Changes between Version 21 and Version 22 of doc/tec/lsm

Timestamp:

Apr 5, 2016 8:24:26 AM (9 years ago)

Author:

maronga

Comment:

--

doc/tec/lsm

@@ -228 +228 @@
 \end{equation*}
 }}}
-where ''m'',,total,, is the total water content of the soil. Only those layer are summed up which have a soil moisture above wilting point (plants do not extract water from such layers). The root extraction is then given by
+where ''m'',,total,, is the total water content of the soil and ''R'',,fr,, is the root fraction in soil layer ''k'. Only those layer are summed up which have a soil moisture above wilting point (plants do not extract water from such layers). The root profiles must prescribed in such a way that
+#!Latex
+\begin{equation*}
+\sum \limits_{k = 0}^3 R_\mathrm{fr}(k) = 1
+\end{equation*}
+}}}
+The root extraction is then given by
 {{{
 #!Latex
@@ -301 +307 @@
 * [=#clapp]'''Clapp, RB and Hornberger GM.''' 1978. Empirical Equations for Some Soil Hydraulic Properties. Water Res. Res., 14: 601-604.
  
-* [=#duynkerke]Duynkerke PG. 1999. Turbulence, radiation and fog in Dutch stable boundary layers. Boundary-Layer Meteorol. 90: 447–477, doi:10.1023/A:1026441904734.
+* [=#duynkerke]'''Duynkerke PG.''' 1999. Turbulence, radiation and fog in Dutch stable boundary layers. Boundary-Layer Meteorol. 90: 447–477, doi:10.1023/A:1026441904734.
 
 * [=#heus]'''Heus T, Van Heerwaarden CC, Jonker HJJ, Siebesma AP, Axelsen S, Dries K, Geoffroy O, Moene AF, Pino D, De Roode SR, Vil`a-Guerau de Arellano J.''' 2010. Formulation of the dutch atmospheric large-eddy simulation (dales) and overview of its applications. Geosci. Model Dev. 3: 415–444.