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首页> 外文期刊>Geophysical Research Letters >Thick escaping magnetospheric ion layer in magnetopause reconnection with MMS observations
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Thick escaping magnetospheric ion layer in magnetopause reconnection with MMS observations

机译:借助MMS观测,磁层顶重新连接中厚层逃逸的磁层离子层

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摘要

The structure of asymmetric magnetopause reconnection is explored with multiple point and high-time-resolution ion velocity distribution observations from the Magnetospheric Multiscale mission. On 9 September 2015, reconnection took place at the magnetopause, which separated the magnetosheath and the magnetosphere with a density ratio of 25:2. The magnetic field intensity was rather constant, even higher in the asymptotic magnetosheath. The reconnected field line region had a width of approximately 540 km. In this region, streaming and gyrating ions are discriminated. The large extension of the reconnected field line region toward the magnetosheath can be identified where a thick layer of escaping magnetospheric ions was formed. The scale of the magnetosheath side of the reconnected field line region relative to the scale of its magnetospheric side was 4.5:1.
机译:通过对磁层多尺度任务的多点和高分辨率的离子速度分布观测,探索了不对称的更年期重新连接的结构。 2015年9月9日,磁层顶重新连接,磁层与磁层之间的密度比为25:2。磁场强度是相当恒定的,在渐近的磁石场中甚至更高。重新连接的场线区域的宽度约为540 km。在该区域,区分了流态离子和回转离子。可以确定重新连接的场线区域朝向磁荒的大延伸,在该处形成了逃逸的磁层离子的厚层。重新连接的场线区域的磁石表面侧的比例相对于其磁层一侧的比例为4.5:1。

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