Flooding in Boscastle

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Flooding in Boscastle

In this report I will assess the causes, both natural and artificial, of the flooding in Boscastle on 17 Aug 2004 and the impact of the floods on the local environment, as well as the measures that could, and are being undertaken to deal with the effects of flooding.

Boscastle, is located in the south-west of England, on the coast, near Cornwall. The settlements position in relation to the mouth of a very narrow river valley leaves it vulnerable to flooding. Flood risk is heightened whenever storm waters are denied a wide flood plain to spread into: in a narrow valley, whatever land exists either side of the channel will become rapidly submerged, once the river has burst its banks. These were the heaviest rains in living memory for the people of the village - 185mm fell in just five hours. Given that the total annual rainfall for much of southern England is around 1,000mm, this is a lot of water to have arrived in such a very short time.

Fortunately, no one died on this occasion, despite the great hydraulic force of the water flowing through the town's streets. In contrast, property damage was high. At least thirty cars were washed straight into the harbour and many more were left upturned and badly damaged. A three-metre high wave of water was reported to have crashed through one street at 40 miles per hour. Fridge-freezers were picked up and swept out of kitchens as water entered properties. Six properties collapsed entirely, as a result of traction and abrasional damage.
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What were the physical factors?

* Three rivers - the Valency, Jordan and Paradise - converge on the village of Boscastle. The majority of the damage was attributable to the Valency.

* Heavy rain was caused by extreme frontal activity. In total, an input of 3 million tonnes of water was added to a tiny drainage basin, whose size is just 40 square kilometres.

* 185mm arrived in just five hours, the majority falling in the first two hours. Under such conditions, infiltration-excess overland flow is inevitable, with the rate of input of rainwater ...

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