Articles | Volume 18, issue 4
https://doi.org/10.5194/gmd-18-977-2025
https://doi.org/10.5194/gmd-18-977-2025
Model description paper
 | 
21 Feb 2025
Model description paper |  | 21 Feb 2025

FESOM2.1-REcoM3-MEDUSA2: an ocean–sea ice–biogeochemistry model coupled to a sediment model

Ying Ye, Guy Munhoven, Peter Köhler, Martin Butzin, Judith Hauck, Özgür Gürses, and Christoph Völker

Viewed

Total article views: 4,683 (including HTML, PDF, and XML)
HTML PDF XML Total Supplement BibTeX EndNote
3,542 982 159 4,683 117 175 269
  • HTML: 3,542
  • PDF: 982
  • XML: 159
  • Total: 4,683
  • Supplement: 117
  • BibTeX: 175
  • EndNote: 269
Views and downloads (calculated since 06 Sep 2023)
Cumulative views and downloads (calculated since 06 Sep 2023)

Viewed (geographical distribution)

Total article views: 4,683 (including HTML, PDF, and XML) Thereof 4,571 with geography defined and 112 with unknown origin.
Country # Views %
  • 1
1
 
 
 
 

Cited

Saved (final revised paper)

Latest update: 18 Aug 2026
Download
Short summary
Many biogeochemistry models assume all material reaching the seafloor is remineralized and returned to solution, which is sufficient for studies on short-term climate change. Under long-term climate change, the carbon storage in sediments slows down carbon cycling and influences feedbacks in the atmosphere–ocean–sediment system. This paper describes the coupling of a sediment model to an ocean biogeochemistry model and presents results under the pre-industrial climate and under CO2 perturbation.
Share