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The 71 pages that link to Greenhouse effect, each with the reason it gives.

• Climate changeRelated: Rising concentrations of heat-trapping gases strengthen this process.

• Carbon dioxideRelated: CO₂ contributes to atmospheric warming by absorbing infrared radiation emitted by Earth.

• Carbon cycleRelated: Rising atmospheric carbon dioxide strengthens this heat-trapping effect.

• Greenhouse gas emissionsRelated: Emissions strengthen this process by raising heat-trapping gas concentrations.

• Arctic amplificationRelated: Human-driven greenhouse warming supplies the background forcing that Arctic feedbacks intensify.

• Thermal radiationRelated: Earth's thermal emission interacts with atmospheric gases in this warming process.

• Radiative forcingRelated: Rising greenhouse-gas concentrations reduce outgoing infrared energy, producing positive forcing.

• Water vaporRelated: Water vapor absorbs infrared radiation and strengthens atmospheric warming.

• Planetary habitabilityRelated: It can keep surface water liquid beyond the range predicted from sunlight alone.

• Atmosphere of EarthRelated: Infrared-active gases shape the atmosphere’s surface temperature and energy balance.

• ClimateRelated: It explains how atmospheric composition influences Earth’s average temperature.

• Earth's energy budgetRelated: It alters how efficiently Earth emits absorbed energy to space.

• GreenhouseRelated: Solar energy enters through glazing, while reduced heat loss helps warm the enclosed space.

• Habitable zoneRelated: Atmospheric warming can keep surface water liquid farther from a star.

• Little Ice AgeRelated: Rising greenhouse gas concentrations help distinguish modern warming from historical cooling influences.

• Planetary atmosphereRelated: Atmospheric gases can slow the loss of heat radiated from a planet's surface.

• AtmosphereRelated: Infrared absorption by atmospheric gases raises Earth's surface temperature.

• John TyndallRelated: His gas-absorption experiments established a physical basis for atmospheric heat retention.

• Kirchhoff's law of thermal radiationRelated: The law relates atmospheric infrared emission to absorption at the same spectral modes.

• Climate change attributionRelated: Its intensification by human emissions is a central mechanism assessed in attribution.

• Climate modelingRelated: Models calculate how changing greenhouse-gas concentrations alter outgoing energy.

• Joseph FourierRelated: Fourier estimated how atmospheric gases affect Earth’s temperature in an early study of planetary heat.

• Radiative coolingRelated: Atmospheric infrared absorption limits how freely surface radiation escapes to space.

• Ocean warmingRelated: The enhanced greenhouse effect supplies the excess energy absorbed by the ocean.

• Climate scienceRelated: Changes in greenhouse gases alter the energy escaping to space.

• Arctic methane emissionsRelated: Methane emissions matter climatically because atmospheric methane strengthens this effect.

• TroposphereRelated: Tropospheric greenhouse gases retain heat and contribute to surface warming.

• Atmospheric absorptionRelated: Atmospheric absorption of outgoing infrared radiation is central to this warming process.

• Charles David KeelingRelated: Rising carbon dioxide matters because it strengthens this heat-trapping process.

• InterglacialRelated: Rising greenhouse-gas concentrations amplify orbital warming during deglaciation.

• OutgassingRelated: Outgassed carbon dioxide and water vapor can strengthen greenhouse warming when retained in an atmosphere.

• Anthropogenic climate changeRelated: Human emissions strengthen this natural heat-trapping process.

• Radiative equilibriumRelated: Atmospheric absorption makes the location and level of radiative balance consequential.

• Volcanic outgassingRelated: Outgassed carbon dioxide and water vapor can strengthen this warming when they accumulate.

• Climate change feedbacksRelated: Several major climate feedbacks work by changing this heat-trapping process.

• Outgoing longwave radiationRelated: Absorption delays some surface radiation’s escape, shifting emission to colder atmospheric layers.

• Katharine HayhoeRelated: The enhanced greenhouse effect explains the main physical cause of modern global warming.

• Radiation (physics)Related: Atmospheric radiation absorption helps determine Earth's surface temperature.

• Climate variability and changeRelated: Rising greenhouse-gas concentrations strengthen this heat-trapping process.

• Environmental issuesRelated: Emissions intensify this heat-trapping process and drive human-caused climate change.