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Monitoring Landslides and Tectonic Motions with the Permanent Scatterers Technique

TLDR
In this paper, the evolution of the Ancona landslide (central Italy) was analyzed by processing 61 ERS images acquired in the time span between June 1992 and December 2000.
Abstract
Spaceborne differential synthetic aperture radar interferometry (DInSAR) has already proven its potential for mapping ground deformation phenomena, e.g. volcano dynamics. However, atmospheric disturbances as well as phase decorrelation have prevented hitherto this technique from achieving full operational capability. These drawbacks are overcome by carrying out measurements on a subset of image pixels corresponding to pointwise stable reflectors (Permanent Scatterers, PS) and exploiting long temporal series of interferometric data. Results obtained by processing 55 images acquired by the European Space Agency (ESA) ERS SAR sensors over Southern California show that the PS approach pushes measurement accuracy very close to its theoretical limit (about 1 mm), allowing the description of millimetric deformation phenomena occurring in a complex fault system. A comparison with corresponding displacement time series relative to permanent GPS stations of the Southern California Integrated GPS network (SCIGN) is carried out. Moreover, the pixel-by-pixel character of the PS analysis allows the exploitation of individual phase stable radar targets in low-coherence areas. This makes spaceborne interferometric measurements possible in vegetated areas, as long as a sufficient spatial density of individual isolated man-made structures or exposed rocks is available. The evolution of the Ancona landslide (central Italy) was analysed by processing 61 ERS images acquired in the time span between June 1992 and December 2000. The results have been compared with deformation values detected during optical levelling campaigns ordered by the Municipality of Ancona. The characteristics of PS, GPS and optical levelling surveying are to some extent complementary: a synergistic use of the three techniques could strongly enhance quality and reliability of ground deformation monitoring. D 2002 Elsevier Science B.V. All rights reserved.

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Citations
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Journal ArticleDOI

Persistent scatterer interferometric synthetic aperture radar for crustal deformation analysis, with application to Volcán Alcedo, Galápagos

TL;DR: In this paper, the spatial correlation of interferogram phase was used to find pixels with low-phase variance in all terrains, with or without buildings, for persistent scatterer (PS) analysis.
Journal ArticleDOI

Investigating landslides with space-borne Synthetic Aperture Radar (SAR) interferometry

TL;DR: In this article, the Permanent Scatterers (PS) technique was used for landslide assessment by combining the wide-area coverage typical of satellite imagery with the capability of providing displacement data relative to individual image pixels.
Journal ArticleDOI

Remote sensing of landslides: An analysis of the potential contribution to geo-spatial systems for hazard assessment in mountainous environments

TL;DR: In this paper, the use of remote sensing data in landslides studies during the 1980s, 1990s and 2000s, including a discussion of its potential and research challenges as result of new operational and forthcoming technologies.
Journal ArticleDOI

SAR monitoring of progressive and seasonal ground deformation using the permanent scatterers technique

TL;DR: The detection of both time-uniform and seasonal deformation phenomena is addressed, and a first assessment of the precision achievable by means of the PS Technique is discussed.
Journal ArticleDOI

Investigating landslides and unstable slopes with satellite Multi Temporal Interferometry: Current issues and future perspectives

TL;DR: In this article, the authors discuss relevant technical constraints and data interpretation issues that hamper the use of multi-temporal interferometry (MTI) in landslide assessment, and provide guidelines on how to mitigate MTI technical limitations and avoid erroneous interpretations of radar-derived slope surface deformations.
References
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