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Three-dimensional magnetic structure of the plasmoid created in the magnetotail at substorm onset

Journal Article · · Geophys. Res. Lett.; (United States)
Reconnection of magnetic field lines at a neutral line that forms in the near-earth region of the plasma sheet at substorm onset creates, from some longitudinal sector of the plasma sheet, a plasmoid that is then free to flow out of the magnetotail into the magnetosphere's wake. The magnetic field in the departing plasmoid frequently displays a strong positive or negative Y/sub S/M component that has been difficult to reconcile with the reconnection geometry as it is traditionally depicted in two dimensions. We show that this deviation of the magnetic field is a manifestation of a draping of the newly reconnected field line loops toward the tail's central (midnight) meridian and that the draping is a consequence of the three-dimensional plasma flow associated with the reconnection process.
Research Organization:
University of California, Los Alamos National Laboratory, Los Alamos, NM 87545
OSTI ID:
5496264
Journal Information:
Geophys. Res. Lett.; (United States), Journal Name: Geophys. Res. Lett.; (United States) Vol. 9:3; ISSN GPRLA
Country of Publication:
United States
Language:
English

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