• Sorted by Date • Sorted by Last Name of First Author •
Li, Yang, Zhao, Wenmiao, Mao, Kuanzhen, Jing, Wentao, Huo, Weiqi, and Zhang, Dongming, 2026. Revealing the lagged relationship between groundwater changes and land subsidence in Tianjin based on GRACE and InSAR observations. Scientific Reports, 16(1):27878, doi:10.1038/s41598-026-58032-w.
• from the NASA Astrophysics Data System • by the DOI System •
@ARTICLE{2026NatSR..1627878L,
author = {{Li}, Yang and {Zhao}, Wenmiao and {Mao}, Kuanzhen and {Jing}, Wentao and {Huo}, Weiqi and {Zhang}, Dongming},
title = "{Revealing the lagged relationship between groundwater changes and land subsidence in Tianjin based on GRACE and InSAR observations}",
journal = {Scientific Reports},
keywords = {GRACE, PS-InSAR, SBAS-InSAR, Groundwater storage, Land subsidence, Cross-correlation},
year = 2026,
month = jun,
volume = {16},
number = {1},
eid = {27878},
pages = {27878},
abstract = "{Tianjin has long been plagued by land subsidence, which is primarily
caused by groundwater over-exploitation and poses major threats
to urban construction, economic development, and infrastructure
safety. This study aims to explore the relationship between
groundwater storage (GWS) changes and land subsidence in Tianjin
by combining GRACE and InSAR technologies. To clarify this
relationship macroscopically, GRACE and GLDAS data were used to
analyze GWS changes in the study area from January 2023 to
February 2025, while PS-InSAR was applied to obtain concurrent
land subsidence information. Time-lagged cross-correlation
analysis was introduced to quantify the correlation and lag time
between GWS changes and land subsidence time series. Results
showed: (1) GWS was positive in most areas (maximum annual rate
59.13 mm/yr, concentrated in east-central Jinghai, south-central
Xiqing, Jinnan and central Binhai New Area), decreasing from the
center to north and south, with a significant decline (-9.22
mm/yr) in northern Binhai New Area; severe land subsidence
showed a ``peripheral aggregation'' pattern, with 4 contiguous
zones, 7 funnels and a max rate of 67.62 mm/yr (near Yangjiapo
Town, Binhai New Area); (2) The cross-correlation coefficient
between GWS changes and land subsidence ranged from 0.257 to
0.882 (0.542--0.853, 0.431--0.826, 0.257--0.882, 0.538--0.846
for Zones I-IV respectively), and land subsidence lagged GWS
changes by 41--263 days overall. This study confirms the link
and lag effect between GWS and land subsidence in Tianjin,
providing scientific guidance for subsidence prevention and
early warning.}",
doi = {10.1038/s41598-026-58032-w},
adsurl = {https://ui.adsabs.harvard.edu/abs/2026NatSR..1627878L},
adsnote = {Provided by the SAO/NASA Astrophysics Data System}
}
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