Please use this identifier to cite or link to this item: http://hdl.handle.net/2122/5442
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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.date.accessioned2010-01-07T14:09:03Zen
dc.date.available2010-01-07T14:09:03Zen
dc.date.issued2009en
dc.identifier.urihttp://hdl.handle.net/2122/5442en
dc.description.abstractThe purpose of this work is to set up a new forecasting model, named Double Branching, for large earth- quakes in Italy. The model is time-dependent, since it assumes that each earthquake can generate, or is correlated to, other earthquakes through different physical mechanisms. In a recent paper [Marzocchi, W., Lombardi, A.M., 2008. A Double Branching model for earthquake occurrence, J. Geophys. Res., 113, B08317. doi:10.1029/2007JB005472] we have shown that the model, applied to two worldwide catalogs in different time–magnitude windows, shows a good fit to the data and its earthquake forecasting performances are superior to what is obtained by the ETAS (single branching model) and by the Poisson models. Remarkably, the model can be tested in a forward perspective, which is the most straightforward way to evaluate the reliability of any forecasting model. Here, we apply this model to the Italian historical seismicity of the last four centuries, with magnitude Mw≥5.5. This application shows that the time-dependent features are comparable to what observed in other applications for different time–space–magnitude window. Moreover, the comparison of the forecasting capability of the Double Branching model and of a spatially-variable stationary Poisson process (used in Italy for seismic hazard assessment) shows that the former has significantly better performances. Finally we provide some probability maps for different temporal windows.en
dc.language.isoEnglishen
dc.publisher.nameElsevieren
dc.relation.ispartofTectonophysicsen
dc.relation.ispartofseries/475 (2009)en
dc.subjectearthquake forecastingen
dc.subjectstochastic modelen
dc.titleDouble Branching model to forecast the next M≥5.5 earthquakes in Italyen
dc.typearticleen
dc.description.statusPublisheden
dc.type.QualityControlPeer-revieweden
dc.description.pagenumber514-523en
dc.subject.INGV04. Solid Earth::04.06. Seismology::04.06.02. Earthquake interactions and probabilityen
dc.identifier.doi10.1016/j.tecto.2009.06.014en
dc.description.obiettivoSpecifico3.1. Fisica dei terremotien
dc.description.obiettivoSpecifico4.2. TTC - Modelli per la stima della pericolosità sismica a scala nazionaleen
dc.description.journalTypeJCR Journalen
dc.description.fulltextreserveden
dc.contributor.authorLombardi, A. M.en
dc.contributor.authorMarzocchi, W.en
dc.contributor.departmentIstituto Nazionale di Geofisica e Vulcanologia, Sezione Roma1, Roma, Italiaen
dc.contributor.departmentIstituto Nazionale di Geofisica e Vulcanologia, Sezione Roma1, Roma, 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 Nazionale di Geofisica e Vulcanologia (INGV), Sezione Roma1, Roma, Italia-
crisitem.author.orcid0000-0002-8326-7135-
crisitem.author.orcid0000-0002-9114-1516-
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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