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Evapotranspiration is the net water loss caused by evaporation of moisture from the soil surface and transpiration by vegetation. Three conditions must be met for continuous evaporation. First, it requires latent heat of approximately 590 cal/g of water evaporated at 15 °C. Second, a vapor pressure gradient between the evaporative surface and the Evapotranspiration is the the combination of evaporation from the ground surface and transpiration by vegetation. It includes both evaporation of free water from the surface of vegetation and the land surface. It also includes transpiration which is the process of vegetation extracting it from the soil through the plant root system. ET_type Type of the estimation obtained which is Potential Evapotranspiration. message1 A message to inform the users about how solar radiation has been calculated by using which data. message5 A message to inform the users about if the Class-A pan evaporation is from actual data or from PenPan estimation. Evapotranspiration (ET) The combination of two separate processes whereby water is lost on the one hand from the soil surface by evaporation and on the other hand from the crop by transpiration is referred to as evapotranspiration (ET). Evaporation What is evapotranspiration (ET)? Evapotranspiration is a term to describe crop water demand by combining evaporation and transpiration. Evaporation is the process through which water is removed from moist soil and wet surfaces (such as dew on leaves). Transpiration is the process through which water is drawn up through the