Changes between Version 318 and Version 319 of doc/app/errmsg


Ignore:
Timestamp:
Jun 7, 2017 8:22:14 AM (8 years ago)
Author:
Giersch
Comment:

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  • doc/app/errmsg

    v318 v319  
    6363||[=#PA0038 PA0038]   || turbulent_outflow = .T. requires bc_lr = "dirichlet/radiation" || When using the turbulent outflow method, non-cyclic boundary condition along the x direction must be used. See also [../inipar#turbulent_outflow turbulent_outflow]. ||
    6464||[=#PA0039 PA0039]   ||   || message number is unused ||
    65 ||[=#PA0040 PA0040]   ||LWC is not conserved during collision! LWC after condensation: ... LWC after collision: ... || This should not happen. Please write a [https://palm.muk.uni-hannover.de/trac/newticket ticket]. LWC means liquid water content.  ||
     65||[=#PA0040 PA0040]   ||LWC is not conserved during collision! LWC after condensation: ... LWC after collision: ... || LWC means liquid water content. This should not happen. Please write a [https://palm.muk.uni-hannover.de/trac/newticket ticket].  ||
    6666||[=#PA0041 PA0041]   ||simulating a plant canopy requires a non-zero drag coefficient, given value is canopy_drag_coeff = 0.0   || When simulating a plant canopy, a non-zero [../canpar#canopy_drag_coeff canopy_drag_coeff] must be set in the parameter file under NAMELIST {{{&canopy_par}}}. The [/wiki/doc/app/canpar canopy model] in PALM adds an additional sink/source terms to the momentum equations, the prognostic equation for temperature, and the subgrid scale turbulent kinetic energy equation. In case of [../inipar#humidity humidity] = ''.TRUE.'' or [../inipar#passive_scalar passive_scalar] = ''.TRUE.'', an additional source/sink term is added to the prognostic equation of the respective scalar.\\ If [../canpar#canopy_drag_coeff canopy_drag_coeff] = 0.0, the additional terms equal zero and there would be no effect on the flow.  ||
    6767||[=#PA0042 PA0042]   ||use_top_fluxes must be .TRUE. in ocean mode   ||In [../inipar#ocean ocean] mode, fluxes at the water surface must be prescribed as driving boundary conditions. In atmosphere-ocean coupled runs, these fluxes are provided by the atmosphere run. ||