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The MINIS Balloon Campaign: Duskside Relativistic Electron Precipitation.

机译:MINIS气球运动:黄昏边的相对论电子沉淀。

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摘要

The Earth's radiation belts are a dynamic population of highly-energetic (> MeV) electrons and ions trapped in the dipole geometry of the Earth's magnetic field . These particles can strongly influence atmospheric chemistry, satellite operations, human explorers, long distance communications and even the electrical grid. The belts are also the most accessible laboratory for study of the particle acceleration that we see taking place throughout the universe. This dissertation presents the results from the MINIS balloon campaign, a January 2005 effort to observe the loss of relativistic electrons from the belts through relativistic electron precipitation (REP). MINIS launched 6 balloon payloads equipped with X-ray spectrometers into high-altitude, high-latitude, long-duration flights. These flights took place during a dramatic series of solar activity that set off a -99 Dst geomagnetic storm. During the storm sudden commencement phase, three payloads measured bremsstrahlung X-rays from electrons hitting the top of the atmosphere, making MINIS the first multi-point measurement of relativistic electron precipitation. The observations took place at dusk local times, consistent with other high energy precipitation observations from single point balloons. Measuring the scale size and motions of the precipitation region as well as its energy and intensity allow improved measurement of the average loss rate as well as more tightly constraining the instantaneous loss rate from the belts. Scale sizes and motions can also be better tied to the physical structures in the belts which lead to these particle losses. During the MINIS observed precipitation, the scale size was at least 0.6 L (a unit of Earth radii when mapped to the magnetic equator) by 1 hour of magnetic local time, and expansion rates of the precipitation were well faster than the drift rate for ∼MeV electrons. The MINIS balloons also served as a proof of concept for a much larger balloon campaign that began in January 2013 and will continue at least until February 2014. That campaign, BARREL, and estimates of what it will observe as well as a possible satellite mission to observe REP are also detailed here.
机译:地球的辐射带是动态高能(> MeV)电子和离子的动态聚集体,它们被困在地球磁场的偶极子几何结构中。这些粒子会强烈影响大气化学,卫星运行,人类探索者,远距离通信甚至电网。这些带也是研究整个宇宙中发生的粒子加速度的最便捷的实验室。本文介绍了MINIS气球运动的结果,该运动是2005年1月进行的,目的是通过相对论电子沉淀(REP)观察带中相对论电子的损失。 MINIS向高空,高纬度,长途飞行发射了6个装有X射线光谱仪的气球有效载荷。这些飞行发生在一系列剧烈的太阳活动期间,引发了-99 Dst地磁风暴。在暴风雨的突然开始阶段,三个有效载荷测量了撞击到大气层顶部的电子发出的X致辐射X射线,使MINIS成为相对论性电子降水的第一个多点测量。这些观测是在当地黄昏进行的,这与从单点气球上进行的其他高能降水观测一致。测量沉淀区域的水垢大小和运动及其能量和强度,可以改进平均损失率的测量,并更加严格地限制传送带的瞬时损失率。鳞片的大小和运动也可以更好地与皮带中的物理结构联系在一起,从而导致这些颗粒损失。在MINIS观测到的降水过程中,在1小时的磁性局部时间中,水垢的大小至少为0.6 L(映射到磁赤道时的地球半径的单位),并且降水的膨胀速率远快于漂移速率〜 MeV电子。 MINIS气球还作为2013年1月开始并至少持续到2014年2月的更大气球运动的概念验证。该运动BARREL及其观测结果的估计以及可能的卫星任务观察REP也在这里详细说明。

著录项

  • 作者

    Sample, John Glen.;

  • 作者单位

    University of California, Berkeley.;

  • 授予单位 University of California, Berkeley.;
  • 学科 Physics General.;Physics Radiation.
  • 学位 Ph.D.
  • 年度 2013
  • 页码 150 p.
  • 总页数 150
  • 原文格式 PDF
  • 正文语种 eng
  • 中图分类
  • 关键词

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