Articles | Volume 9, issue 4
https://doi.org/10.5194/tc-9-1363-2015
https://doi.org/10.5194/tc-9-1363-2015
Research article
 | 
30 Jul 2015
Research article |  | 30 Jul 2015

Tomography-based monitoring of isothermal snow metamorphism under advective conditions

P. P. Ebner, M. Schneebeli, and A. Steinfeld

Viewed

Total article views: 2,415 (including HTML, PDF, and XML)
HTML PDF XML Total BibTeX EndNote
1,300 984 131 2,415 134 129
  • HTML: 1,300
  • PDF: 984
  • XML: 131
  • Total: 2,415
  • BibTeX: 134
  • EndNote: 129
Views and downloads (calculated since 18 Feb 2015)
Cumulative views and downloads (calculated since 18 Feb 2015)

Cited

Saved (final revised paper)

Saved (preprint)

Latest update: 27 Mar 2024
Short summary
Time-lapse X-ray microtomography was used to investigate the structural dynamics of isothermal snow metamorphism exposed to an advective airflow and possible effects on natural snowpacks were discussed. The results showed that isothermal advection with saturated air have no influence on the coarsening rate that is typical for isothermal snow metamorphism. It is driven by sublimation-deposition caused by Kelvin effect and is the limiting factor independently of the transport regime in the pores.