Water Lecture 3- Causes and Consequences of Flooding Flashcards
Is the amount of annual rainfall in the Uk increasing?
Yes
What is the physical basis of flooding?
Flow through saturated and unsaturated.
Name two not slow flows through soil.
Macropore flow
Pipeflow
What is macropore flow?
Due to root or animal activity(note crane fly larvae in image to right and earthworm in image below)
What is pipeflow?
Often occur naturally in peat or marl soils
Artificial drainage pipes are commonly found in agricultural soils in the UK
What are the 4 effects of catchment characteristics on controlling water flows into channels?
- Diffuse flows. Hillslope flows get faster as they get deeper (so we get more rapid runoff as the
amount of runoff increases) - Faster flows with steeper slopes (more rapid
runoff in steeper catchments) - Faster flows when the bed surface is smoother or less rough (so runoff is more rapid in urban areas compared to rural areas)
- Deeper and faster flows will start to form channels (rills and gullies), which are more efficient at moving water
What is the discharge equation?
Width x depth x velocity
Is water compressible?
No and so density is constant
What is discharge proportional to?
Mass
Q1 = Q2
Name two critical processes in drainage networks.
Flow accumulation
Flow attenuation
What is flow accumulation?
The process of accumulation leads to increases in flood wave peaks – addition of Q
What is flow attenuation?
The process of attenuation leads to decreases in flood wave peaks
(Attenuation is the inverse of conveyance)
Discuss an example of flow accumulation.
Scenario A – rain falls over entire catchment, so flow depends on catchment area. As flows
combine, Q increases with distance downstream - accumulation.
Discuss an example of flow attenuation.
Scenario B – rain just falls in channel headwaters – little inflow further downstream - attenuation
Downstream movement of water is slowed due to secondary circulation, friction, storage etc
What causes attenuation?
- Different timings of sub-catchment response
- Transfer of water to floodplains
- Momentum/energy loss within the water wave
What is Manning’s n?
Manning’s n is an empirical parameter that allows us to relate flow depth to velocity or discharge
What does increased roughness lead to?
Slower flow and then deeper flow.
What is velocity equation?
v = depth 2/2 slope 1/2 divided over manning’s n
Is attenuation carefully managed in rivers?
Attenuation is carefully managed
in rivers:
May be introduced immediately upstream of towns and cities to take the ‘tops’ of flood waves
May be used further upstream to slow flood waves (natural flood management)
What happens with flood defences which can cause problems?
If you defend a town/river by stopping water going onto the floodplain you locally reduce
attenuation
* → has the effect of increasing flood risk downstream
What does dredging involve?
Deepening of the river bed
What are pros of dredging?
Improve land drainage and flow conveyance
Improve navigation
Economic use for sand and gravel extraction
What are cons of dredging?
Can increase flooding downstream, not effective at reducing flood risk
Flow continuity/mass balance – floodplains cover large areas so channels would need to be much
deeper/wider to contain the same amount of flow
Cost:
* Scour and fill – short lived impact, need to repeat after each major flood
* Stabilization of bridges, culverts etc.
* Where to put dredged silt (may be contaminated)
Increase subsequent erosion (and thus siltation) by destabilizing banks
Disturbance of fish spawning grounds/other parts of ecosystem (and thus related ecosystem services)