Changes between Version 165 and Version 166 of doc/app/particle_parameters

Timestamp:

Jul 14, 2017 4:55:58 PM (8 years ago)

Author:

hoffmann

Comment:

--

doc/app/particle_parameters

@@ -5 +5 @@
 
 ||='''Parameter Name'''  =||='''[../fortrantypes FORTRAN Type]'''  =||='''Default Value'''  =||='''Explanation'''  =||
+|----------------
+{{{#!td style="vertical-align:top; text-align:left;width: 150px"
+[=#aero_type '''aero_type''']
+}}}
+{{{#!td style="vertical-align:top; text-align:left;style="width: 50px"
+C*15
+}}}
+{{{#!td style="vertical-align:top; text-align:left;style="width: 75px"
+maritime
+}}}
+{{{#!td
+Define a aerosol spectrum using three log-normal distributions and the values stated in Jaenicke (1993, doi: 10.1016/S0074-6142(08)60210-7). Possible values are 'polar', 'background', 'maritime', 'continental', 'desert', 'rural', and 'urban'. If 'user' is chosen, the aerosol spectrum is steered by [#rm rm], [#na na], and [#log_sigma log_sigma]. Note that [#curvature_solute_effects curvature_solute_effects] needs to be true to consider aerosol spectra. Note that this aerosol spectrum spectrum determines the aerosol mass, initial wet radius, and the weighting factor of all super-droplets. The weighting factors can be manipulated with [#aero_weight aero_weight].
+}}}
+|----------------
+{{{#!td style="vertical-align:top; text-align:left;width: 150px"
+[=#aero_weight '''aero_weight''']
+}}}
+{{{#!td style="vertical-align:top; text-align:left;style="width: 50px"
+R
+}}}
+{{{#!td style="vertical-align:top; text-align:left;style="width: 75px"
+1.0
+}}}
+{{{#!td
+Scale the number concentration defined by [#aero_type aero_type] to the desired amount of aerosols by keeping the typical shape of the spectrum. 
+}}}
 |----------------
 {{{#!td style="vertical-align:top; text-align:left;width: 150px"