Mid-depth warming in the equatorial Atlantic Ocean serves as a fingerprint of a slowdown of the Atlantic Meridional Overturning Circulation on decadal scales, according to ocean model experiments, and has emerged from natural variability in the early 2000s.
Mid-depth warming in the equatorial Atlantic Ocean serves as a fingerprint of a slowdown of the Atlantic Meridional Overturning Circulation on decadal scales, according to ocean model experiments, and has emerged from natural variability in the early 2000s.
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