首页> 外文期刊>Journal of Geophysical Research, A. Space Physics: JGR >Observations of dipolarization at geosynchronous orbits and its response in the polar cap convection during extreme southward interplanetary magnetic field conditions
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Observations of dipolarization at geosynchronous orbits and its response in the polar cap convection during extreme southward interplanetary magnetic field conditions

机译:在极端南向行星际磁场条件下,地球同步轨道上的双极化现象及其在极盖对流中的响应

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摘要

Analysis of the polar cap convection and geosynchronous magnetic field measurements, in the context of dipolarization events, during extreme southward interplanetary magnetic field (IMF) conditions is presented in the paper. Clear dipolarization events at geosynchronous orbits are always followed by an increase in the polar cap convection with a time delay. The distribution of the time delay between the onset of dipolarization at geosynchronous orbit and polar cap convection response varied between 6 and 15 min with an average of 9 min. The polar cap convection response to the dipolarization events enabled the deduction of the dipolarization timescales at geosynchronous orbits and in the ionosphere. A comparison of these two timescales revealed that the timescales of dipolarization events deduced from geosynchronous magnetic field measurements were always shorter (average 11 min) than the timescales deduced from the polar cap convection measurements (average 33 min).
机译:本文介绍了在极地南极星际磁场(IMF)情况下,在双极化事件的背景下对极帽对流和地球同步磁场测量的分析。在地球同步轨道上发生清晰的双极化事件之后,总是会随着时间的推移增加极盖对流。在地球同步轨道上的双极化开始和极顶对流响应之间的时间延迟分布在6至15分钟之间变化,平均为9分钟。极顶对流对偶极子事件的响应使得能够推论地球同步轨道和电离层中偶极子的时标。这两个时间尺度的比较显示,从地球同步磁场测量得出的双极化事件的时间尺度(平均11分钟)总是比从极地对流对流测量得出的时间尺度(平均33分钟)短。

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