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Radar observations of cleft dynamicsA continuous radar monitoring, during a six hour period which included an onset and recovery of global substorm activity, of an ionospheric density enhancement associated with the cleft is reported. Observations of the cleft showed a rapid equatorward excursion to 70 deg Lambda before occurrence of a major substorm intensification, continued location at low magnetic latitude during substorm expansion, and a poleward retreat to about 73.5 deg Lambda during substorm recovery in response to a northward turning of the IMF. Furthermore, the latitudinal width of the cleft density enhancement varied from less than 1 deg during the presubstorm equatorward motion to about 4 deg after substorm recovery.
Document ID
19800060999
Acquisition Source
Legacy CDMS
Document Type
Reprint (Version printed in journal)
Authors
Foster, J. C.
(Utah State Univ. Logan, UT, United States)
Stiles, G. S.
(Utah State Univ. Logan, UT, United States)
Doupnik, J. R.
(Utah State University of Agriculture and Applied Science, Logan, Utah, United States)
Date Acquired
August 10, 2013
Publication Date
July 1, 1980
Publication Information
Publication: Journal of Geophysical Research
Volume: 85
Subject Category
Geophysics
Accession Number
80A45169
Funding Number(s)
CONTRACT_GRANT: NSG-5216
CONTRACT_GRANT: NSF ATM-76-17334
Distribution Limits
Public
Copyright
Other

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