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Rivers, floods and management

Rivers, floods
and management
Rivers, floods and management

The drainage basin hydrological cycle
Rivers, floods and management
River discharge
The storm hydrograph
Rivers, floods and management
River discharge
What factors might result in a ‘flashy’ hydrograph?
• short-lived but intense rainfall
• impermeable underlying rock such
as granite
• steep relief
• urban area, where water is
channelled through drains to the
stream
• small round drainage basin
Rivers, floods and management
River discharge
What factors might create a hydrograph like this?
• dense woodland vegetation
• high infiltration capacity of soil
• permeable underlying rock, such as
limestone
• elongated drainage basin
Rivers, floods and management

The long profile
Rivers, floods and management

The Hjülstrom curve
Rivers, floods and management

Amanda Barker

An upper course channel
Rivers, floods and management

Amanda Barker

A middle course channel
Rivers, floods and management

Amanda Barker

A lowland channel in flood
Rivers, floods and management

High Force waterfall
• vertical erosion
(by hydraulic action
and corrasion)
below the waterfall
deepens the plunge
pool

the resistant Whin
Sill and results in
headward erosion

John Pallister

• undercutting of the
softer rock leads to
eventual collapse of
Rivers, floods and management

The development of an oxbow lake
Rivers, floods and management

Reasons for formation of a delta
• the sediment load carried by the river is substantial
• the river has a large drainage basin
• the mouth of the river is located on a coastline where ocean currents and
tides are weak so the rate of deposition exceeds the rate of sediment
removal
Rivers, floods and management

Features related to rejuvenation
• knick points, rapids and
waterfalls
• river terraces

The city of Durham is built inside
an entrenched meander

Aerofilms

• incised meanders, both
entrenched and ingrown
Rivers, floods and management
Flooding
Physical causes of flooding
• excessive precipitation over
a long period of time

• the nature of the drainage
basin

• intensive precipitation over
a short period of time

• relief

• snowmelt

• natural vegetation

• climatic hazards such as
hurricanes

• rock and soil type
Rivers, floods and management
Flooding
Influence of human activities on flooding
• Urbanisation creates impermeable surfaces so reducing infiltration.
Surface water is therefore transported more rapidly through drains to
the river.
• Deforestation reduces interception and increases runoff.
• Some methods of river management, such as channelisation, increase
flood risk downstream.
• Global warming leads to more extreme rainfall events.
Rivers, floods and management
Flooding
Areas of high flood risk in England and Wales
Rivers, floods and management
Flooding
Responses to flooding
Short-term responses:

Long-term responses:

• media broadcasts of information

• government and/or foreign aid

• emergency relief, rescue, shelter,
food

• disaster planning for the future

• armed services for evacuation and
building emergency defences

• flood management programmes
Rivers, floods and management
Flooding
Examples of hard engineering
• channelisation, to raise, straighten or strengthen banks
• dams and weirs
• diversion channels
• dredging
• retention basins and balancing lakes
• artificially raising the height of the floodplain
Rivers, floods and management
Flooding
Examples of soft engineering
• afforestation
• floodplain zoning
• land-use management, e.g. contour ploughing
• wetland and riverbank conservation
• river restoration
• improved forecasting and warning

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River presentation

  • 1. Rivers, floods and management Rivers, floods and management
  • 2. Rivers, floods and management The drainage basin hydrological cycle
  • 3. Rivers, floods and management River discharge The storm hydrograph
  • 4. Rivers, floods and management River discharge What factors might result in a ‘flashy’ hydrograph? • short-lived but intense rainfall • impermeable underlying rock such as granite • steep relief • urban area, where water is channelled through drains to the stream • small round drainage basin
  • 5. Rivers, floods and management River discharge What factors might create a hydrograph like this? • dense woodland vegetation • high infiltration capacity of soil • permeable underlying rock, such as limestone • elongated drainage basin
  • 6. Rivers, floods and management The long profile
  • 7. Rivers, floods and management The Hjülstrom curve
  • 8. Rivers, floods and management Amanda Barker An upper course channel
  • 9. Rivers, floods and management Amanda Barker A middle course channel
  • 10. Rivers, floods and management Amanda Barker A lowland channel in flood
  • 11. Rivers, floods and management High Force waterfall • vertical erosion (by hydraulic action and corrasion) below the waterfall deepens the plunge pool the resistant Whin Sill and results in headward erosion John Pallister • undercutting of the softer rock leads to eventual collapse of
  • 12. Rivers, floods and management The development of an oxbow lake
  • 13. Rivers, floods and management Reasons for formation of a delta • the sediment load carried by the river is substantial • the river has a large drainage basin • the mouth of the river is located on a coastline where ocean currents and tides are weak so the rate of deposition exceeds the rate of sediment removal
  • 14. Rivers, floods and management Features related to rejuvenation • knick points, rapids and waterfalls • river terraces The city of Durham is built inside an entrenched meander Aerofilms • incised meanders, both entrenched and ingrown
  • 15. Rivers, floods and management Flooding Physical causes of flooding • excessive precipitation over a long period of time • the nature of the drainage basin • intensive precipitation over a short period of time • relief • snowmelt • natural vegetation • climatic hazards such as hurricanes • rock and soil type
  • 16. Rivers, floods and management Flooding Influence of human activities on flooding • Urbanisation creates impermeable surfaces so reducing infiltration. Surface water is therefore transported more rapidly through drains to the river. • Deforestation reduces interception and increases runoff. • Some methods of river management, such as channelisation, increase flood risk downstream. • Global warming leads to more extreme rainfall events.
  • 17. Rivers, floods and management Flooding Areas of high flood risk in England and Wales
  • 18. Rivers, floods and management Flooding Responses to flooding Short-term responses: Long-term responses: • media broadcasts of information • government and/or foreign aid • emergency relief, rescue, shelter, food • disaster planning for the future • armed services for evacuation and building emergency defences • flood management programmes
  • 19. Rivers, floods and management Flooding Examples of hard engineering • channelisation, to raise, straighten or strengthen banks • dams and weirs • diversion channels • dredging • retention basins and balancing lakes • artificially raising the height of the floodplain
  • 20. Rivers, floods and management Flooding Examples of soft engineering • afforestation • floodplain zoning • land-use management, e.g. contour ploughing • wetland and riverbank conservation • river restoration • improved forecasting and warning