Analysis of the Asymmetry of the Equatorial Ionization Anomaly in North-south Direction Using TEC Data of Ground IGS Observation
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Analysis of the Asymmetry of the Equatorial Ionization Anomaly in North-south Direction Using TEC Data of Ground IGS Observation
Acta Scientiarum Naturalium Universitatis SunYatseniVol. 52, Issue 4, Pages: 130-137(2013)
作者机构:
1. 广州气象卫星地面站,广东,广州,510640
2.
3. 华南理工大学 理学院,广东,广州,510640
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Published:2013,
Published Online:25 July 2013,
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HUANG Jiang, DENG Baichang, HUANG Linfeng, et al. Analysis of the Asymmetry of the Equatorial Ionization Anomaly in North-south Direction Using TEC Data of Ground IGS Observation. [J]. Acta Scientiarum Naturalium Universitatis SunYatseni 52(4):130-137(2013)
DOI:
HUANG Jiang, DENG Baichang, HUANG Linfeng, et al. Analysis of the Asymmetry of the Equatorial Ionization Anomaly in North-south Direction Using TEC Data of Ground IGS Observation. [J]. Acta Scientiarum Naturalium Universitatis SunYatseni 52(4):130-137(2013)DOI:
Analysis of the Asymmetry of the Equatorial Ionization Anomaly in North-south Direction Using TEC Data of Ground IGS Observation
The total electron content (TEC) measured by GPS observations from the network of International GNSS Service (IGS) at the altitude of about 450 km in the 110°E longitude sector for more than a solar cycle term from January 2000 to December 2011 are used to study the northsouth asymmetry of the equatorial ionization anomaly (EIA). The parameters of the EIA crest obtained from the daytime TEC profiles for conditions of different solar activity have been used to study the solar cycle variations of EIA in the Southeast Asian region. Results show that the latitudinal position
occurrence time and strength of the EIA crest are found to be asymmetric about the magnetic equator and the conditions of solar activity have a remarkable effect on EIA crest and the northsouth asymmetry. The strength of EIA crest is obviously higher during periods of high solar activity
and the TEC average value of the EIA crest is obviously higher in the northern hemisphere during the daytime in all seasonal. The strength of the north crest is higher than that of the south crest in summer and autumn during low solar activity period
while smaller in winter.During high solar activity period
the occurrence time of the northern crest appears about 1 h later than that of the southern crest from June to August. And during low solar activity period
the occurrence time of the northern crest appears about 1 h earlier than that of southern crest in winter
while about 2 h later from May to September. With the solar activity increased gradually
the mean value of asymmetry index (Ia) increased obviously during winter solstice.