Greenhouse Gases
Explore the different gases that trap heat and their varying impacts on climate
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Carbon Dioxide (COβ)
The most important greenhouse gas, produced by burning fossil fuels and deforestation.
Current Level
420 ppm
Pre-Industrial
280 ppm
Atmospheric Lifetime
100-300 years
Global Warming Potential
1x COβ
Major Sources:
Fossil fuel combustionDeforestationIndustrial processes
How Greenhouse Gases Trap Heat
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Incoming Solar Radiation
Visible light from the sun passes through greenhouse gases and warms Earth's surface.
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Outgoing Infrared Radiation
Heat radiated from Earth as infrared light is absorbed and re-emitted by greenhouse gases.
The Molecular Mechanism
Greenhouse gases have molecular structures that vibrate when they absorb infrared radiation. This vibration transfers energy to surrounding air molecules, increasing atmospheric temperature.
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Asymmetric Molecules
Bend and stretch to absorb IR
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Energy Transfer
Vibrations heat the air
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Global Warming
Atmosphere retains more heat
Greenhouse Gas Contributions to Warming
63%
COβ
Primary contributor
19%
CHβ
High potency
6%
NβO
Long lifetime
12%
Others
HFCs, PFCs, etc.