Atmospheric Chemistry and Meteorological Controls on Air Quality Response to Emission Reductions: Insights from China and the United States

Author(s)
Zhao, Fanghe
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Abstract
The effectiveness of emission control strategies for mitigating air pollution depends critically on the complex interactions between anthropogenic emissions, atmospheric chemistry, and meteorological conditions. This dissertation investigates these interactions through comprehensive observational and modeling studies in China and the United States, revealing fundamental constraints on the efficacy of emission reduction policies and providing new insights for air quality management. Field measurements in the North China Plain reveal that springtime surface ozone concentrations exceed those in California by 50% despite similar meteorological conditions. Analysis of aromatic volatile organic compounds (VOCs) shows ARO2 and ARO1 concentrations 7.42 and 5.23 times higher than California levels, respectively. Box model calculations with the Master Chemical Mechanism demonstrate that aromatics contribute 73% of total ozone production, with ARO1 alone accounting for 62.8%. The implementation of observation-constrained emission redistribution based on industrial source patterns fundamentally shifts the regional chemical regime from VOC-limited to transitional conditions. The revised emission inventory correlates strongly with satellite-observed glyoxal columns, providing independent validation and highlighting the critical importance of accurate industrial emission characterization for ozone pollution assessment. A decade-long analysis (2015-2024) of China's Spring Festival, characterized by consistent 30-50% NOₓ reductions, reveals an unexpected shift in atmospheric oxidant response. The oxidant response (ΔOx = ΔO₃ + ΔNO₂) to identical emission reduction patterns has transitioned from negative to positive values over this period. Chemical transport modeling successfully reproduces these trends with correlation coefficients of 0.65-0.80 across regions. Machine learning analysis identifies cloud cover and subsequent radiation changes as primary drivers, yielding robust correlations (R = 0.85-0.94) between normalized ΔOx and meteorological parameters. These findings demonstrate that meteorological variability can fundamentally override the expected chemical responses to emission reductions. Long-term analysis of SO₂ emission controls in the United States (2004-2023) reveals declining wintertime control efficacy despite successful implementation of coal-to-gas transitions in power generation. While SO₂ and sulfate concentrations decreased significantly in both the Rust Belt and Southeast regions, wintertime sulfate fractions increased from ~40% to 55-60%, contrasting with stable summer values of ~65%. This seasonal divergence manifests as slower sulfate decreases during 2004-2013 compared to 2013-2023, despite greater SO₂ reductions in the earlier period. The analysis attributes this diminishing effectiveness to enhanced SO₂ oxidation efficiency as atmospheric conditions transition from SO₂-saturated to oxidant-limited regimes. This chemical damping effect, driven by limited H₂O₂ availability, represents a fundamental constraint on the benefits of continued emission reductions. High-resolution inverse modeling of TROPOMI NO₂ observations during the COVID-19 lockdown reveals complex and counterintuitive emission patterns. Despite widespread reports of emission decreases and reduced economic activity, analysis shows 25% NOₓ emission increases over the Jiang-Han Plain region, specifically along supply routes to locked-down cities. Post-lockdown recovery patterns demonstrate rapid emission rebounds in northern Jiangsu and Fujian provinces, areas characterized by high concentrations of small-scale enterprises. These differential recovery rates between large and small businesses highlight the heterogeneous nature of emission sources and the importance of maintaining essential supply chains during disruption events. This research advances atmospheric chemistry understanding through quantification of aromatic VOC contributions to ozone production, demonstration of meteorological controls on emission reduction effectiveness, identification of chemical limitations in long-term control efficacy, and revelation of unexpected emission behaviors during socioeconomic disruptions. The findings collectively challenge the conventional linear relationship assumed between emission reductions and air quality improvements. Successful air quality management requires dynamic, observation-constrained frameworks that account for chemical regime transitions, meteorological variability, and non-linear atmospheric responses. The implications extend beyond regional air quality to global atmospheric chemistry and climate policy. As nations implement increasingly stringent emission controls, the diminishing returns identified in this work will become more prevalent, requiring adaptive strategies that consider both chemical saturation effects and meteorological influences. The research underscores the necessity of high-resolution monitoring networks capable of capturing fine-scale emission variations and atmospheric responses. Future air quality management must evolve from static, prescriptive approaches to dynamic systems that integrate real-time observations, advanced modeling capabilities, and machine learning techniques to predict and respond to changing atmospheric conditions. Only through such comprehensive, scientifically informed strategies can we effectively address the persistent challenge of air pollution in an era of rapid industrialization and climate change.
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Date
2025-08-13
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Dissertation (PhD)
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