2016
DOI: 10.1016/j.procs.2016.09.267
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Multi-sensor InSAR Analysis of Surface Displacement over Coastal Urban City of Trondheim

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Cited by 3 publications
(2 citation statements)
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“…From the original PSI method proposed by Ferretti et al [23], several approaches were proposed in subsequent years [26,[29][30][31][32][33][34]. These methods have been used for monitoring land deformation using European Remote-Sensing (ERS) and Environmental Satellite (Envisat) data [35], S1 data [36][37][38], by means of a multitrack PSI technique using the Advanced Land Observation Satellite phased array type L-band synthetic aperture radar (ALOS PALSAR) data in China [38] and with a multisensor approach employing TerraSAR-X (TSX), Radarsat-2 and S1 [39]. They have also been used for monitoring subsidence induced by mining activities using Radarsat-2, S1 and ALOS-2 data [40], subsidence induced by water depletion in aquifers using ERS-1/2 and Envisat data [41], land deformation using Constellation of Small Satellites for the Mediterranean Basin Observation (COSMO-SkyMed, CSK) over the historic center of Rome [42], building deformation using TSX [43,44], landslides using CSK and Envisat data [45], volcano crustal deformation using ERS-1/2 data [15,46] and extraction of hydrocarbons and groundwater [47,48].…”
Section: Introductionmentioning
confidence: 99%
“…From the original PSI method proposed by Ferretti et al [23], several approaches were proposed in subsequent years [26,[29][30][31][32][33][34]. These methods have been used for monitoring land deformation using European Remote-Sensing (ERS) and Environmental Satellite (Envisat) data [35], S1 data [36][37][38], by means of a multitrack PSI technique using the Advanced Land Observation Satellite phased array type L-band synthetic aperture radar (ALOS PALSAR) data in China [38] and with a multisensor approach employing TerraSAR-X (TSX), Radarsat-2 and S1 [39]. They have also been used for monitoring subsidence induced by mining activities using Radarsat-2, S1 and ALOS-2 data [40], subsidence induced by water depletion in aquifers using ERS-1/2 and Envisat data [41], land deformation using Constellation of Small Satellites for the Mediterranean Basin Observation (COSMO-SkyMed, CSK) over the historic center of Rome [42], building deformation using TSX [43,44], landslides using CSK and Envisat data [45], volcano crustal deformation using ERS-1/2 data [15,46] and extraction of hydrocarbons and groundwater [47,48].…”
Section: Introductionmentioning
confidence: 99%
“…Several methods have proposed to observe disaster and environmental change on the land surface using phase information, especially interferometric SAR (InSAR) and differential InSAR (DInSAR) [4]- [7] for single event change by a pair of images, and permanent scatterer InSAR (PSI) [8]- [11] to derive velocity of land surface deformation. There are various challenges in deriving long-term land deformation using different datasets acquired by different satellite SAR missions, for example, Shamshiri et al [12] proposed the InSAR timeseries technique using small baseline subset (SBAS) approach to observe the urban displacement using the observed period overlap of TerraSAR-X, Radarsat-2, and Sentinel-1 satellites. Then, Zhao et al [13] proposed a statistical-based modification of quantile-quantile adjustment (MQQA) to merge the long-term ground displacement time-series using multisensors.…”
Section: Introductionmentioning
confidence: 99%