Articles | Volume 20, issue 8
https://doi.org/10.5194/tc-20-4563-2026
https://doi.org/10.5194/tc-20-4563-2026
Research article
 | 
20 Aug 2026
Research article |  | 20 Aug 2026

The multilayer ocean circulation melting the 79N Glacier ice tongue

Markus Reinert, Claudia Wekerle, Knut Klingbeil, Marvin Lorenz, and Hans Burchard

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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-2025-6459', Jonathan Wiskandt, 23 Feb 2026
    • RC2: 'Reply on RC1', Anonymous Referee #2, 01 Mar 2026
      • AC2: 'Reply on RC2', Markus Reinert, 26 May 2026
    • AC1: 'Reply on RC1', Markus Reinert, 26 May 2026

Peer review completion

AR – Author's response | RR – Referee report | ED – Editor decision | EF – Editorial file upload
ED: Submit a revised manuscript (03 Jun 2026) by Jan De Rydt
AR by Markus Reinert on behalf of the Authors (10 Jul 2026)  Author's response   Author's tracked changes   Manuscript 
ED: Referee Nomination & Report Request started (23 Jul 2026) by Jan De Rydt
RR by Jonathan Wiskandt (04 Aug 2026)
ED: Publish subject to technical corrections (11 Aug 2026) by Jan De Rydt
AR by Markus Reinert on behalf of the Authors (11 Aug 2026)  Author's response   Manuscript 
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Short summary
The Greenland Ice Sheet is an important contributor to global sea level rise. In northern Greenland, floating glacier tongues are primarily melted by ocean currents. These processes are difficult to observe, so we developed a realistic numerical model to study ocean-driven melting at Greenland's largest floating ice tongue, the 79° North Glacier. Our simulation reveals the details of the oceanic currents bringing warm water toward the ice base, melting and shaping the glacier tongue from below.
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