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A comprehensive analysis of new ocean records, contributed to by ACSIS scientists, has revealed that the circulation of the Atlantic Ocean has slowed down since the so-called Little Ice Age (which ended in the mid 19th century). Melting of ice in the Arctic is thought to have contributed to the weakening of the Atlantic meridional overturning circulation (AMOC), and with human-induced global warming likely to cause more Arctic melting, scientists warn that further disruption could affect weather, sea levels and fish stocks in the future.

Findings in the new study imply North Atlantic circulation is more variable than previously thought, and suggests current climate models may have weaknesses in their simulation of the AMOC.

Read more about the AMOC

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