1. Introduction
Advancements in recent decades in climate science and economic modelling, juxtaposed against the real-time observation of the dire consequences of extreme weather events, have revealed important lessons about the macroeconomic consequences of climate change. These are understood to varying degrees. The best understood lessons include: both the contributions to and consequences of climate change are unequally distributed, estimates of the economic costs of climate change and corresponding uncertainty, tend to grow, rather than fall over time, well-designed carbon pricing mechanisms can effectively reduce emissions and inequality, poorly designed ones do not and it is exceedingly difficult to aggregate from the wealth of climate microeconomic studies to make inferences about macroeconomic outcomes.
Among the less understood lessons are the observation that climate investments are cheaper than the alternative—namely, climate-driven disasters. The effects of climate change are severe even in wealthy countries (Kahn et al., Reference Kahn, Mohaddes, Ng, Pesaran, Raissi and Yang2021), and the consequences of climate change are landing sooner than early models predicted. Many of the biggest risks may fall in the realm of social and political instability rather than extreme weather, and the financial system is far behind and poorly equipped to measure and manage these risks. Recent evidence also shows that many low-carbon and climate resilient investments—from energy and transport infrastructure to buildings and agriculture—are cheaper than their fossil fuel-based counterparts, leading to the potential stranding of the carbon-intensive legacy assets they replace (Office for Budget Responsibility, 2021).
Here, we shed light on the comparatively under-researched question of how climate change might affect the financial system and in particular, fiscal sustainability and sovereign debt markets. First, we provide a taxonomy of how the physical and transition impacts from climate change translate into fiscal risks. Second, we review a small but increasingly urgent literature on how these fiscal risks affect sovereign creditworthiness and the cost of public borrowing, with direct implications for fiscal sustainability. Finally, we demonstrate the taxonomy’s usefulness using two examples—one sovereign (the UK) and one industry (renewable energy). Combined, the case studies elucidate two potential uses for our taxonomy, (i) identifying economically relevant blind spots in climate risk analyses and (ii) for understanding feedback mechanisms that must be considered in any attempt to estimate both the costs of decarbonisation and the pace at which it can be achieved. We conclude by reflecting on the types of metrics that could improve the economic assessment of climate risks and how they relate to fiscal decision-making.
Our decision to focus on sovereign debt—even in the midst of a zeal for metrics relating to environmental, social and governance investing—is deliberate. Sovereign debt, which is expected to top $92 trillion this year (IIF, 2021) is by far the world’s largest asset class. It is the safe haven to which investors flee in times of turmoil, and its sustainability is what determines the capacity of nations to weather shocks, from Covid-19 to climate change.
Whilst climate-economic models have described in ever greater detail the potential costs of the physical impacts of climate change, we highlight the importance of understanding the transition impacts and how they affect fiscal sustainability. Our contribution to this special issue is timely, not just with respect to COP26 in Glasgow, Scotland, but also in the midst of unprecedented fiscal disruption in response to the Covid-19 pandemic. Concern over debt-rollover, fiscal space and the ability to respond to future shocks are now paramount in policy circles. These discussions must include an understanding of how climate change—and our responses to it—will affect the public finances and sovereign debt markets. The topics discussed here are of interest to policy-makers and investors concerned with financial system stability, institutional investors and pension managers, and the flow of accurate information through markets—a necessary condition for the efficient management of risk.
2. Taxonomy for translating physical and transition risk into sovereign risk
Although much of the scientific and media attention is understandably focussed on extreme weather events, sea-level rise and ecosystem collapse, there are several transmission channels through which climate change can affect public finances and sovereign risks (see, for instance, Figure 1 and Volz et al., Reference Volz, Beirne, Ambrosio Preudhomme, Fenton, Mazzacurati, Renzhi and Stampe2020). It is now increasingly recognised that the fiscal consequences of climate change and the policy responses to it are not limited merely to the direct physical damages.Footnote 1 Indeed, some of the most significant near-term impacts on the global economy and public finances, especially in advanced economies, will derive from the climate transition as much as the physical risks from climate change itself. The ‘transition’ reflects the process of decarbonisation, for example the policies, consumer preferences, litigious actions and technological development that accompany the drive to reduce emissions. Chief among these may be an accelerated pace of human capital obsolescence (and the social disruption this would inevitably bring) as a labour force adapted to the fossil fuel economy struggles to find productive roles in a low carbon world. As a result, it is important to consider the potential risks and opportunities associated with the structural transformation of the economy.
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Figure 1. Climate change to sovereign risk: a review of impact pathways. Source: Adapted from Volz et al. (Reference Volz, Beirne, Ambrosio Preudhomme, Fenton, Mazzacurati, Renzhi and Stampe2020).
2.1. Depletion of natural capital and ecosystem services
Climate change is expected to have dramatic and adverse effects on natural capital (IPBES, 2019). Traditionally, integrated assessment models (IAMs) such as DICE have modelled climate as an independent feature of nature, ignoring feedback loops with the rest of natural capital (such as biodiversity). In contrast, Bastien-Olvera and Moore (Reference Bastien-Olvera and Moore2020) construct a GreenDICE model to simultaneously model these linkages, showing that they have long-lasting implications for human welfare, carbon prices and the optimum investment strategy for addressing climate change. They find that the macroeconomic consequences of emissions are even greater when climate-induced natural capital loss is included and because early investments in biodiversity and ecosystems can partially offset the costs of climate change, they are important components of any climate strategy (Agarwala and Coyle, Reference Agarwala and Coyle2020). The nexus of climate and natural capital has several impacts on sovereign risk, especially for countries in which agriculture, forestry and fisheries are key industries. But it also impacts the frequency, intensity and resilience to extreme weather events such as storm surges, fires, floods and extreme temperatures. The key point is that climate change affects the productive capital stock, output, supply chains and resilience both directly and indirectly through its interaction with other components of natural capital. The associated impacts on the public finances and sovereign risk must be accounted.
2.2. Fiscal impacts of climate-related disasters
Public finances and debt sustainability face exposure to different fiscal risks related to climate disasters (Koetsier, Reference Koetsier2017). These include both macroeconomic risks and contingent liabilities. Macroeconomic risks related to natural disasters and extreme weather include risks of a disruption of economic activity, which may adversely affect tax income and other public revenues and increase social transfer payments (e.g. Schuler et al., Reference Schuler, Oliveira, Mele, Antonio and Pigato2019); changes to commodity prices that could affect revenue or increase spending via fossil fuel or food subsidies; effects on inflation and interest rates through supply or demand shocks and exchange rate effects (e.g. Farhi and Gabaix, Reference Farhi and Gabaix2016). Contingent liabilities can explicitly or implicitly expose governments to fiscal risks (Mitchell, Mechler, and Peters, Reference Mitchell, Mechler, Peters, Markandya, Galarraga and de Murieta2014; Hochrainer-Stigler et al., Reference Hochrainer-Stigler, Keating, Handmer and Ladds2018; Schuler et al., Reference Schuler, Oliveira, Mele, Antonio and Pigato2019). Natural disasters may damage or destroy physical government assets and public infrastructure, requiring significant expenditure on relief programmes, damage repair or reconstruction. Indeed, in the United States alone, there have been 298 climate-related disaster events with damages in excess of $1 billion since 1980 with a total cost of $1.975 trillion in 2021 (NOAA, 2021).
Natural disasters may also affect the assets or operations of state-owned enterprises. Disasters may damage or destroy private property and require government support for households and corporations to rebuild homes and businesses. To the extent that disasters cause instability to the financial sector, they may force governments to bail out ailing financial institutions. Moreover, disasters can cause a severe humanitarian crisis, which may require public emergency measures, including rescue missions, temporary relocation of people, provision of food and shelter or medical treatment. Such crisis response measures can be very expensive and have a significant impact on public spending.Footnote 2 Moreover, economic shocks from extreme weather events, although short term in nature, can also have lasting impacts on growth (Acevedo, Reference Acevedo2014; Botzen, Deschenes, and Sanders, Reference Botzen, Deschenes and Sanders2019; Klomp and Valckx, Reference Klomp and Valckx2014) and public finances.
2.3. Fiscal consequences of adaptation and mitigation policies
The public sector will have to finance a considerable share of adaptation and mitigation measures. To achieve the Paris climate goals and limit global warming to manageable levels, large investments are needed in a low-carbon transformation of infrastructure and energy systems. Moreover, economies need to invest in resilience to address vulnerabilities from extreme weather events and the effects of gradual global warming. The Global Commission on the Economy and Climate (2019) estimated that globally, until 2030, it will be necessary to spend around $90 trillion on infrastructure, including energy, all of which needs to be sustainable and climate resilient. While parts of these investments will have to be financed by the private sector, governments will have to play an important role not only in setting the right incentives through climate policies, but also through direct fiscal spending.
A related concern is that structural shifts throughout the low-carbon transition can disrupt traditional sources of government revenue. Tax revenues from oil and gas production, as well as fuel duties can be a significant source of government revenue. For instance, in 2018, the UK Treasury received about 61.3 per cent of the price charged for each litre of pump fuel sold to consumers; the averages for the G7 and OECD are 50 and 49 per cent, respectively (OPEC, 2019). Losing such revenues due to the phaseout of fossil fuels can add significant pressure to public finances. But for some sovereigns, the risk is more acute. Jaffe (Reference Jaffe2020) points out that by far the largest holders of fossil fuel assets are state-owned enterprises. Whilst private oil majors have already begun to diversify their portfolios, the risk that sovereign holdings of fossil fuel reserves may become stranded assets is even more directly linked to sovereign creditworthiness.
2.4. Climate-driven aggregate supply and demand shocks and impacts on output
Both the physical and transition impacts of climate change can cause aggregate supply and demand shocks, with significant implications for output, employment and public finances. The supply- and demand-side effects of gradual global warming and transition impacts can cause fundamental and enduring structural changes to the economy (Semieniuk et al., Reference Semieniuk, Campiglio, Mercure, Volz and Edwards2021). Such impacts can be anticipated across sectors and industries. Both the supply and demand for particular types and locations of housing, insurance products, agricultural output, transport infrastructure and even university degrees and training programmes are likely to be affected (Hepburn et al., Reference Hepburn, O’Callaghan, Stern, Stiglitz and Zenghelis2020).
Current models vary in their projections of the reduction in national output (GDP) arising from different warming scenarios. Conservative estimates project reductions in global per capita GDP of between 7 and 13 per cent, varying significantly across countries depending on the pace of temperature increases and variability of climate conditions, by 2100 (Kahn et al., Reference Kahn, Mohaddes, Ng, Pesaran, Raissi and Yang2021), mid-range estimates indicate a 7–14 per cent reduction for a 3.5C warming world (Kalkuhl and Wenz, Reference Kalkuhl and Wenz2020), whilst estimates at the higher range indicate a loss of 21 per cent (Burke, Hsiang, and Miguel, Reference Burke, Hsiang and Miguel2015). A country’s long-term growth potential will inevitably have ramifications for its public finances and debt sustainability. These could be even larger if, as recent research suggests, the volatility of temperature rises with its average (Kahn et al., Reference Kahn, Mohaddes, Ng, Pesaran, Raissi and Yang2021). Kotz et al. (Reference Kotz, Wenz, Stechemesser, Kalkujl and Levermann2021) show that independent of the rise in average temperature, an increase in the variability of temperature by 1° results in a 5 percentage point reduction in regional growth rates, on average.
2.5. Impacts on innovation, competitiveness and efficiency
Most accounts of the effect of climate policies on innovation take an optimistic tone. From Hicks (Reference Hicks1932) to Stern (Reference Stern2007), it is argued for instance that carbon prices will induce innovation in low carbon alternatives. However, this presupposes that carbon prices are sufficient to overcome not only the emissions externality, but also any additional market failures (e.g. asymmetric market power, lobbying influence and path dependencies) that tend to favour the status quo. Moreover, if climate-induced innovation takes the form of more efficient complements for carbon intensive industries, such as a more fuel-efficient internal combustion engine, they could serve to further lock-in carbon intensive infrastructure and production. If in contrast, climate-induced innovation accelerates the adoption substitutes such as electric vehicles, the transition may be faster.
Even if the net effect of climate on innovation is positive, genuine concerns about how this translates into fiscal risk remain. For instance, if climate-driven innovations render human and physical capital obsolete, the employment and subsequent social effects could be severe (see Section 2.9). Assets that were initially expected to be productive for many years may become stranded abruptly. In order to meet climate targets consistent with a 50/50 chance of limiting temperatures to 2° above pre-industrial times, a third of global oil reserves, half of gas reserves and 80 per cent of current coal reserves will have to remain in the ground or, if they are burned, the emissions will have to be captured and stored (McGlade and Ekins, Reference McGlade and Ekins2015). But the risk from stranding does not end with fossil fuels. ‘Downstream’ transport infrastructure, refineries, carbon-intensive industrial facilities and power generation assets also risk being stranded. Financial services heavily invested in all these fossil fuel entangled sectors will also be hit with great concerns around systemic risk and sovereign risk, if large financial institutions or governments become insolvent (Pfeiffer et al., Reference Pfeiffer, Millar, Hepburn and Beinhocker2016). Skills, ideas and institutions will also become outmoded.
Another concern is the global distribution of innovation and its rewards. Countries which delay investment and transition could miss out on first-mover advantages, learning by doing and global competitiveness (see Section 6). Finally, the possibility cannot be ruled out that delayed action means that climate change imposes significant physical losses on national output, unevenly distributed across countries. In such a world, it is reasonable to consider that innovation and competitiveness in the hardest hit countries would suffer significantly.
2.6. Effects of climate change on productivity
The direct and transition effects of climate change on productivity are likely to be negative on net, owing largely to its effects on human, physical and natural capital. The likely effects of warming, and especially rising temperature volatility, on human health and labour productivity are increasingly well established and their consequences for national output are of first order concern (Day et al., Reference Day, Fankhauser, Kingsmill, Costa and Mavrogianni2019). Despite difficulties in distinguishing between supply and productivity effects, empirical studies and model results generally agree that the effect of climate on labour will vary across sectors (indoor vs. outdoor work; see Kahn et al., Reference Kahn, Mohaddes, Ng, Pesaran, Raissi and Yang2021 for a within-country study of the ten sectors in the United States) and countries (it will be more severe in the tropics) (Dasgupta et al., Reference Dasgupta, van Maanen, Gosling, Piontek, Otto and Schleussner2021). Estimates indicate that heat stress has already reduced labour capacity by 10 per cent in peak temperature months over recent decades, and could rise to a 20 per cent reduction in labour capacity globally in the hottest months by 2050 (Dunne et al., Reference Dunne, Stouffer and John2013).
The productivity effects are of course not limited to impacts on human capital. Recent years have seen physical infrastructure forced to operate at reduced capacity due to extreme weather events. Obvious examples for the UK include trains operating at reduced speeds due to high temperatures (which affect metal tracks), airport disruption due to winter storms and local transport disruptions due to floods. In Texas, winter storm Uri in February 2021 triggered a wave of blackouts as energy infrastructure seized in sub-zero temperatures, leaving more than two-thirds of Texans without power for an average of 42 h during the week of the storm, and an official death tollFootnote 3 of 151 (Watson et al., Reference Watson, Cross and Jones2021). Both the impairment and stranding of physical infrastructure have consequences for productivity estimates and subsequently, macroeconomic risks.
2.7. Climate risks to financial system stability
Climate change, and policy responses to it, pose a material and systemic risk for the financial sector (Bolton et al., Reference Bolton, Despres, Awazu Pereira Da Silva, Samama and Svartzman2020; Monasterolo, Reference Monasterolo2020; NGFS, 2019). Using an IAM to estimate the expected ‘climate value at risk’ (climate VaR) of global financial assets, Dietz et al. (Reference Dietz, Bowen, Dixon and Gradwell2016) show that 1.8 per cent of total global financial assets were at risk of climate change along a business-as-usual emissions path, and because risks are concentrated in the tails, this rises to 16.9 per cent for the 99th percentile of climate VaR. This has direct consequences for pensions and investment funds, especially given their heavy exposure to assets that could become stranded in a disorderly transition to net zero (Battiston et al., Reference Battiston, Mandel, Monasterolo, Schütze and Visentin2017).
Such climate-induced financial vulnerabilities can spill over to the public sector and give way to a negative feedback loop between financial sector instability and sovereign risk (Acharya et al., Reference Acharya, Drechsler and Schnabl2014; Angelini et al., Reference Angelini, Grande and Panetta2014; Dell’Ariccia et al., Reference Dell’Ariccia, Ferreira, Jenkinson, Laeven, Martin, Minoiu and Popov2018; Farhi and Tirole, Reference Farhi and Tirole2018; Gennaioli et al., Reference Gennaioli, Martin and Rossi2018). A weakening of the sovereign balance sheet due to public debt-funded bailouts of banks can further weaken the credit profile of banks due to their sovereign debt holdings and lead to a ‘doom loop’ (Farhi and Tirole, Reference Farhi and Tirole2018). Governments may also rely on domestic banks as a source of funding during periods of financial crisis, putting additional pressure on them to hold more government bonds and worsening the negative feedback effects between financial sector and sovereign risk.
2.8. Impacts on international trade and capital flows
Climate change can have substantial impacts on an economy’s trade in goods and services and capital flows with the rest of the world with potentially significant ramifications for countries’ balance of payments positions and, ultimately, sovereign risk. Both the physical impacts of climate change and the disruptions resulting from the climate policies that trading partners adopt, technological change or changes to consumption patterns can affect international trade and financial flows. Historically, balance of payment problems have often been at the root of country risk and led to external debt crises (Bouchet et al., Reference Bouchet, Fishkin and Goguel2018). Protracted current account imbalances tend to cause liquidity problems and, if not resolved, solvency problems. The current account balance is therefore an important indicator of sovereign risk.
Decarbonising the global economy may have counterintuitive consequences for many fossil fuel-rich nations. Ultimately, the magnitude and even the sign of the effect on fossil fuel export revenues depends on the characteristics of resource endowments, including carbon intensity and ease of extraction. Some models suggest that oil and gas owners may benefit during the transition if carbon taxes make dirtier fuels, such as coal and heavy oil less competitive (Coulomb and Henriet, Reference Coulomb and Henriet2018). Whilst the most carbon-intensive fossil fuels will likely be stranded, some estimates suggest the so-called ‘Grey Paradox’ could increase the net present value of OPEC revenue by up to 4 per cent (Persson et al., Reference Persson, Azar, Johansson and Lindgren2007).
2.9. Impacts of climate change on political stability
The economic and social effects of climate change may accentuate the social tensions within a society and fuel political instability. Moreover, climate change leads to large-scale migration movements, which could also lead to political tensions or even inter- and intrastate conflicts. Political instability can undermine the ability or willingness of a government to repay its debt. For instance, Clark (Reference Clark1997) emphasised the potential impact of political events on the probability of sovereign default, while Cuadra and Sapriza (Reference Cuadra and Sapriza2008) maintained that countries that are politically unstable and more polarised have higher default rates and as a result have to pay a higher default risk premium in international credit markets.
These transmission channels are not independent of each other. Climate impacts can magnify the transmission of risk through multiple channels. The socioeconomic and fiscal effects of climate change are multifaceted and depend on the policies taken or not to mitigate and adapt to these risks. Nor is it guaranteed that all of the impacts through these transmission channels will necessarily be negative, that is, exacerbating risk. Particularly around issues of innovation, competitiveness and productivity, well-designed climate policies can actually serve to reduce sovereign risk. This is especially likely if mitigation and adaptation policies enhance human, physical and natural capital (Agarwala et al., Reference Agarwala, Cinamon Nair, Cordonier Segger, Coyle, Felici, Goodair, Leam, Lu, Manley, Wdowin and Zenghelis2020). Similarly, a revolution in green finance could help support a just transition characterised by high returns as low-carbon investments and technologies begin to out-compete their carbon-intensive counterparts. Climate-proofing public finances hence ought to be a key priority of public policy.
3. Climate risks and sovereign creditworthiness
Despite growing evidence of the risk channels outlined in Section 2, mainstream estimates of sovereign risk—especially sovereign credit ratings—have so far been slow to adjust. Although credit ratings agencies have started to discuss climate-related risks, even acquiring climate data firms, there is little evidence that sovereign ratings have been affected. This is an important consideration. The efficient market hypothesis depends on the availability of reliable information about risk. If sovereign ratings cannot be shown to respond to the growing scientific and economic evidence of the consequences of climate change, markets and investors may struggle to correctly identify, price and manage risk throughout their portfolios.
Recent empirical analyses suggest that the scientific and economic evidence is sufficient to demonstrate an effect of climate on sovereign creditworthiness. By introducing an integrated assessment model into the European Stability Mechanism’s debt sustainability analysis optimisation model, Zenios (Reference Zenios2021) finds that adverse climate effects on debt dynamics arise as early as 2030. He argues that European institutions including the European Commission, European Central Bank, European Stability Mechanism, European Fiscal Board and member states’ finance ministries should incorporate climate change into sovereign risk assessments.
Cevik and Jalles (Reference Cevik and Jalles2020a) estimate the effect of climate vulnerability on credit ratings of 67 sovereigns between 1995 and 2017, finding that vulnerability negatively affects sovereign credit ratings. However, the result is not robust to different model specifications. More fundammentally, this backwards-looking analysis cannot be used to make inferences about the future affect of climate change on creditworthiness, which is clearly the more important question for managing the public finances over the medium- to long-run.
Klusak et al. (Reference Klusak, Agarwala, Burke, Kraemer and Mohaddes2021) is the first paper which offers a forward-look into the effects of climate on sovereign credit ratings. Combining climate-economic models with observed sovereign ratings and an artificial intelligence (AI) model, they construct the world’s first climate adjusted sovereign rating for 108 sovereigns under three climate scenarios. Results indicate that climate change will exert downward pressure on ratings as early as 2030 with an increasing magnitude throughout the century (see Figure 2). Preliminary results show that if global emissions follow their recent trend, the UK could see a 1-notch downgrade (on a 20-notch rating scale) by 2030, growing to more than three notches by the end of century under a high emissions scenario (RCP 8.5). If instead emissions profiles are consistent with limiting warming to 2C, the UK’s sovereign downgrade would be limited to approximately 1 notch by 2100.
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Figure 2. Climate-adjusted ratings to 2100 (RCP 8.5 vs. 2.6). Source: Klusak et al. (Reference Klusak, Agarwala, Burke, Kraemer and Mohaddes2021). The horizontal axis indicates current ratings by S&P and the thick black line represents exact matches between current and predicted ratings. The dotted lines are the best fit lines for climate-adjusted ratings under RCP 8.5 and 2.6, respectively, for 2030, 2050, 2070 and 2100 (Panels A and B). RCP 2.6 and RCP 8.5 are consistent with warming of less than 2C and 4.5–5C relative to pre-industrial levels, respectively.
4. Climate change and the cost of sovereign debt
Weak fiscal positions characterised by high debt, high deficits and low growth increase sovereign the cost of public borrowing (Barrell and Holland, Reference Barrell and Holland2009). Whilst early climate models indicated that the worst effect of climate change would accrue far in the future, sovereign debt markets may be expected to price these effects in earlier. Indeed, empirical evidence suggests that climate vulnerability has already raised the average cost of debt in climate-vulnerable developing countries. A first analysis of the nexus between climate vulnerability and the cost of capital by Kling et al. (Reference Kling, Lo, Murinde and Volz2018) showed that countries with higher exposure to climate vulnerability incur a risk premium on their sovereign debt.Footnote 4 Conducting a panel and principal component analysis with annual data for a sample of developing and advanced 46 countries over the period 1996–2016, Kling et al. (Reference Kling, Lo, Murinde and Volz2018) find that, controlling for macroeconomic factors, climate vulnerability has increased debt costs for a subgroup of 25 climate-vulnerable developing countries by 1.17 percentage points. In absolute terms, this translates into $40 billion in additional interest payments for 40 climate-vulnerable countries over the period 2007–2016 on government debt alone. Projections suggest additional interest payments attributable to climate vulnerability to increase to between $146 and 168 billion for the same group of countries over the next decade (Buhr et al., Reference Buhr, Volz, Donovan, Kling, Lo, Murinde and Pullin2018).
Subsequent studies have corroborated the positive effect of physical climate vulnerability on the cost of government debt. Using data for 98 advanced and developing countries over the period 1995–2017, Cevik and Jalles (Reference Cevik and Jalles2020b) replicate the methodology and measures employed by Kling et al. (Reference Kling, Lo, Murinde and Volz2018) and confirm their findings. Using refined measures of climate risk and resilience and a higher data frequency for 40 advanced and emerging economies, Beirne et al. (Reference Beirne, Renzhi and Volz2021a) also confirm the findings of a climate risk premium by Kling et al. (Reference Kling, Lo, Murinde and Volz2018). Moreover, Beirne et al. (Reference Beirne, Renzhi and Volz2021a) develop a set of panel structural VAR models that indicate the reaction of bond yields to climate risk shocks becomes permanent after around 18 quarters with high-risk economies experiencing the largest permanent effects on yields. Beirne et al. (Reference Beirne, Renzhi and Volz2021b) conduct an in-depth analysis of the link between climate change and sovereign risk in Southeast Asia, one of the regions most heavily affected by climate change. Both the country-specific and the panel estimates for six Southeast Asian countries with monthly data for the period 2002–2018 show that greater climate vulnerability appears to have a sizable positive effect on sovereign bond yields, while greater resilience to climate change has an offsetting effect, albeit to a lesser extent.
Looking at climate transition risk, Battiston and Monasterolo (Reference Battiston and Monasterolo2020) employ a financial pricing model with forward-looking simulations to estimate effects of climate risk on the sovereign bond yields of 34 countries. They find that economies that are highly exposed to carbon-intensive sectors incur higher yields on their sovereign bonds. Klusak et al. (Reference Klusak, Agarwala, Burke, Kraemer and Mohaddes2021) use an AI-based approach to estimate the additional cost of sovereign and corporate debt resulting from climate-driven downgrades under various warming scenarios. Under the low emissions scenario (RCP 2.6) the UK’s 0.92-notch downgrade by 2100 would amount to an increase in the annual interest payment on public debt of $2.0–3.0 billion and an increase of $250–440 million on corporate debt. Under the high emissions scenario (RCP 8.5), this rises to $7.54–11.31 billion and $0.94–1.65 billion in additional interest payments on sovereign and corporate debt respectively. Relative to 2020–2021 levels, the increase in annual debt servicing costs for UK central government debt (net of the Asset Purchase Facility) ranges from 9 to 13.6 per cent under RCP 2.6–33.8–50.7 per cent under RCP 8.5 (House of Commons, 2021). These preliminary estimates should be considered severe underestimates because the effect of downgrades is placed on the pre-pandemic level of debt. The figures would grow with the level of debt over the century.
For comparison, figures for G7 plus China show that climate-induced downgrades could increase the cost of sovereign debt by $18.18–27.27 billion ($113.93–170.89 billion) under the RCP 2.6 (RCP 8.5) scenario. The additional annual interest payments of corporations will reach $5.35–9.36 billion (20.75–36.31 billion) by 2100.
5. Measuring the impact of a transition to net zero on the UK economy and public finances: Using OBR and CCC projections
In this section, we demonstrate how the transmission pathways set out in Section 2 map onto the likely impacts of the UK’s transition to net zero on the national economy and the public finances, drawing insights from the UK OBR’s recent Fiscal Risks Report (OBR, 2021). The report uses the highly credible UK Climate Change Committee (CCC) figures to conclude that meeting net zero will leave GDP 1.4 per cent lower than the hypothetical counterfactual path in 2050 and public debt 21 per cent of GDP higher. It is important to note that the report makes no attempt to account for the positive impact on UK debt from forgone climate damages and risks, reflecting the fact that the UK is a marginal player when it comes to global emissions. The focus is therefore solely on transition costs from the UK’s efforts to reduce emissions and efforts to adapt to a changing climate and associated risks. Nevertheless, the headline analysis needs to be interpreted carefully and masks a much richer story.
Firstly, the likely costs and benefits are unevenly distributed through time. Higher net spending outlays early on are likely to generate higher net revenues down the line, thereby promoting rather than eroding public debt sustainability over the longer term.
Early fiscal outlays must be viewed as investment costs, which expand the public sector’s net worth by generating net revenues or public returns down the line. Indeed, the CCC numbers which the OBR uses show that by 2050, operating costs in most sectors are expected to be lower than under a net zero scenario relative to baseline, a trend that would be expected to continue through the second half of the century with the potential to boost the public finances. Starting with cars, and moving progressively sector by sector, the falls in operating costs become so large that in total they begin to offset the additional capex costs (see Figure 3) from around 2040 net ‘costs’ become negative.
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Figure 3. (Colour online) Capital and investment costs and operating cost savings in the Balanced Net Zero Pathway. Source: UK Climate Change Committee (CCC), Sixth Carbon Budget (2021).
By truncating the cost benefit analysis at 2050, and assessing the integral only over the next 30 years, the OBR analysis includes the bulk of the (front-loaded) investment cost, but excludes decades and centuries of future net gains. To illustrate the point, consider a policymaker charged with assessing the case for education spending. The cost savings over this period from eliminating public spending on primary, secondary and tertiary education might well exceed the forgone net revenues from lower wages and social disruption in the first 30 years. Yet, a policymaker would be rash to scrap all education spending knowing that a stream of positive net returns will accrue for many decades into the future, just because they fell outside the analytically arbitrary cut-off date for the projection.
The second question surrounds the presumed impact of early action on productivity growth. The baseline numbers assume that additional investment to address climate impacts and transition requirements crowds out alternative investment and leaves UK productivity lower by mid-century. But this is far from a foregone conclusion. An accurate prediction of the impact of a low-carbon transition on GDP in 30 years’ time is, of course, unrealistic. But it is important to note that the numbers quoted by the OBR are hugely sensitive to changes in the economy’s dynamic productive potential. The OBR’s own calculations suggest a boost to annual productivity growth of less than 0.05 per cent would potentially wipe this out this loss.Footnote 5
Such a productivity gain is not trivial, were it available. But it is important to recognise that this is not an absolute gain, it is a hypothetical gain assessed against a baseline scenario in which the UK charts a future based on high-carbon goods and services. However, such a scenario is highly vulnerable to negative output shocks associated with stranded and devalued assets. All told, there is evidence to suggest that the OBR are being overly conservative. Over time, investing in cleaner, more efficient and innovative production is likely to be more productive than relying on the technologies of the previous century (Way et al., Reference Way, Ives, Mealy and Farmer2021). This is even before account is taken of climate damages, which can mount much more quickly as productivity growth is eroded through endogenous impact of destroyed or devalued capital (Dietz and Stern, Reference Dietz and Stern2015).
The economics of innovation and productivity means the cost of meeting various decarbonisation and resource-management targets are not only hard to predict, but that they are path-dependent (Aghion et al., Reference Aghion, Hepburn, Teytelboym and Zenghelis2014). Initial conditions and decisions made today, in changing behaviour and generating innovation, matter greatly. Relatively small interventions can generate a virtuous cycle of innovation, investment and falling costs of green technologies as evidenced in the renewable energy and vehicle sectors. By contrast, lock-in of resource- and carbon-intensive infrastructure, behaviour and institutions increases the cost of attaining sustainable pathways.
The sheer scale of the low-carbon transition generates productivity enhancing network effects and economies of scale in production and discovery. These are already apparent having caught most commentators by surprise. The price of solar photovoltaic has dropped by 83 per cent since 2010, a period over which the price of wind turbines fell nearly 40 per cent (Liebreich, 2018). These technologies are increasingly producing cheaper power than most coal- and many gas-fired power plants (Figure 4).
![](https://static.cambridge.org/binary/version/id/urn:cambridge.org:id:binary:20220127055256720-0671:S0027950121000375:S0027950121000375_fig4.png?pub-status=live)
Figure 4. (Colour online) Levelised costs of electricity (constant 2019 US dollars per kWh). Source: Committee on Climate Change, 2020.
The important lesson from Figure 4 is not just that renewable energy now competes with fossil fuels (net of infrastructure and subsidies), but rather how this transition came about and what lessons can be learned to stimulate further innovations. The pace and extent of cost reductions required a series of several interconnected, amplifying feedback mechanisms. These include:
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• Learning-by-doing. With deployment, lessons are learned on how to manufacture, distribute, install, run and maintain equipment more efficiently.
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• Economies of scale in production and distribution. Unit cost fall as production and distribution ramp up once large, fixed costs are incurred.
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• Network and coordination effects. This reflects the greater advantages of moving in tandem with others, such that the gains are higher the more economic agents are taking similar action.
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• Sector spill-overs. Not only have sustainable technologies been shown to have predictably higher cost-reducing learning rates, but they have also been shown to have positive productivity spill-overs into other sectors of the economy. Using data on 1 million patents and 3 million citations, Dechezleprêtre et al. (Reference Dechezlepretre, Martin and Mohnen2014) suggest that productivity enhancing spill-overs from low-carbon innovation are over 40 per cent greater than from conventional technologies (in the fossil fuel energy production and transportation sectors).
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• Social and institutional feedbacks. Acceptable standards of behaviour and social norms are liable to change (Licht, Reference Licht2008; Ostrom, Reference Ostrom2000; Posner, Reference Posner1997).
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• Evolution of consumer behaviour. Consumer tastes are key in the attribution of future value to goods and services and consumers routinely influence one another, leading to positive feedbacks and crowd effects and changing consumption patterns. The heterogeneity of real-world consumer behaviour is readily inferred from standard innovation diffusion theory where technology adoption typically follows s-shaped patterns starting with innovators and early adopters, through the majority to finally affect laggards (Mercure et al., Reference Mercure, Chester, Lynch, Jarvis and Jarvis2021)
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• Expectations. People’s changing expectations with shape the nature and pace of change. Perception of new technologies as superior leads to behaviour change which itself facilitates their successful adoption (Van der Meijden and Smulders, Reference Van der Meijden and Smulders2017). Expectations that the cost of a net zero transition will be inevitable and affordable can become self-fulfilling (Zenghelis, Reference Zenghelis2021a).
Figure 5 demonstrates how these economic phenomena interact to drive innovation and transition. Note that initially, low levels of installed capacity are associated with high costs. This means markets alone were highly unlikely to deliver the necessary transition. Early-on, government leadership (subsidies and signals) was needed to drive initial investments. Learning-by-doing and economies of scale drove efficiency gains as installed capacity grew. Notably, coal has not become significantly cheaper over the same time period. Instead, social norms and consumer behaviour have driven demand for renewable energy, and in many parts of the world, for the complementary purchases such as electric vehicles. Strong policy signals on the phase-out of internal combustion engines have further shaped expectations, and manufacturers are responding by increasing the range of EVs available on the market.
![](https://static.cambridge.org/binary/version/id/urn:cambridge.org:id:binary:20220127055256720-0671:S0027950121000375:S0027950121000375_fig5.png?pub-status=live)
Figure 5. (Colour online) Renewable electricity costs fall as installed capacity rises. Source: Our World in Data (2021).
Whilst it remains to be seen whether the story of renewable energy is an exception—the timescales, cost profiles and innovation pathways in other sectors may differ—it is clear that an early start, corresponding to the OBR net zero scenario, is therefore likely to cut the costs of transition and improve economic performance compared with delay and indecision. It may also be pivotal to shaping the long-term sustainability of the public finances.
The potential net benefits from early action would be expected to be higher if the UK moves in tandem with the other countries in imposing ambitious policies to generate innovation at scale. In such an environment, the net gains from low carbon investments would be far higher and the estimated increase in borrowing costs and corresponding downgrades in sovereign ratings reported in Sections 3 and 4 would also be far smaller, testifying to the importance of global coordination. Although Klusak et al. (Reference Klusak, Agarwala, Burke, Kraemer and Mohaddes2021) identify the possibility of climate-driven downgrades even under RCP 2.6, their model makes no adjustment for early investments in adaptation. As the treatment of climate change in sovereign ratings methods becomes more sophisticated, one would expect investments in adaptive capacity to reduce the downward pressure of climate on ratings.
6. Competitive position and macroeconomic context
The transition will also affect any advanced economy’s competitive position in changing world markets. Most European countries are small to medium sized open economies. Productivity and growth over long time periods will be driven by comparative as well as absolute advantages in new markets and these are not set in stone but are shaped by policy. This goes beyond comparing absolute investment and operating costs.
Falling behind on policies and investments may induce significant displacement of high productivity (and high productivity growth) activities to other countries, if the world shifts to low carbon resource efficient markets (e.g. as a result of global policies hostile to high carbon activities and undercutting technologies outcompeting high carbon incumbents).
Hidalgo et al. (Reference Hidalgo, Klinger, Barabási and Hausmann2007) and Mealy and Teytelboym (Reference Mealy and Teytelboym2021) use network analysis to demonstrate that it is easier for countries to become competitive in new green products that require similar production capabilities and know-how to existing sectors. This helps demonstrate how green transitions are highly path-dependent: countries which successfully invest early in green capabilities have greater success in diversifying into future green product markets. This also has potential implications for industrial policy seeking to develop comparative advantages in fast growing new sectors. The potential fiscal risks should be clear.
Other studies focus on ‘revealed technological advantage’ to determine where opportunities for sustainable growth and recovery might reside. Martin et al. (Reference Martin, Unsworth, Valero and Verhoeven2020) compare broad categories of technologies and find that the UK is relatively specialised in wind and ocean energy, as well as biotechnology and pharmaceuticals. They argue that the returns to public investments in these technologies are likely to be disproportionately high, improving the UK’s longstanding poor productivity performance and competitiveness while also addressing large-scale disparities across and within regions (see also Stern and Valero, Reference Stern and Valero2021).
The impact of adopting policies to transition the economy to net zero, and associated risks, is a function of the broader global macroeconomic context. Recent evidence on productivity strongly suggests the world needs markedly higher investment (Zenghelis, Reference Zenghelis2021b). Weak private confidence has meant ex ante desired investment lagged desired saving for more than a decade, driving real risk-free interests rates to below zero.Footnote 6
Negative rates in turn push the efficacy of monetary policy to its limits, fuelling asset price rises that disproportionately benefited the rich. A fundamental policy error following the crash of 2008 was introducing austerity programmes to balance budgets prematurely. Reduced public borrowing to invest exacerbated the problem of excess net saving (Auerbach and Gorodnichenko, Reference Auerbach and Gorodnichenko2017). Research suggests European countries suffered a decade of lower growth than the United States, which adopted a far more relaxed fiscal stance (Jordà and Taylor, Reference Jordà and Taylor2016).
7. Conclusion and policy imperatives
Climate change poses new risks which will affect the financial system, fiscal sustainability and sovereign debt markets. At the same time, attempts to meet agreed climate targets will require an unprecedented structural transformation of the global economy over the next two or three decades. The changing landscape of risks warrants new risk management and hedging strategies to contain climate risk and minimise the impact of asset stranding and asset devaluation. Yet, conditional on action being taken early, the opportunities from managing a net zero transition would substantially outweigh the costs.
Public investment in complimentary assets alongside supportive policies and institutions are prerequisites to ‘crowd in’ sustainable capacity and bolster the structural resilience of the economy. This historic growth opportunity has been reflected in large stimulus and recovery packages adopted in the Europe, the United States and other advanced economies. Each has placed clean investment at its heart.
Yet the call for public investment to boost productive capacity, following an unprecedented government response to the global pandemic, understandably has raised concerns about fiscal space. Public debt relative to GDP is already close to historic highs in many European countries. Combined with record broad money supply growth it has also rekindled fears of the return of inflation (Haldane, Reference Haldane2021).
These justifiable fears notwithstanding, the risks from higher public debt in the short term, are far lower than the likely benefits (Stern and Zenghelis, Reference Stern and Zenghelis2021). There are increasing opportunities associated with a public drive to steer a zero-carbon economy which can crowd in investment and expand capacity. The IMF Fiscal Monitor for October 2020 argued that an additional £1 in public borrowing to invest in ‘job-rich, highly productive and greener activities’ would generate an additional £2.7 of additional output (IMF, 2020; Gaspar et al., Reference Gaspar, Mauro, Pattillo and Espinoza2020). This marks scope for strong crowding-in. The markets agree: they continue to lend to governments at real interest rates which remain at near-record lows. The most promising way to bring down public debt in the medium term is to borrow to invest now (Chudik et al., Reference Chudik, Mohaddes, Pesaran and Raissi2017).
A fundamental feature of transition and climate change is that the infrastructure, skills and ideas of the last century can quickly become a liability. Resource- and carbon-intensive physical, human and knowledge assets risk becoming devalued or obsolete. Early indications suggest that this may already be affecting some asset prices, even as fossil fuels continue to play a key role in the economy. However, due to the difficulty of translating climate risks to financial risks, markets have been slow to respond. It is for this reason that the Financial Stability Board’s Task Force for Climate Related Disclosure is calling for mandatory disclosure and stress testing of assets (TCFD, 2017).
It is increasingly recognised that growth is not only compatible with sustainability, but also requires it (Zenghelis, Reference Zenghelis2021b). Recent studies have highlighted the urgent need to strengthen the quality of natural assets (New Climate Economy, 2018). They also point to numerous near-term opportunities associated with tackling particulate pollution, congestion, ill-health, biodiversity loss, inefficiency and waste and building more attractive, liveable cities. This is especially true after the COVID pandemic, which marks a period of dislocation and change affording a potential opportunity to lock in to pathways which create durable and resilient jobs (Stern et al., Reference Stern, Unsworth, Valero, Zenghelis, Rydge and Robins2020).
A recent survey of 231 economic experts from G20 countries, including central bank and finance ministry officials, found that major fiscal recovery packages that focussed on clean R&D spending, clean energy infrastructure, connectivity infrastructure, building upgrades, energy efficiency and investment in green spaces were considered best placed to boost long term growth (Hepburn et al., Reference Hepburn, O’Callaghan, Stern, Stiglitz and Zenghelis2020).
7.1. Just and inclusive policies will lower transition costs
With many of the key barriers to the low-carbon transition being political and behavioural, rather than technological and economic, policymakers recognise the need to act quickly and carefully to ensure that change is in the interest of the many. This means compensating, reskilling and retooling those who stand to lose out, enabling them to participate in the new economy and provide the jobs of the 21st century. It also means supporting overstretched consumers who may face higher charges to fund transitional infrastructure investment. Ensuring a just transition will be central to maintaining social cohesion (Robins et al., Reference Robins, Gouldson, Irwin, Sudmant and Rydge2019; Rydge et al., Reference Rydge, Martin and Valero2018).
So how big are transition risks? The correct answer is that it is ‘endogenous’ (Ekins and Zenghelis, Reference Ekins and Zenghelis2021). It depends on the choices and actions we take today and in the future. The longer we wait to manage that transition, the bigger the dislocation risks and the higher the adjustment costs. Understanding the processes which drive innovation, change social norms and build stronger institutions will help decision-makers steer growth in a manner that is not only cleaner and more secure, but also more innovative, competitive and productive. This reduces transition risk. By this logic, any optimism must be conditional. It requires credible and ambitious action in the near term to avoid catastrophic and irreversible environmental risk and unleash private ingenuity and finance to build a more efficient, innovative and productive economy.
Acknowledgements
The authors are grateful Yamini Cinamon Nair for excellent research assistance and to Moritz Kramer, Stavros Zenios, NIESR and the organisers and participants of the 17th EUROFRAME Conference for insightful comments. We also thank the Editorial team and anonymous referees for helpful suggestions. MA, MB and PK acknowledge funding from the INSPIRE Network, MA & DZ acknowledge funding from the Wealth Economy project supported by LetterOne and The Productivity Institute, funded by the UK Economic and Social Research Council (grant number ES/V002740/1).