Abstract
The structure of Earth's magnetosphere is poorly understood when the interplanetary magnetic field is northward. Under this condition, uncharacteristically energetic plasma is observed in the magnetotail lobes, which is not expected in the textbook model of the magnetosphere. Using satellite observations, we show that these lobe plasma signatures occur on high-latitude magnetic field lines that have been closed by the fundamental plasma process of magnetic reconnection. Previously, it has been suggested that closed flux can become trapped in the lobe and that this plasma-trapping process could explain another poorly understood phenomenon: the presence of auroras at extremely high latitudes, called transpolar arcs. Observations of the aurora at the same time as the lobe plasma signatures reveal the presence of a transpolar arc. The excellent correspondence between the transpolar arc and the trapped closed flux at high altitudes provides very strong evidence of the trapping mechanism as the cause of transpolar arcs.
Highlights
The night side of the terrestrial magnetosphere forms a structured magnetotail, consisting of a plasma sheet at low latitudes that is sandwiched between two regions called the magnetotail lobes (Fig 1.)
One Sentence Summary: Plasma observed in the magnetotail lobes is due to ‘trapped’ closed magnetic flux, and reveals the process behind the formation of transpolar arcs
This requires the presence of magnetic mirrors on both sides of the observation site, double loss cones are unambiguous indicators that the magnetic field lines observed by a spacecraft are closed
Summary
The night side of the terrestrial magnetosphere forms a structured magnetotail, consisting of a plasma sheet at low latitudes that is sandwiched between two regions called the magnetotail lobes (Fig 1.). One Sentence Summary: Plasma observed in the magnetotail lobes is due to ‘trapped’ closed magnetic flux, and reveals the process behind the formation of transpolar arcs.
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