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Potential evaporation estimation through an unstressed surface-energy balance and its sensitivity to climate change

Potential evaporation (ET<sub>P</sub>) is a basic input for many hydrological and agronomic models, as well as a key variable in most actual evaporation estimations. It has been approached through several diffusive and energy balance methods, out of which the Penman–Monteith equation is...

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Autori principali: A. Barella-Ortiz, J. Polcher, A. Tuzet, K. Laval
Natura: Artigo
Lingua:Inglês
Pubblicazione: Copernicus Publications 2013-11-01
Serie:Hydrology and Earth System Sciences
Accesso online:http://www.hydrol-earth-syst-sci.net/17/4625/2013/hess-17-4625-2013.pdf
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