Greenhouse gases play a crucial role in climate change and atmospheric science. They trap heat in the atmosphere, influencing weather patterns and global temperatures. Understanding these gases, like CO2 and methane, is essential for addressing environmental challenges and promoting sustainability.
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Carbon dioxide (CO2)
- Major greenhouse gas produced by burning fossil fuels, deforestation, and industrial processes.
- Has a long atmospheric lifetime, contributing to long-term climate change.
- Absorbs infrared radiation, leading to the greenhouse effect and global warming.
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Methane (CH4)
- More effective than CO2 at trapping heat in the atmosphere, with a global warming potential 25 times greater over 100 years.
- Emitted during the production and transport of coal, oil, and natural gas, as well as from livestock and other agricultural practices.
- Shorter atmospheric lifetime than CO2, but significant in the near term for climate change.
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Water vapor (H2O)
- The most abundant greenhouse gas, but its concentration is primarily controlled by natural processes.
- Acts as a feedback mechanism; as the atmosphere warms, it holds more water vapor, which further enhances warming.
- Plays a crucial role in weather patterns and the hydrological cycle.
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Nitrous oxide (N2O)
- Emitted from agricultural activities, fossil fuel combustion, and certain industrial processes.
- Has a global warming potential approximately 298 times that of CO2 over a 100-year period.
- Contributes to ozone layer depletion in the stratosphere.
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Ozone (O3)
- Found in two layers of the atmosphere: the stratosphere (good ozone) and the troposphere (bad ozone).
- Tropospheric ozone is a harmful pollutant and a potent greenhouse gas formed from chemical reactions between VOCs and NOx in sunlight.
- Stratospheric ozone protects life on Earth by absorbing harmful ultraviolet radiation.
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Chlorofluorocarbons (CFCs)
- Synthetic compounds used in refrigeration, air conditioning, and aerosol propellants.
- Known for their role in ozone depletion in the stratosphere.
- Have a high global warming potential, leading to their phase-out under the Montreal Protocol.
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Hydrofluorocarbons (HFCs)
- Used as substitutes for CFCs in refrigeration and air conditioning.
- While they do not deplete the ozone layer, they are potent greenhouse gases with a high global warming potential.
- International efforts are underway to phase down HFCs under the Kigali Amendment to the Montreal Protocol.
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Perfluorocarbons (PFCs)
- Byproducts of aluminum production and semiconductor manufacturing.
- Extremely potent greenhouse gases with a global warming potential thousands of times greater than CO2.
- Long atmospheric lifetimes, contributing to long-term climate change.
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Sulfur hexafluoride (SF6)
- Used in electrical insulation and in the manufacturing of semiconductors.
- Has a global warming potential over 22,000 times that of CO2, making it one of the most potent greenhouse gases.
- Very long atmospheric lifetime, contributing to its impact on climate change.
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Nitrogen trifluoride (NF3)
- Used in the production of flat-panel displays and solar cells.
- Has a global warming potential over 17,000 times that of CO2.
- Its atmospheric concentration is increasing, raising concerns about its contribution to climate change.