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arXiv 1406.3565astro-ph.SR
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慢磁声波传播中的频率相关阻尼

Frequency-dependent damping in propagating slow magneto-acoustic waves

S. Krishna Prasad, D. Banerjee, T. Van Doorsselaere

摘要:

在极地羽流和活动区扇环中经常观测到振荡慢磁声波。这些波的观测周期从几分钟到几十分钟不等,当它们沿着支撑结构传播时,它们的振幅会迅速衰减。以前,热传导,压缩粘度,辐射,密度分层,和面积发散,被确定为在慢波振幅的变化的一些原因。我们最近的研究表明,在这些波中观察到的阻尼是频率相关的。我们使用成像数据SDO/AIA,详细研究这种依赖性,并首次从观测中,我们试图推导出阻尼长度和频率之间的定量关系,这些振荡。我们开发了一种新的分析方法来获得这种关系。所观察到的频率依赖性似乎不同意与当前的线性波理论,它被发现,在极地地区观察到的波显示出不同的依赖性,从那些观察到的盘上的循环结构,尽管在其属性的相似性。

英文摘要:

Propagating slow magneto-acoustic waves are often observed in polar plumes and active region fan loops. The observed periodicities of these waves range from a few minutes to few tens of minutes and their amplitudes were found to decay rapidly as they travel along the supporting structure. Previously, thermal conduction, compressive viscosity, radiation, density stratification, and area divergence, were identified to be some of the causes for change in the slow wave amplitude. Our recent studies indicate that the observed damping in these waves is frequency dependent. We used imaging data from SDO/AIA, to study this dependence in detail and for the first time from observations we attempted to deduce a quantitative relation between damping length and frequency of these oscillations. We developed a new analysis method to obtain this relation. The observed frequency dependence does not seem to agree with the current linear wave theory and it was found that the waves observed in the polar regions show a different dependence from those observed in the on-disk loop structures despite the similarity in their properties.

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