option A flood mitigation Flashcards
hydrograph elements
rising limb
peak flow/ discharge
lag time
run off curve
base flow
recessional limb
rising limb
-amount of discharge and speed at which its increasing
-(flash flood= very steep)
-generally steep in urbanised catchments
peak discharge
-higher in larger basins
-steep catchments- lower infiltration rates
- flat catchment- high infiltration rates so more through flow and lower peaks.
lag time
-time interval between peak rainfall and peak discharge
-influenced by basin shape, steep, stream order
runoff curve
-relationship between overland flow and throughflow
-low infiltration=high moisture, impremeable surface, strong rainfall, overland flow
base flow
-seepage of groundwater into the channel
-slow movement and main long term supply of river discharge
how does seasonal change impact (river regime)
- amount and nature of precipitation
-seasonal variations in temperature and evapotranspiration
-changes in vegetation cover
variations in rock, soil types and shape and size of basin
recurrence interval
frequency in which events of a certain size occur
catastrophe of flood
high magnitude but low frequency
urbanisation hydrological impact
-shorter lag time
-steeper rising limb
- higher peak flow
-steeper recessional limb
factors influencing flood risks
-precipitation type and intensity
- temperature+
evapotranspiration
-antecendent moisture
-size of basin
drainage density
rock and soil impermeability
-slopes
-vegetation type
-land use
how did urbinization increase flood risk
-creation of impermeable surfaces (roads, roofs, pavements)
-smooth surface served with dense network of drains gutters and underground swerves- increase in drainage density
-natural river channels often constricted by bridge supports or riverside facilities- reduce carrying capacity
impact of urbanisation on lower part of basin
- increased erosion.
- more water getting into rivers
increased speed of flow and transport of materials- enlarged channels
.less erosion due to riverbank protection schemes
deforestation
removal of tress and forest and their ecosystems
deforestation effects of hydrological cycle
-more overland flow leading to more frequent erosion
-rivers transporting more sediment
-reduced evapotranspiration