Shallow water waves generated by subaerial solid landslides

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Abstract

Subaerial landslides are common events, which may generate very large water waves. The numerical modelling and simulation of these events are thus of primary interest for forecasting and mitigation of tsunami disasters. In this paper, we aim at describing these extreme events using a simplified shallow water model to derive relevant scaling laws. To cope with the problem, two different numerical codes are employed: one, SPHysics, is based on a Lagrangian meshless approach to accurately describe the impact stage whereas the other, Gerris, based on a two-phase finite-volume method is used to study the propagation of the wave. To validate Gerris for this very particular problem, two numerical cases of the literature are reproduced: a vertical sinking box and a 2-D wedge sliding down a slope. Then, to get insights into the problem of subaerial landslide-generated tsunamis and to further validate the codes for this case of landslides, a series of experiments is conducted in a water wave tank and successfully compared with the results of both codes. Based on a simplified approach, we derive different scaling laws in excellent agreement with the experiments and numerical simulations. ©The Authors 2013. Published by Oxford University Press on behalf of The Royal Astronomical Society.

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Viroulet, S., Cébron, D., Kimmoun, O., & Kharif, C. (2013). Shallow water waves generated by subaerial solid landslides. Geophysical Journal International, 193(2), 747–762. https://doi.org/10.1093/gji/ggs133

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