{"refrec":{"BRefID":200580,"RR":"<b>Van Steenbergen, N.; Deschamps, M.; Boeckx, L.; Van Eerdenbrugh, K.; Willems, P.; Mostaert, F.</b> (2010). Onderhoud voorspellingsmodellen: onderzoek naar gebruik radarbeelden voor voorspellingsmodellen. versie 2.0. <i>WL Rapporten</i>, 729_05d. Waterbouwkundig Laboratorium: Antwerpen. III, 34 pp.","BEntID":192844,"PublicFlag":1,"CheckedFlag":0,"wosflag":0,"vabbflag":0,"RefStringPartII":". versie 2.0. <i>WL Rapporten</i>, 729_05d. Waterbouwkundig Laboratorium: Antwerpen.  III, 34 pp.","DocTypID":13,"DocType":"Reports","MarineFlag":0,"FreshFlag":0,"BrackishFlag":0,"TerrestrialFlag":0,"Authorstring":"Van Steenbergen, N.; Deschamps, M.; Boeckx, L.; Van Eerdenbrugh, K.; Willems, P.; Mostaert, F.","OrigTitleTranslFlag":0,"Authorstringtrunc":"Van Steenbergen, N. <i>et al.</i>","Englishabstract":null,"AbstractOtherLang":"In deze studie wordt onderzocht of radarbeelden als invoer kunnen gebruikt worden voor hydrologische modellen. Hiervoor wordt het bekken van de Herk als gevalstudie gebruikt. Op basis van radarbeelden die verkregen zijn van de neerslagradar van het KMI te Wideumont wordt de ruimtelijke neerslag berekend voor het hydrologisch model van de Herk en dit voor 7 periodes. De radarbeelden worden ook aangepast aan de pluviograafgegevens door middel van de methode van Brandes (voor verschillende tijdsvensters) en de kriging methode. Er wordt een onderlinge vergelijking tussen de ruimtelijke neerslag van de verschillende gegevensbronnen en correctiemethoden gemaakt. Ook wordt de uitvoer van het hydrologisch model van de Herk op basis van de verschillende invoer vergeleken met de debietsmetingen. Hieruit blijkt dat na een grafische en statistische vergelijking, de invoer op basis van ruwe radarbeelden geen verbetering is in vergelijking met de invoer op basis van pluviograafgegevens. Wel is het zo dat indien deze radarbeelden aangepast worden aan de hand van pluviograafmetingen de resultaten verbeteren en een even betrouwbare invoer wordt bekomen. Dit geldt zeker voor de Brandes methode waarbij de aanpassingsfactoren worden berekend op basis van een tijdsperiode van een dag of langer. Ook wordt aangetoond dat met de kriging methode de resultaten meer constant zijn dan met de andere methodes en zelfs in vergelijking met de invoer op basis van pluviometers. Ook is het mogelijk om de onzekerheid van de kriging methode te bepalen en aan de hand hiervan onzekerheidsbanden op te stellen","BibLvlCode":"MS","StandardTitle":"Onderhoud voorspellingsmodellen: onderzoek naar gebruik radarbeelden voor voorspellingsmodellen","OrigTitleLangCode":"nl","OrigTitleLangCodeExtended":"dut","OrigTitleLangID":41,"DateLastModified":{"date":"2026-06-11 01:43:40.863815","timezone_type":1,"timezone":"+02:00"},"UserAccessRight":null,"UserAccID":null,"AuthorKeywords":null,"OtherDescriptors":null,"Notes":null,"AnaPub":null,"MonPub":2010,"DateUpdate":"2020-09-18","DateCreate":"2010-12-02","SecASFANote":null,"ConfID":null,"PeerRev":0,"VlizCoreFlag":0,"WoScode":null,"VABBcode":null,"OpenAcc":0},"refs":null,"anarec":null,"monrec":{"MonID":200580,"ISBN":null,"PubliDate":2010,"IssueDate":null,"Volume":"729_05d","Issue":null,"Pagination":"III, 34","Place":"Antwerpen","Edition":"versie 2.0","BRefXtra":null,"BRefXtraRR":null,"SerID":24938,"SerRR":"WL Rapporten. 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