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首页> 外文期刊>Journal of Geophysical Research, A. Space Physics: JGR >Variability of the pitch angle distribution of radiation belt ultrarelativistic electrons during and following intense geomagnetic storms: Van Allen Probes observations
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Variability of the pitch angle distribution of radiation belt ultrarelativistic electrons during and following intense geomagnetic storms: Van Allen Probes observations

机译:的螺旋角分布的变化在辐射带ultrarelativistic电子和强烈的磁暴:货车艾伦探针观察

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摘要

Fifteen months of pitch angle resolved Van Allen Probes Relativistic Electron-Proton Telescope (REPT) measurements of differential electron flux are analyzed to investigate the characteristic variability of the pitch angle distribution of radiation belt ultrarelativistic (>2 MeV) electrons during storm conditions and during the long-term poststorm decay. By modeling the ultrarelativistic electron pitch angle distribution as sin ~nα, where α is the equatorial pitch angle, we examine the spatiotemporal variations of the n value. The results show that, in general, n values increase with the level of geomagnetic activity. In principle, ultrarelativistic electrons respond to geomagnetic storms by becoming more peaked at 90° pitch angle with n values of 2–3 as a supportive signature of chorus acceleration outside the plasmasphere. High n values also exist inside the plasmasphere, being localized adjacent to the plasmapause and exhibiting energy dependence, which suggests a significant contribution from electromagnetic ion cyclotron (EMIC) wave scattering. During quiet periods, n values generally evolve to become small, i.e., 0–1. The slow and long-term decays of the ultrarelativistic electrons after geomagnetic storms, while prominent, produce energy and L-shell-dependent decay time scales in association with the solar and geomagnetic activity and wave-particle interaction processes. At lower L shells inside the plasmasphere, the decay time scales τ_d for electrons at REPT energies are generally larger, varying from tens of days to hundreds of days, which can be mainly attributed to the combined effect of hiss-induced pitch angle scattering and inward radial diffusion. As L shell increases to L~3.5, a narrow region exists (with a width of ~0.5 L), where the observed ultrarelativistic electrons decay fastest, possibly resulting from efficient EMIC wave scattering. As L shell continues to increase, τ_d generally becomes larger again, indicating an overall slower loss process by waves at high L shells. Our investigation based upon the sin~nα function fitting and the estimate of decay time scale offers a convenient and useful means to evaluate the underlying physical processes that play a role in driving the acceleration and loss of ultrarelativistic electrons and to assess their relative contributions.
机译:15个月的螺旋角范艾伦解决探讨相对论Electron-Proton望远镜(报告)的测量微分电子通量分析了调查的特点的螺旋角分布的变化辐射带ultrarelativistic(> 2兆电子伏)电子在风暴条件和期间长期poststorm衰变。ultrarelativistic电子螺旋角分配罪~ nα,α赤道螺旋角,我们检查n值的时空变化。结果表明,在一般情况下,n值增加与地磁活动的水平。原则,ultrarelativistic电子回应地磁风暴越来越达到90°螺旋角与n值2 - 3的支持签名以外的合唱加速度等离子体层。等离子体层,本地化毗邻等离子体层顶和展出能源依赖,这意味着一个重大贡献的电磁离子回旋波位的散射。通常会演变成小,即0 - 1。缓慢而长期的衰变ultrarelativistic电子在地磁风暴,而突出,产生能量L-shell-dependent衰变时间尺度与太阳和地磁活动和波粒相互作用过程。在较低L壳内等离子体层,衰减时间尺度τ_d电子报告从数万能量通常较大,不同天的天,可以主要归因于hiss-induced的综合效应螺旋角散射和内径向扩散。狭窄的区域存在(~ 0.5 L的宽度),观察ultrarelativistic电子在哪里衰减最快,可能产生的效率位的波散射。增加,τ_d一般再次变大,指示一个总体损失过程慢波高L贝壳。在罪~ nα函数拟合和预测的衰变时间尺度提供了方便评估底层物理有用的手段在驾驶过程中发挥作用加速度和ultrarelativistic损失电子和评估其相对的的贡献。

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