Articles | Volume 15, issue 1
https://doi.org/10.5194/tc-15-265-2021
https://doi.org/10.5194/tc-15-265-2021
Research article
 | 
19 Jan 2021
Research article |  | 19 Jan 2021

Debris cover and the thinning of Kennicott Glacier, Alaska: in situ measurements, automated ice cliff delineation and distributed melt estimates

Leif S. Anderson, William H. Armstrong, Robert S. Anderson, and Pascal Buri

Viewed

Total article views: 3,195 (including HTML, PDF, and XML)
HTML PDF XML Total Supplement BibTeX EndNote
2,101 975 119 3,195 326 138 118
  • HTML: 2,101
  • PDF: 975
  • XML: 119
  • Total: 3,195
  • Supplement: 326
  • BibTeX: 138
  • EndNote: 118
Views and downloads (calculated since 18 Sep 2019)
Cumulative views and downloads (calculated since 18 Sep 2019)

Viewed (geographical distribution)

Total article views: 3,195 (including HTML, PDF, and XML) Thereof 2,915 with geography defined and 280 with unknown origin.
Country # Views %
  • 1
1
 
 
 
 

Cited

Latest update: 29 Jun 2024
Download
Short summary
Many glaciers are thinning rapidly beneath debris cover (loose rock) that reduces melt, including Kennicott Glacier in Alaska. This contradiction has been explained by melt hotspots, such as ice cliffs, scattered within the debris cover. However, at Kennicott Glacier declining ice flow explains the rapid thinning. Through this study, Kennicott Glacier is now the first glacier in Alaska, and the largest glacier globally, where melt across its debris-covered tongue has been rigorously quantified.