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The Florida Current is a thermal ocean current that flows from the Straits of Florida around the Florida Peninsula and along the southeastern coast of the United States before joining the Gulf Stream Current near Cape Hatteras. Its contributing currents are the Loop Current and the Antilles Current. The current was discovered by Spanish ...
Surface temperatures in the western North Atlantic: Most of the North American landmass is black and dark blue (cold), while the Gulf Stream is red (warm). Source: NASA The Gulf Stream 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 ...
It transports more warm tropical water to northern latitudes than any other boundary current; more than 40 Sv (40 million m 3 /s; 1.4 billion cu ft/s) in the south and 20 Sv (20 million m 3 /s; 710 million cu ft/s) as it crosses the Mid-Atlantic Ridge. It reaches speeds of 2 knots (3.7 km/h; 2.3 mph; 1.0 m/s) near the North American coast ...
It includes off the coast of Florida, where water temperatures in the Florida Keys were close to 97 degrees in some spots last week. It is important because warm ocean water breeds stronger ...
“The warm Gulf Stream has shifted more east than usual, causing (sea surface temperatures) well below average,” the office said in a tweet. Temperatures 15 degrees below the norm were recorded ...
This week the surface ocean temperature of the some of the waters around Florida reached 100 degrees, near-hot tub heat levels.
The Gulf Stream separates from the US coast near Cape Hatteras (35°N, 75°W) and then travels eastwards across the North Atlantic, becoming the North Atlantic current at about 55°W. In the region between 75°W and 55°W it is subject to meanders and is frequently accompanied by eddies. The northern edge of the current is marked by a sharp ...
View of the currents surrounding the gyre. The North Atlantic Gyre of the Atlantic Ocean is one of five great oceanic gyres.It is a circular ocean current, with offshoot eddies and sub-gyres, across the North Atlantic from the Intertropical Convergence Zone (calms or doldrums) to the part south of Iceland, and from the east coasts of North America to the west coasts of Europe and Africa.