A Statistical Approach to Quantify Taylor Microscale for Turbulent Flow Surrogate Model

M. Ross, J. Matulis, H. Bindra
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Abstract

Non-equilibrium statistical mechanics models can be used to construct reduced order models from the time-dynamics data such as numerical or physical fluid mechanics experiments. One of the well-established statistical projection methods is the Kramers-Moyal expansion (KM) method. The first two terms of the KM expansion result can be used to construct a non-linear Langevin equation, which can serve as the statistically-trained reduced-order model. This non-linear Langevin equation can be approximated to the Fokker-Planck equation, which is similar to Advection-Diffusion equation, thereby preserving some characteristics of fluctuations associated with fluid mechanics. The KM method captures continuous-time dynamics, however, any data obtained through measurement is discrete. In order to accurately capture the time dynamics of the discrete data, the method for calculating the KM coefficients must be carefully chosen and implemented. To better represent the solution from discrete data, the drift and diffusion coefficients can be calculated at multiple time scales and then extrapolated to a time scale of zero, assuming a linear correlation. One challenge in using this method is that the calculated KM coefficients are only accurate for time scales greater than the Taylor microscale. This means that the extrapolation must use only the KM coefficients calculated for time scales greater than the Taylor microscale, however, this value is not always provided from the data nor simple to calculate. This work presents a method of approximating the Taylor microscale from the data through the relationship between the Markov property and the Taylor microscale and implementing this method to find the extrapolated KM coefficients. The KM method implementing the Taylor microscale estimation was applied to existing DNS turbulent channel flow data to model a time series. This generated time series was then compared to the DNS data using a statistical analysis including probability density function, autocorrelation, and power spectral density.
湍流代理模型泰勒微尺度量化的统计方法
非平衡统计力学模型可用于从时间动力学数据(如数值或物理流体力学实验)中构建降阶模型。Kramers-Moyal展开(KM)方法是一种完善的统计投影方法。KM展开结果的前两项可用于构造非线性朗格万方程,该方程可作为统计训练的降阶模型。这种非线性Langevin方程可以近似为类似平流扩散方程的Fokker-Planck方程,从而保留了一些与流体力学相关的波动特征。KM方法捕获连续时间动力学,然而,通过测量获得的任何数据都是离散的。为了准确地捕捉离散数据的时间动态,必须仔细选择和实施KM系数的计算方法。为了更好地表示离散数据的解,可以在多个时间尺度上计算漂移和扩散系数,然后外推到零时间尺度,假设线性相关。使用这种方法的一个挑战是,所计算的KM系数仅对大于泰勒微尺度的时间尺度准确。这意味着外推必须只使用大于泰勒微尺度的时间尺度计算的KM系数,然而,这个值并不总是从数据中提供的,也不容易计算。本文提出了一种通过马尔可夫性质与泰勒微尺度之间的关系从数据中近似泰勒微尺度的方法,并实现该方法来寻找外推的KM系数。将实现泰勒微尺度估计的KM方法应用于已有的DNS湍流通道流量数据,对时间序列进行建模。然后,使用统计分析(包括概率密度函数、自相关和功率谱密度)将生成的时间序列与DNS数据进行比较。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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