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magnetosheath

atmospheric science

Quick Summary

The magnetosheath is a region of magnetic turbulence located between the magnetopause and the bow shock, approximately 10 to 13 Earth radii sunward. This area is characterized by erratic variations in both the magnitude and direction of Earth's magnetic field. It is believed to be caused by magnetohydrodynamic shock waves generated by high-velocity solar wind particles. The magnetosheath plays a role in the interaction between Earth's magnetosphere and the solar wind.12

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