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dimitri |
1.16 |
C $Header: /u/gcmpack/MITgcm/model/src/swfrac.F,v 1.15 2009/08/04 21:51:53 jmc Exp $ |
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cnh |
1.9 |
C $Name: $ |
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adcroft |
1.1 |
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edhill |
1.10 |
#include "PACKAGES_CONFIG.h" |
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adcroft |
1.1 |
#include "CPP_OPTIONS.h" |
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cnh |
1.9 |
CBOP |
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C !ROUTINE: SWFRAC |
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C !INTERFACE: |
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adcroft |
1.1 |
SUBROUTINE SWFRAC( |
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jmc |
1.13 |
I imax, fact, |
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U swdk, |
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I myTime, myIter, myThid ) |
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cnh |
1.9 |
C !DESCRIPTION: \bv |
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C *==========================================================* |
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jmc |
1.13 |
C | SUBROUTINE SWFRAC |
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cnh |
1.9 |
C | o Compute solar short-wave flux penetration. |
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C *==========================================================* |
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jmc |
1.13 |
C | Compute fraction of solar short-wave flux penetrating to |
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C | specified depth, swdk, due to exponential decay in |
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C | Jerlov water type jwtype. |
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C | Reference : Two band solar absorption model of Paulson |
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C | and Simpson (1977, JPO, 7, 952-956) |
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C | Notes |
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C | ===== |
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dimitri |
1.16 |
C | Parameter jwtype is hardcoded to 2 for time being. |
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jmc |
1.13 |
C | Below 200m the solar penetration gets set to zero, |
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C | otherwise the limit for the exponent (+/- 5678) needs to |
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C | be taken care of. |
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C | Written by : Jan Morzel |
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C | Date : July 12, 1995 |
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cnh |
1.9 |
C *==========================================================* |
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C \ev |
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adcroft |
1.1 |
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cnh |
1.9 |
C !USES: |
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adcroft |
1.1 |
IMPLICIT NONE |
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cnh |
1.9 |
C !INPUT/OUTPUT PARAMETERS: |
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adcroft |
1.1 |
C === Routine arguments === |
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C input arguments |
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cnh |
1.9 |
C imax :: number of vertical grid points |
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C fact :: scale factor to apply to depth array |
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jmc |
1.13 |
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 |
1.5 |
INTEGER imax |
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heimbach |
1.6 |
_RL fact |
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jmc |
1.13 |
_RL myTime |
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INTEGER myIter |
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INTEGER myThid |
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heimbach |
1.6 |
C input/output arguments |
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cnh |
1.9 |
C swdk :: on input: vertical depth for desired sw fraction |
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C (fact*swdk) is negative distance (m) from surface |
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C swdk :: on output: short wave (radiation) fractional decay |
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heimbach |
1.6 |
_RL swdk(imax) |
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adcroft |
1.5 |
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cnh |
1.9 |
C !LOCAL VARIABLES: |
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adcroft |
1.5 |
C === Local variables === |
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jmc |
1.13 |
C max number of different water types |
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INTEGER nwtype , jwtype |
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heimbach |
1.6 |
PARAMETER(nwtype=5) |
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_RL facz |
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adcroft |
1.5 |
_RL rfac(nwtype),a1(nwtype),a2(nwtype) |
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adcroft |
1.1 |
INTEGER i |
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heimbach |
1.11 |
#ifdef ALLOW_CAL |
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jmc |
1.14 |
c _RL fac |
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c LOGICAL first, changed |
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c INTEGER count0, count1 |
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c INTEGER jerl(12) |
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c DATA jerl / 2 , 2 , 2 , 3 , 3 , 3 , 4 , 4 , 4 , 4 , 3 , 2 / |
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heimbach |
1.11 |
#endif /* ALLOW_CAL */ |
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cnh |
1.9 |
CEOP |
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jmc |
1.15 |
C Jerlov water type : |
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C I IA IB II III |
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C jwtype : 1 2 3 4 5 |
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DATA rfac / 0.58 _d 0, 0.62 _d 0, 0.67 _d 0, 0.77 _d 0, 0.78 _d 0/ |
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DATA a1 / 0.35 _d 0, 0.6 _d 0, 1.0 _d 0, 1.5 _d 0, 1.4 _d 0/ |
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DATA a2 / 23.0 _d 0, 20.0 _d 0, 17.0 _d 0, 14.0 _d 0, 7.9 _d 0/ |
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heimbach |
1.11 |
#ifdef ALLOW_CAL |
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edhill |
1.10 |
ceh3 this should have an IF ( useCALENDAR ) THEN |
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mlosch |
1.12 |
CML( |
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jmc |
1.13 |
C myIter = 0 makes cal_getMonthsRec always return count0=12 |
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mlosch |
1.12 |
C so that jerl(count0) = 2. |
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C The following lines are meant to be an example of how to |
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C include time dependent water types. However, it would probably |
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C make more sense to first think about a regionally varying |
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C water type before implementing a time dependence. |
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jmc |
1.13 |
CML CALL cal_GetMonthsRec( |
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mlosch |
1.12 |
CML O fac, first, changed, count0, count1, |
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jmc |
1.13 |
CML I myTime, myIter, myThid ) |
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mlosch |
1.12 |
CML jwtype=jerl(count0) |
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CML) |
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jwtype=2 |
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heimbach |
1.11 |
#else /* ALLOW_CAL undef */ |
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heimbach |
1.7 |
jwtype=2 |
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heimbach |
1.11 |
#endif /* ALLOW_CAL */ |
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heimbach |
1.6 |
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adcroft |
1.1 |
DO i = 1,imax |
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jmc |
1.15 |
facz = fact*swdk(i) |
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IF ( facz .LT. -200. _d 0 ) THEN |
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swdk(i) = 0. _d 0 |
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ELSE |
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swdk(i) = rfac(jwtype) * exp( facz/a1(jwtype) ) |
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& + (1. _d 0 - rfac(jwtype)) * exp( facz/a2(jwtype) ) |
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ENDIF |
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adcroft |
1.1 |
ENDDO |
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adcroft |
1.4 |
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adcroft |
1.1 |
RETURN |
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END |
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