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Changes between Version 360 and Version 361 of doc/app/initialization_parameters


Ignore:
Timestamp:
Aug 29, 2017 3:06:02 PM (7 years ago)
Author:
schwenkel
Comment:

--

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  • doc/app/initialization_parameters

    v360 v361  
    2020|----------------
    2121{{{#!td style="vertical-align:top;width: 150px"
    22 [=#aerosol_bulk '''aerosol_bulk''']
    23 }}}
    24 {{{#!td style="vertical-align:top;width: 50px"
    25 C*20
    26 }}}
    27 {{{#!td style="vertical-align:top;width: 75px"
    28 'nacl'
    29 }}}
    30 {{{#!td
    31 Parameter to choose the used aerosol type. Currently three approximations are available:\\\\
    32 '' 'nacl' ''\\
    33       It is assumed that the aerosol is nacl. \\\\
    34 '' 'c3h4o4' '' \\
    35       It is assumed that the aerosol is malonic acid.\\\\
    36 '' 'nh4no3' '' \\
    37       It is assumed that the aerosol is ammonium sulfate. \\\\
    38 The molecular weight, denisty and the solubility (vant Hoff factor)  of this specific type is considered.
    39 }}}
    40 |----------------
    41 {{{#!td style="vertical-align:top;width: 150px"
    4222[=#approximation '''approximation''']
    4323}}}
    … …  
    176156Simulation time of precursor run.\\\\
    177157Sets the time period a precursor run shall run uncoupled. This parameter is used to set up the precursor run control for atmosphere-ocean-coupled runs. It has to be set individually to the atmospheric / oceanic precursor run. The time in the data output will show negative values during the precursor run. See [[app/examples/coupled#precursur_runs| coupled runs]] for further information.
    178 }}}
    179 |----------------
    180 {{{#!td style="vertical-align:top"
    181 [=#curvature_solution_effects_bulk '''curvature_solution_effects_bulk''']
    182 }}}
    183 {{{#!td style="vertical-align:top"
    184 L
    185 }}}
    186 {{{#!td style="vertical-align:top"
    187 .F.
    188 }}}
    189 {{{#!td
    190 Parameter to switch on an activation scheme which considers curvature and solution effects of cloud droplet activation. Therefore a parameterization of Khvorostyanov and Curry, 2006 is used. The physio-chemical aerosol properties can be prescribed with [#aerosol_bulk aerosol_bulk], [#dry_aerosol_radius dry_aerosol_radius] and [#sigma_bulk sigma_bulk].
    191158}}}
    192159|----------------
    … …  
    17911758This parameter only comes into effect for ocean runs (see parameter [#ocean ocean]).\\\\
    17921759The height levels have to be assigned in descending order. The default values result in a constant salinity profile regardless of the values of sa_vertical_gradient (unless the bottom boundary of the model is lower than -100000.0 m). For the piecewise construction of salinity profiles see [#sa_vertical_gradient sa_vertical_gradient].
    1793 }}}
    1794 |----------------
    1795 {{{#!td style="vertical-align:top"
    1796 [=#sigma_bulk '''sigma_bulk''']
    1797 }}}
    1798 {{{#!td style="vertical-align:top"
    1799 R
    1800 }}}
    1801 {{{#!td style="vertical-align:top"
    1802 2.0
    1803 }}}
    1804 {{{#!td
    1805 The dispersion of the dry aerosol spectrum.
    18061760}}}
    18071761|----------------
    … …  
    30382992|----------------
    30392993{{{#!td style="vertical-align:top;width: 150px"
     2994[=#aerosol_bulk '''aerosol_bulk''']
     2995}}}
     2996{{{#!td style="vertical-align:top;width: 50px"
     2997C*20
     2998}}}
     2999{{{#!td style="vertical-align:top;width: 75px"
     3000'nacl'
     3001}}}
     3002{{{#!td
     3003Parameter to choose the used aerosol type. Currently three approximations are available:\\\\
     3004'' 'nacl' ''\\
     3005      It is assumed that the aerosol is nacl. \\\\
     3006'' 'c3h4o4' '' \\
     3007      It is assumed that the aerosol is malonic acid.\\\\
     3008'' 'nh4no3' '' \\
     3009      It is assumed that the aerosol is ammonium sulfate. \\\\
     3010The molecular weight, denisty and the solubility (vant Hoff factor)  of this specific type is considered.
     3011}}}
     3012|----------------
     3013{{{#!td style="vertical-align:top;width: 150px"
    30403014[=#call_microphysics_at_all_substeps '''call_microphysics_at_all_substeps''']
    30413015}}}
    … …  
    30673041}}}
    30683042|----------------
     3043{{{#!td style="vertical-align:top"
     3044[=#curvature_solution_effects_bulk '''curvature_solution_effects_bulk''']
     3045}}}
     3046{{{#!td style="vertical-align:top"
     3047L
     3048}}}
     3049{{{#!td style="vertical-align:top"
     3050.F.
     3051}}}
     3052{{{#!td
     3053Parameter to switch on an activation scheme which considers curvature and solution effects of cloud droplet activation. Therefore a parameterization of Khvorostyanov and Curry, 2006 is used. The physio-chemical aerosol properties can be prescribed with [#aerosol_bulk aerosol_bulk], [#dry_aerosol_radius dry_aerosol_radius] and [#sigma_bulk sigma_bulk].
     3054}}}
     3055|----------------
    30693056{{{#!td style="vertical-align:top;width: 150px"
    30703057[=#cloud_water_sedimentation '''cloud_water_sedimentation''']
    … …  
    31003087|----------------
    31013088{{{#!td style="vertical-align:top;width: 150px"
     3089[=#na_init '''na_init''']
     3090}}}
     3091{{{#!td style="vertical-align:top;width: 50px"
     3092R
     3093}}}
     3094{{{#!td style="vertical-align:top;width: 75px"
     3095100.0E6
     3096}}}
     3097{{{#!td
     3098Background dry aerosol concentration. If [#cloud_scheme cloud_scheme] = 'morrison' is used this parameter replaces [#nc_const nc_const]. Activation is parameterized assuming that the number of activated CCN cannot be larger than na_init.
     3099This parameter only comes into effect if the microphysical cloud scheme according to Morrison and Grabowski (2007) is used ([#cloud_scheme cloud_scheme] = 'morrison').
     3100}}}
     3101|----------------
     3102{{{#!td style="vertical-align:top;width: 150px"
    31023103[=#nc_const '''nc_const''']
    31033104}}}
    … …  
    31273128
    31283129This parameter only comes into effect if the microphysical cloud scheme according to Seifert and Beheng (2006) is used ([#cloud_scheme cloud_scheme] = 'seifert_beheng').
     3130}}}
     3131|----------------
     3132{{{#!td style="vertical-align:top"
     3133[=#sigma_bulk '''sigma_bulk''']
     3134}}}
     3135{{{#!td style="vertical-align:top"
     3136R
     3137}}}
     3138{{{#!td style="vertical-align:top"
     31392.0
     3140}}}
     3141{{{#!td
     3142The dispersion of the dry aerosol spectrum.
    31293143}}}
    31303144|----------------
                                                                                                                                                                                                                                                                                                                                                                               
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