Untangling the relationship between AMOC variability and North Atlantic upper�ocean temperature and salinity
The relationship between Atlantic meridional overturning circulation (AMOC) variability and high-latitude North Atlantic buoyancy changes is complicated by the latter both driving, and responding to, AMOC changes. A maximum covariance analysis applied to a 1,201-year preindustrial control simulation reveals two leading modes that separate these two distinct roles of North Atlantic temperature and salinity as related to AMOC variability. A linear combination of the two modes accounts for most of the variation of a widely used AMOC index. The same analysis applied to another control simulation known to possess two distinct regimes of AMOC variability-oscillatory and red-noise-suggests that the North Atlantic buoyancy-forced AMOC variability is present in both regimes but is weaker in the latter, and moreover there is pronounced multidecadal/centennial AMOC behavior in the latter regime that is unrelated to North Atlantic buoyancy forcing.
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http://n2t.net/ark:/85065/d78d00rm
eng
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publication
2016-01-01T00:00:00Z
publication
2021-07-28T00:00:00Z
Copyright 2021 American Geophysical Union.
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