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The greenhouse effect

Without in its , the Earth would be about 32掳C colder on average than it is now. Greenhouse gases:

  • absorb heat radiated from the Earth
  • then release in all directions, which keeps the Earth warm

An example of greenhouse gases are carbon dioxide, methane and water vapour.

from the Sun is only partly absorbed by the Earth. The rest is radiated into the atmosphere. Although some of the infrared radiation escapes, some is absorbed by greenhouse gases. This keeps the energy in the atmosphere, warming it up. This gradual warming of the atmosphere over many years is referred to as .

The diagram gives more details about this process. It is called the .

Image and text to explain how the greenhouse effects works.
Figure caption,
How the greenhouse effect works