Near-coast tsunami waveguiding: phenomenon and simulations

Embrecht W.C. van Groesen, D. Adytia, D. Adytia, A. Andonowati

    Research output: Contribution to journalArticleAcademicpeer-review

    8 Citations (Scopus)
    38 Downloads (Pure)

    Abstract

    In this paper we show that shallow, elongated parts in a sloping bottom toward the coast will act as a waveguide and lead to large enhanced wave amplification for tsunami waves. Since this is even the case for narrow shallow regions, near-coast tsunami waveguiding may contribute to an explanation that tsunami heights and coastal effects as observed in reality show such high variability along the coastline. For accurate simulations, the complicated flow near the waveguide has to be resolved accurately, and grids that are too coarse will greatly underestimate the effects. We will present some results of extensive simulations using shallow water and a linear dispersive Variational Boussinesq model.
    Original languageUndefined
    Pages (from-to)175-185
    Number of pages11
    JournalNatural hazards and earth system sciences
    Volume8
    Issue number2
    DOIs
    Publication statusPublished - 2008

    Keywords

    • METIS-255886
    • EWI-15080
    • IR-65390

    Cite this

    van Groesen, Embrecht W.C. ; Adytia, D. ; Adytia, D. ; Andonowati, A. / Near-coast tsunami waveguiding: phenomenon and simulations. In: Natural hazards and earth system sciences. 2008 ; Vol. 8, No. 2. pp. 175-185.
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    Near-coast tsunami waveguiding: phenomenon and simulations. / van Groesen, Embrecht W.C.; Adytia, D.; Adytia, D.; Andonowati, A.

    In: Natural hazards and earth system sciences, Vol. 8, No. 2, 2008, p. 175-185.

    Research output: Contribution to journalArticleAcademicpeer-review

    TY - JOUR

    T1 - Near-coast tsunami waveguiding: phenomenon and simulations

    AU - van Groesen, Embrecht W.C.

    AU - Adytia, D.

    AU - Adytia, D.

    AU - Andonowati, A.

    PY - 2008

    Y1 - 2008

    N2 - In this paper we show that shallow, elongated parts in a sloping bottom toward the coast will act as a waveguide and lead to large enhanced wave amplification for tsunami waves. Since this is even the case for narrow shallow regions, near-coast tsunami waveguiding may contribute to an explanation that tsunami heights and coastal effects as observed in reality show such high variability along the coastline. For accurate simulations, the complicated flow near the waveguide has to be resolved accurately, and grids that are too coarse will greatly underestimate the effects. We will present some results of extensive simulations using shallow water and a linear dispersive Variational Boussinesq model.

    AB - In this paper we show that shallow, elongated parts in a sloping bottom toward the coast will act as a waveguide and lead to large enhanced wave amplification for tsunami waves. Since this is even the case for narrow shallow regions, near-coast tsunami waveguiding may contribute to an explanation that tsunami heights and coastal effects as observed in reality show such high variability along the coastline. For accurate simulations, the complicated flow near the waveguide has to be resolved accurately, and grids that are too coarse will greatly underestimate the effects. We will present some results of extensive simulations using shallow water and a linear dispersive Variational Boussinesq model.

    KW - METIS-255886

    KW - EWI-15080

    KW - IR-65390

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    DO - 10.5194/nhess-8-175-2008

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    JF - Natural hazards and earth system sciences

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