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Intuitively, the transport of an oscillating flow in a short channel should be constrained to be approximately the same at all cross sections; that is, the transport is nondivergent. This intuitive constraint is quantified by developing a generalized definition of ““shortness”” given by the...
The phase of the M 2 surface elevation tide changes by 100°° along a 40-km length of Cook Strait, New Zealand. Acoustic Doppler Current Profiler measurements are presented that show a change of only 12°° in the phase of depth-averaged semidiurnal tidal currents along this same length. This phase...
A four-level numerical model, which is driven by wind stress and surface heat flux, is used to study responses of horizontal temperature fields in the subtropical––subpolar system to a sudden change in the magnitude of the wind stress curl. Weakly nonlinear responses to O (1) change in the wind...
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