Journal article
Oxygen torus and its coincidence with EMIC wave in the deep inner magnetosphere: Van Allen Probe B and Arase observations
Earth, planets, and space, Vol.72(1), pp.111-111
08/03/2020
DOI: 10.1186/s40623-020-01235-w
PMCID: PMC7410109
PMID: 32831576
Abstract
We investigate the longitudinal structure of the oxygen torus in the inner magnetosphere for a specific event found on 12 September 2017, using simultaneous observations from the Van Allen Probe B and Arase satellites. It is found that Probe B observed a clear enhancement in the average plasma mass (M) up to 3–4 amu at L = 3.3–3.6 and magnetic local time (MLT) = 9.0 h. In the afternoon sector at MLT ~ 16.0 h, both Probe B and Arase found no clear enhancements in M. This result suggests that the oxygen torus does not extend over all MLT but is skewed toward the dawn. Since a similar result has been reported for another event of the oxygen torus in a previous study, a crescent-shaped torus or a pinched torus centered around dawn may be a general feature of the O+ density enhancement in the inner magnetosphere. We newly find that an electromagnetic ion cyclotron (EMIC) wave in the H+ band appeared coincidently with the oxygen torus. From the lower cutoff frequency of the EMIC wave, the ion composition of the oxygen torus is estimated to be 80.6% H+, 3.4% He+, and 16.0% O+. According to the linearized dispersion relation for EMIC waves, both He+ and O+ ions inhibit EMIC wave growth and the stabilizing effect is stronger for He+ than O+. Therefore, when the H+ fraction or M is constant, the denser O+ ions are naturally accompanied by the more tenuous He+ ions, resulting in a weaker stabilizing effect (i.e., larger growth rate). From the Probe B observations, we find that the growth rate becomes larger in the oxygen torus than in the adjacent regions in the plasma trough and the plasmasphere.
Details
- Title: Subtitle
- Oxygen torus and its coincidence with EMIC wave in the deep inner magnetosphere: Van Allen Probe B and Arase observations
- Creators
- M. Nosé - Nagoya UniversityA. Matsuoka - Kyoto UniversityA. Kumamoto - Tohoku UniversityY. Kasahara - Kanazawa UniversityM. Teramoto - Kyushu Institute of TechnologyS. Kurita - Kyoto UniversityJ. Goldstein - The University of Texas at San AntonioL. M. Kistler - Nagoya UniversityS. Singh - Geological Survey of IndiaA. Gololobov - North-Eastern Federal UniversityK. Shiokawa - Nagoya, JapanS. Imajo - Nagoya UniversityS. Oimatsu - Kyoto UniversityK. Yamamoto - The University of TokyoY. Obana - Osaka Electro-Communication UniversityM. Shoji - Nagoya UniversityF. Tsuchiya - Tohoku UniversityI. Shinohara - Japan Aerospace Exploration AgencyY. Miyoshi - Nagoya UniversityW. S. Kurth - University of IowaC. A. Kletzing - University of IowaC. W. Smith - Durham, NH USAR. J. MacDowall - Goddard Space Flight CenterH. Spence - University of New HampshireG. D. Reeves - Los Alamos National Laboratory
- Resource Type
- Journal article
- Publication Details
- Earth, planets, and space, Vol.72(1), pp.111-111
- DOI
- 10.1186/s40623-020-01235-w
- PMID
- 32831576
- PMCID
- PMC7410109
- NLM abbreviation
- Earth Planets Space
- ISSN
- 1343-8832
- eISSN
- 1880-5981
- Publisher
- Springer Berlin Heidelberg
- Grant note
- ; NAS5-01072 / ; 16H04057; 17K18804; 17K0566; 16H06286; 15H05815; 15H05747 / ; 20H01959 / ;
- Language
- English
- Date published
- 08/03/2020
- Academic Unit
- Physics and Astronomy
- Record Identifier
- 9984428829302771
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