Flood Occurrence and Management

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    Introduction

    A flood is usually caused by

    rain, heavy thunderstorms,

    and thawing of snow.

    Its considered to be atemporary condition of two or

    more acres of dry land either:

    Overflowed with inland or

    tidal waters

    Rapid or runoff of surfacewaters

    Mudflows

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    CAUSES OF FLOODS

    PRECIPITATION

    INADEQUATE CAPACITY (WITHIN

    BANKS)

    BANK EROSION AND SILTING

    LAND SLIDES

    TIDAL AND BACK WATER EFFECTS

    POOR DRAINAGE

    SNOW MELT AND GLACIAL OUT

    BURSTS

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    How does Flooding Start and

    end?

    The shore or land by or surrounding a body of

    water erodes and this erosion causes waves

    currents that result in a flood.

    Flood disasters have been increased because

    of the expansion of settlements and growth in

    floodplains.

    Floods could be slow or fast but usually occurover a matter of days.

    After the water eventually goes down or dries

    up. On coastal floods, low tides and high tides

    makes a change in heights.

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    Why does it occur ?

    A flood is too much water in the wrong place.

    Sometimes a flood occurs from :

    Sewer (drain) backup Collapse of land along the shore of a lake or

    another body of water. This results in waves

    or currents during a flood

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    Flooding is the most worldwide natural disaster.It occurs in every country and wherever there israinfall or coastal hazards.

    They are most likely to happen in tropical areasand tsunamis.

    Most common floods happen around the worldslargest/greatest rivers.

    Believe it or not, smaller rivers could causemore damage even though people dont pay asmuch attention to them.

    Most Flooding occurs during the beginning ofspring.

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    Types of floods:-

    1. Flash Floods

    2. River Floods3. Coastal Floods

    4. Lakeshore Floods5. Urban and Ice Jams

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    Flash Floods

    Flash floods happen in a short

    time, they have a great volume

    of water, and are local floods.

    The runoff of intense rain

    results in high flood waves.

    Flash floods result in failure of

    dams and more.

    It usually happens in desert

    areas and mountain regions.

    They are a threat in steep land,high runoff rates,

    thunderstorms, and narrow

    streams.

    This is a picture of a town

    after a Flash Flood

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    River Floods

    Riverine floods are caused by

    melting of snow and precipitation

    over large areas. They take place inrivers. Floods in large rivers take

    hours to days.

    The ground conditions effects the

    runoff.

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    Coastal Floods

    Coastal floods are caused by

    tides, storms, tropical cyclones,

    or tsunamis.

    They happen in the ocean andeffects the general public and

    maritime interests along the

    coastline.

    They are caused by heavy surf,tidal piling, and storm surges,

    Other factors are tidal cycles,

    behaviors of the storm, river or

    stream runoff, no offshore reefsor other barriers, and high

    Venezuela in December of 1999.

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    Urban Floods and Ice Jams

    Urban floods are when the

    land is turned from fields or

    woods into roads and parking

    lots. Since this happens it

    cant absorb the rainfall.

    During the urban floods all

    the streets become rivers and

    basements becomefull of

    water, they are death traps. Ice Jam is floating ice that

    adds up at a man-made or

    natural area and stops the

    flow of water. This causes the

    area to flood.

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    Lakeshore Floods

    Lakeshore floods affect the

    general public as well as some

    areas of the Great Lakes.

    These floods extend from the

    beaches to rivers that flow intolakes. The extent of the flooding is

    dependant on surrounding the

    shore terrain. The causes of these

    lakeshore floods are seiches in the

    Great Lakes.

    The Webster dictionarys definition

    ofSeiches is:

    The flow of periodically changing

    direction of the surface of a

    landlocked body of water (like a

    lake) that varies from a few

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    FLOOD MANAGEMENT

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    Human response to Flooding:

    1. Flood protection decreases risk of

    bankfull capacity being exceeded

    2. Flood abatement reduces stormflow and

    reduces peak discharge levels

    3. Behavioural responsessocieties adopt

    different coping strategies

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    Flood Protection

    1) Modification to channel or banks:

    Bank raising and dredging both increase bank fullcapacity

    By increasing the hydraulic radius, channels alsobecome more efficient (velocity increases and sowater levels drop)

    Widely used (e.g. Mississippi 3000 kms of raisedlevees up to 15 m high)

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    Flood Protection

    2. Artificial channel linings :-

    Concrete lined channels createsmootherwetted perimeterand soincrease velocity

    Thus water levels drop and flood risk is

    reduced Expensive, and high maintenance

    E.g. Los Angeles

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    Flood Protection

    3. Dam construction :-

    Multi-purpose, but key tool for flood protection

    Controlled release of water stored in reservoir throughsluice gates can spread discharge over a longerperiod (reducing peak flows)

    Effectiveness depends on relative scaleof reservoirs

    catchment area to that of the whole drainage basin Geo-politics can cause problems

    e.g. India and Bangladesh (Ganges), Spain andPortugal (Tagus), Zimbabwe and Mozambique(Limpopo and Floods of 2000)

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    Flood Protection

    4. Flood relief channels:

    It effectively increases bank full capacityand diverts flow away from high impactzones

    It requires there to be space on floodplains

    to skirt around high impact zones, so notalways possible

    e.g. River Exe at Exeter, River Thames atWindsor

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    Flood Protection

    5. Spreading grounds:

    Diverting flood water to low impact flood plainzones, for storage

    Reduces downstream peak flows

    Low impact zones can be recreational land use

    Flood water will evaporate or eventually infiltrate,replenishing groundwater supplies

    E.g. Los Angeles basin

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    Flood Protection

    6. Debris dams:

    To trap sediment in upper catchments to prevent

    downstream bed aggradation Maintains higher bank full capacities

    downstream

    Periodic need for emptying, but can be used for

    construction materials Especially important in semi-arid, mountainous

    catchments

    E.g. Los Angeles Basin

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    Flood Protection

    7. Straightening of sinuous

    rivers:

    Increases gradient increases flow rates

    Thus water levels drop and flood risk is

    reduced Also reduces deposition and averts bed

    aggradation

    Also keeps channels navigable

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    Behavioural responses

    1. Accepting the loss Fatalism often only

    option in countries like Haiti or Bangladesh

    2. Public relief funds Emergency response

    to hazard event requires funding, materials,

    technical support, rebuilding. Sources vary

    from UN agencies to governments andNGOs

    3. Flood insurance A standard response in

    flood prone communities in the North

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    Behavioural responses

    4. Monitoring and Prediction Data on rainfall

    and stream discharge can be used to produce

    accurate predictions of the timing of flood

    surges Can be used for communities to prepare for

    actual flood event or for authorities to organise

    evacuations

    Not always possibleflash floods have too

    short a lag time (e.g. Boscastle, Devon, U.K.,

    2004), lack of technical equipment / personnel

    (Haiti, 2004), or communication systems

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    Behavioural responses

    5. Floodplain zoning

    Planning authorities can prohibit certainland-uses in the more flood pronefloodplain zones

    6. Flood proofing

    Individuals bear responsibility for

    reducing likely flood damage to property Techniques: water-proof garden walls,

    windows and doors; sandbags; buildings

    on stilts; removal of damageable goods

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    THANK

    YOU