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thermohaline convection |
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thermohaline convection [¦thər·mō′hā‚līn kən′vek·shən] (oceanography) Vertical water movement observed when sea water, due to conditions of decreasing temperature or increasing salinity, becomes heavier than the water beneath it. 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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