磁层赤道质量密度峰的形成是由地源波触发的

IF 2.9 3区 地球科学
ZuXiang Xue, ZhiGang Yuan, XiongDong Yu, Huang ShiYong, Zheng Qiao
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引用次数: 4

摘要

我们报告了范艾伦探测器任务同时观测到的两波段电磁离子回旋波和环形alfvsamn波。通过波频分析,发现质量密度ρ在磁赤道处局部达到峰值。离子的垂直通量(<100 eV)随着位向波的出现而同时增加,表明这些离子被位向波加热。此外,测量到的离子分布也支持赤道峰的形成,这与频率分析的结果一致。赤道处局部质量密度峰的形成应该是由于赤道离子浓度的增强,而赤道离子浓度的增强是由EMIC波对低能离子的垂直加热引起的。
本文章由计算机程序翻译,如有差异,请以英文原文为准。

Formation of the mass density peak at the magnetospheric equator triggered by EMIC waves

Formation of the mass density peak at the magnetospheric equator triggered by EMIC waves

We report a simultaneous observation of two band electromagnetic ion cyclotron (EMIC) waves and toroidal Alfvén waves by the Van Allen Probe mission. Through wave frequency analyses, the mass density ρ is found to be locally peaked at the magnetic equator. Perpendicular fluxes of ions (< 100 eV) increase simultaneously with the appearances of EMIC waves, indicating a heating of these ions by EMIC waves. In addition, the measured ion distributions also support the equatorial peak formation, which accords with the result of the frequency analyses. The formation of local mass density peaks at the equator should be due to enhancements of equatorial ion concentrations, which are triggered by EMIC waves’ perpendicular heating on low energy ions.

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来源期刊
Earth and Planetary Physics
Earth and Planetary Physics GEOSCIENCES, MULTIDISCIPLINARY-
自引率
17.20%
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174
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