| 1 |
SUBROUTINE clmain(dtime,itap,date0,pctsrf,pctsrf_new, |
module clmain_m |
| 2 |
. t,q,u,v, |
|
| 3 |
. jour, rmu0, co2_ppm, |
IMPLICIT NONE |
| 4 |
. ok_veget, ocean, npas, nexca, ts, |
|
| 5 |
. soil_model,cdmmax, cdhmax, |
contains |
| 6 |
. ksta, ksta_ter, ok_kzmin, ftsoil,qsol, |
|
| 7 |
. paprs,pplay,snow,qsurf,evap,albe,alblw, |
SUBROUTINE clmain(dtime, itap, date0, pctsrf, pctsrf_new, t, q, u, v,& |
| 8 |
. fluxlat, |
jour, rmu0, co2_ppm, ok_veget, ocean, npas, nexca, ts,& |
| 9 |
. rain_f, snow_f, solsw, sollw, sollwdown, fder, |
soil_model, cdmmax, cdhmax, ksta, ksta_ter, ok_kzmin, ftsoil,& |
| 10 |
. rlon, rlat, cufi, cvfi, rugos, |
qsol, paprs, pplay, snow, qsurf, evap, albe, alblw, fluxlat,& |
| 11 |
. debut, lafin, agesno,rugoro, |
rain_f, snow_f, solsw, sollw, sollwdown, fder, rlon, rlat, cufi,& |
| 12 |
. d_t,d_q,d_u,d_v,d_ts, |
cvfi, rugos, debut, lafin, agesno, rugoro, d_t, d_q, d_u, d_v,& |
| 13 |
. flux_t,flux_q,flux_u,flux_v,cdragh,cdragm, |
d_ts, flux_t, flux_q, flux_u, flux_v, cdragh, cdragm, q2,& |
| 14 |
. q2, |
dflux_t, dflux_q, zcoefh, zu1, zv1, t2m, q2m, u10m, v10m, pblh,& |
| 15 |
. dflux_t,dflux_q, |
capcl, oliqcl, cteicl, pblt, therm, trmb1, trmb2, trmb3, plcl,& |
| 16 |
. zcoefh,zu1,zv1, t2m, q2m, u10m, v10m, |
fqcalving, ffonte, run_off_lic_0, flux_o, flux_g, tslab, seaice) |
| 17 |
cIM cf. AM : pbl |
|
| 18 |
. pblh,capCL,oliqCL,cteiCL,pblT, |
! From phylmd/clmain.F, version 1.6 2005/11/16 14:47:19 |
| 19 |
. therm,trmb1,trmb2,trmb3,plcl, |
! Author: Z.X. Li (LMD/CNRS), date: 1993/08/18 |
| 20 |
. fqcalving,ffonte, run_off_lic_0, |
! Objet : interface de "couche limite" (diffusion verticale) |
| 21 |
cIM "slab" ocean |
|
| 22 |
. flux_o, flux_g, tslab, seaice) |
! Tout ce qui a trait aux traceurs est dans "phytrac" maintenant. |
| 23 |
|
! Pour l'instant le calcul de la couche limite pour les traceurs |
| 24 |
! |
! se fait avec "cltrac" et ne tient pas compte de la différentiation |
| 25 |
! $Header: /home/cvsroot/LMDZ4/libf/phylmd/clmain.F,v 1.6 2005/11/16 14:47:19 lmdzadmin Exp $ |
! des sous-fractions de sol. |
| 26 |
! |
|
| 27 |
c |
! Pour pouvoir extraire les coefficients d'échanges et le vent |
| 28 |
c |
! dans la première couche, trois champs supplémentaires ont été |
| 29 |
cAA REM: |
! créés : "zcoefh", "zu1" et "zv1". Pour l'instant nous avons |
| 30 |
cAA----- |
! moyenné les valeurs de ces trois champs sur les 4 sous-surfaces |
| 31 |
cAA Tout ce qui a trait au traceurs est dans phytrac maintenant |
! du modèle. Dans l'avenir, si les informations des sous-surfaces |
| 32 |
cAA pour l'instant le calcul de la couche limite pour les traceurs |
! doivent être prises en compte, il faudra sortir ces mêmes champs |
| 33 |
cAA se fait avec cltrac et ne tient pas compte de la differentiation |
! en leur ajoutant une dimension, c'est-à-dire "nbsrf" (nombre de |
| 34 |
cAA des sous-fraction de sol. |
! sous-surfaces). |
| 35 |
cAA REM bis : |
|
| 36 |
cAA---------- |
! Arguments: |
| 37 |
cAA Pour pouvoir extraire les coefficient d'echanges et le vent |
! dtime----input-R- interval du temps (secondes) |
| 38 |
cAA dans la premiere couche, 3 champs supplementaires ont ete crees |
! itap-----input-I- numero du pas de temps |
| 39 |
cAA zcoefh,zu1 et zv1. Pour l'instant nous avons moyenne les valeurs |
! date0----input-R- jour initial |
| 40 |
cAA de ces trois champs sur les 4 subsurfaces du modele. Dans l'avenir |
! t--------input-R- temperature (K) |
| 41 |
cAA si les informations des subsurfaces doivent etre prises en compte |
! q--------input-R- vapeur d'eau (kg/kg) |
| 42 |
cAA il faudra sortir ces memes champs en leur ajoutant une dimension, |
! u--------input-R- vitesse u |
| 43 |
cAA c'est a dire nbsrf (nbre de subsurface). |
! v--------input-R- vitesse v |
| 44 |
USE ioipsl |
! ts-------input-R- temperature du sol (en Kelvin) |
| 45 |
USE interface_surf |
! paprs----input-R- pression a intercouche (Pa) |
| 46 |
use dimens_m |
! pplay----input-R- pression au milieu de couche (Pa) |
| 47 |
use indicesol |
! radsol---input-R- flux radiatif net (positif vers le sol) en W/m**2 |
| 48 |
use dimphy |
! rlat-----input-R- latitude en degree |
| 49 |
use dimsoil |
! rugos----input-R- longeur de rugosite (en m) |
| 50 |
use temps |
! cufi-----input-R- resolution des mailles en x (m) |
| 51 |
use iniprint |
! cvfi-----input-R- resolution des mailles en y (m) |
| 52 |
use YOMCST |
|
| 53 |
use yoethf |
! d_t------output-R- le changement pour "t" |
| 54 |
use fcttre |
! d_q------output-R- le changement pour "q" |
| 55 |
use conf_phys_m |
! d_u------output-R- le changement pour "u" |
| 56 |
use gath_cpl, only: gath2cpl |
! d_v------output-R- le changement pour "v" |
| 57 |
IMPLICIT none |
! d_ts-----output-R- le changement pour "ts" |
| 58 |
c====================================================================== |
! flux_t---output-R- flux de chaleur sensible (CpT) J/m**2/s (W/m**2) |
| 59 |
c Auteur(s) Z.X. Li (LMD/CNRS) date: 19930818 |
! (orientation positive vers le bas) |
| 60 |
c Objet: interface de "couche limite" (diffusion verticale) |
! flux_q---output-R- flux de vapeur d'eau (kg/m**2/s) |
| 61 |
c Arguments: |
! flux_u---output-R- tension du vent X: (kg m/s)/(m**2 s) ou Pascal |
| 62 |
c dtime----input-R- interval du temps (secondes) |
! flux_v---output-R- tension du vent Y: (kg m/s)/(m**2 s) ou Pascal |
| 63 |
c itap-----input-I- numero du pas de temps |
! dflux_t derive du flux sensible |
| 64 |
c date0----input-R- jour initial |
! dflux_q derive du flux latent |
| 65 |
c t--------input-R- temperature (K) |
!IM "slab" ocean |
| 66 |
c q--------input-R- vapeur d'eau (kg/kg) |
! flux_g---output-R- flux glace (pour OCEAN='slab ') |
| 67 |
c u--------input-R- vitesse u |
! flux_o---output-R- flux ocean (pour OCEAN='slab ') |
| 68 |
c v--------input-R- vitesse v |
|
| 69 |
c ts-------input-R- temperature du sol (en Kelvin) |
! tslab-in/output-R temperature du slab ocean (en Kelvin) |
| 70 |
c paprs----input-R- pression a intercouche (Pa) |
! uniqmnt pour slab |
| 71 |
c pplay----input-R- pression au milieu de couche (Pa) |
|
| 72 |
c radsol---input-R- flux radiatif net (positif vers le sol) en W/m**2 |
! seaice---output-R- glace de mer (kg/m2) (pour OCEAN='slab ') |
| 73 |
c rlat-----input-R- latitude en degree |
!cc |
| 74 |
c rugos----input-R- longeur de rugosite (en m) |
! ffonte----Flux thermique utilise pour fondre la neige |
| 75 |
c cufi-----input-R- resolution des mailles en x (m) |
! fqcalving-Flux d'eau "perdue" par la surface et necessaire pour limiter la |
| 76 |
c cvfi-----input-R- resolution des mailles en y (m) |
! hauteur de neige, en kg/m2/s |
| 77 |
c |
! on rajoute en output yu1 et yv1 qui sont les vents dans |
| 78 |
c d_t------output-R- le changement pour "t" |
! la premiere couche |
| 79 |
c d_q------output-R- le changement pour "q" |
! ces 4 variables sont maintenant traites dans phytrac |
| 80 |
c d_u------output-R- le changement pour "u" |
! itr--------input-I- nombre de traceurs |
| 81 |
c d_v------output-R- le changement pour "v" |
! tr---------input-R- q. de traceurs |
| 82 |
c d_ts-----output-R- le changement pour "ts" |
! flux_surf--input-R- flux de traceurs a la surface |
| 83 |
c flux_t---output-R- flux de chaleur sensible (CpT) J/m**2/s (W/m**2) |
! d_tr-------output-R tendance de traceurs |
| 84 |
c (orientation positive vers le bas) |
!IM cf. AM : PBL |
| 85 |
c flux_q---output-R- flux de vapeur d'eau (kg/m**2/s) |
! trmb1-------deep_cape |
| 86 |
c flux_u---output-R- tension du vent X: (kg m/s)/(m**2 s) ou Pascal |
! trmb2--------inhibition |
| 87 |
c flux_v---output-R- tension du vent Y: (kg m/s)/(m**2 s) ou Pascal |
! trmb3-------Point Omega |
| 88 |
c dflux_t derive du flux sensible |
! Cape(klon)-------Cape du thermique |
| 89 |
c dflux_q derive du flux latent |
! EauLiq(klon)-------Eau liqu integr du thermique |
| 90 |
cIM "slab" ocean |
! ctei(klon)-------Critere d'instab d'entrainmt des nuages de CL |
| 91 |
c flux_g---output-R- flux glace (pour OCEAN='slab ') |
! lcl------- Niveau de condensation |
| 92 |
c flux_o---output-R- flux ocean (pour OCEAN='slab ') |
! pblh------- HCL |
| 93 |
c tslab-in/output-R temperature du slab ocean (en Kelvin) ! uniqmnt pour slab |
! pblT------- T au nveau HCL |
| 94 |
c seaice---output-R- glace de mer (kg/m2) (pour OCEAN='slab ') |
|
| 95 |
ccc |
USE histcom, ONLY : histbeg_totreg, histdef, histend, histsync |
| 96 |
c ffonte----Flux thermique utilise pour fondre la neige |
use histwrite_m, only: histwrite |
| 97 |
c fqcalving-Flux d'eau "perdue" par la surface et necessaire pour limiter la |
use calendar, ONLY : ymds2ju |
| 98 |
c hauteur de neige, en kg/m2/s |
USE dimens_m, ONLY : iim, jjm |
| 99 |
cAA on rajoute en output yu1 et yv1 qui sont les vents dans |
USE indicesol, ONLY : epsfra, is_lic, is_oce, is_sic, is_ter, nbsrf |
| 100 |
cAA la premiere couche |
USE dimphy, ONLY : klev, klon, zmasq |
| 101 |
cAA ces 4 variables sont maintenant traites dans phytrac |
USE dimsoil, ONLY : nsoilmx |
| 102 |
c itr--------input-I- nombre de traceurs |
USE temps, ONLY : annee_ref, itau_phy |
| 103 |
c tr---------input-R- q. de traceurs |
USE dynetat0_m, ONLY : day_ini |
| 104 |
c flux_surf--input-R- flux de traceurs a la surface |
USE iniprint, ONLY : prt_level |
| 105 |
c d_tr-------output-R tendance de traceurs |
USE suphec_m, ONLY : rd, rg, rkappa |
| 106 |
cIM cf. AM : PBL |
USE conf_phys_m, ONLY : iflag_pbl |
| 107 |
c trmb1-------deep_cape |
USE gath_cpl, ONLY : gath2cpl |
| 108 |
c trmb2--------inhibition |
use hbtm_m, only: hbtm |
| 109 |
c trmb3-------Point Omega |
|
| 110 |
c Cape(klon)-------Cape du thermique |
REAL, INTENT (IN) :: dtime |
| 111 |
c EauLiq(klon)-------Eau liqu integr du thermique |
REAL date0 |
| 112 |
c ctei(klon)-------Critere d'instab d'entrainmt des nuages de CL |
INTEGER, INTENT (IN) :: itap |
| 113 |
c lcl------- Niveau de condensation |
REAL t(klon, klev), q(klon, klev) |
| 114 |
c pblh------- HCL |
REAL u(klon, klev), v(klon, klev) |
| 115 |
c pblT------- T au nveau HCL |
REAL, INTENT (IN) :: paprs(klon, klev+1) |
| 116 |
c====================================================================== |
REAL, INTENT (IN) :: pplay(klon, klev) |
| 117 |
c$$$ PB ajout pour soil |
REAL, INTENT (IN) :: rlon(klon), rlat(klon) |
| 118 |
c |
REAL cufi(klon), cvfi(klon) |
| 119 |
REAL dtime |
REAL d_t(klon, klev), d_q(klon, klev) |
| 120 |
real date0 |
REAL d_u(klon, klev), d_v(klon, klev) |
| 121 |
integer, intent(in):: itap |
REAL flux_t(klon, klev, nbsrf), flux_q(klon, klev, nbsrf) |
| 122 |
REAL t(klon,klev), q(klon,klev) |
REAL dflux_t(klon), dflux_q(klon) |
| 123 |
REAL u(klon,klev), v(klon,klev) |
!IM "slab" ocean |
| 124 |
cIM 230604 BAD REAL radsol(klon) ??? |
REAL flux_o(klon), flux_g(klon) |
| 125 |
REAL, intent(in):: paprs(klon,klev+1) |
REAL y_flux_o(klon), y_flux_g(klon) |
| 126 |
real, intent(in):: pplay(klon,klev) |
REAL tslab(klon), ytslab(klon) |
| 127 |
REAL, intent(in):: rlon(klon), rlat(klon) |
REAL seaice(klon), y_seaice(klon) |
| 128 |
real cufi(klon), cvfi(klon) |
REAL y_fqcalving(klon), y_ffonte(klon) |
| 129 |
REAL d_t(klon, klev), d_q(klon, klev) |
REAL fqcalving(klon, nbsrf), ffonte(klon, nbsrf) |
| 130 |
REAL d_u(klon, klev), d_v(klon, klev) |
REAL run_off_lic_0(klon), y_run_off_lic_0(klon) |
| 131 |
REAL flux_t(klon,klev, nbsrf), flux_q(klon,klev, nbsrf) |
|
| 132 |
REAL dflux_t(klon), dflux_q(klon) |
REAL flux_u(klon, klev, nbsrf), flux_v(klon, klev, nbsrf) |
| 133 |
cIM "slab" ocean |
REAL rugmer(klon), agesno(klon, nbsrf) |
| 134 |
REAL flux_o(klon), flux_g(klon) |
REAL, INTENT (IN) :: rugoro(klon) |
| 135 |
REAL y_flux_o(klon), y_flux_g(klon) |
REAL cdragh(klon), cdragm(klon) |
| 136 |
REAL tslab(klon), ytslab(klon) |
! jour de l'annee en cours |
| 137 |
REAL seaice(klon), y_seaice(klon) |
INTEGER jour |
| 138 |
cIM cf JLD |
REAL rmu0(klon) ! cosinus de l'angle solaire zenithal |
| 139 |
REAL y_fqcalving(klon), y_ffonte(klon) |
! taux CO2 atmosphere |
| 140 |
REAL fqcalving(klon,nbsrf), ffonte(klon,nbsrf) |
REAL co2_ppm |
| 141 |
REAL run_off_lic_0(klon), y_run_off_lic_0(klon) |
LOGICAL, INTENT (IN) :: debut |
| 142 |
|
LOGICAL, INTENT (IN) :: lafin |
| 143 |
REAL flux_u(klon,klev, nbsrf), flux_v(klon,klev, nbsrf) |
LOGICAL ok_veget |
| 144 |
REAL rugmer(klon), agesno(klon,nbsrf),rugoro(klon) |
CHARACTER (len=*), INTENT (IN) :: ocean |
| 145 |
REAL cdragh(klon), cdragm(klon) |
INTEGER npas, nexca |
| 146 |
integer jour ! jour de l'annee en cours |
|
| 147 |
real rmu0(klon) ! cosinus de l'angle solaire zenithal |
REAL pctsrf(klon, nbsrf) |
| 148 |
REAL co2_ppm ! taux CO2 atmosphere |
REAL ts(klon, nbsrf) |
| 149 |
LOGICAL, intent(in):: debut |
REAL d_ts(klon, nbsrf) |
| 150 |
logical, intent(in):: lafin |
REAL snow(klon, nbsrf) |
| 151 |
logical ok_veget |
REAL qsurf(klon, nbsrf) |
| 152 |
character*6 ocean |
REAL evap(klon, nbsrf) |
| 153 |
integer npas, nexca |
REAL albe(klon, nbsrf) |
| 154 |
c |
REAL alblw(klon, nbsrf) |
| 155 |
REAL pctsrf(klon,nbsrf) |
|
| 156 |
REAL ts(klon,nbsrf) |
REAL fluxlat(klon, nbsrf) |
| 157 |
REAL d_ts(klon,nbsrf) |
|
| 158 |
REAL snow(klon,nbsrf) |
REAL rain_f(klon), snow_f(klon) |
| 159 |
REAL qsurf(klon,nbsrf) |
REAL fder(klon) |
| 160 |
REAL evap(klon,nbsrf) |
|
| 161 |
REAL albe(klon,nbsrf) |
REAL sollw(klon, nbsrf), solsw(klon, nbsrf), sollwdown(klon) |
| 162 |
REAL alblw(klon,nbsrf) |
REAL rugos(klon, nbsrf) |
| 163 |
c$$$ PB |
! la nouvelle repartition des surfaces sortie de l'interface |
| 164 |
REAL fluxlat(klon,nbsrf) |
REAL pctsrf_new(klon, nbsrf) |
| 165 |
C |
|
| 166 |
real rain_f(klon), snow_f(klon) |
REAL zcoefh(klon, klev) |
| 167 |
REAL fder(klon) |
REAL zu1(klon) |
| 168 |
cIM cf. JLD REAL sollw(klon), solsw(klon), sollwdown(klon) |
REAL zv1(klon) |
| 169 |
REAL sollw(klon,nbsrf), solsw(klon,nbsrf), sollwdown(klon) |
|
| 170 |
REAL rugos(klon,nbsrf) |
!$$$ PB ajout pour soil |
| 171 |
C la nouvelle repartition des surfaces sortie de l'interface |
LOGICAL, INTENT (IN) :: soil_model |
| 172 |
REAL pctsrf_new(klon,nbsrf) |
!IM ajout seuils cdrm, cdrh |
| 173 |
cAA |
REAL cdmmax, cdhmax |
| 174 |
REAL zcoefh(klon,klev) |
|
| 175 |
REAL zu1(klon) |
REAL ksta, ksta_ter |
| 176 |
REAL zv1(klon) |
LOGICAL ok_kzmin |
| 177 |
cAA |
|
| 178 |
c$$$ PB ajout pour soil |
REAL ftsoil(klon, nsoilmx, nbsrf) |
| 179 |
LOGICAL soil_model |
REAL ytsoil(klon, nsoilmx) |
| 180 |
cIM ajout seuils cdrm, cdrh |
REAL qsol(klon) |
| 181 |
REAL cdmmax, cdhmax |
|
| 182 |
cIM: 261103 |
EXTERNAL clqh, clvent, coefkz, calbeta, cltrac |
| 183 |
REAL ksta, ksta_ter |
|
| 184 |
LOGICAL ok_kzmin |
REAL yts(klon), yrugos(klon), ypct(klon), yz0_new(klon) |
| 185 |
cIM: 261103 |
REAL yalb(klon) |
| 186 |
REAL ftsoil(klon,nsoilmx,nbsrf) |
REAL yalblw(klon) |
| 187 |
REAL ytsoil(klon,nsoilmx) |
REAL yu1(klon), yv1(klon) |
| 188 |
REAL qsol(klon) |
REAL ysnow(klon), yqsurf(klon), yagesno(klon), yqsol(klon) |
| 189 |
c====================================================================== |
REAL yrain_f(klon), ysnow_f(klon) |
| 190 |
EXTERNAL clqh, clvent, coefkz, calbeta, cltrac |
REAL ysollw(klon), ysolsw(klon), ysollwdown(klon) |
| 191 |
c====================================================================== |
REAL yfder(klon), ytaux(klon), ytauy(klon) |
| 192 |
REAL yts(klon), yrugos(klon), ypct(klon), yz0_new(klon) |
REAL yrugm(klon), yrads(klon), yrugoro(klon) |
| 193 |
REAL yalb(klon) |
|
| 194 |
REAL yalblw(klon) |
REAL yfluxlat(klon) |
| 195 |
REAL yu1(klon), yv1(klon) |
|
| 196 |
real ysnow(klon), yqsurf(klon), yagesno(klon), yqsol(klon) |
REAL y_d_ts(klon) |
| 197 |
real yrain_f(klon), ysnow_f(klon) |
REAL y_d_t(klon, klev), y_d_q(klon, klev) |
| 198 |
real ysollw(klon), ysolsw(klon), ysollwdown(klon) |
REAL y_d_u(klon, klev), y_d_v(klon, klev) |
| 199 |
real yfder(klon), ytaux(klon), ytauy(klon) |
REAL y_flux_t(klon, klev), y_flux_q(klon, klev) |
| 200 |
REAL yrugm(klon), yrads(klon),yrugoro(klon) |
REAL y_flux_u(klon, klev), y_flux_v(klon, klev) |
| 201 |
c$$$ PB |
REAL y_dflux_t(klon), y_dflux_q(klon) |
| 202 |
REAL yfluxlat(klon) |
REAL ycoefh(klon, klev), ycoefm(klon, klev) |
| 203 |
C |
REAL yu(klon, klev), yv(klon, klev) |
| 204 |
REAL y_d_ts(klon) |
REAL yt(klon, klev), yq(klon, klev) |
| 205 |
REAL y_d_t(klon, klev), y_d_q(klon, klev) |
REAL ypaprs(klon, klev+1), ypplay(klon, klev), ydelp(klon, klev) |
| 206 |
REAL y_d_u(klon, klev), y_d_v(klon, klev) |
|
| 207 |
REAL y_flux_t(klon,klev), y_flux_q(klon,klev) |
LOGICAL ok_nonloc |
| 208 |
REAL y_flux_u(klon,klev), y_flux_v(klon,klev) |
PARAMETER (ok_nonloc=.FALSE.) |
| 209 |
REAL y_dflux_t(klon), y_dflux_q(klon) |
REAL ycoefm0(klon, klev), ycoefh0(klon, klev) |
| 210 |
REAL ycoefh(klon,klev), ycoefm(klon,klev) |
|
| 211 |
REAL yu(klon,klev), yv(klon,klev) |
!IM 081204 hcl_Anne ? BEG |
| 212 |
REAL yt(klon,klev), yq(klon,klev) |
REAL yzlay(klon, klev), yzlev(klon, klev+1), yteta(klon, klev) |
| 213 |
REAL ypaprs(klon,klev+1), ypplay(klon,klev), ydelp(klon,klev) |
REAL ykmm(klon, klev+1), ykmn(klon, klev+1) |
| 214 |
c |
REAL ykmq(klon, klev+1) |
| 215 |
LOGICAL ok_nonloc |
REAL yq2(klon, klev+1), q2(klon, klev+1, nbsrf) |
| 216 |
PARAMETER (ok_nonloc=.FALSE.) |
REAL q2diag(klon, klev+1) |
| 217 |
REAL ycoefm0(klon,klev), ycoefh0(klon,klev) |
!IM 081204 hcl_Anne ? END |
| 218 |
|
|
| 219 |
cIM 081204 hcl_Anne ? BEG |
REAL u1lay(klon), v1lay(klon) |
| 220 |
real yzlay(klon,klev),yzlev(klon,klev+1),yteta(klon,klev) |
REAL delp(klon, klev) |
| 221 |
real ykmm(klon,klev+1),ykmn(klon,klev+1) |
INTEGER i, k, nsrf |
| 222 |
real ykmq(klon,klev+1) |
|
| 223 |
real yq2(klon,klev+1),q2(klon,klev+1,nbsrf) |
INTEGER ni(klon), knon, j |
| 224 |
real q2diag(klon,klev+1) |
|
| 225 |
cIM 081204 real yustar(klon),y_cd_m(klon),y_cd_h(klon) |
REAL pctsrf_pot(klon, nbsrf) |
| 226 |
cIM 081204 hcl_Anne ? END |
! "pourcentage potentiel" pour tenir compte des éventuelles |
| 227 |
c |
! apparitions ou disparitions de la glace de mer |
| 228 |
REAL u1lay(klon), v1lay(klon) |
|
| 229 |
REAL delp(klon,klev) |
REAL zx_alf1, zx_alf2 !valeur ambiante par extrapola. |
| 230 |
INTEGER i, k, nsrf |
|
| 231 |
cAA INTEGER it |
! maf pour sorties IOISPL en cas de debugagage |
| 232 |
INTEGER ni(klon), knon, j |
|
| 233 |
c Introduction d'une variable "pourcentage potentiel" pour tenir compte |
CHARACTER (80) cldebug |
| 234 |
c des eventuelles apparitions et/ou disparitions de la glace de mer |
SAVE cldebug |
| 235 |
REAL pctsrf_pot(klon,nbsrf) |
CHARACTER (8) cl_surf(nbsrf) |
| 236 |
|
SAVE cl_surf |
| 237 |
c====================================================================== |
INTEGER nhoridbg, nidbg |
| 238 |
REAL zx_alf1, zx_alf2 !valeur ambiante par extrapola. |
SAVE nhoridbg, nidbg |
| 239 |
c====================================================================== |
INTEGER ndexbg(iim*(jjm+1)) |
| 240 |
c |
REAL zx_lon(iim, jjm+1), zx_lat(iim, jjm+1), zjulian |
| 241 |
c maf pour sorties IOISPL en cas de debugagage |
REAL tabindx(klon) |
| 242 |
c |
REAL debugtab(iim, jjm+1) |
| 243 |
CHARACTER*80 cldebug |
LOGICAL first_appel |
| 244 |
SAVE cldebug |
SAVE first_appel |
| 245 |
CHARACTER*8 cl_surf(nbsrf) |
DATA first_appel/ .TRUE./ |
| 246 |
SAVE cl_surf |
LOGICAL :: debugindex = .FALSE. |
| 247 |
INTEGER nhoridbg, nidbg |
INTEGER idayref |
| 248 |
SAVE nhoridbg, nidbg |
REAL t2m(klon, nbsrf), q2m(klon, nbsrf) |
| 249 |
INTEGER ndexbg(iim*(jjm+1)) |
REAL u10m(klon, nbsrf), v10m(klon, nbsrf) |
| 250 |
REAL zx_lon(iim,jjm+1), zx_lat(iim,jjm+1), zjulian |
|
| 251 |
REAL tabindx(klon) |
REAL yt2m(klon), yq2m(klon), yu10m(klon) |
| 252 |
REAL debugtab(iim,jjm+1) |
REAL yustar(klon) |
| 253 |
LOGICAL first_appel |
! -- LOOP |
| 254 |
SAVE first_appel |
REAL yu10mx(klon) |
| 255 |
DATA first_appel/.true./ |
REAL yu10my(klon) |
| 256 |
LOGICAL debugindex |
REAL ywindsp(klon) |
| 257 |
SAVE debugindex |
! -- LOOP |
| 258 |
DATA debugindex/.false./ |
|
| 259 |
integer idayref |
REAL yt10m(klon), yq10m(klon) |
| 260 |
REAL t2m(klon,nbsrf), q2m(klon,nbsrf) |
!IM cf. AM : pbl, hbtm (Comme les autres diagnostics on cumule ds |
| 261 |
REAL u10m(klon,nbsrf), v10m(klon,nbsrf) |
! physiq ce qui permet de sortir les grdeurs par sous surface) |
| 262 |
c |
REAL pblh(klon, nbsrf) |
| 263 |
REAL yt2m(klon), yq2m(klon), yu10m(klon) |
REAL plcl(klon, nbsrf) |
| 264 |
REAL yustar(klon) |
REAL capcl(klon, nbsrf) |
| 265 |
c -- LOOP |
REAL oliqcl(klon, nbsrf) |
| 266 |
REAL yu10mx(klon) |
REAL cteicl(klon, nbsrf) |
| 267 |
REAL yu10my(klon) |
REAL pblt(klon, nbsrf) |
| 268 |
REAL ywindsp(klon) |
REAL therm(klon, nbsrf) |
| 269 |
c -- LOOP |
REAL trmb1(klon, nbsrf) |
| 270 |
c |
REAL trmb2(klon, nbsrf) |
| 271 |
REAL yt10m(klon), yq10m(klon) |
REAL trmb3(klon, nbsrf) |
| 272 |
cIM cf. AM : pbl, hbtm2 (Comme les autres diagnostics on cumule ds physic ce qui |
REAL ypblh(klon) |
| 273 |
c permet de sortir les grdeurs par sous surface) |
REAL ylcl(klon) |
| 274 |
REAL pblh(klon,nbsrf) |
REAL ycapcl(klon) |
| 275 |
REAL plcl(klon,nbsrf) |
REAL yoliqcl(klon) |
| 276 |
REAL capCL(klon,nbsrf) |
REAL ycteicl(klon) |
| 277 |
REAL oliqCL(klon,nbsrf) |
REAL ypblt(klon) |
| 278 |
REAL cteiCL(klon,nbsrf) |
REAL ytherm(klon) |
| 279 |
REAL pblT(klon,nbsrf) |
REAL ytrmb1(klon) |
| 280 |
REAL therm(klon,nbsrf) |
REAL ytrmb2(klon) |
| 281 |
REAL trmb1(klon,nbsrf) |
REAL ytrmb3(klon) |
| 282 |
REAL trmb2(klon,nbsrf) |
REAL y_cd_h(klon), y_cd_m(klon) |
| 283 |
REAL trmb3(klon,nbsrf) |
REAL uzon(klon), vmer(klon) |
| 284 |
REAL ypblh(klon) |
REAL tair1(klon), qair1(klon), tairsol(klon) |
| 285 |
REAL ylcl(klon) |
REAL psfce(klon), patm(klon) |
| 286 |
REAL ycapCL(klon) |
|
| 287 |
REAL yoliqCL(klon) |
REAL qairsol(klon), zgeo1(klon) |
| 288 |
REAL ycteiCL(klon) |
REAL rugo1(klon) |
| 289 |
REAL ypblT(klon) |
|
| 290 |
REAL ytherm(klon) |
! utiliser un jeu de fonctions simples |
| 291 |
REAL ytrmb1(klon) |
LOGICAL zxli |
| 292 |
REAL ytrmb2(klon) |
PARAMETER (zxli=.FALSE.) |
| 293 |
REAL ytrmb3(klon) |
|
| 294 |
REAL y_cd_h(klon), y_cd_m(klon) |
REAL zt, zqs, zdelta, zcor |
| 295 |
c REAL ygamt(klon,2:klev) ! contre-gradient pour temperature |
REAL t_coup |
| 296 |
c REAL ygamq(klon,2:klev) ! contre-gradient pour humidite |
PARAMETER (t_coup=273.15) |
| 297 |
REAL uzon(klon), vmer(klon) |
|
| 298 |
REAL tair1(klon), qair1(klon), tairsol(klon) |
CHARACTER (len=20) :: modname = 'clmain' |
| 299 |
REAL psfce(klon), patm(klon) |
|
| 300 |
c |
!------------------------------------------------------------ |
| 301 |
REAL qairsol(klon), zgeo1(klon) |
|
| 302 |
REAL rugo1(klon) |
ytherm = 0. |
| 303 |
c |
|
| 304 |
LOGICAL zxli ! utiliser un jeu de fonctions simples |
IF (debugindex .AND. first_appel) THEN |
| 305 |
PARAMETER (zxli=.FALSE.) |
first_appel = .FALSE. |
| 306 |
c |
|
| 307 |
REAL zt, zqs, zdelta, zcor |
! initialisation sorties netcdf |
| 308 |
REAL t_coup |
|
| 309 |
PARAMETER(t_coup=273.15) |
idayref = day_ini |
| 310 |
C |
CALL ymds2ju(annee_ref, 1, idayref, 0., zjulian) |
| 311 |
character (len = 20) :: modname = 'clmain' |
CALL gr_fi_ecrit(1, klon, iim, jjm+1, rlon, zx_lon) |
| 312 |
LOGICAL check |
DO i = 1, iim |
| 313 |
PARAMETER (check=.false.) |
zx_lon(i, 1) = rlon(i+1) |
| 314 |
|
zx_lon(i, jjm+1) = rlon(i+1) |
| 315 |
|
END DO |
| 316 |
c initialisation Anne |
CALL gr_fi_ecrit(1, klon, iim, jjm+1, rlat, zx_lat) |
| 317 |
ytherm(:) = 0. |
cldebug = 'sous_index' |
| 318 |
C |
CALL histbeg_totreg(cldebug, zx_lon(:, 1), zx_lat(1, :), 1, & |
| 319 |
if (check) THEN |
iim, 1, jjm+1, itau_phy, zjulian, dtime, nhoridbg, nidbg) |
| 320 |
write(*,*) modname,' klon=',klon |
! no vertical axis |
| 321 |
CC call flush(6) |
cl_surf(1) = 'ter' |
| 322 |
endif |
cl_surf(2) = 'lic' |
| 323 |
IF (debugindex .and. first_appel) THEN |
cl_surf(3) = 'oce' |
| 324 |
first_appel=.false. |
cl_surf(4) = 'sic' |
| 325 |
! |
DO nsrf = 1, nbsrf |
| 326 |
! initialisation sorties netcdf |
CALL histdef(nidbg, cl_surf(nsrf), cl_surf(nsrf), '-', iim, jjm+1, & |
| 327 |
! |
nhoridbg, 1, 1, 1, -99, 'inst', dtime, dtime) |
| 328 |
idayref = day_ini |
END DO |
| 329 |
CALL ymds2ju(annee_ref, 1, idayref, 0.0, zjulian) |
CALL histend(nidbg) |
| 330 |
CALL gr_fi_ecrit(1,klon,iim,jjm+1,rlon,zx_lon) |
CALL histsync(nidbg) |
| 331 |
DO i = 1, iim |
END IF |
| 332 |
zx_lon(i,1) = rlon(i+1) |
|
| 333 |
zx_lon(i,jjm+1) = rlon(i+1) |
DO k = 1, klev ! epaisseur de couche |
| 334 |
ENDDO |
DO i = 1, klon |
| 335 |
CALL gr_fi_ecrit(1,klon,iim,jjm+1,rlat,zx_lat) |
delp(i, k) = paprs(i, k) - paprs(i, k+1) |
| 336 |
cldebug='sous_index' |
END DO |
| 337 |
CALL histbeg_totreg(cldebug, iim,zx_lon(:,1),jjm+1, |
END DO |
| 338 |
$ zx_lat(1,:),1,iim,1,jjm |
DO i = 1, klon ! vent de la premiere couche |
| 339 |
$ +1, itau_phy,zjulian,dtime,nhoridbg,nidbg) |
zx_alf1 = 1.0 |
| 340 |
! no vertical axis |
zx_alf2 = 1.0 - zx_alf1 |
| 341 |
cl_surf(1)='ter' |
u1lay(i) = u(i, 1)*zx_alf1 + u(i, 2)*zx_alf2 |
| 342 |
cl_surf(2)='lic' |
v1lay(i) = v(i, 1)*zx_alf1 + v(i, 2)*zx_alf2 |
| 343 |
cl_surf(3)='oce' |
END DO |
| 344 |
cl_surf(4)='sic' |
|
| 345 |
DO nsrf=1,nbsrf |
! Initialization: |
| 346 |
CALL histdef(nidbg, cl_surf(nsrf),cl_surf(nsrf), "-",iim, |
rugmer = 0. |
| 347 |
$ jjm+1,nhoridbg, 1, 1, 1, -99, 32, "inst", dtime,dtime) |
cdragh = 0. |
| 348 |
END DO |
cdragm = 0. |
| 349 |
CALL histend(nidbg) |
dflux_t = 0. |
| 350 |
CALL histsync(nidbg) |
dflux_q = 0. |
| 351 |
ENDIF |
zu1 = 0. |
| 352 |
|
zv1 = 0. |
| 353 |
DO k = 1, klev ! epaisseur de couche |
ypct = 0. |
| 354 |
DO i = 1, klon |
yts = 0. |
| 355 |
delp(i,k) = paprs(i,k)-paprs(i,k+1) |
ysnow = 0. |
| 356 |
ENDDO |
yqsurf = 0. |
| 357 |
ENDDO |
yalb = 0. |
| 358 |
DO i = 1, klon ! vent de la premiere couche |
yalblw = 0. |
| 359 |
zx_alf1 = 1.0 |
yrain_f = 0. |
| 360 |
zx_alf2 = 1.0 - zx_alf1 |
ysnow_f = 0. |
| 361 |
u1lay(i) = u(i,1)*zx_alf1 + u(i,2)*zx_alf2 |
yfder = 0. |
| 362 |
v1lay(i) = v(i,1)*zx_alf1 + v(i,2)*zx_alf2 |
ytaux = 0. |
| 363 |
ENDDO |
ytauy = 0. |
| 364 |
c |
ysolsw = 0. |
| 365 |
c initialisation: |
ysollw = 0. |
| 366 |
c |
ysollwdown = 0. |
| 367 |
DO i = 1, klon |
yrugos = 0. |
| 368 |
rugmer(i) = 0.0 |
yu1 = 0. |
| 369 |
cdragh(i) = 0.0 |
yv1 = 0. |
| 370 |
cdragm(i) = 0.0 |
yrads = 0. |
| 371 |
dflux_t(i) = 0.0 |
ypaprs = 0. |
| 372 |
dflux_q(i) = 0.0 |
ypplay = 0. |
| 373 |
zu1(i) = 0.0 |
ydelp = 0. |
| 374 |
zv1(i) = 0.0 |
yu = 0. |
| 375 |
ENDDO |
yv = 0. |
| 376 |
ypct = 0.0 |
yt = 0. |
| 377 |
yts = 0.0 |
yq = 0. |
| 378 |
ysnow = 0.0 |
pctsrf_new = 0. |
| 379 |
yqsurf = 0.0 |
y_flux_u = 0. |
| 380 |
yalb = 0.0 |
y_flux_v = 0. |
| 381 |
yalblw = 0.0 |
!$$ PB |
| 382 |
yrain_f = 0.0 |
y_dflux_t = 0. |
| 383 |
ysnow_f = 0.0 |
y_dflux_q = 0. |
| 384 |
yfder = 0.0 |
ytsoil = 999999. |
| 385 |
ytaux = 0.0 |
yrugoro = 0. |
| 386 |
ytauy = 0.0 |
! -- LOOP |
| 387 |
ysolsw = 0.0 |
yu10mx = 0. |
| 388 |
ysollw = 0.0 |
yu10my = 0. |
| 389 |
ysollwdown = 0.0 |
ywindsp = 0. |
| 390 |
yrugos = 0.0 |
! -- LOOP |
| 391 |
yu1 = 0.0 |
d_ts = 0. |
| 392 |
yv1 = 0.0 |
!§§§ PB |
| 393 |
yrads = 0.0 |
yfluxlat = 0. |
| 394 |
ypaprs = 0.0 |
flux_t = 0. |
| 395 |
ypplay = 0.0 |
flux_q = 0. |
| 396 |
ydelp = 0.0 |
flux_u = 0. |
| 397 |
yu = 0.0 |
flux_v = 0. |
| 398 |
yv = 0.0 |
d_t = 0. |
| 399 |
yt = 0.0 |
d_q = 0. |
| 400 |
yq = 0.0 |
d_u = 0. |
| 401 |
pctsrf_new = 0.0 |
d_v = 0. |
| 402 |
y_flux_u = 0.0 |
zcoefh = 0. |
| 403 |
y_flux_v = 0.0 |
|
| 404 |
C$$ PB |
! Boucler sur toutes les sous-fractions du sol: |
| 405 |
y_dflux_t = 0.0 |
|
| 406 |
y_dflux_q = 0.0 |
! Initialisation des "pourcentages potentiels". On considère ici qu'on |
| 407 |
ytsoil = 999999. |
! peut avoir potentiellement de la glace sur tout le domaine océanique |
| 408 |
yrugoro = 0. |
! (à affiner) |
| 409 |
c -- LOOP |
|
| 410 |
yu10mx = 0.0 |
pctsrf_pot = pctsrf |
| 411 |
yu10my = 0.0 |
pctsrf_pot(:, is_oce) = 1. - zmasq |
| 412 |
ywindsp = 0.0 |
pctsrf_pot(:, is_sic) = 1. - zmasq |
| 413 |
c -- LOOP |
|
| 414 |
DO nsrf = 1, nbsrf |
DO nsrf = 1, nbsrf |
| 415 |
DO i = 1, klon |
! chercher les indices: |
| 416 |
d_ts(i,nsrf) = 0.0 |
ni = 0 |
| 417 |
ENDDO |
knon = 0 |
| 418 |
END DO |
DO i = 1, klon |
| 419 |
C§§§ PB |
! Pour déterminer le domaine à traiter, on utilise les surfaces |
| 420 |
yfluxlat=0. |
! "potentielles" |
| 421 |
flux_t = 0. |
IF (pctsrf_pot(i, nsrf) > epsfra) THEN |
| 422 |
flux_q = 0. |
knon = knon + 1 |
| 423 |
flux_u = 0. |
ni(knon) = i |
| 424 |
flux_v = 0. |
END IF |
| 425 |
DO k = 1, klev |
END DO |
| 426 |
DO i = 1, klon |
|
| 427 |
d_t(i,k) = 0.0 |
! variables pour avoir une sortie IOIPSL des INDEX |
| 428 |
d_q(i,k) = 0.0 |
IF (debugindex) THEN |
| 429 |
c$$$ flux_t(i,k) = 0.0 |
tabindx = 0. |
| 430 |
c$$$ flux_q(i,k) = 0.0 |
DO i = 1, knon |
| 431 |
d_u(i,k) = 0.0 |
tabindx(i) = real(i) |
| 432 |
d_v(i,k) = 0.0 |
END DO |
| 433 |
c$$$ flux_u(i,k) = 0.0 |
debugtab = 0. |
| 434 |
c$$$ flux_v(i,k) = 0.0 |
ndexbg = 0 |
| 435 |
zcoefh(i,k) = 0.0 |
CALL gath2cpl(tabindx, debugtab, klon, knon, iim, jjm, ni) |
| 436 |
ENDDO |
CALL histwrite(nidbg, cl_surf(nsrf), itap, debugtab) |
| 437 |
ENDDO |
END IF |
| 438 |
cAA IF (itr.GE.1) THEN |
|
| 439 |
cAA DO it = 1, itr |
IF (knon==0) CYCLE |
| 440 |
cAA DO k = 1, klev |
|
| 441 |
cAA DO i = 1, klon |
DO j = 1, knon |
|
cAA d_tr(i,k,it) = 0.0 |
|
|
cAA ENDDO |
|
|
cAA ENDDO |
|
|
cAA ENDDO |
|
|
cAA ENDIF |
|
|
|
|
|
c |
|
|
c Boucler sur toutes les sous-fractions du sol: |
|
|
c |
|
|
C Initialisation des "pourcentages potentiels". On considere ici qu'on |
|
|
C peut avoir potentiellementdela glace sur tout le domaine oceanique |
|
|
C (a affiner) |
|
|
|
|
|
pctsrf_pot = pctsrf |
|
|
pctsrf_pot(:,is_oce) = 1. - zmasq(:) |
|
|
pctsrf_pot(:,is_sic) = 1. - zmasq(:) |
|
|
|
|
|
DO 99999 nsrf = 1, nbsrf |
|
|
|
|
|
c chercher les indices: |
|
|
DO j = 1, klon |
|
|
ni(j) = 0 |
|
|
ENDDO |
|
|
knon = 0 |
|
|
DO i = 1, klon |
|
|
|
|
|
C pour determiner le domaine a traiter on utilise les surfaces "potentielles" |
|
|
C |
|
|
IF (pctsrf_pot(i,nsrf).GT.epsfra) THEN |
|
|
knon = knon + 1 |
|
|
ni(knon) = i |
|
|
ENDIF |
|
|
ENDDO |
|
|
c |
|
|
if (check) THEN |
|
|
write(*,*)'CLMAIN, nsrf, knon =',nsrf, knon |
|
|
CC call flush(6) |
|
|
endif |
|
|
c |
|
|
c variables pour avoir une sortie IOIPSL des INDEX |
|
|
c |
|
|
IF (debugindex) THEN |
|
|
tabindx(:)=0. |
|
|
c tabindx(1:knon)=(/FLOAT(i),i=1:knon/) |
|
|
DO i=1,knon |
|
|
tabindx(1:knon)=FLOAT(i) |
|
|
END DO |
|
|
debugtab(:,:)=0. |
|
|
ndexbg(:)=0 |
|
|
CALL gath2cpl(tabindx,debugtab,klon,knon,iim,jjm,ni) |
|
|
CALL histwrite(nidbg,cl_surf(nsrf),itap,debugtab,iim*(jjm+1) |
|
|
$ ,ndexbg) |
|
|
ENDIF |
|
|
IF (knon.EQ.0) GOTO 99999 |
|
|
DO j = 1, knon |
|
|
i = ni(j) |
|
|
ypct(j) = pctsrf(i,nsrf) |
|
|
yts(j) = ts(i,nsrf) |
|
|
cIM "slab" ocean |
|
|
c PRINT *, 'tslab = ', i, tslab(i) |
|
|
ytslab(i) = tslab(i) |
|
|
c |
|
|
ysnow(j) = snow(i,nsrf) |
|
|
yqsurf(j) = qsurf(i,nsrf) |
|
|
yalb(j) = albe(i,nsrf) |
|
|
yalblw(j) = alblw(i,nsrf) |
|
|
yrain_f(j) = rain_f(i) |
|
|
ysnow_f(j) = snow_f(i) |
|
|
yagesno(j) = agesno(i,nsrf) |
|
|
yfder(j) = fder(i) |
|
|
ytaux(j) = flux_u(i,1,nsrf) |
|
|
ytauy(j) = flux_v(i,1,nsrf) |
|
|
ysolsw(j) = solsw(i,nsrf) |
|
|
ysollw(j) = sollw(i,nsrf) |
|
|
ysollwdown(j) = sollwdown(i) |
|
|
yrugos(j) = rugos(i,nsrf) |
|
|
yrugoro(j) = rugoro(i) |
|
|
yu1(j) = u1lay(i) |
|
|
yv1(j) = v1lay(i) |
|
|
yrads(j) = ysolsw(j)+ ysollw(j) |
|
|
ypaprs(j,klev+1) = paprs(i,klev+1) |
|
|
y_run_off_lic_0(j) = run_off_lic_0(i) |
|
|
c -- LOOP |
|
|
yu10mx(j) = u10m(i,nsrf) |
|
|
yu10my(j) = v10m(i,nsrf) |
|
|
ywindsp(j) = SQRT(yu10mx(j)*yu10mx(j) + yu10my(j)*yu10my(j) ) |
|
|
c -- LOOP |
|
|
END DO |
|
|
C |
|
|
C IF bucket model for continent, copy soil water content |
|
|
IF ( nsrf .eq. is_ter .and. .not. ok_veget ) THEN |
|
|
DO j = 1, knon |
|
|
i = ni(j) |
|
|
yqsol(j) = qsol(i) |
|
|
END DO |
|
|
ELSE |
|
|
yqsol(:)=0. |
|
|
ENDIF |
|
|
c$$$ PB ajour pour soil |
|
|
DO k = 1, nsoilmx |
|
|
DO j = 1, knon |
|
| 442 |
i = ni(j) |
i = ni(j) |
| 443 |
ytsoil(j,k) = ftsoil(i,k,nsrf) |
ypct(j) = pctsrf(i, nsrf) |
| 444 |
END DO |
yts(j) = ts(i, nsrf) |
| 445 |
END DO |
ytslab(i) = tslab(i) |
| 446 |
DO k = 1, klev |
ysnow(j) = snow(i, nsrf) |
| 447 |
DO j = 1, knon |
yqsurf(j) = qsurf(i, nsrf) |
| 448 |
i = ni(j) |
yalb(j) = albe(i, nsrf) |
| 449 |
ypaprs(j,k) = paprs(i,k) |
yalblw(j) = alblw(i, nsrf) |
| 450 |
ypplay(j,k) = pplay(i,k) |
yrain_f(j) = rain_f(i) |
| 451 |
ydelp(j,k) = delp(i,k) |
ysnow_f(j) = snow_f(i) |
| 452 |
yu(j,k) = u(i,k) |
yagesno(j) = agesno(i, nsrf) |
| 453 |
yv(j,k) = v(i,k) |
yfder(j) = fder(i) |
| 454 |
yt(j,k) = t(i,k) |
ytaux(j) = flux_u(i, 1, nsrf) |
| 455 |
yq(j,k) = q(i,k) |
ytauy(j) = flux_v(i, 1, nsrf) |
| 456 |
ENDDO |
ysolsw(j) = solsw(i, nsrf) |
| 457 |
ENDDO |
ysollw(j) = sollw(i, nsrf) |
| 458 |
c |
ysollwdown(j) = sollwdown(i) |
| 459 |
c |
yrugos(j) = rugos(i, nsrf) |
| 460 |
c calculer Cdrag et les coefficients d'echange |
yrugoro(j) = rugoro(i) |
| 461 |
CALL coefkz(nsrf, knon, ypaprs, ypplay, |
yu1(j) = u1lay(i) |
| 462 |
cIM 261103 |
yv1(j) = v1lay(i) |
| 463 |
. ksta, ksta_ter, |
yrads(j) = ysolsw(j) + ysollw(j) |
| 464 |
cIM 261103 |
ypaprs(j, klev+1) = paprs(i, klev+1) |
| 465 |
. yts, yrugos, yu, yv, yt, yq, |
y_run_off_lic_0(j) = run_off_lic_0(i) |
| 466 |
. yqsurf, |
yu10mx(j) = u10m(i, nsrf) |
| 467 |
. ycoefm, ycoefh) |
yu10my(j) = v10m(i, nsrf) |
| 468 |
cIM 081204 BEG |
ywindsp(j) = sqrt(yu10mx(j)*yu10mx(j)+yu10my(j)*yu10my(j)) |
| 469 |
cCR test |
END DO |
| 470 |
if (iflag_pbl.eq.1) then |
|
| 471 |
cIM 081204 END |
! IF bucket model for continent, copy soil water content |
| 472 |
CALL coefkz2(nsrf, knon, ypaprs, ypplay,yt, |
IF (nsrf==is_ter .AND. .NOT. ok_veget) THEN |
| 473 |
. ycoefm0, ycoefh0) |
DO j = 1, knon |
| 474 |
DO k = 1, klev |
i = ni(j) |
| 475 |
DO i = 1, knon |
yqsol(j) = qsol(i) |
| 476 |
ycoefm(i,k) = MAX(ycoefm(i,k),ycoefm0(i,k)) |
END DO |
| 477 |
ycoefh(i,k) = MAX(ycoefh(i,k),ycoefh0(i,k)) |
ELSE |
| 478 |
ENDDO |
yqsol = 0. |
| 479 |
ENDDO |
END IF |
| 480 |
endif |
!$$$ PB ajour pour soil |
| 481 |
c |
DO k = 1, nsoilmx |
| 482 |
cIM cf JLD : on seuille ycoefm et ycoefh |
DO j = 1, knon |
| 483 |
if (nsrf.eq.is_oce) then |
i = ni(j) |
| 484 |
do j=1,knon |
ytsoil(j, k) = ftsoil(i, k, nsrf) |
| 485 |
c ycoefm(j,1)=min(ycoefm(j,1),1.1E-3) |
END DO |
| 486 |
ycoefm(j,1)=min(ycoefm(j,1),cdmmax) |
END DO |
|
c ycoefh(j,1)=min(ycoefh(j,1),1.1E-3) |
|
|
ycoefh(j,1)=min(ycoefh(j,1),cdhmax) |
|
|
enddo |
|
|
endif |
|
|
|
|
|
c |
|
|
cIM: 261103 |
|
|
if (ok_kzmin) THEN |
|
|
cIM cf FH: 201103 BEG |
|
|
c Calcul d'une diffusion minimale pour les conditions tres stables. |
|
|
call coefkzmin(knon,ypaprs,ypplay,yu,yv,yt,yq,ycoefm |
|
|
. ,ycoefm0,ycoefh0) |
|
|
c call dump2d(iim,jjm-1,ycoefm(2:klon-1,2), 'KZ ') |
|
|
c call dump2d(iim,jjm-1,ycoefm0(2:klon-1,2),'KZMIN ') |
|
|
|
|
|
if ( 1.eq.1 ) then |
|
| 487 |
DO k = 1, klev |
DO k = 1, klev |
| 488 |
DO i = 1, knon |
DO j = 1, knon |
| 489 |
ycoefm(i,k) = MAX(ycoefm(i,k),ycoefm0(i,k)) |
i = ni(j) |
| 490 |
ycoefh(i,k) = MAX(ycoefh(i,k),ycoefh0(i,k)) |
ypaprs(j, k) = paprs(i, k) |
| 491 |
ENDDO |
ypplay(j, k) = pplay(i, k) |
| 492 |
ENDDO |
ydelp(j, k) = delp(i, k) |
| 493 |
endif |
yu(j, k) = u(i, k) |
| 494 |
cIM cf FH: 201103 END |
yv(j, k) = v(i, k) |
| 495 |
endif !ok_kzmin |
yt(j, k) = t(i, k) |
| 496 |
cIM: 261103 |
yq(j, k) = q(i, k) |
| 497 |
|
END DO |
| 498 |
|
END DO |
| 499 |
IF (iflag_pbl.ge.3) then |
|
| 500 |
|
! calculer Cdrag et les coefficients d'echange |
| 501 |
cccccccccccccccccccccccccccccccccccccccccccccccccccccccccccccccccccccc |
CALL coefkz(nsrf, knon, ypaprs, ypplay, ksta, ksta_ter, yts,& |
| 502 |
c MELLOR ET YAMADA adapte a Mars Richard Fournier et Frederic Hourdin |
yrugos, yu, yv, yt, yq, yqsurf, ycoefm, ycoefh) |
| 503 |
cccccccccccccccccccccccccccccccccccccccccccccccccccccccccccccccccccc |
!IM 081204 BEG |
| 504 |
|
!CR test |
| 505 |
yzlay(1:knon,1)= |
IF (iflag_pbl==1) THEN |
| 506 |
. RD*yt(1:knon,1)/(0.5*(ypaprs(1:knon,1)+ypplay(1:knon,1))) |
!IM 081204 END |
| 507 |
. *(ypaprs(1:knon,1)-ypplay(1:knon,1))/RG |
CALL coefkz2(nsrf, knon, ypaprs, ypplay, yt, ycoefm0, ycoefh0) |
| 508 |
do k=2,klev |
DO k = 1, klev |
| 509 |
yzlay(1:knon,k)= |
DO i = 1, knon |
| 510 |
. yzlay(1:knon,k-1)+RD*0.5*(yt(1:knon,k-1)+yt(1:knon,k)) |
ycoefm(i, k) = max(ycoefm(i, k), ycoefm0(i, k)) |
| 511 |
. /ypaprs(1:knon,k)*(ypplay(1:knon,k-1)-ypplay(1:knon,k))/RG |
ycoefh(i, k) = max(ycoefh(i, k), ycoefh0(i, k)) |
| 512 |
enddo |
END DO |
| 513 |
do k=1,klev |
END DO |
| 514 |
yteta(1:knon,k)= |
END IF |
| 515 |
. yt(1:knon,k)*(ypaprs(1:knon,1)/ypplay(1:knon,k))**rkappa |
|
| 516 |
. *(1.+0.61*yq(1:knon,k)) |
!IM cf JLD : on seuille ycoefm et ycoefh |
| 517 |
enddo |
IF (nsrf==is_oce) THEN |
| 518 |
yzlev(1:knon,1)=0. |
DO j = 1, knon |
| 519 |
yzlev(1:knon,klev+1)=2.*yzlay(1:knon,klev)-yzlay(1:knon,klev-1) |
! ycoefm(j, 1)=min(ycoefm(j, 1), 1.1E-3) |
| 520 |
do k=2,klev |
ycoefm(j, 1) = min(ycoefm(j, 1), cdmmax) |
| 521 |
yzlev(1:knon,k)=0.5*(yzlay(1:knon,k)+yzlay(1:knon,k-1)) |
! ycoefh(j, 1)=min(ycoefh(j, 1), 1.1E-3) |
| 522 |
enddo |
ycoefh(j, 1) = min(ycoefh(j, 1), cdhmax) |
| 523 |
DO k = 1, klev+1 |
END DO |
| 524 |
DO j = 1, knon |
END IF |
| 525 |
i = ni(j) |
|
| 526 |
yq2(j,k)=q2(i,k,nsrf) |
!IM: 261103 |
| 527 |
enddo |
IF (ok_kzmin) THEN |
| 528 |
enddo |
!IM cf FH: 201103 BEG |
| 529 |
|
! Calcul d'une diffusion minimale pour les conditions tres stables. |
| 530 |
|
CALL coefkzmin(knon, ypaprs, ypplay, yu, yv, yt, yq, ycoefm, & |
| 531 |
c Bug introduit volontairement pour converger avec les resultats |
ycoefm0, ycoefh0) |
| 532 |
c du papier sur les thermiques. |
|
| 533 |
if (1.eq.1) then |
IF (1==1) THEN |
| 534 |
y_cd_m(1:knon) = ycoefm(1:knon,1) |
DO k = 1, klev |
| 535 |
y_cd_h(1:knon) = ycoefh(1:knon,1) |
DO i = 1, knon |
| 536 |
else |
ycoefm(i, k) = max(ycoefm(i, k), ycoefm0(i, k)) |
| 537 |
y_cd_h(1:knon) = ycoefm(1:knon,1) |
ycoefh(i, k) = max(ycoefh(i, k), ycoefh0(i, k)) |
| 538 |
y_cd_m(1:knon) = ycoefh(1:knon,1) |
END DO |
| 539 |
endif |
END DO |
| 540 |
call ustarhb(knon,yu,yv,y_cd_m, yustar) |
END IF |
| 541 |
|
!IM cf FH: 201103 END |
| 542 |
if (prt_level > 9) THEN |
!IM: 261103 |
| 543 |
WRITE(lunout,*)'USTAR = ',yustar |
END IF !ok_kzmin |
| 544 |
ENDIF |
|
| 545 |
|
IF (iflag_pbl>=3) THEN |
| 546 |
c iflag_pbl peut etre utilise comme longuer de melange |
! MELLOR ET YAMADA adapté à Mars, Richard Fournier et Frédéric Hourdin |
| 547 |
|
yzlay(1:knon, 1) = rd*yt(1:knon, 1)/(0.5*(ypaprs(1:knon, & |
| 548 |
if (iflag_pbl.ge.11) then |
1)+ypplay(1:knon, 1)))*(ypaprs(1:knon, 1)-ypplay(1:knon, 1))/rg |
| 549 |
call vdif_kcay(knon,dtime,rg,rd,ypaprs,yt |
DO k = 2, klev |
| 550 |
s ,yzlev,yzlay,yu,yv,yteta |
yzlay(1:knon, k) = yzlay(1:knon, k-1) & |
| 551 |
s ,y_cd_m,yq2,q2diag,ykmm,ykmn,yustar, |
+ rd * 0.5 * (yt(1:knon, k-1) + yt(1:knon, k)) & |
| 552 |
s iflag_pbl) |
/ ypaprs(1:knon, k) & |
| 553 |
else |
* (ypplay(1:knon, k-1) - ypplay(1:knon, k)) / rg |
| 554 |
call yamada4(knon,dtime,rg,rd,ypaprs,yt |
END DO |
| 555 |
s ,yzlev,yzlay,yu,yv,yteta |
DO k = 1, klev |
| 556 |
s ,y_cd_m,yq2,ykmm,ykmn,ykmq,yustar, |
yteta(1:knon, k) = yt(1:knon, k)*(ypaprs(1:knon, 1) & |
| 557 |
s iflag_pbl) |
/ ypplay(1:knon, k))**rkappa * (1.+0.61*yq(1:knon, k)) |
| 558 |
endif |
END DO |
| 559 |
|
yzlev(1:knon, 1) = 0. |
| 560 |
ycoefm(1:knon,1)=y_cd_m(1:knon) |
yzlev(1:knon, klev+1) = 2.*yzlay(1:knon, klev) - yzlay(1:knon, klev-1) |
| 561 |
ycoefh(1:knon,1)=y_cd_h(1:knon) |
DO k = 2, klev |
| 562 |
ycoefm(1:knon,2:klev)=ykmm(1:knon,2:klev) |
yzlev(1:knon, k) = 0.5*(yzlay(1:knon, k)+yzlay(1:knon, k-1)) |
| 563 |
ycoefh(1:knon,2:klev)=ykmn(1:knon,2:klev) |
END DO |
| 564 |
|
DO k = 1, klev + 1 |
| 565 |
|
DO j = 1, knon |
| 566 |
ENDIF |
i = ni(j) |
| 567 |
|
yq2(j, k) = q2(i, k, nsrf) |
| 568 |
cccccccccccccccccccccccccccccccccccccccccccccccccccccccccccccccccccccc |
END DO |
| 569 |
c calculer la diffusion des vitesses "u" et "v" |
END DO |
| 570 |
cccccccccccccccccccccccccccccccccccccccccccccccccccccccccccccccccccc |
|
| 571 |
|
! Bug introduit volontairement pour converger avec les resultats |
| 572 |
CALL clvent(knon,dtime,yu1,yv1,ycoefm,yt,yu,ypaprs,ypplay,ydelp, |
! du papier sur les thermiques. |
| 573 |
s y_d_u,y_flux_u) |
IF (1==1) THEN |
| 574 |
CALL clvent(knon,dtime,yu1,yv1,ycoefm,yt,yv,ypaprs,ypplay,ydelp, |
y_cd_m(1:knon) = ycoefm(1:knon, 1) |
| 575 |
s y_d_v,y_flux_v) |
y_cd_h(1:knon) = ycoefh(1:knon, 1) |
| 576 |
|
ELSE |
| 577 |
c pour le couplage |
y_cd_h(1:knon) = ycoefm(1:knon, 1) |
| 578 |
ytaux = y_flux_u(:,1) |
y_cd_m(1:knon) = ycoefh(1:knon, 1) |
| 579 |
ytauy = y_flux_v(:,1) |
END IF |
| 580 |
|
CALL ustarhb(knon, yu, yv, y_cd_m, yustar) |
| 581 |
c FH modif sur le cdrag temperature |
|
| 582 |
c$$$PB : déplace dans clcdrag |
IF (prt_level>9) THEN |
| 583 |
c$$$ do i=1,knon |
PRINT *, 'USTAR = ', yustar |
| 584 |
c$$$ ycoefh(i,1)=ycoefm(i,1)*0.8 |
END IF |
| 585 |
c$$$ enddo |
|
| 586 |
|
! iflag_pbl peut etre utilise comme longuer de melange |
| 587 |
cccccccccccccccccccccccccccccccccccccccccccccccccccccccccccccccccccccc |
|
| 588 |
c calculer la diffusion de "q" et de "h" |
IF (iflag_pbl>=11) THEN |
| 589 |
cccccccccccccccccccccccccccccccccccccccccccccccccccccccccccccccccccccc |
CALL vdif_kcay(knon, dtime, rg, rd, ypaprs, yt, yzlev, yzlay, & |
| 590 |
CALL clqh(dtime, itap, date0,jour, debut,lafin, |
yu, yv, yteta, y_cd_m, yq2, q2diag, ykmm, ykmn, yustar, & |
| 591 |
e rlon, rlat, cufi, cvfi, |
iflag_pbl) |
| 592 |
e knon, nsrf, ni, pctsrf, |
ELSE |
| 593 |
e soil_model, ytsoil,yqsol, |
CALL yamada4(knon, dtime, rg, rd, ypaprs, yt, yzlev, yzlay, yu, & |
| 594 |
e ok_veget, ocean, npas, nexca, |
yv, yteta, y_cd_m, yq2, ykmm, ykmn, ykmq, yustar, iflag_pbl) |
| 595 |
e rmu0, co2_ppm, yrugos, yrugoro, |
END IF |
| 596 |
e yu1, yv1, ycoefh, |
|
| 597 |
e yt,yq,yts,ypaprs,ypplay, |
ycoefm(1:knon, 1) = y_cd_m(1:knon) |
| 598 |
e ydelp,yrads,yalb, yalblw, ysnow, yqsurf, |
ycoefh(1:knon, 1) = y_cd_h(1:knon) |
| 599 |
e yrain_f, ysnow_f, yfder, ytaux, ytauy, |
ycoefm(1:knon, 2:klev) = ykmm(1:knon, 2:klev) |
| 600 |
c -- LOOP |
ycoefh(1:knon, 2:klev) = ykmn(1:knon, 2:klev) |
| 601 |
e ywindsp, |
END IF |
| 602 |
c -- LOOP |
|
| 603 |
c$$$ e ysollw, ysolsw, |
! calculer la diffusion des vitesses "u" et "v" |
| 604 |
e ysollw, ysollwdown, ysolsw,yfluxlat, |
CALL clvent(knon, dtime, yu1, yv1, ycoefm, yt, yu, ypaprs, ypplay, & |
| 605 |
s pctsrf_new, yagesno, |
ydelp, y_d_u, y_flux_u) |
| 606 |
s y_d_t, y_d_q, y_d_ts, yz0_new, |
CALL clvent(knon, dtime, yu1, yv1, ycoefm, yt, yv, ypaprs, ypplay, & |
| 607 |
s y_flux_t, y_flux_q, y_dflux_t, y_dflux_q, |
ydelp, y_d_v, y_flux_v) |
| 608 |
s y_fqcalving,y_ffonte,y_run_off_lic_0, |
|
| 609 |
cIM "slab" ocean |
! pour le couplage |
| 610 |
s y_flux_o, y_flux_g, ytslab, y_seaice) |
ytaux = y_flux_u(:, 1) |
| 611 |
c |
ytauy = y_flux_v(:, 1) |
| 612 |
c calculer la longueur de rugosite sur ocean |
|
| 613 |
yrugm=0. |
! calculer la diffusion de "q" et de "h" |
| 614 |
IF (nsrf.EQ.is_oce) THEN |
CALL clqh(dtime, itap, date0, jour, debut, lafin, rlon, rlat,& |
| 615 |
DO j = 1, knon |
cufi, cvfi, knon, nsrf, ni, pctsrf, soil_model, ytsoil,& |
| 616 |
yrugm(j) = 0.018*ycoefm(j,1) * (yu1(j)**2+yv1(j)**2)/RG |
yqsol, ok_veget, ocean, npas, nexca, rmu0, co2_ppm, yrugos,& |
| 617 |
$ + 0.11*14e-6 / sqrt(ycoefm(j,1) * (yu1(j)**2+yv1(j)**2)) |
yrugoro, yu1, yv1, ycoefh, yt, yq, yts, ypaprs, ypplay,& |
| 618 |
yrugm(j) = MAX(1.5e-05,yrugm(j)) |
ydelp, yrads, yalb, yalblw, ysnow, yqsurf, yrain_f, ysnow_f, & |
| 619 |
ENDDO |
yfder, ytaux, ytauy, ywindsp, ysollw, ysollwdown, ysolsw,& |
| 620 |
ENDIF |
yfluxlat, pctsrf_new, yagesno, y_d_t, y_d_q, y_d_ts,& |
| 621 |
DO j = 1, knon |
yz0_new, y_flux_t, y_flux_q, y_dflux_t, y_dflux_q,& |
| 622 |
y_dflux_t(j) = y_dflux_t(j) * ypct(j) |
y_fqcalving, y_ffonte, y_run_off_lic_0, y_flux_o, y_flux_g,& |
| 623 |
y_dflux_q(j) = y_dflux_q(j) * ypct(j) |
ytslab, y_seaice) |
| 624 |
yu1(j) = yu1(j) * ypct(j) |
|
| 625 |
yv1(j) = yv1(j) * ypct(j) |
! calculer la longueur de rugosite sur ocean |
| 626 |
ENDDO |
yrugm = 0. |
| 627 |
c |
IF (nsrf==is_oce) THEN |
| 628 |
DO k = 1, klev |
DO j = 1, knon |
| 629 |
DO j = 1, knon |
yrugm(j) = 0.018*ycoefm(j, 1)*(yu1(j)**2+yv1(j)**2)/rg + & |
| 630 |
|
0.11*14E-6/sqrt(ycoefm(j, 1)*(yu1(j)**2+yv1(j)**2)) |
| 631 |
|
yrugm(j) = max(1.5E-05, yrugm(j)) |
| 632 |
|
END DO |
| 633 |
|
END IF |
| 634 |
|
DO j = 1, knon |
| 635 |
|
y_dflux_t(j) = y_dflux_t(j)*ypct(j) |
| 636 |
|
y_dflux_q(j) = y_dflux_q(j)*ypct(j) |
| 637 |
|
yu1(j) = yu1(j)*ypct(j) |
| 638 |
|
yv1(j) = yv1(j)*ypct(j) |
| 639 |
|
END DO |
| 640 |
|
|
| 641 |
|
DO k = 1, klev |
| 642 |
|
DO j = 1, knon |
| 643 |
|
i = ni(j) |
| 644 |
|
ycoefh(j, k) = ycoefh(j, k)*ypct(j) |
| 645 |
|
ycoefm(j, k) = ycoefm(j, k)*ypct(j) |
| 646 |
|
y_d_t(j, k) = y_d_t(j, k)*ypct(j) |
| 647 |
|
y_d_q(j, k) = y_d_q(j, k)*ypct(j) |
| 648 |
|
!§§§ PB |
| 649 |
|
flux_t(i, k, nsrf) = y_flux_t(j, k) |
| 650 |
|
flux_q(i, k, nsrf) = y_flux_q(j, k) |
| 651 |
|
flux_u(i, k, nsrf) = y_flux_u(j, k) |
| 652 |
|
flux_v(i, k, nsrf) = y_flux_v(j, k) |
| 653 |
|
!$$$ PB y_flux_t(j, k) = y_flux_t(j, k) * ypct(j) |
| 654 |
|
!$$$ PB y_flux_q(j, k) = y_flux_q(j, k) * ypct(j) |
| 655 |
|
y_d_u(j, k) = y_d_u(j, k)*ypct(j) |
| 656 |
|
y_d_v(j, k) = y_d_v(j, k)*ypct(j) |
| 657 |
|
!$$$ PB y_flux_u(j, k) = y_flux_u(j, k) * ypct(j) |
| 658 |
|
!$$$ PB y_flux_v(j, k) = y_flux_v(j, k) * ypct(j) |
| 659 |
|
END DO |
| 660 |
|
END DO |
| 661 |
|
|
| 662 |
|
evap(:, nsrf) = -flux_q(:, 1, nsrf) |
| 663 |
|
|
| 664 |
|
albe(:, nsrf) = 0. |
| 665 |
|
alblw(:, nsrf) = 0. |
| 666 |
|
snow(:, nsrf) = 0. |
| 667 |
|
qsurf(:, nsrf) = 0. |
| 668 |
|
rugos(:, nsrf) = 0. |
| 669 |
|
fluxlat(:, nsrf) = 0. |
| 670 |
|
DO j = 1, knon |
| 671 |
|
i = ni(j) |
| 672 |
|
d_ts(i, nsrf) = y_d_ts(j) |
| 673 |
|
albe(i, nsrf) = yalb(j) |
| 674 |
|
alblw(i, nsrf) = yalblw(j) |
| 675 |
|
snow(i, nsrf) = ysnow(j) |
| 676 |
|
qsurf(i, nsrf) = yqsurf(j) |
| 677 |
|
rugos(i, nsrf) = yz0_new(j) |
| 678 |
|
fluxlat(i, nsrf) = yfluxlat(j) |
| 679 |
|
!$$$ pb rugmer(i) = yrugm(j) |
| 680 |
|
IF (nsrf==is_oce) THEN |
| 681 |
|
rugmer(i) = yrugm(j) |
| 682 |
|
rugos(i, nsrf) = yrugm(j) |
| 683 |
|
END IF |
| 684 |
|
!IM cf JLD ?? |
| 685 |
|
agesno(i, nsrf) = yagesno(j) |
| 686 |
|
fqcalving(i, nsrf) = y_fqcalving(j) |
| 687 |
|
ffonte(i, nsrf) = y_ffonte(j) |
| 688 |
|
cdragh(i) = cdragh(i) + ycoefh(j, 1) |
| 689 |
|
cdragm(i) = cdragm(i) + ycoefm(j, 1) |
| 690 |
|
dflux_t(i) = dflux_t(i) + y_dflux_t(j) |
| 691 |
|
dflux_q(i) = dflux_q(i) + y_dflux_q(j) |
| 692 |
|
zu1(i) = zu1(i) + yu1(j) |
| 693 |
|
zv1(i) = zv1(i) + yv1(j) |
| 694 |
|
END DO |
| 695 |
|
IF (nsrf==is_ter) THEN |
| 696 |
|
DO j = 1, knon |
| 697 |
|
i = ni(j) |
| 698 |
|
qsol(i) = yqsol(j) |
| 699 |
|
END DO |
| 700 |
|
END IF |
| 701 |
|
IF (nsrf==is_lic) THEN |
| 702 |
|
DO j = 1, knon |
| 703 |
|
i = ni(j) |
| 704 |
|
run_off_lic_0(i) = y_run_off_lic_0(j) |
| 705 |
|
END DO |
| 706 |
|
END IF |
| 707 |
|
!$$$ PB ajout pour soil |
| 708 |
|
ftsoil(:, :, nsrf) = 0. |
| 709 |
|
DO k = 1, nsoilmx |
| 710 |
|
DO j = 1, knon |
| 711 |
|
i = ni(j) |
| 712 |
|
ftsoil(i, k, nsrf) = ytsoil(j, k) |
| 713 |
|
END DO |
| 714 |
|
END DO |
| 715 |
|
|
| 716 |
|
DO j = 1, knon |
| 717 |
|
i = ni(j) |
| 718 |
|
DO k = 1, klev |
| 719 |
|
d_t(i, k) = d_t(i, k) + y_d_t(j, k) |
| 720 |
|
d_q(i, k) = d_q(i, k) + y_d_q(j, k) |
| 721 |
|
!$$$ PB flux_t(i, k) = flux_t(i, k) + y_flux_t(j, k) |
| 722 |
|
!$$$ flux_q(i, k) = flux_q(i, k) + y_flux_q(j, k) |
| 723 |
|
d_u(i, k) = d_u(i, k) + y_d_u(j, k) |
| 724 |
|
d_v(i, k) = d_v(i, k) + y_d_v(j, k) |
| 725 |
|
!$$$ PB flux_u(i, k) = flux_u(i, k) + y_flux_u(j, k) |
| 726 |
|
!$$$ flux_v(i, k) = flux_v(i, k) + y_flux_v(j, k) |
| 727 |
|
zcoefh(i, k) = zcoefh(i, k) + ycoefh(j, k) |
| 728 |
|
END DO |
| 729 |
|
END DO |
| 730 |
|
|
| 731 |
|
!cc diagnostic t, q a 2m et u, v a 10m |
| 732 |
|
|
| 733 |
|
DO j = 1, knon |
| 734 |
i = ni(j) |
i = ni(j) |
| 735 |
ycoefh(j,k) = ycoefh(j,k) * ypct(j) |
uzon(j) = yu(j, 1) + y_d_u(j, 1) |
| 736 |
ycoefm(j,k) = ycoefm(j,k) * ypct(j) |
vmer(j) = yv(j, 1) + y_d_v(j, 1) |
| 737 |
y_d_t(j,k) = y_d_t(j,k) * ypct(j) |
tair1(j) = yt(j, 1) + y_d_t(j, 1) |
| 738 |
y_d_q(j,k) = y_d_q(j,k) * ypct(j) |
qair1(j) = yq(j, 1) + y_d_q(j, 1) |
| 739 |
C§§§ PB |
zgeo1(j) = rd*tair1(j)/(0.5*(ypaprs(j, 1)+ypplay(j, & |
| 740 |
flux_t(i,k,nsrf) = y_flux_t(j,k) |
1)))*(ypaprs(j, 1)-ypplay(j, 1)) |
| 741 |
flux_q(i,k,nsrf) = y_flux_q(j,k) |
tairsol(j) = yts(j) + y_d_ts(j) |
| 742 |
flux_u(i,k,nsrf) = y_flux_u(j,k) |
rugo1(j) = yrugos(j) |
| 743 |
flux_v(i,k,nsrf) = y_flux_v(j,k) |
IF (nsrf==is_oce) THEN |
| 744 |
c$$$ PB y_flux_t(j,k) = y_flux_t(j,k) * ypct(j) |
rugo1(j) = rugos(i, nsrf) |
| 745 |
c$$$ PB y_flux_q(j,k) = y_flux_q(j,k) * ypct(j) |
END IF |
| 746 |
y_d_u(j,k) = y_d_u(j,k) * ypct(j) |
psfce(j) = ypaprs(j, 1) |
| 747 |
y_d_v(j,k) = y_d_v(j,k) * ypct(j) |
patm(j) = ypplay(j, 1) |
| 748 |
c$$$ PB y_flux_u(j,k) = y_flux_u(j,k) * ypct(j) |
|
| 749 |
c$$$ PB y_flux_v(j,k) = y_flux_v(j,k) * ypct(j) |
qairsol(j) = yqsurf(j) |
| 750 |
ENDDO |
END DO |
| 751 |
ENDDO |
|
| 752 |
|
CALL stdlevvar(klon, knon, nsrf, zxli, uzon, vmer, tair1, qair1, zgeo1, & |
| 753 |
|
tairsol, qairsol, rugo1, psfce, patm, yt2m, yq2m, yt10m, yq10m, & |
| 754 |
evap(:,nsrf) = - flux_q(:,1,nsrf) |
yu10m, yustar) |
| 755 |
c |
!IM 081204 END |
| 756 |
albe(:, nsrf) = 0. |
|
| 757 |
alblw(:, nsrf) = 0. |
DO j = 1, knon |
|
snow(:, nsrf) = 0. |
|
|
qsurf(:, nsrf) = 0. |
|
|
rugos(:, nsrf) = 0. |
|
|
fluxlat(:,nsrf) = 0. |
|
|
DO j = 1, knon |
|
|
i = ni(j) |
|
|
d_ts(i,nsrf) = y_d_ts(j) |
|
|
albe(i,nsrf) = yalb(j) |
|
|
alblw(i,nsrf) = yalblw(j) |
|
|
snow(i,nsrf) = ysnow(j) |
|
|
qsurf(i,nsrf) = yqsurf(j) |
|
|
rugos(i,nsrf) = yz0_new(j) |
|
|
fluxlat(i,nsrf) = yfluxlat(j) |
|
|
c$$$ pb rugmer(i) = yrugm(j) |
|
|
IF (nsrf .EQ. is_oce) then |
|
|
rugmer(i) = yrugm(j) |
|
|
rugos(i,nsrf) = yrugm(j) |
|
|
endif |
|
|
cIM cf JLD ?? |
|
|
agesno(i,nsrf) = yagesno(j) |
|
|
fqcalving(i,nsrf) = y_fqcalving(j) |
|
|
ffonte(i,nsrf) = y_ffonte(j) |
|
|
cdragh(i) = cdragh(i) + ycoefh(j,1) |
|
|
cdragm(i) = cdragm(i) + ycoefm(j,1) |
|
|
dflux_t(i) = dflux_t(i) + y_dflux_t(j) |
|
|
dflux_q(i) = dflux_q(i) + y_dflux_q(j) |
|
|
zu1(i) = zu1(i) + yu1(j) |
|
|
zv1(i) = zv1(i) + yv1(j) |
|
|
END DO |
|
|
IF ( nsrf .eq. is_ter ) THEN |
|
|
DO j = 1, knon |
|
|
i = ni(j) |
|
|
qsol(i) = yqsol(j) |
|
|
END DO |
|
|
END IF |
|
|
IF ( nsrf .eq. is_lic ) THEN |
|
|
DO j = 1, knon |
|
| 758 |
i = ni(j) |
i = ni(j) |
| 759 |
run_off_lic_0(i) = y_run_off_lic_0(j) |
t2m(i, nsrf) = yt2m(j) |
| 760 |
END DO |
q2m(i, nsrf) = yq2m(j) |
| 761 |
END IF |
|
| 762 |
c$$$ PB ajout pour soil |
! u10m, v10m : composantes du vent a 10m sans spirale de Ekman |
| 763 |
ftsoil(:,:,nsrf) = 0. |
u10m(i, nsrf) = (yu10m(j)*uzon(j))/sqrt(uzon(j)**2+vmer(j)**2) |
| 764 |
DO k = 1, nsoilmx |
v10m(i, nsrf) = (yu10m(j)*vmer(j))/sqrt(uzon(j)**2+vmer(j)**2) |
| 765 |
DO j = 1, knon |
|
| 766 |
|
END DO |
| 767 |
|
|
| 768 |
|
DO i = 1, knon |
| 769 |
|
y_cd_h(i) = ycoefh(i, 1) |
| 770 |
|
y_cd_m(i) = ycoefm(i, 1) |
| 771 |
|
END DO |
| 772 |
|
CALL hbtm(knon, ypaprs, ypplay, yt2m, yt10m, yq2m, yq10m, yustar, & |
| 773 |
|
y_flux_t, y_flux_q, yu, yv, yt, yq, ypblh, ycapcl, yoliqcl, & |
| 774 |
|
ycteicl, ypblt, ytherm, ytrmb1, ytrmb2, ytrmb3, ylcl) |
| 775 |
|
|
| 776 |
|
DO j = 1, knon |
| 777 |
i = ni(j) |
i = ni(j) |
| 778 |
ftsoil(i, k, nsrf) = ytsoil(j,k) |
pblh(i, nsrf) = ypblh(j) |
| 779 |
END DO |
plcl(i, nsrf) = ylcl(j) |
| 780 |
END DO |
capcl(i, nsrf) = ycapcl(j) |
| 781 |
c |
oliqcl(i, nsrf) = yoliqcl(j) |
| 782 |
DO j = 1, knon |
cteicl(i, nsrf) = ycteicl(j) |
| 783 |
i = ni(j) |
pblt(i, nsrf) = ypblt(j) |
| 784 |
DO k = 1, klev |
therm(i, nsrf) = ytherm(j) |
| 785 |
d_t(i,k) = d_t(i,k) + y_d_t(j,k) |
trmb1(i, nsrf) = ytrmb1(j) |
| 786 |
d_q(i,k) = d_q(i,k) + y_d_q(j,k) |
trmb2(i, nsrf) = ytrmb2(j) |
| 787 |
c$$$ PB flux_t(i,k) = flux_t(i,k) + y_flux_t(j,k) |
trmb3(i, nsrf) = ytrmb3(j) |
| 788 |
c$$$ flux_q(i,k) = flux_q(i,k) + y_flux_q(j,k) |
END DO |
| 789 |
d_u(i,k) = d_u(i,k) + y_d_u(j,k) |
|
| 790 |
d_v(i,k) = d_v(i,k) + y_d_v(j,k) |
DO j = 1, knon |
| 791 |
c$$$ PB flux_u(i,k) = flux_u(i,k) + y_flux_u(j,k) |
DO k = 1, klev + 1 |
| 792 |
c$$$ flux_v(i,k) = flux_v(i,k) + y_flux_v(j,k) |
i = ni(j) |
| 793 |
zcoefh(i,k) = zcoefh(i,k) + ycoefh(j,k) |
q2(i, k, nsrf) = yq2(j, k) |
| 794 |
ENDDO |
END DO |
| 795 |
ENDDO |
END DO |
| 796 |
c |
!IM "slab" ocean |
| 797 |
c |
IF (nsrf==is_oce) THEN |
| 798 |
ccc diagnostic t,q a 2m et u, v a 10m |
DO j = 1, knon |
| 799 |
c |
! on projette sur la grille globale |
| 800 |
DO j=1, knon |
i = ni(j) |
| 801 |
i = ni(j) |
IF (pctsrf_new(i, is_oce)>epsfra) THEN |
| 802 |
uzon(j) = yu(j,1) + y_d_u(j,1) |
flux_o(i) = y_flux_o(j) |
| 803 |
vmer(j) = yv(j,1) + y_d_v(j,1) |
ELSE |
| 804 |
tair1(j) = yt(j,1) + y_d_t(j,1) |
flux_o(i) = 0. |
| 805 |
qair1(j) = yq(j,1) + y_d_q(j,1) |
END IF |
| 806 |
zgeo1(j) = RD * tair1(j) / (0.5*(ypaprs(j,1)+ypplay(j,1))) |
END DO |
| 807 |
& * (ypaprs(j,1)-ypplay(j,1)) |
END IF |
| 808 |
tairsol(j) = yts(j) + y_d_ts(j) |
|
| 809 |
rugo1(j) = yrugos(j) |
IF (nsrf==is_sic) THEN |
| 810 |
IF(nsrf.EQ.is_oce) THEN |
DO j = 1, knon |
| 811 |
rugo1(j) = rugos(i,nsrf) |
i = ni(j) |
| 812 |
ENDIF |
! On pondère lorsque l'on fait le bilan au sol : |
| 813 |
psfce(j)=ypaprs(j,1) |
! flux_g(i) = y_flux_g(j)*ypct(j) |
| 814 |
patm(j)=ypplay(j,1) |
IF (pctsrf_new(i, is_sic)>epsfra) THEN |
| 815 |
c |
flux_g(i) = y_flux_g(j) |
| 816 |
qairsol(j) = yqsurf(j) |
ELSE |
| 817 |
ENDDO |
flux_g(i) = 0. |
| 818 |
c |
END IF |
| 819 |
CALL stdlevvar(klon, knon, nsrf, zxli, |
END DO |
| 820 |
& uzon, vmer, tair1, qair1, zgeo1, |
|
| 821 |
& tairsol, qairsol, rugo1, psfce, patm, |
END IF |
| 822 |
cIM & yt2m, yq2m, yu10m) |
!nsrf.EQ.is_sic |
| 823 |
& yt2m, yq2m, yt10m, yq10m, yu10m, yustar) |
IF (ocean=='slab ') THEN |
| 824 |
cIM 081204 END |
IF (nsrf==is_oce) THEN |
| 825 |
c |
tslab(1:klon) = ytslab(1:klon) |
| 826 |
c |
seaice(1:klon) = y_seaice(1:klon) |
| 827 |
DO j=1, knon |
!nsrf |
| 828 |
i = ni(j) |
END IF |
| 829 |
t2m(i,nsrf)=yt2m(j) |
!OCEAN |
| 830 |
|
END IF |
| 831 |
c |
END DO |
| 832 |
q2m(i,nsrf)=yq2m(j) |
|
| 833 |
c |
! On utilise les nouvelles surfaces |
| 834 |
c u10m, v10m : composantes du vent a 10m sans spirale de Ekman |
! A rajouter: conservation de l'albedo |
| 835 |
u10m(i,nsrf)=(yu10m(j) * uzon(j))/sqrt(uzon(j)**2+vmer(j)**2) |
|
| 836 |
v10m(i,nsrf)=(yu10m(j) * vmer(j))/sqrt(uzon(j)**2+vmer(j)**2) |
rugos(:, is_oce) = rugmer |
| 837 |
c |
pctsrf = pctsrf_new |
| 838 |
ENDDO |
|
| 839 |
c |
END SUBROUTINE clmain |
|
cIM cf AM : pbl, HBTM |
|
|
DO i = 1, knon |
|
|
y_cd_h(i) = ycoefh(i,1) |
|
|
y_cd_m(i) = ycoefm(i,1) |
|
|
ENDDO |
|
|
c print*,'appel hbtm2' |
|
|
CALL HBTM(knon, ypaprs, ypplay, |
|
|
. yt2m,yt10m,yq2m,yq10m,yustar, |
|
|
. y_flux_t,y_flux_q,yu,yv,yt,yq, |
|
|
. ypblh,ycapCL,yoliqCL,ycteiCL,ypblT, |
|
|
. ytherm,ytrmb1,ytrmb2,ytrmb3,ylcl) |
|
|
c print*,'fin hbtm2' |
|
|
c |
|
|
DO j=1, knon |
|
|
i = ni(j) |
|
|
pblh(i,nsrf) = ypblh(j) |
|
|
plcl(i,nsrf) = ylcl(j) |
|
|
capCL(i,nsrf) = ycapCL(j) |
|
|
oliqCL(i,nsrf) = yoliqCL(j) |
|
|
cteiCL(i,nsrf) = ycteiCL(j) |
|
|
pblT(i,nsrf) = ypblT(j) |
|
|
therm(i,nsrf) = ytherm(j) |
|
|
trmb1(i,nsrf) = ytrmb1(j) |
|
|
trmb2(i,nsrf) = ytrmb2(j) |
|
|
trmb3(i,nsrf) = ytrmb3(j) |
|
|
ENDDO |
|
|
c |
|
|
|
|
|
do j=1,knon |
|
|
do k=1,klev+1 |
|
|
i=ni(j) |
|
|
q2(i,k,nsrf)=yq2(j,k) |
|
|
enddo |
|
|
enddo |
|
|
cIM "slab" ocean |
|
|
IF(OCEAN.EQ.'slab '.OR.OCEAN.EQ.'force ') THEN |
|
|
IF (nsrf.EQ.is_oce) THEN |
|
|
DO j = 1, knon |
|
|
c on projette sur la grille globale |
|
|
i = ni(j) |
|
|
IF(pctsrf_new(i,is_oce).GT.epsfra) THEN |
|
|
flux_o(i) = y_flux_o(j) |
|
|
ELSE |
|
|
flux_o(i) = 0. |
|
|
ENDIF |
|
|
ENDDO |
|
|
ENDIF |
|
|
c |
|
|
IF (nsrf.EQ.is_sic) THEN |
|
|
DO j = 1, knon |
|
|
i = ni(j) |
|
|
cIM 230604 on pondere lorsque l'on fait le bilan au sol : flux_g(i) = y_flux_g(j)*ypct(j) |
|
|
IF(pctsrf_new(i,is_sic).GT.epsfra) THEN |
|
|
flux_g(i) = y_flux_g(j) |
|
|
ELSE |
|
|
flux_g(i) = 0. |
|
|
ENDIF |
|
|
ENDDO |
|
|
ENDIF !nsrf.EQ.is_sic |
|
|
ENDIF !OCEAN |
|
|
c |
|
|
IF(OCEAN.EQ.'slab ') THEN |
|
|
IF(nsrf.EQ.is_oce) then |
|
|
tslab(1:klon) = ytslab(1:klon) |
|
|
seaice(1:klon) = y_seaice(1:klon) |
|
|
ENDIF !nsrf |
|
|
ENDIF !OCEAN |
|
|
99999 CONTINUE |
|
|
C |
|
|
C On utilise les nouvelles surfaces |
|
|
C A rajouter: conservation de l'albedo |
|
|
C |
|
|
rugos(:,is_oce) = rugmer |
|
|
pctsrf = pctsrf_new |
|
| 840 |
|
|
| 841 |
RETURN |
end module clmain_m |
|
END |
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