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! |
module radlwsw_m |
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! $Header: /home/cvsroot/LMDZ4/libf/phylmd/radlwsw.F,v 1.4 2005/06/06 13:16:33 fairhead Exp $ |
|
| 3 |
! |
IMPLICIT none |
| 4 |
SUBROUTINE radlwsw(dist, rmu0, fract, |
|
| 5 |
. paprs, pplay,tsol,albedo, alblw, t,q,wo, |
contains |
| 6 |
. cldfra, cldemi, cldtaupd, |
|
| 7 |
. heat,heat0,cool,cool0,radsol,albpla, |
SUBROUTINE radlwsw(dist, mu0, fract, paprs, play, tsol, albedo, alblw, & |
| 8 |
. topsw,toplw,solsw,sollw, |
t, q, wo, cldfra, cldemi, cldtaupd, heat, heat0, cool, cool0, radsol, & |
| 9 |
. sollwdown, |
albpla, topsw, toplw, solsw, sollw, sollwdown, topsw0, toplw0, solsw0, & |
| 10 |
. topsw0,toplw0,solsw0,sollw0, |
sollw0, lwdn0, lwdn, lwup0, lwup, swdn0, swdn, swup0, swup, ok_ade, & |
| 11 |
. lwdn0, lwdn, lwup0, lwup, |
ok_aie, tau_ae, piz_ae, cg_ae, topswad, solswad, cldtaupi, topswai, & |
| 12 |
. swdn0, swdn, swup0, swup, |
solswai) |
| 13 |
. ok_ade, ok_aie, |
|
| 14 |
. tau_ae, piz_ae, cg_ae, |
! From LMDZ4/libf/phylmd/radlwsw.F, version 1.4 2005/06/06 13:16:33 |
| 15 |
. topswad, solswad, |
! Author: Z. X. Li (LMD/CNRS) |
| 16 |
. cldtaupi, topswai, solswai) |
! Date: 1996/07/19 |
| 17 |
c |
|
| 18 |
use dimphy |
! Objet : interface entre le modèle et les rayonnements solaire et |
| 19 |
use clesphys |
! infrarouge |
| 20 |
use YOMCST |
|
| 21 |
use raddim, only: kflev, kdlon |
! ATTENTION: swai and swad have to be interpreted in the following manner: |
| 22 |
use yoethf |
|
| 23 |
IMPLICIT none |
! not ok_ade and not ok_aie |
| 24 |
c====================================================================== |
! both are zero |
| 25 |
c Auteur(s): Z.X. Li (LMD/CNRS) date: 19960719 |
|
| 26 |
c Objet: interface entre le modele et les rayonnements |
! ok_ade and not ok_aie |
| 27 |
c Arguments: |
! aerosol direct forcing is F_{AD} = topsw - topswad |
| 28 |
c dist-----input-R- distance astronomique terre-soleil |
! indirect is zero |
| 29 |
c rmu0-----input-R- cosinus de l'angle zenithal |
|
| 30 |
c fract----input-R- duree d'ensoleillement normalisee |
! not ok_ade and ok_aie |
| 31 |
c co2_ppm--input-R- concentration du gaz carbonique (en ppm) |
! aerosol indirect forcing is F_{AI} = topsw - topswai |
| 32 |
c solaire--input-R- constante solaire (W/m**2) |
! direct is zero |
| 33 |
c paprs----input-R- pression a inter-couche (Pa) |
|
| 34 |
c pplay----input-R- pression au milieu de couche (Pa) |
! ok_ade and ok_aie |
| 35 |
c tsol-----input-R- temperature du sol (en K) |
! aerosol indirect forcing is F_{AI} = topsw - topswai |
| 36 |
c albedo---input-R- albedo du sol (entre 0 et 1) |
! aerosol direct forcing is F_{AD} = topswai - topswad |
| 37 |
c t--------input-R- temperature (K) |
|
| 38 |
c q--------input-R- vapeur d'eau (en kg/kg) |
USE clesphys, ONLY: solaire |
| 39 |
c wo-------input-R- contenu en ozone (en kg/kg) correction MPL 100505 |
USE dimphy, ONLY: klev, klon |
| 40 |
c cldfra---input-R- fraction nuageuse (entre 0 et 1) |
use lw_m, only: lw |
| 41 |
c cldtaupd---input-R- epaisseur optique des nuages dans le visible (present-day value) |
USE raddim, ONLY: kdlon |
| 42 |
c cldemi---input-R- emissivite des nuages dans l'IR (entre 0 et 1) |
USE suphec_m, ONLY: rg |
| 43 |
c ok_ade---input-L- apply the Aerosol Direct Effect or not? |
use sw_m, only: sw |
| 44 |
c ok_aie---input-L- apply the Aerosol Indirect Effect or not? |
USE yoethf_m, ONLY: rvtmp2 |
| 45 |
c tau_ae, piz_ae, cg_ae-input-R- aerosol optical properties (calculated in aeropt.F) |
|
| 46 |
c cldtaupi-input-R- epaisseur optique des nuages dans le visible |
! Arguments: |
| 47 |
c calculated for pre-industrial (pi) aerosol concentrations, i.e. with smaller |
|
| 48 |
c droplet concentration, thus larger droplets, thus generally cdltaupi cldtaupd |
real, intent(in):: dist ! distance astronomique terre-soleil |
| 49 |
c it is needed for the diagnostics of the aerosol indirect radiative forcing |
real, intent(in):: mu0(klon) ! cosinus de l'angle zenithal |
| 50 |
c |
real, intent(in):: fract(klon) ! duree d'ensoleillement normalisee |
| 51 |
c heat-----output-R- echauffement atmospherique (visible) (K/jour) |
real, intent(in):: paprs(klon, klev+1) ! pression a inter-couche (Pa) |
| 52 |
c cool-----output-R- refroidissement dans l'IR (K/jour) |
real, intent(in):: play(klon, klev) ! pression au milieu de couche (Pa) |
| 53 |
c radsol---output-R- bilan radiatif net au sol (W/m**2) (+ vers le bas) |
|
| 54 |
c albpla---output-R- albedo planetaire (entre 0 et 1) |
real tsol(klon), albedo(klon), alblw(klon) |
| 55 |
c topsw----output-R- flux solaire net au sommet de l'atm. |
! albedo---input-R- albedo du sol (entre 0 et 1) |
| 56 |
c toplw----output-R- ray. IR montant au sommet de l'atmosphere |
! tsol-----input-R- temperature du sol (en K) |
| 57 |
c solsw----output-R- flux solaire net a la surface |
real, intent(in):: t(klon, klev) |
| 58 |
c sollw----output-R- ray. IR montant a la surface |
! t--------input-R- temperature (K) |
| 59 |
c solswad---output-R- ray. solaire net absorbe a la surface (aerosol dir) |
real q(klon, klev) |
| 60 |
c topswad---output-R- ray. solaire absorbe au sommet de l'atm. (aerosol dir) |
! q--------input-R- vapeur d'eau (en kg/kg) |
| 61 |
c solswai---output-R- ray. solaire net absorbe a la surface (aerosol ind) |
|
| 62 |
c topswai---output-R- ray. solaire absorbe au sommet de l'atm. (aerosol ind) |
real, intent(in):: wo(klon, klev) |
| 63 |
c |
! column-density of ozone in a layer, in kilo-Dobsons |
| 64 |
c ATTENTION: swai and swad have to be interpreted in the following manner: |
|
| 65 |
c --------- |
real cldfra(klon, klev), cldemi(klon, klev) |
| 66 |
c ok_ade=F & ok_aie=F -both are zero |
! cldfra---input-R- fraction nuageuse (entre 0 et 1) |
| 67 |
c ok_ade=T & ok_aie=F -aerosol direct forcing is F_{AD} = topsw-topswad |
! cldemi---input-R- emissivite des nuages dans l'IR (entre 0 et 1) |
| 68 |
c indirect is zero |
|
| 69 |
c ok_ade=F & ok_aie=T -aerosol indirect forcing is F_{AI} = topsw-topswai |
real cldtaupd(klon, klev) |
| 70 |
c direct is zero |
! input-R- epaisseur optique des nuages dans le visible (present-day value) |
| 71 |
c ok_ade=T & ok_aie=T -aerosol indirect forcing is F_{AI} = topsw-topswai |
|
| 72 |
c aerosol direct forcing is F_{AD} = topswai-topswad |
real, intent(out):: heat(klon, klev) |
| 73 |
c |
! échauffement atmosphérique (visible) (K/jour) |
| 74 |
|
|
| 75 |
c====================================================================== |
real heat0(klon, klev) |
| 76 |
c |
real cool(klon, klev) |
| 77 |
real rmu0(klon), fract(klon), dist |
! cool-----output-R- refroidissement dans l'IR (K/jour) |
| 78 |
cIM real co2_ppm |
real cool0(klon, klev) |
| 79 |
cIM real solaire |
real radsol(klon) |
| 80 |
c |
! radsol---output-R- bilan radiatif net au sol (W/m**2) (+ vers le bas) |
| 81 |
real, intent(in):: paprs(klon,klev+1) |
real albpla(klon) |
| 82 |
real, intent(in):: pplay(klon,klev) |
! albpla---output-R- albedo planetaire (entre 0 et 1) |
| 83 |
real albedo(klon), alblw(klon), tsol(klon) |
real topsw(klon) |
| 84 |
real t(klon,klev), q(klon,klev) |
! topsw----output-R- flux solaire net au sommet de l'atm. |
| 85 |
real, intent(in):: wo(klon,klev) |
|
| 86 |
real cldfra(klon,klev), cldemi(klon,klev), cldtaupd(klon,klev) |
real, intent(out):: toplw(klon) |
| 87 |
real heat(klon,klev), cool(klon,klev) |
! rayonnement infrarouge montant au sommet de l'atmosphère |
| 88 |
real heat0(klon,klev), cool0(klon,klev) |
|
| 89 |
real radsol(klon), topsw(klon), toplw(klon) |
real, intent(out):: solsw(klon) ! flux solaire net à la surface |
| 90 |
real solsw(klon), sollw(klon), albpla(klon) |
|
| 91 |
real topsw0(klon), toplw0(klon), solsw0(klon), sollw0(klon) |
real, intent(out):: sollw(klon) |
| 92 |
real sollwdown(klon) |
! rayonnement infrarouge montant à la surface |
| 93 |
cIM output 3D |
|
| 94 |
REAL*8 ZFSUP(KDLON,KFLEV+1) |
real, intent(out):: sollwdown(klon) |
| 95 |
REAL*8 ZFSDN(KDLON,KFLEV+1) |
real topsw0(klon) |
| 96 |
REAL*8 ZFSUP0(KDLON,KFLEV+1) |
real, intent(out):: toplw0(klon) |
| 97 |
REAL*8 ZFSDN0(KDLON,KFLEV+1) |
real solsw0(klon), sollw0(klon) |
| 98 |
c |
!IM output 3D: SWup, SWdn, LWup, LWdn |
| 99 |
REAL*8 ZFLUP(KDLON,KFLEV+1) |
REAL lwdn0(klon, klev+1), lwdn(klon, klev+1) |
| 100 |
REAL*8 ZFLDN(KDLON,KFLEV+1) |
REAL lwup0(klon, klev+1), lwup(klon, klev+1) |
| 101 |
REAL*8 ZFLUP0(KDLON,KFLEV+1) |
REAL swdn0(klon, klev+1), swdn(klon, klev+1) |
| 102 |
REAL*8 ZFLDN0(KDLON,KFLEV+1) |
REAL swup0(klon, klev+1), swup(klon, klev+1) |
| 103 |
c |
|
| 104 |
REAL*8 zx_alpha1, zx_alpha2 |
logical ok_ade, ok_aie |
| 105 |
c |
! switches whether to use aerosol direct (indirect) effects or not |
| 106 |
c |
! ok_ade---input-L- apply the Aerosol Direct Effect or not? |
| 107 |
INTEGER k, kk, i, j, iof, nb_gr |
! ok_aie---input-L- apply the Aerosol Indirect Effect or not? |
| 108 |
EXTERNAL lw, sw |
|
| 109 |
c |
real tau_ae(klon, klev, 2), piz_ae(klon, klev, 2), cg_ae(klon, klev, 2) |
| 110 |
cIM ctes ds clesphys.h REAL*8 RCO2, RCH4, RN2O, RCFC11, RCFC12 |
! input-R- aerosol optical properties (calculated in aeropt.F) |
| 111 |
REAL*8 PSCT |
|
| 112 |
c |
real topswad(klon), solswad(klon) |
| 113 |
REAL*8 PALBD(kdlon,2), PALBP(kdlon,2) |
! output: aerosol direct forcing at TOA and surface |
| 114 |
REAL*8 PEMIS(kdlon), PDT0(kdlon), PVIEW(kdlon) |
! topswad---output-R- ray. solaire absorbe au sommet de l'atm. (aerosol dir) |
| 115 |
REAL*8 PPSOL(kdlon), PDP(kdlon,klev) |
! solswad---output-R- ray. solaire net absorbe a la surface (aerosol dir) |
| 116 |
REAL*8 PTL(kdlon,kflev+1), PPMB(kdlon,kflev+1) |
|
| 117 |
REAL*8 PTAVE(kdlon,kflev) |
real cldtaupi(klon, klev) |
| 118 |
REAL*8 PWV(kdlon,kflev), PQS(kdlon,kflev), POZON(kdlon,kflev) |
! cloud optical thickness for pre-industrial aerosol concentrations |
| 119 |
REAL*8 PAER(kdlon,kflev,5) |
! (i.e. with a smaller droplet concentration and thus larger droplet radii) |
| 120 |
REAL*8 PCLDLD(kdlon,kflev) |
! -input-R- epaisseur optique des nuages dans le visible |
| 121 |
REAL*8 PCLDLU(kdlon,kflev) |
! calculated for pre-industrial (pi) aerosol concentrations, |
| 122 |
REAL*8 PCLDSW(kdlon,kflev) |
! i.e. with smaller droplet concentration, thus larger droplets, |
| 123 |
REAL*8 PTAU(kdlon,2,kflev) |
! thus generally cdltaupi cldtaupd it is needed for the |
| 124 |
REAL*8 POMEGA(kdlon,2,kflev) |
! diagnostics of the aerosol indirect radiative forcing |
| 125 |
REAL*8 PCG(kdlon,2,kflev) |
|
| 126 |
c |
real topswai(klon), solswai(klon) |
| 127 |
REAL*8 zfract(kdlon), zrmu0(kdlon), zdist |
! output: aerosol indirect forcing atTOA and surface |
| 128 |
c |
! topswai---output-R- ray. solaire absorbe au sommet de l'atm. (aerosol ind) |
| 129 |
REAL*8 zheat(kdlon,kflev), zcool(kdlon,kflev) |
! solswai---output-R- ray. solaire net absorbe a la surface (aerosol ind) |
| 130 |
REAL*8 zheat0(kdlon,kflev), zcool0(kdlon,kflev) |
|
| 131 |
REAL*8 ztopsw(kdlon), ztoplw(kdlon) |
! Local: |
| 132 |
REAL*8 zsolsw(kdlon), zsollw(kdlon), zalbpla(kdlon) |
|
| 133 |
cIM |
double precision tauae(kdlon, klev, 2) ! aer opt properties |
| 134 |
REAL*8 zsollwdown(kdlon) |
double precision pizae(kdlon, klev, 2) |
| 135 |
c |
double precision cgae(kdlon, klev, 2) |
| 136 |
REAL*8 ztopsw0(kdlon), ztoplw0(kdlon) |
|
| 137 |
REAL*8 zsolsw0(kdlon), zsollw0(kdlon) |
!IM output 3D |
| 138 |
REAL*8 zznormcp |
DOUBLE PRECISION ZFSUP(KDLON, KLEV+1) |
| 139 |
cIM output 3D : SWup, SWdn, LWup, LWdn |
DOUBLE PRECISION ZFSDN(KDLON, KLEV+1) |
| 140 |
REAL swdn(klon,kflev+1),swdn0(klon,kflev+1) |
DOUBLE PRECISION ZFSUP0(KDLON, KLEV+1) |
| 141 |
REAL swup(klon,kflev+1),swup0(klon,kflev+1) |
DOUBLE PRECISION ZFSDN0(KDLON, KLEV+1) |
| 142 |
REAL lwdn(klon,kflev+1),lwdn0(klon,kflev+1) |
|
| 143 |
REAL lwup(klon,kflev+1),lwup0(klon,kflev+1) |
DOUBLE PRECISION ZFLUP(KDLON, KLEV+1) |
| 144 |
c-OB |
DOUBLE PRECISION ZFLDN(KDLON, KLEV+1) |
| 145 |
cjq the following quantities are needed for the aerosol radiative forcings |
DOUBLE PRECISION ZFLUP0(KDLON, KLEV+1) |
| 146 |
|
DOUBLE PRECISION ZFLDN0(KDLON, KLEV+1) |
| 147 |
real topswad(klon), solswad(klon) ! output: aerosol direct forcing at TOA and surface |
|
| 148 |
real topswai(klon), solswai(klon) ! output: aerosol indirect forcing atTOA and surface |
DOUBLE PRECISION zx_alpha1, zx_alpha2 |
| 149 |
real tau_ae(klon,klev,2), piz_ae(klon,klev,2), cg_ae(klon,klev,2) ! aerosol optical properties (see aeropt.F) |
INTEGER k, kk, i, iof, nb_gr |
| 150 |
real cldtaupi(klon,klev) ! cloud optical thickness for pre-industrial aerosol concentrations |
DOUBLE PRECISION PSCT |
| 151 |
! (i.e., with a smaller droplet concentrationand thus larger droplet radii) |
|
| 152 |
logical ok_ade, ok_aie ! switches whether to use aerosol direct (indirect) effects or not |
DOUBLE PRECISION PALBD(kdlon, 2), PALBP(kdlon, 2) |
| 153 |
real*8 tauae(kdlon,kflev,2) ! aer opt properties |
DOUBLE PRECISION PEMIS(kdlon), PDT0(kdlon), PVIEW(kdlon) |
| 154 |
real*8 pizae(kdlon,kflev,2) |
DOUBLE PRECISION PPSOL(kdlon), PDP(kdlon, klev) |
| 155 |
real*8 cgae(kdlon,kflev,2) |
DOUBLE PRECISION PTL(kdlon, klev+1), PPMB(kdlon, klev+1) |
| 156 |
REAL*8 PTAUA(kdlon,2,kflev) ! present-day value of cloud opt thickness (PTAU is pre-industrial value), local use |
DOUBLE PRECISION PTAVE(kdlon, klev) |
| 157 |
REAL*8 POMEGAA(kdlon,2,kflev) ! dito for single scatt albedo |
DOUBLE PRECISION PWV(kdlon, klev), PQS(kdlon, klev) |
| 158 |
REAL*8 ztopswad(kdlon), zsolswad(kdlon) ! Aerosol direct forcing at TOAand surface |
DOUBLE PRECISION POZON(kdlon, klev) ! mass fraction of ozone |
| 159 |
REAL*8 ztopswai(kdlon), zsolswai(kdlon) ! dito, indirect |
DOUBLE PRECISION PAER(kdlon, klev, 5) |
| 160 |
cjq-end |
DOUBLE PRECISION PCLDLD(kdlon, klev) |
| 161 |
!rv |
DOUBLE PRECISION PCLDLU(kdlon, klev) |
| 162 |
tauae(:,:,:)=0. |
DOUBLE PRECISION PCLDSW(kdlon, klev) |
| 163 |
pizae(:,:,:)=0. |
DOUBLE PRECISION PTAU(kdlon, 2, klev) |
| 164 |
cgae(:,:,:)=0. |
DOUBLE PRECISION POMEGA(kdlon, 2, klev) |
| 165 |
!rv |
DOUBLE PRECISION PCG(kdlon, 2, klev) |
| 166 |
|
|
| 167 |
c |
DOUBLE PRECISION zfract(kdlon), zrmu0(kdlon) |
| 168 |
c------------------------------------------- |
|
| 169 |
nb_gr = klon / kdlon |
DOUBLE PRECISION zheat(kdlon, klev), zcool(kdlon, klev) |
| 170 |
IF (nb_gr*kdlon .NE. klon) THEN |
DOUBLE PRECISION zheat0(kdlon, klev), zcool0(kdlon, klev) |
| 171 |
PRINT*, "kdlon mauvais:", klon, kdlon, nb_gr |
DOUBLE PRECISION ztopsw(kdlon), ztoplw(kdlon) |
| 172 |
stop 1 |
DOUBLE PRECISION zsolsw(kdlon), zsollw(kdlon), zalbpla(kdlon) |
| 173 |
ENDIF |
DOUBLE PRECISION zsollwdown(kdlon) |
| 174 |
IF (kflev .NE. klev) THEN |
|
| 175 |
PRINT*, "kflev differe de klev, kflev, klev" |
DOUBLE PRECISION ztopsw0(kdlon), ztoplw0(kdlon) |
| 176 |
stop 1 |
DOUBLE PRECISION zsolsw0(kdlon), zsollw0(kdlon) |
| 177 |
ENDIF |
DOUBLE PRECISION zznormcp |
| 178 |
c------------------------------------------- |
|
| 179 |
DO k = 1, klev |
!jq the following quantities are needed for the aerosol radiative forcings |
| 180 |
DO i = 1, klon |
|
| 181 |
heat(i,k)=0. |
DOUBLE PRECISION PTAUA(kdlon, 2, klev) |
| 182 |
cool(i,k)=0. |
! present-day value of cloud opt thickness (PTAU is pre-industrial |
| 183 |
heat0(i,k)=0. |
! value), local use |
| 184 |
cool0(i,k)=0. |
|
| 185 |
ENDDO |
DOUBLE PRECISION POMEGAA(kdlon, 2, klev) ! dito for single scatt albedo |
| 186 |
ENDDO |
|
| 187 |
c |
DOUBLE PRECISION ztopswad(kdlon), zsolswad(kdlon) |
| 188 |
zdist = dist |
! Aerosol direct forcing at TOAand surface |
| 189 |
c |
|
| 190 |
cIM anciennes valeurs |
DOUBLE PRECISION ztopswai(kdlon), zsolswai(kdlon) ! dito, indirect |
| 191 |
c RCO2 = co2_ppm * 1.0e-06 * 44.011/28.97 |
real, parameter:: dobson_u = 2.1415e-05 ! Dobson unit, in kg m-2 |
| 192 |
c |
|
| 193 |
cIM : on met RCO2, RCH4, RN2O, RCFC11 et RCFC12 dans clesphys.h /lecture ds conf_phys.F90 |
!---------------------------------------------------------------------- |
| 194 |
c RCH4 = 1.65E-06* 16.043/28.97 |
|
| 195 |
c RN2O = 306.E-09* 44.013/28.97 |
tauae = 0. |
| 196 |
c RCFC11 = 280.E-12* 137.3686/28.97 |
pizae = 0. |
| 197 |
c RCFC12 = 484.E-12* 120.9140/28.97 |
cgae = 0. |
| 198 |
cIM anciennes valeurs |
|
| 199 |
c RCH4 = 1.72E-06* 16.043/28.97 |
nb_gr = klon / kdlon |
| 200 |
c RN2O = 310.E-09* 44.013/28.97 |
IF (nb_gr * kdlon /= klon) THEN |
| 201 |
c |
PRINT *, "kdlon mauvais :", klon, kdlon, nb_gr |
| 202 |
c PRINT*,'IMradlwsw : solaire, co2= ', solaire, co2_ppm |
stop 1 |
| 203 |
PSCT = solaire/zdist/zdist |
ENDIF |
| 204 |
c |
|
| 205 |
DO 99999 j = 1, nb_gr |
heat = 0. |
| 206 |
iof = kdlon*(j-1) |
cool = 0. |
| 207 |
c |
heat0 = 0. |
| 208 |
DO i = 1, kdlon |
cool0 = 0. |
| 209 |
zfract(i) = fract(iof+i) |
PSCT = solaire / dist**2 |
| 210 |
zrmu0(i) = rmu0(iof+i) |
|
| 211 |
PALBD(i,1) = albedo(iof+i) |
loop_iof: DO iof = 0, klon - kdlon, kdlon |
| 212 |
! PALBD(i,2) = albedo(iof+i) |
DO i = 1, kdlon |
| 213 |
PALBD(i,2) = alblw(iof+i) |
zfract(i) = fract(iof+i) |
| 214 |
PALBP(i,1) = albedo(iof+i) |
zrmu0(i) = mu0(iof+i) |
| 215 |
! PALBP(i,2) = albedo(iof+i) |
PALBD(i, 1) = albedo(iof+i) |
| 216 |
PALBP(i,2) = alblw(iof+i) |
PALBD(i, 2) = alblw(iof+i) |
| 217 |
cIM cf. JLD pour etre en accord avec ORCHIDEE il faut mettre PEMIS(i) = 0.96 |
PALBP(i, 1) = albedo(iof+i) |
| 218 |
PEMIS(i) = 1.0 |
PALBP(i, 2) = alblw(iof+i) |
| 219 |
PVIEW(i) = 1.66 |
! cf. JLD pour etre en accord avec ORCHIDEE il faut mettre |
| 220 |
PPSOL(i) = paprs(iof+i,1) |
! PEMIS(i) = 0.96 |
| 221 |
zx_alpha1 = (paprs(iof+i,1)-pplay(iof+i,2)) |
PEMIS(i) = 1.0 |
| 222 |
. / (pplay(iof+i,1)-pplay(iof+i,2)) |
PVIEW(i) = 1.66 |
| 223 |
zx_alpha2 = 1.0 - zx_alpha1 |
PPSOL(i) = paprs(iof+i, 1) |
| 224 |
PTL(i,1) = t(iof+i,1) * zx_alpha1 + t(iof+i,2) * zx_alpha2 |
zx_alpha1 = (paprs(iof+i, 1)-play(iof+i, 2)) & |
| 225 |
PTL(i,klev+1) = t(iof+i,klev) |
/ (play(iof+i, 1)-play(iof+i, 2)) |
| 226 |
PDT0(i) = tsol(iof+i) - PTL(i,1) |
zx_alpha2 = 1.0 - zx_alpha1 |
| 227 |
ENDDO |
PTL(i, 1) = t(iof+i, 1) * zx_alpha1 + t(iof+i, 2) * zx_alpha2 |
| 228 |
DO k = 2, kflev |
PTL(i, klev+1) = t(iof+i, klev) |
| 229 |
DO i = 1, kdlon |
PDT0(i) = tsol(iof+i) - PTL(i, 1) |
| 230 |
PTL(i,k) = (t(iof+i,k)+t(iof+i,k-1))*0.5 |
ENDDO |
| 231 |
ENDDO |
DO k = 2, klev |
| 232 |
ENDDO |
DO i = 1, kdlon |
| 233 |
DO k = 1, kflev |
PTL(i, k) = (t(iof+i, k)+t(iof+i, k-1))*0.5 |
| 234 |
DO i = 1, kdlon |
ENDDO |
| 235 |
PDP(i,k) = paprs(iof+i,k)-paprs(iof+i,k+1) |
ENDDO |
| 236 |
PTAVE(i,k) = t(iof+i,k) |
DO k = 1, klev |
| 237 |
PWV(i,k) = MAX (q(iof+i,k), 1.0e-12) |
DO i = 1, kdlon |
| 238 |
PQS(i,k) = PWV(i,k) |
PDP(i, k) = paprs(iof+i, k)-paprs(iof+i, k+1) |
| 239 |
c wo: cm.atm (epaisseur en cm dans la situation standard) |
PTAVE(i, k) = t(iof+i, k) |
| 240 |
c POZON: kg/kg |
PWV(i, k) = MAX (q(iof+i, k), 1.0e-12) |
| 241 |
IF (bug_ozone) then |
PQS(i, k) = PWV(i, k) |
| 242 |
POZON(i,k) = MAX(wo(iof+i,k),1.0e-12)*RG/46.6968 |
POZON(i, k) = wo(iof+i, k) * RG * dobson_u * 1e3 & |
| 243 |
. /(paprs(iof+i,k)-paprs(iof+i,k+1)) |
/ (paprs(iof+i, k) - paprs(iof+i, k+1)) |
| 244 |
. *(paprs(iof+i,1)/101325.0) |
PCLDLD(i, k) = cldfra(iof+i, k)*cldemi(iof+i, k) |
| 245 |
ELSE |
PCLDLU(i, k) = cldfra(iof+i, k)*cldemi(iof+i, k) |
| 246 |
c le calcul qui suit est maintenant fait dans ozonecm (MPL) |
PCLDSW(i, k) = cldfra(iof+i, k) |
| 247 |
POZON(i,k) = wo(i,k) |
PTAU(i, 1, k) = MAX(cldtaupi(iof+i, k), 1.0e-05) |
| 248 |
ENDIF |
! (1e-12 serait instable) |
| 249 |
PCLDLD(i,k) = cldfra(iof+i,k)*cldemi(iof+i,k) |
PTAU(i, 2, k) = MAX(cldtaupi(iof+i, k), 1.0e-05) |
| 250 |
PCLDLU(i,k) = cldfra(iof+i,k)*cldemi(iof+i,k) |
! (pour 32-bit machines) |
| 251 |
PCLDSW(i,k) = cldfra(iof+i,k) |
POMEGA(i, 1, k) = 0.9999 - 5.0e-04 * EXP(-0.5 * PTAU(i, 1, k)) |
| 252 |
PTAU(i,1,k) = MAX(cldtaupi(iof+i,k), 1.0e-05)! 1e-12 serait instable |
POMEGA(i, 2, k) = 0.9988 - 2.5e-03 * EXP(-0.05 * PTAU(i, 2, k)) |
| 253 |
PTAU(i,2,k) = MAX(cldtaupi(iof+i,k), 1.0e-05)! pour 32-bit machines |
PCG(i, 1, k) = 0.865 |
| 254 |
POMEGA(i,1,k) = 0.9999 - 5.0e-04 * EXP(-0.5 * PTAU(i,1,k)) |
PCG(i, 2, k) = 0.910 |
| 255 |
POMEGA(i,2,k) = 0.9988 - 2.5e-03 * EXP(-0.05 * PTAU(i,2,k)) |
|
| 256 |
PCG(i,1,k) = 0.865 |
! Introduced for aerosol indirect forcings. The |
| 257 |
PCG(i,2,k) = 0.910 |
! following values use the cloud optical thickness |
| 258 |
c-OB |
! calculated from present-day aerosol concentrations |
| 259 |
cjq Introduced for aerosol indirect forcings. |
! whereas the quantities without the "A" at the end are |
| 260 |
cjq The following values use the cloud optical thickness calculated from |
! for pre-industial (natural-only) aerosol concentrations |
| 261 |
cjq present-day aerosol concentrations whereas the quantities without the |
PTAUA(i, 1, k) = MAX(cldtaupd(iof+i, k), 1.0e-05) |
| 262 |
cjq "A" at the end are for pre-industial (natural-only) aerosol concentrations |
! (1e-12 serait instable) |
| 263 |
cjq |
PTAUA(i, 2, k) = MAX(cldtaupd(iof+i, k), 1.0e-05) |
| 264 |
PTAUA(i,1,k) = MAX(cldtaupd(iof+i,k), 1.0e-05)! 1e-12 serait instable |
! (pour 32-bit machines) |
| 265 |
PTAUA(i,2,k) = MAX(cldtaupd(iof+i,k), 1.0e-05)! pour 32-bit machines |
POMEGAA(i, 1, k) = 0.9999 - 5.0e-04 * EXP(-0.5 * PTAUA(i, 1, k)) |
| 266 |
POMEGAA(i,1,k) = 0.9999 - 5.0e-04 * EXP(-0.5 * PTAUA(i,1,k)) |
POMEGAA(i, 2, k) = 0.9988 - 2.5e-03 * EXP(-0.05 * PTAUA(i, 2, k)) |
| 267 |
POMEGAA(i,2,k) = 0.9988 - 2.5e-03 * EXP(-0.05 * PTAUA(i,2,k)) |
!jq-end |
| 268 |
cjq-end |
ENDDO |
| 269 |
ENDDO |
ENDDO |
| 270 |
ENDDO |
|
| 271 |
c |
DO k = 1, klev+1 |
| 272 |
DO k = 1, kflev+1 |
DO i = 1, kdlon |
| 273 |
DO i = 1, kdlon |
PPMB(i, k) = paprs(iof+i, k)/100.0 |
| 274 |
PPMB(i,k) = paprs(iof+i,k)/100.0 |
ENDDO |
| 275 |
ENDDO |
ENDDO |
| 276 |
ENDDO |
|
| 277 |
c |
DO kk = 1, 5 |
| 278 |
DO kk = 1, 5 |
DO k = 1, klev |
| 279 |
DO k = 1, kflev |
DO i = 1, kdlon |
| 280 |
DO i = 1, kdlon |
PAER(i, k, kk) = 1.0E-15 |
| 281 |
PAER(i,k,kk) = 1.0E-15 |
ENDDO |
| 282 |
ENDDO |
ENDDO |
| 283 |
ENDDO |
ENDDO |
| 284 |
ENDDO |
|
| 285 |
c-OB |
DO k = 1, klev |
| 286 |
DO k = 1, kflev |
DO i = 1, kdlon |
| 287 |
DO i = 1, kdlon |
tauae(i, k, 1) = tau_ae(iof+i, k, 1) |
| 288 |
tauae(i,k,1)=tau_ae(iof+i,k,1) |
pizae(i, k, 1) = piz_ae(iof+i, k, 1) |
| 289 |
pizae(i,k,1)=piz_ae(iof+i,k,1) |
cgae(i, k, 1) =cg_ae(iof+i, k, 1) |
| 290 |
cgae(i,k,1) =cg_ae(iof+i,k,1) |
tauae(i, k, 2) = tau_ae(iof+i, k, 2) |
| 291 |
tauae(i,k,2)=tau_ae(iof+i,k,2) |
pizae(i, k, 2) = piz_ae(iof+i, k, 2) |
| 292 |
pizae(i,k,2)=piz_ae(iof+i,k,2) |
cgae(i, k, 2) =cg_ae(iof+i, k, 2) |
| 293 |
cgae(i,k,2) =cg_ae(iof+i,k,2) |
ENDDO |
| 294 |
ENDDO |
ENDDO |
| 295 |
ENDDO |
|
| 296 |
c |
CALL LW(PPMB, PDP, PPSOL, PDT0, PEMIS, PTL, PTAVE, PWV, POZON, PAER, & |
| 297 |
c====================================================================== |
PCLDLD, PCLDLU, PVIEW, zcool, zcool0, ztoplw, zsollw, ztoplw0, & |
| 298 |
cIM ctes ds clesphys.h CALL LW(RCO2,RCH4,RN2O,RCFC11,RCFC12, |
zsollw0, zsollwdown, ZFLUP, ZFLDN, ZFLUP0, ZFLDN0) |
| 299 |
CALL LW( |
CALL SW(PSCT, zrmu0, zfract, PPMB, PDP, PPSOL, PALBD, PALBP, PTAVE, & |
| 300 |
. PPMB, PDP, |
PWV, PQS, POZON, PAER, PCLDSW, PTAU, POMEGA, PCG, zheat, zheat0, & |
| 301 |
. PPSOL,PDT0,PEMIS, |
zalbpla, ztopsw, zsolsw, ztopsw0, zsolsw0, ZFSUP, ZFSDN, ZFSUP0, & |
| 302 |
. PTL, PTAVE, PWV, POZON, PAER, |
ZFSDN0, tauae, pizae, cgae, PTAUA, POMEGAA, ztopswad, zsolswad, & |
| 303 |
. PCLDLD,PCLDLU, |
ztopswai, zsolswai, ok_ade, ok_aie) |
| 304 |
. PVIEW, |
|
| 305 |
. zcool, zcool0, |
DO i = 1, kdlon |
| 306 |
. ztoplw,zsollw,ztoplw0,zsollw0, |
radsol(iof+i) = zsolsw(i) + zsollw(i) |
| 307 |
. zsollwdown, |
topsw(iof+i) = ztopsw(i) |
| 308 |
. ZFLUP, ZFLDN, ZFLUP0,ZFLDN0) |
toplw(iof+i) = ztoplw(i) |
| 309 |
cIM ctes ds clesphys.h CALL SW(PSCT, RCO2, zrmu0, zfract, |
solsw(iof+i) = zsolsw(i) |
| 310 |
CALL SW(PSCT, zrmu0, zfract, |
sollw(iof+i) = zsollw(i) |
| 311 |
S PPMB, PDP, |
sollwdown(iof+i) = zsollwdown(i) |
| 312 |
S PPSOL, PALBD, PALBP, |
|
| 313 |
S PTAVE, PWV, PQS, POZON, PAER, |
DO k = 1, klev+1 |
| 314 |
S PCLDSW, PTAU, POMEGA, PCG, |
lwdn0 ( iof+i, k) = ZFLDN0 ( i, k) |
| 315 |
S zheat, zheat0, |
lwdn ( iof+i, k) = ZFLDN ( i, k) |
| 316 |
S zalbpla,ztopsw,zsolsw,ztopsw0,zsolsw0, |
lwup0 ( iof+i, k) = ZFLUP0 ( i, k) |
| 317 |
S ZFSUP,ZFSDN,ZFSUP0,ZFSDN0, |
lwup ( iof+i, k) = ZFLUP ( i, k) |
| 318 |
S tauae, pizae, cgae, ! aerosol optical properties |
ENDDO |
| 319 |
s PTAUA, POMEGAA, |
|
| 320 |
s ztopswad,zsolswad,ztopswai,zsolswai, ! diagnosed aerosol forcing |
topsw0(iof+i) = ztopsw0(i) |
| 321 |
J ok_ade, ok_aie) ! apply aerosol effects or not? |
toplw0(iof+i) = ztoplw0(i) |
| 322 |
|
solsw0(iof+i) = zsolsw0(i) |
| 323 |
c====================================================================== |
sollw0(iof+i) = zsollw0(i) |
| 324 |
DO i = 1, kdlon |
albpla(iof+i) = zalbpla(i) |
| 325 |
radsol(iof+i) = zsolsw(i) + zsollw(i) |
|
| 326 |
topsw(iof+i) = ztopsw(i) |
DO k = 1, klev+1 |
| 327 |
toplw(iof+i) = ztoplw(i) |
swdn0 ( iof+i, k) = ZFSDN0 ( i, k) |
| 328 |
solsw(iof+i) = zsolsw(i) |
swdn ( iof+i, k) = ZFSDN ( i, k) |
| 329 |
sollw(iof+i) = zsollw(i) |
swup0 ( iof+i, k) = ZFSUP0 ( i, k) |
| 330 |
sollwdown(iof+i) = zsollwdown(i) |
swup ( iof+i, k) = ZFSUP ( i, k) |
| 331 |
cIM |
ENDDO |
| 332 |
DO k = 1, kflev+1 |
ENDDO |
| 333 |
lwdn0 ( iof+i,k) = ZFLDN0 ( i,k) |
! transform the aerosol forcings, if they have to be calculated |
| 334 |
lwdn ( iof+i,k) = ZFLDN ( i,k) |
IF (ok_ade) THEN |
| 335 |
lwup0 ( iof+i,k) = ZFLUP0 ( i,k) |
DO i = 1, kdlon |
| 336 |
lwup ( iof+i,k) = ZFLUP ( i,k) |
topswad(iof+i) = ztopswad(i) |
| 337 |
ENDDO |
solswad(iof+i) = zsolswad(i) |
| 338 |
c |
ENDDO |
| 339 |
topsw0(iof+i) = ztopsw0(i) |
ELSE |
| 340 |
toplw0(iof+i) = ztoplw0(i) |
DO i = 1, kdlon |
| 341 |
solsw0(iof+i) = zsolsw0(i) |
topswad(iof+i) = 0.0 |
| 342 |
sollw0(iof+i) = zsollw0(i) |
solswad(iof+i) = 0.0 |
| 343 |
albpla(iof+i) = zalbpla(i) |
ENDDO |
| 344 |
cIM |
ENDIF |
| 345 |
DO k = 1, kflev+1 |
IF (ok_aie) THEN |
| 346 |
swdn0 ( iof+i,k) = ZFSDN0 ( i,k) |
DO i = 1, kdlon |
| 347 |
swdn ( iof+i,k) = ZFSDN ( i,k) |
topswai(iof+i) = ztopswai(i) |
| 348 |
swup0 ( iof+i,k) = ZFSUP0 ( i,k) |
solswai(iof+i) = zsolswai(i) |
| 349 |
swup ( iof+i,k) = ZFSUP ( i,k) |
ENDDO |
| 350 |
ENDDO !k=1, kflev+1 |
ELSE |
| 351 |
ENDDO |
DO i = 1, kdlon |
| 352 |
cjq-transform the aerosol forcings, if they have |
topswai(iof+i) = 0.0 |
| 353 |
cjq to be calculated |
solswai(iof+i) = 0.0 |
| 354 |
IF (ok_ade) THEN |
ENDDO |
| 355 |
DO i = 1, kdlon |
ENDIF |
| 356 |
topswad(iof+i) = ztopswad(i) |
|
| 357 |
solswad(iof+i) = zsolswad(i) |
DO k = 1, klev |
| 358 |
ENDDO |
DO i = 1, kdlon |
| 359 |
ELSE |
! scale factor to take into account the difference |
| 360 |
DO i = 1, kdlon |
! between dry air and water vapour specific heat capacity |
| 361 |
topswad(iof+i) = 0.0 |
zznormcp = 1. + RVTMP2 * PWV(i, k) |
| 362 |
solswad(iof+i) = 0.0 |
heat(iof+i, k) = zheat(i, k) / zznormcp |
| 363 |
ENDDO |
cool(iof+i, k) = zcool(i, k)/zznormcp |
| 364 |
ENDIF |
heat0(iof+i, k) = zheat0(i, k)/zznormcp |
| 365 |
IF (ok_aie) THEN |
cool0(iof+i, k) = zcool0(i, k)/zznormcp |
| 366 |
DO i = 1, kdlon |
ENDDO |
| 367 |
topswai(iof+i) = ztopswai(i) |
ENDDO |
| 368 |
solswai(iof+i) = zsolswai(i) |
end DO loop_iof |
| 369 |
ENDDO |
|
| 370 |
ELSE |
END SUBROUTINE radlwsw |
| 371 |
DO i = 1, kdlon |
|
| 372 |
topswai(iof+i) = 0.0 |
end module radlwsw_m |
|
solswai(iof+i) = 0.0 |
|
|
ENDDO |
|
|
ENDIF |
|
|
cjq-end |
|
|
DO k = 1, kflev |
|
|
c DO i = 1, kdlon |
|
|
c heat(iof+i,k) = zheat(i,k) |
|
|
c cool(iof+i,k) = zcool(i,k) |
|
|
c heat0(iof+i,k) = zheat0(i,k) |
|
|
c cool0(iof+i,k) = zcool0(i,k) |
|
|
c ENDDO |
|
|
DO i = 1, kdlon |
|
|
C scale factor to take into account the difference between |
|
|
C dry air and watter vapour scpecific heat capacity |
|
|
zznormcp=1.0+RVTMP2*PWV(i,k) |
|
|
heat(iof+i,k) = zheat(i,k)/zznormcp |
|
|
cool(iof+i,k) = zcool(i,k)/zznormcp |
|
|
heat0(iof+i,k) = zheat0(i,k)/zznormcp |
|
|
cool0(iof+i,k) = zcool0(i,k)/zznormcp |
|
|
ENDDO |
|
|
ENDDO |
|
|
c |
|
|
99999 CONTINUE |
|
|
RETURN |
|
|
END |
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