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,& |
9 |
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 |
17 |
!AA des sous-fraction de sol. |
18 |
|
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!AA Pour pouvoir extraire les coefficient d'echanges et le vent |
20 |
!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). |
26 |
|
27 |
! 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) |
32 |
! itap-----input-I- numero du pas de temps |
33 |
! 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) |
36 |
! 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 |
42 |
! rlat-----input-R- latitude en degree |
43 |
! rugos----input-R- longeur de rugosite (en m) |
44 |
! cufi-----input-R- resolution des mailles en x (m) |
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! cvfi-----input-R- resolution des mailles en y (m) |
46 |
|
47 |
! 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 |
69 |
!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 |
80 |
! EauLiq(klon)-------Eau liqu integr du thermique |
81 |
! 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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|
86 |
!$$$ PB ajout pour soil |
87 |
|
88 |
USE histcom, ONLY : histbeg_totreg, histdef, histend, histsync |
89 |
use histwrite_m, only: histwrite |
90 |
use calendar, ONLY : ymds2ju |
91 |
USE dimens_m, ONLY : iim, jjm |
92 |
USE indicesol, ONLY : epsfra, is_lic, is_oce, is_sic, is_ter, nbsrf |
93 |
USE dimphy, ONLY : klev, klon, zmasq |
94 |
USE dimsoil, ONLY : nsoilmx |
95 |
USE temps, ONLY : annee_ref, itau_phy |
96 |
USE dynetat0_m, ONLY : day_ini |
97 |
USE iniprint, ONLY : prt_level |
98 |
USE yomcst, ONLY : rd, rg, rkappa |
99 |
USE conf_phys_m, ONLY : iflag_pbl |
100 |
USE gath_cpl, ONLY : gath2cpl |
101 |
|
102 |
IMPLICIT NONE |
103 |
|
104 |
REAL, INTENT (IN) :: dtime |
105 |
REAL date0 |
106 |
INTEGER, INTENT (IN) :: itap |
107 |
REAL t(klon, klev), q(klon, klev) |
108 |
REAL u(klon, klev), v(klon, klev) |
109 |
REAL, INTENT (IN) :: paprs(klon, klev+1) |
110 |
REAL, INTENT (IN) :: pplay(klon, klev) |
111 |
REAL, INTENT (IN) :: rlon(klon), rlat(klon) |
112 |
REAL cufi(klon), cvfi(klon) |
113 |
REAL d_t(klon, klev), d_q(klon, klev) |
114 |
REAL d_u(klon, klev), d_v(klon, klev) |
115 |
REAL flux_t(klon, klev, nbsrf), flux_q(klon, klev, nbsrf) |
116 |
REAL dflux_t(klon), dflux_q(klon) |
117 |
!IM "slab" ocean |
118 |
REAL flux_o(klon), flux_g(klon) |
119 |
REAL y_flux_o(klon), y_flux_g(klon) |
120 |
REAL tslab(klon), ytslab(klon) |
121 |
REAL seaice(klon), y_seaice(klon) |
122 |
REAL y_fqcalving(klon), y_ffonte(klon) |
123 |
REAL fqcalving(klon, nbsrf), ffonte(klon, nbsrf) |
124 |
REAL run_off_lic_0(klon), y_run_off_lic_0(klon) |
125 |
|
126 |
REAL flux_u(klon, klev, nbsrf), flux_v(klon, klev, nbsrf) |
127 |
REAL rugmer(klon), agesno(klon, nbsrf) |
128 |
REAL, INTENT (IN) :: rugoro(klon) |
129 |
REAL cdragh(klon), cdragm(klon) |
130 |
! jour de l'annee en cours |
131 |
INTEGER jour |
132 |
REAL rmu0(klon) ! cosinus de l'angle solaire zenithal |
133 |
! taux CO2 atmosphere |
134 |
REAL co2_ppm |
135 |
LOGICAL, INTENT (IN) :: debut |
136 |
LOGICAL, INTENT (IN) :: lafin |
137 |
LOGICAL ok_veget |
138 |
CHARACTER (len=*), INTENT (IN) :: ocean |
139 |
INTEGER npas, nexca |
140 |
|
141 |
REAL pctsrf(klon, nbsrf) |
142 |
REAL ts(klon, nbsrf) |
143 |
REAL d_ts(klon, nbsrf) |
144 |
REAL snow(klon, nbsrf) |
145 |
REAL qsurf(klon, nbsrf) |
146 |
REAL evap(klon, nbsrf) |
147 |
REAL albe(klon, nbsrf) |
148 |
REAL alblw(klon, nbsrf) |
149 |
|
150 |
REAL fluxlat(klon, nbsrf) |
151 |
|
152 |
REAL rain_f(klon), snow_f(klon) |
153 |
REAL fder(klon) |
154 |
|
155 |
REAL sollw(klon, nbsrf), solsw(klon, nbsrf), sollwdown(klon) |
156 |
REAL rugos(klon, nbsrf) |
157 |
! la nouvelle repartition des surfaces sortie de l'interface |
158 |
REAL pctsrf_new(klon, nbsrf) |
159 |
|
160 |
REAL zcoefh(klon, klev) |
161 |
REAL zu1(klon) |
162 |
REAL zv1(klon) |
163 |
|
164 |
!$$$ PB ajout pour soil |
165 |
LOGICAL, INTENT (IN) :: soil_model |
166 |
!IM ajout seuils cdrm, cdrh |
167 |
REAL cdmmax, cdhmax |
168 |
|
169 |
REAL ksta, ksta_ter |
170 |
LOGICAL ok_kzmin |
171 |
|
172 |
REAL ftsoil(klon, nsoilmx, nbsrf) |
173 |
REAL ytsoil(klon, nsoilmx) |
174 |
REAL qsol(klon) |
175 |
|
176 |
EXTERNAL clqh, clvent, coefkz, calbeta, cltrac |
177 |
|
178 |
REAL yts(klon), yrugos(klon), ypct(klon), yz0_new(klon) |
179 |
REAL yalb(klon) |
180 |
REAL yalblw(klon) |
181 |
REAL yu1(klon), yv1(klon) |
182 |
REAL ysnow(klon), yqsurf(klon), yagesno(klon), yqsol(klon) |
183 |
REAL yrain_f(klon), ysnow_f(klon) |
184 |
REAL ysollw(klon), ysolsw(klon), ysollwdown(klon) |
185 |
REAL yfder(klon), ytaux(klon), ytauy(klon) |
186 |
REAL yrugm(klon), yrads(klon), yrugoro(klon) |
187 |
|
188 |
REAL yfluxlat(klon) |
189 |
|
190 |
REAL y_d_ts(klon) |
191 |
REAL y_d_t(klon, klev), y_d_q(klon, klev) |
192 |
REAL y_d_u(klon, klev), y_d_v(klon, klev) |
193 |
REAL y_flux_t(klon, klev), y_flux_q(klon, klev) |
194 |
REAL y_flux_u(klon, klev), y_flux_v(klon, klev) |
195 |
REAL y_dflux_t(klon), y_dflux_q(klon) |
196 |
REAL ycoefh(klon, klev), ycoefm(klon, klev) |
197 |
REAL yu(klon, klev), yv(klon, klev) |
198 |
REAL yt(klon, klev), yq(klon, klev) |
199 |
REAL ypaprs(klon, klev+1), ypplay(klon, klev), ydelp(klon, klev) |
200 |
|
201 |
LOGICAL ok_nonloc |
202 |
PARAMETER (ok_nonloc=.FALSE.) |
203 |
REAL ycoefm0(klon, klev), ycoefh0(klon, klev) |
204 |
|
205 |
!IM 081204 hcl_Anne ? BEG |
206 |
REAL yzlay(klon, klev), yzlev(klon, klev+1), yteta(klon, klev) |
207 |
REAL ykmm(klon, klev+1), ykmn(klon, klev+1) |
208 |
REAL ykmq(klon, klev+1) |
209 |
REAL yq2(klon, klev+1), q2(klon, klev+1, nbsrf) |
210 |
REAL q2diag(klon, klev+1) |
211 |
!IM 081204 hcl_Anne ? END |
212 |
|
213 |
REAL u1lay(klon), v1lay(klon) |
214 |
REAL delp(klon, klev) |
215 |
INTEGER i, k, nsrf |
216 |
|
217 |
INTEGER ni(klon), knon, j |
218 |
! Introduction d'une variable "pourcentage potentiel" pour tenir compte |
219 |
! des eventuelles apparitions et/ou disparitions de la glace de mer |
220 |
REAL pctsrf_pot(klon, nbsrf) |
221 |
|
222 |
REAL zx_alf1, zx_alf2 !valeur ambiante par extrapola. |
223 |
|
224 |
! maf pour sorties IOISPL en cas de debugagage |
225 |
|
226 |
CHARACTER (80) cldebug |
227 |
SAVE cldebug |
228 |
CHARACTER (8) cl_surf(nbsrf) |
229 |
SAVE cl_surf |
230 |
INTEGER nhoridbg, nidbg |
231 |
SAVE nhoridbg, nidbg |
232 |
INTEGER ndexbg(iim*(jjm+1)) |
233 |
REAL zx_lon(iim, jjm+1), zx_lat(iim, jjm+1), zjulian |
234 |
REAL tabindx(klon) |
235 |
REAL debugtab(iim, jjm+1) |
236 |
LOGICAL first_appel |
237 |
SAVE first_appel |
238 |
DATA first_appel/ .TRUE./ |
239 |
LOGICAL :: debugindex = .FALSE. |
240 |
INTEGER idayref |
241 |
REAL t2m(klon, nbsrf), q2m(klon, nbsrf) |
242 |
REAL u10m(klon, nbsrf), v10m(klon, nbsrf) |
243 |
|
244 |
REAL yt2m(klon), yq2m(klon), yu10m(klon) |
245 |
REAL yustar(klon) |
246 |
! -- LOOP |
247 |
REAL yu10mx(klon) |
248 |
REAL yu10my(klon) |
249 |
REAL ywindsp(klon) |
250 |
! -- LOOP |
251 |
|
252 |
REAL yt10m(klon), yq10m(klon) |
253 |
!IM cf. AM : pbl, hbtm2 (Comme les autres diagnostics on cumule ds |
254 |
! physiq ce qui permet de sortir les grdeurs par sous surface) |
255 |
REAL pblh(klon, nbsrf) |
256 |
REAL plcl(klon, nbsrf) |
257 |
REAL capcl(klon, nbsrf) |
258 |
REAL oliqcl(klon, nbsrf) |
259 |
REAL cteicl(klon, nbsrf) |
260 |
REAL pblt(klon, nbsrf) |
261 |
REAL therm(klon, nbsrf) |
262 |
REAL trmb1(klon, nbsrf) |
263 |
REAL trmb2(klon, nbsrf) |
264 |
REAL trmb3(klon, nbsrf) |
265 |
REAL ypblh(klon) |
266 |
REAL ylcl(klon) |
267 |
REAL ycapcl(klon) |
268 |
REAL yoliqcl(klon) |
269 |
REAL ycteicl(klon) |
270 |
REAL ypblt(klon) |
271 |
REAL ytherm(klon) |
272 |
REAL ytrmb1(klon) |
273 |
REAL ytrmb2(klon) |
274 |
REAL ytrmb3(klon) |
275 |
REAL y_cd_h(klon), y_cd_m(klon) |
276 |
REAL uzon(klon), vmer(klon) |
277 |
REAL tair1(klon), qair1(klon), tairsol(klon) |
278 |
REAL psfce(klon), patm(klon) |
279 |
|
280 |
REAL qairsol(klon), zgeo1(klon) |
281 |
REAL rugo1(klon) |
282 |
|
283 |
! utiliser un jeu de fonctions simples |
284 |
LOGICAL zxli |
285 |
PARAMETER (zxli=.FALSE.) |
286 |
|
287 |
REAL zt, zqs, zdelta, zcor |
288 |
REAL t_coup |
289 |
PARAMETER (t_coup=273.15) |
290 |
|
291 |
CHARACTER (len=20) :: modname = 'clmain' |
292 |
LOGICAL check |
293 |
PARAMETER (check=.FALSE.) |
294 |
|
295 |
!------------------------------------------------------------ |
296 |
|
297 |
! initialisation Anne |
298 |
ytherm = 0. |
299 |
|
300 |
IF (check) THEN |
301 |
PRINT *, modname, ' klon=', klon |
302 |
END IF |
303 |
|
304 |
IF (debugindex .AND. first_appel) THEN |
305 |
first_appel = .FALSE. |
306 |
|
307 |
! initialisation sorties netcdf |
308 |
|
309 |
idayref = day_ini |
310 |
CALL ymds2ju(annee_ref, 1, idayref, 0.0, zjulian) |
311 |
CALL gr_fi_ecrit(1, klon, iim, jjm+1, rlon, zx_lon) |
312 |
DO i = 1, iim |
313 |
zx_lon(i, 1) = rlon(i+1) |
314 |
zx_lon(i, jjm+1) = rlon(i+1) |
315 |
END DO |
316 |
CALL gr_fi_ecrit(1, klon, iim, jjm+1, rlat, zx_lat) |
317 |
cldebug = 'sous_index' |
318 |
CALL histbeg_totreg(cldebug, zx_lon(:, 1), zx_lat(1, :), 1, & |
319 |
iim, 1, jjm+1, itau_phy, zjulian, dtime, nhoridbg, nidbg) |
320 |
! no vertical axis |
321 |
cl_surf(1) = 'ter' |
322 |
cl_surf(2) = 'lic' |
323 |
cl_surf(3) = 'oce' |
324 |
cl_surf(4) = 'sic' |
325 |
DO nsrf = 1, nbsrf |
326 |
CALL histdef(nidbg, cl_surf(nsrf), cl_surf(nsrf), '-', iim, jjm+1, & |
327 |
nhoridbg, 1, 1, 1, -99, 'inst', dtime, dtime) |
328 |
END DO |
329 |
CALL histend(nidbg) |
330 |
CALL histsync(nidbg) |
331 |
END IF |
332 |
|
333 |
DO k = 1, klev ! epaisseur de couche |
334 |
DO i = 1, klon |
335 |
delp(i, k) = paprs(i, k) - paprs(i, k+1) |
336 |
END DO |
337 |
END DO |
338 |
DO i = 1, klon ! vent de la premiere couche |
339 |
zx_alf1 = 1.0 |
340 |
zx_alf2 = 1.0 - zx_alf1 |
341 |
u1lay(i) = u(i, 1)*zx_alf1 + u(i, 2)*zx_alf2 |
342 |
v1lay(i) = v(i, 1)*zx_alf1 + v(i, 2)*zx_alf2 |
343 |
END DO |
344 |
|
345 |
! initialisation: |
346 |
|
347 |
DO i = 1, klon |
348 |
rugmer(i) = 0.0 |
349 |
cdragh(i) = 0.0 |
350 |
cdragm(i) = 0.0 |
351 |
dflux_t(i) = 0.0 |
352 |
dflux_q(i) = 0.0 |
353 |
zu1(i) = 0.0 |
354 |
zv1(i) = 0.0 |
355 |
END DO |
356 |
ypct = 0.0 |
357 |
yts = 0.0 |
358 |
ysnow = 0.0 |
359 |
yqsurf = 0.0 |
360 |
yalb = 0.0 |
361 |
yalblw = 0.0 |
362 |
yrain_f = 0.0 |
363 |
ysnow_f = 0.0 |
364 |
yfder = 0.0 |
365 |
ytaux = 0.0 |
366 |
ytauy = 0.0 |
367 |
ysolsw = 0.0 |
368 |
ysollw = 0.0 |
369 |
ysollwdown = 0.0 |
370 |
yrugos = 0.0 |
371 |
yu1 = 0.0 |
372 |
yv1 = 0.0 |
373 |
yrads = 0.0 |
374 |
ypaprs = 0.0 |
375 |
ypplay = 0.0 |
376 |
ydelp = 0.0 |
377 |
yu = 0.0 |
378 |
yv = 0.0 |
379 |
yt = 0.0 |
380 |
yq = 0.0 |
381 |
pctsrf_new = 0.0 |
382 |
y_flux_u = 0.0 |
383 |
y_flux_v = 0.0 |
384 |
!$$ PB |
385 |
y_dflux_t = 0.0 |
386 |
y_dflux_q = 0.0 |
387 |
ytsoil = 999999. |
388 |
yrugoro = 0. |
389 |
! -- LOOP |
390 |
yu10mx = 0.0 |
391 |
yu10my = 0.0 |
392 |
ywindsp = 0.0 |
393 |
! -- LOOP |
394 |
DO nsrf = 1, nbsrf |
395 |
DO i = 1, klon |
396 |
d_ts(i, nsrf) = 0.0 |
397 |
END DO |
398 |
END DO |
399 |
!§§§ PB |
400 |
yfluxlat = 0. |
401 |
flux_t = 0. |
402 |
flux_q = 0. |
403 |
flux_u = 0. |
404 |
flux_v = 0. |
405 |
DO k = 1, klev |
406 |
DO i = 1, klon |
407 |
d_t(i, k) = 0.0 |
408 |
d_q(i, k) = 0.0 |
409 |
!$$$ flux_t(i, k) = 0.0 |
410 |
!$$$ flux_q(i, k) = 0.0 |
411 |
d_u(i, k) = 0.0 |
412 |
d_v(i, k) = 0.0 |
413 |
!$$$ flux_u(i, k) = 0.0 |
414 |
!$$$ flux_v(i, k) = 0.0 |
415 |
zcoefh(i, k) = 0.0 |
416 |
END DO |
417 |
END DO |
418 |
!AA IF (itr.GE.1) THEN |
419 |
!AA DO it = 1, itr |
420 |
!AA DO k = 1, klev |
421 |
!AA DO i = 1, klon |
422 |
!AA d_tr(i, k, it) = 0.0 |
423 |
!AA ENDDO |
424 |
!AA ENDDO |
425 |
!AA ENDDO |
426 |
!AA ENDIF |
427 |
|
428 |
|
429 |
! Boucler sur toutes les sous-fractions du sol: |
430 |
|
431 |
! Initialisation des "pourcentages potentiels". On considere ici qu'on |
432 |
! peut avoir potentiellementdela glace sur tout le domaine oceanique |
433 |
! (a affiner) |
434 |
|
435 |
pctsrf_pot = pctsrf |
436 |
pctsrf_pot(:, is_oce) = 1. - zmasq |
437 |
pctsrf_pot(:, is_sic) = 1. - zmasq |
438 |
|
439 |
DO nsrf = 1, nbsrf |
440 |
! chercher les indices: |
441 |
ni = 0 |
442 |
knon = 0 |
443 |
DO i = 1, klon |
444 |
! pour determiner le domaine a traiter on utilise les surfaces |
445 |
! "potentielles" |
446 |
IF (pctsrf_pot(i, nsrf) > epsfra) THEN |
447 |
knon = knon + 1 |
448 |
ni(knon) = i |
449 |
END IF |
450 |
END DO |
451 |
|
452 |
IF (check) THEN |
453 |
PRINT *, 'CLMAIN, nsrf, knon =', nsrf, knon |
454 |
END IF |
455 |
|
456 |
! variables pour avoir une sortie IOIPSL des INDEX |
457 |
IF (debugindex) THEN |
458 |
tabindx = 0. |
459 |
DO i = 1, knon |
460 |
tabindx(i) = real(i) |
461 |
END DO |
462 |
debugtab = 0. |
463 |
ndexbg = 0 |
464 |
CALL gath2cpl(tabindx, debugtab, klon, knon, iim, jjm, ni) |
465 |
CALL histwrite(nidbg, cl_surf(nsrf), itap, debugtab) |
466 |
END IF |
467 |
|
468 |
IF (knon==0) CYCLE |
469 |
|
470 |
DO j = 1, knon |
471 |
i = ni(j) |
472 |
ypct(j) = pctsrf(i, nsrf) |
473 |
yts(j) = ts(i, nsrf) |
474 |
ytslab(i) = tslab(i) |
475 |
ysnow(j) = snow(i, nsrf) |
476 |
yqsurf(j) = qsurf(i, nsrf) |
477 |
yalb(j) = albe(i, nsrf) |
478 |
yalblw(j) = alblw(i, nsrf) |
479 |
yrain_f(j) = rain_f(i) |
480 |
ysnow_f(j) = snow_f(i) |
481 |
yagesno(j) = agesno(i, nsrf) |
482 |
yfder(j) = fder(i) |
483 |
ytaux(j) = flux_u(i, 1, nsrf) |
484 |
ytauy(j) = flux_v(i, 1, nsrf) |
485 |
ysolsw(j) = solsw(i, nsrf) |
486 |
ysollw(j) = sollw(i, nsrf) |
487 |
ysollwdown(j) = sollwdown(i) |
488 |
yrugos(j) = rugos(i, nsrf) |
489 |
yrugoro(j) = rugoro(i) |
490 |
yu1(j) = u1lay(i) |
491 |
yv1(j) = v1lay(i) |
492 |
yrads(j) = ysolsw(j) + ysollw(j) |
493 |
ypaprs(j, klev+1) = paprs(i, klev+1) |
494 |
y_run_off_lic_0(j) = run_off_lic_0(i) |
495 |
yu10mx(j) = u10m(i, nsrf) |
496 |
yu10my(j) = v10m(i, nsrf) |
497 |
ywindsp(j) = sqrt(yu10mx(j)*yu10mx(j)+yu10my(j)*yu10my(j)) |
498 |
END DO |
499 |
|
500 |
! IF bucket model for continent, copy soil water content |
501 |
IF (nsrf==is_ter .AND. .NOT. ok_veget) THEN |
502 |
DO j = 1, knon |
503 |
i = ni(j) |
504 |
yqsol(j) = qsol(i) |
505 |
END DO |
506 |
ELSE |
507 |
yqsol = 0. |
508 |
END IF |
509 |
!$$$ PB ajour pour soil |
510 |
DO k = 1, nsoilmx |
511 |
DO j = 1, knon |
512 |
i = ni(j) |
513 |
ytsoil(j, k) = ftsoil(i, k, nsrf) |
514 |
END DO |
515 |
END DO |
516 |
DO k = 1, klev |
517 |
DO j = 1, knon |
518 |
i = ni(j) |
519 |
ypaprs(j, k) = paprs(i, k) |
520 |
ypplay(j, k) = pplay(i, k) |
521 |
ydelp(j, k) = delp(i, k) |
522 |
yu(j, k) = u(i, k) |
523 |
yv(j, k) = v(i, k) |
524 |
yt(j, k) = t(i, k) |
525 |
yq(j, k) = q(i, k) |
526 |
END DO |
527 |
END DO |
528 |
|
529 |
! calculer Cdrag et les coefficients d'echange |
530 |
CALL coefkz(nsrf, knon, ypaprs, ypplay, ksta, ksta_ter, yts,& |
531 |
yrugos, yu, yv, yt, yq, yqsurf, ycoefm, ycoefh) |
532 |
!IM 081204 BEG |
533 |
!CR test |
534 |
IF (iflag_pbl==1) THEN |
535 |
!IM 081204 END |
536 |
CALL coefkz2(nsrf, knon, ypaprs, ypplay, yt, ycoefm0, ycoefh0) |
537 |
DO k = 1, klev |
538 |
DO i = 1, knon |
539 |
ycoefm(i, k) = max(ycoefm(i, k), ycoefm0(i, k)) |
540 |
ycoefh(i, k) = max(ycoefh(i, k), ycoefh0(i, k)) |
541 |
END DO |
542 |
END DO |
543 |
END IF |
544 |
|
545 |
!IM cf JLD : on seuille ycoefm et ycoefh |
546 |
IF (nsrf==is_oce) THEN |
547 |
DO j = 1, knon |
548 |
! ycoefm(j, 1)=min(ycoefm(j, 1), 1.1E-3) |
549 |
ycoefm(j, 1) = min(ycoefm(j, 1), cdmmax) |
550 |
! ycoefh(j, 1)=min(ycoefh(j, 1), 1.1E-3) |
551 |
ycoefh(j, 1) = min(ycoefh(j, 1), cdhmax) |
552 |
END DO |
553 |
END IF |
554 |
|
555 |
|
556 |
!IM: 261103 |
557 |
IF (ok_kzmin) THEN |
558 |
!IM cf FH: 201103 BEG |
559 |
! Calcul d'une diffusion minimale pour les conditions tres stables. |
560 |
CALL coefkzmin(knon, ypaprs, ypplay, yu, yv, yt, yq, ycoefm, ycoefm0, & |
561 |
ycoefh0) |
562 |
! call dump2d(iim, jjm-1, ycoefm(2:klon-1, 2), 'KZ ') |
563 |
! call dump2d(iim, jjm-1, ycoefm0(2:klon-1, 2), 'KZMIN ') |
564 |
|
565 |
IF (1==1) THEN |
566 |
DO k = 1, klev |
567 |
DO i = 1, knon |
568 |
ycoefm(i, k) = max(ycoefm(i, k), ycoefm0(i, k)) |
569 |
ycoefh(i, k) = max(ycoefh(i, k), ycoefh0(i, k)) |
570 |
END DO |
571 |
END DO |
572 |
END IF |
573 |
!IM cf FH: 201103 END |
574 |
!IM: 261103 |
575 |
END IF !ok_kzmin |
576 |
|
577 |
IF (iflag_pbl>=3) THEN |
578 |
|
579 |
!ccccccccccccccccccccccccccccccccccccccccccccccccccccccccccccccccccccc |
580 |
! MELLOR ET YAMADA adapte a Mars Richard Fournier et Frederic Hourdin |
581 |
!ccccccccccccccccccccccccccccccccccccccccccccccccccccccccccccccccccc |
582 |
|
583 |
yzlay(1:knon, 1) = rd*yt(1:knon, 1)/(0.5*(ypaprs(1:knon, & |
584 |
1)+ypplay(1:knon, 1)))*(ypaprs(1:knon, 1)-ypplay(1:knon, 1))/rg |
585 |
DO k = 2, klev |
586 |
yzlay(1:knon, k) = yzlay(1:knon, k-1) & |
587 |
+ rd*0.5*(yt(1:knon, k-1) +yt(1: knon, k)) & |
588 |
/ ypaprs(1:knon, k) *(ypplay(1:knon, k-1)-ypplay(1:knon, k))/ & |
589 |
rg |
590 |
END DO |
591 |
DO k = 1, klev |
592 |
yteta(1:knon, k) = yt(1:knon, k)*(ypaprs(1:knon, 1) & |
593 |
/ ypplay(1:knon, k))**rkappa * (1.+0.61*yq(1:knon, k)) |
594 |
END DO |
595 |
yzlev(1:knon, 1) = 0. |
596 |
yzlev(1:knon, klev+1) = 2.*yzlay(1:knon, klev) - yzlay(1:knon, klev-1) |
597 |
DO k = 2, klev |
598 |
yzlev(1:knon, k) = 0.5*(yzlay(1:knon, k)+yzlay(1:knon, k-1)) |
599 |
END DO |
600 |
DO k = 1, klev + 1 |
601 |
DO j = 1, knon |
602 |
i = ni(j) |
603 |
yq2(j, k) = q2(i, k, nsrf) |
604 |
END DO |
605 |
END DO |
606 |
|
607 |
|
608 |
! Bug introduit volontairement pour converger avec les resultats |
609 |
! du papier sur les thermiques. |
610 |
IF (1==1) THEN |
611 |
y_cd_m(1:knon) = ycoefm(1:knon, 1) |
612 |
y_cd_h(1:knon) = ycoefh(1:knon, 1) |
613 |
ELSE |
614 |
y_cd_h(1:knon) = ycoefm(1:knon, 1) |
615 |
y_cd_m(1:knon) = ycoefh(1:knon, 1) |
616 |
END IF |
617 |
CALL ustarhb(knon, yu, yv, y_cd_m, yustar) |
618 |
|
619 |
IF (prt_level>9) THEN |
620 |
PRINT *, 'USTAR = ', yustar |
621 |
END IF |
622 |
|
623 |
! iflag_pbl peut etre utilise comme longuer de melange |
624 |
|
625 |
IF (iflag_pbl>=11) THEN |
626 |
CALL vdif_kcay(knon, dtime, rg, rd, ypaprs, yt, yzlev, yzlay, yu, yv, yteta, & |
627 |
y_cd_m, yq2, q2diag, ykmm, ykmn, yustar, iflag_pbl) |
628 |
ELSE |
629 |
CALL yamada4(knon, dtime, rg, rd, ypaprs, yt, yzlev, yzlay, yu, yv, yteta, & |
630 |
y_cd_m, yq2, ykmm, ykmn, ykmq, yustar, iflag_pbl) |
631 |
END IF |
632 |
|
633 |
ycoefm(1:knon, 1) = y_cd_m(1:knon) |
634 |
ycoefh(1:knon, 1) = y_cd_h(1:knon) |
635 |
ycoefm(1:knon, 2:klev) = ykmm(1:knon, 2:klev) |
636 |
ycoefh(1:knon, 2:klev) = ykmn(1:knon, 2:klev) |
637 |
|
638 |
|
639 |
END IF |
640 |
|
641 |
!ccccccccccccccccccccccccccccccccccccccccccccccccccccccccccccccccccccc |
642 |
! calculer la diffusion des vitesses "u" et "v" |
643 |
!ccccccccccccccccccccccccccccccccccccccccccccccccccccccccccccccccccc |
644 |
|
645 |
CALL clvent(knon, dtime, yu1, yv1, ycoefm, yt, yu, ypaprs, ypplay, & |
646 |
ydelp, y_d_u, y_flux_u) |
647 |
CALL clvent(knon, dtime, yu1, yv1, ycoefm, yt, yv, ypaprs, ypplay, & |
648 |
ydelp, y_d_v, y_flux_v) |
649 |
|
650 |
! pour le couplage |
651 |
ytaux = y_flux_u(:, 1) |
652 |
ytauy = y_flux_v(:, 1) |
653 |
|
654 |
! FH modif sur le cdrag temperature |
655 |
!$$$PB : déplace dans clcdrag |
656 |
!$$$ do i=1, knon |
657 |
!$$$ ycoefh(i, 1)=ycoefm(i, 1)*0.8 |
658 |
!$$$ enddo |
659 |
|
660 |
! calculer la diffusion de "q" et de "h" |
661 |
CALL clqh(dtime, itap, date0, jour, debut, lafin, rlon, rlat,& |
662 |
cufi, cvfi, knon, nsrf, ni, pctsrf, soil_model, ytsoil,& |
663 |
yqsol, ok_veget, ocean, npas, nexca, rmu0, co2_ppm, yrugos,& |
664 |
yrugoro, yu1, yv1, ycoefh, yt, yq, yts, ypaprs, ypplay,& |
665 |
ydelp, yrads, yalb, yalblw, ysnow, yqsurf, yrain_f, ysnow_f, & |
666 |
yfder, ytaux, ytauy, ywindsp, ysollw, ysollwdown, ysolsw,& |
667 |
yfluxlat, pctsrf_new, yagesno, y_d_t, y_d_q, y_d_ts,& |
668 |
yz0_new, y_flux_t, y_flux_q, y_dflux_t, y_dflux_q,& |
669 |
y_fqcalving, y_ffonte, y_run_off_lic_0, y_flux_o, y_flux_g,& |
670 |
ytslab, y_seaice) |
671 |
|
672 |
! calculer la longueur de rugosite sur ocean |
673 |
yrugm = 0. |
674 |
IF (nsrf==is_oce) THEN |
675 |
DO j = 1, knon |
676 |
yrugm(j) = 0.018*ycoefm(j, 1)*(yu1(j)**2+yv1(j)**2)/rg + & |
677 |
0.11*14E-6/sqrt(ycoefm(j, 1)*(yu1(j)**2+yv1(j)**2)) |
678 |
yrugm(j) = max(1.5E-05, yrugm(j)) |
679 |
END DO |
680 |
END IF |
681 |
DO j = 1, knon |
682 |
y_dflux_t(j) = y_dflux_t(j)*ypct(j) |
683 |
y_dflux_q(j) = y_dflux_q(j)*ypct(j) |
684 |
yu1(j) = yu1(j)*ypct(j) |
685 |
yv1(j) = yv1(j)*ypct(j) |
686 |
END DO |
687 |
|
688 |
DO k = 1, klev |
689 |
DO j = 1, knon |
690 |
i = ni(j) |
691 |
ycoefh(j, k) = ycoefh(j, k)*ypct(j) |
692 |
ycoefm(j, k) = ycoefm(j, k)*ypct(j) |
693 |
y_d_t(j, k) = y_d_t(j, k)*ypct(j) |
694 |
y_d_q(j, k) = y_d_q(j, k)*ypct(j) |
695 |
!§§§ PB |
696 |
flux_t(i, k, nsrf) = y_flux_t(j, k) |
697 |
flux_q(i, k, nsrf) = y_flux_q(j, k) |
698 |
flux_u(i, k, nsrf) = y_flux_u(j, k) |
699 |
flux_v(i, k, nsrf) = y_flux_v(j, k) |
700 |
!$$$ PB y_flux_t(j, k) = y_flux_t(j, k) * ypct(j) |
701 |
!$$$ PB y_flux_q(j, k) = y_flux_q(j, k) * ypct(j) |
702 |
y_d_u(j, k) = y_d_u(j, k)*ypct(j) |
703 |
y_d_v(j, k) = y_d_v(j, k)*ypct(j) |
704 |
!$$$ PB y_flux_u(j, k) = y_flux_u(j, k) * ypct(j) |
705 |
!$$$ PB y_flux_v(j, k) = y_flux_v(j, k) * ypct(j) |
706 |
END DO |
707 |
END DO |
708 |
|
709 |
|
710 |
evap(:, nsrf) = -flux_q(:, 1, nsrf) |
711 |
|
712 |
albe(:, nsrf) = 0. |
713 |
alblw(:, nsrf) = 0. |
714 |
snow(:, nsrf) = 0. |
715 |
qsurf(:, nsrf) = 0. |
716 |
rugos(:, nsrf) = 0. |
717 |
fluxlat(:, nsrf) = 0. |
718 |
DO j = 1, knon |
719 |
i = ni(j) |
720 |
d_ts(i, nsrf) = y_d_ts(j) |
721 |
albe(i, nsrf) = yalb(j) |
722 |
alblw(i, nsrf) = yalblw(j) |
723 |
snow(i, nsrf) = ysnow(j) |
724 |
qsurf(i, nsrf) = yqsurf(j) |
725 |
rugos(i, nsrf) = yz0_new(j) |
726 |
fluxlat(i, nsrf) = yfluxlat(j) |
727 |
!$$$ pb rugmer(i) = yrugm(j) |
728 |
IF (nsrf==is_oce) THEN |
729 |
rugmer(i) = yrugm(j) |
730 |
rugos(i, nsrf) = yrugm(j) |
731 |
END IF |
732 |
!IM cf JLD ?? |
733 |
agesno(i, nsrf) = yagesno(j) |
734 |
fqcalving(i, nsrf) = y_fqcalving(j) |
735 |
ffonte(i, nsrf) = y_ffonte(j) |
736 |
cdragh(i) = cdragh(i) + ycoefh(j, 1) |
737 |
cdragm(i) = cdragm(i) + ycoefm(j, 1) |
738 |
dflux_t(i) = dflux_t(i) + y_dflux_t(j) |
739 |
dflux_q(i) = dflux_q(i) + y_dflux_q(j) |
740 |
zu1(i) = zu1(i) + yu1(j) |
741 |
zv1(i) = zv1(i) + yv1(j) |
742 |
END DO |
743 |
IF (nsrf==is_ter) THEN |
744 |
DO j = 1, knon |
745 |
i = ni(j) |
746 |
qsol(i) = yqsol(j) |
747 |
END DO |
748 |
END IF |
749 |
IF (nsrf==is_lic) THEN |
750 |
DO j = 1, knon |
751 |
i = ni(j) |
752 |
run_off_lic_0(i) = y_run_off_lic_0(j) |
753 |
END DO |
754 |
END IF |
755 |
!$$$ PB ajout pour soil |
756 |
ftsoil(:, :, nsrf) = 0. |
757 |
DO k = 1, nsoilmx |
758 |
DO j = 1, knon |
759 |
i = ni(j) |
760 |
ftsoil(i, k, nsrf) = ytsoil(j, k) |
761 |
END DO |
762 |
END DO |
763 |
|
764 |
DO j = 1, knon |
765 |
i = ni(j) |
766 |
DO k = 1, klev |
767 |
d_t(i, k) = d_t(i, k) + y_d_t(j, k) |
768 |
d_q(i, k) = d_q(i, k) + y_d_q(j, k) |
769 |
!$$$ PB flux_t(i, k) = flux_t(i, k) + y_flux_t(j, k) |
770 |
!$$$ flux_q(i, k) = flux_q(i, k) + y_flux_q(j, k) |
771 |
d_u(i, k) = d_u(i, k) + y_d_u(j, k) |
772 |
d_v(i, k) = d_v(i, k) + y_d_v(j, k) |
773 |
!$$$ PB flux_u(i, k) = flux_u(i, k) + y_flux_u(j, k) |
774 |
!$$$ flux_v(i, k) = flux_v(i, k) + y_flux_v(j, k) |
775 |
zcoefh(i, k) = zcoefh(i, k) + ycoefh(j, k) |
776 |
END DO |
777 |
END DO |
778 |
|
779 |
|
780 |
!cc diagnostic t, q a 2m et u, v a 10m |
781 |
|
782 |
DO j = 1, knon |
783 |
i = ni(j) |
784 |
uzon(j) = yu(j, 1) + y_d_u(j, 1) |
785 |
vmer(j) = yv(j, 1) + y_d_v(j, 1) |
786 |
tair1(j) = yt(j, 1) + y_d_t(j, 1) |
787 |
qair1(j) = yq(j, 1) + y_d_q(j, 1) |
788 |
zgeo1(j) = rd*tair1(j)/(0.5*(ypaprs(j, 1)+ypplay(j, & |
789 |
1)))*(ypaprs(j, 1)-ypplay(j, 1)) |
790 |
tairsol(j) = yts(j) + y_d_ts(j) |
791 |
rugo1(j) = yrugos(j) |
792 |
IF (nsrf==is_oce) THEN |
793 |
rugo1(j) = rugos(i, nsrf) |
794 |
END IF |
795 |
psfce(j) = ypaprs(j, 1) |
796 |
patm(j) = ypplay(j, 1) |
797 |
|
798 |
qairsol(j) = yqsurf(j) |
799 |
END DO |
800 |
|
801 |
CALL stdlevvar(klon, knon, nsrf, zxli, uzon, vmer, tair1, qair1, zgeo1, & |
802 |
tairsol, qairsol, rugo1, psfce, patm, yt2m, yq2m, yt10m, yq10m, & |
803 |
yu10m, yustar) |
804 |
!IM 081204 END |
805 |
|
806 |
DO j = 1, knon |
807 |
i = ni(j) |
808 |
t2m(i, nsrf) = yt2m(j) |
809 |
q2m(i, nsrf) = yq2m(j) |
810 |
|
811 |
! u10m, v10m : composantes du vent a 10m sans spirale de Ekman |
812 |
u10m(i, nsrf) = (yu10m(j)*uzon(j))/sqrt(uzon(j)**2+vmer(j)**2) |
813 |
v10m(i, nsrf) = (yu10m(j)*vmer(j))/sqrt(uzon(j)**2+vmer(j)**2) |
814 |
|
815 |
END DO |
816 |
|
817 |
!IM cf AM : pbl, HBTM |
818 |
DO i = 1, knon |
819 |
y_cd_h(i) = ycoefh(i, 1) |
820 |
y_cd_m(i) = ycoefm(i, 1) |
821 |
END DO |
822 |
! print*, 'appel hbtm2' |
823 |
CALL hbtm(knon, ypaprs, ypplay, yt2m, yt10m, yq2m, yq10m, yustar, y_flux_t, & |
824 |
y_flux_q, yu, yv, yt, yq, ypblh, ycapcl, yoliqcl, ycteicl, ypblt, ytherm, & |
825 |
ytrmb1, ytrmb2, ytrmb3, ylcl) |
826 |
! print*, 'fin hbtm2' |
827 |
|
828 |
DO j = 1, knon |
829 |
i = ni(j) |
830 |
pblh(i, nsrf) = ypblh(j) |
831 |
plcl(i, nsrf) = ylcl(j) |
832 |
capcl(i, nsrf) = ycapcl(j) |
833 |
oliqcl(i, nsrf) = yoliqcl(j) |
834 |
cteicl(i, nsrf) = ycteicl(j) |
835 |
pblt(i, nsrf) = ypblt(j) |
836 |
therm(i, nsrf) = ytherm(j) |
837 |
trmb1(i, nsrf) = ytrmb1(j) |
838 |
trmb2(i, nsrf) = ytrmb2(j) |
839 |
trmb3(i, nsrf) = ytrmb3(j) |
840 |
END DO |
841 |
|
842 |
|
843 |
DO j = 1, knon |
844 |
DO k = 1, klev + 1 |
845 |
i = ni(j) |
846 |
q2(i, k, nsrf) = yq2(j, k) |
847 |
END DO |
848 |
END DO |
849 |
!IM "slab" ocean |
850 |
IF (nsrf==is_oce) THEN |
851 |
DO j = 1, knon |
852 |
! on projette sur la grille globale |
853 |
i = ni(j) |
854 |
IF (pctsrf_new(i, is_oce)>epsfra) THEN |
855 |
flux_o(i) = y_flux_o(j) |
856 |
ELSE |
857 |
flux_o(i) = 0. |
858 |
END IF |
859 |
END DO |
860 |
END IF |
861 |
|
862 |
IF (nsrf==is_sic) THEN |
863 |
DO j = 1, knon |
864 |
i = ni(j) |
865 |
!IM 230604 on pondere lorsque l'on fait le bilan au sol : flux_g(i) = y_flux_g(j)*ypct(j) |
866 |
IF (pctsrf_new(i, is_sic)>epsfra) THEN |
867 |
flux_g(i) = y_flux_g(j) |
868 |
ELSE |
869 |
flux_g(i) = 0. |
870 |
END IF |
871 |
END DO |
872 |
|
873 |
END IF |
874 |
!nsrf.EQ.is_sic |
875 |
IF (ocean=='slab ') THEN |
876 |
IF (nsrf==is_oce) THEN |
877 |
tslab(1:klon) = ytslab(1:klon) |
878 |
seaice(1:klon) = y_seaice(1:klon) |
879 |
!nsrf |
880 |
END IF |
881 |
!OCEAN |
882 |
END IF |
883 |
END DO |
884 |
|
885 |
! On utilise les nouvelles surfaces |
886 |
! A rajouter: conservation de l'albedo |
887 |
|
888 |
rugos(:, is_oce) = rugmer |
889 |
pctsrf = pctsrf_new |
890 |
|
891 |
END SUBROUTINE clmain |