substorm-wedge current system
Quick Summary
The substorm-wedge current system is a phenomenon observed during magnetospheric substorms, which are distinct events from magnetic storms. This system involves the diversion of tail current into the ionosphere, creating westward and eastward electrojets. These currents enhance auroral activity and cause sudden changes in Earth's magnetic field, inducing strong electric fields. These fields energize particles, leading to auroras and increased atmospheric conductivity. On the ground, these effects can disrupt electrical transmission lines and pipelines.1
Magnetospheric substorms are characterized by an "expansion phase" where magnetic field lines reconnect, releasing energy and causing auroral displays. The "substorm-wedge current system" is crucial in this process, as it helps localize the reconnection region and divert current to the ionosphere. This system is a key component in understanding the dynamics of Earth's magnetosphere during these events.123
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