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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| Effect of climate change on the hydrological regime of navigable water courses in Belgium: subreport 5. Comparison of lumped and distributed models in the climate change impact assessment Vansteenkiste, T.; Pereira, F.; Willems, P.; Mostaert, F. (2012). Effect of climate change on the hydrological regime of navigable water courses in Belgium: subreport 5. Comparison of lumped and distributed models in the climate change impact assessment. Versie 2.0. WL Rapporten, 706_18. Waterbouwkundig Laboratorium/K.U. Leuven: Antwerpen. III, 32 pp.
Deel van: WL Rapporten. Waterbouwkundig Laboratorium: Antwerpen.
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| Beschikbaar in | Auteurs |
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| Documenttype: Projectrapport | |
| Trefwoorden |
Numerical modelling Water management > Hydraulics > Boundary conditions Water management > Hydraulics > Conceptual models België [Marine Regions] |
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| Abstract |
To investigate the uncertainty attributed from the hydrological model structure, several models with different spatial resolutions and process descriptions were considered in the study. Although there are almost countless numbers of model codes, five codes had been chosen to be representative for the different classifications. They range from the simple, lumped, conceptual NAM, PDM and VHM models over the intermediate conceptual-physically based, distributed WetSpa model to the highly detailed, physically based, fully distributed MIKE SHE model, which accounts for the 3-0 groundwater flow and interacts with a MIKE 11 river model to simulate the physical basis of the groundwater-river flow exchange. |
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