On the relationship between thin Birkeland current arcs and reversed flow channels in the winter cusp/cleft ionosphere

• Published in: Journal of Geophysical Research: Space Physics 2008-09, Vol.113 (A9), p.n/a
• Main Authors: Moen, J., Rinne, Y., Carlson, H. C., Oksavik, K., Fujii, R., Opgenoorth, H.
• Format: Article
• Language: English
• Subjects: Earth sciences; Earth, ocean, space; Exact sciences and technology; flow channel; FTE; inverted V
• ISSN: 0148-0227; 2156-2202
• DOI: 10.1029/2008JA013061

In this paper we study reversed flow events (RFEs) that seem regulated by Birkeland current arcs in the winter cusp ionosphere above Svalbard. An RFE is a longitudinally elongated, 100–200 km wide channel, in which the flow direction is opposite to the background convection, persisting for 10–20 min. The RFE onset occurs with the brightening of a discrete arc near the open‐closed boundary. The auroral arc is situated exactly at a sharp clockwise flow reversal, consistent with a converging electric field and an upward field‐aligned current. One category of RFEs propagates into the polar cap in tandem with poleward moving auroral forms, while another category of RFEs moves with the cusp/cleft boundary. The RFE phenomenon is addressed to a region void of electron precipitation, and in lack of direct sunlight the E‐region conductivity will be very low. We propose two possible explanations: (1) the RFE channel may be a region where two MI current loops, forced by independent voltage generators, couple through a poorly conducting ionosphere and (2) the reversed flow channel may be the ionospheric footprint of an inverted V‐type coupling region. Electron beams of