Abstract
Antarctic Bottom Water (AABW) is derived from dense water that sinks from the Antarctic continental shelf to the deep ocean. The sinking of AABW is balanced by a return flow of lighter water, and the resulting overturning circulation determines the density stratification of the deep ocean, regulates ocean storage of heat and carbon, and supplies oxygen to the deep sea. In this Review, we highlight progress in understanding how and why AABW is changing and the consequences for the deep overturning circulation. Since the mid-1980s, ocean heat content below 4,000 dbar has increased at a rate of 12.9 (±1.8) trillion watts, and the AABW has thinned by more than 50 dbar decade−1, with more rapid thinning observed closer to the sources of AABW. The abyssal overturning circulation has slowed in response to freshening of shelf waters by glacial melt and changes in sea ice formation. Numerical model simulations indicate that these trends will accelerate under projected increases in meltwater input. Future research priorities include sustained observations in the deep ocean and on the Antarctic continental shelf; exploration of feedbacks between ocean circulation, sea ice, dense water formation and ice shelf melt; and improved representation of AABW in ocean and climate models.
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Acknowledgements
G.C.J. was supported by NOAA Global Ocean Monitoring and Observation Program and NOAA Research (PMEL Contribution Number 5771). A.L.S. was supported by the National Aeronautics and Space Administration ROSES Physical Oceanography programme under grant number 80NSSC23K0357. S.R.R. and A.F. were supported by the Australian Antarctic Program Partnership (AAPP), through grant funding from the Australian Government as part of the Antarctic Science Collaboration Initiative programme. A.S. acknowledges funding from NERC (NE/V014285/1). A.K.M. and M.H.E. were supported by Australian Research Council (ARC) Discovery projects DP190100494 and DP250100759, and by the ARC Special Research Initiative, Australian Centre for Excellence in Antarctic Science (SR200100008). S.N. was supported by Grants-in-Aids for Scientific Research (24K15266 and 25H00002) of the Ministry of Education, Culture, Sports, Science and Technology in Japan. The authors also acknowledge support from the National Computational Infrastructure (NCI Australia) and Australian Community Climate and Earth System Simulator National Research Infrastructure (ACCESS-NRI), both funded by the Australian Government’s National Collaborative Research Infrastructure Strategy. The authors thank L. Bell for drafting the figures. The authors acknowledge the use of the CSIRO Marine National Facility in undertaking this research.
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S.R.R., G.C.J., S.Z., Q.L., A.K.M, A.S. and S.N. researched data for the article. S.R.R., A.L.S, G.C.J., S.Z., A.F., Q.L., A.K.M., A.S., K.L.G., M.H.E. and S.A. contributed substantially to the discussion of the content. S.R.R., A.L.S, G.C.J., S.Z., A.F., Q.L., A.K.M. and S.N. wrote the article. All authors reviewed and/or edited the manuscript before submission.
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Glossary
- Baroclinic instabilities
-
Dynamical instabilities involving release of potential energy of the mean flow to form time-varying eddies in the ocean or weather systems in the atmosphere.
- Diapycnal
-
A process that moves water across density surfaces.
- El Niño
-
A climate pattern involving interactions between the ocean and atmosphere in the tropical Pacific that oscillates irregularly over 2–7-year cycles, with extensive impacts on temperature and rainfall over much of the globe.
- Isopycnals
-
Surfaces of constant seawater density.
- Overturning circulation
-
An ocean circulation feature involving flow in different directions at different depths, joining to form a loop, such as equatorward flow of Antarctic Bottom Water balanced by poleward flow of lighter water at shallower depths.
- Polynya
-
An area of open water surrounded by sea ice, usually formed by strong winds blowing sea ice offshore.
- Potential vorticity
-
A measure of the rotation of a fluid, equal to the dot product of the vorticity (swirling motion) and the stratification (change in density with depth); the potential vorticity of a column of fluid in the ocean or atmosphere is analogous to angular momentum and is approximately conserved following the flow.
- Sills
-
Low points in ocean ridges through which ocean currents can pass from one basin to another.
- Southern Annular Mode
-
An index tracking north–south movements of the strong westerly winds at mid-latitude to high-latitude of the southern hemisphere.
- Ventilate
-
Transport of surface waters and their physical and chemical properties (such as heat, oxygen and carbon dioxide) into the interior of the ocean.
- Water mass
-
A volume of ocean with similar physical or chemical characteristics, such as Antarctic Bottom Water.
- Winter Water
-
A volume of cold water formed at the sea surface by winter heat loss to the atmosphere.
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Rintoul, S.R., Stewart, A.L., Johnson, G.C. et al. Antarctic Bottom Water in a changing climate. Nat Rev Earth Environ 7, 86–102 (2026). https://doi.org/10.1038/s43017-025-00750-2
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DOI: https://doi.org/10.1038/s43017-025-00750-2


