1 |
module clmain_m |
2 |
|
3 |
IMPLICIT NONE |
4 |
|
5 |
contains |
6 |
|
7 |
SUBROUTINE clmain(dtime, pctsrf, t, q, u, v, julien, mu0, ftsol, cdmmax, & |
8 |
cdhmax, ksta, ksta_ter, ok_kzmin, ftsoil, qsol, paprs, pplay, fsnow, & |
9 |
qsurf, evap, falbe, fluxlat, rain_fall, snow_f, fsolsw, fsollw, frugs, & |
10 |
agesno, rugoro, d_t, d_q, d_u, d_v, d_ts, flux_t, flux_q, flux_u, & |
11 |
flux_v, cdragh, cdragm, q2, dflux_t, dflux_q, ycoefh, t2m, q2m, & |
12 |
u10m_srf, v10m_srf, pblh, capcl, oliqcl, cteicl, pblt, therm, trmb1, & |
13 |
trmb2, trmb3, plcl, fqcalving, ffonte, run_off_lic_0) |
14 |
|
15 |
! From phylmd/clmain.F, version 1.6, 2005/11/16 14:47:19 |
16 |
! Author: Z. X. Li (LMD/CNRS), date: 1993/08/18 |
17 |
! Objet : interface de couche limite (diffusion verticale) |
18 |
|
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! Tout ce qui a trait aux traceurs est dans "phytrac". Le calcul |
20 |
! de la couche limite pour les traceurs se fait avec "cltrac" et |
21 |
! ne tient pas compte de la diff\'erentiation des sous-fractions |
22 |
! de sol. |
23 |
|
24 |
use clqh_m, only: clqh |
25 |
use clvent_m, only: clvent |
26 |
use coefkz_m, only: coefkz |
27 |
use coefkzmin_m, only: coefkzmin |
28 |
use coefkz2_m, only: coefkz2 |
29 |
USE conf_gcm_m, ONLY: lmt_pas |
30 |
USE conf_phys_m, ONLY: iflag_pbl |
31 |
USE dimphy, ONLY: klev, klon, zmasq |
32 |
USE dimsoil, ONLY: nsoilmx |
33 |
use hbtm_m, only: hbtm |
34 |
USE indicesol, ONLY: epsfra, is_lic, is_oce, is_sic, is_ter, nbsrf |
35 |
USE interfoce_lim_m, ONLY: interfoce_lim |
36 |
use stdlevvar_m, only: stdlevvar |
37 |
USE suphec_m, ONLY: rd, rg, rkappa |
38 |
use time_phylmdz, only: itap |
39 |
use ustarhb_m, only: ustarhb |
40 |
use yamada4_m, only: yamada4 |
41 |
|
42 |
REAL, INTENT(IN):: dtime ! interval du temps (secondes) |
43 |
|
44 |
REAL, INTENT(inout):: pctsrf(klon, nbsrf) |
45 |
! tableau des pourcentages de surface de chaque maille |
46 |
|
47 |
REAL, INTENT(IN):: t(klon, klev) ! temperature (K) |
48 |
REAL, INTENT(IN):: q(klon, klev) ! vapeur d'eau (kg / kg) |
49 |
REAL, INTENT(IN):: u(klon, klev), v(klon, klev) ! vitesse |
50 |
INTEGER, INTENT(IN):: julien ! jour de l'annee en cours |
51 |
REAL, intent(in):: mu0(klon) ! cosinus de l'angle solaire zenithal |
52 |
REAL, INTENT(IN):: ftsol(:, :) ! (klon, nbsrf) temp\'erature du sol (en K) |
53 |
REAL, INTENT(IN):: cdmmax, cdhmax ! seuils cdrm, cdrh |
54 |
REAL, INTENT(IN):: ksta, ksta_ter |
55 |
LOGICAL, INTENT(IN):: ok_kzmin |
56 |
|
57 |
REAL, INTENT(inout):: ftsoil(klon, nsoilmx, nbsrf) |
58 |
! soil temperature of surface fraction |
59 |
|
60 |
REAL, INTENT(inout):: qsol(:) ! (klon) |
61 |
! column-density of water in soil, in kg m-2 |
62 |
|
63 |
REAL, INTENT(IN):: paprs(klon, klev + 1) ! pression a intercouche (Pa) |
64 |
REAL, INTENT(IN):: pplay(klon, klev) ! pression au milieu de couche (Pa) |
65 |
REAL, INTENT(inout):: fsnow(:, :) ! (klon, nbsrf) \'epaisseur neigeuse |
66 |
REAL qsurf(klon, nbsrf) |
67 |
REAL evap(klon, nbsrf) |
68 |
REAL, intent(inout):: falbe(klon, nbsrf) |
69 |
REAL, intent(out):: fluxlat(:, :) ! (klon, nbsrf) |
70 |
|
71 |
REAL, intent(in):: rain_fall(klon) |
72 |
! liquid water mass flux (kg / m2 / s), positive down |
73 |
|
74 |
REAL, intent(in):: snow_f(klon) |
75 |
! solid water mass flux (kg / m2 / s), positive down |
76 |
|
77 |
REAL, INTENT(IN):: fsolsw(klon, nbsrf), fsollw(klon, nbsrf) |
78 |
REAL, intent(inout):: frugs(klon, nbsrf) ! longueur de rugosit\'e (en m) |
79 |
real agesno(klon, nbsrf) |
80 |
REAL, INTENT(IN):: rugoro(klon) |
81 |
|
82 |
REAL d_t(klon, klev), d_q(klon, klev) |
83 |
! d_t------output-R- le changement pour "t" |
84 |
! d_q------output-R- le changement pour "q" |
85 |
|
86 |
REAL, intent(out):: d_u(klon, klev), d_v(klon, klev) |
87 |
! changement pour "u" et "v" |
88 |
|
89 |
REAL, intent(out):: d_ts(:, :) ! (klon, nbsrf) variation of ftsol |
90 |
|
91 |
REAL, intent(out):: flux_t(klon, nbsrf) |
92 |
! flux de chaleur sensible (Cp T) (W / m2) (orientation positive vers |
93 |
! le bas) à la surface |
94 |
|
95 |
REAL, intent(out):: flux_q(klon, nbsrf) |
96 |
! flux de vapeur d'eau (kg / m2 / s) à la surface |
97 |
|
98 |
REAL, intent(out):: flux_u(klon, nbsrf), flux_v(klon, nbsrf) |
99 |
! tension du vent (flux turbulent de vent) à la surface, en Pa |
100 |
|
101 |
REAL, INTENT(out):: cdragh(klon), cdragm(klon) |
102 |
real q2(klon, klev + 1, nbsrf) |
103 |
|
104 |
REAL, INTENT(out):: dflux_t(klon), dflux_q(klon) |
105 |
! dflux_t derive du flux sensible |
106 |
! dflux_q derive du flux latent |
107 |
! IM "slab" ocean |
108 |
|
109 |
REAL, intent(out):: ycoefh(:, :) ! (klon, klev) |
110 |
! Pour pouvoir extraire les coefficients d'\'echange, le champ |
111 |
! "ycoefh" a \'et\'e cr\'e\'e. Nous avons moyenn\'e les valeurs de |
112 |
! ce champ sur les quatre sous-surfaces du mod\`ele. |
113 |
|
114 |
REAL, INTENT(inout):: t2m(klon, nbsrf), q2m(klon, nbsrf) |
115 |
|
116 |
REAL, INTENT(inout):: u10m_srf(:, :), v10m_srf(:, :) ! (klon, nbsrf) |
117 |
! composantes du vent \`a 10m sans spirale d'Ekman |
118 |
|
119 |
! Ionela Musat. Cf. Anne Mathieu : planetary boundary layer, hbtm. |
120 |
! Comme les autres diagnostics on cumule dans physiq ce qui permet |
121 |
! de sortir les grandeurs par sous-surface. |
122 |
REAL pblh(klon, nbsrf) ! height of planetary boundary layer |
123 |
REAL capcl(klon, nbsrf) |
124 |
REAL oliqcl(klon, nbsrf) |
125 |
REAL cteicl(klon, nbsrf) |
126 |
REAL, INTENT(inout):: pblt(klon, nbsrf) ! T au nveau HCL |
127 |
REAL therm(klon, nbsrf) |
128 |
REAL trmb1(klon, nbsrf) |
129 |
! trmb1-------deep_cape |
130 |
REAL trmb2(klon, nbsrf) |
131 |
! trmb2--------inhibition |
132 |
REAL trmb3(klon, nbsrf) |
133 |
! trmb3-------Point Omega |
134 |
REAL plcl(klon, nbsrf) |
135 |
REAL fqcalving(klon, nbsrf), ffonte(klon, nbsrf) |
136 |
! ffonte----Flux thermique utilise pour fondre la neige |
137 |
! fqcalving-Flux d'eau "perdue" par la surface et necessaire pour limiter la |
138 |
! hauteur de neige, en kg / m2 / s |
139 |
REAL run_off_lic_0(klon) |
140 |
|
141 |
! Local: |
142 |
|
143 |
LOGICAL:: firstcal = .true. |
144 |
|
145 |
! la nouvelle repartition des surfaces sortie de l'interface |
146 |
REAL, save:: pctsrf_new_oce(klon) |
147 |
REAL, save:: pctsrf_new_sic(klon) |
148 |
|
149 |
REAL y_fqcalving(klon), y_ffonte(klon) |
150 |
real y_run_off_lic_0(klon) |
151 |
REAL rugmer(klon) |
152 |
REAL ytsoil(klon, nsoilmx) |
153 |
REAL yts(klon), yrugos(klon), ypct(klon), yz0_new(klon) |
154 |
REAL yalb(klon) |
155 |
REAL snow(klon), yqsurf(klon), yagesno(klon) |
156 |
real yqsol(klon) ! column-density of water in soil, in kg m-2 |
157 |
REAL yrain_f(klon) ! liquid water mass flux (kg / m2 / s), positive down |
158 |
REAL ysnow_f(klon) ! solid water mass flux (kg / m2 / s), positive down |
159 |
REAL yrugm(klon), yrads(klon), yrugoro(klon) |
160 |
REAL yfluxlat(klon) |
161 |
REAL y_d_ts(klon) |
162 |
REAL y_d_t(klon, klev), y_d_q(klon, klev) |
163 |
REAL y_d_u(klon, klev), y_d_v(klon, klev) |
164 |
REAL y_flux_t(klon), y_flux_q(klon) |
165 |
REAL y_flux_u(klon), y_flux_v(klon) |
166 |
REAL y_dflux_t(klon), y_dflux_q(klon) |
167 |
REAL coefh(klon, 2:klev), coefm(klon, 2:klev) |
168 |
real ycdragh(klon), ycdragm(klon) |
169 |
REAL yu(klon, klev), yv(klon, klev) |
170 |
REAL yt(klon, klev), yq(klon, klev) |
171 |
REAL ypaprs(klon, klev + 1), ypplay(klon, klev), ydelp(klon, klev) |
172 |
REAL ycoefm0(klon, klev), ycoefh0(klon, klev) |
173 |
REAL yzlay(klon, klev), zlev(klon, klev + 1), yteta(klon, klev) |
174 |
REAL ykmm(klon, klev + 1), ykmn(klon, klev + 1) |
175 |
REAL yq2(klon, klev + 1) |
176 |
REAL delp(klon, klev) |
177 |
INTEGER i, k, nsrf |
178 |
INTEGER ni(klon), knon, j |
179 |
|
180 |
REAL pctsrf_pot(klon, nbsrf) |
181 |
! "pourcentage potentiel" pour tenir compte des \'eventuelles |
182 |
! apparitions ou disparitions de la glace de mer |
183 |
|
184 |
REAL yt2m(klon), yq2m(klon), wind10m(klon) |
185 |
REAL ustar(klon) |
186 |
|
187 |
REAL yt10m(klon), yq10m(klon) |
188 |
REAL ypblh(klon) |
189 |
REAL ylcl(klon) |
190 |
REAL ycapcl(klon) |
191 |
REAL yoliqcl(klon) |
192 |
REAL ycteicl(klon) |
193 |
REAL ypblt(klon) |
194 |
REAL ytherm(klon) |
195 |
REAL ytrmb1(klon) |
196 |
REAL ytrmb2(klon) |
197 |
REAL ytrmb3(klon) |
198 |
REAL u1(klon), v1(klon) |
199 |
REAL tair1(klon), qair1(klon), tairsol(klon) |
200 |
REAL psfce(klon), patm(klon) |
201 |
|
202 |
REAL qairsol(klon), zgeo1(klon) |
203 |
REAL rugo1(klon) |
204 |
|
205 |
!------------------------------------------------------------ |
206 |
|
207 |
ytherm = 0. |
208 |
|
209 |
DO k = 1, klev ! epaisseur de couche |
210 |
DO i = 1, klon |
211 |
delp(i, k) = paprs(i, k) - paprs(i, k + 1) |
212 |
END DO |
213 |
END DO |
214 |
|
215 |
! Initialization: |
216 |
rugmer = 0. |
217 |
cdragh = 0. |
218 |
cdragm = 0. |
219 |
dflux_t = 0. |
220 |
dflux_q = 0. |
221 |
ypct = 0. |
222 |
yqsurf = 0. |
223 |
yrain_f = 0. |
224 |
ysnow_f = 0. |
225 |
yrugos = 0. |
226 |
ypaprs = 0. |
227 |
ypplay = 0. |
228 |
ydelp = 0. |
229 |
yu = 0. |
230 |
yv = 0. |
231 |
yt = 0. |
232 |
yq = 0. |
233 |
y_dflux_t = 0. |
234 |
y_dflux_q = 0. |
235 |
yrugoro = 0. |
236 |
d_ts = 0. |
237 |
flux_t = 0. |
238 |
flux_q = 0. |
239 |
flux_u = 0. |
240 |
flux_v = 0. |
241 |
fluxlat = 0. |
242 |
d_t = 0. |
243 |
d_q = 0. |
244 |
d_u = 0. |
245 |
d_v = 0. |
246 |
ycoefh = 0. |
247 |
|
248 |
! Initialisation des "pourcentages potentiels". On consid\`ere ici qu'on |
249 |
! peut avoir potentiellement de la glace sur tout le domaine oc\'eanique |
250 |
! (\`a affiner) |
251 |
|
252 |
pctsrf_pot(:, is_ter) = pctsrf(:, is_ter) |
253 |
pctsrf_pot(:, is_lic) = pctsrf(:, is_lic) |
254 |
pctsrf_pot(:, is_oce) = 1. - zmasq |
255 |
pctsrf_pot(:, is_sic) = 1. - zmasq |
256 |
|
257 |
! Tester si c'est le moment de lire le fichier: |
258 |
if (mod(itap - 1, lmt_pas) == 0) then |
259 |
CALL interfoce_lim(julien, pctsrf_new_oce, pctsrf_new_sic) |
260 |
endif |
261 |
|
262 |
! Boucler sur toutes les sous-fractions du sol: |
263 |
|
264 |
loop_surface: DO nsrf = 1, nbsrf |
265 |
! Chercher les indices : |
266 |
ni = 0 |
267 |
knon = 0 |
268 |
DO i = 1, klon |
269 |
! Pour d\'eterminer le domaine \`a traiter, on utilise les surfaces |
270 |
! "potentielles" |
271 |
IF (pctsrf_pot(i, nsrf) > epsfra) THEN |
272 |
knon = knon + 1 |
273 |
ni(knon) = i |
274 |
END IF |
275 |
END DO |
276 |
|
277 |
if_knon: IF (knon /= 0) then |
278 |
DO j = 1, knon |
279 |
i = ni(j) |
280 |
ypct(j) = pctsrf(i, nsrf) |
281 |
yts(j) = ftsol(i, nsrf) |
282 |
snow(j) = fsnow(i, nsrf) |
283 |
yqsurf(j) = qsurf(i, nsrf) |
284 |
yalb(j) = falbe(i, nsrf) |
285 |
yrain_f(j) = rain_fall(i) |
286 |
ysnow_f(j) = snow_f(i) |
287 |
yagesno(j) = agesno(i, nsrf) |
288 |
yrugos(j) = frugs(i, nsrf) |
289 |
yrugoro(j) = rugoro(i) |
290 |
yrads(j) = fsolsw(i, nsrf) + fsollw(i, nsrf) |
291 |
ypaprs(j, klev + 1) = paprs(i, klev + 1) |
292 |
y_run_off_lic_0(j) = run_off_lic_0(i) |
293 |
END DO |
294 |
|
295 |
! For continent, copy soil water content |
296 |
IF (nsrf == is_ter) yqsol(:knon) = qsol(ni(:knon)) |
297 |
|
298 |
ytsoil(:knon, :) = ftsoil(ni(:knon), :, nsrf) |
299 |
|
300 |
DO k = 1, klev |
301 |
DO j = 1, knon |
302 |
i = ni(j) |
303 |
ypaprs(j, k) = paprs(i, k) |
304 |
ypplay(j, k) = pplay(i, k) |
305 |
ydelp(j, k) = delp(i, k) |
306 |
yu(j, k) = u(i, k) |
307 |
yv(j, k) = v(i, k) |
308 |
yt(j, k) = t(i, k) |
309 |
yq(j, k) = q(i, k) |
310 |
END DO |
311 |
END DO |
312 |
|
313 |
! calculer Cdrag et les coefficients d'echange |
314 |
CALL coefkz(nsrf, ypaprs, ypplay, ksta, ksta_ter, yts(:knon), & |
315 |
yrugos, yu, yv, yt, yq, yqsurf(:knon), coefm(:knon, :), & |
316 |
coefh(:knon, :), ycdragm(:knon), ycdragh(:knon)) |
317 |
|
318 |
IF (iflag_pbl == 1) THEN |
319 |
CALL coefkz2(nsrf, knon, ypaprs, ypplay, yt, ycoefm0(:knon, 2:), & |
320 |
ycoefh0(:knon, 2:)) |
321 |
ycoefm0(:knon, 1) = 0. |
322 |
ycoefh0(:knon, 1) = 0. |
323 |
coefm(:knon, :) = max(coefm(:knon, :), ycoefm0(:knon, 2:)) |
324 |
coefh(:knon, :) = max(coefh(:knon, :), ycoefh0(:knon, 2:)) |
325 |
ycdragm(:knon) = max(ycdragm(:knon), 0.) |
326 |
ycdragh(:knon) = max(ycdragh(:knon), 0.) |
327 |
END IF |
328 |
|
329 |
! on met un seuil pour ycdragm et ycdragh |
330 |
IF (nsrf == is_oce) THEN |
331 |
ycdragm(:knon) = min(ycdragm(:knon), cdmmax) |
332 |
ycdragh(:knon) = min(ycdragh(:knon), cdhmax) |
333 |
END IF |
334 |
|
335 |
IF (ok_kzmin) THEN |
336 |
! Calcul d'une diffusion minimale pour les conditions tres stables |
337 |
CALL coefkzmin(knon, ypaprs, ypplay, yu, yv, yt, yq, & |
338 |
ycdragm(:knon), ycoefh0(:knon, 2:)) |
339 |
ycoefm0(:knon, 2:) = ycoefh0(:knon, 2:) |
340 |
coefm(:knon, :) = max(coefm(:knon, :), ycoefm0(:knon, 2:)) |
341 |
coefh(:knon, :) = max(coefh(:knon, :), ycoefh0(:knon, 2:)) |
342 |
END IF |
343 |
|
344 |
IF (iflag_pbl >= 6) THEN |
345 |
! Mellor et Yamada adapt\'e \`a Mars, Richard Fournier et |
346 |
! Fr\'ed\'eric Hourdin |
347 |
yzlay(:knon, 1) = rd * yt(:knon, 1) / (0.5 * (ypaprs(:knon, 1) & |
348 |
+ ypplay(:knon, 1))) & |
349 |
* (ypaprs(:knon, 1) - ypplay(:knon, 1)) / rg |
350 |
|
351 |
DO k = 2, klev |
352 |
yzlay(:knon, k) = yzlay(:knon, k-1) & |
353 |
+ rd * 0.5 * (yt(1:knon, k-1) + yt(1:knon, k)) & |
354 |
/ ypaprs(1:knon, k) & |
355 |
* (ypplay(1:knon, k-1) - ypplay(1:knon, k)) / rg |
356 |
END DO |
357 |
|
358 |
DO k = 1, klev |
359 |
yteta(1:knon, k) = yt(1:knon, k) * (ypaprs(1:knon, 1) & |
360 |
/ ypplay(1:knon, k))**rkappa * (1. + 0.61 * yq(1:knon, k)) |
361 |
END DO |
362 |
|
363 |
zlev(:knon, 1) = 0. |
364 |
zlev(:knon, klev + 1) = 2. * yzlay(:knon, klev) & |
365 |
- yzlay(:knon, klev - 1) |
366 |
|
367 |
DO k = 2, klev |
368 |
zlev(:knon, k) = 0.5 * (yzlay(:knon, k) + yzlay(:knon, k-1)) |
369 |
END DO |
370 |
|
371 |
DO k = 1, klev + 1 |
372 |
DO j = 1, knon |
373 |
i = ni(j) |
374 |
yq2(j, k) = q2(i, k, nsrf) |
375 |
END DO |
376 |
END DO |
377 |
|
378 |
ustar(:knon) = ustarhb(yu(:knon, 1), yv(:knon, 1), ycdragm(:knon)) |
379 |
CALL yamada4(dtime, rg, zlev(:knon, :), yzlay(:knon, :), & |
380 |
yu(:knon, :), yv(:knon, :), yteta(:knon, :), yq2(:knon, :), & |
381 |
ykmm(:knon, :), ykmn(:knon, :), ustar(:knon)) |
382 |
coefm(:knon, :) = ykmm(:knon, 2:klev) |
383 |
coefh(:knon, :) = ykmn(:knon, 2:klev) |
384 |
END IF |
385 |
|
386 |
CALL clvent(dtime, yu(:knon, 1), yv(:knon, 1), coefm(:knon, :), & |
387 |
ycdragm(:knon), yt(:knon, :), yu(:knon, :), ypaprs(:knon, :), & |
388 |
ypplay(:knon, :), ydelp(:knon, :), y_d_u(:knon, :), & |
389 |
y_flux_u(:knon)) |
390 |
CALL clvent(dtime, yu(:knon, 1), yv(:knon, 1), coefm(:knon, :), & |
391 |
ycdragm(:knon), yt(:knon, :), yv(:knon, :), ypaprs(:knon, :), & |
392 |
ypplay(:knon, :), ydelp(:knon, :), y_d_v(:knon, :), & |
393 |
y_flux_v(:knon)) |
394 |
|
395 |
! calculer la diffusion de "q" et de "h" |
396 |
CALL clqh(dtime, julien, firstcal, nsrf, ni(:knon), & |
397 |
ytsoil(:knon, :), yqsol(:knon), mu0, yrugos, yrugoro, & |
398 |
yu(:knon, 1), yv(:knon, 1), coefh(:knon, :), ycdragh(:knon), & |
399 |
yt, yq, yts(:knon), ypaprs, ypplay, ydelp, yrads(:knon), & |
400 |
yalb(:knon), snow(:knon), yqsurf, yrain_f, ysnow_f, & |
401 |
yfluxlat(:knon), pctsrf_new_sic, yagesno(:knon), y_d_t, y_d_q, & |
402 |
y_d_ts(:knon), yz0_new, y_flux_t(:knon), y_flux_q(:knon), & |
403 |
y_dflux_t(:knon), y_dflux_q(:knon), y_fqcalving, y_ffonte, & |
404 |
y_run_off_lic_0) |
405 |
|
406 |
! calculer la longueur de rugosite sur ocean |
407 |
yrugm = 0. |
408 |
IF (nsrf == is_oce) THEN |
409 |
DO j = 1, knon |
410 |
yrugm(j) = 0.018 * ycdragm(j) * (yu(j, 1)**2 + yv(j, 1)**2) & |
411 |
/ rg + 0.11 * 14E-6 & |
412 |
/ sqrt(ycdragm(j) * (yu(j, 1)**2 + yv(j, 1)**2)) |
413 |
yrugm(j) = max(1.5E-05, yrugm(j)) |
414 |
END DO |
415 |
END IF |
416 |
DO j = 1, knon |
417 |
y_dflux_t(j) = y_dflux_t(j) * ypct(j) |
418 |
y_dflux_q(j) = y_dflux_q(j) * ypct(j) |
419 |
END DO |
420 |
|
421 |
DO k = 2, klev |
422 |
DO j = 1, knon |
423 |
i = ni(j) |
424 |
coefh(j, k) = coefh(j, k) * ypct(j) |
425 |
coefm(j, k) = coefm(j, k) * ypct(j) |
426 |
END DO |
427 |
END DO |
428 |
DO j = 1, knon |
429 |
i = ni(j) |
430 |
ycdragh(j) = ycdragh(j) * ypct(j) |
431 |
ycdragm(j) = ycdragm(j) * ypct(j) |
432 |
END DO |
433 |
DO k = 1, klev |
434 |
DO j = 1, knon |
435 |
i = ni(j) |
436 |
y_d_t(j, k) = y_d_t(j, k) * ypct(j) |
437 |
y_d_q(j, k) = y_d_q(j, k) * ypct(j) |
438 |
y_d_u(j, k) = y_d_u(j, k) * ypct(j) |
439 |
y_d_v(j, k) = y_d_v(j, k) * ypct(j) |
440 |
END DO |
441 |
END DO |
442 |
|
443 |
flux_t(ni(:knon), nsrf) = y_flux_t(:knon) |
444 |
flux_q(ni(:knon), nsrf) = y_flux_q(:knon) |
445 |
flux_u(ni(:knon), nsrf) = y_flux_u(:knon) |
446 |
flux_v(ni(:knon), nsrf) = y_flux_v(:knon) |
447 |
|
448 |
evap(:, nsrf) = -flux_q(:, nsrf) |
449 |
|
450 |
falbe(:, nsrf) = 0. |
451 |
fsnow(:, nsrf) = 0. |
452 |
qsurf(:, nsrf) = 0. |
453 |
frugs(:, nsrf) = 0. |
454 |
DO j = 1, knon |
455 |
i = ni(j) |
456 |
d_ts(i, nsrf) = y_d_ts(j) |
457 |
falbe(i, nsrf) = yalb(j) |
458 |
fsnow(i, nsrf) = snow(j) |
459 |
qsurf(i, nsrf) = yqsurf(j) |
460 |
frugs(i, nsrf) = yz0_new(j) |
461 |
fluxlat(i, nsrf) = yfluxlat(j) |
462 |
IF (nsrf == is_oce) THEN |
463 |
rugmer(i) = yrugm(j) |
464 |
frugs(i, nsrf) = yrugm(j) |
465 |
END IF |
466 |
agesno(i, nsrf) = yagesno(j) |
467 |
fqcalving(i, nsrf) = y_fqcalving(j) |
468 |
ffonte(i, nsrf) = y_ffonte(j) |
469 |
cdragh(i) = cdragh(i) + ycdragh(j) |
470 |
cdragm(i) = cdragm(i) + ycdragm(j) |
471 |
dflux_t(i) = dflux_t(i) + y_dflux_t(j) |
472 |
dflux_q(i) = dflux_q(i) + y_dflux_q(j) |
473 |
END DO |
474 |
IF (nsrf == is_ter) THEN |
475 |
qsol(ni(:knon)) = yqsol(:knon) |
476 |
else IF (nsrf == is_lic) THEN |
477 |
DO j = 1, knon |
478 |
i = ni(j) |
479 |
run_off_lic_0(i) = y_run_off_lic_0(j) |
480 |
END DO |
481 |
END IF |
482 |
|
483 |
ftsoil(:, :, nsrf) = 0. |
484 |
ftsoil(ni(:knon), :, nsrf) = ytsoil(:knon, :) |
485 |
|
486 |
DO j = 1, knon |
487 |
i = ni(j) |
488 |
DO k = 1, klev |
489 |
d_t(i, k) = d_t(i, k) + y_d_t(j, k) |
490 |
d_q(i, k) = d_q(i, k) + y_d_q(j, k) |
491 |
d_u(i, k) = d_u(i, k) + y_d_u(j, k) |
492 |
d_v(i, k) = d_v(i, k) + y_d_v(j, k) |
493 |
END DO |
494 |
END DO |
495 |
|
496 |
DO j = 1, knon |
497 |
i = ni(j) |
498 |
DO k = 2, klev |
499 |
ycoefh(i, k) = ycoefh(i, k) + coefh(j, k) |
500 |
END DO |
501 |
END DO |
502 |
|
503 |
DO j = 1, knon |
504 |
i = ni(j) |
505 |
ycoefh(i, 1) = ycoefh(i, 1) + ycdragh(j) |
506 |
END DO |
507 |
|
508 |
! diagnostic t, q a 2m et u, v a 10m |
509 |
|
510 |
DO j = 1, knon |
511 |
i = ni(j) |
512 |
u1(j) = yu(j, 1) + y_d_u(j, 1) |
513 |
v1(j) = yv(j, 1) + y_d_v(j, 1) |
514 |
tair1(j) = yt(j, 1) + y_d_t(j, 1) |
515 |
qair1(j) = yq(j, 1) + y_d_q(j, 1) |
516 |
zgeo1(j) = rd * tair1(j) / (0.5 * (ypaprs(j, 1) + ypplay(j, & |
517 |
1))) * (ypaprs(j, 1)-ypplay(j, 1)) |
518 |
tairsol(j) = yts(j) + y_d_ts(j) |
519 |
rugo1(j) = yrugos(j) |
520 |
IF (nsrf == is_oce) THEN |
521 |
rugo1(j) = frugs(i, nsrf) |
522 |
END IF |
523 |
psfce(j) = ypaprs(j, 1) |
524 |
patm(j) = ypplay(j, 1) |
525 |
|
526 |
qairsol(j) = yqsurf(j) |
527 |
END DO |
528 |
|
529 |
CALL stdlevvar(klon, knon, nsrf, u1(:knon), v1(:knon), tair1(:knon), & |
530 |
qair1, zgeo1, tairsol, qairsol, rugo1, psfce, patm, yt2m, & |
531 |
yq2m, yt10m, yq10m, wind10m(:knon), ustar) |
532 |
|
533 |
DO j = 1, knon |
534 |
i = ni(j) |
535 |
t2m(i, nsrf) = yt2m(j) |
536 |
q2m(i, nsrf) = yq2m(j) |
537 |
|
538 |
u10m_srf(i, nsrf) = (wind10m(j) * u1(j)) & |
539 |
/ sqrt(u1(j)**2 + v1(j)**2) |
540 |
v10m_srf(i, nsrf) = (wind10m(j) * v1(j)) & |
541 |
/ sqrt(u1(j)**2 + v1(j)**2) |
542 |
END DO |
543 |
|
544 |
CALL hbtm(ypaprs, ypplay, yt2m, yq2m, ustar(:knon), y_flux_t(:knon), & |
545 |
y_flux_q(:knon), yu, yv, yt, yq, ypblh(:knon), ycapcl, & |
546 |
yoliqcl, ycteicl, ypblt, ytherm, ytrmb1, ytrmb2, ytrmb3, ylcl) |
547 |
|
548 |
DO j = 1, knon |
549 |
i = ni(j) |
550 |
pblh(i, nsrf) = ypblh(j) |
551 |
plcl(i, nsrf) = ylcl(j) |
552 |
capcl(i, nsrf) = ycapcl(j) |
553 |
oliqcl(i, nsrf) = yoliqcl(j) |
554 |
cteicl(i, nsrf) = ycteicl(j) |
555 |
pblt(i, nsrf) = ypblt(j) |
556 |
therm(i, nsrf) = ytherm(j) |
557 |
trmb1(i, nsrf) = ytrmb1(j) |
558 |
trmb2(i, nsrf) = ytrmb2(j) |
559 |
trmb3(i, nsrf) = ytrmb3(j) |
560 |
END DO |
561 |
|
562 |
DO j = 1, knon |
563 |
DO k = 1, klev + 1 |
564 |
i = ni(j) |
565 |
q2(i, k, nsrf) = yq2(j, k) |
566 |
END DO |
567 |
END DO |
568 |
else |
569 |
fsnow(:, nsrf) = 0. |
570 |
end IF if_knon |
571 |
END DO loop_surface |
572 |
|
573 |
! On utilise les nouvelles surfaces |
574 |
frugs(:, is_oce) = rugmer |
575 |
pctsrf(:, is_oce) = pctsrf_new_oce |
576 |
pctsrf(:, is_sic) = pctsrf_new_sic |
577 |
|
578 |
firstcal = .false. |
579 |
|
580 |
END SUBROUTINE clmain |
581 |
|
582 |
end module clmain_m |