{"refrec":{"BRefID":365244,"RR":"<b>Stark, J.; Plancke, Y.</b> (2023). Representatie stijgsnelheid en verhang Terneuzen-Hansweert in numerieke modellen: verkennende kalibratieoefening met NeVla model. Versie 3.0. <i>WL Rapporten</i>, 22_069_1. Waterbouwkundig Laboratorium: Antwerpen. VII, 23 pp. <a href=\"https://dx.doi.org/10.48607/196\" target=\"_blank\">https://dx.doi.org/10.48607/196</a>","BEntID":362964,"PublicFlag":1,"CheckedFlag":0,"wosflag":0,"vabbflag":0,"RefStringPartII":". Versie 3.0. <i>WL Rapporten</i>, 22_069_1. Waterbouwkundig Laboratorium: Antwerpen.  VII, 23 pp. <a href=\"https://dx.doi.org/10.48607/196\" target=\"_blank\">https://dx.doi.org/10.48607/196</a>","DocTypID":13,"DocType":"Reports","MarineFlag":0,"FreshFlag":0,"BrackishFlag":0,"TerrestrialFlag":0,"Authorstring":"Stark, J.; Plancke, Y.","OrigTitleTranslFlag":0,"Authorstringtrunc":"Stark, J.; Plancke, Y.","Englishabstract":null,"AbstractOtherLang":"In dit rapport wordt een kalibratieoefening gepresenteerd voor het (Delft3D) NeVla model waarin getracht  wordt om door middel van aanpassingen in het bodemruwheidsveld de representatie van de belangrijkste  indicatoren voor de sterkte van de dwarsstroming, i.e., het maximale verhang tussen Terneuzen en  Hansweert en de maximale stijgsnelheid te Hansweert, te verbeteren. Uit een eerdere validatieoefening is  namelijk gebleken dat het NeVla voorspelmodel zowel de sterkte van de dwarsstromingen zelf alsmede de  waterstandsindicatoren niet goed representeert voor de hoogste springtijen.<br>De huidige kalibratieoefening toont aan dat het inderdaad mogelijk is de representatie van deze parameters  te verbeteren door de ruwheid in de hoofdgeul (i.e., Gat van Ossenisse) en nevengeul (i.e., Middelgat) tussen  Terneuzen en Hansweert te verlagen. De gemiddelde afwijking voor het maximale verhang tussen Terneuzen  en Hansweert neemt dan af van 23 cm in de huidige NeVla configuratie naar 3-4 cm in enkele kalibratieruns  en de afwijking van de maximale stijgsnelheid te Hansweert neemt af van 0,29 cm∙min-1 naar minder dan  0,05 cm∙min-1 in de meest optimale kalibratieruns. Een verlaging van de bodemruwheid in dit gebied leidt  echter tot een overschatting van de getijslag verder opwaarts in het estuarium, waardoor extra aanpassingen  aan het ruwheidsveld noodzakelijk zijn om de algehele modelprestatie op peil te houden.","BibLvlCode":"MS","StandardTitle":"Representatie stijgsnelheid en verhang Terneuzen-Hansweert in numerieke modellen: verkennende kalibratieoefening met NeVla model","OrigTitleLangCode":"nl","OrigTitleLangCodeExtended":"dut","OrigTitleLangID":41,"DateLastModified":{"date":"2026-04-18 01:39:43.873435","timezone_type":1,"timezone":"+02:00"},"UserAccessRight":null,"UserAccID":null,"AuthorKeywords":"Delft3D; NeVla; Dwarsstroming","OtherDescriptors":null,"Notes":null,"AnaPub":null,"MonPub":2023,"DateUpdate":"2023-08-28","DateCreate":"2023-06-21","SecASFANote":null,"ConfID":null,"PeerRev":0,"VlizCoreFlag":1,"WoScode":null,"VABBcode":null,"OpenAcc":0},"refs":null,"anarec":null,"monrec":{"MonID":365244,"ISBN":null,"PubliDate":2023,"IssueDate":null,"Volume":"22_069_1","Issue":null,"Pagination":"VII, 23","Place":"Antwerpen","Edition":"Versie 3.0","BRefXtra":null,"BRefXtraRR":null,"SerID":24938,"SerRR":"WL Rapporten. 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