Publications related to the GRACE Missions (no abstracts)

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Potential Seasonal Terrestrial Water Storage Monitoring from GPS Vertical Displacements: A Case Study in the Lower Three-Rivers Headwater Region, China

Zhang, Bao, Yao, Yibin, Fok, Hok Sum, Hu, Yufeng, and Chen, Qiang, 2016. Potential Seasonal Terrestrial Water Storage Monitoring from GPS Vertical Displacements: A Case Study in the Lower Three-Rivers Headwater Region, China. Sensors, 16(9):1526, doi:10.3390/s16091526.

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@ARTICLE{2016Senso..16.1526Z,
       author = {{Zhang}, Bao and {Yao}, Yibin and {Fok}, Hok Sum and {Hu}, Yufeng and {Chen}, Qiang},
        title = "{Potential Seasonal Terrestrial Water Storage Monitoring from GPS Vertical Displacements: A Case Study in the Lower Three-Rivers Headwater Region, China}",
      journal = {Sensors},
     keywords = {GPS, terrestrial water storage, GRACE, GLDAS, three-rivers},
         year = 2016,
        month = sep,
       volume = {16},
       number = {9},
          eid = {1526},
        pages = {1526},
     abstract = "{This study uses the observed vertical displacements of Global
        Positioning System (GPS) time series obtained from the Crustal
        Movement Observation Network of China (CMONOC) with careful pre-
        and post-processing to estimate the seasonal crustal deformation
        in response to the hydrological loading in lower three-rivers
        headwater region of southwest China, followed by inferring the
        annual EWH changes through geodetic inversion methods. The
        Helmert Variance Component Estimation (HVCE) and the Minimum
        Mean Square Error (MMSE) criterion were successfully employed.
        The GPS inferred EWH changes agree well qualitatively with the
        Gravity Recovery and Climate Experiment (GRACE)-inferred and the
        Global Land Data Assimilation System (GLDAS)-inferred EWH
        changes, with a discrepancy of 3.2-3.9 cm and 4.8-5.2 cm,
        respectively. In the research areas, the EWH changes in the
        Lancang basin is larger than in the other regions, with a
        maximum of 21.8-24.7 cm and a minimum of 3.1-6.9 cm.}",
          doi = {10.3390/s16091526},
       adsurl = {https://ui.adsabs.harvard.edu/abs/2016Senso..16.1526Z},
      adsnote = {Provided by the SAO/NASA Astrophysics Data System}
}

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