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arXiv 1902.04431physics.space-ph
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向阳面磁层顶表面本征模的直接观测

Direct observations of a surface eigenmode of the dayside magnetopause

M. O. Archer, H. Hietala, M. D. Hartinger, F. Plaschke, V. Angelopoulos

摘要:

磁层和周围等离子体之间的突然边界,即磁层顶,长期以来一直被认为是支持表面波的。有人提出,作用在边界上的脉冲可能会导致这些波在向阳面被电离层捕获,从而导致磁层顶表面的驻波或本征模。到目前为止,还没有发现直接的观察证据,对间接证据的搜索也证明是不确定的,导致人们猜测这种机制可能不会发生。利用偶然的多点航天器观测,在一个罕见的孤立的快速等离子体射流撞击边界,在这里,我们表明,由此产生的磁层顶运动和磁层超低频波在定义明确的频率是一致的,只能解释的磁层顶表面本征模。因此,我们通过直接观测表明,这种机制,这应该对全球磁层系统的影响,事实上确实发生。

英文摘要:

The abrupt boundary between a magnetosphere and the surrounding plasma, the magnetopause, has long been known to support surface waves. It was proposed that impulses acting on the boundary might lead to a trapping of these waves on the dayside by the ionosphere, resulting in a standing wave or eigenmode of the magnetopause surface. No direct observational evidence of this has been found to date and searches for indirect evidence have proved inconclusive, leading to speculation that this mechanism might not occur. By using fortuitous multipoint spacecraft observations during a rare isolated fast plasma jet impinging on the boundary, here we show that the resulting magnetopause motion and magnetospheric ultra-low frequency waves at well-defined frequencies are in agreement with and can only be explained by the magnetopause surface eigenmode. We therefore show through direct observations that this mechanism, which should impact upon the magnetospheric system globally, does in fact occur.

机构、总结、中文摘要均由AI分析而来,可能存在错误,请以论文正文为准。

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