Please use this identifier to cite or link to this item: http://hdl.handle.net/2122/9264
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dc.contributor.authorallEbrahimian, H.; university of Naples federico IIen
dc.contributor.authorallJalayer, F.; university of Naples federico IIen
dc.contributor.authorallAsprone, D.; university of Naples federico IIen
dc.contributor.authorallLombardi, A. M.; Istituto Nazionale di Geofisica e Vulcanologia, Sezione Roma1, Roma, Italiaen
dc.contributor.authorallMarzocchi, W.; Istituto Nazionale di Geofisica e Vulcanologia, Sezione Roma1, Roma, Italiaen
dc.contributor.authorallProta, A.; university of Naples federico IIen
dc.contributor.authorallManfredi, G.; university of Naples federico IIen
dc.date.accessioned2015-01-15T10:17:00Zen
dc.date.available2015-01-15T10:17:00Zen
dc.date.issued2014en
dc.identifier.urihttp://hdl.handle.net/2122/9264en
dc.description.abstractSeismic aftershock-hazard analysis is one of the first steps toward estab- lishing an integrated risk-based decision-making support framework for emergency management in the event of an ongoing aftershock sequence. This work focuses on providing adaptive daily forecasts of the mean daily rate of exceeding various spectral acceleration values (the aftershock hazard). Two well-established earthquake- occurrence models suitable for daily seismicity forecasts associated with the evolution of an aftershock sequence, namely, the modified Omori’s aftershock model (MO) and the epidemic-type aftershock sequence (ETAS) are adopted. An adaptive and evolution- ary MO-based aftershock occurrence model with distinct spatial and temporal compo- nents is proposed. In this model, the parameters deciding the temporal decay are updated based on the data provided by the ongoing aftershock sequence. This model adopts an evolutionary spatial seismicity pattern loosely based on spatial clustering of aftershock events in the sequence. Bayesian updating is also employed to provide sequence-based parameter estimates for a given ground-motion prediction model. Daily forecasts of the mean rate of exceedance of various spectral acceleration levels are calculated based on alternative occurrence models and the updated ground-motion prediction relation. As a numerical example, daily forecasts of the aftershock-hazard curve are obtained for the L’Aquila aftershock sequence based on the MO-based and ETAS occurrence models, and an updated version of the Sabetta and Pugliese (1996) ground-motion prediction model. These daily hazard forecasts are then compared with the observed daily rates of exceeding various spectral acceleration thresholds.en
dc.language.isoEnglishen
dc.publisher.nameSeismological Society of Americaen
dc.relation.ispartofBulletin of the Seismological Society of Americaen
dc.relation.ispartofseries/104 (2014)en
dc.subjectearthquake forecasten
dc.subjectaftershocken
dc.titleAdaptive daily forecasting of seismic aftershock hazarden
dc.typearticleen
dc.description.statusPublisheden
dc.type.QualityControlPeer-revieweden
dc.description.pagenumber145 – 161en
dc.subject.INGV04. Solid Earth::04.06. Seismology::04.06.11. Seismic risken
dc.identifier.doi10.1785/0120130040en
dc.description.obiettivoSpecifico3T. Pericolosità sismica e contributo alla definizione del rischioen
dc.description.journalTypeJCR Journalen
dc.description.fulltextreserveden
dc.relation.issn0037-1106en
dc.relation.eissn1943-3573en
dc.contributor.authorEbrahimian, H.en
dc.contributor.authorJalayer, F.en
dc.contributor.authorAsprone, D.en
dc.contributor.authorLombardi, A. M.en
dc.contributor.authorMarzocchi, W.en
dc.contributor.authorProta, A.en
dc.contributor.authorManfredi, G.en
dc.contributor.departmentuniversity of Naples federico IIen
dc.contributor.departmentuniversity of Naples federico IIen
dc.contributor.departmentuniversity of Naples federico IIen
dc.contributor.departmentIstituto Nazionale di Geofisica e Vulcanologia, Sezione Roma1, Roma, Italiaen
dc.contributor.departmentIstituto Nazionale di Geofisica e Vulcanologia, Sezione Roma1, Roma, Italiaen
dc.contributor.departmentuniversity of Naples federico IIen
dc.contributor.departmentuniversity of Naples federico IIen
item.openairetypearticle-
item.cerifentitytypePublications-
item.languageiso639-1en-
item.grantfulltextreserved-
item.openairecristypehttp://purl.org/coar/resource_type/c_18cf-
item.fulltextWith Fulltext-
crisitem.author.deptuniversity of Naples federico II-
crisitem.author.deptIstituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione Roma1, Roma, Italia-
crisitem.author.deptuniversity of Naples federico II-
crisitem.author.orcid0000-0002-7580-8309-
crisitem.author.orcid0000-0002-8326-7135-
crisitem.author.orcid0000-0002-9114-1516-
crisitem.author.orcid0000-0003-3820-663X-
crisitem.author.orcid0000-0002-4860-4511-
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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