Articles | Volume 21, issue 5
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


Interactive discussion

Status: closed
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
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
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.
Final-revised paper