North Atlantic Current North Atlantic Current The North Atlantic Current (NAC), also known as North Atlantic Drift and North Atlantic Sea Movement, is a powerful warm western boundary current within the Atlantic Ocean that extends the Gulf Stream northeastward. The NAC originates from where the Gulf Stream turns north at the Southeast Newfoundland Rise, a submarine ridge that stretches southeast from the Grand Banks. The NAC flows northward east of the Grand Banks, from 40°N to 51°N, before turning sharply east to cross the Atlantic. It transports more warm tropical water to northern latitudes than any other boundary current; more than 40 Sv
Atlantic Europe parts of Scandinavia and the Baltic), resulting in similar landscapes with common endemic plant and animal species. From a strictly physical point of view most of the Atlantic European shoreline can be considered a single biogeographical region. Physical geographers label this biogeographical area as the "European Atlantic Domain", part of the Euro-Siberian botanic region. The Atlantic Bronze Age is a cultural complex of the Bronze Age period of approximately 1300–700 BC, that marked the economic and cultural exchange between the current territories of Portugal, Spain, France, Great Britain and Ireland. Via the Bell Beaker culture, Atlantic and Central Europe were