Sound signals of tsunamis from a slender fault

DOI10.1017/jfm.2017.811zbMath1419.76579OpenAlexW2771657489MaRDI QIDQ5226210

Chiang C. Mei, Usama Kadri

Publication date: 31 July 2019

Published in: Journal of Fluid Mechanics (Search for Journal in Brave)

Full work available at URL: https://doi.org/10.1017/jfm.2017.811

zbMATH Keywords

acousticscoastal engineeringhydrodynamic noise

Mathematics Subject Classification ID

Hydrology, hydrography, oceanography (86A05) Hydro- and aero-acoustics (76Q05)

Related Items (6)

Time-domain wave response of a compressible ocean due to an arbitrary ocean bottom motion ⋮ Acoustic-gravity waves generated by surface disturbances ⋮ Electromagnetic field generated by tsunamigenic seabed deformation ⋮ Effects of the sound speed vertical profile on the evolution of hydroacoustic waves ⋮ Acoustic–gravity waves from multi-fault rupture ⋮ On the propagation of acoustic–gravity waves due to a slender rupture in an elastic seabed

Cites Work

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• Tsunamis and acoustic-gravity waves from underwater earthquakes
• Progressive waves in a compressible-Ocean with an elastic bottom
• On resonant triad interactions of acoustic–gravity waves
• Generation of an acoustic-gravity wave by two gravity waves, and their subsequent mutual interaction
• Asymptotic Expansions of Fourier Integrals Involving Logarithmic Singularities
• Depth-integrated equation for large-scale modelling of low-frequency hydroacoustic waves
• The effect of a sudden change of shape of the bottom of a slightly compressible ocean

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