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The Contrail Education Project

 

Contrail Science

What are contrails?

Contrails are clouds formed when water vapor condenses and freezes around small particles (aerosols) that exist in aircraft exhaust. Some of that water vapor comes from the air around the plane; and, some is added by the exhaust of the aircraft.
The exhaust of an aircraft contains both gas (vapor) and solid particles. Both of these are important in the formation of contrails. Some elements of the exhaust gasses are not involved in contrail formation but do constitute air pollution. Emissions include carbon dioxide, water vapor, nitrogen oxides (NOx), carbon monoxide, hydrocarbons such as methane, sulfates (SOx), and soot and metal particles.

Are there different types of contrails?

Contrails are all made of the same materials and are formed in the same way, but exist for different lengths of time. Because of the differences in contrail "life-spans", contrails can be divided into three groups: short-lived, persistent (non-spreading), and persistent spreading. See the Contrail Formation Guide  [PDF] for more information on how contrails form or download a presentation [PDF] to learn how to "read" they sky.

Example of Short Lived Contrails Short-lived contrails look like short white lines following along behind the plane, disappearing almost as fast as the airplane goes across the sky, perhaps lasting only a few minutes or less. The air that the airplane is passing through is somewhat moist, and there is only a small amount of water vapor available to form a contrail. The ice particles that do form quickly return again to a vapor state.


Example of Persistent (non-spreading) contrails Persistent (non-spreading) contrails look like long white lines that remain visible after the airplane has disappeared. This shows that the air where the airplane is flying is quite humid, and there is a large amount of water vapor available to form a contrail. Persistent contrails can be further divided into two classes: those that spread and those that don't. Persistent contrails look like long, narrow white pencil-lines across the sky.


Example of Persistent Spreading  contrails Persistent spreading contrails look like long, broad, fuzzy white lines. This is the type most likely to affect climate because they cover a larger area and last longer than short-lived or persistent contrails.


Contrail cousins are things that look like contrails but actually arise from a different physical process. For example, under the right conditions you will see vapor trails form from the wingtips of a jet on takeoff or landing. This phenomenon results from a decrease in pressure and temperature in the wingtip vortex. If conditions are right, liquid water drops form inside the vortex and make it visible. These evaporate very quickly after they form.

Can contrails move, or do they stay in the location where they were formed?

Because contrails are formed at high altitudes where the winds are usually very strong, they will move away from the area where they originated. Often, when we look up into the sky, we will see old persistent contrails that formed far away but moved overhead because of the wind.

How are contrails different from other clouds?

Contrails are "human-induced" clouds since they are formed by water vapor condensing and freezing on particles from airplane exhaust. Contrails are always made of ice particles, due to the very cold temperatures at high altitude. Other types of clouds can be formed by water vapor that condenses on particles which are present in the atmosphere due to many sources, such as from volcanoes or dust storms, not specifically from aircraft exhaust. Those clouds are sometimes made of water droplets, and sometimes ice crystals, depending on the temperature where they form.

Contrails only form at very high altitudes (usually above 8 km) where the air is extremely cold (less than -40 degrees C). Other clouds can form at a range of altitudes, from very close to the ground, such as fog, to very high off the ground, such as cirrus clouds.

When were contrails first observed?

Contrails were first noticed during high-altitude flights in the 1920's. However, interest in contrails really blossomed during WWII when bombers could be sighted from miles away. In fact, numerous WWII veteran accounts tell of problems to aviation due to massive contrail formations. Planes could not find their targets, and sometimes collided with each other. In 1953, a scientist named H. Appleman published a chart that can be used to determine when a jet airplane would or would not produce a contrail.

What do contrails contain?

Persistent contrails are ice clouds, so they are mostly made of ice. They also are likely to contain aircraft exhaust products (including soot and dissolved gases like sulfur dioxide) , but they are overwhelmingly made from moisture condensed out of the surrounding air. In one example reported by Knollenburg (October 1972, Journal of the Atmospheric Sciences, Pages 1367-1374), the amount of moisture released by the burning of jet fuel from a research aircraft was 1.7 grams of water for every meter of flight path. However, the total water measured in a persistent contrail produced by the aircraft was conservatively measured (that is, it was likely an underestimate) to be between 20700 to 41200 grams of water for every meter of the contrail path! Nearly all of the contrail is created from the moisture in the atmosphere.

The exhaust products from aircraft are often measured using an emission index (mass (in grams) of exhaust product divided by mass (in kg) of jet fuel burned). The sum total of the exhaust products turns out to be greater than one (the mass of the exhaust products is greater than the mass of the fuel burned because the exhaust contains oxygen from surrounding air combined with fuel during combustion).

The emission indices of some of the products of jet fuel combustion are as follows:


Carbon dioxide (CO2): 3150
Water vapor (H20): 1230 (Knollenburg (1972) estimated 1370)
Nitric oxides (NOX): 8 to 20
Sulfur dioxide (SO2): 0.5


The emission indices of most other products such as unburned hydrocarbons and carbon monoxide are likely to be on the order of 2 or less. Thus for the Knollenburg example, the research aircraft burned 1.26 grams of fuel per meter of flight, so the concentrations of most constituents (other than CO2 or water/ice) are going to be at most 20*1.26/1000=0.025 gram per meter of flight compared to 21,000 to 41,000 grams for ice.

To learn more about contrails access this repository of articles associated with Contrail Science.



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