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STARE: Observations of a field‐aligned line current
Author(s) -
Nielsen E.,
Bruns M.,
Pardowitz I.,
Perplies H.,
Bemmann L.,
Janhunen P.,
Huuskonen A.
Publication year - 1999
Publication title -
geophysical research letters
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 2.007
H-Index - 273
eISSN - 1944-8007
pISSN - 0094-8276
DOI - 10.1029/1998gl900252
Subject(s) - ionosphere , earth's magnetic field , current (fluid) , radar , geophysics , field line , line (geometry) , magnetopause , physics , field (mathematics) , incoherent scatter , geology , magnetosphere , magnetic field , computer science , telecommunications , geometry , mathematics , quantum mechanics , thermodynamics , pure mathematics
For the first time a magnetospheric line current entering the ionosphere has been unambiguously observed. The observation was made with STARE ( = Scandinavian Twin Auroral Radar Experiment), a ground based coherent radar system, which has been updated with modern computer technique, and recently taken into operation. A counter clockwise turning swirl of ionospheric electron drift velocities is synonymous with the presence of a line current flowing along the geomagnetic field lines into the ionosphere. A Flux Transfer Event on the magnetopause has been predicted to connect to the ionosphere via a line current.

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