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jmc |
1.42 |
C $Header: /u/gcmpack/MITgcm/pkg/kpp/kpp_calc.F,v 1.41 2007/05/03 14:51:05 mlosch Exp $ |
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adcroft |
1.9 |
C $Name: $ |
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adcroft |
1.1 |
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#include "KPP_OPTIONS.h" |
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dimitri |
1.25 |
CBOP |
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C !ROUTINE: KPP_CALC |
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C !INTERFACE: ========================================================== |
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jmc |
1.42 |
SUBROUTINE KPP_CALC( |
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I bi, bj, myTime, myIter, myThid ) |
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dimitri |
1.25 |
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C !DESCRIPTION: \bv |
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jmc |
1.42 |
C *==========================================================* |
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adcroft |
1.1 |
C | SUBROUTINE KPP_CALC | |
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C | o Compute all KPP fields defined in KPP.h | |
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jmc |
1.42 |
C *==========================================================* |
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adcroft |
1.1 |
C | This subroutine serves as an interface between MITGCMUV | |
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C | code and NCOM 1-D routines in kpp_routines.F | |
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jmc |
1.42 |
C *==========================================================* |
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adcroft |
1.1 |
IMPLICIT NONE |
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c======================================================================= |
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c |
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c written by : jan morzel, august 11, 1994 |
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c modified by : jan morzel, january 25, 1995 : "dVsq" and 1d code |
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c detlef stammer, august, 1997 : for MIT GCM Classic |
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c d. menemenlis, july, 1998 : for MIT GCM UV |
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c |
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c compute vertical mixing coefficients based on the k-profile |
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c and oceanic planetary boundary layer scheme by large & mcwilliams. |
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c |
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c summary: |
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c - compute interior mixing everywhere: |
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c interior mixing gets computed at all interfaces due to constant |
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c internal wave background activity ("fkpm" and "fkph"), which |
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c is enhanced in places of static instability (local richardson |
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c number < 0). |
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c Additionally, mixing can be enhanced by adding contribution due |
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c to shear instability which is a function of the local richardson |
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c number |
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c - double diffusivity: |
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c interior mixing can be enhanced by double diffusion due to salt |
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c fingering and diffusive convection (ifdef "kmixdd"). |
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c - kpp scheme in the boundary layer: |
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c |
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c a.boundary layer depth: |
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c at every gridpoint the depth of the oceanic boundary layer |
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c ("hbl") gets computed by evaluating bulk richardson numbers. |
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c b.boundary layer mixing: |
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c within the boundary layer, above hbl, vertical mixing is |
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c determined by turbulent surface fluxes, and interior mixing at |
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c the lower boundary, i.e. at hbl. |
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c |
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jmc |
1.42 |
c this subroutine provides the interface between the MITGCM and |
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c the routine "kppmix", where boundary layer depth, vertical |
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adcroft |
1.1 |
c viscosity, vertical diffusivity, and counter gradient term (ghat) |
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c are computed slabwise. |
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c note: subroutine "kppmix" uses m-k-s units. |
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c |
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c time level: |
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c input tracer and velocity profiles are evaluated at time level |
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c tau, surface fluxes come from tau or tau-1. |
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c |
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c grid option: |
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c in this "1-grid" implementation, diffusivity and viscosity |
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c profiles are computed on the "t-grid" (by using velocity shear |
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c profiles averaged from the "u,v-grid" onto the "t-grid"; note, that |
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c the averaging includes zero values on coastal and seafloor grid |
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c points). viscosity on the "u,v-grid" is computed by averaging the |
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c "t-grid" viscosity values onto the "u,v-grid". |
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c |
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c vertical grid: |
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c mixing coefficients get evaluated at the bottom of the lowest |
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c layer, i.e., at depth zw(Nr). these values are only useful when |
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c the model ocean domain does not include the entire ocean down to |
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c the seafloor ("upperocean" setup) and allows flux through the |
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c bottom of the domain. for full-depth runs, these mixing |
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c coefficients are being zeroed out before leaving this subroutine. |
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c |
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c------------------------------------------------------------------------- |
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c global parameters updated by kpp_calc |
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c KPPviscAz - KPP eddy viscosity coefficient (m^2/s) |
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c KPPdiffKzT - KPP diffusion coefficient for temperature (m^2/s) |
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c KPPdiffKzS - KPP diffusion coefficient for salt and tracers (m^2/s) |
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c KPPghat - Nonlocal transport coefficient (s/m^2) |
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c KPPhbl - Boundary layer depth on "t-grid" (m) |
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c KPPfrac - Fraction of short-wave flux penetrating mixing layer |
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c-- KPP_CALC computes vertical viscosity and diffusivity for region |
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c (-2:sNx+3,-2:sNy+3) as required by CALC_DIFFUSIVITY and requires |
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jmc |
1.28 |
c values of uVel, vVel, surfaceForcingU, surfaceForcingV in the |
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heimbach |
1.2 |
c region (-2:sNx+4,-2:sNy+4). |
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adcroft |
1.1 |
c Hence overlap region needs to be set OLx=4, OLy=4. |
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dimitri |
1.25 |
c \ev |
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adcroft |
1.1 |
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dimitri |
1.25 |
C !USES: =============================================================== |
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adcroft |
1.1 |
#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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#include "KPP.h" |
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#include "KPP_PARAMS.h" |
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#include "FFIELDS.h" |
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#include "GRID.h" |
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dimitri |
1.36 |
#include "GAD.h" |
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mlosch |
1.35 |
#ifdef ALLOW_SHELFICE |
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# include "SHELFICE.h" |
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#endif /* ALLOW_SHELFICE */ |
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adcroft |
1.1 |
#ifdef ALLOW_AUTODIFF_TAMC |
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#include "tamc.h" |
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#include "tamc_keys.h" |
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#else /* ALLOW_AUTODIFF_TAMC */ |
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heimbach |
1.16 |
integer ikppkey |
116 |
adcroft |
1.1 |
#endif /* ALLOW_AUTODIFF_TAMC */ |
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jmc |
1.32 |
EXTERNAL DIFFERENT_MULTIPLE |
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LOGICAL DIFFERENT_MULTIPLE |
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adcroft |
1.1 |
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dimitri |
1.25 |
C !INPUT PARAMETERS: =================================================== |
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adcroft |
1.1 |
c Routine arguments |
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jmc |
1.42 |
c bi, bj :: Current tile indices |
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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 :: My Thread Id. number |
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adcroft |
1.1 |
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INTEGER bi, bj |
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jmc |
1.42 |
_RL myTime |
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INTEGER myIter |
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adcroft |
1.1 |
INTEGER myThid |
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#ifdef ALLOW_KPP |
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dimitri |
1.25 |
C !LOCAL VARIABLES: ==================================================== |
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heimbach |
1.4 |
c Local constants |
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c minusone, p0, p5, p25, p125, p0625 |
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c imin, imax, jmin, jmax - array computation indices |
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_RL minusone |
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parameter( minusone=-1.0) |
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dimitri |
1.37 |
_RL p0 , p5 , p25 , p125 , p0625 |
143 |
heimbach |
1.4 |
parameter( p0=0.0, p5=0.5, p25=0.25, p125=0.125, p0625=0.0625 ) |
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dimitri |
1.17 |
integer imin ,imax ,jmin ,jmax |
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heimbach |
1.15 |
parameter(imin=2-OLx,imax=sNx+OLx-1,jmin=2-OLy,jmax=sNy+OLy-1) |
146 |
heimbach |
1.4 |
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adcroft |
1.1 |
c Local arrays and variables |
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c work? (nx,ny) - horizontal working arrays |
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c ustar (nx,ny) - surface friction velocity (m/s) |
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c bo (nx,ny) - surface turbulent buoyancy forcing (m^2/s^3) |
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c bosol (nx,ny) - surface radiative buoyancy forcing (m^2/s^3) |
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c shsq (nx,ny,Nr) - local velocity shear squared |
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c at interfaces for ri_iwmix (m^2/s^2) |
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c dVsq (nx,ny,Nr) - velocity shear re surface squared |
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c at grid levels for bldepth (m^2/s^2) |
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c dbloc (nx,ny,Nr) - local delta buoyancy at interfaces |
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c for ri_iwmix and bldepth (m/s^2) |
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c Ritop (nx,ny,Nr) - numerator of bulk richardson number |
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c at grid levels for bldepth |
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c vddiff (nx,ny,Nrp2,1)- vertical viscosity on "t-grid" (m^2/s) |
161 |
dimitri |
1.24 |
c vddiff (nx,ny,Nrp2,2)- vert. diff. on next row for salt&tracers (m^2/s) |
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c vddiff (nx,ny,Nrp2,3)- vert. diff. on next row for temperature (m^2/s) |
163 |
adcroft |
1.1 |
c ghat (nx,ny,Nr) - nonlocal transport coefficient (s/m^2) |
164 |
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c hbl (nx,ny) - mixing layer depth (m) |
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c kmtj (nx,ny) - maximum number of wet levels in each column |
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c z0 (nx,ny) - Roughness length (m) |
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c zRef (nx,ny) - Reference depth: Hmix * epsilon (m) |
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c uRef (nx,ny) - Reference zonal velocity (m/s) |
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c vRef (nx,ny) - Reference meridional velocity (m/s) |
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171 |
dimitri |
1.37 |
integer work1 ( 1-OLx:sNx+OLx, 1-OLy:sNy+OLy ) |
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_RL worka ( 1-OLx:sNx+OLx, 1-OLy:sNy+OLy ) |
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_RL work2 ( 1-OLx:sNx+OLx, 1-OLy:sNy+OLy ) |
174 |
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_RL work3 ( 1-OLx:sNx+OLx, 1-OLy:sNy+OLy ) |
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_RL ustar ( 1-OLx:sNx+OLx, 1-OLy:sNy+OLy ) |
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_RL bo ( 1-OLx:sNx+OLx, 1-OLy:sNy+OLy ) |
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_RL bosol ( 1-OLx:sNx+OLx, 1-OLy:sNy+OLy ) |
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_RL shsq ( 1-OLx:sNx+OLx, 1-OLy:sNy+OLy, Nr ) |
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_RL dVsq ( 1-OLx:sNx+OLx, 1-OLy:sNy+OLy, Nr ) |
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_RL dbloc ( 1-OLx:sNx+OLx, 1-OLy:sNy+OLy, Nr ) |
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_RL Ritop ( 1-OLx:sNx+OLx, 1-OLy:sNy+OLy, Nr ) |
182 |
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_RL vddiff( 1-OLx:sNx+OLx, 1-OLy:sNy+OLy, 0:Nrp1, mdiff ) |
183 |
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_RL ghat ( 1-OLx:sNx+OLx, 1-OLy:sNy+OLy, Nr ) |
184 |
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_RL hbl ( 1-OLx:sNx+OLx, 1-OLy:sNy+OLy ) |
185 |
heimbach |
1.33 |
cph( |
186 |
dimitri |
1.37 |
_RL TTALPHA( 1-OLx:sNx+OLx, 1-OLy:sNy+OLy, Nrp1 ) |
187 |
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_RL SSBETA ( 1-OLx:sNx+OLx, 1-OLy:sNy+OLy, Nrp1 ) |
188 |
heimbach |
1.33 |
cph) |
189 |
adcroft |
1.1 |
#ifdef KPP_ESTIMATE_UREF |
190 |
dimitri |
1.37 |
_RL z0 ( 1-OLx:sNx+OLx, 1-OLy:sNy+OLy ) |
191 |
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_RL zRef ( 1-OLx:sNx+OLx, 1-OLy:sNy+OLy ) |
192 |
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_RL uRef ( 1-OLx:sNx+OLx, 1-OLy:sNy+OLy ) |
193 |
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_RL vRef ( 1-OLx:sNx+OLx, 1-OLy:sNy+OLy ) |
194 |
adcroft |
1.1 |
#endif /* KPP_ESTIMATE_UREF */ |
195 |
jmc |
1.42 |
|
196 |
dimitri |
1.37 |
_RL tempvar2 |
197 |
mlosch |
1.35 |
integer i, j, k, kp1, km1, im1, ip1, jm1, jp1 |
198 |
adcroft |
1.1 |
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199 |
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#ifdef KPP_ESTIMATE_UREF |
200 |
dimitri |
1.37 |
_RL tempvar1, dBdz1, dBdz2, ustarX, ustarY |
201 |
adcroft |
1.1 |
#endif |
202 |
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203 |
heimbach |
1.16 |
#ifdef ALLOW_AUTODIFF_TAMC |
204 |
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act1 = bi - myBxLo(myThid) |
205 |
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max1 = myBxHi(myThid) - myBxLo(myThid) + 1 |
206 |
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act2 = bj - myByLo(myThid) |
207 |
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max2 = myByHi(myThid) - myByLo(myThid) + 1 |
208 |
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act3 = myThid - 1 |
209 |
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max3 = nTx*nTy |
210 |
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act4 = ikey_dynamics - 1 |
211 |
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ikppkey = (act1 + 1) + act2*max1 |
212 |
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& + act3*max1*max2 |
213 |
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& + act4*max1*max2*max3 |
214 |
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#endif /* ALLOW_AUTODIFF_TAMC */ |
215 |
dimitri |
1.25 |
CEOP |
216 |
heimbach |
1.16 |
|
217 |
adcroft |
1.1 |
c Check to see if new vertical mixing coefficient should be computed now? |
218 |
jmc |
1.32 |
IF ( DIFFERENT_MULTIPLE(kpp_freq,myTime,deltaTClock) |
219 |
jmc |
1.31 |
1 .OR. myTime .EQ. startTime ) THEN |
220 |
jmc |
1.42 |
|
221 |
adcroft |
1.1 |
c----------------------------------------------------------------------- |
222 |
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c prepare input arrays for subroutine "kppmix" to compute |
223 |
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c viscosity and diffusivity and ghat. |
224 |
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c All input arrays need to be in m-k-s units. |
225 |
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c |
226 |
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c note: for the computation of the bulk richardson number in the |
227 |
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c "bldepth" subroutine, gradients of velocity and buoyancy are |
228 |
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c required at every depth. in the case of very fine vertical grids |
229 |
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c (thickness of top layer < 2m), the surface reference depth must |
230 |
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c be set to zref=epsilon/2*zgrid(k), and the reference value |
231 |
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c of velocity and buoyancy must be computed as vertical average |
232 |
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c between the surface and 2*zref. in the case of coarse vertical |
233 |
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c grids zref is zgrid(1)/2., and the surface reference value is |
234 |
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c simply the surface value at zgrid(1). |
235 |
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c----------------------------------------------------------------------- |
236 |
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237 |
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c------------------------------------------------------------------------ |
238 |
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c density related quantities |
239 |
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c -------------------------- |
240 |
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c |
241 |
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c work2 - density of surface layer (kg/m^3) |
242 |
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c dbloc - local buoyancy gradient at Nr interfaces |
243 |
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c g/rho{k+1,k+1} * [ drho{k,k+1}-drho{k+1,k+1} ] (m/s^2) |
244 |
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c dbsfc (stored in Ritop to conserve stack memory) |
245 |
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c - buoyancy difference with respect to the surface |
246 |
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c g * [ drho{1,k}/rho{1,k} - drho{k,k}/rho{k,k} ] (m/s^2) |
247 |
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c ttalpha (stored in vddiff(:,:,:,1) to conserve stack memory) |
248 |
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c - thermal expansion coefficient without 1/rho factor |
249 |
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c d(rho{k,k})/d(T(k)) (kg/m^3/C) |
250 |
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c ssbeta (stored in vddiff(:,:,:,2) to conserve stack memory) |
251 |
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c - salt expansion coefficient without 1/rho factor |
252 |
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c d(rho{k,k})/d(S(k)) (kg/m^3/PSU) |
253 |
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c------------------------------------------------------------------------ |
254 |
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255 |
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CALL TIMER_START('STATEKPP [KPP_CALC]', myThid) |
256 |
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CALL STATEKPP( |
257 |
mlosch |
1.40 |
O work2, dbloc, Ritop, |
258 |
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O TTALPHA, SSBETA, |
259 |
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I ikppkey, bi, bj, myThid ) |
260 |
adcroft |
1.1 |
CALL TIMER_STOP ('STATEKPP [KPP_CALC]', myThid) |
261 |
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262 |
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DO k = 1, Nr |
263 |
dimitri |
1.34 |
DO j = 1-OLy, sNy+OLy |
264 |
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DO i = 1-OLx, sNx+OLx |
265 |
adcroft |
1.1 |
ghat(i,j,k) = dbloc(i,j,k) |
266 |
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ENDDO |
267 |
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ENDDO |
268 |
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ENDDO |
269 |
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270 |
heimbach |
1.4 |
#ifdef KPP_SMOOTH_DBLOC |
271 |
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c horizontally smooth dbloc with a 121 filter |
272 |
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c smooth dbloc stored in ghat to save space |
273 |
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c dbloc(k) is buoyancy gradientnote between k and k+1 |
274 |
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c levels therefore k+1 mask must be used |
275 |
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276 |
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DO k = 1, Nr-1 |
277 |
dimitri |
1.37 |
CALL SMOOTH_HORIZ ( |
278 |
heimbach |
1.4 |
I k+1, bi, bj, |
279 |
jmc |
1.42 |
U ghat (1-OLx,1-OLy,k), |
280 |
mlosch |
1.40 |
I myThid ) |
281 |
heimbach |
1.4 |
ENDDO |
282 |
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283 |
adcroft |
1.1 |
#endif /* KPP_SMOOTH_DBLOC */ |
284 |
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285 |
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#ifdef KPP_SMOOTH_DENS |
286 |
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c horizontally smooth density related quantities with 121 filters |
287 |
dimitri |
1.37 |
CALL SMOOTH_HORIZ ( |
288 |
heimbach |
1.4 |
I 1, bi, bj, |
289 |
jmc |
1.42 |
U work2, |
290 |
mlosch |
1.40 |
I myThid ) |
291 |
adcroft |
1.1 |
DO k = 1, Nr |
292 |
dimitri |
1.37 |
CALL SMOOTH_HORIZ ( |
293 |
heimbach |
1.4 |
I k+1, bi, bj, |
294 |
jmc |
1.42 |
U dbloc (1-OLx,1-OLy,k), |
295 |
mlosch |
1.40 |
I myThid ) |
296 |
dimitri |
1.37 |
CALL SMOOTH_HORIZ ( |
297 |
adcroft |
1.1 |
I k, bi, bj, |
298 |
jmc |
1.42 |
U Ritop (1-OLx,1-OLy,k), |
299 |
mlosch |
1.40 |
I myThid ) |
300 |
dimitri |
1.37 |
CALL SMOOTH_HORIZ ( |
301 |
adcroft |
1.1 |
I k, bi, bj, |
302 |
jmc |
1.42 |
U TTALPHA(1-OLx,1-OLy,k), |
303 |
mlosch |
1.40 |
I myThid ) |
304 |
dimitri |
1.37 |
CALL SMOOTH_HORIZ ( |
305 |
adcroft |
1.1 |
I k, bi, bj, |
306 |
jmc |
1.42 |
U SSBETA(1-OLx,1-OLy,k), |
307 |
mlosch |
1.40 |
I myThid ) |
308 |
adcroft |
1.1 |
ENDDO |
309 |
|
|
#endif /* KPP_SMOOTH_DENS */ |
310 |
|
|
|
311 |
|
|
DO k = 1, Nr |
312 |
mlosch |
1.35 |
km1 = max(1,k-1) |
313 |
dimitri |
1.34 |
DO j = 1-OLy, sNy+OLy |
314 |
|
|
DO i = 1-OLx, sNx+OLx |
315 |
adcroft |
1.1 |
|
316 |
|
|
c zero out dbloc over land points (so that the convective |
317 |
|
|
c part of the interior mixing can be diagnosed) |
318 |
jmc |
1.28 |
dbloc(i,j,k) = dbloc(i,j,k) * maskC(i,j,k,bi,bj) |
319 |
mlosch |
1.35 |
& * maskC(i,j,km1,bi,bj) |
320 |
jmc |
1.28 |
ghat(i,j,k) = ghat(i,j,k) * maskC(i,j,k,bi,bj) |
321 |
mlosch |
1.35 |
& * maskC(i,j,km1,bi,bj) |
322 |
jmc |
1.28 |
Ritop(i,j,k) = Ritop(i,j,k) * maskC(i,j,k,bi,bj) |
323 |
mlosch |
1.35 |
& * maskC(i,j,km1,bi,bj) |
324 |
adcroft |
1.1 |
if(k.eq.nzmax(i,j,bi,bj)) then |
325 |
|
|
dbloc(i,j,k) = p0 |
326 |
|
|
ghat(i,j,k) = p0 |
327 |
|
|
Ritop(i,j,k) = p0 |
328 |
|
|
endif |
329 |
|
|
|
330 |
|
|
c numerator of bulk richardson number on grid levels |
331 |
|
|
c note: land and ocean bottom values need to be set to zero |
332 |
|
|
c so that the subroutine "bldepth" works correctly |
333 |
|
|
Ritop(i,j,k) = (zgrid(1)-zgrid(k)) * Ritop(i,j,k) |
334 |
|
|
|
335 |
jmc |
1.42 |
ENDDO |
336 |
|
|
ENDDO |
337 |
|
|
ENDDO |
338 |
adcroft |
1.1 |
|
339 |
heimbach |
1.11 |
cph( |
340 |
|
|
cph this avoids a single or double recomp./call of statekpp |
341 |
heimbach |
1.16 |
CADJ store work2 = comlev1_kpp, key = ikppkey |
342 |
heimbach |
1.27 |
#ifdef KPP_AUTODIFF_EXCESSIVE_STORE |
343 |
heimbach |
1.16 |
CADJ store dbloc, Ritop, ghat = comlev1_kpp, key = ikppkey |
344 |
|
|
CADJ store vddiff = comlev1_kpp, key = ikppkey |
345 |
heimbach |
1.33 |
CADJ store TTALPHA, SSBETA = comlev1_kpp, key = ikppkey |
346 |
heimbach |
1.11 |
#endif |
347 |
|
|
cph) |
348 |
|
|
|
349 |
mlosch |
1.35 |
CML#ifdef ALLOW_SHELFICE |
350 |
|
|
CMLC For the pbl parameterisation to work underneath the ice shelves |
351 |
|
|
CMLC it needs to know the surface (ice-ocean) fluxes. However, masking |
352 |
|
|
CMLC and indexing problems make this part of the code not work |
353 |
|
|
CMLC underneath the ice shelves and the following lines are only here |
354 |
|
|
CMLC to remind me that this still needs to be sorted out. |
355 |
mlosch |
1.41 |
CML shelfIceFac = 0. _d 0 |
356 |
|
|
CML IF ( useShelfIce ) selfIceFac = 1. _d 0 |
357 |
mlosch |
1.35 |
CML DO j = jmin, jmax |
358 |
|
|
CML DO i = imin, imax |
359 |
mlosch |
1.41 |
CML surfForcT = surfaceForcingT(i,j,bi,bj) |
360 |
|
|
CML & + shelficeForcingT(i,j,bi,bj) * shelfIceFac |
361 |
|
|
CML surfForcS = surfaceForcingS(i,j,bi,bj) |
362 |
|
|
CML & + shelficeForcingS(i,j,bi,bj) * shelfIceFac |
363 |
jmc |
1.42 |
CML ENDDO |
364 |
|
|
CML ENDDO |
365 |
mlosch |
1.35 |
CML#endif /* ALLOW_SHELFICE */ |
366 |
heimbach |
1.11 |
|
367 |
mlosch |
1.41 |
c------------------------------------------------------------------------ |
368 |
|
|
c friction velocity, turbulent and radiative surface buoyancy forcing |
369 |
|
|
c ------------------------------------------------------------------- |
370 |
|
|
c taux / rho = surfaceForcingU (N/m^2) |
371 |
|
|
c tauy / rho = surfaceForcingV (N/m^2) |
372 |
|
|
c ustar = sqrt( sqrt( taux^2 + tauy^2 ) / rho ) (m/s) |
373 |
|
|
c bo = - g * ( alpha*surfaceForcingT + |
374 |
|
|
c beta *surfaceForcingS ) / rho (m^2/s^3) |
375 |
|
|
c bosol = - g * alpha * Qsw * drF(1) / rho (m^2/s^3) |
376 |
adcroft |
1.1 |
c------------------------------------------------------------------------ |
377 |
|
|
c velocity shear |
378 |
|
|
c -------------- |
379 |
|
|
c Get velocity shear squared, averaged from "u,v-grid" |
380 |
|
|
c onto "t-grid" (in (m/s)**2): |
381 |
|
|
c dVsq(k)=(Uref-U(k))**2+(Vref-V(k))**2 at grid levels |
382 |
|
|
c shsq(k)=(U(k)-U(k+1))**2+(V(k)-V(k+1))**2 at interfaces |
383 |
mlosch |
1.41 |
c |
384 |
|
|
c note: Vref can depend on the surface fluxes that is why we compute |
385 |
|
|
c dVsq in the subroutine that does the surface related stuff |
386 |
|
|
c (admittedly this is a bit messy) |
387 |
adcroft |
1.1 |
c------------------------------------------------------------------------ |
388 |
jmc |
1.42 |
|
389 |
mlosch |
1.41 |
CALL KPP_FORCING_SURF( |
390 |
|
|
I work2, surfaceForcingU, surfaceForcingV, |
391 |
jmc |
1.42 |
I surfaceForcingT, surfaceForcingS, surfaceForcingTice, |
392 |
|
|
I Qsw, ttalpha, ssbeta, |
393 |
mlosch |
1.41 |
O ustar, bo, bosol, dVsq, |
394 |
|
|
I ikppkey, iMin, iMax, jMin, jMax, bi, bj, myTime, myThid ) |
395 |
|
|
|
396 |
|
|
CMLcph( |
397 |
|
|
CMLCADJ store ustar = comlev1_kpp, key = ikppkey |
398 |
|
|
CMLcph) |
399 |
adcroft |
1.1 |
|
400 |
heimbach |
1.4 |
c initialize arrays to zero |
401 |
|
|
DO k = 1, Nr |
402 |
mlosch |
1.41 |
DO j = 1-OLy, sNy+OLy |
403 |
|
|
DO i = 1-OLx, sNx+OLx |
404 |
|
|
shsq(i,j,k) = p0 |
405 |
jmc |
1.42 |
ENDDO |
406 |
|
|
ENDDO |
407 |
|
|
ENDDO |
408 |
adcroft |
1.1 |
|
409 |
|
|
c shsq computation |
410 |
|
|
DO k = 1, Nrm1 |
411 |
mlosch |
1.41 |
kp1 = k + 1 |
412 |
|
|
DO j = jmin, jmax |
413 |
|
|
jm1 = j - 1 |
414 |
|
|
jp1 = j + 1 |
415 |
|
|
DO i = imin, imax |
416 |
|
|
im1 = i - 1 |
417 |
|
|
ip1 = i + 1 |
418 |
|
|
shsq(i,j,k) = p5 * ( |
419 |
jmc |
1.42 |
& (uVel(i, j, k,bi,bj)-uVel(i, j, kp1,bi,bj)) * |
420 |
|
|
& (uVel(i, j, k,bi,bj)-uVel(i, j, kp1,bi,bj)) + |
421 |
|
|
& (uVel(ip1,j, k,bi,bj)-uVel(ip1,j, kp1,bi,bj)) * |
422 |
|
|
& (uVel(ip1,j, k,bi,bj)-uVel(ip1,j, kp1,bi,bj)) + |
423 |
|
|
& (vVel(i, j, k,bi,bj)-vVel(i, j, kp1,bi,bj)) * |
424 |
|
|
& (vVel(i, j, k,bi,bj)-vVel(i, j, kp1,bi,bj)) + |
425 |
|
|
& (vVel(i, jp1,k,bi,bj)-vVel(i, jp1,kp1,bi,bj)) * |
426 |
|
|
& (vVel(i, jp1,k,bi,bj)-vVel(i, jp1,kp1,bi,bj)) ) |
427 |
adcroft |
1.1 |
#ifdef KPP_SMOOTH_SHSQ |
428 |
mlosch |
1.41 |
shsq(i,j,k) = p5 * shsq(i,j,k) + p125 * ( |
429 |
jmc |
1.42 |
& (uVel(i, jm1,k,bi,bj)-uVel(i, jm1,kp1,bi,bj)) * |
430 |
|
|
& (uVel(i, jm1,k,bi,bj)-uVel(i, jm1,kp1,bi,bj)) + |
431 |
|
|
& (uVel(ip1,jm1,k,bi,bj)-uVel(ip1,jm1,kp1,bi,bj)) * |
432 |
|
|
& (uVel(ip1,jm1,k,bi,bj)-uVel(ip1,jm1,kp1,bi,bj)) + |
433 |
|
|
& (uVel(i, jp1,k,bi,bj)-uVel(i, jp1,kp1,bi,bj)) * |
434 |
|
|
& (uVel(i, jp1,k,bi,bj)-uVel(i, jp1,kp1,bi,bj)) + |
435 |
|
|
& (uVel(ip1,jp1,k,bi,bj)-uVel(ip1,jp1,kp1,bi,bj)) * |
436 |
|
|
& (uVel(ip1,jp1,k,bi,bj)-uVel(ip1,jp1,kp1,bi,bj)) + |
437 |
|
|
& (vVel(im1,j, k,bi,bj)-vVel(im1,j, kp1,bi,bj)) * |
438 |
|
|
& (vVel(im1,j, k,bi,bj)-vVel(im1,j, kp1,bi,bj)) + |
439 |
|
|
& (vVel(im1,jp1,k,bi,bj)-vVel(im1,jp1,kp1,bi,bj)) * |
440 |
|
|
& (vVel(im1,jp1,k,bi,bj)-vVel(im1,jp1,kp1,bi,bj)) + |
441 |
|
|
& (vVel(ip1,j, k,bi,bj)-vVel(ip1,j, kp1,bi,bj)) * |
442 |
|
|
& (vVel(ip1,j, k,bi,bj)-vVel(ip1,j, kp1,bi,bj)) + |
443 |
|
|
& (vVel(ip1,jp1,k,bi,bj)-vVel(ip1,jp1,kp1,bi,bj)) * |
444 |
|
|
& (vVel(ip1,jp1,k,bi,bj)-vVel(ip1,jp1,kp1,bi,bj)) ) |
445 |
adcroft |
1.1 |
#endif |
446 |
jmc |
1.42 |
ENDDO |
447 |
|
|
ENDDO |
448 |
|
|
ENDDO |
449 |
adcroft |
1.1 |
|
450 |
heimbach |
1.11 |
cph( |
451 |
heimbach |
1.27 |
#ifdef KPP_AUTODIFF_EXCESSIVE_STORE |
452 |
heimbach |
1.16 |
CADJ store dvsq, shsq = comlev1_kpp, key = ikppkey |
453 |
heimbach |
1.11 |
#endif |
454 |
|
|
cph) |
455 |
|
|
|
456 |
adcroft |
1.1 |
c----------------------------------------------------------------------- |
457 |
|
|
c solve for viscosity, diffusivity, ghat, and hbl on "t-grid" |
458 |
|
|
c----------------------------------------------------------------------- |
459 |
|
|
|
460 |
dimitri |
1.36 |
c precompute background vertical diffusivities, which are needed for |
461 |
|
|
c matching diffusivities at bottom of KPP PBL |
462 |
|
|
CALL CALC_3D_DIFFUSIVITY( |
463 |
|
|
I bi,bj,1-Olx,sNx+OLx,1-Oly,sNy+OLy, |
464 |
|
|
I GAD_SALINITY, .FALSE., .FALSE., |
465 |
|
|
O KPPdiffKzS(1-Olx,1-Oly,1,bi,bj), |
466 |
|
|
I myThid) |
467 |
|
|
CALL CALC_3D_DIFFUSIVITY( |
468 |
|
|
I bi,bj,1-Olx,sNx+OLx,1-Oly,sNy+OLy, |
469 |
|
|
I GAD_TEMPERATURE, .FALSE., .FALSE., |
470 |
|
|
O KPPdiffKzT(1-Olx,1-Oly,1,bi,bj), |
471 |
|
|
I myThid) |
472 |
|
|
|
473 |
dimitri |
1.34 |
DO j = 1-OLy, sNy+OLy |
474 |
|
|
DO i = 1-OLx, sNx+OLx |
475 |
adcroft |
1.1 |
work1(i,j) = nzmax(i,j,bi,bj) |
476 |
|
|
work2(i,j) = Fcori(i,j,bi,bj) |
477 |
jmc |
1.42 |
ENDDO |
478 |
|
|
ENDDO |
479 |
adcroft |
1.1 |
CALL TIMER_START('KPPMIX [KPP_CALC]', myThid) |
480 |
|
|
CALL KPPMIX ( |
481 |
mlosch |
1.40 |
I work1, shsq, dVsq, ustar |
482 |
|
|
I , maskC(1-Olx,1-Oly,1,bi,bj) |
483 |
adcroft |
1.1 |
I , bo, bosol, dbloc, Ritop, work2 |
484 |
dimitri |
1.36 |
I , KPPdiffKzS(1-Olx,1-Oly,1,bi,bj) |
485 |
|
|
I , KPPdiffKzT(1-Olx,1-Oly,1,bi,bj) |
486 |
heimbach |
1.16 |
I , ikppkey |
487 |
adcroft |
1.1 |
O , vddiff |
488 |
|
|
U , ghat |
489 |
mlosch |
1.40 |
O , hbl |
490 |
|
|
I , mytime, mythid ) |
491 |
adcroft |
1.1 |
CALL TIMER_STOP ('KPPMIX [KPP_CALC]', myThid) |
492 |
|
|
|
493 |
|
|
c----------------------------------------------------------------------- |
494 |
heimbach |
1.4 |
c zero out land values and transfer to global variables |
495 |
adcroft |
1.1 |
c----------------------------------------------------------------------- |
496 |
|
|
|
497 |
|
|
DO j = jmin, jmax |
498 |
heimbach |
1.4 |
DO i = imin, imax |
499 |
|
|
DO k = 1, Nr |
500 |
mlosch |
1.35 |
km1 = max(1,k-1) |
501 |
jmc |
1.28 |
KPPviscAz(i,j,k,bi,bj) = vddiff(i,j,k-1,1) * maskC(i,j,k,bi,bj) |
502 |
mlosch |
1.35 |
& * maskC(i,j,km1,bi,bj) |
503 |
jmc |
1.28 |
KPPdiffKzS(i,j,k,bi,bj)= vddiff(i,j,k-1,2) * maskC(i,j,k,bi,bj) |
504 |
mlosch |
1.35 |
& * maskC(i,j,km1,bi,bj) |
505 |
jmc |
1.28 |
KPPdiffKzT(i,j,k,bi,bj)= vddiff(i,j,k-1,3) * maskC(i,j,k,bi,bj) |
506 |
mlosch |
1.35 |
& * maskC(i,j,km1,bi,bj) |
507 |
jmc |
1.28 |
KPPghat(i,j,k,bi,bj) = ghat(i,j,k) * maskC(i,j,k,bi,bj) |
508 |
mlosch |
1.35 |
& * maskC(i,j,km1,bi,bj) |
509 |
jmc |
1.42 |
ENDDO |
510 |
mlosch |
1.35 |
k = 1 |
511 |
|
|
#ifdef ALLOW_SHELFICE |
512 |
|
|
if ( useShelfIce ) k = kTopC(i,j,bi,bj) |
513 |
|
|
#endif /* ALLOW_SHELFICE */ |
514 |
|
|
KPPhbl(i,j,bi,bj) = hbl(i,j) * maskC(i,j,k,bi,bj) |
515 |
|
|
|
516 |
jmc |
1.42 |
ENDDO |
517 |
|
|
ENDDO |
518 |
adcroft |
1.1 |
|
519 |
|
|
#ifdef KPP_SMOOTH_VISC |
520 |
|
|
c horizontal smoothing of vertical viscosity |
521 |
|
|
DO k = 1, Nr |
522 |
heimbach |
1.4 |
CALL SMOOTH_HORIZ ( |
523 |
adcroft |
1.1 |
I k, bi, bj, |
524 |
jmc |
1.42 |
U KPPviscAz(1-OLx,1-OLy,k,bi,bj), |
525 |
mlosch |
1.40 |
I myThid ) |
526 |
jmc |
1.42 |
ENDDO |
527 |
|
|
C jmc: No EXCH inside bi,bj loop !!! |
528 |
|
|
c _EXCH_XYZ_R8(KPPviscAz , myThid ) |
529 |
adcroft |
1.1 |
#endif /* KPP_SMOOTH_VISC */ |
530 |
|
|
|
531 |
|
|
#ifdef KPP_SMOOTH_DIFF |
532 |
|
|
c horizontal smoothing of vertical diffusivity |
533 |
|
|
DO k = 1, Nr |
534 |
heimbach |
1.4 |
CALL SMOOTH_HORIZ ( |
535 |
adcroft |
1.1 |
I k, bi, bj, |
536 |
jmc |
1.42 |
U KPPdiffKzS(1-OLx,1-OLy,k,bi,bj), |
537 |
mlosch |
1.40 |
I myThid ) |
538 |
heimbach |
1.4 |
CALL SMOOTH_HORIZ ( |
539 |
adcroft |
1.1 |
I k, bi, bj, |
540 |
jmc |
1.42 |
U KPPdiffKzT(1-OLx,1-OLy,k,bi,bj), |
541 |
mlosch |
1.40 |
I myThid ) |
542 |
jmc |
1.42 |
ENDDO |
543 |
adcroft |
1.1 |
#endif /* KPP_SMOOTH_DIFF */ |
544 |
heimbach |
1.11 |
|
545 |
|
|
cph( |
546 |
|
|
cph crucial: this avoids full recomp./call of kppmix |
547 |
heimbach |
1.16 |
CADJ store KPPhbl = comlev1_kpp, key = ikppkey |
548 |
heimbach |
1.11 |
cph) |
549 |
adcroft |
1.1 |
|
550 |
|
|
C Compute fraction of solar short-wave flux penetrating to |
551 |
|
|
C the bottom of the mixing layer. |
552 |
|
|
DO j=1-OLy,sNy+OLy |
553 |
|
|
DO i=1-OLx,sNx+OLx |
554 |
|
|
worka(i,j) = KPPhbl(i,j,bi,bj) |
555 |
|
|
ENDDO |
556 |
|
|
ENDDO |
557 |
|
|
CALL SWFRAC( |
558 |
heimbach |
1.4 |
I (sNx+2*OLx)*(sNy+2*OLy), minusone, |
559 |
jmc |
1.42 |
U worka, |
560 |
|
|
I myTime, myIter, myThid ) |
561 |
adcroft |
1.1 |
DO j=1-OLy,sNy+OLy |
562 |
|
|
DO i=1-OLx,sNx+OLx |
563 |
heimbach |
1.4 |
KPPfrac(i,j,bi,bj) = worka(i,j) |
564 |
adcroft |
1.1 |
ENDDO |
565 |
|
|
ENDDO |
566 |
|
|
|
567 |
|
|
ENDIF |
568 |
|
|
|
569 |
adcroft |
1.9 |
#endif /* ALLOW_KPP */ |
570 |
adcroft |
1.1 |
|
571 |
heimbach |
1.8 |
RETURN |
572 |
|
|
END |
573 |
|
|
|
574 |
jmc |
1.42 |
SUBROUTINE KPP_CALC_DUMMY( |
575 |
|
|
I bi, bj, myTime, myIter, myThid ) |
576 |
|
|
C *==========================================================* |
577 |
heimbach |
1.8 |
C | SUBROUTINE KPP_CALC_DUMMY | |
578 |
|
|
C | o Compute all KPP fields defined in KPP.h | |
579 |
|
|
C | o Dummy routine for TAMC |
580 |
jmc |
1.42 |
C *==========================================================* |
581 |
heimbach |
1.8 |
C | This subroutine serves as an interface between MITGCMUV | |
582 |
|
|
C | code and NCOM 1-D routines in kpp_routines.F | |
583 |
jmc |
1.42 |
C *==========================================================* |
584 |
heimbach |
1.8 |
IMPLICIT NONE |
585 |
|
|
|
586 |
|
|
#include "SIZE.h" |
587 |
|
|
#include "EEPARAMS.h" |
588 |
|
|
#include "PARAMS.h" |
589 |
|
|
#include "KPP.h" |
590 |
|
|
#include "KPP_PARAMS.h" |
591 |
|
|
#include "GRID.h" |
592 |
dimitri |
1.36 |
#include "GAD.h" |
593 |
heimbach |
1.8 |
|
594 |
|
|
c Routine arguments |
595 |
jmc |
1.42 |
c bi, bj :: Current tile indices |
596 |
|
|
c myTime :: Current time in simulation |
597 |
|
|
c myIter :: Current iteration number in simulation |
598 |
|
|
c myThid :: My Thread Id. number |
599 |
heimbach |
1.8 |
|
600 |
|
|
INTEGER bi, bj |
601 |
jmc |
1.42 |
_RL myTime |
602 |
|
|
INTEGER myIter |
603 |
heimbach |
1.8 |
INTEGER myThid |
604 |
|
|
|
605 |
|
|
#ifdef ALLOW_KPP |
606 |
|
|
|
607 |
|
|
c Local constants |
608 |
|
|
integer i, j, k |
609 |
|
|
|
610 |
|
|
DO j=1-OLy,sNy+OLy |
611 |
|
|
DO i=1-OLx,sNx+OLx |
612 |
|
|
KPPhbl (i,j,bi,bj) = 1.0 |
613 |
|
|
KPPfrac(i,j,bi,bj) = 0.0 |
614 |
|
|
DO k = 1,Nr |
615 |
|
|
KPPghat (i,j,k,bi,bj) = 0.0 |
616 |
jmc |
1.21 |
KPPviscAz (i,j,k,bi,bj) = viscAr |
617 |
heimbach |
1.8 |
ENDDO |
618 |
|
|
ENDDO |
619 |
|
|
ENDDO |
620 |
dimitri |
1.36 |
|
621 |
|
|
CALL CALC_3D_DIFFUSIVITY( |
622 |
|
|
I bi,bj,1-Olx,sNx+OLx,1-Oly,sNy+OLy, |
623 |
|
|
I GAD_SALINITY, .FALSE., .FALSE., |
624 |
|
|
O KPPdiffKzS(1-Olx,1-Oly,1,bi,bj), |
625 |
|
|
I myThid) |
626 |
|
|
CALL CALC_3D_DIFFUSIVITY( |
627 |
|
|
I bi,bj,1-Olx,sNx+OLx,1-Oly,sNy+OLy, |
628 |
|
|
I GAD_TEMPERATURE, .FALSE., .FALSE., |
629 |
|
|
O KPPdiffKzT(1-Olx,1-Oly,1,bi,bj), |
630 |
|
|
I myThid) |
631 |
|
|
|
632 |
heimbach |
1.8 |
#endif |
633 |
adcroft |
1.1 |
RETURN |
634 |
|
|
END |