Changeset 97
- Timestamp:
- Jun 21, 2007 8:23:15 AM (17 years ago)
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- palm/trunk
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palm/trunk/DOC/app/chapter_3.0.html
r62 r97 1 1 <!DOCTYPE HTML PUBLIC "-//W3C//DTD HTML 4.0 Transitional//EN"> 2 2 <html><head> 3 <meta http-equiv="CONTENT-TYPE" content="text/html; charset=windows-1252"><title>PALM 4 chapter 3.0</title> <meta name="GENERATOR" content="StarOffice 7 (Win32)"> <meta name="AUTHOR" content="Marcus Oliver Letzel"> <meta name="CREATED" content="20040723;15213734"> <meta name="CHANGED" content="20041112;13170538"> <meta name="KEYWORDS" content="parallel LES model"> <style> 3 <meta http-equiv="CONTENT-TYPE" content="text/html; charset=windows-1252"><title>PALM chapter 3.0</title> <meta name="GENERATOR" content="StarOffice 7 (Win32)"> <meta name="AUTHOR" content="Marcus Oliver Letzel"> <meta name="CREATED" content="20040723;15213734"> <meta name="CHANGED" content="20041112;13170538"> <meta name="KEYWORDS" content="parallel LES model"> <style> 5 4 <!-- 6 5 @page { size: 21cm 29.7cm } 7 6 --> 8 7 </style></head> 9 10 8 <body style="direction: ltr;" lang="en-US"><h2 style="font-style: normal; line-height: 100%;"><font size="4">3.0 11 9 Execution of model runs</font></h2> … … 41 39 changed by the user. Some of the most important parameters are not 42 40 preset with default values and must be adjusted by the user in each 43 case. Such a typical, minimum parameter set is described in <a href="chapter_4.4. html">chapter44 4.4 </a>. For the subsequent analysis of model runs, graphical41 case. Such a typical, minimum parameter set is described in <a href="chapter_4.4.1.html">chapter 42 4.4.1</a>. For the subsequent analysis of model runs, graphical 45 43 visualization of model data is particularly important. <a href="chapter_4.5.html">Chapter 46 44 4.5</a> describes, how such outputs are produced with the model. </p> -
palm/trunk/DOC/app/chapter_3.2.html
r62 r97 1 1 <!DOCTYPE HTML PUBLIC "-//W3C//DTD HTML 4.0 Transitional//EN"> 2 2 <html><head> 3 <meta http-equiv="CONTENT-TYPE" content="text/html; charset=windows-1252"><title>PALM 4 chapter 3.2</title> <meta name="GENERATOR" content="StarOffice 7 (Win32)"> <meta name="AUTHOR" content="Marcus Oliver Letzel"> <meta name="CREATED" content="20040726;13164873"> <meta name="CHANGED" content="20050119;9245042"> <meta name="KEYWORDS" content="parallel LES model"> <style> 3 <meta http-equiv="CONTENT-TYPE" content="text/html; charset=windows-1252"><title>PALM chapter 3.2</title> <meta name="GENERATOR" content="StarOffice 7 (Win32)"> <meta name="AUTHOR" content="Marcus Oliver Letzel"> <meta name="CREATED" content="20040726;13164873"> <meta name="CHANGED" content="20050119;9245042"> <meta name="KEYWORDS" content="parallel LES model"> <style> 5 4 <!-- 6 5 @page { size: 21cm 29.7cm } 7 6 --> 8 7 </style></head> 9 10 8 <body style="direction: ltr;" lang="en-US"><h3 style="line-height: 100%;">3.2 Example of a minimum 11 9 configuration … … 20 18 here) 21 19 and can be used, together with the <a href="http://www.muk.uni-hannover.de/%7Eraasch/PALM_group/INSTALL/example_p3d">parameter 22 file</a> presented in <a href="chapter_4.4. html">chapter23 4.4 </a>, for the execution of a simple model run. In chapter 4.420 file</a> presented in <a href="chapter_4.4.1.html">chapter 21 4.4.1</a>, for the execution of a simple model run. In chapter 4.4.1 24 22 the 25 23 complete <b>mrun</b> options which are necessary for the … … 85 83 will 86 84 interpret these colons as blanks (2 colons written one behind the 87 other will be interpreted as a colon). Thus in the example above </font><tt><font face="Thorndale, serif">fopts88 has the value </font></tt>“<font style="font-size: 10pt; font-family: monospace;" size="2"><i>-O385 other will be interpreted as a colon). Thus in the example above</font> fopts 86 has the value<tt><font face="Thorndale, serif"> </font></tt>“<font style="font-size: 10pt; font-family: monospace;" size="2"><i>-O3 89 87 -g 90 88 -qrealsize=8 -Q -q64 -qmaxmem=-1 -qtune=pwr4 -qarch=pwr4 -qnosave … … 184 182 explained in detail in the <b>mrun</b> 185 183 description (<a href="http://www.muk.uni-hannover.de/institut/software/mrun_beschreibung.html#chapter6.3">chapter 186 6.3</a>, in German) and are described here only as far as being184 6.3</a>, in German) and are described here only as far as 187 185 necessary. A 188 186 file connection statement usually consists of entries in 5 columns -
palm/trunk/DOC/app/chapter_3.4.html
r62 r97 1 1 <!DOCTYPE html PUBLIC "-//W3C//DTD HTML 4.01 Transitional//EN"> 2 2 <html><head> 3 <meta content="text/html; charset=ISO-8859-1" http-equiv="content-type"><title>chapter_3.4</title> 3 <meta content="text/html; charset=ISO-8859-1" http-equiv="content-type"><title>chapter_3.4</title></head> 4 4 <body><h3 style="line-height: 100%;"><font color="#000000">3.4 Input and 5 5 output files</font></h3> … … 85 85 is needed by the model in each case. Its content and structure is 86 86 described in detail in</font> <a href="chapter_4.0.html">chapter 87 4.0</a>. <a href="chapter_4.4. html">Chapter88 4.4 </a> <font color="#000000">shows a simple87 4.0</a>. <a href="chapter_4.4.1.html">Chapter 88 4.4.1</a> <font color="#000000">shows a simple 89 89 example. </font> </p> </td> </tr> <tr valign="top"> <td style="text-align: center;" width="8%"> <p align="center">13</p> </td> 90 90 <td width="12%"> <p><a name="BININ"></a>BININ/</p> -
palm/trunk/DOC/app/chapter_4.0.html
r83 r97 131 131 within routine <span style="font-family: monospace;">user_parin</span> 132 132 in file <span style="font-family: monospace;">user_interface.f90</span>). 133 <a href="chapter_4.4. html">Chapter134 4.4 </a> shows a simple but complete example of the input file133 <a href="chapter_4.4.1.html">Chapter 134 4.4.1</a> shows a simple but complete example of the input file 135 135 PARIN. 136 136 This example file can be used together with the configuration file -
palm/trunk/DOC/app/chapter_4.1.html
r83 r97 208 208 </td> </tr> <tr> <td style="vertical-align: top;"> <p><a name="pc_pt_t"></a><b>bc_pt_t</b></p> 209 209 </td> <td style="vertical-align: top;">C * 20</td> 210 <td style="vertical-align: top;"><span style="font-style: italic;">'initial gradient'</span></td>210 <td style="vertical-align: top;"><span style="font-style: italic;">'initial_ gradient'</span></td> 211 211 <td style="vertical-align: top;"> <p style="font-style: normal;">Top boundary condition of the 212 212 potential temperature. </p> <p>Allowed are the … … 299 299 bc_s_t_val * dzu(nz+1)</p> </ul> <p style="font-style: normal;">(up to k=nz the prognostic 300 300 equation for the scalar concentration is 301 solved).</p> </td> </tr> <tr> <td style="vertical-align: top;"> <p><a name="bc_uv_b"></a><b>bc_uv_b</b></p> 301 solved).</p> </td> </tr> <tr><td style="vertical-align: top;"><a name="bc_sa_t"></a><span style="font-weight: bold;">bc_sa_t</span></td><td style="vertical-align: top;">C * 20</td><td style="vertical-align: top;"><span style="font-style: italic;">'neumann'</span></td><td style="vertical-align: top;"><p style="font-style: normal;">Top boundary condition of the salinity. </p> <p>This parameter only comes into effect for ocean runs (see parameter <a href="#ocean">ocean</a>).</p><p style="font-style: normal;">Allowed are the 302 values <span style="font-style: italic;">'dirichlet' </span>(sa(k=nz+1) 303 does not change during the run) and <span style="font-style: italic;">'neumann'</span> 304 (sa(k=nz+1)=sa(k=nz))<span style="font-style: italic;"></span>. <br><br> 305 When a constant salinity flux is used at the top boundary (<a href="chapter_4.1.html#top_salinityflux">top_salinityflux</a>), 306 <b>bc_sa_t</b> = <span style="font-style: italic;">'neumann'</span> 307 must be used, because otherwise the resolved scale may contribute to 308 the top flux so that a constant value cannot be guaranteed.</p></td></tr><tr> <td style="vertical-align: top;"> <p><a name="bc_uv_b"></a><b>bc_uv_b</b></p> 302 309 </td> <td style="vertical-align: top;">C * 20</td> 303 310 <td style="vertical-align: top;"><span style="font-style: italic;">'dirichlet'</span></td> … … 331 338 Neumann condition yields the free-slip condition with u(k=nz+1) = 332 339 u(k=nz) and v(k=nz+1) = v(k=nz) (up to k=nz the prognostic equations 333 for the velocities are solved).</p> </td> </tr> <tr> 340 for the velocities are solved).</p> </td> </tr> <tr><td style="vertical-align: top;"><a name="bottom_salinityflux"></a><span style="font-weight: bold;">bottom_salinityflux</span></td><td style="vertical-align: top;">R</td><td style="vertical-align: top;"><span style="font-style: italic;">0.0</span></td><td style="vertical-align: top;"><p>Kinematic salinity flux near the surface (in psu m/s). </p>This parameter only comes into effect for ocean runs (see parameter <a href="chapter_4.1.html#ocean">ocean</a>).<p>The 341 respective salinity flux value is used 342 as bottom (horizontally homogeneous) boundary condition for the salinity equation. This additionally requires that a Neumann 343 condition must be used for the salinity, which is currently the only available condition.<br> </p> </td></tr><tr> 334 344 <td style="vertical-align: top;"><span style="font-weight: bold;"><a name="building_height"></a>building_height</span></td> 335 345 <td style="vertical-align: top;">R</td> <td style="vertical-align: top;"><span style="font-style: italic;">50.0</span></td> <td>Height … … 1111 1121 be an integral multiple of 1112 1122 the number of processors in x-direction (due to data transposition 1113 restrictions).</p> </td> </tr> <tr> <td style="vertical-align: top;"> <p><a name="omega"></a><b>omega</b></p> 1123 restrictions).</p> </td> </tr> <tr><td style="vertical-align: top;"><a name="ocean"></a><span style="font-weight: bold;">ocean</span></td><td style="vertical-align: top;">L</td><td style="vertical-align: top;"><span style="font-style: italic;">.F.</span></td><td style="vertical-align: top;">Parameter to switch on ocean runs.<br><br>By default PALM is configured to simulate atmospheric flows. However, starting from version 3.3, <span style="font-weight: bold;">ocean</span> = <span style="font-style: italic;">.T.</span> allows simulation of ocean turbulent flows. Setting this switch has several effects:<br><br><ul><li>An additional prognostic equation for salinity is solved.</li><li>Potential temperature in buoyancy and stability-related terms is replaced by potential density.</li><li>Potential 1124 density is calculated from the equation of state for seawater after 1125 each timestep, using the algorithm proposed by Jackett et al. (2006, J. 1126 Atmos. Oceanic Technol., <span style="font-weight: bold;">23</span>, 1709-1728).<br>So far, only the initial hydrostatic pressure is entered into this equation.</li><li>z=0 (sea surface) is assumed at the model top (vertical grid index <span style="font-family: Courier New,Courier,monospace;">k=nzt</span> on the w-grid), with negative values of z indicating the depth.</li><li>Initial profiles are constructed (e.g. from <a href="#pt_vertical_gradient">pt_vertical_gradient</a> / <a href="#pt_vertical_gradient_level">pt_vertical_gradient_level</a>) starting from the sea surface, using surface values given by <a href="#pt_surface">pt_surface</a>, <a href="#sa_surface">sa_surface</a>, <a href="#ug_surface">ug_surface</a>, and <a href="#vg_surface">vg_surface</a>.</li><li>Zero salinity flux is used as default boundary condition at the bottom of the sea.</li><li>If switched on, random perturbations are by default imposed to the upper model domain from zu(nzt*2/3) to zu(nzt-3).</li></ul><br>Relevant parameters to be exclusively used for steering ocean runs are <a href="#bc_sa_t">bc_sa_t</a>, <a href="#bottom_salinityflux">bottom_salinityflux</a>, <a href="#sa_surface">sa_surface</a>, <a href="#sa_vertical_gradient">sa_vertical_gradient</a>, <a href="#sa_vertical_gradient_level">sa_vertical_gradient_level</a>, and <a href="#top_salinityflux">top_salinityflux</a>.<br><br>Section <a href="chapter_4.2.2.html">4.4.2</a> gives an example for appropriate settings of these and other parameters neccessary for ocean runs.<br><br><span style="font-weight: bold;">ocean</span> = <span style="font-style: italic;">.T.</span> does not allow settings of <a href="#timestep_scheme">timestep_scheme</a> = <span style="font-style: italic;">'leapfrog'</span> or <span style="font-style: italic;">'leapfrog+euler'</span> as well as <a href="#scalar_advec">scalar_advec</a> = <span style="font-style: italic;">'ups-scheme'</span>.<br><br><span style="font-weight: bold;">Current limitations:</span><br>Using 1127 a vertical grid stretching is not recommended since it would still 1128 stretch the grid towards the top boundary of the model (sea surface) 1129 instead of the bottom boundary.</td></tr><tr> <td style="vertical-align: top;"> <p><a name="omega"></a><b>omega</b></p> 1114 1130 </td> <td style="vertical-align: top;">R</td> 1115 1131 <td style="vertical-align: top;"><i>7.29212E-5</i></td> … … 1241 1257 temperature to be used in all buoyancy terms (in K).<br><br>By 1242 1258 default, the instantaneous horizontal average over the total model 1243 domain is used.< /td></tr><tr> <td style="vertical-align: top;"> <p><a name="pt_surface"></a><b>pt_surface</b></p>1259 domain is used.<br><br><span style="font-weight: bold;">Attention:</span><br>In case of ocean runs (see <a href="chapter_4.1.html#ocean">ocean</a>), always a reference temperature is used in the buoyancy terms with a default value of <span style="font-weight: bold;">pt_reference</span> = <a href="#pt_surface">pt_surface</a>.</td></tr><tr> <td style="vertical-align: top;"> <p><a name="pt_surface"></a><b>pt_surface</b></p> 1244 1260 </td> <td style="vertical-align: top;">R</td> 1245 1261 <td style="vertical-align: top;"><i>300.0</i></td> … … 1247 1263 potential temperature (in K). </p> <p>This 1248 1264 parameter assigns the value of the potential temperature 1249 ptat the surface (k=0)<b>.</b> Starting from this value,1265 <span style="font-weight: bold;">pt</span> at the surface (k=0)<b>.</b> Starting from this value, 1250 1266 the 1251 1267 initial vertical temperature profile is constructed with <a href="#pt_vertical_gradient">pt_vertical_gradient</a> 1252 1268 and <a href="#pt_vertical_gradient_level">pt_vertical_gradient_level 1253 1269 </a>. 1254 This profile is also used for the 1d-model as a stationary profile.</p> 1270 This profile is also used for the 1d-model as a stationary profile.</p><p><span style="font-weight: bold;">Attention:</span><br>In case of ocean runs (see <a href="#ocean">ocean</a>), 1271 this parameter gives the temperature value at the sea surface, which is 1272 at k=nzt. The profile is then constructed from the surface down to the 1273 bottom of the model.</p> 1255 1274 </td> </tr> <tr> <td style="vertical-align: top;"> <p><a name="pt_surface_initial_change"></a><b>pt_surface_initial</b> 1256 1275 <br> <b>_change</b></p> </td> <td style="vertical-align: top;">R</td> <td style="vertical-align: top;"><span style="font-style: italic;">0.0</span><br> </td> … … 1291 1310 100 m and for z > 1000.0 m up to the top boundary it is 1292 1311 0.5 K / 100 m (it is assumed that the assigned height levels correspond 1293 with uv levels). </p> </td> </tr> <tr> <td style="vertical-align: top;"> <p><a name="pt_vertical_gradient_level"></a><b>pt_vertical_gradient</b> 1312 with uv levels).</p><p><span style="font-weight: bold;">Attention:</span><br>In case of ocean runs (see <a href="chapter_4.1.html#ocean">ocean</a>), 1313 the profile is constructed like described above, but starting from the 1314 sea surface (k=nzt) down to the bottom boundary of the model. Height 1315 levels have then to be given as negative values, e.g. <span style="font-weight: bold;">pt_vertical_gradient_level</span> = <span style="font-style: italic;">-500.0</span>, <span style="font-style: italic;">-1000.0</span>.</p> </td> </tr> <tr> <td style="vertical-align: top;"> <p><a name="pt_vertical_gradient_level"></a><b>pt_vertical_gradient</b> 1294 1316 <br> <b>_level</b></p> </td> <td style="vertical-align: top;">R (10)</td> <td style="vertical-align: top;"> <p><i>10 *</i> 1295 1317 <span style="font-style: italic;">0.0</span><br> … … 1297 1319 <p>Height level from which on the temperature gradient defined by 1298 1320 <a href="#pt_vertical_gradient">pt_vertical_gradient</a> 1299 is effective (in m). </p> <p>The height levels 1300 are to be assigned in ascending order. The 1321 is effective (in m). </p> <p>The height levels have to be assigned in ascending order. The 1301 1322 default values result in a neutral stratification regardless of the 1302 1323 values of <a href="#pt_vertical_gradient">pt_vertical_gradient</a> 1303 1324 (unless the top boundary of the model is higher than 100000.0 m). 1304 For the piecewise construction of temperature profiles see <a href="#pt_vertical_gradient">pt_vertical_gradient</a>.</p> 1325 For the piecewise construction of temperature profiles see <a href="#pt_vertical_gradient">pt_vertical_gradient</a>.</p><span style="font-weight: bold;">Attention:</span><br>In case of ocean runs (see <a href="chapter_4.1.html#ocean">ocean</a>), the (negative) height levels have to be assigned in descending order. 1305 1326 </td> </tr> <tr> <td style="vertical-align: top;"> <p><a name="q_surface"></a><b>q_surface</b></p> 1306 1327 </td> <td style="vertical-align: top;">R</td> … … 1453 1474 is switched 1454 1475 on (see <a href="#prandtl_layer">prandtl_layer</a>).</p> 1455 </td> </tr> <tr> <td style="vertical-align: top;"> <p><a name="scalar_advec"></a><b>scalar_advec</b></p> 1476 </td> </tr> <tr><td style="vertical-align: top;"><a name="sa_surface"></a><span style="font-weight: bold;">sa_surface</span></td><td style="vertical-align: top;">R</td><td style="vertical-align: top;"><span style="font-style: italic;">35.0</span></td><td style="vertical-align: top;"> <p>Surface salinity (in psu). </p>This parameter only comes into effect for ocean runs (see parameter <a href="chapter_4.1.html#ocean">ocean</a>).<p>This 1477 parameter assigns the value of the salinity <span style="font-weight: bold;">sa</span> at the sea surface (k=nzt)<b>.</b> Starting from this value, 1478 the 1479 initial vertical salinity profile is constructed from the surface down to the bottom of the model (k=0) by using <a href="chapter_4.1.html#sa_vertical_gradient">sa_vertical_gradient</a> 1480 and <a href="chapter_4.1.html#sa_vertical_gradient_level">sa_vertical_gradient_level 1481 </a>.</p></td></tr><tr><td style="vertical-align: top;"><a name="sa_vertical_gradient"></a><span style="font-weight: bold;">sa_vertical_gradient</span></td><td style="vertical-align: top;">R(10)</td><td style="vertical-align: top;"><span style="font-style: italic;">10 * 0.0</span></td><td style="vertical-align: top;"><p>Salinity gradient(s) of the initial salinity profile (in psu 1482 / 100 m). </p> <p>This parameter only comes into effect for ocean runs (see parameter <a href="chapter_4.1.html#ocean">ocean</a>).</p><p>This salinity gradient 1483 holds starting from the height 1484 level defined by <a href="chapter_4.1.html#sa_vertical_gradient_level">sa_vertical_gradient_level</a> 1485 (precisely: for all uv levels k where zu(k) < 1486 sa_vertical_gradient_level, sa_init(k) is set: sa_init(k) = 1487 sa_init(k+1) - dzu(k+1) * <b>sa_vertical_gradient</b>) down to the bottom boundary or down to the next height level defined 1488 by <a href="chapter_4.1.html#sa_vertical_gradient_level">sa_vertical_gradient_level</a>. 1489 A total of 10 different gradients for 11 height intervals (10 intervals 1490 if <a href="chapter_4.1.html#sa_vertical_gradient_level">sa_vertical_gradient_level</a>(1) 1491 = <i>0.0</i>) can be assigned. The surface salinity at k=nzt is 1492 assigned via <a href="chapter_4.1.html#sa_surface">sa_surface</a>. 1493 </p> <p>Example: </p> <ul><p><b>sa_vertical_gradient</b> 1494 = <i>1.0</i>, <i>0.5</i>, <br> 1495 <b>sa_vertical_gradient_level</b> = <i>-500.0</i>, 1496 -<i>1000.0</i>,</p></ul> <p>That 1497 defines the salinity to be constant down to z = -500.0 m with a salinity given by <a href="chapter_4.1.html#sa_surface">sa_surface</a>. 1498 For -500.0 m < z <= -1000.0 m the salinity gradient is 1499 1.0 psu / 1500 100 m and for z < -1000.0 m down to the bottom boundary it is 1501 0.5 psu / 100 m (it is assumed that the assigned height levels correspond 1502 with uv levels).</p></td></tr><tr><td style="vertical-align: top;"><a name="sa_vertical_gradient_level"></a><span style="font-weight: bold;">sa_vertical_gradient_level</span></td><td style="vertical-align: top;">R(10)</td><td style="vertical-align: top;"><span style="font-style: italic;">10 * 0.0</span></td><td style="vertical-align: top;"><p>Height level from which on the salinity gradient defined by <a href="chapter_4.1.html#sa_vertical_gradient">sa_vertical_gradient</a> 1503 is effective (in m). </p> <p>This parameter only comes into effect for ocean runs (see parameter <a href="chapter_4.1.html#ocean">ocean</a>).</p><p>The height levels have to be assigned in descending order. The 1504 default values result in a constant salinity profile regardless of the 1505 values of <a href="chapter_4.1.html#sa_vertical_gradient">sa_vertical_gradient</a> 1506 (unless the bottom boundary of the model is lower than -100000.0 m). 1507 For the piecewise construction of salinity profiles see <a href="chapter_4.1.html#sa_vertical_gradient">sa_vertical_gradient</a>.</p></td></tr><tr> <td style="vertical-align: top;"> <p><a name="scalar_advec"></a><b>scalar_advec</b></p> 1456 1508 </td> <td style="vertical-align: top;">C * 10</td> 1457 1509 <td style="vertical-align: top;"><i>'pw-scheme'</i></td> … … 1835 1887 Prandtl-layer is available at the top boundary so far.</p><p>See 1836 1888 also <a href="#surface_heatflux">surface_heatflux</a>.</p> 1837 </td></tr><tr> <td style="vertical-align: top;"> 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> 1890 salinityflux</span></td><td style="vertical-align: top;"><p>Kinematic 1891 salinity flux at the top boundary, i.e. the sea surface (in psu m/s). </p> 1892 <p>This parameter only comes into effect for ocean runs (see parameter <a href="chapter_4.1.html#ocean">ocean</a>).</p><p>If a value is assigned to this parameter, the internal 1893 two-dimensional surface heat flux field <span style="font-family: monospace;">saswst</span> is 1894 initialized with the value of <span style="font-weight: bold;">top_salinityflux</span> as 1895 top (horizontally homogeneous) boundary condition for the salinity equation. This additionally requires that a Neumann 1896 condition must be used for the salinity (see <a href="chapter_4.1.html#bc_sa_t">bc_sa_t</a>), 1897 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> 1899 <p><span style="font-weight: bold;">Note:</span><br>The 1900 application of a salinity flux at the model top additionally requires the setting of 1901 initial parameter <a href="chapter_4.1.html#use_top_fluxes">use_top_fluxes</a> 1902 = .T..<span style="font-style: italic;"></span><span style="font-weight: bold;"></span> </p><p>See 1903 also <a href="chapter_4.1.html#bottom_salinityflux">bottom_salinityflux</a>.</p></td></tr><tr> <td style="vertical-align: top;"> 1838 1904 <p><a name="ug_surface"></a><span style="font-weight: bold;">ug_surface</span></p> 1839 1905 </td> <td style="vertical-align: top;">R<br> </td> … … 1857 1923 value, it is recommended to use a Galilei-transformation of the 1858 1924 coordinate system, if possible (see <a href="#galilei_transformation">galilei_transformation</a>), 1859 in order to obtain larger time steps.<br> </td> </tr> 1925 in order to obtain larger time steps.<br><br><span style="font-weight: bold;">Attention:</span><br>In case of ocean runs (see <a href="chapter_4.1.html#ocean">ocean</a>), 1926 this parameter gives the velocity value at the sea surface, which is 1927 at k=nzt. The profile is then constructed from the surface down to the 1928 bottom of the model.<br> </td> </tr> 1860 1929 <tr> <td style="vertical-align: top;"> <p><a name="ug_vertical_gradient"></a><span style="font-weight: bold;">ug_vertical_gradient</span></p> 1861 1930 </td> <td style="vertical-align: top;">R(10)<br> … … 1872 1941 total of 10 different gradients for 11 height intervals (10 1873 1942 intervals if <a href="#ug_vertical_gradient_level">ug_vertical_gradient_level</a>(1) 1874 = 0.0) can be assigned. The surface geostrophic wind is assigned by <a href="#ug_surface">ug_surface</a>. <br> </td> 1943 = 0.0) can be assigned. The surface geostrophic wind is assigned by <a href="#ug_surface">ug_surface</a>.<br><br><span style="font-weight: bold;">Attention:</span><br>In case of ocean runs (see <a href="chapter_4.1.html#ocean">ocean</a>), 1944 the profile is constructed like described above, but starting from the 1945 sea surface (k=nzt) down to the bottom boundary of the model. Height 1946 levels have then to be given as negative values, e.g. <span style="font-weight: bold;">ug_vertical_gradient_level</span> = <span style="font-style: italic;">-500.0</span>, <span style="font-style: italic;">-1000.0</span>.<br> </td> 1875 1947 </tr> <tr> <td style="vertical-align: top;"> 1876 1948 <p><a name="ug_vertical_gradient_level"></a><span style="font-weight: bold;">ug_vertical_gradient_level</span></p> … … 1880 1952 gradient defined by <a href="#ug_vertical_gradient">ug_vertical_gradient</a> 1881 1953 is effective (in m).<br> <br> 1882 The height levels are to be assigned in ascending order. For the1954 The height levels have to be assigned in ascending order. For the 1883 1955 piecewise construction of a profile of the u-component of the 1884 geostrophic wind component (ug) see <a href="#ug_vertical_gradient">ug_vertical_gradient</a>.<br> 1885 </td> </tr> <tr> <td style="vertical-align: top;"> <p><a name="ups_limit_e"></a><b>ups_limit_e</b></p> 1956 geostrophic wind component (ug) see <a href="#ug_vertical_gradient">ug_vertical_gradient</a>.<br><br><span style="font-weight: bold;">Attention:</span><br>In case of ocean runs (see <a href="chapter_4.1.html#ocean">ocean</a>), the (negative) height levels have to be assigned in descending order.</td> </tr> <tr> <td style="vertical-align: top;"> <p><a name="ups_limit_e"></a><b>ups_limit_e</b></p> 1886 1957 </td> <td style="vertical-align: top;">R</td> 1887 1958 <td style="vertical-align: top;"><i>0.0</i></td> … … 2063 2134 if possible (see <a href="#galilei_transformation">galilei_transformation</a>), 2064 2135 in order to obtain larger 2065 time steps.</td> </tr> <tr> <td style="vertical-align: top;"> <p><a name="vg_vertical_gradient"></a><span style="font-weight: bold;">vg_vertical_gradient</span></p> 2136 time steps.<br><br><span style="font-weight: bold;">Attention:</span><br>In case of ocean runs (see <a href="chapter_4.1.html#ocean">ocean</a>), 2137 this parameter gives the velocity value at the sea surface, which is 2138 at k=nzt. The profile is then constructed from the surface down to the 2139 bottom of the model.</td> </tr> <tr> <td style="vertical-align: top;"> <p><a name="vg_vertical_gradient"></a><span style="font-weight: bold;">vg_vertical_gradient</span></p> 2066 2140 </td> <td style="vertical-align: top;">R(10)<br> 2067 2141 </td> <td style="vertical-align: top;"><span style="font-style: italic;">10 … … 2081 2155 = 2082 2156 0.0) can be assigned. The surface 2083 geostrophic wind is assigned by <a href="#vg_surface">vg_surface</a>.</td> 2157 geostrophic wind is assigned by <a href="#vg_surface">vg_surface</a>.<br><br><span style="font-weight: bold;">Attention:</span><br>In case of ocean runs (see <a href="chapter_4.1.html#ocean">ocean</a>), 2158 the profile is constructed like described above, but starting from the 2159 sea surface (k=nzt) down to the bottom boundary of the model. Height 2160 levels have then to be given as negative values, e.g. <span style="font-weight: bold;">vg_vertical_gradient_level</span> = <span style="font-style: italic;">-500.0</span>, <span style="font-style: italic;">-1000.0</span>.</td> 2084 2161 </tr> <tr> <td style="vertical-align: top;"> 2085 2162 <p><a name="vg_vertical_gradient_level"></a><span style="font-weight: bold;">vg_vertical_gradient_level</span></p> … … 2089 2166 gradient defined by <a href="#vg_vertical_gradient">vg_vertical_gradient</a> 2090 2167 is effective (in m).<br> <br> 2091 The height levels are to be assigned in ascending order. For the2168 The height levels have to be assigned in ascending order. For the 2092 2169 piecewise construction of a profile of the v-component of the 2093 geostrophic wind component (vg) see <a href="#vg_vertical_gradient">vg_vertical_gradient</a>.< /td>2170 geostrophic wind component (vg) see <a href="#vg_vertical_gradient">vg_vertical_gradient</a>.<br><br><span style="font-weight: bold;">Attention:</span><br>In case of ocean runs (see <a href="chapter_4.1.html#ocean">ocean</a>), the (negative) height levels have to be assigned in descending order.</td> 2094 2171 </tr> <tr> <td style="vertical-align: top;"> 2095 2172 <p><a name="wall_adjustment"></a><b>wall_adjustment</b></p> -
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r89 r97 405 405 = <span style="font-style: italic;">.TRUE.</span></td></tr><tr><td style="width: 106px; vertical-align: top;"><span style="font-style: italic;">qv</span></td><td style="width: 196px; vertical-align: top;">water vapor 406 406 content (specific humidity)</td><td style="vertical-align: top;">kg/kg</td><td style="vertical-align: top;">requires <a href="chapter_4.1.html#cloud_physics">cloud_physics</a> 407 = <span style="font-style: italic;">.TRUE.</span></td></tr><tr><td align="undefined" valign="undefined"><span style="font-style: italic;">rho</span></td><td align="undefined" valign="undefined">potential density</td><td align="undefined" valign="undefined">kg/m<sup>3</sup></td><td align="undefined" valign="undefined">requires <a href="chapter_4.1.html#ocean">ocean</a> 407 408 = <span style="font-style: italic;">.TRUE.</span></td></tr><tr><td style="width: 106px; vertical-align: top;"><span style="font-style: italic;">s</span></td><td style="width: 196px; vertical-align: top;">concentration of 408 409 the scalar</td><td style="vertical-align: top;">1/m<sup>3</sup></td><td style="vertical-align: top;">requires <a href="chapter_4.1.html#passive_scalar">passive_scalar</a> 410 = <span style="font-style: italic;">.TRUE.</span></td></tr><tr><td align="undefined" valign="undefined"><span style="font-style: italic;">sa</span></td><td align="undefined" valign="undefined">salinity</td><td align="undefined" valign="undefined">psu</td><td align="undefined" valign="undefined">requires <a href="chapter_4.1.html#ocean">ocean</a> 409 411 = <span style="font-style: italic;">.TRUE.</span></td></tr><tr><td style="width: 106px; vertical-align: top;"><span style="font-style: italic;">t*</span></td><td style="width: 196px; vertical-align: top;">(near surface) 410 412 characteristic temperature</td><td style="vertical-align: top;">K</td><td style="vertical-align: top;">only horizontal cross section … … 663 665 kg/kg).</td> </tr> <tr> <td style="vertical-align: top;"><font color="#ff6600"><i>ql</i></font></td> 664 666 <td style="vertical-align: top;">Liquid water content 665 (in kg/kg).</td> </tr> <tr> <td style="vertical-align: middle;"><font color="#ff6600">s</font></td>667 (in kg/kg).</td> </tr> <tr><td align="undefined" valign="undefined"><span style="font-style: italic; color: rgb(255, 102, 0);">rho</span></td><td align="undefined" valign="undefined">Potential density (in kg/m<sup>3</sup>).</td></tr><tr> <td style="vertical-align: middle; font-style: italic;"><font color="#ff6600">s</font></td> 666 668 <td style="vertical-align: top;">Scalar concentration (in 667 kg/m<sup>3</sup>).</td> </tr> <tr> <td style="vertical-align: middle;"><font color="#ff6600"><i>e</i></font></td>669 kg/m<sup>3</sup>).</td> </tr> <tr><td align="undefined" valign="undefined"><span style="font-style: italic; background-color: rgb(255, 255, 255); color: rgb(255, 102, 0);">sa</span></td><td align="undefined" valign="undefined">Salinity (in psu).</td></tr><tr> <td style="vertical-align: middle;"><font color="#ff6600"><i>e</i></font></td> 668 670 <td style="vertical-align: top;">Turbulent kinetic energy 669 671 (TKE, subgrid-scale) (in m<sup>2</sup>/s<sup>2</sup>).</td> … … 741 743 </tr> <tr> <td style="vertical-align: middle;"><font color="#33ff33"><i>w*s*</i></font></td> 742 744 <td style="vertical-align: top;">Resolved vertical scalar 743 concentration flux (in kg/m<sup>3</sup> )</td> </tr>745 concentration flux (in kg/m<sup>3</sup> m/s).</td> </tr> 744 746 <tr> <td style="vertical-align: middle;"><font color="#33ff33"><i>ws</i></font></td> 745 747 <td style="vertical-align: top;">Total vertical scalar 746 748 concentration flux (w"s" + w*s*) (in kg/m<sup>3 </sup>m/s).</td> 747 </tr> <tr> <td style="vertical-align: top;"><font color="#33ff33"><i>w*e*</i></font></td> 749 </tr> <tr><td align="undefined" valign="undefined"><span style="font-style: italic; color: rgb(51, 255, 51);">w"sa"</span></td><td align="undefined" valign="undefined">Subgrid-scale vertical 750 salinity flux (in psu<sup> </sup>m/s).</td></tr><tr><td align="undefined" valign="undefined"><span style="font-style: italic; color: rgb(51, 255, 51);">w*sa*</span></td><td align="undefined" valign="undefined">Resolved vertical salinity flux (in psu m/s).</td></tr><tr><td align="undefined" valign="undefined"><span style="font-style: italic; color: rgb(51, 255, 51);">wsa</span></td><td align="undefined" valign="undefined">Total vertical salinity flux (w"sa" + w*sa*) (in psu<sup> </sup>m/s).</td></tr><tr> <td style="vertical-align: top;"><font color="#33ff33"><i>w*e*</i></font></td> 748 751 <td style="vertical-align: top;">Vertical flux of 749 752 perturbation energy (resolved)</td> </tr> <tr> <td style="vertical-align: top;"><font color="#ff6600"><i>u*2</i></font></td> … … 856 859 </tr> <tr> <td style="vertical-align: top;"><p><a name="disturbance_level_b"></a><b>disturbance_level_b</b></p> 857 860 </td> <td style="vertical-align: top;">R</td> 858 <td style="vertical-align: top;"><i>zu(3) </i></td>861 <td style="vertical-align: top;"><i>zu(3) or<br>zu(nz*2/3)<br>see right</i></td> 859 862 <td style="vertical-align: top;"> <p lang="en-GB"><font face="Thorndale, serif"><font size="3">Lower 860 863 limit of the vertical range for which random perturbations are to be 861 864 imposed on the horizontal wind field (</font></font>in <font face="Thorndale, serif"><font size="3">m). 862 865 </font></font> </p> <p><span lang="en-GB"><font face="Thorndale, serif">This 863 parameter must hold the condition zu <i>(3)</i><= <b>disturbance_level_b</b>864 <= <i>zu(</i></font></span><i><a href="chapter_4.1.html#nz"><span lang="en-GB"><font face="Thorndale, serif">nz-1</font></span></a><span lang="en-GB"><font face="Thorndale, serif">)</font></span></i><span lang="en-GB"><font face="Thorndale, serif">.866 parameter must hold the condition zu(3) <= <b>disturbance_level_b</b> 867 <= zu(</font></span><a href="chapter_4.1.html#nz"><span lang="en-GB"><font face="Thorndale, serif">nz-1</font></span></a><span lang="en-GB"><font face="Thorndale, serif">)</font></span><span lang="en-GB"><font face="Thorndale, serif">. 865 868 Additionally, <b>disturbance_level_b</b> 866 869 <= </font></span><a href="#disturbance_level_t"><span lang="en-GB"><font face="Thorndale, serif">disturbance_level_t</font></span></a> 867 870 <span lang="en-GB"><font face="Thorndale, serif">must 868 also hold. <br> </font></span></p> <p><span lang="en-GB"><font face="Thorndale, serif">The871 also hold.</font></span></p><p><span lang="en-GB"><font face="Thorndale, serif">In case of ocean runs (see <a href="chapter_4.1.html#ocean">ocean</a>) </font></span><span lang="en-GB"><span style="font-family: Thorndale,serif;">the default value is <span style="font-weight: bold;">disturbance_level_b</span> = <span style="font-style: italic;">(nz * 2) / 3</span>.</span></span><a href="chapter_4.1.html#nz"><span lang="en-GB"></span></a><span lang="en-GB"></span><span lang="en-GB"></span></p> <p><span lang="en-GB"><font face="Thorndale, serif">The 869 872 parameter </font></span><a href="#create_disturbances"><span lang="en-GB"><font face="Thorndale, serif">create_disturbances</font></span></a><font face="Thorndale, serif"><span lang="en-GB"> 870 873 describes how to impose … … 872 875 </font> </p> </td> </tr> <tr> <td style="vertical-align: top;"> <p><a name="disturbance_level_t"></a><b>disturbance_level_t</b></p> 873 876 </td> <td style="vertical-align: top;">R</td> 874 <td style="vertical-align: top;"><i>zu(nz/3) </i></td>877 <td style="vertical-align: top;"><i>zu(nz/3) or<br>zu(nzt-3)<br>see right</i></td> 875 878 <td style="vertical-align: top;"> <p lang="en-GB"><font face="Thorndale, serif"><font size="3">Upper 876 879 limit of the vertical range for which random perturbations are to be … … 882 885 <span lang="en-GB"><font face="Thorndale, serif"><= 883 886 <b>disturbance_level_t</b> 884 must also hold.< br> </font></span></p><p><span lang="en-GB"><font face="Thorndale, serif">The887 must also hold.</font></span></p><span lang="en-GB"><font face="Thorndale, serif">In case of ocean runs (see <a href="chapter_4.1.html#ocean">ocean</a>) </font></span><span lang="en-GB"><span style="font-family: Thorndale,serif;">the default value is <span style="font-weight: bold;">disturbance_level_t</span> = <span style="font-style: italic;">nzt - 3</span>.</span></span><p><span lang="en-GB"><font face="Thorndale, serif">The 885 888 parameter </font></span><a href="#create_disturbances"><span lang="en-GB"><font face="Thorndale, serif">create_disturbances</font></span></a><font face="Thorndale, serif"><span lang="en-GB"> 886 889 describes how to impose -
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r62 r97 8 8 --> 9 9 </style></head> 10 <body style="direction: ltr;" lang="en-US"><h3 style="line-height: 100%;">4.4 Example of a minimum 11 parameter set</h3> 12 <p style="line-height: 100%;">In this chapter a brief, 13 simple and 14 complete parameter set is described, which can be used to carry out a 15 model run. The presented example is available via <a href="http://www.muk.uni-hannover.de/%7Eraasch/PALM_group/INSTALL/example_p3d">example 16 file</a> and can be used (together with the <a href="http://www.muk.uni-hannover.de/%7Eraasch/PALM_group/INSTALL/.mrun.config">configuration 17 file</a> described in <a href="chapter_3.2.html">chapter 18 3.2)</a> for the execution of a simple model run. </p> 19 <p style="line-height: 100%;">This run simulates a 20 quasi-stationary, 10 <body style="direction: ltr;" lang="en-US"><h3 style="line-height: 100%;">4.4 Examples of 11 parameter sets</h3> 12 <p style="line-height: 100%;">This chapter gives examples of complete 13 parameter sets for a variety of model runs. These parameter files can 14 be found in the directory <span style="font-family: Courier New,Courier,monospace;">trunk/INSTALL</span> and can be used together with the <span style="font-weight: bold;">mrun</span> configuration file (<span style="font-family: Courier New,Courier,monospace;">.mrun.config</span>) to carry out the respective model runs.</p><p style="line-height: 100%;">For 15 a description of the basic parameter settings which are generally 16 required, see chapter 4.4.1, which explains the settings for a simple 17 run of a quasi-stationary, 21 18 convective, atmospheric boundary layer with <font color="#000000">zero 22 19 mean horizontal 23 wind.</font> For evaluation purposes, cross sections and 24 horizontally averaged vertical 25 profiles of typical boundary layer variables 26 are output at the end of the run. The run shall be carried out in 27 batch mode on the IBM Regatta "hanni" of the HLRN.</p> 28 <p style="line-height: 100%;">The parameter file necessary 29 to carry 30 out a run must be provided to the model as an input file under the 31 local name <a href="chapter_3.4.html#PARIN">PARIN</a> 32 and has the following contents:</p> 33 <pre style="line-height: 100%;">&inipar <a href="chapter_4.1.html#nx">nx</a> = <span style="font-style: italic;">39</span>, <a href="chapter_4.1.html#ny">ny</a> = <span style="font-style: italic;">39</span>, <a href="chapter_4.1.html#nz">nz</a> = <span style="font-style: italic;">40</span>,<br> <a href="chapter_4.1.html#dx">dx</a> = <span style="font-style: italic;">50.0</span>, <a href="chapter_4.1.html#dy">dy</a> = <span style="font-style: italic;">50.0</span>, <a href="chapter_4.1.html#dz">dz</a> = <span style="font-style: italic;">50.0</span>,<br> <a href="chapter_4.1.html#dz_stretch_level">dz_stretch_level</a> = <span style="font-style: italic;">1200.0</span>,<br> <a href="chapter_4.1.html#fft_method">fft_method</a> = <span style="font-style: italic;">'temperton-algorithm'</span>,<br> <a href="chapter_4.1.html#initializing_actions">initializing_actions</a> = <span style="font-style: italic;">'set_constant_profiles'</span>,<br> <a href="chapter_4.1.html#ug_surface">ug_surface</a> = <span style="font-style: italic;">0.0</span>, <a href="chapter_4.1.html#vg_surface">vg_surface</a> = <span style="font-style: italic;">0.0</span>,<br> <a href="chapter_4.1.html#pt_vertical_gradient">pt_vertical_gradient</a> = <span style="font-style: italic;">0.0</span>, <span style="font-style: italic;">1.0</span>,<br> <a href="chapter_4.1.html#pt_vertical_gradient_level">pt_vertical_gradient_level</a> = <span style="font-style: italic;">0.0</span>, <span style="font-style: italic;">800.0</span>,<br> <a href="chapter_4.1.html#surface_heatflux">surface_heatflux</a> = <span style="font-style: italic;">0.1</span>, <a href="chapter_4.1.html#bc_pt_b">bc_pt_b</a> = <span style="font-style: italic;">'neumann'</span>,/<br><br>&d3par <a href="chapter_4.2.html#end_time">end_time</a> = <span style="font-style: italic;">3600.0</span>,<br> <a href="chapter_4.2.html#create_disturbances">create_disturbances</a> = <span style="font-style: italic;">.T.</span>,<br> <a href="chapter_4.2.html#dt_disturb">dt_disturb</a> = <span style="font-style: italic;">150.0</span>, <a href="chapter_4.2.html#disturbance_energy_limit">disturbance_energy_limit</a> = <span style="font-style: italic;">0.01</span>,<br> <a href="chapter_4.2.html#dt_run_control">dt_run_control</a> = <span style="font-style: italic;">0.0</span>,<br> <a href="chapter_4.2.html#data_output">data_output</a> = <span style="font-style: italic;">'w_xy'</span>, <span style="font-style: italic;">'w_xz'</span>, <span style="font-style: italic;">'w_xz_av'</span>, <span style="font-style: italic;">'pt_xy'</span>, <span style="font-style: italic;">'pt_xz'</span>,<br> <a href="chapter_4.2.html#dt_data_output">dt_data_output</a> = <span style="font-style: italic;">900.0</span>,<br> <a href="chapter_4.2.html#dt_data_output_av">dt_data_output_av</a> = <span style="font-style: italic;">1800.0</span>,<br> <a href="chapter_4.2.html#averaging_interval">averaging_interval</a> = <span style="font-style: italic;">900.0</span>,<br> <a href="chapter_4.2.html#dt_averaging_input">dt_averaging_input</a> = <span style="font-style: italic;">10.0</span>,<br> <a href="chapter_4.2.html#section_xy">section_xy</a> = <span style="font-style: italic;">2</span>, <span style="font-style: italic;">10</span>, <a href="chapter_4.2.html#section_xz">section_xz</a> = <span style="font-style: italic;">20</span>,<br> <a href="chapter_4.2.html#data_output_2d_on_each_pe">data_output_2d_on_each_pe</a> = <span style="font-style: italic;">.F.</span>,<br> <a href="chapter_4.2.html#dt_dopr">dt_dopr</a> = <span style="font-style: italic;">900.0</span>, <a href="chapter_4.2.html#averaging_interval_pr">averaging_interval_pr</a> = <span style="font-style: italic;">600.0</span>,<br> <a href="chapter_4.2.html#dt_averaging_input_pr">dt_averaging_input_pr</a> = <span style="font-style: italic;">10.0</span>,<br> <a href="chapter_4.2.html#data_output_pr">data_output_pr</a> = <span style="font-style: italic;">'#pt'</span>, <span style="font-style: italic;">'w”pt”'</span>, <span style="font-style: italic;">'w*pt*'</span>, <span style="font-style: italic;">'wpt'</span>, <span style="font-style: italic;">'w*2'</span>, <span style="font-style: italic;">'pt*2'</span>,<br> <a href="chapter_4.2.html#cross_profiles">cross_profiles</a> = <span style="font-style: italic;">' pt '</span>, <span style="font-style: italic;">' w"pt" w*pt* wpt '</span>, <span style="font-style: italic;">' w*2 '</span>, <span style="font-style: italic;">' pt*2 '</span>,<br> <a href="chapter_4.2.html#cross_xtext">cross_xtext</a> = <span style="font-style: italic;">'pot. temperature in K'</span>,<br> <span style="font-style: italic;">'heat flux in K ms>->1'</span>,<br> <span style="font-style: italic;">'velocity variance in m>2s>->2'</span>,<br> <span style="font-style: italic;">'temperature variance in K>2'</span>,<br> <a href="chapter_4.2.html#z_max_do1d">z_max_do1d</a> = <span style="font-style: italic;">1500.0</span>, /</pre><p style="line-height: 100%;"><br><br></p> 34 <p style="line-height: 100%;">The initialization 35 parameters (<tt><font style="font-size: 10pt;" size="2">&inipar</font></tt>) 36 are located at the beginning of the file. For analysis of a 37 convective boundary layer of approx. 1000 m thickness the horizontal 38 size of the model domain should amount to at least 2 km x 2 km. In 39 order to resolve the convective structures a grid spacing of <b>dx</b> 40 = 41 <b>dy</b> = <b>dz</b> = <i>50 m</i> 42 is enough, since the typical 43 diameter of convective plumes is more than 100 m. Thereby the 44 upper array index in the two horizontal directions needs to be <b>nx</b> 45 = <b>ny</b> = <i>39</i>. <font color="#000000">Since in 46 each case the lower array index has the value 0, 40 grid points are 47 used along both horizontal directions.</font> In the vertical 48 direction 49 the domain must be high enough to include the entrainment processes at 50 the top of the boundary layer as well as the propagation of gravity 51 waves, which were stimulated by 52 the convection. However, in the stably stratified region the grid 53 resolution has not necessarily to be as high as within the boundary 54 layer. This can be obtained by a vertical stretching of the grid 55 starting 56 from 1200 m via <b>dz_stretch_level</b> = <i>1200.0 57 m.</i> This saves 58 grid points and computing time. <font color="#800000">T</font><font color="#000000">he 59 upper boundary of the model is located at (see </font><a href="chapter_4.1.html#dz_stretch_factor"><font color="#000000">dz_stretch_factor</font></a><font color="#000000">) 60 … m (computed by the model)</font>.</p><p style="line-height: 100%;">Fast Fourier transformations are 61 calculated using the Temperton-algorithm, which -on the IBM Regatta- is 62 faster than the default system-specific algorithm (from IBM essl 63 library).</p><p style="line-height: 100%;">The 64 initial profiles for 65 wind and temperature can be assigned via <b>initializing_actions</b> 66 = <span style="font-style: italic;">'set_constant_profiles'</span>. 67 The wind speed, constant with 68 height, amounts to <b>ug_surface</b> = <b>vg_surface</b> 69 = <i>0.0 m/s</i>. In order 70 to allow for a fast onset of convection, a neutral stratified layer up 71 to z 72 = 800 m capped by an inversion with dtheta/dz = 1K/100 m is given: 73 <b>pt_vertical_gradient</b> = <i>0.0, 1.0</i>, 74 <b>pt_vertical_gradient_level</b> = <i>0.0, 800.0.</i> 75 The surface 76 temperature, which by default amounts to 300 K, provides the fixed 77 point for the temperature profile (see <a href="chapter_4.1.html#pt_surface">pt_surface</a>). 78 Convection is driven by a given, near-surface sensible heat flux via <b>surface_heatflux</b> 79 = <i>0.1 K m/s.</i> A given surface sensible heta flux 80 requires the 81 bottom boundary condition for potential temperature to be <b>bc_pt_b</b> 82 = 83 <span style="font-style: italic;">'neumann'</span> . 84 Thus 85 all initialization parameters are determined. These can not be 86 changed during the run (also not for restart runs). </p> 87 <p style="line-height: 100%;">Now the run parameters (<tt><font style="font-size: 10pt;" size="2">&d3par</font></tt>) 88 must be specified. To produce a quasi stationary boundary layer the 89 simulated time should be at least one hour, i.e. <b>end_time</b> 90 = <i>3600 91 s.</i> To stimulate convection, the initially homogeneous (zero) 92 wind 93 field must be disturbed (<b>create_disturbances</b> = <i>.T.</i>). 94 These perturbations should be repeated in a temporal interval of 95 <b>dt_disturb</b> = <i>150.0 s</i> until the 96 energy of the 97 perturbations exceeds the value <b>disturbance_energy_limit</b> 98 = 0.<i>01 99 m<sup>2</sup>/s<sup>2</sup></i>. After 100 each time step run time 101 informations (e.g. size of the timestep, maximum velocities, etc.) are 102 to be written to the local file <a href="chapter_3.4.html#RUN_CONTROL">RUN_CONTROL</a> 103 (<b>dt_run_control</b> = <i>0.0 s</i>).</p><p style="line-height: 100%;">Instantaneous cross section data 104 of vertical velocity (<span style="font-style: italic;">w</span>) 105 and potential temperature (<span style="font-style: italic;">pt</span>) 106 are to be output for horizontal (<span style="font-style: italic;">xy</span>) 107 and vertical (<span style="font-style: italic;">xz</span>) 108 cross sections, and additionally, time averaged (<span style="font-style: italic;">av</span>) vertical cross 109 section data are to be output for the vertical velocity: <span style="font-weight: bold;">data_output</span> = <span style="font-style: italic;">'w_xy'</span>, <span style="font-style: italic;">'w_xz'</span>, <span style="font-style: italic;">'w_xz_av'</span>, <span style="font-style: italic;">'pt_xy'</span>, <span style="font-style: italic;">'pt_xz'</span>. Output of 110 instantaneous (time averaged) data is done after each 900 (1800)s: <span style="font-weight: bold;">dt_data_output</span> = <span style="font-style: italic;">900.0</span>, <span style="font-weight: bold;">dt_data_output_av</span> = <span style="font-style: italic;">1800.0</span>. The 111 averaged data are time averaged over the last 900.0 s, where the 112 temporal interval of data entering the average is 10 s: <span style="font-weight: bold;">averaging_interval</span> = 113 <span style="font-style: italic;">900.0</span>, <span style="font-weight: bold;">dt_averaging_input</span> = 114 <span style="font-style: italic;">10.0</span>. 115 Horizontal cross sections are output for vertical levels with grid 116 index k=2 and k=10, vertical cross sections are output for index j=20: <span style="font-weight: bold;">section_xy</span> = <span style="font-style: italic;">2</span>, <span style="font-style: italic;">10</span>, <span style="font-weight: bold;">section_xz</span> = <span style="font-style: italic;">20</span>. For runs on 117 more than one processor, cross section data are collected and output on 118 PE0: <span style="font-weight: bold;">data_output_2d_on_each_pe</span> 119 = <span style="font-style: italic;">.F.</span>.</p><p style="line-height: 100%;">Output 120 of vertical profiles is to be done after each 900 s. The profiles shall 121 be temporally averaged<font color="#000000"> over the last 122 <font color="#000000">600 </font>seconds, </font>whereby 123 the temporal interval of the profiles entering the average has to be 124 10 s: <b>dt_dopr</b> = <i>900.0 s</i>, <b>averaging_interval_pr</b> 125 = 126 <i>600.0 s</i>, <b>dt_averaging_input_pr</b> = 127 <i>10.0 s.</i> The temperature 128 profile including the initial temperature profile (therefore <span style="font-style: italic;">'#pt'</span>), 129 the subgrid scale, resolved and total vertical sensible heat flux as 130 well as the variances of the vertical velocity and the potential 131 temperature are to be output: <b>data_output_pr</b> 132 = <span style="font-style: italic;">'#pt'</span><i>, 133 'w"pt”', 134 'w*pt*', 'wpt', 'w*2', 'pt*2'</i>.</p><p style="line-height: 100%;">If the data output format for 135 graphic software <span style="font-weight: bold;">profil</span> 136 is selected (see <a href="chapter_4.2.html#data_output_format">data_output_format</a>), 137 the temperature 138 profile and the individual variances are to be drawn into independent 139 coordinate systems, and in contrast to this all heat flux profiles are 140 to 141 be 142 drawn into the same system: <b>cross_profiles</b> = <span style="font-style: italic;">'pt'</span><i>, 143 'w"pt"w*pt*wpt', 'w*2', 'pt*2'</i>. The legend of the x 144 axes of these systems is set to <b>cross_xtext</b>= <i>'pot. 145 temperature in K', 'heat flux in K ms>->1', 'velocity 146 variance 147 in m>2s>->2', 'temperature variance in K>2'</i>. 148 The profiles are to be drawn up to a height level of <b>z_max_do1d</b> 149 = 150 <i>1500.0 m</i>. </p> 151 <p style="line-height: 100%;">Before starting the mo<font color="#000000">del 152 on the parallel computer, the number of processing elements must be 153 specified.</font> Since relatively few grid points are used for 154 this run, choosing of e.g. 8 PEs is sufficient. By default, a 1d domain 155 decomposition along x is used on the IBM-Regatta, which means that a 156 virtual processor topology (grid) of 8*1 (x*y) is used. (<span style="font-weight: bold;">Note:</span> the user may 157 adjust this 158 default domain decomposition with the help of the parameters <a href="chapter_4.1.html#npex">npex</a> 159 and <a href="chapter_4.1.html#npey">npey</a>). 160 </p><p style="line-height: 100%;">Provided that the 161 parameters 162 file described above are set within the file </p> 163 <ul> <pre style="margin-bottom: 0.5cm; line-height: 100%;"><font style="font-size: 10pt;" size="2">~/palm/current_version/JOBS/example/INPUT/example_p3d</font></pre></ul><p style="line-height: 100%;">and that the conditions 164 mentioned in the 165 first sections of <a href="chapter_3.2.html">chapter 166 3.2</a> are met, the model run can be started with the command </p> 167 <p style="line-height: 100%;"><font face="Cumberland, monospace"><font style="font-size: 10pt;" size="2">mrun 168 -d example -h ibmh -K parallel -X 8 -T 8 -t 1800 -q cdev -r 169 “d3# xy# xz# pr#”</font></font></p> 170 <p style="line-height: 100%;">The output files will appear 171 in the 172 directories </p> 173 <blockquote style="line-height: 100%;"><tt><font style="font-size: 10pt;" size="2">~/palm/current_version/JOBS/example/MONITORING</font></tt><font style="font-size: 10pt;" size="2"><br> </font><tt><font style="font-size: 10pt;" size="2">~/palm/current_version/JOBS/example/OUTPUT 174 ,</font></tt></blockquote> 175 <p style="line-height: 100%;">while the job protocol will 176 appear in 177 directory <font style="font-size: 10pt;" size="2"><font face="Cumberland, monospace">~/</font></font><tt><font style="font-size: 10pt;" size="2"><font face="Cumberland, monospace">job_queue</font></font></tt>. 178 <br> 20 wind.</font> 21 All other examples only explain those settings which are specific for 22 the respective runs (e.g. only the specific ocean parameters are 23 described in the parameter set for simulating ocean convection).<br> 179 24 </p> 180 <hr><p style="line-height: 100%;"><br><font color="#000080"><font color="#000080"><a href="chapter_4.3.html"><font color="#000080"><img name="Grafik1" src="left.gif" align="bottom" border="2" height="32" width="32"></font></a><a href="index.html"><font color="#000080"><img name="Grafik2" src="up.gif" align="bottom" border="2" height="32" width="32"></font></a><a href="chapter_4. 5.html"><font color="#000080"><img name="Grafik3" src="right.gif" align="bottom" border="2" height="32" width="32"></font></a></font></font></p><p style="line-height: 100%;"><i>Last change: 25 <hr><p style="line-height: 100%;"><br><font color="#000080"><font color="#000080"><a href="chapter_4.3.html"><font color="#000080"><img name="Grafik1" src="left.gif" align="bottom" border="2" height="32" width="32"></font></a><a href="index.html"><font color="#000080"><img name="Grafik2" src="up.gif" align="bottom" border="2" height="32" width="32"></font></a><a href="chapter_4.4.1.html"><font color="#000080"><img style="border: 2px solid ; width: 32px; height: 32px;" alt="" name="Grafik3" src="right.gif"></font></a></font></font></p><p style="line-height: 100%;"><i>Last change: 181 26 </i>$Id$ 182 27 <br> <br> -
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r62 r97 163 163 horizontal (xy) cross sections as example. The parameter settings 164 164 described below are those of the <a href="http://www.muk.uni-hannover.de/%7Eraasch/PALM_group/INSTALL/example_p3d">example 165 parameter file</a> (see <a href="chapter_4.4. html">chapter166 4.4 </a>) so this parameter file can be used to retrace the165 parameter file</a> (see <a href="chapter_4.4.1.html">chapter 166 4.4.1</a>) so this parameter file can be used to retrace the 167 167 following explanations.<br><br><ol><li>Output 168 168 of xy cross … … 348 348 NetCDF dataset described here contains data of instantaneous horizontal 349 349 cross sections and has been created using the settings of the <a href="http://www.muk.uni-hannover.de/%7Eraasch/PALM_group/INSTALL/example_p3d">example 350 parameter file</a> (see <a href="chapter_4.4. html">chapter351 4.4 </a>),350 parameter file</a> (see <a href="chapter_4.4.1.html">chapter 351 4.4.1</a>), 352 352 i.e. it contains section data of the w-velocity-component and of the 353 353 potential temperature for vertical grid levels with index <span style="font-family: monospace;">k = 2</span> and <span style="font-family: monospace;">k = 10</span>, -
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r62 r97 1 1 <!DOCTYPE HTML PUBLIC "-//W3C//DTD HTML 4.0 Transitional//EN"> 2 2 <html><head> 3 <meta http-equiv="CONTENT-TYPE" content="text/html; charset=windows-1252"><title>PALM 4 chapter 4.5</title> <meta name="GENERATOR" content="StarOffice 7 (Win32)"> <meta name="AUTHOR" content="Siegfried Raasch"> <meta name="CREATED" content="20041015;12234229"> <meta name="CHANGED" content="20041022;13412723"> <meta name="KEYWORDS" content="parallel LES model"> <style> 3 <meta http-equiv="CONTENT-TYPE" content="text/html; charset=windows-1252"><title>PALM chapter 4.5</title> <meta name="GENERATOR" content="StarOffice 7 (Win32)"> <meta name="AUTHOR" content="Siegfried Raasch"> <meta name="CREATED" content="20041015;12234229"> <meta name="CHANGED" content="20041022;13412723"> <meta name="KEYWORDS" content="parallel LES model"> <style> 5 4 <!-- 6 5 @page { size: 21cm 29.7cm } … … 63 62 </p> For most purposes it should be sufficient to read <a href="../app/chapter_4.5.1.html">chapter 4.5.1</a> 64 63 which explains the PALM-NetCDF-output.<hr> 65 <p style="line-height: 100%;"><br><font color="#000080"><font color="#000080"><a href="chapter_4.4. html"><font color="#000080"><img src="left.gif" name="Grafik1" align="bottom" border="2" height="32" width="32"></font></a><a href="index.html"><font color="#000080"><img src="up.gif" name="Grafik2" align="bottom" border="2" height="32" width="32"></font></a><a href="chapter_4.5.1.html"><font color="#000080"><img src="right.gif" name="Grafik3" align="bottom" border="2" height="32" width="32"></font></a></font></font></p>64 <p style="line-height: 100%;"><br><font color="#000080"><font color="#000080"><a href="chapter_4.4.2.html"><font color="#000080"><img style="border: 2px solid ; width: 32px; height: 32px;" alt="" src="left.gif" name="Grafik1"></font></a><a href="index.html"><font color="#000080"><img src="up.gif" name="Grafik2" align="bottom" border="2" height="32" width="32"></font></a><a href="chapter_4.5.1.html"><font color="#000080"><img src="right.gif" name="Grafik3" align="bottom" border="2" height="32" width="32"></font></a></font></font></p> 66 65 <p style="line-height: 100%;"> <span style="font-style: italic;">Last 67 66 change:</span> $Id$<br> -
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r89 r97 123 123 </td> <td style="vertical-align: middle;" width="5%"> 124 124 <p>I</p> </td> <td style="vertical-align: middle;" width="7%"> <p>C 125 * 20</p> </td> <td style="vertical-align: middle;" width="16%"> <p><i>' neumann'</i></p>125 * 20</p> </td> <td style="vertical-align: middle;" width="16%"> <p><i>'initial_gradient'</i></p> 126 126 </td> <td style="vertical-align: middle;" width="57%"> 127 127 <p>Top boundary condition of the … … 156 156 <p>Top boundary condition of the 157 157 scalar concentration. <br> </p> </td> </tr> 158 <tr> <td style="vertical-align: middle;" width="15%">158 <tr><td align="undefined" valign="undefined"><a href="chapter_4.1.html#bc_sa_t"><span style="font-weight: bold;">bc_sa_t</span></a></td><td align="undefined" valign="undefined">I</td><td align="undefined" valign="undefined">C * 20</td><td align="undefined" valign="undefined"><span style="font-style: italic;">'neumann'</span></td><td align="undefined" valign="undefined">Top boundary condition of the salinity. </td></tr><tr> <td style="vertical-align: middle;" width="15%"> 159 159 <p><a href="chapter_4.1.html#bc_uv_b"><b>bc_uv_b</b></a></p> 160 160 </td> <td style="vertical-align: middle;" width="5%"> … … 171 171 <p>Top boundary condition of the 172 172 horizontal velocity components u and v.</p> </td> </tr> 173 <tr> <td style="font-weight: bold;"><a href="chapter_4.1.html#building_height">building_height</a></td>173 <tr><td align="undefined" valign="undefined"><a href="chapter_4.1.html#bottom_salinityflux"><span style="font-weight: bold;">bottom_salinityflux</span></a></td><td align="undefined" valign="undefined">I</td><td align="undefined" valign="undefined">R</td><td align="undefined" valign="undefined"><span style="font-style: italic;">0.0</span></td><td align="undefined" valign="undefined">Kinematic salinity flux near the surface (in psu m/s).</td></tr><tr> <td style="font-weight: bold;"><a href="chapter_4.1.html#building_height">building_height</a></td> 174 174 <td>I</td> <td>R</td> <td style="font-style: italic;">50.0</td> <td>Height 175 175 of a single building in m.</td> </tr> <tr> <td style="font-weight: bold;"><a href="chapter_4.1.html#building_length_x">building_length_x</a></td> … … 324 324 <p>R</p> </td> <td style="vertical-align: middle;" width="7%"> <p>R</p> 325 325 </td> <td style="vertical-align: middle;" width="16%"> 326 <p><i>zu(3) </i></p> </td> <td style="vertical-align: middle;" width="57%"> <p lang="en-GB"><font face="Thorndale, serif"><font size="3">Lower326 <p><i>zu(3) or zu(nz*2/3)</i></p> </td> <td style="vertical-align: middle;" width="57%"> <p lang="en-GB"><font face="Thorndale, serif"><font size="3">Lower 327 327 limit of the vertical range for which random perturbations are to be 328 328 imposed on the horizontal wind field (</font></font>in <font face="Thorndale, serif"><font size="3">m). … … 332 332 <p>R</p> </td> <td style="vertical-align: middle;" width="7%"> <p>R</p> 333 333 </td> <td style="vertical-align: middle;" width="16%"> 334 <p><i>zu(nz/3) </i></p> </td> <td style="vertical-align: middle;" width="57%"> <p lang="en-GB"><font face="Thorndale, serif"><font size="3">Upper334 <p><i>zu(nz/3) or zu(nzt-3)</i></p> </td> <td style="vertical-align: middle;" width="57%"> <p lang="en-GB"><font face="Thorndale, serif"><font size="3">Upper 335 335 limit of the vertical range for which random perturbations are to be 336 336 imposed on the horizontal wind field (</font></font>in <font face="Thorndale, serif"><font size="3">m). <br> … … 832 832 <p><i>nz+1</i></p> </td> <td style="vertical-align: middle;" width="57%"> Limits 833 833 the output of 3d volume data along the vertical direction (grid point 834 index k).</td> </tr> <tr> <td style="vertical-align: middle;" width="15%"> <p><a href="chapter_4.1.html#omega"><b>omega</b></a></p>834 index k).</td> </tr> <tr><td align="undefined" valign="undefined"><a href="chapter_4.1.html#ocean"><span style="font-weight: bold;">ocean</span></a></td><td align="undefined" valign="undefined">I</td><td align="undefined" valign="undefined">L</td><td align="undefined" valign="undefined"><span style="font-style: italic;">.F.</span></td><td align="undefined" valign="undefined">Parameter to switch on ocean runs.</td></tr><tr> <td style="vertical-align: middle;" width="15%"> <p><a href="chapter_4.1.html#omega"><b>omega</b></a></p> 835 835 </td> <td style="vertical-align: middle;" width="5%"> 836 836 <p>I</p> </td> <td style="vertical-align: middle;" width="7%"> <p>R</p> … … 1194 1194 </td> <td style="vertical-align: middle;" width="16%"> 1195 1195 <p><i>0.1</i></p> </td> <td style="vertical-align: middle;" width="57%"> <p>Roughness 1196 length (in m). <br> </p> </td> </tr> <tr> 1196 length (in m). <br> </p> </td> </tr> <tr><td align="undefined" valign="undefined"><a href="chapter_4.1.html#sa_surface"><span style="font-weight: bold;">sa_surface</span></a></td><td align="undefined" valign="undefined">I</td><td align="undefined" valign="undefined">R</td><td align="undefined" valign="undefined"><span style="font-style: italic;">35.0</span></td><td align="undefined" valign="undefined">Surface salinity (in psu).</td></tr><tr><td align="undefined" valign="undefined"><a href="chapter_4.1.html#sa_vertical_gradient"><span style="font-weight: bold;">sa_vertical_gradient</span></a></td><td align="undefined" valign="undefined">I</td><td align="undefined" valign="undefined">R(10)</td><td align="undefined" valign="undefined"><span style="font-style: italic;">10 * 0.0</span></td><td align="undefined" valign="undefined">Salinity gradient(s) of the initial salinity profile (in psu 1197 / 100 m).</td></tr><tr><td align="undefined" valign="undefined"><a href="chapter_4.1.html#sa_vertical_gradient_level"><span style="font-weight: bold;">sa_vertical_gradient_level</span></a></td><td align="undefined" valign="undefined">I</td><td align="undefined" valign="undefined">R(10)</td><td align="undefined" valign="undefined"><span style="font-style: italic;">10 * 0.0</span></td><td align="undefined" valign="undefined">Height level from which on the salinity gradient defined by <a href="chapter_4.1.html#sa_vertical_gradient">sa_vertical_gradient</a> 1198 is effective (in m).</td></tr><tr> 1197 1199 <td style="vertical-align: middle;" width="15%"> <p><a href="chapter_4.1.html#scalar_advec"><b>scalar_advec</b></a></p> 1198 1200 </td> <td style="vertical-align: middle;" width="5%"> … … 1369 1371 <td>I</td> <td>C * 40</td> <td><span style="font-style: italic;">'flat'</span></td> <td>Topography 1370 1372 mode.</td> </tr> <tr><td><a style="font-weight: bold;" href="chapter_4.1.html#top_heatflux">top_heatflux</a></td><td>I</td><td>R</td><td><span style="font-style: italic;">no prescribed heatflux</span></td><td>Kinematic 1371 sensible heat flux at the top surface (in K m/s).</td></tr><tr> 1373 sensible heat flux at the top surface (in K m/s).</td></tr><tr><td align="undefined" valign="undefined"><a href="chapter_4.1.html#top_salinityflux"><span style="font-weight: bold;">top_salinityflux</span></a></td><td align="undefined" valign="undefined">I</td><td align="undefined" valign="undefined">R</td><td align="undefined" valign="undefined"><span style="font-style: italic;">no prescribed</span><br style="font-style: italic;"><span style="font-style: italic;">salinityflux</span></td><td align="undefined" valign="undefined">Kinematic 1374 salinity flux at the top boundary, i.e. the sea surface (in psu m/s).</td></tr><tr> 1372 1375 <td style="vertical-align: middle;" width="15%"> <p><a href="chapter_4.1.html#ug_surface"><b>ug_surface</b></a></p> 1373 1376 </td> <td style="vertical-align: middle;" width="5%"> -
palm/trunk/DOC/app/chapter_5.0.html
r83 r97 200 200 as the </font><a href="http://www.muk.uni-hannover.de/%7Eraasch/PALM_group/INSTALL/example_p3d"><font color="#000080">parameter 201 201 file</font></a><font color="#000000"> 202 (described in </font><a href="chapter_4.4. html"><font color="#000080">chapter203 4.4 </font></a>)<font color="#000000">. The202 (described in </font><a href="chapter_4.4.1.html"><font color="#000080">chapter 203 4.4.1</font></a>)<font color="#000000">. The 204 204 parameter file must be 205 205 copied from the PALM working copy by<br> -
palm/trunk/DOC/app/index.html
r94 r97 148 148 <p><span style="font-family: Thorndale;" lang="EN-GB">Current 149 149 model 150 version: 3. 2b<br>For date of last change see bottom line of each page. <o:p></o:p></span></p>150 version: 3.<br>For date of last change see bottom line of each page. <o:p></o:p></span></p> 151 151 <div style="text-align: center;" class="MsoNormal" align="center"><span style="font-family: Thorndale;"> 152 152 <hr align="center" size="2" width="100%"></span></div> … … 189 189 </span><span style="font-family: Thorndale;"><a href="chapter_4.3.html"><span style="" lang="EN-GB">4.3</span></a></span><span style="font-family: Thorndale;" lang="EN-GB"> User-defined 190 190 parameters <br> 191 </span><span style="font-family: Thorndale;"><a href="chapter_4.4.html"><span style="" lang="EN-GB">4.4</span></a></span><span style="font-family: Thorndale;" lang="EN-GB"> Example of a 192 minimum parameter set <br> 191 </span><span style="font-family: Thorndale;"><a href="chapter_4.4.html"><span style="" lang="EN-GB">4.4</span></a></span><span style="font-family: Thorndale;" lang="EN-GB"> Examples of parameter sets</span></p><div style="margin-left: 120px;"> <a href="chapter_4.4.1.html">4.4.1</a> A minimum parameter set for the CBL<br> <a href="chapter_4.4.2.html">4.4.2</a> A parameter set for ocean runs</div><p style="margin: 0cm 0cm 0.0001pt 72pt;"><span style="font-family: Thorndale;" lang="EN-GB"> 193 192 </span><span style="font-family: Thorndale;"><a href="chapter_4.5.html"><span style="" lang="EN-GB">4.5</span></a></span><span style="font-family: Thorndale;" lang="EN-GB"> Data analysis and 194 193 visualization <o:p></o:p></span></p> -
palm/trunk/DOC/tec/technical_documentation.html
r90 r97 12 12 <br><table nosave="" cellpadding="0" cellspacing="0"> <caption> <br> </caption><tbody> 13 13 </tbody><tbody> </tbody> <tbody> <tr nosave=""> <td nosave=""><b>Current 14 model version:</b></td> <td><span style="font-weight: bold;">3. 2b</span></td> </tr>14 model version:</b></td> <td><span style="font-weight: bold;">3.3</span></td> </tr> 15 15 <tr nosave=""> <td nosave=""><b>Last 16 16 change of this document</b>: </td> <td nosave=""><b>$Id$</b></td> </tr> … … 2311 2311 replaced by multiplication of the inverse. For performance 2312 2312 optimisation, this is done in the loop calculating the divergence 2313 instead of using a seperate loop.<br><br>Variables <span style="font-family: Courier New,Courier,monospace;">var_hom</span> and <span style="font-family: Courier New,Courier,monospace;">var_sum</span> are both renamed <span style="font-family: Courier New,Courier,monospace;">pr_palm</span>.</td><td style="vertical-align: top;">data_output_profiles, flow_statistics, init_3d_model, modules, parin, pres, read_var_list, run_control, time_integration</td></tr><tr><td style="vertical-align: top;"> </td><td style="vertical-align: top;"> </td><td style="vertical-align: top;"> </td><td style="vertical-align: top;">E</td><td style="vertical-align: top;">Bugfix: <span style="font-family: Courier New,Courier,monospace;">work_fft*_vec</span> removed from some PRIVATE-declarations (<span style="font-family: Courier New,Courier,monospace;">poisfft</span>).<br><br>Bugfix: <span style="font-family: Courier New,Courier,monospace;">field_chr</span> renamed <span style="font-family: Courier New,Courier,monospace;">field_char</span> (<span style="font-family: Courier New,Courier,monospace;">user_interface</span>).<br><br>Bugfix: output of <span style="font-family: Courier New,Courier,monospace;">use_upstream_for_tke</span> (<span style="font-family: Courier New,Courier,monospace;">header</span>).</td><td style="vertical-align: top;">header, poisfft, user_interface</td></tr> 2313 instead of using a seperate loop.<br><br>Variables <span style="font-family: Courier New,Courier,monospace;">var_hom</span> and <span style="font-family: Courier New,Courier,monospace;">var_sum</span> are both renamed <span style="font-family: Courier New,Courier,monospace;">pr_palm</span>.</td><td style="vertical-align: top;">data_output_profiles, flow_statistics, init_3d_model, modules, parin, pres, read_var_list, run_control, time_integration</td></tr><tr><td style="vertical-align: top;"> </td><td style="vertical-align: top;"> </td><td style="vertical-align: top;"> </td><td style="vertical-align: top;">E</td><td style="vertical-align: top;">Bugfix: <span style="font-family: Courier New,Courier,monospace;">work_fft*_vec</span> removed from some PRIVATE-declarations (<span style="font-family: Courier New,Courier,monospace;">poisfft</span>).<br><br>Bugfix: <span style="font-family: Courier New,Courier,monospace;">field_chr</span> renamed <span style="font-family: Courier New,Courier,monospace;">field_char</span> (<span style="font-family: Courier New,Courier,monospace;">user_interface</span>).<br><br>Bugfix: output of <span style="font-family: Courier New,Courier,monospace;">use_upstream_for_tke</span> (<span style="font-family: Courier New,Courier,monospace;">header</span>).</td><td style="vertical-align: top;">header, poisfft, user_interface</td></tr><tr><td style="vertical-align: top;">21/06/07</td><td style="vertical-align: top;">SR</td><td style="vertical-align: top;">3.3</td><td style="vertical-align: top;">N</td><td style="vertical-align: top;">This version allows runs for the ocean. Ocean runs can be switched on with the ne inipar-parameter <span style="font-family: Courier New,Courier,monospace;">ocean</span>.<br><br>Setting this switch has several effects:<br><ul><li>An additional prognostic equation for salinity is solved.</li><li>Potential temperature in buoyancy and stability-related terms is replaced by potential density.</li><li>Potential 2314 density is calculated from the equation of state for seawater after 2315 each timestep, using the algorithm proposed by Jackett et al. (2006, J. 2316 Atmos. Oceanic Technol., <span style="font-weight: bold;">23</span>, 1709-1728).<br>So far, only the initial hydrostatic pressure is entered into this equation.</li><li>z=0 (sea surface) is assumed at the model top (vertical grid index <span style="font-family: Courier New,Courier,monospace;">k=nzt</span> on the w-grid), with negative values of z indicating the depth.</li><li>Initial profiles are constructed (e.g. from <a href="http://www.muk.uni-hannover.de/%7Eraasch/PALM_group/doc/app/chapter_4.1.html#pt_vertical_gradient">pt_vertical_gradient</a> / <a href="http://www.muk.uni-hannover.de/%7Eraasch/PALM_group/doc/app/chapter_4.1.html#pt_vertical_gradient_level">pt_vertical_gradient_level</a>) starting from the sea surface, using surface values given by <a href="http://www.muk.uni-hannover.de/%7Eraasch/PALM_group/doc/app/chapter_4.1.html#pt_surface">pt_surface</a>, <a href="http://www.muk.uni-hannover.de/%7Eraasch/PALM_group/doc/app/chapter_4.1.html#sa_surface">sa_surface</a>, <a href="http://www.muk.uni-hannover.de/%7Eraasch/PALM_group/doc/app/chapter_4.1.html#ug_surface">ug_surface</a>, and <a href="http://www.muk.uni-hannover.de/%7Eraasch/PALM_group/doc/app/chapter_4.1.html#vg_surface">vg_surface</a>.</li><li>Zero salinity flux is used as default boundary condition at the bottom of the sea.</li><li>If switched on, random perturbations are by default imposed to the upper model domain from zu(nzt*2/3) to zu(nzt-3).</li></ul>Relevant new inipar-parameters to be exclusively used for steering ocean runs are <span style="font-family: Courier New,Courier,monospace;">bc_sa_t</span>, <span style="font-family: Courier New,Courier,monospace;">bottom_salinityflux</span>, <span style="font-family: Courier New,Courier,monospace;">sa_surface</span>, <span style="font-family: Courier New,Courier,monospace;">sa_vertical_gradient</span>, <span style="font-family: Courier New,Courier,monospace;">sa_vertical_gradient_level</span>, and <span style="font-family: Courier New,Courier,monospace;">top_salinityflux</span>.<br><br>Salinity (<span style="font-family: Courier New,Courier,monospace;">sa</span>) and potential density (<span style="font-family: Courier New,Courier,monospace;">rho</span>) are included as new 2d/3d output quantities. Vertical profiles of salinity (<span style="font-family: Courier New,Courier,monospace;">sa</span>), salinity fluxes (<span style="font-family: Courier New,Courier,monospace;">w"sa"</span>, <span style="font-family: Courier New,Courier,monospace;">w*sa*</span>, <span style="font-family: Courier New,Courier,monospace;">wsa</span>), and potential density (<span style="font-family: Courier New,Courier,monospace;">rho</span>) can also be output.<span style="font-family: Courier New,Courier,monospace;"></span></td><td style="vertical-align: top;">advec_s_bc, 2317 average_3d_data, boundary_conds, buoyancy, check_parameters, 2318 data_output_2d, data_output_3d, diffusion_e, flow_statistics, header, 2319 init_grid, init_3d_model, modules, netcdf, parin, production_e, 2320 prognostic_equations, read_var_list, sum_up_3d_data, swap_timelevel, 2321 time_integration, user_interface, write_var_list, write_3d_binary<br><br><span style="font-weight: bold;">new:</span><br>eqn_state_seawater, init_ocean</td></tr><tr><td style="vertical-align: top;"> </td><td style="vertical-align: top;"> </td><td style="vertical-align: top;"> </td><td style="vertical-align: top;">C</td><td style="vertical-align: top;">Inipar-parameter <span style="font-family: Courier New,Courier,monospace;">use_pt_reference</span> renamed <span style="font-family: Courier New,Courier,monospace;">use_reference.</span><br>Internal variable <span style="font-family: Courier New,Courier,monospace;">hydro_press</span> renamed <span style="font-family: Courier New,Courier,monospace;">hyp</span>, routine <span style="font-family: Courier New,Courier,monospace;">calc_mean_pt_profile</span> renamed <span style="font-family: Courier New,Courier,monospace;">calc_mean_profile</span>.<br><br>The format of the <span style="font-family: Courier New,Courier,monospace;">RUN_CONTROL</span> file has been adjusted for ocean runs.</td><td style="vertical-align: top;">advec_particles, 2322 buoyancy, calc_liquid_water_content, check_parameters, diffusion_e, 2323 diffusivities, header, init_cloud_physics, modules, production_e, 2324 prognostic_equations, run_control</td></tr><tr><td style="vertical-align: top;"> </td><td style="vertical-align: top;"> </td><td style="vertical-align: top;"> </td><td style="vertical-align: top;">E</td><td style="vertical-align: top;"></td><td style="vertical-align: top;"></td></tr> 2314 2325 </tbody> 2315 2326 </table> <b><blink>Attention:</blink></b> -
palm/trunk/INSTALL/example_rc
r91 r97 1 1 2 ************************* ---------------------------- 3 * PALM 3. 2b Rev: 91 *3D - run without 1D - prerun4 ************************* ---------------------------- 5 6 Date: 30-05-07 Run: example7 Time: 1 1:36:42Run-No.: 002 ************************* ------------------------------------------ 3 * PALM 3.3 Rev: 96M * atmosphere - 3D - run without 1D - prerun 4 ************************* ------------------------------------------ 5 6 Date: 21-06-07 Run: example 7 Time: 10:04:24 Run-No.: 00 8 8 Run on host: ibmh 9 9 Number of PEs: 8 Processor grid (x,y): ( 8, 1) forced … … 67 67 68 68 Bottom surface fluxes are used in diffusion terms at k=1 69 Predefined constant heatflux: 0.100 K m/s69 Predefined constant heatflux: 0.100000 K m/s 70 70 71 71 … … 161 161 162 162 Height: 0.0 0.0 m 163 vg: 0.00 0.00 m/ S163 vg: 0.00 0.00 m/s 164 164 Gradient: ------ 0.00 1/100s 165 165 Gridpoint: 0 0 … … 182 182 ----------------------------- 183 183 184 Disturbance impulse (u,v) every : 150.00 s185 Disturbance amplitude : 0.25 m/s186 Lower disturbance level : 125.00 m (GP 3)187 Upper disturbance level : 625.00 m (GP 13)184 Disturbance impulse (u,v) every : 150.00 s 185 Disturbance amplitude : 0.25 m/s 186 Lower disturbance level : 125.00 m (GP 3) 187 Upper disturbance level : 625.00 m (GP 13) 188 188 Disturbances cease as soon as the disturbance energy exceeds 0.010 m**2/s**2 189 189 Random number generator used : numerical-recipes … … 200 200 ------------------ 201 201 202 RUN ITER. HH:MM:SS.SS DT(E) UMAX VMAX WMAX U* W* THETA*Z_I ENERG. 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0 117 00:26:30.35 12.4000A -1.8927 -2.4874 3.6369 0.111 1.38 -1.309800. 0.258E+00 0.258E+00 0.215E-03 0.283E-13 1 12 21 1 21 29 11 31 25 0.000 0.000 0322 0 118 00:26:42.15 11.8000A -1.8986 -2.4592 3.8114 0.111 1.32 -1.289700. 0.257E+00 0.256E+00 0.204E-03 0.269E-13 1 12 21 1 21 29 12 32 24 0.000 0.000 0323 0 119 00:26:53.75 11.6000A -1.8863 -2.3871 3.8812 0.112 1.38 -1.266800. 0.255E+00 0.255E+00 0.200E-03 0.264E-13 1 12 21 1 21 29 12 32 24 0.000 0.000 0324 0 120 00:27:06.05 12.3000A -1.8581 2.3788 3.6552 0.112 1.38 -1.261800. 0.254E+00 0.253E+00 0.212E-03 0.279E-13 1 12 21 1 9 14 6 17 31 0.000 0.000 0325 0 121 00:27:17.75 11.7000A 1.8904 2.3906 3.8390 0.113 1.38 -1.271800. 0.252E+00 0.252E+00 0.202E-03 0.265E-13 1 18 21 1 9 14 7 17 31 0.000 0.000 0326 0 122 00:27:29.15 11.4000A 1.9592 2.3621 3.9512 0.113 1.38 -1.324800. 0.251E+00 0.250E+00 0.197E-03 0.258E-13 1 18 21 1 9 14 7 17 31 0.000 0.000 0327 0 123 00:27:40.85 11.7000A 1.9816 2.3757 3.8623 0.113 1.38 -1.271800. 0.249E+00 0.249E+00 0.201E-03 0.264E-13 1 18 21 1 10 14 8 17 31 0.000 0.000 0328 0 124 00:27:51.65 10.8000A 1.9569 2.4083 4.1477 0.114 1.38 -1.261800. 0.248E+00 0.248E+00 0.186E-03 0.244E-13 1 18 21 1 10 14 8 17 31 0.000 0.000 0329 0 125 00:28:03.35 11.7000A 1.8962 2.4093 3.8427 0.114 1.38 -1.251800. 0.246E+00 0.246E+00 0.201E-03 0.263E-13 1 18 21 1 10 14 8 17 31 0.000 0.000 0330 0 126 00:28:14.55 11.2000A 2.0100 2.3683 4.0348 0.115 1.35 -1.277750. 0.245E+00 0.244E+00 0.192E-03 0.251E-13 1 17 21 1 10 14 9 17 31 0.000 0.000 0331 0 127 00:28:26.45 11.9000A 2.0906 2.2885 3.7964 0.115 1.35 -1.246750. 0.243E+00 0.243E+00 0.202E-03 0.266E-13 1 17 21 1 10 14 9 17 31 0.000 0.000 0332 0 128 00:28:38.55 12.1000A 2.0912 2.1695 3.7179 0.115 1.35 -1.228750. 0.241E+00 0.241E+00 0.205E-03 0.270E-13 1 17 21 1 10 14 10 17 31 0.000 0.000 0333 0 129 00:28:51.25 12.7000A 2.0014 2.2106 3.5318 0.115 1.35 -1.221750. 0.239E+00 0.239E+00 0.214E-03 0.282E-13 1 17 21 1 12 13 10 17 31 0.000 0.000 0334 0 130 00:29:04.95 13.7000A 1.9390 2.2557 3.2948 0.116 1.38 -1.212800. 0.237E+00 0.237E+00 0.229E-03 0.302E-13 1 20 22 1 12 13 15 31 24 0.000 0.000 0335 0 131 00:29:18.55 13.6000A 1.9902 2.2448 3.3144 0.116 1.41 -1.192850. 0.235E+00 0.235E+00 0.226E-03 0.298E-13 1 20 22 1 12 13 15 31 24 0.000 0.000 0336 0 132 00:29:33.05 14.5000A 2.0400 2.1833 3.1107 0.116 1.35 -1.200750. 0.232E+00 0.232E+00 0.239E-03 0.315E-13 1 20 22 1 12 13 12 22 13 0.000 0.000 0337 0 133 00:29:47.05 14.0000A 2.0818 2.2418 3.2104 0.115 1.35 -1.279750. 0.230E+00 0.230E+00 0.230E-03 0.303E-13 1 20 22 1 8 16 16 31 24 0.000 0.000 0338 0 134 00:30:01.75 14.7000A 2.1591 2.3083 3.0512 0.115 1.35 -1.240750. 0.228E+00 0.227E+00 0.239E-03 0.315E-13 1 19 22 1 8 16 4 13 17 0.000 0.000 0339 0 135 00:30:16.45 14.7000A 2.2191 2.2636 3.0590 0.115 1.35 -1.210750. 0.225E+00 0.225E+00 0.238E-03 0.312E-13 1 19 22 1 8 16 13 22 13 0.000 0.000 0340 0 136 00:30:31.25 14.8000A 2.2333 2.1717 3.0444 0.115 1.35 -1.222750. 0.223E+00 0.223E+00 0.237E-03 0.312E-13 1 19 22 1 9 16 5 13 17 0.000 0.000 0341 0 137 00:30:44.75 13.5000A 2.2022 2.1157 3.3321 0.114 1.41 -1.211850. 0.221E+00 0.221E+00 0.215E-03 0.282E-13 1 19 22 1 9 16 10 12 34 0.000 0.000 0342 0 138 00:30:57.95 13.2000A 2.1843 2.1377 3.4048 0.114 1.41 -1.209850. 0.219E+00 0.219E+00 0.209E-03 0.273E-13 1 19 23 1 14 12 10 12 34 0.000 0.000 0343 0 139 00:31:11.35 13.4000A 2.2430 2.2057 3.3692 0.113 1.41 -1.234850. 0.217E+00 0.217E+00 0.210E-03 0.274E-13 1 19 23 1 14 12 11 12 34 0.000 0.000 0344 0 140 00:31:24.65 13.3000A 2.2595 2.2050 3.3818 0.113 1.38 -1.262800. 0.216E+00 0.215E+00 0.207E-03 0.269E-13 1 19 23 1 14 12 11 12 34 0.000 0.000 0345 0 141 00:31:38.15 13.5000A 2.2351 2.1414 3.3251 0.112 1.38 -1.359800. 0.214E+00 0.213E+00 0.207E-03 0.270E-13 1 19 23 1 14 12 12 11 19 0.000 0.000 0346 0 142 00:31:51.75 13.6000A 2.1849 2.0937 3.3170 0.111 1.38 -1.246800. 0.212E+00 0.212E+00 0.206E-03 0.268E-13 1 19 23 2 13 13 12 11 19 0.000 0.000 0347 0 143 00:32:05.85 14.1000A 2.1665 2.0911 3.1984 0.110 1.38 -1.277800. 0.211E+00 0.210E+00 0.212E-03 0.274E-13 1 19 24 1 12 12 13 11 19 0.000 0.000 0348 0 144 00:32:19.35 13.5000A 2.2330 2.1961 3.3346 0.109 1.38 -1.268800. 0.209E+00 0.209E+00 0.201E-03 0.259E-13 1 19 24 2 14 13 13 11 19 0.000 0.000 0349 0 145 00:32:33.05 13.7000A 2.2358 2.2598 3.2746 0.109 1.38 -1.293800. 0.208E+00 0.207E+00 0.202E-03 0.260E-13 1 19 24 2 14 13 14 12 21 0.000 0.000 0350 0 146 00:32:47.05 14.0000A 2.1896 2.3099 3.2130 0.108 1.38 -1.292800. 0.207E+00 0.206E+00 0.205E-03 0.263E-13 1 19 24 1 13 12 14 11 19 0.000 0.000 0351 0 147 00:33:01.35 14.3000A 2.1024 2.3477 3.1369 0.107 1.38 -1.310800. 0.205E+00 0.205E+00 0.208E-03 0.267E-13 1 19 24 1 13 12 15 12 21 0.000 0.000 0352 0 148 00:33:16.25 14.9000A 1.9940 2.3109 3.0124 0.106 1.38 -1.321800. 0.204E+00 0.204E+00 0.215E-03 0.276E-13 1 19 24 1 13 12 15 11 19 0.000 0.000 0353 0 149 00:33:30.85 14.6000A 2.0083 2.2570 3.0910 0.105 1.38 -1.327800. 0.204E+00 0.203E+00 0.209E-03 0.268E-13 1 17 24 1 13 13 16 12 21 0.000 0.000 0354 0 150 00:33:46.25 15.4000A 2.0296 2.2387 2.9235 0.105 1.38 -1.371800. 0.203E+00 0.202E+00 0.219E-03 0.281E-13 1 17 24 1 13 13 5 29 18 0.000 0.000 0355 0 151 00:34:00.95 14.7000A 1.9808 2.2175 3.0615 0.104 1.38 -1.383800. 0.202E+00 0.202E+00 0.208E-03 0.267E-13 1 17 24 1 14 13 6 29 18 0.000 0.000 0356 0 152 00:34:15.15 14.2000A -1.9396 2.3781 3.1723 0.104 1.38 -1.361800. 0.202E+00 0.201E+00 0.200E-03 0.257E-13 1 39 5 1 14 13 8 28 17 0.000 0.000 0357 0 153 00:34:28.55 13.4000A 2.0675 2.4704 3.3549 0.103 1.38 -1.363800. 0.202E+00 0.201E+00 0.189E-03 0.242E-13 1 17 25 1 14 13 9 28 17 0.000 0.000 0358 0 154 00:34:41.35 12.8000A -2.1421 2.4901 3.5091 0.103 1.38 -1.394800. 0.202E+00 0.201E+00 0.180E-03 0.230E-13 1 39 4 1 14 13 9 28 17 0.000 0.000 0359 0 155 00:34:53.85 12.5000A -2.1948 2.4409 3.5981 0.102 1.38 -1.476800. 0.202E+00 0.201E+00 0.176E-03 0.225E-13 1 39 4 1 14 13 10 28 17 0.000 0.000 0360 0 156 00:35:06.25 12.4000A -2.2082 2.3277 3.6269 0.102 1.38 -1.437800. 0.202E+00 0.201E+00 0.174E-03 0.222E-13 1 39 4 1 14 13 10 28 17 0.000 0.000 0361 0 157 00:35:18.45 12.2000A -2.1825 2.3456 3.6988 0.102 1.38 -1.430800. 0.202E+00 0.201E+00 0.172E-03 0.218E-13 1 39 4 1 15 13 11 28 17 0.000 0.000 0362 0 158 00:35:30.25 11.8000A -2.1227 2.4465 3.8015 0.101 1.38 -1.429800. 0.202E+00 0.202E+00 0.166E-03 0.211E-13 1 39 4 1 15 13 12 28 17 0.000 0.000 0363 0 159 00:35:42.05 11.8000A -2.0764 2.4870 3.8084 0.101 1.38 -1.436800. 0.203E+00 0.202E+00 0.166E-03 0.211E-13 1 39 3 1 15 13 13 28 17 0.000 0.000 0364 0 160 00:35:53.35 11.3000A -2.1034 2.4705 3.9746 0.101 1.38 -1.445800. 0.203E+00 0.202E+00 0.159E-03 0.201E-13 1 39 3 1 15 13 13 28 17 0.000 0.000 0365 0 161 00:36:04.85 11.5000A -2.0989 2.4038 3.9139 0.101 1.38 -1.433800. 0.203E+00 0.203E+00 0.162E-03 0.205E-13 1 39 3 1 15 13 14 28 17 0.000 0.000 0366 0 162 00:36:16.15 11.3000A -2.0703 2.2906 3.9650 0.100 1.38 -1.390800. 0.204E+00 0.203E+00 0.159E-03 0.201E-13 1 38 3 1 15 13 14 28 17 0.000 0.000 0367 0 163 00:36:27.75 11.6000A -2.0480 2.1660 3.8904 0.100 1.38 -1.357800. 0.205E+00 0.204E+00 0.163E-03 0.206E-13 1 38 3 2 16 13 15 28 17 0.000 0.000 0368 0 164 00:36:39.35 11.6000A -2.1133 2.1887 3.8849 0.100 1.38 -1.347800. 0.205E+00 0.204E+00 0.164E-03 0.207E-13 1 36 1 2 16 13 15 28 17 0.000 0.000 0369 0 165 00:36:51.55 12.2000A -2.1418 2.1803 3.6824 0.100 1.38 -1.337800. 0.206E+00 0.205E+00 0.172E-03 0.217E-13 1 36 1 2 16 13 15 29 17 0.000 0.000 0370 0 166 00:37:04.25 12.7000A -2.1389 2.1311 3.5539 0.100 1.41 -1.324850. 0.207E+00 0.206E+00 0.179E-03 0.227E-13 1 36 0 2 16 13 14 27 16 0.000 0.000 0371 0 167 00:37:16.25 12.0000A -2.2340 -2.1121 3.7401 0.100 1.41 -1.331850. 0.207E+00 0.207E+00 0.170E-03 0.215E-13 1 36 0 1 33 14 16 29 17 0.000 0.000 0372 0 168 00:37:28.45 12.2000A -2.2833 -2.1292 3.6824 0.100 1.41 -1.384850. 0.208E+00 0.208E+00 0.173E-03 0.218E-13 1 36 0 1 33 14 15 27 16 0.000 0.000 0373 0 169 00:37:40.55 12.1000A -2.2947 -2.1121 3.7140 0.100 1.41 -1.353850. 0.209E+00 0.208E+00 0.171E-03 0.216E-13 1 36 0 1 33 14 16 27 16 0.000 0.000 0374 0 170 00:37:52.85 12.3000A -2.2741 -2.0710 3.6688 0.100 1.41 -1.364850. 0.210E+00 0.209E+00 0.174E-03 0.220E-13 1 36 0 1 33 14 16 27 16 0.000 0.000 0375 0 171 00:38:05.65 12.8000A -2.2272 -2.0980 3.5117 0.100 1.43 -1.378900. 0.211E+00 0.210E+00 0.181E-03 0.229E-13 1 36 0 1 32 16 17 27 16 0.000 0.000 0376 0 172 00:38:18.75 13.1000A -2.1531 -2.1396 3.4286 0.100 1.43 -1.432900. 0.212E+00 0.211E+00 0.186E-03 0.235E-13 1 36 0 1 32 17 17 27 16 0.000 0.000 0377 0 173 00:38:31.35 12.6000A -2.1886 -2.1599 3.5630 0.100 1.43 -1.399900. 0.213E+00 0.212E+00 0.179E-03 0.226E-13 1 35 39 1 32 15 16 29 18 0.000 0.000 0378 0 174 00:38:44.55 13.2000A -2.2034 -2.2233 3.4144 0.101 1.43 -1.360900. 0.214E+00 0.213E+00 0.188E-03 0.237E-13 1 35 39 1 32 15 16 29 18 0.000 0.000 0379 0 175 00:38:58.35 13.8000A -2.1963 -2.2318 3.2641 0.101 1.43 -1.355900. 0.215E+00 0.214E+00 0.197E-03 0.248E-13 1 35 38 1 32 15 17 29 18 0.000 0.000 0380 0 176 00:39:11.65 13.3000A -2.2648 -2.1778 3.3896 0.101 1.43 -1.382900. 0.217E+00 0.216E+00 0.190E-03 0.240E-13 1 35 37 1 32 15 17 29 18 0.000 0.000 0381 0 177 00:39:24.75 13.1000A -2.3021 -2.1965 3.4373 0.101 1.41 -1.350850. 0.218E+00 0.217E+00 0.188E-03 0.238E-13 1 35 37 1 31 17 9 24 19 0.000 0.000 0382 0 178 00:39:38.35 13.6000A -2.2284 -2.2747 3.3046 0.101 1.41 -1.355850. 0.220E+00 0.219E+00 0.196E-03 0.247E-13 1 35 37 1 31 15 11 4 0 0.000 0.000 0383 0 179 00:39:51.15 12.8000A -2.0787 -2.3151 3.5256 0.102 1.41 -1.352850. 0.221E+00 0.220E+00 0.186E-03 0.234E-13 1 35 37 1 31 15 10 24 19 0.000 0.000 0384 0 180 00:40:04.85 13.7000A -2.1455 -2.2906 3.2776 0.102 1.41 -1.378850. 0.223E+00 0.222E+00 0.199E-03 0.251E-13 2 35 37 1 31 15 8 4 1 0.000 0.000 0385 0 181 00:40:17.85 13.0000A -2.1908 -2.2108 3.4580 0.102 1.41 -1.446850. 0.225E+00 0.224E+00 0.190E-03 0.240E-13 2 35 37 1 31 15 11 24 19 0.000 0.000 0386 0 182 00:40:31.55 13.7000A -2.1518 -2.2091 3.2922 0.102 1.41 -1.524850. 0.227E+00 0.226E+00 0.201E-03 0.253E-13 2 35 37 1 30 17 9 25 19 0.000 0.000 0387 0 183 00:40:44.95 13.4000A -2.0486 -2.1944 3.3582 0.102 1.41 -1.488850. 0.228E+00 0.227E+00 0.197E-03 0.250E-13 2 35 37 1 30 17 9 25 19 0.000 0.000 0388 0 184 00:40:58.45 13.5000A -2.1237 -2.1819 3.3254 0.102 1.41 -1.514850. 0.230E+00 0.229E+00 0.200E-03 0.253E-13 1 33 39 1 30 16 10 25 19 0.000 0.000 0389 0 185 00:41:11.85 13.4000A -2.3131 -2.1145 3.3668 0.102 1.41 -1.464850. 0.232E+00 0.231E+00 0.199E-03 0.253E-13 1 33 39 1 30 16 10 25 19 0.000 0.000 0390 0 186 00:41:25.25 13.4000A -2.3425 -2.1211 3.3569 0.102 1.41 -1.447850. 0.234E+00 0.233E+00 0.200E-03 0.255E-13 1 33 39 1 29 16 6 19 12 0.000 0.000 0391 0 187 00:41:38.65 13.4000A -2.2166 -2.1463 3.3697 0.102 1.41 -1.448850. 0.237E+00 0.236E+00 0.202E-03 0.257E-13 1 33 39 1 29 16 10 24 19 0.000 0.000 0392 0 188 00:41:51.95 13.3000A -2.2932 -2.1146 3.3771 0.102 1.41 -1.747850. 0.239E+00 0.238E+00 0.201E-03 0.257E-13 1 33 38 1 29 16 12 23 19 0.000 0.000 0393 0 189 00:42:05.05 13.1000A -2.2620 -2.0345 3.4445 0.102 1.41 -1.442850. 0.241E+00 0.240E+00 0.199E-03 0.255E-13 1 33 38 1 29 16 12 23 19 0.000 0.000 0394 0 190 00:42:17.35 12.3000A -2.1635 -2.0145 3.6599 0.102 1.41 -1.421850. 0.243E+00 0.242E+00 0.188E-03 0.242E-13 1 33 37 1 28 16 13 23 19 0.000 0.000 0395 0 191 00:42:30.25 12.9000A -2.2627 -2.0551 3.4893 0.102 1.41 -1.415850. 0.245E+00 0.244E+00 0.198E-03 0.255E-13 1 33 37 1 28 16 13 23 19 0.000 0.000 0396 0 192 00:42:42.75 12.5000A -2.2475 -2.0437 3.5914 0.102 1.41 -1.393850. 0.247E+00 0.246E+00 0.193E-03 0.250E-13 1 33 37 1 28 16 14 23 19 0.000 0.000 0397 0 193 00:42:54.65 11.9000A -2.1510 -1.9858 3.7727 0.102 1.41 -1.389850. 0.249E+00 0.248E+00 0.185E-03 0.240E-13 1 33 37 1 28 16 13 22 19 0.000 0.000 0398 0 194 00:43:06.85 12.2000A -2.1072 -1.9327 3.6867 0.102 1.41 -1.377850. 0.251E+00 0.251E+00 0.191E-03 0.247E-13 3 33 37 1 27 17 9 25 21 0.000 0.000 0399 0 195 00:43:18.25 11.4000A -2.2110 -1.9839 3.9372 0.103 1.41 -1.381850. 0.253E+00 0.252E+00 0.179E-03 0.232E-13 3 33 36 1 27 16 14 22 19 0.000 0.000 0400 0 196 00:43:30.35 12.1000A -2.3085 -1.9925 3.7169 0.103 1.41 -1.389850. 0.255E+00 0.254E+00 0.191E-03 0.248E-13 3 33 36 1 27 16 10 25 21 0.000 0.000 0401 0 197 00:43:42.45 12.1000A -2.2490 -1.9568 3.7300 0.103 1.41 -1.488850. 0.257E+00 0.256E+00 0.192E-03 0.249E-13 3 33 36 1 27 16 15 22 19 0.000 0.000 0402 0 198 00:43:55.05 12.6000A -2.1129 -2.1141 3.5698 0.103 1.41 -1.407850. 0.259E+00 0.258E+00 0.201E-03 0.260E-13 4 33 36 16 24 19 13 24 21 0.000 0.000 0403 0 199 00:44:07.45 12.4000A -2.1621 -2.1360 3.6177 0.103 1.41 -1.389850. 0.261E+00 0.260E+00 0.198E-03 0.257E-13 4 33 35 16 24 19 13 24 21 0.000 0.000 0404 0 200 00:44:20.05 12.6000A -2.1546 -2.0910 3.5651 0.103 1.41 -1.546850. 0.262E+00 0.262E+00 0.202E-03 0.262E-13 4 33 35 16 23 19 14 24 21 0.000 0.000 0405 0 201 00:44:32.35 12.3000A -2.1403 -2.1132 3.6536 0.103 1.41 -1.387850. 0.264E+00 0.263E+00 0.198E-03 0.257E-13 6 33 35 16 23 19 14 24 21 0.000 0.000 0406 0 202 00:44:45.05 12.7000A 2.1499 -2.0291 3.5545 0.103 1.41 -1.383850. 0.266E+00 0.265E+00 0.206E-03 0.266E-13 17 26 27 17 23 19 13 26 20 0.000 0.000 0407 0 203 00:44:57.35 12.3000A -2.3283 -2.2776 3.6453 0.103 1.41 -1.376850. 0.268E+00 0.267E+00 0.200E-03 0.259E-13 7 33 35 17 23 19 13 29 18 0.000 0.000 0408 0 204 00:45:09.95 12.6000A -2.2436 -2.2474 3.5840 0.103 1.41 -1.389850. 0.269E+00 0.269E+00 0.206E-03 0.267E-13 7 33 34 17 23 19 14 29 18 0.000 0.000 0409 0 205 00:45:21.95 12.0000A -2.4079 2.1885 3.7346 0.103 1.41 -1.347850. 0.271E+00 0.270E+00 0.197E-03 0.255E-13 7 33 34 2 33 8 14 29 18 0.000 0.000 0410 0 206 00:45:34.65 12.7000A -2.2052 -2.0276 3.5531 0.103 1.41 -1.347850. 0.273E+00 0.272E+00 0.209E-03 0.271E-13 8 33 34 18 19 17 14 29 18 0.000 0.000 0411 0 207 00:45:47.85 13.2000A -2.2890 -1.9557 3.4207 0.103 1.41 -1.335850. 0.274E+00 0.274E+00 0.218E-03 0.282E-13 8 33 34 18 19 17 15 29 18 0.000 0.000 0412 0 208 00:46:00.95 13.1000A -2.4871 -1.9230 3.4310 0.103 1.41 -1.346850. 0.276E+00 0.275E+00 0.218E-03 0.281E-13 8 33 33 17 21 19 6 12 21 0.000 0.000 0413 0 209 00:46:14.55 13.6000A -2.4420 -1.9949 3.3004 0.103 1.41 -1.331850. 0.278E+00 0.277E+00 0.227E-03 0.293E-13 8 33 33 19 19 17 11 13 19 0.000 0.000 0414 0 210 00:46:27.25 12.7000A -2.3831 -2.0990 3.5476 0.103 1.41 -1.325850. 0.279E+00 0.278E+00 0.214E-03 0.276E-13 9 33 33 19 19 17 11 22 13 0.000 0.000 0415 0 211 00:46:40.15 12.9000A -2.2837 -2.0889 3.4969 0.103 1.41 -1.353850. 0.281E+00 0.280E+00 0.218E-03 0.283E-13 9 33 33 19 19 17 10 33 32 0.000 0.000 0416 0 212 00:46:52.75 12.6000A -2.1846 -1.9886 3.5727 0.103 1.41 -1.326850. 0.282E+00 0.281E+00 0.214E-03 0.278E-13 9 33 32 19 19 17 12 22 13 0.000 0.000 0417 0 213 00:47:04.65 11.9000A -2.1743 1.9090 3.7804 0.103 1.41 -1.334850. 0.283E+00 0.283E+00 0.204E-03 0.264E-13 9 33 32 16 13 2 12 22 13 0.000 0.000 0418 0 214 00:47:17.05 12.4000A -2.2333 1.9174 3.6276 0.103 1.41 -1.350850. 0.285E+00 0.284E+00 0.213E-03 0.277E-13 10 33 32 16 13 2 12 22 13 0.000 0.000 0419 0 215 00:47:29.25 12.2000A -2.2272 -1.9391 3.6992 0.103 1.41 -1.362850. 0.286E+00 0.285E+00 0.210E-03 0.273E-13 10 33 32 18 17 15 9 13 21 0.000 0.000 0420 0 216 00:47:41.25 12.0000A -2.2859 1.8975 3.7647 0.103 1.41 -1.350850. 0.287E+00 0.286E+00 0.207E-03 0.269E-13 11 33 32 8 17 21 9 13 21 0.000 0.000 0421 0 217 00:47:53.65 12.4000A -2.2967 1.8824 3.6182 0.103 1.41 -1.374850. 0.288E+00 0.287E+00 0.214E-03 0.279E-13 11 33 32 13 37 32 10 13 21 0.000 0.000 0422 0 218 00:48:04.85 11.2000A -2.3389 -1.8994 4.0037 0.103 1.41 -1.387850. 0.289E+00 0.288E+00 0.195E-03 0.253E-13 12 14 20 18 16 15 8 32 34 0.000 0.000 0423 0 219 00:48:16.35 11.5000A -2.3017 -1.8955 3.9243 0.103 1.41 -1.346850. 0.290E+00 0.289E+00 0.200E-03 0.259E-13 12 33 32 18 16 15 8 32 34 0.000 0.000 0424 0 220 00:48:27.95 11.6000A -2.2801 -1.8107 3.8921 0.103 1.41 -1.346850. 0.291E+00 0.290E+00 0.202E-03 0.262E-13 12 33 32 18 16 15 9 32 34 0.000 0.000 0425 0 221 00:48:38.95 11.0000A -2.3353 1.8971 4.0946 0.103 1.41 -1.448850. 0.292E+00 0.291E+00 0.192E-03 0.249E-13 12 14 19 19 34 18 9 32 34 0.000 0.000 0426 0 222 00:48:50.35 11.4000A -2.3480 1.9730 3.9428 0.103 1.41 -1.364850. 0.293E+00 0.292E+00 0.199E-03 0.258E-13 13 33 32 19 34 18 10 36 36 0.000 0.000 0427 0 223 00:49:01.15 10.8000A -2.4248 1.9834 4.1749 0.103 1.41 -1.370850. 0.294E+00 0.292E+00 0.190E-03 0.245E-13 13 33 32 19 34 18 11 36 36 0.000 0.000 0428 0 224 00:49:11.95 10.8000A -2.3497 2.0124 4.1524 0.102 1.41 -1.364850. 0.294E+00 0.293E+00 0.190E-03 0.245E-13 13 33 31 9 11 24 11 36 36 0.000 0.000 0429 0 225 00:49:22.55 10.6000A -2.2984 1.9886 4.2486 0.102 1.41 -1.354850. 0.295E+00 0.294E+00 0.187E-03 0.241E-13 13 33 31 9 11 24 12 36 36 0.000 0.000 0430 0 226 00:49:33.25 10.7000A -2.1881 -1.9134 4.1931 0.102 1.41 -1.366850. 0.295E+00 0.294E+00 0.189E-03 0.243E-13 13 33 30 17 12 16 12 36 36 0.000 0.000 0431 0 227 00:49:43.95 10.7000A -2.1459 -1.8974 4.1883 0.102 1.41 -1.415850. 0.296E+00 0.294E+00 0.189E-03 0.243E-13 13 33 30 17 12 16 13 36 36 0.000 0.000 0432 0 228 00:49:55.25 11.3000A -2.1716 1.9677 3.9908 0.102 1.41 -1.485850. 0.296E+00 0.295E+00 0.199E-03 0.256E-13 13 33 33 10 11 24 13 36 36 0.000 0.000 0433 0 229 00:50:05.95 10.7000A -2.0255 1.9272 4.2063 0.102 1.41 -1.460850. 0.296E+00 0.295E+00 0.189E-03 0.242E-13 13 33 33 10 11 24 14 36 36 0.000 0.000 0434 0 230 00:50:17.25 11.3000A -2.1013 2.0264 3.9819 0.101 1.41 -1.422850. 0.296E+00 0.295E+00 0.199E-03 0.255E-13 14 34 33 12 25 11 14 36 36 0.000 0.000 0435 0 231 00:50:28.45 11.2000A -2.2268 2.0277 4.0155 0.101 1.41 -1.397850. 0.297E+00 0.295E+00 0.197E-03 0.253E-13 14 33 33 12 25 11 13 34 36 0.000 0.000 0436 0 232 00:50:39.95 11.5000A -2.1561 1.9510 3.9187 0.101 1.41 -1.401850. 0.297E+00 0.295E+00 0.202E-03 0.259E-13 14 33 33 13 25 11 14 36 35 0.000 0.000 0437 0 233 00:50:51.25 11.3000A 2.0123 2.0613 3.9748 0.101 1.41 -1.356850. 0.297E+00 0.295E+00 0.198E-03 0.254E-13 1 10 23 13 25 11 9 10 35 0.000 0.000 0438 0 234 00:51:02.65 11.4000A 1.9909 1.9421 3.9506 0.100 1.41 -1.348850. 0.297E+00 0.295E+00 0.199E-03 0.255E-13 1 10 23 13 25 11 15 34 36 0.000 0.000 0439 0 235 00:51:13.75 11.1000A 2.0510 1.8487 4.0423 0.100 1.41 -1.358850. 0.297E+00 0.295E+00 0.194E-03 0.248E-13 1 12 24 13 26 11 10 10 35 0.000 0.000 0440 0 236 00:51:25.55 11.8000A 2.0598 1.8076 3.8212 0.100 1.43 -1.355900. 0.297E+00 0.295E+00 0.206E-03 0.263E-13 1 12 24 13 26 11 10 10 35 0.000 0.000 0441 0 237 00:51:36.85 11.3000A -2.1549 -1.9421 3.9902 0.100 1.43 -1.364900. 0.296E+00 0.295E+00 0.197E-03 0.252E-13 19 27 23 13 13 15 11 10 35 0.000 0.000 0442 0 238 00:51:48.65 11.8000A -2.3317 -1.9758 3.8232 0.099 1.43 -1.375900. 0.296E+00 0.295E+00 0.205E-03 0.263E-13 19 27 23 13 13 15 11 10 35 0.000 0.000 0443 0 239 00:52:00.55 11.9000A -2.3765 1.8428 3.7772 0.099 1.43 -1.393900. 0.296E+00 0.295E+00 0.207E-03 0.266E-13 19 27 23 19 29 15 15 35 35 0.000 0.000 0444 0 240 00:52:12.75 12.2000A -2.2713 1.8206 3.6794 0.099 1.43 -1.437900. 0.296E+00 0.294E+00 0.212E-03 0.272E-13 19 27 23 6 10 23 15 35 35 0.000 0.000 0445 0 241 00:52:24.95 12.2000A 2.2123 1.8394 3.6844 0.099 1.43 -1.442900. 0.295E+00 0.294E+00 0.212E-03 0.272E-13 1 12 25 6 10 23 16 35 35 0.000 0.000 0446 0 242 00:52:37.05 12.1000A -2.2668 1.8654 3.7059 0.099 1.43 -1.438900. 0.295E+00 0.294E+00 0.210E-03 0.271E-13 19 27 22 7 10 23 16 35 35 0.000 0.000 0447 0 243 00:52:49.65 12.6000A -2.2589 1.9678 3.5851 0.099 1.43 -1.476900. 0.294E+00 0.293E+00 0.218E-03 0.282E-13 19 27 22 7 10 23 10 17 15 0.000 0.000 0448 0 244 00:53:02.05 12.4000A -2.0980 1.9365 3.6415 0.099 1.41 -1.429850. 0.294E+00 0.293E+00 0.215E-03 0.278E-13 19 27 22 7 10 23 11 18 17 0.000 0.000 0449 0 245 00:53:14.35 12.3000A 2.0541 1.9614 3.6444 0.099 1.41 -1.435850. 0.293E+00 0.292E+00 0.213E-03 0.276E-13 1 12 26 7 11 23 11 19 15 0.000 0.000 0450 0 246 00:53:26.55 12.2000A -1.9838 1.9415 3.6825 0.099 1.41 -1.442850. 0.293E+00 0.292E+00 0.212E-03 0.274E-13 18 25 8 7 11 23 12 19 15 0.000 0.000 0451 0 247 00:53:38.55 12.0000A 1.9982 1.8132 3.7485 0.099 1.41 -1.438850. 0.292E+00 0.291E+00 0.209E-03 0.270E-13 2 34 37 7 11 23 12 19 15 0.000 0.000 0452 0 248 00:53:50.55 12.0000A 1.9976 -1.7695 3.7382 0.099 1.41 -1.427850. 0.292E+00 0.290E+00 0.209E-03 0.271E-13 2 34 37 12 25 25 12 19 15 0.000 0.000 0453 0 249 00:54:02.65 12.1000A 1.9531 -1.8877 3.7181 0.099 1.41 -1.414850. 0.291E+00 0.290E+00 0.212E-03 0.273E-13 2 34 37 12 25 25 14 19 15 0.000 0.000 0454 0 250 00:54:15.05 12.4000A 1.9897 -1.8085 3.6162 0.099 1.41 -1.430850. 0.290E+00 0.289E+00 0.217E-03 0.280E-13 2 12 25 17 9 14 14 19 15 0.000 0.000 0455 0 251 00:54:27.55 12.5000A 2.0719 -1.8378 3.5940 0.099 1.41 -1.468850. 0.289E+00 0.288E+00 0.218E-03 0.282E-13 2 12 25 18 15 14 13 18 15 0.000 0.000 0456 0 252 00:54:39.95 12.4000A 2.0900 -1.8826 3.6288 0.099 1.41 -1.485850. 0.288E+00 0.287E+00 0.216E-03 0.280E-13 2 12 25 18 15 14 13 18 15 0.000 0.000 0457 0 253 00:54:52.45 12.5000A -2.1700 1.8954 3.6132 0.099 1.43 -1.456900. 0.287E+00 0.286E+00 0.218E-03 0.282E-13 19 37 32 6 6 25 14 18 15 0.000 0.000 0458 0 254 00:55:04.75 12.3000A -2.2313 1.9010 3.6714 0.099 1.43 -1.490900. 0.286E+00 0.285E+00 0.215E-03 0.278E-13 19 37 32 6 6 25 14 17 15 0.000 0.000 0459 0 255 00:55:17.25 12.5000A -2.1618 -1.9215 3.5906 0.099 1.43 -1.466900. 0.285E+00 0.284E+00 0.218E-03 0.282E-13 19 37 32 18 15 12 15 17 15 0.000 0.000 0460 0 256 00:55:29.75 12.5000A -2.1188 -2.0635 3.6038 0.099 1.43 -1.395900. 0.284E+00 0.282E+00 0.218E-03 0.282E-13 19 37 31 18 15 12 15 17 15 0.000 0.000 0461 0 257 00:55:42.25 12.5000A 2.1225 -2.0613 3.6075 0.099 1.43 -1.380900. 0.282E+00 0.281E+00 0.218E-03 0.282E-13 1 15 26 18 15 12 16 17 15 0.000 0.000 0462 0 258 00:55:54.75 12.5000A 2.2212 -2.0370 3.5998 0.099 1.43 -1.413900. 0.281E+00 0.279E+00 0.218E-03 0.281E-13 1 15 26 18 14 12 16 17 15 0.000 0.000 0463 0 259 00:56:07.75 13.0000A 2.2177 -2.1735 3.4537 0.099 1.43 -1.389900. 0.279E+00 0.278E+00 0.226E-03 0.292E-13 1 15 26 18 14 12 9 31 39 0.000 0.000 0464 0 260 00:56:20.75 13.0000A 2.1323 -2.1258 3.4580 0.099 1.43 -1.378900. 0.278E+00 0.276E+00 0.225E-03 0.291E-13 1 15 26 18 14 12 10 31 39 0.000 0.000 0465 0 261 00:56:33.35 12.6000A 1.9967 2.0399 3.5714 0.099 1.43 -1.369900. 0.276E+00 0.275E+00 0.218E-03 0.282E-13 1 15 26 1 13 24 10 31 39 0.000 0.000 0466 0 262 00:56:45.75 12.4000A -2.0360 2.0467 3.6366 0.099 1.43 -1.369900. 0.275E+00 0.274E+00 0.215E-03 0.277E-13 6 34 37 1 13 24 11 31 39 0.000 0.000 0467 0 263 00:56:58.15 12.4000A -1.9791 1.9729 3.6331 0.098 1.43 -1.377900. 0.274E+00 0.272E+00 0.214E-03 0.277E-13 19 37 29 1 13 24 11 31 39 0.000 0.000 0468 0 264 00:57:10.65 12.5000A -2.0077 -1.9707 3.6083 0.098 1.43 -1.394900. 0.272E+00 0.271E+00 0.216E-03 0.278E-13 17 19 17 18 4 34 12 31 39 0.000 0.000 0469 0 265 00:57:23.55 12.9000A -2.0128 -1.9940 3.5009 0.098 1.43 -1.406900. 0.271E+00 0.269E+00 0.223E-03 0.286E-13 17 19 17 6 11 29 13 31 39 0.000 0.000 0470 0 266 00:57:35.55 12.0000A -1.9421 -2.1178 3.7511 0.098 1.43 -1.421900. 0.270E+00 0.268E+00 0.208E-03 0.266E-13 17 19 17 6 11 29 13 31 39 0.000 0.000 0471 0 267 00:57:47.85 12.3000A -1.8740 -2.1095 3.6684 0.098 1.43 -1.452900. 0.269E+00 0.267E+00 0.213E-03 0.272E-13 5 11 35 6 11 29 13 31 39 0.000 0.000 0472 0 268 00:58:00.45 12.6000A -1.8624 2.0602 3.5713 0.097 1.43 -1.428900. 0.268E+00 0.266E+00 0.218E-03 0.278E-13 5 11 35 2 13 25 10 18 19 0.000 0.000 0473 0 269 00:58:12.35 11.9000A -1.8333 -2.1000 3.7701 0.097 1.43 -1.435900. 0.267E+00 0.265E+00 0.206E-03 0.262E-13 16 20 17 7 11 29 11 18 19 0.000 0.000 0474 0 270 00:58:24.25 11.9000A -1.8415 -2.0953 3.7739 0.097 1.43 -1.457900. 0.266E+00 0.264E+00 0.206E-03 0.262E-13 16 20 17 5 11 30 11 18 19 0.000 0.000 0475 0 271 00:58:36.05 11.8000A -1.8307 -2.1794 3.8107 0.097 1.40 -1.487850. 0.265E+00 0.264E+00 0.204E-03 0.260E-13 7 11 34 5 11 30 12 18 19 0.000 0.000 0476 0 272 00:58:48.05 12.0000A -1.8313 -2.2191 3.7376 0.097 1.40 -1.527850. 0.265E+00 0.263E+00 0.208E-03 0.264E-13 5 10 35 5 11 30 12 18 19 0.000 0.000 0477 0 273 00:58:59.75 11.7000A -1.9459 -2.2205 3.8314 0.097 1.40 -1.574850. 0.264E+00 0.262E+00 0.203E-03 0.258E-13 16 21 17 5 11 30 14 34 39 0.000 0.000 0478 0 274 00:59:11.85 12.1000A -2.0447 -2.2284 3.7215 0.097 1.40 -1.552850. 0.264E+00 0.262E+00 0.210E-03 0.267E-13 16 21 17 5 10 30 14 34 39 0.000 0.000 0479 0 275 00:59:24.15 12.3000A -2.0819 -2.2455 3.6602 0.096 1.40 -1.548850. 0.263E+00 0.261E+00 0.214E-03 0.272E-13 16 21 17 5 10 30 10 8 35 0.000 0.000 0480 0 276 00:59:36.45 12.3000A -2.0530 -2.2175 3.6709 0.096 1.43 -1.553900. 0.263E+00 0.261E+00 0.214E-03 0.272E-13 16 21 17 5 10 30 13 18 20 0.000 0.000 0481 0 277 00:59:48.65 12.2000A -2.0658 2.1702 3.6915 0.096 1.43 -1.547900. 0.262E+00 0.261E+00 0.213E-03 0.270E-13 16 21 16 1 9 28 13 18 20 0.000 0.000 0482 0 278 01:00:00.05 11.4000A -2.0744 2.2581 3.9420 0.096 1.43 -1.572900. 0.262E+00 0.260E+00 0.199E-03 0.252E-13 16 21 16 1 9 28 14 18 20 0.000 0.000 0202 RUN ITER. HH:MM:SS.SS DT(E) UMAX VMAX WMAX U* W* THETA* Z_I ENERG. DISTENERG DIVOLD DIVNEW UMAX(KJI) VMAX(KJI) WMAX(KJI) ADVECX ADVECY MGCYC 203 ----------------------------------------------------------------------------------------------------------------------------------------------------------------------------------------------------- 204 0 0 00:00:00.00 20.0000A -0.2192D -0.2169D -0.1214 0.000 1.38 0.000 800. 0.106E-02 0.106E-02 0.000E+00 0.000E+00 11 32 5 5 37 29 4 26 0 0.000 0.000 0 205 0 1 00:00:20.00 20.0000A -0.2192 -0.2169 -0.1214 0.001 0.79 ****** 150. 0.106E-02 0.106E-02 0.437E-05 0.287E-15 11 32 5 5 37 29 4 26 0 0.000 0.000 0 206 0 2 00:00:40.00 20.0000D -0.2170 -0.2168 -0.1216 0.001 0.79 ****** 150. 0.106E-02 0.106E-02 0.439E-05 0.295E-15 11 32 5 5 37 29 4 26 0 0.000 0.000 0 207 0 3 00:01:00.00 20.0000D -0.2146 -0.2174 -0.1218 0.001 0.79 ****** 150. 0.106E-02 0.106E-02 0.442E-05 0.301E-15 11 32 5 4 5 2 4 26 0 0.000 0.000 0 208 0 4 00:01:20.00 20.0000D -0.2119 -0.2192 -0.1220 0.001 1.29 ****** 650. 0.106E-02 0.106E-02 0.444E-05 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0.278E+00 0.180E-03 0.241E-13 3 38 18 1 22 27 15 23 6 0.000 0.000 0 307 0 103 00:23:47.85 11.5000A 1.7381 1.9490 3.9019 0.102 1.35 -1.324 750. 0.277E+00 0.277E+00 0.202E-03 0.271E-13 3 38 18 2 7 15 16 23 6 0.000 0.000 0 308 0 104 00:23:58.75 10.9000A -1.6589 2.0091 4.1429 0.103 1.35 -1.318 750. 0.277E+00 0.276E+00 0.192E-03 0.257E-13 1 27 23 1 7 14 16 23 6 0.000 0.000 0 309 0 105 00:24:10.55 11.8000A 1.7071 2.0640 3.8135 0.104 1.35 -1.323 750. 0.275E+00 0.275E+00 0.207E-03 0.277E-13 1 15 27 1 7 14 16 23 6 0.000 0.000 0 310 0 106 00:24:22.05 11.5000A 1.7476 2.0964 3.9100 0.105 1.35 -1.334 750. 0.274E+00 0.274E+00 0.202E-03 0.269E-13 1 15 27 1 7 14 15 36 27 0.000 0.000 0 311 0 107 00:24:33.45 11.4000A 1.7641 2.1010 3.9387 0.105 1.35 -1.329 750. 0.273E+00 0.273E+00 0.200E-03 0.267E-13 1 15 27 1 7 14 15 36 27 0.000 0.000 0 312 0 108 00:24:45.55 12.1000A 1.7574 2.0835 3.7283 0.106 1.35 -1.315 750. 0.272E+00 0.271E+00 0.212E-03 0.282E-13 1 15 27 1 7 14 9 12 1 0.000 0.000 0 313 0 109 00:24:57.15 11.6000A 1.7389 -2.1091 3.8696 0.107 1.35 -1.311 750. 0.270E+00 0.270E+00 0.203E-03 0.270E-13 3 36 19 1 22 29 16 36 27 0.000 0.000 0 314 0 110 00:25:08.45 11.3000A 1.7672 -2.2221 3.9936 0.107 1.35 -1.295 750. 0.269E+00 0.269E+00 0.198E-03 0.262E-13 3 36 19 1 22 29 10 12 1 0.000 0.000 0 315 0 111 00:25:19.95 11.5000A -1.7773 -2.3191 3.9018 0.108 1.35 -1.322 750. 0.267E+00 0.267E+00 0.201E-03 0.267E-13 1 37 20 1 22 29 10 12 1 0.000 0.000 0 316 0 112 00:25:31.45 11.5000A -1.7930 -2.3896 3.9135 0.108 1.35 -1.301 750. 0.266E+00 0.266E+00 0.201E-03 0.266E-13 1 37 20 1 22 29 11 12 1 0.000 0.000 0 317 0 113 00:25:42.55 11.1000A -1.7866 -2.4196 4.0363 0.109 1.35 -1.344 750. 0.264E+00 0.264E+00 0.194E-03 0.256E-13 1 37 20 1 22 29 11 12 1 0.000 0.000 0 318 0 114 00:25:55.05 12.5000A 1.7963 -2.4040 3.6053 0.109 1.35 -1.324 750. 0.263E+00 0.262E+00 0.218E-03 0.287E-13 2 33 15 1 22 29 11 12 1 0.000 0.000 0 319 0 115 00:26:06.45 11.4000A -1.8333 -2.3929 3.9399 0.110 1.38 -1.300 800. 0.261E+00 0.261E+00 0.199E-03 0.262E-13 1 12 21 1 21 29 11 32 24 0.000 0.000 0 320 0 116 00:26:17.95 11.5000A -1.8698 -2.4627 3.9033 0.110 1.38 -1.316 800. 0.260E+00 0.259E+00 0.200E-03 0.264E-13 1 12 21 1 21 29 11 32 24 0.000 0.000 0 321 0 117 00:26:30.35 12.4000A -1.8927 -2.4874 3.6369 0.111 1.38 -1.309 800. 0.258E+00 0.258E+00 0.215E-03 0.283E-13 1 12 21 1 21 29 11 31 25 0.000 0.000 0 322 0 118 00:26:42.15 11.8000A -1.8986 -2.4592 3.8114 0.111 1.32 -1.289 700. 0.257E+00 0.256E+00 0.204E-03 0.269E-13 1 12 21 1 21 29 12 32 24 0.000 0.000 0 323 0 119 00:26:53.75 11.6000A -1.8863 -2.3871 3.8812 0.112 1.38 -1.266 800. 0.255E+00 0.255E+00 0.200E-03 0.264E-13 1 12 21 1 21 29 12 32 24 0.000 0.000 0 324 0 120 00:27:06.05 12.3000A -1.8581 2.3788 3.6552 0.112 1.38 -1.261 800. 0.254E+00 0.253E+00 0.212E-03 0.279E-13 1 12 21 1 9 14 6 17 31 0.000 0.000 0 325 0 121 00:27:17.75 11.7000A 1.8904 2.3906 3.8390 0.113 1.38 -1.271 800. 0.252E+00 0.252E+00 0.202E-03 0.265E-13 1 18 21 1 9 14 7 17 31 0.000 0.000 0 326 0 122 00:27:29.15 11.4000A 1.9592 2.3621 3.9512 0.113 1.38 -1.324 800. 0.251E+00 0.250E+00 0.197E-03 0.258E-13 1 18 21 1 9 14 7 17 31 0.000 0.000 0 327 0 123 00:27:40.85 11.7000A 1.9816 2.3757 3.8623 0.113 1.38 -1.271 800. 0.249E+00 0.249E+00 0.201E-03 0.264E-13 1 18 21 1 10 14 8 17 31 0.000 0.000 0 328 0 124 00:27:51.65 10.8000A 1.9569 2.4083 4.1477 0.114 1.38 -1.261 800. 0.248E+00 0.248E+00 0.186E-03 0.244E-13 1 18 21 1 10 14 8 17 31 0.000 0.000 0 329 0 125 00:28:03.35 11.7000A 1.8962 2.4093 3.8427 0.114 1.38 -1.251 800. 0.246E+00 0.246E+00 0.201E-03 0.263E-13 1 18 21 1 10 14 8 17 31 0.000 0.000 0 330 0 126 00:28:14.55 11.2000A 2.0100 2.3683 4.0348 0.115 1.35 -1.277 750. 0.245E+00 0.244E+00 0.192E-03 0.251E-13 1 17 21 1 10 14 9 17 31 0.000 0.000 0 331 0 127 00:28:26.45 11.9000A 2.0906 2.2885 3.7964 0.115 1.35 -1.246 750. 0.243E+00 0.243E+00 0.202E-03 0.266E-13 1 17 21 1 10 14 9 17 31 0.000 0.000 0 332 0 128 00:28:38.55 12.1000A 2.0912 2.1695 3.7179 0.115 1.35 -1.228 750. 0.241E+00 0.241E+00 0.205E-03 0.270E-13 1 17 21 1 10 14 10 17 31 0.000 0.000 0 333 0 129 00:28:51.25 12.7000A 2.0014 2.2106 3.5318 0.115 1.35 -1.221 750. 0.239E+00 0.239E+00 0.214E-03 0.282E-13 1 17 21 1 12 13 10 17 31 0.000 0.000 0 334 0 130 00:29:04.95 13.7000A 1.9390 2.2557 3.2948 0.116 1.38 -1.212 800. 0.237E+00 0.237E+00 0.229E-03 0.302E-13 1 20 22 1 12 13 15 31 24 0.000 0.000 0 335 0 131 00:29:18.55 13.6000A 1.9902 2.2448 3.3144 0.116 1.41 -1.192 850. 0.235E+00 0.235E+00 0.226E-03 0.298E-13 1 20 22 1 12 13 15 31 24 0.000 0.000 0 336 0 132 00:29:33.05 14.5000A 2.0400 2.1833 3.1107 0.116 1.35 -1.200 750. 0.232E+00 0.232E+00 0.239E-03 0.315E-13 1 20 22 1 12 13 12 22 13 0.000 0.000 0 337 0 133 00:29:47.05 14.0000A 2.0818 2.2418 3.2104 0.115 1.35 -1.279 750. 0.230E+00 0.230E+00 0.230E-03 0.303E-13 1 20 22 1 8 16 16 31 24 0.000 0.000 0 338 0 134 00:30:01.75 14.7000A 2.1591 2.3083 3.0512 0.115 1.35 -1.240 750. 0.228E+00 0.227E+00 0.239E-03 0.315E-13 1 19 22 1 8 16 4 13 17 0.000 0.000 0 339 0 135 00:30:16.45 14.7000A 2.2191 2.2636 3.0590 0.115 1.35 -1.210 750. 0.225E+00 0.225E+00 0.238E-03 0.312E-13 1 19 22 1 8 16 13 22 13 0.000 0.000 0 340 0 136 00:30:31.25 14.8000A 2.2333 2.1717 3.0444 0.115 1.35 -1.222 750. 0.223E+00 0.223E+00 0.237E-03 0.312E-13 1 19 22 1 9 16 5 13 17 0.000 0.000 0 341 0 137 00:30:44.75 13.5000A 2.2022 2.1157 3.3321 0.114 1.41 -1.211 850. 0.221E+00 0.221E+00 0.215E-03 0.282E-13 1 19 22 1 9 16 10 12 34 0.000 0.000 0 342 0 138 00:30:57.95 13.2000A 2.1843 2.1377 3.4048 0.114 1.41 -1.209 850. 0.219E+00 0.219E+00 0.209E-03 0.273E-13 1 19 23 1 14 12 10 12 34 0.000 0.000 0 343 0 139 00:31:11.35 13.4000A 2.2430 2.2057 3.3692 0.113 1.41 -1.234 850. 0.217E+00 0.217E+00 0.210E-03 0.274E-13 1 19 23 1 14 12 11 12 34 0.000 0.000 0 344 0 140 00:31:24.65 13.3000A 2.2595 2.2050 3.3818 0.113 1.38 -1.262 800. 0.216E+00 0.215E+00 0.207E-03 0.269E-13 1 19 23 1 14 12 11 12 34 0.000 0.000 0 345 0 141 00:31:38.15 13.5000A 2.2351 2.1414 3.3251 0.112 1.38 -1.359 800. 0.214E+00 0.213E+00 0.207E-03 0.270E-13 1 19 23 1 14 12 12 11 19 0.000 0.000 0 346 0 142 00:31:51.75 13.6000A 2.1849 2.0937 3.3170 0.111 1.38 -1.246 800. 0.212E+00 0.212E+00 0.206E-03 0.268E-13 1 19 23 2 13 13 12 11 19 0.000 0.000 0 347 0 143 00:32:05.85 14.1000A 2.1665 2.0911 3.1984 0.110 1.38 -1.277 800. 0.211E+00 0.210E+00 0.212E-03 0.274E-13 1 19 24 1 12 12 13 11 19 0.000 0.000 0 348 0 144 00:32:19.35 13.5000A 2.2330 2.1961 3.3346 0.109 1.38 -1.268 800. 0.209E+00 0.209E+00 0.201E-03 0.259E-13 1 19 24 2 14 13 13 11 19 0.000 0.000 0 349 0 145 00:32:33.05 13.7000A 2.2358 2.2598 3.2746 0.109 1.38 -1.293 800. 0.208E+00 0.207E+00 0.202E-03 0.260E-13 1 19 24 2 14 13 14 12 21 0.000 0.000 0 350 0 146 00:32:47.05 14.0000A 2.1896 2.3099 3.2130 0.108 1.38 -1.292 800. 0.207E+00 0.206E+00 0.205E-03 0.263E-13 1 19 24 1 13 12 14 11 19 0.000 0.000 0 351 0 147 00:33:01.35 14.3000A 2.1024 2.3477 3.1369 0.107 1.38 -1.310 800. 0.205E+00 0.205E+00 0.208E-03 0.267E-13 1 19 24 1 13 12 15 12 21 0.000 0.000 0 352 0 148 00:33:16.25 14.9000A 1.9940 2.3109 3.0124 0.106 1.38 -1.321 800. 0.204E+00 0.204E+00 0.215E-03 0.276E-13 1 19 24 1 13 12 15 11 19 0.000 0.000 0 353 0 149 00:33:30.85 14.6000A 2.0083 2.2570 3.0910 0.105 1.38 -1.327 800. 0.204E+00 0.203E+00 0.209E-03 0.268E-13 1 17 24 1 13 13 16 12 21 0.000 0.000 0 354 0 150 00:33:46.25 15.4000A 2.0296 2.2387 2.9235 0.105 1.38 -1.371 800. 0.203E+00 0.202E+00 0.219E-03 0.281E-13 1 17 24 1 13 13 5 29 18 0.000 0.000 0 355 0 151 00:34:00.95 14.7000A 1.9808 2.2175 3.0615 0.104 1.38 -1.383 800. 0.202E+00 0.202E+00 0.208E-03 0.267E-13 1 17 24 1 14 13 6 29 18 0.000 0.000 0 356 0 152 00:34:15.15 14.2000A -1.9396 2.3781 3.1723 0.104 1.38 -1.361 800. 0.202E+00 0.201E+00 0.200E-03 0.257E-13 1 39 5 1 14 13 8 28 17 0.000 0.000 0 357 0 153 00:34:28.55 13.4000A 2.0675 2.4704 3.3549 0.103 1.38 -1.363 800. 0.202E+00 0.201E+00 0.189E-03 0.242E-13 1 17 25 1 14 13 9 28 17 0.000 0.000 0 358 0 154 00:34:41.35 12.8000A -2.1421 2.4901 3.5091 0.103 1.38 -1.394 800. 0.202E+00 0.201E+00 0.180E-03 0.230E-13 1 39 4 1 14 13 9 28 17 0.000 0.000 0 359 0 155 00:34:53.85 12.5000A -2.1948 2.4409 3.5981 0.102 1.38 -1.476 800. 0.202E+00 0.201E+00 0.176E-03 0.225E-13 1 39 4 1 14 13 10 28 17 0.000 0.000 0 360 0 156 00:35:06.25 12.4000A -2.2082 2.3277 3.6269 0.102 1.38 -1.437 800. 0.202E+00 0.201E+00 0.174E-03 0.222E-13 1 39 4 1 14 13 10 28 17 0.000 0.000 0 361 0 157 00:35:18.45 12.2000A -2.1825 2.3456 3.6988 0.102 1.38 -1.430 800. 0.202E+00 0.201E+00 0.172E-03 0.218E-13 1 39 4 1 15 13 11 28 17 0.000 0.000 0 362 0 158 00:35:30.25 11.8000A -2.1227 2.4465 3.8015 0.101 1.38 -1.429 800. 0.202E+00 0.202E+00 0.166E-03 0.211E-13 1 39 4 1 15 13 12 28 17 0.000 0.000 0 363 0 159 00:35:42.05 11.8000A -2.0764 2.4870 3.8084 0.101 1.38 -1.436 800. 0.203E+00 0.202E+00 0.166E-03 0.211E-13 1 39 3 1 15 13 13 28 17 0.000 0.000 0 364 0 160 00:35:53.35 11.3000A -2.1034 2.4705 3.9746 0.101 1.38 -1.445 800. 0.203E+00 0.202E+00 0.159E-03 0.201E-13 1 39 3 1 15 13 13 28 17 0.000 0.000 0 365 0 161 00:36:04.85 11.5000A -2.0989 2.4038 3.9139 0.101 1.38 -1.433 800. 0.203E+00 0.203E+00 0.162E-03 0.205E-13 1 39 3 1 15 13 14 28 17 0.000 0.000 0 366 0 162 00:36:16.15 11.3000A -2.0703 2.2906 3.9650 0.100 1.38 -1.390 800. 0.204E+00 0.203E+00 0.159E-03 0.201E-13 1 38 3 1 15 13 14 28 17 0.000 0.000 0 367 0 163 00:36:27.75 11.6000A -2.0480 2.1660 3.8904 0.100 1.38 -1.357 800. 0.205E+00 0.204E+00 0.163E-03 0.206E-13 1 38 3 2 16 13 15 28 17 0.000 0.000 0 368 0 164 00:36:39.35 11.6000A -2.1133 2.1887 3.8849 0.100 1.38 -1.347 800. 0.205E+00 0.204E+00 0.164E-03 0.207E-13 1 36 1 2 16 13 15 28 17 0.000 0.000 0 369 0 165 00:36:51.55 12.2000A -2.1418 2.1803 3.6824 0.100 1.38 -1.337 800. 0.206E+00 0.205E+00 0.172E-03 0.217E-13 1 36 1 2 16 13 15 29 17 0.000 0.000 0 370 0 166 00:37:04.25 12.7000A -2.1389 2.1311 3.5539 0.100 1.41 -1.324 850. 0.207E+00 0.206E+00 0.179E-03 0.227E-13 1 36 0 2 16 13 14 27 16 0.000 0.000 0 371 0 167 00:37:16.25 12.0000A -2.2340 -2.1121 3.7401 0.100 1.41 -1.331 850. 0.207E+00 0.207E+00 0.170E-03 0.215E-13 1 36 0 1 33 14 16 29 17 0.000 0.000 0 372 0 168 00:37:28.45 12.2000A -2.2833 -2.1292 3.6824 0.100 1.41 -1.384 850. 0.208E+00 0.208E+00 0.173E-03 0.218E-13 1 36 0 1 33 14 15 27 16 0.000 0.000 0 373 0 169 00:37:40.55 12.1000A -2.2947 -2.1121 3.7140 0.100 1.41 -1.353 850. 0.209E+00 0.208E+00 0.171E-03 0.216E-13 1 36 0 1 33 14 16 27 16 0.000 0.000 0 374 0 170 00:37:52.85 12.3000A -2.2741 -2.0710 3.6688 0.100 1.41 -1.364 850. 0.210E+00 0.209E+00 0.174E-03 0.220E-13 1 36 0 1 33 14 16 27 16 0.000 0.000 0 375 0 171 00:38:05.65 12.8000A -2.2272 -2.0980 3.5117 0.100 1.43 -1.378 900. 0.211E+00 0.210E+00 0.181E-03 0.229E-13 1 36 0 1 32 16 17 27 16 0.000 0.000 0 376 0 172 00:38:18.75 13.1000A -2.1531 -2.1396 3.4286 0.100 1.43 -1.432 900. 0.212E+00 0.211E+00 0.186E-03 0.235E-13 1 36 0 1 32 17 17 27 16 0.000 0.000 0 377 0 173 00:38:31.35 12.6000A -2.1886 -2.1599 3.5630 0.100 1.43 -1.399 900. 0.213E+00 0.212E+00 0.179E-03 0.226E-13 1 35 39 1 32 15 16 29 18 0.000 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16 6 19 12 0.000 0.000 0 391 0 187 00:41:38.65 13.4000A -2.2166 -2.1463 3.3697 0.102 1.41 -1.448 850. 0.237E+00 0.236E+00 0.202E-03 0.257E-13 1 33 39 1 29 16 10 24 19 0.000 0.000 0 392 0 188 00:41:51.95 13.3000A -2.2932 -2.1146 3.3771 0.102 1.41 -1.747 850. 0.239E+00 0.238E+00 0.201E-03 0.257E-13 1 33 38 1 29 16 12 23 19 0.000 0.000 0 393 0 189 00:42:05.05 13.1000A -2.2620 -2.0345 3.4445 0.102 1.41 -1.442 850. 0.241E+00 0.240E+00 0.199E-03 0.255E-13 1 33 38 1 29 16 12 23 19 0.000 0.000 0 394 0 190 00:42:17.35 12.3000A -2.1635 -2.0145 3.6599 0.102 1.41 -1.421 850. 0.243E+00 0.242E+00 0.188E-03 0.242E-13 1 33 37 1 28 16 13 23 19 0.000 0.000 0 395 0 191 00:42:30.25 12.9000A -2.2627 -2.0551 3.4893 0.102 1.41 -1.415 850. 0.245E+00 0.244E+00 0.198E-03 0.255E-13 1 33 37 1 28 16 13 23 19 0.000 0.000 0 396 0 192 00:42:42.75 12.5000A -2.2475 -2.0437 3.5914 0.102 1.41 -1.393 850. 0.247E+00 0.246E+00 0.193E-03 0.250E-13 1 33 37 1 28 16 14 23 19 0.000 0.000 0 397 0 193 00:42:54.65 11.9000A -2.1510 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10.6000A -2.2984 1.9886 4.2486 0.102 1.41 -1.354 850. 0.295E+00 0.294E+00 0.187E-03 0.241E-13 13 33 31 9 11 24 12 36 36 0.000 0.000 0 430 0 226 00:49:33.25 10.7000A -2.1881 -1.9134 4.1931 0.102 1.41 -1.366 850. 0.295E+00 0.294E+00 0.189E-03 0.243E-13 13 33 30 17 12 16 12 36 36 0.000 0.000 0 431 0 227 00:49:43.95 10.7000A -2.1459 -1.8974 4.1883 0.102 1.41 -1.415 850. 0.296E+00 0.294E+00 0.189E-03 0.243E-13 13 33 30 17 12 16 13 36 36 0.000 0.000 0 432 0 228 00:49:55.25 11.3000A -2.1716 1.9677 3.9908 0.102 1.41 -1.485 850. 0.296E+00 0.295E+00 0.199E-03 0.256E-13 13 33 33 10 11 24 13 36 36 0.000 0.000 0 433 0 229 00:50:05.95 10.7000A -2.0255 1.9272 4.2063 0.102 1.41 -1.460 850. 0.296E+00 0.295E+00 0.189E-03 0.242E-13 13 33 33 10 11 24 14 36 36 0.000 0.000 0 434 0 230 00:50:17.25 11.3000A -2.1013 2.0264 3.9819 0.101 1.41 -1.422 850. 0.296E+00 0.295E+00 0.199E-03 0.255E-13 14 34 33 12 25 11 14 36 36 0.000 0.000 0 435 0 231 00:50:28.45 11.2000A -2.2268 2.0277 4.0155 0.101 1.41 -1.397 850. 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3.6415 0.099 1.41 -1.429 850. 0.294E+00 0.293E+00 0.215E-03 0.278E-13 19 27 22 7 10 23 11 18 17 0.000 0.000 0 449 0 245 00:53:14.35 12.3000A 2.0541 1.9614 3.6444 0.099 1.41 -1.435 850. 0.293E+00 0.292E+00 0.213E-03 0.276E-13 1 12 26 7 11 23 11 19 15 0.000 0.000 0 450 0 246 00:53:26.55 12.2000A -1.9838 1.9415 3.6825 0.099 1.41 -1.442 850. 0.293E+00 0.292E+00 0.212E-03 0.274E-13 18 25 8 7 11 23 12 19 15 0.000 0.000 0 451 0 247 00:53:38.55 12.0000A 1.9982 1.8132 3.7485 0.099 1.41 -1.438 850. 0.292E+00 0.291E+00 0.209E-03 0.270E-13 2 34 37 7 11 23 12 19 15 0.000 0.000 0 452 0 248 00:53:50.55 12.0000A 1.9976 -1.7695 3.7382 0.099 1.41 -1.427 850. 0.292E+00 0.290E+00 0.209E-03 0.271E-13 2 34 37 12 25 25 12 19 15 0.000 0.000 0 453 0 249 00:54:02.65 12.1000A 1.9531 -1.8877 3.7181 0.099 1.41 -1.414 850. 0.291E+00 0.290E+00 0.212E-03 0.273E-13 2 34 37 12 25 25 14 19 15 0.000 0.000 0 454 0 250 00:54:15.05 12.4000A 1.9897 -1.8085 3.6162 0.099 1.41 -1.430 850. 0.290E+00 0.289E+00 0.217E-03 0.280E-13 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12.5000A 2.1225 -2.0613 3.6075 0.099 1.43 -1.380 900. 0.282E+00 0.281E+00 0.218E-03 0.282E-13 1 15 26 18 15 12 16 17 15 0.000 0.000 0 462 0 258 00:55:54.75 12.5000A 2.2212 -2.0370 3.5998 0.099 1.43 -1.413 900. 0.281E+00 0.279E+00 0.218E-03 0.281E-13 1 15 26 18 14 12 16 17 15 0.000 0.000 0 463 0 259 00:56:07.75 13.0000A 2.2177 -2.1735 3.4537 0.099 1.43 -1.389 900. 0.279E+00 0.278E+00 0.226E-03 0.292E-13 1 15 26 18 14 12 9 31 39 0.000 0.000 0 464 0 260 00:56:20.75 13.0000A 2.1323 -2.1258 3.4580 0.099 1.43 -1.378 900. 0.278E+00 0.276E+00 0.225E-03 0.291E-13 1 15 26 18 14 12 10 31 39 0.000 0.000 0 465 0 261 00:56:33.35 12.6000A 1.9967 2.0399 3.5714 0.099 1.43 -1.369 900. 0.276E+00 0.275E+00 0.218E-03 0.282E-13 1 15 26 1 13 24 10 31 39 0.000 0.000 0 466 0 262 00:56:45.75 12.4000A -2.0360 2.0467 3.6366 0.099 1.43 -1.369 900. 0.275E+00 0.274E+00 0.215E-03 0.277E-13 6 34 37 1 13 24 11 31 39 0.000 0.000 0 467 0 263 00:56:58.15 12.4000A -1.9791 1.9729 3.6331 0.098 1.43 -1.377 900. 0.274E+00 0.272E+00 0.214E-03 0.277E-13 19 37 29 1 13 24 11 31 39 0.000 0.000 0 468 0 264 00:57:10.65 12.5000A -2.0077 -1.9707 3.6083 0.098 1.43 -1.394 900. 0.272E+00 0.271E+00 0.216E-03 0.278E-13 17 19 17 18 4 34 12 31 39 0.000 0.000 0 469 0 265 00:57:23.55 12.9000A -2.0128 -1.9940 3.5009 0.098 1.43 -1.406 900. 0.271E+00 0.269E+00 0.223E-03 0.286E-13 17 19 17 6 11 29 13 31 39 0.000 0.000 0 470 0 266 00:57:35.55 12.0000A -1.9421 -2.1178 3.7511 0.098 1.43 -1.421 900. 0.270E+00 0.268E+00 0.208E-03 0.266E-13 17 19 17 6 11 29 13 31 39 0.000 0.000 0 471 0 267 00:57:47.85 12.3000A -1.8740 -2.1095 3.6684 0.098 1.43 -1.452 900. 0.269E+00 0.267E+00 0.213E-03 0.272E-13 5 11 35 6 11 29 13 31 39 0.000 0.000 0 472 0 268 00:58:00.45 12.6000A -1.8624 2.0602 3.5713 0.097 1.43 -1.428 900. 0.268E+00 0.266E+00 0.218E-03 0.278E-13 5 11 35 2 13 25 10 18 19 0.000 0.000 0 473 0 269 00:58:12.35 11.9000A -1.8333 -2.1000 3.7701 0.097 1.43 -1.435 900. 0.267E+00 0.265E+00 0.206E-03 0.262E-13 16 20 17 7 11 29 11 18 19 0.000 0.000 0 474 0 270 00:58:24.25 11.9000A -1.8415 -2.0953 3.7739 0.097 1.43 -1.457 900. 0.266E+00 0.264E+00 0.206E-03 0.262E-13 16 20 17 5 11 30 11 18 19 0.000 0.000 0 475 0 271 00:58:36.05 11.8000A -1.8307 -2.1794 3.8107 0.097 1.40 -1.487 850. 0.265E+00 0.264E+00 0.204E-03 0.260E-13 7 11 34 5 11 30 12 18 19 0.000 0.000 0 476 0 272 00:58:48.05 12.0000A -1.8313 -2.2191 3.7376 0.097 1.40 -1.527 850. 0.265E+00 0.263E+00 0.208E-03 0.264E-13 5 10 35 5 11 30 12 18 19 0.000 0.000 0 477 0 273 00:58:59.75 11.7000A -1.9459 -2.2205 3.8314 0.097 1.40 -1.574 850. 0.264E+00 0.262E+00 0.203E-03 0.258E-13 16 21 17 5 11 30 14 34 39 0.000 0.000 0 478 0 274 00:59:11.85 12.1000A -2.0447 -2.2284 3.7215 0.097 1.40 -1.552 850. 0.264E+00 0.262E+00 0.210E-03 0.267E-13 16 21 17 5 10 30 14 34 39 0.000 0.000 0 479 0 275 00:59:24.15 12.3000A -2.0819 -2.2455 3.6602 0.096 1.40 -1.548 850. 0.263E+00 0.261E+00 0.214E-03 0.272E-13 16 21 17 5 10 30 10 8 35 0.000 0.000 0 480 0 276 00:59:36.45 12.3000A -2.0530 -2.2175 3.6709 0.096 1.43 -1.553 900. 0.263E+00 0.261E+00 0.214E-03 0.272E-13 16 21 17 5 10 30 13 18 20 0.000 0.000 0 481 0 277 00:59:48.65 12.2000A -2.0658 2.1702 3.6915 0.096 1.43 -1.547 900. 0.262E+00 0.261E+00 0.213E-03 0.270E-13 16 21 16 1 9 28 13 18 20 0.000 0.000 0 482 0 278 01:00:00.05 11.4000A -2.0744 2.2581 3.9420 0.096 1.43 -1.572 900. 0.262E+00 0.260E+00 0.199E-03 0.252E-13 16 21 16 1 9 28 14 18 20 0.000 0.000 0 -
palm/trunk/SCRIPTS/mrun
r83 r97 119 119 # config file, code related to ftp filetransfer 120 120 # removed (incl. option -f) 121 # 19/06/07 - Siggi - time limit for cdata jobs increased 121 122 122 123 … … 3176 3177 if [[ $localhost = ibmh || $localhost = ibmb ]] 3177 3178 then 3178 subjob -d -v -q cdata -X 0 -m 1000 -t 7200 archive_${frelout[$i]} 3179 # subjob -d -v -q cdata -X 0 -m 1000 -t 43200 archive_${frelout[$i]} 3180 subjob -v -q cdata -X 0 -m 1000 -t 43200 archive_${frelout[$i]} 3179 3181 elif [[ $localhost = nech ]] 3180 3182 then … … 3300 3302 fi 3301 3303 3302 subjob -v -d -q cdata -X 0 -m 1000 -t 7200 archive_${frelout[$i]}3304 subjob -v -d -q cdata -X 0 -m 1000 -t 43200 archive_${frelout[$i]} 3303 3305 printf " Archiving of $tmp_data_catalog/${frelout[$i]} initiated (batch job submitted)\n" 3304 3306 file_saved=true -
palm/trunk/SOURCE/CURRENT_MODIFICATIONS
r96 r97 1 1 New: 2 2 --- 3 ocean version including prognostic equation for salinity and equation of state for seawater4 + inipar-parameters bc_sa_t, bottom_salinityflux, ocean, sa_surface, sa_vertical_gradient, sa_vertical_gradient_level, top_salinityflux5 3 6 average_3d_data, boundary_conds, buoyancy, check_parameters, data_output_2d, data_output_3d, diffusion_e, flow_statistics, header, init_grid, init_3d_model, modules, parin, prognostic_equations, read_var_list, sum_up_3d_data, swap_timelevel, time_integration, user_interface, write_var_list, write_3d_binary7 8 New:9 eqn_state_seawater, init_ocean10 4 11 5 Changed: 12 6 ------- 13 hydro_press renamed hyp, routine calc_mean_pt_profile renamed calc_mean_profile14 15 advec_particles, buoyancy, calc_liquid_water_content, init_cloud_physics, modules, prognostic_equations16 7 17 8 … … 19 10 ------ 20 11 21 Bugfix: height above topography instead of height above level k=0 is used for calculating the mixing length (diffusion_e and diffusivities).22 12 23 diffusion_e, prognostic_equations24 25 26 27 28 To be completed (adjusted to ocean version):29 ----------------30 31 boundary conditions for salinity (check_parameters)32 output of salinity profile (header)33 34 initialization of ug,vg profiles35 36 calculation of w*37 output of theta* and z_i (e.g. run_control file)38 39 default disturbance level40 41 Bott-Chlond scheme to be extended for salinity42 43 Upstream-spline scheme to be extended for salinity????? -
palm/trunk/SOURCE/advec_s_bc.f90
r77 r97 4 4 ! Actual revisions: 5 5 ! ----------------- 6 ! 6 ! Advection of salinity included 7 ! Bugfix: Error in boundary condition for TKE removed 7 8 ! 8 9 ! Former revisions: … … 755 756 ENDIF 756 757 758 ELSEIF ( sk_char == 'sa' ) THEN 759 760 ! 761 !-- Salinity boundary condition at the bottom boundary. 762 !-- So far, always Neumann (i.e. here zero gradient) is used 763 DO i = nxl, nxr 764 DO j = nys, nyn 765 sk_p(nzb-1,j,i) = sk_p(nzb,j,i) 766 sk_p(nzb-2,j,i) = sk_p(nzb,j,i) 767 ENDDO 768 ENDDO 769 770 ! 771 !-- Salinity boundary condition at the top boundary. 772 !-- Dirichlet or Neumann (zero gradient) 773 DO i = nxl, nxr 774 DO j = nys, nyn 775 sk_p(nzt+2,j,i) = sk_p(nzt+1,j,i) 776 sk_p(nzt+3,j,i) = sk_p(nzt+1,j,i) 777 ENDDO 778 ENDDO 779 757 780 ELSEIF ( sk_char == 'q' ) THEN 758 781 759 782 ! 760 !-- Specific humidity boundary condition at the bottom boundary 761 IF ( ibc_q_b == 0 ) THEN 762 ! 763 !-- Dirichlet (fixed surface humidity) 764 DO i = nxl, nxr 765 DO j = nys, nyn 766 sk_p(nzb-1,j,i) = sk_p(nzb,j,i) 767 sk_p(nzb-2,j,i) = sk_p(nzb,j,i) 768 ENDDO 769 ENDDO 770 771 ELSE 772 ! 773 !-- Neumann (i.e. here zero gradient) 774 DO i = nxl, nxr 775 DO j = nys, nyn 776 sk_p(nzb-1,j,i) = sk_p(nzb,j,i) 777 sk_p(nzb-2,j,i) = sk_p(nzb,j,i) 778 ENDDO 779 ENDDO 780 781 ENDIF 783 !-- Specific humidity boundary condition at the bottom boundary. 784 !-- Dirichlet (fixed surface humidity) or Neumann (i.e. zero gradient) 785 DO i = nxl, nxr 786 DO j = nys, nyn 787 sk_p(nzb-1,j,i) = sk_p(nzb,j,i) 788 sk_p(nzb-2,j,i) = sk_p(nzb,j,i) 789 ENDDO 790 ENDDO 782 791 783 792 ! … … 809 818 ! 810 819 !-- TKE boundary condition at bottom and top boundary (generally Neumann) 811 sk_p(nzb-1,j,i) = sk_p(nzb,j,i) 812 sk_p(nzb-2,j,i) = sk_p(nzb,j,i) 813 sk_p(nzt+2,j,i) = sk_p(nzt+1,j,i) 814 sk_p(nzt+3,j,i) = sk_p(nzt+1,j,i) 820 DO i = nxl, nxr 821 DO j = nys, nyn 822 sk_p(nzb-1,j,i) = sk_p(nzb,j,i) 823 sk_p(nzb-2,j,i) = sk_p(nzb,j,i) 824 sk_p(nzt+2,j,i) = sk_p(nzt+1,j,i) 825 sk_p(nzt+3,j,i) = sk_p(nzt+1,j,i) 826 ENDDO 827 ENDDO 815 828 816 829 ELSE -
palm/trunk/SOURCE/buoyancy.f90
r96 r97 4 4 ! Actual revisions: 5 5 ! ----------------- 6 ! Routine reneralized to be used with temperature AND density: 7 ! argument theta renamed var, new argument var_reference, 8 ! use_pt_reference renamed use_reference, 6 9 ! calc_mean_pt_profile renamed calc_mean_profile 7 10 ! … … 46 49 ! Call for all grid points 47 50 !------------------------------------------------------------------------------! 48 SUBROUTINE buoyancy( theta, wind_component, pr )51 SUBROUTINE buoyancy( var, var_reference, wind_component, pr ) 49 52 50 53 USE arrays_3d … … 57 60 58 61 INTEGER :: i, j, k, pr, wind_component 59 REAL, DIMENSION(:,:,:), POINTER :: theta 62 REAL :: var_reference 63 REAL, DIMENSION(:,:,:), POINTER :: var 60 64 61 65 … … 63 67 ! 64 68 !-- Normal case: horizontal surface 65 IF ( use_pt_reference ) THEN 66 DO i = nxl, nxr 67 DO j = nys, nyn 68 DO k = nzb_s_inner(j,i)+1, nzt-1 69 tend(k,j,i) = tend(k,j,i) + g * 0.5 * ( & 70 ( theta(k,j,i) - hom(k,1,pr,0) ) / pt_reference + & 71 ( theta(k+1,j,i) - hom(k+1,1,pr,0) ) / pt_reference & 69 IF ( use_reference ) THEN 70 DO i = nxl, nxr 71 DO j = nys, nyn 72 DO k = nzb_s_inner(j,i)+1, nzt-1 73 tend(k,j,i) = tend(k,j,i) + atmos_ocean_sign * g * 0.5 * & 74 ( & 75 ( var(k,j,i) - hom(k,1,pr,0) ) / var_reference + & 76 ( var(k+1,j,i) - hom(k+1,1,pr,0) ) / var_reference & 72 77 ) 73 78 ENDDO … … 78 83 DO j = nys, nyn 79 84 DO k = nzb_s_inner(j,i)+1, nzt-1 80 tend(k,j,i) = tend(k,j,i) + g * 0.5 * ( & 81 ( theta(k,j,i) - hom(k,1,pr,0) ) / hom(k,1,pr,0) + & 82 ( theta(k+1,j,i) - hom(k+1,1,pr,0) ) / hom(k+1,1,pr,0) & 85 tend(k,j,i) = tend(k,j,i) + atmos_ocean_sign * g * 0.5 * & 86 ( & 87 ( var(k,j,i) - hom(k,1,pr,0) ) / hom(k,1,pr,0) + & 88 ( var(k+1,j,i) - hom(k+1,1,pr,0) ) / hom(k+1,1,pr,0) & 83 89 ) 84 90 ENDDO … … 136 142 ! Call for grid point i,j 137 143 !------------------------------------------------------------------------------! 138 SUBROUTINE buoyancy_ij( i, j, theta, wind_component, pr )144 SUBROUTINE buoyancy_ij( i, j, var, var_reference, wind_component, pr ) 139 145 140 146 USE arrays_3d … … 147 153 148 154 INTEGER :: i, j, k, pr, wind_component 149 REAL, DIMENSION(:,:,:), POINTER :: theta 155 REAL :: var_reference 156 REAL, DIMENSION(:,:,:), POINTER :: var 150 157 151 158 … … 153 160 ! 154 161 !-- Normal case: horizontal surface 155 IF ( use_ pt_reference ) THEN156 DO k = nzb_s_inner(j,i)+1, nzt-1 157 tend(k,j,i) = tend(k,j,i) + g * 0.5 * (&158 ( theta(k,j,i) - hom(k,1,pr,0) ) / pt_reference + &159 ( theta(k+1,j,i) - hom(k+1,1,pr,0) ) / pt_reference &160 )161 ENDDO 162 ELSE 163 DO k = nzb_s_inner(j,i)+1, nzt-1 164 tend(k,j,i) = tend(k,j,i) + g * 0.5 * (&165 ( theta(k,j,i) - hom(k,1,pr,0) ) / hom(k,1,pr,0) + &166 ( theta(k+1,j,i) - hom(k+1,1,pr,0) ) / hom(k+1,1,pr,0) &167 )162 IF ( use_reference ) THEN 163 DO k = nzb_s_inner(j,i)+1, nzt-1 164 tend(k,j,i) = tend(k,j,i) + atmos_ocean_sign * g * 0.5 * ( & 165 ( var(k,j,i) - hom(k,1,pr,0) ) / var_reference + & 166 ( var(k+1,j,i) - hom(k+1,1,pr,0) ) / var_reference & 167 ) 168 ENDDO 169 ELSE 170 DO k = nzb_s_inner(j,i)+1, nzt-1 171 tend(k,j,i) = tend(k,j,i) + atmos_ocean_sign * g * 0.5 * ( & 172 ( var(k,j,i) - hom(k,1,pr,0) ) / hom(k,1,pr,0) + & 173 ( var(k+1,j,i) - hom(k+1,1,pr,0) ) / hom(k+1,1,pr,0) & 174 ) 168 175 ENDDO 169 176 ENDIF -
palm/trunk/SOURCE/check_parameters.f90
r96 r97 4 4 ! Actual revisions: 5 5 ! ----------------- 6 ! Initial salinity profile is calculated. 6 ! Initial salinity profile is calculated, salinity boundary conditions are 7 ! checked, 7 8 ! z_max_do1d is checked only in case of ocean = .f., 8 ! +initial temperature profile for the ocean version, 9 ! +initial temperature and geostrophic velocity profiles for the ocean version, 10 ! use_pt_reference renamed use_reference 9 11 ! 10 12 ! Former revisions: … … 163 165 WRITE( action, '(A,A)' ) 'timestep_scheme = ', timestep_scheme 164 166 ENDIF 167 IF ( momentum_advec == 'ups-scheme' ) THEN 168 WRITE( action, '(A,A)' ) 'momentum_advec = ', momentum_advec 169 ENDIF 165 170 IF ( action /= ' ' ) THEN 166 171 IF ( myid == 0 ) THEN … … 447 452 i = 1 448 453 gradient = 0.0 449 ug_vertical_gradient_level_ind(1) = 0 450 ug(0) = ug_surface 451 DO k = 1, nzt+1 452 IF ( ug_vertical_gradient_level(i) < zu(k) .AND. & 453 ug_vertical_gradient_level(i) >= 0.0 ) THEN 454 gradient = ug_vertical_gradient(i) / 100.0 455 ug_vertical_gradient_level_ind(i) = k - 1 456 i = i + 1 457 IF ( i > 10 ) THEN 458 IF ( myid == 0 ) THEN 459 PRINT*, '+++ check_parameters: upper bound 10 of array', & 460 ' "ug_vertical_gradient_level_ind" exceeded' 461 ENDIF 462 CALL local_stop 463 ENDIF 464 ENDIF 465 IF ( gradient /= 0.0 ) THEN 466 IF ( k /= 1 ) THEN 467 ug(k) = ug(k-1) + dzu(k) * gradient 454 455 IF ( .NOT. ocean ) THEN 456 457 ug_vertical_gradient_level_ind(1) = 0 458 ug(0) = ug_surface 459 DO k = 1, nzt+1 460 IF ( ug_vertical_gradient_level(i) < zu(k) .AND. & 461 ug_vertical_gradient_level(i) >= 0.0 ) THEN 462 gradient = ug_vertical_gradient(i) / 100.0 463 ug_vertical_gradient_level_ind(i) = k - 1 464 i = i + 1 465 IF ( i > 10 ) THEN 466 IF ( myid == 0 ) THEN 467 PRINT*, '+++ check_parameters: upper bound 10 of array', & 468 ' "ug_vertical_gradient_level_ind" exceeded' 469 ENDIF 470 CALL local_stop 471 ENDIF 472 ENDIF 473 IF ( gradient /= 0.0 ) THEN 474 IF ( k /= 1 ) THEN 475 ug(k) = ug(k-1) + dzu(k) * gradient 476 ELSE 477 ug(k) = ug_surface + 0.5 * dzu(k) * gradient 478 ENDIF 468 479 ELSE 469 ug(k) = ug_surface + 0.5 * dzu(k) * gradient 470 ENDIF 471 ELSE 472 ug(k) = ug(k-1) 473 ENDIF 474 ENDDO 480 ug(k) = ug(k-1) 481 ENDIF 482 ENDDO 483 484 ELSE 485 486 ug_vertical_gradient_level_ind(1) = nzt+1 487 DO k = nzt, 0, -1 488 IF ( ug_vertical_gradient_level(i) > zu(k) .AND. & 489 ug_vertical_gradient_level(i) <= 0.0 ) THEN 490 gradient = ug_vertical_gradient(i) / 100.0 491 ug_vertical_gradient_level_ind(i) = k + 1 492 i = i + 1 493 IF ( i > 10 ) THEN 494 IF ( myid == 0 ) THEN 495 PRINT*, '+++ check_parameters: upper bound 10 of array', & 496 ' "ug_vertical_gradient_level_ind" exceeded' 497 ENDIF 498 CALL local_stop 499 ENDIF 500 ENDIF 501 IF ( gradient /= 0.0 ) THEN 502 IF ( k /= nzt ) THEN 503 ug(k) = ug(k+1) - dzu(k+1) * gradient 504 ELSE 505 ug(k) = ug_surface - 0.5 * dzu(k+1) * gradient 506 ug(k+1) = ug_surface + 0.5 * dzu(k+1) * gradient 507 ENDIF 508 ELSE 509 ug(k) = ug(k+1) 510 ENDIF 511 ENDDO 512 513 ENDIF 475 514 476 515 u_init = ug … … 478 517 ! 479 518 !-- In case of no given gradients for ug, choose a vanishing gradient 480 IF ( ug_vertical_gradient_level(1) == - 1.0) THEN519 IF ( ug_vertical_gradient_level(1) == -9999999.9 ) THEN 481 520 ug_vertical_gradient_level(1) = 0.0 482 521 ENDIF … … 488 527 i = 1 489 528 gradient = 0.0 490 vg_vertical_gradient_level_ind(1) = 0 491 vg(0) = vg_surface 492 DO k = 1, nzt+1 493 IF ( vg_vertical_gradient_level(i) < zu(k) .AND. & 494 vg_vertical_gradient_level(i) >= 0.0 ) THEN 495 gradient = vg_vertical_gradient(i) / 100.0 496 vg_vertical_gradient_level_ind(i) = k - 1 497 i = i + 1 498 IF ( i > 10 ) THEN 499 IF ( myid == 0 ) THEN 500 PRINT*, '+++ check_parameters: upper bound 10 of array', & 501 ' "vg_vertical_gradient_level_ind" exceeded' 502 ENDIF 503 CALL local_stop 504 ENDIF 505 ENDIF 506 IF ( gradient /= 0.0 ) THEN 507 IF ( k /= 1 ) THEN 508 vg(k) = vg(k-1) + dzu(k) * gradient 529 530 IF ( .NOT. ocean ) THEN 531 532 vg_vertical_gradient_level_ind(1) = 0 533 vg(0) = vg_surface 534 DO k = 1, nzt+1 535 IF ( vg_vertical_gradient_level(i) < zu(k) .AND. & 536 vg_vertical_gradient_level(i) >= 0.0 ) THEN 537 gradient = vg_vertical_gradient(i) / 100.0 538 vg_vertical_gradient_level_ind(i) = k - 1 539 i = i + 1 540 IF ( i > 10 ) THEN 541 IF ( myid == 0 ) THEN 542 PRINT*, '+++ check_parameters: upper bound 10 of array', & 543 ' "vg_vertical_gradient_level_ind" exceeded' 544 ENDIF 545 CALL local_stop 546 ENDIF 547 ENDIF 548 IF ( gradient /= 0.0 ) THEN 549 IF ( k /= 1 ) THEN 550 vg(k) = vg(k-1) + dzu(k) * gradient 551 ELSE 552 vg(k) = vg_surface + 0.5 * dzu(k) * gradient 553 ENDIF 509 554 ELSE 510 vg(k) = vg_surface + 0.5 * dzu(k) * gradient 511 ENDIF 512 ELSE 513 vg(k) = vg(k-1) 514 ENDIF 515 ENDDO 555 vg(k) = vg(k-1) 556 ENDIF 557 ENDDO 558 559 ELSE 560 561 vg_vertical_gradient_level_ind(1) = 0 562 DO k = nzt, 0, -1 563 IF ( vg_vertical_gradient_level(i) > zu(k) .AND. & 564 vg_vertical_gradient_level(i) <= 0.0 ) THEN 565 gradient = vg_vertical_gradient(i) / 100.0 566 vg_vertical_gradient_level_ind(i) = k + 1 567 i = i + 1 568 IF ( i > 10 ) THEN 569 IF ( myid == 0 ) THEN 570 PRINT*, '+++ check_parameters: upper bound 10 of array', & 571 ' "vg_vertical_gradient_level_ind" exceeded' 572 ENDIF 573 CALL local_stop 574 ENDIF 575 ENDIF 576 IF ( gradient /= 0.0 ) THEN 577 IF ( k /= nzt ) THEN 578 vg(k) = vg(k+1) - dzu(k+1) * gradient 579 ELSE 580 vg(k) = vg_surface - 0.5 * dzu(k+1) * gradient 581 vg(k+1) = vg_surface + 0.5 * dzu(k+1) * gradient 582 ENDIF 583 ELSE 584 vg(k) = vg(k+1) 585 ENDIF 586 ENDDO 587 588 ENDIF 516 589 517 590 v_init = vg … … 519 592 ! 520 593 !-- In case of no given gradients for vg, choose a vanishing gradient 521 IF ( vg_vertical_gradient_level(1) == - 1.0) THEN594 IF ( vg_vertical_gradient_level(1) == -9999999.9 ) THEN 522 595 vg_vertical_gradient_level(1) = 0.0 523 596 ENDIF … … 707 780 708 781 ! 709 !-- Reference temperature to be used in buoyancy terms 710 IF ( pt_reference /= 9999999.9 ) use_pt_reference = .TRUE. 782 !-- Ocean runs always use reference values in the buoyancy term. Therefore 783 !-- set the reference temperature equal to the surface temperature. 784 IF ( ocean .AND. pt_reference == 9999999.9 ) pt_reference = pt_surface 785 786 ! 787 !-- Reference value has to be used in buoyancy terms 788 IF ( pt_reference /= 9999999.9 ) use_reference = .TRUE. 789 790 ! 791 !-- Sign of buoyancy/stability terms 792 IF ( ocean ) atmos_ocean_sign = -1.0 793 794 ! 795 !-- Ocean version is using flux boundary conditions at the top 796 IF ( ocean ) use_top_fluxes = .TRUE. 711 797 712 798 ! … … 1020 1106 1021 1107 IF ( top_salinityflux == 9999999.9 ) constant_top_salinityflux = .FALSE. 1108 IF ( ibc_sa_t == 1 .AND. top_salinityflux == 9999999.9 ) THEN 1109 IF ( myid == 0 ) THEN 1110 PRINT*, '+++ check_parameters:' 1111 PRINT*, ' boundary_condition: bc_sa_t = ', bc_sa_t 1112 PRINT*, ' requires to set top_salinityflux ' 1113 ENDIF 1114 CALL local_stop 1115 ENDIF 1022 1116 1023 1117 ! … … 2474 2568 ! 2475 2569 !-- Determine upper and lower hight level indices for random perturbations 2476 IF ( disturbance_level_b == -1.0 ) THEN 2477 disturbance_level_b = zu(nzb+3) 2478 disturbance_level_ind_b = nzb + 3 2570 IF ( disturbance_level_b == -9999999.9 ) THEN 2571 IF ( ocean ) THEN 2572 disturbance_level_b = zu((nzt*2)/3) 2573 disturbance_level_ind_b = ( nzt * 2 ) / 3 2574 ELSE 2575 disturbance_level_b = zu(nzb+3) 2576 disturbance_level_ind_b = nzb + 3 2577 ENDIF 2479 2578 ELSEIF ( disturbance_level_b < zu(3) ) THEN 2480 2579 IF ( myid == 0 ) PRINT*, '+++ check_parameters: disturbance_level_b=',& … … 2496 2595 ENDIF 2497 2596 2498 IF ( disturbance_level_t == -1.0 ) THEN 2499 disturbance_level_t = zu(nzt/3) 2500 disturbance_level_ind_t = nzt / 3 2597 IF ( disturbance_level_t == -9999999.9 ) THEN 2598 IF ( ocean ) THEN 2599 disturbance_level_t = zu(nzt-3) 2600 disturbance_level_ind_t = nzt - 3 2601 ELSE 2602 disturbance_level_t = zu(nzt/3) 2603 disturbance_level_ind_t = nzt / 3 2604 ENDIF 2501 2605 ELSEIF ( disturbance_level_t > zu(nzt-2) ) THEN 2502 2606 IF ( myid == 0 ) PRINT*, '+++ check_parameters: disturbance_level_t=',& -
palm/trunk/SOURCE/diffusion_e.f90
r94 r97 8 8 ! This is also a bugfix, because the height above the topography is now 9 9 ! used instead of the height above level k=0. 10 ! theta renamed var, dpt_dz renamed dvar_dz, +new argument var_reference 11 ! use_pt_reference renamed use_reference 10 12 ! 11 13 ! Former revisions: … … 50 52 ! Call for all grid points 51 53 !------------------------------------------------------------------------------! 52 SUBROUTINE diffusion_e( ddzu, dd2zu, ddzw, diss, e, km, l_grid, theta, &53 rif, tend, zu, zw )54 SUBROUTINE diffusion_e( ddzu, dd2zu, ddzw, diss, e, km, l_grid, var, & 55 var_reference, rif, tend, zu, zw ) 54 56 55 57 USE control_parameters … … 61 63 62 64 INTEGER :: i, j, k 63 REAL :: d pt_dz, l_stable, phi_m65 REAL :: dvar_dz, l_stable, phi_m, var_reference 64 66 REAL :: ddzu(1:nzt+1), dd2zu(1:nzt), ddzw(1:nzt+1), & 65 67 l_grid(1:nzt), zu(0:nzt+1), zw(0:nzt+1) 66 68 REAL, DIMENSION(nzb:nzt+1,nys-1:nyn+1,nxl-1:nxr+1) :: diss, tend 67 69 REAL, DIMENSION(:,:), POINTER :: rif 68 REAL, DIMENSION(:,:,:), POINTER :: e, km, theta70 REAL, DIMENSION(:,:,:), POINTER :: e, km, var 69 71 REAL, DIMENSION(nzb+1:nzt,nys:nyn) :: dissipation, l, ll 70 72 … … 73 75 !-- This if clause must be outside the k-loop because otherwise 74 76 !-- runtime errors occur with -C hopt on NEC 75 IF ( use_ pt_reference ) THEN77 IF ( use_reference ) THEN 76 78 77 79 DO i = nxl, nxr … … 91 93 ! 92 94 !-- Calculate the mixing length (for dissipation) 93 dpt_dz = ( theta(k+1,j,i) - theta(k-1,j,i) ) * dd2zu(k) 94 IF ( dpt_dz > 0.0 ) THEN 95 dvar_dz = atmos_ocean_sign * & 96 ( var(k+1,j,i) - var(k-1,j,i) ) * dd2zu(k) 97 IF ( dvar_dz > 0.0 ) THEN 95 98 l_stable = 0.76 * SQRT( e(k,j,i) ) / & 96 SQRT( g / pt_reference * dpt_dz ) + 1E-599 SQRT( g / var_reference * dvar_dz ) + 1E-5 97 100 ELSE 98 101 l_stable = l_grid(k) … … 180 183 ! 181 184 !-- Calculate the mixing length (for dissipation) 182 dpt_dz = ( theta(k+1,j,i) - theta(k-1,j,i) ) * dd2zu(k) 183 IF ( dpt_dz > 0.0 ) THEN 185 dvar_dz = atmos_ocean_sign * & 186 ( var(k+1,j,i) - var(k-1,j,i) ) * dd2zu(k) 187 IF ( dvar_dz > 0.0 ) THEN 184 188 l_stable = 0.76 * SQRT( e(k,j,i) ) / & 185 SQRT( g / theta(k,j,i) * dpt_dz ) + 1E-5189 SQRT( g / var(k,j,i) * dvar_dz ) + 1E-5 186 190 ELSE 187 191 l_stable = l_grid(k) … … 270 274 !------------------------------------------------------------------------------! 271 275 SUBROUTINE diffusion_e_ij( i, j, ddzu, dd2zu, ddzw, diss, e, km, l_grid, & 272 theta, rif, tend, zu, zw )276 var, var_reference, rif, tend, zu, zw ) 273 277 274 278 USE control_parameters … … 280 284 281 285 INTEGER :: i, j, k 282 REAL :: d pt_dz, l_stable, phi_m286 REAL :: dvar_dz, l_stable, phi_m, var_reference 283 287 REAL :: ddzu(1:nzt+1), dd2zu(1:nzt), ddzw(1:nzt+1), & 284 288 l_grid(1:nzt), zu(0:nzt+1), zw(0:nzt+1) 285 289 REAL, DIMENSION(nzb:nzt+1,nys-1:nyn+1,nxl-1:nxr+1) :: diss, tend 286 290 REAL, DIMENSION(:,:), POINTER :: rif 287 REAL, DIMENSION(:,:,:), POINTER :: e, km, theta291 REAL, DIMENSION(:,:,:), POINTER :: e, km, var 288 292 REAL, DIMENSION(nzb+1:nzt) :: dissipation, l, ll 289 293 … … 303 307 !-- Calculate the mixing length (for dissipation) 304 308 DO k = nzb_s_inner(j,i)+1, nzt 305 dpt_dz = ( theta(k+1,j,i) - theta(k-1,j,i) ) * dd2zu(k) 306 IF ( dpt_dz > 0.0 ) THEN 307 IF ( use_pt_reference ) THEN 309 dvar_dz = atmos_ocean_sign * & 310 ( var(k+1,j,i) - var(k-1,j,i) ) * dd2zu(k) 311 IF ( dvar_dz > 0.0 ) THEN 312 IF ( use_reference ) THEN 308 313 l_stable = 0.76 * SQRT( e(k,j,i) ) / & 309 SQRT( g / pt_reference * dpt_dz ) + 1E-5314 SQRT( g / var_reference * dvar_dz ) + 1E-5 310 315 ELSE 311 316 l_stable = 0.76 * SQRT( e(k,j,i) ) / & 312 SQRT( g / theta(k,j,i) * dpt_dz ) + 1E-5317 SQRT( g / var(k,j,i) * dvar_dz ) + 1E-5 313 318 ENDIF 314 319 ELSE -
palm/trunk/SOURCE/diffusivities.f90
r94 r97 1 SUBROUTINE diffusivities( theta)1 SUBROUTINE diffusivities( var, var_reference ) 2 2 3 3 !------------------------------------------------------------------------------! … … 7 7 ! This is also a bugfix, because the height above the topography is now 8 8 ! used instead of the height above level k=0. 9 ! theta renamed var, dpt_dz renamed dvar_dz, +new argument var_reference 10 ! use_pt_reference renamed use_reference 9 11 ! 10 12 ! Former revisions: … … 41 43 INTEGER :: i, j, k, omp_get_thread_num, sr, tn 42 44 43 REAL :: d pt_dz, l_stable, phi_m = 1.045 REAL :: dvar_dz, l_stable, var_reference 44 46 45 REAL :: theta(nzb:nzt+1,nys-1:nyn+1,nxl-1:nxr+1) 47 REAL, SAVE :: phi_m = 1.0 48 49 REAL :: var(nzb:nzt+1,nys-1:nyn+1,nxl-1:nxr+1) 46 50 47 51 REAL, DIMENSION(1:nzt) :: l, ll, sqrt_e … … 58 62 ! 59 63 !-- Compute the turbulent diffusion coefficient for momentum 60 !$OMP PARALLEL PRIVATE (d pt_dz,i,j,k,l,ll,l_stable,phi_m,sqrt_e,sr,tn)64 !$OMP PARALLEL PRIVATE (dvar_dz,i,j,k,l,ll,l_stable,phi_m,sqrt_e,sr,tn) 61 65 !$ tn = omp_get_thread_num() 62 66 … … 94 98 !-- Determine the mixing length 95 99 DO k = nzb_s_inner(j,i)+1, nzt 96 dpt_dz = ( theta(k+1,j,i) - theta(k-1,j,i) ) * dd2zu(k) 97 IF ( dpt_dz > 0.0 ) THEN 98 IF ( use_pt_reference ) THEN 100 dvar_dz = atmos_ocean_sign * & ! inverse effect of pt/rho gradient 101 ( var(k+1,j,i) - var(k-1,j,i) ) * dd2zu(k) 102 IF ( dvar_dz > 0.0 ) THEN 103 IF ( use_reference ) THEN 99 104 l_stable = 0.76 * sqrt_e(k) / & 100 SQRT( g / pt_reference * dpt_dz ) + 1E-5105 SQRT( g / var_reference * dvar_dz ) + 1E-5 101 106 ELSE 102 107 l_stable = 0.76 * sqrt_e(k) / & 103 SQRT( g / theta(k,j,i) * dpt_dz ) + 1E-5108 SQRT( g / var(k,j,i) * dvar_dz ) + 1E-5 104 109 ENDIF 105 110 ELSE -
palm/trunk/SOURCE/eqn_state_seawater.f90
r96 r97 8 8 ! Former revisions: 9 9 ! ----------------- 10 ! $Id :$10 ! $Id$ 11 11 ! 12 12 ! Initial revision … … 18 18 ! salinity, and pressure. 19 19 ! For coefficients see Jackett et al., 2006: J. Atm. Ocean Tech. 20 ! eqn_state_seawater calculates the potential density referred at hyp(0). 21 ! eqn_state_seawater_func calculates density. 20 22 !------------------------------------------------------------------------------! 21 23 … … 70 72 DO i = nxl, nxr 71 73 DO j = nys, nyn 72 DO k = nzb_ u_inner(j,i)+1, nzt74 DO k = nzb_s_inner(j,i)+1, nzt 73 75 ! 74 76 !-- Pressure is needed in dbar 75 p1 = hyp( k) * 1E-477 p1 = hyp(0) * 1E-4 76 78 p2 = p1 * p1 77 79 p3 = p2 * p1 … … 102 104 103 105 ENDDO 106 ! 107 !-- Neumann conditions are assumed at bottom and top boundary 108 rho(nzt+1,j,i) = rho(nzt,j,i) 109 rho(nzb_s_inner(j,i),j,i) = rho(nzb_s_inner(j,i)+1,j,i) 104 110 ENDDO 105 111 ENDDO … … 122 128 REAL :: p1, p2, p3, pt1, pt2, pt3, pt4, sa1, sa15, sa2 123 129 124 DO k = nzb_ u_inner(j,i)+1, nzt130 DO k = nzb_s_inner(j,i)+1, nzt 125 131 ! 126 132 !-- Pressure is needed in dbar 127 p1 = hyp( k) * 1E-4133 p1 = hyp(0) * 1E-4 128 134 p2 = p1 * p1 129 135 p3 = p2 * p1 … … 152 158 ) 153 159 ENDDO 160 ! 161 !-- Neumann conditions are assumed at bottom and top boundary 162 rho(nzt+1,j,i) = rho(nzt,j,i) 163 rho(nzb_s_inner(j,i),j,i) = rho(nzb_s_inner(j,i)+1,j,i) 154 164 155 165 END SUBROUTINE eqn_state_seawater_ij -
palm/trunk/SOURCE/flow_statistics.f90
r96 r97 5 5 ! ----------------- 6 6 ! Statistics for ocean version (salinity, density) added, 7 ! calculation of Deardorff velocity scale adjusted to be used with the ocean8 ! version (HAS STILL TO BE COMPLETED!!!)7 ! calculation of z_i and Deardorff velocity scale adjusted to be used with 8 ! the ocean version 9 9 ! 10 10 ! Former revisions: … … 558 558 ! 559 559 !-- Salinity flux and density (density does not belong to here, 560 !-- but so far there is no suitable place to calculate)560 !-- but so far there is no other suitable place to calculate) 561 561 IF ( ocean ) THEN 562 562 pts = 0.5 * ( sa(k,j,i) - hom(k,1,23,sr) + & … … 611 611 612 612 ! 613 !-- Density at top follows Neumann condition 614 IF ( ocean ) sums_l(nzt+1,64,tn) = sums_l(nzt,64,tn) 615 616 ! 613 617 !-- Divergence of vertical flux of resolved scale energy and pressure 614 618 !-- fluctuations. First calculate the products, then the divergence. … … 709 713 ! 710 714 !-- Fluxes at the surface must be zero (e.g. due to the Prandtl-layer) 711 sums (nzb,58) = 0.0712 sums (nzb,59) = 0.0713 sums (nzb,60) = 0.0714 sums (nzb,61) = 0.0715 sums (nzb,62) = 0.0716 sums (nzb,63) = 0.0715 sums_l(nzb,58,tn) = 0.0 716 sums_l(nzb,59,tn) = 0.0 717 sums_l(nzb,60,tn) = 0.0 718 sums_l(nzb,61,tn) = 0.0 719 sums_l(nzb,62,tn) = 0.0 720 sums_l(nzb,63,tn) = 0.0 717 721 718 722 ENDIF … … 857 861 z_i(1) = 0.0 858 862 first = .TRUE. 859 ! IF ( .NOT. ocean ) THEN 863 IF ( ocean ) THEN 864 DO k = nzt, nzb+1, -1 865 IF ( first .AND. hom(k,1,18,sr) < 0.0 ) THEN 866 first = .FALSE. 867 height = zw(k) 868 ENDIF 869 IF ( hom(k,1,18,sr) < 0.0 .AND. & 870 hom(k-1,1,18,sr) > hom(k,1,18,sr) ) THEN 871 IF ( zw(k) < 1.5 * height ) THEN 872 z_i(1) = zw(k) 873 ELSE 874 z_i(1) = height 875 ENDIF 876 EXIT 877 ENDIF 878 ENDDO 879 ELSE 860 880 DO k = nzb, nzt-1 861 881 IF ( first .AND. hom(k,1,18,sr) < 0.0 ) THEN … … 873 893 ENDIF 874 894 ENDDO 875 ! ELSE 876 ! ENDIF 877 878 ! 879 !-- Second scheme: Starting from the top model boundary, look for the first 880 !-- characteristic kink in the temperature profile, where the originally 881 !-- stable stratification notably weakens. 895 ENDIF 896 897 ! 898 !-- Second scheme: Starting from the top/bottom model boundary, look for 899 !-- the first characteristic kink in the temperature profile, where the 900 !-- originally stable stratification notably weakens. 882 901 z_i(2) = 0.0 883 DO k = nzt-1, nzb+1, -1 884 IF ( ( hom(k+1,1,4,sr) - hom(k,1,4,sr) ) > & 885 2.0 * ( hom(k,1,4,sr) - hom(k-1,1,4,sr) ) ) THEN 886 z_i(2) = zu(k) 887 EXIT 888 ENDIF 889 ENDDO 902 IF ( ocean ) THEN 903 DO k = nzb+1, nzt-1 904 IF ( ( hom(k,1,4,sr) - hom(k-1,1,4,sr) ) > & 905 2.0 * ( hom(k+1,1,4,sr) - hom(k,1,4,sr) ) ) THEN 906 z_i(2) = zu(k) 907 EXIT 908 ENDIF 909 ENDDO 910 ELSE 911 DO k = nzt-1, nzb+1, -1 912 IF ( ( hom(k+1,1,4,sr) - hom(k,1,4,sr) ) > & 913 2.0 * ( hom(k,1,4,sr) - hom(k-1,1,4,sr) ) ) THEN 914 z_i(2) = zu(k) 915 EXIT 916 ENDIF 917 ENDDO 918 ENDIF 890 919 891 920 hom(nzb+6,1,pr_palm,sr) = z_i(1) -
palm/trunk/SOURCE/header.f90
r94 r97 4 4 ! Actual revisions: 5 5 ! ----------------- 6 ! Output of model height, stretch level, Prandtl-layer height and initial7 ! temperature profile adjusted to be used also with the ocean version.6 ! Adjustments for the ocean version. 7 ! use_pt_reference renamed use_reference 8 8 ! 9 9 ! Former revisions: … … 103 103 PRINT*,'+++ header: unknown action(s): ',initializing_actions 104 104 ENDIF 105 ENDIF 106 IF ( ocean ) THEN 107 run_classification = 'ocean - ' // run_classification 108 ELSE 109 run_classification = 'atmosphere - ' // run_classification 105 110 ENDIF 106 111 … … 391 396 roben = 'e(nzt+1) = e(nzt) = e(nzt-1)' 392 397 393 WRITE ( io, 301 ) runten, roben 394 395 ENDIF 396 397 IF ( humidity .OR. passive_scalar ) THEN 398 IF ( humidity ) THEN 399 IF ( ibc_q_b == 0 ) THEN 400 runten = 'q(0) = q_surface' 401 ELSE 402 runten = 'q(0) = q(1)' 403 ENDIF 404 IF ( ibc_q_t == 0 ) THEN 405 roben = 'q(nzt) = q_top' 406 ELSE 407 roben = 'q(nzt) = q(nzt-1) + dq/dz' 408 ENDIF 409 ELSE 410 IF ( ibc_q_b == 0 ) THEN 411 runten = 's(0) = s_surface' 412 ELSE 413 runten = 's(0) = s(1)' 414 ENDIF 415 IF ( ibc_q_t == 0 ) THEN 416 roben = 's(nzt) = s_top' 417 ELSE 418 roben = 's(nzt) = s(nzt-1) + ds/dz' 419 ENDIF 420 ENDIF 421 422 WRITE ( io, 302 ) runten, roben 423 398 WRITE ( io, 301 ) 'e', runten, roben 399 400 ENDIF 401 402 IF ( ocean ) THEN 403 runten = 'sa(0) = sa(1)' 404 IF ( ibc_sa_t == 0 ) THEN 405 roben = 'sa(nzt+1) = sa_surface' 406 ELSE 407 roben = 'sa(nzt+1) = sa(nzt)' 408 ENDIF 409 WRITE ( io, 301 ) 'sa', runten, roben 410 ENDIF 411 412 IF ( humidity ) THEN 413 IF ( ibc_q_b == 0 ) THEN 414 runten = 'q(0) = q_surface' 415 ELSE 416 runten = 'q(0) = q(1)' 417 ENDIF 418 IF ( ibc_q_t == 0 ) THEN 419 roben = 'q(nzt) = q_top' 420 ELSE 421 roben = 'q(nzt) = q(nzt-1) + dq/dz' 422 ENDIF 423 WRITE ( io, 301 ) 'q', runten, roben 424 ENDIF 425 426 IF ( passive_scalar ) THEN 427 IF ( ibc_q_b == 0 ) THEN 428 runten = 's(0) = s_surface' 429 ELSE 430 runten = 's(0) = s(1)' 431 ENDIF 432 IF ( ibc_q_t == 0 ) THEN 433 roben = 's(nzt) = s_top' 434 ELSE 435 roben = 's(nzt) = s(nzt-1) + ds/dz' 436 ENDIF 437 WRITE ( io, 301 ) 's', runten, roben 424 438 ENDIF 425 439 … … 442 456 IF ( constant_top_heatflux ) THEN 443 457 WRITE ( io, 306 ) top_heatflux 458 ENDIF 459 IF ( ocean .AND. constant_top_salinityflux ) THEN 460 WRITE ( io, 309 ) top_salinityflux 444 461 ENDIF 445 462 IF ( humidity .OR. passive_scalar ) THEN … … 887 904 !-- Other quantities 888 905 WRITE ( io, 411 ) g 889 IF ( use_pt_reference ) WRITE ( io, 412 ) pt_reference 906 IF ( use_reference ) THEN 907 IF ( ocean ) THEN 908 WRITE ( io, 412 ) prho_reference 909 ELSE 910 WRITE ( io, 413 ) pt_reference 911 ENDIF 912 ENDIF 890 913 891 914 ! … … 1011 1034 TRIM( gradients ), TRIM( slices ) 1012 1035 ENDIF 1036 ENDIF 1037 1038 ! 1039 !-- Initial salinity profile 1040 !-- Building output strings, starting with surface salinity 1041 IF ( ocean ) THEN 1042 WRITE ( temperatures, '(F6.2)' ) sa_surface 1043 gradients = '------' 1044 slices = ' 0' 1045 coordinates = ' 0.0' 1046 i = 1 1047 DO WHILE ( sa_vertical_gradient_level_ind(i) /= -9999 ) 1048 1049 WRITE (coor_chr,'(F7.2)') sa_init(sa_vertical_gradient_level_ind(i)) 1050 temperatures = TRIM( temperatures ) // ' ' // TRIM( coor_chr ) 1051 1052 WRITE (coor_chr,'(F7.2)') sa_vertical_gradient(i) 1053 gradients = TRIM( gradients ) // ' ' // TRIM( coor_chr ) 1054 1055 WRITE (coor_chr,'(I7)') sa_vertical_gradient_level_ind(i) 1056 slices = TRIM( slices ) // ' ' // TRIM( coor_chr ) 1057 1058 WRITE (coor_chr,'(F7.1)') sa_vertical_gradient_level(i) 1059 coordinates = TRIM( coordinates ) // ' ' // TRIM( coor_chr ) 1060 1061 i = i + 1 1062 ENDDO 1063 1064 WRITE ( io, 425 ) TRIM( coordinates ), TRIM( temperatures ), & 1065 TRIM( gradients ), TRIM( slices ) 1013 1066 ENDIF 1014 1067 … … 1135 1188 1136 1189 99 FORMAT (1X,78('-')) 1137 100 FORMAT (/1X,'*************************',11X, 28('-')/ &1190 100 FORMAT (/1X,'*************************',11X,42('-')/ & 1138 1191 1X,'* ',A,' *',11X,A/ & 1139 1X,'*************************',11X, 28('-')// &1192 1X,'*************************',11X,42('-')// & 1140 1193 ' Date: ',A8,11X,'Run: ',A20/ & 1141 1194 ' Time: ',A8,11X,'Run-No.: ',I2.2/ & … … 1256 1309 ' B. bound.: ',A/ & 1257 1310 ' T. bound.: ',A) 1258 301 FORMAT (/' e'// & 1259 ' B. bound.: ',A/ & 1260 ' T. bound.: ',A) 1261 302 FORMAT (/' q'// & 1311 301 FORMAT (/' ',A// & 1262 1312 ' B. bound.: ',A/ & 1263 1313 ' T. bound.: ',A) … … 1268 1318 ' zp = ',F6.2,' m z0 = ',F6.4,' m kappa = ',F4.2/ & 1269 1319 ' Rif value range: ',F6.2,' <= rif <=',F6.2) 1270 306 FORMAT (' Predefined constant heatflux: ',F 6.3,' K m/s')1320 306 FORMAT (' Predefined constant heatflux: ',F9.6,' K m/s') 1271 1321 307 FORMAT (' Heatflux has a random normal distribution') 1272 1322 308 FORMAT (' Predefined surface temperature') 1323 309 FORMAT (' Predefined constant salinityflux: ',F9.6,' psu m/s') 1273 1324 310 FORMAT (//' 1D-Model:'// & 1274 1325 ' Rif value range: ',F6.2,' <= rif <=',F6.2) … … 1352 1403 ' f* = ',F9.6,' 1/s') 1353 1404 411 FORMAT (/' Gravity : g = ',F4.1,' m/s**2') 1354 412 FORMAT (/' Reference temperature in buoyancy terms: ',F8.4,' K') 1405 412 FORMAT (/' Reference density in buoyancy terms: ',F8.3,' kg/m**3') 1406 413 FORMAT (/' Reference temperature in buoyancy terms: ',F8.4,' K') 1355 1407 415 FORMAT (/' Cloud physics parameters:'/ & 1356 1408 ' ------------------------'/) … … 1382 1434 424 FORMAT (/' Characteristic levels of the geo. wind component vg:'// & 1383 1435 ' Height: ',A,' m'/ & 1384 ' vg: ',A,' m/ S'/ &1436 ' vg: ',A,' m/s'/ & 1385 1437 ' Gradient: ',A,' 1/100s'/ & 1386 1438 ' Gridpoint: ',A) 1439 425 FORMAT (/' Characteristic levels of the initial salinity profile:'// & 1440 ' Height: ',A,' m'/ & 1441 ' Salinity: ',A,' psu'/ & 1442 ' Gradient: ',A,' psu/100m'/ & 1443 ' Gridpoint: ',A) 1387 1444 450 FORMAT (//' LES / Turbulence quantities:'/ & 1388 1445 ' ---------------------------'/) -
palm/trunk/SOURCE/init_3d_model.f90
r96 r97 529 529 hom(:,1,24,:) = SPREAD( kh(:,nys,nxl), 2, statistic_regions+1 ) 530 530 531 IF ( ocean ) THEN 532 ! 533 !-- Store initial salinity profile 534 hom(:,1,26,:) = SPREAD( sa(:,nys,nxl), 2, statistic_regions+1 ) 535 ENDIF 531 536 532 537 IF ( humidity ) THEN -
palm/trunk/SOURCE/init_ocean.f90
r96 r97 40 40 hyp(nzt+1) = surface_pressure * 100.0 41 41 42 hyp(nzt) = hyp(nzt+1) + rho_surface * g * 0.5 * dzu(nzt+1)43 rho_ref 42 hyp(nzt) = hyp(nzt+1) + rho_surface * g * 0.5 * dzu(nzt+1) 43 rho_reference = rho_surface * 0.5 * dzu(nzt+1) 44 44 45 45 DO k = nzt-1, 0, -1 … … 48 48 pt_l = 0.5 * ( pt_init(k) + pt_init(k+1) ) 49 49 50 rho_l 50 rho_l = eqn_state_seawater_func( hyp(k+1), pt_l, sa_l ) 51 51 52 hyp(k) = hyp(k+1) + rho_l * g * dzu(k+1)53 rho_ref = rho_ref+ rho_l * dzu(k+1)52 hyp(k) = hyp(k+1) + rho_l * g * dzu(k+1) 53 rho_reference = rho_reference + rho_l * dzu(k+1) 54 54 55 55 ENDDO 56 56 57 rho_ref = rho_ref / ( zw(nzt) - zu(nzb) ) 58 print*, '*** rho_ref = ', rho_ref 57 rho_reference = rho_reference / ( zw(nzt) - zu(nzb) ) 58 59 ! 60 !-- Calculate the reference potential density 61 prho_reference = 0.0 62 DO k = 0, nzt 63 64 sa_l = 0.5 * ( sa_init(k) + sa_init(k+1) ) 65 pt_l = 0.5 * ( pt_init(k) + pt_init(k+1) ) 66 67 prho_reference = prho_reference + dzu(k+1) * & 68 eqn_state_seawater_func( hyp(0), pt_l, sa_l ) 69 70 ENDDO 71 72 prho_reference = prho_reference / ( zu(nzt) - zu(nzb) ) 59 73 60 74 -
palm/trunk/SOURCE/modules.f90
r96 r97 5 5 ! Actual revisions: 6 6 ! ----------------- 7 ! + ocean, r, + salinity variables7 ! +atmos_ocean_sign, ocean, r, + salinity variables 8 8 ! defaults of .._vertical_gradient_levels changed from -1.0 to -9999999.9 9 ! hydro_press renamed hyp 9 ! hydro_press renamed hyp, use_pt_reference renamed use_reference 10 10 ! 11 11 ! Former revisions: … … 324 324 sloping_surface = .FALSE., stop_dt = .FALSE., & 325 325 terminate_run = .FALSE., use_prior_plot1d_parameters = .FALSE.,& 326 use_ pt_reference = .FALSE., use_surface_fluxes = .FALSE., &326 use_reference = .FALSE., use_surface_fluxes = .FALSE., & 327 327 use_top_fluxes = .FALSE., use_ug_for_galilei_tr = .TRUE., & 328 328 use_upstream_for_tke = .FALSE., wall_adjustment = .TRUE. … … 333 333 REAL :: advected_distance_x = 0.0, advected_distance_y = 0.0, & 334 334 alpha_surface = 0.0, asselin_filter_factor = 0.1, & 335 atmos_ocean_sign = 1.0, & 335 336 averaging_interval = 0.0, averaging_interval_pr = 9999999.9, & 336 337 averaging_interval_sp = 9999999.9, bc_pt_t_val, bc_q_t_val, & … … 340 341 building_wall_south = 9999999.9, cfl_factor = -1.0, & 341 342 cos_alpha_surface, disturbance_amplitude = 0.25, & 342 disturbance_energy_limit = 0.01, disturbance_level_b = -1.0, & 343 disturbance_level_t = -1.0, dt = -1.0, dt_averaging_input = 0.0, & 343 disturbance_energy_limit = 0.01, & 344 disturbance_level_b = -9999999.9, & 345 disturbance_level_t = -9999999.9, & 346 dt = -1.0, dt_averaging_input = 0.0, & 344 347 dt_averaging_input_pr = 9999999.9, dt_data_output = 9999999.9, & 345 348 dt_data_output_av = 9999999.9, dt_disturb = 9999999.9, & … … 360 363 overshoot_limit_w = 0.0, particle_maximum_age = 9999999.9, & 361 364 phi = 55.0, prandtl_number = 1.0, & 362 precipitation_amount_interval = 9999999.9, &363 pt_reference = 9999999.9, &364 pt_s lope_offset = 0.0, pt_surface = 300.0, &365 pt_surface_initial_change = 0.0, q_surface = 0.0, &366 q_surface_initial_change = 0.0, rayleigh_damping_factor= -1.0, &367 r ayleigh_damping_height = -1.0, residual_limit = 1.0E-4, &368 r estart_time = 9999999.9, rho_ref, rho_surface, rif_max = 1.0, &365 precipitation_amount_interval = 9999999.9, prho_reference, & 366 pt_reference = 9999999.9, pt_slope_offset = 0.0, & 367 pt_surface = 300.0, pt_surface_initial_change = 0.0, & 368 q_surface = 0.0, q_surface_initial_change = 0.0, & 369 rayleigh_damping_factor = -1.0, rayleigh_damping_height = -1.0, & 370 residual_limit = 1.0E-4, restart_time = 9999999.9, rho_reference, & 371 rho_surface, rif_max = 1.0, & 369 372 rif_min = -5.0, roughness_length = 0.1, sa_surface = 35.0, & 370 373 simulated_time = 0.0, simulated_time_at_begin, sin_alpha_surface, & … … 401 404 tsc(10) = (/ 0.0, 1.0, 0.0, 0.0, 0.0, 0.0, 0.0, 0.0, 0.0, 0.0 /), & 402 405 ug_vertical_gradient(10) = 0.0, & 403 ug_vertical_gradient_level(10) = - 1.0, &406 ug_vertical_gradient_level(10) = -9999999.9, & 404 407 vg_vertical_gradient(10) = 0.0, & 405 vg_vertical_gradient_level(10) = - 1.0, &408 vg_vertical_gradient_level(10) = -9999999.9, & 406 409 volume_flow(1:2) = 0.0, volume_flow_area(1:2) = 0.0, & 407 410 volume_flow_initial(1:2) = 0.0, wall_heatflux(0:4) = 0.0 -
palm/trunk/SOURCE/netcdf.f90
r77 r97 7 7 ! Current revisions: 8 8 ! ------------------ 9 ! 9 ! Grids defined for rho and sa 10 10 ! 11 11 ! Former revisions: … … 345 345 !-- Most variables are defined on the scalar grid 346 346 CASE ( 'e', 'p', 'pc', 'pr', 'pt', 'q', 'ql', 'ql_c', 'ql_v', & 347 'ql_vp', 'qv', ' s', 'vpt' )347 'ql_vp', 'qv', 'rho', 's', 'sa', 'vpt' ) 348 348 349 349 grid_x = 'x' … … 870 870 CASE ( 'e_xy', 'p_xy', 'pc_xy', 'pr_xy', 'pt_xy', 'q_xy',& 871 871 'ql_xy', 'ql_c_xy', 'ql_v_xy', 'ql_vp_xy', & 872 'qv_xy', ' s_xy', 'vpt_xy' )872 'qv_xy', 'rho_xy', 's_xy', 'sa_xy', 'vpt_xy' ) 873 873 874 874 grid_x = 'x' … … 1414 1414 CASE ( 'e_xz', 'p_xz', 'pc_xz', 'pr_xz', 'pt_xz', 'q_xz', & 1415 1415 'ql_xz', 'ql_c_xz', 'ql_v_xz', 'ql_vp_xz', 'qv_xz', & 1416 ' s_xz', 'vpt_xz' )1416 'rho_xz', 's_xz', 'sa_xz', 'vpt_xz' ) 1417 1417 1418 1418 grid_x = 'x' … … 1925 1925 CASE ( 'e_yz', 'p_yz', 'pc_yz', 'pr_yz', 'pt_yz', 'q_yz', & 1926 1926 'ql_yz', 'ql_c_yz', 'ql_v_yz', 'ql_vp_yz', 'qv_yz', & 1927 ' s_yz', 'vpt_yz' )1927 'rho_yz', 's_yz', 'sa_yz', 'vpt_yz' ) 1928 1928 1929 1929 grid_x = 'x' -
palm/trunk/SOURCE/palm.f90
r90 r97 63 63 INTEGER :: i, run_description_header_i(80) 64 64 65 version = 'PALM 3. 2b'65 version = 'PALM 3.3' 66 66 67 67 #if defined( __parallel ) -
palm/trunk/SOURCE/production_e.f90
r77 r97 4 4 ! Actual revisions: 5 5 ! ----------------- 6 ! 6 ! energy production by density flux (in ocean) added 7 ! use_pt_reference renamed use_reference 7 8 ! 8 9 ! Former revisions: … … 364 365 IF ( .NOT. humidity ) THEN 365 366 366 IF ( use_pt_reference ) THEN 367 368 DO j = nys, nyn 369 DO k = nzb_diff_s_inner(j,i), nzt_diff 370 tend(k,j,i) = tend(k,j,i) - kh(k,j,i) * g/pt_reference * & 367 IF ( use_reference ) THEN 368 369 IF ( ocean ) THEN 370 ! 371 !-- So far in the ocean no special treatment of density flux in 372 !-- the bottom and top surface layer 373 DO j = nys, nyn 374 DO k = nzb_s_inner(j,i), nzt 375 tend(k,j,i) = tend(k,j,i) + & 376 kh(k,j,i) * g / prho_reference * & 377 ( rho(k+1,j,i)-rho(k-1,j,i) ) * dd2zu(k) 378 ENDDO 379 ENDDO 380 381 ELSE 382 383 DO j = nys, nyn 384 DO k = nzb_diff_s_inner(j,i), nzt_diff 385 tend(k,j,i) = tend(k,j,i) + & 386 kh(k,j,i) * g / pt_reference * & 371 387 ( pt(k+1,j,i) - pt(k-1,j,i) ) * dd2zu(k) 388 ENDDO 389 390 IF ( use_surface_fluxes ) THEN 391 k = nzb_diff_s_inner(j,i)-1 392 tend(k,j,i) = tend(k,j,i) + g / pt_reference * shf(j,i) 393 ENDIF 394 395 IF ( use_top_fluxes ) THEN 396 k = nzt 397 tend(k,j,i) = tend(k,j,i) + g / pt_reference * & 398 tswst(j,i) 399 ENDIF 372 400 ENDDO 373 401 374 IF ( use_surface_fluxes ) THEN 375 k = nzb_diff_s_inner(j,i)-1 376 tend(k,j,i) = tend(k,j,i) + g / pt_reference * shf(j,i) 377 ENDIF 378 379 IF ( use_top_fluxes ) THEN 380 k = nzt 381 tend(k,j,i) = tend(k,j,i) + g / pt_reference * tswst(j,i) 382 ENDIF 383 ENDDO 402 ENDIF 384 403 385 404 ELSE 386 405 387 DO j = nys, nyn 388 DO k = nzb_diff_s_inner(j,i), nzt_diff 389 tend(k,j,i) = tend(k,j,i) - kh(k,j,i) * g / pt(k,j,i) * & 406 IF ( ocean ) THEN 407 ! 408 !-- So far in the ocean no special treatment of density flux in 409 !-- the bottom and top surface layer 410 DO j = nys, nyn 411 DO k = nzb_s_inner(j,i), nzt 412 tend(k,j,i) = tend(k,j,i) - & 413 kh(k,j,i) * g / rho(k,j,i) * & 414 ( rho(k+1,j,i)-rho(k-1,j,i) ) * dd2zu(k) 415 ENDDO 416 ENDDO 417 418 ELSE 419 420 DO j = nys, nyn 421 DO k = nzb_diff_s_inner(j,i), nzt_diff 422 tend(k,j,i) = tend(k,j,i) - & 423 kh(k,j,i) * g / pt(k,j,i) * & 390 424 ( pt(k+1,j,i) - pt(k-1,j,i) ) * dd2zu(k) 425 ENDDO 426 427 IF ( use_surface_fluxes ) THEN 428 k = nzb_diff_s_inner(j,i)-1 429 tend(k,j,i) = tend(k,j,i) + g / pt(k,j,i) * shf(j,i) 430 ENDIF 431 432 IF ( use_top_fluxes ) THEN 433 k = nzt 434 tend(k,j,i) = tend(k,j,i) + g / pt(k,j,i) * tswst(j,i) 435 ENDIF 391 436 ENDDO 392 437 393 IF ( use_surface_fluxes ) THEN 394 k = nzb_diff_s_inner(j,i)-1 395 tend(k,j,i) = tend(k,j,i) + g / pt(k,j,i) * shf(j,i) 396 ENDIF 397 398 IF ( use_top_fluxes ) THEN 399 k = nzt 400 tend(k,j,i) = tend(k,j,i) + g / pt(k,j,i) * tswst(j,i) 401 ENDIF 402 ENDDO 438 ENDIF 403 439 404 440 ENDIF … … 762 798 IF ( .NOT. humidity ) THEN 763 799 764 IF ( use_pt_reference ) THEN 765 766 DO k = nzb_diff_s_inner(j,i), nzt_diff 767 tend(k,j,i) = tend(k,j,i) - kh(k,j,i) * g / pt_reference * & 800 IF ( use_reference ) THEN 801 802 IF ( ocean ) THEN 803 ! 804 !-- So far in the ocean no special treatment of density flux in the 805 !-- bottom and top surface layer 806 DO k = nzb_s_inner(j,i), nzt 807 tend(k,j,i) = tend(k,j,i) + kh(k,j,i) * g / prho_reference * & 808 ( rho(k+1,j,i) - rho(k-1,j,i) ) * dd2zu(k) 809 ENDDO 810 811 ELSE 812 813 DO k = nzb_diff_s_inner(j,i), nzt_diff 814 tend(k,j,i) = tend(k,j,i) - kh(k,j,i) * g / pt_reference * & 768 815 ( pt(k+1,j,i) - pt(k-1,j,i) ) * dd2zu(k) 769 ENDDO 770 771 IF ( use_surface_fluxes ) THEN 772 k = nzb_diff_s_inner(j,i)-1 773 tend(k,j,i) = tend(k,j,i) + g / pt_reference * shf(j,i) 816 ENDDO 817 818 IF ( use_surface_fluxes ) THEN 819 k = nzb_diff_s_inner(j,i)-1 820 tend(k,j,i) = tend(k,j,i) + g / pt_reference * shf(j,i) 821 ENDIF 822 823 IF ( use_top_fluxes ) THEN 824 k = nzt 825 tend(k,j,i) = tend(k,j,i) + g / pt_reference * tswst(j,i) 826 ENDIF 827 774 828 ENDIF 775 829 776 IF ( use_top_fluxes ) THEN 777 k = nzt 778 tend(k,j,i) = tend(k,j,i) + g / pt_reference * tswst(j,i) 830 ELSE 831 832 IF ( ocean ) THEN 833 ! 834 !-- So far in the ocean no special treatment of density flux in the 835 !-- bottom and top surface layer 836 DO k = nzb_s_inner(j,i), nzt 837 tend(k,j,i) = tend(k,j,i) + kh(k,j,i) * g / rho(k,j,i) * & 838 ( rho(k+1,j,i) - rho(k-1,j,i) ) * dd2zu(k) 839 ENDDO 840 841 ELSE 842 843 DO k = nzb_diff_s_inner(j,i), nzt_diff 844 tend(k,j,i) = tend(k,j,i) - kh(k,j,i) * g / pt(k,j,i) * & 845 ( pt(k+1,j,i) - pt(k-1,j,i) ) * dd2zu(k) 846 ENDDO 847 848 IF ( use_surface_fluxes ) THEN 849 k = nzb_diff_s_inner(j,i)-1 850 tend(k,j,i) = tend(k,j,i) + g / pt(k,j,i) * shf(j,i) 851 ENDIF 852 853 IF ( use_top_fluxes ) THEN 854 k = nzt 855 tend(k,j,i) = tend(k,j,i) + g / pt(k,j,i) * tswst(j,i) 856 ENDIF 857 779 858 ENDIF 780 859 781 ELSE 782 783 DO k = nzb_diff_s_inner(j,i), nzt_diff 784 tend(k,j,i) = tend(k,j,i) - kh(k,j,i) * g / pt(k,j,i) * & 785 ( pt(k+1,j,i) - pt(k-1,j,i) ) * dd2zu(k) 786 ENDDO 787 788 IF ( use_surface_fluxes ) THEN 789 k = nzb_diff_s_inner(j,i)-1 790 tend(k,j,i) = tend(k,j,i) + g / pt(k,j,i) * shf(j,i) 791 ENDIF 792 793 IF ( use_top_fluxes ) THEN 794 k = nzt 795 tend(k,j,i) = tend(k,j,i) + g / pt(k,j,i) * tswst(j,i) 796 ENDIF 797 798 ENDIF 860 ENDIF 799 861 800 862 ELSE -
palm/trunk/SOURCE/prognostic_equations.f90
r96 r97 5 5 ! ----------------- 6 6 ! prognostic equation for salinity, density is calculated from equation of 7 ! state for seawater, +eqn_state_seawater_mod 8 ! new argument zw in calls of diffusion_e, calc_mean_pt_profile renamed 7 ! state for seawater and is used for calculation of buoyancy, 8 ! +eqn_state_seawater_mod 9 ! diffusion_e is called with argument rho in case of ocean runs, 10 ! new argument zw in calls of diffusion_e, new argument pt_/prho_reference 11 ! in calls of buoyancy and diffusion_e, calc_mean_pt_profile renamed 9 12 ! calc_mean_profile 10 13 ! … … 148 151 ENDIF 149 152 CALL coriolis( i, j, 1 ) 150 IF ( sloping_surface ) CALL buoyancy( i, j, pt, 1, 4 )153 IF ( sloping_surface ) CALL buoyancy( i, j, pt, pt_reference, 1, 4 ) 151 154 CALL user_actions( i, j, 'u-tendency' ) 152 155 … … 283 286 ENDIF 284 287 CALL coriolis( i, j, 3 ) 285 IF ( .NOT. humidity) THEN286 CALL buoyancy( i, j, pt, 3,4 )288 IF ( ocean ) THEN 289 CALL buoyancy( i, j, rho, prho_reference, 3, 64 ) 287 290 ELSE 288 CALL buoyancy( i, j, vpt, 3, 44 ) 291 IF ( .NOT. humidity ) THEN 292 CALL buoyancy( i, j, pt, pt_reference, 3, 4 ) 293 ELSE 294 CALL buoyancy( i, j, vpt, pt_reference, 3, 44 ) 295 ENDIF 289 296 ENDIF 290 297 CALL user_actions( i, j, 'w-tendency' ) … … 654 661 .NOT. use_upstream_for_tke ) THEN 655 662 IF ( .NOT. humidity ) THEN 656 CALL diffusion_e( i, j, ddzu, dd2zu, ddzw, diss, e, km, & 657 l_grid, pt, rif, tend, zu, zw ) 663 IF ( ocean ) THEN 664 CALL diffusion_e( i, j, ddzu, dd2zu, ddzw, diss, e, km, & 665 l_grid, rho, prho_reference, rif, tend, & 666 zu, zw ) 667 ELSE 668 CALL diffusion_e( i, j, ddzu, dd2zu, ddzw, diss, e, km, & 669 l_grid, pt, pt_reference, rif, tend, & 670 zu, zw ) 671 ENDIF 658 672 ELSE 659 CALL diffusion_e( i, j, ddzu, dd2zu, ddzw, diss, e, km, & 660 l_grid, vpt, rif, tend, zu, zw ) 673 CALL diffusion_e( i, j, ddzu, dd2zu, ddzw, diss, e, km, & 674 l_grid, vpt, pt_reference, rif, tend, zu, & 675 zw ) 661 676 ENDIF 662 677 ELSE … … 680 695 IF ( .NOT. humidity ) THEN 681 696 CALL diffusion_e( i, j, ddzu, dd2zu, ddzw, diss, e_m, & 682 km_m, l_grid, pt_m, rif_m, tend, zu,&683 zw )697 km_m, l_grid, pt_m, pt_reference, & 698 rif_m, tend, zu, zw ) 684 699 ELSE 685 700 CALL diffusion_e( i, j, ddzu, dd2zu, ddzw, diss, e_m, & 686 km_m, l_grid, vpt_m, rif_m, tend, zu,&687 zw )701 km_m, l_grid, vpt_m, pt_reference, & 702 rif_m, tend, zu, zw ) 688 703 ENDIF 689 704 ELSE 690 705 IF ( .NOT. humidity ) THEN 691 CALL diffusion_e( i, j, ddzu, dd2zu, ddzw, diss, e, km, & 692 l_grid, pt, rif, tend, zu, zw ) 706 IF ( ocean ) THEN 707 CALL diffusion_e( i, j, ddzu, dd2zu, ddzw, diss, e, & 708 km, l_grid, rho, prho_reference, & 709 rif, tend, zu, zw ) 710 ELSE 711 CALL diffusion_e( i, j, ddzu, dd2zu, ddzw, diss, e, & 712 km, l_grid, pt, pt_reference, rif, & 713 tend, zu, zw ) 714 ENDIF 693 715 ELSE 694 716 CALL diffusion_e( i, j, ddzu, dd2zu, ddzw, diss, e, km, & 695 l_grid, vpt, rif, tend, zu, zw ) 717 l_grid, vpt, pt_reference, rif, tend, & 718 zu, zw ) 696 719 ENDIF 697 720 ENDIF … … 797 820 ENDIF 798 821 CALL coriolis( i, j, 1 ) 799 IF ( sloping_surface ) CALL buoyancy( i, j, pt, 1, 4 ) 822 IF ( sloping_surface ) CALL buoyancy( i, j, pt, pt_reference, 1, & 823 4 ) 800 824 CALL user_actions( i, j, 'u-tendency' ) 801 825 … … 896 920 ENDIF 897 921 CALL coriolis( i, j, 3 ) 898 IF ( .NOT. humidity) THEN899 CALL buoyancy( i, j, pt, 3,4 )922 IF ( ocean ) THEN 923 CALL buoyancy( i, j, rho, prho_reference, 3, 64 ) 900 924 ELSE 901 CALL buoyancy( i, j, vpt, 3, 44 ) 925 IF ( .NOT. humidity ) THEN 926 CALL buoyancy( i, j, pt, pt_reference, 3, 4 ) 927 ELSE 928 CALL buoyancy( i, j, vpt, pt_reference, 3, 44 ) 929 ENDIF 902 930 ENDIF 903 931 CALL user_actions( i, j, 'w-tendency' ) … … 1114 1142 IF ( .NOT. humidity ) THEN 1115 1143 CALL diffusion_e( i, j, ddzu, dd2zu, ddzw, diss, e_m, & 1116 km_m, l_grid, pt_m, rif_m, tend, zu,&1117 zw )1144 km_m, l_grid, pt_m, pt_reference, & 1145 rif_m, tend, zu, zw ) 1118 1146 ELSE 1119 1147 CALL diffusion_e( i, j, ddzu, dd2zu, ddzw, diss, e_m, & 1120 km_m, l_grid, vpt_m, rif_m, tend, zu,&1121 zw )1148 km_m, l_grid, vpt_m, pt_reference, & 1149 rif_m, tend, zu, zw ) 1122 1150 ENDIF 1123 1151 ELSE 1124 1152 IF ( .NOT. humidity ) THEN 1125 CALL diffusion_e( i, j, ddzu, dd2zu, ddzw, diss, e, km, & 1126 l_grid, pt, rif, tend, zu, zw ) 1153 IF ( ocean ) THEN 1154 CALL diffusion_e( i, j, ddzu, dd2zu, ddzw, diss, e, & 1155 km, l_grid, rho, prho_reference, & 1156 rif, tend, zu, zw ) 1157 ELSE 1158 CALL diffusion_e( i, j, ddzu, dd2zu, ddzw, diss, e, & 1159 km, l_grid, pt, pt_reference, rif, & 1160 tend, zu, zw ) 1161 ENDIF 1127 1162 ELSE 1128 1163 CALL diffusion_e( i, j, ddzu, dd2zu, ddzw, diss, e, km, & 1129 l_grid, vpt, rif, tend, zu, zw ) 1164 l_grid, vpt, pt_reference, rif, tend, & 1165 zu, zw ) 1130 1166 ENDIF 1131 1167 ENDIF … … 1224 1260 ENDIF 1225 1261 CALL coriolis( 1 ) 1226 IF ( sloping_surface ) CALL buoyancy( pt, 1, 4 )1262 IF ( sloping_surface ) CALL buoyancy( pt, pt_reference, 1, 4 ) 1227 1263 CALL user_actions( 'u-tendency' ) 1228 1264 … … 1367 1403 ENDIF 1368 1404 CALL coriolis( 3 ) 1369 IF ( .NOT. humidity) THEN1370 CALL buoyancy( pt, 3,4 )1405 IF ( ocean ) THEN 1406 CALL buoyancy( rho, prho_reference, 3, 64 ) 1371 1407 ELSE 1372 CALL buoyancy( vpt, 3, 44 ) 1408 IF ( .NOT. humidity ) THEN 1409 CALL buoyancy( pt, pt_reference, 3, 4 ) 1410 ELSE 1411 CALL buoyancy( vpt, pt_reference, 3, 44 ) 1412 ENDIF 1373 1413 ENDIF 1374 1414 CALL user_actions( 'w-tendency' ) … … 1753 1793 THEN 1754 1794 IF ( .NOT. humidity ) THEN 1755 CALL diffusion_e( ddzu, dd2zu, ddzw, diss, e, km, l_grid, pt, & 1756 rif, tend, zu, zw ) 1795 IF ( ocean ) THEN 1796 CALL diffusion_e( ddzu, dd2zu, ddzw, diss, e, km, l_grid, rho, & 1797 prho_reference, rif, tend, zu, zw ) 1798 ELSE 1799 CALL diffusion_e( ddzu, dd2zu, ddzw, diss, e, km, l_grid, pt, & 1800 pt_reference, rif, tend, zu, zw ) 1801 ENDIF 1757 1802 ELSE 1758 1803 CALL diffusion_e( ddzu, dd2zu, ddzw, diss, e, km, l_grid, vpt, & 1759 rif, tend, zu, zw )1804 pt_reference, rif, tend, zu, zw ) 1760 1805 ENDIF 1761 1806 ELSE … … 1777 1822 IF ( .NOT. humidity ) THEN 1778 1823 CALL diffusion_e( ddzu, dd2zu, ddzw, diss, e_m, km_m, l_grid, & 1779 pt_m, rif_m, tend, zu, zw )1824 pt_m, pt_reference, rif_m, tend, zu, zw ) 1780 1825 ELSE 1781 1826 CALL diffusion_e( ddzu, dd2zu, ddzw, diss, e_m, km_m, l_grid, & 1782 vpt_m, rif_m, tend, zu, zw )1827 vpt_m, pt_reference, rif_m, tend, zu, zw ) 1783 1828 ENDIF 1784 1829 ELSE 1785 1830 IF ( .NOT. humidity ) THEN 1786 CALL diffusion_e( ddzu, dd2zu, ddzw, diss, e, km, l_grid, pt, & 1787 rif, tend, zu, zw ) 1831 IF ( ocean ) THEN 1832 CALL diffusion_e( ddzu, dd2zu, ddzw, diss, e, km, l_grid, & 1833 rho, prho_reference, rif, tend, zu, zw ) 1834 ELSE 1835 CALL diffusion_e( ddzu, dd2zu, ddzw, diss, e, km, l_grid, & 1836 pt, pt_reference, rif, tend, zu, zw ) 1837 ENDIF 1788 1838 ELSE 1789 1839 CALL diffusion_e( ddzu, dd2zu, ddzw, diss, e, km, l_grid, vpt, & 1790 rif, tend, zu, zw )1840 pt_reference, rif, tend, zu, zw ) 1791 1841 ENDIF 1792 1842 ENDIF -
palm/trunk/SOURCE/run_control.f90
r90 r97 4 4 ! Actual revisions: 5 5 ! ----------------- 6 ! 6 ! Timestep format changed 7 7 ! 8 8 ! Former revisions: … … 113 113 100 FORMAT (///'Run-control output:'/ & 114 114 &'------------------'// & 115 &'RUN ITER. HH:MM:SS.SS DT(E) UMAX VMAX WMAX U*', &116 &' W* THETA* Z_I ENERG. DISTENERG DIVOLD DIVNE', &117 &'W UMAX(KJI) VMAX(KJI) WMAX(KJI) ADVECX ADVECY MG', &118 &'CYC'/&119 120 121 122 &'--')123 101 FORMAT (I3,1X,I6,1X,A8,F3.2,1X,F 7.4,A1,A1,F8.4,A1,F8.4,A1,F8.4,2X,F5.3,2X, &115 &'RUN ITER. HH:MM:SS.SS DT(E) UMAX VMAX WMAX U', & 116 &'* W* THETA* Z_I ENERG. DISTENERG DIVOLD DIV', & 117 &'NEW UMAX(KJI) VMAX(KJI) WMAX(KJI) ADVECX ADVECY ', & 118 &'MGCYC'/ & 119 &'----------------------------------------------------------------', & 120 &'----------------------------------------------------------------', & 121 &'----------------------------------------------------------------', & 122 &'-----') 123 101 FORMAT (I3,1X,I6,1X,A8,F3.2,1X,F8.4,A1,A1,F8.4,A1,F8.4,A1,F8.4,2X,F5.3,2X, & 124 124 F4.2, & 125 2X,F6.3,2X,F 5.0,1X,4(E10.3,1X),3(3(I4),1X),F8.3,1X,F8.3,5X,I3)125 2X,F6.3,2X,F6.0,1X,4(E10.3,1X),3(3(I4),1X),F8.3,1X,F8.3,5X,I3) 126 126 127 127 END SUBROUTINE run_control -
palm/trunk/SOURCE/time_integration.f90
r95 r97 4 4 ! Actual revisions: 5 5 ! ----------------- 6 ! Ghostpoint exchange for salinity and density 6 ! diffusivities is called with argument rho in case of ocean runs, 7 ! new argument pt_/prho_reference in calls of diffusivities, 8 ! ghostpoint exchange for salinity and density 7 9 ! 8 10 ! Former revisions: … … 249 251 CALL cpu_log( log_point(17), 'diffusivities', 'start' ) 250 252 IF ( .NOT. humidity ) THEN 251 CALL diffusivities( pt ) 253 IF ( ocean ) THEN 254 CALL diffusivities( rho, prho_reference ) 255 ELSE 256 CALL diffusivities( pt, pt_reference ) 257 ENDIF 252 258 ELSE 253 CALL diffusivities( vpt )259 CALL diffusivities( vpt, pt_reference ) 254 260 ENDIF 255 261 CALL cpu_log( log_point(17), 'diffusivities', 'stop' )
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