Changes between Version 13 and Version 14 of doc/app/bcmequ

Timestamp:

May 11, 2020 11:35:10 AM (5 years ago)

Author:

schwenkel

Comment:

--

doc/app/bcmequ

@@ -104 +104 @@
 }}}
 
+{{{#!td style="vertical-align:top; text-align:left"
 '''Morrison no rain'''
 
-Instead of using the Morrison scheme as an extension of the Seifert Beheng scheme. The extension are used as a stand-alone scheme. Therefore, rain processes are neglected but explicit consideration of diffusional growth and activation with prognostic quantities of ''N'',,c,, and ''q'',,c,,. This scheme might be appropriate for fog simulation.
+Instead of using the Morrison scheme as an extension of the Seifert Beheng scheme. The extension are used as a stand-alone scheme. Therefore, rain processes are neglected but explicit consideration of diffusional growth and activation with prognostic quantities of ''N'',,c,, and ''q'',,c,,. This scheme is computational inexpensive and appropiate for conditions where teh production of rain can be neglected (i.e. fog).
+}}}
+{{{#!td style="text-align:left;style=width: 50px"
+[[Image(morrison_no_rain.png)]]
+}}}
 
 In the next subsections we will describe the diagnostic/prognostic determination (in dependence of the chosen scheme) of ''q'',,c,,. From Sect. [wiki:doc/tec/microphysics#Autoconversion autoconversion] on, the microphysical processes considered in the sink/source terms of ''θ'',,l,,, ''q'', ''N'',,r,, and ''q'',,r,,, as well as ''N'',,c,, and ''q'',,c,, for the [#morrison2007 Morrison et al. (2007)] scheme.