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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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Negen, E.H. (author)
report 1994
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Karssen, B. (author)
report 1994
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Steetzel, H.J. (author)
report 1995
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Rijn, L.C. van (author), Reniers, A.J.H.M. (author), Zitman, T.J. (author), Ribberink, J.S. (author)
report 1995
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report 1995
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Rijn, L.C. van (author)
report 1995
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Ribberink, J.S. (author)
report 1996
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Roelfzema, A. (author)
report 1996
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Rijn, L.C. van (author), Ribberink, J.S. (author), Dunsbergen, D.W. (author)
report 1996
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Bosboom, J. (author), Aarninkhof, S.G.J. (author), Roelvink, J.A. (author), Walstra, D.J.R. (author)
report 1996
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Ahmed, A.S.M. (author)
The developmeot of the coastal area is oeeded for tourism and commercial purposes for a country located nearby a coast. Coastal development may lead to local erosion of the shoreline. Coastal defence structures, like an offshore breakwaters, may be used to solve tbis problem. An offshore breakwater is a breakwater parallel to the shore and...
report 1997
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Baan, P.J.A. (author), Hulsbergen, C.H. (author), Marchand, M. (author)
report 1997
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Marchand, M. (author)
report 1998
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Plant, N.G. (author)
This study showed that, in spite of annual and intra-annual forcing, interannual frequencies explained over 70% of the temporal morphologic variability observed at a beach near Duck, NC. Dominant interannual variability is not consistent with most existing conceptual models, which predict morphologic response at the same time scale as the...
report 1998
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Walstra, D.J.R. (author), Rijn, L.C. van (author), Aarninkhof, S.G.J. (author)
report 1998
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Bakker, W.T. (author)
This book deals on "Coastal Dynamics", which will be defined in a narrow sense as a mathematical theory, which starts from given equations of motion for the sediment, which leads with the continuity equation and given boundary conditions to a calculated (eventually schematized) coastal topography, which is generally a function of time. This is...
report 1998
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D' Angremond, K. (author), Somers, C.M.G. (author)
Natural system, coastal dynamics, climatology, oceanography, morphology. Coastal formations, Coast and culture, The Netherlands.
lecture notes 1998
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Stive, M.J.F. (author), Meerendonk, E. van (author), Rijn, L.C. van (author), Weck, A.W. van der (author), Walstra, D.J.R. (author), Roelvink, J.A. (author)
report 1998
document
Stive, M.J.F. (author)
report 1999
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