The FAO Penman-Monteith method is maintained as the sole standard method for the computation of ETo from meteorological data.
cal_ET0_from_PM(delta, Rn, G, gamma, Tem, u2, es, ea)
A vector for reference evapotranspiration [mm day-1].
slope vapour pressure curve (kPa °C). From cal_slopeOfSaturationVapourPressureCurve()
net Radiation at the crop surface [MJ m-2 day-1]. From cal_netRadiation()
soil heat flux density [MJ m-2 day-1].
psychrometric constant (kPa °C).
air temperature at 2 m height [°C].
wind speed at 2 m height [m s-1].
saturation vapour pressure [kPa].
actual vapour pressure [kPa].
Allen, R. G., Pereira, L. S., Raes, D., & Smith, M. FAO Irrigation and drainage paper No. 56. Rome: Food and Agriculture Organization of the United Nations, 1998.