Randomized trial assesses groundwater storage changes in river basins, indicating significant declines over two decades.
The present work focused on the synergistic utilization of Gravity Recovery and Climate Experiment (GRACE) and GRACE-Follow On (FO) derived Ensemble Terrestrial Water Storage Anomaly (TWSA) from Jet Propulsion Lab (JPL), Centre for Space Research (CSR) and Goddard Space Flight Centre (GSFC), downscaled (GOU) TWSA and a gap filled JPL TWSA data and other hydrological variables to assess variability in groundwater storage (GWS) change in the last two decades (2002-2022) over Indus and Ganga river basins. The Indus basin witnessed a significant decline with a rate of change between -2.11 to -3.0 cm/yr and Ganga basin witnessed a significant decline of -1.27 cm/yr to -1.88 cm/yr after removing soil moisture estimates respectively. GWSA obtained from downscaled TWSA also indicated a significant negative trend. However, the magnitude of trend was considerably lower (0.9 cm/yr) than the ensemble (-1.27 cm/yr) and gap filled (-1.88 cm/yr) datasets. Ground observations also indicated a decline in GWSA in the Ganga basin with a rate of change -0.26 cm/yr. Validation of results with in-situ well data showed highest positive correlation (R = 0.78) and least Root Mean Squared Error (RMSE = 17.5 cm) with in-situ GWSA in the Indus basin during 2002-2022. Downscaling of GRACE TWSA employing self-supervised data assimilation can significantly reduce the general overestimation of trends in GWSA computed from GRACE and GRACE FO observations.
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Choubey et al. (2026) studied this question.
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