• Sorted by Date • Sorted by Last Name of First Author •
Wu, Chengcheng, Lu, Chengpeng, Park, Edward, Wang, Yunfeng, Xie, Yangcun, Plattner, Alain M., Li, Zhibin, Liu, Bo, Shu, Longcang, and Zhang, Yong, 2025. Deciphering coastal plain groundwater dynamics: insights from satellite and hydrologic data in Pinghu City, China. Journal of Hydrology, 661:133706, doi:10.1016/j.jhydrol.2025.133706.
• from the NASA Astrophysics Data System • by the DOI System •
@ARTICLE{2025JHyd..66133706W,
author = {{Wu}, Chengcheng and {Lu}, Chengpeng and {Park}, Edward and {Wang}, Yunfeng and {Xie}, Yangcun and {Plattner}, Alain M. and {Li}, Zhibin and {Liu}, Bo and {Shu}, Longcang and {Zhang}, Yong},
title = "{Deciphering coastal plain groundwater dynamics: insights from satellite and hydrologic data in Pinghu City, China}",
journal = {Journal of Hydrology},
keywords = {Anomalous groundwater dynamics, Groundwater storage, GRACE satellite, Random Forest model, SBAS-InSAR, Isotope hydrology},
year = 2025,
month = nov,
volume = {661},
eid = {133706},
pages = {133706},
abstract = "{Groundwater, the planet's largest active freshwater resource, plays a
critical role in sustaining ecosystems, economies, and
societies. Over the past two decades, China's groundwater
regulation policies have significantly elevated groundwater
levels (GWLs) in many regions. However, some areas have
experienced unexpected or anomalous GWL declines unrelated to
groundwater extraction. The purpose of this study is to
investigate the causes of anomalous groundwater dynamics
processes in a coastal multilayered aquifer in Pinghu city,
China. By leveraging multi-source satellite data analyses,
including GRACE, InSAR, and isotope techniques, this study
identified that leakage within groundwater systems and changes
in precipitation, evapotranspiration were the primary drivers of
groundwater storage (GWS) reduction across all monitoring
stations in Pinghu City, China. The Random Forest model yielded
the highest accuracy (R$^{2}$ = 0.72, CC = 0.85, RMSE = 0.11)
among the three downscaling methods. A strong correlation
(around 0.75) is observed between GWS changes and meteorological
variables. The Hongni (HN) station, which monitors multiple deep
confined aquifers, was particularly sensitive to GWS
fluctuations. To interpret these dynamics, a conceptual model
was developed to characterize the interactions within the multi-
layered aquifer system, consisting of both unconfined and
confined aquifers separated by leakable aquitards. The layered
aquifer-aquitard structure observed in Pinghu City is a
characteristic feature of coastal and alluvial depositional
systems globally. The developed conceptual model was also proven
to be effective in the coastal multilayered aquifer in Texas,
USA. This model offers a valuable framework for investigating
groundwater dynamics in coastal plains with analogous geological
settings. The analysis further revealed a temporal effect of key
factors influencing the response of deep aquifers, providing
critical insights into the mechanisms driving changes in deep
groundwater systems.}",
doi = {10.1016/j.jhydrol.2025.133706},
adsurl = {https://ui.adsabs.harvard.edu/abs/2025JHyd..66133706W},
adsnote = {Provided by the SAO/NASA Astrophysics Data System}
}
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