Directory: | ./ |
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File: | phys/soil.f90 |
Date: | 2022-01-11 19:19:34 |
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Lines: | 78 | 100 | 78.0% |
Branches: | 53 | 80 | 66.2% |
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1 | ! | ||
2 | ! $Header$ | ||
3 | ! | ||
4 | 911247 | SUBROUTINE soil(ptimestep, indice, knon, snow, ptsrf, qsol, & | |
5 | 1440 | lon, lat, ptsoil, pcapcal, pfluxgrd) | |
6 | |||
7 | USE dimphy | ||
8 | USE mod_phys_lmdz_para | ||
9 | USE indice_sol_mod | ||
10 | USE print_control_mod, ONLY: lunout | ||
11 | |||
12 | IMPLICIT NONE | ||
13 | |||
14 | !======================================================================= | ||
15 | ! | ||
16 | ! Auteur: Frederic Hourdin 30/01/92 | ||
17 | ! ------- | ||
18 | ! | ||
19 | ! Object: Computation of : the soil temperature evolution | ||
20 | ! ------- the surfacic heat capacity "Capcal" | ||
21 | ! the surface conduction flux pcapcal | ||
22 | ! | ||
23 | ! Update: 2021/07 : soil thermal inertia, formerly a constant value, | ||
24 | ! ------ can also be now a function of soil moisture (F Cheruy's idea) | ||
25 | ! depending on iflag_inertie, read from physiq.def via conf_phys_m.F90 | ||
26 | ! ("Stage L3" Eve Rebouillat, with E Vignon, A Sima, F Cheruy) | ||
27 | ! | ||
28 | ! Method: Implicit time integration | ||
29 | ! ------- | ||
30 | ! Consecutive ground temperatures are related by: | ||
31 | ! T(k+1) = C(k) + D(k)*T(k) (*) | ||
32 | ! The coefficients C and D are computed at the t-dt time-step. | ||
33 | ! Routine structure: | ||
34 | ! 1) C and D coefficients are computed from the old temperature | ||
35 | ! 2) new temperatures are computed using (*) | ||
36 | ! 3) C and D coefficients are computed from the new temperature | ||
37 | ! profile for the t+dt time-step | ||
38 | ! 4) the coefficients A and B are computed where the diffusive | ||
39 | ! fluxes at the t+dt time-step is given by | ||
40 | ! Fdiff = A + B Ts(t+dt) | ||
41 | ! or Fdiff = F0 + Capcal (Ts(t+dt)-Ts(t))/dt | ||
42 | ! with F0 = A + B (Ts(t)) | ||
43 | ! Capcal = B*dt | ||
44 | ! | ||
45 | ! Interface: | ||
46 | ! ---------- | ||
47 | ! | ||
48 | ! Arguments: | ||
49 | ! ---------- | ||
50 | ! ptimestep physical timestep (s) | ||
51 | ! indice sub-surface index | ||
52 | ! snow(klon) snow | ||
53 | ! ptsrf(klon) surface temperature at time-step t (K) | ||
54 | ! qsol(klon) soil moisture (kg/m2 or mm) | ||
55 | ! lon(klon) longitude in radian | ||
56 | ! lat(klon) latitude in radian | ||
57 | ! ptsoil(klon,nsoilmx) temperature inside the ground (K) | ||
58 | ! pcapcal(klon) surfacic specific heat (W*m-2*s*K-1) | ||
59 | ! pfluxgrd(klon) surface diffusive flux from ground (Wm-2) | ||
60 | ! | ||
61 | !======================================================================= | ||
62 | INCLUDE "YOMCST.h" | ||
63 | INCLUDE "dimsoil.h" | ||
64 | INCLUDE "comsoil.h" | ||
65 | !----------------------------------------------------------------------- | ||
66 | ! Arguments | ||
67 | ! --------- | ||
68 | REAL, INTENT(IN) :: ptimestep | ||
69 | INTEGER, INTENT(IN) :: indice, knon !, knindex | ||
70 | REAL, DIMENSION(klon), INTENT(IN) :: snow | ||
71 | REAL, DIMENSION(klon), INTENT(IN) :: ptsrf | ||
72 | REAL, DIMENSION(klon), INTENT(IN) :: qsol | ||
73 | REAL, DIMENSION(klon), INTENT(IN) :: lon | ||
74 | REAL, DIMENSION(klon), INTENT(IN) :: lat | ||
75 | |||
76 | REAL, DIMENSION(klon,nsoilmx), INTENT(INOUT) :: ptsoil | ||
77 | REAL, DIMENSION(klon), INTENT(OUT) :: pcapcal | ||
78 | REAL, DIMENSION(klon), INTENT(OUT) :: pfluxgrd | ||
79 | |||
80 | !----------------------------------------------------------------------- | ||
81 | ! Local variables | ||
82 | ! --------------- | ||
83 | INTEGER :: ig, jk, ierr | ||
84 | REAL :: min_period,dalph_soil | ||
85 | REAL, DIMENSION(nsoilmx) :: zdz2 | ||
86 | REAL :: z1s | ||
87 | 2880 | REAL, DIMENSION(klon) :: ztherm_i | |
88 | 2880 | REAL, DIMENSION(klon,nsoilmx,nbsrf) :: C_coef, D_coef | |
89 | |||
90 | ! Local saved variables | ||
91 | ! --------------------- | ||
92 | REAL, SAVE :: lambda | ||
93 | !$OMP THREADPRIVATE(lambda) | ||
94 | REAL, DIMENSION(nsoilmx), SAVE :: dz1, dz2 | ||
95 | !$OMP THREADPRIVATE(dz1,dz2) | ||
96 | LOGICAL, SAVE :: firstcall=.TRUE. | ||
97 | !$OMP THREADPRIVATE(firstcall) | ||
98 | |||
99 | !----------------------------------------------------------------------- | ||
100 | ! Depthts: | ||
101 | ! -------- | ||
102 | REAL fz,rk,fz1,rk1,rk2 | ||
103 | fz(rk)=fz1*(dalph_soil**rk-1.)/(dalph_soil-1.) | ||
104 | |||
105 | |||
106 | !----------------------------------------------------------------------- | ||
107 | ! Calculation of some constants | ||
108 | ! NB! These constants do not depend on the sub-surfaces | ||
109 | !----------------------------------------------------------------------- | ||
110 | |||
111 |
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1440 | IF (firstcall) THEN |
112 | !----------------------------------------------------------------------- | ||
113 | ! ground levels | ||
114 | ! grnd=z/l where l is the skin depth of the diurnal cycle: | ||
115 | !----------------------------------------------------------------------- | ||
116 | |||
117 | 1 | min_period=1800. ! en secondes | |
118 | 1 | dalph_soil=2. ! rapport entre les epaisseurs de 2 couches succ. | |
119 | !$OMP MASTER | ||
120 |
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1 | IF (is_mpi_root) THEN |
121 | 1 | OPEN(99,file='soil.def',status='old',form='formatted',iostat=ierr) | |
122 |
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1 | IF (ierr == 0) THEN ! Read file only if it exists |
123 | ✗ | READ(99,*) min_period | |
124 | ✗ | READ(99,*) dalph_soil | |
125 | ✗ | WRITE(lunout,*)'Discretization for the soil model' | |
126 | ✗ | WRITE(lunout,*)'First level e-folding depth',min_period, & | |
127 | ✗ | ' dalph',dalph_soil | |
128 | ✗ | CLOSE(99) | |
129 | END IF | ||
130 | ENDIF | ||
131 | !$OMP END MASTER | ||
132 | 1 | CALL bcast(min_period) | |
133 | 1 | CALL bcast(dalph_soil) | |
134 | |||
135 | ! la premiere couche represente un dixieme de cycle diurne | ||
136 | 1 | fz1=SQRT(min_period/3.14) | |
137 | |||
138 |
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12 | DO jk=1,nsoilmx |
139 | 11 | rk1=jk | |
140 | 11 | rk2=jk-1 | |
141 | 12 | dz2(jk)=fz(rk1)-fz(rk2) | |
142 | ENDDO | ||
143 |
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11 | DO jk=1,nsoilmx-1 |
144 | 10 | rk1=jk+.5 | |
145 | 10 | rk2=jk-.5 | |
146 | 11 | dz1(jk)=1./(fz(rk1)-fz(rk2)) | |
147 | ENDDO | ||
148 | 1 | lambda=fz(.5)*dz1(1) | |
149 | 1 | WRITE(lunout,*)'full layers, intermediate layers (seconds)' | |
150 |
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12 | DO jk=1,nsoilmx |
151 | 11 | rk=jk | |
152 | 11 | rk1=jk+.5 | |
153 | 11 | rk2=jk-.5 | |
154 | 11 | WRITE(lunout,*)'fz=', & | |
155 | 23 | fz(rk1)*fz(rk2)*3.14,fz(rk)*fz(rk)*3.14 | |
156 | ENDDO | ||
157 | |||
158 | 1 | firstcall =.FALSE. | |
159 | END IF | ||
160 | |||
161 | |||
162 | !----------------------------------------------------------------------- | ||
163 | ! Calcul de l'inertie thermique a partir de la variable rnat. | ||
164 | ! on initialise a inertie_sic meme au-dessus d'un point de mer au cas | ||
165 | ! ou le point de mer devienne point de glace au pas suivant | ||
166 | ! on corrige si on a un point de terre avec ou sans glace | ||
167 | ! | ||
168 | ! iophys can be used to write the ztherm_i variable in a phys.nc file | ||
169 | ! and check the results; to do so, add "CALL iophys_ini" in physiq_mod | ||
170 | ! and add knindex to the list of inputs in all the calls to soil.F90 | ||
171 | ! (and to soil.F90 itself !) | ||
172 | !----------------------------------------------------------------------- | ||
173 | |||
174 |
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1440 | IF (indice == is_sic) THEN |
175 |
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105315 | DO ig = 1, knon |
176 | 105315 | ztherm_i(ig) = inertie_sic | |
177 | ENDDO | ||
178 |
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480 | IF (iflag_sic == 0) THEN |
179 | ✗ | DO ig = 1, knon | |
180 | ✗ | IF (snow(ig) > 0.0) ztherm_i(ig) = inertie_sno | |
181 | ENDDO | ||
182 | ! Otherwise sea-ice keeps the same inertia, even when covered by snow | ||
183 | ENDIF | ||
184 | ! CALL iophys_ecrit_index('ztherm_sic', 1, 'ztherm_sic', 'USI', & | ||
185 | ! knon, knindex, ztherm_i) | ||
186 |
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960 | ELSE IF (indice == is_lic) THEN |
187 |
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73440 | DO ig = 1, knon |
188 | 72960 | ztherm_i(ig) = inertie_lic | |
189 |
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73440 | IF (snow(ig) > 0.0) ztherm_i(ig) = inertie_sno |
190 | ENDDO | ||
191 | ! CALL iophys_ecrit_index('ztherm_lic', 1, 'ztherm_lic', 'USI', & | ||
192 | ! knon, knindex, ztherm_i) | ||
193 |
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480 | ELSE IF (indice == is_ter) THEN |
194 | ! | ||
195 | ! La relation entre l'inertie thermique du sol et qsol change d'apres | ||
196 | ! iflag_inertie, defini dans physiq.def, et appele via comsoil.h | ||
197 | ! | ||
198 |
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248160 | DO ig = 1, knon |
199 | ! iflag_inertie=0 correspond au cas inertie=constant, comme avant | ||
200 |
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247680 | IF (iflag_inertie==0) THEN |
201 | 247680 | ztherm_i(ig) = inertie_sol | |
202 | ✗ | ELSE IF (iflag_inertie == 1) THEN | |
203 | ! I = a_qsol * qsol + b modele lineaire deduit d'une | ||
204 | ! regression lineaire I = a_mrsos * mrsos + b obtenue sur | ||
205 | ! sorties MO d'une simulation LMDZOR(CMIP6) sur l'annee 2000 | ||
206 | ! sur tous les points avec frac_snow=0 | ||
207 | ! Difference entre qsol et mrsos prise en compte par un | ||
208 | ! facteur d'echelle sur le coefficient directeur de regression: | ||
209 | ! fact = 35./150. = mrsos_max/qsol_max | ||
210 | ! et a_qsol = a_mrsos * fact (car a = dI/dHumidite) | ||
211 | ✗ | ztherm_i(ig) = 30.0 *35.0/150.0 *qsol(ig) +770.0 | |
212 | ! AS : pour qsol entre 0 - 150, on a I entre 770 - 1820 | ||
213 | ✗ | ELSE IF (iflag_inertie == 2) THEN | |
214 | ! deux regressions lineaires, sur les memes sorties, | ||
215 | ! distinguant le type de sol : sable ou autre (limons/argile) | ||
216 | ! Implementation simple : regression type "sable" seulement pour | ||
217 | ! Sahara, defini par une "boite" lat/lon (NB : en radians !! ) | ||
218 | ✗ | IF (lon(ig)>-0.35 .AND. lon(ig)<0.70 .AND. lat(ig)>0.17 .AND. lat(ig)<0.52) THEN | |
219 | ! Valeurs theoriquement entre 728 et 2373 ; qsol valeurs basses | ||
220 | ✗ | ztherm_i(ig) = 47. *35.0/150.0 *qsol(ig) +728. ! boite type "sable" pour Sahara | |
221 | ELSE | ||
222 | ! Valeurs theoriquement entre 550 et 1940 ; qsol valeurs moyennes et hautes | ||
223 | ✗ | ztherm_i(ig) = 41. *35.0/150.0 *qsol(ig) +505. | |
224 | ENDIF | ||
225 | ✗ | ELSE IF (iflag_inertie == 3) THEN | |
226 | ! AS : idee a tester : | ||
227 | ! si la relation doit etre une droite, | ||
228 | ! definissons-la en fonction des valeurs min et max de qsol (0:150), | ||
229 | ! et de l'inertie (900 : 2000 ou 2400 ; choix ici: 2000) | ||
230 | ! I = I_min + qsol * (I_max - I_min)/(qsol_max - qsol_min) | ||
231 | ✗ | ztherm_i(ig) = 900. + qsol(ig) * (2000. - 900.)/150. | |
232 | ELSE | ||
233 | ✗ | WRITE (lunout,*) "Le choix iflag_inertie = ",iflag_inertie," n'est pas defini. Veuillez choisir un entier entre 0 et 3" | |
234 | ENDIF | ||
235 | ! | ||
236 | ! Fin de l'introduction de la relation entre l'inertie thermique du sol et qsol | ||
237 | !------------------------------------------- | ||
238 | !AS : donc le moindre flocon de neige sur un point de grid | ||
239 | ! fait que l'inertie du point passe a la valeur pour neige ! | ||
240 |
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248160 | IF (snow(ig) > 0.0) ztherm_i(ig) = inertie_sno |
241 | |||
242 | ENDDO | ||
243 | ! CALL iophys_ecrit_index('ztherm_ter', 1, 'ztherm_ter', 'USI', & | ||
244 | ! knon, knindex, ztherm_i) | ||
245 | ✗ | ELSE IF (indice == is_oce) THEN | |
246 | ✗ | DO ig = 1, knon | |
247 | ! This is just in case, but SST should be used by the model anyway | ||
248 | ✗ | ztherm_i(ig) = inertie_sic | |
249 | ENDDO | ||
250 | ! CALL iophys_ecrit_index('ztherm_oce', 1, 'ztherm_oce', 'USI', & | ||
251 | ! knon, knindex, ztherm_i) | ||
252 | ELSE | ||
253 | ✗ | WRITE(lunout,*) "valeur d indice non prevue", indice | |
254 | ✗ | call abort_physic("soil", "", 1) | |
255 | ENDIF | ||
256 | |||
257 | |||
258 | !----------------------------------------------------------------------- | ||
259 | ! 1) | ||
260 | ! Calculation of Cgrf and Dgrd coefficients using soil temperature from | ||
261 | ! previous time step. | ||
262 | ! | ||
263 | ! These variables are recalculated on the local compressed grid instead | ||
264 | ! of saved in restart file. | ||
265 | !----------------------------------------------------------------------- | ||
266 |
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17280 | DO jk=1,nsoilmx |
267 | 17280 | zdz2(jk)=dz2(jk)/ptimestep | |
268 | ENDDO | ||
269 | |||
270 |
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426915 | DO ig=1,knon |
271 | 425475 | z1s = zdz2(nsoilmx)+dz1(nsoilmx-1) | |
272 | C_coef(ig,nsoilmx-1,indice)= & | ||
273 | 425475 | zdz2(nsoilmx)*ptsoil(ig,nsoilmx)/z1s | |
274 | 426915 | D_coef(ig,nsoilmx-1,indice)=dz1(nsoilmx-1)/z1s | |
275 | ENDDO | ||
276 | |||
277 |
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14400 | DO jk=nsoilmx-1,2,-1 |
278 |
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3843675 | DO ig=1,knon |
279 | z1s = 1./(zdz2(jk)+dz1(jk-1)+dz1(jk) & | ||
280 | 3829275 | *(1.-D_coef(ig,jk,indice))) | |
281 | C_coef(ig,jk-1,indice)= & | ||
282 | 3829275 | (ptsoil(ig,jk)*zdz2(jk)+dz1(jk)*C_coef(ig,jk,indice)) * z1s | |
283 | 3842235 | D_coef(ig,jk-1,indice)=dz1(jk-1)*z1s | |
284 | ENDDO | ||
285 | ENDDO | ||
286 | |||
287 | !----------------------------------------------------------------------- | ||
288 | ! 2) | ||
289 | ! Computation of the soil temperatures using the Cgrd and Dgrd | ||
290 | ! coefficient computed above | ||
291 | ! | ||
292 | !----------------------------------------------------------------------- | ||
293 | |||
294 | ! Surface temperature | ||
295 |
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426915 | DO ig=1,knon |
296 | ptsoil(ig,1)=(lambda*C_coef(ig,1,indice)+ptsrf(ig))/ & | ||
297 | 426915 | (lambda*(1.-D_coef(ig,1,indice))+1.) | |
298 | ENDDO | ||
299 | |||
300 | ! Other temperatures | ||
301 |
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15840 | DO jk=1,nsoilmx-1 |
302 |
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4270590 | DO ig=1,knon |
303 | ptsoil(ig,jk+1)=C_coef(ig,jk,indice)+D_coef(ig,jk,indice) & | ||
304 | 4269150 | *ptsoil(ig,jk) | |
305 | ENDDO | ||
306 | ENDDO | ||
307 | |||
308 |
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1440 | IF (indice == is_sic) THEN |
309 |
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105315 | DO ig = 1 , knon |
310 | 105315 | ptsoil(ig,nsoilmx) = RTT - 1.8 | |
311 | END DO | ||
312 | ENDIF | ||
313 | |||
314 | !----------------------------------------------------------------------- | ||
315 | ! 3) | ||
316 | ! Calculate the Cgrd and Dgrd coefficient corresponding to actual soil | ||
317 | ! temperature | ||
318 | !----------------------------------------------------------------------- | ||
319 |
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426915 | DO ig=1,knon |
320 | 425475 | z1s = zdz2(nsoilmx)+dz1(nsoilmx-1) | |
321 | 425475 | C_coef(ig,nsoilmx-1,indice) = zdz2(nsoilmx)*ptsoil(ig,nsoilmx)/z1s | |
322 | 426915 | D_coef(ig,nsoilmx-1,indice) = dz1(nsoilmx-1)/z1s | |
323 | ENDDO | ||
324 | |||
325 |
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14400 | DO jk=nsoilmx-1,2,-1 |
326 |
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3843675 | DO ig=1,knon |
327 | z1s = 1./(zdz2(jk)+dz1(jk-1)+dz1(jk) & | ||
328 | 3829275 | *(1.-D_coef(ig,jk,indice))) | |
329 | C_coef(ig,jk-1,indice) = & | ||
330 | 3829275 | (ptsoil(ig,jk)*zdz2(jk)+dz1(jk)*C_coef(ig,jk,indice)) * z1s | |
331 | 3842235 | D_coef(ig,jk-1,indice) = dz1(jk-1)*z1s | |
332 | ENDDO | ||
333 | ENDDO | ||
334 | |||
335 | !----------------------------------------------------------------------- | ||
336 | ! 4) | ||
337 | ! Computation of the surface diffusive flux from ground and | ||
338 | ! calorific capacity of the ground | ||
339 | !----------------------------------------------------------------------- | ||
340 |
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426915 | DO ig=1,knon |
341 | pfluxgrd(ig) = ztherm_i(ig)*dz1(1)* & | ||
342 | 425475 | (C_coef(ig,1,indice)+(D_coef(ig,1,indice)-1.)*ptsoil(ig,1)) | |
343 | pcapcal(ig) = ztherm_i(ig)* & | ||
344 | 425475 | (dz2(1)+ptimestep*(1.-D_coef(ig,1,indice))*dz1(1)) | |
345 | 425475 | z1s = lambda*(1.-D_coef(ig,1,indice))+1. | |
346 | 425475 | pcapcal(ig) = pcapcal(ig)/z1s | |
347 | pfluxgrd(ig) = pfluxgrd(ig) & | ||
348 | + pcapcal(ig) * (ptsoil(ig,1) * z1s & | ||
349 | - lambda * C_coef(ig,1,indice) & | ||
350 | - ptsrf(ig)) & | ||
351 | 426915 | /ptimestep | |
352 | ENDDO | ||
353 | |||
354 | 1440 | END SUBROUTINE soil | |
355 |