Numerical tsunami modeling and the bottom relief


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The effect of the quality of bathymetric data on the accuracy of tsunami-wave field calculation is considered. A review of the history of the numerical tsunami modeling development is presented. Particular emphasis is made on the World Ocean bottom models. It is shown that the modern digital bathymetry maps, for example, GEBCO, do not adequately simulate the sea bottom in numerical models of wave propagation, leading to considerable errors in estimating the maximum tsunami run-ups on the coast.

作者简介

E. Kulikov

Shirshov Institute of Oceanology

编辑信件的主要联系方式.
Email: kulikove@ocean.ru
俄罗斯联邦, Nakhimovskii pr. 36, Moscow, 117997

V. Gusiakov

Institute of Computational Technologies, Siberian Branch; Institute of Computational Mathematics and Mathematical Geophysics, Siberian Branch

Email: kulikove@ocean.ru
俄罗斯联邦, pr. Akademika Lavrent’eva 6, Novosibirsk, 630090; pr. Akademika Lavrent’eva 6, Novosibirsk, 630090

A. Ivanova

Shirshov Institute of Oceanology

Email: kulikove@ocean.ru
俄罗斯联邦, Nakhimovskii pr. 36, Moscow, 117997

B. Baranov

Shirshov Institute of Oceanology

Email: kulikove@ocean.ru
俄罗斯联邦, Nakhimovskii pr. 36, Moscow, 117997

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