Ignore:
Timestamp:
Nov 30, 2018, 12:55:49 AM (7 years ago)
Author:
jvatant
Message:

Major radiative transfer contribution : Add the 'corrk_recombin' option that allows to use
correlated-k for single species instead of pre-mix and enables more flexiblity for variable species.
-> Algorithm inspired from Lacis and Oinas 1991 and Amundsen et al 2016

+ Added 'recombin_corrk.F90' - Important improvements in 'sugas_corrk.90' and 'callcork.F90'

  • Must have the desired variable species as tracers -> TBD : Enable to force composition even if no tracers
  • To have decent CPU time recombining is not done on all gridpoints and wavelenghts but we calculate a gasi/v_recomb variable on the reference corrk-k T,P grid (only for T,P values who match the atmospheric conditions ) which is then processed as a standard pre-mix in optci/v routines, but updated every time tracers on the ref P grid have varied > 1%.


READ CAREFULY :

  • In case of 'corrk_recombin', the variable L_NREFVAR doesn't have the same meaning as before and doesn't stand for the different mixing ratios but the different species.
  • Input corr-k should be found in corrkdir within 'corrk_gcm_IR/VI_XXX.dat' and can contain a 'fixed' specie ( compulsory if you include self-broadening ) that MUST have been created with correct mixing ratios, or a variable specie for which mixing ratio MUST have been set to 1 ( no self-broadening then, assume it's a trace sepecie ) -> You can't neither have CIA of variable species included upstream in the corr-k
File:
1 edited

Legend:

Unmodified
Added
Removed
  • trunk/LMDZ.TITAN/README

    r2003 r2050  
    14961496== 24/09/18 == JVO
    14971497Fix the outdated value of surface CH4 in the chemistry (0.048 Niemann 2005 -> 0.0565 Niemann 2010)
     1498
     1499== 28/11/18 == JVO
     1500Add a simple seasonal+latitudinal variation model (season_haze.F90) for the vertical mean profile
     1501of haze. Based on Karkoscha,2016 . Activable through "seashaze" key (default=T).
     1502
     1503== 29/11/18 == JVO ( r2050 )
     1504Major radiative transfer contribution : Add the 'corrk_recombin' option that allows to use
     1505correlated-k for single species instead of pre-mix and enables more flexiblity for variable species.
     1506-> Algorithm inspired from Lacis and Oinas 1991 and Amundsen et al 2016
     1507
     1508+ Added 'recombin_corrk.F90' - Important improvements in 'sugas_corrk.90' and 'callcork.F90'
     1509
     1510- Must have the desired variable species as tracers
     1511  -> TBD : Enable to force composition even if no tracers
     1512
     1513- To have decent CPU time recombining is not done on all gridpoints and wavelenghts but we
     1514  calculate a gasi/v_recomb variable on the reference corrk-k T,P grid (only for T,P values
     1515  who match the atmospheric conditions ) which is then processed as a standard pre-mix in
     1516  optci/v routines, but updated every time tracers on the ref P grid have varied > 1%.
     1517 
     1518READ CAREFULY :
     1519- In case of 'corrk_recombin', the variable L_NREFVAR doesn't have the same meaning as before
     1520  and doesn't stand for the different mixing ratios but the different species.
     1521- Input corr-k should be found in corrkdir within 'corrk_gcm_IR/VI_XXX.dat' and can
     1522  contain a 'fixed' specie ( compulsory if you include self-broadening ) that MUST have
     1523  been created with correct mixing ratios, or a variable specie for which mixing ratio
     1524  MUST have been set to 1 ( no self-broadening then, assume it's a trace sepecie )
     1525  -> You can't neither have CIA of variable species included upstream in the corr-k
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