Articles | Volume 23, issue 19
https://doi.org/10.5194/acp-23-10869-2023
https://doi.org/10.5194/acp-23-10869-2023
Research article
 | 
05 Oct 2023
Research article |  | 05 Oct 2023

Vortex preconditioning of the 2021 sudden stratospheric warming: barotropic–baroclinic instability associated with the double westerly jets

Ji-Hee Yoo, Hye-Yeong Chun, and Min-Jee Kang

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Interactive discussion

Status: closed

Comment types: AC – author | RC – referee | CC – community | EC – editor | CEC – chief editor | : Report abuse
  • RC1: 'Comment on egusphere-2023-1044', Anonymous Referee #1, 02 Jul 2023
    • AC1: 'Reply on RC1', Ji-Hee Yoo, 04 Jul 2023
  • RC2: 'Comment on egusphere-2023-1044', Anonymous Referee #2, 07 Jul 2023
    • AC2: 'Reply on RC2', Ji-Hee Yoo, 08 Jul 2023

Peer review completion

AR: Author's response | RR: Referee report | ED: Editor decision | EF: Editorial file upload
AR by Ji-Hee Yoo on behalf of the Authors (09 Aug 2023)  Author's response   Author's tracked changes   Manuscript 
ED: Publish as is (29 Aug 2023) by Peter Haynes
AR by Ji-Hee Yoo on behalf of the Authors (30 Aug 2023)
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Short summary
The January 2021 sudden stratospheric warming was preceded by unusual double westerly jets with polar stratospheric and subtropical mesospheric cores. This wind structure promotes anomalous dissipation of tropospheric planetary waves between the two maxima, leading to unusually strong shear instability. Shear instability generates the westward-propagating planetary waves with zonal wavenumber 2 in situ, thereby splitting the polar vortex just before the onset.
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