Changes between Version 462 and Version 463 of doc/app/errmsg

Timestamp:

Jul 14, 2017 5:04:44 PM (8 years ago)

Author:

hoffmann

Comment:

--

doc/app/errmsg

@@ -426 +426 @@
 ||[=#PA0347 PA0347]   ||maxtry > 40 in Rosenbrock method ||Error may appear if curvature and solution effects are included in the calculation of droplet growth by condensation (see [../inipar#curvature_solution_effects curvature_solution effects]. \\\\It means that the Rosenbrock method, used for integrating the stiff droplet growth equation, was unable to find an internal timestep which gives a sufficiently small truncation error within 40 tries. \\\\So far, this problem has not appeared. It might happen if some of the cloud physics parameters, which determine the growth by condensation, are given unrealistic values or if the droplet radius is extremely small. ||
 ||[=#PA0348 PA0348]   ||zero stepsize in Rosenbrock method ||Error may appear if curvature and solution effects are included in the calculation of droplet growth by condensation (see [../inipar#curvature_solution_effects curvature_solution effects]. \\\\It means that within the Rosenbrock method, used for integrating the stiff droplet growth equation, the internal timestep has become zero, so that the integration cannot be performed. \\\\So far, this problem has not appeared. It might happen if some of the cloud physics parameters, which determine the growth by condensation, are given unrealistic values or if the droplet radius is extremely small. ||
-||[=#PA0349 PA0349]   ||use_sgs_for_particles = .TRUE. not allowed with curvature_solution_effects = .TRUE. ||When Lagrangian particles are used as cloud droplets, they are only allowed to be transported with the resolved-scale flow. The application of the stochastic subgrid-scale transport model is limited to passively advected particles. Since cloud droplets have inertia, a transport with the SGS model would give wrong results.||
+||[=#PA0349 PA0349]   || || Not used anymore. ||
 ||[=#PA0350 PA0350]   ||unknown collision kernel: collision_kernel = "..." ||see package parameter [../parpar#collision_kernel collision_kernel] for allowed values ||
 ||[=#PA0351 PA0351]   ||heatflux must not be set for pure neutral flow ||Inipar parameter [../inipar#neutral neutral] = .TRUE. has been set, but non-zero values for parameters [../inipar#surface_heatflux surface_heatflux] and / or [../inipar#top_heatflux top_heatflux] are given at the same time. This is not allowed for simulating a flow with pure neutral stratification where the temperature equation is switched off. Check your parameter file. ||
@@ -641 +641 @@
 ||[=#PA0418 PA0418]   ||illegal nesting datatransfer mode: ... ||Allowed values for [../nestpar#nesting_datatransfer_mode nesting_datatransfer_mode] are 'cascade', 'mixed' or 'overlap'. ||
 ||[=#PA0419 PA0419]   ||mismatch between root model and client settings \\ <parameter name>(root) = ... \\ <parameter name>(client) = ... \\ client value is set to root value ||The displayed parameter has been assigned different values for the root domain and a client domain (the id of the client domain is listed in the first line of the message) but it must have the same value for all domains. PALM automatically adjusts the client domain value to the one given for the root domain. In order to get rid of this warning message, adjust the parameter in the respective NAMELIST-parameter file of the client (or root) domain.|| 
-||[=#PA0420 PA0420]   ||unknown collision algorithm: collision_algorithm = ... || The allowed values of [../parpar#collision_algrithm collision_algorithm]  are 'all_or_nothing' and 'average_impact'. || 
+||[=#PA0420 PA0420]   ||  || Not used anymore. || 
 ||[=#PA0421 PA0421]   ||recycling_yshift = .T. requires more than one processor in y direction|| The distance of the y-shift is calculated by INT( npey / 2 ). With only one processor in y direction, no y-shift is possible. || 
 ||[=#PA0422 PA0422]   ||data_output_pr = ... is not available for cloud_scheme = saturation_adjust || If the output is not necessary, delete the variable from the namelist. If it is necessary, use [../inipar#cloud_scheme cloud_scheme] = kessler or  seifert_beheng. || 
@@ -680 +680 @@
 ||[=#PA0457 PA0457]   ||NetCDF attribute lod (level of detail) is not set properly.   ||This error can occur when you try to input topography data via NetCDF. Topography input via NetCDF enables one of two different modes. Therefore the variable {{{lod}}} which determines the mode internally can only have the value 1 or 2. For more information see [/wiki/doc/tec/topography#topo topography implementation].  ||
 ||[=#PA0458 PA0458]   || soil_moisture must not exceed its saturation value  ||This error can occur when the soil moisture is higher than the saturation moisture for the given vegetation type. Check and may adjust parameters [../lsmpar#saturation_moisture saturation_moisture] or [../lsmpar#soil_moisture soil_moisture]. ||
+||[=#PA0459 PA0459]   || unknown aerosol type  'aero_type = ...'  ||Chose an appropriate value for [../parpar#aero_type aero_type]. ||
 ||[=#UI0001 UI0001]   ||unknown location "..."   ||The location has to be one of 'before_timestep', 'after_integration', 'after_timestep', 'u_tendency' 'v_tendency', 'w_tendency', 'pt_tendency', 'sa_tendency', 'e_tendency', 'q_tendency', 's_tendency'.  ||
 ||[=#UI0002 UI0002]   ||location "..." is not allowed to be called with parameters "i" and "j"   || ** ||