Changes between Version 65 and Version 66 of doc/tec/lsm

Timestamp:

Jul 21, 2022 1:41:18 PM (3 years ago)

Author:

maronga

Comment:

--

doc/tec/lsm

@@ -16 +16 @@
 \end{equation*}
 }}}
-where ''C'',,0,, and ''T'',,0,, are the heat capacity and radiative temperature of the surface skin layer, respectively. Note that  ''C'',,0,, is usually zero as it is assumed that the skin layer does not have a heat capacity (see also below). ''R'',,n,,, ''H'', ''LE'', and ''G'' are the net radiation, sensible heat flux, latent heat flux, and ground (soil) heat flux at the surface, respectively. 
+where ''C'',,0,, and ''T'',,0,, are the heat capacity and radiative temperature of the surface skin layer, respectively. Note that  ''C'',,0,, is usually zero as it is assumed that the skin layer has no vertical extent and thus does not have a heat capacity (see also below). ''R'',,n,,, ''H'', ''LE'', and ''G'' are the net radiation, sensible heat flux, latent heat flux, and ground (soil) heat flux at the surface, respectively. 
 
 === Parameterization of ''H'' ===
@@ -43 +43 @@
 \end{equation*}
 }}}
-with ''Λ'' being the total thermal conductivity between skin layer and the uppermost soil layer, and ''T'',,soil,1,, being the temperature of the uppermost soil layer. ''Λ''  is calculated as a combination of the conductivity between the canopy and the soil-top (constant value) and the conductivity of the top half of the uppermost soil layer:
+with ''Λ'' being the total thermal conductivity between the skin and the center of the uppermost soil layer, and ''T'',,soil,1,, being the temperature of the uppermost soil layer. ''Λ''  is calculated as a combination of the conductivity between the canopy and the soil-top (constant value) and the conductivity of the top half of the uppermost soil layer:
 {{{
 #!Latex