Articles | Volume 18, issue 4
https://doi.org/10.5194/tc-18-1653-2024
https://doi.org/10.5194/tc-18-1653-2024
Research article
 | 
09 Apr 2024
Research article |  | 09 Apr 2024

A rigorous approach to the specific surface area evolution in snow during temperature gradient metamorphism

Anna Braun, Kévin Fourteau, and Henning Löwe

Viewed

Total article views: 841 (including HTML, PDF, and XML)
HTML PDF XML Total BibTeX EndNote
614 174 53 841 42 41
  • HTML: 614
  • PDF: 174
  • XML: 53
  • Total: 841
  • BibTeX: 42
  • EndNote: 41
Views and downloads (calculated since 13 Sep 2023)
Cumulative views and downloads (calculated since 13 Sep 2023)

Viewed (geographical distribution)

Total article views: 841 (including HTML, PDF, and XML) Thereof 818 with geography defined and 23 with unknown origin.
Country # Views %
  • 1
1
 
 
 
 

Cited

Latest update: 17 Jul 2024
Download
Short summary
The specific surface of snow dictates key physical properties and continuously evolves in natural snowpacks. This is referred to as metamorphism. This work develops a rigorous physical model for this evolution, which is able to reproduce X-ray tomography measurements without using unphysical tuning parameters. Our results emphasize that snow crystal growth at the micrometer scale ultimately controls the pace of metamorphism.