Changes between Version 322 and Version 323 of doc/app/errmsg
- Timestamp:
- Jun 7, 2017 9:08:34 AM (8 years ago)
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doc/app/errmsg
v322 v323 621 621 }}} 622 622 }}} 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_DATAfile 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. || 624 624 ||[=#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.. || 625 625 ||[=#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.. ||