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首页> 外文期刊>Journal of Geophysical Research, A. Space Physics: JGR >Statistical Analysis of Hiss Waves in Plasmaspheric Plumes Using Van Allen Probe Observations
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Statistical Analysis of Hiss Waves in Plasmaspheric Plumes Using Van Allen Probe Observations

机译:van Allen探针观测统计分析Plasmasbheric Plumes中的Hiss波

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Plasmaspheric hiss waves commonly observed in high-density regions in the Earth's magnetosphere are known to be one of the main contributors to the loss of radiation belt electrons. There has been a lot of effort to investigate the distributions of hiss waves in the plasmasphere, while relatively little attention has been given to those in the plasmaspheric plume. In this study, we present for the first time a statistical analysis of the occurrence and the spatial distribution of wave amplitudes and wave normal angles for hiss waves in plumes using Van Allen Probes observations during the period of October 2012 to December 2016. Statistical results show that a wide range of hiss wave amplitudes in plumes from a few picotesla to >100 pT is observed, but a modest (<20 pT) wave amplitude is more commonly observed regardless of geomagnetic activity in both the midnight-to-dawn and dusk sector. By contrast, stronger amplitude hiss occurs preferentially during geomagnetically active times in the dusk sector. The wave normal angles are distributed over a broad range from 0° to 90° with a bimodal distribution: a quasi-field-aligned population (<20°) with an occurrence rate of <60% and an oblique one (>50°) with a relative low occurrence rate of ?20%. Therefore, from a statistical point of view, we confirm that the hiss intensity (a few tens of picotesla) and field-aligned hiss wave adopted in previous simulation studies are a reasonable assumption but stress that the activity dependence of the wave amplitude should be considered.
机译:众所周知,在地球磁层的高密度区域中常见地观察到的熔化柱波浪是辐射带电子损失的主要贡献者之一。已经有很多努力调查鼠标在玻璃体中的发布波浪的分布,虽然对血浆中的羽毛中的那些人相对较少。在这项研究中,我们首次出现了使用范艾伦探针在2012年10月至2016年10月期间使用Van Allen探针观测的悬垂波振荡和波浪正常角度的统计分析和波浪幅度的空间分布。统计结果表明观察到从少数Picotesla到> 100pt的羽毛中的各种Hiss波浪振幅,但不管午夜到黎明和黄昏部门的地磁活动如何,更常见的(<20pt)波幅度。相比之下,在黄昏扇区的地磁活动时间期间优先发生更强的幅度。波动正常角度在0°至90°的宽范围内分布,双峰分布:拟域对齐的群体(<20°),发生率<60%,倾斜(> 50°)相对低发生的速率?20%。因此,从统计的角度来看,我们确认先前模拟研究中采用的嘶嘶声强度(几十个Picotesla)和现场对齐的Hiss波是合理的假设,但应考虑波振幅的活动依赖性。

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