{"refrec":{"BRefID":359690,"RR":"<b>Vandenbruwaene, W.; Bertels, J.; Michielsen, S.; Thant, S.; van den Berg, M.; Brackx, M.; Hertoghs, R.; Claeys, S.; Plancke, Y.; Meire, D.; Vereecken, H.; Deschamps, M.</b> (2022). Monitoring Effecten Ontwikkelingsschets (MONEOS) – Jaarboek monitoring 2021: data rapportage monitoring waterbeweging en fysische parameters in Zeeschelde en bijrivieren. Versie 3.0. <i>WL Rapporten</i>, PA047_11. Waterbouwkundig Laboratorium: Antwerpen. XIV, 91 + 19 p. bijl. pp. <a href=\"https://dx.doi.org/10.48607/139\" target=\"_blank\">https://dx.doi.org/10.48607/139</a>","BEntID":357405,"PublicFlag":1,"CheckedFlag":0,"wosflag":0,"vabbflag":0,"RefStringPartII":". Versie 3.0. <i>WL Rapporten</i>, PA047_11. Waterbouwkundig Laboratorium: Antwerpen.  XIV, 91 + 19 p. bijl. pp. <a href=\"https://dx.doi.org/10.48607/139\" target=\"_blank\">https://dx.doi.org/10.48607/139</a>","DocTypID":13,"DocType":"Reports","MarineFlag":0,"FreshFlag":0,"BrackishFlag":0,"TerrestrialFlag":0,"Authorstring":"Vandenbruwaene, W.; Bertels, J.; Michielsen, S.; Thant, S.; van den Berg, M.; Brackx, M.; Hertoghs, R.; Claeys, S.; Plancke, Y.; Meire, D.; Vereecken, H.; Deschamps, M.","OrigTitleTranslFlag":0,"Authorstringtrunc":"Vandenbruwaene, W. <i>et al.</i>","Englishabstract":null,"AbstractOtherLang":"Voorliggend MONEOS jaarboek presenteert de resultaten van de systeemmonitoring in het Schelde  estuarium uitgevoerd door het WL-HIC in het jaar 2021. De uitgevoerde monitoring betreft de continue  metingen van waterstand, debiet, stroming, saliniteit en sedimentconcentratie, alsook vaarten (halftij-eb en  13-uursmetingen), golfmetingen en periodieke metingen zwevende stof. Het jaar 2021 wordt in de maanden  januari, februari, juli, en december gekenmerkt door verhoogde bovenafvoer. Te Schelle is de totale  berekende bovenafvoer in de maand december abnormaal hoog. Meest opvallende vaststelling is echter de  uitzonderlijke hoge bovenafvoer in de maand juli. In de afgelopen normaalperiode (periode van 30 jaar  voorafgaand aan het beschouwde kalenderjaar) is de berekende bovenafvoer voor juli nog nooit zo hoog  geweest. Dit is te wijten aan de hoge neerslaghoeveelheden die gevallen zijn in het begin van de maand juli,  en de extreme neerslaghoeveelheden die gevallen zijn in de periode 13-16 juli over het oosten (en in mindere  mate het centrum) van het land. Dit resulteerde in uitzonderlijke hoge afvoeren langsheen de Demer, de Dijle  en de Netes. Wat betreft het getij is er in het jaar 2021 slechts 1 stormvloed opgetreden. Op 7 november  wordt te Antwerpen een waterstand van 6,62 mTAW bereikt. De retourperiode voor deze waterstand  bedraagt minder dan een half jaar. In tegenstelling tot de voorafgaande droge jaren (periode 2017-2020)  wordt het jaar 2021 gekenmerkt door min of meer normale bovenafvoer, met uitzondering van de hoge  bovenafvoer in de maand juli. De normale afvoer in combinatie met de uitzonderlijke hoge afvoer in de  maand juli, resulteert in duidelijk lagere zoutgehaltes in het Schelde estuarium. Te Prosperpolder bedraagt  het maximale zoutgehalte in de zomer om en bij de 15 PSU, terwijl dit voor het jaar 2020 nog opliep tot 21  PSU. Voor de sedimentconcentraties is het beeld iets minder éénduidig. Voornamelijk in de periode maart  tot en met september zijn de sedimentconcentraties voor het jaar 2021 lager in vergelijking met de voorgaande jaren. 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