Atlantic Ocean
The Gulf Stream is a powerful current in the Atlantic Ocean. It starts in the Gulf of Mexico and flows into the Atlantic at the tip of Florida, accelerating along the eastern coastlines of the United States and Newfoundland.  The Gulf Stream, located along the eastern coast of the United States, is a fast, intense current known as a western-boundary current. These currents are located on the western side of every ocean basin. The Gulf Stream is a result of the wind pattern acting on most of the North Atlantic Ocean. The combination of the Trade Winds (10°- 25°N) blowing to the west and the Westerlies (35°- 55°N) blowing to the east cause the North Atlantic to rotate clockwise. Along the east coast of Florida the current is fed by the Antilles Current, and the flow, now called the Gulf Stream, runs parallel to the coast until reaching Cape Hatteras where it leaves the coast and enters deeper water. While flowing in deep water the Stream often forms large meanders or flucuations in its path. The Gulf Stream is a strong, fast moving, warm ocean current that originates in the Gulf of Mexico and flows into the Atlantic Ocean. It makes up a portion of the North Atlantic Subtropical Gyre. The majority of the Gulf Stream is classified as a western boundary current. The North Atlantic Current then flows further north and feeds the Norwegian Current and moves the relatively warm water along the west coast of Europe. The rest of the Gulf Stream flows into the Canary Current which moves along the eastern side of the Atlantic Ocean and back south to the equator. The Gulf Stream Current—the main conveyor of heat from south to north in the Atlantic—swirls surface waters in this infrared image from the Suomi NPP satellite on April 16, 2013, centered around 180 miles due east of Atlantic City, NJ. It moves north along the coast of Florida and then turns eastward off of North Carolina, flowing northeast across the Atlantic. Off the Atlantic seaboard of the United States, the Gulf Stream flows at a rate nearly 300 times faster than the typical flow of the Amazon River. The Gulf Streamthe second largest ocean current, after the Antarctic Circumpolar Current The Gulf Stream has its source in the warm waters of the eastern part of the Gulf of Mexico. These waters pass through the Straits of Florida to become the Gulf Stream, which flows northeastward from approximately Cape Hatteras, North Carolina, across the Atlantic toward Europe. At its greatest the Gulf Stream is approximately 100 miles wide and several hundred feet deep -- far larger than any river on earth.  While flowing in this deeper ocean water, the Gulf Stream is its most powerful (at about 150 Sverdrups), forms large meanders, and splits into several currents, the largest of which is the North Atlantic Current. The North Atlantic Current then flows further north and feeds the Norwegian Current and moves the relatively warm water along the west coast of Europe. The rest of the Gulf Stream flows into the Canary Current which moves along the eastern side of the Atlantic Ocean and back south to the equator. The Gulf Stream, together with its northern extension towards Europe, the North Atlantic Drift, is a powerful, warm, and swift Atlantic ocean current that originates at the tip of Florida, and follows the eastern coastlines of the United States and Newfoundland before crossing the Atlantic Ocean. The North Atlantic Current of the Gulf Stream, along with similar warm air currents, helps keep Ireland and the western coast of Great Britain a couple of degrees warmer than the east. However, the difference is most dramatic in the western coastal islands of Scotland. Today, it is understood that the waters feeding into the Gulf Stream begin flowing off the west coast of Northern Africa (map) . There, the Atlantic North Equatorial Current flows from that continent across the Atlantic Ocean. The North Atlantic Current then flows further north and feeds the Norwegian Current and moves the relatively warm water along the west coast of Europe. The rest of the Gulf Stream flows into the Canary Current which moves along the eastern side of the Atlantic Ocean and back south to the equator. The Gulf Stream is one of the strong ocean currents that carries warm water from the sunny tropics to higher latitudes. The current stretches from the Gulf of Mexico up the East Coast of the United States, departs from North America south of the Chesapeake Bay, and heads across the Atlantic to the British Isles. In the Atlantic, warm, high-salinity water flows northward in the Gulf Stream along the east coast of North America. Some of this water continues northeastward in the North Atlantic Current toward Iceland and Norway. Off the coast of Greenland, a portion of the surface water cools, becomes dense, and sink
http://www.livescience.com/26273-gulf-stream.html http://marine.coastal.edu/gulfstream/p2.htm http://geography.about.com/od/physicalgeography/a/gulfstream.htm http://oceanservice.noaa.gov/facts/gulfstreamspeed.html http://robinsonlibrary.com/geography/oceanography/dynamics/gulf.htm http://geography.about.com/od/physicalgeography/a/gulfstream.htm https://en.wikipedia.org/wiki/Gulf_stream http://geography.about.com/od/physicalgeography/a/gulfstream.htm http://www.earthlyissues.com/gulfstream.htm
where does the gulf stream flow