一种新形式的部分细丝喷发的观测

Abril Sahade, Judith T. Karpen and Spiro K. Antiochos
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引用次数: 0

摘要

日冕物质抛射(cme)和日冕喷流是两种被研究得最好的太阳爆发形式,它们具有相同的潜在物理原理。先前的研究表明部分喷发会产生日冕射流。我们首次报道了对三次局部喷发的详细分析,这些喷发在喷发开始后分割并产生了cme。我们利用来自太阳动力学观测站/大气成像组件、日地关系观测站和太阳轨道器的多波长观测数据来重建事件的三维演变。磁场外推表明,初始细丝被伪流线结构覆盖,细丝支撑通量与外部开场通过零点相互作用后发生分裂。突破机制似乎在停止系统和分裂系统方面发挥了关键作用。然而,这种最初的演化和随后分裂成日珥部分上方未喷发的喷发通量绳,对太阳喷发理论提出了严峻的挑战。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Observations of a New Form of Partial Filament Eruption
Coronal mass ejections (CMEs) and coronal jets are two of the best-studied forms of solar eruptions, with the same underlying physics. Previous studies have presented partial eruptions producing coronal jets. We report, for the first time, a detailed analysis of three partial eruptions that segmented after the eruption began and produced CMEs. We use multiwavelength observations from the Solar Dynamics Observatory/Atmospheric Imaging Assembly, Solar TErrestrial RElations Observatory, and Solar Orbiter to reconstruct the three-dimensional evolution of the events. The magnetic field extrapolations indicated that the initial filaments were overlaid by pseudostreamer structures, and the splitting occurred after the interaction between the filament-supporting flux and external open field through their null points. The breakout mechanism seems to play a key role in both halting the system and splitting it. However, this initial evolution and the consequent splitting into an erupting flux rope above the prominence segment that failed to erupt pose severe challenges to theories of solar eruptions.
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