Magnetic field dipolarization in the deep inner magnetosphere and its role in development of O+-rich ring current
Document Type
Article
Publication Date
1-1-2010
Abstract
We studied magnetic field dipolarization and associated ion acceleration in the deep inner magnetosphere, using magnetic field data obtained by the magnetometer on board the Mission Demonstration Satellite 1 (MDS-1) and the energetic neutral atom (ENA) flux data obtained by the high-energy neutral analyzer imager on board the Imager for Magnetopause-to-Aurora Global Exploration satellite. Because the MDS-1 satellite has a geosynchronous transfer orbit, we could survey magnetic field variations at L = 3.0-6.5. Analyzing data in the period from February to July 2002, we found that (1) dipolarization can be detected over a wide range of L (i.e., L = 3.5-6.5, which is far inside the geosynchronous altitude); (2) when the MDS-1 satellite was located close to auroral breakup longitude, the occurrence probability of dipolarization was about 50% just inside the geosynchronous altitude and about 16% at L = 3.5-5.0, suggesting that dipolarization in the deep inner magnetosphere is not unusual; (3) magnetic storms were developing whenever dipolarization was found at L = 3.5-5.0; (4) dipolarization was accompanied by magnetic field fluctuations having a characteristic timescale of 3-5 s, which is comparable to the local gyroperiod of O+ ions; and (5) after dipolarization, the oxygen ENA flux in the nightside ring current region was predominantly enhanced by a factor of 2-5 and stayed at an enhanced level for more than 1 h, while clear enhancement was scarcely seen in the hydrogen ENA flux. From these results, we conjectured a scenario for the generation of an O+-rich ring current, in which preexisting thermal O+ ions in the outer plasmasphere (i.e., an oxygen torus known from satellite observations) experience local and nonadiabatic acceleration by magnetic field fluctuations that accompany dipolarization in the deep inner magnetosphere (L = 3.5-5.0). Copyright 2010 by the American Geophysical Union.
Identifier
77957563043 (Scopus)
Publication Title
Journal of Geophysical Research Space Physics
External Full Text Location
https://doi.org/10.1029/2010JA015321
e-ISSN
21699402
Issue
9
Volume
115
Grant
22340145
Fund Ref
Japan Society for the Promotion of Science
Recommended Citation
Nosé, M.; Koshiishi, H.; Matsumoto, H.; Cson Brandt, P.; Keika, K.; Koga, K.; Goka, T.; and Obara, T., "Magnetic field dipolarization in the deep inner magnetosphere and its role in development of O+-rich ring current" (2010). Faculty Publications. 6587.
https://digitalcommons.njit.edu/fac_pubs/6587
