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Simple computational procedure whereby average daily potential evapotranspiration is represented as proportional to product of day-time hours squared and to saturated water vapor concentration at mean temperature; day time factor depends on consideration of disparity between net radiation and temperature, and fact that transpiration is restricted during darkness since leaf stomata are closed; comparison with C.W.Thornthwaite's method and other methods. (31 refs.)
Simple computational procedure whereby average daily potential evapotranspiration is represented as proportional to product of day-time hours squared and to saturated water vapor concentration at mean temperature; day time factor depends on consideration of disparity between net radiation and temperature, and fact that transpiration is restricted during darkness since leaf stomata are closed; comparison with C.W.Thornthwaite's method and other methods. (31 refs.)
Estimating Potential Evapotranspiration
Hamon, W. R. (author)
Journal of the Hydraulics Division ; 87 ; 107-120
2021-01-01
141961-01-01 pages
Article (Journal)
Electronic Resource
Unknown
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