Articles | Volume 19, issue 3
https://doi.org/10.5194/os-19-671-2023
https://doi.org/10.5194/os-19-671-2023
Research article
 | 
22 May 2023
Research article |  | 22 May 2023

Sudden, local temperature increase above the continental slope in the southern Weddell Sea, Antarctica

Elin Darelius, Vår Dundas, Markus Janout, and Sandra Tippenhauer

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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-2022-1477', Karen J. Heywood, 12 Feb 2023
  • RC2: 'Comment on egusphere-2022-1477', Anonymous Referee #2, 24 Feb 2023

Peer review completion

AR: Author's response | RR: Referee report | ED: Editor decision | EF: Editorial file upload
AR by Elin Darelius on behalf of the Authors (28 Mar 2023)  Author's response   Author's tracked changes   Manuscript 
ED: Publish subject to minor revisions (review by editor) (12 Apr 2023) by Laura de Steur
AR by Elin Darelius on behalf of the Authors (19 Apr 2023)  Author's response   Author's tracked changes   Manuscript 
ED: Publish subject to technical corrections (19 Apr 2023) by Laura de Steur
AR by Elin Darelius on behalf of the Authors (20 Apr 2023)  Author's response   Manuscript 
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Short summary
Antarctica's ice shelves are melting from below as ocean currents bring warm water into the ice shelf cavities. The melt rates of the large Filchner–Ronne Ice Shelf in the southern Weddell Sea are currently low, as the water in the cavity is cold. Here, we present data from a scientific cruise to the region in 2021 and show that the warmest water at the upper part of the continental slope is now about 0.1°C warmer than in previous observations, while the surface water is fresher than before.