Inner Radiation Belt Simulations of the Proton Flux Response in the South Atlantic Anomaly during the Geomagnetic Storm of 15 May 2005

IF 4.3 3区 材料科学 Q1 ENGINEERING, ELECTRICAL & ELECTRONIC
Kirolosse M. Girgis, T. Hada, S. Matsukiyo, A. Yoshikawa
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引用次数: 2

Abstract

A test particle simulation code was developed to simulate the inner proton belt response during the intense geomagnetic storm of 15 May 2005. The guiding center model was implemented to compute the proton trajectories with an energy range of 70–180 MeV. The time-varying magnetic field model implemented in the simulations was computed by the Tsyganenko model TS05 with the associated inductive electric field. One of the most important features of the low-earth orbit (LEO) environment is the South Atlantic Anomaly, which imposes a dangerous radiation load on most LEO missions. This research aims to investigate the proton flux variations in the anomaly region with respect to space weather conditions. The results showed that during the main phase of the geomagnetic storm, the proton flux in the SAA decreased, whereas, throughout the initial and recovery phases, the proton flux was increased at most of the altitudes. Satellite measurements confirmed numerical results.
2005年5月15日地磁风暴期间南大西洋异常质子通量响应的内辐射带模拟
开发了一个测试粒子模拟程序,以模拟2005年5月15日强烈地磁暴期间的内部质子带响应。实现了引导中心模型来计算能量范围为70–180 MeV的质子轨迹。仿真中实现的时变磁场模型由Tsyganenko模型TS05和相关的感应电场计算。近地轨道环境最重要的特征之一是南大西洋异常,它给大多数近地轨道任务带来了危险的辐射负荷。本研究旨在研究异常区域的质子通量随空间天气条件的变化。结果表明,在地磁暴的主阶段,SAA中的质子通量减少,而在整个初始和恢复阶段,大部分海拔高度的质子通量增加。卫星测量证实了数值结果。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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来源期刊
CiteScore
7.20
自引率
4.30%
发文量
567
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