Physical Mechanism of the Two-Dimensional Inverse Energy Cascade

Shiyi Chen, Robert E. Ecke, Gregory L. Eyink, Michael Rivera, Minping Wan, and Zuoli Xiao
Phys. Rev. Lett. 96, 084502 – Published 28 February 2006

Abstract

We study the physical mechanisms of the two-dimensional inverse energy cascade using theory, numerics, and experiment. Kraichnan’s prediction of a 5/3 spectrum with constant, negative energy flux is verified in our simulations of 2D Navier-Stokes equations. We observe a similar but shorter range of inverse cascade in laboratory experiments. Our theory predicts, and the data confirm, that inverse cascade results mainly from turbulent stress proportional to small-scale strain rotated by 45°. This “skew-Newtonian” stress is explained by the elongation and thinning of small-scale vortices by large-scale strain which weakens their velocity and transfers their energy upscale.

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  • Received 6 October 2005

DOI:https://doi.org/10.1103/PhysRevLett.96.084502

©2006 American Physical Society

Authors & Affiliations

Shiyi Chen1,2,3,5, Robert E. Ecke3,4, Gregory L. Eyink1,2,3, Michael Rivera4, Minping Wan1, and Zuoli Xiao1

  • 1Department of Mechanical Engineering, The Johns Hopkins University, Baltimore, Maryland 21218, USA
  • 2Applied Mathematics & Statistics, The Johns Hopkins University, Baltimore, Maryland 21218, USA
  • 3Center for Nonlinear Studies and Theoretical Division, Los Alamos National Laboratory, Los Alamos, New Mexico 87545, USA
  • 4Materials Science & Technology Division, Los Alamos National Laboratory, Los Alamos, New Mexico 87545, USA
  • 5College of Engineering, 60 Yan-Nan Yuan, Peking University, P.O. Box 100871, Beijing, China

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Issue

Vol. 96, Iss. 8 — 3 March 2006

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