__NOTOC__ A tidal bore (or just bore, or eagre) is a tidal phenomenon in which the leading edge of the incoming tide forms a wave (or waves) of water that travel up a river or narrow bay against the direction of the current. As such, it is a true tidal wave (not to be confused with a tsunami).
Bores occur in relatively few locations worldwide, usually in areas with a large tidal range (typically more than 20 feet between high and low water), and where incoming tides are funnelled into a shallow, narrowing river via a broad bay. The funnel-like shape not only increases the height of the tide, but it can also decrease the duration of the flood tide down to a point where the flood appears as a sudden increase in the water level.
Bores take on various forms, ranging from a single breaking wavefront—effectively a shock wave—to ‘undular bores’ comprising a smooth wavefront followed by a train of solitary waves (solitons). Larger bores can be particularly dangerous for shipping, but also present a challenge to surfers.
The word bore derives through Old English from the Old Norse word bara, meaning a wave or swell.
Rivers that have been known to exhibit bores include:
Tide | Fluid dynamics | Wave mechanics
Gezeitenwelle | Mascaret | Baro-fluxo | 海嘯 | Vuorovesiporras
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"Tidal bore".
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