Japan Geoscience Union Meeting 2022

Presentation information

Print

[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

Tue. May 24, 2022 3:30 PM - 5:00 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:Hiroyo Ohya(Graduate School of Engineering, Chiba University), Michi Nishioka(National Institute of Information and Communications Technology), Susumu Saito(Electronic Navigation Research Institute, National Institute of Maritime, Port, and Aviation Technology)


4:30 PM - 4:45 PM

[PEM13-11] Enhancement of short period GPS-TEC oscillations over rainfall area

*Toshihiko Iyemori1, Akiyasu Yamada1, Tadashi Aoyama2, Kornyanat Hozumi3, Yoshihiro Yokoyama4, Yoko Odagi1, Sano Yasuharu5, Vijak Pangsapa6, Thanawat Jarupongsakul6, Akinori Saito1, Masato Iguchi1 (1.Kyoto University, 2.F-Factory Co., Ltd., 3.National Institute of Information and Communications Technology, 4.Swedish Institute of Space Physics, 5.Asahi University, 6.Faculty of Science, Chulalongkorn University)

Keywords:rainfall, GPS-TEC oscillation, vertical acoustic resonance

Rainfall effects to the amplitude of short period GPS-TEC oscillations are investigated by using the precipitation data obtained on the ground and estimated from satellite observations (JAXA/GSMaP) and the GPS-TEC data obtained at a tropical station, PHIM, in Phimai, Thailand, and the data obtained at a mid-latitude station, NAKG, in Tokara Nakanoshima Island, Japan. A statistical analysis of the TEC power spectral density (PSD) in the period range from 50 seconds to 1200 seconds over PHIM clearly shows an enhancement in the cases of rainfall from that in no-rainfall cases, in particular, on the dusk side. The enhancement is observed both acoustic wave periods less than 5-6 minutes and internal gravity wave periods more than 10 minutes. On the other hand, the PSD does not show such clear enhancement over NAKG on the dusk side, although it shows a small enhancement on both dayside and night side. Some clear PSD bulges near the three main vertical acoustic resonance periods (i.e., around 270, 230 and 200 seconds) appear in the average PSD profile of the TEC at PHIM, which suggests that the resonance effect contribute to some extent the PSD enhancement under rainy condition.