Falkland Current (also called Malvinas Current or Falklands Current) is a cold water current that flows northward along the Atlantic coast of Patagonia as far north as the mouth of the Río de la Plata. This current results from the movement of water from the West Wind Drift as it rounds Cape Horn.
Norwegian Current (also known as the Norway Coastal Current) is one of two dominant arctic inflows of water. It can be traced from near Shetland, north of Scotland, otherwise from the eastern North Sea at depths of up to 100 metres. It finally passes the Opening into the Barents Sea, a large outcrop of the Arctic Ocean.
In the North Atlantic Ocean, the Cayenne current is joined and reinforced by the North Equatorial Current. This current heads north-westwards as a large mass of equatorial water into the Caribbean sea. This current is further split into two currents: The Florida current and The Gulf Stream. All of these currents are warm currents.