日本地球惑星科学連合2014年大会

講演情報

口頭発表

セッション記号 P (宇宙惑星科学) » P-EM 太陽地球系科学・宇宙電磁気学・宇宙環境

[P-EM36_28AM2] 大気圏・電離圏

2014年4月28日(月) 11:00 〜 12:45 312 (3F)

コンビーナ:*大塚 雄一(名古屋大学太陽地球環境研究所)、津川 卓也(情報通信研究機構)、川村 誠治(独立行政法人 情報通信研究機構)、座長:川村 誠治(独立行政法人 情報通信研究機構)、新堀 淳樹(京都大学生存圏研究所)

11:45 〜 12:00

[PEM36-11] 母子里および鹿児島で観測された昼間トウィーク空電の初検出

*大矢 浩代1塩川 和夫2三好 由純2 (1.千葉大学大学院工学研究科、2.名古屋大学太陽地球環境研究所)

It is well known that tweek atmospherics can be observed only at night except for solar eclipse days, because daytime attenuation rate of the tweeks is much larger (~70 dB/1000 km) than that in nighttime (~3 dB/1000 km). In this presentation, we firstly report detection of daytime tweeks at Moshiri (Geographic coordinate: 44.37oN, 142.27oE) and Kagoshima (31.48oN, 130.72oE), Japan, on non-solar eclipse days in December, 1980. The daytime tweeks were observed both before and during a large magnetic storm during 16-20 December, 1980. The minimum Dst value was -240 nT at 04:00 UT on 20 December. The average occurrence numbers of the daytime tweeks at Moshiri and Kagoshima were 2.7 and 0.3 tweeks per minute, respectively. The local times (LT) when the daytime tweeks occurred were through 07:00 - 17:00 LT at Moshiri, while they were 07:00 - 09:00 LT and 15:00 - 17:00 LT at Kagoshima. All the daytime tweeks show clear frequency dispersion. The average duration was 18.94 ms, while that of nighttime tweeks is ~50 ms. The average reflection heights of daytime tweeks at Moshiri and Kagoshima were 86.2 km and 94.7 km, respectively. The average reflection heights of nighttime tweeks at Moshiri and Kagoshima in same period were 87.1 km and 92.1 km, respectively. The variation of the daytime tweek reflection height was higher than that of nighttime tweeks. The horizontal propagation distance in daytime cannot be estimated from the dispersion, because the duration was too short to estimate the distance. We found through a theoretical consideration that the VLF/ELF attenuation on the D-region ionosphere depends not only on the ionospheric height, but also the sharpness of electron density profiles, β. The β is a conventional parameter proposed by Wait and Spies [1964]. When the β increases, the attenuation decreases. Even daytime, when the β is occasionally large, the attenuation would become less down to be able to observe the tweeks. In this talk, we will show the results of the daytime tweeks and discuss their occurrence mechanism.