Abstract
It is of great significance for the validation of remotely sensed evapotranspiration (ET) products to solve the spatial-scale mismatch between site observations and remote sensing estimations. To overcome this challenge, this paper proposes a comprehensive framework for obtaining the ground truth ET at the satellite pixel scale (1 × 1 km resolution in MODIS satellite imagery). The main idea of this framework is to first quantitatively evaluate the spatial heterogeneity of the land surface, then combine the eddy covariance (EC)-observed ET (ET_EC) to be able to compare and optimize the upscaling methods (among five data-driven and three mechanism-driven methods) through direct validation and cross-validation, and finally use the optimal method to obtain the ground truth ET at the satellite pixel scale. The results showed that the ET_EC was superior over homogeneous underlying surfaces with a root mean square error (RMSE) of 0.34 mm/d. Over moderately and highly heterogeneous underlying surfaces, the Gaussian process regression (GPR) method performed better (the RMSEs were 0.51 mm/d and 0.60 mm/d, respectively). Finally, an integrated method (namely, using the ET_EC for homogeneous surfaces and the GPR method for moderately and highly heterogeneous underlying surfaces) was proposed to obtain the ground truth ET over fifteen typical underlying surfaces in the Heihe River Basin. Furthermore, the uncertainty of ground truth ET was quantitatively evaluated. The results showed that the ground truth ET at the satellite pixel scale is relatively reliable with an uncertainty of 0.02–0.41 mm/d. The upscaling framework proposed in this paper can be used to obtain the ground truth ET at the satellite pixel scale and its uncertainty, and it has great potential to be applied in more regions around the globe for remotely sensed ET products’ validation.
Highlights
IntroductionThe evapotranspiration (ET) of the land surface is a significant part of the global hydrologic cycle and plays an important role among climate systems, energy balance processes, and carbon cycles [1]
Remote sensing technology is effective for monitoring ET [3], and a variety of remotely sensed ET products have been produced and available, such as the Moderate Resolution Imaging Spectroradiometer (MODIS) Global Evapotranspiration
The ground truth ET at the satellite pixel scale over fifteen typical underlying surfaces in the HRB was obtained by satellite pixel scale over fifteen typical underlying surfaces in the HRB was obtained by an an integrated method, and the uncertainty of the ground truth ET was analyzed
Summary
The evapotranspiration (ET) of the land surface is a significant part of the global hydrologic cycle and plays an important role among climate systems, energy balance processes, and carbon cycles [1]. Accurate monitoring and estimations of ET are critical for water resource management and for modeling regional and global climate and hydrological cycles [2]. Remote sensing technology is effective for monitoring ET [3], and a variety of remotely sensed ET products have been produced and available, such as the Moderate Resolution Imaging Spectroradiometer (MODIS) Global Evapotranspiration. It is significant to validate remotely sensed ET products before being used in practical applications
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