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arXiv 2008.06887astro-ph.SR
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小尺度表面运动在从遥远的稳定通量绳向太阳喷流的扭转转移中的作用

The role of small-scale surface motions in the transfer of twist to a solar jet from a remote stable flux rope

Reetika Joshi, Brigitte Schmieder, Guillaume Aulanier, Véronique Bommier, Ramesh Chandra

摘要:

喷流通常具有螺旋结构,其中包含喷射出的等离子体,这些等离子体既热又冷,并且比日冕密度大。已经提出了各种机制来解释喷流如何主要归因于磁通量的出现和环境之间的磁重联,或者扭曲的光球运动使系统进入不稳定状态。用AIA和IRIS对一个扭曲射流进行了多波长观测,以了解扭曲是如何被注入射流的。我们根据用UNNOFIT代码计算的HMI矢量磁场分析,跟踪了活动区的磁历史。这个区域是两个新兴的磁通量(EMF)的崩溃的结果,覆盖在拱丝系统,已经很好地观察到与AIA,IRIS和NVST在H-α。在磁场图中,我们发现了沿着两个电磁场之间的极性反转线的长S形磁通绳(FR)图案的证据,这是重联的位置。在喷流之前,FR的延伸是存在的,它的一部分被分离,并形成了一个小的双极与秃斑(BP)区域,动态地成为一个X-电流片的圆顶的一个EMF的重联发生。在重联的时候,Mg II光谱显示出蓝翼的强烈延伸,在10 Mm的距离上(从-300 km/s到几km/s)逐渐减少。这是扭转转移到射流的标志。与数值磁流体动力学(MHD)模拟的比较证实了长FR的存在。我们推测,有一个转移的扭曲射流在FR的重联网站没有FR喷发的延长。连接将从BP重连区域的低层大气开始,并沿着上面形成的电流片在X点延伸。

英文摘要:

Jets often have a helical structure containing ejected plasma that is both hot and also cooler and denser than the corona. Various mechanisms have been proposed to explain how jets are primarily attributed to a magnetic reconnection between the emergence of magnetic flux and environment or that of twisted photospheric motions that bring the system into a state of instability. Multi-wavelength observations of a twisted jet observed with AIA and IRIS were used to understand how the twist was injected into the jet. We followed the magnetic history of the active region based on the analysis of HMI vector magnetic field computed with the UNNOFIT code. This region is the result of the collapse of two emerging magnetic fluxes (EMFs) overlaid by arch filament systems that have been well-observed with AIA, IRIS, and NVST in H-alpha. In the magnetic field maps, we found evidence of the pattern of a long sigmoidal flux rope (FR) along the polarity inversion line between the two EMFs, which is the site of the reconnection. Before the jet, an extension of the FR was present and a part of it was detached and formed a small bipole with a bald patch (BP) region, which dynamically became an X-current sheet over the dome of one EMF where the reconnection took place. At the time of the reconnection, the Mg II spectra exhibited a strong extension of the blue wing that is decreasing over a distance of 10 Mm (from -300 km/s to a few km/s). This is the signature of the transfer of the twist to the jet. A comparison with numerical magnetohydrodynamics (MHD) simulations confirms the existence of the long FR. We conjecture that there is a transfer of twist to the jet during the extension of the FR to the reconnection site without FR eruption. There connection would start in the low atmosphere in the BP reconnection region and extend at an X-point along the current sheet formed above.

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