- Timestamp:
- Mar 19, 2024, 11:06:57 AM (8 months ago)
- Location:
- trunk/LMDZ.MARS
- Files:
-
- 2 edited
Legend:
- Unmodified
- Added
- Removed
-
trunk/LMDZ.MARS/changelog.txt
r3272 r3273 4574 4574 == 19/03/2024 == LL 4575 4575 Adapt soil water to run with massive ice and not pore filling ice + constant diffusion coefficient 4576 Small fixes in vdifc for the interaction between the subsurface and frost (the flux from the surface frost to the subsurface was oo large if one removes all the frost at the surface) 4577 -
trunk/LMDZ.MARS/libf/phymars/vdifc_mod.F
r3262 r3273 1169 1169 & *qsat_ssi(ig,islope) 1170 1170 1171 1171 ! Flux from the subsurface 1172 if(old_wsublimation_scheme) then 1173 zdqsdif_ssi_atm(ig,islope)=rho(ig) 1174 & *dryness(ig)*zcdv(ig,islope) 1175 & *1/(1+resist(ig,islope)) 1176 & *(zq1temp(ig)-qsat_ssi(ig,islope)) 1177 else 1178 zdqsdif_ssi_atm(ig,islope)=rho(ig)* 1179 & *dryness(ig) *zcdh(ig,islope) 1180 & *1/(1+resist(ig,islope)) 1181 & *(zq1temp(ig)-qsat_ssi(ig,islope)) 1182 endif 1172 1183 1173 1184 else … … 1214 1225 & *(qsat(ig)-qsat_ssi(ig,islope)) 1215 1226 1216 ! Line to comment for now since we don't have a mass of subsurface frost in our computation (otherwise, we would not conserve the H2O mass in the system) 1227 ! Line to comment for now since we don't have a mass of subsurface frost 1228 ! in our computation (otherwise, we would not conserve the H2O mass in 1229 ! the system) 1230 1231 1232 if ((-zdqsdif_tot(ig)+zdqsdif_ssi_frost(ig,islope)) 1233 & *subtimestep.ge.(zqsurf(ig))) then 1234 zdqsdif_ssi_frost(ig,islope) = 1235 & zqsurf(ig)/subtimestep 1236 & + zdqsdif_tot(ig) 1237 endif 1238 1217 1239 zdqsdif_tot(ig) = zdqsdif_tot(ig) - 1218 1240 & zdqsdif_ssi_frost(ig,islope)
Note: See TracChangeset
for help on using the changeset viewer.