The Cryosphere
The Cryosphere
TC
Articles | Volume 17, issue 8
Articles | Volume 17, issue 8
https://doi.org/10.5194/tc-17-3363-2023
© Author(s) 2023. This work is distributed under
the Creative Commons Attribution 4.0 License.
https://doi.org/10.5194/tc-17-3363-2023
© Author(s) 2023. This work is distributed under
the Creative Commons Attribution 4.0 License.
Articles | Volume 17, issue 8
Research article
 | 
21 Aug 2023
Research article |  | 21 Aug 2023

Permafrost saline water and Early to mid-Holocene permafrost aggradation in Svalbard

Dotan Rotem, Vladimir Lyakhovsky, Hanne Hvidtfeldt Christiansen, Yehudit Harlavan, and Yishai Weinstein

Viewed

Total article views: 1,386 (including HTML, PDF, and XML)
HTML PDF XML Total BibTeX EndNote
965 359 62 1,386 37 35
  • HTML: 965
  • PDF: 359
  • XML: 62
  • Total: 1,386
  • BibTeX: 37
  • EndNote: 35
Views and downloads (calculated since 31 Aug 2022)
Cumulative views and downloads (calculated since 31 Aug 2022)

Viewed (geographical distribution)

Total article views: 1,386 (including HTML, PDF, and XML) Thereof 1,334 with geography defined and 52 with unknown origin.
Country # Views %
  • 1
1
 
 
 
 

Cited

Latest update: 13 Dec 2024
Download
Short summary
Frozen saline pore water, left over from post-glacial marine ingression, was found in shallow permafrost in a Svalbard fjord valley. This suggests that freezing occurred immediately after marine regression due to isostatic rebound. We conducted top-down freezing simulations, which confirmed that with Early to mid-Holocene temperatures (e.g. −4 °C), freezing could progress down to 20–40 m within 200 years. This, in turn, could inhibit flow through the sediment, therefore preserving saline fluids.
Read more