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===================================================================
--- /palm/trunk/DOC/app/chapter_3.0.html	(revision 96)
+++ /palm/trunk/DOC/app/chapter_3.0.html	(revision 97)
@@ -1,11 +1,9 @@
 <!DOCTYPE HTML PUBLIC "-//W3C//DTD HTML 4.0 Transitional//EN">
 <html><head>
-<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>
+<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>
 <!--
 @page { size: 21cm 29.7cm }
 -->
 </style></head>
-
 <body style="direction: ltr;" lang="en-US"><h2 style="font-style: normal; line-height: 100%;"><font size="4">3.0
 Execution of model runs</font></h2>
@@ -41,6 +39,6 @@
 changed by the user. Some of the most important parameters are not
 preset with default values and must be adjusted by the user in each
-case. Such a typical, minimum parameter set is described in <a href="chapter_4.4.html">chapter
-4.4</a>. For the subsequent analysis of model runs, graphical
+case. Such a typical, minimum parameter set is described in <a href="chapter_4.4.1.html">chapter
+4.4.1</a>. For the subsequent analysis of model runs, graphical
 visualization of model data is particularly important. <a href="chapter_4.5.html">Chapter
 4.5</a> describes, how such outputs are produced with the model. </p>
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--- /palm/trunk/DOC/app/chapter_3.2.html	(revision 96)
+++ /palm/trunk/DOC/app/chapter_3.2.html	(revision 97)
@@ -1,11 +1,9 @@
 <!DOCTYPE HTML PUBLIC "-//W3C//DTD HTML 4.0 Transitional//EN">
 <html><head>
-<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>
+<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>
 <!--
 @page { size: 21cm 29.7cm }
 -->
 </style></head>
-
 <body style="direction: ltr;" lang="en-US"><h3 style="line-height: 100%;">3.2 Example of a minimum
 configuration
@@ -20,6 +18,6 @@
 here)
 and can be used, together with the <a href="http://www.muk.uni-hannover.de/%7Eraasch/PALM_group/INSTALL/example_p3d">parameter
-file</a> presented in <a href="chapter_4.4.html">chapter
-4.4</a>, for the execution of a simple model run. In chapter 4.4
+file</a> presented in <a href="chapter_4.4.1.html">chapter
+4.4.1</a>, for the execution of a simple model run. In chapter 4.4.1
 the
 complete <b>mrun</b> options which are necessary for the
@@ -85,6 +83,6 @@
 will
 interpret these colons as blanks (2 colons written one behind the
-other will be interpreted as a colon). Thus in the example above </font><tt><font face="Thorndale, serif">fopts
-has the value </font></tt>&ldquo;<font style="font-size: 10pt; font-family: monospace;" size="2"><i>-O3
+other will be interpreted as a colon). Thus in the example above</font> fopts
+has the value<tt><font face="Thorndale, serif"> </font></tt>&ldquo;<font style="font-size: 10pt; font-family: monospace;" size="2"><i>-O3
 -g
 -qrealsize=8 -Q -q64 -qmaxmem=-1 -qtune=pwr4 -qarch=pwr4 -qnosave
@@ -184,5 +182,5 @@
 explained in detail in the <b>mrun</b>
 description (<a href="http://www.muk.uni-hannover.de/institut/software/mrun_beschreibung.html#chapter6.3">chapter
-6.3</a>, in German) and are described here only as far as being
+6.3</a>, in German) and are described here only as far as
 necessary. A
 file connection statement usually consists of entries in 5 columns
Index: /palm/trunk/DOC/app/chapter_3.4.html
===================================================================
--- /palm/trunk/DOC/app/chapter_3.4.html	(revision 96)
+++ /palm/trunk/DOC/app/chapter_3.4.html	(revision 97)
@@ -1,5 +1,5 @@
 <!DOCTYPE html PUBLIC "-//W3C//DTD HTML 4.01 Transitional//EN">
 <html><head>
-<meta content="text/html; charset=ISO-8859-1" http-equiv="content-type"><title>chapter_3.4</title> </head>
+<meta content="text/html; charset=ISO-8859-1" http-equiv="content-type"><title>chapter_3.4</title></head>
 <body><h3 style="line-height: 100%;"><font color="#000000">3.4 Input and
 output files</font></h3>
@@ -85,6 +85,6 @@
 is needed by the model in each case. Its content and structure is
 described in detail in</font> <a href="chapter_4.0.html">chapter
-4.0</a>. <a href="chapter_4.4.html">Chapter
-4.4</a> <font color="#000000">shows a simple
+4.0</a>. <a href="chapter_4.4.1.html">Chapter
+4.4.1</a> <font color="#000000">shows a simple
 example. </font> </p> </td> </tr> <tr valign="top"> <td style="text-align: center;" width="8%"> <p align="center">13</p> </td>
 <td width="12%"> <p><a name="BININ"></a>BININ/</p>
Index: /palm/trunk/DOC/app/chapter_4.0.html
===================================================================
--- /palm/trunk/DOC/app/chapter_4.0.html	(revision 96)
+++ /palm/trunk/DOC/app/chapter_4.0.html	(revision 97)
@@ -131,6 +131,6 @@
 within routine <span style="font-family: monospace;">user_parin</span>
 in file <span style="font-family: monospace;">user_interface.f90</span>).
-<a href="chapter_4.4.html">Chapter
-4.4</a> shows a simple but complete example of the input file
+<a href="chapter_4.4.1.html">Chapter
+4.4.1</a> shows a simple but complete example of the input file
 PARIN.
 This example file can be used together with the configuration file
Index: /palm/trunk/DOC/app/chapter_4.1.html
===================================================================
--- /palm/trunk/DOC/app/chapter_4.1.html	(revision 96)
+++ /palm/trunk/DOC/app/chapter_4.1.html	(revision 97)
@@ -208,5 +208,5 @@
 </td> </tr> <tr> <td style="vertical-align: top;"> <p><a name="pc_pt_t"></a><b>bc_pt_t</b></p>
 </td> <td style="vertical-align: top;">C * 20</td>
-<td style="vertical-align: top;"><span style="font-style: italic;">'initial gradient'</span></td>
+<td style="vertical-align: top;"><span style="font-style: italic;">'initial_ gradient'</span></td>
 <td style="vertical-align: top;"> <p style="font-style: normal;">Top boundary condition of the
 potential temperature.&nbsp; </p> <p>Allowed are the
@@ -299,5 +299,12 @@
 bc_s_t_val * dzu(nz+1)</p> </ul> <p style="font-style: normal;">(up to k=nz the prognostic
 equation for the scalar concentration is
-solved).</p> </td> </tr> <tr> <td style="vertical-align: top;"> <p><a name="bc_uv_b"></a><b>bc_uv_b</b></p>
+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.&nbsp; </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
+values <span style="font-style: italic;">'dirichlet' </span>(sa(k=nz+1)
+does not change during the run) and <span style="font-style: italic;">'neumann'</span>
+(sa(k=nz+1)=sa(k=nz))<span style="font-style: italic;"></span>.&nbsp;<br><br>
+When a constant salinity flux is used at the top boundary (<a href="chapter_4.1.html#top_salinityflux">top_salinityflux</a>),
+<b>bc_sa_t</b> = <span style="font-style: italic;">'neumann'</span>
+must be used, because otherwise the resolved scale may contribute to
+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>
 </td> <td style="vertical-align: top;">C * 20</td>
 <td style="vertical-align: top;"><span style="font-style: italic;">'dirichlet'</span></td>
@@ -331,5 +338,8 @@
 Neumann condition yields the free-slip condition with u(k=nz+1) =
 u(k=nz) and v(k=nz+1) = v(k=nz) (up to k=nz the prognostic equations
-for the velocities are solved).</p> </td> </tr> <tr>
+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).&nbsp;</p>This parameter only comes into effect for ocean runs (see parameter <a href="chapter_4.1.html#ocean">ocean</a>).<p>The
+respective salinity flux value is used
+as bottom (horizontally homogeneous) boundary condition for the salinity equation. This additionally requires that a Neumann
+condition must be used for the salinity, which is currently the only available condition.<br> </p> </td></tr><tr>
 <td style="vertical-align: top;"><span style="font-weight: bold;"><a name="building_height"></a>building_height</span></td>
 <td style="vertical-align: top;">R</td> <td style="vertical-align: top;"><span style="font-style: italic;">50.0</span></td> <td>Height
@@ -1111,5 +1121,11 @@
 be an integral multiple of
 the number of processors in x-direction (due to data transposition
-restrictions).</p> </td> </tr> <tr> <td style="vertical-align: top;"> <p><a name="omega"></a><b>omega</b></p>
+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&nbsp;ocean runs.<br><br>By default PALM is configured to simulate&nbsp;atmospheric flows. However, starting from version 3.3, <span style="font-weight: bold;">ocean</span> = <span style="font-style: italic;">.T.</span> allows&nbsp;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
+density is calculated from the equation of state for seawater after
+each timestep, using the algorithm proposed by Jackett et al. (2006, J.
+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&nbsp;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
+a vertical grid stretching is not recommended since it would still
+stretch the grid towards the top boundary of the model (sea surface)
+instead of the bottom boundary.</td></tr><tr> <td style="vertical-align: top;"> <p><a name="omega"></a><b>omega</b></p>
 </td> <td style="vertical-align: top;">R</td>
 <td style="vertical-align: top;"><i>7.29212E-5</i></td>
@@ -1241,5 +1257,5 @@
 temperature to be used in all buoyancy terms (in K).<br><br>By
 default, the instantaneous horizontal average over the total model
-domain is used.</td></tr><tr> <td style="vertical-align: top;"> <p><a name="pt_surface"></a><b>pt_surface</b></p>
+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>
 </td> <td style="vertical-align: top;">R</td>
 <td style="vertical-align: top;"><i>300.0</i></td>
@@ -1247,10 +1263,13 @@
 potential temperature (in K).&nbsp; </p> <p>This
 parameter assigns the value of the potential temperature
-pt at the surface (k=0)<b>.</b> Starting from this value,
+<span style="font-weight: bold;">pt</span> at the surface (k=0)<b>.</b> Starting from this value,
 the
 initial vertical temperature profile is constructed with <a href="#pt_vertical_gradient">pt_vertical_gradient</a>
 and <a href="#pt_vertical_gradient_level">pt_vertical_gradient_level
 </a>.
-This profile is also used for the 1d-model as a stationary profile.</p>
+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>),
+this parameter gives the temperature value at the sea surface, which is
+at k=nzt. The profile is then constructed from the surface down to the
+bottom of the model.</p>
 </td> </tr> <tr> <td style="vertical-align: top;"> <p><a name="pt_surface_initial_change"></a><b>pt_surface_initial</b>
 <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>
@@ -1291,5 +1310,8 @@
 100 m and for z &gt; 1000.0 m up to the top boundary it is
 0.5 K / 100 m (it is assumed that the assigned height levels correspond
-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>
+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>),
+the profile is constructed like described above, but starting from the
+sea surface (k=nzt) down to the bottom boundary of the model. Height
+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>
 <br> <b>_level</b></p> </td> <td style="vertical-align: top;">R (10)</td> <td style="vertical-align: top;"> <p><i>10 *</i>&nbsp;
 <span style="font-style: italic;">0.0</span><br>
@@ -1297,10 +1319,9 @@
 <p>Height level from which on the temperature gradient defined by
 <a href="#pt_vertical_gradient">pt_vertical_gradient</a>
-is effective (in m).&nbsp; </p> <p>The height levels
-are to be assigned in ascending order. The
+is effective (in m).&nbsp; </p> <p>The height levels have to be assigned in ascending order. The
 default values result in a neutral stratification regardless of the
 values of <a href="#pt_vertical_gradient">pt_vertical_gradient</a>
 (unless the top boundary of the model is higher than 100000.0 m).
-For the piecewise construction of temperature profiles see <a href="#pt_vertical_gradient">pt_vertical_gradient</a>.</p>
+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&nbsp;(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="q_surface"></a><b>q_surface</b></p>
 </td> <td style="vertical-align: top;">R</td>
@@ -1453,5 +1474,36 @@
 is switched
 on (see <a href="#prandtl_layer">prandtl_layer</a>).</p>
-</td> </tr> <tr> <td style="vertical-align: top;"> <p><a name="scalar_advec"></a><b>scalar_advec</b></p>
+</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).&nbsp;</p>This parameter only comes into effect for ocean runs (see parameter <a href="chapter_4.1.html#ocean">ocean</a>).<p>This
+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,
+the
+initial vertical salinity profile is constructed from the surface down to the bottom of the model (k=0) by using&nbsp;<a href="chapter_4.1.html#sa_vertical_gradient">sa_vertical_gradient</a>
+and&nbsp;<a href="chapter_4.1.html#sa_vertical_gradient_level">sa_vertical_gradient_level
+</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
+/ 100 m).&nbsp; </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
+holds starting from the height&nbsp;
+level defined by <a href="chapter_4.1.html#sa_vertical_gradient_level">sa_vertical_gradient_level</a>
+(precisely: for all uv levels k where zu(k) &lt;
+sa_vertical_gradient_level, sa_init(k) is set: sa_init(k) =
+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
+by <a href="chapter_4.1.html#sa_vertical_gradient_level">sa_vertical_gradient_level</a>.
+A total of 10 different gradients for 11 height intervals (10 intervals
+if <a href="chapter_4.1.html#sa_vertical_gradient_level">sa_vertical_gradient_level</a>(1)
+= <i>0.0</i>) can be assigned. The surface salinity at k=nzt is
+assigned via <a href="chapter_4.1.html#sa_surface">sa_surface</a>.&nbsp;
+</p> <p>Example:&nbsp; </p> <ul><p><b>sa_vertical_gradient</b>
+= <i>1.0</i>, <i>0.5</i>,&nbsp; <br>
+<b>sa_vertical_gradient_level</b> = <i>-500.0</i>,
+-<i>1000.0</i>,</p></ul> <p>That
+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>.
+For -500.0 m &lt; z &lt;= -1000.0 m the salinity gradient is
+1.0 psu /
+100 m and for z &lt; -1000.0 m down to the bottom boundary it is
+0.5 psu / 100 m (it is assumed that the assigned height levels correspond
+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>
+is effective (in m).&nbsp; </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
+default values result in a constant salinity profile regardless of the
+values of <a href="chapter_4.1.html#sa_vertical_gradient">sa_vertical_gradient</a>
+(unless the bottom boundary of the model is lower than -100000.0 m).
+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>
 </td> <td style="vertical-align: top;">C * 10</td>
 <td style="vertical-align: top;"><i>'pw-scheme'</i></td>
@@ -1835,5 +1887,19 @@
 Prandtl-layer is available at the top boundary so far.</p><p>See
 also <a href="#surface_heatflux">surface_heatflux</a>.</p>
-</td></tr><tr> <td style="vertical-align: top;">
+</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>
+salinityflux</span></td><td style="vertical-align: top;"><p>Kinematic
+salinity flux at the top boundary, i.e. the sea surface (in psu m/s).&nbsp; </p>
+<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
+two-dimensional surface heat flux field <span style="font-family: monospace;">saswst</span> is
+initialized with the value of <span style="font-weight: bold;">top_salinityflux</span>&nbsp;as
+top (horizontally homogeneous) boundary condition for the salinity equation. This additionally requires that a Neumann
+condition must be used for the salinity (see <a href="chapter_4.1.html#bc_sa_t">bc_sa_t</a>),
+because otherwise the resolved scale may contribute to
+the top flux so that a constant value cannot be guaranteed.<span style="font-style: italic;"></span>&nbsp;</p>
+<p><span style="font-weight: bold;">Note:</span><br>The
+application of a salinity flux at the model top additionally requires the setting of
+initial parameter <a href="chapter_4.1.html#use_top_fluxes">use_top_fluxes</a>
+= .T..<span style="font-style: italic;"></span><span style="font-weight: bold;"></span> </p><p>See
+also <a href="chapter_4.1.html#bottom_salinityflux">bottom_salinityflux</a>.</p></td></tr><tr> <td style="vertical-align: top;">
 <p><a name="ug_surface"></a><span style="font-weight: bold;">ug_surface</span></p>
 </td> <td style="vertical-align: top;">R<br> </td>
@@ -1857,5 +1923,8 @@
 value, it is recommended to use a Galilei-transformation of the
 coordinate system, if possible (see <a href="#galilei_transformation">galilei_transformation</a>),
-in order to obtain larger time steps.<br> </td> </tr>
+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>),
+this parameter gives the velocity value at the sea surface, which is
+at k=nzt. The profile is then constructed from the surface down to the
+bottom of the model.<br> </td> </tr>
 <tr> <td style="vertical-align: top;"> <p><a name="ug_vertical_gradient"></a><span style="font-weight: bold;">ug_vertical_gradient</span></p>
 </td> <td style="vertical-align: top;">R(10)<br>
@@ -1872,5 +1941,8 @@
 total of 10 different gradients for 11 height intervals (10
 intervals&nbsp; if <a href="#ug_vertical_gradient_level">ug_vertical_gradient_level</a>(1)
-= 0.0) can be assigned. The surface geostrophic wind is assigned by <a href="#ug_surface">ug_surface</a>. <br> </td>
+= 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>),
+the profile is constructed like described above, but starting from the
+sea surface (k=nzt) down to the bottom boundary of the model. Height
+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>
 </tr> <tr> <td style="vertical-align: top;">
 <p><a name="ug_vertical_gradient_level"></a><span style="font-weight: bold;">ug_vertical_gradient_level</span></p>
@@ -1880,8 +1952,7 @@
 gradient defined by <a href="#ug_vertical_gradient">ug_vertical_gradient</a>
 is effective (in m).<br> <br>
-The height levels are to be assigned in ascending order. For the
+The height levels have to be assigned in ascending order. For the
 piecewise construction of a profile of the u-component of the
-geostrophic wind component (ug) see <a href="#ug_vertical_gradient">ug_vertical_gradient</a>.<br>
-</td> </tr> <tr> <td style="vertical-align: top;"> <p><a name="ups_limit_e"></a><b>ups_limit_e</b></p>
+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&nbsp;(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>
 </td> <td style="vertical-align: top;">R</td>
 <td style="vertical-align: top;"><i>0.0</i></td>
@@ -2063,5 +2134,8 @@
 if possible (see <a href="#galilei_transformation">galilei_transformation</a>),
 in order to obtain larger
-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>
+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>),
+this parameter gives the velocity value at the sea surface, which is
+at k=nzt. The profile is then constructed from the surface down to the
+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>
 </td> <td style="vertical-align: top;">R(10)<br>
 </td> <td style="vertical-align: top;"><span style="font-style: italic;">10
@@ -2081,5 +2155,8 @@
 =
 0.0) can be assigned. The surface
-geostrophic wind is assigned by <a href="#vg_surface">vg_surface</a>.</td>
+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>),
+the profile is constructed like described above, but starting from the
+sea surface (k=nzt) down to the bottom boundary of the model. Height
+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>
 </tr> <tr> <td style="vertical-align: top;">
 <p><a name="vg_vertical_gradient_level"></a><span style="font-weight: bold;">vg_vertical_gradient_level</span></p>
@@ -2089,7 +2166,7 @@
 gradient defined by <a href="#vg_vertical_gradient">vg_vertical_gradient</a>
 is effective (in m).<br> <br>
-The height levels are to be assigned in ascending order. For the
+The height levels have to be assigned in ascending order. For the
 piecewise construction of a profile of the v-component of the
-geostrophic wind component (vg) see <a href="#vg_vertical_gradient">vg_vertical_gradient</a>.</td>
+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&nbsp;(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="wall_adjustment"></a><b>wall_adjustment</b></p>
Index: /palm/trunk/DOC/app/chapter_4.2.html
===================================================================
--- /palm/trunk/DOC/app/chapter_4.2.html	(revision 96)
+++ /palm/trunk/DOC/app/chapter_4.2.html	(revision 97)
@@ -405,6 +405,8 @@
 = <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
 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>
+= <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&nbsp;<a href="chapter_4.1.html#ocean">ocean</a>
 = <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
 the scalar</td><td style="vertical-align: top;">1/m<sup>3</sup></td><td style="vertical-align: top;">requires&nbsp;<a href="chapter_4.1.html#passive_scalar">passive_scalar</a>
+= <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&nbsp;<a href="chapter_4.1.html#ocean">ocean</a>
 = <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)
 characteristic temperature</td><td style="vertical-align: top;">K</td><td style="vertical-align: top;">only horizontal cross section
@@ -663,7 +665,7 @@
 kg/kg).</td> </tr> <tr> <td style="vertical-align: top;"><font color="#ff6600"><i>ql</i></font></td>
 <td style="vertical-align: top;">Liquid water content
-(in kg/kg).</td> </tr> <tr> <td style="vertical-align: middle;"><font color="#ff6600">s</font></td>
+(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>
 <td style="vertical-align: top;">Scalar concentration (in
-kg/m<sup>3</sup>).</td> </tr> <tr> <td style="vertical-align: middle;"><font color="#ff6600"><i>e</i></font></td>
+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>
 <td style="vertical-align: top;">Turbulent kinetic energy
 (TKE, subgrid-scale) (in m<sup>2</sup>/s<sup>2</sup>).</td>
@@ -741,9 +743,10 @@
 </tr> <tr> <td style="vertical-align: middle;"><font color="#33ff33"><i>w*s*</i></font></td>
 <td style="vertical-align: top;">Resolved vertical scalar
-concentration flux (in kg/m<sup>3</sup>)</td> </tr>
+concentration flux (in kg/m<sup>3</sup> m/s).</td> </tr>
 <tr> <td style="vertical-align: middle;"><font color="#33ff33"><i>ws</i></font></td>
 <td style="vertical-align: top;">Total vertical scalar
 concentration flux (w"s" + w*s*) (in kg/m<sup>3 </sup>m/s).</td>
-</tr> <tr> <td style="vertical-align: top;"><font color="#33ff33"><i>w*e*</i></font></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">Subgrid-scale vertical
+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>
 <td style="vertical-align: top;">Vertical flux of
 perturbation energy (resolved)</td> </tr> <tr> <td style="vertical-align: top;"><font color="#ff6600"><i>u*2</i></font></td>
@@ -856,15 +859,15 @@
 </tr> <tr> <td style="vertical-align: top;"><p><a name="disturbance_level_b"></a><b>disturbance_level_b</b></p>
 </td> <td style="vertical-align: top;">R</td>
-<td style="vertical-align: top;"><i>zu(3)</i></td>
+<td style="vertical-align: top;"><i>zu(3) or<br>zu(nz*2/3)<br>see right</i></td>
 <td style="vertical-align: top;"> <p lang="en-GB"><font face="Thorndale, serif"><font size="3">Lower
 limit of the vertical range for which random perturbations are to be
 imposed on the horizontal wind field (</font></font>in <font face="Thorndale, serif"><font size="3">m).&nbsp;
 </font></font> </p> <p><span lang="en-GB"><font face="Thorndale, serif">This
-parameter must hold the condition zu<i>(3)</i> &lt;= <b>disturbance_level_b</b>
-&lt;= <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">.
+parameter must hold the condition zu(3) &lt;= <b>disturbance_level_b</b>
+&lt;= 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">.
 Additionally, <b>disturbance_level_b</b>
 &lt;= </font></span><a href="#disturbance_level_t"><span lang="en-GB"><font face="Thorndale, serif">disturbance_level_t</font></span></a>
 <span lang="en-GB"><font face="Thorndale, serif">must
-also hold. <br> </font></span></p> <p><span lang="en-GB"><font face="Thorndale, serif">The
+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
 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">
 describes how to impose
@@ -872,5 +875,5 @@
 </font> </p> </td> </tr> <tr> <td style="vertical-align: top;"> <p><a name="disturbance_level_t"></a><b>disturbance_level_t</b></p>
 </td> <td style="vertical-align: top;">R</td>
-<td style="vertical-align: top;"><i>zu(nz/3)</i></td>
+<td style="vertical-align: top;"><i>zu(nz/3) or<br>zu(nzt-3)<br>see right</i></td>
 <td style="vertical-align: top;"> <p lang="en-GB"><font face="Thorndale, serif"><font size="3">Upper
 limit of the vertical range for which random perturbations are to be
@@ -882,5 +885,5 @@
 <span lang="en-GB"><font face="Thorndale, serif">&lt;=
 <b>disturbance_level_t</b>
-must also hold.<br> </font></span></p> <p><span lang="en-GB"><font face="Thorndale, serif">The
+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
 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">
 describes how to impose
Index: /palm/trunk/DOC/app/chapter_4.4.1.html
===================================================================
--- /palm/trunk/DOC/app/chapter_4.4.1.html	(revision 97)
+++ /palm/trunk/DOC/app/chapter_4.4.1.html	(revision 97)
@@ -0,0 +1,179 @@
+<!DOCTYPE HTML PUBLIC "-//W3C//DTD HTML 4.0 Transitional//EN">
+<html><head>
+<meta content="text/html; charset=windows-1252" http-equiv="CONTENT-TYPE"><title>PALM chapter 4.4</title>
+<meta content="StarOffice 7 (Win32)" name="GENERATOR">
+<meta content="Siegfried Raasch" name="AUTHOR"> <meta content="20041013;13430732" name="CREATED"> <meta content="20041117;11162734" name="CHANGED"> <meta content="parallel LES model" name="KEYWORDS"> <style>
+<!--
+@page { size: 21cm 29.7cm }
+-->
+</style></head>
+<body style="direction: ltr;" lang="en-US"><h3 style="line-height: 100%;">4.4.1 A minimum
+parameter set for the CBL</h3>
+
+<p style="line-height: 100%;">In this chapter a brief,
+simple and
+complete parameter set is described, which can be used to simulate a&nbsp;quasi-stationary,
+convective, atmospheric boundary layer with&nbsp; <font color="#000000">zero
+mean horizontal
+wind.</font> For evaluation purposes, cross sections and
+horizontally averaged vertical
+profiles of typical boundary layer variables
+are output at the end of the run. The run shall be carried out in
+batch mode on the IBM Regatta "hanni" of the HLRN.</p>
+<p style="line-height: 100%;">The parameter file necessary
+to carry
+out a run must be provided to the model as an input file under the
+local name <a href="chapter_3.4.html#PARIN">PARIN</a>
+and has the following contents:</p>
+<pre style="line-height: 100%;">&amp;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>&amp;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&rdquo;pt&rdquo;'</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&gt;-&gt;1'</span>,<br> <span style="font-style: italic;">'velocity variance in m&gt;2s&gt;-&gt;2'</span>,<br> <span style="font-style: italic;">'temperature variance in K&gt;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%;">The initialization
+parameters (<tt><font style="font-size: 10pt;" size="2">&amp;inipar</font></tt>)
+are located at the beginning of the file. For analysis of a
+convective boundary layer of approx. 1000 m thickness the horizontal
+size of the model domain should amount to at least 2 km x 2 km. In
+order to resolve the convective structures a grid spacing of <b>dx</b>
+=
+<b>dy</b> = <b>dz</b> = <i>50 m</i>
+is enough, since the typical
+diameter of convective plumes is more than 100 m. Thereby the
+upper array index in the two horizontal directions needs to be <b>nx</b>
+= <b>ny</b> = <i>39</i>. <font color="#000000">Since in
+each case the lower array index has the value 0, 40 grid points are
+used along both horizontal directions.</font> In the vertical
+direction
+the domain must be high enough to include the entrainment processes at
+the top of the boundary layer as well as the propagation of gravity
+waves, which were stimulated by
+the convection. However, in the stably stratified region the grid
+resolution has not necessarily to be as high as within the boundary
+layer. This can be obtained by a vertical stretching of the grid
+starting
+from 1200 m via <b>dz_stretch_level</b> = <i>1200.0
+m.</i> This saves
+grid points and computing time. <font color="#800000">T</font><font color="#000000">he
+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">)
+&hellip; m (computed by the model)</font>.</p><p style="line-height: 100%;">Fast Fourier transformations are
+calculated using the Temperton-algorithm, which -on the IBM Regatta- is
+faster than the default system-specific algorithm (from IBM essl
+library).</p><p style="line-height: 100%;">The
+initial profiles for
+wind and temperature can be assigned via <b>initializing_actions</b>
+= <span style="font-style: italic;">'set_constant_profiles'</span>.
+The wind speed, constant with
+height, amounts to <b>ug_surface</b> = <b>vg_surface</b>
+= <i>0.0 m/s</i>. In order
+to allow for a fast onset of convection, a neutral stratified layer up
+to z
+= 800 m capped by an inversion with dtheta/dz = 1K/100 m is given:
+<b>pt_vertical_gradient</b> = <i>0.0, 1.0</i>,
+<b>pt_vertical_gradient_level</b> = <i>0.0, 800.0.</i>
+The surface
+temperature, which by default amounts to 300 K, provides the fixed
+point for the temperature profile (see <a href="chapter_4.1.html#pt_surface">pt_surface</a>).
+Convection is driven by a given, near-surface sensible heat flux via <b>surface_heatflux</b>
+= <i>0.1 K m/s.</i> A given surface sensible heta flux
+requires the
+bottom boundary condition for potential temperature to be <b>bc_pt_b</b>
+=
+<span style="font-style: italic;">'neumann'</span> .
+Thus
+all initialization parameters are determined. These can not be
+changed during the run (also not for restart runs). </p>
+<p style="line-height: 100%;">Now the run parameters (<tt><font style="font-size: 10pt;" size="2">&amp;d3par</font></tt>)
+must be specified. To produce a quasi stationary boundary layer the
+simulated time should be at least one hour, i.e. <b>end_time</b>
+= <i>3600
+s.</i> To stimulate convection, the initially homogeneous (zero)
+wind
+field must be disturbed (<b>create_disturbances</b> = <i>.T.</i>).
+These perturbations should be repeated in a temporal interval of
+<b>dt_disturb</b> = <i>150.0 s</i> until the
+energy of the
+perturbations exceeds the value <b>disturbance_energy_limit</b>
+= 0.<i>01
+m<sup>2</sup>/s<sup>2</sup></i>. After
+each time step run time
+informations (e.g. size of the timestep, maximum velocities, etc.) are
+to be written to the local file <a href="chapter_3.4.html#RUN_CONTROL">RUN_CONTROL</a>
+(<b>dt_run_control</b> = <i>0.0 s</i>).</p><p style="line-height: 100%;">Instantaneous cross section data
+of vertical velocity (<span style="font-style: italic;">w</span>)
+and potential temperature (<span style="font-style: italic;">pt</span>)
+are to be output for horizontal (<span style="font-style: italic;">xy</span>)
+and vertical (<span style="font-style: italic;">xz</span>)
+cross sections, and additionally, time averaged (<span style="font-style: italic;">av</span>) vertical cross
+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
+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
+averaged data are time averaged over the last 900.0 s, where the
+temporal interval of data entering the average is 10 s: <span style="font-weight: bold;">averaging_interval</span> =
+<span style="font-style: italic;">900.0</span>, <span style="font-weight: bold;">dt_averaging_input</span> =
+<span style="font-style: italic;">10.0</span>.
+Horizontal cross sections are output for vertical levels with grid
+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
+more than one processor, cross section data are collected and output on
+PE0: <span style="font-weight: bold;">data_output_2d_on_each_pe</span>
+= <span style="font-style: italic;">.F.</span>.</p><p style="line-height: 100%;">Output
+of vertical profiles is to be done after each 900 s. The profiles shall
+be temporally averaged<font color="#000000"> over the last
+<font color="#000000">600 </font>seconds, </font>whereby
+the temporal interval of the profiles entering the average has to be
+10 s: <b>dt_dopr</b> = <i>900.0 s</i>, <b>averaging_interval_pr</b>
+=
+<i>600.0 s</i>, <b>dt_averaging_input_pr</b> =
+<i>10.0 s.</i> The temperature
+profile including the initial temperature profile (therefore <span style="font-style: italic;">'#pt'</span>),
+the subgrid scale, resolved and total vertical sensible heat flux as
+well as the variances of the vertical velocity and the potential
+temperature are to be output:&nbsp; <b>data_output_pr</b>
+= <span style="font-style: italic;">'#pt'</span><i>,
+'w"pt&rdquo;',
+'w*pt*', 'wpt', 'w*2', 'pt*2'</i>.</p><p style="line-height: 100%;">If the data output format for
+graphic software <span style="font-weight: bold;">profil</span>
+is selected (see <a href="chapter_4.2.html#data_output_format">data_output_format</a>),
+the temperature
+profile and the individual variances are to be drawn into independent
+coordinate systems, and in contrast to this all heat flux profiles are
+to
+be
+drawn into the same system: <b>cross_profiles</b> = <span style="font-style: italic;">'pt'</span><i>,
+'w"pt"w*pt*wpt', 'w*2', 'pt*2'</i>. The legend of the x
+axes of these systems is set to <b>cross_xtext</b>= <i>'pot.
+temperature in K', 'heat flux in K ms&gt;-&gt;1', 'velocity
+variance
+in m&gt;2s&gt;-&gt;2', 'temperature variance in K&gt;2'</i>.
+The profiles are to be drawn up to a height level of <b>z_max_do1d</b>
+=
+<i>1500.0 m</i>. </p>
+<p style="line-height: 100%;">Before starting the mo<font color="#000000">del
+on the parallel computer, the number of processing elements must be
+specified.</font> Since relatively few grid points are used for
+this run, choosing of e.g. 8 PEs is sufficient. By default, a 1d domain
+decomposition along x is used on the IBM-Regatta, which means that a
+virtual processor topology (grid) of 8*1 (x*y) is used. (<span style="font-weight: bold;">Note:</span> the user may
+adjust this
+default domain decomposition with the help of the parameters <a href="chapter_4.1.html#npex">npex</a>
+and <a href="chapter_4.1.html#npey">npey</a>).
+</p><p style="line-height: 100%;">Provided that the
+parameters
+file described above are set within the file </p>
+<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
+mentioned in the
+first sections of <a href="chapter_3.2.html">chapter
+3.2</a> are met, the model run can be started with the command </p>
+<p style="line-height: 100%;"><font face="Cumberland, monospace"><font style="font-size: 10pt;" size="2">mrun
+-d example -h ibmh -K parallel -X 8 -T 8 -t 1800 -q cdev -r
+&ldquo;d3# xy# xz# pr#&rdquo;</font></font></p>
+<p style="line-height: 100%;">The output files will appear
+in the
+directories </p>
+<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
+,</font></tt></blockquote>
+<p style="line-height: 100%;">while the job protocol will
+appear in
+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>.
+<br>
+&nbsp; </p>
+<hr><p style="line-height: 100%;"><br><font color="#000080"><font color="#000080"><a href="chapter_4.4.html"><font color="#000080"><img style="border: 2px solid ; width: 32px; height: 32px;" alt="" name="Grafik1" src="left.gif"></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_4.4.2.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:&nbsp;
+</i>$Id$
+<br>&nbsp; <br>
+&nbsp; </p>
+</body></html>
Index: /palm/trunk/DOC/app/chapter_4.4.2.html
===================================================================
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+<!DOCTYPE HTML PUBLIC "-//W3C//DTD HTML 4.0 Transitional//EN">
+<html><head>
+<meta content="text/html; charset=windows-1252" http-equiv="CONTENT-TYPE"><title>PALM chapter 4.4</title>
+<meta content="StarOffice 7 (Win32)" name="GENERATOR">
+<meta content="Siegfried Raasch" name="AUTHOR"> <meta content="20041013;13430732" name="CREATED"> <meta content="20041117;11162734" name="CHANGED"> <meta content="parallel LES model" name="KEYWORDS"> <style>
+<!--
+@page { size: 21cm 29.7cm }
+-->
+</style></head>
+<body style="direction: ltr;" lang="en-US"><h3 style="line-height: 100%;">4.4.2 A&nbsp;parameter set for ocean runs</h3>
+<p style="line-height: 100%;">... to be completed ...</p><p style="line-height: 100%;">In this chapter a brief,
+simple and
+complete parameter set is described, which can be used to carry out a
+model run. The presented example is available via <a href="http://www.muk.uni-hannover.de/%7Eraasch/PALM_group/INSTALL/example_p3d">example
+file</a> and can be used (together with the <a href="http://www.muk.uni-hannover.de/%7Eraasch/PALM_group/INSTALL/.mrun.config">configuration
+file</a> described in <a href="chapter_3.2.html">chapter
+3.2)</a> for the execution of a simple model run. </p>
+<p style="line-height: 100%;">This run simulates a
+quasi-stationary,
+convective, atmospheric boundary layer with&nbsp; <font color="#000000">zero
+mean horizontal
+wind.</font> For evaluation purposes, cross sections and
+horizontally averaged vertical
+profiles of typical boundary layer variables
+are output at the end of the run. The run shall be carried out in
+batch mode on the IBM Regatta "hanni" of the HLRN.</p>
+<p style="line-height: 100%;">The parameter file necessary
+to carry
+out a run must be provided to the model as an input file under the
+local name <a href="chapter_3.4.html#PARIN">PARIN</a>
+and has the following contents:</p>
+<pre style="line-height: 100%;">&amp;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>&amp;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&rdquo;pt&rdquo;'</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&gt;-&gt;1'</span>,<br> <span style="font-style: italic;">'velocity variance in m&gt;2s&gt;-&gt;2'</span>,<br> <span style="font-style: italic;">'temperature variance in K&gt;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>
+<p style="line-height: 100%;">The initialization
+parameters (<tt><font style="font-size: 10pt;" size="2">&amp;inipar</font></tt>)
+are located at the beginning of the file. For analysis of a
+convective boundary layer of approx. 1000 m thickness the horizontal
+size of the model domain should amount to at least 2 km x 2 km. In
+order to resolve the convective structures a grid spacing of <b>dx</b>
+=
+<b>dy</b> = <b>dz</b> = <i>50 m</i>
+is enough, since the typical
+diameter of convective plumes is more than 100 m. Thereby the
+upper array index in the two horizontal directions needs to be <b>nx</b>
+= <b>ny</b> = <i>39</i>. <font color="#000000">Since in
+each case the lower array index has the value 0, 40 grid points are
+used along both horizontal directions.</font> In the vertical
+direction
+the domain must be high enough to include the entrainment processes at
+the top of the boundary layer as well as the propagation of gravity
+waves, which were stimulated by
+the convection. However, in the stably stratified region the grid
+resolution has not necessarily to be as high as within the boundary
+layer. This can be obtained by a vertical stretching of the grid
+starting
+from 1200 m via <b>dz_stretch_level</b> = <i>1200.0
+m.</i> This saves
+grid points and computing time. <font color="#800000">T</font><font color="#000000">he
+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">)
+&hellip; m (computed by the model)</font>.</p><p style="line-height: 100%;">Fast Fourier transformations are
+calculated using the Temperton-algorithm, which -on the IBM Regatta- is
+faster than the default system-specific algorithm (from IBM essl
+library).</p><p style="line-height: 100%;">The
+initial profiles for
+wind and temperature can be assigned via <b>initializing_actions</b>
+= <span style="font-style: italic;">'set_constant_profiles'</span>.
+The wind speed, constant with
+height, amounts to <b>ug_surface</b> = <b>vg_surface</b>
+= <i>0.0 m/s</i>. In order
+to allow for a fast onset of convection, a neutral stratified layer up
+to z
+= 800 m capped by an inversion with dtheta/dz = 1K/100 m is given:
+<b>pt_vertical_gradient</b> = <i>0.0, 1.0</i>,
+<b>pt_vertical_gradient_level</b> = <i>0.0, 800.0.</i>
+The surface
+temperature, which by default amounts to 300 K, provides the fixed
+point for the temperature profile (see <a href="chapter_4.1.html#pt_surface">pt_surface</a>).
+Convection is driven by a given, near-surface sensible heat flux via <b>surface_heatflux</b>
+= <i>0.1 K m/s.</i> A given surface sensible heta flux
+requires the
+bottom boundary condition for potential temperature to be <b>bc_pt_b</b>
+=
+<span style="font-style: italic;">'neumann'</span> .
+Thus
+all initialization parameters are determined. These can not be
+changed during the run (also not for restart runs). </p>
+<p style="line-height: 100%;">Now the run parameters (<tt><font style="font-size: 10pt;" size="2">&amp;d3par</font></tt>)
+must be specified. To produce a quasi stationary boundary layer the
+simulated time should be at least one hour, i.e. <b>end_time</b>
+= <i>3600
+s.</i> To stimulate convection, the initially homogeneous (zero)
+wind
+field must be disturbed (<b>create_disturbances</b> = <i>.T.</i>).
+These perturbations should be repeated in a temporal interval of
+<b>dt_disturb</b> = <i>150.0 s</i> until the
+energy of the
+perturbations exceeds the value <b>disturbance_energy_limit</b>
+= 0.<i>01
+m<sup>2</sup>/s<sup>2</sup></i>. After
+each time step run time
+informations (e.g. size of the timestep, maximum velocities, etc.) are
+to be written to the local file <a href="chapter_3.4.html#RUN_CONTROL">RUN_CONTROL</a>
+(<b>dt_run_control</b> = <i>0.0 s</i>).</p><p style="line-height: 100%;">Instantaneous cross section data
+of vertical velocity (<span style="font-style: italic;">w</span>)
+and potential temperature (<span style="font-style: italic;">pt</span>)
+are to be output for horizontal (<span style="font-style: italic;">xy</span>)
+and vertical (<span style="font-style: italic;">xz</span>)
+cross sections, and additionally, time averaged (<span style="font-style: italic;">av</span>) vertical cross
+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
+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
+averaged data are time averaged over the last 900.0 s, where the
+temporal interval of data entering the average is 10 s: <span style="font-weight: bold;">averaging_interval</span> =
+<span style="font-style: italic;">900.0</span>, <span style="font-weight: bold;">dt_averaging_input</span> =
+<span style="font-style: italic;">10.0</span>.
+Horizontal cross sections are output for vertical levels with grid
+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
+more than one processor, cross section data are collected and output on
+PE0: <span style="font-weight: bold;">data_output_2d_on_each_pe</span>
+= <span style="font-style: italic;">.F.</span>.</p><p style="line-height: 100%;">Output
+of vertical profiles is to be done after each 900 s. The profiles shall
+be temporally averaged<font color="#000000"> over the last
+<font color="#000000">600 </font>seconds, </font>whereby
+the temporal interval of the profiles entering the average has to be
+10 s: <b>dt_dopr</b> = <i>900.0 s</i>, <b>averaging_interval_pr</b>
+=
+<i>600.0 s</i>, <b>dt_averaging_input_pr</b> =
+<i>10.0 s.</i> The temperature
+profile including the initial temperature profile (therefore <span style="font-style: italic;">'#pt'</span>),
+the subgrid scale, resolved and total vertical sensible heat flux as
+well as the variances of the vertical velocity and the potential
+temperature are to be output:&nbsp; <b>data_output_pr</b>
+= <span style="font-style: italic;">'#pt'</span><i>,
+'w"pt&rdquo;',
+'w*pt*', 'wpt', 'w*2', 'pt*2'</i>.</p><p style="line-height: 100%;">If the data output format for
+graphic software <span style="font-weight: bold;">profil</span>
+is selected (see <a href="chapter_4.2.html#data_output_format">data_output_format</a>),
+the temperature
+profile and the individual variances are to be drawn into independent
+coordinate systems, and in contrast to this all heat flux profiles are
+to
+be
+drawn into the same system: <b>cross_profiles</b> = <span style="font-style: italic;">'pt'</span><i>,
+'w"pt"w*pt*wpt', 'w*2', 'pt*2'</i>. The legend of the x
+axes of these systems is set to <b>cross_xtext</b>= <i>'pot.
+temperature in K', 'heat flux in K ms&gt;-&gt;1', 'velocity
+variance
+in m&gt;2s&gt;-&gt;2', 'temperature variance in K&gt;2'</i>.
+The profiles are to be drawn up to a height level of <b>z_max_do1d</b>
+=
+<i>1500.0 m</i>. </p>
+<p style="line-height: 100%;">Before starting the mo<font color="#000000">del
+on the parallel computer, the number of processing elements must be
+specified.</font> Since relatively few grid points are used for
+this run, choosing of e.g. 8 PEs is sufficient. By default, a 1d domain
+decomposition along x is used on the IBM-Regatta, which means that a
+virtual processor topology (grid) of 8*1 (x*y) is used. (<span style="font-weight: bold;">Note:</span> the user may
+adjust this
+default domain decomposition with the help of the parameters <a href="chapter_4.1.html#npex">npex</a>
+and <a href="chapter_4.1.html#npey">npey</a>).
+</p><p style="line-height: 100%;">Provided that the
+parameters
+file described above are set within the file </p>
+<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
+mentioned in the
+first sections of <a href="chapter_3.2.html">chapter
+3.2</a> are met, the model run can be started with the command </p>
+<p style="line-height: 100%;"><font face="Cumberland, monospace"><font style="font-size: 10pt;" size="2">mrun
+-d example -h ibmh -K parallel -X 8 -T 8 -t 1800 -q cdev -r
+&ldquo;d3# xy# xz# pr#&rdquo;</font></font></p>
+<p style="line-height: 100%;">The output files will appear
+in the
+directories </p>
+<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
+,</font></tt></blockquote>
+<p style="line-height: 100%;">while the job protocol will
+appear in
+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>.
+<br>
+&nbsp; </p>
+<hr><p style="line-height: 100%;"><br><font color="#000080"><font color="#000080"><a href="chapter_4.4.1.html"><font color="#000080"><img style="border: 2px solid ; width: 32px; height: 32px;" alt="" name="Grafik1" src="left.gif"></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 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:&nbsp;
+</i>$Id$
+<br>&nbsp; <br>
+&nbsp; </p>
+</body></html>
Index: /palm/trunk/DOC/app/chapter_4.4.html
===================================================================
--- /palm/trunk/DOC/app/chapter_4.4.html	(revision 96)
+++ /palm/trunk/DOC/app/chapter_4.4.html	(revision 97)
@@ -8,175 +8,20 @@
 -->
 </style></head>
-<body style="direction: ltr;" lang="en-US"><h3 style="line-height: 100%;">4.4 Example of a minimum
-parameter set</h3>
-<p style="line-height: 100%;">In this chapter a brief,
-simple and
-complete parameter set is described, which can be used to carry out a
-model run. The presented example is available via <a href="http://www.muk.uni-hannover.de/%7Eraasch/PALM_group/INSTALL/example_p3d">example
-file</a> and can be used (together with the <a href="http://www.muk.uni-hannover.de/%7Eraasch/PALM_group/INSTALL/.mrun.config">configuration
-file</a> described in <a href="chapter_3.2.html">chapter
-3.2)</a> for the execution of a simple model run. </p>
-<p style="line-height: 100%;">This run simulates a
-quasi-stationary,
+<body style="direction: ltr;" lang="en-US"><h3 style="line-height: 100%;">4.4 Examples of
+parameter sets</h3>
+<p style="line-height: 100%;">This chapter gives examples of complete
+parameter sets for a variety of model runs. These parameter files can
+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
+a description of the basic parameter settings which are generally
+required, see chapter 4.4.1, which explains the settings for a simple
+run of a quasi-stationary,
 convective, atmospheric boundary layer with&nbsp; <font color="#000000">zero
 mean horizontal
-wind.</font> For evaluation purposes, cross sections and
-horizontally averaged vertical
-profiles of typical boundary layer variables
-are output at the end of the run. The run shall be carried out in
-batch mode on the IBM Regatta "hanni" of the HLRN.</p>
-<p style="line-height: 100%;">The parameter file necessary
-to carry
-out a run must be provided to the model as an input file under the
-local name <a href="chapter_3.4.html#PARIN">PARIN</a>
-and has the following contents:</p>
-<pre style="line-height: 100%;">&amp;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>&amp;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&rdquo;pt&rdquo;'</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&gt;-&gt;1'</span>,<br> <span style="font-style: italic;">'velocity variance in m&gt;2s&gt;-&gt;2'</span>,<br> <span style="font-style: italic;">'temperature variance in K&gt;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>
-<p style="line-height: 100%;">The initialization
-parameters (<tt><font style="font-size: 10pt;" size="2">&amp;inipar</font></tt>)
-are located at the beginning of the file. For analysis of a
-convective boundary layer of approx. 1000 m thickness the horizontal
-size of the model domain should amount to at least 2 km x 2 km. In
-order to resolve the convective structures a grid spacing of <b>dx</b>
-=
-<b>dy</b> = <b>dz</b> = <i>50 m</i>
-is enough, since the typical
-diameter of convective plumes is more than 100 m. Thereby the
-upper array index in the two horizontal directions needs to be <b>nx</b>
-= <b>ny</b> = <i>39</i>. <font color="#000000">Since in
-each case the lower array index has the value 0, 40 grid points are
-used along both horizontal directions.</font> In the vertical
-direction
-the domain must be high enough to include the entrainment processes at
-the top of the boundary layer as well as the propagation of gravity
-waves, which were stimulated by
-the convection. However, in the stably stratified region the grid
-resolution has not necessarily to be as high as within the boundary
-layer. This can be obtained by a vertical stretching of the grid
-starting
-from 1200 m via <b>dz_stretch_level</b> = <i>1200.0
-m.</i> This saves
-grid points and computing time. <font color="#800000">T</font><font color="#000000">he
-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">)
-&hellip; m (computed by the model)</font>.</p><p style="line-height: 100%;">Fast Fourier transformations are
-calculated using the Temperton-algorithm, which -on the IBM Regatta- is
-faster than the default system-specific algorithm (from IBM essl
-library).</p><p style="line-height: 100%;">The
-initial profiles for
-wind and temperature can be assigned via <b>initializing_actions</b>
-= <span style="font-style: italic;">'set_constant_profiles'</span>.
-The wind speed, constant with
-height, amounts to <b>ug_surface</b> = <b>vg_surface</b>
-= <i>0.0 m/s</i>. In order
-to allow for a fast onset of convection, a neutral stratified layer up
-to z
-= 800 m capped by an inversion with dtheta/dz = 1K/100 m is given:
-<b>pt_vertical_gradient</b> = <i>0.0, 1.0</i>,
-<b>pt_vertical_gradient_level</b> = <i>0.0, 800.0.</i>
-The surface
-temperature, which by default amounts to 300 K, provides the fixed
-point for the temperature profile (see <a href="chapter_4.1.html#pt_surface">pt_surface</a>).
-Convection is driven by a given, near-surface sensible heat flux via <b>surface_heatflux</b>
-= <i>0.1 K m/s.</i> A given surface sensible heta flux
-requires the
-bottom boundary condition for potential temperature to be <b>bc_pt_b</b>
-=
-<span style="font-style: italic;">'neumann'</span> .
-Thus
-all initialization parameters are determined. These can not be
-changed during the run (also not for restart runs). </p>
-<p style="line-height: 100%;">Now the run parameters (<tt><font style="font-size: 10pt;" size="2">&amp;d3par</font></tt>)
-must be specified. To produce a quasi stationary boundary layer the
-simulated time should be at least one hour, i.e. <b>end_time</b>
-= <i>3600
-s.</i> To stimulate convection, the initially homogeneous (zero)
-wind
-field must be disturbed (<b>create_disturbances</b> = <i>.T.</i>).
-These perturbations should be repeated in a temporal interval of
-<b>dt_disturb</b> = <i>150.0 s</i> until the
-energy of the
-perturbations exceeds the value <b>disturbance_energy_limit</b>
-= 0.<i>01
-m<sup>2</sup>/s<sup>2</sup></i>. After
-each time step run time
-informations (e.g. size of the timestep, maximum velocities, etc.) are
-to be written to the local file <a href="chapter_3.4.html#RUN_CONTROL">RUN_CONTROL</a>
-(<b>dt_run_control</b> = <i>0.0 s</i>).</p><p style="line-height: 100%;">Instantaneous cross section data
-of vertical velocity (<span style="font-style: italic;">w</span>)
-and potential temperature (<span style="font-style: italic;">pt</span>)
-are to be output for horizontal (<span style="font-style: italic;">xy</span>)
-and vertical (<span style="font-style: italic;">xz</span>)
-cross sections, and additionally, time averaged (<span style="font-style: italic;">av</span>) vertical cross
-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
-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
-averaged data are time averaged over the last 900.0 s, where the
-temporal interval of data entering the average is 10 s: <span style="font-weight: bold;">averaging_interval</span> =
-<span style="font-style: italic;">900.0</span>, <span style="font-weight: bold;">dt_averaging_input</span> =
-<span style="font-style: italic;">10.0</span>.
-Horizontal cross sections are output for vertical levels with grid
-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
-more than one processor, cross section data are collected and output on
-PE0: <span style="font-weight: bold;">data_output_2d_on_each_pe</span>
-= <span style="font-style: italic;">.F.</span>.</p><p style="line-height: 100%;">Output
-of vertical profiles is to be done after each 900 s. The profiles shall
-be temporally averaged<font color="#000000"> over the last
-<font color="#000000">600 </font>seconds, </font>whereby
-the temporal interval of the profiles entering the average has to be
-10 s: <b>dt_dopr</b> = <i>900.0 s</i>, <b>averaging_interval_pr</b>
-=
-<i>600.0 s</i>, <b>dt_averaging_input_pr</b> =
-<i>10.0 s.</i> The temperature
-profile including the initial temperature profile (therefore <span style="font-style: italic;">'#pt'</span>),
-the subgrid scale, resolved and total vertical sensible heat flux as
-well as the variances of the vertical velocity and the potential
-temperature are to be output:&nbsp; <b>data_output_pr</b>
-= <span style="font-style: italic;">'#pt'</span><i>,
-'w"pt&rdquo;',
-'w*pt*', 'wpt', 'w*2', 'pt*2'</i>.</p><p style="line-height: 100%;">If the data output format for
-graphic software <span style="font-weight: bold;">profil</span>
-is selected (see <a href="chapter_4.2.html#data_output_format">data_output_format</a>),
-the temperature
-profile and the individual variances are to be drawn into independent
-coordinate systems, and in contrast to this all heat flux profiles are
-to
-be
-drawn into the same system: <b>cross_profiles</b> = <span style="font-style: italic;">'pt'</span><i>,
-'w"pt"w*pt*wpt', 'w*2', 'pt*2'</i>. The legend of the x
-axes of these systems is set to <b>cross_xtext</b>= <i>'pot.
-temperature in K', 'heat flux in K ms&gt;-&gt;1', 'velocity
-variance
-in m&gt;2s&gt;-&gt;2', 'temperature variance in K&gt;2'</i>.
-The profiles are to be drawn up to a height level of <b>z_max_do1d</b>
-=
-<i>1500.0 m</i>. </p>
-<p style="line-height: 100%;">Before starting the mo<font color="#000000">del
-on the parallel computer, the number of processing elements must be
-specified.</font> Since relatively few grid points are used for
-this run, choosing of e.g. 8 PEs is sufficient. By default, a 1d domain
-decomposition along x is used on the IBM-Regatta, which means that a
-virtual processor topology (grid) of 8*1 (x*y) is used. (<span style="font-weight: bold;">Note:</span> the user may
-adjust this
-default domain decomposition with the help of the parameters <a href="chapter_4.1.html#npex">npex</a>
-and <a href="chapter_4.1.html#npey">npey</a>).
-</p><p style="line-height: 100%;">Provided that the
-parameters
-file described above are set within the file </p>
-<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
-mentioned in the
-first sections of <a href="chapter_3.2.html">chapter
-3.2</a> are met, the model run can be started with the command </p>
-<p style="line-height: 100%;"><font face="Cumberland, monospace"><font style="font-size: 10pt;" size="2">mrun
--d example -h ibmh -K parallel -X 8 -T 8 -t 1800 -q cdev -r
-&ldquo;d3# xy# xz# pr#&rdquo;</font></font></p>
-<p style="line-height: 100%;">The output files will appear
-in the
-directories </p>
-<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
-,</font></tt></blockquote>
-<p style="line-height: 100%;">while the job protocol will
-appear in
-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>.
-<br>
+wind.</font>
+All other examples only explain those settings which are specific for
+the respective runs (e.g. only the specific ocean parameters are
+described in the parameter set for simulating ocean convection).<br>
 &nbsp; </p>
-<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:&nbsp;
+<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:&nbsp;
 </i>$Id$
 <br>&nbsp; <br>
Index: /palm/trunk/DOC/app/chapter_4.5.1.html
===================================================================
--- /palm/trunk/DOC/app/chapter_4.5.1.html	(revision 96)
+++ /palm/trunk/DOC/app/chapter_4.5.1.html	(revision 97)
@@ -163,6 +163,6 @@
 horizontal (xy) cross sections as example. The parameter settings
 described below are those of the <a href="http://www.muk.uni-hannover.de/%7Eraasch/PALM_group/INSTALL/example_p3d">example
-parameter file</a> (see <a href="chapter_4.4.html">chapter
-4.4</a>) so this parameter file can be used to retrace the
+parameter file</a> (see <a href="chapter_4.4.1.html">chapter
+4.4.1</a>) so this parameter file can be used to retrace the
 following explanations.<br><br><ol><li>Output
 of xy cross
@@ -348,6 +348,6 @@
 NetCDF dataset described here contains data of instantaneous horizontal
 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
-parameter file</a> (see <a href="chapter_4.4.html">chapter
-4.4</a>),
+parameter file</a> (see <a href="chapter_4.4.1.html">chapter
+4.4.1</a>),
 i.e. it contains section data of the w-velocity-component and of the
 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>,
Index: /palm/trunk/DOC/app/chapter_4.5.html
===================================================================
--- /palm/trunk/DOC/app/chapter_4.5.html	(revision 96)
+++ /palm/trunk/DOC/app/chapter_4.5.html	(revision 97)
@@ -1,6 +1,5 @@
 <!DOCTYPE HTML PUBLIC "-//W3C//DTD HTML 4.0 Transitional//EN">
 <html><head>
-<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>
+<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>
 <!--
 @page { size: 21cm 29.7cm }
@@ -63,5 +62,5 @@
 </p>&nbsp;For most purposes it should be sufficient to read <a href="../app/chapter_4.5.1.html">chapter 4.5.1</a>
 which explains the PALM-NetCDF-output.<hr>
-<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>
+<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>
 <p style="line-height: 100%;">&nbsp;<span style="font-style: italic;">Last
 change:</span> $Id$<br>
Index: /palm/trunk/DOC/app/chapter_4.6.html
===================================================================
--- /palm/trunk/DOC/app/chapter_4.6.html	(revision 96)
+++ /palm/trunk/DOC/app/chapter_4.6.html	(revision 97)
@@ -123,5 +123,5 @@
 </td> <td style="vertical-align: middle;" width="5%">
 <p>I</p> </td> <td style="vertical-align: middle;" width="7%"> <p>C
-* 20</p> </td> <td style="vertical-align: middle;" width="16%"> <p><i>'neumann'</i></p>
+* 20</p> </td> <td style="vertical-align: middle;" width="16%"> <p><i>'initial_gradient'</i></p>
 </td> <td style="vertical-align: middle;" width="57%">
 <p>Top boundary condition of the
@@ -156,5 +156,5 @@
 <p>Top boundary condition of the
 scalar concentration. <br> </p> </td> </tr>
-<tr> <td style="vertical-align: middle;" width="15%">
+<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.&nbsp;</td></tr><tr> <td style="vertical-align: middle;" width="15%">
 <p><a href="chapter_4.1.html#bc_uv_b"><b>bc_uv_b</b></a></p>
 </td> <td style="vertical-align: middle;" width="5%">
@@ -171,5 +171,5 @@
 <p>Top boundary condition of the
 horizontal velocity components u and v.</p> </td> </tr>
-<tr> <td style="font-weight: bold;"><a href="chapter_4.1.html#building_height">building_height</a></td>
+<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>
 <td>I</td> <td>R</td> <td style="font-style: italic;">50.0</td> <td>Height
 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>
@@ -324,5 +324,5 @@
 <p>R</p> </td> <td style="vertical-align: middle;" width="7%"> <p>R</p>
 </td> <td style="vertical-align: middle;" width="16%">
-<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">Lower
+<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
 limit of the vertical range for which random perturbations are to be
 imposed on the horizontal wind field (</font></font>in <font face="Thorndale, serif"><font size="3">m).&nbsp;
@@ -332,5 +332,5 @@
 <p>R</p> </td> <td style="vertical-align: middle;" width="7%"> <p>R</p>
 </td> <td style="vertical-align: middle;" width="16%">
-<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">Upper
+<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
 limit of the vertical range for which random perturbations are to be
 imposed on the horizontal wind field (</font></font>in <font face="Thorndale, serif"><font size="3">m). <br>
@@ -832,5 +832,5 @@
 <p><i>nz+1</i></p> </td> <td style="vertical-align: middle;" width="57%"> Limits
 the output of 3d volume data along the vertical direction (grid point
-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>
+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&nbsp;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>
 </td> <td style="vertical-align: middle;" width="5%">
 <p>I</p> </td> <td style="vertical-align: middle;" width="7%"> <p>R</p>
@@ -1194,5 +1194,7 @@
 </td> <td style="vertical-align: middle;" width="16%">
 <p><i>0.1</i></p> </td> <td style="vertical-align: middle;" width="57%"> <p>Roughness
-length (in m). <br> </p> </td> </tr> <tr>
+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
+/ 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>
+is effective (in m).</td></tr><tr>
 <td style="vertical-align: middle;" width="15%"> <p><a href="chapter_4.1.html#scalar_advec"><b>scalar_advec</b></a></p>
 </td> <td style="vertical-align: middle;" width="5%">
@@ -1369,5 +1371,6 @@
 <td>I</td> <td>C * 40</td> <td><span style="font-style: italic;">'flat'</span></td> <td>Topography
 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
-sensible heat flux at the top surface (in K m/s).</td></tr><tr>
+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
+salinity flux at the top boundary, i.e. the sea surface (in psu m/s).</td></tr><tr>
 <td style="vertical-align: middle;" width="15%"> <p><a href="chapter_4.1.html#ug_surface"><b>ug_surface</b></a></p>
 </td> <td style="vertical-align: middle;" width="5%">
Index: /palm/trunk/DOC/app/chapter_5.0.html
===================================================================
--- /palm/trunk/DOC/app/chapter_5.0.html	(revision 96)
+++ /palm/trunk/DOC/app/chapter_5.0.html	(revision 97)
@@ -200,6 +200,6 @@
 as the </font><a href="http://www.muk.uni-hannover.de/%7Eraasch/PALM_group/INSTALL/example_p3d"><font color="#000080">parameter
 file</font></a><font color="#000000">
-(described in </font><a href="chapter_4.4.html"><font color="#000080">chapter
-4.4</font></a>)<font color="#000000">. The
+(described in </font><a href="chapter_4.4.1.html"><font color="#000080">chapter
+4.4.1</font></a>)<font color="#000000">. The
 parameter file must be
 copied from the PALM working copy by<br>
Index: /palm/trunk/DOC/app/index.html
===================================================================
--- /palm/trunk/DOC/app/index.html	(revision 96)
+++ /palm/trunk/DOC/app/index.html	(revision 97)
@@ -148,5 +148,5 @@
 <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;&nbsp; 3.2b<br>For date of last change see bottom line of each page. <o:p></o:p></span></p>
+version:&nbsp;&nbsp;&nbsp;&nbsp;&nbsp;&nbsp;&nbsp;&nbsp;&nbsp;&nbsp;&nbsp;&nbsp;&nbsp;&nbsp;&nbsp;&nbsp; 3.<br>For date of last change see bottom line of each page. <o:p></o:p></span></p>
 <div style="text-align: center;" class="MsoNormal" align="center"><span style="font-family: Thorndale;">
 <hr align="center" size="2" width="100%"></span></div>
@@ -189,6 +189,5 @@
 </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
 parameters <br>
-</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
-minimum parameter set <br>
+</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;">&nbsp; <a href="chapter_4.4.1.html">4.4.1</a> A minimum parameter set for the CBL<br>&nbsp; <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">
 </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
 visualization <o:p></o:p></span></p>
Index: /palm/trunk/DOC/tec/technical_documentation.html
===================================================================
--- /palm/trunk/DOC/tec/technical_documentation.html	(revision 96)
+++ /palm/trunk/DOC/tec/technical_documentation.html	(revision 97)
@@ -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;">3.2b</span></td> </tr>
+model version:</b></td> <td><span style="font-weight: bold;">3.3</span></td> </tr>
 <tr nosave=""> <td nosave=""><b>Last
 change of this document</b>:&nbsp;</td> <td nosave=""><b>$Id$</b></td> </tr>
@@ -2311,5 +2311,16 @@
 replaced by multiplication of the inverse. For performance
 optimisation, this is done in the loop calculating the divergence
-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;">&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: <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>
+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;">&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: <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
+density is calculated from the equation of state for seawater after
+each timestep, using the algorithm proposed by Jackett et al. (2006, J.
+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, boundary_conds, buoyancy, check_parameters,
+data_output_2d, data_output_3d, diffusion_e, flow_statistics, header,
+init_grid, init_3d_model, modules, netcdf, parin, production_e,
+prognostic_equations, read_var_list, sum_up_3d_data, swap_timelevel,
+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;">&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.</td><td style="vertical-align: top;">advec_particles,
+buoyancy, calc_liquid_water_content, check_parameters, diffusion_e,
+diffusivities, header, init_cloud_physics, modules, production_e,
+prognostic_equations, 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;"></td><td style="vertical-align: top;"></td></tr>
 </tbody>
 </table>&nbsp;<b><blink>Attention:</blink></b>
Index: /palm/trunk/INSTALL/example_rc
===================================================================
--- /palm/trunk/INSTALL/example_rc	(revision 96)
+++ /palm/trunk/INSTALL/example_rc	(revision 97)
@@ -1,9 +1,9 @@
 
- *************************           ----------------------------
- * PALM 3.2b  Rev: 91    *           3D - run without 1D - prerun
- *************************           ----------------------------
-
- Date:            30-05-07           Run:       example             
- Time:            11:36:42           Run-No.:   00
+ *************************           ------------------------------------------
+ * PALM 3.3  Rev: 96M    *           atmosphere - 3D - run without 1D - prerun
+ *************************           ------------------------------------------
+
+ Date:            21-06-07           Run:       example             
+ Time:            10:04:24           Run-No.:   00
  Run on host:         ibmh
  Number of PEs:          8           Processor grid (x,y): (  8,  1) forced
@@ -67,5 +67,5 @@
 
  Bottom surface fluxes are used in diffusion terms at k=1
-       Predefined constant heatflux:    0.100 K m/s
+       Predefined constant heatflux:    0.100000 K m/s
 
 
@@ -161,5 +161,5 @@
 
        Height:         0.0     0.0  m
-       vg:            0.00    0.00  m/S
+       vg:            0.00    0.00  m/s
        Gradient:    ------    0.00  1/100s
        Gridpoint:        0       0
@@ -182,8 +182,8 @@
  -----------------------------
 
-    Disturbance impulse (u,v) every :  150.00 s
-    Disturbance amplitude           :    0.25 m/s
-    Lower disturbance level         :  125.00 m (GP    3)
-    Upper disturbance level         :  625.00 m (GP   13)
+    Disturbance impulse (u,v) every :   150.00 s
+    Disturbance amplitude           :     0.25 m/s
+    Lower disturbance level         :   125.00 m (GP    3)
+    Upper disturbance level         :   625.00 m (GP   13)
     Disturbances cease as soon as the disturbance energy exceeds 0.010 m**2/s**2
     Random number generator used    : numerical-recipes
@@ -200,283 +200,283 @@
 ------------------
 
-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
---------------------------------------------------------------------------------------------------------------------------------------------------------------------------------------------------
-  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
-  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
-  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
-  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
-  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  0.307E-15   11  32   5    4   5   2    4  26   0    0.000    0.000       0
-  0      5 00:01:40.00 20.0000D  -0.2090  -0.2207  -0.1221  0.001  1.05  ******   350.  0.106E-02  0.105E-02  0.445E-05  0.312E-15   11  32   5    4   5   2    4  26   0    0.000    0.000       0
-  0      6 00:02:00.00 20.0000D  -0.2059  -0.2220  -0.1222  0.001  1.05  ******   350.  0.106E-02  0.105E-02  0.446E-05  0.316E-15   11  32   5    4   5   2    4  26   0    0.000    0.000       0
-  0      7 00:02:20.00 20.0000D  -0.2026  -0.2230  -0.1223  0.001  1.05  ******   350.  0.106E-02  0.105E-02  0.445E-05  0.320E-15   11  32   5    4   5   2    4  26   0    0.000    0.000       0
-  0      8 00:02:40.00 20.0000D  -0.2048D -0.2236D -0.1223  0.002  1.05  ******   350.  0.211E-02  0.210E-02  0.502E-03  0.735E-13    6   0  13    4   5   2    4  26   0    0.000    0.000       0
-  0      9 00:03:00.00 20.0000D   0.3655  -0.2781  -0.1545  0.002  1.05  ******   350.  0.210E-02  0.210E-02  0.645E-05  0.629E-15    4  35   4    5   3  15    5  10  39    0.000    0.000       0
-  0     10 00:03:20.00 20.0000D   0.3644  -0.2782  -0.1534  0.002  1.05  ******   350.  0.210E-02  0.209E-02  0.643E-05  0.635E-15    4  35   4    7  14  12    5  10  39    0.000    0.000       0
-  0     11 00:03:40.00 20.0000D   0.3618  -0.2787  -0.1522  0.002  1.05  ******   350.  0.210E-02  0.209E-02  0.641E-05  0.644E-15    4  35   4    7  14  12    5  10  39    0.000    0.000       0
-  0     12 00:04:00.00 20.0000D   0.3577  -0.2783  -0.1508  0.002  1.05  ******   350.  0.209E-02  0.209E-02  0.640E-05  0.655E-15    4  35   4    7  14  12    5  10  39    0.000    0.000       0
-  0     13 00:04:20.00 20.0000D   0.3521  -0.2784  -0.1492  0.002  1.05  ******   350.  0.209E-02  0.208E-02  0.639E-05  0.666E-15    4  35   4    7  13  38    5  10  39    0.000    0.000       0
-  0     14 00:04:40.00 20.0000D   0.3451  -0.2830  -0.1475  0.002  1.05  ******   350.  0.208E-02  0.208E-02  0.639E-05  0.679E-15    4  35   4    7  13  38    5  10  39    0.000    0.000       0
-  0     15 00:05:00.00 20.0000D   0.3369D -0.2870D -0.1492  0.002  1.09  ******   400.  0.315E-02  0.314E-02  0.500E-03  0.720E-13    4  35   4    7  13  38    5  14  27    0.000    0.000       0
-  0     16 00:05:20.00 20.0000D   0.4067  -0.3928  -0.2200  0.003  1.09  ******   400.  0.314E-02  0.313E-02  0.834E-05  0.984E-15   11  16  39    7  13  12    8  21  26    0.000    0.000       0
-  0     17 00:05:40.00 20.0000D   0.4077  -0.3940  -0.2210  0.003  1.09  ******   400.  0.313E-02  0.313E-02  0.837E-05  0.100E-14   11  16  39    7  13  12    8  21  26    0.000    0.000       0
-  0     18 00:06:00.00 20.0000D   0.4066  -0.3929  -0.2218  0.003  1.09  ******   400.  0.313E-02  0.312E-02  0.843E-05  0.102E-14   11  16  39    7  13  12    8  21  26    0.000    0.000       0
-  0     19 00:06:20.00 20.0000D   0.4033  -0.3896  -0.2223  0.003  1.09  ******   400.  0.313E-02  0.312E-02  0.854E-05  0.105E-14   11  16  39    7  13  12    8  21  26    0.000    0.000       0
-  0     20 00:06:40.00 20.0000D   0.3979  -0.3842  -0.2226  0.004  1.09  ******   400.  0.313E-02  0.312E-02  0.870E-05  0.108E-14   11  16  39    7  13  12    8  21  26    0.000    0.000       0
-  0     21 00:07:00.00 20.0000D   0.3905  -0.3783  -0.2225  0.004  1.09  ******   400.  0.314E-02  0.313E-02  0.891E-05  0.112E-14   11  16  39    8  34  19    8  21  26    0.000    0.000       0
-  0     22 00:07:20.00 20.0000D  -0.3882  -0.3787  -0.2221  0.005  1.28  ******   650.  0.315E-02  0.315E-02  0.919E-05  0.116E-14    8   2  33    8  34  19    8  21  26    0.000    0.000       0
-  0     23 00:07:40.00 20.0000D  -0.3895D -0.3795D  0.2353  0.005  1.28  ******   650.  0.427E-02  0.426E-02  0.510E-03  0.750E-13    8   2  33    7  14  26    2  15  28    0.000    0.000       0
-  0     24 00:08:00.00 20.0000D  -0.4530   0.4560   0.2930  0.006  1.28  ******   650.  0.431E-02  0.429E-02  0.120E-04  0.156E-14    5  15  27   10  34  34    2  15  28    0.000    0.000       0
-  0     25 00:08:20.00 20.0000D  -0.4651   0.4519   0.3245  0.007  1.28  ******   650.  0.437E-02  0.435E-02  0.125E-04  0.164E-14    5  15  27   10  34  34    2  15  28    0.000    0.000       0
-  0     26 00:08:40.00 20.0000D  -0.4754   0.4441   0.3621  0.008  1.28  ******   650.  0.445E-02  0.444E-02  0.132E-04  0.173E-14    5  15  27   10  34  34    2  15  28    0.000    0.000       0
-  0     27 00:09:00.00 20.0000D  -0.4838   0.4329   0.4063  0.009  1.28  ******   650.  0.458E-02  0.457E-02  0.140E-04  0.184E-14    5  15  27   10  34  34    2  15  28    0.000    0.000       0
-  0     28 00:09:20.00 20.0000D  -0.4902  -0.4216   0.4578  0.010  1.28  ******   650.  0.476E-02  0.475E-02  0.151E-04  0.198E-14    5  15  27    9  21  22    2  15  28    0.000    0.000       0
-  0     29 00:09:40.00 20.0000D  -0.4950  -0.4329   0.5173  0.012  1.28  ******   650.  0.502E-02  0.501E-02  0.163E-04  0.215E-14    5  15  27    9  21  22    2  15  28    0.000    0.000       0
-  0     30 00:10:00.00 20.0000D  -0.4983D -0.4412D  0.5854  0.014  1.28  ******   650.  0.641E-02  0.639E-02  0.507E-03  0.730E-13    5  15  27    9  21  22    2  15  28    0.000    0.000       0
-  0     31 00:10:20.00 20.0000D  -0.4993   0.4599  -0.6462  0.016  1.28  -9.856   650.  0.690E-02  0.687E-02  0.215E-04  0.285E-14    6  12  30    9  19  25    1  29  23    0.000    0.000       0
-  0     32 00:10:40.00 20.0000D  -0.4953   0.4539  -0.7422  0.018  1.28  -8.537   650.  0.756E-02  0.754E-02  0.237E-04  0.315E-14    5  15  27    9  20  25    1  29  23    0.000    0.000       0
-  0     33 00:11:00.00 20.0000D  -0.4984   0.4588  -0.8473  0.021  1.28  -7.415   650.  0.848E-02  0.846E-02  0.265E-04  0.353E-14    6  11  30    9  20  25    1  29  23    0.000    0.000       0
-  0     34 00:11:20.00 20.0000D  -0.5439   0.5026  -0.9603  0.024  1.28  -6.452   650.  0.972E-02  0.970E-02  0.298E-04  0.398E-14    1  15  30    1  19  22    1  29  23    0.000    0.000       0
-  0     35 00:11:40.00 20.0000D  -0.6113   0.5752   1.1044  0.028  1.28  -5.663   650.  0.114E-01  0.114E-01  0.338E-04  0.452E-14    1  15  30    1  19  22    3  15  28    0.000    0.000       0
-  0     36 00:12:00.00 20.0000D  -0.6810   0.6539   1.2707  0.032  1.28  -5.139   650.  0.136E-01  0.136E-01  0.386E-04  0.517E-14    1  15  30    1  19  22    3  15  28    0.000    0.000       0
-  0     37 00:12:20.00 20.0000A  -0.7664   0.7360   1.4378  0.036  1.28  -4.420   650.  0.165E-01  0.165E-01  0.443E-04  0.596E-14    1  16  29    1  19  22    3  15  28    0.000    0.000       0
-  0     38 00:12:40.00 20.0000A  -0.8769   0.8160   1.6035  0.041  1.28  -3.848   650.  0.203E-01  0.203E-01  0.512E-04  0.690E-14    1  16  29    1  19  22    3  20  36    0.000    0.000       0
-  0     39 00:13:00.00 20.0000A  -0.9901   0.9084   1.8194  0.046  1.28  -3.441   650.  0.251E-01  0.250E-01  0.593E-04  0.801E-14    1  16  29    1  29  28    4  14  27    0.000    0.000       0
-  0     40 00:13:20.00 20.0000A  -1.0994   1.0182   2.1169  0.051  1.28  -3.077   650.  0.311E-01  0.311E-01  0.690E-04  0.931E-14    1  16  29    1  29  28    4  20  36    0.000    0.000       0
-  0     41 00:13:39.30 19.3000A  -1.1974   1.1241   2.3261  0.056  1.28  -2.719   650.  0.382E-01  0.381E-01  0.771E-04  0.104E-13    1  16  29    1  29  28    4  20  36    0.000    0.000       0
-  0     42 00:13:56.40 17.1000A  -1.2745   1.2164   2.6255  0.061  1.28  -2.551   650.  0.456E-01  0.456E-01  0.777E-04  0.105E-13    1  16  29    1  29  28    5  20  36    0.000    0.000       0
-  0     43 00:14:12.40 16.0000A  -1.3241   1.2858   2.8102  0.065  1.28  -2.340   650.  0.536E-01  0.536E-01  0.815E-04  0.111E-13    1  16  29    1  29  28    6  19  36    0.000    0.000       0
-  0     44 00:14:27.00 14.6000A  -1.3522   1.3367   3.0857  0.068  1.28  -2.255   650.  0.618E-01  0.618E-01  0.821E-04  0.112E-13    1  16  29    1  29  28    6  20  36    0.000    0.000       0
-  0     45 00:14:40.60 13.6000A  -1.3619   1.3696   3.3043  0.071  1.28  -2.074   650.  0.702E-01  0.702E-01  0.835E-04  0.114E-13    1  16  29    1  29  28    7  19  36    0.000    0.000       0
-  0     46 00:14:53.60 13.0000A   1.4325   1.3882   3.4638  0.073  1.29  -2.007   650.  0.788E-01  0.788E-01  0.865E-04  0.119E-13    1  31  18    1  29  28    7  20  36    0.000    0.000       0
-  0     47 00:15:05.70 12.1000A   1.5161   1.3958   3.7293  0.075  1.29  -2.032   650.  0.874E-01  0.874E-01  0.866E-04  0.119E-13    1  31  18    1  29  28    8  19  36    0.000    0.000       0
-  0     48 00:15:17.40 11.7000A   1.5815  -1.4015   3.8470  0.077  1.38  -1.953   800.  0.961E-01  0.961E-01  0.894E-04  0.123E-13    1  31  18    1   9  25    8  20  36    0.000    0.000       0
-  0     49 00:15:28.40 11.0000A   1.6308  -1.4504   4.0884  0.078  1.38  -1.899   800.  0.105E+00  0.105E+00  0.893E-04  0.123E-13    1  31  18    1   9  25    9  19  36    0.000    0.000       0
-  0     50 00:15:39.40 11.0000A   1.6631  -1.4840   4.0981  0.079  1.38  -1.888   800.  0.113E+00  0.113E+00  0.944E-04  0.130E-13    1  31  18    1   9  25   10  19  36    0.000    0.000       0
-  0     51 00:15:49.60 10.2000A   1.6810   1.5468   4.3988  0.080  1.38  -1.858   800.  0.122E+00  0.122E+00  0.920E-04  0.127E-13    1  31  18    7   2   7   10  19  36    0.000    0.000       0
-  0     52 00:15:59.80 10.2000A   1.6847   1.5305   4.3919  0.080  1.38  -1.844   800.  0.131E+00  0.130E+00  0.966E-04  0.133E-13    1  31  18    7   2   7   11  19  36    0.000    0.000       0
-  0     53 00:16:09.48  9.6800A   1.6878   1.5439   4.6501  0.081  1.38  -1.835   800.  0.139E+00  0.139E+00  0.955E-04  0.131E-13    1  30  18    1  27   0   11  19  36    0.000    0.000       0
-  0     54 00:16:19.25  9.7700A   1.6962   1.6596   4.6047  0.081  1.38  -1.853   800.  0.147E+00  0.147E+00  0.100E-03  0.138E-13    1  30  18    8   2   7   12  19  36    0.000    0.000       0
-  0     55 00:16:28.46  9.2100A   1.7048   1.6956   4.8878  0.081  1.38  -2.005   800.  0.155E+00  0.155E+00  0.981E-04  0.135E-13    1  29  18    8   2   7   11  15  27    0.000    0.000       0
-  0     56 00:16:37.78  9.3200A   1.7400   1.5901   4.8274  0.082  1.38  -1.850   800.  0.163E+00  0.163E+00  0.103E-03  0.142E-13    1  29  18    1   5   2   13  19  36    0.000    0.000       0
-  0     57 00:16:46.73  8.9500A   1.7670   1.5937   5.0281  0.082  1.38  -1.830   800.  0.171E+00  0.171E+00  0.102E-03  0.140E-13    1  29  18    1   5   2   12  15  27    0.000    0.000       0
-  0     58 00:16:55.71  8.9800A   1.7843   1.6305   5.0093  0.082  1.38  -1.812   800.  0.179E+00  0.179E+00  0.105E-03  0.145E-13    1  29  18    9   2   7   14  19  36    0.000    0.000       0
-  0     59 00:17:04.42  8.7100A   1.7943   1.6153   5.1679  0.082  1.41  -1.858   850.  0.186E+00  0.186E+00  0.105E-03  0.145E-13    1  29  18   11  16   1   13  15  27    0.000    0.000       0
-  0     60 00:17:13.15  8.7300A   1.7951   1.5585   5.1540  0.082  1.41  -1.806   850.  0.193E+00  0.193E+00  0.108E-03  0.148E-13    1  29  18    1   5   2   15  19  36    0.000    0.000       0
-  0     61 00:17:21.69  8.5400A   1.7875   1.7492   5.2705  0.082  1.41  -1.824   850.  0.200E+00  0.200E+00  0.108E-03  0.149E-13    1  29  18   12  16   1   14  15  27    0.000    0.000       0
-  0     62 00:17:30.33  8.6400A   1.7726   1.6729   5.2097  0.083  1.41  -1.868   850.  0.207E+00  0.207E+00  0.111E-03  0.153E-13    1  29  18   12  16   1   16  19  36    0.000    0.000       0
-  0     63 00:17:38.54  8.2100A   1.7512   1.7136   5.4791  0.083  1.41  -1.812   850.  0.213E+00  0.213E+00  0.108E-03  0.149E-13    1  29  18   13  16   1   14  14  28    0.000    0.000       0
-  0     64 00:17:47.28  8.7400A   1.7261   1.8291   5.1478  0.083  1.41  -1.822   850.  0.219E+00  0.219E+00  0.117E-03  0.161E-13    1  29  18   13  16   1   14  14  28    0.000    0.000       0
-  0     65 00:17:55.25  7.9700A   1.7271   1.5714   5.6455  0.083  1.41  -1.793   850.  0.225E+00  0.225E+00  0.108E-03  0.149E-13    1  29  19    1   6   2   15  14  28    0.000    0.000       0
-  0     66 00:18:03.50  8.2500A   1.7483   1.8631   5.4546  0.083  1.41  -1.776   850.  0.231E+00  0.231E+00  0.114E-03  0.156E-13    1  29  19   14  16   1   15  14  28    0.000    0.000       0
-  0     67 00:18:11.46  7.9600A   1.7639   1.7088   5.6559  0.083  1.41  -1.768   850.  0.236E+00  0.236E+00  0.112E-03  0.153E-13    1  29  19   14  16   1   16  14  28    0.000    0.000       0
-  0     68 00:18:19.33  7.8700A   1.7739   1.7265   5.7156  0.084  1.41  -1.778   850.  0.240E+00  0.240E+00  0.112E-03  0.153E-13    1  37  16   15  16   1   16  14  28    0.000    0.000       0
-  0     69 00:18:27.50  8.1700A  -1.8506   1.8104   5.5085  0.084  1.41  -1.984   850.  0.245E+00  0.245E+00  0.118E-03  0.161E-13    5  11  13   15  16   1   11  35  25    0.000    0.000       0
-  0     70 00:18:35.38  7.8800A  -1.9665   1.6657   5.7142  0.084  1.43  -1.805   900.  0.249E+00  0.249E+00  0.115E-03  0.156E-13    5  11  13    9  10  14   17  14  28    0.000    0.000       0
-  0     71 00:18:43.38  8.0000A  -2.0243   1.7641   5.6245  0.084  1.43  -1.762   900.  0.253E+00  0.253E+00  0.119E-03  0.160E-13    5  11  13   15  17   1   12  35  25    0.000    0.000       0
-  0     72 00:18:51.52  8.1400A  -2.0270  -1.6138   5.5283  0.084  1.43  -1.756   900.  0.257E+00  0.257E+00  0.122E-03  0.164E-13    5  11  13    9   4   1   12  35  25    0.000    0.000       0
-  0     73 00:18:59.44  7.9200A  -1.9748   1.7937   5.6800  0.085  1.43  -1.765   900.  0.261E+00  0.260E+00  0.120E-03  0.161E-13    5  11  13   10  10  14   13  35  25    0.000    0.000       0
-  0     74 00:19:07.41  7.9700A  -1.8731   1.8470   5.6477  0.085  1.43  -1.771   900.  0.264E+00  0.264E+00  0.122E-03  0.164E-13    5  11  13   10  10  14   13  35  25    0.000    0.000       0
-  0     75 00:19:15.34  7.9300A  -1.8088   1.7554   5.6772  0.085  1.43  -1.751   900.  0.266E+00  0.266E+00  0.123E-03  0.164E-13    6  19  34   10  10  14   14  35  25    0.000    0.000       0
-  0     76 00:19:23.21  7.8700A  -1.8408  -1.7349   5.7174  0.086  1.43  -1.758   900.  0.269E+00  0.269E+00  0.123E-03  0.164E-13   14  36  38   12   4  39   14  35  25    0.000    0.000       0
-  0     77 00:19:31.21  8.0000A  -1.9588   1.8210   5.6231  0.086  1.41  -1.760   850.  0.271E+00  0.271E+00  0.126E-03  0.168E-13    6  11  13   11  10  14   15  35  25    0.000    0.000       0
-  0     78 00:19:39.05  7.8400A  -2.0921   1.7637   5.7409  0.086  1.41  -1.733   850.  0.273E+00  0.273E+00  0.125E-03  0.165E-13    6  11  13   11  10  14   15  35  25    0.000    0.000       0
-  0     79 00:19:47.29  8.2400A  -2.1688  -1.7744   5.4629  0.086  1.41  -1.722   850.  0.275E+00  0.275E+00  0.132E-03  0.175E-13    6  11  13   13   4  39   16  35  25    0.000    0.000       0
-  0     80 00:19:55.22  7.9300A  -2.1889  -1.7066   5.6748  0.087  1.41  -1.714   850.  0.277E+00  0.276E+00  0.128E-03  0.169E-13    6  11  13   14   0   7   16  35  25    0.000    0.000       0
-  0     81 00:20:04.01  8.7900A  -2.1498  -1.6970   5.1191  0.087  1.41  -1.722   850.  0.278E+00  0.278E+00  0.143E-03  0.188E-13    6  11  13   14   0   7   17  35  25    0.000    0.000       0
-  0     82 00:20:12.31  8.3000A  -2.0439  -1.6572   5.4206  0.087  1.41  -1.690   850.  0.279E+00  0.279E+00  0.136E-03  0.179E-13    6  11  13    1   8  26   17  35  25    0.000    0.000       0
-  0     83 00:20:21.44  9.1300A  -2.1149  -1.6451   4.9296  0.088  1.41  -1.675   850.  0.280E+00  0.280E+00  0.150E-03  0.197E-13   18  15  27    1   8  26   17  35  25    0.000    0.000       0
-  0     84 00:20:30.62  9.1800A  -2.1695   1.6594   4.9006  0.088  1.41  -1.688   850.  0.281E+00  0.281E+00  0.151E-03  0.199E-13   18  15  27    3   8  16   18  35  25    0.000    0.000       0
-  0     85 00:20:40.56  9.9400A  -2.0500   1.6815   4.5251  0.089  1.41  -1.633   850.  0.281E+00  0.281E+00  0.164E-03  0.216E-13   18  15  27   10  22  25   18  35  25    0.000    0.000       0
-  0     86 00:20:50.13  9.5700A  -1.9408  -1.6689   4.7042  0.089  1.41  -1.596   850.  0.282E+00  0.281E+00  0.159E-03  0.209E-13    7  11  13   16   8  23   16  38  15    0.000    0.000       0
-  0     87 00:21:00.43 10.3000A  -2.0142  -1.7997   4.3758  0.090  1.41  -1.587   850.  0.282E+00  0.282E+00  0.172E-03  0.226E-13    7  11  13   15  39   7   16  38  15    0.000    0.000       0
-  0     88 00:21:09.99  9.5600A  -2.0167  -1.8320   4.7087  0.090  1.41  -1.596   850.  0.282E+00  0.282E+00  0.161E-03  0.212E-13    7  11  13   15  39   7   15   8  22    0.000    0.000       0
-  0     89 00:21:19.94  9.9500A  -1.9510  -1.7678   4.5214  0.091  1.41  -1.719   850.  0.282E+00  0.282E+00  0.168E-03  0.222E-13    7  11  13    1  22  28   15   8  22    0.000    0.000       0
-  0     90 00:21:29.84  9.9000A  -1.8253  -1.8361   4.5445  0.092  1.41  -1.603   850.  0.282E+00  0.282E+00  0.168E-03  0.222E-13    7  11  13    1  22  28   14  35  16    0.000    0.000       0
-  0     91 00:21:39.78  9.9400A  -1.8430  -1.8900   4.5279  0.092  1.38  -1.600   800.  0.282E+00  0.282E+00  0.170E-03  0.225E-13    1  19  35    1  22  28   16   8  22    0.000    0.000       0
-  0     92 00:21:49.65  9.8700A  -1.8498  -1.9272   4.5601  0.093  1.38  -1.612   800.  0.282E+00  0.282E+00  0.169E-03  0.224E-13    1  19  35    1  22  28   15  35  16    0.000    0.000       0
-  0     93 00:22:00.25 10.6000A  -1.8201  -1.9456   4.2321  0.094  1.38  -1.607   800.  0.282E+00  0.282E+00  0.182E-03  0.242E-13    1  19  35    1  22  28   15  35  16    0.000    0.000       0
-  0     94 00:22:10.85 10.6000A  -1.7954  -1.9438   4.2395  0.094  1.38  -1.565   800.  0.282E+00  0.282E+00  0.183E-03  0.243E-13   14   5  33    1  22  28   16  35  16    0.000    0.000       0
-  0     95 00:22:21.65 10.8000A  -1.8093   1.9326   4.1777  0.095  1.38  -1.519   800.  0.282E+00  0.282E+00  0.187E-03  0.249E-13    1  19  34    1  10  16   14  23  12    0.000    0.000       0
-  0     96 00:22:32.65 11.0000A  -1.7911   1.8969   4.0858  0.096  1.38  -1.570   800.  0.282E+00  0.281E+00  0.191E-03  0.255E-13    1  19  34    1  10  16   14  23  12    0.000    0.000       0
-  0     97 00:22:43.85 11.2000A   1.7603  -1.8590   4.0137  0.097  1.38  -1.432   800.  0.281E+00  0.281E+00  0.195E-03  0.261E-13    3  38  17    1  22  27   13  23   6    0.000    0.000       0
-  0     98 00:22:54.95 11.1000A   1.7363  -1.9231   4.0593  0.098  1.38  -1.406   800.  0.281E+00  0.281E+00  0.194E-03  0.259E-13    3  38  17    1  22  27   14  23   6    0.000    0.000       0
-  0     99 00:23:05.15 10.2000A   1.7280  -1.9681   4.4107  0.099  1.38  -1.447   800.  0.280E+00  0.280E+00  0.179E-03  0.239E-13    3  38  18    1  22  27   14  23   6    0.000    0.000       0
-  0    100 00:23:16.05 10.9000A   1.8183  -1.9898   4.1417  0.100  1.38  -1.390   800.  0.280E+00  0.280E+00  0.192E-03  0.256E-13    3  38  18    1  22  27   14  23   6    0.000    0.000       0
-  0    101 00:23:26.15 10.1000A   1.8483  -1.9896   4.4515  0.101  1.38  -1.368   800.  0.279E+00  0.279E+00  0.178E-03  0.238E-13    3  38  18    1  22  27   15  23   6    0.000    0.000       0
-  0    102 00:23:36.35 10.2000A   1.8176  -1.9679   4.4276  0.101  1.38  -1.356   800.  0.278E+00  0.278E+00  0.180E-03  0.241E-13    3  38  18    1  22  27   15  23   6    0.000    0.000       0
-  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
-  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
-  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
-  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
-  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
-  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
-  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
-  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
-  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
-  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
-  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
-  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
-  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
-  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
-  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
-  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
-  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
-  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
-  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
-  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
-  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
-  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
-  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
-  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
-  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
-  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
-  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
-  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
-  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
-  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
-  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
-  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
-  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
-  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
-  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
-  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
-  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
-  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
-  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
-  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
-  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
-  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
-  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
-  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
-  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
-  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
-  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
-  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
-  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
-  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
-  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
-  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
-  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
-  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
-  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
-  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
-  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
-  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
-  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
-  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
-  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
-  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
-  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
-  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
-  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
-  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
-  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
-  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
-  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
-  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
-  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    0.000       0
-  0    174 00:38:44.55 13.2000A  -2.2034  -2.2233   3.4144  0.101  1.43  -1.360   900.  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       0
-  0    175 00:38:58.35 13.8000A  -2.1963  -2.2318   3.2641  0.101  1.43  -1.355   900.  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       0
-  0    176 00:39:11.65 13.3000A  -2.2648  -2.1778   3.3896  0.101  1.43  -1.382   900.  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       0
-  0    177 00:39:24.75 13.1000A  -2.3021  -2.1965   3.4373  0.101  1.41  -1.350   850.  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       0
-  0    178 00:39:38.35 13.6000A  -2.2284  -2.2747   3.3046  0.101  1.41  -1.355   850.  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       0
-  0    179 00:39:51.15 12.8000A  -2.0787  -2.3151   3.5256  0.102  1.41  -1.352   850.  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       0
-  0    180 00:40:04.85 13.7000A  -2.1455  -2.2906   3.2776  0.102  1.41  -1.378   850.  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       0
-  0    181 00:40:17.85 13.0000A  -2.1908  -2.2108   3.4580  0.102  1.41  -1.446   850.  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       0
-  0    182 00:40:31.55 13.7000A  -2.1518  -2.2091   3.2922  0.102  1.41  -1.524   850.  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       0
-  0    183 00:40:44.95 13.4000A  -2.0486  -2.1944   3.3582  0.102  1.41  -1.488   850.  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       0
-  0    184 00:40:58.45 13.5000A  -2.1237  -2.1819   3.3254  0.102  1.41  -1.514   850.  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       0
-  0    185 00:41:11.85 13.4000A  -2.3131  -2.1145   3.3668  0.102  1.41  -1.464   850.  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       0
-  0    186 00:41:25.25 13.4000A  -2.3425  -2.1211   3.3569  0.102  1.41  -1.447   850.  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       0
-  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
-  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
-  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
-  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
-  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
-  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
-  0    193 00:42:54.65 11.9000A  -2.1510  -1.9858   3.7727  0.102  1.41  -1.389   850.  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       0
-  0    194 00:43:06.85 12.2000A  -2.1072  -1.9327   3.6867  0.102  1.41  -1.377   850.  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       0
-  0    195 00:43:18.25 11.4000A  -2.2110  -1.9839   3.9372  0.103  1.41  -1.381   850.  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       0
-  0    196 00:43:30.35 12.1000A  -2.3085  -1.9925   3.7169  0.103  1.41  -1.389   850.  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       0
-  0    197 00:43:42.45 12.1000A  -2.2490  -1.9568   3.7300  0.103  1.41  -1.488   850.  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       0
-  0    198 00:43:55.05 12.6000A  -2.1129  -2.1141   3.5698  0.103  1.41  -1.407   850.  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       0
-  0    199 00:44:07.45 12.4000A  -2.1621  -2.1360   3.6177  0.103  1.41  -1.389   850.  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       0
-  0    200 00:44:20.05 12.6000A  -2.1546  -2.0910   3.5651  0.103  1.41  -1.546   850.  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       0
-  0    201 00:44:32.35 12.3000A  -2.1403  -2.1132   3.6536  0.103  1.41  -1.387   850.  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       0
-  0    202 00:44:45.05 12.7000A   2.1499  -2.0291   3.5545  0.103  1.41  -1.383   850.  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       0
-  0    203 00:44:57.35 12.3000A  -2.3283  -2.2776   3.6453  0.103  1.41  -1.376   850.  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       0
-  0    204 00:45:09.95 12.6000A  -2.2436  -2.2474   3.5840  0.103  1.41  -1.389   850.  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       0
-  0    205 00:45:21.95 12.0000A  -2.4079   2.1885   3.7346  0.103  1.41  -1.347   850.  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       0
-  0    206 00:45:34.65 12.7000A  -2.2052  -2.0276   3.5531  0.103  1.41  -1.347   850.  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       0
-  0    207 00:45:47.85 13.2000A  -2.2890  -1.9557   3.4207  0.103  1.41  -1.335   850.  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       0
-  0    208 00:46:00.95 13.1000A  -2.4871  -1.9230   3.4310  0.103  1.41  -1.346   850.  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       0
-  0    209 00:46:14.55 13.6000A  -2.4420  -1.9949   3.3004  0.103  1.41  -1.331   850.  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       0
-  0    210 00:46:27.25 12.7000A  -2.3831  -2.0990   3.5476  0.103  1.41  -1.325   850.  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       0
-  0    211 00:46:40.15 12.9000A  -2.2837  -2.0889   3.4969  0.103  1.41  -1.353   850.  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       0
-  0    212 00:46:52.75 12.6000A  -2.1846  -1.9886   3.5727  0.103  1.41  -1.326   850.  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       0
-  0    213 00:47:04.65 11.9000A  -2.1743   1.9090   3.7804  0.103  1.41  -1.334   850.  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       0
-  0    214 00:47:17.05 12.4000A  -2.2333   1.9174   3.6276  0.103  1.41  -1.350   850.  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       0
-  0    215 00:47:29.25 12.2000A  -2.2272  -1.9391   3.6992  0.103  1.41  -1.362   850.  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       0
-  0    216 00:47:41.25 12.0000A  -2.2859   1.8975   3.7647  0.103  1.41  -1.350   850.  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       0
-  0    217 00:47:53.65 12.4000A  -2.2967   1.8824   3.6182  0.103  1.41  -1.374   850.  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       0
-  0    218 00:48:04.85 11.2000A  -2.3389  -1.8994   4.0037  0.103  1.41  -1.387   850.  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       0
-  0    219 00:48:16.35 11.5000A  -2.3017  -1.8955   3.9243  0.103  1.41  -1.346   850.  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       0
-  0    220 00:48:27.95 11.6000A  -2.2801  -1.8107   3.8921  0.103  1.41  -1.346   850.  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       0
-  0    221 00:48:38.95 11.0000A  -2.3353   1.8971   4.0946  0.103  1.41  -1.448   850.  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       0
-  0    222 00:48:50.35 11.4000A  -2.3480   1.9730   3.9428  0.103  1.41  -1.364   850.  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       0
-  0    223 00:49:01.15 10.8000A  -2.4248   1.9834   4.1749  0.103  1.41  -1.370   850.  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       0
-  0    224 00:49:11.95 10.8000A  -2.3497   2.0124   4.1524  0.102  1.41  -1.364   850.  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       0
-  0    225 00:49:22.55 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
-  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
-  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
-  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
-  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
-  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
-  0    231 00:50:28.45 11.2000A  -2.2268   2.0277   4.0155  0.101  1.41  -1.397   850.  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       0
-  0    232 00:50:39.95 11.5000A  -2.1561   1.9510   3.9187  0.101  1.41  -1.401   850.  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       0
-  0    233 00:50:51.25 11.3000A   2.0123   2.0613   3.9748  0.101  1.41  -1.356   850.  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       0
-  0    234 00:51:02.65 11.4000A   1.9909   1.9421   3.9506  0.100  1.41  -1.348   850.  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       0
-  0    235 00:51:13.75 11.1000A   2.0510   1.8487   4.0423  0.100  1.41  -1.358   850.  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       0
-  0    236 00:51:25.55 11.8000A   2.0598   1.8076   3.8212  0.100  1.43  -1.355   900.  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       0
-  0    237 00:51:36.85 11.3000A  -2.1549  -1.9421   3.9902  0.100  1.43  -1.364   900.  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       0
-  0    238 00:51:48.65 11.8000A  -2.3317  -1.9758   3.8232  0.099  1.43  -1.375   900.  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       0
-  0    239 00:52:00.55 11.9000A  -2.3765   1.8428   3.7772  0.099  1.43  -1.393   900.  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       0
-  0    240 00:52:12.75 12.2000A  -2.2713   1.8206   3.6794  0.099  1.43  -1.437   900.  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       0
-  0    241 00:52:24.95 12.2000A   2.2123   1.8394   3.6844  0.099  1.43  -1.442   900.  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       0
-  0    242 00:52:37.05 12.1000A  -2.2668   1.8654   3.7059  0.099  1.43  -1.438   900.  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       0
-  0    243 00:52:49.65 12.6000A  -2.2589   1.9678   3.5851  0.099  1.43  -1.476   900.  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       0
-  0    244 00:53:02.05 12.4000A  -2.0980   1.9365   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
-  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
-  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
-  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
-  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
-  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
-  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    2  12  25   17   9  14   14  19  15    0.000    0.000       0
-  0    251 00:54:27.55 12.5000A   2.0719  -1.8378   3.5940  0.099  1.41  -1.468   850.  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       0
-  0    252 00:54:39.95 12.4000A   2.0900  -1.8826   3.6288  0.099  1.41  -1.485   850.  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       0
-  0    253 00:54:52.45 12.5000A  -2.1700   1.8954   3.6132  0.099  1.43  -1.456   900.  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       0
-  0    254 00:55:04.75 12.3000A  -2.2313   1.9010   3.6714  0.099  1.43  -1.490   900.  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       0
-  0    255 00:55:17.25 12.5000A  -2.1618  -1.9215   3.5906  0.099  1.43  -1.466   900.  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       0
-  0    256 00:55:29.75 12.5000A  -2.1188  -2.0635   3.6038  0.099  1.43  -1.395   900.  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       0
-  0    257 00:55:42.25 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
-  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
-  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
-  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
-  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
-  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
-  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
-  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
-  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
-  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
-  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
-  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
-  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
-  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
-  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
-  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
-  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
-  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
-  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
-  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
-  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
-  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
+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
+-----------------------------------------------------------------------------------------------------------------------------------------------------------------------------------------------------
+  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
+  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
+  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
+  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
+  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  0.307E-15   11  32   5    4   5   2    4  26   0    0.000    0.000       0
+  0      5 00:01:40.00  20.0000D  -0.2090  -0.2207  -0.1221  0.001  1.05  ******    350.  0.106E-02  0.105E-02  0.445E-05  0.312E-15   11  32   5    4   5   2    4  26   0    0.000    0.000       0
+  0      6 00:02:00.00  20.0000D  -0.2059  -0.2220  -0.1222  0.001  1.05  ******    350.  0.106E-02  0.105E-02  0.446E-05  0.316E-15   11  32   5    4   5   2    4  26   0    0.000    0.000       0
+  0      7 00:02:20.00  20.0000D  -0.2026  -0.2230  -0.1223  0.001  1.05  ******    350.  0.106E-02  0.105E-02  0.445E-05  0.320E-15   11  32   5    4   5   2    4  26   0    0.000    0.000       0
+  0      8 00:02:40.00  20.0000D  -0.2048D -0.2236D -0.1223  0.002  1.05  ******    350.  0.211E-02  0.210E-02  0.502E-03  0.735E-13    6   0  13    4   5   2    4  26   0    0.000    0.000       0
+  0      9 00:03:00.00  20.0000D   0.3655  -0.2781  -0.1545  0.002  1.05  ******    350.  0.210E-02  0.210E-02  0.645E-05  0.629E-15    4  35   4    5   3  15    5  10  39    0.000    0.000       0
+  0     10 00:03:20.00  20.0000D   0.3644  -0.2782  -0.1534  0.002  1.05  ******    350.  0.210E-02  0.209E-02  0.643E-05  0.635E-15    4  35   4    7  14  12    5  10  39    0.000    0.000       0
+  0     11 00:03:40.00  20.0000D   0.3618  -0.2787  -0.1522  0.002  1.05  ******    350.  0.210E-02  0.209E-02  0.641E-05  0.644E-15    4  35   4    7  14  12    5  10  39    0.000    0.000       0
+  0     12 00:04:00.00  20.0000D   0.3577  -0.2783  -0.1508  0.002  1.05  ******    350.  0.209E-02  0.209E-02  0.640E-05  0.655E-15    4  35   4    7  14  12    5  10  39    0.000    0.000       0
+  0     13 00:04:20.00  20.0000D   0.3521  -0.2784  -0.1492  0.002  1.05  ******    350.  0.209E-02  0.208E-02  0.639E-05  0.666E-15    4  35   4    7  13  38    5  10  39    0.000    0.000       0
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+  0     88 00:21:09.99   9.5600A  -2.0167  -1.8320   4.7087  0.090  1.41  -1.596    850.  0.282E+00  0.282E+00  0.161E-03  0.212E-13    7  11  13   15  39   7   15   8  22    0.000    0.000       0
+  0     89 00:21:19.94   9.9500A  -1.9510  -1.7678   4.5214  0.091  1.41  -1.719    850.  0.282E+00  0.282E+00  0.168E-03  0.222E-13    7  11  13    1  22  28   15   8  22    0.000    0.000       0
+  0     90 00:21:29.84   9.9000A  -1.8253  -1.8361   4.5445  0.092  1.41  -1.603    850.  0.282E+00  0.282E+00  0.168E-03  0.222E-13    7  11  13    1  22  28   14  35  16    0.000    0.000       0
+  0     91 00:21:39.78   9.9400A  -1.8430  -1.8900   4.5279  0.092  1.38  -1.600    800.  0.282E+00  0.282E+00  0.170E-03  0.225E-13    1  19  35    1  22  28   16   8  22    0.000    0.000       0
+  0     92 00:21:49.65   9.8700A  -1.8498  -1.9272   4.5601  0.093  1.38  -1.612    800.  0.282E+00  0.282E+00  0.169E-03  0.224E-13    1  19  35    1  22  28   15  35  16    0.000    0.000       0
+  0     93 00:22:00.25  10.6000A  -1.8201  -1.9456   4.2321  0.094  1.38  -1.607    800.  0.282E+00  0.282E+00  0.182E-03  0.242E-13    1  19  35    1  22  28   15  35  16    0.000    0.000       0
+  0     94 00:22:10.85  10.6000A  -1.7954  -1.9438   4.2395  0.094  1.38  -1.565    800.  0.282E+00  0.282E+00  0.183E-03  0.243E-13   14   5  33    1  22  28   16  35  16    0.000    0.000       0
+  0     95 00:22:21.65  10.8000A  -1.8093   1.9326   4.1777  0.095  1.38  -1.519    800.  0.282E+00  0.282E+00  0.187E-03  0.249E-13    1  19  34    1  10  16   14  23  12    0.000    0.000       0
+  0     96 00:22:32.65  11.0000A  -1.7911   1.8969   4.0858  0.096  1.38  -1.570    800.  0.282E+00  0.281E+00  0.191E-03  0.255E-13    1  19  34    1  10  16   14  23  12    0.000    0.000       0
+  0     97 00:22:43.85  11.2000A   1.7603  -1.8590   4.0137  0.097  1.38  -1.432    800.  0.281E+00  0.281E+00  0.195E-03  0.261E-13    3  38  17    1  22  27   13  23   6    0.000    0.000       0
+  0     98 00:22:54.95  11.1000A   1.7363  -1.9231   4.0593  0.098  1.38  -1.406    800.  0.281E+00  0.281E+00  0.194E-03  0.259E-13    3  38  17    1  22  27   14  23   6    0.000    0.000       0
+  0     99 00:23:05.15  10.2000A   1.7280  -1.9681   4.4107  0.099  1.38  -1.447    800.  0.280E+00  0.280E+00  0.179E-03  0.239E-13    3  38  18    1  22  27   14  23   6    0.000    0.000       0
+  0    100 00:23:16.05  10.9000A   1.8183  -1.9898   4.1417  0.100  1.38  -1.390    800.  0.280E+00  0.280E+00  0.192E-03  0.256E-13    3  38  18    1  22  27   14  23   6    0.000    0.000       0
+  0    101 00:23:26.15  10.1000A   1.8483  -1.9896   4.4515  0.101  1.38  -1.368    800.  0.279E+00  0.279E+00  0.178E-03  0.238E-13    3  38  18    1  22  27   15  23   6    0.000    0.000       0
+  0    102 00:23:36.35  10.2000A   1.8176  -1.9679   4.4276  0.101  1.38  -1.356    800.  0.278E+00  0.278E+00  0.180E-03  0.241E-13    3  38  18    1  22  27   15  23   6    0.000    0.000       0
+  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
+  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
+  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
+  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
+  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
+  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
+  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
+  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
+  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
+  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
+  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
+  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
+  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
+  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
+  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
+  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
+  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
+  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
+  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
+  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
+  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
+  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
+  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
+  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
+  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
+  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
+  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
+  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
+  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
+  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
+  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
+  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
+  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
+  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
+  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
+  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
+  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
+  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
+  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
+  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
+  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
+  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
+  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
+  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
+  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
+  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
+  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
+  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
+  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
+  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
+  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
+  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
+  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
+  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
+  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
+  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
+  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
+  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
+  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
+  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
+  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
+  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
+  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
+  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
+  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
+  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
+  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
+  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
+  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
+  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
+  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    0.000       0
+  0    174 00:38:44.55  13.2000A  -2.2034  -2.2233   3.4144  0.101  1.43  -1.360    900.  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       0
+  0    175 00:38:58.35  13.8000A  -2.1963  -2.2318   3.2641  0.101  1.43  -1.355    900.  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       0
+  0    176 00:39:11.65  13.3000A  -2.2648  -2.1778   3.3896  0.101  1.43  -1.382    900.  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       0
+  0    177 00:39:24.75  13.1000A  -2.3021  -2.1965   3.4373  0.101  1.41  -1.350    850.  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       0
+  0    178 00:39:38.35  13.6000A  -2.2284  -2.2747   3.3046  0.101  1.41  -1.355    850.  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       0
+  0    179 00:39:51.15  12.8000A  -2.0787  -2.3151   3.5256  0.102  1.41  -1.352    850.  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       0
+  0    180 00:40:04.85  13.7000A  -2.1455  -2.2906   3.2776  0.102  1.41  -1.378    850.  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       0
+  0    181 00:40:17.85  13.0000A  -2.1908  -2.2108   3.4580  0.102  1.41  -1.446    850.  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       0
+  0    182 00:40:31.55  13.7000A  -2.1518  -2.2091   3.2922  0.102  1.41  -1.524    850.  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       0
+  0    183 00:40:44.95  13.4000A  -2.0486  -2.1944   3.3582  0.102  1.41  -1.488    850.  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       0
+  0    184 00:40:58.45  13.5000A  -2.1237  -2.1819   3.3254  0.102  1.41  -1.514    850.  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       0
+  0    185 00:41:11.85  13.4000A  -2.3131  -2.1145   3.3668  0.102  1.41  -1.464    850.  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       0
+  0    186 00:41:25.25  13.4000A  -2.3425  -2.1211   3.3569  0.102  1.41  -1.447    850.  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       0
+  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
+  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
+  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
+  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
+  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
+  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
+  0    193 00:42:54.65  11.9000A  -2.1510  -1.9858   3.7727  0.102  1.41  -1.389    850.  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       0
+  0    194 00:43:06.85  12.2000A  -2.1072  -1.9327   3.6867  0.102  1.41  -1.377    850.  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       0
+  0    195 00:43:18.25  11.4000A  -2.2110  -1.9839   3.9372  0.103  1.41  -1.381    850.  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       0
+  0    196 00:43:30.35  12.1000A  -2.3085  -1.9925   3.7169  0.103  1.41  -1.389    850.  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       0
+  0    197 00:43:42.45  12.1000A  -2.2490  -1.9568   3.7300  0.103  1.41  -1.488    850.  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       0
+  0    198 00:43:55.05  12.6000A  -2.1129  -2.1141   3.5698  0.103  1.41  -1.407    850.  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       0
+  0    199 00:44:07.45  12.4000A  -2.1621  -2.1360   3.6177  0.103  1.41  -1.389    850.  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       0
+  0    200 00:44:20.05  12.6000A  -2.1546  -2.0910   3.5651  0.103  1.41  -1.546    850.  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       0
+  0    201 00:44:32.35  12.3000A  -2.1403  -2.1132   3.6536  0.103  1.41  -1.387    850.  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       0
+  0    202 00:44:45.05  12.7000A   2.1499  -2.0291   3.5545  0.103  1.41  -1.383    850.  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       0
+  0    203 00:44:57.35  12.3000A  -2.3283  -2.2776   3.6453  0.103  1.41  -1.376    850.  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       0
+  0    204 00:45:09.95  12.6000A  -2.2436  -2.2474   3.5840  0.103  1.41  -1.389    850.  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       0
+  0    205 00:45:21.95  12.0000A  -2.4079   2.1885   3.7346  0.103  1.41  -1.347    850.  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       0
+  0    206 00:45:34.65  12.7000A  -2.2052  -2.0276   3.5531  0.103  1.41  -1.347    850.  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       0
+  0    207 00:45:47.85  13.2000A  -2.2890  -1.9557   3.4207  0.103  1.41  -1.335    850.  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       0
+  0    208 00:46:00.95  13.1000A  -2.4871  -1.9230   3.4310  0.103  1.41  -1.346    850.  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       0
+  0    209 00:46:14.55  13.6000A  -2.4420  -1.9949   3.3004  0.103  1.41  -1.331    850.  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       0
+  0    210 00:46:27.25  12.7000A  -2.3831  -2.0990   3.5476  0.103  1.41  -1.325    850.  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       0
+  0    211 00:46:40.15  12.9000A  -2.2837  -2.0889   3.4969  0.103  1.41  -1.353    850.  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       0
+  0    212 00:46:52.75  12.6000A  -2.1846  -1.9886   3.5727  0.103  1.41  -1.326    850.  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       0
+  0    213 00:47:04.65  11.9000A  -2.1743   1.9090   3.7804  0.103  1.41  -1.334    850.  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       0
+  0    214 00:47:17.05  12.4000A  -2.2333   1.9174   3.6276  0.103  1.41  -1.350    850.  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       0
+  0    215 00:47:29.25  12.2000A  -2.2272  -1.9391   3.6992  0.103  1.41  -1.362    850.  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       0
+  0    216 00:47:41.25  12.0000A  -2.2859   1.8975   3.7647  0.103  1.41  -1.350    850.  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       0
+  0    217 00:47:53.65  12.4000A  -2.2967   1.8824   3.6182  0.103  1.41  -1.374    850.  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       0
+  0    218 00:48:04.85  11.2000A  -2.3389  -1.8994   4.0037  0.103  1.41  -1.387    850.  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       0
+  0    219 00:48:16.35  11.5000A  -2.3017  -1.8955   3.9243  0.103  1.41  -1.346    850.  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       0
+  0    220 00:48:27.95  11.6000A  -2.2801  -1.8107   3.8921  0.103  1.41  -1.346    850.  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       0
+  0    221 00:48:38.95  11.0000A  -2.3353   1.8971   4.0946  0.103  1.41  -1.448    850.  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       0
+  0    222 00:48:50.35  11.4000A  -2.3480   1.9730   3.9428  0.103  1.41  -1.364    850.  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       0
+  0    223 00:49:01.15  10.8000A  -2.4248   1.9834   4.1749  0.103  1.41  -1.370    850.  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       0
+  0    224 00:49:11.95  10.8000A  -2.3497   2.0124   4.1524  0.102  1.41  -1.364    850.  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       0
+  0    225 00:49:22.55  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
+  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
+  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
+  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
+  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
+  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
+  0    231 00:50:28.45  11.2000A  -2.2268   2.0277   4.0155  0.101  1.41  -1.397    850.  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       0
+  0    232 00:50:39.95  11.5000A  -2.1561   1.9510   3.9187  0.101  1.41  -1.401    850.  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       0
+  0    233 00:50:51.25  11.3000A   2.0123   2.0613   3.9748  0.101  1.41  -1.356    850.  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       0
+  0    234 00:51:02.65  11.4000A   1.9909   1.9421   3.9506  0.100  1.41  -1.348    850.  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       0
+  0    235 00:51:13.75  11.1000A   2.0510   1.8487   4.0423  0.100  1.41  -1.358    850.  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       0
+  0    236 00:51:25.55  11.8000A   2.0598   1.8076   3.8212  0.100  1.43  -1.355    900.  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       0
+  0    237 00:51:36.85  11.3000A  -2.1549  -1.9421   3.9902  0.100  1.43  -1.364    900.  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       0
+  0    238 00:51:48.65  11.8000A  -2.3317  -1.9758   3.8232  0.099  1.43  -1.375    900.  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       0
+  0    239 00:52:00.55  11.9000A  -2.3765   1.8428   3.7772  0.099  1.43  -1.393    900.  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       0
+  0    240 00:52:12.75  12.2000A  -2.2713   1.8206   3.6794  0.099  1.43  -1.437    900.  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       0
+  0    241 00:52:24.95  12.2000A   2.2123   1.8394   3.6844  0.099  1.43  -1.442    900.  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       0
+  0    242 00:52:37.05  12.1000A  -2.2668   1.8654   3.7059  0.099  1.43  -1.438    900.  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       0
+  0    243 00:52:49.65  12.6000A  -2.2589   1.9678   3.5851  0.099  1.43  -1.476    900.  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       0
+  0    244 00:53:02.05  12.4000A  -2.0980   1.9365   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
+  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
+  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
+  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
+  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
+  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
+  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    2  12  25   17   9  14   14  19  15    0.000    0.000       0
+  0    251 00:54:27.55  12.5000A   2.0719  -1.8378   3.5940  0.099  1.41  -1.468    850.  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       0
+  0    252 00:54:39.95  12.4000A   2.0900  -1.8826   3.6288  0.099  1.41  -1.485    850.  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       0
+  0    253 00:54:52.45  12.5000A  -2.1700   1.8954   3.6132  0.099  1.43  -1.456    900.  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       0
+  0    254 00:55:04.75  12.3000A  -2.2313   1.9010   3.6714  0.099  1.43  -1.490    900.  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       0
+  0    255 00:55:17.25  12.5000A  -2.1618  -1.9215   3.5906  0.099  1.43  -1.466    900.  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       0
+  0    256 00:55:29.75  12.5000A  -2.1188  -2.0635   3.6038  0.099  1.43  -1.395    900.  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       0
+  0    257 00:55:42.25  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
+  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
+  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
+  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
+  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
+  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
+  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
+  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
+  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
+  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
+  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
+  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
+  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
+  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
+  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
+  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
+  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
+  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
+  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
+  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
+  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
+  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
Index: /palm/trunk/SCRIPTS/mrun
===================================================================
--- /palm/trunk/SCRIPTS/mrun	(revision 96)
+++ /palm/trunk/SCRIPTS/mrun	(revision 97)
@@ -119,4 +119,5 @@
      #                     config file, code related to ftp filetransfer
      #                     removed (incl. option -f)
+     # 19/06/07 - Siggi  - time limit for cdata jobs increased
 
 
@@ -3176,5 +3177,6 @@
                    if [[ $localhost = ibmh  ||  $localhost = ibmb ]]
                    then
-                      subjob  -d  -v  -q cdata  -X 0  -m 1000  -t 7200  archive_${frelout[$i]}
+#                      subjob  -d  -v  -q cdata  -X 0  -m 1000  -t 43200  archive_${frelout[$i]}
+                      subjob   -v  -q cdata  -X 0  -m 1000  -t 43200  archive_${frelout[$i]}
                    elif [[ $localhost = nech ]]
                    then
@@ -3300,5 +3302,5 @@
                 fi
 
-                subjob  -v  -d  -q cdata  -X 0  -m 1000  -t 7200  archive_${frelout[$i]}
+                subjob  -v  -d  -q cdata  -X 0  -m 1000  -t 43200  archive_${frelout[$i]}
                 printf "              Archiving of $tmp_data_catalog/${frelout[$i]} initiated (batch job submitted)\n"
                 file_saved=true
Index: /palm/trunk/SOURCE/CURRENT_MODIFICATIONS
===================================================================
--- /palm/trunk/SOURCE/CURRENT_MODIFICATIONS	(revision 96)
+++ /palm/trunk/SOURCE/CURRENT_MODIFICATIONS	(revision 97)
@@ -1,17 +1,8 @@
 New:
 ---
-ocean version including prognostic equation for salinity and equation of state for seawater
-+ inipar-parameters bc_sa_t, bottom_salinityflux, ocean, sa_surface, sa_vertical_gradient, sa_vertical_gradient_level, top_salinityflux
 
-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_binary
-
-New:
-eqn_state_seawater, init_ocean
 
 Changed:
 -------
-hydro_press renamed hyp, routine calc_mean_pt_profile renamed calc_mean_profile
-
-advec_particles, buoyancy, calc_liquid_water_content, init_cloud_physics, modules, prognostic_equations
 
 
@@ -19,25 +10,3 @@
 ------
 
-Bugfix: height above topography instead of height above level k=0 is used for calculating the mixing length (diffusion_e and diffusivities).
 
-diffusion_e, prognostic_equations
-
-
-
-
-To be completed (adjusted to ocean version):
-----------------
-
-boundary conditions for salinity (check_parameters)
-output of salinity profile (header)
-
-initialization of ug,vg profiles
-
-calculation of w*
-output of theta* and z_i (e.g. run_control file)
-
-default disturbance level
-
-Bott-Chlond scheme to be extended for salinity
-
-Upstream-spline scheme to be extended for salinity?????
Index: /palm/trunk/SOURCE/advec_s_bc.f90
===================================================================
--- /palm/trunk/SOURCE/advec_s_bc.f90	(revision 96)
+++ /palm/trunk/SOURCE/advec_s_bc.f90	(revision 97)
@@ -4,5 +4,6 @@
 ! Actual revisions:
 ! -----------------
-! 
+! Advection of salinity included
+! Bugfix: Error in boundary condition for TKE removed
 !
 ! Former revisions:
@@ -755,29 +756,37 @@
        ENDIF
 
+    ELSEIF ( sk_char == 'sa' )  THEN
+
+!
+!--    Salinity boundary condition at the bottom boundary.
+!--    So far, always Neumann (i.e. here zero gradient) is used
+       DO  i = nxl, nxr
+          DO  j = nys, nyn
+             sk_p(nzb-1,j,i) = sk_p(nzb,j,i)
+             sk_p(nzb-2,j,i) = sk_p(nzb,j,i)
+          ENDDO
+       ENDDO
+
+!
+!--    Salinity boundary condition at the top boundary.
+!--    Dirichlet or Neumann (zero gradient)
+       DO  i = nxl, nxr
+          DO  j = nys, nyn
+             sk_p(nzt+2,j,i)   = sk_p(nzt+1,j,i)
+             sk_p(nzt+3,j,i)   = sk_p(nzt+1,j,i)
+          ENDDO
+       ENDDO
+
     ELSEIF ( sk_char == 'q' )  THEN
 
 !
-!--    Specific humidity boundary condition at the bottom boundary
-       IF ( ibc_q_b == 0 )  THEN
-!
-!--       Dirichlet (fixed surface humidity)
-          DO  i = nxl, nxr
-             DO  j = nys, nyn
-                sk_p(nzb-1,j,i) = sk_p(nzb,j,i)
-                sk_p(nzb-2,j,i) = sk_p(nzb,j,i)
-             ENDDO
-          ENDDO
-
-       ELSE
-!
-!--       Neumann (i.e. here zero gradient)
-          DO  i = nxl, nxr
-             DO  j = nys, nyn
-                sk_p(nzb-1,j,i) = sk_p(nzb,j,i)
-                sk_p(nzb-2,j,i) = sk_p(nzb,j,i)
-             ENDDO
-          ENDDO
-
-       ENDIF
+!--    Specific humidity boundary condition at the bottom boundary.
+!--    Dirichlet (fixed surface humidity) or Neumann (i.e. zero gradient)
+       DO  i = nxl, nxr
+          DO  j = nys, nyn
+             sk_p(nzb-1,j,i) = sk_p(nzb,j,i)
+             sk_p(nzb-2,j,i) = sk_p(nzb,j,i)
+          ENDDO
+       ENDDO
 
 !
@@ -809,8 +818,12 @@
 !
 !--    TKE boundary condition at bottom and top boundary (generally Neumann)
-       sk_p(nzb-1,j,i) = sk_p(nzb,j,i)
-       sk_p(nzb-2,j,i) = sk_p(nzb,j,i)
-       sk_p(nzt+2,j,i) = sk_p(nzt+1,j,i)
-       sk_p(nzt+3,j,i) = sk_p(nzt+1,j,i)
+       DO  i = nxl, nxr
+          DO  j = nys, nyn
+             sk_p(nzb-1,j,i) = sk_p(nzb,j,i)
+             sk_p(nzb-2,j,i) = sk_p(nzb,j,i)
+             sk_p(nzt+2,j,i) = sk_p(nzt+1,j,i)
+             sk_p(nzt+3,j,i) = sk_p(nzt+1,j,i)
+          ENDDO
+       ENDDO
 
     ELSE
Index: /palm/trunk/SOURCE/buoyancy.f90
===================================================================
--- /palm/trunk/SOURCE/buoyancy.f90	(revision 96)
+++ /palm/trunk/SOURCE/buoyancy.f90	(revision 97)
@@ -4,4 +4,7 @@
 ! Actual revisions:
 ! -----------------
+! Routine reneralized to be used with temperature AND density:
+! argument theta renamed var, new argument var_reference,
+! use_pt_reference renamed use_reference,
 ! calc_mean_pt_profile renamed calc_mean_profile
 !
@@ -46,5 +49,5 @@
 ! Call for all grid points
 !------------------------------------------------------------------------------!
-    SUBROUTINE buoyancy( theta, wind_component, pr )
+    SUBROUTINE buoyancy( var, var_reference, wind_component, pr )
 
        USE arrays_3d
@@ -57,5 +60,6 @@
 
        INTEGER ::  i, j, k, pr, wind_component
-       REAL, DIMENSION(:,:,:), POINTER  ::  theta
+       REAL    ::  var_reference
+       REAL, DIMENSION(:,:,:), POINTER  ::  var
 
 
@@ -63,11 +67,12 @@
 !
 !--       Normal case: horizontal surface
-          IF ( use_pt_reference )  THEN
-             DO  i = nxl, nxr
-                DO  j = nys, nyn
-                   DO  k = nzb_s_inner(j,i)+1, nzt-1
-                      tend(k,j,i) = tend(k,j,i) + g * 0.5 * (                 &
-                        ( theta(k,j,i)   - hom(k,1,pr,0)   ) / pt_reference + &
-                        ( theta(k+1,j,i) - hom(k+1,1,pr,0) ) / pt_reference   &
+          IF ( use_reference )  THEN
+             DO  i = nxl, nxr
+                DO  j = nys, nyn
+                   DO  k = nzb_s_inner(j,i)+1, nzt-1
+                      tend(k,j,i) = tend(k,j,i) + atmos_ocean_sign * g * 0.5 * &
+                                                            (                  &
+                          ( var(k,j,i)   - hom(k,1,pr,0)   ) / var_reference + &
+                          ( var(k+1,j,i) - hom(k+1,1,pr,0) ) / var_reference   &
                                                             )
                    ENDDO
@@ -78,7 +83,8 @@
                 DO  j = nys, nyn
                    DO  k = nzb_s_inner(j,i)+1, nzt-1
-                      tend(k,j,i) = tend(k,j,i) + g * 0.5 * (                  &
-                        ( theta(k,j,i)   - hom(k,1,pr,0)   ) / hom(k,1,pr,0) + &
-                        ( theta(k+1,j,i) - hom(k+1,1,pr,0) ) / hom(k+1,1,pr,0) &
+                      tend(k,j,i) = tend(k,j,i) + atmos_ocean_sign * g * 0.5 * &
+                                                            (                  &
+                          ( var(k,j,i)   - hom(k,1,pr,0)   ) / hom(k,1,pr,0) + &
+                          ( var(k+1,j,i) - hom(k+1,1,pr,0) ) / hom(k+1,1,pr,0) &
                                                             )
                    ENDDO
@@ -136,5 +142,5 @@
 ! Call for grid point i,j
 !------------------------------------------------------------------------------!
-    SUBROUTINE buoyancy_ij( i, j, theta, wind_component, pr )
+    SUBROUTINE buoyancy_ij( i, j, var, var_reference, wind_component, pr )
 
        USE arrays_3d
@@ -147,5 +153,6 @@
 
        INTEGER ::  i, j, k, pr, wind_component
-       REAL, DIMENSION(:,:,:), POINTER  ::  theta
+       REAL    ::  var_reference
+       REAL, DIMENSION(:,:,:), POINTER  ::  var
 
 
@@ -153,17 +160,17 @@
 !
 !--       Normal case: horizontal surface
-          IF ( use_pt_reference )  THEN
-             DO  k = nzb_s_inner(j,i)+1, nzt-1
-                 tend(k,j,i) = tend(k,j,i) + g * 0.5 * (                      &
-                        ( theta(k,j,i)   - hom(k,1,pr,0)   ) / pt_reference + &
-                        ( theta(k+1,j,i) - hom(k+1,1,pr,0) ) / pt_reference   &
-                                                       )
-             ENDDO
-          ELSE
-             DO  k = nzb_s_inner(j,i)+1, nzt-1
-                 tend(k,j,i) = tend(k,j,i) + g * 0.5 * (                       &
-                        ( theta(k,j,i)   - hom(k,1,pr,0)   ) / hom(k,1,pr,0) + &
-                        ( theta(k+1,j,i) - hom(k+1,1,pr,0) ) / hom(k+1,1,pr,0) &
-                                                       )
+          IF ( use_reference )  THEN
+             DO  k = nzb_s_inner(j,i)+1, nzt-1
+                 tend(k,j,i) = tend(k,j,i) + atmos_ocean_sign * g * 0.5 * (   &
+                         ( var(k,j,i)   - hom(k,1,pr,0)   ) / var_reference + &
+                         ( var(k+1,j,i) - hom(k+1,1,pr,0) ) / var_reference   &
+                                                                          )
+             ENDDO
+          ELSE
+             DO  k = nzb_s_inner(j,i)+1, nzt-1
+                 tend(k,j,i) = tend(k,j,i) + atmos_ocean_sign * g * 0.5 * (    &
+                          ( var(k,j,i)   - hom(k,1,pr,0)   ) / hom(k,1,pr,0) + &
+                          ( var(k+1,j,i) - hom(k+1,1,pr,0) ) / hom(k+1,1,pr,0) &
+                                                                          )
              ENDDO
           ENDIF
Index: /palm/trunk/SOURCE/check_parameters.f90
===================================================================
--- /palm/trunk/SOURCE/check_parameters.f90	(revision 96)
+++ /palm/trunk/SOURCE/check_parameters.f90	(revision 97)
@@ -4,7 +4,9 @@
 ! Actual revisions:
 ! -----------------
-! Initial salinity profile is calculated.
+! Initial salinity profile is calculated, salinity boundary conditions are
+! checked,
 ! z_max_do1d is checked only in case of ocean = .f.,
-! +initial temperature profile for the ocean version,
+! +initial temperature and geostrophic velocity profiles for the ocean version,
+! use_pt_reference renamed use_reference
 !
 ! Former revisions:
@@ -163,4 +165,7 @@
           WRITE( action, '(A,A)' )  'timestep_scheme = ', timestep_scheme
        ENDIF
+       IF ( momentum_advec == 'ups-scheme' )  THEN
+          WRITE( action, '(A,A)' )  'momentum_advec = ', momentum_advec
+       ENDIF
        IF ( action /= ' ' )  THEN
           IF ( myid == 0 )  THEN
@@ -447,30 +452,64 @@
        i = 1
        gradient = 0.0
-       ug_vertical_gradient_level_ind(1) = 0
-       ug(0) = ug_surface
-       DO  k = 1, nzt+1
-          IF ( ug_vertical_gradient_level(i) < zu(k)  .AND. &
-               ug_vertical_gradient_level(i) >= 0.0 )  THEN
-             gradient = ug_vertical_gradient(i) / 100.0
-             ug_vertical_gradient_level_ind(i) = k - 1
-             i = i + 1
-             IF ( i > 10 )  THEN
-                IF ( myid == 0 )  THEN
-                   PRINT*, '+++ check_parameters: upper bound 10 of array', &
-                           ' "ug_vertical_gradient_level_ind" exceeded'
-                ENDIF
-                CALL local_stop
-             ENDIF
-          ENDIF
-          IF ( gradient /= 0.0 )  THEN
-             IF ( k /= 1 )  THEN
-                ug(k) = ug(k-1) + dzu(k) * gradient
+
+       IF ( .NOT. ocean )  THEN
+
+          ug_vertical_gradient_level_ind(1) = 0
+          ug(0) = ug_surface
+          DO  k = 1, nzt+1
+             IF ( ug_vertical_gradient_level(i) < zu(k)  .AND. &
+                  ug_vertical_gradient_level(i) >= 0.0 )  THEN
+                gradient = ug_vertical_gradient(i) / 100.0
+                ug_vertical_gradient_level_ind(i) = k - 1
+                i = i + 1
+                IF ( i > 10 )  THEN
+                   IF ( myid == 0 )  THEN
+                      PRINT*, '+++ check_parameters: upper bound 10 of array', &
+                              ' "ug_vertical_gradient_level_ind" exceeded'
+                   ENDIF
+                   CALL local_stop
+                ENDIF
+             ENDIF
+             IF ( gradient /= 0.0 )  THEN
+                IF ( k /= 1 )  THEN
+                   ug(k) = ug(k-1) + dzu(k) * gradient
+                ELSE
+                   ug(k) = ug_surface + 0.5 * dzu(k) * gradient
+                ENDIF
              ELSE
-                ug(k) = ug_surface + 0.5 * dzu(k) * gradient
-             ENDIF
-          ELSE
-             ug(k) = ug(k-1)
-          ENDIF
-       ENDDO
+                ug(k) = ug(k-1)
+             ENDIF
+          ENDDO
+
+       ELSE
+
+          ug_vertical_gradient_level_ind(1) = nzt+1
+          DO  k = nzt, 0, -1
+             IF ( ug_vertical_gradient_level(i) > zu(k)  .AND. &
+                  ug_vertical_gradient_level(i) <= 0.0 )  THEN
+                gradient = ug_vertical_gradient(i) / 100.0
+                ug_vertical_gradient_level_ind(i) = k + 1
+                i = i + 1
+                IF ( i > 10 )  THEN
+                   IF ( myid == 0 )  THEN
+                      PRINT*, '+++ check_parameters: upper bound 10 of array', &
+                              ' "ug_vertical_gradient_level_ind" exceeded'
+                   ENDIF
+                   CALL local_stop
+                ENDIF
+             ENDIF
+             IF ( gradient /= 0.0 )  THEN
+                IF ( k /= nzt )  THEN
+                   ug(k) = ug(k+1) - dzu(k+1) * gradient
+                ELSE
+                   ug(k)   = ug_surface - 0.5 * dzu(k+1) * gradient
+                   ug(k+1) = ug_surface + 0.5 * dzu(k+1) * gradient
+                ENDIF
+             ELSE
+                ug(k) = ug(k+1)
+             ENDIF
+          ENDDO
+
+       ENDIF
 
        u_init = ug
@@ -478,5 +517,5 @@
 !
 !--    In case of no given gradients for ug, choose a vanishing gradient
-       IF ( ug_vertical_gradient_level(1) == -1.0 )  THEN
+       IF ( ug_vertical_gradient_level(1) == -9999999.9 )  THEN
           ug_vertical_gradient_level(1) = 0.0
        ENDIF  
@@ -488,30 +527,64 @@
        i = 1
        gradient = 0.0
-       vg_vertical_gradient_level_ind(1) = 0
-       vg(0) = vg_surface
-       DO  k = 1, nzt+1
-          IF ( vg_vertical_gradient_level(i) < zu(k)  .AND. &
-               vg_vertical_gradient_level(i) >= 0.0 )  THEN
-             gradient = vg_vertical_gradient(i) / 100.0
-             vg_vertical_gradient_level_ind(i) = k - 1
-             i = i + 1
-             IF ( i > 10 )  THEN
-                IF ( myid == 0 )  THEN
-                   PRINT*, '+++ check_parameters: upper bound 10 of array', &
-                           ' "vg_vertical_gradient_level_ind" exceeded'
-                ENDIF
-                CALL local_stop
-             ENDIF
-          ENDIF
-          IF ( gradient /= 0.0 )  THEN
-             IF ( k /= 1 )  THEN
-                vg(k) = vg(k-1) + dzu(k) * gradient
+
+       IF ( .NOT. ocean )  THEN
+
+          vg_vertical_gradient_level_ind(1) = 0
+          vg(0) = vg_surface
+          DO  k = 1, nzt+1
+             IF ( vg_vertical_gradient_level(i) < zu(k)  .AND. &
+                  vg_vertical_gradient_level(i) >= 0.0 )  THEN
+                gradient = vg_vertical_gradient(i) / 100.0
+                vg_vertical_gradient_level_ind(i) = k - 1
+                i = i + 1
+                IF ( i > 10 )  THEN
+                   IF ( myid == 0 )  THEN
+                      PRINT*, '+++ check_parameters: upper bound 10 of array', &
+                              ' "vg_vertical_gradient_level_ind" exceeded'
+                   ENDIF
+                   CALL local_stop
+                ENDIF
+             ENDIF
+             IF ( gradient /= 0.0 )  THEN
+                IF ( k /= 1 )  THEN
+                   vg(k) = vg(k-1) + dzu(k) * gradient
+                ELSE
+                   vg(k) = vg_surface + 0.5 * dzu(k) * gradient
+                ENDIF
              ELSE
-                vg(k) = vg_surface + 0.5 * dzu(k) * gradient
-             ENDIF
-          ELSE
-             vg(k) = vg(k-1)
-          ENDIF
-       ENDDO
+                vg(k) = vg(k-1)
+             ENDIF
+          ENDDO
+
+       ELSE
+
+          vg_vertical_gradient_level_ind(1) = 0
+          DO  k = nzt, 0, -1
+             IF ( vg_vertical_gradient_level(i) > zu(k)  .AND. &
+                  vg_vertical_gradient_level(i) <= 0.0 )  THEN
+                gradient = vg_vertical_gradient(i) / 100.0
+                vg_vertical_gradient_level_ind(i) = k + 1
+                i = i + 1
+                IF ( i > 10 )  THEN
+                   IF ( myid == 0 )  THEN
+                      PRINT*, '+++ check_parameters: upper bound 10 of array', &
+                              ' "vg_vertical_gradient_level_ind" exceeded'
+                   ENDIF
+                   CALL local_stop
+                ENDIF
+             ENDIF
+             IF ( gradient /= 0.0 )  THEN
+                IF ( k /= nzt )  THEN
+                   vg(k) = vg(k+1) - dzu(k+1) * gradient
+                ELSE
+                   vg(k)   = vg_surface - 0.5 * dzu(k+1) * gradient
+                   vg(k+1) = vg_surface + 0.5 * dzu(k+1) * gradient
+                ENDIF
+             ELSE
+                vg(k) = vg(k+1)
+             ENDIF
+          ENDDO
+
+       ENDIF
 
        v_init = vg
@@ -519,5 +592,5 @@
 !
 !--    In case of no given gradients for vg, choose a vanishing gradient
-       IF ( vg_vertical_gradient_level(1) == -1.0 )  THEN
+       IF ( vg_vertical_gradient_level(1) == -9999999.9 )  THEN
           vg_vertical_gradient_level(1) = 0.0
        ENDIF
@@ -707,6 +780,19 @@
 
 !
-!-- Reference temperature to be used in buoyancy terms
-    IF ( pt_reference /= 9999999.9 )  use_pt_reference = .TRUE.
+!-- Ocean runs always use reference values in the buoyancy term. Therefore
+!-- set the reference temperature equal to the surface temperature.
+    IF ( ocean  .AND.  pt_reference == 9999999.9 )  pt_reference = pt_surface
+
+!
+!-- Reference value has to be used in buoyancy terms
+    IF ( pt_reference /= 9999999.9 )  use_reference = .TRUE.
+
+!
+!-- Sign of buoyancy/stability terms
+    IF ( ocean )  atmos_ocean_sign = -1.0
+
+!
+!-- Ocean version is using flux boundary conditions at the top
+    IF ( ocean )  use_top_fluxes = .TRUE.
 
 !
@@ -1020,4 +1106,12 @@
 
        IF ( top_salinityflux == 9999999.9 )  constant_top_salinityflux = .FALSE.
+       IF ( ibc_sa_t == 1  .AND.   top_salinityflux == 9999999.9 )  THEN
+          IF ( myid == 0 )  THEN
+             PRINT*, '+++ check_parameters:'
+             PRINT*, '    boundary_condition: bc_sa_t = ', bc_sa_t
+             PRINT*, '    requires to set top_salinityflux '
+          ENDIF
+          CALL local_stop
+       ENDIF
 
 !
@@ -2474,7 +2568,12 @@
 !
 !-- Determine upper and lower hight level indices for random perturbations
-    IF ( disturbance_level_b == -1.0 )  THEN
-       disturbance_level_b     = zu(nzb+3)
-       disturbance_level_ind_b = nzb + 3
+    IF ( disturbance_level_b == -9999999.9 )  THEN
+       IF ( ocean ) THEN
+          disturbance_level_b     = zu((nzt*2)/3)
+          disturbance_level_ind_b = ( nzt * 2 ) / 3
+       ELSE
+          disturbance_level_b     = zu(nzb+3)
+          disturbance_level_ind_b = nzb + 3
+       ENDIF
     ELSEIF ( disturbance_level_b < zu(3) )  THEN
        IF ( myid == 0 )  PRINT*, '+++ check_parameters:  disturbance_level_b=',&
@@ -2496,7 +2595,12 @@
     ENDIF
 
-    IF ( disturbance_level_t == -1.0 )  THEN
-       disturbance_level_t     = zu(nzt/3)
-       disturbance_level_ind_t = nzt / 3
+    IF ( disturbance_level_t == -9999999.9 )  THEN
+       IF ( ocean )  THEN
+          disturbance_level_t     = zu(nzt-3)
+          disturbance_level_ind_t = nzt - 3
+       ELSE
+          disturbance_level_t     = zu(nzt/3)
+          disturbance_level_ind_t = nzt / 3
+       ENDIF
     ELSEIF ( disturbance_level_t > zu(nzt-2) )  THEN
        IF ( myid == 0 )  PRINT*, '+++ check_parameters:  disturbance_level_t=',&
Index: /palm/trunk/SOURCE/diffusion_e.f90
===================================================================
--- /palm/trunk/SOURCE/diffusion_e.f90	(revision 96)
+++ /palm/trunk/SOURCE/diffusion_e.f90	(revision 97)
@@ -8,4 +8,6 @@
 ! This is also a bugfix, because the height above the topography is now
 ! used instead of the height above level k=0.
+! theta renamed var, dpt_dz renamed dvar_dz, +new argument var_reference
+! use_pt_reference renamed use_reference
 !
 ! Former revisions:
@@ -50,6 +52,6 @@
 ! Call for all grid points
 !------------------------------------------------------------------------------!
-    SUBROUTINE diffusion_e( ddzu, dd2zu, ddzw, diss, e, km, l_grid, theta, &
-                            rif, tend, zu, zw )
+    SUBROUTINE diffusion_e( ddzu, dd2zu, ddzw, diss, e, km, l_grid, var, &
+                            var_reference, rif, tend, zu, zw )
 
        USE control_parameters
@@ -61,10 +63,10 @@
 
        INTEGER ::  i, j, k
-       REAL            ::  dpt_dz, l_stable, phi_m
+       REAL            ::  dvar_dz, l_stable, phi_m, var_reference
        REAL            ::  ddzu(1:nzt+1), dd2zu(1:nzt), ddzw(1:nzt+1), &
                            l_grid(1:nzt), zu(0:nzt+1), zw(0:nzt+1)
        REAL, DIMENSION(nzb:nzt+1,nys-1:nyn+1,nxl-1:nxr+1) :: diss, tend
        REAL, DIMENSION(:,:), POINTER   ::  rif
-       REAL, DIMENSION(:,:,:), POINTER ::  e, km, theta
+       REAL, DIMENSION(:,:,:), POINTER ::  e, km, var
        REAL, DIMENSION(nzb+1:nzt,nys:nyn) ::  dissipation, l, ll
  
@@ -73,5 +75,5 @@
 !--    This if clause must be outside the k-loop because otherwise
 !--    runtime errors occur with -C hopt on NEC
-       IF ( use_pt_reference )  THEN
+       IF ( use_reference )  THEN
 
           DO  i = nxl, nxr
@@ -91,8 +93,9 @@
 !
 !--                Calculate the mixing length (for dissipation)
-                   dpt_dz = ( theta(k+1,j,i) - theta(k-1,j,i) ) * dd2zu(k)
-                   IF ( dpt_dz > 0.0 ) THEN
+                   dvar_dz = atmos_ocean_sign * &
+                             ( var(k+1,j,i) - var(k-1,j,i) ) * dd2zu(k)
+                   IF ( dvar_dz > 0.0 ) THEN
                       l_stable = 0.76 * SQRT( e(k,j,i) ) / &
-                                        SQRT( g / pt_reference * dpt_dz ) + 1E-5
+                                 SQRT( g / var_reference * dvar_dz ) + 1E-5
                    ELSE
                       l_stable = l_grid(k)
@@ -180,8 +183,9 @@
 !
 !--                Calculate the mixing length (for dissipation)
-                   dpt_dz = ( theta(k+1,j,i) - theta(k-1,j,i) ) * dd2zu(k)
-                   IF ( dpt_dz > 0.0 ) THEN
+                   dvar_dz = atmos_ocean_sign * &
+                             ( var(k+1,j,i) - var(k-1,j,i) ) * dd2zu(k)
+                   IF ( dvar_dz > 0.0 ) THEN
                       l_stable = 0.76 * SQRT( e(k,j,i) ) / &
-                                        SQRT( g / theta(k,j,i) * dpt_dz ) + 1E-5
+                                        SQRT( g / var(k,j,i) * dvar_dz ) + 1E-5
                    ELSE
                       l_stable = l_grid(k)
@@ -270,5 +274,5 @@
 !------------------------------------------------------------------------------!
     SUBROUTINE diffusion_e_ij( i, j, ddzu, dd2zu, ddzw, diss, e, km, l_grid, &
-                               theta, rif, tend, zu, zw )
+                               var, var_reference, rif, tend, zu, zw )
 
        USE control_parameters
@@ -280,10 +284,10 @@
 
        INTEGER         ::  i, j, k
-       REAL            ::  dpt_dz, l_stable, phi_m
+       REAL            ::  dvar_dz, l_stable, phi_m, var_reference
        REAL            ::  ddzu(1:nzt+1), dd2zu(1:nzt), ddzw(1:nzt+1), &
                            l_grid(1:nzt), zu(0:nzt+1), zw(0:nzt+1)
        REAL, DIMENSION(nzb:nzt+1,nys-1:nyn+1,nxl-1:nxr+1) ::  diss, tend
        REAL, DIMENSION(:,:), POINTER   ::  rif
-       REAL, DIMENSION(:,:,:), POINTER ::  e, km, theta
+       REAL, DIMENSION(:,:,:), POINTER ::  e, km, var
        REAL, DIMENSION(nzb+1:nzt)    ::  dissipation, l, ll
 
@@ -303,12 +307,13 @@
 !--    Calculate the mixing length (for dissipation)
        DO  k = nzb_s_inner(j,i)+1, nzt
-          dpt_dz = ( theta(k+1,j,i) - theta(k-1,j,i) ) * dd2zu(k)
-          IF ( dpt_dz > 0.0 ) THEN
-             IF ( use_pt_reference )  THEN
+          dvar_dz = atmos_ocean_sign * &
+                    ( var(k+1,j,i) - var(k-1,j,i) ) * dd2zu(k)
+          IF ( dvar_dz > 0.0 ) THEN
+             IF ( use_reference )  THEN
                 l_stable = 0.76 * SQRT( e(k,j,i) ) / &
-                                  SQRT( g / pt_reference * dpt_dz ) + 1E-5
+                                  SQRT( g / var_reference * dvar_dz ) + 1E-5
              ELSE
                 l_stable = 0.76 * SQRT( e(k,j,i) ) / &
-                                  SQRT( g / theta(k,j,i) * dpt_dz ) + 1E-5
+                                  SQRT( g / var(k,j,i) * dvar_dz ) + 1E-5
              ENDIF
           ELSE
Index: /palm/trunk/SOURCE/diffusivities.f90
===================================================================
--- /palm/trunk/SOURCE/diffusivities.f90	(revision 96)
+++ /palm/trunk/SOURCE/diffusivities.f90	(revision 97)
@@ -1,3 +1,3 @@
- SUBROUTINE diffusivities( theta )
+ SUBROUTINE diffusivities( var, var_reference )
 
 !------------------------------------------------------------------------------!
@@ -7,4 +7,6 @@
 ! This is also a bugfix, because the height above the topography is now
 ! used instead of the height above level k=0.
+! theta renamed var, dpt_dz renamed dvar_dz, +new argument var_reference
+! use_pt_reference renamed use_reference
 ! 
 ! Former revisions:
@@ -41,7 +43,9 @@
     INTEGER ::  i, j, k, omp_get_thread_num, sr, tn
 
-    REAL    ::  dpt_dz, l_stable, phi_m = 1.0
+    REAL    ::  dvar_dz, l_stable, var_reference
 
-    REAL    ::  theta(nzb:nzt+1,nys-1:nyn+1,nxl-1:nxr+1)
+    REAL, SAVE ::  phi_m = 1.0
+
+    REAL    ::  var(nzb:nzt+1,nys-1:nyn+1,nxl-1:nxr+1)
 
     REAL, DIMENSION(1:nzt) ::  l, ll, sqrt_e
@@ -58,5 +62,5 @@
 !
 !-- Compute the turbulent diffusion coefficient for momentum
-    !$OMP PARALLEL PRIVATE (dpt_dz,i,j,k,l,ll,l_stable,phi_m,sqrt_e,sr,tn)
+    !$OMP PARALLEL PRIVATE (dvar_dz,i,j,k,l,ll,l_stable,phi_m,sqrt_e,sr,tn)
 !$  tn = omp_get_thread_num()
 
@@ -94,12 +98,13 @@
 !--       Determine the mixing length
           DO  k = nzb_s_inner(j,i)+1, nzt
-             dpt_dz = ( theta(k+1,j,i) - theta(k-1,j,i) ) * dd2zu(k)
-             IF ( dpt_dz > 0.0 ) THEN
-                IF ( use_pt_reference )  THEN
+             dvar_dz = atmos_ocean_sign * &  ! inverse effect of pt/rho gradient
+                       ( var(k+1,j,i) - var(k-1,j,i) ) * dd2zu(k)
+             IF ( dvar_dz > 0.0 ) THEN
+                IF ( use_reference )  THEN
                    l_stable = 0.76 * sqrt_e(k) / &
-                                     SQRT( g / pt_reference * dpt_dz ) + 1E-5
+                                     SQRT( g / var_reference * dvar_dz ) + 1E-5
                 ELSE
                    l_stable = 0.76 * sqrt_e(k) / &
-                                     SQRT( g / theta(k,j,i) * dpt_dz ) + 1E-5
+                                     SQRT( g / var(k,j,i) * dvar_dz ) + 1E-5
                 ENDIF
              ELSE
Index: /palm/trunk/SOURCE/eqn_state_seawater.f90
===================================================================
--- /palm/trunk/SOURCE/eqn_state_seawater.f90	(revision 96)
+++ /palm/trunk/SOURCE/eqn_state_seawater.f90	(revision 97)
@@ -8,5 +8,5 @@
 ! Former revisions:
 ! -----------------
-! $Id:$
+! $Id$
 !
 ! Initial revision
@@ -18,4 +18,6 @@
 ! salinity, and pressure.
 ! For coefficients see Jackett et al., 2006: J. Atm. Ocean Tech.
+! eqn_state_seawater calculates the potential density referred at hyp(0).
+! eqn_state_seawater_func calculates density.
 !------------------------------------------------------------------------------!
 
@@ -70,8 +72,8 @@
        DO  i = nxl, nxr
           DO  j = nys, nyn
-             DO  k = nzb_u_inner(j,i)+1, nzt
+             DO  k = nzb_s_inner(j,i)+1, nzt
 !
 !--             Pressure is needed in dbar
-                p1 = hyp(k) * 1E-4
+                p1 = hyp(0) * 1E-4
                 p2 = p1 * p1
                 p3 = p2 * p1
@@ -102,4 +104,8 @@
 
              ENDDO
+!
+!--          Neumann conditions are assumed at bottom and top boundary
+             rho(nzt+1,j,i)            = rho(nzt,j,i)
+             rho(nzb_s_inner(j,i),j,i) = rho(nzb_s_inner(j,i)+1,j,i)
           ENDDO
        ENDDO
@@ -122,8 +128,8 @@
        REAL ::  p1, p2, p3, pt1, pt2, pt3, pt4, sa1, sa15, sa2
 
-       DO  k = nzb_u_inner(j,i)+1, nzt
+       DO  k = nzb_s_inner(j,i)+1, nzt
 !
 !--       Pressure is needed in dbar
-          p1 = hyp(k) * 1E-4
+          p1 = hyp(0) * 1E-4
           p2 = p1 * p1
           p3 = p2 * p1
@@ -152,4 +158,8 @@
                        )
        ENDDO
+!
+!--    Neumann conditions are assumed at bottom and top boundary
+       rho(nzt+1,j,i)            = rho(nzt,j,i)
+       rho(nzb_s_inner(j,i),j,i) = rho(nzb_s_inner(j,i)+1,j,i)
 
     END SUBROUTINE eqn_state_seawater_ij
Index: /palm/trunk/SOURCE/flow_statistics.f90
===================================================================
--- /palm/trunk/SOURCE/flow_statistics.f90	(revision 96)
+++ /palm/trunk/SOURCE/flow_statistics.f90	(revision 97)
@@ -5,6 +5,6 @@
 ! -----------------
 ! Statistics for ocean version (salinity, density) added,
-! calculation of Deardorff velocity scale adjusted to be used with the ocean
-! version (HAS STILL TO BE COMPLETED!!!)
+! calculation of z_i and Deardorff velocity scale adjusted to be used with
+! the ocean version
 !
 ! Former revisions:
@@ -558,5 +558,5 @@
 !
 !--             Salinity flux and density (density does not belong to here,
-!--             but so far there is no suitable place to calculate)
+!--             but so far there is no other suitable place to calculate)
                 IF ( ocean )  THEN
                    pts = 0.5 * ( sa(k,j,i)   - hom(k,1,23,sr) + &
@@ -611,4 +611,8 @@
 
 !
+!--    Density at top follows Neumann condition
+       IF ( ocean )  sums_l(nzt+1,64,tn) = sums_l(nzt,64,tn)
+
+!
 !--    Divergence of vertical flux of resolved scale energy and pressure
 !--    fluctuations. First calculate the products, then the divergence.
@@ -709,10 +713,10 @@
 !
 !--       Fluxes at the surface must be zero (e.g. due to the Prandtl-layer)
-          sums(nzb,58) = 0.0
-          sums(nzb,59) = 0.0
-          sums(nzb,60) = 0.0
-          sums(nzb,61) = 0.0
-          sums(nzb,62) = 0.0
-          sums(nzb,63) = 0.0
+          sums_l(nzb,58,tn) = 0.0
+          sums_l(nzb,59,tn) = 0.0
+          sums_l(nzb,60,tn) = 0.0
+          sums_l(nzb,61,tn) = 0.0
+          sums_l(nzb,62,tn) = 0.0
+          sums_l(nzb,63,tn) = 0.0
 
        ENDIF
@@ -857,5 +861,21 @@
        z_i(1) = 0.0
        first = .TRUE.
-!       IF ( .NOT. ocean )  THEN
+       IF ( ocean )  THEN
+          DO  k = nzt, nzb+1, -1
+             IF ( first .AND. hom(k,1,18,sr) < 0.0 )  THEN
+                first = .FALSE.
+                height = zw(k)
+             ENDIF
+             IF ( hom(k,1,18,sr) < 0.0  .AND. &
+                  hom(k-1,1,18,sr) > hom(k,1,18,sr) )  THEN
+                IF ( zw(k) < 1.5 * height )  THEN
+                   z_i(1) = zw(k)
+                ELSE
+                   z_i(1) = height
+                ENDIF
+                EXIT
+             ENDIF
+          ENDDO
+       ELSE
           DO  k = nzb, nzt-1
              IF ( first .AND. hom(k,1,18,sr) < 0.0 )  THEN
@@ -873,19 +893,28 @@
              ENDIF
           ENDDO
-!       ELSE
-!       ENDIF
-
-!
-!--    Second scheme: Starting from the top model boundary, look for the first 
-!--    characteristic kink in the temperature profile, where the originally 
-!--    stable stratification notably weakens.
+       ENDIF
+
+!
+!--    Second scheme: Starting from the top/bottom model boundary, look for
+!--    the first characteristic kink in the temperature profile, where the
+!--    originally stable stratification notably weakens.
        z_i(2) = 0.0
-       DO  k = nzt-1, nzb+1, -1
-          IF ( ( hom(k+1,1,4,sr) - hom(k,1,4,sr) ) > &
-               2.0 * ( hom(k,1,4,sr) - hom(k-1,1,4,sr) ) )  THEN
-             z_i(2) = zu(k)
-             EXIT
-          ENDIF
-       ENDDO
+       IF ( ocean )  THEN
+          DO  k = nzb+1, nzt-1
+             IF ( ( hom(k,1,4,sr) - hom(k-1,1,4,sr) ) > &
+                  2.0 * ( hom(k+1,1,4,sr) - hom(k,1,4,sr) ) )  THEN
+                z_i(2) = zu(k)
+                EXIT
+             ENDIF
+          ENDDO
+       ELSE
+          DO  k = nzt-1, nzb+1, -1
+             IF ( ( hom(k+1,1,4,sr) - hom(k,1,4,sr) ) > &
+                  2.0 * ( hom(k,1,4,sr) - hom(k-1,1,4,sr) ) )  THEN
+                z_i(2) = zu(k)
+                EXIT
+             ENDIF
+          ENDDO
+       ENDIF
 
        hom(nzb+6,1,pr_palm,sr) = z_i(1)
Index: /palm/trunk/SOURCE/header.f90
===================================================================
--- /palm/trunk/SOURCE/header.f90	(revision 96)
+++ /palm/trunk/SOURCE/header.f90	(revision 97)
@@ -4,6 +4,6 @@
 ! Actual revisions:
 ! -----------------
-! Output of model height, stretch level, Prandtl-layer height and initial
-! temperature profile adjusted to be used also with the ocean version. 
+! Adjustments for the ocean version.
+! use_pt_reference renamed use_reference
 !
 ! Former revisions:
@@ -103,4 +103,9 @@
           PRINT*,'+++ header:  unknown action(s): ',initializing_actions
        ENDIF
+    ENDIF
+    IF ( ocean )  THEN
+       run_classification = 'ocean - ' // run_classification
+    ELSE
+       run_classification = 'atmosphere - ' // run_classification
     ENDIF
 
@@ -391,35 +396,44 @@
        roben = 'e(nzt+1) = e(nzt) = e(nzt-1)'
 
-       WRITE ( io, 301 )  runten, roben       
-
-    ENDIF
-
-    IF ( humidity  .OR.  passive_scalar )  THEN
-       IF ( humidity )  THEN
-          IF ( ibc_q_b == 0 )  THEN
-             runten = 'q(0)     = q_surface'
-          ELSE
-             runten = 'q(0)     = q(1)'
-          ENDIF
-          IF ( ibc_q_t == 0 )  THEN
-             roben =  'q(nzt)   = q_top'
-          ELSE
-             roben =  'q(nzt)   = q(nzt-1) + dq/dz'
-          ENDIF
-       ELSE
-          IF ( ibc_q_b == 0 )  THEN
-             runten = 's(0)     = s_surface'
-          ELSE
-             runten = 's(0)     = s(1)'
-          ENDIF
-          IF ( ibc_q_t == 0 )  THEN
-             roben =  's(nzt)   = s_top'
-          ELSE
-             roben =  's(nzt)   = s(nzt-1) + ds/dz'
-          ENDIF
-       ENDIF
-
-       WRITE ( io, 302 ) runten, roben
-
+       WRITE ( io, 301 )  'e', runten, roben       
+
+    ENDIF
+
+    IF ( ocean )  THEN
+       runten = 'sa(0)    = sa(1)'
+       IF ( ibc_sa_t == 0 )  THEN
+          roben =  'sa(nzt+1) = sa_surface'
+       ELSE
+          roben =  'sa(nzt+1) = sa(nzt)'
+       ENDIF
+       WRITE ( io, 301 ) 'sa', runten, roben
+    ENDIF
+
+    IF ( humidity )  THEN
+       IF ( ibc_q_b == 0 )  THEN
+          runten = 'q(0)     = q_surface'
+       ELSE
+          runten = 'q(0)     = q(1)'
+       ENDIF
+       IF ( ibc_q_t == 0 )  THEN
+          roben =  'q(nzt)   = q_top'
+       ELSE
+          roben =  'q(nzt)   = q(nzt-1) + dq/dz'
+       ENDIF
+       WRITE ( io, 301 ) 'q', runten, roben
+    ENDIF
+
+    IF ( passive_scalar )  THEN
+       IF ( ibc_q_b == 0 )  THEN
+          runten = 's(0)     = s_surface'
+       ELSE
+          runten = 's(0)     = s(1)'
+       ENDIF
+       IF ( ibc_q_t == 0 )  THEN
+          roben =  's(nzt)   = s_top'
+       ELSE
+          roben =  's(nzt)   = s(nzt-1) + ds/dz'
+       ENDIF
+       WRITE ( io, 301 ) 's', runten, roben
     ENDIF
 
@@ -442,4 +456,7 @@
        IF ( constant_top_heatflux )  THEN
           WRITE ( io, 306 )  top_heatflux
+       ENDIF
+       IF ( ocean  .AND.  constant_top_salinityflux )  THEN
+          WRITE ( io, 309 )  top_salinityflux
        ENDIF
        IF ( humidity  .OR.  passive_scalar )  THEN
@@ -887,5 +904,11 @@
 !-- Other quantities
     WRITE ( io, 411 )  g
-    IF ( use_pt_reference )  WRITE ( io, 412 )  pt_reference
+    IF ( use_reference )  THEN
+       IF ( ocean )  THEN
+          WRITE ( io, 412 )  prho_reference
+       ELSE
+          WRITE ( io, 413 )  pt_reference
+       ENDIF
+    ENDIF
 
 !
@@ -1011,4 +1034,34 @@
                              TRIM( gradients ), TRIM( slices )
        ENDIF
+    ENDIF
+
+!
+!-- Initial salinity profile
+!-- Building output strings, starting with surface salinity
+    IF ( ocean )  THEN
+       WRITE ( temperatures, '(F6.2)' )  sa_surface
+       gradients = '------'
+       slices = '     0'
+       coordinates = '   0.0'
+       i = 1
+       DO  WHILE ( sa_vertical_gradient_level_ind(i) /= -9999 )
+
+          WRITE (coor_chr,'(F7.2)')  sa_init(sa_vertical_gradient_level_ind(i))
+          temperatures = TRIM( temperatures ) // ' ' // TRIM( coor_chr )
+
+          WRITE (coor_chr,'(F7.2)')  sa_vertical_gradient(i)
+          gradients = TRIM( gradients ) // ' ' // TRIM( coor_chr )
+
+          WRITE (coor_chr,'(I7)')  sa_vertical_gradient_level_ind(i)
+          slices = TRIM( slices ) // ' ' // TRIM( coor_chr )
+
+          WRITE (coor_chr,'(F7.1)')  sa_vertical_gradient_level(i)
+          coordinates = TRIM( coordinates ) // ' '  // TRIM( coor_chr )
+
+          i = i + 1
+       ENDDO
+
+       WRITE ( io, 425 )  TRIM( coordinates ), TRIM( temperatures ), &
+                          TRIM( gradients ), TRIM( slices )
     ENDIF
 
@@ -1135,7 +1188,7 @@
 
  99 FORMAT (1X,78('-'))
-100 FORMAT (/1X,'*************************',11X,28('-')/        &
+100 FORMAT (/1X,'*************************',11X,42('-')/        &
             1X,'* ',A,' *',11X,A/                               &
-            1X,'*************************',11X,28('-')//        &
+            1X,'*************************',11X,42('-')//        &
             ' Date:            ',A8,11X,'Run:       ',A20/      &
             ' Time:            ',A8,11X,'Run-No.:   ',I2.2/     &
@@ -1256,8 +1309,5 @@
              ' B. bound.: ',A/ &
              ' T. bound.: ',A)
-301 FORMAT (/'                     e'// &
-             ' B. bound.: ',A/ &
-             ' T. bound.: ',A)
-302 FORMAT (/'                     q'// &
+301 FORMAT (/'                     ',A// &
              ' B. bound.: ',A/ &
              ' T. bound.: ',A)
@@ -1268,7 +1318,8 @@
              '       zp = ',F6.2,' m   z0 = ',F6.4,' m   kappa = ',F4.2/ &
              '       Rif value range:   ',F6.2,' <= rif <=',F6.2)
-306 FORMAT ('       Predefined constant heatflux:   ',F6.3,' K m/s')
+306 FORMAT ('       Predefined constant heatflux:   ',F9.6,' K m/s')
 307 FORMAT ('       Heatflux has a random normal distribution')
 308 FORMAT ('       Predefined surface temperature')
+309 FORMAT ('       Predefined constant salinityflux:   ',F9.6,' psu m/s')
 310 FORMAT (//'    1D-Model:'// &
              '       Rif value range:   ',F6.2,' <= rif <=',F6.2)
@@ -1352,5 +1403,6 @@
             '                            f*    = ',F9.6,' 1/s')
 411 FORMAT (/'    Gravity             :   g     = ',F4.1,' m/s**2')
-412 FORMAT (/'    Reference temperature in buoyancy terms: ',F8.4,' K')
+412 FORMAT (/'    Reference density in buoyancy terms: ',F8.3,' kg/m**3')
+413 FORMAT (/'    Reference temperature in buoyancy terms: ',F8.4,' K')
 415 FORMAT (/'    Cloud physics parameters:'/ &
              '    ------------------------'/)
@@ -1382,7 +1434,12 @@
 424 FORMAT (/'    Characteristic levels of the geo. wind component vg:'// &
             '       Height:      ',A,'  m'/ &
-            '       vg:          ',A,'  m/S'/ &
+            '       vg:          ',A,'  m/s'/ &
             '       Gradient:    ',A,'  1/100s'/ &
             '       Gridpoint:   ',A)
+425 FORMAT (/'    Characteristic levels of the initial salinity profile:'// &
+            '       Height:     ',A,'  m'/ &
+            '       Salinity:   ',A,'  psu'/ &
+            '       Gradient:   ',A,'  psu/100m'/ &
+            '       Gridpoint:  ',A)
 450 FORMAT (//' LES / Turbulence quantities:'/ &
               ' ---------------------------'/)
Index: /palm/trunk/SOURCE/init_3d_model.f90
===================================================================
--- /palm/trunk/SOURCE/init_3d_model.f90	(revision 96)
+++ /palm/trunk/SOURCE/init_3d_model.f90	(revision 97)
@@ -529,4 +529,9 @@
        hom(:,1,24,:) = SPREAD( kh(:,nys,nxl), 2, statistic_regions+1 )
 
+       IF ( ocean )  THEN
+!
+!--       Store initial salinity profile
+          hom(:,1,26,:)  = SPREAD( sa(:,nys,nxl), 2, statistic_regions+1 )
+       ENDIF
 
        IF ( humidity )  THEN
Index: /palm/trunk/SOURCE/init_ocean.f90
===================================================================
--- /palm/trunk/SOURCE/init_ocean.f90	(revision 96)
+++ /palm/trunk/SOURCE/init_ocean.f90	(revision 97)
@@ -40,6 +40,6 @@
     hyp(nzt+1) = surface_pressure * 100.0
 
-    hyp(nzt)   = hyp(nzt+1) + rho_surface * g * 0.5 * dzu(nzt+1)
-    rho_ref    = rho_surface * 0.5 * dzu(nzt+1)
+    hyp(nzt)      = hyp(nzt+1) + rho_surface * g * 0.5 * dzu(nzt+1)
+    rho_reference = rho_surface * 0.5 * dzu(nzt+1)
 
     DO  k = nzt-1, 0, -1
@@ -48,13 +48,27 @@
        pt_l = 0.5 * ( pt_init(k) + pt_init(k+1) )
 
-       rho_l   = eqn_state_seawater_func( hyp(k+1), pt_l, sa_l )
+       rho_l = eqn_state_seawater_func( hyp(k+1), pt_l, sa_l )
 
-       hyp(k)  = hyp(k+1) + rho_l * g * dzu(k+1)
-       rho_ref = rho_ref + rho_l * dzu(k+1)
+       hyp(k)        = hyp(k+1) + rho_l * g * dzu(k+1)
+       rho_reference = rho_reference + rho_l * dzu(k+1)
 
     ENDDO
 
-    rho_ref = rho_ref / ( zw(nzt) - zu(nzb) )
-    print*, '*** rho_ref = ', rho_ref
+    rho_reference = rho_reference / ( zw(nzt) - zu(nzb) )
+
+!
+!-- Calculate the reference potential density
+    prho_reference = 0.0
+    DO  k = 0, nzt
+
+       sa_l = 0.5 * ( sa_init(k) + sa_init(k+1) )
+       pt_l = 0.5 * ( pt_init(k) + pt_init(k+1) )
+
+       prho_reference = prho_reference + dzu(k+1) * &
+                        eqn_state_seawater_func( hyp(0), pt_l, sa_l )
+
+    ENDDO
+
+    prho_reference = prho_reference / ( zu(nzt) - zu(nzb) )
 
 
Index: /palm/trunk/SOURCE/modules.f90
===================================================================
--- /palm/trunk/SOURCE/modules.f90	(revision 96)
+++ /palm/trunk/SOURCE/modules.f90	(revision 97)
@@ -5,7 +5,7 @@
 ! Actual revisions:
 ! -----------------
-! +ocean, r, + salinity variables
+! +atmos_ocean_sign, ocean, r, + salinity variables
 ! defaults of .._vertical_gradient_levels changed from -1.0 to -9999999.9
-! hydro_press renamed hyp
+! hydro_press renamed hyp, use_pt_reference renamed use_reference
 !
 ! Former revisions:
@@ -324,5 +324,5 @@
                 sloping_surface = .FALSE., stop_dt = .FALSE., &
                 terminate_run = .FALSE., use_prior_plot1d_parameters = .FALSE.,&
-                use_pt_reference = .FALSE., use_surface_fluxes = .FALSE., &
+                use_reference = .FALSE., use_surface_fluxes = .FALSE., &
                 use_top_fluxes = .FALSE., use_ug_for_galilei_tr = .TRUE., &
                 use_upstream_for_tke = .FALSE., wall_adjustment = .TRUE.
@@ -333,4 +333,5 @@
     REAL ::  advected_distance_x = 0.0, advected_distance_y = 0.0, &
              alpha_surface = 0.0, asselin_filter_factor = 0.1, &
+             atmos_ocean_sign = 1.0, &
              averaging_interval = 0.0, averaging_interval_pr = 9999999.9, &
              averaging_interval_sp = 9999999.9, bc_pt_t_val, bc_q_t_val, &
@@ -340,6 +341,8 @@
              building_wall_south = 9999999.9, cfl_factor = -1.0, &
              cos_alpha_surface, disturbance_amplitude = 0.25, &
-             disturbance_energy_limit = 0.01, disturbance_level_b = -1.0, &
-             disturbance_level_t = -1.0, dt = -1.0, dt_averaging_input = 0.0, &
+             disturbance_energy_limit = 0.01, &
+             disturbance_level_b = -9999999.9, &
+             disturbance_level_t = -9999999.9, &
+             dt = -1.0, dt_averaging_input = 0.0, &
              dt_averaging_input_pr = 9999999.9, dt_data_output = 9999999.9, &
              dt_data_output_av = 9999999.9, dt_disturb = 9999999.9, &
@@ -360,11 +363,11 @@
              overshoot_limit_w = 0.0, particle_maximum_age = 9999999.9, &
              phi = 55.0, prandtl_number = 1.0, &
-             precipitation_amount_interval = 9999999.9, &
-             pt_reference = 9999999.9, &
-             pt_slope_offset = 0.0, pt_surface = 300.0, &
-             pt_surface_initial_change = 0.0, q_surface = 0.0, &
-             q_surface_initial_change = 0.0, rayleigh_damping_factor = -1.0, &
-             rayleigh_damping_height = -1.0, residual_limit = 1.0E-4, &
-             restart_time = 9999999.9, rho_ref, rho_surface, rif_max = 1.0, &
+             precipitation_amount_interval = 9999999.9, prho_reference, &
+             pt_reference = 9999999.9, pt_slope_offset = 0.0, &
+             pt_surface = 300.0, pt_surface_initial_change = 0.0, &
+             q_surface = 0.0, q_surface_initial_change = 0.0, &
+             rayleigh_damping_factor = -1.0, rayleigh_damping_height = -1.0, &
+             residual_limit = 1.0E-4, restart_time = 9999999.9, rho_reference, &
+             rho_surface, rif_max = 1.0, &
              rif_min = -5.0, roughness_length = 0.1, sa_surface = 35.0, &
              simulated_time = 0.0, simulated_time_at_begin, sin_alpha_surface, &
@@ -401,7 +404,7 @@
              tsc(10) = (/ 0.0, 1.0, 0.0, 0.0, 0.0, 0.0, 0.0, 0.0, 0.0, 0.0 /), &
              ug_vertical_gradient(10) = 0.0, &
-             ug_vertical_gradient_level(10) = -1.0, &
+             ug_vertical_gradient_level(10) = -9999999.9, &
              vg_vertical_gradient(10) = 0.0, &
-             vg_vertical_gradient_level(10) = -1.0, &
+             vg_vertical_gradient_level(10) = -9999999.9, &
              volume_flow(1:2) = 0.0, volume_flow_area(1:2) = 0.0, &
              volume_flow_initial(1:2) = 0.0, wall_heatflux(0:4) = 0.0
Index: /palm/trunk/SOURCE/netcdf.f90
===================================================================
--- /palm/trunk/SOURCE/netcdf.f90	(revision 96)
+++ /palm/trunk/SOURCE/netcdf.f90	(revision 97)
@@ -7,5 +7,5 @@
 ! Current revisions:
 ! ------------------
-! 
+! Grids defined for rho and sa
 !
 ! Former revisions:
@@ -345,5 +345,5 @@
 !--             Most variables are defined on the scalar grid
                 CASE ( 'e', 'p', 'pc', 'pr', 'pt', 'q', 'ql', 'ql_c', 'ql_v', &
-                       'ql_vp', 'qv', 's', 'vpt' )
+                       'ql_vp', 'qv', 'rho', 's', 'sa', 'vpt' )
 
                    grid_x = 'x'
@@ -870,5 +870,5 @@
                       CASE ( 'e_xy', 'p_xy', 'pc_xy', 'pr_xy', 'pt_xy', 'q_xy',&
                              'ql_xy', 'ql_c_xy', 'ql_v_xy', 'ql_vp_xy',        &
-                             'qv_xy', 's_xy', 'vpt_xy' )
+                             'qv_xy', 'rho_xy', 's_xy', 'sa_xy', 'vpt_xy' )
 
                          grid_x = 'x'
@@ -1414,5 +1414,5 @@
                    CASE ( 'e_xz', 'p_xz', 'pc_xz', 'pr_xz', 'pt_xz', 'q_xz',  &
                           'ql_xz', 'ql_c_xz', 'ql_v_xz', 'ql_vp_xz', 'qv_xz', &
-                          's_xz', 'vpt_xz' )
+                          'rho_xz', 's_xz', 'sa_xz', 'vpt_xz' )
 
                       grid_x = 'x'
@@ -1925,5 +1925,5 @@
                    CASE ( 'e_yz', 'p_yz', 'pc_yz', 'pr_yz', 'pt_yz', 'q_yz',  &
                           'ql_yz', 'ql_c_yz', 'ql_v_yz', 'ql_vp_yz', 'qv_yz', &
-                          's_yz', 'vpt_yz' )
+                          'rho_yz', 's_yz', 'sa_yz', 'vpt_yz' )
 
                       grid_x = 'x'
Index: /palm/trunk/SOURCE/palm.f90
===================================================================
--- /palm/trunk/SOURCE/palm.f90	(revision 96)
+++ /palm/trunk/SOURCE/palm.f90	(revision 97)
@@ -63,5 +63,5 @@
     INTEGER           ::  i, run_description_header_i(80)
 
-    version = 'PALM 3.2b'
+    version = 'PALM 3.3'
 
 #if defined( __parallel )
Index: /palm/trunk/SOURCE/production_e.f90
===================================================================
--- /palm/trunk/SOURCE/production_e.f90	(revision 96)
+++ /palm/trunk/SOURCE/production_e.f90	(revision 97)
@@ -4,5 +4,6 @@
 ! Actual revisions:
 ! -----------------
-! 
+! energy production by density flux (in ocean) added
+! use_pt_reference renamed use_reference
 !
 ! Former revisions:
@@ -364,41 +365,76 @@
           IF ( .NOT. humidity )  THEN
 
-             IF ( use_pt_reference )  THEN
-
-                DO  j = nys, nyn
-                   DO  k = nzb_diff_s_inner(j,i), nzt_diff
-                      tend(k,j,i) = tend(k,j,i) - kh(k,j,i) * g/pt_reference * &
+             IF ( use_reference )  THEN
+
+                IF ( ocean )  THEN
+!
+!--                So far in the ocean no special treatment of density flux in
+!--                the bottom and top surface layer
+                   DO  j = nys, nyn
+                      DO  k = nzb_s_inner(j,i), nzt
+                         tend(k,j,i) = tend(k,j,i) +                    &
+                                       kh(k,j,i) * g / prho_reference * &
+                                       ( rho(k+1,j,i)-rho(k-1,j,i) ) * dd2zu(k)
+                      ENDDO
+                   ENDDO
+
+                ELSE
+
+                   DO  j = nys, nyn
+                      DO  k = nzb_diff_s_inner(j,i), nzt_diff
+                         tend(k,j,i) = tend(k,j,i) +                  &
+                                       kh(k,j,i) * g / pt_reference * &
                                        ( pt(k+1,j,i) - pt(k-1,j,i) ) * dd2zu(k)
+                      ENDDO
+
+                      IF ( use_surface_fluxes )  THEN
+                         k = nzb_diff_s_inner(j,i)-1
+                         tend(k,j,i) = tend(k,j,i) + g / pt_reference * shf(j,i)
+                      ENDIF
+
+                      IF ( use_top_fluxes )  THEN
+                         k = nzt
+                         tend(k,j,i) = tend(k,j,i) + g / pt_reference * &
+                                                     tswst(j,i)
+                      ENDIF
                    ENDDO
 
-                   IF ( use_surface_fluxes )  THEN
-                      k = nzb_diff_s_inner(j,i)-1
-                      tend(k,j,i) = tend(k,j,i) + g / pt_reference * shf(j,i)
-                   ENDIF
-
-                   IF ( use_top_fluxes )  THEN
-                      k = nzt
-                      tend(k,j,i) = tend(k,j,i) + g / pt_reference * tswst(j,i)
-                   ENDIF
-                ENDDO
+                ENDIF
 
              ELSE
 
-                DO  j = nys, nyn
-                   DO  k = nzb_diff_s_inner(j,i), nzt_diff
-                      tend(k,j,i) = tend(k,j,i) - kh(k,j,i) * g / pt(k,j,i) * &
+                IF ( ocean )  THEN
+!
+!--                So far in the ocean no special treatment of density flux in
+!--                the bottom and top surface layer
+                   DO  j = nys, nyn
+                      DO  k = nzb_s_inner(j,i), nzt
+                         tend(k,j,i) = tend(k,j,i) -                &
+                                       kh(k,j,i) * g / rho(k,j,i) * &
+                                       ( rho(k+1,j,i)-rho(k-1,j,i) ) * dd2zu(k)
+                      ENDDO
+                   ENDDO
+
+                ELSE
+
+                   DO  j = nys, nyn
+                      DO  k = nzb_diff_s_inner(j,i), nzt_diff
+                         tend(k,j,i) = tend(k,j,i) -               &
+                                       kh(k,j,i) * g / pt(k,j,i) * &
                                        ( pt(k+1,j,i) - pt(k-1,j,i) ) * dd2zu(k)
+                      ENDDO
+
+                      IF ( use_surface_fluxes )  THEN
+                         k = nzb_diff_s_inner(j,i)-1
+                         tend(k,j,i) = tend(k,j,i) + g / pt(k,j,i) * shf(j,i)
+                      ENDIF
+
+                      IF ( use_top_fluxes )  THEN
+                         k = nzt
+                         tend(k,j,i) = tend(k,j,i) + g / pt(k,j,i) * tswst(j,i)
+                      ENDIF
                    ENDDO
 
-                   IF ( use_surface_fluxes )  THEN
-                      k = nzb_diff_s_inner(j,i)-1
-                      tend(k,j,i) = tend(k,j,i) + g / pt(k,j,i) * shf(j,i)
-                   ENDIF
-
-                   IF ( use_top_fluxes )  THEN
-                      k = nzt
-                      tend(k,j,i) = tend(k,j,i) + g / pt(k,j,i) * tswst(j,i)
-                   ENDIF
-                ENDDO
+                ENDIF
 
              ENDIF
@@ -762,39 +798,65 @@
        IF ( .NOT. humidity )  THEN
 
-          IF ( use_pt_reference )  THEN
-
-             DO  k = nzb_diff_s_inner(j,i), nzt_diff
-                tend(k,j,i) = tend(k,j,i) - kh(k,j,i) * g / pt_reference * &
+          IF ( use_reference )  THEN
+
+             IF ( ocean )  THEN
+!
+!--             So far in the ocean no special treatment of density flux in the
+!--             bottom and top surface layer
+                DO  k = nzb_s_inner(j,i), nzt
+                   tend(k,j,i) = tend(k,j,i) + kh(k,j,i) * g / prho_reference * &
+                                      ( rho(k+1,j,i) - rho(k-1,j,i) ) * dd2zu(k)
+                ENDDO
+
+             ELSE
+
+                DO  k = nzb_diff_s_inner(j,i), nzt_diff
+                   tend(k,j,i) = tend(k,j,i) - kh(k,j,i) * g / pt_reference * &
                                        ( pt(k+1,j,i) - pt(k-1,j,i) ) * dd2zu(k)
-             ENDDO
-
-             IF ( use_surface_fluxes )  THEN
-                k = nzb_diff_s_inner(j,i)-1
-                tend(k,j,i) = tend(k,j,i) + g / pt_reference * shf(j,i)
+                ENDDO
+
+                IF ( use_surface_fluxes )  THEN
+                   k = nzb_diff_s_inner(j,i)-1
+                   tend(k,j,i) = tend(k,j,i) + g / pt_reference * shf(j,i)
+                ENDIF
+
+                IF ( use_top_fluxes )  THEN
+                   k = nzt
+                   tend(k,j,i) = tend(k,j,i) + g / pt_reference * tswst(j,i)
+                ENDIF
+
              ENDIF
 
-             IF ( use_top_fluxes )  THEN
-                k = nzt
-                tend(k,j,i) = tend(k,j,i) + g / pt_reference * tswst(j,i)
+          ELSE
+
+             IF ( ocean )  THEN
+!
+!--             So far in the ocean no special treatment of density flux in the
+!--             bottom and top surface layer
+                DO  k = nzb_s_inner(j,i), nzt
+                   tend(k,j,i) = tend(k,j,i) + kh(k,j,i) * g / rho(k,j,i) * &
+                                      ( rho(k+1,j,i) - rho(k-1,j,i) ) * dd2zu(k)
+                ENDDO
+
+             ELSE
+
+                DO  k = nzb_diff_s_inner(j,i), nzt_diff
+                   tend(k,j,i) = tend(k,j,i) - kh(k,j,i) * g / pt(k,j,i) * &
+                                       ( pt(k+1,j,i) - pt(k-1,j,i) ) * dd2zu(k)
+                ENDDO
+
+                IF ( use_surface_fluxes )  THEN
+                   k = nzb_diff_s_inner(j,i)-1
+                   tend(k,j,i) = tend(k,j,i) + g / pt(k,j,i) * shf(j,i)
+                ENDIF
+
+                IF ( use_top_fluxes )  THEN
+                   k = nzt
+                   tend(k,j,i) = tend(k,j,i) + g / pt(k,j,i) * tswst(j,i)
+                ENDIF
+
              ENDIF
 
-          ELSE
-
-             DO  k = nzb_diff_s_inner(j,i), nzt_diff
-                tend(k,j,i) = tend(k,j,i) - kh(k,j,i) * g / pt(k,j,i) * &
-                                       ( pt(k+1,j,i) - pt(k-1,j,i) ) * dd2zu(k)
-             ENDDO
-
-             IF ( use_surface_fluxes )  THEN
-                k = nzb_diff_s_inner(j,i)-1
-                tend(k,j,i) = tend(k,j,i) + g / pt(k,j,i) * shf(j,i)
-             ENDIF
-
-             IF ( use_top_fluxes )  THEN
-                k = nzt
-                tend(k,j,i) = tend(k,j,i) + g / pt(k,j,i) * tswst(j,i)
-             ENDIF
-
-         ENDIF
+          ENDIF
 
        ELSE
Index: /palm/trunk/SOURCE/prognostic_equations.f90
===================================================================
--- /palm/trunk/SOURCE/prognostic_equations.f90	(revision 96)
+++ /palm/trunk/SOURCE/prognostic_equations.f90	(revision 97)
@@ -5,6 +5,9 @@
 ! -----------------
 ! prognostic equation for salinity, density is calculated from equation of
-! state for seawater, +eqn_state_seawater_mod
-! new argument zw in calls of diffusion_e, calc_mean_pt_profile renamed
+! state for seawater and is used for calculation of buoyancy,
+! +eqn_state_seawater_mod
+! diffusion_e is called with argument rho in case of ocean runs,
+! new argument zw in calls of diffusion_e, new argument pt_/prho_reference
+! in calls of buoyancy and diffusion_e, calc_mean_pt_profile renamed
 ! calc_mean_profile
 !
@@ -148,5 +151,5 @@
           ENDIF
           CALL coriolis( i, j, 1 )
-          IF ( sloping_surface )  CALL buoyancy( i, j, pt, 1, 4 )
+          IF ( sloping_surface )  CALL buoyancy( i, j, pt, pt_reference, 1, 4 )
           CALL user_actions( i, j, 'u-tendency' )
 
@@ -283,8 +286,12 @@
           ENDIF
           CALL coriolis( i, j, 3 )
-          IF ( .NOT. humidity )  THEN
-             CALL buoyancy( i, j, pt, 3, 4 )
+          IF ( ocean )  THEN
+             CALL buoyancy( i, j, rho, prho_reference, 3, 64 )
           ELSE
-             CALL buoyancy( i, j, vpt, 3, 44 )
+             IF ( .NOT. humidity )  THEN
+                CALL buoyancy( i, j, pt, pt_reference, 3, 4 )
+             ELSE
+                CALL buoyancy( i, j, vpt, pt_reference, 3, 44 )
+             ENDIF
           ENDIF
           CALL user_actions( i, j, 'w-tendency' )
@@ -654,9 +661,17 @@
                   .NOT. use_upstream_for_tke )  THEN
                 IF ( .NOT. humidity )  THEN
-                   CALL diffusion_e( i, j, ddzu, dd2zu, ddzw, diss, e, km, &
-                                     l_grid, pt, rif, tend, zu, zw )
+                   IF ( ocean )  THEN
+                      CALL diffusion_e( i, j, ddzu, dd2zu, ddzw, diss, e, km,   &
+                                        l_grid, rho, prho_reference, rif, tend, &
+                                        zu, zw )
+                   ELSE
+                      CALL diffusion_e( i, j, ddzu, dd2zu, ddzw, diss, e, km, &
+                                        l_grid, pt, pt_reference, rif, tend,  &
+                                        zu, zw )
+                   ENDIF
                 ELSE
-                   CALL diffusion_e( i, j, ddzu, dd2zu, ddzw, diss, e, km, &
-                                     l_grid, vpt, rif, tend, zu, zw )
+                   CALL diffusion_e( i, j, ddzu, dd2zu, ddzw, diss, e, km,     &
+                                     l_grid, vpt, pt_reference, rif, tend, zu, &
+                                     zw )
                 ENDIF
              ELSE
@@ -680,18 +695,26 @@
                    IF ( .NOT. humidity )  THEN
                       CALL diffusion_e( i, j, ddzu, dd2zu, ddzw, diss, e_m, &
-                                        km_m, l_grid, pt_m, rif_m, tend, zu, &
-                                        zw )
+                                        km_m, l_grid, pt_m, pt_reference,   &
+                                        rif_m, tend, zu, zw )
                    ELSE
                       CALL diffusion_e( i, j, ddzu, dd2zu, ddzw, diss, e_m, &
-                                        km_m, l_grid, vpt_m, rif_m, tend, zu, &
-                                        zw )
+                                        km_m, l_grid, vpt_m, pt_reference,  &
+                                        rif_m, tend, zu, zw )
                    ENDIF
                 ELSE
                    IF ( .NOT. humidity )  THEN
-                      CALL diffusion_e( i, j, ddzu, dd2zu, ddzw, diss, e, km, &
-                                        l_grid, pt, rif, tend, zu, zw )
+                      IF ( ocean )  THEN
+                         CALL diffusion_e( i, j, ddzu, dd2zu, ddzw, diss, e,  &
+                                           km, l_grid, rho, prho_reference,   &
+                                           rif, tend, zu, zw )
+                      ELSE
+                         CALL diffusion_e( i, j, ddzu, dd2zu, ddzw, diss, e,  &
+                                           km, l_grid, pt, pt_reference, rif, &
+                                           tend, zu, zw )
+                      ENDIF
                    ELSE
                       CALL diffusion_e( i, j, ddzu, dd2zu, ddzw, diss, e, km, &
-                                        l_grid, vpt, rif, tend, zu, zw )
+                                        l_grid, vpt, pt_reference, rif, tend, &
+                                        zu, zw )
                    ENDIF
                 ENDIF
@@ -797,5 +820,6 @@
              ENDIF
              CALL coriolis( i, j, 1 )
-             IF ( sloping_surface )  CALL buoyancy( i, j, pt, 1, 4 )
+             IF ( sloping_surface )  CALL buoyancy( i, j, pt, pt_reference, 1, &
+                                                    4 )
              CALL user_actions( i, j, 'u-tendency' )
 
@@ -896,8 +920,12 @@
              ENDIF
              CALL coriolis( i, j, 3 )
-             IF ( .NOT. humidity )  THEN
-                CALL buoyancy( i, j, pt, 3, 4 )
+             IF ( ocean )  THEN
+                CALL buoyancy( i, j, rho, prho_reference, 3, 64 )
              ELSE
-                CALL buoyancy( i, j, vpt, 3, 44 )
+                IF ( .NOT. humidity )  THEN
+                   CALL buoyancy( i, j, pt, pt_reference, 3, 4 )
+                ELSE
+                   CALL buoyancy( i, j, vpt, pt_reference, 3, 44 )
+                ENDIF
              ENDIF
              CALL user_actions( i, j, 'w-tendency' )
@@ -1114,18 +1142,26 @@
                    IF ( .NOT. humidity )  THEN
                       CALL diffusion_e( i, j, ddzu, dd2zu, ddzw, diss, e_m, &
-                                        km_m, l_grid, pt_m, rif_m, tend, zu, &
-                                        zw )
+                                        km_m, l_grid, pt_m, pt_reference,   &
+                                        rif_m, tend, zu, zw )
                    ELSE
                       CALL diffusion_e( i, j, ddzu, dd2zu, ddzw, diss, e_m, &
-                                        km_m, l_grid, vpt_m, rif_m, tend, zu, &
-                                        zw )
+                                        km_m, l_grid, vpt_m, pt_reference,  &
+                                        rif_m, tend, zu, zw )
                    ENDIF
                 ELSE
                    IF ( .NOT. humidity )  THEN
-                      CALL diffusion_e( i, j, ddzu, dd2zu, ddzw, diss, e, km, &
-                                        l_grid, pt, rif, tend, zu, zw )
+                      IF ( ocean )  THEN
+                         CALL diffusion_e( i, j, ddzu, dd2zu, ddzw, diss, e, &
+                                           km, l_grid, rho, prho_reference,  &
+                                           rif, tend, zu, zw )
+                      ELSE
+                         CALL diffusion_e( i, j, ddzu, dd2zu, ddzw, diss, e,  &
+                                           km, l_grid, pt, pt_reference, rif, &
+                                           tend, zu, zw )
+                      ENDIF
                    ELSE
                       CALL diffusion_e( i, j, ddzu, dd2zu, ddzw, diss, e, km, &
-                                        l_grid, vpt, rif, tend, zu, zw )
+                                        l_grid, vpt, pt_reference, rif, tend, &
+                                        zu, zw )
                    ENDIF
                 ENDIF
@@ -1224,5 +1260,5 @@
     ENDIF
     CALL coriolis( 1 )
-    IF ( sloping_surface )  CALL buoyancy( pt, 1, 4 )
+    IF ( sloping_surface )  CALL buoyancy( pt, pt_reference, 1, 4 )
     CALL user_actions( 'u-tendency' )
 
@@ -1367,8 +1403,12 @@
     ENDIF
     CALL coriolis( 3 )
-    IF ( .NOT. humidity )  THEN
-       CALL buoyancy( pt, 3, 4 )
+    IF ( ocean )  THEN
+       CALL buoyancy( rho, prho_reference, 3, 64 )
     ELSE
-       CALL buoyancy( vpt, 3, 44 )
+       IF ( .NOT. humidity )  THEN
+          CALL buoyancy( pt, pt_reference, 3, 4 )
+       ELSE
+          CALL buoyancy( vpt, pt_reference, 3, 44 )
+       ENDIF
     ENDIF
     CALL user_actions( 'w-tendency' )
@@ -1753,9 +1793,14 @@
        THEN
           IF ( .NOT. humidity )  THEN
-             CALL diffusion_e( ddzu, dd2zu, ddzw, diss, e, km, l_grid, pt, &
-                               rif, tend, zu, zw )
+             IF ( ocean )  THEN
+                CALL diffusion_e( ddzu, dd2zu, ddzw, diss, e, km, l_grid, rho, &
+                                  prho_reference, rif, tend, zu, zw )
+             ELSE
+                CALL diffusion_e( ddzu, dd2zu, ddzw, diss, e, km, l_grid, pt, &
+                                  pt_reference, rif, tend, zu, zw )
+             ENDIF
           ELSE
              CALL diffusion_e( ddzu, dd2zu, ddzw, diss, e, km, l_grid, vpt, &
-                               rif, tend, zu, zw )
+                               pt_reference, rif, tend, zu, zw )
           ENDIF
        ELSE
@@ -1777,16 +1822,21 @@
              IF ( .NOT. humidity )  THEN
                 CALL diffusion_e( ddzu, dd2zu, ddzw, diss, e_m, km_m, l_grid, &
-                                  pt_m, rif_m, tend, zu, zw )
+                                  pt_m, pt_reference, rif_m, tend, zu, zw )
              ELSE
                 CALL diffusion_e( ddzu, dd2zu, ddzw, diss, e_m, km_m, l_grid, &
-                                  vpt_m, rif_m, tend, zu, zw )
+                                  vpt_m, pt_reference, rif_m, tend, zu, zw )
              ENDIF
           ELSE
              IF ( .NOT. humidity )  THEN
-                CALL diffusion_e( ddzu, dd2zu, ddzw, diss, e, km, l_grid, pt, &
-                                  rif, tend, zu, zw )
+                IF ( ocean )  THEN
+                   CALL diffusion_e( ddzu, dd2zu, ddzw, diss, e, km, l_grid, &
+                                     rho, prho_reference, rif, tend, zu, zw )
+                ELSE
+                   CALL diffusion_e( ddzu, dd2zu, ddzw, diss, e, km, l_grid, &
+                                     pt, pt_reference, rif, tend, zu, zw )
+                ENDIF
              ELSE
                 CALL diffusion_e( ddzu, dd2zu, ddzw, diss, e, km, l_grid, vpt, &
-                                  rif, tend, zu, zw )
+                                  pt_reference, rif, tend, zu, zw )
              ENDIF
           ENDIF
Index: /palm/trunk/SOURCE/run_control.f90
===================================================================
--- /palm/trunk/SOURCE/run_control.f90	(revision 96)
+++ /palm/trunk/SOURCE/run_control.f90	(revision 97)
@@ -4,5 +4,5 @@
 ! Actual revisions:
 ! -----------------
-! 
+! Timestep format changed
 !
 ! Former revisions:
@@ -113,15 +113,15 @@
 100 FORMAT (///'Run-control output:'/ &
               &'------------------'// &
-           &'RUN  ITER. HH:MM:SS.SS   DT(E)     UMAX     VMAX     WMAX     U*', &
-           &'    W*   THETA*   Z_I     ENERG.   DISTENERG    DIVOLD     DIVNE', &
-           &'W     UMAX(KJI)    VMAX(KJI)    WMAX(KJI)   ADVECX   ADVECY   MG', &
-           &'CYC'/ &
-           &'----------------------------------------------------------------', &
-           &'----------------------------------------------------------------', &
-           &'----------------------------------------------------------------', &
-           &'--')
-101 FORMAT (I3,1X,I6,1X,A8,F3.2,1X,F7.4,A1,A1,F8.4,A1,F8.4,A1,F8.4,2X,F5.3,2X, &
+          &'RUN  ITER. HH:MM:SS.SS    DT(E)     UMAX     VMAX     WMAX     U', &
+          &'*    W*   THETA*    Z_I     ENERG.   DISTENERG    DIVOLD     DIV', &
+          &'NEW     UMAX(KJI)    VMAX(KJI)    WMAX(KJI)   ADVECX   ADVECY   ', &
+          &'MGCYC'/                                                            &
+          &'----------------------------------------------------------------', &
+          &'----------------------------------------------------------------', &
+          &'----------------------------------------------------------------', &
+          &'-----')
+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, &
             F4.2, &
-            2X,F6.3,2X,F5.0,1X,4(E10.3,1X),3(3(I4),1X),F8.3,1X,F8.3,5X,I3)
+            2X,F6.3,2X,F6.0,1X,4(E10.3,1X),3(3(I4),1X),F8.3,1X,F8.3,5X,I3)
 
  END SUBROUTINE run_control
Index: /palm/trunk/SOURCE/time_integration.f90
===================================================================
--- /palm/trunk/SOURCE/time_integration.f90	(revision 96)
+++ /palm/trunk/SOURCE/time_integration.f90	(revision 97)
@@ -4,5 +4,7 @@
 ! Actual revisions:
 ! -----------------
-! Ghostpoint exchange for salinity and density
+! diffusivities is called with argument rho in case of ocean runs,
+! new argument pt_/prho_reference in calls of diffusivities,
+! ghostpoint exchange for salinity and density
 !
 ! Former revisions:
@@ -249,7 +251,11 @@
              CALL cpu_log( log_point(17), 'diffusivities', 'start' )
              IF ( .NOT. humidity ) THEN
-                CALL diffusivities( pt )
+                IF ( ocean )  THEN
+                   CALL diffusivities( rho, prho_reference )
+                ELSE
+                   CALL diffusivities( pt, pt_reference )
+                ENDIF
              ELSE
-                CALL diffusivities( vpt )
+                CALL diffusivities( vpt, pt_reference )
              ENDIF
              CALL cpu_log( log_point(17), 'diffusivities', 'stop' )
