|Table of Contents|

Evolution of the 2018 Baige Landslides Revealed by Optical Remote Sensing Pixel Offsets in Jinsha River Basin, China(PDF)

《地球科学与环境学报》[ISSN:1672-6561/CN:61-1423/P]

Issue:
2022年第06期
Page:
1002-1015
Research Field:
纪念刘国昌先生诞辰110周年专辑
Publishing date:

Info

Title:
Evolution of the 2018 Baige Landslides Revealed by Optical Remote Sensing Pixel Offsets in Jinsha River Basin, China
Author(s):
DONG Yue1; 2;  DING Ming-tao1; 2; 3*;  LI Xin-long1; 2;  ZHANG Xue-song1; 2;  HUANG Wu-biao1; 2;  LIU Zhen-jiang1; 2;  LI Zhen-hong1; 2; 3
(1. School of Geological Engineering and Geomatics, Chang'an University, Xi'an 710054, Shaanxi, China; 2. Big Data Center for Geosciences and Satellites, Chang'an University, Xi'an 710054, Shaanxi, China; 3. Key Laboratory of Western China's Mineral Resources and Geological Engineering of Ministry of Education, Chang' an University, Xi'an 710054, Shaanxi, China)
Keywords:
optical remote sensing;  offset-tracking technology;  time-series inversion algorithm;  COSI-Corr;  CARST;  DEM differential;  deformation monitoring;  Baige landslide;  Jinsha River Basin
PACS:
P237
DOI:
10.19814/j.jese.2022.05025
Abstract:
With the increasing number of optical remote sensing satellites and the improvement of image quality, the optical images show great potential for monitoring surface deformation. Taking the typical high-elevation Baige landslides during 2018 in Jinsha River Basin as examples, the pixel offset-tracking method and time-series inversion algorithm were employed to process Sentinel-2 optical images for extracting the surface displacement time series of “10·10” and “11·3” Baige landslides. The results show that ① the cumulative surface displacement before “10·10” Baige landslide is up to 31.69 m from 13 November 2015 to 5 February 2018, the time series displacement presents an obvious process characteristics of “initial start→constant deformation→accelerated deformation”; ② the cumulative surface displacement before “11·3” Baige landslide in the EW direction is about 12.89 m(about 1 pixel)from 28 October 2018 to 2 November 2018, which is consistent with radar image offset-tracking results; ③ after “11·3” Baige landslide, the cumulative surface displacement in the EW direction of some residual deposits is up to 7.71 m from 16 January 2020 to 4 February 2022, and clear sliding signs can be observed, indicating a high risk for a new disaster. Furthermore, the reliability of the optical image offset-tracking method for detecting surface deformation is demonstrated through the comparisons between two offset-tracking softwares of COSI-Corr and CARST with InSAR and UAV 3D results.

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Last Update: 2022-11-25