Japan Geoscience Union Meeting 2014

Presentation information

Oral

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

[P-EM37_30AM2] Structure and Dynamics of the Magnetosphere

Wed. Apr 30, 2014 11:00 AM - 12:45 PM 414 (4F)

Convener:*Yoshizumi Miyoshi(Solar-Terrestrial Environement Laboratory, Nagoya University), Hiroshi Hasegawa(Institute of Space and Astronautical Science, Japan Aerospace Exploration Agency), Chair:Mariko Teramoto(Japan Aerospace Exploration Agency), Hiroshi Hasegawa(Institute of Space and Astronautical Science, Japan Aerospace Exploration Agency)

11:30 AM - 11:45 AM

[PEM37-03] High-resolution correlation analysis between VLF/ELF chorus waves and pulsating aurora observed at Athabasca, Canada

*Naoki SUNAGAWA1, Kazuo SHIOKAWA1, Yoshizumi MIYOSHI1, Ryuho KATAOKA2, Mitsunori OZAKI3, Kaoru SAWAI3, Schofield IAN4, Connors MARTIN4 (1.Solar-Terrestrial Environment, 2.National Institute of Polar Research, 3.Kanazawa University, 4.Athabasca University)

Keywords:pulsating aurora, chorus waves, Wave-particle interactions, ground-based observation

We investigate dynamic switching of arrival time difference between pulsating aurora intensity and chorus waves which were observed on 7 February 2013 at Athabasca in Canada (L=4.4), using a crossed-loop antenna and a narrow field-of-view EMCCD camera. Power spectra of pulsating auroral intensity and chorus wave intensity at 1.5-2.5 kHz show a same pulsation period at 0.1-0.15 Hz. Arrival time difference between pulsating aurora intensity and chorus waves are evaluated by using cross-correlation analysis. We found that two patterns of arrival time difference switches with a time scale of a few tens seconds. One pattern shows that electrons reached ionosphere later than the associated chorus waves with a delay time of 2 s, consistent with the theoretical value for south-going electrons reflected at the ionosphere in the southern hemisphere. The other pattern shows that electrons reached ionosphere earlier by 4.5 s than the associated chorus waves, consistent with the theoretical value for south-going chorus waves reflected at the ionosphere in the southern hemisphere. These results firstly show that interaction process of high-energy electrons and chorus waves are changing with a time scale of a few tens seconds.