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Cluster observations of an ion-scale current sheet in the magnetotail under the presence of a guide field

Cluster observations of an ion-scale current sheet in the magnetotail under the presence of a guide field

Publication date: 26 April 2008

Authors: Nakamura, R. et al.

Journal: J. Geophys. Res.
Volume: 113
Issue: A07
ID: A07S16
Year: 2008

Copyright: American Geophysical Union

We report on Cluster observations of a thin current sheet interval under the presence of a strong |BY| during a fast earthward flow interval between 1655 UT and 1703 UT on 17 August 2003. The strong |BY| in the tail could be associated with a strong IMF |BY|, but the large fluctuations in BY, not seen in the IMF, suggest that a varying reconnection rate causes a varying transport of BY-dominated magnetic flux and/or a change in BY due to the Hall-current system. During the encounter of the high-speed flow, an intense current layer was observed around 1655:53 UT with a peak current density of 182 nA/m², the largest current density observed by the Cluster four-spacecraft magnetic field measurement in the magnetotail. The half width of this current layer was estimated to be ~290 km, which was comparable to the ion-inertia length. Its unique signature is that the strong current is mainly field-aligned current flowing close to the center of the plasma sheet. The event was associated with parallel heating of electrons with asymmetries, which suggests that electrons moving along the field lines can contribute to a strong dawn-to-dusk current when the magnetotail current sheet becomes sufficiently thin and active in a strong guide field case.

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Last Update: Sep 1, 2019 9:09:03 AM
27-Jul-2021 15:47 UT

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