTVAC1108FORTRAN IV 


AN/UYK-1 LOGANDS 
ATLAS I EMA 

ATLAS 1 EMA 

ATLAS I FORTRAN V 
ELLIOTT803ALGOL 60 
HP 2115A FORTRAN 
HP 2115A FORTRAN 
ICT 1301 MAC 

1G¢f 1301 MAC 

Vet 1301, IMAG 

LET L201 MAE 
NGIees Ol eMAG 
MERCURY CHER 374 
MERCURY CHLF 3/4 
MERCURY NOT GIVEN 
PB-250 BASIC 
PB-440 MACHINE 


COMPUTER PROGRAM ABSTRACT FORM 


This is a source sheet for the NODC publication Computer Programs 
in Oceanography. Please use a separate form for each program. 


GENERAL INFORMATION 
Title of program 


Person to be contacted for further information concerning this pro- 
gram (NODC will refer all inquiries to this person), 

Name Telephone Number 

Institution 

Address 


Are you willing to make the source program available to the 
oceanographic community? If yes, please forward a doc- 
umented copy of the program to the NODC. Whenever the NODC acts 
as an intermediary in the transmittal of this program, you will 
be given full credit. 


PROGRAM DESCRIPTION 


Purpose of program 


Input to program (type and format of data) 


Output from program (form and content) 


General procedure followed (i.e., mathematical methods or statis- 
tical techniques used, approximations, etc.) 


Source language of program 
Documentation available 


HARDWARE REQUIREMENTS 


Core storage necessary (number of characters or words, please 
specify) 


Additional storage requirements 


Number of tape units used 


Special input-output requirements 


Other requirements 


Computer for which program has been written 


143 


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Internet Archive Audio

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