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Record-breaking glacier mass loss in Central Asia in 2025

Lander Van TrichtState Key Laboratory of Hydrology-Water Resources and Hydraulic EngineeringMarin KneibState Key Laboratory of Hydrology-Water Resources and Hydraulic EngineeringMatthias HussSwiss Federal Institute for Forest, Snow and Landscape Research (WSL)Harry ZekollariLaboratory of Hydraulics, Hydrology and Glaciology (VAW), ETH ZürichErlan AzisovCentral Asian Institute of Applied Geosciences (CAIAG)Martina BarandunUniversity of FribourgSultan BelekovHydrometeorological Service under the Ministry of Emergency Situations of the Kyrgyz Republic (Kyrgyzhydromet)Joel FiddesMountain Futures GmbHMartin HoelzleUniversity of FribourgKabutov KhusravCenter for the Research of Glaciers, Tajik National Academy of SciencesVassiliy KapitsaCentral Asian Regional Glaciological CentreNikolay KassatkinCentral Asian Regional Glaciological CentreRuslan KenzhebaevCentral Asian Institute of Applied Geosciences (CAIAG)Adilet MakeshovTien Shan International Scientific CentreEnrico MatteaUniversity of FribourgE.S. MilesUniversity of FribourgHofiz NavruzshoevCenter for the Research of Glaciers, Tajik National Academy of SciencesMagali PondsDepartment of Water and Climate, Vrije Universiteit BrusselViktor PopovninLomonosov Moscow State UniversityOleg RybakEarth System Science and Departement Geografie, Vrije Universiteit BrusselTomas SaksUniversity of FribourgRysbek SatylkanovTien Shan International Scientific CentreGulomjon UmirzakovHydrometeorological Research InstituteYing XieMuztagh Ata Station for Westerly Environment Observation and Research, Chinese Academy of SciencesWei YangHydrometeorological Research InstituteDaniel FarinottiState Key Laboratory of Hydrology-Water Resources and Hydraulic Engineering
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Abstract The year 2025, designated by the United Nations as the ‘International Year of Glaciers’ Preservation’, ironically became the most negative glacier mass-balance year on record in Central Asia. In situ observations reveal exceptionally strong and spatially coherent ice losses across the region, although not all individual glaciers experienced record losses. Regional simulations with the Global Glacier Evolution Model support these findings, indicating that 64% of glaciers larger than 1 km 2 (∼4000 glaciers) reached their most negative annual mass balance within the study period. Within a single year, glaciers in Central Asia lost an estimated 30 ± 6 km 3 of ice (26 ± 9 Gt), corresponding to ∼2% of their present-day total mass. Mass loss was strongest in the western Tien Shan and western Pamir (−2% to −4%) and more moderate in the eastern Tien Shan and eastern Pamir (−1% to −1.5%). Climate reanalysis attributes the extreme 2025 losses to persistently above-average spring and summer temperatures, an unusually early onset of the melt season, and reduced snowfall frequency during late spring and summer. Together, these conditions enhanced melt-amplifying feedbacks by accelerating snow loss, leading to earlier exposure of low-albedo ice surfaces. The 2025 losses mark an alarming milestone for Central Asian glaciers and may become the new normal in the future.

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