Abstract

In this paper, the scaling property of the inverse energy cascade and forward enstrophy cascade of the vorticity filed ω(x, y) in two-dimensional (2D) turbulence is analyzed. This is accomplished by applying a Hilbert-based technique, namely Hilbert-Huang transform, to a vorticity field obtained from a 81922 grid-points direct numerical simulation of the 2D turbulence with a forcing scale kf = 100 and an Ekman friction. The measured joint probability density function p(C, k) of mode Ci(x) of the vorticity ω and instantaneous wavenumber k(x) is separated by the forcing scale kf into two parts, which correspond to the inverse energy cascade and the forward enstrophy cascade. It is found that all conditional probability density function p(C|k) at given wavenumber k has an exponential tail. In the inverse energy cascade, the shape of p(C|k) does collapse with each other, indicating a nonintermittent cascade. The measured scaling exponent \documentclass[12pt]{minimal}\begin{document}$\zeta _{\omega }^I(q)$\end{document}ζωI(q) is linear with the statistical order q, i.e., \documentclass[12pt]{minimal}\begin{document}$\zeta _{\omega }^I(q)=-q/3$\end{document}ζωI(q)=−q/3, confirming the nonintermittent cascade process. In the forward enstrophy cascade, the core part of p(C|k) is changing with wavenumber k, indicating an intermittent forward cascade. The measured scaling exponent \documentclass[12pt]{minimal}\begin{document}$\zeta _{\omega }^F(q)$\end{document}ζωF(q) is nonlinear with q and can be described very well by a log-Poisson fitting: \documentclass[12pt]{minimal}\begin{document}$\zeta _{\omega }^F(q)=\frac{1}{3}q+0.45\left( 1-0.43^{q}\right)$\end{document}ζωF(q)=13q+0.451−0.43q. However, the extracted vorticity scaling exponents ζω(q) for both inverse energy cascade and forward enstrophy cascade are not consistent with Kraichnan's theory prediction. New theory for the vorticity field in 2D turbulence is required to interpret the observed scaling behavior.

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