Niagara River Flow: 2,400 m³/s Average, 22 km/h at Falls, Seasonal Extremes
The Niagara River — 58 km (36 mi) connecting Lake Erie to Lake Ontario — carries the entire Great Lakes outflow (except Chicago diversion). Its hydraulics are among Earth's most studied.
Flow Metrics
| Metric | Value | Context |
| Average flow | 2,400 m³/s (85,000 ft³/s) | ~1/5 of Mississippi at mouth |
| Current at Falls | ~22 km/h (14 mph) | Velocity over crest; varies by section |
| Peak flow (spring) | 6,000 m³/s (212,000 ft³/s) | Snowmelt + rain; regulated by control works |
| Minimum flow (winter) | 1,400 m³/s (50,000 ft³/s) | Treaty-mandated (1950 Niagara Treaty) |
| Horseshoe Falls share | 90% | Canadian side; American Falls 10% |
Regulation and Power
- International Niagara Control Works (1954) — adjustable gates above falls regulate flow per 1950 Treaty (min. 2,832 m³/s day, 1,416 m³/s night tourist season; 1,416 m³/s off-season).
- Power diversion: Sir Adam Beck (ON) and Robert Moses (NY) plants divert ~50–75% of flow via tunnels — 4.4 GW combined capacity.
- Welland Canal bypasses river for shipping (8 locks, 99 m lift).
Hydraulic Sections
- Upper Niagara (Lake Erie to Falls): Shallow, swift, island-braided — 35 km, 15 km/h avg.
- Falls: Horseshoe (57 m drop, 790 m crest), American (21–34 m, 320 m), Bridal Veil (24 m, 15 m).
- Lower Niagara (Gorge): Deep (60 m), narrow, turbulent — 11 km to Lake Ontario. Class V-VI rapids, whirlpool.
Climate Change Signal
Great Lakes levels fluctuating (record highs 2019–20, lows 2013). Earlier snowmelt, more intense rain events alter hydrograph. Treaty review (2024+) may adjust flow rules for ecosystem resilience.