The groundwater table fluctuation (GTF) zone is an important medium for the hydrologic
cycle between unsaturated soil and saturated aquifers, which accelerates the migration …

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

Tidal water table fluctuations in a coastal aquifer are driven by tides on a moving boundary
that varies with the beach slope. One-dimensional models based on the Boussinesq …

Submarine groundwater discharge (SGWD) and associated nutrient fluxes at Hasaki Beach
along the Kashima coast in Japan were investigated through field measurements and …

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 …

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 …

Specific yield is a key parameter for estimating water table depth in land surface models,
which can strongly modulate the interaction between soil moisture and groundwater and …

Wave-induced beach groundwater flow has been linked to sediment transport in the near-
shore zone and chemical transfer from the aquifer to the ocean. The flow dynamics …

On sand and gravel beaches, the increase of the gradient of the beachface with increasing
sediment size has been attributed to swash infiltration. The present study uses a process …

The responses of the fresh-saline water interface (FSI) and the groundwater level (GWL) to
the Mediterranean Sea tide were monitored in the coastal aquifer of Israel, modeled …