Articles | Volume 15, issue 1
https://doi.org/10.5194/acp-15-297-2015
https://doi.org/10.5194/acp-15-297-2015
Research article
 | 
13 Jan 2015
Research article |  | 13 Jan 2015

A global non-hydrostatic model study of a downward coupling through the tropical tropopause layer during a stratospheric sudden warming

N. Eguchi, K. Kodera, and T. Nasuno

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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 Nawo Eguchi on behalf of the Authors (03 Jul 2014)  Author's response   Manuscript 
ED: Referee Nomination & Report Request started (02 Aug 2014) by Peter Haynes
RR by Anonymous Referee #1 (15 Aug 2014)
RR by Anonymous Referee #2 (27 Aug 2014)
ED: Reconsider after minor revisions (Editor review) (11 Sep 2014) by Peter Haynes
AR by Nawo Eguchi on behalf of the Authors (22 Sep 2014)  Author's response   Manuscript 
ED: Reconsider after minor revisions (Editor review) (30 Oct 2014) by Peter Haynes
AR by Nawo Eguchi on behalf of the Authors (10 Nov 2014)  Author's response   Manuscript 
ED: Publish as is (16 Nov 2014) by Peter Haynes
AR by Nawo Eguchi on behalf of the Authors (18 Nov 2014)  Manuscript 
Short summary
The dynamical coupling process between stratosphere and troposphere in the tropical tropopause layer (TTL) during stratospheric sudden warming (SSW) was investigated using simulation data of global non-hydrostatic model (NICAM) that does not use cumulus parameterization. The results suggested that increased stratospheric tropical upwelling associated with SSW induced decreased static stability in TTL, which contributes to increased convective activity and changes in its large-scale organizations
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