Articles | Volume 3, issue 1
Weather Clim. Dynam., 3, 45–58, 2022
https://doi.org/10.5194/wcd-3-45-2022
Weather Clim. Dynam., 3, 45–58, 2022
https://doi.org/10.5194/wcd-3-45-2022

Research article 18 Jan 2022

Research article | 18 Jan 2022

Sudden stratospheric warmings during El Niño and La Niña: sensitivity to atmospheric model biases

Nicholas L. Tyrrell 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 wcd-2021-62', Ronald Kwan Kit Li, 28 Oct 2021
    • AC1: 'Reply on RC1', Nicholas Tyrrell, 01 Dec 2021
  • RC2: 'Comment on wcd-2021-62', Anonymous Referee #2, 06 Nov 2021
    • AC2: 'Reply on RC2', Nicholas Tyrrell, 01 Dec 2021

Peer review completion

AR: Author's response | RR: Referee report | ED: Editor decision
AR by Nicholas Tyrrell on behalf of the Authors (01 Dec 2021)  Author's response    Author's tracked changes    Manuscript
ED: Referee Nomination & Report Request started (02 Dec 2021) by Juliane Schwendike
RR by Ronald Kwan Kit Li (03 Dec 2021)
ED: Publish as is (03 Dec 2021) by Juliane Schwendike
Short summary
El Niño events are known to effect the variability of the wintertime stratospheric polar vortex. The observed relationship differs from what is seen in climate models. Climate models have errors in their average winds and temperature, and in this work we artificially reduce those errors to see how that changes the communication of El Niño events to the polar stratosphere. We find reducing errors improves stratospheric variability, but does not explain the differences with observations.