Motion of Fluid Particles in the Field of a Generalized Surface Solitary Wave in a Fluid under Ice Cover

We consider a fluid layer of finite depth described by the Euler equations. The ice cover is modeled by a geometrically nonlinear elastic Kirchhoff–Love plate. The fluid particles move under the ice cover in the field of generalized solitary wave type nonlinear surface traveling waves of small but finite amplitude. The equations of the model admit a solution describing such surface waves. Generalized solitary waves are solitary waves up to terms that are exponentially small in amplitude; therefore, for approximations of algebraic order in amplitude, the trajectories of particles are determined by the surface solitary wave. In the analysis we use explicit asymptotic expressions for solutions describing wave structures at the water–ice interface, such as a generalized solitary wave, as well as asymptotic solutions for the velocity field generated by these waves in the bulk of the fluid.

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Publication Details

Journal
Proceedings of the Steklov Institute of Mathematics
Published
2024-12-01
DOI
https://doi.org/10.1134/s0081543824060099
Primary Topic
Arctic and Antarctic ice dynamics
Type
article
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article

Motion of Fluid Particles in the Field of a Generalized Surface Solitary Wave in a Fluid under Ice Cover

A. T. Il’íchev, A. S. Savin
Proceedings of the Steklov Institute of Mathematics
Arctic and Antarctic ice dynamics
article

Motion of Fluid Particles in the Field of a Generalized Surface Solitary Wave in a Fluid under Ice Cover

A. T. Il’íchev, A. S. Savin
article en

Abstract

We consider a fluid layer of finite depth described by the Euler equations. The ice cover is modeled by a geometrically nonlinear elastic Kirchhoff–Love plate. The fluid particles move under the ice cover in the field of generalized solitary wave type nonlinear surface traveling waves of small but finite amplitude. The equations of the model admit a solution describing such surface waves. Generalized solitary waves are solitary waves up to terms that are exponentially small in amplitude; therefore, for approximations of algebraic order in amplitude, the trajectories of particles are determined by the surface solitary wave. In the analysis we use explicit asymptotic expressions for solutions describing wave structures at the water–ice interface, such as a generalized solitary wave, as well as asymptotic solutions for the velocity field generated by these waves in the bulk of the fluid.

Proceedings of the Steklov Institute of MathematicsVol. 327(1)
Russian Academy of Sciences (RU), Bauman Moscow State Technical University (RU), Steklov Mathematical Institute (RU), V.I. Vernadsky Institute of Geochemistry and Analytical Chemistry (RU)
Life below water
Openalex Percentile: Top 71%
Arctic and Antarctic ice dynamics
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Motion of Fluid Particles in the Field of a Generalized Surface Solitary Wave in a Fluid under Ice Cover — A. T. Il’íchev, A. S. Savin · Proceedings of the Steklov Institute of Mathematics (2024) | TGRS Research Map | TGRS