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Expanding groundwater drawdown funnels in North China Plain: A new insight from satellite gravimetry

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    1. Blind downscaling reveals 5 km funnel expansion trends in North China Plain.

      Funnel morphology changed with > 30 m deepening and horizontal broadening.

      Response time rose from 20 to 60 months, indicating aquifer buffering decline.

      Causal analysis shows early climate control, later pumping, then partial rebound.

  • Quantifying the evolution and recovery of groundwater drawdown funnels in the North China Plain (NCP) remains a grand challenge due to limited spatial resolution, vertical ambiguity, and attribution complexity in current satellite-based monitoring. Here, we present an integrative framework that addresses these bottlenecks by combining data-driven downscaling of GRACE gravimetric data, stratified signal separation using multi-depth well observations, and causality analysis driven by climate and groundwater abstraction indicators. This framework enables ~5 km resolution groundwater storage reconstruction, delineates 3D funnel morphology via Gaussian fitting, and attributes dynamic changes through wavelet-informed causality inference. Our key findings include: (1) The NCP groundwater system experienced a three-stage trajectory—initial slow decline (–0.05 cm/year), accelerated depletion (-0.19 cm/year), and partial recovery (+0.16 cm/year)—with funnel radius expanding from 209 km in 2002 to 340 km in 2022. (2) Funnel morphology transformed substantially, with the lowest groundwater level deepening from 20.93 m to 52.95 m and lateral half-width expanding from 0.56 m to 4.01 m over two decades. (3) The combined analysis of the transfer function noise (TFN) model and causality analysis based on information flow further revealed that early funnel changes were dominated by climate (~75% contribution), later shifts by intensive pumping (~90%), and recent recovery partially driven by precipitation (~16%), with aquifer response time increasing from 20 to 60 months, indicating a weakened response and delayed recovery. The lagged responses revealed by the causality analysis redefines our understanding of anthropogenic impacts on aquifer systems and offers a transferable path toward sustainable groundwater governance under changing climate and socioeconomic pressures.
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  • Cite this article:

    Yao J., Hao H., Wang M., et al. (2026). Expanding groundwater drawdown funnels in North China Plain: A new insight from satellite gravimetry. The Innovation Water 1:100010. https://doi.org/10.59717/j.tiw.2026.100010
    Yao J., Hao H., Wang M., et al. (2026). Expanding groundwater drawdown funnels in North China Plain: A new insight from satellite gravimetry. The Innovation Water 1:100010. https://doi.org/10.59717/j.tiw.2026.100010

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