Articles | Volume 21, issue 5
https://doi.org/10.5194/os-21-2419-2025
https://doi.org/10.5194/os-21-2419-2025
Research article
 | 
16 Oct 2025
Research article |  | 16 Oct 2025

Mechanisms of warm-water intrusions onto the West Spitsbergen Shelf during winter

Lukas Frank, Jon Albretsen, Ragnheid Skogseth, Frank Nilsen, and Marius O. Jonassen

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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 egusphere-2025-1721', Anonymous Referee #1, 27 May 2025
    • AC1: 'Reply on RC1', Lukas Frank, 11 Jun 2025
  • RC2: 'Comment on egusphere-2025-1721', Joseph Gradone, 30 May 2025
    • AC2: 'Reply on RC2', Lukas Frank, 11 Jun 2025
  • AC3: 'Comment on egusphere-2025-1721', Lukas Frank, 11 Jun 2025

Peer review completion

AR: Author's response | RR: Referee report | ED: Editor decision | EF: Editorial file upload
AR by Lukas Frank on behalf of the Authors (26 Jun 2025)  Author's response   Author's tracked changes   Manuscript 
ED: Referee Nomination & Report Request started (08 Jul 2025) by Matt Rayson
RR by Joseph Gradone (08 Jul 2025)
RR by Anonymous Referee #1 (15 Jul 2025)
ED: Publish as is (07 Aug 2025) by Matt Rayson
AR by Lukas Frank on behalf of the Authors (07 Aug 2025)
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Short summary
West of Svalbard, warm Atlantic Water frequently deviates from the West Spitsbergen Current onto shallow shelf areas, with significant implications for the regional climate system. The intrusions can be triggered by different processes, but their depths ultimately depend on the density difference between the intruding water and the ambient shelf water. These findings are an important step toward a better understanding of how warm Atlantic Water eventually reaches the fjords of Svalbard.
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