Mediterranean seas

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Dilution basin
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A mediterranean sea (/ˌmɛdɪtəˈrniən/ MED-i-tə-RAY-nee-ən) is, in oceanography, a mostly enclosed sea that has limited exchange of water with outer oceans and whose water circulation is dominated by salinity and temperature differences rather than by winds or tides.[1][2] The eponymous Mediterranean Sea, for example, is almost completely enclosed by Asia, Europe, and Africa.

List of mediterranean seas

The mediterranean seas of the Atlantic Ocean

The mediterranean seas of the Indian Ocean

The mediterranean seas of the Pacific Ocean

Types of mediterranean seas

There are two types of mediterranean sea.

Concentration basin

Dilution basin

  • A dilution basin has a lower salinity due to freshwater gains such as rainfall and rivers, and its water exchange consists of outflow of the fresher mediterranean water in the upper layer and inflow of the saltier oceanic water in the lower layer of the channel. Renewal of deep water may not be sufficient to supply oxygen to the bottom.

Exceptions

See also

  • Inland sea (geology)
  • Marginal sea

References

  1. ^ a b c Kämpf, Jochen (2010). "5.5.2 : Mediterranean Seas". Advanced Ocean Modelling: Using Open-Source Software. Heidelberg: Springer Science & Business Media. p. 138. . Retrieved 2017-09-05. Mediterranean seas of the Indian Ocean are the Persian Gulf and the Red Sea, and the Australasian Mediterranean Sea, including the Banda, Sulu, Sulawesi and Java Seas, being connected with the Pacific Ocean.
  2. . Retrieved 23 May 2019.
  3. .
  4. ^ The Oceans Their Physics, Chemistry, and General Biology. pp. 15, 35 and 637–643.
  5. ISSN 0079-6611
    .
  6. ^ "Hudson Bay Estuaries". pew.org. Retrieved 2019-05-23.