The Role of Farside Magnetic Structures in Modeling the 2024 Solar Eclipse

Guanglu Shi, Jiahui Shan, Li Feng, Jun Chen and Weiqun Gan
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Abstract

The corona is a crucial region that connects the solar surface to the solar wind and serves as the primary site of solar activity. The 2024 total solar eclipse (TSE) provides a unique opportunity to investigate the large-scale coronal structure. Combined with TSE observations, we study the impact of the magnetic structure of the farside active region, located in the eastern hemisphere of the Sun that has not yet rotated into the Earth field of view, on a global magnetohydrodynamic simulation. To address the limitation of single-view measurements for the routine synoptic map, we correct the magnetic field in the farside region by incorporating full-disk magnetograms measured several days after the TSE, allowing us to capture the temporal evolution of the photospheric magnetic field in near real time. Simulation results demonstrate that the local magnetic field in the farside active region can significantly influence the global coronal structure, by altering the position of the heliospheric current sheet, and further affect the global distribution of plasma parameters, even in polar regions. A comparison of the simulation results with white-light TSE + Large Angle and Spectrometric Coronagraph C2 observations and in situ measurements by the Parker Solar Probe reveals that the composite synoptic map improves the accuracy of the coronal modeling. This work provides robust support for advancing our understanding of coronal evolution, as well as deepening the link between the photosphere and large-scale coronal structure. Furthermore, it establishes a theoretical foundation for the future development of multiview stereoscopic measurements of the photospheric magnetic field.
月球背面磁结构在模拟2024年日食中的作用
日冕是连接太阳表面和太阳风的关键区域,也是太阳活动的主要场所。2024年的日全食(TSE)提供了一个独特的机会来研究大规模的日冕结构。结合TSE观测,我们研究了位于太阳东半球尚未旋转进入地球视野的远侧活动区的磁结构对全球磁流体动力学模拟的影响。为了解决常规天气图单视图测量的局限性,我们通过结合TSE后几天测量的全盘磁图来校正远侧区域的磁场,使我们能够近乎实时地捕获光球磁场的时间演变。模拟结果表明,远侧活动区的局部磁场可以通过改变日球层电流片的位置来显著影响全球日冕结构,并进一步影响等离子体参数的全球分布,甚至在极区也是如此。将模拟结果与白光TSE +大角度日冕仪C2和光谱日冕仪观测结果以及帕克太阳探测器的原位测量结果进行比较,表明复合天气图提高了日冕模拟的精度。这项工作为推进我们对日冕演化的理解,以及加深光球层与大尺度日冕结构之间的联系提供了强有力的支持。为今后光球磁场的多视点立体测量奠定了理论基础。
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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