Changes between Version 839 and Version 840 of doc/app/errmsg

Timestamp:

Nov 8, 2022 5:00:07 PM (2 years ago)

Author:

suehring

Comment:

--

doc/app/errmsg

@@ -688 +688 @@
 ||[=#PA0465 PA0465]   || surface_type = netcdf requires static input file.  || Either provide the file [../iofiles#PIDS_STATIC PIDS_STATIC] or change the value of [../land_surface_parameters#surface_type surface_type] to a value different than netcdf. ||
 ||[=#PA0466 PA0466]   || wrong component of wave breaking: ...  || Only the two Cartesian components 1 and 2 are allowed for adding wave breaking effects in ocean mode. ||
-||[=#PA0467 PA0467]   || y_shift /= 0 is only allowed for cyclic boundary conditions in both directions or with turbulent_inflow_method = 'recycle_...'. || y_shift defines a shift in the cyclic boundary conditions. It can therefore only be used with cyclic boundary conditions or with the the turbulence recycling method. See [../initialization_parameters#y_shift y_shift]. ||
+||[=#PA0467 PA0467]   || y_shift /= 0 is only allowed for cyclic boundary conditions in both directions or with turbulent_inflow_method = 'recycle_...'. || y_shift defines a shift in the cyclic boundary conditions. It can therefore only be used with cyclic boundary conditions or with the turbulence recycling method. See [../initialization_parameters#y_shift y_shift]. ||
 ||[=#PA0468 PA0468]   || y_shift /= 0 is only allowed for multigrid pressure solvers  || y_shift defines a shift in the cyclic boundary conditions. The data then becomes not truly cyclic anymore. Therefore, the fft pressure solver is no longer viable. See [../initialization_parameters#y_shift y_shift]. ||
 ||[=#PA0469 PA0469]   || unknown aerosol species for bulk microphysics  || aerosol species must be set to a known type. See [../initialization_parameters#aerosol_bulk aerosol_bulk]. ||
@@ -912 +912 @@
 ||[=#PA0701 PA0701]  || A constant flux layer is not allowed if a closed channel shall be used || So far, the constant flux layer approach is only implemented for the bottom boundary but bottom and top boundary shall be treated equal for closed channel flows. Therefore, it is not allowed. ||
 ||[=#PA0702 PA0702]  || The ocean mode is not allowed if a closed channel shall be used || self-explanatory ||
-||[=#PA0703 PA0703]  || A closed channel requires the upwind scheme of Wicker and Skamarock as the advection scheme || Only the the upwind scheme of Wicker and Skamarock is realized and tested for a symmetric degradation of the advection scheme (from 5th, to 3rd to 1st order) close to the bottom and top boundary.  ||
+||[=#PA0703 PA0703]  || A closed channel requires the upwind scheme of Wicker and Skamarock as the advection scheme || Only the upwind scheme of Wicker and Skamarock is realized and tested for a symmetric degradation of the advection scheme (from 5th, to 3rd to 1st order) close to the bottom and top boundary.  ||
 ||[=#PA0704 PA0704]  || End of line or file detected for file [../iofiles#TOPOGRAPHY_DATA TOPOGRAPHY_DATA] at line ...  ||File does not contain enough data. Check the respective line given in the error message. \\ a) The number of columns (`ncols`) is less than [../initialization_parameters#nx nx]+1. \\ b) The number of rows (`nrows`) is less than [../initialization_parameters#ny ny]+1. \\ Solution: Make sure that `ncols` matches `nx+1` and that `nrows` matches `ny+1`.   ||
 ||[=#PA0705 PA0705]  || If virtual measurements are taken, the number of surrounding grid points must not be larger than the number of ghost points - 1 ||When virtual measurements are taken, data is sampled at given station grid coordinates. It is possible that also the adjoining grid points can be sampled, however, the number of grid points additionally sampled in each direction must not be larger than the number of ghost points - 1 to avoid any segmentations faults. In the future we will improve this to allow a more flexible number of offset grid points. ||