The effect of climate change on extreme waves in front of the Dutch coast
Publication date
2012
Authors
Winter, R.C. de
Sterl, A.
Vries, J.W. de
Weber, S.L.
Ruessink, B.G.
Editors
Advisors
Supervisors
Document Type
Article
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(c) UU Universiteit Utrecht, 2012
Abstract
Coastal safety may be influenced by climate
change, as changes in wave conditions (height, period,
direction) may increase the vulnerability of dunes and
other coastal defences. Dune erosion depends on mean
water level, storm surge height and wave conditions. In
this paper, we investigate the change in wave conditions
in the North Sea in a changing climate. Until now, the
effect of climate change on annual maximum wave conditions
has been investigated, while events with higher
return periods are actually most damaging for the coast
(e.g. severe dune erosion). Here, we use the 17-member
Ensemble SimulationS of Extreme weather under Nonlinear
Climate changeE (ESSENCE) change of climate
change simulations, to analyse A1b-induced changes in
the mean wave climate, the annual maxima and wave
conditions with return periods of up to 1:10,000 years
in front of the Dutch coast. The mean wave climate is
not projected to differ between 1961–1990 and 2071–
2100, with both wave height (Hs) and wave period (Tm)
remaining unaltered. In the annual maximum conditions,
a decrease is projected; especially, the annual Tm
maximum decreases significantly by 0.3 to 0.6 s over
Responsible Editor: Birgit Andrea Klein
S. L. Weber, deceased 12 August 2011.
R. C. de Winter (B) · S. L. Weber · B. G. Ruessink
Department of Physical Geography, Faculty of Geosciences,
Institute for Marine and Atmospheric Research,
Utrecht University, P.O. Box 80.115,
3508 TC Utrecht, Netherlands
e-mail: r.c.dewinter@uu.nl
R. C. de Winter · A. Sterl · J. W. de Vries · S. L. Weber
Royal Netherlands Meteorological Institute (KNMI),
P.O. Box 201, 3730 AE De Bilt, Netherlands
the whole study area. Furthermore, we find that the
direction of the annual maximum wave conditions shifts
from north and north-west to west and south-west for
both Hs and Tm. This is induced by a similar shift in
the direction of the extreme wind speeds. Despite the
decrease in annual maximum conditions, the return Hs
and Tm are not projected to change significantly as a
result of climate change in front of the Dutch coast for
the period 2071–2100 relative to 1961–1990.
Keywords
Climate change, Waves, Extremes, North Sea