The number of conjugate states for the flow of a fluid system of two layers is investigated by means of the momentum principle. The uniqueness of the conjugate state is proved for the cases in which the modified Froude number for either layer is predominantly large. Specific experimental results for three special cases demonstrate the uniqueness of the state downstream from the hydraulic jump, and show that, for a first approximation, the simple analysis provides a means for determining the downstream depths, with smaller errors for lower jumps.
CITATION STYLE
Yih, C.-S., & Guha, C. R. (1955). Hydraulic Jump in a Fluid System of Two Layers. Tellus A: Dynamic Meteorology and Oceanography, 7(3), 358–366. https://doi.org/10.3402/tellusa.v7i3.8874
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