Hostname: page-component-848d4c4894-hfldf Total loading time: 0 Render date: 2024-05-09T02:04:50.814Z Has data issue: false hasContentIssue false
  • English
  • Français

Onset of secondary instabilities on the zigzag instability in stratified fluids

Published online by Cambridge University Press:  29 June 2011

PIERRE AUGIER  and
PAUL BILLANT
PIERRE AUGIER*
Affiliation:
LadHyX, CNRS, Ecole Polytechnique, 91128 Palaiseau Cedex, France
PAUL BILLANT
Affiliation:
LadHyX, CNRS, Ecole Polytechnique, 91128 Palaiseau Cedex, France
*
†Email address for correspondence: pierre.augier@ladhyx.polytechnique.fr
Get access Rights & Permissions [Opens in a new window]

Abstract

Recently, Deloncle, Billant & Chomaz (J. Fluid Mech., vol. 599, 2008, p. 229) and Waite & Smolarkiewicz (J. Fluid Mech., vol. 606, 2008, p. 239) have performed numerical simulations of the nonlinear evolution of the zigzag instability of a pair of counter-rotating vertical vortices in a stratified fluid. Both studies report the development of a small-scale secondary instability when the vortices are strongly bent if the Reynolds number Re is sufficiently high. However, the two papers are at variance about the nature of this secondary instability: it is a shear instability according to Deloncle et al. (J. Fluid Mech., vol. 599, 2008, p. 229) and a gravitational instability according to Waite & Smolarkiewicz (J. Fluid Mech., vol. 606, 2008, p. 239). They also profoundly disagree about the condition for the onset of the secondary instability: ReF2h > O(1) according to the former or ReFh > 80 according to the latter, where Fh is the horizontal Froude number. In order to understand the origin of these discrepancies, we have carried out direct numerical simulations of the zigzag instability of a Lamb–Chaplygin vortex pair for a wide range of Reynolds and Froude numbers. The threshold for the onset of a secondary instability is found to be ReF2h ≃ 4 for Re ≳ 3000 and ReFh = 80 for Re ≲ 1000 in agreement with both previous studies. We show that the scaling analysis of Deloncle et al. (J. Fluid Mech., vol. 599, 2008, p. 229) can be refined to obtain a universal threshold: (Re − Re0)F2h ≃ 4, with Re0 ≃ 400, which works for all Re. Two different regimes for the secondary instabilities are observed: when (Re − Re0)F2h ≃ 4, only the shear instability develops while when (Re − Re0)F2h ≫ 4, both shear and gravitational instabilities appear almost simultaneously in distinct regions of the vortices. However, the shear instability seems to play a dominant role in the breakdown into small scales in the range of parameters investigated.

JFM classification

Geophysical and Geological Flows: Stratified flows Instability: Transition to turbulence Vortex Flows: Vortex instability
Type
Papers
Information
Journal of Fluid Mechanics , Volume 682 , 10 September 2011 , pp. 120 - 131
Copyright
Copyright © Cambridge University Press 2011

Access options

Get access to the full version of this content by using one of the access options below. (Log in options will check for institutional or personal access. Content may require purchase if you do not have access.)

References

REFERENCES

Billant, P. 2010 Zigzag instability of vortex pairs in stratified and rotating fluids. Part 1. General stability equations. J. Fluid Mech. 660, 354–395.CrossRefGoogle Scholar
Billant, P. & Chomaz, J.-M. 2000 a Experimental evidence for a new instability of a vertical columnar vortex pair in a strongly stratified fluid. J. Fluid Mech. 418, 167–188.CrossRefGoogle Scholar
Billant, P. & Chomaz, J.-M. 2000 b Three-dimensional stability of a vertical columnar vortex pair in a stratified fluid. J. Fluid Mech. 419, 65–91.CrossRefGoogle Scholar
Billant, P., Deloncle, A., Chomaz, J.-M. & Otheguy, P. 2010 Zigzag instability of vortex pairs in stratified and rotating fluids. Part 2. Analytical and numerical analyses. J. Fluid Mech. 660, 396–429.CrossRefGoogle Scholar
Deloncle, A., Billant, P. & Chomaz, J.-M. 2008 Nonlinear evolution of the zigzag instability in stratified fluids: a shortcut on the route to dissipation. J. Fluid Mech. 599, 229–238.CrossRefGoogle Scholar
Deloncle, A., Billant, P. & Chomaz, J.-M. 2011 Three-dimensional stability of vortex arrays in a stratified and rotating fluid. J. Fluid Mech. 678, 482–510.CrossRefGoogle Scholar
Fritts, D. C. & Alexander, M. J. 2003 Gravity wave dynamics and effects in the middle atmosphere. Rev. Geophys. 41 (1), 1003.CrossRefGoogle Scholar
Howard, L. N. 1961 Note on a paper of John W. Miles. J. Fluid Mech. 10, 509–512.CrossRefGoogle Scholar
Lelong, M. P. & Dunkerton, T. J. 1998 Inertia-gravity wave breaking in three dimensions. Part II: Convectively unstable waves. J. Atmos. Sci. 55 (15), 2489–2501.2.0.CO;2>CrossRefGoogle Scholar
Miles, J. W. 1961 On the stability of heterogeneous shear flows. J. Fluid Mech. 10, 496–508.CrossRefGoogle Scholar
Otheguy, P., Billant, P. & Chomaz, J.-M. 2007 Theoretical analysis of the zigzag instability of a vertical co-rotating vortex pair in a strongly stratified fluid. J. Fluid Mech. 584, 103–123.CrossRefGoogle Scholar
Otheguy, P., Chomaz, J.-M. & Billant, P. 2006 Elliptic and zigzag instabilities on co-rotating vertical vortices in a stratified fluid. J. Fluid Mech. 553, 253–272.CrossRefGoogle Scholar
Riley, J. J. & Lelong, M.-P. 2000 Fluid motions in the presence of strong stable stratification. Annu. Rev. Fluid Mech. 32, 613–657.CrossRefGoogle Scholar
Waite, M. L. 2011 Stratified turbulence at the buoyancy scale. Phys. Fluids (In press).CrossRefGoogle Scholar
Waite, M. L. & Smolarkiewicz, P. K. 2008 Instability and breakdown of a vertical vortex pair in a strongly stratified fluid. J. Fluid Mech. 606, 239–273.CrossRefGoogle Scholar

Augier and Billant supplementary movie

Movie 1. Time evolution of the total density in the vertical cross-sections yz and xz indicated in blue and red, respectively, in figure 1 for Fh = 0.1, Re = 2500. The colour contours indicate the Richardson number where Ri<1/4. The red vertical lines indicate the location of the xz cross-sections. Conversely, the blue vertical lines indicate the location of the yz cross-sections

Download Augier and Billant supplementary movie(Video)
Video 9 MB

Augier and Billant supplementary movie

Movie 1. Time evolution of the total density in the vertical cross-sections yz and xz indicated in blue and red, respectively, in figure 1 for Fh = 0.1, Re = 2500. The colour contours indicate the Richardson number where Ri<1/4. The red vertical lines indicate the location of the xz cross-sections. Conversely, the blue vertical lines indicate the location of the yz cross-sections

Download Augier and Billant supplementary movie(Video)
Video 25.4 MB

Augier and Billant supplementary movie

Movie 2. Time evolution of the total density in the vertical cross-sections yz and xz indicated in blue and red, respectively, in figure 1 for Fh = 0.1, Re = 1000. The colour contours indicate the Richardson number where Ri<1/4. The red vertical lines indicate the location of the xz cross-sections. Conversely, the blue vertical lines indicate the location of the yz cross-sections

Download Augier and Billant supplementary movie(Video)
Video 8.8 MB

Augier and Billant supplementary movie

Movie 2. Time evolution of the total density in the vertical cross-sections yz and xz indicated in blue and red, respectively, in figure 1 for Fh = 0.1, Re = 1000. The colour contours indicate the Richardson number where Ri<1/4. The red vertical lines indicate the location of the xz cross-sections. Conversely, the blue vertical lines indicate the location of the yz cross-sections

Download Augier and Billant supplementary movie(Video)
Video 17.9 MB