Changes between Version 36 and Version 37 of doc/app/bulk_cloud_parameters

Timestamp:

Feb 7, 2021 10:25:30 AM (4 years ago)

Author:

wagner

Comment:

--

doc/app/bulk_cloud_parameters

@@ -34 +34 @@
       It is assumed that the aerosol is ammonium sulfate. \\\\
 The molecular weight, denisty and the solubility (vant Hoff factor)  of this specific type is considered.
+}}}
+|----------------
+{{{#!td style="vertical-align:top;width: 150px"
+[=#bulk_cloud_model '''bulk_cloud_model''']
+}}}
+{{{#!td style="vertical-align:top;width: 50px"
+L
+}}}
+{{{#!td style="vertical-align:top;width: 75px"
+.F.
+}}}
+{{{#!td
+
 }}}
 |----------------
@@ -160 +173 @@
 |----------------
 {{{#!td style="vertical-align:top;width: 150px"
+[=#ice_crystal_sedimentation '''ice_crystal_sedimentation''']
+}}}
+{{{#!td style="vertical-align:top;width: 50px"
+L
+}}}
+{{{#!td style="vertical-align:top;width: 75px"
+.F.
+}}}
+{{{#!td
+Parameter to consider sedimentation of ice crystal according to Seifert and Beheng 2006.
+
+This parameter only comes into effect if the microphysical cloud scheme according to Seifert and Beheng (2006) ([#cloud_scheme cloud_scheme] = 'seifert_beheng') or by Morrison et al. (2005)  ([#cloud_scheme cloud_scheme] = 'morrison') in combination with ice microphyiscs  ([#microphysics_ice_phase microphysics_ice_phase] = .TRUE.) is used.
+}}}
+|----------------
+{{{#!td style="vertical-align:top;width: 150px"
+[=#in_init '''in_init''']
+}}}
+{{{#!td style="vertical-align:top;width: 50px"
+R
+}}}
+{{{#!td style="vertical-align:top;width: 75px"
+1000.0
+}}}
+{{{#!td
+
+}}}
+
+|----------------
+{{{#!td style="vertical-align:top;width: 150px"
 [=#limiter_sedimentation '''limiter_sedimentation''']
 }}}
@@ -174 +216 @@
 
 If [#c_sedimentation c_sedimentation] <= 1.0 there is no need to use the limiter.
-}}}
-|----------------
-{{{#!td style="vertical-align:top;width: 150px"
-[=#ice_crystal_sedimentation '''ice_crystal_sedimentation''']
-}}}
-{{{#!td style="vertical-align:top;width: 50px"
-L
-}}}
-{{{#!td style="vertical-align:top;width: 75px"
-.F.
-}}}
-{{{#!td
-Parameter to consider sedimentation of ice crystal according to Seifert and Beheng 2006.
-
-This parameter only comes into effect if the microphysical cloud scheme according to Seifert and Beheng (2006) ([#cloud_scheme cloud_scheme] = 'seifert_beheng') or by Morrison et al. (2005)  ([#cloud_scheme cloud_scheme] = 'morrison') in combination with ice microphyiscs  ([#microphysics_ice_phase microphysics_ice_phase] = .TRUE.) is used.
 }}}
 |----------------
@@ -220 +247 @@
 |----------------
 {{{#!td style="vertical-align:top;width: 150px"
-[=#ni_init '''ni_init''']
-}}}
-{{{#!td style="vertical-align:top;width: 50px"
-R
-}}}
-{{{#!td style="vertical-align:top;width: 75px"
-1.0E3
-}}}
-{{{#!td
-Background initial ice nucleii concentration. If [#microphysics_ice_phase microphysics_ice_phase] = .TRUE., this parameter is used for the nucleation process calculating the resulting number of ice crystals.  
-}}}
-|----------------
-{{{#!td style="vertical-align:top;width: 150px"
 [=#nc_const '''nc_const''']
 }}}
@@ -286 +300 @@
 }}}
 |----------------
+{{{#!td style="vertical-align:top"
+[=#switch_off_module '''switch_off_module''']
+}}}
+{{{#!td style="vertical-align:top"
+L
+}}}
+{{{#!td style="vertical-align:top"
+.F.
+}}}
+{{{#!td
+
+}}}
+
+|----------------
 {{{#!td style="vertical-align:top;width: 150px"
 [=#ventilation_effect '''ventilation_effect''']