EISCAT observation of a high-latitude ionization trough associated with a reversed westward plasma flow

Details EISCAT observation of a high-latitude ionization trough associated with a reversed westward plasma flow EISCAT observation of a high-latitude ionization trough associated with a reversed westward plasma flow

Oct 2000

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=2000georl..27.3269m&link_type=abstract

Geophysical Research Letters, Volume 27, Issue 20, p. 3269-3272

Physics

Ionosphere, Ionosphere: Auroral Ionosphere, Ionosphere: Ionosphere/Magnetosphere Interactions, Magnetospheric Physics: Storms And Substorms

Scientific paper

Trough-like plasma structures in the high-latitude ionosphere near the polar cap boundary are investigated with EISCAT CP3 data and in-situ satellite observations. Emphasis is placed on one interesting event occurring in the morning sector during the recovery phase of a moderate magnetic storm. The event features are probably ionospheric signatures of cusp processes caused by magnetic reconnection on the dayside magnetopause.

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