Committed warming inferred from observations

[1]  B. Stevens.  Reply to “Comments on ‘Rethinking the Lower Bound on Aerosol Radiative Forcing’” , 2015, Journal of Climate.

[2]  K. Armour.  Energy budget constraints on climate sensitivity in light of inconstant climate feedbacks , 2017 .

[3]  Kevin Cowtan,et al.  Reconciled climate response estimates from climate models and the energy budget of Earth , 2016 .

[4]  Norman G. Loeb,et al.  Improving estimates of Earth's energy imbalance , 2016 .

[5]  T. Andrews,et al.  Variation in climate sensitivity and feedback parameters during the historical period , 2016 .

[6]  T. Andrews,et al.  Small global-mean cooling due to volcanic radiative forcing , 2016, Climate Dynamics.

[7]  G. Schmidt,et al.  Implications for climate sensitivity from the response to individual forcings , 2016 .

[8]  Olivier Boucher,et al.  Declining uncertainty in transient climate response as CO2 forcing dominates future climate change , 2015 .

[9]  John P. Krasting,et al.  Dominance of the Southern Ocean in Anthropogenic Carbon and Heat Uptake in CMIP5 Models , 2015 .

[10]  J. Curry,et al.  The implications for climate sensitivity of AR5 forcing and heat uptake estimates , 2015, Climate Dynamics.

[11]  Olivier Boucher,et al.  Adjustments in the Forcing-Feedback Framework for Understanding Climate Change , 2014 .

[12]  Thomas L. Frölicher,et al.  Continued global warming after CO 2 emissions stoppage , 2014 .

[13]  Reto Knutti,et al.  Energy budget constraints on climate response , 2013 .

[14]  J. Gregory,et al.  Climate models without preindustrial volcanic forcing underestimate historical ocean thermal expansion , 2013 .

[15]  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 .

[16]  T. Stocker,et al.  SBSTA-IPCC Special Event Climate Change 2013: The Physical Science Basis , 2013 .

[17]  H. Matthews,et al.  Climate response to zeroed emissions of greenhouse gases and aerosols , 2012 .

[18]  P. Jones,et al.  Quantifying uncertainties in global and regional temperature change using an ensemble of observational estimates: The HadCRUT4 data set , 2012 .

[19]  Cecilia M. Bitz,et al.  The reversibility of sea ice loss in a state‐of‐the‐art climate model , 2011 .

[20]  S. Marshall,et al.  Ongoing climate change following a complete cessation of carbon dioxide emissions , 2011 .

[21]  G. Roe,et al.  Climate commitment in an uncertain world , 2011 .

[22]  S. Solomon,et al.  Irreversible climate change due to carbon dioxide emissions , 2009, Proceedings of the National Academy of Sciences.

[23]  V. Ramanathan,et al.  On avoiding dangerous anthropogenic interference with the climate system: Formidable challenges ahead , 2008, Proceedings of the National Academy of Sciences.

[24]  David Archer,et al.  The millennial atmospheric lifetime of anthropogenic CO2 , 2008 .

[25]  T. Wigley.  The Climate Change Commitment , 2005, Science.

[26]  Bill Hare,et al.  How Much Warming are We Committed to and How Much can be Avoided? , 2006 .

[27]  Nicolas Gruber,et al.  The Oceanic Sink for Anthropogenic CO2 , 2004, Science.

[28]  S. Raper,et al.  An Observationally Based Estimate of the Climate Sensitivity , 2002 .

[29]  T. Wigley,et al.  Could reducing fossil-fuel emissions cause global warming? , 1991, Nature.

[30]  J. Hansen,et al.  Climate Response Times: Dependence on Climate Sensitivity and Ocean Mixing , 1985, Science.

[31]  K. Bryan,et al.  Transient Climate Response to Increasing Atmospheric Carbon Dioxide , 1982, Science.