What are the hazards associated with flooding? Flashcards

1
Q

What are the physical causes of floods?

A
  • Usually by altering the balance of stores, inputs and outputs in the system
  • Climate – snow melt, heavy rain (thunderstorms), low evaporation, storm surges
  • Previous weather conditions e.g. a long period of wet weather
  • Relief – very flat, low lying area
  • Drainage – density, regime, hydrograph, drainage pattern and density, drainage type
  • Vegetation – grass versus trees
  • Rock type – permeability, porosity, water table
  • Soil conditions – wet versus dry, bakes impermeable by a drought
  • Natural disaster – earthquake, landslide
  • Subsidence – area is sinking (isostatic, removal of groundwater, etc.)
  • Rising sea level – global warming melting ice sheets
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2
Q

What are the human causes of floods?

A
  • Usually by putting human activities in areas at risk and interfering with the natural cycle/hydrology
  • Construction of impermeable surfaces, e.g. town, roads
  • Removal of vegetation cover – deforestation, removal of coastal marshes/mangroves, farming
  • Soil erosion, leading to silting of channels and storage lakes
  • Drainage – ditches, waste disposal, drains, excessive irrigation
  • Changing rivers – dams, diversions, embankments, removing or adding deposi
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3
Q

What are primary impacts of flooding?

A
  • Deaths – humans, pets and livestock
  • Evacuation
  • Destruction of buildings/possessions
  • Disease from polluted water
  • Stress
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4
Q

What are secondary impacts of flooding?

A
  • Transport links broken (bridges, roads, rail)
  • Cost of clean up and replacement
  • Loss of jobs
  • Crops ruined (animals may starve)
  • Rehousing costs
  • May take over a year to dry out buildings
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5
Q

What are tertiary impacts of flooding?

A
  • Flood prone areas decline as property values decrease

- Difficult for owners to get insurance or sell property

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6
Q

Responses to flooding - what is preventative planning?

A
  • Planning – avoid flood plains and green sectors, e.g. parks
  • Planned retreat – leave certain areas to flood
  • Reduce surface flow, e.g. afforestation, contour ploughing
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7
Q

Responses to flooding - what is structural planning?

A
  • Channel modification, e.g. overflows, storage areas, dams, widen channels
  • Embankments – raise them, reinforce them, put up flood gates
  • Flood relief channels
  • Flood barrages, e.g. on the River Thames
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8
Q

Responses to flooding - what is management?

A
  • Early warnings – better weather and river level forecasts, communications
  • Flood insurance
  • Public relief funds
  • Accept the risk and live accordingly
  • Ignore the risk (‘head in the sand’ approach)
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9
Q

Responses to flooding - what is emergency rescue?

A
  • Rescue people and animals
  • Save property and possessions
  • Use sandbags, erect flood barriers, pump out property
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10
Q

Background to flooding on the River Severn

A
  • The river Severn is the third largest British river
  • It rises in the mountains of central Wales above 800m – On leaving the mountains, it initially flows east before turning south to its estuary in the Bristol Channel
  • Two major reservoirs in the upper catchment provide flood water storage
  • However, the lower catchment, especially between Worcester and Gloucester, fed by major tributaries such as the Avon and the Teme, is particularly vulnerable to flooding
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11
Q

What physical factors affect flooding on the River Severn?

A
  • Rock type, relief, climate and vegetation
  • Large parts of the upper catchment in central Wales are above 300m, where slopes are steep and the main rock types have low permeability
  • As a result, runoff is rapid and small tributaries, which feed into the main river, are highly responsive to rainfall and therefore liable to flash floods
  • The main relief feature in the lower catchment is an extensive floodplain, only a few metres above sea level
    o Much of the land adjacent to the River Severn floods regularly in winter
    o Flooding is also more likely to occur in the lower catchment because of the convergence of a number of major tributaries in this area
  • The Warwickshire Avon joins the river Severn at Tewkesbury, and the River Teme’s confluence with the Severn is just south of Worcester
  • Mean annual rainfall in the mountains in central Wales exceeds 2000mm, and because of orographic uplift, rainfall is often intense and prolonged
  • Low rates of evaporation mean that most rainfall is converted to runoff and river flow
  • Vegetation cover influences rates of interception, evapotranspiration and runoff
    o Nearly 45% of land use in upper catchment compromises rough pasture and moorland
    o This promotes rapid runoff and increases the flood risk
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12
Q

What human factors affect flooding on the River Severn?

A
  • The main human factor contributing to the flood risk is building on the Severn floodplain
  • Large parts of the settlements of Upton-upon-Severn and Tewkesbury occupy the floodplain
  • Without adequate flood defences, these areas are exposed to a high level of risk
  • Within the lower Severn and Avon catchments there is evidence that recent urbanisation has accelerated the loss of floodplain land, reducing natural water storage and placing more properties at risk
  • Rural land-use change and land-use management may also have contributed to higher peak floes
  • Improved drainage of farmland speeds the movement of rainwater into rivers; so too does the conversion of pasture to arable and the clear felling of forestry plantations
  • The lack of hard flood defences also exposes much of the lower Severn valley to flooding
    o There are few flood embankments, and other forms of river engineering such as flood relief channels, channel widening and straightening are absent
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13
Q

When did the River Severn flood badly?

A

July 2007

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14
Q

What happened during the River Severn flooding, July 2007

A
  • Large parts of England and Wales, including Humberside, South Yorkshire, and the lower Severn valley and the Thames valley were affected by sever flooding in the summer of 2007
  • The floods in the Severn valley followed an extreme rainfall event on 20 July, when 135 mm of rain fell at Pershore in just 16 hours
  • Flash floods in several small catchments such as the Isbourne in Worcestershire then fed into the major rivers, raising the Severn at Worcester nearly 6m above normal and the River Avon at Evesham to the highest level ever recorded
  • The severity of flooding was due to exceptional rainfall, but also to soils already saturated by heavy rains in June
  • Where flood defences were overwhelmed it was because the flow level exceeded their design
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15
Q

What was the human reaction to the July 2007 floods?

A
  • General management responses towards river flooding in the UK are shown in tables on next page
  • Immediate responses included the erection of temporary flood barriers and flood warning issued by television, radio, the Environment Agency’s ‘Floodline’ and the internet
  • The Severn Trent water authority’s response to the disruption to water supplies was the immediate distribution of 5 million litres per day of bottled water and the deployment of 1500 water bowsers
  • The government provided £87 million of emergency aid for funding schools, transport and businesses hardest hit by the floods and the European Union contributed a further £31 million in compensation
  • Overall spending on flood defences by the UK government doubled between 1997 and 2007 and the experience of the 2007 floods promoted the government to pledge an increase on flood defenced to £800 million by 2010-2011
  • However, apart from the provision of temporary flood barriers for Upton-on-Severn, and raising some flood embankments around Gloucester, the Environment Agency (EA) has no plans for major new flood protection schemes in the lower Severn valet
  • People living in the flood-prone areas will learn how to live with floods, and rely on the EA’s flood warning system and on flood insurance
  • Huge investment in new river flood defences, like coastal defences, like coastal defences is seen in the long term as being unsustainable
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16
Q

What were the societal impacts of the July 2007 floods?

A
  • Considerable destruction to electricity and water supplies
  • Flooding of a sub station near Gloucester left 50,000 households without power (some for up to 2 days)
  • A water treatment plant in Tewkesbury was also flooded with the result that water supplies for 140,000 households were cut off and without water for at least 5 days
  • Safe drinking water was not restored until 7 August
  • Ten thousand motorists were left stranded on the M5 and surrounding roads and forced to abandon their cars
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17
Q

What were the economic impacts of the July 2007 floods?

A
  • The total insured loss estimated for the 20 July flood even was £1-1.5 billion
  • These losses include damage to property, motor vehicles, disruption to businesses and the expense of providing temporary accommodation for those forced to leave their homes
  • There were large-scale damage to property and disruption of businesses: 27,000 domestic insurance claims and 6800 business claims were made
  • Many motor vehicles were damaged completely, and abandoned vehicles blocked roads and traffic flows
  • The M5 was closed due to flooding and landslides on 20 July
  • Crops were submerged and maize, potatoes and hay crops lost
  • Where floodwater contained sewage, crops had to be destroyed
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18
Q

What were the environmental impacts of the July 2007 floods?

A
  • Thousands of small mammals drowned, ground nesting birds were badly affected and large numbers of mature fish were left stranded on the floodplain when water levels receded
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19
Q

What non-structural measures approaches are the to river flood management in the UK?

A
  • Catchment flood management plans
  • Afforestation and land-use change
  • Controlling development on floodplains
  • Flood insurance: exposure and vulnerability
  • Washlands or flood basins
  • Flood warnings
  • Flood risk maps
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20
Q

What are catchment flood management plans?

A
  • A holistic approach to environmental management of drainage basins
  • The primary concern is sustainable flood management
  • Other environmental issues include water abstraction, pollution, land-sue change and wildlife conservation in drainage basins
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21
Q

What are the advantages of flood management plans?

A
  • Drainage basins are natural units
  • Until now they have been managed piecemeal by different agencies e.g water authorities, Environment agency (EA), DEFRA
  • CFMPs provide an opportunity for coordinated planning of environmental resources within natural geographic units
22
Q

What is afforestation and land-use change?

A
  • Changing land use in headwaters can help prevent flooding
  • Afforestation slows runoff, increases water loss through evapotranspiration and reduces peak flows
  • Discouraging artificial drainage in upland catchments and conserving areas of wetland can also reduce peak flows
23
Q

What are the advantages/disadvantages of afforestation and land-use change?

A
  • There is difficulty in getting landowners to agree to land-use changes
  • Changes such as afforestation and wetland conservation often benefit wildlife and improve amenity
24
Q

What is controlling development on floodplains?

A
  • The government provides local authorities with guidelines aimed at controlling floodplain development
  • Climate change will increase flood risks so floodplain development must be sustainable
  • Currently 10% of England is exposed to significant flood risks
25
Q

What are the advantages/disadvantages of controlling development on floodplains?

A
  • There is a huge demand for new housing in the UK and limited space to accommodate it
  • The govt. wants to encourage redevelopment of brownfield sites
  • However, many of these are close to rivers and are vulnerable to flooding
26
Q

What is flood insurance: exposure and vulnerability?

A
  • Insurance premiums will rise as flood hazards increase with climate change
  • Many householders may be unable to afford premiums, or will be forced to buy insurance with large excesses
27
Q

What are the advantages/disadvantages of flood insurance

A
  • Insurance premiums will rise as flood hazards increase with climate change
  • Many householders may be unable to afford premiums, or will be forced to buy insurance with large excesses
28
Q

What are washlands or flood basins?

A
  • Floodwaters are stored temporarily on floodplains reducing the flood peak and saving settlements downstream from potential flooding
29
Q

What are the advantages/disadvantages of wash lands or flood basins?

A
  • Wash lands can be used for grazing for most of the year and when flooded provide valuable refuges for wildlife
  • Wash lands work with nature because they occupy areas that flood naturally
30
Q

What are flood warnings?

A
  • The EA provides information on flood risks through telephone ‘Flood lines’ and websites
  • There are three levels of alert: flood watch; flood warning; and severe flood warning
  • A flood warning means that flooding is imminent and people at risk should take immediate action
31
Q

What are the advantages/disadvantages of flood warnings?

A
  • Flood alerts allow people to prepare for flooding and minimise the damage to property and the threat to life
32
Q

What are flood risk maps?

A
  • The EA publishes maps on its website which show areas at risk from river and coastal flooding
33
Q

What are the advantages/disadvantages of flood risk maps?

A
  • The EA’s flood maps 1:50,000, give only a general view of areas at risk
  • More detailed maps, based on GPS data, will eventually become available and enable insurance companies to asses risk more accurately
34
Q

What structural measures approaches are the to river flood management in the UK?

A
  • Flood embankments or levees
  • Dams and reservoirs
  • Channel straightening
  • Flood relief channels
35
Q

What are flood embankments/levees?

A
  • Flood embankments are walls on either side of a river’s channel
  • By increasing channel capacity they reduce the risk of floodwaters spilling onto the floodplain
36
Q

What are the advantages/disadvantages of flood embankments/levees?

A
  • Flood embankments are often unsightly and may cause rivers to flow above the floodplain
  • If flood embankments fail the potential damage is much greater than a normal flood
  • Embankments can also raise flood levels, accelerate channel erosion, are expensive to build and maintain, and in the long term unsustainable
37
Q

What are dams and reservoirs?

A
  • Damming of rivers and their tributaries allows floodwaters to be stored and released gradually
38
Q

What are the advantages/disadvantages of dams and reservoirs?

A
  • Dam construction involves huge capital costs and reservoirs may flood valuable farmland and/or environmentally important valets
  • Unusually large flood events can overtop dams
  • Apart from flood management, dams have other benefits, e.g. HEP production, water supply, water-based recreation and leisure
39
Q

What is channel straightening?

A
  • Meanders are removed, increasing channel gradient, flow velocity and depth
  • To prevent meanders reforming, straightened channels may have to be lined with concrete
40
Q

What are the advantages/disadvantages of channel straightening?

A
  • Increasing gradient gives a river surplus energy which results in it scouring its bed, eroding laterally, and re-establishing it meandering channel
  • Straightening a river is only sustainable if the channel is hardened to prevent erosion
  • Channel straightening is also unattractive aesthetically
41
Q

What are flood relief channels?

A
  • Artificial channels are constructed, diverting some of the flow from a river to reduce the risk of flooding
  • The Jubilee River scheme created a relief channel on the River Thames to give flood protection to communities in Maidenhead, Windsor and Eton
42
Q

What are the advantages/disadvantages of flood relief channels?

A
  • Flood relief channels are effective in preventing flooding in places they were designed to protect, but do nothing to stop flooding further downstream
  • They are used infrequently and when empty are unsightly concrete boxes
43
Q

What is a storm surges?

A

Rapid rise of sea level above normal high tide, in which water is piled up against the shore by strong onshore winds

44
Q

How are storm surges generated?

A

by tropical and extra-tropical storms
- The low air pressure and wind direction (inward-blowing winds) combine to produce large, temporary rises in sea level that have the capacity to cause extensive flooding of coastal lowlands
o They are usually associated with strong winds and large onshore waves which increase the damage potential
- The largest surges are produced by hurricane landfalls, but extra-tropical storms can also produce large surges in appropriate settings
- The north sea region experiences significant surges due to extra-tropical storms, and the locations susceptible to flooding feature large populations and substantial investments

45
Q

Background to Bangladesh

A
  • Bangladesh is situated astride the Tropic of Cancer, between 20 degrees and 26 degrees
  • It is bordered to the north, east and west by India, to the southeast by Myanmar
  • It is a low income country and one of the most densely populated in the world
  • The coastal districts suffer high levels of exposure to flooding
46
Q

Physical factors affecting flooding in Bangladesh

A
  • Few places in the world are at greater risk from flooding than the coastal districts of Bangladesh
  • Most of Bangladesh occupies the Ganges-Brahmaputra delta, a vast area of alluvial islands, shifting river channels and tidal inlets only a metre or two above sea level
  • Flooding occurs frequently when strong onshore winds and low pressure in the Bay of Bengal coincide with exceptional Spring tides
  • Storm surges up to 10m high, generated by tropical cyclones that originate in the Indian Ocean and track northwards through the Bay of Bengal, slam into the delta every few years causing massive devastation and death
    o These cyclones, powered by the ocean’s warm surface waters, drive storm surges to the delta coast
  • The natural funnel shape of the Bay of Bengal steepens the storm surge which overwhelms the low-lying tidal floodplains of the delta
47
Q

Human factors affecting flooding in Bangladesh

A
  • Bangladesh’s densely populated delta lands adds to the regions exposure to coastal flooding
  • Pressure of population on the land forces millions of people to risk their lives and live in places exposed to storm surges and tidal flooding
  • So does too Bangladesh’s poverty: Bangladesh is one of Asia’s poorest countries, its GDP per capita being just $423 in 2005
    o Roughly around two in every five Bangladeshis cannot afford enough food to sustain a healthy life, making the population even more vulnerable to flooding and other natural disasters
  • In the past, a dearth of investment in coastal defensive structures such as levees, storm surge shelters and flood warning systems has also left the population highly vulnerable to flood disasters
48
Q

When was cyclone Sidr?

A

2007

49
Q

What is Cyclone Sidr? What were the affects?

A
  • Cyclone Sidra made a landfall on the southwest coast of Bangladesh on 15 November 2007
  • A category 4 cyclone, Sidr was the most powerful storm to hit Bangladesh since 1991
  • Its impact was widespread and devastating
    o At its height winds reached speeds of up to 240kph and generated a 5m storm surge which swept inland
  • Large areas of the coast were flooded, and over 4000 people died
  • Over 1.5 million homes were damaged and 1 million ha of crops destroyed
  • The total economic cost was around US$450 million and nearly 9 million people were affected
  • One-quarter of coastal mangrove forests was badly damaged by the storm surge and hurricane-force winds
    o Parts of the forest could take up to 40 years to recover
    o It’s a world heritage sight with a unique ecosystem
50
Q

What was the human response to Cyclone Sidr?

A
  • Significant progress on hazard mitigation in Bangladesh occurred between 1991 and 2007
    o This is evident in the relatively low death toll caused by Cyclone Sidr compared to previous cyclones
  • Satellites monitored the progress of Sidr and the authorities were able to provide an early warning and evacuate over 1 million people in the most hazardous areas
  • Cyclone walls, planted with tress, also saved lives in some of the most exposed areas
  • Short term aid in the form of disaster relief funds, emergency food, blankets and clothing came from the USA and from NGOs such as Oxfam and the Red Cross
  • The World Food Programme sent food rations for over 400,000 people, and for longer term relief, the World bank pledged US$250 million in aid
51
Q

Coastal flood management…

A

Like river flood management, coastal management relies on two approaches:

o Hard engineering
o Soft engineering

  • Hard structures raise the level of the coastline and provide a barrier to the sea
  • Where wave energy is greater and where important settlements need protection, sea walls are built (expensive and require constant maintenance) – only justified where the value of property exceeds their cost of construction
  • Hard structures can also cause problems within the coastal system
    o Sea walls stop erosion and the input od sediment to the coastal system – nearby stretches of coast, unprotected by sea walls, may suffer accelerated erosion
  • Current policies of coastal flood management in England and Wales are based around Shoreline Management Planes (SMPs)
    o The coastline of England and Wales is divided into 11 natural units – they are self contained in terms of sediment supply and sediment movements
    o SMPs have been developed for each cell
    o Within each cell, smaller lengths of coastline or sub-cells have been defined
    o Management policies for the sub-cells state whether existing sea defences are to be
    • Advanced – moving coastal defences into areas now covered by the sea
    • Maintained – keeping the shoreline in its present position
    • Abandoned – allowing the shoreline to be moved inland in a controlled manner
    • Ignored – literally doing nothing and allowing nature to take its course
  • The new philosophy is to work with nature wherever possible
    o Working with nature means interrupting sediment movements as little as possible; allowing the sea to recreate the natural boundary between land and sea; getting rid of some hard structures which squeeze salt marshes and mud flats and result in their erosion; and recognising that rising sea levels will in future make the costs of maintaining and increasing existing defences unsustainable