A.2.1: Hydrograph Characteristics Flashcards

1
Q

Hydrographs

A

Shows how a river channel responds to the key processes of the hydrological cycle

Measures the speed at which rain falling on a drainage basin reaches the river channel

Graph of river discharge plotted against time

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2
Q

Rising limb

A

Indicates amount of discharge and the speed at which it is increasing

Very steep in a flash flood or in small drainage basins where the response is rapid

Generally steep in urbanised catchments

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3
Q

Peak flow or discharge

A

Higher in larger basins

Steep catchments have lower infiltration rates

Flat catchments have high infiltrates rates, so more throughflow and lower peaks

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4
Q

Lag time

A

Time interval between peak rainfall and peak discharge

Influenced by basin shape, steepness, stream order

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5
Q

Run-off curve

A

Illustrates relationship between overland flow and throughflow

If there is low infiltration, high antecedent moisture, impermeable surfaces and strong rainfall, overland flow will dominate

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6
Q

Base flow

A

The seepage of groundwater into the channel - very important where rocks have high pore space

A slow movement, and the main, long-term supplier of the river’s discharge

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7
Q

Recessional limb

A

Influenced by geological composition and behaviour of local aquifers

Larger catchments have less-steep recessional limbs, likewise flatter areas

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8
Q

Hydrograph size (area under the graph)

A

The higher the rainfall, the greater the discharge

The larger the basin size, the greater the discharge

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9
Q

Influence of geology on hydrographs

A

Different rock types and structures influence how quickly rainwater reaches the river channel.

Impermeable rocks (and soils) generate more overland flow, so a shorter lag time and a higher peak flow

Permeable surfaces allow more water to percolate through the ground, leading to a more moderated and delayed river response.

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10
Q

Influence of seasonality on hyrographs

A

Variations in a river’s flow depend on:
- The amount and nature of precipitation
- Seasonal variations in temperature and evapotranspiration
- Changes in vegetation cover
- Variations in rock types, soil types and the shape and size of the drainage basin

Seasonal changes in climate generally have the greatest impact on changes in river flow

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11
Q

Draw a hydrograph

A

Check book

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