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C $Header: /u/gcmpack/models/MITgcmUV/model/src/calc_gs.F,v 1.31 2001/09/19 02:43:27 adcroft Exp $ |
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adcroft |
1.31 |
C $Name: $ |
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#include "CPP_OPTIONS.h" |
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CBOP |
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C !ROUTINE: CALC_GS |
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C !INTERFACE: |
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SUBROUTINE CALC_GS( |
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I bi,bj,iMin,iMax,jMin,jMax,k,kM1,kUp,kDown, |
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adcroft |
1.28 |
I xA,yA,uTrans,vTrans,rTrans,maskUp, |
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adcroft |
1.21 |
I KappaRS, |
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adcroft |
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U fVerS, |
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adcroft |
1.31 |
I myTime,myIter,myThid ) |
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C !DESCRIPTION: \bv |
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C *==========================================================* |
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C | SUBROUTINE CALC_GS |
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C | o Calculate the salt tendency terms. |
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C *==========================================================* |
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C | A procedure called EXTERNAL_FORCING_S is called from |
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C | here. These procedures can be used to add per problem |
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C | E-P flux source terms. |
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C | Note: Although it is slightly counter-intuitive the |
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C | EXTERNAL_FORCING routine is not the place to put |
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C | file I/O. Instead files that are required to |
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C | calculate the external source terms are generally |
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C | read during the model main loop. This makes the |
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C | logisitics of multi-processing simpler and also |
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C | makes the adjoint generation simpler. It also |
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C | allows for I/O to overlap computation where that |
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C | is supported by hardware. |
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C | Aside from the problem specific term the code here |
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C | forms the tendency terms due to advection and mixing |
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C | The baseline implementation here uses a centered |
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C | difference form for the advection term and a tensorial |
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C | divergence of a flux form for the diffusive term. The |
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C | diffusive term is formulated so that isopycnal mixing and |
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C | GM-style subgrid-scale terms can be incorporated b simply |
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C | setting the diffusion tensor terms appropriately. |
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C *==========================================================* |
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C \ev |
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C !USES: |
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IMPLICIT NONE |
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C == GLobal variables == |
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#include "SIZE.h" |
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#include "DYNVARS.h" |
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#include "EEPARAMS.h" |
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#include "PARAMS.h" |
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adcroft |
1.30 |
#include "GAD.h" |
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1.1 |
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C !INPUT/OUTPUT PARAMETERS: |
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C == Routine arguments == |
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C fVerS :: Flux of salt (S) in the vertical |
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1.1 |
C direction at the upper(U) and lower(D) faces of a cell. |
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1.32 |
C maskUp :: Land mask used to denote base of the domain. |
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C xA :: Tracer cell face area normal to X |
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C yA :: Tracer cell face area normal to X |
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C uTrans :: Zonal volume transport through cell face |
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C vTrans :: Meridional volume transport through cell face |
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C rTrans :: Vertical volume transport through cell face |
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C bi, bj, iMin, iMax, jMin, jMax :: Range of points for which calculation |
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C results will be set. |
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C myThid :: Instance number for this innvocation of CALC_GT |
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_RL fVerS (1-OLx:sNx+OLx,1-OLy:sNy+OLy,2) |
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_RS xA (1-OLx:sNx+OLx,1-OLy:sNy+OLy) |
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_RS yA (1-OLx:sNx+OLx,1-OLy:sNy+OLy) |
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_RL uTrans(1-OLx:sNx+OLx,1-OLy:sNy+OLy) |
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_RL vTrans(1-OLx:sNx+OLx,1-OLy:sNy+OLy) |
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_RL rTrans(1-OLx:sNx+OLx,1-OLy:sNy+OLy) |
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_RS maskUp(1-OLx:sNx+OLx,1-OLy:sNy+OLy) |
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_RL KappaRS(1-OLx:sNx+OLx,1-OLy:sNy+OLy,Nr) |
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INTEGER k,kUp,kDown,kM1 |
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INTEGER bi,bj,iMin,iMax,jMin,jMax |
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_RL myTime |
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INTEGER myIter |
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INTEGER myThid |
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CEOP |
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heimbach |
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#ifdef ALLOW_AUTODIFF_TAMC |
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C-- only the kUp part of fverS is set in this subroutine |
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C-- the kDown is still required |
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fVerS(1,1,kDown) = fVerS(1,1,kDown) |
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adcroft |
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#endif |
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adcroft |
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CALL GAD_CALC_RHS( |
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I bi,bj,iMin,iMax,jMin,jMax,k,kM1,kUp,kDown, |
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I xA,yA,uTrans,vTrans,rTrans,maskUp, |
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I diffKhS, diffK4S, KappaRS, Salt, |
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I GAD_SALINITY, saltAdvScheme, |
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U fVerS, gS, |
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I myThid ) |
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C-- External forcing term(s) |
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CALL EXTERNAL_FORCING_S( |
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I iMin,iMax,jMin,jMax,bi,bj,k, |
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1.31 |
I myTime,myThid) |
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IF ( saltAdvScheme.EQ.ENUM_CENTERED_2ND |
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& .OR.saltAdvScheme.EQ.ENUM_UPWIND_3RD |
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& .OR.saltAdvScheme.EQ.ENUM_CENTERED_4TH ) THEN |
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CALL ADAMS_BASHFORTH2( |
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I bi, bj, K, |
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U gS, gSnm1, |
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I myIter, myThid ) |
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ENDIF |
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#ifdef NONLIN_FRSURF |
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IF (nonlinFreeSurf.GT.0) THEN |
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CALL FREESURF_RESCALE_G( |
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I bi, bj, K, |
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U gS, |
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I myThid ) |
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ENDIF |
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#endif /* NONLIN_FRSURF */ |
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cnh |
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RETURN |
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END |
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