论文标题

太阳轨道观察到的镜像模式风暴

Mirror mode storms observed by Solar Orbiter

论文作者

Dimmock, A. P., Yordanova, E., Graham, D. B., Khotyaintsev, Yu. V., Blanco-Cano, X., Kajdič, P., Karlsson, T., Fedorov, A., Owen, C. J., Werner, E. A. L. E., Johlander, A.

论文摘要

镜像模式在空间等离子体中无处不在,并从压力各向异性生长。与其他不稳定性一起,它们在限制血浆中包含的自由能力方面发挥了基本作用。这项研究的重点是太阳能轨道在太阳风中观察到的镜子模式,以0.5和1 AU之间的地中心距离。通常,镜像模式的时间尺度从几秒钟到数十秒钟,被认为是准MHD结构。在太阳风中,它们通常也作为孤立的结构出现。但是,在某些条件下,测量了延长的较高频率镜像模式的延长和爆发列车,这些模式以前被标记为镜像模式风暴。目前,只有少数现有研究集中在镜像模式风暴上,这意味着仍然存在许多开放问题。在这项研究中,太阳能轨道器已用于研究镜像模式风暴的几个关键方面:它们对地中心距离,与局部等离子体特性,时间/空间尺度,振幅以及与大型太阳风瞬变的连接相关的依赖。主要结果是镜像模式风暴通常接近局部离子尺度,并且不能再将其视为准MHD,从而破坏了常用的长波长假设。通常观察到它们接近当前的床单和星际间冲击的下游。在缓慢的太阳风速期间观察到这些事件,并且倾向于更接近太阳的较高发生的趋势。发生的情况很低,因此它们在调节环境太阳风中不发挥基本作用,而是在瞬变内部起着更大的作用。

Mirror modes are ubiquitous in space plasma and grow from pressure anisotropy. Together with other instabilities, they play a fundamental role in constraining the free energy contained in the plasma. This study focuses on mirror modes observed in the solar wind by Solar Orbiter for heliocentric distances between 0.5 and 1 AU. Typically, mirror modes have timescales from several to tens of seconds and are considered quasi-MHD structures. In the solar wind, they also generally appear as isolated structures. However, in certain conditions, prolonged and bursty trains of higher frequency mirror modes are measured, which have been labeled previously as mirror mode storms. At present, only a handful of existing studies have focused on mirror mode storms, meaning that many open questions remain. In this study, Solar Orbiter has been used to investigate several key aspects of mirror mode storms: their dependence on heliocentric distance, association with local plasma properties, temporal/spatial scale, amplitude, and connections with larger-scale solar wind transients. The main results are that mirror mode storms often approach local ion scales and can no longer be treated as quasi-MHD, thus breaking the commonly used long-wavelength assumption. They are typically observed close to current sheets and downstream of interplanetary shocks. The events were observed during slow solar wind speeds and there was a tendency for higher occurrence closer to the Sun. The occurrence is low, so they do not play a fundamental role in regulating ambient solar wind but may play a larger role inside transients.

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