Linked from

The 27 pages that link to Greenhouse gas, each with the reason it gives.

• Air pollutionCompared with: Some pollutants also warm the climate, but many greenhouse gases are not directly toxic at ambient levels.

• Ice coreRelated: Core air samples track past concentrations of gases that influence Earth's energy balance.

• Carbon footprintNarrower topic: Carbon footprints aggregate emissions from these heat-trapping gases.

• HydrocarbonNarrower topic: Burning hydrocarbons releases carbon dioxide, a major greenhouse gas.

• Pleistocene glaciationRelated: Changing carbon dioxide and methane levels reinforced Pleistocene climate swings.

• Carbon offsetNarrower topic: Offsets address emissions of these heat-trapping gases.

• HydrofluorocarbonNarrower topic: HFCs are synthetic greenhouse gases whose emissions add to radiative forcing.

• Soil carbon sequestrationRelated: Soil carbon changes can affect atmospheric carbon dioxide, while management also affects other gases.

• Crude oilRelated: Burning crude-oil products releases carbon dioxide, a major greenhouse gas.

• Ice ageNarrower topic: Carbon dioxide and methane changes amplify temperature shifts across glacial cycles.

• Last Glacial PeriodNarrower topic: Carbon dioxide and methane concentrations changed alongside temperature and helped amplify climate shifts.

• Quaternary glaciationRelated: Changes in carbon dioxide and methane reinforced glacial cooling and interglacial warming.

• Dimethyl etherNarrower topic: The climate impact of dimethyl ether depends partly on its feedstock and production emissions.

• Atmospheric absorptionRelated: Greenhouse gases provide many of the atmosphere’s strongest infrared absorbers.

• Hypervalent moleculeNarrower topic: Sulfur hexafluoride is an exceptionally potent greenhouse gas, linking a canonical example to climate impacts.

• SevofluraneRelated: Exhaled sevoflurane reaches the atmosphere, where its persistence and warming effect raise environmental concerns.

• Fluorine chemistryNarrower topic: Some fluorinated gases have exceptionally high heat-trapping effects and long atmospheric lifetimes.

• Atmospheric aerosolCompared with: Unlike aerosols, greenhouse gases are molecular gases that generally warm the climate.

• SeagrassRelated: Disturbed seagrass sediments can release stored carbon as carbon dioxide.

• By-productBroader topic: Some production by-products, especially carbon dioxide and methane, contribute to climate change.

• Eunice Newton FooteNarrower topic: Foote’s results concerned gases later classified by their role in atmospheric heat absorption.

• IsofluraneRelated: Wasted isoflurane is released into the atmosphere and contributes to anesthetic-related emissions.

• HaloalkaneNarrower topic: Some fluorinated haloalkanes trap substantial heat despite low atmospheric concentrations.

• Last InterglacialNarrower topic: Carbon dioxide and methane levels provide context for the interval's warmth beyond orbital forcing.

• 1,1,1,2-TetrafluoroethaneRelated: R-134a absorbs infrared radiation and warms the climate when released.

• Carbon tetrafluorideNarrower topic: CF₄’s infrared absorption makes its persistent emissions relevant to climate change.

• Climate change in JapanRelated: Human emissions of these gases drive the global warming affecting Japan.