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

Viewed

Total article views: 4,729 (including HTML, PDF, and XML)
HTML PDF XML Total Supplement BibTeX EndNote
3,230 1,349 150 4,729 319 95 145
  • HTML: 3,230
  • PDF: 1,349
  • XML: 150
  • Total: 4,729
  • Supplement: 319
  • BibTeX: 95
  • EndNote: 145
Views and downloads (calculated since 10 Jun 2025)
Cumulative views and downloads (calculated since 10 Jun 2025)

Viewed (geographical distribution)

Total article views: 4,729 (including HTML, PDF, and XML) Thereof 4,689 with geography defined and 40 with unknown origin.
Country # Views %
  • 1
1
 
 
 
 

Cited

Saved (final revised paper)

Latest update: 09 Aug 2026
Download
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.
Share