Articles | Volume 3, issue 3
Weather Clim. Dynam., 3, 905–935, 2022
https://doi.org/10.5194/wcd-3-905-2022
Weather Clim. Dynam., 3, 905–935, 2022
https://doi.org/10.5194/wcd-3-905-2022
Research article
08 Aug 2022
Research article | 08 Aug 2022

Summertime Rossby waves in climate models: substantial biases in surface imprint associated with small biases in upper-level circulation

Fei Luo 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-2021-48', Anonymous Referee #1, 08 Sep 2021
  • RC2: 'Comment on wcd-2021-48', Anonymous Referee #2, 28 Sep 2021
  • AC1: 'Response_Letter_to_RC1_and_RC2', Fei Luo, 05 Nov 2021

Peer review completion

AR: Author's response | RR: Referee report | ED: Editor decision
AR by Fei Luo on behalf of the Authors (18 Dec 2021)  Author's response    Author's tracked changes    Manuscript
ED: Referee Nomination & Report Request started (23 Dec 2021) by Irina Rudeva
RR by Anonymous Referee #3 (18 Jan 2022)
RR by Anonymous Referee #1 (31 Jan 2022)
ED: Publish subject to revisions (further review by editor and referees) (01 Feb 2022) by Irina Rudeva
AR by Fei Luo on behalf of the Authors (30 Mar 2022)  Author's response    Author's tracked changes    Manuscript
ED: Publish subject to revisions (further review by editor and referees) (01 Apr 2022) by Irina Rudeva
ED: Referee Nomination & Report Request started (08 Apr 2022) by Irina Rudeva
RR by Anonymous Referee #3 (05 Jun 2022)
ED: Publish subject to minor revisions (review by editor) (06 Jun 2022) by Irina Rudeva
AR by Fei Luo on behalf of the Authors (09 Jun 2022)  Author's response    Author's tracked changes    Manuscript
ED: Publish subject to technical corrections (14 Jun 2022) by Irina Rudeva
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Short summary
Recent studies have identified the weather systems in observational data, where wave patterns with high-magnitude values that circle around the whole globe in either wavenumber 5 or wavenumber 7 are responsible for the extreme events. In conclusion, we find that the climate models are able to reproduce the large-scale atmospheric circulation patterns as well as their associated surface variables such as temperature, precipitation, and sea level pressure.