在分层粘性等离子体中演化的非线性扭转阿尔弗波:日冕洞羽流

S.M. Hejazi, S. Vasheghani Farahani, K. Hajisharifi, H. Mehdian
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引用次数: 0

摘要

我们模拟了以平行结构为特征的太阳大气结构。我们重点研究了弱非线性机制下的阿尔弗波,以突出耗散效应突出时非线性波陡峭化的效率。我们还考虑了冲击形成所涉及的局部和平衡条件,以及冲击对日冕地震学的贡献。日冕羽流是通过在圆柱几何中实施磁流体动力学(MHD)理论进行分析建模的。在这里,分层和粘度存在于羽流内部,而外部介质的影响以及平衡条件则隐含在磁场平行于羽流轴线的地方。我们采用了二阶薄通量管近似,得到了一个波方程,该方程指出了与非线性、耗散和分层项以及代表大气条件的项有关的效应。科恩-库尔斯鲁德-伯格斯(Cohen-Kulsrud-Burgers)型方程所提取的剪切粘度对非线性阿尔弗波的影响在传播到更高海拔时证明更为有效。与无量纲粘度相关的耗散效应表明,耗散效应不是线性的。同时,冲击形成的延迟使得能量转换在更高的高度进行,从而将日冕加热维持在更高的水平。这种横向结构提高了平行结构和粘性阻尼的效率,因为它与外部等离子体-β成正比。据观察,Alfv\'en 脉冲可能在日冕等离子体的低层或向高区域传播时发生反向冲击,这意味着在不同高度发生了能量转换。观测到一个峰值,表明相互作用在太阳半径 1.5 美元左右的高度发生逆转。这种效应在日冕地震学中起着关键作用。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Non-linear torsional Alfv\'en waves evolving in stratified viscous plasmas: Coronal hole plumes
We model solar atmospheric structures characterised by parallel structuring. We focus on Alfv\'en waves in the weakly non-linear regime to highlight the efficiency of non-linear wave steepening when dissipative effects are prominent. We also consider the local and equilibrium conditions involved in shock formation and the shock's contributions to coronal seismology. Coronal plumes were modelled analytically by implementing the magnetohydrodynamic (MHD) theory in cylindrical geometry. Here, the stratification and viscosity are present internal to the plume, whilst effects of the external medium, together with equilibrium conditions, are implied where the magnetic fields are parallel to the plume axis. We implemented a second-order thin flux tube approximation to obtain a wave equation that points to effects tied to non-linear, dissipative, and stratification terms, as well as terms representing atmospheric conditions. The impact of shear viscosity on non-linear Alfv\'en waves extracted by the Cohen-Kulsrud-Burgers-type equation proves more efficient when propagated to higher altitudes. The dissipative effects linked to the dimensionless viscosity indicate that the dissipative effects are not linear. Meanwhile, the delay in shock formation enables energy conversions at higher altitudes, thereby maintaining coronal heating at higher levels. The efficiency of parallel structuring and viscous damping is enhanced by such transverse structuring, as it is directly proportional to the external plasma-beta . It is observed that Alfv\'en pulses may undergo a backward shock, either in the lower levels of coronal plasma or as they propagate toward higher regions, implying a conversion of energy occurring at various altitudes. A peak was observed, indicating that the interplay reverses at heights around $1.5$ solar radii. Such effects are shown to play a key role in the context of coronal seismology.
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