The Evapotranspiration (ET) method is a widely used technique for determining the amount of water needed by crops. It accounts for both evaporation from the soil surface and transpiration from plant leaves.
Rainfall data is crucial as it reduces the need for irrigation when natural precipitation meets or exceeds the crop’s water requirements.
ET = Evapotranspiration
Delta = Slope of the saturation vapor pressure curve
R_n = Net radiation at the crop surface
G = Soil heat flux density
gamma = Psychrometric constant
u_2 = Wind speed at 2 meters height
e_s = Saturation vapor pressure at air temperature
e_a = Actual vapor pressure in the atmosphere
lambda = Latent heat of vaporization of water
What is Evapotranspiration (ET) in agriculture?
How does rainfall affect irrigation schedules?
What are the key variables in the ET formula?
How do I interpret the result from this calculator?
Can this calculator be used for all types of crops?
What is the significance of wind speed in the ET calculation?
How often should I update my irrigation schedule using this calculator?
Results are for informational purposes only and do not constitute professional advice.
