Atmospheric demand: Difference between revisions

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Revision as of 16:28, 26 January 2012



atmospheric demand[edit | edit source]

The evapotranspiration that would be achieved from a well-aerated soil/ plant surface at field water-holding capacity.

Water loss may differ from pan evaporation according to the index of evaporating surface to horizontal area, roughness, and other physical and biological attributes of a site.


The evapotranspiration that would be achieved from a well-aerated soil/ plant surface at field water-holding capacity.

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