Greenhouse Gases

Explore the different gases that trap heat and their varying impacts on climate

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Select a Greenhouse Gas

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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%
Nβ‚‚O
Long lifetime
12%
Others
HFCs, PFCs, etc.
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