首页> 外文期刊>Journal of Earth Science & Climatic Change >Traces of Long-Memory in Pre-Seismic MHz Electromagnetic TimeSeries-Part 1: Investigation Through the R/S Analysis and Time-EvolvingSpectral Fractals
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Traces of Long-Memory in Pre-Seismic MHz Electromagnetic TimeSeries-Part 1: Investigation Through the R/S Analysis and Time-EvolvingSpectral Fractals

机译:前兆兆赫电磁时间序列中长记忆的痕迹-第1部分:通过R / S分析和随时间变化的谱分形进行研究

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This paper reports characteristic pre seismic electromagnetic disturbances in the MHz range detected prior to seven significant earthquakes of M L ≥ 5.0 which occurred in Greece between 2009 and 2015. The whole data set was investigated through Rescaled Range (R/S) analysis and wavelet based spectral fractal analysis. The long-memory trends hidden in the analysed signals were investigated via the Hurst exponent (H). The R/S method indicated that in the majority of the segments of the investigated signals, the H - exponents were in the range 0.7-0.9. Several exponents were above 0.9. This is associated with persistency. In several segments, the Hurst exponent exhibited small variance. Noteworthy fluctuations were also found. In many cases the H - time fluctuations were independent of the time evolution of the associated electromagnetic signals. The spectral fractal method, being more suited for this purpose, highlighted the characteristic signals’ epochs, governed by long-lasting fractal organisation. The calculated Hurst exponents in the characteristic long-lasting fractal epochs were associated with medium anti-persistent behaviour or with continuous switching between anti-persistency and persistency. The H - exponents of the random fractal organised segments were mainly persistent. From the data presented in this paper, it is deduced that the R/S method provides additional information on the estimation of the Hurst exponent when combined with the spectral fractal method. Both techniques should be employed in sequential steps to enhance the precursory value of the results.
机译:本文报告了2009年至2015年在希腊发生的ML≥5.0的七次重大地震之前检测到的兆赫范围内的特征性地震前电磁干扰。通过重标度范围(R / S)分析和基于小波的频谱对整个数据集进行了研究。分形分析。通过赫斯特(Hurst)指数(H)研究隐藏在分析信号中的长内存趋势。 R / S方法表明,在所研究信号的大部分片段中,H-指数在0.7-0.9范围内。一些指数高于0.9。这与持久性有关。在几个细分中,赫斯特指数表现出较小的方差。还发现了明显的波动。在许多情况下,H-时间波动与相关电磁信号的时间演变无关。频谱分形方法更适合于此目的,它突出了特征信号的历元,由持久的分形组织决定。在特征持久的分形纪元中计算出的赫斯特指数与中等抗持久性或抗持久性和持久性之间的连续切换有关。分形有组织的片段的H-指数主要是持久的。从本文提供的数据中可以推论,当与频谱分形方法结合使用时,R / S方法提供了有关Hurst指数估计的附加信息。两种技术都应在顺序步骤中使用,以提高结果的前期价值。

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