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The variations in current asymmetry indicate the presence of small-scale circulations of sediment that are induced by smaller channels that penetrate the bar. The current meter observations and depth-averaged current patterns obtained with an ADCP revealed processes of advective flow acceleration and deceleration, as well as flow convergence and divergence, over the bars in the small channels.","AbstractOtherLang":null,"BibLvlCode":"AM","StandardTitle":"Hydrodynamics of a bar in a flood channel - the Westerschelde estuary","OrigTitleLangCode":"en","OrigTitleLangCodeExtended":"eng","OrigTitleLangID":15,"DateLastModified":{"date":"2024-12-10 01:33:17.368041","timezone_type":1,"timezone":"+01:00"},"UserAccessRight":null,"UserAccID":null,"AuthorKeywords":null,"OtherDescriptors":null,"Notes":null,"AnaPub":1997,"MonPub":null,"DateUpdate":"2013-04-17","DateCreate":"2013-04-17","SecASFANote":null,"ConfID":null,"PeerRev":null,"VlizCoreFlag":1,"WoScode":null,"VABBcode":null,"OpenAcc":0},"refs":null,"anarec":{"AnaID":224630,"PubliDate":1997,"Pagination":"4491-4504","XtraPublOfAnaID":null,"ISBN":"0-7844-0242-6","Volume":null,"Issue":null,"BRefMon":35741,"BRefMonRR":"<B>Edge, B.L. 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