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Variability of plasma-line enhancement in ionospheric modification experiments.A simple explanation for the variations of plasma-line intensity is suggested. The explanation is based on the fact that the plasma waves responsible for scattering the radar waves occur over a very limited range of heights. The explanation further makes use of the fact that the position of these height ranges of generation depends primarily on the gradient of the number density and to a lesser extent on the temperature and the orientation of the diagnostic radar beam.
Document ID
19720033804
Acquisition Source
Legacy CDMS
Document Type
Reprint (Version printed in journal)
Authors
Fejer, J. A.
(California, University La Jolla, Calif., United States)
Date Acquired
August 6, 2013
Publication Date
January 1, 1972
Publication Information
Publication: Journal of Geophysical Research
Volume: 77
Subject Category
Geophysics
Accession Number
72A17470
Funding Number(s)
CONTRACT_GRANT: DA-31-124-ARO(D)-257
CONTRACT_GRANT: NGR-05-009-076
Distribution Limits
Public
Copyright
Other

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