A review of progress towards understanding the transient global mean surface temperature response to radiative perturbation
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DOI[10.1186/s40645-016-0096-3]のデータに遷移します
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- 資料種別
- 記事
- 著者・編者
- Masakazu YoshimoriMasahiro WatanabeHideo Shiogama
- 出版年月日等
- 2016-07-18
- 出版年（W3CDTF）
- 2016-07-18
- タイトル（掲載誌）
- Progress in earth and planetary science
- 巻号年月日等（掲載誌）
- 3(21)
- 掲載巻
- 3(21)
- ISSN（掲載誌）
- 2197-4284
- ISSN-L（掲載誌）
- 2197-4284
- 本文の言語コード
- eng
- DOI
- 10.1186/s40645-016-0096-3
- 国立国会図書館永続的識別子
- info:ndljp/pid/10265304
- コレクション（共通）
- コレクション（障害者向け資料：レベル1）
- コレクション（個別）
- 国立国会図書館デジタルコレクション > 電子書籍・電子雑誌 > その他
- 収集根拠
- オンライン資料収集制度
- 受理日（W3CDTF）
- 2017-01-19T19:10:18+09:00
- 保存日（W3CDTF）
- 2017-01-18
- 記録形式（IMT）
- application/pdf
- オンライン閲覧公開範囲
- 国立国会図書館内限定公開
- デジタル化資料送信
- 図書館・個人送信対象外
- 遠隔複写可否（NDL）
- 可
- 掲載誌（国立国会図書館永続的識別子）
- info:ndljp/pid/10016350
- 連携機関・データベース
- 国立国会図書館 : 国立国会図書館デジタルコレクション
- 要約等
- コレクション : 国立国会図書館デジタルコレクション > 電子書籍・電子雑誌 > その他
- DOI
- 10.1186/s40645-016-0096-3
- オンライン閲覧公開範囲
- インターネット公開
- 関連情報（URI）
- 参照
- Responses of Basal Melting of Antarctic Ice Shelves to the Climatic Forcing of the Last Glacial Maximum and CO2 DoublingThe role of atmospheric heat transport and regional feedbacks in the Arctic warming at equilibriumThe post‐2002 global surface warming slowdown caused by the subtropical Southern Ocean heating acceleration
- 参照
- Rapid Adjustments of Cloud and Hydrological Cycle to Increasing CO2: a ReviewOcean oxygen depletion due to decomposition of submarine methane hydrateSources of Spread in Multimodel Projections of the Greenland Ice Sheet Surface Mass BalanceSpatial patterns of radiative forcing and surface temperature responseThe implications for climate sensitivity of AR5 forcing and heat uptake estimatesA new method for diagnosing radiative forcing and climate sensitivityInsolation-driven 100,000-year glacial cycles and hysteresis of ice-sheet volumeRecent global-warming hiatus tied to equatorial Pacific surface coolingContribution of natural decadal variability to global warming acceleration and hiatusRelative contribution of feedback processes to Arctic amplification of temperature change in MIROC GCMTime-Varying Climate Sensitivity from Regional FeedbacksClimate feedbacks under a very broad range of forcingGlobal deep ocean oxygenation by enhanced ventilation in the Southern Ocean under long‐term global warmingEfficacy of climate forcingsClimate models at their limit?Comment on “Heat capacity, time constant, and sensitivity of Earth's climate system” by S. E. SchwartzTransient Climate Response in a Two-Layer Energy-Balance Model. Part II: Representation of the Efficacy of Deep-Ocean Heat Uptake and Validation for CMIP5 AOGCMsInterpretation of High Projections for Global-Mean WarmingQuantifying Carbon Cycle FeedbacksCall Off the QuestRadiative forcing and climate responseThe Nonlinear and Nonlocal Nature of Climate FeedbacksThe climate response to CO<sub>2</sub> of the Hadley Centre coupled AOGCM with and without flux adjustmentAn Assessment of the Primary Sources of Spread of Global Warming Estimates from Coupled Atmosphere–Ocean ModelsThe Climate Sensitivity and Its Components Diagnosed from Earth Radiation Budget DataOcean heat uptake and its consequences for the magnitude of sea level rise and climate changeAn Overview of CMIP5 and the Experiment DesignAn assessment of methods for computing radiative forcing in climate modelsNon-linear climate feedback analysis in an atmospheric general circulation modelEmergent Constraints for Cloud FeedbacksHeat capacity, time constant, and sensitivity of Earth's climate systemResponse of a Coupled Ocean–Atmosphere Model to Increasing Atmospheric Carbon Dioxide: Sensitivity to the Rate of IncreaseClimate Sensitivity of the Community Climate System Model, Version 4The inconstancy of the transient climate response parameter under increasing CO<sub>2</sub>Adjustments in the Forcing-Feedback Framework for Understanding Climate ChangeTransient climate response estimated from radiative forcing and observed temperature changeModel-based evidence of deep-ocean heat uptake during surface-temperature hiatus periodsInterpretation of Simulated Global Warming Using a Simple ModelDeep-ocean heat uptake and equilibrium climate responseForcing, feedbacks and climate sensitivity in CMIP5 coupled atmosphere‐ocean climate modelsStratosphere adjusted radiative forcing calculationsin a comprehensive climate modelClimate commitment in an uncertain worldReply to comments by G. Foster et al., R. Knutti et al., and N. Scafetta on “Heat capacity, time constant, and sensitivity of Earth's climate system”The time‐dependence of climate sensitivityTemperature scaling pattern dependence on representative concentration pathway emission scenariosVertical heat transports in the ocean and their effect on time-dependent climate changeIrreversible climate change due to carbon dioxide emissionsQuantifying the sources of spread in climate change experimentsImplications for climate sensitivity from the response to individual forcingsLong-Term Climate Change Commitment and Reversibility: An EMIC IntercomparisonA Comparison of Climate Feedback Strength between CO2 Doubling and LGM ExperimentsObservational estimate of climate sensitivity from changes in the rate of ocean heat uptake and comparison to CMIP5 modelsShortwave and longwave radiative contributions to global warming under increasing CO <sub>2</sub>Bayesian estimation of climate sensitivity based on a simple climate model fitted to observations of hemispheric temperatures and global ocean heat contentAn alternative to radiative forcing for estimating the relative importance of climate change mechanismsClimate sensitivity: Analysis of feedback mechanismsClimate sensitivities of two versions of FGOALS model to idealized radiative forcingEquilibrium Response of an Atmosphere–Mixed Layer Ocean Model to Different Radiative Forcing Agents: Global and Zonal Mean ResponseTransient Climate Response in a Two-Layer Energy-Balance Model. Part I: Analytical Solution and Parameter Calibration Using CMIP5 AOGCM ExperimentsInhomogeneous forcing and transient climate sensitivityA Conceptual Model of Ocean Heat Uptake under Climate ChangeInfluence of Ocean and Atmosphere Components on Simulated Climate SensitivitiesTowards quantifying uncertainty in transient climate changeThe impact of forcing efficacy on the equilibrium climate sensitivityEvaluating adjusted forcing and model spread for historical and future scenarios in the CMIP5 generation of climate modelsQuantifying global climate feedbacks, responses and forcing under abrupt and gradual CO2 forcingTransient Response of the Hadley Centre Coupled Ocean-Atmosphere Model to Increasing Carbon Dioxide. Part III: Analysis of Global-Mean Response Using Simple ModelsAn Observationally Based Estimate of the Climate SensitivityConsistent Differences in Climate Feedbacks between Atmosphere–Ocean GCMs and Atmospheric GCMs with Slab-Ocean Models*Time Variation of Effective Climate Sensitivity in GCMsTropospheric Adjustment Induces a Cloud Component in CO2 ForcingConstraining Transient Climate Sensitivity Using Coupled Climate Model Simulations of Volcanic EruptionsRecent Progress in Constraining Climate Sensitivity With Model EnsemblesInfluence of the Thermohaline Circulation on Projected Sea Level RiseCORRIGENDUMConnecting Changing Ocean Circulation with Changing ClimateThe Climate Sensitivity of the Community Climate System Model Version 3 (CCSM3)Objective estimation of the probability density function for climate sensitivityClimate Impact of Increasing Atmospheric Carbon DioxideComment on “Heat capacity, time constant, and sensitivity of Earth's climate system” by S. E. SchwartzEmpirical analysis of the solar contribution to global mean air surface temperature changeA lower and more constrained estimate of climate sensitivity using updated observations and detailed radiative forcing time seriesLong-Term Climate Commitments Projected with Climate–Carbon Cycle ModelsDependence of Precipitation Scaling Patterns on Emission Scenarios for Representative Concentration PathwaysEnergy budget constraints on climate responseClimate Response Times: Dependence on Climate Sensitivity and Ocean MixingComparison of equilibrium and transient responses to CO<sub>2</sub> increase in eight state-of-the-art climate modelsRobust increase in equilibrium climate sensitivity under global warmingThe equilibrium sensitivity of the Earth's temperature to radiation changesEquilibrium climate sensitivity in light of observations over the warming hiatusHow Much More Global Warming and Sea Level Rise?Probing the Fast and Slow Components of Global Warming by Returning Abruptly to Preindustrial ForcingImportance of Ocean Heat Uptake Efficacy to Transient Climate ChangeClimate Feedbacks in CCSM3 under Changing CO2 Forcing. Part II: Variation of Climate Feedbacks and Sensitivity with ForcingCloud Adjustment and its Role in CO2 Radiative Forcing and Climate Sensitivity: A ReviewStrengthening of ocean heat uptake efficiency associated with the recent climate hiatusThe Role of Climate Sensitivity and Ocean Heat Uptake on AOGCM Transient Temperature ResponseEquilibrium Climate Sensitivity: Is It Accurate to Use a Slab Ocean Model?The Dependence of Radiative Forcing and Feedback on Evolving Patterns of Surface Temperature Change in Climate ModelsThe Shape of Things to Come: Why Is Climate Change So Predictable?Analytical solution for the effect of increasing CO2 on global mean temperatureImpact of the Atlantic meridional overturning circulation on ocean heat storage and transient climate changeTransient Temperature Changes Due to Increasing CO2 Using Simple ModelsThe dependence of transient climate sensitivity and radiative feedbacks on the spatial pattern of ocean heat uptakeDependency of Feedbacks on Forcing and Climate State in Physics Parameter EnsemblesCorrection to “Deep ocean heat uptake as a major source of spread in transient climate change simulations”Climate sensitivity and response
- 連携機関・データベース
- 国立情報学研究所 : CiNii Research
- 提供元機関・データベース
- 雑誌記事索引データベースCrossref科学研究費助成事業データベース科学研究費助成事業データベースCrossrefCrossrefCrossref
- 書誌ID（NDLBibID）
- 10265304