A.2.2 Factors affecting flood risk Flashcards
Why do floods occur?
Occurs when a river can no longer contain all the water it is transporting in its channel.
The water flows out of the channel onto a flood plain
Difference between small floods and larger floods
Most small floods are contained on the flood plain close to the river
Larger floods, which occur less often, cover a larger part of the flood plain
Recurrence interval
The frequency with which events of a certain size occur.
Very large events happen very infrequently, small events happen very frequently.
Urbanisation impact on hydrographs
Urban hydrographs are different from rural ones because there are more impermeable surfaces and drainage channels.
Urban hydrographs have:
- A shorter lag time
- A steeper rising limb
- A higher peak flow (discharge)
- A steeper recessional limb
Hydrological impact of urbanisation
Increases the magnitude and frequency of floods in at least three ways:
1. Creation of highly impermeable surfaces (e.g. roads, roofs, pavements)
- Smooth surfaces served with a dense network of drains, gutters and underground sewers increase drainage density
- Natural river channels are constricted by bridge supports or riverside facilities reducing their carrying capacity
Urbanisation impacts on hydrological processes
Increased erosion due to more water getting into rivers
Increased speed of flow and transport of materials due to enlarged channels
Less erosion due to riverbank protection schemes
Deforestation impact on hydrographs
Deforestation reduces interception, increases overland flow and reduces evapotranspiration.
Causes hydrographs to have shorter lag time and higher peak flows (discharge)
Hydrological impact of deforestation
Cause of increased flood run-off and decrease in channel capacity.
Occurs due to an increase in deposition within the channel.
Deforestation impacts on hydrological processes
- More overland flow leading to more frequent erosion
- Rivers transporting more sediment
- Reduced evapotranspiration
Channel modification impact on hydrographs
Channelisation may create new channels, which are likely to be quite straight. This speeds up water movement so time lags are likely to be reduced
Enlarging channels through levees enables rivers to carry more water, enabling rivers to carry more water. Thus the peak flow may be higher
Hydrological impact of deforestation
Widening and deepening of the channel increases the amount of water the river can hold
Straightening of the channel speeds up the flow and remove water from the area quickly
Removing sediment from a channelโs bed allows the river to carry more water, reducing the risk of flooding