Experimental evidence for a new instability of a vertical columnar vortex pair in a strongly stratified fluid
By P. Billant, Jean-Marc Chomaz. Journal of Fluid Mechanics, 2000
199 citations recorded by the source corpus.
Subfields: Atmospheric Science, Computational Mechanics, Oceanography
View Paper: https://www.semanticscholar.org/paper/c9223698f44bc2735b00fbf123e0f18564471197
How researchers see this paper
The researchers whose trusted networks rank it highest, strongest advocate first. Every researcher gets a different order.
In Atmospheric Science
- E. Lindborg
- Geert Brethouwer
- P. Billant
- Jean-Marc Chomaz
- Michael L. Waite
- P. Bartello
- Larry Mahrt
- Luca Biferale
In Computational Mechanics
- E. Lindborg
- Geert Brethouwer
- P. Billant
- Jean-Marc Chomaz
- P. Bartello
- Michael L. Waite
- A. Alexakis
- T. Leweke
In Oceanography
- E. Lindborg
- Michael L. Waite
- P. Bartello
- Geert Brethouwer
- Larry Mahrt
- P. Billant
- Jean-Marc Chomaz
- Luca Biferale
Citations in the corpus
- Dynamics and Instabilities of Vortex Pairs (2016, background): “Vertical Pairs Counter- and corotating vertical pairs in strong stratification exhibit a Crow-type zigzag instability, involving antisymmetric and symmetric displacements, respectively (Williamson & Chomaz 1997, Billant & Chomaz 2000, Otheguy et al. 2006).”
- Stably Stratified Atmospheric Boundary Layers (2014, background): “Laboratory and numerically simulated two-dimensional modes can be characterized by significant vertical coherence, such as columnar vortices (Billant & Chomaz 2000) that are vulnerable to breakdown through instability.”
- Scaling analysis and simulation of strongly stratified turbulent flows (2007, background): “This ensures that the large-scale, purely two-dimensional vortices induced by the forcing can become unstable through a mechanism such as the zigzag instability ( Billant & Chomaz 2000a ) leading to the spontaneous development of layers.”
- Cascades and transitions in turbulent flows (2018, background): “This transition can be understood by noting that stratified turbulence leads to the formation of layers of width `z ' in`in/N [297, 319].”
- Stratified turbulence dominated by vortical motion (2004, background): “Thoroddsen & Atta 1992; Fincham, Maxworthy & Spedding 1996; Billant & Chomaz 2000 ).”