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Nonlinear Processes in Geophysics An interactive open-access journal of the European Geosciences Union

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Nonlin. Processes Geophys., 24, 167-178, 2017
https://doi.org/10.5194/npg-24-167-2017
© Author(s) 2017. This work is distributed under
the Creative Commons Attribution 3.0 License.
Research article
20 Apr 2017
Dynamics of the Hadley circulation in an axisymmetric model undergoing stratification periodic forcing
Nazario Tartaglione
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Interactive discussionStatus: closed
AC: Author comment | RC: Referee comment | SC: Short comment | EC: Editor comment
Printer-friendly Version - Printer-friendly version      Supplement - Supplement
 
RC1: 'discussin comments', Anonymous Referee #1, 20 Dec 2016 Printer-friendly Version 
AC1: 'Reply', Nazario Tartaglione, 20 Dec 2016 Printer-friendly Version 
 
RC2: 'interacrive discussion', Anonymous Referee #1, 20 Dec 2016 Printer-friendly Version 
 
RC3: 'Referee review', Anonymous Referee #2, 22 Dec 2016 Printer-friendly Version 
 
AC2: 'Author response', Nazario Tartaglione, 24 Jan 2017 Printer-friendly Version Supplement 
Peer review completion
AR: Author's response | RR: Referee report | ED: Editor decision
AR by Nazario Tartaglione on behalf of the Authors (24 Jan 2017)  Author's response  Manuscript
ED: Reconsider after major revisions (further review by Editor and Referees) (27 Jan 2017) by Victor Shrira  
ED: Reconsider after major revisions (further review by Editor and Referees) (30 Jan 2017) by Victor Shrira  
ED: Referee Nomination & Report Request started (31 Jan 2017) by Victor Shrira
RR by Anonymous Referee #1 (14 Feb 2017)
RR by Anonymous Referee #2 (16 Feb 2017)  
ED: Publish subject to minor revisions (further review by Editor) (26 Feb 2017) by Victor Shrira  
AR by Nazario Tartaglione on behalf of the Authors (08 Mar 2017)  Author's response  Manuscript
ED: Publish as is (09 Mar 2017) by Victor Shrira  
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Publications Copernicus
Short summary
This paper aims to show how the tropical circulation responds to changes of the vertical stratification of the imposed temperature that drives the model. These changes mimic the presence of water vapor cycles. Thus, for simplicity's sake we impose a periodic change of this stratification with variable periods of 10–90 days. The model responds with quasi-periodic oscillations having two or more dominant frequencies. After a long forcing time period, chaotic behavior starts to appear cyclically.
This paper aims to show how the tropical circulation responds to changes of the vertical...
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