*Rei Sugimura1, Kazuo Shiokawa1, Yuichi Otsuka1, Shin-ichiro Oyama1, Martin G Connors2, Akira Kadokura3, Alexey Poddelsky4, Igor Poddelsky4, Nozomu Nishitani1, Simon G Shepherd5, J Michael Ruohoniemi6, Charles Smith7, Robert MacDowall8, Harlan Spence7, Geoff Reeves9, Herbert O Funsten 9, Yoshizumi Miyoshi1, Iku Shinohara10, Yoshiya Kasahara11, Fuminori Tsuchiya12, Atsushi Kumamoto12, Satoko Nakamura1, Atsuki Shinbori1, Kazushi Asamura13, Shoichiro Yokota14, Yoichi Kazama15, Chae-Woo Jun1, Shiang-Yu Wang15, Sunny W.Y. Tam16, Satoshi Kasahara17, Kunihiro Keika18, Tomoaki Hori1, Ayako Matsuoka10
(1.Institute for Space-Earth Environmental Research, Nagoya University, 2.Athabasca University, 3.National Institute of Polar Research, 4.Institute of Cosmophysical Research and Radiowave Propagation, Far Eastern Branch of the Russian Academy of Sciences, 5.Thayer School of Engineering, Dartmouth College, 6.Bradley Department of Electrical and Computer Engineering, Virginia Tech, 7.Institute for the Study of Earth, Oceans, and Space, University of New Hampshire, 8.NASA Goddard Space Flight Center, Greenbelt, 9.Los Alamos National Laboratory, 10.Institute of Space and Astronautical Science, Japan Aerospace Exploration Agency, 11.Graduate School of Natural Science and Technology, Kanazawa University, 12.Graduate School of Science, Tohoku University, 13.Japan Aerospace Exploration Agency, 14.Department of Earth and Space Science, Graduate School of Science, Osaka University, 15.Academia Sinica Institute of Astronomy and Astrophysics, 16.Institute of Space and Plasma Sciences, National Cheng Kung University, 17.Department of Earth and Planetary Science, School of Science, University of Tokyo, 18.Graduate School of Science, Tokyo University)
Keywords:STEVE, SAR arc, Arase satellite
Strong Thermal Emission Velocity Enhancement (STEVE) is a latitudinally-narrow, purple band of emission seen at subauroral latitudes, which was discovered in 2016. Well-known Stable Auroral Red (SAR) arcs also occurs at subauroral latitude. Red and green arcs, which are similar to SAR arcs at subauroral latitudes but accompanied by green (557.7 nm) emission, have also been reported. However, the characteristics of the magnetospheric plasma and electromagnetic field variations as a source of these three types of optical emissions have not fully been studied, because of limited conjugate observations between magnetospheric satellites and ground-based optical and radio instruments. In this study, we report the auroral morphology as seen in all-sky image data obtained at seven ground stations (Athabasca, Gakona, Husafell, Kapuskasing, Magadan, Nyrola and Tromsø) during about four years from January 2017 to April 2021. By referring to the optical images as well as the ionospheric footprint of magnetospheric satellites (Arase and Van Allen Probes) calculated with the Tsyganenko magnetic field model (TS04), we have identified four cases of STEVE, four cases of SAR arc, three cases of green and red arcs in which these satellites were located in the conjugate regions in the magnetosphere of the optical emissions. For all three types of optical emissions, satellite data showed that the plasmasphere and ring-current particles spatially overlapped in the conjugate regions of the magnetosphere. Some electromagnetic waves in mHz to kHz were observed for STEVE and red and green arc events. SuperDARN radar data showed a strong westward plasma flow in the ionosphere, especially during the STEVE events, while the plasma flows associated with SAR arcs and red and green arcs are relatively weak and variable. Heat fluxes due to Coulomb collisions were larger for STEVE compared to SAR arc. However, the heat flux may have been underestimated for events that low-energy electrons were not measured. These analyses have provided the first-ever comparison of magnetospheric particle and electromagnetic field characteristics for the three types of optical emissions in the subauroral region. In the presentation, we will discuss the differences and similarities of the magnetospheric and ionospheric processes responsible for producing these three-types of emissions.