Submarine groundwater discharge (SGD) is an ubiquitous coastal process that is driven by a composite of climatologic, hydrogeologic, and oceanographic processes. For example, terrestrial hydraulic gradients that reflect both short and long term climatic conditions almost always transport both surface and ground water toward the coast. In coastal waters, physical oceanographic processes such as wave set-up, tidal pumping, and density-driven circulation impact these hydraulic gradients and thus affect rates of submarine groundwater discharge.
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Mercury dynamics in a coastal aquifer: Maunalua Bay, Oʻahu, Hawaiʻi - Estuarine, Coastal and Shelf Science
A geochemical and geophysical assessment of coastal groundwater discharge at select sites in Maui and Oʻahu, Hawaiʻi - Groundwater in the Coastal Zones of Asia-Pacific
Integration of bed characteristics, geochemical tracers, current measurements, and numerical modeling for assessing the provenance of beach sand in the San Francisco Bay coastal system - Marine Geology
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