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Evapotranspiration is one of the important components of the hydrological cycle; its estimation and analysis are crucial for better assessment of the hydrology of natural and reconstructed landscapes. The complexity of the evapotranspiration process have imposed some limitations on previously developed evapotranspiration estimation models. Limited literature exists on the modeling of actual evapotranspiration (AET), which depends on the available soil moisture, and is more complicated than the potential evapotranspiration . This book presents the modeling and analysis of AET using data...