Ocean current

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An ocean current is a current that flows more or less permanently in one of the Earth's oceans.

Ocean currents may flow for thousands of kilometers. They are very important in determining the climates of the continents bordering on the oceans they flow in. The most striking example is the Gulf stream, which makes north-west Europe much more temperate than any other region at the same latitude. However the importance of currents is also illustrated by the [[El Ni�o]] effect, in which the temporary reversal of an ocean current causes devastating climatic change in South America, whose effects spread as far as Australia.

Currents that flow under the surface of the ocean, and are thus hidden from immediate detection, are called submarine rivers.

Ocean currents are also very important in the dispersal of many life forms. A dramatic example is the life-cycle of the eel.

Important currents include:

Contents 1 Arctic Ocean 2 Atlantic Ocean 3 Pacific Ocean 4 Indian Ocean 5 Southern Ocean 5.1 References

Arctic Ocean

• East Greenland Current
• Norwegian Current

Atlantic Ocean

• Benguela Current
• Guinea Current
• Gulf stream

Pacific Ocean

• Aleutian Current
• Humboldt Current (or Peru Current)
• Kuroshio Current (or Japan Current)
• North Equatorial Current
• South Equatorial Current
• Cromwell current

Indian Ocean

Southern Ocean

• Antarctic Circumpolar Current

References

• Adapted from the Wikipedia article, "Ocean_current" http://en.wikipedia.org/wiki/Ocean_current, used under the GNU Free Documentation License