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Influences of IMF By Polarity on Dayside Electron Precipitation in Terms of Energy Channels

机译:国际货币基金组织(IMF)的影响通过极性的光面电子降水的能源通道

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The B_y component of the interplanetary magnetic field (IMF) has long been suggested to play a crucial role in modulating precipitating electrons that create the dayside aurora. However, the effects of the By polarity on dayside precipitating electrons have never been examined in terms of energy channels. The present study statistically analyzes these effects using number fluxes of four energy channels. Our results show that the flux response of the dayside electron precipitation to the B_y polarity is not fixed in different energy channels. We infer that the response in the energy range of 688–1,000 eV is associated with interhemispheric field-aligned currents, while the response in the energy range of 154–224 eV is likely related to the direct entry of magnetosheath electrons via antiparallel reconnection. In addition, local time distributions of precipitating electrons reveal two types of preexisting hemispheric asymmetry regardless of the By polarities. The first (second) type, which appears in the 06–12 magnetic local time (MLT) (12–18 MLT) sector, indicates higher (lower) flux in the Southern Hemisphere than in the Northern Hemisphere. All of the present results improve our understanding at the dayside aurora and the IMF By effects on it, which would not have been retrieved without the use of individual energy channels.
机译:行星际磁场的的话分量字段(IMF)长期以来一直建议发挥至关重要的作用在调节沉淀电子创建的光面极光。然而,通过极性的影响从来没有的光面沉淀电子检查能源通道。研究统计分析这些影响使用通量数量四个能源通道。结果表明,该反应的通量的光面电子降水的话极性并不固定在不同的能量频道。能源范围688 - 1000 eV是相关联的两半球间的field-aligned电流,响应的能量范围154 - 224 eV可能相关的直接入口磁鞘电子通过反平行的重新连接。分布的沉淀电子显示两种类型的既存的半球不对称不管极性。(二)类型,它发表在《06-12磁(MLT)当地时间(12 - 18 MLT)部门,表明高(低)通量在南部比北半球的半球。改善我们的理解的结果在的光面极光和国际货币基金组织的影响,就不会没有检索使用个人的能源通道。

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  • 来源
    《Journal of Geophysical Research, A. Space Physics: JGR》 |2022年第3期|2021JA030082-1-2021JA030082-16|共16页
  • 作者单位

    Department of Space Science and Engineering, National Central University, Taoyuan, Taiwan;

    School of Physics and Astronomy, University of Minnesota, Minneapolis, MN, USA;

    State Key Laboratory of Marine Geology, School of Ocean and Earth Science, Tongji University, Shanghai, China;

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