Changeset 1092 for LMDZ4/branches/LMDZ4-dev
- Timestamp:
- Feb 3, 2009, 11:26:58 AM (16 years ago)
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- 1 edited
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LMDZ4/branches/LMDZ4-dev/libf/phylmd/newmicro.F (modified) (2 diffs)
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LMDZ4/branches/LMDZ4-dev/libf/phylmd/newmicro.F
r766 r1092 110 110 REAL zclear(klon) 111 111 REAL zcloud(klon) 112 113 c ************************** 114 c * * 115 c * DEBUT PARTIE OPTIMISEE * 116 c * * 117 c ************************** 118 119 REAL diff_paprs(klon, klev), zfice1, zfice2(klon, klev) 120 REAL rad_chaud_tab(klon, klev), zflwp_var, zfiwp_var 121 112 122 c 113 123 c Calculer l'epaisseur optique et l'emmissivite des nuages 114 124 c 115 cIM inversion des DO 116 DO i = 1, klon 117 xflwp(i)=0. 118 xfiwp(i)=0. 119 cccccccccccc!CDIR NOVECTOR 125 c IM inversion des DO 126 xflwp = 0.d0 127 xfiwp = 0.d0 128 xflwc = 0.d0 129 xfiwc = 0.d0 130 120 131 DO k = 1, klev 121 c 122 xflwc(i,k)=0. 123 xfiwc(i,k)=0. 124 c 125 rad_chaud = rad_chau1 126 IF (k.LE.3) rad_chaud = rad_chau2 127 pclc(i,k) = MAX(pclc(i,k), seuil_neb) 128 zflwp(i) = 1000.*pqlwp(i,k)/RG/pclc(i,k) 129 . *(paprs(i,k)-paprs(i,k+1)) 130 zfice = 1.0 - (t(i,k)-t_glace) / (273.13-t_glace) 131 zfice = MIN(MAX(zfice,0.0),1.0) 132 zfice = zfice**nexpo 133 radius = rad_chaud * (1.-zfice) + rad_froid * zfice 134 coef = coef_chau * (1.-zfice) + coef_froi * zfice 135 pcltau(i,k) = 3.0/2.0 * zflwp(i) / radius 136 pclemi(i,k) = 1.0 - EXP( - coef * zflwp(i)) 137 138 if (ok_newmicro) then 139 140 c -- liquid/ice cloud water paths: 141 142 zfice = 1.0 - (t(i,k)-t_glace) / (273.13-t_glace) 143 zfice = MIN(MAX(zfice,0.0),1.0) 144 145 zflwp(i) = 1000.*(1.-zfice)*pqlwp(i,k)/pclc(i,k) 146 : *(paprs(i,k)-paprs(i,k+1))/RG 147 zfiwp(i) = 1000.*zfice*pqlwp(i,k)/pclc(i,k) 148 : *(paprs(i,k)-paprs(i,k+1))/RG 149 150 xflwp(i) = xflwp(i)+ (1.-zfice)*pqlwp(i,k) 151 : *(paprs(i,k)-paprs(i,k+1))/RG 152 xfiwp(i) = xfiwp(i)+ zfice*pqlwp(i,k) 153 : *(paprs(i,k)-paprs(i,k+1))/RG 154 155 cIM Total Liquid/Ice water content 156 xflwc(i,k) = xflwc(i,k)+(1.-zfice)*pqlwp(i,k) 157 xfiwc(i,k) = xfiwc(i,k)+zfice*pqlwp(i,k) 158 cIM In-Cloud Liquid/Ice water content 159 c xflwc(i,k) = xflwc(i,k)+(1.-zfice)*pqlwp(i,k)/pclc(i,k) 160 c xfiwc(i,k) = xfiwc(i,k)+zfice*pqlwp(i,k)/pclc(i,k) 161 162 c -- effective cloud droplet radius (microns): 163 164 c for liquid water clouds: 132 DO i = 1, klon 133 diff_paprs(i,k) = (paprs(i,k)-paprs(i,k+1))/RG 134 ENDDO 135 ENDDO 136 137 IF (ok_newmicro) THEN 138 139 140 DO k = 1, klev 141 DO i = 1, klon 142 zfice2(i,k) = 1.0 - (t(i,k)-t_glace) / (273.13-t_glace) 143 zfice2(i,k) = MIN(MAX(zfice2(i,k),0.0),1.0) 144 c IM Total Liquid/Ice water content 145 xflwc(i,k) = (1.-zfice2(i,k))*pqlwp(i,k) 146 xfiwc(i,k) = zfice2(i,k)*pqlwp(i,k) 147 c IM In-Cloud Liquid/Ice water content 148 c xflwc(i,k) = xflwc(i,k)+(1.-zfice)*pqlwp(i,k)/pclc(i,k) 149 c xfiwc(i,k) = xfiwc(i,k)+zfice*pqlwp(i,k)/pclc(i,k) 150 ENDDO 151 ENDDO 152 165 153 IF (ok_aie) THEN 166 ! Formula "D" of Boucher and Lohmann, Tellus, 1995 167 ! 168 cdnc(i,k) = 10.**(bl95_b0+bl95_b1* 169 . log(MAX(sulfate(i,k),1.e-4))/log(10.))*1.e6 !-m-3 170 ! Cloud droplet number concentration (CDNC) is restricted 171 ! to be within [20, 1000 cm^3] 172 ! 173 cdnc(i,k)=MIN(1000.e6,MAX(20.e6,cdnc(i,k))) 174 ! 175 ! 176 cdnc_pi(i,k) = 10.**(bl95_b0+bl95_b1* 177 . log(MAX(sulfate_pi(i,k),1.e-4))/log(10.))*1.e6 !-m-3 178 cdnc_pi(i,k)=MIN(1000.e6,MAX(20.e6,cdnc_pi(i,k))) 179 ! 180 ! 181 ! air density: pplay(i,k) / (RD * zT(i,k)) 182 ! factor 1.1: derive effective radius from volume-mean radius 183 ! factor 1000 is the water density 184 ! _chaud means that this is the CDR for liquid water clouds 185 ! 186 rad_chaud = 187 . 1.1 * ( (pqlwp(i,k) * pplay(i,k) / (RD * T(i,k)) ) 188 . / (4./3. * RPI * 1000. * cdnc(i,k)) )**(1./3.) 189 ! 190 ! Convert to um. CDR shall be at least 3 um. 191 ! 192 c rad_chaud = MAX(rad_chaud*1.e6, 3.) 193 rad_chaud = MAX(rad_chaud*1.e6, 5.) 194 195 ! Pre-industrial cloud opt thickness 196 ! 197 ! "radius" is calculated as rad_chaud above (plus the 198 ! ice cloud contribution) but using cdnc_pi instead of 199 ! cdnc. 200 radius = 201 . 1.1 * ( (pqlwp(i,k) * pplay(i,k) / (RD * T(i,k)) ) 202 . / (4./3. * RPI * 1000. * cdnc_pi(i,k)) )**(1./3.) 203 radius = MAX(radius*1.e6, 5.) 204 205 tc = t(i,k)-273.15 206 rei = 0.71*tc + 61.29 207 if (tc.le.-81.4) rei = 3.5 208 if (zflwp(i).eq.0.) radius = 1. 209 if (zfiwp(i).eq.0. .or. rei.le.0.) rei = 1. 210 cldtaupi(i,k) = 3.0/2.0 * zflwp(i) / radius 211 . + zfiwp(i) * (3.448e-03 + 2.431/rei) 212 ENDIF ! ok_aie 213 ! For output diagnostics 214 ! 215 ! Cloud droplet effective radius [um] 216 ! 217 ! we multiply here with f * xl (fraction of liquid water 218 ! clouds in the grid cell) to avoid problems in the 219 ! averaging of the output. 220 ! In the output of IOIPSL, derive the real cloud droplet 221 ! effective radius as re/fl 222 ! 223 fl(i,k) = pclc(i,k)*(1.-zfice) 224 re(i,k) = rad_chaud*fl(i,k) 225 226 c-jq end 154 DO k = 1, klev 155 DO i = 1, klon 156 ! Formula "D" of Boucher and Lohmann, Tellus, 1995 157 ! 158 cdnc(i,k) = 10.**(bl95_b0+bl95_b1* 159 & log(MAX(sulfate(i,k),1.e-4))/log(10.))*1.e6 !-m-3 160 ! Cloud droplet number concentration (CDNC) is restricted 161 ! to be within [20, 1000 cm^3] 162 ! 163 cdnc(i,k)=MIN(1000.e6,MAX(20.e6,cdnc(i,k))) 164 ! 165 ! 166 cdnc_pi(i,k) = 10.**(bl95_b0+bl95_b1* 167 & log(MAX(sulfate_pi(i,k),1.e-4))/log(10.))*1.e6 !-m-3 168 cdnc_pi(i,k)=MIN(1000.e6,MAX(20.e6,cdnc_pi(i,k))) 169 ENDDO 170 ENDDO 171 DO k = 1, klev 172 DO i = 1, klon 173 ! rad_chaud_tab(i,k) = 174 ! & MAX(1.1e6 175 ! & *((pqlwp(i,k)*pplay(i,k)/(RD * T(i,k))) 176 ! & /(4./3*RPI*1000.*cdnc(i,k)) )**(1./3.),5.) 177 rad_chaud_tab(i,k) = 178 & 1.1 179 & *((pqlwp(i,k)*pplay(i,k)/(RD * T(i,k))) 180 & /(4./3*RPI*1000.*cdnc(i,k)) )**(1./3.) 181 rad_chaud_tab(i,k) = MAX(rad_chaud_tab(i,k) * 1e6, 5.) 182 ENDDO 183 ENDDO 184 ELSE 185 DO k = 1, MIN(3,klev) 186 DO i = 1, klon 187 rad_chaud_tab(i,k) = rad_chau2 188 ENDDO 189 ENDDO 190 DO k = MIN(3,klev)+1, klev 191 DO i = 1, klon 192 rad_chaud_tab(i,k) = rad_chau1 193 ENDDO 194 ENDDO 195 196 ENDIF 227 197 228 rel = rad_chaud 229 c for ice clouds: as a function of the ambiant temperature 230 c [formula used by Iacobellis and Somerville (2000), with an 231 c asymptotical value of 3.5 microns at T<-81.4 C added to be 232 c consistent with observations of Heymsfield et al. 1986]: 233 tc = t(i,k)-273.15 234 rei = 0.71*tc + 61.29 235 if (tc.le.-81.4) rei = 3.5 236 237 c -- cloud optical thickness : 238 239 c [for liquid clouds, traditional formula, 240 c for ice clouds, Ebert & Curry (1992)] 241 242 if (zflwp(i).eq.0.) rel = 1. 243 if (zfiwp(i).eq.0. .or. rei.le.0.) rei = 1. 244 pcltau(i,k) = 3.0/2.0 * ( zflwp(i)/rel ) 245 . + zfiwp(i) * (3.448e-03 + 2.431/rei) 246 247 c -- cloud infrared emissivity: 248 249 c [the broadband infrared absorption coefficient is parameterized 250 c as a function of the effective cld droplet radius] 251 252 c Ebert and Curry (1992) formula as used by Kiehl & Zender (1995): 253 k_ice = k_ice0 + 1.0/rei 254 255 pclemi(i,k) = 1.0 256 . - EXP( - coef_chau*zflwp(i) - DF*k_ice*zfiwp(i) ) 257 258 endif ! ok_newmicro 259 260 lo = (pclc(i,k) .LE. seuil_neb) 261 IF (lo) pclc(i,k) = 0.0 262 IF (lo) pcltau(i,k) = 0.0 263 IF (lo) pclemi(i,k) = 0.0 264 265 IF (lo) cldtaupi(i,k) = 0.0 266 IF (.NOT.ok_aie) cldtaupi(i,k)=pcltau(i,k) 267 ENDDO 268 ENDDO 269 ccc DO k = 1, klev 270 ccc DO i = 1, klon 271 ccc t(i,k) = t(i,k) 272 ccc pclc(i,k) = MAX( 1.e-5 , pclc(i,k) ) 273 ccc lo = pclc(i,k) .GT. (2.*1.e-5) 274 ccc zflwp = pqlwp(i,k)*1000.*(paprs(i,k)-paprs(i,k+1)) 275 ccc . /(rg*pclc(i,k)) 276 ccc zradef = 10.0 + (1.-sigs(k))*45.0 277 ccc pcltau(i,k) = 1.5 * zflwp / zradef 278 ccc zfice=1.0-MIN(MAX((t(i,k)-263.)/(273.-263.),0.0),1.0) 279 ccc zmsac = 0.13*(1.0-zfice) + 0.08*zfice 280 ccc pclemi(i,k) = 1.-EXP(-zmsac*zflwp) 281 ccc if (.NOT.lo) pclc(i,k) = 0.0 282 ccc if (.NOT.lo) pcltau(i,k) = 0.0 283 ccc if (.NOT.lo) pclemi(i,k) = 0.0 284 ccc ENDDO 285 ccc ENDDO 286 cccccc print*, 'pas de nuage dans le rayonnement' 287 cccccc DO k = 1, klev 288 cccccc DO i = 1, klon 289 cccccc pclc(i,k) = 0.0 290 cccccc pcltau(i,k) = 0.0 291 cccccc pclemi(i,k) = 0.0 292 cccccc ENDDO 293 cccccc ENDDO 294 C 295 C COMPUTE CLOUD LIQUID PATH AND TOTAL CLOUDINESS 296 C 297 cIM cf. CR:test: calcul prenant ou non en compte le recouvrement 298 cinitialisations 198 DO k = 1, klev 199 ! IF(.not.ok_aie) THEN 200 rad_chaud = rad_chau1 201 IF (k.LE.3) rad_chaud = rad_chau2 202 ! ENDIF 203 DO i = 1, klon 204 IF (pclc(i,k) .LE. seuil_neb) THEN 205 206 c -- effective cloud droplet radius (microns): 207 208 c for liquid water clouds: 209 ! For output diagnostics 210 ! 211 ! Cloud droplet effective radius [um] 212 ! 213 ! we multiply here with f * xl (fraction of liquid water 214 ! clouds in the grid cell) to avoid problems in the 215 ! averaging of the output. 216 ! In the output of IOIPSL, derive the real cloud droplet 217 ! effective radius as re/fl 218 ! 219 220 fl(i,k) = seuil_neb*(1.-zfice2(i,k)) 221 re(i,k) = rad_chaud_tab(i,k)*fl(i,k) 222 223 pclc(i,k) = 0.0 224 pcltau(i,k) = 0.0 225 pclemi(i,k) = 0.0 226 cldtaupi(i,k) = 0.0 227 ELSE 228 229 c -- liquid/ice cloud water paths: 230 231 zflwp_var= 1000.*(1.-zfice2(i,k))*pqlwp(i,k)/pclc(i,k) 232 & *diff_paprs(i,k) 233 zfiwp_var= 1000.*zfice2(i,k)*pqlwp(i,k)/pclc(i,k) 234 & *diff_paprs(i,k) 235 236 c -- effective cloud droplet radius (microns): 237 238 c for liquid water clouds: 239 240 IF (ok_aie) THEN 241 radius = 242 & 1.1 243 & *((pqlwp(i,k)*pplay(i,k)/(RD * T(i,k))) 244 & /(4./3.*RPI*1000.*cdnc_pi(i,k)))**(1./3.) 245 radius = MAX(radius*1e6, 5.) 246 247 tc = t(i,k)-273.15 248 rei = 0.71*tc + 61.29 249 if (tc.le.-81.4) rei = 3.5 250 if (zflwp_var.eq.0.) radius = 1. 251 if (zfiwp_var.eq.0. .or. rei.le.0.) rei = 1. 252 cldtaupi(i,k) = 3.0/2.0 * zflwp_var / radius 253 & + zfiwp_var * (3.448e-03 + 2.431/rei) 254 ENDIF ! ok_aie 255 ! For output diagnostics 256 ! 257 ! Cloud droplet effective radius [um] 258 ! 259 ! we multiply here with f * xl (fraction of liquid water 260 ! clouds in the grid cell) to avoid problems in the 261 ! averaging of the output. 262 ! In the output of IOIPSL, derive the real cloud droplet 263 ! effective radius as re/fl 264 ! 265 266 fl(i,k) = pclc(i,k)*(1.-zfice2(i,k)) 267 re(i,k) = rad_chaud_tab(i,k)*fl(i,k) 268 269 rel = rad_chaud_tab(i,k) 270 c for ice clouds: as a function of the ambiant temperature 271 c [formula used by Iacobellis and Somerville (2000), with an 272 c asymptotical value of 3.5 microns at T<-81.4 C added to be 273 c consistent with observations of Heymsfield et al. 1986]: 274 tc = t(i,k)-273.15 275 rei = 0.71*tc + 61.29 276 if (tc.le.-81.4) rei = 3.5 277 c -- cloud optical thickness : 278 279 c [for liquid clouds, traditional formula, 280 c for ice clouds, Ebert & Curry (1992)] 281 282 if (zflwp_var.eq.0.) rel = 1. 283 if (zfiwp_var.eq.0. .or. rei.le.0.) rei = 1. 284 pcltau(i,k) = 3.0/2.0 * ( zflwp_var/rel ) 285 & + zfiwp_var * (3.448e-03 + 2.431/rei) 286 c -- cloud infrared emissivity: 287 288 c [the broadband infrared absorption coefficient is parameterized 289 c as a function of the effective cld droplet radius] 290 291 c Ebert and Curry (1992) formula as used by Kiehl & Zender (1995): 292 k_ice = k_ice0 + 1.0/rei 293 294 pclemi(i,k) = 1.0 295 & - EXP( -coef_chau*zflwp_var - DF*k_ice*zfiwp_var) 296 297 ENDIF 298 299 ENDDO 300 ENDDO 301 302 DO k = 1, klev 303 DO i = 1, klon 304 xflwp(i) = xflwp(i)+ xflwc(i,k) * diff_paprs(i,k) 305 xfiwp(i) = xfiwp(i)+ xfiwc(i,k) * diff_paprs(i,k) 306 ENDDO 307 ENDDO 308 309 ELSE 310 DO k = 1, klev 311 rad_chaud = rad_chau1 312 IF (k.LE.3) rad_chaud = rad_chau2 313 DO i = 1, klon 314 315 IF (pclc(i,k) .LE. seuil_neb) THEN 316 317 pclc(i,k) = 0.0 318 pcltau(i,k) = 0.0 319 pclemi(i,k) = 0.0 320 cldtaupi(i,k) = 0.0 321 322 ELSE 323 324 zflwp_var = 1000.*pqlwp(i,k)*diff_paprs(i,k) 325 & /pclc(i,k) 326 327 zfice1 = MIN( 328 & MAX( 1.0 - (t(i,k)-t_glace) / (273.13-t_glace) 329 & ,0.0),1.0)**nexpo 330 331 radius = rad_chaud * (1.-zfice1) + rad_froid * zfice1 332 coef = coef_chau * (1.-zfice1) + coef_froi * zfice1 333 334 pcltau(i,k) = 3.0 * zflwp_var / (2.0 * radius) 335 pclemi(i,k) = 1.0 - EXP( - coef * zflwp_var) 336 337 ENDIF 338 339 ENDDO 340 ENDDO 341 ENDIF 342 343 IF (.NOT.ok_aie) THEN 344 DO k = 1, klev 345 DO i = 1, klon 346 cldtaupi(i,k)=pcltau(i,k) 347 ENDDO 348 ENDDO 349 ENDIF 350 351 ccc DO k = 1, klev 352 ccc DO i = 1, klon 353 ccc t(i,k) = t(i,k) 354 ccc pclc(i,k) = MAX( 1.e-5 , pclc(i,k) ) 355 ccc lo = pclc(i,k) .GT. (2.*1.e-5) 356 ccc zflwp = pqlwp(i,k)*1000.*(paprs(i,k)-paprs(i,k+1)) 357 ccc . /(rg*pclc(i,k)) 358 ccc zradef = 10.0 + (1.-sigs(k))*45.0 359 ccc pcltau(i,k) = 1.5 * zflwp / zradef 360 ccc zfice=1.0-MIN(MAX((t(i,k)-263.)/(273.-263.),0.0),1.0) 361 ccc zmsac = 0.13*(1.0-zfice) + 0.08*zfice 362 ccc pclemi(i,k) = 1.-EXP(-zmsac*zflwp) 363 ccc if (.NOT.lo) pclc(i,k) = 0.0 364 ccc if (.NOT.lo) pcltau(i,k) = 0.0 365 ccc if (.NOT.lo) pclemi(i,k) = 0.0 366 ccc ENDDO 367 ccc ENDDO 368 ccccc print*, 'pas de nuage dans le rayonnement' 369 ccccc DO k = 1, klev 370 ccccc DO i = 1, klon 371 ccccc pclc(i,k) = 0.0 372 ccccc pcltau(i,k) = 0.0 373 ccccc pclemi(i,k) = 0.0 374 ccccc ENDDO 375 ccccc ENDDO 376 C 377 C COMPUTE CLOUD LIQUID PATH AND TOTAL CLOUDINESS 378 C 379 c IM cf. CR:test: calcul prenant ou non en compte le recouvrement 380 c initialisations 299 381 DO i=1,klon 300 382 zclear(i)=1. … … 308 390 cIM cf CR DO k=1,klev 309 391 DO k = klev, 1, -1 310 DO i = 1, klon 311 pctlwp(i) = pctlwp(i) 312 . + pqlwp(i,k)*(paprs(i,k)-paprs(i,k+1))/RG 313 cIM cf. CR 314 IF (NOVLP.EQ.1) THEN 392 DO i = 1, klon 393 pctlwp(i) = pctlwp(i) 394 & + pqlwp(i,k)*diff_paprs(i,k) 395 ENDDO 396 ENDDO 397 c IM cf. CR 398 IF (NOVLP.EQ.1) THEN 399 DO k = klev, 1, -1 400 DO i = 1, klon 315 401 zclear(i)=zclear(i)*(1.-MAX(pclc(i,k),zcloud(i))) 316 s/(1.-MIN(zcloud(i),1.-ZEPSEC))402 & /(1.-MIN(zcloud(i),1.-ZEPSEC)) 317 403 pct(i)=1.-zclear(i) 318 if (pplay(i,k).LE.cetahb*paprs(i,1)) then404 IF (pplay(i,k).LE.cetahb*paprs(i,1)) THEN 319 405 pch(i) = pch(i)*(1.-MAX(pclc(i,k),zcloud(i))) 320 s/(1.-MIN(zcloud(i),1.-ZEPSEC))321 else if(pplay(i,k).GT.cetahb*paprs(i,1) .AND.322 . pplay(i,k).LE.cetamb*paprs(i,1)) then406 & /(1.-MIN(zcloud(i),1.-ZEPSEC)) 407 ELSE IF (pplay(i,k).GT.cetahb*paprs(i,1) .AND. 408 & pplay(i,k).LE.cetamb*paprs(i,1)) THEN 323 409 pcm(i) = pcm(i)*(1.-MAX(pclc(i,k),zcloud(i))) 324 s/(1.-MIN(zcloud(i),1.-ZEPSEC))325 else if (pplay(i,k).GT.cetamb*paprs(i,1)) then410 & /(1.-MIN(zcloud(i),1.-ZEPSEC)) 411 ELSE IF (pplay(i,k).GT.cetamb*paprs(i,1)) THEN 326 412 pcl(i) = pcl(i)*(1.-MAX(pclc(i,k),zcloud(i))) 327 s/(1.-MIN(zcloud(i),1.-ZEPSEC))413 & /(1.-MIN(zcloud(i),1.-ZEPSEC)) 328 414 endif 329 415 zcloud(i)=pclc(i,k) 330 ELSE IF (NOVLP.EQ.2) THEN 416 ENDDO 417 ENDDO 418 ELSE IF (NOVLP.EQ.2) THEN 419 DO k = klev, 1, -1 420 DO i = 1, klon 331 421 zcloud(i)=MAX(pclc(i,k),zcloud(i)) 332 422 pct(i)=zcloud(i) 333 if (pplay(i,k).LE.cetahb*paprs(i,1)) then423 IF (pplay(i,k).LE.cetahb*paprs(i,1)) THEN 334 424 pch(i) = MIN(pclc(i,k),pch(i)) 335 else if(pplay(i,k).GT.cetahb*paprs(i,1) .AND.336 . pplay(i,k).LE.cetamb*paprs(i,1)) then425 ELSE IF (pplay(i,k).GT.cetahb*paprs(i,1) .AND. 426 & pplay(i,k).LE.cetamb*paprs(i,1)) THEN 337 427 pcm(i) = MIN(pclc(i,k),pcm(i)) 338 else if (pplay(i,k).GT.cetamb*paprs(i,1)) then428 ELSE IF (pplay(i,k).GT.cetamb*paprs(i,1)) THEN 339 429 pcl(i) = MIN(pclc(i,k),pcl(i)) 340 430 endif 341 ELSE IF (NOVLP.EQ.3) THEN 431 ENDDO 432 ENDDO 433 ELSE IF (NOVLP.EQ.3) THEN 434 DO k = klev, 1, -1 435 DO i = 1, klon 342 436 zclear(i)=zclear(i)*(1.-pclc(i,k)) 343 437 pct(i)=1-zclear(i) 344 if (pplay(i,k).LE.cetahb*paprs(i,1)) then345 pch(i) = pch(i)*(1.0-pclc(i,k))346 else if(pplay(i,k).GT.cetahb*paprs(i,1) .AND.347 . pplay(i,k).LE.cetamb*paprs(i,1)) then348 pcm(i) = pcm(i)*(1.0-pclc(i,k))349 else if (pplay(i,k).GT.cetamb*paprs(i,1)) then350 pcl(i) = pcl(i)*(1.0-pclc(i,k))438 IF (pplay(i,k).LE.cetahb*paprs(i,1)) THEN 439 pch(i) = pch(i)*(1.0-pclc(i,k)) 440 ELSE IF (pplay(i,k).GT.cetahb*paprs(i,1) .AND. 441 & pplay(i,k).LE.cetamb*paprs(i,1)) THEN 442 pcm(i) = pcm(i)*(1.0-pclc(i,k)) 443 ELSE IF (pplay(i,k).GT.cetamb*paprs(i,1)) THEN 444 pcl(i) = pcl(i)*(1.0-pclc(i,k)) 351 445 endif 352 ENDIF 353 ENDDO 354 ENDDO 355 C 446 ENDDO 447 ENDDO 448 ENDIF 449 450 C 356 451 DO i = 1, klon 357 c IM cf. CR pct(i)=1.-pct(i)452 c IM cf. CR pct(i)=1.-pct(i) 358 453 pch(i)=1.-pch(i) 359 454 pcm(i)=1.-pcm(i) 360 455 pcl(i)=1.-pcl(i) 361 456 ENDDO 457 362 458 C 363 459 RETURN
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