The natural greenhouse effect
1. Sunlight (shortwave radiation) enters the earth passing through the atmosphere and is absorbed in the earth's surface
2. The absorbed energy warms the earth's surface while some of it is reflected by the earth back to space in the form of infrared or long-wave radiation
3. The energy that is reflected in space passes through the atmosphere where greenhouses gases are naturally present
4. These greenhouse gases (water vapor, carbon dioxide, methane, and nitrous oxide) absorb most of this energy and then re-emit it in different directions
5. Some of the sun's energy escapes into space while others become "trapped" because of the greenhouse gases that form a layer in the atmosphere
6. The "trapped" energy warms the earth and the lower part of the atmosphere – making the earth habitable for a living