Articles | Volume 3, issue 2
Weather Clim. Dynam., 3, 483–504, 2022
https://doi.org/10.5194/wcd-3-483-2022
Weather Clim. Dynam., 3, 483–504, 2022
https://doi.org/10.5194/wcd-3-483-2022
Research article
11 Apr 2022
Research article | 11 Apr 2022

A global climatology of polar lows investigated for local differences and wind-shear environments

Patrick Johannes Stoll

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Interactive discussion

Status: closed

Comment types: AC – author | RC – referee | CC – community | EC – editor | CEC – chief editor | : Report abuse

Peer review completion

AR: Author's response | RR: Referee report | ED: Editor decision
AR by Patrick Stoll on behalf of the Authors (12 Jan 2022)  Author's response    Author's tracked changes    Manuscript
ED: Referee Nomination & Report Request started (19 Jan 2022) by Helen Dacre
RR by Anonymous Referee #2 (24 Jan 2022)
RR by Anonymous Referee #3 (14 Feb 2022)
ED: Publish subject to minor revisions (review by editor) (14 Feb 2022) by Helen Dacre
AR by Patrick Stoll on behalf of the Authors (23 Feb 2022)  Author's response    Author's tracked changes    Manuscript
ED: Publish as is (25 Feb 2022) by Helen Dacre
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Short summary
Polar lows are small but intense cyclones and constitute one of the major natural hazards in the polar regions. To be aware of when and where polar lows occur, this study maps polar lows globally by utilizing new atmospheric datasets. Polar lows develop in all marine areas adjacent to sea ice or cold landmasses, mainly in the winter half year. The highest frequency appears in the Nordic Seas. Further, it is found that polar lows are rather similar in the different ocean sub-basins.