Changes between Version 202 and Version 203 of doc/app/parlist


Ignore:
Timestamp:
Jul 4, 2017 2:40:52 PM (8 years ago)
Author:
hoffmann
Comment:

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  • doc/app/parlist

    v202 v203  
    4646|| [../inipar#bc_pt_b bc_pt_b] || ini || Boundary conditions || C*20 || 'dirichlet' || Bottom boundary condition of the potential temperature. ||
    4747|| [../inipar#bc_pt_t bc_pt_t] || ini || Boundary conditions || C*20 || 'initial_gradient' || Top boundary condition of the potential temperature. ||
    48 || [../inipar#bc_q_b bc_q_b] || ini || Boundary conditions || C*20 || 'dirichlet' || Bottom boundary condition of the specific humidity / total water content.  ||
    49 || [../inipar#bc_q_t bc_q_t] || ini || Boundary conditions || C*20 || 'neumann' || Top boundary condition of the specific humidity / total water content. ||
     48|| [../inipar#bc_q_b bc_q_b] || ini || Boundary conditions || C*20 || 'dirichlet' || Bottom boundary condition of the water vapor / total water mixing ratio.  ||
     49|| [../inipar#bc_q_t bc_q_t] || ini || Boundary conditions || C*20 || 'neumann' || Top boundary condition of the water vapor / total water mixing ratio. ||
    5050|| [../inipar#bc_s_b bc_s_b] || ini || Boundary conditions || C*20 || 'dirichlet' || Bottom boundary condition of the scalar concentration.  ||
    5151|| [../inipar#bc_s_t bc_st] || ini || Boundary conditions || C*20 || 'neumann' || Top boundary condition of the scalar concentration.  ||
     
    182182|| [../wind_turbine_par#gen_eff gen_eff] || wtm ||  || R || 0.944 || Electric efficiency of the generator. ||
    183183|| [../dvrpar#groundplate_color groundplate_color] || dvr || || R(3) || 0.0, 0.6, 0.0 || Color of the ground plate. ||
    184 || [../inipar#humidity humidity] [=#h] || ini || Mode || L || .F. || Parameter to switch on the prognostic equation for specific humidity q. ||
     184|| [../inipar#humidity humidity] [=#h] || ini || Mode || L || .F. || Parameter to switch on the prognostic equation for water vapor mixing ratio q. ||
    185185|| [../lsmpar#hydraulic_conductivity hydraulic_conductivity] || lsm ||  || R || depends on [../lsmpar#veg_type veg_type] || Hydraulic conductivity of the soil at saturation (in m/s). ||
    186186|| [../wind_turbine_par#inertia_gen inertia_gen] [=#i] || wtm || || R || 534.116 || Inertia of the generator (in kg/m^2^). ||
     
    309309|| [../inipar#pt_vertical_gradient pt_vertical_gradient] || ini || Initialization || R(10) || 10*0.0 || Temperature gradient(s) of the initial temperature profile (in K / 100 m). ||
    310310|| [../inipar#pt_vertical_gradient_level pt_vertical_gradient] \\ [../inipar#pt_vertical_gradient_level _level] || ini || Initialization || R(10) || 10*0.0 || Height level above which the temperature gradient defined by [../inipar#pt_vertical_gradient pt_vertical_gradient] is effective (in m). ||
    311 || [../inipar#q_surface q_surface] [=#q] || ini || Initialization || R || 0.0 || Surface specific humidity / total water content (kg/kg). ||
    312 || [../inipar#q_surface_initial_change q_surface_initial] \\ [../inipar#q_surface_initial_change _change] || ini || Initialization || R || 0.0 || Change in surface specific humidity / total water content to be made at the beginning of the 3d run (kg/kg). ||
     311|| [../inipar#q_surface q_surface] [=#q] || ini || Initialization || R || 0.0 || Surface water vapor / total water mixing ratio (kg/kg). ||
     312|| [../inipar#q_surface_initial_change q_surface_initial] \\ [../inipar#q_surface_initial_change _change] || ini || Initialization || R || 0.0 || Change in surface water vapor / total water mixing ratio to be made at the beginning of the 3d run (kg/kg). ||
    313313|| [../inipar#q_vertical_gradient q_vertical_gradient] || ini || Initialization || R(10) || 10*0.0 || Humidity gradient(s) of the initial humidity profile (in 1/100 m). ||
    314314|| [../inipar#q_vertical_gradient_level q_vertical_gradient] \\ [../inipar#q_vertical_gradient_level _level] || ini || Initialization || R(10) || 10*0.0 || Height level above which the humidity gradient defined by [../inipar#q_vertical_gradient q_vertical_gradient] is effective (in m). ||