The colors of the aurora largely result from light released by excited oxygen atoms and nitrogen molecules and ions. Have you ever wondered how aurora colors work and why sometimes the aurora is just green or red, while other times it is a whole rainbow of hues? The short answer is that nitrogen and oxygen in the upper atmosphere release light in specific colors in response to solar radiation. Here we learn what causes the different colors in the aurora borealis (northern lights) and the aurora australis (southern lights).
What looks green to the north might glow red overhead and purple to the south-all at once. Second, local conditions matter more than most aurora guides admit. Thin clouds scatter and desaturate colors.
City lights and camera white balance can shift tones toward yellow or magenta. Auroras are vibrant light displays created when energetic particles from the Sun interact with Earth's magnetic field and atmosphere. These events, also seen on other planets like Saturn and Jupiter, result in a range of colors depending on altitude and the atmospheric gases involved.
Scientists study auroras using tools like rockets, balloons, and ground-based instruments, while public. The following colours can be seen when the northern lights are in the sky. Green: Green is the most common colour seen from the ground and is produced when charged particles collide with oxygen molecules at altitudes of 100 to 300 km.
Pink and dark red: Occasionally, the lower edge of an aurora will have a pink or dark red fringe, which is produced by nitrogen molecules at altitudes of around. Green, red and purple aurora over Mefjord in Norway. (Getty Images/ Westend61) During intense outbursts of the northern lights, onlookers may see three or four colors at the same time.
Learn why aurora colors glow green and red, how ionized particles collide with atmosphere layers, the physics of green aurora, and the science behind red aurora. The majority of auroral displays are predominantly green for two reasons: the first of which is that the human eye detects green more readily than other colours. This is why photographic images of the Northern Lights will often show colours that were not visible at the time to the naked eye.
However, the main factor in determining the colours of any given display is the altitude at which the. While green is the most common colour to see in the aurora, and red the second most common, there are also other colours. In particular, ionised nitrogen molecules (N₂⁺, which are missing one electron and have a positive electrical charge), can emit blue and red light.
This can produce a magenta hue at low altitudes. The northern and southern lights, auroras visible from the poles, glow with a range of different colored lights. Here's the reason for each of those colors.