Tidal River Bores

In most tidal rivers the change from The turbulence following the bore The bore occurs probably 250 times ebb to flood is a gradual process. stirs up the sediment so the river can per year ranging from a small ripple The ebb current downstream slows, appear to change colour. Often to the highest waves. However, it is there is a period of slack water and debris torn from the banks by the generally at its best when a very high then very slowly the flood tide starts bore is caught in the after‐rush spring tide is predicted, something flowing upstream. In a few rivers sometimes including whole trees. At in excess of 14 metres at however, the behaviour is Maisemore the sound of the river Avonmouth. Hence there are remarkably different. The onset of passing over the weir and the sound probably just a few occasions in the the flood tide is marked by a distinct of the bore rushing upstream are year at the spring tides that occur and sometimes very vigorous wave cancelled instantly as the bore closest to the equinoxes when the called a bore. simultaneously drowns the weir and bores are at their most spectacular. is itself halted. There are many other Approximately 100 rivers around the interesting effects associated with However a good bore cannot be world are known to produce bores, the passage of the bore. guaranteed as it can be affected by of which perhaps 20 or so are in the other factors. For example if there is United Kingdom. This is a The Severn Bore can be seen from a lot of extra water in the river due to consequence of the large tidal its first small beginnings near heavy rainfall the bore is diminished. ranges that occur in several all the way up to the This together with other factors such locations around the British Isles. Maisemore Weir above . It as wind can also alter the timing of is at its most developed between the bore by perhaps a quarter of an The Severn Bore and Gloucester hour or so. The approximate times to In the UK the most famous and although it is certainly worth seeing expect the bore at various locations spectacular example of a river bore in its estuary form above Newnham. is the Severn Bore, and as such it attracts thousands of tourists.

It can be seen as a wave or series of waves, sometimes 2 metres in height, that sweep up the , breaking in the shallows at the side of the river sometimes splashing onlookers! Being the onset of the flood tide it is accompanied by a rapid rise in water level which continues for about one and a half hours after the bore has passed. With the passage of the bore the whole character of the river changes instantly from a calm, tranquil slowly ebbing stream to a turbulent fast flowing river with a strong upstream River Severn bore – the most impressive of the 20 river bores current. you are likely to see in the UK.

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relative to High Water Avonmouth leaflets provided by the Severn Trent high, 3km wide and travel at speeds (HWA) are: Water Authority. in excess of 15 mph. At certain locations reflected waves can reach Newnham 15 min before HWA Tidal predictions for Avonmouth and 10m and the roar can be heard over Epney 25 min after HWA other ports can be found on the an hour before its arrival. Minsterworth 45 min after HWA National Tidal and Sea Level Facility Stonebench 1 hr after HWA (NTSLF) website: When a large bore is forecast many 1 hr 20 min after HWA people line the banks to watch its Maisemore 1 hr 25 min after HWA http://www.ntslf.org/ progress. Great care is required. The times shown on the site are UT, Several tragic accidents have The Severn Bore is more fully occurred when reflected waves described in the book "The Severn add 1 hour for British Summer Time. suddenly increase the bore height Bore" by Fred Rowbotham (3rd The Qiantang Tidal River Bore and break over the banks washing edition 1983, David & Charles, away unwary people. Newton Abbott) and also in various The Qiantang bore is the largest tidal river bore in the world. It can be 4m

The Qiantang Tidal River Bore

This document is provided for information purposes only. It cannot be republished without prior permission. The National Oceanography Centre can accept no liability in relation to the use of this document. For further information please contact [email protected].