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dc.contributor.authorCastelle, Brunoen_US
dc.contributor.authorBourget, Julienen_US
dc.contributor.authorMolnar, Nathalieen_US
dc.contributor.authorStrauss, Darrellen_US
dc.contributor.authorDeschamps, Sophieen_US
dc.contributor.authorTomlinson, Rodgeren_US
dc.contributor.editorHans F. Burcharthen_US
dc.date.accessioned2017-05-03T12:10:45Z
dc.date.available2017-05-03T12:10:45Z
dc.date.issued2007en_US
dc.date.modified2009-09-15T07:38:16Z
dc.identifier.issn03783839en_US
dc.identifier.doi10.1016/j.coastaleng.2006.08.007en_AU
dc.identifier.urihttp://hdl.handle.net/10072/18959
dc.description.abstractCurrumbin Creek on the Australian Gold Coast is a wave-dominated tidal inlet which exhibits a particularly active morphology. The recent history of Currumbin Creek entrance has seen rapid growth of the entrance for access to the ocean by fishermen, as a world class surfing site, and as a recreational area. Before the construction of two groynes in the 70's, Currumbin Creek entrance was highly variable in terms of inlet location and sand bar characteristics due to a cyclical behaviour of spit migration. Nowadays, the entrance is stabilised. However, natural processes continue with the entrance infilling causing flood and navigation issues, resulting in a regular dredging program to maintain an open entrance and for regular beach nourishment plans. This paper investigates the behaviour of the entrance and adjacent beaches from aerial photographs and numerical modelling. Before groyne construction, sand by-passing was intense resulting in channel migration and sometimes the closure of the mouth. After training works, the longshore drift is diverted further north from the mouth leading to new circulation patterns behind the headland. During fair weather conditions, the sand transported by the longshore current is trapped by Currumbin rock groyne resulting in a negative sediment budget in Palm Beach. For high energy conditions, the diverted longshore current splits in the southern Palm Beach, resulting in a circulation cell. The sediment of the southern beaches is stirred up and transported both northward and toward the inlet.en_US
dc.description.peerreviewedYesen_US
dc.description.publicationstatusYesen_AU
dc.languageEnglishen_US
dc.language.isoen_AU
dc.publisherElsevier BVen_US
dc.publisher.placeNetherlandsen_US
dc.publisher.urihttp://www.elsevier.com/locate/coastalengen_AU
dc.relation.ispartofstudentpublicationNen_AU
dc.relation.ispartofpagefrom77en_US
dc.relation.ispartofpageto90en_US
dc.relation.ispartofissue1en_US
dc.relation.ispartofjournalCoastal Engineeringen_US
dc.relation.ispartofvolume54en_US
dc.rights.retentionYen_AU
dc.subject.fieldofresearchcode291199en_US
dc.titleDynamics of a wave-dominated tidal inlet and influence on adjacent beaches, Currumbin Creek, Gold Coast, Australiaen_US
dc.typeJournal articleen_US
dc.type.descriptionC1 - Peer Reviewed (HERDC)en_US
dc.type.codeC - Journal Articlesen_US
gro.facultyGriffith Sciences, Griffith School of Environmenten_US
gro.rights.copyrightCopyright 2007 Elsevier. Please refer to the journal's website for access to the definitive, published version.en_AU
gro.date.issued2007
gro.hasfulltextNo Full Text


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