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The 34 pages that link to Climate sensitivity, each with the reason it gives.

• PaleoclimatologyRelated: Past warm periods help constrain how strongly climate responds to greenhouse gases.

• Greenhouse effectRelated: It measures the total warming that follows an enhanced greenhouse effect.

• Climate modelRelated: Model simulations use sensitivity to assess how strongly the climate responds to added greenhouse gases.

• Radiative forcingRelated: It connects a forcing magnitude to the resulting temperature response.

• PaleoclimateRelated: Ancient warm and cold intervals help estimate how strongly temperature responds to greenhouse gases.

• Global warmingRelated: It describes how much warming follows sustained greenhouse-gas forcing.

• Ice–albedo feedbackRelated: Uncertainty in feedback strength contributes to uncertainty in projected warming.

• ClimateRelated: Its estimated range captures uncertainty in the strength of climate response.

• Earth's energy budgetRelated: The budget connects imposed energy changes to eventual warming.

• UncertaintyBroader topic: Its estimated range captures uncertainty about the climate system's response.

• Greenland ice sheetRelated: Uncertainty in future warming strongly affects projections of Greenland’s mass loss.

• Climate variabilityCompared with: Climate sensitivity describes a response to forcing, while variability also arises within the climate system.

• Svante ArrheniusRelated: Arrhenius estimated how much climate could warm as atmospheric carbon dioxide increased.

• PaleoceanographyRelated: Past ocean records constrain how strongly climate responds to greenhouse-gas changes.

• Climate change attributionRelated: Sensitivity constrains expected warming from forcing but does not by itself attribute observed changes.

• Climate modelingRelated: Model estimates still differ, especially because clouds and other feedbacks remain uncertain.

• Aerosol-cloud interactionsRelated: Uncertainty in aerosol-cloud forcing affects estimates of climate response.

• Climate projectionRelated: It strongly influences how much warming a model projects for a given forcing pathway.

• Ocean warmingRelated: Uncertainty in climate sensitivity influences projections of the energy available for ocean uptake.

• Social cost of carbonRelated: It helps determine how much warming an additional tonne of emissions causes.

• Carbonate–silicate cycleRelated: The cycle's feedbacks influence how temperature responds to persistent carbon dioxide changes.

• Cirrus cloudRelated: Uncertainty in cirrus feedback contributes to uncertainty in estimates of climate sensitivity.

• ClimatologyRelated: Its estimated range affects the scale of projected warming.

• Anthropogenic climate changeRelated: It links greenhouse-gas increases to the eventual temperature response.

• Climate change vulnerabilityRelated: Sensitivity helps explain why exposed systems suffer different levels of harm.

• James HansenRelated: Hansen’s model projections depended on how strongly temperature responds to greenhouse forcing.

• Climate change feedbacksRelated: Feedback strength helps determine how much temperature changes for a given forcing.

• Outgoing longwave radiationRelated: The response of outgoing radiation to warming helps determine how much temperature rises.

• William NordhausRelated: This parameter shapes the temperature consequences calculated in Nordhaus’s model.

• Atmospheric scienceRelated: Atmospheric feedbacks determine how strongly temperature responds to greenhouse-gas forcing.

• Late Paleozoic icehouseRelated: Estimating sensitivity helps explain how carbon dioxide changes produced the observed cooling.

• Tipping points in the climate systemRelated: It helps relate greenhouse-gas forcing to the background warming that raises tipping risks.

• History of climate change scienceRelated: Its estimated range has shaped projections since early quantitative climate studies.

• Mikhail BudykoRelated: Budyko used energy-balance reasoning to estimate how strongly temperature responds to forcing.