A hydraulic jump is a phenomenon in fluid dynamics that occurs when a high-velocity liquid flow transitions to a lower-velocity flow, resulting in a sudden change in water depth. This often happens in open channel flow systems, such as rivers or irrigation channels, where a fast-moving stream of fluid encounters an obstruction or change in elevation.
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A hydraulic jump connects shallow supercritical flow to deeper subcritical flow while conserving discharge and momentum and dissipating mechanical energy. Its Rankine-Hugoniot condition uses the channel's actual area and integrated hydrostatic pressure, which depend on cross-sectional geometry.