Understanding aurora
Aurora colours explained
The colour of an aurora display tells you something specific about altitude and atmospheric composition. Green means energetic particles hitting oxygen at around 100 km. Red means the same interaction, much higher up. Here is what each colour means.
Why aurora produces different colours
Charged particles from the solar wind collide with gas molecules in the upper atmosphere. Each gas at each altitude emits a specific wavelength of light when excited. The colour you see depends on which gas was hit and at what altitude the collision happened.
This is the same principle as a neon sign: a sealed tube of gas produces a fixed colour because you are always exciting the same atoms at the same pressure. The atmosphere works like a stack of tubes at different pressures, each producing a different output when energised.
Colour by colour breakdown
Each aurora colour corresponds to a specific gas, altitude range, and physical process. The rarity of each colour tracks with how unusual the conditions required to produce it are.
Green (557.7 nm) - the most common colour
Oxygen atoms at 100-150 km altitude. Green dominates because oxygen is abundant at this altitude and this is where most auroral particles deposit their energy. An oxygen atom takes around 0.7 seconds to release this emission - long enough to build a stable visible glow. Visible from Kp 3 upward from high latitudes.
Red (630 nm) - high altitude, high activity
Oxygen atoms at 200-300 km altitude. Much rarer than green. The atmosphere is thin enough at this height that oxygen atoms can remain excited for up to 2 minutes before another collision occurs, giving them time to emit red light. Strong red displays require G2+ storms and energetic particle fluxes. Red is more common during solar maximum and tends to appear as a slow diffuse glow at the top of a display rather than moving curtains.
Blue and violet (427.8 nm and 391.4 nm) - the lower edge
Ionised nitrogen molecules at 60-100 km altitude. Appear as a blue fringe at the base of green curtains during stronger displays. Nitrogen produces several emission lines including blue and red-purple wavelengths. Usually visible in photographs before the naked eye registers them.
Pink and magenta - the lower border on bright displays
A mix of nitrogen emissions (red-purple) and green oxygen at the very base of a display, around 90-100 km. Appears as a distinct pink lower border on bright curtains. Often visible during G3+ storms. More common photographically but can be seen with the naked eye during strong events.
White - not a distinct emission
White aurora appears when multiple colour channels overlap and saturate. This is more common in photography than to the naked eye. A camera sensor pushed into saturation by a bright multi-colour display will render the overlap zone as white.
What colours are visible to the naked eye
Camera sensors are more sensitive to certain wavelengths than the human eye at night. Green (557.7 nm) falls within the range of the rod cells used in scotopic (dark-adapted) vision, so green aurora registers clearly. Red (630 nm) is harder for dark-adapted eyes - most people see faint red displays as pale grey or white until activity is strong enough to make the emission bright.
Blue and violet are also difficult for the naked eye but appear clearly in photographs with appropriate exposure times of 5-15 seconds. A test shot facing north will often show colour the eye cannot detect. This is particularly useful at Kp 3-4, where the display may look faint to you but is clearly green on camera.
During a strong storm (Kp 7+), red aurora becomes clearly visible to the naked eye. The May 2024 G5 storm produced red aurora visible across Spain, Texas, and New Zealand - levels bright enough that even the eye's reduced red sensitivity was overcome.
What aurora colour tells you about Kp
Green aurora can appear at Kp 3-4 from high latitudes. Red at the top of a display usually indicates Kp 5+. A full multi-colour display with visible red and pink requires Kp 6 or higher and typically a genuine geomagnetic storm.
If you can see clearly distinct red above the green, Kp is almost certainly at G2 or above. Pink borders at the base of curtains suggest G3. An overhead display with green, red, and pink all visible simultaneously is consistent with G4-G5 conditions. Colour can serve as a rough on-site activity gauge when you do not have a data connection.
Solar maximum and colour variety
During solar maximum - which spans 2025-2026 for the current cycle - higher energy particle fluxes penetrate deeper into the atmosphere and also excite oxygen at greater heights. This produces more frequent red displays and extends the vertical extent of the aurora visible at any given latitude.
The number of displays increases near solar maximum, but the colour variety is one of the most pronounced changes. Observers at mid-latitudes who have watched aurora for years consistently note that red and pink are more common at cycle peaks. If you have not seen a multi-colour display before, the 2025-2026 window offers better odds than any other period in the next decade.
Related pages
What Causes the Northern Lights?
The solar and magnetic physics that drives aurora borealis.
What Is the Kp Index?
How geomagnetic activity levels relate to aurora visibility.
Solar Maximum 2025-2026
Why this solar cycle peak is producing more red aurora than usual.
Aurora Photography Settings
Camera settings to capture colour that the naked eye misses.
Common questions
Questions about aurora colour, what determines it, and why cameras show more than your eyes do.
Why is aurora usually green?
Why does aurora turn red sometimes?
Can aurora be other colours?
Why do photos show more colour than I saw?
Sean Barraclough
Creator of Aurora Tonight