Permutation entropy and complexity analysis of large-scale solar wind structures and streams

IF 1.7 4区 地球科学 Q3 ASTRONOMY & ASTROPHYSICS
Emilia K. J. Kilpua, Simon Good, Matti Ala-Lahti, Adnane Osmane, Venla Koikkalainen
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Abstract

Abstract. In this work, we perform a statistical study of magnetic field fluctuations in the solar wind at 1 au using permutation entropy and complexity analysis and the investigation of the temporal variations of the Hurst exponents. Slow and fast wind, magnetic clouds, interplanetary coronal mass ejection (ICME)-driven sheath regions, and slow–fast stream interaction regions (SIRs) have been investigated separately. Our key finding is that there are significant differences in permutation entropy and complexity values between the solar wind types at larger timescales and little difference at small timescales. Differences become more distinct with increasing timescales, suggesting that smaller-scale turbulent features are more universal. At larger timescales, the analysis method can be used to identify localised spatial structures. We found that, except in magnetic clouds, fluctuations are largely anti-persistent and that the Hurst exponents, in particular in compressive structures (sheaths and SIRs), exhibit a clear locality. Our results shows that, in all cases apart from magnetic clouds at the largest scales, solar wind fluctuations are stochastic, with the fast wind having the highest entropies and low complexities. Magnetic clouds, in turn, exhibit the lowest entropy and highest complexity, consistent with them being coherent structures in which the magnetic field components vary in an ordered manner. SIRs, slow wind and ICME sheaths are intermediate in relation to magnetic clouds and fast wind, reflecting the increasingly ordered structure. Our results also indicate that permutation entropy–complexity analysis is a useful tool for characterising the solar wind and investigating the nature of its fluctuations.
大规模太阳风结构和风流的置换熵与复杂性分析
摘要在这项工作中,我们利用置换熵和复杂性分析以及赫斯特指数的时间变化研究,对 1 au 太阳风中的磁场波动进行了统计研究。我们分别研究了慢风和快风、磁云、行星际日冕物质抛射(ICME)驱动的鞘区以及慢-快流相互作用区(SIRs)。我们的主要发现是,在较大的时间尺度下,太阳风类型之间的置换熵和复杂度值存在显著差异,而在较小的时间尺度下则差异不大。随着时间尺度的增加,差异变得更加明显,这表明较小尺度的湍流特征更具有普遍性。在较大的时间尺度上,分析方法可用于识别局部空间结构。我们发现,除了在磁云中,波动在很大程度上是反持久的,赫斯特指数,特别是在压缩结构(鞘和 SIR)中,表现出明显的局部性。我们的研究结果表明,除了尺度最大的磁云之外,太阳风波动在所有情况下都是随机的,其中快速风的熵最高,复杂度低。磁云则表现出最低的熵和最高的复杂性,这与它们是磁场成分有序变化的相干结构相一致。与磁云和快风相比,SIRs、慢风和集成电路鞘处于中间位置,反映出结构越来越有序。我们的结果还表明,置换熵复杂性分析是描述太阳风特征和研究其波动性质的有用工具。
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来源期刊
Annales Geophysicae
Annales Geophysicae 地学-地球科学综合
CiteScore
4.30
自引率
0.00%
发文量
42
审稿时长
2 months
期刊介绍: Annales Geophysicae (ANGEO) is a not-for-profit international multi- and inter-disciplinary scientific open-access journal in the field of solar–terrestrial and planetary sciences. ANGEO publishes original articles and short communications (letters) on research of the Sun–Earth system, including the science of space weather, solar–terrestrial plasma physics, the Earth''s ionosphere and atmosphere, the magnetosphere, and the study of planets and planetary systems, the interaction between the different spheres of a planet, and the interaction across the planetary system. Topics range from space weathering, planetary magnetic field, and planetary interior and surface dynamics to the formation and evolution of planetary systems.
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