2017 年 9 月 7-8 日地磁风暴期间粒子注入对环流发展的影响

C. Ferradas, M.-C. Fok, N. Maruyama, M. G. Henderson, S. Califf, S. A. Thaller, B. T. Kress
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引用次数: 0

摘要

在本研究中,我们通过在利用内磁层-电离层综合模型对环流进行数值模拟时应用时空变化的数据驱动外边界条件,研究了粒子注入对 2017 年 9 月 7-8 日地磁风暴期间环流发展的作用。我们通过比较两个模拟运行的结果来量化粒子注入的作用:一个是由原始时间间隔(即 1.5 分钟)的测量结果定义的模型外部边界条件,另一个是用 2 小时的运行平均窗口对同一边界条件进行时间平滑。这两次运行的比较结果表明,观测到的粒子注入显著增强了电场,对环流的发展产生了重大影响,即:1)增强了环流;2)使环流分布向黎明方向倾斜;3)通过延长部分环流的持续时间推迟了对称环流的形成;4)在内侧边缘造成了以 O+为主的 O+-更丰富的环流分布。此外,这些效应通过环流离子的加热增强了质球和电离层的能量沉积。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
The effects of particle injections on the ring current development during the 7-8 September 2017 geomagnetic storm
In this study we investigate the role of particle injections on the ring current development during the 7-8 September 2017 geomagnetic storm by applying a temporally and spatially varying data-driven outer boundary condition in numerical simulations of the ring current with the Comprehensive Inner Magnetosphere-Ionosphere model. We quantify the role of particle injections by comparing the results from two simulation runs: one with the model outer boundary condition defined by measurements at their original time cadence, namely, 1.5 min, and one with the same boundary condition smoothed in time with a 2-h running average window. The comparison between these two runs reveals that the observed particle injections enhanced the electric field remarkably, which had a significant effect on the ring current development, namely, they 1) strengthened the ring current, 2) skewed the ring current distribution dawnward, 3) delayed the formation of the symmetric ring current by prolonging the duration of the partial ring current, and 4) caused a O+-richer ring current with a O+ dominant ring current distribution at the inner edge. Furthermore, these effects enhanced the energy deposition to the plasmasphere and ionosphere via heating by the ring current ions.
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