Abstract
A hydraulic jump is a rapidly varied phenomenon in free surface flow. It corresponds to a discontinuous transition from supercritical to sub-critical flows in an open channel where no appurtenances are provided. In general, the fluid considered is water, and the discharge per unit width is larger than 0.1 m3 s-1 such that scale effects are practically eliminated.
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References, Part 1. Chapters 1 to 5
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Hager, W.H. (1992). Introduction. In: Energy Dissipators and Hydraulic Jump. Water Science and Technology Library, vol 8. Springer, Dordrecht. https://doi.org/10.1007/978-94-015-8048-9_1
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