Earth’s Energy Balance
Age 16 · Science
Solar radiation arrives as shortwave light, and Earth returns energy to space as infrared radiation. Greenhouse gases absorb some infrared and send part of it back toward the surface, keeping the planet warmer than it would be otherwise.
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Age 16: open this week
Browse Age 16In the picture
- Badge 1 sits on the Sun, the source of incoming solar radiation.
- Badge 2 sits on a cloud top where some shortwave sunlight is reflected away.
- Badge 3 sits on a greenhouse gas molecule in the atmosphere.
- Badge 4 sits where infrared radiation leaves Earth’s surface.
- Badge 5 sits on an infrared ray bending back toward Earth after interacting with a greenhouse gas molecule.
Examples
- A car interior warms in sunlight because visible light enters and infrared struggles to escape.
- A blanket traps body heat, similar to how greenhouse gases slow Earth’s heat loss.
Key takeaways
- Incoming solar radiation and outgoing infrared radiation must balance over time.
- Greenhouse gases reduce outgoing infrared, warming the surface and lower atmosphere.
Quiz: Earth’s Energy Balance (Age 16)
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In Earth’s energy budget, how does radiation arrive at the planet and how does it leave?
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What is the greenhouse effect’s main role in Earth’s energy balance?
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What does it mean for Earth’s energy budget to be balanced?
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