Changes between Version 248 and Version 249 of doc/app/initialization_parameters

Timestamp:

Dec 2, 2014 5:30:30 PM (10 years ago)

Author:

maronga

Comment:

--

doc/app/initialization_parameters

@@ -46 +46 @@
 {{{#!td
 Parameter to switch on the condensation scheme.\\\\ 
-For '''cloud_physics''' = ''.T.'', equations for the total water content and the liquid water potential temperature are solved instead of those for specific humidity and potential temperature. Note that a grid volume is assumed to be either completely saturated or completely unsaturated (0%-or-100%-scheme). Precipitation can additionally be switched on with parameter [#precipitation precipitation]. The parameterization of cloud and precipitation physics can be steered with [#cloud_scheme cloud_scheme]. Also cloud-top cooling by longwave radiation can be utilized (see [#radiation radiation]).\\\\
+For '''cloud_physics''' = ''.T.'', equations for the total water content and the liquid water potential temperature are solved instead of those for specific humidity and potential temperature. Note that a grid volume is assumed to be either completely saturated or completely unsaturated (0%-or-100%-scheme). Precipitation can additionally be switched on with parameter [#precipitation precipitation]. The parameterization of cloud and precipitation physics can be steered with [#cloud_scheme cloud_scheme]. Also cloud-top cooling by longwave radiation can be utilized (see [#cloud_top_radiation cloud_top_radiation]).\\\\
 '''cloud_physics''' = ''.T.'' requires [#humidity humidity] = ''.T.''.\\\\
 Detailed information about the condensation scheme is given in the description of the [[cloud physics module]] (pdf-file).\\\\
@@ -69 +69 @@
       One-moment cloud microphysics according to Kessler (1969). Steering parameter: [#precipitation precipitation]\\\\
 Both schemes are based on a 0%-100%-scheme to diagnose the cloud water content and differ in the precipitation process. Therefore, it is not allowed to choose [#cloud_scheme cloud_scheme] = 'seifert_beheng' if precipitation is not allowed ([#precipitation precipitation] = .F.) in order to save computational resources.   
+}}}
+|----------------
+{{{#!td style="vertical-align:top"
+[=#cloud_top_radiation '''cloud_top_radiation''']
+}}}
+{{{#!td style="vertical-align:top"
+L
+}}}
+{{{#!td style="vertical-align:top"
+.F.
+}}}
+{{{#!td
+Parameter to switch on longwave radiation cooling at cloud-tops.\\\\
+Long-wave radiation processes are parameterized by the effective emissivity, which considers only the absorption and emission of long-wave radiation at cloud droplets. The radiation scheme can be used only with [#cloud_physics cloud_physics] = ''.T.''.
 }}}
 |----------------
@@ -403 +417 @@
 '''Attention:'''\\
 This parameter has no effect in case of ocean runs (see [#ocean ocean]), where potential density is used in the buoyancy term (see [#reference_state reference_state] for more details).
-}}}
-|----------------
-{{{#!td style="vertical-align:top"
-[=#radiation '''radiation''']
-}}}
-{{{#!td style="vertical-align:top"
-L
-}}}
-{{{#!td style="vertical-align:top"
-.F.
-}}}
-{{{#!td
-Parameter to switch on longwave radiation cooling at cloud-tops.\\\\
-Long-wave radiation processes are parameterized by the effective emissivity, which considers only the absorption and emission of long-wave radiation at cloud droplets. The radiation scheme can be used only with [#cloud_physics cloud_physics] = ''.T.''.
 }}}
 |----------------