000 02320nam  2200325za 4500
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008180213s2018    bccabd  ob   f000 0 eng d
020 |a9780660251134
040 |aCaOODSP|beng
041 |aeng|bfre
043 |an-cn-bc
0861 |aFs97-18/322E-PDF
24500|aNumerical modelling of a Cascadia Subduction Zone tsunami at the Canadian Coast Guard base in Seal Cove, Prince Rupert, British Columbia |h[electronic resource] / |cby Isaac V. Fine … [et al.].
260 |aSidney, B.C. : |bOcean Sciences Division, Fisheries and Oceans Canada, Institute of Ocean Sciences, |c2018.
300 |av, 34 p. : |bcol. charts, col. ill., col. maps.
4901 |aCanadian technical report of hydrography and ocean sciences, |x1488-5417 ; |v322
504 |aIncludes bibliographical references.
5203 |a"The last major megathrust earthquake along the Cascadia Subduction Zone (CSZ) off the west coast of North America occurred in January 1700. The massive tsunami waves generated by this moment magnitude (Mw) 9.0 event caused significant destruction as far away as Japan on the opposite side of the Pacific Ocean. Future CSZ events pose a high risk for destructive tsunamis along the British Columbia coast. This work uses a nested-grid numerical tsunami model to predict the tsunami waves and currents at Sea Cove near Prince Rupert generated by an Mw 9.0 CSZ failure. Two updated earthquake source models are used: A buried rupture model (A) and a splay-fracture model (B). Both models include new source areas to the west of Vancouver Island. The analysis is in anticipation of upgrades and modernization of the Canadian Coast Guard facility at Seal Cove"--Abstract, p. iv.
546 |aIncludes abstract in French.
693 4|aTsunamis
693 4|aBritish Columbia
693 4|aMathematical models
7001 |aFine, Isaac.
7101 |aCanada. |bDepartment of Fisheries and Oceans. |bPacific Region. |bOcean Sciences Division.
7102 |aInstitute of Ocean Sciences, Patricia Bay.
830#0|aCanadian technical report of hydrography and ocean sciences,|x1488-5417 ; |v322.|w(CaOODSP)9.504781
85640|qPDF|s10.77 MB|uhttps://publications.gc.ca/collections/collection_2018/mpo-dfo/Fs97-18-322-eng.pdf