Instabilities in internal gravity waves

Internal gravity waves are propagating disturbances in stably stratified fluids, and can transport momentum and energy over large spatial extents. From a fundamental viewpoint, internal waves are interesting due to the nature of their dispersion relation, and their linear dynamics are reasonably wel...

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Main Authors: Dheeraj Varma, Manikandan Mathur, Thierry Dauxois
Format: Article
Language:English
Published: AIMS Press 2023-03-01
Series:Mathematics in Engineering
Subjects:
Online Access:https://www.aimspress.com/article/doi/10.3934/mine.2023016?viewType=HTML
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author Dheeraj Varma
Manikandan Mathur
Thierry Dauxois
author_facet Dheeraj Varma
Manikandan Mathur
Thierry Dauxois
author_sort Dheeraj Varma
collection DOAJ
description Internal gravity waves are propagating disturbances in stably stratified fluids, and can transport momentum and energy over large spatial extents. From a fundamental viewpoint, internal waves are interesting due to the nature of their dispersion relation, and their linear dynamics are reasonably well-understood. From an oceanographic viewpoint, a qualitative and quantitative understanding of significant internal wave generation in the ocean is emerging, while their dissipation mechanisms are being debated. This paper reviews the current knowledge on instabilities in internal gravity waves, primarily focusing on the growth of small-amplitude disturbances. Historically, wave-wave interactions based on weakly nonlinear expansions have driven progress in this field, to investigate spontaneous energy transfer to various temporal and spatial scales. Recent advances in numerical/experimental modeling and field observations have further revealed noticeable differences between various internal wave spatial forms in terms of their instability characteristics; this in turn has motivated theoretical calculations on appropriately chosen internal wave fields in various settings. After a brief introduction, we present a pedagogical discussion on linear internal waves and their different two-dimensional spatial forms. The general ideas concerning triadic resonance in internal waves are then introduced, before proceeding towards instability characteristics of plane waves, wave beams and modes. Results from various theoretical, experimental and numerical studies are summarized to provide an overall picture of the gaps in our understanding. An ocean perspective is then given, both in terms of the relevant outstanding questions and the various additional factors at play. While the applications in this review are focused on the ocean, several ideas are relevant to atmospheric and astrophysical systems too.
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spelling doaj.art-045cf0aebeb94c2a8b19b8beaac7c0bd2023-05-17T01:32:06ZengAIMS PressMathematics in Engineering2640-35012023-03-015113410.3934/mine.2023016Instabilities in internal gravity wavesDheeraj Varma0Manikandan Mathur 1Thierry Dauxois 21. ENS de Lyon, CNRS, Laboratoire de Physique, F-69342 Lyon, France2. Department of Aerospace Engineering, Indian Institute of Technology Madras, Chennai-600036, India 3. Geophysical Flows Lab, Indian Institute of Technology Madras, Chennai-600036, India1. ENS de Lyon, CNRS, Laboratoire de Physique, F-69342 Lyon, France 2. Department of Aerospace Engineering, Indian Institute of Technology Madras, Chennai-600036, IndiaInternal gravity waves are propagating disturbances in stably stratified fluids, and can transport momentum and energy over large spatial extents. From a fundamental viewpoint, internal waves are interesting due to the nature of their dispersion relation, and their linear dynamics are reasonably well-understood. From an oceanographic viewpoint, a qualitative and quantitative understanding of significant internal wave generation in the ocean is emerging, while their dissipation mechanisms are being debated. This paper reviews the current knowledge on instabilities in internal gravity waves, primarily focusing on the growth of small-amplitude disturbances. Historically, wave-wave interactions based on weakly nonlinear expansions have driven progress in this field, to investigate spontaneous energy transfer to various temporal and spatial scales. Recent advances in numerical/experimental modeling and field observations have further revealed noticeable differences between various internal wave spatial forms in terms of their instability characteristics; this in turn has motivated theoretical calculations on appropriately chosen internal wave fields in various settings. After a brief introduction, we present a pedagogical discussion on linear internal waves and their different two-dimensional spatial forms. The general ideas concerning triadic resonance in internal waves are then introduced, before proceeding towards instability characteristics of plane waves, wave beams and modes. Results from various theoretical, experimental and numerical studies are summarized to provide an overall picture of the gaps in our understanding. An ocean perspective is then given, both in terms of the relevant outstanding questions and the various additional factors at play. While the applications in this review are focused on the ocean, several ideas are relevant to atmospheric and astrophysical systems too.https://www.aimspress.com/article/doi/10.3934/mine.2023016?viewType=HTMLtriadic resonancesubharmonicsuperharmonicplane wavewave beammode
spellingShingle Dheeraj Varma
Manikandan Mathur
Thierry Dauxois
Instabilities in internal gravity waves
Mathematics in Engineering
triadic resonance
subharmonic
superharmonic
plane wave
wave beam
mode
title Instabilities in internal gravity waves
title_full Instabilities in internal gravity waves
title_fullStr Instabilities in internal gravity waves
title_full_unstemmed Instabilities in internal gravity waves
title_short Instabilities in internal gravity waves
title_sort instabilities in internal gravity waves
topic triadic resonance
subharmonic
superharmonic
plane wave
wave beam
mode
url https://www.aimspress.com/article/doi/10.3934/mine.2023016?viewType=HTML
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AT manikandanmathur instabilitiesininternalgravitywaves
AT thierrydauxois instabilitiesininternalgravitywaves