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Upstream GPS Vertical Displacement and its Standardization for Mekong River Basin Surface Runoff Reconstruction and Estimation

Fok, Hok Sum, Zhou, Linghao, Liu, Yongxin, Ma, Zhongtian, and Chen, Yutong, 2019. Upstream GPS Vertical Displacement and its Standardization for Mekong River Basin Surface Runoff Reconstruction and Estimation. Remote Sensing, 12(1):18, doi:10.3390/rs12010018.

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@ARTICLE{2019RemS...12...18F,
       author = {{Fok}, Hok Sum and {Zhou}, Linghao and {Liu}, Yongxin and {Ma}, Zhongtian and {Chen}, Yutong},
        title = "{Upstream GPS Vertical Displacement and its Standardization for Mekong River Basin Surface Runoff Reconstruction and Estimation}",
      journal = {Remote Sensing},
     keywords = {Runoff, GPS, GRACE satellite gravimetry, Mekong River Basin, PDSI},
         year = 2019,
        month = dec,
       volume = {12},
       number = {1},
          eid = {18},
        pages = {18},
     abstract = "{Surface runoff (R), which is another expression for river water
        discharge of a river basin, is a critical measurement for
        regional water cycles. Over the past two decades, river water
        discharge has been widely investigated, which is based on
        remotely sensed hydraulic and hydrological variables as well as
        indices. This study aims to demonstrate the potential of
        upstream global positioning system (GPS) vertical displacement
        (VD) and its standardization to statistically derive R time
        series, which has not been reported in recent literature. The
        correlation between the in situ R at estuaries and averaged GPS-
        VD and its standardization in the river basin upstream on a
        monthly temporal scale of the Mekong River Basin (MRB) is
        examined. It was found that the reconstructed R time series from
        the latter agrees with and yields a similar performance to that
        from the terrestrial water storage based on gravimetric
        satellite (i.e., Gravity Recovery and Climate Experiment
        (GRACE)) and traditional remote sensing data. The reconstructed
        R time series from the standardized GPS-VD was found to have a
        2-7\% accuracy increase against those without standardization.
        On the other hand, it is comparable to data that are obtained by
        the Palmer drought severity index (PDSI). Similar accuracies are
        exhibited by the estimated R when externally validated through
        another station location with in situ time series. The
        comparison of the estimated R at the entrance of river delta
        against that at the estuaries indicates a 1-3\% relative error
        induced by the residual ocean tidal effect at the estuary. The
        reconstructed R from the standardized GPS-VD yields the lowest
        total relative error of less than 9\% when accounting for the
        main upstream area of the MRB. The remaining errors may be the
        result of the combined effect of the proposed methodology,
        remaining environmental signals in the data time series, and
        potential time lag (less than a month) between the upstream MRB
        and estuary.}",
          doi = {10.3390/rs12010018},
       adsurl = {https://ui.adsabs.harvard.edu/abs/2019RemS...12...18F},
      adsnote = {Provided by the SAO/NASA Astrophysics Data System}
}

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