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Tests of a New Hypothesis for Non-Bathymetrically Driven Rip Currents
Rip currents-strong, isolated, offshore-directed flows-can occur in the absence of bathymetric features such as rip channels. No consensus exists regarding the cause of these impressive but life-threatening features, sometimes called "flash" rip currents. In a new model, flash rip currents...
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Published in: | Journal of coastal research 2003-03, Vol.19 (2), p.269-277 |
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container_title | Journal of coastal research |
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creator | MURRAYT, A. Brad LEBARS, Michael GUILLONT, Cyril |
description | Rip currents-strong, isolated, offshore-directed flows-can occur in the absence of bathymetric features such as rip channels. No consensus exists regarding the cause of these impressive but life-threatening features, sometimes called "flash" rip currents. In a new model, flash rip currents self-organize because of feedbacks resulting from a newly hypothesized interaction between waves and currents. Robust predictions arise from this numerical model: Flash rip currents become less prevalent with increasing beach slope and increasing variations in incident-wave heights. The results of field tests of these predictions support this model, but are not consistent with some other models, as applied to the flash rip currents on beaches such as those in Southern California. |
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Brad ; LEBARS, Michael ; GUILLONT, Cyril</creator><creatorcontrib>MURRAYT, A. Brad ; LEBARS, Michael ; GUILLONT, Cyril</creatorcontrib><description>Rip currents-strong, isolated, offshore-directed flows-can occur in the absence of bathymetric features such as rip channels. No consensus exists regarding the cause of these impressive but life-threatening features, sometimes called "flash" rip currents. In a new model, flash rip currents self-organize because of feedbacks resulting from a newly hypothesized interaction between waves and currents. Robust predictions arise from this numerical model: Flash rip currents become less prevalent with increasing beach slope and increasing variations in incident-wave heights. The results of field tests of these predictions support this model, but are not consistent with some other models, as applied to the flash rip currents on beaches such as those in Southern California.</description><identifier>ISSN: 0749-0208</identifier><identifier>EISSN: 1551-5036</identifier><identifier>CODEN: JCRSEK</identifier><language>eng</language><publisher>Lawrence, KS: Coastal Education and Research Foundation (CERF)</publisher><subject>Bathymetry ; Beaches ; Dynamics of the ocean (upper and deep oceans) ; Earth, ocean, space ; Engineering Sciences ; Exact sciences and technology ; External geophysics ; Fluid mechanics ; Fluids mechanics ; Image rectification ; Mechanics ; Modeling ; Observational research ; Ocean currents ; Ocean, Atmosphere ; Parametric models ; Physics ; Physics of the oceans ; Sciences of the Universe ; Simulations ; Standard deviation ; Waves</subject><ispartof>Journal of coastal research, 2003-03, Vol.19 (2), p.269-277</ispartof><rights>Copyright 2003 Coastal Education & Research Foundation [CERF]</rights><rights>2003 INIST-CNRS</rights><rights>Distributed under a Creative Commons Attribution 4.0 International License</rights><lds50>peer_reviewed</lds50><woscitedreferencessubscribed>false</woscitedreferencessubscribed><orcidid>0000-0002-4884-6190</orcidid></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><linktopdf>$$Uhttps://www.jstor.org/stable/pdf/4299168$$EPDF$$P50$$Gjstor$$H</linktopdf><linktohtml>$$Uhttps://www.jstor.org/stable/4299168$$EHTML$$P50$$Gjstor$$H</linktohtml><link.rule.ids>230,314,776,780,881,58213,58446</link.rule.ids><backlink>$$Uhttp://pascal-francis.inist.fr/vibad/index.php?action=getRecordDetail&idt=14768645$$DView record in Pascal Francis$$Hfree_for_read</backlink><backlink>$$Uhttps://hal.science/hal-00084098$$DView record in HAL$$Hfree_for_read</backlink></links><search><creatorcontrib>MURRAYT, A. Brad</creatorcontrib><creatorcontrib>LEBARS, Michael</creatorcontrib><creatorcontrib>GUILLONT, Cyril</creatorcontrib><title>Tests of a New Hypothesis for Non-Bathymetrically Driven Rip Currents</title><title>Journal of coastal research</title><description>Rip currents-strong, isolated, offshore-directed flows-can occur in the absence of bathymetric features such as rip channels. No consensus exists regarding the cause of these impressive but life-threatening features, sometimes called "flash" rip currents. In a new model, flash rip currents self-organize because of feedbacks resulting from a newly hypothesized interaction between waves and currents. Robust predictions arise from this numerical model: Flash rip currents become less prevalent with increasing beach slope and increasing variations in incident-wave heights. The results of field tests of these predictions support this model, but are not consistent with some other models, as applied to the flash rip currents on beaches such as those in Southern California.</description><subject>Bathymetry</subject><subject>Beaches</subject><subject>Dynamics of the ocean (upper and deep oceans)</subject><subject>Earth, ocean, space</subject><subject>Engineering Sciences</subject><subject>Exact sciences and technology</subject><subject>External geophysics</subject><subject>Fluid mechanics</subject><subject>Fluids mechanics</subject><subject>Image rectification</subject><subject>Mechanics</subject><subject>Modeling</subject><subject>Observational research</subject><subject>Ocean currents</subject><subject>Ocean, Atmosphere</subject><subject>Parametric models</subject><subject>Physics</subject><subject>Physics of the oceans</subject><subject>Sciences of the Universe</subject><subject>Simulations</subject><subject>Standard deviation</subject><subject>Waves</subject><issn>0749-0208</issn><issn>1551-5036</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2003</creationdate><recordtype>article</recordtype><recordid>eNo9kNFKwzAUhoMoOKdv4EVuFLwoJGnSJpdzTiuMCTKvS5YmNKNrapJN-vZmbOzqHM7_8cF_rsAEM4YzhvLiGkxQSUWGCOK34C6ELUK44LScgMVahxigM1DClf6D1Ti42OpgAzTOw5Xrs1cZ23Gno7dKdt0I37w96B5-2wHO997rPoZ7cGNkF_TDeU7Bz_tiPa-y5dfH53y2zFpSiJjlUknZlJxsqDFMNERjZni5wZghRRVisjGcEKGYMpirtGJCBWmIUaUgOc2n4OXkbWVXD97upB9rJ21dzZb18YYQ4hQJfsCJfT6xg3e_-9Sy3tmgdNfJXrt9qDEXyc5ZAp_OoAypofGyVzZc9JiWBS_okXs8cdsQnb_klAiRnpn_AxvAbPw</recordid><startdate>20030301</startdate><enddate>20030301</enddate><creator>MURRAYT, A. Brad</creator><creator>LEBARS, Michael</creator><creator>GUILLONT, Cyril</creator><general>Coastal Education and Research Foundation (CERF)</general><general>Coastal Education and Research Foundation</general><scope>IQODW</scope><scope>7TG</scope><scope>7TN</scope><scope>F1W</scope><scope>H96</scope><scope>KL.</scope><scope>L.G</scope><scope>1XC</scope><orcidid>https://orcid.org/0000-0002-4884-6190</orcidid></search><sort><creationdate>20030301</creationdate><title>Tests of a New Hypothesis for Non-Bathymetrically Driven Rip Currents</title><author>MURRAYT, A. Brad ; LEBARS, Michael ; GUILLONT, Cyril</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-h269t-3acaad782b4ff59d2e15f87b1150c4c05adf8229c5cf18c82212492d2fc792343</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>2003</creationdate><topic>Bathymetry</topic><topic>Beaches</topic><topic>Dynamics of the ocean (upper and deep oceans)</topic><topic>Earth, ocean, space</topic><topic>Engineering Sciences</topic><topic>Exact sciences and technology</topic><topic>External geophysics</topic><topic>Fluid mechanics</topic><topic>Fluids mechanics</topic><topic>Image rectification</topic><topic>Mechanics</topic><topic>Modeling</topic><topic>Observational research</topic><topic>Ocean currents</topic><topic>Ocean, Atmosphere</topic><topic>Parametric models</topic><topic>Physics</topic><topic>Physics of the oceans</topic><topic>Sciences of the Universe</topic><topic>Simulations</topic><topic>Standard deviation</topic><topic>Waves</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>MURRAYT, A. Brad</creatorcontrib><creatorcontrib>LEBARS, Michael</creatorcontrib><creatorcontrib>GUILLONT, Cyril</creatorcontrib><collection>Pascal-Francis</collection><collection>Meteorological & Geoastrophysical Abstracts</collection><collection>Oceanic Abstracts</collection><collection>ASFA: Aquatic Sciences and Fisheries Abstracts</collection><collection>Aquatic Science & Fisheries Abstracts (ASFA) 2: Ocean Technology, Policy & Non-Living Resources</collection><collection>Meteorological & Geoastrophysical Abstracts - Academic</collection><collection>Aquatic Science & Fisheries Abstracts (ASFA) Professional</collection><collection>Hyper Article en Ligne (HAL)</collection><jtitle>Journal of coastal research</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>MURRAYT, A. Brad</au><au>LEBARS, Michael</au><au>GUILLONT, Cyril</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Tests of a New Hypothesis for Non-Bathymetrically Driven Rip Currents</atitle><jtitle>Journal of coastal research</jtitle><date>2003-03-01</date><risdate>2003</risdate><volume>19</volume><issue>2</issue><spage>269</spage><epage>277</epage><pages>269-277</pages><issn>0749-0208</issn><eissn>1551-5036</eissn><coden>JCRSEK</coden><abstract>Rip currents-strong, isolated, offshore-directed flows-can occur in the absence of bathymetric features such as rip channels. No consensus exists regarding the cause of these impressive but life-threatening features, sometimes called "flash" rip currents. In a new model, flash rip currents self-organize because of feedbacks resulting from a newly hypothesized interaction between waves and currents. Robust predictions arise from this numerical model: Flash rip currents become less prevalent with increasing beach slope and increasing variations in incident-wave heights. The results of field tests of these predictions support this model, but are not consistent with some other models, as applied to the flash rip currents on beaches such as those in Southern California.</abstract><cop>Lawrence, KS</cop><pub>Coastal Education and Research Foundation (CERF)</pub><tpages>9</tpages><orcidid>https://orcid.org/0000-0002-4884-6190</orcidid></addata></record> |
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source | JSTOR Archival Journals and Primary Sources Collection; Allen Press Journals |
subjects | Bathymetry Beaches Dynamics of the ocean (upper and deep oceans) Earth, ocean, space Engineering Sciences Exact sciences and technology External geophysics Fluid mechanics Fluids mechanics Image rectification Mechanics Modeling Observational research Ocean currents Ocean, Atmosphere Parametric models Physics Physics of the oceans Sciences of the Universe Simulations Standard deviation Waves |
title | Tests of a New Hypothesis for Non-Bathymetrically Driven Rip Currents |
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