Articles | Volume 17, issue 1
https://doi.org/10.5194/os-17-59-2021
https://doi.org/10.5194/os-17-59-2021
Research article
 | 
13 Jan 2021
Research article |  | 13 Jan 2021

Antarctic Bottom Water and North Atlantic Deep Water in CMIP6 models

Céline Heuzé

Viewed

Total article views: 5,076 (including HTML, PDF, and XML)
HTML PDF XML Total BibTeX EndNote
3,562 1,427 87 5,076 129 80
  • HTML: 3,562
  • PDF: 1,427
  • XML: 87
  • Total: 5,076
  • BibTeX: 129
  • EndNote: 80
Views and downloads (calculated since 10 Jul 2020)
Cumulative views and downloads (calculated since 10 Jul 2020)

Viewed (geographical distribution)

Total article views: 5,076 (including HTML, PDF, and XML) Thereof 4,664 with geography defined and 412 with unknown origin.
Country # Views %
  • 1
1
 
 
 
 

Cited

Discussed (final revised paper)

Latest update: 17 Apr 2024
Download
Short summary
Dense waters sinking by Antarctica and in the North Atlantic control global ocean currents and carbon storage. We need to know how these change with climate change, and thus we need accurate climate models. Here we show that dense water sinking in the latest models is better than in the previous ones, but there is still too much water sinking. This impacts how well models represent the deep ocean density and the deep currents globally. We also suggest ways to improve the models.