In this paper, laboratory data for free surface displacements and velocity
fields in front of a caisson breakwater covered with wave-dissipating block
s, together with wave pressures acting on the caisson, are presented and di
scussed. The core of the breakwater is made of a concrete caisson with a ve
rtical front wall. The caisson is protected by a thick layer of tetrapods a
nd is supported by a rubble mound. The breakwater is placed on the 1/25 imp
ermeable slope. Two types of incident waves are used in the experiments: no
nbreaking waves and spilling-type breaking waves. In the breaking wave case
, the incident wave breaks offshore before it reaches the breakwater. The v
elocity data are obtained by using both the Laser Doppler Velocimeter (LDV)
and the Electromagnetic Current Meter (EMCM). The raw data are analyzed us
ing a numerical-filtering scheme so that turbulent fluctuations are separat
ed from the phase-dependent wave motions. The vertical profiles of the time
-averaged (over a wave period) turbulent velocity components at several ver
tical cross-sections in front of the breakwater are then analyzed. The spat
ial variations of the time-averaged turbulence velocity suggest that turbul
ence is generated inside the protective armor layer and transported into th
e flow region in front of the breakwater. The wave pressures on the vertica
l face and on the bottom of the caisson are also reported. (C) 2001 Elsevie
r Science B.V. All rights reserved.