1867年维尔京群岛海啸:观测和模拟

Narcisse Zahibo , Efim Pelinovsky , Ahmet Yalciner , Andrey Kurkin , Andrey Koselkov , Andrey Zaitsev
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引用次数: 39

摘要

1867年维尔京群岛发生的海啸对加勒比群岛产生了重大影响。瓜德罗普岛的两个沿海地区(Deshayes和St. Rose)记录到的最大海啸高度为10米。本文还讨论了加勒比海的历史资料。在非线性浅水理论的框架下对1867年海啸进行了模拟。考察了阿内加达海道海啸震源的四个不同方位。研究了加勒比海海啸波的方向性。计算了加勒比海沿岸几个沿海地点的水面波动时程。数值模拟结果与观测数据有较好的一致性。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
The 1867 Virgin Island tsunami: observations and modeling

The 1867 Virgin Island tsunami was of a great effect for the Caribbean Islands. A maximal tsunami height of 10 m was recorded for two coastal locations (Deshayes and St. Rose) in Guadeloupe. The historical data of this event for the Caribbean Sea are discussed. The modeling of the 1867 tsunami is performed in the framework of the nonlinear shallow-water theory. The four different orientations of the tsunami source in the Anegada Passage are examined. The directivity of the tsunami wave in the Caribbean is investigated. The time histories of water surface fluctuations are calculated for several coastal locations on the coasts of the Caribbean Sea. Results of the numerical simulations are in reasonable agreement with data of observations.

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