Carbon - EQ3 - 6.9 - Feedback Mechanisms Flashcards

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1
Q

When does feedback occur

A
  • when an output change is redirected back to an input
  • a positive feedback cycle increases change while a negative one decreases change
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2
Q

Describe the impilcations of the feeback mechanism from carbon from peatlands & permafrost

A
  • Boreal and tundra biome and climate areas will shift northwards as temperatures increase
  • Peatlands and permafrost within these will release methane with drying or melting, which traps more heat, causing further drying/melting
  • These organic layers are a large carbon store, with faster decomposition in a warmer climate that releases more CO, to the atmosphere.
  • More soil carbon is also released into rivers
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3
Q

Describe the impilcations of the feeback mechanism from Forest Dieback

A
  • Tropical rainforest areas could become drier and change to less productive grasslands, so absorb less CO, from the atmosphere - warming will increase, causing more dieback
  • Drought stress in boreal forests, with more disease, pests and wildfires, could change it to grassland and shrubs
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4
Q

Describe the impilcations of the feeback mechanism from Thermohaline Circulation Changes

A
  • More freshwater (for example, from melting of the Greenland ice sheet), changes seawater density, which changes ocean currents
  • For example, in the North Atlantic this may cause the Gulf Stream not to flow as far north
  • Such circulation changes could change how the oceans and atmosphere transfer heat energy, causing greater warming and more ice melt
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5
Q

What are peatlands

A
  • Peatlands are carbon-rich wetlands which occupy 3% of the global land surface and 12% of UK land area
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6
Q

Consequences of climate change for the peatlands

why are peatlands important

A
  • peatlands have a net cooling effect on climate, reduce flood risk, and support biodiversity
  • healthy peatlands can reduce flood risk by slowing the flow of water from the uplands, and by providing floodplain storage in the lowlands
  • they also provide important nesting and feeding grounds for many wading birds, as well as important habitats for rare insects and plants
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7
Q

Consequences of climate change for the peatlands

Are peatlands a carbon store or sink

A
  • Peatlands store vast quantities of carbon - ‘locking in’ an estimated 3.2 billion tonnes in the UK alone,
  • However, overall, peatlands in the UK and around the world are estimated to be a net source of greenhouse gas emissions to the atmosphere, as opposed to a net sink,
  • due to the way they have been managed now and in the past
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8
Q

Consequences of climate change for the peatlands

What is the impact of peatland degredation

A
  • Draining the soil so it is not waterlogged, in order to make it suitable for crop and tree growth —> decomposition of plant material and soil shrinkage —> source of COz emissions into the atmosphere.
  • drainage means the land surface reduces an average of 1cm to 2 cm per year through subsidence due to peat oxidation
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9
Q

Consequences of climate change for the peatlands

How many greenhouse gas emissions are UK peatlands producing

A
  • emissions from peatlands could exceed the equivalent of around 20 million tonnes of COz each year
  • globally, scientists estimate peatlands are emitting the equivalent of 1-2 billion tonnes of COz, which is around 2-4% of all human greenhouse gas emissions
  • a large proportion of these emissions are being produced by the tropical peatlands of Southeast Asia.
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10
Q

Uncertainties about peatlands

Why is peatland exploited by humans

A
  • farmers and foresters have drained large areas of upland and lowland peat throughout the UK
  • Large areas of upland bog have also been drained for conifer forestry and livestock grazing,
  • while other areas are rotationally burned as part of grouse shooting estates
  • growing medium by the horticulture industry and by gardeners
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11
Q

Uncertainties about peatlands

With climate change, how would peatlands change from extreme weather

A
  • Drying out the peat soil allows shrubby vegetation to grow, and makes the land more vulnerable to severe wildfires
  • Fire (caused by managed burning, accidental spread or arson) also produces CO2
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12
Q

Uncertainties about peatlands

how is semi-natural peatland peatlands expected to be change by climate change

A
  • 41% of the UK peat area remains under semi-natural peatland vegetation,
  • but has been affected by human activities including drainage, burn-management, livestock grazing and the cutting of peat for fuel
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13
Q

Uncertainties about peatlands

would restoring the UK’s degraded peatlands be economically viable

A
  • restoring the UK’s degraded peatlands could cost between £8bn-£22bn over the next 100 years,
  • but would save £109bn in terms of reduced carbon emissions
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14
Q

Uncertainties about peatlands

how will degrading peatlands affect farming in the long term

A
  • affects the long-term viability of agriculture in those areas:
  • peat subsidence due to drainage also increases the need for expensive pumping to maintain conditions suitable for crop growth —> increases flood risk
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15
Q

Consequences of climate change for the peatlands

Why is there a particular problem with peatland emissions in Southeast Asia

A
  • Fire is often used as a tool to clear land for cultivation, and these fires often run out of control into adjacent forests
  • These fires produce toxic smog across Indonesia, Malaysia and Singapore’, contributing to dangerous levels of particulate matter harmful to human health
  • The degradation of peatlands through drainage and burning, plus the fires themselves, produce significant COz emissions every year
  • The IPCC estimates tropical peatland cultivation generates the equivalent of 440 million tonnes of COz per year, with peat fires generating on average a further 200 million tonnes
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