flood risk and hydrographs Flashcards

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1
Q

describe the location of the River Tees:

A
  • north of England
  • source is located in the Pennines
  • flows east to its mouth, joins the North Sea
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2
Q

describe the River Tees in its upper course:

A
  • 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.
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3
Q

describe the River Tees in its middle course:

A
  • begins lateral erosion, forming meanders
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4
Q

describe the River Tees in its lower course:

A
  • 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.
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5
Q

what is river discharge?

A

the volume of water flowing in a river per second. (measured in cumecs)

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6
Q

what is the difference between water infiltration and percolation?

A

infiltration: water seeping from the surface into the soil.
percolation: water seeping from the soil into permeable rock.

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7
Q

what is the difference between streamflow, throughflow and groundwater flow?

A

streamflow: water flowing in the river channel.
throughflow: water flowing downhill through soil.
groundwater flow: water flowing through permeable rock.

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8
Q

how can surface run-off affect floodrisk?

A

surface run-off is rapid. if this is increased, the flood risk increases, as the river is likely to reach its bankfull capacity faster.

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9
Q

how can precipitation increase flood-risk?
(physical)

A

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

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10
Q

define ‘transpiration’:

A

evaporation of water from plants.

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11
Q

how can geology within the drainage basin increase flood risk?
(physical)

A
  • impermeable soil and rock doesn’t allow infiltration or percolation
  • increases surface run-off
  • increases river discharge
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12
Q

how can the relief of the drainage basin increase flood risk?
(physical)

A
  • 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.
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13
Q

how can urbanisation affect flood risk?
(human)

A
  • buildings and roads are made from impermeable material (e.g. concrete, tarmac)
  • reduces infiltration
  • increases surface run-off
  • increases river discharge
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14
Q

how can deforestation within the drainage basin increase flood risk?
(human)

A
  • removing trees reduces interception, vegetation storage and transpiration
  • increases the amount of precipitation that reaches the surface
  • increases surface run-off
  • increases river discharge
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15
Q

what is a hydrograph?

A

it shows how a river discharge (at a certain point within the river) changes overtime, in relation to precipitation.

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16
Q

what is lag time on a hydrograph?

A

the time delay between the peak rainfall and the peak discharge. there’s a delay because not all of the rain falls directly into the river channel. it will either flow over the surface (rapid) or flow underground (slower).

17
Q

what is the rising limb and falling limb on a hydrograph?

A

RISING LIMB:
- increase in river discharge as the rainwater enters the channel
- the steeper the line, the faster rainwater is entering

FALLING LIMB:
- the decrease in river discharge as the river returns back to normal (base flow)

18
Q

how can the relief of the drainage basin affect the hydrograph results?

A
  • steeper valleys will reduce infiltration and increase surface run-off
  • rainwater will reach the river channel faster, reducing the lag time
  • this will create a steeper rising limb and higher peak discharge
19
Q

how can the geology of the drainage basin affect the hydrograph results?

A
  • impermeable soils and rock will reduce infiltration/percolation and increase surface run-off
  • rainwater will reach the channel faster, reducing lag time
  • this will create a steeper rising limb and higher peak discharge
20
Q

how can urbanisation of the drainage basin affect the hydrograph results?

A
  • increasing buildings and roads increases impermeable surfaces
  • this will reduce infiltration and increase surface run-off
  • rainwater will reach the channel faster, reducing lag time
  • this will create a steeper rising limb and higher peak discharge
21
Q

how can deforestation of the drainage basin affect the hydrograph results?

A
  • removing trees reduces interception and transpiration
  • this increases surface run-off, as more rainwater reaches the surface
  • rainwater will reach the channel faster, reducing lag time
  • this will create a steeper rising limb and higher peak discharge