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磁静日期间中国大陆地区外源弱磁场研究
引用本文:冯彦, 安振昌, 毛飞, 孙涵, 蒋勇, 柳士俊. 磁静日期间中国大陆地区外源弱磁场研究[J]. 空间科学学报, 2012, 32(3): 321-335. doi: 10.11728/cjss2012.03.321
作者姓名:冯彦  安振昌  毛飞  孙涵  蒋勇  柳士俊
作者单位:1.南京信息工程大学数理学院 南京 210044;;2.中国科学院地质与地球物理研究所 北京 100029;;3.中国气象科学研究院 北京 100081;;4.国家卫星气象中心遥感应用试验基地/广西气象减灾研究所 南宁 530022;;5.中国气象局培训中心 北京 100081
基金项目:国家高技术研究发展计划课题研究专项资助
摘    要:利用第四代地磁场综合模型CM4, 研究了中国大陆地区1960-2000年磁静日期间地磁外源弱磁场的变化情况, 计算并分析了外源场中的电离层感应场、环形场以及磁层感应场的分布和变化. 结果显示, 北向分量X的磁层感应场强度总体呈先增加后减少的趋势, 共减少了约7.3nT; 东向分量Y的磁层感应场强度呈先减少后增加的趋势, 共增加了约0.8nT; 垂直分量Z的磁层感应场强度呈先增加后减少的趋势, 共增加了约5.5nT. 三个分量的电离层感应场以及环形场变化幅度很小, 其分布在1960-1970和1970-1980年, 1980-1990 和1990-2000年呈现正负互相变换的现象, 认为该现象可能与太阳11年活动周期有关. 最后对弱磁场随时间变化的结果进行了分析说明.

关 键 词:CM4模型   电离层感应场   磁层感应场
收稿时间:2010-06-12
修稿时间:2011-10-19

Study on External Weak Magnetic Field During Magnetic Quiet Periods Over Chinese Mainland
Feng Yan, An Zhenchang, Mao Fei, Sun Han, Jiang Yong, Liu Shijun. Study on external weak magnetic field during magnetic quiet periods over Chinese mainland[J]. Chinese Journal of Space Science, 2012, 32(3): 321-335. doi: 10.11728/cjss2012.03.321
Authors:FENG Yan  AN Zhenchang  MAO Fei  SUN Han  JIANG Yong  LIU Shijun
Affiliation:1. The College of Mathematics and Physics, Nanjing University of Information and Technology, Nanjing 210044;;2. Institute of Geology and Geophysics, Chinese Academy of Sciences, Beijing 100029;;3. Chinese Academy of Meteorological Sciences, Beijing 100081;;4. Remote Sensing Application and Experiment Station of National Satellite Meteorological Center/Guangxi Meteorological Disaster Mitigation Institute, Nanning 530022;;5. Training Center, China Meteorological Administration, Beijing 100081
Abstract:The fourth generation comprehensive model of magnetic field CM4 was used to research the variation of external weak field in magnetically quiet periods over Chinese mainland during 1960—2000.The distribution and variation of ionospheric induced field,toroidal field and magnetospheric induced field separated from the external field were also calculated and analyzed.Results show that in terms of lithospheric induced field,component X’s trend of variation was increased firstly,then decreased with time,the amplitude is about 7.3 nT;Component Y’s trend of variation was initially decreased,and increased with time,the amplitude is about 0.8nT;Component Z’s trend of variation was increased and then decreased with time,the amplitude is about 5.5 nT.The variation amplitude of toroidal field and magnetospheric induced field of three components are relative small.Their distribution during 1960-1970 and 1970-1980,1980-1990 and 1990-2000 show an interesting phenomenon that areas of positive and negative values exchanged each other,which may has something related with solar 11 years’ activities.Finally,analysis and explaination of these results were given.
Keywords:CM4  Ionospheric induced field  Magnetospheric induced field
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