The Northern Lights, or Aurora Borealis, are caused by interactions between the Earth's magnetic field and particles from the Sun. When solar storms eject electrons and protons from the Sun's surface, they travel through space and enter the Earth's atmosphere near the magnetic poles. There, the particles excite oxygen and nitrogen atoms in the atmosphere, causing them to glow in colorful patterns of light known as the Northern Lights. The size and shape of the Aurora is determined by the level of activity on the Sun - more active periods result in a larger and more extended light display.