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Io's neutral clouds: From the atmosphere to the plasma torus.

机译:艾欧的中性云:从大气层到等离子环面。

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摘要

Since the discovery of sodium thirty years ago, observations of Io's neutral features have provided essential insight into understanding the relationship between the Io's atmosphere and the Io torus, a ring of plasma encircling Jupiter. In this thesis I use observations and models of lo's corona, extended neutral clouds, and fast sodium jet to probe the interactions between the atmosphere, torus, and neutral clouds.; A corona and neutral cloud model, based on the model of Wilson and Schneider (1999), has been developed to study neutral loss from Io. Neutrals are ejected from Io's exobase and their trajectories followed under the influence of gravity until lost into the plasma torus. I also developed description of the plasma torus based on Voyager and ground-based observations to accurately determine neutral lifetimes.; Mutual eclipsing events between Galilean satellites were used to measure the shape of lo's sodium corona, revealing a corona that is only approximately spherically symmetric around Io. I discovered a previously undetected asymmetry: the sub-Jupiter corona is denser than the anti-Jupiter corona. Modeling implies that sodium source from the sub-Jupiter hemisphere must be twice as large as from the anti-Jupiter hemisphere.; The Galileo spacecraft has imaged a remarkable atmospheric escape process occurring in Io's ionosphere. Electrodynamic consequences of Io's motion through Jupiter's magnetosphere drive mega-amp currents through lo's ionosphere; some sodium ions carrying this current are neutralized as they leave the atmosphere. The Galileo images show that the resulting fast sodium jet removes ∼5 × 1025 atoms sec−1 from Io's atmosphere. The source region of the jet is much smaller than Io itself implying that the ionosphere is densest near Io's equator.; A model-based comparison of the neutral oxygen and sodium clouds details differences in the morphologies and spatial extent of each: sodium extends only 1/4 the way around Jupiter while oxygen forms a complete torus. Sodium emission results from resonant scattering making it relatively easy to determine sodium abundance. The oxygen intensity is highly dependent on the highly variable plasma torus. This complicates the analysis of oxygen observations since the nature and magnitude of plasma variations has not been well characterized.
机译:自从三十年前发现钠以来,对艾欧中性特征的观察已为理解艾欧大气和艾欧环面(环绕木星的等离子环)之间的关系提供了重要的见识。在本文中,我将使用lo的电晕,扩展的中性云和快速的钠射流的观测和模型来探测大气,环面和中性云之间的相互作用。已经研究了基于Wilson和Schneider(1999)模型的电晕和中性云模型来研究Io的中性损失。中性粒子从Io的外基中弹出,其轨迹在重力作用下跟随,直到丢失到等离子体圆环中。我还基于Voyager和地面观测结果开发了对等离子体圆环的描述,以准确确定中性寿命。伽利略卫星之间的相互食蚀事件用于测量lo's钠电晕的形状,揭示出电晕仅在Io附近呈球形对称。我发现了以前未发现的不对称性:亚木星电晕比反木星电晕更密。模拟表明,来自木星半球的钠源必须是来自反木星半球的钠源的两倍。伽利略号航天器对艾奥电离层中发生的异常大气逃逸过程进行了成像。 Io在木星磁层中运动的电动力结果驱动兆安级电流流经lo的电离层。一些载有该电流的钠离子在离开大气层时被中和。伽利略图像显示,由此产生的快速钠射流从艾奥大气中去除了约5×10 25 sec -1 个原子。射流的源区比Io本身小得多,这意味着电离层在Io的赤道附近最密集。基于模型的中性氧气云和钠云的比较详细说明了每种云的形态和空间范围的差异:钠仅在木星周围延伸1/4,而氧气形成完整的圆环。钠的发射是由共振散射引起的,因此相对容易确定钠的丰度。氧强度高度依赖于高度可变的等离子体圆环。由于等离子体变化的性质和大小尚未得到很好的表征,这使氧观测的分析变得复杂。

著录项

  • 作者

    Burger, Matthew Howard.;

  • 作者单位

    University of Colorado at Boulder.;

  • 授予单位 University of Colorado at Boulder.;
  • 学科 Physics Astronomy and Astrophysics.
  • 学位 Ph.D.
  • 年度 2003
  • 页码 207 p.
  • 总页数 207
  • 原文格式 PDF
  • 正文语种 eng
  • 中图分类 天文学 ;
  • 关键词

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