{"refrec":{"BRefID":219204,"RR":"<b>Deschamps, M.; Van Steenbergen, N.; Boeckx, L.; Mostaert, F.</b> (2012). Was maart 2012: beschrijving meteorologische en hydrologische gebeurtenissen. versie 2.0. <i>WL Rapporten</i>, 00_119. Waterbouwkundig Laboratorium: Antwerpen. IV, 37 pp.","BEntID":210943,"PublicFlag":1,"CheckedFlag":0,"wosflag":0,"vabbflag":0,"RefStringPartII":". versie 2.0. <i>WL Rapporten</i>, 00_119. Waterbouwkundig Laboratorium: Antwerpen.  IV, 37 pp.","DocTypID":13,"DocType":"Reports","MarineFlag":0,"FreshFlag":0,"BrackishFlag":0,"TerrestrialFlag":0,"Authorstring":"Deschamps, M.; Van Steenbergen, N.; Boeckx, L.; Mostaert, F.","OrigTitleTranslFlag":0,"Authorstringtrunc":"Deschamps, M. <i>et al.</i>","Englishabstract":null,"AbstractOtherLang":"Een grote hoeveelheid neerslag begin maart 2012 zorgde voor hoge afvoeren op de bevaarbare waterlopen in het westen van Vlaanderen. De grootste hoeveelheid neerslag viel in de Franse bekkens van de IJzer, Leie en Bovenschelde (tot 95mm te Radinghem). Op de IJzer te Roesbrugge werd de hoogste afvoer ooit geregistreerd (106m<sup>3</sup>/s). De IJzer overstroomde en de Blankaart bereikte een maximaal peil van 4.28m TAW (2e hoogste waarde sinds begin van de metingen). Ook op de Leie te Menen werd de hoogste afvoer sinds de start van de metingen gemeten (233m<sup>3</sup>/s). Alle afwateringskanalen moesten benut worden om Gent te beschermen tegen wateroverlast. De keersluis te Beernem werd gesloten om Brugge te beschermen. De voorspellingsmodellen reageerden goed op de voorspelde neerslag, verbetering van de nauwkeurigheid van de voorspellingen is nodig. 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