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978-0-00-812422-9 COLLINS CAMBRIDGE AS AND A LEVEL GEOGRAPHY

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River groups

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figure 1.8 (a) Drainage patterns in France. The map shows the drainage basins colour coded to their respective graphs on the facing page.

Storm hydrographs

Hydrographs enable us to look at the relationship between rainfall and

discharge after each rainfall event as river levels top up and subsequently

drop over time. The response of a catchment to a rainfall event may be rapid

or gradual depending on many factors (outlined below). The shape of the

hydrograph may reflect the speed at which the water has travelled and the

obstacles and stores in its way.

Hydrographs are particularly important for identifying the potential risk of

flooding to an area.

There are several key features to any hydrograph. They represent the various

stages to the graph and help to identify the nature of the discharge. Most

hydrographs show time or duration on the x-axis followed by two scales on

the y-axis – one for the rainfall/precipitation and one for discharge. Be sure to

identify which is which.

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Hydrology and fluvial geomorphology

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