论文标题
两个太阳喷发事件的磁通绳特性的定量表征
Quantitative Characterization of Magnetic Flux Rope Properties for Two Solar Eruption Events
论文作者
论文摘要
为了弥合冠状质量弹出(CMES)的地球层观测和太阳观测之间的间隙,关键步骤之一是提高对它们相应的磁性结构(如磁通绳(MFR))的理解。但是,在太阳上或在CME爆发之前或在CME爆发之前确认存在连贯的MFR并定量表征CME-MFR是一个挑战,这是一个挑战。在这项研究中,我们研究了MFR结构,该结构源自两个活性区域(ARS),AR 11719和AR 12158,并定量估计它们的磁性。我们使用预处理的光电矢量磁力图执行非无线电场外推。此外,还采用了遥感观测来找到太阳上MFR的间接证据,并分析了喷发过程中与耀斑丝带相关的磁重新连接通量的时间演变。通过对外推和观察的组合分析,定量地确定了一个事件,在耀斑喷发之前进行了连贯的“预先存在的” MFR结构。然后估算了估计的CME-MFR,形成CME-MFR,包括轴向磁通量,场线扭曲和重新连接通量,并将其与相应的原位建模结果进行比较。我们发现,这两种事件都与伴随的耀斑相关的磁重新连接将大量通量注入了爆发的CME-MFR。
In order to bridge the gap between heliospheric and solar observations of coronal mass ejections (CMEs), one of the key steps is to improve the understanding of their corresponding magnetic structures like the magnetic flux ropes (MFRs). But it remains a challenge to confirm the existence of a coherent MFR before or upon the CME eruption on the Sun and to quantitatively characterize the CME-MFR due to the lack of direct magnetic field measurement in the corona. In this study, we investigate the MFR structures, originating from two active regions (ARs), AR 11719 and AR 12158, and estimate their magnetic properties quantitatively. We perform the nonlinear force-free field extrapolations with preprocessed photospheric vector magnetograms. In addition, remote-sensing observations are employed to find indirect evidence of MFRs on the Sun and to analyze the time evolution of magnetic reconnection flux associated with the flare ribbons during the eruption. A coherent "pre-existing" MFR structure prior to the flare eruption is identified quantitatively for one event from the combined analysis of the extrapolation and observation. Then the characteristics of MFRs for two events on the Sun before and during the eruption, forming the CME-MFR, including the axial magnetic flux, field-line twist, and reconnection flux, are estimated and compared with the corresponding in situ modeling results. We find that the magnetic reconnection associated with the accompanying flares for both events injects significant amount of flux into the erupted CME-MFRs.