Changes between Version 55 and Version 56 of doc/app/initialization_parameters

Timestamp:

Sep 14, 2010 9:49:18 AM (14 years ago)

Author:

kanani

Comment:

--

doc/app/initialization_parameters

@@ -258 +258 @@
 |----------------
 {{{#!td style="vertical-align:top"
-[=#<insert_parameter_name> '''<insert_parameter_name>''']
-}}}
-{{{#!td style="vertical-align:top"
-<insert type>
-}}}
-{{{#!td style="vertical-align:top"
-<insert value>
-}}}
-{{{#!td
-<insert explanation>
+[=#humidity '''humidity''']
+}}}
+{{{#!td style="vertical-align:top"
+L
+}}}
+{{{#!td style="vertical-align:top"
+.F.
+}}}
+{{{#!td
+Parameter to switch on the prognostic equation for specific humidity q.\\\\
+The initial vertical profile of q can be set via parameters [#q_surface q_surface], [#q_vertical_gradient q_vertical_gradient] and [#q_vertical_gradient_level q_vertical_gradient_level]. Boundary conditions can be set via [#q_surface_initial_change q_surface_initial_change] and [#surface_waterflux surface_waterflux].\\\\
+If the condensation scheme is switched on ([#cloud_physics cloud_physics] = ''.T.''), q becomes the total liquid water content (sum of specific humidity and liquid water content).
 }}}
 |----------------
@@ -846 +848 @@
 This parameter only comes into effect for ocean runs (see parameter [#ocean ocean]).\\\\
 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.
+}}}
+|----------------
+{{{#!td style="vertical-align:top"
+[=#inflow_damping_height '''inflow_damping_height''']
+}}}
+{{{#!td style="vertical-align:top"
+R
+}}}
+{{{#!td style="vertical-align:top"
+from precursor run
+}}}
+{{{#!td
+Height below which the turbulence signal is used for turbulence recycling (in m).\\\\
+In case of a turbulent inflow (see [#turbulent_inflow turbulent_inflow]), this parameter defines the vertical thickness of the turbulent layer up to which the turbulence extracted at the recycling plane (see [#recycling_width recycling_width]) shall be imposed to the inflow. Above this level the turbulence signal is linearly damped to zero. The transition range within which the signal falls to zero is given by the parameter [#inflow_damping_width inflow_damping_width].\\\\
+By default, this height is set as the height of the convective boundary layer as calculated from a precursor run. See chapter [[3.9]] about proper settings for getting this CBL height from a precursor run. 
+}}}
+|----------------
+{{{#!td style="vertical-align:top"
+[=#<insert_parameter_name> '''<insert_parameter_name>''']
+}}}
+{{{#!td style="vertical-align:top"
+<insert type>
+}}}
+{{{#!td style="vertical-align:top"
+<insert value>
+}}}
+{{{#!td
+<insert explanation>
+}}}
+|----------------
+{{{#!td style="vertical-align:top"
+[=#<insert_parameter_name> '''<insert_parameter_name>''']
+}}}
+{{{#!td style="vertical-align:top"
+<insert type>
+}}}
+{{{#!td style="vertical-align:top"
+<insert value>
+}}}
+{{{#!td
+<insert explanation>
+}}}
+|----------------
+{{{#!td style="vertical-align:top"
+[=#<insert_parameter_name> '''<insert_parameter_name>''']
+}}}
+{{{#!td style="vertical-align:top"
+<insert type>
+}}}
+{{{#!td style="vertical-align:top"
+<insert value>
+}}}
+{{{#!td
+<insert explanation>
+}}}
+|----------------
+{{{#!td style="vertical-align:top"
+[=#<insert_parameter_name> '''<insert_parameter_name>''']
+}}}
+{{{#!td style="vertical-align:top"
+<insert type>
+}}}
+{{{#!td style="vertical-align:top"
+<insert value>
+}}}
+{{{#!td
+<insert explanation>
+}}}
+|----------------
+{{{#!td style="vertical-align:top"
+[=#<insert_parameter_name> '''<insert_parameter_name>''']
+}}}
+{{{#!td style="vertical-align:top"
+<insert type>
+}}}
+{{{#!td style="vertical-align:top"
+<insert value>
+}}}
+{{{#!td
+<insert explanation>
 }}}
 |----------------