论文标题

激活的太阳能龙卷风般的突出

Coronal Mini-jets in an Activated Solar Tornado-like Prominence

论文作者

Chen, Huadong, Zhang, Jun, De Pontieu, Bart, Ma, Suli, Kliem, Bernhard, Priest, Eric

论文摘要

来自$接口〜区域〜成像〜光谱仪$($ iris $)的高分辨率观察表明,存在一种特定类型的小太阳能喷气机,该太阳能飞机是单独或从龙卷风中悬挂在电晕中的龙卷风般突出的簇中出现的。在这项研究中,我们对龙卷风事件中的43个选定的迷你射流进行了详细的统计分析。 Our results show that the mini-jets typically have: (1) a projected length of 1.0-6.0 Mm, (2) a width of 0.2-1.0 Mm, (3) a lifetime of 10-50 s, (4) a velocity of 100-350 km s$^{-1}$, and (5) an acceleration of 3-20 km s$^{-2}$.根据光谱诊断和EM-LOCI分析,这些喷气机似乎是多热的小等离子体弹出,估计平均电子密度为$ \ sim $ 2.4 $ \ times $ 10 $^{10} $^{10} $ cm $^{ - 3} $,大约平均温度为$ \ sim $ \ sim $ \ syly $ \ $ \ kin,能量密度和消散的磁场强度大致估计为$ \ sim $ 9 erg cm $^{ - 3} $,3 erg cm $^{ - 3} $和16 g。在某些微型固定的脚部上,微型固定,紫外线和EUV亮丽的加速度,以及主机突出的激活表明,龙卷风迷你夹可能是由精细的外部或内部磁性重新连接(a)在突出性场和背景或背景或背景或(b)内部或(b)之间的扭转或贴上薄弱的薄弱的范围之间创建的。这些观察结果提供了对电晕中此类重新连接事件的几何形状的见解,并对突出磁场的结构以及导致突出和冠状质量弹出的不稳定性具有影响。

High-resolution observations from the $Interface~Region~Imaging~Spectrometer$ ($IRIS$) reveal the existence of a particular type of small solar jets, which arose singly or in clusters from a tornado-like prominence suspended in the corona. In this study, we perform a detailed statistical analysis of 43 selected mini-jets in the tornado event. Our results show that the mini-jets typically have: (1) a projected length of 1.0-6.0 Mm, (2) a width of 0.2-1.0 Mm, (3) a lifetime of 10-50 s, (4) a velocity of 100-350 km s$^{-1}$, and (5) an acceleration of 3-20 km s$^{-2}$. Based on spectral diagnostics and EM-Loci analysis, these jets seem to be multi-thermal small-scale plasma ejections with an estimated average electron density of $\sim$2.4 $\times$ 10$^{10}$ cm$^{-3}$ and an approximate mean temperature of $\sim$2.6 $\times$ 10$^{5}$ K. Their mean kinetic energy density, thermal energy density and dissipated magnetic field strength are roughly estimated to be $\sim$9 erg cm$^{-3}$, 3 erg cm$^{-3}$, and 16 G, respectively. The accelerations of the mini-jets, the UV and EUV brightenings at the footpoints of some mini-jets, and the activation of the host prominence suggest that the tornado mini-jets are probably created by fine-scale external or internal magnetic reconnections (a) between the prominence field and the enveloping or background field or (b) between twisted or braided flux tubes within the prominence. The observations provide insight into the geometry of such reconnection events in the corona and have implications for the structure of the prominence magnetic field and the instability that is responsible for the eruption of prominences and coronal mass ejections.

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