Tide-induced residual current was studied through solution of the two-dimensional nonlinear shallow-water equation. A simple numerical method was developed and applied to Minas Channel and Minas Basin at the head of the Bay of Fundy where strong residual currents of up to 0.76 m/sec have been measured....
Tee, K. T.. 1976. "Tide-induced residual current, a 2-D nonlinear numerical tidal model." Journal of Marine Research 34, (4). https://elischolar.library.yale.edu/journal_of_marine_research/1379