Hydrology and Earth System Sciences
Hydrology and Earth System Sciences
HESS
Articles | Volume 27, issue 14
Articles | Volume 27, issue 14
https://doi.org/10.5194/hess-27-2807-2023
© Author(s) 2023. This work is distributed under
the Creative Commons Attribution 4.0 License.
https://doi.org/10.5194/hess-27-2807-2023
© Author(s) 2023. This work is distributed under
the Creative Commons Attribution 4.0 License.
Articles | Volume 27, issue 14
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

Viewed

Total article views: 2,364 (including HTML, PDF, and XML)
HTML PDF XML Total Supplement BibTeX EndNote
1,801 500 63 2,364 66 58 78
  • HTML: 1,801
  • PDF: 500
  • XML: 63
  • Total: 2,364
  • Supplement: 66
  • BibTeX: 58
  • EndNote: 78
Views and downloads (calculated since 07 Sep 2022)
Cumulative views and downloads (calculated since 07 Sep 2022)

Viewed (geographical distribution)

Total article views: 2,364 (including HTML, PDF, and XML) Thereof 2,294 with geography defined and 70 with unknown origin.
Country # Views %
  • 1
1
 
 
 
 

Cited

Latest update: 15 Sep 2025
Download
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.
Read more
Share