Low‐elevation coastal areas are increasingly vulnerable to seawater flooding as sea levels
rise and the frequency and intensity of large storms increase with climate change. Seawater …

Sea-level rise (SLR) influences groundwater hydraulics and in particular seawater intrusion
(SWI) in many coastal aquifers. The quantification of the combined and relative impacts of …

Sustainable coastal resource management requires sound understanding of interactions
between coastal unconfined aquifers and the ocean as these interactions influence the flux …

Seawater intrusion (SI) is a global issue, exacerbated by increasing demands for freshwater
in coastal zones and predisposed to the influences of rising sea levels and changing …

Massive withdrawal of groundwater resources due to population growth and rapid
industrialization has led to seawater intrusion into the coastal aquifers across the globe. The …

Projected sea-level rise will raise coastal water tables, resulting in groundwater hazards that
threaten shallow infrastructure and coastal ecosystem resilience. Here we model a range of …

Water resources are of enormous societal and ecological importance. In coastal areas, they
are under ever greater pressure due to population growth, more affluent lifestyles, food …

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

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

The biogeochemical reactivity of sandy beach aquifers is closely linked to physical flow and
solute transport processes. Thus, a clearer understanding of the hydrodynamics in the …