Linked from

The 29 pages that link to Climate change feedbacks, each with the reason it gives.

• Climate changeBroader topic: Feedbacks such as ice loss can intensify or moderate initial warming.

• Radiative forcingRelated: Feedbacks modify the eventual warming associated with a given forcing.

• Climate sensitivityRelated: Feedbacks turn the initial warming from doubled carbon dioxide into a larger or smaller temperature response.

• Feedback loopRelated: It applies the reinforcing and balancing distinction to Earth's climate.

• Global warming potentialNarrower topic: GWP focuses on gas-driven radiative effects, not the full climate response and its feedbacks.

• Global warmingRelated: Feedbacks such as melting ice amplify the temperature response to forcing.

• ClimateRelated: Feedbacks determine how strongly climate responds to an initial disturbance.

• Greenhouse gasRelated: Warming can trigger feedbacks that alter greenhouse-gas concentrations and strengthen or weaken their effects.

• Carbon sinkRelated: Sink responses to warming can reinforce or counteract climate change.

• Earth's energy budgetRelated: Feedbacks alter how much the budget imbalance changes temperature.

• Little Ice AgeNarrower topic: Feedbacks help explain how modest external influences could produce persistent regional cooling.

• Permafrost carbon cycleRelated: Carbon emissions from thaw can amplify the warming that caused the thaw.

• Cloud feedbackNarrower topic: Cloud feedback is one component of the broader climate feedback system.

• Earth system scienceRelated: Feedbacks explain how interactions can magnify or stabilize system changes.

• Impact winterRelated: Sea ice and snow can amplify cooling by reflecting more sunlight.

• Silicate weatheringRelated: Warmer, wetter conditions can accelerate weathering and strengthen carbon-dioxide drawdown.

• Climate scienceRelated: Feedbacks determine how strongly the system responds to an initial forcing.

• ClimatologyRelated: Feedbacks determine how strongly climate responds to external forcing.

• Permafrost carbon feedbackNarrower topic: The permafrost response is a positive feedback within the broader climate system.

• Gaia hypothesisRelated: Climate feedbacks show how regulation can fail or turn destabilizing.

• Anthropogenic climate changeRelated: Feedbacks such as increased water vapor amplify warming initiated by human emissions.

• Radiative equilibriumRelated: Feedbacks alter emitted or absorbed radiation as a system approaches a changed balance.

• Abrupt climate changeRelated: Positive feedbacks can accelerate an initially gradual shift.

• Climate systemBroader topic: Feedbacks determine whether an initial disturbance is strengthened or reduced.

• Milutin MilankovićNarrower topic: Orbital forcing sets a pace, while feedbacks help determine the climate response.

• Climate change in CanadaRelated: Snow and ice loss amplify warming by reducing the reflection of sunlight.

• Tipping points in the climate systemRelated: Feedbacks link individual tipping risks to the wider climate response.

• Climate variability and changeRelated: Feedbacks such as declining snow cover can magnify an initial temperature shift.

• Effects of climate changeRelated: Feedbacks such as melting ice can accelerate or moderate some impacts.