Observationally Constrained NO <sub>x</sub> ‐Catalyzed Ozone Production in the Upper Troposphere During the Asian Summer Monsoon

Abstract Intense and frequent convection occurring during the Asian Summer Monsoon (ASM) rapidly transports surface emissions to the upper troposphere (UT). Depending on their chemical reactivities, pollutants transported to the UT via this mechanism may either undergo chemistry in the UT region or be transported into the lower stratosphere. The Asian Summer Monsoon Chemical and CLimate Impact Project (ACCLIP) used high‐altitude research aircraft to characterize chemistry in the tropopause region within the ASM anticyclone and outflows of monsoon convection during summer 2022. Here, we use measurements of trace gases from ACCLIP and results from a 0‐D model constrained by airborne observations to calculate net ozone production rates in airmasses influenced by recent convection and in the summer monsoon background upper troposphere/lower stratospheric air. We find that ozone production inside the polluted air downstream of recent convection is up to one order of magnitude higher than that in the cleaner background upper troposphere. The ozone production is driven by NO + HO 2 produced from CO and OVOC oxidation, rather than from organic peroxy radicals produced from volatile organic compounds inside the highly polluted airmasses. Consistent with previous modeling work, we find efficient HO x (OH + HO 2 ) cycling is dominated by reactions with CO. Ozone production in this region is primarily NO x ‐limited and increases with higher NO x such as during convective events with lightning NO x production. Further, we find that the dominant impact of enhanced NO x here is through acceleration of HO x cycling, and thus an increase in ozone production.

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Publication Details

Journal
Journal of Geophysical Research Atmospheres
Published
2025-10-04
DOI
https://doi.org/10.1029/2024jd043218
Citations
1
Primary Topic
Atmospheric chemistry and aerosols
Type
article
Field-Weighted Citation Impact
1.30
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article

Observationally Constrained NO x ‐Catalyzed Ozone Production in the Upper Troposphere During the Asian Summer Monsoon

Charles K. Gatebe, Silvia Viciani, R. Hendershot, Colin Gurganus et al.
1 citations
Journal of Geophysical Research Atmospheres
Atmospheric chemistry and aerosols
1.30
article

Observationally Constrained NO x ‐Catalyzed Ozone Production in the Upper Troposphere During the Asian Summer Monsoon

Charles K. Gatebe, Silvia Viciani, R. Hendershot, Colin Gurganus, S. Schauffler, Victoria Treadaway, M. Barucci, E. Atlas, Katie Smith, Laura L. Pan, Gordon A. Novak, Laura T. Iraci, Jason M. St. Clair, T. P. Bui, Jonathan M. Dean‐Day, R. Lueb, Glenn M. Wolfe, Joshua P. DiGangi, Glenn S. Diskin, Daniel C. Anderson, T. Campos, Erin R. Delaria, Giovanni Bianchini, Andrew W. Rollins, Troy Thornberry, James R. Podolske, Francesco D’Amato, Yonghoon Choi, R. S. Gao, Eleanor M. Waxman, R. P. McLaughlin
article en
1 citations

Abstract

Abstract Intense and frequent convection occurring during the Asian Summer Monsoon (ASM) rapidly transports surface emissions to the upper troposphere (UT). Depending on their chemical reactivities, pollutants transported to the UT via this mechanism may either undergo chemistry in the UT region or be transported into the lower stratosphere. The Asian Summer Monsoon Chemical and CLimate Impact Project (ACCLIP) used high‐altitude research aircraft to characterize chemistry in the tropopause region within the ASM anticyclone and outflows of monsoon convection during summer 2022. Here, we use measurements of trace gases from ACCLIP and results from a 0‐D model constrained by airborne observations to calculate net ozone production rates in airmasses influenced by recent convection and in the summer monsoon background upper troposphere/lower stratospheric air. We find that ozone production inside the polluted air downstream of recent convection is up to one order of magnitude higher than that in the cleaner background upper troposphere. The ozone production is driven by NO + HO 2 produced from CO and OVOC oxidation, rather than from organic peroxy radicals produced from volatile organic compounds inside the highly polluted airmasses. Consistent with previous modeling work, we find efficient HO x (OH + HO 2 ) cycling is dominated by reactions with CO. Ozone production in this region is primarily NO x ‐limited and increases with higher NO x such as during convective events with lightning NO x production. Further, we find that the dominant impact of enhanced NO x here is through acceleration of HO x cycling, and thus an increase in ozone production.

Journal of Geophysical Research AtmospheresVol. 130(19)
NSF National Center for Atmospheric Research (US), Ames Research Center (US), Goddard Space Flight Center (US), Langley Research Center (US), University of Miami (US), Cooperative Institute for Research in Environmental Sciences (US), University of Colorado Boulder (US), Bay Area Environmental Research Institute (US), NOAA Chemical Sciences Laboratory (US), National Research Council (IT), University of Maryland, Baltimore County (US)
Openalex Percentile: Top 17%
Atmospheric chemistry and aerosols
1.30
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