Articles | Volume 19, issue 8
https://doi.org/10.5194/tc-19-3107-2025
https://doi.org/10.5194/tc-19-3107-2025
Research article
 | 
18 Aug 2025
Research article |  | 18 Aug 2025

Trace metal distributions in the transition zone from the Greenland Ice Sheet to the surface water in Kangerlussuaq fjord (67° N)

Clara R. Vives, Jørgen Bendtsen, Rasmus D. Dahms, Niels Daugbjerg, Kristina V. Larsen, and Minik T. Rosing

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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-2025-677', Anonymous Referee #1, 20 Mar 2025
    • AC1: 'Reply on RC1', Clara Vives, 15 Apr 2025
  • RC2: 'Comment on egusphere-2025-677', Anonymous Referee #2, 15 Apr 2025

Peer review completion

AR: Author's response | RR: Referee report | ED: Editor decision | EF: Editorial file upload
ED: Publish subject to minor revisions (review by editor) (21 May 2025) by Elizabeth Bagshaw
AR by Clara Vives on behalf of the Authors (23 May 2025)  Author's response   Author's tracked changes   Manuscript 
ED: Publish subject to technical corrections (09 Jun 2025) by Elizabeth Bagshaw
AR by Clara Vives on behalf of the Authors (10 Jun 2025)  Manuscript 
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Short summary
Glacial rock flour (GRF) from Greenlandic glaciers transports silicate and trace metals into fjords, influencing marine biogeochemistry. Trace metal concentrations are high in riverine and low-salinity waters but decrease sharply as salinity increases, challenging estimates based on freshwater input alone. Silicate rises due to GRF weathering but declines in fjords due to mixing. Uranium and molybdenum originate from the ocean, highlighting complex trace metal and nutrient dynamics.
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