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Surface Subsidence Analysis by Multi-Temporal InSAR and GRACE: A Case Study in Beijing.
Jiming Guo1,2,3, Lv Zhou4,5,6, Chaolong Yao7,8
1School of Geodesy and Geomatics, Wuhan University, Wuhan 430079, China. jmguo@sgg.whu.edu.cn.
Surface subsidence in Beijing is significantly impacted by groundwater changes. This study used multi-temporal InSAR and GRACE data to link groundwater depletion to land subsidence, revealing key spatial relationships.
Area of Science:
- Geosciences
- Remote Sensing
- Environmental Science
Background:
- Surface subsidence is a critical geohazard.
- Understanding its drivers, like groundwater changes, is essential for urban planning.
- Beijing has experienced significant land subsidence.
Purpose of the Study:
- To investigate the relationship between surface subsidence and groundwater changes in Beijing.
- To quantify surface subsidence using advanced remote sensing techniques.
- To analyze the correlation between groundwater level fluctuations and land subsidence patterns.
Main Methods:
- Utilized Multi-temporal Interferometric Synthetic Aperture Radar (multi-temporal InSAR) with ENVISAT ASAR images to map subsidence.
- Verified InSAR results with ground leveling data, achieving accuracy better than 5 mm/year.
- Employed Gravity Recovery and Climate Experiment (GRACE) data to derive groundwater change trends.
Main Results:
- Identified prominent and uneven surface subsidence in Beijing, with Tongzhou experiencing over 140 mm/year.
- Observed a consistent long-term decreasing trend between groundwater changes and surface subsidence.
- Found that the spatial extent of subsidence funnels was generally wider than groundwater depression areas.
Conclusions:
- Groundwater changes have a significant impact on surface subsidence in Beijing.
- A strong correlation exists between groundwater depletion and land subsidence.
- The findings provide crucial insights for sustainable groundwater management and urban development.
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