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Field‐aligned currents associated with dipolarization fronts
Author(s) -
Sun W. J.,
Fu S. Y.,
Parks G. K.,
Liu J.,
Yao Z. H.,
Shi Q. Q.,
Zong Q.G.,
Huang S. Y.,
Pu Z. Y.,
Xiao T.
Publication year - 2013
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 - 10.1002/grl.50902
Subject(s) - earth's magnetic field , physics , front (military) , current (fluid) , cluster (spacecraft) , magnetic field , field (mathematics) , spacecraft , astrophysics , computational physics , geophysics , meteorology , astronomy , mathematics , quantum mechanics , computer science , pure mathematics , thermodynamics , programming language
Current densities associated with dipolarization fronts (DFs) have been calculated in the geomagnetic tail using the curlometer technique applied to high‐resolution magnetic fieldB → data obtained by the four Cluster spacecraft. We then use the relationb →· ∇ × B →to characterize the behavior of field‐aligned current (FAC) during 25 DF events. Our results show that the magnitude of FAC density ( J // ) ranges from 5 to 20 nA/m 2 , and they are observed in Northern and Southern Hemispheres flowing along both directions of theB → ‐field. The FACs have dimensions characteristic of the DFs and with region‐1 current sense flowing inside the DFs and region‐2 sense just in front of DF (in the B z dips). Most of our observations come from 15 to 20 R E in the tail, different from previous statistical studies based mainly on observations made around 9–12 R E . We suggest that DFs can sustain significant FACs and appear as “wedgelets” in the early stage.
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