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Unilateral Emission Cuts and Carbon Leakages in a Dynamic North–South Trade Model

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Abstract

The effects of a unilateral cut in emissions are analyzed in a dynamic two-country model. Two (intermediate) goods are produced, one of which uses the fossil fuel. These inputs are traded and combine to produce a final good. The effect of a cut in fossil fuel use by a bloc (e.g. Annexure 1 countries in the Kyoto Protocol) depends on whether the fuel is priced at marginal cost or above. In the latter case a “green paradox” may appear. The paper’s contribution lies in analyzing the dynamics and trade implications of the unilateral action.

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Notes

  1. The stock of carbon in the atmosphere will raise the mean temperature and increase weather variability. The world will see a rise in the sea-level (due to a melting of polar ice-caps) and a melting of glaciers where some of the big rivers of the world originate. The rise in the sea level will cause migration from the areas that would get inundated, while changes in the weather will require a major change of cropping pattern etc. Parts of the world would see land becoming more arid. Coping with this would require massive redeployment of resources.

  2. “In the last 100 years, 63 % of the cumulative emissions of greenhouse gases have come from the developed economies. Of that, the US has accounted for 25 % and Western Europe for 21 %. China and India, home to 40 % of the world’s population, have contributed, respectively, 7 and 2 % of the last 100 years of cumulative emissions.” Dutta and Radner (2012) p. 2.

  3. See Eichner and Pethig (2011), Dutta and Radner (2012) and van der Ploeg and Withagen (2012b) for discussions on these issues.

  4. For instance, Eichner and Pethig (2011) and van der Meijden et al. (2014) have an intermediate input (oil) and only a single final good.

  5. The concept is due to Hans Werner Sinn (2008). It has spawned a large literature, most of it in a partial equilibrium setting. See e.g. (in addition to the references in the text) Gerlagh (2011), Hoel (2010), Chakravorty et al. (2011).

  6. The green paradox is based on the reaction of producers to the decline in the price of fossil fuels when subsidies to clean fuel or taxes on the fossil fuel are set at arbitrary (as opposed to optimal) levels. Hoel (2010) discusses the nature of those taxes; see also van der Meijden et al. (2014). One can possibly appeal to (even in the absence of uncertainty) to Weitzman’s quantitative restriction argument because the effects of the green paradox occurring would be catastrophic.

  7. In Smulders et al. (2012) there is a sunk cost of using the clean fuel.

  8. A three-period model is also discussed as an extension.

  9. In the two papers closest to ours, Maria and Werf (2008) look at carbon leakage but not the dynamic nature of fossil fuel pricing; while Eichner and Pethig (2011) have only one final good and no capital accumulation. Since they also do not allow for borrowing or lending, their intertemporal substitution parameter is redundant. In equilibrium, countries consume the production of their final good output. For an analysis of borrowing and lending and the effect of carbon leakage on the world interest rate, see van der Meijden et al. (2014).

  10. Their conclusion about “aid” from the rich to the poor countries to make the latter participate in cutting back emissions is similar to the policy implications obtained in this paper. I focus on different issues, though.

  11. We could treat the oil producers as part of the two economies. Then the gross output of the dirty good is also the value-added in that economy.

  12. The two economies are different in terms of their endowments and policies. Making them even more dissimilar by assuming different rates of time preference can easily be incorporated.

  13. Elisa and Wing (2013) discuss the importance of malleability of capital for climate change policies.

  14. The specific factors are in given supply.

  15. Our analysis imposes quantitative restrictions on fossil fuel use as is common in the literature e.g. Eichner and Pethig (2011). It is possible to include an abatement technology but it does not seem worth the additional complications.

  16. If R and S are imported then \(\Omega \) is the GDP, otherwise the returns to the domestically-owned factors have to be added back.

  17. The output supply is the derivative of the GDP function \(\Omega \) with respect to its price e.g. \(\hbox {Y}= \Omega _{p}.\,\Omega _{pp}\), the own price response, is then positive etc.

  18. Nothing hinges on this. Assuming zero depreciation makes no difference to the analysis. A rate of depreciation that lies between zero and one would necessitate carrying the parameter of depreciation in calculating the expected marginal product of capital.

  19. Note this is different from the way some others use this term e.g. Eichner and Pethig (2011). They use this term to imply 100 % or more leakage within the same period. It is also different from the definition(s) given by Gerlagh (2011).

  20. Ritter and Schopf (2014) and Eichner and Pethig (2011) look at similar policies.

  21. We can look at a permanent unilateral policy by combining the two cases discussed in the text.

  22. Eichner and Pethig (2011) do not discuss marginal cost pricing of the fossil fuel—in their analysis the marginal cost is zero.

  23. As mentioned earlier, I will discuss the modifications introduced by a stock-dependent marginal cost for the fossil fuel later.

  24. In a large class of competitive models, there is equivalence between taxes and quantitative restrictions. This does not carry over to other scenarios e.g. When there is strategic interaction between agents, or even non competitive behavior. I am grateful to a referee for emphasizing this point.

  25. We would require very high supply elasticities for investment for this not to hold. After all, capital accumulation and the consequent increase in income, creates demand for both the intermediate inputs, not just for Y.

  26. In Eq. (18), the term \(\Omega _R^2\) is the effect of a change in R on the GDP of the North, etc.

  27. This is because fossil fuel use changes in period 2 but the unilateral reduction happened in period 1.

  28. van der Meijden et al. (2014), within a framework of an integrated world capital market, discuss the consequences of a change in the interest rate used in the Hotelling Rule from changes in saving and investment. See also the discussion in Strand (2010).

  29. In Indian English it is called “preponing”, in symmetry with postponing”.

References

  • Acemoglu D, Aghion P, Bursztyn L, Hemous D (2012) The environment and directed technical change. Am Econ Rev 102:131–166

    Article  Google Scholar 

  • Babiker MH (2005) Climate change policy, market structure, and carbon leakage. J Int Econ 65:421–445

    Article  Google Scholar 

  • Barrett S (2003) Environment and statecraft: the strategy of environmental treaty-making. Oxford University Press, Oxford

    Book  Google Scholar 

  • Burniaux J-M, Martins JO (2000) Carbon emission leakage: a general equilibrium view. In: OECD Economics Department Working Paper 242

  • Chakravorty U, Magne B, Leach A, Moreaux M (2011) Would Hotelling kill the electric car? J Environ Econ Manag 61:281–296

    Article  Google Scholar 

  • Chatterji S, Ghoshal S, Walsh S, Whalley J (2011) Unilateral measures emissions mitigation. In: NBER Working Paper 15441

  • Copeland B, Taylor MS (2015) Free trade and global warming: a trade theory view of the Kyoto Protocol. J Environ Econ Manag 49:205–234

    Article  Google Scholar 

  • di Maria C, van der Werf E (2008) Carbon leakage revisited: unilateral climate policy with directed technical change. Environ Resour Econ 39:55–74

    Article  Google Scholar 

  • Dutta P, Radner R (2012) Capital growth in a global warming model: will China and India sign a climate treaty? Econ Theor 49:411–443

    Article  Google Scholar 

  • Eichner T, Pethig R (2011) Carbon leakage, the green paradox and perfect futures markets. Int Econ Rev 52:767–805

    Article  Google Scholar 

  • Eichner T, Pethig R (2012) Flattening the carbon extraction path in unilateral cost effective action. J Environ Econ Manag 66:185–201

    Article  Google Scholar 

  • Eichner T, Pethig R (2014) Unilateral climate policy with production-based and consumption-based carbon emmision taxes. Environ Resour Econ. doi:10.1007/s10640-014-9786-8

  • Elisa L, Wing IS (2013) Carbon malleability, emission leakage and the cost of partial carbon policies: general equilibrium analysis of the European Union Emission Trading System. Environ Resour Econ 55:257–289

    Article  Google Scholar 

  • Finus M (2001) Game theory and international environmental cooperation. Edward Elgar, Cheltenham

    Book  Google Scholar 

  • Gerlagh R (2011) Too much oil. CESifo Econ Stud 57:79–102

    Article  Google Scholar 

  • Hoel M (2010) Is there a green paradox. In: CESifo Working Paper No. 3168

  • IPCC (2007) Climate change 2007, vol I, II, III. Cambridge University Press, Cambridge

    Google Scholar 

  • Ritter H, Schopf M (2014) Unilateral climate policies: harmful or even disastrous? Environ Resour Econ 58:155–178

    Article  Google Scholar 

  • Sinn H-W (2008) Public policies against global warming: a supply side approach. Int Tax Public Financ 15:360–394

    Article  Google Scholar 

  • Smulders S, Tsur Y, Zemel A (2012) Announcing climate policy: can a green paradox arise without scarcity? J Environ Econ Manag 64:364–376

    Article  Google Scholar 

  • Strand J (2010) Optimal fossil-fuel taxation with backstop technologies and tenure risk. Energy Econ 32:418–422

    Article  Google Scholar 

  • van der Meijden G, van der Ploeg F, Withagen C (2014) International capital markets, oil producers and the green paradox. In: OxCarre Working Paper No. 130

  • Van der Ploeg F, Withagen C (2011) Growth and the optimal carbon tax: when to switch from exhaustible resources to renewable? In: OxCarre Discussion Paper No. 55

  • Van der Ploeg F, Withagen C (2012a) Is there really a “green paradox”? J Environ Econ Manag 64:342–363

    Article  Google Scholar 

  • Van der Ploeg F, Withagen C (2012b) Too much coal, too little oil. J Public Econ 96:62–77

    Article  Google Scholar 

  • Whalley J (2011) What role for trade in a post-2012 global climate policy regime?. In: NBER Working Paper No. 17498

Download references

Acknowledgments

Some of the material was presented in invited lectures at conferences in Exeter and the Singapore Economic Review Conference. The paper was also presented at the World Congress of Environment and Resource Economics in Istanbul, and at seminars in Oxford, Toulouse and the OECD. I am grateful to Jean-Pierre Amigues, Thomas Eichner, Michael Finus, Elisa Lanzi, Peter Lloyd, Michel Moreau and Francois Salanie for helpful comments.

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Correspondence to Partha Sen.

Appendices

Appendix 1

Differentiating Eqs. (15a)–(15d), we have:

$$\begin{aligned}&\left[ \begin{array}{cccc} {{U}^{\prime \prime }(C_1 )}&{} {-\beta (1+r_1 ){U}^{\prime \prime }(C_2 )}&{} {-\beta {U}^{\prime }(C_2 )}&{} 0 \\ 1&{} 0&{} 0&{} 1 \\ 0&{} 1&{} 0&{} {-\Omega _K^2 /z^{2}} \\ 0&{} 0&{} 1&{} {-\Omega _{KK}^2 /z^{2}} \\ \end{array} \right] \left[ \begin{array}{c} {dC_1 } \\ {dC_2 } \\ {dr_1 } \\ {dI_1 } \\ \end{array} \right] \nonumber \\&\quad =\left[ \begin{array}{c} 0 \\ {\{\Omega _p^1 -(\Omega _1 z_p^1 /z^{1})\}/z^{1}} \\ 0 \\ 0 \\ \end{array} \right] dp_1 + \left[ \begin{array}{c} 0 \\ {\Omega _q^1 /z^{1}} \\ 0 \\ 0 \\ \end{array} \right] dq_1\nonumber \\&\quad +\left[ \begin{array}{c} 0 \\ 0 \\ {\{\Omega _p^2 -(\Omega _2 z_p^2 /z^{2})\}/z^{2}} \\ {\{\Omega _{pK}^2 -(\Omega _K^2 z_p^2 /z^{2})\}/z^{2}} \\ \end{array} \right] dp_2 +\left[ \begin{array}{c} 0 \\ 0 \\ {\Omega _q^2 /z^{2}} \\ {\Omega _{Kq}^2 /z^{2}} \\ \end{array} \right] dq_2 \end{aligned}$$
(23)

Notationally, a change in the price of the clean energy (m) is just like the one for q i.e.

$$\begin{aligned}&\left[ 0 \quad {\Omega _m^1 /z^{1}}\quad 0\quad 0 \right] ^{\prime } \hbox {for}\, \hbox {dm}_{1}\, \hbox {and}\, \left[ 0\quad 0\quad {\Omega _m^2 /z^{2}}\quad {\Omega _{Km}^2 /z^{2}} \right] ^{\prime } \,\hbox {for}\, \hbox {dm}_{2} \end{aligned}$$

If we take the home country (North) to be the importer of the X-good (that uses fossil fuel), then a rise in \(\hbox {p}_{1}\) increases both \(\hbox {C}_{1}\) and \(\hbox {I}_{1}\). These are just the terms of trade effects on real income. A rise in \(\hbox {p}_{1}\) would then reduce both \(\hbox {C}_{1}^{*}\) and \(\hbox {I}_{1}^{*}\) . An increase in \(\hbox {q}_{1}\) decreases \(\hbox {C}_{1},\hbox { I}_{1},\,C_{1}^{*}\) and \(I_{1}^{*}\). The partial effects for the North used in the text are given below (for the South the expressions are identical except \(\Omega ^{*2}\) replaces \(\Omega ^{2}\) etc.):

$$\begin{aligned} \partial I_1/\partial p_2&= -\left[ \left\{ \Omega _{Kp}^2 {-}\left( z_p^2 \Omega _K^2 /z^{2}\right) \right\} \beta {U}^{\prime }(C_2){+}\left\{ \Omega _p^2 -z_p^2 C_2\right\} (\beta {U}^{\prime \prime }(C_2)(1+r_1 )\right] /(\Sigma z^{2})\\ \partial C_2 /\partial p_2&= -\left[ \left\{ \Omega _{Kp}^2 -\left( z_p^2 \Omega _K^{*2} /z^{2}\right) \right\} \beta {U}^{\prime }(C_2)\Omega _K^2 -\left\{ \Omega _p^2 -z_p^2 C_2\right\} \right. \\&\times \left. \left\{ \beta {U}^{\prime \prime }(C_2)\Omega _{KK}^2 +{U}^{\prime \prime }(C_1 )\right\} \right] /\left( \Sigma z^{2}\right) \\ \partial C_2 /\partial q_2&= \left[ \left\{ \beta {U}^{\prime \prime }(C_2)\Omega _{KK}^2 +{U}^{\prime \prime }(C_1 )\right\} \Omega _q^2 -\beta {U}^{\prime \prime }(C_2)\Omega _{Kq}^2 \right] /\left( \Sigma z^{2}\right) <0\\ \partial C_1 /\partial q_1&= -\Omega _q^1 \beta \left\{ {U}^{\prime }(C_2 )\Omega _{KK}^2 +(1+r_1 ){U}^{\prime \prime }(C_2 )\Omega _K^2 \right\} /\left( \Sigma z^{1}\right) <0\\ \partial I_1 /\partial q_1&= {U}^{\prime \prime }(C_1 )\Omega _q^1 /\left( \Sigma z^{1}\right) >0\\ \partial I_1 /\partial p_2&= \left[ {U}^{\prime \prime }(C_1 )+\beta {U}^{\prime }(C_2 )\left\{ \Omega _{pK}^2 -\left( \Omega _K^2 z_p^2 /z^{2}\right) \right\} +(1+r_1 )\beta {U}^{\prime \prime }(C_2 )\right. \\&\left. \times \left\{ \Omega _p^2 -\left( \Omega _2 z_p^2 /z^{2}\right) \right\} \right] /\left( \Sigma z^{2}\right) \\ \partial I_1 /\partial q_2&= \left[ {U}^{\prime \prime }(C_1 )+\beta \left\{ {U}^{\prime }(C_2 )\Omega _{Kq}^2 +(1+r_1 ){U}^{\prime \prime }(C_2 )\Omega _q^2 \right\} \right] /\left( \Sigma z^{2}\right) \\ \partial C_1 /\partial p_1&= \left\{ \Omega _p^1 -\left( \Omega _1 z_p^1 /z^{1}\right) \right\} \beta \left\{ {U}^{\prime }(C_2 )\Omega _{KK}^2 +(1+r_1 ){U}^{\prime \prime }(C_2 )\Omega _K^2 \right\} /\left( \Sigma z^{1}\right) >0\\ \partial I_1 /\partial p_1&= \left\{ \Omega _p^1 -\left( \Omega _1 z_p^1 /z^{1}\right) \right\} {U}^{\prime \prime }(C_1 )/\left( \Sigma z^{1}\right) >0 \end{aligned}$$

where \(\Sigma \equiv \beta \left\{ {U}^{\prime }(C_2)\Omega _{KK}^2 +(1+r_1 ){U}^{\prime \prime }(C_2 )\Omega _K^2 \right\} +{U}^{\prime \prime }(C_1 )<0\)

Appendix 2

Outline of proof of Proposition 1

We want to show that there is leakage but \(<\)100 % i.e.

$$\begin{aligned} 0\ge \frac{d{R}_2^{*}}{d\overline{R}_2^{*}}=\frac{dR_2^*}{dp_2 }\frac{dp_2 }{d\overline{R}_2 }\ge -1 \end{aligned}$$
(24)

The market-clearing condition in the intermediate goods market for period 2 is given by Eq. (16b):

$$\begin{aligned} \Omega _1 \left( 1,p_2 ,\overline{K}_1 +I_1 ,q_2 ;m \right) +\Omega _1^*\left( 1,p_2 ,\overline{K}_1^*+I_1^*,q_2 ;m^{*} \right) =\tilde{X}_2 +\tilde{X}_2^*\end{aligned}$$

Differentiating this and setting, \(R_2 =\overline{R}_2\) we obtain the change in the price \(\hbox {p}_{2}\):

To obtain the leakage, we note that

$$\begin{aligned} R_2^*=R^{*}(p_2 ,K_2^*,(p_2 )) \end{aligned}$$
(25)

The first term is the effect of p\(_{2 }\)on the product mix and the second is the capital accumulation effect of p\(_{2}\). So we have:

$$\begin{aligned} \frac{dR_2^*}{dp_2 }=\frac{\partial R_2^*}{\partial p_2 }+\left( {\frac{\partial R_2^*}{\partial K_2^*}} \right) \left( \frac{\partial I_1^*}{\partial p_2 }\right) \end{aligned}$$
(26)

As noted above, \(\partial I^{*}_{1} / \partial p_{2} >0\). We have:

\(0\ge \frac{dR_2^*}{dp_2 }\ge \frac{\partial R_2^*}{\partial p_2 }\) because \(\left( {\frac{\partial R_2^*}{\partial K_2^*}} \right) \left( \frac{\partial I_1^*}{\partial p_2 }\right) \ge 0\).

In the South due to consumption smoothing, investment declines; this implies that emissions in the South are lower than it would have been had we not taken into account the dynamic effects. Thus an upper bound to carbon leakage is given by the “static” leakage (i.e. holding \(dI_1^*=0\)).

$$\begin{aligned} \left| {\frac{dR_2^*}{dp_2 }} \right| =\left| {\frac{\partial R_2^*}{\partial p_2 }+\left( {\frac{\partial R_2^*}{\partial K_2^*}} \right) \left( \frac{\partial I_1^*}{\partial p_2 }\right) } \right| \le \left| {\frac{\partial R_2^*}{\partial p_2 }} \right| \end{aligned}$$
(27)

The first term in curly brackets on the right hand side of Eq. (27) is the static effect (negative) and the second one is the dynamic effect (positive).

Note that the change in fossil fuel use is obtained from the two equations, equating the marginal product of capital intersectorally and the marginal product of the fossil fuel to its given marginal cost. (we need to solve for S and substitute): That is, we use the three marginal productivity conditions:

$$\begin{aligned} F_K \left( {K_2^{X*} ,R_2^*,Z^{X*}} \right)&= p_2 G_K \left( {K_2^*-K_2^{X*} ,S_2^*,Z^{Y*}} \right) \end{aligned}$$
(28)
$$\begin{aligned} F_R \left( {K_2^{X*} ,R_2^*,Z^{X*}} \right)&= c.\end{aligned}$$
(29)
$$\begin{aligned} G_S \left( {K_2^*-K_2^{X*} ,S_2^*,Z^{Y*}} \right)&= m\Rightarrow dS_2^*=-\left( \frac{G_{KS}^*}{G_{SS}^*}\right) \left( {dK_2^*-dK_2^{X*} } \right) \end{aligned}$$
(30)

After substitution we have:

$$\begin{aligned} \left[ \begin{array}{cc} {[F_{KK}^*+p_1 (G_{SS}^*)^{-1}\{G_{KK}^*G_{SS}^*-(G_{KS}^*)^{2}\}]}&{} {F_{KR}^*} \\ {F_{KR}^*}&{} {F_{RR}^*} \\ \end{array} \right] \left[ \begin{array}{c} {dK_2^{X*} } \\ {dR_2^*} \\ \end{array} \right] = \left[ \begin{array}{c} {G_K^*dp_2 } \\ 0 \\ \end{array} \right] \end{aligned}$$

And so:

$$\begin{aligned}&\frac{\partial R_2^*}{\partial p_2 }=-G_K^*F_{KR}^*\Big /\left[ \left\{ F_{KK}^*F_{RR}^*-\left( F_{KR}^*\right) ^{2}\right\} +p_1 F_{RR}^*\left( G_{SS}^*\right) ^{-1}\right. \nonumber \\&\left. \quad \left\{ G_{KK}^*G_{SS}^*-\left( G_{KS}^*\right) ^{2}\right\} \right] <0 \end{aligned}$$
(31)

Now note that as the X-intermediate sector expands due to a fall in \(\hbox {p}_{2}\), the marginal product of capital in the Y sector rises. And this causes both \(K_2^{X*}\) and \(R_2^*\) to rise as shown in Fig. 1 below. The line RR is the combination of \(K_2^{X*}\) and \(R_2^*\) that gives a marginal product of R. The line KK is the intersectoral equality of the marginal product of capital.

Fig. 1
figure 1

Period one fossil fuel reduction with marginal cost pricing

The slopes are as shown because \([\{F_{KK}^*F_{RR}^*-(F_{KR}^*)^{2}\}+p_1 F_{RR}^*(G_{SS}^*)^{-1}\{G_{KK}^*G_{SS}^*-(G_{KS}^*)^{2}\}]>0\). The initial equilibrium is at A and the new one with \(d\overline{R}_2 <0\) at B. The vertical distance of \(d\overline{R}_2 <0\) is given by the point on \(\hbox {K}'\hbox {K}'\) vertically below A. So from the diagram as the KK line shifts down with \(d\overline{R}_2 <0\), there is an increase in \(dR_2^*\)but is less than \(\left| {d\overline{{R}}_2}\right| \) (KK has a slope steeper than RR). The algebra is trivial.

Therefore we have: \(1<\left( \left| {\frac{dR_2^*}{d\overline{R}_2 }} \right| \right) _{dI_1^*=0} <\left| {\frac{dR_2^*}{d\overline{R}_2 }} \right| <0 \blacksquare \)

Proof of Proposition 2

It proceeds as above for period 2. For period 1, we have:

$$\begin{aligned} \frac{dp_1 }{d\overline{R}_1 }&= \frac{\left\{ {\left( {\frac{z_1^1 }{z^{1}}} \right) \Omega _{\overline{R}}^1 -\Omega _{\mathop {1R}\limits }^1 } \right\} }{\left\{ \Omega _{1p}^1 +\Omega _{1p}^{*1}\right\} }\\ R_1^*&= R^{*} (p_1 )\\ \frac{dR_1^*}{dp_1 }&= -G_K^*F_{KR}^*\Big /\left[ \left\{ F_{KK}^*F_{RR}^*-\left( F_{KR}^*\right) ^{2}\right\} \right. \nonumber \\&\left. +p_1 F_{RR}^*\left( G_{SS}^*\right) ^{-1}\left\{ G_{KK}^*G_{SS}^*-\left( G_{KS}^*\right) ^{2}\right\} \right] <0 \blacksquare \end{aligned}$$

Appendix 3

Equations for Sect. 4.1:

$$\begin{aligned} R_1^*&= -\Omega _q \left( 1,p_1 ,\overline{{K}}_1^*,q_1 ;m^{*}\right) \quad R_2^*=-\Omega _q \left( 1,p_2 ,K_2^*,q_2 ;m^{*}\right) \\ R_1&= -\Omega _q \left( 1,p_1 ,\overline{{K}}_1 ,q_1 ;m \right) \,\quad R_2 =\overline{{R}}_2\\ d\overline{{R}}_2&= d\Omega _q^{*1} +d\Omega _q^1 +d\Omega _q^{*2} \end{aligned}$$

We have from Eqs. (12), (16a) and (16b) to solve for \(\hbox {p}_{2},\hbox { p}_{1}\) and \(\hbox {q}_{1}\):

$$\begin{aligned}&\left\{ \Omega _{qp}^{*2} +\Omega _{qK}^*\left( \partial I_{*1} /\partial p_2 \right) +\Omega _{pq}^2 +\Omega _{qK} \left( \partial I_1 /\partial p_2 \right) \right\} dp_2 \nonumber \\&+\left\{ \Omega _{qK} \left( \partial I_1 /\partial p_1 \right) +\Omega _{qK}^*\left( \partial I_{*1} /\partial p_1 \right) \right\} dp_1\nonumber \\&\quad \left[ \left\{ \Omega _{qq}^{*2} +\Omega _{qK}^*\left( \partial I_{*1} /\partial q_2 \right) \right\} \rho +\left( \Omega _{qq}^{*1} +\Omega _{qq}^1 \right) \right] dq_1 =d\overline{{R}}_2 \end{aligned}$$
(32)
$$\begin{aligned}&\left( \Omega _{pp}^1 +\Omega _{pp}^{*1} \right) dp_1 +\left( \Omega _{pq}^1 +\Omega _{pq}^{*1} \right) dq_1 =0\end{aligned}$$
(33)
$$\begin{aligned}&\left\{ \Omega _{qp}^{*2} \!+\!\Omega _{qK}^*\left( \partial I_{*1} /\partial p_2 \right) \!+\!\Omega _{qK} \left( \partial I_1 /\partial p_2 \right) \right\} dp_2 {+}\Omega _{qK}^*\left( \partial I_{*1} /\partial p_1 \right) dp_1 {+}\left( \Omega _{qp}^1 {+}\Omega _{qp}^{*1} \right) dp_1 \nonumber \\&\quad +\left\{ \Omega _{qq}^{*2} \rho +\Omega _{qq}^1 +\Omega _{qq}^{*1} +\Omega _{qK}^*\rho \left( \partial I_{*1} /\partial q_1 \right) \right\} dq_1 =\left( 1-\Omega _{qK} \left( \partial I_1 /\partial p_2 \right) \right) d\overline{{R}}_2 \end{aligned}$$
(34)

Equations for Sect. 4.2:

In Sect. 4, any policy to restrict fossil fuel use in period 2 also impacts period 1 via a change in \(\hbox {q}_{1}\) and hence \(\hbox {p}_{1}\). As in Sect. 3.2, a cap on fossil fuel use at \(\overline{{R}}_1\) in period 1, of course, will have an impact on \(\hbox {p}_{2}\) via investment. But now there is the additional channel of a fall in \(\hbox {q}_{2}\).

$$\begin{aligned} R_2&= -\Omega _q \left( 1,p_2 ,K_2 ,q_2 ;m \right) \quad \,\,\, R_1^*=-\Omega _q \left( 1,p_1 ,\overline{{K}}_1^*,q_1 ;m^{*}\right) \\ R_2^*&= -\Omega _q \left( 1,p_2 ,K_2^*,q_2 ;m^{*}\right) \quad R_1 =\overline{{R}}_1 \end{aligned}$$

Equation (12) implies:

$$\begin{aligned} d\overline{{R}}_1 =d\Omega _q^{*1} +d\Omega _q^2 +d\Omega _q^{*2} \end{aligned}$$

Equations (12), (16a) and (16b) give (again to solve for \(\hbox {p}_{2},\hbox { p}_{1}\) and \(\hbox {q}_{1}\)):

$$\begin{aligned}&\left\{ \Omega _{qp}^{*2} +\Omega _{qK}^*\left( \partial I_{*1} /\partial p_2 \right) +\Omega _{pq}^2 +\Omega _{qK} \left( \partial I_1 /\partial p_2 \right) \right\} dp_2 \nonumber \\&\quad +\left[ \left( \Omega _{qq}^2 +\Omega _{qq}^{*2} +\Omega _{qK}^*\left( \partial I_{*1} /\partial q_2 \right) + \Omega _{qK} \left( \partial I_1 /\partial q_2 \right) \right) \rho +\Omega _{qq}^{*1} \right] dq_1\nonumber \\&\quad +\left\{ \Omega _{qK} \left( \partial I_1 /\partial p_1 \right) +\Omega _{qK}^*\left( \partial I_{*1} /\partial p_1 \right) +\left( \Omega _{pp}^1 +\Omega _{pp}^{*1} \right) \right\} dp_1 =d\overline{{R}}_1 \end{aligned}$$
(35)
$$\begin{aligned}&\left( \Omega _{pp}^1 +\Omega _{pp}^{*1} \right) dp_1 +\left( \Omega _{pq}^1 +\Omega _{pq}^{*1} \right) dq_1 =\left\{ \left( 1-\left( z_p^1 /z^{1}\right) \right) \Omega _{\overline{{R}}}^1 -\Omega _{p\overline{{R}}}^1 \right\} d\overline{{R}}_1\end{aligned}$$
(36)
$$\begin{aligned}&\left\{ \Omega _{pp}^{*2} +\Omega _{pK}^{*2} \left( \partial I_{*1} /\partial p_2 \right) +\Omega _{pp}^2 +\Omega _{pK}^2 \left( \partial I_1 /\partial p_2 \right) \right\} dp_2\nonumber \\&\quad +\left\{ \Omega _{pq}^{*2} \rho +\Omega _{pq}^2 \rho +\Omega _{qK}^{*2} \rho \left( \partial I_{*1} /\partial q_1 \right) +\Omega _{qK}^2 \rho \left( \partial I_1 /\partial q_1 \right) \right\} dq_1 +\left\{ \Omega _{pK}^{2*} \left( \partial I_{*1} /\partial p_1 \right) \right. \nonumber \\&\quad \left. +\,\Omega _{pK}^2 \left( \partial I_1 /\partial p_1 \right) \right\} dp_1 =0 \end{aligned}$$
(37)

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Sen, P. Unilateral Emission Cuts and Carbon Leakages in a Dynamic North–South Trade Model. Environ Resource Econ 64, 131–152 (2016). https://doi.org/10.1007/s10640-014-9860-2

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