Titlebook: Environmental Hydraulics: Stratified Flows; Stratified Flows Flemming Bo Pedersen Textbook 1986 Springer-Verlag Berlin Heidelberg 1986 Ocea

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Winddriven Stratified FlowThe wind is often one of the most important external forcing functions with respect to the currents and mixing processes in the ocean, in estuaries and lakes.

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Horizontal Buoyant FlowA horizontal buoyant flow is the flow created by a horizontally directed source of mass, momentum, and buoyancy into an ambient fluid. The horizontal direction is preserved by the existence of two stable density jumps embedding the flow, as for instance a free surface and an interface.

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Buddhist Testimony and Christian Testimony,l/water) or where the actual mixing has no appreciable influence on the dynamics of the flow, as for instance the stationary salt water wedge (treated below). Therefore, we have an ample motivation to discuss the motion of non-miscible stratified fluids, in as much as it leaves us the possibility to

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