3.1.1.2 The water cycle Flashcards

(53 cards)

1
Q

Description of the lithosphere

A
  • surface water, including biological and groundwater
  • Finland and Canada have the most lakes
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2
Q

Description of the hydrosphere

A
  • oceans cover 70% of the earth’s surface
  • contains 97% of water
  • saline
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3
Q

Description of the cryosphere

A
  • water held in ice
  • if ice sheets melted, sea levels would rise by 60m
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4
Q

Description of atmosphere

A
  • commonly water vapour
  • warm air holds more vapour than cold air
  • increase in water vapour leads to an increase in temperatures (positive feedback)
  • absorbs and reflects solar radiation
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5
Q

Name the 5 factors driving the change in water stores

A
  • evaporation
  • condensation
  • cloud formation
  • precipitation
  • cryospheric processes
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6
Q

What do the rates of evaporation depend upon

A
  • amount of solar energy
  • the availability of water
  • humidity of the air (the more humid the air, the less evaporation)
  • temperature of the air (warmer air can hold more water)
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7
Q

Define relative humidity

A

The amount of water vapour in the air compared to how much it could possibly hold at that temperature.

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8
Q

How could condensation occur

A
  • air is cooled
  • there is a fall in pressure
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9
Q

What does cloud formation require

A

A condensation nuclei

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10
Q

Define dew point

A

The point where the air is at maximum saturation

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11
Q

What are the two main causes of precipitation

A
  • air temperature is reduced to dew point
  • volume of air increases as it rises, without an increase in temperature (adiabatic cooling)
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12
Q

Define orographic rainfall

A

Air is forced to rise over hills/ mountains

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13
Q

Define convectional rainfall

A

Warm air rises away from surfaces and cools

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14
Q

Define frontal rainfall

A

Air masses of different temperatures meet and the warm air rises

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15
Q

Define accumulation

A

Inputs of a glacial system due to snowfall compressing into glacial ice

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16
Q

Define ablation

A

Outputs of a glacial system due to melting

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17
Q

Define sublimation

A

Ice changing directly into water vapour

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18
Q

What is a drainage basin

A

An area of land drained by a river and its tributaries

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19
Q

What is the name of the boundary of a drainage basin

A

Watershed

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20
Q

Define evapotranspiration

A

Combined loss of water through evaporation and transpiration

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21
Q

Define runoff

A

The output of water from the drainage basin system as it moves across the surface

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22
Q

Define interception as a store

A

A short term storm where vegetation can hold precipitation on leaves and branches

23
Q

Define surface storage

A

Puddles
Generally more common in built environments where there is less infiltration

24
Q

Define soil water storage

A

Pore spaces between soil particles fill with water

25
What percentage of sand is pore spaces
20-45%
26
What percentage of clay is pore spaces
40-60%
27
Define groundwater storage
Water stores underground in permeable and porous rocks
28
Define channel store
The volume of water in a river channel
29
Define stemflow
Water flowing down the stems of plants and trees
30
Define infiltration
Water which soaks into the soils
31
Define overland flow
Rainfall which flows over the ground because the soil is saturated or because rainfall exceeds infiltration capacity
32
Define channel flow
The flow of water in rivers
33
Define throughfall
Water moving from vegetation to the ground
34
Define throughflow
The lateral movement of water down a slope to a river channel
35
Define percolation
Downward movement of water to underground stores
36
Define groundwater flow
Slow movement of water within saturated rock
37
Factors affecting infiltration rate
- increased vegetation means an increased rate (roots) - the gradient of hill slopes (topography) - the flow supply
38
Main factor affecting soil storage
Type of soil (sand or clay)
39
Factors affecting interception rates
- type of vegetation (coniferous intercepts 35% precipitation whereas deciduous intercepts 25% annually) - plant density - precipitation intensity
40
Define the water balance
The long term balance between the inputs and outputs of a drainage basin system
41
Define positive water balance
Precipitation exceeds evapotranspiration
42
How do seasonal changes affect the water balance
- In winter, the increased precipitation may lead to a soil moisture surplus and increased runoff - In summer, utilisation of water by humans and vegetation may be high and there could be a soil moisture defecit
43
What measures river flow
Discharge
44
How do drainage basin characteristics affect the flood hydrograph
Larger drainage basins catch more precipitation meaning a large peak discharge, however this discharge must travel further so there is a lower lag time. Opposite for small drainage basins
45
How does the amount of water already present in the drainage basin (antecedent moisture) affect lag time.
If the soil is already saturated, there will be more surface runoff (the fastest flow) therefore there will be a shorter lag time.
46
How does rock type affect the flood hydrograph
Impermeable rock reduces infiltration, increases surface runoff, reducing lag time. Peak discharge increases as more water reaches the river faster
47
Human factors on the storm hydrograph
- Impermeable surfaces increases runoff - Man made drainage systems also reduce lag time
48
How do storm events change the water cycle over time
During a storm event there is less infiltration, more surface runoff and therefore more flooding
49
How do seasonal events change the water cycle over time
- wet seasons have a water surplus - dry seasons have a water deficit (link to water balance)
50
How do farming practices change the water cycle over time
- huge quantities of water are used in food production which redistributes water away from natural pathways - farmers dig ditches to avoid waterlogging plants which increases overland flow - depleted groundwater stores to be used for irrigation
51
How does water abstraction change the water cycle over time
- the process of taking water from a ground source - can cause rivers to dry up and damage to wetland environments - salt water intrusion in coastal areas
52
How does Israel combat against abstraction
- 86% water reuse - 600,000m^3 per day desalination plant
53
How does deforestation change the water cycle over time
- lowers evapotranspiration and interception - increases overland flow and throughflow as vegetation usually slows down these processes - increased discharge and increased risk of flooding