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 COMPLEX 

 DEMODULATION. ALLOWING EXAMINATION OF PERIODS UP TO 100 DAYS. SPECIAL 

 APPLICATION TO THE SEARCH FOR THE EXISTENCE OF EQU I VALENT-BArOTROP IC 

 TOPOGRAPHIC (ROSSBY) WAVES ON THE WESTERN SIDE OF THE NORTH ATLANTIC. 

 THE AUTOSPECTRA LEvEl OFF AT LOWEST FREQUENCIES. NO LONGER INCREASING 

 AS A POWER LAW. STRONG COHERENCES WERE FOUND AT LOW FREQUENCIES BE- 

 TWEEN THE U AND V COMPONENTS AND BETWEEN THE LEVELS. REF. A TECHNICAL 

 REPORT NO. 69-67 (UNPUBLISHED MANUSCRIPT). AUG 1969. BY RORY THOMPSON. 



DR. N. P. FOFONOFF. CHAIRMAN 

 DEPT. OF PHYSICAL OCEANOGRAPHY 

 WOODS HOLE 0CEAN06RAPHIC 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 

 DATA, AS WELL AS GIVING CALCULATIONS FOR USE IN TESTING HYPOTHESES. 

 A CONTROL CARD DETERMINES THE TEST PERFORMED. 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-TEST. BIMODAL DATA MAY BE TREATED BY PROGRAM 

 CIRCSTAT. REF. TECHNICAL REPORT NO. 3. OFFICE OF NAVAL RESEARCH. FEB. 

 1967. BY THOMAS A. JONES. 



DEPARTMENT OF GEOLOGY 

 NORTHWESTERN UNIVERSITY 

 EVANSTON. ILLINOIS 60201 



BOMM (TIME SERIES) 



LANGUAGE - FORTRAN. 



COMPASS 

 COMPUTER - IBM OS/360, 



CDC 3600 



A COLLECTION OF PROGRAMS HAVING TIME SERIES AS OPERANDS PRIMARILY DE- 

 SIGNED FOR ANALYSIS, CORRELATION AND DECOMPOSITION OF RECORDS. COPIES 

 AVAILABLE THROUGH 'SHARE' AND 'COOP'. AUTHORS — SIR EDWARD BUllARD, 

 MRS. FlORANCE OGALBY DORMER, WALTER MUNK AND GAYLORD MILLER. 



MRS. FLORENCE 0. DORMER 



INSTITUTE OF GEOPHYSICS AND PLANETARY PHYSICS 



SCRIPPS INSTITUTION OF OCEANOGRAPHY 



P.O. 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 MEASURED. 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 ESTIMATES. THE DATA IS 

 THEN SUBJECTED TO ANALYSIS OF VARIANCE. USING ORTHOGONAL POLYNOMIALS, 

 AND PRINCIPAL COMPONENT ANALYSIS, AND SPECIFIED CONTOURS OF THE DEPEN- 

 DENT VARIABLE ARE PLOTTED, BOTH WITHOUT AND WITH TRANSFORMATION. REF. 

 FRB TECHNICAL REPORT NO. 87 (PUBLISHED MANUSCRIPT, AUG 1968) tiy J. K. 

 LINDSEY. DIRECT INQUIRIES TO — 



FISHERIES RESEARCH BOARD OF CANADA 

 BIOLOGICAL STATION 

 NANAIMO, B. C. 



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