DocumentCode
1465947
Title
Ionospheric Response to the Geomagnetic Storm on August 21, 2003 Over China Using GNSS-Based Tomographic Technique
Author
Wen, Debao ; Yuan, Yunbin ; Ou, Jikun ; Zhang, Kefei
Author_Institution
Sch. of Traffic & Transp. Eng., Changsha Univ. of Sci. & Technol., Changsha, China
Volume
48
Issue
8
fYear
2010
Firstpage
3212
Lastpage
3217
Abstract
The impacts of the August 21, 2003 geomagnetic storm on the ionosphere over China have been first investigated by using the so-called computerized ionospheric tomography (CIT) technique and the observations of the Crustal Movement Observation Network of China. Tomographic results show that the main ionospheric effects of this geomagnetic storm over China are as follows: (1) the negative storm phase effect appears in the F region and (2) the positive storm phase effect occurs above the F region. Meanwhile, some key features in the ionospheric structure have been revealed in the ionospheric images during the storm; this includes the disturbances and an elongated region of the reduced electron density at the latitude around 32°N. Statistical comparisons are carried out to confirm the reliability of the global-navigation-satellite-system-based CIT reconstruction results using the profile obtained from ionosonde observations.
Keywords
F-region; magnetic storms; magnetosphere; AD 2003 08 21; China; Crustal Movement Observation Network; F region; GNSS-based tomographic technique; computerized ionospheric tomography technique; electron density; geomagnetic storm; global-navigation-satellite-system-based CIT reconstruction; ionosonde observations; ionospheric effects; ionospheric images; ionospheric response; ionospheric structure; negative storm phase effect; positive storm phase effect; Electron density; geomagnetic storm; global navigation satellite systems (GNSS); ionosphere; tomography;
fLanguage
English
Journal_Title
Geoscience and Remote Sensing, IEEE Transactions on
Publisher
ieee
ISSN
0196-2892
Type
jour
DOI
10.1109/TGRS.2010.2044579
Filename
5444895
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