Changeset 110 for palm/trunk/DOC/tec/technical_documentation.html
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- Oct 5, 2007 5:13:14 AM (17 years ago)
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palm/trunk/DOC/tec/technical_documentation.html
r98 r110 2314 2314 density is calculated from the equation of state for seawater after 2315 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, 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> 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 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, 2321 check_open, check_parameters, diffusion_u, diffusion_v, 2322 flow_statistics, header, init_pegrid, init_rankine, init_3d_model, 2323 local_stop, modules, palm, parin, prandtl_fluxes, pres, 2324 prognostic_equations, read_var_list, read_3d_binary, swap_timelevel, 2325 timestep, time_integration, write_var_list, write_3d_binary<br><br><span style="font-weight: bold;">new:</span><br>surface_coupler</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;">Remaining variables <span style="font-family: Courier New,Courier,monospace;">iran</span> changed to <span style="font-family: Courier New,Courier,monospace;">iran_part</span> (advec_particles, init_particles).<br><br>In case that the presure solver is not called for every Runge-Kutta substep (<span style="font-family: Courier New,Courier,monospace;">call_psolver_at_all_substeps</span> = <span style="font-style: italic;">.F.</span>), 2326 it is called after the first substep instead of the last. In that case, 2327 random perturbations are also added to the velocity field after the 2328 first substep.<br><br>Initialization of <span style="font-family: Courier New,Courier,monospace;">km</span>, <span style="font-family: Courier New,Courier,monospace;">kh</span> = 0.00001 for <span style="font-family: Courier New,Courier,monospace;">ocean</span> = <span style="font-style: italic;">.T.</span> (for <span style="font-family: Courier New,Courier,monospace;">ocean</span> = <span style="font-style: italic;">.F.</span> it remains 0.01).<br><br>Allow <span style="font-family: Courier New,Courier,monospace;">data_output_pr</span> = '<span style="font-style: italic;">q</span>', '<span style="font-style: italic;">wq</span>', '<span style="font-style: italic;">w"q"</span>', '<span style="font-style: italic;">w*q*</span>' for <span style="font-family: Courier New,Courier,monospace;">humidity</span> = <span style="font-style: italic;">.T.</span> (instead of <span style="font-family: Courier New,Courier,monospace;">cloud_physics</span> = <span style="font-style: italic;">.T.</span>).</td><td style="vertical-align: top;">advec_particles, check_for_restart, check_parameters, init_particles, init_3d_model, time_integration<br></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;">Bugs from code parts for non-cyclic boundary conditions are removed:<br>loops for u and v are starting from index <span style="font-family: Courier New,Courier,monospace;">nxlu</span>, <span style="font-family: Courier New,Courier,monospace;">nysv</span>, 2329 respectively. The radiation boundary condition is used for every 2330 Runge-Kutta substep. Velocity phase speeds for the radiation boundary 2331 conditions are calculated for the first Runge-Kutta substep only and 2332 reused for the further substeps. New arrays <span style="font-family: Courier New,Courier,monospace;">c_u</span>, <span style="font-family: Courier New,Courier,monospace;">c_v</span>, and <span style="font-family: Courier New,Courier,monospace;">c_w</span> 2333 are defined for this purpose. Several index errors are removed from the 2334 radiation boundary condition code parts. Upper bounds for calculating <span style="font-family: Courier New,Courier,monospace;">u_0</span> and <span style="font-family: Courier New,Courier,monospace;">v_0</span> (in production_e) are <span style="font-style: italic;">nxr+1</span> and <span style="font-style: italic;">nyn+1</span> because otherwise these values are not available in case of non-cyclic boundary conditions.<br><br>+<span style="font-family: Courier New,Courier,monospace;">dots_num_palm</span> in module user, +module netcdf_control in user_init (both in user_interface)<br><br>Bugfix: wrong sign removed from the buoyancy production term in the case <span style="font-family: Courier New,Courier,monospace;">use_reference</span> = <span style="font-style: italic;">.T.</span> (production_e)<br><br>Bugfix: Error message concerning output of particle concentration (pc) modified (check_parameters).<br><br>Bugfix: Rayleigh damping for ocean fixed.</td><td style="vertical-align: top;">advec_u_pw, 2335 advec_u_up, advec_v_pw, advec_v_up, boundary_conds, buoyancy, 2336 check_parameters, coriolis, diffusion_u, diffusion_v, header, 2337 init_pegrid, init_3d_model, modules, production_e, 2338 prognostic_equations, user_interface<br></td></tr> 2317 2339 </tbody> 2318 2340 </table> <b><blink>Attention:</blink></b>
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