Articles | Volume 14, issue 12
https://doi.org/10.5194/tc-14-4627-2020
https://doi.org/10.5194/tc-14-4627-2020
Research article
 | 
21 Dec 2020
Research article |  | 21 Dec 2020

Numerical modelling of permafrost spring discharge and open-system pingo formation induced by basal permafrost aggradation

Mikkel Toft Hornum, Andrew Jonathan Hodson, Søren Jessen, Victor Bense, and Kim Senger

Viewed

Total article views: 4,977 (including HTML, PDF, and XML)
HTML PDF XML Total Supplement BibTeX EndNote
3,922 961 94 4,977 260 88 87
  • HTML: 3,922
  • PDF: 961
  • XML: 94
  • Total: 4,977
  • Supplement: 260
  • BibTeX: 88
  • EndNote: 87
Views and downloads (calculated since 12 Feb 2020)
Cumulative views and downloads (calculated since 12 Feb 2020)

Viewed (geographical distribution)

Total article views: 4,977 (including HTML, PDF, and XML) Thereof 4,693 with geography defined and 284 with unknown origin.
Country # Views %
  • 1
1
 
 
 
 

Cited

Latest update: 29 Jun 2024
Short summary
In Arctic fjord valleys, considerable amounts of methane may be stored below the permafrost and escape directly to the atmosphere through springs. A new conceptual model of how such springs form and persist is presented and confirmed by numerical modelling experiments: in uplifted Arctic valleys, freezing pressure induced at the permafrost base can drive the flow of groundwater to the surface through vents in frozen ground. This deserves attention as an emission pathway for greenhouse gasses.