Articles | Volume 3, issue 2
Weather Clim. Dynam., 3, 601–623, 2022
https://doi.org/10.5194/wcd-3-601-2022
Weather Clim. Dynam., 3, 601–623, 2022
https://doi.org/10.5194/wcd-3-601-2022
Research article
19 May 2022
Research article | 19 May 2022

Storm track response to uniform global warming downstream of an idealized sea surface temperature front

Sebastian Schemm 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-2022-3', Anonymous Referee #1, 11 Feb 2022
  • RC2: 'Comment on wcd-2022-3', Anonymous Referee #2, 01 Mar 2022

Peer review completion

AR: Author's response | RR: Referee report | ED: Editor decision
AR by Sebastian Schemm on behalf of the Authors (21 Mar 2022)  Author's response    Author's tracked changes    Manuscript
ED: Referee Nomination & Report Request started (31 Mar 2022) by Yang Zhang
RR by Anonymous Referee #1 (06 Apr 2022)
RR by Anonymous Referee #2 (25 Apr 2022)
ED: Publish subject to minor revisions (review by editor) (29 Apr 2022) by Yang Zhang
AR by Sebastian Schemm on behalf of the Authors (30 Apr 2022)  Author's response    Author's tracked changes    Manuscript
ED: Publish as is (04 May 2022) by Yang Zhang
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Short summary
Much of the change in our daily weather patterns is due to the development and intensification of extratropical cyclones. The response of these systems to climate change is an important topic of ongoing research. This study is the first to reproduce the changes in the North Atlantic circulation and extratropical cyclone characteristics found in fully coupled Earth system models under high-CO2 scenarios, but in an idealized, reduced-complexity simulation with uniform warming.