The Cryosphere
The Cryosphere
TC
Articles | Volume 20, issue 1
Articles | Volume 20, issue 1
https://doi.org/10.5194/tc-20-47-2026
© Author(s) 2026. This work is distributed under
the Creative Commons Attribution 4.0 License.
Special issue:
https://doi.org/10.5194/tc-20-47-2026
© Author(s) 2026. This work is distributed under
the Creative Commons Attribution 4.0 License.
Articles | Volume 20, issue 1
Research article
 | 
06 Jan 2026
Research article |  | 06 Jan 2026

The coupling between hydrology, the development of the active layer and the chemical signature of surface water in a periglacial catchment in West Greenland

Johan Rydberg, Emma Lindborg, Christian Bonde, Benjamin M. C. Fischer, Tobias Lindborg, and Ylva Sjöberg

Viewed

Total article views: 4,060 (including HTML, PDF, and XML)
HTML PDF XML Total Supplement BibTeX EndNote
3,177 699 184 4,060 227 173 201
  • HTML: 3,177
  • PDF: 699
  • XML: 184
  • Total: 4,060
  • Supplement: 227
  • BibTeX: 173
  • EndNote: 201
Views and downloads (calculated since 03 Apr 2025)
Cumulative views and downloads (calculated since 03 Apr 2025)

Viewed (geographical distribution)

Total article views: 4,060 (including HTML, PDF, and XML) Thereof 3,972 with geography defined and 88 with unknown origin.
Country # Views %
  • 1
1
 
 
 
 

Saved (final revised paper)

Latest update: 03 Oct 2026
Download
Short summary
When water moves through a catchment it is affected by interaction with soil particles and groundwater. For this interaction to occur the water must move through the ground, something that is restricted by ground ice in permafrost landscapes. Here we look at the interplay between hydrology, water-age, and water chemistry in a catchment in West Greenland, and even if the permafrost leads to short flow paths and young water-age, there is considerable interaction between water and soil particles.
Read more
Share
Special issue
Northern hydrology in transition – impacts of a changing...