Please use this identifier to cite or link to this item: http://hdl.handle.net/2122/3883
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dc.contributor.authorallTheodoulidis, N.; Institute of Engineering Seismology and Earthquake Engineering (ITSAK), Thessaloniki, Greeceen
dc.contributor.authorallCultrera, G.; Istituto Nazionale di Geofisica e Vulcanologia, Sezione Roma1, Roma, Italiaen
dc.contributor.authorallDe Rubeis, V.; Istituto Nazionale di Geofisica e Vulcanologia, Sezione Roma1, Roma, Italiaen
dc.contributor.authorallCara, F.; Istituto Nazionale di Geofisica e Vulcanologia, Sezione Roma1, Roma, Italiaen
dc.contributor.authorallPanou, A.; Institute of Engineering Seismology and Earthquake Engineering (ITSAK), Thessaloniki, Greeceen
dc.contributor.authorallPagani, M.; Istituto per la Dinamica dei Processi Ambientali, CNR, Milano, Italyen
dc.contributor.authorallTeves-Costa, P.; University of Lisbon, FCUL & Centro de Geofisica da Universidade de Lisboa, Lisboa, Portugalen
dc.date.accessioned2008-06-04T14:18:27Zen
dc.date.available2008-06-04T14:18:27Zen
dc.date.issued2008en
dc.identifier.urihttp://hdl.handle.net/2122/3883en
dc.description.abstractIn the framework of the SESAME project one of the taskswas the compilation of all available ambient noise measurements within urban environments affected by historical or/and recent strong earthquakes in Europe. The aim of such a task was to give an answer to the question; “How does horizontal-to-vertical ambient noise spectral ratio compare with damage in modern cities?”. For this purpose five European urban areas, namely, Angra do Heroismo (Portugal), Fabriano and Palermo (Italy), Thessaloniki and Kalamata (Greece) were selected for which spatial damage information was available either in terms of modified Mercalli intensity or in EMS98 damage grades. The geological setting of the examined sites as well as the causative earthquakes are satisfactorily known. Ambient noise recordings compiled for all examined sites have been homogeneously processed by a technique developed and agreed upon SESAME project. Using a standard multivariate statistical analysis, namely, factor analysis and canonical correlation, the horizontal-to-vertical ambient noise spectral ratio (HVNSR) is correlated with damage pattern observed within examined urban areas. Results show that, in some cases (Thessaloniki, Palermo), the HVNSR seems to be able to differentiate between areas previously shown to be associated with higher damage. In other cases however (Angra do Heroismo, Fabriano, Kalamata), the correlation is not statistically significant indicating thus the complex character of the parameters involved, implying that currently there is no a straightforward way that a value of HVNSR can correctly predict the extent to which a given region will be associated with increased damage.en
dc.language.isoEnglishen
dc.publisher.nameSpringeren
dc.relation.ispartofBulletin of Earthquake Engineeringen
dc.relation.ispartofseries/6 (2008)en
dc.subjectAmbient noiseen
dc.subjectSite effecten
dc.subjectMacroseismic intensityen
dc.subjectFactor and canonical analysisen
dc.titleCorrelation between damage distribution and ambient noise H/V spectral ratio: the SESAME project resultsen
dc.typearticleen
dc.description.statusPublisheden
dc.type.QualityControlPeer-revieweden
dc.description.pagenumber109–140en
dc.subject.INGV04. Solid Earth::04.06. Seismology::04.06.99. General or miscellaneousen
dc.identifier.doi10.1007/s10518-008-9060-yen
dc.description.obiettivoSpecifico4.1. Metodologie sismologiche per l'ingegneria sismicaen
dc.description.journalTypeJCR Journalen
dc.description.fulltextreserveden
dc.contributor.authorTheodoulidis, N.en
dc.contributor.authorCultrera, G.en
dc.contributor.authorDe Rubeis, V.en
dc.contributor.authorCara, F.en
dc.contributor.authorPanou, A.en
dc.contributor.authorPagani, M.en
dc.contributor.authorTeves-Costa, P.en
dc.contributor.departmentInstitute of Engineering Seismology and Earthquake Engineering (ITSAK), Thessaloniki, Greeceen
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.departmentIstituto Nazionale di Geofisica e Vulcanologia, Sezione Roma1, Roma, Italiaen
dc.contributor.departmentInstitute of Engineering Seismology and Earthquake Engineering (ITSAK), Thessaloniki, Greeceen
dc.contributor.departmentIstituto per la Dinamica dei Processi Ambientali, CNR, Milano, Italyen
dc.contributor.departmentUniversity of Lisbon, FCUL & Centro de Geofisica da Universidade de Lisboa, Lisboa, Portugalen
item.openairetypearticle-
item.cerifentitytypePublications-
item.languageiso639-1en-
item.grantfulltextrestricted-
item.openairecristypehttp://purl.org/coar/resource_type/c_18cf-
item.fulltextWith Fulltext-
crisitem.author.deptITSAK, Thessaloniki, Grrece-
crisitem.author.deptIstituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione Roma1, Roma, Italia-
crisitem.author.deptIstituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione Roma1, Roma, Italia-
crisitem.author.deptIstituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione Roma1, Roma, Italia-
crisitem.author.deptITSAK, Thessaloniki, Greece-
crisitem.author.deptCNR-IDPA, Milan, Italy-
crisitem.author.deptICTE-UL, Lisbon, Portugal-
crisitem.author.orcid0000-0002-3335-5655-
crisitem.author.orcid0000-0001-7119-631X-
crisitem.author.orcid0000-0002-1702-563X-
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-
crisitem.department.parentorgIstituto Nazionale di Geofisica e Vulcanologia-
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