The North Atlantic Current is a vast, slow moving warm current. It is created from the Gulf Stream and the Labrador Current joining at southern Greenland, which creates the widening and slowing of the Gulf Stream. The North Atlantic Current splits near western Europe, one part creating the warm Norway Current flowing northward along the coast of Norway and the other creating the cold Canary Current deflecting southward, eventually warming and rejoining the North Equatorial Current.
There are many ocean currents of the north Atlantic.Here are some of the most well known and biggest. Labrador current flowing south through Greenland and Canada (cold water current). North Atlantic drift flowing along the east coast of America to all the way in between Iceland and Britain (warm water current) Canaries current flowing from Ireland all the way along the European and African coast to the Equator (cold water current). North Equatorial current flowing from south Brazil right up to The Caribbean and California (warm water current). Hope I helped
in europe
The "north Atlantic current" is very strong.I really like the "north Atlantic current."The "north Atlantic current" is driven by the global thermohaline circulation (THC), it is wind driven
That would be the North Atlantic Current.
No curret runs through the Sargasso Sea. The Sargasso Seais a region in the middle of the Atlantic Ocean|North Atlantic Ocean, surrounded by ocean currents. It is bounded on the west by the Gulf Stream; on the north, by the North Atlantic Current; on the east, by the Canary Current; and on the south, by the North Atlantic Equatorial Current. This system of currents forms the North Atlantic Subtropical Gyre.
north atlantic current
a surface current
the north Atlantic drift
North Atlantic Gyre
north atlantic ocean
How do currents that flow along the west coast of continents compare with Currents that flow along the east coasts of continents
The North Atlantic Current brings much warmer weather to Europe. This explains why Europe is some 15˚F warmer than areas of the same latitude.
north atlantic drift
gulf stream is