Aurora (theory)

Aurora, in a scientific context, typically refers to the Aurora Borealis (Northern Lights) or Aurora Australis (Southern Lights). These phenomena occur when charged particles from the Sun collide with Earth's magnetic field and atmosphere. This interaction excites atmospheric gases like oxygen and nitrogen, causing them to emit light. The colors and patterns result from the type of gas and altitude of the collisions. Essentially, auroras are natural light displays created by solar activity interacting with Earth's magnetic environment, demonstrating a fascinating connection between our planet and the Sun.