Forced and Unforced Flexural-gravity Solitary Waves

Flexural-gravity waves beneath an ice sheet are investigated. Forced waves generated by a moving load as well as freely propagating solitary waves are considered for the nonlinear problem as proposed by Plotnikov and Toland [2011]. In the unforced case, a Hamiltonian reformulation of the governing e...

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Bibliographic Details
Published in:Procedia IUTAM
Main Authors: Guyenne, P, Parau, Emilian
Format: Article in Journal/Newspaper
Language:English
Published: 2014
Subjects:
Online Access:https://ueaeprints.uea.ac.uk/id/eprint/48542/
https://ueaeprints.uea.ac.uk/id/eprint/48542/1/guyenne_ep_iutam2014.pdf
https://doi.org/10.1016/j.piutam.2014.01.047
Description
Summary:Flexural-gravity waves beneath an ice sheet are investigated. Forced waves generated by a moving load as well as freely propagating solitary waves are considered for the nonlinear problem as proposed by Plotnikov and Toland [2011]. In the unforced case, a Hamiltonian reformulation of the governing equations is presented in three dimensions. A weakly nonlinear analysis is performed to derive a cubic nonlinear Schrödinger equation near the minimum phase velocity in two dimensions. Both steady and time-dependent fully nonlinear computations are presented in the two-dimensional case, and the influence of finite depth is also discussed.