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具有间歇性和低频可变性的时间序列的非线性拉普拉斯谱分析。

Nonlinear Laplacian spectral analysis for time series with intermittency and low-frequency variability.

机构信息

Center for Atmosphere Ocean Science, Courant Institute of Mathematical Sciences, New York University, New York, NY 10012, USA.

出版信息

Proc Natl Acad Sci U S A. 2012 Feb 14;109(7):2222-7. doi: 10.1073/pnas.1118984109. Epub 2012 Jan 17.

Abstract

Many processes in science and engineering develop multiscale temporal and spatial patterns, with complex underlying dynamics and time-dependent external forcings. Because of the importance in understanding and predicting these phenomena, extracting the salient modes of variability empirically from incomplete observations is a problem of wide contemporary interest. Here, we present a technique for analyzing high-dimensional, complex time series that exploits the geometrical relationships between the observed data points to recover features characteristic of strongly nonlinear dynamics (such as intermittency and rare events), which are not accessible to classical singular spectrum analysis. The method employs Laplacian eigenmaps, evaluated after suitable time-lagged embedding, to produce a reduced representation of the observed samples, where standard tools of matrix algebra can be used to perform truncated singular-value decomposition despite the nonlinear geometrical structure of the dataset. We illustrate the utility of the technique in capturing intermittent modes associated with the Kuroshio current in the North Pacific sector of a general circulation model and dimensional reduction of a low-order atmospheric model featuring chaotic intermittent regime transitions, where classical singular spectrum analysis is already known to fail dramatically.

摘要

科学和工程中的许多过程都会呈现出多尺度的时空模式,具有复杂的潜在动力学和时变的外部强迫。由于理解和预测这些现象非常重要,因此从不完全观测中经验性地提取显著的变异性模式是一个具有广泛当代意义的问题。在这里,我们提出了一种分析高维复杂时间序列的技术,该技术利用观测数据点之间的几何关系来恢复强非线性动力学特征(例如间歇性和稀有事件),而经典奇异谱分析无法获得这些特征。该方法采用拉普拉斯特征映射,在适当的时滞嵌入后进行评估,以产生观测样本的降维表示,其中尽管数据集具有非线性几何结构,但仍可以使用矩阵代数的标准工具来执行截断奇异值分解。我们说明了该技术在捕捉与北太平洋环流模型中的黑潮相关的间歇性模式以及具有混沌间歇性状态转变的低阶大气模型的降维方面的效用,其中经典奇异谱分析已经被证明会严重失败。

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