![]() History Benjamin Franklin's chart of the Gulf Stream printed in London in 1769Įuropean discovery of the Gulf Stream dates to the 1512 expedition of Juan Ponce de León, after which it became widely used by Spanish ships sailing from the Caribbean to Spain. Its presence has led to the development of strong cyclones of all types, both within the atmosphere and within the ocean. ![]() A consensus exists that the climate of Northwest Europe is warmer than other areas of similar latitude at least partially because of the strong North Atlantic Current. The Gulf Stream influences the climate of the coastal areas of the East Coast of the United States from Florida to southeast Virginia (near 36°N latitude), and to a greater degree, the climate of Northwest Europe. ![]() Around 40☀′N 30☀′W / 40.000°N 30.000°W / 40.000 -30.000, it splits in two, with the northern stream, the North Atlantic Drift, crossing to Northern Europe and the southern stream, the Canary Current, recirculating off West Africa. The process of western intensification causes the Gulf Stream to be a northward-accelerating current off the east coast of North America. The Gulf Stream, together with its northern extension the North Atlantic Drift, is a warm and swift Atlantic ocean current that originates in the Gulf of Mexico and flows through the Straits of Florida and up the eastern coastline of the United States, then veers east near 36°N latitude (North Carolina) and moves toward Northwest Europe as the North Atlantic Current. Surface temperatures in the western North Atlantic: The North American landmass is black and dark blue (cold), while the Gulf Stream is red (warm). For other uses, see Gulf Stream (disambiguation). ![]()
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