Steady Internal Waves in Deep Stratified Flows


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Abstract

A long-wave approximation that describes travelling solitary waves within the framework of the model of a weakly stratified two-layer fluid is considered. It is demonstrated that wave regimes occur near the boundary of the parametric domain of shear instability in the stratified flow. This property offers an explanation for the mechanism of intense mixing in deep bottom layers.

About the authors

N. I. Makarenko

Lavrentyev Institute of Hydrodynamics, Siberian Branch; Novosibirsk National Research State University

Author for correspondence.
Email: makarenko@hydro.nsc.ru
Russian Federation, Novosibirsk, 630090; Novosibirsk, 630090

J. L. Maltseva

Lavrentyev Institute of Hydrodynamics, Siberian Branch; Novosibirsk National Research State University

Author for correspondence.
Email: maltseva@hydro.nsc.ru
Russian Federation, Novosibirsk, 630090; Novosibirsk, 630090

E. G. Morozov

Shirshov Institute of Oceanology, Russian Academy of Sciences

Author for correspondence.
Email: egmorozov@mail.ru
Russian Federation, Moscow, 117997

R. Yu. Tarakanov

Shirshov Institute of Oceanology, Russian Academy of Sciences

Author for correspondence.
Email: rtarakanov@gmail.com
Russian Federation, Moscow, 117997

K. A. Ivanova

Institute of Mathematics

Author for correspondence.
Email: ivanova.kseniya15@gmail.com
Switzerland, Zurich


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