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- Negen, E.H. (author) report 1994
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Capobianco, M. (author), De Vriend, H.J. (author), Nicholls, R.J. (author), Stive, M.J.F. (author)Long-term prediction of sediment transport and of morphological behaviour in the coastal zone, in response to human interference or to change in environmental conditions (collectively global change) is an increasingly important issue in coastal zone management, especially in relation to the needs for environmentally compatible development....conference paper 1993
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- Rijn, L.C. van (author) report 1993
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Winter, T. (author)A literature review is undertaken to understand the causes and the effects of the first process. Using the resulting equations, the UNIBEST-TC program is verified for the process of wave transmission over and through a submerged breakwater. Due to the fact that only impermeable breakwaters can be implemented in the program, deviations occur. For...master thesis 1993
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- Karssen, B. (author), Wang, Z.B. (author) report 1993
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- Bilse, D.P. (author) report 1993
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- Wang, Z.B. (author), Fokkink, R.J. (author), Karssen, B. (author) report 1993
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Kamphuis, J.W. (author)To solve coastal sediment transport and morphology problems, it is necessary to construct a hydrodynamics model to simulate the fluid flow. The hydrodynamics model is then used to calculate sediment transport rates and in turn, these sediment transport rates are used to determine morphology. The hydrodynamics model is based on the Equation of...report 1992
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- Steijn, R.C. (author), Hartsuiker, G. (author) report 1992
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- Karssen, B. (author), Wang, Z.B. (author) report 1991
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- Hoozemans, F.M.J. (author) report 1991
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- Steijn, R.C. (author) report 1991
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- Wang, Z.B. (author) report 1991
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Anonymus, A. (author)Translation of two Dutch governmental reports about the decision to maintain the Dutch coastline by means of artificial beach nourishment and to maintain the coastline of 1990 (so in fact compensate all erosion by artificial beach replenishment).report 1990
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Short, A.D. (author)The 120 km long central Netherlands coast consists of an essentially continuous sandy Holocene regressive/transgressive barrier system facing the southern North Sea. The beach and surf zone is composed of predominantly quartz sands which are coarsest at the shoreline (D50 = 286 Um) and fine seaward. Overall shoreface gradients vary between a low...report 1990
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- Zitman, T.J. (author) report 1990
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Louisse, C. (author), Verhagen, H.J. (author)Overview of the Netherlands policy on coastal protection and coastal defenceconference paper 1990
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- Stive, M.J.F. (author), Eysink, W.D. (author) report 1989
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- Hartsuiker, G. (author) report 1989
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- Roelvink, J.A. (author), Stive, M.J.F. (author) report 1989