Quantifying the Limits of a Linear Temperature Response to Cumulative CO2 Emissions

AbstractRecent studies have shown that the transient climate response to cumulative carbon emissions (TCRE) of the global temperature can be well approximated by a constant value for cumulative emissions up to about 2 TtC. However, there has been little attention given in the literature to how the TCRE varies across the range of emissions rates represented by the current RCP emissions scenarios. The authors use an ensemble of simulations generated using the University of Victoria Earth System Climate Model to quantify how the temperature response to cumulative emissions varies as a function of both the total magnitude and the rate of CO2 emissions. This study shows that the 500-yr response to a pulse CO2 emission (1.81°C TtC−1) does not depend on the magnitude of cumulative emissions up to 3 TtC. The TCRE (1.66°C TtC−1), which relates to the short-term response, is relatively insensitive to constant-rate emissions up to 30 GtC yr−1. This experiment shows that the formal way of estimating the TCRE—that is,...

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

[2]  B. Samuels,et al.  Connecting changing ocean circulation with changing climate , 2013 .

[3]  R. Stouffer Time Scales of Climate Response , 2004 .

[4]  S. Solomon,et al.  Cumulative carbon as a policy framework for achieving climate stabilization , 2012, Philosophical Transactions of the Royal Society A: Mathematical, Physical and Engineering Sciences.

[5]  Simon Buckle,et al.  Mitigation of climate change , 2009, The Daunting Climate Change.

[6]  Corinne Le Quéré,et al.  Persistent growth of CO2 emissions and implications for reaching climate targets , 2014 .

[7]  K.,et al.  Carbon–Concentration and Carbon–Climate Feedbacks in CMIP5 Earth System Models , 2012 .

[8]  John Barrett,et al.  Drivers, Trends and Mitigation , 2014 .

[9]  David Archer,et al.  Fate of fossil fuel CO2 in geologic time , 2005 .

[10]  C. Tebaldi,et al.  Long-term Climate Change: Projections, Commitments and Irreversibility , 2013 .

[11]  J. Canadell,et al.  Global and regional drivers of accelerating CO2 emissions , 2007, Proceedings of the National Academy of Sciences.

[12]  Alvaro Montenegro,et al.  Lifetime of Anthropogenic Climate Change: Millennial Time Scales of Potential CO2 and Surface Temperature Perturbations , 2009 .

[13]  Masson-Delmotte,et al.  The Physical Science Basis , 2007 .

[14]  Myles R. Allen,et al.  Constraining the Ratio of Global Warming to Cumulative CO2 Emissions Using CMIP5 Simulations , 2013 .

[15]  H. Damon Matthews,et al.  The proportionality of global warming to cumulative carbon emissions , 2009, Nature.

[16]  Marika M. Holland,et al.  The UVic earth system climate model: Model description, climatology, and applications to past, present and future climates , 2001, Data, Models and Analysis.

[17]  Corinne Le Quéré,et al.  Trends in the sources and sinks of carbon dioxide , 2009 .

[18]  W. Collins,et al.  Global climate projections , 2007 .

[19]  Sergey Paltsev,et al.  MIT Integrated Global System Model (IGSM) Version 2: Model Description and Baseline Evaluation , 2005 .

[20]  M. Allen,et al.  Cumulative carbon emissions, emissions floors and short-term rates of warming: implications for policy , 2011, Philosophical Transactions of the Royal Society A: Mathematical, Physical and Engineering Sciences.

[21]  A. I. Shlyakhter,et al.  Integrated risk analysis of global climate change , 1995 .

[22]  Andreas Oschlies,et al.  Future changes in climate, ocean circulation, ecosystems, and biogeochemical cycling simulated for a business‐as‐usual CO2 emission scenario until year 4000 AD , 2008 .

[23]  N. Gillett,et al.  Is the climate response to CO2 emissions path dependent? , 2012 .

[24]  R. Betts,et al.  The impact of new land surface physics on the GCM simulation of climate and climate sensitivity , 1999 .

[25]  J. Hansen,et al.  Climate-chemical interactions and effects of changing atmospheric trace gases , 1987 .

[26]  Wei Li,et al.  Decomposition of China’s CO2 emissions from agriculture utilizing an improved Kaya identity , 2014, Environmental Science and Pollution Research.

[27]  Corinne Le Quéré,et al.  Climate Change 2013: The Physical Science Basis , 2013 .

[28]  K. Calvin,et al.  The RCP greenhouse gas concentrations and their extensions from 1765 to 2300 , 2011 .

[29]  Ken Caldeira,et al.  Stabilizing climate requires near‐zero emissions , 2008 .

[30]  A. Weaver,et al.  Nonlinearity of Carbon Cycle Feedbacks , 2010 .

[31]  Elena Shevliakova,et al.  Trajectory sensitivity of the transient climate response to cumulative carbon emissions , 2014 .

[32]  Katrin J. Meissner,et al.  The role of land surface dynamics in glacial inception: a study with the UVic Earth System Model , 2003 .

[33]  N. Meinshausen,et al.  Warming caused by cumulative carbon emissions towards the trillionth tonne , 2009, Nature.

[34]  Philip Goodwin,et al.  Sensitivity of climate to cumulative carbon emissions due to compensation of ocean heat and carbon uptake , 2015 .