Preprints
https://doi.org/10.5194/egusphere-2026-3114
https://doi.org/10.5194/egusphere-2026-3114
11 Jun 2026
 | 11 Jun 2026
Status: this preprint is open for discussion and under review for Atmospheric Chemistry and Physics (ACP).

Quantifying Drivers of Tropospheric OH and Its Trends: Sensitivity to Atmospheric Processes and Implications for Methane Lifetime

Xuewei Hou, Ryan Hossaini, Oliver Wild, Andrea Mazzeo, Richard J. Pope, Ye Wang, Siyuan Wang, Yuanhong Zhao, James Lee, Bin Zhu, Tianliang Zhao, and Alok K. Pandey

Abstract. The hydroxyl radical (OH) is a critical determinant of global oxidative capacity and trace gas lifetimes, but its variation remains poorly constrained. This study investigates the sensitivity of modelled tropospheric OH concentration changes to physical and chemical processes using the FRSGC/UCI chemistry transport model. The simulated tropospheric O3 and NO2 agree well with satellite observations, but that annual variations in CO do not, likely due to uncertainties in biomass burning emissions in the southern hemisphere and overestimated CO trends over Asia. This discrepancy, along with the background increase in CO, may lead to an underestimation of OH increase or overestimation of OH decrease from 2000 to 2017. Changes in tropospheric OH column show substantial spatial heterogeneity, with increases in OH in high-emission regions and decreases in the tropics. Global mean OH trends are dependent on the assumed trend in emissions: with dynamic emissions there is little change in OH, while under annually invariant emissions, there is a substantial increase in OH due to meteorological conditions alone. Inclusion of water vapor UV absorption, heterogeneous reactions, and updates to the OH + NO2 reaction rate have a smaller impact on OH trend, but decrease OH levels by 3.6%, 5.8%, and 7.0%, respectively, increasing CH4 lifetimes by 4.2%, 5.2%, and 8.4%. Incorporating oceanic CH3CHO emissions reduces global mean OH by up to 1.5%, increasing the CH4 lifetime by up to 1.6%. These results provide a quantitative basis for understanding the drivers of tropospheric OH variability and their implications for global methane chemistry.

Competing interests: At least one of the (co-)authors is a member of the editorial board of Atmospheric Chemistry and Physics.

Publisher's note: Copernicus Publications remains neutral with regard to jurisdictional claims made in the text, published maps, institutional affiliations, or any other geographical representation in this paper. While Copernicus Publications makes every effort to include appropriate place names, the final responsibility lies with the authors. Views expressed in the text are those of the authors and do not necessarily reflect the views of the publisher.
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Xuewei Hou, Ryan Hossaini, Oliver Wild, Andrea Mazzeo, Richard J. Pope, Ye Wang, Siyuan Wang, Yuanhong Zhao, James Lee, Bin Zhu, Tianliang Zhao, and Alok K. Pandey

Status: open (until 23 Jul 2026)

Comment types: AC – author | RC – referee | CC – community | EC – editor | CEC – chief editor | : Report abuse
  • CC1: 'Data Provider Acknowledgement', Glenn Wolfe, 11 Jun 2026 reply
    • AC1: 'Reply on CC1', Xuewei Hou, 11 Jun 2026 reply
Xuewei Hou, Ryan Hossaini, Oliver Wild, Andrea Mazzeo, Richard J. Pope, Ye Wang, Siyuan Wang, Yuanhong Zhao, James Lee, Bin Zhu, Tianliang Zhao, and Alok K. Pandey
Xuewei Hou, Ryan Hossaini, Oliver Wild, Andrea Mazzeo, Richard J. Pope, Ye Wang, Siyuan Wang, Yuanhong Zhao, James Lee, Bin Zhu, Tianliang Zhao, and Alok K. Pandey
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Latest update: 11 Jun 2026
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Short summary
The atmosphere’s ability to remove pollutants and greenhouse gases is largely controlled by the hydroxyl radical, but the causes of its long-term changes remain uncertain. Using a global atmospheric model, we quantified the effects of emissions, weather, and key chemical processes on hydroxyl radical levels between 2000 and 2017. Our findings improve understanding of atmospheric self-cleansing and help reduce uncertainties in future climate assessments.
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