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Alfvén vortex filaments observed in magnetosheath downstream of a quasi-perpendicular bow shock

机译:阿尔芬涡丝磁鞘中观察到下游的quasi-perpendicular弓形激波

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Magnetic field fluctuations in the frequency range [0.02–12.5] Hz are studied with the four Cluster satellites in the Earth magnetosheath downstream of a quasi-perpendicular bow shock. The turbulent spectrum presents a spectral break accompanied by a broad maximum usually interpreted as due to Alfvén ion cyclotron waves. In this paper we establish that this spectral knee corresponds to space-localized coherent magnetic structures in the form of Alfvén vortices. The Alfvén vortex is a nonlinear cylindrical Alfvén wave, quasi-parallel to the mean magnetic field B 0 and propagating in a plane perpendicular to B 0. In this plane the observed vortices are localized within 20c/ω pi . The frequent observations of such structures indicate their stability in the plasma. Therefore the Alfvén vortices can be an important element in the magnetosheath turbulence. The possible origins of these vortices, such as a strong turbulence or the filamentation instability of an Alfvén wave, are discussed.
机译:磁场波动的频率范围(0.02 - -12.5)赫兹研究四个集群卫星在地球磁鞘下游的quasi-perpendicular弓形激波。谱提出了一种光谱打破陪同广泛的最大的通常解释为由于阿尔芬离子回旋波。建立光谱膝盖对应space-localized连贯的磁结构阿尔芬漩涡的形式。一个非线性圆柱阿尔芬波,quasi-parallel平均磁场B 0在一个平面垂直于传播B 0。这个平面上观察到的漩涡是本地化在20 c /ωπ。这种结构表示他们的稳定等离子体。磁鞘中重要的元素动荡。漩涡,如强烈的动荡丝状形成阿尔芬波的不稳定性进行了讨论。

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