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https://doi.org/10.5194/egusphere-2024-1760
© Author(s) 2024. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
https://doi.org/10.5194/egusphere-2024-1760
© Author(s) 2024. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Status: this preprint is open for discussion.
Brief Communication: Accurate and autonomous snow water equivalent measurements using a cosmic ray sensor on a Himalayan glacier
Abstract. We analyze snow water equivalent (SWE) measurements from a cosmic ray sensor (CRS) on the lower accumulation area of Mera Glacier (Central Himalaya, Nepal) between November 2019 and November 2021. The CRS aligned well with field observations and revealed accumulation in pre-monsoon and monsoon, followed by ablation in post-monsoon and winter. COSIPY simulations suggest significant surface melting, water percolation and refreezing within the snowpack, consistent with CRS observations, yet liable to be missed by surface mass balance surveys. We conclude that CRS can be used to complement more resource-intensive manual measurements to determine mass fluxes on remote, high-altitude Himalayan glaciers.
How to cite. Pokhrel, N., Wagnon, P., Brun, F., Khadka, A., Matthews, T., Goutard, A., Shrestha, D., Perry, B., and Réveillet, M.: Brief Communication: Accurate and autonomous snow water equivalent measurements using a cosmic ray sensor on a Himalayan glacier, EGUsphere [preprint], https://doi.org/10.5194/egusphere-2024-1760, 2024.
Publisher's note: Copernicus Publications remains neutral with regard to jurisdictional claims made in the text, published maps, institutional affiliations, or any other geographical representation in this preprint. The responsibility to include appropriate place names lies with the authors.
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Navaraj Pokhrel
CORRESPONDING AUTHOR
Univ. Grenoble Alpes, IRD, CNRS, INRAE, Grenoble INP, IGE, Grenoble, France
Central Department of Hydrology and Meteorology, Tribhuvan University, Kirtipur, Nepal
Patrick Wagnon
Univ. Grenoble Alpes, IRD, CNRS, INRAE, Grenoble INP, IGE, Grenoble, France
Fanny Brun
Univ. Grenoble Alpes, IRD, CNRS, INRAE, Grenoble INP, IGE, Grenoble, France
Arbindra Khadka
Univ. Grenoble Alpes, IRD, CNRS, INRAE, Grenoble INP, IGE, Grenoble, France
Central Department of Hydrology and Meteorology, Tribhuvan University, Kirtipur, Nepal
International Centre for Integrated Mountain Development, Kathmandu, Nepal
Tom Matthews
Department of Geography, King’s College London, London, United Kingdom
Audrey Goutard
Univ. Grenoble Alpes, IRD, CNRS, INRAE, Grenoble INP, IGE, Grenoble, France
Dibas Shrestha
Central Department of Hydrology and Meteorology, Tribhuvan University, Kirtipur, Nepal
Baker Perry
Department of Geography and Planning, Appalachian State University, Boone, North Carolina, USA
Marion Réveillet
Univ. Grenoble Alpes, IRD, CNRS, INRAE, Grenoble INP, IGE, Grenoble, France
Short summary
We studied snow processes in the accumulation area of Mera Glacier (Central Himalaya, Nepal) by deploying a cosmic ray counting sensor that allows to track the evolution of the snow water equivalent. We suspect significant surface melting, water percolation and refreezing within the snowpack, that might be missed by traditional mass balance surveys.
We studied snow processes in the accumulation area of Mera Glacier (Central Himalaya, Nepal) by...