Dynamics of turbulence in the field of nonlinear internal waves

Abstract A modification of the semi-empirical theory of stratified turbulent flow, which includes an equation for the density fluctuations (the potential energy of turbulence), is applied to describe the effect of internal gravity waves (IWs) on the small-scale turbulence. After considering the periodic IWs, special attention is paid to the action of internal solitons, such as the classical Gardner solitons and a strongly nonlinear solitary wave regularly observed in the Oregon Bay of the USA. It is confirmed that the presence of potential energy allows the existence of finite turbulence at any Richardson number.

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Publication Details

Journal
Journal of Nonlinear Waves
Published
2025-01-01
DOI
https://doi.org/10.1017/jnw.2025.10017
Primary Topic
Oceanographic and Atmospheric Processes
Type
article
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article

Dynamics of turbulence in the field of nonlinear internal waves

I. A. Soustova, Lev A. Ostrovsky, Alexandra Kuznetsova
Journal of Nonlinear Waves
Oceanographic and Atmospheric Processes
article

Dynamics of turbulence in the field of nonlinear internal waves

I. A. Soustova, Lev A. Ostrovsky, Alexandra Kuznetsova
article en

Abstract

Abstract A modification of the semi-empirical theory of stratified turbulent flow, which includes an equation for the density fluctuations (the potential energy of turbulence), is applied to describe the effect of internal gravity waves (IWs) on the small-scale turbulence. After considering the periodic IWs, special attention is paid to the action of internal solitons, such as the classical Gardner solitons and a strongly nonlinear solitary wave regularly observed in the Oregon Bay of the USA. It is confirmed that the presence of potential energy allows the existence of finite turbulence at any Richardson number.

Journal of Nonlinear WavesVol. 1
National Research University Higher School of Economics (RU), University of Colorado System (US), Prokhorov General Physics Institute (RU)
Openalex Percentile: Top 71%
Oceanographic and Atmospheric Processes
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