Extensive research efforts in the last decade have improved knowledge of swash-zone
processes. This paper reviews and synthesizes from 2004 onward the research advances of …

The existence of sandy beaches relies on the onshore transport of sand by waves during
post-storm conditions. Most operational sediment transport models employ wave-averaged …

The main goal of this paper is to provide insights into swash flow dynamics, generated by a
non-breaking solitary wave on a steep slope. Both laboratory experiments and numerical …

Two parallel experiments involving the evolution and runup induced by plunging regular
waves near the shoreline of a slo** bed are considered:(1) a rigid‐bed experiment …

A 3D large eddy simulation coupled with a free surface tracking scheme was used to
simulate cross‐shore hydrodynamics as observed in a large wave flume experiment. The …

A detailed experimental investigation of the hydrodynamics of large-scale, bore-driven
swash on impermeable, rough beach slopes is described. The experiments were carried out …

The swash of solitary waves on a plane beach is studied using large-scale experiments. Ten
wave cases are examined which range from non-breaking waves to plunging breakers. The …

A large‐scale wave flume experiment has been carried out involving a T= 4 s regular wave
with H= 0.85 m wave height plunging over a fixed barred beach profile. Velocity profiles …

Swash–swash interaction is a common natural phenomenon in the nearshore region,
characterized by complex fluid motion. The characteristics of swash–swash interaction are …

Observations of the Surf-Zone Turbulent Dissipation Rate in: Journal of Physical Oceanography
Volume 42 Issue 3 (2012) Jump to Content Jump to Main Navigation Logo Logo Logo Logo …