Short-wave cooperative instabilities in representative aircraft vortices

David Fabre, Laurent Jacquin

Research output: Contribution to journalArticlepeer-review

Abstract

This paper considers the short-wave cooperative instabilities in a family of vortices representative of aircraft wakes. These vortices are characterized by two core scales, an internal core scale a1 and an external core scale a2, and their azimuthal velocity follows a power law V(r)∼r and the intermediate zone (a1<r<a2). The results are compared to the cases of the Rankine (constant) and Lamb-Oseen (Gaussian) vortices, and to the elliptic instability theory. The unstable wavelengths and the structure of the unstable modes are characterized as functions of the base flow parameters α and a2/a1. For 0.5≤α≤1, the wavelength of the instability is of the order of the internal scale a1 and the unstable modes only affect the internal core. In this case the growth rate of the instability is in accordance with the predictions of the elliptical instability theory and is a growing function of the parameter a2/a1 . For 0≤α<0.4, the wavelength of the instability is of the order of the external scale a2 and the unstable modes extend into the intermediate zone. In this case the growth rate of the instability differs from the predictions of the elliptical instability theory and is independent upon the parameter a2/a1- Interestingly, a sharp transition between these two regimes occurs for 0.4<α<0.5, in a range of parameters corresponding to experimentally measured trailing wakes. In this range, the bands of wave numbers affected by the instability are particularly large and may coalesce into a broadband spectrum.

Original languageEnglish
Pages (from-to)1366-1378
Number of pages13
JournalPhysics of Fluids
Volume16
Issue number5
DOIs
Publication statusPublished - 1 Jan 2004
Externally publishedYes

Fingerprint

Dive into the research topics of 'Short-wave cooperative instabilities in representative aircraft vortices'. Together they form a unique fingerprint.

Cite this