The evapotranspiration calculated by the above seven models, together with precipitation, is used in the water balance model to calculate other water balance components. the Makkink model and the Priestley–Taylor model. the Thornthwaite model and the Hargreaves model, and the other two belong to the radiation-based category, i.e. Two of the four potential evapotranspiration models belong to the temperature-based category, i.e. the CRAE model of Morton, the advection–aridity (AA) model of Brutsaert and Stricker, and the GG model of Granger and Gray, and four models calculate first potential evapotranspiration and then actual evapotranspiration by considering the soil moisture condition. Of the seven evapotranspiration models evaluated, three models calculate actual evapotranspiration directly using the complementary relationship approach, i.e. This study evaluates seven evapotranspiration models and their performance in water balance studies by using lysimeter measurement data at the M¨onchengladbach hydrological and meteorological station in Germany.
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