Driving ionospheric outflows and magnetospheric O+ energy density with Alfvén waves

Abstract We show how dispersive Alfvén waves observed in the inner magnetosphere during geomagnetic storms can extract O+ ions from the topside ionosphere and accelerate these ions to energies exceeding 50 keV in the equatorial plane. This occurs through wave trapping, a variant of “shock” surfing,...

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Bibliographic Details
Main Authors: C. C. Chaston, J. W. Bonnell, G. D. Reeves, R. M. Skoug
Format: Article
Language:English
Published: Wiley 2016-05-01
Series:Geophysical Research Letters
Subjects:
Online Access:https://doi.org/10.1002/2016GL069008
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