地磁扰动期间热层大气N_2数密度异常增变
The abnormal variation of N_2 number density in thermosphere during geomagnetic disturbance
查看参考文献13篇
文摘
|
采用天宫一号轨道大气环境探测器的在轨探测数据,分析了2012年3月和10月地磁扰动期间的热层大气成分数据,对磁暴期间N——2异常增变的涨幅、时间、空间特性,低纬地区N_2异常增变特点,以及冬夏半球N_2异常增变的差异进行探讨,探讨认为:N_2数密度的异常增变与地磁扰动及其扰动程度密切相关,增变现象通常出现在夏半球高纬区域上空,磁扰期间所出现的N2数密度异常增变现象与地磁扰动对热层大气加热机理紧密相关. |
其他语种文摘
|
The response of N_2 number density in thermosohere during two geomagnetic disturbance on March and October 2012 is analysed in this paper, data taken by Atmospheric Environment Detector on board Tiangong-1 spacecraft are used. Discuss the abnormal increase range, time and space characteristics, low latitude distribution and features of summer and winter hemisphere of N_2 number density during the geomagnetic storms. These results are as follows: the abnormal increase of N_2 number density is closely related to geomagnetic disturbance and its intensity, abnormal increase phenomenon usually appears in the high latitudes region of summer hemisphere, N_2 number density increase during the geomagnetic disturbance is closely related to the mechanism of atmospheric heat. |
来源
|
中国科学. 技术科学
,2014,44(8):883-889 【核心库】
|
DOI
|
10.1360/092013-1117
|
关键词
|
热层大气
;
大气成分
;
地磁暴
;
大气密度
|
地址
|
中国科学院空间科学与应用研究中心, 北京, 100190
|
语种
|
中文 |
文献类型
|
研究性论文 |
ISSN
|
1674-7259 |
学科
|
机械、仪表工业 |
基金
|
国家921工程项目
|
文献收藏号
|
CSCD:5219126
|
参考文献 共
13
共1页
|
1.
Daglis I A.
Space Storms and Space Weather Hazards,2001
|
被引
3
次
|
|
|
|
2.
Prolss G W.
Physics of the Earth's Space Environment,2004
|
被引
1
次
|
|
|
|
3.
Qin G. The thermospheric composition different responses to geomagnetic storm in the winter and summer hemisphere measured by "SZ" Atmospheric Composition Detectors.
Adv Space Res,2008,42:1281-1287
|
被引
4
次
|
|
|
|
4.
秦国泰. “神舟三号”大气成分探测器探测结果—2002年4月磁暴期间大气成分的异常变化.
空间科学学报,2004,24:41-47
|
被引
1
次
|
|
|
|
5.
秦国泰. 2005年8月24日强磁暴事件对高层大气密度的扰动.
空间科学学报,2008,28:137-141
|
被引
8
次
|
|
|
|
6.
Mansilla G A. Some effects in the upper atmosphere during geomagnetic storms.
Adv Space Res,2011,47:930-937
|
被引
1
次
|
|
|
|
7.
Burns A G. Large enhancements in the O/N2 ratio in the evening sector of the winter hemisphere during geomagnetic storms.
J Geophys Res,1995,100:14661-14671
|
被引
4
次
|
|
|
|
8.
Taeusch D R. Neutral composition variation above 400 kilometers during a magnetic storm.
J Geophys Res,1971,76:8318-8325
|
被引
2
次
|
|
|
|
9.
Benson R C. Atmospheric helium density measurements at 900 km from the neutral mass spectrometer on MSX, EOS.
Proc Amer Geophys Union,1997,78:17
|
被引
1
次
|
|
|
|
10.
Balan N. New aspects of thermospheric and ionospheric storms revealed by CHAMP.
J Geophys Res,2011,116:A07305
|
被引
2
次
|
|
|
|
11.
Balan N. Ionospheric and thermospheric storms at equatorial latitudes observed by CHAMP, ROCSAT, and DMSP.
J Geophys Res,2012,117:A01313
|
被引
1
次
|
|
|
|
12.
Liu H. Global distribution of the thermospheric total mass density derived from CHAMP.
J Geophys Res,2005,110:A04301
|
被引
7
次
|
|
|
|
13.
Liu H. Strong disturbance of the upper thermospheric density due to magnetic storms: CHAMP observations.
J Geophys Res,2005,110:A09S29
|
被引
15
次
|
|
|
|
|