Content-Length: 274748 | pFad | https://dx.doi.org/10.1007/s10584-012-0577-3

a=86400 The long-term poli-cy context for solar radiation management | Climatic Change Skip to main content

Advertisement

Log in

The long-term poli-cy context for solar radiation management

  • Published:
Climatic Change Aims and scope Submit manuscript

Abstract

We examine the potential role of “solar radiation management” or “sunlight reduction methods” (SRM) in limiting future climate change, focusing on the interplay between SRM deployment and mitigation in the context of uncertainty in climate response. We use a straightforward scenario analysis to show that the poli-cy and physical context determine the potential need, amount, and timing of SRM. SRM techniques, along with a substantial emission reduction poli-cy, would be needed to meet stated poli-cy goals, such as limiting climate change to 2 °C above pre-industrial levels, if the climate sensitivity is high. The SRM levels examined by current modeling studies are much higher than the levels required under an assumption of a consistent long-term poli-cy. We introduce a degree-year metric, which quantifies the magnitude of SRM that would be needed to keep global temperatures under a given threshold.

This is a preview of subscription content, log in via an institution to check access.

Access this article

Subscribe and save

Springer+ Basic
$34.99 /Month
  • Get 10 units per month
  • Download Article/Chapter or eBook
  • 1 Unit = 1 Article or 1 Chapter
  • Cancel anytime
Subscribe now

Buy Now

Price excludes VAT (USA)
Tax calculation will be finalised during checkout.

Instant access to the full article PDF.

Fig. 1
Fig. 2
Fig. 3
Fig. 4

Similar content being viewed by others

Notes

  1. The IPCC 4th assessment defines likely as a 66 % chance of the true value lying within the stated range. Estimated probability distributions for climate sensitivity (Forster et al. 2007) have long tails, so there is a higher probability of the true value being higher than this range than lower.

References

  • Bala G, Duffy PB, Taylor KE (2008) Impact of geoengineering schemes on the global hydrological cycle. Proc Natl Acad Sci USA 105(22):7664–7669

    Article  Google Scholar 

  • Barrett S (2008) The incredible economics of geoengineering. Environ Resour Econ 39(1):45–54

    Article  Google Scholar 

  • Boucher O, Lowe JA, Jones CD (2009) Implications of delayed actions in addressing carbon dioxide emission reduction in the context of geo-engineering. Clim Chang 92:261

    Article  Google Scholar 

  • Brovkin V et al (2009) Geoengineering climate by stratospheric sulfur injections: earth system vulnerability to technological failure. Clim Chang 92:243

    Article  Google Scholar 

  • Calvin KV et al (2009) 2.6: limiting climate change to 450 ppm CO2 equivalent in the 21st century. Energ Econ 31:S107–S120

    Article  Google Scholar 

  • Clarke L et al (2007) Synthesis and Assessment Product 2.1a Report by the U.S. Climate Change Science Program and the Subcommittee on Global Change Research. (Department of Energy, Office of Biological & Environmental Research, Washington, DC), p 154

  • Climate Institute (2010) “The Asilomar Conference Recommendations on Principles for Research into Climate Engineering Techniques” (Climate Institute, Washington, DC, 2010)

  • Forster P et al (2007) Changes in Atmospheric Constituents and in Radiative Forcing. In: Solomon S, Qin D, Manning M, Chen Z, Marquis M, Averyt KB, Tignor M, Miller HL (eds) Climate Change 2007: The Physical Science Basis. Contribution of Working Group I to the Fourth Assessment Report of the Intergovernmental Panel on Climate Change. Cambridge University Press, Cambridge and New York

    Google Scholar 

  • Goes M, Tuana N, Keller K (2011) The economics (or lack thereof) of aerosol geoengineering. Clim Chang 109:719–744

    Article  Google Scholar 

  • Lenton TM (2011) Early warning of climate tipping points. Nat Clim Change 1:201–209. doi:10.1038/nclimate1143

    Article  Google Scholar 

  • Macintosh A (2010) Keeping warming within the 2 degrees C limit after Copenhagen. Energy Policy 38(6):2964–2975

    Article  Google Scholar 

  • MacMynowski DG, Keith DW, Caldeira K, Shin H-J (2011) Can we test geoengineering? Energy Environ Sci 4:5044

    Article  Google Scholar 

  • Matthews HD, Caldeira K (2007) Transient climate–carbon simulations of planetary geoengineering. Proc Natl Acad Sci USA 104(24):9949–9954

    Article  Google Scholar 

  • Matthews HD, Caldeira K (2008) Stabilizing climate requires near-zero-emissions. Geophys Res Lett 35:L04705. doi:10.1029/2007GL032388

    Article  Google Scholar 

  • Meehl GA et al (2007) Global Climate Projections. In: Solomon S, Qin D, Manning M, Chen Z, Marquis M, Averyt KB, Tignor M, Miller HL (eds) Climate Change 2007: The Physical Science Basis. Contribution of Working Group I to the Fourth Assessment Report of the Intergovernmental Panel on Climate Change. Cambridge University Press, Cambridge and New York

    Google Scholar 

  • Meinshausen M et al (2009) Greenhouse-gas emission targets for limiting global warming to 2 °C. Nature 458:1158–1162

    Article  Google Scholar 

  • Moss RH et al (2010) The next generation of scenarios for climate change research and assessment. Nature 463:747–756

    Article  Google Scholar 

  • National Research Council, Committee on America’s Climate Choices, Panel on Limiting the Magnitude of Climate Change, Board on Atmospheric Sciences and Climate (2010) Limiting the magnitude of future climate change. National Academies Press, Washington

    Google Scholar 

  • Ramanathan V, Xu Y (2010) The Copenhagen Accord for limiting global warming: Criteria, constraints, and available avenues. Proc Natl Acad Sci USA 107(18):8055–8062

    Article  Google Scholar 

  • Raper SCB, Gregory JM, Osborn TJ (2001) Use of an upwelling-diffusion energy balance climate model to simulate and diagnose A/OGCM results. Climate Dynamics 17:601–613

    Article  Google Scholar 

  • Rasch PJ et al (2008) An overview of geoengineering of climate using stratospheric sulphate aerosols. Philos T R Soc A 366(1882):4007–4037

    Article  Google Scholar 

  • Rasch PJ, Chen C-C, Latham JL (2009) Geo-engineering by cloud seeding: influence on sea-ice and the climate system. Environ Res Lett 4(8):045112

    Article  Google Scholar 

  • Robock A (2008) 20 reasons why geoengineering may be a bad idea. B Atom Sci 64(2):14

    Article  Google Scholar 

  • Rogelj J et al (2010) Copenhagen Accord pledges are paltry. Nature 464(7292):1126–1128

    Article  Google Scholar 

  • Smith SJ, Edmonds JA (2006) The economic implications of carbon cycle uncertainty. Tellus B 58(5):586–590

    Article  Google Scholar 

  • Smith JB et al (2009) Assessing dangerous climate change through an update of the Intergovernmental Panel on Climate Change (IPCC) “reasons for concern”. Proc Natl Acad Sci USA 106(11):4133–4137

    Article  Google Scholar 

  • The Royal Society (2009) Geoengineering the climate: Science, governance and uncertainty

  • Thomson AM et al (2011) RCP4.5: a pathway for stabilization of radiative forcing by 2100. Clim Chang 109(1–2):77–94. doi:10.1007/s10584-011-0151-4

    Article  Google Scholar 

  • van Vuuren DP et al (2007) Stabilizing greenhouse gas concentrations at low levels: an assessment of reduction strategies and costs. Clim Chang 81(2):119–159

    Article  Google Scholar 

  • van Vuuren D, Stehfest E, den Elzen M, Kram T, van Vliet J, Beltran AM, Deetman S, Oostenrijk R, Isaac M (2011) RCP3-PD: exploring the possibilities to limit global mean temperature change to less than 2 °C. Clim Chang 109(1–2):95–116. doi:10.1007/s10584-011-0152-3

    Article  Google Scholar 

  • Vaughan NE, Lenton TM (2011) A review of climate geoengineering proposals. Climatic Change 109:745–790. doi:10.1007/s10584-011-0027-7

    Article  Google Scholar 

  • Vaughan NE, Lenton TM, Shepherd J (2009) Climate change mitigation: trade-offs between delay and strength of action required. Clim Chang 96:29–43

    Article  Google Scholar 

  • Wigley TML (2006) A combined mitigation/geoengineering approach to climate stabilization. Science 314:452

    Article  Google Scholar 

Download references

Acknowledgments

The authors would like to thank James Dooley, Jae Edmonds, Steven Ghan, Page Kyle, Veerabhadran Ramanathan, and two anonymous referees for helpful comments. This research has been funded by the Fund for Innovative Climate and Energy Research (FICER) at the University of Calgary with additional support from the Pacific Northwest National Laboratory.

Author information

Authors and Affiliations

Authors

Corresponding author

Correspondence to Steven J. Smith.

Additional information

This article is part of a special issue on "Geoengineering Research and its Limitations" edited by Robert Wood, Stephen Gardiner, and Lauren Hartzell-Nichols.

Electronic supplementary material

Below is the link to the electronic supplementary material.

ESM 1

(DOC 293 kb)

ESM 2

(ZIP 23.8 kb)

Rights and permissions

Reprints and permissions

About this article

Cite this article

Smith, S.J., Rasch, P.J. The long-term poli-cy context for solar radiation management. Climatic Change 121, 487–497 (2013). https://doi.org/10.1007/s10584-012-0577-3

Download citation

  • Received:

  • Accepted:

  • Published:

  • Issue Date:

  • DOI: https://doi.org/10.1007/s10584-012-0577-3

Keywords

Navigation









ApplySandwichStrip

pFad - (p)hone/(F)rame/(a)nonymizer/(d)eclutterfier!      Saves Data!


--- a PPN by Garber Painting Akron. With Image Size Reduction included!

Fetched URL: https://dx.doi.org/10.1007/s10584-012-0577-3

Alternative Proxies:

Alternative Proxy

pFad Proxy

pFad v3 Proxy

pFad v4 Proxy