Changes between Version 322 and Version 323 of doc/app/errmsg


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Timestamp:
Jun 7, 2017 9:08:34 AM (8 years ago)
Author:
sward
Comment:

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  • doc/app/errmsg

    v322 v323  
    621621   }}}
    622622}}}
    623 ||[=#PA0395 PA0395]   ||zu(nzt+1) = ... m is higher than the maximum height in LSF_DATA which is ...m. Interpolation on PALM grid is not possible. || LSF_DATA has a maximum vertical height that is smaller than the vertical extent of the grid used in PALM. Hence, interpolation of the LSF_DATA onto the PALM grid is not possible. Reduce either the vertical extent of the PALM modeling domain or enlarge the LSF_DATA file correspondingly.  ||
     623||[=#PA0395 PA0395]   ||zu(nzt+1) = ... m is higher than the maximum height in LSF_DATA which is ...m. Interpolation on PALM grid is not possible. || {{{LSF_DATA}}} has a maximum vertical height that is smaller than the vertical extent of the grid used in PALM. Hence, interpolation of the {{{LSF_DATA}}} onto the PALM grid is not possible. Reduce either the vertical extent of the PALM modeling domain or enlarge the {{{LSF_DATA}}} file correspondingly.  ||
    624624||[=#PA0396 PA0396]   ||The usage of use_subsidence_tendencies requires large_scale_subsidence = .T.. || If  [../inipar#use_subsidence_tendencies use_subsidence_tendencies] is used, subsidence tendencies for temperature and humidity are read in from the external file {{{LSF_DATA}}}. However, these tendencies can only be applied to the prognostic variables if [../inipar#large_scale_subsidence large_scale_subsidence] = .T.. ||
    625625||[=#PA0397 PA0397]   ||The usage of use_subsidence_tendencies requires large_scale_forcing = .T.. || If  [../inipar#use_subsidence_tendencies use_subsidence_tendencies] is used, subsidence tendencies for temperature and humidity are read in from the external file {{{LSF_DATA}}}. This requires [../inipar#large_scale_forcing large_scale_forcing] = .T.. ||