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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- Buoyancy forcing and the subpolar Atlantic meridional overturning circulation M. Buckley et al. 10.1098/rsta.2022.0181
- Last Interglacial subsurface warming on the Antarctic shelf triggered by reduced deep-ocean convection N. Yeung et al. 10.1038/s43247-024-01383-x
- Response of Northern North Atlantic and Atlantic Meridional Overturning Circulation to Reduced and Enhanced Wind Stress Forcing K. Lohmann et al. 10.1029/2021JC017902
- Finale: impact of the ORCHESTRA/ENCORE programmes on Southern Ocean heat and carbon understanding A. Meijers et al. 10.1098/rsta.2022.0070
- Future Response of Antarctic Continental Shelf Temperatures to Ice Shelf Basal Melting and Calving M. Thomas et al. 10.1029/2022GL102101
- Circum-Antarctic bottom water formation mediated by tides and topographic waves X. Han et al. 10.1038/s41467-024-46086-1
- Sensitivity of simulated water mass transformation on the Antarctic shelf to tides, topography and model resolution F. Boeira Dias et al. 10.3389/fmars.2023.1027704
- Projected West Antarctic Ocean Warming Caused by an Expansion of the Ross Gyre F. Gómez‐Valdivia et al. 10.1029/2023GL102978
- On the Origins of Open Ocean Oxygen Minimum Zones X. Davila et al. 10.1029/2023JC019677
- An Amundsen Sea source of decadal temperature changes on the Antarctic continental shelf S. Drijfhout et al. 10.1007/s10236-023-01587-3
- Decadal variability of oxygen uptake, export, and storage in the Labrador Sea from observations and CMIP6 models J. Koelling et al. 10.3389/fmars.2023.1202299
- 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.
- Development of the UKESM-TOPAZ Earth System Model (Version 1.0) and Preliminary Evaluation of its Biogeochemical Simulations H. Lee et al. 10.1007/s13143-021-00263-0
- Deep mixed ocean volume in the Labrador Sea in HighResMIP models T. Koenigk et al. 10.1007/s00382-021-05785-x
- 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: 13 Dec 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...