Heat Trapped in the Air
Age 18 · Science
Carbon dioxide and methane molecules in the atmosphere absorb infrared radiation rising from Earth’s surface. They re-emit some of that energy back downward, so the surface becomes warmer than it would be without those gases.
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Age 18: open this week
Browse Age 18In the picture
- A yellow sun ray passing through the atmosphere: incoming solar energy reaches Earth’s surface.
- A carbon dioxide molecule in the atmosphere: it absorbs and re-emits infrared heat.
- A methane molecule in the atmosphere: it absorbs and re-emits infrared heat.
- A red wavy arrow rising from land: infrared heat leaves the warmed surface.
- A red wavy arrow escaping into space: some infrared heat is not absorbed and leaves the atmosphere.
Examples
- A car parked in the sun gets hotter inside because glass slows heat from escaping.
- A greenhouse stays warm because glass lets sunlight in but slows heat from leaving.
Key takeaways
- More carbon dioxide and methane in the air increase the amount of infrared heat returned to the surface.
- This added heat raises Earth’s average surface temperature.
Quiz: Heat Trapped in the Air (Age 18)
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What do carbon dioxide and methane molecules do to infrared heat in the atmosphere?
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What happens when there is more carbon dioxide and methane in the air?
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What happens to infrared heat that is not absorbed in the atmosphere?
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