日本地球惑星科学連合2022年大会

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[E] 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-EM13] Coupling Processes in the Atmosphere-Ionosphere System

2022年5月25日(水) 10:45 〜 12:15 302 (幕張メッセ国際会議場)

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)、コンビーナ:大塚 雄一(名古屋大学宇宙地球環境研究所)、Chang Loren(Institute of Space Science, National Central University)、コンビーナ:Deng Yue(University of Texas at Arlington)、座長:堤 雅基(国立極地研究所)、横山 竜宏(京都大学)、木暮 優(九州大学)


12:00 〜 12:15

[PEM13-24] Long-term meteor wind observations as by-products of routine mesosphere measurements of PANSY radar, Antarctica

*堤 雅基1、橋本 大志1、西村 耕司2、佐藤 亨3高麗 正史4佐藤 薫4 (1.国立極地研究所、2.京大・生存研、3.京大・国際高等教育院、4.東大・理)

キーワード:南極、PANSYレーダー、流星風観測、昭和基地

PANSY radar at Syowa station (69S, 39E) has been conducting continuous mesosphere, stratosphere and troposphere observations as the only MST/IS radar in the Antarctic [Sato et al., 2014]. These observation techniques are characterized by their three dimensional wind velocity measurement ability including vertical wind component with high time/height resolutions.
The mesosphere observations, however, need ionized media in the mesosphere and are limited to day-light hours. To compensate this we have developed an external interferometry system for reception which can detect meteor echoes throughout a day in the height region of 70-95 km as purely by-products of the routine mesosphere measurements. A pioneering external meteor system attached to the MU radar, Japan, by Nakamura et al [1997] is a proto-type of the current system.
The newly developed system, consisting of five Yagi antennas, has continuously been operating since March 2021. Figure 1 shows daily mean wind velocities observed from March 2021 to January 2022. The zonal component is eastward in winter and westward in summer showing a clear seasonal pattern. The meridional component blows equatorward (northward) in summer, corresponding to the gravity-wave driven meridional circulation pattern. Analyses of atmospheric waves are further to be made.

References
Sato et al., 2014, J. Atmos. Sol.-Terr. Phys., 118, 2−15, doi:10.1016/j.jastp.2013.08.022.
Nakamura et al., 1997, Radio Sci., 32, 1203-1214.