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Timestamp:
Nov 3, 2023, 6:02:56 PM (13 months ago)
Author:
llange
Message:

Mars PCM

  • Introducing the possibily to compute water adsorption / desorption -routine soilwater.F90) -. FOR NOW IT WORKS ONLY IN 1D, DON'T TEST IN 3D (by default, adsorption is not called, if not specified in the callphys.def). By default, when using the adsorption, the number of subtimestep used in the water subimation scheme is 1 (otherwise, it crashes)
  • New grid for the soil layers (better resolution) as it is needed to solve the diffusion equations. It does not increase the CPU time.

PYM & LL

File:
1 edited

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  • trunk/LMDZ.MARS/changelog.txt

    r3113 r3115  
    43104310Introducing qsoil to model H2O adsorption/desorption in the subsurface. For now, I've fixed the number of tracers in the subsurface to t
    43114311hree (H2O vap, H2O ice, H2O ads).
    4312 
     4312Changing the soil grid (better resolution) as given by Pierre Yves Meslin
     4313Adding the possibility to compute H2O adsorption desorption and exchange with
     4314the near-surface atmosphere, only works in 1D for now. By default, subtimestep
     4315for water sublimation is 1 when adsorption is activated (otherwise it crashes)
     4316
     4317
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