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Observing The Atlantic Meridional Overturning Circulation Yields A Decade Of Inevitable Surprises

M. A. Srokosz, H. L. Bryden

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On the success (or not) of climate models Atlantic Meridional Overturning Circulation (AMOC) transports huge amounts of heat from low to high latitudes and has a major influence on climate. Climate models have predicted that global warming will cause the AMOC to slow, but concrete evidence of such a slowdown has been scarce. Srokosz and Bryden review a decade of observations of the AMOC that reveal an unexpected amount of variability over time scales from seasonal to decadal, as well as a general weakening over this time. Science , this issue 10.1126/science.1255575