Upscaling Evapotranspiration from a Single-Site to Satellite Pixel Scale

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...

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Main Authors: Xiang Li, Shaomin Liu, Xiaofan Yang, Yanfei Ma, Xinlei He, Ziwei Xu, Tongren Xu, Lisheng Song, Yuan Zhang, Xiao Hu, Qian Ju, Xiaodong Zhang
Format: Article
Language:English
Published: MDPI AG 2021-10-01
Series:Remote Sensing
Subjects:
Online Access:https://www.mdpi.com/2072-4292/13/20/4072
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author Xiang Li
Shaomin Liu
Xiaofan Yang
Yanfei Ma
Xinlei He
Ziwei Xu
Tongren Xu
Lisheng Song
Yuan Zhang
Xiao Hu
Qian Ju
Xiaodong Zhang
author_facet Xiang Li
Shaomin Liu
Xiaofan Yang
Yanfei Ma
Xinlei He
Ziwei Xu
Tongren Xu
Lisheng Song
Yuan Zhang
Xiao Hu
Qian Ju
Xiaodong Zhang
author_sort Xiang Li
collection DOAJ
description 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.
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spelling doaj.art-6b7ad48ec4c54cf5bf4df5b4cb78f07e2023-11-22T19:53:44ZengMDPI AGRemote Sensing2072-42922021-10-011320407210.3390/rs13204072Upscaling Evapotranspiration from a Single-Site to Satellite Pixel ScaleXiang Li0Shaomin Liu1Xiaofan Yang2Yanfei Ma3Xinlei He4Ziwei Xu5Tongren Xu6Lisheng Song7Yuan Zhang8Xiao Hu9Qian Ju10Xiaodong Zhang11State Key Laboratory of Earth Surface Processes and Resource Ecology, Faculty of Geographical Science, Beijing Normal University, Beijing 100875, ChinaState Key Laboratory of Earth Surface Processes and Resource Ecology, Faculty of Geographical Science, Beijing Normal University, Beijing 100875, ChinaState Key Laboratory of Earth Surface Processes and Resource Ecology, Faculty of Geographical Science, Beijing Normal University, Beijing 100875, ChinaHebei Technology Innovation Center for Remote Sensing Identification of Environmental Change, School of Geography, Hebei Normal University, Shijiazhuang 050024, ChinaState Key Laboratory of Earth Surface Processes and Resource Ecology, Faculty of Geographical Science, Beijing Normal University, Beijing 100875, ChinaState Key Laboratory of Earth Surface Processes and Resource Ecology, Faculty of Geographical Science, Beijing Normal University, Beijing 100875, ChinaState Key Laboratory of Earth Surface Processes and Resource Ecology, Faculty of Geographical Science, Beijing Normal University, Beijing 100875, ChinaSchool of Geographical Sciences, Southwest University, Chongqing 400715, ChinaState Key Laboratory of Earth Surface Processes and Resource Ecology, Faculty of Geographical Science, Beijing Normal University, Beijing 100875, ChinaState Key Laboratory of Earth Surface Processes and Resource Ecology, Faculty of Geographical Science, Beijing Normal University, Beijing 100875, ChinaState Key Laboratory of Earth Surface Processes and Resource Ecology, Faculty of Geographical Science, Beijing Normal University, Beijing 100875, ChinaShanghai Aerospace Electronic Technology Institute, Shanghai 201109, ChinaIt 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.https://www.mdpi.com/2072-4292/13/20/4072upscaling methodsground truth at the satellite pixel scaleeddy covariance systemuncertainty
spellingShingle Xiang Li
Shaomin Liu
Xiaofan Yang
Yanfei Ma
Xinlei He
Ziwei Xu
Tongren Xu
Lisheng Song
Yuan Zhang
Xiao Hu
Qian Ju
Xiaodong Zhang
Upscaling Evapotranspiration from a Single-Site to Satellite Pixel Scale
Remote Sensing
upscaling methods
ground truth at the satellite pixel scale
eddy covariance system
uncertainty
title Upscaling Evapotranspiration from a Single-Site to Satellite Pixel Scale
title_full Upscaling Evapotranspiration from a Single-Site to Satellite Pixel Scale
title_fullStr Upscaling Evapotranspiration from a Single-Site to Satellite Pixel Scale
title_full_unstemmed Upscaling Evapotranspiration from a Single-Site to Satellite Pixel Scale
title_short Upscaling Evapotranspiration from a Single-Site to Satellite Pixel Scale
title_sort upscaling evapotranspiration from a single site to satellite pixel scale
topic upscaling methods
ground truth at the satellite pixel scale
eddy covariance system
uncertainty
url https://www.mdpi.com/2072-4292/13/20/4072
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