Changes between Version 135 and Version 136 of doc/app/particle_parameters

Timestamp:

Apr 15, 2016 12:24:40 PM (9 years ago)

Author:

hoffmann

Comment:

--

doc/app/particle_parameters

@@ -141 +141 @@
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 {{{#!td
-Parameter to consider solution and curvature effects on the equilibrium vapor pressure of cloud droplets.
-
-This parameter only comes into effect if Lagrangian cloud droplets are used (see [#cloud_droplets cloud_droplets]) and if the droplet radius is smaller than ''1.0E-6'' m. In case of '''curvature_solution_effects''' = ''.T.'', solution and curvature effects are included in the growth equation of droplets by condensation. Since in this case the growth equation is a stiff o.d.e, it is integrated in time using the Rosenbrock method (see Numerical Recipes in FORTRAN, 2nd Edition, p.731). If the droplet radius is larger or equal ''1.0E-6'' m, solution and curvature effects are neglected and the growth is calculated by a simple analytic formula (as for '''curvature_solution_effects''' = ''.F.'').\\\\
-'''Attention:''' '''curvature_solution_effects''' = ''.T.'' may significantly increase CPU time of jobs.
+Parameter to consider solution and curvature effects on the equilibrium vapor pressure of cloud droplets. For the initialization of the corresponding dry aerosol spectrum, see [#init_aerosol_probabilistic init_aerosol_probabilistic].In this case, the radius growth equation is a stiff o.d.e, which is integrated in time using a Rosenbrock method (see Numerical Recipes in FORTRAN, 2nd Edition, p.731). '''curvature_solution_effects''' = ''.T.'' may significantly increase CPU time of jobs.
 }}}
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