LE.to.ET

ET.to.LE

converts evaporative water flux from mass (ET=evapotranspiration)
 to energy (LE=latent heat flux) units, or vice versa.

Calculation of physical (e.g. aerodynamic conductance, surface temperature),
and physiological (e.g. canopy conductance, water-use efficiency) ecosystem properties
from eddy covariance data and accompanying meteorological measurements. Calculations
assume the land surface to behave like a 'big-leaf' and return bulk ecosystem/canopy variables.

Juergen Knauer

bigleaf

Physical and Physiological Ecosystem Properties from Eddy
Covariance Data

Thomas Wutzler

Alison Bennett

Soenke Zaehle

Tarek El-Madany

Mirco Migliavacca

LE.to.ET function

<dl><dt>LE</dt>
<dd>Latent heat flux (W m-2)</dd>
<dt>Tair</dt>
<dd>Air temperature (deg C)</dd>
<dt>ET</dt>
<dd>Evapotranspiration (kg m-2 s-1)</dd></dl>

Arguments

Conversion between Latent Heat Flux and Evapotranspiration — LE.to.ET

<dl>

<dt>LE</dt>
<dd>Latent heat flux (W m-2)</dd>


<dt>Tair</dt>
<dd>Air temperature (deg C)</dd>


<dt>ET</dt>
<dd>Evapotranspiration (kg m-2 s-1)</dd>

</dl>

LE.to.ET: Conversion between Latent Heat Flux and Evapotranspiration

Description

Usage

Arguments

Details

Examples