Articles | Volume 17, issue 9
Atmos. Chem. Phys., 17, 5677–5701, 2017
https://doi.org/10.5194/acp-17-5677-2017
Atmos. Chem. Phys., 17, 5677–5701, 2017
https://doi.org/10.5194/acp-17-5677-2017

Research article 08 May 2017

Research article | 08 May 2017

The radiative role of ozone and water vapour in the annual temperature cycle in the tropical tropopause layer

Alison Ming et al.

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AC: Author comment | RC: Referee comment | SC: Short comment | EC: Editor comment
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Peer-review completion

AR: Author's response | RR: Referee report | ED: Editor decision
AR by Alison Ming on behalf of the Authors (06 Mar 2017)  Author's response    Manuscript
ED: Referee Nomination & Report Request started (10 Mar 2017) by Qiang Fu
RR by Anonymous Referee #1 (15 Mar 2017)
RR by Susan Solomon (27 Mar 2017)
ED: Reconsider after minor revisions (Editor review) (28 Mar 2017) by Qiang Fu
AR by Alison Ming on behalf of the Authors (07 Apr 2017)  Author's response    Manuscript
ED: Publish as is (13 Apr 2017) by Qiang Fu
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Short summary
This work quantifies the contribution of the seasonal changes in ozone and water vapour to the temperature cycle in a region of the atmosphere about ~ 18 km up in the tropics (the lower stratosphere). This region is important because most of the air entering the stratosphere does so through this region and temperature fluctuations there influence how much water vapour enters the stratosphere and hence the properties of the stratosphere.
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