Articles | Volume 30, issue 7
https://doi.org/10.5194/hess-30-1849-2026
https://doi.org/10.5194/hess-30-1849-2026
Research article
 | 
08 Apr 2026
Research article |  | 08 Apr 2026

Increasing glacier runoff in northwestern Greenland simulated from 1950 to 2023

Ken Kondo and Koji Fujita

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Short summary
Increased runoff due to ice melt in Greenland contributes to sea-level rise and flooding in coastal settlements. We reconstructed glacier runoff in northwestern Greenland in 1950–2023. Long-term modeling shows a recent increase in runoff linked to changes in atmospheric circulation, characterized by enhanced northward transport of heat and moisture. The results highlight a strong influence of atmospheric variability on glacier runoff and its impacts on local communities in northern Greenland.
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