LatentHeatFlux_PenmanMonteith_gsinvert: Calculate the surface conductance by inverting the...

In laubblatt/phaselag: Calculate the phase lag between two variables

Description

Calculate the surface conductance by inverting the Penman-Monteith formulation

Usage

LatentHeatFlux_PenmanMonteith_gsinvert(AE, s, esurf, eair, ga, LE,
  rho = 1.2, cp = 1004, psychro = 0.65)

Arguments

AE	Available Energy usually Net Radiation - Soil Heat flux in W m-2
s	slope of the saturation vapor pressure curve in hPa/K
esurf	surface water vapour pressure hPa
eair	vapour pressure in air hPa
ga	aerodynamic conductance for water vapor in m/s
LE	Latent Heat flux in W/m2
rho	Air density kg/m3
cp	heat capacity of air J/(kg K)
psychro	psychrometric constant hPa/K

Value

gs surface / or stomatal conductance for water vapor in m/s

Author(s)

Maik Renner, mrenner [at] bgc-jena.mpg.de

See Also

[aerodynamic_conductance_withcanopy_Thom1975()] ga needs a leaf boundary layer conductance (also known as excess resistance)

laubblatt/phaselag documentation built on Sept. 30, 2020, 11:21 a.m.