Japan Geoscience Union Meeting 2021

Presentation information

[E] Poster

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

[P-EM12] Dynamics of the Inner Magnetospheric System

Sat. Jun 5, 2021 5:15 PM - 6:30 PM Ch.04

convener:Kunihiro Keika(Department of Earth and Planetary Science, Graduate School of Science, The University of Tokyo), Yoshizumi Miyoshi(Institute for Space-Earth Environmental Research, Nagoya University), W Lauren Blum(University of Colorado Boulder), Yuri Shprits(Helmholtz Centre Potsdam GFZ German Research Centre for Geosciences)

5:15 PM - 6:30 PM

[PEM12-P31] Statistical analyses of low energy ion heating by electromagnetic ion cyclotron waves via wave-particle interaction analyses: Arase observations

*Masafumi Shoji1, Yoshizumi Miyoshi1, Lynn M Kistler1,2, Kazushi Asamura3, Yasumasa Kasaba4, Ayako Matsuoka5, Yoshiya Kasahara6, Shoya Matsuda3, Fuminori Tsuchiya4, Atsushi Kumamoto4, Satoko Nakamura1, Masahiro Kitahara1, Shun Imajo1, Chae-Woo Jun1, Iku Shinohara3 (1.Institute for Space-Earth Environmental Research, Nagoya Univ., 2.University of New Hampshire, 3.ISAS/JAXA, 4.Tohoku Univ., 5.Kyoto Univ., 6.Kanazawa Univ.)

Keywords:Wave-particle interaction, Ion heating

Electromagnetic ion cyclotron (EMIC) waves are generated through the cyclotron wave-particle interaction, affecting the plasma environment in the magnetosphere. Heating of ions by EMIC waves in the inner magnetosphere has been investigated using spacecraft observations by comparing the pitch angle distribution of the ions and the wave emissions. We can directly detect the energy transfer between the plasma waves and the ions via the wave-particle interaction analysis (WPIA) method which calculates the inner product between the wave electric fields and the ion velocities. We adapt the WPIA method to the Arase spacecraft data and investigate the spatial distribution of the positive region in the inner magnetosphere. From March 21st 2017 to September 27th 2019, we select 60 EMIC wave events with associated proton flux enhancement between 10 eV to 100 eV which are a suitable dataset for the WPIA method observed by PWE/EFD, MGF, and LEP-i onboard the Arase satellite. The peak of the proton heating occurrence appears in the dayside and post noon regions. Typical EMIC waves inside the plasma plume contribute to the peak in the afternoon sector in both geomagnetically quiet and active times. On the other hand, in the dayside region, the proton heating takes place predominantly during quiet times. It suggests that the protons in the region are energized by the EMIC waves generated through compression of the ambient magnetic field. We also discuss the species dependence of the ion heating.