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magnetotail current

atmospheric science
Also known as: tail current

Quick Summary

The magnetotail current is a system of electrical currents flowing from dawn to dusk on the nightside of Earth, extending far beyond 200 Earth radii. This current is generated by the motion of charged particles, primarily due to curvature drift, in a region where Earth's magnetic field is significantly stretched out into a tail-like configuration by the solar wind.1

This tail current is closely related to the magnetopause current and is produced by the same mechanism of charge deflection. However, it differs because a portion of the tail current flows within Earth's magnetic field in a region known as the plasma sheet. The overall configuration of Earth's magnetosphere, including the magnetotail, is a result of the interaction between Earth's magnetic field and the solar wind. This interaction can lead to phenomena like auroras, which are visible light emissions caused by charged particles from the solar wind colliding with Earth's upper atmosphere.123

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