While not fully integrated in the economic modelling toolkit, the scenario analysis presented in Chapter 2 includes estimates of the economic benefits from reduced climate damages between the modelled scenarios. Benefits from reduced climate damages are quantified starting from the emission and temperature pathways underlying the Current Policies and Enhanced Policies scenarios. These scenarios are on pathways that would imply an average global temperature increase by the end of the century of 2.4°C and 1.7°C, respectively.
Considering the uncertainty in the quantification of economic costs of climate change, for each scenario, this report employs three different damage functions (Barrage and Nordhaus, 2024[56]; Howard and Sterner, 2017[57]; Bilal and Känzig, 2026[58]), aiming to reflect the broad range of estimates from the literature. While virtually all studies agree that the global long-term damages from climate change will be substantial, there is significant uncertainty surrounding the exact magnitude of these impacts. Although specific channels through which climate change can affect economic and welfare outcomes are empirically well-established for a range of channels and across multiple sectors, quantifying the aggregate expected economic impact of climate change on economic output has proven to be challenging and remains an active and heavily debated area of research (O’Neill, 2022[105]; Howard and Sterner, 2017[57]; Tol, 2024[106]).
Uncertainty surrounds each step needed for the calculations of the economic benefits from reduced climate damages. The climate system’s response to rising GHG concentrations, which forms the basis to calculate economic damages, depends on the extent to which rising GHG concentrations translate into temperature increases, sea-level rise or the likelihood and the frequency and severity of highly stochastic extreme weather events (O’Neill, 2022[105]). Similarly, there are uncertainties on how these climate projections translate into economic damages. Climate change affects socioeconomic systems through both gradual and sudden impacts and these effects are difficult to predict in both timing and location. Moreover, damages will unfold over decades, with cumulative effects that are not immediately observable. Researchers have employed a variety of methodological approaches to estimate the economic damages. These approaches differ in terms of their underlying assumptions, data sources, methods and model structures, leading to a wide range of estimates in the literature.
The three damage functions employed for the analysis in this report are representative of the much wider set of damage curves existing in the literature. The curves rely on different approaches and lead to diverging estimates. The 2023 DICE damage function (Barrage and Nordhaus, 2024[56]) represents a low-end estimate. The function is calibrated using an enumerative strategy and is widely used in integrated assessment models. As a middle-ground, the damage function from Howard and Sterner (2017[57]) is based on a meta-analysis of previous studies on the global impacts of climate change. At the higher end, a reduced form function calibrated around the findings of Bilal and Känzig (2026[58]) is employed. This function is based on econometric estimates of the effect of global temperature shocks on global GDP, using cross country data. The medium- and high-range damage curves were chosen to align to the OECD Long-Term Macroeconomic Model (LTM) (OECD, 2025[107]), which incorporates climate damages, also reflecting a range of estimates.
The three damage functions used in this report have the same functional form and express global climate damages () as the fraction of global output lost in year t relative to a no-warming scenario. The calculation of the global output loss relies on a reduced-form quadratic function of the global surface temperature anomaly () in year t compared to pre-industrial levels (1850-1900). For Howard and Sterner and DICE 2023 the single parameter in the global damage function is aligned with the author’s preferred specification from the respective publications. For the Bilal and Känzig damage function, the parameter from the most recent update of the OECD Long-Term Macroeconomic Model is employed (OECD, 2025[107]):
Howard and Sterner:
DICE 2023:
Bilal and Känzig:
As the modelling in this study only projects emissions until 2035, it is assumed that emission pathways consistent with the Enhanced Policies and Current Policies scenarios are maintained beyond 2035 and follow the ones of the IEA’s scenarios on which this report’s scenarios were calibrated to (IEA, 2023[48]).1 However, due to limited data availability for the IEA scenarios, temperature trajectories had to be approximated using the 2024 climate scenarios of the Network for Greening the Financial System (NGFS, 2024[59]). Specifically, temperature projections for the Enhanced Policies scenario are approximated using the median (50th) percentile of the temperature distribution estimated with the Model for the Assessment of Greenhouse Gas Induced Climate Change (MAGICC) climate model NGFS “Below 2°C” pathway. Likewise, projections for the Current Policies scenario are approximated using the NGFS “Fragmented World” pathway. Both approximations are chosen based on the alignment of the end of century temperatures with the projected temperature levels for the corresponding IEA WEO scenario.2
The disaggregation of global economic damages into region-level estimates for the three damage functions is further aligned with the OECD LTM (OECD, 2025[107]).The attribution rule is designed to meet two broad objectives: 1) individual-country damages aggregate up to the global damage function and 2) the cross-country distribution of damages relate to country-specific characteristics in a way consistent with the scientific literature. Country-specific damage factors are based on a corresponding reduced-form estimation from a meta-analysis of Tol (2024[106]), which suggests that most of the cross-country variance in economic damages from climate change can be reduced into two dimensions: i) current climate conditions and ii) national income levels. Subnational differences in impacts can be significant, but such regional differences could not be considered.