Articles | Volume 22, issue 21
https://doi.org/10.5194/acp-22-14303-2022
https://doi.org/10.5194/acp-22-14303-2022
Research article
 | 
08 Nov 2022
Research article |  | 08 Nov 2022

Stratospheric water vapour and ozone response to the quasi-biennial oscillation disruptions in 2016 and 2020

Mohamadou A. Diallo, Felix Ploeger, Michaela I. Hegglin, Manfred Ern, Jens-Uwe Grooß, Sergey Khaykin, and Martin Riese

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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 acp-2022-382', Anonymous Referee #1, 14 Jun 2022
    • AC1: 'Reply on RC1', Mohamadou Diallo, 10 Oct 2022
  • RC2: 'Comment on acp-2022-382', Anonymous Referee #2, 30 Jun 2022
    • AC2: 'Reply on RC2', Mohamadou Diallo, 10 Oct 2022
  • RC3: 'Comment on acp-2022-382', Anonymous Referee #3, 30 Jun 2022
    • AC3: 'Reply on RC3', Mohamadou Diallo, 10 Oct 2022

Peer review completion

AR: Author's response | RR: Referee report | ED: Editor decision
AR by Mohamadou Diallo on behalf of the Authors (15 Oct 2022)  Author's response    Author's tracked changes    Manuscript
ED: Publish as is (18 Oct 2022) by Suvarna Fadnavis
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Short summary
The quasi-biennial oacillation disruption events in both 2016 and 2020 decreased lower-stratospheric water vapour and ozone. Differences in the strength and depth of the anomalous lower-stratospheric circulation and ozone are due to differences in tropical upwelling and cold-point temperature induced by lower-stratospheric planetary and gravity wave breaking. The differences in water vapour are due to higher cold-point temperature in 2020 induced by Australian wildfire.
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