De Schipper
Delft University of Technology
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Featured researches published by De Schipper.
Jubilee conference proceedings, NCK-days 2012 : Crossing borders in coastal research, Enschede, Nederland, 13-16 maart 2012 | 2012
De Schipper; S. de Vries; R.W.M.R.J.B. Ranasinghe; Ad J. H. M. Reniers; M.J.F. Stive
Typically a beach is out of equilibrium after a nourishment is installed. To observe how a nourished beach behaves on the timescale of storms a monitoring campaign was set up at Vlugtenburg beach after a nourishment in the spring of 2009. Here we show a sediment budget analysis of the first 2.5 years for a coastal domain spanning 1750 m alongshore from -9 to +5 m NAP. To investigate the redistribution of nourished sand different sections of the profile are examined. Observations show that the initial response (first 6 to 12 months after construction) is large where the sediment eroded from the beach is transported offshore to form a subtidal bar. In the following period (until present) the losses in the domain are on the order of 40 m3 per m alongshore per year. These losses are concentrated in the profile around the waterline.
Coastal Sediments 2015 | 2015
S. de Vries; Mitchell D. Harley; De Schipper; Gerben Ruessink; Ping Wang; Julie D Rosati; Jun Cheng
The development of dunes is characterized by the alternating effects of erosion during storm events and growth during milder conditions. The quantification of dune growth due to aeolian processes has received some attention but uncertainty remains on where the dune sand, which accommodates growing dunes, originates from in the coastal profile. In this paper we hypothesize that sediment eroded from the upper beach is the main sediment supply for aeolian sediment transport governing dune growth. To test this hypothesis we have analyzed morphological profiles collected monthly at three different field sites (Noordwijk, Vlugtenburg and Narrabeen) during several years. No significant erosive trend due to aeolian processes was found at the upper beach at this temporal resolution. We conclude that it is highly unlikely that the main supply for aeolian sediment transport governing dune growth was located at the upper beach. The intertidal zone might be a relevant alternative source of sediment in the cross shore profile.
Coastal Dynamics 2013: 7th International Conference on Coastal Dynamics, Arcachon, France, 24-28 June 2013 | 2013
De Schipper; S. de Vries; R.W.M.R.J.B. Ranasinghe; Ad J. H. M. Reniers; M.J.F. Stive
Coastal Dynamics 2013: 7th International Conference on Coastal Dynamics, Arcachon, France, 24-28 June 2013 | 2013
M.E. Wengrove; Martijn Henriquez; De Schipper; Robert A. Holman; M.J.F. Stive
Coastal Dynamics 2013: 7th International Conference on Coastal Dynamics, Arcachon, France, 24-28 June 2013 | 2013
M.J.F. Stive; De Schipper; Arjen Luijendijk; R.W.M.R.J.B. Ranasinghe; J.S.M. van Thiel de Vries; Stefan Aarninkhof; C. van Gelder-Maas; S. de Vries; Martijn Henriquez; Sarah Marx
ICCE 2014: Proceedings of 34th International Conference on Coastal Engineering, Seoul, Korea, 15-20 juni 2014 | 2014
A.O. Kaji; Arjen Luijendijk; J.S.M. van Thiel de Vries; De Schipper; M.J.F. Stive
Oikos | 2010
De Schipper; R.W.M.R.J.B. Ranasinghe; Ad Reniers; M.J.F. Stive
E-proceedings of the 36th IAHR World Congress, The Hague, the Netherlands, 28 June-3 July 2015 | 2015
S. de Vries; M. Radermacher; De Schipper; M.J.F. Stive
Proceedings of Coastal Dynamics 2017 | 2017
M. Radermacher; Wessel Geerlof; De Schipper; B.J.A. Huisman; S.G.J. Aarninkhof; Ad Reniers; Troels Aagaard; Rolf Deigaard; David R. Fuhrman
Proceedings of the 35th IAHR World Congress, Chengdu, China, 8-13 September 2013 | 2013
M.J.F. Stive; De Schipper; Arjen Luijendijk; R.W.M.R.J.B. Ranasinghe; S.G.J. Aarninkhof
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