Abstract

In recent years, satellite synthetic aperture radar interferometry (InSAR) has been adopted as a spaceborne geodetic tool to successfully measure surface deformation of a few well-known landslides in the Three Gorges area. In consideration of the fact that most events of slope failure happened at places other than those famous landslides since the reservoir impoundment in 2003, focusing on a limited number of slopes is insufficient to meet the requirements of regional-scale landslide disaster prevention and early warning. As a result, it has become a vital task to evaluate the overall stability of slopes across the vast area of Three Gorges using wide-coverage InSAR datasets. In this study, we explored the approach of carrying out joint analysis of multi-path InSAR data stacks for wide-area landslide deformation mapping. As an example, three ALOS (Advanced Land Observing Satellite) PALSAR (Phased Array type L-band Synthetic Aperture Radar) data stacks of neighboring ascending paths covering the area along the Yangtze River from Fengjie to Zigui were analyzed. A key problem to be solved is the separation of the tropospheric signal from the interferometric phase, for which we employed a hybrid description model of the atmospheric phase screen (APS) to improve APS estimation from time series interferograms. The estimated atmospheric phase was largely correlated with the seasonal rainfall in the temporal dimension. The experimental results show that about 30 slopes covering total areas of 48 km2 were identified to be landslides in active deformation and should be kept under routine surveillance. Analyses of time series displacement measurements revealed that most landslides in the mountainous area far away from Yangtze River suffered from linear deformation, whereas landslides located on the river bank were destabilized predominantly by the influences of reservoir water level fluctuation and rainfall.

Highlights

  • Landslides including rock falls and debris flows are one of the most destructive geological hazards, accounting for around 80% of geological disasters [1]

  • Of SAR acquisitions, isolated interferograms are not allowed in Stanford Method for Persistent Scatterers (StaMPS) small baselines subset InSAR (SBAS) analysis

  • County is shownrate in Figure totaldirection of 1,775,238 points identified in our obtained displacement map in4.theALOS

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Summary

Introduction

Landslides including rock falls and debris flows are one of the most destructive geological hazards, accounting for around 80% of geological disasters [1]. In the Three Gorges area landslides are a major threat to navigation, people’s lives and properties. Wide areas of the Three Gorges are recognized as being at high risk, areas near the bank of the Yangtze River [2]. The significant increase of the water level causes overland flooding in many areas in the Three Gorges which significantly affects the stability of the slopes. Periodical fluctuation of the water level and seasonal rainfall. The detection and mapping of active slopes is a critical task for landslide disaster prevention and developing early warnings

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