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The Effect of Subfilter-Scale Physics on Regularization Models

机译:子滤波器规模物理对正则化模型的影响

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摘要

The subfilter-scale (SFS) physics of regularization models are investigated to understand the regularizations' performance as SFS models. Suppression of spectrally local SFS interactions and conservation of small-scale circulation in the Lagrangian-averaged Navier-Stokes a-model (LANS-a) is found to lead to the formation of rigid bodies. These contaminate the superfilter-scale energy spectrum with a scaling that approaches k~+1 as the SFS spectra is resolved. The Clark-α and Leray-α models, truncations of LANS-a, do not conserve small-scale circulation and do not develop rigid bodies. LANS-a, however, is closest to Navier-Stokes in intermittency properties. All three models are found to be stable at high Reynolds number. Differences between L2 and H-1 norm models are clarified. For magnetohydrodynamics (MHD), the presence of the Lorentz force as a source (or sink) for circulation and as a facilitator of both spectrally nonlocal large to small scale interactions as well as local SFS interactions prevents the formation of rigid bodies in Lagrangian-averaged MHD (LAMHD-α). LAMHD-α performs well as a predictor of superfilter-scale energy spectra and of intermittent current sheets at high Reynolds numbers. It may prove generally applicable as a MHD-LES.
机译:研究了正则化模型的子过滤器规模(SFS)物理原理,以了解正则化作为SFS模型的性能。发现在拉格朗日平均Navier-Stokes a模型(LANS-a)中,频谱局部SFS相互作用的抑制和小规模环流的守恒导致了刚体的形成。随着SFS光谱的解析,这些污染以接近k〜+ 1的比例污染了超滤器级能谱。 Clarks-α和Leray-α模型是LANS-a的截断,不保留小规模的循环,也不形成刚体。然而,LANS-a在间歇性方面最接近Navier-Stokes。发现所有三个模型在高雷诺数下都是稳定的。阐明了L2和H-1规范模型之间的差异。对于磁流体动力学(MHD),洛伦兹力作为循环的源(或汇)并作为频谱非局部大到小规模相互作用以及局部SFS相互作用的促进剂的存在,阻止了拉格朗日平均中刚体的形成MHD(LAMHD-α)。在高雷诺数下,LAMHD-α可以很好地预测超滤器级能谱和间歇电流表。它可能被证明普遍适用于MHD-LES。

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  • 来源
    《Journal of Scientific Computing》 |2011年第1期|p.21-34|共14页
  • 作者单位

    Department of Applied Mathematics & Statistics, The Johns Hopkins University, Baltimore, MD, USA;

    Department of Mathematics, Imperial College London, London, UK;

    National Center for Atmospheric Research, Boulder, CO, USA;

    Departamento de Fi'sica, Facultad de Ciencias Exactas y Naturales, Universidad de Buenos Aires,Ciudad Universitaria, Buenos Aires, Argentina;

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