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Tidal Bore

D2. Hydrography, tides, waves, bathymetry and marine geology

Definition

Wave that travels upstream against the river current with a rising tide.

A tidal bore is a wave of translation, a moving step in water level, that travels upstream against the current as a rising tide enters a funnel-shaped estuary or river. It forms where a large tidal range, typically above 6 meters, meets a shallow, narrowing, gently sloped channel, so the leading edge of the flood steepens into a single surge or undular train. The Qiantang in China, the Severn in England, and the Amazon Pororoca are classic examples. The bore can run several knots and a meter or more high, a hazard to small craft and a fixed timing for upstream navigation.

Source: IHO Tidal and Water Level glossary; standard tidal-dynamics references