A.2.1: Hydrograph Characteristics Flashcards
Hydrographs
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
Rising limb
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
Peak flow or discharge
Higher in larger basins
Steep catchments have lower infiltration rates
Flat catchments have high infiltrates rates, so more throughflow and lower peaks
Lag time
Time interval between peak rainfall and peak discharge
Influenced by basin shape, steepness, stream order
Run-off curve
Illustrates relationship between overland flow and throughflow
If there is low infiltration, high antecedent moisture, impermeable surfaces and strong rainfall, overland flow will dominate
Base flow
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
Recessional limb
Influenced by geological composition and behaviour of local aquifers
Larger catchments have less-steep recessional limbs, likewise flatter areas
Hydrograph size (area under the graph)
The higher the rainfall, the greater the discharge
The larger the basin size, the greater the discharge
Influence of geology on hydrographs
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.
Influence of seasonality on hyrographs
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
Draw a hydrograph
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