Articles | Volume 16, issue 4
https://doi.org/10.5194/bg-16-881-2019
© Author(s) 2019. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
https://doi.org/10.5194/bg-16-881-2019
© Author(s) 2019. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Research article
| 
22 Feb 2019
Research article |
| 22 Feb 2019
| 22 Feb 2019
The oceanic cycle of carbon monoxide and its emissions to the atmosphere
Ludivine Conte
CORRESPONDING AUTHOR
Laboratoire des Sciences du Climat et de l'Environnement, IPSL,
CEA/CNRS/UVSQ, Gif-sur-Yvette, 91191, France
Sophie Szopa
Laboratoire des Sciences du Climat et de l'Environnement, IPSL,
CEA/CNRS/UVSQ, Gif-sur-Yvette, 91191, France
Roland Séférian
Centre National de Recherches Météorologiques,
Météo-France/CNRS, Toulouse, 31057, France
Laurent Bopp
Laboratoire de Météorologie Dynamique, IPSL, Ecole Normale
Supérieure/PSL Research University, CNRS, Ecole Polytechnique,
Sorbonne Université, Paris, 75005, France
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- The response of aquatic ecosystems to the interactive effects of stratospheric ozone depletion, UV radiation, and climate change P. Neale et al. 10.1007/s43630-023-00370-z
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- Southern Hemisphere atmospheric history of carbon monoxide over the late Holocene reconstructed from multiple Antarctic ice archives X. Faïn et al. 10.5194/cp-19-2287-2023
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Latest update: 06 Nov 2024
Short summary
The ocean is a source of atmospheric carbon monoxide, a key component for the oxidizing capacity of the atmosphere. We use a global ocean biogeochemistry model to dynamically assess the oceanic CO budget and its emission to the atmosphere at the global scale. The total emissions of CO to the atmosphere are 4.0 Tg C yr−1. The oceanic CO emission maps produced are relevant for use by atmospheric chemical models, especially to study the oxidizing capacity of the atmosphere above the remote ocean.
The ocean is a source of atmospheric carbon monoxide, a key component for the oxidizing capacity...
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