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Understanding source sustainability in hard rock aquifers using Gravity Recovery and Climate Experiment: A case study from Telangana, India

Paswan, Abhilash Kumar, Rao, Narakula Srinivasa, L, Raghu, and Tiwari, Virendra Mani, 2025. Understanding source sustainability in hard rock aquifers using Gravity Recovery and Climate Experiment: A case study from Telangana, India. Near Surface Geophysics, 23(4):287–297, doi:10.1002/nsg.70002.

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BibTeX

@ARTICLE{2025NSGeo..23..287P,
       author = {{Paswan}, Abhilash Kumar and {Rao}, Narakula Srinivasa and {L}, Raghu and {Tiwari}, Virendra Mani},
        title = "{Understanding source sustainability in hard rock aquifers using Gravity Recovery and Climate Experiment: A case study from Telangana, India}",
      journal = {Near Surface Geophysics},
     keywords = {GRACE, Groundwater storage, Hard rock aquifers, Telangana, Terrestrial water storage},
         year = 2025,
        month = aug,
       volume = {23},
       number = {4},
        pages = {287-297},
     abstract = "{The rise in groundwater extraction, exacerbated by climate change, poses
        a significant sustainability threat, particularly in hard rock
        terrains with limited storage capacity. In Telangana, India, a
        region characterized by semi-arid climatic conditions and
        dominated by crystalline hard rock aquifers across approximately
        85\% of its geographical area, groundwater serves as a primary
        water source. An analysis of terrestrial water storage (TWS)
        over Telangana for the period 2002{\textendash}2020 reveals
        pronounced seasonality and significant inter-annual variability.
        This inter-annual variability closely reflects the region's
        rainfall patterns and anthropogenic water extraction and is
        linked to El Ni{\~n}o-Southern Oscillation (ENSO) events.
        Positive TWS anomalies (TWSA) are associated with the Kharif
        season and the southwest monsoon, whereas negative anomalies
        correspond to the Rabi and summer seasons, where increased
        groundwater extraction for Rabi cropping is prevalent. The study
        identifies a strong correlation at a 2-month time lag between
        rainfall and TWSA- (R = 0.78) and rainfall and groundwater
        storage anomalies (GWSA) (R = 0.71), with the majority of TWS
        changes attributable to groundwater storage, showing a strong
        correlation with observed water levels. The TWS data effectively
        capture drought events, demonstrating the utility of Gravity
        Recovery and Climate Experiment (GRACE) in understanding water
        resource sustainability in the region. These findings underscore
        the value of GRACE data in complementing observed datasets for
        informed decision-making in water resource management.}",
          doi = {10.1002/nsg.70002},
       adsurl = {https://ui.adsabs.harvard.edu/abs/2025NSGeo..23..287P},
      adsnote = {Provided by the SAO/NASA Astrophysics Data System}
}

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