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Observations of fast auroral waves.Results of simultaneous observation of a fast wave event from the Ester Dome Observatory (EDO) near College, Alaska, the Poker Flat Rocket Launching Facility (PKR), and Fort Yukon, Alaska (FYU). The display occurred on Mar. 27, 1971, and the general morphology is described and discussed. It is suggested that fast auroral waves occur when a preceding substorm has enhanced the particle population in the region of the magnetosphere near L = 6 in the midnight sector; then transverse hydromagnetic waves, associated with the onset of further local substorm activity, become visible through their action on this enhanced particle population as they propagate inwards in the equatorial region.
Document ID
19720041296
Acquisition Source
Legacy CDMS
Document Type
Reprint (Version printed in journal)
Authors
Boyd, J. S.
Davis, T. N.
Brown, N. B.
Hallinan, T. J.
Wallis, D. D.
(Alaska, University College, Alaska, United States)
Date Acquired
August 6, 2013
Publication Date
March 1, 1972
Publication Information
Publication: Planetary and Space Science
Volume: 20
Subject Category
Geophysics
Accession Number
72A24962
Funding Number(s)
CONTRACT_GRANT: NAS6-1832
CONTRACT_GRANT: NSF GA-28079
Distribution Limits
Public
Copyright
Other

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