Articles | Volume 25, issue 1
https://doi.org/10.5194/hess-25-237-2021
https://doi.org/10.5194/hess-25-237-2021
Research article
 | 
15 Jan 2021
Research article |  | 15 Jan 2021

Hillslope and groundwater contributions to streamflow in a Rocky Mountain watershed underlain by glacial till and fractured sedimentary bedrock

Sheena A. Spencer, Axel E. Anderson, Uldis Silins, and Adrian L. Collins

Viewed

Total article views: 2,722 (including HTML, PDF, and XML)
HTML PDF XML Total BibTeX EndNote
1,897 760 65 2,722 67 71
  • HTML: 1,897
  • PDF: 760
  • XML: 65
  • Total: 2,722
  • BibTeX: 67
  • EndNote: 71
Views and downloads (calculated since 16 Mar 2020)
Cumulative views and downloads (calculated since 16 Mar 2020)

Viewed (geographical distribution)

Total article views: 2,722 (including HTML, PDF, and XML) Thereof 2,517 with geography defined and 205 with unknown origin.
Country # Views %
  • 1
1
 
 
 
 

Cited

Latest update: 07 Nov 2024
Download
Short summary
We used unique chemical signatures of precipitation, hillslope soil water, and groundwater sources of streamflow to explore seasonal variation in runoff generation in a snow-dominated mountain watershed underlain by glacial till and permeable bedrock. Reacted hillslope water reached the stream first at the onset of snowmelt, followed by a dilution effect by snowmelt from May to June. Groundwater and riparian water were important sources later in the summer. Till created complex subsurface flow.