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magnetic reconnection

atmospheric science

Quick Summary

Magnetic reconnection is a fundamental process in atmospheric science where the Sun's magnetic field, carried by the solar wind, links with Earth's magnetic field. This interaction occurs within Earth's magnetosphere, a region shaped by the solar wind.

When these magnetic fields connect, energy is released through dynamic reconfigurations of the magnetosphere, known as geomagnetic substorms. This process often leads to energetic particles precipitating into the ionosphere, causing visible auroral displays. Magnetic reconnection also generates a magnetospheric electric field and drives magnetospheric convection, influencing phenomena like magnetic storms and the Van Allen radiation belts.12

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