2022 年 2 月连续地磁暴事件期间的内辐射带模拟

Space Weather Pub Date : 2024-07-01 DOI:10.1029/2023sw003789
Kirolosse M. Girgis, Tohru Hada, Akimasa Yoshikawa, S. Matsukiyo, Abraham C.‐L. Chian, Ezequiel Echer
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引用次数: 0

摘要

从 2022 年 1 月 29 日开始,一系列太阳爆发引发了 2022 年 2 月 3 日的中度地磁暴,随后又发生了另一场地磁暴。尽管无强度风暴对空间技术的影响通常很小,但 49 颗 Starlink 卫星中有 38 颗发生了轨道衰减,重新进入地球大气层。这些卫星的损失归因于大气阻力条件的增强。本研究利用我们的测试粒子模拟代码进行数值模拟,研究两次磁暴期间内辐射带的动态。我们的分析表明,从第一场磁暴的恢复阶段过渡到第二场磁暴的初始阶段期间,质子密度和通量都有所增加,这主要是由强烈的太阳风动压驱动的。此外,我们还评估了单次事件骤变(SEU)率,与最初的平静状态相比,它增加了 50%。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Inner Radiation Belt Simulations During the Successive Geomagnetic Storm Event of February 2022
Starting from 29 January 2022, a series of solar eruptions triggered a moderate geomagnetic storm on 3 February 2022, followed subsequently by another. Despite the typically minimal impact of unintense storms on space technology, 38 out of the 49 Starlink satellites underwent orbital decay, re‐entering Earth's atmosphere. These satellite losses were attributed to enhanced atmospheric drag conditions. This study employs numerical simulations, utilizing our test particle simulation code, to investigate the dynamics of the inner radiation belt during the two magnetic storms. Our analysis reveals an increase in proton density and fluxes during the transition from the recovery phase of the first storm to the initial phase of the second, primarily driven by intense solar wind dynamic pressure. Additionally, we assess Single Event Upset (SEU) rates, which exhibit a 50% increase in comparison to initial quiet conditions.
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