Boscastle flood of 2004

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Boscastle flood of 2004
Boscastle 0011.jpg
The old Cornish Stores shop
Date16 August 2004
LocationBoscastle; Crackington Haven
Deaths0
Property damageExtensive
Looking upstream from the bridge after the flood Boscastle 05.jpg
Looking upstream from the bridge after the flood

The Boscastle flood of 2004 (Cornish : An Lanwes Kastel Boterel 2004) occurred on Monday, 16 August 2004 in the two villages of Boscastle and Crackington Haven [1] in Cornwall, England, United Kingdom. The villages suffered extensive damage after flash floods caused by an exceptional amount of rain that fell over eight hours that afternoon. The flood in Boscastle was filmed and extensively reported but the floods in Crackington Haven and Rocky Valley were not mentioned beyond the local news. The floods were the worst in local memory. A study commissioned by the Environment Agency from hydraulics consulting firm HR Wallingford concluded that it was among the most extreme ever experienced in Britain. The peak flow was about 140 m³/s, between 5:00pm and 6:00pm BST. The annual chance of this (or a greater) flood in any one year is about 1 in 400. [2] The probability each year of the heaviest three-hour rainfall is about 1 in 1300 (although rainfall probability is not the same as flood probability). At midday on 16 August 2004, heavy thundery showers had developed across the South West due to a weak disturbance to the northeast of the United Kingdom. [3]

Cornish is a revived language that became extinct as a first language in the late 18th century. It is a member of the Brittonic Southwestern branch of the Celtic languages of the Indo-European language family, that was native to Cornwall in south-west England. A revival began in the early 20th century. Some have expressed the opinion that the language is an important part of Cornish identity, culture and heritage. Cornish is currently a recognised minority language under the European Charter for Regional or Minority Languages. It has a growing number of second language speakers. A few parents are inspired to create new first language speakers, by teaching their children the language from birth.

Boscastle village and fishing port on the north coast of Cornwall, England

Boscastle is a village and fishing port on the north coast of Cornwall, England, UK, in the civil parish of Forrabury and Minster. It is 14 miles (23 km) south of Bude and 5 miles (8 km) northeast of Tintagel. The harbour is a natural inlet protected by two stone harbour walls built in 1584 by Sir Richard Grenville and is the only significant harbour for 20 miles (32 km) along the coast. The village extends up the valleys of the River Valency and River Jordan. Heavy rainfall on 16 August 2004 caused extensive damage to the village.

Crackington Haven village in United Kingdom

Crackington Haven is a coastal village in Cornwall, England, United Kingdom. It is in the civil parish of St Gennys at grid reference SX140972 at the head of a cove on the Atlantic coast. The village is seven miles (11 km) south-southwest of Bude and four miles (7 km) north-northeast of Boscastle.

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The last time Boscastle had suffered notable flooding was in 1996 as a result of Hurricane Lili, but floods are recorded in 1847, 1957, on 3 June 1958 (one man drowned) and in 1963. On 16 August 1952 the small town of Lynmouth, 50 miles (80 km) north-east along the north coast in Devon near Exmoor, suffered extensive damage in a catastrophic flood, in which 34 people lost their lives. Coincidentally, this was 52 years to the day before Boscastle's 2004 flood.

Flood Overflow of water that submerges land that is not normally submerged

A flood is an overflow of water that submerges land that is usually dry. In the sense of "flowing water", the word may also be applied to the inflow of the tide. Floods are an area of study of the discipline hydrology and are of significant concern in agriculture, civil engineering and public health.

Hurricane Lili (1996) Category 3 Atlantic hurricane in 1996

Hurricane Lili was a relatively long-lived hurricane of the 1996 Atlantic hurricane season that affected countries from Central America to the United Kingdom. Lili formed on October 14 from a tropical wave, which emerged from the coast of west Africa on October 4. After the storm formed, further strengthening of Lili was gradual, first to tropical storm status on October 16 and then to hurricane status on October 17. The next day, Lili struck Cuba and moved across the central portion of the island, the first hurricane to hit the country since Hurricane Kate in 1985. After emerging into the Atlantic Ocean, the hurricane accelerated northeastward, briefly peaking as a category 3 hurricane on the Saffir-Simpson Hurricane Scale near the Bahamas. For almost an entire week, Hurricane Lili oscillated in intensity while fluctuating several times in forward speed. About two weeks passed before Lili transitioned into an extratropical storm north of the Azores on October 27, which subsequently moved across Ireland and Great Britain.

Lynmouth village in the United Kingdom

Lynmouth is a village in Devon, England, on the northern edge of Exmoor. The village straddles the confluence of the West Lyn and East Lyn rivers, in a gorge 700 feet (210 m) below Lynton, which was the only place to expand to once Lynmouth became as built-up as possible. The villages are connected by the Lynton and Lynmouth Cliff Railway, which works two cable-connected cars by gravity, using water tanks.

Causes of the flood

On the 16th, warm air picking up moisture – due to residual heat from the Atlantic Ocean – travelled towards the South West Cornish coast as prevailing winds. Upon contact with the topographically vertical coast, these winds experienced a strong up-drafting force thus causing internal moisture to reach the atmosphere, and consequently cool as a string of storm clouds. With convergence and coalescence, enhanced moisture levels resulted in heavy rainfall on the afternoon of 16 August 2004. 185 mm (7 inches) of rain fell over the high ground just inland of Boscastle. At the peak of the downpour, at about 15:40 GMT, 24.1mm of rain (almost one inch) was recorded as falling in just 15 minutes at Lesnewth, 2.5 miles (4 km) up the valley from Boscastle. In Boscastle, 89 mm (3.5 inches) of rain was recorded in 60 minutes. The rain was very localised: Otterham and Lesnewth, both a few miles inland from Boscastle, recorded 24 hour totals of 200 mm and 185 mm respectively on the day, [4] whereas four of the nearest 10 rain gauges showed less than 3 mm of rain in the same period. The cause of the very heavy localised rain is thought to be an extreme example of what has become known as the Brown Willy effect.

Greenwich Mean Time time zone

Greenwich Mean Time (GMT) is the mean solar time at the Royal Observatory in Greenwich, London, reckoned from midnight. At different times in the past, it has been calculated in different ways, including being calculated from noon; as a consequence, it cannot be used to specify a precise time unless a context is given.

Lesnewth civil parish and village in Cornwall, England

Lesnewth is a civil parish and village in Cornwall, England, United Kingdom. It is about six miles east of Tintagel Head and two miles east of Boscastle.

Otterham British village

Otterham is a village and a civil parish in north Cornwall, England, United Kingdom. The village is situated approximately ten miles (16 km) south of Bude and six miles (9.7 km) north of Camelford.

The torrential rain led to a 2 m (7 ft) rise in river levels in one hour. A 3 m (10 ft) wave, believed to have been triggered by water pooling behind debris caught under a bridge and then being suddenly released as the bridge collapsed, surged down the main road. Water speed was over 4 m/s (10 mph), more than enough to cause structural damage. It is estimated that 20,000,000 cubic metres (5.3×109 US gal) of water flowed through Boscastle that day alone. The steep valley sides, and the saturated surface ensured a high amount of surface run-off.

Debris is rubble, wreckage, ruins, litter and discarded garbage/refuse/trash, scattered remains of something destroyed, discarded, or as in geology, large rock fragments left by a melting glacier etc. Depending on context, debris can refer to a number of different things. The first apparent use of the French word in English is in a 1701 description of the army of Prince Rupert upon its retreat from a battle with the army of Oliver Cromwell, in England.

Changes in farming practice in the area also possibly contributed, sewage could have been a cause as well, with a reduction of trees and hedges higher up the valley causing water to flow through more quickly than would have been the case in the past. No one died in the flood.

Impact of the flood

75 cars, 5 caravans, 6 buildings and several boats were washed into the sea; approximately 100 homes and businesses were destroyed, and some had to be demolished; trees were uprooted and debris were scattered over a large area. In an operation lasting from mid-afternoon until 2:30 AM, a fleet of 7 Westland Sea King helicopters rescued about 150 people clinging to trees and the roofs of buildings and cars. No major injuries or loss of life were reported. The estimated cost of damage was £15 million. [5]

Westland Sea King series of military helicopters

The Westland WS-61 Sea King is a British licence-built version of the American Sikorsky S-61 helicopter of the same name, built by Westland Helicopters. The aircraft differs considerably from the American version, with Rolls-Royce Gnome engines, British-made anti-submarine warfare systems and a fully computerised flight control system. The Sea King was primarily designed for performing anti-submarine warfare (ASW) missions. A Sea King variant was adapted by Westland as troop transport known as the Commando.

Helicopter Type of rotor craft in which lift and thrust are supplied by rotors

A helicopter, or chopper, is a type of rotorcraft in which lift and thrust are supplied by rotors. This allows the helicopter to take off and land vertically, to hover, and to fly forward, backward, and laterally. These attributes allow helicopters to be used in congested or isolated areas where fixed-wing aircraft and many forms of VTOL aircraft cannot perform.

Work since the flood

The rebuilt Harbour Light in October 2006, now used as tea rooms. The shop is over the river. Boscastle Harbour Light 2006.JPG
The rebuilt Harbour Light in October 2006, now used as tea rooms. The shop is over the river.

Most work takes place in the winter season (October–May), during the off-season. The carpark is reduced to half the space (120 spaces) in winter, for works to take place, and then back to 240 spaces in summer.

2004

2005

2006

2007

2008

The lower bridge

The New Lower Bridge, taken on 20 December 2007. SP A0036.jpg
The New Lower Bridge, taken on 20 December 2007.

The main structure of the former lower bridge survived the flood, however the stone walls did not, and were washed away. On 1 May 2005, the official reopening of the village, wooden fences were used on the bridge to temporarily replace the stone walls. The bridge used to have a concrete plaque on it saying "This bridge is the private property of the lord of the manor, August 1887". This was lost during the flood, but then recovered from the harbour in good condition. This bridge has now been replaced with a new one.

During the flood of 2004, 14 cars became lodged beneath it, this had caused a huge backlog of flood water and debris, adding to the damage caused in the surrounding area.

The original proposal was for a stone bridge, this was rejected. The second proposal is for a modern concrete bridge, with steel railings. Public consultations were held and villagers were asked to select their preference from four designs; most did not choose the one which has been proposed. This plan was rejected.

The new bridge is a few metres further down the river than the old bridge. The bridge was installed on 18 December 2007, and was made by Cornish Concrete, a company based near Truro. The main arch is made from reinforced concrete, with metal railings.

The old stone bridge, which was over 100 years old, was demolished in early April 2008.

Mini flood – 21 June 2007

Boscastle flooded again, although not nearly as badly as the 2004 floods. After an afternoon of intense localised rainfall, and a week of steady rain everyday, a small flood happened on 21 June 2007. 30 mm fell on the area in one hour. Roads had become flooded in the area and in the village, most water came from the saturated fields around the village. Many drains had become blocked. Roads around the Tintagel, Camelford and Davidstow area were closed off to stop people visiting the village. River levels were alarmingly high, but the banks contained the water. However the many culverts of the River Jordan had overflowed onto the villages roads, adding to the amount of water on the roads. The new storm culvert joining the River Jordan to the River Valency was at full capacity, but did not flood. Services and organisations called in included:

The Environment Agency's flood defences installed after the 2004 flood worked and kept the water in the river channel. A few properties in the village were flooded by 3 ft (0.91 m) from water flowing down the streets, rather than from the river flooding, although the damage was not nearly as bad as the 2004 flood. The two main roads (B3266, B3263) were blocked with flood waste and debris, although this was cleared and the roads reopened the following morning. The Environment Agency looked at the culverts around the village and will change them all to modern drainage

See also

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References

  1. ↑ "Crackington Haven". cornwall365.co.uk. Cornwall 365. Archived from the original on 22 January 2015. Retrieved 22 January 2015.
  2. ↑ Ross, S. R. J. (2012). AQA GCSE Geography A. Cheltenham: Nelson Thornes. p. 65. ISBN   978-1-4085-1708-6.
  3. ↑ "17 August 2004 surface analysis". Institute of Meteorology. Free University of Berlin . Retrieved 4 April 2012.
  4. ↑ "Met Office (Boscastle Flood)" (PDF). metoffice.gov.uk. Met Office. Retrieved 14 November 2016.
  5. ↑ Ross, S. R. J. (2012). AQA GCSE Geography A. Cheltenham: Nelson Thornes. p. 64. ISBN   978-1-4085-1708-6.

Coordinates: 50°41′26″N4°41′42″W / 50.69044°N 4.69505°W / 50.69044; -4.69505

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