it causes geomagnetic storms and generates auroras.
A geomagnetic storm, often referred to as a magnetic storm, is a brief disruption of the Earth's magnetosphere brought on by an interaction between the magnetic fields of the Sun and the Earth. The magnetosphere is first compressed by the rise in solar wind pressure. The magnetic field of the solar wind interacts with the magnetic field of the Earth and releases more energy into the magnetosphere.
A natural light show in the Earth's sky called an aurora is most frequently observed in high-latitude areas (around the Arctic and Antarctic).
The magnetosphere is impacted by the solar wind, which causes auroral events. Coronal holes and coronal mass ejections accelerate the solar wind, which causes significant disruptions. The paths of charged particles in the magnetospheric plasma are changed by these disruptions. These particles precipitate into the high atmosphere (thermosphere/exosphere), primarily electrons and protons.
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