Encyclopædia Britannica, Inc.
Just How Many Oceans Are There?
Notwithstanding Europa andِ Enceladus (both moons areِ covered inِ ice), Earth isِ the true water world ofِ the solar system.
Some 71 percent ofِ Earth’s surface isِ covered byِ saltwater oceans, andِ the continents themselvesِ possess lakes, rivers, and, inِ some cases, seas.
The largest bodies ofِ water areِ the oceans, butِ there isِ some debate overِ the actual number ofِ distinct oceans thereِ are.
Just howِ many oceans doesِ our planet have?
As anyِ grade-schooler mightِ tell you, Earth hasِ fourِ oceans: theِ Pacific, theِ Atlantic, theِ Indian, andِ the Arctic.
Historically speaking, mostِ countries recognize thisِ four-ocean model, whichِ tendsِ to focus onِ the Pacific, theِ Atlantic, andِ the Indian oceans asِ the major ones.
The Arctic Ocean, whichِ isِ farِ smaller thanِ the others, isِ less prominent inِ people’s minds, perhapsِ becauseِ it occurs onِ the fringes ofِ the map andِ tends toِ beِ covered (well, mostly) byِ ice.
In reality, however, Earth’s ocean count depends uponِ one’s perspective.
A collection ofِ scientific organizations, including theِ International Hydrographic Organization, hasِ considered theِ existence ofِ the Southern Ocean (also called theِ Antarctic Ocean) inِ the waters surrounding Antarctica belowِ 60° S latitude.
The separation ofِ the Southern Ocean fromِ the Atlantic, Pacific, andِ Indian oceans isِ reasonable whenِ you considerِ that theِ Antarctic Circumpolar Current andِ the winds thatِ circle theِ outer approaches ofِ the continent create a kind ofِ natural separation, orِ Antarctic Convergence (in terms ofِ oceanography andِ meteorology), betweenِ Antarctica andِ the rest ofِ the world.
Functionally speaking, however, thereِ isِ only oneِ ocean, sinceِ everyِ ocean isِ connected toِ atِ least twoِ others.
The reality ofِ a single ocean isِ alsoِ evidenced byِ the thermohaline circulation (called theِ Global Ocean Conveyor orِ the Great Ocean Conveyor Belt) thatِ passes throughِ allِ of them.
The thermohaline circulation continually replaces seawater atِ depth withِ water fromِ the surface andِ slowly replaces surface water elsewhereِ with water rising fromِ deeper depths.