Nonlinear Dynamics of Waves Over a Nonuniformly Periodic Bottom

The numerical simulation of exact equations of motion (in conformal variables) for unsteady plane potential flows of an ideal fluid with a free surface over a strongly nonuniform bottom profile has revealed the nonlinear compression of a long wave packet undergoing Bragg reflection from a section with a smoothly increasing height of periodically located barriers. In this case, a short high packet of standing waves with sharp crests is formed and is then transformed into a backward wave. It is essential that the effect as a function of the frequency of the incident wave is insignificant in the middle of the barrier-induced spectral gap, but is maximal closer to its upper edge, when the forward wave penetrates deeply into the scattering region and forms, together with the appearing backward wave, a semblance of a Bragg soliton for some time interval.

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Publication Details

Journal
Journal of Experimental and Theoretical Physics Letters
Published
2025-10-01
DOI
https://doi.org/10.1134/s002136402560836x
Primary Topic
Ocean Waves and Remote Sensing
Type
article
Field-Weighted Citation Impact
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article

Nonlinear Dynamics of Waves Over a Nonuniformly Periodic Bottom

V. P. Ruban
Journal of Experimental and Theoretical Physics Letters
Ocean Waves and Remote Sensing
article

Nonlinear Dynamics of Waves Over a Nonuniformly Periodic Bottom

V. P. Ruban
article en

Abstract

The numerical simulation of exact equations of motion (in conformal variables) for unsteady plane potential flows of an ideal fluid with a free surface over a strongly nonuniform bottom profile has revealed the nonlinear compression of a long wave packet undergoing Bragg reflection from a section with a smoothly increasing height of periodically located barriers. In this case, a short high packet of standing waves with sharp crests is formed and is then transformed into a backward wave. It is essential that the effect as a function of the frequency of the incident wave is insignificant in the middle of the barrier-induced spectral gap, but is maximal closer to its upper edge, when the forward wave penetrates deeply into the scattering region and forms, together with the appearing backward wave, a semblance of a Bragg soliton for some time interval.

Journal of Experimental and Theoretical Physics LettersVol. 122(7)
Landau Institute for Theoretical Physics (RU)
Openalex Percentile: Top 65%
Ocean Waves and Remote Sensing
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