varwg.meteo.meteox2y.penman_monteith¶
- varwg.meteo.meteox2y.penman_monteith(at, u, Rn, rh)[source]¶
Calculates the reference crop evaporation following the Penman-Monteith method and the FAO-56 determinations published in ASCE Standardized Reference Evapotranspiration Equation
- Parameters:
- atnp.array of floats
mean daily air temperature at 2m-height [deg C]
- unp.array of floats
mean daily wind speed at 2m-height [m/s]
- Rnnp.array of floats
measured net radiation at the crop surface [MJ m^-2 d^-1]
- rhnp.array of floats
relative humidity [%]
- Returns:
- etonp.array of floats
- FAO Penman-Monteith standardized reference crop evapotranspiration for
short (~=0.12m) surfaces [mm d^-1]
Notes
Units for the 0.408 coefficient are m^2 mm MJ^-1
The FAO-56 Penman-Monteith equation is a grass reference equation that was derived from the Penman-Monteith form of the combination equation (Monteith 1965, 1981) by fixing h = 0.12 m for clipped grass and by assuming measurement heights of z = 2 m (at, rh, u) and using a latent heat of vaporization of 2.45 MJ kg-1. The result is an equation that defines the reference evapotranspiration from a hypothetical grass surface having a fixed height of 0.12 m, bulk surface resistance of 70 s m-1, and albedo of 0.23.
in relationship to the net radiation, the soil heat flux is very small and is fixed with G = 0.1*Rn