Articles | Volume 9, issue 3
https://doi.org/10.5194/tc-9-1105-2015
© Author(s) 2015. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
https://doi.org/10.5194/tc-9-1105-2015
© Author(s) 2015. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
Modelling glacier change in the Everest region, Nepal Himalaya
International Centre for Integrated Mountain Development, Kathmandu, Nepal
W. W. Immerzeel
International Centre for Integrated Mountain Development, Kathmandu, Nepal
Department of Physical Geography, Utrecht University, Utrecht, the Netherlands
P. Wagnon
International Centre for Integrated Mountain Development, Kathmandu, Nepal
IRD/UJF – Grenoble 1/CNRS/G-INP, LTHE UMR 5564, LGGE UMR 5183, Grenoble, 38402, France
C. Vincent
UJF – Grenoble 1/CNRS, Laboratoire de Glaciologie et Géophysique de l'Environnement (LGGE) UMR 5183, Grenoble, 38041, France
S. Bajracharya
International Centre for Integrated Mountain Development, Kathmandu, Nepal
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- Trends and variability in streamflow and snowmelt runoff timing in the southern Tianshan Mountains Y. Shen et al. 10.1016/j.jhydrol.2017.12.035
- Variations in near‐surface debris temperature through the summer monsoon on Khumbu Glacier, Nepal Himalaya M. Gibson et al. 10.1002/esp.4425
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- Sub-alpine trees testify late 20th century rapid retreat of Gangotri glacier, Central Himalaya J. Singh et al. 10.1016/j.quaint.2020.08.052
- Glacial Lake Evolution (1962–2018) and Outburst Susceptibility of Gurudongmar Lake Complex in the Tista Basin, Sikkim Himalaya (India) A. Chowdhury et al. 10.3390/w13243565
- Debris Emergence Elevations and Glacier Change J. Shea et al. 10.3389/feart.2021.709957
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Short summary
A glacier mass balance and redistribution model that integrates field observations and downscaled climate fields is developed to examine glacier sensitivity to future climate in the Everest region of Nepal. The modelled sensitivity of glaciers to future climate change is high, and glacier mass loss is sustained through the 21st century for both middle- and high-emission scenarios. Projected temperature increases will expose large glacier areas to melt and reduce snow accumulations.
A glacier mass balance and redistribution model that integrates field observations and...