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How do contrails form?
Quick answer
Contrails form when hot, moist exhaust from jet engines meets frigid air at cruising altitude. The water vapour condenses onto soot particles and instantly freezes into ice crystals, creating a visible line. Whether the line vanishes in seconds or lingers for hours depends on the humidity and temperature of the surrounding air.
Contrails form when hot, humid exhaust from aircraft engines mixes with cold, low-pressure air at high altitudes, causing water vapour to condense and freeze into ice crystals. They persist when the surrounding air is already humid and cold enough to keep the ice from sublimating.
Step by step
- A jet engine burns fuel, releasing a stream of hot gas that contains water vapour, carbon dioxide and tiny soot particles.
- The exhaust exits into ambient air that is typically −40 °C or colder at cruising altitude, causing rapid cooling of the plume.
- The sudden cooling makes the water vapour supersaturated, so it condenses onto the soot particles and forms microscopic liquid droplets.
- Those droplets freeze almost instantly into ice crystals, which scatter light and appear as a white line behind the aircraft.
- If the surrounding air is humid and cold, the ice crystals grow and the contrail persists; if the air is dry, the crystals sublimate and the trail disappears.
Key things to understand
- Jet engines burn fuel, producing exhaust that, besides heated air, carries water vapour, carbon dioxide and soot particles.
- At cruising altitudes of 8–12 km (26,000–39,000 ft), air is typically −40 °C or colder and often low in pressure.
- The sudden mixing of hot exhaust with cold ambient air creates a temporary supersaturation of water vapour.
- Water vapour condenses onto soot particles from the exhaust, forming tiny liquid droplets that quickly freeze into ice crystals.
- Whether the contrail lingers or fades depends on the surrounding humidity: dry air makes it evaporate quickly, humid air lets it spread.
Labelled diagram
- Engine exhaust
Hot gas with water vapour, CO2 and soot leaves the engine nozzle.
- Cold ambient air
At 8–12 km, air is −40 °C or colder, causing rapid cooling.
- Condensation
Water vapour condenses onto soot particles, forming tiny droplets.
- Freezing
Droplets freeze into ice crystals, creating a visible white line.
- Persistence or fade
Humid air lets crystals grow and spread; dry air makes them sublimate.
Real-world examples
- On a clear day over London, you can often see planes leaving short-lived contrails that vanish within a minute as they fly through dry air.
- Over the North Atlantic, where humidity is often high, contrails from transatlantic flights can spread into wide cirrus sheets that last for hours.
- During the Second World War, heavy bomber formations at high altitude sometimes created multiple contrails that made them easier to spot from the ground.
- Near airports, you rarely see contrails because aircraft are usually below the cold, high-altitude layer where ice crystals can form.
Common mistake
✗ Myth: Contrails are chemical trails deliberately sprayed by aircraft.
✓ Fact: Contrails are simply ice clouds formed from water vapour and soot in engine exhaust. Atmospheric scientists have sampled contrails directly and found only water ice and normal combustion products, with no evidence of secret chemical spraying.
People also ask
What causes contrails?
Why do contrails sometimes stay for hours?
Do contrails contribute to global warming?
Why do some contrails disappear quickly while others spread across the sky?
At what altitude do contrails form?
Do contrails affect the climate?
Are contrails the same as chemtrails?
Part of the guide: Water & Weather Phenomena →

