Changes between Version 57 and Version 58 of doc/tec/lsm

Timestamp:

Nov 20, 2019 11:45:12 AM (6 years ago)

Author:

maronga

Comment:

--

doc/tec/lsm

@@ -164 +164 @@
 \end{equation*}
 }}}
-where ''m'',,,liq,ref,,, = 0.2 mm is the reference liquid water column on a single leaf or bare soil. Exceeding liquid water is directly removed from the surface and infiltrated in the underlying soil. For positive values of ''LE'',,liq,,, liquid water is evaporating from the surface, while negative values indicate precipitation (rain, dew).
+where ''m'',,,liq,ref,,, = 0.2 mm is the reference liquid water column on a single leaf or bare soil. Exceeding liquid water is directly removed from the surface and infiltrated in the underlying soil. For positive values of ''LE'',,liq,,, liquid water is evaporating from the surface, while negative values indicate precipitation (rain, dew). The values of ''c,,,liq,,, are calculated either as the ratio
+{{{
+#!Latex
+\begin{equation*}
+m_\mathrm{liq} / m_\mathrm{liq,max}
+\end{equation*}
+}}}
+for vegetation (following the HTESSEL scheme, [#viterbo Viterbo & Beljaars, 1995]) and 
+{{{
+#!Latex
+\begin{equation*}
+m_\mathrm{liq} / m_\mathrm{liq,max})^{0.67}
+\end{equation*}
+}}}
+following [#masson Masson (2000)].
 
 == Soil model ==
@@ -428 +442 @@
 
 * [=#viterbo]'''Viterbo P, Beljaars ACM.''' 1995. An Improved Land Surface Parameterization Scheme in the ECMWF Model and Its Validation. J. Climate 8: 2716–2748.
+
+* [=#masson]'''Masson, V.''' 2000. A physically-based scheme for the urban energy budget in atmospheric models, Boundary-layer Meteorol., 94, 357–397.