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arXiv 2303.03072astro-ph.SR
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光球层瞬态丝状结构在孔隙边界处的衰减及色球层响应

Decay of a photospheric transient filament at the boundary of a pore and the chromospheric response

Philip Lindner, Rolf Schlichenmaier, Nazaret Bello González, Jaime de la Cruz Rodríguez

AI总结:

本研究通过分析孔隙边界瞬态光球层丝状结构的衰减,结合光谱偏振观测与反演,发现其与高层大气温度升高及双向流动相关,提出磁重联驱动该过程的机制。

摘要:

孔隙与太阳黑子之间的中间阶段是一种罕见现象,可表现为瞬态光球层类半影丝状结构的形成。尽管此类丝状结构演化过程中磁场变化迅速,但尚未有研究将其与磁重联事件联系起来。我们分析了瑞典太阳望远镜对NOAA AR 12739中一个孔隙的观测数据,包括Fe I 6173 Å和Ca II 8542 Å线的光谱偏振数据,以及Ca II K 3934 Å线的光谱数据。利用VFISV Milne-Eddington反演代码和多谱线非局部热动平衡(Non-LTE)反演代码STiC,获取了光球层和色球层的大气参数。在孔隙边界处的光球层倾角图中,发现了多个倾斜磁场的丝状结构,尽管该孔隙从未发展出半影。其中一条丝状结构在连续谱强度图中显示出清晰对应体,并伴有光球层蓝移。在其衰减过程中,观测到Ca II 8542 Å线蓝翼的增亮。Ca II K 3934 Å和Ca II 8542 Å线在该区域显示出复杂的谱线轮廓。利用所有可用谱线数据进行的随深度变化的STiC反演结果显示,在log tau=-3.5处存在温度升高(约1000开尔文)和双向流动(幅度高达8公里/秒)。衰减丝状结构(在光球层观测到)与高层光球层/低层色球层中的温度升高及双向流动在时间和空间上的相关性表明它们之间存在联系。我们提出了在光球层上升磁通管边缘发生磁重联的情景。这导致了光球层中丝状结构的衰减,以及观测到的高层光球层/低层色球层中的温度升高和双向流动。

英文摘要:

Intermediate stages between pores and sunspots are a rare phenomenon and can manifest with the formation of transient photospheric penumbral-like filaments. Although the magnetic field changes rapidly during the evolution of such filaments, they have not been shown to be connected to magnetic reconnection events yet. We analyzed observations of a pore in NOAA AR 12739 from the Swedish Solar Telescope including spectropolarimetric data of the Fe I 6173 Å and the Ca II 8542 Å line and spectroscopic data of the Ca II K 3934 Å line. The VFISV Milne-Eddington inversion code and the multi-line Non-LTE inversion code STiC were utilized to obtain atmospheric parameters in the photosphere and the chromosphere. Multiple filamentary structures of inclined magnetic fields are found in photospheric inclination maps at the boundary of the pore, although the pore never developed a penumbra. One of the filaments shows a clear counterpart in continuum intensity maps in addition to photospheric blueshifts. During its decay, a brightening in the blue wing of the Ca II 8542 Å line is observed. The Ca II K 3934 Å and the Ca II 8542 Å lines show complex spectral profiles in this region. Depth-dependent STiC inversion results using data from all available lines yield a temperature increase (roughly 1000 Kelvin) and bidirectional flows (magnitudes up to 8 km/s) at log tau=-3.5. The temporal and spatial correlation of the decaying filament (observed in the photosphere) to the temperature increase and the bidirectional flows in the high photosphere/low chromosphere suggests that they are connected. We propose scenarios in which magnetic reconnection happens at the edge of a rising magnetic flux tube in the photosphere. This leads to both the decay of the filament in the photosphere and the observed temperature increase and the bidirectional flows in the high photosphere/low chromosphere.

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