The Birth of a Major Coronal Mass Ejection with Intricate Magnetic Structure from Multiple Active Regions

J. H. Guo, Y. W. Ni, B. Schmieder, Y. Guo, C. Xia, P. Devi, R. Chandra, S. Poedts, R. Joshi, Y. H. Zhou, H. T. Li and P. F. Chen
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Abstract

Coronal mass ejections (CMEs) are the eruptions of magnetized plasma from the Sun and are considered the main driver of adverse space weather events. Hence, understanding their formation process, particularly the magnetic topology, is critical for accurate space weather prediction. Here, based on imaging observations and three-dimensional (3D) data-constrained thermodynamic magnetohydrodynamic (MHD) simulation in spherical coordinates, we exhibit the birth of a CME with intricate magnetic structure from multiple active regions (ARs) due to 3D magnetic reconnection. It is observed as a coronal jet between ARs, accompanied by the back-flowing of filament materials along the jet spine after the passage of the eruptive filament. This jet connects two dimming regions within different ARs. This is an observational proxy of 3D magnetic reconnection between the CME flux rope and the null-point magnetic field lines crossing ARs. Hereafter, the thermodynamic data-constrained MHD simulation successfully reproduces the observed jet and the reconnection process that flux ropes partake in, leading to a CME flux rope with a complex magnetic structure distinct from its progenitor. The generality of this scenario is then validated by data-inspired MHD simulations in a simple multipolar magnetic configuration. This work demonstrates the role of multiple ARs in forming CMEs with intricate magnetic structures. On the one hand, a noncoherent flux rope where not all twisted magnetic field lines wind around one common axis is naturally formed. On the other hand, our findings suggest that the topology of a real CME flux rope may not be solely determined by a single AR, particularly during periods of solar maximum.
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来自多个活动区的具有复杂磁结构的大日冕物质抛射的诞生
日冕物质抛射(cme)是太阳磁化等离子体的喷发,被认为是不利空间天气事件的主要驱动因素。因此,了解它们的形成过程,特别是磁拓扑结构,对准确的空间天气预测至关重要。在这里,基于成像观测和球面坐标下三维(3D)数据约束的热力学磁流体动力学(MHD)模拟,我们展示了由于三维磁重联而从多个活跃区(ARs)产生的具有复杂磁结构的CME的诞生。它被观测为ARs之间的日冕喷流,伴随着喷出的喷流通过后,长丝物质沿着喷流脊回流。这个喷流连接了不同ar内两个变暗的区域。这是CME通量绳与穿越ARs的零点磁场线之间的三维磁重联的观测代理。此后,热力学数据约束的MHD模拟成功地再现了观测到的射流和磁链参与的重联过程,导致CME磁链具有不同于其前身的复杂磁性结构。然后,在简单的多极磁结构中,通过数据启发的MHD模拟验证了这种情况的普遍性。这项工作证明了多个ar在形成具有复杂磁结构的cme中的作用。一方面,一个非相干磁通绳,其中不是所有的扭曲磁场线缠绕在一个共同的轴自然形成。另一方面,我们的研究结果表明,一个真正的日冕物质抛射通量绳的拓扑结构可能不仅仅是由一个单一的AR决定的,特别是在太阳极大期。
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