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Plasma injection at synchronous orbit and spatial and temporal auroral morphologyAnalysis of ATS 5 particle spectrograms and simultaneous meridian-scanning photometer data obtained at the base of the ATS field line has revealed systematic relationships between temporal and spatial auroral morphology and particle-injection events. The details of these relationships depend on previous injection events, the local time of the observatory with respect to current-injection events, and the extent and magnitude of current injections. A persistent zone of weak aurora is related to steady plasma-sheet drizzle, and the equatorward edge of this aurora delineates field lines threading the inner edge of the plasma sheet. Auroras associated with injection events superimpose on this preexisting pattern, with the lowest latitude of new precipitation depending on local time. In general, plasma energization is not required between the equatorial plane and the ionosphere to account for observed auroral intensities. The data indicate occasional occurrence of enhanced loss-cone fluxes, suggesting low-altitude field-aligned acceleration. A summary figure shows how various characteristic auroral-precipitation regions are related to the shape, extent, and orientation of the substorm injection boundary and to the subsequent drift paths of injected plasma.
Document ID
19760053300
Acquisition Source
Legacy CDMS
Document Type
Reprint (Version printed in journal)
Authors
Eather, R. H.
(Boston College Chestnut Hill, Mass., United States)
Mende, S. B.
(Lockheed Research Laboratories Palo Alto, Calif., United States)
Judge, R. J. R.
(California, University La Jolla, Calif., United States)
Date Acquired
August 8, 2013
Publication Date
June 1, 1976
Publication Information
Publication: Journal of Geophysical Research
Volume: 81
Subject Category
Geophysics
Accession Number
76A36266
Funding Number(s)
CONTRACT_GRANT: NSF C-659
CONTRACT_GRANT: NASW-2552
CONTRACT_GRANT: NGR-22-003-017
CONTRACT_GRANT: NSF GA-42560
Distribution Limits
Public
Copyright
Other

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