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Nonlinear time series analysis of the fluctuations of the geomagnetic horizontal field

机译:地磁水平场波动的非线性时间序列分析

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A detailed nonlinear time series analysis of the hourly data of the geomagnetic horizontal intensity H measured at Kodaikanal (10.2° N; 77.5° E; mag: dip 3.5° N) has been carried out to investigate the dynamical behaviour of the fluctuations of H. The recurrence plots, spatiotemporal entropy and the result of the surrogate data test show the deterministic nature of the fluctuations, rejecting the hypothesis that H belong to the family of linear stochastic signals. The low dimensional character of the dynamics is evident from the estimated value of the correlation dimension and the fraction of false neighbours calculated for various embedding dimensions. The exponential decay of the power spectrum and the positive Lyapunov exponent indicate chaotic behaviour of the underlying dynamics of H. This is also supported by the results of the comparison of the chaotic characteristics of the time series of H with the pseudo-chaotic characteristics of coloured noise time series. We have also shown that the error involved in the short-term prediction of successive values of H, using a simple but robust, zero-order nonlinear prediction method, increases exponentially. It has also been suggested that there exists the possibility of characterizing the geomagnetic fluctuations in terms of the invariants in chaos theory, such as Lyapunov exponents and correlation dimension. The results of the analysis could also have implications in the development of a suitable model for the daily fluctuations of geomagnetic horizontal intensity.Key words. Geomagnetism and paleomagnetism (time variations, diurnal to secular) – History of geophysics (solar-planetary relationships) Magnetospheric physics (storms and substorms)
机译:已经对Kodaikanal(10.2°N; 77.5°E; mag:dip 3.5°N)测得的地磁水平强度 H 的小时数据进行了详细的非线性时间序列分析,以研究动力 H 波动的行为。递归图,时空熵和替代数据检验的结果表明了波动的确定性,拒绝了 H 属于线性随机信号族的假设。动力学的低维特征从相关维的估计值和针对各种嵌入维计算出的虚假邻居的比例显而易见。功率谱的指数衰减和正Lyapunov指数表明 H 的基本动力学的混沌行为。将 H 的时间序列的混沌特性与有色噪声时间序列的伪混沌特性进行比较的结果也证明了这一点。我们还表明,使用简单但健壮的零阶非线性预测方法,对 H 的连续值进行短期预测时所涉及的误差呈指数增长。也有人建议,有可能根据混沌理论中的不变量,例如李雅普诺夫指数和相关维数,来表征地磁波动。分析结果也可能对地磁水平强度日变化的合适模型的开发产生影响。 关键词。 地磁和古磁学(时间变化,从白天到长期)–地球物理学的历史(太阳与行星的关系)磁层物理学(风暴和亚暴)

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