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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: | , , , |
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Natura: | Artigo |
Lingua: | Inglês |
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Copernicus Publications
2013-11-01
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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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