Ignore:
Timestamp:
May 29, 2012, 11:50:48 AM (13 years ago)
Author:
emillour
Message:

Mars GCM:

  • Added the possibility to use the "cold" (iaervar=6) or "warm" (iaervar=7) dust scenarios (derived from the 7 MY24 to MY30 scenarios) in aeropacity.F and read_dust_scenario.F

EM

File:
1 edited

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Added
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  • trunk/LMDZ.MARS/deftank/callphys.def.outliers

    r627 r677  
    33#Run with or without tracer transport ?
    44tracer=.true.
     5
     6#Where are the external files (dust, topography; chemistry,...)
     7#datadir=/u/forget/WWW/datagcm/datafile
    58
    69#Diurnal cycle ?  if diurnal=False, diurnal averaged solar heating
     
    2326#  =1 Dust opt.deph read in startfi; =2 Viking scenario; =3 MGS scenario,
    2427#  =4 Mars Year 24 from TES assimilation (old version of MY24; dust_tes.nc file)
    25 #  =24 Mars Year 24 from TES assimilation (ie: MCD reference case)
    26 #  =25 Mars Year 25 from TES assimilation (ie: a year with a global dust storm)
    27 #  =26 Mars Year 26 from TES assimilation
     28#  =6 "cold" (low dust) scenario ; =7 "warm" (high dust) scenario
     29#  =24 Mars Year 24  ; =25 Mars Year 25 (year with a global dust storm) ; ...
     30#  =30 Mars Year 30
    2831iaervar = 26
    2932# Dust opacity at 610 Pa (when constant, i.e. for the iaervar=1 case)
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