Consequences of twenty-first-century policy for multi-millennial climate and sea-level change

Most of the policy debate surrounding the actions needed to mitigate and adapt to anthropogenic climate change has been framed by observations of the past 150 years as well as climate and sea-level projections for the twenty-first century. The focus on this 250-year window, however, obscures some of the most profound problems associated with climate change. Here, we argue that the twentieth and twenty-first centuries, a period during which the overwhelming majority of human-caused carbon emissions are likely to occur, need to be placed into a long-term context that includes the past 20 millennia, when the last Ice Age ended and human civilization developed, and the next ten millennia, over which time the projected impacts of anthropogenic climate change will grow and persist. This long-term perspective illustrates that policy decisions made in the next few years to decades will have profound impacts on global climate, ecosystems and human societies — not just for this century, but for the next ten millennia and beyond.

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

[2]  M. Ha-Duong,et al.  Climate change 2014 - Mitigation of climate change , 2015 .

[3]  J. Jouzel,et al.  Synchronous Change of Atmospheric CO2 and Antarctic Temperature During the Last Deglacial Warming , 2013, Science.

[4]  B. Smith,et al.  Marine Ice Sheet Collapse Potentially Under Way for the Thwaites Glacier Basin, West Antarctica , 2014, Science.

[5]  M. Allen,et al.  Cumulative emissions and climate policy , 2014 .

[6]  Atul K. Jain,et al.  Global Carbon Budget 2018 , 2014, Earth System Science Data.

[7]  J. Houghton,et al.  Climate change 1995: the science of climate change. , 1996 .

[8]  Stefan Rahmstorf,et al.  Dynamic sea level changes following changes in the thermohaline circulation , 2005 .

[9]  Dean N. Williams,et al.  An interactive web application for visualizing climate data , 2013 .

[10]  T. Stocker,et al.  Atmospheric CO2 concentrations over the last glacial termination. , 2001, Science.

[11]  Global Energy Assessment Writing Team Global Energy Assessment: Toward a Sustainable Future , 2012 .

[12]  Corinne Le Quéré,et al.  The challenge to keep global warming below 2 °C , 2013 .

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

[14]  David Archer,et al.  Multiple timescales for neutralization of fossil fuel CO2 , 1997 .

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

[16]  Benjamin D. Santer,et al.  Ocean response to greenhouse warming , 1990, Nature.

[17]  W. Landman Climate change 2007: the physical science basis , 2010 .

[18]  Peter U. Clark,et al.  The multimillennial sea-level commitment of global warming , 2013, Proceedings of the National Academy of Sciences.

[19]  T. Delworth,et al.  Probing the Fast and Slow Components of Global Warming by Returning Abruptly to Preindustrial Forcing , 2010 .

[20]  D. Stammer Response of the global ocean to Greenland and Antarctic ice melting , 2008 .

[21]  A. Ganopolski,et al.  Multistability and critical thresholds of the Greenland ice sheet , 2010 .

[22]  Bilal U. Haq,et al.  Sea-level rise and coastal subsidence: causes, consequences, and strategies. , 1996 .

[23]  N. Meinshausen,et al.  Greenhouse-gas emission targets for limiting global warming to 2 °C , 2009, Nature.

[24]  Climate Stabilization Targets : Emissions , Concentrations , and Impacts over Decades to Millennia Committee on Stabilization Targets for Atmospheric Greenhouse Gas Concentrations ; National Research Council , 2011 .

[25]  J. Mitrovica,et al.  Postglacial sea-level change on a rotating Earth , 1998 .

[26]  T. Wigley,et al.  Global Sea-level Rise: Past and Future , 1996 .

[27]  Julia C. Hargreaves,et al.  Long-term climate commitments projected with climate-carbon cycle models , 2008 .

[28]  C. Wunsch,et al.  Atmospheric loading and the oceanic “inverted barometer” effect , 1997 .

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

[30]  K. Caldeira,et al.  Combustion of available fossil fuel resources sufficient to eliminate the Antarctic Ice Sheet , 2015, Science Advances.

[31]  P. Ciais,et al.  Long-term climate implications of twenty-first century options for carbon dioxide emission mitigation , 2011 .

[32]  J. Mitrovica,et al.  On post-glacial sea level – II. Numerical formulation and comparative results on spherically symmetric models , 2005 .

[33]  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.

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

[35]  N. Nakicenovic,et al.  Global Energy Assessment – Toward a Sustainable Future , 2012 .

[36]  A. Levermann,et al.  Ice plug prevents irreversible discharge from East Antarctica , 2014 .

[37]  Andrew J. Weaver The Science of Climate Change , 2003 .

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

[39]  V. Brovkin,et al.  Atmospheric lifetime of fossil-fuel carbon dioxide , 2009 .

[40]  T. Wigley Global‐mean temperature and sea level consequences of greenhouse gas concentration stabilization , 1995 .

[41]  K. Lambeck,et al.  Sea level and global ice volumes from the Last Glacial Maximum to the Holocene , 2014, Proceedings of the National Academy of Sciences.

[42]  J. Annan,et al.  A perspective on model-data surface temperature comparison at the Last Glacial Maximum , 2015 .

[43]  V. Masson‐Delmotte,et al.  Changes in atmospheric CO2 and its carbon isotopic ratio during the penultimate deglaciation , 2010 .

[44]  Andrei P. Sokolov,et al.  Long-Term climate change commitment and reversibility: An EMIC intercomparison , 2013 .

[45]  P. Clark,et al.  A new projection of sea level change in response to collapse of marine sectors of the Antarctic Ice Sheet , 2010 .

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

[47]  A. Weaver,et al.  Long term climate implications of 2050 emission reduction targets , 2007 .

[48]  On Postglacial Sea Level , 2007 .

[49]  F. Joos,et al.  A Coupled Dynamical Ocean–Energy Balance Atmosphere Model for Paleoclimate Studies , 2011 .

[50]  R. B. Pearce,et al.  Migration of the Antarctic Polar Front through the mid-Pleistocene transition: evidence and climatic implications , 2010 .

[51]  H. Oeschger,et al.  Transient Temperature Changes Due to Increasing CO2 Using Simple Models , 1984, Annals of Glaciology.

[52]  K. Arrow,et al.  Determining Benefits and Costs for Future Generations , 2013, Science.

[53]  Thorkild Aarup,et al.  Understanding sea level rise and variability , 2007 .

[54]  S. Randalls History of the 2°C climate target , 2010 .

[55]  P. Sands The United Nations Framework Convention on Climate Change , 1992 .

[56]  O. Edenhofer,et al.  Climate change 2014 : mitigation of climate change , 2014 .

[57]  A. Payne,et al.  Retreat of Pine Island Glacier controlled by marine ice-sheet instability , 2014 .

[58]  J. Weertman,et al.  Stability of the Junction of an Ice Sheet and an Ice Shelf , 1974, Journal of Glaciology.

[59]  W. G. Strand,et al.  How Much More Global Warming and Sea Level Rise? , 2005, Science.

[60]  A. Abe‐Ouchi,et al.  Insolation-driven 100,000-year glacial cycles and hysteresis of ice-sheet volume , 2013, Nature.

[61]  Yvonne Freeh,et al.  Understanding Sea-Level Rise and Variability , 2011 .

[62]  P. Clark,et al.  Global warming preceded by increasing carbon dioxide concentrations during the last deglaciation , 2012, Nature.

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

[64]  William D. Nordhaus,et al.  The Climate Casino , 2013 .

[65]  J. Kutzbach,et al.  Northern Hemisphere forcing of Southern Hemisphere climate during the last deglaciation , 2013, Nature.

[66]  S. Rahmstorf,et al.  Sea-level rise due to polar ice-sheet mass loss during past warm periods , 2015, Science.

[67]  M. Tamisiea,et al.  Recent mass balance of polar ice sheets inferred from patterns of global sea-level change , 2001, Nature.

[68]  J. Kasting,et al.  Effects of fuel and forest conservation on future levels of atmospheric carbon dioxide. , 1992, Global and planetary change.

[69]  Stewart J. Cohen,et al.  Climate Change 2014: Impacts,Adaptation, and Vulnerability. Part A: Global and Sectoral Aspects. Contribution of Working Group II to the Fifth Assessment Report of the Intergovernmental Panel on Climate Change , 2014 .

[70]  C. Buizert,et al.  Centennial-scale changes in the global carbon cycle during the last deglaciation , 2014, Nature.

[71]  Alexander H. Jarosch,et al.  Past and future sea-level change from the surface mass balance of glaciers , 2012 .

[72]  A. R. Price,et al.  Millennial timescale carbon cycle and climate change in an efficient Earth system model , 2006 .

[73]  Us Nas,et al.  Climate intervention: Carbon dioxide removal and reliable sequestration , 2017 .

[74]  B. Scheuchl,et al.  Widespread, rapid grounding line retreat of Pine Island, Thwaites, Smith, and Kohler glaciers, West Antarctica, from 1992 to 2011 , 2014 .

[75]  Ben Marzeion,et al.  Loss of cultural world heritage and currently inhabited places to sea-level rise , 2014 .

[76]  G.,et al.  Climate Response Times : Dependence on Climate Sensitivity and Ocean Mixing , 2022 .

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

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

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

[80]  K. Lambeck,et al.  Paleoenvironmental Records, Geophysical Modeling, and Reconstruction of Sea-Level Trends and Variability on Centennial and Longer Timescales , 2010 .

[81]  J. Mitrovica,et al.  On the origin of late Holocene sea-level highstands within equatorial ocean basins , 2002 .

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

[83]  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.

[84]  E. Northrop The Climate Casino: Risk, Uncertainty, and Economics for a Warming World , 2015 .

[85]  Shaun A Marcott,et al.  A Reconstruction of Regional and Global Temperature for the Past 11,300 Years , 2013, Science.

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

[87]  Acknowledgements , 1992, Experimental Gerontology.