One of the most striking features of rotating turbulence is the inevitable appearance of large-scale columnar structures. Whilst these structures are frequently observed, the processes by which they are created are still poorly understood. In this paper we consider the emergence of these structures from freely decaying, rotating turbulence with Ro ∼ 1. Our study follows the conjecture by Davidson, Staplehurst & Dalziel (J. Fluid Mech., vol. 557, 2006, p. 135) that the structure formation may be due to linear inertial wave propagation, which was shown to be consistent with the growth of columnar eddies in inhomogeneous turbulence. Here we extend that work and consider the case of homogeneous turbulence.We describe laboratory experiments where homogeneous turbulence is created in a rotating tank. The turbulence is generated with Ro ∼ 1, and as the energy decays, the formation of columnar vortices is observed. The axial growth of these columnar structures is then measured using two-point correlations and in all cases the results are consistent with structure formation via linear inertial wave propagation. In particular, we obtain a self-similar collapse of the two-point correlations when the axial coordinate is normalized by Ωtb, where b is a measure of the integral scale in the horizontal plane and Ω is the rotation rate. Although our results do not exclude the possibility of significant nonlinear dynamics, they are consistent with the conjecture of Davidson et al. (2006) that linear dynamics play a strong guiding hand in structure formation.
IntroductionWe consider rapidly rotating turbulence in which the fluctuating velocity, u, is small in comparison with |Ω|l, where Ω = Ωê z is the bulk rotation rate and l the integral scale of the turbulence. It is well known that such turbulence is characterized by the growth of columnar eddies aligned with the rotation axis (Hopfinger, Browand & Gagne 1982) and there has been considerable debate as to the physical mechanisms responsible for this anisotropy.Most researchers agree that inertial waves play a crucial role in the formation of these columnar vortices, which makes them quite different to, say, the coherent vortices seen in two-dimensional turbulence. Indeed, when inertia is weak by comparison with the Coriolis force, u · ∇u 2u × Ω, the motion is simply a linear superposition of inertial waves. Many theories have emerged, but typically they focus on the case of small Rossby number, Ro = u/2Ωl 1, and suggest that anisotropy results from a weak nonlinear coupling of inertial waves operating over a long period of time,