Generation of a Tsunami from the Submarine Landslide Near the East Coast of Sakhalin Island
- Authors: Ivanova A.A.1, Kulikov E.A.1, Fine I.V.2, Baranov B.V.1
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Affiliations:
- Shirshov Institute of Oceanology
- Institute of Ocean Sciences
- Issue: Vol 73, No 2 (2018)
- Pages: 234-239
- Section: Physics of Earth, Atmosphere, and Hydrosphere
- URL: https://journal-vniispk.ru/0027-1349/article/view/164984
- DOI: https://doi.org/10.3103/S002713491802008X
- ID: 164984
Cite item
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.
Keywords
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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