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Global Warming and a Potential Tipping Point in the Atlantic Thermohaline Circulation: The Role of Risk Aversion

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Abstract

The risk of catastrophes is one of the greatest threats of climate change. Yet, conventional assumptions shared by many integrated assessment models such as DICE lead to the counterintuitive result that higher concern about climate change risks does not lead to stronger near-term abatement efforts. This paper examines whether this result still holds in a refined DICE model that employs the Epstein–Zin utility specification and that is fully coupled with a dynamic tipping point model describing the evolution of the Atlantic thermohaline circulation (THC). Risk is captured by the possibility of a future collapse of the circulation and it is nourished by fat-tailed uncertainty about climate sensitivity. This uncertainty is assumed to resolve in the middle of the second half of this century and the near-term abatement efforts, which are undertaken before that point of time, can be adjusted afterwards. These modelling choices allow posing the question of whether aversion to this specific tipping point risk has a significant effect on near-term policy efforts. The simulations, however, provide evidence that it has little effect. For the more likely climate sensitivity values, a collapse of the circulation would occur in the more distant future. In this case, acting after learning can prevent the catastrophe, implying the remarkable insensitivity of the near-term policy to risk aversion. For the rather unlikely and high climate sensitivity values, the expected damage costs are not great enough to justify taking very costly measures to safeguard the THC. Our simulations also provide some indication that risk aversion might have some effect on near-term policy, if inertia limiting the speed of decarbonisation is accounted for. As it is highly uncertain how restrictive this kind of inertia will be, future research might investigate the effects of risk aversion if additional uncertainty about inertia is considered.

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Notes

  1. Long-run predictions about the THC, however, involve tremendous uncertainties and the estimates of future circulation strength are therefore somewhat speculative (Matei et al. 2012). As reviewed by Lenton and Ciscar (2013), the expert elicitation study by Kriegler et al. (2009) and the IPCC (2007) suggest that rather high temperatures (\(>\)4 \(^{\circ }\)C) are needed to push the THC towards collapse. However, these models are criticised for being biased towards the stability of the THC dynamics (Drijfhout et al. 2011; Hofmann and Rahmstorf 2009) and observations indicate a higher vulnerability of the THC (Drijfhout et al. 2011; Hawkins et al. 2011). A recent probabilistic assessment of different representative concentration pathways (RCPs) by Schleussner et al. (2014) shows that a significant slowdown of the THC is within the likely range, in particular for the unmitigated climate change scenario.

  2. For a recent survey see DeLong and Magin (2009).

  3. The benchmark study by Weitzman (2009) reveals that, as a result of plausible values of uncertain parameters, the probability of extreme losses is much larger than predicted by, for instance, normal distribution. Particularly, as shown by Urban and Keller (2010) for Atlantic meridional overturning circulation, the policy-relevant projections are strongly linked to tail-area parameter estimates.

  4. It must be noted, that while the simplified treatment of uncertainty serves the purpose of our study well, in reality uncertainty about a potential THC collapse is likely not to be resolved even if the climate sensitivity value is perfectly known. In fact, the projections of a THC collapse depend on many more uncertain parameters, some of which are correlated. Accordingly, Urban and Keller (2010) propose the concept that breaks important new ground in risk analysis. The authors use the nonparametric Bayesian inversion approach to derive probabilistic projections of a THC collapse by accounting for the tail areas of the parameter probability distributions and for more observational constraints of relevance.

  5. The most important modifications to DICE-2007 implemented by Cai et al. (2012a) involve recalibrations of the parameters owing to the different time units. In addition, the atmospheric temperature response function is adjusted to rule out warming being affected by future atmospheric carbon concentrations. Note that ‘continuous’ refers to a time-discretization of 1-year time steps.

  6. The next section describes in detail how these values and their probabilities are derived.

  7. Note that it is not within the scope of this paper to explore the learning process itself. The assumptions regarding the learning process are made for the mere reason to keep the analysis tractable and to limit computational costs. In reality, learning about climate sensitivity will most likely happen gradually as observations of the temperature evolution and/or research findings provide more information. For an overview of studies assessing the learning time-scales and for a recent approach to exploring them, see Urban et al. (2014). Ackerman et al. (2013) have chosen learning to take place in a meaningful time interval: the period of uncertainty must be long enough to rule out the dominance of the wait-and-see strategy and short enough to grant learning and particularly acting after learning some importance. Indeed, this way of modelling learning is not uncommon in the literature (e.g. Hall et al. 2012; Iverson and Perrings 2012; McInerney et al. 2012; Neubersch et al. 2014). In the next section, we shall undertake a robustness analysis to test for the sensitivity of our results. For further information on learning about a threshold in the THC, see Keller and McInerney (2008). For a general survey of learning-related questions, see O’Neill et al. (2006).

  8. Of course, there are also other extensions of the DICE model that replace the original damage function by a rate-dependent version, for example Goes et al. (2011).

  9. These simulations show that the result with respect to the effect of risk aversion is robust to alternative choices for \(m_{crit}\).

  10. Urban et al. (2014) report faster learning rates for lower climate sensitivities than for higher values.

  11. A possible approach for a more refined modelling of inertia is to implement quadratic adjustment costs in the costs function. See Ha-Duong et al. (1997) for implementation in an IAM and see Dixit and Pindyck (1994) for application in real option models tackling general questions of investment under uncertainty.

  12. The GAMS code is available upon request.

  13. The GRG is a generalisation of the reduced gradient (RG) technique which allows nonlinear constraints. The key idea behind the GRG is to transform the constrained problem to bound constrained and thus reduce the number of independent variables. The further search is performed in the direction of the gradient of the superbasic variables. There are many possible GRG algorithms and CONOPT3 identifies the most appropriate for the particular problem setting. Please refer to Abadie (1969) for the concept of GRG and to Drud (1992) for its implementation in CONOPT.

References

  • Abadie J, Carpentier J (1969) Generalization of the Wolfe reduced gradient method to the case of nonlinear constraints. In: Fletcher R(ed) Optimization. Academic Press, New York, pp 37–47

  • Ackerman F, DeCanio S, Howarth R, Sheeran K (2009) Limitations of integrated assessment models of climate change. Clim Change 95(3–4):297–315

    Article  Google Scholar 

  • Ackerman F, Stanton EA, Bueno R (2013) Epstein-Zin utility in DICE: is risk aversion irrelevant to climate policy? Environ Res Econ 56(1):73–84

    Article  Google Scholar 

  • Bansal R, Yaron A (2004) Risks for the long run: a potential resolution of asset pricing puzzles. J Finance 59(4):1481–1509

    Article  Google Scholar 

  • Barro RJ (2013) Environmental protection, rare disasters, and discount rates. In: Working paper 19258, National Bureau of Economic Research

  • Cai Y, Judd KL, Lontzek TS (2012a) Continuous-time methods for integrated assessment models. In: Working paper 18365, National Bureau of Economic Research

  • Cai Y, Judd KL, Lontzek TS (2012b) Open science is necessary. Nat Clim Change 2:299–299

    Article  Google Scholar 

  • Cai Y, Judd KL, Lontzek TS (2013) The social cost of stochastic and irreversible climate change. In: Working paper 18704, National Bureau of Economic Research

  • Cass D (1965) Optimum growth in an aggregative model of capital accumulation. Rev Econ Stud 32(3):233–240

    Article  Google Scholar 

  • Cline WR (1992) The economics of global warming. No. 39 in Peterson Institute Press: All Books. Peterson Institute for International Economics

  • Crost B, Traeger CP (2010) Risk and aversion in the integrated assessment of climate change. In: CUDARE working paper series 1104R, University of California at Berkeley, Department of Agricultural and Resource Economics and Policy

  • DeLong JB, Magin K (2009) The US equity return premium: past, present, and future. J Econ Perspect 23(1):193–208

    Article  Google Scholar 

  • den Elzen MG, van Vuuren D, van Vliet J (2010) Postponing emission reductions from 2020 to 2030 increases climate risks and long-term costs. Clim Change 99(1–2):313–320. doi:10.1007/s10584-010-9798-5

    Article  Google Scholar 

  • Dixit AK, Pindyck RS (1994) Investment under Uncertainty. Princeton University Press, Princeton

    Google Scholar 

  • Drijfhout S, Weber S, Swaluw E (2011) The stability of the MOC as diagnosed from model projections for pre-industrial, present and future climates. Clim Dyn 37(7–8):1575–1586

    Article  Google Scholar 

  • Drud A (1992) Conopt—a large-scale GRG code. ORSA J Comput 6:207–216

    Article  Google Scholar 

  • Epstein LG, Zin SE (1989) Substitution, risk aversion, and the temporal behavior of consumption and asset returns: a theoretical framework. Econometrica 57(4):937–969

    Article  Google Scholar 

  • Epstein LG, Zin SE (1991) Substitution, risk aversion, and the temporal behavior of consumption and asset returns: an empirical analysis. J Polit Econ 99:263–286

    Article  Google Scholar 

  • Ganachaud A, Wunsch C (2000) Improved estimates of global ocean circulation, heat transport and mixing from hydrographic data. Nature 408:453–457

    Article  Google Scholar 

  • Goes M, Tuana N, Keller K (2011) The economics (or lack thereof) of aerosol geoengineering. Clim Change 109(3–4):719–744

    Article  Google Scholar 

  • Grübler A, Nakic̀enovic̀ N, Victor DG (1999) Dynamics of energy technologies and global change. Energy Policy 27(5):247–280

    Article  Google Scholar 

  • Ha-Duong M, Grubb MJ, Hourcade J-C (1997) Influence of socioeconomic inertia and uncertainty on optimal \({\rm CO}_2\)-emission abatement. Nature 390:270–273

    Article  Google Scholar 

  • Ha-Duong M, Treich N (2004) Risk aversion, intergenerational equity and climate change. Environ Res Econ 28(2):195–207

    Article  Google Scholar 

  • Hall JW, Lempert RJ, Keller K, Hackbarth A, Mijere C, McInerney DJ (2012) Robust climate policies under uncertainty: a comparison of robust decision making and info-gap methods. Risk Anal 32(10):1657–1672

    Article  Google Scholar 

  • Hawkins E, Smith RS, Allison LC, Gregory JM, Woollings TJ, Pohlmann H, de Cuevas B (2011) Bistability of the Atlantic overturning circulation in a global climate model and links to ocean freshwater transport. Geophys Res Lett 38(10):L10605

    Article  Google Scholar 

  • Hofmann M, Rahmstorf S (2009) On the stability of the Atlantic meridional overturning circulation. Proc Nat Acad Sci 106(49):20584–20589

    Article  Google Scholar 

  • Hope C (2006) The marginal impact of \({\rm CO}_2\) from PAGE2002: an integrated assessment model incorporating the IPCC’s five reasons for concern. Integr Assess 6(1):19–56

    Google Scholar 

  • IPCC (2007) Summary for policymakers. In: Solomon SD, Qin M, Manning Z, Chen M, Marquis K, Averyt M, Tignor Miller H (eds) Climate change 2007: the physical science basis. In: Contribution of working group I to the fourth assessment report of the intergovernmental panel on climate change. Cambridge University Press, Cambridge

  • Iverson T, Perrings C (2012) Precaution and proportionality in the management of global environmental change. Glob Environ Change 22(1):161–177

    Article  Google Scholar 

  • Jensen S, Traeger C (2014) Optimal climate change mitigation under long-term growth uncertainty: stochastic integrated assessment and analytic findings. Eure Econ Rev 69(C):104–125

  • Kaufman N (2012) The bias of integrated assessment models that ignore climate catastrophes. Clim Change 110(3–4):575–595

    Article  Google Scholar 

  • Keller K, Bolker BM, Bradford DF (2004) Uncertain climate thresholds and optimal economic growth. J Environ Econ Manage 48:723–741

    Article  Google Scholar 

  • Keller K, McInerney D (2008) The dynamics of learning about a climate threshold. Clim Dyn 30(2–3):321–332

    Article  Google Scholar 

  • Keller K, Tan K, Morel FM, Bradford DF (Jan. 2000) Preserving the ocean circulation: implications for climate policy. In: NBER working papers 7476, National Bureau of Economic Research, Inc

  • Kelly DL, Kolstad CD (1999) Bayesian learning, growth, and pollution. J Econ Dyn Control 23:491–518

    Article  Google Scholar 

  • Koopmans TC (1963) On the concept of optimal economic growth. In: Cowles Foundation discussion papers 163, Cowles Foundation for Research in Economics, Yale University

  • Kopp RE, Hsiang SM, Oppenheimer M (2013) Empirically calibrating damage functions and considering stochasticity when integrated assessment models are used as decision tools. In: Impacts world 2013 conference proceedings

  • Kreps DM, Porteus EL (1978) Temporal resolution of uncertainty and dynamic choice theory. Econometrica 46(1):185–200

    Article  Google Scholar 

  • Kriegler E, Hall JW, Held H, Dawson R, Schellnhuber HJ (2009) Imprecise probability assessment of tipping points in the climate system. Proc Natl Acad Sci 106(13):5041–5046

  • Kuhlbrodt T, Rahmstorf S, Zickfeld K, Vikebø F, Sundby S, Hofmann M, Link PM, Bondeau A, Cramer W, Jaeger C (2009) An integrated assessment of changes in the thermohaline circulation. Clim Change 96(4):489–537

    Article  Google Scholar 

  • Lecocq F, Hourcade JC, Ha-Duong M (1998) Decision making under uncertainty and inertia constraints: sectoral implications of the when flexibility. Energy Econ 20(4/5):539–555

    Article  Google Scholar 

  • Lemoine D, Traeger C (2014) Watch your step: optimal policy in a tipping climate. Am Econ J Econ Policy 6(1):137–166

    Article  Google Scholar 

  • Lempert RJ, Sanstad AH, Schlesinger ME (2006) Multiple equilibria in a stochastic implementation of DICE with abrupt climate change. Energy Econ 28(5–6):677–689

    Article  Google Scholar 

  • Lenton T, Ciscar J-C (2013) Integrating tipping points into climate impact assessments. Clim Change 117(3):585–597

    Article  Google Scholar 

  • Lenton TM, Held H, Kriegler E, Hall JW, Lucht W, Rahmstorf S, Schellnhuber HJ (2008) Tipping elements in the Earth’s climate system. Proc Natl Acad Sci USA 105:1786–1793

    Article  Google Scholar 

  • Link P, Tol R (2011) Estimation of the economic impact of temperature changes induced by a shutdown of the thermohaline circulation: an application of FUND. Clim Change 104(2):287–304

    Article  Google Scholar 

  • Lontzek TS, Cai Y, Judd KL (2012) Tipping points in a dynamic stochastic IAM. In: RDCEP working paper 12-03, RDCEP

  • Manabe S, Stouffer RJ (1994) Multiple-century response of a coupled ocean-atmosphere model to an increase of atmospheric carbon dioxide. J Clim 7:5–23

    Article  Google Scholar 

  • Marten AL, Newbold SC (2013) Temporal resolution and DICE. Nat Clim Change 3(6):526–527. doi:10.1038/nclimate1893

    Article  Google Scholar 

  • Mastrandrea MD, Schneider SH (2001) Integrated assessment of abrupt climatic changes. Clim Policy 1(4):433–449

    Article  Google Scholar 

  • Matei D, Baehr J, Jungclaus JH, Haak H, Müller WA, Marotzke J (2012) Multiyear prediction of monthly mean Atlantic meridional overturning circulation at 26.5 \(^\circ \)n. Science 335(6064):76–79

    Article  Google Scholar 

  • McCarl B (2013) McCarl expanded GAMS user guide. GAMS Development Corporation, Washington

    Google Scholar 

  • McInerney D, Keller K (2008) Economically optimal risk reduction strategies in the face of uncertain climate thresholds. Clim Change 91:29–41

    Article  Google Scholar 

  • McInerney D, Lempert R, Keller K (2012) What are robust strategies in the face of uncertain climate threshold responses? Clim Change 112(3–4):547–568

    Article  Google Scholar 

  • Mehra R, Prescott EC (1985) The equity premium: a puzzle. J Monet Econ 15(2):145–161

    Article  Google Scholar 

  • Moles CG, Banga JR, Keller K (2004) Solving nonconvex climate control problems: pitfalls and algorithm performances. Appl Soft Comput 5(1):35–44. doi:10.1016/j.asoc.2004.03.011

    Article  Google Scholar 

  • Neubersch D, Held H, Otto A (2014) Operationalizing climate targets under learning: an application of cost-risk analysis. Clim Change 126(3):305–318

    Article  Google Scholar 

  • Nordhaus W (2008) A question of balance: weighing the options on global warming policies. Yale University Press, New Haven

    Google Scholar 

  • Nordhaus W (2013) The climate Casino. Yale University Press. http://www.jstor.org/stable/j.ctt5vkrpp

  • Nævdal E, Oppenheimer M (2007) The economics of the thermohaline circulation—a problem with multiple thresholds of unknown locations. Resour Energy Econ 29(4):262–283

    Article  Google Scholar 

  • O’Neill BC, Crutzen P, Grübler A, Duong MH, Keller K, Kolstad C, Koomey J, Lange A, Obersteiner M, Oppenheimer M, Pepper W, Sanderson W, Schlesinger M, Treich N, Ulph A, Webster M, Wilson C (2006) Learning and climate change. Clim Policy 6(5):585–589

    Article  Google Scholar 

  • Pindyck RS (2013) Climate change policy: what do the models tell us? In: Working paper 19244, National Bureau of Economic Research

  • Rahmstorf S, Ganopolski A (1999) Long-term global warming scenarios computed with an efficient coupled climate model. Clim Change 43(2):353–367

    Article  Google Scholar 

  • Ramsey FP (1928) A mathematical theory of saving. Econ J 38(152):543–559

    Article  Google Scholar 

  • Ring M, Schlesinger M (2012) Bayesian learning of climate sensitivity I: synthetic observations. Atmos Clim Sci 2(4):464–473

    Google Scholar 

  • Roe GH, Baker MB (2007) Why is climate sensitivity so unpredictable? Science 318(5850):629–632

    Article  Google Scholar 

  • Schleussner C-F, Levermann A, Meinshausen M (2014) Probabilistic projections of the Atlantic overturning. Clim Change 127(3–4):579–586

    Article  Google Scholar 

  • Schneider SH, Thompson L (2000) Simple climate model used in economic studies of global change. In: DeCanio SJ, Howarth RB, Sanstad AH, Schneider SH, Thompson SL (eds) New directions in the economics and integrated assessment of global climate change. Pew Center on Global Climate Change, Chapter 5, pp 59–80

  • Stern N (2013) The structure of economic modeling of the potential impacts of climate change: grafting gross underestimation of risk onto already narrow science models. J Econ Lit 51(3):838–859

    Article  Google Scholar 

  • Stocker TF, Schmittner A (1997) Influence of CO2 emission rates on the stability of the thermohaline circulation. Nat 388:862–865

  • Stommel H (1961) Thermohaline convection with two stable regimes of flow. Tellus 13(2):224–230

    Article  Google Scholar 

  • Tallarini TDJ (2000) Risk-sensitive real business cycles. J Monet Econ 45(3):507–532

    Article  Google Scholar 

  • Tol R (1998) Potential slowdown of the thermohaline circulation and climate policy. Discussion paper ds98/06, Institute for Environmental Studies Vrije Universiteit Amsterdam

  • Tol R (2009) An analysis of mitigation as a response to climate change. In: Discussion paper, Copenhagen Consensus on Climate

  • Trenberth KE, Caron JM (2001) Estimates of meridional atmosphere and ocean heat transports. J Clim 14:3433–3443

    Article  Google Scholar 

  • Urban NM, Holden PB, Edwards NR, Sriver RL, Keller K (2014) Historical and future learning about climate sensitivity. Geophys Res Lett 41(7):2543–2552

    Article  Google Scholar 

  • Urban NM, Keller K (2009) Complementary observational constraints on climate sensitivity. Geophys Res Lett 36(4):l04708. doi:10.1029/2008GL036457

    Article  Google Scholar 

  • Urban NM, Keller K (2010) Probabilistic hindcasts and projections of the coupled climate, carbon cycle and Atlantic meridional overturning circulation system: a Bayesian fusion of century-scale observations with a simple model. Tellus A 62(5):737–750

    Article  Google Scholar 

  • Vissing-Jørgensen A, Attanasio OP (2003) Stock-market participation, intertemporal substitution, and risk-aversion. Am Econ Rev 93(2):383–391

    Article  Google Scholar 

  • Waisman H, Guivarch C, Grazi F, Hourcade J (2012) The Imaclim-R model: infrastructures, technical inertia and the costs of low carbon futures under imperfect foresight. Clim Change 114(1):101–120

    Article  Google Scholar 

  • Weitzman M (2009) On modeling and interpreting the economics of catastrophic climate change. Rev Econ Stat 91:1–19

    Article  Google Scholar 

  • Yohe G, Andronova N, Schlesinger M (2004) To hedge or not against an uncertain climate future? Science 306(5695):416–417. http://www.sciencemag.org/content/306/5695/416.short

  • Zickfeld K, Bruckner T (2003) Reducing the risk of abrupt climate change: emissions corridors preserving the Atlantic thermohaline circulation. Integr Assess 4(2):106–115

    Article  Google Scholar 

  • Zickfeld K, Bruckner T (2008) Reducing the risk of Atlantic thermohaline circulation collapse: sensitivity analysis of emissions corridors. Clim Change 91:291–315

    Article  Google Scholar 

  • Zickfeld K, Levermann A, Morgan M, Kuhlbrodt T, Rahmstorf S, Keith D (2007) Expert judgements on the response of the Atlantic meridional overturning circulation to climate change. Clim Change 82:235–265

    Article  Google Scholar 

  • Zickfeld K, Slawig T, Rahmstorf S (2004) A low-order model for the response of the Atlantic thermohaline circulation to climate change. Ocean Dyn 54:8–26

    Article  Google Scholar 

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Acknowledgments

We would like to thank the anonymous referee for constructive comments that helped improve the contents of this paper. We are also indebted to the German Science Foundation for its financial support through its funding of the Cluster of Excellence ‘Integrated Climate System Analysis and Prediction’ (CliSAP) of the University of Hamburg. After the period in which the research was conducted, Nicole Glanemann changed her affiliation from the University of Hamburg to the Potsdam Institute for Climate Impact Research and WHU—Otto Beisheim School of Management in Vallendar. We would like to express gratitude to Frank Ackerman, Ramon Bueno, and Elisabeth A. Stanton for sharing the GAMS code of their EZ-DICE model. We would also like to acknowledge Kirsten Zickfeld for providing background information on the four-box THC model and for offering the MATLAB code. Furthermore, we are grateful to Chao Li for his expert advice on Atlantic thermohaline circulation. Of course, any remaining mistakes are solely the responsibility of the authors.

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Correspondence to Mariia Belaia.

Appendices

Appendix 1: Robustness Check

As this research clearly relates to the study by Ackerman et al. (2013), here we clarify whether our model could reproduce their results. We may demonstrate this for their \(E_1\) model run. We keep the default damage function of the original DICE model, i.e. we set \(a_2 = 0.0028388\) and ignore the feedback from the THC module to DICE. Note that there are different assumptions in the two models. Firstly, we apply the updated transient temperature change equation from Cai et al. (2012a), where, in contrast to Nordhaus (2008) and Ackerman et al. (2013), the radiative forcing depends only on current carbon concentration in the atmosphere. Secondly, while the EZ-DICE model by Ackerman et al. (2013) is designed for decadal time steps, our model incorporates annual time steps as the DICE-CJL model by Cai et al. (2012a).

Comparing the results of the two models, we recognise that the assumptions in our model offer a more differentiated view of the optimal policy (Fig. 15). While in Ackerman et al. (2013) only one policy path is given for three very different climate sensitivity values, \(S_3\)\(S_5\), our model produces two distinct control trajectories. The discrepancy mainly comes from the model recalibration by Cai et al. (2012a) associated with the refined time scale. This is explained and discussed in more detail by Marten and Newbold (2013).

Fig. 15
figure 15

Comparison of the optimal emission redution policies generated by the two models, the EZ-DICE model by Ackerman et al. (2013) (left) and the IAM in our paper, in which the feedback from the THC to DICE model is ignored (right)

Appendix 2: Numerical Solution

Here, we draw attention to the non-convex nature of the optimisation problem. This non-convexity occurs, for instance, when considering tipping elements that switch to another state at some point in time. As finding the computational solution to such a problem is non-trivial, we explain our numerical approach in more detail in the following.

Fig. 16
figure 16

Frequency of solutions found by a multi-start approach for different initial values

The more refined time step compared to DICE gives rise to a higher dimension of the decision variables space, which amounts to 1200 variables (consumption and abatement paths over 600 years). Furthermore, the existence of the THC stability threshold induces local optima, which creates numerical problems that are commonly tackled by global optimisation methods. Yet, the global solvers available in GAMS are rather restricted with respect to the allowable size of the model. Instead we implement a multi-start heuristic approach to the CONOPT3 solver in the GAMS environment using different initial values.Footnote 12 The algorithm in CONOPT3 is based on a generalised reduced gradient (GRG) technique, which relies on the gradient information and has a comparative advantage in handling large models such as ours.Footnote 13 The three pillars of successfully applying the solver to a non-linear problem are the initial values, scaling, and bounds. Furthermore, the solver is designed to operate with smooth functions only, which is why throughout the model design process, e.g. developing the damage cost function \(f_{THC}\), we verify this property to ensure convergence.

The approach we implement calls the NLP solver CONOPT3 from 100 random initial vectors within the bounds of the variables. The highest value from the multi-starts corresponds to the approximation of the global solution, which is used in the analyses. The histogram in Fig. 16 depicts the solutions of the multi-start approach for the default simulation (Fig. 5). Out of 100 model runs, 50 converge to a feasible solution with 18 converging to the optimum. As mentioned above, many of the solutions recovered by our algorithm are local. In this respect, a good alternative could be to refer to the differential evolution algorithm, which converges to the same solution for many initial conditions (see Keller et al. 2004; Moles et al. 2004).

To illustrate the non-convexity of the problem, we perturb the near-term optimal emissions-control rate and inspect the associated change in the objective function (first-period Epstein–Zin utility). As the reference we choose the value of the first-period Epstein–Zin utility that corresponds to the optimal emissions-control rate for the scenario in which the THC-related damage costs are neglected. Figure 17 depicts the relative change of the first-period Epstein–Zin utility value for different abatement rates in the year 2075. The point G is associated with global optimum. An increase in the abatement rate leads to a decrease in utility. The reason is that the benefits associated with delaying the THC collapse do not exceed the near-term costs. Utility is continuously decreasing with the emissions-control rate in the near-term until the abatement efforts are sufficient to prevent the THC collapse in state \(S_5\). As soon as the circulation is safeguarded, the THC-induced damage costs over the long period of time sum up to nearly zero. This is reflected in the sudden increase in the first-period Epstein–Zin utility at about 68.6 % of abatement in the year 2075. Nevertheless, the costs of preventing the THC collapse in \(S_5\) exceeds the benefits. Thus, preserving the THC describes only a local optimum, which is depicted by L.

Fig. 17
figure 17

Relative percentage change in the first-period Epstein–Zin utility for different values of abatement rates in the year 2075. The percentage change is considered relative to the first-period Epstein–Zin utility for the emissions-control rate that neglects potential THC-related damages. The points G and L indicate the location of the global and local optimum, respectively

Appendix 3: Calibration

Please refer to Table 2 for parameters crucial to the present study and to Table 3 for the THC model parameters. For the DICE-CJL model parameters, refer to Cai et al. (2012a) as well as Cai et al. (2012b) and the accompanying website.

Table 2 Parameters crucial to the present study
Table 3 The THC model parameters (Zickfeld et al. 2004)

Appendix 4: Sensitivity Analysis with Respect to \(m_{crit}\)

Here, we discuss briefly an alternative calibration for \(m_{crit}\). For the simulation illustrated in Fig. 18, we adopt the assumption that \(m_{crit}\) is zero. In Sect. 3 we conjecture that this assumption might render the threat of a THC collapse and the aversion to the risk involved as less important. Figure 18 confirms this conjecture. Risk aversion has little effect on near-term policy. In both cases of alternative attitudes to risk, the near-term policy efforts are lower than in the baseline case (by 6.58 percentage points), as the THC damage costs are incurred only when circulation stops altogether. These reduced efforts lead to a slowdown in more states of nature than in the baseline case.

Changing the value of \(m_{crit}\) by \(\pm 3\) Sv, as in Figs. 19 and 20, shows that the results on the effects of risk aversion are rather robust with respect to \(m_{crit}\).

Fig. 18
figure 18

Sensitivity of the results with respect to \(m_{crit}=0\) Sv i.e. THC-related damages are associated with the circulation breakdown. a, c Optimal emission reduction policy. b, d Possible trajectories of the overturning strength

Fig. 19
figure 19

Sensitivity of the results with respect to lower value of critical weakening, \(m_{crit}=7\) Sv. a, c Optimal emission reduction policy. b, d Possible trajectories of the overturning strength

Fig. 20
figure 20

Sensitivity of the results with respect to higher value of critical weakening, \(m_{crit}=13\) Sv. a, c Optimal emission reduction policy. b, d Possible trajectories of the overturning strength

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Belaia, M., Funke, M. & Glanemann, N. Global Warming and a Potential Tipping Point in the Atlantic Thermohaline Circulation: The Role of Risk Aversion. Environ Resource Econ 67, 93–125 (2017). https://doi.org/10.1007/s10640-015-9978-x

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  • DOI: https://doi.org/10.1007/s10640-015-9978-x

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