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首页> 外文期刊>The Astrophysical journal >TRANSVERSE OSCILLATIONS OF LOOPS WITH CORONAL RAIN OBSERVED BY HINODE/SOLAR OPTICAL TELESCOPE
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TRANSVERSE OSCILLATIONS OF LOOPS WITH CORONAL RAIN OBSERVED BY HINODE/SOLAR OPTICAL TELESCOPE

机译:蛇行/太阳光学望远镜观测到的冠状雨水的横向振荡

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The condensations composing coronal rain, falling down along loop-like structures observed in cool chromospheric lines such as Hα and Ca II H, have long been a spectacular phenomenon of the solar corona. However, considered a peculiar sporadic phenomenon, it has not received much attention. This picture is rapidly changing due to recent high-resolution observations with instruments such as the Hinode/Solar Optical Telescope (SOT), CRISP of the Swedish 1-m Solar Telescope, and the Solar Dynamics Observatory. Furthermore, numerical simulations have shown that coronal rain is the loss of thermal equilibrium of loops linked to footpoint heating. This result has highlighted the importance that coronal rain can play in the field of coronal heating. In this work, we further stress the importance of coronal rain by showing the role it can play in the understanding of the coronal magnetic field topology. We analyze Hinode/SOT observations in the Ca II H line of a loop in which coronal rain puts in evidence in-phase transverse oscillations of multiple strand-like structures. The periods, amplitudes, transverse velocities, and phase velocities are calculated, allowing an estimation of the energy flux of the wave and the coronal magnetic field inside the loop through means of coronal seismology. We discuss the possible interpretations of the wave as either standing or propagating torsional Alfvén or fast kink waves. An estimate of the plasma beta parameter of the condensations indicates a condition that may allow the often observed separation and elongation processes of the condensations. We also show that the wave pressure from the transverse wave can be responsible for the observed low downward acceleration of coronal rain.
机译:冠状雨的凝结沿着像Hα和Ca II H这样的冷色球线中观察到的环状结构下降,长期以来一直是太阳日冕的一种引人注目的现象。然而,被认为是一种特殊的零星现象,它并没有引起太多关注。由于使用诸如Hinode / Solar光学望远镜(SOT),瑞典1-m太阳望远镜的CRISP和太阳动力学天文台等仪器进行的高分辨率观测,此图片正在迅速改变。此外,数值模拟表明日冕雨是与脚点加热有关的回路热平衡的损失。这一结果突出了日冕雨在日冕加热领域中的重要性。在这项工作中,我们通过展示日冕雨在理解日冕磁场拓扑中可以发挥的作用,进一步强调日冕雨的重要性。我们分析了一个循环的Ca II H线中的Hinode / SOT观测结果,在该循环中冠状雨水证明了多股状结构的同相横向振荡。计算周期,幅度,横向速度和相速度,从而可以通过日冕地震学估算波的能量通量和回路内部的日冕磁场。我们讨论了波浪的可能解释,如驻波或传播扭转阿尔夫芬或快速扭结波。对缩合物的血浆β参数的估计表明了一种条件,该条件可能允许经常观察到的缩合物的分离和伸长过程。我们还表明,来自横波的波压可能是观测到的日冕雨低向下加速度的原因。

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