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- W2341671803 endingPage "20160052" @default.
- W2341671803 startingPage "20160052" @default.
- W2341671803 abstract "Tsunamis generated by landslides and volcanic island collapses account for some of the most catastrophic events recorded, yet critically important field data related to the landslide motion and tsunami evolution remain lacking. Landslide-generated tsunami source and propagation scenarios are physically modelled in a three-dimensional tsunami wave basin. A unique pneumatic landslide tsunami generator was deployed to simulate landslides with varying geometry and kinematics. The landslides were generated on a planar hill slope and divergent convex conical hill slope to study lateral hill slope effects on the wave characteristics. The leading wave crest amplitude generated on a planar hill slope is larger on average than the leading wave crest generated on a convex conical hill slope, whereas the leading wave trough and second wave crest amplitudes are smaller. Between 1% and 24% of the landslide kinetic energy is transferred into the wave train. Cobble landslides transfer on average 43% more kinetic energy into the wave train than corresponding gravel landslides. Predictive equations for the offshore propagating wave amplitudes, periods, celerities and lengths generated by landslides on planar and divergent convex conical hill slopes are derived, which allow an initial rapid tsunami hazard assessment." @default.
- W2341671803 created "2016-06-24" @default.
- W2341671803 creator A5018796061 @default.
- W2341671803 creator A5074167085 @default.
- W2341671803 date "2016-04-01" @default.
- W2341671803 modified "2023-10-17" @default.
- W2341671803 title "Physical modelling of tsunamis generated by three-dimensional deformable granular landslides on planar and conical island slopes" @default.
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- W2341671803 doi "https://doi.org/10.1098/rspa.2016.0052" @default.
- W2341671803 hasPubMedCentralId "https://www.ncbi.nlm.nih.gov/pmc/articles/4887769" @default.
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