留言板

尊敬的读者、作者、审稿人, 关于本刊的投稿、审稿、编辑和出版的任何问题, 您可以本页添加留言。我们将尽快给您答复。谢谢您的支持!

姓名
邮箱
手机号码
标题
留言内容
验证码

利用IGS-TEC数据分析中国华南地区电离层赤道异常北驼峰的变化特征

黄林峰 蒋勇 王劲松 黄江

黄林峰, 蒋勇, 王劲松, 黄江. 利用IGS-TEC数据分析中国华南地区电离层赤道异常北驼峰的变化特征[J]. 空间科学学报, 2015, 35(2): 152-158. doi: 10.11728/cjss2015.02.152
引用本文: 黄林峰, 蒋勇, 王劲松, 黄江. 利用IGS-TEC数据分析中国华南地区电离层赤道异常北驼峰的变化特征[J]. 空间科学学报, 2015, 35(2): 152-158. doi: 10.11728/cjss2015.02.152
Huang Linfeng, Jiang Yong, Wang Jingsong, Huang Jiang. Using IGS-TEC data to analyze the variation of EIA crest over South China Region[J]. Journal of Space Science, 2015, 35(2): 152-158. doi: 10.11728/cjss2015.02.152
Citation: Huang Linfeng, Jiang Yong, Wang Jingsong, Huang Jiang. Using IGS-TEC data to analyze the variation of EIA crest over South China Region[J]. Journal of Space Science, 2015, 35(2): 152-158. doi: 10.11728/cjss2015.02.152

利用IGS-TEC数据分析中国华南地区电离层赤道异常北驼峰的变化特征

doi: 10.11728/cjss2015.02.152
基金项目: 国家自然科学基金项目(41174165),国家高技术研究发展 计划项目(2012AA121005)和江苏省普通高校研究生科研创新计划项目(CXLX13_503)共同资助
详细信息
  • 中图分类号: P352

Using IGS-TEC data to analyze the variation of EIA crest over South China Region

  • 摘要: 利用2010年11月至2011年10月IGS提供的全球电子浓度总含量(TEC)数据, 分析太阳活动上升期华南地区(经度110°E, 纬度5°—35°N) 上空电离层赤道异常(EIA)北驼峰的变化特征. 结果显示, 电离层赤道异常北驼峰区TEC峰值I具有明显的季节和半年变化特征; 北驼峰峰值出现的时间T和纬度L的日变化有一个相对较大的变化区间, 其季节和半年变化特征并不明显; 太阳活动对北驼峰变化影响比较明显, 而地磁活动对北驼峰变化影响不明显.

     

  • [1] Chen Yanhong, Wan Weixing, Liu Libo, et al. Astaistical TEC model based on the observation at Wuhanionospheric observatory[J]. Chin. J. Space Sci., 2002, 22(1):27-35. In Chinese (陈艳红, 万卫星, 刘立波, 等. 武汉地区电离层电子浓度总含量的统计经验模式研究[J]. 空间科学学报, 2002, 22(1):27-35)
    [2] Yu Tao, Wan Weixing, Liu Libo, et al. Numerical study for the semi-annual variation of electric fields at the mid- and low-latitudes[J]. Chin. J. Space Sci., 2004, 24 (3): 182-193. In Chinese (余涛, 万卫星, 刘立波, 等. 电离层电场半年变化的模拟研究[J]. 空间科学学报, 2004, 24(3):182-193)
    [3] Cai C. Monitoring seasonal variations of ionospheric TEC using GPS measurements[J]. Geo-spatial Inf. Sci., 2007, 10(2):96-99
    [4] Wu C C, Liou K, Shan S J, et al. Variation of ionospheric total electron content in Taiwan region of the equatorial anomaly from 1994 to 2003[J]. Adv. Space Res., 2008, 41(4):611-616
    [5] Wu C C, Fry C D, Liu J Y, et al. Annual TEC variation in the equatorial anomaly region during the solar minimum: September 1996—August 1997[J]. J. Atmos. Solar-Terr. Phy., 2004, 66(3):199-207
    [6] Yu You, Wan Weixing, Liu Libo, et al. A global ionospheirc TEC perturbation index[J]. Chin. J. Geophys., 2009(9):2189-2194. In Chinese (余优, 万卫星, 刘立波, 等. 全球电离层TEC起伏特性分析[J]. 地球物理学报, 2009(9):2189-2194)
    [7] Wang Weimin, Xu Zhenzhong, Zhang Ren, et al. Correlation analysis of the TEC at Wuhan station with solar activities and geomagnetic activities during 23rd solar cycle[J]. Chin. J. Space Sci., 2012, 32(1):40-47. In Chinese (王伟民, 徐振中, 张韧, 等. 武汉站第23周电离层TEC与太阳及地 磁活动的相关性分析[J]. 空间科学学报, 2012, 32(1):40-47)
    [8] Cai Chaojun, Huang Jiang, Deng Baichang, et al. Applicability analysis of IRI-2007 in predicting TEC over Guangzhou region[J]. Chin. J. Space Sci., 2013, 33(3):277-285. In Chinese (蔡超军, 黄江, 邓柏昌, 等. IRI-2007预测TEC在广州地区的适 用性分析[J]. 空间科学学报, 2013, 33(3):277-285)
    [9] Chen Peiren. Longitudinal variation of the equatorial anomaly[J]. Chin. J. Geophys., 1991, 34(2):147-153
    [10] Huang Y N, Cheng K. Solar cycle variations of the equatorial ionospheric anomaly in total electron content in the Asian region[J]. J.Geophys. Res., 1996, 101(A11):24513-24520
    [11] Yu Tao, Wan Weixing, Liu Libo, et al. Using IGS data to analyze the global TEC annual and semiannual variation[J]. Chin. J. Geophys., 2006, 49(4):943-949
    [12] Zhao B, Wan W, Liu L, et al. Characteristics of the ionospheric total electron content of the equatorial ionization anomaly in the Asian-Australian region during 1996—2004[J]. Ann. Geophys., 2009, 27(10):3861-3873
    [13] Zhang M L, Wan W X, Liu L B, et al. Variability study of the crest-to-trough TEC ratio of the equatorial ionization anomaly around 120°E longitude[J]. Adv. Space Res., 2009, 43(6):1762-1769
    [14] Mukherjee S, Sarkar S, Purohit P K, et al. Seasonal variation of total electron content at crest of equatorial anomaly station during low solar activity conditions[J]. Adv. Space Res., 2010, 46(3):291-295
    [15] Xu Zhenzhong, Wang Weimin, Wang Bo, et al. Analysis and prediction of ionospheric total electron content of the Equatorial Ionization Anomaly around 120°E longitude[J]. Chin. J. Geophys., 2012, 55(7):2185-2192
    [16] Ma G, Maruyama T. Derivation of TEC and estimation of instrumental biases from GEONET in Japan[J]. Ann. Geophys., 2003, 21:2083-2093
    [17] Wan Weixing, Ning Baiqi, Liu Libo, et al. Now casting the ionospheric total electron content over China[J]. Chin. J. Geophys., 2007, 22(4):1040-1045
    [18] Stening R J. Modeling the low latitude F-region[J]. J. Atmos. Terr. Phys., 1992, 54(11/12):1387-1421
  • 加载中
计量
  • 文章访问数:  1245
  • HTML全文浏览量:  17
  • PDF下载量:  1387
  • 被引次数: 0
出版历程
  • 收稿日期:  2014-03-04
  • 修回日期:  2014-10-08
  • 刊出日期:  2015-03-15

目录

    /

    返回文章
    返回