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arXiv 2501.06403astro-ph.SR
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太阳上由日冕EUV喷流驱动的多期远程增亮

Multi-episodes of remote brightenings driven by a coronal EUV jet on the Sun

Chao Zhang, Zhenghua Huang, Hengyuan Wei, Youqian Qi, Mijie Shi, Hui Fu, Xiuhui Zuo, Weixin Liu, Mingzhe Sun, Ming Xiong, Lidong Xia

AI总结:

本文观测太阳EUV喷流引发的两期远程增亮,结合光变、能量与冷热流分析,揭示其分别源于非热电子加热和慢激波热流。

摘要:

远程增亮(RB)是磁环足点处的紧凑增亮,这些磁环远程连接并约束太阳大气中的一次爆发。在此,我们报告对一次由速度约为90 km s^-1的EUV喷流产生的RB的观测。连接RB与喷流的磁环表观长度约为59 Mm。有趣的是,该RB至少呈现两期增亮,其特征表现为光变曲线中的两个峰值。维持RB第一和第二个峰值的能量分别为6.3×10^26 erg和8.4×10^26 erg,并在总能量中占据显著比例。RB增亮的第一个峰值与喷流峰值重合,时间延迟为12秒,而第二个峰值滞后108秒。除抛射流之外,我们还识别出另外两个源自爆发位置的流。其中一个相对较冷,温度为log_10 T/K=5.8–6.1,速度约为275±15 km s^-1。另一个较热,温度为log_10 T/K=7.0–7.3,传播速度快得多,约为750±70 km s^-1。我们将RB的第二个峰值直接归因于这种热流,而数值实验表明该热流是慢激波的结果。考虑到RB第一个峰值与爆发之间的极短时间延迟,我们推断第一期增亮由非热电子加热导致。我们的研究表明,RB中的动力学过程可为认识相应爆发的本质提供重要洞见,并有助于理解能量如何在整个太阳大气中分配。

英文摘要:

Remote brightening (RB) is compact brightening at footpoints of magnetic loops, which are remotely-connecting to and confining an eruption in the solar atmosphere. Here, we report on observations of an RB resulting from an EUV jet with a speed of about 90\,km\,s$^{-1}$. The loops connecting the RB and the jet have an apparent length of about 59\,Mm. Intriguingly, the RB exhibits at least two episodes of brightenings, as characterised by two peaks in its lightcurve. The energies, which sustain the first and second peaks of the RB, are $6.3\times10^{26}$\,erg and $8.4\times10^{26}$\,erg, respectively, and take a significant proportion of the total energy. The first peak of the RB brightenings coincides with the jet's peak with a time delay of 12 seconds, while the second peak lags behind by 108 seconds. Besides the flows of the ejecta, we have identified two additional flows originating from the eruption site. One is relatively cool with a temperature of $log_{10}T/K=5.8-6.1$ and has a speed of about $275\pm15$\,km\,s$^{-1}$. The other is hot with a temperature of $log_{10}T/K=7.0-7.3$ and travels much faster with a speed of about 750$\pm$\,70\,km\,s$^{-1}$. We attribute the second peak of RB directly to this hot flow, which our numerical experiments suggest is the result of a slow shock wave. Considering the minimal time delay between the first peak of RB and the eruption, we infer this first episode is due to heating by nonthermal electrons. Our research demonstrates that the dynamics in an RB can offer vital insights into the nature of the corresponding eruption and help understand how the energy is distributed throughout the solar atmosphere.

机构、总结、中文摘要均由AI分析而来,可能存在错误,请以论文正文为准。

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