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Latent heat flux
Latent heat flux is the flux of heat from the Earth's surface to the atmosphere that is associated with evaporation of water at the surface and subsequent condensation of water vapor in the troposphere. It is an important component of Earth's surface energy budget. Latent heat flux is commonly measured with the Bowen ratio technique, or by eddy covariance.
|This article is licensed under the GNU Free Documentation License. It uses material from the Wikipedia article "Latent_heat_flux". A list of authors is available in Wikipedia.|