Abstract

Abstract. Projections of future atmospheric composition change and its impacts on air quality and climate depend heavily on chemistry–climate models that allow us to investigate the effects of changing emissions and meteorology. These models are imperfect as they rely on our understanding of the chemical, physical and dynamical processes governing atmospheric composition, on the approximations needed to represent these numerically, and on the limitations of the observations required to constrain them. Model intercomparison studies show substantial diversity in results that reflect underlying uncertainties, but little progress has been made in explaining the causes of this or in identifying the weaknesses in process understanding or representation that could lead to improved models and to better scientific understanding. Global sensitivity analysis provides a valuable method of identifying and quantifying the main causes of diversity in current models. For the first time, we apply Gaussian process emulation with three independent global chemistry-transport models to quantify the sensitivity of ozone and hydroxyl radicals (OH) to important climate-relevant variables, poorly characterised processes and uncertain emissions. We show a clear sensitivity of tropospheric ozone to atmospheric humidity and precursor emissions which is similar for the models, but find large differences between models for methane lifetime, highlighting substantial differences in the sensitivity of OH to primary and secondary production. This approach allows us to identify key areas where model improvements are required while providing valuable new insight into the processes driving tropospheric composition change.

Highlights

  • Atmospheric photochemistry and transport processes play important roles in the Earth system by controlling the impact of natural and anthropogenic trace gas emissions on air quality and global climate

  • The atmospheric abundance of both gases has increased substantially due to anthropogenic activity, and their fates are strongly coupled through the short-lived hydroxyl (OH) radical

  • Global sensitivity analysis provides a valuable approach to determine the major drivers of model behaviour, and it has been applied to atmospheric chemistry schemes to explore uncertainties in tropospheric O3 (Derwent and Murrells, 2013; Christian et al, 2017; Ridley et al, 2017; Newsome and Evans, 2017)

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Summary

Introduction

Atmospheric photochemistry and transport processes play important roles in the Earth system by controlling the impact of natural and anthropogenic trace gas emissions on air quality and global climate. Models have difficulty reproducing recent observed trends in surface O3 driven by changes in precursor emissions, natural sources, stratospheric influx and transport patterns (Parrish et al, 2014) This is a major concern because changes in the tropospheric abundance of O3 influence our assessment of radiative forcing and the attainment of air quality objectives on regional and urban scales Global sensitivity analysis provides a valuable approach to determine the major drivers of model behaviour, and it has been applied to atmospheric chemistry schemes to explore uncertainties in tropospheric O3 (Derwent and Murrells, 2013; Christian et al, 2017; Ridley et al, 2017; Newsome and Evans, 2017). We investigate how the sensitivities differ across three independent chemistry-transport models and demonstrate how this approach may be used to explore the diversity in model responses and to identify where model results differ

Approach
Model responses and contributions to variance
Investigating model differences
Findings
Conclusions
Full Text
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