Changes between Version 10 and Version 11 of doc/tec/lsf

Timestamp:

Nov 11, 2015 2:31:19 PM (10 years ago)

Author:

boeske

Comment:

--

doc/tec/lsf

@@ -9 +9 @@
 {{{
 #!Latex
-\[ \left. \dfrac{\partial \varphi}{\partial t} \right|_{\text{LS}} = - \left( u_{\text{LS}} \dfrac{\partial \varphi_{\text{LS}}}{\partial x \vphantom{y}} + v_{\text{LS}} \dfrac{\partial \varphi_{\text{LS}}}{\partial y} \right) \]
-}}}
-with
-{{{
-#!Latex
-\[ \varphi \in \{\theta,q\} \]
+$\left. \dfrac{\partial \varphi}{\partial t} \right|_{\text{LS}} = - \left( u_{\text{LS}} \dfrac{\partial \varphi_{\text{LS}}}{\partial x \vphantom{y}} + v_{\text{LS}} \dfrac{\partial \varphi_{\text{LS}}}{\partial y} \right)$ \quad with \quad $\varphi \in \{\theta,q\}$
 }}}
 to the prognostic equations. These tendencies are typically derived from larger scale models and should be spatially averaged over a large domain so that local-scale perturbations are avoided.
@@ -25 +20 @@
 {{{
 #!Latex
-\[ \left. \dfrac{\partial \varphi}{\partial t} \right|_{\text{subs}} = - w_{\text{subs}} \dfrac{\partial \varphi_{\text{LES}}}{\partial z \vphantom{y}} = - w_{\text{LS}} \dfrac{\partial \varphi_{\text{LES}}}{\partial z \vphantom{y}}.  \]
+$\left. \dfrac{\partial \varphi}{\partial t} \right|_{\text{subs}} = - w_{\text{subs}} \dfrac{\partial \varphi_{\text{LES}}}{\partial z \vphantom{y}} = - w_{\text{LS}} \dfrac{\partial \varphi_{\text{LES}}}{\partial z \vphantom{y}}.$
 }}}
 \\
@@ -31 +26 @@
 {{{
 #!Latex
-\[ \left. \dfrac{\partial \varphi}{\partial t} \right|_{\text{subs}} = - w_{\text{LS}} \dfrac{\partial \varphi_{\text{LS}}}{\partial z \vphantom{y}} . \]
+$\left. \dfrac{\partial \varphi}{\partial t} \right|_{\text{subs}} = - w_{\text{LS}} \dfrac{\partial \varphi_{\text{LS}}}{\partial z \vphantom{y}} .$
 }}}
 This method can be used by setting the control parameter [wiki:doc/app/inipar#use_subsidence_tendencies use_subsidence_tendencies] to ''.T.''.