The World Ocean, world ocean, or global ocean is a term used to define all the world's oceans as one large interconnected ocean.
The 'World Ocean' is centered on the southern oceans. The Atlantic, Indian, and Pacific Oceans can be seen as bays or lobes going northward from the Southern Ocean. Farther north, the Atlantic opens into the Arctic Ocean, which is connected to the Pacific by the Bering Strait:
- The Southern Ocean would be the ocean surrounding Antarctica, generally the ocean south of sixty degrees south latitude. Parts of the Southern Ocean are covered in sea ice, the extent of which varies according to the season. The Southern Ocean is the second smallest of the five named oceans.
- The Atlantic Ocean, the second biggest, extends from the Southern Ocean between South America, Africa, North America and Europe, to the Arctic Ocean. The Atlantic meets the Indian Ocean south of Africa at Cape Agulhas.
- The Indian Ocean extends northward from the Southern Ocean to India, between Africa and Australia. The Indian Ocean joins the Pacific Ocean to the west, near Australia.
- The Pacific Ocean, the biggest of all, also reaches northward from the Southern Ocean to the Arctic Ocean. It is in the gap between Australia, Asia, North America and Oceania. The Pacific Ocean meets the Atlantic south of South America at Cape Horn.
- The Arctic Ocean is the smallest of the five. It joins the Atlantic near Greenland and Iceland, and joins the Pacific at the Bering Strait. It is on the North Pole, touching North America in the Western hemisphere and Scandinavia and Asia in the Eastern hemisphere. Parts of the Arctic Ocean are covered in sea ice, the extent of which varies according to the season. Some people do not consider the Arctic Ocean an actual ocean, because it is mostly surrounded by land with only a bit of exchange of water with the other oceans. Consequently, it is considered by some to be a sea of the Atlantic, referred to as the Arctic Mediterranean Sea or Arctic Sea.
The approximate shape of the 'World Ocean' can for most purposes be treated as constant, although in detail it is not. Climate change continually changes its structure, and continental drift does so over a much longer timescale.