论文标题
一项纳米丝和非热颗粒的虹膜观察性特征的统计研究
A Statistical Study of IRIS Observational Signatures of Nanoflares and Non-thermal Particles
论文作者
论文摘要
纳米体被认为是太阳外气氛中磁能释放和冠状加热的主要机制之一。我们通过使用界面区域成像光谱仪(IRIS)观察到的有关染色体和过渡区域对纳米氟的反应的统计研究,通过使用算法自动检测这些事件。观察到对这些小加热事件的初始大气反应,虹膜是在加热到高温(> 4 MK)的冠状环的脚步处的短暂亮点。对于在143小时内观察到的四个活跃区域,我们在虹膜缝隙下检测到了1082个脚步亮度,对于我们从虹膜MG II和SI IV光谱中提取物理参数的人,分别在染色体和过渡区域形成。我们研究了频谱参数的分布以及参数之间的关系,还将它们与纳米热循环的radyn数值模拟的预测进行了比较。我们发现,这些事件以及非热颗粒的存在在耀斑生产活性区域往往更频繁,而热大气成像组装94Å的发射较高。我们找到了以强Si IV非热速度(不依赖于HeliePentric X坐标,即,即磁场和视线线之间的角度)和不对称MG II光谱的高度动态运动的证据。这些发现对活性区域中纳米氟和非热颗粒的性质及其对较低大气的影响提供了严格的新约束。
Nanoflares are regarded as one of the major mechanisms of magnetic energy release and coronal heating in the solar outer atmosphere. We conduct a statistical study on the response of the chromosphere and transition region to nanoflares, as observed by the Interface Region Imaging Spectrograph (IRIS), by using an algorithm for the automatic detection of these events. The initial atmospheric response to these small heating events is observed, with IRIS, as transient brightening at the footpoints of coronal loops heated to high temperatures (>4 MK). For four active regions, observed over 143 hours, we detected 1082 footpoint brightenings under the IRIS slit, and for those we extracted physical parameters from the IRIS Mg II and Si IV spectra that are formed in the chromosphere and transition region, respectively. We investigate the distribution of the spectral parameters, and the relationship between the parameters, also comparing them with predictions from RADYN numerical simulations of nanoflare-heated loops. We find that these events, and the presence of non-thermal particles, tend to be more frequent in flare productive active regions, and where the hot Atmospheric Imaging Assembly 94 Å emission is higher. We find evidence for highly dynamic motions characterized by strong Si IV non-thermal velocity (not dependent on the heliocentric x coordinate, i.e., on the angle between the magnetic field and the line-of-sight) and asymmetric Mg II spectra. These findings provide tight new constraints on the properties of nanoflares, and non-thermal particles, in active regions, and their effects on the lower atmosphere.