Changeset 531 for palm/trunk/DOC


Ignore:
Timestamp:
Apr 21, 2010 6:47:21 AM (12 years ago)
Author:
heinze
Message:

call of subsidence added in prognostic equations for humidity/passive scalar, some bugfixes

Location:
palm/trunk/DOC/app
Files:
2 edited

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  • palm/trunk/DOC/app/chapter_4.1.html

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    29   <title>PALM chapter 4.1</title></head>
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     18  <meta http-equiv="content-type" content="text/html; charset=ISO-8859-1"><title>PALM chapter 4.1</title></head><body>
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    34133401      <br>
    34143402      <br>
    3415          Sets 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.
    3416      
    3417       </td>
     3403Sets the time period a precursor run shall run uncoupled. This
     3404parameter is used to set up the precursor run control for
     3405atmosphere-ocean-coupled runs. It has to be set individually to the
     3406atmospheric / oceanic precursor run. The time in the data output will
     3407show negative values during the precursor run. See documentation for
     3408further information. </td>
    34183409
    34193410    </tr>
    34203411
    3421       <td style="vertical-align: top;"><a name="cthf"></a><span style="font-weight: bold;">cthf</span></td>
     3412      <tr><td style="vertical-align: top;"><a name="cthf"></a><span style="font-weight: bold;">cthf</span></td>
    34223413
    34233414      <td style="vertical-align: top;">R</td>
     
    1564315634
    1564415635A more effective control of
    15645 the &ldquo;overshoots&rdquo; can be achieved with parameter <a href="#cut_spline_overshoot">cut_spline_overshoot</a>.
     15636the &#8220;overshoots&#8221; can be achieved with parameter <a href="#cut_spline_overshoot">cut_spline_overshoot</a>.
    1564615637      </td>
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    17251  </tr>
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    1725317244 <tr>
     
    1730317294   <p><span style="font-weight: bold;">Attention:</span><br>
    1730417295
    17305       The large scale vertical motion is only applied to the prognostic equation for the potential
    17306       temperature because it cannot be applied to the momentum equations due to incompressibility.
     17296      The large scale vertical motion is only applied to the prognostic equation for the scalar quantities (potential
     17297      temperature, humidity if  <a href="chapter_4.1.html#humidity">humidity</a> = .T. or passive scalar if <a href="chapter_4.1.html#passive_scalar">passive_scalar</a> = .T.) because it cannot be applied to the momentum equations due to incompressibility.
    1730717298      Thus, the model is not mass consistent.</p>
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    17315  </tr>
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    1734417335default values result in a profile which is zero everywhere regardless of the
    1734517336values of <a href="#ws_vertical_gradient">ws_vertical_gradient</a>.
    17346 For the piecewise construction of temperature profiles see <a href="#ws_vertical_gradient">ws_vertical_gradient</a>.</p>
     17337For the piecewise construction of the subsidence/ascent velocity profile see <a href="#ws_vertical_gradient">ws_vertical_gradient</a>.</p>
    1734717338      </td>
    1734817339
  • palm/trunk/DOC/app/chapter_4.2.html

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    4809  </tr>
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     4812            <td style="vertical-align: top;"><font color="#ff6666"><i>hyp</i></font></td>
     4813            <td style="vertical-align: top;">Hydrostatic pressure (in dbar)<br>
     4814            </td>
     4815          </tr>
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