7.1.2
Drainage Basin Hydrological Cycle
Hydrological Cycle in a Drainage Basin
Hydrological Cycle in a Drainage Basin
The hydrological cycle doesn't just work at a global level - this cycle also works in smaller, open systems such as in drainage basins. The main features of the drainage basin hydrological cycle are:
![Illustrative background for Inputs into drainage basins](https://image-v2.cdn.app.senecalearning.com/courseImages/chemistry/10.4.1 The Haber process/clouds-2329680_640-min,h_400,q_80,w_640.jpg)
![Illustrative background for Inputs into drainage basins ?? "content](https://image-v2.cdn.app.senecalearning.com/courseImages/chemistry/10.4.1 The Haber process/clouds-2329680_640-min,h_400,q_80,w_640.jpg)
Inputs into drainage basins
Inputs into drainage basins
- There are three types of precipitation that input into a drainage basin:
- Orographic - when air masses rise over mountains causing it to condense and rain.
- Frontal - when two air masses meet at an area of low pressure creating rain.
- Convectional - rainfall caused by water turning to water vapour due to solar radiation.
![Illustrative background for Outputs from drainage basins](https://image-v2.cdn.app.senecalearning.com/courseImages/chemistry/10.1.1 Potable water/lake-2063957_640-min,h_400,q_80,w_640.jpg)
![Illustrative background for Outputs from drainage basins ?? "content](https://image-v2.cdn.app.senecalearning.com/courseImages/chemistry/10.1.1 Potable water/lake-2063957_640-min,h_400,q_80,w_640.jpg)
Outputs from drainage basins
Outputs from drainage basins
- The water processes we identify as outputs in a drainage basin are:
- Evaporation - when water turns to water vapour and leaves the drainage basin.
- Transpiration - when water leaves plants through holes in their leaves.
- Channel flow - the volume of water that is flowing in a river channel.
![Illustrative background for Flows](https://image-v2.cdn.app.senecalearning.com/courseImages/chemistry/10.1.1 Potable water/rain-122691_640-min,h_400,q_80,w_640.jpg)
![Illustrative background for Flows ?? "content](https://image-v2.cdn.app.senecalearning.com/courseImages/chemistry/10.1.1 Potable water/rain-122691_640-min,h_400,q_80,w_640.jpg)
Flows
Flows
- The drainage basin hydrological cycle includes the following water flows:
- Interception - when plants capture precipitation in their leaves.
- Infiltration - when precipitation enters into the soil.
- Direct runoff - when water from precipitation or snowmelt flows across the ground’s surface because the surface is impermeable i.e. tarmac.
![Illustrative background for More flows](https://image-v2.cdn.app.senecalearning.com/courseImages/chemistry/10.1.1 Potable water/nature-landscape-stream-waterfall-395711-min,h_400,q_80,w_640.jpeg)
![Illustrative background for More flows ?? "content](https://image-v2.cdn.app.senecalearning.com/courseImages/chemistry/10.1.1 Potable water/nature-landscape-stream-waterfall-395711-min,h_400,q_80,w_640.jpeg)
More flows
More flows
- The following are also flows that happen in a drainage basin:
- Saturated overland flow - when the ground is full of water, resulting in runoff.
- Throughflow - the horizontal flow of water through soil/rock layers.
- Percolation - the vertical flow of water between soil and rock layers.
- Groundwater flow - the flow of water horizontality once it has reached the water table.
Physical Factors Affecting Drainage Basins
Physical Factors Affecting Drainage Basins
There are physical components that can impact the relative inputs, flows and outputs of a drainage basin.
![Illustrative background for Climate](https://image-v2.cdn.app.senecalearning.com/2018-04/236beac5-76db-428d-b3dc-19adb4f452d4/AdobeStock_84598705,h_400,q_80,w_640.jpeg)
![Illustrative background for Climate ?? "content](https://image-v2.cdn.app.senecalearning.com/2018-04/236beac5-76db-428d-b3dc-19adb4f452d4/AdobeStock_84598705,h_400,q_80,w_640.jpeg)
Climate
Climate
- Where cold climates allow for precipitation to fall as snow, the water can be stored and held back until it is thawed (melted).
- This may reduce the channel flow during the winter but lead to an increase during the spring and summer months due to glacial melt water.
![Illustrative background for Soil type](https://image-v2.cdn.app.senecalearning.com/courseImages/biology/1.1.4/rake-2915742_640 (1)-min,h_400,q_80,w_640.jpg)
![Illustrative background for Soil type ?? "content](https://image-v2.cdn.app.senecalearning.com/courseImages/biology/1.1.4/rake-2915742_640 (1)-min,h_400,q_80,w_640.jpg)
Soil type
Soil type
- Impermeable soils can stop infiltration and lead to surface saturation resulting in increased surface runoff.
- Where there are permeable soils, infiltration and percolation can happen. This can cause groundwater to recharge.
![Illustrative background for Vegetation cover](https://image-v2.cdn.app.senecalearning.com/courseImages/biology/4.1.1 Photosynthesis/forest-2960091_640-min,h_400,q_80,w_640.jpg)
![Illustrative background for Vegetation cover ?? "content](https://image-v2.cdn.app.senecalearning.com/courseImages/biology/4.1.1 Photosynthesis/forest-2960091_640-min,h_400,q_80,w_640.jpg)
Vegetation cover
Vegetation cover
- When an area has a high coverage of vegetation, the interception and evapotranspiration increases but the surface runoff decreases.
![Illustrative background for Relief of the land](https://image-v2.cdn.app.senecalearning.com/memory-location-images/Davos, Switzerland-min,h_400,q_80,w_640.jpg)
![Illustrative background for Relief of the land ?? "content](https://image-v2.cdn.app.senecalearning.com/memory-location-images/Davos, Switzerland-min,h_400,q_80,w_640.jpg)
Relief of the land
Relief of the land
- Steeper slopes mean faster surface runoff and shorter times for water storage.
![Illustrative background for Rock type](https://image-v2.cdn.app.senecalearning.com/2018-08/c1080a93-81ad-4aa5-8ea0-ec3e8ecffdab/caves-water-underground-rocks-,h_400,q_80,w_640.jpg)
![Illustrative background for Rock type ?? "content](https://image-v2.cdn.app.senecalearning.com/2018-08/c1080a93-81ad-4aa5-8ea0-ec3e8ecffdab/caves-water-underground-rocks-,h_400,q_80,w_640.jpg)
Rock type
Rock type
- Some rocks are impermeable and can stop the infiltration of water into the ground. Similarly to impermeable soils, these types of rocks can cause the ground to saturate and lead to surface runoff and increase flows in rivers.
- In contrast, permeable rocks allow for infiltration and percolation to happen.
Human Factors Affecting Drainage Basins
Human Factors Affecting Drainage Basins
Humans can impact the inputs, outputs, flows and stores of water in a drainage basin.
![Illustrative background for Over-abstraction](https://image-v2.cdn.app.senecalearning.com/courseImages/biology/2.5.2 - Plant tissues 2/water-drop-275938_640-min,h_400,q_80,w_640.jpg)
![Illustrative background for Over-abstraction ?? "content](https://image-v2.cdn.app.senecalearning.com/courseImages/biology/2.5.2 - Plant tissues 2/water-drop-275938_640-min,h_400,q_80,w_640.jpg)
Over-abstraction
Over-abstraction
- Abstraction is the process by which humans remove water from underground water stores (e.g. aquifers).
- Over-abstraction is when the volume of water being removed is greater than the volume of groundwater being replenished.
- Over-abstraction can lead to rivers drying up during periods of low rainfall.
![Illustrative background for Deforestation](https://image-v2.cdn.app.senecalearning.com/2018-04/a940f043-76a6-4019-a232-08f66c019d21/shutterstock_520269400,h_400,q_80,w_640.jpg)
![Illustrative background for Deforestation ?? "content](https://image-v2.cdn.app.senecalearning.com/2018-04/a940f043-76a6-4019-a232-08f66c019d21/shutterstock_520269400,h_400,q_80,w_640.jpg)
Deforestation
Deforestation
- Deforestation is the term used to describe the removal of trees. The impact of deforestation reduces interception and consequently, rainfall strikes soil directly, leading to soil compaction.
- Soil compaction and the removal of tree roots can reduce infiltration.
- Ultimately deforestation causes an increase in surface runoff, resulting in more soil erosion and flooding.
![Illustrative background for Urbanisation](https://image-v2.cdn.app.senecalearning.com/memory-location-images/New York, USA-min,h_400,q_80,w_640.jpg)
![Illustrative background for Urbanisation ?? "content](https://image-v2.cdn.app.senecalearning.com/memory-location-images/New York, USA-min,h_400,q_80,w_640.jpg)
Urbanisation
Urbanisation
- Urbanisation is a change of land use that results in moving away from the natural environment to towns and cities.
- Urbanisation leads to a large number of impermeable surfaces i.e. tarmac, slate, concrete. These impermeable surfaces reduce infiltration, whilst increasing surface runoff.
![Illustrative background for Reservoirs](https://image-v2.cdn.app.senecalearning.com/courseImages/physics/1.5.2 - Energy resources/hydroelectric-dam-min,h_400,q_80,w_640.jpg)
![Illustrative background for Reservoirs ?? "content](https://image-v2.cdn.app.senecalearning.com/courseImages/physics/1.5.2 - Energy resources/hydroelectric-dam-min,h_400,q_80,w_640.jpg)
Reservoirs
Reservoirs
- Reservoirs are man-made stores that disrupt the natural water flow, by delaying the flow and increasing water lost from evaporation.
- Dams reduce the water flow further downstream resulting in loss of vegetation.
- When vegetation grows on the reservoir’s surface, an increase in evapotranspiration happens and in turn increase in salinity of the water.
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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