North Equatorial Current play an important role in water-mass exchange. It also plays an essential role in water and heat exchange between the tropical and subtropical gyres.
The North Equatorial Current got its name from the fact that it is north of the equator and vise versa with the South Equatorial Current, the fact that it is South of the Equator.
North Equatorial flow clockwise and southern counter-clockwise.
the wind direction is different
Cameroon to the north and east. Gabon to the south and east.
Cameroon to the north and east. Gabon to the south and east.
The North Equatorial Current got its name from the fact that it is north of the equator and vise versa with the South Equatorial Current, the fact that it is South of the Equator.
As it is called the 'North Equatorial Current' the name would suggest that it is located North of the equator, in the Northern hemisphere.
Probably by what kind of current they get there.
They are complimentary the gulf stream caries warm surface waters north. The north equatorial current carries cold deep waters south.
north equatorial
North Equatorial Current
North Equatorial flow clockwise and southern counter-clockwise.
How do currents that flow along the west coast of continents compare with Currents that flow along the east coasts of continents
false, it begins in Florida.The Gulf Stream is a warm-water current. It begins in Florida and flows in a generally northeastern direction. The Gulf Stream is part of a larger current system that includes the North Atlantic Current, the Canary Current, and the North Equatorial 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.
the wind direction is different
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.