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C $Header: /u/gcmpack/MITgcm/pkg/icefront/icefront_thermodynamics.F,v 1.1 2010/01/20 23:33:45 dimitri Exp $ |
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C $Name: $ |
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|
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#include "ICEFRONT_OPTIONS.h" |
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|
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CBOP |
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C !ROUTINE: ICEFRONT_THERMODYNAMICS |
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C !INTERFACE: |
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SUBROUTINE ICEFRONT_THERMODYNAMICS( |
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I myTime, myIter, myThid ) |
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C !DESCRIPTION: \bv |
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C *=============================================================* |
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C | S/R ICEFRONT_THERMODYNAMICS |
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C | o shelf-ice main routine. |
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C | compute temperature and (virtual) salt flux at the |
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C | shelf-ice ocean interface |
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C | |
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C | stresses at the ice/water interface are computed in separate |
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C | routines that are called from mom_fluxform/mom_vecinv |
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C *=============================================================* |
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|
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C !USES: |
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IMPLICIT NONE |
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|
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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 "GRID.h" |
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#include "DYNVARS.h" |
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#include "FFIELDS.h" |
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#include "ICEFRONT.h" |
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|
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C !INPUT/OUTPUT PARAMETERS: |
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C === Routine arguments === |
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C myIter :: iteration counter for this thread |
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C myTime :: time counter for this thread |
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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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CEOP |
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|
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#ifdef ALLOW_ICEFRONT |
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C !LOCAL VARIABLES : |
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C === Local variables === |
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C I,J,K,Kp1,bi,bj :: loop counters |
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C tLoc, sLoc, pLoc :: local in-situ temperature, salinity, pressure |
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C theta/saltFreeze :: temperature and salinity of water at the |
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C ice-ocean interface (at the freezing point) |
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C freshWaterFlux :: local variable for fresh water melt flux due to |
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C melting in kg/m^2/s (negative density x melt rate) |
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C convertFW2SaltLoc:: local copy of convertFW2Salt |
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C cFac :: 1 for conservative form, 0, otherwise |
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C auxiliary variables and abbreviations: |
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C a0, a1, a2, b, c0 |
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C eps1, eps2, eps3, eps4, eps5, eps6, eps7 |
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C aqe, bqe, cqe, discrim, recip_aqe |
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C drKp1, recip_drLoc |
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INTEGER I,J,K,Kp1 |
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INTEGER bi,bj |
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_RL tLoc(1:sNx,1:sNy) |
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_RL sLoc(1:sNx,1:sNy) |
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_RL pLoc(1:sNx,1:sNy) |
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_RL thetaFreeze, saltFreeze |
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_RL freshWaterFlux, convertFW2SaltLoc |
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_RL a0, a1, a2, b, c0 |
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_RL eps1, eps2, eps3, eps4, eps5, eps6, eps7 |
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_RL cFac, rFac |
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_RL aqe, bqe, cqe, discrim, recip_aqe |
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_RL drKp1, recip_drLoc |
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_RL tmpFac |
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|
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_RL SW_TEMP |
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EXTERNAL SW_TEMP |
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|
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C---+----1----+----2----+----3----+----4----+----5----+----6----+----7-|--+----| |
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|
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C are we doing the conservative form of Jenkins et al. (2001)? |
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cFac = 0. _d 0 |
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IF ( ICEFRONTconserve ) cFac = 1. _d 0 |
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C with "real fresh water flux" (affecting ETAN), there is more to modify |
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rFac = 1. _d 0 |
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IF ( ICEFRONTconserve .AND. useRealFreshWaterFlux ) rFac = 0. _d 0 |
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C linear dependence of freezing point on salinity |
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a0 = -0.0575 _d 0 |
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a1 = 0.0 _d -0 |
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a2 = 0.0 _d -0 |
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c0 = 0.0901 _d 0 |
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b = -7.61 _d -4 |
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#ifdef ALLOW_ISOMIP_TD |
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IF ( useISOMIPTD ) THEN |
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C non-linear dependence of freezing point on salinity |
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a0 = -0.0575 _d 0 |
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a1 = 1.710523 _d -3 |
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a2 = -2.154996 _d -4 |
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b = -7.53 _d -4 |
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c0 = 0. _d 0 |
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ENDIF |
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convertFW2SaltLoc = convertFW2Salt |
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C hardcoding this value here is OK because it only applies to ISOMIP |
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C where this value is part of the protocol |
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IF ( convertFW2SaltLoc .EQ. -1. ) convertFW2SaltLoc = 33.4 _d 0 |
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#endif /* ALLOW_ISOMIP_TD */ |
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|
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DO bj = myByLo(myThid), myByHi(myThid) |
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DO bi = myBxLo(myThid), myBxHi(myThid) |
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DO J = 1-Oly,sNy+Oly |
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DO I = 1-Olx,sNx+Olx |
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icefrontHeatFlux (I,J,bi,bj) = 0. _d 0 |
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icefrontFreshWaterFlux(I,J,bi,bj) = 0. _d 0 |
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icefrontForcingT (I,J,bi,bj) = 0. _d 0 |
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icefrontForcingS (I,J,bi,bj) = 0. _d 0 |
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ENDDO |
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ENDDO |
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DO J = 1, sNy |
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DO I = 1, sNx |
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C-- make local copies of temperature, salinity and depth (pressure) |
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C-- underneath the ice |
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K = 1 |
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pLoc(I,J) = ABS(R_icefront(I,J,bi,bj)) |
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tLoc(I,J) = theta(I,J,K,bi,bj) |
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sLoc(I,J) = MAX(salt(I,J,K,bi,bj), 0. _d 0) |
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ENDDO |
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ENDDO |
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|
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C-- turn potential temperature into in-situ temperature relative |
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C-- to the surface |
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DO J = 1, sNy |
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DO I = 1, sNx |
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tLoc(I,J) = SW_TEMP(sLoc(I,J),tLoc(I,J),pLoc(I,J),0.D0) |
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ENDDO |
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ENDDO |
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|
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#ifdef ALLOW_ISOMIP_TD |
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IF ( useISOMIPTD ) THEN |
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DO J = 1, sNy |
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DO I = 1, sNx |
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K = 1 |
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IF ( K .NE. 0 .AND. pLoc(I,J) .GT. 0. _d 0 ) THEN |
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C-- Calculate freezing temperature as a function of salinity and pressure |
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thetaFreeze = |
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& sLoc(I,J) * ( a0 + a1*sqrt(sLoc(I,J)) + a2*sLoc(I,J) ) |
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& + b*pLoc(I,J) + c0 |
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C-- Calculate the upward heat and fresh water fluxes |
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icefrontHeatFlux(I,J,bi,bj) = maskC(I,J,K,bi,bj) * |
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& ICEFRONTheatTransCoeff * ( tLoc(I,J) - thetaFreeze ) |
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& *HeatCapacity_Cp*rUnit2mass |
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C upward heat flux into the shelf-ice implies basal melting, |
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C thus a downward (negative upward) fresh water flux (as a mass flux), |
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C and vice versa |
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icefrontFreshWaterFlux(I,J,bi,bj) = |
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& - icefrontHeatFlux(I,J,bi,bj) |
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& *recip_ICEFRONTlatentHeat |
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C-- compute surface tendencies |
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icefrontForcingT(i,j,bi,bj) = |
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& - icefrontHeatFlux(I,J,bi,bj) |
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& *recip_Cp*mass2rUnit |
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& - cFac * icefrontFreshWaterFlux(I,J,bi,bj)*mass2rUnit |
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& * ( thetaFreeze - tLoc(I,J) ) |
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icefrontForcingS(i,j,bi,bj) = |
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& icefrontFreshWaterFlux(I,J,bi,bj) * mass2rUnit |
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& * ( cFac*sLoc(I,J) + (1. _d 0-cFac)*convertFW2SaltLoc ) |
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C-- stress at the ice/water interface is computed in separate |
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C routines that are called from mom_fluxform/mom_vecinv |
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ELSE |
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icefrontHeatFlux (I,J,bi,bj) = 0. _d 0 |
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icefrontFreshWaterFlux(I,J,bi,bj) = 0. _d 0 |
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icefrontForcingT (I,J,bi,bj) = 0. _d 0 |
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icefrontForcingS (I,J,bi,bj) = 0. _d 0 |
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ENDIF |
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ENDDO |
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ENDDO |
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ELSE |
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#else |
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IF ( .TRUE. ) THEN |
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#endif /* ALLOW_ISOMIP_TD */ |
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C use BRIOS thermodynamics, following Hellmers PhD thesis: |
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C Hellmer, H., 1989, A two-dimensional model for the thermohaline |
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C circulation under an ice shelf, Reports on Polar Research, No. 60 |
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C (in German). |
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|
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C a few abbreviations |
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eps1 = rUnit2mass*HeatCapacity_Cp*ICEFRONTheatTransCoeff |
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eps2 = rUnit2mass*ICEFRONTlatentHeat*ICEFRONTsaltTransCoeff |
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eps5 = rUnit2mass*HeatCapacity_Cp*ICEFRONTsaltTransCoeff |
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|
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DO J = 1, sNy |
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DO I = 1, sNx |
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K = 1 |
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IF ( K .NE. 0 .AND. pLoc(I,J) .GT. 0. _d 0 ) THEN |
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C solve quadratic equation to get salinity at icefront-ocean interface |
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C note: this part of the code is not very intuitive as it involves |
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C many arbitrary abbreviations that were introduced to derive the |
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C correct form of the quadratic equation for salinity. The abbreviations |
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C only make sense in connection with my notes on this (M.Losch) |
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eps3 = rhoIcefront*ICEFRONTheatCapacity_Cp |
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& * ICEFRONTkappa/pLoc(I,J) |
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eps4 = b*pLoc(I,J) + c0 |
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eps6 = eps4 - tLoc(I,J) |
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eps7 = eps4 - ICEFRONTthetaSurface |
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aqe = a0 *(eps1+eps3) |
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recip_aqe = 0. _d 0 |
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IF ( aqe .NE. 0. _d 0 ) recip_aqe = 0.5 _d 0/aqe |
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bqe = eps1*eps6 + eps3*eps7 - eps2 |
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cqe = eps2*sLoc(I,J) |
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discrim = bqe*bqe - 4. _d 0*aqe*cqe |
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#undef ALLOW_ICEFRONT_DEBUG |
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#ifdef ALLOW_ICEFRONT_DEBUG |
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IF ( discrim .LT. 0. _d 0 ) THEN |
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print *, 'ml-icefront: discrim = ', discrim,aqe,bqe,cqe |
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print *, 'ml-icefront: pLoc = ', pLoc(I,J) |
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print *, 'ml-icefront: tLoc = ', tLoc(I,J) |
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print *, 'ml-icefront: sLoc = ', sLoc(I,J) |
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print *, 'ml-icefront: tsurface= ', |
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& ICEFRONTthetaSurface |
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print *, 'ml-icefront: eps1 = ', eps1 |
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print *, 'ml-icefront: eps2 = ', eps2 |
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print *, 'ml-icefront: eps3 = ', eps3 |
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print *, 'ml-icefront: eps4 = ', eps4 |
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print *, 'ml-icefront: eps5 = ', eps5 |
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print *, 'ml-icefront: eps6 = ', eps6 |
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print *, 'ml-icefront: eps7 = ', eps7 |
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print *, 'ml-icefront: rU2mass = ', rUnit2mass |
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print *, 'ml-icefront: rhoIce = ', rhoIcefront |
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print *, 'ml-icefront: cFac = ', cFac |
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print *, 'ml-icefront: Cp_W = ', HeatCapacity_Cp |
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print *, 'ml-icefront: Cp_I = ', |
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& ICEFRONTHeatCapacity_Cp |
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print *, 'ml-icefront: gammaT = ', |
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& ICEFRONTheatTransCoeff |
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print *, 'ml-icefront: gammaS = ', |
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& ICEFRONTsaltTransCoeff |
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print *, 'ml-icefront: lat.heat= ', |
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& ICEFRONTlatentHeat |
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STOP 'ABNORMAL END in S/R ICEFRONT_THERMODYNAMICS' |
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ENDIF |
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#endif /* ALLOW_ICEFRONT_DEBUG */ |
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saltFreeze = (- bqe - SQRT(discrim))*recip_aqe |
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IF ( saltFreeze .LT. 0. _d 0 ) |
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& saltFreeze = (- bqe + SQRT(discrim))*recip_aqe |
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thetaFreeze = a0*saltFreeze + eps4 |
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C-- upward fresh water flux due to melting (in kg/m^2/s) |
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freshWaterFlux = rUnit2mass*ICEFRONTsaltTransCoeff |
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& * ( saltFreeze - sLoc(I,J) ) / saltFreeze |
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C-- Calculate the upward heat and fresh water fluxes; |
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C-- MITgcm sign conventions: downward (negative) fresh water flux |
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C-- implies melting and due to upward (positive) heat flux |
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icefrontHeatFlux(I,J,bi,bj) = |
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& ( eps3*( thetaFreeze - ICEFRONTthetaSurface ) |
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& - cFac*freshWaterFlux*( ICEFRONTlatentHeat |
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& - HeatCapacity_Cp*( thetaFreeze - rFac*tLoc(I,J) ) ) |
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& ) |
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icefrontFreshWaterFlux(I,J,bi,bj) = freshWaterFlux |
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C-- compute surface tendencies |
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icefrontForcingT(i,j,bi,bj) = |
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& ( ICEFRONTheatTransCoeff |
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& - cFac*icefrontFreshWaterFlux(I,J,bi,bj)*mass2rUnit ) |
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& * ( thetaFreeze - tLoc(I,J) ) |
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icefrontForcingS(i,j,bi,bj) = |
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& ( ICEFRONTsaltTransCoeff |
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& - cFac*icefrontFreshWaterFlux(I,J,bi,bj)*mass2rUnit ) |
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& * ( saltFreeze - sLoc(I,J) ) |
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ELSE |
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icefrontHeatFlux (I,J,bi,bj) = 0. _d 0 |
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icefrontFreshWaterFlux(I,J,bi,bj) = 0. _d 0 |
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icefrontForcingT (I,J,bi,bj) = 0. _d 0 |
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icefrontForcingS (I,J,bi,bj) = 0. _d 0 |
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ENDIF |
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ENDDO |
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ENDDO |
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ENDIF |
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C endif (not) useISOMIPTD |
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ENDDO |
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ENDDO |
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|
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#ifdef ALLOW_DIAGNOSTICS |
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IF ( useDiagnostics ) THEN |
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CALL DIAGNOSTICS_FILL_RS(icefrontFreshWaterFlux,'SHIfwFlx', |
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& 0,1,0,1,1,myThid) |
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CALL DIAGNOSTICS_FILL_RS(icefrontHeatFlux, 'SHIhtFlx', |
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& 0,1,0,1,1,myThid) |
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C SHIForcT (Ice shelf forcing for theta [W/m2], >0 increases theta) |
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tmpFac = HeatCapacity_Cp*rUnit2mass |
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CALL DIAGNOSTICS_SCALE_FILL(icefrontForcingT,tmpFac,1, |
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& 'SHIForcT',0, 1,0,1,1,myThid) |
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C SHIForcS (Ice shelf forcing for salt [g/m2/s], >0 increases salt) |
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tmpFac = rUnit2mass |
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CALL DIAGNOSTICS_SCALE_FILL(icefrontForcingS,tmpFac,1, |
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& 'SHIForcS',0, 1,0,1,1,myThid) |
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ENDIF |
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#endif /* ALLOW_DIAGNOSTICS */ |
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|
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#endif /* ALLOW_ICEFRONT */ |
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RETURN |
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END |
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