Atmosphere Layers

Travel upward through the protective layers surrounding Earth.

Troposphere

The troposphere contains most atmospheric mass and nearly all weather.

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Stratosphere

The stratosphere contains the ozone layer, which absorbs much of the Sun's harmful ultraviolet radiation.

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Mesosphere

Most meteors burn up in the mesosphere as collisions with air particles heat them.

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Thermosphere

Sparse gases in the thermosphere absorb energetic solar radiation and can reach very high temperatures.

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Exosphere

The exosphere is the outermost region, where particles are so far apart that some escape into space.

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Boundaries

Pauses between layers mark changes in temperature trend.

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Troposphere

The troposphere contains most atmospheric mass and nearly all weather. Temperature generally decreases with height because the surface warms the air from below.

Stratosphere

The stratosphere contains the ozone layer, which absorbs much of the Sun's harmful ultraviolet radiation. Temperature rises with height as ozone captures solar energy.

Mesosphere

Most meteors burn up in the mesosphere as collisions with air particles heat them. It is the coldest major atmospheric layer near its upper boundary.

Thermosphere

Sparse gases in the thermosphere absorb energetic solar radiation and can reach very high temperatures. Auroras glow here when charged solar particles excite atmospheric gases.

Exosphere

The exosphere is the outermost region, where particles are so far apart that some escape into space. It gradually blends into interplanetary space rather than ending at a sharp edge.

Boundaries

Pauses between layers mark changes in temperature trend. The tropopause caps most weather, while the stratopause, mesopause, and thermopause separate higher regions.