Retreat and reformation of X-line during quasi-continuous reconnection at the high- latitude magnetopause

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2706 Cusp, 2723 Magnetic Reconnection (7526, 7835), 2724 Magnetopause And Boundary Layers, 2784 Solar Wind/Magnetosphere Interactions

Scientific paper

It is known that magnetic reconnection can persist for hours, e.g., at Earth's magnetopause. However, it remains unknown in what manner reconnection can be continuous in regions where flow tangential to the current sheet is significant on one side of the current sheet, such as at the high- latitude or flank magnetopause; whether a single X-line sits still and remains active for an extended period of time, or an X-line retreats with the tangential flow and then a new X-line reforms at or near the original reconnection site. Here we present observations on 19-20 November 2006 by the Cluster spacecraft that were skimming the high-latitude dusk-flank magnetopause, which are consistent with more than one reconnection X-line present on the tailward side of the polar cusp under northward interplanetary magnetic field. Evidence of quasi-continuous reconnection over 16 hours exists in the form of Alfvenic acceleration of magnetosheath ions found almost always when either of the satellites traversed the magnetopause current layer. The data indicate that for most of the time, a dominant X-line was between Cluster and the cusp (sunward of Cluster), but ion velocity distributions consisting of two magnetosheath (shocked-solar-wind) populations demonstrate that for part of the time, more than one X-line existed. Further, the motion of reconnected field lines shows that some X-line(s) retreated tailward and was anti-sunward of Cluster. It is inferred that following the X-line retreat, another X-line reformed sunward of Cluster, leading to multiple X- lines.

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