Titlebook: Rotating Hydraulics; Nonlinear Topographi Larry J. Pratt,John A. Whitehead Textbook 2007 Springer-Verlag New York 2007 Coast.Jet stream.Met

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Time-Dependence and Shocks,, most likely due to the meandering of the edge of the jet-like overflow back and forth across the instrument. Worthington concluded “the currents associated with the overflow water were too strong on this occasion to be measured using existing mooring technology”.

fulmination

Potential Vorticity Hydraulics,tant to the general circulation. As discussed in Section 2.1, these waves depend on lateral gradients of potential vorticity to provide a restoring mechanism. For the gradients that typically exist in geophysical applications, the waves are generally much slower than long gravity waves and can have wave speeds in the range of the current velocity.

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Coastal Applications, changes in the position of the right sidewall. As the position of the right wall changes the current moves with it, undergoing no other change in cross-sectional form. Only variations in bottom elevation influence the flow in a meaningful way. This aspect has been demonstrated under the usual condi

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Two-Layer Flows in Rotating Channels, convincing when the interfacial region separating the upper and lower fluids is relatively thin. The exchange flow in the Strait of Gibraltar exhibits this behavior, at least at certain locations and times (Figure I.9). The vertical density and velocity profiles taken near the Camerinal Sill show a