What an aurora is
The Sun constantly emits a stream of charged particles, the solar wind. Earth’s magnetic field deflects most of them, but some are funneled toward the polar regions. There, at about 100 to 300 kilometers altitude, these particles collide with the atmospheric gases and make them glow: that is an aurora.
The color depends on the gas and the altitude. Green, the most common, comes from oxygen at roughly 100 to 200 kilometers; red comes from oxygen at higher altitudes; and purple and blue tones come from nitrogen. In the north it is called aurora borealis, and in the south, aurora australis.
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