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火星电离层电子浓度昼夜变化特性研究

本站小编 Free考研考试/2022-01-03

张学习1,,
雷久侯1,,,
万卫星2,
钟嘉豪1
1. 中国科学技术大学 地球和空间科学学院, 合肥 230026
2. 中国科学院地质与地球物理研究所, 北京 100029

基金项目: 国家自然科学基金(41325017,41274157)资助


详细信息
作者简介: 张学习, 硕士研究生, 主要研究方向为电离层变化.E-mail:kerstudy@mail.ustc.edu.cn
通讯作者: 雷久侯, 教授, 主要研究方向包括电离层热层大气变化特性及其应用研究等.E-mail:leijh@ustc.edu.cn
中图分类号: P352

收稿日期:2018-02-12
修回日期:2018-03-26
上线日期:2018-08-05



An investigation on the variations of dayside and nightside electron densities of the Martian ionosphere

ZHANG XueXi1,,
LEI JiuHou1,,,
WAN WeiXing2,
ZHONG JiaHao1
1. School of Earth and Space Sciences, University of Science and Technology of China, Hefei 230026, China
2. Institute of Geology and Geophysics, Chinese Academy of Sciences, Beijing 100029, China


More Information
Corresponding author: LEI JiuHou,E-mail:leijh@ustc.edu.cn
MSC: P352

--> Received Date: 12 February 2018
Revised Date: 26 March 2018
Available Online: 05 August 2018


摘要
本文利用MAVEN卫星Langmuir Probe and Waves(LPW)仪器的在轨电子浓度探测数据,研究了火星电离层电子浓度随太阳天顶角(Solar Zenith Angle,SZA)的变化以及昼夜电子浓度变化的异同.基于2014年至2017年期间MAVEN的电子浓度数据,我们发现:在200 km以下,白天电离层电子浓度主要受光化学平衡控制,由于白天光电离过程使得昼夜电子浓度差异较大,此时电离层昼夜传输能影响到的最大范围约在SZA=110°;而在200 km以上,白天电离层受输运过程控制,此时昼夜电子浓度差别较小,电离层昼夜间电子浓度变化较为缓慢.通过研究MAVEN在deep-dip(低高度深入探测)期间的电子浓度数据,我们发现火星磁场会显著影响夜间200 km以下的电子浓度分布结构,强磁场中闭合磁力线对电子沉降过程的阻碍作用使得在夜间该区域的电子浓度小于相邻区域.同时,通过比较deep-dip期间昼夜电子浓度随高度的变化,发现夜间电子沉降作用的影响可能主要集中在160 km以下.
火星/
MAVEN/
电离层/
电子浓度/
太阳天顶角/
昼夜

In this study, electron density data from Langmuir Probe and Waves (LPW) instrument onboard MAVEN are used to investigate the variations of the Martian ionosphere with Solar Zenith Angle (SZA) and the day-night difference of electron density. By analyzing electron density data during 2014-2017, we found that, the photochemical process is more important than the transport process below 200 km, and the day-night plasma transport can affect the electron density at SZA < 110°. For the region above 200 km, the transport process can greatly affect the structure of the topside ionosphere, and the day-night difference of electron densities is much smaller than that below 200 km, and electron density decreases gradually with increasing SZA. In addition, we analyzed the electron density data during MAVEN's deep-dip campaigns. It was found that the strong geomagnetic fields in the southern hemisphere could affect the electron density at night. The closed geomagnetic lines might obstruct the electron precipitating process and cause a decrease in electron density as compared with surrounding regions. By comparing the electron density profiles during the deep-dip campaigns, it was found that the precipitation electrons probably affect the electron density below 160 km at night.
Mars/
MAVEN/
Ionosphere/
Electron density/
Solar zenith angle/
Day-night



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http://www.geophy.cn/data/article/export-pdf?id=dqwlxb_14616
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