Articles | Volume 20, issue 9
https://doi.org/10.5194/tc-20-5533-2026
https://doi.org/10.5194/tc-20-5533-2026
Research article
 | 
29 Sep 2026
Research article |  | 29 Sep 2026

In-situ tracer percolation experiments to quantify the influence of near-surface melting on Svalbard snow signatures

Dorothea Elisabeth Baur, Andrea Spolaor, Federico Scoto, and Elizabeth R. Thomas

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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-2026-399', Anonymous Referee #1, 16 Mar 2026
    • AC1: 'Reply on RC1', Dorothea Elisabeth Moser, 10 Jun 2026
  • RC2: 'Comment on egusphere-2026-399', Anonymous Referee #2, 20 Mar 2026
    • AC2: 'Reply on RC2', Dorothea Elisabeth Moser, 10 Jun 2026

Peer review completion

AR – Author's response | RR – Referee report | ED – Editor decision | EF – Editorial file upload
ED: Submit a revised manuscript (18 Jun 2026) by Sebastian Gerland
AR by Dorothea Elisabeth Baur on behalf of the Authors (18 Jun 2026)  Author's response   Author's tracked changes   Manuscript 
ED: Publish subject to revisions (further review by editor and referees) (22 Jun 2026) by Sebastian Gerland
AR by Dorothea Elisabeth Baur on behalf of the Authors (22 Jun 2026)  Author's response   Author's tracked changes   Manuscript 
ED: Referee Nomination & Report Request started (23 Jun 2026) by Sebastian Gerland
RR by Anonymous Referee #2 (23 Jun 2026)
RR by Stephen Warren (03 Jul 2026)
ED: Publish subject to technical corrections (18 Jul 2026) by Sebastian Gerland
AR by Dorothea Elisabeth Baur on behalf of the Authors (23 Jul 2026)  Author's response   Manuscript 
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Short summary
The Arctic is warming rapidly, and winter rain-on-snow events are becoming more common. These events can alter snow layers and disturb climate information stored in glaciers. We studied how small rain-on-snow events affect snow structure and water isotopes near Ny-Ålesund, Svalbard. Field experiments show that meltwater flow creates complex features, but isotope changes remain confined to them, meaning seasonal climate signals can still be preserved where enough snow accumulates.
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