Over het archief
In 2012 verloren we Jean Jacques Peters, voormalig ingenieur van het Waterbouwkundig Laboratorium (1964 tot 1979) en internationaal expert in sedimenttransport, rivierhydraulica en -morfologie. Als eerbetoon aan hem hebben we potamology (http://www.potamology.com/) gecreëerd, een virtueel gedenkarchief dat als doel heeft om zijn manier van denken en morfologische aanpak van rivierproblemen in de wereld in stand te houden en te verspreiden.
Het merendeel van z’n werk hebben we toegankelijk gemaakt via onderstaande zoekinterface.
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| one publication added to basket [201098] | |
| The North Atlantic Oscillation's relation with the Scheldt streamflow: Examination of the contribution to the NAO index's influence over the Belgian Continental Shelf's benthos Levy, Y.; Verwaest, T.; De Mulder, T.; Mostaert, F. (2010). The North Atlantic Oscillation's relation with the Scheldt streamflow: Examination of the contribution to the NAO index's influence over the Belgian Continental Shelf's benthos. version 2.0. WL Adviezen, 814_02b. Flanders Hydraulics Research: Antwerp. II, 28 + 1 p. app. pp.
Deel van: WL Adviezen. Waterbouwkundig Laboratorium: Antwerpen.
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| Documenttype: Projectrapport | |
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Literature and desktop study North Atlantic Oscillation Marien/Kust |
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Contactgegevens
Opdrachtgever: Vlaamse overheid; Beleidsdomein Mobiliteit en Openbare Werken; Vlaams Ministerie Mobiliteit en Openbare Werken; Departement Mobiliteit en Openbare Werken; Waterbouwkundig Laboratorium; Eigen Vermogen Flanders Hydraulics (EVFH)
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| Abstract |
Lineary regressions were first established between both NAO index and streamflow at various timescales. No timescales, wether seasonal, monthly or ten-days, have revealed significant linear relation with practically null R2 throughout the analysis. An unlineary relation, for which the Spearman’s correlation coefficient was used, hardly reveals any different yearly NAO / Q relation with a ρ not exceeding 15 %. Before concluding uncorrelation between the two factors, differentiating stormflow from baseflow within the streamflow might reveal more robust relationships at the shortest timescales, given the watershed’s time of concentration. An endeavor to follow other authors’ preceding NAO correlations with environmental factors on their methodology did motivate the use of cumsum logarithmic transformations. These have only corroborated the absence of correlation between NAO and Scheldt streamflow. |
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