Domenico Trotta, Andrew P. Dimmock, Xochitl Blanco-Cano, Robert J. Forsyth, Heli Hietala, Naïs Fargette, Andrea Larosa, Noé Lugaz, Erika Palmerio, Simon W. Good, Juska E. Soljento, Emilia K. J. Kilpua, Emiliya Yordanova, Oreste Pezzi, Georgios Nicolaou, Timothy S. Horbury, Rami Vainio, Nina Dresing, Christopher J. Owen and Robert F. Wimmer-Schweingruber
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引用次数: 0
摘要
我们报告了太阳轨道器于2022年3月8日在0.5au的短日心距离上观测到的快速磁致正反冲击对的直接观测结果。这种结构与完全形成的流相互作用区域有一些共同特征,是由于两个连续的日冕物质抛射(CME)之间的相互作用造成的,以前从未观测到产生一对正向反向冲击的情况。极紫外照相机和日冕仪的远程观测支持了这一设想,在这些观测中发现了两个与现场特征相符的候选喷发。在相互作用区域,我们发现了增强的高能粒子活动、强烈的非径向流偏转和磁重联的证据。在 1 au 处,径向排列良好的 Wind 观测显示了一个复杂的事件,具有流相互作用区和 CME-CME 相互作用的观测特征,从而表明了研究太阳爆发现象的复杂动力学的重要性。
Observation of a Fully-formed Forward–Reverse Shock Pair due to the Interaction between Two Coronal Mass Ejections at 0.5 au
We report direct observations of a fast magnetosonic forward–reverse shock pair observed by Solar Orbiter on 2022 March 8 at the short heliocentric distance of 0.5 au. The structure, sharing some features with fully-formed stream interaction regions, is due to the interaction between two successive coronal mass ejections (CMEs), never previously observed to give rise to a forward–reverse shock pair. The scenario is supported by remote observations from extreme ultraviolet cameras and coronagraphs, where two candidate eruptions compatible with the in situ signatures have been found. In the interaction region, we find enhanced energetic particle activity, strong nonradial flow deflections, and evidence of magnetic reconnection. At 1 au, well radially aligned Wind observations reveal a complex event, with characteristic observational signatures of both stream interaction region and CME–CME interaction, thus demonstrating the importance of investigating the complex dynamics governing solar eruptive phenomena.