Articles | Volume 12, issue 12
https://doi.org/10.5194/tc-12-3891-2018
https://doi.org/10.5194/tc-12-3891-2018
Research article
 | 
13 Dec 2018
Research article |  | 13 Dec 2018

Glacial and geomorphic effects of a supraglacial lake drainage and outburst event, Everest region, Nepal Himalaya

Evan S. Miles, C. Scott Watson, Fanny Brun, Etienne Berthier, Michel Esteves, Duncan J. Quincey, Katie E. Miles, Bryn Hubbard, and Patrick Wagnon

Viewed

Total article views: 4,728 (including HTML, PDF, and XML)
HTML PDF XML Total Supplement BibTeX EndNote
3,127 1,492 109 4,728 627 121 124
  • HTML: 3,127
  • PDF: 1,492
  • XML: 109
  • Total: 4,728
  • Supplement: 627
  • BibTeX: 121
  • EndNote: 124
Views and downloads (calculated since 21 Aug 2018)
Cumulative views and downloads (calculated since 21 Aug 2018)

Viewed (geographical distribution)

Total article views: 4,728 (including HTML, PDF, and XML) Thereof 4,089 with geography defined and 639 with unknown origin.
Country # Views %
  • 1
1
 
 
 
 

Cited

Discussed (final revised paper)

Latest update: 02 Oct 2024
Download
Short summary
We use high-resolution satellite imagery and field visits to assess the growth and drainage of a lake on Changri Shar Glacier in the Everest region, and its impact. The lake filled and drained within 3 months, which is a shorter interval than would be detected by standard monitoring protocols, but forced re-routing of major trails in several locations. The water appears to have flowed beneath Changri Shar and Khumbu glaciers in an efficient manner, suggesting pre-existing developed flow paths.