Changes between Version 331 and Version 332 of doc/app/errmsg


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Timestamp:
Jun 7, 2017 9:53:06 AM (8 years ago)
Author:
sward
Comment:

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  • doc/app/errmsg

    v331 v332  
    447447||[=#PA0372 PA0372]   ||No time dependent vertical profiles in LSF_DATA for end of run found ||PALM detected an end-of-file condition for the profile data in [../../app/iofiles#LSF_DATA LSF_DATA] and aborts. Possible reasons could be that no time dependent profile data is provided in the large scale forcing file.   ||
    448448||[=#PA0373 PA0373]   ||Time dependent large scale profile forcing from LSF_DATA sets in after end of simulation - lsf_vert is set to FALSE  ||This messages appears in the case that the first time step of the profile data read in from [../../app/iofiles#LSF_DATA LSF_DATA] is larger than the end time of the simulation. In this case the geostrophic wind profiles and large scale subsidence profile prescribed in [../../app/iofiles#LSF_DATA LSF_DATA] cannot be used. ||
    449 ||[=#PA0374 PA0374]   ||Nudging requires large_scale_forcing = .T.. Surface fluxes and geostrophic wind should be prescribed in file LSF_DATA  ||In order to use nudging it is required to use large_scale_forcing = .T., too. The surface values and profiles needed in [../../app/iofiles#LSF_DATA LSF_DATA] should correspond to the data provided in [../../app/iofiles#NUDGING_DATA NUDGING_DATA].  ||
     449||[=#PA0374 PA0374]   ||Nudging requires large_scale_forcing = .T.. Surface fluxes and geostrophic wind should be prescribed in file LSF_DATA  ||In order to use nudging it is required to use [../inipar#large_scale_forcing large_scale_forcing] = .T., too. The surface values and profiles needed in [../../app/iofiles#LSF_DATA LSF_DATA] should correspond to the data provided in [../../app/iofiles#NUDGING_DATA NUDGING_DATA].  ||
    450450||[=#PA0375 PA0375]   ||Non-cyclic lateral boundaries do not allow for the usage of large scale forcing from external file. ||Large scale [../inipar#large_scale_forcing forcing] (and also nudging) are not implemented/tested for non-cyclic boundary conditions so far.  ||
    451 ||[=#PA0376 PA0376]   ||The usage of large scale forcing from external file LSF_DATA requires humidity = .T.. ||If you want to use [../inipar#large_scale_forcing large_scale_forcing] (and also nudging) from an external file, you need to run PALM with [../inipar#humidity humidity].  ||
     451||[=#PA0376 PA0376]   ||The usage of large scale forcing from external file [../../app/iofiles#LSF_DATA LSF_DATA] requires humidity = .T.. ||If you want to use [../inipar#large_scale_forcing large_scale_forcing] (and also nudging) from an external file, you need to run PALM with [../inipar#humidity humidity].  ||
    452452||[=#PA0377 PA0377]   ||The usage of large scale forcing from external file LSF_DATA is not implemented for non-flat topography  ||Please use [../inipar#topography topography] = 'flat' or refrain from using large scale [../inipar#large_scale_forcing forcing]. ||
    453 ||[=#PA0378 PA0378]   ||The usage of large scale forcing from external file LSF_DATA is not implemented for ocean runs ||Please use [../inipar#ocean ocean] = .F. or refrain from using large scale [../inipar#large_scale_forcing forcing].  ||
     453||[=#PA0378 PA0378]   ||The usage of large scale forcing from external file [../../app/iofiles#LSF_DATA LSF_DATA] is not implemented for ocean runs ||Please use [../inipar#ocean ocean] = .F. or refrain from using large scale [../inipar#large_scale_forcing forcing].  ||
    454454||[=#PA0379 PA0379]   ||   || message number is unused ||
    455455||[=#PA0380 PA0380]   ||There is no default large scale vertical velocity profile set. Specify the subsidence velocity profile via subs_vertical_gradient and  subs_vertical_gradient_level. ||With [../inipar#large_scale_subsidence large_scale_subsidence] = .T. but without [../inipar#large_scale_forcing large_scale_forcing] a profile for the subsidence velocity w_subs has to be prescribed. See [../inipar#subs_vertical_gradient_level subs_vertical_gradient_level]. ||
     
    621621   }}}
    622622}}}
    623 ||[=#PA0395 PA0395]   ||zu(nzt+1) = ... m is higher than the maximum height in LSF_DATA which is ...m. Interpolation on PALM grid is not possible. || {{{LSF_DATA}}} has a maximum vertical height that is smaller than the vertical extent of the grid used in PALM. Hence, interpolation of the {{{LSF_DATA}}} onto the PALM grid is not possible. Reduce either the vertical extent of the PALM modeling domain or enlarge the {{{LSF_DATA}}} file correspondingly.  ||
    624 ||[=#PA0396 PA0396]   ||The usage of use_subsidence_tendencies requires large_scale_subsidence = .T.. || If  [../inipar#use_subsidence_tendencies use_subsidence_tendencies] is used, subsidence tendencies for temperature and humidity are read in from the external file {{{LSF_DATA}}}. However, these tendencies can only be applied to the prognostic variables if [../inipar#large_scale_subsidence large_scale_subsidence] = .T.. ||
    625 ||[=#PA0397 PA0397]   ||The usage of use_subsidence_tendencies requires large_scale_forcing = .T.. || If  [../inipar#use_subsidence_tendencies 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.. ||
     623||[=#PA0395 PA0395]   ||zu(nzt+1) = ... m is higher than the maximum height in LSF_DATA which is ...m. Interpolation on PALM grid is not possible. || [../../app/iofiles#LSF_DATA LSF_DATA] has a maximum vertical height that is smaller than the vertical extent of the grid used in PALM. Hence, interpolation of the [../../app/iofiles#LSF_DATA LSF_DATA] onto the PALM grid is not possible. Reduce either the vertical extent of the PALM modeling domain or enlarge the [../../app/iofiles#LSF_DATA LSF_DATA] file correspondingly.  ||
     624||[=#PA0396 PA0396]   ||The usage of use_subsidence_tendencies requires large_scale_subsidence = .T.. || If  [../inipar#use_subsidence_tendencies use_subsidence_tendencies] is used, subsidence tendencies for temperature and humidity are read in from the external file [../../app/iofiles#LSF_DATA LSF_DATA]. However, these tendencies can only be applied to the prognostic variables if [../inipar#large_scale_subsidence large_scale_subsidence] = .T.. ||
     625||[=#PA0397 PA0397]   ||The usage of use_subsidence_tendencies requires large_scale_forcing = .T.. || If  [../inipar#use_subsidence_tendencies use_subsidence_tendencies] is used, subsidence tendencies for temperature and humidity are read in from the external file [../../app/iofiles#LSF_DATA LSF_DATA]. This requires [../inipar#large_scale_forcing large_scale_forcing] = .T.. ||
    626626||[=#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. ||
    627627||[=#PA0399 PA0399]   ||lsm requires setting of [../inipar#bc_pt_b bc_pt_b] = "dirichlet" and [../inipar#bc_q_b 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. ||