Changeset 111
- Timestamp:
- Oct 5, 2007 5:57:32 AM (17 years ago)
- Location:
- palm/trunk
- Files:
-
- 4 edited
-
DOC/app/chapter_4.1.html (modified) (4 diffs)
-
DOC/app/index.html (modified) (1 diff)
-
DOC/tec/technical_documentation.html (modified) (2 diffs)
-
INSTALL/example_rc (modified) (1 diff)
Legend:
- Unmodified
- Added
- Removed
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palm/trunk/DOC/app/chapter_4.1.html
r108 r111 1 1 <!DOCTYPE html PUBLIC "-//W3C//DTD HTML 4.01 Transitional//EN"> 2 <html> 3 <head> 2 <html><head> 4 3 5 4 … … 16 15 17 16 18 <title>PALM chapter 4.1</title> 19 </head> 20 17 <title>PALM chapter 4.1</title></head> 21 18 22 19 <body> … … 5141 5138 <p>A value for this 5142 5139 parameter must be assigned. Since the lower 5143 array bound in PALM starts with i= 0, the actual number of grid points5140 array bound in PALM starts with j = 0, the actual number of grid points 5144 5141 is equal to <b>ny+1</b>. In case of cyclic boundary 5145 5142 conditions along … … 10505 10502 10506 10503 10507 </body> 10508 </html> 10504 </body></html> -
palm/trunk/DOC/app/index.html
r108 r111 180 180 <p><span style="font-family: Thorndale;" lang="EN-GB">Current 181 181 model 182 version: 3. 3<br>182 version: 3.4<br> 183 183 For date of last change see bottom line of each page. <o:p></o:p></span></p> 184 184 -
palm/trunk/DOC/tec/technical_documentation.html
r110 r111 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. 3</span></td> </tr>14 model version:</b></td> <td><span style="font-weight: bold;">3.4</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> … … 2316 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, average_3d_data,<br>boundary_conds, buoyancy,<br>check_parameters, data_output_2d,<br>data_output_3d, diffusion_e,<br>diffusivities, flow_statistics, header,<br>init_grid, init_3d_model, modules,<br>netcdf, parin, production_e,<br>prognostic_equations,<br>read_3d_binary, read_var_list,<br>sum_up_3d_data, swap_timelevel,<br>time_integration, user_interface,<br>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.<br><br>Defaults of <span style="font-family: Courier New,Courier,monospace;">.._vertical_gradient_levels</span> changed from <span style="font-style: italic;">-1.0</span> to <span style="font-style: italic;">-9999999.9</span>.</td><td style="vertical-align: top;">advec_particles, buoyancy, <br>calc_liquid_water_content, <br>check_parameters, diffusion_e,<br>diffusivities, header,<br>init_cloud_physics, modules,<br>production_e, prognostic_equations,<br>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;">Bugfix: height above topography instead of height above level k=0 is used for calculating the mixing length (<span style="font-family: Courier New,Courier,monospace;">diffusion_e</span> and <span style="font-family: Courier New,Courier,monospace;">diffusivities</span>).<br><br>Bugfix: error in boundary condition for TKE removed (<span style="font-family: Courier New,Courier,monospace;">advec_s_bc</span>).</td><td style="vertical-align: top;">advec_s_bc, diffusion_e, diffusivities</td></tr><tr><td style="vertical-align: top;">05/10/07</td><td style="vertical-align: top;">SR</td><td style="vertical-align: top;">3.4</td><td style="vertical-align: top;">N</td><td style="vertical-align: top;">This version allows runs for a coupled atmosphere-ocean LES.<br><br>Coupling frequency is controlled by new d3par-parameter <span style="font-family: Courier New,Courier,monospace;">dt_coupling</span>, the coupling mode ('<span style="font-style: italic;">atmosphere_to_ocean</span>' or '<span style="font-style: italic;">ocean_to_atmosphere</span>') for the respective processes is read from environment variable <span style="font-family: Courier New,Courier,monospace;">coupling_mode</span>, which is set by the mpiexec-command in <span style="font-weight: bold;">mrun</span>. Communication between the two models is handled by the intercommunicator <span style="font-family: Courier New,Courier,monospace;">comm_inter</span>. Local files opened by the ocean model get the additional suffic "<span style="font-family: Courier New,Courier,monospace;">_O</span>". 2317 2317 Saturation at k=nzb is assumed for the atmosphere coupled to ocean. 2318 Usage of the coupled model is described in the new section 3.8.<br><br>A momentum flux can be set as top boundary condition using the new inipar parameters <span style="font-family: Courier New,Courier,monospace;">top_momentumflux_u|v</span>.<br><br>Non-cyclic boundary conditions can be used along all horizontal directions.<br><br>Quantities w*p* and w"e can be output as vertical profiles.<br><br>Initial profiles are reset to constant profiles in case that <span style="font-family: Courier New,Courier,monospace;">initializing_actions</span> /= '<span style="font-style: italic;">set_constant_profiles</span>'. (init_rankine)<br><br>Optionally calculate km and kh from initial TKE e_init.<br><br><span style="font-weight: bold;">Attention:</span> <br> 2319 The format of the testresult-file (run control output) has changed 2320 due to this modification.</td><td style="vertical-align: top;">boundary_conds, 2318 Usage of the coupled model is described in the new section 3.8.<br><br>A momentum flux can be set as top boundary condition using the new inipar parameters <span style="font-family: Courier New,Courier,monospace;">top_momentumflux_u|v</span>.<br><br>Non-cyclic boundary conditions can be used along all horizontal directions.<br><br>Quantities w*p* and w"e can be output as vertical profiles.<br><br>Initial profiles are reset to constant profiles in case that <span style="font-family: Courier New,Courier,monospace;">initializing_actions</span> /= '<span style="font-style: italic;">set_constant_profiles</span>'. (init_rankine)<br><br>Optionally calculate km and kh from initial TKE e_init.<br> 2319 </td><td style="vertical-align: top;">boundary_conds, 2321 2320 check_open, check_parameters, diffusion_u, diffusion_v, 2322 2321 flow_statistics, header, init_pegrid, init_rankine, init_3d_model, -
palm/trunk/INSTALL/example_rc
r98 r111 1 1 2 2 ************************* ------------------------------------------ 3 * PALM 3. 3 Rev: 99* atmosphere - 3D - run without 1D - prerun3 * PALM 3.4 Rev: 110 * atmosphere - 3D - run without 1D - prerun 4 4 ************************* ------------------------------------------ 5 5 6 Date: 21-06-07 Run: example7 Time: 10:04:24Run-No.: 006 Date: 05-10-07 Run: example 7 Time: 07:44:33 Run-No.: 00 8 8 Run on host: ibmh 9 9 Number of PEs: 8 Processor grid (x,y): ( 8, 1) forced
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