Ross Gyre

The Ross Gyre is one of the two gyres that exist within the Southern Ocean. The gyre is located in the Ross Sea, and rotates clockwise. The gyre is formed by interactions between the Antarctic Circumpolar Current and the Antarctic Continental Shelf. Sea ice has been noted to persist in the central area of the gyre.^[1]

There is some evidence that global warming has resulted in some decrease of the salinity of the waters of the Ross Gyre since the 1950s.^[2]

References

Arctic Ocean	East Greenland Norwegian Transpolar Drift Stream

Atlantic Ocean	Agulhas Angola Antilles Azores Baffin Island Benguela Brazil Canary Cape Horn Caribbean East Greenland East Iceland Falkland Florida Guinea Gulf Stream Irminger Labrador Lomonosov Loop North Atlantic North Brazil North Equatorial Norwegian Portugal Slope Jet South Atlantic South Equatorial Spitsbergen West Greenland

Indian Ocean	Agulhas East Madagascar Equatorial Counter Current Indian Monsoon Current Indonesian Throughflow Leeuwin Madagascar Mozambique Somali South Australian South Equatorial West Australian

Pacific Ocean	Alaska Aleutian California Cromwell East Australia Equatorial Counter Current Humboldt Indonesian Throughflow Kamchatka Kuroshio Mindanao North Equatorial North Pacific Oyashio South Equatorial

Southern Ocean	Antarctic Circumpolar Current

Major gyres	Indian Ocean Gyre North Atlantic Gyre South Atlantic Gyre North Pacific Gyre South Pacific Gyre

Other gyres	Beaufort Gyre Ross Gyre Weddell Gyre