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Liu, Wei; Fedorov, Alexey; Sevellec, Florian. |
We explore the mechanisms by which Arctic sea ice decline affects the Atlantic meridional overturning circulation (AMOC) in a suite of numerical experiments perturbing the Arctic sea ice radiative budget within a fully coupled climate model. The imposed perturbations act to increase the amount of heat available to melt ice, leading to a rapid Arctic sea ice retreat within 5 years after the perturbations are activated. In response, the AMOC gradually weakens over the next similar to 100 years. The AMOC changes can be explained by the accumulation in the Arctic and subsequent downstream propagation to the North Atlantic of buoyancy anomalies controlled by temperature and salinity. Initially, during the first decade or so, the Arctic sea ice loss results in... |
Tipo: Text |
Palavras-chave: Arctic; Meridional overturning circulation; Climate models. |
Ano: 2019 |
URL: https://archimer.ifremer.fr/doc/00599/71107/69388.pdf |
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