日本地球惑星科学連合2018年大会

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[EE] 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-EM15] Dynamics in magnetosphere and ionosphere

2018年5月20日(日) 09:00 〜 10:30 303 (幕張メッセ国際会議場 3F)

コンビーナ:田中 良昌(国立極地研究所)、堀 智昭(名古屋大学宇宙地球環境研究所)、中溝 葵(情報通信研究機構 電磁波研究所、共同)、尾崎 光紀(金沢大学理工研究域電子情報学系)、座長:新堀 敦樹(ISEE, Nagoya Univ.)、佐藤 由佳(極地研究所)

09:45 〜 10:00

[PEM15-04] Direct evidence for throat aurora being the ionospheric signature of magnetopause transient and reflectiing localized magnetopause indentations

*Han Desheng1 (1.School of Ocean and Earth Science, Tongji University)

キーワード:throat aurora, magnetosheath high speed jet, magnetopause transient, magnetopause indentation

Magnetopause transients, observing as brief entries into the magnetosheath by satellites, are commonly observed in the vicinity of the magnetopause and have been explained by several possible mechanisms. However, satellite observations alone are insufficient to determine the dynamics and context of transients. Throat auroras are characterized as north-south aligned discrete auroral forms extending from the equatorward edge of the discrete auroral oval that are only observed near dayside convection throat region and have been suggested as the ionospheric signature of localized magnetopause indentations. Using coordinated observations from the Magnetospheric Multiscale Mission (MMS) and ground-based all-sky imagers, we show one-to-one correspondences between transients observed by MMS near the subsolar magnetopause and throat auroras observed on the ground. The correspondence is valid not only for typical throat aurora with larger spatial scale but also for these with tiny scales. We even notice that the transient durations observed by satellite are approximately proportional to the width (east-west extension) of the throat aurora. These results provide direct evidence that throat auroras are ground signatures for the magnetopause transients. With the aid of auroral observations, we suggest that these transients reflect localized magnetopause indentations but are not produced by motion of the entire magnetopause. We also found that most transients are associated with earthward flow enhancements, which indicates that high-speed jets in the magnetosheath could be a driver for producing these transients.