Flood | |
---|---|
Directed by | Tony Mitchell |
Written by | Justin Bodle Matthew Cope Nick Morley |
Based on | Flood by Richard Doyle |
Produced by | Justin Bodle |
Starring | |
Cinematography | Pierre Jodoin |
Edited by | Simon Webb |
Music by | Debbie Wiseman |
Production companies | |
Distributed by | Lionsgate |
Release date |
|
Running time | 110 minutes |
Countries | United Kingdom South Africa Canada |
Language | English |
Budget | $24 million [1] |
Box office | $8.272 million [2] |
Flood is a 2007 British-Canadian disaster film, directed by Tony Mitchell. It features Robert Carlyle, Jessalyn Gilsig, David Suchet and Tom Courtenay and is mainly set in London, England. It is based on the novel of the same name by Richard Doyle. [3]
A storm surge travels between the United Kingdom and mainland Europe, raising sea levels at the same time as the spring tide. Several parts of Scotland are devastated as a result, including Wick.
The Met Office's head forecaster, Keith Hopkins, mistakenly believes the storm will head towards the Netherlands. However, Leonard Morrison, a marine physics professor who has based his career on believing that the Thames barrier was built in the wrong place, disproves Hopkins' theory with his independent but sophisticated computer model - which predicts that the storm and spring tide would merge to form a 46 metre-high surge. After a series of mis-informed meetings with Deputy Prime Minister Campbell (who becomes outraged at the inaccurate forecasts) Hopkins feels guilt ridden as valuable time has been wasted. During a last-minute meeting at COBRA in Whitehall, the authorities realise that Central London would be inundated in three hours. Campbell declares a state of emergency, which on the short notice causes severe panic and congestion in the city.
As the COBRA authorities and military forces struggle to evacuate over one million people from the city, Police Commissioner Patricia Nash is designated the emergency coordinator by Campbell and works with the rest of the team, including Major General Ashcroft, transport chief Johnson, and a guilt-stricken Hopkins.
Leonard travels to the barrier where he meets his estranged son Rob, an engineer, and Rob's ex-wife Sam, the barrier manager. Sam oversees raising the barrier, but the tsunami arrives and overwhelms it. The flood sweeps into the city, destroying everything in its path. Rob and Sam jump into the Thames to escape the swamped barrier, whilst Leonard is saved by a military helicopter and taken to Whitehall to advise COBRA.
Rob and Sam end up with other survivors in the London Underground. They meet two maintenance workers, Bill and Zack, but when the surge floods the station, Bill drowns whilst sealing a door to save everyone else. The group escape to the surface via a vertical shaft and find themselves in the flooded Trafalgar Square, where Rob and Sam contact Leonard. They return with him to the barrier, where Leonard believes the water flow can be reversed back out of London, as the tide has turned and the water level is starting to recede.
General Ashcroft disagrees and lobbies the Prime Minister to authorise an air strike to destroy the barrier, hoping to create a surge to push the water back out of London. Hopkins, feeling guilty about the thousands of casualties, disappears and dies by suicide. Nash clashes with Ashcroft, wanting to give the Morrisons a chance to remedy the situation.
Rob, Sam and Leonard discover the controls to initiate the reverse flow are now underwater. They realise someone can activate them, but they will likely die doing so. As Rob and Sam try to decide which of them should go, Leonard quietly makes the choice for them by going himself. He is successful in activating the controls but drowns whilst doing so. As the air strike is aborted and the floods recede, Rob is consoled by Sam as Morrison's body is recovered, who is among the over 200,000 casualties in the disaster. Campbell holds a radio broadcast to the survivors in the city, assuring them that London will survive and recover.
The film was shot on location in London for two weeks and in South Africa for 11 weeks. [3] It is notable for the use of intricate production design and special effects in depicting famous London landmarks such as the London Underground, Houses of Parliament and The O2 being partially submerged under water.
Twenty-six studio sets were constructed with built-in water effects to shoot the actors in a wide range of flood sequences. Miniature sets in water tanks were used to shoot larger flooded buildings such as the Thames Barrier, London Underground and car parks. Computer generated visual effects were used to create shots of flooded London by combining shots of London with digitally created water. Locations in Cape Town were used for Whitehall, the Scottish coastline, London Underground and the Thames Barrier.
A 110-minute version of the film was given a limited theatrical release in the UK, premiering on 24 August 2007 [3] and was released on DVD in the UK in October 2007. [4] An extended two-part TV version was screened on ITV1 on May 4 and 5 2008 and released on DVD in the United States in September 2008 and in the United Kingdom in October 2008. [5] It also played as a mini-series in Lithuania, Spain, Italy, the United States (via Ion Television), New Zealand, South Africa, Canada, Finland and Denmark. The extended version was repeated on ITV3 on 10 and 11 January 2009.
Anna Smith at the BBC gave the film 3 stars out of five with the reviewer calling it "an American disaster movie on rather sodden British soil." [6]
The River Thames, known alternatively in parts as the River Isis, is a river that flows through southern England including London. At 346 kilometres (215 mi), it is the longest river entirely in England and the second-longest in the United Kingdom, after the River Severn.
The Thames Barrier is a retractable barrier system built to protect the floodplain of most of Greater London from exceptionally high tides and storm surges moving up from the North Sea. It has been operational since 1982. When needed, it is closed (raised) during high tide; at low tide, it can be opened to restore the river's flow towards the sea. Built about 2 miles east of the Isle of Dogs, its northern bank is in Silvertown in the London Borough of Newham and its southern bank is in the New Charlton area of the Royal Borough of Greenwich.
Storm tides of the North Sea are coastal floods associated with extratropical cyclones crossing over the North Sea, the severity of which is affected by the shallowness of the sea and the orientation of the shoreline relative to the storm's path, as well as the timing of tides. The water level can rise to more than 5 metres (17 ft) above the normal tide as a result of storm tides.
The Maeslantkering is a storm surge barrier on the Nieuwe Waterweg, in South Holland, Netherlands. It was constructed from 1991 to 1997. As part of the Delta Works the barrier responds to water level predictions calculated by a centralized computer system called BOS. It automatically closes when Rotterdam is threatened by floods.
A storm surge, storm flood, tidal surge, or storm tide is a coastal flood or tsunami-like phenomenon of rising water commonly associated with low-pressure weather systems, such as cyclones. It is measured as the rise in water level above the normal tidal level, and does not include waves.
The Thames Estuary is where the River Thames meets the waters of the North Sea, in the south-east of Great Britain.
The 1953 North Sea flood was a major flood caused by a heavy storm surge that struck the Netherlands, north-west Belgium, England and Scotland. Most sea defences facing the surge were overwhelmed, resulting in extensive flooding.
A flood barrier, surge barrier or storm surge barrier is a specific type of floodgate, designed to prevent a storm surge or spring tide from flooding the protected area behind the barrier. A surge barrier is almost always part of a larger flood protection system consisting of floodwalls, levees, and other constructions and natural geographical features. Flood barrier may also refer to barriers placed around or at individual buildings to keep floodwaters from entering the buildings.
The Tideway is the part of the River Thames in England which is subject to tides. This stretch of water is downstream from Teddington Lock. The Tideway comprises the upper Thames Estuary including the Pool of London.
The 1928 Thames flood was a disastrous flood of the River Thames that affected much of riverside London on 7 January 1928, as well as places further downriver. Fourteen people died and thousands were made homeless when floodwaters poured over the top of the Thames Embankment and part of the Chelsea Embankment collapsed. It was the last major flood to affect central London, and, along with the disastrous North Sea flood of 1953, helped lead to the implementation of new flood control measures that culminated in the construction of the Thames Barrier in the 1970s.
Flood is a 2002 disaster thriller novel by Richard Doyle. Set in present-day London, the novel depicts a disastrous flood and fire of London, caused by a storm, and the consequential accident at an oil refinery, and failure of the Thames Barrier. The plot is similar to his 1976 novel Deluge, updated to include the construction of the Thames Flood Barrier.
Flood control methods are used to reduce or prevent the detrimental effects of flood waters. Flooding can be caused by a mix of both natural processes, such as extreme weather upstream, and human changes to waterbodies and runoff. Flood control methods can be either of the structural type and of the non-structural type. Structural methods hold back floodwaters physically, while non-structural methods do not. Building hard infrastructure to prevent flooding, such as flood walls, is effective at managing flooding. However, best practice within landscape engineering is more and more to rely on soft infrastructure and natural systems, such as marshes and flood plains, for handling the increase in water.
Juliette Mole is an English actress and artist, now based in London. She is married to the actor Lloyd Owen.
Coastal flooding occurs when dry and low-lying land is submerged (flooded) by seawater. The range of a coastal flooding is a result of the elevation of floodwater that penetrates the inland which is controlled by the topography of the coastal land exposed to flooding. The seawater can flood the land via several different paths: direct flooding, overtopping or breaching of a barrier. Coastal flooding is largely a natural event. Due to the effects of climate change and an increase in the population living in coastal areas, the damage caused by coastal flood events has intensified and more people are being affected.
Cyclone Xaver, also known as the North Sea flood or tidal surge of 2013, was a winter storm that affected northern Europe. Force 12 winds and heavy snowfall were predicted along the storm's path, and there were warnings of a significant risk of storm surge leading to coastal flooding along the coasts of the North and Irish Seas.
The 2013–2014 United Kingdom winter floods saw areas of the United Kingdom inundated following severe storms. The south of England saw heavy rainfalls associated with these storms which caused widespread flooding, power cuts and major disruptions to transport. Economically, the worst affected areas were Somerset, Devon, Dorset and Cornwall in the south west and the Thames Valley in the south east.
The New York Harbor Storm-Surge Barrier is a proposed flood barrier system to protect the New York-New Jersey Harbor Estuary from storm surges. The proposed system would consist of one barrier located across the mouth of Lower New York Bay, possibly between Sandy Hook (N.J.) and Rockaway (N.Y.), and a second on the upper East River to provide a ring of protection to most of the bi-state region. Through extensive use of floodgates, both barriers would have largely open cross-sections during normal conditions to minimize environmental impacts on the estuary and port operations.
The River Hull tidal surge barrier is a flood control gate located on the River Hull in the city of Kingston upon Hull, in the East Riding of Yorkshire, England. The barrier impounds the river in times of tidal surges, preventing water moving upstream of the river from the Humber Estuary, and flooding the areas of the city which are near to the river, or susceptible to flooding. It is held horizontal when not in use, and turns 90 degrees before being lowered to the riverbed in the event of a tidal surge. It is the second largest flood barrier in the United Kingdom after the Thames Barrier in London.
Lagoon Hull is a proposed £1.5 billion development on the Humber Estuary foreshore between Hessle and Kingston upon Hull, in the East Riding of Yorkshire, England. The proposed lagoon would be formed from a stone causeway and will provide an outer lock gate in the Humber Estuary which would effectively dam the River Hull, making it a non-tidal waterway. The 11-kilometre (6.8 mi) long causeway would also provide a dual carriageway from the A63 at Hessle which would run to Hull Docks, taking traffic away from the city centre. The scheme is being vaunted as one that will prevent future flooding in Hull when sea levels rise, and contribute to less flooding in the wider Humber Estuary.
The Embanking of the tidal Thames is the historical process by which the lower River Thames, at one time a broad, shallow waterway winding through malarious marshlands, has been transformed by human intervention into a deep, narrow tidal canal flowing between solid artificial walls, and restrained by these at high tide. The Victorian civil engineering works in central London, usually called "the Embankment", are just a small part of the process.