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Propagating disturbances in the lower solar corona.

机译:在较低的日冕中传播的干扰。

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摘要

TRACE observations allow us to see propagating coronal waves in multiple narrowband filters and with high spatiotemporal resolution. I analyze four wave-front propagations observed in TRACE, in particular an event from 13 June 1998. Studying morphology and dynamics, I conclude observationally that three of the four fronts are fast-mode MHD waves.; Having developed new mapping algorithms, I automate the tracking of waves with bright fronts by finding reproducible fronts, natural trajectories, and fastmode velocities in large regions of the quiet corona. I use this automated method to examine the 13 June 1998 event in detail, and determine density and flux changes along several propagation tracks. Various properties of the front—density, amplitude, flux—are found to increase through much of its lifetime, and when these properties stabilize, it experiences almost no dispersion. This suggests that the wave is traveling through a dispersionless medium.; Through comparison of EUV passbands, I am able to place altitude and temperature constraints on the 13 June 1998 event, and show that the front moves only through the lowest part of the corona, trapped in a wave guide. This analysis is reinforced analytically, by considering a propagating MHD wave in a hydrostatic atmosphere, and through existing theories.; Conclusions offer explanations for the dearth of soft x-ray observations of propagating waves, as well as the seeming uniformity of EUV events. In light of the above-mentioned propagation constraints, I address the usefulness of such waves in coronal seismology. Finally, I discuss how seemingly contradictory theories are merely disparate descriptions of the same kind of event.*; *This dissertation is compound (contains both a paper copy and CD as part of the dissertation). The CD requires the following system applications: QuickTime; Windows MediaPlayer or RealPlayer.
机译:TRACE观测使我们能够在多个窄带滤光片中以高时空分辨率看到正在传播的日冕波。我分析了在TRACE中观测到的四个波前传播,特别是1998年6月13日的事件。研究形态和动力学时,我得出结论,四个前沿中的三个是快速模式MHD波。开发了新的映射算法后,我通过在安静电晕的大部分区域中找到可重现的前沿,自然轨迹和快速模式速度来自动跟踪具有明亮前沿的波。我使用这种自动方法来详细研究1998年6月13日的事件,并确定沿几个传播轨道的密度和通量变化。发现前面板的各种特性(密度,振幅,通量)在其整个使用寿命中都会增加,并且当这些特性稳定时,几乎不会出现分散。这表明波正在传播通过无色散介质。通过对EUV通带的比较,我能够对1998年6月13日的事件设置高度和温度限制,并表明前部仅移动通过电晕的最低部分,并被困在波导中。通过考虑在静水压力下传播的MHD波并通过现有理论,从分析上加强了这一分析。结论为缺乏传播波的软X射线观测以及EUV事件的表面均匀性提供了解释。鉴于上述传播限制,我讨论了此类波在日冕地震学中的有用性。最后,我讨论了看似矛盾的理论如何仅仅是对同一事件的不同描述。 *本论文是复合的(论文包含纸质副本和CD)。该CD需要以下系统应用程序:QuickTime; Windows MediaPlayer或RealPlayer。

著录项

  • 作者单位

    Montana State University.;

  • 授予单位 Montana State University.;
  • 学科 Physics Fluid and Plasma.; Physics Astronomy and Astrophysics.
  • 学位 Ph.D.
  • 年度 2003
  • 页码 p.3880
  • 总页数 168
  • 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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