Flood Response Flashcards

1
Q

The basics

A
  • flow downhill under gravity
  • flow velocity moderated by frictional resistance and sediment transport controlled by flow velocity and velocity profile
  • flow depth can also vary significantly with channel cross-section and roughness
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2
Q

Flood Propagation

A

downstream flood peak and timing

  • if/when the flood will occur and how long the flood water is going to be there
  • raised deeper water overtakes shallower water
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3
Q

Catchment area

A
  • small catchments, response times are short

- as catchment area increase the range of travel times to channel outlet increases

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4
Q

Discharge

A
  • determined by climate (precipitation and evapotranspiration, and storage factors)
  • raised water level represents a disturbance which propagates down stream as a wave
  • a higher discharge may equal earlier peak and therefore flooding
  • higher discharge = higher rainfall
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5
Q

Speed/Velocity

A
  • raised water level/depth can be identified by the velocity of the flow, deeper the water, faster the flow
  • higher velocity = increased flood activity
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6
Q

Storage

A
  • zones of potential storage gives lags in channels and on floodplains
  • delays peak flow and reduces peak magnitude
  • weirs and flood control dams function as local reservoirs
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7
Q

Groundwater

A
  • all pores are filled with water
  • aquifers hold water
  • effects on overland flow, subsurface flow and groundwater flow
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8
Q

Cross sectional area

A
  • water depth, channel slope, resistance, roughness and disturbance
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9
Q

Hillslope

A
  • steep V-shaped valleys increase runoff and pathway to stream
  • infiltration may effect overland flow
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10
Q

Vegetation

A
  • intercept, store and transport water to subsurface
  • highly vegetated areas are going to take more time to reach the catchment
  • urbanised areas, impermeable rock will transport precipitation quicker through runoff
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11
Q

Tributries

A
  • collect all the water and transport it to the main stream

- more tributries = higher catchment rate

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12
Q

Boscastle Floods

A
  • prolonged heavy rainfall
  • deep V shaped valley upstream
  • impermeable surface in urban areas around catchment
  • 2 major tributries, Valancy and Jordon
  • reduction in trees and hedges
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