The trouble with negative emissions
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14 October 2016
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- Glen Peters
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RE: Troubles without negative emissions
"The trouble with negative emissions" (1) raises important technological risk and intertemporal equity arguments against overreliance on negative emissions technologies (NETs) to achieve ambitious climate targets. Instead of discounting the value of NETs (1, 2), we argue that NETs are indispensable in an era of planetary risks associated with an increasingly disturbed climate system, and need to be sufficiently prepared in advance. Climate mitigation strategies that deplete the full capacity of NETs in order to undo an emission overshoot in the first half of the 21st century indeed represent a dangerous high-stakes gamble. The use of NETs was originally conceived as a risk management tool to buffer against not only climate system uncertainties (3, 4), but also those associated with global politics (5), risks which have not dissipated (6). Clearly, ambitious climate targets such as that of the Paris Agreement would become unattainable without a sufficiently large negative emission buffer should natural land and ocean carbon sinks weaken or switch to sources of emissions. Likewise, massive amounts of negative emissions will be needed if major countries continue to believe that an emission peak in2030 is still compatible with the Paris Agreement (7).
Large investments are needed in the natural, technological and human resources necessary to form a NET bulwark against unanticipated carbon cycle emergencies. An acceleration of ecosystem restoration programs recarbonizing global landscapes, soils and wetlands with resilient native species appears as a first no-regret investment. Such a restoration and conservation of ecosystems would not only be an essential climate risk hedging measure, but also a step toward meeting the Sustainable Development Goals (8). Concurrently, substantial R&D investments are needed to enhance the sustainability of carbon removal technologies, taking advantage of a large set of biological and chemical pathways. Finally, the size and dynamic properties of a minimum negative emission reserve is still to be worked out based on a quantified political and climate system risk calculus.
References and Notes
1. K. Anderson, G. Peters, The trouble with negative emissions. Science(80-. ). 354 (2016).
2. S. Fuss, J. Canadell, G. Peters, Betting on negative emissions. Nat. Clim.… (2014) (available athttp://www.nature.com/nclimate/journal/v4/n10/full/nclimate2392.html).
3. E. A. G. Schuur et al., Climate change and the permafrost carbonfeedback. Nature. 520, 171–179 (2015).
4. T. M. Lenton et al., Tipping elements in the Earth's climate system.Proc. Natl. Acad. Sci. U. S. A. 105, 1786–93 (2008).
5. M. Obersteiner et al., Managing climate risk. Science (80-. ). 294, 786–787 (2001).
6. R. Knutti, J. Sedláček, Robustness and uncertainties in the new CMIP5climate model projections. Nat. Clim. Chang. 3, 1–5 (2012).
7. UNEP, The Emissions Gap Report 2016 (United Nations EnvironmentProgramme (UNEP), Nairobi, 2016;http://uneplive.unep.org/theme/index/13#egr).
8. M. Obersteiner et al., Assessing the land resource--food price nexus ofthe Sustainable Development Goals. Sci. Adv. 2, e1501499 (2016).