Articles | Volume 27, issue 14
https://doi.org/10.5194/hess-27-2807-2023
https://doi.org/10.5194/hess-27-2807-2023
Research article
 | 
28 Jul 2023
Research article |  | 28 Jul 2023

Warming of the Willamette River, 1850–present: the effects of climate change and river system alterations

Stefan A. Talke, David A. Jay, and Heida L. Diefenderfer

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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-2022-793', Anonymous Referee #1, 27 Oct 2022
    • AC1: 'Reply on RC1', Stefan Talke, 08 May 2023
  • RC2: 'Comment on egusphere-2022-793', Anonymous Referee #2, 08 Feb 2023
    • AC2: 'Reply on RC2', Stefan Talke, 08 May 2023
  • EC1: 'Comment on egusphere-2022-793', Jan Seibert, 08 May 2023

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) (09 May 2023) by Jan Seibert
AR by Stefan Talke on behalf of the Authors (10 May 2023)  Author's response   Author's tracked changes   Manuscript 
ED: Referee Nomination & Report Request started (10 May 2023) by Jan Seibert
RR by Anonymous Referee #1 (06 Jun 2023)
RR by Anonymous Referee #2 (13 Jun 2023)
ED: Publish as is (18 Jun 2023) by Jan Seibert
AR by Stefan Talke on behalf of the Authors (21 Jun 2023)
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Short summary
Archival measurements and a statistical model show that average water temperature in a major US West Coast river has increased by 1.8 °C since 1850, at a rate of 1.1 °C per century. The largest factor driving modeled changes are warming air temperatures (nearly 75 %). The remainder is primarily caused by depth increases and other modifications to the river system. Near-freezing conditions, common historically, no longer occur, and the number of warm water days has significantly increased.