CALCULATES THE OPTIMUM TRACK SHIP ROUTE OF A VC2AP3 VESSEL ON A TRANS- 

 PACIFIC VOYAGE. THE PROGRAM CAN BE MODIFIED EASILY TO PROVIDE ROUTES 

 FOR OTHER TYPE VESSELS IN ANY OCEAN AREA OF THE N. HEMISPHERE. USES 

 TWO ADVANCES IN THE CALCULUS OF VARIATIONS METHOD FOR MINIMAl-TIME 

 SHIP ROUTING. INCORPORATES LONG-RANGE (5-DAY AND 30-DAY) WEATHER 

 FORECASTS TO EXTRAPOLATE THE FNWC OCEAN WAVE FIELD FORECASTS TO EIGHT 

 DAYS. MAIN PROGRAM AND SUBROUTINES LISTED IN TECHNICAL REPORT NO. 81 

 (JULY 1967)» BY G.J. HALTINER» W.E. BlEICK» AND F.D. FAULKNER. 



NAVAL POSTGRADUATE SCHOOL 

 MONTEREY. CALIFORNIA 93940 



SEICHE ANALYSIS 



LANGUAGE - 



FORTRAN I I 

 AND ALGOL 

 IBM 360/50 



COMPUTER - 

 (COPY ON FILE AT NODC ) 



COMPUTES THE SEICHE PARAMETERS IN ACTUAL BASINS* GULFS OR BAYS. REF. 

 SPECIAL REPORT NO. 4 'DIGITAL COMPUTER PROGRAMS FOR THE DEFAnT METHOD 

 OF SEICHE ANALYSIS', JULY 1968, BY EVERETT J. FEE. 



THE LIBRARIAN 



CENTER FOR GREAT LAKES STUDIES 

 UNIVERSITY OF WISCONSIN-MILWAUKEE 

 MILWAUKEE, WISCONSIN 53201 USA 



PROFIL (TSUNAMI PROFILES) 



LANGUAGE 

 COMPUTER 



FORTRAN IV 

 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 THEORY. 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', BY R.H. CROSS AND R.L. WIEGEL. 



UNIVERSITY OF CALIFORNIA 

 HYDRAULIC ENGINEERING LABORATORY 

 BERKELEY, 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 SHORE, APPLYING THE PRINCIPLE OF CONSERVATION OF ENERGY FLUX. THE 

 FIFTH ORDER GRAVITY WAVE THEORY OF SKJElBREIA AND HENDRIKSON (I960) IS 

 USED IN THE CALCULATIONS. THE QUALITATIVE FEATURES OF THE RESULTS ARE 

 THE SAME AS THOSE OBTAINED BY LE MEHAUTE AND WEBB (1964). HOWEVER, 

 THE SHOALING COEFFICIENT IS SMALLER IN MAGNITUDE. REF. NESCO REPORT 

 SN-134-9 (1966), BY R.C.Y. KOH AND B.J. LE MEHAUTE. PROGRAMERS — ROB- 

 ERT WHALIN AND MARYANN MOORE. 



NATIONAL ENGINEERING SCIENCE CO. 

 711 SOUTH FAIR OAKS AVE. 

 PASADENA, CALIFORNIA 



SUBROUTINE LENGl 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 DEPTH, USING SMALL- AMP L I TUDE (AND STOKES' SECOND-ORDER) WAVE 

 THEORY. OUTPUT ARE WAVE LENGTH AND SPEED, AND THE DEEP-WATER WAVE 

 LENGTH. THE IMPLICIT EQUATIONS ARE APPROXIMATED, THEN ITERATION IS 

 PERFORMED TO REDUCE THE ERROR. 



PROF. RALPH H. CROSS 



ROOM 48-209 HYDRODYNAMICS LABORATORY 



MASSACHUSETTS INSTITUTE OF TECHNOLOGY 



PAGE 107 



