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Relativistic Electrons in Earth’s Outer Radiation Belt: Wave-Particle Interactions and Precipitation Loss

机译:地球外辐射带中的相对论电子:波粒相互作用和降水损失

摘要

Earthu27s outer radiation belt is a highly dynamic region of the magnetosphere composed of relativistic electrons with often unpredictable variations in energy and spatial extent. Understanding this variable radiation environment is critical for protecting both spacecraft and humans in space. A number of competing acceleration and loss processes combine to produce net enhancements or depletions of the outer radiation belt. Electron precipitation into the atmosphere is a critical part of this loss, and quantified understanding of this mechanism is needed in order to understand and ultimately predict radiation belt dynamics. In the following work, we investigate the contribution of electron precipitation to radiation belt losses, looking at what times precipitation is important and at how much loss it contributes. Through a combination of long-term existing data sets as well as new CubeSat measurements we perform both statistical and detailed event studies to better understand the nature and extent of MeV electron loss to the atmosphere. We analyze measurements of precipitating electrons directly as well as electromagnetic waves that may be causing this precipitation. Our studies provide a more cohesive picture of outer radiation belt dynamics and the relationship between precipitating energetic electrons and global magnetospheric conditions.
机译:地球的外部辐射带是磁层的一个高度动态区域,由相对论电子组成,其能量和空间范围的变化通常是不可预测的。了解这种可变的辐射环境对于保护航天器和太空中的人类至关重要。许多竞争性的加速和损耗过程相结合,产生了外部辐射带的净增强或损耗。电子向大气中的沉淀是这种损失的关键部分,因此需要对这种机理进行定量的了解,才能理解并最终预测辐射带的动力学。在接下来的工作中,我们研究了电子沉淀对辐射带损耗的贡献,研究了什么时候沉淀很重要以及它贡献了多少损耗。通过长期使用的现有数据集以及新的CubeSat测量值的组合,我们可以进行统计和详细的事件研究,以更好地了解MeV电子向大气损失的性质和程度。我们分析了直接沉淀电子的测量以及可能引起这种沉淀的电磁波。我们的研究为外部辐射带动力学以及沉淀的高能电子与整体磁层状况之间的关系提供了更加紧密的联系。

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    Blum Lauren Weber;

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  • 年度 2014
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