Ocean Currents
An ocean current is continuous, directed movement of ocean water. Ocean currents are rivers of hot or cold water within the ocean. The currents are generated from the forces acting upon the water like the planet rotation, the wind, the temperature, salinity (hence isopycnal) differences and the gravitation of the moon. The depth contours, the shoreline and other currents influence the current's direction and strength. The meshing of all of these characteristics is what creates the great flow of the global conveyor belt which plays a dominant part in the climate of many of the Earth’s regions.
An ocean current is continuous, directed movement of ocean water. Ocean currents are rivers of hot or cold water within the ocean. The currents are generated from the forces acting upon the water like the planet rotation, the wind, the temperature, salinity (hence isopycnal) differences and the gravitation of the moon. The depth contours, the shoreline and other currents influence the current's direction and strength. The meshing of all of these characteristics is what creates the great flow of the global conveyor belt which plays a dominant part in the climate of many of the Earth’s regions.

Arctic Ocean
East Greenland Current
Norwegian Current
Beaufort Gyre (water or ice flow)
Transpolar Drift (water or ice flow)
East Greenland Current
Norwegian Current
Beaufort Gyre (water or ice flow)
Transpolar Drift (water or ice flow)
Atlantic Ocean
Angola Current
Antilles Current
Baffin Island Current
Benguela current
Brazil Current
Canary Current
Cape Horn Current
Caribbean Current
East Greenland Current
Falkland Current
Gulf Stream
Guinea Current
Labrador Current
Lomonosov current (a deep current)
North Atlantic Current
North Brazil Current
Norwegian Current
Portugal Current
South Atlantic Current
Spitsbergen Current
West Greenland Current
West Wind Drift
Angola Current
Antilles Current
Baffin Island Current
Benguela current
Brazil Current
Canary Current
Cape Horn Current
Caribbean Current
East Greenland Current
Falkland Current
Gulf Stream
Guinea Current
Labrador Current
Lomonosov current (a deep current)
North Atlantic Current
North Brazil Current
Norwegian Current
Portugal Current
South Atlantic Current
Spitsbergen Current
West Greenland Current
West Wind Drift
Pacific Ocean
Alaska Current
Aleutian Current
California Current
Cromwell current (a deep current)
East Australian Current
Equatorial Counter Current
Humboldt Current (or Peru Current)
Kamchatka Current
Kuroshio Current (or Japan Current, Kuro Siwo)
Mindanao Current
North Equatorial Current
North Pacific Current (or North Pacific Drift)
Oyashio Current (or Oya Siwo)
South Equatorial Current
West Wind Drift
Alaska Current
Aleutian Current
California Current
Cromwell current (a deep current)
East Australian Current
Equatorial Counter Current
Humboldt Current (or Peru Current)
Kamchatka Current
Kuroshio Current (or Japan Current, Kuro Siwo)
Mindanao Current
North Equatorial Current
North Pacific Current (or North Pacific Drift)
Oyashio Current (or Oya Siwo)
South Equatorial Current
West Wind Drift
Indian Ocean
Agulhas Current
East Madagascar Current
Equatorial Counter Current
Indonesian Through-flow
Leeuwin Current
Madagascar Current
Mozambique Current
Somali Current
South Australian Counter Current
South Equatorial Current
Southwest and Northeast Monsoon Drift (or Indian Monsoon Current)
West Australian Current
West Wind Drift
Southern Ocean
Antarctic Circumpolar Current
Weddell Gyre
Tasman Outflow
Agulhas Current
East Madagascar Current
Equatorial Counter Current
Indonesian Through-flow
Leeuwin Current
Madagascar Current
Mozambique Current
Somali Current
South Australian Counter Current
South Equatorial Current
Southwest and Northeast Monsoon Drift (or Indian Monsoon Current)
West Australian Current
West Wind Drift
Southern Ocean
Antarctic Circumpolar Current
Weddell Gyre
Tasman Outflow

No comments:
Post a Comment