The North Atlantic Current (also known as North Atlantic Drift and North Atlantic Sea Movement) is a powerful warm ocean current that continues the Gulf Stream northeast. West of Continental Europe it splits into two major branches. One branch goes southeast, later to become the Canary Current as it passes northwest Africa and turns southwest. The other major branch continues north along the coast of northwestern Europe. It is thought to have a considerable warming influence on the climate, although a minority have disputed this. Other branches include the Irminger Current and the Norwegian Current. Driven by the global thermohaline circulation (THC), the North Atlantic Current is also often considered part of the wind-driven Gulf Stream which goes further east and north from the North American coast, across the Atlantic and into the Arctic Ocean.
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“I am fearful when I see people substituting fear for reason.”
—Edmund H. North (1911–1990)
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“We set up a certain aim, and put ourselves of our own will into the power of a certain current. Once having done that, we find ourselves committed to usages and customs which we had not before fully known, but from which we cannot depart without giving up the end which we have chosen. But we have no right, therefore, to claim that we are under the yoke of necessity. We might as well say that the man whom we see struggling vainly in the current of Niagara could not have helped jumping in.”
—Anna C. Brackett (1836–1911)