Articles | Volume 16, issue 19
https://doi.org/10.5194/acp-16-12477-2016
© Author(s) 2016. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
https://doi.org/10.5194/acp-16-12477-2016
© Author(s) 2016. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
Global tropospheric hydroxyl distribution, budget and reactivity
Max Planck Institute for Chemistry, Atmospheric Chemistry Department,
P.O. Box 3060, 55020 Mainz, Germany
Sergey Gromov
Max Planck Institute for Chemistry, Atmospheric Chemistry Department,
P.O. Box 3060, 55020 Mainz, Germany
Andrea Pozzer
Max Planck Institute for Chemistry, Atmospheric Chemistry Department,
P.O. Box 3060, 55020 Mainz, Germany
Domenico Taraborrelli
Max Planck Institute for Chemistry, Atmospheric Chemistry Department,
P.O. Box 3060, 55020 Mainz, Germany
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Latest update: 05 Oct 2024
Short summary
The self-cleaning capacity of the atmosphere is controlled by hydroxyl (OH) radicals in the troposphere. There are primary and secondary OH sources, the former through the photodissociation of ozone, the latter through OH recycling. We used a global model, showing that secondary sources are larger than assumed previously, which buffers OH. Complementary OH formation mechanisms in pristine and polluted environments, connected through transport of ozone, can maintain stable global OH levels.
The self-cleaning capacity of the atmosphere is controlled by hydroxyl (OH) radicals in the...
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