Geomagnetic conjugate observation of nighttime medium-scale and large-scale traveling ionospheric disturbances: FRONT3 campaign

被引:102
作者
Shiokawa, K [1 ]
Otsuka, Y
Tsugawa, T
Ogawa, T
Saito, A
Ohshima, K
Kubota, M
Maruyama, T
Nakamura, T
Yamamoto, M
Wilkinson, P
机构
[1] Nagoya Univ, Solar Terr Environm Lab, Toyokawa 4428507, Japan
[2] Kyoto Univ, Grad Sch Sci, Sakyo Ku, Kyoto 6068502, Japan
[3] Natl Inst Informat & Commun Technol, Tokyo 1848795, Japan
[4] Kyoto Univ, Res Inst Sustainable Humanosphere, Kyoto 6110011, Japan
[5] IPS Radio & Space Serv, Haymarket, NSW 1240, Australia
关键词
D O I
10.1029/2004JA010845
中图分类号
P1 [天文学];
学科分类号
0704 ;
摘要
[1] The third FRONT (F-region Radio and Optical measurement of Nighttime TID) campaign was carried out during the new-moon period of May - June 2003, in order to investigate the geomagnetic conjugacy of medium-scale and large-scale traveling ionospheric disturbances ( MSTIDs/LSTIDs) at midlatitudes. Seven all-sky airglow imagers were operated in Japan and Australia. For almost all clear-sky nights, we observed MSTIDs in the 630-nm airglow images with horizontal wavelengths of 100 - 400 km propagating southwestward in Japan and northwestward in Australia. All of them show a one-to-one correspondence of wave structures between the Northern and Southern Hemispheres, indicating strong electrodynamic coupling between the two hemispheres through the geomagnetic field line. We also found that airglow intensity variations with a timescale longer than that of MSTIDs often show a good correlation between the two hemispheres. On 28 May, we succeeded in detecting an equatorward propagating LSTID ( spatial scale similar to 1000 km) as airglow enhancements at the conjugate stations. The airglow peak of the LSTID in the Northern Hemisphere was similar to 20 min earlier than that in the Southern Hemisphere, indicating that the observed LSTID is caused by a wave in the neutral atmosphere rather than by an electric field structure.
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