日本地球惑星科学連合2019年大会

講演情報

[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-EM11] Dynamics of Magnetosphere and Ionosphere

2019年5月29日(水) 15:30 〜 17:00 A04 (東京ベイ幕張ホール)

コンビーナ:中溝 葵(情報通信研究機構 電磁波研究所)、尾崎 光紀(金沢大学理工研究域電子情報学系)、藤本 晶子(九州工業大学)、堀 智昭(名古屋大学宇宙地球環境研究所)、座長:長谷川 洋(宇宙航空研究開発機構 宇宙科学研究所)

15:30 〜 15:45

[PEM11-01] A Case Study Based on Ground Observations of the Conjugate Ionospheric Response to Interplanetary Shock in Polar Regions

*He Fang1Zejun HU1Hongqiao HU1 (1.Polar Research Institute of China)

キーワード:polar ionosphere, conjugate, substorm, response, irregularity

This study uses data acquired by an imaging riometer, an ionosphere total electron content (TEC) monitor, and three specific wavelength auroral imagers at the conjugate Antarctic Zhongshan (ZHS) and Arctic Yellow River (YRS) stations to investigate the response of the polar ionosphere to a space weather event induced by solar flare activity on July 14, 2012. After the geomagnetic storm suddenly commenced and a magnetospheric substorm was triggered by the arrival of an interplanetary shock wave and its interaction with the magnetosphere at 18:10 UT, significantly enhanced auroral activity was observed by the auroral imagers at the ZHS. Meanwhile, the polar conjugate observation stations in the two hemispheres recorded notable growth of the two-dimensional cosmic noise adsorption and similar motion tendencies. According to our analysis and comparison of the ionospheric TEC data acquired by the conjugate stations, the TEC at both locations presented a considerable growth tendency after the interplanetary shock wave arrived, although the two stations experienced different sunlight conditions (polar night in the Antarctic region and polar day in the Arctic region). However, a comparison with high-frequency radar data demonstrated that different sources were responsible for the electron density enhancement of the ionosphere. In the Arctic polar day region, the increased electron density may have been caused by anti-sunward convection of the plasma irregularity, whereas in the Antarctic polar night region, the increased electron density may have been caused by energetic particle precipitation at the magnetospheric tail. Different physical processes might be the cause of the differential responses of the ionosphere at the two studied geomagnetic conjugate stations in the same solar activity event due to different local photoionization conditions.