Numerical simulation of submarine landslides and generated tsunamis: application to the on-going Mayotte seismo-volcanic crisis

被引:6
作者
Poulain, Pablo [1 ,2 ]
Le Friant, Anne [1 ]
Pedreros, Rodrigo [2 ]
Mangeney, Anne [1 ]
Filippini, Andrea G. [2 ]
Grandjean, Gilles [2 ]
Lemoine, Anne [2 ]
Fernandez-Nieto, Enrique D. [3 ]
Castro Diaz, Manuel J. [4 ]
Peruzzetto, Marc [2 ]
机构
[1] Univ Paris Cite, Inst Phys Globe Paris, Paris, France
[2] Bur Rech Geol & Minieres, Orleans, France
[3] Univ Seville, Dept Matemat Aplicada, Seville, Spain
[4] Univ Malaga, Dept Anal Matemat, Malaga, Spain
关键词
BOUSSINESQ-TYPE EQUATIONS; DEBRIS AVALANCHE; GRANULAR FLOWS; WATER-WAVES; FLANK COLLAPSE; SURFACE-WAVES; ONE-LAYER; MODEL; 2-LAYER; PROPAGATION;
D O I
10.5802/crgeos.138
中图分类号
P [天文学、地球科学];
学科分类号
07 ;
摘要
SinceMay 2018, Mayotte Island has been experiencing seismo-volcanic activities that could trigger submarine landslides and, in turn, tsunamis. To address these hazards, we use the HySEA numerical model to simulate granular flow dynamics and the Boussinesq FUNWAVE-TVD numerical model to simulate wave propagation and subsequent inundations. We investigate 8 landslide scenarios (volumes from 11.25x10(6) m(3) to 800x10(6) m(3)Mayotte, Seismo-volcanic crisis, Submarine landslide, Debris-avalanches, Tsunamis, Numerical modeling, Coastal flooding hazard). The scenario posing the greatest threat involves destabilization on the eastern side ofMayotte's lagoon at a shallowdepth and can generate sea-surface deformations of up to 2 m. We show that the barrier reef surroundingMayotte plays a prominent role in controlling water-wave propagation and in protecting the island. The tsunami travel time to the coast is very short (a few minutes) and the tsunami is not necessarily preceded by a sea withdrawal. Our simulation results provide a key to establishing hazard maps and evacuation plans and improving early-warning systems.
引用
收藏
页码:361 / 390
页数:30
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