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A simple method of computing the second-order, three-dimensional, tidally-induced residual current is presented. The depth-averaged residual current and the mean-surface gradient from the depth-averag...
A simple method for computing first-order three-dimensional tidal currents is presented. The method involves solving separately the equations for the depth-averaged velocity and the vertical velocity ...
Theory is developed to describe barotropic tidal currents on “smooth” continental shelves, that is, continental shelves with longshore scales much greater than the shelf width. Two models are consider...
A description is given of the K1 tide over the northeast continental shelf off North America from Nova Scotia to Cape Hatteras. Analyzed pressure data obtained from W. Brown and J. Irish (University o...
The properties of the semidiurnal internal tide, in the region of the shelf-break, at a location on the Australian North West Shelf are discussed. Information is derived from an analysis of thermistor...
After an initial 40-hour “diffusion” period, the time decay of tsunami variance was found to be uniformly exponents for 28 events among eight Pacific tide stations. Thew results essentially confirm Mu...
The interaction of the tides with the sill of Knight Inlet, a fjord located on the coast of British Columbia, is investigated. The seasonal variation in the stratification of the inlet causes a large ...
The solution of the fully nonlinear three-dimensional hydrodynamic equations in polar coordinates, for tides, is developed using a finite-difference grid in the horizontal and the Galerkin method in t...
Extending previous work in the North Pacific, tsunami response was examined in the Atlantic and Indian oceans, and in three smaller seas, with the objective of exploring scale effects. Energy diffusi...
Evidence of an internal tide on the eastern side of the Rockall Trough is derived from recording current meters and thermistor chains sited at the edge and near the center of the Malin Shelf. Although...
The time variations of the salt wedge intrusion in the Fraser estuary, British Columbia, were monitored during a variety of tidal and run-off conditions using instruments and sampling methods that pro...
A stratified fluid response to barotropic oscillatory now over a large-amplitude obstacle is examined on the basis of the results of laboratory and numerical experiments. It is demonstrated that, when...
Tidal computations are reported for the Gulf of Maine with emphasis on its seaward banks. Georges Bank, Browns Bank, Nantucket Shoals, and the nearshore region off Cape Sable. The model is 3D and nonl...
Using data from the Coastal Ocean Dynamics Experiment (CODE) and the Island Coastal Current Experiment, the internal tide off the west coast of the Vancouver Island was studied. Although the semidiurn...
This paper discusses the energetics of the internal waves generated by the tide on the northern edge of Georges Bank in the outer Gulf of Maine–-a region of strong tidal flow, a density/temperature fr...

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