Ducted propagation of whistler mode chorus waves observed by the Arase satellite near the plasmapause at high latitudes
Yuri Ampuku1, Fuminori Tsuchiya1, Satoshi Kurita2, Yasumasa Kasaba1, Yuto Katoh1, Mizuki Fukizawa3, Yoshizumi Miyoshi4, Iku Shinohara5, Yoshiya Kasahara6, Syoya Matsuda6, Atsushi Kumamoto1, Ayako Matsuoka7, Satoko Nakamura8 and Masahiro Kitahara1, (1)Tohoku University, Department of Geophysics, Graduate School of Science, Sendai, Japan, (2)Kyoto University, Research Institute for Sustainable Humanosphere, Kyoto, Japan, (3)National Institute of Polar Research, Tachikawa, Japan, (4)Nagoya University, Institute for Space-Earth Environmental Research (ISEE), Nagoya, Japan, (5)Japan Aerospace Exploration Agency (JAXA), Institute of Space and Astronautical Science (ISAS), Sagamihara, Japan, (6)Kanazawa University, Graduate School of Natural Science and Technology, Kanazawa, Japan, (7)Kyoto University, Kyoto, Japan, (8)Nagoya University, Institute for Space-Earth Environmental Research, Nagoya, Japan
