Tides are the alternating rise and fall of the surface of the seas and oceans. They are due
mainly to the gravitational attraction (pull) of the moon and sun on the rotating earth. Two
high and two low tides occur daily around Britain and, with average weather conditions, their
movements can be predicted with considerable accuracy.
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Related links
[UK National Tidal & Sea Level Facility]
[NTSLF online tidal predictions]
[Questions and
answers about tides]
The Doodson-Légé Tide Predicting Machine
Tides have been predicted at the Proudman Oceanographic Laboratory, Bidston Observatory, since
1924, firstly by hand and then by the early tide predicting machines.
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Tidal river bores
In most tidal rivers the change from ebb to flood is a gradual process. The ebb current
downstream slows, there is a period of slack water and then very slowly the flood tide
starts flowing upstream. In a few rivers however, the behaviour is remarkably different. The
onset of the flood tide is marked by a distinct and sometimes very vigorous wave - a bore.
The largest example of a river bore in the UK is the Severn Bore. Although large in UK terms it
is dwarfed by the largest river bore in the world, found in China - The Qiantang Bore.
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Related links
[Local bores to Merseyside]