Gyres: Difference between revisions
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<div class="definition"><div class="short_definition">Oceanic current systems of planetary scale driven by the global [[wind]] system.</div><br/> <div class="paragraph">The subtropical gyres are driven by the [[trade winds]] and by the [[westerlies]] of the temperate regions, the subpolar gyres by the westerlies and the [[polar easterlies]]. Gyres consist of a narrow, swift-flowing western [[boundary current]], an eastward-flowing [[zonal]] current, a broad and slow-moving eastern boundary current, and a westward flowing zonal current. Eight gyres are distinguished in the World Ocean: In the Atlantic, the [[Brazil]], [[South Atlantic]], [[Benguela]], and [[South Equatorial Currents]] form the subtropical gyre of the Southern Hemisphere; the [[Gulf Stream]], [[Azores]], [[Canary]], and [[North Equatorial Currents]] form the subtropical gyre in the Northern Hemisphere; the [[Labrador]], [[North Atlantic]], [[Irminger]], and [[East Greenland Currents]] form the subpolar gyre. In the Pacific, the [[East Australian]], [[South Pacific]], [[Peru/Chile]], and South Equatorial Currents form the subtropical gyre of the Southern Hemisphere; the [[Kuroshio]], [[North Pacific]], [[California]], and North Equatorial Currents form the subtropical gyre of the Northern Hemisphere; the [[Oyashio]], [[Aleutian]], California, and [[Alaskan Currents]] and the [[Alaskan Stream]] form the subpolar gyre; a second subpolar gyre exists in the Bering Sea. In the Indian Ocean, the [[Agulhas]], [[South Indian]], [[West Australian]], and South Equatorial Currents form the only subtropical gyre.</div><br/> </div> | <div class="definition"><div class="short_definition">Oceanic current systems of planetary scale driven by the global [[wind]] system.</div><br/> <div class="paragraph">The subtropical gyres are driven by the [[trade winds]] and by the [[westerlies]] of the temperate regions, the subpolar gyres by the westerlies and the [[polar easterlies]]. Gyres consist of a narrow, swift-flowing western [[boundary currents|boundary current]], an eastward-flowing [[zonal]] current, a broad and slow-moving eastern boundary current, and a westward flowing zonal current. Eight gyres are distinguished in the World Ocean: In the Atlantic, the [[Brazil Current|Brazil]], [[South Atlantic Current|South Atlantic]], [[Benguela Current|Benguela]], and [[South Equatorial Currents]] form the subtropical gyre of the Southern Hemisphere; the [[Gulf Stream]], [[Azores Current|Azores]], [[Canary Current|Canary]], and [[North Equatorial Currents]] form the subtropical gyre in the Northern Hemisphere; the [[Labrador Current|Labrador]], [[North Atlantic Current|North Atlantic]], [[Irminger Current|Irminger]], and [[East Greenland Currents]] form the subpolar gyre. In the Pacific, the [[East Australian Current|East Australian]], [[South Pacific Current|South Pacific]], [[Peru/Chile Current|Peru/Chile]], and South Equatorial Currents form the subtropical gyre of the Southern Hemisphere; the [[Kuroshio]], [[North Pacific Current|North Pacific]], [[California Current|California]], and North Equatorial Currents form the subtropical gyre of the Northern Hemisphere; the [[Oyashio]], [[Aleutian Current|Aleutian]], California, and [[Alaska Current|Alaskan Currents]] and the [[Alaskan Stream]] form the subpolar gyre; a second subpolar gyre exists in the Bering Sea. In the Indian Ocean, the [[Agulhas Current|Agulhas]], [[South Indian Ocean Current|South Indian]], [[West Australian Current|West Australian]], and South Equatorial Currents form the only subtropical gyre.</div><br/> </div> | ||
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Latest revision as of 16:06, 25 April 2012
gyres
Oceanic current systems of planetary scale driven by the global wind system.
The subtropical gyres are driven by the trade winds and by the westerlies of the temperate regions, the subpolar gyres by the westerlies and the polar easterlies. Gyres consist of a narrow, swift-flowing western boundary current, an eastward-flowing zonal current, a broad and slow-moving eastern boundary current, and a westward flowing zonal current. Eight gyres are distinguished in the World Ocean: In the Atlantic, the Brazil, South Atlantic, Benguela, and South Equatorial Currents form the subtropical gyre of the Southern Hemisphere; the Gulf Stream, Azores, Canary, and North Equatorial Currents form the subtropical gyre in the Northern Hemisphere; the Labrador, North Atlantic, Irminger, and East Greenland Currents form the subpolar gyre. In the Pacific, the East Australian, South Pacific, Peru/Chile, and South Equatorial Currents form the subtropical gyre of the Southern Hemisphere; the Kuroshio, North Pacific, California, and North Equatorial Currents form the subtropical gyre of the Northern Hemisphere; the Oyashio, Aleutian, California, and Alaskan Currents and the Alaskan Stream form the subpolar gyre; a second subpolar gyre exists in the Bering Sea. In the Indian Ocean, the Agulhas, South Indian, West Australian, and South Equatorial Currents form the only subtropical gyre.