Wuhan Surface Subsidence Analysis in 2015–2016 Based on Sentinel-1A Data by SBAS-InSAR

• Published in: Remote sensing (Basel, Switzerland) Vol. 9; no. 10; p. 982
• Main Authors: Zhou, Lv, Guo, Jiming, Hu, Jiyuan, Li, Jiangwei, Xu, Yongfeng, Pan, Yuanjin, Shi, Miao
• Format: Journal Article
• Language: English
• Published: Basel MDPI AG 01.10.2017
• Subjects: Anthropogenic factors; carbonate karstification; Comparative analysis; Compressibility; Construction; Construction industry; engineering construction; Groundwater; Image acquisition; Industrial areas; Industrial development; Interferometric synthetic aperture radar; Interferometry; Overexploitation; Precipitation; Radar imaging; Rivers; SBAS-InSAR; Seasonal variations; Sentinel-1A; Soil compressibility; Soil layers; Subsidence; surface subsidence; water level changes; Water levels; Wuhan
• ISSN: 2072-4292; 2072-4292
• DOI: 10.3390/rs9100982

The Terrain Observation with Progressive Scans (TOPS) acquisition mode of Sentinel-1A provides a wide coverage per acquisition and features a repeat cycle of 12 days, making this acquisition mode attractive for surface subsidence monitoring. A few studies have analyzed wide-coverage surface subsidence of Wuhan based on Sentinel-1A data. In this study, we investigated wide-area surface subsidence characteristics in Wuhan using 15 Sentinel-1A TOPS Synthetic Aperture Radar (SAR) images acquired from 11 April 2015 to 29 April 2016 with the Small Baseline Subset Interferometric SAR (SBAS InSAR) technique. The Sentinel-1A SBAS InSAR results were validated by 110 leveling points at an accuracy of 6 mm/year. Based on the verified SBAS InSAR results, prominent uneven subsidence patterns were identified in Wuhan. Specifically, annual average subsidence rates ranged from −82 mm/year to 18 mm/year in Wuhan, and maximum subsidence rate was detected in Houhu areas. Surface subsidence time series presented nonlinear subsidence with pronounced seasonal variations. Comparative analysis of surface subsidence and influencing factors (i.e., urban construction, precipitation, industrial development, carbonate karstification and water level changes in Yangtze River) indicated a relatively high spatial correlation between locations of subsidence bowl and those of engineering construction and industrial areas. Seasonal variations in subsidence were correlated with water level changes and precipitation. Surface subsidence in Wuhan was mainly attributed to anthropogenic activities, compressibility of soil layer, carbonate karstification, and groundwater overexploitation. Finally, the spatial-temporal characteristics of wide-area surface subsidence and the relationship between surface subsidence and influencing factors in Wuhan were determined.