Abstract
An experimental and analytical study of the hydraulics of two layer exchange flows in and beyond the limit of arresting barotropic net flow is presented. These arrested wedge flows are a limiting case of the inviscid, one dimensional, two-layer theory. The two-layer equations are modified to include the effects of friction and flow nonuniformity. A boundary layer model, along with the resultant Coriolis coefficients, was used with the modified hydraulic theory to compare with laboratory experiments.
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