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- Doets, I.J.E. (author), Mosselman, E. (author), Henrotte, J.J. (author) conference paper 2015
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- Mosselman, E. (author), Kok, M. (author), Leenen, H. (author), Van, M. (author) conference paper 2012
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- Mosselman, E. (author) conference paper 2010
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- Mosselman, E. (author) conference paper 2014
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- Mosselman, E. (author), Marquez, L.G. (author), Klinger, W. (author), Montes, A. (author), Prado, D. (author), Jimenez, J.L. (author) conference paper 2014
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- Van Oorschot, M. (author), Kleinhans, M. (author), Middelkoop, H. (author), Geerling, G. (author), Buijse, T. (author), Mosselman, E. (author) conference paper 2015
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- Hoitink, A.J.F. (author), Eekhout, J.P.C. (author), Makaske, B. (author), Mosselman, E. (author) conference paper 2013
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- Verbruggen, W. (author), Mosselman, E. (author), Zolezzi, G. (author), Sloff, C.J. (author) conference paper 2013
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Van Oorschot, M. (author), Kleinhans, M. (author), Middelkoop, H. (author), Geerling, G. (author), Buijse, T. (author), Mosselman, E. (author)Modelling vegetation and morphodynamics is often one-way traffic that either takes into account the effect of vegetation on morphodynamics or vice versa. The few models that do incorporate an interaction have until now represented vegetation as cylinders causing hydraulic resistance that do not change over time. We coupled a morphodynamic model...conference paper 2014
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Mosselman, E. (author), Le, T.B. (author)Recent years have seen a marked increase in the availability of morphodynamic models and a proliferation of new morphodynamic codes. As a consequence, morphodynamic models are increasingly developed, used and evaluated by non-experts, sometimes leading to mistakes. This presentation draws attention to five types of common mistakes. First, new...conference paper 2014
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- Lindhart, M. (author), Mosselman, E. (author), Avila, H. (author) conference paper 2015
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- Mosselman, E. (author) conference paper 2015
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Van der Meer, C. (author), Mosselman, E. (author), Sloff, C.J. (author), Jagers, B. (author), Zolezzi, G. (author), Tubino, M. (author)Local geometrical perturbations of alluvial channels can generate a pattern of non-migrating bars and pools. This phenomenon is known as “overdeepening”, because the pools locally enhance the scour in river bends. Overdeepening occurs only downstream of a perturbation if the channel is in the subresonant and subcritically damped regime, which...conference paper 2011
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Spruyt, A. (author), Mosselman, E. (author), Jagers, B. (author)River bank retreat and advance are modes of morphological evolution in addition to bed level changes and changes in bed sediment composition. They produce planform changes such as width adjustment and meander bend migration. However, their reproduction in a 2D numerical model still remains a challenge. Defining bank-lines along the nearest grid...conference paper 2011
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- Mosselman, E. (author) conference paper 2015
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- Mosselman, E. (author) conference paper 2012
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Verbruggen, W. (author), Mosselman, E. (author), Zolezzi, G. (author), Sloff, C.J. (author)Local geometrical perturbations in alluvial channels can generate a pattern of alternate bars called ‘overdeepening’. Previous linear analyses and laboratory experiments showed that these bars arise downstream of perturbations in the relatively narrow and deep channels corresponding to subresonant conditions, but both upstream and downstream of...conference paper 2013
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- Mosselman, E. (author) doctoral thesis 1992
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- De Keizer, O. (author), Mosselman, E. (author) journal article 2015
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Kleinhans, M.G. (author), Jagers, H.R.A. (author), Mosselman, E. (author), Sloff, C.J. (author)At river bifurcations, water and sediment are divided over two branches. The dynamics of the bifurcation determine the long-term evolution (centuries) of the downstream branches, potentially leading to avulsion, but the dynamics are poorly understood. The long-term evolution can only be studied by one-dimensional models because of computational...journal article 2008
Searched for: faculty%3A%22Civil%255C%252BEngineering%255C%252Band%255C%252BGeosciences%22
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