Unexpected frequency of horizontal oscillations of magnetic structures in the solar photosphere

M. Berretti, M. Stangalini, G. Verth, S. Jafarzadeh, D. Jess, F. Berrilli, S. Grant, T. Duckenfield, V. Fedun
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Abstract

It is well known that the dominant frequency of oscillations in the solar photosphere is approx 3 mHz, which is the result of global resonant modes pertaining to the whole stellar structure. However, analyses of the horizontal motions of nearly $1$ million photospheric magnetic elements spanning the entirety of solar cycle 24 have revealed an unexpected dominant frequency, approx 5 mHz, a frequency typically synonymous with the chromosphere. Given the distinctly different physical properties of the magnetic elements examined in our statistical sample, when compared to largely quiescent solar plasma where approx 3 mHz frequencies are omnipresent, we argue that the dominant approx 5 mHz frequency is not caused by the buffeting of magnetic elements, but instead is due to the nature of the underlying oscillatory driver itself. This novel result was obtained by exploiting the unmatched spatial and temporal coverage of magnetograms acquired by the Helioseismic and Magnetic Imager (HMI) on board NASA's Solar Dynamics Observatory (SDO). Our findings provide a timely avenue for future exploration of the magnetic connectivity between sub-photospheric, photospheric, and chromospheric layers of the Sun's dynamic atmosphere.
太阳光层磁性结构水平振荡的意外频率
众所周知,太阳光层的主要振荡频率约为 3 mHz,这是涉及整个恒星结构的全球共振模式的结果。然而,对跨越整个太阳周期 24 的近 100 万美元的光球层磁性元素的水平运动进行分析后,发现了一个意想不到的主导频率,约为 5 mHz,这个频率通常是色球层的同义词。鉴于在我们的统计样本中检测到的磁性元素的物理特性与基本处于静态的太阳等离子体截然不同,在静态太阳等离子体中,约 3 mHz 的频率无处不在,因此我们认为,约 5 mHz 的主导频率不是由磁性元素的冲击造成的,而是由基本振荡驱动本身的性质造成的。这一新颖的结果是利用美国宇航局太阳动力学天文台(SDO)上的太阳地震和磁成像仪(HMI)所获取的磁图的无与伦比的空间和时间覆盖范围而获得的。我们的发现为今后探索太阳动态大气层的副光球层、光球层和色球层之间的磁联系提供了一个及时的途径。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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