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The water cycle Flashcards

(83 cards)

1
Q

What are systems made up of

A

Stores, Flows, boundaries, inputs and outputs

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2
Q

Define input

A

When matter or energy is added into the system

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3
Q

Define output

A

When matter or energy leaves the system

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4
Q

Define stores

A

Where matter or energy builds up

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5
Q

Define Flows/Transfers

A

When matter or energy moves from one store to another.

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6
Q

Define boundaries

A

The limits of the system.

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7
Q

What is an example of a system within the water cycle and why?

A

Drainage basin system

Water enters as rain (input)

The system’s watershed is the boundary

Some water is stored in soil and vegetation

Water then travels from the drainage basin to the river then flows down the river.

Water then leaves the system where the river meets the sea.

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8
Q

What is an open system

A

When both energy and matter can enter and leave the system.

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9
Q

What is a closed system

A

-Matter can’t enter or leave a closed system - it cycles between stores.

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10
Q

What are Earth’s subsystems

A

Cryosphere

Lithosphere

Hydrosphere

Atmosphere

Biosphere

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11
Q

What is the cryosphere

A

The cryosphere includes all of the parts of the Earth system where its cold enough for water to freeze. e.g. glacial landscapes

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12
Q

What is the lithosphere

A

The lithosphere is the outermost part of the Earth. It includes the crust and the upper parts of the mantle

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13
Q

What is the biosphere

A

The biosphere is the part of the Earth’s systems where living things are found. It includes all the living parts of the Earth.

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14
Q

What is the hydrosphere

A

The hydrosphere includes all of the water on Earth.

It may be in liquid form, solid state or gas.

It can also be saline or fresh.

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15
Q

What is the atmosphere

A

The atmosphere is the layer of gas between the Earth’s surface and space, held in place by gravity.

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16
Q

How is the Earth an example of a cascading system?

A

All the subsystems are interlinked, the output of a system is the input of another, and so on.

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17
Q

What is positive feedback

A

When the effects of an action are amplified by subsequent knock on effects that occur, moving the system further from its previous state

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18
Q

What is negative feedback

A

When the effects of an action are nullified by subsequent knock on effects that occur, moving the system closer to its previous state.

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19
Q
A
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20
Q

How much of the Earth’s total water is stored in Oceans?

A

96.5%

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21
Q

Global distribution of Earth’s fresh water

A

Glaciers and ice caps - 68.7%

Ground Water - 30.1%

Fresh waters - 2.5%

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22
Q

Global distribution of Earth’s surface water and other fresh water

A

Ground ice and permafrost - 69%

Rivers and Lakes - 21.4%

Soil Moisture - 3.8%

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23
Q

Residence time of Water in shallow groundwater

A

100-200 years

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24
Q

Residence time of water in deep groundwater

A

10,000 + years

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25
Residence time of water in glaciers
20-100,000+ years
26
Residence time of Water in Lakes
2 weeks to 100 years
27
Residence time of water in seasonal snow cover
2 to 6 months
28
Residence time of water in Soil water
1 to 2 months
29
Residence time of water in rivers
2 to 6 months
30
Define evaporation
The process of a substance in a liquid state changing to a gaseous state due to an increase in temperature/pressure.
31
Define condensation
The conversion of a vapour or gas to a liquid.
32
Define convectional rainfall
When the land warms up, it heats the air above it. This causes the air to expand and rise. As the air rises it cools and condenses. If this process continues then rain will fall.
33
Define sublimation
The transition of a substances directly from the solid to the gas phase without passing through the intermediate liquid phase.
34
Define transpiration
The process by which moisture is carried through plants from roots to small pores on the underside of leaves It then changes to vapour and is then released into the atmosphere.
35
Define precipitation
Transfer of water from the atmosphere to the ground. It can take the form of rain, snow, hail, dew.
36
Define interception
Water intercepted and stored on the leaves of plants
37
Define overland flow
Transfer of water over the land surface
38
Define infiltration
Transfer of water from the ground surface into soil Here it then percolates into underlying rocks.
39
Define through flow
Water flowing through soil towards a river channel
40
Define percolation
Water soaking into rocks
41
Define Groundwater Flow
Transfer of water very slowly through rocks.
42
What is an aquifer?
An aquifer is a body of permeable rock or unconsolidated material such as sand or slit that can store and transmit groundwater.
43
key points of an aquifer
Acts like an underground reservoir Water can be extracted using wells or springs
44
Where do aquifers most commonly form
Aquifers most commonly form in areas where the geology allows water to be stored and transmitted easily (permeable rocks or sediments).
45
The soil water budget?
The soil water budget is a model that shows the balance between water inputs, outputs, and storage in the soil over time.
46
What is the upper layer of saturated rock in an aquifer called?
The water table
47
When does the water table rise or fall
The water table can rise or fall depending on factors like rainfall, drought, or extraction.
48
What is a fossil aquifer
A non-renewable store of ancient groundwater that was formed under climatic conditions and is no longer being replenished by the current climate.
49
What is a saline aquifer
A saline aquifer is an underground water-bearing rock formation that contains salty or brackish water instead of fresh water (Essentially an aquifer that contains saline water).
50
Examples of Temporal changes in cryospheric processes
-During the last ice age (approx 18,000 years ago), ice sheets covered 30% of land, today only 10%. -Interglacial periods (e.g. 3 million years ago) saw higher temperatures, melting ice and faster water cycles -Today only 1.7% of Earth’s water is in cryospheric stores, compared to much more in the past
51
Examples of spatial changes in cryospheric processes
-95% of cryospheric water is stored in Antarctica (90%) and Greenland (5%) -Melting at the poles would cause significant spatial changes globally (e.g. sea level rise) -Shrinking arctic sea ice in summer reduces albedo and changes regional climate feedbacks
52
What percentage of Earth’s water is freshwater
2.5%
53
Ways that Long-term global temperature change can impact the water cycle
-Cryospheric store reduction - melting -Increased evaporation and transpiration rates -More extreme wetather -Shifts in Runoff and River Flow -Soil moisture impact
54
The role of crypospheric changes in the water cycle
The cryosphere acts as a long-term store of freshwater, as 68.7% of Earth’s freshwater is stored in glaciers and ice caps Water travels slowly through cryosphere and has long residence time, it stabilises the water cycle in the long-term When water exits the cryosphere as ice caps melt, this releases water from long-term storage into active cycling, increasing sea levels and the size of hydrospheric storage.
55
Temporal changes in Lithospheric processes regarding the water cycle.
-Deforestation over decades - reduces interception and infiltration, increasing surface runoff -Soil degradation over time - Reduces soil’s ability to absorb and store water. -Land use change - Increasing impermeable surfaces, reduced infiltration and increased runoff.
56
When does cloud formation occur
When warm air cools down, causing water vapour to condense into water droplets, which condense as clouds.
57
What is required for clouds to form other than water droplets?
Condensation nuclei, tiny particles that the water droplets can condense upon to form clouds.
58
What is the process of accumulation (cryospheric processes)
-The input of snow and ice into a glacier or ice mass, increasing the magnitude of the cryospheric store
59
What is the process of ablation (cryospheric process)
The loss or output of mass from a glacier, decreasing the magnitude of the cryospheric store
60
What is stem flow?
Water running down a plant stem or tree trunk
61
What is base flow
Groundwater flow that feeds into rivers through river banks or river beds.
62
What is interflow
Water flowing downhill through permeable rock above the water table.
63
What is channel flow
Water flowing down the river or the stream itself.
64
What is a drainage basin?
The area surrounding the river where the rain falling on the land flows into that river. It is also called a river catchment
65
True or false: Drainage basins are systems
True as they have inputs and outputs
66
What is the water balance?
The water balance shows the balance between inputs (precipitation) and outputs (channel discharge and evapotranspiration)
67
Explain the water balance during wet season
During wet seasons, precipitation exceeds evapotranspiration, so there is a water surplus. Ground stores fill with water so there’s more surface runoff and higher discharge.
68
What occurs with the water balance after a water deficit during wet seasons?
Ground stores are recharged in the next wet season as there’s a deficit of water in ground stores.
69
Explain the water balance during dry seasons
During dry seasons, evapotranspiration exceeds precipitation, some water is lost through the river or some is used, so stores deplete. This means there is a water deficit
70
What is river discharge
The volume of water that flows in a river per unit of time
71
Relationship between runoff and discharge
High runoff causes high river discharge
72
What is peak discharge?
The highest point on the flood hydrograph, where river discharge is greatest.
73
What is meant by lag time?
The time between peak rainfall and peak discharge.
74
What are the factors affecting runoff and the shape of the flood hydrograph?
-Size of drainage basins -Shape of drainage basin -Ground steepness -Rock and soil type
75
How can the size of the drainage basin affect runoff and the hydrograph?
-Larger drainage basins catch more precipitation, so will therefore have a higher peak discharge than smaller basins. -Smaller drainage basins will have a shorter lag time, because the precipitation has to travel a shorter distance to the river than larger basins.
76
How can the shape of the drainage basin affect runoff and the hydrograph shape?
-Circular basins are more likely to have a flashy hydro graph than long, narrow basins. Because all points of the watershed (boundary) will be the same distance from the point of discharge measurement. So more water reaches river at the same time.
77
How can ground steepness affect runoff and hydrograph shape?
-The steeper the ground, the faster surface runoff will flow into the river, reducing lag time. -Run off is also higher as water will have less time to infiltrate the soil.
78
How can rock and soil type affect runoff and hydrograph shape?
-Impermeable rocks and soils don’t store water or let water infiltrate. This increases surface runoff. -Therefore peak discharge will increase as more water will reach the river instead of being infiltrated.
79
What are the 3 ways that humans have affected runoff
-Farming practises -Land Use Change -Water Abstraction
80
Ways that farming practises has affected runoff
-Ploughing - breaks up the surface so more water can infiltrate, reducing runoff -Crops increase infiltration and interception compared to bare ground, decreasing runoff. Also evapotranspiration increases. -Livestock, such as cattle, trample and compact the soil, decreasing infiltration and increasing run off. -Irrigation can increase run off as not all of the water will infiltrate.
81
Ways that land use change has affected run off
Deforestation - reduces the amount of water that is intercepted by vegetation, increasing the amount of water that reaches the surface so more runoff. Dead vegetation also stores water preventing it from flowing as run off, when this is removed run off is increased Construction of new buildings and roads creates impermeable surfaces meaning water can’t infiltrate so run off increases.
82
How much of Earth’s carbon is stored in the lithosphere?
Over 99.9% of the carbon on earth is stored in sedimentary rocks.
83
How much of earth’s carbon is stored in the cryosphere
0.01%