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


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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.

About the authors

A. A. Ivanova

Shirshov Institute of Oceanology

Author for correspondence.
Email: lapoul@gmail.com
Russian Federation, Moscow, 117997

E. A. Kulikov

Shirshov Institute of Oceanology

Email: lapoul@gmail.com
Russian Federation, Moscow, 117997

I. V. Fine

Institute of Ocean Sciences

Email: lapoul@gmail.com
Canada, Sidney

B. V. Baranov

Shirshov Institute of Oceanology

Email: lapoul@gmail.com
Russian Federation, Moscow, 117997

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