Sub-auroral F-layer irregularities and the ring current

Details Sub-auroral F-layer irregularities and the ring current Sub-auroral F-layer irregularities and the ring current

Apr 1989

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=1989angeo...7..169a&link_type=abstract

Annales Geophysicae (ISSN 0980-8752), vol. 7, April 1989, p. 169-176. Research supported by the U.S. Navy and NSF.

Physics

6

F Region, Geomagnetism, Ionospheric Disturbances, Magnetohydrodynamic Stability, Ring Currents, Auroral Zones, Kp Index, Magnetic Storms, Plasmapause

Scientific paper

Scintillation and ionosonde data from several stations ranging from 50-71 deg corrected geomagnetic latitude in both hemispheres are studied. It is shown that the energy from magnetic storms stored most probably in the ring current is a primary source of energy for the formations of F-layer irregularities at subauroral latitudes in the region of the plasmapause during the recovery phase of a geomagnetic storm.

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