Changes between Version 197 and Version 198 of doc/app/errmsg


Ignore:
Timestamp:
Mar 4, 2015 12:27:21 PM (10 years ago)
Author:
maronga
Comment:

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  • doc/app/errmsg

    v197 v198  
    628628||[=#PA0397 PA0397]   ||The usage of use_subsidence_tendencies requires large_scale_forcing = .T.. || If 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.. ||
    629629||[=#PA0398 PA0398]   ||run will be terminated because user forced a job finialization using a flag file: DO_STOP_NOW: "..." DO_RESTART_NOW: "..." ||The user can force an unscheduled termination/restart of the running job by creating one of the flag files {{{DO_STOP_NOW}}} or {{{DO_RESTART_NOW}}} in the temporary directory of the job. ||
    630 ||[=#PA0399 PA0399]   ||||
    631 ||[=#PA0400 PA0400]   ||||
    632 ||[=#PA0401 PA0401]   ||||
    633 ||[=#PA0402 PA0402]   ||||
     630||[=#PA0399 PA0399]   ||lsm requires setting of bc_pt_b = "dirichlet" and bc_q_b  = "dirichlet" ||In case the land surface model (LSM) is used, the surface fluxes have to be calculated by means of surface values of potential temperature and humidity (that are provided by the LSM), which reflects setting dirichlet boundary conditions. ||
     631||[=#PA0400 PA0400]   ||lsm requires prandtl_layer = .T.||The land surface model (LSM) requires the assumption of a constant flux layer (Prandtl layer) between the surface and the first computational grid point in order to calculate heat and momentum fluxes. ||
     632||[=#PA0401 PA0401]   ||veg_type = 0 (user defined) requires setting of root_fraction(0:3) = 9999999.9 and SUM(root_fraction) = 1||In case a user-defined vegetation is used, the root distribution of the plants to each of the soil layers must be explicitly set using the parameter root_fraction. The sum of the fractions then must sum up to 1. ||
     633||[=#PA0402 PA0402]   ||lsm requires radiation = .T.||The land surface model (LSM) can only be used in combination with a radiation model that provides the incoming shortwave radiation as well as the net radiation at the surface. ||
    634634||[=#PA0403 PA0403]   ||||
    635635||[=#PA0404 PA0404]   ||||