Articles | Volume 9, issue 4
https://doi.org/10.5194/esurf-9-845-2021
https://doi.org/10.5194/esurf-9-845-2021
Research article
 | 
02 Aug 2021
Research article |  | 02 Aug 2021

Climatic controls on mountain glacier basal thermal regimes dictate spatial patterns of glacial erosion

Jingtao Lai and Alison M. Anders

Viewed

Total article views: 2,896 (including HTML, PDF, and XML)
HTML PDF XML Total BibTeX EndNote
1,991 834 71 2,896 45 46
  • HTML: 1,991
  • PDF: 834
  • XML: 71
  • Total: 2,896
  • BibTeX: 45
  • EndNote: 46
Views and downloads (calculated since 31 Mar 2021)
Cumulative views and downloads (calculated since 31 Mar 2021)

Viewed (geographical distribution)

Total article views: 2,896 (including HTML, PDF, and XML) Thereof 2,653 with geography defined and 243 with unknown origin.
Country # Views %
  • 1
1
 
 
 
 

Cited

Latest update: 20 Nov 2024
Download
Short summary
Glaciers are strong erosive agents, and they have created many unique landforms in mountain belts. Climate has been viewed as a primary control on glacial erosion, yet our understanding of the mechanism by which climate impacts glacial erosion remains limited. Using computer simulations, we find that climate controls glacial erosion by modulating the temperature of the basal ice. Our results suggest that a warm and/or wet climate can create warm basal ice and, therefore, enhance erosion.