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Rip tide
Current caused by the tide pulling water through an inlet / From Wikipedia, the free encyclopedia
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This article is about currents caused by the tide pulling water through an inlet. For currents appearing near beaches, see Rip current. For other uses, see Riptide (disambiguation).
A rip tide, or riptide, is a strong offshore current that is caused by the tide pulling water through an inlet along a barrier beach, at a lagoon or inland marina where tide water flows steadily out to sea during ebb tide. It is a strong tidal flow of water within estuaries and other enclosed tidal areas. The riptides become the strongest where the flow is constricted. When there is a falling or ebbing tide, the outflow water is strongly flowing through an inlet toward the sea, especially once stabilised by jetties.[1]
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