Japan Geoscience Union Meeting 2022

Presentation information

[E] Poster

P (Space and Planetary Sciences ) » P-EM Solar-Terrestrial Sciences, Space Electromagnetism & Space Environment

[P-EM10] Dynamics of Magnetosphere and Ionosphere

Thu. Jun 2, 2022 11:00 AM - 1:00 PM Online Poster Zoom Room (5) (Ch.05)

convener:Yuka Sato(Nippon Institute of Technology), convener:Akimasa Ieda(Institute for Space-Earth Environmental Research, Nagoya University), Akiko Fujimoto(Kyushu Institute of Technology), convener:Shun Imajo(Data Analysis Center for Geomagnetism and Space Magnetism, Graduate School of Science, Kyoto University), Chairperson:Yuka Sato(Nippon Institute of Technology), Akimasa Ieda(Institute for Space-Earth Environmental Research, Nagoya University), Akiko Fujimoto(Kyushu Institute of Technology), Shun Imajo(Data Analysis Center for Geomagnetism and Space Magnetism, Graduate School of Science, Kyoto University)


11:00 AM - 1:00 PM

[PEM10-P02] Temporal variations of 2-D distributions of precipitating low-energy electron fluxes associated with the auroral arc near the nightside polar cap boundary

*kazuki yashima1, Satoshi Taguchi1, Keisuke Hosokawa2 (1.Department of Geophysics, Graduate School of Science, Kyoto University, 2.Department of Communication Engineering and Informatics, The University of Electro-Communications)

Keywords:Aurora, broadband electron precipitation, polar cap boundary

Near the nightside polar cap boundary there often occurs intense low-energy electron precipitation as well as the inverted-V type electron precipitation. The intense low-energy electron precipitation, which is thought to be associated with Alfvenic electron acceleration, produces a tall red aurora. Previous satellite observations have shown the detailed energy profiles of that low-energy electron precipitation, and their spatial features. However, we still do not understand how the low-energy component of the electron precipitation grows or decays near the nightside polar cap boundary. In this study, to understand the temporal characteristics of the low-energy electron fluxes near the nightside polar cap boundary we have developed an automated method for deriving 2-D distributions of the low-energy electron fluxes by comparing 630-nm auroral image data obtained by an all-sky imager (located at Longyearbyen, Svalbard) with 630-nm emission distributions calculated by the Global Airglow model. The result from this automated method has revealed the energy fluxes of the low-energy electron precipitation are enhanced intermittently. We discuss this feature in terms of the motion of the auroral arc.