Kraichnan-Leith-Batchelor similarity theory and two-dimensional inverse cascades

摘要

We study the scaling properties and Kraichnan-Leith-Batchelor (KLB) theory of forced inverse cascades in generalized two-dimensional (2D) fluids ($lpha$-turbulence models) simulated at resolution $8192^2$. We consider $lpha=1$ (surface quasigeostrophic flow), $lpha=2$ (2D vorticity dynamics) and $lpha=3$. The forcing scale is well-resolved, a direct cascade is present and there is no large-scale dissipation. Coherent vortices spanning a range of sizes, most larger than the forcing scale, are present for both $lpha=1$ and $lpha=2$. The active scalar field for $lpha=3$ contains comparatively few and small vortices. The energy spectral slopes in the inverse cascade are steeper than the KLB prediction $-(7-lpha)/3$ in all three systems. Since we stop the simulations well before the cascades have reached the domain scale, vortex formation and spectral steepening are not due to condensation effects; nor are they caused by large-scale dissipation, which is absent. One- and two-point pdfs, hyperflatness factors and structure functions indicate that the inverse cascades are intermittent and non-Gaussian over much of the inertial range for $lpha=1$ and $lpha=2$, while the $lpha=3$ inverse cascade is much closer to Gaussian and non-intermittent. For $lpha=3$ the steep spectrum is close to that associated with enstrophy equipartition. Continuous wavelet analysis shows approximate KLB scaling $mathcal{E}(k) propto k^{-2}$ ($lpha=1$) and $mathcal{E}(k) propto k^{-5/3}$ ($lpha=2$) in the interstitial regions between the coherent vortices. Our results demonstrate that coherent vortex formation ($lpha=1$ and $lpha=2$) and non-realizability ($lpha=3$) cause 2D inverse cascades to deviate from the KLB predictions, but that the flow between the vortices exhibits KLB scaling and non-intermittent statistics for $lpha=1$ and $lpha=2$. The results will appear in cite{BurgessEA2015}, which has been accepted to the emph{Journal of Fluid Mechanics}.