Changes between Version 43 and Version 44 of doc/app/initialization_parameters


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Timestamp:
Sep 14, 2010 8:31:48 AM (14 years ago)
Author:
kanani
Comment:

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  • doc/app/initialization_parameters

    v43 v44  
    172172<insert explanation>
    173173}}}
    174 |----------------
    175 {{{#!td style="vertical-align:top"
    176 [=#<insert_parameter_name> '''<insert_parameter_name>''']
    177 }}}
    178 {{{#!td style="vertical-align:top"
    179 <insert type>
    180 }}}
    181 {{{#!td style="vertical-align:top"
    182 <insert value>
    183 }}}
    184 {{{#!td
    185 <insert explanation>
    186 }}}
    187174[[BR]]
    188175
     
    250237In case of the leapfrog scheme a quite restrictive value of '''cfl_factor''' = ''0.1'' is used because for larger values the velocity divergence significantly effects the accuracy of the model results. Possibly larger values may be used with the leapfrog scheme but these are to be determined by appropriate test runs.\\\\
    251238The default value for the Euler scheme is '''cfl_factor''' = ''0.8.''
     239}}}
     240|----------------
     241{{{#!td style="vertical-align:top"
     242[=#cycle_mg '''cycle_mg''']
     243}}}
     244{{{#!td style="vertical-align:top"
     245C*1
     246}}}
     247{{{#!td style="vertical-align:top"
     248'w'
     249}}}
     250{{{#!td
     251Type of cycle to be used with the multi-grid method.\\\\
     252This parameter determines which type of cycle is applied in the multi-grid method used for solving the Poisson equation for perturbation pressure (see [#psolver psolver]). It defines in which way it is switched between the fine and coarse grids. So-called v- and w-cycles are realized (i.e. '''cycle_m'''g may be assigned the values '' 'v' '' or '' 'w' ''). The computational cost of w-cycles is much higher than that of v-cycles, however, w-cycles give a much better convergence.
     253}}}
     254|----------------
     255{{{#!td style="vertical-align:top"
     256[=#<insert_parameter_name> '''<insert_parameter_name>''']
     257}}}
     258{{{#!td style="vertical-align:top"
     259<insert type>
     260}}}
     261{{{#!td style="vertical-align:top"
     262<insert value>
     263}}}
     264{{{#!td
     265<insert explanation>
     266}}}
     267|----------------
     268{{{#!td style="vertical-align:top"
     269[=#<insert_parameter_name> '''<insert_parameter_name>''']
     270}}}
     271{{{#!td style="vertical-align:top"
     272<insert type>
     273}}}
     274{{{#!td style="vertical-align:top"
     275<insert value>
     276}}}
     277{{{#!td
     278<insert explanation>
     279}}}
     280|----------------
     281{{{#!td style="vertical-align:top"
     282[=#<insert_parameter_name> '''<insert_parameter_name>''']
     283}}}
     284{{{#!td style="vertical-align:top"
     285<insert type>
     286}}}
     287{{{#!td style="vertical-align:top"
     288<insert value>
     289}}}
     290{{{#!td
     291<insert explanation>
     292}}}
     293|----------------
     294{{{#!td style="vertical-align:top"
     295[=#<insert_parameter_name> '''<insert_parameter_name>''']
     296}}}
     297{{{#!td style="vertical-align:top"
     298<insert type>
     299}}}
     300{{{#!td style="vertical-align:top"
     301<insert value>
     302}}}
     303{{{#!td
     304<insert explanation>
    252305}}}
    253306[[BR]]
     
    544597||='''Parameter Name'''  =||='''FORTRAN Type'''  =||='''Default Value'''  =||='''Explanation'''  =||
    545598|----------------
    546 {{{#!td style="vertical-align:top; text-align:left;width: 150px"
    547 [=# '''''']
    548 }}}
    549 {{{#!td style="vertical-align:top; text-align:left;style="width: 50px"
    550 
    551 }}}
    552 {{{#!td style="vertical-align:top; text-align:left;style="width: 100px"
    553 
    554 }}}
    555 {{{#!td
    556 
     599{{{#!td style="vertical-align:top;width: 150px"
     600[=#damp_level_1d '''damp_level_1d''']
     601}}}
     602{{{#!td style="vertical-align:top;width: 50px"
     603R
     604}}}
     605{{{#!td style="vertical-align:top;width: 100px"
     606zu(nz+1)
     607}}}
     608{{{#!td
     609Height where the damping layer begins in the [[1d-model]] (in m).\\\\
     610This parameter is used to switch on a damping layer for the 1d-model, which is generally needed for the damping of inertia oscillations. Damping is done by gradually increasing the value of the eddy diffusivities about 10% per vertical grid level (starting with the value at the height given by '''damp_level_1d''', or possibly from the next grid pint above), i.e. K,,m,,(k+1) = 1.1 * K,,m,,(k). The values of K,,m,, are limited to 10 m^2^/s at maximum.\\\\
     611This parameter only comes into effect if the 1d-model is switched on for the initialization of the 3d-model using [#initializing_actions initializing_actions] = '' 'set_1d-model_profiles'.''
    557612}}}
    558613|----------------
     
    804859Average heat flux that is prescribed at the top of the plant canopy.\\\\
    805860If [#plant_canopy plant_canopy] is set ''.T.'', the user can prescribe a heat flux at the top of the plant canopy.
    806 It is assumed that solar radiation penetrates the canopy and warms the foliage which, in turn, warms the air in contact with it.
     861It is assumed that solar radiation penetrates the canopy and warms the foliage which, in turn, warms the air in contact with it.\\\\
    807862'''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)).
     863}}}
     864|----------------
     865{{{#!td style="vertical-align:top"
     866[=#<insert_parameter_name> '''<insert_parameter_name>''']
     867}}}
     868{{{#!td style="vertical-align:top"
     869<insert type>
     870}}}
     871{{{#!td style="vertical-align:top"
     872<insert value>
     873}}}
     874{{{#!td
     875<insert explanation>
     876}}}
     877|----------------
     878{{{#!td style="vertical-align:top"
     879[=#<insert_parameter_name> '''<insert_parameter_name>''']
     880}}}
     881{{{#!td style="vertical-align:top"
     882<insert type>
     883}}}
     884{{{#!td style="vertical-align:top"
     885<insert value>
     886}}}
     887{{{#!td
     888<insert explanation>
     889}}}
     890|----------------
     891{{{#!td style="vertical-align:top"
     892[=#<insert_parameter_name> '''<insert_parameter_name>''']
     893}}}
     894{{{#!td style="vertical-align:top"
     895<insert type>
     896}}}
     897{{{#!td style="vertical-align:top"
     898<insert value>
     899}}}
     900{{{#!td
     901<insert explanation>
     902}}}
     903|----------------
     904{{{#!td style="vertical-align:top"
     905[=#<insert_parameter_name> '''<insert_parameter_name>''']
     906}}}
     907{{{#!td style="vertical-align:top"
     908<insert type>
     909}}}
     910{{{#!td style="vertical-align:top"
     911<insert value>
     912}}}
     913{{{#!td
     914<insert explanation>
     915}}}
     916|----------------
     917{{{#!td style="vertical-align:top"
     918[=#<insert_parameter_name> '''<insert_parameter_name>''']
     919}}}
     920{{{#!td style="vertical-align:top"
     921<insert type>
     922}}}
     923{{{#!td style="vertical-align:top"
     924<insert value>
     925}}}
     926{{{#!td
     927<insert explanation>
    808928}}}
    809929[[BR]]