椭圆Ornstein-Uhlenbeck过程

Pub Date : 2023-01-01 DOI:10.4310/sii.2023.v16.n1.a11
Adam Sykulski, Sofia Charlotta Olhede, Hanna Sykulska-Lawrence
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引用次数: 0

摘要

我们引入了椭圆Ornstein-Uhlenbeck (OU)过程,它是众所周知的单变量OU过程在二元时间序列上的推广。该过程在复平面上绘制出随时间的椭圆随机振荡,这在耦合二元时间序列的许多应用中都可以观察到。该模型的吸引力在于椭圆振荡是使用一个简单的一阶SDE生成的,而替代模型需要更复杂的矢量化或高阶SDE表示。第二个有用的特征是,参数估计可以在频域鲁棒地执行,仅使用建模和观测功率谱密度,而不必建模和计算单个时间序列分量的交叉谱。我们确定了模型的性质,包括平稳性的条件和椭圆振荡的几何结构。我们通过测量地球极运动的周期性和椭圆性来证明该模型的实用性。
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The elliptical Ornstein–Uhlenbeck process
We introduce the elliptical Ornstein-Uhlenbeck (OU) process, which is a generalisation of the well-known univariate OU process to bivariate time series. This process maps out elliptical stochastic oscillations over time in the complex plane, which are observed in many applications of coupled bivariate time series. The appeal of the model is that elliptical oscillations are generated using one simple first order SDE, whereas alternative models require more complicated vectorised or higher order SDE representations. The second useful feature is that parameter estimation can be performed robustly in the frequency domain using only the modelled and observed power spectral density, without having to model and compute cross spectra of individual time series components. We determine properties of the model including the conditions for stationarity, and the geometrical structure of the elliptical oscillations. We demonstrate the utility of the model by measuring periodic and elliptical properties of Earth's polar motion.
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