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OCEANGGAPHY

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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

PRICE $1.35

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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

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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

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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

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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

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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

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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

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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

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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 YY itn Wane be arsiwe 4 Tle 1 weve i te: wh, . hoe ry Nap Ste, ha EE ify a Reh LO bee ane. ay) mata a Ryi Pe ane awe ie eA ye ia ay ae Can pri ay Pav le ine ; VAL ringer als 1 Py eae on q mri Dee ee WA +9 HN Ae Sie eo RceRrraee | MART BOY aa ea mT AY ET aes eri) ae 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 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

7074 7074 1074 7074 7074 7074 7074 7074 7074 71074 71074 T7074 71074 7074 T1074 71074 T7074 7074 T1074 7074 7074 7074 T1074 T1074 7074 TOT4 7074 T1074 7074 TOT4 7074 71074 T1074 TO7T4 T7074 T7074 7074 T1074 7074 7074 T7074 T7074 7074 T1074 71074 T1074 7074 T1074 7074 T1074 7074 T1074 71074 T7074 7074 7109

709

7109

709

709

709

7090 7090 7090 7090 7090

7090 7090 7090

FORTRAN FORTRAN FORTRAN FURTRAN 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 FURTRAN FORTRAN AND MAP FORTRAN FORTRAN FORTRAN

II 64 II 64 i 63

II 47 II 90 Tel 29 II 27

TT 94 II 50

IV 48 IV 110 IV 49

SAVED (BLAST TEST

DATA REDUCTION)

STATISTICAL AND PEAK-TO-PEAK ANAL.

AVGe TEMPERATURES

IN WATER COLUMN

DYNAMIC HEIGHT AND CURRENT DYNAMICS GENERAL MAP PROJECTION MAP PROJECTION DISTORTIONS

TREND MAP » WIND CURRENTS

WITH RESIDUALS

THEORETICAL RADIAL TIDAL FORCE

SIMULATION OF MARI

NE SEDIMENTATION

CALCULATE AND PLOT TIME-TREND CURVES

ASTRONOMICAL TIDE

PREDICTION

Q-MODE CLUSTER ANALYSIS

VECTOR TREND ANALe SEA IGE STUDIES

DIRECTIONAL DATA

WAVE FORCE DISTRIBUTION WAVE FORCES AND MOMENTS

REFRACTION SIMULATION WAVEIN AND CHLORINITY CONTINUOUS CONTINUOUS SOURCE CONTINUOUS SOURCE» DENSITY — THERMOST

OF WAVE

DIFRAK - SALIN

S

OF WIND-GENERATED WAVES

ENS

LINE SOURCE

PER UNIT DEPTH WITH COOLING TERM ERIC ANOMALY

LATERAL RELATIVE DISTRIBUTION

SURFACE WAVE RAYS TOTAL CO(2)

MAGNETIC ANOMALIES AND GRADIENTS OCEANOGRAPHIC DATA PROGRAM F

SYNOPTIC PROGRAM

PROFIL SIMULATION OF MARI

(TSUNAMI PROFILES)

NE SEDIMENTATION

OPTIMIZATION OF VTE WATER PLANTS

SeTeDe CORRECTION TIME TERM: CONDU

BKGEOL

SEISMIC REFRACTION INTERPe (THERMAL CONDUCTIVITY)

(SEDIMENT STATISTICS)

CONCENTRATIONS PER SQUARE METER

PHYTOPLANKTON NUMBERS»

SDGVEL SEDIMENT GRANULOME SYNOPTIC PROGRAM

CURRENT

BOMM (TIME SERIES) SPECIFIC CONDUCTIV WAVE STATISTICS BLACKY CURRENT OBJECTIVE THERMOCL

ETCe

(SOUNDING CORRECTION)

TRIC ANALYSIS

ME Ye

(TIME SERIES ANALYSIS)

INE ANALYSIS

CURRENT METER DYNAMICS

INVENTORY PLOT SUBROUTINE 'MAP!# DETRND»s ETCe LENGL PROFILE

PROF1 (WATER ELEVe REFL1 (REFLECTED W UMAX1»s ETCe (MAXe

(SPECTRA SUBROUTINES) (WAVE LENGTH AND SPEED)

OVER WAVE PERIOD) AVE) FLOW VELOC.)

PAGE 140

AND MAP FORTRAN AND MAP FORTRAN AND MAP MAD MAD MAD MAD MAD

IBM 7090

IBM 7090 IBM IBM IBM IBM IBM

7090 7090 7090 7090 7090 IBM 7090 MAD

IBM 7090 MAD 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 7/7040 DCS IBM7094-IIFURTRAN 77040 DCS IBM7094-IIFURTRAN /7040 DCS 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

FORTRAN FORTRAN FORTRAN

’

1V 49 IV 49 81

93

65

65

47

68

104

1V 33 FAP 46 Ive 04 lV 55 IV 34 IV 75 Iv 109 my 109) nV 110 ey Did 50%110 11 12 II 71 II 71 ie Til 1a 90 11 70 i 1S 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

1V 41 lV 63 1V 48 mY 1Orz IV. 108 my | «LOB IV. 108 iw?» 1OS)

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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DS

DS

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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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