Earth System Dynamics
Earth System Dynamics
ESD
Articles | Volume 16, issue 2
Articles | Volume 16, issue 2
https://doi.org/10.5194/esd-16-347-2025
© Author(s) 2025. This work is distributed under
the Creative Commons Attribution 4.0 License.
https://doi.org/10.5194/esd-16-347-2025
© Author(s) 2025. This work is distributed under
the Creative Commons Attribution 4.0 License.
Articles | Volume 16, issue 2
Research article
 | 
04 Mar 2025
Research article |  | 04 Mar 2025

Freshwater input from glacier melt outside Greenland alters modeled northern high-latitude ocean circulation

Jan-Hendrik Malles, Ben Marzeion, and Paul G. Myers

Viewed

Total article views: 574 (including HTML, PDF, and XML)
HTML PDF XML Total BibTeX EndNote
397 135 42 574 21 24
  • HTML: 397
  • PDF: 135
  • XML: 42
  • Total: 574
  • BibTeX: 21
  • EndNote: 24
Views and downloads (calculated since 18 Jun 2024)
Cumulative views and downloads (calculated since 18 Jun 2024)

Viewed (geographical distribution)

Total article views: 574 (including HTML, PDF, and XML) Thereof 515 with geography defined and 59 with unknown origin.
Country # Views %
  • 1
1
 
 
 
 
Latest update: 08 Mar 2025
Download
Short summary
Glaciers in the high-latitude Northern Hemisphere (outside Greenland) are losing mass at roughly half the Greenland ice sheet's rate. Still, this is usually not included in the freshwater input data for ocean circulation models. Also, the submarine melt of glaciers (outside the ice sheets) has not been quantified yet. We tackle both issues by using a glacier model's output as additional fresh water for the ocean model and by using the ocean model's output to model submarine melt.
Read more
Share
Altmetrics
Final-revised paper
Preprint