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| | 350 | || [../sppar#skip_time_dosp skip_time_dosp] || P || output || R || \ |
| | 351 | || value of [../d3par#skip_time_data_output skip_time] \\ [../d3par#skip_time_data_output _data_output] || \ |
| | 352 | || No output of spectra data before this interval has passed (in s). || |
| | 353 | || [../d3par#skip_time_do2d_xy skip_time_do2d_xy] || R || output || R || \ |
| | 354 | || value of [../d3par#skip_time_data_output skip_time] \\ [../d3par#skip_time_data_output _data_output] || \ |
| | 355 | || No output of instantaneous horizontal cross section data before this interval has passed (in s). || |
| | 356 | || [../d3par#skip_time_do2d_xz skip_time_do2d_xz] || R || output || R || \ |
| | 357 | || value of [../d3par#skip_time_data_output skip_time] \\ [../d3par#skip_time_data_output _data_output] || \ |
| | 358 | || No output of instantaneous vertical (xz) cross section data before this interval has passed (in s). || |
| | 359 | || [../d3par#skip_time_do2d_yz skip_time_do2d_yz] || R || output || R || \ |
| | 360 | || value of [../d3par#skip_time_data_output skip_time] \\ [../d3par#skip_time_data_output _data_output] || \ |
| | 361 | || No output of instantaneous vertical (yz) cross section data before this interval has passed (in s). || |
| | 362 | || [../d3par#skip_time_do3d skip_time_do3d] || R || output || R || \ |
| | 363 | || value of [../d3par#skip_time_data_output skip_time] \\ [../d3par#skip_time_data_output _data_output] || \ |
| | 364 | || No output of instantaneous 3d volume data before this interval has passed (in s). || |
| | 365 | || [../dvrpar#slicer_range_limits_dvrp slicer_range_limits_dvrp] || P || dvr || R(2,10) || 10*(-1,1) || \ |
| | 366 | || Ranges of values to which a color table has to be mapped (units of the respective quantity). || |
| | 367 | || [../sppar#spectra_direction spectra_direction] || P || output || C*2(10) || 10*' ' || Direction(s) along which spectra are to be calculated. || |
| | 368 | || [../d3par#statistic_regions statistic_regions] || I || output || I || 0 || \ |
| | 369 | || Number of additional user-defined subdomains for which statistical analysis and corresponding output (profiles, time series) shall be made. || |
| | 370 | || [../dvrpar#superelevation superelevation] || P || dvr || R || 1.0 || Superelevation factor for the vertical coordinate. || |
| | 371 | || [../dvrpar#superelevation_x superelevation_x] || P || dvr || R || 1.0 || Superelevation factor for the horizontal (x) coordinate. || |
| | 372 | || [../dvrpar#superelevation_y superelevation_y] || P || dvr || R || 1.0 || Superelevation factor for the horizontal (y) coordinate. || |
| | 373 | || [../inipar#surface_heatflux surface_heatflux] || I || bc || R || no prescribed heatflux || \ |
| | 374 | || Kinematic sensible heat flux at the bottom surface (in K m/s). || |
| | 375 | || [../inipar#surface_pressure surface_pressure] || I || ini || R || 1013.25 || Atmospheric pressure at the surface (in hPa). || |
| | 376 | || [../inipar#surface_scalarflux surface_scalarflux] || I || bc || R || 0.0 || Scalar flux at the surface (in kg/(m^2^s)). || |
| | 377 | || [../inipar#surface_waterflux surface_waterflux] || I || bc || R || 0.0 || Kinematic water flux near the surface (in m/s). || |
| | 378 | || [../inipar#s_surface s_surface] || I || ini || R || 0.0 || Surface value of the passive scalar (in kg/m^3^). || |
| | 379 | || [../inipar#s_surface_initial_change s_surface_initial_change] || I || ini || R || 0.0 || \ |
| | 380 | || Change in surface scalar concentration to be made at the beginning of the 3d run (in kg/m^3^). || |
| | 381 | || [../inipar#s_vertical_gradient s_vertical_gradient] || I || ini || R(10) || 10*0.0 || \ |
| | 382 | || Scalar concentration gradient(s) of the initial scalar concentration profile (in kg/m^3^ / 100 m). || |
| | 383 | || [../inipar#s_vertical_gradient_level s_vertical_gradient_level] || I || ini || R(10) || 10*0.0 || \ |
| | 384 | || Height level from which on the scalar gradient defined by [../inipar#s_vertical_gradient s_vertical_gradient] is effective (in m). || |
| | 385 | || [../d3par#termination_time_needed termination_time_needed] [=#t] || R || run steering || R || 35.0 || \ |
| | 386 | || CPU time needed for terminal actions at the end of a run in batch mode (in s). || |
| | 387 | || [../dvrpar#threshold threshold] || P || dvr || R(10) || 0.0 || \ |
| | 388 | || Threshold value for which an isosurface is to be created by the '''dvrp''' software. || |
| | 389 | || [../inipar#timestep_scheme timestep_scheme] || I || num || C*20 || 'runge-kutta-3' || \ |
| | 390 | || Time step scheme to be used for integration of the prognostic variables. || |
| | 391 | || [../inipar#topography topography] || I || topo || C*40 || 'flat' || Topography mode. || |
| | 392 | || [../dvrpar#topography_color topography_color] || P || dvr || R(3) || 0.8, 0.7, 0.6 || Color of the topography. || |
| | 393 | || [../inipar#topography_grid_convention topography_grid_convention] || I || topo || C*11 || \ |
| | 394 | || default depends on \\ value of [../inipar#topography topography] || Convention for defining the topography grid. || |
| | 395 | || [../inipar#top_heatflux top_heatflux] || I || bc || R || no prescribed heatflux || Kinematic sensible heat flux at the top surface (in K m/s). || |
| | 396 | || [../inipar#top_momentumflux_u top_momentumflux_u] || I || bc || R || no prescribed momentumflux || \ |
| | 397 | || Momentum flux along x at the top boundary (in m^2^/s^2^). || |
| | 398 | || [../inipar#top_momentumflux_v top_momentumflux_v] || I || bc || R || no prescribed momentumflux || \ |
| | 399 | || Momentum flux along y at the top boundary (in m^2^/s^2^). || |
| | 400 | || [../inipar#top_salinityflux top_salinityflux] || I || bc || R || no prescribed salinityflux || \ |
| | 401 | || Kinematic salinity flux at the top boundary, i.e. the sea surface (in psu m/s). || |
| | 402 | || [../inipar#turbulent_inflow turbulent_inflow] || I || bc || L || .F. || \ |
| | 403 | || Generates a turbulent inflow at side boundaries using a turbulence recycling method. || |
| | 404 | || [../inipar#u_bulk u_bulk] [=#u] || I || mode || R || 0.0 || u-component of the predefined bulk velocity (in m/s). || |
| | 405 | || [../inipar#ug_surface ug_surface] || I || ini || R || 0.0 || u-component of the geostrophic wind at the surface (in m/s). || |
| | 406 | || [../inipar#ug_vertical_gradient ug_vertical_gradient] || I || ini || R(10) || 10*0.0 || \ |
| | 407 | || Gradient(s) of the initial profile of the u-component of the geostrophic wind (in 1/100s). || |
| | 408 | || [../inipar#ug_vertical_gradient_level ug_vertical_gradient_level] || I || ini || R(10) || 10*0.0 || \ |
| | 409 | || Height level from which on the gradient defined by [../inipar#ug_vertical_gradient ug_vertical_gradient] is effective (in m). || |
| | 410 | || [../parpar#use_particle_tails use_particle_tails] || P || particles || L || .F. || Give particles a tail. || |
| | 411 | || [../d3par#use_prior_plot1d_parameters use_prior_plot1d_parameters] || R || output || L || .F. || \ |
| | 412 | || Additional plot of vertical profile data with '''profil''' from preceding runs of the job chain. || |
| | 413 | || [../parpar#use_sgs_for_particles use_sgs_for_particles] || P || particles || L || .F. || Use subgrid-scale velocities for particle advection. || |
| | 414 | || [../inipar#use_surface_fluxes use_surface_fluxes] || I || bc || L || .F. || \ |
| | 415 | || Parameter to steer the treatment of the subgrid-scale vertical fluxes within the diffusion terms at k=1 (bottom boundary). || |
| | 416 | || [../inipar#use_top_fluxes use_top_fluxes] || I || bc || L || .F. || \ |
| | 417 | || Parameter to steer the treatment of the subgrid-scale vertical fluxes within the diffusion terms at k=nz (top boundary). || |
| | 418 | || [../inipar#use_ug_for_galilei_tr use_ug_for_galilei_tr] || I || mode || L || .T. || \ |
| | 419 | || Switch to determine the translation velocity in case that a Galilean transformation is used. || |
| | 420 | || [../inipar#use_upstream_for_tke use_upstream_for_tke] || I || num || L || .F. || \ |
| | 421 | || Parameter to choose the advection/timestep scheme to be used for the subgrid-scale TKE. || |
| | 422 | || [../parpar#vertical_particle_advection vertical_particle_advection] [=#v] || P || particles || L || .T. || \ |
| | 423 | || Switch on/off vertical particle transport. || |
| | 424 | || [../inipar#v_bulk v_bulk] || I || mode || R || 0.0 || v-component of the predefined bulk velocity (in m/s). || |
| | 425 | || [../inipar#vg_surface vg_surface] || I || ini || R || 0.0 || v-component of the geostrophic wind at the surface (in m/s). || |
| | 426 | || [../inipar#vg_vertical_gradient vg_vertical_gradient] || I || ini || R(10) || 10*0.0 || \ |
| | 427 | || Gradient(s) of the initial profile of the v-component of the geostrophic wind (in 1/100s). || |
| | 428 | || [../inipar#vg_vertical_gradient_level vg_vertical_gradient_level] || I || ini || R(10) || 10*0.0 || \ |
| | 429 | || Height level from which on the gradient defined by [../inipar#vg_vertical_gradient vg_vertical_gradient] is effective (in m). || |
| | 430 | || [../inipar#wall_adjustment wall_adjustment] [=#w] || I || bc || L || .T. || \ |
| | 431 | || Parameter to restrict the mixing length in the vicinity of the bottom boundary (and near vertical walls of a non-flat [../inipar#topography topography]). || |
| | 432 | || [../inipar#wall_heatflux wall_heatflux] || I || topo || R(5) || 5*0.0 || \ |
| | 433 | || Prescribed kinematic sensible heat flux in K m/s at the five topography faces. || |
| | 434 | || [../inipar#wall_humidityflux wall_humidityflux] || I || topo || R(5) || 5*0.0 || \ |
| | 435 | || Prescribed kinematic humidtiy flux in m/s at the five topography faces. || |
| | 436 | || [../inipar#wall_scalarflux wall_scalarflux] || I || topo || R(5) || 5*0.0 || Prescribed scalar flux in kg/(m^2^ s) at the five topography faces. || |
| | 437 | || [../inipar#ws_vertical_gradient ws_vertical_gradient] || I || mode || R(10) || 10*0.0 || \ |
| | 438 | || Gradient(s) of the profile for the large scale subsidence/ascent velocity in ((m/s) / 100 m). || |
| | 439 | || [../inipar#ws_vertical_gradient_level ws_vertical_gradient_level] || I || mode || R(10) || 10*0.0 || \ |
| | 440 | || Height level from which on the gradient for the subsidence/ascent velocity defined by [../inipar#ws_vertical_gradient ws_vertical_gradient] is effective (in m). || |
| | 441 | || [../parpar#write_particle_statistics write_particle_statistics] || P || particles || L || .F. || Switch on/off output of particle informations. || |
| | 442 | || [../d3par#z_max_do1d z_max_do1d] || R || output || R || zu(nzt+1) (model top) || \ |
| | 443 | || Height level up to which horizontally averaged profiles are to be plotted with '''profil''' (in m). || |
| | 444 | || [../d3par#z_max_do1d_normalized z_max_do1d_normalized] || R || output || R || determined by plot \\ data || \ |
| | 445 | || Normalized height level up to which horizontally averaged profiles are to be plotted with '''profil'''. || |
| | 446 | || [../d3par#z_max_do2d z_max_do2d] || R || output || R || zu(nz) || \ |
| | 447 | || Height level up to which 2d cross sections are to be plotted with '''iso2d''' (in m). || |
