Articles | Volume 39, issue 2
https://doi.org/10.5194/angeo-39-357-2021
https://doi.org/10.5194/angeo-39-357-2021
Regular paper
 | 
14 Apr 2021
Regular paper |  | 14 Apr 2021

Modelling the residual mean meridional circulation at different stages of sudden stratospheric warming events

Andrey V. Koval, Wen Chen, Ksenia A. Didenko, Tatiana S. Ermakova, Nikolai M. Gavrilov, Alexander I. Pogoreltsev, Olga N. Toptunova, Ke Wei, Anna N. Yarusova, and Anton S. Zarubin

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Interactive discussion

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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
ED: Reconsider after major revisions (further review by editor and referees) (31 Dec 2020) by Petr Pisoft
AR by Andrey Koval on behalf of the Authors (31 Dec 2020)  Author's response    Author's tracked changes    Manuscript
ED: Referee Nomination & Report Request started (05 Jan 2021) by Petr Pisoft
RR by Anonymous Referee #3 (29 Jan 2021)
RR by Anonymous Referee #2 (11 Feb 2021)
ED: Publish subject to minor revisions (review by editor) (12 Feb 2021) by Petr Pisoft
AR by Andrey Koval on behalf of the Authors (01 Mar 2021)  Author's response    Author's tracked changes    Manuscript
ED: Publish as is (05 Mar 2021) by Petr Pisoft
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Short summary
Numerical modelling is used to simulate atmospheric circulation and calculate residual mean meridional circulation (RMC) during sudden stratospheric warming (SSW) events. Calculating the RMC is used to take into account wave effects on the transport of atmospheric quantities and gas species in the meridional plane. The results show that RMC undergoes significant changes at different stages of SSW and contributes to SSW development.