Articles | Volume 15, issue 8
https://doi.org/10.5194/nhess-15-1763-2015
https://doi.org/10.5194/nhess-15-1763-2015
Research article
 | 
11 Aug 2015
Research article |  | 11 Aug 2015

Scenario-based numerical modelling and the palaeo-historic record of tsunamis in Wallis and Futuna, Southwest Pacific

G. Lamarche, S. Popinet, B. Pelletier, J. Mountjoy, J. Goff, S. Delaux, and J. Bind

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Cited articles

Andréfouët, S. and Diberg, G.: Cartographie et inventaire du système récifal de Wallis, Futuna et Alofi par imagerie satellitaire Landsat 7 ETM+ et orthophotographiquies aériennes à haute résolution spatiale, IRD, Nouméa, New Caledonia, 55 pp., 2006.
Aswani, S. and Graves, M. W.: The Tongan Maritime Expansion: A Case in the Evolutionary Ecology of Social Complexity, Asian Perspect., 37, 135–164, 1998.
Baba, T., Mleczko, R., Burbidge, D., Cummins, P., and Thio, H.: The Effect of the Great Barrier Reef on the Propagation of the 2007 Solomon Islands Tsunami Recorded in Northeastern Australia, PAGEOPH, 165, 2003–2018, 2008.
Barrientos, S. E. and Ward, S. N.: The 1960 Chile earthquake: inversion for slip distribution from surface deformation, Geophys. J. Int., 103, 589–598, 1990.
Beavan, J., Wang, X., Holden, C., Wilson, K., Power, W., Prasetya, G., Bevis, M., and Kautoke, R.: Near-simultaneous great earthquakes at Tongan megathrust and outer rise in September 2009, Nature, 466, 959–963, 2010.
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Short summary
The research investigates the tsunami hazard in the remote French territory of Wallis and Futuna, Southwest Pacific, using numerical computer modelling of tsunami generation, propagation and inundation. Wallis consists of the inhabited island of Uvéa that is surrounded by a lagoon delimited by a barrier reef, whereas Futuna and the island of Alofi form the Horn Archipelago located ca. 240 km east. Futuna and Alofi are surrounded by a narrow fringing reef and emerge from the North Fiji Transform.
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