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- The Greenland Sea is often viewed as the northern terminus of the Atlantic Meridional Overturning Circulation. It has also been proposed that the shutdown of open-ocean deep convection in the Labrador or Greenland Seas would substantially weaken the Atlantic Meridional Overturning Circulation.
www.nature.com › articles › s43247/021/00182-yHorizontal circulation across density surfaces contributes ...
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Apr 19, 2024 · Nature Geoscience - Mooring observations and hydrographic data suggest the Atlantic Meridional Overturning Circulation abyssal limb has weakened over the past two decades in the North...
Jun 8, 2021 · Our results suggest that the Arctic Ocean, not the Greenland Sea, is the northern terminus of the mean Atlantic Overturning Circulation; open-ocean deep convection, in either the Labrador...
- Rong Zhang, Matthew Thomas, Matthew Thomas
- 2021
Feb 25, 2021 · Nature Geoscience - The Atlantic Meridional Overturning Circulation (AMOC) is currently distinctly weaker than it has been for the last millennium, according to a synthesis of proxy...
- Levke Caesar, Levke Caesar, G. D. McCarthy, D. J. R. Thornalley, N. Cahill, Stefan Rahmstorf, Stefan...
- 2021
Dec 20, 2016 · The Atlantic Meridional Overturning Circulation (AMOC) is a massive, looped belt of water that connects the world’s oceans, carrying warm waters north and cold waters south. The system not...
- Emily Underwood
- 2016
In this scenario, a weakened AMOC would also slow down Arctic sea ice decline and delay the emergence of an ice-free Arctic by around 6 years, as well as preventing over 50% of sea ice loss on the edges of Labrador Sea, Greenland Sea, Barents Sea, and Sea of Okhotsk in the years 2061–2080.
Dec 13, 2016 · The most recent IPCC assessment report concludes that the Atlantic Meridional Overturning Circulation (AMOC) could weaken substantially, but is very unlikely to collapse in the 21 st century.
Oct 23, 2023 · First, the sea ice cover was reduced over the GIN Sea (Greenland, Iceland, and Norwegian Seas), which increased the heat loss to the atmosphere and enhanced the deep convection in the North Atlantic and, in turn, the AMOC [95,104].