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Choy, D.Y. (author)
Offshore sand waves of several meters high and hundreds of meters long are formed in shallow seas due to the tidal currents. These sand waves can, amongst others, influence the burial depth of cables of offshore wind farms and obstruct navigation channels. For the Far Large Offshore Wind programme (FLOW), one of the goals of Deltares is to...
master thesis 2015
document
Steetzel, H.J. (author), Wang, Z.B. (author)
report 2004
document
Nakato, T. (author), Kennedy, J.F. (author), Vadnal, J.L. (author)
The principal features of the numerical model developed herein for calculation of flow and sediment-transport distributions in alluvial-river bends may be summarized as follows: i. The secondary-flow strength and the bed topography are uncoupled from the calculation of distributions of lateral shift velocity and streamwise velocity. This is...
report 1983
document
Karelse, M. (author), Perrels, P.A.J. (author)
report 1982
document
Roelfzema, A. (author)
report 1979
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