Please use this identifier to cite or link to this item: http://hdl.handle.net/2122/11000
DC FieldValueLanguage
dc.date.accessioned2018-03-06T08:45:44Zen
dc.date.available2018-03-06T08:45:44Zen
dc.date.issued2018-06en
dc.identifier.urihttp://hdl.handle.net/2122/11000en
dc.description.abstractThe amount of coastal subsidence on the Sele River coastal plain has been examined and measured with local vertical land movement data. The vertical displacements, derived by satellite radar differential interferometry processing (Ps-InSAR), show that the analysed coastal sector is characterised by a southeastward decrease of vertical subsidence rates. These results have been coupled with sea-level rise (SLR) scenarios, in order to identify the most critical areas. In general, the subsidence mostly affects areas where alluvial deposits are thicker, the back-dune areas and the Sele River mouth, all late Holocene in age. Five local SLR scenarios allow identifying zones in the plain potentially prone to inundation and the shoreline retreat for the years 2065 and 2100. For these dates, 2.2% and 7.06% of the investigated area will have a topography lower than the estimated future sea level. Moreover, results show that the extent of the areas potentially exposed to inundation and erosion increases moving from south to north.en
dc.language.isoEnglishen
dc.relation.ispartofJournal of Flood Risk Managementen
dc.relation.ispartofseries/11 (2018)en
dc.subjectClimate changeen
dc.subjectcoastal erosionen
dc.subjectmapping of hazard and risken
dc.subjectremote sensingen
dc.titleCoastal subsidence detected by Synthetic Aperture Radar interferometry and its effects coupled with future sea-level rise: the case of the Sele Plain (Southern Italy)en
dc.typearticleen
dc.description.statusPublisheden
dc.type.QualityControlPeer-revieweden
dc.description.pagenumber191-206en
dc.subject.INGV05.08. Risken
dc.identifier.doi10.1111/jfr3.12308en
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dc.description.obiettivoSpecifico7A. Geofisica per il monitoraggio ambientaleen
dc.description.journalTypeJCR Journalen
dc.contributor.authorDi Paola, G.en
dc.contributor.authorAlberico, I.en
dc.contributor.authorAucelli, P. P. C.en
dc.contributor.authorMatano, F.en
dc.contributor.authorRizzo, A.en
dc.contributor.authorVilardo, Giuseppeen
dc.contributor.departmentDepartment of Science and Technology, University of Naples “Parthenope”, Naples, Italyen
dc.contributor.departmentIAMC - Istituto per l'ambiente marino costiero, Naples, Italyen
dc.contributor.departmentDepartment of Science and Technology, University of Naples “Parthenope”, Naples, Italyen
dc.contributor.departmentIAMC - Istituto per l'ambiente marino costiero, Naples, Italyen
dc.contributor.departmentDepartment of Science and Technology, University of Naples “Parthenope”, Naples, Italyen
dc.contributor.departmentIstituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione OV, Napoli, Italiaen
item.openairetypearticle-
item.cerifentitytypePublications-
item.languageiso639-1en-
item.grantfulltextrestricted-
item.openairecristypehttp://purl.org/coar/resource_type/c_18cf-
item.fulltextWith Fulltext-
crisitem.author.deptIstituto per l’Ambiente Marino Costiero, Consiglio Nazionale delle Ricerche, Calata Porta di Massa, Interno Porto di Napoli, 80133 Naples, Italy-
crisitem.author.deptDepartment of Science and Technology, University of Naples “Parthenope”, Naples, Italy-
crisitem.author.deptIstituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione OV, Napoli, Italia-
crisitem.author.orcid0000-0002-4536-2975-
crisitem.author.orcid0000-0001-7021-9364-
crisitem.author.orcid0000-0001-7240-4467-
crisitem.author.parentorgIstituto Nazionale di Geofisica e Vulcanologia-
crisitem.classification.parent05. General-
crisitem.department.parentorgIstituto Nazionale di Geofisica e Vulcanologia-
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