Ground water of both terrestrial and marine origin flows into coastal surface waters as submarine groundwater discharge, and constitutes an important source of nutrients, contaminants and trace elements to the coastal ocean^{1, 2, 3, 4, 5}. Large saline discharges have been observed by direct measurements^{3, 6, 7, 8, 9, 10} and inferred from geochemical tracers^{11, 12, 13}, but sufficient seawater inflow has not been observed to balance this outflow. Geochemical tracers also suggest a time lag between changes in submarine groundwater discharge rates^{12, 14} and the seasonal oscillations of inland recharge that drive groundwater flow towards the coast. Here we use measurements of hydraulic gradients and offshore fluxes taken at Waquoit Bay, Massachusetts, together with a modelling study of a generalized coastal groundwater system to show that a shift in the freshwater–saltwater interface—controlled by seasonal changes in water table elevation—can explain large saline discharges that lag inland recharge cycles. We find that sea water is drawn into aquifers as the freshwater–saltwater interface moves landward during winter, and discharges back into coastal waters as the interface moves seaward in summer. Our results demonstrate the connection between the seasonal hydrologic cycle inland and the saline groundwater system in coastal aquifers, and suggest a potentially important seasonality in the chemical loading of coastal waters.

1. Department of Civil and Environmental Engineering, MIT, Cambridge, Massachusetts 02139, USA
2. Marine Policy Center, Woods Hole Oceanographic Institution, Woods Hole, Massachusetts 02543, USA

Correspondence to: Charles F. Harvey¹ Correspondence and requests for materials should be addressed to C.F.H. (Email: charvey@mit.edu).

Received 25 March 2005; Accepted 9 August 2005

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