Publications related to the GRACE Missions (no abstracts)

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Mass Change Index for Characterizing Hydrological Extremes Every Few Days From Satellite Gravity Measurements

Tang, Miao, Han, Shin–Chan, Yuan, Linguo, Yang, Xinghai, Yeo, In–Young, Rodell, Matthew, Li, Bailing, Lee, Eunjee, and Jiang, Zhongshan, 2025. Mass Change Index for Characterizing Hydrological Extremes Every Few Days From Satellite Gravity Measurements. Water Resources Research, 61(12):e2025WR040534, doi:10.1029/2025WR040534.

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BibTeX

@ARTICLE{2025WRR....6140534T,
       author = {{Tang}, Miao and {Han}, Shin-Chan and {Yuan}, Linguo and {Yang}, Xinghai and {Yeo}, In-Young and {Rodell}, Matthew and {Li}, Bailing and {Lee}, Eunjee and {Jiang}, Zhongshan},
        title = "{Mass Change Index for Characterizing Hydrological Extremes Every Few Days From Satellite Gravity Measurements}",
      journal = {Water Resources Research},
     keywords = {satellite gravimetry, mass change, hydrological indices, hydrological extremes},
         year = 2025,
        month = dec,
       volume = {61},
       number = {12},
          eid = {e2025WR040534},
        pages = {e2025WR040534},
     abstract = "{We introduce a new hydrological index that enables assessment of extreme
        events every few days from the GRACE Follow-On (GRACE-FO)
        satellite mission. The Mass Change Index (MCI) was developed by
        standardizing instantaneous satellite gravity anomalies computed
        directly from orbit perturbations. It is based on hydrology-
        related gravity change, namely, total water storage change, and
        thus equally sensitive to wet and dry anomalies. The key
        innovation of MCI is its sensitivity to instantaneous mass
        changes as opposed to monthly mean changes. GRACE-FO's ground
        track permits MCI retrievals every 5─6 days in most low and mid
        latitude regions. We demonstrate the application of MCI to
        investigate hydrological extremes in the middle-lower Yangtze
        River Basin (MLYRB). MCI detects extreme wet conditions
        (standardized index of 2.0─3.0) along the Yangtze River
        mainstream related to the catastrophic flood in 2020, consistent
        with daily streamflow observations. In contrast, a typical
        GRACE-FO based monthly drought index significantly
        underestimates the severity of the event and misidentifies
        timing of the onset. MCI also detects extreme dry conditions
        ({\ensuremath{-}}2.0 to {\ensuremath{-}}2.5) prevailing within
        MLYRB, related to the unprecedented heatwave and drought event
        during the summer of 2022. A streamflow index and the monthly
        drought index both underestimate the severity of the event. MCI
        retains information in intersatellite range measurements that
        may be lost when processing monthly gravity solutions. It can
        also be processed more rapidly, increasing its potential value
        for hydrological monitoring systems and other operational
        applications.}",
          doi = {10.1029/2025WR040534},
       adsurl = {https://ui.adsabs.harvard.edu/abs/2025WRR....6140534T},
      adsnote = {Provided by the SAO/NASA Astrophysics Data System}
}

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