Changes between Version 100 and Version 101 of doc/app/initialization_parameters

Timestamp:

Sep 15, 2010 1:01:29 PM (14 years ago)

Author:

kanani

Comment:

--

doc/app/initialization_parameters

@@ -379 +379 @@
 }}}
 {{{#!td
-v-component of the predefined bulk velocity (in m/s).
-
-This parameter comes into effect if conserve_volume_flow = .T. and conserve_volume_flow_mode = 'bulk_velocity'.
+v-component of the predefined bulk velocity (in m/s).\\\\
+This parameter comes into effect if [#conserve_volume_flow conserve_volume_flow] = ''.T.'' and [#conserve_volume_flow_mode conserve_volume_flow_mode] = '' 'bulk_velocity'.''
 }}}
 |----------------
@@ -394 +393 @@
 }}}
 {{{#!td
-Gradient(s) of the profile for the large scale subsidence/ascent velocity (in (m/s) / 100 m). 
-
-This gradient holds starting from the height  level defined by ws_vertical_gradient_level (precisely: for all uv levels k where zu(k) > ws_vertical_gradient_level, w_subs(k) is set: w_subs(k) = w_subs(k-1) + dzu(k) * ws_vertical_gradient) up to the top boundary or up to the next height level defined by ws_vertical_gradient_level. A total of 10 different gradients for 11 height intervals (10 intervals if ws_vertical_gradient_level(1) = 0.0) can be assigned.  
-
-Example: 
-
-      ws_vertical_gradient = -0.002, 0.0, 
-      ws_vertical_gradient_level = 0.0, 1000.0,
-
-That defines the subsidence/ascent profile to be linear up to z = 1000.0 m with a surface value of 0 m/s. For z > 1000.0 m up to the top boundary the gradient is 0.0 (m/s) / 100 m (it is assumed that the assigned height levels correspond with uv levels).
-
-With an appropriate construction of w_subs the height of the boundary layer z_i can be kept approximately constant.
-
-Attention:
-The large scale vertical motion is only applied to the prognostic equation for the scalar quantities (potential temperature, humidity if humidity = .T. or passive scalar if passive_scalar = .T.) because it cannot be applied to the momentum equations due to incompressibility. Thus, the model is not mass consistent.
+Gradient(s) of the profile for the large scale subsidence/ascent velocity (in (m/s) / 100 m).\\\\
+This gradient holds starting from the height level defined by [#ws_vertical_gradient_level ws_vertical_gradient_level] (precisely: for all uv levels k where zu(k) > ws_vertical_gradient_level, '''w_subs'''(k) is set: w_subs(k) = w_subs(k-1) + dzu(k) * '''ws_vertical_gradient''') up to the top boundary or up to the next height level defined by ws_vertical_gradient_level. A total of 10 different gradients for 11 height intervals (10 intervals if ws_vertical_gradient_level(1) = 0.0) can be assigned.\\\\
+'''Example:'''\\\\
+      '''ws_vertical_gradient''' = ''-0.002,'' ''0.0,''\\ 
+      [#ws_vertical_gradient_level ws_vertical_gradient_level] = ''0.0,'' ''1000.0,''\\\\
+That defines the subsidence/ascent profile to be linear up to z = 1000.0 m with a surface value of 0 m/s. For z > 1000.0 m up to the top boundary the gradient is 0.0 (m/s) / 100 m (it is assumed that the assigned height levels correspond with uv levels).\\\\
+With an appropriate construction of '''w_subs''' the height of the boundary layer ''z_i'' can be kept approximately constant.\\\\
+'''Attention:'''\\
+The large scale vertical motion is only applied to the prognostic equation for the scalar quantities (potential temperature, humidity if [#humidity humidity] = ''.T.'' or passive scalar if [#passive_scalar passive_scalar] = ''.T.'') because it cannot be applied to the momentum equations due to incompressibility. Thus, the model is not mass consistent.
 }}}
 |----------------
@@ -423 +416 @@
 }}}
 {{{#!td
-
-        
-
-Height level from which on the gradient for the subsidence/ascent velocity defined by ws_vertical_gradient is effective (in m). 
-
-The height levels have to be assigned in ascending order. The default values result in a profile which is zero everywhere regardless of the values of ws_vertical_gradient. For the piecewise construction of the subsidence/ascent velocity profile see ws_vertical_gradient.
+Height level from which on the gradient for the subsidence/ascent velocity defined by [#ws_vertical_gradient ws_vertical_gradient] is effective (in m).\\\\
+The height levels have to be assigned in ascending order. The default values result in a profile which is zero everywhere regardless of the values of ws_vertical_gradient. For the piecewise construction of the subsidence/ascent velocity profile see [#ws_vertical_gradient ws_vertical_gradient].
 }}}
 [[BR]]