Please use this identifier to cite or link to this item: http://hdl.handle.net/2122/3066
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dc.contributor.authorallIervolino, I.; Dipartimento di Analisi e Progettazione Strutturale, Università di Napoli Federico II, Naples, Italyen
dc.contributor.authorallConvertito, V.; Istituto Nazionale di Geofisica e Vulcanologia, Sezione OV, Napoli, Italiaen
dc.contributor.authorallGiorgio, M.;  Dipartimento di Ingegneria Aerospaziale e Meccanica, Seconda Università di Napoli, Aversa, Italyen
dc.contributor.authorallManfredi, G.; Dipartimento di Analisi e Progettazione Strutturale, Università di Napoli Federico II, Naples, Italyen
dc.contributor.authorallZollo, A.;  RISSC-Lab, Dipartimento di Scienze Fisiche, Università di Napoli Federico II, Naples, Italyen
dc.contributor.editorallGasparini, P.en
dc.date.accessioned2007-12-11T12:06:16Zen
dc.date.available2007-12-11T12:06:16Zen
dc.date.issued2007en
dc.identifier.urihttp://hdl.handle.net/2122/3066en
dc.description.abstractEarthquake early warning systems (EEWS), based on real-time prediction of ground motion or structural response measures, may play a role in re- ducing vulnerability and/or exposure of buildings and lifelines. Indeed, seismologists have recently developed efficient methods for real-time es- timation of an event’s magnitude and location based on limited informa- tion of the P-waves. Therefore, when an event occurs, estimates of magni- tude and source-to-site distance are available, and the prediction of the structural demand at the site may be performed by Probabilistic Seismic Hazard Analysis (PSHA) and then by Probabilistic Seismic Demand Analysis (PSDA) depending upon EEWS measures. Such an approach contains a higher level of information with respect to traditional seismic risk analysis and may be used for real-time risk management. However, this kind of prediction is performed in very uncertain conditions which may affect the effectiveness of the system and therefore have to be taken into due account. In the present study the performance of the EWWS under development in the Campania region (southern Italy) is assessed by simu- lation. The earthquake localization is formulated in a Voronoi cells ap- proach, while a Bayesian method is used for magnitude estimation. Simu- lation has an empirical basis but requires no recorded signals. Our results, in terms of hazard analysis and false/missed alarm probabilities, lead us to conclude that the PSHA depending upon the EEWS significantly improves seismic risk prediction at the site and is close to what could be produced if magnitude and distance were deterministically known.en
dc.language.isoEnglishen
dc.publisher.nameSpringeren
dc.relation.ispartofEarthquake Early Warning Systemen
dc.subjectEarthquake Earlyen
dc.subjectCampania Regionen
dc.titleThe Crywolf Issue in Earthquake Early Warning Applications for the Campania Regionen
dc.typebook chapteren
dc.description.statusPublisheden
dc.type.QualityControlUnreferreden
dc.description.pagenumber211-232en
dc.subject.INGV04. Solid Earth::04.06. Seismology::04.06.03. Earthquake source and dynamicsen
dc.subject.INGV04. Solid Earth::04.06. Seismology::04.06.04. Ground motionen
dc.subject.INGV04. Solid Earth::04.06. Seismology::04.06.11. Seismic risken
dc.description.obiettivoSpecifico4.1. Metodologie sismologiche per l'ingegneria sismicaen
dc.description.fulltextreserveden
dc.contributor.authorIervolino, I.en
dc.contributor.authorConvertito, V.en
dc.contributor.authorGiorgio, M.en
dc.contributor.authorManfredi, G.en
dc.contributor.authorZollo, A.en
dc.contributor.departmentDipartimento di Analisi e Progettazione Strutturale, Università di Napoli Federico II, Naples, Italyen
dc.contributor.departmentIstituto Nazionale di Geofisica e Vulcanologia, Sezione OV, Napoli, Italiaen
dc.contributor.department Dipartimento di Ingegneria Aerospaziale e Meccanica, Seconda Università di Napoli, Aversa, Italyen
dc.contributor.departmentDipartimento di Analisi e Progettazione Strutturale, Università di Napoli Federico II, Naples, Italyen
dc.contributor.department RISSC-Lab, Dipartimento di Scienze Fisiche, Università di Napoli Federico II, Naples, Italyen
dc.contributor.editorGasparini, P.en
item.openairetypebook chapter-
item.cerifentitytypePublications-
item.languageiso639-1en-
item.grantfulltextrestricted-
item.openairecristypehttp://purl.org/coar/resource_type/c_18cf-
item.fulltextWith Fulltext-
crisitem.author.deptUniversità degli Studi di Napoli Federico II-
crisitem.author.deptIstituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione OV, Napoli, Italia-
crisitem.author.deptUniversità degli Studi di Napoli Federico II-
crisitem.author.deptIstituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione OV, Napoli, Italia-
crisitem.author.orcid0000-0002-4076-2718-
crisitem.author.orcid0000-0002-7115-7502-
crisitem.author.orcid0000-0002-5348-5289-
crisitem.author.orcid0000-0002-4860-4511-
crisitem.author.orcid0000-0002-8191-9566-
crisitem.author.parentorgIstituto Nazionale di Geofisica e Vulcanologia-
crisitem.author.parentorgIstituto Nazionale di Geofisica e Vulcanologia-
crisitem.classification.parent04. Solid Earth-
crisitem.classification.parent04. Solid Earth-
crisitem.classification.parent04. Solid Earth-
crisitem.department.parentorgIstituto Nazionale di Geofisica e Vulcanologia-
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