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jmc |
1.30 |
C $Header: /u/gcmpack/MITgcm/model/src/the_correction_step.F,v 1.29 2005/04/15 14:06:14 jmc Exp $ |
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edhill |
1.24 |
C $Name: $ |
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adcroft |
1.2 |
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edhill |
1.24 |
#include "PACKAGES_CONFIG.h" |
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adcroft |
1.2 |
#include "CPP_OPTIONS.h" |
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cnh |
1.14 |
CBOP |
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C !ROUTINE: THE_CORRECTION_STEP |
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C !INTERFACE: |
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adcroft |
1.2 |
SUBROUTINE THE_CORRECTION_STEP(myTime, myIter, myThid) |
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cnh |
1.14 |
C !DESCRIPTION: \bv |
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C *==========================================================* |
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C | SUBROUTINE THE_CORRECTION_STEP |
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C *==========================================================* |
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C |1rst Part : Update U,V,T,S. |
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C | |
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C | The arrays used for time stepping are cycled. |
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C | Tracers: |
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jmc |
1.21 |
C | T(n) = Gt(n) |
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cnh |
1.14 |
C | Momentum: |
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jmc |
1.21 |
C | V(n) = Gv(n) - dt * grad Eta |
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cnh |
1.14 |
C | |
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C |part1: update U,V,T,S |
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jmc |
1.21 |
C | U*,V* (contained in gU,gV) have the surface |
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cnh |
1.14 |
C | pressure gradient term added and the result stored |
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C | in U,V (contained in uVel, vVel) |
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jmc |
1.19 |
C | T* (contained in gT) is copied to T (theta) |
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C | S* (contained in gS) is copied to S (salt) |
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cnh |
1.14 |
C | |
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jmc |
1.19 |
C |part2: Adjustments & Diagnostics |
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cnh |
1.14 |
C | o Convective Adjustment |
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C *==========================================================* |
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C \ev |
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C !USES: |
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adcroft |
1.2 |
IMPLICIT NONE |
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C == Global variables === |
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#include "SIZE.h" |
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#include "EEPARAMS.h" |
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#include "PARAMS.h" |
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#include "DYNVARS.h" |
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jmc |
1.16 |
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cnh |
1.14 |
C !INPUT/OUTPUT PARAMETERS: |
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adcroft |
1.2 |
C == Routine arguments == |
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C myTime - Current time in simulation |
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C myIter - Current iteration number in simulation |
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C myThid - Thread number for this instance of the routine. |
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_RL myTime |
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INTEGER myIter |
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INTEGER myThid |
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cnh |
1.14 |
C !LOCAL VARIABLES: |
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adcroft |
1.2 |
C == Local variables |
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jmc |
1.6 |
_RL phiSurfX(1-OLx:sNx+OLx,1-OLy:sNy+OLy) |
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_RL phiSurfY(1-OLx:sNx+OLx,1-OLy:sNy+OLy) |
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adcroft |
1.2 |
INTEGER iMin,iMax |
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INTEGER jMin,jMax |
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INTEGER bi,bj |
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INTEGER k,i,j |
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cnh |
1.14 |
CEOP |
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adcroft |
1.9 |
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adcroft |
1.2 |
DO bj=myByLo(myThid),myByHi(myThid) |
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DO bi=myBxLo(myThid),myBxHi(myThid) |
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heimbach |
1.7 |
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adcroft |
1.2 |
C-- Set up work arrays that need valid initial values |
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DO j=1-OLy,sNy+OLy |
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DO i=1-OLx,sNx+OLx |
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jmc |
1.6 |
phiSurfX(i,j)=0. |
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phiSurfY(i,j)=0. |
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adcroft |
1.2 |
ENDDO |
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ENDDO |
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C Loop range: Gradients of Eta are evaluated so valid |
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C range is all but first row and column in overlaps. |
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iMin = 1-OLx+1 |
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iMax = sNx+OLx |
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jMin = 1-OLy+1 |
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jMax = sNy+OLy |
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jmc |
1.6 |
C- Calculate gradient of surface Potentiel |
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CALL CALC_GRAD_PHI_SURF( |
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adcroft |
1.2 |
I bi,bj,iMin,iMax,jMin,jMax, |
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jmc |
1.5 |
I etaN, |
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jmc |
1.6 |
O phiSurfX,phiSurfY, |
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adcroft |
1.2 |
I myThid ) |
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C-- Loop over all layers, top to bottom |
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DO K=1,Nr |
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C- Update velocity fields: V(n) = V** - dt * grad Eta |
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adcroft |
1.3 |
IF (momStepping) |
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& CALL CORRECTION_STEP( |
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adcroft |
1.2 |
I bi,bj,iMin,iMax,jMin,jMax,K, |
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jmc |
1.6 |
I phiSurfX,phiSurfY,myTime,myThid ) |
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adcroft |
1.2 |
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jmc |
1.29 |
C- Update tracer fields: T(n) = T** |
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adcroft |
1.2 |
IF (tempStepping) |
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& CALL CYCLE_TRACER( |
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jmc |
1.29 |
I bi,bj,K, |
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U theta,gT, |
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I myTime,myIter,myThid ) |
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adcroft |
1.2 |
IF (saltStepping) |
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& CALL CYCLE_TRACER( |
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jmc |
1.29 |
I bi,bj,K, |
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U salt,gS, |
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I myTime,myIter,myThid ) |
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adcroft |
1.2 |
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#ifdef ALLOW_OBCS |
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IF (useOBCS) THEN |
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CALL OBCS_APPLY_UV(bi,bj,K,uVel,vVel,myThid) |
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ENDIF |
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#endif /* ALLOW_OBCS */ |
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C-- End DO K=1,Nr |
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ENDDO |
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adcroft |
1.9 |
C--- 2nd Part : Adjustment. |
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C |
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C Static stability is calculated and the tracers are |
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C convective adjusted where statically unstable. |
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adcroft |
1.2 |
C-- Convectively adjust new fields to be statically stable |
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mlosch |
1.20 |
iMin = 1 |
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iMax = sNx |
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jMin = 1 |
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jMax = sNy |
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mlosch |
1.25 |
CALL CONVECTIVE_ADJUSTMENT( |
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I bi, bj, iMin, iMax, jMin, jMax, |
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I myTime, myIter, myThid ) |
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adcroft |
1.2 |
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jmc |
1.28 |
C-- End of 1rst bi,bj loop |
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adcroft |
1.2 |
ENDDO |
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ENDDO |
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RETURN |
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END |
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