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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. (Autor:in)
Journal of the Hydraulics Division ; 87 ; 107-120
01.01.2021
141961-01-01 pages
Aufsatz (Zeitschrift)
Elektronische Ressource
Unbekannt
Estimating potential evapotranspiration
Engineering Index Backfile | 1961
|Estimating Potential Evapotranspiration
ASCE | 2021
|Discussion of “Estimating Potential Evapotranspiration”
ASCE | 2021
|Closure to “Estimating Potential Evapotranspiration”
ASCE | 2021
|Estimating evapotranspiration from solar radiation
Engineering Index Backfile | 1963
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