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<p>Since the 1970s, air pollutant emissions controls in the United States (US) have lowered concentrations of ozone (O<sub>3</sub>) and aerosols, which have opposing radiative effects on surface temperature. Using a pair of initial-condition ensembles generated by a fully-coupled chemistry-climate model, we simulate the “world avoided” by US air pollution controls. In this counterfactual world, we find tropospheric column O<sub>3</sub> increases, robust to natural internal variability, extending across the Northern Hemisphere. Robust aerosol increases, dominated by sulfate, remain localized near the US. Wintertime Northwest Atlantic cloud droplet number concentration is particularly sensitive to US aerosol. While an ensemble mean US surface cooling signal (−0.4 °C) implies that aerosol-driven cooling prevails over any O<sub>3</sub>-induced warming, we find that large regional internal variability will confound its detection in any single transient realization. Larger signal-to-noise ratios for composition versus climate variables underscore the greater detectability of emissions-driven changes in tropospheric composition compared to their associated climate impacts.</p>

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Detecting tropospheric composition and climate responses to US air pollution controls in the context of internally-arising variability

  • 期刊论文

  • 出版模式：

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  • 发表日期：

    2025年7月1日

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  • Stephanie Elkins,
  • Arlene M. Fiore,
  • Gustavo P. Correa,
  • Jean-François Lamarque,
  • Steven J. Smith,
  • Vaishali Naik,
  • Yangyang Xu

摘要

Since the 1970s, air pollutant emissions controls in the United States (US) have lowered concentrations of ozone (O3) and aerosols, which have opposing radiative effects on surface temperature. Using a pair of initial-condition ensembles generated by a fully-coupled chemistry-climate model, we simulate the “world avoided” by US air pollution controls. In this counterfactual world, we find tropospheric column O3 increases, robust to natural internal variability, extending across the Northern Hemisphere. Robust aerosol increases, dominated by sulfate, remain localized near the US. Wintertime Northwest Atlantic cloud droplet number concentration is particularly sensitive to US aerosol. While an ensemble mean US surface cooling signal (−0.4 °C) implies that aerosol-driven cooling prevails over any O3-induced warming, we find that large regional internal variability will confound its detection in any single transient realization. Larger signal-to-noise ratios for composition versus climate variables underscore the greater detectability of emissions-driven changes in tropospheric composition compared to their associated climate impacts.