Please use this identifier to cite or link to this item: http://hdl.handle.net/2122/3037
DC FieldValueLanguage
dc.contributor.authorallZollo, A.; RISSC-Lab, Dipartimento di Scienze Fisiche, Università di Napoli Federico IIen
dc.contributor.authorallLancieri, M.; RISSC-Lab, Dipartimento di Scienze Fisiche, Università di Napoli Federico IIen
dc.contributor.editorallGasparini, P.en
dc.date.accessioned2007-12-10T15:25:47Zen
dc.date.available2007-12-10T15:25:47Zen
dc.date.issued2007en
dc.identifier.urihttp://hdl.handle.net/2122/3037en
dc.description.abstractA prototype system for earthquake early warning and rapid shake map evaluation is being developed and tested in southern Italy based on a dense, dynamic seismic network (accelerometers + seismometers) under installation in the Apenninic belt region (Irpinia Seismic Network). It can be classified as a regional Earthquake Early Warning System consisting of a broad-based seismic sensor network covering a portion or the entire area which is threatened by the quake's strike. The real time magnitude estimate will take advantage from the high spatial density of the network in the source region and the broad dynamic range of installed instruments. Based on the offline analysis of high quality strong-motion data bases recorded in Italy, several methods are envisaged, using different observed quantities (peak amplitude, dominant frequency, square velocity integral, …) to be measured on seismograms, as a function of time, both on P and early-S wave signals. Results from the analysis of the Italian strong motion database point out the possibility of using low-pass filtered displacement and velocity peak amplitudes measured in time windows lasting less than 3-4 sec after the first P- or S-wave arrivals. These parameters show they are robustly correlated with moment magnitude. The correlation found of 3Hz low-pass filtered PGV and PGD with magnitude is discussed and interpreted in terms of plausible dynamic models of the earthquake rupture process during its initial stage.en
dc.language.isoEnglishen
dc.publisher.nameSpringeren
dc.relation.ispartofEarthquake Early Warning Systemsen
dc.subjectReal-time Estimationen
dc.subjectMagnitudeen
dc.subjectSeismic Early Warningen
dc.title4 Real-time Estimation of Earthquake Magnitude for Seismic Early Warningen
dc.typebook chapteren
dc.description.statusPublisheden
dc.type.QualityControlUnreferreden
dc.description.pagenumber45-63en
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.authorZollo, A.en
dc.contributor.authorLancieri, M.en
dc.contributor.departmentRISSC-Lab, Dipartimento di Scienze Fisiche, Università di Napoli Federico IIen
dc.contributor.departmentRISSC-Lab, Dipartimento di Scienze Fisiche, Università di Napoli Federico IIen
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.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.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-
Appears in Collections:Book chapters
Files in This Item:
File Description SizeFormat Existing users please Login
ZolLan-2007.pdf2.22 MBAdobe PDF
Show simple item record

Page view(s)

126
checked on Apr 24, 2024

Download(s)

22
checked on Apr 24, 2024

Google ScholarTM

Check