Changes between Version 401 and Version 402 of doc/app/initialization_parameters

Timestamp:

Sep 26, 2018 1:17:14 PM (6 years ago)

Author:

schwenkel

Comment:

--

doc/app/initialization_parameters

@@ -8 +8 @@
 ==== [#ini Initialization] ====
 ==== [#topo Topography] ====
-==== [#cphys Cloud physics] 
 ==== [#others Others] ====
 \\\\
@@ -255 +254 @@
 Parameter to switch on the prognostic equation for the water vapor mixing ratio 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 water mixing ratio (sum of water vapor and liquid water).
+If the bulk cloud model is switched on (see [../bcmpar#bulk_cloud_model bulk_cloud_model] = ''.T.''), q becomes the total water mixing ratio (sum of water vapor and liquid water). The bulk cloud model physics must be steered via  [../bcmpar bulk cloud parameters]. 
 }}}
 |----------------
@@ -2593 +2592 @@
 {{{#!td
 Atmospheric pressure at the surface (in hPa).\\\\ 
-Starting from this surface value, the vertical pressure profile is calculated once at the beginning of the run assuming a neutrally stratified atmosphere. This is needed for converting between the liquid water potential temperature and the potential temperature (see [#cloud_physics cloud_physics]).
+Starting from this surface value, the vertical pressure profile is calculated once at the beginning of the run assuming a neutrally stratified atmosphere. This is needed for converting between the liquid water potential temperature and the potential temperature (see [../bcmpar#bulk_cloud_model bulk_cloud_model] = ''.T.'').
 }}}
 |----------------