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Flooding in drainage basinsHydrographs

Flooding is a major issue in drainage basins in Wales, the UK and around the world. This section will explore what a drainage basin is, what processes operate in a drainage basin and why flooding occurs. It will also look at the effects of flooding in one UK location, and what can be done to manage and reduce the threat of future flooding.

Part of GeographyLandscapes and physical processes

Hydrographs

A hydrograph shows how a river is affected by a storm. This helps to understand discharge patterns of a particular drainage basin and helps to predict flooding and plan flood prevention measures.

As you can see in the graph below, the peak rainfall is the time of highest rainfall. The peak discharge is the time when the river reaches its highest flow. There is a delay because it takes time for the water to find its way to the river. This is called lag time.

A typical hydrograph with a bar chart showing precipitation, and a line graph of run-off.

The normal (base) flow of the river starts to rise when run-off, ground and soil water reaches the river. This is shown on the hydrograph as the rising limb.

The falling limb shows that water is still reaching the river but in decreasing amounts. The run-off/discharge of the river is measured in cumecs - this stands for cubic metres per second. is measured in mm - this stands for millimetres.

Storm Hydrograph.