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Maximum entropy spectral analysis of climatic time series revisited: Assessing the statistical significance of estimated spectral peaks

机译:重新讨论气候时间序列的最大熵谱分析:评估估算谱峰的统计显着性

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摘要

One of the most often used methods in the spectral analysis of climatic time series is the parametric method of maximum entropy based on an autoregressive model. The method of maximum entropy is particularly appealing because of its high resolution and its good performance with short time series. Its main drawback is that the statistical significance of the spectral peaks is difficult to assess; consequently, there is a risk of accepting spurious peaks as having a physical origin. We propose to use a computer intensive method, the permutation test, for assessing the statistical significance of the spectral peaks, showing its implementation and the results using simulated and real data. With the simulated data we illustrate the applicability to a short time series but with rich signal content, while with the time series of the Southern Oscillation Index (SOI) we illustrate how it may be used in the estimation of the spectrogram.
机译:在气候时间序列的频谱分析中最常用的方法之一是基于自回归模型的最大熵的参数方法。最大熵方法由于其高分辨率和短时间序列的良好性能而特别吸引人。它的主要缺点是光谱峰的统计显着性难以评估。因此,存在接受虚假峰为物理起源的风险。我们建议使用计算机密集型方法(置换测试)评估光谱峰的统计显着性,并使用模拟和真实数据显示其实现方式和结果。利用仿真数据,我们说明了适用于短时间序列但信号内容丰富的适用性,而利用南方涛动指数(SOI)的时间序列,我们说明了如何将其用于频谱图估计。

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