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      -Advanced Models for Tsunami and Rogue Waves

      , ,
      Abstract and Applied Analysis
      Hindawi Limited

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          Abstract

          A wavelet , that satisfies the q-advanced differential equation for , is used to model N-wave oscillations observed in tsunamis. Although q-advanced ODEs may seem nonphysical, we present an application that model tsunamis, in particular the Japanese tsunami of March 11, 2011, by utilizing a one-dimensional wave equation that is forced by . The profile is similar to tsunami models in present use. The function is a wavelet that satisfies a q-advanced harmonic oscillator equation. It is also shown that another wavelet, , matches a rogue-wave profile. This is explained in terms of a resonance wherein two small amplitude forcing waves eventually lead to a large amplitude rogue. Since wavelets are used in the detection of tsunamis and rogues, the signal-analysis performance of and is examined on actual data.

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          Most cited references17

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          Oceanic Rogue Waves

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            A note on tsunamis: their generation and propagation in an ocean of uniform depth

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              The Run-Up of N-Waves on Sloping Beaches

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                Author and article information

                Journal
                Abstract and Applied Analysis
                Abstract and Applied Analysis
                Hindawi Limited
                1085-3375
                1687-0409
                2012
                2012
                : 2012
                :
                : 1-26
                Article
                10.1155/2012/414060
                d3bbd934-b152-417f-b554-55ac264ecc00
                © 2012

                http://creativecommons.org/licenses/by/3.0/

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