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A Bayesian Three-Cornered Hat (BTCH) Method: Improving the Terrestrial Evapotranspiration Estimation

He, Xinlei, Xu, Tongren, Xia, Youlong, Bateni, Sayed M., Guo, Zhixia, Liu, Shaomin, Mao, Kebiao, Zhang, Yuan, Feng, Huaize, and Zhao, Jingxue, 2020. A Bayesian Three-Cornered Hat (BTCH) Method: Improving the Terrestrial Evapotranspiration Estimation. Remote Sensing, 12(5):878, doi:10.3390/rs12050878.

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@ARTICLE{2020RemS...12..878H,
       author = {{He}, Xinlei and {Xu}, Tongren and {Xia}, Youlong and {Bateni}, Sayed M. and {Guo}, Zhixia and {Liu}, Shaomin and {Mao}, Kebiao and {Zhang}, Yuan and {Feng}, Huaize and {Zhao}, Jingxue},
        title = "{A Bayesian Three-Cornered Hat (BTCH) Method: Improving the Terrestrial Evapotranspiration Estimation}",
      journal = {Remote Sensing},
     keywords = {evapotranspiration, Bayesian-based three-cornered hat method, total water storage anomaly},
         year = 2020,
        month = mar,
       volume = {12},
       number = {5},
          eid = {878},
        pages = {878},
     abstract = "{In this study, a Bayesian-based three-cornered hat (BTCH) method is
        developed to improve the estimation of terrestrial
        evapotranspiration (ET) by integrating multisource ET products
        without using any a priori knowledge. Ten long-term (30 years)
        gridded ET datasets from statistical or empirical, remotely-
        sensed, and land surface models over contiguous United States
        (CONUS) are integrated by the BTCH and ensemble mean (EM)
        methods. ET observations from eddy covariance towers (ET$_{EC}$)
        at AmeriFlux sites and ET values from the water balance method
        (ET$_{WB}$) are used to evaluate the BTCH- and EM-integrated ET
        estimates. Results indicate that BTCH performs better than EM
        and all the individual parent products. Moreover, the trend of
        BTCH-integrated ET estimates, and their influential factors
        (e.g., air temperature, normalized differential vegetation
        index, and precipitation) from 1982 to 2011 are analyzed by the
        Mann-Kendall method. Finally, the 30-year (1982 to 2011) total
        water storage anomaly (TWSA) in the Mississippi River Basin
        (MRB) is retrieved based on the BTCH-integrated ET estimates.
        The TWSA retrievals in this study agree well with those from the
        Gravity Recovery and Climate Experiment (GRACE).}",
          doi = {10.3390/rs12050878},
       adsurl = {https://ui.adsabs.harvard.edu/abs/2020RemS...12..878H},
      adsnote = {Provided by the SAO/NASA Astrophysics Data System}
}

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