Geography Unit 1
It's a brief view about the case studies of impact of flooding
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- Created by: Leroy Nyamayaro
- Created on: 14-05-12 15:57
Pakistan Floods, 2010- Causes
Causes:
- heavy & prolonged rains in the monsoon season fill rivers to burstin point
- at its peak- discharge on river indus was 40 times above normal
- floods covered one fifth of the country
- the lowlying central and southern Pakistan mean't it comprised of vast alluvial plains and occupied by millions of poor farmers
- himalaya mountain range to the north increased precipitation and meltwater from snow
- deforestation ?
- limited protection from flood management schemes.
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Impacts of Pakistan Floods ;)
Impacts:)
- final death toll of 2000 deaths
- 1.2 million homes destroyed and villages swept away
- 10 million pple displaced
- 8 million needed emergency relief aid
- shortages of food & clean drinking water and inadequate sanitation
- by Sept, outbreak of water borne dzzs e.g cholera
- economic costs between $3.5 & $5 billion
- Pakistan's GDP was to fall by 2 %
- damaged physical infrastructure e.g roads
- 3.2 million ha of crops lost or badly damaged
- commercial crops worst affected e.g rice by 20-30 % decline
- agriculture contributes to Pakistan's GDP by one fifth
- and also employs 45% of the country's workforce
- poor farmers & landless labourers wiht few resources were affected
- concerns of spread of disease and malnutrition after 2 months of the disaster.
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North Devon/Cornwall UK
Causes of flood at Lynmouth in north Devon and Boscastle in Cornwall in 2004:
- onshore winds bring warm moisture-laden air frm Atlantic ocean which is uplifted as it meets uplands of Exmoor & Bodmin Moor= trigger torrential downpours.
- steep drainage basins on Lyn,Valency, & impermeable geology & sparse tree cover ??????
- villages such as Lynmouth & Boscastle occupy the floors of steep,narrow valleys down whc floodwaters are funnelled.
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Lower Severn Floods, Gloucestershire&Worcestershir
Causes:
- xtreme precipitation on 20 JUly, 135 mm of rain fell at Pershore on Worcestershire in 16 hrs
- flash floods in several local tributary catchments raised the level of the Severn at Worcester- 6 m above normal
- heavy antecedent soil moisture- soils were already saturated by record rainfall in June
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Impacts of Lower Severn Floods
Impacts:
- by 21 July,widespread floodin all along river severn frm Upton to Gloucester
- floods hit town and villages on River Avon
- Tewkesbury- floodwaters entered the town's ancient abbey for the first time in 247 yrs.
- near Glos,foodwaters shut down electricity substation-leavin 50 000 households wiht out power for 2 days
- tewkesbury, water treatment plant flooded, cuttin water supply to 140 000 households for 5 days
- 10 000 motorists left stranded on M5- forced to abandon thier cars becoz of floodwater & landslides
- insured losses were estimated between £1 billion - £1.5 billion
- large scale damage to property & disruption of businesses
- 27 000 domestic insurance claims
- 6 800 business claims made
- crops were submerged & maize, potatoes were destroyed.
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Coastal Flooding: Eastern England
Causes:
- low pressure areas/depressions accompanied by gale winds force winds
- high tides present major flood hazards to the low lying coastal areas
- breaching of sea defences by elevated sea levels known as storm surges
- generated hurricane winds moved through the North Sea
- as it moved south, the shallow funnel-shape of southern part of north sea amplified its height
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Eastern England Floods
IMPACTS:
- eastern england & southern netherlands were hit by greatest north sea storm surge on record.
- surge heights reached 3m at Kings Lynn & 3.36m in Netherlands
- flood embarkments were breached & sea walls crumbled
- in east and southeast england 307 pple died
- 75 000 ha of farmland were flooded
- 24 000 homes damaged
- however, in contrast of the 2007 floods in the same area- surge was accurately forecast
- thames barrier closed & flood warnings issued
- pple at risk were prepared for evacuation
- tidal peak passed without incident, though sea level at Great Yarmouth rose to within 10 cm of the top of the sea walls
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Coastal Erosion at Happisburgh, Norfolk
In northeast Norfolk coastal erosion rates often exceed 5 m a year!!!
PHYSICAL CAUSES:
- coastline comprisin weak sands & gravel & soft clay is easily undercut by wave action
- the long fetch to north & northeast means that wave energy is high along this coast.
HUMAN CAUSES:
- erosion has accelerated since 1990 when 300 m of sea defences (revetments) were destroyed by a storm
- decision not to repair revetments increased erosion
- led to loss of six cliff top homes
- gorvernment policy of 'no active intervention' the village of Happisburgh cud disappear before end of century.
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Hard Engineering at North Bay, Scarborough
Strengthening hard defences:
- north bay, surrounded by built up urban environment, is protected by hard defences
- concrete sea walls extend along the entire length of the bay & protect the narrow promenade, coastal road & steep coastal slope
- btwn 2000&2005 hard defences were strengthened in southern part of bay
- thousands of tonnes of rip rap at coast of £26 million were imported by barge & positioned at the foot of the sea wall
- aim was to prevent wave overtopping, damage to infrastructure on promenade and landslips on coastal slope
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ISSUES:
- hard defences are controversial apart from cost
- may cause significant loss of sediment in the Bay
- advanced line of defences & highly reflective nature of sea walls may have increased energy levels over the remaining upper beach- resulting in sediment being removed offshore
- without hard defences, north bay wud hve a broader upper beach that wud provide natural protection for the coast
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Soft engineering at Freiston Shore, Lincolnshire
Background&Issues:
- in 1983, 66 ha of salt marsh at Freiston was reclaimed frm the sea
- reclaimed land was protected by an earthen flood embarkment and converted to arable farming.
- costs of maintainin sea defences, with the relatively low value of the reclaimed land- made managed realignment a more cost-effective, and a more sustainable alternative.
RESPONSES & IMPACT:
- environment agency, english nature & RSPB produced more sustainable realignment plan which involved breachin flood embarkment- allow the are to return to mix of salt marshes&saline lagoons
- within 13 months of breachin, inter-tidal area was colonised by 11 species of salt marsh plants, 8 species of fish& numerous waders,geese and ducks
- Today, Freiston attracts 60 000 visitors a yr, bringin £150 000 a yr to the local economy&creatin four full time jobs.
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