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ACP | Articles | Volume 19, issue 15
Atmos. Chem. Phys., 19, 9833–9846, 2019
https://doi.org/10.5194/acp-19-9833-2019
© Author(s) 2019. This work is distributed under
the Creative Commons Attribution 4.0 License.
Atmos. Chem. Phys., 19, 9833–9846, 2019
https://doi.org/10.5194/acp-19-9833-2019
© Author(s) 2019. This work is distributed under
the Creative Commons Attribution 4.0 License.

Research article 02 Aug 2019

Research article | 02 Aug 2019

Separating the role of direct radiative heating and photolysis in modulating the atmospheric response to the amplitude of the 11-year solar cycle forcing

Ewa M. Bednarz et al.

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AC: Author comment | RC: Referee comment | SC: Short comment | EC: Editor comment
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AR: Author's response | RR: Referee report | ED: Editor decision
AR by Ewa Bednarz on behalf of the Authors (30 Apr 2019)  Author's response    Manuscript
ED: Referee Nomination & Report Request started (03 May 2019) by Jens-Uwe Grooß
RR by Rémi Thiéblemont (21 May 2019)
ED: Publish subject to technical corrections (21 May 2019) by Jens-Uwe Grooß
AR by Ewa Bednarz on behalf of the Authors (27 May 2019)  Author's response    Manuscript
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Short summary
The atmospheric response to the amplitude of 11-year solar cycle in UM-UKCA is separated into the contributions from changes in direct radiative heating and photolysis rates, and the results compared with a control case with both effects included. We find that while the tropical responses are largely additive, this is not necessarily the case in the high latitudes. We suggest that solar-induced changes in ozone are important for modulating the SH dynamical response to the 11-year solar cycle.
The atmospheric response to the amplitude of 11-year solar cycle in UM-UKCA is separated into...
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