<efrbr:recordSet xmlns:xsi="http://www.w3.org/2001/XMLSchema-instance" xmlns:efrbr="http://vfrbr.info/efrbr/1.1" xmlns:efrbr-work="http://vfrbr.info/efrbr/1.1/work" xmlns:efrbr-expression="http://vfrbr.info/efrbr/1.1/expression" xmlns:efrbr-manifestation="http://vfrbr.info/efrbr/1.1/manifestation" xmlns:efrbr-person="http://vfrbr.info/efrbr/1.1/person" xmlns:efrbr-corporateBody="http://vfrbr.info/efrbr/1.1/corporateBody" xmlns:efrbr-concept="http://vfrbr.info/efrbr/1.1/concept" xmlns:efrbr-structure="http://vfrbr.info/efrbr/1.1/structure" xmlns:efrbr-responsible="http://vfrbr.info/efrbr/1.1/responsible" xmlns:efrbr-subject="http://vfrbr.info/efrbr/1.1/subject" xmlns:efrbr-other="http://vfrbr.info/efrbr/1.1/other" xsi:schemaLocation="http://vfrbr.info/efrbr/1.1 http://vfrbr.info/schemas/1.1/efrbr.xsd"><efrbr:entities><efrbr-work:work identifier="http://purl.tuc.gr/dl/dias/E945AF8B-0D34-4EFC-86FF-5674AF6C8E66"><efrbr-work:titleOfTheWork>Tsunami sources in the southern California Bight</efrbr-work:titleOfTheWork></efrbr-work:work><efrbr-expression:expression identifier="http://purl.tuc.gr/dl/dias/E945AF8B-0D34-4EFC-86FF-5674AF6C8E66"><efrbr-expression:titleOfTheExpression>Tsunami sources in the southern California Bight</efrbr-expression:titleOfTheExpression><efrbr-expression:formOfExpression vocabulary="DIAS:TYPES">
            Peer-Reviewed Journal Publication
            Δημοσίευση σε Περιοδικό με Κριτές
         </efrbr-expression:formOfExpression><efrbr-expression:dateOfExpression type="issued">2015-10-10</efrbr-expression:dateOfExpression><efrbr-expression:dateOfExpression type="published">2004</efrbr-expression:dateOfExpression><efrbr-expression:languageOfExpression vocabulary="iso639-1">en</efrbr-expression:languageOfExpression><efrbr-expression:summarizationOfContent>Locally generated tsunamis due to faulting or slope failures offshore southern California threaten nearby coastal cities. Disruption of operations at port facilities due to tsunami attack could severely impact the regional and national economies. This study examines three faults and two landslides scenarios as potential tsunami sources. Computed runup ranges from 0.5 to 6 m depending on the source and location. Bathymetric features such as the broad San Pedro Shelf are shown to contribute to tsunami wave focusing while retarding tsunami arrival times, suggesting the usefulness of an early warning system.</efrbr-expression:summarizationOfContent><efrbr-expression:useRestrictionsOnTheExpression type="creative-commons">http://creativecommons.org/licenses/by/4.0/</efrbr-expression:useRestrictionsOnTheExpression><efrbr-expression:note type="journal name">Geophysical Research Letters</efrbr-expression:note><efrbr-expression:note type="journal volume">4</efrbr-expression:note><efrbr-expression:note type="journal number">28</efrbr-expression:note><efrbr-expression:note type="page range">643–646</efrbr-expression:note></efrbr-expression:expression><efrbr-person:person identifier="http://users.isc.tuc.gr/~ksynolakis"><efrbr-person:nameOfPerson vocabulary="TUC:LDAP">
            Synolakis Kostas
            Συνολακης Κωστας
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            Mark R. Legg
         </efrbr-person:nameOfPerson></efrbr-person:person><efrbr-person:person identifier="41B32BCA-DA56-46C7-8ECA-FCE0879FFAE0"><efrbr-person:nameOfPerson vocabulary="">
            José C. Borrero
         </efrbr-person:nameOfPerson></efrbr-person:person><efrbr-concept:concept identifier="http://id.loc.gov/authorities/subjects/sh85138348"><efrbr-concept:termForTheConcept>
            Earthquake sea waves
            Seismic sea waves
            Seismic surges
            Tidal waves
            Tunamis
            tsunamis
            earthquake sea waves
            seismic sea waves
            seismic surges
            tidal waves
            tunamis
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