Articles | Volume 13, issue 2
https://doi.org/10.5194/tc-13-591-2019
https://doi.org/10.5194/tc-13-591-2019
Research article
 | Highlight paper
 | 
18 Feb 2019
Research article | Highlight paper |  | 18 Feb 2019

Thaw processes in ice-rich permafrost landscapes represented with laterally coupled tiles in a land surface model

Kjetil S. Aas, Léo Martin, Jan Nitzbon, Moritz Langer, Julia Boike, Hanna Lee, Terje K. Berntsen, and Sebastian Westermann

Viewed

Total article views: 6,931 (including HTML, PDF, and XML)
HTML PDF XML Total BibTeX EndNote
5,409 1,415 107 6,931 99 112
  • HTML: 5,409
  • PDF: 1,415
  • XML: 107
  • Total: 6,931
  • BibTeX: 99
  • EndNote: 112
Views and downloads (calculated since 07 Nov 2018)
Cumulative views and downloads (calculated since 07 Nov 2018)

Viewed (geographical distribution)

Total article views: 6,931 (including HTML, PDF, and XML) Thereof 5,753 with geography defined and 1,178 with unknown origin.
Country # Views %
  • 1
1
 
 
 
 

Cited

Discussed (final revised paper)

Latest update: 24 Apr 2024
Short summary
Many permafrost landscapes contain large amounts of excess ground ice, which gives rise to small-scale elevation differences. This results in lateral fluxes of snow, water, and heat, which we investigate and show how it can be accounted for in large-scale models. Using a novel model technique which can account for these differences, we are able to model both the current state of permafrost and how these landscapes change as permafrost thaws, in a way that could not previously be achieved.