The Angola Current is a water flow along southwest Africa. It used to be named the South Current because it flowed southward. Ten years after being named this they changed it to the Angola Current because it flows along the coast of Angola for a long distance and is strongest there. By changing it to the Angola Current it describes where is it located, not just what direction it flows.

The Angola Current forms the eastern part of a cyclonic gyre. In the upper layer it seems to be formed mostly by the southeast part of the South Equatorial Countercurrent and the southern waters from the north of the Benguela Current. On the other hand, in the laye

The Canary Current flows along the African coast north to south. It is wide and slow like most eastern boundary currents. It flows year round towards the equator. The surface waters are cool because as it travels south it entrains water from the coast. On average, the current is about 500 m deep and flows at a low speed. The Canary Island Archipelago is deeper than 3000 m. This is an obstacle to the movement of the Canary Current.

The Canary Current system contains coastal upwelling witch is when cold waters from below rise to the surface, and eddies witch is water moving contrary to the direction of the main current. The eddies have a length scale of 100 to 300 km.

Some topics in this essay:
Angola Current, Canary Current, Florida Current, Flam August, Hamilton Bank, Brazil Current, Circumpolar Current, Lea July, Baffin Bay, Cape Hatteras, angola current, florida current, canary current, cape hatteras, current flows, current malvinas current, straits florida, ocean currents, continental slope, labrador current, malvinas current, current canary current, currents angola current, straits florida cape, current labrador current,