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Flooding is one of the most destructive natural hazards in the UK. This lesson examines the causes of river flooding, the factors that influence flood risk, and the strategies used to manage and reduce the impact of floods.
A river floods when its discharge (the volume of water flowing in the channel) exceeds the capacity of the channel. Water spills over the banks and onto the surrounding floodplain.
| Cause | Explanation |
|---|---|
| Prolonged rainfall | Extended periods of rain saturate the soil, reducing infiltration. Surface runoff increases, feeding more water into the river. |
| Intense rainfall | Heavy, short bursts of rain (convectional storms) produce more water than the ground can absorb. Surface runoff is rapid. |
| Snowmelt | A sudden thaw after prolonged cold weather releases large volumes of water into rivers very quickly. |
| Impermeable rock | Areas underlain by impermeable rocks (e.g., clay, granite) do not allow water to infiltrate. Surface runoff is high. |
| Steep slopes | Water runs off steep hillsides quickly, reaching the river channel faster. |
| Saturated soil | If the soil is already waterlogged from previous rainfall, additional rain cannot infiltrate and runs straight into the river. |
| Cause | Explanation |
|---|---|
| Urbanisation | Concrete, tarmac, and buildings create impermeable surfaces that prevent infiltration. Water runs off quickly into drains and rivers. |
| Deforestation | Removing trees reduces interception (trees catch rainfall on their leaves) and transpiration. More water reaches the ground surface and runs into rivers. |
| Agriculture | Ploughing compacts the soil, reducing infiltration. Field drains may channel water into rivers more quickly. |
| Climate change | Warmer temperatures lead to more evaporation, more moisture in the atmosphere, and potentially more intense rainfall events. |
| Building on floodplains | Construction on floodplains reduces the land available to absorb floodwater. |
Exam Tip: In exam answers about the causes of flooding, always give both physical and human causes. A top answer will explain how human activities increase the risk by speeding up the transfer of water from the land to the river.
A flood hydrograph (also called a storm hydrograph) shows how a river's discharge changes over time in response to a rainfall event.
| Feature | Definition |
|---|---|
| Peak discharge | The maximum discharge reached during the storm event |
| Peak rainfall | The point of maximum rainfall intensity |
| Lag time | The time delay between peak rainfall and peak discharge |
| Rising limb | The part of the graph showing discharge increasing as water enters the river |
| Falling limb (recession limb) | The part of the graph showing discharge decreasing after the peak |
| Base flow | The normal (background) discharge of the river between storms, fed by groundwater |
| Feature | Flashy Hydrograph | Flat Hydrograph |
|---|---|---|
| Peak discharge | High | Low |
| Lag time | Short | Long |
| Rising limb | Steep | Gentle |
| Falling limb | Steep | Gentle |
| Flood risk | High | Low |
| Typical conditions | Impermeable rock, urbanised area, steep slopes, deforested, saturated soil | Permeable rock, rural area, gentle slopes, forested, dry soil |
Exam Tip: A "flashy" hydrograph (high peak, short lag time) indicates high flood risk. When explaining a flashy hydrograph, always link to factors that speed up surface runoff: impermeable surfaces, steep slopes, lack of vegetation, saturated ground.
Hard engineering uses man-made structures to control or contain floodwater.
| Strategy | Description | Advantages | Disadvantages |
|---|---|---|---|
| Dams and reservoirs | A dam is built across a river, creating a reservoir behind it. Water is stored and released slowly, reducing peak discharge downstream. | Very effective at controlling flooding; reservoir provides water supply, recreation, and hydroelectric power | Very expensive (millions of pounds); floods a large area of land behind the dam; displaces communities; traps sediment |
| Channel straightening | Meanders are cut through to create a straighter, shorter channel. Water moves through the area more quickly. | Moves floodwater through towns quickly | Increases flood risk downstream (water arrives faster); removes natural habitats; can increase erosion |
| Embankments (artificial levees) | Raised earth or concrete banks are built along the river to increase the channel's capacity. | Relatively cheap; effective at containing floodwater | If breached, flooding is sudden and severe; can give a false sense of security; restrict access to the river |
| Flood relief channels | An artificial channel is built to divert excess water away from the main river during floods. | Effective at reducing flood risk in specific areas | Expensive; may transfer the flood problem elsewhere; takes up land |
| Flood barriers and gates | Moveable barriers that can be raised during flood events to prevent tidal or river flooding. | Very effective; can be opened/closed as needed | Very expensive (e.g., the Thames Barrier cost over £530 million) |
Soft engineering works with natural processes to reduce flood risk.
| Strategy | Description | Advantages | Disadvantages |
|---|---|---|---|
| Flood warnings and preparation | The Environment Agency monitors river levels and issues flood warnings to communities. | Saves lives; relatively cheap; allows people to prepare | Does not prevent flooding; relies on people taking action; may not give enough warning time |
| Floodplain zoning | Planning restrictions prevent building on floodplains. Different zones allow different land uses (e.g., parks and sports fields on the highest-risk areas). | Prevents new development in flood-risk areas; preserves natural floodplain | Difficult to apply to existing built-up areas; restricts development; politically unpopular |
| Afforestation | Planting trees in the upper catchment area to increase interception and transpiration, reducing surface runoff. | Cheap; natural; creates wildlife habitat; reduces soil erosion; absorbs CO₂ | Takes many years for trees to grow and become fully effective; may not prevent flooding in extreme events |
| River restoration | Returning the river to its natural state by removing man-made features (e.g., straightened channels, concrete banks), allowing the river to meander and reconnect with its floodplain. | Natural; creates wildlife habitat; stores floodwater on the floodplain; cheap to maintain | May increase local flooding in the restored area; takes time; requires land |
| Managed flooding | Allowing certain areas of the floodplain to flood deliberately during high-water events, reducing the flood peak downstream. | Effective at reducing peak discharge; can create wetland habitats | Loss of agricultural land; compensation must be paid to landowners |
| Sustainable drainage systems (SuDS) | Permeable surfaces, green roofs, swales, and ponds designed to slow the flow of surface water into rivers in urban areas. | Reduces surface runoff; relatively cheap; can be attractive; reduces pollution in rivers | Requires retrofitting in existing urban areas; may not cope with extreme events |
On 16 August 2004, the village of Boscastle in north Cornwall experienced a devastating flash flood.
| Type | Details |
|---|---|
| Physical | 75 mm of rain fell in 2 hours (a month's worth). The ground was already saturated from previous weeks of rain. The village sits at the confluence of the River Valency and River Jordan in a narrow, steep-sided valley, funnelling water into the village. |
| Human | Development on the floodplain had increased impermeable surfaces. The channel had been narrowed by buildings. A car park near the river acted as a dam when cars were swept into the river and blocked the channel. |
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