SUITLAND. MARYLAND 20390 



VELOCITY AND HORIZONTAL EDDY COEFFICIENTS LANGUAGE - FORTRAN 



COMPUTER - IBM 709 



COMPUTATION OF VELOCITY AND HORIZONTAL MIXING EDDY COEFFICIENTS ALONG 

 ISENTROPIC SURFACES. AUTHOR — A.D. KIRWAN. 



TEXAS A AND M UNIVERSITY 

 COLLEGE OF GEOSCIENCES 

 DEPARTMENT OF OCEANOGRAPHY 

 COLLEGE STATION. 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 INFLOW, WITH APPLICATION TO THE UPPER 

 CHESAPEAKE BAY AND THE SUSQUEHANNA RIVER. BASED ON A SALT CONTINUITY 

 EQUATION IN WHICH THE SEAWARD SALT ADVECTION IS BALANCED BY TURBULENT 

 DIFFUSION TOWARD THE HEAD OF THE BAY. 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 TIME. REF. 69- 

 7, TECH. REPORT 54 (MAY 1969, 70P.) BY WIlLIAM BOICOURT. 



CHESAPEAKE BAY INSTITUTE 

 THE JOHNS HOPKINS UNIVERSITY 

 BALTIMORE, MD. 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 DATA, AND FOR HARMONIC ANALYSIS AND 

 POWER SPECTRUM ANALYSIS. REF. TECHNICAL REPORT NO. 37, NATO SuBCOM- 

 MITEE ON OCEANOGRAPHIC RESEARCH (105 P., FEB 1967). AUTHOR — DR. H.E. 

 SWEERS (OF THE CANADIAN OCEANOGRAPHIC DATA CENTRE). 



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 DRIFTED, NUMBER OF DAYS ADRIFT, AND SPEED IN NAUTICAL 

 MILES PER DAY. COMPUTES MARSDEN AND 1/4-DEGREE SQUARES OF RELEASE = 

 OUTPUT ON MAGNETIC TAPE. AUTHOR — JUDY YAVNER. USED WITH A TAPE TO 

 PRINT/CARD EDITING AND SELECTION PROGRAM. AUTHOR — JOHN JENSON. 



COMPUTER SYSTEMS DIVISION, CODE 2400 

 NATIONAL OCEANOGRAPHIC DATA CENTER 

 WASHINGTON, D.C. 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 

 AS A VERTICAL LINE SOURCE OF UNIT DEPTH AND UNIT RATE OF DISCHARGE IN 

 AN UNBOUNDED MEDIUM. INPUT ARE THE VELOCITY (A CONSTANT), THE LONGI- 

 TUDINAL AND TRANSVERSE COORDINATES, AND THE DIFFUSION VELOCITY, I.E., 



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