论文标题
部分可观测时空混沌系统的无模型预测
Observations of a Flare-ignited broad Quasi-periodic Fast-propagating wave train
论文作者
论文摘要
大规模的极端粉状物(EUV)波经常被视为伴有的耀斑和冠状质量弹出现象(CMES)。先前的研究主要集中于带有单波的EUV波,通常认为这是由CME的横向膨胀驱动的。使用太阳能动态观测站和太阳陆地关系观测站进行的高时空分辨率多角度成像观察,我们介绍了对宽度的宽度快速传播(QFP)波动的观察,该波动列车由多个波动表面组成,由多个波动表面组成。 (CH)速度为840 +/- 67 km/s,波前在通过CH的边界时显示出有趣的折射效果。由于CH的月球形状,从CH的北臂和南臂发射的波前开始彼此接近并最终碰撞,从而导致碰撞部位的强度增强。这种增强可能会暗示两个传输波列之间的干扰。波列的估计磁力马赫数约为1.13,这表明观察到的波列是弱冲击。时期分析表明,波列的时期为$ \ sim $ 90秒,与随附的耀斑的同意。根据我们的分析结果,我们得出结论,宽QFP波序列是大振幅快速磁力波或由伴随耀斑中某些非线性能量释放过程驱动的弱冲击。
Large-scale Extreme-ultraviolet (EUV) waves are frequently observed as an accompanying phenomenon of flares and coronal mass ejections (CMEs). Previous studies mainly focus on EUV waves with single wavefronts that are generally thought to be driven by the lateral expansion of CMEs. Using high spatio-temporal resolution multi-angle imaging observations taken by the Solar Dynamic Observatory and the Solar Terrestrial Relations Observatory, we present the observation of a broad quasi-periodic fast propagating (QFP) wave train composed of multiple wavefronts along the solar surface during the rising phase of a GOES M3.5 flare on 2011 February 24. The wave train transmitted through a lunate coronal hole (CH) with a speed of 840 +/-67 km/s, and the wavefronts showed an intriguing refraction effect when they passed through the boundaries of the CH. Due to the lunate shape of the CH, the transmitted wavefronts from the north and south arms of the CH started to approach each other and finally collided, leading to the significant intensity enhancement at the collision site. This enhancement might hint the occurrence of interference between the two transmitted wave trains. The estimated magnetosonic Mach number of the wave train is about 1.13, which indicates that the observed wave train was a weak shock. Period analysis reveals that the period of wave train was $\sim$90 seconds, in good agreement with that of the accompanying flare. Based on our analysis results, we conclude that the broad QFP wave train was a large-amplitude fast-mode magnetosonic wave or a weak shock driven by some non-linear energy release processes in the accompanying flare.