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8 - Linking science and action: targets, timetables and emission budgets

Published online by Cambridge University Press:  04 April 2011

Katherine Richardson
Affiliation:
University of Copenhagen
Will Steffen
Affiliation:
Australian National University, Canberra
Diana Liverman
Affiliation:
University of Arizona and University of Oxford
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Summary

‘There are times in the history of humanity when fateful decisions are made. The decision … on whether to enter a comprehensive global agreement for strong action on climate change is one of them. …On a balance of probabilities, the failure of our generation would lead to consequences that would haunt humanity until the end of time.’

Political leaders of 194 countries (as of January 2010) have signed the United Nations Framework Convention on Climate Change (UNFCCC), which states in Article 2 that the Convention's ‘ultimate objective … is to achieve… stabilization of greenhouse gas concentrations in the atmosphere at a level that would prevent dangerous anthropogenic interference with the climate system …’. As we have seen in the preceding chapters, scientists are able to document with a very high degree of certainty that human activities exert measurable influence on several components of the climate system. In addition, most scientists agree that, on the basis of observed changes in the climate system, there is a very high probability (>90% according to the IPCC) that these changes are primarily the result of anthropogenic influences on the climate system. Furthermore, many impacts on human societies and nature have already been recorded (Chapters 5 and 6). These impacts can only be expected to increase in the future.

With Article 2 of the UNFCCC as the point of departure, the next step is to determine what actually constitutes ‘dangerous anthropogenic interference with the climate system’, or ‘dangerous climate change’ as it is often called in shorthand.

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Publisher: Cambridge University Press
Print publication year: 2011

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References

Allen, M. R., Frame, D. J., Huntingford, C.et al. (2009). Warming caused by cumulative carbon emissions: Towards the trillionth tonne. Nature, 458, 116366.CrossRefGoogle ScholarPubMed
Annan, J. D. and Hargreaves, J. C. (2006). Using multiple observationally-based constraints to estimate climate sensitivity. Geophysical Research Letters, 33, L06704.CrossRefGoogle Scholar
Bohannon, J. (2008). Weighing the climate risks of an untapped fossil fuel. Science, 319, 1753.CrossRefGoogle ScholarPubMed
Chakravarty, S., Chikkatur, A., Coninck, H.et al. (2009). Climate policy based on individual emissions. IOP Conference Series: Earth and Environmental Science, 6, 102005.Google Scholar
Charney, J. G. (1979). Carbon Dioxide and Climate: A Scientific Assessment. Washington, D.C.: National Academies Press.Google Scholar
Collins, M. (2007). Ensembles and probabilities: a new era in the prediction of climate change. Philosophical Transactions of the Royal Society A – Mathematical, Physical & Engineering Sciences, 365, 1957–70.CrossRefGoogle ScholarPubMed
Accord, Copenhagen (2009). Draft decision -/CP.15, http://unfccc.int/resource/docs/2009/cop15/eng/l07.pdf
,Council of the European Union (2005). Presidency Conclusions. Brussels, 22–23 March. European Commission.Google Scholar
Edenhofer, O., Knopf, B., Leimbach, M. and Bauer, N. (2010). The economics of low stabilization: Model comparison of mitigation strategies and costs. The Energy Journal, 31, 11–48.CrossRefGoogle Scholar
England, M. H., Sen Gupta, A. and Pitman, A. J. (2009). Constraining future greenhouse gas emissions by a cumulative target. Proceedings of the National Academy of Sciences (USA), 106, 16539–40.CrossRefGoogle ScholarPubMed
,European Environment Agency (2009). CSI 013 – Atmospheric greenhouse gas concentrations–Assessment published Mar 2009. http://themes.eea.europa.eu/IMS/IMS/ISpecs/ISpecification20041007131717/IAssessment1234255180259/view_content.
Friedlingstein, P., Cox, P., Betts, R.et al. (2006). Climate-carbon cycle feedback analysis: Results from the C4MIP model intercomparison. Journal of Climate, 19, 3337–53.CrossRefGoogle Scholar
,German Advisory Council on Global Change (WBGU) (2009). Solving the Climate Dilemma: The Budget Approach. Special Report. Berlin: WBGU Secretariat.Google Scholar
Hansen, J., Sato, M., Kharecha, P.et al. (2008). Target atmospheric CO2: Where should humanity aim?Open Atmospheric Science Journal, 2, 217–31.CrossRefGoogle Scholar
Hooijer, A., Page, S., Canadell, J. G.et al. (2009). Current and future CO2 emissions from drained peatlands in Southeast Asia. Biogeosciences Discussions, 6, 7207–30.CrossRefGoogle Scholar
,Intergovernmental Panel on Climate Change (IPCC) (2007a). Climate Change 2007. Synthesis Report, eds. The Core Writing Team, Pachauri, R. K. and Reisinger, A.. Cambridge, UK and New York, NY: Cambridge University Press.Google Scholar
,Intergovernmental Panel on Climate Change (IPCC) (2007b). Climate Change 2007: The Physical Science Basis. Contribution of Working Group I to the Fourth Assessment Report of the Intergovernmental Panel on Climate Change, eds. Solomon, S., Qin, D., Manning, M., Marquis, M., Averyt, K., Tignor, M. M. B., Miller, H. L. Jr and Chen, Z.. Cambridge, UK and New York, NY: Cambridge University Press.Google Scholar
Knopf, B., Edenhofer, O., Barker, T.et al. (2009). The economics of low stabilisation: Implications for technological change and policy. In Making Climate Change Work for Us – ADAM Synthesis Book, eds. Hulme, M. and Neufeldt, H.. Cambridge, UK: Cambridge University Press.Google Scholar
Knutti, R. and Hegerl, G. C. (2008). The equilibrium sensitivity of the Earth's temperature to radiation changes. Nature Geoscience, 1, 735–43.CrossRefGoogle Scholar
Knutti, R., Meehl, G. A., Allen, M. R. and Stainforth, D. A. (2006). Constraining climate sensitivity from the seasonal cycle in surface temperature. Journal of Climate, 19, 4224–33.CrossRefGoogle Scholar
Kurz, W. A., Dymond, C. C., Stinson, G.et al. (2008a). Mountain pine beetle and forest carbon feedback to climate change. Nature, 452, 987–90.CrossRefGoogle ScholarPubMed
Kurz, W.A., Stinson, G., Rampley, G. J., Dymond, C. C. and Neilson, E. T. (2008b). Risk of natural disturbances makes future contribution of Canada's forests to the global carbon cycle highly uncertain. Proceedings of the National Academy of Sciences (USA), 105, 1551–55.CrossRefGoogle ScholarPubMed
Quéré, C., Raupach, M. R., Canadell, J. G.et al. (2009). Trends in the sources and sinks of carbon dioxide. Nature Geoscience, 2, 831–36.CrossRefGoogle Scholar
Lowe, J. A., Huntingford, C., Raper, S. C. B.et al. (2009). How difficult is it to recover from dangerous levels of global warming?Environmental Research Letters, 4, 014012.CrossRefGoogle Scholar
Matthews, H. D., Gillett, N. P., Stott, P. A. and Zickfeld, K. (2009). The proportionality of global warming to cumulative carbon emissions. Nature, 459, 829–32.CrossRefGoogle ScholarPubMed
Meinshausen, M., Meinshausen, N., Hare, W.et al. (2009). Greenhouse gas emission targets for limiting global warming to 2 °C. Nature, 458, 1158–62.CrossRefGoogle ScholarPubMed
Murphy, J. M., Sexton, D. M. H., Barnett, D. N.et al. (2004). Quantification of modelling uncertainties in a large ensemble of climate change simulations. Nature, 430, 768–72.CrossRefGoogle Scholar
Petit, J. R., Jouzel, J., Raynaud, D.et al. (1999). Climate and atmospheric history of the past 420,000 years from the Vostok ice core, Antarctica. Nature, 399, 429–36.CrossRefGoogle Scholar
Piani, C., Frame, D. J., Stainforth, D. A. and Allen, M. R. (2005). Constraints on climate change from a multi-thousand member ensemble of simulations. Geophysical Research Letters, 32, L23825.CrossRefGoogle Scholar
Ramanathan, V. and Feng, Y. (2008). On avoiding dangerous anthropogenic interference with the climate system: Formidable challenges ahead. Proceedings of the National Academy of Sciences (USA), 105, 14245–50.CrossRefGoogle ScholarPubMed
Randall, D. A., Wood, R. A., Bony, S.et al. (2007). Climate models and their evaluation. In Climate Change 2007: The Physical Science Basis. Contribution of Working Group I to the Fourth Assessment Report of the Intergovernmental Panel on Climate Change, eds. Solomon, S., Qin, D., Manning, M., Marquis, M., Averyt, K., Tignor, M. M. B., Miller, H. L. Jr and Chen, Z.. Cambridge, UK and New York, NY: Cambridge University Press, pp. 589–662.Google Scholar
Raupach, M. R. and Canadell, J. G. (2008). Observing a vulnerable carbon cycle. In The Continental-scale Greenhouse Gas Balance of Europe, eds. Dolman, A. J., Valentini, R. and Freibauer, A.. New York, NY: Springer, pp. 5–32.Google Scholar
Roe, G. H. and Baker, M. B. (2007). Why is climate sensitivity so unpredictable?Science, 318, 629–32.CrossRefGoogle ScholarPubMed
Sanderson, B. M., Knutti, R., Aina, T.et al. (2008). Constraints on model response to greenhouse gas forcing and the role of subgrid-scale processes. Journal of Climate, 21, 2384–2400.CrossRefGoogle Scholar
Schneider von Deimling, T., Held, H., Ganopolski, A. and Rahmstorf, S. (2006). Climate sensitivity estimated from ensemble simulations of glacial climate. Climate Dynamics, 27, 149–63.CrossRefGoogle Scholar
Schuur, E. A. G., Vogel, J. G., Crummer, K. G.et al. (2009). The effect of permafrost thaw on old carbon release and net carbon exchange from tundra. Nature, 459, 556–59.CrossRefGoogle ScholarPubMed
Solomon, S., Plattner, G.-K., Knutti, R. and Friedlingstein, P. (2009). Irreversible climate change due to carbon dioxide emissions. Proceedings of the National Academy of Sciences(USA), 106, 1704–09.CrossRefGoogle ScholarPubMed
Stainforth, D. A., Aina, T., Christensen, C.et al. (2005). Uncertainty in predictions of the climate response to rising levels of greenhouse gases. Nature, 433, 403–06.CrossRefGoogle ScholarPubMed
Tarnocai, C., Canadell, J. G., Schuur, E. A. G.et al. (2009). Soil organic carbon pools in the northern circumpolar permafrost region. Global Biogeochemical Cycles, 23, GB2023.CrossRefGoogle Scholar
Tebaldi, C. and Knutti, R. (2007). The use of the multi-model ensemble in probabilistic climate projections. Philosophical Transactions of the Royal Society A – Mathematical, Physical & Engineering Sciences, 365, 2053–75.CrossRefGoogle ScholarPubMed
,World Resources Institute (WRI) (2009). Climate Analysis Indicators Tool Version 6.0, http://cait.wri.org.
Zickfeld, K., Eby, M., Matthews, H. D. and Weaver, A. J. (2009). Setting cumulative emissions targets to reduce the risk of dangerous climate change. Proceedings of the National Academy of Sciences (USA), 106, 16129–34.CrossRefGoogle ScholarPubMed

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