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topographic curl effect |
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topographic curl effect [¦täp·ə¦graf·ik ′kərl i‚fəkt] (oceanography) A term in Ekman's differential equation for the effects of variable wind stress, variable depth, variable friction, and variable latitude on the deep current; tends to make the curlG(velocity of deep current) positive when the current flows over increasing depth and negative when the depth decreases in the direction of the current. 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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