The swash zone largely influences nearshore hydrodynamics and morphodynamics through
dissipating or reflecting wave energy and controlling whether sediment will be stored on the …

The dominant hydrodynamic forcing and resulting sediment transport mechanisms in the
swash zone are reviewed, combined with a discussion of future measurement and …

The world's coastlines represent a myriad of dynamic and constantly changing
environments. Heavily settled and intensely used areas, they are of enormous importance to …

Hydrodynamic forcing with respect to sediment transport and morphologic change, paying
particular attention to relevant swash asymmetries, is reviewed. The hydrodynamics are …

A study of swash zone sediment transport was conducted at Gleneden Beach, Oregon
during February 25–28, 1994. The data collected included suspended sediment …

Field measurements of vertical pore‐pressure gradients within the bed are used to quantify
instantaneous (8 Hz) rates of swash infiltration‐exfiltration across the beach face. Cyclic …

Concurrent measurements of swash flow velocity and sediment transport were obtained
from a natural beach to develop a means for predicting sediment transport in the swash …

An understanding of the interaction between surface and groundwater flows in the swash
zone is necessary to understand beach profile evolution. Coastal researchers have …

The morphological behaviour of the coastline is important for a great number of reasons.
Erosion and accretion of the shoreline in response to dynamic wave conditions are functions …

Observations of morphological change and swash sediment loads, concurrent with
measurements of water level, waves and currents, were obtained during a spring-to-spring …