Development of the wave motion induced by near-bottom periodic disturbances in a two-layer shear current

The behavior of wave motion arising in an ideal incompressible homogeneous fluid under switching-on periodic bottom disturbances is studied in the linear approximation for the two-dimensional non-stationary problem. In the undisturbed state, the velocities of two-layer fluid flow are linear functions of the vertical coordinate in each of the layers with different gradients and coincide on the boundary of the layers. The upper boundary of fluid can be either free or bounded by the rigid cover. The dispersion dependences and the group velocities of the appearing wave modes are determined. The vertical displacements of the free surface and the interface between the layers are calculated. A comparison with the solution for a single-layer fluid is carried out.

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Journal
Известия Российской академии наук Механика жидкости и газа
Published
2024-10-19
DOI
https://doi.org/10.31857/s1024708424020069
Primary Topic
Ocean Waves and Remote Sensing
Type
article
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article

Development of the wave motion induced by near-bottom periodic disturbances in a two-layer shear current

И. В. Стурова
Известия Российской академии наук Механика жидкости и газа
Ocean Waves and Remote Sensing
article

Development of the wave motion induced by near-bottom periodic disturbances in a two-layer shear current

И. В. Стурова
article en

Abstract

The behavior of wave motion arising in an ideal incompressible homogeneous fluid under switching-on periodic bottom disturbances is studied in the linear approximation for the two-dimensional non-stationary problem. In the undisturbed state, the velocities of two-layer fluid flow are linear functions of the vertical coordinate in each of the layers with different gradients and coincide on the boundary of the layers. The upper boundary of fluid can be either free or bounded by the rigid cover. The dispersion dependences and the group velocities of the appearing wave modes are determined. The vertical displacements of the free surface and the interface between the layers are calculated. A comparison with the solution for a single-layer fluid is carried out.

Известия Российской академии наук Механика жидкости и газа(2)
Lavrentyev Institute of Hydrodynamics (RU)
Openalex Percentile: Top 81%
Ocean Waves and Remote Sensing
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