不同纬度太阳极地磁场的长期变化

Shuhong Yang, Jie Jiang, Zifan Wang, Yijun Hou, Chunlan Jin, Qiao Song, Yukun Luo, Ting Li, Jun Zhang, Yuzong Zhang, Guiping Zhou, Yuanyong Deng, Jingxiu Wang
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引用次数: 0

摘要

太阳的两极磁场在控制太阳活动和驱动快速太阳风方面发挥着重要作用。然而,由于我们对太阳的观测仅限于黄道面,极区在很大程度上仍是未知区域。我们利用2012年至2021年由Hinode观测到的高空间分辨率和极坐标精度的矢量磁图,研究了不同纬度极冠磁场的长期变化。日出期磁力测量结果表明,南北极帽的极性反转过程是非同步的。平均径向磁通密度的变化表明,在每个极冠中,极性反转是从纬度 70 度到极点依次完成的,反映了其中的磁通向极迁移过程。这些结果澄清了不同纬度的极地磁极反转过程。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Long-term variation of the solar polar magnetic fields at different latitudes
The polar magnetic fields of the Sun play an important role in governing solar activity and powering fast solar wind. However, because our view of the Sun is limited in the ecliptic plane, the polar regions remain largely uncharted. Using the high spatial resolution and polarimetric precision vector magnetograms observed by Hinode from 2012 to 2021, we investigate the long-term variation of the magnetic fields in polar caps at different latitudes. The Hinode magnetic measurements shows that the polarity reversal processes in the north and south polar caps are non-simultaneous. The variation of the averaged radial magnetic flux density reveals that, in each polar cap, the polarity reversal is completed successively from the 70$\degr$ latitude to the pole, reflecting a poleward magnetic flux migration therein. These results clarify the polar magnetic polarity reversal process at different latitudes.
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