Articles | Volume 5, issue 4
https://doi.org/10.5194/wcd-5-1473-2024
https://doi.org/10.5194/wcd-5-1473-2024
Research article
 | 
04 Dec 2024
Research article |  | 04 Dec 2024

Concurrent Bering Sea and Labrador Sea ice melt extremes in March 2023: a confluence of meteorological events aligned with stratosphere–troposphere interactions

Thomas J. Ballinger, Kent Moore, Qinghua Ding, Amy H. Butler, James E. Overland, Richard L. Thoman, Ian Baxter, Zhe Li, and Edward Hanna

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Interactive discussion

Status: closed

Comment types: AC – author | RC – referee | CC – community | EC – editor | CEC – chief editor | : Report abuse
  • CC1: 'Comment on egusphere-2024-925', Ruonan Zhang, 18 Jun 2024
    • AC1: 'Reply on CC1', Thomas Ballinger, 09 Aug 2024
  • RC1: 'Comment on egusphere-2024-925', Anonymous Referee #1, 19 Jun 2024
    • AC2: 'Reply on RC1', Thomas Ballinger, 09 Aug 2024
  • RC2: 'Comment on egusphere-2024-925', Anonymous Referee #2, 01 Jul 2024
    • AC3: 'Reply on RC2', Thomas Ballinger, 09 Aug 2024

Peer review completion

AR: Author's response | RR: Referee report | ED: Editor decision | EF: Editorial file upload
AR by Thomas Ballinger on behalf of the Authors (12 Aug 2024)  Author's response   Author's tracked changes   Manuscript 
ED: Referee Nomination & Report Request started (23 Aug 2024) by Irina Rudeva
RR by Anonymous Referee #2 (06 Sep 2024)
RR by Anonymous Referee #3 (14 Sep 2024)
ED: Publish subject to minor revisions (review by editor) (17 Sep 2024) by Irina Rudeva
AR by Thomas Ballinger on behalf of the Authors (25 Sep 2024)  Author's response   Author's tracked changes   Manuscript 
ED: Publish as is (30 Sep 2024) by Irina Rudeva
AR by Thomas Ballinger on behalf of the Authors (07 Oct 2024)
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Short summary
This study chronicles the meteorological conditions that led to the anomalous, tandem March 2023 ice melt event in the Labrador and Bering seas. A sudden stratospheric warming event initiated the development of an anticyclonic circulation pattern over the Greenland–Labrador region, while the La Niña background state supported ridging conditions over Alaska, both of which aided northward transport of warm, moist air and drove the concurrent sea ice melt extremes.