What is a drainage basin? How is it different to the global hydrological cycle? Flashcards

1
Q

What is a drainage basin?

A

An area of land drained by a river and its tributaries (river system).

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2
Q

What kind of systems are drainage basins?

A

local open systems

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3
Q

How are drainage basins cascading systems?

A

One drainage basin’s outputs are the inputs to another.

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4
Q

What is a watershed?

A

A ridge of high land separating drainage basins.

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5
Q

What is a river?

A

A large natural stream of water flowing in a channel to the sea, a lake or another river.

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6
Q

What is a confluence?

A

The junction of two rivers of approximately equal width.

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7
Q

What is a tributary?

A

A river or stream flowing into a larger river or lake.

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8
Q

What is a mouth?

A

The point where the river comes to an end, usually when entering the sea or ocean

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9
Q

What is a source?

A

The original point from which a river flows.

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10
Q

Define interception storage

A

When precipitation lands on buildings, vegetation and concrete before it reaches the soil.

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11
Q

Define vegetation storage

A

Any water taken up by vegetation which is held within plants.

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12
Q

Define surface storage.

A

The total volume of water held on the earth’s surface in lakes, ponds and puddles.

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13
Q

Define groundwater storage.

A

The storage of water underground in permeable rock strata.

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14
Q

Define throughflow.

A

The movement of water flowing downhill through permeable rock above the water table.

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15
Q

Define channel flow

A

The movement of water within the river channel, known also as river discharge.

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16
Q

Define ground water flow.

A

The deeper movement of water through the underlying permeable rock strata below the water table.

17
Q

Define infiltration.

A

The downwards movement of water into the soil surface.

18
Q

Define percolation

A

The downwards flow of water within the soil due to gravity.

19
Q

Define stem flow

A

The movement of water running down a plant stem or tree trunk.

20
Q

Define throughfall

A

Any precipitation which penetrates through the canopy and reaches the soil surface by canopy drip.

21
Q

Define runoff

A

The movement of water over the surface of the land (usually if the ground is too saturated or frozen).

22
Q

Define evaporation

A

The transformation of water droplets into water vapour by heating.

23
Q

Define evapotranspiration

A

The loss of water from the drainage basin into the atmosphere from the leaves of plants and other surfaces by heating.

24
Q

Define transpiration

A

Evaporation of water from plant leaves.

25
Q

Define discharge.

A

The amount of water that passes a given point in a given amount of time.

26
Q

Describe the characteristics of a temperate coniferous forest. How do these characteristics affect stemflow and interception separately?

A
  1. Mishapen and curved tree shape, can have a wide trunk, canopy is more open.
  2. Interception - reduced since the canopy has more gaps (increased SR)
  3. Stemflow - slow and reduced by the nature of the trunk (reduced SR)
27
Q

Describe the characteristics of a temperate deciduous forest. How do these characteristics affect stemflow and interception separately?

A
  1. Straight stems and dense canopy
  2. Interception - increased due to dense canopy (reduced SR)
  3. Stemflow - increased since water movement is aided by gravity and trunk shape (increased SR)
28
Q

How might throughflow vary in different ecosystems?

A
  1. Coarse, sandy soil absorbs and transfers water rapidly, increasing the speed of throughflow
  2. Clay soils drain more slowly and have a high field capacity (lots of water is retained in soil storage), decreasing the speed of throughflow
29
Q

How might groundwater flow vary in different ecosystems?

A
  1. If the bedrock is impermeable, no further downward movement of water occurs (less groundwater flow)
  2. If the bedrock is permeable, water will seep into cracks in the rock and slowly pass through (increased groundwater flow)
30
Q

Give an example of a permeable rock.

A

limestone

31
Q

Compare the flow rate of sandstone with the flow rate of unconsolidated gravel.

A

Sandstone - 200cm per hour (less permeable
Unconsolidated gravels - 20,000cm per hour (more permeable)

32
Q

Give an example of a positive feedback in the water cycle.

A
  1. Sea levels rise due to thermal expansion and ice melt
  2. Ice shelves become unstable, leading to increased carving
  3. Ice melt increases, sea levels rise again.
33
Q

Give an example of a negative feedback in the water cycle.

A
  1. Increased surface temperatures increases evaporation from oceans
  2. Increased cloud cover
  3. Clouds reflect the sunlight and cause a reduction in surface temperatures
  4. Reduced evaporation.
34
Q

What is the difference between the drainage basin and the hydrological cycle in terms of systems?

A

A drainage basin is an open system where the inputs and output can change whereas the hydrological cycle is a closed system so no water enter or leaves the system.

35
Q

Give two factors which can impact the dynamic equilibrium in a drainage basin.

A
  1. Human activity (e.g modifying the drainage basin)
  2. Extreme events like storms or droughts