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Radar observations of cleft dynamics

Journal Article · · J. Geophys. Res.; (United States)
The ionospheric F region is perturbed by low-energy particle precipitation in the cleft. On January 28--29, 1977, UT an ionospheric density enhancement associated with the cleft was monitored continuously by the Chatanika incoherent scatter radar during a 6-hour period including an onset and recovery of global substorm activity. A strongly southward interplanetary magnetic field (IMF) brought the cleft into the field of view of the radar (invariant latitudes less than 75 /sup 0/). The observed motions of the cleft included a rapid equatorward excursion (approx.4 /sup 0/..lambda../h) to 70 /sup 0/ before occurrence of a major substorm intensification, continued location at low magnetic latitude during substorm expansion, and a poleward retreat to approx.73.5 /sup 0/..lambda.. during substorm recovery in response to a northward turning of the IMF. The latitudinal width of the cleft density enhancement varied from less than 1 /sup 0/ during the presubstorm equatorward motion to approx.4 /sup 0/ after substorm recovery. F region densities immediately poleward of the cleft were reduced by a factor of 10 from their quiet time value.
Research Organization:
Center for Atmospheric and Space Sciences, Utah State University, Logan, Utah 84322
OSTI ID:
5096718
Journal Information:
J. Geophys. Res.; (United States), Journal Name: J. Geophys. Res.; (United States) Vol. 85:A7; ISSN JGREA
Country of Publication:
United States
Language:
English