Effect of intermittent structures on the spectral index of the magnetic field in the slow solar wind

IF 1.7 4区 地球科学 Q3 ASTRONOMY & ASTROPHYSICS
Xin Wang, Xuanhao Fan, Yuxin Wang, Honghong Wu, Lei Zhang
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引用次数: 0

Abstract

Abstract. Intermittent structures are ubiquitous in the solar wind turbulence, and they can significantly affect the power spectral index (which reflects the cascading process of the turbulence) of magnetic field fluctuations. However, to date, an analytical relationship between the intermittency level and the magnetic spectral index has not been shown. Here, we present the continuous variation in the magnetic spectral index in the inertial range as a function of the intermittency level. Using the measurements from the Wind spacecraft, we find 42 272 intervals with different levels of intermittency and with a duration of 5–6 min from 46 slow-wind streams between 2005 and 2013. Among them, each of the intermittent intervals is composed of one dominant intermittent structure and background turbulent fluctuations. For each interval, a magnetic spectral index αB is determined for the Fourier spectrum of the magnetic field fluctuations in the inertial range between 0.01 and 0.3 Hz. A parameter Imax, which corresponds to the maximum of the trace of the partial variance increments of the intermittent structure, is introduced as an indicator of the intermittency level. Our statistical result shows that, as Imax increases from 0 to 20, the magnetic spectrum becomes gradually steeper and the magnetic spectral index αB decreases from −1.63 to −2.01. Accordingly, for the first time, an empirical relation is established between αB and Imax: αB=0.4exp⁡(-Imax/5)-2.02. The result will help us to uncover more details about the contributions of the intermittent structures to the magnetic power spectra and, furthermore, about the physical nature of the energy cascade taking place in the solar wind. It will also help to improve turbulence theories that contain intermittent structures.
间歇性结构对慢速太阳风磁场光谱指数的影响
摘要间歇性结构在太阳风湍流中普遍存在,对磁场波动的功率谱指数(反映湍流的级联过程)有显著影响。然而,到目前为止,还没有显示出间歇性水平与磁谱指数之间的分析关系。在这里,我们给出了在惯性范围内磁谱指数的连续变化作为间歇性水平的函数。利用Wind航天器的测量数据,我们发现2005年至2013年间,46个慢风流中有42 272个间歇期,间歇程度不同,持续时间为5-6分钟。其中,每个间歇区间由一个主导间歇结构和背景湍流波动组成。对于每个区间,确定了磁场在0.01 ~ 0.3 Hz惯性范围内波动的傅立叶谱的磁谱指数αB。引入了一个对应于间歇性结构部分方差增量轨迹最大值的参数imax,作为间歇性水平的指标。统计结果表明,随着Imax从0增大到20,磁谱逐渐变陡,磁谱指数α b从- 1.63减小到- 2.01。据此,首次建立了αB与Imax之间的经验关系:αB=0.4exp (-Imax/5)-2.02。这一结果将帮助我们揭示更多关于间歇性结构对磁功率谱的贡献的细节,进一步,关于在太阳风中发生的能量级联的物理性质。这也将有助于改进包含间歇结构的湍流理论。
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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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