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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.
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.
Estimating potential evapotranspiration
ASCE -- Proc (J Hydraulics Div)
Hamon, W.R. (author)
1961
14 pages
Article (Journal)
English
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Estimating Potential Evapotranspiration
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Discussion of “Estimating Potential Evapotranspiration”
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