EGU25-14383, updated on 15 Mar 2025
https://doi.org/10.5194/egusphere-egu25-14383
EGU General Assembly 2025
© Author(s) 2025. This work is distributed under
the Creative Commons Attribution 4.0 License.
Poster | Monday, 28 Apr, 16:15–18:00 (CEST), Display time Monday, 28 Apr, 14:00–18:00
 
Hall X2, X2.82
Monitoring Surface Deformation and Classifying Activity of Deep-Seated Landslide Sites Using Multi-Temporal InSAR
Chih-Yu Kuo1,2, Suet-Yee Au3, Ya-Hsin Chan1, Rou-Fei Chen3, Kun-Che Chan4, En-Ju Lin4, and Pi-Wen Tsai5
Chih-Yu Kuo et al.
  • 1Research Center for Applied Sciences, Academia Sinica, Taipei, Taiwan (cykuo06@gate.sinica.edu.tw)
  • 2Department of Civil Engineering, National Taiwan University, Taipei, Taiwan
  • 3Institute of Mineral Resources Engineering, National Taipei University of Technology, Taipei, Taiwan
  • 4Agency of Rural Development and Soil and Water Conservation, Ministry of Agriculture, Taiwan
  • 5Department of Mathematics, National Taiwan Normal University, Taipei, Taiwan

Through the application of Multi-temporal Interferometric Synthetic Aperture Radar (MTInSAR) for long-term monitoring of surface deformation, the Agency of Rural Development and Soil and Water Conservation (ARGSWC), Ministry of Agriculture, has identified 315 deep-seated landslide sites with protecting targets across Taiwan as of 2024. For this study, imagery from January 2022 to October 2023 from the ALOS-2 satellite, released by the Japan Aerospace Exploration Agency (JAXA), is used for the MTInSAR monitoring. Based on the MTInSAR surface displacement data, activity indices for the deep-seated landslide sites have been developed, including both the arithmetic mean and inverse area-weighted deformations. The k-mean clustering and risk matrix method are then employed to classify and rank the landslide activity. The analysis reveals that approximately 5.8%, 10.7% and 83.6% of the deep-seated landslide sites are classified as high, medium and low activity, respectively. In addition, statistical clustering techniques are applied to group the surface deformation data, which are then compared to slope units derived from the aerial LiDAR Digital Elevation Model (DEM) for the landslide sites. This approach helps to identify active landslide blocks or subzones within the landslide sites.

How to cite: Kuo, C.-Y., Au, S.-Y., Chan, Y.-H., Chen, R.-F., Chan, K.-C., Lin, E.-J., and Tsai, P.-W.: Monitoring Surface Deformation and Classifying Activity of Deep-Seated Landslide Sites Using Multi-Temporal InSAR, EGU General Assembly 2025, Vienna, Austria, 27 Apr–2 May 2025, EGU25-14383, https://doi.org/10.5194/egusphere-egu25-14383, 2025.