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Chapter 9 Circulation of the Ocean

AB
coastal upwellingupwelling adjacent to coast, induced by wind
countercurrentsurface current flowing in opposite direction from adjacent surface current
currentmass flow of water
eddycircular movement of water
El Ninosouthward-flowing nutrient-poor current of warm water off the coast of South America
ENSOEl Nino and the Southern Oscillation
Gulf Streamlargest western boundary current
gyrecircuit of mid-latitude currents around periphery of ocean basin
La Ninawhen normal tropical Pacific circulation strengths and surface temperatures drop
surface currentwater flowing horizontally in upper waters of ocean surface
undercurrentcurrent flowing beneath a surfact current, in opposite direction
upwellingcirculation pattern w/ deep cold nutrient-laden water moves towards surface


High School Science teacher
Flanagan H.S.
Pembroke Pines, FL

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