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Thus, the exosphere no longer behaves like a gas, and the particles constantly escape into space.

These free-moving particles follow ballistic trajectories and may migrate in and out of the magnetosphere or the solar wind.

The three major constituents of air, and therefore of Earth's atmosphere, are nitrogen, oxygen, and argon.

Water vapor accounts for roughly 0.25% of the atmosphere by mass.

The exosphere is located too far above Earth for any meteorological phenomena to be possible.

However, the aurora borealis and aurora australis sometimes occur in the lower part of the exosphere, where they overlap into the thermosphere.

Various industrial pollutants also may be present as gases or aerosols, such as chlorine (elemental or in compounds), fluorine compounds and elemental mercury vapor.

The atmosphere has a mass of about 5.15 three quarters of which is within about 11 km (6.8 mi; 36,000 ft) of the surface.

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Filtered air includes trace amounts of many other chemical compounds.

Many substances of natural origin may be present in locally and seasonally variable small amounts as aerosols in an unfiltered air sample, including dust of mineral and organic composition, pollen and spores, sea spray, and volcanic ash.