Please use this identifier to cite or link to this item: http://hdl.handle.net/2122/8970
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dc.contributor.authorallTonini, R.; Istituto Nazionale di Geofisica e Vulcanologia, Sezione Roma1, Roma, Italiaen
dc.contributor.authorallArmigliato, A.; Università di Bolognaen
dc.contributor.authorallPagnoni, G.; Università di Bolognaen
dc.contributor.authorallTinti, S.; Università di Bolognaen
dc.date.accessioned2014-03-17T14:54:16Zen
dc.date.available2014-03-17T14:54:16Zen
dc.date.issued2014en
dc.identifier.urihttp://hdl.handle.net/2122/8970en
dc.description.abstractThe Mw = 9.1 mega-thrust Sumatra–Andaman earthquake that occurred on December 26, 2004, was followed by a devastating tsunami that killed hundreds of thousands of people and caused catastrophic effects on human settlements and environments along many coasts of the Indian Ocean, where even countries very far from the source were affected. One of these cases is represented by the Republic of Seychelles, where the tsunami reached the region about 7 h after the earthquake and produced relevant damages, despite the country was more than 4,500 km far from the seismic source. In the present work, we present and discuss a study of the 2004 Sumatra tsunami by means of numerical simulations with the attention focused on the effects observed at the Seychelles Archipelago, a region never previously investigated with this approach. The case is interesting since these islands lay on a very shallow oceanic platform with steep slopes so as the ocean depth changes from thousands to few tens of meters over short distances, with significant effects on the tsunami propagation features: the waves are strongly refracted by the oceanic platform and the tsunami signal is modified by the introduction of additional frequencies. The study is used also to validate the UBO-TSUFD numerical code on a real tsunami event in the far field, and the results are compared with the available observations, i.e., the sea level time series recorded at the Pointe La Rue station, Mahe ́ Island, and run-up measurements and inundation lines surveyed few weeks after the tsunami at Praslin Island, where the tsunami hit during low tide. Synthetic results are found in good agreement with observations, even though some of the observations remain not fully solved. Moreover, simulations have been run in high-tide condition since the 2004 Sumatra tsunami hitting at high tide can be taken as the worst-case scenario for the Seychelles islands and used for tsunami hazard and risk assessmentsen
dc.language.isoEnglishen
dc.publisher.nameSpringer Science+Business Media B.V.en
dc.relation.ispartofNatural Hazardsen
dc.relation.ispartofseries/70 (2014)en
dc.subjectTsunami; Numerical modeling; Indian Ocean; Tsunami scenariosen
dc.titleModeling the 2004 Sumatra tsunami at Seychelles Islands: site-effect analysis and comparison with observationsen
dc.typearticleen
dc.description.statusPublisheden
dc.description.pagenumber1507–1525en
dc.subject.INGV05. General::05.09. Miscellaneous::05.09.99. General or miscellaneousen
dc.identifier.doi10.1007/s11069-013-0886-5en
dc.description.obiettivoSpecifico4T. Fisica dei terremoti e scenari cosismicien
dc.description.journalTypeJCR Journalen
dc.publisherSpringer Netherlandsen
dc.description.fulltextrestricteden
dc.relation.issn0921-030Xen
dc.relation.eissn1573-0840en
dc.contributor.authorTonini, R.en
dc.contributor.authorArmigliato, A.en
dc.contributor.authorPagnoni, G.en
dc.contributor.authorTinti, S.en
dc.contributor.departmentIstituto Nazionale di Geofisica e Vulcanologia, Sezione Roma1, Roma, Italiaen
dc.contributor.departmentUniversità di Bolognaen
dc.contributor.departmentUniversità di Bolognaen
dc.contributor.departmentUniversità di Bolognaen
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 ONT, Roma, Italia-
crisitem.author.deptUniversità di Bologna-
crisitem.author.deptDipartimento di Fisica, Università di Bologna-
crisitem.author.deptUniversità di Bologna-
crisitem.author.orcid0000-0001-7617-7206-
crisitem.author.orcid0000-0003-0901-5471-
crisitem.author.parentorgIstituto Nazionale di Geofisica e Vulcanologia-
crisitem.classification.parent05. General-
crisitem.department.parentorgIstituto Nazionale di Geofisica e Vulcanologia-
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