Changes between Version 32 and Version 33 of doc/tec/microphysics

Timestamp:

May 22, 2018 3:02:29 PM (7 years ago)

Author:

schwenkel

Comment:

--

doc/tec/microphysics

@@ -129 +129 @@
 }}}
 where S is the supersaturation, ''R'',,c,, the integral radius and G(T,p) a function of temperature and pressure considering heat conductivity and diffusion.
-Using this explicit approach the used timestep must fulfill a new criterion, since it is assumed that the supersaturation is constant during one timestep. The typical timescale is given by 
-#!Latex
-\begin{align*}
-  & \left.\frac{\partial q_\mathrm{c}}{\partial t}
-  \right|_{\text{cond,evap}}= \frac{4
-  \pi\,G(T,p)}{\rho_\mathrm{a}}S\, R_\mathrm{c},
+Using this explicit approach the used timestep must fulfill a new criterion, since it is assumed that the supersaturation is constant during one timestep. The typical timescale is given by [#arnason1971 Arnason and Brown (1971)]
+#!Latex
+\begin{align*}
+  & \Delat t =
 \end{align*}
 }}}
@@ -411 +409 @@
 == References ==
 
-* [=#arnason1971]'''Arnason G, Brown J P S.''' 1971. Growth of cloud droplets by condensation: A problem in computational stability. J. Atmos. Sci. 28: 72-77.
+* [=#arnason1971]'''Arnason G, Brown J.''' 1971. Growth of cloud droplets by condensation: A problem in computational stability. J. Atmos. Sci. 28: 72-77.
 
 * [=#emanuel1994]'''Emanuel KA.''' 1994. Atmospheric Convection. Oxford University Press.