The Impact of the 8–10 March 2012 Geomagnetic Storm on Inner Zone Protons as Measured by Van Allen Probes

IF 2.6 2区 地球科学 Q2 ASTRONOMY & ASTROPHYSICS
Zhao Li, Miles Engel, Mary Hudson, Brian Kress, Maulik Patel, Richard Selesnick
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Abstract

The Relativistic Electron Proton Telescope (REPT) instrument on the Van Allen Probes observed a double-peaked inner zone proton population throughout the 7 year lifetime of the mission. M. Hudson et al. (2023) showed that a strong SEP event accompanied by a CME-shock in early March 2012 provided the Solar Energetic Proton (SEP) source for the higher L trapped proton population, which then diffused radially inward to be observed by REPT at L = 2 $L=2$ . The study followed trajectories of SEP protons launched isotropically from a sphere at 7 Re for 2.5 hr in fields calculated by the LFM-RCM global MHD model, which includes electric fields needed to model the transport and trapping of the protons by the shock, and then a radial diffusion simulation was run for 2 years using the result from the test-particle simulation as the initial condition. The simulation result was compared with REPT measurement in November 2013 and showed reasonable agreement. However, the simulation overestimated the Phase Space Density by a factor of four due to lack of field line curvature scattering during the storm in the model. In this study, a test-particle simulation is performed for 2 days following the injection and trapping of protons in March 2012 using TS05 fields to simulate the field line curvature scattering of the trapped SEP due to the buildup of the ring current during the geomagnetic storm. The resulting sample distribution was then weighted using the flux at the end of the two-hour MHD-test particle simulation. A radial diffusion simulation is then run using the initial profile that included the loss effect, with improved comparison with REPT measurements after 2 years.

范艾伦探测器测量到的 2012 年 3 月 8-10 日地磁风暴对内层质子的影响
范艾伦探测器上的相对论电子质子望远镜(REPT)仪器在 7 年的飞行任务期间观测到了双峰内区质子群。M. Hudson 等人(2023 年)的研究表明,2012 年 3 月初伴随着一次 CME 冲击的强 SEP 事件为较高 L 值的被困质子群提供了太阳高能质子(SEP)源,然后质子群径向向内扩散,在 L = 2 $L=2$ 时被 REPT 观测到。这项研究在 LFM-RCM 全局 MHD 模型计算的场中,对从 7 Re 的球体等向发射的 SEP 质子轨迹进行了 2.5 小时的跟踪,其中包括模拟冲击对质子的传输和捕获所需的电场,然后以测试粒子模拟的结果为初始条件,进行了为期 2 年的径向扩散模拟。模拟结果与 2013 年 11 月的 REPT 测量结果进行了比较,结果显示两者吻合。然而,由于模型中缺乏风暴期间的场线曲率散射,模拟结果将相空间密度高估了四倍。在本研究中,利用 TS05 磁场对 2012 年 3 月质子注入和捕获后的 2 天进行了测试粒子模拟,以模拟地磁暴期间环流积聚导致的被捕获的 SEP 的场线曲率散射。然后,利用两小时 MHD 测试粒子模拟结束时的通量对所得样本分布进行加权。然后使用包含损耗效应的初始剖面进行径向扩散模拟,并与两年后的 REPT 测量结果进行改进比较。
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
Journal of Geophysical Research: Space Physics
Journal of Geophysical Research: Space Physics Earth and Planetary Sciences-Geophysics
CiteScore
5.30
自引率
35.70%
发文量
570
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