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Inoceanography, amediterranean sea (/ˌmɛdɪtəˈreɪniən/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.
There are two types of mediterranean sea.
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.
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.
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.
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