日本地球惑星科学連合2024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-EM11] Space Weather and Space Climate

2024年5月28日(火) 13:45 〜 15:15 展示場特設会場 (2) (幕張メッセ国際展示場 6ホール)

コンビーナ:片岡 龍峰(国立極地研究所)、Aronne Mary(NASA Goddard Space Flight Center)、伴場 由美(国立研究開発法人 情報通信研究機構)、Pulkkinen Antti(NASA Goddard Space Flight Center)、座長:片岡 龍峰(国立極地研究所)、Mary Aronne

14:45 〜 15:00

[PEM11-20] The research progress on the polar cap Sporadic-E layers

*Yong Wang1、P. T. Jayachandran2、Qing-He Zhang1,5、David R Themens2、Robert Gilies3、Ashton Reimer4、Roger Varney4、Yu-Zhang Ma1、Zan-Yang Xing1 (1.Shandong University、2.University of New Brunswick、3.University of Calgary、4.SRI International、5.Center for Space Science and Applied Research, Chinese Academy of Sciences)

キーワード:the polar cap, sporadic-E layers, Comprehensive characteristics, Multi-measurements at the Resolute

At high latitudes, the Sporadic-E layer (Es layer) is a common phenomenon but is still poorly understood due to sparse measurements and the difficulty of conventional mechanisms to operate. In this study, an interesting case of polar cap Es layer is firstly studied by using the twin incoherent scatter radars (RISR-N and RISR-C), a Canadian Advanced Digital Ionosonde (CADI), and a Magnetometer, all at Resolute, Canada. From several electron density profiles of the twin radars, the horizontal scale of the polar cap Es layer is found to be greater than 350 km. Moreover, the polar cap Es layer is determined to be drifting from the bottom F region (>150 km) to the lower E region. Furthermore, a unique appearance of double polar cap Es layers is observed. As a result, these peculiar signatures inspire a newly proposed process that involves the combination of localized electric fields and gravity waves.