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The Gulf Stream is a powerful western boundary current in the North Atlantic Ocean that strongly influences the climate of the East Coast of the United States and many Western European countries. Click the image for a larger view.
Some scientists believe that prior temperature anomalies have already begun to alter and slow the Gulf Stream and the balance of the currents circulating through the Atlantic over the past 100 years or so. The temperature of surface ocean water can vastly affect the temperature of nearby land areas. In a short-term example, people along the New England coast notice the routine chilling effect the cold Labrador Current and a sea breeze have on their weather during a number of days in the spring.