Changes between Version 26 and Version 27 of doc/tec/microphysics

Timestamp:

May 22, 2018 2:12:36 PM (7 years ago)

Author:

schwenkel

Comment:

--

doc/tec/microphysics

@@ -77 +77 @@
 == Diffusional growth of cloud water ==
 
-The diagnostic estimation of ''q'',,c,, is based on the assumption that water supersaturations are immediately removed by the diffusional growth of cloud droplets only. This can be justified since the bulk surface area of cloud droplets exceeds that of rain drops considerably ([#stevens2008 Stevens and Seifert, 2008]). Following this saturation adjustment approach, ''q'',,c,, is obtained by
+By the usage of [#seifert2001 Seifert and Beheng (2001],[#seifert2006  2006)] the diagnostic estimation of ''q'',,c,, is based on the assumption that water supersaturations are immediately removed by the diffusional growth of cloud droplets only. This can be justified since the bulk surface area of cloud droplets exceeds that of rain drops considerably ([#stevens2008 Stevens and Seifert, 2008]). Following this saturation adjustment approach, ''q'',,c,, is obtained by
 {{{
 #!Latex
@@ -119 +119 @@
 }}}
 
+In contrast to that an explicit approach for the diffusional growth is applied in case of [#morrison2007 Morrison (2007)]. The condensation rate is calculated follwoing 
 == Autoconversion ==
 
@@ -406 +407 @@
 * [=#bougeault1981]'''Bougeault, P.''' 1981. Modeling the trade-wind cumulus boundary layer. Part I: Testing the ensemble cloud relations against numerical data. J. Atmos. Sci. 38: 2414–2428.
 
+* [=#khairoutdinov2000]'''Khairoutdinov M, Kogan Y.''' 2000. A new cloud physics parameterization in a large-eddy simulation model of marine stratocumulus. Mon. Weat. Rev. 128: 229–243.
+
 * [=#sommeria1977]'''Sommeria G, Deardorff JW.''' 1977. Subgrid-scale condensation in models of nonprecipitating clouds. J. Atmos. Sci. 34: 344–355.