Ignore:
Timestamp:
Mar 4, 2020, 6:31:04 PM (5 years ago)
Author:
abierjon
Message:

Mars GCM:
Bug fixes in the slope winds parametrization and its interactions with rocketduststorm : now, it is considered that the sub-grid dust storm is decorrelated from the dust entrainment above the sub-grid scale topography, so that : 1) the background dust available for slope winds is updated after the rocketduststorm parametrization ; 2) the extra-heating on top of the mountains is calculated regarding topdust and background dust tracers' optical depths only (and not stormdust optical depth).
AB

Location:
trunk/LMDZ.MARS/libf/phymars
Files:
2 edited

Legend:

Unmodified
Added
Removed

  • trunk/LMDZ.MARS/libf/phymars/physiq_mod.F

    r2247 r2248  
    11241124           hsummit(:)=14000.
    11251125         endif
     1126         clearatm=.true.
    11261127         nohmons=.false.
    11271128         pdqtop(:,:,:)=0. 

  • trunk/LMDZ.MARS/libf/phymars/topmons_mod.F90

    r2246 r2248  
    257257
    258258      !! Update the initial mixing ratios
    259       zq0(1:ngrid,1:nlayer,1:nq)=pq(1:ngrid,1:nlayer,1:nq) !+pdq(1:ngrid,1:nlayer,1:nq)*ptimestep update after rocket dust storm scheme ?
     259      zq0(1:ngrid,1:nlayer,1:nq)=pq(1:ngrid,1:nlayer,1:nq)+pdq(1:ngrid,1:nlayer,1:nq)*ptimestep ! update of the background dust after rocket dust storm scheme
    260260      zq(1:ngrid,1:nlayer,1:nq)=zq0(1:ngrid,1:nlayer,1:nq)
    261261      zq_dust_mass(1:ngrid,1:nlayer)=zq(1:ngrid,1:nlayer,igcm_dust_mass)
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