Tantalizing evidence for the glacial North Atlantic bottom water [Earth, Atmospheric, and Planetary Sciences]

The global Meridional Overturning Circulation (MOC) is one of the key components of the global climate system. Over timescales of 102 to 103 y, MOC connects the cold, carbon-rich waters in the deep ocean with warmer, carbon-poorer surface waters through localized deep water formation and more widespread upwelling of deep...

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