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module physiq_m |
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|
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IMPLICIT none |
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|
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contains |
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|
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SUBROUTINE physiq(lafin, dayvrai, time, paprs, play, pphi, pphis, u, v, t, & |
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qx, omega, d_u, d_v, d_t, d_qx) |
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|
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! From phylmd/physiq.F, version 1.22 2006/02/20 09:38:28 |
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! (subversion revision 678) |
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|
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! Author: Z. X. Li (LMD/CNRS) 1993 |
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|
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! This is the main procedure for the "physics" part of the program. |
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|
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use aaam_bud_m, only: aaam_bud |
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USE abort_gcm_m, ONLY: abort_gcm |
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use aeropt_m, only: aeropt |
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use ajsec_m, only: ajsec |
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use calltherm_m, only: calltherm |
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USE clesphys, ONLY: cdhmax, cdmmax, ecrit_hf, ecrit_ins, ecrit_mth, & |
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ecrit_reg, ecrit_tra, ksta, ksta_ter, ok_kzmin |
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USE clesphys2, ONLY: cycle_diurne, conv_emanuel, nbapp_rad, new_oliq, & |
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ok_orodr, ok_orolf |
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USE clmain_m, ONLY: clmain |
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use clouds_gno_m, only: clouds_gno |
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use comconst, only: dtphys |
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USE comgeomphy, ONLY: airephy |
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USE concvl_m, ONLY: concvl |
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USE conf_gcm_m, ONLY: offline, raz_date, day_step, iphysiq |
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USE conf_phys_m, ONLY: conf_phys |
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use conflx_m, only: conflx |
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USE ctherm, ONLY: iflag_thermals, nsplit_thermals |
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use diagcld2_m, only: diagcld2 |
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use diagetpq_m, only: diagetpq |
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use diagphy_m, only: diagphy |
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USE dimens_m, ONLY: llm, nqmx |
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USE dimphy, ONLY: klon |
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USE dimsoil, ONLY: nsoilmx |
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use drag_noro_m, only: drag_noro |
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use dynetat0_m, only: day_ref, annee_ref |
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USE fcttre, ONLY: foeew, qsatl, qsats, thermcep |
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use fisrtilp_m, only: fisrtilp |
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USE hgardfou_m, ONLY: hgardfou |
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USE indicesol, ONLY: clnsurf, epsfra, is_lic, is_oce, is_sic, is_ter, & |
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nbsrf |
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USE ini_histins_m, ONLY: ini_histins |
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use netcdf95, only: NF95_CLOSE |
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use newmicro_m, only: newmicro |
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use nuage_m, only: nuage |
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USE orbite_m, ONLY: orbite |
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USE ozonecm_m, ONLY: ozonecm |
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USE phyetat0_m, ONLY: phyetat0, rlat, rlon |
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USE phyredem_m, ONLY: phyredem |
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USE phyredem0_m, ONLY: phyredem0 |
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USE phystokenc_m, ONLY: phystokenc |
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USE phytrac_m, ONLY: phytrac |
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USE qcheck_m, ONLY: qcheck |
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use radlwsw_m, only: radlwsw |
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use readsulfate_m, only: readsulfate |
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use readsulfate_preind_m, only: readsulfate_preind |
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use yoegwd, only: sugwd |
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USE suphec_m, ONLY: rcpd, retv, rg, rlvtt, romega, rsigma, rtt |
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use transp_m, only: transp |
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use transp_lay_m, only: transp_lay |
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use unit_nml_m, only: unit_nml |
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USE ymds2ju_m, ONLY: ymds2ju |
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USE yoethf_m, ONLY: r2es, rvtmp2 |
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use zenang_m, only: zenang |
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|
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logical, intent(in):: lafin ! dernier passage |
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|
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integer, intent(in):: dayvrai |
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! current day number, based at value 1 on January 1st of annee_ref |
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|
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REAL, intent(in):: time ! heure de la journ\'ee en fraction de jour |
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|
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REAL, intent(in):: paprs(:, :) ! (klon, llm + 1) |
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! pression pour chaque inter-couche, en Pa |
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|
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REAL, intent(in):: play(:, :) ! (klon, llm) |
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! pression pour le mileu de chaque couche (en Pa) |
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|
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REAL, intent(in):: pphi(:, :) ! (klon, llm) |
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! géopotentiel de chaque couche (référence sol) |
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|
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REAL, intent(in):: pphis(:) ! (klon) géopotentiel du sol |
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|
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REAL, intent(in):: u(:, :) ! (klon, llm) |
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! vitesse dans la direction X (de O a E) en m/s |
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|
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REAL, intent(in):: v(:, :) ! (klon, llm) vitesse Y (de S a N) en m/s |
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REAL, intent(in):: t(:, :) ! (klon, llm) temperature (K) |
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|
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REAL, intent(in):: qx(:, :, :) ! (klon, llm, nqmx) |
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! (humidit\'e sp\'ecifique et fractions massiques des autres traceurs) |
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|
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REAL, intent(in):: omega(:, :) ! (klon, llm) vitesse verticale en Pa/s |
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REAL, intent(out):: d_u(:, :) ! (klon, llm) tendance physique de "u" (m s-2) |
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REAL, intent(out):: d_v(:, :) ! (klon, llm) tendance physique de "v" (m s-2) |
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REAL, intent(out):: d_t(:, :) ! (klon, llm) tendance physique de "t" (K/s) |
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|
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REAL, intent(out):: d_qx(:, :, :) ! (klon, llm, nqmx) |
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! tendance physique de "qx" (s-1) |
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|
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! Local: |
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|
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LOGICAL:: firstcal = .true. |
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|
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LOGICAL, PARAMETER:: check = .FALSE. |
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! Verifier la conservation du modele en eau |
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|
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LOGICAL, PARAMETER:: ok_stratus = .FALSE. |
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! Ajouter artificiellement les stratus |
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|
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logical:: ok_journe = .false., ok_mensuel = .true., ok_instan = .false. |
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! sorties journalieres, mensuelles et instantanees dans les |
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! fichiers histday, histmth et histins |
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|
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LOGICAL ok_region ! sortir le fichier regional |
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PARAMETER (ok_region = .FALSE.) |
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|
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! pour phsystoke avec thermiques |
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REAL fm_therm(klon, llm + 1) |
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REAL entr_therm(klon, llm) |
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real, save:: q2(klon, llm + 1, nbsrf) |
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|
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INTEGER, PARAMETER:: ivap = 1 ! indice de traceur pour vapeur d'eau |
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INTEGER, PARAMETER:: iliq = 2 ! indice de traceur pour eau liquide |
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|
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REAL, save:: t_ancien(klon, llm), q_ancien(klon, llm) |
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LOGICAL, save:: ancien_ok |
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|
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REAL d_t_dyn(klon, llm) ! tendance dynamique pour "t" (K/s) |
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REAL d_q_dyn(klon, llm) ! tendance dynamique pour "q" (kg/kg/s) |
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|
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real da(klon, llm), phi(klon, llm, llm), mp(klon, llm) |
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|
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REAL swdn0(klon, llm + 1), swdn(klon, llm + 1) |
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REAL swup0(klon, llm + 1), swup(klon, llm + 1) |
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SAVE swdn0, swdn, swup0, swup |
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|
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REAL lwdn0(klon, llm + 1), lwdn(klon, llm + 1) |
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REAL lwup0(klon, llm + 1), lwup(klon, llm + 1) |
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SAVE lwdn0, lwdn, lwup0, lwup |
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|
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! prw: precipitable water |
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real prw(klon) |
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|
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! flwp, fiwp = Liquid Water Path & Ice Water Path (kg/m2) |
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! flwc, fiwc = Liquid Water Content & Ice Water Content (kg/kg) |
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REAL flwp(klon), fiwp(klon) |
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REAL flwc(klon, llm), fiwc(klon, llm) |
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|
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! Variables propres a la physique |
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|
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INTEGER, save:: radpas |
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! Radiative transfer computations are made every "radpas" call to |
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! "physiq". |
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|
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REAL radsol(klon) |
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SAVE radsol ! bilan radiatif au sol calcule par code radiatif |
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|
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INTEGER:: itap = 0 ! number of calls to "physiq" |
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|
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REAL, save:: ftsol(klon, nbsrf) ! skin temperature of surface fraction |
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|
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REAL, save:: ftsoil(klon, nsoilmx, nbsrf) |
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! soil temperature of surface fraction |
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|
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REAL, save:: fevap(klon, nbsrf) ! evaporation |
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REAL fluxlat(klon, nbsrf) |
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SAVE fluxlat |
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|
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REAL, save:: fqsurf(klon, nbsrf) |
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! humidite de l'air au contact de la surface |
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|
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REAL, save:: qsol(klon) |
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! column-density of water in soil, in kg m-2 |
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|
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REAL, save:: fsnow(klon, nbsrf) ! epaisseur neigeuse |
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REAL, save:: falbe(klon, nbsrf) ! albedo visible par type de surface |
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|
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! Param\`etres de l'orographie \`a l'\'echelle sous-maille (OESM) : |
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REAL, save:: zmea(klon) ! orographie moyenne |
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REAL, save:: zstd(klon) ! deviation standard de l'OESM |
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REAL, save:: zsig(klon) ! pente de l'OESM |
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REAL, save:: zgam(klon) ! anisotropie de l'OESM |
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REAL, save:: zthe(klon) ! orientation de l'OESM |
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REAL, save:: zpic(klon) ! Maximum de l'OESM |
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REAL, save:: zval(klon) ! Minimum de l'OESM |
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REAL, save:: rugoro(klon) ! longueur de rugosite de l'OESM |
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REAL zulow(klon), zvlow(klon) |
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INTEGER igwd, itest(klon) |
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|
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REAL, save:: agesno(klon, nbsrf) ! age de la neige |
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REAL, save:: run_off_lic_0(klon) |
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|
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! Variables li\'ees \`a la convection d'Emanuel : |
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REAL, save:: Ma(klon, llm) ! undilute upward mass flux |
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REAL, save:: qcondc(klon, llm) ! in-cld water content from convect |
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REAL, save:: sig1(klon, llm), w01(klon, llm) |
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|
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! Variables pour la couche limite (Alain Lahellec) : |
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REAL cdragh(klon) ! drag coefficient pour T and Q |
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REAL cdragm(klon) ! drag coefficient pour vent |
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|
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! Pour phytrac : |
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REAL ycoefh(klon, llm) ! coef d'echange pour phytrac |
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REAL yu1(klon) ! vents dans la premiere couche U |
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REAL yv1(klon) ! vents dans la premiere couche V |
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REAL ffonte(klon, nbsrf) !Flux thermique utilise pour fondre la neige |
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REAL fqcalving(klon, nbsrf) !Flux d'eau "perdue" par la surface |
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! !et necessaire pour limiter la |
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! !hauteur de neige, en kg/m2/s |
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REAL zxffonte(klon), zxfqcalving(klon) |
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|
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REAL pfrac_impa(klon, llm)! Produits des coefs lessivage impaction |
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save pfrac_impa |
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REAL pfrac_nucl(klon, llm)! Produits des coefs lessivage nucleation |
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save pfrac_nucl |
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REAL pfrac_1nucl(klon, llm)! Produits des coefs lessi nucl (alpha = 1) |
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save pfrac_1nucl |
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REAL frac_impa(klon, llm) ! fractions d'aerosols lessivees (impaction) |
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REAL frac_nucl(klon, llm) ! idem (nucleation) |
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|
| 228 |
REAL, save:: rain_fall(klon) |
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! liquid water mass flux (kg/m2/s), positive down |
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|
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REAL, save:: snow_fall(klon) |
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! solid water mass flux (kg/m2/s), positive down |
| 233 |
|
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REAL rain_tiedtke(klon), snow_tiedtke(klon) |
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|
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REAL evap(klon), devap(klon) ! evaporation and its derivative |
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REAL sens(klon), dsens(klon) ! chaleur sensible et sa derivee |
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REAL dlw(klon) ! derivee infra rouge |
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SAVE dlw |
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REAL bils(klon) ! bilan de chaleur au sol |
| 241 |
REAL, save:: fder(klon) ! Derive de flux (sensible et latente) |
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REAL ve(klon) ! integr. verticale du transport meri. de l'energie |
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REAL vq(klon) ! integr. verticale du transport meri. de l'eau |
| 244 |
REAL ue(klon) ! integr. verticale du transport zonal de l'energie |
| 245 |
REAL uq(klon) ! integr. verticale du transport zonal de l'eau |
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|
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REAL, save:: frugs(klon, nbsrf) ! longueur de rugosite |
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REAL zxrugs(klon) ! longueur de rugosite |
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|
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! Conditions aux limites |
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|
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INTEGER julien |
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INTEGER, SAVE:: lmt_pas ! number of time steps of "physics" per day |
| 254 |
REAL, save:: pctsrf(klon, nbsrf) ! percentage of surface |
| 255 |
REAL pctsrf_new(klon, nbsrf) ! pourcentage surfaces issus d'ORCHIDEE |
| 256 |
REAL, save:: albsol(klon) ! albedo du sol total visible |
| 257 |
REAL, SAVE:: wo(klon, llm) ! column density of ozone in a cell, in kDU |
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|
| 259 |
real, save:: clwcon(klon, llm), rnebcon(klon, llm) |
| 260 |
real, save:: clwcon0(klon, llm), rnebcon0(klon, llm) |
| 261 |
|
| 262 |
REAL rhcl(klon, llm) ! humiditi relative ciel clair |
| 263 |
REAL dialiq(klon, llm) ! eau liquide nuageuse |
| 264 |
REAL diafra(klon, llm) ! fraction nuageuse |
| 265 |
REAL cldliq(klon, llm) ! eau liquide nuageuse |
| 266 |
REAL cldfra(klon, llm) ! fraction nuageuse |
| 267 |
REAL cldtau(klon, llm) ! epaisseur optique |
| 268 |
REAL cldemi(klon, llm) ! emissivite infrarouge |
| 269 |
|
| 270 |
REAL fluxq(klon, llm, nbsrf) ! flux turbulent d'humidite |
| 271 |
REAL fluxt(klon, llm, nbsrf) ! flux turbulent de chaleur |
| 272 |
REAL fluxu(klon, llm, nbsrf) ! flux turbulent de vitesse u |
| 273 |
REAL fluxv(klon, llm, nbsrf) ! flux turbulent de vitesse v |
| 274 |
|
| 275 |
REAL zxfluxt(klon, llm) |
| 276 |
REAL zxfluxq(klon, llm) |
| 277 |
REAL zxfluxu(klon, llm) |
| 278 |
REAL zxfluxv(klon, llm) |
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|
| 280 |
! Le rayonnement n'est pas calcul\'e tous les pas, il faut donc que |
| 281 |
! les variables soient r\'emanentes. |
| 282 |
REAL, save:: heat(klon, llm) ! chauffage solaire |
| 283 |
REAL, save:: heat0(klon, llm) ! chauffage solaire ciel clair |
| 284 |
REAL, save:: cool(klon, llm) ! refroidissement infrarouge |
| 285 |
REAL, save:: cool0(klon, llm) ! refroidissement infrarouge ciel clair |
| 286 |
REAL, save:: topsw(klon), toplw(klon), solsw(klon) |
| 287 |
REAL, save:: sollw(klon) ! rayonnement infrarouge montant \`a la surface |
| 288 |
real, save:: sollwdown(klon) ! downward LW flux at surface |
| 289 |
REAL, save:: topsw0(klon), toplw0(klon), solsw0(klon), sollw0(klon) |
| 290 |
REAL, save:: albpla(klon) |
| 291 |
REAL fsollw(klon, nbsrf) ! bilan flux IR pour chaque sous surface |
| 292 |
REAL fsolsw(klon, nbsrf) ! flux solaire absorb. pour chaque sous surface |
| 293 |
|
| 294 |
REAL conv_q(klon, llm) ! convergence de l'humidite (kg/kg/s) |
| 295 |
REAL conv_t(klon, llm) ! convergence of temperature (K/s) |
| 296 |
|
| 297 |
REAL cldl(klon), cldm(klon), cldh(klon) !nuages bas, moyen et haut |
| 298 |
REAL cldt(klon), cldq(klon) !nuage total, eau liquide integree |
| 299 |
|
| 300 |
REAL zxtsol(klon), zxqsurf(klon), zxsnow(klon), zxfluxlat(klon) |
| 301 |
|
| 302 |
REAL dist, mu0(klon), fract(klon) |
| 303 |
real longi |
| 304 |
REAL z_avant(klon), z_apres(klon), z_factor(klon) |
| 305 |
REAL za, zb |
| 306 |
REAL zx_t, zx_qs, zcor |
| 307 |
real zqsat(klon, llm) |
| 308 |
INTEGER i, k, iq, nsrf |
| 309 |
REAL, PARAMETER:: t_coup = 234. |
| 310 |
REAL zphi(klon, llm) |
| 311 |
|
| 312 |
! cf. Anne Mathieu variables pour la couche limite atmosphérique (hbtm) |
| 313 |
|
| 314 |
REAL, SAVE:: pblh(klon, nbsrf) ! Hauteur de couche limite |
| 315 |
REAL, SAVE:: plcl(klon, nbsrf) ! Niveau de condensation de la CLA |
| 316 |
REAL, SAVE:: capCL(klon, nbsrf) ! CAPE de couche limite |
| 317 |
REAL, SAVE:: oliqCL(klon, nbsrf) ! eau_liqu integree de couche limite |
| 318 |
REAL, SAVE:: cteiCL(klon, nbsrf) ! cloud top instab. crit. couche limite |
| 319 |
REAL, SAVE:: pblt(klon, nbsrf) ! T a la Hauteur de couche limite |
| 320 |
REAL, SAVE:: therm(klon, nbsrf) |
| 321 |
REAL, SAVE:: trmb1(klon, nbsrf) ! deep_cape |
| 322 |
REAL, SAVE:: trmb2(klon, nbsrf) ! inhibition |
| 323 |
REAL, SAVE:: trmb3(klon, nbsrf) ! Point Omega |
| 324 |
! Grandeurs de sorties |
| 325 |
REAL s_pblh(klon), s_lcl(klon), s_capCL(klon) |
| 326 |
REAL s_oliqCL(klon), s_cteiCL(klon), s_pblt(klon) |
| 327 |
REAL s_therm(klon), s_trmb1(klon), s_trmb2(klon) |
| 328 |
REAL s_trmb3(klon) |
| 329 |
|
| 330 |
! Variables pour la convection de K. Emanuel : |
| 331 |
|
| 332 |
REAL upwd(klon, llm) ! saturated updraft mass flux |
| 333 |
REAL dnwd(klon, llm) ! saturated downdraft mass flux |
| 334 |
REAL dnwd0(klon, llm) ! unsaturated downdraft mass flux |
| 335 |
REAL cape(klon) ! CAPE |
| 336 |
SAVE cape |
| 337 |
|
| 338 |
INTEGER iflagctrl(klon) ! flag fonctionnement de convect |
| 339 |
|
| 340 |
! Variables du changement |
| 341 |
|
| 342 |
! con: convection |
| 343 |
! lsc: large scale condensation |
| 344 |
! ajs: ajustement sec |
| 345 |
! eva: \'evaporation de l'eau liquide nuageuse |
| 346 |
! vdf: vertical diffusion in boundary layer |
| 347 |
REAL d_t_con(klon, llm), d_q_con(klon, llm) |
| 348 |
REAL d_u_con(klon, llm), d_v_con(klon, llm) |
| 349 |
REAL d_t_lsc(klon, llm), d_q_lsc(klon, llm), d_ql_lsc(klon, llm) |
| 350 |
REAL d_t_ajs(klon, llm), d_q_ajs(klon, llm) |
| 351 |
REAL d_u_ajs(klon, llm), d_v_ajs(klon, llm) |
| 352 |
REAL rneb(klon, llm) |
| 353 |
|
| 354 |
REAL mfu(klon, llm), mfd(klon, llm) |
| 355 |
REAL pen_u(klon, llm), pen_d(klon, llm) |
| 356 |
REAL pde_u(klon, llm), pde_d(klon, llm) |
| 357 |
INTEGER kcbot(klon), kctop(klon), kdtop(klon) |
| 358 |
REAL pmflxr(klon, llm + 1), pmflxs(klon, llm + 1) |
| 359 |
REAL prfl(klon, llm + 1), psfl(klon, llm + 1) |
| 360 |
|
| 361 |
INTEGER, save:: ibas_con(klon), itop_con(klon) |
| 362 |
real ema_pct(klon) ! Emanuel pressure at cloud top, in Pa |
| 363 |
|
| 364 |
REAL rain_con(klon), rain_lsc(klon) |
| 365 |
REAL, save:: snow_con(klon) ! neige (mm / s) |
| 366 |
real snow_lsc(klon) |
| 367 |
REAL d_ts(klon, nbsrf) |
| 368 |
|
| 369 |
REAL d_u_vdf(klon, llm), d_v_vdf(klon, llm) |
| 370 |
REAL d_t_vdf(klon, llm), d_q_vdf(klon, llm) |
| 371 |
|
| 372 |
REAL d_u_oro(klon, llm), d_v_oro(klon, llm) |
| 373 |
REAL d_t_oro(klon, llm) |
| 374 |
REAL d_u_lif(klon, llm), d_v_lif(klon, llm) |
| 375 |
REAL d_t_lif(klon, llm) |
| 376 |
|
| 377 |
REAL, save:: ratqs(klon, llm) |
| 378 |
real ratqss(klon, llm), ratqsc(klon, llm) |
| 379 |
real:: ratqsbas = 0.01, ratqshaut = 0.3 |
| 380 |
|
| 381 |
! Parametres lies au nouveau schema de nuages (SB, PDF) |
| 382 |
real:: fact_cldcon = 0.375 |
| 383 |
real:: facttemps = 1.e-4 |
| 384 |
logical:: ok_newmicro = .true. |
| 385 |
real facteur |
| 386 |
|
| 387 |
integer:: iflag_cldcon = 1 |
| 388 |
logical ptconv(klon, llm) |
| 389 |
|
| 390 |
! Variables pour effectuer les appels en s\'erie : |
| 391 |
|
| 392 |
REAL t_seri(klon, llm), q_seri(klon, llm) |
| 393 |
REAL ql_seri(klon, llm) |
| 394 |
REAL u_seri(klon, llm), v_seri(klon, llm) |
| 395 |
REAL tr_seri(klon, llm, nqmx - 2) |
| 396 |
|
| 397 |
REAL zx_rh(klon, llm) |
| 398 |
|
| 399 |
REAL zustrdr(klon), zvstrdr(klon) |
| 400 |
REAL zustrli(klon), zvstrli(klon) |
| 401 |
REAL zustrph(klon), zvstrph(klon) |
| 402 |
REAL aam, torsfc |
| 403 |
|
| 404 |
INTEGER, SAVE:: nid_ins |
| 405 |
|
| 406 |
REAL ve_lay(klon, llm) ! transport meri. de l'energie a chaque niveau vert. |
| 407 |
REAL vq_lay(klon, llm) ! transport meri. de l'eau a chaque niveau vert. |
| 408 |
REAL ue_lay(klon, llm) ! transport zonal de l'energie a chaque niveau vert. |
| 409 |
REAL uq_lay(klon, llm) ! transport zonal de l'eau a chaque niveau vert. |
| 410 |
|
| 411 |
real date0 |
| 412 |
|
| 413 |
! Variables li\'ees au bilan d'\'energie et d'enthalpie : |
| 414 |
REAL ztsol(klon) |
| 415 |
REAL d_h_vcol, d_qt, d_ec |
| 416 |
REAL, SAVE:: d_h_vcol_phy |
| 417 |
REAL zero_v(klon) |
| 418 |
CHARACTER(LEN = 20) tit |
| 419 |
INTEGER:: ip_ebil = 0 ! print level for energy conservation diagnostics |
| 420 |
INTEGER:: if_ebil = 0 ! verbosity for diagnostics of energy conservation |
| 421 |
|
| 422 |
REAL d_t_ec(klon, llm) ! tendance due \`a la conversion Ec -> E thermique |
| 423 |
REAL ZRCPD |
| 424 |
|
| 425 |
REAL t2m(klon, nbsrf), q2m(klon, nbsrf) ! temperature and humidity at 2 m |
| 426 |
REAL u10m(klon, nbsrf), v10m(klon, nbsrf) ! vents a 10 m |
| 427 |
REAL zt2m(klon), zq2m(klon) ! temp., hum. 2 m moyenne s/ 1 maille |
| 428 |
REAL zu10m(klon), zv10m(klon) ! vents a 10 m moyennes s/1 maille |
| 429 |
|
| 430 |
! Aerosol effects: |
| 431 |
|
| 432 |
REAL sulfate(klon, llm) ! SO4 aerosol concentration (micro g/m3) |
| 433 |
|
| 434 |
REAL, save:: sulfate_pi(klon, llm) |
| 435 |
! SO4 aerosol concentration, in \mu g/m3, pre-industrial value |
| 436 |
|
| 437 |
REAL cldtaupi(klon, llm) |
| 438 |
! cloud optical thickness for pre-industrial (pi) aerosols |
| 439 |
|
| 440 |
REAL re(klon, llm) ! Cloud droplet effective radius |
| 441 |
REAL fl(klon, llm) ! denominator of re |
| 442 |
|
| 443 |
! Aerosol optical properties |
| 444 |
REAL, save:: tau_ae(klon, llm, 2), piz_ae(klon, llm, 2) |
| 445 |
REAL, save:: cg_ae(klon, llm, 2) |
| 446 |
|
| 447 |
REAL topswad(klon), solswad(klon) ! aerosol direct effect |
| 448 |
REAL topswai(klon), solswai(klon) ! aerosol indirect effect |
| 449 |
|
| 450 |
REAL aerindex(klon) ! POLDER aerosol index |
| 451 |
|
| 452 |
LOGICAL:: ok_ade = .false. ! apply aerosol direct effect |
| 453 |
LOGICAL:: ok_aie = .false. ! apply aerosol indirect effect |
| 454 |
|
| 455 |
REAL:: bl95_b0 = 2., bl95_b1 = 0.2 |
| 456 |
! Parameters in equation (D) of Boucher and Lohmann (1995, Tellus |
| 457 |
! B). They link cloud droplet number concentration to aerosol mass |
| 458 |
! concentration. |
| 459 |
|
| 460 |
SAVE u10m |
| 461 |
SAVE v10m |
| 462 |
SAVE t2m |
| 463 |
SAVE q2m |
| 464 |
SAVE ffonte |
| 465 |
SAVE fqcalving |
| 466 |
SAVE rain_con |
| 467 |
SAVE topswai |
| 468 |
SAVE topswad |
| 469 |
SAVE solswai |
| 470 |
SAVE solswad |
| 471 |
SAVE d_u_con |
| 472 |
SAVE d_v_con |
| 473 |
|
| 474 |
real zmasse(klon, llm) |
| 475 |
! (column-density of mass of air in a cell, in kg m-2) |
| 476 |
|
| 477 |
integer, save:: ncid_startphy, itau_phy |
| 478 |
|
| 479 |
namelist /physiq_nml/ ok_journe, ok_mensuel, ok_instan, fact_cldcon, & |
| 480 |
facttemps, ok_newmicro, iflag_cldcon, ratqsbas, ratqshaut, if_ebil, & |
| 481 |
ok_ade, ok_aie, bl95_b0, bl95_b1, iflag_thermals, nsplit_thermals |
| 482 |
|
| 483 |
!---------------------------------------------------------------- |
| 484 |
|
| 485 |
IF (if_ebil >= 1) zero_v = 0. |
| 486 |
IF (nqmx < 2) CALL abort_gcm('physiq', & |
| 487 |
'eaux vapeur et liquide sont indispensables') |
| 488 |
|
| 489 |
test_firstcal: IF (firstcal) THEN |
| 490 |
! initialiser |
| 491 |
u10m = 0. |
| 492 |
v10m = 0. |
| 493 |
t2m = 0. |
| 494 |
q2m = 0. |
| 495 |
ffonte = 0. |
| 496 |
fqcalving = 0. |
| 497 |
piz_ae = 0. |
| 498 |
tau_ae = 0. |
| 499 |
cg_ae = 0. |
| 500 |
rain_con = 0. |
| 501 |
snow_con = 0. |
| 502 |
topswai = 0. |
| 503 |
topswad = 0. |
| 504 |
solswai = 0. |
| 505 |
solswad = 0. |
| 506 |
|
| 507 |
d_u_con = 0. |
| 508 |
d_v_con = 0. |
| 509 |
rnebcon0 = 0. |
| 510 |
clwcon0 = 0. |
| 511 |
rnebcon = 0. |
| 512 |
clwcon = 0. |
| 513 |
|
| 514 |
pblh =0. ! Hauteur de couche limite |
| 515 |
plcl =0. ! Niveau de condensation de la CLA |
| 516 |
capCL =0. ! CAPE de couche limite |
| 517 |
oliqCL =0. ! eau_liqu integree de couche limite |
| 518 |
cteiCL =0. ! cloud top instab. crit. couche limite |
| 519 |
pblt =0. ! T a la Hauteur de couche limite |
| 520 |
therm =0. |
| 521 |
trmb1 =0. ! deep_cape |
| 522 |
trmb2 =0. ! inhibition |
| 523 |
trmb3 =0. ! Point Omega |
| 524 |
|
| 525 |
IF (if_ebil >= 1) d_h_vcol_phy = 0. |
| 526 |
|
| 527 |
iflag_thermals = 0 |
| 528 |
nsplit_thermals = 1 |
| 529 |
print *, "Enter namelist 'physiq_nml'." |
| 530 |
read(unit=*, nml=physiq_nml) |
| 531 |
write(unit_nml, nml=physiq_nml) |
| 532 |
|
| 533 |
call conf_phys |
| 534 |
|
| 535 |
! Initialiser les compteurs: |
| 536 |
|
| 537 |
frugs = 0. |
| 538 |
CALL phyetat0(pctsrf, ftsol, ftsoil, fqsurf, qsol, & |
| 539 |
fsnow, falbe, fevap, rain_fall, snow_fall, solsw, sollw, dlw, & |
| 540 |
radsol, frugs, agesno, zmea, zstd, zsig, zgam, zthe, zpic, zval, & |
| 541 |
t_ancien, q_ancien, ancien_ok, rnebcon, ratqs, clwcon, & |
| 542 |
run_off_lic_0, sig1, w01, ncid_startphy, itau_phy) |
| 543 |
|
| 544 |
! ATTENTION : il faudra a terme relire q2 dans l'etat initial |
| 545 |
q2 = 1e-8 |
| 546 |
|
| 547 |
lmt_pas = day_step / iphysiq |
| 548 |
print *, 'Number of time steps of "physics" per day: ', lmt_pas |
| 549 |
|
| 550 |
radpas = lmt_pas / nbapp_rad |
| 551 |
|
| 552 |
! On remet le calendrier a zero |
| 553 |
IF (raz_date) itau_phy = 0 |
| 554 |
|
| 555 |
CALL printflag(radpas, ok_journe, ok_instan, ok_region) |
| 556 |
|
| 557 |
! Initialisation pour le sch\'ema de convection d'Emanuel : |
| 558 |
IF (conv_emanuel) THEN |
| 559 |
ibas_con = 1 |
| 560 |
itop_con = 1 |
| 561 |
ENDIF |
| 562 |
|
| 563 |
IF (ok_orodr) THEN |
| 564 |
rugoro = MAX(1e-5, zstd * zsig / 2) |
| 565 |
CALL SUGWD(paprs, play) |
| 566 |
else |
| 567 |
rugoro = 0. |
| 568 |
ENDIF |
| 569 |
|
| 570 |
ecrit_ins = NINT(ecrit_ins/dtphys) |
| 571 |
ecrit_hf = NINT(ecrit_hf/dtphys) |
| 572 |
ecrit_mth = NINT(ecrit_mth/dtphys) |
| 573 |
ecrit_tra = NINT(86400.*ecrit_tra/dtphys) |
| 574 |
ecrit_reg = NINT(ecrit_reg/dtphys) |
| 575 |
|
| 576 |
! Initialisation des sorties |
| 577 |
|
| 578 |
call ini_histins(dtphys, ok_instan, nid_ins, itau_phy) |
| 579 |
CALL ymds2ju(annee_ref, 1, day_ref, 0., date0) |
| 580 |
! Positionner date0 pour initialisation de ORCHIDEE |
| 581 |
print *, 'physiq date0: ', date0 |
| 582 |
CALL phyredem0(lmt_pas, itau_phy) |
| 583 |
ENDIF test_firstcal |
| 584 |
|
| 585 |
! We will modify variables *_seri and we will not touch variables |
| 586 |
! u, v, t, qx: |
| 587 |
t_seri = t |
| 588 |
u_seri = u |
| 589 |
v_seri = v |
| 590 |
q_seri = qx(:, :, ivap) |
| 591 |
ql_seri = qx(:, :, iliq) |
| 592 |
tr_seri = qx(:, :, 3:nqmx) |
| 593 |
|
| 594 |
ztsol = sum(ftsol * pctsrf, dim = 2) |
| 595 |
|
| 596 |
IF (if_ebil >= 1) THEN |
| 597 |
tit = 'after dynamics' |
| 598 |
CALL diagetpq(airephy, tit, ip_ebil, 1, 1, dtphys, t_seri, q_seri, & |
| 599 |
ql_seri, u_seri, v_seri, paprs, d_h_vcol, d_qt, d_ec) |
| 600 |
! Comme les tendances de la physique sont ajout\'es dans la |
| 601 |
! dynamique, la variation d'enthalpie par la dynamique devrait |
| 602 |
! \^etre \'egale \`a la variation de la physique au pas de temps |
| 603 |
! pr\'ec\'edent. Donc la somme de ces 2 variations devrait \^etre |
| 604 |
! nulle. |
| 605 |
call diagphy(airephy, tit, ip_ebil, zero_v, zero_v, zero_v, zero_v, & |
| 606 |
zero_v, zero_v, zero_v, zero_v, ztsol, d_h_vcol + d_h_vcol_phy, & |
| 607 |
d_qt, 0.) |
| 608 |
END IF |
| 609 |
|
| 610 |
! Diagnostic de la tendance dynamique : |
| 611 |
IF (ancien_ok) THEN |
| 612 |
DO k = 1, llm |
| 613 |
DO i = 1, klon |
| 614 |
d_t_dyn(i, k) = (t_seri(i, k) - t_ancien(i, k)) / dtphys |
| 615 |
d_q_dyn(i, k) = (q_seri(i, k) - q_ancien(i, k)) / dtphys |
| 616 |
ENDDO |
| 617 |
ENDDO |
| 618 |
ELSE |
| 619 |
DO k = 1, llm |
| 620 |
DO i = 1, klon |
| 621 |
d_t_dyn(i, k) = 0. |
| 622 |
d_q_dyn(i, k) = 0. |
| 623 |
ENDDO |
| 624 |
ENDDO |
| 625 |
ancien_ok = .TRUE. |
| 626 |
ENDIF |
| 627 |
|
| 628 |
! Ajouter le geopotentiel du sol: |
| 629 |
DO k = 1, llm |
| 630 |
DO i = 1, klon |
| 631 |
zphi(i, k) = pphi(i, k) + pphis(i) |
| 632 |
ENDDO |
| 633 |
ENDDO |
| 634 |
|
| 635 |
! Check temperatures: |
| 636 |
CALL hgardfou(t_seri, ftsol) |
| 637 |
|
| 638 |
! Incrémenter le compteur de la physique |
| 639 |
itap = itap + 1 |
| 640 |
julien = MOD(dayvrai, 360) |
| 641 |
if (julien == 0) julien = 360 |
| 642 |
|
| 643 |
forall (k = 1: llm) zmasse(:, k) = (paprs(:, k) - paprs(:, k + 1)) / rg |
| 644 |
|
| 645 |
! Prescrire l'ozone : |
| 646 |
wo = ozonecm(REAL(julien), paprs) |
| 647 |
|
| 648 |
! \'Evaporation de l'eau liquide nuageuse : |
| 649 |
DO k = 1, llm |
| 650 |
DO i = 1, klon |
| 651 |
zb = MAX(0., ql_seri(i, k)) |
| 652 |
t_seri(i, k) = t_seri(i, k) & |
| 653 |
- zb * RLVTT / RCPD / (1. + RVTMP2 * q_seri(i, k)) |
| 654 |
q_seri(i, k) = q_seri(i, k) + zb |
| 655 |
ENDDO |
| 656 |
ENDDO |
| 657 |
ql_seri = 0. |
| 658 |
|
| 659 |
IF (if_ebil >= 2) THEN |
| 660 |
tit = 'after reevap' |
| 661 |
CALL diagetpq(airephy, tit, ip_ebil, 2, 1, dtphys, t_seri, q_seri, & |
| 662 |
ql_seri, u_seri, v_seri, paprs, d_h_vcol, d_qt, d_ec) |
| 663 |
call diagphy(airephy, tit, ip_ebil, zero_v, zero_v, zero_v, zero_v, & |
| 664 |
zero_v, zero_v, zero_v, zero_v, ztsol, d_h_vcol, d_qt, d_ec) |
| 665 |
END IF |
| 666 |
|
| 667 |
frugs = MAX(frugs, 0.000015) |
| 668 |
zxrugs = sum(frugs * pctsrf, dim = 2) |
| 669 |
|
| 670 |
! Calculs nécessaires au calcul de l'albedo dans l'interface avec |
| 671 |
! la surface. |
| 672 |
|
| 673 |
CALL orbite(REAL(julien), longi, dist) |
| 674 |
IF (cycle_diurne) THEN |
| 675 |
CALL zenang(longi, time, dtphys * radpas, mu0, fract) |
| 676 |
ELSE |
| 677 |
mu0 = - 999.999 |
| 678 |
ENDIF |
| 679 |
|
| 680 |
! Calcul de l'abedo moyen par maille |
| 681 |
albsol = sum(falbe * pctsrf, dim = 2) |
| 682 |
|
| 683 |
! R\'epartition sous maille des flux longwave et shortwave |
| 684 |
! R\'epartition du longwave par sous-surface lin\'earis\'ee |
| 685 |
|
| 686 |
forall (nsrf = 1: nbsrf) |
| 687 |
fsollw(:, nsrf) = sollw + 4. * RSIGMA * ztsol**3 & |
| 688 |
* (ztsol - ftsol(:, nsrf)) |
| 689 |
fsolsw(:, nsrf) = solsw * (1. - falbe(:, nsrf)) / (1. - albsol) |
| 690 |
END forall |
| 691 |
|
| 692 |
fder = dlw |
| 693 |
|
| 694 |
! Couche limite: |
| 695 |
|
| 696 |
CALL clmain(dtphys, itap, pctsrf, pctsrf_new, t_seri, q_seri, u_seri, & |
| 697 |
v_seri, julien, mu0, ftsol, cdmmax, cdhmax, ksta, ksta_ter, & |
| 698 |
ok_kzmin, ftsoil, qsol, paprs, play, fsnow, fqsurf, fevap, falbe, & |
| 699 |
fluxlat, rain_fall, snow_fall, fsolsw, fsollw, fder, rlat, frugs, & |
| 700 |
firstcal, agesno, rugoro, d_t_vdf, d_q_vdf, d_u_vdf, d_v_vdf, d_ts, & |
| 701 |
fluxt, fluxq, fluxu, fluxv, cdragh, cdragm, q2, dsens, devap, & |
| 702 |
ycoefh, yu1, yv1, t2m, q2m, u10m, v10m, pblh, capCL, oliqCL, cteiCL, & |
| 703 |
pblT, therm, trmb1, trmb2, trmb3, plcl, fqcalving, ffonte, & |
| 704 |
run_off_lic_0) |
| 705 |
|
| 706 |
! Incr\'ementation des flux |
| 707 |
|
| 708 |
zxfluxt = 0. |
| 709 |
zxfluxq = 0. |
| 710 |
zxfluxu = 0. |
| 711 |
zxfluxv = 0. |
| 712 |
DO nsrf = 1, nbsrf |
| 713 |
DO k = 1, llm |
| 714 |
DO i = 1, klon |
| 715 |
zxfluxt(i, k) = zxfluxt(i, k) + fluxt(i, k, nsrf) * pctsrf(i, nsrf) |
| 716 |
zxfluxq(i, k) = zxfluxq(i, k) + fluxq(i, k, nsrf) * pctsrf(i, nsrf) |
| 717 |
zxfluxu(i, k) = zxfluxu(i, k) + fluxu(i, k, nsrf) * pctsrf(i, nsrf) |
| 718 |
zxfluxv(i, k) = zxfluxv(i, k) + fluxv(i, k, nsrf) * pctsrf(i, nsrf) |
| 719 |
END DO |
| 720 |
END DO |
| 721 |
END DO |
| 722 |
DO i = 1, klon |
| 723 |
sens(i) = - zxfluxt(i, 1) ! flux de chaleur sensible au sol |
| 724 |
evap(i) = - zxfluxq(i, 1) ! flux d'\'evaporation au sol |
| 725 |
fder(i) = dlw(i) + dsens(i) + devap(i) |
| 726 |
ENDDO |
| 727 |
|
| 728 |
DO k = 1, llm |
| 729 |
DO i = 1, klon |
| 730 |
t_seri(i, k) = t_seri(i, k) + d_t_vdf(i, k) |
| 731 |
q_seri(i, k) = q_seri(i, k) + d_q_vdf(i, k) |
| 732 |
u_seri(i, k) = u_seri(i, k) + d_u_vdf(i, k) |
| 733 |
v_seri(i, k) = v_seri(i, k) + d_v_vdf(i, k) |
| 734 |
ENDDO |
| 735 |
ENDDO |
| 736 |
|
| 737 |
IF (if_ebil >= 2) THEN |
| 738 |
tit = 'after clmain' |
| 739 |
CALL diagetpq(airephy, tit, ip_ebil, 2, 2, dtphys, t_seri, q_seri, & |
| 740 |
ql_seri, u_seri, v_seri, paprs, d_h_vcol, d_qt, d_ec) |
| 741 |
call diagphy(airephy, tit, ip_ebil, zero_v, zero_v, zero_v, zero_v, & |
| 742 |
sens, evap, zero_v, zero_v, ztsol, d_h_vcol, d_qt, d_ec) |
| 743 |
END IF |
| 744 |
|
| 745 |
! Update surface temperature: |
| 746 |
|
| 747 |
DO i = 1, klon |
| 748 |
zxtsol(i) = 0. |
| 749 |
zxfluxlat(i) = 0. |
| 750 |
|
| 751 |
zt2m(i) = 0. |
| 752 |
zq2m(i) = 0. |
| 753 |
zu10m(i) = 0. |
| 754 |
zv10m(i) = 0. |
| 755 |
zxffonte(i) = 0. |
| 756 |
zxfqcalving(i) = 0. |
| 757 |
|
| 758 |
s_pblh(i) = 0. |
| 759 |
s_lcl(i) = 0. |
| 760 |
s_capCL(i) = 0. |
| 761 |
s_oliqCL(i) = 0. |
| 762 |
s_cteiCL(i) = 0. |
| 763 |
s_pblT(i) = 0. |
| 764 |
s_therm(i) = 0. |
| 765 |
s_trmb1(i) = 0. |
| 766 |
s_trmb2(i) = 0. |
| 767 |
s_trmb3(i) = 0. |
| 768 |
|
| 769 |
IF (abs(pctsrf(i, is_ter) + pctsrf(i, is_lic) + pctsrf(i, is_oce) & |
| 770 |
+ pctsrf(i, is_sic) - 1.) > EPSFRA) print *, & |
| 771 |
'physiq : probl\`eme sous surface au point ', i, & |
| 772 |
pctsrf(i, 1 : nbsrf) |
| 773 |
ENDDO |
| 774 |
DO nsrf = 1, nbsrf |
| 775 |
DO i = 1, klon |
| 776 |
ftsol(i, nsrf) = ftsol(i, nsrf) + d_ts(i, nsrf) |
| 777 |
zxtsol(i) = zxtsol(i) + ftsol(i, nsrf)*pctsrf(i, nsrf) |
| 778 |
zxfluxlat(i) = zxfluxlat(i) + fluxlat(i, nsrf)*pctsrf(i, nsrf) |
| 779 |
|
| 780 |
zt2m(i) = zt2m(i) + t2m(i, nsrf)*pctsrf(i, nsrf) |
| 781 |
zq2m(i) = zq2m(i) + q2m(i, nsrf)*pctsrf(i, nsrf) |
| 782 |
zu10m(i) = zu10m(i) + u10m(i, nsrf)*pctsrf(i, nsrf) |
| 783 |
zv10m(i) = zv10m(i) + v10m(i, nsrf)*pctsrf(i, nsrf) |
| 784 |
zxffonte(i) = zxffonte(i) + ffonte(i, nsrf)*pctsrf(i, nsrf) |
| 785 |
zxfqcalving(i) = zxfqcalving(i) + & |
| 786 |
fqcalving(i, nsrf)*pctsrf(i, nsrf) |
| 787 |
s_pblh(i) = s_pblh(i) + pblh(i, nsrf)*pctsrf(i, nsrf) |
| 788 |
s_lcl(i) = s_lcl(i) + plcl(i, nsrf)*pctsrf(i, nsrf) |
| 789 |
s_capCL(i) = s_capCL(i) + capCL(i, nsrf) *pctsrf(i, nsrf) |
| 790 |
s_oliqCL(i) = s_oliqCL(i) + oliqCL(i, nsrf) *pctsrf(i, nsrf) |
| 791 |
s_cteiCL(i) = s_cteiCL(i) + cteiCL(i, nsrf) *pctsrf(i, nsrf) |
| 792 |
s_pblT(i) = s_pblT(i) + pblT(i, nsrf) *pctsrf(i, nsrf) |
| 793 |
s_therm(i) = s_therm(i) + therm(i, nsrf) *pctsrf(i, nsrf) |
| 794 |
s_trmb1(i) = s_trmb1(i) + trmb1(i, nsrf) *pctsrf(i, nsrf) |
| 795 |
s_trmb2(i) = s_trmb2(i) + trmb2(i, nsrf) *pctsrf(i, nsrf) |
| 796 |
s_trmb3(i) = s_trmb3(i) + trmb3(i, nsrf) *pctsrf(i, nsrf) |
| 797 |
ENDDO |
| 798 |
ENDDO |
| 799 |
|
| 800 |
! Si une sous-fraction n'existe pas, elle prend la température moyenne : |
| 801 |
DO nsrf = 1, nbsrf |
| 802 |
DO i = 1, klon |
| 803 |
IF (pctsrf(i, nsrf) < epsfra) ftsol(i, nsrf) = zxtsol(i) |
| 804 |
|
| 805 |
IF (pctsrf(i, nsrf) < epsfra) t2m(i, nsrf) = zt2m(i) |
| 806 |
IF (pctsrf(i, nsrf) < epsfra) q2m(i, nsrf) = zq2m(i) |
| 807 |
IF (pctsrf(i, nsrf) < epsfra) u10m(i, nsrf) = zu10m(i) |
| 808 |
IF (pctsrf(i, nsrf) < epsfra) v10m(i, nsrf) = zv10m(i) |
| 809 |
IF (pctsrf(i, nsrf) < epsfra) ffonte(i, nsrf) = zxffonte(i) |
| 810 |
IF (pctsrf(i, nsrf) < epsfra) & |
| 811 |
fqcalving(i, nsrf) = zxfqcalving(i) |
| 812 |
IF (pctsrf(i, nsrf) < epsfra) pblh(i, nsrf) = s_pblh(i) |
| 813 |
IF (pctsrf(i, nsrf) < epsfra) plcl(i, nsrf) = s_lcl(i) |
| 814 |
IF (pctsrf(i, nsrf) < epsfra) capCL(i, nsrf) = s_capCL(i) |
| 815 |
IF (pctsrf(i, nsrf) < epsfra) oliqCL(i, nsrf) = s_oliqCL(i) |
| 816 |
IF (pctsrf(i, nsrf) < epsfra) cteiCL(i, nsrf) = s_cteiCL(i) |
| 817 |
IF (pctsrf(i, nsrf) < epsfra) pblT(i, nsrf) = s_pblT(i) |
| 818 |
IF (pctsrf(i, nsrf) < epsfra) therm(i, nsrf) = s_therm(i) |
| 819 |
IF (pctsrf(i, nsrf) < epsfra) trmb1(i, nsrf) = s_trmb1(i) |
| 820 |
IF (pctsrf(i, nsrf) < epsfra) trmb2(i, nsrf) = s_trmb2(i) |
| 821 |
IF (pctsrf(i, nsrf) < epsfra) trmb3(i, nsrf) = s_trmb3(i) |
| 822 |
ENDDO |
| 823 |
ENDDO |
| 824 |
|
| 825 |
! Calculer la dérive du flux infrarouge |
| 826 |
|
| 827 |
DO i = 1, klon |
| 828 |
dlw(i) = - 4. * RSIGMA * zxtsol(i)**3 |
| 829 |
ENDDO |
| 830 |
|
| 831 |
IF (check) print *, "avantcon = ", qcheck(paprs, q_seri, ql_seri) |
| 832 |
|
| 833 |
! Appeler la convection |
| 834 |
|
| 835 |
if (conv_emanuel) then |
| 836 |
da = 0. |
| 837 |
mp = 0. |
| 838 |
phi = 0. |
| 839 |
CALL concvl(dtphys, paprs, play, t_seri, q_seri, u_seri, v_seri, sig1, & |
| 840 |
w01, d_t_con, d_q_con, d_u_con, d_v_con, rain_con, ibas_con, & |
| 841 |
itop_con, upwd, dnwd, dnwd0, Ma, cape, iflagctrl, qcondc, pmflxr, & |
| 842 |
da, phi, mp) |
| 843 |
snow_con = 0. |
| 844 |
clwcon0 = qcondc |
| 845 |
mfu = upwd + dnwd |
| 846 |
|
| 847 |
IF (thermcep) THEN |
| 848 |
zqsat = MIN(0.5, r2es * FOEEW(t_seri, rtt >= t_seri) / play) |
| 849 |
zqsat = zqsat / (1. - retv * zqsat) |
| 850 |
ELSE |
| 851 |
zqsat = merge(qsats(t_seri), qsatl(t_seri), t_seri < t_coup) / play |
| 852 |
ENDIF |
| 853 |
|
| 854 |
! Properties of convective clouds |
| 855 |
clwcon0 = fact_cldcon * clwcon0 |
| 856 |
call clouds_gno(klon, llm, q_seri, zqsat, clwcon0, ptconv, ratqsc, & |
| 857 |
rnebcon0) |
| 858 |
|
| 859 |
forall (i = 1:klon) ema_pct(i) = paprs(i, itop_con(i) + 1) |
| 860 |
mfd = 0. |
| 861 |
pen_u = 0. |
| 862 |
pen_d = 0. |
| 863 |
pde_d = 0. |
| 864 |
pde_u = 0. |
| 865 |
else |
| 866 |
conv_q = d_q_dyn + d_q_vdf / dtphys |
| 867 |
conv_t = d_t_dyn + d_t_vdf / dtphys |
| 868 |
z_avant = sum((q_seri + ql_seri) * zmasse, dim=2) |
| 869 |
CALL conflx(dtphys, paprs, play, t_seri(:, llm:1:- 1), & |
| 870 |
q_seri(:, llm:1:- 1), conv_t, conv_q, zxfluxq(:, 1), omega, & |
| 871 |
d_t_con, d_q_con, rain_con, snow_con, mfu(:, llm:1:- 1), & |
| 872 |
mfd(:, llm:1:- 1), pen_u, pde_u, pen_d, pde_d, kcbot, kctop, & |
| 873 |
kdtop, pmflxr, pmflxs) |
| 874 |
WHERE (rain_con < 0.) rain_con = 0. |
| 875 |
WHERE (snow_con < 0.) snow_con = 0. |
| 876 |
ibas_con = llm + 1 - kcbot |
| 877 |
itop_con = llm + 1 - kctop |
| 878 |
END if |
| 879 |
|
| 880 |
DO k = 1, llm |
| 881 |
DO i = 1, klon |
| 882 |
t_seri(i, k) = t_seri(i, k) + d_t_con(i, k) |
| 883 |
q_seri(i, k) = q_seri(i, k) + d_q_con(i, k) |
| 884 |
u_seri(i, k) = u_seri(i, k) + d_u_con(i, k) |
| 885 |
v_seri(i, k) = v_seri(i, k) + d_v_con(i, k) |
| 886 |
ENDDO |
| 887 |
ENDDO |
| 888 |
|
| 889 |
IF (if_ebil >= 2) THEN |
| 890 |
tit = 'after convect' |
| 891 |
CALL diagetpq(airephy, tit, ip_ebil, 2, 2, dtphys, t_seri, q_seri, & |
| 892 |
ql_seri, u_seri, v_seri, paprs, d_h_vcol, d_qt, d_ec) |
| 893 |
call diagphy(airephy, tit, ip_ebil, zero_v, zero_v, zero_v, zero_v, & |
| 894 |
zero_v, zero_v, rain_con, snow_con, ztsol, d_h_vcol, d_qt, d_ec) |
| 895 |
END IF |
| 896 |
|
| 897 |
IF (check) THEN |
| 898 |
za = qcheck(paprs, q_seri, ql_seri) |
| 899 |
print *, "aprescon = ", za |
| 900 |
zx_t = 0. |
| 901 |
za = 0. |
| 902 |
DO i = 1, klon |
| 903 |
za = za + airephy(i)/REAL(klon) |
| 904 |
zx_t = zx_t + (rain_con(i)+ & |
| 905 |
snow_con(i))*airephy(i)/REAL(klon) |
| 906 |
ENDDO |
| 907 |
zx_t = zx_t/za*dtphys |
| 908 |
print *, "Precip = ", zx_t |
| 909 |
ENDIF |
| 910 |
|
| 911 |
IF (.not. conv_emanuel) THEN |
| 912 |
z_apres = sum((q_seri + ql_seri) * zmasse, dim=2) |
| 913 |
z_factor = (z_avant - (rain_con + snow_con) * dtphys) / z_apres |
| 914 |
DO k = 1, llm |
| 915 |
DO i = 1, klon |
| 916 |
IF (z_factor(i) > 1. + 1E-8 .OR. z_factor(i) < 1. - 1E-8) THEN |
| 917 |
q_seri(i, k) = q_seri(i, k) * z_factor(i) |
| 918 |
ENDIF |
| 919 |
ENDDO |
| 920 |
ENDDO |
| 921 |
ENDIF |
| 922 |
|
| 923 |
! Convection s\`eche (thermiques ou ajustement) |
| 924 |
|
| 925 |
d_t_ajs = 0. |
| 926 |
d_u_ajs = 0. |
| 927 |
d_v_ajs = 0. |
| 928 |
d_q_ajs = 0. |
| 929 |
fm_therm = 0. |
| 930 |
entr_therm = 0. |
| 931 |
|
| 932 |
if (iflag_thermals == 0) then |
| 933 |
! Ajustement sec |
| 934 |
CALL ajsec(paprs, play, t_seri, q_seri, d_t_ajs, d_q_ajs) |
| 935 |
t_seri = t_seri + d_t_ajs |
| 936 |
q_seri = q_seri + d_q_ajs |
| 937 |
else |
| 938 |
! Thermiques |
| 939 |
call calltherm(dtphys, play, paprs, pphi, u_seri, v_seri, t_seri, & |
| 940 |
q_seri, d_u_ajs, d_v_ajs, d_t_ajs, d_q_ajs, fm_therm, entr_therm) |
| 941 |
endif |
| 942 |
|
| 943 |
IF (if_ebil >= 2) THEN |
| 944 |
tit = 'after dry_adjust' |
| 945 |
CALL diagetpq(airephy, tit, ip_ebil, 2, 2, dtphys, t_seri, q_seri, & |
| 946 |
ql_seri, u_seri, v_seri, paprs, d_h_vcol, d_qt, d_ec) |
| 947 |
END IF |
| 948 |
|
| 949 |
! Caclul des ratqs |
| 950 |
|
| 951 |
! ratqs convectifs \`a l'ancienne en fonction de (q(z = 0) - q) / q |
| 952 |
! on \'ecrase le tableau ratqsc calcul\'e par clouds_gno |
| 953 |
if (iflag_cldcon == 1) then |
| 954 |
do k = 1, llm |
| 955 |
do i = 1, klon |
| 956 |
if(ptconv(i, k)) then |
| 957 |
ratqsc(i, k) = ratqsbas + fact_cldcon & |
| 958 |
* (q_seri(i, 1) - q_seri(i, k)) / q_seri(i, k) |
| 959 |
else |
| 960 |
ratqsc(i, k) = 0. |
| 961 |
endif |
| 962 |
enddo |
| 963 |
enddo |
| 964 |
endif |
| 965 |
|
| 966 |
! ratqs stables |
| 967 |
do k = 1, llm |
| 968 |
do i = 1, klon |
| 969 |
ratqss(i, k) = ratqsbas + (ratqshaut - ratqsbas) & |
| 970 |
* min((paprs(i, 1) - play(i, k)) / (paprs(i, 1) - 3e4), 1.) |
| 971 |
enddo |
| 972 |
enddo |
| 973 |
|
| 974 |
! ratqs final |
| 975 |
if (iflag_cldcon == 1 .or. iflag_cldcon == 2) then |
| 976 |
! les ratqs sont une conbinaison de ratqss et ratqsc |
| 977 |
! ratqs final |
| 978 |
! 1e4 (en gros 3 heures), en dur pour le moment, est le temps de |
| 979 |
! relaxation des ratqs |
| 980 |
ratqs = max(ratqs * exp(- dtphys * facttemps), ratqss) |
| 981 |
ratqs = max(ratqs, ratqsc) |
| 982 |
else |
| 983 |
! on ne prend que le ratqs stable pour fisrtilp |
| 984 |
ratqs = ratqss |
| 985 |
endif |
| 986 |
|
| 987 |
CALL fisrtilp(dtphys, paprs, play, t_seri, q_seri, ptconv, ratqs, & |
| 988 |
d_t_lsc, d_q_lsc, d_ql_lsc, rneb, cldliq, rain_lsc, snow_lsc, & |
| 989 |
pfrac_impa, pfrac_nucl, pfrac_1nucl, frac_impa, frac_nucl, prfl, & |
| 990 |
psfl, rhcl) |
| 991 |
|
| 992 |
WHERE (rain_lsc < 0) rain_lsc = 0. |
| 993 |
WHERE (snow_lsc < 0) snow_lsc = 0. |
| 994 |
DO k = 1, llm |
| 995 |
DO i = 1, klon |
| 996 |
t_seri(i, k) = t_seri(i, k) + d_t_lsc(i, k) |
| 997 |
q_seri(i, k) = q_seri(i, k) + d_q_lsc(i, k) |
| 998 |
ql_seri(i, k) = ql_seri(i, k) + d_ql_lsc(i, k) |
| 999 |
cldfra(i, k) = rneb(i, k) |
| 1000 |
IF (.NOT.new_oliq) cldliq(i, k) = ql_seri(i, k) |
| 1001 |
ENDDO |
| 1002 |
ENDDO |
| 1003 |
IF (check) THEN |
| 1004 |
za = qcheck(paprs, q_seri, ql_seri) |
| 1005 |
print *, "apresilp = ", za |
| 1006 |
zx_t = 0. |
| 1007 |
za = 0. |
| 1008 |
DO i = 1, klon |
| 1009 |
za = za + airephy(i)/REAL(klon) |
| 1010 |
zx_t = zx_t + (rain_lsc(i) & |
| 1011 |
+ snow_lsc(i))*airephy(i)/REAL(klon) |
| 1012 |
ENDDO |
| 1013 |
zx_t = zx_t/za*dtphys |
| 1014 |
print *, "Precip = ", zx_t |
| 1015 |
ENDIF |
| 1016 |
|
| 1017 |
IF (if_ebil >= 2) THEN |
| 1018 |
tit = 'after fisrt' |
| 1019 |
CALL diagetpq(airephy, tit, ip_ebil, 2, 2, dtphys, t_seri, q_seri, & |
| 1020 |
ql_seri, u_seri, v_seri, paprs, d_h_vcol, d_qt, d_ec) |
| 1021 |
call diagphy(airephy, tit, ip_ebil, zero_v, zero_v, zero_v, zero_v, & |
| 1022 |
zero_v, zero_v, rain_lsc, snow_lsc, ztsol, d_h_vcol, d_qt, d_ec) |
| 1023 |
END IF |
| 1024 |
|
| 1025 |
! PRESCRIPTION DES NUAGES POUR LE RAYONNEMENT |
| 1026 |
|
| 1027 |
! 1. NUAGES CONVECTIFS |
| 1028 |
|
| 1029 |
IF (iflag_cldcon <= - 1) THEN |
| 1030 |
! seulement pour Tiedtke |
| 1031 |
snow_tiedtke = 0. |
| 1032 |
if (iflag_cldcon == - 1) then |
| 1033 |
rain_tiedtke = rain_con |
| 1034 |
else |
| 1035 |
rain_tiedtke = 0. |
| 1036 |
do k = 1, llm |
| 1037 |
do i = 1, klon |
| 1038 |
if (d_q_con(i, k) < 0.) then |
| 1039 |
rain_tiedtke(i) = rain_tiedtke(i) - d_q_con(i, k)/dtphys & |
| 1040 |
*zmasse(i, k) |
| 1041 |
endif |
| 1042 |
enddo |
| 1043 |
enddo |
| 1044 |
endif |
| 1045 |
|
| 1046 |
! Nuages diagnostiques pour Tiedtke |
| 1047 |
CALL diagcld1(paprs, play, rain_tiedtke, snow_tiedtke, ibas_con, & |
| 1048 |
itop_con, diafra, dialiq) |
| 1049 |
DO k = 1, llm |
| 1050 |
DO i = 1, klon |
| 1051 |
IF (diafra(i, k) > cldfra(i, k)) THEN |
| 1052 |
cldliq(i, k) = dialiq(i, k) |
| 1053 |
cldfra(i, k) = diafra(i, k) |
| 1054 |
ENDIF |
| 1055 |
ENDDO |
| 1056 |
ENDDO |
| 1057 |
ELSE IF (iflag_cldcon == 3) THEN |
| 1058 |
! On prend pour les nuages convectifs le maximum du calcul de |
| 1059 |
! la convection et du calcul du pas de temps pr\'ec\'edent diminu\'e |
| 1060 |
! d'un facteur facttemps. |
| 1061 |
facteur = dtphys * facttemps |
| 1062 |
do k = 1, llm |
| 1063 |
do i = 1, klon |
| 1064 |
rnebcon(i, k) = rnebcon(i, k) * facteur |
| 1065 |
if (rnebcon0(i, k) * clwcon0(i, k) & |
| 1066 |
> rnebcon(i, k) * clwcon(i, k)) then |
| 1067 |
rnebcon(i, k) = rnebcon0(i, k) |
| 1068 |
clwcon(i, k) = clwcon0(i, k) |
| 1069 |
endif |
| 1070 |
enddo |
| 1071 |
enddo |
| 1072 |
|
| 1073 |
! On prend la somme des fractions nuageuses et des contenus en eau |
| 1074 |
cldfra = min(max(cldfra, rnebcon), 1.) |
| 1075 |
cldliq = cldliq + rnebcon*clwcon |
| 1076 |
ENDIF |
| 1077 |
|
| 1078 |
! 2. Nuages stratiformes |
| 1079 |
|
| 1080 |
IF (ok_stratus) THEN |
| 1081 |
CALL diagcld2(paprs, play, t_seri, q_seri, diafra, dialiq) |
| 1082 |
DO k = 1, llm |
| 1083 |
DO i = 1, klon |
| 1084 |
IF (diafra(i, k) > cldfra(i, k)) THEN |
| 1085 |
cldliq(i, k) = dialiq(i, k) |
| 1086 |
cldfra(i, k) = diafra(i, k) |
| 1087 |
ENDIF |
| 1088 |
ENDDO |
| 1089 |
ENDDO |
| 1090 |
ENDIF |
| 1091 |
|
| 1092 |
! Precipitation totale |
| 1093 |
DO i = 1, klon |
| 1094 |
rain_fall(i) = rain_con(i) + rain_lsc(i) |
| 1095 |
snow_fall(i) = snow_con(i) + snow_lsc(i) |
| 1096 |
ENDDO |
| 1097 |
|
| 1098 |
IF (if_ebil >= 2) CALL diagetpq(airephy, "after diagcld", ip_ebil, 2, 2, & |
| 1099 |
dtphys, t_seri, q_seri, ql_seri, u_seri, v_seri, paprs, d_h_vcol, & |
| 1100 |
d_qt, d_ec) |
| 1101 |
|
| 1102 |
! Humidit\'e relative pour diagnostic : |
| 1103 |
DO k = 1, llm |
| 1104 |
DO i = 1, klon |
| 1105 |
zx_t = t_seri(i, k) |
| 1106 |
IF (thermcep) THEN |
| 1107 |
zx_qs = r2es * FOEEW(zx_t, rtt >= zx_t)/play(i, k) |
| 1108 |
zx_qs = MIN(0.5, zx_qs) |
| 1109 |
zcor = 1./(1. - retv*zx_qs) |
| 1110 |
zx_qs = zx_qs*zcor |
| 1111 |
ELSE |
| 1112 |
IF (zx_t < t_coup) THEN |
| 1113 |
zx_qs = qsats(zx_t)/play(i, k) |
| 1114 |
ELSE |
| 1115 |
zx_qs = qsatl(zx_t)/play(i, k) |
| 1116 |
ENDIF |
| 1117 |
ENDIF |
| 1118 |
zx_rh(i, k) = q_seri(i, k)/zx_qs |
| 1119 |
zqsat(i, k) = zx_qs |
| 1120 |
ENDDO |
| 1121 |
ENDDO |
| 1122 |
|
| 1123 |
! Introduce the aerosol direct and first indirect radiative forcings: |
| 1124 |
IF (ok_ade .OR. ok_aie) THEN |
| 1125 |
! Get sulfate aerosol distribution : |
| 1126 |
CALL readsulfate(dayvrai, time, firstcal, sulfate) |
| 1127 |
CALL readsulfate_preind(dayvrai, time, firstcal, sulfate_pi) |
| 1128 |
|
| 1129 |
CALL aeropt(play, paprs, t_seri, sulfate, rhcl, tau_ae, piz_ae, cg_ae, & |
| 1130 |
aerindex) |
| 1131 |
ELSE |
| 1132 |
tau_ae = 0. |
| 1133 |
piz_ae = 0. |
| 1134 |
cg_ae = 0. |
| 1135 |
ENDIF |
| 1136 |
|
| 1137 |
! Param\`etres optiques des nuages et quelques param\`etres pour |
| 1138 |
! diagnostics : |
| 1139 |
if (ok_newmicro) then |
| 1140 |
CALL newmicro(paprs, play, t_seri, cldliq, cldfra, cldtau, cldemi, & |
| 1141 |
cldh, cldl, cldm, cldt, cldq, flwp, fiwp, flwc, fiwc, ok_aie, & |
| 1142 |
sulfate, sulfate_pi, bl95_b0, bl95_b1, cldtaupi, re, fl) |
| 1143 |
else |
| 1144 |
CALL nuage(paprs, play, t_seri, cldliq, cldfra, cldtau, cldemi, cldh, & |
| 1145 |
cldl, cldm, cldt, cldq, ok_aie, sulfate, sulfate_pi, bl95_b0, & |
| 1146 |
bl95_b1, cldtaupi, re, fl) |
| 1147 |
endif |
| 1148 |
|
| 1149 |
IF (MOD(itap - 1, radpas) == 0) THEN |
| 1150 |
! Appeler le rayonnement mais calculer tout d'abord l'albedo du sol. |
| 1151 |
! Calcul de l'abedo moyen par maille |
| 1152 |
albsol = sum(falbe * pctsrf, dim = 2) |
| 1153 |
|
| 1154 |
! Rayonnement (compatible Arpege-IFS) : |
| 1155 |
CALL radlwsw(dist, mu0, fract, paprs, play, zxtsol, albsol, t_seri, & |
| 1156 |
q_seri, wo, cldfra, cldemi, cldtau, heat, heat0, cool, cool0, & |
| 1157 |
radsol, albpla, topsw, toplw, solsw, sollw, sollwdown, topsw0, & |
| 1158 |
toplw0, solsw0, sollw0, lwdn0, lwdn, lwup0, lwup, swdn0, swdn, & |
| 1159 |
swup0, swup, ok_ade, ok_aie, tau_ae, piz_ae, cg_ae, topswad, & |
| 1160 |
solswad, cldtaupi, topswai, solswai) |
| 1161 |
ENDIF |
| 1162 |
|
| 1163 |
! Ajouter la tendance des rayonnements (tous les pas) |
| 1164 |
|
| 1165 |
DO k = 1, llm |
| 1166 |
DO i = 1, klon |
| 1167 |
t_seri(i, k) = t_seri(i, k) + (heat(i, k) - cool(i, k)) * dtphys/86400. |
| 1168 |
ENDDO |
| 1169 |
ENDDO |
| 1170 |
|
| 1171 |
IF (if_ebil >= 2) THEN |
| 1172 |
tit = 'after rad' |
| 1173 |
CALL diagetpq(airephy, tit, ip_ebil, 2, 2, dtphys, t_seri, q_seri, & |
| 1174 |
ql_seri, u_seri, v_seri, paprs, d_h_vcol, d_qt, d_ec) |
| 1175 |
call diagphy(airephy, tit, ip_ebil, topsw, toplw, solsw, sollw, & |
| 1176 |
zero_v, zero_v, zero_v, zero_v, ztsol, d_h_vcol, d_qt, d_ec) |
| 1177 |
END IF |
| 1178 |
|
| 1179 |
! Calculer l'hydrologie de la surface |
| 1180 |
DO i = 1, klon |
| 1181 |
zxqsurf(i) = 0. |
| 1182 |
zxsnow(i) = 0. |
| 1183 |
ENDDO |
| 1184 |
DO nsrf = 1, nbsrf |
| 1185 |
DO i = 1, klon |
| 1186 |
zxqsurf(i) = zxqsurf(i) + fqsurf(i, nsrf)*pctsrf(i, nsrf) |
| 1187 |
zxsnow(i) = zxsnow(i) + fsnow(i, nsrf)*pctsrf(i, nsrf) |
| 1188 |
ENDDO |
| 1189 |
ENDDO |
| 1190 |
|
| 1191 |
! Calculer le bilan du sol et la d\'erive de temp\'erature (couplage) |
| 1192 |
|
| 1193 |
DO i = 1, klon |
| 1194 |
bils(i) = radsol(i) - sens(i) + zxfluxlat(i) |
| 1195 |
ENDDO |
| 1196 |
|
| 1197 |
! Param\'etrisation de l'orographie \`a l'\'echelle sous-maille : |
| 1198 |
|
| 1199 |
IF (ok_orodr) THEN |
| 1200 |
! S\'election des points pour lesquels le sch\'ema est actif : |
| 1201 |
igwd = 0 |
| 1202 |
DO i = 1, klon |
| 1203 |
itest(i) = 0 |
| 1204 |
IF (zpic(i) - zmea(i) > 100. .AND. zstd(i) > 10.) THEN |
| 1205 |
itest(i) = 1 |
| 1206 |
igwd = igwd + 1 |
| 1207 |
ENDIF |
| 1208 |
ENDDO |
| 1209 |
|
| 1210 |
CALL drag_noro(klon, llm, dtphys, paprs, play, zmea, zstd, zsig, zgam, & |
| 1211 |
zthe, zpic, zval, itest, t_seri, u_seri, v_seri, zulow, zvlow, & |
| 1212 |
zustrdr, zvstrdr, d_t_oro, d_u_oro, d_v_oro) |
| 1213 |
|
| 1214 |
! ajout des tendances |
| 1215 |
DO k = 1, llm |
| 1216 |
DO i = 1, klon |
| 1217 |
t_seri(i, k) = t_seri(i, k) + d_t_oro(i, k) |
| 1218 |
u_seri(i, k) = u_seri(i, k) + d_u_oro(i, k) |
| 1219 |
v_seri(i, k) = v_seri(i, k) + d_v_oro(i, k) |
| 1220 |
ENDDO |
| 1221 |
ENDDO |
| 1222 |
ENDIF |
| 1223 |
|
| 1224 |
IF (ok_orolf) THEN |
| 1225 |
! S\'election des points pour lesquels le sch\'ema est actif : |
| 1226 |
igwd = 0 |
| 1227 |
DO i = 1, klon |
| 1228 |
itest(i) = 0 |
| 1229 |
IF (zpic(i) - zmea(i) > 100.) THEN |
| 1230 |
itest(i) = 1 |
| 1231 |
igwd = igwd + 1 |
| 1232 |
ENDIF |
| 1233 |
ENDDO |
| 1234 |
|
| 1235 |
CALL lift_noro(klon, llm, dtphys, paprs, play, rlat, zmea, zstd, zpic, & |
| 1236 |
itest, t_seri, u_seri, v_seri, zulow, zvlow, zustrli, zvstrli, & |
| 1237 |
d_t_lif, d_u_lif, d_v_lif) |
| 1238 |
|
| 1239 |
! Ajout des tendances : |
| 1240 |
DO k = 1, llm |
| 1241 |
DO i = 1, klon |
| 1242 |
t_seri(i, k) = t_seri(i, k) + d_t_lif(i, k) |
| 1243 |
u_seri(i, k) = u_seri(i, k) + d_u_lif(i, k) |
| 1244 |
v_seri(i, k) = v_seri(i, k) + d_v_lif(i, k) |
| 1245 |
ENDDO |
| 1246 |
ENDDO |
| 1247 |
ENDIF |
| 1248 |
|
| 1249 |
! Stress n\'ecessaires : toute la physique |
| 1250 |
|
| 1251 |
DO i = 1, klon |
| 1252 |
zustrph(i) = 0. |
| 1253 |
zvstrph(i) = 0. |
| 1254 |
ENDDO |
| 1255 |
DO k = 1, llm |
| 1256 |
DO i = 1, klon |
| 1257 |
zustrph(i) = zustrph(i) + (u_seri(i, k) - u(i, k)) / dtphys & |
| 1258 |
* zmasse(i, k) |
| 1259 |
zvstrph(i) = zvstrph(i) + (v_seri(i, k) - v(i, k)) / dtphys & |
| 1260 |
* zmasse(i, k) |
| 1261 |
ENDDO |
| 1262 |
ENDDO |
| 1263 |
|
| 1264 |
CALL aaam_bud(rg, romega, rlat, rlon, pphis, zustrdr, zustrli, zustrph, & |
| 1265 |
zvstrdr, zvstrli, zvstrph, paprs, u, v, aam, torsfc) |
| 1266 |
|
| 1267 |
IF (if_ebil >= 2) CALL diagetpq(airephy, 'after orography', ip_ebil, 2, & |
| 1268 |
2, dtphys, t_seri, q_seri, ql_seri, u_seri, v_seri, paprs, d_h_vcol, & |
| 1269 |
d_qt, d_ec) |
| 1270 |
|
| 1271 |
! Calcul des tendances traceurs |
| 1272 |
call phytrac(itap, lmt_pas, julien, time, firstcal, lafin, dtphys, t, & |
| 1273 |
paprs, play, mfu, mfd, pde_u, pen_d, ycoefh, fm_therm, entr_therm, & |
| 1274 |
yu1, yv1, ftsol, pctsrf, frac_impa, frac_nucl, da, phi, mp, upwd, & |
| 1275 |
dnwd, tr_seri, zmasse, ncid_startphy, nid_ins, itau_phy) |
| 1276 |
|
| 1277 |
IF (offline) call phystokenc(dtphys, t, mfu, mfd, pen_u, pde_u, pen_d, & |
| 1278 |
pde_d, fm_therm, entr_therm, ycoefh, yu1, yv1, ftsol, pctsrf, & |
| 1279 |
frac_impa, frac_nucl, pphis, airephy, dtphys, itap) |
| 1280 |
|
| 1281 |
! Calculer le transport de l'eau et de l'energie (diagnostique) |
| 1282 |
CALL transp(paprs, t_seri, q_seri, u_seri, v_seri, zphi, ve, vq, ue, uq) |
| 1283 |
|
| 1284 |
! diag. bilKP |
| 1285 |
|
| 1286 |
CALL transp_lay(paprs, t_seri, q_seri, u_seri, v_seri, zphi, & |
| 1287 |
ve_lay, vq_lay, ue_lay, uq_lay) |
| 1288 |
|
| 1289 |
! Accumuler les variables a stocker dans les fichiers histoire: |
| 1290 |
|
| 1291 |
! conversion Ec -> E thermique |
| 1292 |
DO k = 1, llm |
| 1293 |
DO i = 1, klon |
| 1294 |
ZRCPD = RCPD * (1. + RVTMP2 * q_seri(i, k)) |
| 1295 |
d_t_ec(i, k) = 0.5 / ZRCPD & |
| 1296 |
* (u(i, k)**2 + v(i, k)**2 - u_seri(i, k)**2 - v_seri(i, k)**2) |
| 1297 |
t_seri(i, k) = t_seri(i, k) + d_t_ec(i, k) |
| 1298 |
d_t_ec(i, k) = d_t_ec(i, k) / dtphys |
| 1299 |
END DO |
| 1300 |
END DO |
| 1301 |
|
| 1302 |
IF (if_ebil >= 1) THEN |
| 1303 |
tit = 'after physic' |
| 1304 |
CALL diagetpq(airephy, tit, ip_ebil, 1, 1, dtphys, t_seri, q_seri, & |
| 1305 |
ql_seri, u_seri, v_seri, paprs, d_h_vcol, d_qt, d_ec) |
| 1306 |
! Comme les tendances de la physique sont ajoute dans la dynamique, |
| 1307 |
! on devrait avoir que la variation d'entalpie par la dynamique |
| 1308 |
! est egale a la variation de la physique au pas de temps precedent. |
| 1309 |
! Donc la somme de ces 2 variations devrait etre nulle. |
| 1310 |
call diagphy(airephy, tit, ip_ebil, topsw, toplw, solsw, sollw, sens, & |
| 1311 |
evap, rain_fall, snow_fall, ztsol, d_h_vcol, d_qt, d_ec) |
| 1312 |
d_h_vcol_phy = d_h_vcol |
| 1313 |
END IF |
| 1314 |
|
| 1315 |
! SORTIES |
| 1316 |
|
| 1317 |
! prw = eau precipitable |
| 1318 |
DO i = 1, klon |
| 1319 |
prw(i) = 0. |
| 1320 |
DO k = 1, llm |
| 1321 |
prw(i) = prw(i) + q_seri(i, k)*zmasse(i, k) |
| 1322 |
ENDDO |
| 1323 |
ENDDO |
| 1324 |
|
| 1325 |
! Convertir les incrementations en tendances |
| 1326 |
|
| 1327 |
DO k = 1, llm |
| 1328 |
DO i = 1, klon |
| 1329 |
d_u(i, k) = (u_seri(i, k) - u(i, k)) / dtphys |
| 1330 |
d_v(i, k) = (v_seri(i, k) - v(i, k)) / dtphys |
| 1331 |
d_t(i, k) = (t_seri(i, k) - t(i, k)) / dtphys |
| 1332 |
d_qx(i, k, ivap) = (q_seri(i, k) - qx(i, k, ivap)) / dtphys |
| 1333 |
d_qx(i, k, iliq) = (ql_seri(i, k) - qx(i, k, iliq)) / dtphys |
| 1334 |
ENDDO |
| 1335 |
ENDDO |
| 1336 |
|
| 1337 |
DO iq = 3, nqmx |
| 1338 |
DO k = 1, llm |
| 1339 |
DO i = 1, klon |
| 1340 |
d_qx(i, k, iq) = (tr_seri(i, k, iq - 2) - qx(i, k, iq)) / dtphys |
| 1341 |
ENDDO |
| 1342 |
ENDDO |
| 1343 |
ENDDO |
| 1344 |
|
| 1345 |
! Sauvegarder les valeurs de t et q a la fin de la physique: |
| 1346 |
DO k = 1, llm |
| 1347 |
DO i = 1, klon |
| 1348 |
t_ancien(i, k) = t_seri(i, k) |
| 1349 |
q_ancien(i, k) = q_seri(i, k) |
| 1350 |
ENDDO |
| 1351 |
ENDDO |
| 1352 |
|
| 1353 |
call write_histins |
| 1354 |
|
| 1355 |
IF (lafin) then |
| 1356 |
call NF95_CLOSE(ncid_startphy) |
| 1357 |
CALL phyredem(pctsrf, ftsol, ftsoil, fqsurf, qsol, & |
| 1358 |
fsnow, falbe, fevap, rain_fall, snow_fall, solsw, sollw, dlw, & |
| 1359 |
radsol, frugs, agesno, zmea, zstd, zsig, zgam, zthe, zpic, zval, & |
| 1360 |
t_ancien, q_ancien, rnebcon, ratqs, clwcon, run_off_lic_0, sig1, & |
| 1361 |
w01) |
| 1362 |
end IF |
| 1363 |
|
| 1364 |
firstcal = .FALSE. |
| 1365 |
|
| 1366 |
contains |
| 1367 |
|
| 1368 |
subroutine write_histins |
| 1369 |
|
| 1370 |
! From phylmd/write_histins.h, version 1.2 2005/05/25 13:10:09 |
| 1371 |
|
| 1372 |
! Ecriture des sorties |
| 1373 |
|
| 1374 |
use gr_phy_write_m, only: gr_phy_write |
| 1375 |
USE histsync_m, ONLY: histsync |
| 1376 |
USE histwrite_m, ONLY: histwrite |
| 1377 |
|
| 1378 |
integer itau_w ! pas de temps d'\'ecriture |
| 1379 |
|
| 1380 |
!-------------------------------------------------- |
| 1381 |
|
| 1382 |
IF (ok_instan) THEN |
| 1383 |
itau_w = itau_phy + itap |
| 1384 |
CALL histwrite(nid_ins, "phis", itau_w, gr_phy_write(pphis)) |
| 1385 |
CALL histwrite(nid_ins, "aire", itau_w, gr_phy_write(airephy)) |
| 1386 |
CALL histwrite(nid_ins, "psol", itau_w, gr_phy_write(paprs(:, 1))) |
| 1387 |
CALL histwrite(nid_ins, "precip", itau_w, & |
| 1388 |
gr_phy_write(rain_fall + snow_fall)) |
| 1389 |
CALL histwrite(nid_ins, "plul", itau_w, & |
| 1390 |
gr_phy_write(rain_lsc + snow_lsc)) |
| 1391 |
CALL histwrite(nid_ins, "pluc", itau_w, & |
| 1392 |
gr_phy_write(rain_con + snow_con)) |
| 1393 |
CALL histwrite(nid_ins, "tsol", itau_w, gr_phy_write(zxtsol)) |
| 1394 |
CALL histwrite(nid_ins, "t2m", itau_w, gr_phy_write(zt2m)) |
| 1395 |
CALL histwrite(nid_ins, "q2m", itau_w, gr_phy_write(zq2m)) |
| 1396 |
CALL histwrite(nid_ins, "u10m", itau_w, gr_phy_write(zu10m)) |
| 1397 |
CALL histwrite(nid_ins, "v10m", itau_w, gr_phy_write(zv10m)) |
| 1398 |
CALL histwrite(nid_ins, "snow", itau_w, gr_phy_write(snow_fall)) |
| 1399 |
CALL histwrite(nid_ins, "cdrm", itau_w, gr_phy_write(cdragm)) |
| 1400 |
CALL histwrite(nid_ins, "cdrh", itau_w, gr_phy_write(cdragh)) |
| 1401 |
CALL histwrite(nid_ins, "topl", itau_w, gr_phy_write(toplw)) |
| 1402 |
CALL histwrite(nid_ins, "evap", itau_w, gr_phy_write(evap)) |
| 1403 |
CALL histwrite(nid_ins, "sols", itau_w, gr_phy_write(solsw)) |
| 1404 |
CALL histwrite(nid_ins, "soll", itau_w, gr_phy_write(sollw)) |
| 1405 |
CALL histwrite(nid_ins, "solldown", itau_w, gr_phy_write(sollwdown)) |
| 1406 |
CALL histwrite(nid_ins, "bils", itau_w, gr_phy_write(bils)) |
| 1407 |
CALL histwrite(nid_ins, "sens", itau_w, gr_phy_write(- sens)) |
| 1408 |
CALL histwrite(nid_ins, "fder", itau_w, gr_phy_write(fder)) |
| 1409 |
CALL histwrite(nid_ins, "dtsvdfo", itau_w, & |
| 1410 |
gr_phy_write(d_ts(:, is_oce))) |
| 1411 |
CALL histwrite(nid_ins, "dtsvdft", itau_w, & |
| 1412 |
gr_phy_write(d_ts(:, is_ter))) |
| 1413 |
CALL histwrite(nid_ins, "dtsvdfg", itau_w, & |
| 1414 |
gr_phy_write(d_ts(:, is_lic))) |
| 1415 |
CALL histwrite(nid_ins, "dtsvdfi", itau_w, & |
| 1416 |
gr_phy_write(d_ts(:, is_sic))) |
| 1417 |
|
| 1418 |
DO nsrf = 1, nbsrf |
| 1419 |
CALL histwrite(nid_ins, "pourc_"//clnsurf(nsrf), itau_w, & |
| 1420 |
gr_phy_write(pctsrf(:, nsrf)*100.)) |
| 1421 |
CALL histwrite(nid_ins, "fract_"//clnsurf(nsrf), itau_w, & |
| 1422 |
gr_phy_write(pctsrf(:, nsrf))) |
| 1423 |
CALL histwrite(nid_ins, "sens_"//clnsurf(nsrf), itau_w, & |
| 1424 |
gr_phy_write(fluxt(:, 1, nsrf))) |
| 1425 |
CALL histwrite(nid_ins, "lat_"//clnsurf(nsrf), itau_w, & |
| 1426 |
gr_phy_write(fluxlat(:, nsrf))) |
| 1427 |
CALL histwrite(nid_ins, "tsol_"//clnsurf(nsrf), itau_w, & |
| 1428 |
gr_phy_write(ftsol(:, nsrf))) |
| 1429 |
CALL histwrite(nid_ins, "taux_"//clnsurf(nsrf), itau_w, & |
| 1430 |
gr_phy_write(fluxu(:, 1, nsrf))) |
| 1431 |
CALL histwrite(nid_ins, "tauy_"//clnsurf(nsrf), itau_w, & |
| 1432 |
gr_phy_write(fluxv(:, 1, nsrf))) |
| 1433 |
CALL histwrite(nid_ins, "rugs_"//clnsurf(nsrf), itau_w, & |
| 1434 |
gr_phy_write(frugs(:, nsrf))) |
| 1435 |
CALL histwrite(nid_ins, "albe_"//clnsurf(nsrf), itau_w, & |
| 1436 |
gr_phy_write(falbe(:, nsrf))) |
| 1437 |
END DO |
| 1438 |
|
| 1439 |
CALL histwrite(nid_ins, "albs", itau_w, gr_phy_write(albsol)) |
| 1440 |
CALL histwrite(nid_ins, "rugs", itau_w, gr_phy_write(zxrugs)) |
| 1441 |
CALL histwrite(nid_ins, "s_pblh", itau_w, gr_phy_write(s_pblh)) |
| 1442 |
CALL histwrite(nid_ins, "s_pblt", itau_w, gr_phy_write(s_pblt)) |
| 1443 |
CALL histwrite(nid_ins, "s_lcl", itau_w, gr_phy_write(s_lcl)) |
| 1444 |
CALL histwrite(nid_ins, "s_capCL", itau_w, gr_phy_write(s_capCL)) |
| 1445 |
CALL histwrite(nid_ins, "s_oliqCL", itau_w, gr_phy_write(s_oliqCL)) |
| 1446 |
CALL histwrite(nid_ins, "s_cteiCL", itau_w, gr_phy_write(s_cteiCL)) |
| 1447 |
CALL histwrite(nid_ins, "s_therm", itau_w, gr_phy_write(s_therm)) |
| 1448 |
CALL histwrite(nid_ins, "s_trmb1", itau_w, gr_phy_write(s_trmb1)) |
| 1449 |
CALL histwrite(nid_ins, "s_trmb2", itau_w, gr_phy_write(s_trmb2)) |
| 1450 |
CALL histwrite(nid_ins, "s_trmb3", itau_w, gr_phy_write(s_trmb3)) |
| 1451 |
if (conv_emanuel) CALL histwrite(nid_ins, "ptop", itau_w, & |
| 1452 |
gr_phy_write(ema_pct)) |
| 1453 |
CALL histwrite(nid_ins, "temp", itau_w, gr_phy_write(t_seri)) |
| 1454 |
CALL histwrite(nid_ins, "vitu", itau_w, gr_phy_write(u_seri)) |
| 1455 |
CALL histwrite(nid_ins, "vitv", itau_w, gr_phy_write(v_seri)) |
| 1456 |
CALL histwrite(nid_ins, "geop", itau_w, gr_phy_write(zphi)) |
| 1457 |
CALL histwrite(nid_ins, "pres", itau_w, gr_phy_write(play)) |
| 1458 |
CALL histwrite(nid_ins, "dtvdf", itau_w, gr_phy_write(d_t_vdf)) |
| 1459 |
CALL histwrite(nid_ins, "dqvdf", itau_w, gr_phy_write(d_q_vdf)) |
| 1460 |
CALL histwrite(nid_ins, "rhum", itau_w, gr_phy_write(zx_rh)) |
| 1461 |
call histsync(nid_ins) |
| 1462 |
ENDIF |
| 1463 |
|
| 1464 |
end subroutine write_histins |
| 1465 |
|
| 1466 |
END SUBROUTINE physiq |
| 1467 |
|
| 1468 |
end module physiq_m |
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