1 |
SUBROUTINE clmain(dtime, itap, date0, pctsrf, pctsrf_new, t, q, u, v,& |
2 |
jour, rmu0, co2_ppm, ok_veget, ocean, npas, nexca, ts,& |
3 |
soil_model, cdmmax, cdhmax, ksta, ksta_ter, ok_kzmin, ftsoil,& |
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qsol, paprs, pplay, snow, qsurf, evap, albe, alblw, fluxlat,& |
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rain_f, snow_f, solsw, sollw, sollwdown, fder, rlon, rlat, cufi,& |
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cvfi, rugos, debut, lafin, agesno, rugoro, d_t, d_q, d_u, d_v,& |
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d_ts, flux_t, flux_q, flux_u, flux_v, cdragh, cdragm, q2,& |
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dflux_t, dflux_q, zcoefh, zu1, zv1, t2m, q2m, u10m, v10m, pblh,& |
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capcl, oliqcl, cteicl, pblt, therm, trmb1, trmb2, trmb3, plcl,& |
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fqcalving, ffonte, run_off_lic_0, flux_o, flux_g, tslab, seaice) |
11 |
|
12 |
! From phylmd/clmain.F, v 1.6 2005/11/16 14:47:19 |
13 |
|
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!AA Tout ce qui a trait au traceurs est dans phytrac maintenant |
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!AA pour l'instant le calcul de la couche limite pour les traceurs |
16 |
!AA se fait avec cltrac et ne tient pas compte de la differentiation |
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!AA des sous-fraction de sol. |
18 |
|
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!AA Pour pouvoir extraire les coefficient d'echanges et le vent |
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!AA dans la premiere couche, 3 champs supplementaires ont ete crees |
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!AA zcoefh, zu1 et zv1. Pour l'instant nous avons moyenne les valeurs |
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!AA de ces trois champs sur les 4 subsurfaces du modele. Dans l'avenir |
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!AA si les informations des subsurfaces doivent etre prises en compte |
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!AA il faudra sortir ces memes champs en leur ajoutant une dimension, |
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!AA c'est a dire nbsrf (nbre de subsurface). |
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|
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! Auteur(s) Z.X. Li (LMD/CNRS) date: 19930818 |
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! Objet: interface de "couche limite" (diffusion verticale) |
29 |
|
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! Arguments: |
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! dtime----input-R- interval du temps (secondes) |
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! itap-----input-I- numero du pas de temps |
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! date0----input-R- jour initial |
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! t--------input-R- temperature (K) |
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! q--------input-R- vapeur d'eau (kg/kg) |
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! u--------input-R- vitesse u |
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! v--------input-R- vitesse v |
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! ts-------input-R- temperature du sol (en Kelvin) |
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! paprs----input-R- pression a intercouche (Pa) |
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! pplay----input-R- pression au milieu de couche (Pa) |
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! radsol---input-R- flux radiatif net (positif vers le sol) en W/m**2 |
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! rlat-----input-R- latitude en degree |
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! rugos----input-R- longeur de rugosite (en m) |
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! cufi-----input-R- resolution des mailles en x (m) |
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! cvfi-----input-R- resolution des mailles en y (m) |
46 |
|
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! d_t------output-R- le changement pour "t" |
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! d_q------output-R- le changement pour "q" |
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! d_u------output-R- le changement pour "u" |
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! d_v------output-R- le changement pour "v" |
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! d_ts-----output-R- le changement pour "ts" |
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! flux_t---output-R- flux de chaleur sensible (CpT) J/m**2/s (W/m**2) |
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! (orientation positive vers le bas) |
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! flux_q---output-R- flux de vapeur d'eau (kg/m**2/s) |
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! flux_u---output-R- tension du vent X: (kg m/s)/(m**2 s) ou Pascal |
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! flux_v---output-R- tension du vent Y: (kg m/s)/(m**2 s) ou Pascal |
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! dflux_t derive du flux sensible |
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! dflux_q derive du flux latent |
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!IM "slab" ocean |
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! flux_g---output-R- flux glace (pour OCEAN='slab ') |
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! flux_o---output-R- flux ocean (pour OCEAN='slab ') |
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! tslab-in/output-R temperature du slab ocean (en Kelvin) ! uniqmnt pour slab |
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! seaice---output-R- glace de mer (kg/m2) (pour OCEAN='slab ') |
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!cc |
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! ffonte----Flux thermique utilise pour fondre la neige |
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! fqcalving-Flux d'eau "perdue" par la surface et necessaire pour limiter la |
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! hauteur de neige, en kg/m2/s |
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!AA on rajoute en output yu1 et yv1 qui sont les vents dans |
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!AA la premiere couche |
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!AA ces 4 variables sont maintenant traites dans phytrac |
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! itr--------input-I- nombre de traceurs |
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! tr---------input-R- q. de traceurs |
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! flux_surf--input-R- flux de traceurs a la surface |
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! d_tr-------output-R tendance de traceurs |
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!IM cf. AM : PBL |
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! trmb1-------deep_cape |
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! trmb2--------inhibition |
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! trmb3-------Point Omega |
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! Cape(klon)-------Cape du thermique |
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! EauLiq(klon)-------Eau liqu integr du thermique |
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! ctei(klon)-------Critere d'instab d'entrainmt des nuages de CL |
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! lcl------- Niveau de condensation |
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! pblh------- HCL |
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! pblT------- T au nveau HCL |
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|
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!$$$ PB ajout pour soil |
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|
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USE histcom, ONLY : histbeg_totreg, histdef, histend, histsync |
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use histwrite_m, only: histwrite |
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use calendar, ONLY : ymds2ju |
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USE dimens_m, ONLY : iim, jjm |
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USE indicesol, ONLY : epsfra, is_lic, is_oce, is_sic, is_ter, nbsrf |
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USE dimphy, ONLY : klev, klon, zmasq |
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USE dimsoil, ONLY : nsoilmx |
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USE temps, ONLY : annee_ref, itau_phy |
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USE dynetat0_m, ONLY : day_ini |
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USE iniprint, ONLY : prt_level |
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USE yomcst, ONLY : rd, rg, rkappa |
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USE conf_phys_m, ONLY : iflag_pbl |
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USE gath_cpl, ONLY : gath2cpl |
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use hbtm_m, only: hbtm |
102 |
|
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IMPLICIT NONE |
104 |
|
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REAL, INTENT (IN) :: dtime |
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REAL date0 |
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INTEGER, INTENT (IN) :: itap |
108 |
REAL t(klon, klev), q(klon, klev) |
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REAL u(klon, klev), v(klon, klev) |
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REAL, INTENT (IN) :: paprs(klon, klev+1) |
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REAL, INTENT (IN) :: pplay(klon, klev) |
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REAL, INTENT (IN) :: rlon(klon), rlat(klon) |
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REAL cufi(klon), cvfi(klon) |
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REAL d_t(klon, klev), d_q(klon, klev) |
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REAL d_u(klon, klev), d_v(klon, klev) |
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REAL flux_t(klon, klev, nbsrf), flux_q(klon, klev, nbsrf) |
117 |
REAL dflux_t(klon), dflux_q(klon) |
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!IM "slab" ocean |
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REAL flux_o(klon), flux_g(klon) |
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REAL y_flux_o(klon), y_flux_g(klon) |
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REAL tslab(klon), ytslab(klon) |
122 |
REAL seaice(klon), y_seaice(klon) |
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REAL y_fqcalving(klon), y_ffonte(klon) |
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REAL fqcalving(klon, nbsrf), ffonte(klon, nbsrf) |
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REAL run_off_lic_0(klon), y_run_off_lic_0(klon) |
126 |
|
127 |
REAL flux_u(klon, klev, nbsrf), flux_v(klon, klev, nbsrf) |
128 |
REAL rugmer(klon), agesno(klon, nbsrf) |
129 |
REAL, INTENT (IN) :: rugoro(klon) |
130 |
REAL cdragh(klon), cdragm(klon) |
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! jour de l'annee en cours |
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INTEGER jour |
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REAL rmu0(klon) ! cosinus de l'angle solaire zenithal |
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! taux CO2 atmosphere |
135 |
REAL co2_ppm |
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LOGICAL, INTENT (IN) :: debut |
137 |
LOGICAL, INTENT (IN) :: lafin |
138 |
LOGICAL ok_veget |
139 |
CHARACTER (len=*), INTENT (IN) :: ocean |
140 |
INTEGER npas, nexca |
141 |
|
142 |
REAL pctsrf(klon, nbsrf) |
143 |
REAL ts(klon, nbsrf) |
144 |
REAL d_ts(klon, nbsrf) |
145 |
REAL snow(klon, nbsrf) |
146 |
REAL qsurf(klon, nbsrf) |
147 |
REAL evap(klon, nbsrf) |
148 |
REAL albe(klon, nbsrf) |
149 |
REAL alblw(klon, nbsrf) |
150 |
|
151 |
REAL fluxlat(klon, nbsrf) |
152 |
|
153 |
REAL rain_f(klon), snow_f(klon) |
154 |
REAL fder(klon) |
155 |
|
156 |
REAL sollw(klon, nbsrf), solsw(klon, nbsrf), sollwdown(klon) |
157 |
REAL rugos(klon, nbsrf) |
158 |
! la nouvelle repartition des surfaces sortie de l'interface |
159 |
REAL pctsrf_new(klon, nbsrf) |
160 |
|
161 |
REAL zcoefh(klon, klev) |
162 |
REAL zu1(klon) |
163 |
REAL zv1(klon) |
164 |
|
165 |
!$$$ PB ajout pour soil |
166 |
LOGICAL, INTENT (IN) :: soil_model |
167 |
!IM ajout seuils cdrm, cdrh |
168 |
REAL cdmmax, cdhmax |
169 |
|
170 |
REAL ksta, ksta_ter |
171 |
LOGICAL ok_kzmin |
172 |
|
173 |
REAL ftsoil(klon, nsoilmx, nbsrf) |
174 |
REAL ytsoil(klon, nsoilmx) |
175 |
REAL qsol(klon) |
176 |
|
177 |
EXTERNAL clqh, clvent, coefkz, calbeta, cltrac |
178 |
|
179 |
REAL yts(klon), yrugos(klon), ypct(klon), yz0_new(klon) |
180 |
REAL yalb(klon) |
181 |
REAL yalblw(klon) |
182 |
REAL yu1(klon), yv1(klon) |
183 |
REAL ysnow(klon), yqsurf(klon), yagesno(klon), yqsol(klon) |
184 |
REAL yrain_f(klon), ysnow_f(klon) |
185 |
REAL ysollw(klon), ysolsw(klon), ysollwdown(klon) |
186 |
REAL yfder(klon), ytaux(klon), ytauy(klon) |
187 |
REAL yrugm(klon), yrads(klon), yrugoro(klon) |
188 |
|
189 |
REAL yfluxlat(klon) |
190 |
|
191 |
REAL y_d_ts(klon) |
192 |
REAL y_d_t(klon, klev), y_d_q(klon, klev) |
193 |
REAL y_d_u(klon, klev), y_d_v(klon, klev) |
194 |
REAL y_flux_t(klon, klev), y_flux_q(klon, klev) |
195 |
REAL y_flux_u(klon, klev), y_flux_v(klon, klev) |
196 |
REAL y_dflux_t(klon), y_dflux_q(klon) |
197 |
REAL ycoefh(klon, klev), ycoefm(klon, klev) |
198 |
REAL yu(klon, klev), yv(klon, klev) |
199 |
REAL yt(klon, klev), yq(klon, klev) |
200 |
REAL ypaprs(klon, klev+1), ypplay(klon, klev), ydelp(klon, klev) |
201 |
|
202 |
LOGICAL ok_nonloc |
203 |
PARAMETER (ok_nonloc=.FALSE.) |
204 |
REAL ycoefm0(klon, klev), ycoefh0(klon, klev) |
205 |
|
206 |
!IM 081204 hcl_Anne ? BEG |
207 |
REAL yzlay(klon, klev), yzlev(klon, klev+1), yteta(klon, klev) |
208 |
REAL ykmm(klon, klev+1), ykmn(klon, klev+1) |
209 |
REAL ykmq(klon, klev+1) |
210 |
REAL yq2(klon, klev+1), q2(klon, klev+1, nbsrf) |
211 |
REAL q2diag(klon, klev+1) |
212 |
!IM 081204 hcl_Anne ? END |
213 |
|
214 |
REAL u1lay(klon), v1lay(klon) |
215 |
REAL delp(klon, klev) |
216 |
INTEGER i, k, nsrf |
217 |
|
218 |
INTEGER ni(klon), knon, j |
219 |
! Introduction d'une variable "pourcentage potentiel" pour tenir compte |
220 |
! des eventuelles apparitions et/ou disparitions de la glace de mer |
221 |
REAL pctsrf_pot(klon, nbsrf) |
222 |
|
223 |
REAL zx_alf1, zx_alf2 !valeur ambiante par extrapola. |
224 |
|
225 |
! maf pour sorties IOISPL en cas de debugagage |
226 |
|
227 |
CHARACTER (80) cldebug |
228 |
SAVE cldebug |
229 |
CHARACTER (8) cl_surf(nbsrf) |
230 |
SAVE cl_surf |
231 |
INTEGER nhoridbg, nidbg |
232 |
SAVE nhoridbg, nidbg |
233 |
INTEGER ndexbg(iim*(jjm+1)) |
234 |
REAL zx_lon(iim, jjm+1), zx_lat(iim, jjm+1), zjulian |
235 |
REAL tabindx(klon) |
236 |
REAL debugtab(iim, jjm+1) |
237 |
LOGICAL first_appel |
238 |
SAVE first_appel |
239 |
DATA first_appel/ .TRUE./ |
240 |
LOGICAL :: debugindex = .FALSE. |
241 |
INTEGER idayref |
242 |
REAL t2m(klon, nbsrf), q2m(klon, nbsrf) |
243 |
REAL u10m(klon, nbsrf), v10m(klon, nbsrf) |
244 |
|
245 |
REAL yt2m(klon), yq2m(klon), yu10m(klon) |
246 |
REAL yustar(klon) |
247 |
! -- LOOP |
248 |
REAL yu10mx(klon) |
249 |
REAL yu10my(klon) |
250 |
REAL ywindsp(klon) |
251 |
! -- LOOP |
252 |
|
253 |
REAL yt10m(klon), yq10m(klon) |
254 |
!IM cf. AM : pbl, hbtm (Comme les autres diagnostics on cumule ds |
255 |
! physiq ce qui permet de sortir les grdeurs par sous surface) |
256 |
REAL pblh(klon, nbsrf) |
257 |
REAL plcl(klon, nbsrf) |
258 |
REAL capcl(klon, nbsrf) |
259 |
REAL oliqcl(klon, nbsrf) |
260 |
REAL cteicl(klon, nbsrf) |
261 |
REAL pblt(klon, nbsrf) |
262 |
REAL therm(klon, nbsrf) |
263 |
REAL trmb1(klon, nbsrf) |
264 |
REAL trmb2(klon, nbsrf) |
265 |
REAL trmb3(klon, nbsrf) |
266 |
REAL ypblh(klon) |
267 |
REAL ylcl(klon) |
268 |
REAL ycapcl(klon) |
269 |
REAL yoliqcl(klon) |
270 |
REAL ycteicl(klon) |
271 |
REAL ypblt(klon) |
272 |
REAL ytherm(klon) |
273 |
REAL ytrmb1(klon) |
274 |
REAL ytrmb2(klon) |
275 |
REAL ytrmb3(klon) |
276 |
REAL y_cd_h(klon), y_cd_m(klon) |
277 |
REAL uzon(klon), vmer(klon) |
278 |
REAL tair1(klon), qair1(klon), tairsol(klon) |
279 |
REAL psfce(klon), patm(klon) |
280 |
|
281 |
REAL qairsol(klon), zgeo1(klon) |
282 |
REAL rugo1(klon) |
283 |
|
284 |
! utiliser un jeu de fonctions simples |
285 |
LOGICAL zxli |
286 |
PARAMETER (zxli=.FALSE.) |
287 |
|
288 |
REAL zt, zqs, zdelta, zcor |
289 |
REAL t_coup |
290 |
PARAMETER (t_coup=273.15) |
291 |
|
292 |
CHARACTER (len=20) :: modname = 'clmain' |
293 |
|
294 |
!------------------------------------------------------------ |
295 |
|
296 |
! initialisation Anne |
297 |
ytherm = 0. |
298 |
|
299 |
IF (debugindex .AND. first_appel) THEN |
300 |
first_appel = .FALSE. |
301 |
|
302 |
! initialisation sorties netcdf |
303 |
|
304 |
idayref = day_ini |
305 |
CALL ymds2ju(annee_ref, 1, idayref, 0.0, zjulian) |
306 |
CALL gr_fi_ecrit(1, klon, iim, jjm+1, rlon, zx_lon) |
307 |
DO i = 1, iim |
308 |
zx_lon(i, 1) = rlon(i+1) |
309 |
zx_lon(i, jjm+1) = rlon(i+1) |
310 |
END DO |
311 |
CALL gr_fi_ecrit(1, klon, iim, jjm+1, rlat, zx_lat) |
312 |
cldebug = 'sous_index' |
313 |
CALL histbeg_totreg(cldebug, zx_lon(:, 1), zx_lat(1, :), 1, & |
314 |
iim, 1, jjm+1, itau_phy, zjulian, dtime, nhoridbg, nidbg) |
315 |
! no vertical axis |
316 |
cl_surf(1) = 'ter' |
317 |
cl_surf(2) = 'lic' |
318 |
cl_surf(3) = 'oce' |
319 |
cl_surf(4) = 'sic' |
320 |
DO nsrf = 1, nbsrf |
321 |
CALL histdef(nidbg, cl_surf(nsrf), cl_surf(nsrf), '-', iim, jjm+1, & |
322 |
nhoridbg, 1, 1, 1, -99, 'inst', dtime, dtime) |
323 |
END DO |
324 |
CALL histend(nidbg) |
325 |
CALL histsync(nidbg) |
326 |
END IF |
327 |
|
328 |
DO k = 1, klev ! epaisseur de couche |
329 |
DO i = 1, klon |
330 |
delp(i, k) = paprs(i, k) - paprs(i, k+1) |
331 |
END DO |
332 |
END DO |
333 |
DO i = 1, klon ! vent de la premiere couche |
334 |
zx_alf1 = 1.0 |
335 |
zx_alf2 = 1.0 - zx_alf1 |
336 |
u1lay(i) = u(i, 1)*zx_alf1 + u(i, 2)*zx_alf2 |
337 |
v1lay(i) = v(i, 1)*zx_alf1 + v(i, 2)*zx_alf2 |
338 |
END DO |
339 |
|
340 |
! initialisation: |
341 |
|
342 |
DO i = 1, klon |
343 |
rugmer(i) = 0.0 |
344 |
cdragh(i) = 0.0 |
345 |
cdragm(i) = 0.0 |
346 |
dflux_t(i) = 0.0 |
347 |
dflux_q(i) = 0.0 |
348 |
zu1(i) = 0.0 |
349 |
zv1(i) = 0.0 |
350 |
END DO |
351 |
ypct = 0.0 |
352 |
yts = 0.0 |
353 |
ysnow = 0.0 |
354 |
yqsurf = 0.0 |
355 |
yalb = 0.0 |
356 |
yalblw = 0.0 |
357 |
yrain_f = 0.0 |
358 |
ysnow_f = 0.0 |
359 |
yfder = 0.0 |
360 |
ytaux = 0.0 |
361 |
ytauy = 0.0 |
362 |
ysolsw = 0.0 |
363 |
ysollw = 0.0 |
364 |
ysollwdown = 0.0 |
365 |
yrugos = 0.0 |
366 |
yu1 = 0.0 |
367 |
yv1 = 0.0 |
368 |
yrads = 0.0 |
369 |
ypaprs = 0.0 |
370 |
ypplay = 0.0 |
371 |
ydelp = 0.0 |
372 |
yu = 0.0 |
373 |
yv = 0.0 |
374 |
yt = 0.0 |
375 |
yq = 0.0 |
376 |
pctsrf_new = 0.0 |
377 |
y_flux_u = 0.0 |
378 |
y_flux_v = 0.0 |
379 |
!$$ PB |
380 |
y_dflux_t = 0.0 |
381 |
y_dflux_q = 0.0 |
382 |
ytsoil = 999999. |
383 |
yrugoro = 0. |
384 |
! -- LOOP |
385 |
yu10mx = 0.0 |
386 |
yu10my = 0.0 |
387 |
ywindsp = 0.0 |
388 |
! -- LOOP |
389 |
DO nsrf = 1, nbsrf |
390 |
DO i = 1, klon |
391 |
d_ts(i, nsrf) = 0.0 |
392 |
END DO |
393 |
END DO |
394 |
!§§§ PB |
395 |
yfluxlat = 0. |
396 |
flux_t = 0. |
397 |
flux_q = 0. |
398 |
flux_u = 0. |
399 |
flux_v = 0. |
400 |
DO k = 1, klev |
401 |
DO i = 1, klon |
402 |
d_t(i, k) = 0.0 |
403 |
d_q(i, k) = 0.0 |
404 |
!$$$ flux_t(i, k) = 0.0 |
405 |
!$$$ flux_q(i, k) = 0.0 |
406 |
d_u(i, k) = 0.0 |
407 |
d_v(i, k) = 0.0 |
408 |
!$$$ flux_u(i, k) = 0.0 |
409 |
!$$$ flux_v(i, k) = 0.0 |
410 |
zcoefh(i, k) = 0.0 |
411 |
END DO |
412 |
END DO |
413 |
!AA IF (itr.GE.1) THEN |
414 |
!AA DO it = 1, itr |
415 |
!AA DO k = 1, klev |
416 |
!AA DO i = 1, klon |
417 |
!AA d_tr(i, k, it) = 0.0 |
418 |
!AA ENDDO |
419 |
!AA ENDDO |
420 |
!AA ENDDO |
421 |
!AA ENDIF |
422 |
|
423 |
|
424 |
! Boucler sur toutes les sous-fractions du sol: |
425 |
|
426 |
! Initialisation des "pourcentages potentiels". On considere ici qu'on |
427 |
! peut avoir potentiellementdela glace sur tout le domaine oceanique |
428 |
! (a affiner) |
429 |
|
430 |
pctsrf_pot = pctsrf |
431 |
pctsrf_pot(:, is_oce) = 1. - zmasq |
432 |
pctsrf_pot(:, is_sic) = 1. - zmasq |
433 |
|
434 |
DO nsrf = 1, nbsrf |
435 |
! chercher les indices: |
436 |
ni = 0 |
437 |
knon = 0 |
438 |
DO i = 1, klon |
439 |
! pour determiner le domaine a traiter on utilise les surfaces |
440 |
! "potentielles" |
441 |
IF (pctsrf_pot(i, nsrf) > epsfra) THEN |
442 |
knon = knon + 1 |
443 |
ni(knon) = i |
444 |
END IF |
445 |
END DO |
446 |
|
447 |
! variables pour avoir une sortie IOIPSL des INDEX |
448 |
IF (debugindex) THEN |
449 |
tabindx = 0. |
450 |
DO i = 1, knon |
451 |
tabindx(i) = real(i) |
452 |
END DO |
453 |
debugtab = 0. |
454 |
ndexbg = 0 |
455 |
CALL gath2cpl(tabindx, debugtab, klon, knon, iim, jjm, ni) |
456 |
CALL histwrite(nidbg, cl_surf(nsrf), itap, debugtab) |
457 |
END IF |
458 |
|
459 |
IF (knon==0) CYCLE |
460 |
|
461 |
DO j = 1, knon |
462 |
i = ni(j) |
463 |
ypct(j) = pctsrf(i, nsrf) |
464 |
yts(j) = ts(i, nsrf) |
465 |
ytslab(i) = tslab(i) |
466 |
ysnow(j) = snow(i, nsrf) |
467 |
yqsurf(j) = qsurf(i, nsrf) |
468 |
yalb(j) = albe(i, nsrf) |
469 |
yalblw(j) = alblw(i, nsrf) |
470 |
yrain_f(j) = rain_f(i) |
471 |
ysnow_f(j) = snow_f(i) |
472 |
yagesno(j) = agesno(i, nsrf) |
473 |
yfder(j) = fder(i) |
474 |
ytaux(j) = flux_u(i, 1, nsrf) |
475 |
ytauy(j) = flux_v(i, 1, nsrf) |
476 |
ysolsw(j) = solsw(i, nsrf) |
477 |
ysollw(j) = sollw(i, nsrf) |
478 |
ysollwdown(j) = sollwdown(i) |
479 |
yrugos(j) = rugos(i, nsrf) |
480 |
yrugoro(j) = rugoro(i) |
481 |
yu1(j) = u1lay(i) |
482 |
yv1(j) = v1lay(i) |
483 |
yrads(j) = ysolsw(j) + ysollw(j) |
484 |
ypaprs(j, klev+1) = paprs(i, klev+1) |
485 |
y_run_off_lic_0(j) = run_off_lic_0(i) |
486 |
yu10mx(j) = u10m(i, nsrf) |
487 |
yu10my(j) = v10m(i, nsrf) |
488 |
ywindsp(j) = sqrt(yu10mx(j)*yu10mx(j)+yu10my(j)*yu10my(j)) |
489 |
END DO |
490 |
|
491 |
! IF bucket model for continent, copy soil water content |
492 |
IF (nsrf==is_ter .AND. .NOT. ok_veget) THEN |
493 |
DO j = 1, knon |
494 |
i = ni(j) |
495 |
yqsol(j) = qsol(i) |
496 |
END DO |
497 |
ELSE |
498 |
yqsol = 0. |
499 |
END IF |
500 |
!$$$ PB ajour pour soil |
501 |
DO k = 1, nsoilmx |
502 |
DO j = 1, knon |
503 |
i = ni(j) |
504 |
ytsoil(j, k) = ftsoil(i, k, nsrf) |
505 |
END DO |
506 |
END DO |
507 |
DO k = 1, klev |
508 |
DO j = 1, knon |
509 |
i = ni(j) |
510 |
ypaprs(j, k) = paprs(i, k) |
511 |
ypplay(j, k) = pplay(i, k) |
512 |
ydelp(j, k) = delp(i, k) |
513 |
yu(j, k) = u(i, k) |
514 |
yv(j, k) = v(i, k) |
515 |
yt(j, k) = t(i, k) |
516 |
yq(j, k) = q(i, k) |
517 |
END DO |
518 |
END DO |
519 |
|
520 |
! calculer Cdrag et les coefficients d'echange |
521 |
CALL coefkz(nsrf, knon, ypaprs, ypplay, ksta, ksta_ter, yts,& |
522 |
yrugos, yu, yv, yt, yq, yqsurf, ycoefm, ycoefh) |
523 |
!IM 081204 BEG |
524 |
!CR test |
525 |
IF (iflag_pbl==1) THEN |
526 |
!IM 081204 END |
527 |
CALL coefkz2(nsrf, knon, ypaprs, ypplay, yt, ycoefm0, ycoefh0) |
528 |
DO k = 1, klev |
529 |
DO i = 1, knon |
530 |
ycoefm(i, k) = max(ycoefm(i, k), ycoefm0(i, k)) |
531 |
ycoefh(i, k) = max(ycoefh(i, k), ycoefh0(i, k)) |
532 |
END DO |
533 |
END DO |
534 |
END IF |
535 |
|
536 |
!IM cf JLD : on seuille ycoefm et ycoefh |
537 |
IF (nsrf==is_oce) THEN |
538 |
DO j = 1, knon |
539 |
! ycoefm(j, 1)=min(ycoefm(j, 1), 1.1E-3) |
540 |
ycoefm(j, 1) = min(ycoefm(j, 1), cdmmax) |
541 |
! ycoefh(j, 1)=min(ycoefh(j, 1), 1.1E-3) |
542 |
ycoefh(j, 1) = min(ycoefh(j, 1), cdhmax) |
543 |
END DO |
544 |
END IF |
545 |
|
546 |
|
547 |
!IM: 261103 |
548 |
IF (ok_kzmin) THEN |
549 |
!IM cf FH: 201103 BEG |
550 |
! Calcul d'une diffusion minimale pour les conditions tres stables. |
551 |
CALL coefkzmin(knon, ypaprs, ypplay, yu, yv, yt, yq, ycoefm, ycoefm0, & |
552 |
ycoefh0) |
553 |
! call dump2d(iim, jjm-1, ycoefm(2:klon-1, 2), 'KZ ') |
554 |
! call dump2d(iim, jjm-1, ycoefm0(2:klon-1, 2), 'KZMIN ') |
555 |
|
556 |
IF (1==1) THEN |
557 |
DO k = 1, klev |
558 |
DO i = 1, knon |
559 |
ycoefm(i, k) = max(ycoefm(i, k), ycoefm0(i, k)) |
560 |
ycoefh(i, k) = max(ycoefh(i, k), ycoefh0(i, k)) |
561 |
END DO |
562 |
END DO |
563 |
END IF |
564 |
!IM cf FH: 201103 END |
565 |
!IM: 261103 |
566 |
END IF !ok_kzmin |
567 |
|
568 |
IF (iflag_pbl>=3) THEN |
569 |
|
570 |
!ccccccccccccccccccccccccccccccccccccccccccccccccccccccccccccccccccccc |
571 |
! MELLOR ET YAMADA adapte a Mars Richard Fournier et Frederic Hourdin |
572 |
!ccccccccccccccccccccccccccccccccccccccccccccccccccccccccccccccccccc |
573 |
|
574 |
yzlay(1:knon, 1) = rd*yt(1:knon, 1)/(0.5*(ypaprs(1:knon, & |
575 |
1)+ypplay(1:knon, 1)))*(ypaprs(1:knon, 1)-ypplay(1:knon, 1))/rg |
576 |
DO k = 2, klev |
577 |
yzlay(1:knon, k) = yzlay(1:knon, k-1) & |
578 |
+ rd*0.5*(yt(1:knon, k-1) +yt(1: knon, k)) & |
579 |
/ ypaprs(1:knon, k) *(ypplay(1:knon, k-1)-ypplay(1:knon, k))/ & |
580 |
rg |
581 |
END DO |
582 |
DO k = 1, klev |
583 |
yteta(1:knon, k) = yt(1:knon, k)*(ypaprs(1:knon, 1) & |
584 |
/ ypplay(1:knon, k))**rkappa * (1.+0.61*yq(1:knon, k)) |
585 |
END DO |
586 |
yzlev(1:knon, 1) = 0. |
587 |
yzlev(1:knon, klev+1) = 2.*yzlay(1:knon, klev) - yzlay(1:knon, klev-1) |
588 |
DO k = 2, klev |
589 |
yzlev(1:knon, k) = 0.5*(yzlay(1:knon, k)+yzlay(1:knon, k-1)) |
590 |
END DO |
591 |
DO k = 1, klev + 1 |
592 |
DO j = 1, knon |
593 |
i = ni(j) |
594 |
yq2(j, k) = q2(i, k, nsrf) |
595 |
END DO |
596 |
END DO |
597 |
|
598 |
|
599 |
! Bug introduit volontairement pour converger avec les resultats |
600 |
! du papier sur les thermiques. |
601 |
IF (1==1) THEN |
602 |
y_cd_m(1:knon) = ycoefm(1:knon, 1) |
603 |
y_cd_h(1:knon) = ycoefh(1:knon, 1) |
604 |
ELSE |
605 |
y_cd_h(1:knon) = ycoefm(1:knon, 1) |
606 |
y_cd_m(1:knon) = ycoefh(1:knon, 1) |
607 |
END IF |
608 |
CALL ustarhb(knon, yu, yv, y_cd_m, yustar) |
609 |
|
610 |
IF (prt_level>9) THEN |
611 |
PRINT *, 'USTAR = ', yustar |
612 |
END IF |
613 |
|
614 |
! iflag_pbl peut etre utilise comme longuer de melange |
615 |
|
616 |
IF (iflag_pbl>=11) THEN |
617 |
CALL vdif_kcay(knon, dtime, rg, rd, ypaprs, yt, yzlev, yzlay, yu, yv, yteta, & |
618 |
y_cd_m, yq2, q2diag, ykmm, ykmn, yustar, iflag_pbl) |
619 |
ELSE |
620 |
CALL yamada4(knon, dtime, rg, rd, ypaprs, yt, yzlev, yzlay, yu, yv, yteta, & |
621 |
y_cd_m, yq2, ykmm, ykmn, ykmq, yustar, iflag_pbl) |
622 |
END IF |
623 |
|
624 |
ycoefm(1:knon, 1) = y_cd_m(1:knon) |
625 |
ycoefh(1:knon, 1) = y_cd_h(1:knon) |
626 |
ycoefm(1:knon, 2:klev) = ykmm(1:knon, 2:klev) |
627 |
ycoefh(1:knon, 2:klev) = ykmn(1:knon, 2:klev) |
628 |
|
629 |
|
630 |
END IF |
631 |
|
632 |
!ccccccccccccccccccccccccccccccccccccccccccccccccccccccccccccccccccccc |
633 |
! calculer la diffusion des vitesses "u" et "v" |
634 |
!ccccccccccccccccccccccccccccccccccccccccccccccccccccccccccccccccccc |
635 |
|
636 |
CALL clvent(knon, dtime, yu1, yv1, ycoefm, yt, yu, ypaprs, ypplay, & |
637 |
ydelp, y_d_u, y_flux_u) |
638 |
CALL clvent(knon, dtime, yu1, yv1, ycoefm, yt, yv, ypaprs, ypplay, & |
639 |
ydelp, y_d_v, y_flux_v) |
640 |
|
641 |
! pour le couplage |
642 |
ytaux = y_flux_u(:, 1) |
643 |
ytauy = y_flux_v(:, 1) |
644 |
|
645 |
! FH modif sur le cdrag temperature |
646 |
!$$$PB : déplace dans clcdrag |
647 |
!$$$ do i=1, knon |
648 |
!$$$ ycoefh(i, 1)=ycoefm(i, 1)*0.8 |
649 |
!$$$ enddo |
650 |
|
651 |
! calculer la diffusion de "q" et de "h" |
652 |
CALL clqh(dtime, itap, date0, jour, debut, lafin, rlon, rlat,& |
653 |
cufi, cvfi, knon, nsrf, ni, pctsrf, soil_model, ytsoil,& |
654 |
yqsol, ok_veget, ocean, npas, nexca, rmu0, co2_ppm, yrugos,& |
655 |
yrugoro, yu1, yv1, ycoefh, yt, yq, yts, ypaprs, ypplay,& |
656 |
ydelp, yrads, yalb, yalblw, ysnow, yqsurf, yrain_f, ysnow_f, & |
657 |
yfder, ytaux, ytauy, ywindsp, ysollw, ysollwdown, ysolsw,& |
658 |
yfluxlat, pctsrf_new, yagesno, y_d_t, y_d_q, y_d_ts,& |
659 |
yz0_new, y_flux_t, y_flux_q, y_dflux_t, y_dflux_q,& |
660 |
y_fqcalving, y_ffonte, y_run_off_lic_0, y_flux_o, y_flux_g,& |
661 |
ytslab, y_seaice) |
662 |
|
663 |
! calculer la longueur de rugosite sur ocean |
664 |
yrugm = 0. |
665 |
IF (nsrf==is_oce) THEN |
666 |
DO j = 1, knon |
667 |
yrugm(j) = 0.018*ycoefm(j, 1)*(yu1(j)**2+yv1(j)**2)/rg + & |
668 |
0.11*14E-6/sqrt(ycoefm(j, 1)*(yu1(j)**2+yv1(j)**2)) |
669 |
yrugm(j) = max(1.5E-05, yrugm(j)) |
670 |
END DO |
671 |
END IF |
672 |
DO j = 1, knon |
673 |
y_dflux_t(j) = y_dflux_t(j)*ypct(j) |
674 |
y_dflux_q(j) = y_dflux_q(j)*ypct(j) |
675 |
yu1(j) = yu1(j)*ypct(j) |
676 |
yv1(j) = yv1(j)*ypct(j) |
677 |
END DO |
678 |
|
679 |
DO k = 1, klev |
680 |
DO j = 1, knon |
681 |
i = ni(j) |
682 |
ycoefh(j, k) = ycoefh(j, k)*ypct(j) |
683 |
ycoefm(j, k) = ycoefm(j, k)*ypct(j) |
684 |
y_d_t(j, k) = y_d_t(j, k)*ypct(j) |
685 |
y_d_q(j, k) = y_d_q(j, k)*ypct(j) |
686 |
!§§§ PB |
687 |
flux_t(i, k, nsrf) = y_flux_t(j, k) |
688 |
flux_q(i, k, nsrf) = y_flux_q(j, k) |
689 |
flux_u(i, k, nsrf) = y_flux_u(j, k) |
690 |
flux_v(i, k, nsrf) = y_flux_v(j, k) |
691 |
!$$$ PB y_flux_t(j, k) = y_flux_t(j, k) * ypct(j) |
692 |
!$$$ PB y_flux_q(j, k) = y_flux_q(j, k) * ypct(j) |
693 |
y_d_u(j, k) = y_d_u(j, k)*ypct(j) |
694 |
y_d_v(j, k) = y_d_v(j, k)*ypct(j) |
695 |
!$$$ PB y_flux_u(j, k) = y_flux_u(j, k) * ypct(j) |
696 |
!$$$ PB y_flux_v(j, k) = y_flux_v(j, k) * ypct(j) |
697 |
END DO |
698 |
END DO |
699 |
|
700 |
|
701 |
evap(:, nsrf) = -flux_q(:, 1, nsrf) |
702 |
|
703 |
albe(:, nsrf) = 0. |
704 |
alblw(:, nsrf) = 0. |
705 |
snow(:, nsrf) = 0. |
706 |
qsurf(:, nsrf) = 0. |
707 |
rugos(:, nsrf) = 0. |
708 |
fluxlat(:, nsrf) = 0. |
709 |
DO j = 1, knon |
710 |
i = ni(j) |
711 |
d_ts(i, nsrf) = y_d_ts(j) |
712 |
albe(i, nsrf) = yalb(j) |
713 |
alblw(i, nsrf) = yalblw(j) |
714 |
snow(i, nsrf) = ysnow(j) |
715 |
qsurf(i, nsrf) = yqsurf(j) |
716 |
rugos(i, nsrf) = yz0_new(j) |
717 |
fluxlat(i, nsrf) = yfluxlat(j) |
718 |
!$$$ pb rugmer(i) = yrugm(j) |
719 |
IF (nsrf==is_oce) THEN |
720 |
rugmer(i) = yrugm(j) |
721 |
rugos(i, nsrf) = yrugm(j) |
722 |
END IF |
723 |
!IM cf JLD ?? |
724 |
agesno(i, nsrf) = yagesno(j) |
725 |
fqcalving(i, nsrf) = y_fqcalving(j) |
726 |
ffonte(i, nsrf) = y_ffonte(j) |
727 |
cdragh(i) = cdragh(i) + ycoefh(j, 1) |
728 |
cdragm(i) = cdragm(i) + ycoefm(j, 1) |
729 |
dflux_t(i) = dflux_t(i) + y_dflux_t(j) |
730 |
dflux_q(i) = dflux_q(i) + y_dflux_q(j) |
731 |
zu1(i) = zu1(i) + yu1(j) |
732 |
zv1(i) = zv1(i) + yv1(j) |
733 |
END DO |
734 |
IF (nsrf==is_ter) THEN |
735 |
DO j = 1, knon |
736 |
i = ni(j) |
737 |
qsol(i) = yqsol(j) |
738 |
END DO |
739 |
END IF |
740 |
IF (nsrf==is_lic) THEN |
741 |
DO j = 1, knon |
742 |
i = ni(j) |
743 |
run_off_lic_0(i) = y_run_off_lic_0(j) |
744 |
END DO |
745 |
END IF |
746 |
!$$$ PB ajout pour soil |
747 |
ftsoil(:, :, nsrf) = 0. |
748 |
DO k = 1, nsoilmx |
749 |
DO j = 1, knon |
750 |
i = ni(j) |
751 |
ftsoil(i, k, nsrf) = ytsoil(j, k) |
752 |
END DO |
753 |
END DO |
754 |
|
755 |
DO j = 1, knon |
756 |
i = ni(j) |
757 |
DO k = 1, klev |
758 |
d_t(i, k) = d_t(i, k) + y_d_t(j, k) |
759 |
d_q(i, k) = d_q(i, k) + y_d_q(j, k) |
760 |
!$$$ PB flux_t(i, k) = flux_t(i, k) + y_flux_t(j, k) |
761 |
!$$$ flux_q(i, k) = flux_q(i, k) + y_flux_q(j, k) |
762 |
d_u(i, k) = d_u(i, k) + y_d_u(j, k) |
763 |
d_v(i, k) = d_v(i, k) + y_d_v(j, k) |
764 |
!$$$ PB flux_u(i, k) = flux_u(i, k) + y_flux_u(j, k) |
765 |
!$$$ flux_v(i, k) = flux_v(i, k) + y_flux_v(j, k) |
766 |
zcoefh(i, k) = zcoefh(i, k) + ycoefh(j, k) |
767 |
END DO |
768 |
END DO |
769 |
|
770 |
|
771 |
!cc diagnostic t, q a 2m et u, v a 10m |
772 |
|
773 |
DO j = 1, knon |
774 |
i = ni(j) |
775 |
uzon(j) = yu(j, 1) + y_d_u(j, 1) |
776 |
vmer(j) = yv(j, 1) + y_d_v(j, 1) |
777 |
tair1(j) = yt(j, 1) + y_d_t(j, 1) |
778 |
qair1(j) = yq(j, 1) + y_d_q(j, 1) |
779 |
zgeo1(j) = rd*tair1(j)/(0.5*(ypaprs(j, 1)+ypplay(j, & |
780 |
1)))*(ypaprs(j, 1)-ypplay(j, 1)) |
781 |
tairsol(j) = yts(j) + y_d_ts(j) |
782 |
rugo1(j) = yrugos(j) |
783 |
IF (nsrf==is_oce) THEN |
784 |
rugo1(j) = rugos(i, nsrf) |
785 |
END IF |
786 |
psfce(j) = ypaprs(j, 1) |
787 |
patm(j) = ypplay(j, 1) |
788 |
|
789 |
qairsol(j) = yqsurf(j) |
790 |
END DO |
791 |
|
792 |
CALL stdlevvar(klon, knon, nsrf, zxli, uzon, vmer, tair1, qair1, zgeo1, & |
793 |
tairsol, qairsol, rugo1, psfce, patm, yt2m, yq2m, yt10m, yq10m, & |
794 |
yu10m, yustar) |
795 |
!IM 081204 END |
796 |
|
797 |
DO j = 1, knon |
798 |
i = ni(j) |
799 |
t2m(i, nsrf) = yt2m(j) |
800 |
q2m(i, nsrf) = yq2m(j) |
801 |
|
802 |
! u10m, v10m : composantes du vent a 10m sans spirale de Ekman |
803 |
u10m(i, nsrf) = (yu10m(j)*uzon(j))/sqrt(uzon(j)**2+vmer(j)**2) |
804 |
v10m(i, nsrf) = (yu10m(j)*vmer(j))/sqrt(uzon(j)**2+vmer(j)**2) |
805 |
|
806 |
END DO |
807 |
|
808 |
DO i = 1, knon |
809 |
y_cd_h(i) = ycoefh(i, 1) |
810 |
y_cd_m(i) = ycoefm(i, 1) |
811 |
END DO |
812 |
CALL hbtm(knon, ypaprs, ypplay, yt2m, yt10m, yq2m, yq10m, yustar, & |
813 |
y_flux_t, y_flux_q, yu, yv, yt, yq, ypblh, ycapcl, yoliqcl, & |
814 |
ycteicl, ypblt, ytherm, ytrmb1, ytrmb2, ytrmb3, ylcl) |
815 |
|
816 |
DO j = 1, knon |
817 |
i = ni(j) |
818 |
pblh(i, nsrf) = ypblh(j) |
819 |
plcl(i, nsrf) = ylcl(j) |
820 |
capcl(i, nsrf) = ycapcl(j) |
821 |
oliqcl(i, nsrf) = yoliqcl(j) |
822 |
cteicl(i, nsrf) = ycteicl(j) |
823 |
pblt(i, nsrf) = ypblt(j) |
824 |
therm(i, nsrf) = ytherm(j) |
825 |
trmb1(i, nsrf) = ytrmb1(j) |
826 |
trmb2(i, nsrf) = ytrmb2(j) |
827 |
trmb3(i, nsrf) = ytrmb3(j) |
828 |
END DO |
829 |
|
830 |
|
831 |
DO j = 1, knon |
832 |
DO k = 1, klev + 1 |
833 |
i = ni(j) |
834 |
q2(i, k, nsrf) = yq2(j, k) |
835 |
END DO |
836 |
END DO |
837 |
!IM "slab" ocean |
838 |
IF (nsrf==is_oce) THEN |
839 |
DO j = 1, knon |
840 |
! on projette sur la grille globale |
841 |
i = ni(j) |
842 |
IF (pctsrf_new(i, is_oce)>epsfra) THEN |
843 |
flux_o(i) = y_flux_o(j) |
844 |
ELSE |
845 |
flux_o(i) = 0. |
846 |
END IF |
847 |
END DO |
848 |
END IF |
849 |
|
850 |
IF (nsrf==is_sic) THEN |
851 |
DO j = 1, knon |
852 |
i = ni(j) |
853 |
!IM 230604 on pondere lorsque l'on fait le bilan au sol : flux_g(i) = y_flux_g(j)*ypct(j) |
854 |
IF (pctsrf_new(i, is_sic)>epsfra) THEN |
855 |
flux_g(i) = y_flux_g(j) |
856 |
ELSE |
857 |
flux_g(i) = 0. |
858 |
END IF |
859 |
END DO |
860 |
|
861 |
END IF |
862 |
!nsrf.EQ.is_sic |
863 |
IF (ocean=='slab ') THEN |
864 |
IF (nsrf==is_oce) THEN |
865 |
tslab(1:klon) = ytslab(1:klon) |
866 |
seaice(1:klon) = y_seaice(1:klon) |
867 |
!nsrf |
868 |
END IF |
869 |
!OCEAN |
870 |
END IF |
871 |
END DO |
872 |
|
873 |
! On utilise les nouvelles surfaces |
874 |
! A rajouter: conservation de l'albedo |
875 |
|
876 |
rugos(:, is_oce) = rugmer |
877 |
pctsrf = pctsrf_new |
878 |
|
879 |
END SUBROUTINE clmain |