Please use this identifier to cite or link to this item: http://nopr.niscair.res.in/handle/123456789/42969
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dc.contributor.authorUlutaş, Ergin-
dc.date.accessioned2017-10-30T05:47:40Z-
dc.date.available2017-10-30T05:47:40Z-
dc.date.issued2017-11-
dc.identifier.issn0975-1033 (Online); 0379-5136 (Print)-
dc.identifier.urihttp://nopr.niscair.res.in/handle/123456789/42969-
dc.description2273-2285en_US
dc.description.abstractThe 27 February 2010 Maule (Chile) tsunami was numerically modeled using the SWAN (Simulating WAves Near-Shore) code which solves the non-linear long wave equations of fluid flow by a finite difference algorithm. The computational area is divided into two computational domains with a grid of 2 arc min and 0.5 arc min.  Bathymetry data for the domains are interpolated from the General Bathymetry Chart of the Ocean (GEBCO) 30 arc-seconds grid data. Results from uniform and non-uniform slip models are compared with available tide gauges and Deep-ocean Assessment and Reporting of Tsunami (DART) buoy records.en_US
dc.language.isoen_USen_US
dc.publisherNISCAIR-CSIR, Indiaen_US
dc.rights CC Attribution-Noncommercial-No Derivative Works 2.5 Indiaen_US
dc.sourceIJMS Vol.46(11) [November 2017]en_US
dc.subjectTsunami simulationen_US
dc.subjectShallow water theoryen_US
dc.subjectFinite fault modelen_US
dc.subjectSlip distributionen_US
dc.titleThe 27 February 2010 Maule, Chile tsunami: initial height and propagation from uniform and non-uniform fault slip modelsen_US
dc.typeArticleen_US
Appears in Collections:IJMS Vol.46(11) [November 2017]

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