The 1867 Virgin Island Tsunami

The 1867 Virgin Island Tsunami reached large magnitude on the coasts of the Caribbean Islands. A maximum tsunami height of 10 m was reported for two coastal locations (Deshaies and Sainte-Rose) in Guadeloupe. Modelling of the 1867 tsunami is performed in the framework of the nonlinear shallow-wa...

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Main Authors: N. Zahibo, E. Pelinovsky, A. C. Yalciner, A. Kurkin, A. Koselkov, A. Zaitsev
Format: Article
Language:English
Published: Copernicus Publications 2003-01-01
Series:Natural Hazards and Earth System Sciences
Online Access:http://www.nat-hazards-earth-syst-sci.net/3/367/2003/nhess-3-367-2003.pdf
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author N. Zahibo
E. Pelinovsky
A. C. Yalciner
A. Kurkin
A. Koselkov
A. Zaitsev
author_facet N. Zahibo
E. Pelinovsky
A. C. Yalciner
A. Kurkin
A. Koselkov
A. Zaitsev
author_sort N. Zahibo
collection DOAJ
description The 1867 Virgin Island Tsunami reached large magnitude on the coasts of the Caribbean Islands. A maximum tsunami height of 10 m was reported for two coastal locations (Deshaies and Sainte-Rose) in Guadeloupe. Modelling of the 1867 tsunami is performed in the framework of the nonlinear shallow-water theory. The directivity of the tsunami wave source in the Caribbean Sea according to the assumed initial waveform is investigated. The tsunami records at the several coastal regions in the Lesser Antilles, Virgin Islands, Puerto Rico and South America are simulated. The comparison between the computed and observed data is in reasonable agreement.
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spelling doaj.art-b37c6ed29d6c4560b61e8743c3f0bc8a2022-12-21T23:07:15ZengCopernicus PublicationsNatural Hazards and Earth System Sciences1561-86331684-99812003-01-0135367376The 1867 Virgin Island TsunamiN. ZahiboE. PelinovskyA. C. YalcinerA. KurkinA. KoselkovA. ZaitsevThe 1867 Virgin Island Tsunami reached large magnitude on the coasts of the Caribbean Islands. A maximum tsunami height of 10 m was reported for two coastal locations (Deshaies and Sainte-Rose) in Guadeloupe. Modelling of the 1867 tsunami is performed in the framework of the nonlinear shallow-water theory. The directivity of the tsunami wave source in the Caribbean Sea according to the assumed initial waveform is investigated. The tsunami records at the several coastal regions in the Lesser Antilles, Virgin Islands, Puerto Rico and South America are simulated. The comparison between the computed and observed data is in reasonable agreement.http://www.nat-hazards-earth-syst-sci.net/3/367/2003/nhess-3-367-2003.pdf
spellingShingle N. Zahibo
E. Pelinovsky
A. C. Yalciner
A. Kurkin
A. Koselkov
A. Zaitsev
The 1867 Virgin Island Tsunami
Natural Hazards and Earth System Sciences
title The 1867 Virgin Island Tsunami
title_full The 1867 Virgin Island Tsunami
title_fullStr The 1867 Virgin Island Tsunami
title_full_unstemmed The 1867 Virgin Island Tsunami
title_short The 1867 Virgin Island Tsunami
title_sort 1867 virgin island tsunami
url http://www.nat-hazards-earth-syst-sci.net/3/367/2003/nhess-3-367-2003.pdf
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