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The auroral oval - A reevaluation.The auroral oval represents a region of auroral occurrence where particular spectral features have sufficient integrated intensity to exceed all-sky camera thresholds. It has been argued that this is not a good representation of the characteristics of particle precipitation or of energy deposition. Consequently, the auroral oval concept may not be a good one to use to order diverse auroral data on a 24-hour basis. Rather, the precipitation patterns for specific energy classes of protons and electrons should form the basis for the interpretation of high-latitude geophysical measurements.
Document ID
19730039980
Acquisition Source
Legacy CDMS
Document Type
Reprint (Version printed in journal)
Authors
Eather, R. H.
(Boston College Chestnut Hill, Mass., United States)
Date Acquired
August 7, 2013
Publication Date
February 1, 1973
Publication Information
Publication: Reviews of Geophysics and Space Physics
Volume: 11
Subject Category
Geophysics
Accession Number
73A24782
Funding Number(s)
CONTRACT_GRANT: NGR-22-003-018
CONTRACT_GRANT: NSF GA-28044
Distribution Limits
Public
Copyright
Other

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