Articles | Volume 29, issue 11
https://doi.org/10.5194/hess-29-2467-2025
https://doi.org/10.5194/hess-29-2467-2025
Research article
 | 
12 Jun 2025
Research article |  | 12 Jun 2025

The role of catchment characteristics, discharge, and active- layer thaw in seasonal stream chemistry across 10 permafrost catchments

Arsh Grewal, Erin M. Nicholls, and Sean K. Carey

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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-2024-2645', Anonymous Referee #1, 16 Oct 2024
  • RC2: 'Comment on egusphere-2024-2645', Anonymous Referee #2, 20 Dec 2024

Peer review completion

AR: Author's response | RR: Referee report | ED: Editor decision | EF: Editorial file upload
ED: Reconsider after major revisions (further review by editor and referees) (12 Feb 2025) by Andrea Popp
AR by Arsh Grewal on behalf of the Authors (12 Feb 2025)  Author's response   Author's tracked changes   Manuscript 
ED: Referee Nomination & Report Request started (23 Feb 2025) by Andrea Popp
RR by Anonymous Referee #2 (24 Feb 2025)
ED: Publish as is (19 Mar 2025) by Andrea Popp
ED: Publish as is (20 Mar 2025) by Thom Bogaard (Executive editor)
AR by Arsh Grewal on behalf of the Authors (22 Mar 2025)  Manuscript 
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Short summary
Stream chemistry in permafrost watersheds is highly seasonal due to ground thaw and declining streamflow after spring melt, reducing hydrologic connectivity with organic-rich flow paths in fall. We quantified the magnitude of stream chemistry seasonality (driven by processes other than seasonal streamflow) across 10 watersheds. Watersheds with steeper slopes saw a more rapid decline in DOC (dissolved organic carbon) concentrations, while greater permafrost extent led to a greater relative increase in ion concentrations.
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