Journal
GEOPHYSICAL RESEARCH LETTERS
Volume 43, Issue 5, Pages 1793-1801Publisher
AMER GEOPHYSICAL UNION
DOI: 10.1002/2015GL067580
Keywords
substorm; onset arc; acceleration mechanism
Categories
Funding
- NASA [NAS5-02099]
- Canadian Space Agency
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On 16 March 2006, the Reimei spacecraft observed dynamic small-scale vortex-like structures along an east-west elongated onset arc, subsequently followed by the auroral expansion. Within a few seconds when Reimei crossed over the arc, detailed comparisons of the simultaneous conjugate auroral imaging and particle observations with high resolution were made to reveal the fine-scale acceleration processes acting within/around the flux tube of the bright auroral structures. In the surrounding dark region, Alfvenic accelerated electron fluxestime-dispersive, field-aligned electron bursts spanning a broad range of energiesbecame most noticeable. The dominant contributor to the central bright region, on the other hand, was monoenergetic electron fluxes in 3-7keV at larger pitch angles (>30 degrees) rather than the Alfvenic electron fluxes. The Reimei observations suggest that the Alfvenic acceleration process operates in the vicinity of small-scale auroral structures but plays a less significant role in powering the central bright emissions.
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