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Occurrence frequency and location of magnetic islands at the dayside magnetopause

机译:发生频率和磁场的位置岛屿的光面的磁层

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摘要

Simulations of magnetic reconnection often predict the formation of magnetic islands forming and propagating out through the reconnection exhaust region. However, to date, only a few observations of magnetic islands at the Earth's magnetopause have been identified and analyzed. Crossings near reconnection sites at the dayside magnetopause by Cluster from 2001 to 2009 are examined in a systematic effort to determine the frequency and location of magnetic islands. Using the maximum magnetic shear model as a guide for the distance to the reconnection site, 47 magnetopause crossings within 3 RE of the predicted reconnection site are examined. The occurrence of island structures in the reconnection exhaust is investigated in the context of how the type of reconnection, antiparallel or component, affects the frequency of formation of the islands. For Cluster magnetopause crossings confirmed to be near reconnection sites, island signatures, primarily bidirectional streaming electrons in the magnetosheath boundary layer, are seen for approximately 85% of the crossings and are common features for both antiparallel and component reconnection.
机译:磁场重联的模拟预测磁岛形成和的形成通过重新连接排气传播出去地区。磁岛的地球的磁层已确定和分析。重新连接站点的光面的磁层集群中检查从2001年到2009年系统的努力确定频率和磁岛的位置。距离磁剪切模型作为指导重新连接网站,47个磁层口岸在3的预测重新连接站点。在重新连接排气岛结构调查的背景下如何的类型重新连接,反平行的或组件,影响的频率形成的岛屿。集群磁层交叉确认重新连接网站,岛附近签名,主要是双向流电子磁鞘边界层,看到大约85%的过境点,是常见的反平行的和组件的特性重新连接。

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