Abstract
Many of the findings of the Charney Report on CO2-induced climate change published in 1979 are still valid, even after 30 additional years of climate research and observations. This paper considers the reasons why the report was so prescient, and assesses the progress achieved since its publication. We suggest that emphasis on the importance of physical understanding gained through the use of theory and simple models, both in isolation and as an aid in the interpretation of the results of General Circulation Models, provided much of the authors’ insight at the time. Increased emphasis on these aspects of research is likely to continue to be productive in the future, and even to constitute one of the most efficient routes towards improved climate change assessments.
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References
Andrews T, Forster PM (2008) CO2 forcing induces semi-direct effects with consequences for climate feedback interpretations. Geophys Res Lett 35, L04802. doi:10.1029/2007GL032273
Banks HT, Gregory JM (2006) Mechanisms of ocean heat uptake in a coupled climate model and the implications for tracer based predictions of ocean heat uptake. Geophys Res Lett 33(7), L07608. doi:10.1029/2005gl025352
Bolin B, Degens ET, Kempe S, Ketner P (eds) (1979) The global carbon cycle. SCOPE 13, Scientific Committee on Problems of the Environment, International Council of Scientific Unions, Wiley, New York, 491 pp
Bony S, Colman R, Kattsov VM, Allan RP, Bretherton CS, Dufresne JL, Hall A, Hallegatte S, Holland MM, Ingram W, Randall DA, Soden BJ, Tselioudis G, Webb MJ (2006) How well do we understand and evaluate climate change feedback processes ? J Clim 19(15):3445–3482
Bony S, Bellon G, Klocke D, Sherwood S, Fermepin S, Denvil S (2013) Robust direct effect of carbon dioxide on tropical circulation and regional precipitation. Nat Geosci. doi: 10.1038/ngeo1799
Boyle J, Klein SA (2010) Impact of horizontal resolution on climate model forecasts of tropical precipitation and diabatic heating for the TWP-ICE period. J Geophys Res 115, D23113
Brient F, Bony S (2013) Interpretation of the positive low-cloud feedback predicted by a climate model under global warming. Clim Dyn 40(9–10):2415–2431. doi:10.1007/s00382-011-1279-7. ISSN: 0930-7575
Caldeira K, Jain AK, Hoffert MI (2003) Climate sensitivity uncertainty and the need for energy without CO2 emission. Science 299:2052–2054
Charney JG, Coauthors (1979) Carbon dioxide and climate: a scientific assessment. National Academy of Science, Washington, DC, 22 pp
Church JA, Godfrey JS, Jackett DR, McDougall TJ (1991) A model of sea-level rise caused by ocean thermal expansion. J Cli 4(4):438–456
Collins WD et al (2006) Radiative forcing by well-mixed greenhouse gases: estimates from climate models in the Intergovernmental Panel on Climate Change (IPCC) fourth assessment report (AR4). J Geophys Res 111, D14317. doi:10.1029/2005JD006713
Colman RA, McAvaney BJ (2010) On tropospheric adjustment to forcing and climate feedbacks. Clim Dyn 36(9–10):1649–1658
Cox PM, Betts RA, Jones CD, Spall SA, Totterdell IJ (2000) Acceleration of global warming due to carbon-cycle feedbacks in a coupled climate model. Nature 408:184–187
Dahan-Dalmedico A (2001) History and epistemology of models: meteorology (1946–1963) as a case study. Arch Hist Exact Sci 55:395–422, Springer, pp 395–422
Delmas RJ, Ascencio J-M, Legrand M (1980) Polar ice evidence that atmospheric CO2 20,000 yr BP was 50% of present. Nature 284:155–157
Denman KL, Brasseur G, Chidthaisong A, Ciais P, Cox PM, Dickinson RE, Hauglustaine D, Heinze C, Holland E, Jacob D et al (2007) Couplings between changes in the climate system and biogeochemistry. In: Solomon S, Qin Q, 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/New York
Dufresne J-L, Bony S (2008) An assessment of the primary sources of spread of global warming estimates from coupled ocean-atmosphere models. J Clim 21(19):5135–5144
Dufresne J-L, Friedlingstein P, Berthelot M, Bopp L, Ciais P, Fairhead L, Le Treut H, Monfray P (2002) On the magnitude of positive feedback between future climate change and the carbon cycle. Geophys Res Lett 29(10). doi:10.1029/2001GL013777A
Eitzen ZA, Xu KM, Wong T (2009) Cloud and radiative characteristics of tropical deep convective systems in extended cloud objects from CERES observations. J Clim 22:5983–6000
Farneti R, Delworth TL, Rosati AJ, Griffies SM, Zeng F (2010) The role of mesoscale eddies in the rectification of the Southern ocean response to climate change. J Phys Oceanogr 40:1539–1557. doi:10.1175/2010JPO4353.1
Frank DC, Esper J, Raible CC, Buntgen U, Trouet V, Stocker B, Joos F (2010) Ensemble reconstruction constraints on the global carbon cycle sensitivity to climate. Nature 463:527–530
Freeland H et al (2010) Argo – a decade of progress. In: Hall J, Harrison DE, Stammer D (eds) Proceedings of OceanObs’09: sustained ocean observations and information for society, vol 2, Venice, Italy, 21–25 Sept 2009. ESA Publication WPP-306, Roma. doi:10.5270/OceanObs09.cwp.32
Friedlingstein P et al (2006) Climate – carbon cycle feedback analysis, results from the C4MIP model intercomparison. J Clim 19:3337–3353
Friedlingstein P, Houghton RA, Marland G, Hackler J, Boden TA, Conway TJ, Canadell JG, Raupach MR, Ciais P, Le Quéré C (2010) Update on CO2 emissions. Nat Geosci 3:811–812
Gregory JM, Webb M (2008) Tropospheric adjustment induces a cloud component in CO2 forcing. J Clim 21:58–71
Gregory JM et al (2004) A new method for diagnosing radiative forcing and climate sensitivity. Geophys Res Lett 31, L03205. doi:10.1029/2003GL018747
Griffies S et al (2010) Problems and prospects in large-scale ocean circulation models. In: Hall J, Harrison D E, Stammer D (eds) Proceedings of OceanObs’09: sustained ocean observations and information for society, vol 2, Venice, Italy, 21–25 Sept 2009. ESA Publication WPP-306, Roma. doi:10.5270/OceanObs09.cwp.38
Hall A, Qu X (2006) Using the current seasonal cycle to constrain snow albedo feedback in future climate change. Geophys Res Lett 33, L03502. doi:10.1029/2005GL025127
Hannart A, Dufresne J-L, Naveau P (2009) Why climate sensitivity may not be so unpredictable. Geophys Res Lett 36, L16707. doi:10.1029/2009GL039640
Hansen JE, Sato M (2011) Paleoclimate implications for human-made climate change. In: Berger A, Mesinger F, Šijački D (eds) Climate change at the eve of the second decade of the century: inferences from paleoclimate and regional aspects: Proceedings of Milutin Milankovitch 130th anniversary symposium. Springer.
Hansen J, Lacis A, Rind D, Russell G, Stone P, Fung I, Ruedy R, Lerner J (1984) Climate sensitivity: analysis of feedback mechanisms. In: Climate processes and climate sensitivity, Geophysical Monograph. American Geophysical Union, Washington, DC, pp 130–163
Hansen J, Sato M, Nazarenko L, Ruedy R, Lacis A, Koch D, Tegen I, Hall T, Shindell D, Santer B, Stone P, Novakov T, Thomason T, Wang R, Wang Y, Jacob D, Hollandsworth S, Bishop L, Logan J, Thompson A, Stolarski R, Lean J, Willson R, Levitus S, Antonov J, Rayner N, Parker D, Christy J (2002) Climate forcings in Goddard Institute for space studies SI2000 simulations. J Geophys Res 107(D18):4347. doi:10.1029/2001JD001143
Hartmann DL, Larson K (2002) An important constraint on tropical cloud-climate feedback. Geophys Res Lett 29:1951–1954
Hartmann DL, Short DA (1980) On the use of earth radiation budget statistics for studies of clouds and climate. J Atmos Sci 37:1233–1250
Held IM (2005) The gap between simulation and understanding in climate modeling. Bull Am Meteorol Soc 86:1609–1614
Held IM, Soden BJ (2006) Robust responses of the hydrological cycle to global warming. J Climate 19:5686–5699. doi:10.1175/JCLI3990.1
Held IM, Hemler RS, Ramaswamy V (1993) Radiative-convective equilibrium with explicit two-dimensional moist convection. J Atmos Sci 50:3909–3927
Klein SA, Hartmann DL (1993) The seasonal cycle of low stratiform clouds. J Clim 6(8):1587–1606
Kuang Z, Hartmann DL (2007) Testing the fixed anvil temperature hypothesis in a cloud-resolving model. J Clim 20:2051–2057
Le Quéré C, Raupach MR, Canadell JG, Marland G, Bopp L, Ciais P, Conway TJ, Doney SC, Feely RA, Foster P, Friedlingstein P, Gurney K, Houghton RA, House J, Huntingford C, Levy PE, Lomas MR, Majkut J, Metzl N, Ometto JP, Peters GPII, Prentice C, Randerson JT, Running SW, Sarmiento JL, Schuster U, Sitch S, Takahashi T, Viovy N, Van Der Werf GR, Woodward FI (2009) Trends in the sources and sinks of carbon dioxide. Nat Geosci 2:831–836
Legg S et al (2009) Improving oceanic overflow representation in climate models: the gravity current entrainment climate process team. Bull Am Meteorol Soc 90:657–670
Lyman JM, Good SA, Gouretski VV, Ishii M, Johnson GC, Palmer MD, Smith DM, Willis JK (2010) Robust warming of the global upper ocean. Nature 465:334–337. doi:10.1038/nature09043
MacDonald GF, Abarbanel H, Carruthers P, Chamberlain J, Foley H, Munk W, Nierenberg W, Rothaus O, Ruderman M, Vesecky J, Zachariasen F (1979) The long term impact of atmospheric carbon dioxide on climate, JASON technical report JSR-78-07, SRI International, Arlington
Manabe S, Wetherald RT (1967) Thermal equilibrium of the atmosphere with a given distribution of relative humidity. J Atmos Sci 24:241–259
Manabe S, Wetherald RT (1975) The effects of doubling the CO2 concentration on the climate of a general circulation model. J Atmos Sci 32:3–15
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 1 to the fourth assessment report of the Intergovernmental Panel on Climate Change. Cambridge University Press, Cambridge, UK/New York
Meehl GA, Arblaster JM, Fasullo JT, Hu A, Trenberth KE (2011) Model-based evidence of deep-ocean heat uptake during surface-temperature hiatus periods. Nat Clim Change 1:360–364
Mitchell JFB, Ingram WJ (1992) Carbon dioxide and climate: mechanisms of changes in cloud. J Clim 5:5–21
Myhre G, Myhre A, Stordal F (2001) Historical time evolution of total radiative forcing. Atmos Environ 35:2361–2373
Ramanathan V, Lian MS, Cess RD (1979) Increased atmospheric CO2: zonal and seasonal estimates of the effect on radiative energy balance and surface temperature. J Geophys Res 84(C8):4949–4958
Randall DA et al (2007) Climate models and their evaluation. 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 1 to the fourth assessment report of the Intergovernmental Panel on Climate Change. Cambridge University Press, Cambridge, UK/New York
Rieck M, Nuijens L, Stevens B (2012) Marine boundary layer cloud feedbacks in a constant relative humidity atmosphere. J Atmos Sci 69:2538–2550. doi:10.1175/JAS-D-11-0203.1
Roe GH, Baker MB (2007) Why is climate sensitivity so unpredictable? Science 318(5850):629–632. doi:10.1029/2009GL039640
Shine KP, Cook J, Highwood EJ, Joshi MM (2003) An alternative to radiative forcing for estimating the relative importance of climate change mechanisms. Geophys Res Lett 30(20):2047. doi:10.1029/2003GL018141
Soden BJ, Jackson DL, Ramaswamy V, Schwarzkopf MD, Huang X (2005) The radiative signature of upper tropospheric moistening. Science 310:841–844
Somerville RCJ, Remer LA (1984) Cloud optical thickness feedbacks in the CO2 climate problem. J Geophys Res 89(D6):9668–9672. doi:10.1029/JD089iD06p09668
Son S-W, Gerber EP, Perlwitz J, Polvani LM, Gillett N, Seo K-H, CCMVal Co-authors (2010) Impact of stratospheric ozone on the southern hemisphere circulation change: a multimodel assessment. J Geophys Res 115:D00M07. doi:10.1029/2010JD014271
Trenberth KE, Fasullo JT (2010) Tracking earth’s energy. Science 328:316–317
Wetherald R, Manabe S (1988) Cloud feedback processes in a general circulation model. J Atmos Sci 45:1397–1415
Williams KD, Ingram WJ, Gregory JM (2008) Time variation of effective climate sensitivity in GCMs. J Clim 21:5076–5090. doi:10.1175/2008JCLI2371.1
Yohe G, Andronova N, Schlesinger M (2004) To hedge or not against an uncertain climate future? Science 306:416–417
Zelinka MD, Hartmann DL (2010) Why is longwave cloud feedback positive ? J Geophys Res 115, D16117. doi:10.1029/2010JD013817
Zhang M, Bretherton C (2008) Mechanisms of low cloud–climate feedback in idealized single-column simulations with the community atmospheric model, version 3 (CAM3). J Clim 21(18):4859–4878. doi:10.1175/2008JCLI2237.1
Acknowledgments
We thank Hervé Le Treut and Amy Dahan-Dalmedico for valuable comments and discussions with who helped us put the discussions of this opinion paper into an historical context. We are grateful to V. Ramaswamy, two anonymous reviewers and several participants of the WCRP Open Science Conference (Denver, CO, October 2011) for thorough comments and suggestions that helped improve the manuscript. This paper was supported by the French ANR project ClimaConf.
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Bony, S. et al. (2013). Carbon Dioxide and Climate: Perspectives on a Scientific Assessment. In: Asrar, G., Hurrell, J. (eds) Climate Science for Serving Society. Springer, Dordrecht. https://doi.org/10.1007/978-94-007-6692-1_14
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