Japan Geoscience Union Meeting 2022

Presentation information

[E] Oral

P (Space and Planetary Sciences ) » P-EM Solar-Terrestrial Sciences, Space Electromagnetism & Space Environment

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

Wed. May 25, 2022 10:45 AM - 12:15 PM 302 (International Conference Hall, Makuhari Messe)

convener:Huixin Liu(Earth and Planetary Science Division, Kyushu University SERC, Kyushu University), convener:Yuichi Otsuka(Institute for Space-Earth Environmental Research, Nagoya University), Loren Chang(Institute of Space Science, National Central University), convener:Yue Deng(University of Texas at Arlington), Chairperson:Masaki Tsutsumi(National Institute of Polar Research), Tatsuhiro Yokoyama(Kyoto University), Masaru Kogure(Kyushu University)


12:00 PM - 12:15 PM

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

*Masaki Tsutsumi1, Taishi Hashimoto1, Koji Nishimura2, Toru Sato3, Masashi Kohma4, Kaoru Sato4 (1.National Institute of Polar Research, 2.RISH, Kyoto Univ., 3. ILAS, Kyoto Univ. , 4.Graduate School of Science, Univ. of Tokyo )

Keywords:Antarctic, PANSY radar, meteor wind observations, Syowa station

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.