Articles | Volume 16, issue 9
https://doi.org/10.5194/tc-16-3775-2022
https://doi.org/10.5194/tc-16-3775-2022
Research article
 | 
22 Sep 2022
Research article |  | 22 Sep 2022

An 11-year record of wintertime snow-surface energy balance and sublimation at 4863 m a.s.l. on the Chhota Shigri Glacier moraine (western Himalaya, India)

Arindan Mandal, Thupstan Angchuk, Mohd Farooq Azam, Alagappan Ramanathan, Patrick Wagnon, Mohd Soheb, and Chetan Singh

Viewed

Total article views: 3,308 (including HTML, PDF, and XML)
HTML PDF XML Total Supplement BibTeX EndNote
2,454 775 79 3,308 210 51 82
  • HTML: 2,454
  • PDF: 775
  • XML: 79
  • Total: 3,308
  • Supplement: 210
  • BibTeX: 51
  • EndNote: 82
Views and downloads (calculated since 20 Jan 2022)
Cumulative views and downloads (calculated since 20 Jan 2022)

Viewed (geographical distribution)

Total article views: 3,308 (including HTML, PDF, and XML) Thereof 3,120 with geography defined and 188 with unknown origin.
Country # Views %
  • 1
1
 
 
 
 

Cited

Latest update: 13 Dec 2024
Download
Short summary
Snow sublimation is an important component of glacier surface mass balance; however, it is seldom studied in detail in the Himalayan region owing to data scarcity. We present an 11-year record of wintertime snow-surface energy balance and sublimation characteristics at the Chhota Shigri Glacier moraine site at 4863 m a.s.l. The estimated winter sublimation is 16 %–42 % of the winter snowfall at the study site, which signifies how sublimation is important in the Himalayan region.