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module clmain_m |
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IMPLICIT NONE |
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|
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contains |
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|
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SUBROUTINE clmain(dtime, pctsrf, t, q, u, v, julien, mu0, ftsol, cdmmax, & |
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cdhmax, ksta, ksta_ter, ok_kzmin, ftsoil, qsol, paprs, pplay, fsnow, & |
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qsurf, evap, falbe, fluxlat, rain_fall, snow_f, fsolsw, fsollw, fder, & |
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frugs, agesno, rugoro, d_t, d_q, d_u, d_v, d_ts, flux_t, flux_q, & |
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flux_u, flux_v, cdragh, cdragm, q2, dflux_t, dflux_q, ycoefh, zu1, & |
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zv1, t2m, q2m, u10m, v10m, pblh, capcl, oliqcl, cteicl, pblt, therm, & |
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trmb1, trmb2, trmb3, plcl, fqcalving, ffonte, run_off_lic_0) |
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! From phylmd/clmain.F, version 1.6, 2005/11/16 14:47:19 |
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! Author: Z. X. Li (LMD/CNRS), date: 1993/08/18 |
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! Objet : interface de couche limite (diffusion verticale) |
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! Tout ce qui a trait aux traceurs est dans "phytrac". Le calcul |
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! de la couche limite pour les traceurs se fait avec "cltrac" et |
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! ne tient pas compte de la diff\'erentiation des sous-fractions |
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! de sol. |
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|
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! Pour pouvoir extraire les coefficients d'\'echanges et le vent |
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! dans la premi\`ere couche, trois champs ont \'et\'e cr\'e\'es : "ycoefh", |
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! "zu1" et "zv1". Nous avons moyenn\'e les valeurs de ces trois |
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! champs sur les quatre sous-surfaces du mod\`ele. |
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|
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use clqh_m, only: clqh |
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use clvent_m, only: clvent |
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use coefkz_m, only: coefkz |
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use coefkzmin_m, only: coefkzmin |
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USE conf_gcm_m, ONLY: prt_level, lmt_pas |
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USE conf_phys_m, ONLY: iflag_pbl |
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USE dimphy, ONLY: klev, klon, zmasq |
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USE dimsoil, ONLY: nsoilmx |
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use hbtm_m, only: hbtm |
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USE indicesol, ONLY: epsfra, is_lic, is_oce, is_sic, is_ter, nbsrf |
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USE interfoce_lim_m, ONLY: interfoce_lim |
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use stdlevvar_m, only: stdlevvar |
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USE suphec_m, ONLY: rd, rg, rkappa |
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use time_phylmdz, only: itap |
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use ustarhb_m, only: ustarhb |
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use vdif_kcay_m, only: vdif_kcay |
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use yamada4_m, only: yamada4 |
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REAL, INTENT(IN):: dtime ! interval du temps (secondes) |
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|
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REAL, INTENT(inout):: pctsrf(klon, nbsrf) |
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! tableau des pourcentages de surface de chaque maille |
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REAL, INTENT(IN):: t(klon, klev) ! temperature (K) |
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REAL, INTENT(IN):: q(klon, klev) ! vapeur d'eau (kg/kg) |
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REAL, INTENT(IN):: u(klon, klev), v(klon, klev) ! vitesse |
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INTEGER, INTENT(IN):: julien ! jour de l'annee en cours |
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REAL, intent(in):: mu0(klon) ! cosinus de l'angle solaire zenithal |
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REAL, INTENT(IN):: ftsol(:, :) ! (klon, nbsrf) temp\'erature du sol (en K) |
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REAL, INTENT(IN):: cdmmax, cdhmax ! seuils cdrm, cdrh |
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REAL, INTENT(IN):: ksta, ksta_ter |
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LOGICAL, INTENT(IN):: ok_kzmin |
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REAL, INTENT(inout):: ftsoil(klon, nsoilmx, nbsrf) |
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! soil temperature of surface fraction |
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REAL, INTENT(inout):: qsol(klon) |
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! column-density of water in soil, in kg m-2 |
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REAL, INTENT(IN):: paprs(klon, klev+1) ! pression a intercouche (Pa) |
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REAL, INTENT(IN):: pplay(klon, klev) ! pression au milieu de couche (Pa) |
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REAL, INTENT(inout):: fsnow(:, :) ! (klon, nbsrf) \'epaisseur neigeuse |
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REAL qsurf(klon, nbsrf) |
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REAL evap(klon, nbsrf) |
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REAL, intent(inout):: falbe(klon, nbsrf) |
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REAL, intent(out):: fluxlat(:, :) ! (klon, nbsrf) |
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REAL, intent(in):: rain_fall(klon) |
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! liquid water mass flux (kg/m2/s), positive down |
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REAL, intent(in):: snow_f(klon) |
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! solid water mass flux (kg/m2/s), positive down |
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REAL, INTENT(IN):: fsolsw(klon, nbsrf), fsollw(klon, nbsrf) |
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REAL, intent(in):: fder(:) ! (klon) |
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REAL, intent(inout):: frugs(klon, nbsrf) ! longueur de rugosit\'e (en m) |
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real agesno(klon, nbsrf) |
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REAL, INTENT(IN):: rugoro(klon) |
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REAL d_t(klon, klev), d_q(klon, klev) |
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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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REAL, intent(out):: d_u(klon, klev), d_v(klon, klev) |
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! changement pour "u" et "v" |
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REAL, intent(out):: d_ts(:, :) ! (klon, nbsrf) variation of ftsol |
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REAL, intent(out):: flux_t(klon, nbsrf) |
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! flux de chaleur sensible (Cp T) (W/m2) (orientation positive vers |
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! le bas) à la surface |
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REAL, intent(out):: flux_q(klon, nbsrf) |
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! flux de vapeur d'eau (kg/m2/s) à la surface |
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REAL, intent(out):: flux_u(klon, nbsrf), flux_v(klon, nbsrf) |
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! tension du vent à la surface, en Pa |
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REAL, INTENT(out):: cdragh(klon), cdragm(klon) |
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real q2(klon, klev+1, nbsrf) |
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REAL, INTENT(out):: dflux_t(klon), dflux_q(klon) |
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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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REAL, intent(out):: ycoefh(klon, klev) |
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REAL, intent(out):: zu1(klon) |
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REAL zv1(klon) |
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REAL, INTENT(inout):: t2m(klon, nbsrf), q2m(klon, nbsrf) |
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REAL u10m(klon, nbsrf), v10m(klon, nbsrf) |
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! Ionela Musat cf. Anne Mathieu : planetary boundary layer, hbtm |
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! (Comme les autres diagnostics on cumule dans physiq ce qui |
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! permet de sortir les grandeurs par sous-surface) |
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REAL pblh(klon, nbsrf) ! height of planetary boundary layer |
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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, INTENT(inout):: pblt(klon, nbsrf) ! T au nveau HCL |
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REAL therm(klon, nbsrf) |
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REAL trmb1(klon, nbsrf) |
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! trmb1-------deep_cape |
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REAL trmb2(klon, nbsrf) |
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! trmb2--------inhibition |
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REAL trmb3(klon, nbsrf) |
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! trmb3-------Point Omega |
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REAL plcl(klon, nbsrf) |
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REAL fqcalving(klon, nbsrf), ffonte(klon, nbsrf) |
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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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REAL run_off_lic_0(klon) |
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! Local: |
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LOGICAL:: firstcal = .true. |
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! la nouvelle repartition des surfaces sortie de l'interface |
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REAL, save:: pctsrf_new_oce(klon) |
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REAL, save:: pctsrf_new_sic(klon) |
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REAL y_fqcalving(klon), y_ffonte(klon) |
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real y_run_off_lic_0(klon) |
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REAL rugmer(klon) |
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REAL ytsoil(klon, nsoilmx) |
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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 yu1(klon), yv1(klon) |
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! On ajoute en output yu1 et yv1 qui sont les vents dans |
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! la premi\`ere couche. |
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REAL snow(klon), yqsurf(klon), yagesno(klon) |
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real yqsol(klon) |
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! column-density of water in soil, in kg m-2 |
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REAL yrain_f(klon) |
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! liquid water mass flux (kg/m2/s), positive down |
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REAL ysnow_f(klon) |
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! solid water mass flux (kg/m2/s), positive down |
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REAL yfder(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), y_flux_q(klon) |
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REAL y_flux_u(klon), y_flux_v(klon) |
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REAL y_dflux_t(klon), y_dflux_q(klon) |
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REAL coefh(klon, klev), coefm(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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REAL ycoefm0(klon, klev), ycoefh0(klon, klev) |
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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) |
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REAL q2diag(klon, klev+1) |
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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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REAL pctsrf_pot(klon, nbsrf) |
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! "pourcentage potentiel" pour tenir compte des \'eventuelles |
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! apparitions ou disparitions de la glace de mer |
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REAL zx_alf1, zx_alf2 ! valeur ambiante par extrapolation |
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REAL yt2m(klon), yq2m(klon), yu10m(klon) |
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REAL yustar(klon) |
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REAL yt10m(klon), yq10m(klon) |
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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 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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guez |
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guez |
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REAL qairsol(klon), zgeo1(klon) |
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REAL rugo1(klon) |
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guez |
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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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guez |
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!------------------------------------------------------------ |
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guez |
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ytherm = 0. |
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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 |
| 242 |
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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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guez |
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guez |
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! Initialization: |
| 249 |
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rugmer = 0. |
| 250 |
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cdragh = 0. |
| 251 |
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cdragm = 0. |
| 252 |
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dflux_t = 0. |
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dflux_q = 0. |
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zu1 = 0. |
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zv1 = 0. |
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ypct = 0. |
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yqsurf = 0. |
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yrain_f = 0. |
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ysnow_f = 0. |
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yrugos = 0. |
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yu1 = 0. |
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yv1 = 0. |
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ypaprs = 0. |
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ypplay = 0. |
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ydelp = 0. |
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yu = 0. |
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yv = 0. |
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yt = 0. |
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yq = 0. |
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y_dflux_t = 0. |
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y_dflux_q = 0. |
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guez |
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yrugoro = 0. |
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guez |
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d_ts = 0. |
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guez |
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flux_t = 0. |
| 275 |
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flux_q = 0. |
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flux_u = 0. |
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flux_v = 0. |
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guez |
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fluxlat = 0. |
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guez |
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d_t = 0. |
| 280 |
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d_q = 0. |
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d_u = 0. |
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d_v = 0. |
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guez |
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ycoefh = 0. |
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guez |
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|
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guez |
145 |
! Initialisation des "pourcentages potentiels". On consid\`ere ici qu'on |
| 286 |
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! peut avoir potentiellement de la glace sur tout le domaine oc\'eanique |
| 287 |
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! (\`a affiner) |
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guez |
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guez |
202 |
pctsrf_pot(:, is_ter) = pctsrf(:, is_ter) |
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pctsrf_pot(:, is_lic) = pctsrf(:, is_lic) |
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38 |
pctsrf_pot(:, is_oce) = 1. - zmasq |
| 292 |
|
|
pctsrf_pot(:, is_sic) = 1. - zmasq |
| 293 |
guez |
15 |
|
| 294 |
guez |
202 |
! Tester si c'est le moment de lire le fichier: |
| 295 |
|
|
if (mod(itap - 1, lmt_pas) == 0) then |
| 296 |
guez |
221 |
CALL interfoce_lim(julien, pctsrf_new_oce, pctsrf_new_sic) |
| 297 |
guez |
202 |
endif |
| 298 |
|
|
|
| 299 |
guez |
99 |
! Boucler sur toutes les sous-fractions du sol: |
| 300 |
|
|
|
| 301 |
guez |
49 |
loop_surface: DO nsrf = 1, nbsrf |
| 302 |
|
|
! Chercher les indices : |
| 303 |
guez |
38 |
ni = 0 |
| 304 |
|
|
knon = 0 |
| 305 |
|
|
DO i = 1, klon |
| 306 |
guez |
145 |
! Pour d\'eterminer le domaine \`a traiter, on utilise les surfaces |
| 307 |
guez |
38 |
! "potentielles" |
| 308 |
|
|
IF (pctsrf_pot(i, nsrf) > epsfra) THEN |
| 309 |
|
|
knon = knon + 1 |
| 310 |
|
|
ni(knon) = i |
| 311 |
|
|
END IF |
| 312 |
|
|
END DO |
| 313 |
guez |
15 |
|
| 314 |
guez |
62 |
if_knon: IF (knon /= 0) then |
| 315 |
guez |
38 |
DO j = 1, knon |
| 316 |
|
|
i = ni(j) |
| 317 |
guez |
62 |
ypct(j) = pctsrf(i, nsrf) |
| 318 |
guez |
207 |
yts(j) = ftsol(i, nsrf) |
| 319 |
guez |
215 |
snow(j) = fsnow(i, nsrf) |
| 320 |
guez |
62 |
yqsurf(j) = qsurf(i, nsrf) |
| 321 |
guez |
155 |
yalb(j) = falbe(i, nsrf) |
| 322 |
guez |
62 |
yrain_f(j) = rain_fall(i) |
| 323 |
|
|
ysnow_f(j) = snow_f(i) |
| 324 |
|
|
yagesno(j) = agesno(i, nsrf) |
| 325 |
|
|
yfder(j) = fder(i) |
| 326 |
guez |
222 |
yrugos(j) = frugs(i, nsrf) |
| 327 |
guez |
62 |
yrugoro(j) = rugoro(i) |
| 328 |
|
|
yu1(j) = u1lay(i) |
| 329 |
|
|
yv1(j) = v1lay(i) |
| 330 |
guez |
222 |
yrads(j) = fsolsw(i, nsrf) + fsollw(i, nsrf) |
| 331 |
guez |
62 |
ypaprs(j, klev+1) = paprs(i, klev+1) |
| 332 |
|
|
y_run_off_lic_0(j) = run_off_lic_0(i) |
| 333 |
guez |
38 |
END DO |
| 334 |
guez |
3 |
|
| 335 |
guez |
99 |
! For continent, copy soil water content |
| 336 |
|
|
IF (nsrf == is_ter) THEN |
| 337 |
|
|
yqsol(:knon) = qsol(ni(:knon)) |
| 338 |
guez |
62 |
ELSE |
| 339 |
|
|
yqsol = 0. |
| 340 |
|
|
END IF |
| 341 |
guez |
3 |
|
| 342 |
guez |
208 |
ytsoil(:knon, :) = ftsoil(ni(:knon), :, nsrf) |
| 343 |
guez |
3 |
|
| 344 |
guez |
38 |
DO k = 1, klev |
| 345 |
|
|
DO j = 1, knon |
| 346 |
|
|
i = ni(j) |
| 347 |
guez |
62 |
ypaprs(j, k) = paprs(i, k) |
| 348 |
|
|
ypplay(j, k) = pplay(i, k) |
| 349 |
|
|
ydelp(j, k) = delp(i, k) |
| 350 |
|
|
yu(j, k) = u(i, k) |
| 351 |
|
|
yv(j, k) = v(i, k) |
| 352 |
|
|
yt(j, k) = t(i, k) |
| 353 |
|
|
yq(j, k) = q(i, k) |
| 354 |
guez |
38 |
END DO |
| 355 |
|
|
END DO |
| 356 |
guez |
3 |
|
| 357 |
guez |
62 |
! calculer Cdrag et les coefficients d'echange |
| 358 |
guez |
221 |
CALL coefkz(nsrf, ypaprs, ypplay, ksta, ksta_ter, yts(:knon), & |
| 359 |
|
|
yrugos, yu, yv, yt, yq, yqsurf(:knon), coefm(:knon, :), & |
| 360 |
|
|
coefh(:knon, :)) |
| 361 |
guez |
62 |
IF (iflag_pbl == 1) THEN |
| 362 |
|
|
CALL coefkz2(nsrf, knon, ypaprs, ypplay, yt, ycoefm0, ycoefh0) |
| 363 |
|
|
coefm(:knon, :) = max(coefm(:knon, :), ycoefm0(:knon, :)) |
| 364 |
|
|
coefh(:knon, :) = max(coefh(:knon, :), ycoefh0(:knon, :)) |
| 365 |
|
|
END IF |
| 366 |
guez |
3 |
|
| 367 |
guez |
70 |
! on met un seuil pour coefm et coefh |
| 368 |
guez |
62 |
IF (nsrf == is_oce) THEN |
| 369 |
|
|
coefm(:knon, 1) = min(coefm(:knon, 1), cdmmax) |
| 370 |
|
|
coefh(:knon, 1) = min(coefh(:knon, 1), cdhmax) |
| 371 |
guez |
38 |
END IF |
| 372 |
guez |
3 |
|
| 373 |
guez |
62 |
IF (ok_kzmin) THEN |
| 374 |
|
|
! Calcul d'une diffusion minimale pour les conditions tres stables |
| 375 |
|
|
CALL coefkzmin(knon, ypaprs, ypplay, yu, yv, yt, yq, & |
| 376 |
guez |
70 |
coefm(:knon, 1), ycoefm0, ycoefh0) |
| 377 |
guez |
62 |
coefm(:knon, :) = max(coefm(:knon, :), ycoefm0(:knon, :)) |
| 378 |
|
|
coefh(:knon, :) = max(coefh(:knon, :), ycoefh0(:knon, :)) |
| 379 |
guez |
98 |
END IF |
| 380 |
guez |
3 |
|
| 381 |
guez |
62 |
IF (iflag_pbl >= 3) THEN |
| 382 |
guez |
145 |
! Mellor et Yamada adapt\'e \`a Mars, Richard Fournier et |
| 383 |
|
|
! Fr\'ed\'eric Hourdin |
| 384 |
guez |
62 |
yzlay(:knon, 1) = rd * yt(:knon, 1) / (0.5 * (ypaprs(:knon, 1) & |
| 385 |
|
|
+ ypplay(:knon, 1))) & |
| 386 |
|
|
* (ypaprs(:knon, 1) - ypplay(:knon, 1)) / rg |
| 387 |
|
|
DO k = 2, klev |
| 388 |
|
|
yzlay(1:knon, k) = yzlay(1:knon, k-1) & |
| 389 |
|
|
+ rd * 0.5 * (yt(1:knon, k-1) + yt(1:knon, k)) & |
| 390 |
|
|
/ ypaprs(1:knon, k) & |
| 391 |
|
|
* (ypplay(1:knon, k-1) - ypplay(1:knon, k)) / rg |
| 392 |
|
|
END DO |
| 393 |
|
|
DO k = 1, klev |
| 394 |
|
|
yteta(1:knon, k) = yt(1:knon, k)*(ypaprs(1:knon, 1) & |
| 395 |
|
|
/ ypplay(1:knon, k))**rkappa * (1.+0.61*yq(1:knon, k)) |
| 396 |
|
|
END DO |
| 397 |
|
|
yzlev(1:knon, 1) = 0. |
| 398 |
|
|
yzlev(:knon, klev+1) = 2. * yzlay(:knon, klev) & |
| 399 |
|
|
- yzlay(:knon, klev - 1) |
| 400 |
|
|
DO k = 2, klev |
| 401 |
|
|
yzlev(1:knon, k) = 0.5*(yzlay(1:knon, k)+yzlay(1:knon, k-1)) |
| 402 |
|
|
END DO |
| 403 |
|
|
DO k = 1, klev + 1 |
| 404 |
|
|
DO j = 1, knon |
| 405 |
|
|
i = ni(j) |
| 406 |
|
|
yq2(j, k) = q2(i, k, nsrf) |
| 407 |
|
|
END DO |
| 408 |
|
|
END DO |
| 409 |
|
|
|
| 410 |
|
|
CALL ustarhb(knon, yu, yv, coefm(:knon, 1), yustar) |
| 411 |
guez |
99 |
IF (prt_level > 9) PRINT *, 'USTAR = ', yustar |
| 412 |
guez |
62 |
|
| 413 |
guez |
145 |
! iflag_pbl peut \^etre utilis\'e comme longueur de m\'elange |
| 414 |
guez |
62 |
|
| 415 |
|
|
IF (iflag_pbl >= 11) THEN |
| 416 |
guez |
145 |
CALL vdif_kcay(knon, dtime, rg, ypaprs, yzlev, yzlay, yu, yv, & |
| 417 |
|
|
yteta, coefm(:knon, 1), yq2, q2diag, ykmm, ykmn, yustar, & |
| 418 |
|
|
iflag_pbl) |
| 419 |
guez |
62 |
ELSE |
| 420 |
|
|
CALL yamada4(knon, dtime, rg, yzlev, yzlay, yu, yv, yteta, & |
| 421 |
|
|
coefm(:knon, 1), yq2, ykmm, ykmn, ykmq, yustar, iflag_pbl) |
| 422 |
|
|
END IF |
| 423 |
|
|
|
| 424 |
|
|
coefm(:knon, 2:) = ykmm(:knon, 2:klev) |
| 425 |
|
|
coefh(:knon, 2:) = ykmn(:knon, 2:klev) |
| 426 |
guez |
38 |
END IF |
| 427 |
guez |
3 |
|
| 428 |
guez |
62 |
! calculer la diffusion des vitesses "u" et "v" |
| 429 |
guez |
70 |
CALL clvent(knon, dtime, yu1, yv1, coefm(:knon, :), yt, yu, ypaprs, & |
| 430 |
guez |
206 |
ypplay, ydelp, y_d_u, y_flux_u(:knon)) |
| 431 |
guez |
70 |
CALL clvent(knon, dtime, yu1, yv1, coefm(:knon, :), yt, yv, ypaprs, & |
| 432 |
guez |
206 |
ypplay, ydelp, y_d_v, y_flux_v(:knon)) |
| 433 |
guez |
3 |
|
| 434 |
guez |
62 |
! calculer la diffusion de "q" et de "h" |
| 435 |
guez |
221 |
CALL clqh(dtime, julien, firstcal, nsrf, ni(:knon), & |
| 436 |
|
|
ytsoil(:knon, :), yqsol, mu0, yrugos, yrugoro, yu1, yv1, & |
| 437 |
|
|
coefh(:knon, :), yt, yq, yts(:knon), ypaprs, ypplay, ydelp, & |
| 438 |
guez |
222 |
yrads(:knon), yalb(:knon), snow(:knon), yqsurf, yrain_f, & |
| 439 |
|
|
ysnow_f, yfder(:knon), yfluxlat(:knon), pctsrf_new_sic, & |
| 440 |
|
|
yagesno(:knon), y_d_t, y_d_q, y_d_ts(:knon), yz0_new, & |
| 441 |
|
|
y_flux_t(:knon), y_flux_q(:knon), y_dflux_t(:knon), & |
| 442 |
|
|
y_dflux_q(:knon), y_fqcalving, y_ffonte, y_run_off_lic_0) |
| 443 |
guez |
3 |
|
| 444 |
guez |
62 |
! calculer la longueur de rugosite sur ocean |
| 445 |
|
|
yrugm = 0. |
| 446 |
|
|
IF (nsrf == is_oce) THEN |
| 447 |
|
|
DO j = 1, knon |
| 448 |
|
|
yrugm(j) = 0.018*coefm(j, 1)*(yu1(j)**2+yv1(j)**2)/rg + & |
| 449 |
|
|
0.11*14E-6/sqrt(coefm(j, 1)*(yu1(j)**2+yv1(j)**2)) |
| 450 |
|
|
yrugm(j) = max(1.5E-05, yrugm(j)) |
| 451 |
|
|
END DO |
| 452 |
|
|
END IF |
| 453 |
guez |
38 |
DO j = 1, knon |
| 454 |
guez |
62 |
y_dflux_t(j) = y_dflux_t(j)*ypct(j) |
| 455 |
|
|
y_dflux_q(j) = y_dflux_q(j)*ypct(j) |
| 456 |
|
|
yu1(j) = yu1(j)*ypct(j) |
| 457 |
|
|
yv1(j) = yv1(j)*ypct(j) |
| 458 |
guez |
38 |
END DO |
| 459 |
guez |
3 |
|
| 460 |
guez |
62 |
DO k = 1, klev |
| 461 |
|
|
DO j = 1, knon |
| 462 |
|
|
i = ni(j) |
| 463 |
|
|
coefh(j, k) = coefh(j, k)*ypct(j) |
| 464 |
|
|
coefm(j, k) = coefm(j, k)*ypct(j) |
| 465 |
|
|
y_d_t(j, k) = y_d_t(j, k)*ypct(j) |
| 466 |
|
|
y_d_q(j, k) = y_d_q(j, k)*ypct(j) |
| 467 |
|
|
y_d_u(j, k) = y_d_u(j, k)*ypct(j) |
| 468 |
|
|
y_d_v(j, k) = y_d_v(j, k)*ypct(j) |
| 469 |
|
|
END DO |
| 470 |
guez |
38 |
END DO |
| 471 |
guez |
3 |
|
| 472 |
guez |
214 |
flux_t(ni(:knon), nsrf) = y_flux_t(:knon) |
| 473 |
|
|
flux_q(ni(:knon), nsrf) = y_flux_q(:knon) |
| 474 |
|
|
flux_u(ni(:knon), nsrf) = y_flux_u(:knon) |
| 475 |
|
|
flux_v(ni(:knon), nsrf) = y_flux_v(:knon) |
| 476 |
guez |
15 |
|
| 477 |
guez |
206 |
evap(:, nsrf) = -flux_q(:, nsrf) |
| 478 |
|
|
|
| 479 |
guez |
155 |
falbe(:, nsrf) = 0. |
| 480 |
guez |
215 |
fsnow(:, nsrf) = 0. |
| 481 |
guez |
62 |
qsurf(:, nsrf) = 0. |
| 482 |
guez |
222 |
frugs(:, nsrf) = 0. |
| 483 |
guez |
38 |
DO j = 1, knon |
| 484 |
|
|
i = ni(j) |
| 485 |
guez |
62 |
d_ts(i, nsrf) = y_d_ts(j) |
| 486 |
guez |
155 |
falbe(i, nsrf) = yalb(j) |
| 487 |
guez |
215 |
fsnow(i, nsrf) = snow(j) |
| 488 |
guez |
62 |
qsurf(i, nsrf) = yqsurf(j) |
| 489 |
guez |
222 |
frugs(i, nsrf) = yz0_new(j) |
| 490 |
guez |
62 |
fluxlat(i, nsrf) = yfluxlat(j) |
| 491 |
|
|
IF (nsrf == is_oce) THEN |
| 492 |
|
|
rugmer(i) = yrugm(j) |
| 493 |
guez |
222 |
frugs(i, nsrf) = yrugm(j) |
| 494 |
guez |
62 |
END IF |
| 495 |
|
|
agesno(i, nsrf) = yagesno(j) |
| 496 |
|
|
fqcalving(i, nsrf) = y_fqcalving(j) |
| 497 |
|
|
ffonte(i, nsrf) = y_ffonte(j) |
| 498 |
|
|
cdragh(i) = cdragh(i) + coefh(j, 1) |
| 499 |
|
|
cdragm(i) = cdragm(i) + coefm(j, 1) |
| 500 |
|
|
dflux_t(i) = dflux_t(i) + y_dflux_t(j) |
| 501 |
|
|
dflux_q(i) = dflux_q(i) + y_dflux_q(j) |
| 502 |
|
|
zu1(i) = zu1(i) + yu1(j) |
| 503 |
|
|
zv1(i) = zv1(i) + yv1(j) |
| 504 |
guez |
38 |
END DO |
| 505 |
guez |
62 |
IF (nsrf == is_ter) THEN |
| 506 |
guez |
99 |
qsol(ni(:knon)) = yqsol(:knon) |
| 507 |
|
|
else IF (nsrf == is_lic) THEN |
| 508 |
guez |
62 |
DO j = 1, knon |
| 509 |
|
|
i = ni(j) |
| 510 |
|
|
run_off_lic_0(i) = y_run_off_lic_0(j) |
| 511 |
|
|
END DO |
| 512 |
|
|
END IF |
| 513 |
guez |
118 |
|
| 514 |
guez |
62 |
ftsoil(:, :, nsrf) = 0. |
| 515 |
guez |
208 |
ftsoil(ni(:knon), :, nsrf) = ytsoil(:knon, :) |
| 516 |
guez |
62 |
|
| 517 |
guez |
38 |
DO j = 1, knon |
| 518 |
|
|
i = ni(j) |
| 519 |
guez |
62 |
DO k = 1, klev |
| 520 |
|
|
d_t(i, k) = d_t(i, k) + y_d_t(j, k) |
| 521 |
|
|
d_q(i, k) = d_q(i, k) + y_d_q(j, k) |
| 522 |
|
|
d_u(i, k) = d_u(i, k) + y_d_u(j, k) |
| 523 |
|
|
d_v(i, k) = d_v(i, k) + y_d_v(j, k) |
| 524 |
guez |
70 |
ycoefh(i, k) = ycoefh(i, k) + coefh(j, k) |
| 525 |
guez |
62 |
END DO |
| 526 |
guez |
38 |
END DO |
| 527 |
guez |
62 |
|
| 528 |
guez |
99 |
! diagnostic t, q a 2m et u, v a 10m |
| 529 |
guez |
62 |
|
| 530 |
guez |
38 |
DO j = 1, knon |
| 531 |
|
|
i = ni(j) |
| 532 |
guez |
62 |
uzon(j) = yu(j, 1) + y_d_u(j, 1) |
| 533 |
|
|
vmer(j) = yv(j, 1) + y_d_v(j, 1) |
| 534 |
|
|
tair1(j) = yt(j, 1) + y_d_t(j, 1) |
| 535 |
|
|
qair1(j) = yq(j, 1) + y_d_q(j, 1) |
| 536 |
|
|
zgeo1(j) = rd*tair1(j)/(0.5*(ypaprs(j, 1)+ypplay(j, & |
| 537 |
|
|
1)))*(ypaprs(j, 1)-ypplay(j, 1)) |
| 538 |
|
|
tairsol(j) = yts(j) + y_d_ts(j) |
| 539 |
|
|
rugo1(j) = yrugos(j) |
| 540 |
|
|
IF (nsrf == is_oce) THEN |
| 541 |
guez |
222 |
rugo1(j) = frugs(i, nsrf) |
| 542 |
guez |
62 |
END IF |
| 543 |
|
|
psfce(j) = ypaprs(j, 1) |
| 544 |
|
|
patm(j) = ypplay(j, 1) |
| 545 |
guez |
15 |
|
| 546 |
guez |
62 |
qairsol(j) = yqsurf(j) |
| 547 |
guez |
38 |
END DO |
| 548 |
guez |
15 |
|
| 549 |
guez |
62 |
CALL stdlevvar(klon, knon, nsrf, zxli, uzon, vmer, tair1, qair1, & |
| 550 |
|
|
zgeo1, tairsol, qairsol, rugo1, psfce, patm, yt2m, yq2m, & |
| 551 |
|
|
yt10m, yq10m, yu10m, yustar) |
| 552 |
guez |
3 |
|
| 553 |
guez |
62 |
DO j = 1, knon |
| 554 |
|
|
i = ni(j) |
| 555 |
|
|
t2m(i, nsrf) = yt2m(j) |
| 556 |
|
|
q2m(i, nsrf) = yq2m(j) |
| 557 |
guez |
3 |
|
| 558 |
guez |
62 |
! u10m, v10m : composantes du vent a 10m sans spirale de Ekman |
| 559 |
|
|
u10m(i, nsrf) = (yu10m(j)*uzon(j))/sqrt(uzon(j)**2+vmer(j)**2) |
| 560 |
|
|
v10m(i, nsrf) = (yu10m(j)*vmer(j))/sqrt(uzon(j)**2+vmer(j)**2) |
| 561 |
|
|
END DO |
| 562 |
guez |
15 |
|
| 563 |
guez |
206 |
CALL hbtm(ypaprs, ypplay, yt2m, yq2m, yustar, y_flux_t(:knon), & |
| 564 |
|
|
y_flux_q(:knon), yu, yv, yt, yq, ypblh(:knon), ycapcl, & |
| 565 |
|
|
yoliqcl, ycteicl, ypblt, ytherm, ytrmb1, ytrmb2, ytrmb3, ylcl) |
| 566 |
guez |
15 |
|
| 567 |
guez |
38 |
DO j = 1, knon |
| 568 |
|
|
i = ni(j) |
| 569 |
guez |
62 |
pblh(i, nsrf) = ypblh(j) |
| 570 |
|
|
plcl(i, nsrf) = ylcl(j) |
| 571 |
|
|
capcl(i, nsrf) = ycapcl(j) |
| 572 |
|
|
oliqcl(i, nsrf) = yoliqcl(j) |
| 573 |
|
|
cteicl(i, nsrf) = ycteicl(j) |
| 574 |
|
|
pblt(i, nsrf) = ypblt(j) |
| 575 |
|
|
therm(i, nsrf) = ytherm(j) |
| 576 |
|
|
trmb1(i, nsrf) = ytrmb1(j) |
| 577 |
|
|
trmb2(i, nsrf) = ytrmb2(j) |
| 578 |
|
|
trmb3(i, nsrf) = ytrmb3(j) |
| 579 |
guez |
38 |
END DO |
| 580 |
guez |
3 |
|
| 581 |
guez |
38 |
DO j = 1, knon |
| 582 |
guez |
62 |
DO k = 1, klev + 1 |
| 583 |
|
|
i = ni(j) |
| 584 |
|
|
q2(i, k, nsrf) = yq2(j, k) |
| 585 |
|
|
END DO |
| 586 |
guez |
38 |
END DO |
| 587 |
guez |
215 |
else |
| 588 |
|
|
fsnow(:, nsrf) = 0. |
| 589 |
guez |
62 |
end IF if_knon |
| 590 |
guez |
49 |
END DO loop_surface |
| 591 |
guez |
15 |
|
| 592 |
guez |
38 |
! On utilise les nouvelles surfaces |
| 593 |
guez |
222 |
frugs(:, is_oce) = rugmer |
| 594 |
guez |
202 |
pctsrf(:, is_oce) = pctsrf_new_oce |
| 595 |
|
|
pctsrf(:, is_sic) = pctsrf_new_sic |
| 596 |
guez |
15 |
|
| 597 |
guez |
202 |
firstcal = .false. |
| 598 |
|
|
|
| 599 |
guez |
38 |
END SUBROUTINE clmain |
| 600 |
guez |
15 |
|
| 601 |
guez |
38 |
end module clmain_m |
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