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The analysis and modeling of microburst electron precipitation using pitch-angle diffusion theory.

机译:利用节距角扩散理论对微爆电子沉淀进行分析和建模。

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摘要

This dissertation presents a study of the microburst electron precipitation, characterized by quasi-periodic bursty precipitation of electrons in the morningside auroral zone, with a typical duration of {dollar}sim{dollar}.2-.3 seconds. Most of the existing knowledge about this process came from the study of secondary effects like bremsstrahlung X-rays, with little information about the primary electrons which is necessary in order to comprehend the underlying physics. A Nike-BlackBrant V sounding rocket, designed to investigate this phenomenon, was launched on May 6, 1993, from the Poker Flat launching station, Fairbanks, Alaska. This experiment was the first to measure the microburst characteristics in detail, and to look at particles and waves simultaneously. This work was motivated by previously suggested correlation between microbursts and VLF wave activity.; As a starting point, this dissertation begins with a brief descript ion of the geomagnetic environment and a summary of the present knowledge about microbursts. The rocket instrumentation, launch conditions, and an overview of the acquired data are presented in the following chapters. The process of pitch-angle diffusion in the velocity space, due to the cyclotron resonance interaction between electrons and whistler waves, has been considered as a potential mechanism responsible for microbursts. The nature of this interaction is discussed, followed by numerical models developed in the framework of this theory.; We find that an enhancement in the diffusion coefficient D(t) can cause a microburst-like structure in particle precipitation. The microburst width is approximately equal to the quarter-bounce period {dollar}Tsb{lcub}B{rcub},{dollar} and is fairly insensitive to the duration of D(t). This result could possibly explain why microbursts have a characteristic width. Our simulation shows the rise time of the burst is proportional to {dollar}Tsb{lcub}B{rcub},{dollar} which agrees with the observed data. The variation of the shape of the burst can be explained as a consequence of different forms of D(t). We have also examined the possibility of self-induced wave growth. This wave enhancement was favored by a smaller value of total electron density {dollar}Nsb{lcub}e{rcub}{dollar} and a larger value of energetic electron density {dollar}Nsb{lcub}w{rcub}{dollar}, and was also found to be dependent on the length of the interaction region and electron energy. In summary, the pitch-angle diffusion process is suggested to be the primary mechanism behind the microburst electron precipitation.
机译:本文提出了一种微爆发电子沉淀的研究,其特征在于在晨光极光区中电子的准周期性的突发性沉淀,典型持续时间为{sim} {dollar} .2-3秒。关于该过程的大多数现有知识来自对of致辐射X射线等次要效应的研究,而对初级电子的了解很少,这对于理解基础物理学是必不可少的。 1993年5月6日,从阿拉斯加费尔班克斯的Poker Flat发射台发射了一枚旨在调查这种现象的Nike-BlackBrant V探空火箭。该实验是第一个详细测量微爆特征并同时观察粒子和波的实验。这项工作是由先前提出的微爆和VLF波活动之间的相关性所激发的。作为起点,本文从对地磁环境的简要描述和对微爆裂的当前知识的总结开始。以下各章介绍了火箭的仪表,发射条件以及所获取数据的概述。由于电子和啸叫波之间的回旋共振相互作用,速度空间中的俯仰角扩散过程被认为是引起微爆的潜在机制。讨论了这种相互作用的性质,然后讨论了在该理论框架内开发的数值模型。我们发现,扩散系数D(t)的增加会导致颗粒沉淀中的微爆状结构。微脉冲宽度大约等于四分之一弹跳周期{Tsb {lcb} B {rcub},{dollar},并且对D(t)的持续时间相当不敏感。该结果可能可以解释为什么微爆具有一定的宽度。我们的仿真显示,突发的上升时间与{Tsb} Tsb {lcub} B {rcub},{dollar}成正比,与观察到的数据一致。 D(t)不同形式的结果可以解释突发形状的变化。我们还研究了自激波增长的可能性。总电子密度{Nsb {lcub} e {rcub} {dollar}较小的值和高能电子密度{snolNsb {lcub} w {rcub} {dollar}的较大值有助于这种波增强,并且还发现其取决于相互作用区域的长度和电子能量。总之,节距角扩散过程被认为是微爆发电子沉淀的主要机理。

著录项

  • 作者

    Datta, Suvro.;

  • 作者单位

    University of Washington.;

  • 授予单位 University of Washington.;
  • 学科 Physics Fluid and Plasma.
  • 学位 Ph.D.
  • 年度 1995
  • 页码 107 p.
  • 总页数 107
  • 原文格式 PDF
  • 正文语种 eng
  • 中图分类 等离子体物理学;
  • 关键词

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