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首页> 外文期刊>Journal of Geophysical Research, A. Space Physics: JGR >Evolution of relativistic outer belt electrons during an extended quiescent period
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Evolution of relativistic outer belt electrons during an extended quiescent period

机译:相对论外带电子的进化在静止期延长

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To effectively study loss due to hiss-driven precipitation of relativistic electrons in the outer radiation belt, it is useful to isolate this loss by studying a time of relatively quiet geomagnetic activity. We present a case of initial enhancement and slow, steady decay of 700 keV–2 MeV electron populations in the outer radiation belt during an extended quiescent period from ~15 December 2012 to 13 January 2013. We incorporate particle measurements from a constellation of satellites, including the Colorado Student Space Weather Experiment (CSSWE) CubeSat, the Van Allen Probes twin spacecraft, and Time History of Events and Macroscale Interactions during Substorms (THEMIS), to understand the evolution of the electron populations across pitch angle and energy. Additional data from calculated phase space density, as well as hiss and chorus wave data from Van Allen Probes, help complete the picture of the slow precipitation loss of relativistic electrons during a quiet time. Electron loss to the atmosphere during this event is quantified through use of the Loss Index Method, utilizing CSSWE measurements at low Earth orbit. By comparing these results against equatorial Van Allen Probes electron flux data, we conclude the net precipitation loss of the outer radiation belt content to be greater than 92%, suggesting no significant acceleration during this period, and resulting in faster electron loss rates than have previously been reported.
机译:有效地研究由于hiss-driven损失降水的相对论性电子外辐射带,它是有用的孤立这损失通过研究一个相对平静的时期地磁活动。700年的最初的增强和缓慢、稳定的衰变keV-2兆电子伏在外层电子的数量在一个扩展的静止辐射带从2013年1月~ 2012年12月15日到13。我们将粒子测量的卫星星座,包括科罗拉多学生空间天气实验(CSSWE)立方体卫星,范艾伦辐射探测器两航天器,和时间的历史事件和宏观尺度交互在亚暴(裁判)了解电子的发展人口在螺旋角和能量。额外的数据计算相空间密度,以及嘶嘶声和合唱波数据从范艾伦辐射探测器,帮助完成这幅画相对论的缓慢沉淀损失电子在一个安静的时间。在这事件是量化的氛围通过使用损失指数的方法,利用在低地球轨道CSSWE测量。比较这些结果对赤道艾伦探测电子通量数据,我们得出这样的结论净的沉淀损失外辐射带含量大于92%,暗示没有明显的加速度在此期间,和亏损率比电子的速度更快曾被报道。

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