IMAGINARY REACTIONS AND SUCCESSIVE APPROXIMATIONS. CALCULATES THE 

 HYDRODYNAMIC FORCES. AND BOTH NORMAL AND TANGENTIAL DRAGS ARE INCLUD- 

 ED. DOCUMENTED IN NRL REPORT 6894 (MAY 1969), BY R.A. SKOP AND R.E. 

 KAPLAN. MEMORY REQUIREMENTS — APPROX. 16000 WORDS FOR THE ARRAYS IN 

 COMMON AND 2100 WORDS FOR THE MAIN PROGRAM AND SUBPROGRAMS. 



NAVAL RESEARCH LABORATORY 

 4555 OVERLOOK AVENUE, S.W. 

 WASHINGTON, D. C. 20390 



CABLE CONFIGURATION LANGUAGE - FORTRAN IV 



COMPUTER - IBM 1800 SYS 

 (COPY ON FILE AT NODC) 



COMPUTES THE EQUILIBRIUM CONFIGURATION AND TENSIONS OF A CABlE TOWING 

 A SUBMERGED BODY FOR FAIRED, UNFAIRED, AND DISCONTINUOUS (LOWER PART 

 FAIRED) CABLES. THE OUTPUT ON THE LINE PRINTER GIVES THE VALUES OF 

 THE INPUT DATA FOLLOWED BY VARIOUS CALCULATED VALUES. THE SOLUTION IS 

 FOUND FOR THE iHEAVY GENERAL CABLE' LAW OF CABLE LOADINGS AS DESCRIBED 

 BY M.C. FAMES (1968). EXECUTION TIME — ABOUT 30 SECS. FOR EACH CASE. 

 N.I.O. PROGRAM NO. 168. AUTHOR — CATHERINE CLAYSON. 



NATIONAL INSTITUTE OF OCEANOGRAPHY 

 WORMLEY, GODALMING, SURREY 

 ENGLAND 



CURRENT METER ANALYSIS LANGUAGE - FORTRAN IV 



COMPUTER - IBM 1800 SYS 



READS, CALIBRATES AND PLOTS DATA FROM BERGEN OR PlESSEY CURRENT MET- 

 ERS. DATA IS READ FROM CARDS. ANY ONE OF THE READINGS MAY Bt TAKEN 

 As ROTOR COUNT, THE DIFFERENCES BETWEEN CONSECUTIVE READINGS THEN BE- 

 ING USED BY THE PROGRAM AS THE BASIS OF CURRENT SPEED. THREE GRAPHS 

 MAY BE PLOTTED (E.G. SPEED, DIRECTION, AND TEMPERATURE). ALL RESULTS 

 ARE ALSO OUTPUT TO MAGNETIC TAPE. N.I.O. PROGRAM 111 BY W.T.J. SlADE. 

 WRITE-UP IN N.I.O. INTERNAL REPORT NO. N.12, DEC 1968. 



NATIONAL INSTITUTE OF OCEANOGRAPHY 

 WORMLEY, GODALMING, 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 TAPE. N.I.O. SUB-PROGRAM -H, BY 

 W.T.J. SLADE (REF. N.I.O. INTERNAL REPORT NO. N.12). 



NATIONAL INSTITUTE OF OCEANOGRAPHY 

 WORMLEY, GODALMING, SURREY 

 ENGLAND 



VEL LANGUAGE - FORTRAN IV-H 



COMPUTER - SDS SIGMA 7 



COMPUTES GEOSTROPHIC VELOCITY DIFFERENCE BETWEEN TWO OCEANOGRApH I C 

 STATIONS, ACCORDING TO A FORMULA DESCRIBED BY N.P. FOFONOFF AND CHAR- 

 LOTTE FROESE. (PROGRAM WRITTEN AS SUBROUTINE - NO I/P OR 0/P) 



INFORMATION PROCESSING CENTER 

 ATTN. MARY HUNT 



WOODS HOLE OCEANOGRAPHIC INSTITUTION 

 WOODS HOLE, MASSACHUSETTS 02543 



VTR LANGUAGE - FORTRAN IV-H 



COMPUTER - SDS SIGMA 7 



PAGE 073 



