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SUBROUTINE clmain(dtime, itap, date0, pctsrf, pctsrf_new, t, q, u, v,& |
module clmain_m |
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jour, rmu0, co2_ppm, ok_veget, ocean, npas, nexca, ts,& |
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soil_model, cdmmax, cdhmax, ksta, ksta_ter, ok_kzmin, ftsoil,& |
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qsol, paprs, pplay, snow, qsurf, evap, albe, alblw, fluxlat,& |
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rain_f, snow_f, solsw, sollw, sollwdown, fder, rlon, rlat, cufi,& |
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cvfi, rugos, debut, lafin, agesno, rugoro, d_t, d_q, d_u, d_v,& |
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d_ts, flux_t, flux_q, flux_u, flux_v, cdragh, cdragm, q2,& |
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dflux_t, dflux_q, zcoefh, zu1, zv1, t2m, q2m, u10m, v10m, pblh,& |
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capcl, oliqcl, cteicl, pblt, therm, trmb1, trmb2, trmb3, plcl,& |
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fqcalving, ffonte, run_off_lic_0, flux_o, flux_g, tslab, seaice) |
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! From phylmd/clmain.F, v 1.6 2005/11/16 14:47:19 |
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!AA Tout ce qui a trait au traceurs est dans phytrac maintenant |
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!AA pour l'instant le calcul de la couche limite pour les traceurs |
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!AA se fait avec cltrac et ne tient pas compte de la differentiation |
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!AA des sous-fraction de sol. |
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!AA Pour pouvoir extraire les coefficient d'echanges et le vent |
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!AA dans la premiere couche, 3 champs supplementaires ont ete crees |
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!AA zcoefh, zu1 et zv1. Pour l'instant nous avons moyenne les valeurs |
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!AA de ces trois champs sur les 4 subsurfaces du modele. Dans l'avenir |
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!AA si les informations des subsurfaces doivent etre prises en compte |
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!AA il faudra sortir ces memes champs en leur ajoutant une dimension, |
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!AA c'est a dire nbsrf (nbre de subsurface). |
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! Auteur(s) Z.X. Li (LMD/CNRS) date: 19930818 |
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! Objet: interface de "couche limite" (diffusion verticale) |
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! Arguments: |
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! dtime----input-R- interval du temps (secondes) |
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! itap-----input-I- numero du pas de temps |
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! date0----input-R- jour initial |
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! t--------input-R- temperature (K) |
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! q--------input-R- vapeur d'eau (kg/kg) |
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! u--------input-R- vitesse u |
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! v--------input-R- vitesse v |
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! ts-------input-R- temperature du sol (en Kelvin) |
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! paprs----input-R- pression a intercouche (Pa) |
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! pplay----input-R- pression au milieu de couche (Pa) |
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! radsol---input-R- flux radiatif net (positif vers le sol) en W/m**2 |
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! rlat-----input-R- latitude en degree |
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! rugos----input-R- longeur de rugosite (en m) |
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! cufi-----input-R- resolution des mailles en x (m) |
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! cvfi-----input-R- resolution des mailles en y (m) |
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! d_t------output-R- le changement pour "t" |
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! d_q------output-R- le changement pour "q" |
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! d_u------output-R- le changement pour "u" |
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! d_v------output-R- le changement pour "v" |
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! d_ts-----output-R- le changement pour "ts" |
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! flux_t---output-R- flux de chaleur sensible (CpT) J/m**2/s (W/m**2) |
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! (orientation positive vers le bas) |
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! flux_q---output-R- flux de vapeur d'eau (kg/m**2/s) |
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! flux_u---output-R- tension du vent X: (kg m/s)/(m**2 s) ou Pascal |
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! flux_v---output-R- tension du vent Y: (kg m/s)/(m**2 s) ou Pascal |
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! dflux_t derive du flux sensible |
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! dflux_q derive du flux latent |
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!IM "slab" ocean |
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! flux_g---output-R- flux glace (pour OCEAN='slab ') |
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! flux_o---output-R- flux ocean (pour OCEAN='slab ') |
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! tslab-in/output-R temperature du slab ocean (en Kelvin) ! uniqmnt pour slab |
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! seaice---output-R- glace de mer (kg/m2) (pour OCEAN='slab ') |
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!cc |
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! ffonte----Flux thermique utilise pour fondre la neige |
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! fqcalving-Flux d'eau "perdue" par la surface et necessaire pour limiter la |
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! hauteur de neige, en kg/m2/s |
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!AA on rajoute en output yu1 et yv1 qui sont les vents dans |
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!AA la premiere couche |
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!AA ces 4 variables sont maintenant traites dans phytrac |
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! itr--------input-I- nombre de traceurs |
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! tr---------input-R- q. de traceurs |
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! flux_surf--input-R- flux de traceurs a la surface |
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! d_tr-------output-R tendance de traceurs |
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!IM cf. AM : PBL |
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! trmb1-------deep_cape |
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! trmb2--------inhibition |
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! trmb3-------Point Omega |
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! Cape(klon)-------Cape du thermique |
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! EauLiq(klon)-------Eau liqu integr du thermique |
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! ctei(klon)-------Critere d'instab d'entrainmt des nuages de CL |
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! lcl------- Niveau de condensation |
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! pblh------- HCL |
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! pblT------- T au nveau HCL |
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!$$$ PB ajout pour soil |
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USE ioipsl, ONLY : histbeg_totreg, histdef, histend, histsync, & |
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histwrite, ymds2ju |
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USE dimens_m, ONLY : iim, jjm |
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USE indicesol, ONLY : epsfra, is_lic, is_oce, is_sic, is_ter, nbsrf |
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USE dimphy, ONLY : klev, klon, zmasq |
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USE dimsoil, ONLY : nsoilmx |
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USE temps, ONLY : annee_ref, day_ini, itau_phy |
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USE iniprint, ONLY : prt_level |
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USE yomcst, ONLY : rd, rg, rkappa |
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USE conf_phys_m, ONLY : iflag_pbl |
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USE gath_cpl, ONLY : gath2cpl |
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IMPLICIT NONE |
IMPLICIT NONE |
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REAL, INTENT (IN) :: dtime |
contains |
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REAL date0 |
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INTEGER, INTENT (IN) :: itap |
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REAL t(klon, klev), q(klon, klev) |
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REAL u(klon, klev), v(klon, klev) |
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REAL, INTENT (IN) :: paprs(klon, klev+1) |
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REAL, INTENT (IN) :: pplay(klon, klev) |
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REAL, INTENT (IN) :: rlon(klon), rlat(klon) |
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REAL cufi(klon), cvfi(klon) |
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REAL d_t(klon, klev), d_q(klon, klev) |
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REAL d_u(klon, klev), d_v(klon, klev) |
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REAL flux_t(klon, klev, nbsrf), flux_q(klon, klev, nbsrf) |
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REAL dflux_t(klon), dflux_q(klon) |
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!IM "slab" ocean |
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REAL flux_o(klon), flux_g(klon) |
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REAL y_flux_o(klon), y_flux_g(klon) |
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REAL tslab(klon), ytslab(klon) |
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REAL seaice(klon), y_seaice(klon) |
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REAL y_fqcalving(klon), y_ffonte(klon) |
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REAL fqcalving(klon, nbsrf), ffonte(klon, nbsrf) |
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REAL run_off_lic_0(klon), y_run_off_lic_0(klon) |
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REAL flux_u(klon, klev, nbsrf), flux_v(klon, klev, nbsrf) |
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REAL rugmer(klon), agesno(klon, nbsrf) |
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REAL, INTENT (IN) :: rugoro(klon) |
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REAL cdragh(klon), cdragm(klon) |
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! jour de l'annee en cours |
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INTEGER jour |
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REAL rmu0(klon) ! cosinus de l'angle solaire zenithal |
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! taux CO2 atmosphere |
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REAL co2_ppm |
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LOGICAL, INTENT (IN) :: debut |
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LOGICAL, INTENT (IN) :: lafin |
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LOGICAL ok_veget |
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CHARACTER (len=*), INTENT (IN) :: ocean |
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INTEGER npas, nexca |
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REAL pctsrf(klon, nbsrf) |
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REAL ts(klon, nbsrf) |
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REAL d_ts(klon, nbsrf) |
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REAL snow(klon, nbsrf) |
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REAL qsurf(klon, nbsrf) |
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REAL evap(klon, nbsrf) |
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REAL albe(klon, nbsrf) |
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REAL alblw(klon, nbsrf) |
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REAL fluxlat(klon, nbsrf) |
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REAL rain_f(klon), snow_f(klon) |
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REAL fder(klon) |
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REAL sollw(klon, nbsrf), solsw(klon, nbsrf), sollwdown(klon) |
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REAL rugos(klon, nbsrf) |
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! la nouvelle repartition des surfaces sortie de l'interface |
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REAL pctsrf_new(klon, nbsrf) |
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REAL zcoefh(klon, klev) |
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REAL zu1(klon) |
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REAL zv1(klon) |
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!$$$ PB ajout pour soil |
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LOGICAL, INTENT (IN) :: soil_model |
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!IM ajout seuils cdrm, cdrh |
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REAL cdmmax, cdhmax |
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REAL ksta, ksta_ter |
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LOGICAL ok_kzmin |
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REAL ftsoil(klon, nsoilmx, nbsrf) |
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REAL ytsoil(klon, nsoilmx) |
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REAL qsol(klon) |
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EXTERNAL clqh, clvent, coefkz, calbeta, cltrac |
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REAL yts(klon), yrugos(klon), ypct(klon), yz0_new(klon) |
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REAL yalb(klon) |
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REAL yalblw(klon) |
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REAL yu1(klon), yv1(klon) |
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REAL ysnow(klon), yqsurf(klon), yagesno(klon), yqsol(klon) |
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REAL yrain_f(klon), ysnow_f(klon) |
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REAL ysollw(klon), ysolsw(klon), ysollwdown(klon) |
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REAL yfder(klon), ytaux(klon), ytauy(klon) |
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REAL yrugm(klon), yrads(klon), yrugoro(klon) |
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REAL yfluxlat(klon) |
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REAL y_d_ts(klon) |
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REAL y_d_t(klon, klev), y_d_q(klon, klev) |
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REAL y_d_u(klon, klev), y_d_v(klon, klev) |
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REAL y_flux_t(klon, klev), y_flux_q(klon, klev) |
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REAL y_flux_u(klon, klev), y_flux_v(klon, klev) |
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REAL y_dflux_t(klon), y_dflux_q(klon) |
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REAL ycoefh(klon, klev), ycoefm(klon, klev) |
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REAL yu(klon, klev), yv(klon, klev) |
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REAL yt(klon, klev), yq(klon, klev) |
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REAL ypaprs(klon, klev+1), ypplay(klon, klev), ydelp(klon, klev) |
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LOGICAL ok_nonloc |
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PARAMETER (ok_nonloc=.FALSE.) |
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REAL ycoefm0(klon, klev), ycoefh0(klon, klev) |
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!IM 081204 hcl_Anne ? BEG |
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REAL yzlay(klon, klev), yzlev(klon, klev+1), yteta(klon, klev) |
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REAL ykmm(klon, klev+1), ykmn(klon, klev+1) |
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REAL ykmq(klon, klev+1) |
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REAL yq2(klon, klev+1), q2(klon, klev+1, nbsrf) |
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REAL q2diag(klon, klev+1) |
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!IM 081204 hcl_Anne ? END |
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REAL u1lay(klon), v1lay(klon) |
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REAL delp(klon, klev) |
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INTEGER i, k, nsrf |
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INTEGER ni(klon), knon, j |
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! Introduction d'une variable "pourcentage potentiel" pour tenir compte |
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! des eventuelles apparitions et/ou disparitions de la glace de mer |
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REAL pctsrf_pot(klon, nbsrf) |
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REAL zx_alf1, zx_alf2 !valeur ambiante par extrapola. |
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! maf pour sorties IOISPL en cas de debugagage |
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CHARACTER (80) cldebug |
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SAVE cldebug |
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CHARACTER (8) cl_surf(nbsrf) |
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SAVE cl_surf |
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INTEGER nhoridbg, nidbg |
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SAVE nhoridbg, nidbg |
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INTEGER ndexbg(iim*(jjm+1)) |
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REAL zx_lon(iim, jjm+1), zx_lat(iim, jjm+1), zjulian |
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REAL tabindx(klon) |
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REAL debugtab(iim, jjm+1) |
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LOGICAL first_appel |
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SAVE first_appel |
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DATA first_appel/ .TRUE./ |
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LOGICAL :: debugindex = .FALSE. |
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INTEGER idayref |
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REAL t2m(klon, nbsrf), q2m(klon, nbsrf) |
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REAL u10m(klon, nbsrf), v10m(klon, nbsrf) |
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REAL yt2m(klon), yq2m(klon), yu10m(klon) |
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REAL yustar(klon) |
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! -- LOOP |
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REAL yu10mx(klon) |
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REAL yu10my(klon) |
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REAL ywindsp(klon) |
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! -- LOOP |
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REAL yt10m(klon), yq10m(klon) |
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!IM cf. AM : pbl, hbtm2 (Comme les autres diagnostics on cumule ds |
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! physiq ce qui permet de sortir les grdeurs par sous surface) |
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REAL pblh(klon, nbsrf) |
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REAL plcl(klon, nbsrf) |
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REAL capcl(klon, nbsrf) |
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REAL oliqcl(klon, nbsrf) |
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REAL cteicl(klon, nbsrf) |
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REAL pblt(klon, nbsrf) |
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REAL therm(klon, nbsrf) |
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REAL trmb1(klon, nbsrf) |
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REAL trmb2(klon, nbsrf) |
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REAL trmb3(klon, nbsrf) |
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REAL ypblh(klon) |
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REAL ylcl(klon) |
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REAL ycapcl(klon) |
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REAL yoliqcl(klon) |
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REAL ycteicl(klon) |
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REAL ypblt(klon) |
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REAL ytherm(klon) |
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REAL ytrmb1(klon) |
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REAL ytrmb2(klon) |
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REAL ytrmb3(klon) |
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REAL y_cd_h(klon), y_cd_m(klon) |
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REAL uzon(klon), vmer(klon) |
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REAL tair1(klon), qair1(klon), tairsol(klon) |
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REAL psfce(klon), patm(klon) |
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REAL qairsol(klon), zgeo1(klon) |
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REAL rugo1(klon) |
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! utiliser un jeu de fonctions simples |
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LOGICAL zxli |
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PARAMETER (zxli=.FALSE.) |
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REAL zt, zqs, zdelta, zcor |
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REAL t_coup |
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PARAMETER (t_coup=273.15) |
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CHARACTER (len=20) :: modname = 'clmain' |
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LOGICAL check |
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PARAMETER (check=.FALSE.) |
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!------------------------------------------------------------ |
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! initialisation Anne |
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ytherm = 0. |
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IF (check) THEN |
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PRINT *, modname, ' klon=', klon |
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END IF |
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IF (debugindex .AND. first_appel) THEN |
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first_appel = .FALSE. |
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! initialisation sorties netcdf |
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idayref = day_ini |
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CALL ymds2ju(annee_ref, 1, idayref, 0.0, zjulian) |
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CALL gr_fi_ecrit(1, klon, iim, jjm+1, rlon, zx_lon) |
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DO i = 1, iim |
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zx_lon(i, 1) = rlon(i+1) |
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zx_lon(i, jjm+1) = rlon(i+1) |
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END DO |
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CALL gr_fi_ecrit(1, klon, iim, jjm+1, rlat, zx_lat) |
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cldebug = 'sous_index' |
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CALL histbeg_totreg(cldebug, zx_lon(:, 1), zx_lat(1, :), 1, & |
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iim, 1, jjm+1, itau_phy, zjulian, dtime, nhoridbg, nidbg) |
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! no vertical axis |
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cl_surf(1) = 'ter' |
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cl_surf(2) = 'lic' |
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cl_surf(3) = 'oce' |
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cl_surf(4) = 'sic' |
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DO nsrf = 1, nbsrf |
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CALL histdef(nidbg, cl_surf(nsrf), cl_surf(nsrf), '-', iim, jjm+1, & |
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nhoridbg, 1, 1, 1, -99, 'inst', dtime, dtime) |
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END DO |
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CALL histend(nidbg) |
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CALL histsync(nidbg) |
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END IF |
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DO k = 1, klev ! epaisseur de couche |
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DO i = 1, klon |
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delp(i, k) = paprs(i, k) - paprs(i, k+1) |
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END DO |
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END DO |
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DO i = 1, klon ! vent de la premiere couche |
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zx_alf1 = 1.0 |
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zx_alf2 = 1.0 - zx_alf1 |
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u1lay(i) = u(i, 1)*zx_alf1 + u(i, 2)*zx_alf2 |
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v1lay(i) = v(i, 1)*zx_alf1 + v(i, 2)*zx_alf2 |
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END DO |
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! initialisation: |
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DO i = 1, klon |
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rugmer(i) = 0.0 |
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cdragh(i) = 0.0 |
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cdragm(i) = 0.0 |
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dflux_t(i) = 0.0 |
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dflux_q(i) = 0.0 |
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zu1(i) = 0.0 |
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zv1(i) = 0.0 |
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END DO |
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ypct = 0.0 |
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yts = 0.0 |
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ysnow = 0.0 |
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yqsurf = 0.0 |
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yalb = 0.0 |
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yalblw = 0.0 |
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yrain_f = 0.0 |
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ysnow_f = 0.0 |
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yfder = 0.0 |
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ytaux = 0.0 |
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ytauy = 0.0 |
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ysolsw = 0.0 |
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ysollw = 0.0 |
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ysollwdown = 0.0 |
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yrugos = 0.0 |
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yu1 = 0.0 |
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yv1 = 0.0 |
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yrads = 0.0 |
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ypaprs = 0.0 |
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ypplay = 0.0 |
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ydelp = 0.0 |
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|
yu = 0.0 |
|
|
yv = 0.0 |
|
|
yt = 0.0 |
|
|
yq = 0.0 |
|
|
pctsrf_new = 0.0 |
|
|
y_flux_u = 0.0 |
|
|
y_flux_v = 0.0 |
|
|
!$$ PB |
|
|
y_dflux_t = 0.0 |
|
|
y_dflux_q = 0.0 |
|
|
ytsoil = 999999. |
|
|
yrugoro = 0. |
|
|
! -- LOOP |
|
|
yu10mx = 0.0 |
|
|
yu10my = 0.0 |
|
|
ywindsp = 0.0 |
|
|
! -- LOOP |
|
|
DO nsrf = 1, nbsrf |
|
|
DO i = 1, klon |
|
|
d_ts(i, nsrf) = 0.0 |
|
|
END DO |
|
|
END DO |
|
|
!§§§ PB |
|
|
yfluxlat = 0. |
|
|
flux_t = 0. |
|
|
flux_q = 0. |
|
|
flux_u = 0. |
|
|
flux_v = 0. |
|
|
DO k = 1, klev |
|
|
DO i = 1, klon |
|
|
d_t(i, k) = 0.0 |
|
|
d_q(i, k) = 0.0 |
|
|
!$$$ flux_t(i, k) = 0.0 |
|
|
!$$$ flux_q(i, k) = 0.0 |
|
|
d_u(i, k) = 0.0 |
|
|
d_v(i, k) = 0.0 |
|
|
!$$$ flux_u(i, k) = 0.0 |
|
|
!$$$ flux_v(i, k) = 0.0 |
|
|
zcoefh(i, k) = 0.0 |
|
|
END DO |
|
|
END DO |
|
|
!AA IF (itr.GE.1) THEN |
|
|
!AA DO it = 1, itr |
|
|
!AA DO k = 1, klev |
|
|
!AA DO i = 1, klon |
|
|
!AA d_tr(i, k, it) = 0.0 |
|
|
!AA ENDDO |
|
|
!AA ENDDO |
|
|
!AA ENDDO |
|
|
!AA ENDIF |
|
|
|
|
|
|
|
|
! Boucler sur toutes les sous-fractions du sol: |
|
|
|
|
|
! Initialisation des "pourcentages potentiels". On considere ici qu'on |
|
|
! peut avoir potentiellementdela glace sur tout le domaine oceanique |
|
|
! (a affiner) |
|
|
|
|
|
pctsrf_pot = pctsrf |
|
|
pctsrf_pot(:, is_oce) = 1. - zmasq |
|
|
pctsrf_pot(:, is_sic) = 1. - zmasq |
|
|
|
|
|
DO nsrf = 1, nbsrf |
|
|
! chercher les indices: |
|
|
ni = 0 |
|
|
knon = 0 |
|
|
DO i = 1, klon |
|
|
! pour determiner le domaine a traiter on utilise les surfaces |
|
|
! "potentielles" |
|
|
IF (pctsrf_pot(i, nsrf) > epsfra) THEN |
|
|
knon = knon + 1 |
|
|
ni(knon) = i |
|
|
END IF |
|
|
END DO |
|
|
|
|
|
IF (check) THEN |
|
|
PRINT *, 'CLMAIN, nsrf, knon =', nsrf, knon |
|
|
END IF |
|
|
|
|
|
! variables pour avoir une sortie IOIPSL des INDEX |
|
|
IF (debugindex) THEN |
|
|
tabindx = 0. |
|
|
DO i = 1, knon |
|
|
tabindx(i) = real(i) |
|
|
END DO |
|
|
debugtab = 0. |
|
|
ndexbg = 0 |
|
|
CALL gath2cpl(tabindx, debugtab, klon, knon, iim, jjm, ni) |
|
|
CALL histwrite(nidbg, cl_surf(nsrf), itap, debugtab) |
|
|
END IF |
|
|
|
|
|
IF (knon==0) CYCLE |
|
|
|
|
|
DO j = 1, knon |
|
|
i = ni(j) |
|
|
ypct(j) = pctsrf(i, nsrf) |
|
|
yts(j) = ts(i, nsrf) |
|
|
ytslab(i) = tslab(i) |
|
|
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) |
|
|
yu10mx(j) = u10m(i, nsrf) |
|
|
yu10my(j) = v10m(i, nsrf) |
|
|
ywindsp(j) = sqrt(yu10mx(j)*yu10mx(j)+yu10my(j)*yu10my(j)) |
|
|
END DO |
|
|
|
|
|
! IF bucket model for continent, copy soil water content |
|
|
IF (nsrf==is_ter .AND. .NOT. ok_veget) THEN |
|
|
DO j = 1, knon |
|
|
i = ni(j) |
|
|
yqsol(j) = qsol(i) |
|
|
END DO |
|
|
ELSE |
|
|
yqsol = 0. |
|
|
END IF |
|
|
!$$$ PB ajour pour soil |
|
|
DO k = 1, nsoilmx |
|
|
DO j = 1, knon |
|
|
i = ni(j) |
|
|
ytsoil(j, k) = ftsoil(i, k, nsrf) |
|
|
END DO |
|
|
END DO |
|
|
DO k = 1, klev |
|
|
DO j = 1, knon |
|
|
i = ni(j) |
|
|
ypaprs(j, k) = paprs(i, k) |
|
|
ypplay(j, k) = pplay(i, k) |
|
|
ydelp(j, k) = delp(i, k) |
|
|
yu(j, k) = u(i, k) |
|
|
yv(j, k) = v(i, k) |
|
|
yt(j, k) = t(i, k) |
|
|
yq(j, k) = q(i, k) |
|
|
END DO |
|
|
END DO |
|
|
|
|
|
! calculer Cdrag et les coefficients d'echange |
|
|
CALL coefkz(nsrf, knon, ypaprs, ypplay, ksta, ksta_ter, yts,& |
|
|
yrugos, yu, yv, yt, yq, yqsurf, ycoefm, ycoefh) |
|
|
!IM 081204 BEG |
|
|
!CR test |
|
|
IF (iflag_pbl==1) THEN |
|
|
!IM 081204 END |
|
|
CALL coefkz2(nsrf, knon, ypaprs, ypplay, yt, ycoefm0, ycoefh0) |
|
|
DO k = 1, klev |
|
|
DO i = 1, knon |
|
|
ycoefm(i, k) = max(ycoefm(i, k), ycoefm0(i, k)) |
|
|
ycoefh(i, k) = max(ycoefh(i, k), ycoefh0(i, k)) |
|
|
END DO |
|
|
END DO |
|
|
END IF |
|
|
|
|
|
!IM cf JLD : on seuille ycoefm et ycoefh |
|
|
IF (nsrf==is_oce) THEN |
|
|
DO j = 1, knon |
|
|
! ycoefm(j, 1)=min(ycoefm(j, 1), 1.1E-3) |
|
|
ycoefm(j, 1) = min(ycoefm(j, 1), cdmmax) |
|
|
! ycoefh(j, 1)=min(ycoefh(j, 1), 1.1E-3) |
|
|
ycoefh(j, 1) = min(ycoefh(j, 1), cdhmax) |
|
|
END DO |
|
|
END IF |
|
|
|
|
|
|
|
|
!IM: 261103 |
|
|
IF (ok_kzmin) THEN |
|
|
!IM cf FH: 201103 BEG |
|
|
! Calcul d'une diffusion minimale pour les conditions tres stables. |
|
|
CALL coefkzmin(knon, ypaprs, ypplay, yu, yv, yt, yq, ycoefm, ycoefm0, & |
|
|
ycoefh0) |
|
|
! call dump2d(iim, jjm-1, ycoefm(2:klon-1, 2), 'KZ ') |
|
|
! call dump2d(iim, jjm-1, ycoefm0(2:klon-1, 2), 'KZMIN ') |
|
|
|
|
|
IF (1==1) THEN |
|
|
DO k = 1, klev |
|
|
DO i = 1, knon |
|
|
ycoefm(i, k) = max(ycoefm(i, k), ycoefm0(i, k)) |
|
|
ycoefh(i, k) = max(ycoefh(i, k), ycoefh0(i, k)) |
|
|
END DO |
|
|
END DO |
|
|
END IF |
|
|
!IM cf FH: 201103 END |
|
|
!IM: 261103 |
|
|
END IF !ok_kzmin |
|
|
|
|
|
IF (iflag_pbl>=3) THEN |
|
|
|
|
|
!ccccccccccccccccccccccccccccccccccccccccccccccccccccccccccccccccccccc |
|
|
! MELLOR ET YAMADA adapte a Mars Richard Fournier et Frederic Hourdin |
|
|
!ccccccccccccccccccccccccccccccccccccccccccccccccccccccccccccccccccc |
|
|
|
|
|
yzlay(1:knon, 1) = rd*yt(1:knon, 1)/(0.5*(ypaprs(1:knon, & |
|
|
1)+ypplay(1:knon, 1)))*(ypaprs(1:knon, 1)-ypplay(1:knon, 1))/rg |
|
|
DO k = 2, klev |
|
|
yzlay(1:knon, k) = yzlay(1:knon, k-1) & |
|
|
+ rd*0.5*(yt(1:knon, k-1) +yt(1: knon, k)) & |
|
|
/ ypaprs(1:knon, k) *(ypplay(1:knon, k-1)-ypplay(1:knon, k))/ & |
|
|
rg |
|
|
END DO |
|
|
DO k = 1, klev |
|
|
yteta(1:knon, k) = yt(1:knon, k)*(ypaprs(1:knon, 1) & |
|
|
/ ypplay(1:knon, k))**rkappa * (1.+0.61*yq(1:knon, k)) |
|
|
END DO |
|
|
yzlev(1:knon, 1) = 0. |
|
|
yzlev(1:knon, klev+1) = 2.*yzlay(1:knon, klev) - yzlay(1:knon, klev-1) |
|
|
DO k = 2, klev |
|
|
yzlev(1:knon, k) = 0.5*(yzlay(1:knon, k)+yzlay(1:knon, k-1)) |
|
|
END DO |
|
|
DO k = 1, klev + 1 |
|
|
DO j = 1, knon |
|
|
i = ni(j) |
|
|
yq2(j, k) = q2(i, k, nsrf) |
|
|
END DO |
|
|
END DO |
|
|
|
|
|
|
|
|
! Bug introduit volontairement pour converger avec les resultats |
|
|
! du papier sur les thermiques. |
|
|
IF (1==1) THEN |
|
|
y_cd_m(1:knon) = ycoefm(1:knon, 1) |
|
|
y_cd_h(1:knon) = ycoefh(1:knon, 1) |
|
|
ELSE |
|
|
y_cd_h(1:knon) = ycoefm(1:knon, 1) |
|
|
y_cd_m(1:knon) = ycoefh(1:knon, 1) |
|
|
END IF |
|
|
CALL ustarhb(knon, yu, yv, y_cd_m, yustar) |
|
|
|
|
|
IF (prt_level>9) THEN |
|
|
PRINT *, 'USTAR = ', yustar |
|
|
END IF |
|
|
|
|
|
! iflag_pbl peut etre utilise comme longuer de melange |
|
|
|
|
|
IF (iflag_pbl>=11) THEN |
|
|
CALL vdif_kcay(knon, dtime, rg, rd, ypaprs, yt, yzlev, yzlay, yu, yv, yteta, & |
|
|
y_cd_m, yq2, q2diag, ykmm, ykmn, yustar, iflag_pbl) |
|
|
ELSE |
|
|
CALL yamada4(knon, dtime, rg, rd, ypaprs, yt, yzlev, yzlay, yu, yv, yteta, & |
|
|
y_cd_m, yq2, ykmm, ykmn, ykmq, yustar, iflag_pbl) |
|
|
END IF |
|
|
|
|
|
ycoefm(1:knon, 1) = y_cd_m(1:knon) |
|
|
ycoefh(1:knon, 1) = y_cd_h(1:knon) |
|
|
ycoefm(1:knon, 2:klev) = ykmm(1:knon, 2:klev) |
|
|
ycoefh(1:knon, 2:klev) = ykmn(1:knon, 2:klev) |
|
|
|
|
|
|
|
|
END IF |
|
|
|
|
|
!ccccccccccccccccccccccccccccccccccccccccccccccccccccccccccccccccccccc |
|
|
! calculer la diffusion des vitesses "u" et "v" |
|
|
!ccccccccccccccccccccccccccccccccccccccccccccccccccccccccccccccccccc |
|
|
|
|
|
CALL clvent(knon, dtime, yu1, yv1, ycoefm, yt, yu, ypaprs, ypplay, & |
|
|
ydelp, y_d_u, y_flux_u) |
|
|
CALL clvent(knon, dtime, yu1, yv1, ycoefm, yt, yv, ypaprs, ypplay, & |
|
|
ydelp, y_d_v, y_flux_v) |
|
|
|
|
|
! pour le couplage |
|
|
ytaux = y_flux_u(:, 1) |
|
|
ytauy = y_flux_v(:, 1) |
|
|
|
|
|
! FH modif sur le cdrag temperature |
|
|
!$$$PB : déplace dans clcdrag |
|
|
!$$$ do i=1, knon |
|
|
!$$$ ycoefh(i, 1)=ycoefm(i, 1)*0.8 |
|
|
!$$$ enddo |
|
|
|
|
|
! calculer la diffusion de "q" et de "h" |
|
|
CALL clqh(dtime, itap, date0, jour, debut, lafin, rlon, rlat,& |
|
|
cufi, cvfi, knon, nsrf, ni, pctsrf, soil_model, ytsoil,& |
|
|
yqsol, ok_veget, ocean, npas, nexca, rmu0, co2_ppm, yrugos,& |
|
|
yrugoro, yu1, yv1, ycoefh, yt, yq, yts, ypaprs, ypplay,& |
|
|
ydelp, yrads, yalb, yalblw, ysnow, yqsurf, yrain_f, ysnow_f, & |
|
|
yfder, ytaux, ytauy, ywindsp, ysollw, ysollwdown, ysolsw,& |
|
|
yfluxlat, pctsrf_new, yagesno, y_d_t, y_d_q, y_d_ts,& |
|
|
yz0_new, y_flux_t, y_flux_q, y_dflux_t, y_dflux_q,& |
|
|
y_fqcalving, y_ffonte, y_run_off_lic_0, y_flux_o, y_flux_g,& |
|
|
ytslab, y_seaice) |
|
|
|
|
|
! calculer la longueur de rugosite sur ocean |
|
|
yrugm = 0. |
|
|
IF (nsrf==is_oce) THEN |
|
|
DO j = 1, knon |
|
|
yrugm(j) = 0.018*ycoefm(j, 1)*(yu1(j)**2+yv1(j)**2)/rg + & |
|
|
0.11*14E-6/sqrt(ycoefm(j, 1)*(yu1(j)**2+yv1(j)**2)) |
|
|
yrugm(j) = max(1.5E-05, yrugm(j)) |
|
|
END DO |
|
|
END IF |
|
|
DO j = 1, knon |
|
|
y_dflux_t(j) = y_dflux_t(j)*ypct(j) |
|
|
y_dflux_q(j) = y_dflux_q(j)*ypct(j) |
|
|
yu1(j) = yu1(j)*ypct(j) |
|
|
yv1(j) = yv1(j)*ypct(j) |
|
|
END DO |
|
|
|
|
|
DO k = 1, klev |
|
|
DO j = 1, knon |
|
|
i = ni(j) |
|
|
ycoefh(j, k) = ycoefh(j, k)*ypct(j) |
|
|
ycoefm(j, k) = ycoefm(j, k)*ypct(j) |
|
|
y_d_t(j, k) = y_d_t(j, k)*ypct(j) |
|
|
y_d_q(j, k) = y_d_q(j, k)*ypct(j) |
|
|
!§§§ PB |
|
|
flux_t(i, k, nsrf) = y_flux_t(j, k) |
|
|
flux_q(i, k, nsrf) = y_flux_q(j, k) |
|
|
flux_u(i, k, nsrf) = y_flux_u(j, k) |
|
|
flux_v(i, k, nsrf) = y_flux_v(j, k) |
|
|
!$$$ PB y_flux_t(j, k) = y_flux_t(j, k) * ypct(j) |
|
|
!$$$ PB y_flux_q(j, k) = y_flux_q(j, k) * ypct(j) |
|
|
y_d_u(j, k) = y_d_u(j, k)*ypct(j) |
|
|
y_d_v(j, k) = y_d_v(j, k)*ypct(j) |
|
|
!$$$ PB y_flux_u(j, k) = y_flux_u(j, k) * ypct(j) |
|
|
!$$$ PB y_flux_v(j, k) = y_flux_v(j, k) * ypct(j) |
|
|
END DO |
|
|
END DO |
|
|
|
|
|
|
|
|
evap(:, nsrf) = -flux_q(:, 1, nsrf) |
|
|
|
|
|
albe(:, nsrf) = 0. |
|
|
alblw(:, nsrf) = 0. |
|
|
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) |
|
|
!$$$ pb rugmer(i) = yrugm(j) |
|
|
IF (nsrf==is_oce) THEN |
|
|
rugmer(i) = yrugm(j) |
|
|
rugos(i, nsrf) = yrugm(j) |
|
|
END IF |
|
|
!IM cf JLD ?? |
|
|
agesno(i, nsrf) = yagesno(j) |
|
|
fqcalving(i, nsrf) = y_fqcalving(j) |
|
|
ffonte(i, nsrf) = y_ffonte(j) |
|
|
cdragh(i) = cdragh(i) + ycoefh(j, 1) |
|
|
cdragm(i) = cdragm(i) + ycoefm(j, 1) |
|
|
dflux_t(i) = dflux_t(i) + y_dflux_t(j) |
|
|
dflux_q(i) = dflux_q(i) + y_dflux_q(j) |
|
|
zu1(i) = zu1(i) + yu1(j) |
|
|
zv1(i) = zv1(i) + yv1(j) |
|
|
END DO |
|
|
IF (nsrf==is_ter) THEN |
|
|
DO j = 1, knon |
|
|
i = ni(j) |
|
|
qsol(i) = yqsol(j) |
|
|
END DO |
|
|
END IF |
|
|
IF (nsrf==is_lic) THEN |
|
|
DO j = 1, knon |
|
|
i = ni(j) |
|
|
run_off_lic_0(i) = y_run_off_lic_0(j) |
|
|
END DO |
|
|
END IF |
|
|
!$$$ PB ajout pour soil |
|
|
ftsoil(:, :, nsrf) = 0. |
|
|
DO k = 1, nsoilmx |
|
|
DO j = 1, knon |
|
|
i = ni(j) |
|
|
ftsoil(i, k, nsrf) = ytsoil(j, k) |
|
|
END DO |
|
|
END DO |
|
|
|
|
|
DO j = 1, knon |
|
|
i = ni(j) |
|
|
DO k = 1, klev |
|
|
d_t(i, k) = d_t(i, k) + y_d_t(j, k) |
|
|
d_q(i, k) = d_q(i, k) + y_d_q(j, k) |
|
|
!$$$ PB flux_t(i, k) = flux_t(i, k) + y_flux_t(j, k) |
|
|
!$$$ flux_q(i, k) = flux_q(i, k) + y_flux_q(j, k) |
|
|
d_u(i, k) = d_u(i, k) + y_d_u(j, k) |
|
|
d_v(i, k) = d_v(i, k) + y_d_v(j, k) |
|
|
!$$$ PB flux_u(i, k) = flux_u(i, k) + y_flux_u(j, k) |
|
|
!$$$ flux_v(i, k) = flux_v(i, k) + y_flux_v(j, k) |
|
|
zcoefh(i, k) = zcoefh(i, k) + ycoefh(j, k) |
|
|
END DO |
|
|
END DO |
|
|
|
|
|
|
|
|
!cc diagnostic t, q a 2m et u, v a 10m |
|
|
|
|
|
DO j = 1, knon |
|
|
i = ni(j) |
|
|
uzon(j) = yu(j, 1) + y_d_u(j, 1) |
|
|
vmer(j) = yv(j, 1) + y_d_v(j, 1) |
|
|
tair1(j) = yt(j, 1) + y_d_t(j, 1) |
|
|
qair1(j) = yq(j, 1) + y_d_q(j, 1) |
|
|
zgeo1(j) = rd*tair1(j)/(0.5*(ypaprs(j, 1)+ypplay(j, & |
|
|
1)))*(ypaprs(j, 1)-ypplay(j, 1)) |
|
|
tairsol(j) = yts(j) + y_d_ts(j) |
|
|
rugo1(j) = yrugos(j) |
|
|
IF (nsrf==is_oce) THEN |
|
|
rugo1(j) = rugos(i, nsrf) |
|
|
END IF |
|
|
psfce(j) = ypaprs(j, 1) |
|
|
patm(j) = ypplay(j, 1) |
|
|
|
|
|
qairsol(j) = yqsurf(j) |
|
|
END DO |
|
|
|
|
|
CALL stdlevvar(klon, knon, nsrf, zxli, uzon, vmer, tair1, qair1, zgeo1, & |
|
|
tairsol, qairsol, rugo1, psfce, patm, yt2m, yq2m, yt10m, yq10m, & |
|
|
yu10m, yustar) |
|
|
!IM 081204 END |
|
|
|
|
|
DO j = 1, knon |
|
|
i = ni(j) |
|
|
t2m(i, nsrf) = yt2m(j) |
|
|
q2m(i, nsrf) = yq2m(j) |
|
|
|
|
|
! u10m, v10m : composantes du vent a 10m sans spirale de Ekman |
|
|
u10m(i, nsrf) = (yu10m(j)*uzon(j))/sqrt(uzon(j)**2+vmer(j)**2) |
|
|
v10m(i, nsrf) = (yu10m(j)*vmer(j))/sqrt(uzon(j)**2+vmer(j)**2) |
|
|
|
|
|
END DO |
|
|
|
|
|
!IM cf AM : pbl, HBTM |
|
|
DO i = 1, knon |
|
|
y_cd_h(i) = ycoefh(i, 1) |
|
|
y_cd_m(i) = ycoefm(i, 1) |
|
|
END DO |
|
|
! 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) |
|
|
! print*, 'fin hbtm2' |
|
|
|
|
|
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) |
|
|
END DO |
|
|
|
|
|
|
|
|
DO j = 1, knon |
|
|
DO k = 1, klev + 1 |
|
|
i = ni(j) |
|
|
q2(i, k, nsrf) = yq2(j, k) |
|
|
END DO |
|
|
END DO |
|
|
!IM "slab" ocean |
|
|
IF (nsrf==is_oce) THEN |
|
|
DO j = 1, knon |
|
|
! on projette sur la grille globale |
|
|
i = ni(j) |
|
|
IF (pctsrf_new(i, is_oce)>epsfra) THEN |
|
|
flux_o(i) = y_flux_o(j) |
|
|
ELSE |
|
|
flux_o(i) = 0. |
|
|
END IF |
|
|
END DO |
|
|
END IF |
|
6 |
|
|
7 |
IF (nsrf==is_sic) THEN |
SUBROUTINE clmain(dtime, itap, pctsrf, pctsrf_new, t, q, u, v, & |
8 |
DO j = 1, knon |
jour, rmu0, co2_ppm, ok_veget, ocean, ts, & |
9 |
i = ni(j) |
soil_model, cdmmax, cdhmax, ksta, ksta_ter, ok_kzmin, ftsoil, & |
10 |
!IM 230604 on pondere lorsque l'on fait le bilan au sol : flux_g(i) = y_flux_g(j)*ypct(j) |
qsol, paprs, pplay, snow, qsurf, evap, albe, alblw, fluxlat, & |
11 |
IF (pctsrf_new(i, is_sic)>epsfra) THEN |
rain_fall, snow_f, solsw, sollw, fder, rlon, rlat, & |
12 |
flux_g(i) = y_flux_g(j) |
rugos, debut, agesno, rugoro, d_t, d_q, d_u, d_v, & |
13 |
ELSE |
d_ts, flux_t, flux_q, flux_u, flux_v, cdragh, cdragm, q2, & |
14 |
flux_g(i) = 0. |
dflux_t, dflux_q, ycoefh, zu1, zv1, t2m, q2m, u10m, v10m, pblh, & |
15 |
|
capcl, oliqcl, cteicl, pblt, therm, trmb1, trmb2, trmb3, plcl, & |
16 |
|
fqcalving, ffonte, run_off_lic_0, flux_o, flux_g, tslab, seaice) |
17 |
|
|
18 |
|
! From phylmd/clmain.F, version 1.6 2005/11/16 14:47:19 |
19 |
|
! Author: Z. X. Li (LMD/CNRS), date: 1993/08/18 |
20 |
|
! Objet : interface de couche limite (diffusion verticale) |
21 |
|
|
22 |
|
! Tout ce qui a trait aux traceurs est dans "phytrac". Le calcul |
23 |
|
! de la couche limite pour les traceurs se fait avec "cltrac" et |
24 |
|
! ne tient pas compte de la différentiation des sous-fractions de |
25 |
|
! sol. |
26 |
|
|
27 |
|
! Pour pouvoir extraire les coefficients d'échanges et le vent |
28 |
|
! dans la première couche, trois champs ont été créés : "ycoefh", |
29 |
|
! "zu1" et "zv1". Nous avons moyenné les valeurs de ces trois |
30 |
|
! champs sur les quatre sous-surfaces du modèle. |
31 |
|
|
32 |
|
use calendar, ONLY: ymds2ju |
33 |
|
use clqh_m, only: clqh |
34 |
|
use clvent_m, only: clvent |
35 |
|
use coefkz_m, only: coefkz |
36 |
|
use coefkzmin_m, only: coefkzmin |
37 |
|
USE conf_gcm_m, ONLY: prt_level |
38 |
|
USE conf_phys_m, ONLY: iflag_pbl |
39 |
|
USE dimens_m, ONLY: iim, jjm |
40 |
|
USE dimphy, ONLY: klev, klon, zmasq |
41 |
|
USE dimsoil, ONLY: nsoilmx |
42 |
|
USE dynetat0_m, ONLY: day_ini |
43 |
|
USE gath_cpl, ONLY: gath2cpl |
44 |
|
use hbtm_m, only: hbtm |
45 |
|
USE histbeg_totreg_m, ONLY: histbeg_totreg |
46 |
|
USE histdef_m, ONLY: histdef |
47 |
|
USE histend_m, ONLY: histend |
48 |
|
USE histsync_m, ONLY: histsync |
49 |
|
use histwrite_m, only: histwrite |
50 |
|
USE indicesol, ONLY: epsfra, is_lic, is_oce, is_sic, is_ter, nbsrf |
51 |
|
USE suphec_m, ONLY: rd, rg, rkappa |
52 |
|
USE temps, ONLY: annee_ref, itau_phy |
53 |
|
use ustarhb_m, only: ustarhb |
54 |
|
use vdif_kcay_m, only: vdif_kcay |
55 |
|
use yamada4_m, only: yamada4 |
56 |
|
|
57 |
|
! Arguments: |
58 |
|
|
59 |
|
REAL, INTENT(IN):: dtime ! interval du temps (secondes) |
60 |
|
INTEGER, INTENT(IN):: itap ! numero du pas de temps |
61 |
|
REAL, INTENT(inout):: pctsrf(klon, nbsrf) |
62 |
|
|
63 |
|
! la nouvelle repartition des surfaces sortie de l'interface |
64 |
|
REAL, INTENT(out):: pctsrf_new(klon, nbsrf) |
65 |
|
|
66 |
|
REAL, INTENT(IN):: t(klon, klev) ! temperature (K) |
67 |
|
REAL, INTENT(IN):: q(klon, klev) ! vapeur d'eau (kg/kg) |
68 |
|
REAL, INTENT(IN):: u(klon, klev), v(klon, klev) ! vitesse |
69 |
|
INTEGER, INTENT(IN):: jour ! jour de l'annee en cours |
70 |
|
REAL, intent(in):: rmu0(klon) ! cosinus de l'angle solaire zenithal |
71 |
|
REAL co2_ppm ! taux CO2 atmosphere |
72 |
|
LOGICAL ok_veget |
73 |
|
CHARACTER(len=*), INTENT(IN):: ocean |
74 |
|
REAL ts(klon, nbsrf) ! input-R- temperature du sol (en Kelvin) |
75 |
|
LOGICAL, INTENT(IN):: soil_model |
76 |
|
REAL, INTENT(IN):: cdmmax, cdhmax ! seuils cdrm, cdrh |
77 |
|
REAL ksta, ksta_ter |
78 |
|
LOGICAL ok_kzmin |
79 |
|
REAL ftsoil(klon, nsoilmx, nbsrf) |
80 |
|
REAL qsol(klon) |
81 |
|
REAL, INTENT(IN):: paprs(klon, klev+1) ! pression a intercouche (Pa) |
82 |
|
REAL, INTENT(IN):: pplay(klon, klev) ! pression au milieu de couche (Pa) |
83 |
|
REAL snow(klon, nbsrf) |
84 |
|
REAL qsurf(klon, nbsrf) |
85 |
|
REAL evap(klon, nbsrf) |
86 |
|
REAL albe(klon, nbsrf) |
87 |
|
REAL alblw(klon, nbsrf) |
88 |
|
|
89 |
|
REAL fluxlat(klon, nbsrf) |
90 |
|
|
91 |
|
REAL, intent(in):: rain_fall(klon), snow_f(klon) |
92 |
|
REAL, INTENT(IN):: solsw(klon, nbsrf), sollw(klon, nbsrf) |
93 |
|
REAL fder(klon) |
94 |
|
REAL, INTENT(IN):: rlon(klon) |
95 |
|
REAL, INTENT(IN):: rlat(klon) ! latitude en degrés |
96 |
|
|
97 |
|
REAL rugos(klon, nbsrf) |
98 |
|
! rugos----input-R- longeur de rugosite (en m) |
99 |
|
|
100 |
|
LOGICAL, INTENT(IN):: debut |
101 |
|
real agesno(klon, nbsrf) |
102 |
|
REAL, INTENT(IN):: rugoro(klon) |
103 |
|
|
104 |
|
REAL d_t(klon, klev), d_q(klon, klev) |
105 |
|
! d_t------output-R- le changement pour "t" |
106 |
|
! d_q------output-R- le changement pour "q" |
107 |
|
|
108 |
|
REAL, intent(out):: d_u(klon, klev), d_v(klon, klev) |
109 |
|
! changement pour "u" et "v" |
110 |
|
|
111 |
|
REAL d_ts(klon, nbsrf) |
112 |
|
! d_ts-----output-R- le changement pour "ts" |
113 |
|
|
114 |
|
REAL flux_t(klon, klev, nbsrf), flux_q(klon, klev, nbsrf) |
115 |
|
! flux_t---output-R- flux de chaleur sensible (CpT) J/m**2/s (W/m**2) |
116 |
|
! (orientation positive vers le bas) |
117 |
|
! flux_q---output-R- flux de vapeur d'eau (kg/m**2/s) |
118 |
|
|
119 |
|
REAL flux_u(klon, klev, nbsrf), flux_v(klon, klev, nbsrf) |
120 |
|
! flux_u---output-R- tension du vent X: (kg m/s)/(m**2 s) ou Pascal |
121 |
|
! flux_v---output-R- tension du vent Y: (kg m/s)/(m**2 s) ou Pascal |
122 |
|
|
123 |
|
REAL, INTENT(out):: cdragh(klon), cdragm(klon) |
124 |
|
real q2(klon, klev+1, nbsrf) |
125 |
|
|
126 |
|
REAL dflux_t(klon), dflux_q(klon) |
127 |
|
! dflux_t derive du flux sensible |
128 |
|
! dflux_q derive du flux latent |
129 |
|
!IM "slab" ocean |
130 |
|
|
131 |
|
REAL, intent(out):: ycoefh(klon, klev) |
132 |
|
REAL, intent(out):: zu1(klon) |
133 |
|
REAL zv1(klon) |
134 |
|
REAL t2m(klon, nbsrf), q2m(klon, nbsrf) |
135 |
|
REAL u10m(klon, nbsrf), v10m(klon, nbsrf) |
136 |
|
|
137 |
|
!IM cf. AM : pbl, hbtm (Comme les autres diagnostics on cumule ds |
138 |
|
! physiq ce qui permet de sortir les grdeurs par sous surface) |
139 |
|
REAL pblh(klon, nbsrf) |
140 |
|
! pblh------- HCL |
141 |
|
REAL capcl(klon, nbsrf) |
142 |
|
REAL oliqcl(klon, nbsrf) |
143 |
|
REAL cteicl(klon, nbsrf) |
144 |
|
REAL pblt(klon, nbsrf) |
145 |
|
! pblT------- T au nveau HCL |
146 |
|
REAL therm(klon, nbsrf) |
147 |
|
REAL trmb1(klon, nbsrf) |
148 |
|
! trmb1-------deep_cape |
149 |
|
REAL trmb2(klon, nbsrf) |
150 |
|
! trmb2--------inhibition |
151 |
|
REAL trmb3(klon, nbsrf) |
152 |
|
! trmb3-------Point Omega |
153 |
|
REAL plcl(klon, nbsrf) |
154 |
|
REAL fqcalving(klon, nbsrf), ffonte(klon, nbsrf) |
155 |
|
! ffonte----Flux thermique utilise pour fondre la neige |
156 |
|
! fqcalving-Flux d'eau "perdue" par la surface et necessaire pour limiter la |
157 |
|
! hauteur de neige, en kg/m2/s |
158 |
|
REAL run_off_lic_0(klon) |
159 |
|
|
160 |
|
REAL flux_o(klon), flux_g(klon) |
161 |
|
!IM "slab" ocean |
162 |
|
! flux_g---output-R- flux glace (pour OCEAN='slab ') |
163 |
|
! flux_o---output-R- flux ocean (pour OCEAN='slab ') |
164 |
|
|
165 |
|
REAL tslab(klon) |
166 |
|
! tslab-in/output-R temperature du slab ocean (en Kelvin) |
167 |
|
! uniqmnt pour slab |
168 |
|
|
169 |
|
REAL seaice(klon) |
170 |
|
! seaice---output-R- glace de mer (kg/m2) (pour OCEAN='slab ') |
171 |
|
|
172 |
|
! Local: |
173 |
|
|
174 |
|
REAL y_flux_o(klon), y_flux_g(klon) |
175 |
|
real ytslab(klon) |
176 |
|
real y_seaice(klon) |
177 |
|
REAL y_fqcalving(klon), y_ffonte(klon) |
178 |
|
real y_run_off_lic_0(klon) |
179 |
|
|
180 |
|
REAL rugmer(klon) |
181 |
|
|
182 |
|
REAL ytsoil(klon, nsoilmx) |
183 |
|
|
184 |
|
REAL yts(klon), yrugos(klon), ypct(klon), yz0_new(klon) |
185 |
|
REAL yalb(klon) |
186 |
|
REAL yalblw(klon) |
187 |
|
REAL yu1(klon), yv1(klon) |
188 |
|
! on rajoute en output yu1 et yv1 qui sont les vents dans |
189 |
|
! la premiere couche |
190 |
|
REAL ysnow(klon), yqsurf(klon), yagesno(klon), yqsol(klon) |
191 |
|
REAL yrain_f(klon), ysnow_f(klon) |
192 |
|
REAL ysollw(klon), ysolsw(klon) |
193 |
|
REAL yfder(klon), ytaux(klon), ytauy(klon) |
194 |
|
REAL yrugm(klon), yrads(klon), yrugoro(klon) |
195 |
|
|
196 |
|
REAL yfluxlat(klon) |
197 |
|
|
198 |
|
REAL y_d_ts(klon) |
199 |
|
REAL y_d_t(klon, klev), y_d_q(klon, klev) |
200 |
|
REAL y_d_u(klon, klev), y_d_v(klon, klev) |
201 |
|
REAL y_flux_t(klon, klev), y_flux_q(klon, klev) |
202 |
|
REAL y_flux_u(klon, klev), y_flux_v(klon, klev) |
203 |
|
REAL y_dflux_t(klon), y_dflux_q(klon) |
204 |
|
REAL coefh(klon, klev), coefm(klon, klev) |
205 |
|
REAL yu(klon, klev), yv(klon, klev) |
206 |
|
REAL yt(klon, klev), yq(klon, klev) |
207 |
|
REAL ypaprs(klon, klev+1), ypplay(klon, klev), ydelp(klon, klev) |
208 |
|
|
209 |
|
REAL ycoefm0(klon, klev), ycoefh0(klon, klev) |
210 |
|
|
211 |
|
REAL yzlay(klon, klev), yzlev(klon, klev+1), yteta(klon, klev) |
212 |
|
REAL ykmm(klon, klev+1), ykmn(klon, klev+1) |
213 |
|
REAL ykmq(klon, klev+1) |
214 |
|
REAL yq2(klon, klev+1) |
215 |
|
REAL q2diag(klon, klev+1) |
216 |
|
|
217 |
|
REAL u1lay(klon), v1lay(klon) |
218 |
|
REAL delp(klon, klev) |
219 |
|
INTEGER i, k, nsrf |
220 |
|
|
221 |
|
INTEGER ni(klon), knon, j |
222 |
|
|
223 |
|
REAL pctsrf_pot(klon, nbsrf) |
224 |
|
! "pourcentage potentiel" pour tenir compte des éventuelles |
225 |
|
! apparitions ou disparitions de la glace de mer |
226 |
|
|
227 |
|
REAL zx_alf1, zx_alf2 !valeur ambiante par extrapola. |
228 |
|
|
229 |
|
! maf pour sorties IOISPL en cas de debugagage |
230 |
|
|
231 |
|
CHARACTER(80) cldebug |
232 |
|
SAVE cldebug |
233 |
|
CHARACTER(8) cl_surf(nbsrf) |
234 |
|
SAVE cl_surf |
235 |
|
INTEGER nhoridbg, nidbg |
236 |
|
SAVE nhoridbg, nidbg |
237 |
|
INTEGER ndexbg(iim*(jjm+1)) |
238 |
|
REAL zx_lon(iim, jjm+1), zx_lat(iim, jjm+1), zjulian |
239 |
|
REAL tabindx(klon) |
240 |
|
REAL debugtab(iim, jjm+1) |
241 |
|
LOGICAL first_appel |
242 |
|
SAVE first_appel |
243 |
|
DATA first_appel/ .TRUE./ |
244 |
|
LOGICAL:: debugindex = .FALSE. |
245 |
|
INTEGER idayref |
246 |
|
|
247 |
|
REAL yt2m(klon), yq2m(klon), yu10m(klon) |
248 |
|
REAL yustar(klon) |
249 |
|
! -- LOOP |
250 |
|
REAL yu10mx(klon) |
251 |
|
REAL yu10my(klon) |
252 |
|
REAL ywindsp(klon) |
253 |
|
! -- LOOP |
254 |
|
|
255 |
|
REAL yt10m(klon), yq10m(klon) |
256 |
|
REAL ypblh(klon) |
257 |
|
REAL ylcl(klon) |
258 |
|
REAL ycapcl(klon) |
259 |
|
REAL yoliqcl(klon) |
260 |
|
REAL ycteicl(klon) |
261 |
|
REAL ypblt(klon) |
262 |
|
REAL ytherm(klon) |
263 |
|
REAL ytrmb1(klon) |
264 |
|
REAL ytrmb2(klon) |
265 |
|
REAL ytrmb3(klon) |
266 |
|
REAL uzon(klon), vmer(klon) |
267 |
|
REAL tair1(klon), qair1(klon), tairsol(klon) |
268 |
|
REAL psfce(klon), patm(klon) |
269 |
|
|
270 |
|
REAL qairsol(klon), zgeo1(klon) |
271 |
|
REAL rugo1(klon) |
272 |
|
|
273 |
|
! utiliser un jeu de fonctions simples |
274 |
|
LOGICAL zxli |
275 |
|
PARAMETER (zxli=.FALSE.) |
276 |
|
|
277 |
|
!------------------------------------------------------------ |
278 |
|
|
279 |
|
ytherm = 0. |
280 |
|
|
281 |
|
IF (debugindex .AND. first_appel) THEN |
282 |
|
first_appel = .FALSE. |
283 |
|
|
284 |
|
! initialisation sorties netcdf |
285 |
|
|
286 |
|
idayref = day_ini |
287 |
|
CALL ymds2ju(annee_ref, 1, idayref, 0., zjulian) |
288 |
|
CALL gr_fi_ecrit(1, klon, iim, jjm+1, rlon, zx_lon) |
289 |
|
DO i = 1, iim |
290 |
|
zx_lon(i, 1) = rlon(i+1) |
291 |
|
zx_lon(i, jjm+1) = rlon(i+1) |
292 |
|
END DO |
293 |
|
CALL gr_fi_ecrit(1, klon, iim, jjm+1, rlat, zx_lat) |
294 |
|
cldebug = 'sous_index' |
295 |
|
CALL histbeg_totreg(cldebug, zx_lon(:, 1), zx_lat(1, :), 1, & |
296 |
|
iim, 1, jjm+1, itau_phy, zjulian, dtime, nhoridbg, nidbg) |
297 |
|
! no vertical axis |
298 |
|
cl_surf(1) = 'ter' |
299 |
|
cl_surf(2) = 'lic' |
300 |
|
cl_surf(3) = 'oce' |
301 |
|
cl_surf(4) = 'sic' |
302 |
|
DO nsrf = 1, nbsrf |
303 |
|
CALL histdef(nidbg, cl_surf(nsrf), cl_surf(nsrf), '-', iim, jjm+1, & |
304 |
|
nhoridbg, 1, 1, 1, -99, 'inst', dtime, dtime) |
305 |
|
END DO |
306 |
|
CALL histend(nidbg) |
307 |
|
CALL histsync(nidbg) |
308 |
|
END IF |
309 |
|
|
310 |
|
DO k = 1, klev ! epaisseur de couche |
311 |
|
DO i = 1, klon |
312 |
|
delp(i, k) = paprs(i, k) - paprs(i, k+1) |
313 |
|
END DO |
314 |
|
END DO |
315 |
|
DO i = 1, klon ! vent de la premiere couche |
316 |
|
zx_alf1 = 1.0 |
317 |
|
zx_alf2 = 1.0 - zx_alf1 |
318 |
|
u1lay(i) = u(i, 1)*zx_alf1 + u(i, 2)*zx_alf2 |
319 |
|
v1lay(i) = v(i, 1)*zx_alf1 + v(i, 2)*zx_alf2 |
320 |
|
END DO |
321 |
|
|
322 |
|
! Initialization: |
323 |
|
rugmer = 0. |
324 |
|
cdragh = 0. |
325 |
|
cdragm = 0. |
326 |
|
dflux_t = 0. |
327 |
|
dflux_q = 0. |
328 |
|
zu1 = 0. |
329 |
|
zv1 = 0. |
330 |
|
ypct = 0. |
331 |
|
yts = 0. |
332 |
|
ysnow = 0. |
333 |
|
yqsurf = 0. |
334 |
|
yalb = 0. |
335 |
|
yalblw = 0. |
336 |
|
yrain_f = 0. |
337 |
|
ysnow_f = 0. |
338 |
|
yfder = 0. |
339 |
|
ytaux = 0. |
340 |
|
ytauy = 0. |
341 |
|
ysolsw = 0. |
342 |
|
ysollw = 0. |
343 |
|
yrugos = 0. |
344 |
|
yu1 = 0. |
345 |
|
yv1 = 0. |
346 |
|
yrads = 0. |
347 |
|
ypaprs = 0. |
348 |
|
ypplay = 0. |
349 |
|
ydelp = 0. |
350 |
|
yu = 0. |
351 |
|
yv = 0. |
352 |
|
yt = 0. |
353 |
|
yq = 0. |
354 |
|
pctsrf_new = 0. |
355 |
|
y_flux_u = 0. |
356 |
|
y_flux_v = 0. |
357 |
|
!$$ PB |
358 |
|
y_dflux_t = 0. |
359 |
|
y_dflux_q = 0. |
360 |
|
ytsoil = 999999. |
361 |
|
yrugoro = 0. |
362 |
|
! -- LOOP |
363 |
|
yu10mx = 0. |
364 |
|
yu10my = 0. |
365 |
|
ywindsp = 0. |
366 |
|
! -- LOOP |
367 |
|
d_ts = 0. |
368 |
|
!§§§ PB |
369 |
|
yfluxlat = 0. |
370 |
|
flux_t = 0. |
371 |
|
flux_q = 0. |
372 |
|
flux_u = 0. |
373 |
|
flux_v = 0. |
374 |
|
d_t = 0. |
375 |
|
d_q = 0. |
376 |
|
d_u = 0. |
377 |
|
d_v = 0. |
378 |
|
ycoefh = 0. |
379 |
|
|
380 |
|
! Boucler sur toutes les sous-fractions du sol: |
381 |
|
|
382 |
|
! Initialisation des "pourcentages potentiels". On considère ici qu'on |
383 |
|
! peut avoir potentiellement de la glace sur tout le domaine océanique |
384 |
|
! (à affiner) |
385 |
|
|
386 |
|
pctsrf_pot = pctsrf |
387 |
|
pctsrf_pot(:, is_oce) = 1. - zmasq |
388 |
|
pctsrf_pot(:, is_sic) = 1. - zmasq |
389 |
|
|
390 |
|
loop_surface: DO nsrf = 1, nbsrf |
391 |
|
! Chercher les indices : |
392 |
|
ni = 0 |
393 |
|
knon = 0 |
394 |
|
DO i = 1, klon |
395 |
|
! Pour déterminer le domaine à traiter, on utilise les surfaces |
396 |
|
! "potentielles" |
397 |
|
IF (pctsrf_pot(i, nsrf) > epsfra) THEN |
398 |
|
knon = knon + 1 |
399 |
|
ni(knon) = i |
400 |
|
END IF |
401 |
|
END DO |
402 |
|
|
403 |
|
! variables pour avoir une sortie IOIPSL des INDEX |
404 |
|
IF (debugindex) THEN |
405 |
|
tabindx = 0. |
406 |
|
DO i = 1, knon |
407 |
|
tabindx(i) = real(i) |
408 |
|
END DO |
409 |
|
debugtab = 0. |
410 |
|
ndexbg = 0 |
411 |
|
CALL gath2cpl(tabindx, debugtab, klon, knon, iim, jjm, ni) |
412 |
|
CALL histwrite(nidbg, cl_surf(nsrf), itap, debugtab) |
413 |
|
END IF |
414 |
|
|
415 |
|
if_knon: IF (knon /= 0) then |
416 |
|
DO j = 1, knon |
417 |
|
i = ni(j) |
418 |
|
ypct(j) = pctsrf(i, nsrf) |
419 |
|
yts(j) = ts(i, nsrf) |
420 |
|
ytslab(i) = tslab(i) |
421 |
|
ysnow(j) = snow(i, nsrf) |
422 |
|
yqsurf(j) = qsurf(i, nsrf) |
423 |
|
yalb(j) = albe(i, nsrf) |
424 |
|
yalblw(j) = alblw(i, nsrf) |
425 |
|
yrain_f(j) = rain_fall(i) |
426 |
|
ysnow_f(j) = snow_f(i) |
427 |
|
yagesno(j) = agesno(i, nsrf) |
428 |
|
yfder(j) = fder(i) |
429 |
|
ytaux(j) = flux_u(i, 1, nsrf) |
430 |
|
ytauy(j) = flux_v(i, 1, nsrf) |
431 |
|
ysolsw(j) = solsw(i, nsrf) |
432 |
|
ysollw(j) = sollw(i, nsrf) |
433 |
|
yrugos(j) = rugos(i, nsrf) |
434 |
|
yrugoro(j) = rugoro(i) |
435 |
|
yu1(j) = u1lay(i) |
436 |
|
yv1(j) = v1lay(i) |
437 |
|
yrads(j) = ysolsw(j) + ysollw(j) |
438 |
|
ypaprs(j, klev+1) = paprs(i, klev+1) |
439 |
|
y_run_off_lic_0(j) = run_off_lic_0(i) |
440 |
|
yu10mx(j) = u10m(i, nsrf) |
441 |
|
yu10my(j) = v10m(i, nsrf) |
442 |
|
ywindsp(j) = sqrt(yu10mx(j)*yu10mx(j)+yu10my(j)*yu10my(j)) |
443 |
|
END DO |
444 |
|
|
445 |
|
! IF bucket model for continent, copy soil water content |
446 |
|
IF (nsrf == is_ter .AND. .NOT. ok_veget) THEN |
447 |
|
DO j = 1, knon |
448 |
|
i = ni(j) |
449 |
|
yqsol(j) = qsol(i) |
450 |
|
END DO |
451 |
|
ELSE |
452 |
|
yqsol = 0. |
453 |
|
END IF |
454 |
|
|
455 |
|
DO k = 1, nsoilmx |
456 |
|
DO j = 1, knon |
457 |
|
i = ni(j) |
458 |
|
ytsoil(j, k) = ftsoil(i, k, nsrf) |
459 |
|
END DO |
460 |
|
END DO |
461 |
|
|
462 |
|
DO k = 1, klev |
463 |
|
DO j = 1, knon |
464 |
|
i = ni(j) |
465 |
|
ypaprs(j, k) = paprs(i, k) |
466 |
|
ypplay(j, k) = pplay(i, k) |
467 |
|
ydelp(j, k) = delp(i, k) |
468 |
|
yu(j, k) = u(i, k) |
469 |
|
yv(j, k) = v(i, k) |
470 |
|
yt(j, k) = t(i, k) |
471 |
|
yq(j, k) = q(i, k) |
472 |
|
END DO |
473 |
|
END DO |
474 |
|
|
475 |
|
! calculer Cdrag et les coefficients d'echange |
476 |
|
CALL coefkz(nsrf, knon, ypaprs, ypplay, ksta, ksta_ter, yts, yrugos, & |
477 |
|
yu, yv, yt, yq, yqsurf, coefm(:knon, :), coefh(:knon, :)) |
478 |
|
IF (iflag_pbl == 1) THEN |
479 |
|
CALL coefkz2(nsrf, knon, ypaprs, ypplay, yt, ycoefm0, ycoefh0) |
480 |
|
coefm(:knon, :) = max(coefm(:knon, :), ycoefm0(:knon, :)) |
481 |
|
coefh(:knon, :) = max(coefh(:knon, :), ycoefh0(:knon, :)) |
482 |
|
END IF |
483 |
|
|
484 |
|
! on met un seuil pour coefm et coefh |
485 |
|
IF (nsrf == is_oce) THEN |
486 |
|
coefm(:knon, 1) = min(coefm(:knon, 1), cdmmax) |
487 |
|
coefh(:knon, 1) = min(coefh(:knon, 1), cdhmax) |
488 |
|
END IF |
489 |
|
|
490 |
|
IF (ok_kzmin) THEN |
491 |
|
! Calcul d'une diffusion minimale pour les conditions tres stables |
492 |
|
CALL coefkzmin(knon, ypaprs, ypplay, yu, yv, yt, yq, & |
493 |
|
coefm(:knon, 1), ycoefm0, ycoefh0) |
494 |
|
coefm(:knon, :) = max(coefm(:knon, :), ycoefm0(:knon, :)) |
495 |
|
coefh(:knon, :) = max(coefh(:knon, :), ycoefh0(:knon, :)) |
496 |
END IF |
END IF |
|
END DO |
|
497 |
|
|
498 |
END IF |
IF (iflag_pbl >= 3) THEN |
499 |
!nsrf.EQ.is_sic |
! MELLOR ET YAMADA adapté à Mars, Richard Fournier et |
500 |
IF (ocean=='slab ') THEN |
! Frédéric Hourdin |
501 |
IF (nsrf==is_oce) THEN |
yzlay(:knon, 1) = rd * yt(:knon, 1) / (0.5 * (ypaprs(:knon, 1) & |
502 |
tslab(1:klon) = ytslab(1:klon) |
+ ypplay(:knon, 1))) & |
503 |
seaice(1:klon) = y_seaice(1:klon) |
* (ypaprs(:knon, 1) - ypplay(:knon, 1)) / rg |
504 |
!nsrf |
DO k = 2, klev |
505 |
END IF |
yzlay(1:knon, k) = yzlay(1:knon, k-1) & |
506 |
!OCEAN |
+ rd * 0.5 * (yt(1:knon, k-1) + yt(1:knon, k)) & |
507 |
END IF |
/ ypaprs(1:knon, k) & |
508 |
END DO |
* (ypplay(1:knon, k-1) - ypplay(1:knon, k)) / rg |
509 |
|
END DO |
510 |
|
DO k = 1, klev |
511 |
|
yteta(1:knon, k) = yt(1:knon, k)*(ypaprs(1:knon, 1) & |
512 |
|
/ ypplay(1:knon, k))**rkappa * (1.+0.61*yq(1:knon, k)) |
513 |
|
END DO |
514 |
|
yzlev(1:knon, 1) = 0. |
515 |
|
yzlev(:knon, klev+1) = 2. * yzlay(:knon, klev) & |
516 |
|
- yzlay(:knon, klev - 1) |
517 |
|
DO k = 2, klev |
518 |
|
yzlev(1:knon, k) = 0.5*(yzlay(1:knon, k)+yzlay(1:knon, k-1)) |
519 |
|
END DO |
520 |
|
DO k = 1, klev + 1 |
521 |
|
DO j = 1, knon |
522 |
|
i = ni(j) |
523 |
|
yq2(j, k) = q2(i, k, nsrf) |
524 |
|
END DO |
525 |
|
END DO |
526 |
|
|
527 |
|
CALL ustarhb(knon, yu, yv, coefm(:knon, 1), yustar) |
528 |
|
|
529 |
|
IF (prt_level > 9) THEN |
530 |
|
PRINT *, 'USTAR = ', yustar |
531 |
|
END IF |
532 |
|
|
533 |
|
! iflag_pbl peut être utilisé comme longueur de mélange |
534 |
|
|
535 |
|
IF (iflag_pbl >= 11) THEN |
536 |
|
CALL vdif_kcay(knon, dtime, rg, rd, ypaprs, yt, yzlev, yzlay, & |
537 |
|
yu, yv, yteta, coefm(:knon, 1), yq2, q2diag, ykmm, ykmn, & |
538 |
|
yustar, iflag_pbl) |
539 |
|
ELSE |
540 |
|
CALL yamada4(knon, dtime, rg, yzlev, yzlay, yu, yv, yteta, & |
541 |
|
coefm(:knon, 1), yq2, ykmm, ykmn, ykmq, yustar, iflag_pbl) |
542 |
|
END IF |
543 |
|
|
544 |
|
coefm(:knon, 2:) = ykmm(:knon, 2:klev) |
545 |
|
coefh(:knon, 2:) = ykmn(:knon, 2:klev) |
546 |
|
END IF |
547 |
|
|
548 |
|
! calculer la diffusion des vitesses "u" et "v" |
549 |
|
CALL clvent(knon, dtime, yu1, yv1, coefm(:knon, :), yt, yu, ypaprs, & |
550 |
|
ypplay, ydelp, y_d_u, y_flux_u) |
551 |
|
CALL clvent(knon, dtime, yu1, yv1, coefm(:knon, :), yt, yv, ypaprs, & |
552 |
|
ypplay, ydelp, y_d_v, y_flux_v) |
553 |
|
|
554 |
|
! pour le couplage |
555 |
|
ytaux = y_flux_u(:, 1) |
556 |
|
ytauy = y_flux_v(:, 1) |
557 |
|
|
558 |
|
! calculer la diffusion de "q" et de "h" |
559 |
|
CALL clqh(dtime, itap, jour, debut, rlat, knon, nsrf, ni, pctsrf, & |
560 |
|
soil_model, ytsoil, yqsol, ok_veget, ocean, rmu0, co2_ppm, & |
561 |
|
yrugos, yrugoro, yu1, yv1, coefh(:knon, :), yt, yq, yts, & |
562 |
|
ypaprs, ypplay, ydelp, yrads, yalb, yalblw, ysnow, yqsurf, & |
563 |
|
yrain_f, ysnow_f, yfder, ysolsw, yfluxlat, pctsrf_new, & |
564 |
|
yagesno, y_d_t, y_d_q, y_d_ts, yz0_new, y_flux_t, y_flux_q, & |
565 |
|
y_dflux_t, y_dflux_q, y_fqcalving, y_ffonte, y_run_off_lic_0, & |
566 |
|
y_flux_o, y_flux_g, ytslab, y_seaice) |
567 |
|
|
568 |
|
! calculer la longueur de rugosite sur ocean |
569 |
|
yrugm = 0. |
570 |
|
IF (nsrf == is_oce) THEN |
571 |
|
DO j = 1, knon |
572 |
|
yrugm(j) = 0.018*coefm(j, 1)*(yu1(j)**2+yv1(j)**2)/rg + & |
573 |
|
0.11*14E-6/sqrt(coefm(j, 1)*(yu1(j)**2+yv1(j)**2)) |
574 |
|
yrugm(j) = max(1.5E-05, yrugm(j)) |
575 |
|
END DO |
576 |
|
END IF |
577 |
|
DO j = 1, knon |
578 |
|
y_dflux_t(j) = y_dflux_t(j)*ypct(j) |
579 |
|
y_dflux_q(j) = y_dflux_q(j)*ypct(j) |
580 |
|
yu1(j) = yu1(j)*ypct(j) |
581 |
|
yv1(j) = yv1(j)*ypct(j) |
582 |
|
END DO |
583 |
|
|
584 |
|
DO k = 1, klev |
585 |
|
DO j = 1, knon |
586 |
|
i = ni(j) |
587 |
|
coefh(j, k) = coefh(j, k)*ypct(j) |
588 |
|
coefm(j, k) = coefm(j, k)*ypct(j) |
589 |
|
y_d_t(j, k) = y_d_t(j, k)*ypct(j) |
590 |
|
y_d_q(j, k) = y_d_q(j, k)*ypct(j) |
591 |
|
flux_t(i, k, nsrf) = y_flux_t(j, k) |
592 |
|
flux_q(i, k, nsrf) = y_flux_q(j, k) |
593 |
|
flux_u(i, k, nsrf) = y_flux_u(j, k) |
594 |
|
flux_v(i, k, nsrf) = y_flux_v(j, k) |
595 |
|
y_d_u(j, k) = y_d_u(j, k)*ypct(j) |
596 |
|
y_d_v(j, k) = y_d_v(j, k)*ypct(j) |
597 |
|
END DO |
598 |
|
END DO |
599 |
|
|
600 |
|
evap(:, nsrf) = -flux_q(:, 1, nsrf) |
601 |
|
|
602 |
|
albe(:, nsrf) = 0. |
603 |
|
alblw(:, nsrf) = 0. |
604 |
|
snow(:, nsrf) = 0. |
605 |
|
qsurf(:, nsrf) = 0. |
606 |
|
rugos(:, nsrf) = 0. |
607 |
|
fluxlat(:, nsrf) = 0. |
608 |
|
DO j = 1, knon |
609 |
|
i = ni(j) |
610 |
|
d_ts(i, nsrf) = y_d_ts(j) |
611 |
|
albe(i, nsrf) = yalb(j) |
612 |
|
alblw(i, nsrf) = yalblw(j) |
613 |
|
snow(i, nsrf) = ysnow(j) |
614 |
|
qsurf(i, nsrf) = yqsurf(j) |
615 |
|
rugos(i, nsrf) = yz0_new(j) |
616 |
|
fluxlat(i, nsrf) = yfluxlat(j) |
617 |
|
IF (nsrf == is_oce) THEN |
618 |
|
rugmer(i) = yrugm(j) |
619 |
|
rugos(i, nsrf) = yrugm(j) |
620 |
|
END IF |
621 |
|
agesno(i, nsrf) = yagesno(j) |
622 |
|
fqcalving(i, nsrf) = y_fqcalving(j) |
623 |
|
ffonte(i, nsrf) = y_ffonte(j) |
624 |
|
cdragh(i) = cdragh(i) + coefh(j, 1) |
625 |
|
cdragm(i) = cdragm(i) + coefm(j, 1) |
626 |
|
dflux_t(i) = dflux_t(i) + y_dflux_t(j) |
627 |
|
dflux_q(i) = dflux_q(i) + y_dflux_q(j) |
628 |
|
zu1(i) = zu1(i) + yu1(j) |
629 |
|
zv1(i) = zv1(i) + yv1(j) |
630 |
|
END DO |
631 |
|
IF (nsrf == is_ter) THEN |
632 |
|
DO j = 1, knon |
633 |
|
i = ni(j) |
634 |
|
qsol(i) = yqsol(j) |
635 |
|
END DO |
636 |
|
END IF |
637 |
|
IF (nsrf == is_lic) THEN |
638 |
|
DO j = 1, knon |
639 |
|
i = ni(j) |
640 |
|
run_off_lic_0(i) = y_run_off_lic_0(j) |
641 |
|
END DO |
642 |
|
END IF |
643 |
|
!$$$ PB ajout pour soil |
644 |
|
ftsoil(:, :, nsrf) = 0. |
645 |
|
DO k = 1, nsoilmx |
646 |
|
DO j = 1, knon |
647 |
|
i = ni(j) |
648 |
|
ftsoil(i, k, nsrf) = ytsoil(j, k) |
649 |
|
END DO |
650 |
|
END DO |
651 |
|
|
652 |
|
DO j = 1, knon |
653 |
|
i = ni(j) |
654 |
|
DO k = 1, klev |
655 |
|
d_t(i, k) = d_t(i, k) + y_d_t(j, k) |
656 |
|
d_q(i, k) = d_q(i, k) + y_d_q(j, k) |
657 |
|
d_u(i, k) = d_u(i, k) + y_d_u(j, k) |
658 |
|
d_v(i, k) = d_v(i, k) + y_d_v(j, k) |
659 |
|
ycoefh(i, k) = ycoefh(i, k) + coefh(j, k) |
660 |
|
END DO |
661 |
|
END DO |
662 |
|
|
663 |
|
!cc diagnostic t, q a 2m et u, v a 10m |
664 |
|
|
665 |
|
DO j = 1, knon |
666 |
|
i = ni(j) |
667 |
|
uzon(j) = yu(j, 1) + y_d_u(j, 1) |
668 |
|
vmer(j) = yv(j, 1) + y_d_v(j, 1) |
669 |
|
tair1(j) = yt(j, 1) + y_d_t(j, 1) |
670 |
|
qair1(j) = yq(j, 1) + y_d_q(j, 1) |
671 |
|
zgeo1(j) = rd*tair1(j)/(0.5*(ypaprs(j, 1)+ypplay(j, & |
672 |
|
1)))*(ypaprs(j, 1)-ypplay(j, 1)) |
673 |
|
tairsol(j) = yts(j) + y_d_ts(j) |
674 |
|
rugo1(j) = yrugos(j) |
675 |
|
IF (nsrf == is_oce) THEN |
676 |
|
rugo1(j) = rugos(i, nsrf) |
677 |
|
END IF |
678 |
|
psfce(j) = ypaprs(j, 1) |
679 |
|
patm(j) = ypplay(j, 1) |
680 |
|
|
681 |
|
qairsol(j) = yqsurf(j) |
682 |
|
END DO |
683 |
|
|
684 |
|
CALL stdlevvar(klon, knon, nsrf, zxli, uzon, vmer, tair1, qair1, & |
685 |
|
zgeo1, tairsol, qairsol, rugo1, psfce, patm, yt2m, yq2m, & |
686 |
|
yt10m, yq10m, yu10m, yustar) |
687 |
|
|
688 |
|
DO j = 1, knon |
689 |
|
i = ni(j) |
690 |
|
t2m(i, nsrf) = yt2m(j) |
691 |
|
q2m(i, nsrf) = yq2m(j) |
692 |
|
|
693 |
|
! u10m, v10m : composantes du vent a 10m sans spirale de Ekman |
694 |
|
u10m(i, nsrf) = (yu10m(j)*uzon(j))/sqrt(uzon(j)**2+vmer(j)**2) |
695 |
|
v10m(i, nsrf) = (yu10m(j)*vmer(j))/sqrt(uzon(j)**2+vmer(j)**2) |
696 |
|
|
697 |
|
END DO |
698 |
|
|
699 |
|
CALL hbtm(knon, ypaprs, ypplay, yt2m, yt10m, yq2m, yq10m, yustar, & |
700 |
|
y_flux_t, y_flux_q, yu, yv, yt, yq, ypblh, ycapcl, yoliqcl, & |
701 |
|
ycteicl, ypblt, ytherm, ytrmb1, ytrmb2, ytrmb3, ylcl) |
702 |
|
|
703 |
|
DO j = 1, knon |
704 |
|
i = ni(j) |
705 |
|
pblh(i, nsrf) = ypblh(j) |
706 |
|
plcl(i, nsrf) = ylcl(j) |
707 |
|
capcl(i, nsrf) = ycapcl(j) |
708 |
|
oliqcl(i, nsrf) = yoliqcl(j) |
709 |
|
cteicl(i, nsrf) = ycteicl(j) |
710 |
|
pblt(i, nsrf) = ypblt(j) |
711 |
|
therm(i, nsrf) = ytherm(j) |
712 |
|
trmb1(i, nsrf) = ytrmb1(j) |
713 |
|
trmb2(i, nsrf) = ytrmb2(j) |
714 |
|
trmb3(i, nsrf) = ytrmb3(j) |
715 |
|
END DO |
716 |
|
|
717 |
|
DO j = 1, knon |
718 |
|
DO k = 1, klev + 1 |
719 |
|
i = ni(j) |
720 |
|
q2(i, k, nsrf) = yq2(j, k) |
721 |
|
END DO |
722 |
|
END DO |
723 |
|
!IM "slab" ocean |
724 |
|
IF (nsrf == is_oce) THEN |
725 |
|
DO j = 1, knon |
726 |
|
! on projette sur la grille globale |
727 |
|
i = ni(j) |
728 |
|
IF (pctsrf_new(i, is_oce)>epsfra) THEN |
729 |
|
flux_o(i) = y_flux_o(j) |
730 |
|
ELSE |
731 |
|
flux_o(i) = 0. |
732 |
|
END IF |
733 |
|
END DO |
734 |
|
END IF |
735 |
|
|
736 |
|
IF (nsrf == is_sic) THEN |
737 |
|
DO j = 1, knon |
738 |
|
i = ni(j) |
739 |
|
! On pondère lorsque l'on fait le bilan au sol : |
740 |
|
IF (pctsrf_new(i, is_sic)>epsfra) THEN |
741 |
|
flux_g(i) = y_flux_g(j) |
742 |
|
ELSE |
743 |
|
flux_g(i) = 0. |
744 |
|
END IF |
745 |
|
END DO |
746 |
|
|
747 |
|
END IF |
748 |
|
IF (ocean == 'slab ') THEN |
749 |
|
IF (nsrf == is_oce) THEN |
750 |
|
tslab(1:klon) = ytslab(1:klon) |
751 |
|
seaice(1:klon) = y_seaice(1:klon) |
752 |
|
END IF |
753 |
|
END IF |
754 |
|
end IF if_knon |
755 |
|
END DO loop_surface |
756 |
|
|
757 |
|
! On utilise les nouvelles surfaces |
758 |
|
|
759 |
! On utilise les nouvelles surfaces |
rugos(:, is_oce) = rugmer |
760 |
! A rajouter: conservation de l'albedo |
pctsrf = pctsrf_new |
761 |
|
|
762 |
rugos(:, is_oce) = rugmer |
END SUBROUTINE clmain |
|
pctsrf = pctsrf_new |
|
763 |
|
|
764 |
END SUBROUTINE clmain |
end module clmain_m |