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Please use this identifier to cite or link to this item: http://hdl.handle.net/2122/7455
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dc.contributor.authorallCanova, F.; Dipartimento di Scienze della Terra e dell’Ambiente, Università degli Studi di Pavia, Pavia, Italyen
dc.contributor.authorallTolomei, C.; Istituto Nazionale di Geofisica e Vulcanologia, Sezione CNT, Roma, Italiaen
dc.contributor.authorallSalvi, S.; Istituto Nazionale di Geofisica e Vulcanologia, Sezione CNT, Roma, Italiaen
dc.contributor.authorallToscani, G.; Dipartimento di Scienze della Terra e dell’Ambiente, Università degli Studi di Pavia, Pavia, Italyen
dc.contributor.authorallSeno, S.; Dipartimento di Scienze della Terra e dell’Ambiente, Università degli Studi di Pavia, Pavia, Italyen
dc.date.accessioned2012-01-23T07:02:57Zen
dc.date.available2012-01-23T07:02:57Zen
dc.date.issued2012en
dc.identifier.urihttp://hdl.handle.net/2122/7455en
dc.description.abstractWe present the results of a multi-temporal, differential interferometric synthetic aperture radar (DInSAR) analysis aiming to identify active surface deformation phenomena in southeastern Sicily. The study area has been chosen because of its strong seismicity, high concentration of industrial and agricultural activities, and high density of people living in the coastal area. Furthermore, the morphology, lithology and climatic feature of this sector of the Hyblean foreland are suitable for an interferometric analysis, providing a high coherence over the area. We used the Small BAseline Subset (SBAS) multitemporal DInSAR technique from Berardino et al., 2002, to calculate mean ground velocity maps and displacement time series from a large data set of European Remote Sensing Satellites (ERS 1-2) images spanning the time period 1992-2000. The reliability of the DInSAR results was tested calculating the EastSAR and UpSAR values over two permanent global positioning system (GPS) stations in the area, and comparing them with the EastGPS and UpGPS values. The residuals between GPS and DInSAR velocities were 1 and 0.6 mm/yr for the Up and East components, respectively. Four main subsiding areas, previously undetected, have been identified, in correspondence of the towns of Augusta, Siracusa, Priolo, and Villasmundo. The observed deformation phenomena are located within coastal structural basins, filled with Pleistocene and Holocence deposits, except the Villasmundo land subsidence which is located on the Hyblean plateau. The measured deformation rates reach values up to -18 mm/yr in Augusta, -6 mm/yr in Siracusa, -5 mm/yr in Villasmundo and -4.5 mm/yr in Priolo. The examination of velocity profiles, time series, and geological data allows us to relate all the detected deformation patterns primarily to groundwater over-exploitation. A multi-dimensional interpolation with kriging was performed to obtain a field subsidence map. A first order elastic deformation model was used to simulate the peculiar features of the Villasmundo subsidenceen
dc.description.sponsorshipASI-SIGRIS project. ESA Cat1 3769. MIUR Fondo per il sostegno dei giovani.en
dc.language.isoEnglishen
dc.publisher.nameWiley-Blackwellen
dc.relation.ispartofEarth Surface Processes and Landformsen
dc.relation.ispartofseries3/37 (2012)en
dc.subjectsubsidenceen
dc.subjectInSARen
dc.titleLand subsidence along the Ionian coast of SE Sicily (Italy), detection and analysis via Small Baseline Subset (SBAS) multitemporal differential SAR interferometryen
dc.typearticleen
dc.description.statusPublisheden
dc.type.QualityControlPeer-revieweden
dc.description.pagenumber273-286en
dc.subject.INGV05. General::05.08. Risk::05.08.02. Hydrogeological risken
dc.identifier.doi10.1002/esp.2238en
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dc.description.obiettivoSpecifico1.10. TTC - Telerilevamentoen
dc.description.journalTypeJCR Journalen
dc.description.fulltextpartially_openen
dc.relation.issn0197-9337en
dc.relation.eissn1096-9837en
dc.contributor.authorCanova, F.en
dc.contributor.authorTolomei, C.en
dc.contributor.authorSalvi, S.en
dc.contributor.authorToscani, G.en
dc.contributor.authorSeno, S.en
dc.contributor.departmentDipartimento di Scienze della Terra e dell’Ambiente, Università degli Studi di Pavia, Pavia, Italyen
dc.contributor.departmentIstituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione ONT, Roma, Italiaen
dc.contributor.departmentIstituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione ONT, Roma, Italiaen
dc.contributor.departmentDipartimento di Scienze della Terra e dell’Ambiente, Università degli Studi di Pavia, Pavia, Italyen
dc.contributor.departmentDipartimento di Scienze della Terra e dell’Ambiente, Università degli Studi di Pavia, Pavia, Italyen
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crisitem.author.deptDipartimento di Scienze della Terra e dell’Ambiente, Università degli Studi di Pavia, Pavia, Italy-
crisitem.author.deptIstituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione ONT, Roma, Italia-
crisitem.author.deptIstituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione ONT, Roma, Italia-
crisitem.author.deptDipartimento di Scienze della Terra, Università di Pavia. Via Ferrata, 1 - 27100 Pavia, Italy-
crisitem.author.deptDipartimento di Scienze della Terra, Università di Pavia-
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crisitem.author.parentorgIstituto Nazionale di Geofisica e Vulcanologia-
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crisitem.department.parentorgIstituto Nazionale di Geofisica e Vulcanologia-
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