MASSACHUSETTS INSTITUTE OF TECHNOLOGY 

 CAMBRIDGEf MASSACHUSETTS 02139 



SOLAR RADIATION CONVERSION LANGUAGE - FORTRAN 



COMPUTER - IBM 7074 



AVERAGES THE RADIATION READINGS FROM THE EPPLEy PYRHEL I OMET ER AND 

 BECKMAN-WHITLEY RADIOMETER FOR EVERY 15 MINUTES. CONVERTS FROM MV TO 

 LANGLEYS/MIN. and CALCULATES NET RADIATION FROM BOTH INSTRUMENTS. A 

 MODIFICATION OF THIS PROGrAm WAS MADE TO INCLUDE A THQRNTHWAITE NET 

 RADIOMETER. ORIGINAL PROGRAM BY S.M. LAZANOFF REWRITTEN BY mAry E. 

 MYERS. 



COMPUTER DEPARTMENT. CODE 0831 

 NAVAL OCEANOGRAPHIC OFFICE 

 SUITLAND. 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 INTENSITY. OS NO* 53533. 

 AUTHOR — G. VAN VOORHIS. 



MAGNETICS DIVISION. CODE 8200 

 NAVAL OCEANOGRAPHIC OFFICE 

 SUITLAND. MD. 20390 



VAM INTERPOLATION II LANGUAGE - FORTRAN 



COMPUTER - IBM 7074 



COMPUTES INCLINATION. MAGNETIC HEADING, RELATIVE BEARING, AND DECLIN- 

 ATION. OUTPUT CONTAINS TRACK, DATE, AIRCRAFT TIME. POSITION, DECLIN- 

 ATION. DIP. HORIZONTAL INTENSITY (FORCE). ALTITUDE. AND GROUND SPEED 

 FOR EACH FIVE MINUTES oF TImE. OS NC 35032, BY W. H. HAnCoCK. 



NAVAL OCEANOGRAPHIC OFFICE 

 SUITLAND, MD. 20390 



SEISMIC SLOPING LAYER COMPUTATION LANGUAGE - FORTRAN II 



COMPUTER - IBM 709 



GIVES TRUE VELOCITIES AND THICKNESSES OF lAYERS FqR SEISMIC rEFrACTION 



PROFILES. 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 plane 



SEISMIC waves utilizing SNElL'S law. author — JOHN antoine. 



TEXAS A AND M UNIVERSITY 

 COLLEGE of GEOSCIENCES 



department of oceanography 

 college station. texas 77843 



time term. 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 BOUNDARY. READS THE STAN- 

 DARD TRAVEl-TIME DATA CARDS (CARnEGIE INST. WASH. DTM ) . 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 DISTANCE. THESE FEATURES OF THE MATRIX ARE PRESENTED IN 

 GRAPH FORM. AUTHOR— M.J. BERRY. 



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