Forest Evapotranspiration
Forest Evapotranspiration is a hydrological flux representing the total water vapor returned to the atmosphere from forested ecosystems through the combined processes of soil evaporation and plant transpiration, distinguished by its specific dependence on forest canopy structure, species composition, and ecosystem-level physiological controls.
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Kell Wilson, Paul J. Hanson, Patrick J. Mulholland et al. · Agricultural and Forest Meteorology · 2001 · 778 citations
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Chinese Academy of Sciences
Beijing, China
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University of British Columbia
Vancouver, Canada
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Duke University
Durham, United States
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University of Chinese Academy of Sciences
Beijing, China
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University of California, Berkeley
Berkeley, United States
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Nagoya University
Nagoya, Japan
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Kyoto University
Kyoto, Japan
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US Forest Service
Washington, United States
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