Publications related to the GRACE Missions (no abstracts)

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Daily Regional Gravity Field Estimation Using GRACE Follow-On Line-of-Sight Gravity Differences

Li, Hao-si, Yi, Shuang, Han, Shin-Chan, and Tang, He, 2025. Daily Regional Gravity Field Estimation Using GRACE Follow-On Line-of-Sight Gravity Differences. Journal of Geophysical Research (Solid Earth), 130(5):e2024JB030089, doi:10.1029/2024JB030089.

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BibTeX

@ARTICLE{2025JGRB..13030089L,
       author = {{Li}, Hao-si and {Yi}, Shuang and {Han}, Shin-Chan and {Tang}, He},
        title = "{Daily Regional Gravity Field Estimation Using GRACE Follow-On Line-of-Sight Gravity Differences}",
      journal = {Journal of Geophysical Research (Solid Earth)},
     keywords = {GRACE follow-on, line-of-sight gravity difference, daily estimation, missing data imputation},
         year = 2025,
        month = may,
       volume = {130},
       number = {5},
          eid = {e2024JB030089},
        pages = {e2024JB030089},
     abstract = "{As a complement to the conventional monthly global solutions by Gravity
        Recovery and Climate Experiment series of gravimetric
        satellites, this study proposes an alternative method for
        estimating daily regional gravity field by utilizing the orbital
        Line-of-Sight Gravity Difference. The method is based on Slepian
        and B-spline basis functions for spatial and temporal
        parameterizations, respectively. Such parameterization of
        regional gravity field can be used to estimate total water
        storage change in a way compatible with surface mass estimation
        previously designed in the framework of global gravity field
        determination. The formal uncertainty of daily mass changes
        recovery is {\ensuremath{\sim}}5 Gt, equivalent to
        {\ensuremath{\sim}}3 cm of equivalent water height over
        {}400$^{2}$ km$^{2}$. In the evaluation part, the method is
        applied to the 2020 Bangladesh flood and the 2021 Australian
        flood. Our approach demonstrates strong agreement with the
        previous mascon-based studies, yielding Nash-Sutcliffe
        Efficiency values exceeding 0.81, and capturing the onset and
        recession of the flooding events. Additionally, we investigate
        the impact of data gaps, occasionally occur in the space-borne
        missions employing intersatellite laser ranging system. Our
        findings indicate that the B-spline parameterization effectively
        determines surface mass changes even with missing data rates up
        to 20\% or with gap lengths no longer than 2 days, highlighting
        its reliability for continuous monitoring in challenging
        observational scenarios. By providing a new methodological
        framework for daily-scale monitoring from satellite gravimetry,
        this work advances our understanding of the rapid evolution of
        climate extremes, which will ultimately facilitate future
        disaster monitoring and adaption efforts.}",
          doi = {10.1029/2024JB030089},
       adsurl = {https://ui.adsabs.harvard.edu/abs/2025JGRB..13030089L},
      adsnote = {Provided by the SAO/NASA Astrophysics Data System}
}

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