Please use this identifier to cite or link to this item: http://hdl.handle.net/2122/6798
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dc.contributor.authorallConvertito, V.; Istituto Nazionale di Geofisica e Vulcanologia, Sezione OV, Napoli, Italiaen
dc.contributor.authorallDe Matteis, R.; Dipartimento di Studi Geologici ed Ambientali, Universita` degli Studi del Sannio, Benevento, Italyen
dc.contributor.authorallCantore, L.; Dipartimento di Scienze Fisiche, Universita` degli Studi di Napoli ‘‘Federico II’’, Naples, Italyen
dc.contributor.authorallZollo, A.; Dipartimento di Scienze Fisiche, Universita` degli Studi di Napoli ‘‘Federico II’’, Naples, Italyen
dc.contributor.authorallIannaccone, G.; Istituto Nazionale di Geofisica e Vulcanologia, Sezione OV, Napoli, Italiaen
dc.contributor.authorallCaccavale, M.; Dipartimento di Scienze Fisiche, Universita` degli Studi di Napoli ‘‘Federico II’’, Naples, Italyen
dc.date.accessioned2011-01-20T14:03:22Zen
dc.date.available2011-01-20T14:03:22Zen
dc.date.issued2010en
dc.identifier.urihttp://hdl.handle.net/2122/6798en
dc.description.abstractStrong ground-shaking mapping soon after a moderate-to-large earthquake is crucial to recognize the areas that have suffered the largest damage and losses. These maps have a fundamental role for emergency services, loss estimation and planning of emergency actions by the Civil Protection Authorities. This is particularly important for areas with high seismic risk levels, such as the Campania-Lucania Region in southern Italy. Taking advantage of the Irpinia Seismic Network (ISNet), a recently installed dense and wide dynamic seismic network, we have developed a procedure for rapid estimation of ground-shaking maps after moderate-to-large earthquakes (GRSmap). This uses an optimal data gridding scheme designed to account for bi-dimensional features of strong groundmotion fields, such as directivity, radiation patterns and focal mechanisms, to which most damage can be correlated. The basis of the mapping technique is a triangulation procedure to locally correct predicted data at the triangle barycentres where their vertices correspond to seismic stations. The method has been tested off-line using a simulated M 6.6 earthquake located at the centre of ISNet and applied to data of the 23 November 1980 Irpina M 6.9 earthquake recorded by a sparse network. This has highlighted its ability to predict peak ground-motion parameters of large magnitude earthquakes with respect to the attenuation relationships.en
dc.language.isoEnglishen
dc.publisher.nameSpringeren
dc.relation.ispartofNatural hazarden
dc.relation.ispartofseries1/52 (2010)en
dc.subjectGround-shaking mapsen
dc.subjectTriangulation schemeen
dc.subjectSeismic sourceen
dc.subjectSeismic hazarden
dc.titleRapid estimation of ground-shaking maps for seismic emergency management in the Campania Region of southern Italyen
dc.typearticleen
dc.description.statusPublisheden
dc.type.QualityControlPeer-revieweden
dc.description.pagenumber97–115en
dc.subject.INGV04. Solid Earth::04.06. Seismology::04.06.99. General or miscellaneousen
dc.identifier.doi10.1007/s11069-009-9359-2en
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dc.description.obiettivoSpecifico4.2. TTC - Modelli per la stima della pericolosità sismica a scala nazionaleen
dc.description.journalTypeJCR Journalen
dc.description.fulltextreserveden
dc.contributor.authorConvertito, V.en
dc.contributor.authorDe Matteis, R.en
dc.contributor.authorCantore, L.en
dc.contributor.authorZollo, A.en
dc.contributor.authorIannaccone, G.en
dc.contributor.authorCaccavale, M.en
dc.contributor.departmentIstituto Nazionale di Geofisica e Vulcanologia, Sezione OV, Napoli, Italiaen
dc.contributor.departmentDipartimento di Studi Geologici ed Ambientali, Universita` degli Studi del Sannio, Benevento, Italyen
dc.contributor.departmentDipartimento di Scienze Fisiche, Universita` degli Studi di Napoli ‘‘Federico II’’, Naples, Italyen
dc.contributor.departmentDipartimento di Scienze Fisiche, Universita` degli Studi di Napoli ‘‘Federico II’’, Naples, Italyen
dc.contributor.departmentIstituto Nazionale di Geofisica e Vulcanologia, Sezione OV, Napoli, Italiaen
dc.contributor.departmentDipartimento di Scienze Fisiche, Universita` degli Studi di Napoli ‘‘Federico II’’, Naples, Italyen
item.openairetypearticle-
item.cerifentitytypePublications-
item.languageiso639-1en-
item.grantfulltextrestricted-
item.openairecristypehttp://purl.org/coar/resource_type/c_18cf-
item.fulltextWith Fulltext-
crisitem.author.deptIstituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione OV, Napoli, Italia-
crisitem.author.deptGeDipartimento di Studi ologici e Ambientali, Università degli Studi del Sannio, Benevento,Italy-
crisitem.author.deptIstituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione Roma1, Roma, Italia-
crisitem.author.deptIstituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione OV, Napoli, Italia-
crisitem.author.deptIstituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione OV, Napoli, Italia-
crisitem.author.deptUnivesità di Napoli, Federico II, Dip. Scienze Fisiche-
crisitem.author.orcid0000-0002-7115-7502-
crisitem.author.orcid0000-0003-2821-0539-
crisitem.author.orcid0000-0002-3490-5583-
crisitem.author.orcid0000-0002-8191-9566-
crisitem.author.orcid0000-0002-1323-9016-
crisitem.author.orcid0000-0003-4389-9370-
crisitem.author.parentorgIstituto Nazionale di Geofisica e Vulcanologia-
crisitem.author.parentorgIstituto Nazionale di Geofisica e Vulcanologia-
crisitem.author.parentorgIstituto Nazionale di Geofisica e Vulcanologia-
crisitem.author.parentorgIstituto Nazionale di Geofisica e Vulcanologia-
crisitem.classification.parent04. Solid Earth-
crisitem.department.parentorgIstituto Nazionale di Geofisica e Vulcanologia-
crisitem.department.parentorgIstituto Nazionale di Geofisica e Vulcanologia-
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