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arXiv 2402.06016astro-ph.SRphysics.plasm-phphysics.space-ph
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量化太阳轨道器和帕克太阳探测器在0.2至1天文单位间哨声波对超热电子扩散的影响

Quantifying the diffusion of suprathermal electrons by whistler waves between 0.2 and 1 AU with Solar Orbiter and Parker Solar Probe

L. Colomban, M. Kretzschmar, V. Krasnoselkikh, O. V. Agapitov, C. Froment, M. Maksimovic, M. Berthomier, Yu. V. Khotyainsev, D. B. Graham, S. Bale

AI总结:

本研究利用太阳轨道器和帕克太阳探测器数据,统计分析了0.2至1天文单位间的哨声波,并通过准线性理论计算扩散系数,发现哨声波可解释Strahl电子投掷角演化,其中逆向传播波在0.2天文单位处扩散效率高出两个数量级。

摘要:

太阳风电子分布函数随日心距离的演化表现出一些仍无法解释的特征,特别是Strahl(束流)电子投掷角宽度的增加。电子与哨声波之间的波粒相互作用常被用来解释这些现象。我们旨在量化哨声波对超热电子的影响随日心距离的变化。我们首先对太阳轨道器和帕克太阳探测器在0.2至1天文单位间观测到的哨声波(发生率和性质)进行统计分析。然后利用波的特征在准线性理论框架下计算扩散系数。这些系数被积分以推断哨声波在电子传播过程中对其整体影响。在等离子体参考系中检测并表征了110,000个哨声波包。大多数波与磁场对齐,仅约0.5%的波传播角大于45°。在0.3天文单位之外,几乎只观测到背离太阳的波(其中一些发现朝向太阳,但位于开关back内,背景磁场径向分量符号改变)。因此这些波与Strahl对齐,而非逆向传播。在0.2天文单位处,我们发现既有与Strahl对齐的波,也有逆向传播的波。在0.3天文单位之外,积分扩散系数表明观测到的波可以解释测得的Strahl投掷角演化,并能有效使晕(halo)各向同性化。Strahl扩散主要归因于传播角在15°至45°之间的哨声波。在0.2天文单位附近,逆向传播的哨声波对Strahl电子的扩散效率比与Strahl对齐的波高两个数量级。

英文摘要:

The evolution of the solar wind electron distribution function with heliocentric distance exhibits different features that are still unexplained, in particular, the increase of the Strahl pitch angle width. Wave-particle interactions between electrons and whistler waves are often proposed to explain these phenomena. We aim at quantifying the effect of whistler waves on suprathermal electrons as a function of heliocentric distance. We first perform a statistical analysis of whistler waves (occurrence and properties) observed by Solar Orbiter and Parker Solar Probe between 0.2 and 1 AU. The wave characteristics are then used to compute the diffusion coefficients in the framework of quasi-linear theory. These coefficients are integrated in order to deduce the overall effect of whistler waves on electrons along their propagation. 110,000 whistler wave packets are detected and characterized in the plasma frame. Most waves are aligned with the magnetic field and only about 0.5% of them have a propagation angle greater than 45°. Beyond 0.3 AU, almost exclusively anti-sunward waves (some of them are found sunward but are within switchbacks with a change of sign of the radial component of the background magnetic) are observed. These waves are therefore Strahl-aligned and not counter-streaming. At 0.2 AU we find both Strahl-aligned and counter-streaming waves. Beyond 0.3 AU, the integrated diffusion coefficients show that the observed waves can explain the measured Strahl pitch angle evolution and are effective in isotropizing the halo. Strahl diffusion is mainly due to whistler waves with an angle of propagation between 15° and 45°. Near 0.2 AU, counter-streaming whistler waves can diffuse the Strahl electrons more efficiently than the Strahl-aligned waves by two orders of magnitude.

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