Articles | Volume 15, issue 12
https://doi.org/10.5194/acp-15-6767-2015
https://doi.org/10.5194/acp-15-6767-2015
Research article
 | 
18 Jun 2015
Research article |  | 18 Jun 2015

The role of convective overshooting clouds in tropical stratosphere–troposphere dynamical coupling

K. Kodera, B. M. Funatsu, C. Claud, and N. Eguchi

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Status: closed
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 Kunihiko Kodera on behalf of the Authors (14 Dec 2014)  Author's response   Manuscript 
ED: Referee Nomination & Report Request started (31 Jan 2015) by Peter Haynes
RR by Anonymous Referee #2 (09 Feb 2015)
RR by Anonymous Referee #1 (12 Feb 2015)
RR by Anonymous Referee #3 (17 Feb 2015)
ED: Reconsider after major revisions (23 Mar 2015) by Peter Haynes
AR by Kunihiko Kodera on behalf of the Authors (05 May 2015)  Author's response   Manuscript 
ED: Reconsider after minor revisions (Editor review) (20 May 2015) by Peter Haynes
AR by Kunihiko Kodera on behalf of the Authors (25 May 2015)  Author's response   Manuscript 
ED: Publish as is (02 Jun 2015) by Peter Haynes
AR by Kunihiko Kodera on behalf of the Authors (06 Jun 2015)
Short summary
The the role of deep convection in stratosphere–troposphere dynamical coupling in the tropics was studied during two large major stratospheric sudden warming events in January 2009 and January 2010. Convective activity and precipitation increased in the equatorial Southern Hemisphere as a result of a strengthening of the Brewer–Dobson circulation induced by enhanced stratospheric planetary wave activity.
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