Index: /palm/trunk/DOC/app/chapter_4.1.html
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--- /palm/trunk/DOC/app/chapter_4.1.html	(revision 110)
+++ /palm/trunk/DOC/app/chapter_4.1.html	(revision 111)
@@ -1,5 +1,4 @@
 <!DOCTYPE html PUBLIC "-//W3C//DTD HTML 4.01 Transitional//EN">
-<html>
-<head>
+<html><head>
 
 
@@ -16,7 +15,5 @@
   
   
-  <title>PALM chapter 4.1</title>
-</head>
-
+  <title>PALM chapter 4.1</title></head>
 
 <body>
@@ -5141,5 +5138,5 @@
       <p>A value for this
 parameter must be assigned. Since the lower
-array bound in PALM starts with i = 0, the actual number of grid points
+array bound in PALM starts with j = 0, the actual number of grid points
 is equal to <b>ny+1</b>. In case of cyclic boundary
 conditions along
@@ -10505,4 +10502,3 @@
 
 
-</body>
-</html>
+</body></html>
Index: /palm/trunk/DOC/app/index.html
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--- /palm/trunk/DOC/app/index.html	(revision 110)
+++ /palm/trunk/DOC/app/index.html	(revision 111)
@@ -180,5 +180,5 @@
 <p><span style="font-family: Thorndale;" lang="EN-GB">Current
 model
-version:&nbsp;&nbsp;&nbsp;&nbsp;&nbsp;&nbsp;&nbsp;&nbsp;&nbsp;&nbsp;&nbsp;&nbsp;&nbsp;&nbsp;&nbsp;3.3<br>
+version:&nbsp;&nbsp;&nbsp;&nbsp;&nbsp;&nbsp;&nbsp;&nbsp;&nbsp;&nbsp;&nbsp;&nbsp;&nbsp;&nbsp;&nbsp;3.4<br>
 For date of last change see bottom line of each page. <o:p></o:p></span></p>
 
Index: /palm/trunk/DOC/tec/technical_documentation.html
===================================================================
--- /palm/trunk/DOC/tec/technical_documentation.html	(revision 110)
+++ /palm/trunk/DOC/tec/technical_documentation.html	(revision 111)
@@ -12,5 +12,5 @@
 <br><table nosave="" cellpadding="0" cellspacing="0"> <caption>&nbsp; <br> </caption><tbody>
 </tbody><tbody> </tbody> <tbody> <tr nosave=""> <td nosave=""><b>Current
-model version:</b></td> <td><span style="font-weight: bold;">3.3</span></td> </tr>
+model version:</b></td> <td><span style="font-weight: bold;">3.4</span></td> </tr>
 <tr nosave=""> <td nosave=""><b>Last
 change of this document</b>:&nbsp;</td> <td nosave=""><b>$Id$</b></td> </tr>
@@ -2316,7 +2316,6 @@
 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&nbsp;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,&nbsp;data_output_2d,<br>data_output_3d,&nbsp;diffusion_e,<br>diffusivities,&nbsp;flow_statistics,&nbsp;header,<br>init_grid,&nbsp;init_3d_model,&nbsp;modules,<br>netcdf,&nbsp;parin,&nbsp;production_e,<br>prognostic_equations,<br>read_3d_binary,&nbsp;&nbsp;read_var_list,<br>sum_up_3d_data,&nbsp;swap_timelevel,<br>time_integration,&nbsp;user_interface,<br>write_var_list,&nbsp;write_3d_binary<br><br><span style="font-weight: bold;">new:</span><br>eqn_state_seawater,&nbsp;init_ocean</td></tr><tr><td style="vertical-align: top;">&nbsp;</td><td style="vertical-align: top;">&nbsp;</td><td style="vertical-align: top;">&nbsp;</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,&nbsp;buoyancy,&nbsp;<br>calc_liquid_water_content, <br>check_parameters,&nbsp;diffusion_e,<br>diffusivities,&nbsp;header,<br>init_cloud_physics,&nbsp;modules,<br>production_e,&nbsp;prognostic_equations,<br>run_control</td></tr><tr><td style="vertical-align: top;">&nbsp;</td><td style="vertical-align: top;">&nbsp;</td><td style="vertical-align: top;">&nbsp;</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,&nbsp;diffusion_e,&nbsp;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>".
 Saturation at k=nzb is assumed for the atmosphere coupled to ocean.
-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>
-The format of the testresult-file (run control output) has changed
-due to this modification.</td><td style="vertical-align: top;">boundary_conds,
+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>
+</td><td style="vertical-align: top;">boundary_conds,
 check_open, check_parameters, diffusion_u, diffusion_v,
 flow_statistics, header, init_pegrid, init_rankine, init_3d_model,
Index: /palm/trunk/INSTALL/example_rc
===================================================================
--- /palm/trunk/INSTALL/example_rc	(revision 110)
+++ /palm/trunk/INSTALL/example_rc	(revision 111)
@@ -1,9 +1,9 @@
 
  *************************           ------------------------------------------
- * PALM 3.3  Rev: 99     *           atmosphere - 3D - run without 1D - prerun
+ * PALM 3.4  Rev: 110    *           atmosphere - 3D - run without 1D - prerun
  *************************           ------------------------------------------
 
- Date:            21-06-07           Run:       example             
- Time:            10:04:24           Run-No.:   00
+ Date:            05-10-07           Run:       example             
+ Time:            07:44:33           Run-No.:   00
  Run on host:         ibmh
  Number of PEs:          8           Processor grid (x,y): (  8,  1) forced
