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Based on ASTER(Advanced Spaceborne Thermal Emission and Reflection Radiometer) remote sensing data,bare soil evaporation was estimated with the Penman-Monteith model,the Priestley-Taylor model,and the aerodynamics model.Evaporation estimated by each of the three models was compared with actual evaporation,and error sources of the three models were analyzed.The mean absolute relative error was 9% for the Penman-Monteith model,14% for the Priestley-Taylor model,and 32% for the aerodynamics model;the Penman-Monteith model was the best of these three models for estimating bare soil evaporation.The error source of the Penman-Monteith model is the neglect of the advection estimation.The error source of the Priestley-Taylor model is the simplification of the component of aerodynamics as 0.72 times the net radiation.The error source of the aerodynamics model is the difference of vapor pressure and neglect of the radiometric component.The spatial distribution of bare soil evaporation is evident,and its main factors are soil water content and elevation.
Based on ASTER (Advanced Spaceborne Thermal Emission and Reflection Radiometer) remote sensing data, bare soil evaporation was estimated with the Penman-Monteith model, the Priestley-Taylor model, and the aerodynamics model. Evaporation estimated by each of the three models was compared with actual evaporation, and error sources of the three models were analyzed. The mean absolute relative error was 9% for the Penman-Monteith model, 14% for the Priestley-Taylor model, and 32% for the aerodynamics model; the Penman-Monteith model was the best of these three models for estimating bare soil evaporation. The error source of the Penman-Monteith model is the neglect of the advection estimation. The error source of the Priestley-Taylor model is the simplification of the component of aerodynamics as 0.72 times the net radiation. error source of the aerodynamics model is the difference of vapor pressure and neglect of the radiometric component. spatial distribution of bare soil evaporation is evident , and its main factors are soil water content and elevation.