Antarctic Bottom Water (AABW)
node · earth · Southern Ocean and the abyssal basins of all three oceans
The densest water in the world ocean, and the one that fills the deepest basins of all three of them. It forms on Antarctic continental shelves where sea ice grows and rejects brine into water already near the freezing point; the resulting shelf water spills down the slope and spreads north along the bottom. There are four main production regions — the Weddell Sea, which is the largest, the Ross Sea, the Adélie Coast and Cape Darnley. Observations and models both indicate it is in retreat: Weddell Sea Bottom Water volume has fallen by around 30 per cent since 1992, and modelling work published in 2023 projects a substantial slowdown of the abyssal overturning cell driven by Antarctic meltwater freshening the shelf water at source.
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Timeline
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Connections · 2
- Weddell Seaoriginates_in
- Thermohaline Circulationpart_of
Assembled narrative · 1
Assembled from 26 blocks · 1 evidence · 48 related
- Story
- The densest water in the world ocean, and the one that fills the deepest basins of all three of them. It forms on Antarctic continental shelves where sea ice grows and rejects brine into water already near the freezing point; the resulting shelf water spills down the slope and spreads north along the bottom. There are four main production regions — the Weddell Sea, which is the largest, the Ross Sea, the Adélie Coast and Cape Darnley. Observations and models both indicate it is in retreat: Weddell Sea Bottom Water volume has fallen by around 30 per cent since 1992, and modelling work published in 2023 projects a substantial slowdown of the abyssal overturning cell driven by Antarctic meltwater freshening the shelf water at source.
- Knowledge
- Thermohaline Circulation
- Antarctic Bottom Water (AABW)
- Weddell Sea
- Connections
- Polynya
- North Atlantic Deep Water (NADW)
- Weddell Sea
- Thermohaline Circulation
- Antarctic meltwater is projected to slow the abyssal cell
- Antarctic Bottom Water (AABW)
- Southern Ocean
- Antarctic meltwater is projected to slow the abyssal cell
- Atlantic Meridional Overturning Circulation (AMOC)
- Coastal and Equatorial Upwelling
- Antarctic Bottom Water (AABW)
- Southern Ocean
- Argo Profiling Float Array
- Wallace Broecker
- The great ocean conveyor is drawn
- The Argo design array is completed
- IPCC AR6 assesses AMOC decline as very likely and collapse as unlikely this century
- Evidence
- Antarctic meltwater freshening shelf waters is projected to drive a substantial slowdown and warming of the abyssal overturning cell fed by Antarctic Bottom Water. Associated observational figures quoted here — an approximately 30 per cent decline in Weddell Sea Bottom Water volume since 1992 and a greater than 40 per cent decline in shelf sea-ice formation rate — come from adjacent studies summarised alongside it, not from this paper.
Observed changes · 0
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