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greenhouse effect
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The greenhouse effect is how certain gases in Earth's atmosphere trap heat from the sun, similar to how a greenhouse keeps warmth inside. This matters because changes in these gases can affect global temperatures and climate patterns that impact life on Earth.
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Research
14,838 papers- Is the additional greenhouse effect already evident in the current climate?ReviewFresenius' journal of analytical chemistry · 2001Raschke EDOI: 10.1007/s002160100935
- Reassessing the greenhouse effect of biogenic carbon emissions in constructed wetlands.Journal of environmental management · 2024Hu L, Li Z, Kong L et al.DOI: 10.1016/j.jenvman.2024.120263
- CO2 and the greenhouse effect: present assessment and perspectives.ReviewCiba Foundation symposium · 1993Oeschger HDOI: 10.1002/9780470514436.ch2
- Election fireworks.Nature · 2008DOI: 10.1038/451001a
- Overlooked drivers of the greenhouse effect: The nutrient-methane nexus mediated by submerged macrophytes.Water research · 2024Mu J, Li Z, Lu Q et al.DOI: 10.1016/j.watres.2024.122316
- Editorial: Greenhouse Gases and Animal Agriculture Conference, Dublin, 2013.Animal : an international journal of animal bioscience · 2013Dewhurst RJDOI: 10.1017/S1751731113000827
- Capturing greenhouse gases.ReviewScientific American · 2000Herzog H, Eliasson B, Kaarstad ODOI: 10.1038/scientificamerican0200-72
- Greenhouse goo.Scientific American · 2013Biello DDOI: 10.1038/scientificamerican0713-56
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Article
Energy flows down from the sun and up from the Earth and its atmosphere. When greenhouse gases absorb radiation emitted by Earth's surface, they prevent that radiation from escaping into space, causing surface temperatures to rise by about 33 °C (59 °F).
The greenhouse effect occurs when heat-trapping gases in a planet's atmosphere prevent the planet from losing heat to space, raising its surface temperature. Surface heating can happen from an internal heat source (as in the case of Jupiter) or come from an external source, such as a host star. In the case of Earth, the Sun emits shortwave radiation (sunlight) that passes through greenhouse gases to heat the Earth's surface. In response, the Earth's surface emits longwave radiation that is mostly absorbed by greenhouse gases, reducing the rate at which the Earth can cool off.
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