Publications related to the GRACE Missions (no abstracts)

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Unraveling Multiscale Spatiotemporal Linkages of Groundwater Storage and Land Deformation in the North China Plain After the South-to-North Water Diversion Project

Wang, Xincheng, Chen, Beibei, Ma, Ziyao, Gong, Huili, Ma, Rui, Zhou, Chaofan, Meng, Dexin, Zhang, Shubo, Zhang, Chong, Lei, Kunchao, Wang, Haigang, and Zhang, Jincai, 2025. Unraveling Multiscale Spatiotemporal Linkages of Groundwater Storage and Land Deformation in the North China Plain After the South-to-North Water Diversion Project. Remote Sensing, 17(19):3336, doi:10.3390/rs17193336.

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@ARTICLE{2025RemS...17.3336W,
       author = {{Wang}, Xincheng and {Chen}, Beibei and {Ma}, Ziyao and {Gong}, Huili and {Ma}, Rui and {Zhou}, Chaofan and {Meng}, Dexin and {Zhang}, Shubo and {Zhang}, Chong and {Lei}, Kunchao and {Wang}, Haigang and {Zhang}, Jincai},
        title = "{Unraveling Multiscale Spatiotemporal Linkages of Groundwater Storage and Land Deformation in the North China Plain After the South-to-North Water Diversion Project}",
      journal = {Remote Sensing},
     keywords = {GRACE, InSAR, groundwater storage, downscaling, land deformation, ground fissures, North China Plain (NCP)},
         year = 2025,
        month = sep,
       volume = {17},
       number = {19},
          eid = {3336},
        pages = {3336},
     abstract = "{What are the main findings? Groundwater storage in the NCP showed a
        declining trend from 2018 to 2021, with a maximum subsidence
        rate reached ‑177 mm/a. Downscaled GWSA revealed contrasting
        groundwater variations across the northwest and southeast sides
        of the Shunyi fissure. Groundwater storage in the NCP showed a
        declining trend from 2018 to 2021, with a maximum subsidence
        rate reached ‑177 mm/a. Downscaled GWSA revealed contrasting
        groundwater variations across the northwest and southeast sides
        of the Shunyi fissure. What is the implication of the main
        finding? A novel GRACE statistical downscaling algorithm
        integrating a weight allocation strategy and InSAR-derived GWS
        estimation is proposed. The multiscale analysis provides
        insights into groundwater storage and land deformation patterns
        in the NCP after SNWDP. A novel GRACE statistical downscaling
        algorithm integrating a weight allocation strategy and InSAR-
        derived GWS estimation is proposed. The multiscale analysis
        provides insights into groundwater storage and land deformation
        patterns in the NCP after SNWDP. Leveraging multi-source remote
        sensing datasets and dynamic groundwater monitoring well
        observations, this study explores the multiscale spatiotemporal
        linkages of groundwater storage changes and land deformation in
        North China Plain (NCP) after the South-to-North Water Diversion
        Project (SNWDP). Firstly, we employed Gravity Recovery and
        Climate Experiment (GRACE) and interferometric synthetic
        aperture radar (InSAR) technology to estimate groundwater
        storage (GWS) and land deformation. Secondly and significantly,
        we proposed a novel GRACE statistical downscaling algorithm that
        integrates a weight allocation strategy and GWS estimation
        applied with InSAR technology. Finally, the downscaled results
        were employed to analyze spatial differences in land deformation
        across typical ground fissure areas. The results indicate that
        (1) between 2018 and 2021, groundwater storage in the NCP
        exhibited a declining trend, with an average reduction of ‑3.81
        {\ensuremath{\pm}} 0.53 km$^{3}$/a and a maximum land
        deformation rate of ‑177 mm/a; (2) the downscaled groundwater
        storage anomalies (GWSA) showed high correlation with in situ
        measurements (R = 0.75, RMSE = 2.91 cm); and (3) in the Shunyi
        fissure area, groundwater storage on the northern side increased
        continuously, with a maximum growth rate of 28 mm/a, resulting
        in surface uplift exceeding 70 mm.}",
          doi = {10.3390/rs17193336},
       adsurl = {https://ui.adsabs.harvard.edu/abs/2025RemS...17.3336W},
      adsnote = {Provided by the SAO/NASA Astrophysics Data System}
}

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