Editing Atlantic Ocean (section)

=== Gyres ===
{{oceanic gyres}}
The clockwise warm-water [[North Atlantic Gyre]] occupies the northern Atlantic, and the counter-clockwise warm-water [[South Atlantic Gyre]] appears in the southern Atlantic.<ref name="USN-2001" />

In the North Atlantic, surface circulation is dominated by three inter-connected currents: the [[Gulf Stream]] which flows north-east from the North American coast at [[Cape Hatteras]]; the [[North Atlantic Current]], a branch of the Gulf Stream which flows northward from the [[Grand Banks of Newfoundland|Grand Banks]]; and the [[Subpolar Front]], an extension of the North Atlantic Current, a wide, vaguely defined region separating the subtropical gyre from the subpolar gyre. This system of currents transports warm water into the North Atlantic, without which temperatures in the North Atlantic and Europe would plunge dramatically.<ref>{{Harvnb|Marchal|Waelbroeck|Colin de Verdière|2016|loc=Introduction, pp. 1545–1547}}</ref>

[[File:North Atlantic Circulation.gif|thumb|In the subpolar gyre of the North Atlantic warm subtropical waters are transformed into colder subpolar and polar waters. In the Labrador Sea this water flows back to the subtropical gyre.]]
North of the North Atlantic Gyre, the cyclonic [[North Atlantic Subpolar Gyre]] plays a key role in climate variability. It is governed by ocean currents from marginal seas and regional topography, rather than being steered by wind, both in the deep ocean and at sea level.<ref>{{Harvnb|Tréguier|Theetten|Chassignet|Penduff|2005|loc=Introduction, p. 757}}</ref>
The subpolar gyre forms an important part of the global [[thermohaline circulation]]. Its eastern portion includes [[Eddy (fluid dynamics)|eddying]] branches of the [[North Atlantic Current]] which transport warm, saline waters from the subtropics to the northeastern Atlantic. There this water is cooled during winter and forms return currents that merge along the eastern continental slope of Greenland where they form an intense (40–50&nbsp;[[Sverdrup|Sv]]) current which flows around the continental margins of the [[Labrador Sea]]. A third of this water becomes part of the deep portion of the [[North Atlantic Deep Water]] (NADW). The NADW, in turn, feeds the [[meridional overturning circulation]] (MOC), the northward heat transport of which is threatened by anthropogenic climate change. Large variations in the subpolar gyre on a decade-century scale, associated with the [[North Atlantic oscillation]], are especially pronounced in [[Labrador Sea Water]], the upper layers of the MOC.<ref>{{Harvnb|Böning|Scheinert|Dengg|Biastoch|2006|loc=Introduction, p. 1; Fig. 2, p. 2}}</ref>

The South Atlantic is dominated by the anti-cyclonic southern subtropical gyre. The [[South Atlantic Central Water]] originates in this gyre, while [[Antarctic Intermediate Water]] originates in the upper layers of the circumpolar region, near the [[Drake Passage]] and the Falkland Islands. Both these currents receive some contribution from the Indian Ocean. On the African east coast, the small cyclonic [[Angola Gyre]] lies embedded in the large subtropical gyre.<ref>{{Harvnb|Stramma|England|1999|loc=Abstract}}</ref>
The southern subtropical gyre is partly masked by a wind-induced [[Ekman layer]]. The residence time of the gyre is 4.4–8.5&nbsp;years. [[North Atlantic Deep Water]] flows southward below the [[thermocline]] of the subtropical gyre.<ref>{{Harvnb|Gordon|Bosley|1991|loc=Abstract}}</ref>