Ignore:
Timestamp:
Dec 11, 2009 2:15:58 PM (13 years ago)
Author:
heinze
Message:

Large scale vertical motion (subsidence/ascent) can be applied to the prognostic equation for the potential temperature

File:
1 edited

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  • palm/trunk/DOC/app/chapter_4.6.html

    r407 r411  
    1514915149
    1515015150 </tr>
     15151
     15152  <tr>
     15153
     15154 <td><a href="chapter_4.1.html#ws_vertical_gradient"><span style="font-weight: bold;">ws_vertical_gradient</span></a></td>
     15155
     15156 <td>I</td>
     15157
     15158 <td>R(10)</td>
     15159
     15160 <td><span style="font-style: italic;">10 * 0.0</span></td>
     15161
     15162 <td>Gradient(s) of the profile for the large scale subsidence/ascent velocity in ((m/s) / 100 m)</td>
     15163
     15164 </tr>
     15165
     15166  <tr>
     15167
     15168 <td><a href="chapter_4.1.html#ws_vertical_gradient_level"><span style="font-weight: bold;">ws_vertical_gradient_level</span></a></td>
     15169
     15170 <td>I</td>
     15171
     15172 <td>R(10)</td>
     15173
     15174 <td><span style="font-style: italic;">10 * 0.0</span></td>
     15175
     15176 <td>Height level from which on the gradient for the subsidence/ascent velocity defined by
     15177     ws_vertical_gradient is effective (in m).</td>
     15178
     15179 </tr>
    1515115180 
    1515215181 <tr>
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