- Timestamp:
- Nov 26, 2021, 8:27:27 AM (3 years ago)
- Location:
- LMDZ6/branches/Ocean_skin/libf/phylmd
- Files:
-
- 4 edited
Legend:
- Unmodified
- Added
- Removed
-
LMDZ6/branches/Ocean_skin/libf/phylmd/phyredem.F90
r4020 r4021 162 162 CALL put_field_srf1(pass,"TS","Temperature",ftsol(:,:)) 163 163 164 !! CALL put_field_srf1(pass,"DELTA_TS","w-x surface temperature difference", delta_tsurf(:,:))165 164 CALL put_field_srf1(pass,"DELTATS","w-x surface temperature difference", delta_tsurf(:,:)) 166 167 ! CALL put_field_srf1(pass,"BETA_S","Aridity factor", beta_aridity(:,:))168 165 CALL put_field_srf1(pass,"BETAS","Aridity factor", beta_aridity(:,:)) 169 166 ! End surface variables -
LMDZ6/branches/Ocean_skin/libf/phylmd/phys_output_var_mod.F90
r4020 r4021 134 134 ! Ocean-atmosphere interface, subskin ocean and near-surface ocean: 135 135 136 REAL, SAVE, ALLOCATABLE:: tkt(:) 136 REAL, SAVE, ALLOCATABLE:: tkt(:) ! (klon) 137 137 ! épaisseur (m) de la couche de diffusion thermique (microlayer) 138 138 ! cool skin thickness 139 139 140 REAL, SAVE, ALLOCATABLE:: tks(:) 140 REAL, SAVE, ALLOCATABLE:: tks(:) ! (klon) 141 141 ! épaisseur (m) de la couche de diffusion de masse (microlayer) 142 142 143 REAL, SAVE, ALLOCATABLE:: taur(:) ! momentum flux due to rain, in Pa144 145 REAL, SAVE, ALLOCATABLE:: sss(:) 143 REAL, SAVE, ALLOCATABLE:: taur(:) ! (klon) momentum flux due to rain, in Pa 144 145 REAL, SAVE, ALLOCATABLE:: sss(:) ! (klon) 146 146 ! bulk salinity of the surface layer of the ocean, in ppt 147 147 -
LMDZ6/branches/Ocean_skin/libf/phylmd/surf_ocean_mod.F90
r4020 r4021 334 334 delta_sst = t_int - tsurf_new(:knon) 335 335 delta_sal = s_int - sss(:knon) 336 if (activate_ocean_skin >= 2) tsurf_new(:knon) = t_int 337 if (activate_ocean_skin == 2 .and. type_ocean == 'couple') & 338 dt_ds = (tks / tkt) * dter 336 337 if (activate_ocean_skin == 2) then 338 tsurf_new(:knon) = t_int 339 if (type_ocean == 'couple') dt_ds = (tks / tkt) * dter 340 end if 339 341 end if 340 342 -
LMDZ6/branches/Ocean_skin/libf/phylmd/wake.F90
r3798 r4021 2240 2240 d_deltaqw, sigmaw, d_sigmaw, alpha) 2241 2241 ! ------------------------------------------------------ 2242 ! D termination du coefficient alpha tel que les tendances2242 ! D\'etermination du coefficient alpha tel que les tendances 2243 2243 ! corriges alpha*d_G, pour toutes les grandeurs G, correspondent 2244 2244 ! a une humidite positive dans la zone (x) et dans la zone (w).
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