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, zu1, zv1, t2m, & |
12 |
q2m, u10m_srf, v10m_srf, pblh, capcl, oliqcl, cteicl, pblt, therm, & |
13 |
trmb1, 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 |
|
19 |
! 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 |
! Pour pouvoir extraire les coefficients d'\'echanges et le vent |
25 |
! dans la premi\`ere couche, trois champs ont \'et\'e cr\'e\'es : "ycoefh", |
26 |
! "zu1" et "zv1". Nous avons moyenn\'e les valeurs de ces trois |
27 |
! champs sur les quatre sous-surfaces du mod\`ele. |
28 |
|
29 |
use clqh_m, only: clqh |
30 |
use clvent_m, only: clvent |
31 |
use coefkz_m, only: coefkz |
32 |
use coefkzmin_m, only: coefkzmin |
33 |
USE conf_gcm_m, ONLY: prt_level, lmt_pas |
34 |
USE conf_phys_m, ONLY: iflag_pbl |
35 |
USE dimphy, ONLY: klev, klon, zmasq |
36 |
USE dimsoil, ONLY: nsoilmx |
37 |
use hbtm_m, only: hbtm |
38 |
USE indicesol, ONLY: epsfra, is_lic, is_oce, is_sic, is_ter, nbsrf |
39 |
USE interfoce_lim_m, ONLY: interfoce_lim |
40 |
use stdlevvar_m, only: stdlevvar |
41 |
USE suphec_m, ONLY: rd, rg, rkappa |
42 |
use time_phylmdz, only: itap |
43 |
use ustarhb_m, only: ustarhb |
44 |
use vdif_kcay_m, only: vdif_kcay |
45 |
use yamada4_m, only: yamada4 |
46 |
|
47 |
REAL, INTENT(IN):: dtime ! interval du temps (secondes) |
48 |
|
49 |
REAL, INTENT(inout):: pctsrf(klon, nbsrf) |
50 |
! tableau des pourcentages de surface de chaque maille |
51 |
|
52 |
REAL, INTENT(IN):: t(klon, klev) ! temperature (K) |
53 |
REAL, INTENT(IN):: q(klon, klev) ! vapeur d'eau (kg / kg) |
54 |
REAL, INTENT(IN):: u(klon, klev), v(klon, klev) ! vitesse |
55 |
INTEGER, INTENT(IN):: julien ! jour de l'annee en cours |
56 |
REAL, intent(in):: mu0(klon) ! cosinus de l'angle solaire zenithal |
57 |
REAL, INTENT(IN):: ftsol(:, :) ! (klon, nbsrf) temp\'erature du sol (en K) |
58 |
REAL, INTENT(IN):: cdmmax, cdhmax ! seuils cdrm, cdrh |
59 |
REAL, INTENT(IN):: ksta, ksta_ter |
60 |
LOGICAL, INTENT(IN):: ok_kzmin |
61 |
|
62 |
REAL, INTENT(inout):: ftsoil(klon, nsoilmx, nbsrf) |
63 |
! soil temperature of surface fraction |
64 |
|
65 |
REAL, INTENT(inout):: qsol(:) ! (klon) |
66 |
! column-density of water in soil, in kg m-2 |
67 |
|
68 |
REAL, INTENT(IN):: paprs(klon, klev + 1) ! pression a intercouche (Pa) |
69 |
REAL, INTENT(IN):: pplay(klon, klev) ! pression au milieu de couche (Pa) |
70 |
REAL, INTENT(inout):: fsnow(:, :) ! (klon, nbsrf) \'epaisseur neigeuse |
71 |
REAL qsurf(klon, nbsrf) |
72 |
REAL evap(klon, nbsrf) |
73 |
REAL, intent(inout):: falbe(klon, nbsrf) |
74 |
REAL, intent(out):: fluxlat(:, :) ! (klon, nbsrf) |
75 |
|
76 |
REAL, intent(in):: rain_fall(klon) |
77 |
! liquid water mass flux (kg / m2 / s), positive down |
78 |
|
79 |
REAL, intent(in):: snow_f(klon) |
80 |
! solid water mass flux (kg / m2 / s), positive down |
81 |
|
82 |
REAL, INTENT(IN):: fsolsw(klon, nbsrf), fsollw(klon, nbsrf) |
83 |
REAL, intent(inout):: frugs(klon, nbsrf) ! longueur de rugosit\'e (en m) |
84 |
real agesno(klon, nbsrf) |
85 |
REAL, INTENT(IN):: rugoro(klon) |
86 |
|
87 |
REAL d_t(klon, klev), d_q(klon, klev) |
88 |
! d_t------output-R- le changement pour "t" |
89 |
! d_q------output-R- le changement pour "q" |
90 |
|
91 |
REAL, intent(out):: d_u(klon, klev), d_v(klon, klev) |
92 |
! changement pour "u" et "v" |
93 |
|
94 |
REAL, intent(out):: d_ts(:, :) ! (klon, nbsrf) variation of ftsol |
95 |
|
96 |
REAL, intent(out):: flux_t(klon, nbsrf) |
97 |
! flux de chaleur sensible (Cp T) (W / m2) (orientation positive vers |
98 |
! le bas) à la surface |
99 |
|
100 |
REAL, intent(out):: flux_q(klon, nbsrf) |
101 |
! flux de vapeur d'eau (kg / m2 / s) à la surface |
102 |
|
103 |
REAL, intent(out):: flux_u(klon, nbsrf), flux_v(klon, nbsrf) |
104 |
! tension du vent à la surface, en Pa |
105 |
|
106 |
REAL, INTENT(out):: cdragh(klon), cdragm(klon) |
107 |
real q2(klon, klev + 1, nbsrf) |
108 |
|
109 |
REAL, INTENT(out):: dflux_t(klon), dflux_q(klon) |
110 |
! dflux_t derive du flux sensible |
111 |
! dflux_q derive du flux latent |
112 |
! IM "slab" ocean |
113 |
|
114 |
REAL, intent(out):: ycoefh(klon, klev) |
115 |
REAL, intent(out):: zu1(klon), zv1(klon) |
116 |
REAL, INTENT(inout):: t2m(klon, nbsrf), q2m(klon, nbsrf) |
117 |
|
118 |
REAL, INTENT(inout):: u10m_srf(:, :), v10m_srf(:, :) ! (klon, nbsrf) |
119 |
! composantes du vent \`a 10m sans spirale d'Ekman |
120 |
|
121 |
! Ionela Musat. Cf. Anne Mathieu : planetary boundary layer, hbtm. |
122 |
! Comme les autres diagnostics on cumule dans physiq ce qui permet |
123 |
! de sortir les grandeurs par sous-surface. |
124 |
REAL pblh(klon, nbsrf) ! height of planetary boundary layer |
125 |
REAL capcl(klon, nbsrf) |
126 |
REAL oliqcl(klon, nbsrf) |
127 |
REAL cteicl(klon, nbsrf) |
128 |
REAL, INTENT(inout):: pblt(klon, nbsrf) ! T au nveau HCL |
129 |
REAL therm(klon, nbsrf) |
130 |
REAL trmb1(klon, nbsrf) |
131 |
! trmb1-------deep_cape |
132 |
REAL trmb2(klon, nbsrf) |
133 |
! trmb2--------inhibition |
134 |
REAL trmb3(klon, nbsrf) |
135 |
! trmb3-------Point Omega |
136 |
REAL plcl(klon, nbsrf) |
137 |
REAL fqcalving(klon, nbsrf), ffonte(klon, nbsrf) |
138 |
! ffonte----Flux thermique utilise pour fondre la neige |
139 |
! fqcalving-Flux d'eau "perdue" par la surface et necessaire pour limiter la |
140 |
! hauteur de neige, en kg / m2 / s |
141 |
REAL run_off_lic_0(klon) |
142 |
|
143 |
! Local: |
144 |
|
145 |
LOGICAL:: firstcal = .true. |
146 |
|
147 |
! la nouvelle repartition des surfaces sortie de l'interface |
148 |
REAL, save:: pctsrf_new_oce(klon) |
149 |
REAL, save:: pctsrf_new_sic(klon) |
150 |
|
151 |
REAL y_fqcalving(klon), y_ffonte(klon) |
152 |
real y_run_off_lic_0(klon) |
153 |
REAL rugmer(klon) |
154 |
REAL ytsoil(klon, nsoilmx) |
155 |
REAL yts(klon), yrugos(klon), ypct(klon), yz0_new(klon) |
156 |
REAL yalb(klon) |
157 |
|
158 |
REAL u1lay(klon), v1lay(klon) ! vent dans la premi\`ere couche, pour |
159 |
! une sous-surface donnée |
160 |
|
161 |
REAL snow(klon), yqsurf(klon), yagesno(klon) |
162 |
real yqsol(klon) ! column-density of water in soil, in kg m-2 |
163 |
REAL yrain_f(klon) ! liquid water mass flux (kg / m2 / s), positive down |
164 |
REAL ysnow_f(klon) ! solid water mass flux (kg / m2 / s), positive down |
165 |
REAL yrugm(klon), yrads(klon), yrugoro(klon) |
166 |
REAL yfluxlat(klon) |
167 |
REAL y_d_ts(klon) |
168 |
REAL y_d_t(klon, klev), y_d_q(klon, klev) |
169 |
REAL y_d_u(klon, klev), y_d_v(klon, klev) |
170 |
REAL y_flux_t(klon), y_flux_q(klon) |
171 |
REAL y_flux_u(klon), y_flux_v(klon) |
172 |
REAL y_dflux_t(klon), y_dflux_q(klon) |
173 |
REAL coefh(klon, klev), coefm(klon, klev) |
174 |
REAL yu(klon, klev), yv(klon, klev) |
175 |
REAL yt(klon, klev), yq(klon, klev) |
176 |
REAL ypaprs(klon, klev + 1), ypplay(klon, klev), ydelp(klon, klev) |
177 |
|
178 |
REAL ycoefm0(klon, klev), ycoefh0(klon, klev) |
179 |
|
180 |
REAL yzlay(klon, klev), yzlev(klon, klev + 1), yteta(klon, klev) |
181 |
REAL ykmm(klon, klev + 1), ykmn(klon, klev + 1) |
182 |
REAL ykmq(klon, klev + 1) |
183 |
REAL yq2(klon, klev + 1) |
184 |
REAL q2diag(klon, klev + 1) |
185 |
|
186 |
REAL delp(klon, klev) |
187 |
INTEGER i, k, nsrf |
188 |
|
189 |
INTEGER ni(klon), knon, j |
190 |
|
191 |
REAL pctsrf_pot(klon, nbsrf) |
192 |
! "pourcentage potentiel" pour tenir compte des \'eventuelles |
193 |
! apparitions ou disparitions de la glace de mer |
194 |
|
195 |
REAL yt2m(klon), yq2m(klon), yu10m(klon) |
196 |
REAL yustar(klon) |
197 |
|
198 |
REAL yt10m(klon), yq10m(klon) |
199 |
REAL ypblh(klon) |
200 |
REAL ylcl(klon) |
201 |
REAL ycapcl(klon) |
202 |
REAL yoliqcl(klon) |
203 |
REAL ycteicl(klon) |
204 |
REAL ypblt(klon) |
205 |
REAL ytherm(klon) |
206 |
REAL ytrmb1(klon) |
207 |
REAL ytrmb2(klon) |
208 |
REAL ytrmb3(klon) |
209 |
REAL uzon(klon), vmer(klon) |
210 |
REAL tair1(klon), qair1(klon), tairsol(klon) |
211 |
REAL psfce(klon), patm(klon) |
212 |
|
213 |
REAL qairsol(klon), zgeo1(klon) |
214 |
REAL rugo1(klon) |
215 |
|
216 |
! utiliser un jeu de fonctions simples |
217 |
LOGICAL zxli |
218 |
PARAMETER (zxli=.FALSE.) |
219 |
|
220 |
!------------------------------------------------------------ |
221 |
|
222 |
ytherm = 0. |
223 |
|
224 |
DO k = 1, klev ! epaisseur de couche |
225 |
DO i = 1, klon |
226 |
delp(i, k) = paprs(i, k) - paprs(i, k + 1) |
227 |
END DO |
228 |
END DO |
229 |
|
230 |
! Initialization: |
231 |
rugmer = 0. |
232 |
cdragh = 0. |
233 |
cdragm = 0. |
234 |
dflux_t = 0. |
235 |
dflux_q = 0. |
236 |
zu1 = 0. |
237 |
zv1 = 0. |
238 |
ypct = 0. |
239 |
yqsurf = 0. |
240 |
yrain_f = 0. |
241 |
ysnow_f = 0. |
242 |
yrugos = 0. |
243 |
ypaprs = 0. |
244 |
ypplay = 0. |
245 |
ydelp = 0. |
246 |
yu = 0. |
247 |
yv = 0. |
248 |
yt = 0. |
249 |
yq = 0. |
250 |
y_dflux_t = 0. |
251 |
y_dflux_q = 0. |
252 |
yrugoro = 0. |
253 |
d_ts = 0. |
254 |
flux_t = 0. |
255 |
flux_q = 0. |
256 |
flux_u = 0. |
257 |
flux_v = 0. |
258 |
fluxlat = 0. |
259 |
d_t = 0. |
260 |
d_q = 0. |
261 |
d_u = 0. |
262 |
d_v = 0. |
263 |
ycoefh = 0. |
264 |
|
265 |
! Initialisation des "pourcentages potentiels". On consid\`ere ici qu'on |
266 |
! peut avoir potentiellement de la glace sur tout le domaine oc\'eanique |
267 |
! (\`a affiner) |
268 |
|
269 |
pctsrf_pot(:, is_ter) = pctsrf(:, is_ter) |
270 |
pctsrf_pot(:, is_lic) = pctsrf(:, is_lic) |
271 |
pctsrf_pot(:, is_oce) = 1. - zmasq |
272 |
pctsrf_pot(:, is_sic) = 1. - zmasq |
273 |
|
274 |
! Tester si c'est le moment de lire le fichier: |
275 |
if (mod(itap - 1, lmt_pas) == 0) then |
276 |
CALL interfoce_lim(julien, pctsrf_new_oce, pctsrf_new_sic) |
277 |
endif |
278 |
|
279 |
! Boucler sur toutes les sous-fractions du sol: |
280 |
|
281 |
loop_surface: DO nsrf = 1, nbsrf |
282 |
! Chercher les indices : |
283 |
ni = 0 |
284 |
knon = 0 |
285 |
DO i = 1, klon |
286 |
! Pour d\'eterminer le domaine \`a traiter, on utilise les surfaces |
287 |
! "potentielles" |
288 |
IF (pctsrf_pot(i, nsrf) > epsfra) THEN |
289 |
knon = knon + 1 |
290 |
ni(knon) = i |
291 |
END IF |
292 |
END DO |
293 |
|
294 |
if_knon: IF (knon /= 0) then |
295 |
DO j = 1, knon |
296 |
i = ni(j) |
297 |
ypct(j) = pctsrf(i, nsrf) |
298 |
yts(j) = ftsol(i, nsrf) |
299 |
snow(j) = fsnow(i, nsrf) |
300 |
yqsurf(j) = qsurf(i, nsrf) |
301 |
yalb(j) = falbe(i, nsrf) |
302 |
yrain_f(j) = rain_fall(i) |
303 |
ysnow_f(j) = snow_f(i) |
304 |
yagesno(j) = agesno(i, nsrf) |
305 |
yrugos(j) = frugs(i, nsrf) |
306 |
yrugoro(j) = rugoro(i) |
307 |
u1lay(j) = u(i, 1) |
308 |
v1lay(j) = v(i, 1) |
309 |
yrads(j) = fsolsw(i, nsrf) + fsollw(i, nsrf) |
310 |
ypaprs(j, klev + 1) = paprs(i, klev + 1) |
311 |
y_run_off_lic_0(j) = run_off_lic_0(i) |
312 |
END DO |
313 |
|
314 |
! For continent, copy soil water content |
315 |
IF (nsrf == is_ter) yqsol(:knon) = qsol(ni(:knon)) |
316 |
|
317 |
ytsoil(:knon, :) = ftsoil(ni(:knon), :, nsrf) |
318 |
|
319 |
DO k = 1, klev |
320 |
DO j = 1, knon |
321 |
i = ni(j) |
322 |
ypaprs(j, k) = paprs(i, k) |
323 |
ypplay(j, k) = pplay(i, k) |
324 |
ydelp(j, k) = delp(i, k) |
325 |
yu(j, k) = u(i, k) |
326 |
yv(j, k) = v(i, k) |
327 |
yt(j, k) = t(i, k) |
328 |
yq(j, k) = q(i, k) |
329 |
END DO |
330 |
END DO |
331 |
|
332 |
! calculer Cdrag et les coefficients d'echange |
333 |
CALL coefkz(nsrf, ypaprs, ypplay, ksta, ksta_ter, yts(:knon), & |
334 |
yrugos, yu, yv, yt, yq, yqsurf(:knon), coefm(:knon, :), & |
335 |
coefh(:knon, :)) |
336 |
IF (iflag_pbl == 1) THEN |
337 |
CALL coefkz2(nsrf, knon, ypaprs, ypplay, yt, ycoefm0, ycoefh0) |
338 |
coefm(:knon, :) = max(coefm(:knon, :), ycoefm0(:knon, :)) |
339 |
coefh(:knon, :) = max(coefh(:knon, :), ycoefh0(:knon, :)) |
340 |
END IF |
341 |
|
342 |
! on met un seuil pour coefm et coefh |
343 |
IF (nsrf == is_oce) THEN |
344 |
coefm(:knon, 1) = min(coefm(:knon, 1), cdmmax) |
345 |
coefh(:knon, 1) = min(coefh(:knon, 1), cdhmax) |
346 |
END IF |
347 |
|
348 |
IF (ok_kzmin) THEN |
349 |
! Calcul d'une diffusion minimale pour les conditions tres stables |
350 |
CALL coefkzmin(knon, ypaprs, ypplay, yu, yv, yt, yq, & |
351 |
coefm(:knon, 1), ycoefm0, ycoefh0) |
352 |
coefm(:knon, :) = max(coefm(:knon, :), ycoefm0(:knon, :)) |
353 |
coefh(:knon, :) = max(coefh(:knon, :), ycoefh0(:knon, :)) |
354 |
END IF |
355 |
|
356 |
IF (iflag_pbl >= 3) THEN |
357 |
! Mellor et Yamada adapt\'e \`a Mars, Richard Fournier et |
358 |
! Fr\'ed\'eric Hourdin |
359 |
yzlay(:knon, 1) = rd * yt(:knon, 1) / (0.5 * (ypaprs(:knon, 1) & |
360 |
+ ypplay(:knon, 1))) & |
361 |
* (ypaprs(:knon, 1) - ypplay(:knon, 1)) / rg |
362 |
DO k = 2, klev |
363 |
yzlay(1:knon, k) = yzlay(1:knon, k-1) & |
364 |
+ rd * 0.5 * (yt(1:knon, k-1) + yt(1:knon, k)) & |
365 |
/ ypaprs(1:knon, k) & |
366 |
* (ypplay(1:knon, k-1) - ypplay(1:knon, k)) / rg |
367 |
END DO |
368 |
DO k = 1, klev |
369 |
yteta(1:knon, k) = yt(1:knon, k) * (ypaprs(1:knon, 1) & |
370 |
/ ypplay(1:knon, k))**rkappa * (1. + 0.61 * yq(1:knon, k)) |
371 |
END DO |
372 |
yzlev(1:knon, 1) = 0. |
373 |
yzlev(:knon, klev + 1) = 2. * yzlay(:knon, klev) & |
374 |
- yzlay(:knon, klev - 1) |
375 |
DO k = 2, klev |
376 |
yzlev(1:knon, k) = 0.5 * (yzlay(1:knon, k) + yzlay(1:knon, k-1)) |
377 |
END DO |
378 |
DO k = 1, klev + 1 |
379 |
DO j = 1, knon |
380 |
i = ni(j) |
381 |
yq2(j, k) = q2(i, k, nsrf) |
382 |
END DO |
383 |
END DO |
384 |
|
385 |
CALL ustarhb(knon, yu, yv, coefm(:knon, 1), yustar) |
386 |
IF (prt_level > 9) PRINT *, 'USTAR = ', yustar |
387 |
|
388 |
! iflag_pbl peut \^etre utilis\'e comme longueur de m\'elange |
389 |
|
390 |
IF (iflag_pbl >= 11) THEN |
391 |
CALL vdif_kcay(knon, dtime, rg, ypaprs, yzlev, yzlay, yu, yv, & |
392 |
yteta, coefm(:knon, 1), yq2, q2diag, ykmm, ykmn, yustar, & |
393 |
iflag_pbl) |
394 |
ELSE |
395 |
CALL yamada4(knon, dtime, rg, yzlev, yzlay, yu, yv, yteta, & |
396 |
coefm(:knon, 1), yq2, ykmm, ykmn, ykmq, yustar, iflag_pbl) |
397 |
END IF |
398 |
|
399 |
coefm(:knon, 2:) = ykmm(:knon, 2:klev) |
400 |
coefh(:knon, 2:) = ykmn(:knon, 2:klev) |
401 |
END IF |
402 |
|
403 |
! calculer la diffusion des vitesses "u" et "v" |
404 |
CALL clvent(knon, dtime, u1lay(:knon), v1lay(:knon), & |
405 |
coefm(:knon, :), yt, yu, ypaprs, ypplay, ydelp, y_d_u, & |
406 |
y_flux_u(:knon)) |
407 |
CALL clvent(knon, dtime, u1lay(:knon), v1lay(:knon), & |
408 |
coefm(:knon, :), yt, yv, ypaprs, ypplay, ydelp, y_d_v, & |
409 |
y_flux_v(:knon)) |
410 |
|
411 |
! calculer la diffusion de "q" et de "h" |
412 |
CALL clqh(dtime, julien, firstcal, nsrf, ni(:knon), & |
413 |
ytsoil(:knon, :), yqsol(:knon), mu0, yrugos, yrugoro, & |
414 |
u1lay(:knon), v1lay(:knon), coefh(:knon, :), yt, yq, & |
415 |
yts(:knon), ypaprs, ypplay, ydelp, yrads(:knon), yalb(:knon), & |
416 |
snow(:knon), yqsurf, yrain_f, ysnow_f, yfluxlat(:knon), & |
417 |
pctsrf_new_sic, yagesno(:knon), y_d_t, y_d_q, y_d_ts(:knon), & |
418 |
yz0_new, y_flux_t(:knon), y_flux_q(:knon), y_dflux_t(:knon), & |
419 |
y_dflux_q(:knon), y_fqcalving, y_ffonte, y_run_off_lic_0) |
420 |
|
421 |
! calculer la longueur de rugosite sur ocean |
422 |
yrugm = 0. |
423 |
IF (nsrf == is_oce) THEN |
424 |
DO j = 1, knon |
425 |
yrugm(j) = 0.018 * coefm(j, 1) * (u1lay(j)**2 + v1lay(j)**2) & |
426 |
/ rg + 0.11 * 14E-6 & |
427 |
/ sqrt(coefm(j, 1) * (u1lay(j)**2 + v1lay(j)**2)) |
428 |
yrugm(j) = max(1.5E-05, yrugm(j)) |
429 |
END DO |
430 |
END IF |
431 |
DO j = 1, knon |
432 |
y_dflux_t(j) = y_dflux_t(j) * ypct(j) |
433 |
y_dflux_q(j) = y_dflux_q(j) * ypct(j) |
434 |
END DO |
435 |
|
436 |
DO k = 1, klev |
437 |
DO j = 1, knon |
438 |
i = ni(j) |
439 |
coefh(j, k) = coefh(j, k) * ypct(j) |
440 |
coefm(j, k) = coefm(j, k) * ypct(j) |
441 |
y_d_t(j, k) = y_d_t(j, k) * ypct(j) |
442 |
y_d_q(j, k) = y_d_q(j, k) * ypct(j) |
443 |
y_d_u(j, k) = y_d_u(j, k) * ypct(j) |
444 |
y_d_v(j, k) = y_d_v(j, k) * ypct(j) |
445 |
END DO |
446 |
END DO |
447 |
|
448 |
flux_t(ni(:knon), nsrf) = y_flux_t(:knon) |
449 |
flux_q(ni(:knon), nsrf) = y_flux_q(:knon) |
450 |
flux_u(ni(:knon), nsrf) = y_flux_u(:knon) |
451 |
flux_v(ni(:knon), nsrf) = y_flux_v(:knon) |
452 |
|
453 |
evap(:, nsrf) = -flux_q(:, nsrf) |
454 |
|
455 |
falbe(:, nsrf) = 0. |
456 |
fsnow(:, nsrf) = 0. |
457 |
qsurf(:, nsrf) = 0. |
458 |
frugs(:, nsrf) = 0. |
459 |
DO j = 1, knon |
460 |
i = ni(j) |
461 |
d_ts(i, nsrf) = y_d_ts(j) |
462 |
falbe(i, nsrf) = yalb(j) |
463 |
fsnow(i, nsrf) = snow(j) |
464 |
qsurf(i, nsrf) = yqsurf(j) |
465 |
frugs(i, nsrf) = yz0_new(j) |
466 |
fluxlat(i, nsrf) = yfluxlat(j) |
467 |
IF (nsrf == is_oce) THEN |
468 |
rugmer(i) = yrugm(j) |
469 |
frugs(i, nsrf) = yrugm(j) |
470 |
END IF |
471 |
agesno(i, nsrf) = yagesno(j) |
472 |
fqcalving(i, nsrf) = y_fqcalving(j) |
473 |
ffonte(i, nsrf) = y_ffonte(j) |
474 |
cdragh(i) = cdragh(i) + coefh(j, 1) |
475 |
cdragm(i) = cdragm(i) + coefm(j, 1) |
476 |
dflux_t(i) = dflux_t(i) + y_dflux_t(j) |
477 |
dflux_q(i) = dflux_q(i) + y_dflux_q(j) |
478 |
zu1(i) = zu1(i) + u1lay(j) * ypct(j) |
479 |
zv1(i) = zv1(i) + v1lay(j) * ypct(j) |
480 |
END DO |
481 |
IF (nsrf == is_ter) THEN |
482 |
qsol(ni(:knon)) = yqsol(:knon) |
483 |
else IF (nsrf == is_lic) THEN |
484 |
DO j = 1, knon |
485 |
i = ni(j) |
486 |
run_off_lic_0(i) = y_run_off_lic_0(j) |
487 |
END DO |
488 |
END IF |
489 |
|
490 |
ftsoil(:, :, nsrf) = 0. |
491 |
ftsoil(ni(:knon), :, nsrf) = ytsoil(:knon, :) |
492 |
|
493 |
DO j = 1, knon |
494 |
i = ni(j) |
495 |
DO k = 1, klev |
496 |
d_t(i, k) = d_t(i, k) + y_d_t(j, k) |
497 |
d_q(i, k) = d_q(i, k) + y_d_q(j, k) |
498 |
d_u(i, k) = d_u(i, k) + y_d_u(j, k) |
499 |
d_v(i, k) = d_v(i, k) + y_d_v(j, k) |
500 |
ycoefh(i, k) = ycoefh(i, k) + coefh(j, k) |
501 |
END DO |
502 |
END DO |
503 |
|
504 |
! diagnostic t, q a 2m et u, v a 10m |
505 |
|
506 |
DO j = 1, knon |
507 |
i = ni(j) |
508 |
uzon(j) = yu(j, 1) + y_d_u(j, 1) |
509 |
vmer(j) = yv(j, 1) + y_d_v(j, 1) |
510 |
tair1(j) = yt(j, 1) + y_d_t(j, 1) |
511 |
qair1(j) = yq(j, 1) + y_d_q(j, 1) |
512 |
zgeo1(j) = rd * tair1(j) / (0.5 * (ypaprs(j, 1) + ypplay(j, & |
513 |
1))) * (ypaprs(j, 1)-ypplay(j, 1)) |
514 |
tairsol(j) = yts(j) + y_d_ts(j) |
515 |
rugo1(j) = yrugos(j) |
516 |
IF (nsrf == is_oce) THEN |
517 |
rugo1(j) = frugs(i, nsrf) |
518 |
END IF |
519 |
psfce(j) = ypaprs(j, 1) |
520 |
patm(j) = ypplay(j, 1) |
521 |
|
522 |
qairsol(j) = yqsurf(j) |
523 |
END DO |
524 |
|
525 |
CALL stdlevvar(klon, knon, nsrf, zxli, uzon(:knon), vmer(:knon), & |
526 |
tair1, qair1, zgeo1, tairsol, qairsol, rugo1, psfce, patm, & |
527 |
yt2m, yq2m, yt10m, yq10m, yu10m, yustar) |
528 |
|
529 |
DO j = 1, knon |
530 |
i = ni(j) |
531 |
t2m(i, nsrf) = yt2m(j) |
532 |
q2m(i, nsrf) = yq2m(j) |
533 |
|
534 |
u10m_srf(i, nsrf) = (yu10m(j) * uzon(j)) & |
535 |
/ sqrt(uzon(j)**2 + vmer(j)**2) |
536 |
v10m_srf(i, nsrf) = (yu10m(j) * vmer(j)) & |
537 |
/ sqrt(uzon(j)**2 + vmer(j)**2) |
538 |
END DO |
539 |
|
540 |
CALL hbtm(ypaprs, ypplay, yt2m, yq2m, yustar, y_flux_t(:knon), & |
541 |
y_flux_q(:knon), yu, yv, yt, yq, ypblh(:knon), ycapcl, & |
542 |
yoliqcl, ycteicl, ypblt, ytherm, ytrmb1, ytrmb2, ytrmb3, ylcl) |
543 |
|
544 |
DO j = 1, knon |
545 |
i = ni(j) |
546 |
pblh(i, nsrf) = ypblh(j) |
547 |
plcl(i, nsrf) = ylcl(j) |
548 |
capcl(i, nsrf) = ycapcl(j) |
549 |
oliqcl(i, nsrf) = yoliqcl(j) |
550 |
cteicl(i, nsrf) = ycteicl(j) |
551 |
pblt(i, nsrf) = ypblt(j) |
552 |
therm(i, nsrf) = ytherm(j) |
553 |
trmb1(i, nsrf) = ytrmb1(j) |
554 |
trmb2(i, nsrf) = ytrmb2(j) |
555 |
trmb3(i, nsrf) = ytrmb3(j) |
556 |
END DO |
557 |
|
558 |
DO j = 1, knon |
559 |
DO k = 1, klev + 1 |
560 |
i = ni(j) |
561 |
q2(i, k, nsrf) = yq2(j, k) |
562 |
END DO |
563 |
END DO |
564 |
else |
565 |
fsnow(:, nsrf) = 0. |
566 |
end IF if_knon |
567 |
END DO loop_surface |
568 |
|
569 |
! On utilise les nouvelles surfaces |
570 |
frugs(:, is_oce) = rugmer |
571 |
pctsrf(:, is_oce) = pctsrf_new_oce |
572 |
pctsrf(:, is_sic) = pctsrf_new_sic |
573 |
|
574 |
firstcal = .false. |
575 |
|
576 |
END SUBROUTINE clmain |
577 |
|
578 |
end module clmain_m |