论文标题
太阳喷发失败期间通量绳的扭结振荡
Kink Oscillation of a Flux Rope During a Failed Solar Eruption
论文作者
论文摘要
我们报告说,在爆发的爆发耀斑期间,通量绳的衰减扭结振荡,SDO/AIA在太阳肢上观察到,缺乏可检测到的白光冠状质量弹出。事件期间,爆发的通量绳经历了扭结,旋转和明显的腿腿相互作用。在304、171和193Å的多个AIA通道中同时观察到振荡,这表明多族血浆被夹在绳索中。到达活性区域的上覆的环后,通量绳表现出较大的振幅,衰减的扭结振荡,明显的初始振幅为30 mm,周期约为16分钟,衰减时间约为17分钟。我们将这些振荡解释为通量绳的基本站立扭结模式。振荡极化具有清晰的垂直分量,而检测到的波形从正弦信号的偏离表明振荡可以是循环或椭圆极化的。估计的扭结速度为1080 km/s,对应于约760 km/s的AlfVén速度。这种速度以及我们的DEM分析中的绳索中估计的电子密度,大约$ n_e \ $(1.5--2.0)$ \ times 10^9 $ cm $ $^{ - 3} $,产生了约15 g的磁场强度。据我们所知,在我们所知的最佳知识中,衰减了与不抗旋转的扭曲旋转量的衰减。这些振荡为在失败的喷发期间间接测量磁场强度的间接测量提供了独特的机会。
We report a decaying kink oscillation of a flux rope during a confined eruptive flare, observed off the solar limb by SDO/AIA, that lacked a detectable white-light coronal mass ejection. The erupting flux rope underwent kinking, rotation, and apparent leg-leg interaction during the event. The oscillations were observed simultaneously in multiple AIA channels at 304, 171, and 193 Å, indicating that multithermal plasma was entrained in the rope. After reaching the overlying loops in the active region, the flux rope exhibited large-amplitude, decaying kink oscillations with an apparent initial amplitude of 30 Mm, period of about 16 min, and decay time of about 17 min. We interpret these oscillations as a fundamental standing kink mode of the flux rope. The oscillation polarization has a clear vertical component, while the departure of the detected waveform from a sinusoidal signal suggests that the oscillation could be circularly or elliptically polarized. The estimated kink speed is 1080 km/s, corresponding to an Alfvén speed of about 760 km/s. This speed, together with the estimated electron density in the rope from our DEM analysis, $n_e \approx$(1.5--2.0)$\times 10^9$cm$^{-3}$, yields a magnetic field strength of about 15 G. To the best of our knowledge, decaying kink oscillations of a flux rope with non-horizontal polarization during a confined eruptive flare have not been reported before. These oscillations provide unique opportunities for indirect measurements of the magnetic-field strength in low-coronal flux ropes during failed eruptions.