{"refrec":{"BRefID":120828,"RR":"<b>Vanlede, J.; De Mulder, T.; Mostaert, F.</b> (2008). Harmonische voorspelling van waterstanden te Vlissingen, ter aanvulling van de OMES databank. <i>WL Rapporten</i>, 713_22. Waterbouwkundig Laboratorium: Antwerpen. 9 + 21 appendices pp.","BEntID":114949,"PublicFlag":1,"CheckedFlag":0,"wosflag":0,"vabbflag":0,"RefStringPartII":". <i>WL Rapporten</i>, 713_22. Waterbouwkundig Laboratorium: Antwerpen.  9 + 21 appendices pp.","DocTypID":13,"DocType":"Reports","MarineFlag":1,"FreshFlag":0,"BrackishFlag":0,"TerrestrialFlag":0,"Authorstring":"Vanlede, J.; De Mulder, T.; Mostaert, F.","OrigTitleTranslFlag":0,"Authorstringtrunc":"Vanlede, J.; De Mulder, T.; Mostaert, F.","Englishabstract":null,"AbstractOtherLang":"Deze opdracht kadert binnen de bestaande samenwerkingsovereenkomst tussen het WL Borgerhout en het VLIZ.Aan de hand van de publiek beschikbare gegevens uit de Xtide database (http://www.flaterco.com/xtide/), wordt een harmonische voorspelling gemaakt van de tijdstippen van hoog- en laagwater te Vlissingen. In vergelijking met het tijboekje voor 2007 wordt (voor de maand januari) het tijdstip van hoog- en laagwater op 3 minuten na nauwkeurig voorspeld, en de hoogte op 5 cm na.<br>Gebruik makend van de gekende gemiddelde tijkarakteristieken te Vlissingen wordt elk harmonische voorspeld getij verder geclassificeerd als doodtij, gemiddeld tij of springtij.<br>Vanuit de tijdstippen van hoog- en laagwater te Vlissingen als referentiestation kan het overeenkomstige tijdstip van hoog- en laagwater op een willekeurige plaats in het Schelde-estuarium worden berekend aan de hand van de gekende voortplantingseigenschappen van de getijgolf. 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