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Nighttime mesospheric returns associated with a large scale flare eventMagnetic storms associated with large flares can give D region ionization. Special measurements are made at night to evaluate the nature of mesospheric returns obtained under storm conditions. Five periods of time are tabulated varying in length from 20 min to 60 min at which scattered power is observed above the noise level. The three values of k(p) corresponding to the five periods are also given, as is the mean power over noise observed. The scattered powers from 78 to 81 km are comparable with those observed during the day, indicating that a similar ionization density is present. The peak power levels are approximately the same in both cases; but whereas the night data come from an essentially zero background, the day data arise from a substantial level of background scatter. This implies that the periods indicated are the only times at which any substantial particle precipitation is taking place; and that the consequent ionization is confined to the height region shown.
Document ID
19840019035
Acquisition Source
Legacy CDMS
Document Type
Conference Paper
Authors
Bowhill, S. A.
(Illinois Univ. Urbana, IL, United States)
Date Acquired
August 12, 2013
Publication Date
December 1, 1983
Publication Information
Publication: International Council of Scientific Unions Middle Atmosphere Program, Vol. 9
Subject Category
Communications And Radar
Accession Number
84N27103
Funding Number(s)
CONTRACT_GRANT: NSF ATM-81-20371
CONTRACT_GRANT: NSG-7506
Distribution Limits
Public
Copyright
Work of the US Gov. Public Use Permitted.
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