Climate change and the macroeconomics of bank capital regulation

Layer 1 — Overview

Research Question

This paper asks two related questions about the intersection of climate policy and bank capital regulation. First, can differentiated bank capital requirements — imposing higher equity charges on loans to fossil energy firms — serve as a quantitatively meaningful climate policy instrument, in particular relative to carbon taxes? Second, how should optimal bank capital requirements respond to a carbon-tax-induced clean energy transition?

Methodology

The authors build a quantitative multi-sector DSGE model with two layers of default: corporate default at the firm level and bank failure at the bank level. Three intermediate goods sectors are modeled — non-energy, fossil energy, and clean energy — linked via a nested CES final-good production structure. Banks collect deposits from households (who value deposits for liquidity services) and issue defaultable loans to all three sectors. Deposit insurance, combined with limited liability for bank owners, generates an inefficiently high bank risk-taking motive, creating a role for capital regulation. The Ramsey-optimal capital requirement balances the social benefit of liquid deposit provision to households against the social cost of bank failure.

The model is calibrated to quarterly data, targeting a 0.7% annualized bank failure rate, a 2% annualized corporate default rate, a 30% loan recovery rate, a deposit spread of -100 basis points, and a baseline Ramsey-optimal equity requirement of 8% (consistent with Basel III). Sectoral parameters follow Bartocci, Notarpietro, and Pisani (2022) and Fried, Novan, and Peterman (2022): the energy-to-non-energy elasticity of substitution is 0.2, the clean-to-fossil energy elasticity is 3, and full abatement occurs at carbon taxes exceeding 125 $/tonne of carbon (ToC). The clean transition experiment imposes a linear carbon tax path from zero to 10 $/ToC over 40 quarters, announced as an unanticipated but fully credible shock.

Main Findings

Finding 1 — Fossil-penalizing capital requirements are quantitatively negligible as climate policy. Raising the capital requirement on fossil loans from the baseline 8% to 12% (a 150% risk-weight, consistent with current BB- treatment) reduces the fossil capital share within the energy sector by only 0.06 percentage points (from 80.00% to 79.94%) and cuts aggregate emissions by only 0.08%. A 1 $/ToC carbon tax, by contrast, achieves a 5.23% emission reduction while modestly reducing the fossil capital share to 79.80%. The difference arises because capital requirements affect only the size and financing cost of fossil firms, leaving abatement incentives unchanged; the loan-rate effect on fossil firms is small (loan rate rises from 124 bps to 128 bps), consistent with Kashyap, Stein, and Hanson (2010).

Finding 2 — Sustainability-linked capital requirements remain insufficient. Conditioning the fossil capital requirement on firms’ abatement effort (κ_f = 0.12 − η_t) induces an optimal abatement effort of 2.69% and an effective fossil requirement of approximately 9.5%. The implied emission reduction remains far below even a modest carbon tax: the authors state the induced emission reduction falls short by a factor of almost 100 relative to full abatement.

Finding 3 — Ramsey-optimal capital requirements decline monotonically along the transition (in the baseline real model). When a carbon tax gradually rises from zero to 10 $/ToC over 40 quarters, aggregate loan demand contracts permanently because clean, fossil, and non-energy goods are imperfect substitutes and the shock is recessionary for GDP. Banks reduce balance sheets, deposit supply falls, the deposit spread widens by approximately 8 basis points in the long run, and corporate default rates across all sectors rise by almost 0.1 percentage points from the baseline of 2.05% (in steady state). To counteract the deposit scarcity and associated firm risk-taking, the Ramsey-optimal capital requirement declines symmetrically and monotonically to a lower long-run level. Bank capital regulation cannot affect impact default rates because leverage decisions are made before the transition is announced.

Finding 4 — Nominal rigidities produce a temporary tightening before the long-run relaxation. When debt is denominated in nominal terms and Rotemberg price adjustment costs are added, the clean transition is inflationary in the short run (consistent with Ciccarelli and Marotta 2021). Inflation makes deposit financing more attractive, inducing firms to temporarily increase nominal loan issuance; real deposits rise briefly, the deposit spread narrows by around 2 basis points, and the optimal capital requirement tightens over the initial phase of the transition before converging to the same lenient long-run level as the baseline. The short-run tightening is followed by a permanent relaxation.

Finding 5 — Differentiated sector-specific capital requirements are only warranted when banks are not diversified across sectors. In the baseline, perfectly diversified banks face a symmetric aggregate loan demand contraction, so uniform adjustment suffices. When sector-specific banks are introduced (an extreme case meant to bound concentration effects), fossil banks experience a strong reduction in deposit supply while clean banks experience the opposite. The optimal response is temporarily tighter capital requirements for clean banks and relaxed requirements for fossil banks. In the long run, both converge to an aggregate risk-weight of approximately 99.85% relative to the baseline (a small but symmetric relaxation), very close to the diversified baseline.

Scope Conditions

All results are derived within a model calibrated to match broad financial-market and macroeconomic regularities rather than a specific country. Physical risk from climate change is abstracted away throughout. The carbon tax is set exogenously (not derived from a climate policy optimum). Firms cannot switch technologies, providing a conservative lower bound on the sectoral reallocation. Results are robust to halving the deposit demand elasticity parameter (γ_D = 0.6 versus 1.5 in the baseline) and to raising the energy/non-energy substitution elasticity to 3 from 0.2.

Layer 2 — Q&A

Q1: What is the core trade-off that determines the optimal level of bank capital requirements in this model?

A: The optimal capital requirement balances two welfare-relevant effects of bank leverage. Tighter requirements reduce bank failure rates, limiting the resource losses (proportional to deposits under DIA management) and the inefficient risk-taking that deposit insurance induces. At the same time, tighter requirements force banks to reduce deposit-financed lending, shrinking the supply of liquid deposits that households value directly in utility. The Ramsey planner chooses the capital requirement that equates the marginal welfare benefit of lower bank failure against the marginal welfare cost of reduced deposit provision. In the baseline calibration this optimum is at 8%.

Q2: Why does raising capital requirements on fossil loans have such a small effect on carbon emissions?

A: Capital requirements affect the deposit-financing wedge for fossil loans — the share of loans that can be funded via cheap, deposit-financed sources — but they do not enter firms’ first-order condition for abatement. Firms respond by modestly reducing leverage and investment (the loan rate for fossil energy firms rises from 124 bps to 128 bps), but the emission intensity of fossil production is unchanged. In equilibrium, the fossil capital share within the energy sector declines by only 0.06 percentage points (from 80.00% to 79.94%), reducing total emissions by 0.08%. A 1 $/ToC carbon tax produces a 5.23% emission reduction, many times larger, because carbon taxes directly alter the return to abatement and the profitability of fossil relative to clean production.

Q3: How does the sustainability-linked capital requirement work and why is it still insufficient?

A: Under sustainability-linked capital requirements, the fossil loan charge is set as κ_f = κ̃ − η_t, so firms that abate more face lower capital requirements on their loans and thus lower financing costs. This creates a direct financial incentive for abatement that the simple penalizing factor lacks. With κ̃ = 0.12, the equilibrium abatement effort is 2.69% and the effective fossil requirement falls to approximately 9.5%. Despite this improvement relative to the plain fossil factor, the climate impact remains far smaller than even a modest carbon tax: the induced emission reduction falls short by a factor of almost 100 relative to full abatement. The fundamental limitation is that the feedback from abatement to financing cost is attenuated by deposit-financing wedge mechanics, making the instrument too weak to substitute for direct carbon pricing.

Q4: What are the impact, short-run, and long-run effects of the clean transition on default rates and bank failure?

A: On impact, the unexpected compliance cost increase raises fossil firms’ default threshold, causing a sharp but short-lived uptick in fossil firm default rates (from 2.05% to approximately 2.08% in the baseline transition) and a brief increase in bank failure. Clean firm defaults fall slightly on impact due to higher clean energy prices. In the short run, clean firms increase risk-taking (higher leverage) because the relative attractiveness of debt financing improves as deposit spreads widen; fossil firms deleverage. In the long run, aggregate corporate default rates rise by almost 0.1 percentage points from the baseline of 2.05% (equivalently 2.7% in the Appendix B long-run analysis), driven by the widening of the deposit spread (approximately 8 bps), which raises the deposit financing wedge for all firms. Bank failure rates are always tied to binding capital requirements and revert quickly to their steady-state level.

Q5: Why can bank capital regulation not mitigate the impact default spike when the transition is announced?

A: At the moment of announcement, leverage decisions for the current period have already been made. The bank capital requirement binds on new lending decisions but cannot alter the existing capital structure of banks or firms. Therefore the regulator faces a “bygone” on impact: changing the capital requirement in the announcement period does not affect current corporate default rates or bank failure rates. The regulator’s tool only becomes effective for lending decisions going forward, implying that the transition-induced impact default surge cannot be smoothed by macroprudential policy.

Q6: Why do Ramsey-optimal capital requirements decline along the transition rather than tighten to address higher default risk?

A: The key channel is that aggregate loan demand contracts permanently as imperfect substitutability across sectors makes the carbon tax recessionary. Banks shrink their balance sheets, reducing deposit supply. The resulting deposit scarcity makes deposits more valuable to households (widening the spread), which also makes deposit financing cheaper for banks, partially offsetting the loan demand decline but at the cost of higher corporate leverage. The welfare loss from reduced liquidity provision and higher firm default rates dominates, so the planner relaxes capital requirements to stimulate deposit supply. The dominant effect is the large, permanent decline in credit demand, which makes it welfare-improving to allow banks to operate at lower capital ratios to rebuild deposit provision.

Q7: What is the role of the deposit financing wedge in transmitting carbon tax shocks to the entire corporate sector?

A: The deposit financing wedge (Ξ_t) reflects the benefit for banks of funding loans through deposits rather than equity, combining the liquidity premium households pay on deposits and the deposit insurance put (expected repayment is only 1 − F(μ_{t+1}) per unit of deposits issued). When aggregate loan demand falls due to carbon taxes, deposits become scarcer relative to their steady-state level, making the wedge larger. Through the loan pricing condition, all sectors — not just fossil — face more attractive deposit-financed debt, causing clean and non-energy firms to also increase their leverage and default risk along the transition. This is the mechanism through which a sector-specific shock has symmetric aggregate effects that shape optimal bank regulation.

Q8: How do nominal rigidities change the optimal path of capital requirements along the clean transition?

A: With Rotemberg price adjustment costs and nominally denominated debt, the clean transition is inflationary in the short run (consistent with empirical evidence in Ciccarelli and Marotta 2021). Inflation lowers the real value of outstanding nominal loan obligations, incentivizing firms across all sectors to temporarily increase nominal borrowing. Banks accommodate this demand by increasing deposit issuance, which briefly narrows the deposit spread by around 2 basis points. With deposit supply temporarily elevated, the regulator’s trade-off tilts toward reducing bank failure rather than stimulating deposit provision, so optimal capital requirements tighten during the inflationary phase before reverting to the lenient long-run path of the baseline model. The long-run level is unchanged.

Q9: Under what conditions are sector-specific capital requirements welfare-improving?

A: Sector-specific requirements are only welfare-improving when banks are not perfectly diversified across sectors, so that the transition has heterogeneous effects on sector-specific deposit supply and bank failure rates. In the baseline with perfectly diversified banks, the loan demand decline affects all banks uniformly, so a symmetric uniform adjustment is optimal. When sector-specific banks are introduced as an extreme case of carbon concentration, fossil banks experience a sharp reduction in deposit provision while clean banks see deposits temporarily increase. The planner responds by temporarily relaxing requirements for fossil banks and tightening them for clean banks. In the long run, both converge to approximately the same aggregate relaxation as the diversified baseline (aggregate risk-weight of 99.85%).

Q10: How does the carbon tax shock experiment relate to the perfect-foresight transition analysis?

A: In the carbon tax shock experiment, the tax level follows an AR(1) process with persistence ρ_τ = 0.9, starting from a long-run level of 10 $/ToC, with a one-standard-deviation shock implying an additional 10 $/ToC on impact. Fossil firm default rates spike from 2% to approximately 2.8% on impact and revert relatively quickly. Emissions decline by slightly more than 10% on impact and revert as the shock dissipates. The macroeconomic dynamics — GDP, investment, loan demand, and bank failure rate responses — closely resemble the impact and short-run effects of the perfect-foresight transition. Optimal capital requirements decline temporarily in both cases, confirming that the transition-path results are not an artifact of the specific perfect-foresight assumption.

Q11: What is the “forced safety effect” and how does it interact with the model’s capital requirement trade-off?

A: The “forced safety effect” (following Bahaj and Malherbe 2020) refers to the positive effect of tighter capital requirements on loan supply that operates through reducing bank failure probability. When banks are less likely to fail (lower F(μ_{t+1})), the expected bank productivity conditional on not failing — (1 − G(μ_{t+1})) — rises toward one, reducing the discount applied to future loan payoffs in the bank’s stochastic discount factor. This improves the profitability of lending and expands loan supply. In the model, this effect partially offsets the direct loan-supply reduction from higher equity requirements but does not dominate, so the overall effect of tighter requirements on deposit supply is still negative, preserving the core trade-off.

Q12: What robustness checks are performed and do they materially change the main results?

A: The authors consider three main robustness checks. First, reducing the deposit demand elasticity parameter from γ_D = 1.5 to γ_D = 0.6 (recalibrating ω_D = 0.012 to preserve the -100 bp deposit spread target) has almost no effect on the optimal path of capital requirements. Second, raising the energy/non-energy substitution elasticity from ε̃ = 0.2 to ε̃ = 3 (and adjusting the energy weight to maintain a 10% energy share) produces much stronger fossil investment declines and smaller clean investment responses, but aggregate loan demand and bank deposits contract only slightly less, so the relaxation in capital requirements is slightly smaller than in the baseline. Third, recalibrating to a 2% annualized bank failure rate (versus the baseline 0.7%) does not materially change results. The conclusion that capital requirements should decline along the transition is robust across all specifications.

Key Concepts

Deposit financing wedge (Ξ_t): The gain for banks from funding loans via deposits rather than equity. It comprises two components: (i) the liquidity premium — households value deposits for their liquidity services, so the deposit rate lies below the risk-free rate; and (ii) the deposit insurance put — the expected repayment obligation per unit of deposits is only 1 − F(μ_{t+1}), not one, since the DIA covers depositors in the event of bank failure. A larger wedge makes deposit-financed lending more profitable, expanding loan supply. In this paper the wedge is the central transmission mechanism through which capital requirements and aggregate loan demand interact.

Bank failure threshold (μ_t): The realization of the bank-specific idiosyncratic risk shock below which a bank cannot service depositors and transfers all assets and liabilities to the deposit insurance agency. It depends on the ratio of deposit repayment obligations to the aggregate realized loan portfolio return. In the model the threshold increases when aggregate loan payoffs fall (as in a carbon tax shock), temporarily raising bank failure rates.

Ramsey-optimal capital requirement: The sequence of sector-specific (or uniform) capital ratios chosen by a benevolent government planner to maximize household welfare, treating the capital requirement as the sole policy instrument. In this model the Ramsey problem is solved nonlinearly along the perfect-foresight transition path. The planner internalizes that tighter requirements simultaneously reduce bank failure probability and shrink deposit supply; the optimum trades off these two objectives.

Sustainability-linked capital requirement: A capital requirement on fossil loans that explicitly depends on the abatement effort undertaken by fossil firms (κ_f = κ̃ − η_t), creating a direct financing-cost incentive for emission reduction. This contrasts with a plain fossil penalizing factor, which affects only the financing cost of fossil capital without altering abatement incentives. The paper shows that even sustainability-linked requirements are quantitatively negligible as climate policy relative to carbon taxes.

Carbon compliance cost per unit of fossil production (ξ_t): A summary statistic combining the direct carbon tax payment and the abatement cost at the optimal abatement effort. It measures the total policy-induced wedge that reduces the profitability of fossil capital and raises fossil firms’ break-even default threshold. In the transition experiment, compliance costs rise from zero to approximately 4% of fossil production value as the tax increases from 0 to 10 $/ToC.

Asset stranding channel: The mechanism through which an unanticipated tightening of carbon policy raises fossil firms’ default probability on impact (by increasing compliance costs above the level priced into existing loan contracts) and subsequently reduces their loan demand permanently. The paper contrasts its treatment of this channel — where stranding affects bank regulation through aggregate deposit supply effects — against models (such as Carattini, Melkadze, and Heutel 2023) where stranding causes an inefficient credit crunch via a financial accelerator.

Deposit spread (s^D_t): Defined as the annualized difference between the deposit rate and the risk-free rate, expressed in basis points. Because households value deposits for liquidity services, the deposit rate lies permanently below the risk-free rate (spread is negative). In the baseline calibration the target is -100 bps. The spread widens (becomes less negative) when deposits become scarcer, which is the case along the carbon tax transition as bank balance sheets contract.