Article
Article
- Earth Science
- Oceanography
- Ocean
Ocean
Article By:
Gille, Sarah T. Scripps Institution of Oceanography, University of California San Diego, La Jolla, California.
Last reviewed:November 2019
DOI:https://doi.org/10.1036/1097-8542.757648
Show previous versions
- Ocean, published May 2018:Download PDF Get Adobe Acrobat Reader
- Ocean, published June 2014:Download PDF Get Adobe Acrobat Reader
- Temperature, salinity, and density
- Ocean circulation
- Related Primary Literature
- Additional Reading
One of the major subdivisions of the interconnected body of salt water that occupies almost three-quarters of the Earth’s surface. Earth is the only planet in the solar system whose surface is covered with significant quantities of water (Fig. 1). Of the nearly 1.4 billion km3 of water found either on the surface or in relatively accessible underground supplies, about 96% is in the oceans; most of the rest is in glacier-covered Greenland and Antarctica. During much of Earth’s history, the oceans have been a difficult, if not quite impassable, barrier for the movement of land-based plants and animals from one continent or island to another. This article describes and compares some of the major oceans and their features. See also: Glaciology; Greenland; Indian Ocean; Oceanography
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