Carbon - 3.1-3.4 Flashcards

1
Q

3.1 overall

A

Increased human use for resources is putting strain and imbalance on biosphere, carbon and water cycles

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2
Q

How has the biosphere changed? 1

A

• Mainly for commodity prod
• Also land conversion
• 30% of global forest cover cleared, 20% degraded, and rest fragmented
• Energy use has increased (54%), population has increased 36%

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3
Q

How has the biosphere changed? 2

A

• Developed countries use 50% of world’s energy, with N America being highest per capita – 10x Sub-Saharan Africa
• UK / USA temperate forests have the highest amount of clearance – 90% destroyed by 19th century
• Boreal changed later: since 1950s – oil/tar sands in Russia and Canada
• Tropical – mainly Indonesia for palm oil production and logging.

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4
Q

Water cycle impact on this changing biosphere

A

• Transpiration from vegetation to the air
• Vegetation slows surface runoff and through flow.
• Interception of rainfall, increasing evaporation rates.
• Root systems increase rates of percolation.

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5
Q

Soil health impact on biosphere

A

• need decomposing veg and roots, to release methane into atmosphere, add nutrients into soil
- Other vegetation: Provide humus for soil formation, Protects against soil erosion
• Fixes (draws down) nitrogen from the atmosphere

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6
Q

Carbon cycle impact:

A

• Photosynthesis – take in CO2, emit O2, by low lying plants, leaves & shallow roots
• veg acts as a carbon sink
- Forest fires release trapped carbon + Also remove litter which could’ve decomposed
• Lack of water makes decomposition harder
• Dry soils emit CO2 – whilst wet soils store 3x the amount of carbon than vegetation

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7
Q

Management of this changing biosphere

A

• IPCC thinks low-emission food crops, reducing food water, changing diets will help reduce food consumption
• Don’t get rid of any more undisturbed waterlogged peat soils (25% global storage)
• Restore degraded soils + afforestation
• fallow periods – retains soil moisture + organic matter.
• BUT: dangers of monoculture – e.g. commercial trees store less carbon, use more water and disease prone, e.g. China Green Wall

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8
Q

Why are some countries involved in afforestation, while others in deforestation

A

Idea of development level, as countries who have developed over the last 20 years will have had to go through the short term environmental loss, but countries like the UK experienced this same loss many decades before, so now can the economic growth from this original revolution sparks neoliberal thinking, which urges them to protect their environment with the money generated from economic growth. (Kuznets concept)

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9
Q

West Africa forest management project

A
  • IGO project, between 11 countries and 15km wide, requires political unity
  • building a great green wall
  • Senegal has planted 11 million trees
  • dry wells are filling up again, new economy sector developing and school attendance increased
  • £8 billion cost
  • more protected soil because more roots fro, trees - less soil degradation from wind
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10
Q

China great green wall project

A
  • to stop the advancements of the Gobi desert, the desertification and the degradation of arid/ semi arid ecosystems
    Desertification caused by deforestation and unsustainable agricultural practices has led to expansion of gobi desert
  • tree planting project, wall of veg lining edges of gobi desert.
  • Planned to finish by 2050 and plant 100 billion trees through aerial seeding and incentivising land owners to plant seeds
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11
Q

Pros of China project

A
  • has evidenced some mitigated desertification
  • huge carbon sink
  • reduced dust storm intensity
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12
Q

Cons of China project

A
  • some studies have shown further degradation of soil
  • reduction in groundwater availability due to trees
  • no consideration if different tree types for different regions in China.
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13
Q

3.2 overall

A

Fossil fuels acidify the ocean, ruining this carbon sink

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14
Q

Polyps

A
  • tiny, soft bodied - feed on phytoplankton
  • Protected by limestone, skeleton
  • Attached to rocks on the sea floor
  • Divide into thousands of clones
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15
Q

Key point. Regarding carbon and ocean

A

Photosynthesis draws down and uses CO2

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16
Q

What is ocean acidification?

A

• Sea is a carbon sink: absorbing CO2 (sea has 50x storage than land)
- so it could absorb 30% of GHG
• This creates a weak carbonic acid –i.e. the ocean becomes less alkaline
• Fossil fuels make this more intense

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17
Q

How does it cause bleaching?

A

• Carbonic acid reacts with carbon ions – leaving more bicarbonate ions
• so corals need more energy to build shells become thinner / fragile
• More acidic water dissolves protective carbon shells

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18
Q

Can it be natural?

A

• In the deep oceans , there is less photosynthesis - CO2 builds up.
• CO2 is also produced near volcanic vents

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19
Q

Can ocean acidification be made worse?

A

• Combined with warmer temperatures, destructive cyclones, and pollution
• BUT: phytoplankton growth is good for coral

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20
Q

When will ocean acidification cross the threshold?

A

• when the stress is so high that resilience is lost
• E.g. SST being too high
• E.g. pH < 7.8

21
Q

Positive feedback:

A

• Ocean acidification
• Decreased in dimethyl sulphide (produced by phytoplankton)
• Less sulphur compounds in atmosphere
• Less cloud condensation nuclei
• Less cloud cover
• Less sunlight reflection

22
Q

3.3 overall

A

Ecosystems are stressed, leading to drought and forest loss but not always

23
Q

Thermohaline shut down

A
  • hypothesised effect of CC on major ocean circulation
  • higher co2 emissions from anthrop = higher temps = higher glacial melt = higher freshwater input - less saline conditions
  • as THC depends on water density differences, and for the colder water to absorb more, become denser and sink, higher temp - reduce the density differences
    = thermohaline shutdown
  • huge impact on marine life as no utrients, higher occurrence of anorexic events, and drastic temp fall could lead to ice age
24
Q

Impacts of deforestation

A

• Palm Oil – Indonesia
• Loss of habitats
• Leaching
• Soil erosion into rivers

25
Q

Impacts on atmosphere and hydrosphere processes

A

• Hydrological cycle changes: inputs and outputs, i.e. trends in precipitation and evaporation.
• Soil moisture levels change, as well as rates of runoff and stream flow.
• Increased uncertainty over the security of water supplies.
• Increased frequency of drought due to shifting climate belts

26
Q

Impacts on biosphere processes

A

• Ocean and terrestrial photosynthesis regulates the composition of the atmosphere.
• Stored carbon influences soil health and ecosystem productivity.
• Forest health will deteriorate because of water stress

27
Q

Implications for wellbeing of ecosystems

A

• The health of wetland ecosystems are also likely to deteriorate and could suffer irreversible damage.
• Communities reliant on wetland ecosystems are threatened by increased food insecurity.
• Communities particularly in LHD are reliant on forests for fuel, medicines etc will lose vital ecosystem services

28
Q

What changes attitude?

A

• Increased wealth of countries
• Rising knowledge of the importance of the environment in human well-being
• Political systems – when environmental laws are enforced.
• Locals participation in designing (and managing) management systems
• Power and influence of TNCs

29
Q

What does Kuznetsk curve show the timeline of

A

the relationship between an economies growth and its environmental degradation levels

30
Q

Kuznets curve aligns with modern sociological theory

A

which allude to the idea that as an economy develops, they tend to pay more attention to the human rights and environment of their country, and invest in it to fix it

31
Q

The argument can then be made that if countries will follow Kuznets __

A

why not let all countries follow the trend and reach the turning point, just like the western countries have done in the 20th century?

32
Q

Why are people motivated to protect forests?

A
  1. Drought frequency increase - 1 per 10 years in 1911, to yearly mega drought in 2011
  2. Visible dieback of forest - 30% damaged, 5% visibly
  3. 10% drop in photosynthesis as less co2 absorbed
  4. Wildfire co2 emission increase
33
Q

Why are people motivated to protect forests 2

A
  1. Aerosols and wind blown soil cause poor air quality, leading to respiratory Illnesses
  2. 180% increase of hospitalisation, particularly under 5s
  3. loss of ancestral land for the ayoreo in Paraguay
34
Q

3.4 overall

A

The arctic is degraded, with alterations water flow creating unusual geomorphological landscapes

35
Q

Batakgiata Crater

A

• Growing wider 33ft/year
• Melting began in 1960s, helped by deforestation, sun warming soil, ice melts, trees sink, don’t shade
• Damages pipelines, cracks pavement, swallows houses
• Potential release of 50% of methane

36
Q

Changes at the artic

A

• Arctic ponds dry up
• Humidity increases
• Increased melting of ice/snow/permafrost, particularly in spring
• More runoff
• More local river-ice flood

37
Q

Changes in carbon cycle

A

• CH4 from wetlands / sea floors / permafrost
• CO2 from forest fires
• Removal of sink and fires become a source of CO2
• High latitudes have warmed more than twice as fast as the global average.
• Thawing and degradation of permafrost, and hydrologic shifts that include earlier snowmelt and higher river discharge

38
Q

Kuparuk River, Alaska

A

• Mean annual flow has increased by 35% since the 1970s
• Snowmelt floods now arrive earlier.
• Floodwater is warmer, and the heat is transferred into the permafrost (which thaws)
• Old carbon is released from the Arctic floodplains into the atmosphere
- base is melting, which destabilises the infrastructure for community

39
Q

Positive feedback loop from permafrost melting

A

Melt - more carbon - higher temp - more temp

40
Q

Green wall of China facts.

A

• Over-exploitation of land (deforestation for agriculture) led to increasing desertification in NW China.
• 3,600km2 of grassland overtaken by Gobi Desert every year!
• Three-North Shelterbelt program: human-planted wind breaking forests –“afforestation”
• Begun in 1978
• Designed to hold back expansion of Gobi Desert
• 4,500 km long and due for completion in 2050

41
Q

Ocean acidification and coral reefs

A

Slows the rate at which coral reefs generate calcium carbonate, thus showing the growth of coral skeletons, thus making them more vulnerable to any damage

Also coral reefs are threatened by the rise in surface water temperatures, as seen with the widespread bleaching of the Great Barrier Reef

42
Q

Ph and ocean acidification

A
  • Ocean acidification involves a decrease in the ph of oceans, caused by the uptake of carbon dioxide from the atmosphere, released by burning fossil fuels.
  • Average ocean ph has fallen from 8.2 in early 1800s, to 8.1 in 2015, coral reefs stop growing when pH is less than 7.8 - a big risk
43
Q

Growing resource demands

A
  • Deforestation levels: +500k hectares in china from 90-15, 250-500k in India, but Brazil + Indonesia had -500k hectares
  • Grassland conversion: Temperate and tropical grasslands have also become heavily exploited by agriculture, both grassland types have suffered due to overexploitation.
  • Urbanisation: removing space to urbanise means many ecosystems completely destroyed by the insatiable demand for space, not only are carbon sinks lost, but urban tends to mean an area of concentrated GHG emission as well as intense water demand
44
Q

Impacts of forest loss:

A
  • Sequestering co2 from atmosphere
  • Storing carbon
  • Transferring moisture from the soil back into atmosphere by evapotranspiration
45
Q

Link this cc to kuznet

A

Theory seems to correct in suggesting that as countries reach higher levels of development and wealth, societies approach a tipping point when the costs of resource exploitation become fully realised.

46
Q

China and kuznet

A

China in 20th century = increase in income + environmental degradation, rising income worsened these impacts, china beginning to slow down rate of environmental degradation, and are gradually bringing in climate related schemes

47
Q

In reality fix to CC

A

In reality, saving climate depends on the fact that different players have different attitudes towards sustainability and environmental issues. Attitudes are largely determined by motives, so it could be argued that if these are economic, then their attitudes towards the environment may not be sympathetic

48
Q

UK kuznet

A

Uk went from 80% forest centuries ago, to <10% at the end of 1800s, to now 13% as uk developed and implemented forestry commission

49
Q

The arctic:
Plays an important role, as its sea ice regulates evaporation and precipitation.

A
  • Temps here have risen twice as fast as global average
  • There has been a considerable loss of sea ice, e.g. north west passage is now open to summer navigation
  • Much melting of permafrost
  • Carbon uptake by terrestrial plants is increasing due to a lengthening growing session
  • Loss of albedo as ice that once covered land surface gives way to tundra, which gives way to taiga. Sunlight that was previously reflected back into space by white surface is now being increasingly absorbed by the ever darkening land surface, encouraging climate warming.