The Cryosphere
The Cryosphere
TC
Articles | Volume 19, issue 8
Articles | Volume 19, issue 8
https://doi.org/10.5194/tc-19-3193-2025
© Author(s) 2025. This work is distributed under
the Creative Commons Attribution 4.0 License.
https://doi.org/10.5194/tc-19-3193-2025
© Author(s) 2025. This work is distributed under
the Creative Commons Attribution 4.0 License.
Articles | Volume 19, issue 8
Research article
 | 
22 Aug 2025
Research article |  | 22 Aug 2025

Wind and topography underlie correlation between seasonal snowpack, mountain glaciers, and late-summer streamflow

Elijah N. Boardman, Andrew G. Fountain, Joseph W. Boardman, Thomas H. Painter, Evan W. Burgess, Laura Wilson, and Adrian A. Harpold

Viewed

Total article views: 3,439 (including HTML, PDF, and XML)
HTML PDF XML Total Supplement BibTeX EndNote
3,054 323 62 3,439 90 93 149
  • HTML: 3,054
  • PDF: 323
  • XML: 62
  • Total: 3,439
  • Supplement: 90
  • BibTeX: 93
  • EndNote: 149
Views and downloads (calculated since 15 Jan 2025)
Cumulative views and downloads (calculated since 15 Jan 2025)

Viewed (geographical distribution)

Total article views: 3,439 (including HTML, PDF, and XML) Thereof 3,389 with geography defined and 50 with unknown origin.
Country # Views %
  • 1
1
 
 
 
 
Latest update: 29 Jan 2026
Download
Short summary
Watersheds on the downwind side of a mountain range have deeper seasonal snow and more abundant glaciers due to topographic controls that favor wind drifting. Despite receiving less total snow, these drift-prone watersheds produce relatively more late-summer streamflow due to a combination of slow-melting snow drifts and mass loss from glaciers (and other perennial snow/ice features).
Read more
Share