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Generation of a Tsunami from the Submarine Landslide Near the East Coast of Sakhalin Island

  • Physics of Earth, Atmosphere, and Hydrosphere
  • Published:
Moscow University Physics Bulletin Aims and scope

Abstract

The effect of the generation of tsunami waves caused by collapse of the continental slope and by formation of a submarine landslide near the east coast of Sakhalin Island is reproduced within the framework of a hydrodynamic model. The calculations performed using the numerical hydrodynamic model showed that such a submarine landslide can generate a tsunami wave up to 18 m high on the Sakhalin coast.

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Authors and Affiliations

  1. Shirshov Institute of Oceanology, Russian Academy of Sciences, Moscow, 117997, Russia

    A. A. Ivanova, E. A. Kulikov & B. V. Baranov

  2. Institute of Ocean Sciences, Sidney, Canada

    I. V. Fine

Authors
  1. A. A. Ivanova
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  2. E. A. Kulikov
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  3. I. V. Fine
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  4. B. V. Baranov
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Corresponding author

Correspondence to A. A. Ivanova.

Additional information

Original Russian Text © A.A. Ivanova, E.A. Kulikov, I.V. Fine, B.V. Baranov, 2018, published in Vestnik Moskovskogo Universiteta, Seriya 3: Fizika, Astronomiya, 2018, No. 2, pp. 113–118.

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Ivanova, A.A., Kulikov, E.A., Fine, I.V. et al. Generation of a Tsunami from the Submarine Landslide Near the East Coast of Sakhalin Island. Moscow Univ. Phys. 73, 234–239 (2018). https://doi.org/10.3103/S002713491802008X

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  • DOI: https://doi.org/10.3103/S002713491802008X

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