Articles | Volume 17, issue 1
https://doi.org/10.5194/os-17-59-2021
© Author(s) 2021. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
https://doi.org/10.5194/os-17-59-2021
© Author(s) 2021. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Antarctic Bottom Water and North Atlantic Deep Water in CMIP6 models
Department of Earth Sciences, University of Gothenburg, Gothenburg, Sweden
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- Projected West Antarctic Ocean Warming Caused by an Expansion of the Ross Gyre F. Gómez‐Valdivia et al. 10.1029/2023GL102978
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- The Influence of Increased CO2 Concentrations on AMOC Interdecadal Variability Under the LGM Background Y. Gao et al. 10.1029/2023JD039976
3 citations as recorded by crossref.
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- Historical and Future Projected Warming of Antarctic Shelf Bottom Water in CMIP6 Models A. Purich & M. England 10.1029/2021GL092752
Discussed (final revised paper)
Latest update: 14 Nov 2024
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.
Dense waters sinking by Antarctica and in the North Atlantic control global ocean currents and...