1.1.2 Flood Hydrographs Flashcards
Flood hydrographs…
represent rainfall for drainage basin of a river and the discharge of the river
Discharge
volume of water passing through a cross-sectional point of a river over time. Measured in cubic metres per second (cumecs). Made of baseflow + stormflow
Features of flood hydrograph
Rising limb, falling limb, bankfull discharge, lag time, stormflow, baseflow
Axes of flood hydrograph
x - time, y - discharge (cumecs) & rainfall (mm/hr)
Rising limb
Line showing discharge increasing
Falling limb
Line showing discharge decreasing
Lag time
Time between peak rainfall and peak discharge
Baseflow
Level of groundwater flow
Stormflow
Overland flow + throughflow
Bankfull discharge
Max capacity of river. After this the river banks will burst causing flooding
Features of a flashy hydrograph
short lag time
high peak discharge
Steep limbs
Higher flood risk
Features of a subdued hydrograph
Longer lag time
Low peak discharge
Gradual limbs
Lower flood risk
Natural causes of flashy hydrographs
High rainfall intestity, antecedent rain (rain prior to event being measured), impermeable rock, high drainage (many tributaries), small, circular, or steep basin, precipitation type (snow increases lag time)
Human causes of flashy hydrographs
Urbanisation, pastoral farming, deforestation