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

A. A. Ivanova; E. A. Kulikov; I. V. Fine; B. V. Baranov

doi:10.3103/S002713491802008X

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

Autores: Ivanova A.A.¹, Kulikov E.A.¹, Fine I.V.², Baranov B.V.¹
Afiliações:
1. Shirshov Institute of Oceanology
2. Institute of Ocean Sciences
Edição: Volume 73, Nº 2 (2018)
Páginas: 234-239
Seção: Physics of Earth, Atmosphere, and Hydrosphere
URL: https://journals.rcsi.science/0027-1349/article/view/164984
DOI: https://doi.org/10.3103/S002713491802008X
ID: 164984

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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.