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magnetopause

atmospheric science

Quick Summary

The magnetopause is the boundary of the magnetosphere, the region around Earth where magnetic phenomena are significant. This boundary, located about 10 Earth radii from the planet's center, is where the pressure of the solar wind balances the pressure of Earth's magnetic field. The magnetosphere is shaped like a comet, compressed on the side facing the Sun and extended into a long tail on the opposite side. This region is crucial in atmospheric science as it influences the behavior of charged particles in the atmosphere due to ionization and Earth's surface magnetic field. The magnetopause current system, also known as the Chapman-Ferraro current system, forms this boundary and influences Earth's magnetic field in space.12

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