Stefan Rahmstorf – Evidence for a weakening Atlantic Ocean overturning circulation
Climate Change Research Centre (CCRC) 4th Floor, Matthews Building, UNSW, KensingtonPossible 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