Aurora, also known as the polar lights, refers to natural light displays predominantly seen in high-latitude regions around the Arctic and Antarctic. In the Northern Hemisphere, it is called the aurora borealis or northern lights, while in the Southern Hemisphere, it is known as the aurora australis or southern lights. Auroras are caused by the interaction of charged particles from the sun, primarily electrons and protons, with the Earth's magnetosphere. When these particles collide with gases in the Earth's atmosphere, such as oxygen and nitrogen, they emit light, creating vibrant, colorful displays in the sky.

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