Numerical tsunami modeling and the bottom relief
- 作者: Kulikov E.A.1, Gusiakov V.K.2,3, Ivanova A.A.1, Baranov B.V.1
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隶属关系:
- Shirshov Institute of Oceanology
- Institute of Computational Technologies, Siberian Branch
- Institute of Computational Mathematics and Mathematical Geophysics, Siberian Branch
- 期: 卷 71, 编号 6 (2016)
- 页面: 527-536
- 栏目: Physics of Earth, Atmosphere, and Hydrosphere (Review)
- URL: https://journals.rcsi.science/0027-1349/article/view/164642
- DOI: https://doi.org/10.3103/S002713491605012X
- ID: 164642
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详细
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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