Publications related to the GRACE Missions (no abstracts)

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GRACE-derived spatiotemporal changes of terrestrial water storage in the major plateaus of China

Wang, Dong, Tang, Bo-Hui, Li, Yingyun, Fu, Wei, Fu, Zhitao, Zhang, Zhen, and Ge, Zhongxi, 2025. GRACE-derived spatiotemporal changes of terrestrial water storage in the major plateaus of China. Global and Planetary Change, 255:105102, doi:10.1016/j.gloplacha.2025.105102.

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BibTeX

@ARTICLE{2025GPC...25505102W,
       author = {{Wang}, Dong and {Tang}, Bo-Hui and {Li}, Yingyun and {Fu}, Wei and {Fu}, Zhitao and {Zhang}, Zhen and {Ge}, Zhongxi},
        title = "{GRACE-derived spatiotemporal changes of terrestrial water storage in the major plateaus of China}",
      journal = {Global and Planetary Change},
     keywords = {China, Plateau, GRACE, Water storage, Long-term},
         year = 2025,
        month = dec,
       volume = {255},
          eid = {105102},
        pages = {105102},
     abstract = "{Changes in terrestrial water storage (TWS) significantly impact water
        resource regulation in the major plateaus of China (MPC).
        Traditional monitoring methods are limited by high costs and
        sparse site distribution, restricting large-scale and high-
        resolution assessments. The Gravity Recovery and Climate
        Experiment (GRACE) and its follow-on mission offer an effective
        approach for TWS observation in these areas. This study examines
        the spatiotemporal features of TWS in MPC from 2002 to 2022 by
        recovering low-degree signals through coefficient substitution,
        restoring high-degree signals via combined filtering, and
        interpolating missing data using Singular Spectrum Analysis
        (SSA). Key findings reveal a TWS change rate of
        {\ensuremath{-}}0.1 cm/year in the MPC, with semi-annual and
        annual amplitudes of 0.7 cm and 2.3 cm, respectively, peaking
        between September and October. TWS variations in the MPC are
        largest in the Qinghai-Tibet Plateau (QTP) and this dominant
        signal tends to mask the trends in other plateau regions. Among
        these, the Yunnan-Kweichow Plateau (YKP) is exhibiting a
        gradually increasing TWS trend. In the western YKP, TWS declines
        due to concentrated rainfall, while in its eastern regions, a
        combination of reduced seasonal precipitation and water
        migration contributes to an overall upward trend. These findings
        provide critical insights for regional water resource management
        and policy formulation.}",
          doi = {10.1016/j.gloplacha.2025.105102},
       adsurl = {https://ui.adsabs.harvard.edu/abs/2025GPC...25505102W},
      adsnote = {Provided by the SAO/NASA Astrophysics Data System}
}

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