Articles | Volume 12, issue 12
https://doi.org/10.5194/tc-12-3891-2018
© Author(s) 2018. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
https://doi.org/10.5194/tc-12-3891-2018
© Author(s) 2018. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Glacial and geomorphic effects of a supraglacial lake drainage and outburst event, Everest region, Nepal Himalaya
School of Geography, University of Leeds, Leeds, LS2 9JT, UK
Swiss Federal Research Institute WSL, Birmensdorf 8903, Switzerland
C. Scott Watson
School of Geography, University of Leeds, Leeds, LS2 9JT, UK
Department of Hydrology and Atmospheric Sciences, University of Arizona, Tucson, AZ 85721, USA
Fanny Brun
LEGOS, Université de Toulouse, CNES, CNRS, IRD, UPS, 31400 Toulouse, France
Univ. Grenoble Alpes, CNRS, IRD, Grenoble INP, IGE, 38000 Grenoble, France
Etienne Berthier
LEGOS, Université de Toulouse, CNES, CNRS, IRD, UPS, 31400 Toulouse, France
Michel Esteves
Univ. Grenoble Alpes, CNRS, IRD, Grenoble INP, IGE, 38000 Grenoble, France
Duncan J. Quincey
School of Geography, University of Leeds, Leeds, LS2 9JT, UK
Katie E. Miles
Department of Geography and Earth Sciences, Aberystwyth University, SY23 3DB, Aberystwyth, UK
Bryn Hubbard
Department of Geography and Earth Sciences, Aberystwyth University, SY23 3DB, Aberystwyth, UK
Patrick Wagnon
Univ. Grenoble Alpes, CNRS, IRD, Grenoble INP, IGE, 38000 Grenoble, France
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- Exceptional thinning through the entire altitudinal range of Mont-Blanc glaciers during the 2021/22 mass balance year E. Berthier et al. 10.1017/jog.2023.100
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- The Pléiades Glacier Observatory: high-resolution digital elevation models and ortho-imagery to monitor glacier change E. Berthier et al. 10.5194/tc-18-5551-2024
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Discussed (final revised paper)
Latest update: 14 Dec 2024
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.
We use high-resolution satellite imagery and field visits to assess the growth and drainage of a...