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CONTENTS
Introduction.
Sources of Information.
Program Abstracts, by Category.
Biological Oceanography
Chemical Oceanography .
Data Reduction.
Editing and Special Input /Output .
Geoscience. .
Geophysics, Mesinen :
Sediment Analysis and Meehenies
Graphical Display .
Mathematics, Applied. ato
Curve and Surface Fitting
Mathematical and Statistical iaeiinsiis
Navigation and Charting
Physical Oceanography . ¢
Air-Sea Interaction and Heat ‘Budget
Currents and Transfer Processes
Ice in the Sea. SEL CHG Gis we =o
Physical Properties: Analyses and
Summaries :
Physical Quantities, iConputation ‘of é
Sound-Ray Path.
Sound-Normal Modes.
Sound-Speed Computations.
Tides, Astronomical
Waves and Hydromechanics.
Retrieval of Ocean Data .
Index by Agency or Institution.
Index by Programming Language .
Index by Computer Make and Model.
Computer Program Abstract Form.
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INTRODUCTION
This second major revision of the National Ocean-
ographic Data Center's (NODC's) catalog Computer
Programs in Oceanography is issued to foster awareness
of computer programs related to oceanography and to
facilitate their exchange between interested groups.
As in the first revision, the material is
arranged under subject headings, with each entry con-
taining the program title, program language, computer
system the program is written for, indication whether
a copy is on file at NODC, brief program description
provided by originator, and name and address of per-
son to contact for further details.
This catalog only begins to reflect the present
programs originated by NODC for the new in-house com-
puter. Supplements or revised editions will be
issued, and abstracts of NODC's latest programs will
be incorporated, as well as contributions from other
institutions not received in time for inclusion in
this catalog. Also, a revised edition of the NODC
publication G-15, User's Guide to NODC's Data _ Proces-
sing Systems, planned for the near future will con-
tain updated computer programming information.
Documentation on file at NODC or assistance in
locating a program can be obtained by writing to:
The Director
National Oceanographic Data Center
Washington, D. C. 20390
Contributors of new programs are requested to
fill out the abstract form in the back of this cat-
alog and send it to the abcve address.
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SOURCES OF INFORMATION
Catalogs of computer programs pertaining to dis-
ciplines related to oceanography have been compiled
by various organizations. The following is a listing
of such publications known to NODC at this time. The
Center would appreciate further information about
existing computer programs for inclusion in following
editions of this catalog.
RESEARCH COMPUTATION CENTER PROGRAM LIBRARY
A compilation of computer programs written by
Naval Research Laboratory personnel. For further in-
formation, contact:
Mrs. Janet P. Mason, Code 7813
Mathematics and Information Services Division
Naval Research Laboratory
Washington, D. C. 20390
NATIONAL COMPUTER PROGRAM INDEX
Includes GOSSIP (Geologically Oriented Scheme
for Sharing Information in Programming) and the
Rokdoc Package, a library of routines for statistical
analysis, summary, and display of data concerning
sedimentary rocks. Inquiries should be directed to:
Assistant Librarian
Department of Geology
University of Reading
Whiteknights Park
Reading RGG-2AB
England
COOPERATIVE OCEANOGRAPHIC PROGRAMMING EFFORT (COPE)
A compilation of computer programs in use at the
Woods Hole Oceanographic Institution. For further
information, contact:
Editors of COPE
Woods Hole Oceanographic Institution
Woods Hole, Massachusetts 02543
COMPUTER SOFTWARE MANAGEMENT AND INFORMATION CENTER
(COSMIC)
A catalog of programs generated by the NASA
space effort. Many of the programs are of a general
nature. For further information, contact:
COSMIC
Computer Center
University of Georgia
Athens, Georgia 30601
NAVAL ORDNANCE LABORATORY LIBRARY
OF COMPUTER PROGRAMS
A catalog of programs in use at _ the Naval
Ordnance Laboratory. For further information, contact:
Mathematics Department
U. S. Naval Ordnance Laboratory
at White Oak
Silver Spring, Maryland 20910
KANSAS GEOLOGICAL SURVEY - COMPUTER CONTRIBUTIONS
A series of publications devoted to computer
programs and examples of problem-solving applications
in the earth sciences. For further information,
contact:
Dr. Daniel F. Merriam, Editor
Computer Contributions
Kansas Geological Survey
University of Kansas
Lawrence, Kansas 66045
PROGRAM ABSTRACTS BY CATEGORY
BIOLOGICAL OCEANOGRAPHY
—X%—K-H— HK —H—-4— HH — HE
RYLD»> BIOM LANGUAGE - FORTRAN IV
COMPUTER —- IBM 1130
(COPY ON FILE AT NODC)
COMPUTES THE APPROXIMATE YIELD OF A FISH STOCK PER RECRUITMENT By EI-
THER OF TWO METHODS (ARITHMETIC OR EXPONENTIAL APROXIMATIONS)» OR THE
PROGRAM SIMPLY COMPUTES THE STOCK BIOMASS WHEN THERE IS NO FISHINGe
OUTPUT—— AN EQUILIBRIUM YIELD MATRIX WITH UP TO 400 ENTRIES CORRES—
PONDING TO 20 AGES AT ENTRY AND 20 MULTIPLIERSe AUTHORS—-— LeVe PIENAAR
AND JeAe THOMSON» TECHNICAL REPORT NOe 92 (UNPUBLISHED MANUSCRIPT», NOV
1968).e EARLIER VERSION OF PROGRAM WRITTEN BY Le Ee GALES, COLLEGE OF
FISHERIES» UNIVERSITY OF WASHINGTONe DIRECT INQUIRIES TO —
FISHERIES RESEARCH BOARD OF CANADA
BIOLOGICAL STATION
NANAIMOs Be Ce
CHLOROPHYLL PIGMENT AND CAROTENOID PIGMENT LANGUAGE — FORTRAN II
COMPUTER - IBM 1620 II
(COPY ON FILE AT NODC)
TWO SIMILAR BUT SEPARATE ROUTINESe CALCULATION METHOD BASED ON THE
USE OF 1¢0 CMe CELLSe DATA CARDS INPUT, OUTPUT IS PRINTED LISTING AND
PUNCH CARDSe AUTHOR-— DRe MALCOLM HAIRe
INSTITUTE OF MARINE SCIENCE
ADELPHI UNIVERSITY
OAKDALE» LONG ISLANDs NeYe 11769
COMBINED CHLOROPHYLL AND PRODUCTIVITY LANGUAGE — FORTRAN IV
COMPUTER - CDC 6400
(COPY ON FILE_AT NODC) 4 2
COMPUTES ASSIMILATION OF PRODUCTIVITY IN SEA WATER AND. COMPUTES. THE
QUANTITIES OF CHLOROPHYLL As Bs AND Cs» AND THE AMOUNT OF CAROTENOIDS
IN SEA WATERe WRITTEN BY MARSHA WALLIN, NOV 19636 BASED UPON TWO
PROGRAMS PREPARED IN 1962 FOR THE IBM 709 BY MeRe RONAe THE CHLORO-
PHYLL PROGRAM DETERMINES THE AMOUNT OF PLANKTON PIGMENTS USING THE E-
QUATIONS OF RICHARDS AND THOMPSONe THE PRODUCTIVITY PROGRAM (CARBON
14) DETERMINES THE PRODUCTION OF MARINE PHYTOPLANKTON BY USING NEIL-
SEN'S METHOD. OUTPUT CONSISTS OF BOTH PRINTED MATTER AND OF LIBRARY
CARDSe THE LIBRARY CARDS MAY BE USED AS INPUT TO A MULTIPLE REGRES-
SION PROGRAM TO DERIVE A RELATION BETWEEN PRODUCTIVITY AND CHLOROPHYLL
A. FINALLYs A PLOT ROUTINE MAY BE CALLED TO GRAPH ONE OR SEVERAL VAR-
TABLES AS A FUNCTION OF DEPTHs OR TO DISPLAY THE HORIZONTAL DISTRIBU-
TION OF ANY GIVEN PROPERTYe REVISED IN 1969 FoR THE CDC-64006.
DRe Ge Ce ANDERSON
DEPARTMENT OF OCEANOGRAPHY
UNIVERSITY OF WASHINGTON
SEATTLE» WASHe 98105
ECOPROD LANGUAGE -— FORTRAN IV
COMPUTER -— CDC 6600
(COPY ON FILE AT NODC)
COMPUTES GROSS AND NET PRODUCTIVITY» RESPIRATIONs P/R RATIO» PHOTOSYN-
THETIC QUOTIENT, EFFICIENCY, DIFFUSION COEFFICIENT, GIVEN SUNLIGHT DA-
TA AND DIURNAL MEASURES OF OXYGEN AND/OR CARBON DIOXIDEe CORE STORAGE
REQUIRED-- 255,000 60-BIT WORDS» AUTHOR-- WILLIAM LONGLEYe
THE UNIVERSITY OF TEXAS
PAGE 905
MARINE SCIENCE INSTITUTE
PORT ARANSAS» TEXAS 78373
JOB (SPECIES DIVERSITY) LANGUAGE — FORTRAN IV
COMPUTER - CDC 6600
(COPY ON FILE AT NODC)
CALCULATES SPECIES DIVERSITY INDEX FOR NUMBERS OF ORGANISMS AND/OR
WEIGHT OF ORGANISMS» UTILIZING THE DIVERSITY INDEX EQUATION DERIVED
FROM MARGALEFe PROGRAM CALLS SUBROUTINE *tSEASON' WHICH CALCULATES
SEASONAL AVERAGES FOR A GIVEN STATION, SEASONAL LIMITS BEING INDICATED
BY A CONTROL CARDe THIS SUBROUTINE OUTPUTS MEANs STANDARD DEVIATION,
AND RANGE OF DIVERSITY INDICES FOR EACH SEASONAL GROUPe OTHER DESIRED
GROUPINGS MAY BE ENTERED BY A GROUPING CONTROL CARD. CORE STORAGE NEC-—
ESSARY-- 50000 60-BIT WORDSe AUTHOR-- AeDe EATONe
WILLIAM LONGLEY
THE UNIVERSITY OF TEXAS
MARINE SCIENCE INSTITUTE
PORT ARANSAS» TEXAS 78373
OXYGEN LANGUAGE — FORTRAN IV
COMPUTER - CDC 6600
(COPY ON FILE AT NODC)
DETERMINES PRODUCTIVITY BY OXYGEN DIURNAL CURVE METHODe INPUT INCLUDES
OXYGEN CONCENTRATION AND OXYGEN PROBE PARAMETERS. OUTPUT CONTAINS NET
AND GROSS PRODUCTIVITY AND P/R PLUS ORIGINAL DATAs AUTHOR-— WILLTAM
LONGLEY.
THE UNIVERSITY OF TEXAS
MARINE SCIENCE INSTITUTE
PORT ARANSAS»s TEXAS 78373
MARINE BIOLOGICAL ENVIRONMENTAL SUMMARIES LANGUAGE — FORTRAN
COMPUTER ~- IBM 7074
CODED CHARACTERISTICS FOR SPECIFIED LOCALITIES ARE SUMMARIZED FOR THE
FOLLOWING MARINE BIOLOGICAL PHENOMENA-- AMBIENT BACKGROUND NOISE, AT-—
TACHED AND FLOATING MARINE VEGETATIONs BIOLUMINESCENCEs AND DANGEROUS
MARINE LIFEe CHARACTERISTICS INCLUDE-— HABITAT, PERIOD OF ACTIVITYs
FREQUENCYs RANGE OF SOUND» MAXIMUM SOUND PRESSURE LEVEL» AREAL DISTRI-
BUTION OF MARINE VEGETATION, TYPE AND INTENSITY OF BIOLUMINESCENCE 9
AND CAUSES AND EFFECTS OF SPECIFIED DANGEROUS MARINE LIFEs AUTHOR-—
ReMe HOLCOMBE. OS NOo 53338.
OCEANOGRAPHIC ANALYSIS OIVes CODE 3301
NAVAL OCEANOGRAPHIC OFFICE
SUITLANDs MD. 20390
LENGTH-WEIGHT FREQUENCY LANGUAGE — FORTRAN IV
COMPUTER - IBM 360/65
CALCULATES LENGTH-WEIGHT FREQUENCY DISTRIBUTION VALUES FROM SKIPJACK
CATCH DATAs
BUREAU OF COMMERCIAL FISHERIES BIOLOGICAL LABe
ATTNe DRe ReAe BERKLEY» OCEANOGRAPHER
P.O. BOX 3830
HONOLULUs HAWAII 96812
BIODETERIORATION PROJECT LANGUAGE — AUTOCODER
COMPUTER — IBM 7074
(COPY ON FILE AT NODC)
MONTHLY AND YEARLY SUMMARTES OF THE RESULTS OF FOULING MEASURED ON
EXPOSED AND CONTROL PANELSe OS NO, 52272, AUTHOR-- JUDY YAVNER,
PAGE 006
DEVELOPMENT DIVISION» CODE 2300
NATIONAL OCEANOGRAPHIC DATA CENTER
WASHINGTON» DeCe 20390
CONCENTRATIONS PER SQUARE METER OF SURFACE IN THE LANGUAGE — FORTRAN IV
OCEAN AND LAKES FROM CONCENTRATIONS PER VOLUME COMPUTER — IBM 7094-II/
(UWMS-1006) 7040 DCS
(COPY ON FILE AT NODC)
COMPUTES VARIOUS CHEMICAL AND BIOLOGICAL COMPOUND CONCENTRATIONS AS
WELL AS PRODUCTIVITY RATES PER SQUARE METER OF WATER SURFACE, FROM IN-
TEGRATED VALUES ON "PER VOLUME* BASIS. TEN CONCENTRATIONS AND RATES
ARE INTEGRATED OVER UP TO SEVEN PAIRS OF OPTIONAL DEPTH LIMITS. REFo
A 31-PAGE REPORT (UWMS-1006, JUN 1966) BY THE DEPARTMENT OF OCEANO-
GRAPHY» APPLIED MATHEMATICS SECTIONe CORE STORAGE NEEDED- 2231 WORDS.
SOURCE DECK HAS 771 CARDS.
He MACINTOSH» COMPUTER SERVICES
DEPARTMENT OF OCEANOGRAPHY
UNIVERSITY OF WASHINGTON
SEATTLE» WASHe 98105
PHYTOPLANKTON NUMBERS» VOLUMES AND SURFACE AREAS LANGUAGE = FORTRAN IV
BY SPECIES (UWMS-1008 AND UWMS-1009) COMPUTER - IBM 7094-II/
7040 DCS
(COPY ON FILE AT NODC)
TWO PROGRAMS» DIFFERING IN INPUT FORMAT ONLY» COMPUTE CONCENTRATIONS
OF CELL NUMBERS» CELL SURFACE AREAS» AND CELL AND PLASMA VOLUMES IN
MARINE PHYTOPLANKTON POPULATIONS. ALSO MEAN CELL AREAS» MEAN CELL
VOLUMES AND MEAN PLASMA VOLUMES AS WELL AS THE RATIOS CELL AREA TO
CELL VOLUME AND CELL AREA TO PLASMA VOLUME ARE COMPUTED OPTIONALLY.
THE INPUT QUANTITIES ARE OBTAINED FROM MICROSCOPICAL EXAMINATION OF
SEAWATER SAMPLES. A SUBROUTINE COMPUTES THE AREAs VOLUME AND PLASMA
VOLUME OF A CELL FROM MEASURED DIMENSIONS OF DIVERSE SPECIESe CORE
STORAGE REQUIRED-- 239836 WORDS FOR MAIN PROGRAM AND SUBROUTINES IN
FORTRAN AND MAPe SOURCE DECK HAS 1211 CARDSe REFe A 93 PAGE REPORT-—-
SPECTAL REPORT NO. 38 (M66-41,JULY 1936), BY PAAVO Eo. KOVALA AND JERRY
De LARRANCEe
He MACINTOSH» COMPUTER SERVICES
DEPARTMENT OF OCEANOGRAPHY
UNIVERSITY OF WASHINGTON
SEATTLEs WASHe 98105
CHLOROPHYLL CALCULATIONS LANGUAGE — MAC
COMPUTER - ICT 1301
CALCULATES CHLOROPHYLL USING THE FORMULA OF STRICKLAND IN *A MANUAL OF
SEA WATER ANALYSIS' PP. 110-1122 AUTHORS-- AeMe SHIPLEY AND De SACKSe
UNIVERSITY OF CAPE TOWN
OCEANOGRAPHY DEPARTMENT
STTNe MRe AoMe SHIPLEY
PRIVATE BAGs RONDEBOSCH»s CePeo
REPUBLIC OF SOUTH AFRICA
PROGRAM REGROUP LANGUAGE —- FORTRAN
COMPUTER - CDC 3600
(COPY ON FILE AT NODC)
THE PROGRAM DETERMINES THE NUMBERS OF OCCURSENCES AND JOINT OCCUR-
RENCES OF THE SPECIES IN THE SET OF SAMPLESe IT THEN CALCULATES AN
INDEX OF AFFINITY FOR EACH PAIR OF SPECIESe THE SPECIES ARE ORDERED
IN TERMS OF THE NUMBERS OF AFFINITIES THEY HAVE AND THIS LIST IS
PRINTED ALONG WITH A LIST OF NAMES» CODE NUMBERS AND NUMBERS OF OCCUR-
RENCESe THE PROGRAM THEN DETERMINES THE LARGEST GROUP THAT COULD BE
FORMEDs TESTS TO SEE WHETHER THAT MANY SPECIES ALL HAVE AFFINITY wITH
EACH OTHER AND» IF THEY DOs PRINTS OUT THE GROUPe IF THEY DO NOT IT
PAGE 007
TRIES THE NEXT SMALLER GROUP,» ETCe THOSE SPECIES WHICH HAD AFFINITY
ONLY WITH THIS GROUP — AND/OR EARLIER GROUPS — ARE LISTEDe THE RE-
MAINING SPECIES ARE REORDERED AND THE PROCESS CONTINUED UNTIL ALL SPE-
CIES HAVE BEEN PUT EITHER IN GROUPS OR IN THE LIST OF SPECIES wITH
AFFINITIES WITH GROUPSe LIMITS-- 200 SPECIESe DIRECT INQUIRIES TO--
DRe Ese We FAGER
SCRIPPS INSTITUTION OF OCEANOGRAPHY
P.O. BOX 109
LA JOLLA» CALTFORNIA 92037
CHLOR LANGUAGE — FORTRAN IV
COMPUTER - CDC 3600
THIS PROGRAM WILL EITHER CALCULATE CHLOROPHYLL As By C CONCENTRATIONS
IN MICROGRAMS PER LITER OF SEAWATER AND THE CONVERSION FACTORS FOR THE
FLUOROMETER USING SPECTROPHOTOMETER READINGS,» OR CALCULATE CHLOROPHYLL
A AND PHAEOPHYTIN CONCENTRATIONS IN MICROGRAMS PER LITER OF SEAWATER,
USING THE FLUOROMETER READINGS. A SIMILAR PROGRAM WAS WRITTEN EARLIER
AT SeleOo FOR THE CDC 1604.
MRe DAVID WIRTH
OCEANIC RESEARCH DIVISION
SCRIPPS INSTITUTION OF OCEANOGRAPHY
P.O. BOX 109
LA JOLLA» CALIFORN'A 92037
NUTRIENT CHEMISTRY CONCENTRATION LANGUAGE - (NOT GIVEN)
COMPUTER - CDC 1604
COMPUTES CONCENTRATIONS OF INORGANIC PHOSPHORUS, SILICATE, NITRITE»
NITRATE» FROM THE APPROXIMATE RAW DATAe
SCRIPPS INSTITUTION OF OCEANOGRAPHY
LA JOLLA» CALIFORNIA 92037
PRIMARY PRODUCTIVITY LANGUAGE — (NOT GIVEN)
COMPUTER —- CDC 1604
COMPUTES PRIMARY PRODUCTIVITY FROM ACTIVITY OF CARBON» DURATION OF IN-
CUBATIONs TYPE OF INCUBATION, SAMPLE ACTIVITY AND DEPTHe
SCRIPPS INSTITUTION OF OCEANOGRAPHY
LA JOLLA» CALIFORNIA 92037
ZOOPLANKTON VOLUME LANGUAGE — (NOT GIVEN)
COMPUTER - CDC 1604
COMPUTES ZOOPLANKTON VOLUME FROM VARIOUS TY°ES OF HAULe
SCRIPPS INSTITUTION OF OCEANOGRAPHY
LA JOLLA» CALIFORNIA 92037
PAGE 008
CHEMICAL OCEANOGRAPHY
—R-H 8 —-O— FH
ALKALINITY AND SPECIFIC ALKALINITY LANGUAGE — FORTRAN AND
FORCOM
COMPUTER = IBM 1620
THE INPUT CARDS OF THIS PREGRAM ARE PRE-PUNCHED WITH THE STATION NUM-
BER» DATEs WIRE LENGTH AND BOTTLE NUMBER», THEN SENT TO THE CHEMISTRY
LABORATORY WHERE THE PH VALUE AND THE SALINITY VALUE ARE PUNCHED ON
THE CARDSe THE CARDS ARE THEN RETURNED AND PROCESSED THROUGH THE COM-—
PUTERe
UNIVERSITY OF MIAMI
MARINE LABORATORY
COMPUTING CENTER
1 RICKENBACKER CAUSEWAY
VIRGINIA KEY» MIAMI» FLORIDA
SALINITY VALUE CALCULATION LANGUAGE — FORTRAN AND
FORCOM
COMPUTER - IBM 1620
THE INPUT CARDS ARE PRE-PUNCHED WITH STATION NUMBER» DATE» WIRE LENGTH
AND BOTTLE NUMBER» THEN SENT TO THE CHEMISTRY LABORATORY WHERE THE X
AND Y ARM READINGS ARE PUNCHEDe THE CARDS ARE THEN RETURNED AND PRO-
CESSED THROUGH THE COMPUTERe AN 80-80 BOARD ON THE IBM 407 IS USED
FOR LISTING THE OUTPUT OF THIS PROGRAMe
UNIVERSITY OF MIAMI
MARINE LABORATORY
COMPUTING CENTER
1 RICKENBACKER CAUSEWAY
VIRGINIA KEYs MIAMI» FLORIDA
SPECTAL CHEMISTRY CALCULATIONS LANGUAGE - FORTRAN IV
COMPUTER - IBM 1130
READS SPECIAL CHEMISTRY (PHOSPHATEs SILICATEs NITRATE» ETCe) RAW DATA
CARDS» AND COMPUTES FINAL VALUES, OUTPUT FROM THE PROGRAM—~- WORKING
RECORD OF THE DATA FILE» FINAL REPORT IN PUBLISHABLE FORM, PLOTS OF
ANY VARIABLES VSe DEPTH, PLOTS OF ANY VARIABLE vSe VAREABLE» AND STAN-
DARD OBSERVED CARDSe DOCUMENTATION=-— OPERATING INSTRUCTIONS ONLYe
UNIVERSITY OF WASHINGTON
DEPARTMENT OF OCEANOGRAPHY
22A OCEANOGRAPHY TEACHING BLDGe
ATTNe MRSe HELLA MACINTOSH
SEATTLE» WASHe 98105
WATER CHEMISTRY LANGUAGE - FORTRAN Iv
COMPUTER -— IBM 360/65
(COPY ON FILE AT NODC)
CALCULATES THE DIELECTRIC CONSTANT OF WATER O TO 360 DEGe C (WATER
SATURATED FOR T OVER 100 DEGe C), THE DENSITY OF WATER (0 TO 360 DEGe
CC)» THE EXTENDED DEBYE-HUECKEL ACTIVITY COEFFICIENTS OF CHARGED spEC-
IES» THE ACTIVITY PRODUCTS FOR 33 HYDROLYSIS REACTIONS INCLUDING OX-
IDES» HYDROXIDESs CARBONATES»s SULFIDES AND SILICATES» THE CONCENTRA-
TIONS AND ACTIVITIES OF 10 ION PAIRS OR COMPLEXES» AND OF 22 AQUEOUS
SPECIES» THE OXIDATION POTENTIAL CALIBRATIONS» THE STANDARD STATE OXI-
DATION POTENTIALS AND EH VALUES AT EQUILIBRIUM FOR 13 REDOX REACTIONS,
MOLES AND PPM OF CATIONS AT EQUILIBRIUM WITH 42 SOLID PHASES AND THE
CHEMICAL POTENTIALS FOR EACH OF THE 42 REACTIONS ALONG WITH ACTIVITY
PRODUCT/EQUILIBRIUM CONSTANT RATIOS FOR THE HYDROLYSIS REACTIONS.
PROGRAM NO. MO101, FEB 1968,
PAGE 009
Ue Se GEOLOGICAL SURVEY
COMPUTER CENTER DIVISION
ATTNe RALPH EICHERs CHIEF
BRANCH OF SCIENTIFIC APPLICATIONS
WASHINGTON» De Co 20242
TSALBP LANGUAGE — FORTRAN II
COMPUTER -— CDC 3100
CALCULATES THE SALINITY ANOMALY FROM A STANDARD T/S OR THETA/S CURVE
FOR NORTH ATLANTIC CENTRAL WATER BY LeVe WORTHINGTONe THE RESULTS ARE
OUTPUT ON THE LINE PRINTER» STATION BY STATION, STORAGE REQuUIREMENT-—
2540 DECIMALe AUTHOR-- AeBe GRANT (JUNE 1968),
DIRECTOR
ATLANTIC OCEANOGRAPHIC LABORATORY
BEDFORD INSTITUTE
DARTMOUTHs NOVA SCOTIA» CANADA
TSATBP LANGUAGE -— FORTRAN II
COMPUTER -— CDC 3100
CALCULATES THE PERCENTAGE OF OXYGEN SATURATION IN SEA WATER» ACCORDING
TO TABLES AND FORMULAE BY MONTGOMERY (1967)s AS WELL AS AN OXYGEN A-
NOMALY ON A SIGMA-T SURFACE, ACCORDING TO A TABULATED CURVE BY RICH-—
ARDS AND REDFIELD (1955)e THE RESULTS ARE OUTPUT ON THE LINE PRINTER,»
STATION BY STATIONe AUTHOR-- AeBe GRANT (JUNE 1968).6
DIRECTOR
ATLANTIC OCEANOGRAPHIC LABORATORY
BEDFORD INSTITUTE
DARTMOUTHs NOVA SCOTIA» CANADA
PERCENTAGE SATURATION OF OXYGEN IN LANGUAGE — FORTRAN IV-G
ESTUARINE WATERS COMPUTER — IBM 360/65
(COPY ON FILE AT NODC)
COMPUTES THE PERCENTAGE SATURATION OF DISSOLVED OXYGEN IN ESTUARINE»
OR BRACKISH WATERe BECAUSE OF THE TEMPERATURE COMPENSATION AT A FIXED
25 DEGe C IN THE CONDUCTIVITY MEASUREMENTS» SALINITY IS GIVEN AS INPUT
AND IS USED TO COMPUTE CHLORINITY.s» THIS COMPUTED CHLORINITYs WITH THE
ACCOMPANYING TEMPERATURE» IS USED TO DETERMINE THE OXYGEN SOLUBILITY
OF THE WATERe THE MAXIMUM PERCENTAGE SATURATION OF THE DISSOLVED Oxy-
GEN IN THE WATER IS CALCULATED FROM THE GIVEN OXYGEN CONTENT AND THE
COMPUTED OXYGEN SOLUBILITYe THE SAME PROCEDURE IS USED TO ASCERTAIN
THE MINIMUM PERCENTAGE SATURATION OF OXYGENe INDEPENDENTLY OF THE
DISSOLVED OXYGEN DATA, THERE IS ANOTHER SET OF MEASURED TEMPERATURE
AND CONDUCTIVITY FROM WHICH SALINITY IS COMPUTEDe PROGRAM NOs B5285
BY PATRICIA As FULTONs APR 1969-6
Us Se GEOLOGICAL SURVEY
COMPUTER CENTER DIVISION
ATTNe RALPH EICHER»s CHIEF
BRANCH OF SCIENTIFIC APPLICATIONS
WASHINGTONs De Ce 20242
AOU» I SAOU LANGUAGE — FORTRAN
COMPUTER - IBM 360/65
CALCULATES SIGMA-T» SATURATION VALUES OF OXYGEN, APPARENT OXYGEN UTIL-
IZATION» AND RATIOS OF AcQeUe TO PHOSPHATE* USES He O« FORMAT (1960)
CARDS.
BUREAU OF COMMERCIAL FISHERIES
HONOLULU» HAWAIT 96812
PAGE 010
OXYGEN/NITROGEN SATURATION LANGUAGE —- FORTRAN
COMPUTER - IBM 7074
GIVES OXYGEN IN ML/L» MG/L» AND PERCENT SATURATION, ALSO GIVES APPAR-
ENT OXYGEN UTILIZATIONs NITROGEN IN ML/L, AND NITROGEN PERCENT SATURA-
TIONe THE PROGRAM WILL ACCEPT DATA DERIVED FROM EITHER GAS PARTITION-—-
ER OR TITRATION METHODSe OS PROGRAM NOe 59209, BY GORDON WILCHERe
OCEAN SURVEYS DIVISIONs CODE 9230
NAVAL OCEANOGRAPHIC OFFICE
SUITLAND» MD. 20390
SALINITY LANGUAGE — FORTRAN IV
COMPUTER - HONEYWELL516
(COPY ON FILE AT NODC)
CONVERTS READINGS FROM THE SALINOMETER TO SALINITIES» GIVEN THE TEMP—
ERATURE AND CONDUCTIVITY RATIOce TELETYPE I/Oco
COMMANDING OFFICER
UeSe COAST GUARD OCEANOGRAPHIC UNIT
BLDGe 159-E»s NAVY YARD ANNEX
WASHINGTONs De Ce 20390
OXYGEN LANGUAGE — FORTRAN Iv
COMPUTER — HONEYWELL516
(COPY ON FILE AT NODC)
COMPUTES VALUES OF OXYGEN. TELETYPE I/0.
COMMANDING OFFICER
UeSe COAST GUARD OCEANOGRAPHIC UNIT
BLDGe 159-E» NAVY YARD ANNEX
WASHINGTONs De Ceo 20390
PHOSPHATE LANGUAGE - FORTRAN IV
INDUCTIVE SALINOMETER SALINITY CONVERSION
COMPUTER -— HONEYWELL516
(COPY ON FILE AT NODC)
COMPUTES PHOSPHATE VALUES. TELETYPE 1/0.
COMMANDING OFFICER
UeSe COAST GUARD OCEANOGRAPHIC UNIT
BLDGe 159-Es NAVY YARD ANNEX
WASHINGTON» De Ce 20390
LANGUAGE — PDP8 FORTRAN
COMPUTER — PDP-5, 8S
(COPY ON FILE AT NODC)
ACCEPTS BOTTLE NUMBER» TEMPERATURE OF SAMPLE, AND CONDUCTIVITY RATIO
OF SAMPLE AND OUTPUTS A SALINITY CORRECTED FOR TEMPERATURE AND SHEAR.
COMMANDING OFFICER
UeSe COAST GUARD OCEANOGRAPHIC UNIT
BLDGe 159-Es NAVY YARD ANNEX
WASHINGTON» De Co 20390
SPECIFIC CONDUCTIVITY WITH PRESSURE EFFECT LANGUAGE - FORTRAN
COMPUTER - IBM 0S/360
(COPY ON FILE AT NODC)
COMPUTES SPECIFIC CONDUCTIVITIES FROM MEASURED VALUES OF RESISTANCE
FOR THE ELECTROLYTIC SOLUTION AND THE PRESSURES AT WHICH THE MEASURE-
MENTS WERE MADE. THE PROGRAM ALSO DETERMINES OTHER USEFUL QUANTITIES
NEEDED TO DETERMINE THE EFFECT OF PRESSURE ON THE IONIC CONDUCTANCE
THROUGH THE UPPER 2000 METERS OF THE OCEAN'S WATER COLUMNe THE CON-
DUCTIVITY INCREASE WHICH RESULTS SOLELY FROM SOLUTION CONCENTRATION
CHANGES DURING COMPRESSION IS DETERMINED AND FOUND TO BE A SIGNIFICANT
PAGE 011
ERROR SOURCEe REFe THESIS BY MICHAEL Es MAYS (DEC 1968, 89 P)e
NAVAL POSTGRADUATE SCHOOL
MONTEREY» CALIFORNIA 93940
SALINITY — CONDUCTIVITY FORMULA LANGUAGE — FORTRAN
COMPUTER - IBM 7074
EVALUATES A NEWLY DEVELOPED EQUATION RELATING SEA WATER ELECTRICAL
CONDUCTIVITY AND SALINITY. AUTHOR-- Wels GUIDRYe OS NO~ 20184.
COMPUTER DEPARTMENTs CODE 0831
NAVAL OCEANOGRAPHIC OFFICE
SUITLAND» MD. 20390
CHLORINITY — SALINITY LANGUAGE —- FORTRAN II
COMPUTFR — IBM 7094
SUBROUTINE COMPUTES CHLORINITY AND SALINITY FROM MEASUREMENTS OF TEMP—
ERATURE AND CONDUCTIVITYe USES MODIFICATION OF POLLAK*S (1954) EQUA—
TIONS RELATING CONDUCTIVITYs TEMPERATURE» AND CHLORINITYe
HARVEY Ee WALTERS
CHESAPEAKE BAY INSTITUTE
THE JOHNS HOPKINS UNIVERSITY
CHARLES AND 34TH STe
BALTIMORE» MDe 21218
TOTAL CO(2) LANGUAGE — FORTRAN II
COMPUTER — IBM 7094
COMPUTES TOTAL CO(2) FROM MEASUREMENTS OF TEMPERATURE» CHLORINITY» PHs
AND ALKALINITYe FOLLOWS METHOD OF HeWe HARVEY (1960)e¢ LINEAR INTER-
POLATION IN TWO VARIABLES IS PERFORMED IN THE TABLESe OUTPUT IS A
TABULATION FOR EACH STATION OF DEPTHs INPUT DATA» AND TOTAL CO(2).6
OPTIONALLY» OFF-LINE CALCOMP PLOTS OF TOTAL CO(2) VSe DEPTH CAN BE
PRODUCED. CORE STORAGE NECESSARY-- 3430 WORDS PLUS PLOTTER ROUTINESe
HARVEY Ee WALTERS
CHESAPEAKE BAY INSTITUTE
THE JOHNS HOPKINS UNIVERSITY
CHARLES AND 34TH STe
BALTIMORE» MDe 21218
GAMMA-RAY SPECTRA LANGUAGE — FORTRAN
COMPUTER — (NOT GIVEN)
(COPY ON FILE AT NODC)
IDENTIFIES AND MEASURES COMPONENTS IN A MIXTURE OF GAMMA-EMITTING RA-
DIONUCLIDESe THE COMPUTER PROGRAM WILL BE USEFUL IN ANALYZING THE
LARGE NUMBER OF LOW ACTIVITY MIXTURES OF RADIONUCLIDES THAT ARE TO BE
MADE IN THE PROGRAM TO DETERMINE THE PHYSICAL-CHEMICAL SPECIES OF THE
RADIONUCLIDE DEBRIS PRODUCED BY UNDERWATER NUCLEAR EXPLOSIONSe REFe
REPORT TR-67-465 UeSe NAVAL RADIOLOGICAL DEFENSE LABORATORY» By JAMES
Fe PESTANER AND DANIEL Le LOVE>
DIVISION OF BIOLOGY AND MEDICINE
UeSe ATOMIC ENERGY COMMISSION
WASHINGTONs De Co 20545
OPTIMIZATION OF VTE SALINE WATER PLANTS LANGUAGE — FORTRAN IV
COMPUTER - IBM 7094
(COPY ON FILF AT NODC)
PROGRAM AND SUBROUTINES TO DEVELOP AN OPTIMUM DESIGN OF A MIMIMUM COST
VTF (VERTICAL TUBE EVAPORATOR) FALLING FILM PLANT FOR PRODUCING FRESH
WATER FROM SFA WATER. RESEARCH AND DEVELOPMENT PROGRESS REPORT NO«
PAGE 012
404 (FEB 19695 164 P)e
UeSe DEPARTMENT OF THE INTERIOR
OFFICE OF SALINE WATER
WASHINGTON» DeCe 20240
PAGE 013
DATA REDUCTION
—¥ —#—#—#— 8-4 -—*
PHYSICAL OCEANOGRAPHY DATA REDUCTION LANGUAGE - FORTRAN II
PROGRAMS FOR THE CDC 3100 COMPUTER — CDC 3100
(COPY ON FILE AT NODC)
AN OCEANOGRAPHIC DATA PROCESSING SYSTEM DESIGNED TO ACCEPT THE DATA
FROM THE ORIGINAL LOG SHEETSe COMPUTES OBSERVED TEMPERATURES AND
PRESSURES FROM THERMOMETER READINGS» SALINITIES FROM THE CONDUCTIVITY
RATIO READINGS» THE DISSOLVED OXYGEN FROM THE TITRES AND THE REACTIVE
SILICA CONCENTRATIONS FROM THE OpTICAL DENSITIESe THE DATA INPUT MAY
BE PUNCHED PAPER TAPE FROM THE PDP-8 SYSTEM (Bele COMPUTER NOTE 68-5-
C) OR PUNCHED CARDSe THE FINAL PROGRAM IN THE SYSTEM COMPUTES DEPTH,
POTENTIAL TEMPERATUREs SURFACE DENSITY ANOMALY 9 POTENTIAL SURFACE DEN-
SITY ANOMALY AND SPECIFIC VOLUME ANOMALYe THE PROGRAM ALSO CAN COM-—
PUTE THE DYNAMIC HEIGHT AND POTENTIAL ENERGY ANOMALY AT GIVEN PRESS-
URES AND MAY ALSO GIVE A MAGNETIC TAPE OF THE DATA IN CARD IMAGE OF
THE CODC FORMATe CORE STORAGE-- 16Ke REFe Bele COMPUTER NOTE 68-10-C
(OCT 1968» 280 PAGES)» BY Re REINIGERs CeKe ROSS» Pe TRITES AND DeJe
LAWRENCE.
DIRECTOR
ATLANTIC OCEANOGRAPHIC LABORATORY
BEDFORD INSTITUTE
DARTMOUTHs NOVA SCOTIA» CANADA
PHYSICAL OCEANOGRAPHY DATA REDUCTION LANGUAGE — PAL III
PROGRAMS FOR THE PDP-8 COMPUTER — PDP-8
(COPY ON FILE AT NODC)
A SYSTEM OF PROGRAMS THAT ACCEPTS RAW DATA AS RECORDED ON DECK SHEETSe
CALCULATES THE CORRECTED TEMPERATURES» USES THE HIGHEST ORDER LEAST
SQUARES FIT TO OBTAIN THE SMOOTHED PRESSURES» CALCULATES DEPTH, SPE-
CIFIC VOLUME ANOMALYs POTENTIAL TEMPERATURE» AND DENSITY ANOMALIESe
ALSO FORMATS RAW CHEMISTRY DATAe INCLUDES A SET OF PLOTTING ROUTINESe
CORE STORAGE-=- 4Ke REFe Bele COMPUTER NOTE 68-5-C (258 P» MAY 1968),
BY CeKe ROSSs Re REINIGERs AeBe GRANTe
DIRECTOR
ATLANTIC OCEANOGRAPHIC LABORATORY
BEDFORD INSTITUTE
DARTMOUTH» NOVA SCOTIA» CANADA
STADAT 2 LANGUAGE —- FORTRAN II
COMPUTER - GE 225
(COPY ON FILE AT NODC)
A CHAIN OF EIGHT PROGRAMS WHICH REDUCE AND EDIT HYDROGRAPHIC STATION
DATAs CALCULATE AND SMOOTH THERMOMETRIC DEPTHSe BASED UPON wOODS HOLE
Oele PROGRAM 'tHYLOG! (VERSION FOR GE-225)e THE FINAL DATA MAY BE EI-
THER A PRINTOUT OR NODC FORMAT PUNCHCARDSe REFe BIO COMPUTER NOTE 66-
5-Ce AUTHOR-- FeKe KEYTEe (SEE ALSO "ON THE FORMULAS FOR CORRECTING
REVERSING THERMOMETERS! REFe NOe 64-298 WHOI» BY FREEMAN Ke KEYTEe)
BEDFORD INSTITUTE
DARTMOUTHs NeSes CANADA
REDUCTION AND DISPLAY OF DATA ACQUIRED AT SEA LANGUAGE — FORTRAN II
COMPUTER —- IBM 1130
(COPY ON FILE AT NODC)
A SYSTEM OF PROGRAMS (NAVIGATIONs GRAVITY» TOPOGRAPHY» MAGNETICS) FOR
THE REDUCTION» STORAGE AND DISPLAY OF UNDERWAY DATA ACQUIRED AT SEAco
THE COMPUTER INSTALLATION CONSISTS OF AN IBM 1130 AND INCLUDES RANDOM
ACCESS DISK CARTRIDGES AND AN ON-LINE CALCOMP 30 INe PLOTTERe A.IARGE
PAGE 014
NUMBER OF THE PROGRAMS UTILIZE NAVIGATION POINTS TOGETHER WITH RAW
DIGITIZED GEOPHYSICAL DATA PRESEfeTED AS A TIME SERIES, WHERE THE DIFF-
ERENT DATA MAY BE READ AT UNEQUAL TIME INTERVALSe REFe TECHe REPORT
NOe 1 (AUGUST 19695 348 Pe) BY MANIK TALWANI 6
LAMONT—DOHERTY GEOLOGICAL OBSERVATORY
COLUMBIA UNIVERSITY
PALISADES» NEW YORK 10964
RICHARDSON CURRENT METER FILM READING LANGUAGE - DECAL
COMPUTER — PDP-7(9)
A SYSTEM OF PROGRAMS UNDER AN ON-LINE TYPEWRITER CONTROL PROGRAM TO
AUTOMATICALLY READ DATA (CURRENT SPEED AND DIRECTION)» RECORDED ON 16-
MM FILM» INTO A PDP-7 COMPUTER» USING A PROGRAMMABLE FILM READING DE-
VICEe DATA OUTPUT IS AVAILABLE IN THE FORM OF NUMERICAL LISTINGS OR
IN DIGITAL FORM ON MAGNETIC TAPEe A DIGITAL X-Y PLOTTER MAY ALSO BE
USED TO PRODUCE GRAPHS AND HISTOGRAMS OF CURRENT SPEED AND DIRECTIONe
THE MOST IMPORTANT IN THE SYSTEM OF PROGRAMS IS THE *tNINEPOINT FIILM
READER?'.« THE OTHER PROGRAMS ARE-- 'CHANNEL POSITIONING!» *ENTER CHAN-
NELS's *WRITE DATA'»s *GRAPHING's "CLEAR NINEPOINT RECORD!» "AUTOMATIC
FRAME ADVANCEts *LEFT OR RIGHT SCAN*'» *ALL CHANNELS ON TOTALS',» *DOT
SCANNING!» *DIAMOND SCANNERts *MICROSCOPE't»s AND # TEST SINGLE CHANNEL?
BROCHURE DESCRIBING THE SYSTEM IS AVAILABLE ON REQUESTe
DRe DANIEL Me FORSYTH
INFORMATION INTERNATIONAL» INCeo
89 BRIGHTON AVENUE
BOSTONs MASSACHUSETTS 02134
BRAINCON DATA REDUCTION LANGUAGE - FORTRAN IV
COMPUTER = IBM 1800 SYS
(COPY ON FILE AT NODC)
CONVERTS DATA IN THE FORM OF ANGULAR POSITIONS OF THE ROTOR AND COM—
PASS ARCS FROM BRAINCOM TYPE 316 CURRENT METERS INTO VALUES OF CURRENT
SPEED AND DIRECTIONs TILT DIRECTION» N-S AND E-W CURRENT COMPONENTS
AND DISPLACEMENTS (IN KILOMETRES) FROM ANY ARBITRARY ORIGENe DATA IS
OUTPUT TO LINEPRINTER WITH COLUMN HEADINGS AND MAGNETIC TAPE WITHOUT
HEADINGSe EXECUTION TIME-- OF THE ORDER OF 3 MINSe PER 100 CARDS (2
MINSe FOR ONE DAY OF RECORD)e NeleOe PROGRAM NOco 178¢ AUTHOR-— We Je
GOULDe
NATIONAL INSTITUTE OF OCEANOGRAPHY
WORMLEY»s GODALMINGs SURREY
ENGLAND
Q FACTORS LANGUAGE - FORTRAN V
COMPUTER = ATLAS I
CALCULATES THE PRESSURE IN DECIBARS FROM THE READING OF T(U)-T(W) Glv-
EN BY AN UNPROTECTED REVERSING THERMOMETERe THE OUTPUT CONSISTS OF A
TABLE OF VALUES OF PRESSURE FOR TEMPERATURES IN STEPS OF Ocl DEGR Ceo
NeleQce PROGRAM 636 AUTHOR-- ELIZABETH PALETHORPEe DESCRIBED IN NeleOeo
INTERNAL REPORT NOc 7s JAN 19686
NATIONAL INSTITUTE OF OCEANOGRAPHY
WORMLEY» GODALMING»s SURREY
ENGLAND
NIO PROGRAM 59 — THERMOMETER CORRECTIONS FOR LANGUAGE -— CHLF 3/4
DEEP-SEA REVERSING THERMOMETERS COMPUTER -— MERCURY
BOTH PROTECTED AND UNPROTECTED THERMOMETERS CAN BE DEALT WITHe CORR-
ECTIONS ARE DEPENDENT ON THE WATER TEMPERATURE, THE AMBIENT TEMPERA-
TURE IN THE LABORATORY» AND THE INDEX ERRORS OF THE THERMOMETERS» AU-
THOR=- JAMES CREASEe REFo NeIleO5o INTERNAL REPORT NOco N6o
PAGE 015
NATIONAL INSTITUTE OF OCEANOGRAPHY
WORMLEY»s GODALMINGs SURREY
ENGLAND
DEEp LANGUAGE — FORTRAN
COMPUTER — HP 2115A
(COPY ON FILE AT NODC)
DIGITIZES SALINITY-TEMPERATURE-DEPTH DATA ON LINE USING TIME AS CRI-
TERION FOR SELECTING POINTSe INPUT ARE FREQUENCIES FROM SeTeDe SYSTEM
AND STATION HEADING DATA THROUGH TELETYPEe OUTPUT ON PAPER TAPE HAS
STATION IDENTIFICATION FIELDS, TIME INTERVAL BETWEEN DATA POINTS, AND
THE SeTeDe DATA — PRESSURE» TEMPERATURE» SALINITYe REFe FRB TECHNICAL
REPORT NOe 152 (DEC 1969)» BY Ae HUYER AND Ce Ace COLLINS (UNPUBe MSe)
DRe Ce Ae COLLINS
MARINE SCIENCES BRANCHs DEMR
PACIFIC OCEANOGRAPHIC GROUP
BIOLOGICAL STATION
NANAIMOs BeCe» CANADA
TCHK2 (THERMOMETER CORRECT ) LANGUAGE — FORTRAN VI
COMPUTER — IBM 1130
(COPY ON FILE AT NODC)
PURPOSE-- TO CORRECT DEEP-SEA REVERSING THERMOMETERS» TO COMPUTE THER-
MOMETRIC DEPTHSs TO ALLOW SPURIOUS VALUES TO BE REMOVED FROM THE I-Z
TABLE» TO SMOOTH THE L-z TABLEs AND TO PUNCH SMOOTHED DEPTH AND OB-
SERVED TEMPERATURE AND SALINITY AND OXYGEN VALUES ONTO CARDS IN CODC
FORMATe PROGRAM AND SUB-—PROGRAMS DESCRIBED IN FRB MANUSCRIPT REPORT
NOe 1071 (DEC 1969s UNPUBLISHED MANUSCRIPT)» BY Ce Ae COLLINS» Re Le
Ke TRIPE» AND Se Ke WONGe POG HAS TWO OTHER THERMOMETER CORRECTION
PROGRAMS — TCHK1 USES THE L/Z METHOD, TCHK3 COMPUTES PRESSUREe
PACIFIC OCEANOGRAPHIC GROUP
BIOLOGICAL STATION
NANAIMOs BeCes CANADA
TEMPERATURE AND DEPTH CALCULATIONS LANGUAGE — FORTRAN AND
AUTOCODER
COMPUTER — I8M 1620 AND
IBM 1401
(COPY ON FILE AT NODC)
AT PRESENT THERE IS NO PROVISION FOR CALCULATING WIRE ANGLE DEPTHe
DENSITY VALUES USED ARE THOSE FOR THE NORTH ATLANTICe THE INPUT IS IN
TWO PARTSe FIRST THE THERMOMETER TABLES ARE READ INy THEN THE DATA
CARDSe THE OUTPUT CARD IS A REPRODUCTION OF THE INPUT DATA CARD, PLUS
ALL NECESSARY CALCULATIONSe AUTHORS-- DeTe EGER» Dele SHAFFER.
UNIVERSITY OF MIAMI
MARINE LABORATORY
COMPUTING CENTER
1 RICKENBACKER CAUSEWAY
VIRGINIA KEYs MIAMI» FLORIDA
THERMOMETER CORRECTION LANGUAGE — FORTRAN IV
COMPUTER — HONEYWEIL516
(COPY ON FILE AT NODC)
CORRECTS DEEP-SEA REVERSING THERMOMETERS AND CALCULATES THERMOMETRIC
DEPTHS» GIVEN THE THERMOMETER CONSTANTS AND THE INDIVIDUAL THERMOMETER
READINGSe TELETYPE 1/0 -— HIGH SpEED PAPER TAPE READER DESIRABLE
COMMANDING OFFICER
UeSe COAST GUARD OCEANOGRAPHIC UNIT
BLDGe 159-E» NAVY YARD ANNEX
WASHINGTON» De Ce 20390
PAGE 016
THERMOCHECK II -— TEMPERATURE CORRECTION LANGUAGE — FORTRAN IV
COMPUTER -— CDC 3100 AND
IBM 360/65
(COPY ON FILE AT NODC)
CORRECTS DEEP-SEA REVERSING THERMOMETERS,» CALCULATES THERMOMETRIC
DEPTHe AUTHOR-— LEO Me FLETCHERe THE ORIGINAL VERSIONs WITH DOCU-
MENTATIONs WAS WRITTEN IN FORTRAN FOR THE IBM 16206
CANADIAN OCEANOGRAPHIC DATA CENTRE
615 BOOTH STREET
OTTAWAs CANADA
TWO FIVE (HYDROGRAPHIC DATA REDUCTION) LANGUAGE — FORTRAN 63,5
FORTRAN IV
COMPUTER -— CDC 3600»
IBM 1800
PROCESSES RAW DATA TO OBTAIN CORRECTED DEPTH» TEMPERATURE», SALINITY >
AND OXYGEN-- 1) PROTECTED DEEP-SEA REVERSING THERMOMETER READINGS TO
OBTAIN THE CorRECTED IN-SITU WATER TEMPERATUREe 2) UNPROTECTED DEEP-
SEA REVERSING THERMOMETER READINGS TO OBTAIN THE THERMOMETRIC DEPTHs
CORRECTED FOR GRAVITY VARIATIONS AND FOR THE MEAN DENSITY OF THE OVER-
LAYING WATER COLUMN IN ANY OCEANe 3) FITS LEAST SQUARES CURVES TO
WIRE LENGTH VSe (WIRE LENGTH MINUS THERMOMETRIC DEPTH) TO DETERMINE
THE ACCEPTED DEPTHe 4) CALCULATES SALINITY FROM RAW SALINITY READINGS
5) CALCULATES DISSOLVED OXYGEN CONCENTRATIONS FROM TITRATIONSe REFe
A REPORT (UNPUBLISHED MANUSCRIPT) BY NORMA MANTYLAe
MRSe NORMA Le MANTYLA
MARINE LIFE RESEARCH GROUP
SCRIPPS INSTITUTION OF OCEANOGRAPHY
PeOo BOX 109
LA JOLLA» CALIFORNIA 92037
SeleDe DATA PROCESSING LANGUAGE — FORTRAN IV
COMPUTER - CDC 3600
(COPY ON FILE AT NODC)
A PROGRAM WITH SUBROUTINES TO PROCESS SALINITY-TEMPERATURE-DEPTH DATA
RECORDED IN THE FIELDe DESCRIPTION AND LISTINGS IN A BCF SPECIAL SCI-
ENTIFIC REPORT — FISHERIES NOe 588 'PROCESSING OF DIGITAL DATA 1OGGER
STD TAPES AT THE SCRIPPS INSTITUTION OF OCEANOGRAPHY AND THE BUREAU OF
COMMERCIAL FISHERIES» LA JOLLA CALIFORNIA! (JUNE 1969). BY DRe JAMES
He JONES.
DRe BRUCE TAFT
OCEANIC RESEARCH DIVISION
SCRIPPS INSTITUTION OF OCEANOGRAPHY
PeOe BOX 109
LA JOLLAs CALIFORNIA 92037
THERMOMETER CORRECTION AND THERMOMETRIC DEPTH LANGUAGE — FORTRAN
COMPUTER -— IBM 7074
(COPY ON FILE AT NODC)
COMPUTES THERMOMETER CORRECTIONS AND THERMOMETRIC DEPTHS AND THEN
PRINTS THIS DATA IN THE FORMAT OF THE UeSe NAVAL OCEANOGRAPHIC 10G
SHEET "Ate IMR NOe O-9-63 (UNPUBLISHED MANUSCRIPT)» AUTHOR-- Se Co
PORTERe
COMPUTER SYSTEMS DIVISION
NATIONAL OCEANOGRAPHIC DATA CENTER
WASHINGTONs De Ceo 20390
PAGE 017
BATHYMETRIC DATA REDUCTION LANGUAGE —- FORTRAN
COMPUTER — IBM 7074
PROCESSES DATA GATHERED WHILE NAVIGATING WITH ANY CIRCULAR AND/OR Hy-
PERBOLIC SYSTEMe EIGHT OPTIONS ARE AVAILABLE PERTAINING TO POSITION
CONVERSIONs FORM OF INPUTs DATA SMOOTHINGs SPECIAL CORRECTIONS, AND
INTERPOLATION OF POSITION-DEPENDENT VALUES SUCH AS CONTOUR CROSSINGS.
OS NO. 53559.
Ge Ce DONOHUEs CODE 8006
NAVAL OCEANOGRAPHIC OFFICE
SUITLAND» MD. 20390
SYNOPTIC PROGRAM (UWMS-0980) LANGUAGE —- FORTRAN II
COMPUTER — IBM 7094-II/
7040 DCS AND
cDC 6400
(COPY ON FILE AT NODC)
REDUCES DATA FROM RAW SHIP-BOARD OBSERVATIONSe CORRECTS THERMOMETERS
AND COMPUTES THERMOMETRIC DEPTHS, WIRE ANGLE DEPTHS, SALINITIES FROM
BRIDGE READINGS» OXYGEN VALUES FROM TITRATIONSs THEN COMPUTES SIGMA-T >
OXYGEN SATURATION PERCENTs AND APPARENT OXYGEN UTILUZATIONe CORE STO-
RAGE REQUIRED-- 255335 WORDS FOR MAIN PROGRAMs 2058 WORDS FOR SUBROUT—
INESe REFe A 150 PAGE REPORT (UWMS-0980, APR 1967) AND TECHNICAL RE-
PORT NO» 181 (M67-8» JAN 1968)» BY EUGENE Ee COLLIASe THERE IS ALSO
A MORE LIMITED VERSION FOR THE IBM-11305« REVISED 1969 FOR THE CDC-
6400.
He MACINTOSH, COMPUTER SERVICES
DEPARTMENT OF OCEANOGRAPHY
UNIVERSITY OF WASHINGTON
SEATTLE» WASHe 98105
UNDERWAY DATA SYSTEM LANGUAGE — FORTRAN
COMPUTER - IBM 1130
PROCESSES DATA COLLECTED FROM UP TO 7 MONITORED SENSORS AND FROM THE
AUTOANALYZER WHILE UNDERWAY. INPUT-—- PAPER TAPE — RECORDS TAKEN ABOUT
ONCE A MINUTE.’ OUTPUT-- COLLECTED DATA PUNCHED ON CARDS AVERAGED OVER
A GIVEN PERIODe DATA IS THEN USUALLY RUN THROUGH THE IBM CONTOURING
SYSTEM (NCS) AND PLOTTEDe DOCUMENTATION-— OPERATING INSTRUCTIONS ONLY
UNIVERSITY OF WASHINGTON
DEPARTMENT OF OCEANOGRAPHY
22A OCEANOGRAPHY TEACHING BLDGe
ATTNe MRSe HELLA MACINTOSH
SEATTLE» WASH. 98105
SALINITY-TEMPERATURE-DEPTH CALCULATIONS LANGUAGE —- FORTRAN IV,
ASSEMBLER
COMPUTER — I8M 1130
THIS SYSTEM READS AND EDITS PAPER TAPE FROM A BISSETT-BERMAN STD CASTe
THE RAW DATA (FREQUENCIES) ARE CONVERTED TO REAL VALUESe INPUT TO
PROGRAM-— PUNCHED PAPER TAPE FROM THE HEWLETT-PACKARD DAS» FOUR CHAN-
NELS ARE PUNCHED — SALINITY, TEMPERATURE» SOUND VELOCITY, AND DEPTHe
OUTPUT-- LISTING OF REAL VALUES», PLOT OF EACH VARIABLE VSe DEPTH, AND
A SECTION PLOT OF SALINITY AND/OR TEMPERATURE VSe DEPTH FOR A MAXIMUM
OF 10 STATIONSs DOCUMENTATION--— OPERATING INSTRUCTIONS ONLYe
UNIVERSITY OF WASHINGTON
DEPARTMENT OF OCEANOGRAPHY
22A OCEANOGRAPHY TEACHING BLDGe
ATTNe MRSe HELLA MACINTOSH
SEATTLE» WASHe 98105
PAGE 018
Sele
HYDR
TEMP
De CORRECTION LANGUAGE — FORTRAN IV
COMPUTER — IBM 7094
CORRECTS THE SALINITY AS RECORDED BY THE SeTeDe INSTRUMENT FOR ERRORS
INTRODUCED BY THE TEMPERATURE GRADIENTs LOWERING SPEED» AND TIME CON-
STANT OF THE SeTeDe AUTHOR-— Je HUBERTZ.e
TEXAS A AND M UNIVERSITY
COLLEGE OF GEOSCIENCES
DEPARTMENT OF OCEANOGRAPHY
COLLEGE STATIONs TEXAS 77843
(0) LANGUAGE —- FORTRAN IV-E
COMPUTER — IBM 360/50
PROVIDES I/0 FOR HYDROGRAPHIC DATAe USES SUBROUTINES TO CORRECT RE-
VERSING THERMOMETERS AND CALCULATE THERMOMETRIC DEPTHe APPLIES METER
WHEEL CORRECTION» AVERAGES TEMPERATURE VALUES» WRITES ALTERNATE VALUES
WHERE NECESSARYe WRITES APPROPRIATE MESSAGES ON CONDITION OF DATAe
WRITES THERMOMETER HISTORY SHOWING WHICH THERMOMETERS MALFUNCT IONED
AND WHICH PAIRS OF PROTECTED THERMOMETERS YIELD ALTERNATE VALUES.
SUBROUTINES NEEDED-- TEMPs LINT» UTEMPs AZIZe WRITE-UPS FOR THIS AND
OTHER UNIVe OF Re Ie PROGRAMS FOR PROCESSING OF HYDROGRAPHIC DATA ARE
PRINTED IN A MEMORANDUM, DATED JANUARY 19705 WRITTEN BY Re Ke SEXTON®
ROBERT Ke SEXTON
NARRAGANSETT MARINE LABORATORY
UNIVERSITY OF RHODE ISLAND
KINGSTON» RHODE ISLAND 02881
LANGUAGE - FORTRAN IV-E
COMPUTER - IBM 360/50
SUBROUTINE CALCULATES INDEX AND THERMAL EXPANSION CORRECTIONS FOR PRO-
TECTED REVERSING THERMOMETERS», ASSOCIATES A TOLERANCE WITH EACH THER-
MOMETER ACCORDING TO RANGEs SETS MESSAGE INDICATORS FOR VARIOUS DATA
CONDITIONSe AUXILIARY AND MAIN INDEX CORRECTIONS ARE COMPUTED By
LINEAR INTERPOLATION BETWEEN POINTS IN THE THERMOMETER DATA ARRAY 5
"PTHRMt.» THERMAL EXPANSION CORRECTION IS COMPUTED USING EQUATION (29)
PAGE 1ls FROM 'ON THE FORMULA FOR CORRECTING REVERSING THERMOMETERS! 4
BY FeKe KEYTEs WHOIs REFe NOo 64-29.
SUBROUTINES NEEDED-- LINT.
ROBERT Ke SEXTON
NARRAGANSETT MARINE LABORATORY
UNIVERSITY OF RHODE ISLAND
KINGSTON» RHODE ISLAND 02881
UTEmP LANGUAGE - FORTRAN IV-E
COMPUTER — IBM 360/50
SUBROUTINE CALCULATES INDEX AND THERMAL EXPANSION CORRECTIONS FOR UN-
PROTECTED THERMOMETERSe IT SELECTS A #Q* VALUE APPROPRIATE TO THE
DEPTH OF REVERSALe SETS MESSAGE INDICATORS FOR VARIOUS DATA CONDI-
TIONSe AUXILIARY AND MAIN INDEX CORRECTIONS ARE COMPUTED BY LINEAR
INTERPOLATION BETWEEN POINTS IN THE THERMOMETER ARRAY» '"UTHRMte
THERMAL EXPANSION CORRECTION IS COMPUTED USING EQUATION (8)» PAGE 8»
FROM "ON THE FORMULAS FOR CORRECTING REVERSING THERMOMETERS'» BY FeKe
KEYTE» WHOIs REFe NOco 64-29. IF A 'Q' VALUE FOR THE THERMOMETER IN
QUESTION CHANGES WITH DEPTH, WIRE LENGTH IS USED TO COMPUTE THE
CORRECT VALUE BY LINEAR INTERPOLATION BETWEEN PRESSURE POINTSe IF THE
WIRE LENGTH IS OUTSIDE THE END POINTSs #Q* VALUES CORRESPONDING TO THE
END POINT VALUE ARE USEDe
SUBROUTINE NEEDED-- LINT
ROBERT Ke SEXTON
NARRAGANSETT MARINE LABORATORY
PAGE 019
UNIVERSITY OF RHODE ISLAND
KINGSTON» RHODE ISLAND 02881
REVERSING THERMOMETER CORRECTION LANGUAGE — FORTRAN IV
COMPUTER — IBM 360/65
CALCULATIONS OF CORRECTED TEMPERATURES AND THERMOMETRIC DEPTHS FROM
REVERSING THERMOMETER READINGSe OUTPUT INCLUDES AVERAGE TEMPERATURE,
DIFFERENCE BETWEEN CORRECTED TEMPERATURES» AND L-Z VALUESe
BUREAU OF COMMERCIAL FISHERIES BIOLOGICAL LABe
ATTNe DRe Re Ace BARKLEY
PeO5o BOX 3830
HONOLULU» HAWATI 96812
THERMOMETER CORRECTION AND THERMOMETRIC DEPTH LANGUAGE — PAL III
COMPUTER — PDP-5, 8S
(COPY ON FILE AT NODC)
CORRECTS BOTH PROTECTED AND UNPROTECTED REVERSING THERMOMETERSe DET-
ERMINES THERMOMETRIC DEPTH BY AN ITERATIVE PROCESSe CAN CORRECT A
MAXIMUM OF 58 THERMOMETERSe DESIGNED FOR USE ABOARD VESSELe WRITTEN
FoR THE UeSe COAST GUARD BY LTe ReMe O'HAGAN (RETe)s DIGITAL EQUIPMENT
CORPe»s MAYNARD» MASSe COPY OF PROGRAM IS DEPOSITED WITH DECUSe REF.
UeSe COAST GUARD OCEANOGRAPHIC MANUSCRIPT "OCEANOGRAPHIC COMPUTER PRO-
GRAMS FOR THE PDP-5'» 15 OCTe 1964 (UNPUBLISHED MANUSCRIPT) e
DIGITAL EQUIPMENT CORPORATION
MAYNARD» MASSACHUSETTS 01754
HYLOG LANGUAGE — FORTRAN IV-H
COMPUTER -— SDS SIGMA 7
TAKES RAW OCEANOGRAPHIC STATION DATAs CORRECTS THE TEMPERATURES AND
FINDS THE DEPTH OF EACH OBSERVATIONe INPUT-- CARDS AND 9-TRACK MAG-
NETIC TAPE IN GENERALIZED FORMATe CORE STORAGE NEEDED-- 149452 WORDS.
INFORMATION PROCESSING CENTER
ATTNe MARY HUNT
WOODS HOLE OCEANOGRAPHIC INSTITUTION
WOODS HOLEs MASSACHUSETTS 02543
THRCL LANGUAGE — FORTRAN IV-H
COMPUTER - SDS SIGMA 7
PREPARES A MAGNETIC TAPE FILE OF THERMOMETER CALIBRATION RECORDS TO BE
USED WITH PROGRAM 'HYLOGt. THE THERMOMETER CALIBRATIONS ARE INPUT ON
CARDS.
INFORMATION PROCESSING CENTER
ATTNe MARY HUNT
WOODS HOLE OCEANOGRAPHIC INSTITUTION
WOODS HOLEs MASSACHUSETTS 02543
PAGE 020
EDITING AND SPECIAL INPUT/OUTPUT
—H—H%—H—K—HK—H—-H—H—K—H—H—H—H—H—H—*
COMPUTER UTILITY PROGRAM LANGUAGE — FORTRAN
COMPUTER — CDC 3800
PROVIDES I/0 MEDIA TO MEDIA CONVERSIONS AND/OR TRANSFERS UNDER COMPUT—
ER OPERATING SYSTEMS CONTROLe THIS PROGRAM PROVIDES A SIMPLE METHOD
TO COPYs PRINTs COMPAREs PUNCHs SKIP» OR DESCRIBE RECORDS AND FILES
ON AN INPUT SOURCE TO THE CDC 3800 COMPUTERe NRL MEMOe REPORT 19356
AUTHORS-- Te ROZANSKI»s Je BURGESS» De GOSSETTs De SHANNON.’
DORIS E. GOSSETT
RESEARCH COMPUTATION CENTER
MATHEMATICS AND INFORMATION SCIENCES DIVISION
NAVAL RESEARCH LABORATORY» WASHINGTON» De Co 20390
NELEDIT LANGUAGE — FORTRAN
COMPUTER -— CDC 3800
EDITS CARDS OR CARD IMAGES UNDER OPERATING SYSTEM CONTROLe PROVIDES
A SIMPLE METHOD OF RESEQUENCINGs SEQUENCINGs PRINTINGs INSERTING, DEL-
ETING AND REPLACING CARD IMAGES WHICH EXIST ON AN INPUT SOURCE TO THE
COMPUTERe NRL MEMOe REPORT 19366 AUTHORS-- Je BURGESS» De GOSSETT»s
De SHANNON.
DORIS Ee. GOSSETT
RESEARCH COMPUTATION CENTER
MATHEMATICS AND INFORMATION SCIENCES DIVISION
NAVAL RESEARCH LABORATORY» WASHINGTONs De Ce 20390
JOB EDIT FOR L-Z PROGRAM LANGUAGE - AUTOCODER
COMPUTER - IBM 1401
(COPY ON FILE AT NODC)
USES OUTPUT TAPE FROM TEMPERATURE AND DEPTH PROGRAM AS INPUTe AUTHOR--
DeLe SHAFFER.
UNIVERSITY OF MIAMI
MARINE LABORATORY
COMPUTING CENTER
1 RICKENBACKER CAUSEWAY
VIRGINIA KEY» MIAMI» FLORIDA
A TAPE INPUT AND OUTPUT SUBROUTINE LANGUAGE — AUTOCODER
COMPUTER - IBM 7074
(COPY ON FILE AT NODC)
THE *"TAPIO*' (TAPE INPUT AND OUTPUT) PROGRAM IS DESIGNED TO BE CALIED
BY FORTRANe IT CAN BE USED To OPERATE DATA TAPES MUCH FASTER THAN
OTHERWISE POSSIBLE» MAKING USE OF THE FEATURE OF 'SIMULTANEITY*e ALSO,
IT WILL CALL AN *EDIT* PROGRAM AS REQUIREDs FOR INPUT AND OUTPUT PRO-
CEDURESe USING TAPIO MAKES IT NECESSARY TO WRITE YOUR OWN EDIT PRO-
GRAMe REFe IMR NOc M—-2-645 JAN 1965 (UNPUBLISHED MANUSCRIPT )e AUTHOR
— PHILLIP Je LAUTENSCHLAGER.
DATA SYSTEMS CENTER» CODE 083
NAVAL OCEANOGRAPHIC OFFICE
SUITLANDs MDe 20390
LORAN EDIT LANGUAGE — FORTRAN
COMPUTER - IBM 7074
(COPY ON FILE AT NODC)
EDITS LORAN RATES FOR CHARTING COORDINATES AND/OR FINAL LORAN-A AND
LORAN-C TABLE PUBLICATIONe REFe A REPORT IR NOce 69-875 OCT 19695 BY
PAGE 021
KATHLEEN Ae JENNINGS» WHICH DESCRIBES THIS AND OTHER PROGRAMS AND PRO-
CEDURES USED AT THE NAVAL OCEANOGRAPHIC OFFICE IN THE LORAN TABLE ED-
ITING PROCESS. FURTHER INFORMATION MAY BE OBTAINED FROM THE FIELD
MANAGEMENT AND DISSEMINATION DEPTe (CODE 44), OR THE AUTHORe
NAVIGATIONAL SCIENCE DIVe,s CODE 5320
TECHNICAL PRODUCTION DEPT.
NAVAL OCEANOGRAPHIC OFFICE
SUITLAND» MD. 20390
SOUND SPEED EDIT LANGUAGE —- FORTRAN
COMPUTER — IBM 7074
TAKES NODC DATA CARDS HAVING TIME SERIES SOUND SPEED DATA, ADDS ON A
BOTTOM PART BECAUSE THE TIME SERIES DATA DOES NOT GO TO THE BOTTOM OF
THE WATER COLUMN»s AND REARRANGES THE DATA TO MAKE IT ACCEPTABLE TO
THE RAY TRACE PROGRAM OF CISNEYe OS NOs 53817e¢ AUTHOR-—- ReRe GLEASONe
EXPLORATORY OCEANOGRAPHY DIVe, CODE 7200
NAVAL OCEANOGRAPHIC OFFICE
SUITLAND» MD. 20390
CARDS LANGUAGE — FORTRAN IV-E
COMPUTER - IBM 360/50
CONVERTS PUNCHED OUTPUT FROM 'SIGMAT' TO INPUT FOR 'HEIGHT'e
ROBERT Ke SEXTON
NARRAGANSETT MARINE LABORATORY
UNIVERSITY OF RHODE ISLAND
KINGSTON» RHODE ISLAND 02881
DEPTHS LANGUAGE — FORTRAN IV-E
COMPUTER — IBM 360/50
CONVERTS PUNCHED OUTPUT FROM "HYDRO! TO INPUT FOR 'SIGMAT'«
ROBERT Ke SEXTON
NARRAGANSETT MARINE LABORATORY
UNIVERSITY OF RHODE ISLAND
KINGSTON» RHODE ISLAND 02881
RDTHRM LANGUAGE — FORTRAN IV-E
COMPUTER — IBM 360/50
READS THERMOMETER DATA AS IT IS READ BY tHYDROt AND WRITES OUT THE
DATA IN A FORMAT SUITABLE FOR CHECKINGe
ROBERT Ke SEXTON
NARRAGANSETT MARINE LABORATORY
UNIVERSITY OF RHODE ISLAND
KINGSTON» RHODE ISLAND 02881
DATA LANGUAGE — FORTRAN IV-H
COMPUTER — SDS SIGMA 7
SUBROUTINE READS OCEANOGRAPHIC STATION DATA CARDS AND RETURNS THE IN-
FORMATION CONTAINED THEREIN TO THE USERs ONE STATION FOR EACH CALLe
INFORMATION PROCESSING CENTER
ATTNe MARY HUNT
WOODS HOLE OCEANOGRAPHIC INSTITUTION
WOODS HOLE» MASSACHUSETTS 02543
PAGE 022
SCRUB LANGUAGE — FORTRAN IV-H
COMPUTER — SDS SIGMA 7
PROVIDES SEVERAL METHODS BY WHICH DATA STORED IN WHOI STANDARD FORMAT
MAY BE EDITED AND TESTEDe OUTPUT IS THE CORRECTED vERSION OF THE DATA
ON 9-TRACK MAGe TAPE
INFORMATION PROCESSING CENTER
ATTNe JOHN Ae MALTAIS
WOODS HOLE OCEANOGRAPHIC INSTITUTION
WOODS HOLEs MASSACHUSETTS 02543
BATHYTHERMOGRAPH OUTPUT LANGUAGE — SPS
COMPUTER — IBM 1401
(COPY ON FILE AT NODC)
TAPE TO CARD/PRINT EDITING PROGRAMe BLOCKED INPUT WITH MSQ@ OR CRUISE
SEQUENCE FORMS CONTROLe USES TAPE SEARCH, SELECTION AND DUPLICATION.
OS NOs 52291. AUTHOR--— JeCe JENSONe
COMPUTER SYSTEMS DIVISION
NATIONAL OCEANOGRAPHIC DATA CENTER
WASHINGTON>s De Ce 20390
CARD-TO-TAPE FOR INPUT TO THE 7074 LANGUAGE —- SPS II
COMPUTER — IBM 1401
(COPY ON FILE AT NODC)
SPECIAL CARD-TO-TAPE ROUTINE FOR DATA INPUT TO THE IBM 70749 WITH
OPTIONAL ZONE PUNCH EDITINGs PRINTOUT OF TAPE RECORDS» MULTI-FILE
PROVISIONSe AUTHOR-= LARRY WOLCOTTe
COMPUTER DEPARTMENTs CODE 083
NAVAL OCEANOGRAPHIC OFFICE
SUITLANDs MDe 20390
OCEANS II REPORT GENERATOR LANGUAGE — SPS
COMPUTER - IBM 1401
(COPY ON FILE AT NODC)
USED FOR HIGH SPEED PREPARATION OF OCEANS II OUTPUT FOR DATA RECORD
PUBLICATIONe (NOTE-- CODC IS NOW USING A LATER VERSION OF THIS DECKe)
CANADIAN OCEANOGRAPHIC DATA CENTRE
615 BOOTH STREET
OTTAWA» CANADA
CONVERSION» NODC TO ICES LANGUAGE —- SPS
COMPUTER -— IBM 1401
(COPY ON FILE AT NODC)
CONVERTS NODC OCEAN STATION DATA ON CARDS/TAPE TO ICES FORMAT CARDSe
INCLUDES OPTIONAL SUBROUTINE IN SPS LANGUAGE FOR CALCULATION OF OXxYGEN
PERCENT OF SATURATION USING FOX*S FORMULAEe OS NOc 522826 AUTHOR —-
Ce DINGERe NODC-ICES AND ICES-NODC CONVERSION PROGRAMS ARE CURRENTLY
BEING COMPLETELY REWRITTEN FOR THE IBM 360/405 IN ASSEMBLER AND PL/I
LANGUAGES» BY SALLY KEEHNe
COMPUTER SYSTEMS DIVISION
NATIONAL OCEANOGRAPHIC DATA CENTER
WASHINGTON>s De Ce 20390
OCEAN STATION DATA OUTPUTs NODC FORMAT LANGUAGE —- SPS
COMPUTER - IBM 1401
(COPY ON FILE AT NODC)
OCEAN STATION RECORDS ON TAPE ARE PUNCHED ON CARDS AND/OR EDITED INTO
PRINTOUT. OS NOe 52280. ANOTHER VERSION OF THIS PROGRAM PRINTS» FOR
FINAL NODC FILESs MONITORED STATION DATA FROM ZONE-EDITED, BLOCKED AND
SORTED TAPE RECORDSe OS NOe 522875 BY Ce DINGERe A NEW STATION DATA
PAGE 023
OUTPUT PROGRAM IS AT PRESENT BEING WRITTEN FOR THE IBM 360/40» IN PL/I
LANGUAGE, BY JOHN MCHUGH.
COMPUTER SYSTEMS DIVISION
NATIONAL OCEANOGRAPHIC DATA CENTER
WASHINGTON» De Ceo 20390
STATION DATA CONVERSION» CODC To NODC LANGUAGE — SPS
COMPUTER — IBM 1401
(COPY ON FILE AT NODC)
CANADIAN OCEANOGRAPHIC DATA CENTRE STATION DATA IS TRANSFERRED OR CON-
VERTED TO THE NEW NODC FORMATe CODC CRUISE MASTER CARDS MUST BE PRE-
CEDED BY A NODC LEADER CARD. OS NOe 522126 AUTHOR-— RUDI SAENGER.
COMPUTER SYSTEMS DIVISION
NATIONAL OCEANOGRAPHIC DATA CENTER
WASHINGTON» De Ce 20390
PAGE 024
GEOSCIENCE
ee
%-#-# GEOQPHYSICSs MARINE %—#-+
BLACKBODY SPECTRAL RADIANCE LANGUAGE —- FORTRAN
COMPUTER ~— CDC 3800
COMPUTES SPECTRAL RADIANCE OF A BLACKBODY RADIATOR USING ONE DEGREE
INCREMENTS OF TEMPERATURE AND 06605 MICROMETER INCREMENTS OF WAvyE-
LENGTHe INPUT PARAMETERS ARE TEMPERATURE ASD WAVELENGTHe
APPLIED OCEANOGRAPHY BRANCH —- CODE 8310
NAVAL RESEARCH LABORATORY
WASHINGTONs De Ce 20390
BLACKBODY RADIANCE LANGUAGE —- FORTRAN
COMPUTER -— CDC 3808
COMPUTES RADIANCE OF A BLACKBODY RADIATOR IN A SPECIFIED WAVELENGTH
INTERVAL USING ONE DEGREE INCREMENTS OF TEMPERATURE AND 0-05
MICROMETER INCREMENTS OF WAVELENGTHe INPUT PARAMETERS ARE TEMPERATURE
AND WAVELENGTH.
APPLIED OCEANOGRAPHY BRANCH —- CODE 8310
NAVAL RESEARCH LABORATORY
WASHINGTON» De Ce 20390
LONG WAVE RADIATION LANGUAGE - FORTRAN IV
COMPUTER - IBM 360/65
CALCULATES RADIATION VALUES FOR THE SUOMI-KUHN RADIOMETER. INPUT DATA
FROM THE TRADE WIND ZONE OCEANOGRAPHY PROGRAM RADIATION CARDSe
BUREAU OF COMMERCIAL FISHERIES
2570 DOLE STREET
HONOLULUs HAWAII 96812
OBSERVATION DRAPING (GRAVITY) LANGUAGE - FORTRAN
COMPUTER — IBM 7074
REDUCES OBSERVATION DATA TAKEN WITH LACOSTE-ROMBERG SEA/AIR OR SUB-
MARINE GRAVIMETERS TO OBSERVED GRAVITY VALUE AND FREE-AIR ANOMALY.
INTERPOLATES GEOGRAPHIC POSITION FROM SMOOTHED FIX» COURSE» AND SPEEDe
GENERATES BC CHART NOe AND XsY COORDINATES FOR MERCATOR PROYECTION FOR
EACH STATIONe OS NOco 535432 AUTHOR-—- ReKe LATTIMORE®e
GRAVITY DIVISIONs CODE 83
NAVAL OCEANOGRAPHIC OFFICE
SUITLANDs MDe 20390
REDUCTION AND DISPLAY OF DATA ACQUIRED AT SEA LANGUAGE - FORTRAN II
COMPUTER — IBM 1130
(COPY ON FILE AT NODC)
A SYSTEM OF PROGRAMS (NAVIGATIONs GRAVITY» TOPOGRAPHY» MAGNETICS) FOR
THE REDUCTIONs STORAGE AND DISPLAY OF UNDERWAY DATA ACQUIRED AT SEAe
THE COMPUTER INSTALLATION CONSISTS OF AN IBM 1130 AND INCLUDES RANDOM
ACCESS DISK CARTRIDGES AND AN ON-LINE CALCOMP 30 INe PLOTTERe A LARGE
NUMBER OF THE PROGRAMS UTILIZE NAVIGATION POINTS TOGETHER WITH RAW
DIGITIZED GEOPHYSICAL DATA PRESENTED AS A TIME SERIES» WHERE THE DIFF-
ERENT DATA MAY BE READ AT UNEQUAL TIME INTERVALSe REFe TECHe REPORT
NOe 1 (AUGUST 19695 348 Pe) BY MANIK TALWANTe
PAGE 025
LAMONT-DOHERTY GEOLOGICAL OBSERVATORY
COLUMBIA UNIVERSITY
PALISADES» NEW YORK 10964
TALWANI 2-D GRAVITY LANGUAGE — FORTRAN IV-H
COMPUTER - IBM 360/65
(COPY ON FILE AT NODC)
CALCULATES THE VERTICAL COMPONENT OF GRAVITATIONAL ATTRACTION OF TWO-
DIMENSIONAL BODIES OF ARBITRARY SHAPE BY APPROXIMATING THEM TO MANY—
SIDED POLYGONS. THE TECHNIQUE IS FROM TALWANI, WORZELs AND LANDISMAN
IN JGR» VOLe 64 NOw 1» 1959. OUTPUT-- THE GRAVITY VALUES ARE PRINTED
IN TABLES» AND THE CALCULATED PROFILE AND THE OBSERVED PROFILE IF ONE
EXISTS ARE PLOTTED ON THE LINE PRINTER IN EITHER A PAGE SIZE PLOT OR
AN EXTENDED PLOT WITH THE X-AXIS RUNNING DOWN THE PAGEe PROGRAM CON-—
TAINS OPTION OF UNITS IN MILESs KILOFEETs OR KILOMETERSe THE PROGRAM
NOe IS W9206 (MAYs 1968).
Use Se GEOLOGICAL SURVEY
COMPUTER CENTER DIVISION
ATTNe RALPH EICHERs CHIEF
BRANCH OF SCIENTIFIC APPLICATIONS
WASHINGTONs De Ce 20242
PROFILE CARD-TO-TAPE FOR GEOPAC LANGUAGE — FORTRAN IV-H
COMPUTER — IBM 360/65
(COPY ON FILE AT NODC)
USED TO PUT DATAs USUALLY PROFILE DATA» PUNCHED ON CARDS ONTO MAGNETIC
TAPE FOR SUBSEQUENT PROCESSING BY OTHER PROGRAMS IN A PACKAGE OF PRO-
GRAMS FOR TWO-DIMENSIONAL GRAVITY AND MAGNETIC CALCULATIONSe OPTIONS
IN THE PROGRAM ALLOW FOR THE PRELIMINARY OPERATIONS OF SCALING, SHIFT-
ING, OR DETRENDING THE DATAs’ PROFILES MAY ALSO BE CONCATENATED TO
COMBINE SEVERAL DATA SETS AS ONEe PROGRAM NOe W9325,5 BY RALPH EICHERe
Use Se GEOLOGICAL SURVEY
COMPUTER CENTER DIVISION
ATTNe RALPH EICHERs CHIEF
BRANCH OF SCIENTIFIC APPLICATIONS
WASHINGTON»s De Co 20242
2D MAGNETIC ANOMALIES LANGUAGE — FORTRAN
COMPUTER — IBM 1800 SYS
COMPUTES HORIZONTAL AND VERTICAL AND TOTAL MAGNETIC ANOMALIES ARISING
FROM PRISMS OF ARBITRARY CROSS-SECTION AND MAGNETISATION AND INFINITE
IN LENGTHe A VERSION FOR THE ATLAS I IS ALSO IN FORTRANe NeleOe PRO-
GRAM 1025 BY Es PALETHORPE AND Jeo CREASEs REFe NeIleO5w INTERNAL REPORT
NOs NelOs NOV 1968.
NATIONAL INSTITUTE OF OCEANOGRAPHY
WORMLEYs GODALMINGs SURREY
ENGLAND
COMPUTATION AND PLOTTING OF MAGNETIC ANOMALIES LANGUAGE — FORTRAN II
AND GRADIENTS COMPUTER — IBM 7094 W/
CALCOMP
(COPY ON FILE AT NODC)
COMPUTES THE ANOMALY PROFILES FOR TOTAL FIELD» HORIZONTAL AND VERTICAL
COMPONENTS, FIRST AND SECOND VERTICAL DERIVATIVES AND FIRST AND SECOND
HORIZONTAL DERIVATIVES OVER A UNIFORMLY MAGNETIZED TWO-DIMENSIONAL
POLYGON OF IRREGULAR CROSS-SECTIONe OUTPUT MAY BE PRINTED OR PLOTTED.
REF. *POTENTIAL APPLICATIONS OF MAGNETIC GRADIENTS TO MARINE GEOPHYS-—
ICS' BY WILLIAM Ee BYRD» JRe» JUNE 19674 PROGRAM MODIFIED AND EXPAND-
ED FROM TALWANI AND HEIRTZLER (1964).
DEPARTMENT OF GEOLOGY AND GEOPHYSICS
PAGE 026
MASSACHUSETTS INSTITUTE OF TECHNOLOGY
CAMBRIDGE» MASSACHUSETTS 02139
SOLAR RADIATION CONVERSION LANGUAGE — FORTRAN
COMPUTER - IBM 7074
AVERAGES THE RADIATION READINGS FROM THE EPPLEY PYRHELIOMETER AND
BECKMAN-WHITLEY RADIOMETER FOR EVERY 15 MINUTESe CONVERTS FROM My TO
LANGLEYS/MINe AND CALCULATES NET RADIATION FROM BOTH INSTRUMENTSe A
MODIFICATION OF THIS PROGRAM WAS MADE TO INCLUDE A THORNTHWAITE NET
RADIOMETERe ORIGINAL PROGRAM BY SeMe LAZANOFF REWRITTEN BY MARY Eco
MYERSe
COMPUTER DEPARTMENTs CODE 0831
NAVAL OCEANOGRAPHIC OFFICE
SUITLANDs MD. 20390
SEAMOUNT MAGNETIZATION LANGUAGE — FORTRAN
COMPUTER — IBM 7074
COMPUTES THE MAGNITUDE AND DIRECTION OF MAGNETIZATION OF A UNIFORMLY
MAGNETIZED BODY FROM ITS SHAPE AND MAGNETIC INTENSITYe OS NOe 535336
AUTHOR-- Ge VAN VOORHIS.
MAGNETICS DIVISIONs CODE 8200
NAVAL OCEANOGRAPHIC OFFICE
SUITLAND» MDe 20390
VAM INTERPOLATION II LANGUAGE — FORTRAN
COMPUTER - IBM 7074
COMPUTES INCLINATION» MAGNETIC HEADINGs RELATIVE BEARING, AND DECIIN-
ATIONe OUTPUT CONTAINS TRACKs DATEs AIRCRAFT TIMEs POSITION, DECI_IN-
ATIONs DIPs HORIZONTAL INTENSITY (FORCE)»s ALTITUDEs AND GROUND SPEED
FOR EACH FIVE MINUTES OF TIMEe OS NOco 350325 BY We He HANCOCKe
NAVAL OCEANOGRAPHIC OFFICE
SUITLANDs MDe 20390
SEISMIC SLOPING LAYER COMPUTATION LANGUAGE - FORTRAN II
COMPUTER - IBM 709
GIVES TRUE VELOCITIES AND THICKNESSES OF LAYERS FOR SEISMIC REFRACTION
PROFILESe INPUT ARE HORIZONTAL AND AVERAGE VERTICAL WATER VELOCITIES
AND APPARENT ONE-WAY VELOCITIES OF SUBSURFACE INTERFACES DERIVED FROM
TRAVEL-TIME GRAPHS. COMPUTATION FOLLOWS GEOMETRIC METHOD FOR PIANE
SEISMIC WAVES UTILIZING SNELL'S LAWe AUTHOR--— JOHN ANTOINEe
TEXAS A AND M UNIVERSITY
COLLEGE OF GEOSCIENCES
DEPARTMENT OF OCEANOGRAPHY
COLLEGE STATION» TEXAS 77843
TIME TERMs SEISMIC REFRACTION INTERPRETATION LANGUAGE -— FORTRAN IV
COMPUTER -— IBM 7094
(COPY ON FILE AT NODC)
ANALYZES A SET OF DATA THAT APPEARS TO HAVE BEEN GENERATED By A HEAD
WAVE SYSTEM PROPAGATING ALONG A PARTICULAR BOUNDARYe READS THE STAN-
DARD TRAVEL-TIME DATA CARDS (CARNEGIE INST» WASHs DTM)e TIME TERMS ARE
CALCULATED FOR THE BEST LEAST-SQUARE FITTING VELOCITY» IN ADDITION»
CALCULATES THE STANDARD DEVIATION OF THE SOLUTION AS A FUNCTION OF
VELOCITY AND EXAMINES THE MATRIX OF RESIDUALS FOR FREQUENCY AND DEPEN-
DENCE UPON DISTANCEe THESE FEATURES OF THE MATRIX ARE PRESENTED IN
GRAPH FORMe AUTHOR-—- MeJe BERRYe
PAGE 027
UNIVERSITY OF TORONTO
DEPARTMENT OF PHYSICS
GEOPHYSICS LABORATORY
ATTNe DRe Ge Fe WEST
TORONTO 5 ONTARIO
#-#-* SEDIMENT ANALYSIS AND MECHANICS ¥*—-#—*
GEOLOGICAL SAMPLE CONVERSION LANGUAGE — FORTRAN
COMPUTER — IBM 7074
(COPY ON FILE AT NODC) ”
CONVERTS-EDITS TO NODC FORMAT FOR CARDS» DATA ON SAMPLES COLLECTED OR
STUDIED AS PART OF THE JOINT WOODS HOLE Ocle — UeSe GEOLOGICAL SURVEY»
ATLANTIC CONTINENTAL MARGIN PROGRAMe INCLUDES AN INDICATOR OF DEPTH
RANGE VIA TABLE LOOK-UP, AND COMPUTATION OF MARSDEN SQUAREe OS NOe —-
5223le AUTHOR-- Re VAN WIE}
COMPUTER SYSTEMS DIVISION
NATIONAL OCEANOGRAPHIC DATA CENTER
WASHINGTON» De Co 20390
MASS PHYSICAL PROPERTIES LANGUAGE —- FORTRAN
COMPUTER -— IBM 7074
COMPUTES THE RESULTS OF ENGINEERING ANALYSES IN THE GEOLOGICAL LABe
THESE ANALYSES INCLUDE DENSITY» SPECIFIC GRAVITY» VOID RATIOs ATTER-
BURG LIMITS» COHESIONs COMPRESSIVE STRENGTHs CONSOLIDATIONs MOISTURE
CONTENT» ETCe OS NOe 592026
OCEAN SURVEYSs CODE 9200
NAVAL OCEANOGRAPHIC OFFICE
SUITLAND» MDe 20390
SEDIMENT SIZE LANGUAGE — FORTRAN
COMPUTER — IBM 7074
COMPUTES THE FREQUENCY OF THE GRAIN SIZE DISTRIBUTION AND THE STATIS-—
TICAL PARAMETERS» AND RECORDS PERTINENT FIELD DATA AND COMPOSITIONAL
DATA DETERMINED IN THE LABORATORYe THE PROGRAM WILL HANDLE DATA FROM
AN INDEFINITE NUMBER OF CORE SAMPLESe OUTPUT PRINTED IN TABULAR FORMe
REFe INFORMAL MANUSCRIPT IM NOe 66-115 AUGe 19665 "SEDIMENT SIZE COM—
PUTER PROGRAM'» AUTHORS-- DRe JeBe RUCKER AND ReAo STEWART» EXPLORA-
TORY OCEANOGRAPHY DIVe CODE 7220. FURTHER INFORMATION MAY BE OBTAINED
THROUGH DISSEMINATION DEPARTMENT» CODE 449 OR THE AUTHORS»
NAVAL OCEANOGRAPHIC OFFICE
SUITLAND» MD. 20390
GRAIN SIZE LANGUAGE —- FORTRAN II
COMPUTER — GE 225
A COMPUTER PROGRAM FOR GRAIN-SIZE DATAs BY JOHN SHLEE AND JACQUELINE
WEBSTER» 1965» WOODS HOLE OCEANOGRAPHIC INSTITUTION REFe NOe 65-42
(UNPUBLISHED MANUSCRIPT)e THIS PROGRAM AND SEVERAL OTHERS FOR SEDI-
MENT DATA PROCESSING ARE PRODUCTS OF THE UeSe GEOLOGICAL SURVEY'S MA-
RINE GEOLOGY AND HYDROLOGY PROGRAMe
Je WEBSTER
WOODS HOLE OCEANOGRAPHIC INSTITUTION
WOODS HOLE» MASSe
PAGE 028
STANDARD-SIZE ANALYSIS OF SEDIMENTS LANGUAGE — FORTRAN II
COMPUTER -— IBM 1620
COMPUTES THE MEANs STANDARD DEVIATIONs SKEWNESS» AND KURTOSIS BY THE
METHOD OF MOMENTS FOR SIZE DISTRIBUTION OF PARTICLES AS DETERMINED By
STANDARD SEDIMENT ANALYSISs THE FRACTION OF THE TOTAL SAMPLE IN EACH
SIZE CLASSs AND THE FRACTION OF SAND-SIZE MATERIAL COMPOSED OF uP TO
10 DIFFERENT COMPONENTSe AUTHORS-- JoeWe PIERCE» UeSe NATIONAL MUSEUM,
AND Dele GOODs KANSAS GEOLe SURVEYe REFe SPECIAL DISTRIBUTION PUBLI-
CATION 28 (1965)e RUNNING TIME-— LESS THAN 5 HOURS FOR 400 SAMPLESe
DRe DANIEL Fe MERRIAMs EDITOR» COMPUTER CONTRIBUTIONS
KANSAS GEOLOGICAL SURVEY
COMPUTER APPLICATIONS LABORATORY
THE UNIVERSITY OF KANSAS
LAWRENCEs KANSAS 66045
SEDIMENT DATA LANGUAGE — FORTRAN II
COMPUTER — IBM 709 AND
cDC 6400
ALL SEDIMENT DATA COMPUTATIONS, SUCH AS MEANS AND STANDARD DEVIATIONS
OF TEXTUREs TOTAL TEXTURE» CARBONATE AND NON-CARBONATE FRACTIONS» AS
WELL AS ORGANIC NITROGEN AND CARBON DATA HANDLINGe PROGRAM REVISED IN
1964. AUTHOR-- PROF e HeGe GOODELLe
DEPARTMENT OF GEOLOGY
FLORIDA STATE UNIVERSITY
TALLAHASSEEs FLORIDA 32306
ENGINEERING INDEX PROPERTIES OF CORE SAMPLES LANGUAGE — FORTRAN II-D
COMPUTER -— IBM 1620 II
(COPY ON FILE AT NODC)
REDUCES DATA AND TABULATES RESULTS FOR TESTS ON BULK WET DENSITY» VANE
SHEAR STRENGTHS, ORIGINAL WATER CONTENT,» LIQUID LIMIT» PLASTIC LIMIT,
AND SPECIFIC GRAVITY OF SOLIDSe IN ADDITIONs FROM THE ABOVE RESULTS,
OTHER INDEX PROPERTIES ARE SIMULTANEOUSLY COMPUTED AND TABULATEDe THE
OUTPUT TABLE LISTS RESULTS IN COLUMNS REPRESENTING EACH DEPTH SEGMENT
ANALYZEDe PUBLISHED AS AN NCEL TECHNICAL REPORTs REFe NOe R-566 (FEB
1968s 165 P)»s BY MELVIN Ce HIRONAKAo
UeSe NAVAL CIVIL ENGINEERING LABORATORY
PORT HUENEMEs CALIFORNIA 93041
GRAIN SIZE ANALYSIS WITH DIRECT PLOTTING LANGUAGE - FORTRAN II-D
COMPUTER - IBM 1620 II
(COPY ON FILE AT NODC)
INPUT DATA ARE SAMPLE IDENTIFICATIONs SAMPLE WEIGHTS, HYDROMETER READ-
INGSs AND SIEVE READINGSe OUTPUT ON IBM 1627 MODEL I PLOTTER IS A
PARTICLE SIZE DISTRIBUTION CURVEe ANOTHER PROGRAM WRITTEN FOR OUTPUT
ON CARDS OF A TABLE WITH PROPER HEADINGS -AND VALUES FOR PARTICLE DIA-
METERS AND PERCENT FINER BY WEIGHTe REFe NCEL REPORT NOco R-5665 BY
MELVIN Ce HIRONAKAc
UeSe NAVAL CIVIL ENGINEERING LABORATORY
PORT HUENEMEs CALIFORNIA 93041
CARBONATE — ORGANIC CARBON ANALYSIS OF SEDIMENTS LANGUAGE — FORTRAN II-D
COMPUTER — IBM 1620 II
(COPY ON FILE AT NODC)
REDUCES DATA FROM THE CARBON DETERMINATOR AND TABULATES RESULTS OF THE
ANALYSIS OF DEEP OCEAN SEDIMENTS FOR CARBONATE AND ORGANIC CARBON PER-
CENTAGESe OUTPUT IN SAME FORMAT AS IN PROGRAM FOR ENGINEERING INDEX
PROPERTIES» TO WHICH THE OUTPUT FROM THIS PROGRAM IS ADDEDe PROGRAM
LISTINGS AND WRITEUPS INCLUDED IN AN NCEL REPORTs NOe R-566s By MELVIN
HTRONAKAe
PAGE 029
UeSe NAVAL CIVIL ENGINEERING LABORATORY
PORT HUENEME» CALIFORNIA 93041
DIRECT SHEAR TEST WITH DIRECT PLOTTING LANGUAGE — FORTRAN II-D
COMPUTER — IBM 1620 II
(COPY ON FILE AT NODC)
REDUCES DATA AND PLOTS SHEAR STRESS VERSUS SHEAR DISPLACEMENT wITH AP-
PROPRIATE HEADINGS AND LABELS» USING IBM MODEL I PLOTTERe ANOTHER
PROGRAM» tDIRECT SHEAR TEST'» USES THE SAME DATA FORMATS BUT PRESENTS
THE RESULTS IN THE FORM OF TABULATIONS RATHER THAN PLOTSe REFe NCEL
REPORT R-56656 AUTHOR--— MELVIN Ce HIRONAKAc
UeSe NAVAL CIVIL ENGINEERING LABORATORY
PORT HUENEME,» CALIFORNIA 93041
TRIAXIAL COMPRESSION TEST WITH DIRECT PLOTTING LANGUAGE - FORTRAN II-D
COMPUTER — IBM 1620 IT
(COPY ON FILE AT NODC)
REDUCES THE DATA FROM TRIAXIAL COMPRESSION TESTS AND PLOTS STRESS VSe
STRAIN WITH HEADINGS FoR SAMPLE IDENTIFICATION, LATERAL PRESSURE, ETCe
ANOTHER PROGRAM REDUCES THE SAME RAW DATA AND PRESENTS THE RESULTS IN
THE FORM OF TABULATIONS, ONE FOR EACH TESTe LISTINGS AND DESCRIPTIONS
FOR BOTH PROGRAMS INCLUDED IN AN NCEL REPORT,» REFe NOe R-5665 BY MeCe
HIRONAKAe
UeSe NAVAL CIVIL ENGINEERING LABORATORY
PORT HUENEME, CALIFORNIA 93041
CONSOLIDATION TEST (E VSe LOG TIME PLOT) LANGUAGE - FORTRAN II-D
COMPUTER — IBM 1620 II
(COPY ON FILE AT NODC)
REDUCES THE DATA OBTAINED FROM THE CONSOLIDATION TEST READINGSe INPUT
INCLUDES SAMPLE IDENTIFICATION AND CHARACTERISTICS, AND TEST CHARAC-
TERISTICSe THE OUTPUT FROM THIS PROGRAM IS IN TWO FORMS-— PLOTS AND
PUNCHED CARDSe THE LOG OF TIME IS PLOTTED VSe THE VOID RATIOe THE
CARDS ARE USED AS INPUT TO THE NEXT CONSOLIDATION TEST PROGRAM.
UeSe NAVAL CIVIL ENGINEERING LABORATORY
PORT HUENEME» CALIFORNIA 93041
CONSOLIDATION TEST (E VSe LOG P AND C(V) VSe LANGUAGE — FORTRAN II-D
LOG P PLOTS) COMPUTER - IBM 1620 II
(COPY ON FILE AT NODC)
DEVELOPES PLOTS FOR VOID RATIO VSe LOG OF PRESSURE AND COEFFICIENT OF
CONSOLIDATION VSe LOG OF PRESSUREe THE INPUT TO THIS PROGRAM CONSISTS
OF THE OUTPUT CARDS FROM THE PREVIOUS PROGRAM TOGETHER WITH THE VALUES
OF VOID RATIO AND PRESSURE AT 100 0/0 CONSOLIDATION AND THE TIME AND
VOID RATIO AT 50 0/0 CONSOLIDATIONe THESE DATA WERE OBTAINED FROM THE
PLOTS OF VOID RATIO VSe LOG OF TIME IN ACCORDANCE WITH THE TERZAGHI
CONSOLIDATION THEORYe EXAMPLES OF INPUT AND OUTPUT» WITH PROGRAM DE-
SCRIPTIONS AND LISTINGS, INCLUDED IN NCEL REPORT R-566 (FEB 68, 165 P)
BY MELVIN Ce HIRONAKAe
UeSe NAVAL CIVIL ENGINEERING LABORATORY
PORT HUENEME» CALIFORNIA 93041
PERMEABILITY TEST WITH DIRECT PLOTTING LANGUAGE - FORTRAN II-D
COMPUTER - I8M 1620 II
(COPY ON FILE AT NODC)
REDUCES TEST DATA AND PLOTS CURVE OF PERMEABILITY VERSUS TIME WITH AP-
PROPRIATE HEADINGS AND LABELS» USING IBM 1627 MODEL I PLOTTERe THE
PLOTTING SCALE IS A VARIABLE INCORPORATED IN THE PROGRAM, SINCE PERME-
ABILITY VALUES FOR FINE-GRAINED SOILS VARY THROUGHOUT A WIDE RANGEe
REF. NCEL REPORT R-566«e AUTHOR--— MELVIN Ce HIRONAKAe
PAGE 030
UeSe NAVAL CIVIL ENGINEERING LABORATORY
PORT HUENEME» CALIFORNIA 93041
SETTLEMENT ANALYSIS LANGUAGE - FORTRAN II-D
COMPUTER —- IBM 1620 II
(COPY ON FILE AT NODC)
ESTIMATES SETTLEMENT VALUES FROM LABORATORY TEST RESULTS» FOR DEEP
OCEAN FOUNDATION INVESTIGATIONSe INPUT ARE SEDIMENT PROPERTIES AND
STRUCTURE CHARACTERISTICSe OUTPUT IS A TABLE LISTING TOTAL SETTLE-
MENT» FOOTING DIMENSIONS» STRUCTURE LOAD, CHANGE IN THICKNESS OF IN-
CREMENTAL LAYERS AT CORRESPONDING DEPTH IN SEDIMENT» INITIAL STRESS»
AND CHANGE IN STRESSe EQUATIONS, ETCe,s DESCRIBED IN AN NCEL REPORT»
NOe R-566s BY MELVIN Ce HIRONAKAc
UeSe NAVAL CIVIL ENGINEERING LABORATORY
PORT HUENEME» CALIFORNIA 93041
SUMMARY PLOTS LANGUAGE — FORTRAN II-D
COMPUTER - IBM 1620 II
(COPY ON FILE AT NODC)
PLOTS THE RESULTS FROM THE LABORATORY ANALYSIS OF CORE SAMPLESe THE
INPUT DATA ARE THE OUTPUT RESULTS ON CARDS FROM THE PREVIOUS PROGRAMS
AND MISCELLANEOUS ANALYSESe SINCE THE LINK SYSTEM OF PROGRAMMING IS
USED, THE ITEMS TO BE PLOTTED CAN BE INCREASED oR DECREASED wITH
SLIGHT MODIFICATIONSs DEPENDING ON THE USER'S REQUIREMENTSe OUTPUT IS
A SEQUENCE OF PLOTSe THE DEPTH INTO THE SEDIMENT COLUMN IS PLOTTED
WITH REFERENCE TO THE ORDINATEs AND THE VARIOUS PROPERTIES ALONG THE
ABSCISSA ON VARIABLE SCALESe REFe A TECHNICAL REPORT NOe R-566 'COM-
PUTER REDUCTION OF DATA FROM ENGINEERING TESTS ON SOILS AND OCEAN SED-
IMENTS'e AUTHOR-- MELVIN Ce HIRONAKA» NCELe
UeSe NAVAL CIVIL ENGINEERING LABORATORY
PORT HUENEMEs CALIFORNIA 93041
BKGEOL (SEDIMENT ANALYSIS STATISTICS) LANGUAGE - FORTRAN IV
COMPUTER - IBM 7094-II/
7040 DCS
(COPY ON FILE AT NODC)
MODIFICATION OF UeWe ROUTINE 213 FOR THE 709 PREPARED IN FORTRAN II BY
EeEe COLLIAS AND MeRe RONA (REFe TECHe REPORT NOe 875 1963)e ACCEPTS
INPUT DATA IN A MORE ELEMENTARY FORM THAN PREVIOUS PROGRAM AND THE AN-
ALYST MAKES NO CALCULATIONSe INCLUDES PROVISION FOR COMPENSATING FOR
VARIATIONS IN DENSITYs TEMPERATUREs AND ERRORS IN PIPETTING DEPTH AND/
OR TIMEe OUTPUT IS A LIST OF INPUT DATAs LIST OF COMPONENT» RATIOs
TRASKs INMANs AND FOLK AND WARD STATISTICS» SHEPARD DIAGRAM INFORMA-—
TION AND PASSEGA'S C-M VALUESe OPTIONAL PUNCH CARD OUTPUTe PROGRAM
DATE-— MAY 1966. AUTHOR-- WILLIAM ANIKOUCHINEs JORGs ESSAe (A PLOT
ROUTINE WAS PREPARED TO GRAPH PERCENTILE VS PHI-SIZES FROM THE RESULTS
OF THE MAIN PROGRAMe)
We ANIKOUCHINEs RESe ASSOCIATE
JORG-ESSA»s C/O DEPTe OF OCEANOGRAPHY
UNIVERSITY OF WASHINGTON
SEATTLE» WASHe 98105
CONDU LANGUAGE - FORTRAN IV
COMPUTER - IBM 7094-II/
7040 DCS
(COPY ON FILE AT NODC)
CALCULATES THERMAL CONDUCTIVITY OF MARINE SEDIMENTS FROM DATA OBTAINED
WITH A TRANSIENT TYPE NEEDLE PROBE (ALPINE MODEL 328)e TEMPERATURE-
MILLIVOLT CALIBRATION TABLES ARE INPUT AS DATAs WITH LINEAR INTERPOLA-
TION EMPLOYED IN THE TABLE LOOK-UP SUBROUTINE» ADJACENT PAIRS OF TIME
AND TEMPERATURE VALUES ARE USED TO CALCULATE CONDUCTIVITY VALUESe VAL-
UES LYING OUTSIDE OF TWO STANDARD DEVIATIONS ARE REJECTEDe OUTPUT IS
PAGE 031
LISTING AND PLOTSe THE BEST CONDUCTIVITY VALUE IS COMPUTED AND PRINT—
EDe AUTHOR-- WILLIAM ANIKOUCHINE»s JOINT OCEANOGRAPHIC RESEARCH GROUP
(JORG> ESSA)» UNIVe OF WASHINGTONe A COPY OF THIS PROGRAM IS AISO ON
FILE WITH THE PACIFIC OCEANOGRAPHIC LABORATORY, 1801 FAIRVIEW AvEe
EAST» SEATTLE, WASHe,y MRe THEODORE Ve RYAN» DIRECTOR.
RADMe HAROLD Je SEABORG
DIRECTOR» PACIFIC MARINE CENTER
COAST AND GEODETIC SURVEY» USESSA
1801 FAIRVIEW AVENUE, EAST
SEATTLE» WASHe 98102
SEDIMENT GRANULOMETRIC ANALYSIS (UWMS-1003) LANGUAGE —- FORTRAN IV
AND MAP
COMPUTER — IBM 7094-II/
7040 DCS AND
cDC 6400
(COPY ON FILE AT NODC) ;
THE OUTPUT LISTS INPUT DATA, COMPUTED FRACTION PERCENTAGESs ACCUMULAT-—
ED PERCENTAGES» WEIGHT PERCENTAGES OF GRAVEL» SAND» SILTs AND CLAYs
SAND/MUD RATIOs SHEPARD CLASS» TETRAHEDRAL GROUP» PHI-SIZES AT CERTAIN
PERCENTILESs TRASK» INMAN»s FOLK AND WARD VALUES» AND MOMENTS MEASURES
WITH AND WITHOUT SHEPARD!S CORRECTIONSe REFe A REPORT (UWMS-1003,
AUG 1966) BY THE DEPTe OF OCEANOGRAPHYs APPLIED MATHEMATICS SECTIONe
CORE STORAGE NECESSARY-- 5327 WORDSe SOURCE DECK HAS 775 CARDS. RE-
VISED 1969 FOR THE CDC-6400,
He MACINTOSHs COMPUTER SERVICES
DEPARTMENT OF OCEANOGRAPHY
UNIVERSITY OF WASHINGTON
SEATTLE» WASHe 98105
SEDIMENT TEXTURAL ANALYSIS LANGUAGE — FORTRAN
COMPUTER -— (NOT GIVEN)
(COPY ON FILE AT NODC)
A COMPREHENSIVE PROGRAM, DESIGNED FOR SMALL COMPUTERS» FOR THE TEX-
TURAL ANALYSIS OF GROUPED SEDIMENT DATA, INCLUDING SIEVED AND PIPETTED
SAMPLESe THE PROGRAM CONVERTS THE RAW WEIGHTS OF SIZE-GRADED SEDIMENT
INTO WEIGHT PERCENTS» CUMULATIVE PERCENTSs AND A FREQUENCY HISTOGRAM.
COMPUTED STATISTICS INCLUDE-- PERCENTS OF GRAVEL» SAND» SILT» AND CLAY
FoR LITHOFACIES ANALYSIS» AND MEANs STANDARD DEVIATIONs SKEWNESS» AND
KURTOSIS» COMPUTED BY THE METHODS OF MOMENTS» TRASKs INMAN» AND FOLK
AND WARDe REFe A REPORT (UNPUBLISHED) JULY '695 27 Ps BY SAM UPCHURCHe
DIRECTOR
GREAT LAKES RESEARCH CENTER
DEPTe OF THE ARMY» CORPS OF ENGINEERS
LAKE SURVEY DISTRICT
DETROIT» MICHIGAN 48226
PAGE 032
GRAPHICAL DISPLAY
HHH —H-H—-HKH- KKH
GEOLOGICAL SAMPLING INVENTORY PLOT LANGUAGE — FORTRAN
COMPUTER -— IBM 7074 AND
CALCOMP 564
(COPY ON FILE AT NODC)
DISPLAYS GEOLOGICAL SAMPLING INVENTORY DATA AND LOCATION ON CALCOMP
PLOTSs GIVEN THE MARSDEN SQUARE OR ADJACENT RECTANGULAR ARRAY OF
MARSDEN SQUARESe INPUT IS THE NODC GEOSORTED FILE OF GEOLOGICAL
DATAse AUTHOR-— ROBERT VAN WIEe
COMPUTER SYSTEMS DIVISION», CODE 2400
NATIONAL OCEANOGRAPHIC DATA CENTER
WASHINGTONs DeCe 20390
BOTTOM SEDIMENT DISTRIBUTION PLOT LANGUAGE - FORTRAN
COMPUTER —- IBM 7074 W/
CALCOMP 564
(COPY ON FILE AT NODC)
PLOTS BOTTOM SEDIMENT NOTATIONS ON A MERCATOR PROJECTION OF ANY NUMBER
OF DEGREES OF LATITUDE AND LONGITUDE AND TO A SPECIFIED SCALE* CALCOMP
SUBROUTINES ARE USEDs ALSO A COUNT SUBROUTINE DESIGNED BY MRe WALTER
YERGEN OF THIS DIVISIONe REFe IMR NOe O-10-665 MAY 1966 (UNPUBIISHED
MANUSCRIPT)» BY ReJe VAN WYCKHOUSEs WHICH LISTS AN EARLIER PRUGRAM FOR
PRIMARY GRAIN SIZE» AND AN INFORMAL REPORT IR NOe 68-495 JULY 19689 BY
FREDERICK MAASe DDC USERS MAY OBTAIN COPIES OF THE LATTER REPORT DIR-
ECTLY FROM DDC», OR THROUGH THE COMMANDER» NAVAL OCEANOGRAPHIC OFFICE,
ATTNe CODE 40.
OCEANOGRAPHIC ANALYSISs GEOLOGY SECeo
NAVAL OCEANOGRAPHIC OFFICE
SUITLANDs MDe 20390
BIOP (BIOLOGY PLOT) LANGUAGE - FORTRAN IV
COMPUTER - CDC 3600s
CDC 160A
DOES POSITION (LATITUDE, LONGITUDE) PLOTTING OF BIOLOGICAL SPECIES ON
THE CALIFORNIA OFFSHORE IN MERCATOR PROJECTIONe AUTHORS-- MRe MANLEY »
Le We YOUNGe
MARINE LIFE RESEARCH GROUP
SCRIPPS INSTITUTION OF OCEANOGRAPHY
PeOe BOX 109
LA JOLLA» CALIFORNIA 92037
MATHEMATICAL SIMULATION OF MARINE SEDIMENTATION LANGUAGE - FORTRAN IV
COMPUTER — IBM 7040 AND
IBM 7094
BY MATHEMATICAL-MEANSs IN SYMBOLIC THREE-DIMENSIONAL SPACE» THE MODEL
IMITATES THE PROCESSES OF TECTONIC WARPINGs WINNOWING OF SEDIMENTS
ALONG BEACHESs FORMATION OF DELTASs AND THE GROWTH AND INTERACTION OF
ORGANISM COMMUNITIES» INCLUDING ALGAL BANKS AND CORAL REEFSe THE MODEL
IS RUN FORWARDs BY INCREMENTS» THROUGH GEOLOGIC TIMEe OUTPUT IS IN
THE FORM OF LITHOFACIES MAPSs STRUCTURE MAPS», BIOFACIES MAPS» SEA WA-
TER DEPTH MAPS» AND GEOLOGICAL CROSS SECTIONS THAT SHOW BOTH STRUCTURE
AND FACIES RELATIONSHIPSe COMPUTER CONTRIBUTION 95 BY JeWe HARBAUGH
AND WeJe WAHLSTEDT» 1967e
DRe DANIEL Fe MERRIAMs EDITOR
COMPUTER CONTRIBUTIONS
KANSAS GEOLOGICAL SURVEY
PAGE 033
THE UNIVERSITY OF KANSAS
LAWRENCE» KANSAS 66044
VECTOR TREND ANALYSIS OF DIRECTIONAL DATA LANGUAGE - FORTRAN IV
COMPUTER — IBM 7090/94
ANALYZES REGIONAL TRENDS IN DIRECTIONAL DATAe ORTHOGONAL POLYNOMIAL
RESPONSE SURFACES ARE COMPUTED AND PLOTTED AS ISOAZIMUTH AND VECTOR
TREND MAPS TO AID IN INTERPRETING REGIONAL FLOW PATTERNSe EXAMPLES
ARE GIVEN OF THE STUDY OF THE DISTRIBUTION OF CURRENTS WHICH EXISTED
WHEN A SEDIMENT WAS DEPOSITEDe REFe COMPUTER CONTRIBUTION ll» BY
WILLIAM Te FOX (1967)e
DRe DANIEL Fe MERRIAMs EDITOR
COMPUTER CONTRIBUTIONS
KANSAS GEOLOGICAL SURVEY
THE UNIVERSITY OF KANSAS
LAWRENCEs KANSAS 66044
SIMULATION OF DELTAIC SEDIMENTATION LANGUAGE — FORTRAN IV-H
COMPUTER — IBM 360/67,
CALCOMP
A SEDIMENT-LADEN RIVER FLOWING INTO A TIDELESSs CURRENTLESS MARINE BA-
SIN IS MODELED AS A PLANE JET DISCHARGING HORIZONTALLY AT THE OCEAN
SURFACEe A VELOCITY FIELD IS CALCULATED USING EQUATIONS FOR OPEN-
CHANNEL AND PLANE JET FLOWe SEDIMENT BEHAVIOR IS TREATED STATISTICAL—
LYe NOMINAL SEDIMENT PARTICLES ARE TRACED ALONG TRAJECTORIES FROM THE
MOUTH AS THEY SPREAD LATERALLY AND SETTLE VERTICALLYe A DYNAMIC MODEL
PERMITS A DELTA TO BUILD FORWARD DURING SEVERAL TIME INCREMENTS» NOM-
INAL PARTICLE TRAJECTORIES ADJUSTING AUTOMATICALLY TO THE POSITION OF
THE DELTA LIP. AUTHORS-- GeFe BONHAM-CARTER AND AeJe SUTHERLANDe
COMPUTER CONTRIBUTION 24 (APR 1968).
DRe DANIEL Fe MERRIAMs EDITOR
COMPUTER CONTRIBUTIONS
KANSAS GEOLOGICAL SURVEY
THE UNIVERSITY OF KANSAS
LAWRENCEs KANSAS 66044
AUTOMATIC CONTOURING
(ABSTRACT NOT RECEIVED.) COMPUTER CONTRIBUTION 23 "COMPUTER PROGRAMS
FOR AUTOMATIC CONTOURING',s BY DeBe MC INTYRE»s DeDe POLLARD» AND Re
SMITHs (1968).
DRe DANIEL Fe MERRIAMs EDITOR
COMPUTER CONTRIBUTIONS
KANSAS GEOLOGICAL SURVEY
THE UNIVERSITY OF KANSAS
LAWRENCEs KANSAS 66044
GRIDIT» REGRIDIT» AUTOMATED CONTOUR LANGUAGE - FORTRAN
COMPUTER - (NOT GIVEN)
(COPY ON FILE AT NODC)
THREE PROGRAMS WHICH ENABLE THE USER TO GRAPHICALLY PRODUCE A CONTOUR
MAP BY THE COMPUTER-PLOTTER METHOD. THE GRIDIT PROGRAM PRODUCES A
DIGITIZED MATRIX FROM DATA POINTS WHICH HAVE BEEN SCREENED FOR GROSS
ERRORS» REGRIDIT PRODUCES A DIGITIZED MATRIX FROM RAW UNCHECKED DATA
POINTSe AUTOMATED CONTOUR CONSTRUCTS A CONTOUR CHART FROM A DIGITIZED
MATRIXe AN EXAMPLE IS GIVEN FOR USE OF THE PROGRAM IN CONTOURING THE
BATHYMETRY OF OCEAN BOTTOMe REFs IM NOw 67-4 (INFORMAL MANUSCRIPT)
‘AN AUTOMATED PROCEDURE FOR PRODUCING CONTOUR CHARTS', BY ROGER Te
OSBORN» FEBe 1967.
HYDROGRAPHIC DIVes CODE 8100
PAGE 034
NAVAL OCEANOGRAPHIC OFFICE
SUITLAND» MDe 20390
FAA PLOT LANGUAGE - FORTRAN
COMPUTER — I8M 7074
(COPY ON FILE AT NODC)
ACCEPTS THREE CARD IMAGES AND A SUPPLIED SET OF FAA DATA CARDS AS IN-
PUTe THE OUTPUT IS A MAGNETIC TAPE TO DRIVE THE E-51,s E-103»5 OR THE
E-108 CONCORD DIGITAL PLOTTERS USING THE ECHELON MODE.’ THE END PRO-
DUCT IS A FILM POSITIVE WITH A PLUS SYMBOL FOR THE POSITION OF THE FAA
PLOTSe THE MERCATORs TRANSVERSE MERCATORs AND LAMBERT CONIC CONFORMAL
PROJECTION WITH TWO STANDARD PARALLELS ARE THE THREE PROJECTIONS WHICH
CAN BE USED TO PLOT PROGRAM OUTPUTSe OcSe NO 656526 AUTHORS-— RONALD
Me BOLTON AND Je PARRINELLO}’
NAUTICAL CHART DIVISIONs CODE 5620
NAVAL OCEANOGRAPHIC OFFICE
SUITLAND» MDe 20390
SOUNDING PLOT LANGUAGE — FORTRAN
COMPUTER - CDC 3100 AND
IBM 7074
ACCEPTS LORACs LORAN»s OR RAYDIST LANE VALUESe SHIPS TRACK AND SOUND-
INGS ARE PLOTTED ON THE CALCOMP. PRIMARY VERSION IS FOR THE CDC-3100
COMPUTERe AN OBJECT DECK FOR IBM 7074 WILL BE PRODUCEDe PLOTTING IS
DONE IN UTM MODEe OS NOce 58419e¢ AUTHOR-- GeRe BILLSe
GEODESY DIVISIONs CODE 8420
NAVAL OCEANOGRAPHIC OFFICE
SUITLAND» MDe 20390
THREE-DIMENSTONAL SURFACE PLOTS LANGUAGE - FORTRAN
COMPUTER - CDC 3800
SUBROUTINE '"SURFACE* ALLOWS THREE-DIMENSIONAL PLOTS TO BE GENERATED ON
THE 565 CALCOMP PLOTTERe THIS SUBROUTINE WILL PRODUCE A SURFACE PLOT
OF DATA THAT CAN BE REDUCED TO ONE SINGLE-VALUED DEPENDENT AND TWO IN-
DEPENDENT VARIABLESe NRL MEMO’ REPORT 2015¢ AUTHOR-- Je MOORE
JOHN Ce MOORE
RADAR TECHNIQUES
RADAR DIVISION
NAVAL RESEARCH LABORATORY» WASHINGTON» De Ceo 20390
LINE PRINTER PLOTS LANGUAGE — FORTRAN»
COMPASS
COMPUTER - CDC 3800
A SUBROUTINE PACKAGE WRITTEN AT THE UNIVERSITY OF WISCONSIN TO PRODUCE
LINE PRINTER PLOTS HAS BEEN MODIFIED TO RUN ON NRL'S CDC 3800 . NRL
MEMOe REPORT 20466 AUTHOR-- De DENTONe
DIANNA Le DENTON
RESEARCH COMPUTATION CENTER
MATHEMATICS AND INFORMATION SCIENCES DIVISION
NAVAL RESEARCH LABORATORY» WASHINGTON» De Ce 20390
PLOT THETA-S CURVES LANGUAGE — FORTRAN II
COMPUTER - CDC 3100/
PDP-8 AND
CALCOMP
PLOTS POTENTIAL TEMPERATURE VSe SALINITYe CARD INPUT» OUTPUT PRINTED
LISTING AND PUNCHED PAPER TAPEe STATION PLOT USES A PDP-8 COMPUTER»
PAGE 035
PLOT
PAPER TAPE READER» AND CALCOMPe AUTHOR-- Re REINIGERe
DIRECTOR
ATLANTIC OCEANOGRAPHIC LABORATORY
BEDFORD INSTITUTE
DARMOUTHs NOVA SCOTIA» CANADA
STATION POSITIONS LANGUAGE - FORTRAN II
COMPUTER — CDC 3100/
PDP-—8 AND
CALCOMP
PLOTS CRUISE STATION POSITIONS ON MERCATOR'S PROJECTION AND WRITES IN
STATION NUMBERe 'PLOTL* PLOTTING ROUTINE USED WITH PDP-8 COMPUTER AND
THE CALCOMPe AUTHOR-— Re REINIGER (SEPT 1968).
DIRECTOR
ATLANTIC OCEANOGRAPHIC LABORATORY
BEDFORD INSTITUTE
DARTMOUTHs NOVA SCOTIA» CANADA
SECTION PLOTTING LANGUAGE — FORTRAN
COMPUTER - CDC 3100/
PDP-8 AND
CALCOMP
CG
TIME
(C
PLOG
OPY ON FILE AT NODC)
THE PROGRAM USES THE CDC 3100 PLOTTING SUBROUTINES TO GENERATE DATA
FOR THE PDP-8 PLOTTING PROGRAMe THE USER MAY SPECIFY A LEGEND (UP TO
480 CHARACTERS)» LABEL SIZES» SCALE FACTORS» THE PARAMETER TO BE PLOT-
TED AND THE ISOPLETHS TO BE DETERMINEDe THE PLOTTING IS DONE ON A
CALCOMP 31 IN. PLOTTER UNDER CONTROL OF THE PDP-8. CRUISE DATA IS
READ FROM MAGNETIC TAPE BY THE CDC 3100 IN MODIFIED CODC FORMAT OR BI
FORMATe STORAGE REQUIREMENTS—— 11000(8) IN THE CDC 3100 (INCLUDING
PLOTTING SUB-PROGRAMS)e AN ITERATIVE METHOD IS USED IN CONJUNCTION
WITH AN INTERPOLATION FUNCTION TO DETERMINE ISOPLETH DEPTHSe THE IN-
TERPOLATION FUNCTION IS DESCRIBED IN A BEDFORD INSTITUTE REPORT, BIO
66-3 (FEB 1966, UNPUBLISHED MANUSCRIPT) BY ReFe REINIGER AND CeKe ROSS
DIRECTOR
ATLANTIC OCEANOGRAPHIC LABORATORY
BEDFORD INSTITUTE
DARTMOUTHs NOVA SCOTIA» CANADA
SERIES PLOTTING LANGUAGE — FORTRAN 32
COMPUTER — CDC 3100/
PDP-8 AND
CALCOMP
OPY ON FILE AT NODC)
THE PROGRAM USES THE CDC 3100 PLOTTING SUBROUTINES TO GENERATE DATA
FOR THE PDP-8 PLOTTING PROGRAMe THE USER MAY SPECIFY A LEGEND (uP TO
480 CHARACTERS), LABEL SIZES» SCALE FACTORS» THE PARAMETER TO BE PLOT-—
TED AND THE ISOPLETHS TO BE DETERMINEDe THE PLOTTING IS DONE ON A
CALCOMP 31 INe PLOTTER UNDER CONTROL OF THE PDP-8e CRUISE DATA IS
READ FROM MAGNETIC TAPE BY THE CDC 3100 IN BI FORMATe TIME IS PLOTTED
ALONG THE X AXIS (DRUM MOVEMENT) AND DEPTH ALONG THE Z AXIS (PEN MOVE-
MENT)» STATIONS ARE PLOTTED TO THE NEAREST DAYe AUTHOR=— DeJe LAWR-
ENCE (06/06/69).
DIRECTOR
ATLANTIC OCEANOGRAPHIC LABORATORY
BEDFORD INSTITUTE
DARTMOUTHs NOVA SCOTIAs CANADA
LANGUAGE —- FORTRAN IV
COMPUTER ~- IBM 1130/1BM
PAGE 036
1627 PLOTTER
(COPY ON FILE AT NODC)
PLOTS THE RESULTS OF HYDROGRAPHIC CASTS IN A FORMAT SUITABLE FOR PUB-
LICATIONe PRODUCES 8 1/2 BY 10 INe PLOTS OF LOG(10}DEPTH VSe TEMPERA-
TUREs SALINITY» AND OXYGENe
DRe Ce Ae COLLINS
MARINE SCIENCES BRANCH» DEMR
PACIFIC OCEANOGRAPHIC GROUP
BIOLOGICAL STATION
NANAIMO» BeCes CANADA
STPO1 LANGUAGE — FORTRAN IV
COMPUTER — IBM 1130/1BM
1627 PLOTTER
(COPY ON FILE AT NODC)
PLOTS DIGITIZED SeTeDe DATA IN A FORMAT SUITABLE FOR PUBLICATIONe THE
PLOTTER DRAWS AND LABELS AXES AND PLOTS TEMPERATURE AND SALINITY VSe
DEPTHe
DRe Ce Ae COLLINS
MARINE SCIENCES BRANCH» DEMR
PACIFIC OCEANOGRAPHIC GROUP
BIOLOGICAL STATION
NANAIMO» BeCes CANADA
PSAL1 (PLOT TEMPERATURE-SALINITY) LANGUAGE -— FORTRAN VI
COMPUTER -— IBM 1130
(COPY ON FILE AT NODC)
PLOTS T-S AND EXPANDED T-S CURVESe INPUT—- HYDROGRAPHIC DATA IN CODC
FORMATe ANOTHER PROGRAMs PSAL3»s PLOTS OXYGEN-SALINITY AND TEMPERA-
TURE-OXYGEN CURVESe REFe FRB MSe REPORT NOe 1071 (DEC 1969)» BY CeAe
COLLINS» RelLeKe TRIPE AND SeKe WONGe
PACIFIC OCEANOGRAPHIC GROUP
BIOLOGICAL STATION
NANAIMOs BeCes CANADA
GENERAL PURPOSE PLOT AND 'SPECTDPLOT® LANGUAGE — FORTRAN
COMPUTER - IBM 7074 W/
CALCOMP
(COPY ON FILE AT NODC}
TWO PROGRAMS WITH CONSIDERABLE GENERALITY WHICH ALLOW THE USER TO DE-
FINE HIS ORIGIN» SCALE FACTORSs GRID ANNOTATION AND DATA SET» OR ANY
NUMBER OF DATA SETSe AN ADDED PROVISION ALLOWS DATA RECORDED IN THE
FIELD (IeEe ABOARD RESEARCH SHIPS)» TO BE PROCESSED DIRECTLY FROM THE
FIELD TAPES WITH A MINIMUM OF PREPARATORY PROCESSINGe EITHER THE ROT-
ARY-TYPE OR FLAT-BED PLOTTER MAY BE USEDe OS NOSe 20255 AND 202646
INFORMAL REPORT REFe NOe IR 69-65 (AUG 19695 70P)e AUTHOR-- ERNEST Le
MABREYe FURTHER INFORMATION MAY BE OBTAINED FROM THE DISSEMINATION
DEPTe (CODE 44)» OR THE AUTHOR.
SCIENTIFIC APPLICATIONS DIVe.s CODE 0831
COMPUTER DEPARTMENT
NAVAL OCEANOGRAPHIC OFFICE
SUITLAND» MDe 20390
SHIPBOARD SURVEY SYSTEM —- ON-STATION PLOT LANGUAGE - FORTRAN
COMPUTER — IBM 7074
PLOTS SALINITY» SOUND SPEED, TEMPERATURE» AND AMBIENT LIGHT VERSUS
DEPTHe INPUT IS FROM PROGRAM NOe 101322. AUTHOR-- Je WARDENe OS NO,
10131.
COMPUTER DEPARTMENT» CODE 083
NAVAL OCEANOGRAPHIC OFFICE
PAGE 037
SUITLAND» MDe 20390
PROFL LANGUAGE —- FORTRAN IV
COMPUTER -— CDC 3600
PLOTS DATA VALUES AGAINST DEPTH OR OTHER PARAMETERSe
MRe DAVID WIRTH
OCEANIC RESEARCH DIVISION
SCRIPPS INSTITUTION OF OCEANOGRAPHY
PeOw BOX 109
LA JOLLA» CALIFORNIA 92037
OCEANOGRAPHIC STATION CURVE PLOTTING FOR 1401 LANGUAGE -— AUTOCODER
COMPUTER —- IBM 1401
(COPY ON FILE AT NODC)
USES A PLOT AND SYMBOL ROUTINE FOR THE IBM 1401. VARIABLES SCALED IN-
CLUDE DEPTH» TEMPERATURE» SALINITYs SIGMA-Ts DELTA ALPHA s OXYGEN» AND
PHOSPHATE* AUTHOR-— DeLe SHAFFER» INSTITUTE OF MARINE SCIENCE’
UNIVERSITY OF MIAMI
MARINE LABORATORY
COMPUTER CENTER
1 RICKENBACKER CAUSEWAY
VIRGINIA KEYs MIAMI» FLORIDA
THE VORTEX OCEAN MODEL LANGUAGE -— DECAL
COMPUTER - PDP-7(9)
SIMULATES A VORTEX OCEAN MODEL AND DISPLAYS RESULTS ON COMPUTER SCOPE.
COLLECTS STATISTICS ON THE MODELe RESEARCHER CAN CONTROL THE CONF IGU-
RATION OF THE SIMULATION» MAY AT ANY TIME DURING COMPUTATION EXAMINE
OR CHANGE THE VALUE OF ANY VARIABLEe IN THE MODEL» A SET OF VORTICES
INTERACT IN A CIRCULAR OR UNBOUNDED OCEANe NUMBER OF VORTICES CAN BE
VARIED FROM 1 TO 3le ALSO» A SPECIAL TEST POINT USED TO COLLECT STAT-
ISTICS ON THE EFFECTS OF THE VORTICESe EACH VORTEX ROTATES WITH A
STRENGTH, WHERE THE (1)TH VORTEX ROTATES WITH STRENGTH S(I)e THE RO-
TATION OF EACH VORTEX AFFECTS THE POSITION OF ALL OTHERSe OPERATION
IS SUFFICIENTLY FAST TO SHOW SEVERAL VORTICES IN OPERATIONs FLICKER-
FREEe PROGRAM IS CONTROLLED FROM AN ON-LINE TYPEWRITER VIA CONTROL
CHARACTERSe PROGRAM WRITEUP IS AVAILABLE ON REQUEST.
DRe DANIEL Me FORSYTH
INFORMATION INTERNATIONAL» INCe
89 BRIGHTON AVENUE
BOSTONs MASSACHUSETTS 02134
WORLD OCEANOGRAPHIC DATA DISPLAY LANGUAGE — DECAL
COMPUTER — PDP-7(9)
THE WODD SYSTEM ENABLES A RESEARCHER TO CONDUCT AN ANALYSIS OF OCEANO-
GRAPHIC DATA USING A SERIES OF VISUAL DISPLAYS GENERATED BY A DIGITAL
COMPUTERe THE EVENTUAL GOAL OF THE SYSTEM WILL BE TO HOLD AND MAKE A-
VAILABLE FOR DISPLAY THE ENTIRE BODY OF WORLD OCEANOGRAPHIC DATAe THE
RESEARCHER WILL BE ABLE TO SELECT SPECIFIC DATA FOR DISPLAYs IN THE
FORM OF CONTOUR LINES AGAINST A MAP OF SELECTED OCEANIC DATAes HE WILL
BE ABLE TO VARY THE PARAMETERS OF THE DATA SELECTED AND OBSERVE THE
RESULTING VARIATIONS IN THE CONTOUR LINESe AT ITS PRESENT STAGE OF
DEVELOPMENT» THE SYSTEM CONSISTS OF A PDP-7 COMPUTER» A CATHODE RAY
TUBE VISUAL DISPLAY UNIT» A MAGNETIC TAPE UNIT» A LIGHT PEN» INPUT-
OUTPUT TYPEWRITERe BROCHURE DESCRIBING SYSTEM IS AVAILABLE ON REQUEST
DRe DANIEL Me FORSYTH
INFORMATION INTERNATIONAL» INCe
89 BRIGHTON AVENUE
BOSTONs MASSACHUSETTS 02134
PAGE 038
MACHINE PLOTTING ON MERCATOR-PROJECT ION LANGUAGE — FORTRAN
COMPUTER - CDC 1604 W/
CALCOMP 165
(COPY ON FILE AT NODC)
UTILIZES MERIDIONAL PARTS TO LOCATE DATA POINTS ON MERCATOR-PROJECTION
MAPSe FORTRAN PROGRAM USES A SHARED-TIME PLOTTING ROUTINEe THE CON-—
TINENT OUTLINES CAN ALSO BE PLOTTED BY STRAIGHT-LINE SEGMENTSe REF e--
NUWC TP 89 (DEC 19685 44 Pe)e AUTHOR-- LeAw SMOTHERSe PROGRAMMER-—
KeKe STARRe
OCEAN SCIENCES DEPARTMENT
NAVAL UNDERSEA RESEARCH AND DEVELOPMENT CENTER
SAN DIEGO» CALIFORNIA 92132
VACOTS (VERTICALLY ANALYZED CONTOURS OF LANGUAGE — FORTRAN 63
OCEANOGRAPHIC TEMPERATURES AND SALINITIES) COMPUTER -— CDC 3600 W/
CALCOMP
(COPY ON FILE AT NODC)
PROVIDES A RAPID AND ACCURATE MEANS OF CONSTRUCTING VERTICAL CROSS-—
SECTIONS OF SEA TEMPERATURES AND SALINITIESe ALTHOUGH THIS PROGRAM
HAS BEEN DESIGNED TO USE SeTeDe DATA RECORDED ON MAGNETIC TAPE, OTHER
VERSIONS ALSO ARE BEING USED TO CONTOUR BIOLOGICAL» CHEMICAL AND OTHER
PHYSICAL OCEANOGRAPHIC DATA. EACH VERTICAL SECTION IS DIVIDED INTO
TWO PARTS — THE UPPER SECTION FOR THE CONTOURS FROM SURFACE TO 300 Me
AND THE LOWER SECTION FROM 300 Me TO 1000°Me CORE MEMORY SIZE NEEDED
— 32,000 WORDSe RUNNING TIME-- TO ANALYZE AND PLOT CONTOURS AT INTER-
VALS OF 1 DEGREE Ce FOR TEMPERATURE AND el 0/00 FOR SALINITY FROM THE
SURFACE TO 1000 Me FOR 50 STATIONS REQUIRES 4 MINUTES OF COMPUTER TIME
ON THE CDC 3600 AND 25 MINUTES ON THE CALCOMP 30 INe PLOTTERe AUTHOR
— FORREST MILLER.
BUREAU OF COMMERCIAL FISHERIES
PeO5e BOX 271
LA JOLLA» CALIFORNIA 92038
TEMPERATURE-SALINITY PLOT LANGUAGE — FORTRAN
COMPUTER - CDC 3100/
CALCOMP 750
(COPY ON FILE AT NODC)
PROVIDES FOR THE PRODUCTION OF TEMPERATURE-SALINITY DIAGRAMS FROM
SERIAL OCEANOGRAPHIC OBSERVATIONSe INPUT IS DATA CARDS AND A PLOT
CONTROL CARDe OUTPUT IS PLOTTER TAPE AND A PRINTED SUMMARY OF OQUT-OF-
RANGE DATAe REFe MS REPORT NOe 6 (1967)e AUTHOR-- JeRe WILSUNe
OCEANOGRAPHIC RESEARCH DIVISION
MARINE SCIENCES BRANCH
DEPTe OF ENERGY» MINES AND RESOURCES
OTTAWAs CANADA
TEMPERATURE-SALINITY CURVES LANGUAGE — FORTRAN IV
COMPUTER - IBM 360/655
CALCOMP
(COPY ON FILE AT NODC)
PLOTS TEMPERATURE VSe SALINITY CURVES ON 12 INe PLOTTER» EITHER SINGLE
OR MULTIPLE STATIONS. INPUT IS ICES FORMAT HYDROGRAPHIC DATAe CORE
STORAGE USED-- 31K BYTES (INCLUDES PLOT ROUTINES)» AUTHOR-— MARILYNN
BORKOWSKIe
BUREAU OF COMMERCIAL FISHERIES
TROPICAL ATLANTIC BIOLOGICAL LABORATORY
75 VIRGINIA BEACH DRIVE
MIAMI,5 FLORIDA 33149
OXYGEN» PHOSPHATEs DENSITY PLOTS LANGUAGE - FORTRAN IV
COMPUTER — IBM 360/655
CALCOMP
PAGE 039
(COPY ON FILE AT NODC)
PLOTS OXYGEN VSe PHOSPHATE» OXYGEN VSe SIGMA-T» AND PHOSPHATE VSe SIG-
MA-T (SINGLE OR MULTIPLE STATION) FOR PURPOSES OF QUALITY CONTROL AND
STUDY OF WATER TYPESe INPUT IS HYDROGRAPHIC DATA IN ICES FORMATe CORE
STORAGE USED-- 33K BYTES INCLUDING PLOT ROUTINESe AUTHOR-- MARILYNN
BORKOWSKI.
BUREAU OF COMMERCIAL FISHERIES
TROPICAL ATLANTIC BIOLOGICAL LABORATORY
75 VIRGINIA BEACH DRIVE
MIAMI,» FLORIDA 33149
MERCATOR STATION PLOT LANGUAGE — FORTRAN IV
COMPUTER — IBM 360/65,
CALCOMP
WRITES STATION NUMBERS AT THEIR POSITIONS ON A MERCATOR PROYECTION IN
ANY SCALE/DEGREEe INPUT-- STATION HEADER CARDS IN ICES FORMAT.
AUTHOR-— MARILYNN BORKOWSKT.
BUREAU OF COMMERCIAL FISHERIES
TROPICAL ATLANTIC BIOLOGICAL LABORATORY
75 VIRGINIA BEACH DRIVE
MIAMI» FLORIDA 33149
HORIZONTAL SECTIONS LANGUAGE —- FORTRAN IV
COMPUTER — IBM 360/65,
CALCOMP
WRITES IN VALUES OF TEMPERATURE» SALINITY: OXYGEN» PHOSPHATE» ON SEP—
ARATE MERCATOR PROJECTIONS» AT SPECIFIED DEPTHSe INPUT-— HYDROGRAPHIC
DATA IN ICES FORMAT» AT STANDARD DEPTHSe AUTHOR-- MARILYNN BUORKOWSKIe
BUREAU OF COMMERCIAL FISHERIES
TROPICAL ATLANTIC BIOLOGICAL LABORATORY
75 VIRGINIA BEACH DRIVE
MIAMI» FLORIDA 33149
GENERAL MERCATOR PLOT LANGUAGE —- FORTRAN IV
COMPUTER — IBM 360/65,
CALCOMP
PLOTS ANY VARIABLE ON A MERCATOR PROJECTIONe HAS OPTION OF WRITING IN
VALUE OR MAKING A POINT PLOTs AND OF CONNECTING THE POINTS WITH LINESe
INPUT-—- ANY HEADER CARDS IN ICES FORMATe PROJECTION PLOT MAY BE IN
ANY SCALE PER DEGREE» AND MAY INCLUDE A COASTLINE (OBTAINED FROM A
DIGITIZED WORLD TAPE LAYOUT).+ CORE STORAGE NECESSARY-- 42K BYTES (IN-
CLUDES PLOT ROUTINES)»« AUTHOR-- MARILYNN BORKOWSKIe
BUREAU OF COMMERCIAL FISHERIES
TROPICAL ATLANTIC BIOLOGICAL LABORATORY
75 VIRGINIA BEACH DRIVE
MIAMI» FLORIDA 33149
ISOS»s0X0S»sPHOS LANGUAGE — FORTRAN IV
COMPUTER — IBM 360/65
WITH CALCOMP
PLOTS ISENTROPIC SECTIONS FOR SALINITY» OXYGENs OR PHOSPHATE FOR THE
STANDARD STATIONS OF THE TRADE WIND ZONE OCEANOGRAPHY PROGRAMe INPUT
IS THE TRADE WIND ZONE OCEANOGRAPHY PROGRAM ISENTROPIC FORMAT CARDS.
BUREAU OF COMMERCIAL FISHERIES
Pe O. BOX 3830
HONOLULU» HAWAII 96812
PAGE 040
TSIP» THOX s THOT LANGUAGE — FORTRAN IV
COMPUTER - IBM 360/65
WITH CALCOMP
PLOTS TIME HISTORY OF TEMPERATURE» SALINITY» OR OXYGEN FOR STANDARD
STATIONS OF THE TRADE WIND ZONE OCEANOGRAPHY PROGRAM PILOT STUDY. IN-
PUT IS TRADE WIND ZONE OCEANOGRAPHY PROGRAM ISENTROPIC FORMAT CARDS.
BUREAU OF COMMERCIAL FISHERIES
Pe Oc BOX 3830
HONOLULUs HAWAII 96812
BATHYTHERMOGRAM COMPOSITE PLOT LANGUAGE — FORTRAN
COMPUTER — I8M1401/7074
(COPY ON FILE AT NODC)
COMPUTES (1) NUMBER OF OBSERVATIONS AT 50 METER INTERVALS» (2) PERCEN-
TAGE FOR EACH QUALITY CODE, (3) PLOTS PER SEASON AND AREA (AS DETER-
MINED BY A 1401 PROGRAM) USUALLY TO 35 LINES PER PAGE (NEVER EXCEEDING
44)e INPUT--— NODC FORMAT DIGITIZED BT DATAs SORTED BY STATION AND
DEPTHe OUTPUT-— TAPE FOR CALCOMP 670/564 PLOTTERe OS NOeo 52208e AU-
THOR-- RUDI SAENGERe
COMPUTER SYSTEMS DIVISION
NATIONAL OCEANOGRAPHIC DATA CENTER
WASHINGTONs De Co 20390
INVENTORY PLOT LANGUAGE - FORTRAN IV
COMPUTER — IBM 360/405
CALCOMP 763
DISPLAYS AN INVENTORY OF STATION DATA PARAMETERS» BT DATAs GEOLOGICAL
SAMPLES» ETCe (ANY GEOGRAPHICALLY SORTED DATA FILE)» BY 1-DEGREE, 2-
DEGREEs AND 5-DEGREE SQUARESs AND ON ANY OF EIGHT MAP PROJECTIONS OF
SPHEREe OUTPUT-- A TAPE FOR THE CALCOMP 780/763 DRUM PLOTTERe AU-
THOR-— JOHN WARDe WILL USE A STATION DATA PARAMETER INVENTORY PROGRAM
NOW BEING WRITTEN IN ASSEMBLER LANGUAGE BY JEFF GORDON», AND OTHER
PROJECTED PROGRAMS.
COMPUTER SYSTEMS DIVISION
NATIONAL OCEANOGRAPHIC DATA CENTER
WASHINGTON» De Ce 20390
CRUISE TRACK — MERCATOR PROJECTION LANGUAGE — FORTRAN
COMPUTER -— IBM 7074
(COPY ON FILE AT NODC)
INPUT-— NASA DIGITIZED WORLD LAYOUT TAPEs AND NODC FORMAT STATION DATA
(UP TO 600 STATIONS IN A CRUISE).e PROCEDURE-- DETERMINE MAXIMUM AND
MINIMUM LATITUDE» AND ROUND TO NEAREST FIVE DEGREESs THEN DETERMINE
SCALE FACTORs LONGER SIDE EQUAL TO 20 INCHES» OUTPUT-- TAPE FOR CAL-
COMP 670/564 PLOTTERe OS NOe 5221056 AUTHOR-- RUDI SAENGERe NOTE--
THIS WILL SOON BE REPLACED AT NODC BY A NEW MULTI-PROJECTION PROGRAM
FOR CRUISE TRACKS» WRITTEN IN FORTRAN BY JOHN WARD FOR THE IBM 3606
COMPUTER SYSTEMS DIVISION
NATIONAL OCEANOGRAPHIC DATA CENTER
WASHINGTON»s De Ce 20390
VERTICAL SUMMARY HISTOGRAM PLOT LANGUAGE — FORTRAN
COMPUTER -— IBM 7074 AND
CALCOMP 564
(COPY ON FILE AT NODC)
PLOTS PERCENT-FREQUENCY HISTOGRAMS AT EACH OF A MAXIMUM OF 20 STANDARD
DEPTHS» EACH PLOT FOR A GIVEN 1-DEGREE SQUARE AND MONTHe INPUT DATA
ARE PREPARED BY THE STATION DATA VERTICAL ARRAY SUMMARY PROGRAMe NO’
522356 AUTHOR--— ROBERT VAN WIEe
PAGE 041
COMPUTER SYSTEMS DIVISION» CODE 2400
NATIONAL OCEANOGRAPHIC DATA CENTER
WASHINGTONs DeCe 20390
DENSITY-SALINITY MID PLOT LANGUAGE — FORTRAN
COMPUTER — IBM 7074
(cOPY ON FILE AT NODC)
USES SELECTED DENSITY-SALINITY VALUES (OUTPUT FROM PROGRAM NOe 52321)
TO DRAW SINGLE PLOTS AND 6-4-6 COMPOSITE PLOTS IN A GEOGRAPHICALLY
CONTIGUOUS AREAe THE COMPOSITE PLOTS ENABLE ANALYSES OF THESE MID-
POINT VALUES IN RELATION TO THEIR SURROUNDINGSe CORRECTIONS CAN THEN
BE MADE ON THOSE SELECTED DENSITY-SALINITY POINTS TO BETTER REPRESENT
THE MIDPOINT VALUE OF THAT PARTICULAR WATER MASSe OS NOco 523220 AU-
THOR—— ReP. STEIN
DEVELOPMENT DIVISION, CODE 2310
NATIONAL OCEANOGRAPHIC DATA CENTER
WASHINGTONs De Ce 20390
PRESORTED SIGMA-T VERSUS DEPTH AND SALINITY LANGUAGE — FORTRAN
COMPUTER — IBM 7074
(COPY ON FILE AT NODC)
PLOTS SIGMA-T VERSUS DEPTH AND SALINITY» COMPOSITE BY MARSDEN SQUARES
AND AREAS PREPUNCHED IN COL. 3-4e LIMITS-- DEPTH — 0 TO 3000s SIGMA-T
— 22260 TO 29605 SALINITY -— 3265 TO 38¢5¢ INPUT-- NODC FORMAT STATION
DATA ON TAPEs SORTED BY MARSDEN SQUAREs AREAs STATION AND DEPTHe OUT-
PUT-- TAPE FOR CALCOMP 670/564 PLOTTERe OS NOs 522212 AUTHCR-- RUDI
SAENGERe
COMPUTER SYSTEMS DIVISION
NATIONAL OCEANOGRAPHIC DATA CENTER
WASHINGTONs De Ce 20390
STATION DATA PLOT - SIX VARIABLES LANGUAGE — FORTRAN
COMPUTER - IBM 7074
(COPY ON FILE AT NODC)
PLOTS TEMPERATURE VERSUS DEPTHs SALINITY: OXYGEN» PHOSPHATEe*® ALSO
SALINITY AND SIGMA-T VERSUS DEPTHe LIMITS-- DEPTH —- 0 TO 12505 TEMP—
ERATURE — 3¢5 TO 31eO05« INPUT-- NODC FORMAT OBSERVED DATA, SORTED BY
STATION AND DEPTHe OUTPUT--— TAPE FOR CALCOMP 670/564 PLOTTERe OS NOe
52206e AUTHOR-- RUDI SAENGER.
COMPUTER SYSTEMS DIVISION
NATIONAL OCEANOGRAPHIC DATA CENTER
WASHINGTONs De Ce 20390
SOUND VELOCITY DEPTH PROFILES LANGUAGE — FORTRAN
COMPUTER — IBM 7074 W/
CALCOMP 564
(COPY ON FILE AT NODC)
PLOTS CURVES OF DEPTHS VERSUS SOUND VELOCITIES FOR SELECTED MONTHS IN
A 1-DEGe SQUARE AREA FOR WHICH THERE ARE AT LEAST 8 STATIONS EXCEEDING
150 METERS, OR FOR SELECTED SEASONS HAVING 5 OR MORE STATIONS EXCEED-
ING 400 METERSe OS NOe 522284 AUTHOR-- ROBERT VAN WIEe
COMPUTER SYSTEMS DIVISION
NATIONAL OCEANOGRAPHIC DATA CENTER
WASHINGTON, De Ce 20390
VERTICAL SECTION PLOT — STATION DATA LANGUAGE — FORTRAN
COMPUTER — IBM 7074
(COPY ON FILE AT NODC)
(1) EACH VERTICAL SECTION PLOT CONTOURS ONE OF THE FOLLOWING-— TEMPER-.
ATURE» SALINITYs SIGMA-T» GYMNODINIUM BREVEs INORGANIC PHOSPHURUSs TO-
PAGE 042
TAL PHOSPHORUS» NITROGEN» SILICONs OR COPPERe
(2) PLOTS VERTICAL SECTIONS WITH NUMERICAL INSTEAD OF CONTOUR LINES
FOR PARAMETERS INORGANIC PHOSPHORUSs TOTAL PHOSPHORUS» NITROGEN, SILI-
CONs OR COPPERe INPUT-—- OBSERVED NODC FORMAT STATION DATA TAPE ZONE-
EDITED TO 120 CHARACTERS PER RECORD» SORTED BY CRUISE REFERENCE NO6
OUTPUT-- INPUT TAPE TO CALCOMP PLOTTER 670/564. RUNNING TIME-- ABOUT
70 SECTIONS PER HOURe OS NOe 522792 AUTHOR-—- ROBERT VAN WIE» MODIFY-
ING AND CONTINUING OS NOSe 52278 AND 52279 BY DANIEL ROBERTS.
COMPUTER SYSTEMS DIVISION
NATIONAL OCEANOGRAPHIC DATA CENTER
WASHINGTONs De Co 20390
OCEANOGRAPHIC DATA PLOTTING PROGRAM FOR LANGUAGE -— FORTRAN II
NeOeDeCe DATA COMPUTER - I8M 1620 FOR
CALCOMP 560
(COPY ON FILE AT NODC)
THE INPUT DATA CARDS ARE RECEIVED FROM THE NATIONAL OCEANOGRAPHIC DATA
CENTERe THE PROGRAM IS DESIGNED TO PLOT OCEANOGRAPHIC STATION DATA
DOWN TO A DEPTH OF 109000 METERSe THIS IS DONE ON A SERIES OF UP TO
5 GRAPHS, EACH OF WHICH HAS A RANGE OF 23000 METERSe THIS IS A COM-
POSITE GRAPH CONSISTING OF TEMPERATUREs SIGMA-T» SOUND VELOCITY, SAL-
INITYs OXYGEN AND PHOSPHATEe THE SALINITY» PHOSPHATE AND OXYGEN VAL-—
UES ARE PLOTTED VS TEMPERATUREe DENSITYs SOUND VELOCITY AND TEMPERA-
TURE ARE PLOTTED AGAINST DEPTHe ALL TEMPERATURE DEPENDENT VARIABLES
ARE PLOTTED ON THE FIRST GRAPHe THE CONTINUING GRAPHS CONTAIN ONLY
DEPTH DEPENDENT VARIABLESe THE GRAPH IS FULLY IDENTIFIED AS TO REFER-
ENCE NUMBERs STATION LOCATION AND DATEs ETCe EACH CURVE IS IDENTIFIED
BY ITS PLOTTING SYMBOLe AUTHORS-—- DeLe SHAFFER AND DeTe EGERe
UNIVERSITY OF MIAMI
MARINE LABORATORY
COMPUTER CENTER
1 RICKENBACKER CAUSEWAY
VIRGINIA KEY» MIAMI» FLORIDA
OCEANOGRAPHIC DATA PLOTTING PROGRAM, leCeEoSe LANGUAGE — FORTRAN II
COMPUTER -— IBM 1620 FOR
CALCOMP 560
(COPY ON FILE AT NODC)
THE INPUT TO THIS PROGRAM CONSISTS OF THE OUTPUT OF THE IN SITU OCEAN-
OGRAPHIC DATA PROCESSING PROGRAMe HOWEVER» THIS PROGRAM REQUIRES THAT
HEADER CARDS BE INCLUDEDe SINCE THE PROGRAM ESSENTIALLY INTEGRATES
ONE STATION AT A TIME AND THEN PLOTS IT» THE HEADER CARDS SERVE TO IN-
DICATE THE BEGINNING OF A NEW STATIONe AUTHOR-— Dele SHAFFERe
UNIVERSITY OF MIAMI
MARINE LABORATORY
COMPUTER CENTER
1 RICKENBACKER CAUSEWAY
VIRGINIA KEYs MIAMI» FLORIDA
HISTO > LANGUAGE — FORTRAN IV-H
COMPUTER - SDS SIGMA 7
PRODUCES HORIZONTAL BAR HISTOGRAMS OF ANY VARIABLE THAT IS STORED ON
MAGNETIC TAPE IN STANDARD WHOI FORMATe OUTPUT IS A BAR HISTOGRAM
DRAWN BY THE LINE PRINTERe THE WHOI GENERALIZED TAPE FORMAT IS PRE-
SENTED IN A TECHNICAL REPORT 'A NINE CHANNEL DIGITAL MAGNETIC TAPE
FOR STORING OCEANOGRAPHIC DATA'»s REFe NOe 69-555 JULY 19695 BY JOHN Ac
MALTAISe
INFORMATION PROCESSING CENTER
ATTNe JOHN Ae MALTAIS
WOODS HOLE OCEANOGRAPHIC INSTITUTION
WOODS HOLE, MASSACHUSETTS 02543
PAGE 043
LISPLO LANGUAGE — FORTRAN IV-H
COMPUTER -— SDS SIGMA 7
LISTS AND PLOTS THE DATA STORED ON WHOI FORMAT MAGNETIC TAPEs OUTPUT
IS ON THE LINE PRINTERe THREE TYPES OF PLOT ARE POSSIBLE —- A) VARIA-
BLE VS TIME OR SEQUENCE NUMBER» B) ANGLE AND SPEED VS TIMEs C) TWO
VARTABLES (ONE ON A MINUS AND ONE ON A PLUS SCALE) VS TIMEe
INFORMATION PROCESSING CENTER
ATTNe JOHN Aw MALTAIS
WOODS HOLE OCEANOGRAPHIC INSTITUTION
WOODS HOLEs MASSACHUSETTS 62543
TSPLOT LANGUAGE — FORTRAN IV-E
COMPUTER —- IBM 360/50
GENERATES A PUNCHED DECK TO BE USED AS INPUT TO THE BENSON-LEHNER
DELTA INCREMENTAL PLOTTERe FOR EACH HYDROGRAPHIC STATION A SEPARATE
TEMPERATURE VSe SALINITY GRAPH IS DRAWNe SALINITY RANGE IS 320e6 0/00
TO 37e¢8 0/006e ON THE SAME PAGE TWO TEMPERATURE VSe DEPTH GRAPHS ARE
DRAWN» ONE FROM O TO 600 Ms THE OTHER FROM 200 M TO THE BOTTOMe THESE
ARE COMPLETE WITH AXIS» TICK MARKS AND LABELSe SIZE OF GRAPHS IS AN
INPUT VARIABLEe
ROBERT Ke SEXTON
NARRAGANSETT MARINE LABORATORY
UNIVERSITY OF RHODE ISLAND
KINGSTONs RHODE ISLAND 02881
SEQUENTIAL PLOTTING LANGUAGE — FORTRAN
COMPUTER -— (NOT GIVEN)
(COPY ON FILE AT NODC)
SUBROUTINES PRODUCE PLOTS USING A DIGITAL COMPUTER OUTPUT PRINTERe
THE CONSECUTIVE XsY DATA POINTS ARE PLOTTED WITH SYMBOLS CONSISTING OF
LETTERS AND NUMERALSe PERMITS RAPID PLOTTING OF EITHER A SINGLE- OR
MULTIVALUED CURVE WHEN HIGH RESOLUTION IS NOT REQUIREDe REFe NELC RE-
PORT 1613 (MAR 1969» 40 P) BY ReGe ROCKe DIRECT INQUIRIES TO--
NAVAL ELECTRONICS LABORATORY CENTER
SAN DIEGO, CALIFORNIA 92152
DATA FIELD GRID EXPANSION LANGUAGE — MACHINE
COMPUTER - CDC 1604 AND
CDC 3100
EXPANDS A PORTION OF A 63X63 GRID DATA FIELD TO ANY DESIRED SCALE.
THE EXTRACTED PORTION OF THE BASIC FIELD IS OF ARBITRARILY SELECTED
SIZE» SCALE» LOCATIONs ORIENTATION» AND CONTOUR INTERVALe THE METHOD
EMPLOYED IS DOUBLE INTERIOR QUADRATIC INTERPOLATION FROM THE ORIGINAL
GRID POINTS TO THE LOCATION OF THE ARRAY IN THE NEW FIELDe THE TIME
REQUIRED FOR THE EXTRACTION PROCESS IS SIX SECONDS IN THE 1604 AND
LESS THAN TWO SECONDS IN THE 3100 COMPUTERe REFe TECHNICAL MEMO NOs
1, ALSO TECHNICAL NOTE NOe 21 (1966)
COMMANDING OFFICER
FLEET NUMERICAL WEATHER CENTRAL
MONTEREY» CALIFORNIA 93940
PAGE 044
MATHEMATICS» APPLIED
H—-k—H—H—K—K—H#—K—K—H—
*#-#-% CURVE AND SURFACE FITTING *-*-*
LEAST SQUARES CURVE FITTING IN TWO» THREE» AND LANGUAGE — FORTRAN II
FOUR DIMENSIONS COMPUTER -— CDC 3100
(COPY ON FILE AT NODC)
THREE SUBROUTINES» 'UCF's "'BCF's AND 'TCF' (FOR UNIVARIATE® BIVARIATE>
AND TRIVARIATE CURVE-FIT)» FOR USE IN TWO-» THREE-» AND FOUR-SPACEe
CURVE COEFFICIENTS CALCULATED BY REDUCTION TECHNIQUE DUE TO PeDe CROUT
(1941)~2¢ OUTPUT-- PRINTOUT OF COEFFICIENTS» IN NORMALIZED FLOAT ING—
POINTs AND DIFFERENCES CURVE-TO-POINTS» IN SAME FORMATe SATELLITE
SUBROUTINE 'SYMMET*' IS CALLEDs WHICH SOLVES M SIMULTANEOUS ALGEBRAIC
EQUATIONS IN Xe CORE STORAGE NECESSARY-— 2074(8)» 2076(8)»s AND 2256
(8)>5 RESPECTIVELY» + 630(8) FOR SUBROUTINE SYMMETe REFe BeleQe COM-
PUTER NOTE 68-1-Cs JAN 19682¢ AUTHOR-- FeKe KEYTEe
DIRECTOR
ATLANTIC OCEANOGRAPHIC LABORATORY
BEDFORD INSTITUTE
DARTMOUTH» NOVA SCOTIA» CANADA
A GENERALIZED 2-DIMENSIONAL REGRESSION PROCEDURE LANGUAGE - ALGOL AND
FORTRAN IV
COMPUTER -— B5500 AND
IBM 7040
ENABLES SELECTION OF BEST FIT OF A SET OF OBSERVATIONS WITHOUT REGEN-
ERATION OF LOWER ORDER COEFFICIENTSe USES THE MINIMIZATION PROPERTY
OF ORTHOGONAL FUNCTIONSe AUTHOR-- JOHN Re DEMPSEY» NORTHERN NATURAL
GAS COMPANYe PUBLISHED 1966 AS *COMPUTER CONTRIBUTION 2* WITH ALGOL
LANGUAGE LISTINGe A FORTRAN VERSION HAS BEEN RUN ON THE IBM 7040.6
DRe DANIEL Fe MERRIAMs EDITOR» COMPUTER CONTRIBUTIONS
KANSAS GEOLOGICAL SURVEY
THE UNIVERSITY OF KANSAS
LAWRENCE» KANSAS 66044
GENERAL REGRESSION LANGUAGE —- PL/1
COMPUTER -— IBM OS/360
(COPY ON FILE AT NODC)
OBSERVATIONS MAY BE SELECTED BY GROUPS - UP TO 75 GROUPS ARE ALLOWED.
THESE SELECTED OBSERVATIONS ARE TO BE USED TO COMPUTE SIMPLE CORRELA-
TIONS BETWEEN ALL PAIRS OF THE SELECTED VARIABLESe SOME OF THE COR-
RELATION COEFFICIENTS MAY BE FURTHER USED AS NORMAL EQUATION COEFFIC-—
IENTS OR CONSTANTS FOR REGRESSION ANALYSES INVOLVING TWO OR MORE OF
THESE VARIABLESe IF DESIREDs A DIFFERENT SUBSET OF OBSERVATIONS MAY
BE SELECTED TO COMPUTE RESIDUALS», STANDARD ERRORS OF PREDICTED VALUES»
ETCe EITHER CARDS OR TAPE MAY CONTAIN MOST OF THE DATAe IF TAPE IS
TO BE USED FOR THE OBSERVATION MATRIX» IT MUST HAVE BEEN CREATED BY A
DIFFERENT PROGRAM AND BE IN A SPECIAL PL/1 STREAM 1/0 FORMATe
Ue Se GEOLOGICAL SURVEY
COMPUTER CENTER DIVISION
ATTNe RALPH EICHERs CHIEF
BRANCH OF SCIENTIFIC APPLICATIONS
WASHINGTON» De Co 20242
GRAPHIC SYSTEM FOR CURVE FITTING LANGUAGE —- (NOT GIVEN)
COMPUTER -— IBM 360/40
W/ IBM 2250
PAGE 045
PROGRAM SYSTEM CONSISTS OF A SET OF NEARLY INDEPENDENT SECTIONS FUNC-
TIONING ONLY WHEN CALLED BY THE 'tMAIN*t PROGRAMe THE USER ENTERS A
CURVE INTO THE 360/40 VIA A RAND TABLET AND INTERACTIVELY TO SPECIFY
VARIOUS WAYS OF FITTING, EDITING AND DISPLAYING THE CURVE ON AN IBM
2250 SCOPE. THE LAST STEP OUTPUT IS PUNCH CARDS WITH DATA POINTS. OR
COEFFICIENTSe THE SYSTEM FOR IBM 360 ALONG WITH THE PACKAGE OF GRAPH—
ICS USED AT RAND TAKE UP ROUGHLY ONE-HALF OF THE COMPUTER CORE MEMORY.
DOCUMENT BY AeSe PRIVERs SEPT 1969-¢ THE DDC NOw IS AD 693 920.
THE RAND CORPORATION
1700 MAIN ST.
SANTA MONICAy CALIFe 90406
BARTLETT'S CURVE FITTING LANGUAGE — FORTRAN
COMPUTER — IBM 1800 SYS
(COPY ON FILE AT NODC)
BARTLETT'S METHOD FOR COMPUTING THE BEST VALUES FOR FITTING A LINEAR
RELATIONSHIP OR AN EXPONENTIAL RELATIONSHIPe THE 70 0/0 AND 90 0/0
CONFIDENCE LIMITS ON THE SLOPE ARE ALSO’ FOUNDe THE PROGRAM TAKES A
MAXIMUM OF 99 SETS OF DATA EACH WITH A MAXIMUM OF 500 POINTSe NeleOe
PROGRAM 174e AUTHOR--— MAUREEN TYLERe
NATIONAL INSTITUTE OF OCEANOGRAPHY
WORMLEY» GODALMINGs SURREY
ENGLAND
CRVFT LANGUAGE - FORTRAN II
COMPUTER —- GE 225
(COPY ON FILE AT NODC)
ROUTINE TO FIND EITHER BEST LEAST SQUARES FIT TO N POINTS WITHIN SPEC-
IFIED STANDARD DEVIATION 'SIGMA'ts OR FIT A SPECIFIED 'M-CURVE! ORDER
CURVEe FORMER EXECUTED BY M-CURVE NEGATIVEs LATTER BY M-CURVE NON-
NEGATIVEe IN EITHER CASE #SD! IS ACTUAL STANDARD DEVIATION AS CALCUL-
ATEDe AUTHOR-—- FeKe KEYTEe LISTED IN APPENDIX 5 OF BIO COMPUTER NOTE
66-5-Ce A 14-PAGE WRITEUP IS IN THE '#COPE! CATALOG (1965) OF WOODS
HOLE OCEANOGRAPHIC INSTITUTION.
DIRECTOR
ATLANTIC OCEANOGRAPHIC LABORATORY
BEDFORD INSTITUTE
DARTMOUTHs NOVA SCOTIAs CANADA
LEAST SQUARES PLOT LANGUAGE — FORTRAN
COMPUTER -— IBM 7074
FITS AN N-DEGREE POLYNOMIAL (MAXe N=10) OR AN EXPONENTIAL FUNCTION TO
DATA POINTS (MAXe 300)s PLOTTING THE ACTUAL CURVE AND THE COMPUTED
CURVE FOR COMPARISON OR PLOTTING THE DATA POINTS ONLY TO HELP IDENTIFY
THE TYPE OF CURVE THEY REPRESENTe OS NOe 101122 AUTHOR-—- JAMES Se
WARDENe
COMPUTER DEPARTMENTs CODE 083
NAVAL OCEANOGRAPHIC OFFICE
SUITLANDs MD. 20390
CALCULATING AND PLOTTING TIME-TREND CURVES LANGUAGE — FORTRANS FAP
COMPUTER — IBM 7090/94
COMPUTES AND PLOTS A SERIES OF SMOOTHED OR GRADUATED CURVES BASED ON A
SEQUENCE OF GEOLOGIC OBSERVATIONSe NINE SMOOTHING FORMULAE ARE USED
WHICH CORRESPOND TO CYCLES OF INCREASING MAGNITUDE WITHIN THE DATA»
FOR EACH OF TEN VARIABLES WITH UP TO 500 OBSERVATIONS PER VARIABLEe
LEAST SQUARES ANALYSIS IS USED TO FIT A SERIES OF 3RD ORDER POLYNOM-—
TIALS TO THE DATAe STORAGE REQUIREMENTS-- 245757 LOCATIONSe RUNNING
TIME-- ABOUT 2 MINUTES TO COMPUTE ALL NINE CURVES FOR 100 OBSERVATIONS °
PAGE 046
ON A SINGLE VARIABLEe AUTHOR-— WILLIAM Te FOXs WILLIAMS COLLEGE.
(SPECIAL DISTRIBUTION PUBLICATION 12)
DRe DANIEL Fe MERRIAMs EDITOR» COMPUTER CONTRIBUTIONS
KANSAS GEOLOGICAL SURVEY
COMPUTER APPLICATIONS LABORATORY
THE UNIVERSITY OF KANSAS
LAWRENCE» KANSAS 66045
TREND-SURFACE PROGRAM WITH UNRESTRICTED INPUT LANGUAGE — FORTRAN II
AND IV» AND
BALGOL
COMPUTER - IBM 1620
DIFFERS FROM PREVIOUS TREND-SURFACE PROGRAM FOR THE IBM 1620 (SPECIAL
DISTRIBUTION PUBLICATION 145 BY Dele GOOD, 1964) IN ONE MAJOR ASPECT--
DATA ARE NOT STORED IN A DIMENSION ARRAY WITHIN THE COMPUTER» BUT ARE
PROCESSED AND ACCUMULATED AS READ INe THE PROGRAMs THEREFOREs IS THE-
ORETICALLY CAPABLE OF INCORPORATING AN INFINITE NUMBER OF DATA POINTS.
PRODUCES VALUES UP TO THE FOURTH-DEGREE EQUATIONSe STORAGE REQUIRE-
MENTS-— APPROXIMATELY 18K BITSe RUNNING TIME-—- TWO PASSES ARE NECESS-—
ARY» REQUIRING ABOUT 12 MINUTES PER 100 DATA POINTS ON EACH PASSe AU-
THORS-- ROBERT Je SAMPSON AND JOHN Ce DAVIS, IDAHO STATE UNIVe REFe--
SPECIAL DISTRIBUTION PUBLICATION 26 (1966).
DRe DANIEL Fe MERRIAMs EDITOR» COMPUTER CONTRIBUTIONS
KANSAS GEOLOGICAL SURVEY
COMPUTER APPLICATIONS LABORATORY
THE UNIVERSITY OF KANSAS
LAWRENCEs KANSAS 66045
MULTIVARIATE NON-LINEAR REGRESSION LANGUAGE - FORTRAN II
AND IV
COMPUTER - IBM 709 AND
CDC 6400
COMPUTES MULTIVARIATE NON-LINEAR REGRESSION (TREND SURFACE) THROUGH
THE QUINTIC WITH ANALYSIS OF VARIANCE FOR SELECTION OF BEST FITs FOR
N=25006
DEPARTMENT OF GEOLOGY
FLORIDA STATE UNIVERSITY
TALLAHASSEE» FLORIDA 32306
TREND SURFACES FOR DEGREES 1 THROUGH 6 LANGUAGE -— FORTRAN IV
COMPUTER -— IBM 7040
POLYNOMIAL SURFACES ARE FITTED UP TO THE SIXTH DEGREEe THE SURFACES
MAY BE CONTOURED AND THE RESIDUALS PLOTTEDe RANGE IS UP TO 500 DATA
POINTSe APPROXIMATELY 40 MINUTES ARE REQUIRED FOR 200 DATA POINTS FOR
7-1/2 BY 9 TREND-SURFACE MAPS THROUGH SIXTH DEGREEe STORAGE REQUIRE-
MENTS FOR THE 7040-—- 16K AND 4 MAGe TAPESe AUTHORS-— MONT O'LEARY OF
THE UNIVe OF KANSAS» ReHe LIPPERT OF SHELL OIL COes OWEN Te SPITZ OF
KANSAS GEOLe SURVEYe REVISED FROM Dele GOOD'S PROGRAM FOR THE I8M1620
WHICH WAS PUBLISHED IN 1964 AS KANSAS GEOLOGICAL SURVEY SPECIAL DIS-—
TRIBUTION PUBLICATION 14.6
DRe DANIEL Fe MERRIAMs EDITORs COMPUTER CONTRIBUTIONS
KANSAS GEOLOGICAL SURVEY
COMPUTER APPLICATIONS LABORATORY
THE UNIVERSITY OF KANSAS
LAWRENCE» KANSAS 66045
TREND MAP» WITH RESIDUALS AND CONTOURS LANGUAGE — MAD
COMPUTER - IBM 7090
(COPY ON FILE AT NODC)
PAGE 047
USES THE LEAST SQUARES TECHNIQUE TO FIT AN EQUATION TO GEOGRAPHICALLY
DISPERSED DATAe OUTPUT INCLUDES PRINTED MAPSe AUTHOR-- WeRe TOBLER.
THE UNIVERSITY OF MICHIGAN
DEPARTMENT OF GEOGRAPHY
ATTNe DRe We Re TOBLER
ANN ARBOR» MICHIGAN 48104
H-*#—* MATHEMATICAL AND STATISTICAL ANALYSIS *-*-*
SBWRO (SHIPBORNE WAVE RECORDER ANALYSIS) LANGUAGE — FORTRAN Iv
COMPUTER - IBM 1800 SYS
(COPY ON FILE AT NODC)
GIVEN VALUES OF THE HIGHEST AND SECOND HIGHEST CRESTS» THE LOWEST AND
SECOND LOWEST TROUGHS» THE NUMBER OF ZERO CROSSINGS AND THE NUMBER OF
CRESTS IN A SHORT RECORD FROM THE NeIeO5e SHIPBORNE WAVE RECORDER» COM-
PUTES THE SPECTRAL WIDTH PARAMETER AND THE SIGNIFICANT WAVE HEIGHT AND
ALSO THE PREDICTED MAXIMUM HEIGHT IN A PERIOD OF THREE HOURS» AND
STORES THE RESULTS ON LINEPRINTER AND DISKe NeIeO5e PROGRAN NOw 89e
AUTHOR-- EILEEN PAGEe
NATIONAL INSTITUTE OF OCEANOGRAPHY
WORMLEY» GODALMINGs SURREY
ENGLAND
HILOW (GENERATE ARBITRARY FILTER) LANGUAGE - FORTRAN IV
COMPUTER — IBM 1800 SYS
(COPY ON FILE AT NODC)
GENERATES A LOWPASS» BANDPASS» OR HIGHPASS FILTER DEFINED BY 3 PARA-
METERS» WITH OR WITHOUT ITS CONJUGATEs PUNCHES THE MULTIPLIERS ON
CARDS» AND LISTS ITS AMPLITUDE RESPONSE OVER THE FULL FREQUENCY RANGE.
NeIleO5«e PROGRAM NOe 158e AUTHOR-- DeEew CARTWRIGHT.
NATIONAL INSTITUTE OF OCEANOGRAPHY
WORMLEY» GODALMINGs SURREY
ENGLAND
SUBROUTINES DETRNDs AUTCOVs CRSCOVs FOURTR LANGUAGE — FORTRAN IV
COMPUTER -— IBM 360/40
(COPY ON FILE AT NODC)
A SET OF PROGRAMS DEALING WITH SPECTRAe DETRND REMOVES THE MEAN» OR
THE MEAN AND LINEAR TREND (SLOPE) FROM A TIME SERIESe AUTCOV COMPUTES
THE AUTOCOVARIANCE OF THE TIME SERIESe CRSCOV COMPUTES THE AUTO- AND
CROSS-COVARIANCES OF TWO SEQUENCESe FOURTR COMPUTES EITHER THE SINE
OR COSINE FOURIER TRANSFORMe SMOOTHING OF EITHER IS OPTIONALe LISTED
AND DESCRIBED IN THE PUBLICATION 'WATER WAVE TEACHING AIDS'» WHICH
APPEARS AS TECHNICAL NOTE 13 OF THE MeleTe HYDRODYNAMICS LABORATORY e
THESE ROUTINES ARE ADAPTED FROM A PROGRAM WRITTEN AT BELL TELEPHONE
LABS BY MeJeRe HEALY (1962).
PROFe RALPH He CROSS
ROOM 48-209 HYDRODYNAMICS LABORATORY
MASSACHUSETTS INSTITUTE OF TECHNOLOGY
CAMBRIDGE» MASSACHUSETTS 02139
DIGITAL POWER SPECTRUM ANALYSIS LANGUAGE - FORTRAN Iv
COMPUTER — IBM 7090
THE PROGRAM WAS ORIGINALLY INTENDED TO ANALYZE UNDERWATER SOUNDe THE
HYDROPHONE OUTPUT IN ANALOG FORM IS FIRST DIGITIZEDe THE PROGRAM THEN .
COMPUTES THE POWER SPECTRUM ESTIMATE UTILIZING THE FAST FOURIER TRANS-—
FORMes THE POWER IS COMPUTED FOR A LINEAR SET OF FREQUENCIESe THIS
PAGE 048
INFORMATION IS WRITTEN ON AN OUTPUT TAPEe
DRe Je We WRENCH» JRe
HEAD» MATHEMATICAL COMPe DIVISION
NAVAL SHIP RESEARCH AND DEVELOPMENT CENTER
WASHINGTONs DeCe 20007
STATISTICAL AND PEAK-TO-PEAK ANALYSIS LANGUAGE — FORTRAN Iv
AND MAP
COMPUTER -— IBM 7090
USED IN THE ANALYSIS OF SHIP TRIAL DATA TO STUDY THE ELASTIC RESPONSES
OF SURFACE SHIP STRUCTURES TO RANDOM SEA ENVIRONMENTe CALCULATES STA-
TISTICAL AND PEAK TO PEAK PARAMETERS ASSOCIATED WITH DIGITIZED RANDOM
DATAe PROCESSES UP TO 14 CHANNELS OF DATA CONCURRENTLY» AND ALLOWS
SELECTION OF EITHER CALIBRATED OR UNCALIBRATED RESULTSe REFe NSRDC
APPLIED MATHEMATICS LABORATORY TECHNICAL NOTE AML-35-695 MAY 1969,
JB1M PROGRAM FOR STATISTICAL AND PEAK-TO-PEAK ANALYSIS'» BY MICHAEL
CHERNIKe
DRe Je We WRENCHs JRe
HEAD» MATHEMATICAL COMPe DIVISION
NAVAL SHIP RESEARCH AND DEVELOPMENT CENTER
WASHINGTONs DeCe 20007
PARTIAL AND ORDINARY COHERENCE LANGUAGE - FORTRAN IV
AND MAP
COMPUTER -— IBM 7090
PROGRAM PRTCOH CALCULATES THE PARTIAL COHERENCE FOR RANDOM DATA FROM A
LINEAR SYSTEMs AND OCOH CALCULATES THE ORDINARY COHERENCE FROM THE
SAME DATAe THE DATA IS ASSUMED TO BE STATIONARY RANDOM DATA FROM A
MULTIPLE-INPUT S*¥STEM WITH A SINGLE OUTPUTe BOTH PROGRAMS COMPUTE THE
TRANSFER RESPONSE FUNCTION FOR EACH INPUTe REFe APPLIED MATHEMATICS
LABORATORY TECHNICAL NOTE AML-31-695 MAY 19695 *COMPUTER PROGRAMS FOR
PARTIAL AND ORDINARY COHERENCE! BY ANTHONY Ce MELODIAe
DRe Je We WRENCHs JRo
HEADs MATHEMATICAL COMPe DIVISION
NAVAL SHIP RESEARCH AND DEVELOPMENT CENTER
WASHINGTONs DeCe 20007
SAVED (SHOCK AND VIBRATIONAL EXPERIMENTAL DATA LANGUAGE -— FORTRAN IV
REDUCTION) AND MAP
COMPUTER - IBM 7090
REDUCES BLAST TEST DATA FROM ANY ONE OF FOUR TYPES OF TRANSDUCERS-—
VELOCITY METERS» ACCELEROMETERSs PRESSURE GAUGES AND STRAIN GAUGESe
THROUGH PROGRAMMED OPTIONS THE INPUT DATA» AFTER BEING CALIBRATED, MAY
BE SMOOTHEDs FILTERED OR LISTED BEFORE BEING PLOTTED AS A FUNCTION OF
TIMEe FOR VELOCITY DATAs TRANSDUCER CORRECTIONS WERE APPLIED AND DIS-
PLACEMENT IS COMPUTED AND PLOTTEDe FOR ACCELERATION DATAs VELOCITY
AND DISPLACEMENT ARE COMPUTED AND PLOTTED. INPUT DATA IS READ FROM A
DIGITAL MAGNETIC TAPE IN A PREDEFINED FORMATe DESCRIPTION IS IN NSRDC
APPLIED MATHEMATICS LABORATORY TECHNICAL NOTE AML-14-69»5 MARCH 1969¢
ENTITLED "A DIGITAL PROGRAM FOR REDUCING SHOCK AND VIBRATIONAL EXPERI-
MENTAL DATA BY ANTHONY Ve CINCOTTAe
DRe Je We WRENCH» JRe
HEAD» MATHEMATICAL COMPe DIVISION
NAVAL SHIP RESEARCH AND DEVELOPMENT CENTER
WASHINGTONs DeCe 20007
BLACKY (TIME SERIES ANALYSIS) LANGUAGE -— FORTRAN Iv
COMPUTER — IBM 0S/360
(COPY ON FILE AT NODC)
PAGE 049
NePeGeSe LIBRARY PROGRAMe COMPUTES» FOR TWO SIMULTANEOUS TIME SERIES»
CROSS SPECTRAs POWER SPECTRA» PHASE AND COHERENCEe SUBPROGRAMS OBTAIN
THE FILTERED SERIES» REMOVE THE TRENDs AND COMPUTE THE AUTO- AND CROSS
CORRELATIONSe THESIS BY JOHN Ge MCMILLAN (JUNE 1968) USES DIGITAL A-
NALYSIS BY PROGRAM BLACKY IN THE STUDY OF TEMPERATURE FLUCTUATIONS
NEAR THE AIR-SEA INTERFACEs THE WAVE FIELD AT THE SAME POINTs AND THE
DOWNSTREAM WIND VELOCITYe
NAVAL POSTGRADUATE SCHOOL
MONTEREY» CALIFORNIA 93940
SPECTRAL ANALYSIS OF TIME SERIES LANGUAGE — FORTRAN IV
AND AIGOL 60
COMPUTER —- UNIVAC 1108
AND B5500
(COPY ON FILE AT NODC)
FINDS THE SPECTRA» COSPECTRA»s QUADSPECTRA» COHERENCEs AND PHASE OF TWO
TIME SERIES OR A SINGLE SPECTRUM OF ONE SERIESe USES THE FAST FOURIER
TRANSFORM (ALGORITHM OF COOLEY AND TUKEYs 1965)e REFe SPECIAL REPORT
NOe 6» MARCH 1969» BY EVERETT Je FEEe
THE LIBRARIAN
CENTER FOR GREAT LAKES STUDIES
UNIVERSITY OF WISCONSIN-MILWAUKEE
MILWAUKEE» WISCONSIN 53201 USA
WAVEIN AND DIFRAK LANGUAGE - FORTRAN
COMPUTER —- IBM 7094 AND
CDC 6400
A PAIR OF PROGRAMS FOR (1)SPECTRAL ANALYSIS OF WAVE DATAs AND (2) COM-
PUTATION AND PLOT OF THE DIFFRACTION COEFFICIENTSe AUTHOR-- SHOU-SHAN
FAN» CoEeReCos WASHe » DeCe
PROFe ROBERT Le WIEGEL
DEPARTMENT OF CIVIL ENGINEERING
UNIVERSITY OF CALIFORNIA
BERKELEY» CALIFe 94720
POWER SPECTRUM ANALYSIS LANGUAGE — FORTRAN AND
BINARY
COMPUTER — IBM 7090
AND IBM 704
USED IN THE ANALYSIS OF OCEAN WAVE RECORDS» WHICH GIVE THE FLUCTUATION
OF THE HYDROSTATIC PRESSURE AT A POINT UNDER THE SEA AS A FUNCTION OF
TIMEe DIVIDED INTO TWO PROGRAMS—— AML PROBLEM 840-017C COMPUTES ONLY
THE AUTOCORRELATION AND SPECTRAL ESTIMATES FOR EACH SINGLE TIME SER-
IES» AML PROBLEM 840-157B COMPUTES» IN ADDITION, THE TWO CROSS—CORREL-
ATIONSs»s NAMELYs THE IN-PHASE SPECTRUM (CO-SPECTRUM) AND THE OUT-—OF-
PHASE SPECTRUM (QUA-SPECTRUM) FOR THE SIMULTANEOUS TIME RECORDS, ALSO
COMPUTES THE MEASURE OF COHERENCY OF THE SYSTEMe REFe AML REPORT 131
(1963)» *IBM 704 POWER-SPECTRUM ANALYSIS'.e
MRe GENE He GLEISSNER
HEADs APPLIED MATHEMATICS LABORATORY
NAVAL SHIP RESEARCH AND DEVELOPMENT CENTER
WASHINGTONs DeCe 20007
PROJECT COD LIVER LANGUAGE — FORTRAN II
AND MAP
COMPUTER — IBM 7090
DIGITAL POWER SPECTRA ANALYSISe BASIC WORK PERFORMED WITH HYDROPHONES
USED FOR WAVE PHENOMENA STUDYe AN SC-4020 PLOTS DATA FOR DISCRETE AM-—
PLITUDES VSe DISCRETE FREQUENCIESe ALSO USED IS AN ELECTRONIC ENGIN-
PAGE 050
EERING COMPANY DATA FORMAT TRANSLATOR (ANALOG-DIGITAL)e (PROGRAM DOCU-
MENTED BUT CONTROLLED FOR DISTRIBUTION BECAUSE OF CLASSIFIED APPLICA-
TIONS OF THE SPECIALLY DEVELOPED MATHEMATICAL TECHNIQUES USED)
MRe GENE He GLEISSNER
HEADs APPLIED MATHEMATICS LABORATORY
NAVAL SHIP RESEARCH AND DEVELOPMENT CENTER
WASHINGTONs DeCe 20007
POWER SPECTRUM ANALYSIS LANGUAGE —- BASIC
COMPUTER —- PB-250
(COPY ON FILE AT NODC)
COMPUTES POWER SPECTRA» CROSS-SPECTRA»s AND COHERENCIESe THE METHOD OF
TUKEY IS USED TO CALCULATE THE REQUIRED SINGLE AND CROSS SPECTRAe THE
MAXIMUM NUMBER OF LAGS ALLOWED IS 240 FOR SINGLE SPECTRUM AND 128 FOR
CROSS-SPECTRAe MEMORY SIZE-- 696056 AUTHOR-- SeRe CLARKe REFe TECH-
NICAL MEMORANDUM 64-5 (JULY 1964)e ALSO INCLUDED IN THE TECHe MEMO
ARE PRETREATMENT AND CALIBRATION PROGRAMS» REFe ALSO PNL LABe NOTE
61-11 "POWER SPECTRUM ANALYSIS WITH THE LGP-30'.
PACIFIC NAVAL LABORATORY
HeMeCe DOCKYARD
ESQUIMALT» Be Ces CANADA
POWER SPECTRA ESTIMATION LANGUAGE — FORTRAN
COMPUTER — CDC 3200
COMPUTES SPECTRUM AND AUTO-CORRELATION OF ONE TIME SERIES AND/OR THE
SPECTRA» CO-SPECTRUMs QUADRATURE SPECTRUMs AUTO-CORRELATION AND CROSS-
CORRELATION OF TWO SIMULTANEOUS TIME SERIESe PERFORMS FOURIER TRANS-—
FORM ON COVARIANCE FUNCTIONS (TUKEY SPECTRUM ESTIMATION) ALSO PERFORMS
SMOOTHING ON SPECTRA BY METHOD CALLED "HANNING'e NO OFFICIAL DOCU-
MENTATION HAS BEEN PUBLISHED.
NAVAL UNDERWATER WEAPONS RESEARCH
AND ENGINEERING STATION
ATTNe CODE DA3B
NEWPORT» RHODE ISLAND 02840
HARMONIC ANALYSIS LANGUAGE — MAC
COMPUTER - ICT 1301
HARMONIC ANALYSIS USING SHUSTER'S CRITERION FOR THE DETERMINATION OF
SIGNIFICANT AMPLITUDESe AUTHORS-- AeMe SHIPLEY AND De SACKSe
UNIVERSITY OF CAPE TOWN
OCEANOGRAPHY DEPARTMENT
ATTNe MRe AeMe SHIPLEY
PRIVATE BAGs RONDEBOSCHs CePe
REPUBLIC OF SOUTH AFRICA
NUSPEC LANGUAGE — FORTRAN IV-H
COMPUTER - SDS SIGMA 7
A SET OF FOUR PROGRAMS WHICH COMPUTES THE AUTO— AND CROSS-SPECTRAL ES-
TIMATES FOR TIME SERIES» FOR 1 TO 2048 FREQUENCIES.
INFORMATION PROCESSING CENTER
ATTNe ROBERT MILLARD
WOODS HOLE OCEANOGRAPHIC INSTITUTION
WOODS HOLEs MASSACHUSETTS 02543
PAGE 051
BETA-MODEL WITH WHITE FORCING AND VARIABLE BETA LANGUAGE — FORTRAN IV-H
COMPUTER - SDS SIGMA-7
(COPY ON FILE AT NODC)
PROGRAM USED TO ESTIMATE THE SPECTRUM OF CURRENT RECORDS THAT ARE IR-
REGULARLY SAMPLED, AND wITH EXTENSIVE GAPS» BY A NEW FORM OF COMPI_EX
DEMODULATION»s ALLOWING EXAMINATION OF PERIODS UP TO 100 DAYSe SPECIAL
APPLICATION TO THE SEARCH FOR THE EXISTENCE OF EQUIVALENT-—BAROTROPIC
TOPOGRAPHIC (ROSSBY) WAVES ON THE WESTERN SIDE OF THE NORTH ATLANTIC.
THE AUTOSPECTRA LEVEL OFF AT LOWEST FREQUENCIES, NO LONGER INCREASING
AS A POWER LAWe STRONG COHERENCES WERE FOUND AT LOW FREQUENCIES BE-
TWEEN THE U AND V COMPONENTS AND BETWEEN THE LEVELSe REFe A TECHNICAL
REPORT NOe 69-67 (UNPUBLISHED MANUSCRIPT)» AUG 19695 BY RORY THOMPSON.’
DRe Ne Pe FOFONOFFs CHAIRMAN
DEPTe OF PHYSICAL OCEANOGRAPHY
WOODS HOLE OCEANOGRAPHIC INSTITUTION
WOODS HOLE, MASSACHUSETTS 02543
CIRCSTAT LANGUAGE — FORTRAN IV
COMPUTER — CDC 3400
(COPY ON FILE AT NODC)
COMPUTES THE SIGNIFICANT STATISTICS FOR CIRCULAR NORMALLY DISTRIBUTED
DATAs AS WELL AS GIVING CALCULATIONS FOR USE IN TESTING HYPOTHESESe
A CONTROL CARD DETERMINES THE TEST PERFORMEDe IN ALL CASES» THE VEC-
TOR DIRECTION, VECTOR LENGTH», AND VECTOR STRENGTH ARE COMPUTED. TESTS
OF PREFERRED ORIENTATION ARE CONDUCTED BY THE RAYLEIGH R=-TEST OR BY
THE GREENWOOD—DURAND U-TESTe BIMODAL DATA MAY BE TREATED BY PROGRAM
CIRCSTATe REFe TECHNICAL REPORT NOe 39 OFFICE OF NAVAL RESEARCH» FEBe
1967» BY THOMAS Ae JONES.
DEPARTMENT OF GEOLOGY
NORTHWESTERN UNIVERSITY
EVANSTONs ILLINOIS 60201
BOMM (TIME SERIES) LANGUAGE — FORTRAN»
COMPASS
COMPUTER — IBM 0S/3605
CDC 3600
A COLLECTION OF PROGRAMS HAVING TIME SERIES AS OPERANDS PRIMARILY DE-
SIGNED FOR ANALYSIS» CORRELATION AND DECOMPOSITION OF RECORDSe COPIES
AVAILABLE THROUGH 'SHARE' AND 'COOP'e AUTHORS-- SIR EDWARD BULLARD»
MRSe FLORANCE OGALBY DORMER, WALTER MUNK AND GAYLORD MILLERe
MRSe FLORENCE Oe DORMER
INSTITUTE OF GEOPHYSICS AND PLANETARY PHYSICS
SCRIPPS INSTITUTION OF OCEANOGRAPHY
PeO- BOX 109
LA JOLLA» CALIFORNIA 92037
ANALYSIS OF NON-LINEAR RESPONSE SURFACE LANGUAGE — FORTRAN IV
COMPUTER — IBM 1130
(COPY ON FILE AT NODC)
ANALYZES THE DATA FROM RESPONSE SURFACE EXPERIMENTS WHEN TWO OR THREE
FACTORS ARE MEASUREDe OPTIONS ALLOW CALCULATION OF MAXIMUM LIKELIHOOD
ESTIMATES OF POWER TRANSFORMATIONS OF BOTH INDEPENDENT AND DEPENDENT
VARIABLES, AND THE PLOTTING OF THEIR RELATIVE MAXIMUM LIKELIHOOD
GRAPHS» AS A MEASURE OF THE PRECISION OF THE ESTIMATESe THE DATA IS
THEN SUBJECTED TO ANALYSIS OF VARIANCEs USING ORTHOGONAL POLYNOMIALS,
AND PRINCIPAL COMPONENT ANALYSIS», AND SPECIFIED CONTOURS OF THE DEPEN-
DENT VARIABLE ARE PLOTTED, BOTH WITHOUT AND WITH TRANSFORMATIONe REFe
FRB TECHNICAL REPORT NO. 87 (PUBLISHED MANUSCRIPT» AUG 1968) BY Je Ke
LINDSEYe DIRECT INQUIRIES TO--
FISHERIES RESEARCH BOARD OF CANADA
BIOLOGICAL STATION
NANAIMO, Be Ceo
PAGE 052
MULDA LANGUAGE - FORTRAN IV
COMPUTER - IBM 1130
(COPY ON FILE AT NODC)
A COMPLETE MULTIPLE DISCRIMINANT ANALYSIS IS PERFORMED By SIX INTERRE-
LATED PROGRAMS WHICH ARE EXECUTED IN SUCCESSION THROUGH THE LINK FEA-
TURE IN 1130 FORTRANe WILL ACCEPT UP TO 25 VARIATES AND AS MANY AS 10
GROUPSe ANY NUMBER OF ADDITIONAL DATA CARDS CAN BE READ AND PROCESSED
AFTER THE DISCRIMINANT ANALYSIS HAS BEEN COMPLETEDe THE VALUE OF THE
DISCRIMINANT FUNCTION» CLASSIFICATION CHI-SQUARES AND PROBABILITIES OF
GROUP MEMBERSHIP ARE COMPUTED AND PRINTED FOR EACH ADDITIONAL M-VARI-
ATE OBSERVATIONe AUTHORS-- LeVe PIENAAR AND JeAce THOMSON, FRB TECHNI-
CAL REPORT NOo 112» MAR 1969 (UNPUBLISHED MANUSCRIPT)e DIRECT INQUIR-
HES Os
FISHERIES RESEARCH BOARD OF CANADA
BIOLOGICAL STATION
NANAIMOs BeCo ;
SCALING SUBROUTINE LANGUAGE — FORTRAN
COMPUTER -— CDC 3800
SCALES AN ARRAY OF FLOATING POINT NUMBERS» CORRESPONDING TO A SINGLE
COORDINATEs PREPARING THEM FOR INPUT TO THE 565 CALCOMP PLOTTERe NRL
MEMOe REPORT 2047¢ AUTHORS-- Je LANGWORTHY»s Je HOUSTONe
JAMES Be LANGWORTHY
THEORY BRANCH
NUCLEAR PHYSICS DIVISION
NAVAL RESEARCH LABORATORY» WASHINGTON» De Ce 20390
EVALUATE BESSEL FUNCTIONS LANGUAGE — FORTRAN
COMPUTER - CDC 3800
A SET OF SUBROUTINES THAT EVALUATEs IN SINGLE AND DOUBLE PRECISION»
BESSEL FUNCTIONS OF THE FIRST AND SECOND KINDS FOR ORDERS ZERO AND ONE
FOR POSITIVE REAL ARGUMENTS. ALSO TO EVALUATEs IN SINGLE AND DOUBLE
PRECISION» BESSEL FUNCTIONS OF THE FIRST AND SECOND KINDS FOR INTEGER
OR FRACTIONAL ORDERS AND POSITIVE REAL ARGUMENTSe NRL MEMOe REPORTS
1975-19782 AUTHORS-—- Je MASONs Re BAIERe
JANET Pe MASON
RESEARCH COMPUTATION CENTER
MATHEMATICS AND INFORMATION SCIENCES DIVISION
NAVAL RESEARCH LABORATORY» WASHINGTONs De Co 20390
DETERMINANT OF A REAL SYMMETRIC MATRIX LANGUAGE — FORTRAN
COMPUTER - CDC 3800
A SUBROUTINE WRITTEN AT ARGONNE NATIONAL LABORATORY THAT SOLVES» IN-
VERTS»s AND FINDS THE DETERMINANT OF SYMMETRIC REAL MATRICES» HAS BEEN
MODIFIEDe IT REQUIRES THAT ONLY THE UPPER TRIANGULAR PORTION OF THE
MATRIX BE INPUT» THEREBY REDUCING THE MATRIX STORAGE REQUIREMENT TO
N(N+1)/72 LOCATIONSe NRL MEMOe REPORT 20090 AUTHOR-- Jo MASON
JANET Pe MASON
RESEARCH COMPUTATION CENTER
MATHEMATICS AND INFORMATION SCIENCES DIVISION
NAVAL RESEARCH LABORATORY» WASHINGTONs De Ceo 20390
SUBROUTINE TO FIND THE REAL ZEROS OF A LANGUAGE — FORTRAN
SINGLE-VALUED FUNCTION OF ONE REAL VARIABLE COMPUTER - CDC 3800
FINDS THE REAL ZEROS OF A SINGLE-VALUED FUNCTION OF ONE REAL VARIABLE
BY A MODIFIED METHOD OF FALSE POSITIONe FINDS WITHIN A SPECIFIED TOL-
PAGE 053
ERANCE (DELTA) THOSE POINTS X(I) ALONG A GIVEN CLOSED INTERVAL FOR
WHICH THE FUNCTIONAL VALUE FX(I) SATISFIES THE ABSOLUTE VALUE OF FX(T)
LESS THAN DELTA. EACH POINT AND THE CORRESPONDING FUNCTIONAL VALUE
ARE STORED IN A TABLEe NRL MEMO.’ REPORT 1974+¢ AUTHORS-—- Je MASON>
He TOOTHMAN.
JANET P. MASON
RESEARCH COMPUTATION CENTER
MATHEMATICS AND INFORMATION SCIENCES DIVISION
NAVAL RESEARCH LABORATORY» WASHINGTON; De Ce 20390
CROSS-—ASSOCIATION OF NONNUMERIC SEQUENCES LANGUAGE — ALGOL 60 AND
FORTRAN IV
COMPUTER — ELLIOTT 803C
IBM 7040/44
READS A PAIR OF SEQUENCES WHOSE ELEMENTS BELONG TO A NONORDERED SETe
THE DATA ARE READ IN A NUMERIC CODEe THE PROGRAM SLIDES THE SEQUENCES
PAST EACH OTHER ONE OR MORE STEPS AT A TIME AND FOR EACH MATCH POSI-
TION COUNTS THE NUMBER OF COMPARISONS (SIZE OF OVERLAP) e VARIOUS SIG-
NIFICANCE MEASURES AND OVERALL SIMILARITY ESTIMATES ARE MADEe AUTHORS-—
MeJe SACKIN AND PeHeAe SNEATHs UNIVe OF LEICESTER» DeFe MERRIAM, KAN-
SAS GEOLe SURVEYe REFe SPECIAL DISTRIBUTION PUBLICATION 23 (1965).e
DRe DANIEL Fe MERRIAMs EDITOR», COMPUTER CONTRIBUTIONS
KANSAS GEOLOGICAL SURVEY
COMPUTER APPLICATIONS LABORATORY
THE UNIVERSITY OF KANSAS
LAWRENCE» KANSAS 66045
SIMULATION OF TRANSGRESSION AND REGRESSION WITH LANGUAGE - FORTRAN IV
CONTINUOUS-TIME MARKOV MODELS COMPUTER - CDC 6400
REPORT (COMPUTER CONTRIBUTION 26) IS CONCERNED WITH A STOCHASTIC SIMU-
LATION MODEL IN WHICH THE PATTERN OF LITHOLOGIC SUCCESSION IS EXAMINED
IN TERMS OF THE LENGTH OF TIME THAT THE SYSTEM REMAINS IN A GIVEN
STATEs ONCE IT HAS ENTERED THAT STATEe THE MODEL IS ALSO BASED ON
TRANSGRESSIVE-REGRESSIVE MOTION OF A SHORELINE (OR STRANDLINE)», WITH
THE RESULTING LITHOLOGIC UNITS DEVELOPING AS RESPONSES TO THE MOVEMENT
OF SEDIMENTARY MARINE OR NONMARINE ENVIRONMENTS LATERALLY AND THROUGH
TIMEe AUTHOR-- WeCe KRUMBEINe TWO COMPUTER PROGRAMS ARE LISTED IN
THE APPENDIX» ONE FOR TRANSFORMING A TRANSITION PROBABILITY MATRIX TO
ITS CORRESPONDING TRANSITION RATE MATRIX AND VICE VERSA, AND THE OTHER
("BOREHOLE') FOR SIMULATING LATERAL-SHIFT PHENOMENA, SUCH AS TRANS-—
GRESSION AND REGRESSION WITH A CONTINUOUS-TIME DISCRETE-STATE MARKOV
MODELe
DRe DANIEL Fe MERRIAMs EDITOR
COMPUTER CONTRIBUTIONS
KANSAS GEOLOGICAL SURVEY
THE UNIVERSITY OF KANSAS
LAWRENCE» KANSAS 66044
POWER SPECTRUM OF GEOLOGICAL SURFACES LANGUAGE — FORTRAN Iv
COMPUTER -— GE 625 AND
IBM 7040
TWO-DIMENSIONAL POWER SPECTRUM IS USED FOR NUMERICAL DESCRIPTION OF
OBSERVED SURFACESe DATA MUST BE GRIDDED — MAXIMUM IS 100 BY loo
POINTSe RUNNING TIME FOR MAXIMUM ARRAY IS ABOUT 20 MINUTES ON GE 625.
COMPUTER CONTRIBUTION 16% BY JeE5s ESLER AND FeWe PRESTONs 19674
DRe DANIEL Fe MERRIAMs EDITOR
COMPUTER CONTRIBUTIONS
KANSAS GEOLOGICAL SURVEY
THE UNIVERSITY OF KANSAS
LAWRENCE» KANSAS 66044
PAGE 054
TREND ANALYSIS USING DOUBLE FOURTER SERIES LANGUAGE -— FORTRAN IV
COMPUTER — GE 625
HARMONIC ANALYSIS USEFUL FOR DATA SUSPECTED OF CONTAINING OSCILLATORY
PHENOMENAe DESIGNED FOR DATA OBTAINABLE ON A REGULARLY SPACED, RECT-
ANGULAR GRIDe THE PROGRAM COMPUTES COEFFICIENTS OF FOURIER SERIES AND
EVALUATES AND PLOTS THE FUNCTIONe ALSO COMPUTES AND PLOTS RESIDUAL
VALUESe ALLOWS UP TO 71 X 73 GRID POINTS AND UP TO 25TH HARMONIC IN
BOTH DIRECTIONS. COMPUTER CONTRIBUTION 293 BY JOHN We HARBAUGH AND
MICHAEL Je SACKIN (JUNE 1968)e AN EARLIER PROGRAM WAS DEVELOPED FOR
DOUBLE FOURIER SERIES ANALYSIS OF SURFACES WITH IRREGULARLY SPACED
DATAe REFe COMPUTER CONTRIBUTION 53s BY WeRe JAMES (1966).
DRe DANIEL Fe MERRIAMs EDITOR
COMPUTER CONTRIBUTIONS
KANSAS GEOLOGICAL SURVEY
THE UNIVERSITY OF KANSAS
LAWRENCE» KANSAS 66044
FOURIER ANALYSIS — PROGRAM L101 LANGUAGE -— FORTRAN
COMPUTER —- IBM 7090
(COPY ON FILE AT NODC)
OBTAINS AMPLITUDES AND PHASES OF FREQUENCY COMPONENTS IN ANY RECORDe
STANDARD FOURIER ANALYSIS PLUS USE OF TUKEY COSINE WINDOW TO REDUCE
EDGE EFFECTSe CORE STORAGE USED-- 32Ke AUTHOR-- ALSOPe
LAMONT-DOHERTY GEOLOGICAL OBSERVATORY
COLUMBIA UNIVERSITY
PALISADES» NEW YORK 10964
CLUSTER ANALYSIS LANGUAGE - FORTRAN
COMPUTER —- I6M 1800 SYS
(COPY ON FILE AT NODC)
CARRIES OUT A SINGLE LINKAGE CLUSTER ANALYSIS USING DATA IN THE FORM
OF AN UPPER TRIANGULAR SIMILARITY MATRIXe OUTPUT-- A) SIMILARITY LEv-
BEVORMGEUSTERTINGTGEYGUEs) /B) JANELST Oh TE TEINKAGES! THAT OGGURE Ary HAT
SIMILARITY LEVEL» C) AT THE END OF THE CYCLE THE CLUSTER NUMBERS AND A
LIST OF THE ENTITIES MAKING UP EACH CLUSTER IS PRINTEDe RUN TIME--
A MATRIX OF ORDER 60 TOOK APPROXIMATELY 15 MINUTES TO CLUSTERe NeleQe
PROGRAM NO. 1666 AUTHOR-- Me FASHAMe
NATIONAL INSTITUTE OF OCEANOGRAPHY
WORMLEY»s GODALMINGs SURREY
ENGLAND
Q-MODE CLUSTER ANALYSIS LANGUAGE - FORTRAN IV
COMPUTER - IBM 7090/94»5
IBM 360/67
CLASSIFIES OBJECTS INTO GROUPS ON THE BASIS OF A LARGE NUMBER OF NON-
QUANTITATIVE CHARACTERSe HAS BEEN USED FOR GEOLOGICAL SAMPLES, BIO-
LOGICAL TAXONOMYs ETCe RANGE LIMITED TO 130 OBJECTS AND 100 ATTRI-
BUTESe OUTPUT MAY BE USED TO DRAW DENDROGRAMS WITH A CALCOMP PLOTTER.
REFe COMPUTER CONTRIBUTION 17¢ AUTHOR-- GeFe BONHAM-—CARTER» STANFORD
UNIVERSITY.
DRe DANIEL Fe MERRIAMs EDITOR
COMPUTER CONTRIBUTIONS
KANSAS GEOLOGICAL SURVEY
THE UNIVERSITY OF KANSAS
LAWRENCE» KANSAS 66044
MULTIVARIATE DISCRIMINANT ANALYSIS LANGUAGE - FORTRAN II
COMPUTER - IBM 1620
PAGE 05
COMPUTES THE MULTIVARIATE DISCRIMINANT FUNCTION AND MAHALANOBI 5S! GEN-
ERALIZED DISTANCE FOR TWO GROUPS, ANALYZES THE SIGNIFICANCE OF THE
DIFFERENCE BETWEEN THE GROUPS, AND CLASSIFIES INDIVIDUAL SAMPLESe 20
VARIABLES MAY BE CONSIDERED SIMULTANEOUSLY+* THE TWO SAMPLE GROUPS MAY
CONTAIN ANY NUMBER OF SAMPLESe MATRIX INVERSION IS AVOIDED BY USING A
MODIFICATION OF A PROCEDURE SUGGESTED GY RAO IN WHICH SAMPLES ARE OP—
ERATED UPON ONE AT A TIMEe USES POOLED ESTIMATES OF VARIANCE AND CO-
VARIANCE IN A SERIES OF SIMULTANEOUS EQUATIONS, WHICH ARE SOLVED BY
THE GAUSS-JORDAN METHOD OF APPROXIMATIONSe CORE STORAGE USED-—- 20 Ke
AUTHORS—-- JeCe DAVIS AND ReJe SAMPSON» COMPUTER CONTRIBUTION NOs Ge
DRe DANIEL Fe MERRIAMs EDITORs COMPUTER CONTRIBUTIONS
KANSAS GEOLOGICAL SURVEY
THE UNIVERSITY OF KANSAS
LAWRENCE» KANSAS 66044
TWO-DIMENSIONAL AUTOCORRELATION LANGUAGE - FORTRAN
COMPUTER — IBM 7090 AND
IBM 1401
(COPY ON FILE AT NODC)
APPLIES REGRESSION AND CORRELATION ANALYSES TO A SAMPLE OF OCEAN TERR-
AIN.e COMPUTES VARIANCE AND COVARIANCE AS FUNCTION OF POSITION IN DATA
FIELDe REFe ARTHUR De LITTLEs INCe TECHNICAL REPORT NOe 1440464 -—
"STATISTICAL ANALYSES OF QCEAN TERRAIN AND CONTOUR PLOTTING PROCED-—
URESte APPENDICES B AND C OF REPORT DESCRIBE (BUT DO NOT LIST) TWO
ROUTINES USED — 'CORRELATION CONSTANTS?! (IBM 7090 FORTRAN) AND 'tLOCAL
MEANS AND VARIANCES! (IBM 1401 FORTRAN)« THE AeDe NOw IS AD-601-538.
COPIES HAVE BEEN DEPOSITED WITH THE DEFENSE DOCUMENTATION CENTER.
MISS MARIAN Le HOBBS» LIBRARIAN
TRIDENT/ASW LIBRARY
ARTHUR De LITTLEs INCe
35 ACORN PARK
CAMBRIDGE» MASSe 02140
STAT USY IES Wo. Who WIM LANGUAGE — FORTRAN Iv
COMPUTER — CDC 3100
(COPY ON FILE AT NODC)
THREE SEPARATE PROGRAMS FOR THE PROCESSING OF LIMNOLOGICAL DATAe THEY
CALCULATE MEANS», STANDARD DEVIATIONSs STANDARD ERRORS AND OTHER STAT-—
ISTICS OF VARIOUS LIMNOLOGICAL PARAMETERSe STATISTICS I GIVES WEIGHT—
ED CRUISE-MEAN VALUES» CRUISE-MEAN EPILIMNION AND HYPOLIMNION VALUES,
TABULATIONS OF THE RELATION BETWEEN TEMPERATURE AND OTHER PARAMETERS,
AND NEAR-BOTTOM MEANSe STATISTICS II IS ESPECIALLY DESIGNED TO STUDY
REGIONAL ANOMALIES IN THE DISTRIBUTION OF ANY PARAMETERe STATISTICS
III IS A MORE SPECIALIZED PROGRAM ANALYSING THE VARIABILITY IN A SET
OF DATA IN TERMS OF RANDOM AND SYSTEMATIC COMPONENTS INPUT-—- DATA ON
TAPE IN CODC FORMATe PROGRAMS DESCRIBED IN MANUSCRIPT REPORT NOe 13
(1970)>5 BY DRe He Ee SWEERS,.
MARINE SCIENCES BRANCH
DEPARTMENT OF ENERGY, MINES AND RESOURCES
615 BOOTH STREET
OTTAWAs ONTARIOs CANADA
CURRENT LANGUAGE — FORTRAN IV
COMPUTER - OS/360
PROVIDES ELEMENTARY STATISTICS FOR THREE TIME SERIES OF CURRENT TEMP-
ERATURE» SPEED» AND DIRECTIONe MEANS ARE COMPUTED HOURLY» DAILY AND
FOR THE ENTIRE SERIESe A HISTOGRAM IS PROVIDED DAILY AND FOR THE SER-
IES. VARIANCE AND STANDARD DEVIATION ARE COMPUTED FOR THE SERIESe
OPTIONAL GRAPHICAL OUTPUTS HISTOGRAMS ARE PROVIDEDe APPLICATIONS ARE
MADE TO CONTINUOUS BOTTOM CURRENT MEASUREMENTS IN A SUBMARINE CANYON
AND CONCURRENT WIND» WAVE, AND TIDAL DATA» IN THESES BY JeJe DOOLEY»
JUN 19685 AND BY IeJse NJUS»s DEC 19686
PAGE 056
NAVAL POSTGRADUATE SCHOOL
MONTEREYs CALIFORNIA 93940
SINGLE INTEGRATION LANGUAGE — FORTRAN
COMPUTER ~- IBM 7074
EQUALLY SPACED TIME SERIES DATA IS INTEGRATED ONCE USING TICK'S METH-
THE DATA MUST BE SAMPLED AT A RATE OF AT LEAST TWICE THE NYQUIST
ODe
FREQUENCYe OS NOce 53477¢ AUTHOR-- DeBe ROSSe REFe IM NOo 66-36.
EXPLORATORY OCEANOGRAPHY DIVe» CODE 7200
NAVAL OCEANOGRAPHIC OFFICE
SUITLAND» MDe 20390
LANGUAGE -— FORTRAN IV-H
COMPUTER - SDS SIGMA 7
STATS
COMPUTES AND LISTS STATISTICAL QUANTITIES RELATED TO VARIABLES STORED
ON TAPE IN WHOI STANDARD DATA FORMAT.
INFORMATION PROCESSING CENTER
ATTNe JOHN Ace MALTAIS
WOODS HOLE OCEANOGRAPHIC INSTITUTION
WOODS HOLE, MASSACHUSETTS 02543
PAGE 057
NAVIGATION AND CHARTING
H—K—K—HK—-K—¥ —H—H—H—H—H—H
SATELLITE NAVIGATION LANGUAGE — FORTRAN AND
ASSEMBLER
COMPUTER -— IBM 1800 SYS
(COPY ON FILE AT NODC)
A SET OF PROGRAMS FOR VARIOUS ASPECTS OF SATELLITE NAVIGATIONe THE
PROGRAMS FALL NATURALLY INTO TWO SECTIONS» THOSE INVOLVED IN THE ON-
LINE REDUCTION OF DATA FROM THE SATELLITE AND THOSE INVOLVED IN THE
ANALYSIS BOTH ON-LINE AND OFF-LINEe REFe NeIeOe REPORT Ne20»s AUG 28
19696
NATIONAL INSTITUTE OF OCEANOGRAPHY
ATTNe MRe JAMES CREASE
WORMLEY»s GODALMINGs SURREY
ENGLAND
ALERT LANGUAGE — FORTRAN IV
COMPUTER - IBM 1130
(COPY ON FILE AT NODC)
CALCULATES THE RISE AND SET TIMES AND TIME OF CLOSEST APPROACH OF SAT-
ELLITESe OUTPUT FROM PROGRAM IS A LISTING OF ALERT INFORMATION» AND
PUNCH CARDS FOR NEXT PROGRAM 'ASORT'e CORE STORAGE USED-- 5836 WORDS.
DRe Ce Ae COLLINS
MARINE SCIENCES BRANCHs DEMR
PACIFIC OCEANOGRAPHIC GROUP
BIOLOGICAL STATION
NANAIMO»s BeCes CANADA
ASORT LANGUAGE — FORTRAN IV
COMPUTER — IBM 1130
(COPY ON FILE AT NODC)
SORTS THE OUTPUT OF RISE TIMES OF SATELLITES FROM THE PROGRAM *ALERT!
IN CHRONOLOGICAL ORDERe A LISTING IS PRINTED ON THE IBM 1132e CORE
STORAGE REQUIREMENTS-— 129040 WORDSe DESCRIPTIONS OF BOTH PROGRAMS
ARE IN FRB MANUSCRIPT REPORT NOe 1071 (DEC 1969)5 BY CeAew COLLINS» Re
LeKe TRIPEs AND SeKe WONG (UNPUBLISHED MANUSCRIPT) e
DRe Ce Ae COLLINS
MARINE SCIENCES BRANCHs DEMR
PACIFIC OCEANOGRAPHIC GROUP
BIOLOGICAL STATION
NANAIMO s BeCe» CANADA
BECNAV (BEACON NAVIGATION PROGRAM) LANGUAGE — FORTRAN
COMPUTER - CDC 3200
(COPY ON FILE AT NODC)
COMPUTES THE SHIPS POSITION AT EACH FIX FROM TwO OR MORE BEACONS WHOSE
POSITION HAS BEEN ACCURATELY DETERMINEDe A FIX CONSISTS OF THE DELAY
TIMES FROM TWO OR MORE BEACONSe CORE STORAGE NEEDED-— ABOUT 8K WORDS.
AUTHOR-— Se KOCHANSKI» NSSNFe (PROGRAM DOCUMENTATION UNCLASSIFIED BUT
DISTRIBUTION CONTROLLED BY NSSNF)
COMMANDING OFFICER
NAVAL STRATEGIC SYSTEMS NAVIGATION FACILITY
FLUSHING AND WASHINGTON AVENUES
BROOKLYN» NEW YORK 11251
SPANS1A LANGUAGE — FORTRAN
COMPUTER — CDC 3200
(COPY ON FILE AT NODC)
COMPUTES THE RELATIVE POSITION OF A TRIAD OF BEACONS USING THE DELAY
PAGE 058
TI@ES FROM THREE BEACONSe LIMIT, 40 FIXES PER TRACKe CORE STORAGE
NEEDED-- ABOUT 14K WORDSe AUTHOR-— Se KOCHANSKI» NSSNF eo (PROGRAM
DOCUMENTATION UNCLASSIFIED BUT DISTRIBUTION CONTROLLED By NSSNF)
COMMANDING OFFICER
NAVAL STRATEGIC SYSTEMS NAVIGATION FACILITY
FLUSHING AND WASHINGTON AVENUES
BROOKLYN» NEW YORK 11251
SPANS1B LANGUAGE — FORTRAN
COMPUTER -— CDC 3200
(COPY ON FILE AT NODC)
TRANSLATES AND ROTATES A SET OF BEACON COORDINATES FROM LOCAL COORDIN-
ATES TO GEODETIC COORDINATESe INPUT TO PROGRAM-- SHIPS POSITIONS FROM
EXTERNAL FIXES AND CORRESPONDING POSITIONS FROM *#*BECNAV! PROGRAM, AND
BEACON POSITIONS IN LOCAL COORDINATES FROM 'SPANS1A'e AUTHOR-- Se KO-
CHANSKI» NSSNFe (PROGRAM DOCUMENTATION UNCLASSIFIED BUT DISTRIBUTION
CONTROLLED BY NSSNF )
COMMANDING OFFICER
NAVAL STRATEGIC SYSTEMS NAVIGATION FACILITY
FLUSHING AND WASHINGTON AVENUES
BROOKLYNs NEW YORK 11251
GREAT CIRCLE DISTANCE BETWEEN TwO POINTS LANGUAGE -— FORTRAN
COMPUTER — CDC 3800
DETERMINES THE DISTANCE IN NAUTICAL MILES ALONG THE GREAT CIRCLE PATH
BETWEEN TwO POINTS ON THE EARTHs AND THE INITIAL AND FINAL BEARINGS OF
THAT PATHe THE EARTH IS ASSUMED SPHERICAL WITH ONE NAUTICAL MILE PER
MINUTE OF ARCe DOCUMENTATION AVAILABLE-- NRL COMPUTER NOTE 32.6
DAVID CHANG» CODE 8170
ACOUSTICS DIVISION
NAVAL RESEARCH LABORATORY» WASHINGTON» De Ce 20390
GREAT CIRCLE PATHS FROM A POINT LANGUAGE — FORTRAN
COMPUTER - CDC 3800
FROM A GREAT CIRCLE PATH SPECIFIED BY AN INITIAL POINT AND BEARING»
THE PROGRAM GIVES THE LOCATIONS AND BEARINGS OF POINTS AT A GIVEN AR-
RAY OF DISTANCES IN NAUTICAL MILES ALONG THAT PATHe DOCUMENTATION —-
NRL COMPUTER NOTE 336
DAVID CHANGs CODE 8170
ACOUSTICS DIVISION
NAVAL RESEARCH LABORATORY» WASHINGTONs De Ce 20390
ASTRONOMIC POSITIONs AZIMUTH METHOD LANGUAGE -— FORTRAN IV-H
COMPUTER - IBM 360/65
(COPY ON FILE AT NODC)
CALCULATES THE LATITUDE AND LONGITUDE OF AN ASTRONOMIC OBSERVATION
STATIONs GIVEN MEASURED HORIZONTAL ANGLES BETWEEN STARS AND FIXED MARK
ALONG WITH THE OBSERVATION TIMESe A SET OF OBSERVATION EQUATIONS IS
SOLVED BY THE METHOD OF LEAST SQUARES TO OBTAIN CORRECTIONS TO ASSUMED
VALUES OF LATITUDE, LONGITUDE, AND THE AZIMUTH OF THE REFERENCE MARK
AS WELL AS PROBABLE ERRORS FOR THESE THREE QUANTITIESe THE ADJUSTMENT
IS ITERATED FIVE TIMES OR UNTIL THE CORRECTIONS BECOME LESS THAN 00005
SECONDS» EITHER OF WHICH CAUSES A PROGRAM HALT» OUTPUT-- A TABLE OF
INPUT INFORMATION AND A RECORD OF THE PROCESS OF REFINEMENT FOR EACH
SET OF STATION DATA READ INe STORAGE NEEDED-- APPROXe 373500 BYTES
FOR THE PROGRAM PLUS ITS SUBROUTINESe AUTHOR-- SPENCER ROEDDERe A
PREVIOUS VERSION OF THIS PROGRAM WAS WRITTEN IN ALGOL FOR THE BUR-
ROUGHS 2205 IN SINGLE PRECISIONe
UeSe GEOLOGICAL SURVEY
PAGE 059
COMPUTER CENTER DIVISION
ATTNe RALPH EICHERs CHIEF
BRANCH OF SCIENTIFIC APPLICATIONS
WASHINGTONs De Ce 20242
ASTRONOMIC LATITUDE LANGUAGE -— FORTRAN
COMPUTER - (NOT GIVEN)
(COPY ON FILE AT NODC)
DETERMINATION OF FIRST ORDER ASTRONOMIC LATITUDE BY THE STERNECK METH-
ODe ALSO A PROGRAM USING THE METHOD OF *#POLARIS AND SOUTH STAR'e ALSO
SUBROUTINES FOR THE BALDINI, THE GARFINKEL» AND THE UeSe COAST AND GE-
ODETIC SURVEY REFRACTION MODELSe REFe A REPORT *INVESTIGATIONS IN DE-
TERMINING ASTRONOMIC LATITUDES AND THEIR COMPUTER PROGRAMS! IR NOs 68-
21 (189 Pes APR 1968)e¢ AUTHOR-- LARRY BOURQUINs CODE 84305 GEODESY.
FURTHER INFORMATION MAY BE OBTAINED THROUGH DISSEMINATION DEPARTMENT —
CODE 44s OR THE AUTHORe
NAVAL OCEANOGRAPHIC OFFICE
SUITLAND» MDe 20390
DEAD RECKONING NAVIGATION SYSTEM LANGUAGE — FORTRAN
COMPUTER —- IBM 1130
THIS SYSTEM IS USED AS A NAVIGATION AID TO COMPUTE AND PLOT THE CRUISE
TRACK OF THE SHIP AND TO INDICATE THE LOCATIONS AT WHICH DATA WERE
COLLECTED EN ROUTEe’ INPUT TO PROGRAM-—- SHIP'S SPEED AND HEADING» WIND
SPEED AND DIRECTION FROM PAPER TAPE (HEWLETT-PACKARD DATA ACQUISITION
SYSTEM)» AND FIXES ON CARDS. OUTPUT-- PLOT OF CRUISE TRACKe
DOCUMENTATION-— OPERATING INSTRUCTIONS ONLYe
UNIVERSITY OF WASHINGTON
DEPARTMENT OF OCEANOGRAPHY
22A OCEANOGRAPHY TEACHING BLDGe
ATTNe MRSe HELLA MACINTOSH
SEATTLEs WASHe 98105
REDUCTION AND DISPLAY OF DATA ACQUIRED AT SEA LANGUAGE -— FORTRAN II
COMPUTER -— IBM 1130
(COPY ON FILE AT NODC)
A SYSTEM OF PROGRAMS (NAVIGATION, GRAVITYs TOPOGRAPHY» MAGNETICS) FOR
THE REDUCTIONs STORAGE AND DISPLAY OF UNDERWAY DATA ACQUIRED AT SEAe
THE COMPUTER INSTALLATION CONSISTS OF AN IBM 1130 AND INCLUDES RANDOM
ACCESS DISK CARTRIDGES AND AN ON-LINE CALCOMP 30 INe PLOTTERe A !ARGE
NUMBER OF THE PROGRAMS UTILIZE NAVIGATION POINTS TOGETHER WITH RAW
DIGITIZED GEOPHYSICAL DATA PRESENTED AS A TIME SERIES, WHERE THE DIFF-
ERENT DATA MAY BE READ AT UNEQUAL TIME INTERVALSe REFe TECHe REPORT
NOs 1 (AUGUST 19695 348 Pe) BY MANIK TALWANIe
LAMONT-DOHERTY GEOLOGICAL OBSERVATORY
COLUMBIA UNIVERSITY
PALISADES» NEW YORK 10964
SODANO INVERSE LANGUAGE —- FORTRAN
COMPUTER — CDC 3100
(COPY ON FILE AT NODC)
COMPUTES THE NORMAL SECTION LENGTH AND THE FORWARD AND REVERSE AZI-
MUTHS OF THE GEODESIC BETWEEN TWO POINTS FOR WHICH THE GEOGRAPHIC CO-
ORDINATES ARE KNOWNe THIS COMPUTATION IS USEFUL IN DETERMINING AzI-
MUTH AND DISTANCE BETWEEN TRIANGULATION STATIONS FOR WHICH GEOGRAPHIC
POSITIONS HAVE BEEN DETERMINED BUT WHICH ARE NOT CONNECTED BY DIRECT
OBSERVATIONe OS NOe 42366 AUTHOR-—- ANDREW CAMPBELLe MODIFIED By C.
Ee PIERCE, MARCH 1967-6
GEODESY DIVISION» CODE 8420
NAVAL OCEANOGRAPHIC OFFICE
SUITLAND MDe 20390
PAGE 060
SUBROUTINE 'CIRAZD! LANGUAGE — FORTRAN
COMPUTER - IBM 7074
(COPY ON FILE AT NODC)
FINDS THE DISTANCE AND AZIMUTH BETWEEN TWO POINTS ON THE EARTH'S SUR-
FACE WHEN THE EARTH IS ASSUMED TO BE A SPHERE= Re liheR POSE STS USED
FOR THE CENTER POINTs THE ANGLE GIVEN IS WITH RESPECT TO GRID NORTHe
BY USE OF TRIGONOMETRIC IDENTITIES AND ABSOLUTE VALUE FUNCTIONS», THIS
PROGRAM AVOIDS MANY OF THE COMPUTATIONAL PROBLEMS USUALLY FOUND IN
DISTANCE COMPUTATIONSe OceSe NO 5569056 AUTHOR-- BARRY TURETT.
NAUTICAL CHART DIVISION» CODE 5600
NAVAL OCEANOGRAPHIC OFFICE
SUITLAND» MDe 20390
CIRCULAR CHARTING LANGUAGE - FORTRAN
COMPUTER -— IBM 7074
COMPUTES COORDINATES FOR CONCENTRIC CIRCLES AT SPECIFIED INTERVALS
ALONG LATITUDE AND/OR LONGITUDE WITH A FIXED BROADCASTING STATION
POSITION AS COMMON CENTERe COMPUTED DISTANCES ARE GEODESICS BASED
ON ANY SPECIFIED GEOIDe OS NOe 201326 AUTHOR-- CHARLES KIRKLAND.
COMPUTER DEPARTMENTs CODE 0831
NAVAL OCEANOGRAPHIC OFFICE
SUITLANDs MDe 20390
GEODETIC DATUM CONVERSION LANGUAGE - FORTRAN
COMPUTER -— IBM 7074
TRANSFORMS GEODETIC COORDINATES FROM ONE DATUM TO ANOTHER BY UTILIZING
A GIVEN SHIFT (IN TERMS OF RECTANGULAR SPACE COORDINATES) BETWEEN THE
ORIGINS OF TWO DATUMS AND APPLYING THIS SHIFT» TOGETHER WITH DIFFER-
ENCES IN THE SPHEROIDAL PARAMETERS: IN FORMULAS DERIVED FOR THIS PUR-
POSEe OS NOe 55305¢ AUTHOR-- ROBERT Me WILLEMSe
NAVIGATIONAL SCIENCE DIVe» CODE 5300
NAVAL OCEANOGRAPHIC OFFICE
SUITLAND» MDe 20390
GEODETIC DATUM REDUCTION LANGUAGE -— FORTRAN
COMPUTER — IBM 7074
REDUCES GEODETIC POSITIONS FROM ONE GEODETIC DATUM TO ANOTHER BY USE
OF THE VENING MEINESZ EQUATIONSe THE PREFERRED DATUMS INVOLVED ARE
EUROPEAN DATUMs NORTH AMERICAN DATUM AND TOKYO DATUMe OS NOe 55301.
AUTHOR-— DeJe FINDLAYe
NAVIGATIONAL SCIENCE DIVe» CODE 5300
NAVAL OCEANOGRAPHIC OFFICE
SUITLAND» MDe 20390
COMPUTE GEOGRAPHIC POSITIONS LANGUAGE — SPS
COMPUTER -— IBM 1620
(COPY ON FILE AT NODC)
USCGS PROGRAM NOce 15¢ COMPUTES GEOGRAPHIC POSITIONSs GIVEN STARTING
POSITIONs AZIMUTHs AND LENGTH ON ANY ONE OF SIX SPHEROIDSe THREE TYPES
OF COMPUTATIONS CAN BE OBTAINED-- SINGLE POSITIONS» A LOOP, OR A TRA-
VERSEe CONTROL IS BY JOB CARDe LENGTH INPUT MAY BE IN METERS, FEET,
STATUTE OR NAUTICAL MILES» OR ELECTRONIC LANES.
ESSA» COAST AND GEODETIC SURVEY
WASHINGTON SCIENCE CENTER» BLDGe 2
ROCKVILLE» MDe 20852
PAGE 061
LORAN C (VERSION 2) LANGUAGE — SPS
COMPUTER — IBM 1620
(COPY ON FILE AT NODC)
COMPUTES TABLES GIVING THE POINTS OF INTERSECTION OF LORAN C HyPER-
BOLAS WITH MERIDIANS AND/OR PARALLELS OF THE EARTH SPHEROIDe MICRO-
SECOND VALUES ARE COMPUTED AT INTERVALS VARYING FROM 1 1/4 MINe TO 20
MINe FOR ANY OR ALL OF FOUR POSSIBLE PAIRS OF STATIONS.» PROGRAM CAN
ALSO BE USED TO COMPUTE MICROSECOND VALUES AT GRID INTERSECTIONSe STO-
RAGE 100K. PROGRAM CAN BE MODIFIED FOR USE ON IBM1620 OF 60K CAPACITY.
ESSA:s COAST AND GEODETIC SURVEY
WASHINGTON SCIENCE CENTER» BLDGe 2
ROCKVILLE» MDe 20852
GEODETIC POSITION COMPUTATION AND PLOT LANGUAGE — FORTRAN
COMPUTER -— IBM 7074 W/
CALCOMP 564
(COPY ON FILE AT NODC)
COMPUTES GEODETIC POSITIONS AT DESIRED INTERVALS ALONG INCREMENTAL OR
MISCELLANEOUS AZIMUTHSe OPTION TO PLOT OR LISTe PLOT USES THE 'LAMBt
SUBROUTINE WITH TWO STANDARD PARALLELSe OS NOs 55321e AUTHOR-- MERLE
Le NELSONe AN INFORMAL REPORT IR NOe 69-35 LISTS ADDITIONAL COMPUTER
PROGRAMS AND DESCRIBES PROCEDURES FOR PRODUCTION OF SECONDARY PHASE
CORRECTION CHARTS AND TABLESe THESE SUPPLEMENTARY PROGRAMS» WRITTEN
bY MR EDWIN STEPHENSON AND MISS BARBARA GRAY», ARE IN 7074 AUTOCODER OR
FORTRANe INFORMATION MAY BE OBTAINED FROM DISSEMINATION CONTROI DEPT.
CODE 445 OR THE AUTHOR.
NAVAL OCEANOGRAPHIC OFFICE
WASHINGTONs DeCe 20390
LORAN A AND C SKYWAVE LANGUAGE — FORTRAN
COMPUTER — IBM 7074
COMPUTES POINTS FOR LORAN SKYWAVES WHICH ARE PRODUCED WHEN TRANSMITTED
RADIO SIGNALS THAT TRAVEL UPWARD AND OUTWARD ENCOUNTER THE IONOSPHERE.
(TWO DIFFERENT PROGRAM DECKS USED FOR LORAN A AND C SKYWAVES) AUTHOR--
ROBERT VAN WIEe OS NOe 20158.
COMPUTER DEPARTMENT: CODE 083
NAVAL OCEANOGRAPHIC OFFICE
SUITLAND»s MD. 20390
LORAN COORDINATE COMPUTATION LANGUAGE — FORTRAN
COMPUTER — IBM 7074
(COPY ON FILE AT NODC)
COMPUTES CHARTING COORDINATES ALONG LINES OF LATITUDE OR LONGITUDE FOR
LORAN CURVES AT SPECIFIED INTERVALSe INCLUDES SUBROUTINE BSLN, TO
COMPUTE COORDINATES ALONG THE BASELINE AND BASELINE EXTENSIONS» RUN—
NING TIME-- 500-800 POINTS/MINUTE ON THE 7074e REFe IMR NOo N-1-64
(UNPUBLISHED MANUSCRIPT)* OS NOs 20100¢ AUTHOR-- CHARLES KIRKILANDe
COMPUTER DEPARTMENT s CODE 0831
NAVAL OCEANOGRAPHIC OFFICE
SUITLAND» MD. 20390
LORAN TO GEOGRAPHIC, GEOGe TO LORAN CONVERSIONS LANGUAGE — FORTRAN
COMPUTER - IBM 7074
(COPY ON FILE AT NODC)
CONVERTS LORAN TIME OR PHASE DIFFERENCES TO GEOGRAPHIC COORVINATES By
NON-ITERATIVE METHOD (GEODESIC INVERSE DEVELOPED BY EeMe SODANO)e THE
CONVERSIONS ARE FOR LORAN A OR LORAN C OR FOR A MIXTURE OF THE TWOe6
REFe IMR NO« N-3-64 (UNPUBLISHED MANUSCRIPT). AUTHOR-— AeCe CAMPBELL. ,
PAGE 062
GEODESY DIVISION» CODE 8430
NAVAL OCEANOGRAPHIC OFFICE
SUITLAND» MDe 20390
SUBROUTINE SDANO : LANGUAGE — FORTRAN IV
COMPUTER — IBM 1800 SYS
(COPY ON FILE AT NODC)
GIVEN THE GEOGRAPHICAL CO-ORDINATES OF TWO POINTS» SDANO CALCULATES
THE GEODETIC DISTANCE AND AZIMUTHS BETWEEN THEMe BASED ON METHOD OF
EeSe SODANO FOR A NON-ITERATIVE SOLUTION OF THE INVERSE AND DIRECT
GEODETIC PROBLEMSe NeleOQe PROGe NOo —466 AUTHOR-- Me FASHAMe
NATIONAL INSTITUTE OF OCEANOGRAPHY
WORMLEY» GODALMINGs SURREY
ENGLAND
HNV1 (LORAN/DECCA FILE INITIALISATION) LANGUAGE = FORTRAN Iv
COMPUTER - IBM 1800 SYS
(COPY ON FILE AT NODC)
GIVEN INPUT DATA ON A MASTER-SLAVE PAIRs HNV1 CALCULATES CERTAIN GEO-
DETIC VALUES AND STORES THEN ON TAPE FILE FOR LATER USE BY PROGRAM
HNAVe NeIeOo PROGRAM NOe 164¢ AUTHOR-—- Me FASHAMe
NATIONAL INSTITUTE OF OCEANOGRAPHY
WORMLEY» GODALMINGs SURREY
ENGLAND
HNAV (LORAN/DECCA COORDINATES CALCULATION) LANGUAGE - FORTRAN IV
COMPUTER - IBM 1800 SYS
(COPY ON FILE AT NODC)
GIVEN A DECCAs LORAN-A OR LORAN-C FIX» CALCULATES THE LATITUDE AND
LONGITUDE» THE METHOD FOR A HYPERBOLIC SYSTEM WITH SEPARATE MASTER IS
USED FOR ALL CASESe THE CONSTANTS FOR THE HYPERBOLOIDS ARE CALCULATED
IN METRES FOR BOTH LORAN AND DECCA THUS ALLOWING A FIX TO BE CALCULA-
TED IF ONE LORAN READING AND ONE DECCA READING ARE KNOWNe NeleOe PRO-
GRAM NOe 165¢6¢ USES 'SDANO' AND OTHER SUBROUTINESe AUTHOR-- Me FASHAM
NATIONAL INSTITUTE OF OCEANOGRAPHY
WORMLEY»s GODALMINGs SURREY
ENGLAND
SUBROUTINE 'MAP! LANGUAGE — FORTRAN IV
COMPUTER - IBM 360/40,
CALCOMP 763
PROVIDES A WIDE VARIETY OF MAP PROJECTIONS AND GRIDS TO FACILITATE THE
DISPLAY OF GEOGRAPHICAL DATAe THE PROGRAM HAS BEEN WRITTEN IN AS MOD-
ULAR A FORM AS POSSIBLE TO ALLOW FOR EASE OF INSERTION OR DELETION OF
ROUTINESe PRESENTLY UNDER DEVELOPMENT BY JOHN Oc WARDs THIRTEEN MAP
PROJECTIONS ARE NOW AVAILABLEs AND IN THE NEAR FUTURE SIX MORE WILL
BE ADDED.
COMPUTER SYSTEMS DIVISION
NATIONAL OCEANOGRAPHIC DATA CENTER
WASHINGTONs De Ce 20390
INDIVIDUAL POINT GENERATOR FOR MAP PROJECTIONS LANGUAGE — FORTRAN II
COMPUTER -— IBM 7074
(COPY ON FILE AT NODC) . é
CONVERTS GEOGRAPHIC POSITIONS TO DISCRETE POINTS IN RECTANGULAR COOR-
DINATES ON THE FOLLOWING PROJECTIONS-- MERCATOR» TRANSVERSE MERCATOR,
GNOMONICs POLAR STEREOGRAPHICs AZIMUTHAL EQUIDISTANT» LAMBERT CONFORM—
AL (WITH TWO OR ONE STANDARD PARALLELS) s LAMBERT AZIMUTHAL EQUAL AREA
POLARs LAMBERT EQUAL AREA CYLINDRICAL» MILLER» ALBERS EQUAL AREA CON-—
IC» RECTIFIED SKEW ORTHOMORPHICs AND OBLIQUE MERCATORe CARTOGRAPHIC
PAGE 063
DATA MAY BE PRODUCED IN EITHER GRAPHIC OR TABULAR FORMe OS NOew 55646
(MAIN PROGRAM. EACH OF THE 13 PROJECTION SUBROUTINES HAS ITS OWN OPEN
SHOP NUMBER)e AUTHORS-- RONALD BOLTONs LOUIS ROWENs GREGORY VEGA.
REFe INFORMAL REPORT IR NOe 69-23» MAR 1969 !'COMPUTER PROGRAMS AND
SUBROUTINES FOR AUTOMATED CARTOGRAPHY'» BY Je PARRINELLOs NAUTICAL
CHART DIVISIONe FURTHER INFORMATION MAY BE OBTAINED THROUGH DISSEMIN-
ATION DEPARTMENT CODE 445 OR THE AUTHORS.
NAVAL OCEANOGRAPHIC OFFICE
WASHINGTONs DeCe 20390
INDIVIDUAL POINT GENERATOR FOR LANGUAGE — FORTRAN II
DISTANCE AND AZIMUTH COMPUTATIONS COMPUTER — IBM 7074
USES THE GEODETIC LATITUDE AND LONGITUDE OF TWO POINTS TO COMPUTE THE
DISTANCE AND AZIMUTH FROM ONE POINT TO THE OTHERe RESULTS WILL BE IN
TABULAR FORM WITH THE DISTANCE IN METERS AND THE AZIMUTH AND BACK AZI-
MUTH IN DEGREES» MINUTES AND SECONDSe OcSe NOs 656163 BY ReMe BOLTON.
NAUTICAL CHART DIVISION: CODE 5620
UeSe NAVAL OCEANOGRAPHIC OFFICE
WASHINGTON De Ce 20390
PARAMETRIC MAP LANGUAGE — FORTRAN II
COMPUTER — IBM 7074
GENERATES ANY HYPERBOLIC NAVIGATION SYSTEM BY USING PARAMETRIC EQuUA-
TIONSe GENERATES PLOTTING COORDINATES FOR LORAN As LORAN Cs OMEGA AND
DECCA CHARTSe WILL PROCESS ALL LATTICE LINES THAT FALL WITHIN A SPEC-
IFIED GEOGRAPHIC AREA» CAN BE DISPLAYED ON ANY OF THE FOLLOWING MAP
PROJECTIONS-— MERCATORs TRANSVERSE MERCATOR: LAMBERT CONFORMAL CONIC,
OBLIQUE MERCATOR» POLYCONICe OvcSe NOe 53012¢ AUTHORS-- ReAw BOLTON,
ReMe BOLTON’
NAUTICAL CHART DIVISION» CODE 5620
UeSe NAVAL OCEANOGRAPHIC OFFICE
WASHINGTON De Ce 20390
DECCA HI-FIX LANGUAGE — FORTRAN
COMPUTER — PDP—-5s 8S
GENERAL PURPOSE PROGRAM FOR CONVERSION OF HYPERBOLIC COORDINATES TO
X-Y COORDINATE SYSTEMSe TYPE GEOGRAPHIC COORDINATES OF MASTER AND
SLAVE STATIONS — PAPER TAPE OR KEYBOARD INPUT FOR LANE COUNTSs OUTPUT
ON ASR-33 TELEPRINTERe WRITTEN FOR THE UeSe COAST GUARD BY LTe ReMe
O'HAGAN (RETe)e COPY OF PROGRAM WAS DEPOSITED WITH DECUS (DIGITAL E-
QUIPMENT CORP. USERS SOCIETY).
DIGITAL EQUIPMENT CORPORATION
MAYNARDs MASSACHUSETTS 01754
HYPERMAP LANGUAGE — FORTRAN
COMPUTER -— (NOT GIVEN)
(COPY ON FILE AT NODC)
A SERIES OF PROGRAMS FOR DRAWING MAPS AND PLOTTING DATA ON THEMe THE
PROGRAM OPERATES UNDER A SIMPLE COMMAND LANGUAGE WHICH ENABLES THE US-
ER TO REFER TO HIS DATA AND THE MAP DATA BY NAMEe THERE ARE ELEVEN
PROJECTION OPTIONS AVAILABLE IN THE BASIC TRANSFORMATION SUBROUTINE >
A MORE ADVANCED PACKAGE (WITH SEVERAL PROJECTIONS TAKING THE ELLIPTIC-
ITY OF THE EARTH INTO ACCOUNT) IS UNDER DEVELOPMENTe AUTHOR-- DR ROB-
ERT L PARKER» UNIVe OF CALIFORNIA AT SAN DIEGO.
PROFe JOHN De. MUDIE
SCRIPPS INSTITUTION OF OCEANOGRAPHY
LA JOLLA» CALIFe 92037
PAGE 064
GENERAL MAP PROJECTION LANGUAGE — MAD
COMPUTER -— IBM 7090 W/
CALCOMP 763
(COPY ON FILE AT NODC)
CONVERSION (OR GENERATION) OF LATITUDE AND LONGITUDE VALUES TU MAP
PROJECTION COORDINATESe INCLUDES ALL COMMONLY EMPLOYED PROJECTIONS
OF SPHEREe OBLIQUE CASES MAY BE AUTOMATICALLY OBTAINEDe AUTHOR-- We
Re TOBLERe
THE UNIVERSITY OF MICHIGAN
DEPARTMENT OF GEOGRAPHY
ATTNe DRe We Re TOBLER
ANN ARBOR» MICHIGAN 48104
FINITE MAP PROJECTION DISTORTIONS LANGUAGE — MAD
COMPUTER —- IBM 7090
(COPY ON FILE AT NODC)
PROGRAMS AND SUBROUTINES TO ESTIMATE THE ERRORS INTRODUCED BY THE SUB-
STITUTION OF MAP PROJECTION COORDINATES FOR SPHERICAL COORDINATESe
STATISTICAL COMPUTATIONS OF FINITE DISTORTION ARE RELATED TO TISSOT'S
INDICATRIX AS A GENERAL CONTRIBUTION TO THE ANALYSIS OF MAP PROJEC—
TIONSe REFe TECHNICAL REPORT NOs 3 'GEOGRAPHICAL COORDINATE COMPUTA-—
TIONS PART II's BY We Re TOBLERs DEPTe OF GEOGRAPHY.
THE UNIVERSITY OF MICHIGAN
ANN ARBOR» MICHIGAN
PAGE 065
PHYSICAL OCEANOGRAPHY
HK —H KKK KAKA HHH
%#-*-* AIR-SEA INTERACTION AND HEAT BUDGET *-*-*
FUNCTION VAPW LANGUAGE — FORTRAN Iv
COMPUTER — IBM 1801/02
(cOPY ON FILE AT NODC)
SUBPROGRAM CALCULATES SATURATION VAPOUR PRESSURE OVER WATERe INPUT IS
TEMPERATURE IN DEGRe Ke USES AN EQUATION FROM SMITHSONIAN TABLES PAGE
350. THE FUNCTION CONVERTS THE LOG OUTPUT OF THIS EQUATION TO ACTUAL
PRESSURE IN MILLIBARSe NeIeOe PROGe NOewe -—24e AUTHOR-- Re HOWARTHe
NATIONAL INSTITUTE OF OCEANOGRAPHY
WORMLEYs GODALMINGs SURREY
ENGLAND
ATR-SEA LANGUAGE — FORTRAN
COMPUTER — IBM 7074
DETERMINES THE RELATION BETWEEN THE 500 MBe WIND FIELD AND OCEAN SUR-
FACE CONDITIONS (WAVES), THROUGH THE USE OF STATISTICAL METHODSe OcSe
PROGRAM NOe 534645 BY WeHe GEMMILLe
OCEANOGRAPHIC PREDICTION DIVe, CODE 3400
NAVAL OCEANOGRAPHIC OFFICE
SUITLAND» MD. 20390
CLOUD COVER AND DAILY SEA TEMPERATURE LANGUAGE — FORTRAN
COMPUTER — IBM 7074
DIVIDES CLOUD COVER INTO THREE GROUPS AND COMPUTES MEAN TEMPERATURE
BY HOUR OF DAY AND BY DAY FOR EACH DEPTHe OS NOe 53414e AUTHOR-- De
Be NIXe
OCEANOGRAPHIC PREDICTION DIVes CODE 3400
NAVAL OCEANOGRAPHIC OFFICE
SUITLAND» MDe 20390
LAYER DEPTH PLOT LANGUAGE — FORTRAN
COMPUTER -— IBM 7074
COMPUTES AND PLOTS LAYER DEPTH» ON A SYNOPTIC BASIS» FROM VARIOUS
DEFINITIONSe OS NOe 534536¢ AUTHOR-— DeBe NIX
OCEANOGRAPHIC PREDICTION DIVes CODE 3400
NAVAL OCEANOGRAPHIC OFFICE
SUITLAND» MD. 20390
PREDICTION OF VERTICAL TEMPERATURE CHANGE LANGUAGE — FORTRAN
COMPUTER -— IBM 7074
(COPY ON FILE AT NODC)
A TECHNIQUE BASED PRIMARILY ON HEAT BUDGET AND WIND MIXING CALCULA-
TIONS HAS BEEN DEVELOPED FOR PREDICTING THE VERTICAL THERMAL STRUCTURE
OF THE OCEANe THE TECHNIQUE ESSENTIALLY MODIFIES THE INITIAL THERMAL
STRUCTURE THROUGH INCIDENT SOLAR RADIATION» BACK RADIATIONs SENSIBLE
AND EVAPORATIVE HEAT EXCHANGE» CONVECTIVE HEAT TRANSFER IN THE WATER
MASS» AND WIND MIXINGe PREDICTIONS ARE MADE AT 6-HOUR INTERVALS UNTIL
1200Z ON THE DATE OF FORECASTe THE PREDICTED BT IS PRINTED OUT, ALSO
CAN BE PLOTTED WITH A BENSON-LEHNER MODEL J PLOTTERe AUTHORS-- WeHe
GEMMILL AND DeBe NIXe REFe IMR NOs 0-42-65 (UNPUBLISHED MANUSCRIPT).
PAGE 066
SEE ALSO IMR NOe 0-45-65 BY Be THOMPSON, AND IMR NOe 0-13-66 BY BAR-
NETT AND AMSTUTZe PROGRAM LISTINGS SEPARATE FROM MANUSCRIPTSe
OCEANOGRAPHIC PREDICTION DIVe,s CODE 3400
NAVAL OCEANOGRAPHIC OFFICE
SUITLAND» MD. 20390
TWO-DIMENSIONAL POWER SPECTRUM FOR SWOP II LANGUAGE - FORTRAN
COMPUTER - IBM 7074
DETERMINATION OF SPECTRUM ASSOCIATED WITH THE SPATIAL DISTRIBUTION OF
ENERGY AS OBTAINED FROM AN INSTANTANEOUS PICTURE OF THE OCEAN TAKEN
FROM AIRCRAFT (SWOP II1)e OS NOe 534846 AUTHOR-- CeMe WINGERe
OCEANOGRAPHIC PREDICTION DIVe»s CODE 3400
NAVAL OCEANOGRAPHIC OFFICE
SUITLAND» MDe 20390
WIND STRESS LANGUAGE — FORTRAN
COMPUTER - IBM 7074
DETERMINES WIND STRESS ON THE OCEAN SURFACEe OS NOc 534622¢ AUTHOR--
WeHe GEMMILLe
OCEANOGRAPHIC PREDICTION DIVe»s CODE 3400
NAVAL OCEANOGRAPHIC OFFICE
SUITLAND» MD. 20390
TRANSPORT COMPUTATIONS FROM ATMOSPHERIC PRESSURE LANGUAGE - FORTRAN II
AND Iv
COMPUTER -— IBM 16205
IBM 7040 AND
IBM 1130
(COPY ON FILE AT NODC — FORTRAN II FOR 1620 ONLY)
COMPUTES» ACCORDING TO A SYSTEM OF ANALYSIS DESIGNED BY DRe NePe FOF-—
ONOFFs THE STEADY STATE MASS TRANSPORT IN THE OCEAN FROM ATMOSPHERIC
PRESSURE DATAs MERIDIONAL AND ZONAL COMPONENTS OF EKMAN TRANSPORT 9
TOTAL MERIDIONAL TRANSPORT» INTEGRATED TRANSPORT AND INTEGRATED GEO-
STROPHIC TRANSPORTe INPUT ARE SEA LEVEL PRESSURE CARDS FROM THE EX-
TENDED FORECAST DIVe OF THE UeSe WEATHER BUREAUe OUTPUT ARE MEAN
MONTHLY VALUES FOR THE SPECIFIED GRID OF ALTERNATE 5 DEGREES OF LATI-
TUDE AND LONGITUDE IN THE NORTHERN HEMISPHEREe FORTRAN II PROGRAM IS
PUBLISHED IN FISHERIES RESEARCH BOARD OF CANADA, MSe SERIES (OCEANe
AND LIMNOL.) NOw 163% 1963 BY DRe CHARLOTTE FROESEe FORTRAN IV PRO-
GRAM HELD BY STATISTICAL SERVICES» FISHERIES RESEARCH BOARD OF CANADA,
BIOLOGICAL STATIONs NANAIMO, Be Cos CANADA
OCEANOGRAPHER-IN-CHARGE
PACIFIC OCEANOGRAPHIC GROUP
BIOLOGICAL STATION
NANAIMO», Be Ces CANADA
SYNOPTIC ANALYSIS AND FORECASTING OF LANGUAGE — MACHINE
SURFACE CURRENTS COMPUTER - CDC 1604 AND
CDC 3200
INPUT IS SURFACE WIND ANALYSIS/FORECAST»s SEA SURFACE TEMPERATURE ANAL—
YSIS/FORECASTs 600 FEET TEMPERATURE ANALYSIS AND SOME CLIMATOLOGY e
OUTPUT IS SURFACE CURRENT TRANSPORT IN NAUTICAL MILES PER 24 HOURS»
CURRENT DIRECTION AND STREAM FUNCTIONe REFe FNWF TECHNICAL NOTE NOe 9
AND HUBERT (1965)e DIRECT REQUESTS FOR INFORMATION TO--
COMMANDING OFFICER
FLEET NUMERICAL WEATHER CENTRAL
MONTEREY» CALIFORNIA 93940
PAGE 067
WIND CURRENTS LANGUAGE — MAD
COMPUTER — IBM 7090
COMPUTES CURRENTS FROM STANDARD WIND OBSERVATIONS.
VINCENT NOBLE
THE UNIVERSITY OF MICHIGAN
GREAT LAKES RESEARCH DIVISION
INSTITUTE OF SCIENCE AND TECHNOLOGY
1077 NORTH UNIVERSITY BUILDING
ANN ARBOR» MICHIGAN 48104
RADIATION TEMPERATURE OF SEA SURFACE LANGUAGE -— FORTRAN
COMPUTER — (NOT GIVEN)
(COPY ON FILE AT NODC)
EVALUATES THREE EMPIRICAL EQUATIONS», DEVELOPED BY REGRESSION METHODS,
TO OBTAIN AN ESTIMATE OF THE DIFFERENCE BETWEEN SKIN AND BUCKET TEM-—
PERATURES FROM STANDARD WEATHER OBSERVATIONS MADE AT SEAe THESIS BY
ROBERT De BOUDREAUs REFe NO. 65-15T (1965s 79 P)e
DEPTe OF OCEANOGRAPHY
COLLEGE OF GEOSCIENCES
TEXAS A AND M UNIVERSITY
COLLEGE STATIONs TEXAS 77843
SYNOPTIC ANALYSIS AND FORECASTING OF LANGUAGE — MACHINE
POTENTIAL MIXED LAYER DEPTH COMPUTER -— CDC 1604 AND
cDC 3200
INPUT TO PROGRAM-- CLIMATOLOGY, SYNOPTIC WAVE HEIGHT ANALYSIS/FORE-
CAST» SEA SURFACE TEMPERATURE ANALYSIS» 600 FEET TEMPERATURE ANALYSIS/
FORECAST» AND BT OBSERVATIONSe OUTPUT IS MIXED LAYER DEPTH IN FEET AT
GRID POINTS (63X63 FIELD)» TENDENCY OF THERMOCLINE NEXT 24 HOURSs MAG-—
NITUDE» AND SHORT TERM FLUCTUATIONS OF THE THERMOCLINEe REF-- SEE FNWF
TECHNICAL NOTE NOe 10 AND/OR NOe 212¢ DIRECT INQUIRIES TO--
COMMANDING OFFICER
FLEET NUMERICAL WEATHER CENTRAL
MONTEREY» CALIFORNIA 93940
*-*-% CURRENTS AND TRANSFER PROCESSES *-—*-*
SURFACE CURRENT SUMMARY LANGUAGE - AUTOCODER
COMPUTER —- IBM 7074
(COPY ON FILE AT NODC)
THE RESULTANT CURRENT SPEED AND RESULTANT CURRENT DIRECTIONS ARE COM—
PUTED BY MARSDEN SQUARE, 1-DEGe OR 5-DEGe SQUARE AND MONTH FROM H 1-9,
NETHERLANDS 193 OR JAPANESE 118 DATAe OS NOe 52252. AUTHOR-—- MAXINE
JACKSONe
COMPUTER SYSTEMS DIVISION
NATIONAL OCEANOGRAPHIC DATA CENTER
WASHINGTONs De Co 20390
MODIFIED SURFACE CURRENTS LANGUAGE — AUTOCODER
COMPUTER - IBM 7074
(COPY ON FILE AT NODC)
MODIFIES MeHe JACKSON'S PROGRAM TO PROVIDE THE SAME INFORMATION ON A
FILE REPRESENTING THE H 1-95 118 (JAPANESE)s 193 (NETHERLANDS) FILES
COMBINED» AUTHOR-- CeSe CALDWELL>. OS NOew 201566
COMPUTER DEPARTMENT» CODE 083
PAGE 068
NAVAL OCEANOGRAPHIC OFFICE
SUITLAND» MDe 20390
STATISTICAL SURFACE CURRENT ROSE LANGUAGE -— AUTOCODER
COMPUTER — IBM 7074
CALCULATES FREQUENCIES OF A NORMAL DISTRIBUTIONs POPULATING THE
DIRECTION-SPEED GROUPS OF A STANDARD ROSE FORMAT» WHICH BEST FITS
THE ACTUAL DATA SURFACE (REFe SP-64 -A STATISTICAL ROSE PROGRAM—»5
BY We YERGEN)» OS NO 53301le AUTHOR-—- We YERGENe
OCEANOGRAPHIC ANALYSIS DIVe» CODE 3300
NAVAL OCEANOGRAPHIC OFFICE
SUITLAND» MD. 20390
COMPUTE ADVECTION LANGUAGE — FORTRAN
COMPUTER — IBM 1401
COMPUTES HORIZONTAL ADVECTION FROM AN INITIAL POINT IN THE WATER COL—
UMN FROM EQUATIONS DESCRIBED BY Ae FISHER» IM NOe 66-9 (INFORMAI MANU-
SCRIPT)e FROM KNOWN INPUTS OF DENSITYs CURRENT VELOCITIES» AND TEMP—
ERATURE GRADIENTS» ADVECTION IS COMPUTED FROM AN INITIAL POINT OVER A
GIVEN DISTANCEs ASSUMING NO VERTICAL HEAT LOSS» HORIZONTAL COMPONENTS
IN THE XsY PLANE ARE COMPUTED AND A RESULTANT VECTOR IS DETERMINEDe
OS NOe 5349026 AUTHOR-- ReKe FRANKLINe
OCEANOGRAPHIC PREDICTION DIVe» CODE 3400
NAVAL OCEANOGRAPHIC OFFICE
SUITLANDs MDe 20390
GVPAsVPA LANGUAGE - FORTRAN IV
COMPUTER -— IBM 360/65
CALCULATES VELOCITIES AND TRANSPORTS FOR AS MANY AS 50 SUCCESSIVE STA-
TION PAIRSe USES AS INPUT INTERPOLATED DATA ON CARDS FROM PROGRAM
"DYNAM! » WHICH CALCULATES DYNAMIC HEIGHTS AT STANDARD DEPTHSe
BUREAU OF COMMERCIAL FISHERIES
Pe Oo BOX 3830
HONOLULUs HAWAII 96812
STANDARD-VECTOR DEVIATION ROSE FOR CURRENT DATA LANGUAGE — FORTRAN
COMPUTER — IBM 7074
(COPY ON FILE AT NODC)
CALCULATES THE FOLLOWING PARAMETERS FOR A TWO DIMENSIONAL NORMAL EL-
LIPTICAL DISTRIBUTED CURRENT FIELD-- MEAN SPEED,» COMPONENTS OF THE
VECTOR MEAN» COMPONENTS OF THE STANDARD-VECTOR DEVIATION ALONG THE
PRINCIPAL AXES» AND THE INCLINATION OF THE MAJOR AXISe PROGRAM HAS
BEEN IN USE PRINCIPALLY AS AN AID IN AIR-SEA RESCUE OPERATIONSe INPUT
IS CURRENT DATA WHICH HAS BEEN TABULATED IN SPECIFIED SPEED-INTERVAL
CLASSES FOR EIGHT COMPASS POINTS.» REFe IMR O-22-65 (UNPUBLISHED MANU-
SCRIPT)e AUTHOR-- DONALD Ae BURNS» CODE 72006
OCEANOGRAPHIC ANALYSIS DIVe»s CODE 3300
NAVAL OCEANOGRAPHIC OFFICE
SUITLANDs MDe 20390
GULF STREAM PATH LANGUAGE — FORTRAN
COMPUTER - IBM 7074
PREDICTS THE PATH OF THE GULF STREAM BY MEANS OF 1) A SINE GENERATED
FUNCTION» 2) THE CONSERVATION OF POTENTIAL VORTICITYs» AND 3) HARMONIC
ANALYSISe AUTHOR-- WeHe GEMMILLo
OCEANOGRAPHIC PREDICTION DIVe» CODE 3430
NAVAL OCEANOGRAPHIC OFFICE
PAGE 069
SUITLAND» MARYLAND 20390
VELOCITY AND HORIZONTAL EDDY COEFFICIENTS LANGUAGE — FORTRAN
COMPUTER —- IBM 709
COMPUTATION OF VELOCITY AND HORIZONTAL MIXING EDDY COEFFICIENTS ALONG
ISENTROPIC SURFACESe AUTHOR-- AeDe KIRWANe
TEXAS A AND M UNIVERSITY
COLLEGE OF GEOSCIENCES
DEPARTMENT OF OCEANOGRAPHY
COLLEGE STATIONs TEXAS 77843
SALINITY DISTRIBUTION IN ONE-DIMENSIONAL ESTUARY LANGUAGE — FORTRAN
COMPUTER -— (NOT GIVEN)
(COPY ON FILE AT NODC)
A MODEL IS CONSTRUCTED FOR AN ESTUARY TO PREDICT THE SALINITY DISTRIB-
UTION FOR A GIVEN FRESH WATER INFLOWs WITH APPLICATION TO THE UPPER
CHESAPEAKE BAY AND THE SUSQUEHANNA RIVERe BASED ON A SALT CONTINUITY
EQUATION IN WHICH THE SEAWARD SALT ADVECTION IS BALANCED BY TURBUILENT
DIFFUSION TOWARD THE HEAD OF THE BAYe IN FINAL FORM» IT IS A LINEAR»
SECOND-ORDER» AND PARABOLIC PARTIAL DIFFERENTIAL EQUATION WITH VARIA-
BLE COEFFICIENTS WHICH ARE FUNCTIONS OF BOTH SPACE AND TIMEe REFe 69-
7s TECHe REPORT 54 (MAY 19695 7O0Pe) BY WILLIAM BOICOURTe
CHESAPEAKE BAY INSTITUTE
THE JOHNS HOPKINS UNIVERSITY
BALTIMORE» MDe 21218
PROCESSING OF OCEANOGRAPHIC OBSERVATIONS LANGUAGE — FORTRAN II
COMPUTER — IBM 1620 II
(COPY ON FILE AT NODC)
A NUMBER OF PROGRAMS AND SUBROUTINES FOR PROCESSING 'MICHELSENS CON-
TAINER' DATA (AUTOMATIC CURRENT AND TEMPERATURE MEASUREMENTS)» FOR
PROCESSING EKMAN CURRENT METER DATAs AND FOR HARMONIC ANALYSIS AND
POWER SPECTRUM ANALYSISe REFe TECHNICAL REPORT NOe 379 NATO SUBCOM-—
MITEE ON OCEANOGRAPHIC RESEARCH (105 Pes FEB 1967)e« AUTHOR-— DRe HeEeo
SWEERS (OF THE CANADIAN OCEANOGRAPHIC DATA CENTRE) e
GEOPHYSICAL INSTITUTE
UNIVERSITY OF BERGEN
BERGEN» NORWAY
DRIFT BOTTLE DATA COMPUTATION LANGUAGE — AUTOCODER
COMPUTER ~— IBM 7074
(COPY ON FILE AT NODC)
COMPUTES THE FOLLOWING FROM BOTTLE RECOVERY INFORMATION-- BEARING»
NAUTICAL MILES DRIFTEDs NUMBER OF DAYS ADRIFTs AND SPEED IN NAUTICAL
MILES PER DAYe COMPUTES MARSDEN AND 1/4-DEGREE SQUARES OF RELEASE«
OUTPUT ON MAGNETIC TAPEe AUTHOR-- JUDY YAVNERe USED WITH A TAPE TO
PRINT/CARD EDITING AND SELECTION PROGRAMe AUTHOR-— JOHN JENSONe
COMPUTER SYSTEMS DIVISIONs CODE 2400
NATIONAL OCEANOGRAPHIC DATA CENTER
WASHINGTON» DeCe 20390
LATERAL RELATIVE DISTRIBUTION OF MATERIAL FROM LANGUAGE — FORTRAN II
A CONTINUOUS SOURCE IN A CONSTANT CURRENT COMPUTER — IBM 7094
PREDICTS THE RATIO OF THE CONCENTRATION OF A CONTAMINANT TO ITS CENTER
LINE VALUE AS A FUNCTION OF LONGITUDINAL AND TRANSVERSE DISTANCE FROM
THE SOURCE DUE TO HORIZONTAL ADVECTION AND DIFFUSION WHEN DISCHARGED
S A VERTICAL LINE SOURCE OF UNIT DEPTH AND UNIT RATE OF DISCHARGE IN
AN UNBOUNDED MEDIUMe INPUT ARE THE VELOCITY (A CONSTANT)» THE 1 LONGI-
TUDINAL AND TRANSVERSE COORDINATES» AND THE DIFFUSION VELOCITY, IeEe,s
PAGE 070
THE SPREADING COEFFICIENTs A MEASURE OF THE HORIZONTAL DIFFUSIONe THE
OKUBO-PRITCHARD MODEL FOR AN INSTANTANEOUS RELEASE 1S USED FOR THE MO-
DELe AUTHORS-- HeEe WALTERS AND HeHe CARTERe
HARVEY Ee WALTERS
CHESAPEAKE BAY INSTITUTE
THE JOHNS HOPKINS UNIVERSITY
CHARLES AND 34TH STe
BALTIMOREs MDe 21218
CONTINUOUS LINE SOURCE (REFLECTED) LANGUAGE -— FORTRAN II
COMPUTER -— IBM 7094
PREDICTS THE HORIZONTAL STEADY STATE DISTRIBUTION OF A CONTAMINANT DUE
TO HORIZONTAL ADVECTION AND DIFFUSION WHEN DISCHARGED AS A VERTICAL
PLANE SOURCE OF UNIT DEPTH AND UNIT RATE OF DISCHARGE AND LOCATED PER-
PENDICULAR TO A BOUNDARYe THE VELOCITY IS ASSUMED TO BE CONSTANTe THE
OKUBO-PRITCHARD MODEL FOR AN INSTANTANEOUS RELEASE IS USEDe IT IS IN-
TEGRATED LATERALLY TO TRANSFORM A VERTICAL LINE SOURCE SOLUTION TO A
SOLUTION FOR A VERTICAL PLANE SOURCE AND IS TOTALLY RELECTED AT THE
BOUNDARY TO QUANTITATE THE BOUNDARY EFFECTe AUTHORS-— HeEeo WALTERS
AND HeHe CARTERe
HARVEY Ee WALTERS
CHESAPEAKE BAY INSTITUTE
THE JOHNS HOPKINS UNIVERSITY
CHARLES AND 34TH STeo
BALTIMOREs MDe 21218
CONTINUOUS SOURCE IN TIDAL ESTUARY PER LANGUAGE - FORTRAN II
UNIT DEPTH AND UNIT RATE OF RELEASE COMPUTER - IBM 7094
PREDICTS THE CENTERLINE LONGITUDINAL DISTRIBUTION OF A CONTAMINANT AS
A FUNCTION OF PUMPING TIMEs DUE TO HORIZONTAL ADVECTION AND DIFFUSION
WHEN DISCHARGED AS A VERTICAL LINE SOURCE OF UNIT DEPTH AT A CONSTANT
RATE IN A TIDAL ESTUARYe INPUT ARE THE MAXIMUM TIDAL VELOCITY, THE
NON-TIDAL VELOCITY» THE DIFFUSION VELOCITY IeE5se SPREADING COEFFICIENT,
A MEASURE OF HORIZONTAL DIFFUSION» PUMPING TIME IeEe TIME SINCE SOURCE
WAS INITIATED» AND THE LONGITUDINAL DISTANCE FROM THE SOURCE» STORAGE
NECESSARY-- 15000 WORDS (CAN BE EASILY CHANGED TO 7000 WORDS)e AUTHORS
— HeEe WALTERS AND HeHe CARTERe
HARVEY Ee WALTERS
CHESAPEAKE BAY INSTITUTE
THE JOHNS HOPKINS UNIVERSITY
CHARLES AND 34TH STe
BALTIMOREs MDe 21218
CONTINUOUS SOURCE IN TIDAL ESTUARY PER UNIT DEPTH LANGUAGE - FORTRAN II
AND UNIT RATE OF RELEASE» WITH COOLING TERM COMPUTER - IBM 7094
PREDICTS THE CENTERLINE LONGITUDINAL DISTRIBUTION OF HEAT AS A FUNC
TION OF PUMPING TIME DUE TO HORIZONTAL ADVECTIONs DIFFUSION» AND AT-
MOSPHERIC COOLING WHEN DISCHARGED AS A VERTICAL LINE SOURCE AT A CON-
STANT RATE IN A TIDAL ESTUARYe THE OKUBO-PRITCHARD MODEL FOR AN IN-
STANTANEOUS RELEASE IS USED FOR THE MODELe IT IS FURTHER ASSUMED THAT
EACH INFINITESIMAL RELEASE COOLS EXPONENTIALLY WITH TIMEe THE RATE CO-
EFFICIENT IS CALLED THE COOLING COEFFICIENTe CORE STORAGE NECESSARY--
15000 WORDS (CAN BE RUN USING 7000 WORDS)e AUTHORS-- HeEe WALTERS AND
HeHe CARTERe
HARVEY Ee WALTERS
CHESAPEAKE BAY INSTITUTE
THE JOHNS HOPKINS UNIVERSITY
CHARLES AND 34TH STe
BALTIMORE» MDe 21218
PAGE O71
CURRENT METER DYNAMICS LANGUAGE — MAC
COMPUTER — IBM OS/360
PROGRAM WITH SUBROUTINES AS ESTIMATOR FOR DERIVING POSITION AND EULER
ATTITUDE (PITCH AND ROLL) ANGLES SO THAT PRECISE CURRENT METER DYNAM—
ICS CAN BE OBTAINEDe APPLIED TO A REAL CASE PROBLEM FOR WHICH SIMUL-
ATION RESULTS ARE DISCUSSED. THESIS BY MICHEL FROIDEVAUX (JAN 1968)
tAPPLICATION OF STATISTICAL ESTIMATION TO THE DETERMINATION OF OCEAN
CURRENT METER DYNAMICS',
INSTRUMENTATION LABORATORY
MASSACHUSETTS INSTITUTE OF TECHNOLOGY
CAMBRIDGEs MASSACHUSETTS 02139
CURRENT METER TURBULENCE LANGUAGE — FORTRAN
COMPUTER — IBM 7074
GIVES AN INDICATION OF TURBULENCE IN THE OCEAN BY COMPUTING MEASURES
OF THE DEVIATIONS FROM MEANS OVER VARIOUS LENGTHS OF TIMEe OS NOe —
57202~¢ AUTHOR-— ROBERT Re GLEASONe
EXPLORATORY OCEANOGRAPHY DIVe»s CODE 7200
NAVAL OCEANOGRAPHIC OFFICE
SUITLAND» MD. 20390
FLOW METER PLOTS LANGUAGE -— FORTRAN IV
COMPUTER — IBM 360/65,
CAL COMP
(COPY ON FILE AT NODC)
DETERMINES FLOW METER PERFORMANCE AND PLOTS NUMBER OF REVOLUTIONS VS.
TIMEe OUTPUT GIVES THE COfFFICIENT OF CORRELATION AND STANDARD DEVIA-
TIONs AND THE REGRESSION LINE AND 1¢96 STANDARD DEVIATIONS ARE MARKED
OFF ON THE PLOTe CORE STORAGE USED-- 31K BYTES (WITH PLOT ROUTINES).
AUTHOR-— MARILYNN BORKOWSKI.
BUREAU OF COMMERCIAL FISHERIES
TROPICAL ATLANTIC BIOLOGICAL LABORATORY
75 WIRGINIA BEACH DRIVE
MIAMI» FLORIDA 33149
FILM DATA PROCESSING LANGUAGE — FORTRAN-—60
COMPUTER — CDC 1604
ACCEPTS RICHARDSON'S CURRENT DATA FROM A BINARY TAPE SUPPLIED By IN-
FORMATION INTERNATIONALs INCe NORTH-SOUTH AND EAST-WEST VELOCITY COM-
PONENTS ARE COMPUTED FROM THE COMPASSs VANE» RO AND R10 COUNTERS» AND
ALL INFORMATION MAY BE PRINTED EVERY TIME SLICEe A HISTOGRAM OF THESE
COMPONENTS IS PRINTED AT THE END OF EACH FILMe FURTHERMORE» AN ENVEL-—
OPE OF THE CURRENT ANGLES AND CURRENT SPEEDS IS SHOWN AT 2-HOUR INTER-
VALSe FINALLY» 6-HOUR MEANS AND STANDARD DEVIATIONS OF VELOCITY COM-
PONENTS ARE PUNCHED ON CARDS FOR FURTHER PROCESSINGe 1200-CHARACTER
RECORDS ARE READ INTO STORAGE BY MEANS OF A MACHINE LANGUAGE SUBROUT-—
INEe THE REMAINING PROGRAM IS IN FORTRANe AUTHOR-— EMANUEL MEHR,
COLLEGE OF ENGINEERING» NYU.
NEW YORK UNIVERSITY
SCHOOL OF ENGINEERING AND SCIENCE
GEOPHYSICAL SCIENCES LABORATORY
2455 SEDGWICK AVEes BRONX» NeYe 10468
DATUBA LANGUAGE — FORTRAN-63
COMPUTER - CDC 3800
ANALYZES THE DEFLECTIONS OF A TRI-MOORED»s SUBSURFACE» BUOY-CABLE ARRAY.
ACTED ON BY CURRENT—-INDUCED FORCESe SOLUTION IS BY THE METHODS OF
PAGE 072
IMAGINARY REACTIONS AND SUCCESSIVE APPROXIMATIONS»e CALCULATES THE
HYDRODYNAMIC FORCES» AND BOTH NORMAL AND TANGENTIAL DRAGS ARE INCILUD-
EDe DOCUMENTED IN NRL REPORT 6894 (MAY 1969)5 BY ReAcw SKOP AND ReEo
KAPLANe MEMORY REQUIREMENTS-— APPROXe 16000 WORDS FOR THE ARRAYS IN
COMMON AND 2100 WORDS FOR THE MAIN PROGRAM AND SUBPROGRAMSe
NAVAL RESEARCH LABORATORY
4555 OVERLOOK AVENUEs SeWe
WASHINGTON» De Ce 20390
CABLE CONFIGURATION LANGUAGE — FORTRAN Iv
GOMPUTER = IBM 1800 SYS
(COPY ON FILE AT NODC)
COMPUTES THE EQUILIBRIUM CONFIGURATION AND TENSIONS OF A CABLE TOWING
A SUBMERGED BODY FOR FAIRED, UNFAIREDs AND DISCONTINUOUS (LOWER PART
FAIRED) CABLESe THE OUTPUT ON THE LINE PRINTER GIVES THE VALUES OF
THE INPUT DATA FOLLOWED BY VARIOUS CALCULATED VALUESe THE SOLUTION IS
FOUND FOR THE "HEAVY GENERAL CABLE* LAW OF CABLE LOADINGS AS DESCRIBED
BY MeCe EAMES (1968)e EXECUTION TIME-— ABOUT 30 SECSe FOR EACH CASE.
NeleOQo PROGRAM NOe 168¢ AUTHOR-- CATHERINE CLAYSONe
NATIONAL INSTITUTE OF OCEANOGRAPHY
WORMLEY»s GODALMINGs SURREY
ENGLAND
CURRENT METER ANALYSIS LANGUAGE -— FORTRAN IV
COMPUTER -— IBM 1800 SYS
READSs CALIBRATES AND PLOTS DATA FROM BERGEN OR PLESSEY CURRENT MET-—
ERSe DATA IS READ FROM CARDSe ANY ONE OF THE READINGS MAY BE TAKEN
AS ROTOR COUNT, THE DIFFERENCES BETWEEN CONSECUTIVE READINGS THEN BE-
ING USED BY THE PROGRAM AS THE BASIS OF CURRENT SPEEDe THREE GRAPHS
MAY BE PLOTTED (EeGe SPEED» DIRECTION, AND TEMPERATURE) e ALL RESULTS
ARE ALSO OUTPUT TO MAGNETIC TAPEe NelIeO5o PROGRAM 111 BY WeleJe SLADE
WRITE-UP IN NeleO5w INTERNAL REPORT NOe Nel2s DEC 1968-6
NATIONAL INSTITUTE OF OCEANOGRAPHY
WORMLEYs» GODALMINGs SURREY
ENGLAND
CURRENT METER CONVERSION LANGUAGE -— FORTRAN IV
COMPUTER - IBM 1800 SYS
CONVERTS RAW CURRENT METER DATA INTO CALIBRATED OUTPUT FOR RECORDING
ON BOTH LINE-PRINTER AND MAGNETIC TAPEe NeleOs SUB-PROGRAM -ll»s BY
WeTeJo SLADE (REFe NelTeO5s INTERNAL REPORT NOco Nol2)eo
NATIONAL INSTITUTE OF OCEANOGRAPHY
WORMLEY» GODALMINGs SURREY
ENGLAND
VEL LANGUAGE - FORTRAN IV-H
COMPUTER - SDS SIGMA 7
COMPUTES GEOSTROPHIC VELOCITY DIFFERENCE BETWEEN TWO OCEANOGRAPHIC
STATIONSs ACCORDING TO A FORMULA DESCRIBED BY NePe FOFONOFF AND CHAR-
LOTTE FROESEe (PROGRAM WRITTEN AS SUBROUTINE -— NO I/P OR O/P)
INFORMATION PROCESSING CENTER
ATTNe MARY HUNT
WOODS HOLE OCEANOGRAPHIC INSTITUTION
WOODS HOLE» MASSACHUSETTS 02543
VTR LANGUAGE —- FORTRAN IV-H
GOMPUTER SD SieSiG MAN,
PAGE 073
SUBROUTINE COMPUTES VOLUME TRANSPORT BETWEEN TWO STATIONSe
INFORMATION PROCESSING CENTER
ATTNe MARY HUNT
WOODS HOLE OCEANOGRAPHIC INSTITUTION
WOODS HOLE, MASSACHUSETTS 02543
THISTO LANGUAGE —- FORTRAN IV-H
COMPUTER — SDS SIGMA 7
PRODUCES A TWO DIMENSIONAL FREQUENCY DISTRIBUTION OF SAMPLES AVERAGED
OVER CHOSEN INTERVAL AGAINST TIMEe INPUT-- CONTROL CARDS AND 9-TRACK
MAG. TAPEs’ OUTPUT—- A LINE PRINTER PLOT OF AVERAGED COMPASS» VANE»
DIRECTION» AND SPEED AGAINST TIME.
INFORMATION PROCESSING CENTER
ATTNe JOHN Ae MALTAIS
WOODS HOLE OCEANOGRAPHIC INSTITUTION
WOODS HOLE, MASSACHUSETTS 02543
VECTAV LANGUAGE — FORTRAN IV-H
COMPUTER -— SDS SIGMA 7
PRODUCES A NINE TRACK MAGe TAPE IN WHOI FORMAT OF EAST AND NORTH VEL-
OCITY VECTOR AVERAGES AND THEIR CORRESPONDING POLAR REPRESENTATIONSe
INPUT—— CONTROL CARDS AND DATA ON 9-TRACK TAPE.
INFORMATION PROCESSING CENTER
ATTNe JOHN Ae MALTAIS
WOODS HOLE OCEANOGRAPHIC INSTITUTION
WOODS HOLEs MASSACHUSETTS 02543
PROVEC LANGUAGE — FORTRAN IV-H
COMPUTER - SDS SIGMA 7
COMPUTES PROGRESSIVE VECTORS FROM DIRECTION AND SPEED VALUESe INPUT-—
CONTROL CARDS AND 9-TRACK MAGe TAPE IN WHOI FORMATe OUTPUT-—- LISTINGs
ON LINE PRINTER» OF PROGRESSIVE VECTORS AND/OR A MAGe TAPE TO BE USED
WITH A PDP-5 DRIVEN CALCOMP FOR A PLOT OF THE VECTORS.
INFORMATION PROCESSING CENTER
ATTNe JOHN Ae MALTAIS
WOODS HOLE OCEANOGRAPHIC INSTITUTION
WOODS HOLE» MASSACHUSETTS 02543
¥—%—*% ICE IN THE SEA *—*—*
LANGUAGE — FORTRAN 60
ICEGRID MODIFIED
COMPUTER — IBM 1604
(COPY ON FILE AT NODC)
INCORPORATES PROGRAMS 'ICEMELT!' AND "ICEGRID'e TAKES INTO CONSIDERA-
TION THE EFFECTS OF MELTING ON THE PRODUCTION OF FIVE-DAY FORECASTS OF
THE WIND DRIFT AND CONCENTRATION OF SEA ICEs USING EQUATIONS AFTER ZU-
BOV AND AN EARLIER PROGRAM OF KNODLEe USES A 26X21 GRID-POINT ARRAY
WITH VARIABLE SCALEe OUTPUT FIELDS ARE CONCENTRATION, DIRECTION AND
DISTANCE OF MOVEMENTe DOCUMENTED IN THESIS BY KENNETH Me IRVINE (UN-
PUBLISHED» 1965).
NAVAL POSTGRADUATE SCHOOL
MONTEREY» CALIFORNIA 93940
PAGE 074
ICE POTENTIAL LANGUAGE — FORTRAN
COMPUTER — IBM 7074
PROCESSES OBSERVED SEA ICE CONDITIONS SO THEY CAN BE USED IN FORECAST-—
ING SEA ICE CONDITIONSe OS NOe 201412e AUTHOR-- LeAew WALKERe
DATA SYSTEMS CENTER» CODE 0831
NAVAL OCEANOGRAPHIC OFFICE
SUITLANDs MDe 20390
STATISTICAL ANALYSIS OF ICE DATA LANGUAGE — FORTRAN
COMPUTER — IBM 7074
COMPUTES THE MEAN CONCENTRATION VALUES» MEAN AGE SEVERITY VALUES» AND
MEAN FLOE SIZE SEVERITY VALUE OF ICE DATAe AUTHOR-- BARBARA GRAY e
OCEANOGRAPHIC PREDICTIONs CODE 3400
NAVAL OCEANOGRAPHIC OFFICE
SUITLAND» MDe 20390
SEA ICE STUDIES LANGUAGE - FORTRAN IV
COMPUTER — IBM 7090/94
(COPY ON FILE AT NODC)
A GENERALIZED PROGRAM WITH SEVERAL OPTIONS THAT ALLOW CONSIDERABLE
LATITUDE IN THE SPECIFICATION OF INPUT AND OUTPUT DATAe A MAIN PROGRAM
READS IN THE INPUT DATA AND SUMMARIZES THE RESULTS OF EACH YEAR'S IN-
TEGRATIONe SUBROUTINE YARIT CALCULATES THE TEMPERATURE AND THICKNESS
CHANGES OF THE ICE AND SNOW FOR EACH TIME STEP DURING THE YEARe SUB-
ROUTINE FLIP TAKES THE MONTHLY VALUES OF THE INDEPENDENT ENERGY FLUXES
AT THE UPPER BOUNDARY AND PRODUCES SMOOTHED VALUES FOR EACH TIME STEPe
SUBROUTINE SALPR CALCULATES THE SALINITY PROFILE FOR EACH TIME STEPe
FINALLYs SUBROUTINE RITE WRITES THE TEMPERATURE PROFILE» ICE THICKNESS
AND MASS CHANGES FOR EACH 10-DAY PERIOD THROUGHOUT THE YEARe LISTED
IN A MEMORANDUM RM-6093-PR (NOV 19695 173 P) "NUMERICAL PREDICTION OF
THE THERMODYNAMIC RESPONSE OF ARCTIC SEA ICE TO ENVIRONMENTAL CHANGES!
BY GeAe MAYKUT AND Ne UNTERSTEINERe PREPARED FOR UeSe AIR FORCE PRO-
JECT RANDe
THE RAND CORPORATION
1700 MAIN STe
SANTA MONICAs CALIFe 90406
*#-#—- PHYSICAL PROPERTIES - ANALYSES AND SUMMARIES —-*-*
DEVIATION OF TEMPe AND SALINITY PART 1 (DOTS-1) LANGUAGE — AUTOCODER
COMPUTER - IBM 7074
(COPY ON FILE AT NODC)
A PROTOTYPE PROGRAM TO MONITOR NODC FORMAT COMPUTED OCEAN STATION DATA
FOR ERRORS» OS NOe 52305¢ AUTHOR-- SeCe PORTERe
DEVELOPMENT DIVISION, CODE 2320
NATIONAL OCEANOGRAPHIC DATA CENTER
WASHINGTONs DeCe 20390
OBJECTIVE THERMOCLINE ANALYSIS LANGUAGE —- FORTRAN IV-H
COMPUTER — IBM 360 SERe
AND CDC 6500
(COPY ON FILE AT NODC)
READS DIGITIZED BATHYTHERMOGRAPH TRACES AND THEN ANALYZES THEM OBJECT-
IVELY BY GAUSSIAN AND NON-GAUSSIAN METHODS FOR THE TOPs CENTER, AND
BASE OF THE MAIN THERMOCLINEe ADDITIONALLY» SUCH FEATURES AS MULTIPLE
PAGE 075
THERMOCLINES» INVERSIONS» AND THERMAL TRANSIENTS ARE IDENTIFIED ALSO
AND THEIR KEY POINTS ARE INCLUDED IN THE INFORMATIONAL DATA PRINTOUT.
THESIS BY ERIC Fe GROSFILS "OBJECTIVE DIGITAL ANALYSIS OF BATHYTHERMO-—
GRAPH TRACES' (UNPUBLISHED MANUSCRIPT, DECe 1968s 130 P)e
NAVAL POSTGRADUATE SCHOOL
MONTEREY» CALIFORNIA 93940
GRADIENT SUMMARY BY 1-DEG SQUARE» MONTH LANGUAGE — AUTOCODER
COMPUTER — IBM 7074
(COPY ON FILE AT NODC)
COMPUTES AND PRINTS AVERAGE TEMPERATURE GRADIENTS FOR EACH 20 METER
DEPTH INTERVAL» BY EACH OF 12 MONTHS» ALONG WITH THE NUMBER OF OBS THE
MEAN IS BASED ONe ANY SIGNIFICANT POSITIVE GRADIENTS (INCREASE OF 022
DEGe C/20M OR MORE) SUMMARIZED SEPARATELY ON SAME PAGEe INPUT IS NODC
DIGITIZED BT FILE» SORTED GEOGRAPHICALLYe OS NOe 624016 AUTHOR-— JEFF
GORDON (REVISED JULY 1969)e
COMPUTER SYSTEMS DIVe»s CODE 2400
NATIONAL OCEANOGRAPHIC DATA CENTER
WASHINGTONs De Ce 20390
THERMOCLINE AND MIXED LAYER DEPTHS LANGUAGE -— AUTOCODER
COMPUTER -— IBM 7074
(COPY ON FILE AT NODC)
DETERMINES AND PRINTS OUT THE DEPTHS OF THE MIXED LAYER AND TOP OF THE
THERMOCLINE FOR INDIVIDUAL BT OBSERVATIONS» WITH MEANS FOR EACH MONTH
WITHIN A 1-DEGREE SQUAREe USES GRADIENT CRITERIA GIVEN BY CODE 2120
SCIENTIST (BASED LARGELY ON NODC!S GRADIENT SUMMARY PROGRAM OUTPUT) »
AND ENTERED ON CONTROL CARDSe COMPARISON IS MADE WITH ABSOLUTE VALUE
OF GRADIENT/ 10Me OS NOe 624026 AUTHOR-- JEFF GORDON (JULY 1969).
COMPUTER SYSTEMS DIVes CODE 2400
NATIONAL OCEANOGRAPHIC DATA CENTER
WASHINGTON» De Ce 20390
SeEeReCe BI ANALYSIS LANGUAGE -— AUTOCODER
COMPUTER — IBM 7074
(COPY ON FILE AT NODC)
ERROR CHECKS DATA AND COMPUTES LAYER DEPTHs SURFACE EFFECT» MEAN
GRADIENT» MAXIMUM NEGATIVE GRADIENT» ASCENDANT AND FIRST NEGATIVE
GRADIENTe A SOUND VELOCITY COMPUTATION IS ALSO MADEe OS NOe 201136
REPORT NOe O-31-63 (UNPUBLISHED MANUSCRIPT)e AUTHOR-- MeEeo MYERSe
COMPUTER DEPARTMENT» CODE 0831
NAVAL OCEANOGRAPHIC OFFICE
SUITLAND» MDe 20390
GDNP »GRAD LANGUAGE — FORTRAN Iv
COMPUTER - IBM 360/65
WITH CALCOMP
CALCULATES THE GRADIENTS OF DENSITY» TEMPERATURE» AND SALINITY AS
FUNCTIONS OF SIGMA-T ALONG 4 STANDARD SECTIONS IN THE TRADE WIND ZONE
OCEANOGRAPHY PROGRAM PILOT STUDY AREAe CALCOMP DIGITAL PLOTTER RE-
QUIRED FOR PROGRAM 'GRAD'.
BUREAU OF COMMERCIAL FISHERIES
Pe O« BOX 3830
HONOLULU» HAWAII 96812
BT TEMPERATURE GRADIENT DISTRIBUTION LANGUAGE — FORTRAN
COMPUTER — IBM 7074
COMPUTES A FREQUENCY TABLE OF GRADIENTS IN 30 INTERVALS BY DEPTHSe ANY
PAGE 076
EXCEPTIONS TO THE INTERVALS WITH THEIR CORRESPONDING DEPTH AND THE
MEAN GRADIENT FOR EACH DEPTH IS PRINTED ALSO’ OS NOe 10120%¢ AUTHOR -
MeVe JENNINGS.
COMPUTER DEPARTMENT» CODE 0831
NAVAL OCEANOGRAPHIC OFFICE
SUITLAND» MD. 20390
MONTHLY SONIC LAYER DEPTH LANGUAGE -— FORTRAN
COMPUTER -— IBM 7074
CALCULATES SONIC LAYER DEPTH FROM BT TRACES AND CONVERTS POSITION TO
PLOT ON MERCATOR BASE WITHOUT OVERPRINTSe OS NOe 5348056 AUTHOR-- DeBe
NIXe
OCEANOGRAPHIC PREDICTION DIVes CODE 3400
NAVAL OCEANOGRAPHIC OFFICE
SUITLAND» MDe 20390
SEA SURFACE TEMPERATURE DISTRIBUTION LANGUAGE - FORTRAN
COMPUTER - IBM 7074
(COPY ON FILE AT NODC)
TABULATES THE FREQUENCY» PERCENT FREQe» CUMULATIVE PERCENT FREQes AND
MEAN TEMPERATURE FOR ALL ONE-DEGREE SQUARES AND MONTHS PROVIDED By
SEA SURFACE TEMPERATURE SUMMARY CARDS FROM ASHEVILLE», Ne Ce OS NOe
201362 AUTHOR-- Je LECKIEe
COMPUTER DEPARTMENT» CODE 0831
NAVAL OCEANOGRAPHIC OFFICE
SUITLAND» MD. 20390
TEMPERATURE DISTRIBUTION BY ONE-DEGREE SQUARES LANGUAGE — FORTRAN
COMPUTER - IBM 7074
(COPY ON FILE AT NODC)
COMPUTES AND TABULATES A FREQUENCY DISTRIBUTION FOR SELECTED TEMPER-
ATURE INTERVALS AND STANDARD DEPTHS» AND THE MAXIMUMs MINIMUM s AND
MEAN VALUES OF TEMPERATURE FOR EACH STANDARD DEPTHe A REPORT IS PRO-
DUCED FOR EACH ONE-DEGREE SQUAREe OS NOe 20126 PART 5e AUTHOR-- CeSe
CALDWELL.
COMPUTER DEPARTMENT: CODE 083
NAVAL OCEANOGRAPHIC OFFICE
SUITLAND» MD. 20390
TEMPERATURE AVERAGE SUMMARY BY 1-DEGREE SQUARES LANGUAGE — FORTRAN
COMPUTER -— IBM 7074
(COPY ON FILE AT NODC)
COMPUTES FOR EACH ONE-DEGREE SQUARE WITHIN A MARSDEN SQes FROM GEO-
GRAPHIC STATION DATAs A SEASONAL AVERAGE AND FREQUENCY AND A TWELVE
MONTH AVERAGE AND FREQUENCY, AT EACH OF FOURTEEN SELECTED STANDARD
DEPTHSe OS NOe 201232¢ AUTHOR-- CeSe CALDWELL.
COMPUTER DEPARTMENT» CODE 083
NAVAL OCEANOGRAPHIC OFFICE
SUITLANDs MD. 20390
VERTICAL TEMPERATURE GRADIENTS LANGUAGE — FORTRAN
COMPUTER — IBM 7074
(COPY ON FILE AT NODC)
COMPUTES, FROM GEOGRAPHIC STATION DATAs THE VERTICAL TEMPERATURE GRAD-
IENT LARGEST IN ABSOLUTE MAGNITUDE BETWEEN SUCCESSIVE STANDARD DEPTHS,
FOR EACH STATIONe THESE GRADIENTS ARE TABULATED IN FREQUENCY DISTRIBU-
TION FORMAT» AND AVERAGES ARE CALCULATED FOR EACH ONE-DEGREE SQUARE e
OS NO«w 20126 PART 2¢ AUTHOR-- CeSe CALDWELL.
PAGE O77
COMPUTER DEPARTMENT» CODE 083
NAVAL OCEANOGRAPHIC OFFICE
SUITLAND» MD. 20390
DENSITY (SIGMA-T) GRADIENT BY 1-DEGREE SQUARE LANGUAGE — FORTRAN
COMPUTER — IBM 7074
(COPY ON FILE AT NODC)
COMPUTES» FROM GEOGRAPHIC STATION DATA» THE VERTICAL SIGMA-T GRADIENT
LARGEST IN ABSOLUTE MAGNITUDE BETWEEN SUCCESSIVE STANDARD DEPTHS» FOR
EACH STATIONe THESE GRADIENTS ARE TABULATED FOR FREQUENCY DISTRIBUTION
FORMATs AND AVERAGES ARE CALCULATED FOR EACH 1-DEG SQe OS NOs 20122.
AUTHOR-- CeSe CALDWELL.
COMPUTER DEPARTMENT: CODE 083
NAVAL OCEANOGRAPHIC OFFICE
SUITLAND» MD. 20390
THERMOCLINE ONE-DEGREE LANGUAGE - AUTOCODER
COMPUTER - IBM 7074
(COPY ON FILE AT NODC)
PRODUCES A DESCRIPTION OF THE THERMOCLINE BY DEFINING THE TOPs BOTTOM,
MAGNITUDE, AND INTENSITY OF THE THERMOCLINE AND THE MOST EXTREME IN-
TENSITY WITHIN THE THERMOCLINEe THE PRINTED REPORT CONTAINS THE ABOVE
QUANTITIES FOR EACH STATION WITHIN A 1-DEGREE SQUARE, ALSO AVERAGE
VALUES FOR THE 1-DEGREE SQUARE. IN PRODUCTION MODE, THE PROGRAM USES
A CONSTANT THERMOCLINE CRITERIONe IN THE TEST MODE, THE CRITERION MAY
BE INCREMENTED FOR ANOTHER PASS OF THE SAME DATA TAPEs OS NOe 201265
PART 46 AUTHOR-- CeSe CALDWELL.
COMPUTER DEPARTMENTs CODE 083
NAVAL OCEANOGRAPHIC OFFICE
SUTTLAND» MARYLAND 20390
SALINITY GRADIENT BY ONE-DEGREE SQUARE LANGUAGE — FORTRAN
COMPUTER - IBM 7074
(COPY ON FILE AT NODC)
COMPUTESs FROM GEOGRAPHIC STATION DATAs THE VERTICAL SALINITY GRADIENT
LARGEST IN ABSOLUTE MAGNITUDE BETWEEN SUCCESSIVE STANDARD DEPTHS» FOR
EACH STATIONe THIS INFORMATION IS TABULATED IN FREQUENCY DISTRIBUTION
FORM, AND AVERAGES ARE CALCULATED FOR EACH ONE-DEGREE SQUARE. THE FRE-
QUENCY INTERVAL IS 0201 O0/00/M BETWEEN LIMITS OF -0.5 AND +205 O/00/Me
OS NOs 20121. AUTHOR-- CeSe CALDWELL.
COMPUTER DEPARTMENT» CODE 083
NAVAL OCEANOGRAPHIC OFFICE
SUITLAND» MD. 20390
SALINITY DEVIATION COMPUTATION WITH PLOT LANGUAGE — FORTRAN
COMPUTER — IBM 7074
(COPY ON FILE AT NODC)
THE DEVIATIONS OF SALINITY FROM RELATED MODELS ARE COMPUTED FOR SERIAL
OCEANOGRAPHIC STATION DATA AND A SALINITY PROFILE PLOTTEDe OS NOe -
52301le AUTHOR-— SeCe PORTER.
DEVELOPMENT DIVISION, CODE 2320
NATIONAL OCEANOGRAPHIC DATA CENTER
WASHINGTONs De Ce 20390
STATION DATA VERTICAL ARRAY SUMMARY LANGUAGE — AUTOCODER
COMPUTER —- IBM 7074
(COPY ON FILE AT NODC)
SUMMARIZES FOR ANY COMBINATION OF SIX PARAMETERS ( TEMPERATURE» SAL-
INITY» SIGMA-Ts OXYGENs SOUND VELOCITY» DYNAMIC DEPTH) AND COMPUTES
MAXIMUM AND MINIMUM VALUES» NUMBER OF OBSERVATIONSs MEANS AND STANDARD
DEVIATIONS AT STANDARD LEVELSe SUMMARIES MAY BE MONTHLY OR YEARLY AND
PAGE 078
BY SELECTED ONE-DEGREE SQUARESe THERE IS AN OPTION TO GENERATE A SPE-
CIAL CONDENSED TAPE FOR INPUT TO A HISTOGRAM PLOT PROGRAMe OS NOe
52257e AUTHOR-- MAXINE JACKSONe
COMPUTER SYSTEMS DIVISION
NATIONAL OCEANOGRAPHIC DATA CENTER
WASHINGTON» DeCe 20390
MARSDEN SQUARE AVERAGES FROM OCEAN STATION LANGUAGE — FORTRAN
GEO-SORTED FILE COMPUTER -— IBM 7074
(COPY ON FILE AT NODC)
CALCULATES AVERAGE SEA SURFACE SOUND VELOCITY» AVERAGE LAYER DEPTH»
AVERAGE DEPTH OF THE SOUND CHANNEL AXIS» AND AVERAGE SOUND VELOCITY AT
THE SOUND CHANNEL AXISe THESE VALUES ARE CALCULATED FOR EACH ONE-DE-
GREE QUADRANGLE FOR EACH MONTHe A SUBPROGRAM *AREAD! IS CALLED WHICH
GAINS ACCESS TO THE NODC ARCHIVE TAPE FILE OF SORTED OCEANOGRAPHIC DA-
TAe REFe INFORMAL REPORT IR NOe 67-95 (DEC 1967)» ENTITLED "EXTRACT-—
ING INFORMATION FROM THE GEO-SORT FILE BY COMPUTER PROGRAMING!» BY Je
Ce FRANCE» OCEANOGRAPHIC ANALYSIS DIVISION» CODE 33166 FURTHER INFOR-
MATION MAY BE OBTAINED FROM DISSEMINATION DEPTe CODE 445 OR THE AUTHOR
NAVAL OCEANOGRAPHIC OFFICE
WASHINGTONs DeCe 20390
STATION DATA PARAMETER INVENTORY LANGUAGE — FORTRAN
COMPUTER — IBM 7074
(COPY ON FILE AT NODC)
LISTS GEOSORTED STATION DATAs ONE LINE FOR EACH STATIONs SHOWINGs BE-
SIDES NORMAL IDENTIFICATION FIELDSs THE DEPTH TO BOTTOMs MAXIMUM SAMP—
LE DEPTH, PRESENCE OR ABSENCE OF WATER COLOR AND TRANSPARENCY CODES»
MAXIMUM DEPTH OF SOUND VELOCITIES» MINIMUM DEPTH» AND A VERTICAL IN-
DICATOR WHICH IS THE ARITHMETIC AVERAGE OF VERTICAL SAMPLE SPACING IN
TENS OF METERSe OS NO 52230¢ ALSO» PROGRAM CAN WRITE OUTPUT» INTER-
NAL NOTATIONs FOR INPUT TO A PLOTTER PROGRAM (OS NOe 52229)e AUTHOR —
ROBERT VAN WIEe
COMPUTER SYSTEMS DIVISION
NATIONAL OCEANOGRAPHIC DATA CENTER
WASHINGTONs DeCe 20390
DAILY SEAWATER OBSERVATIONS LANGUAGE -— FORTRAN IV
COMPUTER - CDC 3100
INPUTS DAILY OBSERVATIONS OF TEMPERATURE AND SALINITY AND OUTPUTS (1)
QUARTERLY STATISTICS (2) ANNUAL STATISTICS (3) A LISTING OF SEVEN-DAY
NORMALLY WEIGHTED MEANS FOR ONE YEAR (4) A PLOT OF NORMALLY WEIGHTED
MEANS FOR ONE YEARe AUTHOR-- He SOMERSe EARLY VERSION IN FORTRAN II-
D FOR THE IBM 1620.
CANADIAN OCEANOGRAPHIC DATA CENTRE
615 BOOTH STREET
OTTAWA» CANADA
OCEANOGRAPHIC SUMMARY (NOSe 192593) LANGUAGE — FORTRAN IV
COMPUTER - I8M 360/65
SUMMARIZES TEMPERATURE» SALINITY» DEPTH AND OXYGEN By 1-DEGREE SQUARES
AND OTHER DEGREE AREAS WITHIN SELECTED MARSDEN SQUARES» AT SELECTED
SIGMA-T LEVELSe VERSIONS OF PROGRAM FOR CARD OR TAPE INPUT» AND EITHER
CHART OR VERTICAL SECTION OUTPUT.
BUREAU OF COMMERCIAL FISHERIES BIOLOGICAL LABe
ATTNe DRe Re Aco BARKLEY» OCEANOGRAPHER
PeOe BOX 3830
HONOLULU» HAWAII 96812
PAGE 079
SEA SENSE - DATA DISPLAY LANGUAGE — FORTRAN
COMPUTER — IBM 7074
(cOPY ON FILE AT NODC)
EVALUATES NOMAD (NAVAL OCEANOGRAPHIC AND METEOROLOGICAL AUTOMATIC DE-
VICE) BUOY DATAs AND OUTPUTS A DISPLAY OF EACH OF THE 5 METEOROLOGICAL
PARAMETERS. THE DISPLAY IS PRINTED BY THE IBM 1401. IN ADDITION TO
THE DISPLAY» THE PROGRAM TOTALS THE NUMBER OF OBSERVATIONS MISSING FOR
ANY MONTHs AND PRINTS A HISTOGRAM OF THE DATA FOR EACH MONTHe THIS
PROGRAM IS ONE OF A CONTINUING SERIES OF COMPUTER PROGRAMS IN PROJECT
SEA SENSE. AUTHOR-- DIANA LAMAR.
SERVICES DIVISIONs CODE 2210
NATIONAL OCEANOGRAPHIC DATA CENTER
WASHINGTON» De Ce 20390
SEA SENSE — LIMIT LANGUAGE - FORTRAN
COMPUTER — IBM 7074
(COPY ON FILE AT NODC)
COMPARES NOMAD BUOY DATA TO ESTABLISHED NORMALS OF ABSOLUTE VALUES AND
TO ACCEPTABLE MAP DATAe A MONTHLY TOTAL FOR EACH PARAMETER IS COMPUT—
ED AND PRINTED FOR DATA WHICH IS GOOD, BAD» DOUBTFUL AND MISSINGe ALSO
COMPUTES THE PERCENT OF WIND SPEEDS IN EACH BEAUFORT FORCE CATEGORY
AND PRINTS THIS WITH THE NORMALS EXPECTED FOR THAT MONTH. WIND DIREC-—
TION PERCENTS ARE COMPUTED ACCORDING TO THE 9 CATEGORIES OF WIND DI-
RECTIONs AND PRINTED VSe THE NORMALSe ALSO THE MEANS OF NOMAD AND MAP
DATA ARE COMPUTED AND PRINTED VS» THE LIMIT MEANSe AUTHOR-- DIANA LA-
MAR.
SERVICES DIVISION, CODE 2210
NATIONAL OCEANOGRAPHIC DATA CENTER
WASHINGTONs De Ce 20390
SEA SENSE — STANDARD DEVIATION LANGUAGE — FORTRAN
COMPUTER — IBM 7074
(COPY ON FILE AT NODC)
COMPUTES THE MEAN AND STANDARD DEVIATION FOR EACH OF 5 METEOROLOGICAL
PARAMETERS FOR EACH MONTH OF NOMAD BUOY DATAe IF MAP DATA IS AVAIL—
ABLE, THE MEANS AND STANDARD DEVIATIONS AND MEANS AND STANDARD DEVIA-
TIONS OF THE DIFFERENCES BETWEEN NOMAD AND MAP DATA ARE COMPUTED. ALSO
COMPUTES THE TOTAL MEAN SIGNAL STRENGTH AND THE MEANS FOR EACH SYNOP-—
TIC HOUR. AUTHOR-- DIANA LAMARe
SERVICES DIVISION» CODE 2210
NATIONAL OCEANOGRAPHIC DATA CENTER
WASHINGTON» De Co 20390
SYNOPTIC MARINE WEATHER DATA SUMMARY LANGUAGE - FORTRAN-62
COMPUTER — CDC 3600
COMPILATION OF MONTHLY SEA SURFACE TEMPERATURES AND ANOMALIES (DEG—
REES CENTIGRADE)» AIR TEMPERATURES (DEGREES CENTIGRADE)» DEWPOINT TEM—
PERATURES (DEGREES CENTIGRADE)»s BAROMETRIC PRESSURES (MILLIBARS)» X-
AND Y- WIND VECTORS (KNOTS), WIND SPEEDS (KNOTS)»s CLOUD COVER (TENTHS
OF SKY COVERED), AND HEAT BUDGET VALUES (ENERGY EXCHANGE ACROSS AIR-
SEA INTERFACE IN CALORIES/CENTIMETER SQUARED/DAY) WITH NUMBER OF OBS-
ERVATIONS BY FIVE DEGREE QUADRANGLES - PACIFIC OCEANe AUTHOR-- MARVIN
We CLINE
DIRECTOR
FISHERY OCEANOGRAPHY CENTER
BUREAU OF COMMERCIAL FISHERIES
PeOe BOX 271
LA JOLLA, CALIFORNIA 92038
PAGE 080
SEA
SEA
SURFACE TEMPERATURE DATA SUMMARY LANGUAGE — FORTRAN-62
COMPUTER -— CDC 3600
COMPILATION OF MONTHLY SEA SURFACE TEMPERATURES (DEGREES FAHRENHEIT )
WITH NUMBER OF OBSERVATIONS BY ONE-DEGREE QUADRANGLES - PACIFIC OCEAN.
DIRECTOR
FISHERY OCEANOGRAPHY CENTER
BUREAU OF COMMERCIAL FISHERIES
PeOw BOX 271
LA JOLLA» CALIFORNIA 92038
SURFACE TEMPERATURE AND ANOMALY SUMMARY LANGUAGE - FORTRAN-62
COMPUTER — CDC 3600
COMPILATION OF MONTHLY SEA SURFACE TEMPERATURES (DEGREES FAHRENHEIT
AND CENTIGRADE) AND ANOMALIES FROM LONG TERM MEAN WITH NUMBER OF OB-
SERVATIONS BY TWO-DEGREE QUADRANGLES — PACIFIC OCEAN.
DIRECTOR
FISHERY OCEANOGRAPHY CENTER
BUREAU OF COMMERCIAL FISHERIES
PeO5w BOX 271
LA JOLLA» CALIFORNIA 92038
HEMISPHERIC SEA SURFACE TEMPERATURE ANALYSIS LANGUAGE - MACHINE
COMPUTER -— CDC 1604
(A) MAINTAINS UP-TO-DATE LARGE SCALE SYNOPTIC SEA SURFACE TEMPERATURE
DISTRIBUTION FOR NORTHERN HEMISPHERE» (8) SUPPLIES INPUT MATERIAL FOR
DETAILED ANALYSIS OF SELECTED LOCAL REGIONS ON A CURRENT BASIS ONLYe
OUTPUT FROM PROGRAM-- (A) CALCOMP HARD COPY MAP, SCALE 1/60 MILLIONs
WITH ISOTHERMS AT 2-DEG INTERVALS» (B) 63X63 ARRAY OF GRID POINT VAL-
UES ON POLAR STEREOGRAPHIC PROJECTION WITH EQUATOR AN INSCRIBED CIRCLE
(C) CERTAIN MEAN CHARTS OF SEA SURFACE TEMPERATURE FOR 5 DAYS» 15 DAYS
AND MONTHLYe REFe TECHNICAL NOTE NOe 21 (1966).
COMMANDING OFFICER
FLEET NUMERICAL WEATHER CENTRAL
MONTEREY» CALIFORNIA 93940
GG T SEA LANGUAGE — MACHINE
COMPUTER -— CDC 1604
CALCULATES THE LOCATION OF LARGE SCALE HYPER-BAROCLINIC ZONES IN THE
OCEANSe INPUT IS THE OUTPUT FROM THE SEA SURFACE TEMPERATURE ANALY-
SIS PROGRAMe OUTPUT ARE ISOLINES OF THE GG PARAMETERe THE DIRECTION-
AL SECOND SPACE DERIVATIVE OF THE BASIC PARAMETER IS COMPUTEDe CORE
STORAGE-- 32000 48-BIT WORDSe ADDITIONAL STORAGE REQUIREMENTS—— ONE
MILLION WORD DRUMe DATA IS IN THE STANDARD FNWC FORMATe DIRECT RE-
QUESTS FOR INFORMATION TO--
COMMANDING OFFICER
FLEET NUMERICAL WEATHER CENTRAL
MONTEREYs CALIFORNIA 93940
AVERAGE TEMPERATURES IN WATER COLUMN LANGUAGE — MAD
COMPUTER - IBM 7090
COMPUTES AVERAGE TEMPERATURE FOR EACH 10 METER LAYER IN WATER COLUMN.
AVERAGE COMPUTED FOR EACH 1-DEGe LATe X 1-DEGe LONGe SQUARE FOR EACH
MONTHe INPUT—- DIGITIZED BT DATAe
VINCENT NOBLE
THE UNIVERSITY OF MICHIGAN
GREAT LAKES RESEARCH DIVISION
PAGE 081
1077 NORTH UNIVERSITY BUILDING
ANN ARBORs MICHIGAN 48104
SUBSURFACE THERMAL STRUCTURE ANALYSIS LANGUAGE -— SCRAP
COMPUTER -— CDC 1604
PRODUCES ANALYSIS OF (1) TEMPERATURE AT TOP OF THERMOCLINE (2) TEMPER
ATURE AT SELECTED SUBSURFACE LEVELS (3) GRADIENT» MAGNITUDE» AND BOT-
TOM OF THERMOCLINE AND (4) THERMOCLINE TENDENCY AND FLUCTUATIONS. IN-
PUT TO PROGRAM-- (1) SEA SURFACE TEMPERATURE ANALYSIS (2) GRADIENT OF
TRANSIENTS (3) PREVIOUS ANALYSIS OF ALL LEVELS (4) CLIMATOLOGY OF ALL
LEVELS (5) ANALYSIS OF MIXED LAYER DEPTH, AND CURRENT TRANSPORT (6) BT
REPORTS (7) WAVE HEIGHT FORECASTS AND (8) MIXED LAYER DEPTH FORECASTS.
INPUT IS IN FNWC STANDARD FORMAT FIELDSe REFe TECHe NOTE NOe 21.
COMMANDING OFFICER
FLEET NUMERICAL WEATHER CENTRAL
MONTEREYs CALIFORNIA 93940
OCEAN STATION DEPTH SUMMARY LANGUAGE —- SPS
COMPUTER - IBM 1401
(COPY ON FILE AT NODC)
USES THE NODC MASTER CARD FILE FOR OCEAN STATIONS WORLDWIDE» WHICHs IN
ADDITION TO ALL IDENTIFICATION FIELDSs CONTAINS DEPTH TO BOTTOM AND
MAXIMUM SAMPLE INFORMATIONe THE RECORDS ARE PUT ON TAPE, GEO-SORTED,
ZONE-EDITED AND BLOCKED. THE FILE IS UPDATED SEMIANNUALLYe THE SUM-—
MARY PROGRAMs REQUESTED BY NAVOCEANO MARINE SCIENCES DEPTe,s MAKES A
TALLY OF THE NUMBER OF STATIONS WITH MAXe SAMPLES WITHIN GIVEN INTER-
VALS» WITHIN A GIVEN DISTANCE FROM THE BOTTOMs ETCe TOTAL COUNTS ARE
PRINTED FOR EACH MARSDEN SQes AND GRAND TOTALS FOR THE FILEe OS NOe«
52286e¢ AUTHOR-- Ce DINGER
COMPUTER SYSTEMS DIVISION
NATIONAL OCEANOGRAPHIC DATA CENTER
WASHINGTONs De Co 20390
%¥-%-% PHYSICAL QUANTITIES» COMPUTATION OF *-—#-*
STATION DATA COMPUTE LANGUAGE — AUTOCODER
COMPUTER — IBM 7074
(COPY ON FILE AT NODC)
INTERPOLATES FOR TEMPERATUREs SALINITYs AND OXYGEN AT STANDARD DEPTHS.
COMPUTES SIGMA-T AND WILSON'S SOUND SPEED AT OBSERVED AND STANDARD
DEPTHSs COMPUTES SPECIFIC VOLUME ANOMALY AND DYNAMIC DEPTH ANOMALY AT
STANDARD DEPTHSe OS NOw 522515 AUTHOR-- MAXINE JACKSONe ANOTHER PRO-
GRAM FOR NODC STATION DATA COMPUTATIONS WAS WRITTEN LATER FOR THE GE-
235/DATANET 30 SYSTEM IN BASIC LANGUAGE, BY JIM NOELe CURRENTLY» THE
'COMPUTE' PROGRAM IS BEING REWRITTEN IN PL/I FOR THE IBM 0S/360,5 BY
MAXINE JACKSON AND MICHAEL FLANAGANe
COMPUTER SYSTEMS DIVISION
NATIONAL OCEANOGRAPHIC DATA CENTER
WASHINGTON, De Ce 20390
BATHYTHERMOGRAPH DATA CONVERTER LANGUAGE — AUTUYCODER
COMPUTER —- IBM 7074
(COPY ON FILE AT NODC)
CONVERTS BT TEMPERATURE DATA FROM 10 FEET -— FAHRENHEIT» 2 FATHOMS -
FAHRENHEIT, 6 METERS — CENTIGRADE TO 5 METERS — CENTIGRADE INTERVALS.
OS NOs 32253. AUTHOR-—- MAXINE JACKSONe NODC HAS ALSO IN THE PROGRAM
LIBRARY A FORTRAN LANGUAGE ROUTINE TO CONVERT BT DATA, NODC FORMAT >
PAGE 082
FROM FAHRENHEIT/FEET AT 10 FTe INTERVALS TO CELSIUS/METERS AT 5 METER
INTERVALS USING LINEAR INTERPOLATIONe AUTHOR-— RUDI SAENGERe OS NO.
522026
COMPUTER SYSTEMS DIVISION
NATIONAL OCEANOGRAPHIC DATA CENTER
WASHINGTON» De Ce 20390
NIO PROGRAM 58 ATLAS — STATION DATA LANGUAGE — EMA
COMPUTER - ATLAS 1
VARIOUS PROPERTIES OF SEA WATER ARE CALCULATED FROM THE SETS UF READ-
INGS OF PRESSURE (OR DEPTH)» TEMPERATURE AND SALINITY TAKEN AT A STA-
TIONe SOME RESULTS ARE GIVEN AT OBSERVED» AND SOME AT STANDARD, PRES-—
SURESe THERE ARE SEVERAL VERSIONS OF THIS PROGRAM DEPENDING UN WHETH-
ER PRESSURE OR DEPTH IS INPUTe AUTHOR-- JAMES CREASEe REFe NeleOo
INTERNAL REPORT NOe N60
NATIONAL INSTITUTE OF OCEANOGRAPHY
WORMLEY» GODALMINGs SURREY
ENGLAND
INTERPOLATION OF SPECIFIC VOLUME ANOMALY LANGUAGE —- FORTRAN
COMPUTER -— IBM 7074
(COPY ON FILE AT NODC)
COMPUTES SPECIFIC VOLUME ANOMALIES AND DYNAMIC DEPTH ANOMALIES AT OB-
SERVED LEVELSe FIELDS OCCUPY THE SAME POSITIONS AS ON THE NODC FORMAT
STANDARD CARD AND REPLACE SOME CHEMISTRY FIELDSe AT STANDARD DEPTHS
SPECIFIC VOLUME ANOMALIES ARE INTERPOLATED FROM THE OBSERVED LEVEI_S
RATHER THAN COMPUTED FROM INTERPOLATED TEMPERATURE AND SALINITY AS HAS
BEEN DONE PREVIOUSLYe DYNAMIC DEPTH ANOMALIES AT THESE STANDARD
DEPTHS ARE THEN COMPUTED FROM THESE INTERPOLATED SPECIFIC VOLUME ANOM-
ALIESe AN OUTPUT LISTING MAY BE MADE WHICH COMPARES THE TWO FIELDS AT
STANDARD DEPTHS WITH THE SAME TWO FIELDS APPEARING ON THE INPUT DATA
TO SHOW THE RESULTANT DIFFERENCESe OS NOco 5223262 AUTHOR--— ROBERT VAN
WIE.
COMPUTER SYSTEMS DIVISIONs CODE 2400
NATIONAL OCEANOGRAPHIC DATA CENTER
WASHINGTONs DeCe 20390
INTERPOLATION FOR OCEANOGRAPHIC DATA LANGUAGE - FORTRAN
COMPUTER — CDC 3200 AND
IBM 1620
(COPY ON FILE AT NODC)
INTERPOLATES THE VALUES OF DEPTH, TEMPERATURE» AND SALINITY AT ISEN-
TROPIC LEVELS (CONSTANT VALUES OF THE DENSITY FUNCTIONS) e USES A FOUR-
POINT LAGRANGIAN POLYNOMIAL, EXCEPT MODIFICATIONS ARE MADE WHERE COM-—
MON OCEANOGRAPHIC CONDITIONS DISTORT THE POLYNOMIALe A DETAILED TECH-
NICAL REPORT PUBLISHED IN TM NOe 312 (FEBe 1964) 3 AUTHORS-- Je FARRELL
AND Re LAVOIEs COPIES OBTAINABLE FROM DDC» NUWSs NODC.
NAVAL UNDERWATER WEAPONS RESEARCH
AND ENGINEERING STATION
NEWPORT» RHODE ISLAND 02840
PHYSICAL OCEANOGRAPHY DATA REDUCTION LANGUAGE — FORTRAN II
PROGRAMS FOR THE CDC 3100 COMPUTER - CDC 3100
(COPY ON FILE AT NODC)
AN OCEANOGRAPHIC DATA PROCESSING SYSTEM DESIGNED TO ACCEPT THE DATA
FROM THE ORIGINAL LOG SHEETSe COMPUTES OBSERVED TEMPERATURES AND
PRESSURES FROM THERMOMETER READINGS» SALINITIES FROM THE CONDUCTIVITY
RATIO READINGSs THE DISSOLVED OXYGEN FROM THE TITRES AND THE REACTIVE
SILICA CONCENTRATIONS FROM THE OPTICAL DENSITIESe THE DATA INPUT MAY
BE PUNCHED PAPER TAPE FROM THE PDP-8 SYSTEM (Bele COMPUTER NOTE 68-5-
C) OR PUNCHED CARDSe THE FINAL PROGRAM IN THE SYSTEM COMPUTES DEPTH,
PAGE 083
POTENTIAL TEMPERATUREs SURFACE DENSITY ANOMALY, POTENTIAL SURFACE DEN-
SITY ANOMALY AND SPECIFIC VOLUME ANOMALYe THE PROGRAM ALSO CAN COM-
PUTE THE DYNAMIC HEIGHT AND POTENTIAL ENERGY ANOMALY AT GIVEN PRESS—
URES AND MAY ALSO GIVE A MAGNETIC TAPE OF THE DATA IN CARD IMAGE OF
THE CODC FORMAT. CORE STORAGE-- 16Ke REFe Bele COMPUTER NOTE 68-10-C
(OCT 19685 280 PAGES)» BY Re REINIGERs CeKe ROSS» Pe TRITES AND DeJeo
LAWRENCE.
DIRECTOR
ATLANTIC OCEANOGRAPHIC LABORATORY
BEDFORD INSTITUTE
DARTMOUTHs NOVA SCOTTIAs CANADA
WET LANGUAGE — FORTRAN
COMPUTER — HP 2115A
(COPY ON FILE AT NODC)
FOR SHIPBOARD PROCESSING OF DIGITIZED SALINITY-TEMPERATURE-DEPTH DATAs
INPUT IS ON PAPER TAPE (SEE FRB PROGRAM 'DEEP'). OUTPUT ARE PARAMET-
ERS AT STANDARD PRESSURES — TEMPERATURE» SALINITY» SIGMA-Ts DELTA-D>
SPECIFIC GRAVITY ANOMALYs SPECIFIC VOLUME ANOMALY» GEOPOTENTIAL ANOM-—
ALYs AND POTENTIAL ENERGYe DOCUMENTATION IN FRB TECHNICAL REPORT NO’
152 (DECEMBER 1969)» BY Ae HUYER AND Ce Ae COLLINS (UNPUBLISHED MSe).
DRe Ge Ae COLLINS
MARINE SCIENCES BRANCHs DEMR
PACIFIC OCEANOGRAPHIC GROUP
BIOLOGICAL STATION
NANAIMO s BeCes CANADA
STPO2 LANGUAGE — FORTRAN IV
COMPUTER - IBM 1130
(GOPY ON FIEE Al NODE)
COMPUTES DERIVED OCEANOGRAPHIC QUANTITIES FOR BISSETT-—BERMAN SeTeDe
CASTSe PRINTED OUTPUT HAS PRESSURE» TEMPERATURE» SALINITY: DEPTH,
SIGMA-T»s SPECIFIC VOLUME ANOMALY, POTENTIAL TEMPERATURE AND DENSITY»
DYNAMIC HEIGHT, POTENTIAL ENERGY ANOMALY, OXGYEN CONTENTe SOUND VELOC-
ITY OPTIONALe INPUT DATA IS IN CODC FURMATe DOCUMENTED IN FRB MANU-—
SCRIPT REPORT (UNPUBLISHED) NO. 1071 (DECEMBER 1969), BY CeAe COLLINS,
RelLeKe TRIPE AND SeKe WONG
DRe Ge Ae COLLINS
MARINE SCIENCES BRANCHs DEMR
PACIFIC OCEANOGRAPHIC GROUP
BIOLOGICAL STATION
NANAIMOs BeCes CANADA
HYDRO LANGUAGE — FORTRAN IV
COMPUTER -— IBM 1130
(COPY ON FILE AT NODC)
COMPUTES DERIVED OCEANOGRAPHIC QUANTITIES FOR HYDROGRAPHIC CASTS.
OUTPUT ON IBM 1132 PRINTER LISTS PRESSURE, TEMPERATURE», SALINITY,
DEPTH» SIGMA-T»s SPECIFIC VOLUME ANOMALY», POTENTIAL TEMPERATURE AND
DENSITY» DYNAMIC HEIGHT, POTENTIAL ENERGY ANOMALY» AND OXYGEN CONTENT >
WITH SOUND VELOCITY OPTIONALe DESCRIPTION AND LISTINGS IN FRB (UNPUB-
LISHED) MANUSCRIPT REPORT NOe 1071 (DEC 1969).
DRe Ge Ae GEOLLINS
MARINE SCIENCES BRANCH, DEMR
PACIFIC OCEANOGRAPHIC GROUP
BIOLOGICAL STATION
NANAIMOs BeCes CANADA
CADS (CALCULATE DEPENDENT QUANTITIES) LANGUAGE - FORTRAN IV
COMPUTER - IBM 1800
FROM THE OBSERVED DEPTHS, TEMPERATURES AND SALINITIES» CALCULATES THE
PAGE 084
VARIOUS DEPENDENT QUANTITIES» SUCH AS POTENTIAL TEMPERATURES» SPECIFIC
VOLUME ANOMALIES» SIGMASs AND DYNAMIC HEIGHTSe INTERPOLATES FOR THESE
QUANTITIES AT STANDARD DEPTH USING A DOUBLE LAGRANGE'S INTERPOLATION
METHODe FROM A PAIR OF STATIONS WITH A REFERENCE DEPTHs MEAN LATITUDE
AND DISTANCE BETWEEN STATIONSs CALCULATES AT STANDARD DEPTHS RELATIVE
VELOCITIES AND VOLUME TRANSPORTSe AUTHORS-— MRe MANLEYs LeWe YOUNGe
MARINE LIFE RESEARCH GROUP
SCRIPPS INSTITUTION OF OCEANOGRAPHY
PeOe BOX 109
LA JOLLAs CALIFORNIA 92037
GO (POTENTIAL TEMPes SIGMA THETAs OXYGEN) LANGUAGE — FORTRAN IV
COMPUTER - IBM 1800
GIVEN DEPTHS» TEMPERATURES» SALINITIES» AND OXYGENSs CALCULATES POTEN-
TIAL TEMPERATURES» SIGMA THETA'Ss AND OXYGENS IN UNITS OF ML/KGe
AUTHORS-—- MRe MANLEYs Le We YOUNGe
MARINE LIFE RESEARCH GROUP
SCRIPPS INSTITUTION OF OCEANOGRAPHY
PeOcoe BOX 109
LA JOLLA» CALIFORNIA 92037
FUNCTION POTLT (POTENTIAL TEMPERATURE) LANGUAGE -— FORTRAN
COMPUTER - I8M 1800
(COPY ON FILE AT NODC)
SUBPROGRAM COMPUTES POTENTIAL TEMPERATURE OF SEA WATER GIVEN SALINITY>5
TEMPERATURE» AND PRESSUREe P IS IN NEWTONS/SQ Me
NATIONAL INSTITUTE OF OCEANOGRAPHY
WORMLEYs GODALMINGs SURREY
ENGLAND
FUNCTION ALPHA (SPECIFIC VOLUME) LANGUAGE — FORTRAN
COMPUTER - IBM 1800
(COPY ON FILE AT NODC)
SUBPROGRAM COMPUTES SPECIFIC VOLUME OF SEA WATER GIVEN SIGMA-T», SIGMA-
ZEROs TEMPERATURE» AND PRESSUREe P IS IN DECIBARS
NATIONAL INSTITUTE OF OCEANOGRAPHY
WORMLEY » GODALMINGs SURREY
ENGLAND
FUNCTION SIGMO LANGUAGE — FORTRAN
COMPUTER — I8M 1800
(COPY ON FILE AT NODC)
SUBPROGRAM COMPUTES HYDROGRAPHIC FUNCTION SIGMA ZERO FROM SALINITYe
NATIONAL INSTITUTE OF OCEANOGRAPHY
WORMLEY » GODALMINGs SURREY
ENGLAND
FUNCTION SIGMT LANGUAGE
COMPUTER
FORTRAN
IBM 1800
(COPY CN FILE AT NODC)
SUBPROGRAM COMPUTES HYDROGRAPHIC FUNCTION SIGMA-T» FROM SIGMA-O AND
TEMPERATUREe
NATIONAL INSTITUTE OF OCEANOGRAPHY
WORMLEYs GODALMINGs SURREY
ENGLAND
IN SITU OCEANOGRAPHIC DATA PROGRAM LANGUAGE — FORTRAN IV
PAGE 085
COMPUTER —- IBM 360/65
COMPUTES SIGMA-T> DELTA ALPHA (SPECe VOLe ANOMe)»s OXYGEN PER CENT SAT-
URATIONe ICES FORMAT CARD-TO-CARDe OUTPUT CARDS CONTAIN THE COMPUTED
PARAMETERS ALONG WITH THE HYDRO DATAe AUTHOR-- MARILYNN BORKOWSKI »
MODIFYING AN EARLIER PROGRAM BY DeLe SHAFFER FOR THE IBM 16206¢
BUREAU OF COMMERCIAL FISHERIES
TROPICAL ATLANTIC BIOLOGICAL LABORATORY
75 VIRGINIA BEACH DRIVE
MIAMI,» FLORIDA 33149
OCEANS III LANGUAGE — FORTRAN IV
COMPUTER — IBM 360/65
OCEANOGRAPHIC STATION PROGRAM, USED FOR QUALITY CONTROL» INTERNAL ED-
ITINGs UNIT CONVERSION» COMPUTATION OF MARSDEN SQUARE, SIGMA-T, SOUND
VELOCITYe ALSO USED FOR INTERPOLATION TO STANDARD DEPTHS USING RATT—
RAY'S SCHEME AND COMPUTATION OF SPECIFIC VOLUME ANOMALY» DYNAMIC DEPTH
AND POTENTIAL ENERGY ANOMALYe EARLIER VERSION FOR THE IBM 1620 TITLED
OCEANS II IS NO LONGER USED AT CODC.
CANADIAN OCEANOGRAPHIC DATA CENTRE
615 BOOTH STREET
OTTAWAs CANADA
DENSITY-SALINITY LINEAR INTERPOLATION LANGUAGE — FORTRAN
COMPUTER — IBM 7074
(COPY ON FILE AT NODC)
SELECTED DENSITY-SALINITY VALUES TO REPRESENT THE WATER MASS MIDPOINTS
OF PARTICULAR AREASe LINEARLY INTERPOLATES THESE DENSITY-SALINITY
VALUES WITH THE RESULTING SALINITIES GIVEN AT EVERY 0-01 SIGMA-T IN-
CREMENTe OS NOe 52321le AUTHOR-- RePe STEINe
DEVELOPMENT DIVISION, CODE 2300
NATIONAL OCEANOGRAPHIC DATA CENTER
WASHINGTONs De Ce 20390
SeTeDe EDIT AND INTERPOLATE LANGUAGE — FORTRAN
COMPUTER -— IBM 1130
EDITS» AVERAGES, AND INTERPOLATES STD DATA TO 3-METER INTERVALSe OUT-
PUT-— SALINITIES AND TEMPERATURES ON CARDS IN CONDENSED FORMAT, AND A
LISTING OF DISCARDED VALUESe PROGRAM NOs UWMS-11306
UNIVERSITY OF WASHINGTON
DEPARTMENT OF OCEANOGRAPHY
22A OCEANOGRAPHY TEACHING BLDGe
ATTNe MRSe HELLA MACINTOSH
SEATTLE» WASHe 98105
INTERPOLATION LANGUAGE — FORTRAN IV
COMPUTER — IBM 360/65
INTERPOLATES TEMPERATURE» SALINITY» OXYGENs PHOSPHATE FOR STANDARD
DEPTHS» AND DEPTHs TEMPERATURE» SALINITY» OXYGEN» PHOSPHATE FOR STAN-
DARD SIGMA-T SURFACESe INPUT 1S ICES FORMAT DATAe METHOD USED IS
MEAN OF TWO LAGRANGE POLYNOMIALS, WITH LINEAR INTERPOLATION AT TOP AND
BOTTOM OF CASTe CORE STORAGE USED-- 30K BYTESe AUTHOR-— MARILYNN Re
BORKOWSKI.
BUREAU OF COMMERCIAL FISHERIES
TROPICAL ATLANTIC BIOLOGICAL LABORATORY
75 VIRGINIA BEACH DRIVE
MIAMI» FLORIDA 33149
PAGE 086
INTERPOLATION OF OCEAN STATION DATA AT LANGUAGE — FORTRAN
ISENTROPIC LEVELS COMPUTER — IBM 7074 AND
IBM 1620
(COPY ON FILE AT NODC)
INTERPOLATES DEPTHs TEMPERATURE» AND SALINITY AT ISENTROPIC LEVELSe
NUOS (NUWR AND ES) PROGRAM FOR THE I8M 1620 REVISED FOR IBM 7074 BY
RUDI SAENGERe THERE ARE TWO VERSIONS OF THIS PROGRAM — (1A) STARTING
AT SIGMA-T OF FIRST DATA CARD COMPUTING 99 LEVELS» (1B) STARTING AT
SIGMA-T 23200 COMPUTING 50 LEVELSe INPUT CONSISTS OF NODC'S OCEAN
STATION DATA CARDSe
COMPUTER SYSTEMS DIVISION
NATIONAL OCEANOGRAPHIC DATA CENTER
WASHINGTON» De Ce 20390
SHIPBOARD SURVEY -- ON-STATION MODE LANGUAGE — FORTRAN
COMPUTER -— IBM 7074
PROCESSES MAGNETIC TAPES MADE ON-STATION TO-- (1) GENERATE A MAGNETIC
TAPE OF SELECTED RECORDED DATA IN NUMERIC FORMAT FOR INPUT TO A PLOT—-
TER PROGRAM (OS NOe 10131)% (2) COMPUTE SIGMA-Ts» SPECIFIC VOLUME ANOM-
ALY AND DYNAMIC DEPTH ANOMALY» (3) PRODUCE PRINTER LISTINGS OF THE RE-
CORDED DATA AND THE CORRESPONDING COMPUTED VALUES» USED IN SELECTING
STATIONS FOR WHICH DATA IS TO BE PLOTTEDe OS NOe 101322e AUTHOR-- GAY
Me BROOKe
NAVIGATIONAL SCIENCE, CODE 5320
NAVAL OCEANOGRAPHIC OFFICE
SUITLAND» MDe 20390
OCEANOGRAPHIC DATA PROGRAM F LANGUAGE -— FORTRAN Iv
COMPUTER -— IBM 7094
(COPY ON FILE AT NODC)
LAGRANGIAN INTERPOLATIONS AT STANDARD DEPTHS AND COMPUTATION OF SUCH
OCEANOGRAPHIC QUANTITIES AS DYNAMIC HEIGHT» THERMOSTERIC ANOMALY» SIG—
MA-T» SOUND VELOCITY» ETCe ORIGINAL PROGRAM FOR THE IBM 650 BY KILMER
AND DUXBURY» 1959s FOR INTERPOLATION AND CALCULATION OF DYNAMIC HEIGHT
(TEXAS Ae AND Me TECHe REPORT NOe 59-24T)s REVISED NOV 1962 BY NOWLINe
EACH STATION REQUIRES HEADER CARDS TO SPECIFY THE ARRANGEMENT OF THE
PRINTED OUTPUT AND FOR ADDITIONAL INFORMATIONe
TEXAS A AND M UNIVERSITY
COLLEGE OF GEOSCIENCES
DEPARTMENT OF OCEANOGRAPHY
COLLEGE STATIONs TEXAS 77843
SIGMAT LANGUAGE — FORTRAN IV-E
COMPUTER - IBM 360/50
CALCULATES SIGMA-Ts DELTA» DELTA-T»s POTENTIAL TEMPERATURE, POTENTIAL
SIGMA-Ts AND POTENTIAL DELTA AT OBSERVED DEPTHSe THE CALCULATION OF
POTENTIAL TEMPERATURE IS AN APPROXIMATION SINCE DEPTH IS USED INSTEAD
OF PRESSUREe FORMULA USED FOR POTENTIAL TEMPERATURE IS THAT OF
FOFONOFF AND FROESE (1958)e CALCULATION OF OTHER QUANTITIES IS
THE SAME AS IN SUBROUTINE 'SIGMA't.
SUBROUTINES NEEDED-- SIGMA.
ROBERT Ke SEXTON
NARRAGANSETT MARINE LABORATORY
UNIVERSITY OF RHODE ISLAND
KINGSTON» RHODE ISLAND 02881
HEIGHT LANGUAGE - FORTRAN IV-E
COMPUTER - I8M 360/50
PAGE 087
INTE
AZIZ
LINT
DELI
UTILIZES OUTPUT FROM PROGRAM 'CARDS!* TO CALCULATE DYNAMIC HEIGHTS,
GEOSTROPHIC VELOCITIES» TRANSPORTS» AND DELTA VALUES INTERPOLATED AT
STANDARD DEPTHS, AS WELL AS POTENTIAL DELTAs AND SIGMA-T AT OBSERVED
DEPTHSe CAN ALSO YIELD PUNCHED OUTPUT FOR INPUT TO A PLOTTER ROUTINE.
SUBROUTINES NEEDED-- SPEWIT, VEL, MSTRCDs» VTR»s PDENs EXTIME»s SIGMA»
LAINTs DYNHTs HOLESe
ROBERT Ke SEXTON
NARRAGANSETT MARINE LABORATORY
UNIVERSITY OF RHODE ISLAND
KINGSTON» RHODE ISLAND 02881
ST LANGUAGE — FORTRAN IV-E
COMPUTER - IBM 360/50
GIVEN SERIAL OBSERVATIONS OF TEMPERATUREs SALINITY AND DEPTHs IT COM-
PUTES DELTA AT OBSERVED DEPTHS AND CREATES AN ARRAY '#ZSTD' OF STANDARD
DEPTHS EVERY 20 M TO 100 Ms EVERY 100 M TO 800 Ms AND EVERY 200 M
THEREAFTER s AND A CORRESPONDING ARRAY *t*SUMDEL' CONTAINING A NUMERICAL
INTEGRATION OF DELTA WITH DEPTH»: IN DYNAMIC CENTIMETERS.
SUBROUTINES-— SIGMAD, DELINT.
ROBERT Ke SEXTON
NARRAGANSETT MARINE LABORATORY
UNIVERSITY OF RHODE ISLAND
KINGSTONs RHODE ISLAND 02881
LANGUAGE - FORTRAN IV-E
COMPUTER — IBM 360/50
SUBROUTINE COMPUTES THERMOMETRIC DEPTH FROM CORRECTED PROTECTED AND
UNPROTECTED THERMOMETER READINGSe AN ESTIMATE OF DEPTH IS OBTAINED BY
TAKING 100 TIMES THE DIFFERENCE IN UNPROTECTED AND PROTECTED THERMOM—
ETER READINGSe THIS ESTIMATE IS USED TO CALCULATE A FIRST VALUE FOR
MEAN DENSITY» RHOs USING AN EQUATION FROM A POLYNOMIAL FIT OF WUST'S
DATA OF MEAN DENSITY WITH DEPTH IN THE NORTH ATLANTIC ('THERMOMETRIC
MEASUREMENT OF DEPTH! BY Ge WUSTs IN THE HYDROGRAPHIC REVIEW 105 1933,
TABLE 1» PAGE 34)-e THIS DENSITY IS USED IN THE EXPRESSION D (METERS)
EQUALS (TU-TW/Q * RHO) TO CALCULATE DEPTHe THIS DEPTH IS USEV TO RE-
CALCULATE THE MEAN DENSITY» RHO» AND THE LAST TWO STEPS ITERATED UNTIL
SUCCESSIVE CALCULATIONS AGREE TO WITHIN Oe25 METERS.
ROBERT Ke SEXTON
NARRAGANSETT MARINE LABORATORY
UNIVERSITY OF RHODE ISLAND
KINGSTON» RHODE ISLAND 02881
LANGUAGE — FORTRAN IV-E
COMPUTER -— IBM 360/50
SUBROUTINE PROVIDES LINEAR INTERPOLATION OF AN X VALUE FOR THE GIVEN Y
VALUEs IF Y IS OUTSIDE THE LIMITS OF THE Y AXIS» THE CORRESPONDING X
END POINT VALUE IS USED, AND THE MESSAGE INDICATOR IS SET TO SHOW
THISe
ROBERT Ke SEXTON
NARRAGANSETT MARINE LABORATORY
UNIVERSITY OF RHODE ISLAND
KINGSTONs RHODE ISLAND 02881
NT LANGUAGE — FORTRAN IV-E
COMPUTER - IBM 360/50
GIVEN OBSERVED DEPTHs TEMPERATURE AND SALINITY, STANDARD DEPTHS ARE
GENERATED AND PLACED IN THE ARRAY BETWEEN THE OBSERVED DEPTHSe IT
CALCULATES DELTA FOR OBSERVED DEPTHS AND INTERPOLATES DELTAS FOR
PAGE 088
STANDARD DEPTHS.
SUBROUTINES NEEDED-- SIGMAD.
ROBERT Ke SEXTON
NARRAGANSETT MARINE LABORATORY
UNIVERSITY OF RHODE ISLAND
KINGSTONs RHODE ISLAND 02881
SIGMA LANGUAGE -— FORTRAN IV-E
COMPUTER -— IBM 360/50
SUBROUTINE CALCULATES SIGMA-Ts DELTA» IN SITU SPECIFIC VOLUME AND
STANDARD WATER COLUMN SPECIFIC VOLUME FROM THE GIVEN CHLORINITYs TEM—
PERATURE AND DEPTHe THE EQUATIONS USED ARE THOSE CITED BY FOFONOFF IN
"THE SEA'» VOLe ls INTERSCIENCE PUBLISHER s NeYeos 19625 MeNe HILL» EDes
USING EQUATION (21)» PAGE 8, TO COMPUTE SIGMA ZERO, EQUATION (22) AND
THE QUANTITIES FOLLOWING EQUATION (24) TO COMPUTE SIGMA-T, AND USING
EQUATION (25) AND (26)s PAGE 10s TO COMPUTE SPECIFIC VOLUME.
ROBERT Ke SEXTON
NARRAGANSETT MARINE LABORATORY
UNIVERSITY OF RHODE ISLAND
KINGSTONs RHODE ISLAND 02881
SIGMAD LANGUAGE -— FORTRAN IV-E
COMPUTER - IBM 360/50
DOUBLE PRECISION VERSION OF 'SIGMA'.
ROBERT Ke SEXTON
NARRAGANSETT MARINE LABORATORY
UNIVERSITY OF RHODE ISLAND
KINGSTON» RHODE ISLAND 02881
DYNHT LANGUAGE — FORTRAN II
COMPUTER — GE 225
COMPUTES AN ARRAY OF DYNAMIC HEIGHTS (EXPRESSED IN DYNAMIC METERS) FOR
SPECIFIED ARRAYS OF PRESSURE AND SPECIFIC VOLUME ANOMALIESe AUTHOR--
JACQUELINE WEBSTER.
INFORMATION PROCESSING CENTER
WOODS HOLE OCEANOGRAPHIC INSTITUTION
WOODS HOLEs MASSe 02543
PEN LANGUAGE — FORTRAN II
COMPUTER - GE 225
COMPUTES POTENTIAL ENERGY ANOMALY» USING THE TRAPEZOIDAL RULE OF INTE-
GRATIONe PEN SUBROUTINE OCCUPIES 130(8) OR 88(10) LOCATIONS IN MEMO-
RYe AUTHOR-- -JACQUELINE WEBSTER.
INFORMATION PROCESSING CENTER
WOODS HOLE OCEANOGRAPHIC INSTITUTION
WOODS HOLE» MASSe 02543
VFREQ LANGUAGE — FORTRAN II
COMPUTER — GE 225
COMPUTES TABLES OF VAISALA FREQUENCY (RADIANS/SECe) AND IN SITU DENS—
ITY (GRAMS/CCe)s GIVEN TABLES OF DEPTH» TEMPERATURE» AND SALINITY AND
THE LATITUDE OF OBSERVATIONe AUTHOR-— He PERKINSe
INFORMATION PROCESSING CENTER
WOODS HOLE OCEANOGRAPHIC INSTITUTION
PAGE 089
WOODS HOLEs MASSe 02543
DYNAMIC HEIGHT CALCULATION LANGUAGE — FORTRAN II
COMPUTER — IBM 1620
INTEGRATES ONE STATION AT A TIME AND THEN PUNCHES THE VALUES IN ORDERe
THERE IS AN OPTION» UNDER SENSE SWITCH CONTROL,» OF USING THE CALCOMP
560 TO PLOT THE VALUE OF DYNAMIC HEIGHT AGAINST DEPTHe THE INPUT TO
THIS PROGRAM IS THE SAME AS THAT FOR THE OCEANOGRAPHIC DATA PROCESSING
PROGRAM FOR THE IeCeEeSe FORMAT
UNIVERSITY OF MIAMI
MARINE LABORATORY
COMPUTER CENTER
1 RICKENBACKER CAUSEWAY
VIRGINIA KEY» MIAMI» FLORIDA
OCEANOGRAPHIC DATA COMPUTATION LANGUAGE —- FORTRAN II
SEA
COMPUTER — IBM 709 AND
CDC 6400
COMPUTES SALINITY AND SIGMA-T FROM CHLORINITY AND TEMPERATURE INPUT
DATAs AND COMPUTES DISSOLVED OXYGEN AND OXYGEN SATURATION.
DEPARTMENT OF GEOLOGY
FLORIDA STATE UNIVERSITY
TALLAHASSEEs FLORIDA 32306
WATER DENSITY -—- THERMOSTERIC ANOMALY LANGUAGE - FORTRAN II
COMPUTER -— IBM 7094
SUBROUTINE COMPUTES SIGMA-T AND DELTA-T FROM MEASUREMENTS OF TEMPERA-
TURE AND CHLORINITYe SIGMA-T IS CALCULATED BY THE METHOD OF KNUDSEN.
DELTA-T IS COMPUTED BY DEFINITION FROM SIGMA-Te
HARVEY Ee WALTERS
CHESAPEAKE BAY INSTITUTE
THE JOHNS HOPKINS UNIVERSITY
CHARLES AND 34TH STe
BALTIMORE» MDe 21218
SYNOPTIC PROGRAM (UWMS-0980) LANGUAGE —- FORTRAN II
COMPUTER - IBM 7094-II/
7040 DCS AND
CDC 6400
(COPY ON FILE AT NODC)
REDUCES DATA FROM RAW SHIP-BOARD OBSERVATIONSe CORRECTS THERMOMETERS
AND COMPUTES THERMOMETRIC DEPTHS, WIRE ANGLE DEPTHS», SALINITIES FROM
BRIDGE READINGS» OXYGEN VALUES FROM TITRATIONSs THEN COMPUTES SIGMA-Ts
OXYGEN SATURATION PERCENT» AND APPARENT OXYGEN UTILUZATIONe CORE STO-
RAGE REQUIRED-- 255335 WORDS FOR MAIN PROGRAM» 2058 WORDS FOR SUBROUT-—
INESe REFe A 150 PAGE REPORT (UWMS-0980, APR 1967) AND TECHNICAL RE-
PORT NOs 181 (M67-85 JAN 1968)» BY EUGENE Ee COLLIASe THERE IS ALSO
A MORE LIMITED VERSION FOR THE IBM-11305 REVISED 1969 FOR THE CDC-
64006
He MACINTOSH, COMPUTER SERVICES
DEPARTMENT OF OCEANOGRAPHY
UNIVERSITY OF WASHINGTON
SEATTLE, WASH. 98105
INTERPOLATION PROGRAM (UWMS-0959) LANGUAGE — FORTRAN Iv
COMPUTER — CDC 6400
INTERPOLATES HYDROGRAPHIC DATA TO STANDARD DEPTHSs AND COMPUTES THE
PAGE 090
DYNAMIC QUANTITIESe THE INTERPOLATION METHOD TAKES AN AVERAGE OF THE
POINTS OBTAINED FROM TWO PARABOLIC FITS» CORE STORAGE NEEDED-- 32 K
WORDSe DOCUMENTATION-— USAGE INSTRUCTIONS» AN OLDER UNIVERSITY OF
WASHINGTON PROGRAM INTERPOLATION FOR OFFSHORE OCEANOGRAPHIC DATA'»s IN
FORTRAN IV FOR THE IBM 7094, IS IN THE LIBRARY FILE AT THE NODCe THIS
INTERPOLATES OCEAN STATION VARIABLES TO STANDARD DEPTHSs USING LA-
GRANGE SUBROUTINE, CALCULATES ERROR TERMS FOR INTERPOLATIONSs COMPUTES
SIGMA-T» SPECIFIC VOLUME ANOMALYs DYNAMIC DEPTHs AND POTENTIAL ENERGY.
THE DECK HAS ABOUT 1500 CARDS» INCLUDING TWO FAP SUBROUTINES AND A BI-
NARY EDITOR PROGRAMe
UNIVERSITY OF WASHINGTON
DEPARTMENT OF OCEANOGRAPHY
22A OCEANOGRAPHY TEACHING BLDGe
ATTNe MRSe HELLA MACINTOSH
SEATTLE» WASHe 98105
OCEANOGRAPHIC REPORT PREPARATION LANGUAGE — FORTRAN IV
COMPUTER - IBM 360/65
INCLUDES CALCULATION OF SIGMA-T AND SPECIFIC VOLUME ANOMALY FOR OB-
SERVED POINTS» RATTRAY-TYPE LAGRANGE INTERPOLATION AND DYNAMIC DEPTH
CALCULATION AT STANDARD DEPTHS.
BUREAU OF COMMERCIAL FISHERIES BIOLOGICAL LABeo
ATTNe DRe Re Ae BARKLEY
PeO5o BOX 3830
HONOLULU» HAWAII 96812
OCCOMP LANGUAGE —- FORTRAN IV-H
COMPUTER - SDS SIGMA 7
COMPUTES VARIOUS OCEANOGRAPHIC PARAMETERS FROM NODC FORMAT STATION DA-
TA CARDSe OUTPUT IS ON LINE PRINTERe PROGRAM REQUIRES CORE STORAGE
OF 12752 WORDS.
INFORMATION PROCESSING CENTER
ATTNe MARY HUNT
WOODS HOLE OCEANOGRAPHIC INSTITUTION
WOODS HOLEs MASSACHUSETTS 02543
POTEMPs DPOTEM LANGUAGE - FORTRAN IV-H
COMPUTER -— SDS SIGMA 7
(COPY ON FILE AT NODC)
SUBROTUINE COMPUTES THE POTENTIAL TEMPERATURE OF SEA WATER AT A GIVEN
TEMPERATURE» SALINITY AND PRESSURE USING A FORMULA OF NePe FOFONOFF
AND Ce FROESE IN THE PeOQeGe MS REPORT SERIES NOe 27e WRITTEN IN FOR-
TRAN II FOR THE GE 225 BY Je WEBSTERe CONVERTED TO FORTRAN IV-H BY
Me HUNT (APRIL 1968)e DPOTEM IS A FORM OF POTEMP USING DOUBLE PRECIS-—
ION VARIABLES» STORAGE REQUIREMENTS—- 137(10) LOCATIONS FOR POTEMP>s
116(10) LOCATIONS FOR DPOTEMe
INFORMATION PROCESSING CENTER
ATTNe MARY HUNT
WOODS HOLE OCEANOGRAPHIC INSTITUTION
WOODS HOLEs MASSACHUSETTS 02543
SIGMAT»s DSIGMT LANGUAGE -— FORTRAN IV-H
COMPUTER - SDS SIGMA 7
SUBROUTINE COMPUTES SIGMA-T FROM TEMPERATURE AND SALINITY BY KNUDSEN#S
FORMULA REWRITTEN BY FOFONOFF AND TABATAs DSIGMT IS DOUBLE-PRECISION
FORM OF SIGMATe
INFORMATION PROCESSING CENTER
ATTNe MARY HUNT
PAGE O91
WOODS HOLE OCEANOGRAPHIC INSTITUTION
WOODS HOLEs MASSACHUSETTS 02543
SPVOL» DSPVOL LANGUAGE - FORTRAN IV-H
COMPUTER -— SDS SIGMA 7
SUBROUTINE COMPUTES THE SPECIFIC VOLUME OF SEAWATER AT A GIVEN TEMPER-
ATURE» PRESSURE» SIGMA-O AND SIGMA-Ts USING THE FORMULA BY VeWe EKMANs
REWRITTEN BY FOFONOFF AND TABALA (PeQ+eGe MANUSCRIPT SERIES NOe 25)¢
DSPVOL IS A FORM OF SPVOL USING DOUBLE-PRECISION VARIABLESe 'tALPHA',s
THE OUTPUT FROM THE SUBROUTINE» IS THE SPECIFIC VOLUME IN MILLILITRES
PER GRAM. THE USE OF SUBROUTINE SIGMAT WOULD BE REQUIRED BEFORE CALL-
ING SPVOL»s AND DSIGMT WOULD BE REQUIRED BEFORE CALLING DSPVOLe STOR-
AGE REQUIREMENTS—-- 239(10) LOCATIONS FOR SPVOLs 204(10) LOCATIONS FOR
DSPVOLe WRITTEN IN FORTRAN II FOR THE GE 225 BY Je WEBSTER» CONVERTED
TO FORTRAN IV-H BY Me HUNT (APRIL 1968).e
INFORMATION PROCESSING CENTER
ATTNe MARY HUNT
WOODS HOLE OCEANOGRAPHIC INSTITUTION
WOODS HOLE, MASSACHUSETTS 02543
ATG LANGUAGE -— FORTRAN IV-H
COMPUTER - SDS SIGMA 7
CALCULATES ADIABATIC TEMPERATURE GRADIENT FOR SPECIFIED VALUES OF
PRESSUREs TEMPERATURE» AND SALINITY,» USING AN EMPIRICAL FORMULA DEVEL—
OPED BY NePe FOFONOFFe (PROGRAM WRITTEN AS SUBROUTINE e)
INFORMATION PROCESSING CENTER
ATTNe MARY HUNT
WOODS HOLE OCEANOGRAPHIC INSTITUTION
WOODS HOLE», MASSACHUSETTS 02543
FORTRAN IV-H
SDS SIGMA 7
DSTABF LANGUAGE
COMPUTER
SUBROUTINE COMPUTES STABILITY FREQUENCY FROM HYDROGRAPHIC STATION DA-
TAs ACCORDING TO A RELATIONSHIP DERIVED BY HESSELBERG AND SVERDRUPe
INFORMATION PROCESSING CENTER
ATTNe MARY HUNT
WOODS HOLE OCEANOGRAPHIC INSTITUTION
WOODS HOLE, MASSACHUSETTS 02543
SVANOM LANGUAGE - FORTRAN IV-H
COMPUTER - SDS SIGMA 7
SUBROUTINE COMPUTES THE SPECIFIC VOLUME ANOMALY, GIVEN THE PRESSURE
AND THE SPECIFIC VOLUME, FROM AN EMPIRICAL FORMULA DEVISED By FOFONOFF
AND TABATA.
INFORMATION PROCESSING CENTER
ATTNe MARY HUNT
WOODS HOLE OCEANOGRAPHIC INSTITUTION
WOODS HOLEs MASSACHUSETTS 02543
PRESS LANGUAGE -— FORTRAN IV-H
COMPUTER — SDS SIGMA 7
SUBROUTINE COMPUTES A SERIES OF PRESSURES FROM A GIVEN SERIES OF
DEPTHS» TEMPERATURES» SALINITIES, AND THEIR LATITUDEe THE EQUATION
FOR PRESSURE IS INTEGRATED BY SUCCESSIVE APPROXIMATIONS e
PAGE 092
INFORMATION PROCESSING CENTER
ATTNe MARY HUNT
WOODS HOLE OCEANOGRAPHIC INSTITUTION
WOODS HOLE, MASSACHUSETTS 02543
DELTA-ALPHA AND SIGMA-T LANGUAGE -— MAC
GOMP.UTERG—) Gi S130
CALCULATES DELTA-ALPHA AND SIGMA-T AS A FUNCTION OF SALINITY» TEMPERA-—
TUREs AND DEPTHe AUTHORS-- AeMe SHIPLEY AND De SACKS
UNIVERSITY OF CAPE TOWN
OCEANOGRAPHY DEPARTMENT
ATTNe MRe AeMe SHIPLEY
PRIVATE BAGs RONDEBOSCH»s CePe
REPUBLIC OF SOUTH AFRICA
DYNAMIC HEIGHT AND CURRENT DYNAMICS LANGUAGE — MAD
COMPUTER - IBM 7090
COMPUTES DYNAMIC HEIGHT,» VOLUME TRANSPORT» AND NORMAL VELOCITY FOR
FRESH WATERe
VINCENT NOBLE
THE UNIVERSITY OF MICHIGAN
GREAT LAKES RESEARCH DIVISION
INSTITUTE OF SCIENCE AND TECHNOLOGY
1077 NORTH UNIVERSITY BUILDING
ANN ARBOR» MICHIGAN 48104
OCEANOGRAPHIC ANALYSIS AND STATION SUMMARY LANGUAGE — PAL ITI
GOMEUTERT— PDS Songs)
FORMATS AND RECORDS OCEANOGRAPHIC DATA INCLUDING SURFACE ENVIRONMENTAL
PHENOMENA, COMPUTES SIGMA-T, THE ANOMALY OF SPECIFIC VOLUME» AND SOUND
VELOCITY AT OBSERVED VALUES OF DEPTH-TEMPERATURE-SALINITYe COMPUTES
SIGMA-T AND ANOMALY OF SPECIFIC VOLUME FROM SCALED VALUES OF TEMPERA-—
TURE AND SALINITY» THE RESULTS OF A LAGRANGIAN INTERPOLATIONe DOES A
DEPTH INTEGRATION OF ANOMALY OF SPECIFIC VOLUME FROM THE OBSERVED OR
SCALED VALUES IN ORDER TO CALCULATE THE DYNAMIC HEIGHT FROM A LEVEL OF
NO-MOTIONe PRINCIPALLY USED ABOARD OCEANOGRAPHIC VESSEL BY THE FIELD
OCEANOGRAPHER IMMEDIATELY AFTER STATIONe WRITTEN FOR THE UeSe COAST
GUARD BY LTe ReMe O'HAGAN (RETe)s DIGITAL EQUIPMENT CORPe,s MAYNARD»
MASSe COPY OF PROGRAM DEPOSITED WITH DECUSe REFe UeSe COAST GUARD
OCEANOGRAPHIC MANUSCRIPT 'OCEANOGRAPHIC COMPUTER PROGRAMS FOR THE PDP-
5's 15 OCT. 1964 (UNPUBLISHED MANUSCRIPT)e« PROGRAM REVISED IN 19656
DIGITAL EQUIPMENT CORPORATION
MAYNARD» MASSACHUSETTS 01754
DISSOLVED OXYGEN AND POTENTIAL TEMPERATURE LANGUAGE - PAL III
COMPUTER -— PDP-5»5 8S
CALCULATES DISSOLVED OXYGEN FROM A GIVEN THIOSULPHATE TITERe CALCUL—
ATES PERCENT SATURATION OF OXYGEN (FOX'S FORMULAE)» CALCULATES POTEN-
TIAL TEMPERATUREe ASR-33 TELEPRINTER INPUT-OUTPUTe PROGRAM PRINCI-
PALLY USED ABOARD OCEANOGRAPHIC VESSELe WRITTEN FOR THE UeSe COAST
GUARD BY LTe ReMe O'HAGAN (RETe)» DIGITAL EQUIPMENT CORPes MAYNARD»
MASSe COPY DEPOSITED WITH DECUS.
DIGITAL EQUIPMENT CORPORATION
MAYNARDs MASSACHUSETTS 01754
OCEAN STATION COMPUTATIONS LANGUAGE — (NOT GIVEN)
COMPUTER - CDC 1604
PAGE 093
INTERPOLATION AT STANDARD DEPTHS OF TEMPERATURE AND SALINITYs SIGMA-T
AND THE DYNAMICS COMPUTATIONSe»
SCRIPPS INSTITUTION OF OCEANOGRAPHY
LA JOLLA» CALIFORNIA 92037
RADIATION ATTENUATION LANGUAGE — (NOT GIVEN)
COMPUTER — CDC 1604
COMPUTATION OF THE ATTENUATION COEFFICIENTS FROM SUBMARINE IRRADIANCE
MEASUREMENTS.
SCRIPPS INSTITUTION OF OCEANOGRAPHY
LA JOLLA» CALIFORNIA 92037
#-%-% SOUND — RAY PATH *-*-—*
ACOUSTIC RAY TRACING LANGUAGE — FORTRAN II
COMPUTER -— IBM 7090
(COPY ON FILE AT NODC)
CALCULATES UNDERWATER SOUND PROPAGATIONe PROGRAM REQUIRES INPUT WHICH
DESCRIBES THE SOURCEs THE FIELD» THE SURFACE AND THE BOTTOMe OUTPUT
IS A REPORT ON MAGNETIC TAPE WHICH GIVES RAY PATHs SLOPE» CURVATURE9s
AND LENGTH. ALSO GIVEN ARE REFLECTION AND EXTREMA STATISTICS» TRAVEL
TIMEs WAVE FRONT CURVATUREs AND INTENSITYe PROGRAM AND DOCUMENTATION
PUBLISHED IN ARTHUR De LITTLE» INCe TECHNICAL REPORT NOco 1470764e THE
AeDe NOe IS AD 605 328e ALSO AVAILABLE FROM THE DEFENSE DOCUMENTATION
CENTERe
MISS MARIAN Le HOBBSs LIBRARIAN
TRIDENT/ASW LIBRARY
ARTHUR De LITTLE s INCeo
35 ACORN PARK
CAMBRIDGE» MASS. 02140
TRLOSS LANGUAGE — FORTRAN
COMPUTER -— CDC 6600
COMPUTES LONG-RANGE TRANSMISSION LOSS BY PROBABILISTIC METHODS, USING
A STATISTICAL APPROXIMATION TO RAY-TRACINGe INPUT-- PUNCHED CARDS
CONTAINING VELOCITY PROFILES» BOTTOMs TOPOGRAPHY (ROUGH) AND TARGET
RANGES» OUTPUT-- LISTS OF INTENSITIES (RELATIVE TO SOURCE INTENSITY)
AS FUNCTIONS OF DEPTH AT EACH OF THE TARGET RANGESe CORE STORAGE NEC-—
ESSARY-- 30(8)K WORDSe AUTHOR-- MISS ELLEN WILLIAMS.
MARTIAN Le HOBBS» LIBRARIAN
ARTHUR De LITTLE» INC
ACORN PARK
CAMBRIDGEs MASSe 02140
SONAR IN REFRACTIVE WATER LANGUAGE -— FORTRAN IV
COMPUTER — UNIVAC 1108
(COPY ON FILE AT NODC)
TRACES SOUND RAYS» COMPUTES REVERBERATION, COMPUTES ACQUISITION LAMIN-
AE (VERTICAL PLANE)» IN A LINEAR-GRADIENT OR CONTINUOUS-GRADIENT MEDI-
UMe CORE STORAGE USED-- APPROXe 30,000 WORDSe SUPERSEDES ALL PREVI-
OUS VERSIONS OF THE PROGRAM. DOCUMENTED AS NUC TECHNICAL PUBLICATION
NOs 164 (VOLel» 196 P AND VOLe2s 356 P) 'DIGITAL COMPUTER PROGRAMS FOR
ANALYZING ACOUSTIC SEARCH PERFORMANCE IN REFRACTIVE WATERS'» NUC PRO-
GRAMS 800000 AND 800001, BY PHILIP MARSH AND AeBe POYNTER» ORUVNANCE
SYSTEMS DEPARTMENT, DECEMBER 1969-6 (DOCUMENTS UNCLASSIFIED BUT TRANS-
PAGE 094
MITTALS CONTROLLED BY NUCe)
NAVAL UNDERSEA RESEARCH AND DEVELOPMENT CENTER
PASADENA LABORATORY
ATTNe PHILIP MARSH
3202 Ee FOOTHILL BLVD.
PASADENA» CALIFe 91107
RAY SORT LANGUAGE - FORTRAN IV
COMPUTER - UNIVAC 1108
(COPY ON FILE AT NODC)
SORTS CERTAIN SOUND RAY DATA (FROM TAPE WRITTEN BY THE 'SONAR IN RE-
FRACTIVE WATER* PROGRAM) BY DEPTHs INITIAL RAY ANGLE, AND DEPTH-INTER-
SECTION NUMBERe SOURCE PROGRAM HAS 450 INSTRUCTIONSe CORE STORAGE--
ABOUT 312000 WORDSe DOCUMENTED AS NUC TECHNICAL PUBLICATION NOo 164
(VOLel» 196 P AND VOLe2, 356 P) *DIGITAL COMPUTER PROGRAMS FOR ANALY—
ZING ACOUSTIC SEARCH PERFORMANCE IN REFRACTIVE WATERS» NUC PROGRAMS
800000 AND 800001, BY PHILIP MARSH AND AeBe POYNTERs ORDNANCE SYSTEMS
DEPARTMENT» DECEMBER 1969¢ (DOCUMENTS UNCLASSIFIED BUT TRANSMITTAIS
CONTROLLED BY NUCe)
NAVAL UNDERSEA RESEARCH AND DEVELOPMENT CENTER
PASADENA LABORATORY
ATTNe PHILIP MARSH
3202 Ee FOOTHILL BLVDe
PASADENAs CALIFe 91107
RAYMOR LANGUAGE — FORTRAN V
COMPUTER - UNIVAC 1108
(COPY ON FILE AT NODC)
COMPUTES RAYLEIGH-MORSE BOTTOM REFLECTION COEFFICIENTS» ALSO PHASE
CHANGES OF THE REFLECTED AND TRANSMITTED ACOUSTIC WAVEe AUTHOR--
JeCe REEVES.
NAVAL UNDERSEA RESEARCH AND DEVELOPMENT CENTER
PASADENA LABORATORY
3202 Ee FOOTHILL BOULEVARD
PASADENAs CALIFORNIA 91107
NEWFIT LANGUAGE - FORTRAN V
COMPUTER — UNIVAC 1108
(COPY ON FILE AT NODC)
FITS A VELOCITY PROFILE WITH A SERIES OF CURVE SEGMENTS HAVING CONTIN-
UOUS FIRST DERIVATIVES AT POINTS OF INTERSECTIONe OUTPUT-= PRINTED
LISTINGS OF ORIGINAL DATAs FITTED DATAs AND COEFFICIENTS OF CURVE SEG-
MENTS —- ALSO CARDS FOR INPUT TO *#SONAR IN REFRACTIVE WATER! PROGRAMe
NEWFIT IS THE MAIN ROUTINE OF THE NEW CURVE FITTING PROGRAMe A REPORT
AP-PROG-C-8070 (FEB 19685 98 P)» BY MELVIN Oe BROWNs DOCUMENTS THE DE-
TAILS OF THE ENTIRE PROGRAMe CORE STORAGE NECESSARY-- APPROXe 253000
WORDSs INCLUDING LIBRARY AND SYSTEM ROUTINES.
NAVAL UNDERSEA RESEARCH AND DEVELOPMENT CENTER
PASADENA LABORATORY
ATTNe PHILIP MARSH
3202 Ee FOOTHILL BLVDe
PASADENA» CALIFe 91107
PATTERN FUNCTION CALCULATIONS LANGUAGE -— FORTRAN IV
COMPUTER - UNIVAC 1108
(COPY ON FILE AT NODC)
COMPUTES TRANSDUCER PATTERN FUNCTIONS NEEDED IN THE SONAR EQUATIONS
WHEN ESTIMATING SEARCH PERFORMANCE OF ACOUSTIC TORPEDOESe THE DESIRED
PARAMETERS INCLUDE THE TRANSMIT AND RECEIVE DIRECTIVITY INDEXES AND
THE VOLUME AND BOUNDARY REVERBERATION INDEXESe IN A VEHICLE EMPLOYED
IN CIRCULAR SEARCHs THE REVERBERATION INDEXES ARE FUNCTIONS OF TURN
RATE AND ELAPSED TIME IN THE PING CYCLEe THE OUTPUT IS USED BY THE
PAGE 095
‘SONAR IN REFRACTIVE WATER! PROGRAMe THEORYs FLOW CHARTS» AND LISTING
GIVEN IN REPORT AP-PROG-C-7035 (APR 19675 80 P)s BY HERBERT Se KAPLANe
NAVAL UNDERSEA RESEARCH AND DEVELOPMENT CENTER
PASADENA LABORATORY
ATTNe PHILIP MARSH
3202 E5s FOOTHILL BLVDe
PASADENA» CALIFe 91107
HORIZONTAL GRADIENT RAY TRACING LANGUAGE - FORTRAN-63
RAY
COMPUTER - CDC 3800
DESCRIBES ACOUSTIC PATHS OF UP TO 1000 RAYS AS THEY PROGRESS THROUGH
THE OCEAN FROM A POINT SOURCE AT ARBITRARY RANGE AND DEPTHe ALL RAYS
ARE TRACED SIMULTANEOUSLY IN ONE PASS THROUGH THE VELOCITY FIELDe AS
THE RAYS ARE TRACED SEVERAL TYPES OF INTENSITY CALCULATIONS ARE PER-
FORMED AND A MULTIPLOT OF RAYS CONSTRUCTEDe BASIC INPUT CONSISTS OF A
MAGNETIC TAPE GENERATED BY THE 'GENERAL VELOCITY FIELD! PROGRAM. OUT-
PUT--— RANGES» DEPTHSs TRAVEL TIME» SINE OF ANGLE» NUMBER OF TURNING
POINTS» NUMBER OF SURFACE AND BOTTOM HITS» AND SIGNAL STRENGTH OF EACH
RAY AT RANGES SPECIFIED BY THE USER. ALSO» TYPE I» II» III INTENSI-
TIES» TRANSMISSION LOSS AND TRANSMISSION ANOMALYe BASIC IDEAS CON-
TAINED IN HUDSON LAB TECHNICAL REPORT NOe 150 (1968)+¢ PROGRAM DOCU-
MENTATION FORTHCOMINGe
Je Je CORNYN, CODE 8140
ACOUSTICS DIVISION
NAVAL RESEARCH LABORATORY
WASHINGTONs De Ce 20390
TRACING LANGUAGE - FORTRAN IV
COMPUTER - CDC 3800
CALCULATES RAY THEORY» ARRIVALS AND INTENSITIES AT A LARGE NUMBER OF
RECEIVERSe INPUT-- VELOCITY PROFILE EITHER AS V VSe Z OR T2S VSe Ze
ALSO SOURCE AND RECEIVER DEPTHS», INITIAL RAY ANGLES AND RECEIVER RAN-
GES, BEAM PATTERNS (IF ANY), BOTTOM LOSS TABLE, SURFACE LOSSs FREQUEN-
CYe OUTPUT-- LISTINGS AND PLOTSe EITHER COHERENT OR RANDOM PHASE
ARRIVAL SUMS ARE AVAILABLEe
EDWARD Le WRIGHT» CODE 8172
ACOUSTICS DIVISION
NAVAL RESEARCH LABORATORY
WASHINGTONs De Ceo 20390
ACOUSTIC RAY TRACING LANGUAGE — FORTRAN-63
RAY
COMPUTER -— CDC 3800
CALCULATES PATHS OF ACOUSTIC RAYS FROM A POINT SOURCE IN THE OCEAN?
THROUGH A SERIES OF SOUND SPEED PROFILES» ALONG WITH THEIR TRAVEL
TIMES AND TRANSMISSION LOSSESe REFLECTIONS OF THE RAYS FROM A LINEAR
SEGMENTED BOTTOM ARE CALCULATEDe COMPUTES CLOSED FORM PATH ELEMENTS
BETWEEN LAYER BOUNDARIES IN THE PROFILEe RAYS ARE TRACED SEQUENTIAL—
LYe PROGRAM WILL BE DOCUMENTED IN A FORTHCOMING REPORT e
Ee Be WRIGHT
CODE 8177s ACOUSTICS DIVISION
NAVAL RESEARCH LABORATORY
WASHINGTONs De Ce 20390
TRACE PROCESSING LANGUAGE -— FORTRAN-63
COMPUTER -— CDC 3800
USES OUTPUT OF RAY TRACING PROGRAM TO CALCULATE TRANSMISSION LOSS BY A
CHOICE OF THREE METHODS. LOSS AT RECEIVERS IS COMFUTED BY-- A) PHASE-
DEPENDENT RAY SUM, B) RANDOM—PHASE RAY SUMs C) STATISTICAL DISTRIBU-
PAGE 096
RAY
TION OF ARRIVALSe OUTPUT-— TRANSMISSION LOSS AS A FUNCTION OF RANGE
FOR UP TO 20 RECEIVER DEPTHS AND UP TO 200 RANGE INCREMENTS
Ee Be WRIGHT
CODE 8177» ACOUSTICS DIVISION
NAVAL RESEARCH LABORATORY
WASHINGTON»s De Ce 20390
TRACING LANGUAGE - FORTRAN AND
KLERER-MAY
USER |ILANGe
COMPUTER —- (NOT GIVEN)
(COPY ON FILE AT NODC)
A SERIES OF PROGRAMS FOR THE CALCULATION OF THE ACOUSTICAL FIELD IN
LONG-RANGE (SEVERAL HUNDRED TO SEVERAL THOUSAND MILES)» LOW FREQUENCY
UNDERWATER SOUND PROPAGATION IN THE DEEP OCEANe INVOLVES THE CALCULA-
TION OF RAY TRAJECTORIESs AND INTENSITY CALCULATIONS THAT ARE BASED ON
THE MAPPING OF RAY DENSITIES INTO THE FAR ACOUSTICAL FIELDe I/P FOR=
MAT FROM NODC DATA TAPES OR FLEET. NUMERICAL WEATHER CENTRAL CARDS.
REFe 'THE HUDSON LABORATORIES RAY TRACING PROGRAM! (JUNE 19689 363 P.)
AUTHORS-- He DAVISs He FLEMING» WeAe HARDYs Re MININGHAMs AND Se ROS-—
ENBAUMe
RAYTR (RAY-TRACING) LANGUAGE -— FORTRAN Iv
ORD
ORD
COMPUTER -— IBM 360/44
TRACES SOUND RAY PATHS IN A LAYERED FLUID MEDIUMe TRAVEL-TIMES»s REL-
ATIVE TRAVEL-TIMES» TOTAL PATH LENGTHS ALONG THE RAY, INTENSITIES AND
THE COORDINATES OF FOCI ARE ALSO COMPUTEDe THE PROGRAM IS SIMILAR IN
MANY RESPECTS TO HeWe DOSSOs ET AL "RAY TRACING WITH A PB-250'5 TECH.
MEMOe 63-11 (UNPUBLISHED). THE NUMBER OF ALLOWED SOUND-SPEED vS DEPTH
AND BOTTOM PROFILE DATA ENTRIES HAS BEEN INCREASED FROM 32 TO 3606
AUTHOR-- ReWe DE JEANe DESCRIBED IN TECHNICAL MEMO 68-55 FEB 19686
DEFENCE RESEARCH ESTABLISHMENT PACIFIC
VICTORIA» Be Ce CANADA
1 (OLMSTED RAY DIAGRAM PROGRAM NOe 1) LANGUAGE -— FORTRAN
COMPUTER — GE 225
CONSTRUCTS (OPTICAL/ACOUSTIC) RAYS IN A MEDIUM WHERE THE VELOCITY OF
LIGHT/SOUND VARIES CONTINUOUSLY WITH ONE COORDINATE (DEPTH)e THE RAYS
ARE CONFINED TO A RANGE-DEPTH PLANE OF FINITE DEPTH (A LAYER) AND MUST
ORIGINATE FROM A SOURCE PLACED AT ANY DEPTH IN THE LAYER AND AT ANGLES
OF INCIDENCE GREATER THAN O AND LESS THAN 180 DEGe WHEN A RAY REACHES
A VERTEX (OF REFRACTION OR REFLECTION) THE REMAINDER OF THE RAY IS
CONSTRUCTED BY SYMMETRY AND PERIODIC EXTENSION. POINTS ARE THEN COM-
PUTED ALONG THESE RAYS AT INTERVALS OF EQUAL RANGEe AUTHOR-- COERT
OLMSTED>s FEBe 1965-6
WOODS HOLE OCEANOGRAPHIC INSTITUTION
WOODS HOLE» MASSe 02543
2 (OLMSTED RAY DIAGRAM PROGRAM NOe 2) LANGUAGE - FORTRAN
GOMPUTERE IGEN 225
SERVES THE SAME PURPOSE AS ORD 1 EXCEPT THAT THE OUTPUT POINTS ARE AT
EQUAL TIME INCREMENTS RATHER THAN AT EQUAL RANGE INCREMENTS AND THUS,
WHEN PLOTTEDs WILL ENABLE ONE TO TRACE WAVE FRONTS AS WELL AS RAYSe
THERE TS NO SYMMETRICAL OR PERIODIC EXTENSIONe THE RAY PATH IS COM-
PUTED LOCALLY ALL THE WAY OUT TO MAXIMUM RANGEe AUTHOR-- COERT OLM-
STEDs FEBe 1965.
WOODS HOLE OCEANOGRAPHIC INSTITUTION
WOODS HOLEs MASSe 02543
PAGE 097
AN ACOUSTIC MODEL LANGUAGE — FORTRAN
COMPUTER — IBM 7074
PRESENTS A SOLUTION FOR THE RAYLEIGH REFLECTION COEFFICIENT WITH A
FOUR LAYER MODELe OS NOs 20118e¢ AUTHOR-- MeEe MYERS
COMPUTER DEPARTMENT» CODE 0831
NAVAL OCEANOGRAPHIC OFFICE
SUITLAND» MD. 20390
CRITICAL ACOUSTIC RATIO LANGUAGE — FORTRAN
COMPUTER -— IBM 7074
DETERMINATION OF CRITICAL RATIO OF TRIGONOMETRIC FUNCTIONS OF ACOUSTIC
ANGLES INVOLVED IN CONNECTION WITH THE CONVERGENCE INTERVAL FOR A 3-
LAYER MODEL OF THE OCEANe OS NOe 534836 AUTHOR-- CeMe WINGER.
OCEANOGRAPHIC PREDICTION DIVe, CODE 3400
NAVAL OCEANOGRAPHIC OFFICE
SUITLANDs MD. 20390
RAY PATH LANGUAGE - FORTRAN
COMPUTER -— IBM 7074
(COPY ON FILE AT NODC)
COMPUTES RANGES AND TRAVEL TIMES FOR SOUND RAYSe OS NOe 53810¢ AUTHOR
LeWe CISNEY.
EXPLORATORY OCEANOGRAPHY DIVes CODE 7200
NAVAL OCEANOGRAPHIC OFFICE
SUITLANDs MD. 20390
BOTTOM REFLECTION ANALYSIS LANGUAGE — FORTRAN
COMPUTER — IBM 7074
(COPY ON FILE AT NODC)
DETERMINES ENERGY LEVEL OF SOUND SOURCES AT CERTAIN DISCRETE FREQUEN-
CIES BY MEANS OF HARMONIC ANALYSISe OS NOe 538066¢ AUTHOR-- teWe CIS-—
NEY.
EXPLORATORY OCEANOGRAPHY DIVe»s CODE 7200
NAVAL OCEANOGRAPHIC OFFICE
SUITLAND» MD. 20390
CONVERGENCE ZONE RANGE LANGUAGE - FORTRAN
COMPUTER - IBM 7074
(COPY ON FILE AT NODC)
COMPUTES RANGES TO THE FIRST CONVERGENCE ZONEe THE WIDTH OF THE
RESWEPT AND INSONIFIED ZONES AND THE RELIABLE ACOUSTIC PATH RANGE
ARE ALSO COMPUTED. IN ADDITION: LAYER DEPTHs CHANNEL DEPTH», OPTIMUM
DEPTHs BOTTOM VELOCITYs AND DEPTH EXCESS ARE EXTRACTED AND LISTED
IN THE OUTPUT. INPUT EITHER CARD OR TAPE’ OS NOe 53334-¢ (RESTRICTED)
AUTHOR-— Re BUTTERWORTH.
OCEANOGRAPHIC ANALYSIS DIVe»s CODE 3300
NAVAL OCEANOGRAPHIC OFFICE
SUITLAND>s MD. 20390
LIGHT AND SOUND INSTRUCTION D LANGUAGE — FORTRAN
COMPUTER -— IBM 7074
(COPY ON FILE AT NODC)
COMPUTES THE CONVERGENCE ZONE PARAMETERS USING THE V(X) METHOUV (EQUA-
TIONS OF DONALD COLE)» BY ONE-DEGREE QUADRANGLE, BY MONTH AND By SEA-
SONe AUTHOR-- MeCe CHURCH.
PAGE 098
RAY
COMPUTER DEPARTMENT» CODE 083
NAVAL OCEANOGRAPHIC OFFICE
SUITLAND» MDe 20390
TRACING LANGUAGE - FORTRAN II
COMPUTER - IBM 704
(COPY ON FILE AT NODC)
COMPUTES HORIZONTAL RANGEs TRAVEL TIME» AND SPREADING LOSS THROUGH A
MEDIUM CONSISTING OF LAYERS OF CONSTANT VELOCITY GRADIENT (THE v(x)
METHOD OF DONALD COLE)e A PRINTED OUTPUT CONTAINS LAYERED INFORMA-
TIONe OPTION TO WRITE A PLOTTER TAPE FOR USE ON THE EAI 3440 DIGITAL
PLOTTERe REFe USL TECHe MEMORANDUM NOco 907-78-66 (APRIL 1966)
PAULINE ONYX
NAVY UNDERWATER SOUND LABORATORY:s BLDGe 80
FORT TRUMBULL» NEW LONDON» CONNe 06320
BOTTOM REFLECTIVITY LANGUAGE — FORTRAN II
COMPUTER — IBM 704
(COPY ON FILE AT NODC)
TWO
USL PROGRAM NOe 028956 COMPUTES THREE ACOUSTIC REFLECTION COEFFICIENTS
AS A FUNCTION OF INCIDENT ANGLE AND FREQUENCYe THE PROGRAM ACCOUNTS
FOR DIFFERENCE IN PATH LENGTHs DEPTH OF SOURCE AND RECEIVERS» WATER»
BOTTOM SLOPEs VELOCITY GRADIENT AND RECORDED TRAVEL TIMEs REFe USL
TECHe MEMORANDUMS NOSe 913-4-65 AND 907-144-65. THE LATTER REPORT
ALSO SERVES TO DOCUMENT A SUPPLEMENTAL COMPUTER PROGRAM (USL NOe 0427,
IN FORTRAN) FOR COMPUTING MEANS AND STANDARD DEVIATIONS OF THE THREE
REFLECTION COEFFICIENTS.
Re WHITTAKER
NAVY UNDERWATER SOUND LABORATORY» BLDGe 80
FORT TRUMBULL» NEW LONDON», CONNe 06320
DIMENSIONAL RAY TRACE LANGUAGE — SCRAP» MAP
COMPUTER - CDC 1604 AND
CDC 3200
DESCRIBES THE PATH OF SOUND EMITTED FROM A POINT SOURCE AS IT PROGRES-
SES THROUGH THE OCEAN IN ONE HORIZONTAL DIRECTIONs TAKING INTO CONSID-
ERATION BOTH HORIZONTAL AND VERTICAL VARIATION IN THE SOUND VELOCITY
OF THE OCEANe ONE PATH IS TRACED FOR EACH SPECIFIED INITIAL ANGLE
FROM THE HORIZONTALe BEHAVIOR OF RAY PATH IS CONTROLLED BY SOUND VEL-
OCITY GRADIENTS— CORRECTION FOR EARTH CURVATURE IS ADDEDe OUTPUT IS A
PRINTED LIST AND ALSO IN BINARY FORMAT SUITABLE FOR ADAPTATION TO A
PLOTTERe DIRECT INQUIRIES FOR INFORMATION TO-—
COMMANDING OFFICER
FLEET NUMERICAL WEATHER CENTRAL
NAVAL POSTGRADUATE SCHOOL
MONTEREY» CALIFORNIA 93940
THESIS3 (SONOBUOY FIXING ERROR) LANGUAGE — FORTRAN
COMPUTER -— (NOT GIVEN)
CALCULATES THE EFFECTS OF HORIZONTAL VELOCITY GRADIENTS IN SEA WATER
WHEN OBTAINING A FIX ON A TARGET BY TWO PASSIVE DIRECTIONAL SENSORS.
THESIS BY JAMES We PIGMAN (MAY 1966).
NAVAL POSTGRADUATE SCHOOL
MONTEREYs CALIFORNIA 93940
NEAR-FIELD ARRAY TESTING LANGUAGE — FORTRAN
COMPUTER — PDP-8
PROGRAM INVESTIGATES THEORETICALLY THE EFFECT OF IRREGULARITIES IN THE
PAGE 099
POSITIONS OF TRANSDUCER ELEMENTS IN AN ACOUSTIC 'NEAR-FIELD! ARRAYe
REPORT NOe NRL-6728 (MAY 1968» 40P) BY GERALD Ae SABINe DDC NO-~ IS
AD-669-449,.
UNDERWATER SOUND REFERENCE DIVe
NAVAL RESEARCH LABORATORY
ORLANDO», FLORIDA
*¥-*-* SOUND -— NORMAL MODES *-*-*
NORMAL MODE SOLUTIONS FOR SOUND SPEED PROFILES LANGUAGE -— FORTRAN IV
COMPUTER - CDC 3800
PROVIDES A NORMAL MODE SOLUTION OF THE WAVE EQUATION WITH THE SOUND
SPEED PROFILE FOR THE MEDIUM REPRESENTED BY A S€T OF DISCRETE VALUES.
THE SEA BOTTOM IS ASSUMED TO BE A SEMI-INFINITE FLUID, SPECIFIED BY A
CONSTANT DENSITY AND A CONSTANT SPEED OF SOUND AND WITH NO ATTENUA-
TIONe THE INTERFACE BETWEEN THE WATER COLUMN AND THE BOTTOM IS FLAT
AND LEVELe USER SELECTS THE MAXIMUM NUMBER OF MODES DESIREDe OUTPUT—
— THE NORMALIZED EIGENFUNCTIONS OR MODE SHAPES ARE OBTAINED FROM THE
EIGENVALUES AND PLOTTEDe THE GROUP VELOCITY CHARACTERISTIC IS OB-
TAINED OVER A RANGE OF FREQUENCIES AND TABULATEDe PROPAGATION LOSS IS
PLOTTED AS A FUNCTION OF RANGEe DOCUMENTATION WILL BE IN A FORTH-
COMING NRL REPORTe
JOHN CYBULSKI
CODE 8177s ACOUSTICS DIVISION
NAVAL RESEARCH LABORATORY
WASHINGTONs De Ce 20390
PROPAGATION LOSS — NORMAL MODES LANGUAGE — FORTRAN
COMPUTER - CDC 3800
CALCULATES UNDERWATER SOUND PROPAGATION IN A HORIZONTALLY STRATIFIED
MEDIUMe THE PROGRAM CALCULATES A SET OF HORIZONTAL PHASE VELOCITIES
FOR THE NORMAL MODES AND THEN SERIES THE MODE AMPLITUDE FUNCTIONS TO
FIND THE SOUND LEVELSe INPUT-- SOUND VELOCITY PROFILE» SOURCE DEPTH,
POSITION OF RECEIVERS IN RANGE AND DEPTHs SURFACE LOSS» AND BOTTOM
LOSS TABLE. OUTPUT-- PROPAGATION LOSS AT THE VARIOUS RECEIVERS»e PRO-
CEDURE-- APPROXIMATE VALUES OF THE HORIZONTAL PHASE VELOCITY ARE CAL-
CULATED USING RAY THEORY» EXACT VALUES ARE FOUND BY ITERATING IN THE
COMPLEX PLANEe SOUND INTENSITIES ARE CALCULATED BY FORMING THE SERIES
OF NORMAL AMPLITUDE FUNCTIONSe DOCUMENTATION-— FORTHCOMING NRL REPORT
DRe He Pe BUCKER»s JRe
CODE 8170
NAVAL RESEARCH LABORATORY
WASHINGTONs De Co 20390
#-#%-% SOUND - SPEED COMPUTATIONS *-*-*
SOUND VELOCITY LANGUAGE — FORTRAN
COMPUTER = ED.Gs3 2.0/0
(COPY ON FILE AT NODC)
COMPUTES SOUND VELOCITY USING WILSON'S EQUATIONSe OUTPUT CARDS HAVE
VELOCITY OF SOUND IN METERS/SECs PRESSURE IN KG/SQ-CMs SIGMA-T, IN
ADDITION TO INPUT STATION DATA AND IDENTIFICATION’
NAVAL UNDERWATER WEAPONS RESEARCH
PAGE 100
AND ENGINEERING STATION
NEWPORT» RHODE ISLAND 02840
FATHOMETER CORRECTION LANGUAGE — FORTRAN
COMPUTER — CDC 1604
(COPY ON FILE AT NODC)
CORRECTS ECHO SOUNDER READINGS BY COMPUTING ACTUAL TRAVEL TIME FROM A
LINEAR SEGMENT VELOCITY PROFILEe INPUT-- DEPTH VSe VELOCITY POINTS ON
CARDSe OUTPUT IS PRINTED LIST OF ACTUAL DEPTHSs FATHOMETER DEPTHS AND
CORRECTIONS (FATHOMS)e A SUBROUTINE FOR THE CALCOMP PLOTS DIFFERENCES
VSe ECHO SOUNDER DEPTHSe CORE STORAGE USED-- 41006
COMMANDER
NAVAL UNDERSEA RESEARCH AND DEVELOPMENT CENTER
ATTNe De Fe GORDON
SAN DIEGO» CALIFORNIA 92132
GENERAL VELOCITY FIELD LANGUAGE — FORTRAN-63
COMPUTER -— CDC 3800»
DRUM SCOPE
GIVEN A SERIES OF INCOMPLETE VELOCITY PROFILES ALONG A RANGE TRACK THE
PROGRAM EXTRAPOLATES THE DEEP PROFILES TO THE BOTTOM USING WILSON'S
EQUATION AND INTERPOLATES BETWEEN THE DEEP PROFILES IN ORDER TO EXTEND
THE SHALLOW PROFILESe THE RESULT IS A COMPLETE DESCRIPTION OF THE
VELOCITY FIELD OVER THE RANGE-DEPTH PLANEe OUTPUT FROM PROGRAM IN-
CLUDES-- VELOCITYs GRADIENT» AND CURVATURE AT DEPTHS AND RANGES SPECI-
FIED BY USERs A CALCOMP CONTOUR PLOT OF SPECIFIED VELOCITY FIELD» AND
A 3-DIMENSIONAL PLOT OF VELOCITY VSe RANGE AND DEPTHe STORAGE NECES—
SARY-- 1175450 OCTAL WORDS OF CORE AND 2 CDC-863 DRUMSe
Je Je CORNYNs CODE 8140
ACOUSTICS DIVISION
NAVAL RESEARCH LABORATORY» WASHINGTON» De Ce 20390
SVLIM LANGUAGE - FORTRAN II
COMPUTER - CDC 3100
(COPY ON FILE AT NODC)
EXAMPLE OF 'LIMITS*' RETRIEVAL FUNCTIONS USED TO EXTRACT SOUND VELOCITY
PROFILESe THE PROGRAM READS CONTROL CARDS SPECIFYING GEOGRAPHICAL AND
SEASONAL LIMITS OF INTEREST» SCANS A COMPACTED NODC FORMAT FILE FOR
OCEAN STATIONS FALLING WITHIN THE SELECTED LIMITS» CONVERTS THE PRO-
FILE FROM METERS/SEC TO FEET/SEC AND PRINTS THE PROFILEe REFe INFORM-—
AL REPORT IR NOe 69-595 JULY 19696 AUTHOR-- WALT YERGENs EXPLORATORY
OCEANOGRAPHY DIVISION» CODE 7240. FURTHER INFORMATION MAY BE OBTAINED
FROM THE DISSEMINATION DEPARTMENT CODE 445 OR THE AUTHOR.
NAVAL OCEANOGRAPHIC OFFICE
SUITLANDs MARYLAND 20390
DETERMINATION OF POSSIBLE MAGNITUTE OF LANGUAGE -— FORTRAN
ERROR IN VERTICAL SOUND VELOCITY COMPUTER - IBM 7074
(COPY ON FILE AT NODC)
PROGRAM REQUESTED BY THE COAST AND GEODETIC SURVEY TO CORRECT FATHOM-—
ETER READINGSe PROVIDES-- (1) HARMONIC MEAN OF SOUND VELOCITY IN M/
SEC AT CHOSEN DEPTHS (2) MEAN VERTICAL SV AT ABOVE DEPTHS WITHIN ONE
MARSDEN SQe (3) VARIANCE OF 2 (4) DIFFERENCE BETWEEN STANDARD AND COM-—
PUTED SVs TESTED AGAINST GIVEN ALLOWABLE ERROR VALUES (5) NUMBER OF
STATIONS USED AT EACH DEPTH WITHIN EACH MARSDEN SQe INPUT MUST BE IN
NODC FORMAT TAPEs ZONE-EDITEDs IN DEPTH SEQUENCE AND SORTED ON MARSDEN
SQUARESe AUTHOR-- RUDI SAENGERe OS NOe 52203.
COMPUTER SYSTEMS DIVISION
NATIONAL OCEANOGRAPHIC DATA CENTER
WASHINGTONs De Ce 20390
PAGE 101
LIGHT AND SOUND INSTRUCTION B LANGUAGE — FORTRAN
COMPUTER — IBM 7074
COMPUTES THE HARMONIC MEAN SOUND VELOCITYs TRAVEL TIME» AND CORRECTION
RATIO AT 100-FATHOM DEPTH INTERVALS BY ONE-DEGREE SQUAREe OS NOe —
20111. AUTHOR-- MeCe CHURCH.
COMPUTER DEPARTMENT s CODE 083
NAVAL OCEANOGRAPHIC OFFICE
SUITLAND» MD. 20390
VELOCITY OF SOUND IN SEA WATER LANGUAGE — FORTRAN
COMPUTER -— IBM 1620
(COPY ON FILE AT NODC)
COMPUTES ONE PAGE AT A TIME FOR A GIVEN DEPTH AND A GIVEN SET OF 10
SALINITIES AND TEMPERATURES. A TABLE OF PRESSURES IS READ IN AND CON-
VERTED TO DEPTHSe USES LATER VERSION OF WILSON'S FORMULA FOUND IN THE
JASA VOL. 32 NO. 10 (1960).
ESSAs COAST AND GEODETIC SURVEY
WASHINGTON SCIENCE CENTER» BLDGe 2
ROCKVILLE» MDe 20852
WATERVEL LANGUAGE - FORTRAN AND
BINARY
COMPUTER - (NOT GIVEN)
(COPY ON FILE AT NODC)
COMPUTES SOUND VELOCITY AFTER WILSON (1960-2), SOUNDING VELOCITY, RE-
FLECTION TIMEe VALUES INTERPOLATED FROM STANDARD DEPTHSe UNITS CON-
VERSION ENGLISH TO METRICe AUTHOR-- HELEN KIRKe
SCRIPPS INSTITUTION OF OCEANOGRAPHY
ATTNe GeGe SHOR
LA JOLLA» CALIFe 92038
FUNCTION SDVEL LANGUAGE — FORTRAN
COMPUTER — IBM 1800 SYS
(COPY ON FILE AT NODC)
SUBPROGRAM COMPUTES SOUND VELOCITY IN SEA WATER FROM TEMPERATURE» SAL-—
INITY AND PRESSURE USING WILSON'S FORMULAEe A CONVERSION OF PRESSURE
IS MADE FROM NEWTONS/SQ METRE TO KGF/CM SQe
NATIONAL INSTITUTE OF OCEANOGRAPHY
WORMLEY»s GODALMING»s SURREY
ENGLAND
SOUND VELOCITY IN OCEAN WATER LANGUAGE -— FORTRAN II
COMPUTER - 18M 704
(COPY ON FILE AT NODC)
USL PROGRAM NOs 02406 COMPUTES SOUND VELOCITY AS A FUNCTION OF DEPTHs
TEMPERATURE» SALINITY AND LATITUDE» EQUATIONS USED WERE OBTAINED FROM
AN NEL PUBLICATION (MeAe PEDERSEN» ET ALs 1962)2¢ A PRINTED OUTPUT HAS
THE INPUT PARAMETERS AND THE COMPUTED VALUES OF SOUND VELOCITY, PRESS-
URE» AND DENSITY (RHO) FOR EACH DEPTH. REFe USL TECHe MEMORANDUM NO.
907-94-66 (MAY, 1966).
Me Je GOLDSTEIN
NAVY UNDERWATER SOUND LABORATORY» BLDG. 80
FORT TRUMBULL» NEW LONDON» CONN. 06320
SDGVEL (SOUNDING CORRECTION) LANGUAGE — FORTRAN IV
COMPUTER — IBM 7094-IT/
7040 DCS
(COPY ON FILE AT NODC)
PAGE 102
CORRECTS OBSERVED DEPTHS FOR LATITUDINAL AND LONGITUDINAL VARIATION IN
SOUNDING VELOCITYe SOUNDING VELOCITIES CALCULATED By NODC ARE ENTERED
INTO STORAGE AS A LINEAR ARRAYe OBSERVED LATITUDEs LONGITUDEs AND
DEPTH ARE ENTERED INTO THE TABLE AS SEARCH PARAMETERS» AND A THREE-DI-
MENSIONAL LINEAR INTERPOLATION IS PERFORMED TO OBTAIN AN APPROPRIATE
VALUE FOR SOUNDING VELOCITY. THIS IS APPLIED TO THE OBSERVED DEPTHe
AN ITERATION ROUTINE REFINES THE CORRECTED DEPTH TO WITHIN A PREDETER-
MINED ERRORe THE INPUT IS VIA PUNCHED CARDS AND A PRINTED OUTPUT IS
PRODUCEDe ESTIMATED RUNNING TIME-- 0204 SECONDS PER DATA ENTRYe AU-
THOR-— WILLIAM ANIKOUCHINE» JORG, ESSAc
DEPARTMENT OF OCEANOGRAPHY
UNIVERSITY OF WASHINGTON
SEATTLE» WASHe 98105
AN/UYK-1 SOUND VELOCITY LANGUAGE - LOGANDS AND
LOGRAMS
COMPUTER -— AN/UYK~1
COMPUTES SOUND VELOCITY BY TWO DIFFERENT MEANS FOR COMPARISON WITH THE
SOUND VELOCIMETER VALUE OBTAINED THROUGH BISSETT-BERMAN SYSTEMe ALSO
COMPUTES PRESSURE» MEAN, VARIANCEs STANDARD DEVIATION, SIGMA-T, SPEC-
IFIC VOLUMEs SPECIFIC VOLUME ANOMALYs AND DYNAMIC HEIGHT ANOMALY. OS
NO 20154. AUTHOR-— OeAe SMITHe
COMPUTER DEPARTMENT» CODE 0831
NAVAL OCEANOGRAPHIC OFFICE
SUITLANDs MDe 20390
VELOCITY OF SOUND LANGUAGE = MAC
GOMPUTER) = kGiaels3 Os
CALCULATION OF VELOCITY OF SOUND IN SEA WATER» USING WILSON'S EQUA-
TIONe (A MAC ROUTINE WAS ALSO WRITTEN FOR THE CALCULATION OF PRESSURE
IN DECI-BARS) AUTHORS-- AeMe SHIPLEY AND De SACKSe
UNIVERSITY OF CAPE TOWN
OCEANOGRAPHY DEPARTMENT
ATTNe MRe AeMe SHIPLEY
PRIVATE BAGs RONDEBOSCH» CePe
REPUBLIC OF SOUTH AFRICA
SONVEL LANGUAGE — FORTRAN IV-H
COMPUTER -— SDS SIGMA 7
SUBROUTINE COMPUTES THE SPEED OF SOUND IN SEA WATER FROM THE TEMPERA-—
TUREs SALINITY AND PRESSURE ACCORDING TO WeDe WILSON'S FORMULAS. AN
EARLIER VERSION WAS WRITTEN BY JACQUELINE WEBSTER IN FORTRAN II FOR
THE GE 225.
INFORMATION PROCESSING CENTER
ATTNe MARY HUNT
WOODS HOLE OCEANOGRAPHIC INSTITUTION
WOODS HOLE, MASSACHUSETTS 02543
*-%-* TIDES, ASTRONOMICAL *-*-*
HARMONIC ANALYSIS OF TIDAL DATA LANGUAGE — FORTRAN Iv
p COMPUTER -— CDC 6600
(COPY ON FILE AT NODC)
THE PROGRAM GENERATES A VARIABLE LENGTH SINE TABLE IN FIVE QUADRANTS
PAGE 103
AND THE INDEPENDENT VARIABLES WHICH ARE FUNCTIONS OF TIME ARE EXTRACT-
ED FROM THIS TABLEe THE LEAST SQUARES METHOD IS EMPLOYED AND THE HAR-
MONIC CONSTANTS ARE DERIVED BY THE USE OF A MULTIPLE CORRELATION
SCREENING PROCESS WHICH CAN BE TERMINATED WHEN THE REGRESSION EQUATION
CONTAINS A SPECIFIED NUMBER OF TERMS OR WHEN THE NEXT CONSTITUENT WILL
NOT EXPLAIN A PREDETERMINED FRACTION OF THE VARIANCEs TIDE HEIGHTS
ARE READ INTO CORE STORAGE FROM MAGNETIC TAPE OR CARDSe OTHER INPUT
INCLUDES CONSTITUENT SPEEDS IN DEGREES PER SOLAR HOUR» NODE FACTORS»
AND EQUILIBRIUM ARGUMENTS IN DEGREESe THE OUTPUT IS AN ORDERED LIST-
ING OF HARMONIC CONSTANTSe NO PROVISION IS MADE FOR ELIMINATION OF
COMPONENT EFFECTSe CORE STORAGE NECESSARY - 383000 WORDSe AUTHOR —-
ROBERT Ae CUMMINGSe EARLIER VERSIONS WRITTEN FOR THE IBM 1620-1 AND
FOR THE IBM 7030 (STRETCH) COMPUTERSe
OCEANOGRAPHY DIVISION
ESSA» COAST AND GEODETIC SURVEY
ROCKVILLE» MDe 20852
TIDAL CURRENT PREDICTION LANGUAGE — FORTRAN IV
COMPUTER - CDC 6600
(cOPY ON FILE AT NODC)
NIO
COMPUTES HOURLY VELOCITIES OF THE CURRENT» TIMES OF SLACK AND TIMES
AND VELOCITIES OF MAXIMUM CURRENT USING THE HARMONIC METHOD IN WHICH
THE CONSTITUENT VELOCITIES ARE COMBINED INTO THE RESULTANT VELOCITYe
HOURLY VALUES ARE SCREENED TO DETERMINE BETWEEN WHICH HOURS A SLACK
OR MAXIMUM OCCURSe THEN CALCULATION AND COMPARISON OF THE VELOCITIES
ARE MADE AT Oel HOUR INTERVALS UNTIL THE TIME OF SLACK OR EXTREME VEL—
OCITY IS DETERMINEDe CORE STORAGE NECESSARY-- 112000 WORDSe AUTHOR —
ROBERT Ae CUMMINGS.»
OCEANOGRAPHY DIVISION
ESSA» COAST AND GEODETIC SURVEY
ROCKVILLE» MDe 20852
PROGRAM 48 - TIDAL ANALYSIS AND PREDICTION LANGUAGE — CHLF 3/4
COMPUTER — MERCURY
GENERAL PURPOSE PROGRAM FOR (1) THE ANALYSIS OF A YEAR'S HOURLY OB-
SERVED VALUES OF TIDAL HEIGHT INTO 63 TIDAL CONSTITUENTSs (2) THE PRE-
DICTION OF VALUES OF TIDAL HEIGHT FOR A SPECIFIED PERIOD AND SPECIFIED
INTERVAL BETWEEN PREDICTIONSs (3) THE CALCULATION OF RESIDUALS (OBSER-
VATIONS — PREDICTIONS) FOR A SPECIFIED PERIOD AND INTERVALe AUTHOR--
JAMES CREASEe* REFe NeleOo INTERNAL REPORT NOe N55 PAGES 21-2656 THIS
PROGRAM SHOULD BE ADAPTABLE TO THE ATLAS COMPUTER.
NATIONAL INSTITUTE OF OCEANOGRAPHY
WORMLEY » GODALMINGs SURREY
ENGLAND
THEORETICAL RADIAL TIDAL FORCE LANGUAGE — MAD
COMPUTER - IBM 7090
(COPY ON FILE AT NODC)
THERE ARE THREE INPUT FORMATS TO THIS PROGRAM-- 1) ASTRONOMICAL DATA
FROM THE NAUTICAL ALMANACe 2) THE SOLAR EPHEMERIS OBTAINED FROM THE
SAME SOURCEe ONLY THE EARTH-SUN RADIUS VECTOR IS NEEDEDe 3) LIST OF
LOCAL CONSTANTSs LATITUDE AND LONGITUDE IN DEGREES OF ARC AND MINUTES»
ELEVATION IN CENTIMETERSe OUTPUT GIVES LUNAR» SOLAR» AND TOTAL TIDAL
FORCES AND THE VECTOR DATEe PROGRAM ACCOMODATES MAXIMUM OF 725 HOURS
(30 DAYS) OF DATA IN CORE STORAGEe AUTHOR-- HENRY Le POLLAKe
DEPTe OF EARTH AND PLANETARY SCIENCES
414 SPACE RESEARCH COORDINATION CENTER
UNIVERSITY OF PITTSBURGH
PITTSBURGHs PENNA 15213
STRONOMICAL TIDE PREDICTION LANGUAGE -— FORTRAN 66
PAGE 104
COMPUTER - CDC 6600
(COPY ON FILE AT NODC)
COMPUTES HOURLY VALUES ALSO TIME AND HEIGHTS OF HIGH AND LOW WATER
USING THE HARMONIC METHOD IN WHICH THE CONSTITUENT TIDES ARE COMBINED
INTO THE RESULTANT TIDEe HOURLY VALUES ARE SCREENED TO DETERMINE BE-
TWEEN WHICH HOURS A TIDE EXTREME WILL OCCUR»s THEN CALCULATION AND COM—
PARISON OF THE TIDES ARE MADE AT Oel HOUR INTERVALS UNTIL THE EXTREME
TIDE IS DETERMINEDe ANY ARBITRARY DATUM PLANE MAY BE SELECTED. THE
OUTPUT IS OPTIONAL AND MAY BE HOURLY TIDESs HIGH AND LOW TIDES, OR
BOTHe RUNNING TIME FOR BOTH--— ABOUT 25 SECONDS FOR ONE STATION FOR
ONE YEARe AUTHORS--— NeAew PORE (WEATHER BUREAU) AND ReAe CUMMINGS
(COAST AND GEODETIC SURVEY). EARLIER VERSIONS WRITTEN FOR THE IBM 704
AND IN SOS FOR THE IBM 7090/7946 REVISED IN 19666 PROGRAM DESCRIPTION
AND LISTING ARE GIVEN IN WEATHER BUREAU TECHNICAL MEMORANDUM WTBM TDL-
65 JANUARY 1967.
OCEANOGRAPHY DIVISION
ESSA» COAST AND GEODETIC SURVEY
ROCKVILLEs MDe 20852
TIDES LANGUAGE — FORTRAN 60
COMPUTER - (NOT GIVEN)
(COPY ON FILE AT NODC)
PREDICTS TIDES IN THE OPEN SEA UTILIZING THE BASIC HYDRODYNAMIC EQUA-
TIONSs FOR THE PRINCIPAL LUNAR SEMIDIURNAL CONSTITUENT M2e APPLICA-
TION IS MADE TO THE ANALYSIS OF THE TIDAL REGIME IN THE GULF OF MEX-
TCO» REFe THESIS BY THOMAS He GAINERs JRe (MAY 19665 92 P)e
NAVAL POSTGRADUATE SCHOOL
MONTEREY» CALIFORNIA 93940
TIDAL PREDICTION LANGUAGE -— MAC
COMPUTER -— ICT 1301
(COPY ON FILE AT NODC)
COMPUTES TIMES OF HIGH AND LOW WATER FOR A PORT FOR ONE YEARe INPUT,
ON PUNCHED CARDS» ARE SPEED» AMPLITUDES» AND INITIAL ANGLESe USES IT-
ERATION METHODs FOLLOWING NEWTONe SOURCE LANGUAGE-- MANCHESTER AUTO-
CODEe REQUIRES 800 WORDS STORAGE ON ICT 1301le
UNIVERSITY OF CAPE TOWN
OCEANOGRAPHY DEPARTMENT
ATTNe MRe AeMe SHIPLEY
PRIVATE BAGs RONDEBOSCHs CePe
REPUBLIC OF SOUTH AFRICA
PREDICTION OF HOURLY TIDE LANGUAGE — (NOT GIVEN)
COMPUTER — MERCURY
COMPUTES HEIGHT OF TIDE BY EVALUATING A HARMONIC FUNCTION USING 42
COMPONENTS,» FOR EACH HOUR OVER A PERIOD OF 370 DAYSe INCLUDES SUB-
ROUTINE FOR COSINE FUNCTIONe RUNNING TIME ABOUT 50 MINUTES FOR ONE
STATION FOR 370-DAY PERIODe
HYDROGRAPHER OF THE NAVY
ARGENTINE NAVY HYDROGRAPHIC OFFICE
AVENIDA MONTES DE OCA 2124
BUENOS AIRES» REPUBLICA ARGENTINA
%—-#%-—% WAVES AND HYDROMECHANICS *-*-*
SURFACE WAVE RAYS LANGUAGE — FORTRAN II
AND FAP
PAGE 105
COMPUTER — IBM7094/CAL-
COMP 670/564
(COPY ON FILE AT NODC)
CALCULATES AND PLOTS WAVE-RAY PATTERNS FOR A COASTAL AREA OF INTEREST.
GIVEN A GRID OF DEPTH VALUES» THE INITIAL POSITION OF A WAVE RAY» AND
THE DIRECTION OF TRAVEL AND PERIOD OF THE WAVE, SUCCESSIVE POINTS ON
THE RAY PATH ARE CALCULATED FOR OUTPUT ON TAPEe THE PLOTTER USES THIS
TAPE TO PLOT THE WAVE RAYSe FOR EACH POINT ON THE PATHs WATER DEPTH
AND BOTTOM SLOPE ARE INTERPOLATED FROM THE DEPTH GRID» WAVE SPEED AND
CURVATURE ARE COMPUTED ACCORDING TO CLASSIC THEORY» AND THE COORDIN-
ATES OF THE NEXT POINT ARE APPROXIMATED BY AN ITERATION PROCEDURE. AP-
PROXIMATELY 112000 POSITIONS OF STORAGE ARE REQUIRED FOR THE DATA (ExX-
CLUSIVE OF DEPTH GRID) AND THE PROGRAMe IN ADDITION, ONE MEMORY POSI-—
TION IS NECESSARY FOR EACH COORDINATE INTERSECTION ON THE DEPTH GRID.
REPORTED IN TECHNICAL MEMORANDUM NOe 17 (1966) OF THE UeSe ARMY COAST-
AL ENGINEERING RESEARCH CENTER (CERC)»s WASHINGTONs DeCe 20016¢ AUTH-
OR--— We STANLEY WILSON» JOHNS HOPKINS UNIVe CARD DECK AND TM17 DEPOS—
ITSEDMWA ‘GERGe
We Se WILSON
DEPARTMENT OF OCEANOGRAPHY
THE JOHNS HOPKINS UNIVERSITY
BALTIMORE>s MDe 21218
WAVES LANGUAGE — SCRAP
COMPUTER — CDC 1604
COMPUTES WIND WAVE AND SWELL--— HEIGHT, PERIODs DIRECTIONs MEAN WAVE
HETGHT FOR PAST 36 HOURSe INPUT ARE SURFACE WINDSs SEA SURFACE TEMP-
ERATURE» AND ANALYZED WAVE HEIGHTS FOR PAST 72 HOURSe OUTPUT ANALYSIS
INCLUDES 123 24, 362 48 HOUR WIND WAVE AND SWELL HEIGHTS AND COMBINED
HEIGHTS» ETCe CORE STORAGE NEEDED-- 76046(8) WORDS.» ADDITIONAL STOR-
AGE-— 24 UNIVAC DRUM BLOCK AREAS OF 7634(8)~e DIRECT INQUIRIES TO--
COMMANDING OFFICER
FLEET NUMERICAL WEATHER CENTRAL
MONTEREY: CALIFORNIA 93940
GENERATION OF WATER WAVES BY TURBULENT WIND FLOW LANGUAGE — FORTRAN
COMPUTER — IBM 360/67
(COPY ON FILE AT NODC)
PROGRAM COMPUTES VELOCITY PROFILE» NORMAL PRESSUREs TANGENTIAL SHEAR
STRESS» AND WAVE GROWTH RATEe REFe THESIS BY PAUL Re KLINEDINSTs JRes
JUNE 1968 (UNPUBLISHED MSe).
NAVAL POSTGRADUATE SCHOOL
MONTEREYs CALIFORNIA 93940
OPTIMUM TRACK SHIP ROUTING LANGUAGE — MACHINE AND
FORTRAN IV
COMPUTER — PB-440 AND
UNIVAC 1107
SELECTS OPTIMUM ROUTES FOR OCEAN VESSELS TRANSITING Ne ATLANTIC OCEAN,
GIVEN INPUT DATA ON SEA HEIGHTS AND DIRECTIONe OUTPUT-- MAG TAPE AND
PRINTOUT INDICATING OPTIMUM PATH OF SHIP», AND TIME REQUIRED TO CROSS
BY BOTH OPTIMUM AND PRESPECIFIED FIXED ROUTE’ AUTHOR-- FeWe NAGLEe
COMMANDING OFFICER
NAVY WEATHER RESEARCH FACILITY
BLDGe R-485 NAVAL AIR STATION
NORFOLK, VIRGINIA 23511
VC2AP3 SHIP ROUTING LANGUAGE — FORTRAN
COMPUTER —- CDC 1604
PAGE 106
CALCULATES THE OPTIMUM TRACK SHIP ROUTE OF A VC2AP3 VESSEL ON A TRANS-
PACIFIC VOYAGEe THE PROGRAM CAN BE MODIFIED EASILY TO PROVIDE ROUTES
FOR OTHER TYPE VESSELS IN ANY OCEAN AREA OF THE Ne HEMISPHEREe USES
TWO ADVANCES IN THE CALCULUS OF VARIATIONS METHOD FOR MINIMAL~-TIME
SHIP ROUTINGe INCORPORATES LONG-RANGE (5-DAY AND 30-DAY) WEATHER
FORECASTS TO EXTRAPOLATE THE FNWC OCEAN WAVE FIELD FORECASTS TO EIGHT
DAYSe MAIN PROGRAM AND SUBROUTINES LISTED IN TECHNICAL REPORT NOe 81
(JULY 1967) BY GeJe HALTINER» WeEe BLEICKs AND FeDe FAULKNERe
NAVAL POSTGRADUATE SCHOOL
MONTEREYs CALIFORNIA 93940
SEICHE ANALYSIS LANGUAGE — FORTRAN II
AND ALGOL
COMPUTER - IBM 360/50
(COPY ON FILE AT NODC)
COMPUTES THE SEICHE PARAMETERS IN ACTUAL BASINS» GULFS OR BAYSe REF.
SPECIAL REPORT NOo 4 "DIGITAL COMPUTER PROGRAMS FOR THE DEFANT METHOD
OF SENGHE ANALYSUSIo JULY USesio Ei ieVEseri Jo [reales
THE LIBRARIAN
CENTER FOR GREAT LAKES STUDIES
UNIVERSITY OF WISCONSIN-MILWAUKEE
MILWAUKEE sWISCONSIN 53201 USA
PROFIL (TSUNAMI PROFILES) LANGUAGE — FORTRAN IV
COMPUTER - IBM 7094
TREATS A TSUNAMI OR OTHER LONG WAVE AS IF IT WERE A TRAIN OF UNIFORM
PERIODIC WAVES MOVING OVER A BOTTOM OF CONSTANT SLOPE» USING LINEAR
SHALLOW-WATER THEORYe THE RESULTS ARE PLOTTED ON A SERIES OF GRAPHS.
PROGRAM LISTED IN TECHNICAL REPORT HEL 16-1 (OCT 1966) "LONG WAVE PRO-
FILES OVER A SLOPE's BY ReHe CROSS AND Rete WIEGELe
UNIVERSITY OF CALIFORNIA
HYDRAULIC ENGINEERING LABORATORY
BERKELEYs CALIFORNIA 94720
WAVE SHOALING LANGUAGE -— FORTRAN
COMPUTER - IBM 7040
(COPY ON FILE AT NODC)
CALCULATES THE TRANSFORMATION OF A WAVE PROPAGATING FROM DEEP WATER TO
THE SHOREs APPLYING THE PRINCIPLE OF CONSERVATION OF ENERGY FLUXe THE
FIFTH ORDER GRAVITY WAVE THEORY OF SKJELBREIA AND HENDRIKSON (1960) IS
USED IN THE CALCULATIONSe THE QUALITATIVE FEATURES OF THE RESULTS ARE
THE SAME AS THOSE OBTAINED BY LE MEHAUTE AND WEBB (1964)e HOWEVER»
THE SHOALING COEFFICIENT IS SMALLER IN MAGNITUDEe REFe NESCO REPORT
SN-134-9 (1966)s5 BY ReCeYe KOH AND BeJe LE MEHAUTE*’ PROGRAMERS-—- ROB-
ERT WHALIN AND MARYANN MOORE.
NATIONAL ENGINEERING SCIENCE CO6
711 SOUTH FATR OAKS AVEe
PASADENA» CALIFORNIA
SUBROUTINE LENG1 LANGUAGE — FORTRAN Iv
COMPUTER - IBM 360/40
(COPY ON FILE AT NODC)
COMPUTES WAVE LENGTHS AND SPEED OF GRAVITY WAVES» GIVEN THE PERIOD AND
WATER DEPTHs USING SMALL-AMPLITUDE (AND STOKES! SECOND-ORDER) WAVE
THEORYe OUTPUT ARE WAVE LENGTH AND SPEED, AND THE DEEP-WATER WAVE
LENGTHe THE IMPLICIT EQUATIONS ARE APPROXIMATEDs THEN ITERATION IS
PERFORMED TO REDUCE THE ERRORe
PROFe RALPH He CROSS
ROOM 48-209 HYDRODYNAMICS LABORATORY
MASSACHUSETTS INSTITUTE OF TECHNOLOGY
PAGE 107
CAMBRIDGE» MASSACHUSETTS 02139
PROFILE LANGUAGE — FORTRAN IV
COMPUTER — IBM 360/40
(COPY ON FILE AT NODC)
COMPUTES AND PLOTS THE WAVE PROFILE GIVEN THE SPECTRUM (IN THE FORM OF
THE FOURIER COEFFICIENTS) « INPUT-- THE NUMBER OF COMPONENTS» AND THE
NUMBER OF VALUES OF ETA TO BE COMPUTED AND PLOTTEDs ARE READ IN AT Ex-
ECUTION TIMEe OUTPUT-- A PRINTER PLOT (ON A PRINTER WITH A 132-—CHAR-
ACTER LINE) OF ETA VSe Te REFe TECHe NOTE NOe 13 "WATER WAVE TEACHING
AIDS! (ReHe CROSS» SEP 1968)» HYDRODYNAMICS LABORATORYs DEPARTMENT OF
CIVIL ENGINEERINGe
PROFe RALPH He CROSS
ROOM 48-209 HYDRODYNAMICS LABORATORY
MASSACHUSETTS INSTITUTE OF TECHNOLOGY
CAMBRIDGE» MASSACHUSETTS 02139
SUBROUTINE PROF1 LANGUAGE - FORTRAN Iv
COMPUTER - IBM 360/40
(COPY ON FILE AT NODC)
COMPUTES WATER SURFACE ELEVATIONS» ETA(X) OR ETA(T)»s OVER A WAVE PERI-
ODs USING LINEAR WAVE THEORYe INPUT-- WAVE HEIGHTs PERIOD AND LENGTH,
AND THE WATER DEPTHe OUTPUT-—- RETURNS THE THREE ARRAYS OF Xs Ts AND
ETA FOR T=0s PER/40seeesPER AND X=0Os L/405 2L/4090eeesle WRITEUPS AND
LISTING IN TECHNICAL NOTE NOe 13 OF THE HYDRODYNAMICS LABORATORYe AL-—
TERNATIVE SUBROUTINES» PROF2 AND PROF3y ACCOMPLISH THE SAME PURPOSE
USING STOKES! SECOND— AND THIRD-ORDER WAVE EQUATIONS.
PROF e RALPH He CROSS
ROOM 48-209 HYDRODYNAMICS LABORATORY
MASSACHUSETTS INSTITUTE OF TECHNOLOGY
CAMBRIDGEs MASSACHUSETTS 02139
SUBROUTINE REFL1 LANGUAGE — FORTRAN Iv
COMPUTER - IBM 360/40
(COPY ON FILE AT NODC)
COMPUTES WATER SURFACE PROFILES FOR THE PARTIAL (TWO-DIMENSIONAL) RE-
FLECTION OF A LINEAR (SMALL-AMPLITUDE) WAVE FROM A STRUCTURE» INPUT -
THE INCIDENT WAVE HEIGHTs PERIODs AND LENGTHs THE WATER DEPTH» AND THE
REFLECTION COEFFICIENTs OUTPUT-- PRINTS WATER SURFACE PROFILES FOR
TWO WAVE LENGTHS» FOR T = Os T/4s5 T/2, AND 3T/4e DOCUMENTATION IS IN
TECHNICAL NOTE 135 MeIeTe HYDRODYNAMICS LABORATORY (SEPT 1968 92 P)e
PROF e RALPH He CROSS
ROOM 48-209 HYDRODYNAMICS LABORATORY
MASSACHUSETTS INSTITUTE OF TECHNOLOGY
CAMBRIDGE» MASSACHUSETTS 02139
SUBROUTINES UOFT1ls WOFT1s UTOFT1» WTOFTI LANGUAGE — FORTRAN IV
COMPUTER — IBM 360/40
(COPY ON FILE AT NODC)
COMPUTES VALUES OF U(T)» W(T)s THE PARTIAL DERIVATIVE OF U WITH RES-
PECT TO Ts OR THE PARTIAL DERIVATIVE OF W WITH RESPECT TO Ts IeEe THE
HORIZONTAL AND VERTICAL FLOW VELOCITIES AND THEIR ACCELERATIONS OVER A
WAVE PERIOD AT A GIVEN DEPTH» Z» USING LINEAR WAVE THEORYe INPUT ARE
WAVE HEIGHT» PERIOD» AND LENGTH» THE WATER DEPTH» AND THE DESIRED VAL-
UE OF Ze OUTPUT-— RETURNS ARRAYS OF T AND U(T)»s W(T)»s ETCe» FOR T=0,
PER/405 2PER/40,eeesPERe ALTERNATE SETS OF SUBROUTINES CARRY OUT THE
SAME PURPOSE USING STOKES' SECOND- AND THIRD-ORDER WAVE EQUATIONS.
WRITEUPS AND LISTINGS IN TECHNICAL NOTE NOw 13 OF THE MeleTe HYDRODY-
NAMICS LABORATORY (SEPT 1968).
PROFe RALPH He CROSS
ROOM 48-209 HYDRODYNAMICS LABORATORY
MASSACHUSETTS INSTITUTE OF TECHNOLOGY
PAGE 108
CAMBRIDGE» MASSACHUSETTS 02139
SUBROUTINES UMAX1» WMAX1s UTMAX1s WTMAX1 LANGUAGE —- FORTRAN IV
COMPUTER — IBM 360/40
(COPY ON FILE AT NODC)
COMPUTES U(MAX)» W(MAX)s THE PARTIAL DERIVATIVE OF U WITH RESPECT TO T
(MAX)s OR THE PARTIAL DERIVATIVE OF W WITH RESPECT TO T (MAX) IeEe THE
MAXIMUM FLOW VELOCITIES IN THE X AND Z DIRECTIONS AND THEIR CORRESPON-
DING TEMPORAL ACCELERATIONS, AS A FUNCTION OF Zs FROM Z = -H TO Z =
ETA(MAX)» USING LINEAR WAVE THEORYe INPUT-- WAVE HEIGHT» PERIOD» AND
LENGTH» AND THE WATER DEPTHe OUTPUT--— RETURNS ARRAYS OF Z AND UMAX(z)
ETCes FOR Z = -Hs —(29/30)Hs —(28/30)Hseee FOR Z LESS THAN ETA(MAX) 0
ALTERNATE SETS OF ROUTINES CARRY OUT THE SAME PURPOSE USING STOKES!
SECOND- AND THIRD-ORDER EQUATIONSe WRITEUPS AND LISTINGS IN TECHNICAL
NOTE NOs 13 OF THE MeIeTe HYDRODYNAMICS LABORATORY e
PROFe RALPH He CROSS
ROOM 48-209 HYDRODYNAMICS LABORATORY
MASSACHUSETTS INSTITUTE OF TECHNOLOGY
CAMBRIDGE» MASSACHUSETTS 02139
WAVE FORCE DISTRIBUTIONs TEMPORAL AND SPACIAL LANGUAGE — FORTRAN Iv
COMPUTER — IBM 7090/94
(COPY ON FILE AT NODC)
GIVEN THE WATER DENSITY, THE WATER DEPTH», THE PILE DATA»y AND A CHOICE
OF WAVE HEIGHT AND PERIOD COMBINATIONS» THIS PROGRAM COMPUTES THE DIS-
TRIBUTION OF FORCE ALONG A PILE OF ANY SHAPEe ALSO CALCULATED IS THE
FORCE AT THE WATER SURFACEe THESE DISTRIBUTIONS ARE CALCULATED FOR
TWENTY EQUALLY SPACED POINTS THROUGHOUT THE WAVE CYCLEe IF THE VALUES
OF C(M) AND C(D)» (MASS AND DRAG COEFFICIENTS)» ARE UNSPECIFIED, THE
VALUES ASSUMED ARE C(M) = 260 AND C(D) = le6e THE PROGRAM ALLOWS OTH-
ER VALUES TO BE SPECIFIED IN CASE THE SITUATION (IeEes THE PILE SHAPE)
CALLS FOR ITe PROGRAM WRITTEN FOR THE WAVE RESEARCH LAB AT THE UNIVe
OF CALIFe REFe HEL REPORT 9-4 "WAVE FORCE PROGRAMS'» BY ReHe CROSSe
PROFe RALPH He CROSS
ROOM 48-209 HYDRODYNAMICS LABORATORY
MASSACHUSETTS INSTITUTE OF TECHNOLOGY
CAMBRIDGE» MASSACHUSETTS 02139
WAVE FORCES AND MOMENTS LANGUAGE = FORTRAN Iv
COMPUTER - IBM 7090/94
(COPY ON FILE AT NODC)
GIVEN THE DESIRED COMBINATIONS OF WAVE HEIGHT AND PERIOD, PILE DIAMET-
ER» AND WATER DEPTHs COMPUTES THE WAVE LENGTHs CHECKS FOR EXCESSIVE
STEEPNESSs AND COMPUTES THE TOTAL FORCE ONs AND THE MOMENT ABOUT THE
BASE OFs THE PILES CHOSENe THE FORMULAS USED ARE DERIVED FROM LINEAR
THEORY EXCEPT THAT INTEGRATION IS CARRIED TO THE FREE SURFACEs AS CAL—
CULATEDe FORCE AND MOMENT ARE COMPUTED FOR 40 POINTS IN A WAVE CYCLEe
REFe Ue OF CALIFe HEL REPORT 9-4 "WAVE FORCE PROGRAMS! BY ReHe CROSS.
PROFe RALPH He CROSS
ROOM 48-209 HYDRODYNAMICS LABORATORY
MASSACHUSETTS INSTITUTE OF TECHNOLOGY
SEAKEEPING LANGUAGE - FORTRAN IV
COMPUTER - IBM 1130
(COPY ON FILE AT NODC)
PREDICTS HEAVEs PITCH» AND ACCELERATION OF A DESIGNATED HULL FORM IN
REGULAR WAVES OVER A RANGE OF WAVE LENGTHS AND WAVE AMPLITUDES. THE
PROGRAM IS DIVIDED INTO FOUR MAINLINE SECTIONS-- PART I SETS UP THE
INPUT DATA FOR THE TWO CALCULATING SECTIONS OF THE PROGRAMe PART II
CALCULATES THE SIMULATED ADDED MASS AND AMPLITUDE OF THE GENERATED
WAVES OF THE HULL FORMe PART III CALCULATES THE AMPLITUDES OF HEAVE,
PITCH» AND ACCELERATION, AND PART IV PLOTS AND CURVE FITS THIS INFOR-
MATIONe REPORT REFe NOe USCG-PROGRAM-ENE-12 (JUL 685 116 P) By JACK
PAGE 109
We LEWIS, ICEBREAKER DESIGN BRANCHe
Ue Se COAST GUARD HEADQUARTERS
NAVAL ENGINEERING DIVISION
1300 E STes NW
WASHINGTONs De Ce 20591
LONGITUDINAL STRENGTH OF SHIP HULL LANGUAGE —- FORTRAN IV
COMPUTER - IBM 7090
EXTENDS THE STATIC BALANCE METHOD OF CALCULATING SHEAR AND BENDING
MOMENT RESPONSES TO INCLUDE A WIDE RANGE OF WAVE HEIGHTS» LENGTHS,
AND POSITIONS WITH RESPECT TO AMIDSHIPS FOR A SHIP VERTICALLY BALANCED
IN HEAD-ON TROCHOIDAL WAVESe THE PROGRAM HAS THE OPTION OF INCLUDING
OR OMITTING THE SMITH CORRECTIONs AND THE FINAL DATA MAY BE PRESENTED
IN EITHER TABULAR OR GRAPHICAL FORMe PROGRAM YPO4 PROVIDES A MEASURE
OF THE LONGITUDINAL STRENGTH FROM THE STATIC BALANCEe YPO5 IS A METH-
OD OF PLOTTING THE LONGITUDINAL STRENGTH CURVES» PROGRAMMED BY MRSe
SHARON Ee GOODe REFe REPORT NOe 2272 (JAN 67s 93 P)»s BY GEOFFREY Oo
THOMASe DDC NOe IS AD-647-8076
MRe GENE He GLEISSNER
HEAD» APPLIED MATHEMATICS LABORATORY
NAVAL SHIP RESEARCH AND DEVELOPMENT CENTER
WASHINGTON s DeCe 20007
WAVE STATISTICS (PART I AND PART IT) LANGUAGE — FORTRAN IV
COMPUTER - IBM OS/360
DETERMINES WAVE STATISTICS OF A SEA RECORDe THE STATISTICS INCIUDE--
NUMBER OF WAVESs ReMeSes MEAN» MAXe» AND SIGNIFICANT WAVE HEIGHT» AND
SPECTRAL DECOMPOSITION OF THE SEA SURFACEe OUTPUT-- PRINTOUT OF WAVE
STATISTICS, AND PLOT OF SPECTRAL ESTIMATEe AUTHOR--- Je Eo MAMRINGe
PROFe FREDERICK Fe MONROE
DEPTe OF OCEAN ENGINEERING
FLORIDA ATLANTIC UNIVERSITY
BOCA RATONs FLORIDA 33432
WAVEIN AND DIFRAK LANGUAGE — FORTRAN
COMPUTER - IBM 7094 AND
CDC 6400
A PAIR OF PROGRAMS FOR (1)SPECTRAL ANALYSIS OF WAVE DATA,» AND (2) COM-—
PUTATION AND PLOT OF THE DIFFRACTION COEFFICIENTSe AUTHOR-- SHOU-SHAN
FANs CeEeReCes WASHes Dele
PROFe ROBERT Le WIEGEL
DEPARTMENT OF CIVIL ENGINEERING
UNIVERSITY OF CALIFORNIA
BERKELEY» CALIFe 94720
REFRACTION OF WAVES APPROACHING A COASTLINE LANGUAGE -— FORTRAN Iv
COMPUTER -— IBM 7090/94
A PROGRAM TO CONSTRUCT REFRACTION DIAGRAMS AND COMPUTE WAVE HEIGHTS
FOR WAVES MOVING INTO SHOALING WATERe CONSISTS OF MAIN PROGRAM WAVES
I AND SUBROUTINES RAYCONs REFRACs CURVE, DEPTH, HEIGHTs ERROR» WRITERe
SOLVES THE REFRACTION EQUATION AND THE WAVE INTENSITY EQUATION FOR AR-
BITRARY BOTTOM SHAPESe SOLUTION WAS SOUGHT BY USE OF THE NUMERICAL
METHODS OF FINITE DIFFERENCESe ONE OF THREE HYDRAULIC ENGINEERING
PROBLEMS DESCRIBED IN TECHe REPTe NOe TR-80 (JUN 675 185 P) BY Re Se
DOBSONe PROGRAMS ARE LISTED IN THE REPORTe THE DDC NUMBER IS AD-659-
309.6
DEPTs OF CIVIL ENGINEERING
PAGES GIO
STANFORD UNIVERSITY
STANDFORDs CALIFORNIA
SIMULATION OF WIND-GENERATED WAVES LANGUAGE = FORTRAN IV
COMPUTER — IBM 7090/94
INVESTIGATES AND COMPARES THE LABORATORY SIMULATED AND PROTOTYPE "SEAt
DATAe USES PROGRAMS WAVHTS (COMPUTE WAVE HEIGHTS AND THETR STATISTI-
CAL PROPERTIES)» SPECTR (COMPUTE NORMALIZED SPECTRUM)» STATS (COMPUTE
VARIOUS STATISTICAL PROPERTIES OF THE SEA SURFACE RECORD) » AND CONVRT
(CONVERTS SCRAMBLED VOLTAGE RECORDS TO TIME SERIES OF SURFACE DIS-
PLACEMENT)e REFe TECHe REPORT NOo 65 *LABORATORY SIMULATION OF SEA
WAVES? (JUL 1966s 134 P)»s BY JOSEPH Me COLONELLe
STANFORD UNIVERSITY
DEPTe OF CIVIL ENGINEERING
STANFORD» CALIFORNIA
PAGE 111
RETRIEVAL OF OCEAN DATA
—¥—#—K—H#—H—K—H— HHH
BIOLOGICAL STATION FILE LANGUAGE — EMA
COMPUTER — ATLAS I
A SET OF FOUR PROGRAMS WHICH CONSTITUTE A COMPLETE SYSTEM FOR PREPAR-
ING» MAINTAINING AND ACCESSING A MAGNETIC TAPE FILE OF BIOLOGICAL STA-
TION DATAe NeleQe PROGRAMS 945 94/As 94/Bs AND 94/Ce AUTHORS-—- MARG—
ARET RINGROSE AND BRIAN HINDEe
NATIONAL INSTITUTE OF OCEANOGRAPHY
WORMLEY> GODALMINGs SURREY
ENGLAND
GREAT CIRCLE RETRIEVAL LANGUAGE — FORTRAN
COMPUTER - CDC 3800
THERE ARE THREE DIFFERENT OPTIONS AVAILABLE-—- (1) GIVEN TWO POINTS ON
THE EARTH'S SURFACE» THE PROGRAM CALCULATES THE GREAT CIRCLE ROUTE BE-
TWEEN THE TWO POINTS AND THE CORRESPONDING MARSDEN SQUARES ALONG AND
AT A GIVEN DISTANCE FROM THE TRACKe THE DATA TAPES ARE SEARCHED BY
MARSDEN SQUARES AND THE SOUND VELOCITY PROFILES» TEMPERATURE,» SALINITY
AND DEPTH OF OBSERVATION ARE ABSTRACTEDe (2) INDIVIDUAL MARSDEN SQS.
MAY BE INPUT INTO THE PROGRAM AND THE ABOVE QUANTITIES ARE ABSTRACTEDe
(3) A POINT» A RADIUS OF INTEREST IN NAUTICAL MILES» AND A CLUSTER OF
MARSDEN SQUARES MAY BE SPECIFIEDe THE PROGRAM WILL ABSTRACT ALL THE
STATIONS WITHIN A CIRCULAR AREA OF THE POINT FOR THE GIVEN MONTHSe
THE INPUT RETRIEVAL PROGRAM» BY WALTER YERGENs USES DATA TAPES COMPAC-—
TED FROM THE NODC FILE» STORAGE REQUIREMENTS—-— 1053:056 OCTAL WORDS OF
COREs AND ONE CDC DISC FILE.
Be Ge ROBERTSs JRes CODE 8177
ACOUSTICS DIVISION
NAVAL RESEARCH LABORATORY» WASHINGTONs De Co 20390
CORE COMPUTER PROGRAM LANGUAGE - FORTRAN
COMPUTER = (NOT GIVEN)
(COPY ON FILE AT NODC)
A PROGRAM PACKAGE DESIGNED FOR USE ON A RECONNAISSANCE BASIS» LISTING
ALL CORES IN THE L-—DGO COLLECTION CONTAINING CHARACTERISTICS SPECIFIED
BY THE USERe THE PROGRAM OUTPUTS THE REQUIRED LIST OF CORES WITH A
SHORT DESCRIPTION OF EACH COREe AS SPECIFIED ON FOUR CONTROL CARDS»
CORES MAY BE REQUESTED FROM CERTAIN LOCATIONS» OF CERTAIN LENGTHS»
TAKEN IN A CERTAIN RANGE OF WATER DEPTHS» OF SPECIFIED AGE» LITHOLOGY
AND CONTAINING SPECIFIC PALEONTOLOGIC AND MINERALOGIC COMPONENTS.
CORES WHICH ARE ORIENTEDs HAVE APPEARED IN PUBLICATIONS AND HAVE PAL-
EOMAGNETIC DATA AVAILABLE CAN ALSO BE REQUESTED.
MRe ROY Re CAPO
CORE CURATOR
LAMONT-—DOHERTY GEOLOGICAL OBSERVATORY
PALISADES» NEW YORK 10964
STORAGE AND RETRIEVAL OF GEOPHYSICAL DATA LANGUAGE — FORTRAN
COMPUTER -— (NOT GIVEN)
(COPY ON FILE AT NODC)
A SYSTEM OF PROGRAMS AND SUBROUTINES FOR THE STORAGE» EDITING» AND RE-
TRIEVAL OF DATAs SET UP BY THE MARINE GEOPHYSICS GROUP AT BEDFORD IN-
STITUTE OF OCEANOGRAPHY. THE MAIN RETRIEVAL PROGRAM SEARCHES FOR A
PARTICULAR FILE ON TAPE, READS AND PRINTS FILE LABELS» AND CONTROLS
THE PROCESSING SUBROUTINES CALLEDe DOCUMENTED IN BIO COMPUTER NOTE
67-3-C (NOV 1967)s BY De Ie ROSS.
BEDFORD INSTITUTE
PAGE 112
DARTMOUTHs NOVA SCOTIA» CANADA
OCEANS CATALOGUE TI AND II LANGUAGE -— FORTRAN IV
COMPUTER -— CDC 3100
PROGRAM I — FACILITATES UPDATING OF CHARTS THAT DEPICT THE GEOGRAPHIC-—
AL DATA DISTRIBUTION ILLUSTRATED IN THE OCEANOGRAPHIC DATA CATAIOGUE.
PROGRAM II - COMPILES AND LISTS AN INDEX OF CANADIAN REFERENCE NUMBERS
IN GEOGRAPHICAL SEQUENCES FOR THE OCEANOGRAPHIC DATA CATALOGUE. AUTH-
OR-- Je ZEBARTHe
CANADIAN OCEANOGRAPHIC DATA CENTRE
615 BOOTH STREET
OTTAWA» CANADA
PAGE 113
eh
WOLoa
INDEX BY AGENCY OR INSTITUTION
ADELPHI UNIVERSITY
CHLOROPHYLL AND CAROTENOID PIGMENT IBM 16201IFORTRAN II 05
ARGENTINE NAVY HYDROGRAPHIC OFFICE
PREDICTION OF HOURLY TIDE MERCURY NOT GIVEN 105
ARMY CORPS OF ENGINEERS», LAKE SURVEY DISTRICT
SEDIMENT TEXTURAL ANALYSTS NOT GIVEN FORTRAN 32
ARTHUR De LITTLEs INCe
ACOUSTIC RAY TRACING IBM 7090 FORTRAN II 94
TWO-DIMENSTONAL AUTOCORRELATION IBM 7090s FORTRAN 56
IBM 1401
TRLOSS (TRANSMISSION LOSS) CDC 6600 FORTRAN 94
BEDFORD INSTITUTE OF OCEANOGRAPHY
DATA REDUCTION FOR THE CDC 3100 CDC 3100 FORTRAN II 14583
DATA REDUCTION FOR THE PDP-8 PDP-8 PAL III 14
ISALBP (SALINITY ANOMALY) CDC 3100 FORTRAN II 10
ISATBP (OXYGEN ANOMALY AND SATe) CDC 3100 FORTRAN II 10
LEAST SQUARES CURVE FITTING CDC 3100 FORTRAN II 45
PLOT STATION POSITIONS CDC 3100 FORTRAN II 36
PLOT THETA-S CURVES CDC 3100 FORTRAN II 35
SECTION PLOTTING CDC 3100 FORTRAN 36
TIME SERIES PLOTTING CDC 3100 FORTRAN-32 36
STADAT 2 GE 200 SERFORTRAN II 14
RETRIEVAL OF GEOPHYSICAL DATA NOT GIVEN FORTRAN Walz
BERGEN» UNIVERSITY OF
PROCESSING OF OCEANOGRAPHIC OBSe IBM 1620I1IFORTRAN II 70
BUREAU OF COMMERCIAL FISHERIES» HAWAII
AOUsISAOU (CALCe OF OXYGEN» ETCe) IBM 360/65FORTRAN IV 10
GDNP»sGRAD (CALCe OF GRADIENTS) IBM 360/65FORTRAN IV 76
GVPAsVPA (CALC. OF CURRENTS) IBM 360/65FORTRAN IV 69
TSOSsOXOSsPHOS (ISENTROPIC PLOT) IBM 360/65FORTRAN IV 40
LENGTH-WEIGHT FREQUENCY IBM 360/65FORTRAN IV 06
LONG WAVE RADIATION IBM 360/65FORTRAN IV 25
OCEANOGRAPHIC REPORT PREPARATION IBM 360/65FORTRAN IV 91
OCEANOGRAPHIC SUMMARY (NOS. 19293) IBM 360/65FORTRAN IV 719
REVERSING THERMOMETER CORRECTION IBM 360/65FORTRAN IV 20
TSIPsTHOXsTHOT (PLOT TIME HISTORY) IBM 360/65FORTRAN IV 41
BUREAU OF COMMERCIAL FISHERIES, LA JOLLA
SEA SURFACE TEMPe AND ANOMALY SUM, CDC 3600 FORTRAN-62 81
SEA SURFACE TEMPe DATA SUMMARY CDC 3600 FORTRAN-62 81
SYNOPTIC MARINE WEATHER DATA SUMMARY CDC 3600 FORTRAN-62 80
VACOTS (VERTICAL SECTION PLOT) CDC 3600 FORTRAN-63 39
PAGE 115
BUREAU OF COMMERCIAL FISHERIES, MIAMI
FLOW METER PLOTS IBM 360/65FORTRAN IV 72
GENERAL MERCATOR PLOT IBM 360/65FORTRAN IV 40
HORIZONTAL SECTIONS IBM 360/65FORTRAN IV 40
IN SITU OCEANOGRAPHIC DATA IBM 360/65FORTRAN IV 85
INTERPOLATION IBM 360/65FORTRAN IV 86
MERCATOR STATION PLOT IBM 360/65FORTRAN IV 40
OXYGEN» PHOSPHATE» DENSITY PLOTS IBM 360/65FORTRAN IV 39
TEMPERATURE-SALINITY CURVES IBM 360/65FORTRAN IV 39)
CALIFORNIAs UNIVERSITY OF
WAVEIN AND DIFRAK IBM 70945 FORTRAN 509110
CDC 6400
PROFIL (TSUNAMI PROFILES) IBM 7094 FORTRAN IV 107
CANADIAN OCEANOGRAPHIC DATA CENTRE
DAILY SEAWATER OBSERVATIONS CDC 3100s FORTRAN IV> ue
IBM 1620 FORTRAN II-D
OCEANS II REPORT GENERATOR IBM 1401 SPS 23
OCEANS ITI IBM 360/65FORTRAN IV 86
OCEANS CATALOGUE I AND II cDC 3100 FORTRAN IV 113
SUA USU MES 15 1th Vel CDC 3100 FORTRAN IV 56
THERMOCHECK II -— TEMPe CORRECTION CDC 3100s FORTRAN IV 17
IBM 360/65
TEMPERATURE-SALINITY PLOT CDC 3100 FORTRAN 39)
CAPE TOWNs UNIVERSITY OF
CHLOROPHYLL CALCULATIONS KG 3 Ont MAG o7
DELTA-ALPHA AND SIGMA-T lel 1301) (MAG 93
HARMONIC ANALYSIS leh 1308 TMAG Sw
TIDAL PREDICTION UG 3 Ol IMAG 105
VELOCITY OF SOUND ICT 1301 MAC 103
COAST AND GEODETIC SURVEYs SEATTLE
CONDU (THERMAL CONDUCTIVITY) IBM7094-IIFORTRAN IV 31
77040 DCS
COAST AND GEODETIC SURVEYs WASHINGTON»s De Ceo
ASTRONOMICAL TIDE PREDICTION CDC 6600 FORTRAN-66 104
COMPUTE GEOGRAPHIC POSITIONS IBM 1620 SPS 61
HARMONIC ANALYSIS OF TIDAL DATA CDC 6600» FORTRAN IV 103
IBM 7030 FORTRAN II
LORAN C IBM 1620 SPS 62
TIDAL CURRENT PREDICTION CDC 6600 FORTRAN IV 104
VELOCITY OF SOUND IBM 1620 FORTRAN 102
COAST GUARD OCEANOGRAPHIC UNIT
OXYGEN COMPUTATION H-516 FORTRAN IV al
PHOSPHATE COMPUTATION H-516 FORTRAN IV ial
SALINITY CONVERSION H-516 FORTRAN IV ll
THERMOMETER CORRECTION H-516 FORTRAN IV 16
COAST GUARD HEADQUARTERS» OFFICE OF ENGINEERING
SEAKEEP ING IBM 1130 FORTRAN IV 109
PAGE 116
COLUMBIA UNIVERSITY» HUDSON LABORATORIES
RAY TRACING
NOT GIVEN FORTRAN AND
USER LANGe
COMMERCE» DEPARTMENT OF (SEE COAST AND GEODETIC SURVEY)
DEFENSE, DEPARTMENT OF (SEE FLEETecees
DEFENSE RESEARCH ESTABLISHMENT PACIFIC
RAYTR (RAY-TRACING)
DIGITAL EQUIPMENT COMPUTER USERS!
DECCA HI-FIX
DISSOLVED OXYGENs POTENTIAL TEMPe
OCEAN STATION ANALYSIS AND SUMMARY
THERMOMETER CORRe AND THERMOe DEPTH
FLEET NUMERICAL WEATHER CENTRAL
DATA FIELD GRID EXPANSION
FORECASTING OF SURFACE CURRENTS
GG T SEA
POTENTIAL MIXED LAYER DEPTH
SEA SURFACE TEMPERATURE ANALYSIS
NAVAL eoes
IBM 360/44FURTRAN
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CDC
CDC
CDC
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TWO DIMENSTONAL RAY TRACE
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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.
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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
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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
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7074 FORTRAN
7074 AUTOCODER
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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
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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
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OBJECTIVE THERMOCLINE ANALYSIS
SONOBUOY FIXING ERROR
SPECIFIC CONDUCTIVITY
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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
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7074 AUTOCODER
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7074 FORTRAN
7074 FORTRAN II
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1604 FORTRAN-60
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1604 FORTRAN
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3800 FORTRAN-63
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3800 FORTRAN-63
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3800 FORTRAN
3800 FORTRAN
3800 FORTRAN
99
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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
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BECNAV (BEACON NAVIGATION)
SPANSI1A (BEACON POSITION)
SPANS1B (BEACON POSITION)
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3800 FORTRAN 59
3800 FORTRAN 2.
32800 FORTRAN-63 96
3800 FORTRAN» 35
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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
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PATTERN FUNCTION CALCULATIONS
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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
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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
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POWER SPECTRUM ANALYSIS PB-250 BASIC 51
PACIFIC OCEANOGRAPHIC GROUP
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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
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STPO2 (COMPUTE FROM SeTeDe DATA) IBM 1130 FORTRAN Iv 84
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TRANSPORT COMP, FROM ATMOSe PRESSURE IBM 1620, FORTRAN II 67
IBM 70405 AND Iv
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RAND CORPORATION
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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
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SCRIPPS INSTITUTION OF OCEANOGRAPHY
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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
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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
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WISCONSINs UNIVERSITY OF
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SPECTRAL ANALYSIS OF TIME SERIES
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IBM7094-IIFORTRAN IV O7
77040 DCS
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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)
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POTEMP (POTENTIAL TEMPERATURE)
PRESS
PROVEC (PROGRESSIVE VECTORS)
SCRUB (DATA EDIT AND CORRECT)
SIGMAT
SONVEL (SOUND VELOCITY)
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THISTO (TWO-DIMENe FREQe DISTRIBe)
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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
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GE 2255 FORTRAN IlI¢9 91
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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
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MODIFIED SURFACE CURRENTS
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STATION DATA COMPUTE
STATION DATA VERTICAL ARRAY SUMMARY
STATISTICAL SURFACE CURRENT ROSE
SURFACE CURRENT SUMMARY
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THERMOCLINE AND MIXED LAYER DEPTHS
THERMOCLINE ONE-DEGREE
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TEMPERATURE-SALINITY PLOT
BECNAV
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SPANS1B
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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
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B5500 ALGOL
IBM 360/50ALGOL
B5500 ALGOL 60
ELLIOTT803ALGOL 60
I/P IBM 1620 BALGOL
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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
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IBM 7074 AUTOCODER
IBM 7074 AUTOCODER
IBM 7074 AUTOCODER
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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
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WAVEIN AND DIFRAK
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ORD 2 (OLMSTED RAY DIAGRAM NOe 2)
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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
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CLOUD COVER AND DAILY SEA TEMPERATUREIBM
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CRITICAL ACOUSTIC RATIO
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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
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INTERPOLATION OF OCEAN STATION DATA
INTERPOLATION SPECIFIC VOL ANOMALY
LAYER DEPTH PLOT
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LIGHT AND SOUND INSTRUCTION B
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LORAN A AND C SKYWAVE
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MARINE BIOLOGe ENVIRONe SUMMARIES
MARSDEN SQ. AVERAGES FROM GEOFILE
MASS PHYSICAL PROPERTIES
MONTHLY SONIC LAYER DEPTH
PAGE 128
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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
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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
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WAVES GENERATED BY TURBULENT WIND IBM 360/67FORTRAN
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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
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SYNOPTIC PROGRAM
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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
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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
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-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
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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)
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FURTRAN
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FORTRAN
FORTRAN
FORTRAN
FORTRAN
FORTRAN
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FORTRAN
FORTRAN
FORTRAN
FORTRAN
FORTRAN
FORTRAN
FORTRAN
FORTRAN
FORTRAN
FORTRAN
FORTRAN
FORTRAN
FORTRAN
FORTRAN
FORTRAN
FORTRAN
FORTRAN
FORTRAN
FORTRAN
FORTRAN
FORTRAN
FORTRAN
FORTRAN
FORTRAN
FORTRAN
FORTRAN
FORTRAN
FORTRAN
FORTRAN
FORTRAN
FORTRAN
FORTRAN
FORTRAN
FORTRAN
FORTRAN
FORTRAN
FORTRAN
FORTRAN
FORTRAN
FORTRAN
FORTRAN
FORTRAN
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FORTRAN
FORTRAN
FORTRAN
FORTRAN
FORTRAN
FURTRAN
FORTRAN
AND MAP
FORTRAN
FORTRAN
FORTRAN
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II 64
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II 47
II 90
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II 27
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II 50
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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
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CALCULATE AND PLOT TIME-TREND CURVES
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PREDICTION
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DIRECTIONAL DATA
WAVE FORCE DISTRIBUTION
WAVE FORCES AND MOMENTS
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PAGE 140
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AND MAP
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IBM 7094 FORTRAN
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7/7040 DCS
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GVPAsVPA (CALC. OF CURRENTS)
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OCEANOGRAPHIC REPORT PREPARATION
OCEANOGRAPHIC SUMMARY (NOSe 192593)
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HYLOG (HYDROe STAe DATA REDUCTION)
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OCCOMP (OCEANOGRAPHIC COMPUTE)
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PAGE 141
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360/50FORTRAN
360/50FORTRAN
360/50FORTRAN
360/50FORTRAN
360/50FORTRAN
360/50FORTRAN
360/65FORTRAN
360/65FORTRAN
360/65FORTRAN
360/65FORTRAN
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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
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SIGMATFORTRAN
SIGMA7TFORTRAN
SIGMATFORTRAN
SIGMATFORTRAN
SIGMATFORTRAN
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VEL (GEOSTROPHIC VELOCITY)
VTR (VOLUME TRANSPORT)
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NEWFIT
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BIOLOGICAL STATION FILE
STATION DATA (ATLAS)
Q@ FACTORS
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DEEP (SeTeDe DIGITIZING)
WET (SeTeDe DATA PROCESSING)
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TIDAL PREDICTION
VELOCITY OF SOUND
THERMOMETER CORRECTIONS
TIDAL ANALYSIS AND PREDICTION
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POWER SPECTRUM ANALYSIS
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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
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ATLAS 1 EMA
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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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