Storm Hydrographs

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  • Storm Hydrographs
    • river discharge
      • volume of water flowing in a river each second and is measured in cumecs
    • peak discharge, peak rainfall
      • lag time - interval between the peaks
      • falling limb and rising limb
    • Physical Factors affecting Storm Hydrographs
      • large catchment - higher peak discharge but longer lag time
      • circular catchment area - shorter lag time
      • impermeable rocks - reduced lag time and increases peak discharge
      • steep catchment - increases peak discharge and reduces lag time
      • high vegetation - reduce discharge
    • human factors affecting storm hydrographs
      • deforested areas - increase peak discharge
      • impermeable surfaces means shorter lag time and greater peak discharge
      • dams and reservoirs regulate flow by storing water
      • abstraction of aquifers lowers ground water levels and increases percolation and infiltration

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