中国科学院机构知识库网格
Chinese Academy of Sciences Institutional Repositories Grid
Ionospheric response to the geomagnetic storm on 13-17 April 2006 in the West Pacific region

文献类型:期刊论文

作者Zhao, Biqiang1,2; Wan, Weixing1; Liu, Libo1; Igarashi, K.3; Yumoto, K.4; Ning, Baiqi1
刊名JOURNAL OF ATMOSPHERIC AND SOLAR-TERRESTRIAL PHYSICS
出版日期2009
卷号71期号:1页码:88-100
关键词Magnetic storm Total electron content Mid-low latitude
ISSN号1364-6826
DOI10.1016/j.jastp.2008.09.029
文献子类Article
英文摘要This paper presents an investigation of geomagnetic storm effects in the equatorial and middle-low latitude F-region in the West Pacific sector during the intense geomagnetic storm on 13-17 April, 2006. The event, preceded by a minor storm, started at 2130 UT on April 13 while interplanetary magnetic field (IMF) B(z) component was ready to turn southward. From 14-17 the ionosphere was characterized by a large scale enhancement in critical frequency, foF2 (4 similar to 6MHz) and total electron content (TEC) (similar to 30TECU, 1TECU = 1 x 10(16)el/m(2)) followed by a long-duration negative phase observed through the simultaneous ionospheric sounding measurements from 14 stations and GPS network along the meridian 120 degrees E. A periodic wave structure, known as traveling ionospheric disturbances (TIDs) was observed in the morning sector during the initial phase of the storm which should be associated with the impulsive magnetospheric energy injection to the auroral. In the afternoon and nighttime, the positive phase should be caused by the combination of equatorward winds and disturbed electric fields verified through the equatorial F-layer peak height variation and modeled upward drift of Fejer and Scherliess [1997. Empirical models of storm time equatorial electric fields. journal of Geophysical Research 102, 24,047-24,056]. It is shown that the large positive storm effect was more pronounced in the Southern Hemisphere during the morning-noon sector on April 15 and negative phase reached to lower magnetic latitudes in the Northern Hemisphere which may be related to the asymmetry of the thermospheric condition during the storm. (C) 2008 Elsevier Ltd. All rights reserved.
WOS关键词MAGNETICALLY DISTURBED CONDITIONS ; EQUATORIAL ELECTRIC-FIELDS ; LOW LATITUDES ; F3 LAYER ; THERMOSPHERE ; ENHANCEMENTS ; HEMISPHERE ; VELOCITIES ; NOVEMBER ; DYNAMO
WOS研究方向Geochemistry & Geophysics ; Meteorology & Atmospheric Sciences
语种英语
WOS记录号WOS:000263196500010
出版者PERGAMON-ELSEVIER SCIENCE LTD
资助机构National Natural Science Foundation of China(40804041 ; National Natural Science Foundation of China(40804041 ; National Natural Science Foundation of China(40804041 ; National Natural Science Foundation of China(40804041 ; National Important Basic Research(2006CB806306) ; National Important Basic Research(2006CB806306) ; National Important Basic Research(2006CB806306) ; National Important Basic Research(2006CB806306) ; 40725014) ; 40725014) ; 40725014) ; 40725014) ; National Natural Science Foundation of China(40804041 ; National Natural Science Foundation of China(40804041 ; National Natural Science Foundation of China(40804041 ; National Natural Science Foundation of China(40804041 ; National Important Basic Research(2006CB806306) ; National Important Basic Research(2006CB806306) ; National Important Basic Research(2006CB806306) ; National Important Basic Research(2006CB806306) ; 40725014) ; 40725014) ; 40725014) ; 40725014) ; National Natural Science Foundation of China(40804041 ; National Natural Science Foundation of China(40804041 ; National Natural Science Foundation of China(40804041 ; National Natural Science Foundation of China(40804041 ; National Important Basic Research(2006CB806306) ; National Important Basic Research(2006CB806306) ; National Important Basic Research(2006CB806306) ; National Important Basic Research(2006CB806306) ; 40725014) ; 40725014) ; 40725014) ; 40725014) ; National Natural Science Foundation of China(40804041 ; National Natural Science Foundation of China(40804041 ; National Natural Science Foundation of China(40804041 ; National Natural Science Foundation of China(40804041 ; National Important Basic Research(2006CB806306) ; National Important Basic Research(2006CB806306) ; National Important Basic Research(2006CB806306) ; National Important Basic Research(2006CB806306) ; 40725014) ; 40725014) ; 40725014) ; 40725014)
源URL[http://ir.iggcas.ac.cn/handle/132A11/70598]  
专题中国科学院地质与地球物理研究所
通讯作者Zhao, Biqiang
作者单位1.Chinese Acad Sci, Inst Geol & Geophys, Beijing 100029, Peoples R China
2.Chinese Acad Sci, State Key Lab Space Weather, Beijing 100080, Peoples R China
3.Natl Inst Informat & Commun Technol, Tokyo, Japan
4.Kyushu Univ, Space Environm Res Ctr, Fukuoka 812, Japan
推荐引用方式
GB/T 7714
Zhao, Biqiang,Wan, Weixing,Liu, Libo,et al. Ionospheric response to the geomagnetic storm on 13-17 April 2006 in the West Pacific region[J]. JOURNAL OF ATMOSPHERIC AND SOLAR-TERRESTRIAL PHYSICS,2009,71(1):88-100.
APA Zhao, Biqiang,Wan, Weixing,Liu, Libo,Igarashi, K.,Yumoto, K.,&Ning, Baiqi.(2009).Ionospheric response to the geomagnetic storm on 13-17 April 2006 in the West Pacific region.JOURNAL OF ATMOSPHERIC AND SOLAR-TERRESTRIAL PHYSICS,71(1),88-100.
MLA Zhao, Biqiang,et al."Ionospheric response to the geomagnetic storm on 13-17 April 2006 in the West Pacific region".JOURNAL OF ATMOSPHERIC AND SOLAR-TERRESTRIAL PHYSICS 71.1(2009):88-100.

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来源:地质与地球物理研究所

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