@COMMENT This file was generated by bib2html_grace.pl <https://sourceforge.net/projects/bib2html/> version 0.94
@COMMENT written by Patrick Riley <https://sourceforge.net/users/patstg/>
@COMMENT This file was prepared using the NASA Astrophysics Data System (ADS)
@COMMENT https://ui.adsabs.harvard.edu/
@ARTICLE{2025GeoRL..5218580A,
       author = {{Arifin}, A. and {Shamsudduha}, M. and {Ramdhan}, A.~M. and {Rateb}, A. and {Scanlon}, B.~R. and {Setiawan}, T. and {Iman}, M.~I. and {Husna}, A. and {Taylor}, R.~G.},
        title = "{Plausibility Criteria for GRACE-Derived Groundwater Storage Changes From Aquifers Globally}",
      journal = {\grl},
         year = 2025,
        month = nov,
       volume = {52},
       number = {22},
          eid = {e2025GL118580},
        pages = {e2025GL118580},
     abstract = "{Monitoring changes in groundwater storage ({\ensuremath{\Delta}}GWS) is
        critical to assess sustainability of groundwater use under
        climate variability. Satellite gravimetry from the GRACE
        missions is used to infer {\ensuremath{\Delta}}GWS by deducting
        changes in monitored or modeled water components from GRACE-
        derived changes in total water storage
        ({\ensuremath{\Delta}}TWS). As a residual parameter,
        {\ensuremath{\Delta}}GWS is highly sensitive to arithmetic
        inconsistencies and uncertainties in both GRACE data and model-
        derived inputs. Here we present a framework to evaluate the
        physical plausibility of GRACE-derived {\ensuremath{\Delta}}GWS
        estimates across 37 large global aquifer systems. The results
        show that the proportion of plausible {\ensuremath{\Delta}}GWS
        estimates per realization, derived from multiple GRACE products
        and land surface model combinations, varies from <10\% to >60\%.
        Exclusion of implausible estimates improved correlations between
        {\ensuremath{\Delta}}GWS and {\ensuremath{\Delta}}TWS
        substantially (r {\ensuremath{\geq}} 0.9, p-value <0.05) in most
        aquifers (31/37) and with in situ observations in the Bengal
        Basin (r = 0.8, p-value <0.05).}",
          doi = {10.1029/2025GL118580},
       adsurl = {https://ui.adsabs.harvard.edu/abs/2025GeoRL..5218580A},
      adsnote = {Provided by the SAO/NASA Astrophysics Data System}
}
