1.A.4 - The Water Cycle Flashcards

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1
Q

What is a flood hydrograph?

A

Shows the change in discharge caused by a period of rainfall

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2
Q

What are flood hydrographs used for?

A
  • Find out discharge patterns/trends of a particular drainage basin
  • Help predict flooding events, therefore influence implementation of flood prevention measures
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3
Q

What is base flow?

A

the “normal” river level before a rainfall event

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4
Q

What does the rising limb show?

A

The discharge rising as storm enters the drainage basin.

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5
Q

What is peak discharge?

A

The highest flow in the channel for that event.

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6
Q

What is the lag time?

A

The time taken from the peak rainfall to the peak discharge

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7
Q

What does the receding limb show?

A

When the discharge begins to fall

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8
Q

Features of a flashy storm hydrograph

A
  • short lag time
  • steep rising limb
  • steep falling limb
  • high peak discharge
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9
Q

Features of a delayed storm hydrograph

A
  • long lag time
  • gentle rising limb
  • gentle falling limb
  • low peak discharge
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10
Q

Physical factors affecting storm hydrographs

A

The drainage basin’s slope/gradient - DBs with steep sides have a faster overland flow and therefore gets to the river more quickly, causing a higher discharge and short lag time. Results in flashy hydrograph

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11
Q

Physical factors affecting storm hydrographs

A

Rock type - if the soil or rock type in the river basin is impermeable, overland flow will be high as there will be less percolation and the soil will be saturated resulting in a shorter lag time -> flashy hydrograph.

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12
Q

Physical factors affecting storm hydrographs

A

Drainage basin area - large drainage basins catch more precipitation so have a higher peak discharge compared to a smaller basin. Larger DB = longer lag time. Larger DB = flashy

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13
Q

Human factors affecting storm hydrographs

A

Farming practices:
Exposed soil - after harvest, loose soil is washed into rivers which leads to the sedimentation of rivers. This results in less capacity in rivers so an increased flood risk.
Ploughing down slopes - furrows can act as small stream channels, increased runoff and shorter lag time, flashier hydrograph.

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14
Q

Human factors affecting storm hydrographs

A

Landuse change:
Concrete and tarmac surfaces - surfaces are impermeable so there is no infiltration and no throughflow. This means there is an increased runoff, increased flood risk
Deforestation - reduces interception rates so rainwater hits the surface directly, leading to saturated soils which results in rapid overland flowed more runoff. Increased flood risk.

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15
Q

Human factors affecting storm hydrographs - Water Abstraction

A

Happens when:
- high population density
- demand for food
- heavy industry
demand for water exceeds amount available during a certain period.
- low rainfall, high population density

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16
Q

Human factors affecting storm hydrographs - Water Abstraction

A
  • Boreholes take water from the groundwater store -> reduced
  • lowers the water table
  • reduced groundwater flow and through flow
  • long term drop in river levels
17
Q

Human factors affecting storm hydrographs - Water Abstraction

A
  • water taken directly from rivers
  • can be for drinking water
  • most taken for agriculture, irrigation
  • decreases discharge
  • increased runoff from farmland -> pollution