Changes between Version 167 and Version 168 of doc/app/errmsg


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Timestamp:
Mar 20, 2014 2:55:30 PM (11 years ago)
Author:
heinze
Comment:

--

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  • doc/app/errmsg

    v167 v168  
    134134||[=#PA0109 PA0109]   ||output of "..." requires ocean = .TRUE.   || The quantities rho and sa are only calculated in case of [../inipar#ocean ocean] = ''.T.''. ||
    135135||[=#PA0110 PA0110]   ||output of "..." requires passive_scalar = .TRUE.   || The output of the passive scalar s is only available if the prognostic equation for a passive scalar is solved by setting [../inipar#passive_scalar passive_scalar] = ''.T.''. ||
    136 ||[=#PA0111 PA0111]   ||illegal value for data_output: "..." only 2d-horizontal cross sections are allowed for this value   ||  ||
    137 ||[=#PA0112 PA0112]   ||output of "..." requires precipitation = .TRUE.   ||  ||
    138 ||[=#PA0113 PA0113]   ||temporal averaging of precipitation amount "..." is not possible  ||  ||
     136||[=#PA0111 PA0111]   ||illegal value for data_output: "..." only 2d-horizontal cross sections are allowed for this value   ||The listed quantities are pure two-dimensional xy-cross-sections. They are not available as 3d data or xz/yz cross-sections. Note that these quantities are always marked by an asterisk as last character.  ||
     137||[=#PA0112 PA0112]   ||output of "..." requires precipitation = .TRUE.   ||The quantities pra* and prr* are only calculated in case of [../inipar#precipitation precipitation] = ''.T.''.  ||
     138||[=#PA0113 PA0113]   ||temporal averaging of precipitation amount "..." is not possible  ||The quantity precipitation_amount pra* listed in  [../d3par#data_output data_output] contains already the summed precipitation of the last [../d3par#precipitation_amount_interval precipitation_amount_interval]. Therefore, remove the substring _av of pra*.   ||
    139139||[=#PA0114 PA0114]   ||illegal value for data_output or data_output_user = "..."   || No matching variable was found for the given identifier in the parameter file. Possible reasons are: (a) a typo in the parameter file, (b) a user-defined variable has not been defined in {{{user_check_data_output.f90}}}, (c) the string length of the user-defined variable exceeds the current limits (see [../userint/output here]). ||
    140140||[=#PA0115 PA0115]   ||illegal value for data_output = "..."   || No matching variable was found for the given identifier in the parameter file. This error is most likely related to a typo in the parameter file (a output variable was used that does not exist in PALM. ||
     
    142142||[=#PA0118 PA0118]   ||illegal precision: do3d_comp_prec ( ...) = "..."   ||  ||
    143143||[=#PA0119 PA0119]   ||unknown variable "..." given for do3d_comp_prec(...)   ||  ||
    144 ||[=#PA0129 PA0120]   ||unknown value for data_output_format "..."   ||  ||
    145 ||[=#PA0121 PA0121]   ||km_constant = ... < 0.0   ||  ||
    146 ||[=#PA0122 PA0122]   ||prandtl_number = ... < 0.0   ||  ||
    147 ||[=#PA0123 PA0123]   ||prandtl_layer is not allowed with fixed value of km   ||  ||
     144||[=#PA0129 PA0120]   ||unknown value for data_output_format "..."   ||The string(s) given in [../d3par#data_output_format data_output_format] have to be 'netcdf' or 'avs'. Note that 'avs' is an old data format that is not supported anymore. It is recommended to use the netcdf format. ||
     145||[=#PA0121 PA0121]   ||km_constant = ... < 0.0   ||The eddy-diffusivity km has to be positive definite. Change the value of  [../inipar#km_constant km_constant] accordingly.   ||
     146||[=#PA0122 PA0122]   ||prandtl_number = ... < 0.0   ||The Prandtl number Pr has to be positive definite. Change the value of  [../inipar#prandtl_number prandtl_number] accordingly.  ||
     147||[=#PA0123 PA0123]   ||prandtl_layer is not allowed with fixed value of km   ||For laminar flows with a constant eddy diffusivity  [../inipar#km_constant km_constant]=.T., the Prandtl layer has to be switched of via [../inipar#prandtl_layer prandtl_layer]=.T.. ||
    148148{{{#!tr
    149149   {{{#!td
     
    165165   }}}
    166166}}}
    167 ||[=#PA0125 PA0125]   ||rif_min = ... must be less than rif_max = ...   ||  ||
    168 ||[=#PA0126 PA0126]   ||disturbance_level_b = ... must be >= ... (zu(3))    ||  ||
    169 ||[=#PA0127 PA0127]   ||disturbance_level_b = ... must be <= ... (zu(nzt-2))    ||  ||
    170 ||[=#PA0128 PA0128]   ||disturbance_level_t = ... must be <= ... (zu(nzt-2))    ||  ||
    171 ||[=#PA0129 PA0129]   ||disturbance_level_t = ... must be >= disturbance_level_b = ...    ||  ||
    172 ||[=#PA0130 PA0130]   ||disturbance_level_ind_t =... must be >= disturbance_level_b = ...    ||  ||
     167||[=#PA0125 PA0125]   ||rif_min = ... must be less than rif_max = ...   ||The flux-Richardson number which is calculated interactively in PALM can be limited to prevent reaching unrealistic values under certain circumstances. Make sure that [../inipar#rif_min rif_min] is smaller than  [../inipar#rif_max rif_max]. ||
     168||[=#PA0126 PA0126]   ||disturbance_level_b = ... must be >= ... (zu(3))    ||Due to technical reasons the lower disturbance level given by [../inipar#disturbance_level_b disturbance_level_b] has to be larger than zu(3). ||
     169||[=#PA0127 PA0127]   ||disturbance_level_b = ... must be <= ... (zu(nzt-2))    ||Due to technical reasons the lower disturbance level given by [../inipar#disturbance_level_b disturbance_level_b] has to be smaller than zu(nzt-2).   ||
     170||[=#PA0128 PA0128]   ||disturbance_level_t = ... must be <= ... (zu(nzt-2))    ||Due to technical reasons the upper disturbance level given by [../inipar#disturbance_level_t disturbance_level_t] has to be smaller than zu(nzt-2).  ||
     171||[=#PA0129 PA0129]   ||disturbance_level_t = ... must be >= disturbance_level_b = ...    ||Ensure that [../inipar#disturbance_level_t disturbance_level_t]  is larger than [../inipar#disturbance_level_b disturbance_level_b] to obtain at least one layer where disturbances are added. ||
     172||[=#PA0130 PA0130]   ||disturbance_level_ind_t =... must be >= disturbance_level_b = ...    ||This error may occur when the lower and upper disturbance levels [../inipar#disturbance_level_b disturbance_level_b]  and [../inipar#disturbance_level_t disturbance_level_t]  are calculated automatically and there are two few grid points in the vertical direction. There have to be at least seven vertical levels. ||
    173173||[=#PA0131 PA0131]   ||inflow_disturbance_begin out of range    || The parameter [../inipar#inflow_disturbance_begin inflow_disturbance_begin] gives the number of grid points (counted horizontally from the inflow) from which on perturbations are imposed on the horizontal velocity field. This value must not be smaller than zero or larger than nx (in case of non-cyclic lateral boundary conditions along the x-direction) or ny (in case of non-cyclic lateral boundary conditions along the y-direction). ||
    174174||[=#PA0132 PA0132]   ||inflow_disturbance_end out of range    || The parameter [../inipar#inflow_disturbance_end inflow_disturbance_end] gives the number of grid points (counted horizontally from the inflow) up to which perturbations are imposed on the horizontal velocity field. This value must not be smaller than zero or larger than nx (in case of non-cyclic lateral boundary conditions along the x-direction) or ny (in case of non-cyclic lateral boundary conditions along the y-direction). ||