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The Southern Ocean, also known as the Great Southern Ocean, the Antarctic Ocean and the South Polar Ocean, comprises the southernmost waters of the World Ocean south of 60° S latitude. The International Hydrographic Organization has designated the Southern Ocean as an oceanic division encircling Antarcticamarker. Geographers disagree on the Southern Ocean's northern boundary or even its existence (see below), sometimes considering the waters part of the South Pacificmarker, South Atlanticmarker, and Indian Oceansmarker instead.

Some scientists consider the Antarctic Convergence, an ocean zone which fluctuates seasonally, as separating the Southern Ocean from other oceans, rather than 60° S.This ocean zone is where cold, northward flowing waters from the Antarctic mix with warmer sub-Antarctic waters.

The International Hydrographic Organization (IHO) regards the Southern Ocean as the fourth-largest of the five principal oceanic divisions and the latest-defined one. The IHO promulgated the decision on its existence in 2000, though many mariners have long regarded the term as traditional. The Southern Ocean appeared in the IHO's Limits of Oceans and Seas second edition (1937), disappeared from the third edition (1957), and resurfaced in the fourth edition (not formally adopted due to a number of unresolved disputes, including the lodgement of a reservation by Australia). This change reflects the importance placed by oceanographers on ocean currents.

The Southern Ocean


The Southern Ocean includes the Antarctic Circumpolar Current (which circulates around Antarctica), the Amundsen Sea, Bellingshausen Seamarker, parts of the Drake Passagemarker, Ross Seamarker, Cooperation Sea, the Cosmonaut Sea, a small part of the Scotia Sea, and Weddell Seamarker. Its total area comprises 20,327,000 square kilometers (7,848,000 mi²).

The Southern Ocean differs from the other oceans in that its largest boundary, the northern boundary, does not abut a landmass, but merges into the Atlantic, Indian and Pacific Oceans. This calls into question why geographers should consider the Southern Ocean a separate ocean, as opposed to a southward extension of the other three oceans. One reason stems from the fact that much of the water of the Southern Ocean differs from the water in the other oceans. Because of the Antarctic Circumpolar Current, that water gets transported around the Southern Ocean fairly rapidly, so that the water in the Southern Ocean south of, for example, South America, resembles the water in the Southern Ocean south of New Zealand more closely than it resembles the water in the mid-Indian Ocean.

Several processes operate along the coast of Antarctica to produce, in the Southern Ocean, types of water masses not produced elsewhere in the oceans of the Southern Hemisphere. One of these is the Antarctic Bottom Water, a very cold, highly saline, dense water that forms under sea ice.

The Southern Ocean, geologically the youngest of the oceans, formed when Antarctica and South America moved apart, opening the Drake Passagemarker, roughly 30 million years ago. The separation of the continents allowed the formation of the Antarctic Circumpolar Current.

In many respects, the Southern Ocean forms the opposite of the Arctic Oceanmarker, located on the opposite end of the globe.

Arctic and Southern Oceans contrasted
Arctic Ocean Southern Ocean
Surrounded by Eurasia and North America Encircles the Antarctic continent
Warm ocean moderates frigid land Icy landmass feeds cold ocean
Freshwater from rivers feeds the Arctic Ocean The melting of glaciers feeds the Southern
Ice forms at very center of the Arctic Ice forms along the Antarctic coastline


The second edition (1937) of the IHO's Limits of Oceans and Seas included the Southern Ocean; however, it did not appear in the third edition (1953) because of the fluctuation of its northern hydrographic limits with the seasons and because scientists felt that an ocean should be defined as "water surrounded by land" not "water encircling land". Individual member states' hydrographic offices have defined their own boundaries; the United Kingdommarker used the 55°S parallel.

The IHO addressed the question again in a survey in 2000. Of the 68 member nations, 28 responded, and all responding members except Argentinamarker agreed to define a new ocean. The proposal for the name Southern Ocean won 18 votes, beating the alternative Antarctic Ocean. Half of the votes supported ending the ocean at the 60 degrees south line of latitude (with no land interruptions at this latitude), with the other 14 votes cast for other definitions, mostly 50 degrees south, but a few for as far north as 35 degrees south.

Other sources such as the National Geographic Societymarker continue to show the Atlanticmarker, Pacificmarker and Indianmarker Oceans as extending to Antarctica.

Many maps of Australia show the Southern Ocean lying immediately to the south of Australia.

In Australia, cartographical authorities defined the Southern Ocean as including the entire body of water between Antarctica and the south coasts of Australia and New Zealandmarker, although New Zealand authorities do not generally follow suit. Coastal maps of Tasmaniamarker and South Australiamarker label the sea areas as Southern Ocean, while Cape Leeuwinmarker in Western Australiamarker is described as the point where the Indian and Southern Oceans meet.


The Southern Ocean lies in the Southern Hemisphere. It has typical depths of between 4,000 and 5,000 meters (13,000 to 16,000 ft) over most of its extent with only limited areas of shallow water. The Antarctic continental shelf appears generally narrow and unusually deep, its edge lying at depths up to 800 meters (2,600 ft), compared to a global mean of 133 meters (436 ft).

Equinox to equinox in line with the sun's seasonal influence, the Antarctic ice pack fluctuates from an average minimum of 2.6 million square kilometers (1.0 million mi²) in March to about 18.8 million square kilometers (7.2 million mi²) in September, more than a sevenfold increase in area.

The Antarctic Circumpolar Current moves perpetually eastward — chasing and joining itself, and at 21,000 kilometers (13,000 mi) in length — it comprises the world's longest ocean current, transporting 130 million cubic meters (4.6 billion ft³) of water per second — 100 times the flow of all the world's rivers.

The Southern Ocean's greatest depth of 7,235 meters (23,737 ft) occurs at the southern end of the South Sandwich Trench, at 60°00'S, 024°W.


Sea-temperatures vary from about −2 to 10 °C (28 to 50 °F). Cyclonic storms travel eastward around the continent and frequently become intense because of the temperature-contrast between ice and open ocean. The ocean-area from about latitude 40 south to the Antarctic Circle has the strongest average winds found anywhere on Earth. In winter the ocean freezes outward to 65 degrees south latitude in the Pacific sector and 55 degrees south latitude in the Atlantic sector, lowering surface temperatures well below 0 degrees Celsius; at some coastal points intense persistent drainage winds from the interior keep the shoreline ice-free throughout the winter.

Natural resources

Natural hazards

Icebergs can occur at any time of year throughout the ocean. Some may have drafts up to several hundred meters; smaller icebergs, iceberg fragments and sea-ice (generally 0.5 to 1 meter thick) also pose problems for ships. The deep continental shelf has a floor of glacial deposits varying widely over short distances.

Sailors know latitudes from 40 to 70 degrees south as the "Roaring Forties", "Furious Fifties" and "Shrieking Sixties" due to high winds and large waves that form as winds blow around the entire globe unimpeded by any land-mass. Ship ice, especially in May to October, makes the area even more dangerous. The remoteness of the region makes sources of search and rescue scarce.


Current issues

Increased solar ultraviolet radiation resulting from the Antarctic ozone hole has reduced marine primary productivity (phytoplankton) by as much as 15% and has started damaging the DNA of some fish . Illegal, unreported, and unregulated fishing, especially the landing of an estimated five to six times more Patagonian toothfish than the regulated fishery, likely affects the sustainability of the stock. Long-line fishing for toothfish causes a high incidence of seabird mortality.

International agreements

All international agreements regarding the world's oceans apply to the Southern Ocean. In addition, it is subject to these agreements specific to the region:

Many nations prohibit the exploration for and the exploitation of mineral resources south of the fluctuating polar front , which lies in the middle of the Antarctic Circumpolar Current and serves as the dividing line between the very cold polar surface waters to the south and the warmer waters to the north. The Antarctic Treaty covers the portion of the globe south of sixty degrees south,it prohibits new claims to Antarctica and to all islands in the Southern Ocean.


Between 1 July 1998 and 30 June 1999 fisheries landed 119,898 tonnes, of which 85% consisted of krill and 14% of Patagonian toothfish. International agreements came into force in late 1999 to reduce illegal, unreported, and unregulated fishing, which in the 1998-99 season landed five to six times more Patagonian toothfish than the regulated fishery.

Ports and harbors

Major operational ports include: Rothera Stationmarker, Palmer Stationmarker, Villa Las Estrellasmarker, Esperanza Base, Mawson Stationmarker, McMurdo Stationmarker, and offshore anchorages in Antarctica.

Few ports or harbors exist on the southern (Antarctic) coast of the Southern Ocean, since ice conditions limit use of most shores to short periods in midsummer; even then some require icebreaker escort for access. Most Antarctic ports are operated by government research stations and, except in an emergency, remain closed to commercial or private vessels; vessels in any port south of 60 degrees south are subject to inspection by Antarctic Treaty observers.

The Southern Ocean's southernmost port operates at McMurdo Station at . Winter Quarters Baymarker forms a small harbor, on the southern tip of Ross Islandmarker where a floating Ice piermarker makes port operations possible in summer. Operation Deep Freeze personnel constructed the first ice pier at McMurdo in 1973.

See also



  1. Pyne, Stephen J.; The Ice: A Journey to Antarctica. University of Washington Press, 1986. NOTE: Despite the title, Pyne has not published a travel journal here: instead he presents a well-researched study of Antarctica's exploration, earth-sciences, icescape, esthetics, literature, and geopolitics.
  2. The Antarctic Treaty, article 6
  3. The Antarctic Treaty, article 4, clause 2
  4. "Unique ice pier provides harbor for ships," Antarctic Sun. January 8, 2006; McMurdo Station, Antarctica.

Further reading

  • Gille, Sarah T. 2002. "Warming of the Southern Ocean since the 1950s": abstract, article. Science: vol. 295 (no. 5558), pp. 1275–1277.
  • Descriptive Regional Oceanography, P. Tchernia, Pergamon Press, 1980.
  • Matthias Tomczak and J. Stuart Godfrey. 2003. Regional Oceanography: an Introduction. (see the site)

External links

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