Avrora Deis: 20240107062012-31 Min

The aurora occurs when charged particles from the sun interact with the Earth's magnetic field and atmosphere. These charged particles, primarily electrons and protons, originate from solar winds and coronal mass ejections. As they collide with atoms and molecules in the Earth's atmosphere, they excite them, causing them to emit light. The color of the aurora depends on the altitude at which the collisions occur and the type of particles involved. Green is the most common color, produced by collisions at altitudes of around 100 to 200 kilometers. Red is produced at higher altitudes, while blue and violet colors are produced at lower altitudes.