# As Bad as it Gets: How Climate Damage Functions Affect Growth and the Social Cost of Carbon

## Abstract

The paper analyzes the effects of varying climate impacts on the social cost of carbon and economic growth. We use polynomial damage functions in a model of an endogenously growing two-sector economy. The framework includes nonrenewable natural resources which cause greenhouse gas emissions; pollution stock harms capital and reduces economic growth. We find a big effect of the selected damage function on the social cost of carbon and a significant impact on the growth rate. In our calibration a quartic damage function raises the social cost of carbon by more than a factor of ten compared to the linear function. In the social optimum the growth rate remains positive even when the damage function is highly convex. We test the robustness of the results by adding pollution decay, lowering the elasticity of intertemporal substitution, and addressing uncertainty, which does not alter our results. We find that high marginal climate damages require stringent climate policies but do not preclude positive economic growth despite convexity, provided that policies are designed in an efficient manner.

### Keywords

Climate damages Social cost of carbon Endogenous growth Polynomial functions### JEL Classification

Q43 O47 Q56 O41## 1 Introduction

### 1.1 Climate Impacts

There is broad agreement that climate change has widespread effects on the economy and the natural environment. It causes economic damages which worsen with increasing temperatures.^{1} For a thorough assessment of the consequences and the formulation of appropriate climate policies the determination and the use of an appropriate damage function is indispensable: it lies “at the heart” of the economic analysis of climate change (Farmer et al. 2015, p. 332). Such a function specifies how economic damages change as a function of greenhouse gas concentration in the atmosphere. The present paper thoroughly explores the impact of damage modeling in a theoretical setup of an economy with climate change and endogenous growth.

The economic impacts from climate change are difficult to be estimated on a global level (IPCC 2014b). So far, there is no agreement on the form and the parametrization of a general climate damage function. Nordhaus and Boyer (2000, p. 23) state that “estimating the damages from greenhouse warming has proven extremely elusive.” According to Weitzman the literature offers “little guidance on why one specification or another” of a damage function has been selected (Weitzman 2010a). It is thus admitted that a strong empirical basis for the damage functions used in the best-known models is lacking. What is more, climate damages have implausibly small effects on economic growth in most integrated assessment models even under extreme temperature scenarios (Stern 2013; Revesz et al. 2014).

The big challenge for formulating a comprehensive climate damage function is to properly aggregate various highly heterogeneous effects. Climate impacts on different regions and ecosystems are provided in IPCC (2014b) and Roson and Sartori (2016).^{2} Yet, for a global analysis of climate damages, the available data are not sufficiently complete. Bottom-up studies may be used to inspire a general formula, but by their nature they are limited in scope. It thus remains unclear which functional form for the damage function is suitable (Moore and Diaz 2015) and where the limitations are to capture “everything by a simple function” (Farmer et al. 2015, p. 332). Damage functions are one of various elements of integrated assessment models which have recently been criticized. Farmer et al. (2015, p. 329) conclude that also the issues of risks, heterogeneity, and technical change are “inadequately addressed” by climate modelers. In all these areas, model specifications strongly affect the results and associated policy recommendations (Revesz et al. 2014). While recent contributions have addressed the additional issues under critique,^{3} the functional form of the climate damage function has received little attention,^{4} although its potential impact on optimal policies is substantial and the critique has been especially sharp.^{5} The present paper shows how important the specifications of the damage functions are in climate economics. We use higher-order polynomial functions up to a cubic and quartic form to assess the impact of climate damages on welfare and growth. In our model, damages affect the capital stock, reducing both current income and economic growth; for a long-run ecological phenomenon economic dynamics become crucial.

The agreed temperature targets of international climate policy suggest that marginal climate damages become very large or even infinite once the temperature ceiling is reached. Conversely, most economic models use constant or quadratic functions for climate damages so that a specific threshold temperature does not emerge and optimum warming can exceed the ceiling, depending on the benefits of climate policy. We want to keep the assumption of a continuous damage function but aim at including high marginal damages by considering highly convex damage functions. This brings the economic view of optimal pollution closer to the view of climate physics and policymakers favoring temperature targets.^{6}

We find a big effect of the damage function on the social cost of carbon and a significant impact on the economic growth rate. Using a theoretical framework, this paper shows that the negative impact of climate damages on economic growth grows with the degree of convexity of the assumed damage function. Moreover, contrary to the prevalent opinion in public discourse, optimally designed climate policies do not prevent the world economy from experiencing positive growth rates despite the convexity of damage functions. However, if climate policies aiming to correct the pollution externality are sub-optimally chosen, damages to capital become higher and the economic growth rate may become negative in the long run.^{7} Calibrating our model, we confirm that in the social optimum economic growth rates are still positive in the long run even for highly convex damage functions and assuming non logarithmic utility, i.e. for a quartic damage function and a low intertemporal elasticity of consumption substitution. Specifically, a quartic damage function raises the social cost of carbon by more than a factor of ten compared to the linear function, already after 14 years.^{8}

### 1.2 Contribution to the Literature

Modeling externalities in the form of greenhouse gas emissions includes two components: climate sensitivity, i.e. the increase in long-term temperature caused by growing concentration of carbon dioxide in the atmosphere, and climate damage functions, capturing the relationship between temperature rise and induced losses in the economy. Regarding the former, the broadly used RICE/DICE model (Nordhaus and Boyer 2000) uses a small structural model to describe the relationship between pollution stock, radiative forcing, and climate change, suggesting that temperature is a concave function of pollution stock. This crucial assumption is used in most of the climate economics literature, e.g. in Golosov et al. (2014) and van den Bijgaart et al. (2016, p. 78) where it is said that the relation “between atmospheric \(\mathrm{CO}_{2}\) concentrations and equilibrium temperatures can be described through a logarithmic curve..”. However, the IPCC has recently summarized all the relevant research and explains: “Multiple lines of evidence indicate a strong, consistent, almost linear relationship between cumulative \(\mathrm{CO}_{2}\) emissions and projected global temperature change to the year 2100 ..” IPCC (2014a, p. 9). This suggests the IAM tradition should be abandoned and climate sensitivity should be modelled using a linear rather than a concave function, as we will apply below.

With respect to the second component —climate damage functions—, RICE/DICE assumes that climate change affects current output negatively. Specifically, climate damages \(D(\cdot )\) are a quadratic function of temperature while a “damage coefficient” \(\Omega =\) \(1/\left[ 1+D(\cdot )\right] \) is used to multiply final output to reflect the impact of climate change (\(0<\Omega <1\)). The higher the damage, the lower the coefficient and thus output and income.^{9} The functional form of the damage function and its parametrization has been inspired by numerical estimations of predicted climate damages. Nordhaus (2007) estimates that damages are 1.7 percent of output at 2.5 \({^\circ }\)C warming, which provides a parameter value for the quadratic term; Hanemann (2008) presents estimates for the same temperature which are 2.4 times as much, so a different value appears warranted.^{10} To deal with higher temperatures one could use extrapolations of these models. However, Ackerman and Stanton (2012) find that this procedure lets damages grow very slowly with temperature. Only half of world output would be lost when temperatures increase by 19 \({^\circ }\)C in the Nordhaus case or 12 \({^\circ }\)C for the Hanemann specification neither of which is very plausible. Weitzman (2010b) argues that scientific evidence implies much greater losses, especially at higher temperatures. He modifies the RICE/DICE setup by adding a term to the damage function where temperature is raised to the power of 6.76. As a result, damages turn out to be 50 percent of output at 6 \({^\circ }\)C warming and 99 percent at 12 \({^\circ }\)C, which is closer to what natural science predicts. Evidently, adding a quadratic or a higher order term to a linear specification of the *D*-function increases output loss for any given temperature. But the use of the damage coefficient \(\Omega \) for multiplication with output implies that, with rising temperature, a total collapse of the economy is only reached asymptotically, i.e. only a temperature of infinity would entail a total income loss, which is an extreme assumption. Put differently, the relationship between temperature and damages (measured as a share of output \(1-\Omega )\) becomes concave for high temperatures (Ackerman and Stanton 2012, p. 11), which contradicts general expectations. We will use polynomial damage functions including terms of higher order to reach a significant degree of convexity but use the *D*-function for damages instead of coefficient \(\Omega \) so that damage concavity is removed. We will thoroughly analyze the impact of variations of the damage functions in a climate economy model with endogenous growth where emissions occur endogenously through exhaustible resource use.^{11}

While the DICE model considers damages of climate change on current productivity, Weitzman (2010a) analyzes climate effects on individual utility.^{12} We highlight that damages affect not only the output level but also the growth rate of an economy, which is an important aspect of climate change (Moore and Diaz 2015; Bretschger and Vinogradova 2016; Bretschger and Karydas 2017). Moore and Diaz (2015) add induced capital depreciation to the DICE model and find that this entails more stringent climate policies in the optimum and slows down growth, especially in poor countries. We continue this line of research by including the dynamic effects of climate change in a full-fledged macroeconomic growth model with focus on highly convex climate damage functions. We close the gap between the moderately convex cost functions and the strict temperature targets of international climate policy implying that marginal damages become very high when the temperature target is exceeded. An alternative approach is to include a ceiling constraint for pollution stock as presented in Amigues and Moreaux (2013). In the optimum, carbon concentration increases up to the cap where the economy is constrained as long as natural resources are still abundant and natural decay too weak. Conversely, in our model, damages already occur at a level which is lower than the cap and increase in a continuous way so that discontinuities in consumption do not arise. Acemoglu et al. (2012) also assume that the deterioration of environmental quality may induce an environmental disaster in finite time. Such a state would cause infinite damage but in their model it is never formally reached because policy is able to avoid it.

The literature agrees that damages are a convex function of temperature but the degree of the convexity is an open issue, inevitably subject to uncertainty, see for instance Dietz and Stern (2015). The previous idea of IAMs (e.g. Golosov et al. 2014) that the mapping from the atmospheric carbon dioxide concentration to economic damages would amount to a composition of a convex and a concave function and could potentially become almost linear has to be discarded however; the concave relation between carbon emissions and global temperature is not existent. The economic impact of climate change crucially depends on the degree of the convexity of the damage function, which we explore in this contribution.

The structure of the paper is the following: In Sect. 2 the baseline model’s setup, assumptions, and solution are described. In Sect. 3, the long-run steady state of the economy is analysed. Section 4 describes the transition phase of the economy. Section 5 introduces the extensions to the baseline model, namely pollution decay, non-logarithmic utility and uncertainty. Section 6 concludes.

## 2 Baseline Model

### 2.1 The Setup

The model includes two sectors, one for final goods production and one for capital accumulation; it assumes that nonrenewable resource use causes emissions which accumulate aggregate pollution stock. Pollution negatively affects the existing capital stock; capital loss is a highly convex function of pollution stock. Emissions, the social cost of carbon and economic growth are endogenously determined from the model in closed-form solutions. To reduce emissions, the economy needs to decrease resource use and will use and accumulate more capital by reallocating inputs between the sectors.

*F*denotes a function and

*t*the time index. The remaining fraction \(1-\epsilon _{t}\) of capital \(K_{t}\) is used for the accumulation of new capital which is harmed by climate damages. Specifically, we denote by \(\dot{K_{t}}\) the time derivative of capital and by \(D(P_{t})\) a polynomial function expressing the damages of the pollution stock \(P_{t}\) on capital, with the depreciation rate \(\eta D(P_{t})\le 1\) for any \(P_{t}\), so that

^{13}That climate change enters the capital accumulation equation rather than the utility function follows a prominent request by Stern (2013). The stock of greenhouse gases in the atmosphere is accumulated with resource use according to

### 2.2 Assumptions

- 1.
Production

For the production of final goods of Eq. (1) we assume the Cobb–Douglas specificationwith \(A>0.\) Both inputs are essential so that resources are always needed to obtain positive output.$$\begin{aligned} Y_{t}=A(\epsilon _{t}K_{t})^{\alpha }R_{t}^{1-\alpha } \end{aligned}$$(5) - 2.
Utility

When \(\sigma \) denotes the coefficient of relative risk aversion, the utility function takes the formfor \(\sigma \ne 1\) and$$\begin{aligned} U(C_{t})=\frac{C_{t}^{1-\sigma }-1}{1-\sigma } \end{aligned}$$(6)for \(\sigma =1\). For the sake of clarity we assume \(\sigma =1\) in the main part of the paper and provide a separate discussion for the case \(\sigma \ne 1\) in a separate section below.$$\begin{aligned} U(C_{t})=\ln C_{t} \end{aligned}$$(7) - 3.
Pollution decay

It has been found that a small fraction of greenhouse gases in the atmosphere decays rapidly in the short run and a substantial fraction remains in the atmosphere for a very long time period (more than a thousand years). To highlight the second part of the process we abstract in the baseline model from pollution decay, i.e. set \(\theta =0\) but will extend the model in a separate section by adopting a positive decay rate (\(\theta >0\)).

### 2.3 Solving the Model

*t*, that is \(Y_t=C_t\). The associated Hamiltonian reads

The social cost of carbon (SCC) reflects total damages from releasing greenhouse gas emissions to the atmosphere at every point in time. This essential guideline for optimal climate policies has been the subject of many recent contributions (e.g. Van den Bijgaart et al. 2016; Ackerman and Stanton 2012). In our model we label SCC by \(\chi _{t}\), which is equal to the marginal damage due to pollution, that is \(\chi _{t}\equiv -\dfrac{\mu _{Pt}}{\mu _{Yt}}\), whereas the social cost of carbon per unit of output, which under general conditions equals the optimal carbon tax in decentralized equilibrium, is \(\tilde{\chi }_{t}\equiv \dfrac{\chi _{t}}{Y_{t}}=-\dfrac{\mu _{Pt}}{\mu _{Yt}Y_{t}}=-\mu _{Pt}\ \)so that \(\hat{\tilde{\chi }}_{t}=\hat{\mu }_{Pt}\).

## 3 Long-run Steady State

*t*according to

^{14}The Jacobian matrix evaluated at the steady state gives us the eigenvalues, \(\{0,-\rho ,-\rho ,\rho ,\rho \}\), and the corresponding eigenvectors that specify the solution. At this point it is interesting to note that the linearized dynamic system is subject to a zero eigenvalue. This would mean that the dynamic system shows hysteresis. However in our case this does not happen because the corresponding coefficient of this eigenvector has to be set equal to zero, given our initial conditions. Moreover, in order to avoid solutions that result in diverging values of the variables in infinity, we set the coefficients that correspond to positive eigenvalues equal to zero and use appropriate initial values for \(u_{0}\) and \(\chi _{0}\), while taking as exogenous the initial values \(\psi _{0}\), \(P_{0}\) and \(S_{0}\).

^{15}

*B*is high enough (\(B>\eta D(P_{\infty })\)) and the discount rate is sufficiently low \((\rho <\alpha (B-\eta D(P_{\infty })))\). The range of possible \(\rho \) that result in positive growth becomes wider with a higher capital share \(\alpha \).

^{16}Thus, in order to have \(\hat{Y}_{\infty }>0\Leftrightarrow \frac{B-\rho /\alpha }{\eta }>D(P_{\infty })\), there is an upper bound to damage size. For the choice of parameters and further conclusions we proceed to the analysis of transitional dynamics.

## 4 Transition Phase

It can be seen from the figures that a linear damage function results in a constant SCC per output, while higher degree polynomial damage functions cause a higher level of SCC per output that is reached in infinite time. While the increase is not very pronounced for the quadratic case it is highly visible for the cubic and quartic damage functions. It is striking that already after 14 years, the SCC per output differs by more than a factor of ten when the quartic instead of the linear damage function is used.

With the new initial SCC per output we find a significant distinction between two different scenarios. The first is to assume a linear or a quadratic function, where it turns out that the time paths for \(\tilde{\chi }_{t}\) as well as \(\hat{Y}_{t}\) are almost identical. This result illustrates that a second-degree polynomial damage function, despite being convex, does not affect the variables as much as one would probably expect. Conversely, in the second scenario, when we use a quartic damage function we can show that this introduces high-enough convexity to have significant effects on both model variables; the same applies for the cubic function to a somewhat lower degree.^{17}

## 5 Model Extensions

### 5.1 Pollution Decay

From these graphs, it can be seen that the maximum level of pollution stock is reached after the maximum level of the SCC per output is attained. This is due to the fact that future damages are being discounted in the present.

Finally, the growth rate of output is declining to lower levels compared to the no decay case, before it starts increasing again and return almost to its initial level in the very long run. More precisely, the lowest growth rates of output for the four cases are \(2.05\%\) for the linear damage function, \(1.99\%\) for the quadratic, \(1.83\%\) for the cubic and \(0.94\%\) for the quartic. The reason for this behavior is that in addition perfect foresight, there is also pollution decay in this extension of the model. Hence, \(\hat{Y}_{t}\) first reacts sharply to the increasing pollution and eventually returns to a higher level, after pollution has been absorbed by the environment.

### 5.2 Non-logarithmic Utility

We now turn to the case where the intertemporal elasticity of consumption substitution is unequal unity by assuming that utility be given by Eq. (6) where \(\sigma \ne 1.\) Apart from that, the optimization problem is identical to Eq. (8); the first-order conditions of this problem are given in the Appendix. In the non-logarithmic case, the share of capital does not jump to its steady state value but asymptotically approaches a steady-state value. In order to prove that there is such a steady-state value of \(\epsilon _{t}\), we start from the transversality condition \(\lim _{t\rightarrow \infty }\mu _{Kt}K_{t}e^{-\rho t}=0\) and Eq. (41), from which we can see that \(\hat{\mu }_{Kt}+\hat{K}_{t}-\rho <0\Leftrightarrow \epsilon _{t}>0\). However, from the equation of capital accumulation and in order for the growth rate of capital to be constant in the long run, we need \(\lim _{t\rightarrow \infty }\hat{\epsilon }_{t}\le 0\). Hence, we can conclude that \(\lim _{t\rightarrow \infty }\hat{\epsilon }_{t}=0\).

^{18}The share converges to a steady state, which is higher than \(\rho /B\) for all damage functions, as can be seen from Fig. 8.

It is also worth noting that as convexity increases, \(\epsilon _{\infty }\) reaches a lower value. That is because in the long run capital has to be shifted towards the capital producing sector, as damages become more severe and a higher portion of the capital stock gets destroyed.

^{19}We find a peak after several decades (at 35 and 40 years for cubic and quartic damage functions, respectively) before the growth rate starts decreasing again. This is because the initially increased use of the polluting resource causes the economy to grow in a first phase, without inducing sufficient capital accumulation as a compensation for pollution losses in the second phase. As expected from Eq. (29), the long-run growth rate of output for the calibarated value \(\sigma =2\) is half the respective value of the baseline case where \(\sigma =1\).

### 5.3 Uncertainty

The graphs above illustrate the implications of \(\pi \). More specifically, we can see that uncertainty on the form of the climate damage function may lead to miscalculating the SCC, which in turn results in a poorly designed climate policy. Additionally, uncertainty creates a range within which the growth rate of output lies. In other words, policy makers cannot correctly estimate the time path of a critical variable.

## 6 Conclusions

The paper shows that the choice of a specific climate damage function has a big impact on optimal climate policy and economic growth. We derive the effects of different damage functions on the social cost of carbon and the growth rate of the economy for various model specifications. In our baseline model, increasing convexity of the function raises the social cost of carbon sharply, suggesting more stringent climate policy is needed with growing pollution stock. The theory presented in this paper does not provide a criterion for the selection of the most realistic function but derives the economic consequences when high convexity of climate damage functions is significant. This is strongly suggested by empirical findings and implicitly assumed in the fixed temperature targets of international climate policy. In our calibrated model we find that the long-run growth rate is still positive for highly convex functions provided that we are in a social optimum which in reality is achievable by efficient climate policies.

Assuming a natural decay for pollution stock entails a peak in the social cost of carbon and a U-shaped pattern for optimal growth. Over time, the pollution stock grows less rapidly because of fading resource use as before but is now also reduced by natural forces. Note that the turning point of pollution stock is only reached after a very long time delay so that a long first phase of development is very similar to the baseline case without decay. When we posit that the intertemporal elasticity of consumption substitution is below unity we find that the growth rate of the economy becomes lower, resource use is brought forward, and the social cost of carbon grows less rapidly with damage convexity compared to the baseline case. Uncertainty, on the other hand, affects optimal policy, since the SCC per output and the growth rate of the economy now depend on the probability of a higher order damage function.

Our approach can be extended both in the direction of the assumed growth mechanics and the considered climate impact. It would also be rewarding to extend our analysis on risk and uncertainty. A broader use of the damage functions of this paper in integrated assessment models would potentially give rise to novel policy conclusions. This is left for future research.

## Footnotes

- 1.
The effects range from sea level rise, drop in crop yields, and human health to energy demand; in 2017, strong hurricanes have caused immense damage: according to the Economist “Hurricane Harvey already set records as America’s most severe deluge.. The UN reckons that, in the 20 years to 2015, storms and floods caused $1.7trn of destruction; the World Health Organisation estimates that, in real terms, the global cost of hurricane damage is rising by 6% a year. Flood losses in Europe are predicted to increase fivefold by 2050.” Economist (2017, 2 Sept).

- 2.
These authors present estimations of damage functions parameters for 140 countries and regions and for six climate impacts: sea level rise, variation in crop yields, heat effects on labor productivity, human health, tourism and household energy demand showing the heterogeneity of the different damages.

- 3.
Technological change is addressed in Acemoglu et al. (2012), the impact of risk in Bretschger and Vinogradova (2016), the spatial distribution in Brock and Xepapadeas (2017), the time distrubution in Gerlagh and Liski (2017) and Bretschger and Karydas (2017) and the North–South aspects in Bretschger and Suphaphiphat (2014).

- 4.
- 5.
In a well-known contribution, Pindyck (2013, p. 860) writes: “the models’ descriptions of the impact of climate change are completely ad hoc, with no theoretical or empirical foundation.”

- 6.
Temperature targets (2 \( {^\circ } \)C resp. 1.5 \( {^\circ } \)C warming) are an important part of the Paris Climate Agreement.

- 7.
In this paper, we focus on analysing the social planner solution, so this result does not arise.

- 8.
The quartic damage function has a parallel in physics, such as in the Stefan–Boltzmann law.

- 9.
Golosov et al. (2014) adopt a slightly different functional form for

*D*by assuming exponential damages but this approximates the other function well. - 10.
Even the higher estimate of Hanemann (2008) is not compatible with the 2 \( {^\circ }\)C target of international climate policy which implicitly assumes that damages of temperature rise exceeding 2 \( {^\circ }\)C are very high.

- 11.
Optimal resource depletion is characterized in the seminal contributions of Dasgupta and Heal (1974) and Stiglitz (1974); endogenous growth with pollution builds on Bovenberg and Smulders (1995), Barbier (1999), Smulders (1999), and Xepapadeas (2005); optimal carbon taxes in a growing economy have been analyzed by Golosov et al. (2014) and Van der Ploeg and Withagen (2014). As a consequence of optimal resource extraction the use of resources decreases over time so that pollution stock accumulates as a concave function of time which affects the optimal solutions in our model.

- 12.
An early contribution on the effects of stock pollution on utility in an endogenous growth model is Michel and Rotillon (1995).

- 13.
- 14.
By construction of the method the precision of the values is high when we are close to the steady state.

- 15.
The linearized solution of the dynamic system can be found in the Appendix.

- 16.
For a CIES function (with \(\sigma \) for the relative risk aversion) and damages given by \(D_{t} =\frac{\eta }{S_{0}-S_{t}}P_{t}\)\((P_{0}=0)\) Bretschger and Karydas (2017) calculates growth as \(\hat{Y}=\left[ \alpha (B-\eta \phi )-\rho \right] /\sigma \) which is very similar to the result here.

- 17.
To complete the analysis, the time paths for the model variables \(u_{t}\) (depletion rate), \(\psi _{t}\) (ratio of shadow prices), as well as for pollution stock \(P_{t}\) and resource stock \(S_{t}\) are shown in figures that are available from the authors upon request.

- 18.
Additionally, due to lower IES, the polluting resource extraction is shifted towards the present.

- 19.
For ease of comparison, the same damage functions as in the initial baseline case are being used in this extension.

- 20.
This result is modified below when we discuss the model extensions.

## Notes

### Acknowledgements

We thank Christos Karydas, Andreas Schaefer and Aryestis Vlahakis, as well as an anonymous referee for valuable comments.

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