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#include "FFIELDS.h" |
#include "FFIELDS.h" |
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#include "DYNVARS.h" |
#include "DYNVARS.h" |
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#include "GRID.h" |
#include "GRID.h" |
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#ifdef NONLIN_FRSURF |
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#include "SURFACE.h" |
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#endif |
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C !INPUT/OUTPUT PARAMETERS: |
C !INPUT/OUTPUT PARAMETERS: |
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C === Routine arguments === |
C === Routine arguments === |
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C !LOCAL VARIABLES: |
C !LOCAL VARIABLES: |
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C === Local variables === |
C === Local variables === |
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INTEGER i,j |
INTEGER i,j |
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C number of surface interface layer |
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INTEGER kSurface |
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_RL convertVol2Mass |
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CEOP |
CEOP |
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if ( buoyancyRelation .eq. 'OCEANICP' ) then |
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kSurface = Nr |
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convertVol2Mass = gravity*rhoConstFresh |
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else |
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kSurface = 1 |
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convertVol2Mass = 1. _d 0 |
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endif |
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DO j = jMin, jMax |
DO j = jMin, jMax |
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DO i = iMin, iMax |
DO i = iMin, iMax |
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c Zonal wind stress fu: |
c Zonal wind stress fu: |
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surfaceTendencyU(i,j,bi,bj) = fu(i,j,bi,bj) |
surfaceTendencyU(i,j,bi,bj) = |
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& *horiVertRatio*recip_rhoNil*recip_dRf(1) |
& fu(i,j,bi,bj)*horiVertRatio*recip_rhoConst |
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& *recip_drF(kSurface)*recip_hFacW(i,j,kSurface,bi,bj) |
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c Meridional wind stress fv: |
c Meridional wind stress fv: |
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surfaceTendencyV(i,j,bi,bj) = fV(i,j,bi,bj) |
surfaceTendencyV(i,j,bi,bj) = |
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& *horiVertRatio*recip_rhoNil*recip_dRf(1) |
& fv(i,j,bi,bj)*horiVertRatio*recip_rhoConst |
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& *recip_drF(kSurface)*recip_hFacS(i,j,kSurface,bi,bj) |
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c Net heat flux Qnet: |
c Net heat flux Qnet: |
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surfaceTendencyT(i,j,bi,bj) = -Qnet(i,j,bi,bj) |
surfaceTendencyT(i,j,bi,bj) = |
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& *recip_Cp*recip_rhoNil*recip_dRf(1) |
& -Qnet(i,j,bi,bj)*recip_Cp*horiVertRatio*recip_rhoConst |
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& - lambdaThetaClimRelax* |
& *recip_drF(kSurface)*recip_hFacC(i,j,kSurface,bi,bj) |
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& (theta(i,j,1,bi,bj)-SST(i,j,bi,bj)) |
& -lambdaThetaClimRelax |
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& *(theta(i,j,kSurface,bi,bj)-SST(i,j,bi,bj)) |
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#ifdef USE_NATURAL_BCS |
C Salt Flux (restoring term) : |
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c Freshwater flux EmPmR: |
C surfaceTendencyS(i,j,bi,bj) = |
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surfaceTendencyS(i,j,bi,bj) = EmPmR(i,j,bi,bj) |
C & -lambdaSaltClimRelax*(salt(i,j,kSurface,bi,bj)-SSS(i,j,bi,bj)) |
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& *recip_dRf(1)*salt(i,j,1,bi,bj) |
C notes : because truncation is different when this tendency is splitted |
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& - lambdaSaltClimRelax* |
C in 2 parts, keep this salt flux with freshwater flux (see below) |
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& (salt(i,j,1,bi,bj)-SSS(i,j,bi,bj)) |
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#else |
#ifdef ALLOW_PASSIVE_TRACER |
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c Freshwater flux EmPmR: |
c *** define the tracer surface tendency here *** |
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surfaceTendencyS(i,j,bi,bj) = EmPmR(i,j,bi,bj) |
#endif /* ALLOW_PASSIVE_TRACER */ |
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& *recip_dRf(1)*35. |
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& - lambdaSaltClimRelax* |
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& (salt(i,j,1,bi,bj)-SSS(i,j,bi,bj)) |
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#endif |
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ENDDO |
ENDDO |
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ENDDO |
ENDDO |
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c---+----1----+----2----+----3----+----4----+----5----+----6----+----7-|--+----| |
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C Surface salinity tendency and freshwater flux EmPmR: |
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IF (.NOT.useRealFreshWaterFlux .OR. nonlinFreeSurf .LE. 0 ) THEN |
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c- EmPmR does not really affect the water column height (for tracer budget) |
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c and is converted to a salt tendency. |
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IF (convertFW2Salt .EQ. -1.) THEN |
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c- converts EmPmR to salinity tendency using surface local salinity |
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DO j = jMin, jMax |
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DO i = iMin, iMax |
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surfaceTendencyS(i,j,bi,bj) = |
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& + EmPmR(i,j,bi,bj)*salt(i,j,kSurface,bi,bj) |
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& *recip_drF(kSurface)*recip_hFacC(i,j,kSurface,bi,bj) |
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& *convertVol2Mass |
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& -lambdaSaltClimRelax |
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& *(salt(i,j,kSurface,bi,bj)-SSS(i,j,bi,bj)) |
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ENDDO |
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ENDDO |
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ELSE |
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c- converts EmPmR to virtual salt flux using uniform salinity (default=35) |
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DO j = jMin, jMax |
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DO i = iMin, iMax |
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surfaceTendencyS(i,j,bi,bj) = |
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& + EmPmR(i,j,bi,bj)*convertFW2Salt |
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& *recip_drF(kSurface)*recip_hFacC(i,j,kSurface,bi,bj) |
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& *convertVol2Mass |
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& -lambdaSaltClimRelax |
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& *(salt(i,j,kSurface,bi,bj)-SSS(i,j,bi,bj)) |
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ENDDO |
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ENDDO |
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ENDIF |
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#ifdef NONLIN_FRSURF |
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c---+----1----+----2----+----3----+----4----+----5----+----6----+----7-|--+----| |
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ELSE |
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c Salt Flux (restoring term) : |
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DO j = jMin, jMax |
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DO i = iMin, iMax |
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surfaceTendencyS(i,j,bi,bj) = |
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& -lambdaSaltClimRelax |
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& *(salt(i,j,kSurface,bi,bj)-SSS(i,j,bi,bj)) |
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ENDDO |
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ENDDO |
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c- NonLin_FrSurf and RealFreshWaterFlux : PmEpR effectively changes |
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c the water column height ; temp., salt, (tracer) flux associated |
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c with this input/output of water is added here to the surface tendency. |
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c |
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c NB: PmEpR lag 1 time step behind EmPmR ( PmEpR_n = - EmPmR_n-1 ) to stay |
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c consitent with volume change (=d/dt etaN). |
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IF (temp_EvPrRn.NE.UNSET_RL) THEN |
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DO j = jMin, jMax |
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DO i = iMin, iMax |
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surfaceTendencyT(i,j,bi,bj) = surfaceTendencyT(i,j,bi,bj) |
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& + PmEpR(i,j,bi,bj) |
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& *( temp_EvPrRn - theta(i,j,kSurface,bi,bj) ) |
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& *recip_drF(kSurface)*recip_hFacC(i,j,kSurface,bi,bj) |
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& *convertVol2Mass |
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ENDDO |
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ENDDO |
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ENDIF |
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IF (salt_EvPrRn.NE.UNSET_RL) THEN |
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DO j = jMin, jMax |
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DO i = iMin, iMax |
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surfaceTendencyS(i,j,bi,bj) = surfaceTendencyS(i,j,bi,bj) |
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& + PmEpR(i,j,bi,bj) |
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& *( salt_EvPrRn - salt(i,j,kSurface,bi,bj) ) |
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& *recip_drF(kSurface)*recip_hFacC(i,j,kSurface,bi,bj) |
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& *convertVol2Mass |
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ENDDO |
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ENDDO |
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ENDIF |
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#ifdef ALLOW_PASSIVE_TRACER |
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c *** add the tracer flux associated with P-E+R here *** |
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c IF (trac_EvPrRn.NE.UNSET_RL) THEN |
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c & + PmEpR(i,j,bi,bj)*( trac_EvPrRn - tr1(i,j,kSurface,bi,bj) ) |
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c & *recip_drF(kSurface)*recip_hFacC(i,j,kSurface,bi,bj) |
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c ENDIF |
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#endif /* ALLOW_PASSIVE_TRACER */ |
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#endif /* NONLIN_FRSURF */ |
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ENDIF |
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RETURN |
RETURN |
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END |
END |