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

This paper reviews research on beach groundwater dynamics and identifies research
questions which will need to be answered before swash zone sediment transport and beach …

Groundwater flow and chemical transport in subterranean estuaries are poorly understood
despite their potentially important implications for chemical fluxes from aquifers to coastal …

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 …

A parametric analysis is conducted to examine the influence of tides, inland hydraulic
conditions, and aquifer properties on the rate of tide‐induced seawater recirculation through …

A model that simulates surface moisture content on sandy beaches for aeolian transport
applications is developed and integrated into the aeolian transport model AeoLiS. The …

To incorporate groundwater infiltration/exfiltration in the description of swash zone sediment
transport, it is required that the details of groundwater dynamics within the beach face be …

Aquifers on small islands are at risk of salinization due to low elevations and limited
adaptive capacity, and present risks will be exacerbated by climate change. Most studies …

Groundwater dynamics in the coastal unconfined aquifer is one of the most important
physical factors in the coastal zone since it greatly influences the nearshore hydrodynamics …

The action of tides and waves results in a net super-elevation of the mean groundwater
surface above the elevation of mean sea level at the ocean boundary to unconfined coastal …