JpGU-AGU Joint Meeting 2020

講演情報

[E] ポスター発表

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-EM13] Dynamics of Magnetosphere and Ionosphere

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)、佐藤 由佳(日本工業大学)

[PEM13-P28] Ground-based observations of MF/HF auroral radio emissions at three stations

*佐藤 由佳1,2熊本 篤志2加藤 雄人2小川 泰信3門倉 昭3新堀 淳樹4 (1.日本工業大学、2.東北大学大学院理学研究科、3.国立極地研究所、4.名古屋大学宇宙地球環境研究所)

キーワード:電波放射、オーロラ現象、波動粒子相互作用

We launched ground-based observations of MF/HF auroral radio emissions more than a decade ago at two stations (The Husafell Station, Iceland, September 2005; The Kjell Henriksen Observatory, Svalbard, September 2008) and found multiple unknown properties of MF/HF auroral radio emissions, e.g. polarization features [Sato et al., 2008, 2015] and existence of a higher frequency component [Sato et al., 2012]. To make a next siginificant step for a futher understanding of MF/HF auroral radio emissions, we installed a new dedicated instrumentation at the KAIRA (Kilpisjärvi Atmospheric Imaging Receiver Array) site in Kilpisjärvi, Finland (Latitude: 60.07 N, Longitude: 20.76 E) in the summer of 2018. It is a passive receiving system designed to realize a high-resolution spectral, interferometric and polarization measurements using 4 loop antennas and a software-defined radio (SDR) receiver. This SDR receiver can implement high-speed, flexible digital signal processing of RF signals and obtain high-resolution spectra pauselessly throughout the night in a wide frequency range up to 6 MHz. In addition, we plan to upgrade the receiving system in Iceland to utilize a similar SDR receiver this summer. One of the main research subjects of this project is radio emission spontaneously emitted from aurora. There are long-known three types of MF/HF auroral radio emissions identified at ground level: auroral hiss, medium frequency burst (MFB), and auroral roar. Investigation into the generation of these emissions not only offers a tool of great promise for remote sensing of ionospheric plasma processes and parameters but also gives the foundation for understanding various radiation mechanisms that occur in planetary magnetospheres and plasma in space. In combination with the long-term continuous observations in Iceland and Svalbard and future EISCAT_3D experiments, observation with this new instrumentation will provide a first-time opportunity to reveal spatiotemporal variations of macro and fine structures of MF/HF auroral radio emissions associated with substorm evolution. In this presentation, we show detailed specification of the new instrumentations and some initial results.