Infrared
Infrared (IR) radiation is electromagnetic radiation of a wavelength longer than visible light, but shorter than microwave radiation. The name means "below red" (from the Latin infra, "below"), red being the color of visible light of longest wavelength. Infrared radiation spans three orders of magnitude and has wavelengths between 700 nm and 1 mm.
The Earth as an infrared emitter
The Earth's surface absorbs visible radiation from the sun and re-emits much of the energy as infrared back to the atmosphere. Certain gases in the atmosphere, chiefly water vapor, but also carbon dioxide, methane, nitrous oxide, sulfur hexafluoride, and chlorofluorocarbons, absorb this infrared, and re-radiate it in all directions including back to Earth. Thus, the greenhouse effect, keeps the atmosphere and surface much warmer than if the infrared absorbers were absent from the atmosphere.
Related Topics:
Earth - Absorb - Sun - Atmosphere - Water - Carbon dioxide - Methane - Nitrous oxide - Sulfur hexafluoride - Chlorofluorocarbons - Greenhouse effect
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~ Table of Content ~
| ► | Introduction |
| ► | Different regions in the infrared |
| ► | Telecommunication bands in the infrared |
| ► | The Earth as an infrared emitter |
| ► | Applications |
| ► | History |
| ► | See Also |
| ► | External Links |
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