Articles | Volume 13, issue 4
Earth Syst. Dynam., 13, 1611–1623, 2022
https://doi.org/10.5194/esd-13-1611-2022
Earth Syst. Dynam., 13, 1611–1623, 2022
https://doi.org/10.5194/esd-13-1611-2022
Research article
17 Nov 2022
Research article | 17 Nov 2022

El Niño–Southern Oscillation (ENSO) predictability in equilibrated warmer climates

Yiyu Zheng 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: 'Comment on egusphere-2022-89', Anonymous Referee #1, 31 May 2022
    • AC1: 'Reply on RC1', Yiyu Zheng, 25 Aug 2022
  • RC2: 'Comment on egusphere-2022-89', Anonymous Referee #2, 07 Aug 2022
    • AC2: 'Reply on RC2', Yiyu Zheng, 25 Aug 2022
  • AC3: 'Comment on egusphere-2022-89', Yiyu Zheng, 25 Aug 2022

Peer review completion

AR: Author's response | RR: Referee report | ED: Editor decision
ED: Reconsider after major revisions (29 Aug 2022) by Anders Levermann
AR by Yiyu Zheng on behalf of the Authors (02 Sep 2022)  Author's response    Author's tracked changes    Manuscript
ED: Referee Nomination & Report Request started (13 Sep 2022) by Anders Levermann
ED: Publish as is (24 Oct 2022) by Anders Levermann
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Short summary
El Niño–Southern Oscillation (ENSO) is one of the dominant climatic phenomena in the equatorial Pacific. Understanding and predicting how ENSO might change in a warmer climate is both societally and scientifically important. We use 1000-year-long simulations from seven climate models to analyze ENSO in an idealized stable climate. We show that ENSO will be weaker and last shorter under the warming, while the skill of ENSO prediction will unlikely change.
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