Errors in Simple Climate Model Emulations of Past and Future Global Temperature Change
暂无分享,去创建一个
[1] Christopher J. Smith,et al. Biased Estimates of Equilibrium Climate Sensitivity and Transient Climate Response Derived From Historical CMIP6 Simulations , 2021, Geophysical Research Letters.
[2] S. Fueglistaler,et al. The Peculiar Trajectory of Global Warming , 2021, Journal of Geophysical Research: Atmospheres.
[3] M. Zelinka,et al. Greater committed warming after accounting for the pattern effect , 2021, Nature Climate Change.
[4] Martin B. Stolpe,et al. Climate Sensitivity Increases Under Higher CO2 Levels Due to Feedback Temperature Dependence , 2020, Geophysical Research Letters.
[5] T. Mauritsen,et al. The 2000–2012 Global Warming Hiatus More Likely With a Low Climate Sensitivity , 2020, Geophysical Research Letters.
[6] J. Rogelj,et al. Reduced Complexity Model Intercomparison Project Phase 2: Synthesizing Earth System Knowledge for Probabilistic Climate Projections , 2020, Earth's future.
[7] H. Fredriksen,et al. Estimating Radiative Forcing With a Nonconstant Feedback Parameter and Linear Response , 2020, Journal of Geophysical Research: Atmospheres.
[8] Christopher J. Smith,et al. Reduced Complexity Model Intercomparison Project Phase 1: introduction and evaluation of global-mean temperature response , 2020, Geoscientific Model Development.
[9] Calibrating Simple Climate Models to Individual Earth System Models: Lessons Learned From Calibrating Hector , 2020, Earth and Space Science.
[10] T. Andrews,et al. Intermodel Spread in the Pattern Effect and Its Contribution to Climate Sensitivity in CMIP5 and CMIP6 Models , 2020 .
[11] Christopher J. Smith,et al. Effective Radiative Forcing in a GCM With Fixed Surface Temperatures , 2020, Journal of Geophysical Research: Atmospheres.
[12] P. Forster,et al. Energy Budget Constraints on the Time History of Aerosol Forcing and Climate Sensitivity , 2020, Journal of Geophysical Research: Atmospheres.
[13] C. Hannay,et al. Comparison of Equilibrium Climate Sensitivity Estimates From Slab Ocean, 150‐Year, and Longer Simulations , 2020, Geophysical Research Letters.
[14] P. Stott,et al. Optimal Estimation of Stochastic Energy Balance Model Parameters , 2020, Journal of Climate.
[15] R. Colman,et al. Understanding the links between climate feedbacks, variability and change using a two-layer energy balance model , 2020, Climate Dynamics.
[16] T. Andrews,et al. Equilibrium Climate Sensitivity Estimated by Equilibrating Climate Models , 2020, Geophysical Research Letters.
[17] Christopher J. Smith,et al. Effective radiative forcing and adjustments in CMIP6 models , 2020, Atmospheric Chemistry and Physics.
[18] B. Stevens,et al. On simple representations of the climate response to external radiative forcing , 2019, Climate Dynamics.
[19] Jonathan M. Gregory,et al. Accounting for Changing Temperature Patterns Increases Historical Estimates of Climate Sensitivity , 2018, Geophysical Research Letters.
[20] Karen A. McKinnon,et al. An “Observational Large Ensemble” to Compare Observed and Modeled Temperature Trend Uncertainty due to Internal Variability , 2017 .
[21] S. Bony,et al. Prospects for narrowing bounds on Earth's equilibrium climate sensitivity , 2016, Earth's future.
[22] T. Andrews,et al. Recommendations for diagnosing effective radiative forcing from climate models for CMIP6 , 2016 .
[23] Reto Knutti,et al. The Detection and Attribution Model Intercomparison Project (DAMIP v1.0)contribution to CMIP6 , 2016 .
[24] Ken Caldeira,et al. Dependence of global radiative feedbacks on evolving patterns of surface heat fluxes , 2016 .
[25] Robert Pincus,et al. The Radiative Forcing Model Intercomparison Project (RFMIP): Experimental Protocol for CMIP6 , 2016 .
[26] T. Andrews,et al. Small global-mean cooling due to volcanic radiative forcing , 2016, Climate Dynamics.
[27] R. Portmann,et al. A Temporal Kernel Method to Compute Effective Radiative Forcing in CMIP5 Transient Simulations , 2016 .
[28] Veronika Eyring,et al. Overview of the Coupled Model Intercomparison Project Phase 6 (CMIP6) experimental design and organization , 2015 .
[29] T. Andrews,et al. The inconstancy of the transient climate response parameter under increasing CO2 , 2015, Philosophical Transactions of the Royal Society A: Mathematical, Physical and Engineering Sciences.
[30] M. Webb,et al. The Dependence of Radiative Forcing and Feedback on Evolving Patterns of Surface Temperature Change in Climate Models , 2015 .
[31] Jason Lowe,et al. Corrigendum: Nonlinear regional warming with increasing CO 2 concentrations , 2015 .
[32] Olivier Boucher,et al. Adjustments in the Forcing-Feedback Framework for Understanding Climate Change , 2014 .
[33] D. Saint‐Martin,et al. Transient Climate Response in a Two-Layer Energy-Balance Model. Part I: Analytical Solution and Parameter Calibration Using CMIP5 AOGCM Experiments , 2013 .
[34] Olivier Geoffroy,et al. Transient Climate Response in a Two-Layer Energy-Balance Model. Part II: Representation of the Efficacy of Deep-Ocean Heat Uptake and Validation for CMIP5 AOGCMs , 2013 .
[35] T. Andrews,et al. Evaluating adjusted forcing and model spread for historical and future scenarios in the CMIP5 generation of climate models , 2013 .
[36] Cecilia M. Bitz,et al. Time-Varying Climate Sensitivity from Regional Feedbacks , 2012 .
[37] Jonathan M. Gregory,et al. A step‐response simple climate model to reconstruct and interpret AOGCM projections , 2011 .
[38] Isaac M. Held,et al. Importance of Ocean Heat Uptake Efficacy to Transient Climate Change , 2010 .
[39] T. Delworth,et al. Probing the Fast and Slow Components of Global Warming by Returning Abruptly to Preindustrial Forcing , 2010 .
[40] John F. B. Mitchell,et al. The time‐dependence of climate sensitivity , 2000 .