Articles | Volume 26, issue 16
https://doi.org/10.5194/acp-26-11857-2026
© Author(s) 2026. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
https://doi.org/10.5194/acp-26-11857-2026
© Author(s) 2026. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Impact of South American biomass burning emissions on elevated South Atlantic upper tropospheric ozone
Linda Smoydzin
CORRESPONDING AUTHOR
Institute for Atmospheric Physics, Johannes Gutenberg University, Mainz, Germany
Vera Bense
Institute for Atmospheric Physics, Johannes Gutenberg University, Mainz, Germany
Heiko Bozem
Institute for Atmospheric Physics, Johannes Gutenberg University, Mainz, Germany
Philipp Joppe
Institute for Atmospheric Physics, Johannes Gutenberg University, Mainz, Germany
Aerosol Chemistry Department, Max Planck Institute for Chemistry, Mainz, Germany
Daniel Kunkel
Institute for Atmospheric Physics, Johannes Gutenberg University, Mainz, Germany
Hans-Christoph Lachnitt
Institute for Atmospheric Physics, Johannes Gutenberg University, Mainz, Germany
Holger Tost
Institute for Atmospheric Physics, Johannes Gutenberg University, Mainz, Germany
Andreas Zahn
Karlsruhe Institute of Technology, Institute of Meteorology and Climate Research (IMK) Karlsruhe, German
Helmut Ziereis
Institut für Physik der Atmosphäre, Deutsches Zentrum für Luft- und Raumfahrt (DLR), Oberpfaffenhofen, Germany
Martin Riese
Institute for Climate and Energy Systems (ICE-4), Forschungszentrum Jülich, Germany
Peter Hoor
Institute for Atmospheric Physics, Johannes Gutenberg University, Mainz, Germany
Model code and software
Massive-Parallel Trajectory Calculations (MPTRAC) (Version v2.6) L. Hoffmann et al. https://doi.org/10.5281/zenodo.10067751
Short summary
During a research flight in early October elevated upper tropospheric mixing ratios of CO, NO, NOy and O3 were observed over a distance of more than 1000 km east of the Brasilian coast. Ozone mixing ratios are 20–40 ppbv higher than during a flight in early September. By combining aircraft observations with model simulations we find that ozone production from biomass burning over Amazonia caused predominantly the ozone enhancements which have a local effect on the radiative forcing of 50 mW m−2.
During a research flight in early October elevated upper tropospheric mixing ratios of CO, NO,...
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