Changeset 103 for palm/trunk/DOC/app/chapter_4.1.html
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- Jul 30, 2007 10:49:46 AM (17 years ago)
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palm/trunk/DOC/app/chapter_4.1.html
r97 r103 1880 1880 condition must be used for the potential temperature (see <a href="chapter_4.1.html#bc_pt_t">bc_pt_t</a>), 1881 1881 because otherwise the resolved scale may contribute to 1882 the top flux so that a constant value cannot be guaranteed.<span style="font-style: italic;"></span> </p>1882 the top flux so that a constant flux value cannot be guaranteed.<span style="font-style: italic;"></span> </p> 1883 1883 <p><span style="font-weight: bold;">Note:</span><br>The 1884 1884 application of a top heat flux additionally requires the setting of … … 1887 1887 Prandtl-layer is available at the top boundary so far.</p><p>See 1888 1888 also <a href="#surface_heatflux">surface_heatflux</a>.</p> 1889 </td></tr><tr><td style="vertical-align: top;"><a name="top_salinityflux"></a><span style="font-weight: bold;">top_salinityflux</span></td><td style="vertical-align: top;">R</td><td style="vertical-align: top;"><span style="font-style: italic;">no prescribed<br> 1889 </td></tr><tr><td style="vertical-align: top;"><a name="top_momentumflux_u"></a><span style="font-weight: bold;">top_momentumflux_u</span></td><td style="vertical-align: top;">R</td><td style="vertical-align: top;"><span style="font-style: italic;">no prescribed momentumflux</span></td><td style="vertical-align: top;">Momentum flux along x at the top boundary (in m2/s2).<br><p>If a value is assigned to this parameter, the internal 1890 two-dimensional u-momentum flux field <span style="font-family: monospace;">uswst</span> is 1891 initialized with the value of <span style="font-weight: bold;">top_momentumflux_u</span> as 1892 top (horizontally homogeneous) boundary condition for the u-momentum equation.</p><p><span style="font-weight: bold;">Notes:</span><br>The 1893 application of a top momentum flux additionally requires the setting of 1894 initial parameter <a href="chapter_4.1.html#use_top_fluxes">use_top_fluxes</a> 1895 = .T.. Setting of <span style="font-weight: bold;">top_momentumflux_u</span> requires setting of <a href="#top_momentumflux_v">top_momentumflux_v</a> also.</p><p>A Neumann 1896 condition should be used for the u velocity component (see <a href="chapter_4.1.html#bc_uv_t">bc_uv_t</a>), 1897 because otherwise the resolved scale may contribute to 1898 the top flux so that a constant flux value cannot be guaranteed.<span style="font-style: italic;"></span> </p> 1899 <span style="font-weight: bold;"></span><p>No 1900 Prandtl-layer is available at the top boundary so far.</p></td></tr><tr><td style="vertical-align: top;"><a name="top_momentumflux_v"></a><span style="font-weight: bold;">top_momentumflux_v</span></td><td style="vertical-align: top;">R</td><td style="vertical-align: top;"><span style="font-style: italic;">no prescribed momentumflux</span></td><td style="vertical-align: top;">Momentum flux along y at the top boundary (in m2/s2).<br><p>If a value is assigned to this parameter, the internal 1901 two-dimensional v-momentum flux field <span style="font-family: monospace;">vswst</span> is 1902 initialized with the value of <span style="font-weight: bold;">top_momentumflux_v</span> as 1903 top (horizontally homogeneous) boundary condition for the v-momentum equation.</p><p><span style="font-weight: bold;">Notes:</span><br>The 1904 application of a top momentum flux additionally requires the setting of 1905 initial parameter <a href="chapter_4.1.html#use_top_fluxes">use_top_fluxes</a> 1906 = .T.. Setting of <span style="font-weight: bold;">top_momentumflux_v</span> requires setting of <a href="chapter_4.1.html#top_momentumflux_u">top_momentumflux_u</a> also.</p><p>A Neumann 1907 condition should be used for the v velocity component (see <a href="chapter_4.1.html#bc_uv_t">bc_uv_t</a>), 1908 because otherwise the resolved scale may contribute to 1909 the top flux so that a constant flux value cannot be guaranteed.<span style="font-style: italic;"></span> </p> 1910 <span style="font-weight: bold;"></span><p>No 1911 Prandtl-layer is available at the top boundary so far.</p></td></tr><tr><td style="vertical-align: top;"><a name="top_salinityflux"></a><span style="font-weight: bold;">top_salinityflux</span></td><td style="vertical-align: top;">R</td><td style="vertical-align: top;"><span style="font-style: italic;">no prescribed<br> 1890 1912 salinityflux</span></td><td style="vertical-align: top;"><p>Kinematic 1891 1913 salinity flux at the top boundary, i.e. the sea surface (in psu m/s). </p> … … 1896 1918 condition must be used for the salinity (see <a href="chapter_4.1.html#bc_sa_t">bc_sa_t</a>), 1897 1919 because otherwise the resolved scale may contribute to 1898 the top flux so that a constant value cannot be guaranteed.<span style="font-style: italic;"></span> </p>1920 the top flux so that a constant flux value cannot be guaranteed.<span style="font-style: italic;"></span> </p> 1899 1921 <p><span style="font-weight: bold;">Note:</span><br>The 1900 1922 application of a salinity flux at the model top additionally requires the setting of … … 2077 2099 = <i>.TRUE.</i>, the user-assigned top fluxes are used 2078 2100 instead 2079 (see <a href="chapter_4.1.html#top_heatflux">top_heatflux</a>).</p><p>Currently, 2080 only a value for the sensible heatflux can be assigned. In case of <span style="font-weight: bold;">use_top_fluxes</span> = <span style="font-style: italic;">.TRUE.</span>, the latent 2101 (see <a href="chapter_4.1.html#top_heatflux">top_heatflux</a>, <a href="#top_momentumflux_u">top_momentumflux_u</a>, <a href="#top_momentumflux_v">top_momentumflux_v</a>, <a href="#top_salinityflux">top_salinityflux</a>).</p><p>Currently, no value for the latent heatflux can be assigned. In case of <span style="font-weight: bold;">use_top_fluxes</span> = <span style="font-style: italic;">.TRUE.</span>, the latent 2081 2102 heat flux at the top will be automatically set to zero.</p></td></tr><tr> 2082 2103 <td style="vertical-align: top;"> <p><a name="use_ug_for_galilei_tr"></a><b>use_ug_for_galilei_tr</b></p>
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