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Tempered Fractional Brownian Motion: Wavelet Estimation and Modeling of Turbulence in Geophysical Flows

机译:回火分数布朗运动:小波估计和地球物理流湍流建模

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Fractional Brownian motion (fBm) is a Gaussian, stationary-increment process whose self-similarity property is governed by the so-named Hurst parameter H ∈ (0,1). FBm is one of the most widely used models of scale invariance, and its instance H = 1/3 corresponds to the classical Kolmogorov spectrum for the inertial range of turbulence. Tempered fractional Brownian motion (tfBm) was recently introduced as a new canonical model that displays the so-named Davenport spectrum, a model that also accounts for the low frequency behavior of turbulence. The autocorrelation of its increments displays semi-long range dependence, i.e., hyperbolic decay over moderate scales and quasi-exponential decay over large scales. The latter property has now been observed in many phenomena, from wind speed to geophysics to finance. This paper introduces a wavelet framework to construct the first estimation method for tfBm. The properties of the wavelet coefficients and spectrum of tfBm are studied, and the estimator's performance is assessed by means of Monte Carlo experiments. We also use tfBm to model geophysical flow data in the wavelet domain and show that tfBm provides a closer fit than fBm.
机译:分数布朗运动(fBm)是高斯平稳增长过程,其自相似性受所谓的赫斯特参数H∈(0,1)支配。 FBm是比例不变性最广泛使用的模型之一,其实例H = 1/3对应于湍流惯性范围的经典Kolmogorov谱。最近引入了调和分数布朗运动(tfBm)作为新的规范模型,该模型显示了所谓的Davenport频谱,该模型也说明了湍流的低频行为。其增量的自相关显示半长距离依赖性,即中等规模的双曲线衰减和大规模的准指数衰减。从风速到地球物理学再到金融,现在已经在许多现象中观察到了后者的特性。本文介绍了一种小波框架来构造tfBm的第一种估计方法。研究了小波系数和tfBm谱的性质,并通过蒙特卡洛实验评估了估计器的性能。我们还使用tfBm在小波域中对地球物理流数据进行建模,并表明tfBm比fBm更适合。

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