Numerical tsunami modeling and the bottom relief
- Авторы: Kulikov E.A.1, Gusiakov V.K.2,3, Ivanova A.A.1, Baranov B.V.1
-
Учреждения:
- Shirshov Institute of Oceanology
- Institute of Computational Technologies, Siberian Branch
- Institute of Computational Mathematics and Mathematical Geophysics, Siberian Branch
- Выпуск: Том 71, № 6 (2016)
- Страницы: 527-536
- Раздел: 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
Цитировать
Аннотация
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.
Ключевые слова
Об авторах
E. Kulikov
Shirshov Institute of Oceanology
Автор, ответственный за переписку.
Email: kulikove@ocean.ru
Россия, 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
Россия, pr. Akademika Lavrent’eva 6, Novosibirsk, 630090; pr. Akademika Lavrent’eva 6, Novosibirsk, 630090
A. Ivanova
Shirshov Institute of Oceanology
Email: kulikove@ocean.ru
Россия, Nakhimovskii pr. 36, Moscow, 117997
B. Baranov
Shirshov Institute of Oceanology
Email: kulikove@ocean.ru
Россия, Nakhimovskii pr. 36, Moscow, 117997
Дополнительные файлы
