Carbon - EQ3 - 6.9 - Feedback Mechanisms Flashcards
When does feedback occur
- when an output change is redirected back to an input
- a positive feedback cycle increases change while a negative one decreases change
Describe the impilcations of the feeback mechanism from carbon from peatlands & permafrost
- 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
Describe the impilcations of the feeback mechanism from Forest Dieback
- 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
Describe the impilcations of the feeback mechanism from Thermohaline Circulation Changes
- 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
What are peatlands
- Peatlands are carbon-rich wetlands which occupy 3% of the global land surface and 12% of UK land area
Consequences of climate change for the peatlands
why are peatlands important
- 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
Consequences of climate change for the peatlands
Are peatlands a carbon store or sink
- 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
Consequences of climate change for the peatlands
What is the impact of peatland degredation
- 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
Consequences of climate change for the peatlands
How many greenhouse gas emissions are UK peatlands producing
- 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.
Uncertainties about peatlands
Why is peatland exploited by humans
- 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
Uncertainties about peatlands
With climate change, how would peatlands change from extreme weather
- 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
Uncertainties about peatlands
how is semi-natural peatland peatlands expected to be change by climate change
- 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
Uncertainties about peatlands
would restoring the UK’s degraded peatlands be economically viable
- 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
Uncertainties about peatlands
how will degrading peatlands affect farming in the long term
- 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
Consequences of climate change for the peatlands
Why is there a particular problem with peatland emissions in Southeast Asia
- 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