Scientific Reports (Sep 2023)

AMOC decline and recovery in a warmer climate

  • Paulo Nobre,
  • Sandro F. Veiga,
  • Emanuel Giarolla,
  • André L. Marquez,
  • Manoel B. da Silva,
  • Vinícius B. Capistrano,
  • Marta Malagutti,
  • Julio P. R. Fernandez,
  • Helena C. Soares,
  • Marcus J. Bottino,
  • Paulo Y. Kubota,
  • Silvio N. Figueroa,
  • José P. Bonatti,
  • Gilvan Sampaio,
  • Fernanda Casagrande,
  • Mabel C. Costa,
  • Carlos A. Nobre

DOI
https://doi.org/10.1038/s41598-023-43143-5
Journal volume & issue
Vol. 13, no. 1
pp. 1 – 12

Abstract

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Abstract This study presents novel insight into the mechanisms of Atlantic Meridional Overturning Circulation (AMOC) reduction and its recovery under a warmer climate scenario. An one-thousand-year-long numerical simulation of a global coupled ocean–ice–atmosphere climate model, subjected to a stationary atmospheric radiative forcing, depict a coherent picture of the Arctic sea ice melting as a trigger for the initial AMOC reduction, along with decreases in the northward fluxes of salt and heat. Further atmospheric-driven ocean processes contribute to an erosion of the stable stratification of the fresher, yet colder waters in the surface layers of the North Atlantic, contributing to the recovery of a permanently altered AMOC.