2018
DOI: 10.1007/s11069-018-3564-9
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How to avoid false interpretations of Sentinel-1A TOPSAR interferometric data in landslide mapping? A case study: recent landslides in Transdanubia, Hungary

Abstract: It is a crucial issue to better understand the usability of Sentinel-1 satellites in geomorphologic applications, since Sentinel-1 and the Copernicus Program are considered to be the workhorse of Earth observation by the European Space Agency during the next decades. Yet, a very limited experience is available on the applicability of Sentinel-1 images in the detection and identification of surface deformations and especially landslide mapping and monitoring in densely vegetated (low-coherence) areas. Few Synth… Show more

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Cited by 24 publications
(14 citation statements)
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“…In general, D-InSAR favors short baselines (less than 200 m) for C-band systems. Due to the high revisit frequency and the excellent orbital accuracy of Sentinel-1, the perpendicular baseline is usually not a limiting factor, facilitating the application of InSAR in many countries [39]. The perpendicular baseline aspect, though, can be used to select the optimal pair of images [40].…”
Section: Methodsmentioning
confidence: 99%
“…In general, D-InSAR favors short baselines (less than 200 m) for C-band systems. Due to the high revisit frequency and the excellent orbital accuracy of Sentinel-1, the perpendicular baseline is usually not a limiting factor, facilitating the application of InSAR in many countries [39]. The perpendicular baseline aspect, though, can be used to select the optimal pair of images [40].…”
Section: Methodsmentioning
confidence: 99%
“…Geosciences 2020, 10, x FOR PEER REVIEW 4 of 26 complex ground displacement phenomena, especially of fast-moving landslides [1,37,38] and slope deformations, cannot be achieved using Sentinel-1 images due to the limitations of the C-band wavelength and the images' medium spatial resolution [39][40][41].…”
Section: Area Of Studymentioning
confidence: 99%
“…Additionally, although the moderate spatial resolution of the IW swath images for Level-1 SLC products (2.7 × 22 m to 3.5 × 22 m), which are available for Cyprus, has proven to be satisfactory for the detection of land subsidence and/or uplift [22,23,36], the detailed study and monitoring of more complex ground displacement phenomena, especially of fast-moving landslides [1,37,38] and slope deformations, cannot be achieved using Sentinel-1 images due to the limitations of the C-band wavelength and the images' medium spatial resolution [39][40][41].…”
Section: Introductionmentioning
confidence: 99%
“…Recently, the number of successful studies for mapping landslides through Sentinel-1 [1,2,[42][43][44][45][46][47][48] has been increasing; however, little research has addressed the application of Sentinel-2 [3,41,49], or the combination of Sentinel-1 and -2 [4,50] for this objective. Moreover, most of these studies have applied pixel-based image analysis for detecting landslide events using Sentinel images.…”
Section: Introductionmentioning
confidence: 99%