GSTDTAP  > 气候变化
DOI10.1002/2017GL076560
On the Diffusion Rates of Electron Bounce Resonant Scattering by Magnetosonic Waves
Maldonado, Armando A.; Chen, Lunjin
2018-04-28
发表期刊GEOPHYSICAL RESEARCH LETTERS
ISSN0094-8276
EISSN1944-8007
出版年2018
卷号45期号:8页码:3328-3337
文章类型Article
语种英语
国家USA
英文摘要

Magnetosonic waves have been demonstrated as effective for bounce resonant scattering. Electron scattering rates due to bounce resonance interaction with magnetosonic waves are derived in a general form, where the effects of the finite Larmor radius, of violation in the first adiabatic invariant, and of latitudinal wave power distribution are considered. Such bounce resonance diffusion coefficients are important, but missing, from radiation belt modeling. Additionally, we provide a parametric study on the electron energy and equatorial pitch angle, magnetosonic wave, and background parameters to identify the factors that determine effective bounce resonant scattering.


Plain Language Summary Energetic particles, like electrons, emitted from the Sun become trapped in the Earth's magnetic field and form a complicated system of plasma currents known as the magnetosphere. Electrons in the magnetosphere move in ways that are difficult to model. Understanding the behavior of energetic particles in the plasma of the magnetosphere is important for planning both manned, and unmanned, space missions. Typically, there are many waves and particles in the magnetosphere, so identifying and studying each interaction makes modeling a complete magnetosphere possible. Magnetosonic waves are plasma waves that disturb electrons in ways that previous theories could not predict, but data have always shown. In this study, we use our own model to look at the spread of many electrons, bouncing along the magnetic field lines, after encountering multiple magnetosonic waves. It was found that considering the radius of the gyration of the particle and a realistic geometry of the wave are important to the outcome of the interaction. The spread of the particles is called diffusion and can be used in larger-scale models to better predict the dynamics of the magnetosphere as a tool to help plan future space missions.


领域气候变化
收录类别SCI-E
WOS记录号WOS:000435745500003
WOS关键词FREQUENCY ; MAGNETOSPHERE ; NOISE
WOS类目Geosciences, Multidisciplinary
WOS研究方向Geology
引用统计
文献类型期刊论文
条目标识符http://119.78.100.173/C666/handle/2XK7JSWQ/26337
专题气候变化
作者单位Univ Texas Dallas, Dept Phys, Richardson, TX 75083 USA
推荐引用方式
GB/T 7714
Maldonado, Armando A.,Chen, Lunjin. On the Diffusion Rates of Electron Bounce Resonant Scattering by Magnetosonic Waves[J]. GEOPHYSICAL RESEARCH LETTERS,2018,45(8):3328-3337.
APA Maldonado, Armando A.,&Chen, Lunjin.(2018).On the Diffusion Rates of Electron Bounce Resonant Scattering by Magnetosonic Waves.GEOPHYSICAL RESEARCH LETTERS,45(8),3328-3337.
MLA Maldonado, Armando A.,et al."On the Diffusion Rates of Electron Bounce Resonant Scattering by Magnetosonic Waves".GEOPHYSICAL RESEARCH LETTERS 45.8(2018):3328-3337.
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