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Hydrographs and Flooding Simplified Revision Notes

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3.3.5 Hydrographs and Flooding

Hydrographs

infoNote

River discharge is volume of water flowing in a river per second. It's measured in cubic meters per second. Hydrographs show how discharge at a certain point in a river changes over time in relation to rainfall.

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Keywords:

  • Peak discharge:
  • Maximum amount of water held in the channel.
  • Peak rainfall:
  • Maximum amount of rainfall (millimeters).
  • Lag time:
  • Time taken between peak rainfall and peak discharge.
  • Rising limb:
  • Shows the increase in discharge on a hydrograph.
  • Falling limb:
  • Shows the return of discharge to normal/base flow on a hydrograph.
  • Base flow:
  • The normal discharge of the river.

Lag Time

Factors Influencing Lag Time

  • Size of drainage basin

  • Vegetation

  • Valley side steepness

  • Soil type

  • Short or Long Lag Time:

    • Influenced by factors such as vegetation.
    • No Vegetation: Water runs off into the river quicker, leading to a short lag time.
    • Plenty of Vegetation: Plants intercept rainfall, leading to a longer lag time. A short lag time means water reaches the river quickly, increasing flood risk.

Human & Physical Factors Affecting Flood Risk

Factors Affecting Flood Risk

Factors Affecting Flood Risk

  • Rainfall: After a long period of rain, the soil becomes saturated. Any further rain can't infiltrate, which increases runoff into rivers. This increases discharge, so flooding is more likely.

  • Trees: Trees intercept and rainwater, and also take up water from the ground. Cutting down trees therefore by deforestation increased the risk of floods.

  • Rock Type: Clay soils and some rocks are impermeable and don't allow water through and run off is increased.

  • Relief: If a river has steep sides, water will reach the river much quicker, increasing discharge and making flooding more likely.

  • Land Use: Buildings are often made from impermeable materials like concrete, as well as being surrounded by roads. Impermeable surfaces increase runoff and drains quickly take water to rivers.

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