Articles | Volume 22, issue 11
Atmos. Chem. Phys., 22, 7523–7538, 2022
https://doi.org/10.5194/acp-22-7523-2022
Atmos. Chem. Phys., 22, 7523–7538, 2022
https://doi.org/10.5194/acp-22-7523-2022
Research article
10 Jun 2022
Research article | 10 Jun 2022

The roles of the Quasi-Biennial Oscillation and El Niño for entry stratospheric water vapor in observations and coupled chemistry–ocean CCMI and CMIP6 models

Shlomi Ziskin Ziv et al.

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Interactive discussion

Status: closed

Comment types: AC – author | RC – referee | CC – community | EC – editor | CEC – chief editor | : Report abuse
  • RC1: 'Review', Anonymous Referee #1, 09 Feb 2022
  • RC2: 'Comment on acp-2021-972', Anonymous Referee #2, 11 Mar 2022

Peer review completion

AR: Author's response | RR: Referee report | ED: Editor decision
AR by Shlomi Ziskin Ziv on behalf of the Authors (07 Apr 2022)  Author's response    Author's tracked changes    Manuscript
ED: Referee Nomination & Report Request started (07 Apr 2022) by Rolf Müller
RR by Alison Ming (08 Apr 2022)
RR by Anonymous Referee #2 (12 Apr 2022)
RR by Anonymous Referee #3 (19 Apr 2022)
ED: Publish subject to minor revisions (review by editor) (22 Apr 2022) by Rolf Müller
AR by Shlomi Ziskin Ziv on behalf of the Authors (02 May 2022)  Author's response    Author's tracked changes    Manuscript
ED: Publish subject to technical corrections (06 May 2022) by Rolf Müller
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Short summary
Stratospheric water vapor is important for Earth's overall greenhouse effect and for ozone chemistry; however the factors governing its variability on interannual timescales are not fully known, and previous modeling studies have indicated that models struggle to capture this interannual variability. We demonstrate that nonlinear interactions are important for determining overall water vapor concentrations and also that models have improved in their ability to capture these connections.
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