Changes between Version 42 and Version 43 of doc/app/initialization_parameters


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Timestamp:
Sep 14, 2010 8:21:42 AM (14 years ago)
Author:
kanani
Comment:

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  • doc/app/initialization_parameters

    v42 v43  
    118118      The target volume flow is calculated from a predefined bulk velocity (see [#u_bulk u_bulk] and [#v_bulk v_bulk]). This setting is only allowed for cyclic lateral boundary conditions (bc_lr = '' 'cyclic' '' and bc_ns = '' 'cyclic' '').\\\\
    119119Note that '''conserve_volume_flow_mode''' only comes into effect if [#conserve_volume_flow conserve_volume_flow] = ''.T.''.
     120}}}
     121|----------------
     122{{{#!td style="vertical-align:top"
     123[=#coupling_start_time '''coupling_start_time''']
     124}}}
     125{{{#!td style="vertical-align:top"
     126R
     127}}}
     128{{{#!td style="vertical-align:top"
     1290.0
     130}}}
     131{{{#!td
     132Simulation time of precursor run.\\\\
     133Sets 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 documentation for further information.
     134}}}
     135|----------------
     136{{{#!td style="vertical-align:top"
     137[=#<insert_parameter_name> '''<insert_parameter_name>''']
     138}}}
     139{{{#!td style="vertical-align:top"
     140<insert type>
     141}}}
     142{{{#!td style="vertical-align:top"
     143<insert value>
     144}}}
     145{{{#!td
     146<insert explanation>
     147}}}
     148|----------------
     149{{{#!td style="vertical-align:top"
     150[=#<insert_parameter_name> '''<insert_parameter_name>''']
     151}}}
     152{{{#!td style="vertical-align:top"
     153<insert type>
     154}}}
     155{{{#!td style="vertical-align:top"
     156<insert value>
     157}}}
     158{{{#!td
     159<insert explanation>
     160}}}
     161|----------------
     162{{{#!td style="vertical-align:top"
     163[=#<insert_parameter_name> '''<insert_parameter_name>''']
     164}}}
     165{{{#!td style="vertical-align:top"
     166<insert type>
     167}}}
     168{{{#!td style="vertical-align:top"
     169<insert value>
     170}}}
     171{{{#!td
     172<insert explanation>
    120173}}}
    121174|----------------
     
    740793|----------------
    741794{{{#!td style="vertical-align:top"
    742 [=#<insert_parameter_name> '''<insert_parameter_name>''']
    743 }}}
    744 {{{#!td style="vertical-align:top"
    745 <insert type>
    746 }}}
    747 {{{#!td style="vertical-align:top"
    748 <insert value>
    749 }}}
    750 {{{#!td
    751 <insert explanation>
     795[=#cthf '''cthf''']
     796}}}
     797{{{#!td style="vertical-align:top"
     798R
     799}}}
     800{{{#!td style="vertical-align:top"
     8010.0
     802}}}
     803{{{#!td
     804Average heat flux that is prescribed at the top of the plant canopy.\\\\
     805If [#plant_canopy plant_canopy] is set ''.T.'', the user can prescribe a heat flux at the top of the plant canopy.
     806It is assumed that solar radiation penetrates the canopy and warms the foliage which, in turn, warms the air in contact with it.
     807'''Note:''' Instead of using the value prescribed by [#surface_heatflux surface_heatflux], the near surface heat flux is determined from an exponential function that is dependent on the cumulative leaf_area_index (Shaw and Schumann (1992, Boundary Layer Meteorol., '''61''', 47-64)).
    752808}}}
    753809[[BR]]