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Field-aligned currents as a diagnostic tool: Result, a renovated model of the magnetosphere

Journal Article · · J. Geophys. Res.; (United States)
In the outer magnetosphere, currents across magnetic field lines are carried out by protons, because of their greater energy, whereas field-aligned currents are carried by electrons. Consequently, thre is plasma enhancement or depletion on flux tubes where the two types of current connect. Thus field-aligned currents observed at low altitudes can be used to diagnose plasma redistribution in the outer magnetosphere. A stationary current sheet accompanies convection through a stationary plasma boundary. The observations of the location and strength of field-aligned currents are used to create a model of the currents, flows, magnetic topology and plasma distribution in the outer magnetosphere. Differences from previous models include the following: (1) A steady state flow may exist at subauroral latitudes. (2) The upward current sheet (Region 1 dusk, Harang, region II dawn) separates dipolar flux tubes from inflated taillike flux tubes. Flux tubes convecting earthward from the tail coppases in a dipolar shape as they convect through this sheet. (3) There is a significant intrusion of solar wind protons from the dawn flank into the plasma sheet between the region 1 and 11 currents.
Research Organization:
Herzberg Institute of Astrophysics, National Research Council of Canada
OSTI ID:
6673628
Journal Information:
J. Geophys. Res.; (United States), Journal Name: J. Geophys. Res.; (United States) Vol. 89:A1; ISSN JGREA
Country of Publication:
United States
Language:
English

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