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antiestuarine circulation |
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antiestuarine circulation [‚an·tē¦es·chə·wə‚rēn ‚ser·kyü′lā·shən] (oceanography) In an estuary, the inflow of low-salinity surface water over a deeper outflowing (seaward), dense, high-salinity water layer. How to thank TFD for its existence? Tell a friend about us, add a link to this page, add the site to iGoogle, or visit webmaster's page for free fun content. |
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