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GG3021: Rivers

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Discharge/Stage Forecast reliability is required ... of the underlying geology from 0.1 (Peat) to 0.8 (Carboniferous Limestone. ... – PowerPoint PPT presentation

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Title: GG3021: Rivers


1
GG3021 Rivers Landscape
  • Flood Prediction The Flood Ranger Game

2
Reading
  • 1. Jones, J.A (1997) Global Hydrology. Chapter 6.
    Longman
  • 2. Smith, K Ward,R (1998) Floods. Chapter 8.
    Wiley.
  • 3. Discovery Software Ltd (2003) FloodRanger
    Manual (Provided)

3
Flood Forecasts
  • Discharge/Stage Forecast reliability is required
  • Flood stage forecast Too Low gt avoidable
    damage
  • Flood Stage Forecast Too High gt Loss of
    credibility with
  • Vulnerable populations
  • Timing of flood Peak gt Estimates for evacuation
    time etc

4
Flood Forecasts
  • Input to catchment rain/snowmelt
  • Input to channel runoff
  • Conversion runoff volume to flow hydrograph
  • Routing of hydrograph to estimate Qpeak, Shape,
    inundation time as flood wave moves downstream.

5
Session 3 Flow Estimation
  • First attempts to estimate floods in 1840s and
    led to ..
  • The Rational method Flow Size linked to.
  • SIZE OF CATCHMENT (A)
  • RAINFALL INTENSITY (I)
  • A COEFFICIENT OF RUNOFF (c) (Integrates catchment
    variables such as infiltration rate, catchment
    resistance etc)
  • Q c x I x A
  • The Rational method is still a useful flood
    estimator but is VERY DEPENDENT on choice of
    RUNOFF COEFFICIENT.
  • Alternative methods today make use of EMPIRICAL
    relations between existing Flood Records and
    catchment variables sych as area, soil factors
    etc (Flood Estimation Handbook 1999)

6
Unit Hydrograph Method for catchment hydrograph
synthesis(Source J.A.A.Jones, 1997 Chapter 6))
7
-Estimating the flood hydrograph Unit Hydrographs
8
Simulation Models
  • Attempt to simulate real-world processes
    accurately.
  • LUMPED MODEL Treat the whole drainage basin as
    a homogenous whole.
  • SEMI-DISTRIBUTED MODELS Attempt to calculate
    flow conditions from sub-basins, which are
    treated as homogeneous within themselves.
  • DISTRIBUTED MODELS Whole basin is split into
    small areas (eg Grid net) and flows passed from
    one grid cell to another. Spatial and temporal
    variations built in.

9
Catchment Models- Flow routing(SourceShaw )
10
Estimating the flood hydrograph
11
Flood Hydrograph Formation Drainage net
variations due to sub-catchment lithology
(Source Smith Ward)
12
Types of Catchment runoff models(Source Jones,
1997)
13
Elements of Catchment simulation models Lumped
Distributed systems. (Source Jones, 1997)
14
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15
FLOW ROUTING Hydrodynamic Routing Models
  • Continuity Equation
  • DQ/ DX DA/Dt q 0, Q output discharge, A
    cross sectional area of the flow, q lateral
    inflow.
  • Combined with a momentum equation which relates
    rate of change in momentum to applied forces.
    This may be simplified to the manning roughness
    equation
  • N (roughness factor) R0.67S0.5 / V, where R
    hydraulic radius (Cross section area of
    flow/wetted perimeter) S channel gradient V
    mean velocity.
  • This simplification is called the KINEMATIC WAVE
    MODEL.

16
Hydrologic Routing Models
  • Based on the continuity equation and an
    empirical method used to cover momentum elements.
  • DS/Dt Qin Qout , Change in section storage
    input discharge output discharge.
  • Storage consists of that defined by input/output
    discharges (prism storage) and that defined by
    waves within the reach (wedge storage).

17
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18
Flood Propagation Elements of flood attenuation
due to floodplain storage
19
Flood Propagation Relationship of flood wave
velocity (Celerity) to stage.
20
FloodRanger
  • FloodRanger is a flood simulator.
  • Outcome of the Foresight Flood coastal defence
    project
  • 200 billion in assets and 1.7m households are in
    flood threatened locations.
  • The FloodRanger simualation is designed by
    Discovery Software Ltd.
  • AIM To inform understanding and debate about the
    underlying factors affecting risk from flooding.
  • Aimed at non-specialists as well as professionals.

21
FloodRanger Aims
  • To manage the flood risk in a virtual landscape
    over the period 2000-2100. Aim is to minimise
    risks of flooding
  • The Ranger can use Sea defences and River flood
    defence systems such as groynes, sea walls,
    managed retreat, beach replenishment, river flood
    walls, reservoirs, weirs, locks and demountables
  • The Ranger must also meet demands for new
    housing, industrial development and water demand
    to ensure political survival in a democracy.

22
Flood Ranger Economic Background
  • Two world futures scenarios are built in
  • 1. World Markets Future based on short term
    consumerism, globalisation of governance systems.
    Social values are materialistic with high
    consumption and mobility. Strong pressure to
    reduce taxes. Public opinion strongly influenced
    by economic success.
  • 2. Local Stewardship Furure based on community
    and conservation. Diverse political and economic
    systems at regional levels. Cooperative social
    values with high degree of environmental
    awareness. Large degree of public provision but
    hard to levy taxes for flood defence etc. Public
    opinion affected by successful regional economy
    and healthy environment.

23
FloodRanger Background
  • Climate Change Scenarios Based on Carbon
    emissions from UK Climate Impacts Programme 2002
    and the Hadley Climate Models.
  • 1. Low Medium Low Medium High High
  • 2. Climate Parameters in these scenarios include
    air temperature, winter upland precipitation
    winter lowland precipitation rainstorm events
    sea level rise and storm surges.
  • 3. Events are sampled randomly over a decade for
    1/5,1/10, 1/20, 1/30, 1/50, 1/75, 1/100, 1/150
    and 1/200 year events.

24
FloodRanger Background
  • Sea Level rise depends on climate scenario and
    adds to tidal height. Max value 1m for High
    emissions scenario.
  • Runoff controlled by permeability of the
    underlying geology from 0.1 (Peat) to 0.8
    (Carboniferous Limestone.
  • Drainage Net Created by accumulating flow from
    each grid square in the landscape elevation
    model. Flow follows steepest path to the sea.
  • Precipitation modified by altitude and
    north-south gradient. Input to each grid square.

25
FloodRanger background
  • Indicative Floodplain derived by using volume of
    accumulated water and distributed perpendicular
    to the flow of the river.
  • Indicators
  • Health of environment Area lost to building
    from SSSIs etc Length of new roads etc
    (Dependent on economic model chosen)
  • Public Opinion Based on unemployment, Housing
    need, insurance premiums, water demand unmet
    health of environment
  • Flood Risk
  • Insurance Premiums
  • Water Demand f(water demand of people, industry,
    agriculture. Figures depend on Economic scenario
  • Water Available depends on summer rainfall,
    reservoir capacity etc.
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