Hydraulic Jump Calculator

Find the downstream depth after a hydraulic jump.

Downstream depth 1.096
Upstream Froude number 2.915

Formula: y₂ = (y₁/2)·(√(1 + 8·Fr₁²) − 1)

Step-by-step with your numbers:
1. Values used:
2. Upstream depth = 0.3
3. Upstream velocity = 5
4. Gravity = 9.81 m/s²
5.
6. Downstream depth = 1.096
7. Upstream Froude number = 2.915
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A hydraulic jump is the abrupt rise in water level where fast flow slows down.

How the Math Works

A hydraulic jump occurs when fast-flowing water suddenly slows down, creating a turbulent burst that dissipates energy. The Hydraulic Jump Calculator uses the Froude number (Fr₁), which compares flow inertia to gravity, to predict the downstream depth (y₂). Starting with the upstream depth (y₁), the formula y₂ = (y₁/2)·(√(1 + 8·Fr₁²) - 1) applies the Pythagorean theorem concept to account for the momentum change, where the square root term captures how much the water depth amplifies after the jump. This relationship ensures energy conservation while modeling the violent mixing that characterizes hydraulic jumps in open channels.

Practical Applications

Engineers use this calculator during the design of spillways, weirs, and water treatment facilities to ensure safe water depth transitions. By inputting the known upstream depth and flow velocity, you first compute the Froude number, then determine the downstream depth before the jump dissipates. This prevents overtopping, protects downstream structures from scouring, and optimizes energy dissipation in irrigation channels. For instance, when retrofitting an existing dam, you'd calculate the new downstream profile to maintain safe conveyance while preventing erosion of the channel bed.

Day-to-Day Use

While you may not calculate hydraulic jumps daily, this principle protects communities through improved flood control and water management. The energy dissipation from hydraulic jumps reduces damage to bridges, roads, and buildings during flash floods. Municipal water utilities rely on these calculations to design efficient water distribution systems, ensuring pipes don't burst under pressure surges. Even in backyard stream design or aquarium maintenance, understanding how water depth changes with flow velocity helps create safer, more stable aquatic environments for fish and plants.

Worked example

0.3 m at 5 m/s (Fr ≈ 2.9) → downstream depth about 1.10 m.

FAQ

Why does it form?

Supercritical flow must transition to subcritical, dissipating energy in turbulence.