Abstract
This paper aims at providing a consistent framework to appraise alternative modeling choices that have driven the so-called “when flexibility” controversy since the early 1990s, dealing with the optimal timing of mitigation efforts and the social cost of carbon (SCC). The literature has emphasized the critical impact of modeling structures on the optimal climate policy. We estimate within a unified framework the comparative impact of modeling structures and investigate the structural modeling drivers of differences in climate policy recommendations. We use the integrated assessment model (IAM) RESPONSE to capture a wide array of modeling choices. Specifically, we analyse four emblematic modeling choices, namely the forms of the damage function (quadratic vs. sigmoid) and the abatement cost (with or without inertia), the treatment of uncertainty, and the decision framework, deterministic or sequential, with different dates of information arrival. We define an original methodology based on an equivalence criterion to compare modeling structures, and we estimate their comparative impact on two outputs: the optimal SCC and abatement trajectories. We exhibit three key findings: (1) IAMs with a quadratic damage function are insensitive to changes of other features of the modeling structure, (2) IAMs involving a non-convex damage function entail contrasting climate strategies, (3) Precautionary behaviors can only come up in IAMs with non-convexities in damage.
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Notes
The code of the program, with specification of all parameters, is available at http://www.centre-cired.fr/spip.php?article1395.
The climate externality does not enter into the utility function. It is only captured by a damage function.
The logarthmic utility function is a particular case of the constant relative risk aversion utility functions family. In this paper we do not perform sensitivity analysis over the form of the utility function.
In Knightian terminology, this is risk. However, the term uncertainty is commonly used in the IAM literature.
Here and in the rest of the document, \(\mathbb {E}\) stands for the expectation operator over states of nature: \(\mathbb {E}[f]={\sum }_{\omega }p(\omega )f(\omega )\).
See [31, 33] for well-known examples. This kind of uncertainty is sometimes labeled ex-ante uncertainty, because it is resolved by picking values before the optimization program starts. For the planner, inside the model, the parameters are known. It is only outside the model, for the modeler, that the parameters are uncertain. This ex-ante indeterminacy should not be confused with true uncertainty within the model, as in sequential decision-making or stochastic programming. See [8] for the difference between the two types of uncertainty in IAM.
The range of climate sensitivity chosen in our simulations may seem too narrow. However, with upper climate sensitivities, the climate take more time to adjust with a characteristic time proportional at first order to the square of the climate sensitivity [5, 37]. Changing climate sensitivity from 4 to 6 lead to tremendous changes in the long run but not so much in the short run. The equivalence criterion (see 3.3) considers only damages up to 2100. Because this time span is less than the adjustment date for the emissions of early periods for a climate sensitivity of 4, enlarging the range of climate sensitivity, for example up to 6, would not dramatically modify our results.
The choice of adjusting T D is somehow arbitrary as the three other parameters can be seen as equally good candidates. Still we believe that the temperature threshold of the damage function has a greater policy relevance than the magnitude of the damage d since the climate policy debate has always been more focused on temperature targets, in particular the 2 ∘C target, than on the size of the damage which remains highly controversial. Adjusting on κ S or η would have brought unclear interpretation as they are two technical parameters of the sigmoid damage function.
A natural candidate could have been the cumulated abatement cost. But as inertia in abatement cost is modeled as an extra-cost, it is likely that equal cumulated costs imply lower abatement over the whole period in cases with inertia. Then the equivalence criterion would directly make a difference on the level of abatement. A criterion such as equal cumulated undiscounted costs to meet a carbon budget would offset this drawback but is more difficult to handle.
Note that when information on the right state of nature arrives in 2050 (for all the modeling structures with the suffix -2050) then there are as many possible trajectories (and therefore possible points in 2100) as states of nature. Therefore we cannot report one single value in the table. Picking arbitrarily one of the values would be misleading and blur the message as it does not account anymore for the impact of uncertainty.
References
Ambrosi, P., Hourcade, J., Hallegatte, S., Lecocq, F., Dumas, P., Ha-Duong, M. (2003). Optimal control models and elicitation of attitudes towards climate damages. Environmental Modeling and Assessment, 8(3), 133–147.
Archer, D., & Brovkin, V. (2008). The millennial atmospheric lifetime of anthropogenic CO2. Climatic Change, 90(3), 283–297.
Archer, D., Eby, M., Brovkin, V., Ridgwell, A., Cao, L., Mikolajewicz, U., Caldeira, K., Matsumoto, K., Munhoven, G., Montenegro, A., other (2009). Atmospheric lifetime of fossil fuel carbon dioxide. Annual Review of Earth and Planetary Sciences, 37, 117–134.
Arrow, K., & Fisher, A. (1974). Environmental preservation, uncertainty, and irreversibility. The Quarterly Journal of Economics, 88(2), 312–319.
Baker, M.B., & Roe, G.H. (2009). The shape of things to come: why is climate change so predictable? Journal of Climate, 22(17), 4574–4589.
Cass, D. (1965). Optimum growth in an aggregative model of capital accumulation. The Review of Economic Studies, 32(3), 233–240.
Chichilnisky, G., & Heal, G. (1993). Global environmental risks. The Journal of Economic Perspectives, 7(4), 65–86.
Crost, B., & Traeger, C.P. (2013). Optimal climate policy: uncertainty versus monte carlo. Economics Letters, 120(3), 552–558.
Dasgupta, P. (2007). Commentary: the Stern review’s economics of climate change. National Institute Economic Review, 199(1), 4–7.
Dumas, P., Espagne, E., Perrissin-Fabert, B., Pottier, A. (2012). Comprehensive description of the integrated assessment model RESPONSE. Working Paper CIRED.
Espagne, E., Perrissin-Fabert, B., Pottier, A., Nadaud, F., Dumas, P. (2012). Disentangling the Stern / Nordhaus controversy: beyond the discounting clash. FEEM Nota Di Lavoro.
Friedlingstein, P., Cox, P., Betts, R., Bopp, L., Von Bloh, W., Brovkin, V., Cadule, P., Doney, S., Eby, M., Fung, I. (2006). Climate-carbon cycle feedback analysis: results from the c4mip model intercomparison. Journal of Climate, 19(14), 3337–3353.
Gitz, V., & Ciais, P. (2003). Amplifying effects of land-use change on future atmospheric CO2 levels. Global Biogeochemical Cycles, 17(1), 1024–1029.
Golosov, M., Hassler, J., Krusell, P., Tsyvinski, A. (2014). Optimal taxes on fossil fuel in general equilibrium. Econometrica, 82(1), 41–88.
Goulder, L., & Mathai, K. (2000). Optimal CO2 abatement in the presence of induced technological change. Journal of Environmental Economics and Management, 39(1), 1–38.
Ha-Duong, M. (1998). Comment tenir compte de l’irr’eversibilit’e dans l”evaluation int’gr’ee du changement climatique? PhD thesis, EHESS.
Ha-Duong, M. (1998). Quasi-option value and climate policy choices. Energy Economics, 20(5–6), 599–620.
Ha-Duong, M., Grubb, M., Hourcade, J. (1997). Influence of socioeconomic inertia and uncertainty on optimal CO2-emission abatement. Nature, 390(6657), 270–273.
Henry, C. (1974). Investment decisions under uncertainty: the Irreversibility Effect. The American Economic Review, 64(6), 1006–1012.
Hof, A., den Elzen, M., van Vuuren, D. (2008). Analysing the costs and benefits of climate policy: value judgements and scientific uncertainties. Global Environmental Change, 18(3), 412–424.
Hope, C. (2006). The marginal impact of CO2 from PAGE2002: an integrated assessment model incorporating the IPCC’s five reasons for concern. Integrated Assessment, 6(1), 19–56.
IPCC. (2007). Climate change 2007: Mitigation. Contribution of working group III to the fourth assessment report of the intergovernmental panel on climate change. Cambridge: Cambridge University Press.
Keller, K., Bolker, B., Bradford, D. (2004). Uncertain climate thresholds and optimal economic growth. Journal of Environmental Economics and Management, 48(1), 723–741.
Kelly, D., & Kolstad, C. (1999). Bayesian learning, growth, and pollution. Journal of Economic Dynamics and Control, 23(4), 491–518.
Kolstad, C. (1996). Fundamental irreversibilities in stock externalities. Journal of Public Economics, 60(2), 221–233.
Koopmans, T. (1963). Appendix to On the concept of optimal economic growth. Cowles Foundation Discussion Papers.
Kopp, R. E., Golub, A., Keohane, N. O., Onda, C. (2012). The influence of the specification of climate change damages on the social cost of carbon. Economics: The Open-Access, Open-Assessment E-Journal, 6(2012–13), 1–40.
Manne, A., Mendelsohn, R., Richels, R. (1995). Merge: A model for evaluating regional and global effects of GHG reduction policies. Energy Policy, 23(1), 17–34.
Manne, A., & Richels, R. (1992). Buying greenhouse insurance: the economic costs of carbon dioxide emission limits. The MIT Press.
Moyer, E., Woolley, M.D., Glotter, M., Weisbach, D.A. (2013). Climate impacts on economic growth as drivers of uncertainty in the social cost of carbon. Center for Robust Decision Making on Climate and Energy Policy Working Paper, 13, 25.
Nordhaus, W. (1994). Managing the global commons: the economics of climate change. Cambridge: MIT Press.
Nordhaus, W. (2007). A review of the Stern Review on the Economics of Climate Change. Journal of Economic Literature, 45(3), 686–702.
Nordhaus, W. (2008). A question of balance. New Haven: Yale University Press.
Nordhaus, W., & Boyer, J. (2003). Warming the world: economic models of global warming: MIT Press.
Pindyck, R. (2000). Irreversibilities and the timing of environmental policy. Resource and energy economics, 22(3), 233–259.
Ramsey, F. (1928). A mathematical theory of saving. The Economic Journal, 38(152), 543–559.
Roe, G.H., & Bauman, Y. (2013). Climate sensitivity: should the climate tail wag the policy dog? Climatic change, 117(4), 647–662.
Schneider, S., & Thompson, S. (1981). Atmospheric CO2 and climate: importance of the transient response. Journal of Geophysical Research, 86(C4), 3135–3147.
Stern, N. (2006). The economics of climate change. Cambridge University Press.
Sterner, T., & Persson, U.M. (2008). An even sterner review: introducing relative prices into the discounting debate. Review of Environmental Economics and Policy, 2(1), 61–76.
Tol, R.S.J. (1997). On the optimal control of carbon dioxide emissions: an application of FUND. Environmental Modeling & Assessment, 2(3), 151–163.
Tol, R.S.J. (2009). Climate feedbacks on the terrestrial biosphere and the economics of climate policy: an application of fund. Technical Report WP288, Economic and Social Research Institute (ESRI).
Ulph, A., & Ulph, D. (1997). Global warming, irreversibility and learning. The Economic Journal, 107(442), 636–650.
Vogt-Schilb, A., Meunier, G., Hallegatte, S. (2012). How inertia and limited potentials affect the timing of sectoral abatements in optimal climate policy. World Bank Policy Research, 6154.
Weitzman, M. (2007). A review of the Stern Review on the economics of climate change. Journal of Economic Literature, 45 (3), 703–724.
Weitzman, M.L. (2012). GHG targets as insurance against catastrophic climate damages. Journal of Public Economic Theory, 14(2), 221–244.
Wigley, T., Richels, R., Edmonds, J. (1996). Economic and environmental choices in the stabilization of atmospheric CO2 concentrations. Nature, 379(6562), 240–243.
Yohe, G., & Tol, R. (2007). The Stern Review: Implications for climate change. Environment: Science and Policy for Sustainable Development, 49(2), 36–43.
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Appendices
Appendix A: First-Order Conditions Resolution
In this part, our calculations follow the two-step resolution method already described in part 2.3. We distinguish before and after uncertainty is resolved.
1.1 A.1 After uncertainty is resolved
After uncertainty is resolved, we know the state of nature ω. The Lagrangian writes:
The Lagrange multiplier attached to the capital constraint (4) is \(\mu _{t}^{\omega }\); the Lagrange multipliers attached to the carbon cycle dynamics constraints (11) are \(\lambda _{A,t}^{\omega }\), \(\lambda _{B,t}^{\omega }\), and \(\lambda _{O,t}^{\omega }\). The Lagrange multipliers attached to the temperature constraints (13) are \(\nu _{A,t}^{\omega }\) and \(\nu _{O,t}^{\omega }\). The Lagrange multipliers attached to inequality constraints (7) are \(\overline {\tau }^{\omega }_{t}\) and \(\underline {\tau }^{\omega }_{t}\).
At the beginning of the program, stock variables are inherited from the past, i.e., from the maximization program under uncertainty. Some do not depend on the state of nature:
By convention, \(a^{\omega }_{t_{i}}=\overline {a}_{t_{i}}\).
We calculate the first-order conditions with respect to the two flow variables: \(C_{t}^{\omega }\) and \(a_{t}^{\omega }\), and to the six stock variables: \(K_{t}^{\omega }\), \(a_{t}^{\omega }\), \(B_{t}^{\omega }\), \(O_{t}^{\omega }\), \(T_{A,t}^{\omega }\), and \(T_{O,t}^{\omega }\). Recall also that stock variables at t=t i +1 are initial conditions, so we cannot derive first-order conditions for them at this stage. We get:
-
For consumption, ∀t≥t i +1:
$$\begin{array}{@{}rcl@{}} &\frac{\partial \mathbf{L}^{\omega}}{\partial C_{t}^{\omega}} = 0 \quad \Leftrightarrow \\ &\mu_{t}^{\omega} = u'\left(\frac{C_{t}^{\omega}}{N_{t}}\right) \frac{1}{(1+\rho)^{t}} \end{array} $$(18)Then, \(\mu _{t}^{\omega }\) is the discounted marginal utility.
-
For the abatement capacity, ∀t≥t i +1:
$$\begin{array}{@{}rcl@{}} &&\frac{\partial\mathbf{L}^{\omega}}{\partial a_{t}^{\omega}} = 0 \quad \Leftrightarrow \\ && \lambda_{A,t}^{\omega}\sigma_{t}= \mu_{t}^{\omega}\partial_{1} G (a_{t}^{\omega},a_{t-1}^{\omega}) + \mu_{t+1}^{\omega}\partial_{2} G (a_{t+1}^{\omega},a_{t}^{\omega})\frac{Y^{\omega}_{t+1}}{Y^{\omega}_{t}}\\ &&{\kern3pc} +\frac{\overline{\tau}^{\omega}_{t}-\underline{\tau}^{\omega}_{t}}{Y^{\omega}_{t}} \end{array} $$(19)For t=t i +1, recall the conventional notation that \(a_{t_{i}}^{\omega }=\overline {a}_{t_{i}}\). Recall that \(\overline {\tau }^{\omega }_{t}>0\) only when \(a^{\omega }_{t}=1\), and \(\underline {\tau }^{\omega }_{t}>0\) only when \(a^{\omega }_{t}=0\).
-
For capital, ∀t≥t i +2:
$$\begin{array}{@{}rcl@{}} &&\frac{\partial \mathbf{L}^{\omega}}{\partial K_{t}^{\omega}} =0 \quad \Leftrightarrow \\ && \partial_{K}Y_{t}^{\omega}\left(1-\frac{\lambda_{A,t}^{\omega} (1-a_{t}^{\omega})\sigma_{t}}{\mu_{t}^{\omega}}\-G(a_{t}^{\omega},a_{t-1}^{\omega})-D^{\omega}(T_{A,t}^{\omega})\right)\\ &&= (1+\rho)\frac{u'\left(\frac{C_{t-1}^{\omega}}{N_{t-1}}\right)}{u'\left(\frac{C_{t}^{\omega}}{N_{t}}\right)}- (1-\delta) \end{array} $$(20) -
For the carbon stocks, ∀t≥t i +2:
$$\begin{array}{@{}rcl@{}} && \frac{\partial\mathbf{L}^{\omega}}{\partial A_{t}^{\omega}} = 0 \quad \Leftrightarrow \\ && \lambda_{A,t-1}^{\omega} = \lambda_{A,t}^{\omega}c_{AA} +\lambda_{B,{t}}^{\omega}c_{BA} + \nu_{A,t}^{\omega}\sigma_{1}F'(A_{t}^{\omega}) \end{array} $$(21)$$\begin{array}{@{}rcl@{}} &&\frac{\partial\mathbf{L}^{\omega}}{\partial B_{t}^{\omega}} = 0 \quad \Leftrightarrow \\ &&\lambda_{B,t-1}^{\omega} = \lambda_{A,t}^{\omega} c_{AB}+\lambda_{B,{t}}^{\omega}c_{BB} + \lambda_{O,{t}}^{\omega} c_{OB} \end{array} $$(22)$$\begin{array}{@{}rcl@{}} &&\frac{\partial\mathbf{L}^{\omega}}{\partial O_{t}^{\omega}} = 0 \quad \Leftrightarrow \\ &&\lambda_{O,t-1}^{\omega} = \lambda_{B,{t}}^{\omega}c_{BO} + \lambda_{O,{t}}^{\omega} c_{OO} \end{array} $$(23) -
For the temperatures, ∀t≥t i +2:
$$\begin{array}{@{}rcl@{}} && \frac{\partial\mathbf{L}^{\omega}}{\partial T_{A,t}^{\omega}} = 0 \quad \Leftrightarrow \\ && \nu_{A,t-1}^{\omega} = \nu_{A,t}^{\omega} \left(1-\sigma_{1}\left(\frac{F_{2x}}{\vartheta_{2x}^{\omega}}+\sigma_{2}\right)\right)\\ &&{\kern3pc} + \nu_{O,t}^{\omega} \sigma_{3} + \mu_{t}^{\omega} \partial_{T} D^{\omega}(T_{A,t}^{\omega})Y_{t}^{\omega} \end{array} $$(24)$$\begin{array}{@{}rcl@{}} && \frac{\partial\mathbf{L}^{\omega}}{\partial T_{O,t}^{\omega}} = 0 \quad \Leftrightarrow \\ && \nu_{O,t-1}^{\omega} =\nu_{A,t}^{\omega} \sigma_{1}\sigma_{2} + \nu_{O,t}^{\omega} (1-\sigma_{3}) \end{array} $$(25)
1.2 A.2 Before Uncertainty is Resolved
The Lagrangian of the maximization program then equals the expectation over the possible states of nature of the sum of the objective function and a cluster of dynamic equations.
The Lagrangian writes:
We calculate the first-order conditions with respect to all endogenous variables: flow variables \(C_{t}^{\omega }\) and \(\overline {a}_{t}\), and stock variables \(\overline {K}_{t}\), \(\overline {a}_{t}\), \(\overline {B}_{t}\), \(\overline {O}_{t}\), \(T_{A,t}^{\omega }\), and \(T_{O,t}^{\omega }\). The derivation will be specific for stock variables at t i +1, and for the flux variable \(\overline {a}_{t_{i}}\) due to the inertia in abatement cost, for we have to take into account their impact on V(ω). We get:
-
For consumption, ∀t≤t i :
$$\begin{array}{@{}rcl@{}} && \frac{\partial \mathbf{L}^{\omega}}{\partial C_{t}^{\omega}} = 0 \quad \Leftrightarrow \\ && \mu_{t}^{\omega} = u'\left(\frac{C_{t}^{\omega}}{N_{t}}\right) \frac{1}{(1+\rho)^{t}} \end{array} $$(29) -
For the abatement capacity, ∀t<t i :
$$\begin{array}{@{}rcl@{}} &&\frac{\partial\mathbf{L}_{u}}{\partial \overline{a}_{t}} = 0 \quad \Leftrightarrow \\ \lambda_{A,t}\sigma_{t} &= & \mathbb{E}\left[\mu^{\omega}_{t}\right]\partial_{1} G(\overline{a}_{t},\overline{a}_{t-1}) \\ &&+ \mathbb{E}\left[\mu^{\omega}_{t+1}\right]\partial_{2} G(\overline{a}_{t+1},\overline{a}_{t})\frac{\overline{Y}_{t+1}}{\overline{Y}_{t}}+\frac{\overline{\tau}_{t}-\underline{\tau}_{t}}{\overline{Y}_{t}} \end{array} $$(30)For t=t i , actions, which are decided at the beginning of the period, cannot take into account the information that arrives in this period:
$$\begin{array}{@{}rcl@{}} &&\frac{\partial\mathbf{L}_{u}}{\partial \overline{a}_{t_{i}}} = 0 \quad \Leftrightarrow \\ &&\lambda_{A,t_{i}}\sigma_{t_{i}} = \mathbb{E}\left[\mu^{\omega}_{t_{i}}\right] \partial_{1} G(\overline{a}_{t_{i}},\overline{a}_{t_{i}-1})\\ &&{\kern2.6pc} +\mathbb{E}\left[\mu^{\omega}_{t_{i}+1}\partial_{2} G(a^{\omega}_{t_{i}+1},\overline{a}_{t_{i}})\right]\frac{\overline{Y}_{t_{i}+1}}{\overline{Y}_{t_{i}}}+\frac{\overline{\tau}_{t_{i}}-\underline{\tau}_{t_{i}}}{\overline{Y}_{t_{i}}} \end{array} $$(31)because \(\frac {\partial V(\omega )}{\partial \overline {a}_{t_{i}}}=\frac {\partial L^{\omega }}{\partial \overline {a}_{t_{i}}}=\mu ^{\omega }_{t_{i}+1}\partial _{2} G(a^{\omega }_{t_{i}+1},\overline {a}_{t_{i}})\overline {Y}_{t_{i}+1}\).
-
For capital, ∀t≤t i :
$$\begin{array}{@{}rcl@{}} && \frac{\partial\mathbf{L}_{u}}{\partial \overline{K}_{t}} = 0 \quad \Leftrightarrow \\ && \partial_{K} Y_{t} \left(1 - \frac{\lambda_{A,t}(1-\overline{a}_{t})\sigma_{t}}{\mathbb{E}[\mu^{\omega}_{t}]} - G(\overline{a}_{t}, \overline{a}_{t-1})- \frac{\mathbb{E}[\mu^{\omega}_{t} D^{\omega}(T_{A,t})]}{\mathbb{E}\left[\mu^{\omega}_{t}\right]} \right)\\ && = \frac{\mathbb{E}\left[\mu^{\omega}_{t-1}\right]}{\mathbb{E}\left[\mu^{\omega}_{t}\right]} -(1-\delta) \end{array} $$(32)For t=t i +1,
$$\begin{array}{@{}rcl@{}} && \frac{\partial\mathbf{L}_{u}}{\partial \overline{K}_{t_{i}+1}} = 0 \quad \Leftrightarrow \\ &&\partial_{K} Y_{t_{i}+1} \left(1 - \frac{\mathbb{E}[\lambda^{\omega}_{A,t_{i}+1}(1-a^{\omega}_{t_{i}+1})\sigma_{t_{i}+1}]}{\mathbb{E}\left[\mu^{\omega}_{t_{i}+1}\right]}\right. \\ &&{\kern4pc} - \left.\frac{\mathbb{E}[\mu^{\omega}_{t_{i}+1} G(a^{\omega}_{t_{i}+1}, \overline{a}_{t_{i}})]}{\mathbb{E}\left[\mu^{\omega}_{t_{i}+1}\right]} - \frac{\mathbb{E}[\mu^{\omega}_{t_{i}+1} D^{\omega}(T_{A,t_{i}+1})]}{\mathbb{E}\left[\mu^{\omega}_{t_{i}+1}\right]} \right)\\ &&= \frac{\mathbb{E}\left[\mu^{\omega}_{t_{i}}\right]}{\mathbb{E}\left[\mu^{\omega}_{t_{i}+1}\right]} -(1-\delta) \end{array} $$(33)because \(\frac {\partial V(\omega )}{\partial \overline {K}_{t_{i}+1}}=\frac {\partial L^{\omega }}{\partial \overline {K}_{t_{i}+1}}= \mu ^{\omega }_{t_{i}+1}(1-\delta + \partial _{K} Y_{t_{i}+1}(1 - G(a^{\omega }_{t_{i}+1}, \overline {a}_{t_{i}})- D^{\omega }(T_{A,t_{i}+1}) )) - \lambda ^{\omega }_{A,t_{i}+1}(1-a^{\omega }_{t_{i}+1}) \sigma _{t_{i}+1} \partial _{K} Y_{t_{i}+1}\).
-
For the atmospheric carbon multiplier, ∀t≤t i :
$$\begin{array}{@{}rcl@{}} &&\frac{\partial\mathbf{L}_{u}}{\partial \overline{A}_{t}} = 0 \quad \Leftrightarrow \\ &&\lambda_{A,t-1} = \lambda_{A,t}c_{AA}+ \lambda_{B,t}c_{BA}\\&&+\mathbb{E}\left[\nu_{A,t}^{\omega}\sigma_{1}F'(\overline{A}_{t})\right] \end{array} $$(34)$$\begin{array}{@{}rcl@{}} &&\frac{\partial\mathbf{L}_{u}}{\partial \overline{B}_{t}} = 0 \quad \Leftrightarrow \\ && \lambda_{B,t-1} = \lambda_{A,t} c_{AB}+\lambda_{B,{t}}c_{BB} + \lambda_{O,{t}} c_{OB} \end{array} $$(35)$$\begin{array}{@{}rcl@{}} &&\frac{\partial\mathbf{L}_{u}}{\partial \overline{O}_{t}} = 0 \quad \Leftrightarrow \\ &&\lambda_{O,t-1} = \lambda_{B,{t}}c_{BO} + \lambda_{O,{t}} c_{OO} \end{array} $$(36)For t=t i +1,
$$\begin{array}{@{}rcl@{}} &&\frac{\partial\mathbf{L}_{u}}{\partial \overline{A}_{t_{i}+1}} = 0 \quad \Leftrightarrow\\ && \lambda_{A,t_{i}} = \mathbb{E}\left[ \lambda_{A,t_{i}+1}^{\omega}c_{AA}+ \lambda_{B,t_{i}+1}^{\omega}c_{BA}\right.\\&& \left.\qquad\quad+\nu_{A,t_{i}+1}^{\omega}\sigma_{1}F'(\overline{A}_{t_{i}+1})\right] \end{array} $$(37)$$\begin{array}{@{}rcl@{}} &&\frac{\partial\mathbf{L}_{u}}{\partial \overline{B}_{t_{i}+1}} = 0 \quad \Leftrightarrow \\ && \lambda_{B,t_{i}} = \mathbb{E}\left[\lambda^{\omega}_{A,t_{i}+1} c_{AB}+\lambda^{\omega}_{B,{t_{i}+1}}c_{BB} + \lambda^{\omega}_{O,{t_{i}+1}} c_{OB}\right] \end{array} $$(38)$$\begin{array}{@{}rcl@{}} &&\frac{\partial\mathbf{L}_{u}}{\partial \overline{O}_{t_{i}+1}} = 0 \quad \Leftrightarrow \\ && \lambda_{O,t_{i}} = \mathbb{E}\left[\lambda^{\omega}_{B,{t_{i}+1}}c_{BO} + \lambda^{\omega}_{O,{t_{i}+1}} c_{OO}\right] \end{array} $$(39) -
For the temperatures, ∀t≤t i +1:
$$\begin{array}{@{}rcl@{}} &\frac{\partial\mathbf{L}_{u}}{\partial T_{A,t}^{\omega}} = 0 \quad \Leftrightarrow \\ &\nu_{A,t-1}^{\omega} =& \nu_{A,t}^{\omega} \left(1-\sigma_{1}\left(\frac{F_{2x}}{\vartheta_{2x}^{\omega}}+\sigma_{2}\right)\right)\\ && +\nu_{O,t}^{\omega} \sigma_{3} + \mu_{t}^{\omega} \partial_{T} D^{\omega}(T_{A,t}^{\omega})Y_{t}^{\omega} \end{array} $$(40)$$\begin{array}{@{}rcl@{}} &&\frac{\partial\mathbf{L}_{u}}{\partial T_{O,t}^{\omega}} = 0 \quad \Leftrightarrow \\ &&\nu_{O,t-1}^{\omega} =\nu_{A,t}^{\omega} \sigma_{1}\sigma_{2} + \nu_{O,t}^{\omega} (1-\sigma_{3}) \end{array} $$(41)
Appendix B: The Social Cost of Carbon
1.1 B.1 Theoretical Definition
The social cost of carbon (SCC) is “the additional damage caused by an additional ton of carbon emissions. In a dynamic framework, it is the discounted value of the change in the utility of consumption denominated in terms of current consumption” [33].
1.2 B.2 Definition in RESPONSE
At time t, if there is an additional ton of carbon in the atmosphere, this will increase A t+1 by a unit and thus decrease the welfare from t+1. This variation of welfare is captured by ∂ W t+1/∂ A t+1=−λ A,t+1 c A A −λ B,t+1 c B A −ν A,t+1 σ 1 F ′(A t+1). Once on an optimal path, this is equal, thanks to (21) or (34), to −λ A,t . So, on an optimal path, the social cost of carbon is also related to the abatement cost thanks to (19) or (30). The SCC has to be counted in current utility units.
More precisely, the equations for SCC at the different stages of the model are given below.
After uncertainty is resolved (t≥t i +1), for each state of nature ω, the SCC is:
For t=t i +1, this formula is rewritten as:
Before uncertainty is resolved, ∀t≤t i the SCC is:
For t≤t i −1, the formula simplifies to:
Comparing the formula in the uncertain case with the certain case, we can give an interpretation of the uncertain social cost in terms of the social cost if uncertainty had been resolved. The uncertain social cost corresponds to the mean of social cost in the different states of nature, averaged by utility in these states of nature (prices in different states of nature are not comparable, only utility units can be added, this is done by using the multiplier \(\mu ^{\omega }_{t}\)). So if we defined \(SCC^{\omega }_{t}\) as previously (see the formulas after uncertainty is resolved), this interpretation of the social cost is tantamount to the formula: \(SCC_{t}=\frac {\mathbb {E}[\mu ^{\omega }_{t}SCC^{\omega }_{t}]}{\mathbb {E}[\mu ^{\omega }_{t}]}\) before uncertainty is resolved.
1.3 B.3 Computation
To get the value of \(SCC^{\omega }_{t} =\frac {\lambda _{A,t}^{\omega }}{\mu _{t}^{\omega }}\), we use the shadow prices associated to the concentration dynamics for \(\lambda _{A,t}^{\omega }\) and to the capital dynamics for \(\mu _{t}^{\omega }\) computed by GAMS.
Appendix C: Results: Distributions of Abatment and SCC According to Modeling Structures for Different Dates
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Pottier, A., Espagne, E., Perrissin Fabert, B. et al. The Comparative Impact of Integrated Assessment Models’ Structures on Optimal Mitigation Policies. Environ Model Assess 20, 453–473 (2015). https://doi.org/10.1007/s10666-015-9443-9
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DOI: https://doi.org/10.1007/s10666-015-9443-9