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Stefan Rahmstorf – Evidence for a weakening Atlantic Ocean overturning circulation
Stefan Rahmstorf – Evidence for a weakening Atlantic Ocean overturning circulation
Possible changes in Atlantic meridional overturning circulation (AMOC), sometimes referred to as the Gulf Stream System, provide a key source of uncertainty regarding future climate change. Maps of temperature trends over the twentieth century show a conspicuous region of cooling in the northern Atlantic, as well as excessive warming along the North American coast. Both... View Article