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Mediterranean seas

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(Redirected fromDilution basin)
Mostly enclosed sea with limited exchange with outer oceans
This article is about the term. For the namesake sea, seeMediterranean Sea.
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Inoceanography, amediterranean sea (/ˌmɛdɪtəˈrniən/MED-ih-tə-RAY-nee-ən) is a mostly enclosedsea that has limited exchange of water with outeroceans and whose water circulation is dominated bysalinity and temperature differences rather than by winds or tides.[1][2] The eponymousMediterranean Sea, for example, is almost completely enclosed byAfrica,Asia, andEurope.

List of mediterranean seas by ocean

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Atlantic Ocean

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Indian Ocean

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Pacific Ocean

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List of mediterranean seas by type

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There are two types of mediterranean sea.

Concentration basin

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Aconcentration basin has a higher salinity than the outer ocean due to evaporation, and its water exchange consists of inflow of the fresher oceanic water in the upper layer and outflow of the saltier mediterranean water in the lower layer of the connectingchannel.

Dilution basin

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Adilution 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 supplyoxygen to the bottom.

Exceptions

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  • Hudson Bay is so shallow it functions like a hugeestuary.[7]
  • Having shallow channels and deep basins, theSea of Japan could form a mediterranean sea, but the strong currents from the Pacific prevent it from having an independent water circulation.

See also

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References

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  1. ^abcKämpf, Jochen (2010)."5.5.2: Mediterranean Seas".Advanced Ocean Modelling: Using Open-Source Software.Heidelberg:Springer Science & Business Media. p. 138.ISBN 9783642106101. Retrieved2017-09-05.Mediterranean seas of the Indian Ocean are the Persian Gulf and the Red Sea, and the Australasian Mediterranean Sea, including the Banda, Java, Sulawesi, and Sulu seas, being connected with the Pacific Ocean.
  2. ^Tomczak, M.; Godfrey, J. Stuart (2003)."Chapter 7: Arctic oceanography; the path of North Atlantic Deep Water"(PDF).Regional oceanography: an introduction (2nd ed.).Delhi: Daya.ISBN 8170353068.OCLC 52613155. Retrieved23 May 2019.
  3. ^General oceanography : an introduction (2nd ed.). New York: Wiley. 1980. p. 501.ISBN 0471021024.OCLC 6200221.
  4. ^The Oceans Their Physics, Chemistry, and General Biology. pp. 15, 35 and 637–643.
  5. ^Tang, Charles C. L; Ross, Charles K.; Yao, Tom; Petrie, Brian; DeTracey, Brendan M.; Dunlap, Ewa (2004-12-01). "The circulation, water masses and sea-ice of Baffin Bay".Progress in Oceanography.63 (4):183–228.Bibcode:2004PrOce..63..183T.doi:10.1016/j.pocean.2004.09.005.ISSN 0079-6611. "Baffin Bay is a mediterranean sea connected through restrictive straits to the Arctic Ocean and the Labrador Sea/Atlantic Ocean"
  6. ^Sofianos, Sarantis S.; Johns, William E. (2007)."Observations of the summer Red Sea circulation".Journal of Geophysical Research: Oceans.112 (C6).Bibcode:2007JGRC..112.6025S.doi:10.1029/2006jc003886.ISSN 0148-0227.
  7. ^"Hudson Bay Estuaries".pew.org. Retrieved2019-05-23.

Further reading

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Antarctic/Southern Ocean
Arctic Ocean
Atlantic Ocean
Indian Ocean
Pacific Ocean
Endorheic basins
Others
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