论文标题
隐形冠状质量排斥的磁性环境
The Magnetic Environment of a Stealth Coronal Mass Ejection
论文作者
论文摘要
由于其发生率相对较高的发生率和空间天气影响,对隐形冠状质量驱逐(CME)的兴趣正在增加。但是,典型的CME特征,例如极端脱光的调光和爆发后拱廊很难识别,需要广泛的图像处理技术。这些薄弱的观察性签名意味着目前对这些事件的物理学的理解很少。我们对磁场配置进行了广泛的研究,其中发生了2011年3月3日的隐形CME。在隐形CME源活性区域(AR)中观察到了三种不同的耀斑色带形成发作。两次发生在喷发之前,建议发生磁重新连接,以建立将变成爆发的结构。第三次发生在立体-B 171A数据中观察到的空腔喷发的时间内;随后,这成为Coronagraph数据中观察到的传播CME的一部分。我们同时使用冠状磁场的局部(笛卡尔)和全局(球形)模型,这些模型通过观测分析进行了补充和验证。我们发现了冠状零点的证据,其田间线从其邻域计算,将隐身CME CME源区域连接到北半球的两个AR。我们得出的结论是,零点的重新连接通过去除稳定爆发前结构的田地来有助于隐形CME的爆发。该隐形CME尽管签名较弱,但具有其他CME的主要特征,其喷发是由类似机制驱动的。
Interest in stealth coronal mass ejections (CMEs) is increasing due to their relatively high occurrence rate and space weather impact. However, typical CME signatures such as extreme-ultraviolet dimmings and post-eruptive arcades are hard to identify and require extensive image processing techniques. These weak observational signatures mean that little is currently understood about the physics of these events. We present an extensive study of the magnetic field configuration in which the stealth CME of 3 March 2011 occurred. Three distinct episodes of flare ribbon formation are observed in the stealth CME source active region (AR). Two occurred prior to the eruption and suggest the occurrence of magnetic reconnection that builds the structure which will become eruptive. The third occurs in a time close to the eruption of a cavity that is observed in STEREO-B 171A data; this subsequently becomes part of the propagating CME observed in coronagraph data. We use both local (Cartesian) and global (spherical) models of the coronal magnetic field, which are complemented and verified by the observational analysis. We find evidence of a coronal null point, with field lines computed from its neighbourhood connecting the stealth CME source region to two ARs in the northern hemisphere. We conclude that reconnection at the null point aids the eruption of the stealth CME by removing field that acted to stabilise the pre-eruptive structure. This stealth CME, despite its weak signatures, has the main characteristics of other CMEs, and its eruption is driven by similar mechanisms.