Articles | Volume 29, issue 4
https://doi.org/10.5194/hess-29-1083-2025
https://doi.org/10.5194/hess-29-1083-2025
Research article
 | 
27 Feb 2025
Research article |  | 27 Feb 2025

The influence of permafrost and other environmental factors on stream thermal sensitivity across Yukon, Canada

Andras J. Szeitz 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-2024-1741', Anonymous Referee #1, 10 Sep 2024
  • RC2: 'Comment on egusphere-2024-1741', Anonymous Referee #2, 30 Sep 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) (04 Nov 2024) by Christa Kelleher
AR by Andras Szeitz on behalf of the Authors (04 Nov 2024)  Author's response   Author's tracked changes   Manuscript 
ED: Referee Nomination & Report Request started (18 Nov 2024) by Christa Kelleher
RR by Anonymous Referee #1 (03 Jan 2025)
ED: Publish as is (08 Jan 2025) by Christa Kelleher
ED: Publish as is (08 Jan 2025) by Thom Bogaard (Executive editor)
AR by Andras Szeitz on behalf of the Authors (09 Jan 2025)
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Short summary
Stream temperature sensitivity in northern regions responds to many of the same environmental controls as in temperate regions, but the presence of annually frozen ground (permafrost) influences catchment hydrology and stream temperature regimes. Permafrost can have positive and negative influences on thermal regimes. The net effect of northern environmental change on stream temperature is complex and uncertain, but permafrost will likely play a role through its control on cold region hydrology.
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