Global Glacier Melt Accelerating, New Study Projects Significant Mass Loss Through 2100
(EMBARGOED UNTIL NOVEMBER 15, 10:00 AM CEST)
Glaciers worldwide are shrinking at alarming rates, with dramatic implications for sea-level rise, water availability, biodiversity, and the stability of natural ecosystems. A new study, led by Harry Zekollari of the Vrije Universiteit Brussel’s Department of Water and Climate (research partly conducted while a postdoc at ETH Zurich’s Laboratory of Hydraulics, Hydrology and Glaciology), provides the most comprehensive and detailed projections of global glacier changes under the latest climate scenarios. This new research, published in The Cryosphere, projects the future evolution of every glacier on Earth outside of the Greenland and Antarctic ice sheets—a total of over 200,000 glaciers.
“By modeling all those glaciers’ evolution through the 21st century under various climate scenarios, we revealed reveals stark differences in outcomes based on future emissions levels. In the most optimistic, low-emission scenario, glaciers are expected to lose around 25-29% of their mass by 2100. However, under a high-emission scenario, that figure rises significantly, with up to 46-54% of global glacier mass projected to vanish.” Zekollari explained.
The impacts are not uniformly distributed: some regions face far more severe losses. For example, glaciers in the European Alps are among the most vulnerable, projected to lose over 75% of their volume, with many at risk of complete disappearance under high-emission scenarios. By contrast, glaciers in polar regions like Arctic Canada, Iceland, and Svalbard are expected to retain a more substantial part of their mass through the end of the century, though they, too, will face considerable loss.
“Our study represents a shift from prior assessments, showing slightly higher projected losses than those included in recent IPCC reports. These new projections rely on advanced models which are calibrated with detailed, glacier-specific observations rather than regionally aggregated data. This refined approach offers a clearer picture of how individual glaciers are likely to evolve, allowing for more precise projections relevant to local water resources, natural hazards, and glacier-fed hydropower systems.” Zekollari concludes.
Looking ahead, advancements in satellite monitoring and machine learning applications in glacier modelling are expected to enhance the accuracy of glacier projections. These tools will offer valuable new data to inform the science community’s understanding of glaciers’ response to climate change and improve planning for affected regions worldwide.
Full reference:
Zekollari, H., Huss, M., Schuster, L., Maussion, F., Rounce, D. R., Aguayo, R., Champollion, N., Compagno, L., Hugonnet, R., Marzeion, B., Mojtabavi, S., and Farinotti, D.: Twenty-first century global glacier evolution under CMIP6 scenarios and the role of glacier-specific observations, The Cryosphere 2024, 18, 5045–5066, https://doi.org/10.5194/tc-18-5045-2024
Contact:
Harry Zekollari, harry.zekollari@vub.be, +3226293021
