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Hydroelastic solitary waves in deep water

Milewski, P; Vanden-Broeck, J-M; Wang, Z; (2011) Hydroelastic solitary waves in deep water. Journal of Fluid Mechanics , 679 628 - 640. 10.1017/jfm.2011.163. Green open access

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Abstract

The problem of waves propagating on the surface of a two-dimensional ideal fluid of infinite depth bounded above by an elastic sheet is studied with asymptotic and numerical methods. We use a nonlinear elastic model that has been used to describe the dynamics of ice sheets. Particular attention is paid to forced and unforced dynamics of waves having near-minimum phase speed. For the unforced problem, we find that wavepacket solitary waves bifurcate from nonlinear periodic waves of minimum speed. When the problem is forced by a moving load, we find that, for small-amplitude forcing, steady responses are possible at all subcritical speeds, but for larger loads there is a transcritical range of forcing speeds for which there are no steady solutions. In unsteady computations, we find that if the problem is forced at a speed in this range, very large unsteady responses are obtained, and that when the forcing is released, a solitary wave is generated. These solitary waves appear stable, and can coexist within a sea of small-amplitude waves.

Type: Article
Title: Hydroelastic solitary waves in deep water
Open access status: An open access version is available from UCL Discovery
DOI: 10.1017/jfm.2011.163
Publisher version: http://dx.doi.org/10.1017/jfm.2011.163
Language: English
Additional information: © 2011 Cambridge University Press
UCL classification: UCL
UCL > Provost and Vice Provost Offices > UCL BEAMS
UCL > Provost and Vice Provost Offices > UCL BEAMS > Faculty of Maths and Physical Sciences
UCL > Provost and Vice Provost Offices > UCL BEAMS > Faculty of Maths and Physical Sciences > Dept of Mathematics
URI: https://discovery.ucl.ac.uk/id/eprint/1324413
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