Articles | Volume 18, issue 10
https://doi.org/10.5194/essd-18-7253-2026
© Author(s) 2026. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
https://doi.org/10.5194/essd-18-7253-2026
© Author(s) 2026. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Weather station data from the Mount Everest region, Nepal: 3810–8810 m above sea level
Arbindra Khadka
CORRESPONDING AUTHOR
Central Department of Hydrology and Meteorology, Tribhuvan University, Kirtipur, Nepal
Université Grenoble Alpes, CNRS, IRD, IGE, Grenoble, France
Lester Baker Perry
Department of Geography (Climatology), University of Nevada, Reno, Nevada, USA
Research Institute for Environment, Energy, and Economics, Department of Sustainable Technology & the Built Environment, Appalachian State University, Boone, North Carolina
Tom Matthews
Department of Geography, King's College London, London, UK
Tenzing Gyalzen Sherpa
Khumbu Climbing Centre, Phortse, Nepal
Chitra Bahadur Shrestha
Central Department of Hydrology and Meteorology, Tribhuvan University, Kirtipur, Nepal
Dibas Shrestha
Central Department of Hydrology and Meteorology, Tribhuvan University, Kirtipur, Nepal
Deepak Aryal
Central Department of Hydrology and Meteorology, Tribhuvan University, Kirtipur, Nepal
Subash Tuladhar
Department of Hydrology and Meteorology, Kathmandu, Nepal
Niraj Pradhananga
Department of Hydrology and Meteorology, Kathmandu, Nepal
Dinkar Kayastha
Department of Hydrology and Meteorology, Kathmandu, Nepal
Brian Raichle
Research Institute for Environment, Energy, and Economics, Department of Sustainable Technology & the Built Environment, Appalachian State University, Boone, North Carolina
Peter Athans
The North Face, Alameda, California
Dawa Yangzum Sherpa
The North Face, Alameda, California
Keith Garrett
Mount Washington Observatory, North Conway, New Hampshire, USA
Garrett Wheeler
Campbell Scientific, Logan, Utah, USA
Tom Young
RM Young, Traverse City, Michigan, USA
Aurora Elmore
National Oceanic and Atmospheric Administration, Maryland, USA
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Benjamin Graves, Tom Matthews, Tamsin Edwards, Richard Taylor, Megan James, Baker Perry, and Magali Ponds
EGUsphere, https://doi.org/10.5194/egusphere-2026-5187, https://doi.org/10.5194/egusphere-2026-5187, 2026
This preprint is open for discussion and under review for The Cryosphere (TC).
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The future of the world’s glaciers under climate change is simulated using models. However, the modelled response of glaciers to rising temperatures is stronger in some models than in others. This study compares the simulated behaviour of a glacier at high elevation using four models to compare how each one reacts to rising temperatures. Simple models respond more strongly than is realistic, because they do not account for the full range of environmental factors which affect the glacier.
Tom Matthews, Baker Perry, Ben Graves, Fanny Brun, Maria Sanolaria-Otin, Navaraj Pokhrel, Arbindra Khadka, Dibas Shrestha, Ludving Cano, Aris Kwadijk, Walter Immereel, Brandt Maxwell, and Anton Seimon
EGUsphere, https://doi.org/10.5194/egusphere-2026-5200, https://doi.org/10.5194/egusphere-2026-5200, 2026
This preprint is open for discussion and under review for The Cryosphere (TC).
Short summary
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Extreme precipitation shapes hazards and water resources in high mountains, but is rarely observed directly. On 4 October 2025, weather stations on Mt. Everest recorded one of the most extreme snowfall events ever measured. The storm revealed that Himalayan snowfall extremes can be far larger than previously documented, and that intense snowfall can cool the atmosphere sufficiently to prevent rain at impact-sensitive elevations, complicating the picture of how warming will affect future storms.
Megan C. James, Tamsin L. Edwards, Tom Matthews, Alexander T. Bradley, James F. O'Neill, and Harry Zekollari
EGUsphere, https://doi.org/10.5194/egusphere-2026-2069, https://doi.org/10.5194/egusphere-2026-2069, 2026
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As the climate warms, glaciers are shrinking, contributing to sea-level rise, natural hazards and water insecurity. We show for one case study – the very long-term response of Iceland’s glaciers to global warming – that large uncertainties arise from the poorly known parameters within models. This is usually overlooked, but we show neglecting it underestimates uncertainty in our glacier model by as much as 90 %, highlighting the importance of accounting for it in future glacier projections.
Sunil N. Oulkar, Matthew W. Peacey, Michael Mitrev, Duncan J. Quincey, Bryn Hubbard, Tom Matthews, Ankita S. Oulkar, Katie E. Miles, and Ann V. Rowan
Geosci. Instrum. Method. Data Syst., 15, 75–88, https://doi.org/10.5194/gi-15-75-2026, https://doi.org/10.5194/gi-15-75-2026, 2026
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We designed and tested a system that can record and send data in near real time from extreme and remote locations, such as Mount Everest. Using solar power and satellite communication, the system worked reliably at high altitude, showing it can be applied in other remote regions. This approach will help scientists collect vital information on how the environment is changing in areas that are normally very difficult to study.
Motilal Ghimire, Dibas Shrestha, Raju Chauhan, Amrit Thapa, Til Prasad Pangali Sharma, Krishna Prasad Sharma, Sher Bahadur Gurung, Sundar Devkota, Prabin Bhandari, Sikesh Koirala, Yanhong Wu, Niroj Timalsina, and Jeevan Kutu
The Cryosphere, 20, 551–572, https://doi.org/10.5194/tc-20-551-2026, https://doi.org/10.5194/tc-20-551-2026, 2026
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In the Upper Karnali Basin, a critical water source for millions of people, snow and glaciers are shrinking, and snowlines have shifted as temperatures rise over the last two decades. Snow and glacier decline has threatened water supplies for farming, drinking, and hydropower. This study shows how climate change is reshaping the region’s frozen landscapes, risking water security for communities downstream. Protecting these icy reservoirs is vital to safeguarding lives and ecosystems.
Navaraj Pokhrel, Patrick Wagnon, Fanny Brun, Arbindra Khadka, Tom Matthews, Audrey Goutard, Dibas Shrestha, Baker Perry, and Marion Réveillet
The Cryosphere, 18, 5913–5920, https://doi.org/10.5194/tc-18-5913-2024, https://doi.org/10.5194/tc-18-5913-2024, 2024
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We studied snow processes in the accumulation area of Mera Glacier (central Himalaya, Nepal) by deploying a cosmic ray counting sensor that allows one to track the evolution of snow water equivalent. We suspect significant surface melting, water percolation, and refreezing within the snowpack, which might be missed by traditional mass balance surveys.
Maximillian Van Wyk de Vries, Tom Matthews, L. Baker Perry, Nirakar Thapa, and Rob Wilby
Geosci. Model Dev., 17, 7629–7643, https://doi.org/10.5194/gmd-17-7629-2024, https://doi.org/10.5194/gmd-17-7629-2024, 2024
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This paper introduces the AtsMOS workflow, a new tool for improving weather forecasts in mountainous areas. By combining advanced statistical techniques with local weather data, AtsMOS can provide more accurate predictions of weather conditions. Using data from Mount Everest as an example, AtsMOS has shown promise in better forecasting hazardous weather conditions, making it a valuable tool for communities in mountainous regions and beyond.
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Editorial statement
This paper presents a quality-controlled meteorological dataset from six automatic weather stations spanning almost 5,000 m of elevation in the Mount Everest region, from 3,810 to 8,810 m above sea level. The installation and maintenance required to gather this data presents and exceptional effort. These rare observations from some of the highest elevations on Earth provide a valuable resource for investigating high-altitude climate and weather, evaluating atmospheric models and reanalyses, and improving our understanding of the Himalayan climate system.
This paper presents a quality-controlled meteorological dataset from six automatic weather...
Short summary
We installed six automatic weather stations from 3,810 m to 8,810 m on Mount Everest region to better understand weather conditions at high altitudes. These measurements reveal how temperature, humidity, and wind changes with height and season. Our results show differences between observations and widely used ERA5 datasets. This improved knowledge helps scientists better understand mountain weather and climate, climate change and supports water resource planning for communities downstream.
We installed six automatic weather stations from 3,810 m to 8,810 m on Mount Everest region to...
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