1.2.2 Drainage basins Flashcards

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1
Q

What is a drainage basin?

A

The area of land drained by a river and its tributaries.

This is also called local hydrological cycles.

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2
Q

What is the boundary of a drainage basin called?

A
  • The watershed.

Any precipitation falling beyond the watershed enters a different drainage basin.

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3
Q

Are drainage basins open or closed systems?

A

Open - they have inputs and outputs.

Water comes into the system as precipitation and leaves via evaporation, transpiration and river discharge.

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4
Q

Typical drainage basin system diagram

See reverse

A
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5
Q

Inputs in drainage basins

A
  • Precipitation
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6
Q

Outputs in drainage basins

A
  • Evaporation
  • Transpiration
  • Evapotranspiration
  • Channel flow (discharge)
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7
Q

Stores in drainage basins

A
  • Interception
  • Vegetation storage
  • Surface storage
  • Soil storage
  • Groundwater storage
  • Channel storage
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8
Q

Flows in drainage basins

A
  • Infiltration
  • Overland flow (surface runoff)
  • Throughfall
  • Stemflow
  • Throughflow
  • Percolation
  • Groundwater flow
  • Baseflow
  • Interflow
  • Channel flow (discharge)
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9
Q

[Inputs in drainage basins]

Precipitation

A

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.

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10
Q

[Stores in drainage basins]

Interception storage

A

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.

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11
Q

[Stores in drainage basins]

Vegetation storage

A

Water that’s been taken up by plants. It is all the water contained in plants at any one time.

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12
Q

[Stores in drainage basins]

Surface storage

A

Surface storage includes water in puddles, ponds and lakes.

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13
Q

[Stores in drainage basins]

Soil storage

A

Moisture in the soil.

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14
Q

[Stores in drainage basins]

Groundwater storage

A

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.

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15
Q

[Stores in drainage basins]

Channel storage

A

The water held in a river or stream channel.

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16
Q

[Outputs in drainage basins]

Evaporation

A

Water turning into water vapour.

17
Q

[Outputs in drainage basins]

Transpiration

A

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.

18
Q

[Outputs in drainage basins]

Evapotranspiration

A

The process of evaporation and transpiration together.

19
Q

[Outputs in drainage basins]

Channel flow (discharge)

A

The water flowing in the river or stream itself.

20
Q

[Flows in drainage basins]

Infiltration

A

Water soaking into the soil.

Infiltration rates are influenced by soil type, soil structure and how much water’s already in the soil.

21
Q

[Flows in drainage basins]

Overland flow (surface runoff)

A

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.

22
Q

[Flows in drainage basins]

Throughfall

A

Water dropping from one leaf (or part of a plant) to another.

23
Q

[Flows in drainage basins]

Stemflow

A

Water running down a plant stem or a tree trunk.

24
Q

[Flows in drainage basins]

Throughflow

A

Water moving slowly downhill through the soil.

It can happen through ‘pipes’ (either man-made or cracks in the soil/animal burrows).

25
Q

[Flows in drainage basins]

Percolation

A

Water seeping down through soil into the water table.

26
Q

[Flows in drainage basins]

Groundwater flow

A

Water flowing (slowly) below the water table through permeable rock. Water flows slowly through most rocks, but flows quickly through rocks that are highly permeable.

27
Q

[Flows in drainage basins]

Baseflow

A

Groundwater flow that feeds into rivers through river banks and river beds.

28
Q

[Flows in drainage basins]

Interflow

A

Water flowing downhill through permeable rock above the water table.

29
Q

[Flows in drainage basins]

Water balance

A

The balance between inputs (precipitation) and outputs (channel flow and evaporation).

The water balance affects how much water is stored in the basin.

30
Q

How do wet seasons affect the water balance?

A

In wet seasons, precipitation exceeds evapotranspiration. This creates a water surplus. The ground stores fill with water so there’s more surface runoff and higher discharge, so river levels rise.

31
Q

How do dry seasons affect the water balance?

A

In drier seasons, precipitation is lower than evapotranspiration. Ground stores are depleted as some water is used (e.g. by plants and humans) and some flows into the river channel, but isn’t replaced by precipitation.

So, at the end of the dry season, there is a deficit (shortage) of water in the ground. The ground stores are recharged in the next wet season (i.e. autumn).

32
Q

What do we call it when there is enough water?

A

A positive water balance (surplus).

33
Q

What do we call it when there is not enough water?

A

A negative water balance (deficit).

34
Q

Discharge

A

The ‘volume of water passing a measuring point in a given time’.

35
Q

What do river regimes show?

A

The variation in a river’s discharge over a year. They allow for comparison between different rivers.

36
Q

Water balance diagram

A