Flooding - the discharge of a river exceeds the capacity of the river’s channel
the river overflows and covers the adjacent floodplaiin
heavy rainfall is the cause of most floods
Storm hydrograph - shows how quickly a river responds to a rainfall event
water can reach the river by overland flow, throughflow and groundwater flow
A) lag time
B) peak flow
C) rising
D) recession
E) overland flow
F) throughflow
G) base flow
The shorter the lag time and the steeper the rising limb, the quicker the water reaches the river and the greater the chance of flooding
the shape of storm hydrographs vary between river drainage basins and are useful for planning against future flooding and times of drough
Discharge - the volume of water passing a measuring point or gauging station in a given time, measured in cubic metres per second
Lag time - the time difference between peak rainfall and peak discharge
Infiltration capacity - the maximum rate that water enters soil
Antecedent soil moisture - the amount of moisture present in the soil before a rainfall event
Impermeable - does not allow water to pass through
Percolation - the vertical movement of water from the soil into the underlying rock
Interception - the proess which vegetation prevents rainfall from reaching the surface direcltly
intercepted rainfall temporarily heldd as interception storage and then either falls temporarily heldd as interception storage
water either falls directly to the ground or is evaporated back to the atmosphere
Causes of flooding (1)
Weather
heavy, intense rainfall can exceed the infiltration capacity of the soil and lead to an increase in overland flow
stead, prolonger rainfall can saturate the soil and cause the water table to rise, reducing infiltration capacity
overland flow will occur if snowmelt is rapid and the ground beneath is frozen
Previous weather
antecedent soil moisture refers to the amount of water in the soil before a rainfall event
the more saturated the soil the less infiltration and the more overland flow
Causes of flooding (2)
Soil and rock type - impermeable soils and rocks e.g. clay or granite, have a low infiltration capacity and percolation rate which leads to greater overland flow
Relief - steeper gradients can lead to faster overland flow and water has little time to infiltrate
Earthquakes, volcanoes and tropical cyclones - natural hazards can produce tsunamis and storm surges that flood low-lying coastal areas
Deforestation - cutting down trees reduce interception and infiltration
Causes of flooding (3)
Urbanisation - concrete and tarmac are impermeable surfaces that lead to more overland flow
storm drains speed up the movement of water to the nearest river
Agriculture
overgrazing and leaving soil exposed reduces interception
ploughing down rather than across slopes quickly channels the water downwards
heavy farm machinery compacts the soil, making it impermeable
Climate change - enhahnced global warming may lead to a rise in sea-levels as well as more rainfall and storms in certain parts of the world