1.2.2 Drainage basins Flashcards
(36 cards)
What is a drainage basin?
The area of land drained by a river and its tributaries.
This is also called local hydrological cycles.
What is the boundary of a drainage basin called?
- The watershed.
Any precipitation falling beyond the watershed enters a different drainage basin.
Are drainage basins open or closed systems?
Open - they have inputs and outputs.
Water comes into the system as precipitation and leaves via evaporation, transpiration and river discharge.
Typical drainage basin system diagram
See reverse
Inputs in drainage basins
- Precipitation
Outputs in drainage basins
- Evaporation
- Transpiration
- Evapotranspiration
- Channel flow (discharge)
Stores in drainage basins
- Interception
- Vegetation storage
- Surface storage
- Soil storage
- Groundwater storage
- Channel storage
Flows in drainage basins
- Infiltration
- Overland flow (surface runoff)
- Throughfall
- Stemflow
- Throughflow
- Percolation
- Groundwater flow
- Baseflow
- Interflow
- Channel flow (discharge)
[Inputs in drainage basins]
Precipitation
Precipitation includes all the ways moisture comes out of the atmosphere. It is mainly rain, but it also includes other types, like snow, hail, dew and frost.
[Stores in drainage basins]
Interception storage
When precipitation lands on vegetation or other structures (e.g. buildings and concrete/tarmac surfaces) before it reaches the soil.
Interception store is only temporary because the collected water may evaporate quickly or fall from leaves are throughfall.
[Stores in drainage basins]
Vegetation storage
Water that’s been taken up by plants. It is all the water contained in plants at any one time.
[Stores in drainage basins]
Surface storage
Surface storage includes water in puddles, ponds and lakes.
[Stores in drainage basins]
Soil storage
Moisture in the soil.
[Stores in drainage basins]
Groundwater storage
Water stored in the ground in rocks.
The water table is the top surface of the zone of saturation – the zone of soil/rock where all the pores in the soil or rock are full of water. Porous rocks that can hold water are called aquifers.
[Stores in drainage basins]
Channel storage
The water held in a river or stream channel.
[Outputs in drainage basins]
Evaporation
Water turning into water vapour.
[Outputs in drainage basins]
Transpiration
Transpiration is evaporation from within leaves – plants and trees take up water through their roots and transport it to their leaves where it evaporates into the atmosphere.
[Outputs in drainage basins]
Evapotranspiration
The process of evaporation and transpiration together.
[Outputs in drainage basins]
Channel flow (discharge)
The water flowing in the river or stream itself.
[Flows in drainage basins]
Infiltration
Water soaking into the soil.
Infiltration rates are influenced by soil type, soil structure and how much water’s already in the soil.
[Flows in drainage basins]
Overland flow (surface runoff)
Water flowing over the land.
It can flow over the whole surface or in channels. It happens because rain is falling on the ground faster than infiltration can occur.
[Flows in drainage basins]
Throughfall
Water dropping from one leaf (or part of a plant) to another.
[Flows in drainage basins]
Stemflow
Water running down a plant stem or a tree trunk.
[Flows in drainage basins]
Throughflow
Water moving slowly downhill through the soil.
It can happen through ‘pipes’ (either man-made or cracks in the soil/animal burrows).