ZHANG Chenglong, LI Zhenhong, YU Chen, SONG Chuang, XIAO Ruya, PENG Jianbing. Landslide Detection of the Jinsha River Region Using GACOS Assisted InSAR Stacking[J]. Geomatics and Information Science of Wuhan University, 2021, 46(11): 1649-1657. DOI: 10.13203/j.whugis20200675
Citation: ZHANG Chenglong, LI Zhenhong, YU Chen, SONG Chuang, XIAO Ruya, PENG Jianbing. Landslide Detection of the Jinsha River Region Using GACOS Assisted InSAR Stacking[J]. Geomatics and Information Science of Wuhan University, 2021, 46(11): 1649-1657. DOI: 10.13203/j.whugis20200675

Landslide Detection of the Jinsha River Region Using GACOS Assisted InSAR Stacking

  •   Objectives  The Sichuan-Tibet Railway crosses the Jinsha River specifically the section from Xiongsong Town to Shadong Town, Gongjue County, Tibet Autonomous Region, in which exist strong topography variations and many potential geohazards, and hence it urgent to detect the potential geohazards in this region to ensure the railway safety.
      Methods  In this paper, 61 Sentinel-1 ascending, 53 Sentinel-1 descending and 7 advanced land observing satellite 2 (ALOS-2) ascending images are used to derive the annual mean deformation rates in the satellite radar line of sight (LOS) with two advanced InSAR(interferometric synthetic aperture radar) approaches, namely generic atmospheric correction online service for InSAR(GACOS)assisted InSAR Stacking and LiCSBAS. The three LOS annual mean deformation rate maps are then used to determine 2D surface movements (one along the slope and the other perpendicular to the slope) in the study region.
      Results  The comparison between GACOS assisted InSAR Stacking and LiCSBAS results show that they agree with each other with correlation coefficients over 0.92 for the LOS deformation rates and over 0.85 for the 2D deformation rates, suggesting the reliability of GACOS assisted InSAR Stacking. The maximum annual deformation rate of 163 mm/a can be observed in the slope direction and seven landslides (A, B, C, D, E, F, G) can be clearly identified, which in turn lays the foundation for future real-time monitoring. Based on the detailed analysis of the seven regions by using InSAR and optical interpretation results, it is found that the seven landslides had relatively obvious deformation. Landslides A, B, C and D are active landslides, which might cause the result of river blocking due to overall instability. At present, landslides E, F and G are still in the stage of slow deformation.
      Conclusions  This study also find that GACOS assisted InSAR Stacking can effectively remove long-band and topographic related atmospheric delay error with the help of GACOS, which has the advantages of being simple, effective, fast, and easy to popularize and apply. GACOS assisted InSAR Stacking technology can be used to quickly identify potential landslide hazards.
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