{"refrec":{"BRefID":361022,"RR":"<b>Plancke, Y.; Stark, J.</b> (2022). Dwarsstromingen Platen van Ossenisse: deelrapport 1. Bepalen kans op voorkomen van hydrodynamische condities en bijbehorende dwarsstroming. Versie 3.0. <i>WL Rapporten</i>, 22_036_1. Waterbouwkundig Laboratorium: Antwerpen. VI, 20 + 7 bijl. pp. <a href=\"https://dx.doi.org/10.48607/150\" target=\"_blank\">https://dx.doi.org/10.48607/150</a>","BEntID":358737,"PublicFlag":1,"CheckedFlag":0,"wosflag":0,"vabbflag":0,"RefStringPartII":". Versie 3.0. <i>WL Rapporten</i>, 22_036_1. Waterbouwkundig Laboratorium: Antwerpen.  VI, 20 + 7 bijl. pp. <a href=\"https://dx.doi.org/10.48607/150\" target=\"_blank\">https://dx.doi.org/10.48607/150</a>","DocTypID":13,"DocType":"Reports","MarineFlag":0,"FreshFlag":0,"BrackishFlag":0,"TerrestrialFlag":0,"Authorstring":"Plancke, Y.; Stark, J.","OrigTitleTranslFlag":0,"Authorstringtrunc":"Plancke, Y.; Stark, J.","Englishabstract":null,"AbstractOtherLang":"Ter hoogte van de Platen van Ossenisse treden bij sterke springtijen rond het moment van hoogwater  dwarsstromingen op, die een potentieel risico kunnen vormen voor de scheepvaart. Door Rijkswaterstaat  worden er daarom jaarlijks voorwaarschuwingen gepubliceerd, waarin de momenten van “matige” en  “sterke” dwarsstroming worden weergegeven. De dwarsstromingen kennen echter een gradueel verloop,  vandaar dat binnen voorliggend rapport de kans op voorkomen van een bepaalde dwarsstroming ter hoogte  van de oostrand van de Platen van Ossenisse is berekend. Aan de hand van de waterstandsparameters  “verval tussen Terneuzen en Hansweert” en “stijgsnelheid te Hansweert” werd de sterkte van de  dwarsstroming afgeleid voor elke getij over de periode 2010-2021, en werd met behulp van een lineaire  correlatie tussen deze waterstandsparameters en de sterkte van de dwarsstroming vervolgens de kans op  voorkomen van een bepaalde dwarsstroming bepaald.<br>Tevens wordt in dit rapport een vergelijking gemaakt tussen de waterstandsparameters berekend uit de  astronomisch voorspelde waterstanden en de gemeten waterstanden voor de jaren 2020 en 2021. Tenslotte  wordt voor het eerste kwartaal van 2022 een vergelijking gemaakt tussen de astronomisch voorspelde  momenten van dwarsstroming, de door middel van de operationele modellen voorspelde momenten van  dwarsstroming en de uit de waterstandsmetingen afgeleide dwarsstromingen. ","BibLvlCode":"MS","StandardTitle":"Dwarsstromingen Platen van Ossenisse: deelrapport 1. 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