Changes between Version 42 and Version 43 of doc/tec/microphysics

Timestamp:

May 25, 2018 8:51:22 AM (7 years ago)

Author:

schwenkel

Comment:

--

doc/tec/microphysics

@@ -84 +84 @@
 \end{align*}
 }}}
-where ''N'',,CCN,, is the number of activated aerosols, ''N'',,0,, is the number concentration of dry aerosol, S is the supersaturation and k is power index between 0 and 1.
- In PALM the supersaturation is calculated explicitly by their thermodynamic fields of potential temperature and water vapor mixing ratio. 
+where ''N'',,CCN,, is the number of activated aerosols, ''N'',,0,, is the number concentration of dry aerosol, S is the supersaturation and k is power index between 0 and 1. In PALM the supersaturation is calculated explicitly by their thermodynamic fields of potential temperature and water vapor mixing ratio. However, curvature and solution effects can be considered with an analytical extension of the Twomey type activation scheme of [#khvorostyanov2006 Khvorostyanov and Curry (2006)].
 == Diffusional growth of cloud water ==
 
@@ -467 +466 @@
 * [=#cuijpers1993]'''Cuijpers JWM, Duynkerke PG.''' 1993. Large eddy simulation of trade wind cumulus clouds. J. Atmos. Sci. 50: 3894–3908.
 
-* [=#Khvorostyanov2006] '''Khvorostyanov V,  Curry J.''' 2006. Aerosol size spectra and CCN activity spectra: Reconciling the lognormal, algebraic, and power laws. s. J. Geophys. Res. 111.
+* [=#khvorostyanov2006]'''Khvorostyanov V,  Curry J.''' 2006. Aerosol size spectra and CCN activity spectra: Reconciling the lognormal, algebraic, and power laws. J. Geophys. Res. 111.
 
 * [=#dipankar2015]'''Dipankar A, Stevens B, Heinze R, Moseley C, Zängl G, Giorgetta M, Brdar D.''' 2015. Large eddy simulation using the general circulation model ICON. J. Adv. Mod. Earth Syst. 07. [http://dx.doi.org/10.1002/2015MS000431 doi].