Ocean gyresThe Earth's oceans have the following major gyres:2
Tropical circulations are less unified and tend to be mostly east-west with minor north-south extent.
Subtropical gyresThe center of a subtropical gyre is a high pressure zone. Circulation around the high pressure is clockwise in the northern hemisphere and counterclockwise in the southern hemisphere, due to the Coriolis force. The high pressure in the center is due to the westerly winds on the northern side of the gyre and easterly trade winds on the southern side of the gyre. These cause frictional surface currents towards the latitude at the center of the gyre. The buildup of water in the center of the gyre creates equatorward flow in the upper 1000 to 2000 meters of the ocean, through rather complex dynamics. This equatorward flow is returned poleward in an intensified western boundary current (Western intensification). The intensified western boundary current of the North Atlantic's subtropical gyre is the Gulf Stream; in the North Pacific it is the Kuroshio; in the South Atlantic, it is the Brazil Current; in the South Pacific, it is the East Australia Current; in the Indian Ocean, it is the Agulhas Current. Subpolar gyresSubpolar gyres form at high latitudes (around 60 degrees). Circulation of surface wind and ocean water is counterclockwise in the Northern Hemisphere, around a low pressure system (such as the persistent Aleution Low and the Icelandic Low). Surface currents generally move outward from the center of the system. This drives Ekman transport which creates an upwelling of nutrient-rich water from the lower depths.5 Subpolar circulation in the southern hemisphere is dominated by the Antarctic Circumpolar Current due to the lack of large landmasses breaking up the Southern Ocean. There are minor gyres in the Wendall and Ross Seas, which circulate in a clockwise direction.2 References
See also
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