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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:强烈地磁风暴期间和之后,辐射带超相对论电子的俯仰角分布的变化:Van Allen Probes观测

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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:分析了十五个月的俯仰角解析Van Allen Probes相对论电子质子望远镜(REPT)对差分电子通量的测量结果,以研究暴风雨条件下以及在暴雨期间辐射带超相对论(> 2 MeV)电子的俯仰角分布的特征变异性。暴风雨后的长期衰减。通过将超相对论电子俯仰角分布建模为sin〜nα,其中α是赤道俯仰角,我们研究了n值的时空变化。结果表明,通常,n值随地磁活动水平的增加而增加。原则上,超相对论电子通过在90°俯仰角处达到更大的峰值来响应地磁风暴,n值为2-3,这是等离子层外合唱加速的支持信号。高n值也存在于等离子层内部,位于等离子休止区附近并表现出能量依赖性,这表明电磁离子回旋加速器(EMIC)波散射有重要贡献。在安静期间,n值通常会变小,即为0-1。地磁暴过后,超相对论电子缓慢而长期地衰变,尽管突出,但与太阳和地磁活动以及波粒相互作用过程相关,产生了能量和L壳相关的衰变时间尺度。在等离子层内部较低的L壳层处,电子在REPT能量下的衰减时间尺度τ_d通常较大,从数十天到数百天不等,这主要归因于嘶嘶声引起的俯仰角散射和向内的综合作用。径向扩散。当L shell增加到L〜3.5时,将存在一个狭窄区域(宽度约为0.5 L),在该区域中观察到的超相对论电子衰减最快,这可能是由于有效的EMIC波散射所致。随着L壳层继续增加,τ_d通常会再次变大,表明高L壳层处的波浪总体上使损失过程变慢。我们基于sin〜nα函数拟合和衰减时间尺度估计的研究提供了一种方便而有用的手段,来评估在推动超相对论电子的加速和损失中起作用的基础物理过程,并评估其相对贡献。

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