2021
DOI: 10.1080/07038992.2021.1937968
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Benchmarked RADARSAT-2, SENTINEL-1 and RADARSAT Constellation Mission Change-Detection Monitoring at North Slide, Thompson River Valley, British Columbia: ensuring a Landslide-Resilient National Railway Network

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Cited by 10 publications
(4 citation statements)
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“…These have pixel dimensions of 1 m by 3 m in the spotlight-imaging beam mode (FSL30 at ~45° incidence). Such SAR imaging data are uncompromised by clouds and microwave backscatter ( 70 ) and easily discern felled vegetation, as well as disturbances related to slopes or changes of meter-scale surface texture. In addition, satellite LIDAR measurements of tree heights on the southern flanks of Tofua from ISS/GEDI ( 69 ) illustrated canopy heights in potentially disturbed areas ranging from 5-m to over 45-m elevation above sea level, with a typical value of about 20 m, consistent with highly approximated tree size measurements from submeter scale WV images.…”
Section: Methodsmentioning
confidence: 99%
“…These have pixel dimensions of 1 m by 3 m in the spotlight-imaging beam mode (FSL30 at ~45° incidence). Such SAR imaging data are uncompromised by clouds and microwave backscatter ( 70 ) and easily discern felled vegetation, as well as disturbances related to slopes or changes of meter-scale surface texture. In addition, satellite LIDAR measurements of tree heights on the southern flanks of Tofua from ISS/GEDI ( 69 ) illustrated canopy heights in potentially disturbed areas ranging from 5-m to over 45-m elevation above sea level, with a typical value of about 20 m, consistent with highly approximated tree size measurements from submeter scale WV images.…”
Section: Methodsmentioning
confidence: 99%
“…Level III investigations are most suitable for slower moving landslides where boreholes can be drilled for monitoring and unstable slopes instrumented safely. In the Thompson valley transportation corridor, Level III InSAR, UAV and RTK-GNSS change-detection datasets conclusively show that geotechnical solutions to stabilize slopes based on current physical models are only partly successful (Journault et al 2016(Journault et al , 2018Huntley et al 2017bHuntley et al , 2021c. To better understand the impacts of climate, landslide behaviour is further investigated though time-series monitoring of slopes and infrastructure (e.g., fibre optic reflectometry), boreholes (e.g., piezometers, inclinometers, and acoustic emissions), and weather variables (e.g., rain gauges, snow sensors, thermistors, anemometers, soil moisture meters).…”
Section: Level III Investigation (Time-seriesmentioning
confidence: 99%
“…Because RCM was launched only recently, most studies on RCM are based on simulation data using quad-polarized RADARSAT-2 images [2]. The applicability of different satellite platforms (including Radarsat-2, Sentinel-1 and RCM) are analyzed in [11,12] for landslide monitoring. The authors emphasized the RCM advantages of a shorter revisit time and higher spatial resolution for the detection of small-sized slope movements, compared with previous SAR satellites.…”
Section: Introductionmentioning
confidence: 99%