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<identifier>oai:HAL:hal-00330900v1</identifier>
<datestamp>2018-01-05</datestamp>
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<publisher>HAL CCSD</publisher>
<title lang=en>The 1867 Virgin Island Tsunami</title>
<creator>Zahibo, Narcisse</creator>
<creator>Pelinovsky, E.</creator>
<creator>Yalciner, A. C.</creator>
<creator>Kurkin, A.</creator>
<creator>Koselkov, A.</creator>
<creator>Zaitsev, A.</creator>
<contributor>Laboratoire de Physique de l'Atmosphère Tropicale (LPAT) ; Université des Antilles et de la Guyane (UAG)</contributor>
<contributor>Laboratory of Hydrophysics and Nonlinear Acoustics ; Institute of Applied Physics</contributor>
<contributor>Civil Engineering Department ; Ocean Engineering Research Center</contributor>
<contributor>Applied Mathematics Department ; Applied Mathematics Department</contributor>
<description>International audience</description>
<source>Natural Hazards and Earth System Science</source>
<publisher>Copernicus Publications on behalf of the European Geosciences Union</publisher>
<identifier>hal-00330900</identifier>
<identifier>https://hal.archives-ouvertes.fr/hal-00330900</identifier>
<identifier>https://hal.archives-ouvertes.fr/hal-00330900/document</identifier>
<identifier>https://hal.archives-ouvertes.fr/hal-00330900/file/nhess-3-367-2003.pdf</identifier>
<source>https://hal.archives-ouvertes.fr/hal-00330900</source>
<source>Natural Hazards and Earth System Science, Copernicus Publications on behalf of the European Geosciences Union, 2003, 3 (5), pp.367-376</source>
<language>en</language>
<subject>[SDU.ENVI] Sciences of the Universe [physics]/Continental interfaces, environment</subject>
<subject>[SDU.OCEAN] Sciences of the Universe [physics]/Ocean, Atmosphere</subject>
<subject>[SDU.STU] Sciences of the Universe [physics]/Earth Sciences</subject>
<type>info:eu-repo/semantics/article</type>
<type>Journal articles</type>
<description lang=en>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.</description>
<date>2003</date>
<rights>info:eu-repo/semantics/OpenAccess</rights>
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