The Gulf Stream proper and the North Atlantic Drift
European discovery of the Gulf Stream dates to the 1513 expedition of Juan Ponce de León, after which it became widely used by Spanish ships sailing from the Caribbean to Spain. In 1786 Benjamin Franklin studied and mapped the current in detail. The Gulf Stream proper is a western-intensified current, largely driven by wind stress. The North Atlantic Drift, in contrast, is largely thermohaline circulation driven. By carrying warm water northeast across the Atlantic, it makes Western Europe (and especially Northern Europe) warmer than they otherwise would be. However, the extent of its contribution to the actual temperature differential between North America and Europe is a matter of dispute.
Normal behavior of the Gulf Stream
A river of sea water, called the Atlantic North Equatorial Current, flows westward off the coast of northern Africa. When this current interacts with the northeastern coast of South America, the current forks into two branches. One passes into the Caribbean Sea, while a second, the Antilles Current, flows north and east of the West Indies. These two branches rejoin north of the Straits of Florida.
Consequently, the resulting Gulf Stream is a strong ocean current, transporting about 1.4 petawatts of heat, equivalent to 100 times the world energy demand. It transports water at a rate of 30 million cubic meters per second (30 sverdrups) through the Florida Straits. After it passes Cape Hatteras, this rate increases to 80 million cubic meters per second. The volume of the Gulf Stream dwarfs all rivers that empty into the Atlantic combined, which barely total 0.6 million cubic meters per second. It is weaker, however, than the Antarctic Circumpolar Current.
Typically, the Gulf Stream is 80–150 km wide and 800–1200 m deep. The current velocity is fastest near the surface, with the maximum speed typically about 2.5 m/s (approx. 4.9 knots).
As it travels north, the warm water transported by the Gulf Stream undergoes evaporative cooling and brine exclusion. The cooling is wind driven: wind moving over the water cools it and also causes evaporation, leaving a saltier brine. In this process, the water increases in salinity and density, and decreases in temperature. These two processes produce water that is denser and colder (or, more exactly, water that is still liquid at a lower temperature). In the North Atlantic Ocean, the water becomes so dense that it begins to sink down through less salty and less dense water. (The convective action is not unlike that of a lava lamp.) This downdraft of heavy, cold and dense water becomes a part of the North Atlantic Deep Water, a southgoing stream.
Localized effects
North America
The Gulf Stream is influential on the climate of the east coast of Florida, especially southeast Florida(where it is often just a mile or two off the coast), helping to keep temperatures warmer than in the rest of the southeastern United States during the winter. During the summer, the effect is opposite but smaller. The Gulf Stream makes the climate of offshore islands of Massachusetts, Martha’s Vineyard, and Nantucket milder than that of Massachusetts Bay, which is isolated from Gulf Stream effects by Cape Cod.
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