Articles | Volume 21, issue 5
https://doi.org/10.5194/acp-21-3725-2021
https://doi.org/10.5194/acp-21-3725-2021
Research article
 | 
11 Mar 2021
Research article |  | 11 Mar 2021

Influence of the El Niño–Southern Oscillation on entry stratospheric water vapor in coupled chemistry–ocean CCMI and CMIP6 models

Chaim I. Garfinkel, Ohad Harari, Shlomi Ziskin Ziv, Jian Rao, Olaf Morgenstern, Guang Zeng, Simone Tilmes, Douglas Kinnison, Fiona M. O'Connor, Neal Butchart, Makoto Deushi, Patrick Jöckel, Andrea Pozzer, and Sean Davis

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AC: Author comment | RC: Referee comment | SC: Short comment | EC: Editor comment
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AR: Author's response | RR: Referee report | ED: Editor decision
AR by Chaim Garfinkel on behalf of the Authors (03 Dec 2020)  Author's response   Manuscript 
ED: Referee Nomination & Report Request started (19 Dec 2020) by Peter Hess
RR by Anonymous Referee #2 (21 Dec 2020)
RR by Anonymous Referee #1 (27 Dec 2020)
ED: Reconsider after major revisions (05 Jan 2021) by Peter Hess
AR by Chaim Garfinkel on behalf of the Authors (19 Jan 2021)  Author's response   Author's tracked changes   Manuscript 
ED: Publish as is (25 Jan 2021) by Peter Hess
AR by Chaim Garfinkel on behalf of the Authors (01 Feb 2021)  Manuscript 
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Short summary
Water vapor is the dominant greenhouse gas in the atmosphere, and El Niño is the dominant mode of variability in the ocean–atmosphere system. The connection between El Niño and water vapor above ~ 17 km is unclear, with single-model studies reaching a range of conclusions. This study examines this connection in 12 different models. While there are substantial differences among the models, all models appear to capture the fundamental physical processes correctly.
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