Changes between Version 172 and Version 173 of doc/app/parlist
- Timestamp:
- Jul 2, 2015 1:29:23 PM (10 years ago)
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doc/app/parlist
v172 v173 227 227 || [../inipar#lad_vertical_gradient lad_vertical_gradient] || I || canopy || R(10) || 10*0.0 || Gradient(s) of the leaf area density (in m^2^/m^4^). || 228 228 || [../inipar#lad_vertical_gradient_level lad_vertical_gradient] \\ [../inipar#lad_vertical_gradient_level _level] || I || canopy || R(10) || 10*0.0 || \ 229 || Height level from which onthe gradient of the leaf area density defined by [../inipar#lad_vertical_gradient lad_vertical_gradient] is effective (in m). ||229 || Height level above which the gradient of the leaf area density defined by [../inipar#lad_vertical_gradient lad_vertical_gradient] is effective (in m). || 230 230 || [../canpar#lai_beta lai_beta] || C || canopy || R || 0.0 || \ 231 231 || Leaf area index needed for construction of leaf area density profile. || … … 343 343 || Temperature gradient(s) of the initial temperature profile (in K / 100 m). || 344 344 || [../inipar#pt_vertical_gradient_level pt_vertical_gradient] \\ [../inipar#pt_vertical_gradient_level _level] || I || ini || R(10) || 10*0.0 || \ 345 || Height level from which onthe temperature gradient defined by [../inipar#pt_vertical_gradient pt_vertical_gradient] is effective (in m). ||345 || Height level above which the temperature gradient defined by [../inipar#pt_vertical_gradient pt_vertical_gradient] is effective (in m). || 346 346 || [../inipar#q_surface q_surface] [=#q] || I || ini || R || 0.0 || Surface specific humidity / total water content (kg/kg). || 347 347 || [../inipar#q_surface_initial_change q_surface_initial] \\ [../inipar#q_surface_initial_change _change] || I || ini || R || 0.0 || \ … … 350 350 || Humidity gradient(s) of the initial humidity profile (in 1/100 m). || 351 351 || [../inipar#q_vertical_gradient_level q_vertical_gradient] \\ [../inipar#q_vertical_gradient_level _level] || I || ini || R(10) || 10*0.0 || \ 352 || Height level from which onthe humidity gradient defined by [../inipar#q_vertical_gradient q_vertical_gradient] is effective (in m). ||352 || Height level above which the humidity gradient defined by [../inipar#q_vertical_gradient q_vertical_gradient] is effective (in m). || 353 353 || [../inipar#radiation radiation] [=#r] || I || mode || L || .F. || Parameter to switch on longwave radiation cooling at cloud-tops. || 354 354 || [../parpar#radius radius] || P || particles || R(10) || 0.0, 9* \\ 9999999.9 || Particle radius (in m). || … … 383 383 || Salinity gradient(s) of the initial salinity profile (in psu / 100 m). || 384 384 || [../inipar#sa_vertical_gradient_level sa_vertical_gradient] \\ [../inipar#sa_vertical_gradient_level _level] || I || bc || R(10) || 10*0.0 || \ 385 || Height level from which onthe salinity gradient defined by [../inipar#sa_vertical_gradient sa_vertical_gradient] is effective (in m). ||385 || Height level above which the salinity gradient defined by [../inipar#sa_vertical_gradient sa_vertical_gradient] is effective (in m). || 386 386 || [../inipar#scalar_advec scalar_advec] || I || num || C*10 || 'pw-scheme' || Advection scheme to be used for the scalar quantities. || 387 387 || [../inipar#scalar_rayleigh_damping scalar_rayleigh] \\ [../inipar#scalar_rayleigh_damping _damping] || I || num || L || .T. || \ … … 428 428 || Gradient(s) of the profile for the large scale subsidence/ascent velocity in ((m/s) / 100 m). || 429 429 || [../inipar#subs_vertical_gradient_level subs_vertical_gradient] \\ [../inipar#subs_vertical_gradient_level _level] || I || mode || R(10) || 10*0.0 || \ 430 || Height level from which onthe gradient for the subsidence/ascent velocity defined by [../inipar#subs_vertical_gradient subs_vertical_gradient] is effective (in m). ||430 || Height level above which the gradient for the subsidence/ascent velocity defined by [../inipar#subs_vertical_gradient subs_vertical_gradient] is effective (in m). || 431 431 || [../dvrpar#superelevation superelevation] || P || dvr || R || 1.0 || Superelevation factor for the vertical coordinate. || 432 432 || [../dvrpar#superelevation_x superelevation_x] || P || dvr || R || 1.0 || Superelevation factor for the horizontal (x) coordinate. || … … 444 444 || Scalar concentration gradient(s) of the initial scalar concentration profile (in kg/m^3^ / 100 m). || 445 445 || [../inipar#s_vertical_gradient_level s_vertical_gradient] \\ [../inipar#s_vertical_gradient_level _level] || I || ini || R(10) || 10*0.0 || \ 446 || Height level from which onthe scalar gradient defined by [../inipar#s_vertical_gradient s_vertical_gradient] is effective (in m). ||446 || Height level above which the scalar gradient defined by [../inipar#s_vertical_gradient s_vertical_gradient] is effective (in m). || 447 447 || [../d3par#termination_time_needed termination_time] [=#t] \\ [../d3par#termination_time_needed _needed] || R || run steering || R || 35.0 || \ 448 448 || CPU time needed for terminal actions at the end of a run in batch mode (in s). || … … 473 473 || Gradient(s) of the initial profile of the u-component of the geostrophic wind (in 1/100s). || 474 474 || [../inipar#ug_vertical_gradient_level ug_vertical_gradient] \\ [../inipar#ug_vertical_gradient_level _level] || I || ini || R(10) || 10*0.0 || \ 475 || Height level from which onthe gradient defined by [../inipar#ug_vertical_gradient ug_vertical_gradient] is effective (in m). ||475 || Height level above which the gradient defined by [../inipar#ug_vertical_gradient ug_vertical_gradient] is effective (in m). || 476 476 || [../inipar#uv_heights uv_heights] || I || ini || R(100) || 100 * 9999999.9 || Height levels for prescribed u,v-profiles (in m). || 477 477 || [../inipar#use_cmax use_cmax] || I || bc || L || .T. || Parameter to choose calculation method of the phase velocity in case of radiation boundary conditions. || … … 497 497 || Gradient(s) of the initial profile of the v-component of the geostrophic wind (in 1/100s). || 498 498 || [../inipar#vg_vertical_gradient_level vg_vertical_gradient] \\ [../inipar#vg_vertical_gradient_level _level] || I || ini || R(10) || 10*0.0 || \ 499 || Height level from which onthe gradient defined by [../inipar#vg_vertical_gradient vg_vertical_gradient] is effective (in m). ||499 || Height level above which the gradient defined by [../inipar#vg_vertical_gradient vg_vertical_gradient] is effective (in m). || 500 500 || [../inipar#wall_adjustment wall_adjustment] [=#w] || I || bc || L || .T. || \ 501 501 || Parameter to restrict the mixing length in the vicinity of the bottom boundary (and near vertical walls of a non-flat [../inipar#topography topography]). ||
