Internal gravity waves in stratified flows with and without vortical modes

Vincent Labarre, Pierre Augier, Giorgio Krstulovic, and Sergey Nazarenko
Phys. Rev. Fluids 9, 024604 – Published 20 February 2024

Abstract

The comprehension of stratified flows is important for geophysical and astrophysical applications. The weak wave turbulence theory aims to provide a statistical description of internal gravity waves propagating in the bulk of such flows. However, internal gravity waves are usually perturbed by other structures present in stratified flow, namely the shear modes and the vortical modes. In order to check whether a weak internal gravity wave turbulence regime can occur, we perform direct numerical simulations of stratified turbulence without shear modes and with or without vortical modes at various Froude and buoyancy Reynolds numbers. We observe that removing vortical modes naturally helps to have a better overall balance between poloidal kinetic energy, involved in internal gravity waves, and potential energy. However, conversion between kinetic energy and potential energy does not necessarily show fluctuations around zero in our simulations, as we would expect for a system of weak waves. A spatiotemporal analysis reveals that removing vortical modes helps to concentrate the energy around the wave frequency, but it is not enough to observe a weak wave turbulence regime. Yet we observe that internal gravity waves whose frequency are large compared to the eddy turnover time are present, and we also find evidences for slow internal gravity waves interacting by triadic resonance instabilities in our strongly stratified flows simulations. Finally, we propose conditions that should be fulfilled in order to observe a weak internal gravity wave turbulence regime in real flows.

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  • Received 12 June 2023
  • Accepted 4 January 2024

DOI:https://doi.org/10.1103/PhysRevFluids.9.024604

©2024 American Physical Society

Physics Subject Headings (PhySH)

Fluid Dynamics

Authors & Affiliations

Vincent Labarre1,*, Pierre Augier2,†, Giorgio Krstulovic1,‡, and Sergey Nazarenko3,§

  • 1Université Côte d'Azur, Observatoire de la Côte d'Azur, CNRS, Laboratoire Lagrange, Boulevard de l'Observatoire, CS 34229-F 06304 Nice Cedex 4, France
  • 2Laboratoire des Ecoulements Géophysiques et Industriels, Université Grenoble Alpes, CNRS, Grenoble-INP, F-38000 Grenoble, France
  • 3Université Côte d'Azur, CNRS, Institut de Physique de Nice (INPHYNI), 17 rue Julien Lauprêtre 06200 Nice, France

  • *vincent.labarre@oca.eu
  • pierre.augier@univ-grenoble-alpes.fr
  • giorgio.krstulovic@oca.eu
  • §sergey.nazarenko@unice.fr

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Issue

Vol. 9, Iss. 2 — February 2024

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