Articles | Volume 12, issue 12
The Cryosphere, 12, 3891–3905, 2018
https://doi.org/10.5194/tc-12-3891-2018
The Cryosphere, 12, 3891–3905, 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 et al.

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AR by Evan Miles on behalf of the Authors (12 Nov 2018)  Author's response    Manuscript
ED: Publish as is (14 Nov 2018) by Daniel Farinotti
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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.