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Contrails

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What are contrails?

contrails picture 1We have all seen white streaks in the sky like those in the picture. What we are seeing are trails of ice crystals left in the wakes of jet aircraft. These condensation trails (known as 'contrails') sometimes persist for many minutes or even hours. On other occasions, they disappear quite quickly.

The exhausts of aircraft engines are hot and moist, the water vapour in them coming mostly from combustion of hydrogen in the aircraft's fuel. Behind an aircraft, exhaust gases cool rapidly, mainly from mixing with their surroundings but also to a small extent as a result of radiation loss. This cooling takes a finite time (a fraction of a second), so there is normally a gap of some 50 to 100 m behind an aircraft before a contrail appears. The water droplets that are produced freeze very rapidly if the temperature is low enough. The resulting trails of ice crystals persist and spread if the atmosphere at contrail level is moist enough. Contrails (and water droplets) form when the saturation vapour pressure with respect to liquid water is exceeded. They persist when the air is saturated or supersaturated with respect to ice.
contrails 2

 

Once formed, contrails are distorted by upper winds and spread by diffusion, and curtains of ice crystals can sometimes be seen falling from them.

Persistent trails often form large patches of fibrous clouds that look like cirrus, cirrocumulus or cirrostratus. Thus, old contrails sometimes cannot be distinguished from these clouds.

 

Supercooling

airplane

Supercooling is a normal occurrence in the atmosphere. Clouds composed of water droplets can persist at temperatures well below 0°C, even at temperatures below -30°C. At temperatures below about -40°C, however, all cloud droplets freeze very quickly. On long-haul routes, commercial aircraft usually reach altitudes of 10 to 12 km, where temperatures are typically below -40°C. Planes on these routes therefore tend to leave contrails behind them. Over the British Isles, trails rarely form below about 8 km in summer, 6 km in winter. When the weather is as cold as it often is in mid-winter in Alaska, Siberia and central Canada, contrails can even form at ground level. Indeed, airfields in these regions have sometimes had to be closed when low-level clouds (ice fogs) composed of aircraft-generated ice crystals have proved persistent.

 

Condensation on Windows

Condensation can often be seen on windows and doors when a room is hot and the air outside is very cold. We can demonstrate this by heating a beaker of ice (right) with a bunsen burner and observing the outside of the beaker.

Questions: