Book contents
- Frontmatter
- Contents
- List of contributors
- Preface
- Part I Climate system science
- Part II Impacts and adaptation
- Part III Mitigation of greenhouse gases
- Part IV Policy design and decisionmaking under uncertainty
- 25 Climate policy design under uncertainty
- 26 Climate policy assessment using the Asia–Pacific Integrated Model
- 27 Price, quantity, and technology strategies for climate change policy
- 28 What is the economic value of information about climate thresholds?
- 29 Boiled frogs and path dependency in climate policy decisions
- 30 Article 2 and long-term climate stabilization: methods and models for decisionmaking under uncertainty
- 31 Whither integrated assessment? Reflections from the leading edge
- 32 Moving beyond concentrations: the challenge of limiting temperature change
- 33 International climate policy: approaches to policies and measures, and international coordination and cooperation
- Index
- Plate section
- References
28 - What is the economic value of information about climate thresholds?
from Part IV - Policy design and decisionmaking under uncertainty
Published online by Cambridge University Press: 06 December 2010
Book contents
- Frontmatter
- Contents
- List of contributors
- Preface
- Part I Climate system science
- Part II Impacts and adaptation
- Part III Mitigation of greenhouse gases
- Part IV Policy design and decisionmaking under uncertainty
- 25 Climate policy design under uncertainty
- 26 Climate policy assessment using the Asia–Pacific Integrated Model
- 27 Price, quantity, and technology strategies for climate change policy
- 28 What is the economic value of information about climate thresholds?
- 29 Boiled frogs and path dependency in climate policy decisions
- 30 Article 2 and long-term climate stabilization: methods and models for decisionmaking under uncertainty
- 31 Whither integrated assessment? Reflections from the leading edge
- 32 Moving beyond concentrations: the challenge of limiting temperature change
- 33 International climate policy: approaches to policies and measures, and international coordination and cooperation
- Index
- Plate section
- References
Summary
Introduction
The field of integrated assessment of climate change is undergoing a paradigm shift towards the analysis of potentially abrupt and irreversible climate changes (Alley et al., 2003; Keller et al., 2007). Early integrated studies broke important new ground in exploring the relationship between the costs and benefits of reducing carbon dioxide (CO2) emissions (e.g., Nordhaus, 1991; Manne and Richels, 1991; or Tol, 1997). These studies project the climate response to anthropogenic CO2 emissions to be relatively smooth and typically conclude that the projected benefits of reducing CO2 emissions would justify only small reductions in CO2 emissions in a cost–benefit framework. The validity of the often- assumed smooth climate response is, however, questionable, given how the climate system has responded to forcing in the geological past. Before the Anthropocene, the geological time period where humans have started to influence the global biogeochemical cycles considerably (Crutzen, 2002), the predominant responses of the climate system were forced by small changes in solar insolation occurring on timescales of thousands of years (Berger and Loutre, 1991). Yet this slow and smooth forcing apparently triggered abrupt climate changes – a threshold response where the climate system moved between different basins of attraction (Berger, 1990; Clement et al., 2001). Anthropogenic forcing may trigger climate threshold responses in the future (Alley et al., 2003; Keller et al., 2007).
- Type
- Chapter
- Information
- Human-Induced Climate ChangeAn Interdisciplinary Assessment, pp. 343 - 354Publisher: Cambridge University PressPrint publication year: 2007
References
(2000). Ice-core evidence of abrupt climate changes. Proceedings of the National Academy of Sciences of the United States of America 97 (4), 1331–1334.CrossRefGoogle ScholarPubMed
, , et al. (2002). Abrupt Climate Change: Inevitable Surprises. National Research Council.Google Scholar
and (2001). Objective estimation of the probability density function for climate sensitivity. Journal of Geophysical Research-Atmospheres 106 (D19), 22 605–22 611.CrossRefGoogle Scholar
, , and (2004). Monitoring the meridional overturning circulation in the North Atlantic: a model-based array design study. Journal of Marine Research 62 (3), 283–312.CrossRefGoogle Scholar
Baehr, J., Keller, K. and Marotzke, J. (2007). Detecting potential changes in the meridional overturning circulation at 26° N in the Atlantic, Climatic Change, published online 10 January 2007, doi: 2010.1007/S10584-10006-19153-Z.
(1982). Optimal weighting of data to detect climatic change: application to the carbon dioxide problem. Journal of Geophysical Research 87 (C13), 11 161–11 170.CrossRefGoogle Scholar
and (1991). Insolation values for the climate of the last 10 000 000 years. Quaternary Science Reviews 10 (4), 297–317.CrossRefGoogle Scholar
(1990). The Younger Dryas cold spell – a quest for causes. Global and Planetary Change 89 (3), 219–237.CrossRefGoogle Scholar
, and (2003). Climate sensitivity uncertainty and the need for energy without CO2 emission. Science 299, 2052–2054.CrossRefGoogle ScholarPubMed
(1997). Rapid sea-level changes at the close of the last interglacial (substage 5e) recorded in Bahamian island geology: comments and reply. Geology 25 (6), 572–573.2.3.CO;2>CrossRefGoogle Scholar
, , et al. (1999). Simulation of an abrupt change in Saharan vegetation in the mid-Holocene. Geophysical Research Letters 26 (14), 2037–2040.CrossRefGoogle Scholar
, and (2001). An orbitally driven tropical source for abrupt climate change. Journal of Climate 14 (11), 2369–2375.2.0.CO;2>CrossRefGoogle Scholar
Cubasch, U. and Meehl, G. A. (2001). Projections of future climate change, In Climate Change 2001: The Scientific Basis. Contribution of Working Group I of the Third Assessment Report of the Intergovernmental Panel on Climate Change, ed. , , et al. Cambridge: Cambridge University Press, pp. 526–582.Google Scholar
, et al. (1995). Large Arctic temperature change at the Wisconsin–Holocene glacial transition. Science 270, 455–458.CrossRefGoogle Scholar
and (1994). Younger Dryas age advance of Franz Josef Glacier in the Southern Alps of New Zealand. Science 264, 1434–1437.CrossRefGoogle Scholar
and (1994). The production of North Atlantic deep water: Sources, rates, and pathways. Journal of Geophysical Research 99 (C6), 12 319–12 341.CrossRefGoogle Scholar
, et al. (2001). Global temperature change and its uncertainties since 1861. Geophysical Research Letters 28 (13), 2621–2624.CrossRefGoogle Scholar
and (2000). Improved estimates of global ocean circulation, heat transport and mixing from hydrographic data. Nature 408, 453–457.CrossRefGoogle ScholarPubMed
, et al. (2005). A model intercomparison of changes in the Atlantic thermohaline circulation in response to increasing atmospheric CO2 concentration. Geophysical Research Letters 32 L12703; doi: 10.1029/2005GL023209.CrossRefGoogle Scholar
and (1982). Direct estimates and mechanisms of ocean heat transport. Deep-Sea Research 29, 339–359.CrossRefGoogle Scholar
, , et al. (2003). A monitoring design for the Atlantic meridional overturning circulation. Geophysical Research Letters 38 (7) 1413; doi: 1410.1029/2002 GL016776.Google Scholar
, and (2003). Modelling the ocean circulation beneath the Ross Ice Shelf. Antarctic Science 15 (1), 13–23.CrossRefGoogle Scholar
and (1999). The dynamic response of the Greenland and Antarctic ice sheets to multiple-century climatic warming. Journal of Climate 12 (8), 2169–2188.2.0.CO;2>CrossRefGoogle Scholar
(2000). Emissions Scenarios: A Special Report of Working Group III of the Intergovernmental Panel on Climate Change, ed. and . Cambridge: Cambridge University Press.Google Scholar
, , , and (2003). Trends in marine dissolved oxygen: implications for ocean circulation changes and the carbon budget. EOS 84, 197–204.CrossRefGoogle Scholar
, , , and (2000). Preserving the ocean circulation: implications for climate policy. Climatic Change 47, 17–43.CrossRefGoogle Scholar
, , and (2002). Possible biological or physical explanations for decadal scale trends in North Pacific nutrient concentrations and oxygen utilization. Deep-Sea-Research II 49, 345–362.CrossRefGoogle Scholar
, and , (2004). Uncertain climate thresholds and optimal economic growth. Journal of Environmental Economics and Management 48, 723–741.CrossRefGoogle Scholar
, , , and (2005). Avoiding dangerous anthropogenic interference with the climate system. Climatic Change 73, 227–238.CrossRefGoogle Scholar
, , and (2007). Early detection of changes in the North Atlantic meridional overturning circulation: implications for the design of ocean observation systems. Journal of Climate 20, 145–157.CrossRefGoogle Scholar
Keller, K., Schlesinger, M. and Yohe, G. (2007). Managing the risks of climate thresholds: uncertainties and information needs. (An editorial essay). Climatic Change, in press. Published online: 23 January 2007, http://dx.doi.org/2010.1007/S10584-10006-19114-10586.
and (1997). Rapid sea-level changes at the close of the last interglacial (substage 5e) recorded in Bahamian island geology: Comment. Geology 25 (12), 1147.2.3.CO;2>CrossRefGoogle Scholar
, and (2003). The potential role of spectral properties in detecting thresholds in the Earth system: application to the thermohaline circulation. Ocean Dynamics 53, 53–63.CrossRefGoogle Scholar
, , and (2000). Tropical stabilization of the thermohaline circulation in a greenhouse warming simulation. Journal of Climate 13, 1809–1813.2.0.CO;2>CrossRefGoogle Scholar
(2002). A new decision sciences for complex systems. Proceedings of the National Academy of Sciences of the United States of America 99, 7309–7313.CrossRefGoogle ScholarPubMed
(1992). Irregular oscillations of the West Antarctic Ice-Sheet. Nature 359, 29–32.CrossRefGoogle Scholar
(1993). Binge/purge oscillations of the Laurentide ice-sheet as a cause of the North-Atlantics Heinrich events. Paleoceanography 8 (6), 775–784.CrossRefGoogle Scholar
and (1994). Multiple-century response of a coupled ocean-atmosphere model to an increase of atmospheric carbon dioxide. Journal of Climate 7 (1), 5–23.2.0.CO;2>CrossRefGoogle Scholar
and (1995). Simulation of abrupt climate change induced by freshwater input to the North Atlantic ocean. Nature 378, 165–167.CrossRefGoogle Scholar
Marotzke, J., Cunningham, S. A. and Bryden, H. L. (2002). Monitoring the Atlantic Meridional Overturning Circulation at 26.5° N. Proposal accepted by the Natural Environment Research Council (UK). Available at www.noc.soton.ac.uk/rapidmoc.
, , , and (2003). The Max-Planck-Institute global ocean/sea ice model with orthogonal curvilinear coordinates. Ocean Modelling 5 (2), 91–127.CrossRefGoogle Scholar
and (2004). Probabilistic integrated assessment of “dangerous” climate change. Science 304, 571–575.CrossRefGoogle ScholarPubMed
and (2003). Long-term changes in dissolved oxygen concentrations in the oceans caused by protracted global warming. Global Biogeochemical Cycles 17 (4), doi: 10.1029/2002GB001997.CrossRefGoogle Scholar
, and (2000). Changes in dissolved oxygen in the Southern ocean with climate change. Geochemistry, Geophysics, Geosystems 1, Paper number 2000GC000086.CrossRefGoogle Scholar
, and (1979). Comparison of 3 methods for selecting values of input variables in the analysis of output from a computer code. Technometrics 21 (2), 239–245.Google Scholar
, , , and (2004). Collapse and rapid resumption of Atlantic meridional circulation linked to deglacial climate changes. Nature 428, 834–837.CrossRefGoogle ScholarPubMed
Meese, D. A., Alley, R. B., Fiacco, R. J. et al. (1994a). Preliminary depth-age scale of the GISP2 ice core. Special CRREL Report, 94–1.
, et al. (1994b). The accumulation record from the GISP2 core as an indicator of climate change throughout the Holocene. Nature 266, 1680–1682.Google Scholar
(1978). West Antarctic ice sheet and CO2 greenhouse effect: a threat of disaster. Nature 271, 321–325.CrossRefGoogle Scholar
and (1996). Rapid sea-level changes at the close of the last interglacial (substage 5e) recorded in Bahamian island geology. Geology 24 (9), 775–778.2.3.CO;2>CrossRefGoogle Scholar
(1991). To slow or not to slow – the economics of the greenhouse-effect. Economic Journal 101 (407), 920–937.CrossRefGoogle Scholar
(1992). An optimal transition path for controlling greenhouse gases. Science 258, 1315–1319.CrossRefGoogle ScholarPubMed
(1993). Optimal greenhouse-gas reductions and tax policy in the DICE model. American Economic Review 83 (2), 313–317.Google Scholar
(1994). Managing the Global Commons: The Economics of Climate Change. Cambridge, MA: MIT Press.Google Scholar
and (2000). Warming the World: Economic Models of Global Warming. Cambridge, MA: MIT Press.Google Scholar
and (1997). What is the value of scientific knowledge? An application to global warming using the PRICE model. Energy Journal 18 (1), 1–45.CrossRefGoogle Scholar
and (2002). Climate change – dangerous climate impacts and the Kyoto protocol. Science 296, 1971–1972.CrossRefGoogle ScholarPubMed
(1998). Global warming and the stability of the West Antarctic ice sheet. Nature 393, 322–325.CrossRefGoogle Scholar
and (2004). The West Antarctic ice sheet and long term climate policy: an editorial comment. Climatic Change 64 (1–2), 1–10.CrossRefGoogle Scholar
and (2005). Ice sheets, global warming, and Article 2 of the UNFCCC. Climatic Change 68 (3), 257–267.CrossRefGoogle Scholar
Peacock, S., Visbeck, M. and Broecker, W. (2000). Deep water formation rates inferred from global tracer distributions: an inverse approach. In Inverse Methods in Global Biogeochemical Cycles, ed. , , et al. American Geophysical Union, pp. 185–195.CrossRefGoogle Scholar
(2000). The thermohaline ocean circulation: a system with a dangerous threshold?Climatic Change 46, 247–256.CrossRefGoogle Scholar
, , et al. (1995). Ocean variability and its influence on the detectability of greenhouse warming signals. Journal of Geophysical Research: Oceans 100 (C6), 10 693–10 725.CrossRefGoogle Scholar
(2004). Gulf Stream probed for early warnings of system failure. Nature 427, 769.CrossRefGoogle ScholarPubMed
, and (1991). Reduction of deepwater formation in the Greenland Sea during the 1980's: evidence from tracer data. Science 251, 1054–1056.CrossRefGoogle Scholar
and (1999). The stability of the thermohaline circulation in global warming experiments. Journal of Climate 12, 1117–1133.2.0.CO;2>CrossRefGoogle Scholar
, , and (2005). Model projections of the North Atlantic thermohaline circulation for the 21st century assessed by observations. Geophysical Research Letters 32 L23710, doi: 23710.21029/22005GL024368.CrossRefGoogle Scholar
and (1997). Optimal reduction in CO2 emissions. Energy Policy 25 (5), 491–500.CrossRefGoogle Scholar
and (1997). Influence of CO2 emission rates on the stability of the thermohaline circulation. Nature 388, 862–865.CrossRefGoogle Scholar
Stocker, T. F., Clarke, G. K. C., Treut, H. L. et al. (2001). Physical climate processes and feedbacks. In Climate Change 2001: The Scientific Basis. Contribution of Working Group I to the Third Assessment Report of the Intergovernmental Panel on Climate Change, ed. , , et al. Cambridge: Cambridge University Press, pp. 417–470.Google Scholar
(1961). Thermohaline convection with two stable regimes of flow. Tellus 13 (2), 224–230.CrossRefGoogle Scholar
and (1999). Response of a coupled ocean-atmosphere model to increasing atmospheric carbon dioxide: sensitivity to the rate of increase. Journal of Climate 12, 2224–2237.2.0.CO;2>CrossRefGoogle Scholar
, and (1995). The GISP2 18O climate record of the past 16 500 years and the role of the sun, ocean and volcanoes. Quaternary Research 44, 341–354.CrossRefGoogle Scholar
and (2002). Freshwater outbursts to the oceans from glacial lake Agassiz and their role in climate change during the last deglaciation. Quaternary Science Reviews 21 (8–9), 879–887.CrossRefGoogle Scholar
, , et al. (2004). Accelerated sea-level rise from West Antarctica. Science 306, 255–258.CrossRefGoogle ScholarPubMed
(2001). Changes of ENSO stability due to greenhouse warming. Geophysical Research Letters 28 (10), 2061–2064.CrossRefGoogle Scholar
(1994). The damage costs of climate-change: a note on tangibles and intangibles, applied to DICE. Energy Policy 22 (5), 436–438.CrossRefGoogle Scholar
(1997). On the optimal control of carbon dioxide emissions: an application of FUND. Environmental Modeling and Assessment 2, 151–163.CrossRefGoogle Scholar
UNFCCC (1992). UN Framework Convention on Climate Change, Geneva: Palais des Nations. www.unfccc.de/index.html.
and (2002). Global climatic impacts of a collapse of the Atlantic thermohaline circulation. Climatic Change 54 (3), 251–267.CrossRefGoogle Scholar
and (2004). Timely detection of anthropogenic change in the Atlantic meridional overturning circulation. Geophysical Research Letters 31, L14203, doi: 14210.11029/12004GL02036.CrossRefGoogle Scholar
and (2001). Response of interior North America to abrupt climate oscillations in the North Atlantic region during the last deglaciation. Earth-Science Reviews 52 (4), 333–369.CrossRefGoogle Scholar
, , et al (2002). Surface melt-induced acceleration of Greenland ice-sheet flow. Science 297, 218–222.CrossRefGoogle ScholarPubMed
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