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dc.contributor.authorLeVeque, Randall J.
dc.contributor.authorWaagan, Knut
dc.contributor.authorGonzález, Frank I.
dc.contributor.authorRim, Donsub
dc.contributor.authorLin, Guang
dc.date.accessioned2017-09-28T11:16:36Z
dc.date.accessioned2017-09-29T08:48:03Z
dc.date.available2017-09-28T11:16:36Z
dc.date.available2017-09-29T08:48:03Z
dc.date.issued2016
dc.identifier.citationLeVeque, Waagan K, González, Rim, Lin. Generating Random Earthquake Events for Probabilistic Tsunami Hazard Assessment. Pure and Applied Geophysics. 2016;173(12):3671-3692en_GB
dc.identifier.urihttp://hdl.handle.net/20.500.12242/648
dc.identifier.urihttps://ffi-publikasjoner.archive.knowledgearc.net/handle/20.500.12242/648
dc.descriptionLeVeque, Randall J.; Waagan, Knut; González, Frank I.; Rim, Donsub; Lin, Guang. Generating Random Earthquake Events for Probabilistic Tsunami Hazard Assessment. Pure and Applied Geophysics 2016 ;Volum 173.(12) s. 3671-3692en_GB
dc.description.abstractTo perform probabilistic tsunami hazard assessment for subduction zone earthquakes, it is necessary to start with a catalog of possible future events along with the annual probability of occurrence, or a probability distribution of such events that can be easily sampled. For near-field events, the distribution of slip on the fault can have a significant effect on the resulting tsunami. We present an approach to defining a probability distribution based on subdividing the fault geometry into many subfaults and prescribing a desired covariance matrix relating slip on one subfault to slip on any other subfault. The eigenvalues and eigenvectors of this matrix are then used to define a Karhunen-Loève expansion for random slip patterns. This is similar to a spectral representation of random slip based on Fourier series but conforms to a general fault geometry. We show that only a few terms in this series are needed to represent the features of the slip distribution that are most important in tsunami generation, first with a simple one-dimensional example where slip varies only in the down-dip direction and then on a portion of the Cascadia Subduction Zone.en_GB
dc.language.isoenen_GB
dc.titleGenerating Random Earthquake Events for Probabilistic Tsunami Hazard Assessmenten_GB
dc.typeArticleen_GB
dc.date.updated2017-09-28T11:16:36Z
dc.identifier.cristinID1415130
dc.identifier.cristinID1415130
dc.identifier.doi10.1007/s00024-016-1357-1
dc.source.issn0033-4553
dc.source.issn1420-9136
dc.type.documentJournal article
dc.relation.journalPure and Applied Geophysics


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