2022
DOI: 10.3390/rs14030532
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Monitoring and Stability Analysis of the Deformation in the Woda Landslide Area in Tibet, China by the DS-InSAR Method

Abstract: The Woda area in the upper Jinsha River has steep terrain and broken structures, causing landslide disasters frequently. Here, we used the distributed scatterer interferometric SAR (DS-InSAR) method to monitor and analyze the Woda landslide area. With the DS-InSAR method, we derived the deformation of the Woda landslide area from 106 Sentinel-1A ascending images acquired between 5 November 2014 and 4 September 2019 and 102 Sentinel-1A descending images acquired between 31 October 2014 and 11 September 2019. Th… Show more

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Cited by 29 publications
(21 citation statements)
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“…For the three landslides, we conclude that A2, B2 and C2, located in the middle of the slope, have the largest time series deformation. Combined with the existing research results of A and B [7], it is inferred that the deformation is most obvious in the central area of each landslide. In addition, we related the average deformation rate of A1-C3 to the local weather data and the results are shown in Fig.…”
Section: Deformation Detection and Analysismentioning
confidence: 56%
See 2 more Smart Citations
“…For the three landslides, we conclude that A2, B2 and C2, located in the middle of the slope, have the largest time series deformation. Combined with the existing research results of A and B [7], it is inferred that the deformation is most obvious in the central area of each landslide. In addition, we related the average deformation rate of A1-C3 to the local weather data and the results are shown in Fig.…”
Section: Deformation Detection and Analysismentioning
confidence: 56%
“…From October to December, the weather is again dominated by snowfall, and the average deformation rate decreased accordingly. Combining the results of existing analyses of the relationship between rainfall and surface deformation in the region [7], we conclude that rainfall is one of the main influencing factors to accelerate landslide deformation.…”
Section: Deformation Detection and Analysismentioning
confidence: 62%
See 1 more Smart Citation
“…Considering the compromise between the computation cycle and the accuracy of the algorithm, we choose a window size of 400 pixels, a step of 20 pixels, and a search range of 50 pixels. Such settings allow obtaining a displacement value of up to 5 m. In general, in less than 1 month, it seems unlikely that the displacement of a landslide that has not experienced overall failure to exceed this displacement threshold (Kang et al, 2017; Y. Liu et al, 2022; Tang et al, 2015). Meanwhile, DSM‐derived hillshade was selected as the correlation image pair because it represents the surface morphological features that are more favourable for correlation and can yield better sPOT results than other image pairs (Leprince et al, 2007; Lucieer et al, 2014; Turner et al, 2015).…”
Section: Methodsmentioning
confidence: 99%
“…It helps to locate and monitor underground mining subsidence in a wide area with low cost and high efficiency that conventional geophysical techniques, such as leveling [19], three-dimensional laser scanning [20], and the global navigation satellite system (GNSS) [21], are unlikely to do that [22]. However, the application of conventional DInSAR is mainly limited by spatiotemporal incoherence and atmospheric phase screening [23][24][25]. Wu et al obtained the ground surface subsidence of the Kailuan mining area in Tangshan city, China from two ERS-1/2 images with a time span of half a year, using processed DInSAR and analyzing the expansion and evolution process of the subsidence, as well as the influence of spatiotemporal incoherence, atmospheric phase delay and DEM error on DInSAR results [26].…”
Section: Introductionmentioning
confidence: 99%