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The outer plasmasphere as a source of magnetospheric plasmas.

机译:外部等离子层是磁层等离子体的来源。

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摘要

In this dissertation, we consider the supply of outer plasmaspheric plasma to the magnetosphere by means of both global convection modeling and analysis of spacecraft measurements of low-energy ions. First, the convective evolution of the plasmasphere is studied using a dynamic global core plasma model (DGCPM) that includes the influences of spatially and temporally varying convection and refilling processes to calculate the equatorial core plasma density distribution throughout the inner magnetosphere and magnetopause boundary layer regions. An expression for the electric field structure within subauroral ion drift (SAID) features is developed based on observations. It is found that ionospheric subauroral ion drift type convection electric fields in the predusk to midnight sectors, when mapped to the ionosphere, lead to the formation of a density trough embedded in the plasmasphere, provided that the SAID electric field crosses the plasmapause. In a second investigation, a statistical study of brief intervals of cold dense plasma in the midnight sector is undertaken using data from the Los Alamos Magnetospheric Plasma Analyzer (MPA) onboard geosynchronous satellite. The analysis suggests that premidnight cold plasma encounters at geosynchronous orbit most likely arise through corotation-dominated transport of dayside plasmaspheric structures into the premidnight sector. In a third investigation, a model of electric and magnetic field structures in the outer dayside magnetospheric regions is incorporated into the DGCPM to examine the loss of plasmaspheric-origin plasma into the magnetopause boundary layer and the convection of this plasma that remains trapped on closed field lines. The model predicts that plasmaspheric plasma reaching the outer magnetosphere is diverted anti-sunward along the outer flanks of the magnetosphere. The calculated He{dollar}sp+{dollar} densities in the magnetospheric boundary layer regions are consistent with the limited number of observations of He{dollar}sp+{dollar} densities in that region.
机译:本文通过整体对流建模和航天器低能离子测量的分析,考虑了外层等离子向磁层的供应。首先,使用动态全局核心等离子体模型(DGCPM)研究了等离子体层的对流演化,该模型包括时空变化的对流和充填过程的影响,以计算整个内部磁层和磁层顶边界层区域的赤道核心等离子体密度分布。基于观察结果,开发了极光下离子漂移(SAID)功能内电场结构的表达式。发现如果映射到电离层,则在黄昏至午夜扇形区中的电离层极光下离子漂移型对流电场会形成嵌入电浆层的密度槽,前提是SAID电场穿过电浆暂停。在第二项调查中,利用地球同步卫星上的洛斯阿拉莫斯磁层等离子体分析仪(MPA)的数据,对午夜区域冷密集等离子体的短暂间隔进行了统计研究。分析表明,在地球同步轨道上发生的午夜冷等离子体很可能是由于白天等离子层结构向午夜扇形运动的同向运动所致。在第三项研究中,将日外磁层区域的电场和磁场结构模型纳入DGCPM中,以检查起源于磁层顶的边界层中等离子层血浆的损失以及该血浆在对流场中的对流线。该模型预测,到达外磁层的等离子层等离子体将沿着磁层的外侧面逆向偏转。在磁层边界层区域中计算的He {dollar} sp + {dollar}密度与该区域中He {dollar} sp + {dollar}密度的有限观测值一致。

著录项

  • 作者

    Ober, Daniel Michael.;

  • 作者单位

    The University of Alabama in Huntsville.;

  • 授予单位 The University of Alabama in Huntsville.;
  • 学科 Physics Fluid and Plasma.; Geophysics.
  • 学位 Ph.D.
  • 年度 1997
  • 页码 154 p.
  • 总页数 154
  • 原文格式 PDF
  • 正文语种 eng
  • 中图分类 等离子体物理学;地球物理学;
  • 关键词

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