Potential evaporation

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.

Contents

Estimates of potential evaporation (mm)

Thornthwaite equation (1948)

PET = 1.6 \left(\frac{L}{12}\right)\left(\frac{N}{30}\right)\left(\frac{10\, T_a}{I}\right)^\alpha

Where

PET is the estimated potential evapotranspiration (cm/month)

T_a is the average daily temperature (degrees Celsius; if this is negative, use 0) of the month being calculated

N is the number of days in the month being calculated

L is the average day length (hours) of the month being calculated

\alpha = (6.75 \times 10^{-7}) I^3 - (7.71 \times 10^{-5}) I^2 %2B (1.792 \times 10^{-2}) I %2B 0.49239

I = \sum_{i=1}^{12} \left(\frac{T_{ai}}{5}\right)^{1.514} is a heat index which depends on the 12 monthly mean temperatures T_{ai}.[1]

Somewhat modified forms of this equation appear in later publications (1955 and 1957) by Thornthwaite and Mather. [2]

Penman equation (1948)

Penman-Monteith equation (1965)

See also

References

External links