The Cryosphere
The Cryosphere
TC
Articles | Volume 16, issue 9
Articles | Volume 16, issue 9
https://doi.org/10.5194/tc-16-3413-2022
© Author(s) 2022. This work is distributed under
the Creative Commons Attribution 4.0 License.
https://doi.org/10.5194/tc-16-3413-2022
© Author(s) 2022. This work is distributed under
the Creative Commons Attribution 4.0 License.
Articles | Volume 16, issue 9
Research article
 | 
31 Aug 2022
Research article |  | 31 Aug 2022

Grain-size evolution controls the accumulation dependence of modelled firn thickness

Jonathan Kingslake, Robert Skarbek, Elizabeth Case, and Christine McCarthy

Viewed

Total article views: 3,725 (including HTML, PDF, and XML)
HTML PDF XML Total BibTeX EndNote
2,575 994 156 3,725 153 301
  • HTML: 2,575
  • PDF: 994
  • XML: 156
  • Total: 3,725
  • BibTeX: 153
  • EndNote: 301
Views and downloads (calculated since 17 Feb 2022)
Cumulative views and downloads (calculated since 17 Feb 2022)

Viewed (geographical distribution)

Total article views: 3,725 (including HTML, PDF, and XML) Thereof 3,537 with geography defined and 188 with unknown origin.
Country # Views %
  • 1
1
 
 
 
 

Cited

Saved (final revised paper)

Latest update: 29 Oct 2026
Download
Short summary
Firn is snow that has persisted for at least 1 full year on the surface of a glacier or ice sheet. It is an intermediate substance between snow and glacial ice. Firn compacts into glacial ice due to the weight of overlying snow and firn. The rate at which it compacts and the rate at which it is buried control how thick the firn layer is. We explore how this thickness depends on the rate of snow fall and how this dependence is controlled by the size of snow grains at the ice sheet surface.
Read more
Share
Altmetrics
Final-revised paper
Preprint