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Washover processes at the Wadden Island
of Schiermonnikoog, the Netherlands:
Field data and XBeach modeling
D. Wesselman, M. van der Vegt, R. de Winter
Spiekeroog Wangeroog
Construction of sand-drift dikes prevents overwash
North Sea
Wadden
Sea
Schiermonnikoog
Research question
How is sediment transport during inundation influenced
by wave, tide and storm surge conditions, and by
washover geometry?
1. XBeach 1D mode => wave, tide and storm surge1
2. XBeach 2D mode => washover geometry
1Wesselman et al., 2017
XBeach 1D => model set-up + fieldwork
Boundary conditions
• Water level stations
in North Sea and
Wadden Sea
• Wave buoy in North
Sea
Parameter settings
• γ = 0.45 in Roelvink2
(wave breaking)
• Other: Default values
XBeach 1D => Validation
• 6 classes, based
on 25 years of
water level data
• Tidal phase
difference
• Larger water
level increase in
Wadden Sea
• Higher class =>
larger waves
XBeach 1D => Analysis of processes
XBeach 1D => Analysis of processes
XBeach 1D => Analysis of processes
• Currents => dominate sediment transport
• Currents => depend on pressure gradient between North
Sea and Wadden Sea
• Pressure gradient => interplay between tide, storm surge
and wave set-up
• Small but frequenly-occuring inundation events are
important for the net and long-term sediment transport
XBeach 2D => Model set-up
• Constant water level of 2.5 m in North Sea and Wadden Sea
• Constant waves: Class 5 previous study
XBeach 2D => Results
Currents
• Alongshore in shallow water
• Cross-shore through
washover opening
• Flow contraction leads to
acceleration
XBeach 2D => Results
XBeach 2D => Results
Take home messages
• We successfully validated the hydrodynamics in XBeach (1D)
during inundation for mesotidal storm conditions.
• Currents dominate sediment transport at Schiermonnikoog
in the inundation phase.
• Water levels (tide, storm surge, wave set-up) in both the
North Sea and Wadden sea must be taken into account.
• The hydrodynamics and sediment transport are sensitive to
the washover opening dimensions.
1Wesselman D, de Winter R, Engelstad A, McCall R, van
Dongeren A, Hoekstra P, Oost A, van der Vegt M. 2017. The
effect of tides and storms on the sediment transport across a
Dutch barrier island. Earth Surface Processes and Landforms
Additional slides
Increasing washover opening width
Increasingwashoveropeningheight

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DSD-INT 2017 Washover processes at the Wadden Island of Schiermonnikoog, The Netherlands: Field data and XBeach modeling - Wesselman

  • 1. Washover processes at the Wadden Island of Schiermonnikoog, the Netherlands: Field data and XBeach modeling D. Wesselman, M. van der Vegt, R. de Winter
  • 2. Spiekeroog Wangeroog Construction of sand-drift dikes prevents overwash
  • 5. Research question How is sediment transport during inundation influenced by wave, tide and storm surge conditions, and by washover geometry? 1. XBeach 1D mode => wave, tide and storm surge1 2. XBeach 2D mode => washover geometry 1Wesselman et al., 2017
  • 6. XBeach 1D => model set-up + fieldwork Boundary conditions • Water level stations in North Sea and Wadden Sea • Wave buoy in North Sea Parameter settings • γ = 0.45 in Roelvink2 (wave breaking) • Other: Default values
  • 7. XBeach 1D => Validation
  • 8. • 6 classes, based on 25 years of water level data • Tidal phase difference • Larger water level increase in Wadden Sea • Higher class => larger waves XBeach 1D => Analysis of processes
  • 9. XBeach 1D => Analysis of processes
  • 10. XBeach 1D => Analysis of processes • Currents => dominate sediment transport • Currents => depend on pressure gradient between North Sea and Wadden Sea • Pressure gradient => interplay between tide, storm surge and wave set-up • Small but frequenly-occuring inundation events are important for the net and long-term sediment transport
  • 11. XBeach 2D => Model set-up • Constant water level of 2.5 m in North Sea and Wadden Sea • Constant waves: Class 5 previous study
  • 12. XBeach 2D => Results Currents • Alongshore in shallow water • Cross-shore through washover opening • Flow contraction leads to acceleration
  • 13. XBeach 2D => Results
  • 14. XBeach 2D => Results
  • 15. Take home messages • We successfully validated the hydrodynamics in XBeach (1D) during inundation for mesotidal storm conditions. • Currents dominate sediment transport at Schiermonnikoog in the inundation phase. • Water levels (tide, storm surge, wave set-up) in both the North Sea and Wadden sea must be taken into account. • The hydrodynamics and sediment transport are sensitive to the washover opening dimensions.
  • 16. 1Wesselman D, de Winter R, Engelstad A, McCall R, van Dongeren A, Hoekstra P, Oost A, van der Vegt M. 2017. The effect of tides and storms on the sediment transport across a Dutch barrier island. Earth Surface Processes and Landforms
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  • 23. Increasing washover opening width Increasingwashoveropeningheight