Articles | Volume 16, issue 12
https://doi.org/10.5194/tc-16-5041-2022
https://doi.org/10.5194/tc-16-5041-2022
Research article
 | 
20 Dec 2022
Research article |  | 20 Dec 2022

The surface energy balance during foehn events at Joyce Glacier, McMurdo Dry Valleys, Antarctica

Marte G. Hofsteenge, Nicolas J. Cullen, Carleen H. Reijmer, Michiel van den Broeke, Marwan Katurji, and John F. Orwin

Viewed

Total article views: 2,007 (including HTML, PDF, and XML)
HTML PDF XML Total BibTeX EndNote
1,464 491 52 2,007 46 49
  • HTML: 1,464
  • PDF: 491
  • XML: 52
  • Total: 2,007
  • BibTeX: 46
  • EndNote: 49
Views and downloads (calculated since 02 Aug 2022)
Cumulative views and downloads (calculated since 02 Aug 2022)

Viewed (geographical distribution)

Total article views: 2,007 (including HTML, PDF, and XML) Thereof 1,942 with geography defined and 65 with unknown origin.
Country # Views %
  • 1
1
 
 
 
 

Cited

Latest update: 26 Jul 2024
Download
Short summary
In the McMurdo Dry Valleys (MDV), foehn winds can impact glacial meltwater production and the fragile ecosystem that depends on it. We study these dry and warm winds at Joyce Glacier and show they are caused by a different mechanism than that found for nearby valleys, demonstrating the complex interaction of large-scale winds with the mountains in the MDV. We find that foehn winds increase sublimation of ice, increase heating from the atmosphere, and increase the occurrence and rates of melt.