Salt marshes are highly productive intertidal wetlands providing important ecological
services for maintaining coastal biodiversity, buffering against oceanic storms, and acting as …

Groundwater–surface water exchange in salt marsh ecosystems mediates nearshore salt,
nutrient, and carbon budgets with implications for biological productivity and global climate …

Aquifer‐ocean temperature contrasts are common worldwide. Their effects on flow and
salinity distributions in unconfined coastal aquifers are, however, poorly understood. Based …

Salt marshes, distributed globally at the land-ocean interface, are a highly productive eco-
system with valuable ecological functions. While salt marshes are affected by various eco …

Salt is a key solute in salt marshes and under the influence of evapotranspiration can
accumulate to a high concentration level in the marsh soil and precipitate in the solid form to …

Most existing numerical research on tide‐induced groundwater dynamics assumes a
constant surface water salinity on the seaward boundary (constant salinity case). Few …

The tide-induced upper saline plume (USP) in coastal aquifers plays a critical role in
affecting the fate of land-sourced solutes. Early studies focused primarily on a quasi-steady …

Recent studies have shown that, in beach aquifers, tide-induced upper saline plume (USP)
may become unstable in the form of moving salt fingers under certain hydrogeological …

In coastal wetlands the hydrological dynamics and in particular the groundwater flows play a
critical role in the establishment of wetlands and in the transport of salts and nutrients. The …

Tidal wetland ecosystems are sensitive to porewater salinity dynamics. However, it is
unclear how salts move and distribute in these wetlands, particularly how the salts …