Preprints
https://doi.org/10.5194/egusphere-2026-1652
https://doi.org/10.5194/egusphere-2026-1652
13 May 2026
 | 13 May 2026
Status: this preprint is open for discussion and under review for Atmospheric Chemistry and Physics (ACP).

Assessment of the impact of tropical anthropogenic and biomass-burning emissions on tropospheric ozone (2007–2021) using the GEOS-Chem model constrained by satellite observations

Herizo Narivelo, Bastien Sauvage, Klaas Folkert Boersma, Isabelle De Smedt, Isidora Anglou, Michel Van Roozendael, Eric Le Flochmoën, and Brice Barret

Abstract. Ozone (O3) is a secondary species formed and is considered a hazardous pollutant in the troposphere. Over the recent decades, tropospheric O3 has undergone significant regional variations. This paper focuses on the impact of the evolution of anthropogenic and biomass-burning emissions in the tropics upon tropospheric and the chemical regimes of O3 using numerical simulations performed of the last 15-years with the GEOS-Chem model. Satellite datasets derived from OMI (HCHO and NO2) and IASI-SOFRID (CO and O3) are used as observational constraints to ensure the most reliable representation of BB and ANT emissions. The results show that the simulation (REF) combining GFAS for BB and CAMS for ANT emission provides the best match with the selected satellite observations.

The analysis of REF-simulation shows that positive trends in tropospheric ozone column (TOC) are observed mainly in the Northern Hemisphere, in Asia regions, Temperate North America, Europe, and some tropical regions (Equatorial Asia and Southern Hemisphere South America), driven by increased of ANT and BB emissions and favourable photochemical conditions.

Sensitivity tests with fixing emissions in the tropical band, reveal that the increase in tropical TOC is mainly due to tropical ANT emissions, which occur in chemical regimes nd: transparent by VOC-limited. Further results highlight that effective mitigation of future increases in TOC will depend mostly on control of ANT NOx emissions in tropical regions, where chemical conditions favour high O3 production, while underlying the marginal role of BB in moderating regional O3 levels.

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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Herizo Narivelo, Bastien Sauvage, Klaas Folkert Boersma, Isabelle De Smedt, Isidora Anglou, Michel Van Roozendael, Eric Le Flochmoën, and Brice Barret

Status: open (until 24 Jun 2026)

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Herizo Narivelo, Bastien Sauvage, Klaas Folkert Boersma, Isabelle De Smedt, Isidora Anglou, Michel Van Roozendael, Eric Le Flochmoën, and Brice Barret
Herizo Narivelo, Bastien Sauvage, Klaas Folkert Boersma, Isabelle De Smedt, Isidora Anglou, Michel Van Roozendael, Eric Le Flochmoën, and Brice Barret
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Short summary
Tropospheric ozone is a key component of air pollution; it is produced by the photochemical oxidation of volatile organic compounds in the presence of nitrogen oxides. Using satellite observations, we determine the best combination of emission inventories for biomass-burning and anthropogenic sources, we analyse the impact of the evolution of two surface emissions in tropics on tropospheric ozone and its chemical regime, using numerical simulations over the last few decades.
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