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 stabilized by jetties.[1]

During these falling and ebbing tides, a riptide can carry a person far offshore. For example, the ebbing tide at Shinnecock Inlet in Southampton, New York, extends more than 300 metres (980 ft) offshore.[2] Because of this, riptides are typically more powerful than rip currents.


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The Riptide project was conceived and executed at the Shorenstein Center on the Press, Politics and Public Policy by three Shorenstein Center Fellows during the Spring 2013 semester: John Huey, Martin Nisenholtz and Paul Sagan. The Riptide website was designed by Joshua Benton and is hosted by the Nieman Foundation. To learn more about Riptide, visit digitalriptide.org for videos, interviews and full text of the project.

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