Monitoring of landslide activity at the Sirobagarh landslide, Uttarakhand, India, using LiDAR, SAR interferometry and geodetic surveys

被引:18
作者
Tiwari, Ashutosh [1 ]
Narayan, Avadh Bihari [1 ]
Dwivedi, Ramji [2 ]
Dikshit, Onkar [1 ]
Nagarajan, B. [1 ]
机构
[1] Indian Inst Technol Kanpur, Dept Civil Engn, Kanpur, Uttar Pradesh, India
[2] Motilal Nehru Natl Inst Technol, GIS Cell, Allahabad, Uttar Pradesh, India
关键词
Deformation monitoring; geodetic techniques; MT-InSAR approach; LiDAR; cross-correlation; DEFORMATION ANALYSIS; SURFACE DEFORMATION; GPS;
D O I
10.1080/10106049.2018.1524516
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
A robust geodetic framework comprising Terrestrial Laser Scanner (TLS), Global Navigation Satellite Systems (GNSS), Robotic Total Station (RTS) and Multi-temporal InSAR (MT-InSAR) was employed first in India to investigate a landslide-prone Sirobagarh region, Uttarakhand, at different spatial extents, and to evaluate the relationship amongst the displacement estimates obtained from the applied surveying techniques. TLS derived digital elevation models indicated displacements >5 m on the landslide upper scarp. GNSS- and RTS-based observations showed horizontal movements towards the Alaknanda river in the landslide slope direction (maximum values: 0.1305 and 0.045 m, respectively), and downward vertical motion (largest subsidence magnitude: -2.1315 and -0.030 m, respectively). MT-InSAR processing of Sentinel-1a images identified 21071 measurement pixels, highlighting subsidence around the landslide (mean velocity range: -0.110 to 0.008 m/year). Analysis of displacement vectors using vector equality, cross-covariance, cross-correlation and principal component analysis reveals that GNSS vertical displacement estimates were partially correlated with MT-InSAR measurements (correlated for epoch difference 2-3), whereas there was good cross-correlation between MT-InSAR and LiDAR observations throughout. The displacement estimates and their analyses evident unstable movement of the landslide scarp occurring due to debris flow and rainfall, and a relatively moderate subsidence activity in the surrounding areas lying in the landslide zone.
引用
收藏
页码:535 / 558
页数:24
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