Articles | Volume 38
Adv. Geosci., 38, 43–53, 2014
https://doi.org/10.5194/adgeo-38-43-2014
Adv. Geosci., 38, 43–53, 2014
https://doi.org/10.5194/adgeo-38-43-2014

  25 Jul 2014

25 Jul 2014

Impact of a tsunami generated at the Lesser Antilles subduction zone on the Northern Atlantic Ocean coastlines

J. Roger*,1, A. Frère3,2, and H. Hébert2 J. Roger et al.
  • 1Université des Antilles et de la Guyane, Laboratoire LaRGe, 97157 Pointe à Pitre Cedex, Guadeloupe (FWI)
  • 2CEA/DAM/DIF, 91297 Arpajon, France
  • 3Institut de Physique du Globe de Paris, 75007, Paris, France
  • *now at: GMER Etudes Marines, Avenue de l'Europe, 97118 Saint-François, Guadeloupe (FWI)

Abstract. On 11 March 2011, a Mw ~ 9.0 megathrust earthquake occurred off the coast of Tohoku, triggering a catastrophic tsunami reaching heights of 10 m and more in some places and resulting in lots of casualties and destructions. It is one of a handful of catastrophic tsunamis having occurred during the last decade, following the 2004 Indonesian tsunami, and leading to the preparation of tsunami warning systems and evacuation plans all around the world. In the Atlantic Ocean, which has been struck by two certified transoceanic tsunamis over the past centuries (the 1755 "Lisbon" and 1929 Grand Banks events), a warning system is also under discussion, especially for what concerns potential tsunamigenic sources off Iberian Peninsula. In addition, the Lesser Antilles subduction zone is also potentially able to generate powerful megathrust ruptures as the 8 February 1843 Mw ~ 8.0/8.5 earthquake, that could trigger devastating tsunamis propagating across the Northern Atlantic Ocean. The question is in which conditions these tsunamis could be able to reach the Oceanic Islands as well as the eastern shores of the Atlantic Ocean, and what could be the estimated times to react and wave heights to expect? This paper attempts to answer those questions through the use of numerical modelings and recent research results about the Lesser Antilles ability to produce megathrust earthquakes.

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