Potential evaporation or potential evapotranspiration (PET) is defined as the amount of evaporation that would occur if a sufficient water source were available. If the actual evapotranspiration is considered the net result of atmospheric demand for moisture from a surface and the ability of the surface to supply moisture, then PET is a measure of the demand side. Surface and air temperatures, insolation, and wind all affect this. A dryland is a place where annual potential evaporation exceeds annual precipitation.
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Where
is the estimated potential evapotranspiration (cm/month)
is the average daily temperature (degrees Celsius; if this is negative, use ) of the month being calculated
is the number of days in the month being calculated
is the average day length (hours) of the month being calculated
is a heat index which depends on the 12 monthly mean temperatures .[1]
Somewhat modified forms of this equation appear in later publications (1955 and 1957) by Thornthwaite and Mather. [2]