2018
DOI: 10.1080/10106049.2018.1524516
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Monitoring of landslide activity at the Sirobagarh landslide, Uttarakhand, India, using LiDAR, SAR interferometry and geodetic surveys

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Cited by 21 publications
(10 citation statements)
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“…In the case of D-InSAR, the topographic component is removed by using a pre-existing DEM to leave only the phase difference associated to the displacement [48]. Although, a DEM sampled at SAR resolution would be necessary to completely remove the topography, lower resolution global DEMs, available in open access, are suitable when studying ground deformations (e.g., SRTM DEM [49][50][51][52][53][54][55]). The orbital contribution can be removed as we selected SAR images acquired along a same orbit, which we assume to be correctly georeferenced.…”
Section: Radar Remote Sensingmentioning
confidence: 99%
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“…In the case of D-InSAR, the topographic component is removed by using a pre-existing DEM to leave only the phase difference associated to the displacement [48]. Although, a DEM sampled at SAR resolution would be necessary to completely remove the topography, lower resolution global DEMs, available in open access, are suitable when studying ground deformations (e.g., SRTM DEM [49][50][51][52][53][54][55]). The orbital contribution can be removed as we selected SAR images acquired along a same orbit, which we assume to be correctly georeferenced.…”
Section: Radar Remote Sensingmentioning
confidence: 99%
“…To do this, the DEM of the Shuttle Radar Topography Mission (SRTM, 30 m resolution), was subtracted from the preliminary product. During the last decades, many researchers used SRTM DEMs for their InSAR processing [49][50][51][52][53][54][55]. As the same topographic reference (DEM) is used for each pair of images, it does not affect the measurement of relative displacements of a few centimeters.…”
Section: Radar Remote Sensingmentioning
confidence: 99%
“…Analysis of deformations events like landslide, earthquake, land subsidence etc (Tiwari et al, 2018) It assesses infrastructure damages and ground changes.…”
Section: Optical Sar Lidarmentioning
confidence: 99%
“…These thresholds can be used to determine the temporal probability of the occurrence of landslides as a part of a landslide early warning system (LEWS). The thresholds can be estimated using empirical methods [9][10][11][12], probabilistic methods [8,13,14], and/or physical methods [15,16], and we can use other tools like geographic information system (GIS) [17] and global positioning system (GPS) [18,19] and new technologies in order to make the calculation processes automatic [20,21]. When long-term monitoring data is not available for the study area, it is often difficult to identify the triggering rainfall corresponding to landslides [22].…”
Section: Introductionmentioning
confidence: 99%