carbon Flashcards

1
Q

why is carbon important

A

Carbon is the main building block of life. ​

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2
Q

how is carbon held

A

Carbon is held in stores e.g. the atmosphere and can have many forms. For example in the atmosphere, carbon is present as gases (carbon dioxide and methane).​

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3
Q

carbon stores

A

the atmosphere
the hydrosphere
the lithosphere
the biosphere

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4
Q

what carbon is stored in the atmosphere

A

carbon dioxide and methane

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5
Q

what carbon is stored in the hydrosphere

A

dissolved carbon

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6
Q

what carbon is stored in the lithosphere

A

carbonates in limestone and fossil fuels such as coal, oil and gas

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7
Q

what carbon is stored in the biosphere

A

in both living and dead organisms

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8
Q

what is the cycle of carbon

A

how carbon moves from one store to another

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9
Q

what processes are involved in the carbon cycle

A

respiration
photosynthesis
volcanic eruptions

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10
Q

store/reservoir

A

where carbon is held

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11
Q

fluxes

A

the flows of movement between the stores, which can operate at local and global scales

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12
Q

petagrams or gigatonnes

A

The units used to measure carbon; one petagram (Pg), also known as a gigatonne (Gt), is equal to one billion tonnes.​

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13
Q

egs of carbon stores

A

crustal/terrestrial/geological
oceanic (deep)
terrestrial soil
oceanic (surface)
atmospheric
terrestrial ecosystems

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14
Q

crustal/terrestrial/geological
carbon store

A

Sedimentary rocks, very slow cycling over millennia ​

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15
Q

oceanic (deep)
carbon store

A

Most carbon is dissolved, inorganic carbon stored at great depths, very slowly cycled.​

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16
Q

terrestrial soil
carbon store

A

From plant materials (biomass) microorganisms break most organic matter down into C02 in a process which can take days in a hot and humid climate to decades in colder climates​

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17
Q

oceanic (surface)
carbon store

A

Exchanges are rapid with the atmosphere through physical processes such as C02 dissolving in the water and biological processes involving plankton. Some of this carbon sinks into the deeper ocean pool. ​

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18
Q

atmospheric
carbon store

A

C02 and CH4 store carbon as greenhouse gases with a lifetime up to 100 years​

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19
Q

terrestrial ecosystems
carbon store

A

CO2 is taken from the atmosphere by photosynthesis, carbon is stored organically, especially in trees. Rapid exchange with the atmosphere- seconds/minutes.

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20
Q

crustal/terrestrial/geological pentagrams

A

100 000 000 fossil fuels store an extra 4 000

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21
Q

oceanic (deep) pentagrams

A

38 000

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22
Q

terrestrial soil pentagrams

A

1,500

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23
Q

oceanic (surface) pentagrams

A

1,000

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24
Q

atmospheric pentagrams

A

560

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25
Q

terrestrial ecosystems pentagrams

A

560

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26
Q

long term carbon stores

A

crustal/terrestrial/geological
oceanic (deep)

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27
Q

short term stores

A

terrestrial soil
oceanic (surface)
atmospheric
terrestrial ecosystems

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28
Q

where can carbon come from

A

geological carbon
biologicaly derived carbon

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29
Q

geological carbon

A

Carbon can be created through a number of chemical reactions in the rock cycle

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30
Q

biologically derived carbon

A

Carbon can also be present in organic matter as a result of processes such as respiration. This can later be stored in shale, coal and other sedimentary rocks

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31
Q

when is geological carbon formed

A

when rocks such as sedimentary rocks are created e.g. limestone and chalk. ​

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32
Q

why is there balance in the geologicaal carbon cycle

A

There tends to be a natural balance between the amount of carbon being released and the amount being absorbed. ​
However, there can be occasional disruptions and short periods before this balance is restored, such as during a volcanic eruption.​

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33
Q

what happens in the geological carbon cycle

A

This is a natural cycle that moves between land, oceans and the atmosphere.​
It involves a number of chemical reactions that create new stores which trap carbon for significant periods of time

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34
Q

case study example of a geological carbon cycle

A

One of earth’s largest stores of carbon is the Himalayas which started off as oceanic sediments rich in calcium- this is now being weathered and returned back to the oceans. ​

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35
Q

what is biologically derived carbon created from

A

is created from dead organisms such as coal and shale. ​
These organisms absorb carbon during respiration and photosynthesis.​
Once they die they (if they are in oceans) sink to the sea bed.​
They are then buried under sinking sediments and form layers called strata.​
Eventually, the strata are squeezed together as a result of the weight on top, and can create fossil fuels such as coal and oil.​

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36
Q

what is out gassing

A

Terrestrial carbon, held within the mantle, is released into the atmosphere as carbon dioxide (CO2) when volcanoes erupt

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37
Q

what is chemical weathering

A

CO2 within the atmosphere combines with rainfall to produce a weak acid (acid rain) that dissolves carbon-rich rocks, releasing bicarbonates

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38
Q

what happens to weathered carbon calcium sediments in the geoleogical carbon cycle

A

Rivers transport weathered carbon and calcium sediments to oceans, where they are deposited.​
Carbon in organic matter from plants and from animal shells and skeletons sinks to the ocean bed when they die, building up strata of coal, chalk and limestone. ​

Carbon-rich rocks are subducted along plate boundaries and eventually emerge again when volcanoes erupt.​

The presence of intense heating along subduction plate boundaries metamorphoses (alters) sedimentary rocks by baking, creating metamorphic rock. CO2 is released by the metamorphism of rocks rich in carbonates during this process.​

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39
Q

what are the three ways carbon is released in the geological carbon cycle

A

volcanic outgassing
metamorphism
chemical weathering

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40
Q

eg of outgassing

A

in 2010, the Icelandic Eruption emitted between 150,000 and 300,000 tonnes of CO2 per day. It contributed less than 0.3% of global emissions that year.​

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41
Q

in what form is carbon found in the atmosphere

A

a gas

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42
Q

Carbon is stored during the formation of which type of rock?

A

sedimentary

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43
Q

What is the term used for the movements of carbon between stores?​

A

flux

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44
Q

How many tonnes is a petagram/gigatonne equal to?​

A

One billion​

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45
Q

What is the name of the sphere where all living things are found?​

A

biosphere

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46
Q

what is the difference between a carbon source and carbon sink

A

A carbon source is shrinking in size and releasing emissions. Whereas a carbon sink is growing in size and storing more carbon.​

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47
Q

what does the amount of carbon in the atmosphere depend on

A

the balance that exists between the sinks and sources.​

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48
Q

when is the carbon cycle in equilibrium/balanced

A

If sources equal sinks

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49
Q

what happens if the carbon cycle is unbalanced

A

results in posotive or negative feedback

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50
Q

negative feedback loop

A

Earth systems normally operate by negative (stabilising) feedbacks, maintaining a stable state by preventing the system moving beyond certain thresholds. I.e. any change is cancelled out, maintaining equilibrium. ​

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51
Q

posotive feedback

A

Positive (amplifying) feedback loops occur when a small change in one component causes changes in other components. This shifts the system away from its previous state and towards a new one.​

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52
Q

what is the biogeochemical carbon cycle

A

Biological and chemical processes determine just how much of the carbon available on the Earth’s surface is stored or released at any one time. ​
The role of living organisms are critical to the cycle and to controlling the balance between overall storage, release, transfer and absorption of carbon. ​

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53
Q

what 4 key processes are involved in the bio-geochemical carbon cycle

A

photosynthesis
respiration
decomposition
combustion

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54
Q

what is respiration

A

a chemical process that happens in all cells and is common to both plants and animals
glucose is converted into energy that can be used for growth and repair, movement and control of body temperature in mammals
carbon dioxide is then returned to the atmosphere mostly by exhaled air

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55
Q

what is decomposition

A

when organisms die they are consumed by decomposers such as bacteria, fungi and earthworms
during this carbon from their bodies is returned to the atmosphere as carbon dioxide
some organic material passes into the soil where it may be stored for hundreds of years

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56
Q

what is combustion

A

organic material contains carbon
when burned in the presence of oxygen it is converted into energy, carbon dioxide and water- combustion
carbon dioxide released into the atmosphere returning carbon that may have been stored in rock for millions of years

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57
Q

what is photosynthesis

A

the process where plants use the light energy from the sun to produce carbohydrates in the form of glucose
green plants absorb light energy using chloropyll in their leaves
absorbed light energy converts carbon dioxide in the air and water from the soil into glucose- during this oxygen is released into the air
some glucose is used in respiration the rest is converted into starch which is insolublebut can be converted back into glucose for respiration

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58
Q

how much larger is the ocean store for carbon than the atmosphere

A

The ocean’s are one of the Earth’s largest store, being 50 times greater than the atmosphere. ​

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59
Q

where is 93% of CO2 stored

A

in undersea algae, plants and coral, with the remainder dissolved in the water. ​

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60
Q

what are carbon cycle pumps

A

are processes operating within the oceans which circulate and store carbon. ​

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61
Q

what are the three carbon cycle pumps

A

the biological pump, the carbonate pump and the physical pump.​

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62
Q

what are the three ocean pumps

A

biological pump
carbonate pump
physical pump

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63
Q

biological pump

A

this is the sequestration of C02 to oceans by phytoplankton. Phytoplankton float on the surface of the ocean to access sunlight and photosynthesise. They are autotrophs and are the base of the marine food web. Even though they are minute they make up over half the planets biomass. ​
Carbon is then passed up the food chain by consumers which in turn release C02 back to the atmosphere.​
In this way most carbon is cycled in surface waters and only 0.1% reaches the sea floor through decompositions and sedimentation. ​
Phytoplankton sequester over 2 billion metric tonnes of C02 annually to the deep ocean. ​

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64
Q

carbonate pump

A

this relies on inorganic carbon sedimentation. Lots of marine organisms utilise calcium carbonate to make their outer shells/ skeletons. When these organisms die and sink to the sea floor many shells will dissolve on the way and the carbon will become part of the ocean and flow around the planet in currents. Shells that do not dissolve build up slowly on the sea floor forming limestone sediments such as those in the white cliffs of Dover. ​

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65
Q

physical pump

A

This is the oceanic circulation of water including upwelling, down welling and the thermohaline current. C02 in the oceans is mixed much slower than in the atmosphere so there are large spatial differences in concentration. ​
Colder water can absorb more C02 so C02 concentration is 10% higher in the deep ocean than the surface and polar regions store more than tropical regions. ​Warm waters release C02 into the atmosphere and cold waters absorb C02. ​
Large ocean currents like the North Atlantic Drift move water from the tropics to the poles, the water cools and absorbs more C02. ​

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66
Q

when did the iceland volcano erupt

A

2010

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67
Q

how much CO2 did the iceland volcano emmit

A

between 150,000 and 300,000 tonnes of CO2 per day placing it in the same emissions league as small-medium European countries such as Portugal or Ireland

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68
Q

what % of global emmisions of greenhouse gases did the Iceland volcano emit in 2010

A

However it contributed less than 0.3% of global emissions of greenhouse gases in 2010.​

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69
Q

biological pump summed up

A

organic sequestration by phytoplankton

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70
Q

physical pump summed up

A

based on the rise (upwelling) and fall (downwelling) of the circulation of water

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71
Q

carbonate pump summed up

A

Based on CaCO3 used in the shells of marine organisms​

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72
Q

where do phytoplankton live

A

Phytoplankton float on the ocean’s surface to access sunlight and photosynthesise.​

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73
Q

how much of the worlds biomass do phytoplankton make up

A

half

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74
Q

what do phytoplankton absorb

A

The absorb carbon, when eaten that carbon is passed along the food chain.​
Part of that carbon is released through respiration.​
Some carbon reaches the sea floor through decomposition and sedimentation.​
Threatened by warming oceans.​

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75
Q

variations in phytoplankton

A

Thrive along coastlines and continental shelves.​
Found along the equator in the Pacific and Atlantic Oceans.​
Thrive in high latitude areas.​

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76
Q

why do phytoplankton thrive in certain areas

A

Oceans rich in nutrients from deep water upwelling.​
In high latitudes blooms peak in spring and summer when sunlight increases.​
In subtropical oceans blooms decrease because surface waters warm up and become buoyant, with cold, dense water below the water not mixing easily, meaning nutrients are quickly used up.​

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77
Q

what is the fastest part of the carbon cycle

A

terrestrial (land based) sequestration

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78
Q

globally what are the most productive biomes

A

tropical forests and savanah grasslands

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79
Q

what happens in terrestrial sequestration

A

Primary producers (plants) take in carbon through photosynthesis and then release CO2 back into the atmosphere through respiration.​
Consumer animals then eat these plants and absorb the carbon which becomes part of its fats and proteins.​
Initially after the animal has died, microorganisms and detritus feeders such as beetles feed on waste material which becomes part of these micro-organisms.​
After death, tissues decay into the soils. This process is affected by climate and decomposition will happen fastest in tropical climates (warm and damp) or, in Arctic biomes, the process can be ‘locked down’ for substantial time periods. ​

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80
Q

what is 95% of a trees biomass made up of

A

95% of a tree’s biomass (leaves, branches, trunk and roots) is made up from thee CO2 that it sequesters and converts into cellulose.​

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81
Q

what does carbon fixation do

A

turns gaseous carbon into living organic compounds that grow.​

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82
Q

what % of global carbon do soils store

A

20-30%
sequestering about twice the quantity of carbon as the atmosphere and three times that of terrestrial vegetation. Whether the soil sequesters or emits C02 depends on local conditions.​

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83
Q

what factors affect carbon sequestration in soils

A

climate
soil type
management and use of soils

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84
Q

how does climate affect carbon sequestration in soils

A

This dictates plant growth and microbe activity. Rapid decomposition occurs at higher temperatures or under water logged conditions. Places with high rainfall have an increased potential carbon storage than the same soil type in lower rainfall places. Arid soils store only 30 tonnes per hectare compared with 800 tonnes per hectare in cold regions.​

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85
Q

how does soil type affect carbon sequestration in soils

A

Clay-rich soils have a higher carbon content than sandy soils as clay protects carbon from decomposition. ​

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86
Q

how does management and use of soils affect carbon sequestration in soils

A

Since 1850, soils globally have lost 40-90 billion gigatons of carbon through cultivation and disturbance. Current rates of carbon loss due to land-use change are 1.6 ± 0.8 billion gigatons of carbon per year.

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87
Q

what happens to 31% of short wave radiation

A

reflected by clouds, aerosols and gases in the atmosphere and by the land surface.​

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88
Q

what happens to the other 69% of short wave radiation

A

absorbed, particularly by the oceans.

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89
Q

what happens when long wave radiation is reflected back

A

a large amount is re-radiated back to Earth by clouds and GHGs which traps the long wave radiation in our atmosphere. ​

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90
Q

what does the natural greenhouse effect do

A

gives us our life supporting average temperature of 15 degrees. Without this effect our average temperature would be -6.

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91
Q

holocene period

A

The present geological time we are living in is called the Holocene period but many people refer to it now as the Anthropocene because of the profound changes caused by humans. ​

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92
Q

how has the enhanced greenhouse effect affected c02 levels

A

The natural greenhouse effect has become enhanced; C02 in the atmosphere has increased in volume by 40% in the last 300 years. ​

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93
Q

causes of green house gases

A

industry
agriculture
electricity generation
transport
cement production
wetland/peatland loss

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94
Q

how does industry create greenhouse gases

A

combustion of fossil fuels

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95
Q

how does transport create greenhouse gases

A

c02 emmisions

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96
Q

how does agriculture create greenhouse gases

A

livestock-methane
deforestation- farm land
loss of soil carbon from ploughing

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97
Q

how does elecrticity generation create GHGs

A

increased demand due to rising population

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98
Q

how does cement production create GHGs

A

The most consumed product in the world after water.​
Chemical processes involved in production release a substantial amount of carbon dioxide (6% of global carbon emissions). ​

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99
Q

how does wetland/peatland loss cause GHGs

A

The nature of wetlands is shaped by water and rainfall patterns – the unpredictable change due to climate change may result in wetlands drying out.​
Peatlands store 550Gt of carbon – twice as much as all of the world’s forest biomass combined but only cover 3% of the earth’s surface. ​

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100
Q

how has human activity affected carbon distribution

A

Through burning fossil fuels we have transferred considerable amounts of carbon from fossil stores, where exchanges are very slow, into the fast category, significantly disturbing the carbon cycle.​
CO2 levels in the atmosphere are higher than ever before.​
This process has continued since the Industrial Revolution (1760-1840) and accelerated through the oil age (20th century), changing the chemistry of the atmosphere. ​

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101
Q

how have climate patterns- temperature and precipitation distribution affected carbon levels

A

Carbon dioxide and other GHGs naturally help to maintain the Earth’s temperature – and also determines the distribution of temperature and precipitation.​
If the concentrations of these change, it is likely to alter these distribution patterns. ​

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102
Q

how is temperature distributed

A

The amount of solar energy (solar insolation) reaching the Earth’s surface varies at different locations which in turn influences temperature.​
The angle of the sun’s rays makes solar insolation intense at the equator but dispersed over a wider area at the poles. ​
Different characteristics of the Earth’s surface (how light or dark it is) also affects how much heat is absorbed or reflected. ​

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103
Q

how is precipitation distributed

A

The heating of the atmosphere and surface controls the temperature, pressure, movement and moisture content of the air.
Because solar radiation is most intense at the equator, low pressure systems dominate there, meaning rainfall all year round.​
Regional and seasonal variations also ​occur, because of the effects of relief, pressure patterns and wind systems.​

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104
Q

what happens in the enhanced greenhouse effect

A

1) short wave radiation passes through the atmosphere
2) some long wave radiation is reflected back into space
3) some short wave radiation is absorbed and is converted to long wave (heat) radiation

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105
Q

evidence of climate change

A

The IPCC (Intergovernmental Panel for Climate Change) has been collecting evidence of natural changes of heat sources such as volcanism, solar changes and orbital changes such as the Milankovitch cycle and none of these can account for recent changes. ​

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106
Q

how do we know that c02 levels in the atmosphere are higher than ever before

A

compared with air bubbles found in ice cores up to 800,000 years ago

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107
Q

what is the primary energy source driving modern civilisation

A

fossil fuels

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108
Q

what does fossil fuel combustion create

A

fast carbon cycling
Without it, the carbon in the fossil fuels would transfer slowly through volcanic activity.​

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109
Q

between 1750 and 2011 how much did the IPCC estimate concentratio of c02 in the atmosphere would increase by

A

40%
With approximately 50% of those emissions still in our atmosphere today. ​

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110
Q

how long does carbon remain in the atmosphere for

A

2000 years
so c;limate change will continue

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111
Q

what is the combustion of fossil fuels linked to

A

linked greenhouse gas concentrations, rising global temperatures and sea levels.​

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112
Q

what are the three main areas fossil fuel combustion impacts on

A

climate
ecosystems
hydrological cycle

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113
Q

what was the hottest year on record

A

2015
average world temperature 1 degrees C above that of pre-industrial era; 2011 -2015 were the five hottest years on record.​

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114
Q

how does climate change affect marine biodiversity

A

Marine biodiversity may be lost as fish move away from warming sea temperatures and about 80% of coral reefs could be bleached (e.g. Great Barrier Reef). ​

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115
Q

how does climate change affect permafrost

A

Permafrost areas will thaw and add more water to Arctic rivers. ​

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116
Q

how does climate change affect drought

A

The Sahel, Mediterranean, South Africa and South Asia will become drier, with drought more common in the tropics and subtropics – but some uncertainties remain due to other factors (El Nino).​

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117
Q

how does fossil fuels impact oceanic circulation

A

Atlantic and Southern Ocean thermohaline circulation may weaken, altering the transfer of heat by oceans.​

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118
Q

how does fossil fuels and climate change impact flash flooding

A

Uncertainty remains over increased river flooding, since multiple factors are involved, but more flash flooding is likely as a result of more intense precipitation.​

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119
Q

by what year are shifting temperatures going to impact bird habitats

A

By 2080 shifting temperatures may reduce bird habitats in North America, affecting 314 species, with ocean and coastal habitats affected the most, also partly because of coastal flooding and salt encroachment).​

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120
Q

habitat changes will mean that what % of land species with limited adaptability will face extinction

A

10%
as climate gets warmer and wetter or drier
Rates of extinction could rise to 15-40% of all species, especially in high polar regions.​

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121
Q

what will a shift of subtropical high pressure areas northwards cause

A

cause a 20-30% decrease in water availability in Mediterranean climate zones.​

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122
Q

how will fossil fuels and climate change affect ice shelves

A

Antarctic ice shelves will melt, adding more freshwater to the Southern Ocean, changing density and convection.​

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123
Q

how has fossil fuels and climate change impacted average arctic temperatures

A

average Arctic temperature has already increased at twice the global average over the last 200 years. Snow and ice cover will contract with the ablation of glaciers.​

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124
Q

how does climate change affect humidity levels

A

Humidity levels in the atmosphere will increase, consistent with what warmer air can hold.​

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125
Q

how will fossil fuels and climate change impact precipitation

A

Precipitation will increase in higher latitudes and decrease in lower latitudes. Worldwide patterns will change, with wetter eastern parts of N/S America, northern Europe and northern/central Asia.​
Extreme heavy precipitation events will become common, with precipitation increases over northern-hemisphere land areas.​

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126
Q

how will climate change affect cold and warm days

A

The number of cold days and nights will decrease, and warm ones will increase. There have been fewer extreme cold events over the last 50 years, but more extreme heat events.​

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127
Q

how will climate change affect biodiversity

A

Biodiversity will be affected as habitats shift poleward or into deeper ocean waters or higher altitudes. In north Brazil and central-southern Africa, lower rainfall and soil moisture, which causes changes to soil and oxygen will reduce biodiversity. Permafrost will thaw.​
Acidification of sea water (carbonic acid) will threaten corals and the shells of marine creatures will get smaller and thinner.​
Butterflies are a good example of the shift northwards of climate zones (6.1 km per decade). ​

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128
Q

climate negative outcomes to stores and pathways of carbon

A

Atlantic and Southern Ocean thermohaline circulation may weaken, altering the transfer of heat by oceans.​

Antarctic ice shelves will melt, adding more freshwater to the Southern Ocean, changing density and convection.​

Extratropical low-pressure system (depression) tracks will move northwards with climate pattern shift.​

Temperate and tropical zones may experience stronger storm activity because of more heat and moisture in the atmosphere.​

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129
Q

ecosystems negative outcomes to stores and pathways of carbon

A

Biodiversity will be affected as habitats shift poleward or into deeper ocean waters or higher altitudes. In north Brazil and central-southern Africa, lower rainfall and soil moisture, which causes changes to soil and oxygen will reduce biodiversity. Permafrost will thaw.​

By 2080 shifting temperatures may reduce bird habitats in North America, affecting 314 species, with ocean and coastal habitats affected the most, also partly because of coastal flooding and salt encroachment).​

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130
Q

hydrological cycle negative outcomes to stores and pathways of carbon

A

A shift of subtropical high-pressure areas northwards will cause a 20-30% decrease in water availability in Mediterranean climate zones.​

Small glaciers will disappear (e.g. in the Andes and Himalayas), decreasing river discharges once they have gone. ​

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131
Q

what is an energy mix

A

The energy mix of a country is the proportion of each primary energy resource it uses per year. These resources may be domestic or imported. ​

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132
Q

non renewable (finite) energy mix

A

E.g. coal, oil and gas. Exploitation and use of these stocks will lead to their exhaustion. ​

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133
Q

renewable energy mix

A

E.g. solar, wind and wave power.​
These are continuous flows of nature and can be constantly re-used.​

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134
Q

recyclable energy mix

A

E.g. reprocessed uranium and plutonium from nuclear power plants and heat recovery systems​

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135
Q

what factors affect energy mixes

A

Availability of primary energy resources within the country as well as their access to technology to extract the resources.​
The accessibility of primary energy resources from outside the country.​
The energy needs of the country, based on economic development, lifestyle and climate.​
changing energy consumption patterns, linked to population and economic growth.​
National and regional policies that affect energy production and consumption e.g. climate change.​
Cultural and historical legacies and geopolitical links.​
Financial costs of each energy option.​

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135
Q

eg of how The energy needs of the country, based on economic development, lifestyle and climate affect the energy mix

A

US – consumerist lifestyle meaning higher demand. Plus hot/cold climate meaning air conditioning and heating required​

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136
Q

eg of how The accessibility of primary energy resources from outside the country affects the energy mix

A

Europe – Russia exports 80% of it’s natural gas to Europe.​

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137
Q

eg of how Availability of primary energy resources within the country as well as their access to technology to extract the resources affects the energy mix

A

Iceland – Domestic geothermal energy​

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138
Q

eg of how National and regional policies that affect energy production and consumption e.g. climate change can affect the energy mix

A

UK – National policies to reduce emissions and invest in renewables​

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139
Q

eg of how Financial costs of each energy option affect the energy mix

A

Countries with little capital e.g. India, consume the cheapest resources, which is currently fossil fuels

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140
Q

eg of how hanging energy consumption patterns, linked to population and economic growth can affect the energy mix

A

India – population of 1.2 billion meaning high demand​

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141
Q

eg of how Cultural and historical legacies and geopolitical links can affect the energy mix

A

India – struck a deal with Canada for it to provide India with 3.2 million kilos of uranium.​

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142
Q

what are the two types of energy

A

primary
secondary

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143
Q

primary energy

A

natural energy resources that have not been converted into another form of energy e.g. coal, oil, gas. (Consumed in their raw form)​

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144
Q

secondary energy

A

refers to what the primary source has been converted into, usually electricity. ​

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145
Q

what % of the UKs energy mix does coal and oil make up

A

less than 1% combined

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146
Q

what % of the UKs energy mix does natural gas make up

A

38%

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147
Q

what % of the UKs energy mix does wind make up

A

20%

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148
Q

what % of the UKs energy mix does biomass make up

A

12%

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149
Q

what % of the UKs energy mix does solar make up

A

6%

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150
Q

what % of the UKs energy mix does nuclear make up

A

19%

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151
Q

why is the UK in an energy deficit and energy insecure

A

Despite economic and population growth in the UK, the adoption of energy-saving technologies (e.g. home heating and vehicle engines) resulted in the UK consuming less energy in 2015 than in 1998 with more of that energy coming from renewables. ​
However, the UK now imports more energy than it produces domestically (i.e. from it’s own reserves) due to a decline in the North Sea oil and gas reserves. ​

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152
Q

what is energy security

A

being able to access reliable and affordable energy sources – either domestic or from ‘friendly’, overseas countries​

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153
Q

europe is dependent on russian gas for what % of its supply

A

40%
Countries such as Germany are particularly vulnerable (50% - shut down other resources)

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154
Q

what eastern european countries rely solely on russian gas

A

Moldova and North Macedonia for example. Finland and Latvia rely on it for over 90% of their energy.​

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155
Q

what % of the Uks gas supply comes from domestic resources

A

50%
the other half mostly from Norway.​

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156
Q

what % of gas supply did Russian imports make up for the UK in 2021

A

There are no gas pipelines directly linking the UK with Russia and imports from Russia made up less than 4% of total UK gas supply in 2021.​

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157
Q

why does Europe want to wean istelf off russian gas

A

the aim of Europe to wean itself off Russian gas to make it less of a weapon during conflict.​

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158
Q

what does russias economy heavily rely on

A

fossil fuel exports, so it needs to consider the consequences of this, if it decides to threaten the removal of the supply to Europe.​

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159
Q

energy mix

A

The energy mix of a country is the proportion of each primary energy resource it uses per year. ​

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160
Q

recyclable energy

A

A resource that is reused or reprocessed​

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161
Q

primary energy

A

natural energy resources that have not been converted into another form of energy/consumed in raw form​

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162
Q

domestic energy

A

Energy extracted and used within the same country​

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163
Q

what are the three types of resources that make up an energy mix

A

non renewable
renewable
recyclable

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164
Q

what does meeting the demand for energy involve

A

energy pathways from producer to consumer

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165
Q

energy pathway

A

describes the flow of energy between the producer and consumer, and how it reaches the consumer, e.g. pipeline, transmission lines, ship, rail etc. ​

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166
Q

what three objectives does the world energy council suggest energy players have

A

energy security-energy supply must meet demands​
energy equity- there must be accessible and affordable energy for all countries ​
environmental sustainability

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167
Q

how has energy security been threatened during the recent ‘oil age’

A

geopolitical tension e.g. Arab uprising in North Africa, Arab-Israeli war. ​

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168
Q

what are the 5 major players in world energy

A

OPEC
energy companies
TNCs
consumers
governments

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169
Q

what does OPEC stand for

A

Organisation of the Petroleum Exporting Countries.

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170
Q

how many countries is OPEC made up of

A

12 member countries and between them they own around two-thirds of the world’s oil reserves.​

171
Q

what does OPEC do

A

is in a position to control the amount of oil and gas entering the global market, as well as the prices of both commodities.​
It has been accused of holding back production in order to drive up oil prices.​

172
Q

energy companies

A

These are the companies that convert primary energy (oil, gas and oil) into electricity and then distribute it.​
Most companies are involved in the distribution of both gas and electricity.​
They have considerable influence when it comes to setting consumer prices and tariffs. ​

173
Q

TNCs that are major players in world energy

A

Gazprom, BP and Total.​

174
Q

TNCs as major players in world energy

A

Nearly half of the top 20 oil companies are state-owned, so therefore very much under government control.​
Most of these companies are involved in a range of operations, such as exploring, extracting, transporting, refining and producing petrochemicals. ​

175
Q

consumers as major players in world energy

A

They create the demand.​
The most influential consumers are transport, industry and domestic users. ​
Purchasing choices are often based on price/cost issues e.g. petrol prices can be keenly competitive between supermarkets​
Consumers are largely passive players when it comes to fixing energy prices.​

176
Q

role of governments as major players in world energy

A

They can influence the sourcing of energy for geopolitical reasons.​
To meet international obligations, whilst securing energy supplies for the nation’s present and future, as well as supporting the countries economic growth.​
Regulating the role of private companies and setting environmental priorities. ​

177
Q

what has the global demand for different sources of energy increased by since the 1990s

A

50%

178
Q

what % of the global energy mix do fossil fuels make up

A

84% (in 2019)

179
Q

what effect has chinas rapid economic growth had on consumption

A

China’s rapid economic growth has largely driven in the increase of consumption, doubling it’s oil consumption between 2000-2010. This is expected to increase at twice the global average, which means that by 2035 China will be the world’s largest energy importer.​

180
Q

what is the issue with fossil fuel demand

A

The issue is the mismatch between where fossil fuels are found and where the demand for them is greatest.​

181
Q

why is the distribution of fossil fuels uneven across the world

A

Coal, oil and natural gas all from under certain geological conditions which determines where they are found. ​
Because of the disparity between production and areas of high demand, this is called a mismatch.​

182
Q

gas pathways

A

Natural gas is transported via pipelines because it’s efficient and increasingly international. ​
These pathways depend on multilateral (between many countries) and bilateral (between two countries) agreements. ​

183
Q

eg of gazprom as a gas pathway

A

The Russian firm Gazprom exports 80% of their gas to Europe. For security reasons they try to avoid transporting the gas through other countries.

184
Q

eg of a gas pathway

A

the nord stream

185
Q

how long is the nord stream 2

A

The Nord Stream pipeline runs 1200 km along the bed of the Baltic Sea to avoid other countries.
take gas from the Russian coast near St Petersburg to Lubmin in Germany.​

186
Q

how much did the nord stream 2 cost

A

€10bn (£8.4bn) and was completed last September. The Russian state-owned energy giant Gazprom put up half of the cost and western energy firms such as Shell and ENGIE of France are paying the rest.​

187
Q

what existing gas pipeline does the nord stream 2 run parallell to

A

runs parallel to an existing gas pipeline, Nord Stream, which has been working since 2011.​

188
Q

how much gas could the nord stream and nord stream 2 deliver to europe

A

these two pipelines could deliver 110bn cubic metres of gas to Europe every year. That is over a quarter of all the gas that European Union countries use annually.​

189
Q

what % of the worlds oil is moved by tankers

A

50%
travelling on fixed shipping routes, which include narrow sea channels or a convergence of transport routes (a choke point). ​

190
Q

eg of a choke point

A

the Suez Canal
It is just 205m wide but one million barrels of oil; 8% if liquified natural gas and 12% of global trade pass through every day!​

191
Q

how do choke points affect energy prices

A

If choke points are blocked or threatened, even temporarily, then energy prices can quickly rise

192
Q

why are energy pathways key to energy security

A

Due to energy transportation

193
Q

what threats are there to energy pathways

A

Geopolitical factors – concerning ownership, use and control.​
Militant action (including piracy) – e.g. seized ships, bombed pipelines.​
Weather/natural hazards – damage to pipelines in storms or earthquakes. ​
political tensions and disagreements – lead to choke points being blocked.​

194
Q

eg of how geoplotical factors are a threat to energy pathways

A

the ongoing Syrian conflict Russia and USA’s battle for control over Syria. ​

Many argue the main reason for control is the proposed pipeline through Syria to fuel Europe. ​

Russia is the second biggest supplier of oil and gas (after the US and Saudi Arabia) and wants a share in the European market - it is allies with Iran who want the same involvement in the market. Iran want to export its gas via pipelines through Syria so it defends the Syrian government from those trying to overthrow and replace their president Assad.​

195
Q

eg of how militant action is a threat to energy pathways

A

in December 2015, the International Marine Bureau reported piracy attacks along the Strait of Malacca, between Malaysia, Singapore and Indonesia (the world’s second largest chokepoint for oil and gas transit by tanker). Criminal gangs frequently seized ships for hostage payments – over 500 attacks occurred between 2009-2015.​
The Trans-Forcados, Efurtun-Otor and Escravos pipelines in Nigeria were bombed in 2016 by militants resulting in a loss of 300,000 barrels of crude oil a day.​

196
Q

eg of how weather/natural hazards are a threat to energy pathways

A

During a stormy winter in 2013, UK gas reserves fell to 6 hours worth, as storm damage paralysed an import pipeline.​

197
Q

eg of how political tensions and disagreements can be a threat to energy pathways

A

3 out of 4 of Russia’s pipelines cross Ukraine to get to Europe.​
Due to conflict between Russia and Ukraine, this could threaten the energy security of Europe.​
Ukraine could increase prices it charges for allowing the gas to be transferred across its country; or it could stop the flow altogether. ​

198
Q

Suez Canal Blockage 2011

A

In March 2021 a huge container ship blocked the canal, preventing any traffic from passing through.​
A total of 450 ships were delayed, estimated to be $9.6bn of trade each day.​
Crude oil prices rose as a result due to fears supplies would be short!​

199
Q

what are unconventional fossil fuels

A

when fossil fuels are obtained using new, unconventional methods.​

200
Q

unconventional fossil fuels

A

tar sands
deep water oil
shale gas
oil shale

201
Q

tar sands

A

also known as oil sands. These are naturally occurring mixtures of sand, clay, water and a dense viscous form of petroleum called bitumen. Canada has 73% of known global stocks.​

202
Q

extraction of tar sands

A

tar sands have to be mined and then injected with steam to make the tar less viscous so that it can be pumped out.​

203
Q

oil shale

A

Deposits of organic compounds called kerogen in sedimentary rocks that have not undergone sufficient pressure, heat or time to become conventional oil. The USA has 77% of known global reserves. ​

204
Q

extraction of oil shale

A

Either mined or shale is ignited so that the light oil fractions can be pumped out.​

205
Q

shale gas

A

Usually methane in coal seams, or natural gas trapped in fractures and pores of sandstones and shales. ​

206
Q

extraction shale gas

A

Fracking: pumping water and chemicals forces out the gas​

207
Q

deepwater oil

A

As accessible reserves (e.g. North Sea oil) run out, prospecting companies have to look into deeper ocean waters with greater risks and costs, e.g. the Gulf of Mexico and Brazil’s off-shore reserves. ​

208
Q

extraction of deepwater oil

A

Drilling takes place from ocean rigs; already underway in the Gulf of Mexico and Brazil​

209
Q

what has happened to the use of conventional fossil fuels

A

has decreased, whilst unconventional fossil fuels has, and is predicted to continue to increase.​

210
Q

what was the most used fossil fuel in 1990

A

conventional oil
at 8 million barrels per day

211
Q

what is predicted to be the most used fossil fuel in 2030

A

unconventional gas
at 10 million barrels per day

212
Q

what is ‘peak oil’

A

when oil production will reach a global peak, before declining sharply.​
has been predicted for many years

213
Q

why is the use of unconventional fossil fuels increasing

A

As conventional fossil fuels (oil, gas and coal) reach an end, the search for other sources has intensified. ​
Unconventional fossil fuels are becoming more viable, particularly as areas such as Canada and USA discover its reserves. ​

214
Q

how can geopolitics affect use of unconventional fossil fuels

A

geopolitics can make access to resources difficult, or cause the prices of oil and gas to increase, making unconventional fuels like shale gas more economically viable. ​

215
Q

where are Tar sands found

A

Canada

216
Q

where is shale gas found

A

USA

217
Q

where is deep water oil found

A

Brazil

218
Q

what has happened to the UKs energy mix since 2005

A

has decreased

219
Q

overall what contributed most to the uks energy mix between 1996 and 2017

A

natural gas

220
Q

what has seen the biggest drop in the UKs energy mix between 1996 and 2017

A

coal
from it’s peak in 2012 at approximately 130 terawatt hours, down to approximately 20 TWh in 2017. ​

221
Q

what has had the biggest increase in contribution to the uks energy mix between 1996 and 2017

A

Renewables has had the biggest increase in contributions to the UK energy mix, generating approximately 100 terawatt hours in 2017, compared to less than 10 TWh in 1996. ​

222
Q

what energy sources have remained consistent in the UKs energy mix between 1996 to 2017

A

nuclear

223
Q

what is the UK government very mindful of in terms of their energy mix

A

mindful of the need to become energy secure and to play its part in reducing global emissions.​

224
Q

what % of the UKs primary energy in 2021 did did oil and natural gas provide

A

nearly 80%
with petrol being used by transport and most of the gas used to generate electricity.​

225
Q

what has happened to UK energy consumption since 1970

A

Today we consume less energy than we did in 1970, despite the population increase of some 6.5 million – mainly due to a changing economy, moving away from industry.​

226
Q

what is a posotive of the Uks energy usage

A

The UK is now more efficient, both in producing energy and using it.​

227
Q

how much less energy do households and industry use in the UK

A

Household uses 12% less energy while industry uses 60% less – however this has been offset by transport as there’s been a big increase in vehicles and flights.​

228
Q

what are the 4 different ways the UK hopes to reduce its reliance on fossil fuels

A

Increasing renewable energy – especially wind and solar​
Developing a new generation of nuclear power stations, e.g. Hinkley Point C.​
Reduce energy use through technologies such as LED light bulbs.​
Recycling energy which would normally be wasted. ​

229
Q

what do we need to do to reduce enhanced climate change

A

seek alternative resources than fossil fuels

230
Q

recyclable energy

A

reprocessed energy

231
Q

eg of recyclable energy

A

nuclear power
heat recovery systems

232
Q

renewable energy

A

continuous flows of nature and can be constantly re used

233
Q

eg of renewable energy

A

biomass
HEP
solar
wave and tidal
wind

234
Q

how do heat recovery systems work

A

work via a ventilation system which is positioned at the top of the building. Rather than just draw the stale air out and replace it with new stuff, it first of all works to draw the heat from the outgoing air and passes it to the air which is coming in.​

235
Q

what usually happens in buildings without heat recovery systems

A

Normally, air circulates around an office, becomes stale and is replaced by colder air that it is warmed up by the ventilation system. What happens to that already warm, stale air? It simply gets expelled into the atmosphere. Heat recovery systems don’t replace the need for a boiler or other technology to heat your radiators but it does help them work more efficiently by recycling that warm air ensuring that you get the most out of it.​

236
Q

what are biofuels derived from

A

derived immediagtely from living matter

237
Q

eg of biofuels

A

agricultural crops
forestry or fishery products
various forms of waste

238
Q

what is a primary biofuel

A

fuelwood, wood chips and pellets and other organic material used in the unprocessed form, primarily for heating, cooking or electricity generation. ​

239
Q

what is a secondary biofuel

A

derived from the processing of biomass and include liquid biofuels such as ethanol and biodiesel which can be used by vehicles and in industrial processes.​

240
Q

what has happened to biofuel usage

A

There has been a recent surge with the commercial use of a number of new biofuels.​
These new, so-called ‘energy crops’ include wheat, maize, grasses, soy-beans and sugar cane. ​
In the UK, the two main biofuels are oilseed rape and sugar beet

241
Q

what is the biofuel production for the USA

A

15.5 billion litres between 2013-2018

242
Q

what is the biofuel production for brazil

A

11.9 billion litres between 2013 and 2018

243
Q

what is the biofuel production for china

A

1.2 billion litres between 2013 and 2018

244
Q

what is the biofuel production for india

A

1.4 billion litres between 2013 and 2018

245
Q

what is the biofuel production for Europe

A

4.5 billion litres between 2013 and 2018

246
Q

what are radical technologies

A

are new approaches using state of the art technology which aim to reduce carbon emissions in the near future.​

247
Q

radical technologies

A

hydrogen fuel cells
electric cars
carbon capture

248
Q

what are hydrogen fuel cells

A

Hydrogen is the most abundant element in the universe, but usually combined with other elements. Once separate it provides an alternative to oil. Using it in a hydrogen engine in a car produces no pollution, just water as a waste product, making it more efficient than petrol or diesel. Separating hydrogen from other elements requires energy, which could be provided from renewable sources. ​

249
Q

eg of hydrogen fuel cells

A

Toyota developed a car with a range of 270 miles, which went on sale in California in 2015.​
Toyota developed a car with a range of 270 miles, which went on sale in California in 2015.​

250
Q

advantages of hydrogen fuel cells

A

it’s not going to run out​
Produces no pollution – if renewables are used.​
Could reduce dependence on fossil fuels for transport​

251
Q

disadvantages of hydrogen fuel cells

A

Requires a large amount of energy to separate elements.​
Water vapour is considered a greenhouse gas, so an increase in water vapour could lead to an increase in temperatures.​
If renewable sources aren’t available then fossil fuels may be needed to separate the different elements.

252
Q

electric cars/vehicles

A

An electric car uses electric motors, using energy from rechargeable batteries. A charging station, either at home and in public areas are then used to charge these batteries. Electric vehicles range from 62-340 miles depending on battery capacity and linked technologies. They are potentially suited to urban environments, helping reduce city air pollution as their range can be limited. They produce zero emissions and virtually no noise pollution. They are cheaper to run than a normal car due to low maintenance. However they are more expensive to buy as well as being a potentially hazard to pedestrians because they are so quiet.​

253
Q

eg of electrical cars/vehicles

A

The Tesla Model 3 was the world’s best selling electric vehicle from 2018 to 2019 and had a maximum range of 310 miles.​
According to Zap-Map in April 2016 there were 3,919 public charging locations in the UK which had to serve over 60,000 registered electric vehicles, with London having nearly 20% of these charging points compared to Wales who had 3%.​

254
Q

advantages of electric cars/vehicles

A

cheaper to run than a petrol/diesel car​
Produces no pollution.​
Could reduce dependence on fossil fuels for transport.​
Massively reduced noise pollution compared to a petrol/diesel car. ​

255
Q

disadvantages of electric cars/vehicles

A

expensive to buy due to the technology​
Charging times are improving but can take a while for a full charge. ​The quietness could be a hazard to pedestrians​
The ‘greenness’ of an electric vehicle depends on the energy profile of the country e.g. using renewables or non-renewables for charging.​

256
Q

carbon capture and storage

A

A system that collects CO2 emissions from fixed points such as power plants, then transports the gas and injects it into a suitable geological structure (over 800m below ground). CCS could cut global CO2 emissions by 19% and could extend the use of fossil fuels as well as encourage greater efficiency. However it’s expensive as there is complex technology involved and it isn’t certain whether the CO2 will stay trapped underground as it may leak as well as potentially cause earthquakes because of the pressure.​

257
Q

eg of carbon capture and storage

A

Canada opened the first coal-fired power plant with CCS in 2014 at a cost of US$1.3 billion. It reduces emissions by 90%.​
carbon engineering

258
Q

where is carbon engineering based

A

British Columbia Canada

259
Q

how many trees worth of work does one carbon capture plant do

A

40 million

260
Q

in carbon capture what ‘captures’ the carbon dioxide

A

large fans and chemical solutions which the particles stick to

261
Q

what happens to captured carbon

A

Made into pellets and stored in the ground or used to make fuels.​

262
Q

How much does direct air capture cost per ton of CO2? ​

A

$94-232 ​

263
Q

It is believed carbon capture is needed to keep global temperatures from increasing by how much? ​

A

1.5 degrees C

264
Q

Some companies capture carbon at the source and store it underground, how much carbon has Shell’s carbon capture project ‘Quest’ sequestered? ​

A

4 million tonnes

265
Q

How much money did Carbon Engineering raise in it’s most recent funding bid? ​

A

$68 million.​

266
Q

California requires what % of reduction in carbon intensity of fuels by 2030?

A

20%

267
Q

By 2040 what is the estimated % of oil and gas being used for meeting energy demand? ​

A

50%

268
Q

Synthetic Fuel is another potential project Carbon Engineering are developing. How much less carbon would synthetic fuel emmit

A

Between 70-90% less than normal fuels.​

269
Q

What is the price on carbon per ton? ​

A

$5-20 per ton.​

270
Q

What is the carbon price in Norway per metric ton? ​

A

$50 or more ​

271
Q

What is the carbon price in Switzerland per metric ton? ​

A

$99.​

272
Q

Each year how much CO2 is emitted globally? ​

A

40 billion tons​

273
Q

how much land`have Brazil and indonesia lost as a result of growing resource demand

A

net loss of over 500,000 ha of land.​

274
Q

how much land have the USA and india gained as a result of growing demand for resources

A

USA and India have gained between 250-500,000 ha of land.​

275
Q

what are the generalised trends of land gain/loss due to growing demand for resources

A

The most land that has been lost is the southern hemisphere.​
The most land gained is the northern hemisphere. ​

276
Q

regional changes of forest area

A

Tropical forests have lost half of their area since the 1960s, particularly in Africa and South America. ​

277
Q

what has happened to Indonesias rates of deforestation

A

Indonesia has overtaken Brazil in terms of the rate of deforestation. Around 25% of the rainforest has been cleared or burnt in 25 years for palm oil and logging.​

278
Q

how has deforestaion impacted temperate forests

A

Temperate forests (e.g. in the UK and USA) have a long history of exploitation: 90% was deforested by the 19th century.​

279
Q

how has deforestation affected boreal forests

A

Boreal forests have been increasingly threatened since the mid-20th century e.g. by oil and tar sands production in Russia and Canada.​

280
Q

how have human activities impacted the carbon cycle

A

The terrestrial biosphere sequesters/stores about ¼ of CO2 emissions annually, directly slowing down global warming.​
Growing demands for food, fuel and other resources have led to contrasting regional trends of land conversion. ​
This land conversion changes the land from a natural ecosystem to an alternative use, which usually reduces carbon and water stores as well as soil health. ​

281
Q

what human activities have impacted the carbon and hydrological cycle

A

Deforestation of temperate, boreal and tropical forests ​
afforestation
grassland conversation

282
Q

by 2015 what % of all global forest cover had been cleared

A

By 2015 30% of all global forest cover had been cleared, 20% degraded and the rest fragmented​

283
Q

how many hectares of land are deforested annually

A

13 million hectares of land are deforested annually (36 football fields a minute).​

284
Q

what % of earths surface do forests cover

A

Forests cover 30% of earths surface but only 15% are natural​

285
Q

what is 50% of deforestation for

A

for soy, palm oil, beef and paper production​

286
Q

what causes deforestation

A

50% of all deforestation is for soy, palm oil, beef and paper production.​
Dams and reservoirs.​
Infrastructure.​
Open cast mining for rare minerals.​

287
Q

methods used for deforestation

A

Clear cutting – used for loggings, removes all primary forest. ​
Slash-and-burn – used for agriculture – trees and cut and set alight. Ash from the burnt trees provides nutrients in the soil.​

288
Q

impacts of deforestation on the carbon cycle

A

Reduction in storage in soil and biomass, especially above ground. ​
Reduction in CO2 intake through photosynthesis flux.​
Increased combustion flux to atmosphere by burning and decomposing vegetation.​

289
Q

impacts of deforestation on the water cycle

A

Reduced interception leading to changes in infiltration through the soil to ground water stores.​
Increased raindrop erosion and surface run off leading to more sediment in rivers.​
Increased aridity ‘downwind’ from loss of evapotranspiration. ​

290
Q

eg of deforestation

A

Since the 1950s Madagascar’s forests have been deforested at a rapid rate.​
This is due to an expanding population, growing demand for hardwoods and debt repayments. ​
The Madagascan government encouraged farmers to clear more land to grow cash crops.​
Before 1950 there were 11.6 million hectares of tropical forest but by 1985 it had reduced down to 3.8 million hectares. ​

291
Q

How much of the forest in Madagascar has been deforested?

A

90%

292
Q

Who is to blame for the mass deforestation in madagascar?

A

Industrial companies​

293
Q

What do the local people in madagascar use the forest for?

A

Charcoal for electricity and fuel, buildings.​

294
Q

Why are the forests in Madagascar so vulnerable?

A

Expanding population with no other resources, no international aid, no help/money from the government, people have to fend for themselves, growing international demand for tropical hardwood. ​

295
Q

What are the solutions to deforestation in madagascar?

A

External workers to work locally to provide an alternative solution for the local population. ​

296
Q

What are the negative impacts if the rate of deforestation continues in madagascar?

A

No remaining forest, long term droughts and extending monsoon seasons.

297
Q

what are the hydrological impacts of deforestation in madagascar

A

There are lots of impacts on rivers, landscapes and soil health:​
An increase in sediment has turned some rivers red – soil erosion now exceeds 400 tonnes per hectare per year in some areas.​
Extensive logging of inland rainforests and coastal mangroves means that, after heavy rainfall, soil is washed from the hillsides into streams and rivers and eventually clogs the coastal waterways with sediment. ​

298
Q

eg of a river in Madagascar affected by deforestation

A

the Betsibokar river Madagascar

299
Q

afforestation

A

planting trees on land that has never had forest, or has been without forest for a long time.​

300
Q

reforestation

A

planting trees in places with recent tree cover, replacing lost primary forests.​

301
Q

what is afforestation made up of

A

monocultures (1 single crop/species) such as palm oil. They often store less carbon, use more water and are disease prone.

302
Q

what is monoculture

A

is the agricultural practice of producing or growing a single crop, plant, or livestock species, variety, or breed in a field or farming system at a time​

303
Q

eg of afforestation

A

China’s Three-North Shelterbelt Project – a 4,500km green wall of trees designed to reduce desertification – demonstrates many of these issues.​

304
Q

impacts of afforestation on the carbon cycle

A

Monocultures of commercial trees such as in palm oil plantations often store less carbon although it’s better than having no vegetation at all.​
Biodiversity may be impacted as a result of habitat changes.​
Monocultures tend to be more disease prone having a negative impact on biodiversity.​

305
Q

impacts of afforestation on the water cycle

A

Monocultures tend to use more water leading to less infiltration and groundwater rates. ​
Decreased raindrop erosion.​
Evapotranspiration rates may alter surrounding downwind ecosystems. ​

306
Q

what are the two main types of grassland

A

temperate grasslands
tropical/savannah grasslands

307
Q

eg of grassland conversion

A

between 2007 and 2015, a biofuel ‘rush’ swept across the American Midwest – often referred to as the Prairies. ​
During this ‘rush’ farmers were encouraged to grow corn, soya, canola (a type of rapeseed) and sugar cane as part of the US Environmental Protection Agency’s Renewable Fuel Standard Policy
By 2013 the price of corn trebled, and a number of US states were cashing in. ​

308
Q

what did the US Environmental Protection Agency’s Renewable Fuel Standard Policy which aim to do

A

Increase the amount of ethanol being used in petrol​
Boost the economies of rural US states​
Reduce US dependence on overseas oil imports​
Reduce CO2 emissions from transport​

309
Q

grasslands

A

traditionally used for cattle ranching - were ploughed up, and in some states the area of corn being cultivated doubled.​

310
Q

what happened to grassland size between 2007 and 2015 in the USA

A

Over 5.5 million hectares of natural grassland disappeared across the American Midwest, which matches the rate of rainforest deforestation across Brazil, Malaysia and Indonesia.​

311
Q

benefits of natural grasslands

A

Trap moisture and floodwater​
Absorb toxins from the soil, maintaining their health.​
Providing cover for dry soils – preventing soil erosion.​
Maintain natural habitats.​
Acts as a carbon sink and a terrestrial carbon store. ​

312
Q

drawbacks of grassland conversion

A

Soils release CO2 when grasslands are initially removed and through annual ploughing.​
Biofuel crops need carbon-based nitrogen fertiliser and chemical pesticides, so they produce a net increase in CO2 emissions.​
Biofuels consume a lot of water, impacting on local aquifers for irrigation.
Cultivated soils are liable to erosion by surface runoff and wind​
Natural habitats lost​

313
Q

causes of the enhanced greenhouse effect

A

agriculture, industry, transport, deforestation, electricity generation, cement production, wetland/peatland loss.​

314
Q

consequences of the enhanced greenhouse effect

A

increase in frequency and intensity of storms and tropical storms; rising temperatures; rising sea levels; more frequent floods, droughts and heat waves. ​

315
Q

what is drought

A

An extended period of deficient rainfall relative to the statistical average of that region measured over a long period of time.​

316
Q

how does climate change cause drought

A

Shifting of global weather patterns​
Shifting climate zones​
Scientists at the University of Colorado have found that a warming of 2 degrees resulted in about 5% of the Earths land area effectively shifting into a new climate zone. ​
The pace of change then increases for the next 2 degrees of warming with an additional 10% of land area shifting to a new climate zone. ​

317
Q

general trends of risk of drought

A

Mid-latitudes in the northern hemisphere are at the most risk.​
Highly populated countries are at the highest risk of drought.​

318
Q

which european countries have high risk of drought

A

Moldova and Ukraine.​

319
Q

risk of drought for different areas

A

An expansion of subtropical deserts and a poleward movement of stormy, wet weather in the mid-latitudes
Changing snow/rainfall patterns and increasing temperatures in mountain regions could cause reliable streams/springs dry as well as melt glaciers resulting in a very little run off in the future. ​

320
Q

drought case study

A

the amazon basin

321
Q

in what years did the amazon basin suffer severe droughts

A

2005, 2010, and 2015-16

322
Q

how does the amazon basin play a key role in the earths carbon cycle

A

The Amazon Basin plays a key role in the Earth’s carbon cycle, holding 17% of the terrestrial vegetation carbon store.​

323
Q

impacts of drought in the amazon

A

Billions of trees died, releasing greenhouse gases.​
Rivers dried up, lots of fish died.​
The drier the forest gets, the less carbon it can store.​
Fires broke out – burning trees and litter releasing CO2.​
Decomposition of dead vegetation​

324
Q

how much c02 does the rainforest normally absorb

A

1.5 billion tonnes

325
Q

in 2005 how many tonnes of c02 were released from the amazon basin

A

5 billion tonnes

326
Q

in 2010 how many tonnes of c02 were released from the amazon basin

A

8 billion tonnes

327
Q

future concerns about drought in the amazon basin

A

There are further concerns that, as climate change increases temperatures and alters rainfall patterns across South America, the Amazon rainforest will change from a carbon sink to a carbon source – accelerating global warming. ​

328
Q

how many hectares of forest did deforestation affect between 2000 and 2010

A

13 million

329
Q

what is palm oil

A

Palm oil is the most commonly produced vegetable oil - used in foods like frozen pizzas and biscuits as well as cosmetics and biofuels. ​

330
Q

how much palm oil is produced each year

A

66 million tonnes

331
Q

what country is the largest producer of palm oil

A

Indonesia is the largest producer and in 2015 its GHG emissions overtook those of the USA. ​

332
Q

how many land conflicts were linked to palm oil in 2016

A

700
this was because indigenous and local people are often driven out of areas they have inhabited for generations.​

333
Q

how many people depend on forests

A

over 1.6 million people
and over 90% of these are the poorest in societies

334
Q

what % of global diversity are forests a source of

A

80%

335
Q

how did the UN descrive forests

A

fundamental to human wellbeing and survival

336
Q

what % of the global economy income do forests provide

A

1.1%

337
Q

how many formal and informal jobs do forests provide

A

13.2 million formal jobs
41 million informal jobs

338
Q

what do forests provide

A

water purification
Aesthetic, educational, spiritual, recreational​
Improve food and nutrition security​
Source of livestock fodder​
Goods: water, wood, fibres, fuels, foods​
Fuel wood source for 1/3 people globally for cooking and boiling water. ​
A genetic pool- a source for improving plant strains and medicines​
Nutrient cycling- soil formation and primary production ​
Help prevent flooding and landslides​
Maintains atmosphere through photosynthesis​

339
Q

forest recovery

A

Despite huge losses from deforestation each year, the rate of deforestation has slowed!​
Between 1990 and 2015 the rate of net global deforestation slowed down by more than 50% and total forest carbon emissions decreased by 25% according to the Food and Agriculture Organisation of the UN (FAO). ​
This change is particularly happening​

in developed countries. ​

340
Q

what is kuznets curve

A

A model that suggests that societies reach a tipping point where exploitation changes more towards protection. ​

341
Q

what factors affect the timings on kuznets curve

A

Wealth of countries​
Rising knowledge of the role the environment plays in human wellbeing​
Aid given to poorer nations to help choices over exploitation​
Political systems and enforcement of laws​
Participation of locals​
Power of TNCs​

342
Q

eg of forest protection

A

indonesia
In May 2011 Indonesia’s president declared a ‘forest moratorium’ - aimed at trying to reduce deforestation. They received $1 billion funding from the UN and Norwegian government. ​
The Moratorium stopped new lands getting forest clearance permits. ​
By 2013 emissions had fallen by 1-2.5%. However illegal logging is still an issue. ​
In 2015 the moratorium was extended to help Indonesia further reduce its CO2 emissions by 26% by 2020. ​

343
Q

what will help decrease the rate of deforestation

A

increased sustainable management

344
Q

what % of forests are now classed as conserved

A

13% of forests (534 million hectares)

345
Q

which countries have the largest national parks and forest reserves

A

Brazil and the USA

346
Q

which types of forests havce increased/decreased

A

Temperate forest areas (mainly in developed countries) has increased, although tropical rainforests (mainly in developing countries) has decreased.​

347
Q

what has happened to brazils deforestation rate

A

Brazil has halved it’s deforestation rate since 2000 but continues to lose forest.​

348
Q

what has forest cover in the UK dropped from

A

80%-10%
following centuries of exploitation

349
Q

what has the Forestry Commision done to combat the exploitation of forests in the UK

A

planted fast growing conifers like Sitka Spruce.
Forest cover increased by 25% between 1870 and 1947 and by 50% between 1948-1995. By 2016 13% of the UK was forested with increasing numbers of indigenous species being planted. ​

350
Q

why are oceans important for the carbon cycle

A

They are a major carbon sink:​
they have absorbed about 30% of the C02 produced as a result of human activities since 1800, and about 50% of that produced by burning fossil fuels.​
Due to this absorption the acidity of our oceans is changing which is a big problem.​

351
Q

what happens during acidification of oceans

A

During acidification, carbonic acid reacts with carbonate ions in the water to form bicarbonate. The higher the acidity, the more it dissolves carbonate shells​

352
Q

how has ocean acidification affected the pH of the ocean

A

Ocean acidification has lowered the pH of the ocean by about 0.1. That means that it’s now 30% more acidic than it was in 1750, before the Industrial Revolution. ​

353
Q

effects of ocean acidification

A

There are many important natural processes that are affected by the oceans acidity/alkalinity (pH). ​
Most biological activity and all photosynthesis takes place near the surface. ​
Changes in ocean chemistry has substantial direct and indirect affects on these organisms (such as their life cycle) and their habitat. ​
Marine photosynthetic organisms and animals such as corals, make shells and plates out of calcium carbonate (CaCO3). This process of ‘calcification’ is massively affected the less alkaline there is in the oceans. ​

354
Q

what is coral

A

is an animal which is like a small bag. The opening on top is the mouth. Tentacles (little arms) around the mouth carry a sting which paralyses small animals which are then eaten by the coral.​
When the animal dies, new polyps live on top of the older structure.​

355
Q

what gives coral its colour

A

algae

356
Q

what happens when coral becomes stressed

A

When coral becomes stressed, corals evict the algae, turning it white. If bleaching continues, the coral will die due to starvation. ​

357
Q

impact of ocean acidification

A

coral bleaching

358
Q

what causes ocean acidification

A

Increased amount of CO2 absorbed into the oceans producing more bicarbonate and increasing acidity of water. ​

359
Q

What was the pH of the oceans in the late 1800s?

A

8.2​

360
Q

What is the projected pH of the oceans by 2100?​

A

7.8​

361
Q

What is the temperature range that coral survives best in?​

A

23-29˚C​

362
Q

What is happening to the trend of coral bleaching? ​

A

It’s increasing and is occurring more frequently. ​

363
Q

what are the consequences if rising temperatures

A

ocean acidity
rising temps= increased rates of evaporation

364
Q

what does rising temps and therefore rising rates of evaporation impact on

A

precipitation patterns
river
water stores (cryosphere and drainage basin stores)

365
Q

how does rising temperatures impact precipitation pattersn

A

Existing weather patterns will get stronger (wet places will get wetter and dry places will get drier). ​
This is because warm air traps more water – scientists expect more water to fall on wet places.​

366
Q

how does rising temperatures impact river regimes

A

‘the annual variation in discharge or flow, at a particular point’.​
The character of the regime is influenced by climate.​
Increased temperatures = more snow/glacier melt, and an increased in the amount and intensity of precipitation

367
Q

how does rising temperatures impact water stores

A

Cryosphere has been losing mass as ice sheets and glaciers melt.​
Arctic temperatures have risen twice as fast as global averages in the past 20 years.​
This means huge implications for ocean currents, air circulation, sea level rise and flooding.​

368
Q

which river has rising temperatures impacted

A

Yukon is a territory in the far northwest of Canada and a significant part of it lies within the Arctic Circle.​
Like most Arctic and sub-artic areas it has seen temperatures rise sharply, and forecasts are for continued warning.

369
Q

How has The increasing temperature had implications for precipitation patterns, river regimes and water stores in the yukon basin

A

Increasing temperatures lead to increased evaporation and atmospheric water vapour.​

370
Q

what has happened to winter precipitation in yukon

A

Across Yukon, winter precipitation increased between 1950 and 1998. However a greater proportion fell as rain in spring and less as snow (as previously).​

371
Q

what has happened to snowmelt in yukon

A

Snowmelt now begins earlier and snow cover is decreasing. This alters river regimes, bringing earlier peak flows to most river basins.​

372
Q

what happened to the total ice area in yukon between 1958 and 2008

A

shrank by 22%
and, as glaciers recede, streamflow is decreasing – despite an initial increase in meltwater.​

373
Q

what is happeneing to permafrost in yukon

A

Climate change is leading to thawing of permafrost – so water penetrates deeper into the soil, instead of forming surface runoff.​
As the permafrost thaws, climate change could increase the amount of groundwater. ​

374
Q

by what % have inflows into the yukon river increased by since 2000

A

Since 2000, inflows to the Yukon river have increased by 39% due to increasing temperature and precipitation.​

375
Q

how have rising temperatures impacted the arctic

A

Over the last 20 years the ice sheets in the Antarctic and Greenland ice sheets have been losing mass and the Arctic sea ice and northern hemisphere spring snow cover have continued to decrease in extent and thickness.​
The Arctic acts as an early warning system, acting as a barometer of the environmental impacts resulting from fossil fuel use.​

376
Q

what has happened to average arctic temperatures in the past decade

A

In the past few decades, average Arctic temperatures have risen twice as fast as global averages: 3-4- degrees in Alaska and north-west Canada. ​
Which could soon increase another 4-5 degrees over land, and 7 degrees over the ocean. ​

377
Q

effects of rising temperatures on the water cycle

A

Warm water flowing into the Arctic from the Pacific and Atlantic.​
Rising local temperatures – increased evaporation.​
Shrinkage of sea ice; the Arctic ice cap averages only 3m thick and melting is increasing faster than anticipated.​
Run-off of fresh, cold water which will alter marine ecosystems and food chains dependent on the saline waters; predicted to affect areas outside the Arctic Ocean by 2100.​
Funnelling of more cold water into the oceanic conveyor belt.​

378
Q

effects of rising temperatures on the carbon cycle

A

Increased or new emissions of: CH4 (methane) from destabilisation of wetlands and sea floor deposits containing methane hydrate, stored for thousands of years.​
Increased or new emissions of: mainly CH4 and some CO2 from thawing permafrost.​
Increased or new emissions of: CO2 from increased forest fires as boreal forests dry out; they may also absorb CO2 and CH4 from the atmosphere.​

379
Q

where are mangroves found

A

Mangroves are found along tropical and sub-tropical coasts of Africa, Australia, Asia and the Americas.​

380
Q

How much carbon do mangroves sequester per hectare, per year?​

A

They sequester almost 1.5 metric tonnes of carbon per hectare, per year. ​

381
Q

How is it that very little carbon is respired into the atmosphere from mangroves?​

A

Their soils consist of thick organic layers of litter, humus and peat, which contain high levels of carbon – over 10%.​
As they are submerged twice a day by high tides their soils are anaerobic (without oxygen), bacteria and microbes can’t survive without oxygen so decomposition of plant matter is slow – meaning little carbon is respired back into the atmosphere so is stored for thousands of years.​

382
Q

In what ways do mangroves protect coastlines?​

A

Mangroves can provide many benefits to our communities:​
they stabilise the coastline against erosion.​
They provide protection and shelter against extreme weather (e.g. storms winds and floods) and tsunamis, by absorbing and dispersing surges.​

They provide nurseries for coastal fish away from predators.​

383
Q

How much of global mangrove forests have been lost since 1950?​

A

globally half of all mangrove forests have been lost since 1950.​

384
Q

What percentage of forests have been lost due to draining and clearing mangrove forests for tourism, shrimp farming and aquaculture?​

A

We are draining and clearing mangrove forests for tourism, shrimp farming and aquaculture – this has accounted for over 25% of the loss of the forests.​

385
Q

How many people does fishing support?​

A

The FAO (Food and Agriculture Organisation) estimates that fishing supports 500 million people, 90% of which are in developing countries.​

386
Q

Fish provide 16% of the annual protein consumption for how many people?​

A

Fish provide 16% of the annual protein consumption for 3 billion people, and is the main source of cheap protein for 3 billion people.​

387
Q

What % of marine species do coral reefs shelter?​

A

Coral reefs shelter 25% of marine species.​

388
Q

What is happening to marine organisms in the North Sea?​

A

Research carried out in the North Sea, suggests that marine organisms may be responding faster to climate change then terrestrial plants and animals, with some shifts of animals and some plants towards the poles to compensate for a warming environment. ​

389
Q

How much have krill stocks declined by in some parts of the Southern Ocean? ​

A

. Arctic krill stocks (food for whales) are declining by up to 75% per decade in some parts of the Southern Ocean.​

The main cause of damage has been climate change, added to reefs being lost by coastal pollution caused by industrial and agricultural runoff.​

390
Q

egs of degradation of the carbon cycle

A

egs- madagascar, amazon rainforest, indonesia
land conversions-
deforestation eg madagascar
afforestation eg palm oil
grassland conversion eg american midwest

391
Q

implications of degradation of the carbon cycle for human well being

A

Loss of various activates, resources, less maintenance/regulation of atmosphere/carbon cycle = increase mental health difficulties, loss of education (etc.)​
Increased CO2 in atmosphere – rising temperatures = global warming.
Loss of suitable farmland due to soil erosion, lack of nutrients, spread of disease – difficult with an increased population​
Social, economic, environmental ​

392
Q

implications for degredation of the water cycle on human wellbeing

A

Increased amounts of drought – less trees = less water vapour in atmosphere. Amazons pumps 20 billion metric tonnes of water into atmosphere daily. Since 1990 more extreme droughts & flooding due to climate shifts (e.g. Amazon)​
Increased amounts of flooding​
Coral reef and marine species loss = loss of habitats for fish, food sources for people and loss of tourism industry e.g. Great Barrier Reef.​
Mangrove loss – loss of coastal protection/stabilisation.​
Social, economic, environmental ​

393
Q

what do climate scientists predict will happen to surface temperatures

A

Climate Scientists predict that surface temperatures will continue to rise, with increases between 2000-2100 in the range of 2-6°C.​

394
Q

why are Future emissions, atmospheric concentration levels and climate warming uncertain

A

physical factors
human factors
feedback mechanisms

395
Q

physical factors causing uncertainty

A

Oceans and forests act as carbon sinks.​
Their response to increased GHG emissions and higher temperatures will continue to affect the global climate for possible hundreds of years.​
Deforestation - overall the amount of forested land is on a global decline.​

396
Q

what human factors will lead to uncertainty

A

economic growth
energy source
population change

397
Q

how will economic growth lead to uncertainty

A

After economic crashes, e.g. the 2008 Financial Crash, there is an expectation that they’ll be a rise in emissions during recovery of global GDP. Fortunately after 2008, emissions fell to 1% by 2012-13 down from 4%, then fell to 0.5% in 2014. Total carbon emissions still reached a record high. ​

398
Q

how does energy source lead to uncertainty

A

Energy consumption grew by 2% between 2008-2014. However renewables made up two-thirds of the increase in electricity production in 2015.​

399
Q

how does population change lead to uncertainty

A

Increasing affluence means a potential extra billion consumers by 2050. Changing diets and increase mobility means more emissions.​

400
Q

eg of economic growth

A

By 2014 the three largest CO2 emitters were China, the USA and India. In 2000, China overtook the USA because of a global shift in manufacturing projections and its rapid urbanisation and industrialisation. ​
In terms of CO2 per capita, China is ranked 55th at 6.23 metric tonnes per capita; the USA 8th at 17.6 and India 127th at 1.7 – reflecting the level of economic development, with a positive relationship between economic growth and CO2 emissions

401
Q

how do feedback mechanisms lead to uncertainty

A

Feedback mechanisms can either dampen (negative feedback) or amplify (positive feedback) responses to a changing climate.​
Peatlands: Warming causes peat to dry out as water tables fall, increasing decomposition rates and releasing methane. A warming of 4˚C causes a 40% loss of soil organic carbon from shallow peat, and 86% from deep peat.​
Permafrost: The melting of permafrost releases trapped CO2 and methane.​

402
Q

what is a tipping point

A

A climate tipping point is a critical threshold whereby a carbon sink could become a carbon source.​

403
Q

what Two particular phenomena are capable of creating tipping points ​

A

forest die back
Changes to thermohaline circulation​

404
Q

forest dieback

A

Rainfall in the amazon basin is largely recycled from moisture within the forest. If the rainforest is subject to drought, trees die back.​
A tipping point can be reached when the level of die back actually stops the recycling of moisture – resulting in further die back. ​

405
Q

thermohaline circulation

A

Cold, deep water in the North Atlantic forms part of the thermohaline circulation.​
To keep the ‘conveyor belt’ of warm water heading from the Tropics towards Britain, heavy, salty water must sink in the north.​
However, melting of ice sheets release large amounts of freshwater (less salty meaning its lighter) into the ocean – blocking and slowing the conveyor down.​
As ice sheets melt, the ocean circulation is susceptible to a critical tipping point. ​

406
Q

what two approaches for the future did the IPCC outline

A

adaption
mitigation

407
Q

methods of mitigation

A

carbon taxation
renewable switching
energy efficiency
afforestation
carbon capture and storage

408
Q

carbon taxation

A

the carbon price floor tax sets a minimum price companies have to pay to emit c02
it was unpopular with both industry and environmental groups and had debatable effects on emmisions
in 2015 the policy was ‘frozen’
lower road taxes for low carbon emmiting cars were scrapped in 2015
in 2015 oil and gas exploration tax relief was expanded to support fossil fuels hence the fracking debate

409
Q

renewable switching

A

the relationship between big energy providers and the government dictates the amount of switching from fossil fuels to renewables and nuclear power
renewables (solar, wind and wave) provide intermmittent electricity while fossil fuels provide the continuos power essential for our current infrastructure
The Climate change levy designed in 2001 to encourage renewable energy investment and use was cut in 2015

410
Q

energy efficiency

A

the green deal scheme encouraged energy saving improvements to homes such as efficient boilers and lighting and improved insulation- was scrapped in 2015
energy suppliers must comply with the energy company obligation scheme to deliver energy efficient measures to householders

411
Q

afforestation

A

tree planting in the uk is increasing, helping carbon sequestration
it involves the forestry commision, charities such as the national trust and woodland trust, landowners and local authorities
the big tree plant campaign encourages communities to plant 1 million trees mostly in urban areas

412
Q

carbon capture and storage

A

few actual geologic CCs projects exist globally despite its potential
Canadas Boundary dam is the only large scale working scheme
in 2015 the uk government cancelled its investment into full scale projects at gas and coal powered plants in Peterhead in scotland and Drax in yorkshire respectivley

413
Q

what does mitigation need to be succesfull

A

mitigation needs agreement at national, global and individual scales. ​

414
Q

what are the 4 different players in global agreements and national action on mitigation

A
  1. Global - UN roadmaps and goals e.g Kyoto protocol
  2. National- TNCs. Shell’s research and management as well as groups like Greenpeace.
  3. Local - Winchester’s WinACC who lobby for local changes in attitude and actions​
  4. Public - online e-petitioning e.g the 38 degrees campaign. ​
415
Q

global players in mitigation

A

Global - UN roadmaps and goals​
A roadmap is a essentially a ‘toolbox’ - a collection of guidance and advice.​
The UN has a roadmap to help local areas and communities take part in and work towards the Sustainable Development Goals (SDGs). It covers a range of strategies that can be adapted to the specific contexts and needs of different cities ad regions. ​
The UN SDG Roadmap has 5 parts: awareness raising; advocacy; implementation; monitoring; and where do we go from here?​
It aims to support local and regional governments and their associations to implement and monitor the SDGs and to influence national policy-making with a view to creating an enabling environment for action at local and regional level. ​

416
Q

role of national players in mititgation

A

National - TNCs. Shell’s research and management as well as groups like Greenpeace ​
Shell​
Invested heavily in the lowest-carbon biofuel, through a joint venture with Cosan in Brazil as well as supporting second-generation biofuel options.​
‘New Energies’ business was created in 2016, aiming to explore investment opportunities in energy solutions that combine wind and solar power with gas.​
‘Shell Ventures’, established in 1996 invests in start-ups and small/medium enterprises to encourage scale and growth. There focused is mixed, however renewables is an area receiving investment. Specifically supporting customers meeting their personal energy use, as well as investing in wind and solar and storage solutions. ​
Greenpeace​
An international organisation founded in 1971.​
Has the aim of having a green and peaceful world and work on several priority campaigns such as: fossil fuels; deforestation; ocean plastic. ​
Greenpeace investigates those responsible for environmental crime and work with affected communities to identify solutions.​

417
Q

local players in mitigation

A

Local - Winchester’s WinACC who lobby for local changes in attitude and actions​
A local environmental organisation that ‘thinks globally’ but ‘starts locally’.​
WinACC began in 2007, seeking to influence behaviour change at the grassroots (local) and policymakers level, becoming successful on a variety of community projects and the priority given to climate change by Winchester City Council. ​
The group works with the local council to lower the carbon footprint of the Winchester District by inspiring sustainable living. They work with a variety of people including local residents; businesses; educators; and policy and decision makers. ​
There aim is to cut the carbon footprint of Winchester District by 60% by 2030 and to ensure that at least 15% of the energy used in the district comes from local renewable sources by the end of 2020.​

418
Q

public players in mititgation

A

Public - online e-petitioning e.g. the 38 degrees campaign. ​
38 Degrees is an online campaigning organisation, involving more than 2 million people from every corner of the UK. ​
The organisation was launched in 2009 and is a not-for-profit company.​
It aims to empower citizens by providing easy ways for people to take action against issues that they care about, including climate change.​

419
Q

what is the kyototo ptotocol

A

an international agreement linked to the United Nations Framework Convention on Climate Change, which commits its parties by setting internationally binding emission reduction targets.​
Recognising that developed countries are principally responsible for the current high levels of GHG emissions in the atmosphere as a result of more than 150 years of industrial activity, the protocol places a heavier burden on developed nations under the principle of “common but differentiated responsibilities.”​
The Kyoto Protocol was adopted in Kyoto, Japan, on 11 December 1997 and entered into force on 16 February 2005. The detailed rules for the implementation of the Protocol were adopted at COP 7 in Marrakesh, Morocco, in 2001, and are referred to as the “Marrakesh Accords.” Its first commitment period started in 2008 and ended in 2012.​

420
Q

successes of the kyoto agreement

A

operates until 2020, it started a global approach to tackling anthropogenic climate change, it was the beggining of regular UN conferences on climate change
the clean development mechanism supports 75 developing countries in developing less polluting technology
kyoto paved the way for new rules and measurements on low carbon legislation such as the uks 2008 climate change act, china is slowing emmisions (may be due to an economic downturn and greener energy)
by 2012 emmisions were 22.6% lower than 1990 levels well beyond the 5% goal, however 2015 showed a 65% increase above 1990 levels mainly driven by india and china

421
Q

failures of the kyoto agreement

A

slow ratification, the uk was one of the first but others struggled (russia) or withdrew (usa, canada and japan) fearing economic impacts
only industrialised countries were asked to sign, not developing nations, the top emmitters- the usa and china- were left out of the agreement
complex trading systems were started allowing the trading of ‘carbon credits’, buying emmisions allowances from countries not needing them, carbon sinks were allowed to offset emmisions- both these are criticised for allowing polluters to pollute
emmisions reductions may be because of other factors such as cheaper gas replacing coal and a global shift of manufacturing from MEDcs to the global soth

422
Q

paris agreement COP21

A

195 participating countries agreed to the landmark Paris Climate Agreement in November 2016, accounting for 66% of global emissions.​
It was the first universally legally binding global climate deal
There was an overarching aim: to limit temperature increase to 1.5°C above pre-industrial levels.​
Countries set their own goals to reduce emissions. ​
Countries should honestly report their progress every 5 years. ​

423
Q

advantages of the paris agreement

A

Countries can set their own individual targets
195 countries signed up.​
Individual targets all work towards of limiting temperature increase to 1.5˚C above pre-industrial levels. ​

424
Q

disadvantages of the paris agreement

A

No punishment if targets aren’t met
Signing the agreement and acting on it are two different things
A national effort is required for targets to be met, including public backing, which can be tricky
Progress reporting may not be accurate.​
Not a truly global agreement as developing countries are omitted that haven’t created the pollution.​

425
Q

COP26 paris agreement- follow up

A

The COP26 summit brought parties together to accelerate action towards the goals of the Paris Agreement and the UN Framework Convention on Climate Change.​
This meeting reviewed the plans and updates submitted from countries, reviewing how they will reduce their emissions – these are known as nationally determined contributions (NDCs).​
COP26 concluded that all countries agreed to keep the 1.5°C target and the ‘Glasgow Climate Pact’ means that the 1.5°C remains in sight and scales up action on dealing with climate impacts, but it will only be delivered with concerted and immediate global efforts

426
Q
A