{"refrec":{"BRefID":134413,"RR":"<b>Van der Biest, K.; Verwaest, T.; Reyns, J.; Mostaert, F.</b> (2009). CLIMAR: deelrapport 2. Kwantificatie van de secundaire gevolgen van de klimaatsverandering in de Belgische kustvlakte. Versie 2.0. <i>WL Rapporten</i>, 814_01. Waterbouwkundig Laboratorium: Antwerpen. IV, 46 + 22 p. bijlagen pp.","BEntID":128339,"PublicFlag":1,"CheckedFlag":0,"wosflag":0,"vabbflag":0,"RefStringPartII":". Versie 2.0. <i>WL Rapporten</i>, 814_01. Waterbouwkundig Laboratorium: Antwerpen.  IV, 46 + 22 p. bijlagen pp.","DocTypID":13,"DocType":"Reports","MarineFlag":1,"FreshFlag":0,"BrackishFlag":0,"TerrestrialFlag":0,"Authorstring":"Van der Biest, K.; Verwaest, T.; Reyns, J.; Mostaert, F.","OrigTitleTranslFlag":0,"Authorstringtrunc":"Van der Biest, K. <i>et al.</i>","Englishabstract":null,"AbstractOtherLang":"Dit deelrapport werd geschreven in het kader van het BELSPO-project CLIMAR. Het is het tweede deelrapport en beschrijft het door het WL uitgevoerde onderzoek in deel 1 van werkpakket 2: kwantificeren van de secundaire gevolgen van de klimaatswijziging, binnen de lijnen van de case-study “kustoverstromingen”. Ieder scenario van primaire klimaatveranderingen tegen 2100, gedefinieerd in werkpakket 1, wordt vertaald naar één extreme storm. Voor iedere storm wordt een reeks risicoberekeningen uitgevoerd om de omvang van de secundaire gevolgen (overstromingen) te kwantificeren, in termen van schade en slachtoffers. Het eerste model berekent de erosie van strand en duin in de loop van de storm. Vervolgens wordt berekend of er al dan niet een bres ontstaat in de zeewering. De breslocaties worden in een volgend model ingevoerd dat de overstroming van de kustzone simuleert. Tenslotte worden de resultaten van de overstromingsberekening gebruikt voor het inschatten van het aantal dodelijke slachtoffers en de totale monetaire schade.<br>Daarnaast wordt nog een laatste hoofdstuk gewijd aan de berekening van het verlies aan strandoppervlakte in de verschillende klimaatscenario’s. Deze wordt berekend op basis van de ligging van de gemiddelde laagwaterlijn.<br>De resultaten van de berekeningen vormen de basis voor de volgende fase van het project CLIMAR (werkpakket 3): het identificeren van alternatieve aanpassingsstrategieën aan de gevolgen van de klimaatverandering.","BibLvlCode":"MS","StandardTitle":"CLIMAR: deelrapport 2. 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