Articles | Volume 15, issue 1
https://doi.org/10.5194/tc-15-389-2021
https://doi.org/10.5194/tc-15-389-2021
Research article
 | Highlight paper
 | 
28 Jan 2021
Research article | Highlight paper |  | 28 Jan 2021

Macroscopic water vapor diffusion is not enhanced in snow

Kévin Fourteau, Florent Domine, and Pascal Hagenmuller

Viewed

Total article views: 3,871 (including HTML, PDF, and XML)
HTML PDF XML Total BibTeX EndNote
3,073 706 92 3,871 103 86
  • HTML: 3,073
  • PDF: 706
  • XML: 92
  • Total: 3,871
  • BibTeX: 103
  • EndNote: 86
Views and downloads (calculated since 13 Jul 2020)
Cumulative views and downloads (calculated since 13 Jul 2020)

Viewed (geographical distribution)

Total article views: 3,871 (including HTML, PDF, and XML) Thereof 3,572 with geography defined and 299 with unknown origin.
Country # Views %
  • 1
1
 
 
 
 

Cited

Latest update: 14 Nov 2024
Short summary
There has been a long controversy to determine whether the effective diffusion coefficient of water vapor in snow is superior to that in free air. Using theory and numerical modeling, we show that while water vapor diffuses more than inert gases thanks to its interaction with the ice, the effective diffusion coefficient of water vapor in snow remains inferior to that in free air. This suggests that other transport mechanisms are responsible for the large vapor fluxes observed in some snowpacks.