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ACP | Articles | Volume 19, issue 15
Atmos. Chem. Phys., 19, 10161–10190, 2019
https://doi.org/10.5194/acp-19-10161-2019
© Author(s) 2019. This work is distributed under
the Creative Commons Attribution 4.0 License.
Atmos. Chem. Phys., 19, 10161–10190, 2019
https://doi.org/10.5194/acp-19-10161-2019
© Author(s) 2019. This work is distributed under
the Creative Commons Attribution 4.0 License.

Research article 13 Aug 2019

Research article | 13 Aug 2019

On the contribution of chemical oscillations to ozone depletion events in the polar spring

Maximilian Herrmann et al.

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AR: Author's response | RR: Referee report | ED: Editor decision
AR by Maximilian Herrmann on behalf of the Authors (23 May 2019)  Author's response    Manuscript
ED: Publish subject to minor revisions (review by editor) (25 Jun 2019) by Laurens Ganzeveld
AR by Maximilian Herrmann on behalf of the Authors (04 Jul 2019)  Author's response    Manuscript
ED: Publish subject to technical corrections (08 Jul 2019) by Laurens Ganzeveld
AR by Maximilian Herrmann on behalf of the Authors (08 Jul 2019)  Author's response    Manuscript
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Short summary
The oscillations of tropospheric ODEs in the Arctic spring is studied numerically. After the termination of an ODE, the reactive bromine is deposited onto aerosols/the snow surface, and the ozone may regenerate. The replenished ozone is available for the next autocatalytic bromine release, leading to the oscillation of an ODE. Its dependence on the NOx mixing ratio, the inversion layer strength, the ambient temperature, the aerosol density, and the solar radiation is investigated.
The oscillations of tropospheric ODEs in the Arctic spring is studied numerically. After the...
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