This 2D simulation perfectly captures a hydraulic jump as supercritical flow rushes down the slope and transitions abruptly to subcritical flow. The sudden rise in water depth and the turbulent standing waves mark the energy dissipation zone — a classic feature of open channel hydraulics.
The multiple visible wave crests are a result of the model resolving secondary undular jumps, a phenomenon that occurs when the Froude number is only moderately above the critical value, producing oscillations downstream of the main jump.
All stages — terrain preparation, simulation, and 3D rendering — were completed within the STE platform.
You can read more about STE and Install the software for free :
https://ste.hwstr.ir/
