Changes between Version 489 and Version 490 of doc/app/initialization_parameters

Timestamp:

Feb 25, 2021 4:05:45 PM (4 years ago)

Author:

wagner

Comment:

--

doc/app/initialization_parameters

@@ -267 +267 @@
 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 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]. 
+If the bulk cloud model is switched on (see [../bulk_cloud_parameters#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  [../bulk_cloud_parameters bulk cloud parameters]. 
 }}}
 |----------------
@@ -2575 +2575 @@
 {{{#!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 [../bcmpar#bulk_cloud_model bulk_cloud_model] = ''.T.'').
+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 [../bulk_cloud_parameters#bulk_cloud_model bulk_cloud_model] = ''.T.'').
 }}}
 |----------------