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Relativistic electron losses from the outer Van Allen Belts.

机译:范艾伦带外层的相对论电子损耗。

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摘要

Relativistic electron fluxes in Earth's Van Allen Belts can have severe consequences for space based assets. Much effort has been expended to understand the variability of these fluxes and their acceleration and loss mechanisms. For relativistic electrons in the outer radiation belt, the main loss mechanism appears to be precipitation to Earth's ionosphere although the leading form of this precipitation is still under debate. Relativistic electron microbursts have been studied extensively in the past and are clearly seen in the satellite data whereas duskside relativistic electron precipitation events are not as visible in the satellite data but are the only form of relativistic precipitation seen in balloon data.;The focus of this dissertation is to compare balloon and satellite observations of relativistic electron precipitation, explain and correct the apparent deficit of high energy duskside relativistic electron precipitation events observed in satellite data, and reconcile this with what has been observed by balloons since the INTERBOA balloon mission in 1996. After a review of relevant background material covering the magnetosphere and the radiation belts, the SAMPEX mission is introduced and an analysis of data obtained from 1992 to 2004 is presented. 100 ms cadence data from the HILT detector on board SAMPEX is used to identify candidate events whose spectra are then analyzed by means of the lower time resolution count rates from the PET detector. The results of this analysis show that there exist a form of relativistic electron precipitation distinct from microbursts or bands and that this type of event primarily occurs on the dusk side. In addition to the above analysis, several case studies obtained from the SAMPEX data are presented to support this conclusion. Also presented is a review of the BARREL mission and results obtained to date. BARREL is currently in a development phase and has been conducting test flights since 2008 during which significant progress has been made on mission, payload and ground station design. Not enough events have been observed for a statistical comparison, however, as the science campaigns will not launch until December 2012 and Dec. 2013.
机译:范艾伦带地球​​上的相对论电子通量可能对太空资产产生严重影响。为了了解这些通量的可变性及其加速和损失机理,已经付出了很多努力。对于外部辐射带中的相对论电子,主要的损耗机制似乎是地球电离层的降水,尽管这种降水的主要形式仍在争论中。相对论电子微暴在过去已被广泛研究,并在卫星数据中清楚地看到,而黄昏相对论电子降水事件在卫星数据中并不明显,而是气球数据中唯一的相对论降水形式。这篇论文的目的是比较气球和卫星观测到的相对论电子降水,解释并纠正卫星数据中观测到的高能黄昏相对​​论电子降水事件的表观缺陷,并将其与自1996年INTERBOA气球观测以来气球观测到的相吻合。在回顾了覆盖磁层和辐射带的相关背景材料之后,进行了SAMPEX任务,并对1992年至2004年获得的数据进行了分析。来自SAMPEX板上HILT检测器的100 ms脚踏圈速数据用于识别候选事件,然后通过PET检测器的较低时间分辨率计数率分析其光谱。分析结果表明,存在相对论的电子沉淀形式,与微暴或微带不同,这种事件主要发生在黄昏一侧。除了上述分析之外,还提供了一些从SAMPEX数据获得的案例研究以支持这一结论。还介绍了BARREL任务的回顾和迄今获得的结果。 BARREL目前正处于开发阶段,自2008年以来一直在进行试飞,在此期间,任务,有效载荷和地面站设计取得了重大进展。但是,由于科学运动要到2012年12月和2013年12月才会启动,因此没有足够的事件进行统计比较。

著录项

  • 作者

    Comess, Max D.;

  • 作者单位

    University of California, Santa Cruz.;

  • 授予单位 University of California, Santa Cruz.;
  • 学科 Physics Astrophysics.
  • 学位 Ph.D.
  • 年度 2011
  • 页码 138 p.
  • 总页数 138
  • 原文格式 PDF
  • 正文语种 eng
  • 中图分类
  • 关键词

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