The Carbon Cycle and Energy Security V2

How does the carbon cycle operate to maintain planetary health?
1. Most global carbon is locked in terrestrial stores as part of the long-term geological cycle
  1. The biogeochemical cycle consists of carbon stores of different sizes with annual fluxes between stores of varying size, rates and on different time scales
    Annotations:
    - Flux is the rate of exchange between individual stores Amount of carbon measured in Gigatonnes or Petagrams
    - Amounto of carbon is measured in petagrams
    1. Terrestrial
      1. Stored in rocks and plants
        Largest store, Earth's crust 100.000,000 Gt
    2. Oceans (38,000 Gt)
      1. Ocean surface
        2.5% of oceanic carbon stored
      2. Deep ocean
        97.5% of oceanic carbon stored
    3. Atmosphere
      1. 750Gt
        Volcanic activity
        Respiration
        Wildfires
        Outgassing
    4. Human influence - 180Gt added from burning fossil fuels
  2. Most of the earth' carbon is geological, resulting from the formation of sedimentary rocks (limestone) in the oceans and biologically derived carbon in shale, coal and other rocks
    1. Sedimentary rocks
      1. calcareous ooze, shells, skeletons collecting at ocean floor
      2. Corals and Phytoplankton collect on seafloor. Calcium carbonate absorbed by them is compacted forming organic limestone rock
    2. Biologically derived carbon rocks
      1. Remains of living organisms deposited in layers
  3. Chemical weathering removes carbon from silicate rocks. The carbon ends up in the ocean as carbonate rock. Carbonate is released via outgassing at ocean ridges, hotspot volcanoes and subduction zones
    1. Chemical weathering
      1. Volcanic eruptions increase CO2, increased atmospheric moisture and acid rain and increased chemical weathering
    2. Outgassing through tectonic forces with limestone being subjected to extreme heat. Chemical change releases CO2
    3. Volcanic activity at hotspots releases CO2 into atmosphere
2. A balanced carbon cycle is important in sustaining other earth systems but is increasingly altered by human activities.
  1. The concentration of atmospheric carbon (carbon dioxide and methane) strongly influences the natural greenhouse effect, which in turn determines the distribution of temperature and precipitation. (2)
  2. Ocean and terrestrial photosynthesis play an important role in regulating the composition of the atmosphere. Soil health is influenced by stored carbon, which is important for ecosystem productivity.
  3. The process of fossil fuel combustion has altered the balance of carbon pathways and stores with implications for climate, ecosystems and the hydrological cycle.
3. Biogeochemical cycle
  1. Biological processes sequester carbon on land and in the oceans on shorter timescales
    1. Phytoplankton sequester atmospheric carbon during photosynthesis; some of this carbon is returned to the atmosphere during respiration
      1. Oceanic Carbon Pumps
        Biological
        Sequestration through photosynthesis by phytoplankton
        Physical
        Circulation of water and carbon through downwelling, upwelling and thermohaline circulation
        Colder water absorbs CO2
        Warmer water releases CO2
        Carbonate pump
        Inorganic carbon sedimentation
        Calcium carbonate forms shells, shells dissolve before reaching floor and integrate into deep ocean current
    2. Terrestrial primary producers sequester carbon during photosynthesis; some of this carbon is returned to the atmosphere during respiration by consumer organisms.
    3. Biological carbon can be stored as dead organic matter in soils, or returned to the atmosphere via biological decomposition over several years.
What are the consequences for people and the environment of our increasing demand for energy?
1. Energy security is a key goal for countries, with most relying on fossil fuels.
  1. Access to and consumption of energy resources depends on physical availability, cost, technology, public perception, level of economic development and environmental priorities ( national comparisons: USA versus France).
  2. Energy players (P: role of TNCs, The Organisation of the Petroleum Exporting Countries (OPEC), consumers, governments) have different roles in securing pathways and energy supplies.
  3. Consumption (per capita and in terms of units of GDP) and energy mix (domestic and foreign, primary and secondary energy, renewable versus non-renewable).
2. Reliance on fossil fuels to drive economic development is still the global norm.
  1. There is a mismatch between locations of conventional fossil fuel supply (oil, gas, coal) and regions where demand is highest, resulting from physical geography.
  2. Energy pathways (pipelines, transmission lines, shipping routes, road and rail) are a key aspect of security but can be prone to disruption especially as conventional fossil fuel sources deplete ( Russian gas to Europe).
  3. The development of unconventional fossil fuel energy resources (tar sands, oil shale, shale gas, deep water oil) has social costs and benefits, implications for the carbon cycle, and consequences for the resilience of fragile environments. ( Canadian tar sands, USA fracking, Brazilian deep water oil) (P: role of business in developing reserves, versus environmental groups and affected communities)
3. There are alternatives to fossil fuels but each has costs and benefits.
  1. Renewable and recyclable energy (nuclear power, wind power and solar power) could help decouple fossil fuel from economic growth; these energy sources have costs and benefits economically, socially, and environmentally and in terms of their contribution they can make to energy security. ( changing UK energy mix)
  2. Biofuels are an alternative energy source that are increasing globally; growth in biofuels however has implications for food supply as well as uncertainty over how ‘carbon neutral’ they are. ( Biofuels in Brazil) (5)
  3. Radical technologies, including carbon capture and storage and alternative energy sources (hydrogen fuel cells, electric vehicles) could reduce carbon emissions but uncertainty exists as to how far this is possible.
How are the carbon and water cycles linked to the global climate system?
1. Biological carbon cycles and the water cycle are threatened by human activity.
  1. Growing demand for food, fuel and other resources globally has led to contrasting regional trends in land-use cover (deforestation, afforestation, conversion of grasslands to farming) affecting terrestrial carbon stores with wider implications for the water cycle and soil health. (6)
  2. Ocean acidification, as a result of its role as a carbon sink, is increasing due to fossil fuel combustion and risks crossing the critical threshold for the health of coral reefs and other marine ecosystems that provide vital ecosystem services.
  3. Climate change, resulting from the enhanced greenhouse effect, may increase the frequency of drought due to shifting climate belts, which may impact on the health of forests as carbon stores. ( Amazonian drought events)
2. There are implications for human wellbeing from the degradation of the water and carbon cycles.
  1. Forest loss has implications for human wellbeing but there is evidence that forest stores are being protected and even expanded, especially in countries at higher levels of development (environmental Kuznets’ curve model). (A: attitudes of global consumers to environmental issues)
  2. Increased temperatures affect evaporation rates and the quantity of water vapour in the atmosphere with implications for precipitation patterns, river regimes and water stores (cryosphere and drainage basin stores) ( Arctic) (F: uncertainty of global projections).
  3. Threats to ocean health pose threats to human wellbeing, especially in developing regions that depend on marine resources as a food source and for tourism and coastal protection.
3. Further planetary warming risks large-scale release of stored carbon, requiring responses from different players at different scales.
  1. Future emissions, atmospheric concentration levels and climate warming are uncertain owing to natural factors (the role of carbon sinks), human factors (economic growth, population, energy sources) and feedback mechanisms (carbon release from peatlands and permafrost, and tipping points, including forest die back and alterations to the thermohaline circulation). (8) (F: uncertainty of global projections)
  2. Adaptation strategies for a changed climate (water conservation and management, resilient agricultural systems, land-use planning, flood-risk management, solar radiation management) have different costs and risks.
  3. Re-balancing the carbon cycle could be achieved through mitigation (carbon taxation, renewable switching, energy efficiency, afforestation, carbon capture and storage) but this requires global scale agreement and national actions both of which have proved to be problematic. (A: attitudes of different countries, TNCs and people)

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The Carbon Cycle and Energy Security V2

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	Created by Simon Risdon over 1 year ago