flood risk and hydrographs Flashcards
describe the location of the River Tees:
- north of England
- source is located in the Pennines
- flows east to its mouth, joins the North Sea
describe the River Tees in its upper course:
- hard, impermeable rocks
- vertical erosion formed a v-shaped valley
- ‘High Force’, UK’s largest waterfall (by volume, when in full force), is located in the Tees’ upper course.
- band of hard rock (whinstone) is located above an area of soft rock (sandstone and shale), creating the waterfall.
describe the River Tees in its middle course:
- begins lateral erosion, forming meanders
describe the River Tees in its lower course:
- the meanders are much larger, oxbow lakes have formed
- there are also levees, which have formed when the river has previously flooded
- has a large estuary, with mudflats and sandbanks, supporting wildlife in the area.
what is river discharge?
the volume of water flowing in a river per second. (measured in cumecs)
what is the difference between water infiltration and percolation?
infiltration: water seeping from the surface into the soil.
percolation: water seeping from the soil into permeable rock.
what is the difference between streamflow, throughflow and groundwater flow?
streamflow: water flowing in the river channel.
throughflow: water flowing downhill through soil.
groundwater flow: water flowing through permeable rock.
how can surface run-off affect floodrisk?
surface run-off is rapid. if this is increased, the flood risk increases, as the river is likely to reach its bankfull capacity faster.
how can precipitation increase flood-risk?
(physical)
PROLONGED RAINFALL:
- saturates the soil
- reduces infiltration
- increases surface run-off
- increases river discharge
INTENSE, SUDDEN RAINFALL:
- infiltration doesn’t occur fast enough
- increases surface run-off
- increases river discharge
define ‘transpiration’:
evaporation of water from plants.
how can geology within the drainage basin increase flood risk?
(physical)
- impermeable soil and rock doesn’t allow infiltration or percolation
- increases surface run-off
- increases river discharge
how can the relief of the drainage basin increase flood risk?
(physical)
- steep valley sides means that infiltration will not occur fast enough
- increases surface run-off due to gravity
- increases river discharge
- however, low-lying areas are also at risk. the gradient is not steep enough to remove flood water.
how can urbanisation affect flood risk?
(human)
- buildings and roads are made from impermeable material (e.g. concrete, tarmac)
- reduces infiltration
- increases surface run-off
- increases river discharge
how can deforestation within the drainage basin increase flood risk?
(human)
- removing trees reduces interception, vegetation storage and transpiration
- increases the amount of precipitation that reaches the surface
- increases surface run-off
- increases river discharge
what is a hydrograph?
it shows how a river discharge (at a certain point within the river) changes overtime, in relation to precipitation.