Articles | Volume 14, issue 23
https://doi.org/10.5194/bg-14-5487-2017
https://doi.org/10.5194/bg-14-5487-2017
Research article
 | 
06 Dec 2017
Research article |  | 06 Dec 2017

Retrogressive thaw slumps temper dissolved organic carbon delivery to streams of the Peel Plateau, NWT, Canada

Cara A. Littlefair, Suzanne E. Tank, and Steven V. Kokelj

Viewed

Total article views: 3,005 (including HTML, PDF, and XML)
HTML PDF XML Total Supplement BibTeX EndNote
1,702 1,194 109 3,005 303 87 103
  • HTML: 1,702
  • PDF: 1,194
  • XML: 109
  • Total: 3,005
  • Supplement: 303
  • BibTeX: 87
  • EndNote: 103
Views and downloads (calculated since 29 Jun 2017)
Cumulative views and downloads (calculated since 29 Jun 2017)

Viewed (geographical distribution)

Total article views: 3,005 (including HTML, PDF, and XML) Thereof 2,874 with geography defined and 131 with unknown origin.
Country # Views %
  • 1
1
 
 
 
 

Cited

Latest update: 14 Dec 2024
Download
Short summary
This study is the first to examine how permafrost slumping affects dissolved organic carbon (DOC) mobilization in landscapes dominated by glacial tills. Unlike in previous studies, we find that slumping is associated with decreased DOC concentrations in downstream systems – an effect that appears to occur via adsorption to fine-grained sediments. This work adds significantly to our understanding of varying effects of permafrost thaw on organic carbon mobilization across diverse Arctic regions.
Altmetrics
Final-revised paper
Preprint