7.1.5
Storm Hydrographs
Hydrographs
Hydrographs
Hydrographs show how river discharges changes over time at a particular point in a river. Increased runoff leads to a reduced lag time and greater discharge, producing a steep hydrograph because more water gets into the river channel quicker.
![Illustrative background for content](https://image-v2.cdn.app.senecalearning.com/2018-04/9663bd22-31d9-437b-8007-43985ebf8479/3.3.6 hydrographs (1),h_400,q_80,w_640.png)
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![Illustrative background for River discharge](https://image-v2.cdn.app.senecalearning.com/2018-03/76e25e74-612f-42e8-9078-dc72eb606969/shutterstock_705361372,h_400,q_80,w_640.jpg)
![Illustrative background for River discharge ?? "content](https://image-v2.cdn.app.senecalearning.com/2018-03/76e25e74-612f-42e8-9078-dc72eb606969/shutterstock_705361372,h_400,q_80,w_640.jpg)
River discharge
River discharge
- River discharge is the volume of water flowing in a river each second and is measured in cumecs (m3/s).
![Illustrative background for Hydrographs](https://image-v2.cdn.app.senecalearning.com/2018-04/9663bd22-31d9-437b-8007-43985ebf8479/3.3.6 hydrographs (1),h_400,q_80,w_640.png)
![Illustrative background for Hydrographs ?? "content](https://image-v2.cdn.app.senecalearning.com/2018-04/9663bd22-31d9-437b-8007-43985ebf8479/3.3.6 hydrographs (1),h_400,q_80,w_640.png)
Hydrographs
Hydrographs
- Hydrographs show how river discharge changes over time at a particular point of a river. Hydrographs have the following features:
- Peak discharge: maximum discharge in the period of time.
- Peak rainfall: maximum rainfall in the period of time.
- Lag time: the interval between peak rainfall and discharge.
- Rising limb: when the discharge is rising.
- Falling limb: when the discharge is falling.
Physical Factors Affecting Storm Hydrographs
Physical Factors Affecting Storm Hydrographs
The following physical factors affect the shape of a hydrograph:
![Illustrative background for Size, shape and drainage density](https://image-v2.cdn.app.senecalearning.com/2018-08/d8bfe630-6b98-4a0b-bc56-c2b57745d51a/frozen-river-ice,h_400,q_80,w_640.jpg)
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Size, shape and drainage density
Size, shape and drainage density
- The larger the catchment area of the river basin, the higher the peak discharge but the longer the lag time.
- The more circular the catchment area shape, the shorter the lag time.
- Denser drainage networks transport water more efficiently, increasing the flow and peak discharge.
![Illustrative background for Rock type and soil](https://image-v2.cdn.app.senecalearning.com/2018-04/bee1ce77-8e79-4191-9c9d-cdb058944437/shutterstock_254308357,h_400,q_80,w_640.jpg)
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Rock type and soil
Rock type and soil
- If the rock and soil is permeable (i.e. Limestone), precipitation will be able to infiltrate and percolate which lengthens the lag time and reduces the peak discharge.
- Impermeable rocks and soils (i.e. clay) stop precipitation infiltrating so surface runoff increases. Lag time is reduced and peak discharge is increased in these circumstances.
- If the soil is fully saturated or frozen by antecedent conditions, there will not be any infiltration leading to increased surface runoff, increasing the peak discharge.
![Illustrative background for Relief and vegetation](https://image-v2.cdn.app.senecalearning.com/2018-03/b5510a7c-2618-43bc-bbbb-67713b73bd08/shutterstock_748106695,h_400,q_80,w_640.jpg)
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Relief and vegetation
Relief and vegetation
- The steeper the catchment of the river basin, the quicker the water reaches the river which increases peak discharge and reduces lag time.
- River catchments with high levels of vegetation will see high interception and evapotranspiration.
- Tree roots help to promote infiltration and results in catchments with more vegetation having a lower surface runoff, and reduced peak discharge.
Human Factors Affecting Storm Hydrographs
Human Factors Affecting Storm Hydrographs
The following are human factors that influence the peak discharge and the lag time of storm hydrographs:
![Illustrative background for Land use](https://image-v2.cdn.app.senecalearning.com/2018-03/5b23cad5-714a-4d84-bd17-2d68cc8cfc2b/shutterstock_160696304,h_400,q_80,w_640.jpg)
![Illustrative background for Land use ?? "content](https://image-v2.cdn.app.senecalearning.com/2018-03/5b23cad5-714a-4d84-bd17-2d68cc8cfc2b/shutterstock_160696304,h_400,q_80,w_640.jpg)
Land use
Land use
- Areas that remain forested or as their natural habitat will see reduced peak discharge due to an increase in infiltration and interception of precipitation by vegetation.
- There will be less interception in areas that have been deforested. This will increase the peak discharge.
- Ploughing of agricultural land increases surface runoff. This causes lag time to reduce and peak discharge to increase.
![Illustrative background for Urbanisation](https://image-v2.cdn.app.senecalearning.com/2018-08/2d70139b-877b-451f-9c9e-9d5d3c395baf/beijing-,h_400,q_80,w_640.jpg)
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Urbanisation
Urbanisation
- Urbanisation leads to an increase in the number of impermeable surfaces (tarmac, concrete and tiles).
- Impermeable surfaces lead to a decrease in infiltration, an increase in surface runoff and ultimately a reduction in the lag time. A shorter lag time means a greater peak discharge.
![Illustrative background for Water management](https://image-v2.cdn.app.senecalearning.com/2018-04/94c972e6-924d-4a32-9772-966dc3fa4c20/shutterstock_537334648,h_400,q_80,w_640.jpg)
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Water management
Water management
- Dams and reservoirs can be used to regulate the flow of the river by storing water and choosing when to release it downstream.
- Abstraction of aquifers lowers groundwater levels and increases percolation and infiltration when rainfall happens.
1Tectonic Processes & Hazards
1.1Tectonic Processes & Hazards
1.2Natural Disasters
1.3Natural Disaster Case Studies
1.4Trends & Patterns
2Option 2A: Glaciated Landscapes & Change
2.1Glaciated Landscapes Over Time
2.2Periglacial Landscapes
2.3Glacial Processes
2.4Glacial Landforms
3Option 2B: Coastal Landscapes & Change
3.1Coastal Landscapes
3.2Coastal Erosion & Deposition
3.3Coastal Risks
4Globalisation
4.1Globalisation
4.2Negatives of Globalisation
4.3Global Shift
4.5Culture
4.6Measuring Development
5Option 4A: Regenerating Places
5.1Types of Economies
5.2Function of Places
5.3Regeneration
5.4Regeneration Case Studies
6Option 4B: Diverse Places
6.1Population Structure
6.2Past & Present Connections
6.3Urban & Rural Spaces
6.4Diversity
6.5Urban & Rural Case Studies
6.6Case Study - Tower Hamlets
6.7Case Study - Sturton-le-Steeple
7The Water Cycle & Water Insecurity (A2 only)
7.1Hydrological Processes Global to Local
7.2Influences on the Water Cycle
7.3Water Insecurity
8The Carbon Cycle & Energy Security (A2 only)
8.1The Carbon Cycle
8.2Energy Consumption
8.3Alternative Energy
8.4Growing Demand for Resources
9Superpowers (A2 only)
9.1Superpowers
9.2Hard & Soft Power
9.2.1Hard & Soft Power
9.2.2Emerging Powers - China Rivalry
9.2.3Emerging Powers - Chinese Sources of Power
9.2.4Emerging Powers - Brazil
9.2.5Emerging Powers - Russia
9.2.6Emerging Powers - India
9.2.7Theories of Development
9.2.8Power Case Studies: Chinese One Belt One Road
9.2.9Power Case Studies: Pakistan Nuclear Arms
9.2.10Power Case Studies: OPEC
9.3IGOs, TNCs & Alliances
10Option 8A: Health & Human Rights (A2 only)
10.1Human Development
10.2Role of Governments & IGOs
10.3Human Rights
10.4Interventions
11Option 8B: Migration & Identity (A2 only)
11.1Globalisation & Migration
11.2Consequences of Migration
11.3Nation States
11.4Responses to Global Migration
Jump to other topics
1Tectonic Processes & Hazards
1.1Tectonic Processes & Hazards
1.2Natural Disasters
1.3Natural Disaster Case Studies
1.4Trends & Patterns
2Option 2A: Glaciated Landscapes & Change
2.1Glaciated Landscapes Over Time
2.2Periglacial Landscapes
2.3Glacial Processes
2.4Glacial Landforms
3Option 2B: Coastal Landscapes & Change
3.1Coastal Landscapes
3.2Coastal Erosion & Deposition
3.3Coastal Risks
4Globalisation
4.1Globalisation
4.2Negatives of Globalisation
4.3Global Shift
4.5Culture
4.6Measuring Development
5Option 4A: Regenerating Places
5.1Types of Economies
5.2Function of Places
5.3Regeneration
5.4Regeneration Case Studies
6Option 4B: Diverse Places
6.1Population Structure
6.2Past & Present Connections
6.3Urban & Rural Spaces
6.4Diversity
6.5Urban & Rural Case Studies
6.6Case Study - Tower Hamlets
6.7Case Study - Sturton-le-Steeple
7The Water Cycle & Water Insecurity (A2 only)
7.1Hydrological Processes Global to Local
7.2Influences on the Water Cycle
7.3Water Insecurity
8The Carbon Cycle & Energy Security (A2 only)
8.1The Carbon Cycle
8.2Energy Consumption
8.3Alternative Energy
8.4Growing Demand for Resources
9Superpowers (A2 only)
9.1Superpowers
9.2Hard & Soft Power
9.2.1Hard & Soft Power
9.2.2Emerging Powers - China Rivalry
9.2.3Emerging Powers - Chinese Sources of Power
9.2.4Emerging Powers - Brazil
9.2.5Emerging Powers - Russia
9.2.6Emerging Powers - India
9.2.7Theories of Development
9.2.8Power Case Studies: Chinese One Belt One Road
9.2.9Power Case Studies: Pakistan Nuclear Arms
9.2.10Power Case Studies: OPEC
9.3IGOs, TNCs & Alliances
10Option 8A: Health & Human Rights (A2 only)
10.1Human Development
10.2Role of Governments & IGOs
10.3Human Rights
10.4Interventions
11Option 8B: Migration & Identity (A2 only)
11.1Globalisation & Migration
11.2Consequences of Migration
11.3Nation States
11.4Responses to Global Migration
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