Abrupt cooling over the North Atlantic in modern climate models

Giovanni Sgubin (), Didier Swingedouw, Sybren Drijfhout, Yannick Mary and Amine Bennabi
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Giovanni Sgubin: Laboratoire des Sciences du Climat et de l'Environnement (LSCE), Institut Pierre Simon Laplace (IPSL)
Didier Swingedouw: Environnements et Paleoenvironnements Oceaniques et Continenteaux (EPOC), UMR CNRS 5805, Université de Bordeaux
Sybren Drijfhout: Royal Netherlands Meteorological Institute (KNMI)
Yannick Mary: Environnements et Paleoenvironnements Oceaniques et Continenteaux (EPOC), UMR CNRS 5805, Université de Bordeaux
Amine Bennabi: Institut de Mecanique et d'Ingenierie (I2M), Université de Bordeaux

Nature Communications, 2017, vol. 8, issue 1, 1-12

Abstract: Abstract Observations over the 20th century evidence no long-term warming in the subpolar North Atlantic (SPG). This region even experienced a rapid cooling around 1970, raising a debate over its potential reoccurrence. Here we assess the risk of future abrupt SPG cooling in 40 climate models from the fifth Coupled Model Intercomparison Project (CMIP5). Contrary to the long-term SPG warming trend evidenced by most of the models, 17.5% of the models (7/40) project a rapid SPG cooling, consistent with a collapse of the local deep-ocean convection. Uncertainty in projections is associated with the models’ varying capability in simulating the present-day SPG stratification, whose realistic reproduction appears a necessary condition for the onset of a convection collapse. This event occurs in 45.5% of the 11 models best able to simulate the observed SPG stratification. Thus, due to systematic model biases, the CMIP5 ensemble as a whole underestimates the chance of future abrupt SPG cooling, entailing crucial implications for observation and adaptation policy.

Date: 2017
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DOI: 10.1038/ncomms14375

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