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Editorials | Environmental | February 2005  
Guide to Climate Change - The Gulf Stream
BBC


 1 Surface currents carry warm, salty water from the tropics. 2 The water cools, its density increases and it sinks to the deep ocean. 3 The cold water flows back to the equator, driving the "ocean conveyor" which in turn contributes to the Gulf Stream that warms northern Europe. 4 As ice melts, freshwater dilutes the warm salty water from the tropics. 5 The water becomes less dense so does not sink as fast, weakening the "conveyor" and therefore the Gulf Stream. | Gulf Stream
 Dramatic temperature shifts have happened in the past, driven partly by changes in a major ocean currents.
 A "great ocean conveyor" helps transport heat around the globe via surface and deep-sea movements of water.
 Scientists are exploring whether global warming might slow or shut it down - a scenario considered "low probability, high impact".
 This could disrupt mostly wind-driven surface currents such as the Gulf Stream, which brings milder weather to Northern Europe. | 
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