- document
- Ribberink, J.S. (author) report 1989
- document
-
Verhagen, H.J. (author)Sand waves, defined as longshore wave-like movements of the shoreline, measured in a horizontal plane, are described along several stretches of the shoreline of The Netherlands. They have a celerity in the order of 50-200 m/yr, a period of 50- 150 years and an amplitude of 30- 500 m. They are found along the whole Dutch shoreline. Analysis of...report 1989
- document
- Hoozemans, F.M.J. (author) report 1991
- document
- Rijn, L.C. van (author) report 1993
- document
- Steetzel, H.J. (author) report 1995
- document
- Rijn, L.C. van (author), Reniers, A.J.H.M. (author), Zitman, T.J. (author), Ribberink, J.S. (author) report 1995
- document
- report 1995
- document
- Rijn, L.C. van (author) report 1995
- document
- Rijn, L.C. van (author), Ribberink, J.S. (author), Dunsbergen, D.W. (author) report 1996
- document
-
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
- document
- Walstra, D.J.R. (author), Rijn, L.C. van (author), Aarninkhof, S.G.J. (author) report 1998
- document
- 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
- Nipius, L.J. (author) report 2002
- document
- Rijn, L.C. van (author), Walstra, D.J.R. (author), Boer, G. de (author) report 2002
- document
- Wang, Z.B. (author), Steetzel, H.J. (author) report 2003
- document
- Steetzel, H.J. (author), Wang, Z.B. (author) report 2003
- document
- Geleynse, N. (author) report 2007
- document
-
Van der Woerdt, W. (author), Van den Bosch, I. (author), Heerema, R. (author), Ruijs, M. (author)Master project report. The hydraulic efficiency of the river Araranguá will be increased by the construction of jetties at the mouth of the river. The river tends to migrate from south to north which decreases the hydraulic efficiency and causes flooding upstream during events of high discharge. To stop the migration the construction of jetties...student report 2009