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Fedorov et al. 2001
Fedorov, E., Pilipenko, V. and Engebretson, M.J. (2001). ULF wave damping in the auroral acceleration region. Journal of Geophysical Research 106: doi: 10.1029/2000JA000022. issn: 0148-0227.

The width of a resonant peak in the spatial distribution of the ULF Pc5 pulsation amplitude at high latitudes is controlled by the dominant dissipation mechanism of Alfven waves in the ionosphere-magnetosphere system. Among possible mechanisms, mostly Joule dissipation and dispersive effects are considered to terminate the growth and narrowing of a resonant peak pumped by an external source. We estimate the width of the resonance which may be provided by the field-aligned electric field in a thermal, mirror-confined collisionless plasma. We consider a simple case, in which a potential drop is confined within a narrow region above the ionosphere, called the auroral acceleration region. Theoretical estimates show that the mirror-force mechanism can dominate over the ionospheric dissipation and dispersive effects in auroral regions with a sufficiently large field-aligned potential drop. Therefore ground-based monitoring of the resonance width (e.g., with the gradient method) may be used as an indicator of the occurrence of large-scale parallel electric fields in the outer magnetosphere. ¿ 2001 American Geophysical Union

BACKGROUND DATA FILES

Abstract

Keywords
Ionosphere, Auroral ionosphere, Magnetospheric Physics, Electric fields, Magnetospheric Physics, Magnetosphere/ionosphere interactions, Magnetospheric Physics, MHD waves and instabilities
Journal
Journal of Geophysical Research
http://www.agu.org/journals/jb/
Publisher
American Geophysical Union
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