日本地球惑星科学連合2015年大会

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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-EM06] Mesosphere-Thermosphere-Ionosphere Coupling in the Earth's Atmosphere

2015年5月27日(水) 14:15 〜 16:00 A01 (アパホテル&リゾート 東京ベイ幕張)

コンビーナ:*Huixin Liu(九州大学理学研究院地球惑星科学専攻 九州大学宙空環境研究センター)、大塚 雄一(名古屋大学太陽地球環境研究所)、Libo Liu(Institute of Geology and Geophysics, Chinese Academy of Sciences)、新堀 淳樹(京都大学生存圏研究所)、座長:Larisa Goncharenko(Massachusetts Institute of Technology Haystack Observatory)

15:00 〜 15:15

[PEM06-20] Ground-based mesopause temperatures at high-latitude over Yakutia:Comparison with SABER measurements

*Anastasia AMMOSOVA1Petr AMMOSOV1Galina GAVRILYEVA1Igor KOLTOVSKOI1 (1.ShICRA)

キーワード:mesopause temperature, O2 airglow, SABER measurements

Ground-based mesopause temperature at high-latitude over Yakutia: Comparison with SABER measurements

Yu. G. Shafer Institute of Cosmophysical Research and Aeronomy

Petr Ammosov; Galina Gavrilyeva; Anastasia Ammosova; Igor Koltovskoi
tenyka@rambler.ru

Rotational temperatures obtained from the O2 Atmospheric (0?1) nightglow band, with an infrared spectrograph at the Maimaga station (63 N, 129.5 E) for the period September 2002 to March 2013 are presented. Time series includes the years of maximum and minimum solar activity. The set of spectrograph data has been used to analyze the seasonal behaviour of the mesopause temperatures. Atmospheric temperatures deduced from infrared spectrograph and from satellite observations with the Sounding of the Atmosphere using Broadband Emission Radiometry (SABER) instrument on board the TIMED satellite, have also been compared.
The temperatures measured during the satellite passes at distances not larger than 300 km from the intersection of the spectrograph sighting line with the oxygen emitting layer (~94 km) have been compared. A seasonal dependence is observed regarding the difference between the ground based and satellite measurements. However, the time variations in the temperature obtained with the ground based device and on the satellite are similar. Based on the performed analysis, it has been concluded that a series of oxygen rotational temperatures can be used to study temperature variations on different time scales, including long-term trends at the temperature emission altitude (~94 km).