Non-Gaussianity and coherent vortex simulation for two-dimensional turbulence using an adaptive orthogonal wavelet basis

被引:225
作者
Farge, M
Schneider, K
Kevlahan, N
机构
[1] Ecole Normale Super, CNRS, Meteorol Dynam Lab, F-75231 Paris 05, France
[2] Ecole Normale Super, Ctr Math & Leurs Applicat, F-94235 Cachan, France
[3] Univ Karlsruhe, Inst Chem Tech, D-76128 Karlsruhe, Germany
[4] McMaster Univ, Dept Math & Stat, Hamilton, ON L8S 4K1, Canada
关键词
D O I
10.1063/1.870080
中图分类号
O3 [力学];
学科分类号
08 ; 0801 ;
摘要
We decompose turbulent flows into two orthogonal parts: a coherent, inhomogeneous, non-Gaussian component and an incoherent, homogeneous, Gaussian component. The two components have different probability distributions and different correlations, hence different scaling laws. This separation into coherent vortices and incoherent background flow is done for each flow realization before averaging the results and calculating the next time step. To perform this decomposition we have developed a nonlinear scheme based on an objective threshold defined in terms of the wavelet coefficients of the vorticity. Results illustrate the efficiency of this coherent vortex extraction algorithm. As an example we show that in a 256(2) computation 0.7% of the modes correspond to the coherent vortices responsible for 99.2% of the energy and 94% of the enstrophy. We also present a detailed analysis of the nonlinear term, split into coherent and incoherent components, and compare it with the classical separation, e.g., used for large eddy simulation, into large scale and small scale components, We then propose a new method, called coherent vortex simulation (CVS), designed to compute and model two-dimensional turbulent flows using the previous wavelet decomposition at each time step. This method combines both deterministic and statistical approaches: ii) Since the coherent vortices are out of statistical equilibrium, they are computed deterministically in a wavelet basis which is remapped at each time step in order to follow their nonlinear motions. (ii) Since the incoherent background flow is homogeneous and in statistical equilibrium, the classical theory of homogeneous turbulence is valid there and we model statistically the effect of the incoherent background on the coherent vortices. To illustrate the CVS method we apply it to compute a two-dimensional turbulent mixing layer. (C) 1999 American Institute of Physics. [S1070-6631(99)04608-5].
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页码:2187 / 2201
页数:15
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