Changeset 531 for palm/trunk/DOC/app/chapter_4.1.html
- Timestamp:
- Apr 21, 2010 6:47:21 AM (15 years ago)
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palm/trunk/DOC/app/chapter_4.1.html (modified) (8 diffs)
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palm/trunk/DOC/app/chapter_4.1.html
r411 r531 1 1 <!DOCTYPE html PUBLIC "-//W3C//DTD HTML 4.01 Transitional//EN"> 2 2 <html><head> 3 4 3 5 4 6 … … 14 16 15 17 16 <meta http-equiv="content-type" content="text/html; charset=ISO-8859-1"> 17 18 19 20 21 22 23 24 25 26 27 28 29 <title>PALM chapter 4.1</title></head> 30 <body> 18 <meta http-equiv="content-type" content="text/html; charset=ISO-8859-1"><title>PALM chapter 4.1</title></head><body> 31 19 32 20 … … 3413 3401 <br> 3414 3402 <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> 3403 Sets the time period a precursor run shall run uncoupled. This 3404 parameter is used to set up the precursor run control for 3405 atmosphere-ocean-coupled runs. It has to be set individually to the 3406 atmospheric / oceanic precursor run. The time in the data output will 3407 show negative values during the precursor run. See documentation for 3408 further information. </td> 3418 3409 3419 3410 </tr> 3420 3411 3421 <t d 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> 3422 3413 3423 3414 <td style="vertical-align: top;">R</td> … … 15643 15634 15644 15635 A more effective control of 15645 the & ldquo;overshoots” can be achieved with parameter <a href="#cut_spline_overshoot">cut_spline_overshoot</a>.15636 the “overshoots” can be achieved with parameter <a href="#cut_spline_overshoot">cut_spline_overshoot</a>. 15646 15637 </td> 15647 15638 … … 17249 17240 17250 17241 17251 </tr>17242 17252 17243 17253 17244 <tr> … … 17303 17294 <p><span style="font-weight: bold;">Attention:</span><br> 17304 17295 17305 The large scale vertical motion is only applied to the prognostic equation for the potential17306 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. 17307 17298 Thus, the model is not mass consistent.</p> 17308 17299 … … 17313 17304 17314 17305 17315 </tr>17306 17316 17307 17317 17308 <tr> … … 17344 17335 default values result in a profile which is zero everywhere regardless of the 17345 17336 values of <a href="#ws_vertical_gradient">ws_vertical_gradient</a>. 17346 For the piecewise construction of t emperature profilessee <a href="#ws_vertical_gradient">ws_vertical_gradient</a>.</p>17337 For the piecewise construction of the subsidence/ascent velocity profile see <a href="#ws_vertical_gradient">ws_vertical_gradient</a>.</p> 17347 17338 </td> 17348 17339
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