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The morphology of metallic ions in the upper atmosphereAnalysis of metallic ion data from a day-night pair of rockets, OGO 6, and the elliptic phases of AE-C and AE-D shows the presence of Fe(+) ions at altitudes above 400 km only at low magnetic latitudes. The detection probability of this ion decreases with altitude, with a maximum over the Atlantic and a minimum over India; the rocket data indicate ions in the E region during the day and on the bottom of the F layer at night. Mg(+) and Fe(+) are the dominant ions below 250 km at all latitudes, but Al(+), Na(+), Si(+), and Ca(+) are also detectable; a correlation was found between solar activity and metallic ion detection probability at low latitudes and high altitudes at night
Document ID
19810032954
Acquisition Source
Legacy CDMS
Document Type
Reprint (Version printed in journal)
Authors
Kumar, S.
(Texas Univ. at Dallas Richardson, TX, United States)
Hanson, W. B.
(Texas, University Richardson, Tex., United States)
Date Acquired
August 11, 2013
Publication Date
December 1, 1980
Publication Information
Publication: Journal of Geophysical Research
Volume: 85
Subject Category
Geophysics
Accession Number
81A17358
Funding Number(s)
CONTRACT_GRANT: NGR-44-004-120
CONTRACT_GRANT: NAS5-11407
Distribution Limits
Public
Copyright
Other

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