Please use this identifier to cite or link to this item: http://hdl.handle.net/2122/7997
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dc.contributor.authorallVecchio, A.; Università della Calabriaen
dc.contributor.authorallAnzidei, M.; Istituto Nazionale di Geofisica e Vulcanologia, Sezione CNT, Roma, Italiaen
dc.contributor.authorallCapparelli, V.; Università della Calabriaen
dc.contributor.authorallCarbone, V.; Università della Calabriaen
dc.contributor.authorallGuerra, I.; Università della Calabriaen
dc.date.accessioned2012-06-25T07:05:38Zen
dc.date.available2012-06-25T07:05:38Zen
dc.date.issued2012-06en
dc.identifier.urihttp://hdl.handle.net/2122/7997en
dc.description.abstractThe possibility that the tsunami, generated as a consequence of the large Mw 9.0 Tohoku-Oki earthquake of March 11th 2011, could be recorded by the tide gauge stations located in the Mediterranean Sea has been investigated. We find two kinds of transient signatures which should be attributed to the far-field destabilizing effect of the tsunami on the usual tidal components: 1) the excitation of a broad spectrum of frequency fluctuations, superimposed to the diurnal and semidiurnal tidal components, 2) the change of amplitude of the low-frequency tidal components in the Mediterranean, related to the sea surface fluctuation perhaps caused by the direct transmission of the tsunami across Gibraltar.en
dc.language.isoEnglishen
dc.relation.ispartofEPL (Europhysics Letters)en
dc.relation.ispartofseries5/98 (2012)en
dc.subjectTsunamis, earth tides, giant earthquakes, sea levelen
dc.titleHas the Mediterranean Sea felt the March 11th, 2011, Mw 9.0 Tohoku-Oki earthquake?en
dc.typearticleen
dc.description.statusPublisheden
dc.type.QualityControlPeer-revieweden
dc.description.pagenumber59001en
dc.subject.INGV03. Hydrosphere::03.01. General::03.01.99. General or miscellaneousen
dc.identifier.doi10.1209/0295-5075/98/59001en
dc.description.obiettivoSpecifico3.7. Dinamica del clima e dell'oceanoen
dc.description.journalTypeJCR Journalen
dc.description.fulltextembargoed_20120801en
dc.relation.issn0295-5075en
dc.contributor.authorVecchio, A.en
dc.contributor.authorAnzidei, M.en
dc.contributor.authorCapparelli, V.en
dc.contributor.authorCarbone, V.en
dc.contributor.authorGuerra, I.en
dc.contributor.departmentUniversità della Calabriaen
dc.contributor.departmentIstituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione ONT, Roma, Italiaen
dc.contributor.departmentUniversità della Calabriaen
dc.contributor.departmentUniversità della Calabriaen
dc.contributor.departmentUniversità della Calabriaen
item.openairetypearticle-
item.cerifentitytypePublications-
item.languageiso639-1en-
item.grantfulltextopen-
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 della Calabria-
crisitem.author.deptDipartimento di Biologia Ecologia e Scienze della Terra, Università della Calabria, Arcavacata di Rende, Cs-
crisitem.author.orcid0000-0003-1935-1049-
crisitem.author.orcid0000-0002-3182-6679-
crisitem.author.parentorgIstituto Nazionale di Geofisica e Vulcanologia-
crisitem.classification.parent03. Hydrosphere-
crisitem.department.parentorgIstituto Nazionale di Geofisica e Vulcanologia-
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