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Flood Hazard Mitigation

Apr 13, 2018

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Rahnuma Rahman
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    Flood Hazard and MitigationFlood Hazard and Mitigation

    zanur a man, Ph.D., PDFPh.D., PDFBangladesh Water Development Board,Bangladesh Water Development Board,

    Ministry of Water ResourcesMinistry of Water Resources

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    What is Flood?

    Discharge exceeds the capacity of waterDischarge exceeds the capacity of waterbody, like a river,body, like a river, lakes,lakes, oror pondpond of water atof water at

    or near the point where the rain fall andor near the point where the rain fall and

    then proceeds to inundate the surroundingthen proceeds to inundate the surroundingareas to damage the life and socioareas to damage the life and socio

    economic infrastructures is the flood.economic infrastructures is the flood.

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    RAINFALLPOTENTIAL EVAPORATION

    MODEL/EQUATION

    PARAMETERS/ASSUMPTIONS

    RUNOFF COMPONENTS

    EVAPORATION

    RECHARGE

    Rainfall Runoff Model

    Evapo-transpiration

    Water Level

    Run-Off

    Iterception andSurface Retention

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    Types of Flood

    According to Duration of the TravelingAccording to Duration of the Traveling

    Lon Time Travelin floodLon Time Travelin flood

    Short Time Traveling floodShort Time Traveling flood

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    Long Traveling floodLong Traveling flood

    More travel time, Follows river systems, Events (Rainfall and

    Snow melt) may be occurred outside the Flood area

    Example:

    1. Ganges carries water from Himalayan of Uttarakhand: Snow

    melting and heavy rainfall in Himalayan will affect in Bihar and

    then Bangladesh

    2. Brahmaputra starts from Manosh Sarawar in Tibet and

    passes through China, Arunachal, Assam and then

    Bangladesh3. Bihar Arunachal Assam and Bangladesh are getting flooding

    RIVER FLOODRIVER FLOOD

    Continued

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    More travel time, follows tide and current, events

    (eartquake in the sea) may be outside the affectedarea

    Exam le:

    Long Traveling floodLong Traveling flood

    Earthquake occurred in Sumatra, Indonesia. High sea wave

    hits Sri Lanka.

    TSUNAMI

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    Indonesia

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    Short Traveling FloodShort Traveling Flood

    Less travel time, may not follow river, events (heavy

    rainfall) may occurred within or nearby catchment

    area)

    Exam le: hill area ma e heav rainfall and heExam le: hill area ma e heav rainfall and he

    runoff may affect the plain land immediately afterrunoff may affect the plain land immediately after

    steep hilly terrain.steep hilly terrain.

    FLASH FLOODSFLASH FLOODS

    Continued

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    Short Traveling FloodShort Traveling Flood

    Less travel time, not follow river, events (heavy

    rainfall) may occurred in urban area

    Example: Heavy rainfall starts in the paved areas,Example: Heavy rainfall starts in the paved areas,

    when draina e ca aci failed hen beca se of overwhen draina e ca aci failed hen beca se of over

    flow surface runoff occurred.flow surface runoff occurred.

    URBAN FLOODURBAN FLOOD

    Continued

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    Short Traveling FloodShort Traveling Flood

    Very less travel time, may not follow river, events

    (failure of water retention structures) are occurred

    within or nearby affected area)

    Exam le: Wa er re en ion s r c res o re ain wa erExam le: Wa er re en ion s r c res o re ain wa er

    in a reservoir or in a water body may fail and createin a reservoir or in a water body may fail and create

    catastrophic disaster in the downstream of thecatastrophic disaster in the downstream of the

    structure or water bodystructure or water body

    Dam Break Floods andDam Break Floods and

    Glacier Lake Outburst Flood (GLOF)Glacier Lake Outburst Flood (GLOF)

    Continued

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    Short Traveling FloodShort Traveling FloodVery less travel time, may not follow tide and current,

    events (eartquake or depression in the sea) are

    occurred within or nearby affected area

    Example: Earthquake in at Sumatra Indonesia andExample: Earthquake in at Sumatra Indonesia and

    and affect the nearby coastal area.and affect the nearby coastal area.

    Tsunami andTsunami and

    Tidal storm floodsTidal storm floods

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    According to location of the eventsAccording to location of the events

    Tidal Storm Flood (Surge and Cyclone)Tidal Storm Flood (Surge and Cyclone) Coast AreasCoast Areas

    Tsunami (Earthquake in the Sea)Tsunami (Earthquake in the Sea)-- IslandsIslandsand Coastand Coast

    Types of Flood

    Arroyos Flood (DAM Break andArroyos Flood (DAM Break and GlacierGlacierLake Outburst)Lake Outburst)-- Mountain AreasMountain Areas

    River Flood ( Flood in the flood plain)River Flood ( Flood in the flood plain)

    Plain LandPlain Land Rain fed flood (Rural and Urban area)Rain fed flood (Rural and Urban area)--

    Urban AreaUrban Area

    Flash FloodFlash Flood (Hilly areas)(Hilly areas)

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    Flood HazardFlood hazard is the potential risk to life

    from flooding.

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    Types of Flood Hazard

    Primary Hazard Direct Damage

    n r H z r In ir D m

    Tertiary Hazard Long Term Damage

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    Primary HazardsPhysical damage

    crops, roads and railways, bridges, transports, airport, houses, school, business centers, industries, sewer systems, canals, religious places, tourism,

    forest, wildlife,

    Continued

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    Primary Hazards

    Casualties

    Human life and

    Livestock.

    Continued

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    Primary Hazards

    Health damages

    epidemics and

    waterborne diseases

    Continued

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    Primary Hazards

    Displacement

    sediments and rocks (some times suchlarge objects as automobiles),

    houses and bridges.

    Continued

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    Primary Hazards

    Soil Erosion

    river bank,

    levees and buildings

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    Secondary Hazards

    Disruption of services drinking water supplies and sewerage system

    gas and electrical service.

    Continued

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    Secondary Hazards

    Famine and disease transportation systems disrupted and crop

    damages: resulting in shortages of food

    ,

    Continued

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    Secondary Hazards

    Loss of institutional resources Institutional damages of school and colleges

    Institutional and instrumental damage in hospital and

    spensar es

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    Tertiary HazardsEnvironmental effects

    Shifting of the river channels

    Coarse sand deposition on theagricultural land (non-productivity)

    land (productivity).

    Continued

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    Tertiary HazardsLivelihood

    Jobs may be lost due to the disruption ofservices, destruction of industries andbusiness etc.

    Although jobs may be gained to helprebuild or repair flood damage

    Continued

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    Tertiary HazardsPrice escalation due increase of

    taxes,

    duties,

    Continued

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    Tertiary HazardsBiodiversity

    Destruction of wildlife habitat

    Fish migration

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    Flood Hazard Mitigation

    Flood hazard mitigation is the measures

    against the floods to reduce the sufferings

    and dama es of ro erties as well lives

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    Types of Measuresfor mitigation

    Structural measures

    Non-structural measures

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    Structural measures1. Protection of flood intrusion

    embankment polder

    barrage

    regulator

    sluice

    Continued

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    Structural measures2. Improvement of flood flow drainage

    Dredging of channels River training

    Flood risk mapping

    Continued

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    Structural measures3. Adaptation Mechanism

    Constructing flood shelters, Raising home stead,

    railway lines

    Introducing flood proof agriculture

    Continued

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    Non Structural measures

    1. Forecasting and early warning

    Detection of onset Flood Development warning message

    ssem na on o warn ng messageto the decision makers

    Continued

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    Flood Detection:Flood Detection:

    Forecasting ModelsForecasting Models

    Hydrologic Models

    Simplified Models for rapid assessment

    Less data requirement

    Mostly aggregated parameters were used

    Hydraulic Models

    Complex Models for greater accuracy

    Highly data demanding

    Suitable for distributed watershed modeling

    environment

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    Hydrologic Processes in Flood ForecastingRainfall

    Rainfall Excess

    Interception

    InfiltrationDepression Storage

    Losses

    Catchment Data

    Overland flows

    Channel flows

    No FloodNo Yes

    FloodingVulnerability

    Analysis

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    Flood Forecasting and Warning System

    Indian Data

    WMO

    JRCWARPO

    Radio

    wir

    Tele

    River stage

    Rainfall

    R

    e

    a

    l

    T

    i

    m

    e D a t a

    Dissemination

    to the public

    InternetInternet

    FFWC Radio Tower

    FFWC Satellite dish

    24, 48, 72 hr

    forecasts

    water level

    flood extentmaps

    thanainundation

    maps

    Telephone

    Fax

    Fax Modem

    ModemTelevision

    Bulletine

    GIS data layers

    less

    communication

    via modem

    manual entry

    etry

    /Databox/Voice

    SPARRSOSattelite images

    BMD

    Weather forecastSynoptic charts

    Boundary estimation

    Rainfal,Water level

    Data Entry & Processing Modelling & Mapping

    Dissemination

    to various agencies

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    Flood Warning Dissemination

    Weekly Dry Season

    Bulletin

    Daily Flood Bulletin Annual Flood Report

    pec a epor on y oo

    Report

    Mode of Dissemination

    E-Mail

    Fax Wireless Messenger

    WWW

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    Non Structural measures

    2. Response to the flood

    Preparedness for fighting Involvement of community

    Relief distribution among the victims

    Medical support

    Rehabilitation of flood victims

    Continued

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    Protection of vital infrastructure

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    Evacuated Flood Victims

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    Flood victims for relief and rescue

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    Non Structural measures

    2. Flood Damage Assessment

    Assessment of infrastructural loss

    Mobilizing resources for

    reconstruction and rehabilitation

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    Flood Management Cycle

    FloodEvent

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    Vulnerability Analysis Spatial Extent of Flood Inundation

    The spatial extent of the flood inundation is useful inidentifying the vulnerable regions

    Useful for damage assessment and identification of

    safe zones

    Flow velocity A significant parameter during high flows in steep

    slopes for risk assessment

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    Thanks for your attention andfor further uer :

    [email protected]