Water and carbon cycle Flashcards

(94 cards)

1
Q

A system

A

A useful type of model showing different components and the links between them

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2
Q

Why is a system important?

A

A systems approach helps us to understand the relationships between the physical and human world
Also helps to understand how change in one part of a system can impact elsewhere
E.g. Water cycle, Carbon cycle, Coastal system

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3
Q

Open system

A

Open system is a series of inputs, stores, flows and outputs with energy and matter both passing through and entering and leaving the system

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4
Q

Closed system

A

A closed system is a system that transfers energy but not matter across its bpundary and to the sorrounding enviroment

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5
Q

Sub system

A

A sub-system is a smaller, distinct part of a larger system that functions as a component within it.

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6
Q

Cascading system

A

Cascading systems refers to the interrelationships between the earths major sub systems

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7
Q

Dynamic equlibrium

A
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8
Q

Positive feedback

A

When the effects of an action are amplified by the changes to inputs/outputs/processess

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9
Q

Examples of positive feedback

A

Burning more fossil fuels, INCREASE in co2, in

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10
Q

Negative feedback

A

When the effects of an action are nulified or neutralised by the changes to an input/output/processess promoting stability and state of equlibirium

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11
Q

Examples of negative feedback

A
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12
Q

Hydrosphere

A

The hydrosphere includes all water on earth
Liquid, solid, gas form
Saline (96.5% or fresh water (2.5%)

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13
Q

Atmosphere

A

The enevlope of gases sorrounding the earth of another planet

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14
Q

Biosphere

A

The part of the planet occupied by all living things
CONTAINS: 0.0012% OF ALL CARBON

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15
Q

Lithosphere

A

Rigid outerpart of the earths crust and mantle >99.9%

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16
Q

Cascading system

A
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17
Q

Water cycle

A

The water cycle refers to the recyling and transferring of all water on earth
Open system on a local scale
Closed system on global scale

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18
Q

Key points about wc

A
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19
Q

Precipitation

A

Water released from clouds in the form of rain freezing rain, sleet or snow

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20
Q

Interception

A

The process by which water held on the surface of leaves branches, and trunks during and after rainfall is directly evaporated back up into the atmosphere

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21
Q

Soil moisture

A

The amount of water present within the soil

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22
Q

Percolation

A

The process by which water moves through the soil and rock layers beneath the surface enters permable rocks

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23
Q

Soil storage

A

All water stored within the soil

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24
Q

Infiltration

A

Infiltration is the process by which water enters and moves through the soil or porous surface layers from the ground surface.

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25
Ground water
Water stored deep within the ground that infiltrates into the subsurface
26
Ground water storage
The storage of water in underground permable rock strata e.g. Aquifers
27
Throughflow
The lateral unsatured flow of water through the soil typically thrpugh highly permable rock and in the sporadic holitical flow of water
28
Surface run-off
The flow of water over the ground surface anf occurs when soil cannot absorb the water fast enough or the ground is fully saturated
29
Transpiration
The process at which plants lose water through ecaporaion from their leaves and stem
30
Evaporation
The process by which liquid water turns into water vapour
31
Aquifers
A body of rock and or sediment that holds ground water
32
Fossil aquifers
33
Saline aquifers
34
Soil water budget
The soil water budget graph shows the relationship between precipitation and evapotranspiration across the months of the year
35
Residence time
The amount of water stored within a water store divided by either the rate of addition of water to the store or rate of loss from it
36
Water table
37
Reasons water doesnt remain in soil for long?
38
Role of crysopheric processess in water cycle stores
39
Permafrost
40
Latent heat
41
Evaporation
42
Condensation
43
Sublimation
44
Ablation
45
Depostion
46
Freezing
47
ITCZ zone
48
Convectional rainfall
49
Frontall rainfall
50
Releif rainfall orographic
51
When does evaporation occur and what does the role depend on
52
Condensation
53
Formation of clouds
54
Impact of climate change on crysophere
55
Impact of climate change on hydosphere
56
Impact of climate change on atmosphere
57
Impact of climate change on lithosphere
58
Factors affecting the water cycle on a local scale
59
Drainage basin
60
Inputs to dbs
61
Stores of dbs
62
Flows of dbs
63
Outputs of dbs
64
Water balance
65
Water balance calc
66
Soil water budget graph
67
Positive water balance
68
Negative water balance
69
Field capacity
Field capacity is the point at which the soil is saturated and water can no longer infiltrate
70
Soil Moisture surplus
71
Soil moisture deficit
72
Soil moisture recharge
73
Soil moisture utilisation
74
River discharge
75
River regime
The river regime refers to the changes in the river discharge over the course of a year in response to a number of factors
76
UK rainfall
77
Flood hydrograph
78
Base flow
79
Rising limb
80
Falling limb
81
Lag time
82
Peak discharge
83
Flashy hydrograph
84
Physical factors affecting flood hydrograph
85
How does climate affect water cycle
86
geology and releif on cycle
87
vegetation?
88
Landuse
89
Land use change
90
Agriculture
91
Irrigation
92
93
94
Adiabatic cooling
Adibatic cooling is the process of reducing heat through a change in air pressure cuased by volume expansion